format version:	1.1
date:	15/12/2005

Standard Chronostratigraphy	:	Eon	Era	Sub-Era	Period	Sub-Period	Epoch	Stage	Substage		International Commission on Stratigraphy (2006).  Click  <a href="http://www.stratigraphy.org/gssp.htm">GSSP</a>  for official boundary (GSSP) definitions, status and nomenclature.

Eon	block	50	USGS-Named		off
	TOP	0
	Phanerozoic	542
	Proterozoic	2500
	Archean	4500

Era	block	50	USGS-Named		off
	TOP	0
	Cenozoic	65.5
	Mesozoic	251.0
	Paleozoic	542.0
	Neoproterozoic	1000
	Mesoproterozoic	1600
	Paleoproterozoic	2500
	Neoarchean	2800
	Mesoarchean	3200
	Paleoarchean	3600
	Eoarchean / Hadean	4500

Sub-Era	block	90	USGS-Named	
	TOP	0
	Quaternary	2.588		The Quaternary, even though it has not been formally ratified by IUGS, is considered by ICS to be a formal sub-era, which spans the past 2.6 myr according to the International Quaternary Association (INQUA).
	Tertiary	65.5	Tertiary is an informal sub-era.

Period	block	90	USGS-Named
	TOP	0
	Neogene	23.03
	Paleogene	65.5
	Cretaceous	145.46
	Jurassic	199.6
	Triassic	251.0
	Permian	299.0
	Carboniferous	359.2
	Devonian	416.0
	Silurian	443.7
	Ordovician	488.3
	Cambrian	542.0
	Ediacaran	650
	Cryogenian	850
	Tonian	1000
	Stenian	1200
	Ectasian	1400
	Calymmian	1600
	Statherian	1800
	Orosirian	2050
	Rhyacian	2300
	Siderian	2500
	 	2800
	 	3200
	 	3600
	 	4500

Sub-Period	block	50	USGS-Named		off
	TOP	299.0
	Pennsylvanian	318.1
	Mississippian	359.2

Epoch	block		USGS-Named
	TOP	0
	Holocene	0.0115
	Pleistocene	1.806		Late Neogene
	Pliocene	5.333		Middle Neogene
	Miocene	23.03		Early Neogene
	Oligocene	33.9		Late Paleogene
	Eocene	55.8		Middle Paleogene
	Paleocene	65.5		Early Paleogene
	Late	99.6
	Early	145.46
	Late	161.21
	Middle	175.6
	Early	199.6
	Late	228.01	dotted
	Middle	245.17
	Early	251.0
	Lopingian	260.4		Late Permian
	Guadalupian	270.6		Middle Permian
	Cisuralian	299.0		Early Permian
	Late Penn.	306.5		Late Pennsylvanian
	Middle Penn.	311.7		Middle Pennsylvanian
	Early Penn.	318.1		Early Pennsylvanian
	Late Miss.	326.4		Late Mississippian
	Middle Miss.	345.3		Middle Mississippian
	Early Miss.	359.2		Early Mississippian
	Late	385.3
	Middle	397.5
	Early	416.0		Early Devonian
	Pridoli	418.7		latest Silurian
	Ludlow	422.9		Late Silurian
	Wenlock	428.2		Middle Silurian
	Llandovery	443.7		Early Silurian
	Late	460.9
	Middle	471.8
	Early	488.3	
	Furongian	501.0		Late Cambrian
	Series 3	510.0
	Series 2	521.0	dashed
	Series 1	542.0		Early Cambrian
	 	650
	 	850
	 	1000
	 	1200
	 	1400
	 	1600
	 	1800
	 	2050
	 	2300
	 	2500
	 	2800
	 	3200
	 	3600
	 	4500

Stage	block		USGS-Named
	TOP	0.0115
	Lt. Pleist.	0.126
	M. Pleist.	0.781
	E. Pleist.	1.806
	Gelasian	2.588
	Piacenzian	3.6
	Zanclean	5.333
	Messinian	7.248
	Tortonian	11.608
	Serravillian	13.64
	Langhian	15.97
	Burdigalian	20.43
	Aquitanian	23.03
	Chattian	28.4	dashed
	Rupelian	33.9
	Priabonian	37.2
	Bartonian	40.4
	Lutetian	48.6
	Ypresian	55.8
	Thanetian	58.74	dashed
	Selandian	61.72	dashed
	Danian	65.5
	Maastrichtian	70.6
	Campanian	83.5
	Santonian	85.85	dashed
	Coniacian	89.27	dashed
	Turonian	93.55
	Cenomanian	99.6
	Albian	112.0	dashed
	Aptian	125.0		Current working definition for the base of Aptian Stage is the base of Polarity Chron M0r.
	Barremian	129.97
	Hauterivian	136.44
	Valanginian	140.18
	Berriasian	145.46
	Tithonian	150.844
	Kimmeridgian	155.646
	Oxfordian	161.21
	Callovian	164.74
	Bathonian	167.68
	Bajocian	171.60
	Aalenian	175.60
	Toarcian	183.00
	Pliensbachian	189.60
	Sinemurian	196.50
	Hettangian	199.60
	Rhaetian	203.64
	Norian	216.53
	Carnian	228.01	dotted
	Ladinian	237.0
	Anisian	245.17	dashed
	Olenekian	249.75	dashed
	Induan	251.0
	Changhsingian	253.8
	Wuchiapingian	260.4
	Capitanian	265.8
	Wordian	268.0
	Roadian	270.6
	Kungurian	275.6
	Artinskian	284.4
	Sakmarian	294.6
	Asselian	299.0
	Gzhelian	303.9
	Kasimovian	306.5
	Moscovian	311.7
	Bashkirian	318.1
	Serpukhovian	326.4
	Visean	345.3
	Tournaisian	359.2
	Famennian	374.5
	Frasnian	385.3
	Givetian	391.8
	Eifelian	397.5
	Emsian	407.0
	Pragian	411.2
	Lochkovian	416.0
	 	418.7		Pridoli epoch is not divided into stages.
	Ludfordian	421.3
	Gorstian	422.9
	Homerian	426.2
	Sheinwoodian	428.2
	Telychian	436.1
	Aeronian	439.0
	Rhuddanian	443.7
	Hirnantian	445.6
	Katian	455.8
	Sandbian	460.9
	Darriwilian	468.1
	Third	471.8
	Floian	478.6
	Tremadocian	488.3
	(10b)	489.52	dotted
	Stage 10	492.0
	Stage 9	496.00
	Paibian	501.00
	Stage 7	503.00
	Stage 6	506.50
	Stage 5	510.00
	Stage 4	517.00	dotted
	Stage 3	521.00	dashed
	Stage 2	534.60	dotted
	Stage 1	542.0
	 	650
	 	850
	 	1000
	 	1200
	 	1400
	 	1600
	 	1800
	 	2050
	 	2300
	 	2500
	 	2800
	 	3200
	 	3600
	 	4500

Substage	block		USGS		off
	TOP	65.50
	Lt. Maastr.	69.23		Not defined
	E. Maastr.	70.60
	Lt. Camp.	76.38		Not defined
	M. Camp.	80.64		Not defined
	E. Camp.	83.50
	Lt. Sant.	83.99
	M. Sant.	84.94
	E. Sant.	85.85	dashed
	Lt. Coniac.	86.96
	M. Coniac.	88.58
	E. Coniac.	89.27	dashed
	Lt. Turon.	90.48
	M. Turon.	92.13
	E. Turon.	93.55
	Lt. Cenom.	94.75
	M. Cenom.	96.01
	E. Cenom.	99.60
	Lt. Albian	106.42
	M. Albian	108.77
	E. Albian	112.00	dashed
	Lt. Apt. - Clansayesian	115.00
	M. Apt. - Gargasian	121.00
	E. Apt. - Bedoulian	125.00
	Lt. Barrem.	128.30
	E. Barrem.	129.97
	Lt. Haut.	133.85
	E. Haut.	136.44
	Lt. Val.	138.94
	E. Val.	140.18
	Lt. Berr.	142.30
	E. Berr.	145.46
	Lt. Tithon.	147.16
	E. Tithon.	150.844
	Lt. Kimm.	153.06
	E. Kimm. (Bor.)	155.646
	Lt. Oxf.	157.40
	M. Oxf.	159.61
	E. Oxf.	161.21
	Lt. Callov.	162.52
	M. Callov.	163.20
	E. Callov.	164.74
	Lt. Bath.	165.72
	M. Bath.	166.89
	E. Bath.	167.68
	Lt. Bajoc.	169.64
	E. Bajoc.	171.60
	Lt. Aalen.	172.49
	M. Aalen.	174.71
	E. Aalen.	175.60
	Lt. Toarc.	180.50
	M. Toarc.	181.20
	E. Toarc.	183.00
	Lt. Pliens. - Domerian	186.95
	E. Pliens. - Carixian	189.60
	Lt. Sinem.	193.25
	E. Sinem.	196.50
	 	199.60		No substages of Hettangian
	 	203.64		No substages of Rhaetian
	Sevatian	205.71	dotted	Late Norian
	Alaunian	211.30	dotted	Middle Norian
	Lacian	216.53	dotted	Early Norian
	Tuvalian	222.70		Late Carnian
	Julian	228.01	dotted	Early Carnian
	Longobardian	233.34	dotted	Late Ladinian
	Fassanian	237.0		Early Ladinian
	Illyrian	241.6	3	Latest Anisian
	Pelsonian	242.49	3	Late-Middle Anisian
	Bithynian	243.68	3	Early-Middle Anisian
	Aegean	245.17	3	Earliest Anisian
	Spathian	248.08	3	Late Olenekian
	Smithian	249.75	dashed	Early Olenekian
	Dienerian	250.38	3	Late Induan
	Griesbachian	251.00		Early Induan


GSSPs	event	80	USGS-Named			The base of each unit of the geologic time scale is defined at a specific location and point (Global Boundary Stratotype Section and Point, GSSP), where it coincides with an array of paleontological, geochemical, paleomagnetic or other markers for high-resolution global correlation.  The current status of currently ratified GSSPs and possible markers for the other geologic units are summarized at www.stratigraphy.org [Click  <a href="http://www.stratigraphy.org/gssp.htm">GSSP</a> ]
EVENT
	GSSP	1.806		The base of the Pleistocene Series [click  <a href="http://www.stratigraphy.org/pliple.htm">GSSP</a>  for graphics] is defined as the base of the marine claystones conformably overlying the sapropelic Marker Bed "e" in the Vrica Section, Italy.
	GSSP	2.588		The base of the Gelasian Stage and provisional base of the Quaternary Sub-Era [click  <a href="http://www.stratigraphy.org/gelasian.htm">GSSP</a>  for graphics] is defined as the base of the marly layer overlying sapropel MPRS 250, located at 62m in Monte San Nicola section, Italy. The astronomical age of sapropel MPRS 250 (mid-point), corresponding to precessional cycle 250 from the present, is 2.588 Ma, which can be assumed as the age of the boundary.
	GSSP	3.6		The base of the Piacenzian Stage [click  <a href="http://www.stratigraphy.org/piacenzian.htm">GSSP</a>  for graphics] is defined as the base of the beige marl bed of the small-scale carbonate cycle 77. It corresponds to precessional excursion 347 as numbered from the present, with an astrochronological age estimate of 3.600 Ma. The GSSP is located in the Punta Piccola section, Italy.
	GSSP	5.333		The base of the Pliocene Series and the Zanclean Stage [click  <a href="http://www.stratigraphy.org/miopli.htm">GSSP</a>  for graphics] is defined as the base of the Trubi Formation. The age of the Zanclean and Pliocene GSSP at the base of the stage is 5.33 Ma in the orbitally calibrated time scale, and lies within the lowermost reversed episode of the Gilbert Chron (C3n.4r), below the Thvera normal subchron.
	GSSP	7.248		The base of the Messinian stage [click  <a href="http://www.stratigraphy.org/messi.htm">GSSP</a>  for graphics] is defined at the base of the reddish layer of sedimentary cycle no. 15 at Oued Akrech, Morocco, NW Africa. This point coincides closely with the first regular occurrence of the planktonic foraminifer Globorotalia miotumida and the first occurrence of the calcareous nannofossil Amaurolithus delicatus, and falls within the interval of reversed polarity that corresponds to C3Br.1r. The base of the reddish layer and, thus, the Messinian GSSP has been assigned an astronomical age of 7.251Ma.
	GSSP	11.608		The base of the Tortonian Stage [click  <a href="http://www.stratigraphy.org/tortonian.htm">GSSP</a>  for graphics] is defined as the mid-point of the sapropel layer of basic cycle number 76 in the Monte dei Corvi Beach section, located on the Adriatic coast of central Italy, 5km SE of Ancona. This level has been assigned an astronomical age of 11.608 Ma. It coincides almost exactly with the Last Common Occurrences of the calcareous nannofossil Discoaster kugleri and the planktonic foraminifer Globigerinoides subquadratus, and is associated with the short normal-polarity subchron C5r.2n. This level coincides closely with oxygen isotope event Mi-5 and the associated glacio-eustatic sea-level low-stand of supercycle T3.1 and concurrent deep-sea hiatus NH4.
	GSSP	23.03		The base of the Neogene System, Miocene Series and Aquitanian Stage [click  <a href="http://www.stratigraphy.org/palneo.htm">GSSP</a>  for graphics] is defined in the Lemme-Carrosio Section (35m from the top of the section) in the village of Carrosio, south of the town of Gavi and north of Voltaggio (Allessandria Province), Italy.
	GSSP	33.9		The base of the Oligocene Series and Rupelian Stage [click  <a href="http://www.stratigraphy.org/eocoli.htm">GSSP</a>  for graphics] is defined in the Massignano section about 10km southeast of Ancona, Italy. The GSSP is at the base of a 0.5m thick greenish-grey marl bed. At this level, both the planktonic foraminifera Hantkenina and Cribrohantkenina, Eocene genera of the Hantkeninidae, become extinct.
	GSSP	55.8		The base of the Eocene Series and Ypresian Stage [click  <a href="http://www.stratigraphy.org/ypresian.htm">GSSP</a>  for graphics] is defined in the DBH subsection of the Dababiya Section, near Luxor, Egypt, at the base of a lithostratigraphic unit where the base of the so-called Carbon Isotope Excursion (CIE) is recorded.
	GSSP	65.5		The base of the Cenozoic Era, Paleogene System, Paleocene Series and Danian Stage [click  <a href="http://www.stratigraphy.org/danian.htm">GSSP</a>  for graphics] is defined at the reddish layer at the base of the 50cm thick, dark boundary clay in a tributary of the Oued Djerfane, west of El Kef, Tunisia, where it coincides with the Iridum Anomaly fallout from a major asteroid impact.
	GSSP	70.6		The base of the Maastrichtian Stage [click  <a href="http://www.stratigraphy.org/maastrichtian.htm">GSSP</a>  for graphics] is defined at level 115.2 on platform IV of the geological site at Tercis les Bains (Landes, France).
	GSSP	93.55		The base of the Turonian Stage [click  <a href="http://www.stratigraphy.org/turonian.htm">GSSP</a>  for graphics] is defined as the base of Bed 86 of the Bridge Creek Limestone Member at the western end of the Denver and Rio Grande Western Railroad cut near the north boundary of the Pueblo Reservoir State Recreation Area, west of Pueblo, Colorado, USA. The GSSP coincides with the first occurrence of the ammonite Watinoceras devonense, is in the middle of a global positive excursion in carbon 13 isotopes, and is bracketed by widespread bentonites that have yielded age of 93 to 93.5 Ma.
	GSSP	99.6		The base of the Upper Cretaceous Series and Cenomanian Stage [click  <a href="http://www.stratigraphy.org/cenom.htm">GSSP</a>  for graphics] is defined at 36 meters below the top of the Marnes Bleues Formation on the south side of Mont Risou, east of Rosans, Haute-Alpes, France. This level coincides with the first appearance of the planktonic foraminifer Rotalipora globotruncanoides Sigal, 1948, and can be placed in the context of a series of secondary marker levels based on nannofossils, planktonic foraminifera, ammonites and an ornate Carbon-13 curve.
	GSSP	171.60		The base of the Bajocian Stage [click  <a href="http://www.stratigraphy.org/bajocian.htm">GSSP</a>  for graphics] is defined at the base of Bed AB11 of the Murtinheira Section at Cabo Mondego, Portugal. The boundary coincides with the first occurrrence of the ammonite assemblage characterized by Hyperlioceras mundum, Hyperlioceras furcatum, Braunsina aspera, and Braunsina elegantula. The GSSP lies just below the nanno-horizon of the entry of Watznaueria communis and Watznaueria fossacincta, and closely corresponds with an inversion to normal polarity correlated with the Jurassic magnetic polarity time scale.
	GSSP	175.60		The base of the Middle Jurassic Series and Aalenian Stage [click  <a href="http://www.stratigraphy.org/aalenian.htm">GSSP</a>  for graphics] is defined at the base of Bed FZ107 in Fuentelsaz Section, Castilian Branch of the Iberian Range, Spain. The boundary coincides with the first occurrence of the ammonite assemblage characterized by Leioceras opalinum and Leioceras lineatum and corresponds with a normal polarity interval.
	GSSP	189.60		The base of the Pliensbachian Stage is Base of Bed 73b, Wine Haven section, Robin Hood's Bay, Yorkshire, England, UK.  It coincides with the lowest occurrences of Bifericeras donovani and of genera Apoderoceras (base of Phricodoceras taylori subzone of Uptonia jamesoni ammonite zone).
	GSSP	196.50		The base of the Sinemurian Stage [click  <a href="http://www.stratigraphy.org/sinemurian.htm">GSSP</a>  for graphics] is exposed in the cliff north of the village of East Quantoxhead, around 6 km east of Watchet, in the administrative district of West Somerset, southwestern England. The boundary level is 0.90 m above the base of Bed 145 coinciding with the first appearance of the genera Vermiceras (V. quantoxense, V. palmeri) and Metophioceras (M. sp. indet. 1). The basal ammonite assemblage of the Sinemurian in the GSSP is earlier than all other assemblages known elsewhere in Europe. In Europe, a stratigraphical gap between both stages is generally present. Correlation with other faunal provinces is possible using the first appearance of Metophioceras s. str.
	GSSP	237.0		The Base of the Middle Triassic Series and Ladinian Stage [click  <a href="http://www.stratigraphy.org/ladinian.htm">GSSP</a>  for graphics] is defined at the base of a 15 - 20cm thick limestone bed overlying a distinctive groove ("Chiesense groove") of limestone nodules in a shaly matrix, located about 5m above the base of the Buchenstein Beds in the Caffaro River bed (4549'09.5"N, 1028'15.5"E), south of the village of Bagolino (Province of Brescia, Northern Italy). The lower surface of the thick limestone bed has the lowest occurrence of the ammonoid Eoprotrachyceras curionii. Secondary global markers in the uppermost Anisian include the lowest occurrence of conodont Neogondolella praehungarica and a brief normal-polarity magnetic zone recognized in closely correlated sections. The GSSP level is bracketed by U-Pb single zircon age data from volcaniclastic horizons, indicating a boundary age of ca. 241 Ma.
	GSSP	251.0		The base of the Mesozoic Era, Triassic System and Induan Stage [click  <a href="http://www.stratigraphy.org/pertri.htm">GSSP</a>  for graphics] is defined at the first occurrence of the conodont species Hindeodus parvus in the evolutionary lineage Hindeodus latidentatus - Hindeodus parvus - Isarcicella isarcica at the base of Bed 27c in the Meishan Section, Changxing County, Zhejiang Province, China.
	GSSP	253.8		The base of the Changhsingian Stage [click  <a href="http://www.stratigraphy.org/changhsingian.htm">GSSP</a>  for graphics] is the base of Bed 4a-2, 88 cm above base of Changxing Limestone, Meishan D section (Zhejiang province, E. China), where it coincides with the lowest occurrence of conodont Clarkina wangi.
	GSSP	260.4		The base of the Lopingian Series (Upper Permian) and Wuchiapingian Stage [click  <a href="http://www.stratigraphy.org/wuchiapingian.htm">GSSP</a>  for graphics] is the base of Bed 6K/115 in Penglaitan section, S. bank of Hongshui River, 20 km ESE of Laibin country town (Guangxi province, S. China), where it coincides with the lowest occurrence of conodont Clarkina postbitteri postbitteri.  Nearby Tieqiao (Rail-bridge) section is a supplementary reference section. 
	GSSP	265.8		The base of the Capitanian Stage [click  <a href="http://www.stratigraphy.org/capitanian.htm">GSSP</a>  for graphics] is 4.5 m above base of Pinery Limestone Member, Nipple Hill, SE Guadalupe Mountains, Texas, USA, where it coincides with the lowest occurrence of conodont Jinogondolella postserrata.
	GSSP	268.0		The base of the Wordian Stage [click  <a href="http://www.stratigraphy.org/wordian.htm">GSSP</a>  for graphics] is 47.6 m above base of Getaway Ledge outcrop, Guadalupe Pass, SE Guadalupe Mountains, Texas, USA, where it coincides with the lowest occurrence of conodont Jinogondolella aserrata.
	GSSP	270.6		The base of the Guadalupian Series (Middle Permian) and Roadian Stage [click  <a href="http://www.stratigraphy.org/roadian.htm">GSSP</a>  for graphics] is 42.7 m above base of Cutoff Formation, Stratotype Canyon, southern Guadalupe Mountains, Texas, USA, where it coincides with the lowest occurrence of conodont Jinogondolella nanginkensis.
	GSSP	299.0		The base of the Permian System, Cisuralian Series and Asselian Stage [click  <a href="http://www.stratigraphy.org/carper.htm">GSSP</a>  for graphics] is defined as 27 m above the base of Bed 19, Aidaralash Creek, northern Kazakhstan, where it coincides with the lowest occurrence of "isolated-nodular" morphotype of the Streptognathodus "wabaunsensis" conodont chronocline.
	GSSP	318.1		The base of the Pennsylvanian Sub-System (Upper Carboniferous) and Bashkirian Stage [click  <a href="http://www.stratigraphy.org/midcarbon.htm">GSSP</a>  for graphics] is located at Arrow Canyon near Las Vegas, Nevada, in the arid Basin and Range Province of the southwestern USA. The GSSP is located at 82.9m above the top of the Battleship Formation in the lower Bird Spring Formation at the evolutionary first appearance of the conodont Declinognathodus noduliferus s.l. The GSSP coincides exactly with the historically stable Mississippian-Pennsylvanian boundary.
	GSSP	359.2		The base of the Carboniferous System, Mississippian Sub-System and Tournaisian Stage [click  <a href="http://www.stratigraphy.org/devcar.htm">GSSP</a>  for graphics] is at the base of Bed 89 in Trench E' at La Serre, France., where it coincides with the lowest occurrence of the conodont Siphonodella sulcata within the evolutionary lineage from Siphonodella praesulcata to Siphonodella sulcata.
	GSSP	374.5		The base of the Famennian Stage [click  <a href="http://www.stratigraphy.org/famen.htm">GSSP</a>  for graphics] is in a section near the Upper Coumiac Quarry, near Cessenon in southeastern Montagne Noire, France, where it coincides with the the lower boundary of the lower Palmatolepis triangularis Conodont Zone.  This is just above a major extinction horizon (Upper Kellwasser Event), and coincides with the boundary between the Crickites holzapfeli Zone and the Phoenixites frechi Zone in the goniatite scale.
	GSSP	385.3		The base of the Upper Devonian Series and Frasnian Stage [click  <a href="http://www.stratigraphy.org/frasn.htm">GSSP</a>  for graphics] is defined at the base of Bed 42' at Col du Puech de la Suque section E in southeastern Montagne Noire, France. The GSSP also coincides with the lower boundary of the Lower asymmetricus Zone which is defined by the first occurrence of the conodont Ancyrodella rotundiloba.
	GSSP	391.8		The base of the Givetian Stage [click  <a href="http://www.stratigraphy.org/givetian.htm">GSSP</a>  for graphics] is placed in a section at Jebel Mech Irdane in the Tafilalt of Morocco. The Eifelian-Givetian boundary coincides with the level at which conodont Polygnathus pseudofoliatus changes to Polygnathus hemiansatus. The boundary corresponds closely with the base of the goniatite Maenioceras Stufe used as a Middle Devonian division, and the entry of the dacryoconarid Nowakia otomari.
	GSSP	397.5		The base of the Middle Devonian Series and Eifelian Stage [click  <a href="http://www.stratigraphy.org/eifel.htm">GSSP</a>  for graphics] is exposed in the Wetteldorf Richtschnitt, near the town of Schoenecken-Wetteldorf, Eifel Hills, Germany. The Emsian-Eifelian boundary coincides with the first occurrence of the conodont Polygnathus costatus partitus.
	GSSP	407.0		The base of the Emsian Stage [click  <a href="http://www.stratigraphy.org/emsian.htm">GSSP</a>  for graphics] is located at the base of Bed 9/5 in the Zinzil'ban Gorge in the Kitab State Geological Reserve, 170km SSE of Samarkand, Uzbekistan. The GSSP for the Emsian Stage coincides with the first occurrence of the conodont Polygnathus kitabicus within the phylogenetic succession from Polygnathus pireneae to Polygnathus kitabicus.
	GSSP	411.2		The base of the Pragian Stage [click  <a href="http://www.stratigraphy.org/emsian.htm">GSSP</a>  for graphics] is the base of Bed 12 in Velka Chuchle Quarry, in the southwestpart of Prague, Czech Republic, where it coincides with the lowest occurrence of the zone conodont Eognathodus sulcatus sulcatus.
	GSSP	416.0		The base of the Devonian System and Lochkovian Stage [click  <a href="http://www.stratigraphy.org/sildev.htm">GSSP</a>  for graphics] is in Bed 20 of the Klonk Section, Czech Republic, immediately below the lowest occurrence of the graptolite species Monograptus uniformis.
	GSSP	418.7		The base of the Pridoli Series [click  <a href="http://www.stratigraphy.org/pridoli.htm">GSSP</a>  for graphics] is within Bed 96 in the Pozary Section of the Daleje Valley, Prague, Czech Republic, where it coincides with the lowest occurrence of the graptolite species Monograptus parultimus.
	GSSP	421.3		The base of the Ludfordian Stage [click  <a href="http://www.stratigraphy.org/ludfor.htm">GSSP</a>  for graphics] is defined at Pitch Coppice Quarry near Ludlow, UK, at the rapid transition from the hard nodular limestones of the Much Wenlock Limestone Formation (Homerian) into the softer, predominantly argillaceous siltstones of the Lower Elton Formation (Gorstian)..  The biostratigraphy is imprecise, but this GSSP may be near base of the Saetograptus leintwardinensis graptolite zone.
	GSSP	422.9		The base of the Ludlow Series and Gorstian Stage [click  <a href="http://www.stratigraphy.org/gorstian.htm">GSSP</a>  for graphics] is a thin shale seam, coincident with the base of the Leintwardine Formation, at Sunnyhill Quarry, near Ludlow, Shropshire, UK.  The biostratigraphy is imprecise, but this GSSP is just below base of a local acritarch Leptobrachion longhopense range zone and perhaps near the base of the Neodiversograptus nilssoni graptolite zone.
	GSSP	426.2		The base of the Homerian Stage [click  <a href="http://www.stratigraphy.org/homer.htm">GSSP</a>  for graphics] is located along the northern bank of a small stream that feeds the tributary to Sheinton Brook in Whitwell Coppice, 500m north of the hamlet of Homer, UK, and coincides with with the base of the Cyrtograptus lundgreni Graptolite Biozone.
	GSSP	428.2		The base of the Wenlock Series and Sheinwoodian Stage [click  <a href="http://www.stratigraphy.org/shein.htm">GSSP</a>  for graphics] at the base of the Buildwas Formation along the northern bank of Hughley Brook, 200m south-east of Leasows Farm, Shropshire, southwest England, UK.  The biostratigraphy is imprecise, but the GSSP is between the base of acritarch biozone 5 and extinction of conodont Pterospathodus amorphognathoides. However, the current GSSP does not coincide with the base of the Cyrtograptus centrifugus Biozone, as was supposed when the GSSP was defined.  Restudy has recommended a slightly higher and correlatable level on condonts -- the Ireviken datum 2, which coincides approximately with the base of the murchisoni graptolite biozone.
	GSSP	436.1		The base of the Telychian Stage [click  <a href="http://www.stratigraphy.org/telych.htm">GSSP</a>  for graphics] is defined in an abandoned quarry forming part of the Cefn-cerig Road section, Wales, UK, and is just above the highest record of the brachiopod Eocoelia intermedia and below the earliest record of the succeeding species Eocoelia curtisi..
	GSSP	439.0		The base of the Aeronian Stage [click  <a href="http://www.stratigraphy.org/aeron.htm">GSSP</a>  for graphics] is is in the Trefawr Track section, 500m north of Cwm-coed-Aeron Farm, Wales, UK, where it coincides with the base of the Monograptus triangulatus Biozone.
	GSSP	443.7		The base of the Silurian System and Rhuddanian Stage [click  <a href="http://www.stratigraphy.org/ordsil.htm">GSSP</a>  for graphics] is at 1.6m above the base of the Birkhill Shale Formation, in a section at Dob's Linn, near Moffat in the Southern Uplands of Scotland, U.K, at the incoming of graptolites Parakidograptus acuminatus and Akidograptus ascensus.
	GSSP	445.6		The base of the Hirnantian Stage [click  <a href="http://www.stratigraphy.org/hirnantian.htm">GSSP</a>  for graphics] is the beginning of pronounced sea-level fall associated with onset of a major glaciation   The GSSP is 0.39 m below base of Kuanyinchiao Bed, Wangjiawan North section, 42 km N. of Yichang city (west Hubei province, China), where it coincides with the lowest occurrence of graptolite Normalograptus extraordinarius and the base of a major positive carbon-13 isotope excursion.
	GSSP	455.8		The base of the Katian Stage [click  <a href="http://www.stratigraphy.org/katian.htm">GSSP</a>  for graphics] is 4 m above base of Bigfort Chert, Black Knob Ridge section, 5 km NE of Atoka town (S. Oklahoma, USA).  It coincides with the lowest occurrence of graptolite Diplacanthograptus caudatus, and is just below base of Guttenberg carbon-13 isotope excursion.
	GSSP	460.9		The base of the Upper Ordovician Series and Sandbian Stage [click  <a href="http://www.stratigraphy.org/sandbian.htm">GSSP</a>  for graphics] is 1.4m below a phosphorite marker bed in the E14b outcrop along the south bank of the Sularp Brook at Fagelsang, 8km east of the center of the city of Lund, Scane, southern Sweden. This level coincides with the first appearance datum of the graptolite Nemagraptus gracilis.
	GSSP	468.1		The base of the Darriwilian Stage [click  <a href="http://www.stratigraphy.org/darriw.htm">GSSP</a>  for graphics] is in a section through the Ningkuo Shale exposed at Huangnitang, Changshan County, Zhejiang Province, southeast China, where it coincides with the lowest occurrence of the graptolite Undulograptus austrodentatus.
	GSSP	478.6		The base of the Floian Stage [click  <a href="http://www.stratigraphy.org/floian.htm">GSSP</a>  for graphics] in the Diabasbrottet Section at Hunneberg Mountain in southwestern Sweden. The GSSP is in the lower Toyen Shale 2.1m above the top of the Cambrian and is marked by the first appearance of the graptolite Tetragraptus approximatus.
	GSSP	488.3		The base of the Ordovician System and Tremadocian Stage [click  <a href="http://www.stratigraphy.org/camord.htm">GSSP</a>  for graphics] is exposed in the coastal platform at Green Point, western Newfoundland, at 101.8m level, within Bed 23, in the measured section (Lower Broom Point Member, Green Point Formation), coinciding with the first appearance of the conodont Iapetognathus fluctivagus, and 4.8m below the earliest planktic graptolites.
	GSSP	501.00		The base of the Furongian Series (latest Cambrian series) and Paibian Stage [click  <a href="http://www.stratigraphy.org/paibian.htm">GSSP</a>  for graphics] is defined at 396 m, at the lowest occurrence of the agnostoid trilobite Glyptagnostus reticulatus, in the Huaqiao Formation, Paibi section, NW Hunan Province, South China. This level is near the base of a large positive carbon-isotope excursion (SPICE excursion).
	GSSP	542.0		The base of the Phanerozoic Eon, Paleozoic Era and Cambrian System [click  <a href="http://www.stratigraphy.org/procam.htm">GSSP</a>  for graphics] is defined in a coastal section near the town of Fortune in southeastern Newfoundland, Canada. The level is marked by the first occurrence of Phycodes pedum (a trace fossil). The GSSP lies 2.4m above the base of Member 2 in the Chapel Island Formation, just above the transition to storm-influenced facies.
	GSSP	650		The base of the Ediacaran System of upper Neoproterozoic [click  <a href="http://www.stratigraphy.org/ediacaran.htm">GSSP</a>  for graphics] is defined as the base of the Marinoan cap carbonate (Nuccaleena Formation) in the Enorama Creek Section of the central Flinders Ranges, Adelaide Rift Complex, South Australia. The principal observed correlation events are (1) the rapid decay of Marinoan ice sheets and onset of distinct cap carbonates throughout the world, and (2) the beginning of a distinctive pattern of secular changes in carbon isotopes.
LAD
	*__*	0.0115	dashed	Potential Holocene GSSP may coincide with the end of the Younger Dryas cold spell, which is reflected in a shift in deuterium excess values, followed closely by changes in d18O, dust concentration, a range of chemical species, and by a change in annual layer thickness. 
	*__*	0.126	dashed	Potential Upper Pleistocene subseries GSSP may coincide with the base of the Eemian interglacial stage (= base of marine isotope stage 5e) before final glacial episode of Pleistocene.
	*__*	0.781	dashed	Potential Middle Pleistocene subseries GSSP may coincide with the Brunhes-Matuyama magnetic reversal.
	*__*	13.64	dashed	Potential Serravillian GSSP may coincide with lowest occurrence of nannofossil Sphenolithus heteromorphus, within magnetic polarity chronozone C5ABr, and Mi3b isotopic event (global cooling episode).
	*__*	15.97	dashed	Potential Langhian GSSP may coincide with first occurrence of planktonic foraminifer Praeorbulina glomerosa and top of magnetic polarity chronozone C5Cn.1n 
	*__*	20.43	dashed	Potential Burdigalian GSSP may coincide with lowest occurrence of planktonic foraminifer Globigerinoides altiaperturus or near top of magnetic polarity chronozone C6An.
	*__*	28.4	dashed	Potential Chattian GSSP may coincide with extinction of planktonic foraminifer  Chiloguembelina (base Foram Zone P21b); or an isotopic/climatic event.
	*__*	37.2	dashed	Potential Priabonian GSSP may coincide with lowest occurrence of calcareous nannofossil Chiasmolithus oamaruensis (base Zone NP18).
	*__*	40.4	dashed	Potential Bartonian GSSP may coincide with extinction of calcareous nannofossil Reticulofenestra reticulata.
	*__*	48.6	dashed	Potential Lutetian GSSP may coincide with lowest occurrence of planktonic foraminifer genus Hantkenina.
	*__*	58.74	dashed	Potential Thanetian GSSP may coincide with base of magnetic polarity Chron C26n.
	*__*	61.72	dashed	Potential Selandian GSSP possibilities include top or bottom of Foram Zone P3a, or C-13 excursion near base of calcareous nannofossil Zone NP5 (which would be ~1 myr younger than age estimate shown here).
	*__*	83.5	dashed	Potential Campanian GSSP may coincide with extinction of pelagic crinoid Marsupites testudinarius.
	*__*	85.85	dashed	Potential Santonian GSSP may coincide with lowest occurrence of Inoceramid bivalve Cladoceramus undulatoplicatus 
	*__*	89.27	dashed	Potential Coniacian GSSP may coincide with lowest occurrence of Inoceramid bivalve Cremnoceramus rotundatus (sensu Troger non Fiege).
	*__*	112.0	dashed	Potential Albian GSSP candidates include: (1) calcareous nannofossil, lowest occurrence of Praediscosphaera columnata (= P. cretacea of some earlier studies) [USED IN GTS2004], (2) carbon-isotope excursion (black-shale episode), (3) an ammonite. 
	*__*	125.0	dashed	Potential Aptian GSSP may coincide with base of magnetic polarity Chron M0r.
	*__*	129.97	dashed	Potential Barremian GSSP may coincide with lowest occurrence of ammonite Spitidiscus [now Taveraidiscus] hugii - Spitidiscus vandeckii group.
	*__*	136.44	dashed	Potential Hauterivian GSSP may coincide with lowest occurrence of ammonite genus Acanthodiscus (especially A. radiatus).
	*__*	140.18	dashed	Potential Valanginian GSSP may coincide with lowest occurrence of calpionellid Calpionellites darderi (base of Calpionellid Zone E); followed by the lowest occurrence of ammonite "Thurmanniceras" pertransiens.
	*__*	145.46	dashed	Potential Cretaceous System GSSP and base of Berriasian Stage may coincide with lowest occurrence of ammonite Berriasella jacobi.
	*__*	150.844	dashed	Potential Tithonian GSSP may coincide with base of Hybonoticeras hybonotum ammonite zone and lowest occurrence of Gravesia genus, and the base of magnetic polarity chronozone M22An.
	*__*	155.646	dashed	Potential Kimmeridgian GSSP may coincide with base of Pictonia baylei ammonite zone of Boreal realm.
	*__*	161.21	dashed	Potential Oxfordian GSSP may coincide with ammonite Brightia thuouxensis Horizon at base of the Cardioceras scarburgense Subzone (defines base of Quenstedtoceras mariae Zone).
	*__*	164.74	dashed	Potential Callovian GSSP may coincide with lowest occurrence of ammonite genus Kepplerites (Kosmoceratidae) (defines base of Macrocephalites herveyi Zone in sub-Boreal province of Great Britain to southwest Germany).
	*__*	167.68	dashed	Potential Bathonian GSSP may coincide with lowest occurrence of ammonite Parkinsonia (G.) convergens (defines base of Zigzagiceras zigzag Zone).
	*__*	183.00	dashed	Potential Toarcian GSSP may coincide with lowest occurrence of a diversified Eodactylites ammonite fauna; correlates with the NW European Paltus horizon.
	*__*	199.60	dashed	Potential Jurassic System and base of Hettangian Stage may coincide with lowest occurrence of smooth Psiloceras planorbis ammonite group.
	*__*	203.64	dashed	Potential Rhaetian GSSP may coincide with lowest occurrence of ammonite Cochlocera, conodonts Misikella spp. and Epigondolella mosheri, and radiolarian Proparvicingula moniliformis.
	*__*	216.53	dashed	Potential Norian GSSP may coincide with base of Klamathites macrolobatus or Stikinoceras kerri ammonoid zones and the Metapolygnathus communisti or M. primitius conodont zones.
	*__*	228.01	dotted	Potential Carnian GSSP may coincide with lowest occurrence of the ammonoids Daxatina or Trachyceras, and of the conodont Metapolygnathus polygnathiformis.
	*__*	245.17	dashed	Potential Anisian GSSP may coincide with lowest occurrences of conodont Chiosella timorensis.
	*__*	249.75	dashed	Potential Olenekian GSSP may coincide with lowest occurrence of Neospathodus waageni; near lowest occurrence of Flemingites and Euflemingites ammonite genera.
	*__*	275.6	dashed	Potential Kungurian GSSP may coincide with lowest occurrence of conodont Neostreptognathus pnevi-N. exculptus.
	*__*	284.4	dashed	Potential Artinskian GSSP may coincide with lowest occurrence of conodont Sweetognathus whitei.
	*__*	294.6	dashed	Potential Sakmarian GSSP may coincide with lowest occurrence of conodont Sweetognathus merrelli.
	*__*	303.9	dashed	Potential Gzhelian GSSP may coincide with lowest occurrences of the fusulinids Daixina, Jigulites and Rugosofusulina, or lowest occurrence of conodont Idiognathodus simulator (s.str.).  Close to lowest occurrence of ammonoid Shumardites. 
	*__*	306.5	dashed	Potential Kasimovian GSSP may coincide with base of Obsoletes obsoletes and Protriticites pseudomontiparus fusulinid zone, or lowest occurrence of conodont Streptognathodus subexcelsus or of ammonoid Parashumardites.
	*__*	311.7	dashed	Potential Moscovian GSSP may coincide with lowest occurrences of conodonts Declinognathodus donetzianus and/or Idiognathoides postsulcatus, and of fusulinid Aljutovella aljutovica.
	*__*	326.4	dashed	Potential Serpukhovian GSSP may coincide with lowest occurrence of conodont Lochriea crusiformis or of L. ziegleri.
	*__*	345.3	dashed	Potential Visean GSSP may coincide with transition in foraminifer lineage Eoparastaffella simplex morphotype 1/morphotype 2.
	*__*	471.8	dashed	Potential THIRD Ordovician Stage (yet to be named) GSSP may coincide with lowest occurrence of conodont Protoprioniodus aranda or of Baltoniodus triangularis.
	*__*	489.52	dotted	Potential substage of TENTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of Codylodus adesei conodont.
	*__*	492.0	dashed	Potential TENTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Lotagnostus americanus.
	*__*	496.00	dashed	Potential NINTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Agnostotes orientalis.
	*__*	503.00	dashed	Potential SEVENTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Lejopyge laevigata.
	*__*	506.50	dashed	Potential SIXTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Ptychagnostus atavus.
	*__*	510.00	dashed	Potential FIFTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Oryctocephalus indicus.
	*__*	517.00	dotted	Potential FOURTH Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of trilobite Olenellus or Redlichia.
	*__*	521.00	dashed	Potential THIRD Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of Trilobites.
	*__*	534.60	dotted	Potential SECOND Cambrian Stage (yet to be named) GSSP may coincide with lowest occurrence of Small Shelly Fossils, or Archaeocyathid species.


Geomagnetic Polarity	chron					GTS2004 composites [Cenozoic-Late Jurassic from chapter on geomagnetic polarity time scale;  Late Triassic provided by Dennis Kent in June 2005 (after Kent and Olsen, 1999); and other periods after compilations in associated GTS2004 chapter].
C-Sequence	Primary
	TOP		0.000
	N	C1	0.781	C1n (Brunhes)
	R	C1	0.988	C1r.1r (Matuyama)
	N	C1	1.072	C1r.1n (Jaramillo)
	R	C1	1.173	C1r.2r
	N	C1	1.185	C1r.2n (Cobb Mountain)
	R	C1	1.778	C1r.3r
	N	C2	1.945	C2n (Olduvai)
	R	C2	2.128	C2r.1r
	N	C2	2.148	C2r.1n (Reunion)
	R	C2	2.581	C2r.2r (Matuyama continued)
	N	C2A	3.032	C2An.1n (Gauss)
	R	C2A	3.116	C2An.1r (Keana)
	N	C2A	3.207	C2An.2n
	R	C2A	3.330	C2An.2r (Mammoth)
	N	C2A	3.596	C2An.3n (Gauss continued)
	R	C2A	4.187	C2Ar (Gilbert)
	N	C3	4.300	C3n.1n (Cochiti)
	R	C3	4.493	C3n.1r
	N	C3	4.631	C3n.2n (Nunivak)
	R	C3	4.799	C3n.2r
	N	C3	4.896	C3n.3n (Sidufjall)
	R	C3	4.997	C3n.3r
	N	C3	5.235	C3n.4n (Thvera)
	R	C3	6.033	C3r (Gilbert lower part)
	N	C3A	6.252	C3An.1n
	R	C3A	6.436	C3An.1r
	N	C3A	6.733	C3An.2n
	R	C3A	7.140	C3Ar
	N	C3B	7.212	C3Bn
	R	C3B	7.251	C3Br.1r
	N	C3B	7.285	C3Br.1n
	R	C3B	7.454	C3Br.2r
	N	C3B	7.489	C3Br.2n
	R	C3B	7.528	C3Br.3r
	N	C4	7.642	C4n.1n
	R	C4	7.695	C4n.1r
	N	C4	8.108	C4n.2n
	R	C4	8.254	C4r.1r
	N	C4	8.300	C4r.1n
	R	C4	8.769	C4r.2r
	N	C4A	9.098	C4An
	R	C4A	9.312	C4Ar.1r
	N	C4A	9.409	C4Ar.1n
	R	C4A	9.656	C4Ar.2r
	N	C4A	9.717	C4Ar.2n
	R	C4A	9.779	C4Ar.3r
	N	C5	9.934	C5n.1n
	R	C5	9.987	C5n.1r
	N	C5	11.040	C5n.2n
	R	C5	11.118	C5r.1r
	N	C5	11.154	C5r.1n
	R	C5	11.554	C5r.2r
	N	C5	11.614	C5r.2n
	R	C5	12.014	C5r.3r
	N	C5A	12.116	C5An.1n
	R	C5A	12.207	C5An.1r
	N	C5A	12.415	C5An.2n
	R	C5A	12.730	C5Ar.1r
	N	C5A	12.765	C5Ar.1n
	R	C5A	12.820	C5Ar.2r
	N	C5A	12.878	C5Ar.2n
	R	C5A	13.015	C5Ar.3r
	N	C5AA	13.183	C5AAn
	R	C5AA	13.369	C5AAr
	N	C5AB	13.605	C5ABn
	R	C5AB	13.734	C5ABr
	N	C5AC	14.095	C5ACn
	R	C5AC	14.194	C5ACr
	N	C5AD	14.581	C5ADn
	R	C5AD	14.784	C5ADr
	N	C5B	14.877	C5Bn.1n
	R	C5B	15.032	C5Bn.1r
	N	C5B	15.160	C5Bn.2n
	R	C5B	15.974	C5Br
	N	C5C	16.268	C5Cn.1n
	R	C5C	16.303	C5Cn.1r
	N	C5C	16.472	C5Cn.2n
	R	C5C	16.543	C5Cn.2r
	N	C5C	16.721	C5Cn.3n
	R	C5C	17.235	C5Cr
	N	C5D	17.533	C5Dn
	R	C5D	17.717	C5Dr.1r
	N	C5D	17.740	C5Dr.1n
	R	C5D	18.056	C5Dr.2r
	N	C5E	18.524	C5En
	R	C5E	18.748	C5Er
	N	C5E	19.722	C6n
	R	C5E	20.040	C6r
	N	C6A	20.213	C6An.1n
	R	C6A	20.439	C6An.1r
	N	C6A	20.709	C6An.2n
	R	C6A	21.083	C6Ar
	N	C6AA	21.159	C6AAn
	R	C6AA	21.403	C6AAr.1r
	N	C6AA	21.483	C6AAr.1n
	R	C6AA	21.659	C6AAr.2r
	N	C6AA	21.688	C6AAr.2n
	R	C6AA	21.767	C6AAr.3r
	N	C6B	21.936	C6Bn.1n
	R	C6B	21.992	C6Bn.1r
	N	C6B	22.268	C6Bn.2n
	R	C6B	22.487	C6Br
	N	C6C	22.754	C6Cn.1n
	R	C6C	22.902	C6Cn.1r
	N	C6C	23.030	C6Cn.2n
	R	C6C	23.249	C6Cn.2r
	N	C6C	23.375	C6Cn.3n
	R	C6C	24.044	C6Cr
	N	C7	24.102	C7n.1n
	R	C7	24.163	C7n.1r
	N	C7	24.556	C7n.2n
	R	C7	24.915	C7r
	N	C7A	25.091	C7An
	R	C7A	25.295	C7Ar
	N	C8	25.444	C8n.1n
	R	C8	25.492	C8n.1r
	N	C8	26.154	C8n.2n
	R	C8	26.714	C8r
	N	C9	27.826	C9n
	R	C9	28.186	C9r
	N	C10	28.450	C10n.1n
	R	C10	28.525	C10n.1r
	N	C10	28.715	C10n.2n
	R	C10	29.451	C10r
	N	C11	29.740	C11n.1n
	R	C11	29.853	C11n.1r
	N	C11	30.217	C11n.2n
	R	C11	30.627	C11r
	N	C12	31.116	C12n
	R	C12	33.266	C12r
	N	C13	33.738	C13n
	R	C13	34.782	C13r
	N	C15	35.043	C15n
	R	C15	35.404	C15r
	N	C16	35.567	C16n.1n
	R	C16	35.707	C16n.1r
	N	C16	36.276	C16n.2n
	R	C16	36.512	C16r
	N	C17	37.235	C17n.1n
	R	C17	37.345	C17n.1r
	N	C17	37.549	C17n.2n
	R	C17	37.610	C17n.2r
	N	C17	37.771	C17n.3n
	R	C17	38.032	C17r
	N	C18	38.975	C18n.1n
	R	C18	39.041	C18n.1r
	N	C18	39.464	C18n.2n
	R	C18	40.439	C18r
	N	C19	40.671	C19n
	R	C19	41.590	C19r
	N	C20	42.774	C20n
	R	C20	45.346	C20r
	N	C21	47.235	C21n
	R	C21	48.599	C21r
	N	C22	49.427	C22n
	R	C22	50.730	C22r
	N	C23	50.932	C23n.1n
	R	C23	51.057	C23n.1r
	N	C23	51.901	C23n.2n
	R	C23	52.648	C23r
	N	C24	53.004	C24n.1n
	R	C24	53.116	C24n.1r
	N	C24	53.167	C24n.2n
	R	C24	53.286	C24n.2r
	N	C24	53.808	C24n.3n
	R	C24	56.665	C24r
	N	C25	57.180	C25n
	R	C25	58.379	C25r
	N	C26	58.737	C26n
	R	C26	61.650	C26r
	N	C27	61.983	C27n
	R	C27	63.104	C27r
	N	C28	64.128	C28n
	R	C28	64.432	C28r
	N	C29	65.118	C29n
	R	C29	65.861	C29r
	N	C30	67.696	C30n
	R	C30	67.809	C30r
	N	C31	68.732	C31n
	R	C31	70.961	C31r
	N	C32	71.225	C32n.1n
	R	C32	71.474	C32n.1r
	N	C32	72.929	C32n.2n
	R	C32	73.231	C32r.1r
	N	C32	73.318	C32r.1n
	R	C32	73.577	C32r.2r
	N	C33	79.543	C33n
	R	C33	83.300	C33r
Cretaceous Normal Super-Chron ("Cretaceous Quiet Zone")	Primary
	N	C34	102.000	C34n
	R	M"-3"r set	102.200	M"-3"r set
	N	(C34n)	108.000	(C34n)
	R	M"-2"r set	108.200	M"-2"r set
	N	(C34n)	118.500	(C34n)
	R	M"-1"r	118.600	M"-1"r
	N	(C34n)	124.613	(C34n)
M-Sequence	Primary
	R	M0r	125.000	M0r
	N	M1	127.237	M1n
	R	M1	127.606	M1r
	N	M3	128.114	M3n
	R	M3	129.765	M3r
	N	M5	130.798	M5n
	R	M5	131.190	M5r
	N	M6	131.411	M6n
	R	M6	131.558	M6r
	N	M7	131.849	M7n
	R	M7	132.197	M7r
	N	M8	132.518	M8n
	R	M8	132.825	M8r
	N	M9	133.140	M9n
	R	M9	133.498	M9r
	N	M10	133.870	M10n
	R	M10	134.297	M10r
	N	M10N	134.623	M10Nn.1n
	R	M10N	134.668	M10Nn.1r
	N	M10N	134.978	M10Nn.2n
	R	M10N	135.000	M10Nn.2r
	N	M10N	135.280	M10Nn.3n
	R	M10N	135.685	M10Nr
	N	M11	136.443	M11n
	R	M11	136.682	M11r.1r
	N	M11	136.706	M11r.1n
	R	M11	136.900	M11r.2r
	N	M11A	137.386	M11An.1n
	R	M11A	137.439	M11An.1r
	N	M11A	137.514	M11An.2n
	R	M11A	137.600	M11Ar
	N	M12	137.815	M12n
	R	M12	138.559	M12r.1r
	N	M12	138.634	M12r.1n
	R	M12	138.781	M12r.2r
	N	M12A	139.030	M12An
	R	M12A	139.116	M12Ar
	N	M13	139.291	M13n
	R	M13	139.534	M13r
	N	M14	139.770	M14n
	R	M14	140.361	M14r
	N	M15	140.656	M15n
	R	M15	141.048	M15r
	N	M16	142.061	M16n
	R	M16	142.547	M16r
	N	M17	142.835	M17n
	R	M17	144.038	M17r
	N	M18	144.568	M18n
	R	M18	144.879	M18r
	N	M19	144.990	M19n.1n
	R	M19	145.064	M19n.1r
	N	M19	145.947	M19n.2n
	R	M19	146.165	M19r
	N	M20	146.471	M20n.1n
	R	M20	146.523	M20n.1r
	N	M20	147.161	M20n.2n
	R	M20	147.773	M20r
	N	M21	148.544	M21n
	R	M21	148.923	M21r
	N	M22	150.046	M22n.1n
	R	M22	150.083	M22n.1r
	N	M22	150.120	M22n.2n
	R	M22	150.157	M22n.2r
	N	M22	150.210	M22n.3n
	R	M22	150.729	M22r
	N	M22A	150.844	M22An
	R	M22A	151.006	M22Ar
	N	M23	151.336	M23n
	R	M23	151.616	M23r.1r
	N	M23	151.642	M23r.1n
	R	M23	152.261	M23r.2r
	N	M24	152.498	M24n
	R	M24	152.956	M24r.1r
	N	M24	152.981	M24r.1n
	R	M24	153.185	M24r.2r
	N	M24A	153.312	M24An
	R	M24A	153.575	M24Ar
	N	M24B	153.931	M24Bn
	R	M24B	154.084	M24Br
	N	M25	154.372	M25n
	R	M25	154.550	M25r
Pre-M25 Marine Magnetic Anomaly Series	Primary
	U	M25A	154.669	M25An.1n
	R	M25A	154.726	M25An.1r
	U	M25A	154.805	M25An.2n
	R	M25A	154.862	M25An.2r
	U	M25A	154.969	M25An.3n
	R	M25A	155.049	M25Ar
	U	M26	155.128	M26n.1n
	R	M26	155.185	M26n.1r
	U	M26	155.241	M26n.2n
	R	M26	155.298	M26n.2r
	U	M26	155.355	M26n.3n
	R	M26	155.394	M26n.3r
	U	M26	155.536	M26n.4n
	R	M26	155.706	M26r
	N	M27	155.847	M27n
	R	M27	156.005	M27r
	N	M28	156.294	M28n
	R	M28	156.438	M28r
	N	M28	156.534	M28An
	R	M28	156.759	M28Ar
	N	M28	156.808	M28Bn
	R	M28	156.892	M28Br
	N	M28	156.994	M28Cn
	R	M28	157.082	M28Cr
	N	M28	157.159	M28Dn
	R	M28	157.265	M28Dr
	N	M29	157.414	M29n.1n
	R	M29	157.443	M29n.1r
	N	M29	157.507	M29n.2n
	R	M29	157.734	M29r
	N	M29	157.781	M29An
	R	M29	157.844	M29Ar
	N	M30	157.964	M30n
	R	M30	158.118	M30r
	N	M30	158.214	M30An
	R	M30	158.244	M30Ar
	N	M31	158.394	M31n.1n
	R	M31	158.473	M31n.1r
	N	M31	158.500	M31n.2n
	R	M31	158.540	M31n.2r
	N	M31	158.582	M31n.3n
	R	M31	158.634	M31r
	N	M32	158.656	M32n.1n
	R	M32	158.684	M32n.1r
	N	M32	158.778	M32n.2n
	R	M32	158.829	M32n.2r
	N	M32	158.857	M32n.3n
	R	M32	158.938	M32r
	N	M33	159.224	M33n
	R	M33	159.351	M33r
	N	M33	159.427	M33An
	R	M33	159.494	M33Ar
	N	M33	159.559	M33Bn
	R	M33	159.669	M33Br
	N	M33	159.706	M33Cn.1n
	R	M33	159.756	M33Cn.1r
	N	M33	159.874	M33Cn.2n
	R	M33	160.070	M33Cr
	N	M34	160.152	M34n.1n
	R	M34	160.221	M34n.1r
	N	M34	160.267	M34n.2n
	R	M34	160.304	M34n.2r
	N	M34	160.334	M34n.3n
	R	M34	160.383	M34r
	N	M34	160.404	M34An
	R	M34	160.539	M34Ar
	N	M34	160.631	M34Bn.1n
	R	M34	160.666	M34Bn.1r
	N	M34	160.690	M34Bn.2n
	R	M34	160.732	M34Br
	N	M35	160.816	M35n
	R	M35	160.994	M35r
	N	M36	161.098	M36n
	R	M36	161.167	M36r
	N	M36	161.209	M36An
	R	M36	161.229	M36Ar
	N	M36	161.258	M36Bn
	R	M36	161.394	M36Br
	N	M36	161.461	M36Cn
	R	M36	161.580	M36Cr
	N	M37	161.814	M37n.1n
	R	M37	161.925	M37n.1r
	N	M37	162.042	M37n.2n
	R	M37	162.173	M37r
	N	M38	162.279	M38n.1n
	R	M38	162.333	M38n.1r
	N	M38	162.425	M38n.2n
	R	M38	162.460	M38n.2r
	N	M38	162.538	M38n.3n
	R	M38	162.640	M38n.3r
	N	M38	162.870	M38n.4n
	R	M38	162.934	M38n.4r
	N	M38	163.075	M38n.5n
	R	M38	163.159	M38r
	N	M39	163.312	M39n.1n
	R	M39	163.433	M39n.1r
	N	M39	163.549	M39n.2n
	R	M39	163.640	M39n.2r
	N	M39	163.767	M39n.3n
	R	M39	163.856	M39n.3r
	N	M39	164.075	M39n.4n
	R	M39	164.211	M39n.4r
	N	M39	164.301	M39n.5n
	R	M39	164.414	M39n.5r
	N	M39	164.495	M39n.6n
	R	M39	164.609	M39n.6r
	N	M39	164.676	M39n.7n
	R	M39	164.755	M39n.7r
	N	M39	164.854	M39n.8n
	R	M39	164.940	M39r
	N	M40	165.002	M40n.1n
	R	M40	165.072	M40n.1r
	N	M40	165.195	M40n.2n
	R	M40	165.244	M40n.2r
	N	M40	165.289	M40n.3n
	R	M40	165.402	M40n.3r
	N	M40	165.449	M40n.4n
	R	M40	165.546	M40r
	N	M41	165.610	M41n
	R	M41	165.710	M41r
	No Data		165.797		[no data]
S. Spain series	Primary
	R		165.954	Brem-R
	N		166.306	Morr-N
	R		166.444	Subc-R
	N		166.620	Progr-N
	R		167.169	Aur-R
	N		167.287	Aur-N
	R		167.404	Zig-R2
	N		167.444	Zig-N2
	R		167.600	Zig-R1
	N		167.679	Zig-N1
	R		167.738	Park-R4
	N		167.797	Park-N4
	R		167.849	Park-R3
	N		167.885	Park-N3
	R		168.002	Park-R2
	N		168.061	Park-N2
	R		168.179	Park-R1
	N		168.232	Park-N1
	R		168.279	Garan-R4
	N		168.385	Garan-N4
	R		168.443	Garan-R3
	N		168.473	Garan-N3
	R		168.561	Garan-R2
	N		168.620	Garan-N2
	R		168.649	Garan-R1
	N		168.855	Garan-N1
	R		169.404	Nior-R2
	N		169.483	Nior-N1
	R		169.681	Nior-R1
	N		169.757	Humph-N2
	R		169.934	Humph-R2
	N		170.110	Humph-N1
	R		170.169	Nior-R1
	N		170.255	Prop-N6
	R		170.286	Prop-R5
	N		170.318	Prop-N5
	R		170.365	Prop-R4
	N		170.412	Prop-N4
	R		170.424	Prop-R3
	N		170.463	Prop-N3
	R		170.522	Prop-R2
	N		170.561	Prop-N2
	R		170.600	Prop-R1
	N		170.816	Laev-N3
	R		170.963	Laev-R2
	N		171.110	Laev-N2
	R		171.139	Laev-R1
	N		171.208	Laev-N1
	R		171.277	Disc-R2
	N		171.424	Disc-N2
	R		171.522	Disc-R1
S. Switzerland series	Primary
	N		171.600	Disc-N1
	R		172.044	Concav-R
	N		173.044	Brad-N2
	R		173.156	Brad-R1
	N		173.600	Brad-N1
	R		174.600	Murch-R
	N		174.756	Opal-N2
	R		174.844	Opal-R2
	N		175.156	Opal-N1
	R		175.289	Opal-R1
	N		176.090	Aalen-N
	R		176.678	Aalen-R
Toarcian composite series	Primary
	N		177.560	Pseudo-N
	R		178.295	Dispan-R
	N		178.589	Dispan-N
	R		179.128	Thou-R2
	N		179.569	Thou-N1
	R		180.653	Thou-R1
	N		180.738	Var-N
	R		181.025	Bifr-R
	N		181.350	Serp-N3
	R		181.650	Serp-R3
	N		181.950	Serp-N2
	R		182.175	Serp-R2
	N		182.400	Serp-N1
	R		182.550	Serp-R1
	N		182.850	Tenui-N
	R		183.630	Spin-R5
S. Switzerland series	Primary
	N		183.684	Spin-N4
	R		183.720	Spin-R4
	N		183.900	Spin-N3
	R		183.930	Spin-R3
	N		183.960	Spin-N2
	R		184.020	Spin-R2
	N		184.429	Spin-N1
	R		184.658	Spin-R1
	N		185.117	Marg-N5
	R		185.163	Marg-R4
	N		185.392	Marg-N4
	R		185.438	Marg-R3
	N		185.667	Marg-N3
	R		185.896	Marg-R2
	N		185.988	Marg-N2
	R		186.263	Marg-R1
	N		186.400	Marg-N1
	R		187.387	Dav-R2
	N		187.586	Dav-N1
	R		187.769	Dav-R1
	N		187.809	ibex-N1
	R		187.817	Ibex-R7
	N		187.872	Ibex-N7
	R		187.888	Ibex-R6
	N		187.904	Ibex-N6
	R		188.182	Ibex-R5
	N		188.198	Ibex-N5
	R		188.302	Ibex-R4
	N		188.317	Ibex-N4
	R		188.349	Ibex-R3
	N		188.373	Ibex-N3
	R		188.381	Ibex-R2
	N		188.397	Ibex-N2
	R		188.461	Ibex-R1
	N		188.524	Ibex-N1
	R		188.561	James-R2
	N		188.614	James-N2
	R		188.667	James-R1
	N		189.070	James-N1
	No Data		190.290	No Data
Austrian series	Primary
	N		190.635	Sinem-N6
	R		190.980	Sinem-R6
	N		191.118	Sinem-N5
	R		191.256	Sinem-R5
	N		191.394	Sinem-N4
	R		193.740	Sinem-R4
	N		193.878	Sinem-N3
	R		194.292	Sinem-R3
	N		194.568	Sinem-N2
	R		194.844	Sinem-R2
	N		195.327	Sinem-N1
	R		196.810	Sinem-R1
	N		196.965	Hett-N3
	R		198.360	Hett-R2
	N		198.515	Hett-N2
	R		198.670	Hett-R1
	N		199.600	Hett-N1
	U	Rhaet-N?	201.200
Newark basin (eastern USA)	Primary
	N	E24	202.021	E24n
	R	E23	202.048	E23r
	N	E23	203.026	E23n
	R	E22	203.330	E22r
	N	E22	203.565	E22n.2n
	R	E22	203.576	E22n.1r
	N	E22	203.941	E22n.1n
	R	E21	204.256	E21r.3r
	N	E21	204.277	E21r.2n
	R	E21	204.410	E21r.2r
	N	E21	204.458	E21r.1n
	R	E21	204.647	E21r.1r
	N	E21	205.177	E21n
	R	E20	206.554	E20r.2r
	N	E20	206.590	E20r.1n
	R	E20	206.765	E20r.1r
	N	E20	206.884	E20n
	R	E19	207.567	E19r
	N	E19	207.717	E19n
	R	E18	208.098	E18r
	N	E18	208.624	E18n
	R	E17	210.006	E17r
	N	E17	210.466	E17n
	R	E16	210.762	E16r
	N	E16	212.559	E16n
	R	E15	212.871	E15r.2r
	N	E15	212.903	E15r.1n
	R	E15	213.110	E15r.1r
	N	E15	213.942	E15n
	R	E14	215.427	E14r
	N	E14	216.656	E14n
	R	E13	217.469	E13r
	N	E13	218.390	E13n.2n
	R	E13	218.425	E13n.1r
	N	E13	218.953	E13n.1n
	R	E12	219.784	E12r
	N	E12	219.953	E12n
	R	E11	221.956	E11r
	N	E11	222.232	E11n
	R	E10	222.728	E10r
	N	E10	223.219	E10n
	R	E9	224.487	E9r
	N	E9	225.016	E9n
	R	E8	226.634	E8r
	N	E8	227.245	E8n
	R	E7	227.619	E7r
	N	E7	228.924	E7n
	R	E6	229.284	E6r
	N	E6	229.990	E6n
	R	E5	230.384	E5r
	N	E5	230.531	E5n.2n
	R	E5	230.645	E5n.1r
	N	E5	231.047	E5n.1n
	R	E4	231.226	E4r
	N	E4	231.649	E4n
	R	E3	231.817	E3r
	N	E3	232.054	E3n
	R	E2	232.412	E2r
	N	E2	232.818	E2n
	R	E1	233.153	E1r part
	No Data		233.337
Greece, Italy, Austria, Turkey	Primary
	N	Margar-N (lower)	235.291
	R	Curionii-R	237.330
	N		237.525	Nevad-N2
	R		237.990	Nevad-R2
	N	Nevad-N1	239.430
	R		239.925	Nevad-R1
Albania, Greece, Poland	Primary
	N	Hungar-N	240.810
	R		241.149	Parace-R2
	N		241.417	Parace-N1
	R	Balat-R	241.649	Balat-R.r2
	N	Balat-R	241.720	Balat-R.n1
	R	Balat-R	242.229	Balat-R.r1
	N	Kocae-N	242.372	Kocae-N.n2
	R	Kocae-N	242.408	Kocae-N.r1
	N	Kocae-N	243.679	Kocae-N.n1
	R		244.051	Paracr-R
	N	Paracr-N	245.349
	R	SpR2	245.385	SpR2.r3?
	U	SpR2	245.422	SpR2.n3?
	R	SpR2	245.458	SpR2.r2?
Arctic Stratotypes of Early Triassic Stages	Primary
	U	SpR2	245.495	SpR2.n2?
	R	SpR2	245.808	SpR2.r1
	N		246.683	SpN1
	R	SpR1	247.792
	N		247.938	SmN3?
	R		248.233	SmR2
	N		249.100	SmN2
	R		249.308	SmR1?
	N	SmN1	249.750
	R		249.994	DR2
	N		250.069	DN2
	R		250.200	DR1
	N		250.356	DN1
	R		250.500	GR2
	N		250.589	GN2
	R		250.775	GR1
	N	GN1	251.28
Illawara Series	Primary
	R		252.12
	U		253.80
	R		254.21
	N		254.59
	R		254.99
	N		255.13
	R		255.35
	N		255.50
	R		255.72
	N		255.86
	R		256.28
	N		257.37
	R		257.68
	N		258.06
	R		258.72
	N		259.10
	R		260.47
	N		260.62
	R		261.08
	N		261.23
	R		261.76
	N		261.91
	R		262.89
	N		263.50
	R		264.38
	N		264.99
	R		265.21
	N		265.36
	R		265.48
	N		265.64
Kiaman Reversed-polarity Hyperchron	Primary
	R		280.52
	N		280.80
	R		297.99
	N		298.13
	R		299.10
	N	Kartamyshian N	299.31
	R		302.09
	N		302.16
	R		302.43
	N		302.50
Donetzian Mixed-polarity Hyperchron	Primary
	R		305.30
	N		305.37
	R		307.93
	N		308.00
	R		308.96
	N		309.03
	R		309.92
	N		309.99
	R		312.16
	N		312.39
	R		312.63
	N		312.76
	R		312.93
	N		313.06
	R		313.24
	N		313.37
	R		313.56
	N		313.68
	R		314.33
	N		315.31
	R		317.82
	N		318.18
	R		319.42
	N		320.38
	R		323.74
	N		324.71
	R		326.91
	N		328.46
	R		329.46
	N		329.82
	R		330.12
	N		330.20
	R		331.03
	N		331.40
	R		332.27
	N		332.64
	R		332.89
	N		333.24
	R		334.08
	N		335.10
	R		335.94
	N		336.45
	R		336.98
	N		337.06
	R		340.54
	N		342.09
	R		343.11
	N		344.68
	R		347.02
	N		350.46
	R		354.48
	N		354.70
	R		354.94
	N		355.29
	R		356.99
	N		357.95
	No Data	No Data	362.15
	N		365.90
Poorly known	Primary
	No Data	No Data	369.98
	U		374.50
	No Data	No Data	375.66
	U		378.66
	No Data	No Data	385.98
	U		388.98
	No Data	No Data	392.80
Sayan (Rn) hyperchron	Primary
	N		397.50
	R		399.69
	N		400.20
	R		401.19
	N		401.70
	R		413.53
	N		415.03
Ludlow-Pridoli mixed-polarity interval	Primary
	U		422.90
Wenlock Normal-polarity interval	Primary
	N		428.20
Llandovery mixed-polarity interval	Primary
	U		436.10
	No Data	No Data	442.44
	U		443.70
	N		449.28
	U		452.97
	R		454.45
	N		458.03
	R		459.25
Dominated by Normal polarity	Primary
	N		460.90
	R		461.43
	N		462.07
	R		462.73
	N		464.17
	R		466.26
	N		466.76
Poorly known	Primary
	R		479.82
	N		480.55
	R		481.50
Ordov-Camb boundary series	Primary
	U		486.82
	R		488.55
	N		488.77
	R		489.15
	N		489.43
	R		489.98
	N		490.15
	R		490.76
	N		491.09
	R		492.10
	N		492.90
No data: major polar wander	Primary
	No Data	No Data	503.04
Mixed, Reversed-polarity dominant
	N		503.54
	R		528.49
	N		529.98
	R		542.00
Crussol reference section	Secondary		off
	TOP		150.210	Top of section is mid-H. hybonotum Zone; and is probably near top of Chron M22r
	R		150.729	M22r
	N	M22A	150.844	M22An
	R	M22A	151.006	M22Ar
	N	M23	151.336	M23n
	R	M23	151.616	M23r.1r
	N	M23	151.642	M23r.1n
	R	M23	152.261	M23r.2r
	N	M24	152.498	M24n
	R	M24	152.956	M24r.1r
	N	M24	152.981	M24r.1n
	R	M24	153.185	M24r.2r
	N	M24A	153.312	M24An
	R	M24A	153.483	M24Ar.1r
	N	M24A	153.509	M24Ar.1n
	R	M24A	153.575	M24Ar.2r
	N	M24B	154.007	M24Bn
	R	M24B	154.084	M24Br
	N	M25	154.432	M25n
	R	M25	154.550	M25r
	N	M25A	154.669	M25An.1n
	R	M25A	154.698	M25An.1r
	N	M25A	154.805	M25An.2n
	R	M25A	154.834	M25An.2r
	N	M25A	154.969	M25An.3n
	R	M25A	155.049	M25Ar
Composite	Secondary
	U	M26	155.128	M26n.1n
	R	M26	155.185	M26n.1r
	U	M26	155.241	M26n.2n
	R	M26	155.298	M26n.2r
	U	M26	155.355	M26n.3n
	R	M26	155.434	M26n.3r
	U	M26	155.506	M26n.4n
	R	M26	155.691	M26r
	N	M27	155.786	M27n
Aguilon (Spain)	Secondary
	R		155.974	Bim-R2
	N		156.378	Bim-N2
	R		156.629	Bim-R1
	N		156.808	Bim-N1
	R		156.854	Bif-R3
	N		156.901	Bif-N3
	R		157.087	Bif-R2
	N		157.133	Bif-N2
	R		157.226	Bif-R1
	N		157.483	Bif-N1
	R		157.717	Trans-R4
	N		157.785	Trans-N3
	R		157.836	Trans-R3
	N		157.942	Trans-N2
	R		157.980	Trans-R2.r3
	N		157.988	Trans-R2.n2
	R		158.018	Trans-R2.r2
	N		158.026	Trans-R2.n1
England	Secondary
	R		158.169	Trans-R2.r1
	N		158.358	Trans-N1
	R		158.458	Trans-R1
	N		158.585	Plic-N8
	R		158.610	Plic-R7
	N		158.660	Plic-N7
	R		158.686	Plic-R6
	N		158.711	Plic-N6
	R		158.761	Plic-R5
	N		158.787	Plic-N5
	R		158.877	Plic-R4
	N		158.913	Plic-N4
	R		159.006	Plic-R3
	N		159.141	Plic-N3
	R		159.242	Plic-R2
	N		159.344	Plic-N2
	R		159.513	Plic-R1
	N		159.580	Plic-N1
	R		159.732	Cord-R4
	N		159.892	Cord-N4
	R		160.017	Cord-R3
	N		160.100	Cord-N3
	R		160.345	Cord-R2
	N		160.383	Cord-N2
	R		160.461	Cord-R1
	N		160.617	Cord-N1
	R		160.679	Mar-R4
	N		160.702	Mar-N4
	R		160.725	Mar-R3
	N		160.772	Mar-N3
	R		161.048	Mar-R2
	N		161.096	Mar-N2
	R		161.177	Mar-R1
	N		161.209	Mar-N1
	R		161.269	Lamb-R4
	N		161.360	Lamb-N4
	R		161.511	Lamb-R3
	N		161.632	Lamb-N3
	R		161.723	Lamb-R2
England-Burgundy-Swabia Composite	Secondary
	N		161.891	Lamb-N2
	R		161.920	Lamb-R1
	N		161.949	Lamb-N1
	R		162.143	Ath-R2
	N		162.408	Ath-N1
	R		162.459	Ath-R1
	N		162.579	Cor-N
	R		162.673	Cor-R
	N		163.287	Jas-N
	R		163.415	Call-R
	N		163.535	Call-N
	R		163.654	Koen-R2
	N		163.799	Koen-N1
	R		163.902	Koen-R1
	N		164.601	Herv-N2
	R		164.687	Herv-R1
	N		164.748	Herv-N1
	R		164.856	Disc-R2
	N		164.905	Disc-N2
	R		164.944	Disc-R1
	N		165.130	Disc-N1
	No Data		165.307	[no data]
S. Spain series	Secondary
	R		165.365	Retro-R
	N		165.542	Retro-N
Mediteranean Region	Secondary
	TOP		202.290
	N	Retic-N2	202.627
	R	Retic-R1	202.680	Retic-R1.r3
	U	Retic-R1	202.721	Retic-R1.n2
	R	Retic-R1	202.775	Retic-R1.r2
	U	Retic-R1	202.842	Retic-R1.n1
	R	Retic-R1	203.192	Retic-R1.r1
	N	Retic-N1	203.905
	R	Quin-R1	203.967	Quin-R1.r2
	U	Quin-R1	204.029	Quin-R1.n1
	R	Quin-R1	204.630	Quin-R1.r1
	N	Quin-N1	205.189
	R	Macer-R2	206.283
	U	Macer-N1	206.395	Macer-N1.n2
	R	Macer-N1	206.451	Macer-N1.r2
	U	Macer-N1	207.251	Macer-N1.n1
	R	Macer-R1	207.530
	N	Hogar-N1	207.738	Hogar-N1.n2
	R	Hogar-N1	207.860	Hogar-N1.r1
	N	Hogar-N1	208.835	Hogar-N1.n1
	R	Hogar-R1	210.006
	N	Bicren-R1 to N2	210.459	Bicren-N2
	R	Bicren-R1 to N2	210.705	Bicren-R2
	N	Bicren-R1 to N2	210.951	Bicren-N1
	R	Bicren-R1 to N2	211.120	Bicren-R1
	N	Magnus-N	212.545
	R	Malay-R3	212.763	Malay-R3.r2
	N	Malay-R3	212.817	Malay-R3.n1
	R	Malay-R3	213.144	Malay-R3.r1
	N	Malay-N1 to N3	213.308	Malay-N3
	R	Malay-N1 to N3	213.508	Malay-R2
	N	Malay-N1 to N3	213.671	Malay-N2
	R	Malay-N1 to N3	213.798	Malay-R1
	N	Malay-N1 to N3	213.944	Malay-N1
	R		215.275	Jand-R1
	N	Jand-N1	215.375	Jand-N1.n2
	R	Jand-N1	215.426	Jand-N1.r1
	N	Jand-N1	216.533	Jand-N1.n1
	R	Spino-R2	217.021	Spino-R2.r2
	N	Spino-R2	217.085	Spino-R2.n1
	R	Spino-R2	217.170	Spino-R2.r1
	N	Spino-N2	217.722	Spino-N2.n2
	R	Spino-N2	217.786	Spino-N2.r1
	N	Spino-N2	218.125	Spino-N2.n1
	R	Spino-R1	218.317
	N	Spino-N1	218.401	Spino-N1.n3
	R	Spino-N1	218.444	Spino-N1.r2
	N	Spino-N1	218.614	Spino-N1.n2
	R	Spino-N1	218.679	Spino-N1.r1
	N	Spino-N1	218.679	Spino-N1.n1
	No Data		222.700
SW Turkey	Secondary	off
	N	Austro-N2	223.086
	R	Austro-R1	224.271
	N	Austro-N1	224.626
	R	Trachy-R2	226.238	Trachy-R2.r2
	N	Trachy-R2	226.340	Trachy-R2.n1
	R	Trachy-R2	226.531	Trachy-R2.r1
	N	Trachy-N1	227.079	Trachy-N1.n2
	R	Trachy-N1	227.143	Trachy-N1.r1
	N	Trachy-N1	227.261	Trachy-N1.n1
	R	Trachy-R1	227.636
	N	Daxa-N	228.993
	R	Regole-R	229.293
	N	Neum-N	229.930
	R	Neum-R	230.014	Neum-R.r2
	U	Neum-R	230.106	Neum-R.n1
	R	Neum-R	230.322	Neum-R.r1
	N	Long-N2	230.450
	R	Long-R1	230.606
	N	Long-N1	231.541	Long-N1.n2
	U	Long-N1	231.569	Long-N1.r1
	N	Long-N1	231.683	Long-N1.n1
	R	Gred-R3	231.931
	N	Gred-N2	232.014	Gred-N2.n2
	U	Gred-N2	232.096	Gred-N2.r1
	N	Gred-N2	232.212	Gred-N2.n1
	R	Gred-R2	232.510
	N	Gred-N1	232.659	Gred-N1.n2
	U	Gred-N1	232.725	Gred-N1.r1
	N	Gred-N1	232.990	Gred-N1.n1
	R	Gred-R1	233.172
	N	Margar-N	233.337	upper


Sub-Boreal Ammonites	:	Sub-Boreal Zone	Sub-Boreal Subzone		CRETACEOUS = J. Thierry et al. (in Hardenbol et al., SEPM charts, 1998), with GTS2004 revisions; JURASSIC = Groupe Francais d'etude du Jurassique (1997); TRIASSIC = P. Van Veen (in Hardenbol et al., SEPM charts, 1998), with GTS2004 revisions.

Sub-Boreal Zone	block	180	148/206/212	notitle
	TOP	65.50
	Un-Named Interval	66.50
	Pachydiscus gollevillensis	69.23
	Pachy. neubergicus / Acanthoscaphites tridens?	70.60
	Nostoceras hyatti	71.30
	Didymoceras donezianum	75.05
	Bostrychoceras polyplocum	80.50
	Neancyloceras phaleratum	80.64
	Trachyscaphites spiniger	81.22
	Scaphites hippocrepis III	81.63
	Placenticeras bidorsatum	83.53
	Placen. polyopsis	85.85
	Paratexanites serratomarginatus	86.96
	Gauthiericeras margae	87.77
	Peroniceras tridorsatum	88.58
	Forresteria petrocoriensis	89.07
	Subprionocyclus neptuni	90.48
	Collignoniceras woollgari	92.13
	Mammites nodosoides	92.70
	Watinoceras devonense / coloradoense	93.55
	Nigericeras scotti	93.60
	Neocardioceras juddii	93.64
	Burroceras clydense	93.72
	Metoicoceras geslinianum	94.01
	Calycoceras guerangeri	94.75
	Acanthoceras jukesbrownei	95.06
	Acanth. rhotomagense	95.68
	Cunningtoniceras inerme	96.01
	Mantelliceras dixoni	97.81
	Mantel. mantelli	99.54
	Stoliczkaia dispar	100.94
	Mortoniceras inflatum	106.42
	Euhoplites lautus	107.01
	Euhoplites loricatus	108.18
	Hoplites dentatus	108.77
	Douvilleiceras mammillatum	110.83
	Leymeriella tardefurcata	112.00
	Hypacanthoplites jacobi	115.00
	Parahoplites nutfieldiensis	118.00
	Cheloniceras martinoides	121.00
	Tropaeum bowerbanki	121.90
	Deshayesites deshayesi	122.93
	Desh. forbesi	123.97
	Prodeshayesites fissicostatus	125.00
	Parancyloceras bidentatum / Paran. scalare	125.17
	Simanocyloceras stolleyi	126.10
	Ancyloceras inexum / S. pingue	126.92
	Paracrioceras denckmanni	128.02
	Paracr. elegans	128.63
	Haplocrioceras fissicostatum	128.97
	Paracrioceras rarocinctum	129.97
	Craspedodiscus discofalcatus	132.56
	Crasp. gottschei	132.76
	Milanowskia speetonensis	133.69
	Speetoniceras inversum	134.18
	Endemoceras regale	135.15
	Ende. noricum	136.24
	Ende. amblygonium	136.65
	Olcostephanus spp.	136.86
	Dicostella tuberculatum	137.27
	Dichotomites	137.97
	Prodichotomites	139.21
	Polyptychites	139.77
	Paratollia/Platylenticeras	139.98
	Peregrinoceras albidum	140.24
	Surites stenomphalus	140.85
	Surites icenii	141.66
	Hectoroceras kochi	142.16
	Runctonia runctoni	142.84
	Subcraspedites lamplughi	144.46
	Subcrasp. preplicomphalus	145.63
	Subcraspedites primitivus	146.16
	Paracraspedites oppressus	146.32
	Titanites anguiformis	146.71
	Galbanites kerberus	147.03
	Galb. okusensis	147.41
	Glaucolithites glaucolithus	147.71
	Progalbanites albani	148.00
	Virgatopavlovia fittoni	148.39
	Pavlovia rotunda	148.66
	Pav. pallasioides	148.92
	Pectinatites pectinatus	149.37
	Pect. hudlestoni	149.76
	Pect. wheatleyensis	150.02
	Pect. scitulus	150.37
	Pect. elegans	150.63
	Aulacostephanus autissiodorensis	151.17
	Aulacostephanus eudoxus	152.38
	Aulacostephanus mutabilis	153.93
	Rasenia cymodoce	154.97
	Pictonia baylei	155.65
	Ringsteadia pseudocordata	156.89
	Perisphinctes cautisnigrae	157.26
	Perisphinctes pumilus	158.43
	Perisphinctes plicatilis	159.61
	Cardioceras cordatum	160.66
	Quenstedtoceras mariae	161.21
	Quenstedtoceras lamberti	162.01
	Peltoceras athleta	162.52
	Erymnoceras coronatum	162.86
	Kosmoceras jason	163.20
	Sigaloceras calloviense	163.54
	Proplanulites koenigi	164.23
	Macrocephalites herveyi	164.74
	Clydoniceras discus	165.13
	Oxycerites orbis	165.52
	Procerites hodsoni	166.11
	Morrisiceras morrisi	166.31
	Tulites subcontractus	166.50
	Procerites progracilis	166.89
	Zigzagiceras zigzag 	167.68
	Parkinsonia parkinsoni	168.27
	Garantiana garantiana	168.86
	Strenoceras niortense	169.64
	Stephanoceras  humphriesianum	170.23
	Sonninia propinquans	170.62
	Witchellia laeviuscula	171.21
	Hyperlioceras discites	171.60
	Graphoceras concavum	172.49
	Brasilia bradfordensis	173.38
	Ludwigia murchisonae	174.71
	Leioceras opalinum	175.60
	Pleydellia aalensis	176.58
	Dumortieria levesquei	178.54
	Grammoceras thouarsense	180.50
	Haugia variabilis	180.70
	Hildoceras bifrons	181.20
	Harpoceras falciferum	182.70
	Dactylioceras tenuicostatum	183.00
	Pleuroceras spinatum	184.20
	Amaltheus margaritatus	186.95
	Prodactylioceras davoei	187.75
	Tragophylloceras ibex	188.54
	Uptonia jamesoni	189.60
	Echioceras raricostatum	191.22
	Oxynoticeras oxynotum	192.04
	Asteroceras obtusum	193.25
	Caenisites turneri	194.06
	Arnioceras semicostatum	195.28
	Arietites bucklandi	196.50
	Schlotheimia angulata	197.28
	Alsatites liasicus	198.44
	Psiloceras planorbis	199.60
	Choristoceras crickmayi	202.29
	Cochloceras amoenum	203.64
	Gnomohalorites cordilleranus	205.71
	Mesohimavatites columbianus	210.01
	Drepanites rutherfordi	211.30
	Juvavites magnus	212.20
	Malayites dawsoni	214.02
	Stikinoceras kerri	216.53
	Klamathites macrolobatus	217.59
	Tropites welleri	220.95
	Tropites dilleri	222.70
	Sirenites nanseni	224.18
	Austrtrachyceras obesum	225.66
	Trachyceras debatoyense	228.01
	Frankites sutherlandi	229.43
	Maclearnoceras maclearni	229.85
	Meginoceras meginae	231.68
	Tuchodiceras poseidon	234.56
	Eoprotrachyceras matutinum	237.00
	Frechites chischa	239.00
	Eogymnotoceras deleeni	241.60
	Anagymnotoceras varium	243.68
	Lenotropites caurus	244.17
	Silberlingites mulleri	244.67
	[ un-named ]	245.17
	Keyserlingites subrobustus	245.53
	Olenikites pilaticus	246.63
	[ un-named ]	248.08
	Anawasachites tardus	248.92
	Euflemingites romunderi	249.33
	Hedenstr. hedenstroemi	249.75
	Vavilovites sverdrupi	250.22
	Proptychites candidus	250.38
	Propty. strigatus	250.55
	Ophiceras commune	250.73
	Otoceras boreale	251.09
	Otoceras concavum	251.21

Sub-Boreal Subzone	block	180	148/206/212	notitle	off
	TOP	83.53
	Placenticeras paraplanum	84.69
	Texanites gallicus	85.85
	TOP	90.48
	Romaniceras deverianum	90.89
	Roman. ornatissimum	91.31
	Roman. kallesi	91.72
	Kamerunoceras turoniense	92.13
	TOP	94.91
	Turrilites acutus	95.23
	Turr. costatus	95.68
	TOP	97.81
	Mantelliceras saxbii	98.67
	Neostlingoceras carcitanense	99.54
	Mortoniceras perinflatum	100.27
	Mort. rostratum	100.94
	Callihoplites auritus	102.31
	Hysteroceras varicosum	103.68
	Hyst. orbignyi	105.05
	Diploceras cristatum	106.42
	Anahoplites daviesi	106.71
	Euhoplites nitidus	107.01
	Euhop. meandrinus	107.30
	Mojsisovicsia subdelaruei	107.60
	Dimorphoplites niobe	107.89
	Anahoplites intermedius	108.18
	Hoplites spathi	108.48
	Lyelliceras lyelli	108.77
	Pseudosonneratia steinmanni	109.06
	Otohoplites bulliensis	109.36
	Protohoplites puzosianus	109.65
	Otohoplites raulinianus	109.94
	Cleoniceras floridum	110.24
	Sonneratia kitchini	110.53
	Sonn. perinflata	110.83
	Leymeriella regularis	111.12
	Leym. acuticostata	111.71
	Leym. schrammeni	112.00
	Hypacanthoplites anglicus	113.00
	Hypa. rubricosus	114.00
	Nolaniceras nolani	115.00
	Parahoplites nutfieldiensis	116.00
	Tropaeum subarcticum	118.00
	Cheloniceras buxtorfi	119.00
	Chelon. gracile	120.00
	Chelon. debile	121.00
	Chelon. meyendorffi	121.45
	Dufrenoyia transitoria	121.90
	Deshayesites grandis	122.42
	Cheloniceras parinodum	122.93
	Deshayesites callidiscus	123.28
	Deshay. kiliani	123.62
	Deshay. fittoni	123.97
	Prodeshayesites obsoletus	124.48
	Prodeshay. bodei	125.00
	TOP	129.97
	Simbirskites variabilis	130.96
	Simbir. marginatus	132.56
	TOP	137.27
	Prodichotomites ivanovi	137.43
	Dichotomites bidichotomoides	137.58
	Dich. triptychoites	137.73
	Dich. crassus	137.97
	Prodichotomites polytomus	138.72
	Prodich. hollwedensis	139.21
	Polyptychites hapkei	139.31
	Polypty. clarkei	139.40
	Polypty. multicostatus	139.58
	Polypty.  pavlowi	139.77
	Platylenticeras involutum	139.87
	Platy. heteropleurum	139.92
	Platy. robustum	139.98
	TOP	148.92
	Pectinatites paravirgatus	149.15
	Pect. eastlecottensis	149.37
	Pect.  encombensis	149.57
	Pect. reisiformis	149.76
	Pect. wheatleyensis	149.99
	Pect. smedmorensis	150.02
	TOP	150.37
	Gravesia gravesiana	150.50
	Gravesia gigas	150.63
	Gravesia irius	150.84
	Aulacostephanus autissiodorensis	151.17
	Aulacostephanus contejeani	151.57
	Aspidoceras caletanum	151.98
	Orthaspidoceras orthocera	152.38
	Orthaspidoceras lallierianum	153.16
	Aulacostephanus mutabilis	153.93
	Rasenioides chatellaionensis	154.19
	Lithacosphinctes achilles	154.45
	Rasenia cymodoce	154.97
	Paraspidoceras rupellense (regional)	155.65
	Ringsteadia evoluta	156.03
	Ringsteadia pseudocordata	156.53
	Ring. pseudoyo	156.78
	Ring. caledonica	156.89
	Perisphinctes variocostatus	157.04
	Perisphinctes cautisnigrae	157.26
	Perisphinctes nunningtonense	158.14
	Perisphinctes parandieri	158.43
	Perisphinctes antecedens	158.90
	Cardioceras vertebrale	159.61
	Cardioceras cordatum	159.85
	Cardioceras costicardia	160.27
	Cardioceras bukowskii	160.66
	Card. praecordatum	160.89
	Card. scarburgense	161.21
	Quenstedtoceras lamberti	161.81
	Quenst. henrici	162.01
	Kosmoceras spinosum	162.18
	Kosmo. proniae 	162.35
	Kosmo. phaeinum	162.52
	Kosmo. grossouvrei	162.69
	Kosmo. obductum	162.86
	Kosmo. jason	163.03
	Kosmo. medea	163.20
	Kosmo. endodatum	163.37
	Sigaloceras  calloviense	163.54
	Kepplerites galilaei	163.71
	Keppler. (G.) curtilobus	164.06
	Keppler. (G.) gowerianus	164.23
	Macrocephalites kamptus	164.40
	Macro. terebratus	164.57
	Kepplerites keppleri	164.74
	Clydoniceras discus	164.93
	Clyd. hollandi	165.13
	Bullatimorphites (Kh.) hannoveranus	165.33
	Hecticoceras (Prohect.) blanazense	165.52
	TOP	166.11
	Wagnericeras	166.21
	Morrisiceras morrisi	166.31
	TOP	166.89
	Asphinctites tenuiplicatus	167.09
	Oxycerites yeovillensis	167.29
	Morphoceras macrescens	167.48
	Park. (G.) convergens	167.68
	Parkinsonia bomfordi	167.87
	Park. densicostata	168.07
	Park. acris	168.27
	Garantiana tetragona	168.46
	Garant. subgaranti	168.66
	Garant. dichotoma	168.86
	Orthogarant. schroederi	169.05
	Garan. baculata	169.25
	Caumontisphinctes polygyralis	169.44
	Teloceras banksi	169.64
	Teloc. blagdeni	169.84
	Stephanoceras humphriesianum	170.03
	Dorsetensia romani	170.23
	Dorsetensia hebridica	170.42
	Emileia sauzei	170.62
	W. laeviuscula	170.82
	Shirbuirnia trigonalis	171.01
	Euhoploceras ovalis	171.21
	Hyperlio. subsectum	171.40
	Hyperlioceras walkeri 	171.60
	Graphoceras formosum	172.04
	Graph. concavum	172.49
	Brasilia gigantea	172.93
	Brasilia bradfordensis	173.38
	Ludw. murchisonae	173.82
	Ludw. obtusiformis	174.27
	Ludwigia haugi	174.71
	Leioceras bifidatum	175.16
	Leioceras opalinum	175.60
	Pleydellia lugdunensis	176.09
	Pleydellia mactra	176.58
	Dumortieria moorei	177.07
	Dumo. levesquei	177.56
	Phlyseogrammoceras dispansum	178.54
	Pseudogrammoceras fallaciosum	179.03
	Esericeras fascigerum	179.52
	Grammoceras thouarsense	180.01
	Pseduogrammoceras bingmanni	180.50
	Haugia vitiosa	180.57
	Haugia illustris	180.63
	Haugia variabilis	180.70
	crassum	180.83
	Peronoceras fibulatum	180.95
	Dactylioceras commune	181.20
	Harpoceras falciferum	182.20
	Harp. exaratum	182.70
	Dactylioceras semicelatum	182.78
	Dacty. tenuicostatum	182.85
	Dacty. clevelandicum	182.93
	Protogrammoceras paltus	183.00
	Pleuroceras hawskerense	183.60
	Pleur. apyrenum	184.20
	Amaltheus gibbosus	185.12
	Amal. subnodosus	186.03
	Amal. stokesi	186.95
	Oistoceras figulinum	187.22
	Androgynoceras capricornus	187.48
	Andro. maculatum	187.75
	Beaniceras luridum	188.01
	Acanthopleuroceras valdani	188.28
	Tropidoceras masseanum	188.54
	Uptonia jamesoni	188.81
	Platypleuroceras brevispina	189.07
	Polymorphites polymorphus	189.34
	Phricodoceras taylori	189.60
	Paltechioceras aplanatum	190.01
	Leptechioceras macdonnelli	190.41
	Echioceras raricostatum	190.82
	Crucilobiceras densinodulum	191.22
	Oxynoticeras oxynotum	191.63
	Oxy. simpsoni	192.04
	Eparietites denotatus	192.44
	Asteroceras stellare	192.85
	Aster. obtusum	193.25
	Caenisites birchi	193.66
	Caenisites brooki	194.06
	Euagassiceras sauzeanum	194.47
	Agassiceras scipionianum	194.88
	Coroniceras charlesi	195.28
	Arietites bucklandi	195.69
	Coroniceras rotiforme	196.09
	Coron. conybeari	196.50
	Schlotheimia complanata	196.89
	Schlo. extranodosa	197.28
	Alsatites liasicus	197.66
	Alsa. laqueus	198.05
	Waehneroceras portlocki	198.44
	Caloceras johnstoni	199.21
	Psiloceras planorbis	199.60
	TOP	205.71
	5	206.57
	4	207.43
	3	208.29
	2	209.15
	1	210.01
	2	210.65
	1	211.30
	2	211.75
	1	212.20
	3	212.81
	2	213.41
	1	214.02
	2	215.27
	1	216.53
	TOP	217.59
	upper	219.81
	lower	220.95
	TOP	241.60
	Hollandites minor	242.22
	Tetsaoceras hayesi	243.05
	Buddhaites haugei	243.68
	Groenlandites nahwisi	243.93
	Arctohungarites bufonis	244.17
	TOP	248.08
	2	248.50
	1	248.92
	TOP	249.75
	3	249.91
	2	250.06
	1	250.22
	TOP	250.73
	upper	251.00
	lower	251.09


Boreal Ammonites	:	Boreal Substages	Boreal Zones	Boreal Subzones	_METACOLUMN_OFF		GTS2004 Jurassic chapter (original was compiled by Sven Backstrom, via Felix Gradstein, ~1995), and Groupe Francais d'etude du Jurassique (1997)

Boreal Substages	block	60	162/204/215	notitle
	TOP	136.49
	Ryazanian	142.84
	Upper Volgian	145.63	
	Middle Volgian	148.92
	Lower Volgian	150.63
	Kimmeridgian	155.65

Boreal Zones	block	150	162/204/215	notitle
	TOP	139.98
	Peregrinoceras albidum	140.24
	Surites tzikwinianus	141.25
	R. rjasenensis / S. spasskensis	141.66
	Hectoroceras kochi	142.16
	Chetaites sibiricus / Maynci	142.84
	Craspedites nodiger	144.46
	Crasp. subditus	145.63
	Kachpurites fulgens	146.16
	Paracraspedites oppressus	146.32
	Epivirgatites nikitini	147.03
	Virgatites virgatus	148.00
	Dorsoplanites panderi	148.92
	Ilowaiskya pseudoscythica	149.37
	Ilowa. sokolovi	150.02
	Ilowa. klimovi	150.63
	TOP	154	Dashed
	Amoebites kitcheni	155.10
	Amoeboceras bauhini	155.65
	Amoebo. rosenkrantzi	156.27
	Amoebo. regulare	156.84
	Prionodoceras serratum	157.15
	Amoeboceras glosense	158.06
	Cardioceras tenuiserratum	158.69
	Cardioceras densiplicatum	159.61
	TOP	212.20
	Pterosirenites obrucevi	216.53
	Sirenites yakutiensis	217.59
	Neosirenites pentastichus	222.70
	"Neoprotrachyceras" seimkanense	224.18
	"Protrachyceras" omkutchani	225.66
	Stolleyites tenuis	228.01
	Nathorstites lindstroemi	228.72
	Nath. mcconnelli	229.43
	Nath. mclearni	229.85
	Indigirites krugii	230.76
	Tsvetkorites neraensis	231.68
	Tsv. constantis	234.56
	Intornites oleshkoi	237.00
	Frechites nevadanus	239.00
	Gymnotoceras rotelliformis	241.60
	Arctohungarites kharaulakhensis	243.05
	Czekanowskites decipiens	243.68
	Lenotropites caurus	243.93
	Grambergia taimyrensis	245.17
	Olenekites spiniplicatus	245.53
	Parasiberites grambergi	246.63
	Nordophiceras contrarium	247.35
	Bajarunia euomphala	248.08
	Wassachites tardus	248.92
	Hedenstr. hedenstroemi	249.75
	Kingites? korostelevi	249.91
	Vavilovites turgidus	250.06
	Vav. sverdrupi	250.22
	[ un-named ]	250.38
	Wordieoceras decipiens	250.55
	Tompophiceras morphaeus	250.73
	Otoceras boreale	251.09
	[ un-named ]	251.21

Boreal Subzones	block	150	162/204/215	notitle
	TOP	142.84
	Craspedites kaschpuricus	143.65
	Cras. mosquensis	144.46
	TOP	146.32
	Epivirgatites nikitini	146.68
	Lomonossovella blakei	147.03
	Virgatites rosanovi	147.52
	Virg. virgatus	148.00
	Zaraiskites zarajskensis	148.39
	Pavlovia pavlovi	148.92
	TOP	154	Dashed
	Amoebites subkitcheni	155.1
	TOP	155.65
	Amoeboceras rosenkrantzi	155.96
	Amoebo. marstonense	156.27
	TOP	156.84
	Prionodoceras serratum	157.05
	Amoeboceras koldeweyense	157.15
	Amoeb. glosense	157.26
	Amoeb. ilovaiskii	158.06
	Cardioceras blakei	158.43
	Card. tenuiserratum	158.69
	Card. maltonense	158.94
	Cardioceras vertebrale	159.61
	TOP	212.20
	Wangoceras seimkanense	214.02
	Pinacoceras verkhoyanikum	216.53
	TOP	225.66
	Stolleyites tenuis	226.84
	Stolley. planus	228.01
	TOP	237.00
	Parafrechites sublaqueatus	237.67
	Frechites nevadanus	238.33
	Amphipopanoceras dzeginense	239.00
	Gymnotoceras olenekense	241.00
	Amphipopanoceras asseretoi	241.60
	Czekanowskites gastroplanus	242.22
	Arctohungarites laevigatus	243.05
	Arctoh. triformis	243.37
	Arctoh. ventroplanus	243.68
	TOP	243.93
	Lenotropites solitarius	244.17
	Stenopopanoceras mirabile	244.67
	Karangatites evolutus	244.92
	Karang. arkhipovi	245.17
	TOP	248.92
	Lepiskites kolymensis	249.33
	Hedenstr. hedenstroemi	249.75
	TOP	250.73
	Tompophiceras pascoei	250.91
	Otoceras boreale	251.09 

Boreal Sequences	sequence				off	Hardenbol, J., Jacquin, T., Vail, P.R., et al. (SEPM charts. 1998)
	Be3	SB	142.89	Medium	Just below (0.05 myr) base of R. runctoni Zone on SEPM chart.
		MFS	143.22	Medium	SEPM chart displays MFS as about 70% up in Seq. Be2 (Boreal) = 70% up in S. lamplughi Zone.
	Be2	SB	144.46	Minor	Base of S. lamplughi.  Regression peak of Portlandian trend, with widespread LST following (top of Portlandian).
		MFS	145.03	Medium	About 2/3rds up in Be1
	Be1	SB	146.16	Major	Base of S. primitivus Zone
		MFS	146.71	Minor	Base of T. anguiformis Zone
	Ti 6	SB	147.16	Medium	1/3 from top of Galbanites okusensis Zone
		MFS	147.76	Medium	Just below (0.05 myr) the top of P. albani Zone
	Ti 5	SB	148.20	Medium	Middle of Virgatopavlovia fittoni Zone
		MFS	148.66	Major	Base of Pavlovia rotunda Zone
	Ti 4	SB	148.92	Medium	Base of Pavlovia pallasioides Zone.
		MFS	149.15	Medium	Base of paravirgatus s.z. (middle of P. pectinatus Zone).    Transgression peak of Early Tithonian (British "upper Kimmeridge") trend.
	Ti 3	SB	149.66	Medium	Middle of reisiformis s.z. (lower Pectinatites hudlestoni Zone)
		MFS	149.76	Major	Base of Pectinatites hudlestoni Zone
	Ti 2	SB	150.02	Major	Base of Pectinatites (Virgatosphinctoides) wheatleyensis Zone.  Regression peak of lower Tithonian (in "upper Kimm" of British sense).
		MFS	150.40	Medium	3/4ths up in G. gravesiana s.z. (uppermost P. elegans Zone)
	Ti 1	SB	150.50	Major	Base of G. gravesiana s.z. (middle of Pectinatites elegans Zone)
		MFS	150.56	Major	Middle of G. gigas s.z. (lower Pectinatites elegans Zone)
	Kim 7	SB	150.73	Medium	Middle of irius s.z. (uppermost Aulacostephanus autissiodorensis Zone)
		MFS	150.90	Major	Base of irius s.z. (middle of Aulacostephanus autissiodorensis Zone).  Major Peak of Transgression that dominates Middle and Late Jurassic
	Kim 6	SB	151.37	Medium	Middle of contejeani s.z. (uppermost Aulacostephanus eudoxus Zone)
		MFS	151.57	Medium	Base of contegeani s.z. (1/3 from top of Aulacostephanus eudoxus Zone)
	Kim 5	SB	151.98	Medium	Base of caletanum s.z. (2/3 from top of Aulacostephanus eudoxus Zone)
		MFS	152.18	Medium	Middle of orthocera s.z. (lowermost A. eudoxus Zone)
	Kim 4	SB	152.77	Medium	Middle of lallierianum s.z. (1/4 from top of Aulacostephanoides mutabilis Zone)
		MFS	153.16	Medium	Base of lallierianum s.z. (middle of Aulacostephanoides mutabilis Zone)
	Kim 3 	SB	153.98	Medium	1/5th from top of chatellaionensis s.z. (nearly top of Rasenia cymodoce Zone)
		MFS	154.06	Medium	Middle of chatellaionensis s.z. (upper Rasenia cymodoce Zone)
	Kim 2	SB	154.45	Medium	Base of achilles s.z. (middle of Rasenia cymodoce Zone)
		MFS	154.97	Medium	Base of Rasenia cymodoce Zone
	Kim 1	SB	155.31	Minor	Middle of Pictonia baylei Zone
		MFS	155.65	Minor	Base of P. baylei Zone
	Ox8	SB	156.28	Medium	Middle of (Ringsteadia pseudocordata s.z. (middle of R. pseudocordata Zone)
		MFS	156.53	Medium	Base of (Ringsteadia pseudocordata s.z. (middle of R. pseudocordata Zone)
	Ox7	SB	156.82	Medium	2/3 from base of Ringsteadia caledonica s.z. (lower R. pseudocordata Zone)
		MFS	156.86	Minor	1/3 from base of Ringsteadia caledonica s.z. (lower R. pseudocordata Zone)
	Ox6	SB	157.04	Major	Base of P. variocostatus s.z. (middle of P. cautisnigrae Zone).  Regression peak of middle Oxfordian trend.
		MFS	157.70	Minor	Middle of P. nunningtonense s.z. (upper P. pumilus)
	Ox5	SB	158.24	Medium	2/3 from base of Perisphinctes parandieri s.z. (lower P. pumilus Zone)
		MFS	158.34	Minor	1/3 from base of Perisphinctes parandieri s.z. (lower P. pumilus Zone)
	Ox4	SB	158.67	Medium	80% up in Perisphinctes plicatilis Zone
		MFS	159.14	Minor	40% up in Perisphinctes plicatilis Zone
	Ox3	SB	159.38	Medium	20% up in Perisphinctes plicatilis Zone
		MFS	159.61	Medium	Base of Perisphinctes plicatilis Zone
	Ox2	SB	160.06	Medium	Middle of  Cardioceras costicardia  s.z. (middle of C. cordatum Zone)
		MFS	160.46	Medium	Middle of Cardioceras bukowskii s.z. (lower C. cordatum Zone).  Peak of early Oxf Transgression.
	Ox1	SB	160.89	Medium	Base of Cardioceras praecordatum s.z. (middle of Q. mariae Zone)
		MFS	161.05	Medium	Middle of Cardioceras praecordatum s.z. (lower Q. mariae Zone)
	Ox0	SB	161.21	Minor	Base of Q. mariae Zone (base of Oxfordian)
		MFS	161.51	Major	Middle of Quenstedtoceras lamberti s.z. (upper Q.  lamberti Zone)
	Call5	SB	162.01	Medium	Base of Quenstedtoceras lamberti zone.  Regression peak of Callovian trend.
		MFS	162.43	Medium	Middle of Kosmoceras phaeinum s.z.  (lower P. athleta Zone)
	Call4	SB	162.60	Medium	Middle of Kosmoceras grossouvrei s.z. (upper E. coronatum Zone)
		MFS	162.95	Medium	Middle of Kosmoceras jason s.z. (upper K. jason Zone)
	Call3	SB	163.20	Medium	Base of Kosmoceras jason Zone
		MFS	163.46	Minor	Middle of Sigaloceras calloviense s.z. (lower S. calloviense Zone)
	Call2	SB	163.71	Medium	Base of galilaei s.z. (uppermost P. koenigi Zone)
		MFS	163.88	Medium	Middle of curtilobus s.z. (middle of P. koenigi Zone).  Transgression peak of Late Bathonian-Early Callovian trend.
	Call1	SB	164.28	Medium	Just below (0.05 myr) the base of gowerianus s.z. (top of M. herveyi Zone)
		MFS	164.40	Medium	Base of M. kamptus s.z. (middle of M. herveyi Zone)
	Call0	SB	164.74	Minor	Base of M. herveyi Zone (base of Callovian)
		MFS	164.80	Minor	2/3 up in Clydoniceras discus s.z. (top of C. discus Zone)
	Bat5	SB	164.93	Major	Base of Clydoniceras discus s.z. (middle of C. discus Zone)
		MFS	165.13	Medium	Base of Clydoniceras discus Zone
	Bat4	SB	165.47	Medium	Just above (0.05 myr) the base of O. orbis Zone
		MFS	165.88	Medium	40% up in P. hodsoni Zone
	Bat3	SB	166.21	Medium	Base of wagnericeras s.z. (middle of Morrisiceras morrisi Zone).  Peak Regression of Early Bathonian trend.
		MFS	166.50	Medium	Base of Tulites subcontractus Zone
	Bat2	SB	166.70	Medium	Middle of Procerites (or Procentes) progracilis zone
		MFS	166.89	Minor	Base of Procerites (or Procentes) progracilis zone
	Bat1	SB	167.09	Medium	Base of tenuiplicatus s.z. (upper Z. zigzag Zone)
		MFS	167.48	Major	Base of macrescens s.z. (lower Z. zigzag Zone).  Peak Transgression of Bajocian-lowermost Bathonian trend.
	Bj5	SB	167.87	Major	Base of P. bomford s.z. (upper Parkinsonia parkinsoni Zone)
		MFS	168.14	Major	2/3rds up in P. acris s.z. (lower Parkinsonia parkinsoni Zone)
	Bj4	SB	169.00	Medium	Just above (0.05 myr) base of schroederi s.z. (upper S. niortense Zone).  Extended lowstand follows this SB.
		MFS	169.15	Medium	Middle of G. baculata s.z. (middle of Strenoceras niortense Zone)
	Bj3	SB	169.84	Major	Base of T. blagdeni s.z.  (upper S. humpriesianum Zone). Extended lowstand follows this SB.
		MFS	170.03	Major	Base of S. humpriesianum s.z. (middle of S. humpriesianum Zone)
	Bj2	SB	170.52	Medium	Middle of E. sauzei s.z. (lower S. propinguans Zone)
		MFS	170.95	Minor	"1/3rd up in "lower" W. laeviuscula s.z. (middle of Witchellia laeviuscula Zone)"
	Bj1	SB	171.60	Major	Base of H. discites Zone (base of Bajocian).  Extended lowstand follows this SB.
		MFS	172.04	Medium	Base of G. formosus s.z. (middle of Graphoceras concavum Zone)
	Aa2	SB	173.38	Major	Base of B. bradfordensis Zone.  Extended lowstand follows this SB.  Culmination of major Regression trend of late-Early Jurassic.
		MFS	173.82	Minor	Base of L. murchisonae s.z. (upper Ludwigia murchisonae Zone)
	Aa1	SB	174.93	Major	Middle of bifidatum s.z. (upper Leioceras opalinum Zone). Extended lowstand follows this SB.
		MFS	175.16	Minor	Base of bifidatum s.z. middle of Leioceras opalinum Zone).
	Toa7	SB	176.09	Medium	Middle of Pleydellia aalensis Zone
		MFS	176.58	Medium	Base of Pleydellia aalensis Zone
	Toa6	SB	178.30	Medium	1/4th up in D. dispansum s.z. (lower D. levesquei Zone).  Extended lowstand follows this SB.
		MFS	178.79	Minor	Middle of Pseudogrammoceras fallaciosum s.z. (upper Grammoceras thouarsense Zone)
	Toa5	SB	179.62	Medium	60% up in G. striatulum s.z. (middle of G. thouarsense Zone)
		MFS	180.63	Medium	Base of illustris s.z. (lower Haugia variabilis Zone)
	Toa4	SB	180.95	Medium	Base of P. fibulatum s.z. (middle of H. bifrons Zone).  Extended lowstand follows this SB.
		MFS	181.05	Major	Just below (0.1 myr) below Tao4 SB 
	Toa3	SB	181.12	Minor	1/3rd up in commune s.z. (lower H. bifrons Zone)
		MFS	181.70	Major	Middle of Harpoceras falciferum s.z. (upper H. falciferum Zone).  Peak of Early Jurassic Transgression.
	Toa2	SB	182.30	Medium	Just below (0.1 myr) the base of H. falciferum  s.z. (middle of H. falciferum Zone)
		MFS	182.45	Major	Middle of H. exaratum s.z. (lower H. falciferum Zone)
	Toa1	SB	182.74	Minor	Middle of D. semicelatum s.z. (upper D. tenuicostatum Zone)
		MFS	182.89	Medium	Middle of D. clevelandicum s.z. (middle of D. tenuicostatum Zone)
	PI 8	SB	183.10	Medium	0.1 myr below base of Toarcian =  Peak lowstand at Pliensbachian/Toarcian boundary
		MFS	183.80	Medium	Just above (0.1 myr) the middle of P. apyrenum s.z. (lower Pleuroceras spinatum Zone)
	PI 7	SB	184.66	Medium	Middle of A. gibbosus s.z. (upper Amaltheus margaritatus Zone)
		MFS	185.58	Minor	Middle of A. subnodosus s.z. (middle of Amaltheus margaritatus Zone)
	PI 6	SB	186.03	Minor	Base of A. subnodosus s.z. (middle of Amaltheus margaritatus Zone)
		MFS	186.24	Minor	3/4 up in PI 5 sequence;  Peak of relatively brief Transgression in mid-Pliensbachian (Boreal realm only)
	PI 5	SB	186.85	Minor	Just above (.1 myr) the base of Amaltheus margaritatus zone
		MFS	186.95	Minor	Base of Amaltheus margaritatus zone.
	PI 4	SB	187.08	Minor	Middle of Oistoceras figulinum s.z (upper Prodactylioceras davoei Zone).  Peak Regression of a relatively brief mid-Pliensbachian trend.
		MFS	187.32	Medium	1/3rd up in Pl 3 sequence.
	PI 3	SB	187.43	Medium	Just above (0.05 myr) the base of capricornus s.z. (lower P. davoei Zone)
		MFS	187.75	Medium	Base of P. davoie Zone
	PI 2	SB	188.45	Major	1/3rd up in T. massenum s.z. (just above base of T. ibex Zone).  Extended lowstand follows this SB.
		MFS	188.72	Medium	1/3rd up in Uptonia jamesoni s.z. (upper Uptonia jamesoni Zone)
	PI 1	SB	189.16	Medium	2/3rds up in P. polymorphus s.z. (middle of U. jamesoni Zone)
		MFS	189.34	Major	Base of P. polymorphus s.z. (middle of U. jamesoni Zone).  Peak of Late Sinemurian Transgression trend.
	Si 5	SB	190.01	Medium	Base of Paltechioceras aplanatum s.z. (upper E. raricostatum Zone)
		MFS	190.55	Major	2/3rds up in E. raricostatum s.z. (middle E. raricostatum Zone)
	Si 4	SB	191.63	Medium	Base of O. oxynotum s.z. (middle of Oxynoticeras oxynotum Zone). Extended lowstand follows this SB.
		MFS	192.04	Medium	Base of Oxynoticeras oxynotum Zone
	Si 3	SB	193.35	Major	0.1 myr below base of A. obtusum Zone.  Peak Regression of relatively brief middle-Sinemurian trend.
		MFS	193.79	Medium	2/3rds up in Caenisites turneri s.z. (lower C. turneri Zone) 
	Si 2	SB	194.47	Medium	Base of E. sauzeanum s.z. (upper A. semicostatum Zone)
		MFS	194.88	Medium	Base of A. scipionianum s.z. (middle of A. semicostatum Zone). Peak Transgression of earliest Jurassic trend.
	Si 1	SB	195.49	Medium	Middle of Arietites bucklandi subzone (upper Arietites bucklandi Zone)
		MFS	196.09	Medium	Base of C. rotiforme s.z. (lower A. bucklandi Zone)
	He3	SB	196.89	Medium	Base of S. complanata s.z. (middle of S. angulata Zone)
		MFS	198.05	Major	Base of Alsatites laqueus s.z. (middle of A. liasicus Zone)
	He2	SB	198.44	Medium	Base of A. liasicus Zone
		MFS	199.02	Medium	Middle of P. planorbis zone (middle of Caloceras johnstoni s.z.)
	He 1.1	SB	199.21	Minor	Base of Caloceras johnstoni s.z. (lower Psiloceras planorbis Zone)
		MFS	199.41	Minor	Middle of He1 sequence
	He 1	SB	199.60	Minor	Base of Psiloceras planorbis Zone (= base of Jurassic).  Peak Regression of uppermost Triassic (Boreal only).

Boreal T-R Cycles	trend				off	Hardenbol, J., Jacquin, T., Vail, P.R., et al. (SEPM charts. 1998)
	Be2	SB	144.46	Major	Base of S. lamplughi.  Regression peak of Portlandian trend, with widespread LST following (top of Portlandian).
		MFS	149.15	Minor	Base of paravirgatus s.z. (middle of P. pectinatus Zone).    Transgression peak of Early Tithonian (British "upper Kimmeridge") trend.
	Ti 2	SB	150.02	Minor	Base of Pectinatites (Virgatosphinctoides) wheatleyensis Zone.  Regression peak of lower Tithonian (in "upper Kimm" of British sense).
		MFS	150.90	Major	Base of irius s.z. (middle of Aulacostephanus autissiodorensis Zone).  Major Peak of Transgression that dominates Middle and Late Jurassic
	Ox6	SB	157.04	Medium	Base of P. variocostatus s.z. (middle of P. cautisnigrae Zone).  Regression peak of middle Oxfordian trend.
		MFS	160.46	Medium	Middle of Cardioceras bukowskii s.z. (lower C. cordatum Zone).  Peak of early Oxf Transgression.
	Call5	SB	162.01	Medium	Base of Quenstedtoceras lamberti zone.  Regression peak of Callovian trend.
		MFS	163.88	Medium	Middle of curtilobus s.z. (middle of P. koenigi Zone).  Transgression peak of Late Bathonian-Early Callovian trend.
	Bat3	SB	166.21	Major	Base of wagnericeras s.z. (middle of Morrisiceras morrisi Zone).  Peak Regression of Early Bathonian trend.
		MFS	167.48	Major	Base of macrescens s.z. (lower Z. zigzag Zone).  Peak Transgression of Bajocian-lowermost Bathonian trend.
	Aa2	SB	173.38	Major	Base of B. bradfordensis Zone.  Extended lowstand follows this SB.  Culmination of major Regression trend of late-Early Jurassic.
		MFS	181.70	Major	Middle of Harpoceras falciferum s.z. (upper H. falciferum Zone).  Peak of Early Jurassic Transgression.
	PI 8	SB	183.10	Medium	0.1 myr below base of Toarcian =  Peak lowstand at Pliensbachian/Toarcian boundary
		MFS	186.24	Minor	3/4 up in PI 5 sequence;  Peak of relatively brief Transgression in mid-Pliensbachian (Boreal realm only)
	PI 4	SB	187.08	Minor	Middle of Oistoceras figulinum s.z (upper Prodactylioceras davoei Zone).  Peak Regression of a relatively brief mid-Pliensbachian trend.
		MFS	189.34	Minor	Base of P. polymorphus s.z. (middle of U. jamesoni Zone).  Peak of Late Sinemurian Transgression trend.
	Si 3	SB	193.35	Minor	0.1 myr below base of A. obtusum Zone.  Peak Regression of relatively brief middle-Sinemurian trend.
		MFS	194.88	Medium	Base of A. scipionianum s.z. (middle of A. semicostatum Zone). Peak Transgression of earliest Jurassic trend.


Tethyan Ammonites	:	Tethyan Zone	Tethyan Subzone		CRETACEOUS = Thierry et al. (in Hardenbol et al., SEPM charts, 1998), with GTS2004 revisions; JURASSIC = Groupe Francais d'etude du Jurassique (1997); TRIASSIC = Mietto and Manfrin (in Hardenbol et al., SEPM charts, 1998), with GTS2004 and Kozur (2005) revisions.

Tethyan Zone	block	180	236/204/215	notitle
	TOP	65.50
	Anapachydiscus terminus	66.50
	Anapachydiscus fresvillensis	69.23
	Pachydiscus neubergicus to Pachy. epiplectus	70.60
	Nostoceras hyatti	71.30
	Didymoceras cheyennense	75.05
	Bostrychoceras polyplocum	80.50
	Hoplitoplacenticeras marroti / vari	80.64
	Delawarella delawarensis	81.63
	Placenticeras bidorsatum	83.53
	Placent. polyopsis	85.85
	Paratexanites serratomarginatus	86.96
	Gauthiericeras margae	87.77
	Peroniceras tridorsatum	88.58
	Same as Boreal (NW Europe)	112.00
	Hypacanthoplites jacobi	113.00
	Nolaniceras nolani	115.00
	Parahoplites melchioris	118.00
	Epicheloniceras subnodosocostatum	121.00
	Dufrenoyia furcata	121.90
	Deshayesites deshayesi	122.93
	Deshay. weissi	123.97
	Deshay. oglanlensis	125.00
	Pseudocrioceras waagenoides	125.55
	Colchidites sarasini	126.10
	Imerites giraudi	126.65
	Hemihoplites feraudianus	127.20
	Gerhardtia sartousi	127.75
	Ancyloceras vandenheckii	128.30
	Coronites darsi	128.63
	Kotetishvilia compressissima	128.97
	Nicklesia pulchella 	129.30
	Nick. nicklesi	129.64
	Spitidiscus hugii	129.97
	Pseudothurmannia ohmi	131.91
	Pseudoth. balearis	132.56
	Pleisiospitidiscus ligatus	133.21
	Subsaynella sayni	133.85
	Lyticoceras nodosoplicatus	134.50
	Crioceratites loryi	135.80
	Acanthodiscus radiatus	136.44
	Criosarasinella furcillata	137.27
	Neocomites peregrinus	138.11
	Saynoceras verrucosum	138.94
	Busnardoites campylotoxus	139.77
	Tirnovella pertransiens	140.18
	Thurmanniceras otopeta	140.66
	Subthurmannia boissieri	142.30
	Subthurm. occitanica	143.68
	Berriasella jacobi	145.46
	Durangites	146.14
	Micracanthoceras microcanthum	147.16
	Micra. ponti / Burckhardticeras peroni	147.47
	Semiformiceras fallauxi	148.98
	Semiform. semiforme	149.44
	Semiform. darwini	149.89
	Hybonoticeras hybonotum	150.84
	Hybonoticeras beckeri	152.20
	Aulacostephanus eudoxus	152.59
	Aspidoceras acanthicum	153.06
	Crussoliceras divisum	153.39
	Ataxioceras hypselocyclum	154.14
	Sutneria platynota	154.53
	Idoceras planula	155.35
	Epipeltoceras bimammatum	156.81
	Perisphinctes bifurcatus	157.40
	Gregoryceras transversarium	158.43
	Perisphinctes plicatilis	159.61
	Cardioceras cordatum	160.66
	Quenstedtoceras mariae	161.21
	Quenstedtoceras lamberti	162.01
	Peltoceras athleta	162.35
	Erymnoceras coronatum	162.86
	Reineckeia anceps	163.20
	Macrocephalites gracilis	164.23
	Bullatimorphites bullatus	164.74
	Clydoniceras discus	165.13
	Hecticoceras retrocostatum	165.72
	Cadomites bremeri	166.11
	Morrisiceras morrisi	166.31
	Tulites subcontractus	166.50
	Procerites progracilis	166.89
	Procerites aurigerus	167.29
	Zigzagiceras zigzag 	167.68
	Parkinsonia parkinsoni	168.27
	Garantiana garantiana	168.86
	Strenoceras niortense	169.64
	Stephanoceras humphriesianum	170.23
	Sonninia propinquans	170.62
	Witchellia laeviuscula	171.21
	Hyperlioceras discites	171.60
	Graphoceras concavum	172.49
	Brasilia bradfordensis	173.38
	Ludwigia murchisonae	174.71
	Leioceras opalinum	175.60
	Pleydellia aalensis	176.58
	Dumortieria pseudoradiosa	177.56
	Phlyseogrammoceras dispansum	178.54
	Grammoceras thouarsense	180.50
	Haugia variabilis	180.70
	Hildoceras bifrons	181.20
	Harpoceras serpentinum	182.70
	Dactylioceras tenuicostatum	183.00
	Emaciaticeras emaciatum	183.80
	Arieticeras algovianum	185.12
	Fuciniceras lavinianum	186.95
	Prodactylioceras davoei	187.75
	Tragophylloceras ibex	188.41
	Uptonia jamesoni	189.60
	Echioceras raricostatum	191.22
	Oxynoticeras oxynotum	192.04
	Asteroceras obtusum	193.25
	Caenisites turneri	194.06
	Arnioceras semicostatum	195.28
	Arietites bucklandi	196.50
	Schlotheimia angulata	197.28
	Alsatites liasicus	198.44
	Psiloceras planorbis	199.60
	Choristoceras marshi	202.29
	Rhabdoceras suessi	205.71
	Halorites macer	207.57
	Himavatites hogarti	210.01
	Cyrtopleurites bicrenatus	211.30
	Juvavites magnus	212.20
	Malayites paulckei	214.02
	Guembelites jandianus 	216.53
	Anatropites spinosus	218.66
	Tropites subbullatus	220.95
	Tropites dilleri	222.70
	Austrotrachyceras austriacum	225.66
	Trachyceras	228.73
	Protrachyceras	234.56
	Eoprotrachyceras curionii	237.00
	Nevadites	240.00
	Hungarites	241.00
	Paraceratites	241.60
	Balatonites balatonicus	242.49
	Kocaelia	243.68
	Paracrochordiceras	245.17
	[ un-named ]	245.53
	Toziceras pakistanum	246.63
	Tirolites cassianus	248.08
	(mixed assemblage)	248.92
	Meekoceras gracilitatis	249.75
	Flemingites rohilla	250.22
	Gyronites frequens	250.38
	Ophiceras connectens + Oph. tibeticum	250.73
	Otoceras woodwardi	251.09
	Otoceras concavum	251.21
	Pseudotirolites	251.70
	Paratirolites	252.23

Tethyan Subzone	block	150	236/204/215	notitle	off
	TOP	83.53
	Eupachydiscus isculensis	84.69
	Texanites gallicus / texanus	85.85
	TOP	113.00
	Hypacanthoplites rubricosus	114.00
	Diodochoceras nodosocostatum	115.00
	TOP	136.44
	Teschenites callisdiscus	136.86
	Criosarasinella furcillata	137.27
	Olcostephanus nicklesi	137.69
	Neocomites peregrinus	138.11
	Karakaschiceras pronecostatum	138.52
	Saynoceras verrucosum	138.94
	(upper s.z.)	139.35
	(lower s.z.)	139.77
	TOP	140.66
	Tirnovella alpillensis	141.25
	Berriasella picteti	141.55
	Malbosiceras paramimounum	142.30
	Dalmasiceras dalmasi	142.63
	Berriasella privasensis	142.96
	Subthurmannia subalpina	143.68
	Pseudosubplanites grandis	144.82
	Berriasella jacobi	145.46	
	TOP	146.14
	Paraulacosphinctes transitorius	146.96
	Simplisphinctes	147.16
	TOP	147.47
	Simolytoceras admirandum / S. biruncinatum	148.24
	Richterella richteri	148.98
	TOP	149.44
	Franconites vimineus	149.66
	triplicatus	149.89
	TOP	150.84
	Virgataxioceras setatum	151.30
	Sutneria submeula	151.75
	Sutneria pedinopleura	152.20
	TOP	153.06
	Aspidoceras uhlandi	153.23
	Crussoliceras divisum	153.39
	Ataxioceras lothari	153.77
	Parataxioceras hippolytense	154.14
	Ataxioceras guilherandense	154.16
	Ortho. desmoides	154.24
	Orthosphinctes polygyratus	154.53
	Sutneria galar	154.94
	Idoceras planula	155.35
	Taramelliceras hauffianum	155.62
	Epipeltoceras bimammatum	156.09
	Epipelt. berrense	156.45
	Epipelt. semimammatum	156.81
	Perisphinctes grossouvrei	157.27
	Peri. stenocycloides	157.40
	Perisphinctes rotoides	157.73
	Larcheria schilli	157.90
	Perisphinctes luciaeformis	158.09
	Perisphinctes parandieri	158.43
	P. antecedens (C. tenuiserratum ssz)	158.69
	P. ant. (C. maltonense ssz)	158.94
	Cardioceras vertebrale	159.61
	Cardioceras cordatum	159.85
	Cardioceras costicardia	160.27
	Cardioceras bukowskii	160.66
	Card. praecordatum	160.89
	Card. scarburgense	161.21
	Quenstedtoceras lamberti	161.81
	Orionoides poculum	162.01
	Collotia collotiformis	162.18
	Hecticoceras trezeense	162.35
	Rehmannia (L.) rota	162.52
	Erymnoceras leuthardti	162.69
	Erymnoceras baylei	162.86
	Reineckeia tyranniformis	163.03
	Reineckeia stuebeli	163.20
	Indosphinctes patina	163.37
	Hecticoceras (Chan.) michalskii	163.71
	Rehmannia laugieri	163.88
	Reineckeia (Tyr.) pictava	164.06
	Rehmannia grossouvrei	164.11
	Bullat. (Bom.) prahecquense	164.23
	TOP	164.74
	Clydoniceras discus	164.93
	Clyd. hollandi 	165.13
	Bullat. (Kh.) hannoveranus	165.33
	Hecticoceras (Prohect.) blanazense	165.72
	Wagnericeras fortecostatum	165.91
	Bullat. bullatimorphus	166.11
	TOP	166.50
	Procerites progracilis	166.70
	Cadomites orbignyi	166.89
	Asphinctites tenuiplicatus	167.09
	Asphinctites recinctus	167.29
	Morphoceras macrescens	167.48
	Morph. parvum	167.68
	Parkinsonia bomfordi	167.87
	Park. densicostata	168.07
	Park. acris	168.27
	Garantiana tetragona	168.46
	Garant. subgaranti	168.66
	Garant. dichotoma	168.86
	Orthogarant. schroederi	169.05
	Garantiana baculata	169.25
	Caumontisphinctes polygiralis	169.44
	Teloceras banksi	169.64
	Telo. blagdeni	169.84
	Stephanoceras humphriesianum	170.03
	Dorsetensia romani	170.23
	Dorsetensia hebridica	170.42
	Emileia sauzei	170.62
	Witchellia laeviuscula	171.01
	Euhoploceras (F.) ovalis	171.21
	Hyperlioceras subsectum	171.40
	Hyperlioceras walkeri 	171.60
	Graphoceras formosum	172.04
	Graph. concavum	172.49
	Brasilia gigantea	172.93
	Brasilia bradfordensis	173.38
	Ludw. murchisonae	173.82
	Ludwigia haugi	174.71
	Leioceras bifidatum	175.16
	Leioceras opalinum	175.60
	Pleydellia fluitans	176.09
	Pleydellia mactra	176.58
	Dumortieria pseudoradiosa	177.07
	Dumor. levesquei	177.56
	Gruneria gruneri	178.05
	Hammatoceras insigne	178.54
	Pseudogrammoceras fallaciosum	179.03
	Grammoceras striatulum	180.50
	Brodieia alticarinatus	180.63
	Colina gemma	180.70
	Hildoceras semipolitum	180.83
	Hild. bifrons	180.95
	Hild. lusitanicum	181.08
	Hild. sublevisoni	181.20
	Harpoceras falciferum	181.70
	Hildaites pseudoserpentinum	182.20
	Harpoceras strangewaysi	182.70
	Dactylioceras semicelatum	182.93
	Protogrammoceras paltus	183.00
	elisa	183.60
	Pleuroceras solare	183.80
	levidorsatum / meneghini	184.20
	acuratum	184.51
	Ariet. bertrandi / Reynesoceras ragazzoni	185.12
	cornacaldense	186.03
	portisi	186.95
	Oistoceras figulinum	187.22
	Androgynoceras capricornus	187.48
	Andro. maculatum	187.75
	Beaniceras luridum	188.01
	Metaderoceras beirense	188.14
	Dayiceras renzi	188.41
	Uptonia jamesoni	188.94
	Platypleuroceras brevispina	189.20
	Phricodoceras taylori	189.60
	Paltechioceras aplanatum	190.01
	Leptechioceras macdonnelli	190.41
	Echioceras raricostatum	190.82
	Crucilobiceras densinodulum	191.22
	Oxynoticeras oxynotum	191.63
	Oxy. simpsoni	192.04
	Eparietites denotatus	192.44
	Asteroceras stellare	192.85
	Aster. obtusum	193.25
	Caenisites bordoti	193.66
	Caenisites turneri	194.06
	Euagassiceras sauzeanum	194.47
	Agassiceras scipionianum	194.88
	Coroniceras charlesi	195.28
	Arietites bucklandi	195.69
	Coroniceras rotiforme	196.09
	Coron. conybeari	196.50
	Schlotheimia complanata	196.89
	Schlo. extranodosa	197.28
	Alsatites liasicus	197.66
	Alsa. laqueus	198.05
	Waehneroceras portlocki	198.44
	Caloceras torus	198.83
	Caloceras johnstoni	199.21
	Psiloceras planorbis	199.60
	Choristoceras marshi	200.95
	Vandaites stuerzenbaumi	202.29
	Sagenites reticulatus	203.64
	Sagenites quinquepunctatus	205.71
	unnamed s.z.	206.64
	Amarassites semiplicatus	207.57
	Himavatites hogarti 	208.79
	Himavatites watsoni 	210.01
	TOP	212.20
	unnamed s.z.	212.81
	Malayites paulckei	213.41
	Malayites tingriensis	214.02
	Dimorphites selectus	215.27
	Dimorphites n.sp.1	216.53
	Gonionotites italicus	217.59
	Discotropites plinii	218.66
	Tropites subbullatus	219.81
	Projuvavites crasseplicatus	220.95
	TOP	222.70
	Neoprotrachyceras	224.18
	Austrotrachyceras triadicum	225.66
	Trachyceras aonoides	226.94
	Trachyceras aon	228.01
	Daxatina cf. canadensis	228.73
	Frankites regoledanus	229.43
	Protrachyceras neumayri	230.27
	Protrachy. longobardicum	231.68
	Eoprotrachyceras gredleri	233.34
	Protrachyceras margaritosum	234.56
	Anolcites recubariensis	235.78
	Eoprotrachyceras curionii	237.00
	Chieseiceras chiesense	238.00
	Serpianites serpianensis	239.00
	Ticinites crassus	240.00
	Aplococeras avisianum	240.33
	Reitziites reitzi	241.00
	Paraceratites trinodosus	241.30
	Schreyerites abichii	241.60
	Schr. binodosus	241.89
	Bal. balatonicus	242.19
	Cuccoceras cuccense	242.49
	"unnamed"	242.79
	Aghdarbandites ismidicus	243.08
	"unnamed"	243.38
	Nicomedites osmani	243.68
	TOP	250.73
	Ot. woodwardi (upper)	251.00
	Ot. woodwardi (lower)	251.09


Ammonites of North American Western Interior	:	W. Interior Zones	Close-spaced Zones	_METACOLUMN_OFF		W.A. Cobban (in Hardenbol et al., SEPM charts, 1998), with GTS2004 revisions.

W. Interior Zones	block	180	239/212/180	notitle
	TOP	65.50
	[Few usable ammonites]	67.88
	Jeletzkytes nebrascensis	68.33
	Hoploscaphites nicolleti	68.78
	Hopl. birkelundi	69.23
	Baculites clinolobatus	69.68
	Bac. grandis	70.11
	Bac. baculus	70.56
	Bac. eliasi	71.04
	Bac. jenseni	71.56
	Bac. reesidei	72.14
	Bac. cuneatus	72.78
	Bac. compressus	73.50
	Didymoceras cheyennense	74.28
	Exiteloceras jenneyi	75.05
	Didy. stevensoni	75.74
	Didy. nebrascense	76.38
	Baculites scotti	77.00
	Bac. gregoryensis	77.59
	Bac. perplexus (late)	78.15
	Bac. gilberti to Bac. obtusus zones	80.64
	Bac. sp. (weak flank ribs)	80.91
	Bac. sp. (smooth)	81.22
	Scaphites hippocrepis III	81.63
	Scaph. hippocrepis II	82.20
	Scaph. hippocrepis I	82.89
	Scaph. leei III	83.53
	Desmoscaphites bassleri to Clioscaphites vermiformis (4 zones)	84.94
	Clio. saxitonianus	85.85
	Scaphites depressus	86.96
	Scaph. ventricosus	87.88
	Forresteria alluaudi - Scaph. preventricosus	88.58
	Forr. peruana	89.07
	Prionocyclus germari to Prion. macombi (6 zones)	90.48
	Prion. hyatti	90.94
	Prion. percarinatus	91.51
	Collignoniceras woollgari	92.13
	Mammites nodosoides	92.70
	Vascoceras birchbyi	93.15
	Pseudaspidoceras flexuosum	93.41
	Watinoceras devonense	93.55
	Nigericeras scotti to Conlinoceras gilberti (15 zones)	96.01
	[blank]	97.35
	Neogastroplites maclearni to Neogast. haasi (5 zones)	98.83

Close-spaced Zones	block	180	239/212/180	notitle
	Top	78.15
	Bac. gilberti	78.68
	Bac. perplexus (early)	79.16
	Bac. sp. (smooth)	79.61
	Bac. asperiformis	80.00
	Bac. maclearni	80.35
	Bac. obtusus	80.64
	Top	83.53
	Desmoscaphites bassleri	83.99
	Desmo. erdmanni	84.31
	Clioscaphites choteauensis	84.62
	Clio. vermiformis	84.94
	Top	89.07
	Prionocyclus germari	89.40
	Scaphites nigricollensis	89.63
	Scaph. whitfieldi	89.79
	Scaph. ferronensis	89.96
	Scaph. warreni	90.17
	Prionocyclus macombi	90.48
	Top	93.55
	Nigericeras scotti	93.60
	Neocardioceras juddii	93.64
	Burroceras clydense	93.72
	Sciponoceras gracile (Euomphaloceras septemseriatum)	93.85
	S. gracile (Vascoceras diartianum)	94.01
	Dunveganoceras conditum	94.19
	Dunv. albertense	94.38
	Dunv. problematicum	94.57
	Calycoceras canitaurinum - Dunv. pondi	94.75
	Plesiacanthoceras wyomingsense	94.91
	Acanthoceras amphibolum	95.06
	Acanth. bellense	95.23
	Acanth. muldoonense	95.43
	Acanth granerosense	95.68
	Conlinoceras tarrantense - Con. gilberti	96.01
	TOP	97.35
	Neogastroplites maclearni	97.75
	Neogast. americanus	98.11
	Neogast. muelleri	98.41
	Neogast. cornutus	98.64
	Neogast. haasi	98.83
	Neostingloceras carcitanense s.z. (Europe)	99.54

Paleozoic Ammonoids	:	Numbered zone	Zone name	Boreal zone (Perm Cis-Urals)	Low-latitude Permian zone	Devonian geno-subzone	Devonian numbered subzones	Devonian subzone name	Ammonoid major marker		PERMIAN = Kozur (2003), Davydov et al., 2004, and Henderson (2005); CARBONIFEROUS = GTS2004 diagram (Davydov et al., 2004), DEVONIAN = Becker and House (2000)

Numbered zone	block	50	236/204/215	notitle		PERMIAN-CARBONIFEROUS = Davydov (GTS2004); DEVONIAN = Becker and House (2000)
	TOP	251.00
	La3	253.52
	La2	256.44
	La1	260.40
	Ga4	265.80
	Ga3	266.68
	Ga2	269.30
	Ga1	270.60
	Ca6	273.10
	Ca5	275.60
	Ca4	277.80
	Ca3	284.40
	Ca2	292.56
	Ca1	298.80
	Pa12	301.21
	Pa11	303.90
	Pa10	306.50
	Pa9	307.28
	Pa8	309.10
	Pa7	310.92
	Pa6	311.70
	Pa5	312.66
	Pa4	313.94
	Pa3	316.18
	Pa2	316.82
	Pa1	318.52
	Ma8	324.33
	Ma7	326.40
	Ma6	335.85
	Ma5	342.47
	Ma4	345.30
	Ma3	350.86
	Ma2	357.12
	Ma1	359.20
	VI	363.48
	V	364.84
	IV	366.34
	III	368.07
	II	374.50
	I	385.30
	III	388.69
	II	392.01
	I	397.50
	IV	401.95
	III	407.00
	II	412.16

Zone name	block	150	236/204/215			PERMIAN-CARBONIFEROUS = Davydov (GTS2004); DEVONIAN = Becker and House (2000)
	TOP	251.00
	Iranites	253.52
	Araxoceras	256.44
	Roadoceras, Doulingoceras	260.40
	Timorites	265.80
	Waagenoceras	269.30
	Aktubinskia, Artinskia, Neopronorites	284.40
	Sakmarites	292.56
	Svetlanoceras	298.80
	Shumardites	301.21
	Aristoceras / Vidrioceras	303.90
	Parashumardites / Dunbarites	306.50
	Foschistoceras	307.28
	Pseudoparalegoceras	309.10
	Paralegoceras / Eowellerites	310.92
	Diaboloceras / Winslovoceras	311.70
	Diaboloceras / Axinolobus	312.66
	Branneroceras / Gastrioceras	313.94
	Bullingites / Concelloceras	316.18
	Bashkortoceras / Reticuloceras	316.82
	Homoceras / Hudzonoceras	318.52
	Delepinoceras / Fayetteviella	324.33
	Cravenoceras / Uralopronorites	326.40
	Hypergoniatites / Ferganoceras	335.85
	Beyrichoceras / Goniatites	342.47
	Merocanites / Ammonellipsites	345.30
	Protocanites / Pericyclus	350.86
	Protocanites / Gattendorfia	357.12
	Acutimitoceras	359.20
	Wocklumeria	363.48
	Clymenia	364.84
	Platyclymenia	366.34
	Prolobites	368.07
	Cheiloceras	374.50
	Manticoceras	385.30
	Pharciceras	388.69
	Maenioceras	392.01
	Pinacites	395.98
	Anarcestes	400.10
	Anetoceras	407.00

Boreal zone (Perm Cis-Urals)	block	180	148/206/212		off	Wardlaw-Davydov (GTS2004, Fig. 16.3) and Kozur (2003)
	TOP	269.30
	Sverdrupites amundseni, Sverdrupites harkeri	270.60
	Tumaroceras zavadovskyi, Epijuresanites musaltini, Uraloceras tschuvaschovi	275.60
	Neocrimites fredericksi	277.80
	Aktubinskia notabilis	281.10
	Neoshumardites triceps	284.40
	Andrianovia (=Preshumardites) sakmarae	289.50
	Synartinskia principalis	292.56
	Sventanoceras strigosum	296.14
	Sventanoceras serpentinum	298.34
	Sventanoceras primore	298.80
	Shumardites aktjubensis	299.98
	Shumardites confessus	301.21

Low-latitude Permian zone	block	180	236/204/215		off	Wardlaw-Davydov (GTS2004, Fig. 16.3) and Kozur (2003)
	TOP	251.00
	Hypophiceras changingense	251.17
	Pleuronodoceras occidentale	251.36
	Paratirolites waageni	252.23
	Sjevurevotes sjevurevo	252.68
	Dzhulfites spinosus	253.24
	Iranites transcaucasicus	253.52
	Phisonites triangulus	253.80
	Vedioceras ventroplanum	255.78
	Araxoceras latum	256.44
	Roadoceras, Doulingoceras	260.40
	Timorites - Waagenoceras	266.68
	Waagenoceras	269.30
	Demarezites - Perrinites vidriesis	270.60
	Perrinites hilli	273.10
	Perrinites tardus	281.10
	Metaperrinites cumminsi	284.40
	Properrinites boesei	294.60

Devonian geno-subzone	block	120	236/204/215		off	Becker and House (2000)
	TOP	359.20
	Acutimitoceras	360.82
	Cymaclymenia	361.19
	Wocklumeria	361.83
	Parawocklumeria	362.31
	Balvia	362.75
	Linguaclymenia	363.48
	[Kalloclymenia]	363.92
	Ornatoclymenia	364.42
	Clymenia	364.84
	[Pachyclymenia]	365.32
	Protoxyclymenia	365.79
	Prionoceras	366.34
	Prolobites	367.00
	Pseudoclymenia	367.68
	Pernoceras	368.07
	Dimeroceras	368.73
	Posttornoceras	369.30
	Maeneceras	369.73
	Paratornoceras	370.34
	Praemeroceras	370.98
	Paratorleyoceras	371.59
	Ch. (Cheiloceras)	372.20
	Ch. (Raymondiceras)	373.36
	Phoenixites	374.50
	Crickites	375.62
	Archoceras	376.62
	Neomanticoceras	377.92
	Playfordites	379.07
	Beloceras	379.79
	Mesobeloceras	380.41
	Prochorites	381.11
	Probeloceras	381.66
	Sandbergeroceras	382.28
	Timanites	383.32
	Koenenites	384.76
	Neopharciceras	385.30
	Petteroceras	386.39
	Pseudoprobeloceras	386.92
	Synpharciceras	387.47
	Stenopharciceras	388.08
	Pharciceras	388.69
	Afromaenioceras	389.32
	Sellagoniatites	389.97
	TOP	390.59
	Maenioceras	392.01
	Agoniatites	393.44
	Cabrieroceras	395.14
	TOP	395.47
	Pinacites	395.98
	Foordites	396.73
	TOP	397.50
	Anarcestes	399.34
	Sellanarcestes	400.10
	Latanarcestes	401.14
	[Amoenophyllites]	401.95
	Mimosphinctes	403.81
	Mimagoniatites	404.71
	Anetoceras	406.34

Devonian numbered subzones	block	50	236/204/215	notitle	off	Becker and House (2000)
	F	360.82
	E	361.19
	D	361.83
	C	362.31
	B	362.75
	A	363.48
	C	363.92
	B	364.42
	A	364.84
	C	365.32
	B	365.79
	A	366.34
	C	367.00
	B	367.68
	A	368.07
	I	368.73
	H	369.30
	G	369.73
	F	370.34
	E	370.98
	D	371.59
	C	372.20
	B	373.36
	A	374.50
	L	375.62
	K	376.62
	J	377.92
	I	379.07
	H	379.79
	G	380.41
	F	381.11
	E	381.66
	D	382.28
	C	383.32
	B	384.76
	A	385.30
	E	386.39
	D	386.92
	C	387.47
	B	388.08
	A	388.69
	D	389.32
	C	389.97
	B	390.59
	A	392.01
	F	393.44
	E	395.14
	D	395.47
	C	395.98
	B	396.73
	A	397.50
	D	399.34
	C	400.10
	B	401.14
	A	401.95
	E	403.81
	D	404.71
	C	405.52
	B	406.34
	A	407.00

Devonian subzone name	block	180	236/204/215		off	Becker and House (2000)
	TOP	359.20
	Acut. (Stockumites) prorsum	360.82
	Cymaclymenia nigra	361.19
	Epiwo. applanata/Wocklumeria sphaeroides	361.83
	Parawo. paradoxa / Kampto. endogona	362.31
	Balvia (Mayneoceras) lens	362.75
	Kosmo. (Muessenbiaergia) parundulata	363.48
	Piriclymenia piriformis	363.92
	Ornatoclymenia ornata	364.42
	Clymenia laevigata	364.84
	Prot. (Franconiclymenia) serpentina	365.32
	Prot. (Protoxyclymenia) dunkeri	365.79
	Platy. (Platyclymenia) annulata	366.34
	Prolobites delphinus	367.00
	Pseudoclymenia pseudogoniatites	367.68
	Pernoceras "dorsatum"	368.07
	Dimeroceras mamilliferum	368.73
	Posttornoceras contiguum	369.30
	Maeneceras subvaricatum	369.73
	Paratorno. lentiforme	370.34
	Praemeroceras petterae	370.98
	Paratorleyoceras globosum	371.59
	Ch. (Cheiloceras) subpartitum	372.20
	Ch. (Raymondiceras) verneuili	373.36
	Phoenixites frechi	374.50
	Crickites holzapfeli	375.62
	Archoceras varicosum	376.62
	Neomanticoceras paradoxum	377.92
	Playfordites tripartitus	379.07
	Beloceras tenuistriatum	379.79
	Mesobeloceras kayseri	380.41
	Prochorites alveolatus	381.11
	Probeloceras lutheri	381.66
	Sandbergeroceras syngonum	382.28
	Timanites keyserlingi	383.32
	Koenenites styliophilus	384.76
	Petteroceras feisti	385.30
	Petteroceras errans	386.39
	Pseudoprobeloceras pernai	386.92
	Synpharciceras clavilobum	387.47
	Stenopharciceras lunulicosta	388.08
	Pharciceras lateseptatum	388.69
	Afromaenioceras sulcatostriatum	389.32
	Maenioceras terebratum	389.97
	Maenioceras molarium	390.59
	Maenioceras undulatum	392.01
	Agoniatites costulatus	393.44
	Cabrieroceras crisp. plebeiforme	395.14
	Subananarcestes macrocephalus	395.47
	Pinacites jugleri	395.98
	Foordites platypleura	396.73
	Anarcestes ( - Gyroceratites)	397.50
	Anarcestes lateseptatus	399.34
	Sellanarcestes wenkenbachi	400.10
	Latanarcestes noeggerathi	401.14
	Gyroceratites gracilis	401.95
	Mimosphinctes tripartitus	403.81
	Mimagoniatites fecundus	404.71
	Teicherticeras teicherti / Ruanites obliqueseptatus	406.34
	bactritids (ancestral goniatites)	407.00



Ammonoid major marker	event		236/204/215			PERMIAN = Kozur (2003), Davydov et al., 2004, and Henderson (2005); CARBONIFEROUS = GTS2004 diagram (Davydov et al., 2004 and unpublished zonation table), DEVONIAN = Becker and House (2000)
FAD
	Pseudotirolites	251.70
	Paratirolites	252.23
	Iranites, Sinoceltites	253.52
	Araxoceras	256.44
	Anderssonoceras	257.10
	Roadoceras, Doulingoceras	260.40
	Timorites	265.80
	Waagenoceras	269.30
	Demarezites	270.60
	Pseudovidrioceras	273.10
	Propinacoceras	275.60
	Uraloceras, Medlicottia	280.00
	Aktubinskia	281.10
	Artinskia	282.75
	Neopronorites	284.40
	Sakmarites	292.56
	Svetlanoceras	298.80
	Shumardites	301.21
	Vidrioceras / Artinskia	303.90
	Parashumardites	306.50
	Eowellerites	310.92
	Winslowoceras	311.70
	Reticuloceras	316.82
	Homoceras	318.52
	Eumorphoceras	326.40
	Goniatites	342.47
	Dzhaprakoceras	345.30
	Pericyclus	350.86
	Gattendorfia	359.20
	imitoceratids	360.82
	Wocklumeria sphaeroides sphaeroides, sphaeroides aperta and sphaeroides plana	361.83
	Parawocklumeria	362.31
	Balvia	362.75
	Kosmo. sublaevis	363.48
	Piri. piriformis	363.92
	Ornato. ornata	364.42
	Cl. laevigata. Kosmo. inaequistriata lamellosa	364.84
	Protoxy. serpentina	365.32
	Protoxy. dunkeri	365.79
	Platy. annulata, subnautilina, pseudoflexuosa, quiringi; Priono. divisum, frechi	366.34
	Prol. delphinus	367.00
	Ps. pseudogoniatites	367.68
	Pern. dorsatum, delepinei, crebriseptum / Protornoceras	368.07
	dimeroceratid species	368.73
	Post. contiguum	369.30
	M. subvaricatum	369.73
	oxyconic dimeroceratids	370.34
	Praem. petterae	370.98
	advanced cheiloceratids	371.59
	Ch. subpartitum	372.20
	cheiloceratids	373.36
	Crickites	375.62
	Archan. varicosum	376.62
	Regionally different advanced members of oxyconic Virginoceratinae	377.92
	Play. tripartitus	379.07
	Beloceras	379.79
	Mesobeloceras	380.41
	Prochorites alveolatus	381.11
	Probeloceras lutheri	381.66
	Sandbergeroceras	382.28
	Timanites	383.32
	Koenenites	384.76
	Neopharciceras, Pett. feisti, Acanthoclymenia sp.	385.30
	Petteroceras errans	386.39
	Pseudoprobeloceras	386.92
	Synph. clavilobum / plurilobatum	387.47
	multilobed pharciceratids (Steno. lateseptatum)	388.08
	Pharciceras s.str.	388.69
	Afro. sulcatostriatum	389.32
	Maenio terebratum	389.97
	Maenio. molarium	390.59
	maenioceratids	392.01
	Agon. costulatus	393.44
	Cabr. crispiforme	395.14
	Subananarcestes macrocephalus	395.47
	Pin. jugleri /eminens	395.98
	Fidelites occultus / Foordites platypleura	396.73
	Anarcestes	399.34
	Sellanarcestes	400.10
	Latan. noeggerathi acut.	401.14
	Gyro. gracilis, Amoenophyllites	401.95
	Mimosphinctes / Convoluticeras	403.81
	Mimagoniatites	404.71
	Mimosphinctidae	406.34
	Anetoceras	407.00
LAD
	Cravenoceras	319.35
	Goniatites	324.33
	Climenida	359.20
	EXTINCTION of all Devonian ammonoids, apart from Cyma. evoluta, striata, and involvens	361.19
	Spheno. brevispina	363.48
	Manticoceras, Beloceras, Gephuroceratidae, Beloceratidae, Tornoceratidae	374.50
	Koenenitidae	382.28
	Maenio. molarium	389.97
	Gyroceratites	397.50
	Gyro. laevis	401.95



Graptolites (Dev-Ord)	:	Graptolite Zone (Europe)	Graptolite Marker FAD/LAD	Australasia Graptolite zone	_METACOLUMN_OFF

Graptolite Zone (Europe)	block	150	210/212/215	notitle		GTS2004 diagrams (various authors)
	TOP	406.67	dashed
	Monograptus yukonensis	407.84
	Monograptus falcarius	410.36
	Monograptus hercynicus	413.36
	Monograptus praehercynicus,  Monograptus uniformis	416.00
	Monograptus transgrediens, Monograptus boucekiperneri	417.08
	Monograptus lochkovensis,  Monograptus branikensis	418.16
	Monograptus parultimusultimus	418.70
	Monograptus formosus	419.35
	Neocucullograptus kozlowskii, B. cornuatus - P. podoliensis	420.39	dashed
	Saetograptus leintwardinensis, Saetograptus linearis	421.46	dashed
	Lobograptus scanicus	422.42	dashed
	Neodiversograptus nilssoni	422.90
	Colonograptus ludensis	423.73
	Colono. praedeubeli-deubeli	424.39
	Pristio. Parvus - Gotho. nassa	424.88
	Cyrtograptus lundgreni	425.71
	Cyrtograptus perneri, Cyrtograptus rigidus	426.60
	Monograptus beloph.-anten., Monogr. riccartonensis	427.40
	Cyrtograptus murchisoni	427.80
	Cyrtograptus centrifugus	428.20
	Cyrtograptus insectus	428.60
	Cyrtograptus lapworthi	429.39
	Oktavites spiralis	431.36
	Monoclimacis crenulata, Monoclimacis griestoniensis	432.15
	Monograptus crispus	434.13
	Spirograptus turriculatus	434.92
	Spirograptus guerichi	436.10
	Stimulograptus sedgwickii	436.68	dashed
	Lituigraptus convolutus	437.12
	Monograptus argenteus	437.70
	Demirastrites pectinatus, Demirastrites triangulatus	439.00
	Coronograptus cyphus	440.88
	Orthograptus vesiculosus	441.82
	Parakidograptus acuminatus	443.00
	Akidograptus ascensus	443.70
	Normalograptus? persculptus	444.84
	Normalograptus? extraordinarius	445.60
	Paraorthograptus pacificus	447.64
	Dicellograptus complexus	448.66
	Dicellograptus complanatus	449.68
	Pleurograptus linearis	452.74
	Dicranograptus clingani	455.80
	Diplograptus multidens	458.35
	Nemagraptus gracilis	460.90
	Hustedograptus teretiusculus	463.78
	Didymograptus murchisoni	464.86
	Didymograptus artus	466.30
	Aulograptus cucullus (Expansograptus hirundo)	468.10
	Isograptus gibberulus	471.06
	Expansograptus simulans	473.50
	Corymbograptus varicosus	475.20
	[un-named]	476.56
	Tetragraptus phyllograptoides	478.60
	Hunnegraptus copiosus	480.06	dashed
	Araneograptus murrayi	483.45
	Kiaerograptus	484.91	dashed
	Adelograptus, Paradelograptus antiquus	485.88
	Rhabdinopora f. anglic	486.36
	Anisograptus matanensis	487.33
	Rhabdinopora praeparabola, parabola	488.30

Graptolite Marker FAD/LAD	event		210/212/215			GTS2004 diagrams (Cooper and Sadler, 2004)
FAD
	Normalograptus? extraordinarius	445.60
	Dicellograptus complanatus	449.68
	Diplacanthograptus caudatus	455.80
	Nemagraptus gracilis	460.90
	Undulograptus austrodentatus	468.10
	Tetragraptus approximatus	478.60
	Rhabdinopora praeparabola	488.30
	Mongraptus uniformis	416.00
	Monograptus parultimus	418.70
	Saetograptus leintwardinensis	421.46
	Neodiversograptus nilssoni	422.90
	Cyrtograptus lundgreni	425.71
	Monograptus austerus sequens	439.00
	Akidograptus ascensus	443.70
	Normalograptus? extraordinarius	445.60
	Dicellograptus complanatus	449.68
	Diplacanthograptus caudatus	455.80
	Nemagraptus gracilis	460.90
	Undulograptus austrodentatus	468.10
	Tetragraptus approximatus	478.60
	Rhabdinopora praeparabola	488.30
LAD
	GRAPTOLITES	406.67

Australasia Graptolite zone	block	150	210/212/215	notitle		GTS2004 diagrams (Cooper and Sadler, 2004)
	TOP	443.70
	Bo5 / Normalograptus? persculptus	444.84
	Bo4 / Normalograptus? extraordinarius	445.60
	Bo3 / Paraorthograptus pacificus	447.64
	Bo2 / (prepacificus)	449.17
	Bo1 / Climacograptus? uncinatus	450.19
	Ea4 / Dicellograptus gravis	451.21	dashed
	Ea3 / Dicranograptus kirki	452.74
	Ea2 / Diplacanthograptus spiniferus	454.27	dashed
	Ea1 / Diplacanthograptus lanceolatus	456.06
	Gi2 / Orthograptus calcaratus	458.10
	Gi1 / Nemagraptus gracilis	460.90
	Da4 / Archiclimacograptus riddellensis	463.06
	Da3 / Pseudoclimacograptus decoratus	465.22
	Da2 / Undulograptus intersitus	466.30
	Da1 / Undulograptus austrodentatus	468.10
	Ya1-2 / C. morsus, O. upsilon	468.84
	Ca3-4 / I. v. maximodivergens- I.v. maximus	469.95
	Ca2 / Isograptus v. victoriae	470.88	dashed
	Ca1 / Isograptus v. lunatus	471.80
	Ch2 / Isograptus primulus	472.82	dashed
	Ch1 / Didymograptus protobifidus	473.50
	Be4	474.18	dashed
	Be3	474.86	dashed
	Be2	475.54	dashed
	La3 / Tetragraptus approximatus	478.60
	La2 (upper) / Araneograptus pulchellus	483.45
	La2 (lower) / Aorograptus victoriae	485.88
	La1b / P. jacksoni	486.36
	La1a / Anisograptus	487.33
	Pre-La1	488.30


Trilobite Zones (Camb)	:	South China	Siberia	Australia	Laurentia	FAD/LAD	_METACOLUMN_OFF		GTS2004 diagram (Shergold and Cooper, 2004); revised by Shanchi Peng et al (Cambrian Subcommission, Dec 2006)

South China	block	150	215/181/210
	TOP	488.30
	Hysterolenus - Onychopyge	488.91
	Leiostr. constrictum- Shen. brevica	489.52
	Mictosaukia striata - Fatocephalus	489.89
	Archaeul. taoyuanense - Leioagn. cf. bexelli	490.88
	Lotagnostus americanus- Hedinaspis regalis	492.00
	Probinacunaspis nasalis - Peichiashania hunanensis	493.00
	Eolotagnostus decoratus - Kaolishaniella	494.40
	Rhaptagnostus ciliensis / Onchonot. cf. kuruktagensis	495.40
	Agnostotes orientalis- Irvingella angustilimbata	496.00
	Corynexochus plumula - Sinop. cf. kiangshanensis	498.25
	Innitagnostus inexpectans - Proceratopyge protracta	500.00
	Glyptagnostus reticulatus	501.00
	Glyptagnostus stolidotus	501.20
	Linguagnostis reconditus	501.80
	Proagnostus bulbus	502.20
	Lejopyge laevigata	503.00
	Goniagnostus nathorsti	504.05
	Ptychagnostus punctuosus	504.93
	Acidusus atavus	506.50
	Ptychagnostus gibbus	508.95
	Oryctocephalus indicus	510.00
	Ovatoryctocara granulaata -Bathynotus holopygus	511.40
	Protoryctocephalus	512.10
	Arthricocephalites - Changaspis	513.50
	Arthricocephalus	515.25
	Sichuanolenus - Chengkouia	519.40
	Hupeidiscus - Sinodiscus	521.00	dashed
	[ Blank zone ]	527.12
	Heraultipegma yunnanensis	535.34
	Siphogonuchites triangularis - Paragloborilus subglobosus	536.82
	Anabarites trisulcatus - Protohertzium anabarica	540.15

Siberia	block	150	215/181/210
	TOP	488.30
	Eopatokephalus nyaicus	489.52
	Dolgeuloma abunda - D. dolganensis	491.13
	Ketyna ketiensis - Monosulcatina laeve	492.00
	Tukalandaspis egens	494.00
	Irvinella norilica	495.00
	Norilagn. quadratus - Irvingella cipita	495.40
	Agnostotes orientalis - Irvingella perfecta	496.00
	Erixanium sentum	498.25
	[ Blank zone ]	500.00
	Glyptagnostus reticulatus	501.00
	Glyptagnostus stolidotus	501.20
	Pedinocephalina - Toxotis / Acro. granulosa - Kold. prolixa	502.20
	Lejopyge laevigata - Oidalag. trispinifer	503.00
	A. limbataeformis	504.05
	Anopolenus henrici - Corynexochus perforatus	505.80
	Tomagnostus fissus	506.50
	Ptychagnostus gibbus	507.03
	Kounamkites	509.13
	Ovatoryctocara granulaata - Schistocephalus antiquus	511.40
	Anabaraspis splendens	513.85
	Lermontovia grandis	514.90
	Bergeroniellus ketemensis	516.30
	Bergeroniellus ornata	517.00
	Bergeroniellus asiaticus	517.40
	Bergeroniellus gurarii	518.00
	B. micmacciformis -Erbiella	518.60
	Judomia	519.40
	Pagetiellus anabarus	519.80
	Fallotaspis	520.40
	Profallotaspis jakutensis	521.00	dashed
	D. lenaicus-Tum. primigenius	523.72
	Dokidocyathus regularis	527.12
	Nochoroicyathus sunnaginicus	531.20
	[ Blank zone ]	535.34
	Purella antiqua	537.12
	Anabarites trisulcatus	540.15

Australia	block	150	215/181/210
	TOP	488.30
	C. prolindstromi	488.91
	Cordylodus proavus (conodont)	489.52
	Mictosaukia perplexa	489.89
	Neoagn. quasibilobus - Shergoldia nomas	491.38
	Sinosaukia impages	492.00
	Rh. clarki maximus - Rh. papilio	492.60
	Rhaptagn. bifax - N. denticulatus	493.00
	Rh. clarki prolatus - Caz. secatrix	493.40
	Rh.c. patulus - C. squamosa - H. lilyensis	494.00
	Peichiashania tertia - P. quarta	494.40
	Peichiash. secunda - Pro. glabella	495.00
	Wentsuia iota - Rhaptagn. apsis	495.40
	Irvingella tropica	496.00
	Stigmatoa diloma	497.50
	Erixanium sentum	498.50
	Proceratopyge cryptica	500.00
	Glyptagnostus reticulatus	501.00
	Glyptagnostus stolidotus	501.20
	Achmarhachis quasivespa	501.80
	Erediaspis eretes	502.20
	Lejopyge laevigata	503.00
	Goniagnostus nathorsti	504.05
	Ptychagnostus punctuosus	504.93
	Acidusus atavus	506.50
	Ptychagnostus gibbus	507.03
	Xystridura templetonenesis / Redlichia chinensis	513.50
	Pararaia janeae	515.60
	Pararaia bunyerooensis	515.60
	Pararaia tatei	517.20
	"Abadiella" huoi	519.80
	NO ESTABLISHED ZONES	542.00

Laurentia	block	150	215/181/210
	TOP	488.30
	S. brevispicata - M. depressa	489.52
	Eurekia apopsis	489.89
	Saukiella serotina	490.51
	Saukiella junia / Saukiella pyrene - Rasettia maga	493.40
	Ellipsocephaloides - Idahoia	495.00
	Taenicephalus	495.20
	Elvinia	496.00
	Dunderbergia	498.50
	Aphelaspis	501.00
	Crepicephalus	501.80
	Cedaria	502.60
	Lejopyge laevigata	503.00
	Ptychagnostus punctuosus	504.93
	Acidusus atavus	506.50
	Ptychagnostus gibbus	507.03
	Pentagnostus praecurrens	507.73
	Peronopsis bonnerensis	508.08
	Albertella	508.60
	"Plagiura-Poliella"	510.00
	Amecephalus arrojosensis	512.10
	Eokochaspis nodosa	513.50
	Bonnia - Olenellus	518.20
	Nevadella	519.80
	"Fallotaspis" [1st TRILOBITES]	521.00	dashed
	"Wyattia"	542.00

Major Cambrian markers	event
FAD
	Iapetognathus flutivagus	488.30
	Codylodus adesei (conodont)	489.52
	Lotagnostus americanus	492.00
	Agnostotes orientalis, Irvingella	496.00
	Glyptagnostus reticulatus	501.00
	Glyptagnostus stolidotus	501.20
	Linguagnostis reconditus	501.80
	Lejopyge laevigata	503.00
	Ptychagnostus punctuosus	504.93
	Acidusus atavus	506.50
	Ptychagnostus gibbus	507.03
	Oryctocephalus indicus	510.00
	Ovatoryctocara granulaata	510.60
	Arthricocephalus chauveaui	511.88
	Acidiscus, Cephalopyge	512.10
	Serrodiscus, Hebediscus, Triangulaspis	513.80
	Olenellus / Redlichia	515.40
	First occurrence of TRILOBITES	521.00
	First occurrence of ARCHAEOCYATHS	531.20
	SMALL SHELLY FAUNA	540.15
	Trace fossil: Tricophycus pedum	542.00


Conodonts	:	N.Amer. Triassic	Tethys Triassic	Numbered Conodont Zone (Carb-Perm)	Conodont Zone (Ordov-Perm)	Conodont subzone (Late Devonian)	Alternate Frasnian MN set	Conodont major markers	_METACOLUMN_OFF		TRIASSIC = mainly Orchard and Tozer (1997) and Kozur (2003); PALEOZOIC = GTS2004 diagrams (with Permian updated by Henderson, 2005; and Permian-Carboniferous enhanced by V. Davydov)

N.Amer. Triassic	block	180	233/236/173			Mainly Orchard and Tozer (1997) for Late and Middle Triassic, and GTS2004 for Early Triassic
	TOP	199.60
	Norigondolella sp.	200.27
	Misikella posthernsteini	200.95
	Cypridodella mosheri	203.64
	Cypridodella bidentata	205.92
	Cypridodella serrulata	206.94
	Cypridodella postera	207.96
	Cypridodella elongata	208.98
	Cypridodella spiculata	210.01
	Cypridodella multidentata	211.30
	Epigondolella triangularis	213.11
	Epigondolella quadrata	214.52
	Metapolygnathus primitius	216.96
	Metapolygnathus communisti	217.59
	Carnepigondolella zoae	219.81
	Metapolygnathus carpathica	221.30
	Metapolygnathus polygnathiformis	228.01
	Metapolygnathus inclinata	229.43
	Paragondolella n.sp.S	229.85
	Paragondolella foliata	231.68
	Budurovignathus hungaricus	234.56
	Paragondolella ex gr. excelsa	241.91
	Neogondolella regale	244.42
	Neospathodus triangularis / Neospath. crassatus	248.08
	Neospathodus waageni	249.33
	Neospathodus pakistanensis	250.03
	Neospathodus cristagalli / Neospathodus kummeli	250.38
	Neogondolella carinata / Hindeodus parvus	251.00


Tethys Triassic	block	180	233/236/173			Kozur (2003)
	Misikella ultima	200.27
	Misikella posthernsteini	203.64
	Cypridodella bidentata	206.64
	Cypridodella postera	208.98
	Cypridodella spiculata	210.01
	Cypridodella multidentata	211.30
	Epigondolella triangularis - Norigondolella hallstattensis	213.11
	Epigondolella quadrata	214.52
	Epigondolella orchardi - N. navicula	216.96
	Carnepigondolella pseudodiebeli	217.59
	Carnepigondolella zoae	219.81
	Metapolygnathus carpathica	221.30
	P. postinclinata - Metapolygnathus polygnathiformis	222.70
	Gladigondolella tethydis - Metapolygnathus polygnathiformis I.Z.	228.01
	Budurovignahus diebeli - Metapolygnathus polygnathiformis	228.73
	Budurovignathus supralongobardica	229.43
	Budurovignathus mungoensis	231.68
	Budurovignathus hungaricus	234.56
	Budurovignathus truempyi	235.78
	Paragondolella? tram. trammeri - Neogondolella aequidentata	239.00
	Paragondolella? tram. trammeri - Paragondolella alpina	240.00
	Paragondolella alpina - Paragondolella? trammeri praetrammeri	241.00
	Neogondolella mesotriassica	241.15
	Neogondolella constricta	241.30
	Paragondolella bifurcata	241.91
	Paragondolella bulgarica	243.68
	Neogondolella? regalis	244.42
	Chiosella timorensis	245.17
	Chiosella gondolelloides	245.65
	Triassospathodus sosioensis	246.14
	Triassospathodus triangularis	246.63
	Triassospathodus homeri	247.11
	Icriospathodus collinsoni	247.59
	Triassospathodus hungaricus	248.08
	Neospathodus waageni - Scythogondolella milleri	248.63
	Neospathodus waageni - Scythogondolella meeki	249.33
	Chengyuania nepalensis	249.75
	Neospathodus dieneri	250.31
	Sweetospathodus kummeli	250.38
	Clarkina postcarinata	250.49
	Clarkina carinata	250.63
	Isarcicella isarcica	250.82
	Hindeodus parvus	251.00
	Clarkina meishanensis - H. praeparvus	251.20
	Clarkina hauschkei	251.40


Numbered Conodont Zone (Carb-Perm)	block	50	233/236/173	notitle		Davydov (GTS2004)
	TOP	251.00
	Lc10	251.17
	Lc9	251.56
	Lc8	252.40
	Lc7	253.10
	Lc6	253.80
	Lc5	255.78
	Lc4	256.44
	Lc3	258.42
	Lc2	259.08
	Lc1	260.40
	Gc4	263.10
	Gc3	265.80
	Gc2	268.00
	Gc1	270.60
	Cc12	271.60
	Cc11	273.35
	Cc10	275.60
	Cc9	277.80
	Cc8	284.40
	Cc6 - Cc7	294.60
	Cc5	295.48
	Cc4	296.14
	Cc3	297.24
	Cc2	298.34
	Cc1	299.00
	Pc19	299.98
	Pc18	301.21
	Pc17	302.43	dashed
	Pc16	303.17	dashed
	Pc15	303.90
	Pc14	304.68
	Pc13	305.72
	Pc12	306.50
	Pc11	308.06
	Pc10	309.36
	Pc9	310.14
	Pc8	311.18
	Pc7	311.70
	Pc6	312.66
	Pc5	313.94
	Pc4	314.90
	Pc3	315.54	dashed
	Pc2	317.14
	Pc1	318.10
	Mc16	321.01	dashed
	Mc15	323.91	dashed
	Mc14	326.40
	Mc13	328.29	dashed
	Mc12	330.18	dashed
	Mc11	333.02	dashed
	Mc10	337.74	dashed
	Mc9	342.47	dashed
	Mc8	345.30
	Mc7	346.69	dashed
	Mc6	348.08
	Mc5	350.86
	Mc4	352.25
	Mc3	355.03	dashed
	Mc2	356.84	dashed
	Mc1	359.20


Conodont Zone (Ordov-Perm)	block	180	233/236/173			GTS2004 diagrams (with Permian updated by Henderson, 2005)
	TOP	251.00
	Clarkina meishanensis	251.17
	Clarkina yini	251.56
	Clarkina changxingensis	252.40
	Clarkina subcarinata	253.10
	Clarkina wangi	253.80
	Clarkina orientalis	255.78
	Clarkina transcaucasica	256.44
	Clarkina guangyuanensis	256.77
	Clarkina leveni	258.42
	Clarkina asymetrica	259.08
	Clarkina dukouensis	260.07
	Clarkina postbitteri postbitteri	260.40
	Clarkina postbitteri hongshuiensis	260.94
	Jinogondolella altudaensis	263.10
	Jinogondolella postserrata	265.80
	Jinogondolella aserrata	268.00
	Jinogondolella nankingensis	270.60
	Neostreptognathodus sulcoplicatus	271.60
	Neostreptognathodus prayi	273.35
	Neostreptognathodus pequopensis	277.80
	Sweetognathus whitei	284.40
	Sweetognathus binodosus	286.44
	Sweetognathus merrilli - Neogondolella uralensis	294.60	dashed
	Streptognathodus barskovi	295.48
	Streptognathodus postfusus	296.14
	Streptognathodus fusus	297.24
	Streptognathodus constrictus	298.34
	Streptognathodus isolatus	299.00
	Streptognathodus wabaunsensis - St. bellus	299.98
	Streptognathodus simplex	301.21
	Streptognathodus virgilicus	302.43	dashed
	Streptognathodus vitali	303.17	dashed
	Streptognathodus simulator	303.90
	Idiognathodus toretzianus	304.68
	Idiognathodus sagittalis	305.72
	Streptognathodus subexcelsus - St. makhlinae	306.50
	Neognathodus roundyi - Streptognathodus cancellosus	308.06
	Neognathodus medexultimus -Streptognathodus concinnus	309.36
	Streptognathodus dissectus	310.14
	Neognathodus uralicus	311.18
	Declinognathodus donetzianus	311.70
	Neognathodus atokaensis	312.66
	Declinognathodus marginodosus	313.94
	Idiognathodus sinuosus	314.90
	Neognathodus askynensis	315.54	dashed
	Idiognathoides sinuatus	317.14
	Declinagnathodus noduliferus	318.10
	Gnathodus postbilineatus	321.01	dashed
	Gnathodus bollandensis	323.91	dashed
	Lochria cruciformis	326.40
	Lochria nodosa	328.29	dashed
	Lochria nodosa	330.18	dashed
	Lochria mononodosa	333.02	dashed
	Gnathodus billineatus	337.74	dashed
	Gnathodus texanus	342.47	dashed
	Gnathodus pseudosemiglaber - Scalliognathus anchoralis	345.30
	Gnathodus semiglaber -Polygnathus communis	346.69	dashed
	Dollimae bouckaerti	348.08
	Gnathodus typicus - Siphonodella isosticha	350.86
	Siphonodella quadruplicata - upper Patrognathus andersoni	352.25
	lower Patrognathus andersoni	355.03	dashed
	Patrognathus variabilis	356.84	dashed
	Patrognathus crassus	359.20
	Siphonodella praesulcata	363.03
	Palmatolepis expansa	365.32
	Palmatolepis postera	366.09
	Palmatolepis trachytera	367.62
	Palmatolepis marginifera	369.91
	Palmatolepis rhomboidea	371.44
	Palmatolepis crepida	373.12
	Palmatolepis triangularis	374.50
	Palmatolepis linguiformis	376.12
	Palmatolepis rhenana	378.28
	Palmatolepis jamieae	379.14
	Palmatolepis hassi	380.33
	Palmatolepis puactata	382.28
	Palmatolepis transitans	383.14
	falsiovalis	385.30
	norrisi	386.93
	Klapperina disparilis	387.25
	Schmidtognathus hermanni	388.23
	Polygnathus varcus	390.83
	hemiansatus	391.80
	Polygnathus xylus ensensis	392.94
	Tortodus kockelianus	393.80
	Tortodus australis	394.94
	Polygnathus costatus	395.79
	Polygnathus partitus	397.50
	Polygnathus patulus	398.93
	Polygnathus serotinus	400.83
	Polygnathus inversus/ laticostatus	402.25
	nothoperbonus	403.68
	Polygnathus gronbergi / excavatus, Polygnathus kitabicus	407.00
	Polygnathus pireneae	408.47
	Eognathodus kindlei	409.94
	Eognathodus sulcatus	411.20
	Pedavis pesavis	412.16
	Ancyrodelloides delta	413.36
	Latericriodus woschmidt / postwoschmidti	416.00
	Oulodus elegans detortus	417.49
	Ozarkodina remscheidensis Interval Zone	418.70
	Ozarkodina crispa	419.09
	Ozarkodina snajdri	419.74
	Interval Zone	420.39
	Polygnathoides siluricus	420.78
	Ancoradella ploeckensis	421.70
	[ not zoned ]	422.42
	K. stauros	422.90
	Ozarkodina bohemica	424.88
	Ozarkodina sagitta sagitta	426.50
	Kockelella ranuliformis	427.90
	Pterospathodus amorphognathoides	430.18
	Pterospathodus celloni	434.52
	Pterospathodus tenuis - Distomodus staurognathoides	439.00
	Distomodus kentuckyensis	443.00
	Rexroadus nathani	443.70
	Amorphognathus ordovicicus	450.19
	Amorphognathus superbus	455.29
	Amorphognathus tvaerensis	460.14
	Pygodus anserinus	462.34
	Pygodus serra	463.78
	Eoplacognathus suecicus	464.86
	Eoplacognathus variabilis	467.02
	Baltoniodus norrlandicus	468.66
	Paroistodus originalis	469.40
	Baltoniodus navis	470.69
	Baltoniodus triangulatus	471.80
	Oepikodus evae	474.52
	Prioniodus elegans	477.24
	Paroistodus proteus	483.45
	Paltodus deltifer	484.91
	Cordylodus angulatus	486.85
	Iapetognathus fluctivagus	488.30

Conodont subzone (Late Devonian)	block	30	233/236/173	notitle	off	GTS2004 diagram (House et al., 2004)
	TOP	359.20
	3	360.73
	2	361.50
	1	363.03
	4	363.48
	3	363.79
	2	364.56
	1	365.32
	2	365.78
	1	366.09
	2	367.00
	1	367.62
	3	367.92
	2	369.30
	1	369.91
	2	370.98
	1	371.44
	4	371.59
	3	372.05
	2	372.66
	1	373.12
	3	373.58
	2	374.04
	1	374.50
	4	376.66
	3	377.31
	2	377.96
	1	378.28
	2	379.79
	2	386.73
	1	387.25
	2	387.84
	1	388.23
	2	389.92
	1	390.83

Alternate Frasnian MN set	block	50	233/236/173	notitle		GTS2004 diagram (House et al., 2004)
	TOP	374.50
	MN 13	376.34
	MN 12	377.63
	MN 11	379.14
	MN 9\10	379.79
	MN 7\8	380.33
	MN 6	381.20
	MN 5	382.28
	MN 4	383.46
	MN 3	384.22
	MN 2	384.76
	MN 1	385.30


Conodont major markers	event		234/236/192			TRIASSIC = mainly Orchard and Tozer (1997) and Kozur (2003); PALEOZOIC = GTS2004 diagrams (with Permian updated by Henderson, 2005; and Permian-Carboniferous enhanced by V. Davydov)
LAD
	Extinction of CONODONTS	199.60
	Cypridodella mosheri (?), Cypridodella bidentata, Cypridodella postera	200.95
	Metapolygnathus carpathica	214.02
	Metapolygnathus polygnathiformis	217.38
	Gladigondolella tethydis	222.70
	Budurovignahus diebeli	225.66
	Paragondolella excelsa, G. trammeri, C. ciernensis	228.01
	G. cornuta, G. pseudolonga	233.34
	G. hanbulogi	240.00
	Neospathodus waageni, Scythodondolella milleri	245.17
	Neospathodus collinsoni	246.66
	Neospathodus dieneri	247.46
	Neospathodus pakistanensis, Neospathodus cristagalli	248.32
	Clarkina carinata	250.10
	Sweetospathodus kummeli	250.24
	Isarcicella isarcica	250.38
	Idiognathodus	303.17
	Declinognathodus donetzianus	311.18
	Sc. anchoralis	348.08
	Pedavis pesavis	411.20
FAD
	Norigondolella sp. (N.Amer.), Misikella ultima (Tethys)	200.27
	Cypridodella mosheri, Misikella posthernsteini	203.64
	Cypridodella bidentata (N.Amer.)	205.92
	Cypridodella serrulata	206.94
	Cypridodella postera	207.96
	Cypridodella elongata	208.98
	Cypridodella spiculata	210.01
	Cypridodella multidentata	211.30
	Epigondolella triangularis	213.11
	Epigondolella quadrata	214.52
	Metapolygnathus primitius	216.96
	Metapolygnathus communisti, Carnepigondolella pseudodiebelli	217.59
	Carnepigondolella zoae (?)	219.81
	Metapolygnathus carpathica, Carnepigondolella lindae	221.30
	Metapolygnathus polygnathiformis	228.01
	Budurovignahus diebeli	228.73
	Metapolygnathus inclinata, Budurovignathus supralongobardica	229.43
	Paragondolella n.sp.S	229.85
	Paragondolella foliata, Budurovignathus mungoensis	231.68
	C. ciernensis	233.34
	Budurovignathus hungaricus	234.56
	Budurovignathus truempyi	235.78
	Budurovignathus	237.00
	Neogondolella aequidentata	239.00
	Paragondolella? trammeri trammeri, G. pseudolonga	240.00
	Paragondolella alpina	241.00
	Neogondolella mesotriassica	241.15
	Neogondolella constricta	241.30
	Gladigondolella tethydis, Paragondolella excelsus, G. cornuta	241.60
	Paragondolella ex gr. excelsus, Paragondolella bifurcata	241.91
	Nicoraella kockeli, G. hanbulogi	242.49
	Paragondolella bulgarica, G. malayensis budurovi	243.68
	Neogondolella? regalis	244.42
	Chiosella timorensis	245.17
	Chiosella gondolelloides (?)	245.65
	Triassospathodus sosioensis (?)	246.14
	Triassospathodus triangularis	246.63
	Neospathodus homeri	247.11
	Neogondolella jubata	248.08
	Triassospathodus hungaricus	248.08
	Scythogondolella milleri	248.63
	Neospathodus waageni	249.33
	Chengyuania nepalensis	249.75
	Neospathodus pakistanensis	250.03
	Neospathodus dieneri, Hindeodus typicalis, Neospathodus cristagalli	250.31
	Sweetospathodus kummeli	250.38
	Clarkina postcarinata	250.49
	Clarkina carinata	250.63
	Isarcicella isarcica	250.82
	Hindeodus parvus	251.00
	Clarkina meishanensis	251.17
	Clarkina yini	251.56
	Clarkina changxingensis	252.40
	Clarkina subcarinata	253.10
	Clarkina wangi	253.80
	Clarkina orientalis	255.78
	Clarkina transcaucasica	256.44
	Clarkina guangyuanensis	256.77
	Clarkina leveni	258.42
	Clarkina asymetrica	259.08
	Clarkina dukouensis	260.07
	Clarkina postbitteri postbitteri	260.40
	Clarkina postbitteri hongshuiensis	260.94
	Jinogondolella granti	261.48
	Jinogondolella xuanhanensis	262.02
	Jinogondolella prexuanhanensis	262.56
	Jinogondolella altudaensis	263.10
	Jinogondolella shannoni	264.45
	Jinogondolella postserrata	265.80
	Jinogondolella aserrata	268.00
	Jinogondolella nankingensis	270.60
	M. idahoensis lamberti	271.10
	Neostreptognathodus sulcoplicatus	271.60
	Neostreptognathodus prayi	273.35
	Neostreptognathodus pnevi	275.60
	Neostreptognathodus exculptus	277.36
	Neostreptognathodus pequopensis	277.80
	Sweetognathus clarki	278.24
	Sweetognathus whitei	284.40
	Mesogondolella bisselli	285.42
	Sweetognathus binodosus	286.44
	Sweetognathus merrilli	294.60
	Sweetognathus expansus	295.04
	Streptognathodus barskovi	295.48
	Streptognathodus postfusus	296.14
	Streptognathodus fusus	297.24
	Streptognathodus constrictus	298.34
	Streptognathodus isolatus	299.00
	Streptognathodus wabaunsensis	299.98
	Streptognathodus "simulatos"	303.90
	Idiognathodus sagittalis	305.72
	Declinognathodus donetzianus	311.70
	Neognathodus atokaensis	312.66
	Idiognathodus, Declinognathodus marginodosus	313.94
	Streptognathodus	314.90
	Declinognathodus noduliferus	318.10
	Lochriea cruciformis	326.40
	Lochriea nodosa	330.18
	Gnathodus billineatus	337.74
	Gnathodus homopunctatus	345.30
	Siphonodella sulcata	359.20
	Palmatolepis triangularis	374.50
	Ancyrodella rotundiloba 	385.30
	Tortodus kockelianus	393.80
	Polygnathus partitus	397.50
	Polygnathus kitabicus, Polygnathus dehiscens	407.00
	Eognathodus sulcatus	411.20
	Amorphognathus ordovicicus	450.19




Sequences (SEPM Global or Tethyan)	sequence					Hardenbol, J., Jacquin, T., Vail, P.R., et al. (SEPM charts. 1998)
		MFS	0.00	Major	A major transgression-MFS is indicated for Today, which presumes continued melting of glaciers will exceed the Eemian previous maximum highstand.
	LGM	SB	0.02	Major	Last Glacial Maximum; Marine Isotope Stage (MIS) 2
		MSF	0.13	Major	Base of Eemian stage; MIS 5
	MIS 6	SB	0.14	Major	Peak of Illinoian/Saalian glacial; MIS 6
		MFS	0.24	Medium	Onset of main pulse of interglacial MIS 7 MSF after glacial MIS 8
	MIS 8	SB	0.27	Medium	Glacial MIS 8.
		MFS	0.42	Medium	Interglacial MIS 11 MSF after glacial MIS 10
	MIS 12	SB	0.44	Major	Glacial MIS 12 (approx.) is a major peak.  Glacial MIS 10 and 14 are lesser shifts than MIS 12 or MIS 16, therefore are omitted here.
		MFS	0.62	Medium	Onset of major interglacial MIS 15 MSF after glacial MIS 16
	MIS 16	SB	0.64	Major	Glacial MIS 16 (approx.).  Glacial MIS 18 on isotope curve is lesser than either M22 or M16; therefore omitted here.
		MFS	0.84	Medium	Est. interglacial MSF after glacial MIS 22
	MIS 22	SB	0.86	Major	Glacial MIS 22.  Oldest major peak on O-18 curve.  Just below base of Brunhes Normal.  Was called "Oi 1" on SEPM chart, but Pleistocene subcomm doesn't recommend an "Ionian" stage for global use.
		MFS	0.95	Minor	SEPM chart has at approximate mid-point of Sequence "Cala 2".  This seems rather arbitrary, because a full suite of glacial/interglacial oscillations are underway; and a re-assignment to the mor pronounced interglacial MIS 25 (0.95 Ma; just above base of Jaramillo normal-polarity chron), which as a relatively higher "peak" suggesting increased highstand, is used here.  This also corresponds to base of Italian "Ionian Stage".
	MIS 52 (Cala 2)	SB	1.54	Medium	SEPM chart shows as slightly below (0.15 myr) Middle of Foram Zone N22a.  Uncertain re-calibration to marine isotope stages; but might be glacial MIS 52 (1.54 Ma), which has a slightly higher magnitude than adjacent peaks.
		MFS	1.64	Medium	SEPM chart places this MFS at about 0.05 myr above Cala 1 SB.   Uncertain re-calibration to marine isotope stages; but might be interglacial MIS 55-57 (~1.64-1.59 Ma) as appearing to be a more extended inter-glacial lowstand.  This also corresponds to approximate base of "Emilian substage" of Italian "Calabrian stage".
	MIS 58 (Cala 1)	SB	1.65	Medium	"SEPM chart seems to place as an arbitrarily 0.16 myr older than Cala 2 SB.  Assigned here as glacial MIS 58, which has a relatively greater "negative" shift, suggesting a more pronounced lowstand."
		MFS	1.76	Medium	SEPM chart displays as 0.05 myr below Cala 1 SB.  Assigned here to interglacial MIS 63, a more pronounced peak at end of Olduvai normal-polarity zone, which is aobut 0.1 myr older than major glacial MIS 58.
	Ge 2	SB	2.16	Medium	SEPM chart places as slightly above (0.13 myr) Middle of Nanno Zone NN18 or CN12d.  This is close to major glacial MIS 82 (2.16 Ma), which is used here.
		MFS	2.39	Medium	SEPM chart displays as 3/4ths from base of Ge 1 sequence.  Assigned here as interglacial MIS 89, which is the oldest of a set of relatively pronounced interglacials (and implied highstands).
	Ge 1	SB	2.50	Medium	Base Nanno Zone NN17 or CN12c  (LAD of nanno Discoaster surculus).  This corresponds closely to major glacial  MIS 100, and this assignment is used here.
		MFS	2.59	Medium	SEPM chart displays as 0.05 myr below Ge 1 SB.    Re-assigned here as interglacial MIS 103, a major and relatively extended interglacial (and implied lowstand) which defines base of Gelasian stage.  [NOTE:  The glacial MIS 110 (about 0.15 myr before MIS 103) is also a major lowstand, which could be inserted as an additional Sequence below this MFS].
	Pia 2	SB	2.80	Medium	Base Nanno Zone CN12b (LAD of nanno Discoaster tamalis).  Corresponds to glacial MIS 114.   Termination of Pliocene transgressive trend (due to onset of major glacials).
		MFS	2.92	Medium	SEPM chart displays as 3/4ths from base of Pia 1 sequence.  Marine isotope curve suggests this is a very broad highstand, and spans most of "Sequence Pia 1".  This highstand is termination of Pliocene transgressive trend; which is a "Medium" MSF on long-term trend.
	Pia 1	SB	3.27	Medium	Slightly below (0.05 myr) Middle of Nanno Zone CN12a (NN16a).  Corresponds to MIS "M2", which is the middle of subchron C2An.2r (Mammoth Reversed chron) in Italian cycle-strat section.
		MFS	3.98	Medium	Hardenbol's SEPM chart displays as only 0.03 above ZA 2 SB (nearly coincident with SB)
	Za 2	SB	4.01	Medium	SEPM chart displays as just below base of Nanno zone CN11 (=NN15 =LAD A. tricorniculatus).  Recalibration of this Nanno event to cycles places age significantly older (by 0.5 myr).  This correlation via Nannos could be a SB corresponding to Marine Isotope event N2 or N4, with ages of about 4.6 Ma.  Allternataively, the SB corresponds to event Gi16 at about 30% up in Chron C2Ar (middle of Nanno zone CN11b; at 4.0 Ma -- used here).  Need better information on primary calibration of this sequence boundary.
		MFS	4.57	Medium	Arbitrarily drawn as 3/4ths from base of Za 1 sequence
	Za 1	SB	4.62	Minor	SEPM chart could be interpreted as placement in Middle of Foram Zone PL1b; but revised correlation of Nanno zone CN11 would make same the higher Za 2 SB.  Therefore, a calibration relative to Nannos is used here:  4/5ths up in CN10c.  Perhaps the primary calibration is Marine Isotope event S16 or S14 (near middle of Nanno Zone 10c; 4.9 Ma)?
		MFS	5.47	Major	Middle of Nanno Zone CN10a
	Me 2	SB	5.77	Major	Middle of Nanno Zone NN11d (CN9d) = midway between LAD of nanno Discoaster quinqueramus and LAD of Amaurolithus amplificus.  This lowstand is minimum of Late Miocene regression; which is a "medium" SB on long-term scale.
		MFS	5.99	Medium	Just below (0.05 myr) Top of Nanno zone NN11c (top of CN9c = LAD N. amplificus).
	Tor 3/Me 1	SB	7.26	Minor	Slightly below (0.09 myr) middle of Nanno Zone NN11b (=CN9b) = midway between FADs of nanno N. amplificus and A. primus.
		MFS	7.72	Medium	2/3rds up in Nanno Zone NN11a (CN9a)
	Tor 2	SB	9.22	Minor	1/4 up in Nanno Zone NN10 (CN8)
		MFS	10.51	Major	Middle of Sequence Ser 4/Tor 1.  This flooding event is a major short transgression in Late Miocene; and indicated as "major" on long-term trend.
	Ser 4/Tor 1	SB	11.80	Major	0.1 myr above Base of Nanno Zone NN7 (CN5b; FAD D. kugleri -- which aslo coincided with Base of Foram Zone M11 =FAD G. nepenthes in Hardenbol chart; but this foram FAD is now placed 0.2 myr later).  Maximum regression of Middle Miocene trend.  Assigned as major SB for Long-Term trend.
		MFS	12.26	Minor	Middle of Sequence Ser 3
	Ser 3	SB	12.72	Minor	Middle of Nanno Zone NN6 (CN5a)
		MFS	13.12	Minor	Middle of Sequence Ser 2
	Ser 2	SB	13.53	Minor	Base of Nanno Zone NN6 (CN5a) LAD of Sphenolithus heteromorphus
		MFS	13.89	Medium	Middle of Sequence Lan 2/Ser 1
	Lan 2/Ser 1	SB	14.24	Major	FAD of foram Fohsella (Globorotalia) peripheroacuta (former "working definition" of base of Serravallian Stage; but current one is LAD of nanno S. heteromorphus = 13.65 Ma).
		MFS	15.71	Major	Middle of Sequence Bur 5/Lan 1.  Maximum transgression of Miocene.  But, ranked as "mediium" on long-term trends.
	Bur 5/Lan 1	SB	16.97	Medium	FAD of foram Praeorbulina (G.) sicana (= former "working definition of base of Langhian Stage, but but current one is base of Chron C5Br = 15.97 Ma)
		MFS	17.26	Major	Middle of Sequence Bur 4
	Bur 4	SB	17.54	Minor	Base Foram Zone N7 (M4) = LAD of foram Catapsydrax dissimilis (and also Globorotalia zealandica & G. semivera)
		MFS	17.83	Medium	Middle of Sequence Bur 3
	Bur 3	SB	18.12	Minor	In Hardenbol'98, an apparent equivalence was just above FAD of foram Globigerinatella insueta (base Foram Zone N6, M3) and mid-way in Nanno Zone CN2 (approx range of S. belemnos), but cycle-scaling of this Foram FAD and the Nanno LAD by Lourens et al (2004) with Atlantic ODP Sites is about 1 myr younger. The middle of Nanno Zone NN3 (midway between LADs of T. carinatus & S. belemnos) is used here; which is still 0.5 myr earlier than the lifted Foram FAD.
		MFS	18.64	Medium	Middle of Sequence Bur 2
	Bur 2	SB	19.17	Minor	There is no major Foram/Nanno zonal marker near this SB.  It is placed just above (0.1 myr) the mid-point of SBs Bur1 and Bur3.  This proportional placement is used here.
		MFS	19.80	Medium	Middle of Sequence Aq 3/Bur 2
	Aq 3/Bur 1	SB	20.43	Major	"Hardenbol et al (1998) assigned this as Base of Burdigalian Stage, which was placed at the FAD of Foram Globigerinoides altiaperturus by Berggren et al (1995); and has a cycle-calibrated age of 20.06 Ma in Lourens et al (2004).  The GTS2004 Neogene scale by Lourens et al use the FAD of Nanno H. ampliaperta; which is about 0.5 myr earlier; and is approximately at the historical base-Burdigalian.  This Nanno assignment is used here for the SB boundary, which is presumed to delineate the original Burdigalian."
		MFS	20.94	Minor	Middle of Sequence Aq 2
	Aq 2	SB	21.44	Minor	FAD of foram Globoquadrina dehiscens forma spinosa
		MFS	22.24	Major	Middle of Sequence Aq 1
	Ch 4/Aq 1	SB	23.03	Medium	Base of Miocene (= base of polarity Chron C6Cn.2n; FAD of nannofossil Sphenolithus capricornutus; oxygen isotope event Mi-1).  This base-Miocene is cycle-calibrated in Atlantic ODP Site 926.  SB is culmination of a Late Oligocene regressive trend; but ranked "medium" on long-term.
		MFS	23.94	Minor	Middle of Sequence Ch 3
	Ch 3	SB	24.84	Minor	Slightly younger (0.05 myr) than middle of Foram Zone P22
		MFS	26.17	Minor	Middle of Sequence Ch 2
	Ch 2	SB	27.50	Minor	Base of Nanno Zone NP25 (CP19a) = LAD of nanno Sphenolithes distentus
		MFS	27.97	Major	Middle of Sequence Ch 1.  This Sequence Ch 1 is a short, but significant oscillation of long-term sea-level.
	Ch 1/Ru 4	SB	28.45	Major	Base of Chattian stage (working definition has been LAD of Foram Chiloguembelina (top of Zone P21a); but is diachronous among basins.  Therefore, a temporary working definition is base of Chron C10n.1n (28.45 in GTS2004), and LAD of Chiloguembelina is assigned to this Chron boundary.  Major SB in Cenozoic.
		MFS	28.95	Major	Middle of Sequence Ru 3
	Ru 3	SB	29.45	Minor	FAD of foram Globigerina angulisuturalis
		MFS	30.72	Major	Slightly above (0.1 myr) middle of Sequence RU3; as is drawn by Hardenbol et al. 1998.  Culmination of long-term transgression of Late Eocene-Early Oligocene
	Ru 2	SB	32.19	Minor	Base of foram P19 zone (LAD of Pseudohastigerina sp.)
		MFS	32.61	Medium	Arbitrarily 0.1 myr below LAD of nanno Reticulofenestra umbilicus (low-mid latitude)/R. hillae
	Pr 4/Ru 1	SB	33.90	Medium	Base of Oligocene (LAD of Hankenina in Medit.)
		MFS	34.33	Minor	Middle of Sequence Pr 3
	Pr 3	SB	34.76	Minor	Just below (0.05 myr) the middle of Foram Zone P16
		MFS	34.96	Minor	Middle of Sequence Pr 2
	Pr 2	SB	35.17	Minor	Base Nanno Zone NP19 (CP15b) = FAD I. recurvus (but, as re-calibrated by ODP Leg 145, this event is ~1myr younger than in Berggren et al. 1995)
		MFS	36.20	Medium	Middle of Sequence Pr 1
	Pr 1	SB	37.24	Major	Base of Late Eocene (not defined, but working definition in Berggren et al was base of Nanno Zone NP18 = FAD C. oamaruensis; whereas GTS2004 used base Chron C17n.1n).  GTS2004 working definition used here, but neither might match actual SB level.  Assigned here as base of Priabonian for now.
		MFS	37.89	Minor	Middle of Sequence Bart 1
	Bart 1	SB	38.54	Minor	Arbitrarily 0.1 myr above midpoint between LADs of foram Acarinina primitiva and Subbotina frontosa
		MFS	39.71	Medium	Base of Nanno Zone NP17 (CP14b) = LAD C. solitus
	Lu 4	SB	41.67	Medium	Arbitrarily 0.05 m.y. above midpoint between FADs of foram Turborotalia pomeroli and Globigerapsis index.  Culmination of Middle-Eocene regression.
		MFS	41.94	Minor	FAD of foram Globigerapsis index
	Lu 3	SB	42.98	Medium	Middle of Nanno Zone NP15c
		MFS	44.36	Medium	Slightly below (.2 myr) midpoint of Sequence LU 2
	Lu 2	SB	45.35	Minor	Shown on Hardenbol chart as same level as base of Nanno Zone NP15b (CP13b) = FAD C. igas.
		MFS	47.03	Major	Arbitrarily2/3rds up in Nanno Zone NP14b (CP12b).  Termination of short Early Eocene transgression.
	Lu 1	SB	47.47	Major	Arbitrarily1/3rd up in Nanno Zone NP14b (CP12b)
		MFS	48.63	Minor	Midpoint of Sequence Yp 10 = approximate base of Lutetian Stage (working definition)
	Yp 10	SB	49.78	Major	Arbitrarily2/3rds up in Nanno Zone NP13 (CP11).  Culmination of Late Ypresian regression (major SB).
		MFS	49.95	Minor	Middle of Sequence Yp 9
	Yp 9	SB	50.13	Minor	Arbitrarily1/3rd up in Nanno Zone NP13 (CP11)
		MFS	50.60	Minor	Middle of Sequence Yp 8
	Yp 8	SB	51.07	Minor	5/6ths up in Foram Zone P7
		MFS	51.35	Minor	Middle of Sequence Yp 7
	Yp 7	SB	51.62	Minor	Just above (0.05 myr) middle of Foram Zone P7
		MFS	52.05	Minor	Middle of Sequence Yp 6
	Yp 6	SB	52.47	Minor	Slightly above (0.1 myr) base of Foram Zone P7 (FAD M. aragonensis)
		MFS	53.01	Minor	Middle of Sequence Yp 5.  End of Late Paleocene-earliest Eocene trangressive trend.
	Yp 5	SB	53.55	Minor	Middle of Foram  Zone P6b
		MFS	53.65	Minor	MFS is drawn on Hardenbol's chart just below (0.1 myr) SB Yp 5
	Yp 4	SB	54.09	Minor	Base Nanno Zone NP11 (CP9b) = LAD T. contortus
		MFS	54.54	Minor	Middle of Sequence Yp 3
	Yp 3	SB	54.99	Minor	Slightly above (0.1 myr) base of Foram Zone P6a (LAD M. velascoensis)
		MFS	55.09	Minor	Middle of Sequence Yp 2
	Yp 2	SB	55.19	Minor	Slightly below (0.1 myr) base of Foram Zone P6a (LAD M. velascoensis)  [same level as FAD of M. marginodentata]
		MFS	55.24	Major	Middle of Sequence Yp 1
	Th 7/Yp 1	SB	55.29	Minor	Yp 1 is a very brief Sequence on Hardenbol chart.  SB is just 0.1 myr older than SB Yp2 (or 0.2 myr older than base of Foram Zone P6a)
		MFS	55.64	Minor	Middle of Sequence Yp 0
	Th 6/Yp 0	SB	55.98	Minor	Slightly below (0.1 myr) middle of Foram Zone P5
		MFS	56.27	Minor	Middle of Sequence Th 5
	Th 5	SB	56.57	Major	Slightly above (0.1 myr) base of Foram Zone P5 (LAD Gl. pseudomenardii).  Termination of latest-Paleogene regressive trend.
		MFS	56.90	Minor	Middle of Sequence Th 4
	Th 4	SB	57.23	Major	Just below (0.05 myr) foram  Acarinina acarinata & mckannai LADs
		MFS	57.39	Minor	Middle of Sequence Th 3
	Th 3	SB	57.55	Minor	Just above (0.05 myr) middle of Foram Zone P4b
		MFS	57.89	Minor	Middle of Sequence Th 2
	Th 2	SB	58.23	Minor	Middle of Nanno Zone NP7 (CP6)
		MFS	58.78	Medium	Middle of Sequence Th 1 (approx.Top of Selandian stage working definition).  End of Selandian transgressive trend.
	Sel 2/Th 1	SB	59.32	Major	Slightly below (0.15 myr) base of Nanno Zone NP6 (=base CP5; FAD H. kleinpelli)
		MFS	60.39	Minor	Middle of Sequence Sel 1
	Sel 1	SB	61.45	Major	Slightly above (0.2 myr) base of Selandian Stage, or slightly below (0.2 myr) middle of Foram Zone P3a.  The later assignment is used here, because Selandian still lacks a ratified definition.  Culmination of Long-term Regression of latest Cretaceous-Danian.
		MFS	61.89	Minor	Middle of Sequence Da 4 (= approx. Top of Danian stage working definition)
	Da 4	SB	62.32	Major	Below (0.25 myr) base of Foram Zone P2
		MFS	62.81	Minor	Middle of Sequence Da 3
	Da 3	SB	63.29	Minor	Slightly above (0.15 myr) base of Foram Zone P1c (FAD G. compressa & P. inconstans)
		MFS	63.89	Minor	Middle of Sequence Da 2
	Da 2	SB	64.50	Minor	2/3rds up in Nanno Zone NP2 (CP1b)
		MFS	64.85	Minor	Middle of Sequence Da 1
	Da 1	SB	65.21	Minor	Middle of Nanno Zone NP1 (CP1a)
		MFS	66.45	Medium	Middle of Sequence Ma5.  Magnitude of MFS uncertain.
	Ma5	SB	67.70	Minor	Calibration uncertain; seems placed at base of polarity Chron C30n (although Hardenbol p.332 indicates these upper-Lower and Upper Maastrichtian sequences are calibrated to belemnite zones from type area in The Netherlands and Belgium)
		MFS	68.01	Medium	Middle of Sequence Ma4.  Magnitude of MFS uncertain.
	Ma4	SB	68.33	Medium	Base of Jeletzkytes nebrascensis ammonite zone (or about 2/3rds up in B. tegulatus/junior belemnite subzone).
		MFS	68.78	Medium	Middle of Sequence Ma3.  Magnitude of MFS uncertain.
	Ma3	SB	69.23	Medium	Base of Belemnitella junior belemnite zone (base of classical "Upper Maastrichtian")
		MFS	69.46	Major	Middle of Sequence Ma2.  Magnitude of MFS uncertain.
	Ma2	SB	69.68	Major	Base of Belemnella simbrica belemnite zone (approx. middle of Baculites grandis ammonite zone)
		MFS	70.12	Medium	Middle of Sequence Ma1.  Magnitude of MFS uncertain.
	Ma1	SB	70.56	Minor	Base of Baculites baculus ammonite zone (but could be as high as middle of zone ~0.25myr higher)
		MFS	71.04	Medium	Base of Baculites eliasi ammonite zone (base of former "Maastrichtian" in  N.Amer. Ammonite zone scheme).  Magnitude is uncertain.
	Cam9	SB	72.78	Major	Base of Baculites cuneatus ammonite zone (but could be as high as middle of following B. reesidei zone; ~0.75 myr higher!)
		MFS	74.26	Major	Middle of Cam8 sequence.
	Cam8	SB	75.74	Minor	Base of Didymoceras stevensoni ammonite zone.
		MFS	76.37	Minor	Middle of Cam7 sequence. Magnitude uncertain.
	Cam7	SB	77.00	Minor	Base of Baculites scotti ammonite zone.
		MFS	77.30	Minor	Middle of Cam6 sequence. Magnitude uncertain.
	Cam6	SB	77.59	Medium	Base of Baculites gregoryensis ammonite zone.
		MFS	78.80	Major	Middle of Cam5 sequence.
	Cam5	SB	80.00	Major	Base of Baculites asperiformis ammonite zone.
		MFS	80.18	Minor	Middle of Cam4 sequence.  Magnitude uncertain.
	Cam4	SB	80.35	Medium	Base of Baculites maclearni ammonite zone.
		MFS	80.63	Minor	Middle of Cam3 sequence.  Magnitude uncertain.
	Cam3	SB	80.91	Minor	Base of Baculites sp. (weak flank ribs) ammonite zone.
		MFS	81.27	Medium	Middle of Cam2 sequence.  Magnitude uncertain.
	Cam2	SB	81.63	Major	Base of Scaphites hippocrepis III ammonite zone.
		MFS	82.37	Medium	Middle of Cam1 sequence.  Magnitude uncertain.
	Cam1	SB	83.10	Minor	2/3rds up in Scaphites leei III ammonite zone.
		MFS	83.53	Major	Base of Scaphites leei III ammonite zone (= base of Campanian stage in N.Amer. scheme).  Magnitude uncertain.
	Sa3	SB	83.99	Major	Base of Desmoscaphites bassleri ammonite zone.
		MFS	84.15	Minor	Middle of Desmoscaphites erdmanni ammonite zone.
	Sa2	SB	84.62	Minor	Base of Clioscaphites choteauensis ammonite zone.
		MFS	85.25	Minor	Approx. 2/3rds up in Clioscaphites saxitonianus ammonite zone.
	Sa1	SB	85.55	Minor	Approx. 1/3rd up in Clioscaphites saxitonianus ammonite zone.
		MFS	86.25	Medium	Middle of C01 sequence.  Magnitude uncertain.
	Co1	SB	86.96	Minor	Base of Scaphites depressus-Protexanites bourgeoisianus ammonite zone.
		MFS	87.88	Medium	Base of Scaphites ventricosus ammonite zone.  Magnitude uncertain.
	Tu4	SB	89.54	Major	2/3rd up in Subprionocyclus neptuni ammonite zone (Tethyan)
		MFS	89.78	Minor	Middle of Subprionocyclus neptuni ammonite zone (Tethyan)
	Tu3	SB	90.89	Major	Base of Romaniceras deverianum  ammonite zone (Tethyan)
		MFS	90.99	Medium	Just below (0.1 myr) base of Romaniceras deverianum ammonite zone (Tethyan)
	Tu2	SB	91.21	Minor	Just above (0.1 myr) base of Romaniceras ornatissimum ammonite zone (Tethyan)
		MFS	91.41	Medium	Just below (0.1 myr) base of Romaniceras ornatissimum ammonite zone (Tethyan)
	Tu1	SB	92.60	Major	Just above (0.1 myr) base of Mammites nodosoides ammonite zone (Tethyan)
		MFS	93.13	Major	Middle of Watinoceras devonense  ammonite zone (Tethyan)
	Ce5	SB	94.19	Minor	Near or just below base of Metoicoceras geslinianum ammonite zone -- not well-correlated among provinces or to dated N.Amer. Zones.  Following approximate positioning in Hardenbol summary chart, this level is assigned as the base of the N.Amer. Ammonite zone below base-Sciponoceras gracile zone.
		MFS	94.75	Major	Top of Acanthoceras jukesbronei ammonite zone (top of "Middle" Cenomanian)
	Ce4	SB	95.37	Minor	Middle of Acanthoceras rhotomagense  ammonite zone (base of acutus s.z.)  (Tethyan)
		MFS	95.69	Minor	Approx. in middle of Ce3 sequence
	Ce3	SB	96.01	Major	Base of Cunningtoniceras inerme ammonite zone (Tethyan) = base of "Middle" Cenomanian
		MFS	97.21	Medium	1/3rd up in Mantelliceras dixoni ammonite zone (Tethyan)
	Ce2	SB	97.96	Minor	Just below (0.15 myr) the base of Mantelliceras dixoni ammonite zone (Tethyan)
		MFS	98.24	Medium	Middle of Mantelliceras saxbii subzone of Mantelliceras mantelli ammonite zone.
	Ce1	SB	98.67	Medium	Base of Mantelliceras saxbii subzone of Mantelliceras mantelli ammonite zone.
		MFS	98.82	Major	Below (0.15 myr) base of Mantelliceras saxbii subzone of Mantelliceras mantelli ammonite zone.
	Al 11	SB	99.69	Major	Below (0.15 myr) base of Mantelliceras mantelli ammonite zone (Tethyan) = upper Stoliczkaia dispar zone of uppermost Albian.
		MFS	100.27	Minor	Base of Mortoniceras (Durnovarites) perinflatum subzone of S. dispar ammonite zone.
	Al 10	SB	100.94	Minor	Base of Stoliczkaia dispar ammonite zone.
		MFS	101.62	Medium	Middle of sequence Al 9.
	Al 9	SB	102.31	Medium	Base of Callihoplites auritus ammonite subzone (uppermost  Mortoniceras inflatum  ammonite zone).
		MFS	103.68	Major	Base of Hysteroceras varicosum ammonite subzone (upper  Mortoniceras inflatum  ammonite zone).
	Al 8	SB	105.05	Minor	Base of Hysteroceras orbigyni ammonite subzone (upper  Mortoniceras inflatum  ammonite zone).
		MFS	105.74	Medium	Middle of sequence Al 7.
	Al 7	SB	106.42	Major	Base of Diploceras cristatum  ammonite subzone (upper  Mortoniceras inflatum  ammonite zone).
		MFS	107.01	Major	Base of Euhoplites loricatus ammonite zone (Boreal).
	Al 6	SB	107.94	Medium	Just below (0.05 myr) base of Dimorphoplites niobe subzone of Euhoplites loricatus ammonite zone (Boreal).
		MFS	108.06	Medium	Middle of sequence Al 5.
	Al 5	SB	108.18	Major	Base of Anahoplites intermedius subzone of Euhoplites loricatus ammonite zone (Boreal).
		MFS	108.70	Major	Middle of sequence Al 4.
	Al 4	SB	109.21	Medium	Below (0.15 myr) base of Pseudosonneratia (Isohoplites) steinmanni subzone of Douvilleiceras mammillatum ammonite zone (Boreal).
		MFS	109.70	Medium	Just above (0.05 myr) base of Protohoplites puzosianus subzone of Douvilleiceras mammillatum ammonite zone (Boreal).
	Al 3	SB	110.48	Minor	Just above (0.05 myr) base of Sonneratia kitchini subzone of Douvilleiceras mammillatum ammonite zone (Boreal).
		MFS	110.73	Medium	Middle of sequence Al 2.
	Al 2	SB	110.97	Medium	Middle of Leymeriella regularis subzone of Leymeriella tardefurcata ammonite zone (Boreal).
		MFS	111.12	Medium	Base of Leymeriella regularis subzone of Leymeriella tardefurcata ammonite zone (Boreal).
	Al 1	SB	111.36	Medium	Just above (0.05 myr) middle of Leymeriella acuticostata s.z. of Leymeriella tardefurcata ammonite zone (Boreal).
		MFS	111.71	Major	Base of farnhamensis subzone (= lower Leymeriella acuticostata s.z) of Leymeriella tardefurcata ammonite zone (Boreal).
	Ap6	SB	112.40	Major	Just above (0.10 myr) middle of Hypacanthoplites jacobi ammonite zone (Boreal).
		MFS	114.00	Medium	Base of Hypacanthoplites rubricosus subzone of Nolaniceras nolani ammonite zone (Boreal); however, exact MFS is uncertain.
	Ap5	SB	117.85	Medium	Above (0.15 myr) base of Parahoplites nutfieldiensis ammonite zone (Boreal).
		MFS	119.50	Medium	Middle of Parahoplites nutfieldiensis ammonite zone (Boreal); but exact MFS is uncertain.
	Ap4	SB	121.00	Major	Base of Cheloniceras (Epicheloniceras) martinoides ammonite zone (Boreal).
		MFS	122.93	Major	Base of Deshayesites deshayesi ammonite zone (Boreal).
	Ap3	SB	123.97	Major	Base of Deshayesites forbesi ammonite zone (Boreal).
		MFS	124.32	Medium	Just below (0.05 myr) middle of sequence Ap 2.
	Ap2	SB	124.58	Minor	Just below (0.1 myr) top of Prodeshayesites bodei subzone of Prodeshayesites fissicostatus ammonite zone = basal subzone of "classical" Aptian.
		MFS	124.79	Minor	Middle of sequence Ap1
	Ap1	SB	125.00	Medium	Base of Prodeshayesites fissicostatus ammonite zone = base of "classical" Aptian.
		MFS	125.40	Medium	2/3rds up in sequence Barr6.
	Barr6	SB	126.20	Medium	Just below (0.1 myr) top of I. giraudi ammonite zone (Tethyan).
		MFS	126.65	Major	Approximately at base of I. giraudi  ammonite zone (Tethyan).
	Barr5	SB	127.75	Medium	Base of Hemihoplites sartousi ammonite zone (Tethyan).
		MFS	127.95	Minor	Approx. 2/3rds up in sequence Barr4.
	Barr4	SB	128.35	Major	Just below (0.05 myr) top of Holcodiscus caillaudianus ammonite zone (Tethyan).
		MFS	128.49	Major	Middle of upper half ("moutoniceras subzone) of Holcodiscus caillaudianus ammonite zone (Tethyan).
	Barr3	SB	128.63	Medium	Base of upper half ("moutoniceras subzone) of Holcodiscus caillaudianus ammonite zone (Tethyan).
		MFS	128.79	Medium	Approx. 2/3rds up in sequence Barr2.
	Barr2	SB	129.12	Medium	Below (0.15 myr) base of Holcodiscus caillaudianus ammonite zone (Tethyan).
		MFS	129.30	Medium	Middle of Nicklesia nicklesi ammonite zone (Tethyan).
	Barr1	SB	129.64	Major	Base of Nicklesia nicklesi ammonite zone (Tethyan).
		MFS	129.85	Minor	Approxmately at middle of sequence Ha7
	Ha7	SB	130.07	Minor	Just below (0.10 myr) base of Spitidiscus hugii ammonite zone (Tethyan) = 0.10 myr below top of "classic" Hauterivian.
		MFS	131.04	Major	Approxmately at middle of sequence Ha6
	Ha6	SB	132.01	Medium	Just below (0.10 myr) base of Pseudothurmannia angulicostata auct. ammonite zone (Tethyan).
		MFS	132.20	Minor	Approx. 2/3rds up in sequence Ha5.
	Ha5	SB	132.56	Medium	Base of B. balearis ammonite zone (Tethyan).
		MFS	132.75	Medium	MFS is placed in upper 1/5th of Ha4 sequence on Hardenbol's SEPM chart.
	Ha4	SB	133.53	Medium	Middle of Subsaynella sayni ammonite zone (Tethyan).
		MFS	133.78	Medium	Approx. 2/3rds up in sequence Ha3
	Ha3	SB	134.29	Medium	Approximately 1/3rd up in Lyticoceras nodosoplicatus ammonite zone (Tethyan).
		MFS	134.64	Medium	Approx. 3/4ths up in sequence Ha2.
	Ha2	SB	135.70	Medium	Just above (0.10 myr) base of Crioceratites loryi ammonite zone (Tethyan).
		MFS	135.75	Major	Just below (0.05 myr) top of sequence Ha1.
	Ha1	SB	136.22	Minor	Just below (0.10 myr) middle of Acanthodiscus radiatus ammonite zone (Tethyan).
		MFS	136.32	Major	Just below (0.1 myr) top of sequence Va7.
	Va7	SB	136.96	Medium	Just below (0.10 myr) middle of Neocomites (Teschenites) pachydicranus ammonite zone (Tethyan).
		MFS	137.22	Medium	Middle of sequence Va6
	Va6	SB	137.48	Minor	Middle of upper half of Himantoceras trinodosum subzone of Neocomites (Teschenites) pachydicranus ammonite zone (Tethyan).
		MFS	137.63	Medium	Approximately 0.15 myr below SB of seqeunce Va6.
	Va5	SB	137.83	Minor	Essentially the SB is just 0.35 myr below the SB of sequence Va6.
		MFS	138.06	Medium	Middle of sequence Va4.
	Va4	SB	138.29	Minor	Just below (0.05 myr) the middle of the Varlheideites peregrinus subzone (or horizon) of the upper-third of Saynoceras verrucosum ammonite zone (Tethyan).
		MFS	138.62	Minor	Just below (0.10 myr) the base of the Karadaschiceras pronocostatum; subzone (or horizon) of the middle-third of Saynoceras verrucosum ammonite zone (Tethyan).
	Va3	SB	138.94	Medium	Base of Saynoceras verrucosum ammonite zone (Tethyan).
		MFS	139.35	Minor	Approximately middle of sequence Va2.
	Va2	SB	139.77	Major	Base of Thurmanniceras campylotoxus ammonite zone (Tethyan).
		MFS	139.98	Minor	Approximately middle of sequence Va2.
	Va1	SB	140.18	Medium	Base of Thurmanniceras pertransiens ammonite zone (Tethyan).
		MFS	140.42	Minor	Approximately middle of Thurmanniceras otopeta ammonite zone (Tethyan).
	Be8	SB	140.95	Medium	Middle of Tirnovella alpillensis subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
		MFS	141.08	Minor	Approximately 2/3rds up in sequence Be7.
	Be7	SB	141.33	Medium	Middle of upper half of Tirnovella picteti subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
		MFS	141.40	Minor	Middle of Tirnovella picteti subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
	Be6	SB	141.55	Medium	Base of Tirnovella picteti subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
		MFS	141.74	Minor	Middle of sequence Be5
	Be5	SB	141.93	Medium	Middle of Malbosiceras paramimounum subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
		MFS	142.12	Medium	Middle of lower-half of Malbosiceras paramimounum subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).
	Be4	SB	142.96	Major	Base of Berriasella privasensis subzone of Turnovella (Subthurmannia) occitanica ammonite zone (Tethyan).
		MFS	143.12	Major	Just above (0.10) middle of sequence Be3.
	Be3	SB	143.48	Medium	Above (0.20 myr) base of Turnovella subalpina subzone of Turnovella (Subthurmannia) occitanica ammonite zone (Tethyan).    [NOTE: initial age is different from "SEPM", because I am using magnetic-chron calibration.]"
		MFS	144.10	Medium	Middle of sequence Be2.  Placement and magnitude is uncertain.
	Be2	SB	144.72	Minor	Just above (0.10 myr) base of Pseudosubplanites grandis subzone of Berriasella jacobi ammonite zone (Tethyan) = base of "classic" Berriasian.  [NOTE: initial age is different from "SEPM", because I am using magnetic-chron calibration.]
		MFS	145.09	Medium	Middle of sequence Be1.  Placement and magnitude is uncertain.
	Be1	SB	145.46	Major	Base of Berriasella jacobi ammonite zone (Tethyan) = base of "classic" Berriasian.
		MFS	145.75	Medium	Middle of Ti5 sequence
	Ti 5	SB	146.04	Medium	Slightly (0.1 myr) above base of Durangites.  Peak of regression in Tithonian
		MFS	146.35	Minor	About 2/3rds up in Ti4 (SEPM shows that lower 1/3r is extended LST)
	Ti 4	SB	146.96	Major	Base of P. transitorius
		MFS	147.16	Medium	Base of Simplisphinctes
	Ti 3	SB	147.66	Major	1/4 from top of Simolytoceras admirandum + S. biruncinatum
		MFS	147.85	Minor	Middle of Simolytoceras admirandum + S. biruncinatum Zone
	Ti 2	SB	148.61	Medium	Middle of Richterella richteri Zone
		MFS	148.79	Medium	1/4 up within Richterella richteri Zone
	Ti 1	SB	150.37	Major	Middle of Hybonoticeras hybonotum Zone
		MFS	150.77	Medium	Middle of Kim 5
	Kim 5	SB	151.07	Medium	Middle of upper subzone (setatum) of Hybonoticeras beckeri Zone
		MFS	152.39	Major	Middle of Aulacostephanus (Pseudomutabilis) eudoxus.  Peak of maximum flooding in Kimm (and in Late Jurassic)
	Kim 4	SB	152.49	Medium	0.1 myr above base of Aulacostephanus (Pseudomutabilis) eudoxus.
		MFS	152.83	Medium	Middle of Kim 3
	Kim 3	SB	153.16	Medium	0.1 myr above base of Aspidoceras acanthicum Zone
		MFS	153.31	Medium	1/4 from base of Divisum Zone
	Kim 2	SB	153.77	Medium	Middle of  Hypselocyclum/Strombecki Zone
		MFS	154.15	Medium	Very close (~0.05 myr) to Kim 1 SB
	Kim 1	SB	154.20	Minor	Middle of O. desmoides s.z. (middle of S. playynota Zone)
		MFS	154.53	Minor	Base of S. playnota
	Ox8	SB	155.35	Medium	Base of I. planula Zone
		MFS	155.49	Medium	Middle of Epipeltoceras bimammatum  (Taramelliceras hauffianum s.z.)
	Ox7	SB	156.09	Medium	Base of  E. bimammatum  subzone (middle of E. bimammatum Zone)
		MFS	156.45	Minor	Base of berrense s.z. of E. bimammatum Zone.
	Ox6	SB	157.04	Major	Middle of Perisphinctes (Di.) grossouvrei s.z. of Perisphinctes (D.) bifurcatus Zone = Peak lowstand of Oxfordian
		MFS	157.73	Minor	Base of rotoides s.z. (uppermost G. transversarium  Zone)
	Ox5	SB	158.06	Medium	Base of  luciaeformis/wartae s.z. of G. transversarium Zone (top of P. parandieri s.z.)
		MFS	158.43	Medium	Base of P. parandieri s.z.
	Ox4	SB	158.53	Medium	0.1 myr below top of Perisphinctes (Arisphinctes) plicatilis
		MFS	158.94	Minor	Base of P. (D.) antecedens s.z. of P. (A.) plicatilis Zone
	Ox3	SB	159.28	Medium	Middle of Cardioceras vertebrale s.z. of P. (A.) plicatilis Zone
		MFS	159.61	Medium	Base of P. (A.) plicatis Zone
	Ox2	SB	160.06	Medium	Middle of  Cardioceras costicardia s.z. of C. cordatum  Zone
		MFS	160.46	Medium	Middle of Cardioceras bukowskii s.z. of C. cordatum Zone
	Ox1	SB	160.77	Medium	Middle of Cardioceras praecordatum s.z. of Quenstedtoceras mariae Zone
		MFS	160.89	Medium	Top of Cardioceras scarburgense s.z. of Q. mariae Zone
	Ox0	SB	161.21	Minor	Base of Q. mariae Zone
		MFS	161.51	Medium	Middle of Q. (L.) lamberti s.z. of Quenstedtoceras (L.) lamberti Zone = Peak of major transgression in Callov-Oxf
	Call5	SB	162.01	Medium	Base of Q. (L.) lamberti Zone
		MFS	162.26	Major	Middle of trezeense s.z. of P. athleta Zone
	Call4	SB	162.69	Medium	Base of waageni s.z. (middle E. coronatum Zone)
		MFS	162.78	Medium	Middle of  baylei s.z. (lower E. coronatum Zone)
	Call3	SB	163.20	Medium	Base of R. anceps Zone
		MFS	163.37	Medium	Base of patina s.z. (uppermost Gracilis Zone)
	Call2	SB	163.71	Medium	Base of michalskii s.z. (middle of Gracilis Zone)
		MFS	163.88	Medium	Base of laugieri s.z. (middle of Gracilis Zone)
	Call1	SB	164.23	Major	Base of M. gracilis zone
		MFS	164.40	Medium	1/3 from top of B. bullatus zone
	Call0	SB	164.74	Minor	Base of B. bullatus (Base of Callovian)
		MFS	164.84	Medium	Middle of C. discus s.z. (just below top of C. discus zone)
	Bat5	SB	164.93	Major	Base of C. discus s.z. (or middle of C. discus zone)
		MFS	165.13	Minor	Base of C. discus Zone
	Bat4	SB	165.52	Medium	Base of lower blanazense s.z. of P. retrocostatum Zone
		MFS	165.98	Minor	2/3 from top of bremeri zone
	Bat3	SB	166.21	Medium	Middle of Morrisiceras (Morrisiceras) morrisi zone = Peak of regression in Bathonian
		MFS	166.50	Minor	Base of T. subcontractus Zone
	Bat2	SB	166.70	Medium	Middle of P. progracilis Zone
		MFS	166.89	Medium	Base of P. progracilis Zone
	Bat1	SB	167.09	Medium	Base of A. teniuplicatus s.z. (middle of P. aurigerus Zone)
		MFS	167.48	Major	Base of M. macrescens s.z. (middle of Z. zigzag Zone) [underlying uppermost Bajocian is often an extended lowstand or hiatus]
	Bj5	SB	167.97	Major	Middle of Parkinsonia parkinsoni zone
		MFS	168.12	Major	1/4 from base of Parkinsonia parkinsoni zone = Peak of transgression in Bajocian-Bathonian
	Bj4	SB	169.05	Major	Base of "schroederi" s.z. of S. niortense Zone.  Overlying G. garantiana Zone is often an extended lowstand hiatus.
		MFS	169.25	Minor	Middle of Strenoceras niortense zone
	Bj3	SB	169.84	Major	Base of S. niortense Zone
		MFS	170.03	Major	Base of S. humpriesianum s.z. in middle of S. humpriesianum Zone
	Bj2	SB	170.62	Medium	Base of E. sauzei Zone
		MFS	171.01	Minor	Base of Witchellia laeviuscula s.z. (lower W. laeviuscula Zone)
	Bj1	SB	171.60	Major	Base of H. discites Zone (top of Aalenian) .  Overlying basal Bajocian is often an extended lowstand hiatus.
		MFS	172.04	Medium	Base of G. formosus zone (middle of Graphoceras concavum Zone)
	Aa2	SB	173.38	Major	Base of B. bradfordensis Zone = Peak of regression in Middle and Early Jurassic!
		MFS	173.82	Minor	Base of L. murchisonae s.z. (upper L. murchisonae Zone)
	Aa1	SB	174.93	Major	Middle of bifidatum s.z. of Leioceras opalinum Zone
		MFS	175.16	Minor	Base of bifidatum s.z. (middle of L. opalinum Zone)
	Toa7	SB	176.09	Medium	Base of fluitans s.z. (middle of P. aalensis Zone)
		MFS	176.58	Medium	Base of P. aalensis Zone
	Toa6	SB	178.30	Medium	Middle of E. insigne s.z. (lower P. dispansum Zone)
		MFS	178.79	Minor	Middle of Pseudogrammoceras fallaciosum s.z. (upper Grammoceras thouarsense Zone)
	Toa5	SB	179.62	Medium	0.1 myr below top of G. thouarsense s.z. (middle of G. thouarsense Zone)
		MFS	180.63	Medium	Top of Haugia variabilis subzone (middle of H. variabilis Zone)
	Toa4	SB	180.95	Medium	Base of H. bifrons subzone (middle of H. bifrons Zone)
		MFS	181.01	Major	Middle of lusitanicum s.z. (middle of H. bifrons Zone)
	Toa3	SB	181.13	Minor	Just below (0.05 myr) base of lusitanicum s.z. (lower H. bifrons Zone)
		MFS	181.20	Medium	Base of H. bifrons Zone = Peak of major transgression in Middle Jurassic
	Toa2	SB	182.30	Medium	0.1 myr below base of H. pseudoserpentinum s.z. (lower H. serpentinum Zone)
		MFS	182.45	Major	Middle of strangewaysi (levisoni) s.z. (lower H. serpentinum Zone)
	Toa1	SB	182.85	Minor	0.15 myr below top of Dactylioceras tenuicostatum zone
		MFS	182.93	Medium	Base of D. clevelandicum s.z. (lower Dactylioceras tenuicostatum Zone)
	PI 8	SB	183.10	Medium	0.1 myr below base of Toarcian =  Peak lowstand at Pliensbachian/Toarcian boundary
		MFS	183.80	Medium	Base of emaciatum Zone
	PI 7	SB	184.81	Medium	base of bertrandi s.z. (lower algovianum Zone)
		MFS	185.42	Minor	Middle of PL 6
	PI 6	SB	186.03	Minor	Base of conracaldense s.z. (middle of lavinianum Zone)
		MFS	186.24	Major	3/4 up in PI 5 sequence;  Peak of transgression in early Pliensbachian.
	PI 5	SB	186.85	Minor	Just above (.1 myr) the top of Prodactylioceras davoei zone
		MFS	186.91	Medium	1/4 way from SB PI 5 to SB PI 4
	PI 4	SB	187.08	Minor	Middle of Oistoceras figulinum s.z (upper Prodactylioceras davoei Zone)
		MFS	187.31	Medium	1/3rd up in Pl 3 sequence.
	PI 3	SB	187.43	Medium	Just above (0.05 myr) the base of capricornus s.z. (lower P. davoei Zone)
		MFS	187.75	Minor	Base of P. davoie Zone
	PI 2	SB	188.41	Major	Base of T. ibex Zone  (lower half of T. ibex is a long lowstand and common hiatus = Peak of major lowstand in Early Jurassic
		MFS	188.67	Medium	Middle of Uptonia jamesoni s.z. (upper Uptonia jamesoni Zone)
	PI 1	SB	189.20	Medium	Base of P. brevispina s.z. (lower U. jamesoni Zone)
		MFS	189.40	Minor	Middle of Phricodoceras taylori s.z. (lower U. jamesoni Zone)
	Si 5	SB	190.01	Medium	Base of Paltechioceras aplanatum s.z. (upper E. raricostatum Zone)
		MFS	190.61	Medium	Middle of E. raricostatum s.z. (middle E. raricostatum Zone)
	Si 4	SB	191.63	Medium	Base of O. oxynotum s.z. (middle of Oxynoticeras oxynotum Zone)
		MFS	192.04	Major	Base of Oxynoticeras oxynotum Zone
	Si 3	SB	193.35	Medium	0.1 myr below base of A. obtusum Zone
		MFS	193.79	Major	2/3rds up in Caenisites turneri s.z. (lower C. turneri Zone) = Peak of major transgression in Early Jurassic
	Si 2	SB	194.47	Medium	Base of E. sauzeanum s.z. (upper A. semicostatum Zone)
		MFS	194.88	Major	Base of A. scipionianum s.z. (middle of A. semicostatum Zone)
	Si 1	SB	195.49	Medium	Middle of Arietites bucklandi subzone (upper Arietites bucklandi Zone)
		MFS	196.09	Medium	Base of C. rotiforme s.z. (lower A. bucklandi Zone)
	He3	SB	196.89	Medium	Base of S. complanata s.z. (middle of S. angulata Zone)
		MFS	197.86	Major	Middle of Alsatites laqueus s.z. (middle of A. liasicus Zone)
	He2	SB	198.44	Medium	Base of A. liasicus Zone
		MFS	199.02	Medium	Middle of P. planorbis zone (middle of Caloceras johnstoni s.z.)
	He 1.1	SB	199.21	Minor	Base of Caloceras johnstoni s.z. (lower Psiloceras planorbis Zone)
		MFS	199.41	Minor	Middle of He1 sequence
	He 1	SB	199.60	Minor	Base of Psiloceras planorbis Zone (= base of Jurassic)
		MFS	199.94	Medium	Middle of Sequence Rh2
	Rh2	SB	200.27	Minor	Middle of Choristoceras marshi subzone
		MFS	200.81	Medium	Just above (10% up) the base of C. marshi s.z.
	Rh1	SB	201.62	Medium	Middle of Vandaites stuerzenbaumi subzone
		MFS	202.29	Medium	Base of Vandaites stuerzenbaumi subzone
	No2	SB	205.56	Major	Just above (0.15 myr) the base of Sag. quinquepunctatus s.z.  Peak Regression of Middle-Late Triassic major trend.
		MFS	207.57	Minor	Base of Halorites macer zone
	No1	SB	211.48	Medium	Shortly before (0.20 myr) the top of Juvavites magnus Zone (just below top of Lacian substage)
		MFS	216.53	Medium	Base of G. jandianus Zone (base of Norian)
	Car4	SB	218.13	Medium	Middle of D. plinii s.z.
		MFS	219.42	Major	1/3rd up in Tropites subbullatus zone.  Peak of short, but major Transgressin in Late Carnian.
	Car3	SB	221.39	Major	3/4ths up in Tropites dilleri zone.  A short, but major transgressive event follows this lowstand.  This major transgression is interpreted to begin earlier in Boreal series (one sequence earlier).
		MFS	222.26	Medium	1/4th up in Tropites dilleri zone
	Car2	SB	224.13	Medium	Just above (0.05 myr) base of Neoprotrachyceras s.z.
		MFS	226.30	Medium	Middle of Trachyceras aonoides subzone.  Peak of Late Ladinian through early Carnian transgression
	Car1	SB	227.96	Medium	Just above (0.5 myr) base of T. aon s.z. (base of Carnian)
		MFS	228.96	Minor	2/3rds up in F. regoledanus s.z.
	Lad3	SB	229.64	Major	3/4ths up in P. neumayri s.z.  Peak Lowstand of Ladinian regressive trend.
		MFS	230.83	Minor	3/5ths up in P. longobardicum s.z.
	Lad2	SB	232.51	Minor	Middle of "Eoprotrachyceras" gredleri subzone
		MFS	234.66	Medium	Just below (0.1 myr) the top of the Eoprotrachyceras curionii Zone (just below base of Longobardian substage)
	Lad1	SB	235.17	Minor	Middle of A. recubariensis s.z.
		MFS	237.50	Major	Middle of C. chiesense s.z.  Peak flooding of long-term Early Triassic transgression.  This peak is interpreted as later (one higher MFS = base of T. poseidon Zone) in Boreal realm.
	An4	SB	240.38	Medium	Just below (0.5 myr) the top of Reitziites reitzi subzone
		MFS	241.10	Medium	2/3rds up in Paraceratites trinodosus subzone
	An3	SB	241.50	Medium	Just above (0.1 myr) base of Paraceratites Zone
		MFS	242.04	Medium	Middle of B. balatonicus subzone
	An2	SB	242.88	Medium	Just above (0.05 myr) middle of Aghdarbandites ismidicus subzone
		MFS	243.28	Minor	1/3rd up in "unnamed" s.z. of lower Kocaelia Zone
	An1	SB	243.68	Medium	Base of Kocaelia Zone (base of Bithynian substage)
		MFS	244.57	Minor	2/5ths up in Paracrochordiceras Zone
		SB	245.35	Medium	Middle of "gap zone" above Toziceras pakistanum zone
	Ol 4	MFS	245.41	Medium	1/3rd up in "gap zone" above Toziceras pakistanum zone.  Peak of short, but major Regression at end of Early Triassic.  In Boreal realm, this short-major Regression is assigned as spanning most of the Smithian stage instead; implies peak Regression at Ol 1, and the culmination of the underlying transgression at mid-Hedenstroemi Zone.  This fits Arctic better?
	Ol 3	SB	246.63	Medium	Base of T. pakistanum Zone
		MFS	246.92	Medium	3/5ths up I Sequence Ol 2.  Peak flooding of Transgressive trend of Early Triassic.
	Ol 2	SB	247.35	Medium	Middle of Tirolites cassianus zone
		MFS	247.92	Minor	Middle of Sequence Ol 1
	Ol 1	SB	248.08	Major	Base of Tirolites cassianus zone = Base of Spathian
		MFS	248.50	Minor	Middle of Wasatchites spiniger + A. pluriformis + A. prahlada zone
	In2	SB	249.98	Medium	Middle of F. rohilla Zone
		MFS	250.22	Major	Base of F. rohilla Zone
	In1	SB	250.34	Medium	1/5th up in Gyronites frequens Zone (nearly base of Dienerian)
		MFS	251.25	Major	91% above base in Changhsingian Stage.  Haq (GeoArabia) chart displays as medium; but general P/T geology hints at a more major change; therefore magnitude here is -130 m, instead of -125 m from Haq chart. The splice to SEPM base-Triassic from the Haq'05 GeoArabia Paleozoic curve causes an oddity, because Haq'05 didn't display the next MFS as returning to his long-term curve, whereas SEPM was offsets from the long-term.  This causes a possible artifact of a major MFS at basal Triassic, more than either Haq'05 or SEPM'98 is implying.  Therefore, I have "lowered" the next MFS and LST values (in Red) by an additional 20m and  10m respectively to partly offset this anomaly.
	Chang1	SB	251.76	Minor	73% above base in Changhsingian Stage


Late Paleozoic Sequences - Classic literature	sequence				off	Permian = Ross and Ross (1995a,b); Carboniferous = Ross and Ross (1988, 1987) modified after Heckel et al, 2005; Devonian = Johnson et al. (1985)
		MFS	251.00	Medium	Highstand of Changhsing-1 is not attained on Ross-Ross chart, but have arbitrarily placed at end of GSSP-defined Permian here.
	Chang-2?	SB	252.23	Minor	Ross-Ross (Permian'95) shows as base of C. deflecta - C. subcarinata Conodont zone, or Paratirolites kitti Ammonite zone (used here).
		MFS	253.02	Minor	Highstand put arbitrary between the two SBs.
	Chang-1?	SB	253.80	Minor	Ross-Ross (Permian'95) shows as base of C. subcarinata elongata Conodont zone, Palaeofusulina sinensis Fusulinid or Phisonites triangulus Ammonite zone (used here).
		MFS	255.12	Minor	Highstand of Wuchiaping-2 put arbitrarily between the SBs.
	Tansill top (Wuchiaping-2 base)	SB	256.44	Medium	End of Rauserella, Polydiexodina and Codonofusiella paradoxica.  Sequence above Yates has listed incoming of Reichelina, Paradoxiella, Yabeina texana, Codonofusiella extensa (Ross-Ross, Mar. Micro.'95).  However, the Reichelina FAD is coeval with Codonofusiella FAD at base Wuchiapingian GSSP (Henderson'05), therefore it is tentatively considered that this sequence is actually lowest Wuchiaping derived by him from elsewhere).  Here, the SB (well, it would probably be within MFS) of Wuchiaping-2 is tentatively assigned as incoming of Pardunbarulla Fusullinids -- Need better resolution of Wuchaipingian!
		MFS	258.47	Minor	Highstand of Yates Tansill (Wuchiaping-1) put arbitrarily between the SBs.
	Tansill (Wuchiaping-1)	SB	260.50	Minor	Assigned as an arbitrarily 0.1 myr earlier than the Lowstand (assuming a 400 kyr model of sinisoidal sea-level).  See note on Lowstand.  NOTE:  Sequence-strat diagram in Wardlaw et al (2006, Episodes, in prep.) implies that the Tansill is a separate minor sequence from the underlying Yates; and same is implied by Schutter (ExxonMobil, unpubl.).  Alternations of Limestone and Clastics in coeval Bell Canyon suggest higher-order sequences within the major one (Schutter distinquished these, with arbitrary 1 myr period).
		MFS	261.85	Minor	MFS put arbitrarily midway between the SBs.
	Yates	SB	263.30	Minor	See Comment on overlying Tansill SB.  SB arbitrarily put midway in combined Yates-Tansill interval.
		MFS	265.90	Minor	Highstand of Seven RIvers put arbitrarily 0.1 myr below base of Capitanian (see GSSP placement in underlying SB comments).
	Seven Rivers	SB	266.10	Minor	Below base of Capitanian Stage.  Incoming of Parafusulina antimonioensis.  GSSP of Capitanian occurs in equivalent of lowermost HST of Seven Rivers sequence (Wardlaw et al., Episodes, 2006 in prep.), which implies that SB and LST are within latest GSSP-defined-Wordian; therefore, here, the SB has been placed an arbitrarily 0.2 myr below MFS, pending better biostrat control, and assuming a 400-kyr sinisoid.
		MFS	266.58	Medium	MFS put arbitrarily midway between the SBs.
	Queens	SB	267.05	Medium	No major biostrat associations given.  Assigned arbitrarily as mid-way between Graysburg SB and Seven Rivers SB.
		MFS	268.00	Medium	Assigned as base of Wordian (GSSP occurs within the following highstand), so this is quite close.
	Graysburg (top of San Andres)	SB	268.20	Medium	GSSP for Wordian occurs in equivalent of HST of Graysburg sequence (Wardlaw et al., Episodes, 2006 in prep.).  Assuming a 400-kyr model, then this SB is put 0.2myr before the MFS (GSSP).  San Andres sequence is split into two identical sequences in Ross-Ross (Permian'95), but the lower is just a small hump in Mar. Micro.'95 version (used here); and durations are made the same.
		MFS	268.35	Medium	MFS put arbitrarily midway between the SBs.
	Upper San Andres II	SB	268.49	Minor	arbitrarily in Middle of double Upper San Andres sequence
		MFS	268.64	Medium	MFS put arbitrarily midway between the SBs.
	Upper San Andres I	SB	268.78	Minor	10% above base in Wordian Stage.    Cherry Canyon that is equivalent to lower "Upper San Andres", hence below the Graysburg that correlates with base-Wordian GSSP, contains Parafusulina lineata and P. deliciasensis, and Leella fragilis Fusulinids (Wardlaw et al., Episodes, 2006 in prep.).  SB assigned here as the base of that Fusulinid zone.
		MFS	269.17	Minor	Shown as a very minor rise within a longer LST between major highstands in Ross-Ross (Permian '95).  MFS put arbitrarily midway between the SBs.
	Brushy Canyon (top of Road Canyon)	SB	269.56	Major	Base of Traditional Wordian Stage, but GSSP-defined Wordian implies that Brushy Canyon sediment is now entirely middle Roadian.  Brushy Canyon contains Parafusulina rothi and P. maleyi Fusulinids  (Wardlaw et al., Episodes, 2006 in prep.).  Road Canyon is displayed as a single sequence with about 6 superimposed minor sequences in Ross-Ross (Mar. Micro.'95), but as a major double sequence in their Permian'95 diagram (used here) in about a 3:1 relative duration.  SB assigned here to base of that Fusulinid zone.
		MFS	270.26	Medium	MFS put arbitrarily 25% between the SBs (extended HST)
	Road Canyon II	SB	270.49	Minor	1/4th up in Road Canyon main sequence (see Comment on next higher SB)
		MFS	270.60	Minor	MFS put arbitrarily 65% between the SBs (extended LST)
	Road Canyon I	SB	270.80	Medium	Base of Traditional Roadian Stage and onset of Rauserella and Parfusulina boesei and Skinnerina; but GSSP-defined Roadian implies onset of Road Canyon deposition (MFS) is now uppermost Kungurian.  GSSP for base of Roadian occurs in "Middle San Andreas" sequence (implied on diagram to be Road Canyon?) that begins at base of El Centro Member of Cutoff Formation (Wardlaw et al., Episodes, 2006 in prep.).  Therefore, using a 400 kyr model, the SB has been placed 0.2 myr below the GSSP-base-Roadian here.
		MFS	270.83	Medium	Minor sequence (and brief).  MFS put arbitrarily midway between the SBs.
	Iren -2	SB	271.06	Major	Minor sequence (medium-MFS, and brief).  90% of span between Parafusulina fountaini Fusulinid Zone and Base of Road Canyon
		MFS	271.97	Major	Iren (complex HST) peak is quite broad HST.  MFS put 20% between the SBs (rapid rise)
	Iren	SB	272.20	Major	45% of span between Parafusulina fountaini Fusulinid Zone and Base of Road Canyon.  Iren is drawn by Ross-Ross'95 eustatic chart as having 4 minor humps on extended HST.
		MFS	273.06	Major	Filippov (double) peak is quite broad HST.  MFS put 25% between the SBs (rapid rise)
	Filippov	SB	273.35	Major	Base of Cathedralian regional stage.  Base of Parafululina fountaini Fusulinid Zone.  Ross and Ross (1995) shows Cathedralian as onset of Parafusulina durhami, which Davydov (1996) displays as coeval with base of Cf13 (used here).  Double-peaked HST => can split into 2 sequences of ~400 kyr each.
		MFS	273.91	Major	Saran peak is quite broad HST.  MFS put 25% between the SBs (rapid rise)
	Saran	SB	274.09	Major	Single major Sequence on Ross-Ross (Mar.Micro.'95) split into two equivalent sequences of Saran and Sargin on Ross-Ross (Permian'95).  Biostrat association of Parafusulina brooksensis, Pa. vidriensis with "new" SB was formerly listed at middle of the previous single-large one.  Age assigned from estimated age of this assemblage.
		MFS	274.48	Major	MFS put arbitrarily midway between the SBs.  Transgressive phase above SB is Hess Fossil Bed (Taylor Ranch Member) in Texas. 
	Sargin	SB	274.86	Major	Transgressive phase above SB is Hess Fossil Bed (Taylor Ranch Member) in Texas.  Base of Parafusulina spissisepta, Pa. Leonardensis assemblage Fusulinid Zone of Ross-Ross'95.
		MFS	275.14	Major	Main peak MFS of Irgin sequence.  MFS put 25% between the SBs (rapid rise, extended HST).
	Irgin 3	SB	275.23	Medium	SB placed in middle of Sargin complex sequence, as shown on Ross-Ross (Permian'95)
		MFS	275.32	Medium	MFS put arbitrarily midway between the SBs.
	Irgin 2	SB	275.41	Minor	SB placed in middle of lower half of Sargin complex sequence, as shown on Ross-Ross (Permian'95)
		MFS	275.51	Minor	MFS put arbitrarily midway between the SBs.
	Irgin 1	SB	275.60	Major	Onset of Parafusulina (Pa. allisonensis).  SB age assigned as base of that zone.
		MFS	275.96	Major	Burstev peak (highest HST in Permian) put 35% of span between Chalaroschwagerina hawkinsi and P. allisonensis Fusulinid Zones
	Burstev	SB	276.15	Medium	Base of Hessian regional stage.  Incoming of Rubustoschwagerina (single species; but helps to correlate to Tethyan region) and Chalaroschwagerina hawkinsi (SB age assigned as base of that zone)
		MFS	276.36	Medium	MFS put arbitrarily midway between the SBs.
	Sterlitamak 3	SB	276.56	Minor	95% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	276.89	Minor	MFS put arbitrarily midway between the SBs.
	Sterlitamak 2	SB	277.22	Minor	87% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	277.64	Minor	MFS put arbitrarily midway between the SBs.
	Sterlitamak 1	SB	278.05	Major	77% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	279.41	Major	MFS put 25% between the SBs (rapid rise)
	Lenox Hills 4	SB	279.86	Major	55% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	280.79	Major	MFS put 25% between the SBs (rapid rise)
	Lenox Hills 3	SB	281.10	Medium	40% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	282.03	Medium	MFS put 25% between the SBs (rapid rise)
	Lenox Hills 2	SB	282.34	Medium	25% of span between Eoparafusulina linearis and Chalaroschwagerina hawkinsi Fusulinid Zones
		MFS	283.37	Medium	Incoming of Pseudoschwagerina convexa, P. geronica, Chalaroschwagerina nelson, Eoparafusulina linearis, and Schwagerina diversiformis assemblage. The Lenoxian (after Lenox Hills) is diagrammed as a single major hump with four superimposed lesser oscillations by Ross-Ross (Marine Micro'95); but as four major packages of increasing coastal onlap by Ross-Ross (Permian '95).  Age assigned as arbrarily mid-point of Sequence
	Lenox Hills 1 [top of Neal Ranch]	SB	284.40	Major	Major hiatus begins, separating earlier Pseudoschwagerina (P. uddeni species) from P. convexa and P. gerontica; and E. allisonensis from E. linearis.  The package of 4 major Neal Ranch SBs are diagrammed in Ross-Ross (Marine Micro'95) with about 3:1:1:2 ratio of relative thicknesses; and this vague estimate was applied here, until the FADs of Fusulinids are independently provided.  SB Age assigned here to be same as base of Pseudoschwagerina convexa, P. geronica, Chalaroschwagerina nelson, Eoparafusulina linearis, and Schwagerina diversiformis assemblage; even though, technically, these arrive with next transgression.
		MFS	286.39	Major	Begins Neal Ranch highstand 4, which is the maximum onlap of this series.  Arbitrarily as mid-way between SBs.  Incoming of Eoparafusulina allisonensis Fusulinids.  Drawn by Ross-Ross'95 as having 5 superimposed minor oscillations, including a 4-stage Regressive phase into the major hiatus that terminates Neal Ranch.
	Neal Ranch 4 (or Shikhan)	SB	288.38	Major	Assigned as 5/7ths up in Neal Ranch suite. See Lenus Hill SB for details.  Termination of several Fusulinid groups (Leptotriticites, Rugosochusenella, Schwagerina emaciata).
		MFS	289.38	Medium	Begins Neal Ranch highstand 3.  Arbitrarily as mid-way between SBs.
	Neal Ranch 3	SB	290.37	Medium	Assigned as 4/7ths up in Neal Ranch suite. See Lenus Hill SB for details.
		MFS	291.87	Medium	Begins Neal Ranch highstand 2. MFS put 25% between the SBs (rapid rise).   Incoming of Schwagerina compacta - Pseudoschwagerina uddeni and rugosochusenella Fusulinids
	Neal Ranch 2	SB	292.37	Medium	Assigned as 3/7ths up in Neal Ranch suite. See Lenus Hill SB for details.
		MFS	294.31	Medium	Begins peak of Neal Ranch highstand 1.  Assigned as an arbitrary 50% up in sub-Sequence. Incoming of Pseudoschwagerina texana Fusulinids
	Neal Ranch 1a	SB	296.25	Minor	Ross-Ross'95 indicate this as a minor oscillation within the major transgression of lower Nealian.  Assigned as an arbitrary 35% up within the major sequence, which, interestingly, fits the independent age for MFS (incoming of fusulinid assemblage).
		MFS	297.24	Medium	Base of CF4 (Pseudoschwgerina FAD) for initiation of sediments.  Ross-Ross'95 draws this as an intermediate step on a more major transgression.
	Neal Ranch (Red Eagle top)	SB	298.34	Major	Base of Ross-Ross "E. allisonensis - Paraschwagerina" combined zone, which he had started at base of Permian (base-Asselian).  Davydov'96 shifted base of Nealan foram assemblages to upper Asselian, but Ross-Ross'95 (and Davydov'96) indicate that initial sediments overlying major SB have incoming of  Pseudoschwagerina (P. beedei).  Threfore, SB (termination of underlying zone) is placed at top of Cf2 (base of hiatus, using Davydov'96), and following MFS put at base of CF4 (Pseudoschwgerina FAD).
		MFS	299.16	Medium	MFS put arbitrarily midway between the SBs.
	Red Eagle Ls. 	SB	299.98	Major	Base of Triticites meeki - S. longissimoidea zone of Ross-Ross'88.  Schematic -- has 2 peaks (lower Foraker, higher Red Eagle) in Ross-Ross'87 (the higher one is Permian).
		MFS	300.29	Major	MFS put arbitrarily midway between the SBs.
	Brownville Ls.	SB	300.59	Major	Base of Triticites subventricosus - Schubertella shetensis zone of Ross-Ross'88. Schematic -- has 3 peaks (lower Brownville, Falls City, higher Five Point) in Ross-Ross'87.
		MFS	300.90	Major	MFS put arbitrarily midway between the SBs.
	Severy Sh.	SB	301.21	Major	Base of Triticites callosus - T. plummeri zone of Ross-Ross'88.   Schematic -- has 2 peaks in Ross-Ross'87 (lower Howard, higher Tarkio).
		MFS	302.28	Major	MFS put arbitrarily midway between the SBs.
	Ireland Ss.	SB	303.36	Major	20% up in Triticites mcgrewensis, Dunbarinella zone of Ross-Ross'88.   Schematic -- has 4 peaks in Ross-Ross'87 (Oread, Lecompton, Deer Creek, Topeka); and underlying Stranger has a single peak = 5 major peaks used to subdivide this zone equally.
		MFS	303.63	Major	MFS put arbitrarily midway between the SBs.
	Stranger Fm.	SB	303.90	Major	Base of Triticites mcgrewensis, Dunbarinella zone of Ross-Ross'88.  Single peak.
		MFS	303.95	Major	MFS put arbitrarily 3/4ths up between the SBs, due to extended LST.
	Iatan Ls.	SB	304.10	Major	Base of Triticites latensis - Kansanella (K.) joensis zone of Ross-Ross'88.  Schematic -- double peak in Ross-Ross'87 (South Bend and unlabeled).
		MFS	304.19	Major	MFS put arbitrarily midway between the SBs.
	Stoner Ls.	SB	304.29	Major	Base of Triticites primarius, Kansanella neglecta zone of Ross-Ross'88.  Schematic -- triple peak in Ross-Ross'87.
		MFS	304.49	Major	MFS put arbitrarily midway between the SBs.
	Dewey Fm.	SB	304.68	Major	Base of Triticites ohioensis - T. nebraskensis zone of Ross-Ross'88.   Schematic -- double peak in Ross-Ross'87.
		MFS	304.94	Major	Base of Triticites rangerensis Fusulinid Zone (Correlates to Triticites collus Fusulinid Zone). 
	Winterset Ls.	SB	305.20	Major	Base of Kansanella (Oiwanella) winterensis, T. cf. ohioensis zone of Ross-Ross'88.  Assumed to be Dennis peak in Ross-Ross'87.
		MFS	305.27	Major	MFS put arbitrarily midway between the SBs.
	Bethany Falls Ls.	SB	305.33	Major	Base of Quasifusulinoides, Eowaeringella, Okethelia zone of Ross-Ross'88.  Assumed to be Swope peak in Ross-Ross'87
		MFS	305.45	Major	MFS put arbitrarily midway between the SBs.
	Pleasanton Gp.	SB	305.56	Major	This SB is put arbitrarily midway between the SBs. Schematic -- Hertha has double peak in Ross-Ross'87.
		MFS	305.68	Major	MFS put arbitrarily midway between the SBs.
	Glenpool Ls.	SB	305.80	Medium	Top of Beedeina sulphurensis - Bartramella zone of Ross-Ross'88. Drawn as a single peak in Ross-Ross'87, with Hertha just above; which doesn't fit Heckel et al (2000) detailed cycles.
		MFS	305.95	Medium	MFS assigned arbitarily midway between SBs.
	Lenapah Ls.	SB	306.11	Major	Base of Beedeina sulphurensis - Bartramella zone of Ross-Ross'88. Schematic -- triple peak in Ross-Ross'87.
		MFS	306.31	Major	MFS assigned arbitarily midway between SBs.
	Altamont Ls.	SB	306.50	Major	Base of Beedeina cf. B. haworthi - Bartramella zone of Ross-Ross'88.   Schematic -- four-sequence peak in Ross-Ross'87.
		MFS	307.01	Major	MFS assigned arbitarily midway between SBs.
	Pawnee Ls.	SB	307.52	Major	Base of Beedeina novomexicana - Plectofusulina zone of Ross-Ross'88.   Schematic -- Pawnee has a double peak in Ross-Ross'87.
		MFS	307.72	Major	MFS assigned arbitarily midway between SBs.
	Fort Scott Ls.	SB	307.92	Major	Base of Beedeina leei - Wedekindellina henbesti zone of Ross-Ross'88.  On Ross-Ross'87, this zone would be the SB before onset of Inole (which is tenatively assigned much earlier here.).  [However, Heckel et al., 2006, place Ft. Scott into B. haworthi Zone (and it has B. girtyi), and their correlations shift this zone to a mid-Moscovian age.]  Schematic -- Ft. Scott has a double peak in Ross-Ross'87.
		MFS	308.63	Major	Inola (basal peak) is largest; and this MFS assigned 20% between SBs.
	Inola -- lower Cherokee Gp.	SB	308.71	Major	Ross-Ross'88 shows base of Cherokee Group as base of DESMOINESIAN regional stage base = base of Fusulinella famula - F. cabezasensis zone of Ross-Ross'88.   However, this usage would not fit other schemes (e.g., Heckel et al., 2000), which imply Cherokee spans both the pre-Fleming set (beginning at Inola?) and the Verdigris set.  Therefore, I have separated this upper set as "Verdigris" and lower set as "Inola".  On Ross-Ross'87, this Inola set seems to consist of 4 sequences -- a Basal and most major peak of lower Inola, followed by decreasing peaks of upper Inola, Tioweh (= Fleming of Heckel'2000?), and Russel Creek.   Verdigris = Set of 4 sequences -- Basal and most major peak = Verdigris, followed by decreasing peaks of Upper Ardmore, Bevier and Breezy Hill (using Heckel, 2000, Fig 4 for nomenclature).  However, the June'06 time scale would not allow space for such detail -- probably indicating that Cherokee zone must span a longer duration, or that these are 100 kyr (which fits upper Moscovian)!
		MFS	309.97	Major	MFS assigned at 25% between SBs to highlight the estimated Elm Creek coincidence (if I did this correctly!).  Scaling is the Elm Creek maximum peak.
	Finnie (Miss. Valley) =Elm Creek?	SB	310.38	Major	Base of Fusulinella prolifica - F. haywardi zone of Ross-Ross'88.  I have assumed this Finnie matches the suite of a basal minor un-named hump (= longer LST, implying called it a major SB), then a major-peak of Elm creek, followed upward by major-medium Spaniard, medium Donsley and minor-peak Bluejacket.  NEED BETTER REGIONAL CORRELATION.   See Comments on Battery Rock SB (Need a more coherent Atokan regional biostrat and sequence strat that doesn't change dramatically between publications with no commentary by the authors!).
		MFS	310.61	Medium	MFS assigned at 25% between SBs to indicate extended HST of Sellers (if I did this correctly!).  Scaling is the Elm Creek maximum peak.
	Grindstaff (Miss. Valley) =Sellers?	SB	310.84	Medium	Base of Profusulinella regia Fusulinid Zone.  On Ross-Ross'87 diagram, however, this doesn't fit.  I have assumed this Grindstaff matches Sellers peak.
		MFS	311.61	Minor	MFS assigned arbitarily midway between SBs. 
	Pounds (Miss. Valley) =Frensley?	SB	312.39	Minor	Base of Profusulinella decora, Eostaffella powwowensis zone of Ross-Ross'88.     For scaling, assumed magnitude is the Sellers peak on Ross-Ross'87.  Schematic only, because this seqeunce might be dual-peaked (Frensley and Sellers peak, plus an upper minor hump on Ross-Ross'87).  However, age correlation seems quite poor to match Ross-Ross'88 and Ross-Ross'87.
		MFS	313.16	Minor	MFS assigned arbitarily midway between SBs.
	Battery Rock Ss. in Miss. Valley	SB	313.94	Minor	Base of P. copiosa zone of Ross-Ross'88 = base of ATOKAN regional stage.  Contains Seller Lms according to Ross-Ross'88 p.233 Illinois-Basin column; which, however, Schutter (Exxon, unpubl.) correlates with "underlying" Ross-Ross Dye-Kessler of Mid-Continent.  Also, the Ross-Ross'87 Eustatic curve has entirely different set of names within the ATOKAN interval.    For scaling, assumed this is the Bostwick peak on Ross-Ross'87.  Schematic only; because this Sequence might be dual-peaked (Bostwick, then Lester peaks).
		MFS	314.33	Minor	MFS assigned 3.4ths up between SBs, duw to extended LST of Trace Creek (probably a minor sequence)
	Trace Creek	SB	315.49	Minor	SB at 2/4th between Bloyd (Brentwood) SB and Battery (Bostwich) SB.  See Comment at Bloyd 1 SB.  Extended lowtand in lower half.
		MFS	315.72	Minor	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic)
	Dye - Kessler	SB	316.27	Medium	SB at 1/4th between Bloyd (Brentwood) SB and Battery (Bostwich) SB.  See Comment at Bloyd 1 SB.
		MFS	316.50	Medium	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic)
	Bloyd 1 (N11) Brentwood	SB	317.04	Minor	Base of large Millerella spp., Ozawainella?, Eostaffella zone of Ross-Ross'88.  Base is correlated to N11 in Ross-Ross'88; but to N10 in Ross-Ross'87.  Bloyd group divided into 3 sequences in Ross-Ross'87, shown with about a 2:1:1 relative descending duration; but above this point, it becomes difficult to match Ross-Ross'88 and Ross-Ross'87 nomenclature/ages of sequences.
		MFS	317.11	Minor	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic)
	Prairie Grove 2 (N9-N10)	SB	317.26	Minor	Base of Ross-Ross version of Millerella marbiensis; but the assemblage of the next lower zone had to be merged with it to fit the Davydov'96 one.  Therefore, unable to make a separate biostrat-correlation at this point. Set as 4/5 within M. marblensis zone (interval between base-sub-Cane and base-Bloyd); see Comment on sub-Cane Hill SB.
		MFS	317.32	Minor	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic).  Relative MFS on 2nd-order trend, but really just a low rise before another very low LST.
	Prairie Grove 1 (N8)	SB	317.47	Minor	Set as 3/5 within M. marblensis zone (interval between base-sub-Cane and base-Bloyd); see Comment on sub-Cane Hill SB.
		MFS	317.53	Minor	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic)
	sub-Prairie Grove 1 (N7)	SB	317.68	Minor	Set as 2/5 within M. marblensis zone (interval between base-sub-Cane and base-Bloyd); see Comment on sub-Cane Hill SB.
		MFS	317.74	Minor	MFS assigned 70% between SBs (extended LST on Ross-Ross schematic)
	Cane Hill (N5-N6)	SB	317.89	Minor	Set as 1/5 within M. marblensis zone (interval between base-sub-Cane and base-Bloyd); see Comment on sub-Cane Hill SB.
		MFS	317.99	Minor	MFS assigned arbitarily midway between SBs.
	sub-Cane Hill (N4)	SB	318.10	Minor	Base of Millerella marblensis - Eostaffella pinguis pair of zones of Ross-Ross'88.  Set of "N4-N11" equivalents in Namurian studies is suggested by Ross-Ross'88.  Suite from "N4" to "N11" SB seems to display 5 main sequences in Ross-Ross diagram (but within only 1 myr?), therefore set as equal subdivisions here.
		MFS	318.34	Minor	MFS assigned arbitarily midway between SBs.
	Imo (upper)	SB	318.58	Major	TOP of Millerella (primitive), "Millerella" cooperi Foram zone of Ross-Ross'88.
		MFS	318.82	Major	MFS assigned arbitarily midway between SBs.  This is a generalized one, and would correspond to Goreville max on Ross-Ross'87 4-peak version.
	Grove Church - Degonia (N1)	SB	319.06	Major	Base of Millerella (primitive), "Millerella" cooperi Foram zone of Ross-Ross'88.  Ross-Ross'87 show this divided into 4 equal-duration sequences (stratigraphically-up as minor-peak Degonia, major Negli Creek, major Goreville, and medium-peak Grove Church; but these "parasequences" are omitted here for now (would be about 100 kyr in duration each!  Probably, the duration of the Millerella cooperi Foram zone is greatly underestimated, due to mis-calibration with Europe-related standard.
		MFS	321.28	Major	MFS assigned 30% between SBs (sharp rise).  Clore HST is maximum in Serpukovian.
	Clore	SB	322.23	Medium	Base set at 6/9 of span from base-Tar Springs to base-Degonia (see Comment on Tar Springs)
		MFS	324.45	Medium	MFS assigned 30% between SBs (sharp rise)
	Menard	SB	325.40	Medium	Base set at 3/9 of span from base-Tar Springs to base-Degonia (see Comment on Tar Springs)
		MFS	326.46	Major	MFS assigned arbitarily midway between SBs.
	Vienna	SB	327.52	Minor	Base set at 1/9 of span from base-Tar Springs to base-Degonia (see Comment on Tar Springs)
		MFS	328.05	Minor	MFS assigned arbitarily midway between SBs.
	Tar Springs	SB	328.58	Major	TOP of Millerella tortula-designata Foram zone of Ross-Ross'88.  LST corresponds to a "gap" in foram zonation.  Mega-sequence [Tar Springs - Clore] is subdivided in Ross-Ross'87 into 4 sequences with approximate 3:3:2:1 ratio in displayed durations (used here).
		MFS	330.45	Major	MFS assigned arbitarily midway between SBs.
	Glen Dean - Cypress	SB	332.33	Major	About 90% up in Endostaffella discoidea Foram zone of Ross-Ross'88.  Transgressive stage corresponds to Beech Creek-Haney formations.  NOTE: this sequence has internal high-frequence high-amplitude oscillations, which provide an additional set of Sequences (will add later!).
		MFS	333.80	Major	MFS assigned 30% between SBs (sharp rise)
	Ridenhower - Ste. Genevieve	SB	334.43	Major	Base of Endostaffella discoidea Foram zone of Ross-Ross'88.
		MFS	335.09	Major	MFS assigned 60% between SBs (slow rise).  St. Louis is major peak.
	St Louis	SB	336.09	Minor	Middle of G. baileyi Foram zone of Ross-Ross'88.  SB and following LST correspond to evaporites in Illinois Basin, and is probbly Vis2 of GTS2004.
		MFS	336.91	Minor	MFS assigned arbitarily midway between SBs.  Very low sea-level.,
	Salem (upper)	SB	337.74	Major	Base of G. baileyi Foram zone of Ross-Ross'88.  SB and following LST (indeed, essentially all the sequence, because MFS is minor) correspond to evaporites in Illinois Basin.
		MFS	339.06	Major	MFS assigned 65% between SBs (slow rise).  Lower Salem is a major HST.
	Salem (lower)	SB	341.52	Major	Base of Nodosarchaediscus, Archaediscus zone of Ross-Ross'88.
		MFS	343.72	Medium	MFS assigned 25% between SBs -- it is an extended HST on diagram of Ross-Ross'87.
	Warsaw	SB	344.45	Major	Base of E. scitula zone of Ross-Ross'88.  SB corresponds to a foram bed near top of Keokuk formation.
		MFS	344.66	Major	MFS assigned arbitarily midway between SBs.  Upper Keokuk peak is a major one, but sharp.
	Keokuk (Upper)	SB	344.87	Major	Middle of Priscella prisce, Endothyra spp., Tetataxis spp. Foram zone of Ross-Ross'88.  Following LST is a minimum; and probably is "Vis1" of GT2004
		MFS	345.09	Major	MFS assigned arbitarily midway between SBs.
	Keokuk (Lower)	SB	345.30	Major	Base of Priscella prisce, Endothyra spp., Tetataxis spp. Foram zone of Ross-Ross'88.   SB corresponds to a bone bed at top of Burlington formation.
		MFS	346.56	Medium	MFS assigned 65% up between SBs (slow rise)
	Burlington - Fern Glen - Meppen	SB	348.91	Major	Base of Palaeospiroplectammina aff. parva, Tuberendothyra tuberculata zone of Ross-Ross'88. 
		MFS	349.58	Major	MFS assigned 80% up between SBs (slow rise from LST). Maximum Highstand in Early Carboniferous.
	Chouteau	SB	352.25	Medium	Top of Palaeospiroplectammina tchernyshinensis, Granuliferella spp. Zone of Ross-Ross'88.  Following LST is probably "Tm2" of GTS2004.
		MFS	353.75	Medium	MFS assigned 60% up between SBs.
	Hannibal	SB	355.99	Medium	Ross-Ross'87 splits the Hannibal and "Glen Park" (lower Kinderhookian regional stage) into a double-sequence based on Moscow Basin.  SB is arbitrarily placed here as 35% up between delayed onset of basal MFS and the Chouteau SB, which tries to model Ross-Ross'87 schematic diagram.
		MFS	358.00	Major	Ross-Ross'87 schematic curve implies a relatively rapid transgression in lowermost Carboniferous, but Glen Park peak is not pinned to biostrat (in Forams).  Therefore, assigned as an arbitrary 1 myr after LST minimum here, which takes into account span of Tournasian scale (7 myr to Chouteau SB).
	Glen Park	SB	361.50	Major	Base of subzone 2 of S. praesulcta Conodont Zone.  Following extended LST is dashed to end of Famennian.  SB is called Glen Park here to correspond with delayed onset of Glen Park formation in Mid-Continent USA.
		MFS	363.03	Medium	Base of S. praesulcata Conodont Zone.  Sketched by Ross-Ross'88 as slightly lower peak than the lowest Carboniferous one.
		SB	363.79	Minor	Base of subzone 3 of P. expansa Conodont Zone on Johnson's scale; but GTS2004 has 4 subzones => assigned as 1/3rd up in P. expansa zone for now.
		MFS	364.94	Major	Essentially in middle of subzone 1 of P. expansa
	II f	SB	365.78	Medium	Base subzone 2 of P. postera Conodont Zone
		MFS	365.98	Minor	About 1/3rd up in subzone 1 of P. postera Conodont Zone
		SB	366.09	Minor	Base of P. postera Conodont Zone
		MFS	367.31	Medium	MFS shoulder at about middle of subzone 1 of P. trachytera Conodont Zone
		SB	369.15	Major	1/3 above base in marginifera Conodont Zone
		MFS	369.30	Medium	MSF at about base of subzone 2 of P. marginifera Conodont Zone
		SB	371.44	Major	Base of rhomboidea Conodont Zone
		MFS	372.01	Medium	MSF peak at about 2/3rds up in P. crepida Conodont Zone
		SB	372.28	Minor	Middle of P. crepida Conodont Zone
	II e	MFS	373.58	Major	MSF at base of subzone 3 of P. triangularis
	II e	SB	374.04	Major	1/3 above base in P. triangularis Conodont Zone = base-Famennian in Johnson's conodont scheme
		MFS	374.27	Medium	MSF peak in about middle of subzone 1 of P. triangularis
		SB	376.12	Medium	Base of "uppermost subzone of gigas Conodont Zone", which corresponds to base of P. linguiformis Conodont Zone in new standard.  This now makes a long LST (entire P. linguiformis zone spanning over 1 myr of uppermost Frasnian) in current GTS2004 scaling.
		MFS	377.20	Major	MSF shoulder at about base of "upper subzone of gigas Conodont Zone", which corresponds to 50% up in P. rhenana Conodont Zone of new standard.
	II d	SB	377.42	Major	80% up in "lower subzone of gigas Conodont Zone", which corresponds to 40% up in P. rhenana Conodont Zone of new standard.
		MFS	379.44	Minor	MSF Shoulder at about 20% up in Ancyrognathus triangularis Conodont Zone, which corresponds to about 75% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		SB	379.56	Minor	Base of Ancyrognathus triangularis Conodont Zone, which corresponds to about 65% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		MFS	379.68	Minor	MSF Shoulder at about 80% up in "Upper subzone of asymmetrica Conodont Zone", which corresponds to about 55% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		SB	379.86	Minor	Middle of "Upper subzone of asymmetrica Conodont Zone", which corresponds to about 40% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		MFS	379.98	Minor	MSF Shoulder at about 35% up in "Upper subzone of asymmetrica Conodont Zone", which corresponds to about 30% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		SB	380.27	Minor	Base of "Upper subzone of asymmetrica Conodont Zone", which corresponds to about 5% up in P. hassi Conodont Zone in new standard (as drawn on Exxon Devonian chart)
		MFS	380.89	Major	MSF Shoulder at about middle of "Middle subzone of asymmetrica Conodont Zone", which corresponds to about 80% up in combined P. transitans/P. puactata zones in new standard.
	II c	SB	381.74	Medium	SB drawn at about 20% up in "Middle subzone of asymmetrica Conodont Zone", which corresponds to about middle of combined P. transitans/P. puactata zones in new standard.
		MFS	385.30	Minor	MSF Shoulder at about base of "Lower subzone of asymmetrica Conodont Zone", which corresponds to base of "falsioivalis" Conodont Zone of new standard = base of Frasnian
		SB	385.59	Minor	About 70% up in "Lowermost subzone of asymmetrica Conodont Zone", which corresponds to 70% up in "norrisi" Conodont Zone of new standard.
		MFS	385.69	Minor	MSF Shoulder at about 60% up in "Lowermost subzone of asymmetrica Conodont Zone", which corresponds to 60% up in "norrisi" Conodont Zone of new standard.
		SB	385.89	Minor	About 40% up in "Lowermost subzone of asymmetrica Conodont Zone", which corresponds to 40% up in "norrisi" Conodont Zone of new standard.
		MFS	385.98	Medium	MSF Shoulder at about 30% up in "Lowermost subzone of asymmetrica Conodont Zone", which corresponds to 20% up in "norrisi" Conodont Zone of new standard.
	II b	SB	386.28	Minor	Top of K. disparilis Conodont Zone
		MFS	387.15	Minor	MSF peak is about 10% up in K. disparilis Conodont Zone
		SB	387.25	Minor	Base of K. disparilis Conodont Zone
		MFS	387.84	Minor	MSF peak is about the base of subzone 2 of K. hermanni Conodont Zone
		SB	388.23	Minor	Base of K. hermanni Conodont Zone
	II a	MFS	389.49	Major	25% up in upper subzone of P.varcus Conodont Zone (assumed that this is the combined "M" and brief uppermost subzone of Johnson et al '85 scheme)
	II a	SB	390.37	Medium	Middle of lower subzone of P. varcus Conodont Zone
		MFS	390.42	Minor	45% above base of lower subzone of P. varcus Conodont Zone
		SB	390.46	Minor	40% above base of lower subzone of P. varcus Conodont Zone
		MFS	390.60	Minor	25% above base of lower subzone of P. varcus Conodont Zone
		SB	390.64	Minor	20% above base of lower subzone of P. varcus Conodont Zone
		MFS	391.12	Minor	About 80% above base in Johnson's ensensis Conodont Zone (= 70% up in current hemiansatus Zone)
		SB	391.31	Minor	3/4 above base in Johnson's ensensis Conodont Zone (= middle of current hemiansatus Zone)
		MFS	392.48	Minor	MFS peak about 40% above base in ensensis Conodont Zone (see comment on SB)
		SB	392.60	Minor	30% above base in P. ensensis Conodont Zone (after adjusting for split of Johnson's P. ensensis for current basal-Givetian hemiansatus Zone).
		MFS	392.88	Major	MFS peak about 5% up in P. ensensis Conodoont Zone.  
	I f	SB	392.94	Medium	Base of P. ensensis Conodont Zone
		MFS	393.28	Major	MSF peak drawn about 60% above base of T. kockelianus Conodont Zone
	I e	SB	393.37	Medium	1/2 above base in kockelianum Conodont Zone
		MFS	394.65	Minor	MSF peak drawn about 25% above base of T. australis Conodont Zone
		SB	394.76	Minor	15% above base in australis Conodont Zone
		MFS	394.88	Major	MSF peak drawn about 5% above base of T. australis Conodont Zone
	I d	SB	394.94	Medium	Base of T. australis Conodont Zone
		MFS	395.15	Minor	MSF peak drawn about 75% above base in P. costatus Conodont Zone
		SB	395.19	Minor	70% above base in P. costatus Conodont Zone
		MFS	396.65	Minor	MSF peak in middle of P. partitus Zone
		SB	397.50	Minor	Base of P. partitus Conodont Zone
		MFS	398.93	Major	MSF peak at base of P. patulus Conodont Zone
	I c	SB	400.35	Medium	1/4 above base in P. serotinus Conodont Zone
		MFS	402.54	Medium	Drawn about 40% above base in P. inversus Conodont Zone (but, because Johnson's scheme didn't include the underlying nothoperbonus; then that zone is assumed to be included => SB occurs within that "underlying" one).
		SB	402.73	Minor	1/3 above base in P. inversus Conodont Zone (but, because Johnson's scheme didn't include the underlying nothoperbonus; then that zone is assumed to be included => SB occurs within that "underlying" one).
		MFS	404.17	Minor	85% above base in P. grobergi (plus underlying kitabicus) Conodont Zone
		SB	404.34	Minor	80% above base in P. grobergi (plus underlying kitabicus) Conodont Zone
		MFS	407.59	Minor	Drawn about 6/10th up in "dehiscens" Conodont Zone; which is assumed here to be coeval to P. pireneae Conodont Zone.
		SB	407.74	Minor	Middle of "dehiscens" Conodont Zone; which is assumed here to be coeval to P. pireneae Conodont Zone.
		MFS	408.32	Minor	Drawn about 1/10th up in "dehiscens" Conodont Zone; which is assumed here to be coeval to P. pireneae Conodont Zone.
	I b	SB	409.21	Major	Middle of E. kindlei Conodont Zone
		MFS	409.79	Medium	Drawn about 1/10th up in E. kindlei Conodont Zone
		SB	409.94	Minor	Base of E. kindlei Conodont Zone
	I a	MFS	410.78	Major	About 1/3rd up in E. sulcatus Conodont Zone
	I a	SB	411.20	Major	Base of E. sulcatus Conodont Zone (base of Pragian).  Very major -- LST is "off page" (all shelves exposed)


Late Carb Detailed Sequences 	sequence				off	Heckel et al, 2005; and Early Perm from B. Wardlaw (in prep.)
		MFS	282.21	Medium	 
	Barneston 2	SB	282.94	Medium	Age simply projected up using same scaling as Kinney to Barneston 1
		MFS	283.67	Major	 
	Barneston 1	SB	284.40	Major	Sw. whitei in MFS; and SB age for convenience, is assumed to be same.
		MFS	285.13	Medium	 
	Kinney	SB	285.86	Medium	Age estimates assume equal-spacing for all Major and Minor cycles (7 in this Sakmarian suite) between correlation horizons.
		MFS	286.59	Medium	 
	Wreford 2	SB	287.31	Medium	 
		MFS	288.04	Medium	 
	Wreford 1	SB	288.77	Medium	 
		MFS	289.50	Minor	 
	Funston	SB	290.23	Minor	Third-Order SB
		MFS	290.96	Minor	 
	Crouse	SB	291.69	Minor	 
		MFS	292.41	Minor	 
	Middleburg	SB	293.14	Minor	 
		MFS	293.87	Medium	 
	Eiss	SB	294.60	Medium	Sw. merrilli in MFS; and SB age for convenience, is assumed to be same.
		MFS	294.97	Medium	 
	Beattie 2	SB	295.33	Medium	Age estimates assume equal-spacing for all Major and Minor cycles (6 in this Asselian suite) between correlation horizons.
		MFS	295.70	Major	 
	Beattie 1	SB	296.07	Major	 
		MFS	296.43	Major	 
	Upper Grenola (Neva)	SB	296.80	Major	 
		MFS	297.17	Medium	 
	Lower Grenola (Burr)	SB	297.53	Medium	 
		MFS	297.90	Major	Third-Order MFS
	Red Eagle 3	SB	298.27	Major	 
		MFS	298.63	Major	 
	Red Eagle 2	SB	299.00	Major	S. isolatus in MFS; and SB age for convenience, is assumed to be same.
		MFS	299.09	Minor	 
	Red Eagle 1	SB	299.19	Minor	Age estimates assume equal-spacing for all Major and Minor cycles (22 in this Gzelian suite) between correlation horizons.
		MFS	299.28	Major	 
	Foraker 4	SB	299.38	Major	 
		MFS	299.47	Major	 
	Foraker 3	SB	299.57	Major	 
		MFS	299.66	Major	 
	Foraker 2	SB	299.76	Major	 
		MFS	299.85	Medium	 
	Foraker 1	SB	299.95	Medium	 
		MFS	300.04	Minor	 
	Five Point	SB	300.14	Minor	 
		MFS	300.23	Minor	 
	Falls City	SB	300.33	Minor	 
		MFS	300.42	Medium	 
	Brownville	SB	300.51	Medium	Wardlaw unpublished for the above suite; although some events are already in Ross-Ross
		MFS	300.61	Major	 
	Tarkio	SB	300.70	Major	 
		MFS	300.80	Major	 
	Howard	SB	300.89	Major	 
		MFS	300.99	Minor	 
	Bachelor	SB	301.08	Minor	 
		MFS	301.18	Minor	 
	Severy	SB	301.27	Minor	Implied minor event during major Regression on Heckel's diagram
		MFS	301.37	Major	 
	Topeka	SB	301.46	Major	 
		MFS	301.56	Minor	 
	Sheldon	SB	301.65	Minor	 
		MFS	301.75	Minor	 
	Curran	SB	301.84	Minor	 
		MFS	301.93	Medium	 
	Iowa Pooint	SB	302.03	Medium	 
		MFS	302.12	Medium	 
	Calhoun	SB	302.22	Medium	 
		MFS	302.31	Major	 
	Deer Creek	SB	302.41	Major	Conodont S. holtensis FAD (Mid-Continent)
		MFS	302.50	Minor	 
	Ozawkia	SB	302.60	Minor	 
		MFS	302.69	Medium	 
	Tecumseh	SB	302.79	Medium	 
		MFS	302.88	Medium	 
	Avoca	SB	302.98	Medium	 
		MFS	303.07	Major	 
	Lecompton	SB	303.17	Major	Conodont Streptognathodus ruzhencevi (Mid-Continent and Moscow), S. virgilicus FAD (Mid-Continent); Fusulinid Raserites stuckenbergi (Moscow and Donets) = base Pf19.  Highest calibrated event on Heckel et al (2005) synthesis.
		MFS	303.29	Medium	 
	Spring Branch	SB	303.41	Medium	Age estimates assume equal-spacing for all Major and Minor cycles (3 in this Pf20 suite) between correlation horizons.
		MFS	303.53	Medium	 
	Clay Creek	SB	303.66	Medium	 
		MFS	303.78	Major	 
	Oread	SB	303.90	Major	Conodont I. simulator. Proposed base of Gzhelian Stage.
		MFS	303.93	Medium	 
	Toronto	SB	303.96	Medium	Age estimates assume equal-spacing for all Major and Minor cycles (13 in this Late Kosimovian suite) between correlation horizons.
		MFS	303.99	Medium	 
	Amazonia	SB	304.02	Medium	 
		MFS	304.05	Major	 
	Cass	SB	304.08	Major	Base of VIRGILIAN regional stage; former traditional base of Gzhellan.  Ammonoid Pseudaktubites stainbrooki, Eovidrioceras conlini (Mid-Continent); Conodont S. zethus (Mid-Continent, Moscow Basin).  
		MFS	304.11	Minor	 
	Westphalia	SB	304.14	Minor	 
		MFS	304.17	Medium	 
	Iatan	SB	304.20	Medium	 
		MFS	304.23	Medium	 
	South Bend	SB	304.26	Medium	Conodont S. pawhusaensis FAD (Mid-Continent).
		MFS	304.29	Major	 
	Stanton	SB	304.32	Major	Conodont S. firmus FAD and S. gracilis group LAD in mid-cycle (Mid-Continent); rare R. quasiarcticus forams (Moscow Basin), but not interpreted here as FAD because used conodont I. toretzianus instead (2 cycles lower); ammonite Pseudoaktubites newelli (Mid-Continent).
		MFS	304.35	Medium	 
	Plattsburg	SB	304.38	Medium	 
		MFS	304.41	Minor	 
	Farley	SB	304.44	Minor	 
		MFS	304.47	Medium	 
	Wyandotte	SB	304.50	Medium	 
		MFS	304.53	Major	 
	Iola	SB	304.56	Major	 
		MFS	304.59	Minor	 
	Mid-Chanute	SB	304.62	Minor	 
		MFS	304.65	Major	 
	Dewey	SB	304.68	Major	Conodont Idiognathodus toretzianus (type; Donets) has lowest noted level in Heckel et al. (2005) chart, therefore used to assign Pc14 base.  Conodont I. magnificus (N.Amer.)
		MFS	304.75	Minor	 
	Durm-Weterville	SB	304.81	Minor	Age estimates assume equal-spacing for all Major and Minor cycles (4 in this Pf16 suite) between correlation horizons.
		MFS	304.88	Medium	 
	Cherryvale	SB	304.94	Medium	 
		MFS	305.01	Minor	 
	Hogshooter	SB	305.07	Minor	 
		MFS	305.14	Major	 
	Dennis	SB	305.20	Major	apparent FAD of Montiparus subcrassulus (base of Pf16) in Moscow Basin.
		MFS	305.24	Minor	Primitive Tricites forams, and conodont S. confragus FAD (Mid-Continent).
	Mound Valley	SB	305.27	Minor	Age estimates assume equal-spacing for all Major and Minor cycles (7 in this Pc13 suite) between correlation horizons.
		MFS	305.31	Major	 
	Swope	SB	305.35	Major	Conodont I. sagittalis, I. sulciferus (type, Mid-Continent); fusulinid Eowaeringella ultimata (Mid-Continent), and maybe earliest primitive Tricites (Donets).
		MFS	305.39	Minor	 
	Sniabar	SB	305.42	Minor	 
		MFS	305.46	Major	 
	Hertha	SB	305.50	Major	 
		MFS	305.53	Minor	 
	Critzer	SB	305.57	Minor	 
		MFS	305.61	Medium	 
	Exline	SB	305.65	Medium	Base of MISSOURIAN regional stage.  FAD of conodonts Idiognathodus eccentricus (Mid-continent; maybe Moscow), has I. sagittalis.  Age estimated here from equal-duration cycles between control points.
		MFS	305.68	Minor	 
	Checkerboard-South Mound	SB	305.72	Minor	Has conodont I. sagittalis (Mid-Continent).  Assigned here as base of Conodont zone Pc13 (Idiognathodus sagittalis), because Idiognathodus makhlinae of Pc12 is reported below (Moscow Basin).
		MFS	305.79	Minor	LAD of conodont Neognathodus (Mid-Continent, Donets); has conodont Swadelina nodocarinata (Mid-Continent) and S. makhlinae (Moscow Basin).  Ratmirovo is base of KHAMOVNICHIAN regional stage of Mosow Basin; however, the implied biostrat would put it just below the "conodont-defined" base of that regional substage => a potential problem.  For the moment, I left the biostrat-defintions (hence ages) be used for those Russian stages, rather then the lithostrat.
	Glenpool	SB	305.85	Minor	Age estimates assume equal-spacing for all Major and Minor cycles (6 in this basal Kasimovian suite) between correlation horizons.
		MFS	305.92	Major	 
	Lost Branch	SB	305.98	Major	has conodont Swadelina nodocarinata (Mid-Continent, maybe Moscow) and S. makhlinae, I trigonolobatus (Moscow Basin).  Fusulinid Beedeina eximia (Mid-Continent).
		MFS	306.05	Minor	 
	Idenbro	SB	306.11	Minor	 
		MFS	306.18	Medium	 
	Norfleet	SB	306.24	Medium	Fusuliids Beedeina megista, B. acme (Mid-Continent).  Swadelina neoshoensis (type; mid-Continent and Donets)
		MFS	306.31	Major	 
	Altamont	SB	306.37	Major	 
		MFS	306.44	Medium	 
	Farlington	SB	306.50	Medium	Conodont S. subexcelsus (Moscow-Donets) [main calibration], Swadelina neoshoensis and Adetognathus (Mid-Continent) = base of Kasimovian stage
		MFS	306.56	Medium	Mid-Continent conodonts Idiognathodus delicatus, I. claviformis, and fusulinid Beedeina.
	Coal City	SB	306.62	Medium	Age estimates assume equal-spacing for all Major and Minor cycles (5 in this latest Mosovian Pf13 suite) between correlation horizons.
		MFS	306.69	Major	 
	Lower Pawnee	SB	306.75	Major	Conodont Idiognathodus fustiformis (type; Mid-Continent)
		MFS	306.81	Minor	 
	Wimer School	SB	306.87	Minor	 
		MFS	306.94	Medium	 
	Higginsville	SB	307.00	Medium	 
		MFS	307.06	Major	 
	Upper Fort Scott	SB	307.12	Major	Mid-Continent fusulinid Beedeina haworthi and B. girtyi; Boreal fusulinid genera Fululina, Fusiella, Fusulinella.  Age assigned as base-Peskovian (base Pf13) based on Moscow-Basin lithostrat and Davdov GTS2004 fusulinid correlations.
		MFS	307.19	Minor	 
	Morgan School	SB	307.25	Minor	Age estimates simply project downward the same spacing as in the upper Moscovian.
		MFS	307.31	Major	 
	Lower Fort Scott	SB	307.37	Major	Mid-Continent fusulinid Beedeina haworthi; Boreal fusulinid Fusulina cylindrica (hence within foram zone Pf12; but FAD is not yet apparent).  This is lowest cycle in Heckel et al (2005) table.
		MFS	307.44	Minor	 
	Breezy Hill	SB	307.50	Minor	 
		MFS	307.56	Medium	 
	Bevier	SB	307.62	Medium	 
		MFS	307.69	Medium	 
	Upper Ardmore	SB	307.75	Medium	 
		MFS	307.81	Major	 
	Verdigris	SB	307.87	Major	 
		MFS	307.94	Minor	 
	Wheeler	SB	308.00	Minor	 
		MFS	308.06	Medium	 
	Fleming	SB	308.12	Medium	 



Sequences -- Major Paleozoic	sequence				off	Haq and Al-Qahtani (GeoArabia, 2005)
		MFS	251.25	Major	91% above base in Changhsingian Stage.  Haq (GeoArabia) chart displays as minor; but general P/T geology hints at a more major change; therefore magnitude is doubled here (-140 m, instead of -125 m)
	Chang1	SB	251.76	Minor	73% above base in Changhsingian Stage
		MFS	252.26	Minor	55% above base in Changhsingian Stage
	Wuch1	SB	256.97	Minor	52% above base in Wuchiapingian Stage
		MFS	259.01	Medium	21% above base in Wuchiapingian Stage
	Cap1	SB	263.48	Major	43% above base in Capitanian Stage
		MFS	264.77	Medium	19% above base in Capitanian Stage
	Kung2	SB	271.00	Major	92% above base in Kungurian Stage
		MFS	272.50	Minor	62% above base in Kungurian Stage
	Kung1	SB	275.78	Minor	98% above base in Artinskian Stage [essentially, base Kungurian]
		MFS	276.74	Minor	67% above base in Artinskian Stage
	Art2	SB	279.21	Minor	59% above base in Artinskian Stage
		MFS	280.00	Minor	50% above base in Artinskian Stage
	Art1	SB	282.02	Minor	27% above base in Artinskian Stage
		MFS	283.26	Medium	13% above base in Artinskian Stage
	Sak2	SB	286.95	Minor	75% above base in Sakmarian Stage
		MFS	289.50	Medium	50% above base in Sakmarian Stage
	Sak1	SB	292.25	Major	23% above base in Sakmarian Stage
		MFS	293.78	Minor	8% above base in Sakmarian Stage
	Ass2	SB	295.26	Minor	85% above base in Asselian Stage
		MFS	296.27	Medium	62% above base in Asselian Stage
	Ass1	SB	299.00	Medium	Base in Asselian Stage
		MFS	300.23	Medium	75% above base in Gzhelian Stage
	Kas1	SB	304.76	Medium	67% above base in Kasimovian Stage
		MFS	307.02	Major	90% above base in Moscovian Stage
	Bash1	SB	312.72	Medium	84% above base in Bashkirian Stage
		MFS	315.99	Major	33% above base in Bashkirian Stage
	Serp1	SB	324.99	Major	17% above base in Serpukhovian Stage
		MFS	332.45	Major	68% above base in Visean Stage
	Vis1	SB	344.92	Major	2% above base in Visean Stage
		MFS	349.47	Major	70% above base in Tournaisian Stage
	Tour1	SB	356.70	Major	18% above base in Tournaisian Stage
		MFS	358.78	Medium	3% above base in Tournaisian Stage
	Fam2	SB	362.72	Medium	77% above base in Famennian Stage
		MFS	363.94	Medium	69% above base in Famennian Stage
	Fam1	SB	367.31	Major	47% above base in Famennian Stage
		MFS	370.52	Major	26% above base in Famennian Stage
	Fras1	SB	379.04	Major	58% above base in Frasnian Stage
		MFS	382.49	Major	26% above base in Frasnian Stage
	Givet1	SB	388.75	Major	47% above base in Givetian Stage
		MFS	390.24	Medium	24% above base in Givetian Stage
	Eif2	SB	392.77	Medium	83% above base in Eifelian Stage
		MFS	394.02	Medium	61% above base in Eifelian Stage
	Eif1	SB	395.73	Medium	31% above base in Eifelian Stage
		MFS	396.76	Medium	13% above base in Eifelian Stage
	Ems3	SB	398.26	Medium	92% above base in Emsian Stage
		MFS	399.02	Medium	84% above base in Emsian Stage
	Ems2	SB	401.02	Major	63% above base in Emsian Stage
		MFS	402.73	Medium	45% above base in Emsian Stage
	Ems1	SB	405.96	Minor	11% above base in Emsian Stage
		MFS	407.00	Major	Base of Emsian Stage
	Prag2	SB	408.76	Medium	58% above base in Pragian Stage
		MFS	409.27	Medium	46% above base in Pragian Stage
	Prag1	SB	410.99	Medium	5% above base in Pragian Stage
		MFS	412.02	Major	83% above base in Lochkovian Stage
	Prid1	SB	416.51	Major	81% above base in Pridoli Epoch
		MFS	419.51	Medium	69% above base in Ludfordian Stage
	Shein1	SB	428.00	Major	10% above base in Sheinwoodian Stage
		MFS	432.47	Minor	46% above base in Telychian Stage
	Aer1	SB	439.00	Major	Base of Aeronian Stage
		MFS	441.26	Medium	52% above base in Rhuddanian Stage
	Kat1	SB	447.54	Major	81% above base in Sixth Stage
		MFS	451.01	Major	47% above base in Sixth Stage
	Darr1	SB	464.00	Medium	57% above base in Darriwillian Stage
		MFS	468.03	Major	1% above base in Darriwillian Stage
	2nd1	SB	475.47	Major	46% above base in Second Stage
		MFS	476.97	Major	24% above base in Second Stage
	Trem2	SB	481.03	Medium	75% above base in Tremadocian Stage
		MFS	482.48	Minor	60% above base in Tremadocian Stage
	Trem1	SB	488.55	Minor	98% above base in Furongian Epoch [Esentially, base of Tremadocian]
		MFS	493.00	Major	63% above base in Furongian Epoch
	3rd1	SB	504.78	Minor	58% above base in Middle Cambrian Epoch [St. Davids]
		MFS	507.39	Major	29% above base in Middle Cambrian Epoch [St. Davids]
	2nd1	SB	515.28	Medium	76% above base in Early Cambrian Epoch => 52% up in Series 2
		MFS	517.48	Major	66% above base in Early Cambrian Epoch, where base-Atdabanian = mid-Early (=base new Series 1) => 32% up in Series 2
	1st2	SB	527.72	Minor	34% above base in Early Cambrian Epoch = equivalent to 68% up in new Series1.
		MFS	530.24	Medium	28% above base in Early Cambrian Epoch = equivalent to 56% up in new Series1.
	1st1	SB	535.28	Minor	16% above base in Early Cambrian Epoch = equivalent to 32% up in new Series1.
		MFS	537.80	Minor	10% above base in Early Cambrian Epoch = equivalent to 20% up in new Series1.  Magnitude (""minor"") is arbitrary for now.


T-R Cycles	trend					CENOZOIC-MESOZOIC = Hardenbol, J., Jacquin, T., Vail, P.R., et al. (SEPM charts. 1998); PALEOZOIC = GTS2004 diagrams
		MSF	0.00	Major	A major transgression-MFS is indicated for Today, which presumes continued melting of glaciers will exceed the Eemian previous maximum highstand.
	LGM	SB	0.02	Major	Last Glacial Maximum; Marine Isotope Stage (MIS) 2
		MFS	2.92	Medium	SEPM chart displays as 3/4ths from base of Pia 1 sequence.  Marine isotope curve suggests this is a very broad highstand, and spans most of "Sequence Pia 1".  This highstand is termination of Pliocene transgressive trend; which is a "Medium" MSF on long-term trend.
	Me 2	SB	5.77	Medium	Middle of Nanno Zone NN11d (CN9d) = midway between LAD of nanno Discoaster quinqueramus and LAD of Amaurolithus amplificus.  This lowstand is minimum of Late Miocene regression; which is a "medium" SB on long-term scale.
		MFS	10.51	Major	Middle of Sequence Ser 4/Tor 1.  This flooding event is a major short transgression in Late Miocene; and indicated as "major" on long-term trend.
	Ser 4/Tor 1	SB	11.80	Major	0.1 myr above Base of Nanno Zone NN7 (CN5b; FAD D. kugleri -- which aslo coincided with Base of Foram Zone M11 =FAD G. nepenthes in Hardenbol chart; but this foram FAD is now placed 0.2 myr later).  Maximum regression of Middle Miocene trend.  Assigned as major SB for Long-Term trend.
		MSF	15.71	Medium	Middle of Sequence Bur 5/Lan 1.  Maximum transgression of Miocene.  But, ranked as "mediium" on long-term trends.
	Ch 4/Aq 1	SB	23.03	Medium	"Base of Miocene (= base of polarity Chron C6Cn.2n; FAD of nannofossil Sphenolithus capricornutus; oxygen isotope event Mi-1).  This base-Miocene is cycle-calibrated in Atlantic ODP Site 926.  SB is culmination of a Late Oligocene regressive trend; but ranked "medium" on long-term."
		MSF	27.97	Major	Middle of Sequence Ch 1.  This Sequence Ch 1 is a short, but significant oscillation of long-term sea-level.
	Ch 1/Ru 4	SB	28.45	Major	Base of Chattian stage (working definition has been LAD of Foram Chiloguembelina (top of Zone P21a); but is diachronous among basins.  Therefore, a temporary working definition is base of Chron C10n.1n (28.45 in GTS2004), and LAD of Chiloguembelina is assigned to this Chron boundary.  Major SB in Cenozoic.
		MSF	30.72	Medium	Slightly above (0.1 myr) middle of Sequence RU3; as is drawn by Hardenbol et al. 1998.  Culmination of long-term transgression of Late Eocene-Early Oligocene
	Lu 4	SB	41.67	Medium	Arbitrarily 0.05 m.y. above midpoint between FADs of foram Turborotalia pomeroli and Globigerapsis index.  Culmination of Middle-Eocene regression.
		MSF	47.03	Minor	Arbitrarily2/3rds up in Nanno Zone NP14b (CP12b).  Termination of short Early Eocene transgression.
	Yp 10	SB	49.78	Major	Arbitrarily2/3rds up in Nanno Zone NP13 (CP11).  Culmination of Late Ypresian regression (major SB).
		MSF	53.01	Minor	Middle of Sequence Yp 5.  End of Late Paleocene-earliest Eocene trangressive trend.
	Th 5	SB	56.57	Minor	Slightly above (0.1 myr) base of Foram Zone P5 (LAD Gl. pseudomenardii).  Termination of latest-Paleogene regressive trend.
		MSF	58.78	Medium	Middle of Sequence Th 1 (approx.Top of Selandian stage working definition).  End of Selandian transgressive trend.
	Sel 1	SB	61.45	Major	Slightly above (0.2 myr) base of Selandian Stage, or slightly below (0.2 myr) middle of Foram Zone P3a.  The later assignment is used here, because Selandian still lacks a ratified definition.  Culmination of Long-term Regression of latest Cretaceous-Danian.
		MSF	69.46	Medium	Middle of Sequence Ma2.  Magnitude of MFS uncertain.
	Ma1	SB	70.56	Medium	Base of Baculites baculus ammonite zone (but could be as high as middle of zone ~0.25myr higher)
		MFS	74.26	Minor	Middle of Cam8 sequence.
	Cam8	SB	75.74	Minor	Base of Didymoceras stevensoni ammonite zone.
		MFS	78.80	Minor	Middle of Cam5 sequence.
	Cam5	SB	80.00	Minor	Base of Baculites asperiformis ammonite zone.
		MFS	83.53	Minor	Base of Scaphites leei III ammonite zone (= base of Campanian stage in N.Amer. scheme).  Magnitude uncertain.
	Sa3	SB	83.99	Minor	Base of Desmoscaphites bassleri ammonite zone.
		MFS	87.88	Major	Base of Scaphites ventricosus ammonite zone.  Magnitude uncertain.
	Tu4	SB	89.54	Minor	2/3rd up in Subprionocyclus neptuni ammonite zone (Tethyan)
		MFS	93.13	Major	Middle of Watinoceras devonense  ammonite zone (Tethyan).  Maximum of Cretaceous Transgression.
	Ce3	SB	96.01	Major	"Base of Cunningtoniceras inerme ammonite zone (Tethyan) = base of "Middle" Cenomanian"
		MFS	98.82	Major	Below (0.15 myr) base of Mantelliceras saxbii subzone of Mantelliceras mantelli ammonite zone.
	Al 11	SB	99.69	Medium	Below (0.15 myr) base of Mantelliceras mantelli ammonite zone (Tethyan) = upper Stoliczkaia dispar zone of uppermost Albian.
		MFS	103.68	Medium	Base of Hysteroceras varicosum ammonite subzone (upper  Mortoniceras inflatum  ammonite zone).
	Al 7	SB	106.42	Medium	Base of Diploceras cristatum  ammonite subzone (upper  Mortoniceras inflatum  ammonite zone).
		MFS	108.70	Medium	Middle of sequence Al 4.
	Al 4	SB	109.21	Minor	Below (0.15 myr) base of Pseudosonneratia (Isohoplites) steinmanni subzone of Douvilleiceras mammillatum ammonite zone (Boreal).
		MFS	111.71	Major	Base of farnhamensis subzone (= lower Leymeriella acuticostata s.z) of Leymeriella tardefurcata ammonite zone (Boreal).
	Ap6	SB	112.40	Major	Just above (0.10 myr) middle of Hypacanthoplites jacobi ammonite zone (Boreal).
		MFS	122.93	Medium	Base of Deshayesites deshayesi ammonite zone (Boreal).
	Ap3	SB	123.97	Major	Base of Deshayesites forbesi ammonite zone (Boreal).
		MFS	126.65	Medium	Approximately at base of I. giraudi  ammonite zone (Tethyan).
	Barr5	SB	127.75	Minor	Base of Hemihoplites sartousi ammonite zone (Tethyan).
		MFS	128.79	Minor	Approx. 2/3rds up in sequence Barr2.
	Barr1	SB	129.64	Minor	Base of Nicklesia nicklesi ammonite zone (Tethyan).
		MFS	131.04	Minor	Approxmately at middle of sequence Ha6
	Ha5	SB	132.56	Major	Base of B. balearis ammonite zone (Tethyan).
		MFS	134.64	Major	Approx. 3/4ths up in sequence Ha2.
	Va3	SB	138.94	Medium	Base of Saynoceras verrucosum ammonite zone (Tethyan).
		MFS	140.42	Major	Approximately middle of Thurmanniceras otopeta ammonite zone (Tethyan).
	Be7	SB	141.33	Medium	Middle of upper half of Tirnovella picteti subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).  Culmination of Latest Jurassic-Earliest Cretaceous Regression.
		MFS	143.12	Minor	Just above (0.10) middle of sequence Be3.
	Ti 5	SB	146.04	Major	Slightly (0.1 myr) above base of Durangites.  Peak of regression in Tithonian
		MFS	152.39	Major	Middle of Aulacostephanus (Pseudomutabilis) eudoxus.  Peak of maximum flooding in Kimm (and in Late Jurassic)
	Ox6	SB	157.04	Minor	Middle of Perisphinctes (Di.) grossouvrei s.z. of Perisphinctes (D.) bifurcatus Zone = Peak lowstand of Oxfordian
		MFS	161.51	Minor	Middle of Q. (L.) lamberti s.z. of Quenstedtoceras (L.) lamberti Zone = Peak of major transgression in Callov-Oxf
	Bat3	SB	166.21	Medium	Middle of Morrisiceras (Morrisiceras) morrisi zone = Peak of regression in Bathonian
		MFS	168.12	Major	1/4 from base of Parkinsonia parkinsoni zone = Peak of transgression in Bajocian-Bathonian
	Aa2	SB	173.38	Major	Base of B. bradfordensis Zone = Peak of regression in Middle and Early Jurassic!
		MFS	181.20	Major	Base of H. bifrons Zone = Peak of major transgression in Middle Jurassic
	PI 8	SB	183.10	Medium	0.1 myr below base of Toarcian =  Peak lowstand at Pliensbachian/Toarcian boundary
		MFS	186.24	Minor	3/4 up in PI 5 sequence;  Peak of transgression in early Pliensbachian.
	PI 2	SB	188.41	Minor	Base of T. ibex Zone  (lower half of T. ibex is a long lowstand and common hiatus = Peak of major lowstand in Early Jurassic
		MFS	193.79	Minor	2/3rds up in Caenisites turneri s.z. (lower C. turneri Zone) = Peak of major transgression in Early Jurassic
	No2	SB	205.56	Major	Just above (0.15 myr) the base of Sag. quinquepunctatus s.z.  Peak Regression of Middle-Late Triassic major trend.
		MFS	219.42	Minor	1/3rd up in Tropites subbullatus zone.  Peak of short, but major Transgressin in Late Carnian.
	Car3	SB	221.39	Minor	3/4ths up in Tropites dilleri zone.  A short, but major transgressive event follows this lowstand.  This major transgression is interpreted to begin earlier in Boreal series (one sequence earlier).
		MFS	226.30	Minor	Middle of Trachyceras aonoides subzone.  Peak of Late Ladinian through early Carnian transgression
	Lad3	SB	229.64	Medium	3/4ths up in P. neumayri s.z.  Peak Lowstand of Ladinian regressive trend.
		MFS	237.50	Medium	Middle of C. chiesense s.z.  Peak flooding of long-term Early Triassic transgression.  This peak is interpreted as later (one higher MFS = base of T. poseidon Zone) in Boreal realm.
	Ol 4	SB	245.41	Medium	1/3rd up in "gap zone" above Toziceras pakistanum zone.  Peak of short, but major Regression at end of Early Triassic.  In Boreal realm, this short-major Regression is assigned as spanning most of the Smithian stage instead; implies peak Regression at Ol 1, and the culmination of the underlying transgression at mid-Hedenstroemi Zone.  This fits Arctic better?
		MFS	246.92	Major	3/5ths up I Sequence Ol 2.  Peak flooding of Transgressive trend of Early Triassic.
	end-Perm	SB	251.76	Major	75% up in Changhsingian. Conclusion of Late Permian regressive trend.
		MFS	255.78	Major	70% above base in Wuchiapingian
	Wuch1	SB	260.40	Major	Base of Wuchiapingian Stage
		MFS	263.91	Major	35% above base in Capitanian Stage
	Cap1	SB	265.26	Major	10% above base in Capitanian Stage
		MFS	267.12	Major	40% above base in Wordian Stage
	Road1	SB	270.47	Major	5% above base in Roadian Stage
		MFS	271.85	Major	75% above base in Kungurian Stage
	Kung2	SB	273.10	Major	50% above base in Kungurian Stage
		MFS	274.35	Major	25% above base in Kungurian Stage
	Kung1	SB	275.60	Major	Base of Kungurian Stage
		MFS	279.12	Major	60% above base in Artinskian Stage
	Art1	SB	284.40	Major	Base of Artinskian
		MFS	289.50	Major	50% above base in Sakmarian Stage
	Ass1	SB	294.82	Major	95% above base in Asselian Stage
		MFS	299.00	Major	Base of Asselian Stage
	Gzh2	SB	301.45	Major	50% above base in Gzhelian Stage
		MFS	302.43	Major	30% above base in Gzhelian Stage
	Gzh1	SB	303.90	Major	Base of Gzhelian Stage
		MFS	305.72	Major	30% above base in Kasimovian
	Kas1	SB	306.37	Major	5% above base in Kasimovian
		MFS	309.10	Major	50% above base in Moscovian Stage
	Mosc1	SB	310.14	Major	30% above base in Moscovian Stage
		MFS	310.92	Major	15% above base in Moscovian Stage
	Bash2	SB	312.66	Major	85% above base in Bashkirian Stage
		MFS	313.94	Major	65% above base in Bashkirian Stage
	Bash1	SB	317.78	Major	5% above base in Bashkirian Stage
		MFS	323.08	Major	40% above base in Serpukhovian Stage
	Vis2	SB	333.02	Major	65% above base in Visean Stage
		MFS	335.85	Major	50% above base in Visean Stage
	Vis1	SB	343.41	Major	10% above base in Visean Stage
		MFS	345.30	Major	Base of Visean Stage
	Tour2	SB	348.08	Major	80% above base in Tournaisian Stage
		MFS	350.17	Major	65% above base in Tournaisian Stage
	Tour1	SB	357.12	Major	15% above base in Tournaisian Stage
		MFS	358.51	Major	5% above base in Tournaisian Stage
	Fam1	SB	366.09	Major	55% above base in Famennian Stage
		MFS	372.97	Major	10% above base in Famennian Stage
	Fras1	SB	380.44	Major	45% above base in Frasnian Stage
		MFS	388.23	Major	55% above base in Givetian Stage
	Giv1	SB	389.85	Major	30% above base in Givetian Stage
		MFS	391.80	Major	Base of Givetian Stage
	Eif1	SB	393.80	Major	65% above base in Eifelian Stge
		MFS	397.50	Major	Base of Eifelian
	Ems1	SB	400.35	Major	70% above base in Emsian Stage
		MFS	405.58	Major	15% above base in Emsian Stage
	Prag2	SB	407.21	Major	95% above base in Pragian Stage
		MFS	409.73	Major	35% above base in Pragian Stage
	Prag1	SB	411.20	Major	Base of Pragian
		MFS	412.40	Major	75% above base in Lochkovian
	Loch1	SB	416.00	Major	Base of Devonian assumed -- A latest Silurian regressive trend is in Silurian chapter, but a earliest Devonian transgressive trend is in Devonian chapter !
		MFS	422.26	Major	40% above base in Gorstian Stage
	Hom1	SB	424.39	Major	55% above base in Homerian Stage
		MFS	427.30	Major	45% above base in Sheinwoodian Stage
	Shein1	SB	428.00	Major	10% above base in Sheinwoodian Stage
		MFS	428.91	Major	91% above base in Telychian Stage
	Tely2	SB	431.76	Major	55% above base in Telychian Stage
		MFS	432.94	Major	40% above base in Telychian Stage
	Tely1	SB	436.10	Major	Base of Telychian
		MFS	436.68	Major	80% above base in Aeronian Stage
	Aer1	SB	437.26	Major	60% above base in Aeronian Stage
		MFS	438.28	Major	25% above base in Aeronian Stage
	Hirn1	SB	444.75	Major	45% above base in Hirnantian Stage
		MFS	451.72	Major	40% above base in Sixth Stage
	5th1	SB	457.84	Major	60% above base in Fifth Stage
		MFS	460.90	Major	Base of Fifth Stage
	Darr1	SB	463.42	Major	65% above base in Darriwillian
		MFS	474.52	Major	60% above base in Second Stage
	Trem2	SB	483.45	Major	50% above base in Tremadocian Stage
		MFS	486.36	Major	20% above base in Tremadocian
	Trem1	SB	488.30	Major	Base of Tremadocian


Devonian T-R Cycles	trend				off	Johnson et al. (1985)	
		SB	359.2	Major
		MSF	361.5	Major
		SB	365.32	Major
		MSF	372.01	Major
		SB	374.04	Major
		MSF	377.20	Major
		SB	389.49	Major
		MSF	390.42	Major
		SB	399.40	Major
		MSF	402.54	Major
		SB	408.47	Major
		MSF	409.79	Major
		SB	411.20	Major

Major T-R Cycles	trend					CENOZOIC-MESOZOIC = Hardenbol, J., Jacquin, T., Vail, P.R., et al. (SEPM charts. 1998)
		SB	0.00	Major	Today
		MSF	15.71	Medium	Middle of Sequence Bur 5/Lan 1.  Maximum transgression of Miocene.  But, ranked as "mediium" on long-term trends.
	Ch 1/Ru 4	SB	28.45	Major	Base of Chattian stage (working definition has been LAD of Foram Chiloguembelina (top of Zone P21a); but is diachronous among basins.  Therefore, a temporary working definition is base of Chron C10n.1n (28.45 in GTS2004), and LAD of Chiloguembelina is assigned to this Chron boundary.  Major SB in Cenozoic.
		MSF	53.01	Medium	Middle of Sequence Yp 5.  End of Late Paleocene-earliest Eocene trangressive trend.
	Sel 1	SB	61.45	Major	Slightly above (0.2 myr) base of Selandian Stage, or slightly below (0.2 myr) middle of Foram Zone P3a.  The later assignment is used here, because Selandian still lacks a ratified definition.  Culmination of Long-term Regression of latest Cretaceous-Danian.
		MFS	93.13	Major	Middle of Watinoceras devonense  ammonite zone (Tethyan).  Maximum of Cretaceous Transgression.
	Be7	SB	141.33	Major	Middle of upper half of Tirnovella picteti subzone of Berriasella (Fauriella) boissieri ammonite zone (Tethyan).  Culmination of Latest Jurassic-Earliest Cretaceous Regression.
		MFS	152.39	Major	Middle of Aulacostephanus (Pseudomutabilis) eudoxus.  Peak of maximum flooding in Kimm (and in Late Jurassic)
	Aa2	SB	173.38	Major	Base of B. bradfordensis Zone = Peak of regression in Middle and Early Jurassic!
		MFS	181.20	Major	Base of H. bifrons Zone = Peak of major transgression in Middle Jurassic
	No2	SB	205.56	Major	Just above (0.15 myr) the base of Sag. quinquepunctatus s.z.  Peak Regression of Middle-Late Triassic major trend.
		MFS	237.50	Medium	Middle of C. chiesense s.z.  Peak flooding of long-term Early Triassic transgression.  This peak is interpreted as later (one higher MFS = base of T. poseidon Zone) in Boreal realm.
	end-Perm	SB	251.76	Major	75% up in Changhsingian. Conclusion of Late Permian regressive trend.


Sea-Level Curves (meters relative to present)	:	High-Res Plio-Pleist	Short-Term Phanerozoic	Long-Term Phanerozoic (SEPM98-Haq'05)	Long-Term Meso-Ceno (Tapscott SEPM98)	_METACOLUMN_OFF	

High-Res Plio-Pleist	point				off	Miller et al. (Science, 2005) based on conversion of oxygen-isotope data. They have similar detail extending back to 9 Ma, and a generalized curve back to 170 Ma, but the time scales in their table are Berggren et al (1995) and Gradstein et al (1994), which significantly diverge from GTS2004 below 5.32 myr, therefore this older curve is omitted until conversions are available.
nopoints	line		-125	50
	0.000	-1.6
	0.005	-3.3
	0.010	-52.4
	0.015	-120.4
	0.020	-122.2
	0.025	-99.1
	0.030	-102.6
	0.035	-91.0
	0.040	-85.7
	0.045	-80.4
	0.050	-75.3
	0.055	-87.8
	0.060	-76.1
	0.065	-85.2
	0.070	-57.9
	0.075	-52.9
	0.080	-47.4
	0.085	-49.0
	0.090	-55.1
	0.095	-50.6
	0.100	-39.2
	0.105	-42.8
	0.110	-72.4
	0.115	-4.3
	0.120	24.0
	0.125	-1.9
	0.130	-76.3
	0.135	-96.9
	0.140	-107.7
	0.145	-97.0
	0.150	-93.9
	0.155	-102.2
	0.160	-90.3
	0.165	-78.5
	0.170	-67.8
	0.175	-72.0
	0.180	-81.7
	0.185	-45.3
	0.190	-49.0
	0.195	-18.2
	0.200	-34.2
	0.205	-17.6
	0.210	-13.4
	0.215	-7.3
	0.220	-23.6
	0.225	-74.1
	0.230	-68.3
	0.235	-59.5
	0.240	-28.6
	0.245	-60.3
	0.250	-66.8
	0.255	-85.4
	0.260	-79.1
	0.265	-79.7
	0.270	-86.0
	0.275	-54.1
	0.280	-43.4
	0.285	-39.3
	0.290	-39.5
	0.295	-55.8
	0.300	-45.8
	0.305	-39.7
	0.310	-34.8
	0.315	-23.0
	0.320	-31.4
	0.325	11.1
	0.330	-16.8
	0.335	-26.0
	0.340	-83.1
	0.345	-96.8
	0.350	-92.0
	0.355	-90.6
	0.360	-104.0
	0.365	-55.4
	0.370	-85.2
	0.375	-58.4
	0.380	-52.7
	0.385	-52.1
	0.390	-31.9
	0.395	-30.6
	0.400	-9.5
	0.405	12.5
	0.410	12.8
	0.415	-0.2
	0.420	-29.5
	0.425	-84.7
	0.430	-115.3
	0.435	-122.1
	0.440	-122.7
	0.445	-102.4
	0.450	-84.8
	0.455	-87.5
	0.460	-82.7
	0.465	-99.9
	0.470	-96.7
	0.475	-73.7
	0.480	-53.4
	0.485	-35.0
	0.490	-34.9
	0.495	-39.7
	0.500	-23.4
	0.505	-60.8
	0.510	-68.6
	0.515	-78.8
	0.520	-61.2
	0.525	-54.8
	0.530	-78.3
	0.535	-75.3
	0.540	-84.6
	0.545	-73.7
	0.550	-66.5
	0.555	-73.0
	0.560	-65.0
	0.565	-50.6
	0.570	-41.6
	0.575	-25.6
	0.580	-25.6
	0.585	-67.6
	0.590	-79.1
	0.595	-56.5
	0.600	-49.0
	0.605	-52.8
	0.610	-39.2
	0.615	-50.7
	0.620	-72.9
	0.625	-117.8
	0.630	-124.2
	0.635	-114.3
	0.640	-122.7
	0.645	-111.9
	0.650	-106.4
	0.655	-101.6
	0.660	-93.3
	0.665	-80.5
	0.670	-91.7
	0.675	-80.0
	0.680	-82.8
	0.685	-82.4
	0.690	-53.8
	0.695	-62.2
	0.700	-70.5
	0.705	-78.9
	0.710	-87.2
	0.715	-95.1
	0.720	-96.4
	0.725	-63.7
	0.730	-70.4
	0.735	-75.5
	0.740	-77.6
	0.745	-73.6
	0.750	-86.1
	0.755	-91.5
	0.760	-85.4
	0.765	-62.3
	0.770	-53.0
	0.775	-45.1
	0.780	-21.8
	0.785	-44.2
	0.790	-48.5
	0.795	-98.0
	0.800	-82.5
	0.805	-77.2
	0.810	-58.6
	0.815	-41.3
	0.820	-55.7
	0.825	-52.6
	0.830	-51.1
	0.835	-48.4
	0.840	-27.6
	0.845	-24.3
	0.850	-36.2
	0.855	-33.0
	0.860	-19.3
	0.865	-61.6
	0.870	-83.6
	0.875	-109.3
	0.880	-106.9
	0.885	-93.7
	0.890	-90.1
	0.895	-84.3
	0.900	-64.2
	0.905	-60.3
	0.910	-74.6
	0.915	-89.1
	0.920	-66.8
	0.925	-51.5
	0.930	-31.2
	0.935	-22.2
	0.940	-19.8
	0.945	-9.8
	0.950	2.0
	0.955	-40.6
	0.960	-41.1
	0.965	-57.3
	0.970	-38.6
	0.975	-27.9
	0.980	-42.6
	0.985	-46.6
	0.990	-29.3
	0.995	-48.1
	1.000	-54.7
	1.005	-65.7
	1.010	-66.8
	1.015	-31.9
	1.020	-27.0
	1.025	-38.0
	1.030	-68.6
	1.035	-75.2
	1.040	-85.3
	1.045	-75.1
	1.050	-69.1
	1.055	-63.4
	1.060	-56.6
	1.065	-5.8
	1.070	-48.6
	1.075	-15.1
	1.080	-20.4
	1.085	-55.5
	1.090	-68.3
	1.095	-58.7
	1.100	-73.9
	1.105	-40.0
	1.110	-37.7
	1.115	-52.8
	1.120	-70.5
	1.125	-79.4
	1.130	-77.1
	1.135	-75.1
	1.140	-72.0
	1.145	-42.7
	1.150	-38.9
	1.155	-41.1
	1.160	-20.6
	1.165	-26.3
	1.170	-18.3
	1.175	-31.8
	1.180	-19.0
	1.185	-33.4
	1.190	-60.4
	1.195	-56.4
	1.200	-42.1
	1.205	-59.5
	1.210	-57.5
	1.215	-60.0
	1.220	-47.2
	1.225	-29.6
	1.230	-25.1
	1.235	-23.6
	1.240	-7.8
	1.245	-36.6
	1.250	-78.6
	1.255	-91.7
	1.260	-71.6
	1.265	-61.9
	1.270	-42.4
	1.275	-30.8
	1.280	-34.1
	1.285	-61.9
	1.290	-70.3
	1.295	-55.9
	1.300	-55.6
	1.305	-55.0
	1.310	-40.5
	1.315	-29.7
	1.320	-25.5
	1.325	-58.7
	1.330	-56.5
	1.335	-58.2
	1.340	-50.9
	1.345	-40.7
	1.350	-11.8
	1.355	-4.7
	1.360	-36.9
	1.365	-49.8
	1.370	-64.9
	1.375	-58.0
	1.380	-55.4
	1.385	-38.5
	1.390	-25.7
	1.395	-11.6
	1.400	-19.7
	1.405	-36.2
	1.410	-49.7
	1.415	-63.9
	1.420	-69.3
	1.425	-61.9
	1.430	-39.1
	1.435	-7.2
	1.440	-3.5
	1.445	4.3
	1.450	10.1
	1.455	-44.2
	1.460	-75.0
	1.465	-50.1
	1.470	-27.0
	1.475	-22.1
	1.480	-6.5
	1.485	2.7
	1.490	0.0
	1.495	-26.3
	1.500	-60.7
	1.505	-68.1
	1.510	-58.3
	1.515	-41.3
	1.520	-19.4
	1.525	-22.3
	1.530	-41.4
	1.535	-52.8
	1.540	-78.4
	1.545	-66.2
	1.550	-34.2
	1.555	-44.2
	1.560	-31.6
	1.565	-32.4
	1.570	-27.5
	1.575	-60.8
	1.580	-54.1
	1.585	-38.1
	1.590	-33.7
	1.595	-29.9
	1.600	-31.5
	1.605	-25.3
	1.610	-24.0
	1.615	-28.6
	1.620	-33.2
	1.625	-28.1
	1.630	-38.4
	1.635	-32.2
	1.640	-39.3
	1.645	-65.1
	1.650	-49.3
	1.655	-69.8
	1.660	-59.2
	1.665	-60.4
	1.670	-29.9
	1.675	-21.8
	1.680	-20.4
	1.685	-15.0
	1.690	-34.5
	1.695	-56.7
	1.700	-49.2
	1.705	-48.0
	1.710	-36.6
	1.715	-25.1
	1.720	-20.3
	1.725	-32.7
	1.730	-10.0
	1.735	-30.7
	1.740	-17.5
	1.745	-15.2
	1.750	-54.5
	1.755	-25.8
	1.760	-10.9
	1.765	-28.4
	1.770	-2.9
	1.775	-14.2
	1.780	-43.3
	1.785	-28.8
	1.790	-52.0
	1.795	-43.5
	1.800	-18.9
	1.805	-40.0
	1.810	-37.6
	1.815	-9.6
	1.820	-21.6
	1.825	-48.7
	1.830	-23.4
	1.835	-19.7
	1.840	-46.8
	1.845	-14.4
	1.850	-11.2
	1.855	14.4
	1.860	-10.4
	1.865	-22.0
	1.870	-16.0
	1.875	-17.6
	1.880	-17.6
	1.885	-7.6
	1.890	3.2
	1.895	-5.6
	1.900	-11.2
	1.905	-36.8
	1.910	-56.0
	1.915	-68.4
	1.920	-40.0
	1.925	-40.0
	1.930	-16.8
	1.935	-12.0
	1.940	-14.1
	1.945	-11.6
	1.950	-12.8
	1.955	-44.0
	1.960	-37.2
	1.965	-31.6
	1.970	-14.4
	1.975	-3.2
	1.980	5.6
	1.985	-42.4
	1.990	-28.0
	1.995	-29.3
	2.000	-28.3
	2.005	-34.4
	2.010	-29.6
	2.015	-16.0
	2.020	6.1
	2.025	-3.6
	2.030	-17.6
	2.035	-12.8
	2.040	-13.2
	2.045	-36.0
	2.050	-11.2
	2.055	17.6
	2.060	-4.0
	2.065	-6.4
	2.070	-13.6
	2.075	-36.0
	2.080	-36.8
	2.085	-69.6
	2.090	-37.6
	2.095	-41.2
	2.100	-6.0
	2.105	-13.6
	2.110	-24.0
	2.115	-18.7
	2.120	-14.4
	2.125	-32.8
	2.130	-24.6
	2.135	-10.9
	2.140	4.8
	2.145	-8.8
	2.150	-44.3
	2.155	-46.4
	2.160	-64.8
	2.165	-60.8
	2.170	-49.6
	2.175	-38.4
	2.180	-31.7
	2.185	-20.5
	2.190	-5.6
	2.195	-6.8
	2.200	-26.8
	2.205	-28.8
	2.210	-2.0
	2.215	0.4
	2.220	-2.4
	2.225	-6.4
	2.230	-8.8
	2.235	2.4
	2.240	-28.0
	2.245	-47.6
	2.250	-24.0
	2.255	-6.4
	2.260	-1.6
	2.265	13.6
	2.270	3.2
	2.275	-34.4
	2.280	-44.0
	2.285	-41.6
	2.290	-27.5
	2.295	-8.8
	2.300	10.4
	2.305	1.6
	2.310	-7.5
	2.315	-25.4
	2.320	-16.0
	2.325	4.0
	2.330	0.0
	2.335	-1.1
	2.340	-9.9
	2.345	11.2
	2.350	23.2
	2.355	1.6
	2.360	-28.3
	2.365	-40.2
	2.370	-29.3
	2.375	-17.3
	2.380	-8.8
	2.385	6.0
	2.390	24.8
	2.395	20.8
	2.400	-4.8
	2.405	-24.0
	2.410	-19.7
	2.415	-20.0
	2.420	-8.8
	2.425	0.0
	2.430	-7.0
	2.435	-1.6
	2.440	-12.0
	2.445	-54.4
	2.450	-49.6
	2.455	-35.2
	2.460	-36.0
	2.465	-21.6
	2.470	8.8
	2.475	10.8
	2.480	-21.6
	2.485	-57.2
	2.490	-50.4
	2.495	-39.5
	2.500	-30.4
	2.505	-4.6
	2.510	-9.2
	2.515	-28.9
	2.520	-46.4
	2.525	-56.2
	2.530	-53.2
	2.535	-36.6
	2.540	-2.4
	2.545	17.8
	2.550	-21.2
	2.555	-15.8
	2.560	-6.0
	2.565	-7.1
	2.570	-2.8
	2.575	3.4
	2.580	11.2
	2.585	10.7
	2.590	6.3
	2.595	-3.4
	2.600	-35.2
	2.605	-55.4
	2.610	-42.8
	2.615	-41.0
	2.620	-28.8
	2.625	-6.9
	2.630	-4.8
	2.635	4.2
	2.640	-1.6
	2.645	-29.5
	2.650	-26.4
	2.655	-36.2
	2.660	-16.0
	2.665	7.0
	2.670	11.6
	2.675	6.9
	2.680	-1.2
	2.685	-14.6
	2.690	-42.0
	2.695	-39.8
	2.700	-18.8
	2.705	-19.0
	2.710	-40.4
	2.715	-38.2
	2.720	-45.2
	2.725	-29.0
	2.730	-54.8
	2.735	-30.2
	2.740	-25.6
	2.745	-29.8
	2.750	20.4
	2.755	21.8
	2.760	14.4
	2.765	4.6
	2.770	-5.2
	2.775	-18.2
	2.780	-4.8
	2.785	5.4
	2.790	6.5
	2.795	-8.6
	2.800	-2.0
	2.805	-8.0
	2.810	-32.4
	2.815	-39.8
	2.820	-43.2
	2.825	-17.0
	2.830	-12.4
	2.835	-4.0
	2.840	-5.6
	2.845	-22.6
	2.850	-17.2
	2.855	-29.4
	2.860	-26.4
	2.865	-7.8
	2.870	-5.5
	2.875	-15.0
	2.880	-6.4
	2.885	-33.0
	2.890	-40.0
	2.895	-22.6
	2.900	-13.6
	2.905	-5.8
	2.910	-5.6
	2.915	-14.5
	2.920	-8.8
	2.925	-9.0
	2.930	-26.0
	2.935	-40.6
	2.940	-5.6
	2.945	-0.2
	2.950	15.6
	2.955	14.6
	2.960	-1.6
	2.965	3.0
	2.970	-13.7
	2.975	-22.2
	2.980	-6.4
	2.985	12.3
	2.990	13.2
	2.995	17.0
	3.000	2.4
	3.005	-13.3
	3.010	-20.1
	3.015	-32.2
	3.020	-17.6
	3.025	-17.8
	3.030	-15.6
	3.035	3.8
	3.040	9.6
	3.045	8.1
	3.050	-2.5
	3.055	-3.8
	3.060	-11.2
	3.065	7.0
	3.070	14.0
	3.075	20.2
	3.080	7.2
	3.085	-10.2
	3.090	-11.3
	3.095	-6.2
	3.100	-6.4
	3.105	2.7
	3.110	2.0
	3.115	-7.8
	3.120	-18.9
	3.125	-41.0
	3.130	-10.5
	3.135	-33.8
	3.140	-48.8
	3.145	-50.6
	3.150	-24.9
	3.155	-13.9
	3.160	-4.4
	3.165	-10.6
	3.170	-10.5
	3.175	-23.0
	3.180	-20.0
	3.185	-29.5
	3.190	-23.1
	3.195	-2.2
	3.200	-0.2
	3.205	-4.2
	3.210	-12.6
	3.215	-6.0
	3.220	-13.6
	3.225	-23.8
	3.230	-4.4
	3.235	-15.6
	3.240	-7.2
	3.245	-16.2
	3.250	-7.6
	3.255	-15.0
	3.260	-4.6
	3.265	-11.4
	3.270	-13.2
	3.275	-0.6
	3.280	-10.4
	3.285	0.9
	3.290	-7.6
	3.295	-3.5
	3.300	-12.0
	3.305	-67.4
	3.310	-51.3
	3.315	-62.2
	3.320	-48.0
	3.325	-34.3
	3.330	-32.0
	3.335	-39.8
	3.340	-62.0
	3.345	-45.8
	3.350	-51.6
	3.355	-42.2
	3.360	-32.8
	3.365	-31.0
	3.370	-15.6
	3.375	-16.6
	3.380	-15.7
	3.385	-19.4
	3.390	-17.2
	3.395	-27.5
	3.400	-24.0
	3.405	-21.0
	3.410	2.8
	3.415	-30.2
	3.420	-21.2
	3.425	-15.8
	3.430	-29.6
	3.435	-35.4
	3.440	-28.4
	3.445	-18.2
	3.450	-8.4
	3.455	3.0
	3.460	-22.4
	3.465	-10.6
	3.470	4.4
	3.475	-6.5
	3.480	-16.8
	3.485	-13.0
	3.490	-4.9
	3.495	-1.7
	3.500	5.0
	3.505	-2.2
	3.510	2.4
	3.515	-1.1
	3.520	-12.8
	3.525	-1.6
	3.530	-4.8
	3.535	8.8
	3.540	1.6
	3.545	-10.8
	3.550	-17.6
	3.555	3.6
	3.560	-18.4
	3.565	-8.0
	3.570	-10.4
	3.575	4.4
	3.580	-7.2
	3.585	-21.6
	3.590	-28.0
	3.595	-7.5
	3.600	-2.4
	3.605	-9.8
	3.610	-8.5
	3.615	18.4
	3.620	-0.8
	3.625	-23.8
	3.630	-25.1
	3.635	-34.4
	3.640	3.2
	3.645	1.2
	3.650	1.6
	3.655	7.2
	3.660	-2.1
	3.665	-12.6
	3.670	-20.8
	3.675	-26.7
	3.680	-30.0
	3.685	-22.7
	3.690	-17.6
	3.695	-0.8
	3.700	20.8
	3.705	-9.6
	3.710	1.9
	3.715	-11.2
	3.720	-20.0
	3.725	-10.4
	3.730	-4.4
	3.735	6.8
	3.740	6.0
	3.745	4.0
	3.750	3.4
	3.755	-0.3
	3.760	-9.3
	3.765	1.6
	3.770	16.8
	3.775	12.8
	3.780	15.4
	3.785	-7.2
	3.790	-20.8
	3.795	-19.0
	3.800	1.0
	3.805	-2.9
	3.810	-8.0
	3.815	-11.7
	3.820	-9.6
	3.825	-14.0
	3.830	-3.0
	3.835	-0.8
	3.840	-17.4
	3.845	-28.8
	3.850	7.2
	3.855	18.6
	3.860	22.1
	3.865	-0.8
	3.870	14.0
	3.875	-2.4
	3.880	-11.8
	3.885	-18.8
	3.890	-0.6
	3.895	-1.1
	3.900	14.4
	3.905	-12.0
	3.910	-2.4
	3.915	-5.6
	3.920	4.0
	3.925	-5.6
	3.930	-3.6
	3.935	3.2
	3.940	13.3
	3.945	-14.7
	3.950	-14.1
	3.955	5.6
	3.960	-10.8
	3.965	-10.4
	3.970	-16.8
	3.975	-18.4
	3.980	-13.6
	3.985	-24.5
	3.990	-23.2
	3.995	-56.4
	4.000	-40.8
	4.005	-25.6
	4.010	-17.2
	4.015	3.2
	4.020	-16.0
	4.025	-10.4
	4.030	-12.0
	4.035	-33.3
	4.040	-36.6
	4.045	-34.8
	4.050	-34.4
	4.055	-18.4
	4.060	-12.4
	4.065	-11.2
	4.070	-5.9
	4.075	-12.2
	4.080	-3.7
	4.085	-8.6
	4.090	-19.8
	4.095	-20.8
	4.100	-5.2
	4.105	10.4
	4.110	4.0
	4.115	-2.7
	4.120	-10.4
	4.125	-1.2
	4.130	-12.0
	4.135	-3.2
	4.140	-16.8
	4.145	-20.5
	4.150	-7.6
	4.155	12.0
	4.160	10.2
	4.165	6.2
	4.170	0.6
	4.175	9.6
	4.180	-0.4
	4.185	3.2
	4.190	0.8
	4.195	-2.1
	4.200	-2.6
	4.205	6.9
	4.210	-13.6
	4.215	-18.4
	4.220	5.2
	4.225	3.2
	4.230	-7.6
	4.235	-20.0
	4.240	-12.6
	4.245	3.2
	4.250	-12.8
	4.255	-34.0
	4.260	-16.4
	4.265	-16.0
	4.270	4.0
	4.275	10.6
	4.280	9.5
	4.285	-8.8
	4.290	-16.3
	4.295	-7.2
	4.300	0.4
	4.305	-10.7
	4.310	-17.0
	4.315	3.2
	4.320	14.4
	4.325	8.0
	4.330	16.8
	4.335	4.0
	4.340	0.5
	4.345	4.0
	4.350	-14.9
	4.355	-2.4
	4.360	-10.9
	4.365	-7.7
	4.370	2.7
	4.375	-22.4
	4.380	-8.0
	4.385	-8.8
	4.390	-6.4
	4.395	-2.7
	4.400	-17.3
	4.405	-0.4
	4.410	-3.2
	4.415	16.0
	4.420	-21.1
	4.425	-2.0
	4.430	11.2
	4.435	-1.4
	4.440	13.9
	4.445	-3.2
	4.450	-8.0
	4.455	18.8
	4.460	3.0
	4.465	7.5
	4.470	15.4
	4.475	14.2
	4.480	5.3
	4.485	20.8
	4.490	1.6
	4.495	0.4
	4.500	-2.4
	4.505	-3.6
	4.510	-3.2
	4.515	-17.6
	4.520	-19.2
	4.525	1.3
	4.530	9.6
	4.535	-2.4
	4.540	-3.2
	4.545	-6.4
	4.550	-8.4
	4.555	-24.0
	4.560	-21.2
	4.565	-15.2
	4.570	-13.6
	4.575	-12.0
	4.580	-10.1
	4.585	2.4
	4.590	-10.8
	4.595	-31.2
	4.600	-12.0
	4.605	0.8
	4.610	-16.8
	4.615	-18.0
	4.620	-4.4
	4.625	2.4
	4.630	-18.7
	4.635	-21.1
	4.640	-7.2
	4.645	-7.2
	4.650	3.5
	4.655	-1.1
	4.660	8.8
	4.665	-5.1
	4.670	-37.6
	4.675	-8.8
	4.680	-27.2
	4.685	-7.0
	4.690	-18.8
	4.695	-18.4
	4.700	-5.6
	4.705	-20.8
	4.710	-28.0
	4.715	-27.4
	4.720	-33.3
	4.725	-7.2
	4.730	-5.3
	4.735	-29.6
	4.740	4.8
	4.745	-10.4
	4.750	-30.4
	4.755	-31.3
	4.760	-16.3
	4.765	-7.6
	4.770	5.6
	4.775	-9.0
	4.780	-1.0
	4.785	-4.8
	4.790	-23.0
	4.795	-9.6
	4.800	-7.2
	4.805	21.3
	4.810	12.0
	4.815	12.3
	4.820	12.6
	4.825	-30.4
	4.830	-45.6
	4.835	-38.4
	4.840	-7.6
	4.845	-8.0
	4.850	-4.8
	4.855	-1.6
	4.860	-11.2
	4.865	-23.6
	4.870	-42.8
	4.875	-48.4
	4.880	-40.4
	4.885	-41.6
	4.890	-11.2
	4.895	4.0
	4.900	-4.0
	4.905	-10.1
	4.910	-12.8
	4.915	-5.6
	4.920	-3.2
	4.925	-18.4
	4.930	-21.6
	4.935	-20.0
	4.940	-10.4
	4.945	-4.4
	4.950	-14.6
	4.955	-21.6
	4.960	3.0
	4.965	-18.4
	4.970	1.1
	4.975	3.7
	4.980	9.9
	4.985	-0.8
	4.990	4.3
	4.995	-3.4
	5.000	-7.2
	5.005	-6.2
	5.010	-19.2
	5.015	0.0
	5.020	-1.0
	5.025	5.0
	5.030	4.3
	5.035	-2.4
	5.040	-22.1
	5.045	-28.8
	5.050	-19.5
	5.055	-11.7
	5.060	-12.6
	5.065	-8.0
	5.070	-4.3
	5.075	-10.2
	5.080	-4.5
	5.085	12.6
	5.090	-5.6
	5.095	16.0
	5.100	6.0
	5.105	25.6
	5.110	-4.0
	5.115	-17.6
	5.120	-2.4
	5.125	4.0
	5.130	16.0
	5.135	26.8
	5.140	6.4
	5.145	3.2
	5.150	-3.2
	5.155	-5.6
	5.160	-23.2
	5.165	-24.8
	5.170	3.2
	5.175	13.6
	5.180	-2.2
	5.185	1.6
	5.190	2.4
	5.195	7.6
	5.200	8.0
	5.205	8.7
	5.210	1.8
	5.215	2.4
	5.220	2.4
	5.225	-7.7
	5.230	-6.2
	5.235	-4.6
	5.240	-4.8
	5.245	-27.2
	5.250	2.8
	5.255	14.4
	5.260	8.4
	5.265	5.2
	5.270	0.8
	5.275	-12.8
	5.280	2.8
	5.285	11.2
	5.290	16.8
	5.295	3.0
	5.300	-8.0
	5.305	3.2
	5.310	7.5
	5.315	16.8
	5.320	10.4


Short-Term Phanerozoic	point				off	CENOZOIC-MESOZOIC = Hardenbol, J., et al. (SEPM charts. 1998); PALEOZOIC = Haq and Al-Qahtani (2005); amplitudes of SEPM'98 Triassic sequences are offset from long-term Triassic curve by Haq and Al-Qahtani (2005) following advice of Bilal Haq (pers. comm. to J.Ogg, April, 2006).
nopoints	line		-150	285	smoothed
	1.779	27.38
	2.260	-67.91
	2.621	27.38
	3.053	-58.94
	3.492	28.32
	3.837	-23.57
	4.357	74.55
	4.535	68.42
	5.168	97.13
	5.566	-30.64
	6.080	45.64
	6.863	-16.96
	7.815	23.13
	8.752	-24.51
	10.228	12.69
	11.276	-68.38
	12.215	66.47
	12.548	55.68
	13.161	115.11
	13.407	110.40
	13.934	159.92
	14.138	73.60
	15.221	159.39
	16.387	58.04
	17.182	150.96
	17.421	130.21
	18.277	134.92
	19.712	80.68
	20.938	130.62
	21.275	115.58
	22.653	139.58
	22.904	43.89
	23.524	90.11
	24.403	55.21
	25.960	89.64
	26.986	49.08
	27.763	83.04
	28.221	25.96
	29.098	202.38
	29.333	198.13
	32.360	218.42
	33.376	124.08
	34.309	169.36
	34.608	152.85
	34.964	166.53
	35.098	137.28
	36.233	149.96
	36.901	109.92
	37.909	206.09
	38.333	172.66
	39.693	208.45
	41.012	145.77
	41.845	190.52
	42.603	180.68
	44.325	227.38
	45.005	211.81
	47.010	237.75
	47.319	163.70
	49.365	215.11
	49.642	90.11
	50.350	224.55
	50.710	214.64
	51.348	230.21
	51.531	217.94
	52.182	233.51
	52.376	202.85
	53.368	245.71
	53.488	220.24
	53.767	243.82
	53.985	228.32
	54.549	234.92
	54.845	178.79
	55.114	215.52
	55.167	195.30
	55.245	217.47
	55.277	98.60
	57.281	213.70
	58.643	80.21
	60.046	190.45
	60.982	166.06
	61.991	213.70
	62.858	202.85
	66.599	219.36
	67.333	195.77
	68.024	205.44
	68.228	129.97
	69.008	232.74
	69.458	188.93
	71.429	254.50
	72.330	211.57
	74.713	268.65
	76.631	255.91
	78.397	271.48
	79.466	258.27
	80.807	266.23
	81.356	212.52
	82.615	252.61
	82.941	229.97
	83.529	244.06
	83.836	205.44
	84.629	247.42
	85.243	234.69
	85.668	247.42
	86.529	222.89
	87.796	256.79
	89.860	153.55
	91.033	275.57
	91.148	240.82
	91.533	278.96
	92.244	261.57
	93.149	282.49
	93.843	243.27
	95.665	250.31
	95.895	196.42
	96.310	268.59
	97.407	246.89
	98.847	273.84
	99.409	235.16
	100.607	264.34
	101.743	199.78
	104.182	246.89
	105.675	210.16
	107.086	230.44
	107.817	195.91
	108.509	205.91
	108.979	174.31
	109.371	187.99
	110.112	159.69
	111.836	165.28
	112.212	123.84
	112.598	163.46
	116.099	134.22
	122.095	168.59
	123.343	96.01
	124.798	179.97
	125.732	167.97
	126.742	187.93
	127.412	175.55
	128.314	200.72
	129.196	179.50
	130.807	197.42
	131.611	162.89
	133.050	174.31
	133.370	137.67
	134.007	156.39
	134.193	132.64
	135.671	137.99
	136.036	118.65
	136.475	126.20
	136.797	101.67
	138.914	96.89
	139.484	-6.82
	140.150	103.90
	140.934	29.03
	141.739	132.80
	141.866	120.54
	142.736	146.89
	142.882	120.06
	144.243	139.37
	146.165	120.06
	148.558	145.08
	148.801	93.89
	149.114	155.77
	149.480	89.46
	149.789	172.75
	150.102	124.48
	150.469	185.96
	150.663	156.78
	150.950	179.67
	151.634	140.36
	152.519	156.40
	153.806	130.61
	154.597	144.45
	156.079	107.88
	157.125	134.92
	157.867	109.70
	159.081	125.58
	159.279	107.09
	159.752	119.83
	159.956	94.03
	161.674	96.72
	162.692	45.81
	163.715	66.06
	164.528	17.72
	165.441	48.85
	165.694	39.17
	165.894	56.09
	166.430	51.06
	167.135	90.99
	167.628	79.99
	168.458	106.09
	169.376	68.82
	171.065	85.96
	174.214	14.49
	175.843	36.28
	176.008	25.27
	178.626	55.04
	179.287	46.72
	180.646	70.77
	180.849	49.00
	181.608	59.05
	182.603	6.40
	183.878	29.36
	185.315	20.92
	186.466	35.02
	186.722	22.82
	187.150	40.05
	187.337	31.93
	187.765	42.47
	189.259	0.11
	191.706	11.03
	192.804	-16.87
	194.741	-10.89
	196.172	-46.99
	200.516	-38.00
	203.876	-71.48
	217.332	-47.00
	217.861	-100.27
	219.633	-48.00
	222.632	-98.64
	226.298	-62.00
	228.523	-150.65
	234.301	-80.00
	238.356	-122.15
	241.854	-83.00
	243.070	-115.55
	244.571	-83.00
	245.130	-95.18
	247.202	-82.00
	247.790	-92.63
	249.490	-82.00
	249.819	-118.90
	250.643	-102.00
	251.252	-130.00
	251.756	-115.00
	252.260	-100.00
	255.516	-125.00
	256.968	-110.00
	259.014	-95.00
	262.236	-130.00
	263.478	-110.00
	264.774	-80.00
	268.988	-120.00
	271.000	-65.00
	272.500	-30.00
	274.250	-40.00
	275.776	-20.00
	276.744	0.00
	278.240	-20.00
	279.208	0.00
	280.000	15.00
	281.496	-10.00
	282.024	0.00
	283.256	20.00
	286.236	-10.00
	286.950	-5.00
	289.500	15.00
	291.540	-30.00
	292.254	-15.00
	293.784	20.00
	294.498	5.00
	295.260	10.00
	296.272	20.00
	297.988	-10.00
	299.000	0.00
	300.225	20.00
	303.018	-10.00
	304.758	0.00
	307.020	20.00
	311.232	-30.00
	312.724	-15.00
	315.988	10.00
	322.250	-55.00
	324.989	-20.00
	332.448	55.00
	342.087	-10.00
	344.922	25.00
	349.470	65.00
	355.447	5.00
	356.698	20.00
	358.783	60.00
	361.954	30.00
	362.719	40.00
	363.943	65.00
	366.238	25.00
	367.309	40.00
	370.522	85.00
	376.768	25.00
	379.036	60.00
	382.492	115.00
	386.730	45.00
	388.745	80.00
	390.240	115.00
	392.028	70.00
	392.769	90.00
	394.023	110.00
	395.277	70.00
	395.733	80.00
	396.759	125.00
	397.785	80.00
	398.260	105.00
	399.020	125.00
	399.970	75.00
	401.015	100.00
	402.725	140.00
	405.005	115.00
	405.955	120.00
	407.000	130.00
	408.512	85.00
	408.764	100.00
	409.268	125.00
	410.486	80.00
	410.990	100.00
	412.016	125.00
	415.232	45.00
	416.513	80.00
	419.506	140.00
	425.243	90.00
	428.000	110.00
	432.466	150.00
	436.999	125.00
	439.000	145.00
	441.256	175.00
	445.505	130.00
	447.538	150.00
	451.006	190.00
	461.980	75.00
	463.996	85.00
	468.028	115.00
	473.228	60.00
	475.472	80.00
	476.968	110.00
	479.473	60.00
	481.025	80.00
	482.480	95.00
	487.039	75.00
	488.554	80.00
	492.999	90.00
	503.610	25.00
	504.780	30.00
	507.390	35.00
	512.640	-35.00
	515.280	-15.00
	517.480	5.00
	526.040	-55.00
	527.720	-45.00
	530.240	-30.00
	534.020	-60.00
	535.280	-55.00
	537.800	-45.00

Long-Term Phanerozoic (SEPM98-Haq'05)	point				off	CENOZOIC-JURASSIC = detailed in Hardenbol, J., et al. (SEPM charts. 1998); TRIASSIC-PALEOZOIC = Haq and Al-Qahtani (2005), whose Cenozoic-Jurassic is also similar to the version used in Hardenbol et al (SEPM chart).
nopoints	line		-150	285	smoothed
	0.00	60.00	Present
	1.65	74.03	MIS 58 (Cala 1)
	1.78	75.49
	2.26	77.85
	2.50	79.26	Ge 1
	2.62	80.21
	3.05	82.09
	3.27	83.04	Pia 1
	3.49	83.98
	3.84	86.81
	4.01	87.28	Za 2
	4.36	89.17
	4.54	90.11
	4.62	90.99	Za 1
	5.17	97.13
	5.57	100.02
	5.77	101.43	Me 2
	6.08	104.13
	6.86	108.04
	7.26	108.98	Tor 3/Me 1
	7.82	112.75
	8.75	118.89
	9.22	121.72	Tor 2
	10.23	126.84
	11.28	132.09
	11.80	135.87	Ser 4/Tor 1
	12.21	140.05
	12.55	145.30
	12.72	148.60	Ser 3
	13.16	152.38
	13.41	153.32
	13.53	156.62	Ser 2
	13.93	159.92
	14.14	159.92
	14.24	159.86	Lan 2/Ser 1
	15.22	159.39
	16.39	158.51
	16.97	159.92	Bur 5/Lan 1
	17.18	159.45
	17.42	157.57
	17.54	157.09	Bur 4
	18.28	154.74
	19.71	147.19
	20.43	146.65	Aq 3/Bur 1
	20.94	147.13
	21.27	143.42
	21.44	143.42	Aq 2
	22.65	139.58
	22.90	139.64
	23.03	142.00	Ch 4/Aq 1
	23.52	142.94
	24.40	144.83
	24.84	146.18	Ch 3
	25.96	153.79
	26.99	160.40
	27.50	166.93	Ch 2
	27.76	172.66
	28.22	182.57
	28.45	188.23	Ch 1/Ru 4
	29.10	211.34
	29.33	217.00
	29.45	219.36	Ru 3
	32.36	218.42
	33.38	215.58
	33.88	214.64	Pr 4/Ru 1
	34.31	213.70
	34.61	212.28
	34.76	211.81	Pr 3
	34.96	208.51
	35.10	206.62
	35.17	207.09	Pr 2
	36.23	206.09
	36.90	206.62
	37.24	206.09	Pr 1
	37.91	206.09
	38.33	204.74
	38.54	206.09	Bart 1
	39.69	208.45
	41.01	210.40
	41.67	215.52	Lu 4
	41.85	216.94
	42.60	218.89
	42.98	221.72	Lu 3
	44.32	227.38
	45.01	228.79
	45.35	231.62	Lu 2
	47.01	237.75
	47.32	237.28
	47.47	239.64	Lu 1
	49.36	242.94
	49.64	242.94
	49.78	243.89	Yp 10
	50.35	244.36
	50.71	244.83
	51.07	245.30	Yp 8
	51.35	245.77
	51.53	245.77
	51.62	245.77	Yp 7
	52.18	247.19
	52.38	247.19
	52.47	247.19	Yp 6
	53.37	245.71
	53.49	245.71
	53.55	245.71	Yp 5
	53.77	243.82
	53.98	242.94
	54.09	241.53	Yp 4
	54.55	234.92
	54.85	230.21
	54.99	226.84	Yp 3
	55.11	224.48
	55.17	225.02
	55.19	225.49	Yp 2
	55.25	224.55
	55.28	224.08
	55.29	223.13	Th 7/Yp 1
	57.28	213.70
	58.64	211.34
	59.32	212.28	Sel 2/Th 1
	60.05	210.73
	60.98	210.87
	61.45	214.11	Sel 1
	61.99	213.70
	62.86	214.64
	63.29	216.06	Da 3
	66.60	219.36
	67.33	220.30
	67.70	222.42	Ma 5
	68.02	224.31
	68.23	224.78
	68.33	227.08	Ma4
	69.01	232.74
	69.46	239.40
	69.68	241.29	Ma2
	71.43	254.50
	72.33	261.57
	72.78	263.46	Cam9
	74.71	268.65
	76.63	272.42
	77.59	271.95	Cam6
	78.40	271.48
	79.47	270.06
	80.00	266.23	Cam5
	80.81	266.23
	81.36	263.93
	81.63	264.81	Cam2
	82.62	252.61
	82.94	249.31
	83.10	248.84	Cam1
	83.53	244.06
	83.84	244.59
	83.99	245.06	Sa3
	84.63	247.42
	85.24	246.48
	85.55	247.42	Sa1
	85.67	247.42
	86.53	251.20
	86.96	255.38	Co1
	87.80	256.79
	89.86	269.12
	90.89	273.05	Tu3
	91.03	275.57
	91.15	276.20
	91.21	278.71	Tu2
	91.53	278.96
	92.24	279.97
	92.60	282.61	Tu1
	93.15	282.49
	93.84	276.20
	94.19	271.95	Ce5
	95.66	268.11
	95.89	267.64
	96.01	267.64	Ce3
	96.31	268.59
	97.41	267.64
	97.96	274.31	Ce2
	98.85	273.84
	99.41	272.89
	99.69	270.06	Al 11
	100.61	264.34
	101.74	253.08
	102.31	249.78	Al 9
	104.18	246.89
	105.67	242.71
	106.42	239.81	Al 7
	107.09	230.44
	107.82	216.76
	108.18	212.99	Al 5
	108.51	205.91
	108.98	196.01
	109.21	191.29	Al 4
	109.37	187.99
	110.11	174.78
	110.48	170.54	Al 3
	111.84	165.28
	112.21	164.88
	112.40	163.46	Ap6
	112.60	163.46
	116.10	162.99
	117.85	165.01	Ap5
	122.09	168.59
	123.34	175.25
	123.97	176.20	Ap3
	124.80	179.97
	125.73	182.33
	126.20	183.21	Barr6
	126.74	187.93
	127.41	196.01
	127.75	197.42	Barr5
	128.31	200.72
	129.20	202.61
	129.64	201.67	Barr1
	130.81	197.42
	131.61	194.12
	132.01	189.40	Ha6
	133.05	174.31
	133.37	169.12
	133.53	166.70	Ha4
	134.01	156.39
	134.19	154.03
	134.29	151.67	Ha3
	135.67	137.99
	136.04	134.69
	136.22	133.27	Ha1
	136.48	126.20
	136.80	118.65
	136.96	115.76	Va7
	138.91	96.89
	139.48	97.89
	139.77	99.78	Va2
	140.15	103.90
	140.93	118.18
	141.33	126.13	Be7
	141.74	132.80
	141.87	135.16
	141.93	137.52	Be5
	142.74	146.89
	142.88	146.95
	142.96	146.42	Be4
	146.16	136.67
	148.20	144.36	Ti 5
	148.56	145.08
	148.80	148.45
	148.92	150.11	Ti 4
	149.11	155.77
	149.48	158.49
	149.66	165.84	Ti 3
	149.79	172.75
	150.10	181.56
	150.26	185.87	?
	150.47	185.96
	150.66	183.98
	150.76	183.92	?
	150.95	179.67
	151.63	162.69
	151.98	158.92	Kim 5
	152.52	156.40
	153.81	152.63
	154.45	147.66	Kim 2
	154.60	144.45
	156.08	142.00
	156.82	136.81	Ox7
	157.12	134.92
	157.87	128.10
	158.24	127.47	Ox5
	159.08	125.58
	159.28	124.23
	159.38	122.19	Ox3
	159.75	119.83
	159.96	118.26
	160.06	117.00	Ox2
	161.67	96.72
	162.69	80.21
	163.20	75.96	Call3
	163.72	66.06
	164.53	52.00
	164.93	50.11	Bat5
	165.44	48.85
	165.69	51.91
	165.82	53.89	?
	165.89	56.09
	166.43	74.01
	166.70	76.53	Bat2
	167.14	90.99
	167.63	97.28
	167.87	102.94	Bj5
	168.46	106.09
	169.38	102.31
	169.84	99.17	Bj3
	171.07	85.96
	174.21	36.90
	175.79	34.86	?
	175.84	36.28
	176.01	38.16
	176.09	46.34	Toa7
	178.63	55.04
	179.29	57.57
	179.62	59.39	Toa5
	180.65	70.77
	180.85	69.83
	180.95	65.99	Toa4
	181.61	59.05
	182.60	27.47
	183.10	28.26	PI 8
	183.88	29.36
	185.31	33.02
	186.03	33.32	PI 6
	186.47	35.02
	186.72	37.44
	186.85	36.28	PI 5
	187.15	40.05
	187.34	40.68
	187.43	42.94	PI 3
	187.76	42.47
	189.26	28.73
	190.01	24.73	Si 5
	191.71	11.03
	192.80	2.31
	193.35	-2.87	Si 3
	194.74	-10.89
	196.17	-15.55
	196.89	-15.55	He3
	200.27	-37.50	Rh2
	200.52	-38.00
	203.88	-42.00
	205.56	-42.00	No2
	217.33	-47.00
	217.86	-47.50
	218.13	-47.50	Car4
	219.63	-48.00
	222.63	-51.00
	224.13	-56.00	Car2
	226.30	-62.00
	228.52	-69.50
	229.64	-71.00	Lad3
	234.30	-80.00
	238.36	-83.00
	240.38	-83.00	An4
	241.85	-83.00
	243.07	-83.00
	243.68	-83.00	An1
	244.57	-83.00
	245.13	-82.50
	245.41	-82.50	Ol 4
	247.20	-82.00
	247.79	-82.00
	248.08	-82.00	Ol 1
	249.49	-82.00
	249.82	-82.00
	249.98	-82.00	In2
	250.64	-82.00	MFS set as first msf in basal Tri
	251.25	-81.00
	252.25	-80.00
	255.50	-79.00
	259.00	-76.00
	262.25	-70.00
	264.75	-60.00
	269.00	-42.00
	272.50	-25.00
	274.25	-3.00
	276.75	14.00
	278.25	20.00
	280.00	28.00
	281.50	31.00
	283.25	33.00
	286.25	29.00
	289.50	28.00
	291.50	29.00
	293.75	31.00
	294.50	34.00
	296.25	37.00
	298.00	38.00
	300.25	35.00
	303.00	30.00
	307.00	24.00
	311.25	28.00
	316.00	37.00
	322.25	48.00
	332.50	60.00
	342.00	67.00
	349.50	68.00
	355.50	70.00
	358.75	75.00
	362.00	80.00
	364.00	86.00
	366.25	92.00
	370.50	104.00
	376.75	119.00
	382.50	118.00
	386.75	119.00
	390.25	120.00
	392.00	120.00
	394.00	122.00
	395.25	129.00
	396.75	132.00
	397.75	138.00
	399.00	140.00
	400.00	141.00
	402.75	140.00
	405.00	139.00
	407.00	138.00
	408.50	135.00
	409.25	134.00
	410.50	134.00
	412.00	135.00
	415.25	138.00
	419.50	140.00
	425.25	143.00
	432.50	160.00
	437.00	180.00
	441.25	195.00
	445.50	205.00
	451.00	200.00
	462.00	151.00
	468.00	148.00
	473.25	132.00
	477.00	130.00
	479.50	129.00
	482.50	124.00
	487.00	116.00
	493.00	100.00
	504.50	63.00
	509.50	50.00
	516.50	30.00
	523.00	10.00
	531.00	-8.00
	534.00	-18.00
	536.50	-22.00
	539.00	-32.00
	542.00	-43.00
	548.00	-75.00


Long-Term Meso-Ceno (Tapscott SEPM98)	point				off	CENOZOIC-JURASSIC of Tapscott in SEPM charts (1998) is consistent with Hardenbol (SEPM98) Long-Term scaling; but TRIASSIC is significantly elevated relative to Haq and Al-Qahtani (2005).
nopoints	line		-150	285	smoothed 
	0.00	0.00	Present Highstand
	1.65	-0.32	MIS 58 (Cala 1)
	1.78	0.83
	2.26	6.04
	2.50	10.00	Ge 1
	2.62	11.42
	3.05	15.27
	3.27	18.35	Pia 1
	3.49	20.72
	3.84	23.87
	4.01	25.45	Za 2
	4.36	26.64
	4.54	27.13
	4.62	27.38	Za 1
	5.17	27.85
	5.57	25.96
	5.77	25.02	Me 2
	6.08	23.48
	6.86	19.36
	7.26	16.65	Tor 3/Me 1
	7.82	8.15
	8.75	-5.64
	9.22	-10.74	Tor 2
	10.23	-12.72
	11.28	2.85
	11.80	13.59	Ser 4/Tor 1
	12.21	40.78
	12.55	64.42
	12.72	77.57	Ser 3
	13.16	100.80
	13.41	105.75
	13.53	114.06	Ser 2
	13.93	125.96
	14.14	126.91
	14.24	127.01	Lan 2/Ser 1
	15.22	127.21
	16.39	126.91
	16.97	126.43	Bur 5/Lan 1
	17.18	124.74
	17.42	124.08
	17.54	120.09	Bur 4
	18.28	113.46
	19.71	103.87
	20.43	104.46	Aq 3/Bur 1
	20.94	106.64
	21.27	109.21
	21.44	110.30	Aq 2
	22.65	92.20
	22.90	81.52
	23.03	76.91	Ch 4/Aq 1
	23.52	72.72
	24.40	65.11
	24.84	61.55	Ch 3
	25.96	57.57
	26.99	61.34
	27.50	64.32	Ch 2
	27.76	71.25
	28.22	84.92
	28.45	94.38	Ch 1/Ru 4
	29.10	158.85
	29.33	173.13
	29.45	178.93	Ru 3
	32.36	173.60
	33.38	161.34
	33.88	157.17	Pr 4/Ru 1
	34.31	150.55
	34.61	144.41
	34.76	142.93	Pr 3
	34.96	134.92
	35.10	131.76
	35.17	131.16	Pr 2
	36.23	131.36
	36.90	132.65
	37.24	133.93	Pr 1
	37.91	141.06
	38.33	148.60
	38.54	148.60	Bart 1
	39.69	161.34
	41.01	180.68
	41.67	186.05	Lu 4
	41.85	187.28
	42.60	192.08
	42.98	194.55	Lu 3
	44.32	195.14
	45.01	193.36
	45.35	192.47	Lu 2
	47.01	186.54
	47.32	186.05
	47.47	185.75	Lu 1
	49.36	186.93
	49.64	187.21
	49.78	188.02	Yp 10
	50.35	189.17
	50.71	188.91
	51.07	189.41	Yp 8
	51.35	190.40
	51.53	190.89
	51.62	191.06	Yp 7
	52.18	193.96
	52.38	194.94
	52.47	195.77	Yp 6
	53.37	197.71
	53.49	197.61
	53.55	197.52	Yp 5
	53.77	197.19
	53.98	195.44
	54.09	194.85	Yp 4
	54.55	188.62
	54.85	182.19
	54.99	177.83	Yp 3
	55.11	175.96
	55.17	174.67
	55.19	173.60	Yp 2
	55.25	171.51
	55.28	169.83
	55.29	169.36	Th 7/Yp 1
	57.28	147.58
	58.64	141.35
	59.32	141.53	Sel 2/Th 1
	60.05	142.83
	60.98	147.28
	61.45	151.04	Sel 1
	61.99	163.89
	62.86	198.70
	63.29	202.46	Da 3
	66.60	183.28
	67.33	180.51
	67.70	178.13	Ma 5
	68.23	176.67
	68.67	177.14
	68.89	177.14	Ma4
	69.47	187.52
	69.85	197.42
	70.04	202.14	Ma2
	71.79	216.29
	72.69	219.59
	73.14	220.06	Cam9
	74.76	223.37
	76.38	226.20
	77.18	228.08	Cam6
	78.05	229.50
	79.19	230.91
	79.76	230.91	Cam5
	80.65	231.38
	81.26	230.91
	81.56	230.44	Cam2
	82.54	221.48
	82.86	216.29
	83.02	214.88	Cam1
	83.51	212.05
	83.87	209.22
	84.05	207.80	Sa3
	84.64	207.33
	85.21	209.22
	85.50	211.57	Sa1
	85.65	212.99
	86.74	216.29
	87.28	217.23	Co1
	88.02	217.71
	89.83	222.89
	90.74	223.37	Tu3
	90.87	224.31
	90.97	224.78
	91.02	225.25	Tu2
	91.33	225.72
	92.00	226.67
	92.33	226.67	Tu1
	92.97	229.03
	93.77	230.91
	94.17	231.86	Ce5
	95.52	233.27
	95.73	233.27
	95.84	233.74	Ce3
	96.10	234.22
	97.05	233.74
	97.52	233.27	Ce2
	98.31	230.91
	98.80	229.97
	99.05	228.55	Al 11
	99.57	224.78
	100.21	218.65
	100.53	215.82	Al 9
	101.25	212.52
	101.83	209.69
	102.12	208.27	Al 7
	103.32	197.89
	104.64	182.80
	105.30	179.50	Al 5
	105.85	174.31
	106.64	165.82
	107.03	162.99	Al 4
	107.34	161.10
	108.76	151.20
	109.48	149.78	Al 3
	111.67	143.65
	112.28	141.29
	112.58	140.82	Ap6
	112.70	140.35
	114.86	139.40
	115.94	142.23	Ap5
	118.76	149.31
	119.59	152.14
	120.00	152.61	Ap3
	120.69	154.50
	121.46	156.38
	121.84	157.33	Barr6
	122.60	160.63
	123.54	164.40
	124.01	165.82	Barr5
	124.69	167.23
	125.75	167.23
	126.28	166.76	Barr1
	127.05	163.93
	127.58	162.05
	127.84	160.16	Ha6
	129.00	150.72
	129.35	147.42
	129.53	145.06	Ha4
	130.06	137.99
	130.26	135.63
	130.36	133.74	Ha3
	131.36	122.89
	131.63	119.59
	131.76	118.65	Ha1
	132.05	112.99
	132.42	99.31
	132.61	95.06	Va7
	134.97	63.46
	135.65	69.12
	136.00	77.61	Va2
	136.50	87.99
	137.54	103.55
	138.07	109.22	Be7
	138.92	113.93
	139.19	114.88
	139.32	115.82	Be5
	140.67	123.37
	140.91	123.37
	141.03	123.37	Be4
	148.20	119.20	Ti 5
	148.56	119.50
	148.80	119.52
	148.92	119.52	Ti 4
	149.11	120.15
	149.48	120.77
	149.66	121.72	Ti 3
	149.79	123.92
	150.10	129.58
	150.26	134.93	?
	150.47	140.59
	150.66	146.88
	150.76	148.13	?
	150.95	152.22
	151.63	150.65
	151.98	144.36	Kim 5
	152.52	139.33
	153.81	133.67
	154.45	123.60	Kim 2
	154.60	122.03
	156.08	116.69
	156.82	113.54	Ox7
	157.12	112.60
	157.87	111.03
	158.24	111.03	Ox5
	159.08	110.08
	159.28	110.06
	159.38	109.77	Ox3
	159.75	108.51
	159.96	107.25
	160.06	106.94	Ox2
	161.67	89.96
	162.69	72.35
	163.20	67.32	Call3
	163.72	55.99
	164.53	40.59
	164.93	39.01	Bat5
	165.44	42.16
	165.69	45.62
	165.82	48.45	?
	165.89	50.33
	166.43	67.32
	166.70	70.77	Bat2
	167.14	86.81
	167.63	89.96
	167.87	89.33	Bj5
	168.46	87.13
	169.38	83.35
	169.84	81.47	Bj3
	171.07	78.01
	174.21	23.29
	175.79	26.43	?
	175.84	34.93
	176.01	44.36
	176.09	54.11	Toa7
	178.63	59.77
	179.29	60.40
	179.62	61.03	Toa5
	180.65	58.20
	180.85	55.99
	180.95	54.74	Toa4
	181.61	45.93
	182.60	30.21
	183.10	28.64	PI 8
	183.88	28.32
	185.31	29.27
	186.03	30.84	PI 6
	186.47	31.78
	186.72	32.41
	186.85	32.72	PI 5
	187.15	36.50
	187.34	37.76
	187.43	38.38	PI 3
	187.76	38.07
	189.26	25.49
	190.01	22.66	Si 5
	191.71	11.65
	192.80	5.68
	193.35	-1.24	Si 3
	194.74	-11.30
	196.17	-20.73
	196.89	-24.19	He3
	200.27	-14.86	Rh2
	200.52	-14.32
	203.88	14.32
	205.56	25.14	No2
	213.41	65.68
	217.33	59.46
	217.86	57.30
	218.13	56.76	Car4
	219.63	55.14
	222.63	50.81
	224.13	45.95	Car2
	226.30	34.86
	228.52	26.22
	229.64	22.97	Lad3
	234.30	19.46
	238.36	19.73
	240.38	17.57	An4
	241.85	15.95
	243.07	14.05
	243.68	12.97	An1
	244.57	12.97
	245.13	12.43
	245.41	12.43	Ol 4
	247.20	12.97
	247.79	12.97
	248.08	12.97	Ol 1
	249.49	11.89
	249.82	3.51
	249.98	-4.59	In2
	250.64	-32.97




Marine Oxygen-18 Composite (per-mil PDB)	point				off	High-resolution for past 6 myr = Crowhurst (2002); Low-resolution for 6 Ma to 67 Ma = Zachos et al. (2001)
nopoints	line		-0.3	5.5
	0.000	3.43
	0.003	3.37	1
	0.006	3.54
	0.009	3.87
	0.012	4.36
	0.015	4.90
	0.018	5.01	2
	0.021	4.96
	0.024	4.87
	0.027	4.67
	0.030	4.58
	0.033	4.61
	0.036	4.57
	0.039	4.49
	0.042	4.58
	0.045	4.57
	0.048	4.57
	0.051	4.48
	0.054	4.45
	0.057	4.42
	0.060	4.47
	0.063	4.61
	0.066	4.60
	0.069	4.50
	0.072	4.34
	0.075	4.26
	0.078	4.11
	0.081	4.02
	0.084	4.13
	0.087	4.32
	0.090	4.32
	0.093	4.21
	0.096	4.10
	0.099	4.09
	0.102	4.05
	0.105	4.19
	0.108	4.29
	0.111	4.04
	0.114	3.73
	0.117	3.42
	0.120	3.29	5
	0.123	3.35
	0.126	3.78
	0.129	4.35
	0.132	4.48
	0.135	4.76
	0.138	4.88
	0.141	4.91
	0.144	4.86
	0.147	4.81
	0.150	4.91	6
	0.153	4.83
	0.156	4.68
	0.159	4.71
	0.162	4.64
	0.165	4.47
	0.168	4.43
	0.171	4.54
	0.174	4.61
	0.177	4.54
	0.180	4.62
	0.183	4.65
	0.186	4.61
	0.189	4.38
	0.192	4.11
	0.195	3.96
	0.198	3.86
	0.201	4.07
	0.204	3.95
	0.207	3.84
	0.210	3.79
	0.213	3.75	7
	0.216	3.82
	0.219	3.99
	0.222	4.19
	0.225	4.58
	0.228	4.57
	0.231	4.43
	0.234	4.04
	0.237	3.75
	0.240	3.93
	0.243	4.42
	0.246	4.74
	0.249	4.80	8
	0.252	4.72
	0.255	4.71
	0.258	4.68
	0.261	4.71
	0.264	4.71
	0.267	4.73
	0.270	4.69
	0.273	4.53
	0.276	4.54
	0.279	4.33
	0.282	4.08
	0.285	3.99
	0.288	4.00
	0.291	4.18
	0.294	4.35
	0.297	4.37
	0.300	4.28
	0.303	4.30
	0.306	4.23
	0.309	4.27
	0.312	4.17
	0.315	3.88
	0.318	3.98
	0.321	3.73
	0.324	3.61
	0.327	3.43	9
	0.330	3.59
	0.333	3.71
	0.336	4.25
	0.339	4.72
	0.342	5.17	10
	0.345	5.14
	0.348	5.04
	0.351	4.76
	0.354	4.80
	0.357	4.87
	0.360	4.81
	0.363	4.77
	0.366	4.64
	0.369	4.58
	0.372	4.62
	0.375	4.45
	0.378	4.51
	0.381	4.44
	0.384	4.13
	0.387	4.29
	0.390	4.21
	0.393	3.89
	0.396	3.84
	0.399	3.63
	0.402	3.51	11
	0.405	3.59
	0.408	4.07
	0.411	4.54
	0.414	4.88
	0.417	4.80
	0.420	4.72
	0.423	4.64
	0.426	4.56
	0.429	4.59
	0.432	4.62
	0.435	4.66
	0.438	4.68	12
	0.441	4.64
	0.444	4.64
	0.447	4.42
	0.450	4.56
	0.453	4.61
	0.456	4.50
	0.459	4.49
	0.462	4.44
	0.465	4.40
	0.468	4.29
	0.471	4.10
	0.474	3.95
	0.477	3.84	13
	0.480	3.85
	0.483	3.87
	0.486	4.09
	0.489	4.23
	0.492	4.25
	0.495	4.15
	0.498	3.98
	0.501	4.06
	0.504	4.33
	0.507	4.64
	0.510	4.42
	0.513	4.41
	0.516	4.31
	0.519	4.31
	0.522	4.32
	0.525	4.45
	0.528	4.50
	0.531	4.62	14
	0.534	4.60
	0.537	4.58
	0.540	4.55
	0.543	4.53
	0.546	4.27
	0.549	4.23
	0.552	4.01
	0.555	3.94
	0.558	3.77
	0.561	3.73
	0.564	3.69
	0.567	3.58	15
	0.570	3.62
	0.573	3.67
	0.576	3.91
	0.579	4.05
	0.582	4.09
	0.585	4.17
	0.588	4.15
	0.591	4.14
	0.594	4.12
	0.597	4.10
	0.600	4.19
	0.603	4.04
	0.606	4.14
	0.609	3.92
	0.612	3.74
	0.615	3.78
	0.618	3.88
	0.621	4.38
	0.624	4.64
	0.627	5.00
	0.630	5.09
	0.633	4.82
	0.636	4.92
	0.639	5.02
	0.642	4.96
	0.645	4.84
	0.648	4.88
	0.651	4.90	16
	0.654	4.81
	0.657	4.78
	0.660	4.77
	0.663	4.70
	0.666	4.70
	0.669	4.81
	0.672	4.51
	0.675	4.55
	0.678	4.50
	0.681	4.44
	0.684	4.21
	0.687	4.00
	0.690	3.81	17
	0.693	3.94
	0.696	4.01
	0.699	4.15
	0.702	4.28
	0.705	4.28
	0.708	4.27
	0.711	4.38
	0.714	4.61
	0.717	4.77
	0.720	4.90	18
	0.723	4.79
	0.726	4.46
	0.729	4.33
	0.732	4.28
	0.735	4.38
	0.738	4.38
	0.741	4.37
	0.744	4.37
	0.747	4.57
	0.750	4.73
	0.753	4.72
	0.756	4.66
	0.759	4.64
	0.762	4.48
	0.765	4.40
	0.768	4.52
	0.771	4.42
	0.774	4.07
	0.777	3.86
	0.780	3.72
	0.783	3.73	19
	0.786	3.89
	0.789	4.29
	0.792	4.60
	0.795	4.69	20
	0.798	4.68
	0.801	4.67
	0.804	4.57
	0.807	4.21
	0.810	4.06
	0.813	3.97
	0.816	4.09
	0.819	4.08
	0.822	4.15
	0.825	4.07
	0.828	4.06
	0.831	4.11
	0.834	4.04
	0.837	3.90
	0.840	3.86
	0.843	3.81
	0.846	3.78
	0.849	3.93
	0.852	3.83
	0.855	3.66	21
	0.858	3.77
	0.861	3.82
	0.864	3.99
	0.867	4.41
	0.870	4.66
	0.873	5.01
	0.876	5.01	22
	0.879	4.96
	0.882	4.81
	0.885	4.75
	0.888	4.75
	0.891	4.74
	0.894	4.69
	0.897	4.49
	0.900	4.35
	0.903	4.17	23
	0.906	4.17
	0.909	4.28
	0.912	4.46
	0.915	4.58	24
	0.918	4.51
	0.921	4.39
	0.924	4.26
	0.927	4.24
	0.930	4.19
	0.933	4.18
	0.936	4.02
	0.939	3.83
	0.942	3.74
	0.945	3.63
	0.948	3.43	25
	0.951	3.47
	0.954	3.58
	0.957	3.71
	0.960	4.22
	0.963	4.52	26
	0.966	4.44
	0.969	4.24
	0.972	4.20
	0.975	4.09
	0.978	4.12
	0.981	4.17
	0.984	4.06
	0.987	4.18
	0.990	4.14
	0.993	4.05
	0.996	3.88	27
	0.999	4.24
	1.002	4.25
	1.005	4.13
	1.008	4.28	28
	1.011	4.17
	1.014	4.01
	1.017	3.94
	1.020	4.00
	1.023	3.86	29
	1.026	3.90
	1.029	3.99
	1.032	4.09
	1.035	4.37
	1.038	4.55
	1.041	4.52
	1.044	4.42
	1.047	4.27
	1.050	4.29
	1.053	4.36	30
	1.056	4.37
	1.059	4.29
	1.062	3.74
	1.065	3.53
	1.068	3.45
	1.071	3.44	31
	1.074	3.55
	1.077	3.73
	1.080	3.92
	1.083	4.05
	1.086	4.11
	1.089	4.19
	1.092	4.17
	1.095	4.24
	1.098	4.37	32
	1.101	4.24
	1.104	4.05
	1.107	3.88
	1.110	3.80	33
	1.113	3.85
	1.116	4.22
	1.119	4.41
	1.122	4.40
	1.125	4.51
	1.128	4.63	34
	1.131	4.63
	1.134	4.61
	1.137	4.39
	1.140	4.27
	1.143	4.12
	1.146	4.09
	1.149	3.99
	1.152	3.96
	1.155	3.94
	1.158	3.79
	1.161	3.77
	1.164	3.73	35
	1.167	3.81
	1.170	3.86
	1.173	3.87
	1.176	3.75
	1.179	3.60
	1.182	3.74
	1.185	3.99
	1.188	4.00
	1.191	4.26
	1.194	4.40
	1.197	4.50	36
	1.200	4.42
	1.203	4.45
	1.206	4.46
	1.209	4.35
	1.212	4.27
	1.215	4.23
	1.218	4.16
	1.221	3.97
	1.224	3.74
	1.227	3.57
	1.230	3.57
	1.233	3.51	37
	1.236	3.44
	1.239	3.38
	1.242	3.30
	1.245	3.86
	1.248	4.22
	1.251	4.33	38
	1.254	4.00
	1.257	4.23
	1.260	4.25
	1.263	4.07
	1.266	3.96
	1.269	3.94
	1.272	3.83
	1.275	3.71
	1.278	3.62	39
	1.281	3.87
	1.284	4.00
	1.287	4.35
	1.290	4.33
	1.293	4.28
	1.296	4.34	40
	1.299	4.27
	1.302	4.27
	1.305	4.25
	1.308	4.04
	1.311	3.90
	1.314	3.78	41
	1.317	3.97
	1.320	4.10
	1.323	4.21
	1.326	4.26
	1.329	4.30
	1.332	4.34	42
	1.335	4.28
	1.338	4.16
	1.341	3.84
	1.344	3.56	43
	1.347	3.57
	1.350	3.60
	1.353	3.59
	1.356	4.03
	1.359	4.12
	1.362	4.29
	1.365	4.36	44
	1.368	4.34
	1.371	4.28
	1.374	4.20
	1.377	4.11
	1.380	4.12
	1.383	3.86
	1.386	3.79
	1.389	3.77
	1.392	3.72
	1.395	3.56
	1.398	3.53	45
	1.401	3.66
	1.404	3.79
	1.407	3.78
	1.410	3.78
	1.413	4.15
	1.416	4.33	46
	1.419	4.17
	1.422	4.20
	1.425	4.10
	1.428	4.00
	1.431	3.90
	1.434	3.65
	1.437	3.43
	1.440	3.31	47
	1.443	3.38
	1.446	3.41
	1.449	3.46
	1.452	3.47
	1.455	3.81
	1.458	4.26	48
	1.461	4.18
	1.464	4.27
	1.467	4.06
	1.470	3.60
	1.473	3.47
	1.476	3.52
	1.479	3.52
	1.482	3.54
	1.485	3.54
	1.488	3.39	49
	1.491	3.47
	1.494	3.67
	1.497	3.96
	1.500	4.21
	1.503	4.21	50
	1.506	4.20
	1.509	4.32
	1.512	4.22
	1.515	3.95
	1.518	3.73
	1.521	3.83
	1.524	3.74
	1.527	3.77	51
	1.530	3.85
	1.533	4.00
	1.536	4.25
	1.539	4.41
	1.542	4.53	52
	1.545	4.27
	1.548	4.00
	1.551	3.83
	1.554	3.80
	1.557	3.90
	1.560	3.90
	1.563	3.61
	1.566	3.51	53
	1.569	3.98
	1.572	4.34
	1.575	4.40	54
	1.578	4.17
	1.581	4.23
	1.584	4.03
	1.587	3.93
	1.590	3.79
	1.593	3.79
	1.596	3.84
	1.599	3.83
	1.602	3.71
	1.605	3.57
	1.608	3.46	55
	1.611	3.55
	1.614	3.69
	1.617	3.78
	1.620	3.88	56
	1.623	3.83
	1.626	3.72
	1.629	3.76
	1.632	3.93
	1.635	3.65
	1.638	3.61	57
	1.641	3.64
	1.644	3.79
	1.647	4.12
	1.650	4.24
	1.653	4.31	58
	1.656	4.28
	1.659	4.22
	1.662	4.25
	1.665	4.19
	1.668	4.07
	1.671	3.94
	1.674	3.79
	1.677	3.75	59
	1.680	3.81
	1.683	3.78
	1.686	3.98
	1.689	3.99
	1.692	4.00
	1.695	4.08
	1.698	4.39
	1.701	4.47	60
	1.704	4.31
	1.707	4.15
	1.710	3.96
	1.713	3.90
	1.716	4.00
	1.719	4.13
	1.722	4.12
	1.725	4.04
	1.728	4.06
	1.731	4.06
	1.734	3.90	61
	1.737	3.98
	1.740	4.00
	1.743	4.16
	1.746	4.33
	1.749	4.46	62
	1.752	4.46
	1.755	4.09
	1.758	3.73
	1.761	3.73
	1.764	3.45
	1.767	3.43	63
	1.770	3.60
	1.773	3.82
	1.776	3.96
	1.779	4.10
	1.782	4.18
	1.785	4.23
	1.788	4.31	64
	1.791	4.24
	1.794	4.22
	1.797	4.08
	1.800	3.94
	1.803	3.71
	1.806	3.86
	1.809	3.75
	1.812	3.80
	1.815	3.92
	1.818	4.08
	1.821	3.89
	1.824	3.68	65
	1.827	3.80
	1.830	3.91
	1.833	3.99
	1.836	4.10	66
	1.839	4.01
	1.842	4.03
	1.845	3.93
	1.848	3.82
	1.851	3.84
	1.854	3.70	67
	1.857	3.81
	1.860	4.02
	1.863	4.13
	1.866	3.89
	1.869	3.77
	1.872	3.95
	1.875	4.44	68
	1.878	4.39
	1.881	4.26
	1.884	3.99
	1.887	3.75
	1.890	3.64
	1.893	3.56	69
	1.896	3.61
	1.899	3.61
	1.902	3.63
	1.905	3.78
	1.908	4.00
	1.911	4.09
	1.914	4.19
	1.916	4.23	70
	1.919	4.01
	1.922	3.86
	1.925	3.89
	1.928	3.83
	1.931	3.52
	1.934	3.51	71
	1.937	3.61
	1.940	3.59
	1.943	3.59
	1.946	3.53
	1.949	3.46
	1.952	3.67
	1.955	3.92	72
	1.958	3.91
	1.961	3.80
	1.964	3.75
	1.967	3.72
	1.970	3.58
	1.973	3.45
	1.976	3.42
	1.979	3.32	73
	1.982	3.33
	1.985	3.73
	1.988	3.91
	1.991	3.75
	1.994	3.76
	1.997	3.78
	2.000	3.74
	2.003	3.75
	2.006	3.80	74
	2.009	3.77
	2.012	3.69
	2.015	3.60
	2.018	3.43
	2.021	3.34	75
	2.024	3.43
	2.027	3.39
	2.030	3.57
	2.033	3.51
	2.036	3.54
	2.039	3.58
	2.042	3.69	76
	2.045	3.73
	2.048	3.58
	2.051	3.44
	2.054	3.31	77
	2.057	3.43
	2.060	3.52
	2.063	3.62
	2.066	3.69
	2.069	3.61
	2.072	3.76
	2.075	3.90
	2.078	3.84
	2.081	3.86
	2.084	4.14	78
	2.087	4.07
	2.090	3.93
	2.093	4.04
	2.096	3.78
	2.099	3.61
	2.102	3.31	79
	2.105	3.57
	2.108	3.77
	2.111	3.67
	2.114	3.62
	2.117	3.67
	2.120	3.60
	2.123	3.80	80
	2.126	3.77
	2.129	3.71
	2.132	3.67
	2.135	3.54
	2.138	3.35	81
	2.141	3.36
	2.144	3.46
	2.147	3.72
	2.150	3.94
	2.153	3.99
	2.156	3.99
	2.159	4.17
	2.162	4.21	82
	2.165	4.16
	2.168	4.15
	2.171	4.03
	2.174	3.95
	2.177	3.87
	2.180	3.78
	2.183	3.71
	2.186	3.62
	2.189	3.51
	2.192	3.45	83
	2.195	3.50
	2.198	3.65
	2.201	3.72
	2.204	3.75	84
	2.207	3.60
	2.210	3.42
	2.213	3.39
	2.216	3.39	85
	2.219	3.41
	2.222	3.47
	2.225	3.48
	2.228	3.49
	2.231	3.51
	2.234	3.45
	2.237	3.44
	2.240	3.80
	2.243	4.04	86
	2.246	3.98
	2.249	3.86
	2.252	3.64
	2.255	3.52
	2.258	3.50
	2.261	3.32
	2.264	3.22	87
	2.267	3.25
	2.270	3.38
	2.273	3.60
	2.276	3.82
	2.279	3.90
	2.282	4.03	88
	2.285	3.89
	2.288	3.80
	2.291	3.68
	2.294	3.53
	2.297	3.41
	2.300	3.26	89
	2.303	3.38
	2.306	3.37
	2.309	3.44
	2.312	3.65
	2.315	3.71
	2.318	3.72	90
	2.321	3.57
	2.324	3.41
	2.327	3.41
	2.330	3.41
	2.333	3.42
	2.336	3.38
	2.339	3.50
	2.342	3.52
	2.345	3.28
	2.348	3.11	91
	2.351	3.14
	2.354	3.33
	2.357	3.53
	2.360	3.74
	2.363	3.90	92
	2.366	3.86
	2.369	3.76
	2.372	3.69
	2.375	3.62
	2.378	3.57
	2.381	3.48
	2.384	3.34
	2.387	3.22
	2.390	3.09	93
	2.393	3.10
	2.396	3.20
	2.399	3.40
	2.402	3.59
	2.405	3.66
	2.408	3.66
	2.411	3.74	94
	2.414	3.72
	2.417	3.65
	2.420	3.50
	2.423	3.33
	2.426	3.47
	2.429	3.49
	2.432	3.47
	2.435	3.42	95
	2.438	3.45
	2.441	3.73
	2.444	3.92
	2.447	3.96
	2.450	3.89
	2.453	4.02	96
	2.456	3.88
	2.459	3.85
	2.462	3.85
	2.465	3.71
	2.468	3.43
	2.471	3.32
	2.474	3.29	97
	2.477	3.53
	2.480	3.76
	2.483	4.02
	2.486	4.14	98
	2.489	4.10
	2.492	3.98
	2.495	3.89
	2.498	3.89
	2.501	3.61
	2.504	3.49
	2.507	3.42	99
	2.510	3.53
	2.513	3.67
	2.516	3.84
	2.519	3.99
	2.522	4.10	100
	2.525	4.10
	2.528	4.06
	2.531	3.94
	2.534	3.85
	2.537	3.60
	2.540	3.41
	2.543	3.20	101
	2.546	3.30
	2.549	3.57
	2.552	3.60	102
	2.555	3.55
	2.558	3.45
	2.561	3.45
	2.564	3.45
	2.567	3.45
	2.570	3.39
	2.573	3.35
	2.576	3.28
	2.579	3.20	103
	2.582	3.25
	2.585	3.23
	2.588	3.24
	2.591	3.30
	2.594	3.34
	2.597	3.58
	2.600	3.75
	2.603	3.83
	2.606	3.99	104
	2.609	3.90
	2.612	3.87
	2.615	3.85
	2.618	3.73
	2.621	3.63
	2.624	3.47
	2.627	3.38
	2.630	3.40
	2.633	3.39
	2.636	3.31	105 / G1
	2.639	3.35
	2.642	3.51
	2.645	3.70
	2.648	3.76	106 / G2
	2.651	3.72
	2.654	3.77
	2.657	3.69
	2.660	3.54
	2.663	3.42
	2.666	3.17
	2.669	3.13	107 / G3
	2.672	3.20
	2.675	3.22
	2.678	3.27
	2.681	3.34
	2.684	3.49
	2.687	3.57
	2.690	3.83
	2.693	3.85	108 / G4
	2.696	3.76
	2.699	3.60
	2.702	3.49
	2.705	3.53	109 / G5
	2.708	3.60
	2.711	3.75
	2.714	3.76
	2.717	3.83
	2.720	3.83	110 / G6
	2.723	3.66
	2.726	3.55
	2.729	3.65
	2.732	3.52
	2.735	3.59
	2.738	3.64
	2.741	3.59
	2.744	3.68
	2.747	3.44
	2.750	2.99
	2.753	2.98
	2.756	3.03	 111 / G7
	2.759	3.11
	2.762	3.23
	2.765	3.24
	2.768	3.32
	2.771	3.37
	2.774	3.44
	2.777	3.49	G8
	2.780	3.33
	2.783	3.27
	2.786	3.18
	2.789	3.16	G9
	2.792	3.23
	2.795	3.34
	2.798	3.23
	2.801	3.31
	2.804	3.34
	2.807	3.39
	2.810	3.57
	2.813	3.55
	2.816	3.85	G10
	2.819	3.79
	2.822	3.70
	2.825	3.46
	2.828	3.42
	2.831	3.33
	2.834	3.29
	2.837	3.30	G11
	2.840	3.35
	2.843	3.43
	2.846	3.53
	2.849	3.51
	2.852	3.51
	2.855	3.56	G12
	2.858	3.54
	2.861	3.45
	2.864	3.33
	2.867	3.28
	2.870	3.26
	2.873	3.23	G13
	2.876	3.26
	2.879	3.26
	2.882	3.38
	2.885	3.58
	2.888	3.66	G14
	2.891	3.62
	2.894	3.49
	2.897	3.41
	2.900	3.34
	2.903	3.30
	2.906	3.27
	2.909	3.23	G15
	2.912	3.38
	2.915	3.37
	2.918	3.33
	2.921	3.29
	2.924	3.28
	2.927	3.44
	2.930	3.50
	2.933	3.57
	2.936	3.61	G16
	2.939	3.42
	2.942	3.23
	2.945	3.17
	2.948	2.96	G17
	2.951	3.02
	2.954	3.07
	2.957	3.21
	2.960	3.26
	2.963	3.18
	2.966	3.17
	2.969	3.35	G18
	2.972	3.28
	2.975	3.41
	2.978	3.42
	2.981	3.27
	2.984	3.13
	2.987	2.90
	2.990	2.98
	2.993	2.90	G19
	2.996	2.99
	2.999	3.08
	3.002	3.22
	3.005	3.34
	3.008	3.40
	3.011	3.43
	3.014	3.56	G20
	3.017	3.50
	3.020	3.42
	3.023	3.35
	3.026	3.39
	3.029	3.37
	3.032	3.26
	3.035	3.09
	3.038	2.96	G21
	3.041	3.01
	3.044	3.02
	3.047	3.12
	3.050	3.18
	3.053	3.30
	3.056	3.30
	3.059	3.37	G22
	3.062	3.08
	3.065	3.07
	3.068	3.00
	3.071	2.99
	3.074	2.94	K1
	3.077	2.99
	3.080	3.02
	3.083	3.13
	3.086	3.21
	3.089	3.22
	3.092	3.28
	3.095	3.21
	3.098	3.30	K2
	3.101	3.12
	3.104	3.02
	3.107	3.19
	3.110	3.12	KM1
	3.113	3.32
	3.116	3.15
	3.119	3.33
	3.122	3.28
	3.125	3.52
	3.128	3.25
	3.131	3.26
	3.134	3.49
	3.137	3.53
	3.140	3.68
	3.143	3.73	KM2
	3.146	3.65
	3.149	3.42
	3.152	3.41
	3.155	3.24
	3.158	3.17
	3.161	3.09	KM3
	3.164	3.17
	3.167	3.21
	3.170	3.20
	3.173	3.31
	3.176	3.34
	3.179	3.32
	3.182	3.31	KM4
	3.185	3.45
	3.188	3.40
	3.191	3.32
	3.194	3.15
	3.197	3.07
	3.200	3.06
	3.203	3.04	KM5
	3.206	3.10
	3.209	3.22
	3.212	3.21
	3.215	3.10
	3.218	3.22
	3.221	3.22
	3.224	3.33	KM6
	3.227	3.30
	3.230	3.10
	3.233	3.25
	3.236	3.19
	3.239	3.11	KM7
	3.242	3.14
	3.245	3.20
	3.248	3.19
	3.251	3.11
	3.254	3.12
	3.257	3.15
	3.260	3.10
	3.263	3.16
	3.266	3.16
	3.269	3.17
	3.272	3.20
	3.275	3.00
	3.278	3.04
	3.281	3.10
	3.284	2.97	M1
	3.287	3.07
	3.290	3.09
	3.293	3.02
	3.296	3.07
	3.299	3.14
	3.302	3.23
	3.305	3.61
	3.308	3.75	M2
	3.311	3.57
	3.314	3.58
	3.317	3.75
	3.320	3.57
	3.323	3.47
	3.326	3.38
	3.329	3.39
	3.332	3.31	MG1
	3.335	3.36
	3.338	3.50
	3.341	3.73	MG2
	3.344	3.72
	3.347	3.61
	3.350	3.62
	3.353	3.53
	3.356	3.50
	3.359	3.41
	3.362	3.45
	3.365	3.32
	3.368	3.21
	3.371	3.16
	3.374	3.16
	3.377	3.18
	3.380	3.16	MG3
	3.383	3.19
	3.386	3.18
	3.389	3.16
	3.392	3.38
	3.395	3.32
	3.398	3.24
	3.401	3.22
	3.404	3.22
	3.407	3.02
	3.410	2.97
	3.413	3.31
	3.416	3.27
	3.419	3.21
	3.422	3.16
	3.425	3.14
	3.428	3.22
	3.431	3.30
	3.434	3.33
	3.437	3.37	MG4
	3.440	3.29
	3.443	3.23
	3.446	3.08
	3.449	3.00
	3.452	2.94
	3.455	2.90
	3.458	3.07
	3.461	3.12
	3.464	3.16
	3.467	3.09
	3.470	2.89
	3.473	3.03
	3.476	2.99
	3.479	3.09
	3.482	3.16
	3.485	3.06
	3.488	2.97
	3.491	2.98
	3.494	2.98
	3.497	2.74	MG5
	3.500	2.86
	3.503	2.90
	3.506	2.94
	3.509	2.88
	3.512	2.87
	3.515	2.90
	3.518	3.00
	3.521	3.03
	3.524	2.95
	3.527	2.95
	3.530	2.91
	3.533	2.86
	3.536	2.88
	3.539	2.88
	3.542	2.91
	3.545	3.06
	3.548	3.24	MG6
	3.551	3.10
	3.554	2.92
	3.557	2.97
	3.560	3.09
	3.563	3.04
	3.566	3.02
	3.569	3.05
	3.572	2.98
	3.575	2.88
	3.578	2.97
	3.581	3.03
	3.584	3.18
	3.587	3.14
	3.590	3.23
	3.593	3.06
	3.596	2.98
	3.599	2.94
	3.602	2.94
	3.605	3.01
	3.608	3.10
	3.611	2.95
	3.614	2.72	Gi1
	3.617	2.81
	3.620	2.92
	3.623	3.09
	3.626	3.21
	3.629	3.22
	3.632	3.29
	3.635	3.34	Gi2
	3.638	3.08
	3.641	2.88
	3.644	2.89
	3.647	2.87
	3.650	2.87
	3.653	2.79	Gi3
	3.656	2.84
	3.659	2.87
	3.662	3.01
	3.665	3.04
	3.668	3.13
	3.671	3.19
	3.674	3.22
	3.677	3.28	Gi4
	3.680	3.28
	3.683	3.23
	3.686	3.17
	3.689	3.12
	3.692	2.96
	3.695	2.91
	3.698	2.83
	3.701	2.71	Gi5
	3.704	3.01
	3.707	2.98
	3.710	2.87
	3.713	2.96
	3.716	3.06
	3.719	3.14	Gi6
	3.722	3.14
	3.725	2.98
	3.728	2.87
	3.731	2.94
	3.734	2.89
	3.737	2.73	Gi7
	3.740	2.82
	3.743	2.86
	3.746	2.85
	3.749	2.86
	3.752	2.85
	3.755	2.91
	3.758	3.04	Gi8
	3.761	2.94
	3.764	2.88
	3.767	2.81
	3.770	2.71	Gi9
	3.773	2.75
	3.776	2.74
	3.779	2.67
	3.782	2.82
	3.785	3.00
	3.788	3.11
	3.791	3.16
	3.794	3.20	Gi10
	3.797	2.99
	3.800	2.89
	3.803	2.88	Gi11
	3.806	2.97
	3.809	3.01
	3.812	2.99
	3.815	3.06
	3.818	3.03
	3.821	3.04
	3.824	3.10
	3.827	2.98
	3.830	2.94
	3.833	2.89
	3.836	2.93
	3.839	3.02
	3.842	3.18
	3.845	3.18	Gi12
	3.848	3.02
	3.851	2.80
	3.854	2.68
	3.857	2.64
	3.860	2.63	Gi13
	3.863	2.87
	3.866	2.85
	3.869	2.71
	3.872	2.76
	3.875	2.96
	3.878	3.01
	3.881	3.08
	3.884	3.13	Gi14
	3.887	3.12
	3.890	2.85
	3.893	2.85
	3.896	2.94
	3.899	2.85
	3.902	2.92
	3.905	3.03
	3.908	2.96
	3.911	2.92
	3.914	2.95
	3.917	2.88
	3.920	2.87
	3.923	2.99
	3.926	3.02
	3.929	2.99
	3.932	2.90
	3.935	2.85
	3.938	2.75	Gi15
	3.941	2.76
	3.944	3.06
	3.947	3.06
	3.950	3.06
	3.953	2.89
	3.956	2.88
	3.959	3.03
	3.962	3.02
	3.965	3.03
	3.968	3.07
	3.971	3.07
	3.974	3.08
	3.977	3.21
	3.980	3.15
	3.983	3.30
	3.986	3.21
	3.989	3.26
	3.992	3.39
	3.995	3.59	Gi16
	3.998	3.45
	4.001	3.31
	4.004	3.10
	4.007	3.28
	4.010	3.12
	4.013	2.96
	4.016	2.86	Gi17
	4.019	3.06
	4.022	3.11
	4.025	3.03
	4.028	2.98
	4.031	3.09
	4.034	3.28
	4.037	3.40	Gi18
	4.040	3.35
	4.043	3.35
	4.046	3.32
	4.049	3.31
	4.052	3.31
	4.055	3.14
	4.058	3.12
	4.061	3.01
	4.064	3.02
	4.067	2.98
	4.070	2.98	Gi19
	4.073	3.06
	4.076	3.04
	4.079	2.93
	4.082	2.99
	4.085	3.01
	4.088	3.09
	4.091	3.16
	4.094	3.20	Gi20
	4.097	3.10
	4.100	2.98
	4.103	2.83
	4.106	2.74	Gi21
	4.109	2.80
	4.112	2.90
	4.115	2.93
	4.118	2.99
	4.121	3.03
	4.124	3.00
	4.127	2.82
	4.130	2.96
	4.133	2.98
	4.136	2.94
	4.139	3.05
	4.142	3.14
	4.145	3.16	Gi22
	4.148	3.10
	4.151	2.91
	4.154	2.74
	4.157	2.76
	4.160	2.77
	4.163	2.78
	4.166	2.84
	4.169	2.86
	4.172	2.91
	4.175	2.81
	4.178	2.93
	4.181	2.87
	4.184	2.89
	4.187	2.96
	4.190	2.90
	4.193	2.89
	4.196	2.97
	4.199	2.98
	4.202	2.71
	4.205	2.60	Co1
	4.208	2.76
	4.211	3.00
	4.214	3.03
	4.217	3.06
	4.220	2.84
	4.223	2.84
	4.226	2.88
	4.229	2.94
	4.232	3.12
	4.235	3.15
	4.238	3.13
	4.241	3.03
	4.244	2.88
	4.247	2.90
	4.250	3.05
	4.253	3.21
	4.256	3.29	Co2
	4.259	3.11
	4.262	3.15
	4.265	3.11
	4.268	3.05
	4.271	2.84
	4.274	2.81
	4.277	2.70	Cn1
	4.280	2.89
	4.283	2.89
	4.286	3.07
	4.289	3.19
	4.292	3.04
	4.295	3.00
	4.298	2.93
	4.301	2.87
	4.304	2.94
	4.307	3.15
	4.310	3.10
	4.313	2.99
	4.316	2.84
	4.319	2.71
	4.322	2.68
	4.325	2.85
	4.328	2.94
	4.331	2.68
	4.334	2.81
	4.337	2.80
	4.340	2.84
	4.343	2.95
	4.346	2.98
	4.349	3.15
	4.352	3.02
	4.355	2.94
	4.358	2.99
	4.361	3.05
	4.364	3.02
	4.367	2.91
	4.370	2.87
	4.373	3.03
	4.376	3.08
	4.379	3.01
	4.382	3.12
	4.385	3.07
	4.388	3.14	Cn2
	4.391	2.96
	4.394	2.91
	4.397	3.08
	4.400	3.12
	4.403	3.00
	4.406	2.87
	4.409	2.90
	4.412	2.98
	4.415	2.75
	4.418	2.95
	4.421	3.21
	4.424	2.96
	4.427	2.97
	4.430	2.74
	4.433	2.84
	4.436	2.90
	4.439	2.78
	4.442	2.72	N1
	4.445	2.94
	4.448	3.07
	4.451	2.89
	4.454	2.56
	4.457	2.80
	4.460	2.87
	4.463	2.83
	4.466	2.81
	4.469	2.76
	4.472	2.68
	4.475	2.71
	4.478	2.82
	4.481	2.83
	4.484	2.68
	4.487	2.79
	4.490	2.87
	4.493	2.88
	4.496	2.94
	4.499	2.99
	4.502	2.80
	4.505	2.91
	4.508	2.84
	4.511	3.08
	4.514	3.21
	4.517	3.22	N2
	4.520	3.14
	4.523	2.97
	4.526	2.90
	4.529	2.86	N3
	4.532	2.89
	4.535	2.93
	4.538	2.95
	4.541	3.00
	4.544	2.95
	4.547	2.98
	4.550	3.03
	4.553	3.17
	4.556	3.29	N4
	4.559	3.25
	4.562	3.19
	4.565	3.09
	4.568	3.02
	4.571	3.11
	4.574	3.07
	4.577	3.00
	4.580	3.03
	4.583	2.98
	4.586	2.97	N5
	4.589	3.04
	4.592	3.12
	4.595	3.22
	4.598	3.26	N6
	4.601	3.15
	4.604	2.98
	4.607	3.01
	4.610	3.13
	4.613	3.19
	4.616	3.15
	4.619	2.99
	4.622	2.90
	4.625	2.87	N7
	4.628	2.96
	4.631	3.20	N8
	4.634	3.19
	4.637	3.10
	4.640	3.01
	4.643	2.95
	4.646	2.95
	4.649	2.88
	4.652	2.88
	4.655	2.92
	4.658	2.84
	4.661	2.75	NS1 
	4.664	2.77
	4.667	3.30
	4.670	3.32	NS2
	4.673	3.21
	4.676	3.07
	4.679	3.18
	4.682	3.18
	4.685	3.01
	4.688	3.13
	4.691	3.10
	4.694	3.13
	4.697	3.10
	4.700	2.99	NS3
	4.703	3.04
	4.706	3.22
	4.709	3.25
	4.712	3.26	NS4
	4.715	3.23
	4.718	3.25
	4.721	3.20
	4.724	3.05
	4.727	3.00
	4.730	2.98
	4.733	3.02
	4.736	3.05
	4.739	2.93
	4.742	2.87	NS5
	4.745	3.00
	4.748	3.15
	4.751	3.30
	4.754	3.31	NS6
	4.757	3.26
	4.760	3.10
	4.763	2.95
	4.766	2.96
	4.769	2.85
	4.772	2.90
	4.775	3.03
	4.778	3.00
	4.781	2.88	Si1
	4.784	2.92
	4.787	3.01
	4.790	3.19	Si2
	4.793	3.07
	4.796	3.03
	4.799	2.96
	4.802	2.84
	4.805	2.63	Si3
	4.808	2.74
	4.811	2.75
	4.814	2.80
	4.817	2.86
	4.820	2.91
	4.823	2.96
	4.826	3.31
	4.829	3.47	Si4
	4.832	3.42
	4.835	3.38
	4.838	3.30
	4.841	2.99
	4.844	3.03
	4.847	2.95
	4.850	2.87
	4.853	2.83	Si5
	4.856	2.93
	4.859	3.03
	4.862	3.09
	4.865	3.19
	4.868	3.32
	4.871	3.45
	4.874	3.48
	4.877	3.50	Si6
	4.880	3.39
	4.883	3.28
	4.886	3.29
	4.889	3.08
	4.892	2.99
	4.895	2.87	ST1
	4.898	2.90
	4.901	3.00
	4.904	3.04
	4.907	3.00
	4.910	3.05
	4.913	2.98
	4.916	2.98
	4.919	2.97
	4.922	3.00
	4.925	3.09
	4.928	2.98
	4.931	3.12
	4.934	3.15	ST2
	4.937	3.11
	4.940	3.04
	4.943	2.95
	4.946	2.97
	4.949	3.06
	4.952	3.12
	4.955	3.16
	4.958	2.92
	4.961	2.89
	4.964	3.03
	4.967	3.02
	4.970	2.89
	4.973	2.87
	4.976	2.90
	4.979	2.92
	4.982	2.89
	4.985	2.90
	4.988	2.82	T1
	4.991	2.87
	4.994	2.91
	4.997	2.99
	5.000	2.99
	5.003	2.97
	5.006	2.98
	5.009	3.12	T2
	5.012	3.08
	5.015	2.90
	5.018	2.93
	5.021	2.92
	5.024	2.84
	5.027	2.83	T3
	5.030	2.83
	5.033	2.92
	5.036	2.94
	5.039	3.04
	5.042	3.28	T4
	5.045	3.26
	5.048	3.18
	5.051	3.14
	5.054	3.11
	5.057	2.99
	5.060	3.06
	5.063	3.04
	5.066	3.00
	5.069	2.97
	5.072	2.91
	5.075	3.03
	5.078	3.06
	5.081	2.90
	5.084	2.81
	5.087	2.70	T5
	5.090	3.02
	5.093	2.85
	5.096	2.72
	5.099	2.87
	5.102	2.69
	5.105	2.65
	5.108	2.93
	5.111	3.01
	5.114	3.11	T6
	5.117	3.05
	5.120	2.95
	5.123	2.88
	5.126	2.82
	5.129	2.61	T7
	5.132	2.68
	5.135	2.57
	5.138	2.65
	5.141	2.85
	5.144	2.91
	5.147	2.89
	5.150	2.93
	5.153	2.94
	5.156	3.05
	5.159	3.21	T8
	5.162	3.15
	5.165	3.12
	5.168	2.89
	5.171	2.85
	5.174	2.80
	5.177	2.84
	5.180	2.95
	5.183	2.85
	5.186	2.91
	5.189	2.89
	5.192	2.86
	5.195	2.82
	5.198	2.80	TG1
	5.201	2.80
	5.204	2.79
	5.207	2.79
	5.210	2.90
	5.213	2.89
	5.216	2.89
	5.219	2.85
	5.222	2.79
	5.225	2.97
	5.228	2.97
	5.231	2.97
	5.234	2.97
	5.237	2.97
	5.240	2.90
	5.243	2.95
	5.246	3.03	TG2
	5.249	2.86
	5.252	2.84
	5.255	2.75
	5.258	2.77
	5.261	2.79
	5.264	2.88
	5.267	2.82
	5.270	2.91
	5.273	2.98
	5.276	3.07
	5.279	2.92
	5.282	2.89
	5.285	2.79
	5.288	2.86
	5.291	2.78	TG3
	5.294	2.83
	5.297	2.93
	5.300	2.99	TG4
	5.303	2.93
	5.306	2.86
	5.309	2.80
	5.312	2.86
	5.315	2.75
	5.318	2.89
	5.321	2.79
	5.324	2.68
	5.327	2.64
	5.330	2.47	TG5
	5.333	2.87
	5.336	2.87
	5.339	2.93
	5.342	2.92
	5.345	2.94
	5.348	2.89
	5.351	2.93
	5.354	3.14	TG6
	5.357	3.06
	5.360	2.90
	5.363	2.94
	5.366	3.07
	5.369	2.96
	5.372	2.94
	5.375	2.99
	5.378	2.91
	5.381	2.97
	5.384	2.80
	5.387	2.82
	5.390	2.78
	5.393	2.69	TG7
	5.396	2.73
	5.399	2.83
	5.402	2.95
	5.405	2.85
	5.408	2.98
	5.411	2.92
	5.414	2.90
	5.417	3.03
	5.420	3.05	TG8
	5.423	2.97
	5.426	2.82
	5.429	2.80
	5.432	3.05
	5.435	3.02
	5.438	3.09
	5.441	2.82
	5.444	2.78
	5.447	2.84
	5.450	2.89
	5.453	2.93
	5.456	2.89
	5.459	2.51	TG9
	5.462	2.60
	5.465	2.90
	5.468	2.80
	5.471	2.77
	5.474	2.43
	5.477	2.63
	5.480	2.78
	5.483	2.62
	5.486	2.77
	5.489	2.90
	5.492	2.95
	5.495	3.00
	5.498	3.10	TG10
	5.501	3.04
	5.504	2.93
	5.507	2.86
	5.510	2.87
	5.513	2.95
	5.516	2.99
	5.519	2.99
	5.522	2.83
	5.525	2.68	TG11
	5.528	2.76
	5.531	2.92
	5.534	3.04
	5.537	3.19
	5.540	3.24	TG12
	5.543	3.18
	5.546	3.08
	5.549	2.90	TG13
	5.552	2.93
	5.555	3.04
	5.558	3.09
	5.561	3.24	TG14
	5.564	3.16
	5.567	3.17
	5.570	3.31
	5.573	3.24
	5.576	3.05
	5.579	3.03
	5.582	2.99
	5.585	3.03
	5.588	2.97	TG15
	5.591	3.06
	5.594	3.03
	5.597	3.02
	5.600	3.07
	5.603	2.99
	5.606	2.81
	5.609	2.87
	5.612	2.88
	5.615	2.92
	5.618	3.02
	5.621	3.08
	5.624	3.11
	5.627	2.96
	5.630	3.08
	5.633	3.17
	5.636	3.19	TG16
	5.639	3.14
	5.642	3.10
	5.645	3.09
	5.648	3.11
	5.651	3.25
	5.654	3.30
	5.657	3.08
	5.660	2.88	TG17
	5.663	3.02
	5.666	3.01
	5.669	3.07
	5.672	3.18
	5.675	3.23
	5.678	3.08
	5.681	3.28	TG18
	5.684	3.36
	5.687	3.19
	5.690	3.31
	5.693	3.29
	5.696	3.19
	5.699	3.06
	5.702	3.04	TG19
	5.705	3.09
	5.708	3.13
	5.711	3.55	TG20
	5.714	3.38
	5.717	3.38
	5.720	3.20
	5.723	2.95	TG21
	5.726	3.12
	5.729	3.30
	5.732	3.31
	5.735	3.19
	5.738	3.05
	5.741	3.00
	5.744	3.15
	5.747	3.14
	5.750	3.14
	5.753	3.36	TG22
	5.756	3.23
	5.759	3.01
	5.762	3.06
	5.765	3.13
	5.768	3.15
	5.771	3.04
	5.774	3.02
	5.777	3.02
	5.780	2.92
	5.783	2.96
	5.786	3.00
	5.789	3.08
	5.792	3.08
	5.795	3.04
	5.798	3.03
	5.801	3.04
	5.804	3.11
	5.807	2.96
	5.810	3.03
	5.813	3.00
	5.816	3.02
	5.819	3.18
	5.822	3.18
	5.825	3.08
	5.828	3.04
	5.831	2.96
	5.834	3.04
	5.837	3.12
	5.840	3.18
	5.843	3.29
	5.846	3.06
	5.849	3.14
	5.852	3.09
	5.855	3.17
	5.858	3.08
	5.861	2.95
	5.864	3.08
	5.867	3.11
	5.870	3.04
	5.873	3.08
	5.876	2.95
	5.879	2.99
	5.882	2.95
	5.885	3.18
	5.888	3.22
	5.891	3.14
	5.894	3.09
	5.897	3.13
	5.900	3.20
	5.903	3.29
	5.906	3.11
	5.909	3.12
	5.912	3.19
	5.915	3.07
	5.918	3.13
	5.921	3.16
	5.924	3.17
	5.927	3.17
	5.930	3.23
	5.933	3.22
	5.936	3.10
	5.939	3.17
	5.942	3.19
	5.945	2.96
	5.948	2.94
	5.951	2.99
	5.954	3.07
	5.957	3.05
	5.960	2.99
	5.963	3.06
	5.966	3.04
	5.969	3.10
	5.972	3.17
	5.975	3.05
	5.978	3.08
	5.981	3.10
	5.984	2.91
	5.987	2.75
	5.990	2.98
	5.993	3.11
	5.996	3.13
	5.999	2.87
	6.002	3.01
	6.005	3.06
	6.008	3.07
	6.011	2.94
	6.014	2.85
	6.017	3.02
	6.020	3.11
	6.023	3.07
	6.026	2.94
	6.029	3.01
	6.032	3.09
	6.035	2.99
	6.038	3.03
	6.041	3.00
	6.044	3.14
	6.047	3.14
	6.050	3.00
	6.053	3.09
	6.056	2.86
	6.059	2.70
	6.062	2.85
	6.065	2.93
	6.068	2.97
	6.071	2.85
	6.074	2.79
	6.077	2.73
	6.080	2.82
	6.083	3.01
	6.086	2.99
	6.089	2.98
	6.092	2.88
	6.095	2.97
	6.098	2.95
	6.101	2.96
	6.104	2.95
	6.107	2.98
	6.110	3.02
	6.113	3.01
	6.116	2.97
	6.119	2.86
	6.122	2.98
	6.125	3.17
	6.128	3.42
	6.131	3.41
	6.134	3.35
	6.137	3.29
	6.41	3.15
	6.67	3.00
	6.94	2.75
	7.17	2.65
	7.36	2.60
	7.59	2.65
	7.79	2.70
	8.04	2.80
	8.29	2.78
	8.56	2.75
	8.82	2.75
	8.93	2.73
	9.34	2.70
	9.58	2.68
	9.79	2.65
	10.07	2.63
	10.32	2.60
	10.58	2.55
	10.84	2.53
	11.08	2.55
	11.31	2.55
	11.58	2.50
	11.83	2.45
	12.06	2.40
	12.27	2.43
	12.53	2.43
	12.80	2.45
	13.02	2.30
	13.31	2.25
	13.59	2.10
	13.78	2.00
	14.02	1.88
	14.26	1.83
	14.48	1.73
	14.73	1.65
	14.99	1.65
	15.25	1.68
	15.49	1.70
	15.72	1.73
	15.96	1.75
	16.22	1.73
	16.48	1.70
	16.75	1.65
	16.98	1.73
	17.21	1.80
	17.43	1.85
	17.57	1.88
	17.64	1.88
	17.71	1.90
	18.26	1.93
	18.49	1.93
	18.71	1.95
	18.93	1.95
	19.16	1.98
	19.38	2.00
	19.61	2.03
	19.82	2.03
	20.02	2.03
	20.24	2.03
	20.44	2.00
	20.65	2.00
	20.86	1.98
	21.06	1.95
	21.27	1.93
	21.48	1.85
	21.69	1.80
	21.94	1.78
	22.20	1.83
	22.41	1.88
	22.72	1.85
	22.98	2.00
	23.25	2.40
	23.52	1.68
	23.79	1.63
	24.06	2.00
	24.35	2.40
	24.63	1.70
	24.92	1.90
	25.21	2.20
	25.51	2.48
	25.80	2.60
	26.09	2.65
	26.39	2.68
	26.69	2.70
	26.98	2.70
	27.27	2.70
	27.56	2.68
	27.86	2.65
	28.15	2.65
	28.44	2.63
	28.72	2.63
	29.00	2.63
	29.28	2.65
	29.56	2.63
	29.84	2.63
	30.11	2.60
	30.38	2.58
	30.65	2.55
	30.92	2.53
	31.18	2.48
	31.44	2.48
	31.67	2.48
	31.93	2.48
	32.19	2.48
	32.45	2.50
	32.71	2.53
	32.94	2.63
	33.20	2.73
	33.45	2.80
	33.69	2.35
	33.93	1.95
	34.17	1.75
	34.40	1.73
	34.64	1.70
	34.87	1.70
	35.10	1.73
	35.32	1.73
	35.54	1.75
	35.76	1.75
	35.98	1.75
	36.20	1.70
	36.41	1.68
	36.62	1.65
	36.84	1.63
	37.05	1.60
	37.26	1.55
	37.47	1.53
	37.67	1.48
	37.89	1.45
	38.10	1.43
	38.31	1.38
	38.51	1.35
	38.72	1.33
	38.93	1.30
	39.14	1.25
	39.35	1.20
	39.57	1.18
	39.79	1.15
	40.00	1.10
	40.22	1.08
	40.43	1.05
	40.66	1.03
	40.88	1.00
	41.10	0.98
	41.33	0.98
	41.55	0.95
	41.79	0.95
	42.03	0.95
	42.26	0.95
	42.50	0.95
	42.74	0.95
	42.98	0.95
	43.26	0.93
	43.52	0.90
	43.78	0.85
	44.03	0.83
	44.29	0.75
	44.55	0.73
	44.81	0.68
	45.06	0.63
	45.32	0.55
	45.61	0.53
	45.89	0.45
	46.20	0.43
	46.48	0.35
	46.76	0.33
	47.05	0.28
	47.34	0.25
	47.64	0.18
	47.96	0.15
	48.26	0.10
	48.56	0.08
	48.86	0.05
	49.17	0.00
	49.47	-0.03
	49.78	-0.03
	50.08	-0.05
	50.39	-0.05
	50.69	-0.05
	50.99	-0.08
	51.30	-0.08
	51.61	-0.08
	51.91	-0.08
	52.21	-0.05
	52.51	-0.03
	52.82	0.00
	53.11	0.05
	53.40	0.10
	53.69	0.15
	53.98	0.18
	54.26	0.23
	54.55	0.23
	54.81	0.23
	55.09	0.25
	55.38	0.28
	55.67	0.20
	55.73	-0.10
	55.75	0.35
	55.95	0.38
	56.21	0.43
	56.49	0.45
	56.77	0.53
	57.04	0.55
	57.29	0.60
	57.55	0.65
	57.80	0.70
	58.07	0.75
	58.32	0.78
	58.58	0.80
	58.82	0.83
	59.06	0.83
	59.32	0.80
	59.55	0.78
	59.79	0.75
	60.05	0.73
	60.28	0.70
	60.51	0.68
	60.75	0.68
	61.01	0.68
	61.24	0.65
	61.48	0.65
	61.71	0.65
	61.96	0.65
	62.18	0.65
	62.42	0.63
	62.64	0.63
	62.88	0.65
	63.10	0.65
	63.33	0.65
	63.55	0.65
	63.78	0.68
	64.01	0.70
	64.23	0.73
	64.45	0.75
	64.67	0.75
	64.90	0.78
	65.12	0.83
	65.35	0.83
	65.57	0.85
	65.79	0.88
	66.03	0.90
	66.26	0.93
	66.50	0.95
	66.72	0.98
	66.96	0.98
	67.20	1.03
	67.44	1.05


Marine Carbon-13 Composite (per-mil PDB)	point				off	Zachos et al. (2001)
nopoints	line		-0.3	2.2	smoothed
	0.00	0.18
	0.25	0.08
	0.50	0.00
	0.75	-0.08
	1.00	0.15
	1.25	0.40
	1.50	0.30
	1.75	0.18
	2.00	0.10
	2.25	0.00
	2.50	-0.10
	2.75	-0.15
	3.00	-0.20
	3.25	-0.25
	3.50	-0.15
	3.75	-0.05
	4.00	-0.03
	4.25	-0.13
	4.50	-0.20
	4.75	-0.05
	5.00	0.08
	5.26	0.23
	5.55	0.20
	5.86	0.15
	6.13	0.23
	6.41	0.58
	6.67	0.83
	6.94	0.90
	7.17	1.05
	7.36	1.13
	7.59	0.95
	7.79	0.78
	8.04	1.00
	8.29	1.03
	8.56	1.18
	8.82	1.15
	8.93	1.13
	9.34	1.10
	9.58	1.08
	9.79	1.05
	10.07	1.08
	10.32	1.05
	10.58	1.00
	10.84	1.05
	11.08	1.10
	11.31	1.10
	11.58	1.10
	11.83	1.05
	12.06	1.08
	12.27	1.10
	12.53	1.13
	12.80	1.25
	13.02	1.45
	13.31	1.53
	13.59	1.53
	13.78	1.53
	14.02	1.55
	14.26	1.58
	14.48	1.60
	14.73	1.58
	14.99	1.53
	15.25	1.50
	15.49	1.60
	15.72	1.70
	15.96	1.78
	16.22	1.60
	16.48	1.48
	16.75	1.35
	16.98	1.28
	17.21	1.20
	17.43	1.10
	17.57	1.00
	17.64	0.98
	17.71	0.93
	18.26	0.88
	18.49	0.83
	18.71	0.83
	18.93	0.83
	19.16	0.83
	19.38	0.83
	19.61	0.85
	19.82	0.88
	20.02	0.88
	20.24	0.88
	20.44	0.90
	20.65	0.93
	20.86	0.95
	21.06	0.98
	21.27	1.03
	21.48	1.05
	21.69	1.10
	21.94	1.15
	22.20	1.18
	22.41	1.23
	22.72	1.10
	22.98	1.00
	23.25	0.88
	23.52	0.80
	23.79	0.75
	24.06	0.70
	24.35	0.63
	24.63	0.60
	24.92	0.68
	25.21	0.78
	25.51	0.80
	25.80	0.75
	26.09	0.73
	26.39	0.68
	26.69	0.63
	26.98	0.58
	27.27	0.58
	27.56	0.55
	27.86	0.55
	28.15	0.55
	28.44	0.55
	28.72	0.53
	29.00	0.48
	29.28	0.48
	29.56	0.50
	29.84	0.53
	30.11	0.60
	30.38	0.75
	30.65	0.88
	30.92	0.95
	31.18	0.95
	31.44	0.95
	31.67	0.95
	31.93	0.95
	32.19	1.00
	32.45	1.00
	32.71	1.03
	32.94	1.18
	33.20	1.30
	33.45	1.40
	33.69	1.18
	33.93	1.00
	34.17	0.90
	34.40	1.03
	34.64	1.10
	34.87	1.00
	35.10	0.93
	35.32	0.85
	35.54	0.83
	35.76	0.78
	35.98	0.78
	36.20	0.75
	36.41	0.73
	36.62	0.75
	36.84	0.73
	37.05	0.73
	37.26	0.73
	37.47	0.73
	37.67	0.73
	37.89	0.73
	38.10	0.75
	38.31	0.80
	38.51	0.83
	38.72	0.85
	38.93	0.88
	39.14	0.90
	39.35	0.93
	39.57	0.95
	39.79	0.95
	40.00	0.95
	40.22	0.90
	40.43	0.88
	40.66	0.85
	40.88	0.83
	41.10	0.78
	41.33	0.78
	41.55	0.75
	41.79	0.75
	42.03	0.75
	42.26	0.75
	42.50	0.75
	42.74	0.75
	42.98	0.78
	43.26	0.75
	43.52	0.75
	43.78	0.75
	44.03	0.73
	44.29	0.73
	44.55	0.73
	44.81	0.73
	45.06	0.73
	45.32	0.75
	45.61	0.75
	45.89	0.78
	46.20	0.78
	46.48	0.80
	46.76	0.83
	47.05	0.83
	47.34	0.83
	47.64	0.85
	47.96	0.83
	48.26	0.83
	48.56	0.83
	48.86	0.83
	49.17	0.80
	49.47	0.75
	49.78	0.73
	50.08	0.70
	50.39	0.63
	50.69	0.58
	50.99	0.53
	51.30	0.45
	51.61	0.38
	51.91	0.35
	52.21	0.30
	52.51	0.28
	52.82	0.25
	53.11	0.30
	53.40	0.40
	53.69	0.48
	53.98	0.63
	54.26	0.75
	54.55	0.83
	54.81	0.93
	55.09	1.00
	55.38	1.18
	55.67	1.00
	55.73	0.20
	55.75	1.45
	55.95	1.53
	56.21	1.73
	56.49	1.88
	56.77	1.98
	57.04	2.05
	57.29	2.10
	57.55	2.13
	57.80	2.13
	58.07	2.10
	58.32	2.05
	58.58	2.03
	58.82	1.93
	59.06	1.85
	59.32	1.73
	59.55	1.65
	59.79	1.55
	60.05	1.45
	60.28	1.38
	60.51	1.30
	60.75	1.25
	61.01	1.20
	61.24	1.15
	61.48	1.13
	61.71	1.10
	61.96	1.05
	62.18	1.05
	62.42	1.05
	62.64	1.08
	62.88	1.10
	63.10	1.13
	63.33	1.15
	63.55	1.18
	63.78	1.25
	64.01	1.28
	64.23	1.33
	64.45	1.38
	64.67	1.45
	64.90	1.48
	65.12	1.55
	65.35	1.58
	65.57	1.65
	65.79	1.70
	66.03	1.75
	66.26	1.80
	66.50	1.85
	66.72	1.93
	66.96	2.00
	67.20	2.03
	67.44	2.08
	67.68	2.13


Strontium 87/86 ratio	point				off	John McArthur (2004, Lowess version 4, supporting compilation for GTS2004)
nopoints	line		0.7060	0.7100	smoothed
	0.00	0.709174	Present
	0.61	0.709154	Base Pt1b (Top Pt1a)
	1.77	0.709090	Base Pt1a (Top PL6)
	2.00	0.709082	Base N21&N22
	2.39	0.709070	Base PL6 (dual markers)
	3.13	0.709057	Base PL5
	3.81	0.709052	Base PL3
	4.37	0.709047	Base PL2
	5.332	0.709022	Base Miocene
	5.72	0.709008	Base PL1; N18
	6.14	0.708982	M14
	6.58	0.708963	N17b
	7.12	0.708948	Base Messinian
	8.93	0.708911	Base M13b
	10.57	0.708863	Base M13a, N16
	11.47	0.708836	Base M12 & N15
	11.79	0.708834	Base M10; N13
	13.13	0.708806	Base M9b
	13.77	0.708795	Base N11
	14.24	0.708794	Base M7, N10
	14.74	0.708786	Base M6; N9
	16.27	0.708692	Base M5b
	16.97	0.708658	Base M5a; N8
	17.54	0.708622	Base M4a; N7
	20.06	0.708497	Globigerinoides altiaperturus
	21.12	0.708371	Base M2; N5
	22.38	0.708282	Base M1b; N4b
	22.96	0.708248	Base M1; N4
	25.40	0.708132	Paragloborotalia pseudokugleri
	26.83	0.708088	Base P22
	28.45	0.708034	Base P21b
	29.45	0.707993	Base P21a
	30.42	0.707961	Base P20
	32.19	0.707898	Base P19
	33.88	0.707804	Base O1 (base Oligocene)
	34.47	0.707780	Base E16
	35.82	0.707757	Base E15
	37.67	0.707731	Base E14
	39.36	0.707723	Base P14, E13
	41.36	0.707738	Base E11
	42.60	0.707755	Base P12, E10
	45.00	0.707763	Base P11, E9
	48.60	0.707719	Base P10, E8
	50.30	0.707703	Base P9, E7
	52.57	0.707715	Base P7, E5
	54.52	0.707741	Base P6b, E4
	55.09	0.707750	Base P6a, E3
	55.73	0.707758	Base E1 (approx PETM)
	56.67	0.707768	Base P5
	57.30	0.707774	Base P4c
	60.19	0.707796	Base of P4a
	61.72	0.707804	Base P3
	63.44	0.707813	Base P1c
	64.71	0.707822	Base P1b
	65.50	0.707827	Base P0 (base Cenozoic)
	68.33	0.707784	Jeletzkytes nebrascensis
	69.23	0.707766	Hoploscaphites birkelundi
	70.56	0.707717	Baculites baculus
	71.56	0.707717	Baculites jenseni
	73.50	0.707650	Baculites compressus
	74.28	0.707628	Didymoceras cheyennense
	75.05	0.707613	Exiteloceras jenneyi
	76.38	0.707575	Didymoceras nebrascense
	78.68	0.707523	Baculites gilberti
	80.64	0.707496	Baculites obtusus
	82.20	0.707471	Scaphites hippocrepis II
	83.53	0.707447	Scaphites leei III
	83.99	0.707440	Desmoscaphites bassleri
	84.94	0.707434	Clioscaphites vermiformis
	85.85	0.707422	Clioscaphites saxitonianus
	86.96	0.707390	Scaphites depressus
	88.58	0.707340	Forresteria allaudi - Scaphites preventricosus
	89.07	0.707320	Forresteria peruana
	90.48	0.707289	Prionocyclus macombi
	90.94	0.707300	Prionocyclus hyatti
	92.13	0.707324	Collignoniceras woollgari
	93.41	0.707355	Pseudaspidoceras flexuosum
	93.64	0.707361	Neocardioceras juddii
	94.01	0.707368	Sciponoceras gracile (Vascoceras diartianum)
	95.06	0.707386	Acanthoceras amphibolum
	96.01	0.707397	Conlinoceras tarrantense - Conlinoceras gilberti
	98.64	0.707413	Neogastroplites cornutus
	99.60	0.707416	Rotalipora globotruncanoides
	100.94	0.707420	Rotalipora appenninica
	102.93	0.707421	Rotalipora ticinensis
	105.05	0.707404	Rotalipora subticinensis
	106.42	0.707403	Ticinella praeticinensis
	110.89	0.707323	Ticinella primula
	112.02	0.707281	Prediscosphaera columnata
	113.00	0.707237	Hypacanthoplites jacobi
	114.30	0.707202	Ticinella bejaouaensis
	115.00	0.707219	Nolaniceras nolani
	118.00	0.707280	Parahoplites melchioris
	121.00	0.707330	Epicheloniceras subnodosocostatum
	124.50	0.707406	Leupoldina cabri (rare)
	125.00	0.707420	M0r
	126.10	0.707431	Colchidites sarasini
	127.20	0.707478	Hemihoplites feraudianus
	128.30	0.707486	Ancyloceras vandenheckii
	128.97	0.707478	Kotetishvilia compressissima
	129.64	0.707475	Nicklesia nicklesi
	129.97	0.707473	Spitidiscus hugii
	131.91	0.707454	Pseudothurmannia ohmi
	133.21	0.707434	"Pleisiospitidiscus ligatus"
	134.50	0.707409	Lyticoceras nodosoplicatus
	136.44	0.707376	Acanthodiscus radiatus
	137.27	0.707364	Criosarasinella furcillata
	138.11	0.707354	Neocomites peregrinus
	138.94	0.707339	Saynoceras verrucosum
	139.77	0.707314	Busnardoites campylotoxus
	140.18	0.707296	Tirnovella pertransiens
	140.66	0.707279	Thurmanniceras otopeta
	142.30	0.707229	Subthurmannia boissieri
	143.68	0.707196	Subthurmannia occitanica
	145.46	0.707167	Berriasella jacobi
	146.14	0.707158	Durangites
	147.16	0.707141	Micracanthoceras microcanthum
	148.98	0.707090	Semiformiceras fallauxi
	149.89	0.707060	Semiformiceras darwini
	150.84	0.707025	Hybonoticeras hybonotum
	152.20	0.706967	Hybonoticeras beckeri
	152.59	0.706950	Aulacostephanus (Pseudomutabilis) eudoxus
	153.06	0.706932	Aspidoceras acanthicum
	154.14	0.706897	Ataxioceras (A.) hypselocyclum
	154.53	0.706886	Sutneria platynota
	155.35	0.706871	Idoceras planula
	156.81	0.706853	Epipeltoceras bimammatum
	158.43	0.706843	Gregoryceras transversarium
	159.61	0.706842	Perisphinctes (Arisphinctes) plicatilis
	161.21	0.706852	Quenstedtoceras (Q.) mariae
	162.01	0.706864	Quenstedtoceras (Lamberticeras) lamberti
	162.86	0.706883	Erymnoceras coronatum
	164.23	0.706928	Macrocephalites (Dolikephalites) gracilis
	165.13	0.706963	Clydoniceras (C.) discus
	166.11	0.707031	Cadomites (C.) bremeri
	166.89	0.707065	Procerites (P.)  progracilis
	167.68	0.707077	Zigzagiceras (Z.) zigzag 
	168.27	0.707104	Parkinsonia (P.) parkinsoni
	169.64	0.707229	Strenoceras (S.) niortense
	170.62	0.707269	Sonninia propinquans
	171.60	0.707284	Hyperlioceras (H.) discites
	172.49	0.707284	Graphoceras concavum
	173.38	0.707282	Brasilia bradfordensis
	174.71	0.707280	Ludwigia murchisonae
	175.60	0.707278	Leioceras opalinum
	176.58	0.707275	Pleydellia aalensis
	178.54	0.707219	Dumortieria levesquei
	180.50	0.707160	Grammoceras thouarsense
	180.70	0.707150	Haugia variabilis
	181.20	0.707133	Hildoceras bifrons
	182.70	0.707077	Harpoceras falciferum
	183.00	0.707071	Dactylioceras (Orthodactylites) tenuicostatum
	183.60	0.707067	Pleuroceras hawskerense
	184.20	0.707086	Pleuroceras spinatum
	186.95	0.707241	Amaltheus margaritatus
	187.75	0.707293	Prodactylioceras davoei
	188.54	0.707348	Tragophylloceras ibex
	189.60	0.707405	Uptonia jamesoni
	191.22	0.707471	Echioceras raricostatum
	192.04	0.707491	Oxynoticeras oxynotum
	193.25	0.707534	Asteroceras obtusum
	194.06	0.707572	Caenisites turneri
	195.28	0.707645	Arnioceras semicostatum
	196.50	0.707709	Arietites bucklandi
	197.28	0.707733	Schlotheimia angulata
	198.44	0.707733	Alsatites liasicus
	199.60	0.707703	Psiloceras planorbis
	200.95	0.707710	Choristoceras marshi
	202.29	0.707779	Vandaites stuerzenbaumi
	203.64	0.707847	Sagenites reticulatus
	205.71	0.707919	Rhabdoceras suessi
	207.57	0.707895	Halorites macer
	210.01	0.707782	Himavatites hogarti
	211.30	0.707748	Cyrtopleurites bicrenatus
	212.20	0.707745	Juvavites magnus
	214.02	0.707727	Malayites paulckei
	216.53	0.707702	Guembelites jandianus 
	218.66	0.707692	Anatropites spinosus
	220.95	0.707673	Tropites subbullatus
	222.70	0.707648	Tropites dilleri
	225.66	0.707611	Austrotrachyceras austriacum
	226.94	0.707604	Trachyceras aonoides
	228.01	0.707610	Trachyceras aon
	228.73	0.707620	Daxatina cf. canadensis
	230.27	0.707638	Protrachyceras neumayri
	231.68	0.707658	Protrachyceras longobardicum
	233.34	0.707683	Eoprotrachyceras gredleri
	234.56	0.707707	Protrachyceras margaritosum
	237.00	0.707781	Eoprotrachyceras curionii
	238.00	0.707812	Chieseiceras chiesense
	239.00	0.707834	Serpianites serpianensis
	240.00	0.707845	Ticinites crassus
	241.00	0.707876	Reitziites reitzi
	241.60	0.707903	Paraceratites
	242.49	0.707963	Balatonites balatonicus
	243.68	0.708088	Kocaelia
	245.17	0.708158	Paracrochordiceras
	246.63	0.708045	Toziceras pakistanum
	248.08	0.707830	Tirolites cassianus
	249.75	0.707567	Meekoceras gracilitatis
	250.38	0.707506	Gyronites frequens
	250.73	0.707475	Ophiceras connectens + Ophiceras tibeticum
	251.09	0.707445	Otoceras woodwardi
	251.21	0.707437	Otoceras concavum
	251.56	0.707408	Clarkina yini
	253.10	0.707282	Clarkina subcarinata
	253.80	0.707222	Clarkina wangi
	255.78	0.707072	Clarkina orientalis
	256.44	0.707030	Clarkina transcaucasica
	258.42	0.706928	Clarkina leveni
	259.08	0.706902	Clarkina asymetrica
	260.40	0.706872	Clarkina postbitteri postbitteri
	263.10	0.706904	Jinogondolella altudaensis
	265.80	0.707056	Jinogondolella postserrata
	268.00	0.707204	Jinogondolella aserrata
	270.60	0.707297	Jinogondolella nankingensis
	271.60	0.707354	Neostreptognathodus sulcoplicatus
	273.35	0.707465	Neostreptognathodus prayi
	275.60	0.707529	Neostreptognathodus pnevi
	277.80	0.707542	Neostreptognathodus pequopensis
	284.40	0.708055	Sweetognathus whitei
	286.44	0.708104	Sweetognathus binodosus
	294.60	0.708047	Sweetognathus merrilli
	295.48	0.708053	Streptognathodus barskovi
	296.14	0.708058	Streptognathodus postfusus
	297.24	0.708066	Streptognathodus fusus
	298.34	0.708073	Streptognathodus constrictus
	299.00	0.708080	Streptognathodus isolatus
	299.98	0.708115	Streptognathodus wabaunsensis
	301.21	0.708156	Streptognathodus simplex
	303.17	0.708209	Streptognathodus vitali
	303.90	0.708225	Streptognathodus "simulatos"
	304.68	0.708240	Idiognathodus toretzianus
	305.72	0.708255	Idiognathodus sagittalis
	306.50	0.708265	Streptognathodus subexcelsus - St. makhlinae
	308.06	0.708278	Neognathodus roundyi - Streptognathodus cancellosus
	309.36	0.708281	Neognathodus medexultimus -Streptognathodus concinnus
	310.14	0.708280	Streptognathodus dissectus
	311.18	0.708276	Neognathodus uralicus
	311.70	0.708273	Declinognathodus donetzianus
	312.66	0.708267	Neognathodus atokaensis
	313.94	0.708253	Declinognathodus marginodosus
	314.90	0.708241	Idiognathodus sinuosus
	315.54	0.708233	Neognathodus askynensis
	317.14	0.708207	Idiognathoides sinuatus
	318.10	0.708188	Declinagnathodus noduliferus
	321.01	0.708150	Gnathodus postbilineatus
	323.91	0.708048	Gnathodus bollandensis
	326.40	0.707950	Lochria cruciformis
	328.29	0.707862	Lochria nodosa
	330.18	0.707771	Lochria nodosa
	333.02	0.707681	Lochria mononodosa
	337.74	0.707692	Gnathodus billineatus
	342.47	0.707763	Gnathodus texanus
	345.30	0.707844	Gnathodus pseudosemiglaber - Scalliognathus anchoralis
	346.69	0.707891	Gnathodus semiglaber -Polygnathus communis
	348.08	0.707942	Dollimae bouckaerti
	350.86	0.708040	Gnathodus typicus - Siphonodella isosticha
	352.25	0.708091	Siphonodella quadruplicata - upper Patrognathus andersoni
	355.03	0.708170	lower Patrognathus andersoni
	356.84	0.708211	Patrognathus variabilis
	359.20	0.708252	Patrognathus crassus
	363.03	0.708294	Siphonodella praesulcata
	365.32	0.708301	Palmatolepis expansa
	366.09	0.708301	Palmatolepis postera
	367.62	0.708296	Palmatolepis trachytera
	369.91	0.708276	Palmatolepis marginifera
	371.44	0.708255	Palmatolepis rhomboidea
	373.12	0.708227	Palmatolepis crepida
	374.50	0.708197	Palmatolepis triangularis
	376.12	0.708157	Palmatolepis linguiformis
	378.28	0.708088	Palmatolepis rhenana
	379.14	0.708059	Palmatolepis jamieae
	380.33	0.708023	Palmatolepis hassi
	382.28	0.707958	Palmatolepis puactata
	383.14	0.707930	Palmatolepis transitans
	385.30	0.707870	falsiovalis
	386.28	0.707849	norrisi
	387.25	0.707836	Klapperina disparilis
	388.23	0.707831	Schmidtognathus hermanni
	390.83	0.707842	Polygnathus varcus
	391.80	0.707849	hemiansatus
	392.94	0.707861	Polygnathus xylus ensensis
	393.80	0.707873	Tortodus kockelianus
	394.94	0.707893	Tortodus australis
	395.79	0.707910	Polygnathus costatus
	397.50	0.707950	Polygnathus partitus
	398.93	0.707991	Polygnathus patulus
	400.83	0.708065	Polygnathus serotinus
	402.25	0.708132	Polygnathus inversus/ laticostatus
	403.68	0.708209	nothoperbonus
	407.00	0.708397	Polygnathus gronbergi / excavatus, Polygnathus kitabicus
	408.47	0.708480	Polygnathus pireneae
	409.94	0.708563	Eognathodus kindlei
	411.20	0.708627	Eognathodus sulcatus
	412.16	0.708671	Pedavis pesavis
	413.36	0.708716	Ancyrodelloides delta
	416.00	0.708759	Latericriodus woschmidt / postwoschmidti
	417.49	0.708748	Oulodus elegans detortus
	418.70	0.708724	Ozarkodina remscheidensis Interval Zone
	419.09	0.708716	Ozarkodina crispa
	419.74	0.708701	Ozarkodina snajdri
	420.78	0.708648	Polygnathoides siluricus
	421.70	0.708591	Ancoradella ploeckensis
	422.90	0.708515	K. stauros
	424.88	0.708441	Ozarkodina bohemica
	426.50	0.708388	Ozarkodina sagitta sagitta
	427.90	0.708357	Kockelella ranuliformis
	430.18	0.708290	Pterospathodus amorphognathoides
	434.52	0.708208	Pterospathodus celloni
	439.00	0.708108	Pterospathodus tenuis - Distomodus staurognathoides
	443.00	0.707983	Distomodus kentuckyensis
	443.70	0.707959	Rexroadus nathani
	450.19	0.707897	Amorphognathus ordovicicus
	455.29	0.707941	Amorphognathus superbus
	460.14	0.708045	Amorphognathus tvaerensis
	462.34	0.708136	Pygodus anserinus
	463.78	0.708213	Pygodus serra
	464.86	0.708276	Eoplacognathus suecicus
	467.02	0.708420	Eoplacognathus variabilis
	468.66	0.708538	Baltoniodus norrlandicus
	469.40	0.708591	Paroistodus originalis
	470.69	0.708680	Baltoniodus navis
	471.80	0.708750	Baltoniodus triangulatus
	474.52	0.708875	Oepikodus evae
	477.24	0.708920	Prioniodus elegans
	483.45	0.708951	Paroistodus proteus
	484.91	0.708967	Paltodus deltifer
	486.85	0.709009	Cordylodus angulatus
	488.30	0.709050	Iapetognathus fluctivagus
	489.52	0.709093	Codylodus adesei (conodont)
	492.00	0.709169	Lotagnostus americanus
	496.00	0.709203	Agnostotes orientalis, Irvingella
	501.00	0.709167	Glyptagnostus reticulatus
	503.00	0.709127	Lejopyge laevigata
	506.50	0.709047	Acidusus atavus
	510.00	0.708961	Oryctocephalus indicus



Planktonic Foraminifers	:	N,P,Cret Zones	P,E,O,M,PL Zones	Cenozoic subzone	Formal Paleogene zone name	Foram Zone Marker	Other Foram FAD/LAD	Additional Neogene Foram FAD/LAD	All Foram Datums Combined		NEOGENE = Berggren et al. (1995a,b), with revised age calibrations from Lourens et al. (GTS2004 appendix).  PALEOGENE = Berggren et al. (1995a,b) with age updates from Berggren and Pearson (2005).  CRETACEOUS = ODP Leg 171B (citing Erba et al., 1995) and Robaszynski (in Hardenbol et al., SEPM charts, 1998) with partial recalibrations provided by Paul Sikora (EGI)

N,P,Cret Zones	block	80	247/249/153
	TOP	0.00
	N22	2.00
	N20/N21	4.37
	N18/N19	5.72		Pliocene Foram Zone PL1 is Globorotalia tumida/Globoturborotalita nepenthes Concurrent Range Zone = FAD G. tumida to LAD G. nepenthes (Berggren et al., 1995), with 2 subzones.  History of zone and regional events are summarized in Berggren et al. (1995).  Miocene/Pliocene Foram Zone "Pl1a" is the 'Globorotalia tumida/Globorotalia cibaoensis Concurrent Range SubZone' (FAD of Globorotalia tumida to LAD of Globorotalia cibaoensis) (Berggren et al., 1995), and is equivalent to the majority of Zone 'N18' (or 'N19', which now begins BEFORE 'N18') of Blow (1979).  Lourens et al (GTS2004) also place base of "M14" at this level, but Berggren used an earlier event.  There is no major Foram datum to mark the base of the Pliocene.
	N17b	6.58
	N17	8.58		The base of "N17" was defined as the initial evolutionary FAD of Gt. Plesiotumida from its (putative) ancestor Gt. merotumida, but this event is difficult to apply.
	N16	10.57	
	N15	11.47	
	N14	11.63	
	N13	11.79	
	N12	13.41	
	N11	13.77	
	N10	14.24	
	N9	14.74		Miocene Foram Zone "M6" is the 'Globorotalia peripheroronda Partial Range Interval Zone' (FAD of Orb. suturalis to FAD of Globorotalia peripheroacuta) (Berggren et al., 1995), and is equivalent to Zone 'N9' of Blow (1979).  This is a very brief interval the global compilation of datums.  Berggren et al. (1995) used Orbulina "suturalis" (age of 15.09 Ma, based on mid-C5Bn.2n; ref [b] which had 15.1 Ma) to define base of Zone M6, but table in Lourens et al. (GTS2004) uses Orbulina "universa" (and there is no indication of a "suturalis". 
	N8	16.97	
	N7	17.54	
	N6	17.59	
	N5	21.12	
	N4	22.96	
	N3, P22	26.83		Oligocene Foram Zone 'P22' (and 'N3') is defined as the 'Globigerina ciperoensis Partial Range Subzone' (LAD of Parabloborotalia opima opima to FAD of Globorotalia kugleri) by Berggren et al. (1995, SEPM), which is same as Berggren & Miller, 1988.  Note that this is essentially a "gap" zone.
	N2, P21	29.45		Oligocene Foram Zone P21 is the Globigerina angulisuturalis/Paragloborotalia opima opima Concurrent Range Zone (Blow, 1969; Berggren et al., 1995) = FAD to LAD, and is subdivided into 2 subzones.  Subzone 'P21a' (= Zone O4 of Berggren-Pearson '05) is defined as the 'Globigerina angulisuturalis / Chiloguembelina cubensis Concurrent Range Zone' (FAD of G. angul. to LAD of Chil. cubensis) by Berggren et al. (1995, SEPM); which is same as Berggren & Miller (1988).
	N1, P20	30.42		Oligocene Foram Zone "P20" (= Zone O3 of Berggren-Pearson '05) (and "N1") is defined as the 'Globigerina sellii Partial Range Zone' (LAD of '"T." ampliaperatura' to FAD of 'Globigerina angulisuturalis') by Berggren et al. (1995, SEPM), which is same as Berggren & Miller (1988).  Note that this is essentially a "gap" zone.
	P19	32.19		Oligocene Foram Zone 'P19' (= Zone O2 of Berggren-Pearson '04) is defined as the "'Turborotalia' ampliapertura Interval Zone' (LAD of Pseudohastigerina spp. to LAD of 'T.' ampliapertura) by Berggren et al. (1995, SEPM); which is same as Berggren & Miller (1988).  "The historical vicissitudes associated with this zone" are discussed in Berggren & MIller (1988). 
	P18	34.00		Eocene Foram Zone P18 = Turborotalia cerroazulensis-Pseudohastigerina spp. Interval Zone (LAD to LAD) (Berggren et al., 1995). Berggren and Miller (1988) used the HO of 'T. ceroazulensis' (rather than that of 'Hantkenina') to denote the P17/18 boundary because of its greater potential for preservation.  The base is defined by Berggren & Miller (1988) as LAD Turbo. cerroazulensis; rather than LAD Hankenina -- but these are nearly synchronous events.  This zone has undergone numerous changes in definitions (briefly reviewed in Berggren et al., 1995).
	P17	34.16		Eocene Foram Zone P17 is the 'Turborotalia cerroazulensis Interval Zone' (LAD of C. inflata to LAD of T. cerroazulensis) (Berggren et al., 1995).  This is a very brief zone (~0.2 m.y.); and was no longer used by Berggren-Pearson '05 zonation.
	P16	35.26		Eocene Foram Zone P16 is the 'Turborotalia cunialensis/Cribrohantkenina inflata Concurrent Range Zone' (FAD of Turbo. cunialensis to LAD of Crib. inflata) (redefined by Berggren et al., 1995).  Previously, the base was FAD of Crib. inflata; but Berggren et al. changed to the more common and better calibrated Turbo. cunialensis.  Berggren and Pearson (2005) discontinued this P16 Zone and zonal marker due to high diachroneity.
	P15	38.03		Eocene Foram Zone P15 is the 'Porticulasphaera semiinvoluta Interval Zone' (FAD of P. semiinvoluta to FAD of Turborotalia cunialensis) (redefined by Berggren et al., 1995).  Previously, the top of zone was FAD of Crib. inflata (e.g., Blow, 1979), which is less common and poorly calibrated.
	P14	39.36		Eocene Foram Zone P14 (nearly same as E13 of Berggren-Pearson '05) is the 'Truncorotaloides rohri -Morozovella spinulosa Partial Range Zone' (LAD of G. beckmanni to FAD of P. semiinvoluta) (Berggren and Miller, 1988; Berggren et al., 1995).  Therefore, it is essentially a "gap" zone.
	P13	39.80		Eocene Foram Zone P13 (= Zone E12) of Berggren-Pearson '05) is the 'Globigerapsis beckmanni Total Range Zone' (FAD to LAD) (Bolli, 1957; Berggren et al., 1995).
	P12	42.60		Eocene Foram Zone P12 is the 'Morozovella lehneri Partial Range Zone' (LAD of M. aragonensis to FAD of G. beckmanni) (Berggren et al., 1995).  Therefore, it is essentially a "gap" zone.
	P11	45.00		Eocene Foram Zone P11 (= Zone E9 of Berggren-Pearson '05) is the 'Globigerapsis kugleri/Morzovella aragonensis Concurrent Range Zone' (FAD to LAD) (Berggren, 1969, but with complicated history; see redefinition in Berggren et al., 1995).
	P10	48.60		Eocene Foram Zone P10 (= essentially E8 of Berggren-Pearson '05) is the 'Hantkenina nuttalli Interval Zone' (FAD to the FAD of 'Globigerapsis kugleri') (Berggren & Miller, 1988; = Hankenina aragonensis Zone of Bolli, 1957).
	P9	50.30		Eocene Foram Zone P9 (= E7 of Berggren-Pearson '05) is the 'Planorotalites palmerae -Hantkenina nuttalli Interval Zone' (FAD to FAD) (Berggren et al., 1995).
	P8	50.77		Eocene Foram Zone P8 (= essentially E6 of Berggren-Pearson'05) is the Morozovella aragonensis Partial Range Zone = 'gap' between LAD of Moro. formosa formosa to FAD of Planorotalites palmerae (Berggren & Miller, 1988; Berggren et al., 1995).  However, Aubrey et al. (1988, with Berggren as a co-author), places base of P8 at "FAD of Acarinina pentacamerata", and draws this boundary "approximately midway between the boundaries of Zones P6/P7 and P8/P9" (p. 735).  The simultaneous publication of conflicting definitions for base of Zone P8 (both with Berggren as an author, and neither discussing the change) is confusing.
	P7	52.57		Eocene Foram Zone P7 (= essentially E6 of Berggren-Pearson'05) is the 'Morozovella aragonensis/Morozovella formosa formosa Concurrent Range Zone' (Berggren et al., 1995) = FAD of Moro. aragonensis to LAD of Moro. formosa formosa.
	P6b	54.52		Subzone "P6b" of Berggren (1995) scale (= Zone E4 of Berggren-Pearson '05) is same as "P6c" of Berggren & Miller, 1988).  The complete name is "Morozovella formosa formosa/Morozovella lensiformis -Morozovella aragonensis Interval SubZone"; and from simultaneous FAD of Morozovella formosa formosa and/or Moro. lensiformis to FAD of Moro. aragonensis.
	P6a	55.09		Eocene Foram Zone P6 is the Morozovella subbotinae Partial Range Zone (redefined by Berggren et al., 1995) = "gap" from LAD of Morozovella velascoensis to FAD of Moro. aragonensis.  The P5/6a boundary was used in some publications to approx. Paleocene/Eocene boundary.  Near-basal Eocene Foram SubZone "P6a" of new Berggren (1995) scale is same as "P6b" of Berggren & Miller, 1988).  The complete name is "Morozovella velascoensis -Morozovella formosa formosa and/or Morozovella lensiformis Interval SubZone".  Note that this is a "gap" zone between LAD of 'M. velasoensis' and FAD of 'M. formosa formosa/lensiformis'.
	P5	56.67		Paleocene Foram Zone 'P5', as defined by Berggren et al. (1995, SEPM) is the 'Morozovella velascoensis Interval Zone' = LAD of Glob. pseudomenardii to LAD of Moro. velascoensis.  This definition of P5 encompasses the former P5 and P6a zones of Berggren and Miller (1988).
	P4	60.19		Paleocene Foram Zone P4 is the Globanomalina pseudomenardii Total Range Zone  (Bolli, 1957a).  Three subzones are defined by Berggren et al. (1995).  Subzone 'P4a' is defined as the 'Globanomalina pseudomenardii / Acarinina subsphaerica Concurrent Range Zone' by Berggren et al. (1995) = FAD G. pseudomenardii to LAD of A. subsphaerica.  Either Glob. pseudomenardii or  Acar. subsphaerica defines P4a base.
	P3	61.72		Paleocene Foram Zone  P3  is the Morozovella angulata-Globanomalina pseudomenardii Interval Zone = FAD of P. angulata to FAD of G. pseudomenardii (defined in Berggren et al., 1995; emend. of P3 of Berggren and Miller, 1988) with 2 subzones.  Subzone 'P3a' is the 'Morozovella angulata -Muricella albeari Interval Zone' (Berggren et al., 1995).  An earlier version of subzone P3a used the FAD of Igorina pusilla top define the top of subzone, but this FAD is rare and reported to occur at the base of P3 (Berggren et al., 1995).  A working base of the Selandian substage (top of Danian) is the P2/P3 boundary (Berggren et al., 1995).
	P2	62.07		Paleocene Foram Zone 'P2' is the 'Praemurica uncinata -Morozovella angulata Interval Zone' (Berggren et al., 1995) = FAD of P. uncinata to FAD of M. angulata;  equivalent to the same zone of Berggren and Miller (1988).  In general, this brief zone only encompasses 2-3 m in deep sea sites.
	P1	65.15		Paleocene Foram Zone P1 is the Parvularugoglobigerina eugubina-Praemurica uncinata Interval Zone (defined in Berggren et al., 1995; emend. of Berggren and Miller, 1988) from LAD of P. eugubina to FAD of P. uncinata.  Subzone 'P1a' is the 'Parvularugoglobigerina eugubina - Subbotina triloculinoides Interval Subzone' (Berggren et al.,1995), which is an emendation of the former P1a 'Parasubbotina pseudobulloides' subzone of Berggren & Miller (1988), but the range is essentially identical.  Note that this is a "gap" zone (LAD of eugubina to FAD of triloculinoides).
	Pa	65.32		Paleocene Foraminifer Zone P-alpha is the Total Range Zone of "Parvularugoglobigerina eugubina"   [Liu, (1993) emendation of Blow's (1979) "Parvularugoglobigerina eugubina Partial-range Zone"; in turn from Luterbacher & Premoli Silva's (1964) "Globigerina eugubina Zone"; however, Smit (1982) uses "G. eugubina Zone" as "P1a"].  "Estimation of the age and duration of Zones P0 and P-alpha remains fraught with difficulty" (Berggren et al., 1995).
	P0	65.50		Basal Paleocene Planktonic Foraminifer Zone P0 (= Guembelitria cretacea, Partial range zone) is from Keller (1988; emendation of Smit, 1982).  Base = extinction of Rugoglobigerina, Globotruncana, Globotruncanella and associated taxa.  Top = FAD of P. eugubina.  See Berggren et al. (SEPM, 1995) for a page discussing the P0, P-alpha, P1 definition history and problems.  "Estimation of the age and duration of Zones P0 and P-alpha remains fraught with difficulty" (Berggren et al., 1995).
	Abathomphalus mayaroensis	68.36	dashed
	Racemiguembelina fructicosa	69.62	dashed	See NOTE on datum.  This zone may be within the "overlying" one in some regions.
	Gansserina gansseri	72.35
	Globotruncana aegyptiaca	73.27
	Globotruncanella havanensis	74.47		Gap zone (LAD at base; FAD at top); which some zonations extend upward to FAD of G. gansseri as a "Globotruncana falsostuarti Zone"
	Globotruncanita calcarata	75.57
	Globotruncana ventricosa	77.16	dashed
	Globotruncanita elevata	83.53
	Dicarinella asymetrica	84.94		D. asymtrica Zone is also range-zone of the index species.
	Dicarinella concavata	90.79	dashed
	Marginotruncana schneegansi	91.51		Turonian Planktonic Foraminifer zone "M. schneegansi" of Robaszynski's scale appears to be equivalent to "Marginotruncana sigali" foraminifer zone of Caron (1985), which is also begins with the LAD of H. helvetica.  In both cases, the zone is a "gap zone" (LAD at base, FAD at top).  However, the scheme of Caron (1985) has an overlying "Dicarinella primitiva" (base = FAD of D. primitiva), followed by Dicarinella concavata (base = FAD of D. concavata), with the base of D. primitiva approximately at base of Coniacian.  The scheme of Robaszynski places the FAD of D. concavata within the upper Turonian, therefore the D. primitiva zone is eliminated.
	Helvetoglobotruncana helvetica	93.41
	Whiteinella archaeocretacea	93.95		Caron (1985) indicates base of this zone as FAD of W. archaeocretacea, rather than LAD of R. cushmani.
	Rotalipora cushmani	95.33
	Rotalipora reicheli	95.68
	Rotalipora globotruncanoides	99.60
	Rotalipora appenninica	100.94
	Rotalipora ticinensis	102.93
	Rotalipora subticinensis	105.05	dashed
	Ticinella praeticinensis	106.42
	Ticinella primula	110.89
	Hedbergella planispira	112.50		"Gap zone" (LAD at base; FAD at top)
	Ticinella bejaouaensis	114.30
	Hedbergella gorbachikae	116.00
	Globigerinelloides algeriana	119.00
	Globigerinelloides ferreolensis	120.70		"Gap zone" (LAD at base; FAD at top)
	Leupoldina cabri	122.05
	Globigerinelloides blowi	127.88
	Hedbergella similis	129.64
	Hedbergella sigali/delrioensis	136.76
	Globuligerina hoterivica	142.30
	Conoglobigerina gulekhensis	145.46

P,E,O,M,PL Zones	block	50	247/249/153
	TOP	0.00
	Pt1	1.77		Pleistocene Foram Zone Pt1 is the Globigerinoides fistulosus-Globorotalia truncatulinoides Interval Zone = LAD of G. fistulosus to Present, and characterized by G. truncatulinoides (Berggren et al., SEPM, 1995).  Pleistocene Foram Zone "Pt1a" is the 'Globigerinoides fistulosus -Globorotalia tosaensis Interval SubZone' (LAD of Glob. fistulosus to LAD of Glob. tosaensis) (Berggren et al., 1995).  This may be equivalent to the lower part of Zone N23 of Blow (1979); however, the base of N23 boundary is FAD of Globigerina calida calida & Sph. excavata (Blow, 1969), but these datums are not in Beggren's compilations (1985 or 1995).  However, this event probably is just below the LAD of G. fistulosus (Intro. notes to ODP Leg 138 volume, p.28 - Table 6).
	PL6	2.39		Pliocene Foram Zone "Pl6" is the 'Globorotalia miocenica -Globigerinoides fistulosus Interval Zone'  = [LAD of Globorotalia miocenica (in Atlantic) or LAD of Globorotalia pseudomiocenica (in Indo-Pacific)]  to  LAD of Globigerinoides fistulosus (Berggren et al., 1995).  It spans a portion of Zones N21 and N22 of Blow (1979).  The 'N22' concept of Blow (1969) is difficult to apply globally (reviewed in Berggren et al., SEPM, 1995).
	PL5	3.13		Pliocene Foram Zone "Pl5" is the 'Dentoglobigerina altispira -Globorotalia miocenica Interval Zone' = LAD of Dento. altispira to LAD of Globorotalia miocenica (Berggren et al., 1995).  In Indo-Pacific, the top is LAD of Globorotalia pseudomiocenica, which is coeval to G. miocenica.  It spans the majority of Zone N21 of Blow (1979); although definitions for the base of N21 differ: FAD of G. tosaensis, LAD of G. altispira, LAD of S. seminulina.  These have an age range of about 0.3 m.y.
	PL4	3.14		Pliocene Foram Zone "PL4" is the 'Sphaeroidinellopsis seminulina -Dentoglobigerina altispira Interval Zone' = LAD of Sphaeroidinellopsis seminulina to LAD of Dento. altispira (Berggren et al., 1995).  It may span a portion of Zone N21 of Blow (1979).  This interval barely exists -- Berggren et al. (1995) estimated a duration of 30,000 yr; and this scale has about 20,000 yr!  It is essentially equivalent to the lower Kaena polarity subchron (C2An.1r).
	PL3	3.81		Pliocene Foram Zone "Pl3" is the 'Globorotalia margaritae -Sphaeroidinellopsis seminulina Interval Zone' = LAD of Globoturborotalia margaritae to LAD of Sphaerodinellopsis seminulina (Berggren et al., 1995), and is equivalent to the upper portion of Zone 'N20' of Blow (1979).
	PL2	4.37		Pliocene Foram Zone "Pl2" is the 'Globoturborotalita nepenthes -Globorotalia margaritae Interval Zone' = LAD of Globoturborotalita nepenthes to LAD of Gt. margaritae (Berggren et al., 1995), and is equivalent to the lower portion of Zone 'N20' of Blow (1979).
	PL1	5.72		Pliocene Foram Zone PL1 is Globorotalia tumida/Globoturborotalita nepenthes Concurrent Range Zone = FAD G. tumida to LAD G. nepenthes (Berggren et al., 1995), with 2 subzones.  History of zone and regional events are summarized in Berggren et al. (1995).   Miocene/Pliocene Foram Zone "Pl1a" is the 'Globorotalia tumida/Globorotalia cibaoensis Concurrent Range SubZone' (FAD of Globorotalia tumida to LAD of Globorotalia cibaoensis) (Berggren et al., 1995), and is equivalent to the majority of Zone 'N18' (or 'N19', which now begins BEFORE 'N18') of Blow (1979).  Lourens et al (GTS2004) also place base of "M14" at this level, but Berggren used an earlier event.  There is no major Foram datum to mark the base of the Pliocene.
	M14	6.14		Miocene Foram Zone "M14" is the 'Globorotalia lenguaensis -Globorotalia tumida Interval Zone' = LAD of Globorotalia lenguaensis to FAD of Globorotalia tumida (Berggren et al., 1995), and is equivalent to the uppermost part of Zone 'N17' of Blow (1979).  Note that this essentially a "gap" zone.
	M13	10.57		Miocene Foram Zone M13 is the Neogloboquadrina acostaensis/Globorotalia lenguaensis Concurrent Range Zone = FAD N. acostaensis to LAD of G. lenguaensis (Berggren et al., 1995); with 2 subzones.  Miocene Foram Zone "M13a" is the 'Neogloboquadrina acostaensis -Globigerinoides extremus/Globorotalia plesiotumida Interval SubZone' (FAD of Neobloboquadrina acostaensis to FAD of Globig. extremus and/or Globorot.plesiotumida) (Berggren et al., 1995), and is equivalent to Zone 'N16' of Blow (1979).  FAD of Globorotalia plesiotumida is difficult to determine under some conditions.  See extended discussion of subzone M13a/M13b limits in Berggren et al. (1995).
	M12	11.47		Miocene Foram Zone "M12" is the 'Neogloboquadrina mayeri -Neogloboquadrina acostaensis Interval Zone' (LAD of Neogloboquadrina mayeri to FAD of Neobloboquadrina acostaensis) (Berggren et al., 1995), and is equivalent to Zone 'N15' of Blow (1979).  Note that this is essentially a "gap" zone, but is characterized by presence of Globorotalia menardii.
	M11	11.63		Miocene Foram Zone "M11" is the 'Globoturborotalita nepenthes/Neogloboquadrina mayeri Concurrent Range Zone' (FAD of Globoturborotalita nepenthes to LAD of Neogloboquadrina mayeri) (Berggren et al., 1995), and is equivalent to Zone 'N14' of Blow (1979).
	M10	11.79		Miocene Foram Zone "M10" is the 'Globorotalia fohsi robusta -Globoturborotalita nepenthes Interval Zone' (LAD of Globorotalia fohsi robusta/lobata to FAD of Globoturborotalita nepenthes) (Berggren et al., 1995), and is equivalent to upper portion of Zone 'N13' of Blow (1979).  Note that this is essentially a "gap" zone, which may explain its apparent brief extent (0.15 myr) in the global compilation.  However, in some regions, a further subdivision into 2 subzones can be made by Globigerinoides ruber.
	M9b	13.13		Subzone "M9b" is the 'Globorotalia fohsi robusta Total Range Zone' (initial evolutionary appearance of Globorotalia fohsi robusta to its LAD) (Berggren et al., 1995), and is equivalent to uppermost portion of Zone 'N12' and lower 'N13' of Blow (1979).
	M8/M9	13.41		Miocene Foram Zone "M9" is the Globorotalia fohsi lobata-globorotalia fohsi robusta Interval Zone = initial evolutionary appearance of G. fohsi lobata to LAD of its descendant G. fohsi robusta (Berggren et al., 1995).  Base is same as base of N12 of Blow (1969, 1979), and top is probably near mid-N13.  Magnetochronologic calibration of boundaries is based on reinterpretation of magnetostratigraphy in DSDP Hole 563 by Wright and Miller (1992).  Two subzones -- Miocene Foram SubZone "M9a" was the 'Globorotalia fohsi lobata Lineage SubZone' (initial evolutionary appearance of Globorotalia fohsi lobata to evolutionary FAD of its descendent Globorotalia fohsi robusta) (Berggren et al., 1995), and is equivalent to lower portion of Zone 'N12' of Blow (1979).  Miocene Foram Zone "M8" is the 'Globorotalia fohsi s.str. Lineage Zone' ( initial evolutionary appearance of Globorotalia fohsi s.str. to initial evolutionary appearance of Globorotalia fohsi lobata) (Berggren et al., 1995), and is equivalent to Zone 'N11' of Blow (1979).  However, species "lobata" apparently combined with Fohsella "fohsi" in zonal scheme of Lourens et al. (in GTS2004).  This effectively removed the thin "M8" of Berggren et al., 1995.
	M7	14.24		Miocene Foram Zone "M7" is the 'Globorotalia peripheroacuta Lineage Zone' (FAD of Globorotalia peripheroacuta to the initial evolutionary appearance of Globorotalia fohsi s.str.) (Berggren et al., 1995), and is equivalent to Zone 'N10' of Blow (1979).
	M6	14.74		Miocene Foram Zone "M6" is the 'Globorotalia peripheroronda Partial Range Interval Zone' (FAD of Orb. suturalis to FAD of Globorotalia peripheroacuta) (Berggren et al., 1995), and is equivalent to Zone 'N9' of Blow (1979).  This is a very brief interval the global compilation of datums.  Berggren et al. (1995) used Orbulina "suturalis" (age of 15.09 Ma, based on mid-C5Bn.2n; ref [b] which had 15.1 Ma) to define base of Zone M6, but table in Lourens et al. (GTS2004) uses Orbulina "universa" (and there is no indication of a "suturalis". 
	M5	16.97		Miocene Foram Zone M5 is the Praeorbulina sicana-Orbulina suturalis Interval Zone (Berggren et al., 1995), FAD of P. sicana to FAD of O. suturalis; equivalent to Zone "N8" of Blow (1969, 1979.  Two subzones:  Miocene Foram Zone "M5a" is 'Praeorbulina sicana -Praeorbulina glomerosa s.str. Interval Subzone' (FAD of Praeorbulina sicana to FAD of Pr. glomerosa sensu stricto) (Berggren et al., 1995).  This short subzone spans the lowermost part of the 'N8' zone.  The base of this zone is used to denote the base of the Langhian Substage (base of Middle Miocene), although this boundary may be more closely associated with the slightly younger FAD of Praeorbulina glomerosa s.str. (base of Subzone 'M5b'), which would render this substage about 0.3 myr shorter in duration.
	M4	17.54		Miocene Foram Zone "M4" is Catapsydrax dissimilis-Praeorbulina sicana Interval Zone (Berggren et al., 1995); equivalent to N7 of Blow (1969, 1979), and defined as LAD of C. dissimilis and/or C. unicavus to FAD of P. sicana; with 2 subzones.  Note that this is essentially a "gap" zone of 1 myr.  Miocene Foram Zone "M4a" is 'Catapsydrax dissimilis -Globorotalia birnageae Interval SubZone" (LAD of Catapsydrax dissimilis or Cat. unicavus to FAD of Globorotalia birnageae) (Berggren et al., 1995).  This subzone spans the lower part of the 'N7' zone.  Subzone "M4b" is 'Globigerinoides bisphericus Partial Range Zone' (FAD of Globorotalia birnageae to FAD of Praeorbulina sicana) (Berggren et al., 1995).  This short subzone spans the upper part of the 'N7' zone; but now is within the "overlying" M5!
	M3	17.59		Miocene Foram Zone "M3" is 'Globigerinatella insueta/Catapsydrax dissimilis Concurrent Range Zone' (FAD of Globigerinatella insueta to LAD of Catapsydrax dissimilis or Cat. unicavus) (Berggren et al., 1995).  This is equivalent to the 'N6' zone.
	M2	21.12		Miocene Foram Zone "M2" is 'Catapsydrax dissimilis Partial Range Zone' (LAD of Globorotalia kugleri to FAD of Globigerinatella insueta) (Berggren et al., 1995).  This is equivalent to the 'N5' zone.  Note that this 3 m.y. zone is essentially a "gap" zone.
	M1	22.96		Miocene Foram Zone "M1" is the Globorotalia kugleri Total Range Zone (Berggren et al., 1983), defined by total range of G. kugleri; with 2 subzones.  Miocene Foram Zone "M1a" is 'Globigerinoides primordius Interval Subzone" (FAD of Globorotalia kugleri to FAD of Globoquadrina dehiscens) (Berggren et al., 1995).  This is approximately coeval to the 'N4a' subzone of Srinivasan & Kennett (1981).
	O6	26.83		Oligocene Foram Zone 'P22' (and 'N3') is defined as the 'Globigerina ciperoensis Partial Range Subzone' (LAD of Parabloborotalia opima opima to FAD of Globorotalia kugleri) by Berggren et al. (1995, SEPM), which is same as Berggren & Miller, 1988.  Note that this is essentially a "gap" zone.
	O5	28.45		Oligocene Foram Zone 'P21b' [= Zone O5 of Beggren-Pearson '05) is defined as the 'Globigerina angulisuturalis -Paragloborotalia opima opima Interval Subzone' (LAD/LCO of Chiloguembelina cubensis to LAD of Para. opima) by Berggren et al. (1995, SEPM), which is same as Berggren & Miller, 1988.  The base is at LAD of 'Chiloguembelina cubensis' (Berggren & Miller, 1988), however, Berggren (1995, SEPM) indicates the zonal boundary at "last common occurrence"(which he calls the "virtual LAD" instead of extinction of this taxon.
	O4	29.45		Oligocene Foram Zone P21 is the Globigerina angulisuturalis/Paragloborotalia opima opima Concurrent Range Zone (Blow, 1969; Berggren et al., 1995) = FAD to LAD, and is subdivided into 2 subzones.  Subzone 'P21a' (= Zone O4 of Berggren-Pearson '05) is defined as the 'Globigerina angulisuturalis / Chiloguembelina cubensis Concurrent Range Zone' (FAD of G. angul. to LAD of Chil. cubensis) by Berggren et al. (1995, SEPM); which is same as Berggren & Miller (1988).
	O3	30.42		Oligocene Foram Zone "P20" (= Zone O3 of Berggren-Pearson '05) (and "N1") is defined as the 'Globigerina sellii Partial Range Zone' (LAD of '"T." ampliaperatura' to FAD of 'Globigerina angulisuturalis') by Berggren et al. (1995, SEPM), which is same as Berggren & Miller (1988).  Note that this is essentially a "gap" zone.
	O2	32.19		Oligocene Foram Zone 'P19' (= Zone O2 of Berggren-Pearson '04) is defined as the "'Turborotalia' ampliapertura Interval Zone' (LAD of Pseudohastigerina spp. to LAD of 'T.' ampliapertura) by Berggren et al. (1995, SEPM); which is same as Berggren & Miller (1988).  "The historical vicissitudes associated with this zone" are discussed in Berggren & MIller (1988). 
	O1	33.88		Basal LAD = Definition of Eocene/Olig boundary
	E16	34.47
	E15	35.82
	E14	37.67
	E13	39.36		Eocene Foram Zone P14 (nearly same as E13 of Berggren-Pearson '05) is the 'Truncorotaloides rohri -Morozovella spinulosa Partial Range Zone' (LAD of G. beckmanni to FAD of P. semiinvoluta) (Berggren and Miller, 1988; Berggren et al., 1995).  Therefore, it is essentially a "gap" zone.
	E12	39.80		Eocene Foram Zone P13 (= Zone E12) of Berggren-Pearson '05) is the 'Globigerapsis beckmanni Total Range Zone' (FAD to LAD) (Bolli, 1957; Berggren et al., 1995).
	E11	41.36
	E10	42.60		Eocene Foram Zone P12 is the 'Morozovella lehneri Partial Range Zone' (LAD of M. aragonensis to FAD of G. beckmanni) (Berggren et al., 1995).  Therefore, it is essentially a "gap" zone.
	E9	45.00		Eocene Foram Zone P11 (= Zone E9 of Berggren-Pearson '05) is the 'Globigerapsis kugleri/Morzovella aragonensis Concurrent Range Zone' (FAD to LAD) (Berggren, 1969, but with complicated history; see redefinition in Berggren et al., 1995).
	E8	48.60		Eocene Foram Zone P10 (= essentially E8 of Berggren-Pearson '05) is the 'Hantkenina nuttalli Interval Zone' (FAD to the FAD of 'Globigerapsis kugleri') (Berggren & Miller, 1988; = Hankenina aragonensis Zone of Bolli, 1957).
	E7	50.30		Eocene Foram Zone P9 (= E7 of Berggren-Pearson '05) is the 'Planorotalites palmerae -Hantkenina nuttalli Interval Zone' (FAD to FAD) (Berggren et al., 1995).
	E6	50.77		Eocene Foram Zone P8 (= essentially E6 of Berggren-Pearson'05) is the Morozovella aragonensis Partial Range Zone = 'gap' between LAD of Moro. formosa formosa to FAD of Planorotalites palmerae (Berggren & Miller, 1988; Berggren et al., 1995).  However, Aubrey et al. (1988, with Berggren as a co-author), places base of P8 at "FAD of Acarinina pentacamerata", and draws this boundary "approximately midway between the boundaries of Zones P6/P7 and P8/P9" (p. 735).  The simultaneous publication of conflicting definitions for base of Zone P8 (both with Berggren as an author, and neither discussing the change) is confusing.
	E5	52.57		Eocene Foram Zone P7 (= essentially E6 of Berggren-Pearson'05) is the 'Morozovella aragonensis/Morozovella formosa formosa Concurrent Range Zone' (Berggren et al., 1995) = FAD of Moro. aragonensis to LAD of Moro. formosa formosa.
	E4	54.52		Subzone "P6b" of Berggren (1995) scale (= Zone E4 of Berggren-Pearson '05) is same as "P6c" of Berggren & Miller, 1988).  The complete name is "Morozovella formosa formosa/Morozovella lensiformis -Morozovella aragonensis Interval SubZone"; and from simultaneous FAD of Morozovella formosa formosa and/or Moro. lensiformis to FAD of Moro. aragonensis.
	E3	55.09		Eocene Foram Zone P6 is the Morozovella subbotinae Partial Range Zone (redefined by Berggren et al., 1995) = "gap" from LAD of Morozovella velascoensis to FAD of Moro. aragonensis.  The P5/6a boundary was used in some publications to approx. Paleocene/Eocene boundary.  Near-basal Eocene Foram SubZone "P6a" of new Berggren (1995) scale is same as "P6b" of Berggren & Miller, 1988).  The complete name is "Morozovella velascoensis -Morozovella formosa formosa and/or Morozovella lensiformis Interval SubZone".  Note that this is a "gap" zone between LAD of 'M. velasoensis' and FAD of 'M. formosa formosa/lensiformis'.
	E2	55.58
	E1	55.73		Zone E1 and E2 of Berggren-Pearson '05 is attempt to find some events at P/E thermal excursion.  However, the marker species for base of E1 and E2 are rarely noted in previous studies; therefore, usage of these zones may be limited.
	P5	56.67		Paleocene Foram Zone 'P5', as defined by Berggren et al. (1995, SEPM) is the 'Morozovella velascoensis Interval Zone' = LAD of Glob. pseudomenardii to LAD of Moro. velascoensis.  This definition of P5 encompasses the former P5 and P6a zones of Berggren and Miller (1988).
	P4	60.19		Paleocene Foram Zone P4 is the Globanomalina pseudomenardii Total Range Zone  (Bolli, 1957a).  Three subzones are defined by Berggren et al. (1995).  Subzone 'P4a' is defined as the 'Globanomalina pseudomenardii / Acarinina subsphaerica Concurrent Range Zone' by Berggren et al. (1995) = FAD G. pseudomenardii to LAD of A. subsphaerica.  Either Glob. pseudomenardii or  Acar. subsphaerica defines P4a base.
	P3	61.72		Paleocene Foram Zone  P3  is the Morozovella angulata-Globanomalina pseudomenardii Interval Zone = FAD of P. angulata to FAD of G. pseudomenardii (defined in Berggren et al., 1995; emend. of P3 of Berggren and Miller, 1988) with 2 subzones.  Subzone 'P3a' is the 'Morozovella angulata -Muricella albeari Interval Zone' (Berggren et al., 1995).  An earlier version of subzone P3a used the FAD of Igorina pusilla top define the top of subzone, but this FAD is rare and reported to occur at the base of P3 (Berggren et al., 1995).  A working base of the Selandian substage (top of Danian) is the P2/P3 boundary (Berggren et al., 1995).
	P2	62.07		Paleocene Foram Zone 'P2' is the 'Praemurica uncinata -Morozovella angulata Interval Zone' (Berggren et al., 1995) = FAD of P. uncinata to FAD of M. angulata;  equivalent to the same zone of Berggren and Miller (1988).  In general, this brief zone only encompasses 2-3 m in deep sea sites.
	P1	65.15		Paleocene Foram Zone P1 is the Parvularugoglobigerina eugubina-Praemurica uncinata Interval Zone (defined in Berggren et al., 1995; emend. of Berggren and Miller, 1988) from LAD of P. eugubina to FAD of P. uncinata.  Subzone 'P1a' is the 'Parvularugoglobigerina eugubina - Subbotina triloculinoides Interval Subzone' (Berggren et al.,1995), which is an emendation of the former P1a 'Parasubbotina pseudobulloides' subzone of Berggren & Miller (1988), but the range is essentially identical.  Note that this is a "gap" zone (LAD of eugubina to FAD of triloculinoides).
	Pa	65.32		Paleocene Foraminifer Zone P-alpha is the Total Range Zone of "Parvularugoglobigerina eugubina"   [Liu, (1993) emendation of Blow's (1979) "Parvularugoglobigerina eugubina Partial-range Zone"; in turn from Luterbacher & Premoli Silva's (1964) "Globigerina eugubina Zone"; however, Smit (1982) uses "G. eugubina Zone" as "P1a"].  "Estimation of the age and duration of Zones P0 and P-alpha remains fraught with difficulty" (Berggren et al., 1995).
	P0	65.50		Basal Paleocene Planktonic Foraminifer Zone P0 (= Guembelitria cretacea, Partial range zone) is from Keller (1988; emendation of Smit, 1982).  Base = extinction of Rugoglobigerina, Globotruncana, Globotruncanella and associated taxa.  Top = FAD of P. eugubina.  See Berggren et al. (SEPM, 1995) for a page discussing the P0, P-alpha, P1 definition history and problems.  "Estimation of the age and duration of Zones P0 and P-alpha remains fraught with difficulty" (Berggren et al., 1995).

Cenozoic subzone	block	30	247/249/153	notitle	off
	TOP	0.00
	b	0.61		Subzone "Pt1b" is the 'Globorotalia truncatulinoides Partial Range SubZone' (LAD of Glob. toasaensis to present) (Berggren et al., 1995).  This is equivalent to the upper part of Zone N23 of Blow (1979).
	a	1.77		Pleistocene Foram Zone Pt1 is the Globigerinoides fistulosus-Globorotalia truncatulinoides Interval Zone = LAD of G. fistulosus to Present, and characterized by G. truncatulinoides (Berggren et al., SEPM, 1995).  Pleistocene Foram Zone "Pt1a" is the 'Globigerinoides fistulosus -Globorotalia tosaensis Interval SubZone' (LAD of Glob. fistulosus to LAD of Glob. tosaensis) (Berggren et al., 1995).  This may be equivalent to the lower part of Zone N23 of Blow (1979); however, the base of N23 boundary is FAD of Globigerina calida calida & Sph. excavata (Blow, 1969), but these datums are not in Beggren's compilations (1985 or 1995).  However, this event probably is just below the LAD of G. fistulosus (Intro. notes to ODP Leg 138 volume, p.28 - Table 6).
	TOP	4.37
	b	4.52		Subzone "PL 1b" is the 'Globorotalia cibaoensis -Globoturborotalita nepenthes Interval SubZone' = LAD of Globorotalia cibaoensis to LAD of Globoturborotalita nepenthes (Berggren et al., 1995), and is equivalent to the upper Zone 'N18' of Blow (1979).  In low latitudes, the LAD of G. cibaoensis is concomitant with the FAD of Globorotalia puncticulata.  Therefore, since Berggren et al (GSA Bull., 1995) did not list G. cibaoensis, I have used the later equivalence.
	a	5.72		Pliocene Foram Zone PL1 is Globorotalia tumida/Globoturborotalita nepenthes Concurrent Range Zone = FAD G. tumida to LAD G. nepenthes (Berggren et al., 1995), with 2 subzones.  History of zone and regional events are summarized in Berggren et al. (1995).   Miocene/Pliocene Foram Zone "Pl1a" is the 'Globorotalia tumida/Globorotalia cibaoensis Concurrent Range SubZone' (FAD of Globorotalia tumida to LAD of Globorotalia cibaoensis) (Berggren et al., 1995), and is equivalent to the majority of Zone 'N18' (or 'N19', which now begins BEFORE 'N18') of Blow (1979).  Lourens et al (GTS2004) also place base of "M14" at this level, but Berggren used an earlier event.  There is no major Foram datum to mark the base of the Pliocene.
	TOP	6.14
	b	8.93		Subzone "M13b" is the 'Globigerinoides extremus/Globorotalia plesiotumida -Globorotalia lenguaensis Interval SubZone' (FAD of Globig. extremus/Globorot.plesiotumida to LAD of Globorotalia lenguaensis) (Berggren et al., 1995), and is equivalent to the majority of Zone 'N17' of Blow (1969).  M13b base defined either by:  Glob. plesiotumida or Neo. humerosa. The base of "N17" was defined as the initial evolutionary FAD of Gt. Plesiotumida from its (putative) ancestor Gt. merotumida, but this event is difficult to apply.
	a	10.57		Miocene Foram Zone M13 is the Neogloboquadrina acostaensis/Globorotalia lenguaensis Concurrent Range Zone = FAD N. acostaensis to LAD of G. lenguaensis (Berggren et al., 1995); with 2 subzones.  Miocene Foram Zone "M13a" is the 'Neogloboquadrina acostaensis -Globigerinoides extremus/Globorotalia plesiotumida Interval SubZone' (FAD of Neobloboquadrina acostaensis to FAD of Globig. extremus and/or Globorot.plesiotumida) (Berggren et al., 1995), and is equivalent to Zone 'N16' of Blow (1979).  FAD of Globorotalia plesiotumida is difficult to determine under some conditions.  See extended discussion of subzone M13a/M13b limits in Berggren et al. (1995).
	TOP	14.74
	b	16.27		Subzone "M5b" is the 'Praeorbulina glomerosa s.str. -Orbulina suturalis Interval SubZone' (FAD of Prae. glomerosa s.str. to LAD of Orb. suturalis) (Berggren et al., 1995), and is equivalent to the middle and upper part of Zone 'N8' of Blow (1979).
	a	16.97		Miocene Foram Zone M5 is the Praeorbulina sicana-Orbulina suturalis Interval Zone (Berggren et al., 1995), FAD of P. sicana to FAD of O. suturalis; equivalent to Zone "N8" of Blow (1969, 1979.  Two subzones:  Miocene Foram Zone "M5a" is 'Praeorbulina sicana -Praeorbulina glomerosa s.str. Interval Subzone' (FAD of Praeorbulina sicana to FAD of Pr. glomerosa sensu stricto) (Berggren et al., 1995).  This short subzone spans the lowermost part of the 'N8' zone.  The base of this zone is used to denote the base of the Langhian Substage (base of Middle Miocene), although this boundary may be more closely associated with the slightly younger FAD of Praeorbulina glomerosa s.str. (base of Subzone 'M5b'), which would render this substage about 0.3 myr shorter in duration.
	TOP	21.12
	b	22.38		Subzone "M1b" is 'Globorotalia kugleri/Globoquadrina dehiscens Concurrent Range Subzone' (FAD of Globoquadrina dehiscens to LAD of Globorotalia kugleri) (Berggren et al., 1995).  This is equivalent to the 'N4b' subzone of Srinivasan & Kennett (1981).
	a	22.96		Miocene Foram Zone "M1" is the Globorotalia kugleri Total Range Zone (Berggren et al., 1983), defined by total range of G. kugleri; with 2 subzones.  Miocene Foram Zone "M1a" is 'Globigerinoides primordius Interval Subzone" (FAD of Globorotalia kugleri to FAD of Globoquadrina dehiscens) (Berggren et al., 1995).  This is approximately coeval to the 'N4a' subzone of Srinivasan & Kennett (1981).
	TOP	56.67
	c	57.30		Foram SubZone 'P4c' is defined as the 'Acarinina soldadoensis -Globanomalina pseudomenardii Concurrent range Zone' by Berggren et al. (1995); and encompasses the "Zone P5" as originally defined by Blow (1979).
	b	59.99		This is NEW version of SubZone P4b (Berggren et al, 2000).  Previously, Berggren et al. (1995) version of Paleocene Foram Subzone 'P4b' had been defined as the 'Acarinina subsphaerica -Acarinina soldadoensis Interval Zone' -- 'gap' between LAD of 'Acar. subsphaerica' and FAD of 'Acar. soldadoensis'.
	a	60.19		Paleocene Foram Zone P4 is the Globanomalina pseudomenardii Total Range Zone  (Bolli, 1957a).  Three subzones are defined by Berggren et al. (1995).  Subzone 'P4a' is defined as the 'Globanomalina pseudomenardii / Acarinina subsphaerica Concurrent Range Zone' by Berggren et al. (1995) = FAD G. pseudomenardii to LAD of A. subsphaerica.  Either Glob. pseudomenardii or  Acar. subsphaerica defines P4a base.
	b	60.78		Paleocene Foram Zone 'P3b' is redefined as the 'Muricella albeari -Globanomalina pseudomenardii Interval Zone' (Berggren et al., 1995).  Paleocene foram 'Igorina albeari (=Muricella albeari = Globorotalia laevigata)' FAD defines the base of Zone P3b of Berggren et al. (1995, SEPM); which is NOT the P3b of Berggren & Miller (1988) defined by FAD of Igorina pusilla.  Paleocene Foram SubZone P3b was defined as FAD of 'Igorina pusilla' ('Muricella pusilla' in Berggren et al., 1995) in Berggren & Miller (1988).  However, 'Mur. pusilla' has been observed to occur with the FAD of 'Moro. angulata' (base of SubZone P3a), therefore Berggren et al. (1995, SEPM) redefined the SubZone P3b as the FAD of Muricella albeari, which is about 1 myr higher.
	a	61.72		Paleocene Foram Zone P3 is the Morozovella angulata-Globanomalina pseudomenardii Interval Zone = FAD of P. angulata to FAD of G. pseudomenardii (defined in Berggren et al., 1995; emend. of P3 of Berggren and Miller, 1988) with 2 subzones.  Subzone 'P3a' is the 'Morozovella angulata -Muricella albeari Interval Zone' (Berggren et al., 1995).  An earlier version of subzone P3a used the FAD of Igorina pusilla top define the top of subzone, but this FAD is rare and reported to occur at the base of P3 (Berggren et al., 1995).  A working base of the Selandian substage (top of Danian) is the P2/P3 boundary (Berggren et al., 1995).
	TOP	62.07
	c	63.44		Paleocene Foram Zone 'P1c' is the 'Globanomalina compressa/Praemurica inconstans -Praemurica uncinata Interval Subzone' (Berggren et al., 1995).  The base is defined by the FAD of either 'Globan. compressa' or 'Prae. inconstans'.
	b	64.71		Paleocene Foram Zone 'P1b' is the 'Subbotina triloculinoides -Globanomalina compressa/Praemurica inconstans Interval Subzone' (Berggren et al.,1995; emend. Berggren and Miller, 1988) from FAD of S. triloculinoides to FAD's of G. compressa and/or P. inconstans.
	a	65.15		Paleocene Foram Zone P1 is the Parvularugoglobigerina eugubina-Praemurica uncinata Interval Zone (defined in Berggren et al., 1995; emend. of Berggren and Miller, 1988) from LAD of P. eugubina to FAD of P. uncinata.  Subzone 'P1a' is the 'Parvularugoglobigerina eugubina - Subbotina triloculinoides Interval Subzone' (Berggren et al.,1995), which is an emendation of the former P1a 'Parasubbotina pseudobulloides' subzone of Berggren & Miller (1988), but the range is essentially identical.  Note that this is a "gap" zone (LAD of eugubina to FAD of triloculinoides).

Formal Paleogene zone name	block	120	247/249/153	notitle	off
	TOP	22.96
	Globigerina ciperoensis PRZ	26.83
	Paragloborotalia opima HOZ	28.45
	Globigerina angulisuturalis / Chiloguembelina cubensis CRZ	29.45
	Globigerina sellii PRZ	30.42
	Turborotalia ampliapertura HOZ	32.19
	Pseudohastigenrina naguewichiensis HOZ	33.88
	Hankenina alabamensis HOZ	34.47
	Globigerinatheka index HOZ	35.82
	Globigerinatheka semiinvoluta HOZ	37.67
	Morozovella crassata HOZ	39.36
	Orbulinoides beckmanni TRZ	39.80
	Morozovella lehneri PRZ	41.36
	Acarinina topilensis PRZ	42.60
	Globigerinatheka kugleri / Morozovella aragonensis CRZ	45.00
	Guembelitrioides nuttalli LOZ	48.60
	Acarinina cuneicamerata LOZ	50.30
	Acarinina pentacamerata PRZ	50.77
	Morozovella aragonensis / Morozovella subbotinae CRZ	52.57
	Morozovella  formosa LOZ	54.52
	Marozovella marginodentata PZZ	55.09
	Pseudohastigerina wilcoxensis / Morozovella velascoensis CRZ	55.58
	Acarinina sibaiyaensis LOZ	55.73
	Morozovella velascoensis PRZ	56.67
	Acarinina soldadoensis / Globanomalina pseudomenardii CRSZ	57.30
	Acarinina subsphaerica PRSZ	59.99
	Globoanomalina pseudomenardii TRZ (Glob. pseudomenardii / Parasubbotina variospira CRSZ)	60.19
	Igorina albeari LOSZ	60.78
	Morozovella angulata LOZ (Igorina pusilla PRSZ)	61.72
	Praemurica uncinata LOZ	62.07
	Globanomalina compressa / Praemurica inconstans LOSZ	63.44
	Subbotina triloculinoides LOSZ	64.71
	Eoglobigerina edita PRZ (Parasubbotina pseudobulloides PRSZ)	65.15
	Parvularugoglobigerina eugubina TRZ	65.32
	Guembelitria cretacea PRZ	65.50

Foram Zone Marker	event		241/244/181		off
LAD
	Globorotalia tosaensis	0.61		Base Pt1b (Top Pt1a).  Astronomically tuned from ODP Legs 111 & 138. = Refs 1 & 2; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had assigned as early Brunhes ; 0.65 Ma ; [a,e] = C1n.165; and noted that Pleistocene Foram Globorotalia tosaensis LAD is placed earlier, at Latest Brunhes-Jaramillo (0.8-1.0 Ma) by Caproniere et al. (1994).
	Globigerinoides fistulosus	1.77		Base Pt1a (Top PL6).  Astronomically tuned from ODP Legs 111 & 138 (Pacific); but LAD occurs earlier (1.88 Ma) at Atlantic Sites 925 & 926 -- Refs 3 & 4; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had assigned as just above Olduvai; 1.6 Ma [a] = C1r.3r.3
	Menardella (Globorotalia) miocenica (Atl.), Globorotalia pseudomiocenica (Indo-Pac)	2.39		Dual markers for Base of PL6 [or, due to LADs, the top of PL5.  (Atlantic reappearance of Pulleniatina near this level [ref. a]).  Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Essentially same as Berggren et al (1995), who assigned to early Matuyama (below Reunion Subchron); 2.30 Ma [a] =C2r.3r.8. 
	Dentoglobigerina altispira	3.13		Base PL5 (or, due to LAD, top of PL4; and alternate for top of N20 -- see comments on PL5 Zone).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  This LAD is reported as slightly earlier (3.19 Ma) in eastern Medit. (Refs 17, 22, 23) and much earlier (3.47 Ma) at Pacific ODP Legs 111 and 138 (Refs 1, 2, 5, 6) -- GTS2004 Neogene foram table.  Berggren et al. (1995) had similar assignment -- C2An.1r (Kaena); 3.09 Ma [a] ; {But 0.08 myr earlier in Medit. in late Mammoth, early Kaena; or about 3.17 Ma; ref. c,k).}, or a calibration of about C2Ar.1r.3.
	Sphaeroidinellopsis seminulina	3.14		Base PL4 (or, due to LAD, then top of PL3, and alternate for top of Zone N20).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  This LAD is reported as slightly earlier (3.17 Ma) in eastern Medit. (Refs 17, 22, 23) and much earlier (3.59 Ma) at Pacific ODP Legs 111 and 138 (Refs 1, 2, 5, 6) -- GTS2004 Neogene foram table.  Berggren et al. (1995) assigned as base Kaena; 3.12 Ma [b] = C2An.1r.0; and noted that Pliocene foram 'Sphaeroidinellopsis seminulina' LAD occurs about 0.1 m.y. earlier (top of Mammoth, or 3.21 Ma) in Mediterranean (refs. c,e,f,k).   NOTE that calibrations imply NO DURATION of Zone PL4 in Atlantic; and extremely brief (but earlier) elsewhere.  To avoid confusion on graphics, the base of PL4 has been lowered by 0.01 myr (3.14 Ma, instead of 3.13 Ma in Lourens et al., 2004 compilation).
	Hirsutella (Globorotalia) margaritae	3.81		Defines top of PL2; (was approx. base of Piacenzian stage in Berggren et al., 1995).  Cycle-calibrated in Eastern Mediterranean -- Refs 17, 23 & 24; in GTS2004 Neogene foraminifer appendix.  This LAD is reported slightly earlier (3.85 Ma) at Atlantic Sites 95 & 926 (Refs. 8-10) in GTS2004 Neogene foram table.  Berggren et al. (1995) assigned as Gauss/Gilbert boundary; 3.58 Ma [a,o] = Base C2An.3n.  They noted that Pliocene foram 'Globorotalia margaritae' LAD is reported to occur 0.2 m.y. earlier (late Gilbert, or 3.79 Ma) in Mediterranean (refs. c,f,g,k).  The LCO occurs in the Mediterranean just above Cochiti Subchron (3.96 Ma) [ref. c,k]. 
	Globoturborotalita nepenthes	4.37		Base PL2 (or, due to LAD, Defines top of PL1; & N19/N20 boundary.).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as top Cochiti Subchron; 4.20 Ma [a] = C3n.1n.8.
	Globoquadrina dehiscens	5.91		Same chron-age calibration as Berggren et al. (1995) = C3r (early Gilbert); 5.8 Ma [a-d] = C3r.15 [Datum levels in C3r scaled proportionally to match Berggren's relative spacing. ].   Miocene foram 'Globoquadrina dehiscens' LAD is calibrated in ODP Hole 588 in SW Pacific, and is synchronous in nearby Holes 586B,587,590 and in Indian Ocean (ref. c).  However, Berggren (1994 version of SEPM compilation) indicated that this LAD is apparently diachronous by about 1 myr from 3CBn (6.8 Ma) in subtropics to C3n.4r (5.5 Ma) in tropics (ref. a).   Miocene/Pliocene boundary interval Foram Zone "N18" is essentially non-existent in Berggren's table and GTS2004, because its base (FAD G. tumida) is now AFTER the base of N19 (FAD Sphaeroidinella dehiscens).
	Globorotalia lenguaensis (Atl. only)	8.97		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  See NOTE above for Pacific LAD of ~6.14 Ma.
	Neogloboquadrina mayeri	11.47		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina mayeri' LAD is in the lower part of Buff Bay Formation at Buff Bay, Jamaica, 8 cm above FAD of 'Discoaster hamatus' (Berggren, 1993; Aubry, 1993).  In Bodjonegoro 1 borehole (Indonesia) these two datum levels occur together (personal observation, W. Berggren & M. Aubry). In North Atlantic Sites 558, 563 (ref. b) and 608 (ref. l) LAD of 'N. mayeri' was observed in close juxtaposition with FAD of 'N. acostaensis', essentially eliminating Foraminifer Zone N15 (=M12).  This has been varyingly interpreted as due to a hiatus in the North Atlantic (Aubry, 1993) or diachrony (ref. l,m).  Therefore, their assignment is C5r.2r; 11.4 Ma [b,l-n] = C5r.2r.2.  This LAD also defined their Base of Medit. zone Mt9.
	Fohsella fohsi s.l.	11.79		Formerly called 'Globororotalia fohsi robusta'.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globorotalia fohsi robusta' LAD is calibrated in Hole 563 (ref. b) = C5An.1n; 11.9 Ma [b] = top C5An.1n.
	Praeorbulina  sicana	14.53		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C5B.1n; 14.8 Ma [b] = base C5ADr.
	Catapsydrax dissimilis	17.54		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) calibrate Miocene foram 'Catapsydrax dissimilis' LAD as recorded in Holes 558, 563, North Atlantic (ref. b); and observed at top of polarity zone C5Dr in Hole 608 in interval of strong dissolution (refs. k,p) = C5Dn (upper); 17.3 Ma [p] or 18.3 [u] = C5Dn.9.
	Paragloborotalia kugleri	21.12		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) use this level as base of Medit. Zone Mt2, and note that Miocene foram 'Paragloborotalia (formerly Globorotalia) kugleri' LAD is recorded in Hole 516F, South Atlantic (ref. b), and at base of polarity zone C6An in Contessa Highway section (ref. q) = C6Ar; 21.5 Ma [b,q] = C6Ar.6.
	Globigerina euapertura	23.03		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerina euapertura' LAD is recorded near top of polarity chron C6Cn in Hole 748B and near base C6Cn in Holes 747A and 747B (ref. b) = C6Cn.2n; 23.8 Ma [b] = base C6Cn.2n.
	Paragloborotalia opima	26.83		Oligocene foram 'Paragloborotalia opima opima' (Berggren & Miller, 1988) defines top of P21.  This was called "G. opima opima" by Blow (1969), and is listed as only "P. opima" in Berggren 1995, SEPM). Same chron-age calibration as Berggren et al. (1995) -- The LAD is recorded between polarity zones C9n and C8n in Hole 516F (ref. a); individuals become significantly smaller above C9n and are not typical of 'P. opima s.s.' in Hole 558 (ref. 1; see also discussion in Berggren and Miller, 1988) = C9n (upper); 27.1 Ma [a] = C9n.9.
	Chiloguembelina cubensis (LCO)	28.45		Last Common Occurrence used to set age of Base-Chattian on SEPM chart and GTS2004.  Set equivalent to base of Chron C10n.1n.  Calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- This LAD is recorded in mid-part of polarity zone C10n in Holes 747A (ref. a,e) 749 (ref. 2), in the mid-part of concatenated C9n and C10n in Hole 748B (ref. b), and associated approximately with C10n in Holes 689B and 690B (ref. d).  Whether this datum refers to extinction or strong reduction in numbers remains a moot point; records of discontinuouss presence in reduced numbers of this taxon into basal Miocene levels continue (ref. c) (Berggren et al., 1995).  Assigned as C10n (mid); 28.5 Ma [a,b,e] = 
	Turborotalia ampliapertura	30.42		Oligocene foram 'Turborotalia ampliapertura' defines top of P19, and was formerly 'Globigerina ampliapertura' (e.g., Blow, 1969).  Age-calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- LAD is recorded in polarity zone C11r in Holes 516F and 558 (ref. a) and St. Stephen's Quarry, Alabama borehole (ref. d) = C11r; 30.3 Ma [a,f] = C11r.5.
	Pseudohastigerina naguewichiensis	32.19		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Oligocene foram 'Pseudohastigerina spp.' LAD defines top of P18, and is recorded in Holes 516F, 558, 563 (ref. a) and St. Stephen's Quarry, Alabama borehole (ref. f).   Earliest Oligocene foraminifer LAD of Psudohastigerina datum was noted as "C11r" in Berggren tables, but it seems to be a typographic error, because his age placement and chronologic order of this datum was at "32.0 Ma", hence in C12r.  Assignment is C12r; 32.0 Ma [a,f] = C12r.5.
	Hantkenina spp., Hantkenina alabamensis	33.88		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- the youngest of 3 normal "events" in polarity chron C13r in Contessa Highway section (refs. b,c) and above the normal "event" C13n.2n at Massignano (ref. d), where this LAD defines the Eocene/Oligocene boundary, and is dated radiometrically as 33.7 Ma.  Chron calibration = C13r; 33.7 Ma [a-d] = C13r.85.
	Turborotalia cerroazulensis	34.00		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia cerroazulensis" LAD defines top of P17, and is associated with youngest of 3 normal "events" in polarity chron C13r in Contessa Section (ref. b,c) and above normal "event" C13n.2n at Massignano (ref. d).  It is not absolutely clear whether the LAD of 'Hantkenina spp.' and 'T. cerroazulensis' group are synchronous or sequential.  Chron calilbration = C13r; 33.8 Ma [a-d] = C13r.75.
	Cribrohantkenina inflata	34.16		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Cribrohantkenina inflata' LAD defines top of P16, and  is located between LAD of 'Gl. index' and 'T. cunialensis' and 'Hantkenina' in mid-part of polarity chron C13r at Massignano (ref. d) and just below youngest of 3 normal "events" in C13r in Contessa Highway section (ref.b) = C13r; 34.0 Ma [a-d] = C13r.6.
	Globierinatheka index	34.47		One of the few taxa which has an LAD that is isochronous between low and high latitudes and provinces.  Age calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Eocene foram 'Globigerapsis index' LAD is essentially coincident with the LAD of 'Discoaster saipanensis' and 'Discoaster barbadoensis' and with lower of 3 normal "events" in polarity chron C13r in Contessa Highway section (refs. b,c).  This LAD occurs in younger part of polarity chron C13r on Kerguelen Plateau (Site 748) (ref. e) and appears to be globally reliable datum.  Recorded at a level in  Hole 689B (Weddell Sea) identified as C16n (ref. f), but an alternative interpretation of the paleomagnetic stratigraphy (ref. e) suggests this may be C15n, in which case the (apparent) latitudinal diachrony of the HO of Gl. index would be significantly reduced, if not eliminated, inasmuch as dissolution is strong across the Eocene/Oligocene boundary interval at high latitudes.  Chron assignment = C13r; 34.3 Ma [a-e] = C13r.3.
	Globigerinatheka semiinvoluta	35.82		Genus was formerly Porticulasphaera.  Scaling of Berggren-Pearson (2005) -- C15r; 35.3 Ma [a-c]; but Berggren-Pearson (2005) estimate as 35.8 Ma = C16n.2n.8.
	Morozovella crassata	37.67		M. crassata is the senior synonym of Morozovella spinulosa  Assignment by Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- C17n (lower); 38.1 Ma [a]; but 38.0 estimated by Berggren-Pearson (2005) = C17n.3n.6.
	Orbulinoides beckmanni	39.36		Defines top of P14 (or E13).  Age calibration by Berggren and Pearson (2005), which puts this LAD 0.1 myr higher than Berggren et al. (1995) = C18n (lower); 40.1 Ma [a]; but 40.0 Ma by Berggren-Pearson '05, following Wade (2004) using Site 1052 = C18n.2n.2.
	Guembelitrioides nuttalli	41.36		Age assignment by Berggren and Pearson (2005) = C19r; 42.3 Ma = C19r.25
	Morozovella aragonensis	42.60		Defines top of P11 or E9.  Age assignment by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C20n; 43.6 Ma [a] = C20n.15.
	Morozovella subbotinae, Morozovella formosa	50.77		LAD of M. subbotinae defines top of E5, and LAD of M. formosa was top of P7.  Chron-age from Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Eocene Foram Zone P8 base (LAD of 'Morozovella formosa') is drawn as uppermost C23n in chart in Aubry et al. (1988); and is shown with an age of 50.8 Ma in Berggren (1995, SEPM); but the source of these calibrations are not cited.  Assignment = uppermost C23n;  [m,h] = C23n.1n.8
	Morozovella velascoensis	55.09		Berggren and Pearson (2005), which is puts this LAD 0.2 myr higher than Berggren et al. (1995) -- This LAD is recorded in younger part of polarity chron C24r2 in Hole 577 (ref. 9) and in mid-part C24r2 in Hole 577 (at 81.98 m) (ref. k).  However, paleomagnetic data (Bleil, 1985, DSDP Leg 86: 449, Fig. 7b) suggests a hiatus occurs between ~82m & 83 m in Hole 577, which would have the effect of depressing (rendering older) the HO of 'M. velascoensis'.  The HO of 'M. velascoensis' in Hole 577 is in Nannofossil zone CP8 (=NP9) (Monechi, 1985: 310, Table 5) which supports interpretation of hiatus in Hole 577, because the LO of 'M. valascoensis' is in Nannofossil Zone NP10.  Furthermore, Monechi (1985: p.307) indicates absence of extremely condensed sedimentation across the Paleocene/Eocene boundary interval.  Chron assignment here is C24r; 54.7 Ma [a]; but 54.5 Ma (mid-C24r) in Berggren and Pearson, 2005 = C24r.47.
	Globanomalina pseudomenardii	56.67		LAD defines top of Zone P4.  Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomalina pseudomenardii' was called "Planorotallites pseudomenardii' in Berggren & Miller (1988).  The LAD (= base Zone P5) is recorded in Hole 577 at either base of polarity chron C24r (ref. d) and or top C25n (ref. e) and in Hole 752 at top C25n (ref. f).  Juxtaposition/overlap of Gl. pseudomenardii LAD and Gt. subbotinae FAD is observed in Holes 465 and 758 (ref. g).  Chron assignment = C25n (top); 55.9 Ma [a,d-f] = base C24r.
	Parasubbotina variospira	59.99		LAD defines top of P4a (NEW version, Berggren et al, 2000).  Berggren and Pearson (2005) assignment = C26r; 59.2 Ma = C26r.57.
	Parvularugoglobigerina eugubina	65.15		Defines base of P1a.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parvularugoglobigerina eugubina' in Berggren et al. (SEPM, 1995) was called 'Globigerina eugubina' in some other publications.  The LAD, defining the top of Zone P-alpha, is near the FAD of Pa. pseudobulloides; and Berggren et al. (1995) "admittedly somewhat arbitrarily" placed both events just below the polarity chron C29n/r boundary (p.146) = just below C29r/n boundary; 64.8 Ma [a] = C29r.95.
	Racemiguembelina fructicosa; LADs of other Cret. Forams	65.50		Top of Cretaceous
	Globotruncanita calcarata	74.47		SEPM'98 places at Chron C33n.85.
	Dicarinella asymetrica	83.53		Top of Santonian in SEPM'98
	Helvetoglobotruncana helvetica	91.51		Base of  P. percarinatus ammonite zone on SEPM'98 chart. 
	Rotalipora cushmani	93.95		SEPM'98 places arbitrary (?) at 0.4 myr before top of Cenomanian (= top of Rotalipora genus?).  Caron (1985) indicates base of this zone as FAD of W. archaeocretacea, rather than LAD of R. cushmani; and  this FAD is ~0.6 myr below.
	Ticinella bejaouaensis	112.50		Base of foraminifer Hedbergella planispira (defines base of H. planispira foraminifer zone) is greater than 32 long-eccentricity cycles below top of Albian (base of cycle-controlled section) at Piobbico => older than 112.6 Ma.  This calibration is inconsistent, because the base of the H. planispira Zone is placed ABOVE base of P. columnata in Leckie et al. (2002), and in the middle of Lower Albian by Bellier et al. (2000).  However, Hardenbol et al. (1998) place the FAD of H. planispira below the FAD of P. columnata, as is indicated at Piobbico.  SEPM'98 had assigned as 1/2 of H. jacobi Zone. 
	Globigerinelloides algeriana	116.00		Top G. algerianus (= base of Hedbergella trocoidea or Planomalina cheniourensis Zone, depending on author; which is essentially a "gap" zone) = 116.0 Ma  (was 115.2 in Leckie's chart).  SEPM'98 had assigned as 0.1 myr before top of nufieldiensis Zone.   "gap zone" (LAD at base; FAD at top).  Not included in all foraminifer zonations.
	Leupoldina cabri	120.70		Top L. cabri (= base of G. ferreolensis zone) = 120.7 Ma (was 118.2 in Leckie's table).  SEPM'98 had assigned as 1/5 from base of martinoides Zone. 
	Globuligerina oxfordiana, G. stellapolaris, G. caucasica, G. megamonica, G. calloviensis, Globigerina helvetojurassica, Globigerina terquemi. Globigerina gulekhensis	138.74		LADs are in the early Valanginian (Cretaceous), so the age is assummed as 1/3 up from the base of Valanginian
	Globuligerina balakhmatovae	165.72		LAD is in the Late Bathonian, the age is assummed as base of the H. (P.) retrocostatum Zone
FAD
	Truncorotalia (Globorotalia) truncatulinoides	2.00		Base N21&N22.  Age of 2.00 Ma calibrated in Eastern Mediterranean -- Refs 17, 20 & 21; in GTS2004 Neogene foraminifer appendix.  However, this FAD occurs slightly later (1.93 Ma) in Atlantic Sites 925 & 926 (Refs. 7-9 in GTS2004 Neogene foraminifer appendix).  Berggren et al. (1995) assign as mid-Olduvai Subchron; ~1.90 Ma [p,a,f,g,h] = C2n.4; but note that Pliocene Foram "Globorotalia truncatulinoides" FAD is 2.0 Ma (just below Olduvai) in Atl-Medit; but is much earlier at 2.58 Ma (base of Matuyama) in SW Pacfiic.
	Menardella (Globorotalila) miocenica	3.77		Formerly assigned as genus Globorotalia, and an alternate definition for base of Zone N20-N21.   Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C2An.3n; 3.55 Ma [a] = C2An.3n.1.
	Globoconella (Globorotalia)  puncticulata	4.52		Cycle-calibrated in Eastern Mediterranean -- Refs 17, 23 & 24; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) calibrate FAD of Pliocene foram 'Globorotalia puncticulata' to the Nunivak Subchron in the Mediterranean and elsewhere {4.50 Ma [b,c,e,f,g,k] = C3n.2n.85}.  They note that this is approximately the LAD of G. cibaoensis (~0.1 m.y. lower).
	Globorotalia tumida	5.72		Base PL1; N18 (but see Note on Glob. dehiscens).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  This FAD is reported as later (5.57 Ma) at Pacific ODP Legs 111 & 138 (Refs. 2, 5 & 6) in GTS2004 Neogene foram table.  Berggren et al. (1995) notes that Miocene foram 'Globorotalia tumida' FAD (defining base of Berggren's zone Pl 1 = Base of "Pliocene" Foram Zonation; but datum is within latest Miocene) is dated in Hole 588 and synchronouse in other SW Pacific sites (586B,587,590) and in Indian Ocean (Holes 114,219,237,238) (ref.c).  This FAD is at a comparable position, but without paleomagnetic control, at Hole 806B (Ontong-Java Plateau) (ref. d).  They assign as C3r (early Gilbert); 5.6 Ma [a-d] = C3r.45
	Globorotalia plesiotumida 	8.58		M13b base defined either by:  Glob. plesiotumida or Neo. humerosa. Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globorotalia plesiotumida' FAD is recorded in Hole 806B (Ontong-Java Plateau; ref.e), but its FAD was difficult to define owing to questionable lower occurrences.  Berggren et al. (1995) assigned the FAD based on its lowest questionable occurrence, but its effective FCO may be about 0.5 m.y. higher (coeval with FAD of Globorotalia cibaoensis).  In Gulf of Mexico, the FAD is recorded in upper part of Nannofossil Zone NN10, similar to the lower Pacific occurrences, and overlaps the upper part of Discoaster bollii range with the FAD slightly below FAD of nannofossil Minylitha convallis FAD (Zhang et al., 1993; Aubry, 1993).  A similar FAD level is in Buff Bay, Jamaica (Berggren, 1993; Aubry, 1993).  Berggren et al. (1995) assign as (C4r.2r); (8.3) [e] = C4.2r.9.
	Globigerinoides extremus	8.93		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had at (C4r.2r); (8.3) [e] = C4.2r.9.
	Neogloboquadrina acostaensis s.s. -- base regular	10.57		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table.  This FAD is reported younger (9.8 Ma) in Atlantic Sites 925 & 926 (Refs 8, 11, 13) in GTS2004 Neogene foram table.  Berggren et al. (1995) note that Miocene foram 'Neogloboquadrina acostaensis' FAD is calibrated in Holes 558 and 563 (ref. b) and 608 (ref. l) in North Atlantic at the base of chron C5n = C5n.2n; 10.9 Ma [b,l] = C5n.2n.05.
	Globoturborotalia nepenthes	11.63		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) notes that Miocene foram 'Globoturborotalia nepenthes' FAD occurs in North Atlantic Sites 563 (ref. b) and 608 (ref. l) and basal Buff Bay Fm., Jamaica (refs. m,n) = C5r.3r; 11.8 Ma [b,l-n] = C5r.3r.3.  They also use this FAD to define base of Medit. Zone Mt8.  
	Fohsella robusta	13.13		Formerly called 'Globororotalia fohsi robusta'.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globororotalia fohsi robusta' FAD is based on revised interpretation of magnetostratigraphy of Hole 563, in turn based on stable isotope studies in ref.o = C5An.2n; 12.3 Ma [b,k] = C5An.2n.5.
	Fohsella "fohsi"	13.41		Formerly assigned as genus Globorotalia.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8, 11 & 12; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign Miocene foram 'Globorotalia fohsi s.str.' FAD is based on reinterpretation of magnetostratigraphy at Hole 563, in turn based on stable isotope studies at Holes 747A and 608 (see ref. o) = C5Ar.n1-2 (undiff.); 12.7 Ma [b,o] = C5Ar.2r.8.
	Fohsella "praefohsi"	13.77		Formerly assigned as genus Globorotalia.  The form 'Gt. praefohsi' seems intermediate between 'Gt. peripheroacuta' and 'Gt. fohsi s.str'.   Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assigned Miocene foram 'Globorotalia praefohsi' FAD to a much younger level, based on reinterpretation of magnetostratigraphy at Hole 563, in turn based on stable isotope studies at Holes 747A and 608 (see ref. o) = C5Ar.n1-2 (undiff.); 12.7 Ma [b,o] = C5Ar.2r.8, but this FAD age-assignment was nearly identical to FAD of 'Gt. fohsi s.str.'
	Fohsella peripheroacuta	14.24		Formerly assigned as genus Globorotalia, and was used by Berggren et al (1995) to define base of Serravalian stage.  .  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assigned as C5B.1n; 14.8 Ma [b] = base C5ADr = nearly 0.5 myr older than Atlantic-ODP cycle-strat assignment.
	Orbulina universa	14.74		Same as Orbulina suturalis? (see end of this comment).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) used Orbulina "suturalis" (age of 15.09 Ma, based on mid-C5Bn.2n; ref [b] which had 15.1 Ma) to define base of Zone M6, but table in Lourens et al. (GTS2004) uses Orbulina "universa" (and there is no indication of a "suturalis". 
	Praeorbulina glomerosa s.str.	16.27		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) uses to define base of Medit. Zone Mt5b, and assign to C5Cn.1n (upper); 16.1 Ma [b] = C5Cn.1n.8.
	Praeorbulina sicana	16.97		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix -- however this implied revised calibration to polarity chrons would seem to invert Medit. zones Mt4b and Mt5a (this FAD of P. sicana) of Berggren et al. (1995).  Miocene Foram 'Praeorbulina sicana' of Berggren et al (1995) may be same as 'Globigerinoides sicanus' in table of Hodell & Woodruff (1994); however, their age estimates for the FAD differ by 0.7 m.y.  Berggren et al. (1995) assign age as C5Cn.2n (mid); 16.4 Ma [b] = C5Cn.2n.55.
	Globigeriantella insueta s.str.	17.59		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix -- Note that this is much higher FAD than estimated calibrations by Berggren et al. (1995); which results in Zone M3 being nearly non-existent.  Berggren et al. (1995) -- Miocene foram 'Globigerinatella insueta' FAD has an inferred correlation to polarity chron (base of C5En) and corresponding age assignment = (C5En); (18.8 Ma)[t] or 18.85 Ma [u] = base C5En.
	Globoquadrina dehiscens	22.38		Same chron-age calibration as Berggren et al. (1995), who used to define Medit. Zone Mt1b -- Miocene foram 'Globoquadrina dehiscens' FAD is recorded in Holes 516F, 558, 563 (ref. b); South Atlantic (refs. r,s) and Contessa Highway Section (ref. q) = C6Br; 23.2 Ma [b] or 23.4 Ma [u] = C6Br.5.
	Paragloborotalia kugleri	22.96		Paragloborotalia (formerly Globorotalia) kugleri s.str. = M1 base; and approx. Oligocene/Miocene boundary [b,s].  Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) notes that Miocene foram 'Globorotalia kugleri' FAD is recorded in Holes 558, 563 (North Atlantic) and 516F (South Atlantic) (ref. b).   Miocene foram 'Globorotalia kugleri' FAD is recorded in Holes 516F, 558, 563 (ref. a of Oligocene set) = C6Cn.2n; 23.8 Ma [b] or 24.0 Ma [u] = base C6Cn.2n.
	Globigerina angulisuturalis	29.45		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Oligocene foram 'Globoturborotalita (formerly Globigerina) angulisuturalis' FAD, which defines base of P21a, is recorded by Berggren and Miller (1988); Holes 516 and 558 (ref. a), 628A and 803C (ref. c) = C11n (upper); 29.4 Ma [a,c] = top C11n.
	Turborotalia cunialensis	35.26		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia cunialensis' FAD defines base of P16, and is just above (i.e. younger than) LAD of 'P. semiinvoluta' (refs. b,c) = C15r; 35.2 Ma [b-d] = C15r.4.
	Globigerinatheka semiinvoluta 	38.03		Eocene foram 'Porticulasphaera semiinvoluta' defines base of P15, and has a brief overlap with 'Truncorotaloides' (Blow, 1979).  However, a brief, but distinct, separation of 'Acarinina' and 'P. semiinvoluta' is recorded in Nocchi et al. (1986, Fig. a).  Same chron-age calibration as Berggren et al. (1995) = C18n (upper); 38.4 Ma [a,b] = top C18n.1n.
	Orbulinoides beckmanni	39.80		Defines P13 (= E12) base.  Same chron-age calibration as Berggren et al. (1995) = C18r; 40.5 Ma [a] = C18r.66.
	Globigerinatheka kugleri	45.00		Age calibration by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Not well calibrated  [m.n] -- Eocene Foram Zone P11 base (defined as FAD of G. kugleri) is not in table of Berggren (1995, SEPM).  His Eocene figure shows the P10/P11 boundary at about 60% of the distance from P9/P10 to P11/P12, or just above base of Nanno Zone NP15b (which has a magnetic calibration); and I have used this approximate scaling. Estimated by Berggren '95/'05 as 45.8 Ma = C20r.6.
	Guembelitrioides nuttalli, Hantkenina spp.	48.60		First occurrence of Hantkenina (base of P10) is current working definition of base of Lutetian Stage.  FAD of G. nuttalli is suggeste as alternate (base of E8) zonal datum by Berggrena nd Pearson (2005).  Age assignment of these events by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C22n (upper); 49.0 Ma [a] = Base C21r (which makes a convenient global event).
	Acarinina cuneicamerata, Astrorotalia palmerae	50.30		Acarinina cuneicamerata = base E7, Astrorotalia palmerae = base P9.  Genus of Astro. palmerae was Planorotalites in Berggren et al, 1995.  Same chron-age calibration as Berggren et al. (1995) = C22r; 50.4 Ma [a] = C22r.33.
	Morozovella aragonensis	52.57		Defines P7 (=E5) base. Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella argonensis' FAD is recorded in Holes 550 (ref. g,h), 577 (ref. i,j) and in C23r in Hole 527 (ref. g).  The level adopted by Berggren (used shown here) is slightly older than that shown in Ref. a = C23n.2r; 52.3 Ma [g-j] = C23r.1.
	Morozovella  formosa	54.52		Base of Zone P6b (= Zone E4 of Berggren-Pearson. 2005). This taxon is called only "Moro. formosa" in some other charts and papers, and was called Globorotalia formosa in some publications. Same chron-age calibration as Berggren et al. (1995) -- Early Eocene foram 'Morozovella formosa formosa' FAD is calibrated in Hole 577 (ref. i), and defined the P6b/c subzonal boundary of Berggren and Miller (1988).  Chron assignment = C24r; 54.0 Ma [i] = C24r.75.
	Pseudohastigerina wilcoxensis	55.58		Berggren and Pearson (2005) -- FAD is top of PE carbon-isotope excursion.  Following Berggren and Pearson, it is set as 0.15 myr above PE boundary (base of CIE) = C24r; 55.35 Ma.
	Acarinina sibaiyaensis	55.73		Berggren and Pearson (2005) -- marker for Paleo/Eoc.  One of "Excursion taxa" at PE boundary, therefore age is set equal to that PE age = C24r; 55.5 Ma = lower-mid C24r.
	Acarinina soldadoensis	57.30		Paleocene foram 'Acarinina soldadoensis' FAD defines base of Zone P4c of Berggren et al. (1995)/  Berggren and Pearson (2005), has same chron-age calibration as Berggren et al. (1995) -- This datum is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, in association with FAD of Acar. coalingensis-triplex group and Acar. soldadoensis (Berggren et al., 1995, SEPM).Paleocene Foram Zone 'P4' is the range of 'Globanomalina pseudomenardii'  (Bolli, 1957).  It is subdivided by the LAD of 'Acar. subsphaerica' and FAD of 'Acar. soldadoensis' by Berggren et al. (1995) to essentially correspond to foraminifer zones used in the Caucasus.  Chron assignment = C25r; 56.5 Ma [a] = C25r.9.
	Globanomalina pseudomenardii	60.19		Calibration by Berggren and Pearson (2005) is 0.2 myr older than the FAD in Berggren et al. (1995) -- Paleocene foram 'Globanomalina psudomenardii' was called 'Planorotalites pseudomenardii' in Berggren & Miller (1988).  Calibration is from Hole 384, and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM).  The FAD is also recorded in the younger part of polarity chron C26r in Hole 577 (ref. 4) within Nannofossil Zone CP 5/6 (undiff.); but in polarity chron C25r in Zone CP5 (= NP6) in Hole 685 (ref. h) or in C26n in Zone CP5 (= NP5) in Hole 605 (refs. h,i; see also ref. b).  Chron assignment = C26r; 59.2 Ma [a,b,d,h,i]; but 59.4 Ma (mid-C26r) in Berggren and Pearson, 2005 = C26r.5.
	Igorina albeari	60.78		Paleocene foram 'Igorina albeari (=Muricella albeari = Globorotalia laevigata)' FAD defines P3b base.  Berggren and Pearson (2005) is same chron-age calibration as Berggren et al. (1995) -- This FAD occurs approximately mid-way in Zone P3 in Holes 463 and 758A and in the mid-part of polarity chron C26r in Hole 384 (Berggren et al., 1995, SEPM) = C26r; 60.0 Ma [a] = C26r.3.
	Morozovella angulata, Igorina pusilla	61.72		A working definition for base of Selandian stage.  Berggren and Pearson (2005) is same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella angulata' FAD occurs in Hole 577 within lower part of polarity chron C26r (ref. a,e), but precise position difficult to determine because of absence of C27n (Bleil, 1985, DSDP Leg 86).  In Hole 384, this FAD occurs in upper C27n at <2m above FAD of 'Prae. uncinata') in Nannofossil Zone NP4.  In Holes 465 and 758A it is 2m above FAD of 'Prae. uncinata' (Berggren et al., 1995, SEPM).  Chron assignment = C27n (upper); 61,0 Ma [a,b] = C27n.8.
	Praemurica uncinata	62.07		Paleocene foram 'Praemurica uncinata' (formerly 'Morozovella uncinata') FAD defines base of Zone P2.  Berggren and Pearson (2005) moved the FAD 0.4 myr older than in Berggren et al. (1995) on same mag-chron scale.  Notes from Berggren et al. (1995) -- The FAD occurs in Hole 577 (refs. a,e) just above a N->R polarity reversal (= polarity chron C28n); but Polarity chron C27n is missing (Bleil, 1985, DSDP Leg 86: p.446, Fig. 5; p.449, Fig 7B), and there may be a short hiatus at/near the level if FAD of this taxon in C27n (ref. b) is correct.  Alternatively C27n may be missing in the core break between cores 11 and 12 (ca. 101.8 m) in which case the FO of this taxon would be near the C27r/C28n boundary (see ref. b).  In Hole 384, it occurs at the same level as FAD of 'P. praeangulata' in Nannofossil Zone NP4 at the base of C27n, as well as in Holes 465 and 758A (see extended discussion in Berggren et al., 1995, SEPM).  Its FAD was considered equivalent to FAD of 'Praemurica praecursoria' (= 'Globorotalia (Acarinina) praecursoria' of Berggren & Miller, 1988) in an earlier draft by Berggren (1993), but 'praecursoria' was removed from his later versions. Chron assignment = C27n (lower); 61.2 Ma [a,b]; but 61.37 Ma (uppermost C27r) in Berggren and Pearson, 2005 = C27r.92.
	Globanomalina compressa, Praemurica inconstans	63.44		Berggren and Pearson (2005), which is nearly same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica inconstans' FAD is recorded in Holes 689B and 690C (ref. c) and 384 (ref. g).  Paleocene foram 'Globanomalina compressa' was called 'Planorotalites compresus' in Berggren & Miller, 1988.  FAD is recorded in Hole 384 (ref. g).  It also occurs at a comparable level (by correlation) in an interval with no polarity data just above incomplete polarity chron C28n in 750A-14-2, 44cm to 750A-14-2, 40cm (ref. f?).  Berggren & Miller (1988) "believe that G. compressus and Morozovella trinidadensis have approximately coeval FAD's"; therefore, this FAD of compressa was also base of Zone P1c.  Chron assignment = C28n (2/3rds from base); 63.0 Ma [a,b], but 62.87 Ma in Berggren and Pearson, 2005 = C28n.67.
	Subbotina triloculinoides	64.71		Defines P1b base.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Subbotina triloculinoides' FAD is recorded in Hole 384 (ref. g) = C29n; 64.3 Ma [g] = C29n.6.
	Parvularugoglobigerina eugubina	65.32		Defines Pa ('alpha' Greek letter) base.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram "Parvularugoglobigerina eugubina" FAD is estimated at about 0.030 myr after the end-Cretaceous event (Groot et al., 1990; discussed in Berggren, 1995, SEPM).  Chron assignment = C29r; 64.97 Ma [k] = C29r.7 (but fixed as 0.03 myr higher than base of P0).
	Abathomphalus mayaroensis	68.36		Chron C31n.40 (ODP 171B table, in turn from Erba et al, 1995).  This is the Tethyan FAD.  The FAD of A. mayaroensis seems to be older in North Sea (Paul Sikora, EGI database, 2005).  SEPM'98 correlation was approx. top of J. nebrascansis ammonite zone.
	Racemiguembelina fructicosa	69.62	dashed	DASHED:  Chron C31r.60  (ODP 171B table, in turn from Erba et al, 1995; which is nearly same as the C31r.66 placement in SEPM98).  NOTE: However, this FAD in Tethyan realm is calibrated in EGI database (Paul Sikora, 2005) as 67.5 Ma (2 myr young), which is ABOVE the FAD of A. mayaroensis => this Zone may not be applicable.
	Gansserina gansseri	72.35		SEPM'98 places at Chron C32n.40
	Globotruncana aegyptiaca	73.27		SEPM'98 places at Chron C32r.1n.50 (used here).  However, EGI database (Paul Sikora, 2005) calibrates Glob. aegyptiaca FAD at 72.7 Ma; about 0.5 myr younger.
	Globotruncanita calcarata	75.57		Polarity chron C33n.66.  Genus assigned as "Radotruncana" in Leg 171B table, but not in their Figure.
	Globotruncana ventricosa (consistent)	77.16		First consistent occurrence is a better marker for base of this Foram Zone.  EGI calibration is 77.6 Ma (Paul Sikora, 2005), which is 40% up in Chron C33n.
	Globotruncana ventricosa (rare)	79.54	dashed	DASHED at Top of Chron C33r (SEPM'98):  Rare FAD is not a useful datum, because it remains rare until mid-Middle Campanian (Paul Sikora, 2005); therefore consistent occurrence is a better definition of the zone.
	Globotruncanita elevata	83.53		Base of Campanian in SEPM'98.
	Dicarinella asymetrica	84.94		SEPM'98 assigns as Base of Middle Santonian (= base C. vermiformis ammonite zone).  D. asymtrica Zone is also range-zone of the index species.
	Dicarinella concavata	90.79	dashed	Dashed -- One-third up in P. hyatti ammonite zone in SEPM98; but ODP Leg 171B placed about 0.8 myr higher.
	Helvetoglobotruncana helvetica	93.41		Top of W. devonense ammonite zone (= base of P. flexuosum ammonite zone) on SEPM'98 chart.
	Rotalipora cushmani	95.33		SEPM'98 places at mid-point of Acanthoceras muldoonense ammonite zone. See note on R. reicheli.
	Rotalipora reicheli	95.68		SEPM'98 assigns as base of Middle Cenomanian.   Leg 171B table assigns the R. reicheli Zone with an age ~1 myr older, but with same duration.
	Rotalipora globotruncanoides	99.60		Base of Cenomanian (= primary marker of GSSP !! ).  Formerly called "R. greenhornensis"?  SEPM'98 had assigned as latest Albian (mid-point of uppermost subzone, M. perinflatum), but this was prior to GSSP definition of boundary.
	Rotalipora appenninica	100.94		Base of planktonic foraminifer Rotalipora appenninica is nearly the same horizon as base of Planomalina buxtorfi = base of that zone = 3.3 long-eccentricity cycles below top Albian (1.3 myr) => 100.9 Ma.  Leckie et al. (2002) indicate that R. appenninica FAD is just slightly older/below the FAD of P. buxtorfi, but Hardenbol et al. (1998) and Bellier et al., (2000) show the events to be simultaneous, which I will assume here.  The duration is 1.3 myr, nearly identical to the 1.5 myr used in Leckie et al. (2002) and 1.1 myr in Hardenbol et al., 1998.  Considering the thickness at Risou for this R. appenninica zone (in excess of 100 m; Kennedy et al., 2003 in press), I would have preferred a much longer time span.  SEPM'98 had assigned as Base of Stoliczkaia dispar Zone.
	Planomalina buxtorfi	100.94		See below (primary control on Albian scale!).  Base of P. buxtorfi is also used as base of R. appenninica Zone on some scales.
	Rotalipora ticinensis	102.93		Base of Rotalipora ticinensis (= base of that zone) = 8.2 long-eccentricity cycles below top Albian (3.3 myr) on Piobbico cyclostratigraphy => 102.9 Ma.   (primary control on Albian scale!).  SEPM'98 had assigned as 2/5 from base of H. varicosum s.z.
	Rotalipora subticinensis	105.05	dashed	DASH:  SEPM'98 had assigned as FAD is at the base of the H. orbignyi s.z. of the M. (M.) inflatum. (used here).   Base of foraminifer R. subticinensis (base of that subzone) is not indicated in this Piobbico cyclostratigraphy, but Leckie et al. (2002) scales it within the B. breggiensis zone as 0.7 myr below the base of R. ticinensis, which would project as 103.6 Ma in GTS04, but would lose the relative proportions of Leckie's scale.
	Ticinella praeticinensis	106.42		Base of T. praeticinensis foraminifer subzone  = 16.8 long-eccentricity cycles below top Albian (6.8 myr) => 106.4 Ma.  The duration is 3.2 myr, nearly the same as the 3.3 myr used in Leckie et al. (2002).  (NOTE -- Leckie et al., 2002, define the T. praeticinensis foraminifer subzone as the base of B. breggiensis Zone, in turn defined by the base of that species; however, the actual FAD of T. praeticinensis is below/older than the base of B. breggiensis according to both Leckie et al., 2002, and Hardenbol et al., 1998.  Because Premoli Silva is a co-author on both the Leckie et al., 2002 paper and on the Piobbico cycle stratigraphy paper, I'm assuming that the T. praeticinensis subzone is defined as base of B. breggiensis for this scaling.  In contrast, the zonal schemes of Hardenbol et al., 1998, and Bellier et al., 2000, do not have a B. breggiensis zone, but define the base of T. praeticinensis zone by the first occurrence of the name species.  What a mess.)  (primary control on Albian scale!)
	Ticinella primula	110.89		Base of foraminifer T. primula is 27.8 long-eccentricity cycles below top of Albian (11.3 myr) in Piobbico cyclestrat => 110.9 Ma.  The T. primula zone extends up to 106.4 Ma, which is consistent with the 107.1 Ma Ar-Ar age within it (but from the middle of the 3 ammonite zones that it spans) obtained by Obradovich (1993).   (primary control on Albian scale!).  SEPM'98 had placed in middle of O. raulinianus s.z.
	Ticinella bejaouaensis	114.30		Base Ticinella bejaouaensis = 114.6 Ma (was 114.3 in Leckie's chart).  SEPM'98 had estimated as 3/5 up in D. nodosocostatum s.z.
	Globigerinelloides algeriana	119.00		Base Globigerinelloides algerianus = 119.0 Ma (was 117.1 on Leckie's chart).  SEPM'98 had assigned as 3/5 from base of martinoides Zone.
	Leupoldina cabri (consistent)	122.05		Consistent L. cabri (and calibration of FAD in SE France, etc.) is 85% up in D. deshayesi Zone (but see comment below -- rare occurrences are nearly to base of Aptian).  SEPM'98 had assigned as 2/3 from base of Deshayesites deshayesi Zone.
	Leupoldina cabri	124.50		Base of rare L. cabri (after downward extension by Premoli Silva et al., 1999) = 0.5 myr above base Aptian (125.0 Ma) = 124.5 Ma  (but, usually rare until higher; therefore the apparent FAD of L. cabri in the middle of the D. deshayesi ammonite zone in the Bedoule section (Moullade et al., 1998) is probably this delayed first occurrence).
	Globigerinelloides blowi	127.88		SEPM'98 had assigned as Estimated as about 1/4 below top of A. vandenheckii zone.
	Hedbergella similis	129.64		SEPM'98 had assigned as Base of N. nicklesi Zone.
	Hedbergella sigali/delrioensis	136.76		SEPM'98 had assigned as 0.1 myr above mid-H. trinodosum s.z.   Most scales list this as H. sigali Foram Zone.
	Globuligerina hoterivica	142.30		SEPM'98 had assigned as Base of M. paraminounum s.z.   Also called "Favusella" hoterivica
	Conoglobigerina gulekhensis	145.46		SEPM'98 had assigned as Base of Berriasian
	Globuligerina balakhmatovae, G. bathoniana, Globigerina gulekhensis	168.86		FADs are in the Late Bajocian, the age is assummed as base of the G. (G.) garantiana Zone
	Globuligerina oxfordiana, G. stellapolaris, G. caucasica, G. megamonica, G. calloviensis, Globigerina helvetojurassica, Globigerina terquemi, 	170.23		FADs are in the Middle Bajocian, base of the S. (S.) humphriesianum Zone


Other Foram FAD/LAD	event		241/244/181		off
LAD
	Globorotalia flexuosa	0.07		~C1n.913 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 4); 0.068 Ma [g]
	Globoquadrina pseudofoliata	0.22		C1n.715 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 7); 0.22 Ma [b]
	Pulleniatina finalis	1.39		Same chron-age calibration as Berggren et al. (1995) = midway between Olduvai and Jaramillo; 1.40 Ma [a,b] = C1r.3r.66
	Globigerinoides extremus	1.98		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned to top Olduvai (C2n); 1.77 Ma ; [a,c,d] = top C2n.
	Globorotalia pertenuis	2.30		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Genus was "Globorotalia" in SEPM/Berggren, who assigned to top Gauss Subchron; 2.60 Ma [a] = C2An.1n.95.
	Globoturborotalita decoraperta	2.75		Astronomically tuned from ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Menardella multicamerata	2.98		Formerly assigned as genus Globorotalia.  Astronomically tuned from ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as C2An.1r (Kaena); 3.09 Ma [a] = C2Ar.1r.3.
	Hirsutella cibaoensis	3.23		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globorotalia sp.cf. G.  crassula	3.29		North Atlantic LAD.  Same chron-age calibration as Berggren et al. (1995) = lower Mammoth; 3.30 Ma [b] = C2An.2r.3.
	Pulleniatina (Atl.)	3.41		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) have similar calibration as C2An.3n; 3.45 Ma [a] = C2An.3n.5.
	Pulleniatina primalis	3.66		Same chron-age calibration as Berggren et al. (1995) = late Gilbert reversed; 3.65 Ma [a] = C3Ar.9.
	Pulleniatina spectabilis	4.21		Same chron-age calibration as Berggren et al. (1995) = top Cochiti Subchron; 4.20 Ma [a] = C3n.1n.8.
	Globigerinoides seiglei	4.72		Same chron-age calibration as Berggren et al. (1995) = above Sidufjall subchron; 4.7 Ma [a] = C3n.2r.5.
	Globorotalia lenguaensis	6.14		Miocene foram 'Globorotalia lenguaensis' LAD defines top of M13.  Same scaling as Berggren et al. (1995) -- LAD is directly calibrated to C3An.1n in ODP Hole 840 (Tonga Platform; ref. d) and Hole 806B (Ontong-Java Plateau in equatorial West Pacific; ref. 5).  This LAD occurs just below FAD of Pull. primalis at ODP 840 and just above it at ODP 806B.  The corresponding age is about 6.0 Ma (Cande-Kent, 1995).  However, LAD occurs much earlier in the Atlantic:  In Hole 519 (S. Atl.), LAD of G. lenguaensis has been calibrated to upper C4An (about 8.7 Ma; refs. r,s).  In E68-136 (Gulf of Mexico), the LAD occurs about 10m above the FAD of Globorotalia plesiotumida (=base of Foram Zone N17) and within range of Minylitha convallis and above the LAD of Discoaster bollii.  In contrast, in E66-73, the LAD is at the same level as FAD of G. plesiotumida, and below the FAD of M. convallis and LAD of D. bollii (Zhang et al., 1993; Aubry, 1993). Chron-age assignment = C3An.1n; 6.0 Ma [d] =C3An.1n.5. 
	Globorotalia miotumida (conomiozea)	6.52		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Neogloboquadrina  nympha	10.20		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina nympha' LAD is calibrated in Holes 748, 751 (Kerguelen Plateau, south Indian Ocean) = C5n.2n; 10.1 Ma [k] = C5n.2n.8.
	Paragloborotalia siakensis	10.46		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  However, this LAD is reported to be much older (11.2 Ma) in Medit. (Refs. 31 & 32) in GTS2004 Neogene foram table; therefore it is used as base of Zone MM10.  Table by Lourens et al (GTS2004) also uses LAD of P. siakensis to mark their version of M11/12 and N14/15 zonal boundaries; but this would be diachronous with Atlantic.
	Globigerinoides subquadratus	11.54		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Fohsella (Globorotalia) fohsi "lobata"	11.79		Species "lobata" apparently combined with Fohsella "fohsi s.l." in zonal scheme of Lourens et al. (in GTS2004).  The result is to merge the bases of M10 and N13 zonal schemes in their system.  Berggren et al. (1995) -- Miocene foram 'Globorotalia fohsi lobata' LAD is based on reinterpretation of paleomagnetics in Hole 563, based in turn on stable isotope studies at Kerguelen Plateau Site 747 and North Atlantic Hole 608 (ref.o) = C5Ar.1r; 12.1 Ma [b,o] = C5An.1r.8.
	Globorotalia panda	11.89		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia panda' is calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean); with magnetic stratigraphy reinterpreted in ref.o = C5r.3r; 11.8 Ma [n] = C5r.3r.3.
	Tenuitella  selleyi, pseuoedita, minutissima, & clemenciae	12.31		Same chron-age calibration as Berggren et al. (1995) -- Miocene forams 'Tenuitella selleyi' through "clemenciae" simultaneous LADs are calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean) = C5An.2n; 12.3 Ma [p] = C5An.2n.5.
	Globorotalia praescitula	13.73		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren listed LAD as much younger -- C5An.1n; 11.9 Ma [11]; therefore the cycle-calibration needs comparison to other sites.  Berggren et al's assignment of Miocene foram Globorotalia praescitula' LAD was calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean); with magnetic stratigraphy reinterpreted in ref. o = top C5An.1n.
	Fohsella peripheroronda	13.80		Formerly assigned as genus Globorotalia.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) used to define base of Medit. Zone Mt7, with age assignment of C5ADn (lower); 14.6 Ma [b] = base C5ADn = nearly 1 myr older than Atlantic-ODP assignment.
	Globigeriantella insueta s.str.	14.66		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Praeorbulina glomerosa s.str.	14.78		Same chron-age calibration as Berggren et al. (1995) = C5B.1n; 14.8 Ma [b] = base C5ADr
	Globorotalia miozea	15.85		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia miozea' LAD is calibrated in Hole 747A, Kerguelen Plateau; as within lower polarity chron C5B.1n (ref. p) = C5Br (lower); 15.9 Ma [k] = C5Br.15.
	Globorotalia incognita	16.39		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia incognita' LAD is calibrated in Hole 747C, Kerguelen Plateau = C5Cn.2n (mid); 16.4 Ma [k] = C5Cn.2n.5.
	Globorotalia zealandica, Globorotalia semivera	17.26		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia zealandica' is recorded in Hole 747A (ref. p); and observed in lower part of polarity zone C5Dn in Hole 751 (ref.k) = C5Dn (upper); 17.3 Ma [p] = C5Dn.9.
	Globoquadrina dehiscens forma spinosa	17.61		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina dehiscens forma spinosa' LAD is recorded in Hole 615, South Atlantic (ref. b) = C5Dr; 17.9 Ma [b] = C5Dr.6.
	Tenuitella munda	20.78		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Tenuitella munda' LAD is recorded in Hole 747, Kergulen Plateau (ref. p); with the magnetostratigraphy reinterpreted in ref. o = C6Ar; 21.4 Ma [p] = C6Ar.8.
	Globoturborotalita angulisuturalis	20.93		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoturborotalita angulisuturalis' LAD is recorded in Hole 516F (ref. b); with magnetostratigraphy reinterpreted in ref.o = C6Ar; 21.6 Ma [b] or 22.6 Ma [u] = C6Ar.4.
	Paragloborotalia pseudokugleri	21.31		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) have similar age -- Miocene foram 'Paragloborotalia (formerlyGloborotalia) pseudokugleri' LAD is recorded in Hole 516F (ref. b); with magnetostratigraphy reinterpreted in ref.o = C6Ar; 21.6 Ma [b] = C6Ar.4.
	Globoquadrina globularis	21.98		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina globularis' LAD is recorded in Hole 516F, South Atlantic (ref. b) = C6Bn.1r; 22.8 Ma [b] = C6Bn.1r.3.
	Globigerina ciperoensis	22.90		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Tenuitella gemma	23.58		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Tenuitella gemma' LAD is recorded in Hole 747A (ref. e) = C6Cr; 24.3 Ma [e] = C6Cr.7.
	Globigerina labiacrassata	26.83		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerina labiacrassata' LAD (= P 15/16 boundary in Berggren, 1992); is recorded at top of polarity zone C9n in Holes 747A, 748B (ref. b) and 689B and 690B (ref. d) and in lower C8n  in Hole 747A (ref. e) = C9n (upper); 27.1 Ma [b,d] = C9n.9.
	Subbotina angiporoides	30.11		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Subbotina angiporoides' LAD is also the P13/P14a boundary in Stott and Kennett (1990).  This LAD is recorded in early part of polarity zone C11n in Holes 516R (ref. 1), 748B (ref. b) and 689B and 690B (ref. d) = C11n (lower); 30.0 Ma [a,b,d] = C11n.2n.3.
	Turborotalia pomeroli	35.37		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia pomeroli' LAD occurs with LAD of 'P. semiinvoluta' in polarity Chron C16n.2n in Massignano section (ref. 4) = C15r; 35.3 Ma [a-c] = C15r.1.
	Acarinina spp.	37.24		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina spp.' LAD occurs in mid-C17n (ref. 1) or top of polarity chron C18n (ref. b,c) in the Apennines, which is about 1 myr older.  Chron assignment = mid-C17n; 37.5 Ma [a,c] = base C17n.1n.
	Subbotina linaperta, Acarinina collactea	37.43		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Subbotina linaperta' is recorded in mid-C17n in Hole 689B (ref. f) and in polarity zone C17n in Hole 748B (ref. f).  Eocene foram 'Acarinina collactea' LAD is recorded in interval of uninterpretable paleomagnetic data just above level identified as polarity chron C17n in Hole 748B (ref. e) and at level interpreted as C18n in Hole 690B (Weddell Sea (ref. f).  These LADs are grouped together in Berggren and here.  Chron assignment = C17n; 37.7 Ma [a] = C17n.2n.6.
	Planorotalites	38.03		Same chron-age calibration as Berggren et al. (1995) = C18n (upper); 38.5 Ma [a,b] = top C18n.1n.
	Acarinina primitiva	38.50		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina primitiva' is recorded in mid-part of polarity chron C18n in Hole 689 (ref. f) and in interval of uninterpretable paleomagnetic data just above probable C18n in Hole 748B (ref. e).  Chron assignment = C18n; 39.0 Ma [a,f] = C18n.1n.5.
	Subbotina frontosa	38.79		Same chron-age calibration as Berggren et al. (1995) = C18n (mid); 39.3 Ma [a] = C18n.1n.2.
	Acarinina bullbrooki	39.80		Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C18r; 40.5 Ma [a] = C18r.66.
	Morozovella marginodentata	53.03		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella marginodentata' LAD is recorded in Hole 550 (refs. g,h).  Berggren et al. (1995) assign an age of 52.5 Ma, but their correlation with polarity chron C24n.1r does not allow an age younger than 52.7 Ma.  Assignment = C24n.1r; 52.5 Ma [g,h] = C24n.1r.8.
	Morozovella lensiformis	53.06		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella lensiformis' LAD is recorded in Holes 550 (refs. g,h) and 577 (ref. i) = C24n.1r; 52.7 Ma [g-i] = C24n.1r.5.
	Subbotina velascoensis 	53.95		Similar chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Subbotina velascoensis' LAD is recorded in Hole 550 (refs. g,h) = C24r; 53.5 Ma [g,h] = C24r.65.  BUT, Berggren and Pearson (2005) says that that LAD of Sub. velascoensis is in Zone E3, therefore calibration shifted to C24.95 to place below base of Zone E4 [NEED TO RECHECK THIS]
	Morozovella aequa	54.09		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella aequa' LAD is recorded in Hole 550 (refs. g,h); and within polarity zone C24n1 in Hole 577 (ref. i) = C24r; 53.6 Ma [g-i] = C24r.9.
	Morozovella acuta	55.32		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella acuta' LAD is recorded in Hole 550 (refs. g,h), where it occurs mideway between dated Ash Bed -17 (54.5 Ma) and +19 (54.0 Ma) [using older Ar-Ar standards, hence would shift about 0.5 myr older in GTS2004 standard].  Corresponding chron assignment would be equivalent to C24r (mid); 54.7 Ma [h] = C24r.47.
	Acarinina acarinata, Acarinina mckannai	57.18		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Acarinina acarinata' and 'Acar. mckannai' LAD's are calibrated in DSDP Hole 384 (N. Atl.); and at comparable levels but without paleomagnetic control in Holes 465 (Eq. Pac.) and 758A (Indian Ocean) (Berggren et al., 1995, SEPM).  Chron assignment = base C25n.
	Acarinina subsphaerica (common)	57.90		Paleocene foram 'Acarinina subsphaerica' LAD had defined base of Zone P4b of Berggren et al. (1995).  Same chron-age calibration as Berggren et al. (1995) -- This datum is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, and occurs approximately midway in Zone P4 (Berggren et al., 1995, SEPM).  Chron assignment = C26r (C25r); 57.1 Ma [a] = C25r.4.
	Parasubbotina varianta, Parasubbotina variolaria	59.99		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Parasubbotina varianta' and 'Parasubbotina variolaria' LAD's are simultaneous in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM) = C26r; 59.2 M) [a] = C26r.57.
	Globotruncana, Globigerinelloides, Rugoglobigerina, etc (Cret. forams)	65.50		Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) = C29r.7; 65.0 Ma [multiple sources]; which is set in GTS2004 using revised Ar-Ar standard-constant as 65.5 Ma.
	Abathomphalus mayaroensis, Gansserina gansseri	65.80		SEPM'98 had assigned as ~0.3 m.y. before K/T
	Abathomphalus intermedia	66.82		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is middle of Chron C30n
	Rugoglobigerina pennyi	68.32		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 45% up in Chron C31n.
	Globotruncanella ventricosa	69.62	dashed	DASHED at Chron C31r.60
	Archaeoglobigerina bosquensis	77.79		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 2/3rds up in Middle Campanian.
	Ventilabrella eggeri	82.36		SEPM'98 has at Chron C33r.25
	Marginotruncana coronata	82.55		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age (mid-Early Campanian) assigned here as 20% up in Chron C33r to match EGI age.
	Whiteinella baltica	82.74		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Age is just below LAD of M. coronata; assigned here as 15% up in Chron C33r.
	Dicarinella concavata, Sigalia deflaensis	83.53		Top of Santonian in SEPM'98
	Sigalia decoratissima decoratissima	83.95		SEPM'98 places at About 70% up between FAD of S. dec. carpathica and LAD of S. deflaensis Forams
	Sigalia decoratissima carpathica	84.47		SEPM'98 places at About one-third up between FAD of S. dec. carpathica and LAD of S. deflaensis Forams
	Sigalitruncana sigali	84.69		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Age is "mid-Santonian".
	Whiteinella archaeocretacea	84.94		According to EGI database (Paul Sikora, 2005), this LAD goes up to approximate base of Middle Santonian (instead of mid-Coniacian on SEPM chart !! ).
	Whiteinella paradubia	86.05		Useful marker just below Inoceramus marker for base-Santonian (EGI database, Paul Sikora, 2005).  Placed here here arbitrarily as 0.2 myr below base of Santonian in GTS2004.
	Whiteinella aprica	88.58		Useful marker at base of Middle Coniacian (EGI database, Paul Sikora, 2005)
	Dicarinella hagni	89.07		Useful marker not too far above (ca. 0.2 myr?? used here) base of Coniacian (EGI database, relative placement according to Paul Sikora, 2005 -- although his quoted age of 88.3 in SEPM98 scale was nearly mid-Middle Coniacian).
	Dicarinella imbricata	93.85		Useful marker just below OAE2 event (EGI database, Paul Sikora, 2005) = assigned here as 0.3 myr before base-Turonian
	Rotalipora reicheli, Rotalipora appenninica, Rotalipora globotruncanoides	94.75		SEPM'98 places at base of Upper Cenomanian
	Planomalina buxtorti	100.10		SEPM'98 places at 1/5 from base of M. periflatum s.z.
	Rotalipora ticinensis, Ticinella primula	100.47		SEPM'98 places LADs at 2/3 from base of M. rostratum s.z.
	Biticinella breggiensis	100.66		SEPM'98 places at 2/5 from base of M. rostratum s.z.
	Rotalipora subticinensis	101.62		Same assignment as SEPM'98 "for now" = 1/2 from base of C. auritus s.z.   Albian Foraminifer 'R subticinensis' LAD is given 2 ages in Robaszynski's chart, one is 0.13 m.y. older than the one shown here.
FAD
	Bolliella calida	0.22		C1n.715 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 7); 0.22 Ma [b]
	Globorotalia flexuosa	0.40		C1n.486 = Same chron-age calibration as Berggren et al. (1995) = mid-Brunhes (Stage 11); 0.401 Ma [g]
	Globorotalia hirsuta	0.45		C1n.42 = Same chron-age calibration as Berggren et al. (1995) = mid-Brunhes (stage 12); 0.45 Ma [f]
	Globorotalia crassaformis hessi	0.75		C1n.04 = Same chron-age calibration as Berggren et al. (1995) = basal Brunhes ; 0.75 Ma ; [b]
	Sphaeroidinellopsis dehiscens s.str.	3.24		This "dehiscens" species was formerly assigned as genus Sphaeroidinella.  Same chron-age calibration as Berggren et al. (1995) = top Mammoth; 3.25 Ma [a] = C2An.2r.7.  They note that this FAD occurs about 1 myr later in Mediterannean (about 2.19 Ma) [ref. h].
	Globigerinoides fistulosus	3.33		Same chron-age calibration as Berggren et al. (1995) = C2An.2r (base Mammoth); 3.33 Ma [a] = C2An.2r.0.
	Truncorotalia (Globorotalia) crassaformis s.l.	4.31		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as Nunivak Subchron; 4.50 Ma [a,n] = C3n.2n.85.  They noted that Pliocene foram 'Globorotalia crassaformis' FAD is reported to occur about 1 m.y. later (Gilbert/Gauss boundary, or 3.58 Ma) in the Mediterranean (ref. c,k). 
	Sphaeroidinellopsis dehiscens	5.53		This "dehiscens" species was formerly assigned as genus Sphaeroidinella.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as basal Thvera Subchron; 5.2 Ma [a,o] = C3n.4n.13.  They note that Sphaeroidinellopsis spp. (top of acme) in Mediterranean was formerly reported to have approximately same age [ref. c,f,k], but now seems ~100,000yr  younger; however, Lourens et al (GTS2004) put that acme-top about 300,000 yr younger.
	Globorotalia pliozea, Globorotalia sphericomiozea	5.67		Same chron-age calibration as Berggren et al. (1995) = C3r (early Gilbert); 5.6 Ma [a] = C3r.45 [Datum levels in C3r scaled proportionally to match Berggren's relative spacing. ].  Miocene foram 'Globorotalia pliozea' FAD is dated in Hole 588 (SW Pacific) (ref.a).  G. sphericomiozea FAD is top of Zone Mt10. Miocene foram 'Globorotalia sphericomiozea' FAD is dated in Hole 588 (SW Pacific) (ref.a).
	Globorotalia  margaritae	6.08		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Extensive notes in Berggren et al. (1995), who place the global FAD at C3An (mid); 6.0 Ma [a-g] = C3An.1n.5 -- Miocene foram 'Globorotalia margaritae' FAD has this age in the North Atlantic (refs. b,f,g).  The FAD is considered asynchronous between the SW Pacific and Indian Ocean (ref.c) and is observed to occur above (Hole 806B) and below (Hole 840) the FAD of G. tumida (ref. d).  The FAD is nearly 1 myr later in the Mediterranean (about 5.32), where its inital occurrence is recorded immediately above base Zanclian in mid-Thvera [mid-C3An.2n] and first common occurrence (FCO) only shortly thereafter at 5.07 Ma (Langereis and Hilgen, 1991; ref. g).
	Pulleniatina primalis	6.58		Same chron-age calibration as Berggren et al. (1995) = C3An.2n; 6.4 Ma [b,c,e] = C3An.2n.5.  Miocene foram 'Pulleniatina primalis' FAD occurs at this age in the SW Pacific region (SItes 587,588,590; and at 806B, but without paleomagnetic calibration, ref.d) and Indian Ocean (Sites 214,219,238) (ref. c).  FAD is slightly above FAD of G. lenguaensis at Hole 840 (ref.d).
	Globorotalia nicolae	6.83		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Neogloboquadrina atlantica (sin.)	7.02		D-> S coiling.  Same chron-age calibration as Berggren et al. (1995) = C3Ar; 6.8 Ma [g,h] = C3Ar.3.  Miocene foram 'Neogloboquadrina atlantica' (D to S) FAD is recorded in North Atlantic DSDP Hole 609, 611 (inferred age, ref. g); and 642 (paleomag calibration, ref. h).
	Globorotalia miotumida (conomiozea) (FCO)	7.24		Cycle-calibrated in Eastern Mediterranean and Morocco -- Refs 25-30 & 34; in GTS2004 Neogene foraminifer table.  Miocene foram 'Globorotalia conomiozea' FAD marks the Tortonian/Messinian boundary in Cretan sections (ref. h), and base of Medit. Zone Mt 10.  Berggren et al. (1995) assigns as C3Br.1r; '7.12' Ma [i] = C3Br.1r.35.  The FAD is recorded in mid-C3An in Mediterranean in ref. g; see also refs. a & b.  Paleomagnetic age esimate (Berggren et al., 1995) agrees closely with 7.26 Ma for Tort/Mess boundary in NE Appenines, based on Ar 40/39 age of 7.33 Ma just below FAD of Gt. conomiozea (Vai et al., 1993).
	Globorotalia suterae 	7.86		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia suterae' FAD is recorded in Hole 654, Mediterranean.  Paleomagnetic estimate (C4n.2n; 7.8 Ma [j]) agrees perfectly with Ar 40/39 age of 7.72 _0.15 Ma on this datum in northern Appenines (Vai et al., 1993).  Set as C4n.2n.6.
	Globorotalia cibaoensis	7.86		NOTE:  Hirsutella cibaoensis (which seems to be same species) had FAD reported 1.6 myr older (9.44) by Lourens et al. (GTS2004) from astronomical scaling in Atlantic (see below).  Age of Glob. cibaoensis used here is same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia cibaoensis' FAD is recorded in Hole 806B (Ontong-Java Plateau).  Age estimate in ref. e (Table 3) of 6.7 Ma calibrated to Berggren et al. (1985) is incorrect.  Note that FAD of Gt. cibaoensis is at virtually same level as FAD of Gt. plesiotumida (266m), but this level was incorrectly estimated as 297m in ref.e (Table 2; plotted in Fig. 6).  FAD's of Ft. junai, Candeina nitida, and Globigerinoides extremus were similarly misinterpreted in ref.e in Hole 806B, but corrected by Berggren et al. (1995).  They place at C4n.2n; (7.8 Ma) [e] = C4n.2n.6.
	Globorotalia miotumida (conomiozea)	7.89		Cycle-calibrated in Eastern Mediterranean -- Refs 28 & 30; in GTS2004 Neogene foraminifer table
	Globorotalia juanai	8.15		NOTE:  Hirsutella juanai (which seems to be same species) had FAD reported 1.5 myr older (9.69) by Lourens et al. (GTS2004) from astronomical scaling in Atlantic (see below).  Age of Glob. juanai used here is same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia juanai' FAD is recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They place at (C4r.1r); (8.1) [e] = C4r.1r.7.
	Candeina nitida	8.43		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign age from Miocene foram 'Candeina nitida' FAD as recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They assign as (C4r.1r); (8.1) [e] = C4r.1r.7.
	Neogloboquadrina humerosa	8.53		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides extremus' FAD is recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They assign as C4r.2r; 8.5 Ma [b] = C4r.2r.5.
	Neogloboquadrina pachyderma	9.36		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina pachyderma' FAD is calibrated in Holes 748, 751 (Kerguelen Plateau, south Indian Ocean) = C4Ar.1n; > 9.2 Ma [k] = C4Ar.1n.5.
	Hirsutella juanai	9.69		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita apertura	11.18		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita decoraperta	11.49		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina gr.	11.78		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table
	Globorotalia lenguanensis	12.84		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Fohsella fohsi	12.85		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Sphaeroidinellopsis subdehiscens	13.02		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Fohsella (Globorotalia) fohsi "lobata"	13.41		Species "lobata" apparently combined with Fohsella "fohsi" in zonal scheme of Lourens et al. (in GTS2004).  This effectively removed the thin "M8" of Berggren et al., 1995.  Berggren et al. (1995) -- Miocene foram 'Globorotalia fohsi lobata' FAD is based on revised interpretaion of magnetostratigraphy of Hole 563 (ref. f), which indicates this FAD is in C5Ar.1r (ref. 15) rather than C5Ar (ref. b) = C5Ar.1r; 12.5 Ma [t] = C5Ar.1r.6.
	Neogloboquadrina nympha	13.49		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina nympha' FAD is recorded in Holes 747A, 751, Kerguelen Plateau (ref. k).  In Hole 608, the FAD occurs in sample assigned to polarity chron C5AAr, just above C5ABn (ref. o) = C5ABn; 13.4 Ma [k,o] = C5ABn.5.
	Praeorbulina circularis	14.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) had a much older age using C5Cn.1n (upper); 16.0 Ma [b] = C5C.1n.95.
	Globigerinoides diminutus 	16.06		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides diminutus' FAD is discussed in remarks in ref.b = (C5Cn.2n); (16.1 Ma) [b] = C5Cn.1n.7.
	Praeorbulina  curva	16.27		Same chron-age calibration as Berggren et al. (1995) = mid-C5Cn; 16.3 Ma [b] = base C5Cn.1n.
	Globorotalia miozea	16.70		Same chron-age calibration as Berggren et al. (1995) -- However, see NOTE on Praeorbulina sicana age.  They note Miocene foram 'Globorotalia miozea' FAD is recorded in Hole 751, Kerguelen Plateau, south Indian Ocean = C5Cn.3n (lower); 16.7 Ma [k] = C5Cn.3n.1, and used to define base of Medit. Zone Mt4. 
	Globorotalia birnageae	16.70		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia birnageae' FAD is calibrated in Hole 516, South Atlantic (ref. b) = C5Cn.3n (lower); 16.7 Ma [b] or 17.8 Ma [u] = C5Cn.3n.1.  Subzone "M4b" is 'Globigerinoides bisphericus Partial Range Zone' (FAD of Globorotalia birnageae to FAD of Praeorbulina sicana) (Berggren et al., 1995).  This short subzone spans the upper part of the 'N7' zone -- and now seems to be entirely WITHIN Zone M5 (after cycle-calibration).  The FAD of G. birnageae is difficult to determine precisely because of its intergradation with Gl. trilobus s.str.
	Globorotalia praescitula	18.29		Same chron-age calibration as Berggren et al. (1995), who used to define base of Medit. Zone Mt3 -- Miocene foram 'Globorotalia praescitula' FAD is recorded in Holes 747A, 748B, 751 (ref. k), 608 (ref. l); and is recorded in lowest part of polarity zone C5En in Hole 516F (ref. b) = C5En; 18.5 Ma; [k,l] = C5En.5.
	Globigerinoides altiaperturus	20.06		Used by Berggren et al. (1995) as "working"  base of Burdigalian stage -- but 2004 working definition is FAD of nanno H. ampliaperta, as calibrated at Ceara Rise = about 0.4 myr older.  Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides altiaperturus' FAD is recored in Hole 516F, South Atlantic (ref. b); and is within in older part of polarity chron C6r in Contessa Highway section (ref. q) = C6An (upper); 20.5 Ma [b,q] = base C6r.  NOTE:  Berggren's derived age implies that he assigned this FAD to the base of polarity chron C6A; thereby effectively defining the base of the Burdigalian as base of C6A; which would be more convenent and global than a biostratigraphic event!
	Globorotalia incognita	20.93		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia incognita' FAD is recorded in Hole 747A (ref. 11); with magnetostratigraphy reinterpreted in ref. o =C6Ar; 21.6 Ma [k] = C6Ar.4.
	Globoquadrina dehiscens forma spinosa	21.44		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina dehiscens forma spinosa' FAD is recorded in Hole 516F, South Atlantic (ref. b) = C6AAr.1n; 22.2 Ma [b] = C6AAr.1n.5.
	Globigerinoides primordius (FCO)	23.58		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerinoides primordius' (CO) is recorded in Hole 516F (ref. a) = C6Cr; 24.3 Ma [a] or 23.45 Ma? [g] = C6Cr.7.
	Paragloborotalia pseudokugleri	25.40		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Paragloborotalia (formerly Globorotalia) pseudokugleri' FAD is recorded in polarity zone C8n in Hole 803D and in C7n in Hole 628A (ref. c) = C8n; 25.9 Ma [c] = C8n.1n.3.
	Globigerinoides primordius	26.32		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Blobigerinoides primordius' FAD is recorded in Hole 628A (ref. c); and occurs in polarity zone C7n (ref. a) = C8r; 26.7 Ma [c] = C8r.7.
	Globigerinita  boweni	28.45		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerinita boweni' FAD is recorded in Hole 747A (ref. e) = C10n (mid); 28.5 Ma [e] = base C10n.1n
	Tenuitellinata juvenilis	29.80		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Tenuitellinata juvenilis' FAD occurs within an interval of 'no polarity data' between two normal polarity intervals interpreted as parts of polarity chron C11 in Hole 747A (ref. e) = (C11n); (29.7 Ma) [e] = C11n.1r.5.
	Paragloborotalia opima opima	30.77		Oligocene foram 'Paragloborotalia opima opima' = only 'P. opima' in Berggren 1995 SEPM) chart.  Berggren & Miller (1988, p.377) discuss 'opima' subspecies. Same chron-age calibration as Berggren et al. (1995) -- FAD is recorded in Holes 558 and elsewhere (ref. a) = C12n (mid); 30.6 Ma [a] = C12n.5.
	Cassigerinella chipolensis	33.84		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Cassigerinella chipolensis' FAD is recorded in St. Stephen's Quarry, Alabama borehole (ref. f) = C13r; 33.65 Ma [f] = C13r.9.
	Cribrohantkenina inflata	35.55		Eocene foram 'Cribrohantkenina inflata' FAD was used previously as P15/P16 boundary (e.g., Blow, 1979; Berggren and Miller, 1988); but discontinued by Berggren et al. (1995).  Same chron-age calibration as Berggren et al. (1995) --  FAD occurs between FAD of 'Isthmolithus recurvus' and LAD of 'P. semiinvoluta' and 'T. pomeroli' in Spain (Molina, 1986; Monechi, 1986; Molina et al., 1986).  FAD of 'I. recurvus' is in polarity chron C16.n2 (refs. a-d) and LAD of 'T. pomeroli' and 'P. semiinvoluta' occur in C15r in Contessa Highway (ref. a-c) or C16n2, in Massignano section (ref. d); which suggests that FAD of 'C. inflata' corresponds approximately with C16.n2. The FAD is not considered unequivocally determined (ref. c).  Brief overlap of 'C. inflata' and 'P. simiinvoluta' shown in the upper part of G. semiinvoluta Zone = lower Foram Zone P16 of Blow, 1979) in Toumarkine and Luterbacher (1985).  Approximate Chron assignment = C16n or oldest part of C15; (35.5 Ma) [c,d] = C16n.1n.1.
	Turborotalia pomeroli	41.50		Same chron-age calibration as Berggren et al. (1995) = C19r; 42.4 Ma [a] = C19r.1.
	Globigerapsis index	41.94		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Globigerapsis index' FAD is recorded near polarity zone C20n/C20r boundary in Hole 689B (ref. f) = C20n ; 42.9 Ma [a] = C20n.7.
	Morozovella lehneri	42.48		Same chron-age calibration as Berggren et al. (1995) = C20n; 43.5 Ma [a] = C20n.25.
	Subbotina possagonensis	45.09		Same chron-age calibration as Berggren et al. (1995) = C20r; 46.0 Ma = C20r.1.
	Acarinina  pentacamerata	50.77		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina pentacamerata' FAD is recorded at top of polarity zone C23n in Hole 689 (ref. m) = C23n.1n (upper); 50.8 Ma [f] = C23n.1n.8.
	Morozovella lensiformis	54.52		P6b base of Berggren et al, 1995, was either M. formosa or M. lensiformis.  Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella lensiformis' FAD is recorded in Hole 550 (refs. g,h) and 577 (ref. i) = C24r; 54.0 Ma [g-i] = C24r.75.
	Morozovella formosa gracilis, Muricella broedermanni	55.32		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella formosa gracilis' FAD is recorded in Hole 550 (refs. g,h).  Eocene foram 'Muricella broedermanni' (formerly 'Igorina broedermanni') FAD is recorded in Hole 550 (refs. g,h) = C24r (mid); 54.7 Ma [g-i] = C24r.47.
	Morozovella marginodentata	55.44		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella marginodentata' FAD is recorded in Hole 550 (refs. G,h); and Hole 577, at the top of polarity chron C25n (ref. e) = C24r (lower); 54.8 Ma [g-i] = C24r.43.
	Globanomalina australiformis	55.73		Marker for Paleo/Eoc in high southern lat.  Set here as equal to PE boundary.  Discussion of calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomallina australiformis' FAD is used to denote Paleocene/Eocene boundary in high latitudes [= AP4/5 boundary of Stott and Kennett (1990)] is recorded in Holes 689B and 690B (ref. f).  This FAD is recorded also at Sites 738 (ref. l) and 747 and 748 (ref. e), but with no paleomagnetic control.  Set here as C24r; 55.5 Ma [c] on Berggren et al'95 scale = lower-mid C24r.
	Morozovella subbotinae	56.67		M. subbotinae FAD = alternate base-P5 zone marker.  This event was used to define the base of Foram Zone 'P6a' by Berggren and Miller (1988), but Berggren et al. (1995) consider that the expression of this FAD is commonly delayed in cores due to a widespread dissolution event(s) during polarity chron C24r.  Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella subbotinae' FAD is recorded in Hole 577 = C25n (upper); 55.9 Ma [d,e] = base C24r.
	Morozovella aequa, Acarinina coalingensis-triplex	57.30		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella aequa' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, in association with FAD of Acar. coalingensis-triplex group and Acar. soldadoensis (Berggren et al., 1995, SEPM).  Paleocene foram 'Acarinina coalingensis-triplex' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM).  Chron assignment = C25r; 56.5 Ma [a] = C25r.9.
	Acarinina subsphaerica, Acarinina acarinata, Acarinina mckannai	59.90		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Acarinina acarinata',  'Acarinina mckannai' and  'Acarinina subsphaerica' FADs are calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A  (Berggren et al., 1995, SEPM).   The FAD's of three acarininids (acarinata, subsphaerica, mckannai) are observed to coincide closely with the FAD of Gl. pseudomenardii (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 59.1 Ma [a] = C26r.6.
	Morozovella velascoensis	60.78		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella vellascoensis' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM) = C26r; 60.0 Ma [a,b] = C26r.3.
	Praemurica strabocella	61.21		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica strabocella' FAD occurs in Holes 384 and 758A midway between FAD of Moro. angulata and FAD of Muri. albeari, and in Nannofossil Zone NP5.  However, it is recorded in Hole 690 in lower Zone CP5 (=NP6, ref.b); in Hole 689B in CP8 (=NP9) but equated with C26n (ref.2); and in Hole 738 at CP 4/5 (=NP 5/6) boundary (ref.j) (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 60.5 Ma [a] = C26r.15.
	Morozovella conicotruncata	61.65		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella conicotruncata' FAD occurs at virtually the same level as FAD of Moro. angulata in Holes 384, 465, 758A (ref.a) and 577 (ref. f,g), although the definite position in Hole 577 is difficult to determine because of absence of C27n (Bleil, 1985).  Paleocene foram 'Muricella pusilla' (called 'Igorina pusilla' in Berggren & Miller, 1988)FAD is recorded in lower part of polarity chron C26r and top of Nannofossil Zone CP3 (= NP3) in Hole 577 (refs. d,e), but precise position is difficult to determine because of absence of C27n and possible unconformity just above C28n at 102.95 m (see Bleil, 1985:449-450).  This FAD occurs at same level as FAD of Moro. angulata and Moro. coniscotruncata in Holes 465 and 758A (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 61.0 Ma [a,e] = base C26r.
	Praemurica praeangulata	61.92		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica praeangulata' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A [see comments for 'Moro. angulata'], and occurs at approximately the same level in Holes 738 (ref. j) and 750A (Berggren et al., 1995, SEPM).  Chron assignment = C27n (lower); 61.2 Ma [a] = C27n.2.
	Globanomalina imitata	61.98		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomalina imitata' FAD is recorded in Holes 689B and 690B (ref. c) = (?lower C27n); (~61.3 Ma) [c] = base C27n.
	Parasubbotina varianta	63.56		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parasubbotina varianta' is recorded in Hole 384 at mid-Nannofossil Zone NP2, and at comparable level by correlation in Hole 750A (Berggren et al., 1995) = C28n (middle); 63.0 Ma [a] = C28n.55.
	Parasubbotina pseudobulloides	65.19		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parasubbotina pseudobulloides' (='Subbotina pseudobulloides' in Berggren & Miller, 1988) is recorded in Hole 738 (ref. k, Hole 384 (ref. g) and Agost, Spain (ref. l); first common occurrence (FCO) noted in older part of polarity chron C29N in Holes 689, 690 (ref. b).  Its FAD may slightly overlap LAD of P. eugubina (review in Berggren et al., 1995).  {In the SEPM Table 8 of Berggren et al.,1995, P. pseudobulloides FAD was accidentally labled "p. eugubina FAD".}.  Chron assignment = just below C29r/n boundary; 64.8 Ma [a,c,g,j,k] = C29r.9.
	Contusotruncana contusa	69.49		Chron C31r.60  (ODP 171B table, in turn from Erba et al, 1995).  This FAD is a poor marker (Paul Sikora, pers. Commun., 2005).  C. contusa is not listed in SEPM98, but is secondary marker for base of R. fructicosa zone.
	Globotruncana lapparenti, Globotruncana linneiana	70.40		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 25% up in Chron C31r.
	Pseudoguembelina palpabra	71.88		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 72% up in Chron C32n.2n.
	Planoglobulina acervulinoides	72.35		SEPM'98 places at Chron C32n.40
	Pseudoguembelina excolata	73.27		Same level (mid-C32r.1n.50) as FAD G. aegyptiaca.  EGI database (Paul Sikora, 2005) calibrates Ps. excolata FAD at 72.7 Ma; about 0.5 myr younger.
	Pseudotextularia elegans	74.47		SEPM'98 places at Same level (C33n.85) as LAD G. calcarata
	Globotruncanella havanensis	75.07
	Pseudoguembelina costulata	81.61		SEPM'98 has at Chron C33r.45
	Sigalia decoratissima carpathica	84.94		SEPM'98 assigns as Base of Middle Santonian.
	Archaeoglobigerina bosquensis	88.43		Useful marker just above (ca. 0.15 myr) base of Middle Coniacian (EGI database, Paul Sikora, 2005)
	Pseudotextularia nuttalli	89.27		Base of Coniacian on SEPM'98 chart.
	Marginotruncana coronata	91.31		Useful marker at mid-Middle Turonian (EGI database, Paul Sikora, 2005)
	Whiteinella archaeocretacea, Heterohelix globulosa (=reussi)	94.55		SEPM'98 places arbitrary (?) 1.0 myr before top of Cenomanian
	Whiteinella aprica	94.75		Useful marker at base of Late Cenomanian (EGI database, Paul Sikora, 2005)
	Biticinella breggiensis	106.42		Same assignment as SEPM'98 "for now" = Base of Mortoniceras inflatum Zone;  but NOTE that it now coincides with FAD of T. praeticinensis.  FAD of B. breggiensis is used as base of a B. breggiensis Foram Zone in some scales


Additional Neogene Foram FAD/LAD	event		241/244/181		off
EVENT
	Pulleniatina (Atl.) -- reappearance	2.26		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
LAD
	Globoturborotalita obliquus	1.30		Astronomically tuned from ODP Sites 925 & 926.  Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina acostaensis	1.58		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita apertura	1.64		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Menardella exilis	2.09		Atlantic Ocean only; former genus was Globorotalia.  Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assign to Reunion Subchron; 2.15 Ma [a] = C2r.2n.5.
	Menardella limbata	2.24		Astronomically tuned from ODP Legs 111 & 138 (Refs 1, 2, 5 & 6; in GTS2004 Neogene foraminifer appendix).  This LAD occurs earlier (2.39 Ma) at Atlantic Sites 925 & 926 (Refs 7-9 in GTS2004 Neogene foram appendix).
	Globoturborotalita woodi	2.30		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Globoquadrina baroemoenensis	3.23		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globorotalia plesiotumida	3.77		 Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globorotalia nicolae	6.72		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Globorotalita challengeri	9.99		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Cassigerinella chipolensis	10.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Clavatorella bermudezi	12.00		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Cassigerinella martinezpicoi	13.27		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Clavatorella bermudezi -- top of regular	13.82		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix
	Globorotalia archeomenardii	13.87		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Globiquadrina binaiensis	19.09		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Globorotalia mendacis	23.03		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globorotalia mendacis' LAD is recorded in Hole 516F (ref. a) = C6Cn.2n; 23.8 Ma [a] = base C6Cn.2n.
FAD
	Globigerinoides ruber rosa	0.33		Ref 15; in GTS2004 Neogene foraminifer appendix
	Globigerina cariacoensis	1.78		Mediterranean datum.  Top C2n = Same chron-age calibration as Berggren et al. (1995) = top Olduvai (Medit.); 1.7 Ma; [c,d]
	Pulleniatina finalis	2.04		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Truncorotalia (Globorotalia) truncatulinoides [Pacific]	2.58		base C2r = Same chron-age calibration as Berggren et al. (1995) = Gauss/Matuyama boundary; 2.58 Ma [l]
	Globorotalia crassaformis (S coiling)	2.91		Mediterranean coiling change D->S.  C2An.1n.25 = Same chron-age calibration as Berggren et al. (1995) = C2An.1n (late Gauss); 2.92 Ma [c,k].
	Globorotalia crassaformis (D coiling)	3.00		Mediterranean coiling changes.  C2An.1n.1 = Same chron-age calibration as Berggren et al. (1995) = C2An.1n (late Gauss); 3.00 Ma [c,k].
	Globorotalia crassaformis (S coiling)	3.16		Mediterranean coiling changes.  Same chron-age calibration as Berggren et al. (1995) = C2An.2n (late Mammoth, early Kaena); 3.17 Ma [c,k] = C2An.2n.5 
	Globorotalia inflata	3.24		Same chron-age calibration as Berggren et al. (1995) = top Mammoth; 3.25 Ma [a] = C2An.2r.7.  They note that this FAD occurs about 1 myr later (early Matuyama, or about 2.09 Ma) in Mediterranean [ref. f,g,h] and North Atlantic [ref. b] than in South Atlantic (e.g., Berggren et al., in DSDP Leg 72 volume).  In Berggren et al.'s (1995, GSA Bull.) table 5; the S. Atlantic age was apparently accidentally deleted; but should be top of Mammoth chron, or about 3.25 Ma (as in earlier draft of this paper).
	Globorotalia crassaformis (D coiling)	3.26		Mediterranean coiling change.  Same chron-age calibration as Berggren et al. (1995) = mid-Mammoth; 3.26 Ma [c,k] = C2An.2r.6.
	Globorotalia tosaensis	3.35		Same chron-age calibration as Berggren et al. (1995) = just below Mammoth; 3.35 Ma [c,k] = C2An.3n.92.
	Menardella pertenuis	3.52		Genus was "Globorotalia" in SEPM/98 and Berggren et al.'95. Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C2An.3n; 3.45 Ma [a] = C2An.3n.5.
	Menardella exilis	4.45		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Sphaeroidinellopsis kochi	4.53		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globorotalia humilis	5.81		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globigerinoides conglobatus	6.20		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina acostaensis (dex.)	6.58		S-> D coiling.  Same chron-age calibration as Berggren et al. (1995) = C3An.2n; 6.2 Ma [c] (?6.4Ma?) = C3An.2n.5
	Neogloboquadrina acostaensis (sin.)	6.81		D-> S coiling.  Same chron-age calibration as Berggren et al. (1995) = C3An.2r; 6.6 Ma [c] = C3Ar.8.
	Catapsydrax parvulus	7.45		Cycle-calibrated in Eastern Mediterranean -- Refs 28 & 30; in GTS2004 Neogene foraminifer table
	Hirsutella cibaoensis	9.44		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globorotalia partimlabiata	9.94		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table
	Menardella limbata	10.64		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globorotalita challengeri	11.22		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Globorotalia praemenardii	14.38		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Clavatorella bermudezi	14.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Globorotalia archeomenardii	16.26		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Globigerinatella sp.	19.30		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Globiquadrina binaiensis	19.30		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Globigerinoides trilobus s.l.	22.96		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix


All Foram Datums Combined	event		241/244/181		off
LAD
	Globorotalia flexuosa	0.07		~C1n.913 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 4); 0.068 Ma [g]
	Globoquadrina pseudofoliata	0.22		C1n.715 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 7); 0.22 Ma [b]
	Globorotalia tosaensis	0.61		Base Pt1b (Top Pt1a).  Astronomically tuned from ODP Legs 111 & 138. = Refs 1 & 2; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had assigned as early Brunhes ; 0.65 Ma ; [a,e] = C1n.165; and noted that Pleistocene Foram Globorotalia tosaensis LAD is placed earlier, at Latest Brunhes-Jaramillo (0.8-1.0 Ma) by Caproniere et al. (1994).
	Globoturborotalita obliquus	1.30		Astronomically tuned from ODP Sites 925 & 926.  Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Pulleniatina finalis	1.39		Same chron-age calibration as Berggren et al. (1995) = midway between Olduvai and Jaramillo; 1.40 Ma [a,b] = C1r.3r.66
	Neogloboquadrina acostaensis	1.58		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita apertura	1.64		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Globigerinoides fistulosus	1.77		Base Pt1a (Top PL6).  Astronomically tuned from ODP Legs 111 & 138 (Pacific); but LAD occurs earlier (1.88 Ma) at Atlantic Sites 925 & 926 -- Refs 3 & 4; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had assigned as just above Olduvai; 1.6 Ma [a] = C1r.3r.3
	Globigerinoides extremus	1.98		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned to top Olduvai (C2n); 1.77 Ma ; [a,c,d] = top C2n.
	Menardella exilis	2.09		Atlantic Ocean only; former genus was Globorotalia.  Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assign to Reunion Subchron; 2.15 Ma [a] = C2r.2n.5.
	Menardella limbata	2.24		Astronomically tuned from ODP Legs 111 & 138 (Refs 1, 2, 5 & 6; in GTS2004 Neogene foraminifer appendix).  This LAD occurs earlier (2.39 Ma) at Atlantic Sites 925 & 926 (Refs 7-9 in GTS2004 Neogene foram appendix).
	Globorotalia pertenuis	2.30		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Genus was "Globorotalia" in SEPM/Berggren, who assigned to top Gauss Subchron; 2.60 Ma [a] = C2An.1n.95.
	Globoturborotalita woodi	2.30		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Menardella (Globorotalia) miocenica (Atl.), Globorotalia pseudomiocenica (Indo-Pac)	2.39		Dual markers for Base of PL6 [or, due to LADs, the top of PL5.  (Atlantic reappearance of Pulleniatina near this level [ref. a]).  Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix.  Essentially same as Berggren et al (1995), who assigned to early Matuyama (below Reunion Subchron); 2.30 Ma [a] =C2r.3r.8. 
	Globoturborotalita decoraperta	2.75		Astronomically tuned from ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Menardella multicamerata	2.98		Formerly assigned as genus Globorotalia.  Astronomically tuned from ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as C2An.1r (Kaena); 3.09 Ma [a] = C2Ar.1r.3.
	Dentoglobigerina altispira	3.13		Base PL5 (or, due to LAD, top of PL4; and alternate for top of N20 -- see comments on PL5 Zone).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  This LAD is reported as slightly earlier (3.19 Ma) in eastern Medit. (Refs 17, 22, 23) and much earlier (3.47 Ma) at Pacific ODP Legs 111 and 138 (Refs 1, 2, 5, 6) -- GTS2004 Neogene foram table.  Berggren et al. (1995) had similar assignment -- C2An.1r (Kaena); 3.09 Ma [a] ; {But 0.08 myr earlier in Medit. in late Mammoth, early Kaena; or about 3.17 Ma; ref. c,k).}, or a calibration of about C2Ar.1r.3.
	Sphaeroidinellopsis seminulina	3.14		Base PL4 (or, due to LAD, then top of PL3, and alternate for top of Zone N20).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  This LAD is reported as slightly earlier (3.17 Ma) in eastern Medit. (Refs 17, 22, 23) and much earlier (3.59 Ma) at Pacific ODP Legs 111 and 138 (Refs 1, 2, 5, 6) -- GTS2004 Neogene foram table.  Berggren et al. (1995) assigned as base Kaena; 3.12 Ma [b] = C2An.1r.0; and noted that Pliocene foram 'Sphaeroidinellopsis seminulina' LAD occurs about 0.1 m.y. earlier (top of Mammoth, or 3.21 Ma) in Mediterranean (refs. c,e,f,k).   NOTE that calibrations imply NO DURATION of Zone PL4 in Atlantic; and extremely brief (but earlier) elsewhere.  To avoid confusion on graphics, the base of PL4 has been lowered by 0.01 myr (3.14 Ma, instead of 3.13 Ma in Lourens et al., 2004 compilation).
	Hirsutella cibaoensis	3.23		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globoquadrina baroemoenensis	3.23		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globorotalia sp.cf. G.  crassula	3.29		North Atlantic LAD.  Same chron-age calibration as Berggren et al. (1995) = lower Mammoth; 3.30 Ma [b] = C2An.2r.3.
	Pulleniatina (Atl.)	3.41		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) have similar calibration as C2An.3n; 3.45 Ma [a] = C2An.3n.5.
	Pulleniatina primalis	3.66		Same chron-age calibration as Berggren et al. (1995) = late Gilbert reversed; 3.65 Ma [a] = C3Ar.9.
	Globorotalia plesiotumida	3.77		 Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Hirsutella (Globorotalia) margaritae	3.81		Defines top of PL2; (was approx. base of Piacenzian stage in Berggren et al., 1995).  Cycle-calibrated in Eastern Mediterranean -- Refs 17, 23 & 24; in GTS2004 Neogene foraminifer appendix.  This LAD is reported slightly earlier (3.85 Ma) at Atlantic Sites 95 & 926 (Refs. 8-10) in GTS2004 Neogene foram table.  Berggren et al. (1995) assigned as Gauss/Gilbert boundary; 3.58 Ma [a,o] = Base C2An.3n.  They noted that Pliocene foram 'Globorotalia margaritae' LAD is reported to occur 0.2 m.y. earlier (late Gilbert, or 3.79 Ma) in Mediterranean (refs. c,f,g,k).  The LCO occurs in the Mediterranean just above Cochiti Subchron (3.96 Ma) [ref. c,k]. 
	Pulleniatina spectabilis	4.21		Same chron-age calibration as Berggren et al. (1995) = top Cochiti Subchron; 4.20 Ma [a] = C3n.1n.8.
	Globoturborotalita nepenthes	4.37		Base PL2 (or, due to LAD, Defines top of PL1; & N19/N20 boundary.).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as top Cochiti Subchron; 4.20 Ma [a] = C3n.1n.8.
	Globigerinoides seiglei	4.72		Same chron-age calibration as Berggren et al. (1995) = above Sidufjall subchron; 4.7 Ma [a] = C3n.2r.5.
	Globoquadrina dehiscens	5.91		Same chron-age calibration as Berggren et al. (1995) = C3r (early Gilbert); 5.8 Ma [a-d] = C3r.15 [Datum levels in C3r scaled proportionally to match Berggren's relative spacing. ].   Miocene foram 'Globoquadrina dehiscens' LAD is calibrated in ODP Hole 588 in SW Pacific, and is synchronous in nearby Holes 586B,587,590 and in Indian Ocean (ref. c).  However, Berggren (1994 version of SEPM compilation) indicated that this LAD is apparently diachronous by about 1 myr from 3CBn (6.8 Ma) in subtropics to C3n.4r (5.5 Ma) in tropics (ref. a).   Miocene/Pliocene boundary interval Foram Zone "N18" is essentially non-existent in Berggren's table and GTS2004, because its base (FAD G. tumida) is now AFTER the base of N19 (FAD Sphaeroidinella dehiscens).
	Globorotalia lenguaensis	6.14		Miocene foram 'Globorotalia lenguaensis' LAD defines top of M13.  Same scaling as Berggren et al. (1995) -- LAD is directly calibrated to C3An.1n in ODP Hole 840 (Tonga Platform; ref. d) and Hole 806B (Ontong-Java Plateau in equatorial West Pacific; ref. 5).  This LAD occurs just below FAD of Pull. primalis at ODP 840 and just above it at ODP 806B.  The corresponding age is about 6.0 Ma (Cande-Kent, 1995).  However, LAD occurs much earlier in the Atlantic:  In Hole 519 (S. Atl.), LAD of G. lenguaensis has been calibrated to upper C4An (about 8.7 Ma; refs. r,s).  In E68-136 (Gulf of Mexico), the LAD occurs about 10m above the FAD of Globorotalia plesiotumida (=base of Foram Zone N17) and within range of Minylitha convallis and above the LAD of Discoaster bollii.  In contrast, in E66-73, the LAD is at the same level as FAD of G. plesiotumida, and below the FAD of M. convallis and LAD of D. bollii (Zhang et al., 1993; Aubry, 1993). Chron-age assignment = C3An.1n; 6.0 Ma [d] =C3An.1n.5. 
	Globorotalia miotumida (conomiozea)	6.52		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Globorotalia nicolae	6.72		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Globorotalia lenguaensis (Atl. only)	8.97		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  See NOTE above for Pacific LAD of ~6.14 Ma.
	Globorotalita challengeri	9.99		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina  nympha	10.20		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina nympha' LAD is calibrated in Holes 748, 751 (Kerguelen Plateau, south Indian Ocean) = C5n.2n; 10.1 Ma [k] = C5n.2n.8.
	Paragloborotalia siakensis	10.46		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  However, this LAD is reported to be much older (11.2 Ma) in Medit. (Refs. 31 & 32) in GTS2004 Neogene foram table; therefore it is used as base of Zone MM10.  Table by Lourens et al (GTS2004) also uses LAD of P. siakensis to mark their version of M11/12 and N14/15 zonal boundaries; but this would be diachronous with Atlantic.
	Cassigerinella chipolensis	10.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina mayeri	11.47		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina mayeri' LAD is in the lower part of Buff Bay Formation at Buff Bay, Jamaica, 8 cm above FAD of 'Discoaster hamatus' (Berggren, 1993; Aubry, 1993).  In Bodjonegoro 1 borehole (Indonesia) these two datum levels occur together (personal observation, W. Berggren & M. Aubry). In North Atlantic Sites 558, 563 (ref. b) and 608 (ref. l) LAD of 'N. mayeri' was observed in close juxtaposition with FAD of 'N. acostaensis', essentially eliminating Foraminifer Zone N15 (=M12).  This has been varyingly interpreted as due to a hiatus in the North Atlantic (Aubry, 1993) or diachrony (ref. l,m).  Therefore, their assignment is C5r.2r; 11.4 Ma [b,l-n] = C5r.2r.2.  This LAD also defined their Base of Medit. zone Mt9.
	Globigerinoides subquadratus	11.54		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Fohsella fohsi s.l.	11.79		Formerly called 'Globororotalia fohsi robusta'.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globorotalia fohsi robusta' LAD is calibrated in Hole 563 (ref. b) = C5An.1n; 11.9 Ma [b] = top C5An.1n.
	Fohsella (Globorotalia) fohsi "lobata"	11.79		Species "lobata" apparently combined with Fohsella "fohsi s.l." in zonal scheme of Lourens et al. (in GTS2004).  The result is to merge the bases of M10 and N13 zonal schemes in their system.  Berggren et al. (1995) -- Miocene foram 'Globorotalia fohsi lobata' LAD is based on reinterpretation of paleomagnetics in Hole 563, based in turn on stable isotope studies at Kerguelen Plateau Site 747 and North Atlantic Hole 608 (ref.o) = C5Ar.1r; 12.1 Ma [b,o] = C5An.1r.8.
	Globorotalia panda	11.89		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia panda' is calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean); with magnetic stratigraphy reinterpreted in ref.o = C5r.3r; 11.8 Ma [n] = C5r.3r.3.
	Clavatorella bermudezi	12.00		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Tenuitella  selleyi, pseuoedita, minutissima, & clemenciae	12.31		Same chron-age calibration as Berggren et al. (1995) -- Miocene forams 'Tenuitella selleyi' through "clemenciae" simultaneous LADs are calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean) = C5An.2n; 12.3 Ma [p] = C5An.2n.5.
	Cassigerinella martinezpicoi	13.27		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Globorotalia praescitula	13.73		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren listed LAD as much younger -- C5An.1n; 11.9 Ma [11]; therefore the cycle-calibration needs comparison to other sites.  Berggren et al's assignment of Miocene foram Globorotalia praescitula' LAD was calibrated in Hole 747A (Kerguelen Plateau, south Indian Ocean); with magnetic stratigraphy reinterpreted in ref. o = top C5An.1n.
	Fohsella peripheroronda	13.80		Formerly assigned as genus Globorotalia.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) used to define base of Medit. Zone Mt7, with age assignment of C5ADn (lower); 14.6 Ma [b] = base C5ADn = nearly 1 myr older than Atlantic-ODP assignment.
	Clavatorella bermudezi -- top of regular	13.82		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix
	Globorotalia archeomenardii	13.87		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Praeorbulina  sicana	14.53		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C5B.1n; 14.8 Ma [b] = base C5ADr.
	Globigeriantella insueta s.str.	14.66		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Praeorbulina glomerosa s.str.	14.78		Same chron-age calibration as Berggren et al. (1995) = C5B.1n; 14.8 Ma [b] = base C5ADr
	Globorotalia miozea	15.85		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia miozea' LAD is calibrated in Hole 747A, Kerguelen Plateau; as within lower polarity chron C5B.1n (ref. p) = C5Br (lower); 15.9 Ma [k] = C5Br.15.
	Globorotalia incognita	16.39		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia incognita' LAD is calibrated in Hole 747C, Kerguelen Plateau = C5Cn.2n (mid); 16.4 Ma [k] = C5Cn.2n.5.
	Globorotalia zealandica, Globorotalia semivera	17.26		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia zealandica' is recorded in Hole 747A (ref. p); and observed in lower part of polarity zone C5Dn in Hole 751 (ref.k) = C5Dn (upper); 17.3 Ma [p] = C5Dn.9.
	Catapsydrax dissimilis	17.54		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) calibrate Miocene foram 'Catapsydrax dissimilis' LAD as recorded in Holes 558, 563, North Atlantic (ref. b); and observed at top of polarity zone C5Dr in Hole 608 in interval of strong dissolution (refs. k,p) = C5Dn (upper); 17.3 Ma [p] or 18.3 [u] = C5Dn.9.
	Globoquadrina dehiscens forma spinosa	17.61		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina dehiscens forma spinosa' LAD is recorded in Hole 615, South Atlantic (ref. b) = C5Dr; 17.9 Ma [b] = C5Dr.6.
	Globiquadrina binaiensis	19.09		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Tenuitella munda	20.78		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Tenuitella munda' LAD is recorded in Hole 747, Kergulen Plateau (ref. p); with the magnetostratigraphy reinterpreted in ref. o = C6Ar; 21.4 Ma [p] = C6Ar.8.
	Globoturborotalita angulisuturalis	20.93		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoturborotalita angulisuturalis' LAD is recorded in Hole 516F (ref. b); with magnetostratigraphy reinterpreted in ref.o = C6Ar; 21.6 Ma [b] or 22.6 Ma [u] = C6Ar.4.
	Paragloborotalia kugleri	21.12		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) use this level as base of Medit. Zone Mt2, and note that Miocene foram 'Paragloborotalia (formerly Globorotalia) kugleri' LAD is recorded in Hole 516F, South Atlantic (ref. b), and at base of polarity zone C6An in Contessa Highway section (ref. q) = C6Ar; 21.5 Ma [b,q] = C6Ar.6.
	Paragloborotalia pseudokugleri	21.31		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) have similar age -- Miocene foram 'Paragloborotalia (formerlyGloborotalia) pseudokugleri' LAD is recorded in Hole 516F (ref. b); with magnetostratigraphy reinterpreted in ref.o = C6Ar; 21.6 Ma [b] = C6Ar.4.
	Globoquadrina globularis	21.98		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina globularis' LAD is recorded in Hole 516F, South Atlantic (ref. b) = C6Bn.1r; 22.8 Ma [b] = C6Bn.1r.3.
	Globigerina ciperoensis	22.90		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Globigerina euapertura	23.03		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerina euapertura' LAD is recorded near top of polarity chron C6Cn in Hole 748B and near base C6Cn in Holes 747A and 747B (ref. b) = C6Cn.2n; 23.8 Ma [b] = base C6Cn.2n.
	Globorotalia mendacis	23.03		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globorotalia mendacis' LAD is recorded in Hole 516F (ref. a) = C6Cn.2n; 23.8 Ma [a] = base C6Cn.2n.
	Tenuitella gemma	23.58		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Tenuitella gemma' LAD is recorded in Hole 747A (ref. e) = C6Cr; 24.3 Ma [e] = C6Cr.7.
	Paragloborotalia opima	26.83		Oligocene foram 'Paragloborotalia opima opima' (Berggren & Miller, 1988) defines top of P21.  This was called "G. opima opima" by Blow (1969), and is listed as only "P. opima" in Berggren 1995, SEPM). Same chron-age calibration as Berggren et al. (1995) -- The LAD is recorded between polarity zones C9n and C8n in Hole 516F (ref. a); individuals become significantly smaller above C9n and are not typical of 'P. opima s.s.' in Hole 558 (ref. 1; see also discussion in Berggren and Miller, 1988) = C9n (upper); 27.1 Ma [a] = C9n.9.
	Globigerina labiacrassata	26.83		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerina labiacrassata' LAD (= P 15/16 boundary in Berggren, 1992); is recorded at top of polarity zone C9n in Holes 747A, 748B (ref. b) and 689B and 690B (ref. d) and in lower C8n  in Hole 747A (ref. e) = C9n (upper); 27.1 Ma [b,d] = C9n.9.
	Chiloguembelina cubensis (LCO)	28.45		Last Common Occurrence used to set age of Base-Chattian on SEPM chart and GTS2004.  Set equivalent to base of Chron C10n.1n.  Calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- This LAD is recorded in mid-part of polarity zone C10n in Holes 747A (ref. a,e) 749 (ref. 2), in the mid-part of concatenated C9n and C10n in Hole 748B (ref. b), and associated approximately with C10n in Holes 689B and 690B (ref. d).  Whether this datum refers to extinction or strong reduction in numbers remains a moot point; records of discontinuouss presence in reduced numbers of this taxon into basal Miocene levels continue (ref. c) (Berggren et al., 1995).  Assigned as C10n (mid); 28.5 Ma [a,b,e] = 
	Subbotina angiporoides	30.11		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Subbotina angiporoides' LAD is also the P13/P14a boundary in Stott and Kennett (1990).  This LAD is recorded in early part of polarity zone C11n in Holes 516R (ref. 1), 748B (ref. b) and 689B and 690B (ref. d) = C11n (lower); 30.0 Ma [a,b,d] = C11n.2n.3.
	Turborotalia ampliapertura	30.42		Oligocene foram 'Turborotalia ampliapertura' defines top of P19, and was formerly 'Globigerina ampliapertura' (e.g., Blow, 1969).  Age-calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- LAD is recorded in polarity zone C11r in Holes 516F and 558 (ref. a) and St. Stephen's Quarry, Alabama borehole (ref. d) = C11r; 30.3 Ma [a,f] = C11r.5.
	Pseudohastigerina naguewichiensis	32.19		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Oligocene foram 'Pseudohastigerina spp.' LAD defines top of P18, and is recorded in Holes 516F, 558, 563 (ref. a) and St. Stephen's Quarry, Alabama borehole (ref. f).   Earliest Oligocene foraminifer LAD of Psudohastigerina datum was noted as "C11r" in Berggren tables, but it seems to be a typographic error, because his age placement and chronologic order of this datum was at "32.0 Ma", hence in C12r.  Assignment is C12r; 32.0 Ma [a,f] = C12r.5.
	Hantkenina spp., Hantkenina alabamensis	33.88		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- the youngest of 3 normal "events" in polarity chron C13r in Contessa Highway section (refs. b,c) and above the normal "event" C13n.2n at Massignano (ref. d), where this LAD defines the Eocene/Oligocene boundary, and is dated radiometrically as 33.7 Ma.  Chron calibration = C13r; 33.7 Ma [a-d] = C13r.85.
	Turborotalia cerroazulensis	34.00		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia cerroazulensis" LAD defines top of P17, and is associated with youngest of 3 normal "events" in polarity chron C13r in Contessa Section (ref. b,c) and above normal "event" C13n.2n at Massignano (ref. d).  It is not absolutely clear whether the LAD of 'Hantkenina spp.' and 'T. cerroazulensis' group are synchronous or sequential.  Chron calilbration = C13r; 33.8 Ma [a-d] = C13r.75.
	Cribrohantkenina inflata	34.16		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Cribrohantkenina inflata' LAD defines top of P16, and  is located between LAD of 'Gl. index' and 'T. cunialensis' and 'Hantkenina' in mid-part of polarity chron C13r at Massignano (ref. d) and just below youngest of 3 normal "events" in C13r in Contessa Highway section (ref.b) = C13r; 34.0 Ma [a-d] = C13r.6.
	Globierinatheka index	34.47		One of the few taxa which has an LAD that is isochronous between low and high latitudes and provinces.  Age calibration from Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Eocene foram 'Globigerapsis index' LAD is essentially coincident with the LAD of 'Discoaster saipanensis' and 'Discoaster barbadoensis' and with lower of 3 normal "events" in polarity chron C13r in Contessa Highway section (refs. b,c).  This LAD occurs in younger part of polarity chron C13r on Kerguelen Plateau (Site 748) (ref. e) and appears to be globally reliable datum.  Recorded at a level in  Hole 689B (Weddell Sea) identified as C16n (ref. f), but an alternative interpretation of the paleomagnetic stratigraphy (ref. e) suggests this may be C15n, in which case the (apparent) latitudinal diachrony of the HO of Gl. index would be significantly reduced, if not eliminated, inasmuch as dissolution is strong across the Eocene/Oligocene boundary interval at high latitudes.  Chron assignment = C13r; 34.3 Ma [a-e] = C13r.3.
	Turborotalia pomeroli	35.37		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia pomeroli' LAD occurs with LAD of 'P. semiinvoluta' in polarity Chron C16n.2n in Massignano section (ref. 4) = C15r; 35.3 Ma [a-c] = C15r.1.
	Globigerinatheka semiinvoluta	35.82		Genus was formerly Porticulasphaera.  Scaling of Berggren-Pearson (2005) -- C15r; 35.3 Ma [a-c]; but Berggren-Pearson (2005) estimate as 35.8 Ma = C16n.2n.8.
	Acarinina spp.	37.24		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina spp.' LAD occurs in mid-C17n (ref. 1) or top of polarity chron C18n (ref. b,c) in the Apennines, which is about 1 myr older.  Chron assignment = mid-C17n; 37.5 Ma [a,c] = base C17n.1n.
	Subbotina linaperta, Acarinina collactea	37.43		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Subbotina linaperta' is recorded in mid-C17n in Hole 689B (ref. f) and in polarity zone C17n in Hole 748B (ref. f).  Eocene foram 'Acarinina collactea' LAD is recorded in interval of uninterpretable paleomagnetic data just above level identified as polarity chron C17n in Hole 748B (ref. e) and at level interpreted as C18n in Hole 690B (Weddell Sea (ref. f).  These LADs are grouped together in Berggren and here.  Chron assignment = C17n; 37.7 Ma [a] = C17n.2n.6.
	Morozovella crassata	37.67		M. crassata is the senior synonym of Morozovella spinulosa  Assignment by Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- C17n (lower); 38.1 Ma [a]; but 38.0 estimated by Berggren-Pearson (2005) = C17n.3n.6.
	Planorotalites	38.03		Same chron-age calibration as Berggren et al. (1995) = C18n (upper); 38.5 Ma [a,b] = top C18n.1n.
	Acarinina primitiva	38.50		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina primitiva' is recorded in mid-part of polarity chron C18n in Hole 689 (ref. f) and in interval of uninterpretable paleomagnetic data just above probable C18n in Hole 748B (ref. e).  Chron assignment = C18n; 39.0 Ma [a,f] = C18n.1n.5.
	Subbotina frontosa	38.79		Same chron-age calibration as Berggren et al. (1995) = C18n (mid); 39.3 Ma [a] = C18n.1n.2.
	Orbulinoides beckmanni	39.36		Defines top of P14 (or E13).  Age calibration by Berggren and Pearson (2005), which puts this LAD 0.1 myr higher than Berggren et al. (1995) = C18n (lower); 40.1 Ma [a]; but 40.0 Ma by Berggren-Pearson '05, following Wade (2004) using Site 1052 = C18n.2n.2.
	Acarinina bullbrooki	39.80		Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C18r; 40.5 Ma [a] = C18r.66.
	Guembelitrioides nuttalli	41.36		Age assignment by Berggren and Pearson (2005) = C19r; 42.3 Ma = C19r.25
	Morozovella aragonensis	42.60		Defines top of P11 or E9.  Age assignment by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C20n; 43.6 Ma [a] = C20n.15.
	Morozovella subbotinae, Morozovella formosa	50.77		LAD of M. subbotinae defines top of E5, and LAD of M. formosa was top of P7.  Chron-age from Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Eocene Foram Zone P8 base (LAD of 'Morozovella formosa') is drawn as uppermost C23n in chart in Aubry et al. (1988); and is shown with an age of 50.8 Ma in Berggren (1995, SEPM); but the source of these calibrations are not cited.  Assignment = uppermost C23n;  [m,h] = C23n.1n.8
	Morozovella marginodentata	53.03		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella marginodentata' LAD is recorded in Hole 550 (refs. g,h).  Berggren et al. (1995) assign an age of 52.5 Ma, but their correlation with polarity chron C24n.1r does not allow an age younger than 52.7 Ma.  Assignment = C24n.1r; 52.5 Ma [g,h] = C24n.1r.8.
	Morozovella lensiformis	53.06		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella lensiformis' LAD is recorded in Holes 550 (refs. g,h) and 577 (ref. i) = C24n.1r; 52.7 Ma [g-i] = C24n.1r.5.
	Subbotina velascoensis 	53.95		Similar chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Subbotina velascoensis' LAD is recorded in Hole 550 (refs. g,h) = C24r; 53.5 Ma [g,h] = C24r.65.  BUT, Berggren and Pearson (2005) says that that LAD of Sub. velascoensis is in Zone E3, therefore calibration shifted to C24.95 to place below base of Zone E4 [NEED TO RECHECK THIS]
	Morozovella aequa	54.09		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella aequa' LAD is recorded in Hole 550 (refs. g,h); and within polarity zone C24n1 in Hole 577 (ref. i) = C24r; 53.6 Ma [g-i] = C24r.9.
	Morozovella velascoensis	55.09		Berggren and Pearson (2005), which is puts this LAD 0.2 myr higher than Berggren et al. (1995) -- This LAD is recorded in younger part of polarity chron C24r2 in Hole 577 (ref. 9) and in mid-part C24r2 in Hole 577 (at 81.98 m) (ref. k).  However, paleomagnetic data (Bleil, 1985, DSDP Leg 86: 449, Fig. 7b) suggests a hiatus occurs between ~82m & 83 m in Hole 577, which would have the effect of depressing (rendering older) the HO of 'M. velascoensis'.  The HO of 'M. velascoensis' in Hole 577 is in Nannofossil zone CP8 (=NP9) (Monechi, 1985: 310, Table 5) which supports interpretation of hiatus in Hole 577, because the LO of 'M. valascoensis' is in Nannofossil Zone NP10.  Furthermore, Monechi (1985: p.307) indicates absence of extremely condensed sedimentation across the Paleocene/Eocene boundary interval.  Chron assignment here is C24r; 54.7 Ma [a]; but 54.5 Ma (mid-C24r) in Berggren and Pearson, 2005 = C24r.47.
	Morozovella acuta	55.32		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella acuta' LAD is recorded in Hole 550 (refs. g,h), where it occurs mideway between dated Ash Bed -17 (54.5 Ma) and +19 (54.0 Ma) [using older Ar-Ar standards, hence would shift about 0.5 myr older in GTS2004 standard].  Corresponding chron assignment would be equivalent to C24r (mid); 54.7 Ma [h] = C24r.47.
	Globanomalina pseudomenardii	56.67		LAD defines top of Zone P4.  Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomalina pseudomenardii' was called "Planorotallites pseudomenardii' in Berggren & Miller (1988).  The LAD (= base Zone P5) is recorded in Hole 577 at either base of polarity chron C24r (ref. d) and or top C25n (ref. e) and in Hole 752 at top C25n (ref. f).  Juxtaposition/overlap of Gl. pseudomenardii LAD and Gt. subbotinae FAD is observed in Holes 465 and 758 (ref. g).  Chron assignment = C25n (top); 55.9 Ma [a,d-f] = base C24r.
	Acarinina acarinata, Acarinina mckannai	57.18		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Acarinina acarinata' and 'Acar. mckannai' LAD's are calibrated in DSDP Hole 384 (N. Atl.); and at comparable levels but without paleomagnetic control in Holes 465 (Eq. Pac.) and 758A (Indian Ocean) (Berggren et al., 1995, SEPM).  Chron assignment = base C25n.
	Acarinina subsphaerica (common)	57.90		Paleocene foram 'Acarinina subsphaerica' LAD had defined base of Zone P4b of Berggren et al. (1995).  Same chron-age calibration as Berggren et al. (1995) -- This datum is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, and occurs approximately midway in Zone P4 (Berggren et al., 1995, SEPM).  Chron assignment = C26r (C25r); 57.1 Ma [a] = C25r.4.
	Parasubbotina variospira	59.99		LAD defines top of P4a (NEW version, Berggren et al, 2000).  Berggren and Pearson (2005) assignment = C26r; 59.2 Ma = C26r.57.
	Parasubbotina varianta, Parasubbotina variolaria	59.99		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Parasubbotina varianta' and 'Parasubbotina variolaria' LAD's are simultaneous in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM) = C26r; 59.2 M) [a] = C26r.57.
	Parvularugoglobigerina eugubina	65.15		Defines base of P1a.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parvularugoglobigerina eugubina' in Berggren et al. (SEPM, 1995) was called 'Globigerina eugubina' in some other publications.  The LAD, defining the top of Zone P-alpha, is near the FAD of Pa. pseudobulloides; and Berggren et al. (1995) "admittedly somewhat arbitrarily" placed both events just below the polarity chron C29n/r boundary (p.146) = just below C29r/n boundary; 64.8 Ma [a] = C29r.95.
	Racemiguembelina fructicosa, Globotruncana, Globigerinelloides, Rugoglobigerina, LADs of other Cret. Forams	65.50		Top of Cretaceous.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) = C29r.7; 65.0 Ma [multiple sources]; which is set in GTS2004 using revised Ar-Ar standard-constant as 65.5 Ma.
	Abathomphalus mayaroensis, Gansserina gansseri	65.80		SEPM'98 had assigned as ~0.3 m.y. before K/T
	Abathomphalus intermedia	66.82		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is middle of Chron C30n
	Rugoglobigerina pennyi	68.32		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 45% up in Chron C31n.
	Globotruncanella ventricosa	69.62	dashed	DASHED at Chron C31r.60
	Globotruncanita calcarata	74.47		SEPM'98 places at Chron C33n.85.
	Archaeoglobigerina bosquensis	77.79		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 2/3rds up in Middle Campanian.
	Ventilabrella eggeri	82.36		SEPM'98 has at Chron C33r.25
	Marginotruncana coronata	82.55		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age (mid-Early Campanian) assigned here as 20% up in Chron C33r to match EGI age.
	Whiteinella baltica	82.74		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Age is just below LAD of M. coronata; assigned here as 15% up in Chron C33r.
	Dicarinella asymetrica	83.53		Top of Santonian in SEPM'98
	Dicarinella concavata, Sigalia deflaensis	83.53		Top of Santonian in SEPM'98
	Sigalia decoratissima decoratissima	83.95		SEPM'98 places at About 70% up between FAD of S. dec. carpathica and LAD of S. deflaensis Forams
	Sigalia decoratissima carpathica	84.47		SEPM'98 places at About one-third up between FAD of S. dec. carpathica and LAD of S. deflaensis Forams
	Sigalitruncana sigali	84.69		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Age is "mid-Santonian".
	Whiteinella archaeocretacea	84.94		According to EGI database (Paul Sikora, 2005), this LAD goes up to approximate base of Middle Santonian (instead of mid-Coniacian on SEPM chart !! ).
	Whiteinella paradubia	86.05		Useful marker just below Inoceramus marker for base-Santonian (EGI database, Paul Sikora, 2005).  Placed here here arbitrarily as 0.2 myr below base of Santonian in GTS2004.
	Whiteinella aprica	88.58		Useful marker at base of Middle Coniacian (EGI database, Paul Sikora, 2005)
	Dicarinella hagni	89.07		Useful marker not too far above (ca. 0.2 myr?? used here) base of Coniacian (EGI database, relative placement according to Paul Sikora, 2005 -- although his quoted age of 88.3 in SEPM98 scale was nearly mid-Middle Coniacian).
	Helvetoglobotruncana helvetica	91.51		Base of  P. percarinatus ammonite zone on SEPM'98 chart. 
	Dicarinella imbricata	93.85		Useful marker just below OAE2 event (EGI database, Paul Sikora, 2005) = assigned here as 0.3 myr before base-Turonian
	Rotalipora cushmani	93.95		SEPM'98 places arbitrary (?) at 0.4 myr before top of Cenomanian (= top of Rotalipora genus?).  Caron (1985) indicates base of this zone as FAD of W. archaeocretacea, rather than LAD of R. cushmani; and  this FAD is ~0.6 myr below.
	Rotalipora reicheli, Rotalipora appenninica, Rotalipora globotruncanoides	94.75		SEPM'98 places at base of Upper Cenomanian
	Planomalina buxtorti	100.10		SEPM'98 places at 1/5 from base of M. periflatum s.z.
	Rotalipora ticinensis, Ticinella primula	100.47		SEPM'98 places LADs at 2/3 from base of M. rostratum s.z.
	Biticinella breggiensis	100.66		SEPM'98 places at 2/5 from base of M. rostratum s.z.
	Rotalipora subticinensis	101.62		Same assignment as SEPM'98 "for now" = 1/2 from base of C. auritus s.z.   Albian Foraminifer 'R subticinensis' LAD is given 2 ages in Robaszynski's chart, one is 0.13 m.y. older than the one shown here.
	Ticinella bejaouaensis	112.50		Base of foraminifer Hedbergella planispira (defines base of H. planispira foraminifer zone) is greater than 32 long-eccentricity cycles below top of Albian (base of cycle-controlled section) at Piobbico => older than 112.6 Ma.  This calibration is inconsistent, because the base of the H. planispira Zone is placed ABOVE base of P. columnata in Leckie et al. (2002), and in the middle of Lower Albian by Bellier et al. (2000).  However, Hardenbol et al. (1998) place the FAD of H. planispira below the FAD of P. columnata, as is indicated at Piobbico.  SEPM'98 had assigned as 1/2 of H. jacobi Zone. 
	Globigerinelloides algeriana	116.00		Top G. algerianus (= base of Hedbergella trocoidea or Planomalina cheniourensis Zone, depending on author; which is essentially a "gap" zone) = 116.0 Ma  (was 115.2 in Leckie's chart).  SEPM'98 had assigned as 0.1 myr before top of nufieldiensis Zone.   "gap zone" (LAD at base; FAD at top).  Not included in all foraminifer zonations.
	Leupoldina cabri	120.70		Top L. cabri (= base of G. ferreolensis zone) = 120.7 Ma (was 118.2 in Leckie's table).  SEPM'98 had assigned as 1/5 from base of martinoides Zone. 
	Globuligerina oxfordiana, G. stellapolaris, G. caucasica, G. megamonica, G. calloviensis, Globigerina helvetojurassica, Globigerina terquemi. Globigerina gulekhensis	138.74		LADs are in the early Valanginian (Cretaceous), so the age is assummed as 1/3 up from the base of Valanginian
	Globuligerina balakhmatovae	165.72		LAD is in the Late Bathonian, the age is assummed as base of the H. (P.) retrocostatum Zone
FAD
	Bolliella calida	0.22		C1n.715 = Same chron-age calibration as Berggren et al. (1995) = late Brunhes (Stage 7); 0.22 Ma [b]
	Globigerinoides ruber rosa	0.33		Ref 15; in GTS2004 Neogene foraminifer appendix
	Globorotalia flexuosa	0.40		C1n.486 = Same chron-age calibration as Berggren et al. (1995) = mid-Brunhes (Stage 11); 0.401 Ma [g]
	Globorotalia hirsuta	0.45		C1n.42 = Same chron-age calibration as Berggren et al. (1995) = mid-Brunhes (stage 12); 0.45 Ma [f]
	Globorotalia crassaformis hessi	0.75		C1n.04 = Same chron-age calibration as Berggren et al. (1995) = basal Brunhes ; 0.75 Ma ; [b]
	Globigerina cariacoensis	1.78		Mediterranean datum.  Top C2n = Same chron-age calibration as Berggren et al. (1995) = top Olduvai (Medit.); 1.7 Ma; [c,d]
	Truncorotalia (Globorotalia) truncatulinoides	2.00		Base N21&N22.  Age of 2.00 Ma calibrated in Eastern Mediterranean -- Refs 17, 20 & 21; in GTS2004 Neogene foraminifer appendix.  However, this FAD occurs slightly later (1.93 Ma) in Atlantic Sites 925 & 926 (Refs. 7-9 in GTS2004 Neogene foraminifer appendix).  Berggren et al. (1995) assign as mid-Olduvai Subchron; ~1.90 Ma [p,a,f,g,h] = C2n.4; but note that Pliocene Foram "Globorotalia truncatulinoides" FAD is 2.0 Ma (just below Olduvai) in Atl-Medit; but is much earlier at 2.58 Ma (base of Matuyama) in SW Pacfiic.
	Pulleniatina finalis	2.04		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Pulleniatina (Atl.) -- reappearance	2.26		Astronomically tuned from ODP Sites 925 & 926 -- Refs 7-9; in GTS2004 Neogene foraminifer appendix
	Truncorotalia (Globorotalia) truncatulinoides [Pacific]	2.58		base C2r = Same chron-age calibration as Berggren et al. (1995) = Gauss/Matuyama boundary; 2.58 Ma [l]
	Globorotalia crassaformis (S coiling)	2.91		Mediterranean coiling change D->S.  C2An.1n.25 = Same chron-age calibration as Berggren et al. (1995) = C2An.1n (late Gauss); 2.92 Ma [c,k].
	Globorotalia crassaformis (D coiling)	3.00		Mediterranean coiling changes.  C2An.1n.1 = Same chron-age calibration as Berggren et al. (1995) = C2An.1n (late Gauss); 3.00 Ma [c,k].
	Globorotalia crassaformis (S coiling)	3.16		Mediterranean coiling changes.  Same chron-age calibration as Berggren et al. (1995) = C2An.2n (late Mammoth, early Kaena); 3.17 Ma [c,k] = C2An.2n.5 
	Globorotalia inflata	3.24		Same chron-age calibration as Berggren et al. (1995) = top Mammoth; 3.25 Ma [a] = C2An.2r.7.  They note that this FAD occurs about 1 myr later (early Matuyama, or about 2.09 Ma) in Mediterranean [ref. f,g,h] and North Atlantic [ref. b] than in South Atlantic (e.g., Berggren et al., in DSDP Leg 72 volume).  In Berggren et al.'s (1995, GSA Bull.) table 5; the S. Atlantic age was apparently accidentally deleted; but should be top of Mammoth chron, or about 3.25 Ma (as in earlier draft of this paper).
	Sphaeroidinellopsis dehiscens s.str.	3.24		This "dehiscens" species was formerly assigned as genus Sphaeroidinella.  Same chron-age calibration as Berggren et al. (1995) = top Mammoth; 3.25 Ma [a] = C2An.2r.7.  They note that this FAD occurs about 1 myr later in Mediterannean (about 2.19 Ma) [ref. h].
	Globorotalia crassaformis (D coiling)	3.26		Mediterranean coiling change.  Same chron-age calibration as Berggren et al. (1995) = mid-Mammoth; 3.26 Ma [c,k] = C2An.2r.6.
	Globigerinoides fistulosus	3.33		Same chron-age calibration as Berggren et al. (1995) = C2An.2r (base Mammoth); 3.33 Ma [a] = C2An.2r.0.
	Globorotalia tosaensis	3.35		Same chron-age calibration as Berggren et al. (1995) = just below Mammoth; 3.35 Ma [c,k] = C2An.3n.92.
	Menardella pertenuis	3.52		Genus was "Globorotalia" in SEPM/98 and Berggren et al.'95. Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C2An.3n; 3.45 Ma [a] = C2An.3n.5.
	Menardella (Globorotalila) miocenica	3.77		Formerly assigned as genus Globorotalia, and an alternate definition for base of Zone N20-N21.   Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as C2An.3n; 3.55 Ma [a] = C2An.3n.1.
	Truncorotalia (Globorotalia) crassaformis s.l.	4.31		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assigned as Nunivak Subchron; 4.50 Ma [a,n] = C3n.2n.85.  They noted that Pliocene foram 'Globorotalia crassaformis' FAD is reported to occur about 1 m.y. later (Gilbert/Gauss boundary, or 3.58 Ma) in the Mediterranean (ref. c,k). 
	Menardella exilis	4.45		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Globoconella (Globorotalia)  puncticulata	4.52		Cycle-calibrated in Eastern Mediterranean -- Refs 17, 23 & 24; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) calibrate FAD of Pliocene foram 'Globorotalia puncticulata' to the Nunivak Subchron in the Mediterranean and elsewhere {4.50 Ma [b,c,e,f,g,k] = C3n.2n.85}.  They note that this is approximately the LAD of G. cibaoensis (~0.1 m.y. lower).
	Sphaeroidinellopsis kochi	4.53		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8-10; in GTS2004 Neogene foraminifer appendix
	Sphaeroidinellopsis dehiscens	5.53		This "dehiscens" species was formerly assigned as genus Sphaeroidinella.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign as basal Thvera Subchron; 5.2 Ma [a,o] = C3n.4n.13.  They note that Sphaeroidinellopsis spp. (top of acme) in Mediterranean was formerly reported to have approximately same age [ref. c,f,k], but now seems ~100,000yr  younger; however, Lourens et al (GTS2004) put that acme-top about 300,000 yr younger.
	Globorotalia pliozea, Globorotalia sphericomiozea	5.67		Same chron-age calibration as Berggren et al. (1995) = C3r (early Gilbert); 5.6 Ma [a] = C3r.45 [Datum levels in C3r scaled proportionally to match Berggren's relative spacing. ].  Miocene foram 'Globorotalia pliozea' FAD is dated in Hole 588 (SW Pacific) (ref.a).  G. sphericomiozea FAD is top of Zone Mt10. Miocene foram 'Globorotalia sphericomiozea' FAD is dated in Hole 588 (SW Pacific) (ref.a).
	Globorotalia tumida	5.72		Base PL1; N18 (but see Note on Glob. dehiscens).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  This FAD is reported as later (5.57 Ma) at Pacific ODP Legs 111 & 138 (Refs. 2, 5 & 6) in GTS2004 Neogene foram table.  Berggren et al. (1995) notes that Miocene foram 'Globorotalia tumida' FAD (defining base of Berggren's zone Pl 1 = Base of "Pliocene" Foram Zonation; but datum is within latest Miocene) is dated in Hole 588 and synchronouse in other SW Pacific sites (586B,587,590) and in Indian Ocean (Holes 114,219,237,238) (ref.c).  This FAD is at a comparable position, but without paleomagnetic control, at Hole 806B (Ontong-Java Plateau) (ref. d).  They assign as C3r (early Gilbert); 5.6 Ma [a-d] = C3r.45
	Globorotalia humilis	5.81		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globorotalia  margaritae	6.08		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Extensive notes in Berggren et al. (1995), who place the global FAD at C3An (mid); 6.0 Ma [a-g] = C3An.1n.5 -- Miocene foram 'Globorotalia margaritae' FAD has this age in the North Atlantic (refs. b,f,g).  The FAD is considered asynchronous between the SW Pacific and Indian Ocean (ref.c) and is observed to occur above (Hole 806B) and below (Hole 840) the FAD of G. tumida (ref. d).  The FAD is nearly 1 myr later in the Mediterranean (about 5.32), where its inital occurrence is recorded immediately above base Zanclian in mid-Thvera [mid-C3An.2n] and first common occurrence (FCO) only shortly thereafter at 5.07 Ma (Langereis and Hilgen, 1991; ref. g).
	Globigerinoides conglobatus	6.20		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Neogloboquadrina acostaensis (dex.)	6.58		S-> D coiling.  Same chron-age calibration as Berggren et al. (1995) = C3An.2n; 6.2 Ma [c] (?6.4Ma?) = C3An.2n.5
	Pulleniatina primalis	6.58		Same chron-age calibration as Berggren et al. (1995) = C3An.2n; 6.4 Ma [b,c,e] = C3An.2n.5.  Miocene foram 'Pulleniatina primalis' FAD occurs at this age in the SW Pacific region (SItes 587,588,590; and at 806B, but without paleomagnetic calibration, ref.d) and Indian Ocean (Sites 214,219,238) (ref. c).  FAD is slightly above FAD of G. lenguaensis at Hole 840 (ref.d).
	Neogloboquadrina acostaensis (sin.)	6.81		D-> S coiling.  Same chron-age calibration as Berggren et al. (1995) = C3An.2r; 6.6 Ma [c] = C3Ar.8.
	Globorotalia nicolae	6.83		Cycle-calibrated in Eastern Mediterranean -- Refs 25-27; in GTS2004 Neogene foraminifer table
	Neogloboquadrina atlantica (sin.)	7.02		D-> S coiling.  Same chron-age calibration as Berggren et al. (1995) = C3Ar; 6.8 Ma [g,h] = C3Ar.3.  Miocene foram 'Neogloboquadrina atlantica' (D to S) FAD is recorded in North Atlantic DSDP Hole 609, 611 (inferred age, ref. g); and 642 (paleomag calibration, ref. h).
	Globorotalia miotumida (conomiozea) (FCO)	7.24		Cycle-calibrated in Eastern Mediterranean and Morocco -- Refs 25-30 & 34; in GTS2004 Neogene foraminifer table.  Miocene foram 'Globorotalia conomiozea' FAD marks the Tortonian/Messinian boundary in Cretan sections (ref. h), and base of Medit. Zone Mt 10.  Berggren et al. (1995) assigns as C3Br.1r; '7.12' Ma [i] = C3Br.1r.35.  The FAD is recorded in mid-C3An in Mediterranean in ref. g; see also refs. a & b.  Paleomagnetic age esimate (Berggren et al., 1995) agrees closely with 7.26 Ma for Tort/Mess boundary in NE Appenines, based on Ar 40/39 age of 7.33 Ma just below FAD of Gt. conomiozea (Vai et al., 1993).
	Catapsydrax parvulus	7.45		Cycle-calibrated in Eastern Mediterranean -- Refs 28 & 30; in GTS2004 Neogene foraminifer table
	Globorotalia suterae 	7.86		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia suterae' FAD is recorded in Hole 654, Mediterranean.  Paleomagnetic estimate (C4n.2n; 7.8 Ma [j]) agrees perfectly with Ar 40/39 age of 7.72 _0.15 Ma on this datum in northern Appenines (Vai et al., 1993).  Set as C4n.2n.6.
	Globorotalia cibaoensis	7.86		NOTE:  Hirsutella cibaoensis (which seems to be same species) had FAD reported 1.6 myr older (9.44) by Lourens et al. (GTS2004) from astronomical scaling in Atlantic (see below).  Age of Glob. cibaoensis used here is same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia cibaoensis' FAD is recorded in Hole 806B (Ontong-Java Plateau).  Age estimate in ref. e (Table 3) of 6.7 Ma calibrated to Berggren et al. (1985) is incorrect.  Note that FAD of Gt. cibaoensis is at virtually same level as FAD of Gt. plesiotumida (266m), but this level was incorrectly estimated as 297m in ref.e (Table 2; plotted in Fig. 6).  FAD's of Ft. junai, Candeina nitida, and Globigerinoides extremus were similarly misinterpreted in ref.e in Hole 806B, but corrected by Berggren et al. (1995).  They place at C4n.2n; (7.8 Ma) [e] = C4n.2n.6.
	Globorotalia miotumida (conomiozea)	7.89		Cycle-calibrated in Eastern Mediterranean -- Refs 28 & 30; in GTS2004 Neogene foraminifer table
	Globorotalia juanai	8.15		NOTE:  Hirsutella juanai (which seems to be same species) had FAD reported 1.5 myr older (9.69) by Lourens et al. (GTS2004) from astronomical scaling in Atlantic (see below).  Age of Glob. juanai used here is same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia juanai' FAD is recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They place at (C4r.1r); (8.1) [e] = C4r.1r.7.
	Candeina nitida	8.43		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign age from Miocene foram 'Candeina nitida' FAD as recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They assign as (C4r.1r); (8.1) [e] = C4r.1r.7.
	Neogloboquadrina humerosa	8.53		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides extremus' FAD is recorded in Hole 806B (Ontong-Java Plateau), with correction of ref.e estimates made by Berggren et al. (1995).  See partial explanation in Note attached to G. cibaoensis.  They assign as C4r.2r; 8.5 Ma [b] = C4r.2r.5.
	Globorotalia plesiotumida 	8.58		M13b base defined either by:  Glob. plesiotumida or Neo. humerosa. Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globorotalia plesiotumida' FAD is recorded in Hole 806B (Ontong-Java Plateau; ref.e), but its FAD was difficult to define owing to questionable lower occurrences.  Berggren et al. (1995) assigned the FAD based on its lowest questionable occurrence, but its effective FCO may be about 0.5 m.y. higher (coeval with FAD of Globorotalia cibaoensis).  In Gulf of Mexico, the FAD is recorded in upper part of Nannofossil Zone NN10, similar to the lower Pacific occurrences, and overlaps the upper part of Discoaster bollii range with the FAD slightly below FAD of nannofossil Minylitha convallis FAD (Zhang et al., 1993; Aubry, 1993).  A similar FAD level is in Buff Bay, Jamaica (Berggren, 1993; Aubry, 1993).  Berggren et al. (1995) assign as (C4r.2r); (8.3) [e] = C4.2r.9.
	Globigerinoides extremus	8.93		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) had at (C4r.2r); (8.3) [e] = C4.2r.9.
	Neogloboquadrina pachyderma	9.36		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina pachyderma' FAD is calibrated in Holes 748, 751 (Kerguelen Plateau, south Indian Ocean) = C4Ar.1n; > 9.2 Ma [k] = C4Ar.1n.5.
	Hirsutella cibaoensis	9.44		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Hirsutella juanai	9.69		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globorotalia partimlabiata	9.94		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table
	Neogloboquadrina acostaensis s.s. -- base regular	10.57		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table.  This FAD is reported younger (9.8 Ma) in Atlantic Sites 925 & 926 (Refs 8, 11, 13) in GTS2004 Neogene foram table.  Berggren et al. (1995) note that Miocene foram 'Neogloboquadrina acostaensis' FAD is calibrated in Holes 558 and 563 (ref. b) and 608 (ref. l) in North Atlantic at the base of chron C5n = C5n.2n; 10.9 Ma [b,l] = C5n.2n.05.
	Menardella limbata	10.64		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita apertura	11.18		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globorotalita challengeri	11.22		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Globoturborotalita decoraperta	11.49		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Globoturborotalia nepenthes	11.63		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) notes that Miocene foram 'Globoturborotalia nepenthes' FAD occurs in North Atlantic Sites 563 (ref. b) and 608 (ref. l) and basal Buff Bay Fm., Jamaica (refs. m,n) = C5r.3r; 11.8 Ma [b,l-n] = C5r.3r.3.  They also use this FAD to define base of Medit. Zone Mt8.  
	Neogloboquadrina gr.	11.78		Cycle-calibrated in Eastern Mediterranean -- Refs 31 & 32; in GTS2004 Neogene foraminifer table
	Globorotalia lenguanensis	12.84		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix
	Fohsella fohsi	12.85		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Sphaeroidinellopsis subdehiscens	13.02		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 11 & 13; in GTS2004 Neogene foraminifer appendix
	Fohsella robusta	13.13		Formerly called 'Globororotalia fohsi robusta'.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8 & 11; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) note that Miocene foram 'Globororotalia fohsi robusta' FAD is based on revised interpretation of magnetostratigraphy of Hole 563, in turn based on stable isotope studies in ref.o = C5An.2n; 12.3 Ma [b,k] = C5An.2n.5.
	Fohsella (Globorotalia) fohsi "lobata"	13.41		Species "lobata" apparently combined with Fohsella "fohsi" in zonal scheme of Lourens et al. (in GTS2004).  This effectively removed the thin "M8" of Berggren et al., 1995.  Berggren et al. (1995) -- Miocene foram 'Globorotalia fohsi lobata' FAD is based on revised interpretaion of magnetostratigraphy of Hole 563 (ref. f), which indicates this FAD is in C5Ar.1r (ref. 15) rather than C5Ar (ref. b) = C5Ar.1r; 12.5 Ma [t] = C5Ar.1r.6.
	Fohsella "fohsi"	13.41		Formerly assigned as genus Globorotalia.  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 8, 11 & 12; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) assign Miocene foram 'Globorotalia fohsi s.str.' FAD is based on reinterpretation of magnetostratigraphy at Hole 563, in turn based on stable isotope studies at Holes 747A and 608 (see ref. o) = C5Ar.n1-2 (undiff.); 12.7 Ma [b,o] = C5Ar.2r.8.
	Neogloboquadrina nympha	13.49		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Neogloboquadrina nympha' FAD is recorded in Holes 747A, 751, Kerguelen Plateau (ref. k).  In Hole 608, the FAD occurs in sample assigned to polarity chron C5AAr, just above C5ABn (ref. o) = C5ABn; 13.4 Ma [k,o] = C5ABn.5.
	Fohsella "praefohsi"	13.77		Formerly assigned as genus Globorotalia.  The form 'Gt. praefohsi' seems intermediate between 'Gt. peripheroacuta' and 'Gt. fohsi s.str'.   Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 13; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assigned Miocene foram 'Globorotalia praefohsi' FAD to a much younger level, based on reinterpretation of magnetostratigraphy at Hole 563, in turn based on stable isotope studies at Holes 747A and 608 (see ref. o) = C5Ar.n1-2 (undiff.); 12.7 Ma [b,o] = C5Ar.2r.8, but this FAD age-assignment was nearly identical to FAD of 'Gt. fohsi s.str.'
	Fohsella peripheroacuta	14.24		Formerly assigned as genus Globorotalia, and was used by Berggren et al (1995) to define base of Serravalian stage.  .  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) assigned as C5B.1n; 14.8 Ma [b] = base C5ADr = nearly 0.5 myr older than Atlantic-ODP cycle-strat assignment.
	Globorotalia praemenardii	14.38		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Orbulina universa	14.74		Same as Orbulina suturalis? (see end of this comment).  Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al. (1995) used Orbulina "suturalis" (age of 15.09 Ma, based on mid-C5Bn.2n; ref [b] which had 15.1 Ma) to define base of Zone M6, but table in Lourens et al. (GTS2004) uses Orbulina "universa" (and there is no indication of a "suturalis". 
	Clavatorella bermudezi	14.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Praeorbulina circularis	14.89		Astronomically tuned from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) had a much older age using C5Cn.1n (upper); 16.0 Ma [b] = C5C.1n.95.
	Globigerinoides diminutus 	16.06		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides diminutus' FAD is discussed in remarks in ref.b = (C5Cn.2n); (16.1 Ma) [b] = C5Cn.1n.7.
	Globorotalia archeomenardii	16.26		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Praeorbulina  curva	16.27		Same chron-age calibration as Berggren et al. (1995) = mid-C5Cn; 16.3 Ma [b] = base C5Cn.1n.
	Praeorbulina glomerosa s.str.	16.27		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) uses to define base of Medit. Zone Mt5b, and assign to C5Cn.1n (upper); 16.1 Ma [b] = C5Cn.1n.8.
	Globorotalia miozea	16.70		Same chron-age calibration as Berggren et al. (1995) -- However, see NOTE on Praeorbulina sicana age.  They note Miocene foram 'Globorotalia miozea' FAD is recorded in Hole 751, Kerguelen Plateau, south Indian Ocean = C5Cn.3n (lower); 16.7 Ma [k] = C5Cn.3n.1, and used to define base of Medit. Zone Mt4. 
	Globorotalia birnageae	16.70		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia birnageae' FAD is calibrated in Hole 516, South Atlantic (ref. b) = C5Cn.3n (lower); 16.7 Ma [b] or 17.8 Ma [u] = C5Cn.3n.1.  Subzone "M4b" is 'Globigerinoides bisphericus Partial Range Zone' (FAD of Globorotalia birnageae to FAD of Praeorbulina sicana) (Berggren et al., 1995).  This short subzone spans the upper part of the 'N7' zone -- and now seems to be entirely WITHIN Zone M5 (after cycle-calibration).  The FAD of G. birnageae is difficult to determine precisely because of its intergradation with Gl. trilobus s.str.
	Praeorbulina sicana	16.97		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix -- however this implied revised calibration to polarity chrons would seem to invert Medit. zones Mt4b and Mt5a (this FAD of P. sicana) of Berggren et al. (1995).  Miocene Foram 'Praeorbulina sicana' of Berggren et al (1995) may be same as 'Globigerinoides sicanus' in table of Hodell & Woodruff (1994); however, their age estimates for the FAD differ by 0.7 m.y.  Berggren et al. (1995) assign age as C5Cn.2n (mid); 16.4 Ma [b] = C5Cn.2n.55.
	Globigeriantella insueta s.str.	17.59		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix -- Note that this is much higher FAD than estimated calibrations by Berggren et al. (1995); which results in Zone M3 being nearly non-existent.  Berggren et al. (1995) -- Miocene foram 'Globigerinatella insueta' FAD has an inferred correlation to polarity chron (base of C5En) and corresponding age assignment = (C5En); (18.8 Ma)[t] or 18.85 Ma [u] = base C5En.
	Globorotalia praescitula	18.29		Same chron-age calibration as Berggren et al. (1995), who used to define base of Medit. Zone Mt3 -- Miocene foram 'Globorotalia praescitula' FAD is recorded in Holes 747A, 748B, 751 (ref. k), 608 (ref. l); and is recorded in lowest part of polarity zone C5En in Hole 516F (ref. b) = C5En; 18.5 Ma; [k,l] = C5En.5.
	Globigerinatella sp.	19.30		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Globiquadrina binaiensis	19.30		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix. 
	Globigerinoides altiaperturus	20.06		Used by Berggren et al. (1995) as "working"  base of Burdigalian stage -- but 2004 working definition is FAD of nanno H. ampliaperta, as calibrated at Ceara Rise = about 0.4 myr older.  Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globigerinoides altiaperturus' FAD is recored in Hole 516F, South Atlantic (ref. b); and is within in older part of polarity chron C6r in Contessa Highway section (ref. q) = C6An (upper); 20.5 Ma [b,q] = base C6r.  NOTE:  Berggren's derived age implies that he assigned this FAD to the base of polarity chron C6A; thereby effectively defining the base of the Burdigalian as base of C6A; which would be more convenent and global than a biostratigraphic event!
	Globorotalia incognita	20.93		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globorotalia incognita' FAD is recorded in Hole 747A (ref. 11); with magnetostratigraphy reinterpreted in ref. o =C6Ar; 21.6 Ma [k] = C6Ar.4.
	Globoquadrina dehiscens forma spinosa	21.44		Same chron-age calibration as Berggren et al. (1995) -- Miocene foram 'Globoquadrina dehiscens forma spinosa' FAD is recorded in Hole 516F, South Atlantic (ref. b) = C6AAr.1n; 22.2 Ma [b] = C6AAr.1n.5.
	Globoquadrina dehiscens	22.38		Same chron-age calibration as Berggren et al. (1995), who used to define Medit. Zone Mt1b -- Miocene foram 'Globoquadrina dehiscens' FAD is recorded in Holes 516F, 558, 563 (ref. b); South Atlantic (refs. r,s) and Contessa Highway Section (ref. q) = C6Br; 23.2 Ma [b] or 23.4 Ma [u] = C6Br.5.
	Globigerinoides trilobus s.l.	22.96		Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix
	Paragloborotalia kugleri	22.96		Paragloborotalia (formerly Globorotalia) kugleri = M1 base; and approx. Oligocene/Miocene boundary [b,s].  Age estimated from Atlantic ODP Sites 925 & 926 -- Refs 12 & 14; in GTS2004 Neogene foraminifer appendix.  Berggren et al (1995) notes that Miocene foram 'Globorotalia kugleri' FAD is recorded in Holes 558, 563 (North Atlantic) and 516F (South Atlantic) (ref. b).   Miocene foram 'Globorotalia kugleri' FAD is recorded in Holes 516F, 558, 563 (ref. a of Oligocene set) = C6Cn.2n; 23.8 Ma [b] or 24.0 Ma [u] = base C6Cn.2n.
	Globigerinoides primordius (FCO)	23.58		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerinoides primordius' (CO) is recorded in Hole 516F (ref. a) = C6Cr; 24.3 Ma [a] or 23.45 Ma? [g] = C6Cr.7.
	Paragloborotalia pseudokugleri	25.40		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Paragloborotalia (formerly Globorotalia) pseudokugleri' FAD is recorded in polarity zone C8n in Hole 803D and in C7n in Hole 628A (ref. c) = C8n; 25.9 Ma [c] = C8n.1n.3.
	Globigerinoides primordius	26.32		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Blobigerinoides primordius' FAD is recorded in Hole 628A (ref. c); and occurs in polarity zone C7n (ref. a) = C8r; 26.7 Ma [c] = C8r.7.
	Globigerinita  boweni	28.45		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Globigerinita boweni' FAD is recorded in Hole 747A (ref. e) = C10n (mid); 28.5 Ma [e] = base C10n.1n
	Globigerina angulisuturalis	29.45		Berggren and Pearson (2005), which is similar as Berggren et al. (1995) -- Oligocene foram 'Globoturborotalita (formerly Globigerina) angulisuturalis' FAD, which defines base of P21a, is recorded by Berggren and Miller (1988); Holes 516 and 558 (ref. a), 628A and 803C (ref. c) = C11n (upper); 29.4 Ma [a,c] = top C11n.
	Tenuitellinata juvenilis	29.80		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Tenuitellinata juvenilis' FAD occurs within an interval of 'no polarity data' between two normal polarity intervals interpreted as parts of polarity chron C11 in Hole 747A (ref. e) = (C11n); (29.7 Ma) [e] = C11n.1r.5.
	Paragloborotalia opima opima	30.77		Oligocene foram 'Paragloborotalia opima opima' = only 'P. opima' in Berggren 1995 SEPM) chart.  Berggren & Miller (1988, p.377) discuss 'opima' subspecies. Same chron-age calibration as Berggren et al. (1995) -- FAD is recorded in Holes 558 and elsewhere (ref. a) = C12n (mid); 30.6 Ma [a] = C12n.5.
	Cassigerinella chipolensis	33.84		Same chron-age calibration as Berggren et al. (1995) -- Oligocene foram 'Cassigerinella chipolensis' FAD is recorded in St. Stephen's Quarry, Alabama borehole (ref. f) = C13r; 33.65 Ma [f] = C13r.9.
	Turborotalia cunialensis	35.26		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Turborotalia cunialensis' FAD defines base of P16, and is just above (i.e. younger than) LAD of 'P. semiinvoluta' (refs. b,c) = C15r; 35.2 Ma [b-d] = C15r.4.
	Cribrohantkenina inflata	35.55		Eocene foram 'Cribrohantkenina inflata' FAD was used previously as P15/P16 boundary (e.g., Blow, 1979; Berggren and Miller, 1988); but discontinued by Berggren et al. (1995).  Same chron-age calibration as Berggren et al. (1995) --  FAD occurs between FAD of 'Isthmolithus recurvus' and LAD of 'P. semiinvoluta' and 'T. pomeroli' in Spain (Molina, 1986; Monechi, 1986; Molina et al., 1986).  FAD of 'I. recurvus' is in polarity chron C16.n2 (refs. a-d) and LAD of 'T. pomeroli' and 'P. semiinvoluta' occur in C15r in Contessa Highway (ref. a-c) or C16n2, in Massignano section (ref. d); which suggests that FAD of 'C. inflata' corresponds approximately with C16.n2. The FAD is not considered unequivocally determined (ref. c).  Brief overlap of 'C. inflata' and 'P. simiinvoluta' shown in the upper part of G. semiinvoluta Zone = lower Foram Zone P16 of Blow, 1979) in Toumarkine and Luterbacher (1985).  Approximate Chron assignment = C16n or oldest part of C15; (35.5 Ma) [c,d] = C16n.1n.1.
	Globigerinatheka semiinvoluta 	38.03		Eocene foram 'Porticulasphaera semiinvoluta' defines base of P15, and has a brief overlap with 'Truncorotaloides' (Blow, 1979).  However, a brief, but distinct, separation of 'Acarinina' and 'P. semiinvoluta' is recorded in Nocchi et al. (1986, Fig. a).  Same chron-age calibration as Berggren et al. (1995) = C18n (upper); 38.4 Ma [a,b] = top C18n.1n.
	Orbulinoides beckmanni	39.80		Defines P13 (= E12) base.  Same chron-age calibration as Berggren et al. (1995) = C18r; 40.5 Ma [a] = C18r.66.
	Turborotalia pomeroli	41.50		Same chron-age calibration as Berggren et al. (1995) = C19r; 42.4 Ma [a] = C19r.1.
	Globigerapsis index	41.94		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Globigerapsis index' FAD is recorded near polarity zone C20n/C20r boundary in Hole 689B (ref. f) = C20n ; 42.9 Ma [a] = C20n.7.
	Morozovella lehneri	42.48		Same chron-age calibration as Berggren et al. (1995) = C20n; 43.5 Ma [a] = C20n.25.
	Globigerinatheka kugleri	45.00		Age calibration by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Not well calibrated  [m.n] -- Eocene Foram Zone P11 base (defined as FAD of G. kugleri) is not in table of Berggren (1995, SEPM).  His Eocene figure shows the P10/P11 boundary at about 60% of the distance from P9/P10 to P11/P12, or just above base of Nanno Zone NP15b (which has a magnetic calibration); and I have used this approximate scaling. Estimated by Berggren '95/'05 as 45.8 Ma = C20r.6.
	Subbotina possagonensis	45.09		Same chron-age calibration as Berggren et al. (1995) = C20r; 46.0 Ma = C20r.1.
	Guembelitrioides nuttalli, Hantkenina	48.60		First occurrence of Hantkenina (base of P10) is current working definition of base of Lutetian Stage.  FAD of G. nuttalli is suggeste as alternate (base of E8) zonal datum by Berggrena nd Pearson (2005).  Age assignment of these events by Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) = C22n (upper); 49.0 Ma [a] = Base C21r (which makes a convenient global event).
	Acarinina cuneicamerata, Astrorotalia palmerae	50.30		Acarinina cuneicamerata = base E7, Astrorotalia palmerae = base P9.  Genus of Astro. palmerae was Planorotalites in Berggren et al, 1995.  Same chron-age calibration as Berggren et al. (1995) = C22r; 50.4 Ma [a] = C22r.33.
	Acarinina  pentacamerata	50.77		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Acarinina pentacamerata' FAD is recorded at top of polarity zone C23n in Hole 689 (ref. m) = C23n.1n (upper); 50.8 Ma [f] = C23n.1n.8.
	Morozovella aragonensis	52.57		Defines P7 (=E5) base. Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella argonensis' FAD is recorded in Holes 550 (ref. g,h), 577 (ref. i,j) and in C23r in Hole 527 (ref. g).  The level adopted by Berggren (used shown here) is slightly older than that shown in Ref. a = C23n.2r; 52.3 Ma [g-j] = C23r.1.
	Morozovella lensiformis	54.52		P6b base of Berggren et al, 1995, was either M. formosa or M. lensiformis.  Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella lensiformis' FAD is recorded in Hole 550 (refs. g,h) and 577 (ref. i) = C24r; 54.0 Ma [g-i] = C24r.75.
	Morozovella  formosa	54.52		Base of Zone P6b (= Zone E4 of Berggren-Pearson. 2005). This taxon is called only "Moro. formosa" in some other charts and papers, and was called Globorotalia formosa in some publications. Same chron-age calibration as Berggren et al. (1995) -- Early Eocene foram 'Morozovella formosa formosa' FAD is calibrated in Hole 577 (ref. i), and defined the P6b/c subzonal boundary of Berggren and Miller (1988).  Chron assignment = C24r; 54.0 Ma [i] = C24r.75.
	Morozovella formosa gracilis, Muricella broedermanni	55.32		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella formosa gracilis' FAD is recorded in Hole 550 (refs. g,h).  Eocene foram 'Muricella broedermanni' (formerly 'Igorina broedermanni') FAD is recorded in Hole 550 (refs. g,h) = C24r (mid); 54.7 Ma [g-i] = C24r.47.
	Morozovella marginodentata	55.44		Same chron-age calibration as Berggren et al. (1995) -- Eocene foram 'Morozovella marginodentata' FAD is recorded in Hole 550 (refs. G,h); and Hole 577, at the top of polarity chron C25n (ref. e) = C24r (lower); 54.8 Ma [g-i] = C24r.43.
	Pseudohastigerina wilcoxensis	55.58		Berggren and Pearson (2005) -- FAD is top of PE carbon-isotope excursion.  Following Berggren and Pearson, it is set as 0.15 myr above PE boundary (base of CIE) = C24r; 55.35 Ma.
	Globanomalina australiformis	55.73		Marker for Paleo/Eoc in high southern lat.  Set here as equal to PE boundary.  Discussion of calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomallina australiformis' FAD is used to denote Paleocene/Eocene boundary in high latitudes [= AP4/5 boundary of Stott and Kennett (1990)] is recorded in Holes 689B and 690B (ref. f).  This FAD is recorded also at Sites 738 (ref. l) and 747 and 748 (ref. e), but with no paleomagnetic control.  Set here as C24r; 55.5 Ma [c] on Berggren et al'95 scale = lower-mid C24r.
	Acarinina sibaiyaensis	55.73		Berggren and Pearson (2005) -- marker for Paleo/Eoc.  One of "Excursion taxa" at PE boundary, therefore age is set equal to that PE age = C24r; 55.5 Ma = lower-mid C24r.
	Morozovella subbotinae	56.67		M. subbotinae FAD = alternate base-P5 zone marker.  This event was used to define the base of Foram Zone 'P6a' by Berggren and Miller (1988), but Berggren et al. (1995) consider that the expression of this FAD is commonly delayed in cores due to a widespread dissolution event(s) during polarity chron C24r.  Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella subbotinae' FAD is recorded in Hole 577 = C25n (upper); 55.9 Ma [d,e] = base C24r.
	Morozovella aequa, Acarinina coalingensis-triplex	57.30		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella aequa' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, in association with FAD of Acar. coalingensis-triplex group and Acar. soldadoensis (Berggren et al., 1995, SEPM).  Paleocene foram 'Acarinina coalingensis-triplex' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM).  Chron assignment = C25r; 56.5 Ma [a] = C25r.9.
	Acarinina soldadoensis	57.30		Paleocene foram 'Acarinina soldadoensis' FAD defines base of Zone P4c of Berggren et al. (1995)/  Berggren and Pearson (2005), has same chron-age calibration as Berggren et al. (1995) -- This datum is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A, in association with FAD of Acar. coalingensis-triplex group and Acar. soldadoensis (Berggren et al., 1995, SEPM).Paleocene Foram Zone 'P4' is the range of 'Globanomalina pseudomenardii'  (Bolli, 1957).  It is subdivided by the LAD of 'Acar. subsphaerica' and FAD of 'Acar. soldadoensis' by Berggren et al. (1995) to essentially correspond to foraminifer zones used in the Caucasus.  Chron assignment = C25r; 56.5 Ma [a] = C25r.9.
	Acarinina subsphaerica, Acarinina acarinata, Acarinina mckannai	59.90		Same chron-age calibration as Berggren et al. (1995) -- Paleocene forams 'Acarinina acarinata',  'Acarinina mckannai' and  'Acarinina subsphaerica' FADs are calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A  (Berggren et al., 1995, SEPM).   The FAD's of three acarininids (acarinata, subsphaerica, mckannai) are observed to coincide closely with the FAD of Gl. pseudomenardii (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 59.1 Ma [a] = C26r.6.
	Globanomalina pseudomenardii	60.19		Calibration by Berggren and Pearson (2005) is 0.2 myr older than the FAD in Berggren et al. (1995) -- Paleocene foram 'Globanomalina psudomenardii' was called 'Planorotalites pseudomenardii' in Berggren & Miller (1988).  Calibration is from Hole 384, and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM).  The FAD is also recorded in the younger part of polarity chron C26r in Hole 577 (ref. 4) within Nannofossil Zone CP 5/6 (undiff.); but in polarity chron C25r in Zone CP5 (= NP6) in Hole 685 (ref. h) or in C26n in Zone CP5 (= NP5) in Hole 605 (refs. h,i; see also ref. b).  Chron assignment = C26r; 59.2 Ma [a,b,d,h,i]; but 59.4 Ma (mid-C26r) in Berggren and Pearson, 2005 = C26r.5.
	Morozovella velascoensis	60.78		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella vellascoensis' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A (Berggren et al., 1995, SEPM) = C26r; 60.0 Ma [a,b] = C26r.3.
	Igorina albeari	60.78		Paleocene foram 'Igorina albeari (=Muricella albeari = Globorotalia laevigata)' FAD defines P3b base.  Berggren and Pearson (2005) is same chron-age calibration as Berggren et al. (1995) -- This FAD occurs approximately mid-way in Zone P3 in Holes 463 and 758A and in the mid-part of polarity chron C26r in Hole 384 (Berggren et al., 1995, SEPM) = C26r; 60.0 Ma [a] = C26r.3.
	Praemurica strabocella	61.21		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica strabocella' FAD occurs in Holes 384 and 758A midway between FAD of Moro. angulata and FAD of Muri. albeari, and in Nannofossil Zone NP5.  However, it is recorded in Hole 690 in lower Zone CP5 (=NP6, ref.b); in Hole 689B in CP8 (=NP9) but equated with C26n (ref.2); and in Hole 738 at CP 4/5 (=NP 5/6) boundary (ref.j) (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 60.5 Ma [a] = C26r.15.
	Morozovella conicotruncata	61.65		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella conicotruncata' FAD occurs at virtually the same level as FAD of Moro. angulata in Holes 384, 465, 758A (ref.a) and 577 (ref. f,g), although the definite position in Hole 577 is difficult to determine because of absence of C27n (Bleil, 1985).  Paleocene foram 'Muricella pusilla' (called 'Igorina pusilla' in Berggren & Miller, 1988)FAD is recorded in lower part of polarity chron C26r and top of Nannofossil Zone CP3 (= NP3) in Hole 577 (refs. d,e), but precise position is difficult to determine because of absence of C27n and possible unconformity just above C28n at 102.95 m (see Bleil, 1985:449-450).  This FAD occurs at same level as FAD of Moro. angulata and Moro. coniscotruncata in Holes 465 and 758A (Berggren et al., 1995, SEPM).  Chron assignment = C26r; 61.0 Ma [a,e] = base C26r.
	Morozovella angulata, Igorina pusilla	61.72		A working definition for base of Selandian stage.  Berggren and Pearson (2005) is same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Morozovella angulata' FAD occurs in Hole 577 within lower part of polarity chron C26r (ref. a,e), but precise position difficult to determine because of absence of C27n (Bleil, 1985, DSDP Leg 86).  In Hole 384, this FAD occurs in upper C27n at <2m above FAD of 'Prae. uncinata') in Nannofossil Zone NP4.  In Holes 465 and 758A it is 2m above FAD of 'Prae. uncinata' (Berggren et al., 1995, SEPM).  Chron assignment = C27n (upper); 61,0 Ma [a,b] = C27n.8.
	Praemurica praeangulata	61.92		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica praeangulata' FAD is calibrated in DSDP Hole 384; and at comparable levels but without paleomagnetic control in Holes 465 and 758A [see comments for 'Moro. angulata'], and occurs at approximately the same level in Holes 738 (ref. j) and 750A (Berggren et al., 1995, SEPM).  Chron assignment = C27n (lower); 61.2 Ma [a] = C27n.2.
	Globanomalina imitata	61.98		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Globanomalina imitata' FAD is recorded in Holes 689B and 690B (ref. c) = (?lower C27n); (~61.3 Ma) [c] = base C27n.
	Praemurica uncinata	62.07		Paleocene foram 'Praemurica uncinata' (formerly 'Morozovella uncinata') FAD defines base of Zone P2.  Berggren and Pearson (2005) moved the FAD 0.4 myr older than in Berggren et al. (1995) on same mag-chron scale.  Notes from Berggren et al. (1995) -- The FAD occurs in Hole 577 (refs. a,e) just above a N->R polarity reversal (= polarity chron C28n); but Polarity chron C27n is missing (Bleil, 1985, DSDP Leg 86: p.446, Fig. 5; p.449, Fig 7B), and there may be a short hiatus at/near the level if FAD of this taxon in C27n (ref. b) is correct.  Alternatively C27n may be missing in the core break between cores 11 and 12 (ca. 101.8 m) in which case the FO of this taxon would be near the C27r/C28n boundary (see ref. b).  In Hole 384, it occurs at the same level as FAD of 'P. praeangulata' in Nannofossil Zone NP4 at the base of C27n, as well as in Holes 465 and 758A (see extended discussion in Berggren et al., 1995, SEPM).  Its FAD was considered equivalent to FAD of 'Praemurica praecursoria' (= 'Globorotalia (Acarinina) praecursoria' of Berggren & Miller, 1988) in an earlier draft by Berggren (1993), but 'praecursoria' was removed from his later versions. Chron assignment = C27n (lower); 61.2 Ma [a,b]; but 61.37 Ma (uppermost C27r) in Berggren and Pearson, 2005 = C27r.92.
	Globanomalina compressa, Praemurica inconstans	63.44		Berggren and Pearson (2005), which is nearly same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Praemurica inconstans' FAD is recorded in Holes 689B and 690C (ref. c) and 384 (ref. g).  Paleocene foram 'Globanomalina compressa' was called 'Planorotalites compresus' in Berggren & Miller, 1988.  FAD is recorded in Hole 384 (ref. g).  It also occurs at a comparable level (by correlation) in an interval with no polarity data just above incomplete polarity chron C28n in 750A-14-2, 44cm to 750A-14-2, 40cm (ref. f?).  Berggren & Miller (1988) "believe that G. compressus and Morozovella trinidadensis have approximately coeval FAD's"; therefore, this FAD of compressa was also base of Zone P1c.  Chron assignment = C28n (2/3rds from base); 63.0 Ma [a,b], but 62.87 Ma in Berggren and Pearson, 2005 = C28n.67.
	Parasubbotina varianta	63.56		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parasubbotina varianta' is recorded in Hole 384 at mid-Nannofossil Zone NP2, and at comparable level by correlation in Hole 750A (Berggren et al., 1995) = C28n (middle); 63.0 Ma [a] = C28n.55.
	Subbotina triloculinoides	64.71		Defines P1b base.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Subbotina triloculinoides' FAD is recorded in Hole 384 (ref. g) = C29n; 64.3 Ma [g] = C29n.6.
	Parasubbotina pseudobulloides	65.19		Same chron-age calibration as Berggren et al. (1995) -- Paleocene foram 'Parasubbotina pseudobulloides' (='Subbotina pseudobulloides' in Berggren & Miller, 1988) is recorded in Hole 738 (ref. k, Hole 384 (ref. g) and Agost, Spain (ref. l); first common occurrence (FCO) noted in older part of polarity chron C29N in Holes 689, 690 (ref. b).  Its FAD may slightly overlap LAD of P. eugubina (review in Berggren et al., 1995).  {In the SEPM Table 8 of Berggren et al.,1995, P. pseudobulloides FAD was accidentally labled "p. eugubina FAD".}.  Chron assignment = just below C29r/n boundary; 64.8 Ma [a,c,g,j,k] = C29r.9.
	Parvularugoglobigerina eugubina	65.32		Defines Pa ('alpha' Greek letter) base.  Berggren and Pearson (2005) uses same chron-age calibration as Berggren et al. (1995) -- Paleocene foram "Parvularugoglobigerina eugubina" FAD is estimated at about 0.030 myr after the end-Cretaceous event (Groot et al., 1990; discussed in Berggren, 1995, SEPM).  Chron assignment = C29r; 64.97 Ma [k] = C29r.7 (but fixed as 0.03 myr higher than base of P0).
	Abathomphalus mayaroensis	68.36		Chron C31n.40 (ODP 171B table, in turn from Erba et al, 1995).  This is the Tethyan FAD.  The FAD of A. mayaroensis seems to be older in North Sea (Paul Sikora, EGI database, 2005).  SEPM'98 correlation was approx. top of J. nebrascansis ammonite zone.
	Contusotruncana contusa	69.49		Chron C31r.60  (ODP 171B table, in turn from Erba et al, 1995).  This FAD is a poor marker (Paul Sikora, pers. Commun., 2005).  C. contusa is not listed in SEPM98, but is secondary marker for base of R. fructicosa zone.
	Racemiguembelina fructicosa	69.62	dashed	DASHED:  Chron C31r.60  (ODP 171B table, in turn from Erba et al, 1995; which is nearly same as the C31r.66 placement in SEPM98).  NOTE: However, this FAD in Tethyan realm is calibrated in EGI database (Paul Sikora, 2005) as 67.5 Ma (2 myr young), which is ABOVE the FAD of A. mayaroensis => this Zone may not be applicable.
	Globotruncana lapparenti, Globotruncana linneiana	70.40		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 25% up in Chron C31r.
	Pseudoguembelina palpabra	71.88		Useful datum tabulated in EGI database (Paul Sikora, 2005), with age derived from composite standard (1998 time scale).  Implied age is 72% up in Chron C32n.2n.
	Planoglobulina acervulinoides	72.35		SEPM'98 places at Chron C32n.40
	Gansserina gansseri	72.35		SEPM'98 places at Chron C32n.40
	Pseudoguembelina excolata	73.27		Same level (mid-C32r.1n.50) as FAD G. aegyptiaca.  EGI database (Paul Sikora, 2005) calibrates Ps. excolata FAD at 72.7 Ma; about 0.5 myr younger.
	Globotruncana aegyptiaca	73.27		SEPM'98 places at Chron C32r.1n.50 (used here).  However, EGI database (Paul Sikora, 2005) calibrates Glob. aegyptiaca FAD at 72.7 Ma; about 0.5 myr younger.
	Pseudotextularia elegans	74.47		SEPM'98 places at Same level (C33n.85) as LAD G. calcarata
	Globotruncanella havanensis	75.07
	Globotruncanita calcarata	75.57		Polarity chron C33n.66.  Genus assigned as "Radotruncana" in Leg 171B table, but not in their Figure.
	Globotruncana ventricosa (consistent)	77.16		First consistent occurrence is a better marker for base of this Foram Zone.  EGI calibration is 77.6 Ma (Paul Sikora, 2005), which is 40% up in Chron C33n.
	Globotruncana ventricosa (rare)	79.54	dashed	DASHED at Top of Chron C33r (SEPM'98):  Rare FAD is not a useful datum, because it remains rare until mid-Middle Campanian (Paul Sikora, 2005); therefore consistent occurrence is a better definition of the zone.
	Pseudoguembelina costulata	81.61		SEPM'98 has at Chron C33r.45
	Globotruncanita elevata	83.53		Base of Campanian in SEPM'98.
	Sigalia decoratissima carpathica	84.94		SEPM'98 assigns as Base of Middle Santonian.
	Dicarinella asymetrica	84.94		SEPM'98 assigns as Base of Middle Santonian (= base C. vermiformis ammonite zone).  D. asymtrica Zone is also range-zone of the index species.
	Archaeoglobigerina bosquensis	88.43		Useful marker just above (ca. 0.15 myr) base of Middle Coniacian (EGI database, Paul Sikora, 2005)
	Pseudotextularia nuttalli	89.27		Base of Coniacian on SEPM'98 chart.
	Dicarinella concavata	90.79	dashed	Dashed -- One-third up in P. hyatti ammonite zone in SEPM98; but ODP Leg 171B placed about 0.8 myr higher.
	Marginotruncana coronata	91.31		Useful marker at mid-Middle Turonian (EGI database, Paul Sikora, 2005)
	Helvetoglobotruncana helvetica	93.41		Top of W. devonense ammonite zone (= base of P. flexuosum ammonite zone) on SEPM'98 chart.
	Whiteinella archaeocretacea, Heterohelix globulosa (=reussi)	94.55		SEPM'98 places arbitrary (?) 1.0 myr before top of Cenomanian
	Whiteinella aprica	94.75		Useful marker at base of Late Cenomanian (EGI database, Paul Sikora, 2005)
	Rotalipora cushmani	95.33		SEPM'98 places at mid-point of Acanthoceras muldoonense ammonite zone. See note on R. reicheli.
	Rotalipora reicheli	95.68		SEPM'98 assigns as base of Middle Cenomanian.   Leg 171B table assigns the R. reicheli Zone with an age ~1 myr older, but with same duration.
	Rotalipora globotruncanoides	99.60		Base of Cenomanian (= primary marker of GSSP !! ).  Formerly called "R. greenhornensis"?  SEPM'98 had assigned as latest Albian (mid-point of uppermost subzone, M. perinflatum), but this was prior to GSSP definition of boundary.
	Rotalipora appenninica	100.94		Base of planktonic foraminifer Rotalipora appenninica is nearly the same horizon as base of Planomalina buxtorfi = base of that zone = 3.3 long-eccentricity cycles below top Albian (1.3 myr) => 100.9 Ma.  Leckie et al. (2002) indicate that R. appenninica FAD is just slightly older/below the FAD of P. buxtorfi, but Hardenbol et al. (1998) and Bellier et al., (2000) show the events to be simultaneous, which I will assume here.  The duration is 1.3 myr, nearly identical to the 1.5 myr used in Leckie et al. (2002) and 1.1 myr in Hardenbol et al., 1998.  Considering the thickness at Risou for this R. appenninica zone (in excess of 100 m; Kennedy et al., 2003 in press), I would have preferred a much longer time span.  SEPM'98 had assigned as Base of Stoliczkaia dispar Zone.
	Planomalina buxtorfi	100.94		See below (primary control on Albian scale!).  Base of P. buxtorfi is also used as base of R. appenninica Zone on some scales.
	Rotalipora ticinensis	102.93		Base of Rotalipora ticinensis (= base of that zone) = 8.2 long-eccentricity cycles below top Albian (3.3 myr) on Piobbico cyclostratigraphy => 102.9 Ma.   (primary control on Albian scale!).  SEPM'98 had assigned as 2/5 from base of H. varicosum s.z.
	Rotalipora subticinensis	105.05	dashed	DASH:  SEPM'98 had assigned as FAD is at the base of the H. orbignyi s.z. of the M. (M.) inflatum. (used here).   Base of foraminifer R. subticinensis (base of that subzone) is not indicated in this Piobbico cyclostratigraphy, but Leckie et al. (2002) scales it within the B. breggiensis zone as 0.7 myr below the base of R. ticinensis, which would project as 103.6 Ma in GTS04, but would lose the relative proportions of Leckie's scale.
	Biticinella breggiensis	106.42		Same assignment as SEPM'98 "for now" = Base of Mortoniceras inflatum Zone;  but NOTE that it now coincides with FAD of T. praeticinensis.  FAD of B. breggiensis is used as base of a B. breggiensis Foram Zone in some scales
	Ticinella praeticinensis	106.42		Base of T. praeticinensis foraminifer subzone  = 16.8 long-eccentricity cycles below top Albian (6.8 myr) => 106.4 Ma.  The duration is 3.2 myr, nearly the same as the 3.3 myr used in Leckie et al. (2002).  (NOTE -- Leckie et al., 2002, define the T. praeticinensis foraminifer subzone as the base of B. breggiensis Zone, in turn defined by the base of that species; however, the actual FAD of T. praeticinensis is below/older than the base of B. breggiensis according to both Leckie et al., 2002, and Hardenbol et al., 1998.  Because Premoli Silva is a co-author on both the Leckie et al., 2002 paper and on the Piobbico cycle stratigraphy paper, I'm assuming that the T. praeticinensis subzone is defined as base of B. breggiensis for this scaling.  In contrast, the zonal schemes of Hardenbol et al., 1998, and Bellier et al., 2000, do not have a B. breggiensis zone, but define the base of T. praeticinensis zone by the first occurrence of the name species.  What a mess.)  (primary control on Albian scale!)
	Ticinella primula	110.89		Base of foraminifer T. primula is 27.8 long-eccentricity cycles below top of Albian (11.3 myr) in Piobbico cyclestrat => 110.9 Ma.  The T. primula zone extends up to 106.4 Ma, which is consistent with the 107.1 Ma Ar-Ar age within it (but from the middle of the 3 ammonite zones that it spans) obtained by Obradovich (1993).   (primary control on Albian scale!).  SEPM'98 had placed in middle of O. raulinianus s.z.
	Ticinella bejaouaensis	114.30		Base Ticinella bejaouaensis = 114.6 Ma (was 114.3 in Leckie's chart).  SEPM'98 had estimated as 3/5 up in D. nodosocostatum s.z.
	Globigerinelloides algeriana	119.00		Base Globigerinelloides algerianus = 119.0 Ma (was 117.1 on Leckie's chart).  SEPM'98 had assigned as 3/5 from base of martinoides Zone.
	Leupoldina cabri (consistent)	122.05		Consistent L. cabri (and calibration of FAD in SE France, etc.) is 85% up in D. deshayesi Zone (but see comment below -- rare occurrences are nearly to base of Aptian).  SEPM'98 had assigned as 2/3 from base of Deshayesites deshayesi Zone.
	Leupoldina cabri	124.50		Base of rare L. cabri (after downward extension by Premoli Silva et al., 1999) = 0.5 myr above base Aptian (125.0 Ma) = 124.5 Ma  (but, usually rare until higher; therefore the apparent FAD of L. cabri in the middle of the D. deshayesi ammonite zone in the Bedoule section (Moullade et al., 1998) is probably this delayed first occurrence).
	Globigerinelloides blowi	127.88		SEPM'98 had assigned as Estimated as about 1/4 below top of A. vandenheckii zone.
	Hedbergella similis	129.64		SEPM'98 had assigned as Base of N. nicklesi Zone.
	Hedbergella sigali/delrioensis	136.76		SEPM'98 had assigned as 0.1 myr above mid-H. trinodosum s.z.   Most scales list this as H. sigali Foram Zone.
	Globuligerina hoterivica	142.30		SEPM'98 had assigned as Base of M. paraminounum s.z.   Also called "Favusella" hoterivica
	Conoglobigerina gulekhensis	145.46		SEPM'98 had assigned as Base of Berriasian
	Globuligerina balakhmatovae, G. bathoniana, Globigerina gulekhensis	168.86		FADs are in the Late Bajocian, the age is assummed as base of the G. (G.) garantiana Zone
	Globuligerina oxfordiana, G. stellapolaris, G. caucasica, G. megamonica, G. calloviensis, Globigerina helvetojurassica, Globigerina terquemi, 	170.23		FADs are in the Middle Bajocian, base of the S. (S.) humphriesianum Zone





Calpionellids (E.Cret.-latest Jur.)	:	Calpionellid Zone	Calpionellid datums	_METACOLUMN_OFF		J. Remane (in Hardenbol et al., SEPM charts, 1998), with GTS2004 revisions.

Calpionellid Zone	block	40	214/216/167	notitle
	TOP	134
	CALP ZONES	138.94
	E	140.28
	D3	141.25
	D2	141.55
	D1	142.30
	C	142.96
	B	145.25
	A3	145.80
	A2	146.14
	A1	147.16
	Chit.	148.98

Calpionellid datums	event		215/216/182
LAD
	CALPIONELLIDAE	138.94
FAD
	Calpionellites darderi	140.28
	L. hungarica	141.25
	Calpionellopsis oblonga	141.55
	Calpionellopsis simplex	142.30
	T. carpathica (large var.)	142.96
	Calpionella alpina (intermediate var.)	145.25
	C. brevis (acme)	145.80
	Calpionella alpina (large var.)	146.14
	T. carpathica (smallest var.)	147.16
	P. andrusovi	147.47
	Chitinoidella spp.	148.98



Smaller Benthic Foraminifers	:	Boreal Cret markers	Boreal Cret other datums	All Smaller Benthic Foram Boreal Datums Combined	Tethyan Jur Zones (Ruget&Nicollin'97)	Tethyan Jur Subzones (Ruget&Nicollin'97)	Tethyan Jur markers (Ruget&Nicollin'97)	Tethyan Jur Zones (SEPM'98)	Tethyan Cret-Jur markers (SEPM'98)	Tethyan other datums (E.Cret.)	All Smaller Benthic Foram Tethyan SEPM Datums Combined	_METACOLUMN_OFF

Boreal Cret markers	event		228/229/133			F. Magniez-Jannin (in Hardenbol et al., SEPM charts, 1998)
LAD
	Stensioeina pommerana, Bolivinoides draco draco, Bolivinoides decoratus giganteus	65.50
	Bolivinoides draco miliaris	68.32
	Bolivinoides laevigatus	70.14
	Neoflabellina rugosa, Reussella szajnochae	70.60
	Gavelinella (Pseudogavelinella) clementiana, Globorotalites? michelianus	77.66
	Bolivinoides granulatus	80.57
	Stensioeina polonica	80.64
	Bolivinoides strigillatus	82.26
	Stensioeina granulata granulata	85.27
	Lingulogavinella globosa	91.72
	Gavelinella cenomanica	92.84
	Gavelinella baltica	93.13
	Flourensiora mariae, H. (Arenobulimina) advena advena	94.01
	Lingulogavelinella formosa/ jarzevae	95.23
	Arenobulimina (Sabulina) sabulosa	99.58
	Citharinella pinnaeformis	101.39
	Hoeglundina chapmani	104.37
	Arenobulimina macfadyeni	105.05
	Hoeglundina carpenteri	105.74
	Gaudrynia dividens	110.83
	Conorotalites aptiensis	114.00
	Gavelinella barremiana	121.90
	Lenticulina (Gaudriyadhella) ouachensis	122.25
	Hauerina (Wellmannella) antiqua	125.54
	Lenticulina schreiteri	128.32
	Epistomina caracolla	128.97
	Gavelinella sigmoicosta, Haplophragmium aequale, Citharina harpa	129.07
	Hechtina praeantiqua, C. seitzi	134.18
	Saracenaria valanginiana	139.81
FAD
	Bolivinoides draco draco	69.78
	Neoflabellinella reticulata, Osangularia navarroana	70.60
	Reussella szajnochae	75.05
	Bolivinoides draco miliaris	77.66
	Bolivinoides laevigatus	80.64
	Bolivinoides granulatus/ pustulatus?	82.26
	Neoflabellina rugosa	83.53
	Gavelinella (Pseudogavelinella) clementiana, Stensioeina pommerana/ excolata	83.70
	Bolivinoides strigillatus	84.69
	Stensioeina polonica	85.85
	Stensioeina exsculpta exsculpta	87.37
	Stensioeina granulata granulata	88.73
	Globorotalites? michelinianus	91.72
	Stensioeina pokornyi	93.13
	Lingulogavelinella globosa	94.75
	Flourensiora mariae	95.22
	H. (Arenobulimina) advena advena	99.58
	Arenobulimina (Sabulina) sabulosa, Lingulogavelinella formaosa/ jarzevae	101.39
	Citharinella pinnaeformis	105.74
	Simplorbites papyracea	105.05
	Gavelinella cenomanica	106.49
	Hoeglundia carpenteri	108.18
	Arenobulimina macfadyeni, D. gradata	110.09
	P. subfusiformis	111.80
	Gavelinella intermedia	114.00
	Gavelinella brielensis	122.42
	Conorotalites aptiensis	125.17
	Coronotalites intercedens	126.51
	Gavelinella barremiana	128.63
	Coronotalites bartensteini	129.27
	Gavelinella sigmoicosta	132.24
	Hauerina (Wellmannella) antiqua	133.94
	Haplophragmium aequale	135.59
	Citharina harpa, C. seitzi	137.69
	D. (Marssonella) kummi	138.78
	Lenticulina schreiteri, Haplophragmium inconstans erectum	139.44
	Lenticulina saxonica	139.87
	Ammovertella cellensis, Hechtina praeantiqua	140.03
	Epistomina caracolla	142.16
	Conorboides valendisensis, Saracenaria valangiana	142.43

Boreal Cret other datums	event		228/229/133			F. Magniez-Jannin (in Hardenbol et al., SEPM charts, 1998)
LAD
	Neoflabelinella reticulata, Brizalina incrassata, Bolivinoides peterssoni	65.50
	Bolivinoides decoratus decoratus	70.14
	Gavelinella monterelensis	70.43
	Globorotalites hiltermanni, Globorotalites? michelianus	70.48
	Neoflabellina numismalis 	77.66
	Stensioeina exsculpta gracilis	80.57
	Gavelinella cristata	80.64
	Reussella kelleri, Orthokarstenia whitei	81.63
	N. suturalis suturalis	82.26
	Neoflabellina gibbera	84.40
	Gavelinella vombensis	85.04
	Gavelinella intermedia	93.82
	Plectina mariae, Plaeopsilina cenomana	94.01
	Flourensina intermedia	95.06
	H. (Eoguthelina) anglica	95.23
	Dorothia filiformis, Arenobulimina chapmani	99.58
	S. asperula	103.68
	Epistomina spinulifera	104.37
	E. (Pseudotextulariella) cretosa, Citharinella karreri, Conorboides lamplughi	105.74
	H. reticulata	106.42
	P. subfusiformis	110.83
	P. prima	111.80
	Saracenaria (Grimsdaleinella) spinosa	114.00
	Lenticulina heiermanni	122.25
	Lenticulina hauteriviana hauteriviana, Lenticulina guttata	125.54
	Epistomina hechti	126.10
	Lenticulina saxonica, Citharina discors	128.97
	Epistomina ornata	129.97
	T. emslandensis	132.03
	Citharina sparsicostata	133.32
	T. pseudoroemeri	134.18
FAD
	Bolivinoides decoratus giganteus	70.14
	Bolivinoides paleocenicus	70.43
	Bolivinoides peterssoni	70.52
	Bolivinoides incrassata	76.41
	Globorotalites hiltermanni, Pseudouvigerina cristata	77.66
	Gavelinella monterelensis, Neoflabellina numismalis	80.64
	Bolivinoides decoratus decoratus	82.26
	Osangularia cordieriana	82.58
	Bolivinoides culverensis	83.53
	Stensioeina exsculpta gracilis	84.40
	Stensioeina granulata perfecta	84.84
	Gavelinella stelligera, Gavelinella cristata, Reussella szajnochae praecursor	85.04
	N. suturalis suturalis, Neoflabellina gibbera	85.85
	Loxostomum (Bolvinitella) eleyi	87.37
	Gavelinella vombensis, Gavelinella thalmanni, Reussella kelleri, Orthokarstenia whitei	88.73
	Reussella cf. kelleri, Gavelinella cf. vombensis	89.78
	Stensioeina granulata humilis	91.72
	G. hangensis	92.13
	Plaeopsilina cenomana	95.22
	H. (Eoguthelina) anglica	99.58
	T.semensis / eouvigeriniformis, G. (Pseudoplanoglobulina) austinana	100.05
	Flourensina intermedia, H. advena praeadvena	100.60
	Pleurostomella bulbosa, A. bochumensis	101.39
	Textularia chapmani	103.68
	Eggerellina mariae	105.05
	Arenobulimina chapmani, Gavelinella baltica	105.74
	P. schloenbachi	106.71
	Citharinella karreri	106.79
	C. chapmani	107.83
	C. pseudodiscors	108.18
	Quinqueloculina antiqua	108.48
	S. bettenstaedti	108.77
	E. (Pseudotextulariella) cretosa	109.06
	C. d'orbignyi	109.26
	Pleurostomella praebulbosa	111.27
	S. lata	111.80
	P. prima	114.00
	Saracenaria (Grimsdaleinella) spinosa, Gaudryina dividens, Valvulineria sp.	122.42
	Hoeglundina chapmani, Epistomina spinulifera	128.63
	V. procera	129.27
	Citharina acuminata	132.24
	Conorboides lamplughi	132.69
	Lenticulina heiermanni, Lenticulina ouachensis ouachensis	133.13
	D. praeoxycona	133.51
	Textularia bettenstaedti	133.69
	Gaudryinella sherlocki	135.59
	D. moorbergensis	136.32
	Lenticulina hauteriviana hauteriviana, M. bettenstaedi	136.57
	Epistomina ornata	137.45
	Citharina sparsicostata, T. pseudoroemeri	137.52
	D. hechti	138.78
	Citharina discors	139.44
	M. gracillissima, A. reophacoides, V. neocomiensis, C. pseudostriatula	142.43


All Smaller Benthic Foram Boreal Datums Combined	event				off	F. Magniez-Jannin (in Hardenbol et al., SEPM charts, 1998)
LAD
	Stensioeina pommerana, Bolivinoides draco draco, Bolivinoides decoratus giganteus	65.50
	Neoflabelinella reticulata, Brizalina incrassata, Bolivinoides peterssoni	65.50
	Bolivinoides draco miliaris	68.32
	Bolivinoides laevigatus	70.14
	Bolivinoides decoratus decoratus	70.14
	Gavelinella monterelensis	70.43
	Globorotalites hiltermanni, Globorotalites? michelianus	70.48
	Neoflabellina rugosa, Reussella szajnochae	70.60
	Gavelinella (Pseudogavelinella) clementiana, Globorotalites? michelianus	77.66
	Neoflabellina numismalis 	77.66
	Bolivinoides granulatus	80.57
	Stensioeina exsculpta gracilis	80.57
	Stensioeina polonica	80.64
	Gavelinella cristata	80.64
	Reussella kelleri, Orthokarstenia whitei	81.63
	Bolivinoides strigillatus	82.26
	N. suturalis suturalis	82.26
	Neoflabellina gibbera	84.40
	Gavelinella vombensis	85.04
	Stensioeina granulata granulata	85.27
	Lingulogavinella globosa	91.72
	Gavelinella cenomanica	92.84
	Gavelinella baltica	93.13
	Gavelinella intermedia	93.82
	Flourensiora mariae, H. (Arenobulimina) advena advena	94.01
	Plectina mariae, Plaeopsilina cenomana	94.01
	Flourensina intermedia	95.06
	Lingulogavelinella formosa/ jarzevae	95.23
	H. (Eoguthelina) anglica	95.23
	Arenobulimina (Sabulina) sabulosa	99.58
	Dorothia filiformis, Arenobulimina chapmani	99.58
	Citharinella pinnaeformis	101.39
	S. asperula	103.68
	Hoeglundina chapmani	104.37
	Epistomina spinulifera	104.37
	Arenobulimina macfadyeni	105.05
	Hoeglundina carpenteri	105.74
	E. (Pseudotextulariella) cretosa, Citharinella karreri, Conorboides lamplughi	105.74
	H. reticulata	106.42
	Gaudrynia dividens	110.83
	P. subfusiformis	110.83
	P. prima	111.80
	Conorotalites aptiensis	114.00
	Saracenaria (Grimsdaleinella) spinosa	114.00
	Gavelinella barremiana	121.90
	Lenticulina (Gaudriyadhella) ouachensis	122.25
	Lenticulina heiermanni	122.25
	Hauerina (Wellmannella) antiqua	125.54
	Lenticulina hauteriviana hauteriviana, Lenticulina guttata	125.54
	Epistomina hechti	126.10
	Lenticulina schreiteri	128.32
	Epistomina caracolla	128.97
	Lenticulina saxonica, Citharina discors	128.97
	Gavelinella sigmoicosta, Haplophragmium aequale, Citharina harpa	129.07
	Epistomina ornata	129.97
	T. emslandensis	132.03
	Citharina sparsicostata	133.32
	Hechtina praeantiqua, C. seitzi	134.18
	T. pseudoroemeri	134.18
	Saracenaria valanginiana	139.81
FAD
	Bolivinoides draco draco	69.78
	Bolivinoides decoratus giganteus	70.14
	Bolivinoides paleocenicus	70.43
	Bolivinoides peterssoni	70.52
	Neoflabellinella reticulata, Osangularia navarroana	70.60
	Reussella szajnochae	75.05
	Bolivinoides incrassata	76.41
	Bolivinoides draco miliaris	77.66
	Globorotalites hiltermanni, Pseudouvigerina cristata	77.66
	Bolivinoides laevigatus	80.64
	Gavelinella monterelensis, Neoflabellina numismalis	80.64
	Bolivinoides granulatus/ pustulatus?	82.26
	Bolivinoides decoratus decoratus	82.26
	Osangularia cordieriana	82.58
	Neoflabellina rugosa	83.53
	Bolivinoides culverensis	83.53
	Gavelinella (Pseudogavelinella) clementiana, Stensioeina pommerana/ excolata	83.70
	Stensioeina exsculpta gracilis	84.40
	Bolivinoides strigillatus	84.69
	Stensioeina granulata perfecta	84.84
	Gavelinella stelligera, Gavelinella cristata, Reussella szajnochae praecursor	85.04
	Stensioeina polonica	85.85
	N. suturalis suturalis, Neoflabellina gibbera	85.85
	Stensioeina exsculpta exsculpta	87.37
	Loxostomum (Bolvinitella) eleyi	87.37
	Stensioeina granulata granulata	88.73
	Gavelinella vombensis, Gavelinella thalmanni, Reussella kelleri, Orthokarstenia whitei	88.73
	Reussella cf. kelleri, Gavelinella cf. vombensis	89.78
	Globorotalites? michelinianus	91.72
	Stensioeina granulata humilis	91.72
	G. hangensis	92.13
	Stensioeina pokornyi	93.13
	Lingulogavelinella globosa	94.75
	Flourensiora mariae	95.22
	Plaeopsilina cenomana	95.22
	H. (Arenobulimina) advena advena	99.58
	H. (Eoguthelina) anglica	99.58
	T.semensis / eouvigeriniformis, G. (Pseudoplanoglobulina) austinana	100.05
	Flourensina intermedia, H. advena praeadvena	100.60
	Arenobulimina (Sabulina) sabulosa, Lingulogavelinella formaosa/ jarzevae	101.39
	Pleurostomella bulbosa, A. bochumensis	101.39
	Textularia chapmani	103.68
	Simplorbites papyracea	105.05
	Eggerellina mariae	105.05
	Citharinella pinnaeformis	105.74
	Arenobulimina chapmani, Gavelinella baltica	105.74
	Gavelinella cenomanica	106.49
	P. schloenbachi	106.71
	Citharinella karreri	106.79
	C. chapmani	107.83
	Hoeglundia carpenteri	108.18
	C. pseudodiscors	108.18
	Quinqueloculina antiqua	108.48
	S. bettenstaedti	108.77
	E. (Pseudotextulariella) cretosa	109.06
	C. d'orbignyi	109.26
	Arenobulimina macfadyeni, D. gradata	110.09
	Pleurostomella praebulbosa	111.27
	P. subfusiformis	111.80
	S. lata	111.80
	Gavelinella intermedia	114.00
	P. prima	114.00
	Gavelinella brielensis	122.42
	Saracenaria (Grimsdaleinella) spinosa, Gaudryina dividens, Valvulineria sp.	122.42
	Conorotalites aptiensis	125.17
	Coronotalites intercedens	126.51
	Gavelinella barremiana	128.63
	Hoeglundina chapmani, Epistomina spinulifera	128.63
	Coronotalites bartensteini	129.27
	V. procera	129.27
	Gavelinella sigmoicosta	132.24
	Citharina acuminata	132.24
	Conorboides lamplughi	132.69
	Lenticulina heiermanni, Lenticulina ouachensis ouachensis	133.13
	D. praeoxycona	133.51
	Textularia bettenstaedti	133.69
	Hauerina (Wellmannella) antiqua	133.94
	Haplophragmium aequale	135.59
	Gaudryinella sherlocki	135.59
	D. moorbergensis	136.32
	Lenticulina hauteriviana hauteriviana, M. bettenstaedi	136.57
	Epistomina ornata	137.45
	Citharina sparsicostata, T. pseudoroemeri	137.52
	Citharina harpa, C. seitzi	137.69
	D. (Marssonella) kummi	138.78
	D. hechti	138.78
	Lenticulina schreiteri, Haplophragmium inconstans erectum	139.44
	Citharina discors	139.44
	Lenticulina saxonica	139.87
	Ammovertella cellensis, Hechtina praeantiqua	140.03
	Epistomina caracolla	142.16
	Conorboides valendisensis, Saracenaria valangiana	142.43
	M. gracillissima, A. reophacoides, V. neocomiensis, C. pseudostriatula	142.43




Tethyan Jur Zones (Ruget&Nicollin'97)	block	120	227/229/92	notitle		Christiane Ruget and Jean-Pierre Nicollin -- chapter on "Les Petits Foraminiferes Bentiques Degages";  in Groupe Francais d'etude du Jurassique (1997)
	TOP	153.77
	Lenticulina polypora mg P.	154.53
	Lenticulina polypora mg P., Vaginulina pasquetae, Lent. angustissima mg A., Conorboides marginata	159.61
	Lenticulina polypora mg P.	161.02
	TOP	161.21
	Lenticulina quenstedti mg L., F. molleri, F. nikitini, F. franconica	162.18
	Lenticulina quenstedti mg L., Lent. galeata mg L.	164.74
	Lenticulina quenstedti mg L., Lent. galeata mg L., T. acutiangulum	165.72
	Lenticulina quenstedti mg L., Lent. galeata mg L., Lent. polymorpha mg P., T. acutiangulum	167.29
	Lenticulina quenstedti mg L., Lent. galeata mg L., Lent. polymorpha mg P., Lent. argonauta mg P.	168.86
	TOP	169.64
	Lenticulina pseudoradiata mg P.	170.23
	N. regularis, A. tolypa 	171.21
	TOP	171.60
	Planiinvoluta carinata	172.49
	Lenticulina dorbignyi, Lent. tenuistriata	175.60
	Lenticulina dorbignyi,  Lent. tenuistriata, C. fasciata, C. fallax	180.50
	Lenticulina chicheryi,  Lent. pennensis mg Morphogenre, D. utriculata, C. iberica	181.20
	Lenticulina obonensis mg P., Lent. aragonensis mg Saracenaria	182.93
	Lenticulina praeobonensis mg P., Lenticulina sublaevis mg Saracenaria	183.00
	TOP	186.95
	Lenticulina speciosa mg Marginulinopsis, Marginulina prima	189.60
	Marginulina spinata, I. muelensis	191.22
	Dentalina matutina, Dentalina primaeva	193.25
	Lenticulina radiata mg Marginulinopsis, Dentalina semiornata, Dent. multicostata	196.50
	Lenticulina tenuistriata	197.28
	Lenticulina curva mg L., N. radiata	198.44
	Lenticulina quadricosta mg Marginulinopsis, Lent. collenoti, Lent. striata	199.60

Tethyan Jur Subzones (Ruget&Nicollin'97)	block	120	227/229/92	notitle
	TOP	154.53
	Lenticulina triquetra mg Saracenaria	155.08
	TOP	156.81
	H. maynci	156.96
	H. maynci, Marginulina turgida	157.66
	H. maynci, H. planus	159.61
	H. canui 	160.66
	"G." oxfordiana	161.02
	TOP	163.20
	Leticulina cultrata, Lent. ectypa mg A. 	164.74
	TOP	167.29
	T. bartensteini, M. bathonica	167.68
	TOP	168.27
	C. ornithocephala, Lenticulina dictyodes mg A., P. punctulata	168.86
	TOP	169.64
	Lenticulina bicostata mg M., I. nodosaria	169.93
	TOP	172.49
	Reophax sterkii	174.71
	Lagenammina jurassica, Reophax metensis	175.60
	TOP	181.20
	Lenticulina chicheryi mg Astacolus	182.93
	TOP	183.00
	Lenticulina sublaevis mg Saracenaria	184.20
	TOP	186.03
	Bolivina liassica	186.95
	TOP	199.60


Tethyan Jur markers (Ruget&Nicollin'97)	event		228/229/133		Christiane Ruget and Jean-Pierre Nicollin -- chapter on "Les Petits Foraminiferes Bentiques Degages";  in Groupe Francais d'etude du Jurassique (1997)
LAD
	Lenticulina polypora mg P.	153.77
	Vaginulina pasquetae, Lenticulina angustissima mg A., Conorboides marginata, Lent. triquetra mg Saracenaria	154.53
	H. maynci	156.81
	Marginulina turgida	156.96
	H. planus	157.66
	H. canui 	159.61
	"G." oxfordiana	160.66
	Lenticulina quenstedti mg L., Frondicularia molleri, F. nikitini, F. franconica	161.21
	Lenticulina galeata mg L.	162.18
	Leticulina cultrata, Lent. ectypa mg A. 	163.20
	T. acutiangulum	164.74
	Lenticulina polymorpha mg P.	165.72
	Lenticulina argonauta mg P.	167.29
	C. ornithocephala, Lenticulina dictyodes mg A., P. punctulata	168.27
	Lenticulina pseudoradiata mg P., Lent. bicostata mg M., I. nodosaria	169.64
	N. regularis, A. tolypa 	170.23
	Planiinvoluta carinata	171.60
	Lenticulina dorbignyi, Lent. tenuistriata, Reophax sterkii	172.49
	Lagenammina jurassica, Reophax metensis	174.71
	C. fasciata, C. fallax	175.60
	Lenticulina chicheryi,  Lent. pennensis mg Morphogenre, D. utriculata, C. iberica	180.50
	Lenticulina obonensis mg P., Lent. aragonensis mg Saracenaria, Lent. chicheryi morphogenre Astacolus	181.20
	Lenticulina praeobonensis mg P., Lent. sublaevis mg Saracenaria	182.93
	Bolivina liassica	186.03
	Lenticulina radiata mg Marginulinopsis, Lent. speciosa mg Marginulinopsis, Marginulina prima	186.95
	Marginulina spinata, I. muelensis	189.60
	Dentalina matutina, Dentalina primaeva	191.22
	Lenticulina quadricosta mg Marginulinopsis, Dentalina semiornata, Dent. multicostata	193.25
	Lenticulina tenuistriata	196.50
	Lenticulina curva mg L., N. radiata	197.28
	Lenticulina collenoti, Lent. striata	198.44
FAD
	Lenticulina triquetra mg Saracenaria	155.08
	Marginulina turgida	157.66
	Vaginulina pasquetae, Lenticulina angustissima mg A., Conorboides marginata, H. maynci, H. planus	159.61
	H. canui 	160.66
	Lenticulina polypora mg P., "G." oxfordiana	161.02
	Frondicularia molleri, F. nikitini, F. franconica	162.18
	Leticulina cultrata, Lent. ectypa mg A. 	164.74
	T. acutiangulum	167.29
	T. bartensteini, M. bathonica	167.68
	Lenticulina quenstedti mg L., Lenticulina galeata mg L., Lent. polymorpha mg P., Lent. argonauta mg P., C. ornithocephala, Lent. dictyodes mg A., P. punctulata	168.86
	Lenticulina bicostata mg M., I. nodosaria	169.93
	Lenticulina pseudoradiata mg P.	170.23
	N. regularis, A. tolypa 	171.21
	Planiinvoluta carinata	172.49
	Reophax sterkii	174.71
	Lagenammina jurassica, Reophax metensis	175.60
	Lenticulina dorbignyi,  Lent. tenuistriata, C. fasciata, C. fallax	180.50
	Lenticulina chicheryi,  Lent. pennensis mg Morphogenre, D. utriculata, C. iberica	181.20
	Lenticulina obonensis mg P., Lent. aragonensis mg Saracenaria, Lent. chicheryi morphogenre Astacolus	182.93
	Lenticulina praeobonensis mg P.	183.00
	Lenticulina sublaevis mg Saracenaria	184.20
	Bolivina liassica	186.95
	Lenticulina speciosa mg Marginulinopsis, Marginulina prima	189.60
	Marginulina spinata, I. muelensis	191.22
	Dentalina matutina, Dent. primaeva	193.25
	Lenticulina radiata mg Marginulinopsis, Dentalina semiornata, Dent. multicostata	196.50
	Lenticulina tenuistriata	197.28
	Lenticulina curva mg L., N. radiata	198.44
	Lenticulina quadricosta mg Marginulinopsis, Lent. collenoti, Lent. striata	199.60


Tethyan Jur Zones (SEPM'98)	block	120	227/229/92	notitle		F. Magniez-Jannin and C. Ruget (in Hardenbol et al., SEPM charts, 1998)
	TOP	145.46
	Trochammina rosacea, Haplophragmoides canuiformis	154.53
	Lenticulina oxfordiana mg S.	156.09
	Nodosaria plicatilis	157.20
	(un-named)	160.89
	Frondicularia molleri	162.35
	Citharina macilenta, Triplasia bartensteini, Flabellammina althoffi, Frondicularia franconica	164.93
	Tristix acutangulum	167.68
	L. argonauta mg P.	168.86
	L. galeata mg P., L. polymorpha mg P.	170.42
	Nodosaria regularis	175.60
	Spectre tenuistriata	177.56
	Spectre d'orbignyi	180.50
	Spectre chicheryi	182.70
	Lenticulina obonensis mg P., L. aragonensis mg S.	182.90
	Lent. preobonensis mg P.	183.00
	Lent. sublaevis mg S. 	183.60
	Denticulina arbuscula, D. obscura, D. terquemi, Lenticulina speciosa mg M., Marginulina prima	186.03
	Bolivina liassica	186.95
	Marginulina interrupta	187.75
	(un-named)	190.01
	Marginulina spinata	191.22
	I. sulcata, I. muelensis, L. inaequistriata mg P.	196.50
	Ichtyolaria xyphoidea, Vaginulina subporrecta	197.28
	Lenticulina quadricosta mg M., L. curva mg M., Marginulina noervangi	198.44
	Lingulina striata, Ling. collenoti, Lenticulina austroalpina mg L.	199.60

Tethyan Cret-Jur markers (SEPM'98)	event		228/229/133			F. Magniez-Jannin and C. Ruget (in Hardenbol et al., SEPM charts, 1998)
LAD
	O. aff. brotzeni	106.42
	Gavelinella barremiana	120.01
	Spirillina neocomiana	123.45
	D. ouachensis	123.97
	Gavelinella sigmoicosta	127.47
	D. hauteriviana	130.94
	H. vocontianus	133.21
	D. (Epistomina) hechti	133.34
	F. bidentata	138.52
	L. busnardoi	139.91
	D. praehauteriviana	140.47
	L. ectypa costata mg M.	157.20
	T. agglutinans	159.02
	Frondicularia molleri	160.89
	Spectre d'orbignyi	172.04
	Bolivina liassica	186.03
	Lenticulina quadricostata mg M.	193.66
	Galeanella panticae	199.60
FAD
	Gavelinella cenomanica	99.90
	G. brotzeni	106.57
	P. subnodosa, O. aff. brotzeni, Osangularia schloenbachi	113.00
	Gavelinella intermedia	118.99
	Gavelinella barremiana s.s.	127.88
	Gavelinella barremiana s.l.	129.97
	Conorotalites bartensteini	133.21
	Gavelinella sigmoicosta	133.69
	D. ouachensis	135.80
	H. vocontianus	137.40
	Lenticulina eichenbergi	138.52
	D. hauteriviana	139.14
	D. (Epistomina) hechti	140.28
	Lenticulina nodosa nodosa	140.66
	D. sp. cf. kummi	142.30
	Spirillina neocomiana, L. busnardoi, D. praehauteriviana 	145.46
	L. ectypa costata mg M.	158.69
	Frondicularia molleri	162.35
	L. ectypa mg A.	164.74
	A. irregularis	164.93
	Citharina spp., D. utriculata, L. pennensis mg L.M.	181.20
	Bolivina liassica	186.95
	D. tenuistriata, D. varians	188.14
	L. radiata mg M.	194.88
	N. issleri, D. fasciata	195.69
	Lenticulina quadricosta mg M.	197.86


Tethyan other datums (E.Cret.)	event		228/229/133			F. Magniez-Jannin and C. Ruget (in Hardenbol et al., SEPM charts, 1998)
LAD
	Saracenaria (Grimsdaleinella) spinosa	109.06
	G. flandrini	109.50
	D. praeoxycona	121.00
	Lenticulina (Gaudriyadhella) ouachensis	123.09
	S. carinata	123.45
	Lenticulina eichenbergi	125.22
	M. reticulosa	126.37
	L. besairlei	129.57
	M. sardoa	130.94
	D. zedlerae	131.91
	L. o. bartensteini	132.72
FAD
	A. problematicus	101.39
	Plectorecurvoididae alternans	112.00
	D. plummeri, S. complanata praecursor	118.99
	H. nonioninoides	120.25
	G. flandrini	122.24
	Conorotalites aptiensis	126.37
	Coronotalites intercedens	128.80
	D. praeoxycona, Gavelinella aff. barremania	130.61
	S. carinata	133.21
	Textularia bettenstaedti	134.11
	Lenticulina ouachensis bartensteini, D. zedlerae	138.52
	D. (Marssonella) cf. kummi, G. eichenbergi	139.77
	Lenticulina ouachensis	140.66
	D. kummi, Conorboides valendisensis, T. burlini, Lenticulina nodosa, D. hechti	145.46

All Smaller Benthic Foram Tethyan SEPM Datums Combined	event		228/229/133		off
LAD
	O. aff. brotzeni	106.42
	Saracenaria (Grimsdaleinella) spinosa	109.06
	G. flandrini	109.50
	Gavelinella barremiana	120.01
	D. praeoxycona	121.00
	Lenticulina (Gaudriyadhella) ouachensis	123.09
	Spirillina neocomiana	123.45
	S. carinata	123.45
	D. ouachensis	123.97
	Lenticulina eichenbergi	125.22
	M. reticulosa	126.37
	Gavelinella sigmoicosta	127.47
	L. besairlei	129.57
	D. hauteriviana	130.94
	M. sardoa	130.94
	D. zedlerae	131.91
	L. o. bartensteini	132.72
	H. vocontianus	133.21
	D. (Epistomina) hechti	133.34
	F. bidentata	138.52
	L. busnardoi	139.91
	D. praehauteriviana	140.47
	L. ectypa costata mg M.	157.20
	T. agglutinans	159.02
	Frondicularia molleri	160.89
	Spectre d'orbignyi	172.04
	Bolivina liassica	186.03
	Lenticulina quadricostata mg M.	193.66
	Galeanella panticae	199.60
FAD
	Gavelinella cenomanica	99.90
	A. problematicus	101.39
	G. brotzeni	106.57
	Plectorecurvoididae alternans	112.00
	P. subnodosa, O. aff. brotzeni, Osangularia schloenbachi	113.00
	Gavelinella intermedia	118.99
	D. plummeri, S. complanata praecursor	118.99
	H. nonioninoides	120.25
	G. flandrini	122.24
	Conorotalites aptiensis	126.37
	Gavelinella barremiana s.s.	127.88
	Coronotalites intercedens	128.80
	Gavelinella barremiana s.l.	129.97
	D. praeoxycona, Gavelinella aff. barremania	130.61
	Conorotalites bartensteini	133.21
	S. carinata	133.21
	Gavelinella sigmoicosta	133.69
	Textularia bettenstaedti	134.11
	D. ouachensis	135.80
	H. vocontianus	137.40
	Lenticulina eichenbergi	138.52
	Lenticulina ouachensis bartensteini, D. zedlerae	138.52
	D. hauteriviana	139.14
	D. (Marssonella) cf. kummi, G. eichenbergi	139.77
	D. (Epistomina) hechti	140.28
	Lenticulina nodosa nodosa	140.66
	Lenticulina ouachensis	140.66
	D. sp. cf. kummi	142.30
	Spirillina neocomiana, L. busnardoi, D. praehauteriviana 	145.46
	D. kummi, Conorboides valendisensis, T. burlini, Lenticulina nodosa, D. hechti	145.46
	L. ectypa costata mg M.	158.69
	Frondicularia molleri	162.35
	L. ectypa mg A.	164.74
	A. irregularis	164.93
	Citharina spp., D. utriculata, L. pennensis mg L.M.	181.20
	Bolivina liassica	186.95
	D. tenuistriata, D. varians	188.14
	L. radiata mg M.	194.88
	N. issleri, D. fasciata	195.69
	Lenticulina quadricosta mg M.	197.86



Larger Benthic Foraminifers	:	Larger Benthic Foram Zone	Larger Benthic Foram Marker	Other Larger Benthic Foram datums (Ceno-Cret)	All Larger Benthic Foram Datums Combined	Jurassic Benthic Foram datums (Bassoullet'97)	_METACOLUMN_OFF

Larger Benthic Foram Zone	block	100	204/204/82	notitle		Various authors in Hardenbol et al (SEPM charts, 1998):  [Oligocene-Miocene = B. Cahuzac and A. Poignant.  Detailed Paleocene-Eocene = J. Serra-Kiel and L. Hottinger.  Upper Cretaceous = M. Bilotte.  Lower Cretaceous = Annie Arnaud Vanneau.  Jurassic & Triassic = B. Peybernes.]
	TOP	0.00
	Not named	7.25
	SB26	16.97
	SB25	20.43
	SB24	23.03
	SB23	26.83
	SB22b	28.45
	SB22a	30.42
	SB21	33.88
	SB20	35.04
	SB19	37.24
	SB18	37.98
	SB17	40.44
	SB16	40.99
	SB15	42.33
	SB14	45.44
	SB13	48.60
	SB12	49.12
	SB11	50.66
	SB10	52.83
	SB9	53.09
	SB8	54.38
	SB7	55.73
	SB6	55.95
	SB5	56.47
	SB4	57.30
	SB3	58.91
	SB2	60.86
	SB1	65.50
	TOP	145.46
	Anchispirocycina lusitanica + Protopeneropis trochangulata	149.44
	Alveosepta powersi + Kilianina rahonensis	152.59
	Alveosepta jaccardi	161.21
	Kurnubia palastiniensis	162.35
	Ataxella occitanica + Satorina apuliensis	164.93
	Alzonella cuvillieri, Archaeosepta platierensis	168.86
	Callorbis minor	170.62
	Timidonella sarda + Gutnicella cayeuxi	172.49
	TOP	183.00
	Lituosepta compressa + Orbitopsella praecursor + Paleomayncina termieri	193.25
	Involutina liassica	198.44
	No zone assignment	199.60
	TOP	199.60
	Triasina  hantkeni     	205.71
	Triasina oberhauseri	216.53
	(un-named)	228.01
	Lamelliconus gr. procerus- multispirus	229.43
	Aulotortus praegaschei	234.56
	(un-named)	240.00
	Pilammina densa	241.60
	Paulbrownnimannia judicariensis	242.49
	Meandrospira dinarica	245.17
	Meandrospira pusilla	248.08
	(un-named)	250.17
	Rectocornuspira kahlori	250.38

Larger Benthic Foram Marker	event		204/204/120			Various authors in Hardenbol et al (SEPM charts, 1998):  [Oligocene-Miocene = B. Cahuzac and A. Poignant.  Detailed Paleocene-Eocene = J. Serra-Kiel and L. Hottinger.  Upper Cretaceous = M. Bilotte.  Lower Cretaceous = Annie Arnaud Vanneau.  Jurassic & Triassic = B. Peybernes.]
LAD
	Heterostegina spp., Planorbulinella spp.	7.25
	M. tani	20.43
	P. delicata, M. complanatus / formosensis group, G. assilinoides, E. dilatata, S. blanckenhorni	23.03
	B. bulloides	28.45
	Nummulites retiatus, Discocyclina spp., Orbitoclypeus spp., Asterocyclina spp.	33.88
	Nummulites fabianii	35.04
	Nummulites biedai	37.24
	Alveolina elongata, Nummulites perforatus, Num. brnogniarti, Discocyclina pulcra baconica	37.98
	Nummulites herbi, N. aturicus, Assilina gigantea, Discocyclina pulcra balatonica	40.44
	N. sordensis, N. crassus	40.99
	Alveolina munieri, Nummulites beneharnensis, Assilina spira spira	42.33
	Alveolina stipes, Nummulites laevigatus	45.44
	Alveolina violae, N. manfredi, N. campesinus, Assilina major	48.60
	Alveolina dainellii, Nummulites praelaevigatus, Assilina laxispira	49.12
	Alveolina schwageri, A. indicatrix, Nummulites planulatus, Discocyclina archiaci archiaci	50.66
	Aveolina trempina, Nummulites involutus, Assilina adrianensis	52.83
	Alveolina corbarica, Nummulites exilis, Assilina leymerei	53.09
	Alveolina moussoulensis	54.38
	Alveolina ellipsoidalis, A. pasticillata, Nummulites minervensis	55.73
	Nummulites gamardensis	55.95
	Glomalveolina levis, Assilina yvettae	56.47
	Fallotella alavensis	57.30
	M. primitiva	58.91
	Laffittiena bibensis	60.86
	Laffittiena mengaudi	65.50
	Hellenocyclina beotica, Siderolites calcitrapoides, Orbitolites gensacica	65.70
	Orbitolites media, O. (gr.) tissoti, Fallotia jacquoti, L. bisambergensis	68.55
	Arnaudiella grossouvrei	75.38
	Subalveolina dordonica	80.84
	Lacazina group, Pseudostaffella sphaeroidea, S. santoniensis	83.53
	Dictopsella kiliani (Adriatic)	83.76
	Ovalveolina ovum, Chrysalidina gradata, Pseudopatellinella (gr.) cretacea, P. iberica, S. drorimensis	93.72
	O. (O.) concava, O.(C.) paeneconica, O. conica	94.75
	B. biplana, I. hungarica, O. corbarica, O. cuvillieri, N. convexa	96.01
	Orbitolina (Mesorbitolina) texana	100.94
	S. conulus	105.05
	Simplorbitolina manasi	107.30
	D. pyrenaicus	108.77
	Praereticulinella cuvillieri (+ A. reicheli in Adriatic)	114.67
	Palorbitolina lenticularis	120.25
	Praeorbitolina cormyi	121.90
	Rectodictyoconus giganteus, O. cuvillieri	123.45
	Praereticulinella reicheli	123.97
	Campanellula capuensis (Adriatic)	129.97
	C.? favrei	132.56
	V. camposaurii (Adriatic)	135.80
	P. salevensis	136.44
	Pfenderina neocomiensis	137.69
	Feurtillia frequens	140.18
	P. courtionensis	141.25
	Anchispirocyclina lusitanica	144.53
	Kurnubia palastiniensis	145.60
	Alveosepta jaccardi	150.84
	P. aquitanica	152.59
	P. crusei	156.96
	Ataxella occitanica, Satorina apuliensis	163.54
	O. elliptica, Archaeosepta platierensis, Alzonella cuvillieri, K. blancheti	164.74
	Callorbis minor	168.86
	Timidonella sarda, Gutnicella cayeuxi	170.62
	Involutina liassica, Paleomayncina termieri, Lituosepta compressa, Orbitopsella praecursor	183.00
	P. butterlini	188.41
	Triasina hantkeni, Galeanella panticae, Galeanella laticarinata	199.60
	Triasina oberhauseri	205.71
	Aulotortus praegaschei	219.12
	Lamelliconus gr. procerus-multispirus	228.01
	Pilammina densa	240.00
	Paulbrownnimannia judicariensis, Meandrospira dinarica, Meandrospira pusilla	241.60
	Rectocornuspira kahlori	250.17
FAD
	B. melo group	16.97
	M. globulina	20.43
	M. gunteri	23.03
	M. complanatus, C. eidae	26.83
	C. droogeri	28.45
	Nephrolepidina praemaginata, E. formosoides	30.42
	Nummulites vascus, N. fichteli	33.88
	Nummulites retiatus	35.04
	Nummulites fabianii	37.24
	Nummulites biedai, N. striatus	37.98
	Alvoelina elongata, Nummulites perforatus, Num. brongniarti, Discocyclina pulcra baconica	40.44
	Nummulites herbi, N. aturicus, Assilina gigantea, Discocyclina pulcra balatonica	40.99
	Alveolina prorrecta, N. sordensis, N. crassus	42.33
	Alveolina munieri, Nummulites beneharnensis, Assilina spira spira	45.44
	Alveolina stipes, Nummulites laevigatus	48.60
	Alveolina violae, N. manfredi, N. campesinus, Assilina major	49.12
	Alveolina dainellii, Nummulites praelaevigatus, Assilina laxispira	50.66
	Alveolina schwageri, A. indicatrix, Nummulites planulatus, Discocyclina archiaci archiaci	52.83
	Aveolina trempina, Nummulites involutus, Assilina adrianensis	53.09
	Alveolina corbarica, Nummulites exilis, Assilina leymerei	54.38
	Alveolina moussoulensis	55.73
	Alveolina ellipsoidalis, A. pasticillata, Nummulites minervensis	55.95
	Nummulites gamardensis	56.47
	Glomalveolina levis, Assilina yvettae	57.30
	Glomalveolina primaeava, Fallotella alavensis	58.91
	M. primitiva	60.86
	Laffittiena bibensis	65.50
	Hellencyclina beotica, Orbitolites gensacica	69.23
	Laffitteina mengaudi	69.78
	Siderolites (gr.) calcitrapoides, L. bisambergensis	70.60
	Fallotia jacquoti	75.43
	Orbitolites media, Arnaudiella grossouvrei	76.74
	Subalveolina dordonica, O.(gr.) tissoti, Siderolites(gr.) vidali	83.53
	S. santoniensis	83.76
	Lacazina gr.	85.85
	Scandonea samnitica (Adriatic)	85.85
	Pseudostaffella sphaeroidea	89.02
	Dictopsella kiliani (Adriatic)	92.00
	Ovalveoloina ovum, Chrysalidina gradata,  Pseudopatellinella (gr.) cretacea, S. drorimensis	96.01
	P. iberica, O. corbarica	99.58
	O.(C.) paeneconica, O.(O.) concava, N. convexa	100.94
	D. pyrenaicus, I. hungarica	110.24
	S. conulus	112.00
	Simplorbitolina manasi	113.00
	A. reicheli (Adriatic)	115.00
	Orbitolina (Mesorbitolina.) texana, Praereticulinella cuvillieri	118.00
	Praeorbitolina cormyi	122.93
	O. cuvillieri	125.00
	Rectodictyoconus giganteus, Palorbitolina lenticularis	127.20
	Praereticulinella reicheli	128.30
	Campanellula capuensis (Adriatic)	133.85
	C.? favrei, P. salevensis	140.18
	Pfenderina neocomiensis	141.25
	V. camposauri (Adriatic)	141.55
	P. courtionensis	142.96
	Feurtillia frequens	144.53
	Protopeneropis trochangulata, Anchispirocycina lusitanica	149.44
	Kilianina rahonensis, Protopeneropis aquitanica, Alveosepta powersi	152.59
	Alveosepta jaccardi	161.21
	Kurnubia palastiniensis	162.35
	O. elliptica, Ataxella occitanica, Satorina apuliensis, K. blancheti	164.93
	C. basiliensis ?	165.66
	P. crusei	168.66
	Archaeosepta platieresis, Alzonella cuvillieri	168.86
	Callorbis minor	170.62
	Timidonella sarda, Gutnicella cayeuxi	172.49
	P. butterlini	190.41
	Orbitopsella praecursor, Lituosepta compressa, Paleomayncina termieri	193.25
	Involutina liassica	198.44
	Triasina hantkeni	205.71
	Triasina oberhauseri, Galeanella panticae, Galeanella laticarinata	216.53
	Lamelliconus gr. procerus-multispirus	229.43
	Aulotortus praegaschei	234.56
	Paulbrownnimannia judicariensis, Pilammina densa	242.49
	Meandrospira dinarica	245.17
	Meandrospira pusilla	248.08
	Rectocornuspira kahlori	250.38

Other Larger Benthic Foram datums (Ceno-Cret)	event		204/204/120
LAD
	B. melo melo	6.34
	O. complanata	9.53
	N. tournoueri, Miolepidocyclina spp.	17.54
	A. howchini	17.59
	Nummulites bouillei, C. eidae, Myopgypsina septentrionalis, B. pygmaea	23.29
	N. fichteli	25.56
	P. afyonica, B. vonderschmitti, S. granulosus, H. reticulata, A. alpina, A. gomezi	33.88
	A. stellata stellaris, A. alticostata danubica, D. dispansa umbilicata	35.04
	D. dispansa dispansa, N. striatus	35.66
	N. ptukhiani, A. stellata stella, A. alticostata alticostata, D. discus, A. kecskemetii	37.24
	A. schwageri, A. roselli	37.61
	A. stellata stellata, O. douvillei pannonicus, O. varians scalaris	37.98
	O. varians roberti, A. alticostata cuvillierii	40.44
	A. stellata planospira, A. parva, D. pulcra pulcra, O. douvillei chudeaui, O. varians angoumensis	40.99
	N. gratus, A. alticostata gallica, A. stellata adourensis	42.33
	A. callosa, N. obesus, A. stella abrardi, O. douvillei douvillei, O. varians portnayae, D. archiaci bartholomei	45.44
	N. allensis, A. taramellii, D. stratiemanuelis	47.92
	A. canavarii, A. marinellii, A. escheri, A. karreri, A. laxispira, N. evae, D. fortisi simferopolensis	49.12
	A. sicula, A. plana, D. fortisi fortisi, O. schopeni crimensis	50.66
	D. pseudoaugustae	52.15
	G. lepidula, Discosyclina archiaci staroseliensis, O. schopeni suvukayensis	52.83
	A. subpyrenaica, D. tenuis, Discosyclina archiaci bakhchisaraiensis, O. schopeni neumannae	54.38
	A. aff. arenensis, O. schopeni ramaraoi	55.73
	A. aramaea, A. cucumiformis, A. avellana, A. dandotica	55.95
	G. dachalensis, A. azilensis, R. sindensis	56.47
	Glomalveolina primaeava	56.97
	C. rajkae, C.? sireli, N. heberti, D. seunesi n. ssp.	57.30
	Periloculina n.sp. 4, Pseudonummuloculina n.sp., Laffitiena? n.sp., Coskinon n.sp.	58.91
	Protelphidium	60.86
	Rhapsydionina liburnica (Adriatic)	65.50
	Lepidorbitoides socialis,  O.(gr.) apiculata, Omphalocyclus macroporus	65.70
	L. minor	68.55
	Abrardia. mosae, P. dordoniensis, L. campaniensis, Siderolites (gr.) vidali	69.57
	Adriatic: Raadshoovenia salentina, R. scarsellai, S. surrentina, Accordiella conica, K. tergestina, S. mediterranea	70.60
	Scandonea samnitica (Adriatic)	81.30
	Adriatic:  Pegidia dubia, C. fraasi	93.55
	Adriatic:  Sellialveolina viallii, Ov. maccagnoae	94.75
	Adriatic: P. parvus, "V." dercourti	96.01
	O. (M.) parva	106.42
	P. tunesiana (Adriatic)	113.00
	I. rubiensis, D. pachymarginalis	119.50
	N. friburgensis	124.64
	O. debelmasi	127.47
	P. jourdanensis, U. alpillensis	128.97
	Valdanchella miliani	139.56
	C. basiliensis, P. trochangulata	141.25
	P. ultragranulata (Adriatic)	141.48
FAD
	Planorbulinella spp., D. italica	10.55
	P. rokae	13.41
	H. granulatatesta group	16.27
	M. cushmani, M. mediterranea	17.54
	M socini	21.23
	Myopgypsina septentrionalis	25.56
	Nummulites vascus	27.27
	P. delicata, B. pygmaea, O. complanata, B. bulloides	33.88
	A. stellata n. ssp., D. dispansa n. ssp.	35.04
	D. dispansa umbilicata, A. priabonensis	35.66
	A. alpina, S. granulosus, B. vondershmitti, P. afyonica, A. alticostata danubica, A. stella praestellaris, D. trabayensis vicenzensis, D. augustae augustae	37.24
	H. reticulata, A. gomezi, M. drobneae	37.61
	D. dispansa dispansa, A. stellata stellaris, O. varians varians	37.98
	A. schwageri, A. roselli, N. ptukhiani, A. alticostata alticostata, O. varians scalaris	40.44
	O. varians roberti, O. douvillei pannonicus, A. kecskemetii	40.99
	A. stellata planospira, A. stellata stellata, A. alticostata cuvillierii	42.33
	N. gratus, O. douvillei chudeaui, O. varians angoumensis, D. pulcra pulcra, D. discus	45.44
	A. callosa	48.60
	D. stratiemanuelis, O. varians portnayae, A. alticostata gallica, A. stella stella	49.12
	D. fortisi simferopolensis, D. archiaci bartholomei	50.66
	D. fortisi fortisi, O. douvillei douvillei, A. stellata adourensis	52.15
	A. canavarii, A. sicula, A. marinellii, A. karreri, A. plana, A. escheri, O. schopeni crimensis	52.83
	Discosyclina archiaci staroseliensis, O. schopeni suviukayensis, D. pseudoaugustare	54.38
	A. subpyrenaica, N. robustiformis, A. arenensis, Discosyclina archiaci bakhchisaraiensis, O. schopeni neumannae, A. taramellii, N. evae	55.73
	A. aff. arenensis, O. schopeni ramaraoi	55.95
	A. aramaea, A. cucumiformis, A. avellana, A. dandotica, G. lepidula	56.47
	D. tenuis, A. axilensis	57.30
	G. dachalensis, D. seunesi n. ssp.	58.14
	C. rajkae, N. heberti, R. sindensis, O. schopeni ramaraoi, D. seunesi seunesi	58.91
	Periloculina n.sp. 1, Pseudonummuloculina n.sp., Laffitiena? n.sp., Coskinon n.sp., C.? sireli	60.86
	Rhapsydionina liburnica (Adriatic)	69.23
	Laffitteina socialis, Omphalocyclus macroporus	69.78
	O. (gr.) apiculata, L. minor	70.39
	L. campaniensis	76.30
	Abrardia mosae	79.68
	Raadshoovenia salentina (Adriatic)	81.30
	P. dordoniensis	83.76
	Keramosphaerina tergestina (Adriatic)	84.63
	S. surrentina (Adriatic)	87.57
	Adriatic: Accordiella conica, R. scarsellai	89.02
	C. fraasi (Adriatic)	94.68
	Pegidia dubia (Adriatic)	95.06
	Sellialveolina viallii (Adriatic)	96.01
	Adriatic: P. parvus	99.58
	Adriatic: I. hungarica, O. maccagnoae, "V." dercourti	100.94
	O. (M.) parva, D. pachymarginalis, I. rubiensis	121.00
	O. debelmasi, P. jourdanensis, U. alpillensis	130.94
	Valdanchella miliani	141.19 

All Larger Benthic Foram Datums Combined	event		204/204/120		off
LAD
	B. melo melo	6.34
	Heterostegina spp., Planorbulinella spp.	7.25
	O. complanata	9.53
	N. tournoueri, Miolepidocyclina spp.	17.54
	A. howchini	17.59
	M. tani	20.43
	P. delicata, M. complanatus / formosensis group, G. assilinoides, E. dilatata, S. blanckenhorni	23.03
	Nummulites bouillei, C. eidae, Myopgypsina septentrionalis, B. pygmaea	23.29
	N. fichteli	25.56
	B. bulloides	28.45
	Nummulites retiatus, Discocyclina spp., Orbitoclypeus spp., Asterocyclina spp.	33.88
	P. afyonica, B. vonderschmitti, S. granulosus, H. reticulata, A. alpina, A. gomezi	33.88
	Nummulites fabianii	35.04
	A. stellata stellaris, A. alticostata danubica, D. dispansa umbilicata	35.04
	D. dispansa dispansa, N. striatus	35.66
	Nummulites biedai	37.24
	N. ptukhiani, A. stellata stella, A. alticostata alticostata, D. discus, A. kecskemetii	37.24
	A. schwageri, A. roselli	37.61
	Alveolina elongata, Nummulites perforatus, Num. brnogniarti, Discocyclina pulcra baconica	37.98
	A. stellata stellata, O. douvillei pannonicus, O. varians scalaris	37.98
	Nummulites herbi, N. aturicus, Assilina gigantea, Discocyclina pulcra balatonica	40.44
	O. varians roberti, A. alticostata cuvillierii	40.44
	N. sordensis, N. crassus	40.99
	A. stellata planospira, A. parva, D. pulcra pulcra, O. douvillei chudeaui, O. varians angoumensis	40.99
	Alveolina munieri, Nummulites beneharnensis, Assilina spira spira	42.33
	N. gratus, A. alticostata gallica, A. stellata adourensis	42.33
	Alveolina stipes, Nummulites laevigatus	45.44
	A. callosa, N. obesus, A. stella abrardi, O. douvillei douvillei, O. varians portnayae, D. archiaci bartholomei	45.44
	N. allensis, A. taramellii, D. stratiemanuelis	47.92
	Alveolina violae, N. manfredi, N. campesinus, Assilina major	48.60
	Alveolina dainellii, Nummulites praelaevigatus, Assilina laxispira	49.12
	A. canavarii, A. marinellii, A. escheri, A. karreri, A. laxispira, N. evae, D. fortisi simferopolensis	49.12
	Alveolina schwageri, A. indicatrix, Nummulites planulatus, Discocyclina archiaci archiaci	50.66
	A. sicula, A. plana, D. fortisi fortisi, O. schopeni crimensis	50.66
	D. pseudoaugustae	52.15
	Aveolina trempina, Nummulites involutus, Assilina adrianensis	52.83
	G. lepidula, Discosyclina archiaci staroseliensis, O. schopeni suvukayensis	52.83
	Alveolina corbarica, Nummulites exilis, Assilina leymerei	53.09
	Alveolina moussoulensis	54.38
	A. subpyrenaica, D. tenuis, Discosyclina archiaci bakhchisaraiensis, O. schopeni neumannae	54.38
	Alveolina ellipsoidalis, A. pasticillata, Nummulites minervensis	55.73
	A. aff. arenensis, O. schopeni ramaraoi	55.73
	Nummulites gamardensis	55.95
	A. aramaea, A. cucumiformis, A. avellana, A. dandotica	55.95
	Glomalveolina levis, Assilina yvettae	56.47
	G. dachalensis, A. azilensis, R. sindensis	56.47
	Glomalveolina primaeava	56.97
	Fallotella alavensis	57.30
	C. rajkae, C.? sireli, N. heberti, D. seunesi n. ssp.	57.30
	M. primitiva	58.91
	Periloculina n.sp. 4, Pseudonummuloculina n.sp., Laffitiena? n.sp., Coskinon n.sp.	58.91
	Laffittiena bibensis	60.86
	Protelphidium	60.86
	Laffittiena mengaudi	65.50
	Rhapsydionina liburnica (Adriatic)	65.50
	Hellenocyclina beotica, Siderolites calcitrapoides, Orbitolites gensacica	65.70
	Lepidorbitoides socialis,  O.(gr.) apiculata, Omphalocyclus macroporus	65.70
	Orbitolites media, O. (gr.) tissoti, Fallotia jacquoti, L. bisambergensis	68.55
	L. minor	68.55
	Abrardia. mosae, P. dordoniensis, L. campaniensis, Siderolites (gr.) vidali	69.57
	Adriatic: Raadshoovenia salentina, R. scarsellai, S. surrentina, Accordiella conica, K. tergestina, S. mediterranea	70.60
	Arnaudiella grossouvrei	75.38
	Subalveolina dordonica	80.84
	Scandonea samnitica (Adriatic)	81.30
	Lacazina group, Pseudostaffella sphaeroidea, S. santoniensis	83.53
	Dictopsella kiliani (Adriatic)	83.76
	Adriatic:  Pegidia dubia, C. fraasi	93.55
	Ovalveolina ovum, Chrysalidina gradata, Pseudopatellinella (gr.) cretacea, P. iberica, S. drorimensis	93.72
	O. (O.) concava, O.(C.) paeneconica, O. conica	94.75
	Adriatic:  Sellialveolina viallii, Ov. maccagnoae	94.75
	B. biplana, I. hungarica, O. corbarica, O. cuvillieri, N. convexa	96.01
	Adriatic: P. parvus, "V." dercourti	96.01
	Orbitolina (Mesorbitolina) texana	100.94
	S. conulus	105.05
	O. (M.) parva	106.42
	Simplorbitolina manasi	107.30
	D. pyrenaicus	108.77
	P. tunesiana (Adriatic)	113.00
	Praereticulinella cuvillieri (+ A. reicheli in Adriatic)	114.67
	I. rubiensis, D. pachymarginalis	119.50
	Palorbitolina lenticularis	120.25
	Praeorbitolina cormyi	121.90
	Rectodictyoconus giganteus, O. cuvillieri	123.45
	Praereticulinella reicheli	123.97
	N. friburgensis	124.64
	O. debelmasi	127.47
	P. jourdanensis, U. alpillensis	128.97
	Campanellula capuensis (Adriatic)	129.97
	C.? favrei	132.56
	V. camposaurii (Adriatic)	135.80
	P. salevensis	136.44
	Pfenderina neocomiensis	137.69
	Valdanchella miliani	139.56
	Feurtillia frequens	140.18
	P. courtionensis	141.25
	C. basiliensis, P. trochangulata	141.25
	P. ultragranulata (Adriatic)	141.48
	Anchispirocyclina lusitanica	144.53
	Kurnubia palastiniensis	145.60
	Alveosepta jaccardi	150.84
	P. aquitanica	152.59
	P. crusei	156.96
	Ataxella occitanica, Satorina apuliensis	163.54
	O. elliptica, Archaeosepta platierensis, Alzonella cuvillieri, K. blancheti	164.74
	Callorbis minor	168.86
	Timidonella sarda, Gutnicella cayeuxi	170.62
	Involutina liassica, Paleomayncina termieri, Lituosepta compressa, Orbitopsella praecursor	183.00
	P. butterlini	188.41
	Triasina hantkeni, Galeanella panticae, Galeanella laticarinata	199.60
	Triasina oberhauseri	205.71
	Aulotortus praegaschei	219.12
	Lamelliconus gr. procerus-multispirus	228.01
	Pilammina densa	240.00
	Paulbrownnimannia judicariensis, Meandrospira dinarica, Meandrospira pusilla	241.60
	Rectocornuspira kahlori	250.17
FAD
	Planorbulinella spp., D. italica	10.55
	P. rokae	13.41
	H. granulatatesta group	16.27
	B. melo group	16.97
	M. cushmani, M. mediterranea	17.54
	M. globulina	20.43
	M socini	21.23
	M. gunteri	23.03
	Myopgypsina septentrionalis	25.56
	M. complanatus, C. eidae	26.83
	Nummulites vascus	27.27
	C. droogeri	28.45
	Nephrolepidina praemaginata, E. formosoides	30.42
	Nummulites vascus, N. fichteli	33.88
	P. delicata, B. pygmaea, O. complanata, B. bulloides	33.88
	Nummulites retiatus	35.04
	A. stellata n. ssp., D. dispansa n. ssp.	35.04
	D. dispansa umbilicata, A. priabonensis	35.66
	Nummulites fabianii	37.24
	A. alpina, S. granulosus, B. vondershmitti, P. afyonica, A. alticostata danubica, A. stella praestellaris, D. trabayensis vicenzensis, D. augustae augustae	37.24
	H. reticulata, A. gomezi, M. drobneae	37.61
	Nummulites biedai, N. striatus	37.98
	D. dispansa dispansa, A. stellata stellaris, O. varians varians	37.98
	Alvoelina elongata, Nummulites perforatus, Num. brongniarti, Discocyclina pulcra baconica	40.44
	A. schwageri, A. roselli, N. ptukhiani, A. alticostata alticostata, O. varians scalaris	40.44
	Nummulites herbi, N. aturicus, Assilina gigantea, Discocyclina pulcra balatonica	40.99
	O. varians roberti, O. douvillei pannonicus, A. kecskemetii	40.99
	Alveolina prorrecta, N. sordensis, N. crassus	42.33
	A. stellata planospira, A. stellata stellata, A. alticostata cuvillierii	42.33
	Alveolina munieri, Nummulites beneharnensis, Assilina spira spira	45.44
	N. gratus, O. douvillei chudeaui, O. varians angoumensis, D. pulcra pulcra, D. discus	45.44
	Alveolina stipes, Nummulites laevigatus	48.60
	A. callosa	48.60
	Alveolina violae, N. manfredi, N. campesinus, Assilina major	49.12
	D. stratiemanuelis, O. varians portnayae, A. alticostata gallica, A. stella stella	49.12
	Alveolina dainellii, Nummulites praelaevigatus, Assilina laxispira	50.66
	D. fortisi simferopolensis, D. archiaci bartholomei	50.66
	D. fortisi fortisi, O. douvillei douvillei, A. stellata adourensis	52.15
	Alveolina schwageri, A. indicatrix, Nummulites planulatus, Discocyclina archiaci archiaci	52.83
	A. canavarii, A. sicula, A. marinellii, A. karreri, A. plana, A. escheri, O. schopeni crimensis	52.83
	Aveolina trempina, Nummulites involutus, Assilina adrianensis	53.09
	Alveolina corbarica, Nummulites exilis, Assilina leymerei	54.38
	Discosyclina archiaci staroseliensis, O. schopeni suviukayensis, D. pseudoaugustare	54.38
	Alveolina moussoulensis	55.73
	A. subpyrenaica, N. robustiformis, A. arenensis, Discosyclina archiaci bakhchisaraiensis, O. schopeni neumannae, A. taramellii, N. evae	55.73
	Alveolina ellipsoidalis, A. pasticillata, Nummulites minervensis	55.95
	A. aff. arenensis, O. schopeni ramaraoi	55.95
	Nummulites gamardensis	56.47
	A. aramaea, A. cucumiformis, A. avellana, A. dandotica, G. lepidula	56.47
	Glomalveolina levis, Assilina yvettae	57.30
	D. tenuis, A. axilensis	57.30
	G. dachalensis, D. seunesi n. ssp.	58.14
	Glomalveolina primaeava, Fallotella alavensis	58.91
	C. rajkae, N. heberti, R. sindensis, O. schopeni ramaraoi, D. seunesi seunesi	58.91
	M. primitiva	60.86
	Periloculina n.sp. 1, Pseudonummuloculina n.sp., Laffitiena? n.sp., Coskinon n.sp., C.? sireli	60.86
	Laffittiena bibensis	65.50
	Hellencyclina beotica, Orbitolites gensacica	69.23
	Rhapsydionina liburnica (Adriatic)	69.23
	Laffitteina mengaudi	69.78
	Laffitteina socialis, Omphalocyclus macroporus	69.78
	O. (gr.) apiculata, L. minor	70.39
	Siderolites (gr.) calcitrapoides, L. bisambergensis	70.60
	Fallotia jacquoti	75.43
	L. campaniensis	76.30
	Orbitolites media, Arnaudiella grossouvrei	76.74
	Abrardia mosae	79.68
	Raadshoovenia salentina (Adriatic)	81.30
	Subalveolina dordonica, O.(gr.) tissoti, Siderolites(gr.) vidali	83.53
	S. santoniensis	83.76
	P. dordoniensis	83.76
	Keramosphaerina tergestina (Adriatic)	84.63
	Lacazina gr.	85.85
	Scandonea samnitica (Adriatic)	85.85
	S. surrentina (Adriatic)	87.57
	Pseudostaffella sphaeroidea	89.02
	Adriatic: Accordiella conica, R. scarsellai	89.02
	Dictopsella kiliani (Adriatic)	92.00
	C. fraasi (Adriatic)	94.68
	Pegidia dubia (Adriatic)	95.06
	Ovalveoloina ovum, Chrysalidina gradata,  Pseudopatellinella (gr.) cretacea, S. drorimensis	96.01
	Sellialveolina viallii (Adriatic)	96.01
	P. iberica, O. corbarica	99.58
	Adriatic: P. parvus	99.58
	O.(C.) paeneconica, O.(O.) concava, N. convexa	100.94
	Adriatic: I. hungarica, O. maccagnoae, "V." dercourti	100.94
	D. pyrenaicus, I. hungarica	110.24
	S. conulus	112.00
	Simplorbitolina manasi	113.00
	A. reicheli (Adriatic)	115.00
	Orbitolina (Mesorbitolina.) texana, Praereticulinella cuvillieri	118.00
	O. (M.) parva, D. pachymarginalis, I. rubiensis	121.00
	Praeorbitolina cormyi	122.93
	O. cuvillieri	125.00
	Rectodictyoconus giganteus, Palorbitolina lenticularis	127.20
	Praereticulinella reicheli	128.30
	O. debelmasi, P. jourdanensis, U. alpillensis	130.94
	Campanellula capuensis (Adriatic)	133.85
	C.? favrei, P. salevensis	140.18
	Valdanchella miliani	141.19
	Pfenderina neocomiensis	141.25
	V. camposauri (Adriatic)	141.55
	P. courtionensis	142.96
	Feurtillia frequens	144.53
	Protopeneropis trochangulata, Anchispirocycina lusitanica	149.44
	Kilianina rahonensis, Protopeneropis aquitanica, Alveosepta powersi	152.59
	Alveosepta jaccardi	161.21
	Kurnubia palastiniensis	162.35
	O. elliptica, Ataxella occitanica, Satorina apuliensis, K. blancheti	164.93
	C. basiliensis ?	165.66
	P. crusei	168.66
	Archaeosepta platieresis, Alzonella cuvillieri	168.86
	Callorbis minor	170.62
	Timidonella sarda, Gutnicella cayeuxi	172.49
	P. butterlini	190.41
	Orbitopsella praecursor, Lituosepta compressa, Paleomayncina termieri	193.25
	Involutina liassica	198.44
	Triasina hantkeni	205.71
	Triasina oberhauseri, Galeanella panticae, Galeanella laticarinata	216.53
	Lamelliconus gr. procerus-multispirus	229.43
	Aulotortus praegaschei	234.56
	Paulbrownnimannia judicariensis, Pilammina densa	242.49
	Meandrospira dinarica	245.17
	Meandrospira pusilla	248.08
	Rectocornuspira kahlori	250.38



Jurassic Benthic Foram datums (Bassoullet'97)	event		204/204/120			Jean-Paul Bassoullet -- chapter on "Les Grands Foraminiferes";  in Groupe Francais d'etude du Jurassique (1997)
LAD
	Anchispirocyclina lusitanica	144.82
	Protopeneroplis striata, Pseudocyclammina parvula-muluchensis, Freixialina planispiralis, Anchispirocyclina neumannae	145.46
	Anchispirocyclina maynci	145.69
	Kurnubia palastiniensis 	146.96
	Valvulina gr. lugeoni	149.59
	Audienusina fourcadei	149.89
	Labyrinthina mirabilis, Parurgonina caelinensis, Rectocyclammina chouberti	149.89
	Alveosepta powersi (rare)	150.27
	Anchispirocyclina praelusitanica (rare)	150.84
	Neokilianina rahonensis	150.84
	Conicokurnubia orbitoliniformis (rare)	152.20
	Alveosepta jaccardi	152.59
	Kurnubia wellingsi	153.39
	Praekurnubia crusei	156.81
	Mesoendothyra gr. croatica, Pseudocyclammina maynci, Paleopfenderina salernitana  	161.21
	Chablaisia chablaisensis	161.21
	Satorina apuliensis (rare)	161.21
	Trocholina gigantea	162.35
	Ataxella occitanica	164.48
	Conicopfenderina mesojurassica (rare)	164.74
	Haurania deserta, Amijiella amiji, Archaeosepta platierensis, Alzonella cuvillieri, Kilianina blancheti	164.74
	Spiraloconulus giganteus	164.74
	Orbitammina elliptica, Meyendorffina bathonica	164.84
	Spiraloconulus perconigi (rare)	167.68
	Callorbis minor	169.25
	Gunticella gr. cayeuxi	171.21
	Mesoendothyra sp.	175.60
	Pseudocyclammina liasica	182.20
	Involutina liassica	182.70
	Planisepta compressa	184.46
	Bosniella oenensis (rare), Biokovina gradacensis (rare)	184.68
	Orbitopsella dubari	184.68
	"Everticyclammina" sp. A	184.68
	Paleomayncina termieri	185.73
	Orbitopsella praecursor	186.95
	Orbitopsella primaeva	187.75
	Pseudopfenderina butterlini	188.24
	Lituosepta recoarensis	191.43
FAD
	Totinosuella peneropliformis	146.96
	Anchispirocyclina neumannae, Protopeneroplis trochangulata  	147.16
	Anchispirocyclina maynci	148.98
	Anchispirocyclina lusitanica	149.89
	Pseudocyclammina parvula-muluchensis, Freixialina planispiralis	151.52
	Feurtillia frequens	151.75
	Audienusina fourcadei	152.20
	Rectocyclammina chouberti	152.59
	Alveosepta powersi (rare)	154.34
	Neokilianina rahonensis	154.53
	Labyrinthina mirabilis, Parurgonina caelinensis, Everticyclammina virguliana	154.74
	Pseudocyclammina lituus	156.08
	Anchispirocyclina praelusitanica (rare)	156.81
	Alveosepta jaccardi	157.66
	Conicokurnubia orbitoliniformis (rare)	161.21
	Praekurnubia crusei, Nautiloculina oolithica	161.21
	Kurnubia wellingsi	162.86
	Kurnubia palastiniensis	163.03
	Satorina apuliensis (rare)	163.46
	Pseudocyclammina maynci, Paleopfenderina salernitana	164.74
	Chablaisia chablaisensis, "Conicospirillina" basiliensis	164.93
	Praekurnubia crusei, Ataxella occitanica, Trocholina gigantea	165.52
	Orbitammina elliptica, Meyendorffina bathonica, Kilianina blancheti, Valvulina gr. lugeoni	166.11
	Conicopfenderina mesojurassica (rare)	166.31
	Alzonella cuvillieri	166.50
	Spiraloconulus giganteus	166.89
	Archaeosepta platierensis	169.64
	Timidonella sarda (rare)	169.93
	Callorbis minor	170.33
	Spiraloconulus perconigi (rare), Timidonella sarda (rare)	175.16
	Gunticella gr. cayeuxi	175.16
	Protopeneroplis striata, Mesoendothyra gr. croatica	175.60
	Pseudocyclammina liasica	184.13
	Orbitopsella dubari	185.73
	Orbitopsella praecursor	187.55
	Planisepta compressa	188.08
	Orbitopsella primaeva	189.60
	Bosniella oenensis (rare), Biokovina gradacensis (rare)	190.41
	Paleomayncina termieri, Pseudopfenderina butterlini	190.41
	Haurania deserta, Amijiella amiji	191.22
	Lituosepta recoarensis	194.06
	"Everticyclammina" sp. A, "Mesoendothyra" sp.	194.47
	Involutina liassica	199.60


Fusulinids (Carb-Perm)	:	Numbered Global Zone	Global Zone Name	Fusulinid Major Marker	Boreal Fusulinid Zone	Tethyan Fusulinid Zone	N.Amer. Mid-Continent Zone	Mid-Continent Zone (Ross-Ross'95 and '88)	_METACOLUMN_OFF		Davydov (1996, Carb-Perm chapters in GTS2004, unpublished zonation table to GTS2004, and unpublished Permian correlation chart), Ross and Ross (1988, 1995b).

Numbered Global Zone	block	50	204/204/82	notitle
	TOP	251.00
	Lf4	252.40
	Lf3	253.80
	Lf2	256.44
	Lf1	260.40
	Gf6	264.45
	Gf5	266.02
	Gf4	266.68
	Gf3	268.00
	Gf2	269.56
	Gf1	270.60
	Cf13	273.35
	Cf12	275.60
	Cf11	277.80
	Cf10	280.11
	Cf9	284.40
	Cf8	288.48
	Cf7	292.56
	Cf6	294.60
	Cf5	296.14
	Cf4	297.24
	Cf3	298.34
	Cf2	298.67
	Cf1	299.00
	Pf22	299.98
	Pf21	301.21
	Pf20	302.43
	Pf19	303.17
	Pf18	303.90
	Pf17	304.68
	Pf16	305.20
	Pf15	305.72
	Pf14	306.50
	Pf13	307.12
	Pf12	308.06
	Pf11	309.36
	Pf10	310.14
	Pf9	310.84
	Pf8	311.70
	Pf7	312.66
	Pf6	313.94
	Pf5	314.90
	Pf4	315.96
	Pf3	317.04
	Pf2	317.57
	Pf1	318.10
	Mf17	321.01
	Mf16	324.33
	Mf15	326.40
	Mf14	330.18
	Mf13	333.02
	Mf12	335.85
	Mf11	339.63
	Mf10	341.52
	Mf9	342.47
	Mf8	345.30
	Mf7	348.08
	Mf6	348.91
	Mf5	350.86
	Mf4	352.25
	Mf3	355.03
	Mf2	357.31
	Mf1	359.20

Global Zone Name	block	150	204/204/82
	TOP	251.00
	Palaeofusulina sinensis - Parananlingellia	252.40
	Palaeofusulina minima	253.80
	Paradunbarulla	256.44
	Codonofusiella	260.40
	Rauserella	264.45
	Afganella schenki	266.02
	Afganella tereshkovae	266.68
	Neoschwangerina tenuis	268.00
	Cancellina	269.56
	Skinnerella	270.60
	Praeskinnerella pavlovi	273.35
	Brevaxina	275.60
	Chalaroschwagerina vulgaris	277.80
	Parafusulina	280.11
	Pseudofusulina	284.40
	Zigarella urdalensis - Z. plicatissima	288.48
	Schwagerina vernueili	292.56
	Schwagerina moelleri 	294.60
	Sphaeroschwagerina gigas	296.14
	Pseudoschwagerina robusta	297.24
	Schwagerina nux	298.34
	Sphaeroschwagerina fusiformis	298.67
	Sphaeroschwagerina vulgaris 	299.00
	Ultradaixina bosbytauensis / Schwagerina robusta	299.98
	Daixina sokensis	301.21
	Jigulites jigulensis	302.43
	Rauserites stuckenbergi	303.17
	Rauserites rossicus	303.90
	Rauserites quasiarcticus	304.68
	Montiparus subcrassulus	305.20
	Montiparus paramontiparus	305.72
	Protriticites pseudomontiparus - Obsoletes obsoletus	306.50
	Protriticites ovoides - Praeobsoletes burkemensis	307.12
	Fusulinella bocki - Fusulina cylindrica	308.06
	Fusulinella colaniae - Beedyina kamensis	309.36
	Moellerites lopasnensis - Fusulinella subpulchra	310.14
	Aljutovella priscoidea	310.84
	Aljutovella aljutovica	311.70
	Verella spicata - Al. tikhonovichi	312.66
	Profusulinella parva - Ozawainella pararhomboidalis	313.94
	Staffellaeformis staffellaeformis - Pseudostaffella praegorskyi	314.90
	Pseudostaffella antiqua	315.96
	Semistaffella variabilis	317.04
	Semistaffella minuscilaria	317.57
	Plectostaffella bogdanovkensis	318.10
	Monotaxinoides transitoriusis - Eoplectostaffella acuminulata	321.01
	Eostaffellina mirifica - Eo. protvae	324.33
	Pseudoendothyra globosa - Neoarchaediscus parvus	326.40
	Eostaffella tenebrosa - Endothyranopsis sphaericus	330.18
	Eostaffella ikensis - Bradyina rotula	333.02
	Eostaffella proikensis - Archaediscus gigas	335.85
	Endothyranopsis compressus - Archaediscus krestovnikovi	339.63
	Uralodiscus rotundus	341.52
	Uralodiscus primaeva	342.47
	Eoparastaffella simplex	345.30
	Dainella chomatifera	348.08
	Spinoendothyra costifera	348.91
	Latiendothyra latispiralis	350.86
	Palaeospiroplectammina tchernyshinensis - Chernyshinella glomiformis	352.25
	Prochirnyshinella disputabilis - Tournavellina beata	355.03
	Bisphaera malevkensis	357.31
	Quasiendothyra communis	359.20

Fusulinid Major Marker	event		204/204/120
FAD
	Paleofusulina, Colaniella	253.80
	Codonofusiella, Reichelina	260.40
	Nanlingella	262.43
	Rauserella	264.45
	Metadoliolina	266.02
	Yabeina	266.68
	Neoschwagerina	268.00
	Cancellina cutalensis	269.56
	Skinnerella	270.60
	Brevaxina	275.60
	Parafusulina, Chalaroschwagerina, Pamirina 	280.11
	Pseudofusulina prima	284.40
	Pseudofusulina	288.48
	Schwagerina vernueili	292.56
	Schwagerina moelleri 	294.60
	Pseudoschwagerina spp.	297.24
	Sphaeroschwagerina vulgaris 	299.00
	Schwagerina	299.98
	Schellwienia, Dutkevichia	301.21
	Daixina	303.90
	Triticites	305.72
	Protriticites	307.12
	Fusulinella	310.14
	Beedyina	310.84
	Aljutovella aljutovica	311.70
	Verella	312.66
	Schubertella	314.90
	Pseudostaffella	315.96
	M. marblensis	318.10
	Plectostaffella	318.52
	Eosigmoilina explicata	321.01
	Eosigmoilina	326.40
	Howchinia gibba	335.85
	Ar. krestovnikovi	339.63
	Eostaffella	341.52
	ARCHAEDISCIDS	342.47
	Eoparastaffella simplex	345.30
	Dainella	348.08
	Tuberculiate forams	348.91
	Palaeospiroplectammina tchernyshinensis	352.25
LAD
	Fusulinella / Beedyina(?)	305.72
	ARCHAEDISCIDS	310.84
	Quasiendothyra	357.31

Boreal Fusulinid Zone	block	180	204/204/82
	TOP	275.60
	Parafusulina jenkinsi - P. solidissima	277.80
	Parafusulina lutugini - Pseudofusulina solida	280.11
	Pseudofusulina concavutas	284.40
	Zigarella urdalensis - Z. plicatissima	288.48
	Schwagerina vernueili	292.56
	Schwagerina moelleri  - Eoparafusulina paralinearis	294.60
	Schwagerina firma - Sphaeroschwagerina sphaerica - S. gigas	296.14
	Schwagerina fecunda - Pseudoschwagerina robusta	297.24
	Schwagerina nux	298.34
	Sphaeroschwagerina fusiformis	298.67
	Sphaeroschwagerina vulgaris 	299.00
	Ultradaixina bosbytauensis - Schwagerina robusta	299.98
	Daixina sokensis - Schellwienia modesta - Schellwienia arctica - Daixina enormis	301.21
	Daixina ruzhenzevi - Jigulites jigulensis	302.43
	Daixina crispa - Rauserites stuckenbergi	303.17
	Daixina fragilis - Rauserites rossicus	303.90
	Raus. variabilis - Rauserites quasiarcticus	304.68
	Montiparus subcrassulus	305.20
	Montiparus paramontiparus - Wedekindellina ellipsoides	305.72
	Protriticites pseudomontiparus - Obsoletes obsoletus - first Oketaella, Plectofusulina	306.50
	Protriticites ovoides - Praeobsoletes burkemensis - Quasifusulinoides fusiformis	307.12
	Fusulinella bocki - Puchrella eopulchra	308.06
	Fusulinella colaniae - Beedyina kamensis	309.36
	Moellerites lopasnensis - Fusulinella subpulchra	310.14
	first Beedyina - Aljutovella priscoidea	310.84
	Aljutovella aljutovica - Schubertella pauciseptata	311.70
	Verella spicata - Al. tikhonovichi	312.66
	Profusulinella primitiva - Ozawainella pararhomboidalis	313.94
	Staffellaeformis staffellaeformis - Pseudostaffella praegorskyi	314.90
	Pseudostaffella antiqua	315.96
	Plectostaffella varvariensis - Semistaffella variabilis - Eostaffella pseudostruvei - Eo. postmosquensis	317.04
	Plectostaffella bogdanovkensis	318.10
	Eosigmoilina explicata - Monotaxinoides subplana	321.01
	Eostaffellina protvae	324.33
	Pseudoendothyra globosa - Neoarchaediscus parvus	326.40
	Eostaffella tenebrosa - Endothyranopsis sphaericus	330.18
	Eostaffella ikensis	333.02
	Eostaffella proikensis - Archaediscus gigas	335.85
	Endothyranopsis compressus - Archaediscus krestovnikovi [probably Pararchaediscus kokjubensis]	339.63
	Uralodiscus rotundus	341.52
	Uralodiscus primaeva	342.47
	Eoparastaffella simplex - Eoendothyranopsis donica - Eopara. rotunda - Eopara. ovalis	345.30
	Dainella chomatifera - Tournayella (Eoforschia) moelleri	348.08
	Spinoendothyra costifera - Tuberendothyra tuberculata	348.91
	Palaeospiroplectammina tchernyshinensis - Septabrunsiina krainica	350.86
	Chernyshinella glomiformis - Cherny. paraglomiformis	352.25
	Prochirnyshinella disputabilis - Tournavellina beata	355.03
	Bisphaera malevkensis - Earlandia minima	357.31
	Tournayellina pseudobeata	359.20

Tethyan Fusulinid Zone	block	180	204/204/82
	TOP	251.00
	Palaeofusulina sinensis - Parananlingellia	252.40
	Palaeofusulina minima	253.80
	Galowainella meintiensis - Shindella pamirica - Paradunbarulla	256.44
	Codonofusiella kwangsiana - Pseudunbarula arpaensis - Lepidolina kurmaensis	260.40
	Yabeina globosa - first Nanlingella - Lepidolina multisepatata - Dunbarula mathieui	262.43
	Yabeina archaica - Colania - Neoschwagerina margaritae - first Dunbarula. Kahlerina, Rauserella. Abadehella	264.45
	Neoschwagerina deprati - Afganella schenki	266.02
	Neoschwagerina confragaspira - Afganella tereshkovae	266.68
	Neoschwagerina simplex - Praesumatrina schellwieni	267.34
	Neoschwagerina tenuis - Praesumatrina neoschwagerinoides	268.00
	Cancellina cutalensis - Skinnerella yabei - first Eopolydiexodina	269.56
	Armenina pamirensis - first Skinnerella	270.60
	Pseudodoliolina	271.10
	Misellina parvicostata - Praeskinnerella pavlovi	273.35
	Misellina minor - Brevaxina dyhrenfurthi - Praeskinnerella parviflucta	275.60
	Chalaroschwagerina vulgaris - Ch. inflata - Darvasites contractus	277.80
	Chalaroschwagerina solita - Ch. gallowayi - first Pamirina	280.11
	Robustoschwagerina schellwieni - Paraschwagerina mira - Schwagerina moelleri - Darvasites eocontractus - Zigarella postcallosa	294.60
	Schwagerina firma - Sphaeroschwagerina sphaerica	296.14
	Schwagerina fecunda - Pseudoschwagerina robusta	297.24
	Pseudoschwagerina saibulakensis	298.34
	Sphaeroschwagerina fusiformis	298.67
	Sphaeroschwagerina vulgaris aktjubensis	299.00
	Ultradaixina bosbytauensis - Schwagerina robusta	299.98
	Daixina sokensis - Daixiana vasylkovskyi - Schellwienia modesta - Schellwienia malkovskyi - Dutkevitchia dastarensis	301.21
	Daixina ruzhenzevi  - Schagonella implexa	302.43
	Daixina crispa - Schagonella proimplexa	303.17
	Schagoriella primitiva - Rauserites rossicus	303.90
	Raus. variabilis - Rauserites quasiarcticus	304.68
	Montiparus subcrassulus	305.20
	Montiparus paramontiparus	305.72
	Protriticites pseudomontiparus - Obsoletes obsoletus	306.50
	Protriticites ovoides - Praeobsoletes burkemensis - Quasifusulinoides fusiformis	307.12
	Fusulinella bocki - Puchrella eopulchra	308.06
	Fusulinella colaniae - Beedyina kamensis	309.36
	Moellerites lopasnensis - Fusulinella subpulchra	310.14
	first Beedyina - Aljutovella priscoidea	310.84
	Aljutovella aljutovica - Schubertella pauciseptata	311.70
	Biseriella parva - Neoarchaediscus postrugosus	324.33
	Endothyranopsis crassus - Cribrospira mira	335.28
	Eodiscus eospirillinoides - Lituotubella glomospiroides - ? - Dainella chomatica - Plectogyra gibbera	345.02
	Tuberendothyra tuberculata - Tournayella gigantea	348.50
	Septabrunsiina krainica - Septatournayella segmentata	355.03
	Bisphaera malevkensis	357.31
	Vicinesphaera angulata	359.20


N.Amer. Mid-Continent Zone	block	180	204/204/82		 Davydov'96 or unpublished ExxonMobil'01
	TOP	256.44
	Lanchechites splendens - Codonofusiella paradoxica 	260.40
	Polydiexodina capitanensis - Rauserites eratica 	264.45
	Polydiexodina spp. - Parafusulina wordensis - Parafus. lineata - Parafus. deliciasensis	266.68
	Parafusulina rothi - P. maleyi - P. sellardsi	268.00
	Parafusulina bose - P. attenuata - P. splendens - first Skinnerella	270.60
	Parafusulina durhami - P.  fountaini	273.35
	Parafusulina leonardensis - Para. deltoides - Praeskinnerella guembeli	275.60
	Robustoschwagerina stanislavi - Chalaroschwagerina hawkinsi	276.15
	TOP	277.80
	Chalaroschwagerina solita - Ch. nelsoni - Eoparafusulina linearis	284.40
	Schwagerina cribroseptata - Schwagerina tersa - Pseudofusulina lineonada	288.48
	Schwagerina aff. moelleri - Paraschwagerina gigantea - Eoparafusulina allisonensis	294.60
	TOP	298.34	dashed
	Paraschwagerina kansanensis - Schwagerina campa - Pseudofusulina longissimoidea - Leptotriticites koschmanni - Triticites ventricosus	299.98
	Triticites sacramentornsis - Dunbarinella skinneri - Triticites plummeri - Dunbarinella ervinensis	301.21
	Triticites secalicus - Waeringella spriveyi	303.17	dashed
	Triticites cullomensis - Kansanella neglecta	304.29	dashed
	Triticites rangerensis - Kansanella tenius	304.42	dashed
	Triticites ohioensis - Triticites celebroides	304.68	dashed
	Triticites pygmaeus - Eowaeringelia ultimata	305.33
	Bartramella bartrami - Fusulina acme	306.11
	Plectofusulina spp. - Beedyina girtyi	307.12
	Beedyina novomexicana	307.52	dashed
	Wedekindellina henbesti - Wedekindellina excentrica	307.92	dashed
	Beedyina leei - Wedekindellina euthysepta - Fusulinella iowensis	308.71	dashed
	Fusulinella texana - Fusulinella(?) insolita	309.75	dashed
	Fusulinella proxina - Fusulinella acuminata	310.38	dashed
	Profusulinella regia	310.84
	Profusulinella plummeri - Profusulinella copiosa - first Schubertella spp.	311.70
	Pseudostaffella - Hemigordius	315.96
	Millerella marblensis / pressa - Globivalvulina bulloides	318.10
	Millerella (early forms)	319.06
	Brenckleina rugosa - Eosigmoilina robertsoni	325.16
	Millerella / Millerella tortula-designata	331.60
	assemblage of Archaediscus, Endostaffella discoidea, Asteroarchaediscus, and Neoarchaediscus	334.43
	assemblage of "Urbanella", Globospiroplectammina windsorensis, Septabrunsiina mackeei, Archaediscid (angulatus-coiling), Cribrokamaena citrosa	337.74
	Globoendothyra baileyi - Paraarchaediscus (involutus stage)	341.52
	Viseidiscus - Globoendothyra piasae	344.45
	Eoparastaffella-Oendothyranopsis / E. moelleri gr. / Eoforschia-Paradainella	348.08
	Inflatoendothyra - Spinoendothyra - Tuberendothyra tuberculata	348.91
	Palaeospiroplectammina tchernyshinensis - Chernyshinella glomiformis - A. rjausakensis - Eochernychinella - Septabrunsiina minuta - S. aff. krainica	355.03
	Unilocular-Bilocular assemblage (evolutina, bisphaera, calcisphaerids, radiosphaerids)	359.20


Mid-Continent Zone (Ross-Ross'95 and '88)	block	180	214/214/72
	TOP	253.80
	Parabaultonia / Codonofusiella paradoxica - Polydiexodina shumardi / Polydlexodina capitanensis /  	264.45
	Pa. rothi / Pa. wordensis / Pa. sellardsi / Pa. sullivanensis	269.56
	Skinnerina / Pa. boesei / Pa. attenuata	270.60
	? / S. setum  / Parafusulina fountaini / Pa. durhami	273.35
	Parafusulina brooksensis, Pa. vidriensis	274.09
	Parafusulina spissisepta, Pa. leonardensis	274.86
	Parafusulina schucherti / Pa. allisonensis / Pa. bakeri / Pa. diabloensis	275.60
	Robustoschwagerina stanislavi,  Schwagerina guembeli, Schwagerina crassifectoria, Chalaroschwagerina hawkinsi	276.15
	Eoparafusulina linearis - Schwagerina diversiformis - Chalaroschwagerina nelsoni - Pseudoschwagerina gerontica - Sn. laxissima - Pseudoschwagerina convexa 	284.40
	Eoparafusulina allisonensis -Paraschwagerina gigantea / Schwagerina compacta - Pseudoschwagerina uddeni - Stewartina - Rugosochusenella /  Pseudoschwagerina texana / Pseudoschwagerina beedei - Paraschwagerina	297.24	dashed
	TOP	298.34	dashed
	Triticites meeki, T. rockensis, L. gienensis, T. ventricosus, S. longissimoidea	299.98
	Triticites subventricosus, T. whetstonensis, Schubertella shetensis	300.59
	Triticites callosus, T. cullomensis, T. plummeri	301.21
	Triticites mcgrewensis, Dunbarinella	303.90
	Triticites latensis, T. newelli, Kansanella (K.) joensis	304.10	dashed
	Triticites primarius, Kansanella neglecta	304.29	dashed
	Triticites ohioensis, T. collus, T. nebraskensis	304.68
	Kansanella (Oiwanella) winterensis, T. cf. ohioensis	305.20
	Quasifusulinoides, Eowaeringella, Okethelia	305.33
	TOP	305.80
	Beedeina sulphurensis, B. eximia, Bartramella	306.11
	Beedeina cf. B. haworthi, B. cf. B. weintzi, Bartramella	306.50	dashed
	Beedeina novomexicana, B. bowensis, B. euryteines, Wedekindellina ellipsoides, Plectofusulina	307.52	dashed
	Beedeina leei, B. apachensis, B. cedarensis, Wedekindellina henbesti	307.92	dashed
	Beedeina(?) insolita, B. arizonensis, Wedekindella euthysepta	308.31	dashed
	Fusulinella famula, F. iowensis leyi, F. dosensis, F. cabezasensis	308.71	dashed
	Fusulinella prolifica, F. devexa, F. haywardi	310.38	dashed
	Profusulinella regia	310.84
	Profusulinella decora, Eostaffella powwowensis	312.39
	Profusulinella copiosa	313.94
	large Millerella spp., Ozawainella?, Eostaffella	317.04
	Millerella marblensis, Ozawainella(?), Eostaffella cooperi, Millerella pressa, Eostaffella pinguis	318.10
	TOP	318.58
	Millerella (primitive), "Millerella" cooperi	319.06
	Brenckleina rugosa - Eosigmoilina robertsoni	325.16
	Astroarchaediscus baschkiricus	328.38
	TOP	328.58
	"Millerella" tortula, "M." designata	331.60
	Hemiarchaediscus sp.	332.10
	Endostaffella discoidea, Neoarchaediscus, Asteroarchaediscus 	334.43
	Globoendothyra baileyi	337.74
	Nodosarchaediscus, Archaediscus	341.52
	Eoendothyranopsis scitula, Globoendothyra piasae, Skippella redwallensis, Endothyra aff. E. obsoleta	344.45
	Priscella prisce, Endothyra spp., Tetataxis spp.	345.30
	Palaeospiroplectammina aff. parva, Tuberendothyra tuberculata	348.91
	TOP	352.25
	Palaeospiroplectammina tchernyshinensis, Granuliferella spp.	355.03



Calcareous Nannofossils	:	NN,NP,CC Zone	NN,NP,CC Subzone	CN,CP,NC Zone	CN,CP,NC Subzone	Zone Marker (and Jur-Tri) Nanno Datums	Other Nanno FAD/LAD	Additional Plio-Pleist datums	All Tropical Nanno Datums Combined	Boreal UC,BC,NJ,NT Nanno Zone (E.Cret-Carnian)	Boreal UC-BC Nanno Subzone	Boreal NK Nanno zones	Boreal KN Nanno zones	Boreal Nanno Zone Marker	Boreal Nanno Subzone and other markers	All Boreal Nanno Datums Combined

NN,NP,CC Zone	block	40	210/217/221	notitle		NEOGENE = mainly Lourens et al. (GTS2004 tables); PALEOGENE = Tables in Berggren et al. (1995a, b).  Late CRETACEOUS = mainly Erba et al (1995) as tabulated by ODP Leg 171B Init. Repts. (Table 2, p. 17-18).  Middle and Early CRETACEOUS = compiled by Jim Bergen, based on publications by Tim Bralower et al (1995),  J. Bergen (1994) and Eric Kanael
	TOP	0.00
	NN21	0.29		Pleistocene Nanno Zone NN21 may possibly be subdivided further:  Acme of E. huxleyi; LAD Pontosphaera indooceanica; and dominance reversal of G. caribbeanica / E. huxleyi.  The latter event occurs earlier in tropical-subtropical waters (_O18 stage 5b&5a) than in transitional (_O18 stage 4) (Thierstein et al., 1977).  The FAD of Gephyrocapsa ericsonii and G. muellerae approximates the base of NN21.  [From summary in Perch-Nielsen, 1985; Plankton Stratigraphy]
	NN20	0.44
	NN19	1.93		Pleistocene Nanno Zone NN19 can be subdivided by: FAD of G. caribbeanica; LAD of C. macintyrei and of H. sellii, and FAD of G. oceanica (see CN13 subzonation)
	NN18	2.39
	NN17	2.49
	NN16	3.70
	NN15	3.92
	NN14	4.13		Pliocene Nanno Zones NN13 and NN14 are often merged to NN13/NN14, because D. asymmetricus marker is often rare or difficult to identify (Martini, 1980).
	NN13	5.12
	NN12	5.59
	alt NN11a	8.11
	NN11	8.29		Miocene Nannofossil Zone NN11 begins with either the FAD of D. berggreni (an earlier event) or of D. quinqueramus; the definition problem arises depending if these two taxa are considered to be the same species.  Bukry (1981) defined Zone CN8b beginning with FAD of D. neorectus and/or FAD of D. loeblichii, and ending with FAD of D. surculus; but these events are not calibrated in the scales of Berggren (in prep, SEPM) or Leg 145.  Aubry (in Berggren et al., 1995) indicates that FAD of D. berggrenii defines base of both NN11 and CN9; and this placement is shown in this chart.
	NN10	9.53
	NN9	10.55
	NN8	10.89
	NN7	11.90
	NN6	13.53
	NN5	14.91
	NN4	17.95
	NN3	18.28		Berggren et al (1995) had shown FAD of S. belemnos as defining base of CN2.  But Lourens et al (2004) assign base-CN2 as equivalent to base NN3
	NN2	22.82
	NN1	23.14		The LAD of 'R. bisectus' is used to approximate the NP25/NN1 boundary in high latitudes; and was "substituted for H. recta, the marker of the NP15/NN1 boundary in Martini's (1971) zonal scheme" by Aubry (in Berggren et al., 1995).
	NP25	27.27
	NP24	30.04
	NP23	32.51	dashed	Diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  For simplicity, I have placed the associated Zone NP23; CP17 base with the mid-latitude level (32.3 Ma).
	NP22	33.05
	NP21	34.78
	NP19-20	35.17		Zone NP19-20 has definition problems -- Eocene Nanno Zone NP19-20 is combined in most zonations, because base of NP20 (FAD Sphenolithus pseudoradians) was later found to be a very resticted taxon with a time-transgressive FAD (as early as NP15!).  Base of Zone NP19-20 redefined by Aubry to be FAD of 'I. recurvus', rather than LAD of 'C. grandis'.  [Reviewed in Perch-Nielsen, 1985].  However, the age assignments now implies that this shortened NP19-20 is only about 0.1 m.y. duration.  The LAD of 'C. grandis' (Martini, 1976, definition) would appear to be more useful?
	NP18	36.84		Genus 'Chiasmolithus' is rare in low latitudes, so NP17 and NP18 are often combined.  NP 17/18 boundary = Working definition for Middle/Late Eocene boundary.
	NP17	39.71		Genus 'Chiasmolithus' is rare in low latitudes, so NP17 and NP18 are often combined.
	NP16	42.42	dashed
	NP15	46.57		Eocene Nanno Zone NP15-16 is combined in some zonal schemes, because marker of NP16 (base = LAD 'Rhabdolithus gladius') is rare or often absent.  [See Perch-Nielsen, 1985, for details.]   However, Aubry (in Berggren et al., 1995), could distinquish 3 subzones in NP15 using markers similar for subzones of CP13 (with a total duration of 4 m.y.), and estimated that NP16 was a valid zone with duration of nearly 3 m.y.
	NP14	49.43
	NP13	50.47		Eocene Nanno Zone CP11 base is FAD of Toweius? crassus; and this event is often used to approximate base of NP13 (see discussion in Perch-Nielsen, 1985).  Following Aubry (in Berggren et al., 1995), NP13 and CP11 bases are made coeval, but there is no direct CP11 calibration.
	NP12	53.23
	NP11	54.09		Eocene Nanno Zone NP11 is essentially a "gap" zone, recognized by absence of NP10 or NP12 zonal markers.
	NP10	55.67		Base of NP10 is in uppermost Paleocene -- Eocene/Paleocene boundary nanno "Tribrachiatus bramlettei" is assigned to top of Paleocene by Aubrey (in Berggren et al., 1995); but Leg 145 placed it about 2 m.y. higher in lower Eocene.  This is often equated with base of CP9 (FAD of Discoaster diastypus), but there is no direct calibration.  Indeed, Leg 145 table implies about 1.0 m.y. separation (although, this is probably not a direct estimate).
	NP9	56.97		Zone NP9 spans Paleocene/Eocene boundary.  Paleocene Nanno Zone NP9 contains FAD's of several Discoaster species and other groups; producing a peak in nannofossil diversity.  Faciculithus becomes rare toward the top; and this FAD is sometimes used to approximate Paleocene/Eocene boundary (Perch-Nielsen, 1985).
	NP8*	57.66
	NP8	58.14		Paleocene nanno zone "NP8" has different definitions for the base.  H. riedelii FAD was former definition, and is used by Aubrey (in Berggren et al., 1995).  However, Perch-Nielsen (1985) considered this marker to be unreliable, so recommended usage of FAD of D. nobilis (which is also base of CP7).
	NP7	58.32
	NP6	59.17
	NP5	60.48
	NP4	62.82
	NP3	64.28		Paleocene Nanno Zone NP3 is subdivided into 4 subzones in North Sea by progressive FAD's of 'P. rosenkrantzii', N. modestus', and 'P. martinii' (Perch-Nielsen, 1985). [Ref.g]
	NP2	64.91
	NP1	65.50		Paleocene basal Nanno Zone NP1 is a "gap" from the top of the Cretaceous to the FAD of C. tenuis (base of NP2).  Zone NP1 also defined by beginning of acme of Thoracosphaera (calc. dinoflagellate) -- Ref.g.   Zone NP1 has regional subzones (see Ref.g).
	CC26	66.30
	CC25	69.23
	CC24	69.63	dashed
	CC23	75.40
	CC22	76.38
	CC21	77.38
	CC20	78.92
	CC19	80.64
	CC18	83.53
	CC17	83.99
	CC16	84.94
	CC15	85.85
	CC14	86.96
	CC13	89.63
	CC12	91.23		Dual-markers for base of CC12
	CC11	92.70
	CC10	95.56		Base of CC10 has dual-markers (M. decoratus; L. acutus)
	CC9	102.93
	CC8	112.02
	CC7	125.11
	CC6	129.19
	CC5	132.75
	CC4	137.27
	CC3	140.24
	CC2	144.82
	CC1	145.14

NN,NP,CC Subzone	block	30	210/217/221	notitle	off
	TOP	5.59
	d	5.94
	c	6.91
	b	7.42
	a	8.29
	TOP	42.42	dashed 
	c	43.55
	b	45.35
	a	46.57
	b	47.92
	a	49.43
	TOP	92.70
	b	94.43
	a	95.56		Dual-markers for base of CC12
	b	100.40
	a	102.93
	b	109.77
	a	112.02
	b	124.59
	a	125.11
	TOP	129.19
	b	130.99
	a	132.75
	b	135.47
	a	137.27
	b	139.68
	a	140.24

CN,CP,NC Zone	block	40	210/217/221	notitle	off	NEOGENE = mainly Lourens et al. (GTS2004 tables); PALEOGENE = Tables in Berggren et al. (1995a, b).  Late CRETACEOUS = mainly Erba et al (1995) as tabulated by ODP Leg 171B Init. Repts. (Table 2, p. 17-18).  Middle and Early CRETACEOUS = compiled by Jim Bergen, based on publications by Tim Bralower et al (1995),  J. Bergen (1994) and Eric Kanael
	TOP	0.00
	CN15	0.29
	CN14	1.04		Pleistocene Nanno Zone CN14a begins with FAD of Gephyrocapsa oceanica.  But this event is not tabulated by Berggren or Leg 145.  Figure 4 in Berggren et al. (1995) draws the base of CN14a at approximately 1.0 Ma, and Lourens et al (GTS2004) assign it at re-entrance of medium Gephyrocapsa
	CN13	1.93
	CN12	3.70
	CN11	4.50
	CN10	5.59
	CN9	8.29		Miocene Nannofossil Zone NN11 begins with either the FAD of D. berggreni (an earlier event) or of D. quinqueramus; the definition problem arises depending if these two taxa are considered to be the same species.  Bukry (1981) defined Zone CN8b beginning with FAD of D. neorectus and/or FAD of D. loeblichii, and ending with FAD of D. surculus; but these events are not calibrated in the scales of Berggren (in prep, SEPM) or Leg 145.  Aubry (in Berggren et al., 1995) indicates that FAD of D. berggrenii defines base of both NN11 and CN9; and this placement is shown in this chart.
	CN8	9.53
	CN7	10.55
	CN6	10.89
	CN5	13.53
	CN4	14.91
	CN3	17.95
	CN2	18.28		Berggren et al (1995) had shown FAD of S. belemnos as defining base of CN2.  But Lourens et al (2004) assign base-CN2 as equivalent to base NN3
	CN1	23.14
	CP19	30.04
	CP17/18*	31.44
	CP17/18	32.51		Diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  For simplicity, I have placed the associated Zone NP23; CP17 base with the mid-latitude level (32.3 Ma).
	{ CP18 }	33.27
	CP16	34.78
	CP15	36.95		Eocene Nanno zone CP15 is not divided into subzones in Fig. 18 of Aubry (in Berggren et al., 1995), but the FAD of I. recurvus (= base of NP19-20) is used in some schemes for defining a "CP15b" subzone. 
	CP14	42.66
	CP13	46.57
	CP12	49.43
	CP11	50.47		Eocene Nanno Zone CP11 base is FAD of Toweius? crassus; and this event is often used to approximate base of NP13 (see discussion in Perch-Nielsen, 1985).  Following Aubry (in Berggren et al., 1995), NP13 and CP11 bases are made coeval, but there is no direct CP11 calibration.
	CP10	53.23
	CP9	54.52
	CP8	56.97
	CP7	57.66
	CP6	58.32
	CP5	59.17
	CP4	60.48
	CP3	62.82
	CP2	64.28
	CP1	65.50
	NC23	68.73	dashed
	NC22	68.98
	NC21	69.85
	NC20	76.38
	NC19	78.92
	NC18	83.53
	NC17	84.94
	NC16	86.96
	NC15	89.63
	NC14	92.05
	NC12 -13	93.95		LAD of P. asper (R. asper) is used by Bralower et al (1995) to define base of NC13, and LAD of A. albianus for base of NC12, with 1 myr separaation.  But Leg 171B table places these as coeval.
	NC11	94.05
	NC10	102.93
	NC9	109.06
	NC8	112.02
	NC7	121.90
	NC6	125.11
	NC5	133.27
	NC4	133.53
	NC3	140.24
	NC2	144.82
	NC1	145.14

CN,CP,NC Subzone	block	30	210/217/221	notitle	off
	TOP	0.29
	b	0.44
	a	1.04		Pleistocene Nanno Zone CN14a begins with FAD of Gephyrocapsa oceanica.  But this event is not tabulated by Berggren or Leg 145.  Figure 4 in Berggren et al. (1995) draws the base of CN14a at approximately 1.0 Ma, and Lourens et al (GTS2004) assign it at re-entrance of medium Gephyrocapsa
	b	1.73		Pleistocene Nanno Zone CN13b begins with FAD of Gephyrocapsa caribbeanica; but this event is not tabulated by Berggren et al. or Leg 145.  Diagram in Berggren et al. implies that the age is about 1.7 Ma.
	a	1.93
	d	2.39
	c	2.49
	b	2.80
	a	3.70
	b	4.13
	a	4.50
	c	5.12		  
	b	5.35		Pliocene Nannofossil Zone CP10b begins with FAD of C. acutus AND/OR the LAD of genus Triquetrorhabdulus.
	a	5.59
	d	5.94		Miocene Nanno zone "NN11d" and "CN 9d" are taken from chart of Aubry (in Berggren et al., SEPM, 1995).  Similar chart in Berggren et al. (GSA, 1995) has slightly different ages, but does not specify the nannofossil definitions.
	c	6.91
	b	7.42
	a	8.29		Miocene Nannofossil Zone NN11 begins with either the FAD of D. berggreni (an earlier event) or of D. quinqueramus; the definition problem arises depending if these two taxa are considered to be the same species.  Bukry (1981) defined Zone CN8b beginning with FAD of D. neorectus and/or FAD of D. loeblichii, and ending with FAD of D. surculus; but these events are not calibrated in the scales of Berggren (in prep, SEPM) or Leg 145.  Aubry (in Berggren et al., 1995) indicates that FAD of D. berggrenii defines base of both NN11 and CN9; and this placement is shown in this chart.
	TOP	10.89
	b	11.90
	a	13.53
	TOP	18.28
	c	22.82
	a/b	23.14
	b	27.27
	a	30.04
	TOP	32.51	dashed	Diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  For simplicity, I have placed the associated Zone NP23; CP17 base with the mid-latitude level (32.3 Ma).
	c	33.05
	b	33.50		Zone CP16b begins approximately at Eocene/Oligocene boundary.
	a	34.78
	TOP	36.95		Eocene Nanno zone CP15 is not divided into subzones in Fig. 18 of Aubry (in Berggren et al., 1995), but the FAD of I. recurvus (= base of NP19-20) is used in some schemes for defining a "CP15b" subzone. 
	b	39.71
	a	42.66
	c	43.55
	b	45.35
	a	46.57		Eocene Nanno Zone NP15-16 is combined in some zonal schemes, because marker of NP16 (base = LAD 'Rhabdolithus gladius') is rare or often absent.  [See Perch-Nielsen, 1985, for details.]   However, Aubry (in Berggren et al., 1995), could distinquish 3 subzones in NP15 using markers similar for subzones of CP13 (with a total duration of 4 m.y.), and estimated that NP16 was a valid zone with duration of nearly 3 m.y.
	b	47.92
	a	49.43
	TOP	53.23
	b	54.09
	a	54.52
	b	56.24		Base of Paleocene Nanno Zone CP8b concides with FAD of Romboaster spp.  Within Zone NP9 several species of Rhomboaster evolve, and can be used for a fine subdivision (see Perch-Nielsen, 1985).
	a	56.97
	TOP	64.28
	b	64.91
	a	65.50
	TOP	94.05
	b	97.93
	a	102.93
	b	106.42
	a	109.06
	c	109.77
	b	111.69
	a	112.02
	b	119.17
	a	121.90
	b	123.76
	a	125.11
	e	126.12
	d	129.19
	c	130.99
	b	132.02
	a	133.27

Zone Marker (and Jur-Tri) Nanno Datums	event		222/218/215		off	NEOGENE = mainly Lourens et al. (GTS2004 tables); PALEOGENE = Tables in Berggren et al. (1995a, b).  Late CRETACEOUS = mainly Erba et al (1995) as tabulated by ODP Leg 171B Init. Repts. (Table 2, p. 17-18).  Middle and Early CRETACEOUS = compiled by Jim Bergen, based on publications by Tim Bralower et al (1995),  J. Bergen (1994) and Eric Kanael
LAD
	Pseudoemiliania lacunosa	0.44		LAD defines top of NN21, hence base of NN20.  Astronomically tuned in Pacific (ODP Legs 111 & 138) and Atlantic (Leg 154, Sites 925 & 926).  -- Refs 1-5, 9 & 10; in GTS2004 Neogene nannofossil appendix.  Age is recorded slightly older (0.47 myr) in Mediterranean (refs. 11, 17 & 18).  Berggren et al. (1995) have same assignment = O-18 stage 12; 0.46 Ma; [b,d] = C1n.4.
	Discoaster brouweri	1.93		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD of D. brouweri is recorded slightly earlier (1.95 Ma) in Mediterranean (refs. 11, 22-25), and significantly earlier (2.06 Ma) in Pacific ODP Legs 111 and 138 (refs. 4-7).  Berggren et al. (1995) assign in lowermost Olduvai; 1.95 Ma; [d,g] = base C2n.
	Discoaster pentaradiatus	2.39		LAD of D. pentaradiatus (quintatus) defines top of NN17, hence base of NN18.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded earlier (2.51 Ma) in Mediterranean (refs. 20, 22, 25 & 26).  Berggren et al. (1995) places near Matuyama/Gauss boundary; 2.46-2.56 Ma; [g,d] = C2r.3r.25.
	Discoaster surculus	2.49		LAD of D. surculus defines top of NN16, hence base of NN17.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (2.52 Ma and 2.54 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7) and eastern Mediterranean (refs. 20, 22, 25 & 26), respectively.  Berggren et al. (1995) place near Matuyama/Gauss boundary; 2.55-2.59 Ma; [g,d] = C2r.3r.1.
	Discoaster tamalis	2.80		Lourens et al (GTS2004 table) refers to this LAD as a "subtop".  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) and eastern Mediterranean -- Refs 10, 12, 20, 22, 25 & 26; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (2.87 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7).  Pliocene nannofossil 'Discoaster tarnalis' (LAD) occurs at 2.73 Ma in Mediterranean [ref. d] in Berggren et al.'s compilation, with main assignment near top of Gauss; 2.78 Ma; [g,d] = C2An.1n.6.
	Reticulofenestra pseudoumbilicus	3.70		This LAD defines top of NN15, hence base of NN16.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (3.79 Ma and 3.84 Ma) in Pacific (ODP Legs 111 and 138; refs 4-7) and eastern Mediterranean (refs. 22 & 25), respectively.  Berggren et al. (1995) -- Pliocene nannofossil Reticulofenestra pseudoumbilicus (LAD) occurs at 3.66-3.7 Ma in Mediterranean [ref. c] = uppermost part of Upper reversed interval of Gilbert (Med.); 3.75 Ma; [e] = C2Ar.7.
	Discoaster tricorniculatus	3.92		Same chron-age scaling as Berggren et al. (1995) -- mid-way between D. asymmetricus FAD & R. pseudoumbilicus LAD; [b,h] -- not given age in table of Lourens et al (GTS2004).
	Amaurolithus primus	4.50		Lourens et al (GTS2004) referred to this FAD as a "subbottom".  Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix.  Pliocene nannofossil Amaurolithus primus (LAD) occurs in Nunivak (4.55 Ma) in Mediterranean [ref. d], in Berggren et al.'s (1995) compilation (slightly older LAD than Lourens et al.) = near top of Sidufjall; 4.58 Ma; [a,d,c,i] = C3n.3n.8.
	Discoaster quinqueramus	5.59		Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix.  This LAD is reported at same time (5.58 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 10 & 13).  Berggren et al. (1995) -- mid-C3r in Gilbert; 5.3 Ma [l,k,y,aa]; or 4.98 Ma [b] = C3r.5.
	Nicklithus amplificus	5.94		Genus for amplificus was "Amaurolithus" in Berggren's (1995) table; and had been used as base of "Subzone NN11d".  Astronomically tuned in eastern Mediterranean -- Refs 27-29; in GTS2004 Neogene nannofossil appendix.  This LAD (and LCO) is reported at same time (5.98 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  The LCO is at 6.12 Ma and 6.14 Ma in Pacific (ODP Legs 11 & 138; refs. 5-8) and Mediterranean (refs. 27-29), respectively.  Berggren et al. (1995) assigned as base C3r; 5.9 Ma [l,k,y]; or C3A; 5.33 Ma [a] = base C3r.
	Discoaster hamatus	9.53		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  LAD occurs slightly earlier (9.69 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  Correlations, as indicated by Berggren et al. (1995) were inconsistent; with younger LADs being reported elsewhere in previous literature -- C4Ar.2r.5; 9.4 Ma [l,t,k,y]; or C4A; 8.67 Ma [b] or 9.37 Ma [h]; therefore C4Ar.2r.5 seems best estimate (nearly same as astronomical tuning).
	Sphenolithus heteromorphus	13.53		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 14 & 15; in GTS2004 Neogene nannofossil appendix;  but LAD is reported slightly earlier (13.654 Ma) in eastern Mediterranean (ref 37).  This offset, although only 100myr, causes a problem, because the "primary marker" for base-Serravallian GSSP suggested in Mediterranean region is that nannofossil S. heteromorphus LAD.  Berggren et al. (1995) had similar chron-age assignment of C5ABr; 13.6 Ma [l,r] or 13.5 Ma [d,h,i] = C5ABr.6.
	Helicosphaera ampliaperta	14.91		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had placed this LAD about 0.6 myr older,  as C5B; 15.6 Ma [l,r] or 15.8 Ma [a,h] = C5Br.5.
	Sphenolithus belemnos	17.95		Lourens et al (2004) assign this event as a LCO that is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  However, based on coincidence with earlier calibrations, this is probably essentially the LAD (which was the original definition of the zone).  There seems a 0.1 myr difference (J. Bergen, pers. commun., 2005).  Berggren et al. (1995) had summarized as C5E; 18.5 Ma [b,h] or18.27 Ma [i] = C5En.9.
	Triquetrorhabdulus carinatus	18.28		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Note that this event is ~1myr YOUNGER than earlier reports.  Very poorly constrained age -- 19.5 [b] or 23.0 [d]; 23.1 [h] or 19.2 [i].  Early Miocene Nanno 'T. carinatus' LAD is diachronous, and appears to range from 19.5 to 23.0 Ma.  Hodell & Woodruff (1994) have a similar conclusion, although their estimate for this event in Site 289 suggests that it may be reworked.  Earlier version of this database had used an intermediate estimate (19.2 Ma), which is similar to that used by Aubry (ca. 19 Ma) in her charts in Berggren et al. (1995) = C6n.9.
	Dictylcoccites bisectus	23.14		Leg 145 referred to this LAD as top of acme; but I have followed Leg 171 scheme.  High-latitude marker for base of NN1.  Basal Miocene Nanno ' Reticulofenestra bisecta' was called 'Discoaster bisectus' in Berggren (earlier draft), and is called 'Dictyococcites bisectus' in Perch-Nielsen (1985).  The LAD of 'R. bisectus' is used to approximate the NP25/NN1 boundary in high latitudes; and was "substituted for H. recta, the marker of the NP15/NN1 boundary in Martini's (1971) zonal scheme" by Aubry (in Berggren et al., 1995).  Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.2rr; 23.9 Ma; [a,b,j,cc] = C6Cn.2r.5.
	Sphenolithus distentus	27.27		Oligocene Nanno 'Sphenolithus distentus' LAD is correlated to C9n by Aubry (in Berggren et al., 1995) at 27.5 Ma, which is nearly 1 m.y. older than mid-C8n.2n correlation in Leg 145 table.  Used chron-age scaling as  revised by Leg 145 = C9n; 26.3 Ma; [j,x;a,f] = C8n.2n.5.
	Reticulofenestra umbilicus / R.hillae  (south high lat.)	31.44		diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  For simplicity, I have placed the associated Zone NP23; CP17 base with the mid-latitude level (32.3 Ma).  Same chron-age scaling as Berggren et al. (1995) = upper C12r; 31.3 Ma; [j,dd] = C12r.85.
	Reticulofenestra umbilicus / R.hillae  (low-mid lat.)	32.51		Diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  Same chron-age scaling as Berggren et al. (1995) = mid C12r; 32.3 Ma; [j,t] = C12r.35.
	Ericsonia formosa  (mid-low lat.)	33.05		Diachronous (LAD is 7 m.y. earlier in south high lat!) [j]  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C12r; 32.7 Ma; [a,d] = C12r.1.
	Discoaster saipanensis  (low & mid lat.)	34.78		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C13r; 34.2 Ma; [k,r] = C13r.4.
	Chiasmolithus grandis	36.95		Same chron-age scaling as Berggren et al. (1995) = C17n.1n; 37.1 Ma; [a,b,cc] = C17n.1n.4.  This LAD occurs approx. 2 m.y. earlier in Mediterranean [Ref.b].
	Chiasmolithus solitus	39.71		LAD reported higher (C18n) in Hole 748 (ref. m).  Same chron-age scaling as Berggren et al. (1995) = upper C18r; 40.4 Ma; [cc] = C18r.75.
	Blackites gladius	42.42		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = lower C20n; 43.4 Ma; [k,m,n,nn] = C20n.3.
	Chiasmolithus gigas	43.55		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = upper C20r; 44.6 Ma; [a,b,n,mm] = C20r.7.
	Tribrachiatus orthostylus	50.47		Eocene Nanno 'T. orthostylus' LAD (= base of Zone NP12) has a poorly defined age, and may be time-transgressive?  (see discussion in Berggren et al., 1985).  Same chron-age scaling as Berggren et al. (1995) = lower C22r; 50.6 Ma; [a,b,c,n] = C22r.2.
	Tribrachiatus contortus  (Morphotype B)	54.09		Eocene Nanno evolution from Tribrachiatus contortus to Tribrachiatus orthostylus was formerly described as an abundance shift, but Aubry has subdivided it into different morphotypes.  Same chron-age scaling as Berggren et al. (1995) = upper C24r; 53.61 Ma; [i,j] = C24r.9.
	Micula murus, other Cret. nannos	65.50		Chron-age calibration = upper C29r; K/T boundary; [b,g] = C29r.7.
	Reinhardtites levis	69.23		Bralower et al (1995) suggest using this LAD to subdivide NC21 into a/b subzones; but the GTS2004 ages would imply very short durations, so omitted here.  ODP age is 69.8 Ma, but EGI database (2005) calibrates as much higher at 68.4 Ma (North Sea) and 68.6 (Tethys).  This younger age would probably require the overlying succession to also be pushed "higher" to retain same sequence.  SEPM'98 had assigned LAD is top of B. clinolobatus (base of H. birkelundi) ammonite = Late/Early Maastr. boundary.
	Uniplanarius trifidum	69.85		Also known as Quadrum trifidum (and T. trifidus)  Calibrated via Sr 87/86 to US Western Interior ages.  Occurs ~0.75 myr above Tercis GSSP of base-Maastrichtian (used here).
	Tranolithus orionatus  (=T. phacelosus)	69.63	dashed	DASH:  Leg 207 uses this LAD for base-CC24, rather than T. phacelosus (same taxa?); but indicates that it is only 0.4 myr below base-CC25.  Relative-age to R. levis used here and as CC24 base.  SEPM'98 had assigned LAD at base of Maastrichtian.
	Eiffellithus eximius	75.40		EGI database calibrates as base of Upper Campanian (76.4 Ma in Tethyan; 76.3 Ma in Boreal) and Jackie Lees (Burnett) assigns as upper Upper Campanian (ca. 73 Ma).  Therefore, the ODP value of about 75.4 Ma seems suitable, and is used here.  SEPM'98 had assigned LAD is middle of D. stevensoni Z.
	Marthasterites furcatus	80.64		SEPM'98 had assigned LAD as base of Middle Camp (base B. obtusus)
	Rhagodiscus asper, Axopodorhabdus albianus, Corollithion kennedyi	93.95		Leg 171B has this cluster of LADs (C. kennedyi, R. asper, A. albianus) at ~0.4 myr below top of Cenomanian (ammonite zone?)
	Lithraphidites acutus	94.05		LAD assigned as ~0.5 myr below top of Cenomanian in Leg 207 scale (= marker for base of UC5 Zone)
	Microstaurus chiastius	94.43		LAD is 3/4ths up in D. problimaticum Z. (Leg 171B relative placement)
	Hayesites albiensis	100.40		40% up in R. appenninica Foram Zone.  SEPM'98 assigned as Middle of M. perinflatum subzone.
	Micrantholithus hoschulzii	119.17		90% of G. ferrolensis Foram Zone (Bergen & Sikora), which is 90% between LAD of L. cabri and FAD of G. algeriana; which is about 2 myr higher than what would be implied by Leg 207 table relative placement.  Not on SEPM chart.  NOTE: LAD is just below (0.2 myr) the top of N. nolani Z., D. nodosocostatum s.z. (based on Leg 171 projected 114.2 Ma relative to 114.0 for FAD H. albiensis).   But, LAD on Leg 207 table was assigned as 3/4th up in D. furcata zone (based on projected placement of 117.3 Ma in Leg 207 table)
	Conusphaera rothii	123.76		20% up in D. weissi (J. Bergen assignment).  SEPM'98 has assigned as Probably equivalent to C. mexicana of some nannofossil wokers (J. Bergen, pers. commu., 2005).  Not on SEPM chart; but Leg 207 table implies an age about 0.5 myr older than FAD of E. floralis.
	Calcicalathina oblongata	129.19		35% up in Chron M3r (merger of Bralower's and Bergen's placements).  SEPM'98 had assigned as Base of Chron M3r; but LAD was middle of H. caillaudianus Z. in France.
	Lithraphidites bollii	130.99		Middle of Chron M5r [Bralower].  SEPM'98 had assigned LAD as 6/10 up in P. angulicostata auct. Z.
	Speetonia colligata	132.75		70% up in P. ligatus Zone.  SEPM'98 had also assigned LAD as 7/10 up in P. ligatus Z.
	Crucielipsis cuvillieri 	133.27		90% up in S. sayni Zone.  SEPM'98 had assigned as Middle of S.sayni Z.
	Tubodiscus verenae	133.53	dashed	DASH approximation in mid-Hauterivian (arbitrarily put at middle of S. sayni Zone here to avoid overlap with NC5).  Defines base of NC4, but difficult to pinpoint LAD.  SEPM'98 had assigned as Middle of H. trinodosum s.z. (of N. pachydicranus Zone).  With revised zonal scheme, this essentially is base of C. furcillata subzone.
	Polycostella beckmanni	145.51		50% up in Chron M19n.2n.  On SEPM1998 chart, LAD is 55% up in Durangites Z.
	Stephanolithion bigotii bigotii	148.99		LAD is 95% up in Chron M22n.  On SEPM1998 chart, LAD is 80% up in Semiformiceras semiforme Z.
	Triscitum beaminsterense	153.23		Middle of C. divisum Zone. 
	Crepidolithus perforata	154.14		LAD is base of A. hypselocyclum Zone.  Formerly "M. perforata".  On SEPM1998 chart, LAD is 70% up in S. platynota Z.
	Lotharingius crucicentralis	158.79		LAD is 70% up in P. plicatilis Zone.  On SEPM1998 chart, LAD is base of P. (D.) antecedens subzone of P. plicatilis Zone.
	Stephanolithion bigoti maximum	159.61		LAD is base of P. pllicatilis Zone.  On SEPM1998 chart, LAD is 20% up in C. praecordatum s.z. of Q. mariae Zone
	Ansulasphaera helvetica	161.69		LAD is 40% up in L. lamberti.  On SEPM1998 chart, LAD is 25% up in Q. (L.) lamberti zone.
	Stephanolithion hexum	162.28		DASH -- LAD is 20% up in P. athleta Zone.  On SEPM1998 chart, LAD is base of R. anceps Zone.
	Lotharingius velatus	163.92		LAD at 30% up in M. gracilis Zone.  DTS1995 had this FAD is 20% up in M. (D.) gracilis zone, but not in SEPM chart.
	Stephanolithion speciosum	164.23		LAD at base of M. gracilis Zone.  On SEPM1998 chart, LAD is 55% up in B. (K.) bullatus Zone.
	Carinolithus magharensis	167.97		DASH at middle of P. parkinsoni (according to Erba).  But, SE France has reported LAD in middle of S. subfurcatum (middle of S. niortense zone).  On SEPM1998 chart, LAD is 45% up in P. densicostata s.z.  of P. parkinsoni Z., 
	Discorhabdus striatus (acme)	169.05		Top of Acme is 75% up in S. subfurcatum (S. niortense) Zone.  Also known as Biscutum striatum.  DTS1995 had the LAD at 35% up in schroederi s.z. of S. niortense zone; but not on the SEPM chart.
	Carinolithus superbus	169.25		Middle of S. subfurcatum (S. niortense) Zone.  J. Bergen's sections suggest a lower LAD at 25% up in this zone.  DTS1995 had this LAD at 50% up in G. baculata s.z. of S. niortense zone; but not in the SEPM chart.
	Biscutum constans	170.23		Base of S. humphriesianum zone.  Also called D. constans.  On SEPM1998 chart, LAD is base of hebridica s.z. of S. propinquans zone.
	Triscutum sullivani	170.42		LAD in middle of Sauzei Zone (now middle of S. propinguans Zone).  DTS1995 had this LAD at 30% up in hebridica s.z. of S. propinquans zone, but not the SEPM chart.
	Triscutum tiziense	171.21		Base of W. laeviuscula Zone.  On SEPM1998 chart, LAD is 70% up in H.(H.) discites s.z. of the H. discites zone.
	Bussonius prinsii	172.49		LAD is Base of G. concavum Zone.  On SEPM1998 chart, LAD is the base of G. formosus s.z. of the G. concavum zone.
	Axopodorhabdus atavus	175.16		J. Bergen will revisit the calibration.  On SEPM1998 chart, LAD is 50% up in L. opalinum s.z. of L. opalinum zone .
	Crepidolithus cavus	176.03		J. Bergen will revisit the calibration.  DTS1995 had this LAD is 15% up in fluitans s.z. of P. aalensis zone,  but not in the SEPM chart.
	C. cantaluppii	177.27	dashed	DASH at 30% up in "Menegini Zone" (= D. pseudoradiosa Zone).  On SEPM1998 chart, LAD is 80% up in levesquei s.z. of D. pseudoradiosa zone.
	Lotharingius hauffii (acme)	180.50		Base G. thouarsense Zone.  On SEPM1998 chart, LAD is the base of G. thouarsense zone.
	Orthogonoides hamiltoniae	181.28		95% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is the base of sublevisoni s.z. of H. Bifrons zone.
	Palaeopontosphaera grande	181.50		80% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Similiscutum finchii	181.80		60% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 70% up in H. falciferum s.z. of H. falciferum zone.
	Calcivascularis jansae	182.63		5% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Crucirhabdus primulus	182.88		40% up in D. tenuicostatum Zone.  DTS1995 had this LAD at base of D. tenuicostatum s.z. of D. (O.) tenuicostatum zone, but not the SEPM chart.
	Parhabdolithus liasicus liasicus	185.44		55% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  DTS1995 had this LAD at 50% up in cornacaldense s.z. of lavinianum, but not in the SEPM chart.
	Crepidolithus pliensbachensis	188.14		40% up in T. ibex.  On SEPM1998 chart, LAD is 40% up in beirense s.z. of T. ibex.
	Prinsiosphaera triassica, Eoconusphaera ziambachensis, Crucirhabdus minutus, Archaeozygodiscus koessenensis 	199.60
	Orthopithonella misurinae,  Obliquipithonella prasina, Carnicalyxia tabellata, Cassianospica curvata	216.53
FAD
	Emiliania huxleyi	0.29		Astronomically tuned in Pacific (ODP Legs 111 & 138) and Atlantic (Leg 154, Sites 925 & 926) -- Refs 1, 2, 9 & 10; in GTS2004 Neogene nannofossil appendix.  Age is recorded slightly younger (0.27 myr) in Mediterranean (refs. 17 & 18).  Berggren et al. (1995) placed similarly= O-18 stage 8; 0.26 Ma; [b,d] = C1n.67.
	medium (over 4 microns) Gephyrocapsa spp. reentrance (reemG event)	1.04		Astronomically tuned in Pacific (ODP Legs 111 & 138) -- Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  FAD recorded slightly later (1.01 Ma) at Atlantic Leg 154, Sites 925 & 926, and later (0.96 Ma) in Mediterranean (refs. 11, 17-19 & 21).  Berggren et al. (1995) have same = O-18 stage 29 (within Jaramillo); 1.03 Ma; [a] = C1r.1n.5.
	medium (over 4 microns) Gephyrocapsa spp. (=bmG event)	1.73		Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.  This FAD is recorded slightly later (1.67 and 1.69 Ma) in Pacific ODP Legs 111 & 138 (Refs 1-5) and in Atlantic Leg 154, Sites 925 & 926 (Refs 9-11), respectively.  Pleistocene Nanno FAD of this Gephyrocapsa species was called "medium-o" by Berggren (early version of 1995 GSA paper) and "oceanica s.l." by Leg 145 -- both lists give "Rio et al, in press" as source, and have same age.  Berggren et al. (1995) assign as transition O-18 stages59/60 [e] (above top of Olduvai); 1.67-1.70 Ma; [a] = C1r.3r.15.
	Discoaster asymmetricus (FCO)	4.13		Lourens et al (GTS2004) referred to this FCO as a "subbottom".  Astronomically tuned in Pacific (ODP Legs 111 and 138) and in eastern Mediterranean (as 4.12 Ma) -- Refs 5-7, 22 & 25; in GTS2004 Neogene nannofossil appendix.  Pliocene nannofossil 'Discoaster asymmetricus' (FCO) occurs in upper Gilbert (4.15 Ma) in Mediterranean [ref. d], in Berggren et al.'s (1995) compilation =  near top of Cochiti; 4.2 Ma; [d] = C2n.1n.8.
	Ceratolithus rugosus	5.12		Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix. This FAD is reported later (5.05 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  in Berggren et al.'s (1995) compilation => diachronous among regions -- Pliocene nannofossil Cerotolithus rugosus (FAD) occurs near top of Nunivak (4.5 Ma) in Mediterranean [ref. c,d].  Berggren et al. (1995) place within Thvera; 5.0-5.23 Ma; [c,i] = C3n.4n.5.
	Ceratolithus acutus	5.35		Base C. acutus is a marker for base of Pliocene; not tabulated in Berggren et al. (1995).   Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  This FAD is calibrated at essentially same age (5.32 Ma) in Pacific (ODP Legs 111 & 138; refs. 5-8).  Berggren et al. (1995) assigned to uppermost part of C3r in Gilbert; 5.34 Ma [j,k] or 5.68 Ma [i] = C3r.85.
	Nicklithus amplificus	6.91		Genus for amplificus was "Amaurolithus" in Berggren's table; and had been used for a Subzone NN11c (and "CN9c") of their zonal scheme.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.  This FAD occurs later (6.68 Ma) in eastern Mediterranean (refs. 27-29).  Berggren et al. (1995) placed this FAD slightly higher (by 0.3 myr) -- base C3An.2n; 6.6 Ma [l,k,y]; or 6.02 [a] or 6.48 Ma [h] = base C3An.
	Amaurolithus primus	7.42		LAD of Amaurolithus primus is also LAD of genus Amaurolithus.  Astronomically tuned in eastern Mediterranean -- Refs 28 & 30-35; in GTS2004 Neogene nannofossil appendix.    This FAD is recorded slightly later (7.36 Ma) in Atlantic (Leg 154, Sites 925 & 926; refs 10 & 13).  Berggren et al. (1995) summarized: C3Br.2r; 7.2 Ma [l,k.y]; or 6.70 [a], 6.42 [f] or 6.80 Ma [h] = C3Br.2r.7.
	Discoaster quinqueramus	8.11		From Leg 145 compilation; not in Aubry's synthesis in Berggren et al. (1995) = C4; 7.46 Ma [b] or 8.12 Ma [h] = base C4n.2n (for older FAD estimate).
	Discoaster berggrenii	8.29		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had this FAD as slightly older by 0.3 myr = lower C4r; 8.6 Ma [l,k,y]; or C4; 8.00 [a], 7.5 Ma [g], or 8.16 [h] = C4r.2r.2.
	Discoaster hamatus	10.55		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs much younger (10.18 Ma) in eastern Mediterranean (refs. 35 & 36).  Berggren et al. (1995) note that this is "Controversial" and inconsistent datum, with reported ages of C5r.2r; 11.2 [l,u]; or C5;10.5 [b] or 10.9 [h]; therefore C5r.2r.7 (11.2 myr) was used as lowest FAD in a previous version of this chart.  More checks on this calibration is needed.
	Catinaster coalitus	10.89		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs slightly later (10.73 Ma) in eastern Mediterranean (refs. 35 & 36).  Very poorly constrained age, and Atlantic may be 0.4 m.y. before Pacific -- Berggren et al. (1995) give C5r.2r (Atl.); 11.3 Ma [l,h,t] or 11.1 Ma [b]; therefore an older placement (by 0.4 myr) of C5r.2r.5 was used on previous versions of this chart.
	Discoaster kugleri	11.90		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 14 & 15; in GTS2004 Neogene nannofossil appendix;  and simultaneous (11.90 Ma) in eastern Mediterranean (refs 35 & 36).  This "FCO" of Lourens et al (2004) seems to correspond in calibration to the "FAD" of Berggren et al (1995), which they summarized as C5r.3r; 11.8 Ma [l,r]; or C5A; 12.2 [b],12.7 [d],12.8 [h] or 12.0 Ma [i] = C5r.3r.3.
	Discoaster druggi	22.82		Astronomically tuned in eastern Mediterranean (based on projecting astronomical tuning of long-period minima  to base-Miocene; Ref. 40; in GTS2004 Neogene nannofossil appendix), which is consistent with Leg 154.  However, smaller forms appear earlier, at end of Oligocene? (J. Bergen and E. de Kaenel, pers. commun., 2005).  Miocene Nanno 'Discoaster druggi' FAD has been assigned to C6Cn in Leg 145 compilation [ref. b,h], but Aubry (in Berggren et al., 1995) assigns 0.5 m.y. higher (in C6Br); so earlier chart had used C6Br; 23.2 Ma; [l,o] = C6Br.5.
	Sphenolithus ciperoensis	30.04		Oligocene Nanno 'Sphenolithus ciperoensis FAD' is assigned by Aubry (in Berggren et al., 1995) to Subchron C11n.2n, implying an age of 29.9 Ma.  This is about 1.3 m.y. older than estimate in Leg 145 table.  Used same chron-age scaling as Berggren et al. (1995) -- C11n.2n; 29.9 Ma; [j;a,b] = C11n.2n.5.
	Sphenolithus distentus	33.27		Diachronous -- Oligocene Nanno 'Sphenolithus distentus FAD' is "a very inconsistent datum which may occur as low as Nanno Zone NP21 ... or as high as in Zone NP23" (Aubry, in Berggren et al., 1995).  Age estimates in her table range from 31.5 to 33.1 Ma; and the oldest age (33.1 Ma) is used here.  This is approx. 1 m.y. older than the Leg 145 table.  Oldest FAD implies "CP18" begins before "CP17"!  Youngest FAD is ~31.5 Ma  Scaling used here is C12r; 33.1 Ma; [j,y,ee;a,b] = base C12r.
	Clausicoccus subdistichus (base of acme)	33.50		Oligocene Nanno 'Clausicoccus subdistichus' (Aubry, in Berggren et al., 1995) has alternate names of 'Ericsonia subdisticha' (Leg 145 table) and 'Ericsonia obrata' (Massignano section, Premoli Silva et al., 1988).  Same chron-age scaling as Berggren et al. (1995) = lower C13nr; 33.3 Ma; [z] = C13n.5.
	Isthmolithus recurvus	35.17		Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.2n; 36.0 Ma; [k,ll,oo] = C15r.65.
	Chiasmolithus oamaruensis	36.84		Same chron-age scaling as Berggren et al. (1995) = C17n.1n; 37 Ma; [a,b,cc] = C17n.1n.55.
	Reticulofenestra umbilicus	42.66		Same chron-age scaling as Berggren et al. (1995) = basal C20n; 43.7 Ma; [k,d,u,w] = C20n.1.
	Chiasmolithus gigas	45.35		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = base C20r; 46.1 Ma; [a,b,n,mm] = base C20r.
	Nannotetrina fulgens	46.57		Same chron-age scaling as Berggren et al. (1995) = mid C21n; 47.3 Ma; [a,b,c,u] = C21n.35.
	Blackites inflatus	47.92	dashed	Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = upper C21r; 48.5 Ma; [b,u] = C21r.5.
	Discoaster sublodoensis	49.43		Same chron-age scaling as Berggren et al. (1995) = lower C22n; 49.7 Ma; [a,b,c,u] = base C22n.
	Discoaster lodoensis	53.23		Same chron-age scaling as Berggren et al. (1995) = C24n.2r; 52.85 Ma; [a,b,c,n] = C24n.2r.5.
	Discoaster diastypus	54.52		"No firm magnetochronologic calibration" (ref.k).  Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.9 Ma; [a,c] = C24r.75.
	Tribrachiatus bramlettei	55.67		Paleocene Nannofossil Zone NP10 base (FAD of T. bramlettei) is a marker for the Paleocene/Eocene boundary.  Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55 Ma; [h,i] = C24r.35
	Cruciplacolithus eodelus	56.24		Also known as Campylosphaera eodela.  FAD of C.eodelus closely precedes C-13 excursion in many DSDP sites.  Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.5 Ma; [a,b,n] = C24r.15.   NOTE: Paleocene Nanno 'C. eodela' FAD listed by Leg 145 as "58.2 Ma" in Berggren et al. (1985), then converted; but I could not find this event given in Berggren et al. (1985) tables.
	Discoaster multiradiatus	56.97		Same chron-age scaling as Berggren et al. (1995) = mid C25n; 56.2 Ma; [a,c,p] = C25n.4.
	Discoaster nobilis	57.66		Same chron-age scaling as Berggren et al. (1995) = upper mid-C25r; 56.9 Ma; [a,c,j] = C25r.6.
	Heliolithus riedelii	58.14		Paleocene Nanno 'H. riedeli' FAD age estimated from it's placement 0.6 m.y. before FAD of D. nobilis in Berggren et al. (1985)  table.  Chron-age scaling = lower C25r; 57.3 Ma; [j] = C25r.2
	Discoaster mohleri	58.32		Same chron-age scaling as Berggren et al. (1995) = basal C25r; 57.5 Ma; [a,j] = C25r.05.
	Heliolithus kleinpelli	59.17		Paleocene Nanno 'H. kleinpelli' FAD placed "slightly above mid-point of C26r", or 0.6 m.y. older than LAD 'D. danicus', by Berggren et al. (1985), but Leg 145 table has these as coeval events (citing Backman, 1986).  Same chron-age scaling as Berggren et al. (1995) = uppermost C26r;58.4 Ma;[a,c,j] = C26r.85.
	Fasciculithus tympaniformis	60.48		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [j] = C26r.4.  Coeval with FAD Neochiastozygus perfectus (North Sea) -- Ref.g.
	Ellipsolithus macellus	62.82		Paleocene Nanno 'E. macellus' FAD assigned to lower C27r by Berggren et al. (1985; 1995); but Leg 145 places higher (basal C26r) by about 1.6 m.y., citing Backman (1986).  Berggren et al. indicate that this is a solution susceptible taxon; so a lower FAD may be more appropriate?  I used Berggren's (Aubrey's) placement = lower C25r; 62.2 Ma; [j] = C27r.25.  Defines NP4 base.
	Chiasmolithus danicus	64.28		Same chron-age scaling as Berggren et al. (1995) = mid C28r; 63.8 Ma; [a,b,j] = C28r.5.
	Cruciplacolithus tenuis	64.91		Defines NP2 base.  Same chron-age scaling as Berggren et al. (1995) = lower C29n; 64.5 Ma; [a,b,j] = C29n.3.
	Biantholithus sparsus	65.50		Same chron-age scaling as Berggren et al. (1995) = upper C29r; 65.0 Ma; [j] = C29r.7.
	Nephrolithus frequens (low-lat.)	66.30		Leg 207 assigned as 0.8 myr before end-Cretaceous (used here) => closer to Boreal placement on SEPM98.  Boreal FAD is significantly (~1 myr) younger, as suggested on SEPM98 chart.  Low-lat shown on SEPM98 as mid-Chron C31n; but Leg 171B places ~1 myr younger.
	Micula murus	68.73	dashed	DASH:  Leg 207 assigned as 1.2 myr before end-Cretaceous (arbitrary equal-spacing of FADs of M. murus, N. frequens, and M. prinsii); ;but SEPM98 placement used in GTS04 and here (base Chron C31n).  DASHED -- Diachronous (p.16, ODP Leg 171B Expl. Notes). 
	Lithraphidites quadratus	68.98		SEPM98 shows as 0.1 myr after M. murus (used here).  However, GTS04 diagram (Fig.19.1) places Before (mid-way between M. murus and LAD of R. levis) -- used here for "GTS04".
	Uniplanarius trifidum	76.38		Also known as Quadrum trifidum.  Bralower et al. (1995) suggest this is coeval with FAD of foraminifer G. calcarata (about 0.8 myr younger), which may indicate uncertainty in Campanian inter-correlations.  SEPM'98 had assigned FAD as base of Late Campanian (base D. nebrascense zone).
	Uniplanarius sissinghii	77.38		Also known as Quadrum sissinghii.  Seems an arbitrary 1 myr below FAD of U. trifidum in Leg 171/207 tables.
	Ceratolithoides aculeus	78.92		FAD (from ODP 171/207) coincides with mid-B. perplexus (late) zone.
	Aspidolithus parcus parcus	83.53		FAD placed at base of Campanian.  Also called "Broinsonia parca parca" in some schemes.  BUT, base of preceeding A. parcus expansus is probably the one just above the boundary, and parca-parca occurs higher (J. Bergen 2005 pers. Commun.)
	Calculites obscurus	83.99		Leg 207 places at essentially Late/Middle Santonian boundary (base of D. bassleri zone)
	Lucianorhabdus cayeuxii	84.94		Estimates (SEPM, Leg 171/207) seem to converge on placement at Middle/Early Santonian boundary (base of C. vermiformis zone)
	Reinhardtites anthophorus	85.85		Leg 171B assigns to base of Santonian
	Micula decussata	86.96		Same as "Micula staurophora".  FAD is Late/Middle Coniacian boundary in Leg 171 and Tethyan SEPM column; BUT placed at Middle/Early Coniacian in Boreal SEPM column.  
	Marthasterites furcatus	89.63		SEPM'98 had assigned FAD as base of S. nigricollensis
	Eiffellithus eximius, Lucianorhabdus maleformis	91.23		SEPM'98 had assigned FADs as middle of P. percarinatus Z.
	Kamptnerius magnificus	92.05	dashed	DASH:  Not in Leg 207 table or SEPM chart; but highlighted by Bralower-Leckie as base of NC14 with assigned age of 91.8 Ma (using Gradstein et al., 1994 scale), which projects as 5% up in C. woollgari Zone.  However, FAD ranges as low as lower-Lower Turonian and as high as lower-Middle Turonian (Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI]
	Quadrum gartneri	92.70	dashed	DASH:  Base of M. nodosoides Zone [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI].  This is higher than the base of Turonian (Leg 171/207 placements) by 0.8 myr.
	Lithraphidites acutus, Microrhabdulus decoratus	95.56		SEPM'98 has assigned both as Middle of A. granerosense zone (used here); but Leg 207 projects age as base of Middle Cenomanian (~1 myr below)
	Corollithion kennedyi	97.93		SEPM'98 assigned FAD as middle of N. americanus Z.
	Eiffellithus turriseiffelii	102.93		Coeval with FAD of foraminifer R. ticinensis (Bralower-Leckie, 1997).  SEPM'98 assigned as Just below (0.15 myr) the base of H. orbignyi subzone.
	Eiffellithus monechiae	106.42		Coeval with FAD of foraminifer B. breggiensis by Bralower-Leckie (but see note on calibration of that datum).  Called E. cf. E. eximius in Bralower-Leckie chart.  Age assigned as 105 Ma in Leg 207 table (note on SEPM chart) => assigned as mid-A. intermedius ammonite subzone
	Axopodorhabdus albianus	109.06		Base of nannofossil A. albianus (called "P." albianus in Grippo et al., in press) is 23.3 long-eccentricity cycles below top of Albian (9.5 myr) => 109.1 Ma.  This projects to base of P. steinmanni ammonite subzone, rather than to 7/10 up in D. mammillatum Z., P. steinmanni s.z. of SEPM98 column.
	Tranolithus orionatus  (=T. phacelosus)	109.77		Nomenclature is "phacelosus" in older literature, but others seem to be using "orionatus" now (e.g., Bralower, Burnett).  Bralower-Leckie charts places this FAD in middle of T. primula Foram Zone, but this would be inconsistent with cycle-scaling of overlying FAD of A. albianus (base of next higher NC zone), therefore placed at 25% up in this table.  SEPM'98 had assigned Tranolithus "phacelosus" FAD as 7/10 up in D. mammillatum Z., P. steinmanni s.z., or at same level as FAD of Axopodo. albianus.
	Hayesites albiensis	111.69		Middle of H. planispira Foram Zone (LAD of T. bejaouensis to FAD of T. primula) on Bralower-Leckie (GSA Bull., 1997) chart.  SEPM'98 had assigned FAD as top of N. nolani Z., D. nodosocostatum s.z.
	Prediscosphaera columnata	112.02		Base of nannofossil P. columnata is 30.6 long-eccentricity cycles below top of Albian (12.4 myr) => 112.0 Ma = working definition for base of Albian.  (Primary control on Aptian-Albian interval!)    SEPM'98 has assigned as FAD is 2/10 up in L. tardefurcata Z., L. schrammeni s.z.
	Eprolithus floralis 	121.90		Base E. floralis (base NC7A) fixed at 121.9 Ma  (was 119.0 Ma in Leckie's chart), which sets base of D. furcata Zone.  Time-control point for scaling E. Aptian.  SEPM'98 had FAD projected to 8/10 up in D. forbesi Zone (= D. weisi)  on SEPM chart; but now projects much higher (base of D. furcata Zone)
	Rhagodiscus gallagheri	124.59		40% up in D. tuarkyricus (D. oglanlensis) Zone.   [NOTE: New scaling for E. Aptian makes the interval between FADs of R. angustus and E. floralis as 2 myr, instead of only 1 myr.]  
	Hayesites irregularis 	125.11		Also called Rucinolithus irregularis.   95% up in Chron M1n.   SEPM'98 had assigned as just below (0.1 myr) the base of Aptian.
	Flabellites oblongus (consistent)	126.12		50% up in Chron M1n (Bralower, 1993).  SEPM'98 had assigned FAD is 1/10 up in A. vandenheckii Z.
	Rucinolithus terebrodentarius, Rucinolithus windleyae	132.02		Middle of Chron M7r (J. Bergen), which is slightly lower (0.4 myr) than placement on SEPM chart.  The two taxa are combined by some specialists.  Bralower subdivides NC5 with this datum.  SEPM'98 had assigned as Base of Chron M6r when correlated with Italian magnetostratigraphy or just below the top of B. balearis Z. when correlated with French ammonites (which are similar placements, when using the GTS2004 time scale).
	Lithraphidites bollii	135.47		25% up in C. loryi Zone.  Bralower uses this to subdivide NC4, but it seems that base of NC4 (LAD of T. verenae) is ABOVE this L. bollii FAD.  SEPM'98 had assigned LAD as 2/10 up in C. loryi Z.
	Eiffellithus striatus	137.27		Middle of H. trinodosum s.z. (of N. pachydicranus Zone).  With revised zonal scheme, this essentially is base of C. furcillata subzone.
	Eiffellithus windii	139.68		10% up in B. campylotoxus Zone.  SEPM'98 had assigned FAD as 8/10 up in T. pertransiens Zone.  Note:  "SEPM98" age is different than actual SEPM chart, due to change in extent of T. pertransiens.
	Calcicalathina oblongata	140.24		20% up in Chron M14r.  SEPM'98 had assigned FAD as 7/10 up in T. otopeta Zone, which would shift to Berriasian, due to working-group change in boundary.
	Retecapsa augustiforata	144.82		Base of P. grandis subzone (J. Bergen's calibration).    SEPM'98 had assigned FAD as 8/10 up in T. occitanica Z., D. dalmasi s.z.  Alternate name was C. angustiforatus.
	Nannoconus kamtneri, Nannoconus steinmannii	145.14		30% up in Chron M17r (Bralower), which would be AFTER base of CC1; but Bergen correlated to about 50% up in B. jacobi s.z. (used here).  However, Bergen's version might be N. steinmanii minor of Bralower.  SEPM'98 had assigned FAD as middle of B. jacobi Z., P. grandis s.z.
	Rhagodiscus asper	145.68		30% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 54% up in Durangites Z.  
	Nannoconus globulus	145.80		10% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 51% up in Durangites Z.
	Lithraphidites carniolensis	145.95		Base of Chron M19n.  DTS1995 had this FAD is 30% up in Durangites Z., but not on the SEPM chart.  Ask J. Bergen to check.
	Umbria granulosa minor	146.66		FAD is middle of Chron M20n.  On SEPM1998 chart, FAD is 40% up in P. transitorius Z.one.
	Hexalithus noelae, Helenea chiastia	147.47		FAD are 50% up in Chron M20r.  On SEPM1998 chart, FADs are 40% up in M. ponti/B.peroni Z.
	Nannoconus compressus, Polycostella beckmannii	148.47		FAD are 10% up in Chron M21n.  On SEPM1998 chart, FADs are 45% up in S. admirandum/S. biruncinatum Zone.
	Conusphaera mexicana mexicana	149.31		FAD is 70% up in Chron M22n.  On SEPM1998 chart, FAD is 20% up in Semiformiceras semiforme Z.
	Conusphaera mexicana minor	149.95		FAD is 20% up in Chron M22n
	Zeugrhabdotus embergeri	150.47		mid-Chron M22r (based on Bralower).  DTS1995 had this FAD at 50% up in H. beckeri Z. , but not on SEPM chart.
	Faviconus multicolumnatus	155.50		FAD is 90% up in E. bimammatum Zone.  On SEPM1998 chart, FAD is base of T. hauffianum s.z. (upper E. bimammatum Z.one).
	Helenea quadrata	157.10		FAD is middle of B. bifurcatus Zone.  Former name was "M. quadratus".  On SEPM1998 chart, FAD is 25% up in P.(D.) stenocycloides s.z. (lower P. bifurcatus Zone).
	Stephanolithion bigotii maximum	161.61		FAD is 50% up in L. lamberti.  On SEPM1998 chart, FAD is 60% up in Q. (L.) lamberti zone.
	Stephanolithion bigotii bigotii	163.92		FAD at 30% up in M. gracilis Zone.  On SEPM1998 chart, FAD is the base of the M. (D.) gracilis zone.
	Crepidolithus perforata	164.02		FAD at 20% up in M. gracilis Zone
	Triscutum expansus	164.35		FAD at 75% up in B. bullatus Zone.  DTS1995 had this FAD is 60% up in herveyi Z., terebratus s.z.; but not in SEPM.
	Stephanolithion hexum	165.57		FAD is 25% up in O. aspidooides (which is equivalent to 25% up in H. retrocostatum zone).  On SEPM1998 chart, FAD is base of blanazense subzone of H. retrocostatum Zone.
	Axopodorhabdus rahla	165.72		Base of H. retrocostatum Zone (FAD in Tethyan realm),  DTS1995 had this FAD at 5/10 up in fortecostatum s.z. of C. bremeri Z., ;  but not in SEPM.
	Stephanolithion speciosum octum	168.24		FAD is 5% up in P. parkinsoni (upper Bajocian, rather than lower Bathonian as on SEPM chart).  On SEPM1998 chart, FAD is 20% up in recinctus s.z. of P. aurigerus Zone.
	Ansulasphaera helvetica	168.86		Base of G. garantiana Zone (which is much older than its FAD in Boreal realm as reported by Bown).  DTS1995 had this FAD at base of G. (G.) garantiana zone; but not on the SEPM chart.
	Stephanolithion speciosum speciosum	169.93		Middle of S. humphriesianum zone.  DTS1995 had this FAD at 50% up in S. humpriesianum s.z. of S. humpriesianum zone,  but not in the SEPM chart.
	Ellipsagelosphaera britannica (consistent)	171.40		Base of consistent E. britannica is middle of H. discites Zone.  On SEPM1998 chart, FAD is 30% up in the G. formosus s.z. of the G. concavum zone.
	P. grassei	171.60		On SEPM1998 chart, FAD is the base of H. (H.) discites Zone.
	Ellipsagelosphaera britannica (rare)	171.78		Base of Rare for E. britannica is 80% up in G. concavum Zone.  On SEPM1998 chart, FAD is 30% up in the G. formosus s.z. of the G. concavum zone.
	C. margarelii	173.11	dashed	DASH - 30% up in B. bradfordensis Zone (Aalenian, instead of in Toarcian on SEPM chart).  De Kaenel and Erba put this FAD much higher -- up to base of Bajocian!  On SEPM1998 chart, FAD is 20% up in walkeri s.z. H. (H.) discites zone
	Pseudoconus enigma	173.38	dashed	DASH -- Estimated as base of B. bradfordensis Zone.  DTS1995 had this FAD at the base of B. bradfordensis zone; but not in the SEPM chart.
	Triscutum sullivani	174.18		FAD is 40% up in L. murchinsonae Zone.  On SEPM1998 chart, FAD is 90% up in L. haugi s.z. of L. murchinsonae zone.
	Carinolithus magharensis	174.80		FAD is 90% up in L. opalinum Zone.  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Triscutum tiziense	175.16		middle of L. opalinum Zone.  (J. Bergen will revisit the calibration).  On SEPM1998 chart, FAD is 25% up in bifidatum s.z. of L. opalinum zone.
	Lotharingius contractus	175.38		FAD is 25% up in L. opalinum Zone.  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Retecapsa incompta	177.17		70% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Watznaueria fossacincta	177.56		50% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is the base of  levesquei s.z. of D. pseudoradiosa zone.
	Axopodorhabdus depravatus	178.15		20% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is 40% up in grumer s.z. of P. dispansum zone.  
	Biscutum intermedium	178.54		Base "D. levesquei" (= base P. dispansum Zone).  On SEPM1998 chart, FAD is the base of P. dispansum zone.
	Discorhabdus criotus	181.28		95% up in H. serpentinum Zone.  On SEPM1998 chart, FAD is 50% up in lusitanicum s.z of the H. bifrons zone.  Formerly called "B. criotum" (genera change).
	Biscutum striatum	181.35		90% up in H. serpentinum Zone.  On SEPM1998 chart, FAD is 65% up in H. falciferum s.z. of H. falciferum zone.
	Carinolithus superbus	182.63		Assigned as 5% up in H. serpentinum Zone (but disagreement in placement among workers).  On SEPM1998 chart, FAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Lotharingius crucicentralis	182.94		20% up in D. tenuicostatum Zone.  On SEPM1998 chart, FAD 95% up in P. paltus s.z. of D. (O.) tenuicostatum zone.
	Lotharingius sigillatus	183.00		Base D. tenuicostatum Zone (in Tethys).  On SEPM1998 chart, FAD is base of D. (O.) tenuicostatum zone.
	Axopodorhabdus atavus	184.48		90% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  On SEPM1998 chart, FAD is 40% up in acuratum s.z. of algovianum zone.
	Lotharingius hauffii	185.30		60% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  On SEPM1998 chart, FAD is 5% up in acuratum s.z. of algovianum zone.
	Biscutum novum, Biscutum profundum	186.68		10% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  Called D. novus on SEPM chart.  On SEPM1998 chart, FAD is the base of cornacaldense s.z. of lavinianum zone.
	Lotharingius spp.	187.35		mid-P. davoei Zone (Tethyan).  DTS1995 listed FAD as base of A. capricornus s.z. of P. davoei zone, but not in the SEPM chart.
	Bussonius prinsii	188.71		75% up in E. jamesoni Zone  (much lower than SEPM chart).  In DTS1995 FAD is the base of solare s.z. of emaciatum zonet.
	Similiscutum cruciulus	189.00		middle of U. jamesoni Zone.  On SEPM1998 chart, FAD is 55% up in U. jamesoni s.z. U. jamesoni zone.
	Similiscutum precarium	189.92		80% up in E. raricostatum Zone.  On SEPM1998 chart, FAD is 50% up in P. brevispina s.z. of U. jamesoni zone.  Taxa may be synonymous with D. orbiculatus (event on SEPM chart at same level).
	Crelaidolithus granulatus	190.41		50% up in E. raricostatum Zone (J. Bergen).  On SEPM1998 chart, FAD is base of A. maculatum s.z. of P. davoei zone.
	Orthogonoides hamiltoniae	192.40		70% up in A. obtusum Zone.  On SEPM1998 chart, FAD is 55% up in A. obtusum s.z. of A. obtusum zone.
	Parhabdolithus robustus	192.62		On SEPM1998 chart, FAD is 55% up in A. stellare s.z. of A. obtusum zone.
	Crepidolithus crassus	192.77		40% up in A. obtusum Zone.  On SEPM1998 chart, FAD is 55% up in A. obtusum s.z. of A. obtusum zone.
	Schizosphaerella punctulata	199.60
	Obliquipithonella rhombica (calcisphere)	203.64
	Crucirhabdus primulus	208.58
	Crucirhabdus minutus (coccolith), Archaeozygodiscus koessenensis (Ioxolith)	209.58
	Eoconusphaera ziambachensis (nannolith, Incertae sedis)	210.08
	Prinsiosphaera triassica (nannolith, Incertae sedis)	213.92
	Orthopithonella geometrica (calcisphere)	216.53
	EARLIEST NANNOFOSSILS = Orthopithonella misurinae and Obliquipithonella prasina (calcispheres), Carnicalyxia tabellata and Cassianospica curvata (nannoliths, Incertae sedis)	225.36

Other Nanno FAD/LAD	event		222/218/215		off
EVENT
	Sphenolithus ciperoensis -> S. distentus (abundance shift)	28.27		Same chron-age scaling as Leg 145 [ not used by Aubry in Berggren et al. (1995)] -- upper C10n; 28.3 Ma; [a,f] = C10n.1n.7.
	NANNOCONID CRISIS	124.69	dashed	Uncertain calibration.  SEPM'98 has assigned as Just below (0.1 myr) the FAD of R. angustus
LAD
	Helicosphaera sellii	1.26	dashed	Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.   This LAD is recorded slightly earlier (1.34 Ma) in ODP Legs 111 & 138 (Pacific).  Berggren et al. (1995) summarize as Mid-Lat = O-18 stage 37, 1.22 Ma, [b]; Equat. Zone = upper O-18 stage 49, 1.47 Ma, [c] = C1r.3r.99.   [NOTE: H. selli LAD is diachronous among regions]
	Calcidiscus macintyrei	1.60		Astronomically tuned in Pacific ODP Legs 111 & 138 and Atlantic Leg 154, Sites 925 & 926 -- Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (1.66 Ma) in Mediterranean (refs. 11, 22-24).  Berggren et al. (1995) assigns as upper O-18 stages 55 [e]; 1.59 Ma; [c] = C1r.3r.3.
	Discoaster triradiatus	1.95		Same chron-age scaling as Berggren et al. (1995) = in lowermost Olduvai; 1.95 Ma; [d,g] = base C2n.
	Sphenolithus spp.	3.54		LAD is called a "subtop" in Lourens et al. (GTS2004 table).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (3.65 Ma and 3.70 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7) and eastern Mediterranean (refs. 22 & 25), respectively.  Berggren et al (1995) -- Pliocene nannofossil 'Sphenolithus' (LAD) occurs at 3.56-3.6 Ma in Mediterranean [ref. d] = near base of Gauss; 3.6 Ma; [f,d] = base C2An.3n.
	Reticulofenestra antarctica	4.91		Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix
	Ceratolithus acutus	5.04		Astronomically tuned in Pacific (ODP Legs 111 and 138) and at Atlantic Leg 154, Sites 925 & 926 -- Refs 5-8, 10 & 12; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) assign as slightly older (~0.07 m.y.) than A. primus LAD; [h,i].
	Triquetrorhabdulus rugosus	5.28		Marker for base of Pliocene; not tabulated in Berggren et al. (1995).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) assign within uppermost part of C3r in Gilbert; 5.34 Ma [j,k] = C3r.85.
	Discoaster loeblichii	7.53		Same chron-age scaling as Berggren et al. (1995) = base C3Br; 7.4 Ma; [l,k,y] = base C3Br.
	Minylitha convallis	8.68		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  However, Berggren et al. (1995) calibrated this LAD as much higher = C4n.2n; 7.8 Ma; [l,k.y.] = C4n.2n.7
	Discoaster bollii	9.21		Same chron-age scaling as Berggren et al. (1995) = C4Ar.1r; 9.1 Ma; [l,r,t] = C4Ar.1r.5.
	Catinaster calyculus	9.67		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Leg 145 compilation (as LAD of genus Catinaster); not in Berggren et al. (1995) synthesis had assigned as C4A; 8.77 Ma [b] or 9.47 [h] -- averaged as base C4An.  Berggren et al (1995) had used as base of Subzones NN9b & CN7b; but these are not used in Lourens et al (2004).  
	Catinaster coalitus	9.69		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
	Helicosphaera walbersdorfensis (LCO)	10.74		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Coccolithus miopelagicus	10.97		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix.  LAD is recorded slightly earlier (11.02 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  LAD in N.Atl. is slightly earlier than Pacific [ref. l] according to Berggren et al (1995):  C5n.2n(Pac.); 10.9 Ma; [l,k,y]; or C5; 10.4 [d,h] or 9.94 [g]; therefore, C5n.2n.1 seems best chron-age calibration.
	Calcidiscus premacintyrei	11.21		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926). -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
	Discoaster kugleri	11.58		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix;  and simultaneous (11.60 Ma) in eastern Mediterranean (refs 35 & 36).  This "LCO" of Lourens et al (2004) seems to correspond in calibration to the "LAD" of Berggren et al (1995) at C5r.2n; 11.5 Ma [l,r] = C5r.2n.5.
	Cyclicargolithus floridanus	11.81		C. floridanus LCO is much earlier (13.28 Ma) in astronomical tuning from Atlantic and Mediterranean.  Lourens et al (2004) did not tabulate the LAD.  Therefore, LAD is placed using same chron-age scaling as Leg 145 synthesis (not in Berggren et al., 1995) = 11.5 Ma [d] or 11.8 [h] = C5r.3r.5.
	Coronocyclus nitescens	12.12		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Leg 145 compilation (not in Berggren et al's 1995 synthesis) had slightly lower LAD of ~C5A/C5AA; 12.8 Ma [a] or 12.9 Ma [h] = base C5Ar.2n.
	Calcidiscus premacintyrei (LCO)	12.38		Last "regular" occurrence is astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix.  This LRO is recorded slightly earlier (12.45 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 15 & 16).
	Cyclicargolithus floridanus (LCO)	13.28		Last common occurrence is astronomically tuned in eastern Mediterranean -- Ref. 36; in GTS2004 Neogene nannofossil appendix.  This LCO is recorded simultaneously as an "LAD" (13.33 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 15 & 16).  Leg 145 compilation (not in Berggren et al., 1995) had chron-age assignment of C5AA; 13.1 Ma [b] or 13.2 [h] or 13.14 [i] = C5AAr.5.
	Discoaster deflandrei group (acme)	15.80		Highest abundant occurrence is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Leg 145 synthesis (not in Aubry's synthesis in Berggren et al., 1995) = C5B; 15.9 Ma [a,h] = C5Br.15.
	Triquetrorhadulus serratus	22.38		Assumed same chron-age scaling as Leg 145 synthesis = C6Br; 23.2 Ma; [l,o] = C6Br.5.
	Sphenolithus umbrellus	22.83		Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.1r; 23.6 Ma; [l,t] = C6Cn.1r.5.
	Sphenolithus capricornutus	22.97		Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.2n; 23.7 Ma; [l,t] = C6Cn.2n.5.
	Sphenolithus delphix	23.11		Oligocene Nanno 'Spenolithus delphix LAD' may be similar to its 'top of acme'.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 10 & 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had similar chron-age placement (but age is older, due to different chron-scaling):  C6Cn.2n; 23.8 Ma; [l,r,t;h,i] = C6Cn.2n.3.
	Zygrhablithus bijugatus	23.84		Same chron-age scaling as Berggren et al. (1995) = C6Cr; 24.5 Ma [i,j,t] = C6Cr.3.
	Sphenolithus ciperoensis	24.04		Low-latitude marker for base of NN1.  Used as base of CN1a in some publications (in which LAD of D. bisectus becomes base of CN1b, rather than the present combined subzones).  Same chron-age scaling as Berggren et al. (1995) -- base C6Cr; 24.75 Ma [j,a,e,aa] = base C6Cr.
	Chiasmolithus altus	25.62		Same chron-age scaling as Berggren et al. (1995) = upper C8n; 26.1; [dd] = C8n.2n.8
	Sphenolithus predistentius	27.27		Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 -- C9n; 26.3 Ma; [j] = C8n.2n.5.
	Sphenolithus pseudoradians	29.08		Same chron-age scaling as Berggren et al. (1995) -- C10r; 29.1 Ma; [x] = C10r.5.
	Isthmolithus recurvus	31.98		Diachronous -- Oligocene Nanno 'Isthmolithus recurvus LAD' is "one of the most inconsistent datums" (Aubry, in Berggren et al., 1995), with estimated range of 1.3 m.y.  In this table, the youngest LAD is shown = C12r; 31.8 Ma; [j,x,dd] = C12r.6.
	Reticulofenestra oamaruensis	33.84		Restricted to southern high latitudes.  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = uppermost C13r; 33.7 Ma; [ll] = C13r.9.
	Discoaster barbadiensis  (low & mid lat.)	34.47		Diachronous;  another marker for Zone CP16a base.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C13r; 34.3 Ma; [l,aa] = C13r.3.
	Reticulofenestra reticulata  (low & mid lat.)	35.13		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = upper C15r; 35 Ma; [d,aa,bb] = C15r.75.
	Discoaster saipanensis  (high lat.)	35.49		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.1n; 35.4 Ma; [k, ll] = C16n.1n.5.
	Reticulofenestra reticulata  (high lat.)	36.05		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.2n; 36.1 Ma; [ll] = C16n.2n.4.
	Discoaster barbadiensis  (high lat.)	38.50		Diachronous.  Used same chron-age scaling as Berggren et al. (1995) = C18n; ~39 Ma; [m] = C18n.1n.5.
	Nannotetrina spp.	40.95		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C19r; 41.9 Ma; [a,d] = C19r.7.
	Nannotetrina fulgens	42.18		Same chron-age scaling as Berggren et al. (1995) = mid C20n; 43.1 Ma; [k,b,cc] = C20n.5.
	Discoaster sublodoensis	46.48		Leg 145 [not used by Aubry in Berggren et al. (1995)] = mid C21n; 47.2 Ma; [a,c] = C21n.4.
	Discoaster lodoensis	47.30		Leg 145 [not used by Aubry in Berggren et al. (1995)] = top C21r; 47.9 Ma; [a,c] = C21r.95.
	Rhabdosphaera inflata	48.60		Same chron-age scaling as Berggren et al. (1995) = ~base Foram Zone P10; [g,h] =Base C21r (which makes a convenient global event).
	Tribrachiatus bramlettei	54.41		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.89 Ma; [i,j] = C24r.79.
	Tribrachiatus contortus  (Morphotype A)	54.72		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 54.17 Ma; [i,j] = C24r.68.
	Fasciculithus spp.	54.78		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C24r; 54.1 Ma; [a,c] = C24r.66.
	Ericsonia robusta	55.72		Event occurs just prior to top of Paleocene [Ref.c].  Used relative chron-age scaling as Berggren et al. (1995) = C24r.3; 55.1 Ma; [a,c] = C24r.3
	Fasciculithus tympaniformis	56.01		Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.33 Ma; [h,l] = C24r.23.
	Heliolithus kleinpelli	58.26		Same chron-age scaling as Berggren et al. (1995) = lower C25r; 57.7 Ma; [a,c] = C25r.1.
	Hornibrookina teuriensis	59.12		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.3 Ma [j] = C26r.87.
	Chiasmolithus danicus	59.17		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.4 Ma; [a,b] = C26r.85.
	Cruciplacolithus tenuis, Fasciculithus pileatus	60.19		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [a,b] = C26r.5.
	Aspidolithus parcus constrictus	73.43		Boreal; shown as ~0.15 myr after A. parcus LAD in SEPM98
	Aspidolithus parcus	73.58		Base Chron C32r.2r in ODP 171/207 (used here).  Also called "Broinsonia parca" in some schemes.  GTS04 Fig 19.1 shows LAD as much lower (mid-Chron C33n); but SEPM Tethyan/Boreal scales has MUCH higher (4 myr above).
	Lithastrinus grillii	80.64	dashed	DASH:  EGI database calibrates as base of Middle Campanian (80.7 Ma) in Tethyan realm; and Jackie Lees (Burnett) assigns as upper Lower Campanian (ca. 81.5 Ma).  Both are much, much older than ODP Leg 171B table =  0.2 myr above LAD of E. eximius; and SEPM98 Tethys scale has as 0.5 myr above.  An intermediate assignment (= base of Middle Campanian) is used here.
	Reinhardtites anthophorus	75.40		Also called "Rein. elegans".  DASH:  EGI database (2005) calibrates as 74.0 Ma, which is about 1.5 myr higher than SEPM chart (same level as E. eximius); but considering uncertainties with E. eximius, then I've decided to retain SEPM placement.  SEPM'98 Boreal scale has simultaneous with LAD of E. eximius.
	Bukryaster hayii	80.00		LAD coincides with base of B. asperiformis zone in SEPM98 and ODP 171.
	Lithastrinus septenarius	85.04		SEPM'98 had assigned Just below (0.1 myr) the FAD of L. cayeuxii
	Cylindralithus biarcus	94.15		Marker for UC4 Zone; Leg 207 places just 0.1 myr below L. acutus LAD.
	Farhania varolii	112.50		65% up between Niveau Pacquer and Niveau Jacobi [J.Bergen], therefore about middle of H. jacobi Zone.  Also called Eprollithus varolii.
	Seribiscutum primitivum	113.94		20% up in T. bejaouensis Foram Zone (range of T. bejaouensis)
	Nannoconus truitti (acme)	115.00	dashed	Uncertain calibration (J. Bergen); so used SEPM for now = Base of N. nolani Zone.
	Prediscosphaera spinosa	115.60		10% up in Nanno Zone NC7c (J. Bergen)
	Nannoconus steinmannii	122.31		20% up in D. grandis s.z., which would be 60% up in D. deshayesi Zone.  SEPM'98 had assigned as Top of I. giraudi Z.
	Retecapsa angustiforata	123.35		60% up in D. weissi Zone
	Eiffellithus striatus	133.85		Base of S. sayni Zone.
	Eiffellithus windii	136.12		Middle of A. radiatus Zone
	Rucinolithus wisei	138.44		40% up in S. verrucosum Zone (Bergen, but assumed to be former S.verr. version, hence including N. peregrinus s.z.)
	Eiffellithus primus, C. deflanderi	139.35		Middle of B. campylotoxus Zone.
	Haqius noelae	145.14		10% up in Chron M17r (Bralower); but Bergen correlated to coeval with FAD of his N. steinmannii or about 50% up in B. jacobi s.z. (used here).  SEPM'98 had assigned FAD as 1/4 up in B. jacobi Z., P. grandis s.z.
FAD
	Gephyrocapsa caribbeanica to E. huxleyi shift of dominance  [in "transitional" waters]	0.07		Same chron-age scaling as Berggren et al. (1995) = O-18 stage 4; 0.075 Ma; [b,d] = C1n.91
	Reticulofenestra asanoi (FCO)	1.14		Astronomically tuned in Atlantic Leg 154, Sites 925 & 926 -- Refs 9-11; in GTS2004 Neogene nannofossil appendix.  FAD is recorded slightly later (1.08 Ma) in Mediterranean (refs. 18, 19 & 21).
	Discoaster triradiatus -- (acme)	2.22		Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix.  This Acme onset is recorded slightly later (2.14 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs 9 & 10).  Pliocene nannofossil 'Discoaster triradiatus' (onset acme) occurs at 2.25 Ma in Mediterranean [ref. c], in Berggren et al. (1995) compilation = early Matuyama; 2.18 Ma [g]; but 2.25 in Medit. [d] = C2r.2r.6.
	Reticulofenestra pseudoumbilica & Discoaster ovata	4.91		Lourens et al. (GTS2004 table) call both FADs in Mediterranean as a "subbottoms" in their calibration.  Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix.
	Discoaster surculus FCO	7.79		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.
	Discoaster loeblichii	8.77		Same chron-age scaling as Berggren et al. (1995) = base C4r; 8.7 Ma [l,k,y] = base C4r.
	Reticulofenestera pseudoumbilicus FCO	8.79		Lourens et al (2004) tabulate this "paracme" event with astronomical tuning in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Nearly simultaneous (8.71 Ma) in eastern Mediterranean (refs. 28, 33 & 35), where is defines base of MNN11.  Berggren et al. (1995) did not include it.
	Discoaster pentaradiatus (FCO)	9.37		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  LAD may be 0.3 m.y. earlier in Indo-Pacific [l,k,y].
	Minylitha convallis	9.75		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs slightly younger (9.61 Ma) in eastern Mediterranean (refs. 28, 33 & 35).  Berggren et al. (1995) place as C4Ar.2r.5, 9.5 Ma [l,y], or C4A, 8.9 Ma [a]; near Discoaster hamatus LAD, and indicate that this FAD in Pacific may be 0.2 m.y. later [ref. l,k,y] = C4Ar.2r.3.
	Discoaster bellus	10.40		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Discoaster neohamatus	10.52		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs much younger (9.87 Ma) in eastern Mediterranean (refs. 35 & 36).  Leg 145 compilation (not in Berggren et al., 1995) had placed in Chron C5, 8.96 Ma [b] or 9.62 [h] = base C4Ar.3r; which had put that FAD much higher by 0.8 myr.
	Helicosphaera stalis (FCO)	10.71		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Discoaster brouweri	10.76		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs simultaneously (10.73 Ma) in eastern Mediterranean (refs. 35 & 36).
	Catinaster calyculus	10.79		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Berggren et al (1995) note that correlations are disputed: C5n.2n, 10.7 Ma, [l,t,k,y]; or C5, 10.0 Ma [c] or 10.5 [h]; therefore, C5n.2n.2 seems best chron assignment.
	Calcidiscus macintyrei (FCO)	12.46		FCO is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 15 & 16; in GTS2004 Neogene nannofossil appendix
	Reticulofenestra pseudoumbilicus	12.82		Assumed same chron-age scaling as Leg Berggren et al (1995) = C5A ; 12.7 [d] = base C5Ar.2r
	Triquetrorhabdulus rugosus	13.28		Miocene Nanno 'Triquetrorhabdulus rugosus FAD' is estimated as 12.5 Ma in Leg 145 table, but 13.2 Ma  (0.7 m.y. older) in Aubry's synthesis (in Berggren et al., 1995), based on Hole 608 (ref. r); which is used here = C5AAn;13.2 Ma [l,r] or C5A ;12.5 Ma [d] = C5AAr.5.
	Calcidiscus macintyrei	13.37		From Leg 145 compilation; not in Lourens et al (2004) synthesis = base C5An [h] = base C5An.
	Discoaster signus	15.85		Assumed same chron-age scaling as Leg 145 synthesis (not in Aubry's synthesis in Berggren et al., 1995) = C5B; same as Top-Acme of D.defl. [a] = C5Br.15.
	Sphenolithus heteromorphus	17.71		Lourens et al (2004) assign this event as a first-common occurrence (FCO) that is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  However, based on coincidence with earlier calibrations, this is probably essentially the FAD as compiled by Berggren et al (1995) = lower C5D; 18.2 Ma [l,r; b,h,i] = C5Dr.1.
	Sphenolithus belemnos	19.03		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had similar assignment -- C6n; 19.2 Ma [d,h; l,r,t] or 19.7 [i] = C6n.9.
	Helicosphaera ampliaperta	20.43		Suggested as primary marker for base of Burdigalian.  Genus spelled as "Helicopontosphaera" in Lourens et al, 2004 table.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix.
	Helicosphaera carteri (FCO)	22.03		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix
	Sphenolithus disbelemnos	22.76		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix.  This species was not recognized in other schemes.
	Sphenolithus delphix	23.21		Oligocene Nanno 'Spenolithus delphix FAD' may be similar to its 'onset of acme' (Leg 145 table).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 10 & 15; in GTS2004 Neogene nannofossil appendix.  This FAD placement is nearly 1 myr higher than Leg 145 and Berggren et al. (1995) = upper C6Cr; 24.3 Ma; [a,f,t] = C6Cr.7.
	Triquetrorhabdulus carinatus (acme)	25.49		Same chron-age scaling as Leg 145; [not used by Aubry in Berggren et al. (1995)] = base C8n.1r; 26.0 Ma; [a,f] = base C8n.1r.
	Sphenolithus umbrellus	27.27		Scaling by Berggren et al. (1995); revised by Leg 145 = C9n; 26.3 Ma; [j,t] = C8n.2n.5.
	Reticulofenestra oamaruensis	35.49		Restricted to high latitudes.  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.1n; 35.4 Ma; [kk] = C16n.1n.5.
	Reticulofenestra bisecta	37.69		Same chron-age scaling as Berggren et al. (1995) = C17n.3n; 38 Ma; [k,z,cc] = C17n.3n.
	Reticulofenestra hesslandii	39.61		Leg 145 [not used by Aubry in Berggren et al. (1995)] = uppermost C18r; 40.4 Ma; [a,d] = C18r.85.
	Reticulofenestra reticulata	41.13		Same chron-age scaling as Berggren et al. (1995) = mid C19r; 42 Ma; [k,dd,gg,ii] = C19r.5.
	Reticulofenestra umbilicus (>14 micron)	41.22		Eocene Nanno 'R. umbilica' FAD is latitude dependent; and occurs as early as basal C20r in Contessa section (Italy).  Used same chron-age scaling as Berggren et al. (1995) = mid C19r; 42.2 Ma; [a,d] = C19r.4.
	Nannotetrina spp.	47.14		Leg 145 [not used by Aubry in Berggren et al. (1995)] = base C21n; 47.8 Ma; [a,c] = C21n.05.
	Sphenolithus radians	53.76		Leg 145 [not used by Aubry in Berggren et al. (1995)] = base C24n.; 53.2 Ma; [a,c] = C24n.3n.1.
	Tribrachiatus orthostylus	54.15		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.64 Ma; [i,j] = C24r.88.
	Tribrachiatus contortus  (Morphotype B)	54.46		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.93 Ma; [i,j] = C24r.77.
	Rhomboaster spp.	54.66		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C24r; 54.0 Ma; [a,c] = C24r.7
	Tribrachiatus contortus  (Morphotype A)	54.95		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 54.37 Ma; [i,j] = C24r.6.
	Rhomboaster cuspis	55.81		Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.16 Ma; [h,i] = C24r.3
	Discoaster okadai	57.60		Same chron-age scaling as Berggren et al. (1995) = upper mid-C25r; 56.8 Ma; [a,c,j] = C25n.65.
	Sphenolithus anarrhopus	59.17		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.4 Ma [j] = C26r.85.
	Heliiolithus cantabriae	59.76		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.3 Ma; [a,c] = C26r.65.
	Chiamolithus consuetus	60.48		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [j] = C26r.4.
	Fasciculithus ulii	60.69		Same chron-age scaling as Berggren et al. (1995) = lower C26r; 59.9 Ma; [j] = C26r.33.
	Fasciculithus spp.	60.78		Same chron-age scaling as Berggren et al. (1995) = lower C26r; 60.6 Ma; [a,c] = C26r.3.  Approx. FAD of Chiasmolithus bidens followed by FAD of Sphenolithus primus (North Sea) -- Ref.g.
	Sphenolithus primus	61.36		Same chron-age scaling as Berggren et al. (1995) = lowermost C26r; 60.6 Ma; [j] = C26r.1.  Approx. FAD of Neochiastozygus saepes in high latitudes -- Ref.g.
	Chiasmolithus bidens	61.45		Same chron-age scaling as Berggren et al. (1995) = lowermost C26r; 60.7 Ma; [j] = C26r.07.
	Sphenolithus spp.	61.50		Same chron-age scaling as Berggren et al. (1995) = basal C26r; 61.4 Ma; [a,c] = C26r.05.
	Cruciplacolithus primus	65.19		Same chron-age scaling as Berggren et al. (1995) = uppermost C29r; 64.8 Ma; [j] = C29r.9.
	Hornibrookina teuriensis	65.27		Same chron-age scaling as Berggren et al. (1995) = upper C29r; 64.9 Ma; [j] = C29r.8.
	Micula prinsii	65.90		Leg 207 assigned as 0.4 myr before end-Cretaceous.  Diachronous (p.16, ODP Leg 171B Expl. Notes); with Boreal FAD later than Tethyan (Von Salis, 1998, SEPM chart).  Assigned previously (1998) as simply 1 myr prior to end of Cretaceous (ODP Leg 171B assignment, and average of Tethyan/Boreal of von Salis).
	Cribrosphaerella daniae	66.30		Assigned here as synchronous with N. frequens, following von Salis SEPM98.  Boreal marker, approx. synchronous with FAD of N. frequens in Boreal realm (see Note on N. frequens).
	Cribrocorona gallica	68.73		SEPM98 shows as synchronous FAD with M. murus
	Misceomarginatus pleniporus	80.00		Leg 207 listed (but not B. hayii LAD), and is a Boreal marker as "base of UC15".  Seems, from Leg 207 relative placement, to be essentially coeval with LAD of B. hayii.
	Ceratolithoides verbeekii	82.10		SEPM'98 had assigned FAD is ~0.1 myr above base of S.hippocrepi II zone in SEPM.
	Aspidolithus parcus constrictus	82.55		Also called "Broinsonia parca constricta" in some schemes.  FAD assigned here as middle of S. hippocrepis I zone (Leg 207 approximate age coincidence, but they essentially placed it an even 1 myr above FAD of A. parcus).
	Lithastrinus grillii	85.85		SEPM'98 had assigned Same age as FAD of R. anthorphorus
	Lithastrinus septenarius	88.68		SEPM'98 had assigned as Just below (0.1 myr) the Middle/Early Coniacian boundary in Tethyan column.
	Cribrosphaerella ehrenbergii	110.35		70% up in Nanno Zone NC8b.  SEPM'98 had assigned FAD as middle of L. tardefurcata Z., L. schrammeni s.z.
	Acaenolithus viriosus	113.00		30% up between Niveau Pacquer and Niveau Jacobi [J.Bergen], therefore about base of H. jacobi Zone.
	N. regularis	114.00		Bergen did not check calibration on this one.  SEPM'98 had assigned FAD as top of N. nolani Z., D. nodosocostatum s.z.
	Rhagodiscus hamptonii	116.00		Was a potential datum for base of "NC7c" zone; but not that widespread (only SE France and India -- [Bown and Kennedy, 2000].  Coeval with LAD of Foram G. algeriana (base of H. trocoidea Foram Zone, called H. gorbachikae Foram Zone on this chart).   [Note (by J. Bergen): Bralower called this base-NC7c marker as Rhagodiscus achylostaurion.  But true R. acy. Ha its FAD in Barremian.]  Not in SEPM chart.  Assigned as base of N. nolani zone (based on projected placement of 115.2 Ma in Leg 207 table)
	Nannoconus truitti (acme)	120.01	dashed	Uncertain calibration (J. Bergen); so used SEPM for now =  ~1/3rd up in C. martinoides Zone (= 1/3rd up in E. subnodosocostatum Zone).
	Radiolithus planus	121.36		60% up in T. bowerbanki (D. furcata) Zone.
	Braarudosphaera africana	121.41		55% up in T. bowerbanki (D. furcata) Zone.  SEPM'98 had FAD projected to 4/10 up in D. deshayesi Zone; but with new FAD of E. floralis (control age point in GTS2004), then it is near middle of D. furcata Zone)
	Rhagodiscus angustus	122.93		Base of D. deshayesi.  SEPM'98 had assigned FAD assigned as base of D. weissi Zone
	Stoverius achylosum	124.03		80% up in Nanno Zone NC6a (Bralower with Leckie), or in upper-third of OAE1a event.  SEPM'98 has assigned as Same level as FAD B. africana (see its Note).
	Rhadodiscus achlyostaurion 	126.92		Middle of H. feraudianus Zone.  SEPM'98 had assigned as Base of I. giraudi Z.
	Zeugrhabdotus scutula	133.69		25% up in S. sayni Zone.
	Nannoconus bucheri	136.54	dashed	DASH at SEPM placement = Just below (0.1 myr) the base of Hauterivian
	Zeugrhabdotus trivectis	139.27		60% up in B. campylotoxus Zone.
	Micranthololithus speetonensis, R. dekaenelii	139.77		Base of B. campylotoxus Zone.
	Rucinolithus wisei	140.80		75% up in T. alpillensis Zone (Bergreen, 1994).  SEPM'98 had assigned FAD as base of B. picteti subzone.
	Tubodiscus verenae	140.95	dashed	DASH at Middle of T. alpillensis (about 2 ammonite zones LOWER than on SEPM chart), poorly constrained.  SEPM'98 had assigned FAD as 4/10 up in S. verrucosum Z.
	Percivalia fenestrata	141.25		Base of T. alpillensis Zone.  This FAD is used to subdivide NC2 (called NK2) to 2a/2b in scheme of Bralower et al. (1995).  SEPM'98 had assigned FAD as base of T. alpillensis subzone
	Rhaqodiscus nebulosus, Diadorhombus rectus	143.32		Rh. nebulosus FAD is Middle of S. subalpina s.z. (Bergen).  Diado. rectus FAD is 60% up in Chron M17r (Bralower).  SEPM'98 had assigned FAD of Rh. nebulosus as base of M. paramimounum subzone.  SEPM'98 had assigned FAD of Diado. rectus is base of S. subalpina subzone
	Assipetra infracretacea	143.92		10% up in Chron M17r (Bralower).  SEPM'98 assigned FAD as 1/4 up in B. jacobi Z., P. grandis s.z.
	Markalius circumradiatus	144.04		Base Chron M17r (Bralower).  SEPM'98 had assigned FAD just above (0.1 myr) the base of B. jacobi Z., P. grandis s.z.
	Cruciellipsis cuvillieri, Manivitella pemmatoldea	145.03		Middle of Chron M19n.1r.  Therefore, basal Berriasian instead of uppermost Tithonian (using top-Durangites working definition).  On SEPM1998 chart, FADs are 90% up in Durangites Z.
	Speetonia collgata	145.15		90% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 85% up in Durangites Z.
	Rotelapillus laffittei	145.24		80% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 75% up in Durangites Z.

Additional Plio-Pleist datums	event		222/218/215		off	mainly Lourens et al. (GTS2004 tables)
EVENT
	Emiliania huxleyi (acme in Mediterreanean)	0.05
	Transition of Ceratolithus acutus to C. rugosus in Atlantic	5.05		This transition is NOT the FAD of C. acutus, but apparently a change in Atlantic dominance.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
LAD
	Gephyrocapsa sp.3	0.61		Cycle-calibrated in Eastern Mediterranean -- Refs 17, 18 & 20; in GTS2004 Neogene nannofossil appendix
	small Gephyrocapsa spp. dominance	1.02		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9-11; in GTS2004 Neogene nannofossil appendix.  
	large (over 5.5 microns) Gephyrocapsa spp.	1.24		Astronomically tuned in Pacific (ODP Legs 111 & 138) --Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  LAD recorded slightly earlier (1.26 Ma) at Atlantic Leg 154, Sites 925 & 926, and  (1.25 Ma) in Mediterranean (refs. 11, 22-24).  Berggren et al. (1995) have same assignment = O-18 stage 37 [e]; 1.22-1.24 Ma; [a,b] = C1r.3r.97.
FAD
	Gephyrocapsa caribbeanica to E. huxleyi shift of dominance  [in tropical and subtropical waters]	0.09		Same chron-age scaling as Berggren et al. (1995) = O-18 stages 5a-5b; 0.09 Ma; [b,d] = C1n.88
	Gephyrocapsa sp.3	1.02		Astronomically tuned in Pacific (ODP Legs 111 & 138) -- Refs 1-5; in GTS2004 Neogene nannofossil appendix.  FAD is recorded slightly later (0.97 Ma) in Mediterranean (refs. 17, 18 & 21).  Berggren et al. (1995) have same = O-18 stage 25 (above Jaramillo); 0.96 Ma; [b] = C1r.1r.15. 
	small Gephyrocapsa spp. dominance	1.24		Astronomically tuned in Pacific (ODP Legs 111 & 138) --Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.	
	large (over 5.5 microns) Gephyrocapsa spp.	1.62		Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.  This FAD is recorded slightly later (1.46 and 1.56 Ma) in Pacific ODP Legs 111 & 138 (Refs 1-5) and in Atlantic Leg 154, Sites 925 & 926 (Refs 9-11), respectively.  Berggren et al. (1995) assign FAD slightly younger, as upper O-18 stage 48 [e]; 1.46-1.48 Ma; [a] = C1r.3r.55.
	Ceratolithus larrymayeri (sp.1)	5.34		Tabulated in Lourens et al (2004), and would be a regional marker for base of Pliocene.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix


All Tropical Nanno Datums Combined	event		222/218/215		off
LAD
	Pseudoemiliania lacunosa	0.44		LAD defines top of NN21, hence base of NN20.  Astronomically tuned in Pacific (ODP Legs 111 & 138) and Atlantic (Leg 154, Sites 925 & 926).  -- Refs 1-5, 9 & 10; in GTS2004 Neogene nannofossil appendix.  Age is recorded slightly older (0.47 myr) in Mediterranean (refs. 11, 17 & 18).  Berggren et al. (1995) have same assignment = O-18 stage 12; 0.46 Ma; [b,d] = C1n.4.
	Gephyrocapsa sp.3	0.61		Cycle-calibrated in Eastern Mediterranean -- Refs 17, 18 & 20; in GTS2004 Neogene nannofossil appendix
	Reticulofenestra asanoi (common)	0.91		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9-11; in GTS2004 Neogene nannofossil appendix. LAD is at same time (0.90 Ma) in Mediterranean (refs. 17, 18 & 21).  
	small Gephyrocapsa spp. dominance	1.02		Astronomically tuned in Pacific (ODP Legs 111 & 138) -- Refs 1-5; in GTS2004 Neogene nannofossil appendix.    
	large (over 5.5 microns) Gephyrocapsa spp.	1.24		"tlG event"  Astronomically tuned in Pacific (ODP Legs 111 & 138) --Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  LAD recorded slightly earlier (1.26 Ma) at Atlantic Leg 154, Sites 925 & 926, and  (1.25 Ma) in Mediterranean (refs. 11, 22-24).  Berggren et al. (1995) have same assignment = O-18 stage 37 [e]; 1.22-1.24 Ma; [a,b] = C1r.3r.97.
	Helicosphaera sellii	1.26	dashed	Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.   This LAD is recorded slightly earlier (1.34 Ma) in ODP Legs 111 & 138 (Pacific).  Berggren et al. (1995) summarize as Mid-Lat = O-18 stage 37, 1.22 Ma, [b]; Equat. Zone = upper O-18 stage 49, 1.47 Ma, [c] = C1r.3r.99.   [NOTE: H. selli LAD is diachronous among regions]
	Calcidiscus macintyrei	1.60		Astronomically tuned in Pacific ODP Legs 111 & 138 and Atlantic Leg 154, Sites 925 & 926 -- Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (1.66 Ma) in Mediterranean (refs. 11, 22-24).  Berggren et al. (1995) assigns as upper O-18 stages 55 [e]; 1.59 Ma; [c] = C1r.3r.3.
	Discoaster brouweri	1.93		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD of D. brouweri is recorded slightly earlier (1.95 Ma) in Mediterranean (refs. 11, 22-25), and significantly earlier (2.06 Ma) in Pacific ODP Legs 111 and 138 (refs. 4-7).  Berggren et al. (1995) assign in lowermost Olduvai; 1.95 Ma; [d,g] = base C2n.
	Discoaster triradiatus	1.95		Same chron-age scaling as Berggren et al. (1995) = in lowermost Olduvai; 1.95 Ma; [d,g] = base C2n.
	Discoaster pentaradiatus	2.39		LAD of D. pentaradiatus (quintatus) defines top of NN17, hence base of NN18.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded earlier (2.51 Ma) in Mediterranean (refs. 20, 22, 25 & 26).  Berggren et al. (1995) places near Matuyama/Gauss boundary; 2.46-2.56 Ma; [g,d] = C2r.3r.25.
	Discoaster surculus	2.49		LAD of D. surculus defines top of NN16, hence base of NN17.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 9 & 10; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (2.52 Ma and 2.54 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7) and eastern Mediterranean (refs. 20, 22, 25 & 26), respectively.  Berggren et al. (1995) place near Matuyama/Gauss boundary; 2.55-2.59 Ma; [g,d] = C2r.3r.1.
	Discoaster tamalis	2.80		Lourens et al (GTS2004 table) refers to this LAD as a "subtop".  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) and eastern Mediterranean -- Refs 10, 12, 20, 22, 25 & 26; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (2.87 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7).  Pliocene nannofossil 'Discoaster tarnalis' (LAD) occurs at 2.73 Ma in Mediterranean [ref. d] in Berggren et al.'s compilation, with main assignment near top of Gauss; 2.78 Ma; [g,d] = C2An.1n.6.
	Sphenolithus spp.	3.54		LAD is called a "subtop" in Lourens et al. (GTS2004 table).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (3.65 Ma and 3.70 Ma) in Pacific ODP Legs 111 and 138 (refs 4-7) and eastern Mediterranean (refs. 22 & 25), respectively.  Berggren et al (1995) -- Pliocene nannofossil 'Sphenolithus' (LAD) occurs at 3.56-3.6 Ma in Mediterranean [ref. d] = near base of Gauss; 3.6 Ma; [f,d] = base C2An.3n.
	Reticulofenestra pseudoumbilicus	3.70		This LAD defines top of NN15, hence base of NN16.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 11; in GTS2004 Neogene nannofossil appendix.  This LAD is recorded slightly earlier (3.79 Ma and 3.84 Ma) in Pacific (ODP Legs 111 and 138; refs 4-7) and eastern Mediterranean (refs. 22 & 25), respectively.  Berggren et al. (1995) -- Pliocene nannofossil Reticulofenestra pseudoumbilicus (LAD) occurs at 3.66-3.7 Ma in Mediterranean [ref. c] = uppermost part of Upper reversed interval of Gilbert (Med.); 3.75 Ma; [e] = C2Ar.7.
	Discoaster tricorniculatus	3.92		Same chron-age scaling as Berggren et al. (1995) -- mid-way between D. asymmetricus FAD & R. pseudoumbilicus LAD; [b,h] -- not given age in table of Lourens et al (GTS2004).
	Amaurolithus primus	4.50		Lourens et al (GTS2004) referred to this FAD as a "subbottom".  Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix.  Pliocene nannofossil Amaurolithus primus (LAD) occurs in Nunivak (4.55 Ma) in Mediterranean [ref. d], in Berggren et al.'s (1995) compilation (slightly older LAD than Lourens et al.) = near top of Sidufjall; 4.58 Ma; [a,d,c,i] = C3n.3n.8.
	Reticulofenestra antarctica	4.91		Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix
	Ceratolithus acutus	5.04		Astronomically tuned in Pacific (ODP Legs 111 and 138) and at Atlantic Leg 154, Sites 925 & 926 -- Refs 5-8, 10 & 12; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) assign as slightly older (~0.07 m.y.) than A. primus LAD; [h,i].
	Triquetrorhabdulus rugosus	5.28		Marker for base of Pliocene; not tabulated in Berggren et al. (1995).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) assign within uppermost part of C3r in Gilbert; 5.34 Ma [j,k] = C3r.85.
	Discoaster quinqueramus	5.59		Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix.  This LAD is reported at same time (5.58 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 10 & 13).  Berggren et al. (1995) -- mid-C3r in Gilbert; 5.3 Ma [l,k,y,aa]; or 4.98 Ma [b] = C3r.5.
	Nicklithus amplificus	5.94		Genus for amplificus was "Amaurolithus" in Berggren's (1995) table; and had been used as base of "Subzone NN11d".  Astronomically tuned in eastern Mediterranean -- Refs 27-29; in GTS2004 Neogene nannofossil appendix.  This LAD (and LCO) is reported at same time (5.98 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  The LCO is at 6.12 Ma and 6.14 Ma in Pacific (ODP Legs 11 & 138; refs. 5-8) and Mediterranean (refs. 27-29), respectively.  Berggren et al. (1995) assigned as base C3r; 5.9 Ma [l,k,y]; or C3A; 5.33 Ma [a] = base C3r.
	Discoaster loeblichii	7.53		Same chron-age scaling as Berggren et al. (1995) = base C3Br; 7.4 Ma; [l,k,y] = base C3Br.
	Minylitha convallis	8.68		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  However, Berggren et al. (1995) calibrated this LAD as much higher = C4n.2n; 7.8 Ma; [l,k.y.] = C4n.2n.7
	Discoaster bollii	9.21		Same chron-age scaling as Berggren et al. (1995) = C4Ar.1r; 9.1 Ma; [l,r,t] = C4Ar.1r.5.
	Discoaster hamatus	9.53		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  LAD occurs slightly earlier (9.69 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  Correlations, as indicated by Berggren et al. (1995) were inconsistent; with younger LADs being reported elsewhere in previous literature -- C4Ar.2r.5; 9.4 Ma [l,t,k,y]; or C4A; 8.67 Ma [b] or 9.37 Ma [h]; therefore C4Ar.2r.5 seems best estimate (nearly same as astronomical tuning).
	Catinaster calyculus	9.67		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Leg 145 compilation (as LAD of genus Catinaster); not in Berggren et al. (1995) synthesis had assigned as C4A; 8.77 Ma [b] or 9.47 [h] -- averaged as base C4An.  Berggren et al (1995) had used as base of Subzones NN9b & CN7b; but these are not used in Lourens et al (2004).  
	Catinaster coalitus	9.69		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
	Helicosphaera walbersdorfensis (LCO)	10.74		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Coccolithus miopelagicus	10.97		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix.  LAD is recorded slightly earlier (11.02 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  LAD in N.Atl. is slightly earlier than Pacific [ref. l] according to Berggren et al (1995):  C5n.2n(Pac.); 10.9 Ma; [l,k,y]; or C5; 10.4 [d,h] or 9.94 [g]; therefore, C5n.2n.1 seems best chron-age calibration.
	Calcidiscus premacintyrei	11.21		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926). -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
	Discoaster kugleri	11.58		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix;  and simultaneous (11.60 Ma) in eastern Mediterranean (refs 35 & 36).  This "LCO" of Lourens et al (2004) seems to correspond in calibration to the "LAD" of Berggren et al (1995) at C5r.2n; 11.5 Ma [l,r] = C5r.2n.5.
	Cyclicargolithus floridanus	11.81		C. floridanus LCO is much earlier (13.28 Ma) in astronomical tuning from Atlantic and Mediterranean.  Lourens et al (2004) did not tabulate the LAD.  Therefore, LAD is placed using same chron-age scaling as Leg 145 synthesis (not in Berggren et al., 1995) = 11.5 Ma [d] or 11.8 [h] = C5r.3r.5.
	Coronocyclus nitescens	12.12		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Leg 145 compilation (not in Berggren et al's 1995 synthesis) had slightly lower LAD of ~C5A/C5AA; 12.8 Ma [a] or 12.9 Ma [h] = base C5Ar.2n.
	Calcidiscus premacintyrei (LCO)	12.38		Last "regular" occurrence is astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix.  This LRO is recorded slightly earlier (12.45 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 15 & 16).
	Cyclicargolithus floridanus (LCO)	13.28		Last common occurrence is astronomically tuned in eastern Mediterranean -- Ref. 36; in GTS2004 Neogene nannofossil appendix.  This LCO is recorded simultaneously as an "LAD" (13.33 Ma) at Atlantic Leg 154, Sites 925 & 926 (refs. 15 & 16).  Leg 145 compilation (not in Berggren et al., 1995) had chron-age assignment of C5AA; 13.1 Ma [b] or 13.2 [h] or 13.14 [i] = C5AAr.5.
	Sphenolithus heteromorphus	13.53		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 14 & 15; in GTS2004 Neogene nannofossil appendix;  but LAD is reported slightly earlier (13.654 Ma) in eastern Mediterranean (ref 37).  This offset, although only 100myr, causes a problem, because the "primary marker" for base-Serravallian GSSP suggested in Mediterranean region is that nannofossil S. heteromorphus LAD.  Berggren et al. (1995) had similar chron-age assignment of C5ABr; 13.6 Ma [l,r] or 13.5 Ma [d,h,i] = C5ABr.6.
	Helicosphaera ampliaperta	14.91		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had placed this LAD about 0.6 myr older,  as C5B; 15.6 Ma [l,r] or 15.8 Ma [a,h] = C5Br.5.
	Discoaster deflandrei group (acme)	15.80		Highest abundant occurrence is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Leg 145 synthesis (not in Aubry's synthesis in Berggren et al., 1995) = C5B; 15.9 Ma [a,h] = C5Br.15.
	Sphenolithus belemnos	17.95		Lourens et al (2004) assign this event as a LCO that is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  However, based on coincidence with earlier calibrations, this is probably essentially the LAD (which was the original definition of the zone).  There seems a 0.1 myr difference (J. Bergen, pers. commun., 2005).  Berggren et al. (1995) had summarized as C5E; 18.5 Ma [b,h] or18.27 Ma [i] = C5En.9.
	Triquetrorhabdulus carinatus	18.28		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  Note that this event is ~1myr YOUNGER than earlier reports.  Very poorly constrained age -- 19.5 [b] or 23.0 [d]; 23.1 [h] or 19.2 [i].  Early Miocene Nanno 'T. carinatus' LAD is diachronous, and appears to range from 19.5 to 23.0 Ma.  Hodell & Woodruff (1994) have a similar conclusion, although their estimate for this event in Site 289 suggests that it may be reworked.  Earlier version of this database had used an intermediate estimate (19.2 Ma), which is similar to that used by Aubry (ca. 19 Ma) in her charts in Berggren et al. (1995) = C6n.9.
	Triquetrorhadulus serratus	22.38		Assumed same chron-age scaling as Leg 145 synthesis = C6Br; 23.2 Ma; [l,o] = C6Br.5.
	Sphenolithus umbrellus	22.83		Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.1r; 23.6 Ma; [l,t] = C6Cn.1r.5.
	Sphenolithus capricornutus	22.97		Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.2n; 23.7 Ma; [l,t] = C6Cn.2n.5.
	Sphenolithus delphix	23.11		Oligocene Nanno 'Spenolithus delphix LAD' may be similar to its 'top of acme'.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 10 & 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had similar chron-age placement (but age is older, due to different chron-scaling):  C6Cn.2n; 23.8 Ma; [l,r,t;h,i] = C6Cn.2n.3.
	Dictylcoccites bisectus	23.14		Leg 145 referred to this LAD as top of acme; but I have followed Leg 171 scheme.  High-latitude marker for base of NN1.  Basal Miocene Nanno ' Reticulofenestra bisecta' was called 'Discoaster bisectus' in Berggren (earlier draft), and is called 'Dictyococcites bisectus' in Perch-Nielsen (1985).  The LAD of 'R. bisectus' is used to approximate the NP25/NN1 boundary in high latitudes; and was "substituted for H. recta, the marker of the NP15/NN1 boundary in Martini's (1971) zonal scheme" by Aubry (in Berggren et al., 1995).  Assumed same chron-age scaling as Leg 145 synthesis = C6Cn.2rr; 23.9 Ma; [a,b,j,cc] = C6Cn.2r.5.
	Zygrhablithus bijugatus	23.84		Same chron-age scaling as Berggren et al. (1995) = C6Cr; 24.5 Ma [i,j,t] = C6Cr.3.
	Sphenolithus ciperoensis	24.04		Low-latitude marker for base of NN1.  Used as base of CN1a in some publications (in which LAD of D. bisectus becomes base of CN1b, rather than the present combined subzones).  Same chron-age scaling as Berggren et al. (1995) -- base C6Cr; 24.75 Ma [j,a,e,aa] = base C6Cr.
	Chiasmolithus altus	25.62		Same chron-age scaling as Berggren et al. (1995) = upper C8n; 26.1; [dd] = C8n.2n.8
	Sphenolithus distentus	27.27		Oligocene Nanno 'Sphenolithus distentus' LAD is correlated to C9n by Aubry (in Berggren et al., 1995) at 27.5 Ma, which is nearly 1 m.y. older than mid-C8n.2n correlation in Leg 145 table.  Used chron-age scaling as  revised by Leg 145 = C9n; 26.3 Ma; [j,x;a,f] = C8n.2n.5.
	Sphenolithus predistentius	27.27		Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 -- C9n; 26.3 Ma; [j] = C8n.2n.5.
	Sphenolithus pseudoradians	29.08		Same chron-age scaling as Berggren et al. (1995) -- C10r; 29.1 Ma; [x] = C10r.5.
	Reticulofenestra umbilicus / R.hillae  (south high lat.)	31.44		diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  For simplicity, I have placed the associated Zone NP23; CP17 base with the mid-latitude level (32.3 Ma).  Same chron-age scaling as Berggren et al. (1995) = upper C12r; 31.3 Ma; [j,dd] = C12r.85.
	Isthmolithus recurvus	31.98		Diachronous -- Oligocene Nanno 'Isthmolithus recurvus LAD' is "one of the most inconsistent datums" (Aubry, in Berggren et al., 1995), with estimated range of 1.3 m.y.  In this table, the youngest LAD is shown = C12r; 31.8 Ma; [j,x,dd] = C12r.6.
	Reticulofenestra umbilicus / R.hillae  (low-mid lat.)	32.51		Diachronous -- Oligocene Nanno 'Reticulofenestra umbilicus LAD' was specified as ">14 micron" in Leg 145 table.  This LAD occurs earlier (32.3 Ma) in low-mid latitudes than in southern high-latitudes (31.3 Ma) = 1m.y. diachroneity.  Same chron-age scaling as Berggren et al. (1995) = mid C12r; 32.3 Ma; [j,t] = C12r.35.
	Ericsonia formosa  (mid-low lat.)	33.05		Diachronous (LAD is 7 m.y. earlier in south high lat!) [j]  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C12r; 32.7 Ma; [a,d] = C12r.1.
	Reticulofenestra oamaruensis	33.84		Restricted to southern high latitudes.  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = uppermost C13r; 33.7 Ma; [ll] = C13r.9.
	Discoaster barbadiensis  (low & mid lat.)	34.47		Diachronous;  another marker for Zone CP16a base.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C13r; 34.3 Ma; [l,aa] = C13r.3.
	Discoaster saipanensis  (low & mid lat.)	34.78		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = lower C13r; 34.2 Ma; [k,r] = C13r.4.
	Reticulofenestra reticulata  (low & mid lat.)	35.13		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = upper C15r; 35 Ma; [d,aa,bb] = C15r.75.
	Discoaster saipanensis  (high lat.)	35.49		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.1n; 35.4 Ma; [k, ll] = C16n.1n.5.
	Reticulofenestra reticulata  (high lat.)	36.05		Diachronous.  Used same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.2n; 36.1 Ma; [ll] = C16n.2n.4.
	Chiasmolithus grandis	36.95		Same chron-age scaling as Berggren et al. (1995) = C17n.1n; 37.1 Ma; [a,b,cc] = C17n.1n.4.  This LAD occurs approx. 2 m.y. earlier in Mediterranean [Ref.b].
	Discoaster barbadiensis  (high lat.)	38.50		Diachronous.  Used same chron-age scaling as Berggren et al. (1995) = C18n; ~39 Ma; [m] = C18n.1n.5.
	Chiasmolithus solitus	39.71		LAD reported higher (C18n) in Hole 748 (ref. m).  Same chron-age scaling as Berggren et al. (1995) = upper C18r; 40.4 Ma; [cc] = C18r.75.
	Nannotetrina spp.	40.95		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C19r; 41.9 Ma; [a,d] = C19r.7.
	Nannotetrina fulgens	42.18		Same chron-age scaling as Berggren et al. (1995) = mid C20n; 43.1 Ma; [k,b,cc] = C20n.5.
	Blackites gladius	42.42		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = lower C20n; 43.4 Ma; [k,m,n,nn] = C20n.3.
	Chiasmolithus gigas	43.55		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = upper C20r; 44.6 Ma; [a,b,n,mm] = C20r.7.
	Discoaster sublodoensis	46.48		Leg 145 [not used by Aubry in Berggren et al. (1995)] = mid C21n; 47.2 Ma; [a,c] = C21n.4.
	Discoaster lodoensis	47.30		Leg 145 [not used by Aubry in Berggren et al. (1995)] = top C21r; 47.9 Ma; [a,c] = C21r.95.
	Rhabdosphaera inflata	48.60		Same chron-age scaling as Berggren et al. (1995) = ~base Foram Zone P10; [g,h] =Base C21r (which makes a convenient global event).
	Tribrachiatus orthostylus	50.47		Eocene Nanno 'T. orthostylus' LAD (= base of Zone NP12) has a poorly defined age, and may be time-transgressive?  (see discussion in Berggren et al., 1985).  Same chron-age scaling as Berggren et al. (1995) = lower C22r; 50.6 Ma; [a,b,c,n] = C22r.2.
	Tribrachiatus contortus  (Morphotype B)	54.09		Eocene Nanno evolution from Tribrachiatus contortus to Tribrachiatus orthostylus was formerly described as an abundance shift, but Aubry has subdivided it into different morphotypes.  Same chron-age scaling as Berggren et al. (1995) = upper C24r; 53.61 Ma; [i,j] = C24r.9.
	Tribrachiatus bramlettei	54.41		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.89 Ma; [i,j] = C24r.79.
	Tribrachiatus contortus  (Morphotype A)	54.72		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 54.17 Ma; [i,j] = C24r.68.
	Fasciculithus spp.	54.78		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C24r; 54.1 Ma; [a,c] = C24r.66.
	Ericsonia robusta	55.72		Event occurs just prior to top of Paleocene [Ref.c].  Used relative chron-age scaling as Berggren et al. (1995) = C24r.3; 55.1 Ma; [a,c] = C24r.3
	Fasciculithus tympaniformis	56.01		Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.33 Ma; [h,l] = C24r.23.
	Heliolithus kleinpelli	58.26		Same chron-age scaling as Berggren et al. (1995) = lower C25r; 57.7 Ma; [a,c] = C25r.1.
	Hornibrookina teuriensis	59.12		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.3 Ma [j] = C26r.87.
	Chiasmolithus danicus	59.17		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.4 Ma; [a,b] = C26r.85.
	Cruciplacolithus tenuis, Fasciculithus pileatus	60.19		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [a,b] = C26r.5.
	Micula murus, other Cret. nannos	65.50		Chron-age calibration = upper C29r; K/T boundary; [b,g] = C29r.7.
	Reinhardtites levis	69.23		Bralower et al (1995) suggest using this LAD to subdivide NC21 into a/b subzones; but the GTS2004 ages would imply very short durations, so omitted here.  ODP age is 69.8 Ma, but EGI database (2005) calibrates as much higher at 68.4 Ma (North Sea) and 68.6 (Tethys).  This younger age would probably require the overlying succession to also be pushed "higher" to retain same sequence.  SEPM'98 had assigned LAD is top of B. clinolobatus (base of H. birkelundi) ammonite = Late/Early Maastr. boundary.
	Tranolithus orionatus  (=T. phacelosus)	69.63	dashed	DASH:  Leg 207 uses this LAD for base-CC24, rather than T. phacelosus (same taxa?); but indicates that it is only 0.4 myr below base-CC25.  Relative-age to R. levis used here and as CC24 base.  SEPM'98 had assigned LAD at base of Maastrichtian.
	Uniplanarius trifidum	69.85		Also known as Quadrum trifidum (and T. trifidus)  Calibrated via Sr 87/86 to US Western Interior ages.  Occurs ~0.75 myr above Tercis GSSP of base-Maastrichtian (used here).
	Aspidolithus parcus constrictus	73.43		Boreal; shown as ~0.15 myr after A. parcus LAD in SEPM98
	Aspidolithus parcus	73.58		Base Chron C32r.2r in ODP 171/207 (used here).  Also called "Broinsonia parca" in some schemes.  GTS04 Fig 19.1 shows LAD as much lower (mid-Chron C33n); but SEPM Tethyan/Boreal scales has MUCH higher (4 myr above).
	Eiffellithus eximius	75.40		EGI database calibrates as base of Upper Campanian (76.4 Ma in Tethyan; 76.3 Ma in Boreal) and Jackie Lees (Burnett) assigns as upper Upper Campanian (ca. 73 Ma).  Therefore, the ODP value of about 75.4 Ma seems suitable, and is used here.  SEPM'98 had assigned LAD is middle of D. stevensoni Z.
	Reinhardtites anthophorus	75.40		Also called "Rein. elegans".  DASH:  EGI database (2005) calibrates as 74.0 Ma, which is about 1.5 myr higher than SEPM chart (same level as E. eximius); but considering uncertainties with E. eximius, then I've decided to retain SEPM placement.  SEPM'98 Boreal scale has simultaneous with LAD of E. eximius.
	Bukryaster hayii	80.00		LAD coincides with base of B. asperiformis zone in SEPM98 and ODP 171.
	Marthasterites furcatus	80.64		SEPM'98 had assigned LAD as base of Middle Camp (base B. obtusus)
	Lithastrinus grillii	80.64	dashed	DASH:  EGI database calibrates as base of Middle Campanian (80.7 Ma) in Tethyan realm; and Jackie Lees (Burnett) assigns as upper Lower Campanian (ca. 81.5 Ma).  Both are much, much older than ODP Leg 171B table =  0.2 myr above LAD of E. eximius; and SEPM98 Tethys scale has as 0.5 myr above.  An intermediate assignment (= base of Middle Campanian) is used here.
	Lithastrinus septenarius	85.04		SEPM'98 had assigned Just below (0.1 myr) the FAD of L. cayeuxii
	Rhagodiscus asper, Axopodorhabdus albianus, Corollithion kennedyi	93.95		Leg 171B has this cluster of LADs (C. kennedyi, R. asper, A. albianus) at ~0.4 myr below top of Cenomanian (ammonite zone?)
	Lithraphidites acutus	94.05		LAD assigned as ~0.5 myr below top of Cenomanian in Leg 207 scale (= marker for base of UC5 Zone)
	Cylindralithus biarcus	94.15		Marker for UC4 Zone; Leg 207 places just 0.1 myr below L. acutus LAD.
	Microstaurus chiastius	94.43		LAD is 3/4ths up in D. problimaticum Z. (Leg 171B relative placement)
	Hayesites albiensis	100.40		40% up in R. appenninica Foram Zone.  SEPM'98 assigned as Middle of M. perinflatum subzone.
	Farhania varolii	112.50		65% up between Niveau Pacquer and Niveau Jacobi [J.Bergen], therefore about middle of H. jacobi Zone.  Also called Eprollithus varolii.
	Seribiscutum primitivum	113.94		20% up in T. bejaouensis Foram Zone (range of T. bejaouensis)
	Nannoconus truitti (acme)	115.00		Uncertain calibration (J. Bergen); so used SEPM for now = Base of N. nolani Zone.
	Prediscosphaera spinosa	115.60		10% up in Nanno Zone NC7c (J. Bergen)
	Micrantholithus hoschulzii	119.17		90% of G. ferrolensis Foram Zone (Bergen & Sikora), which is 90% between LAD of L. cabri and FAD of G. algeriana; which is about 2 myr higher than what would be implied by Leg 207 table relative placement.  Not on SEPM chart.  NOTE: LAD is just below (0.2 myr) the top of N. nolani Z., D. nodosocostatum s.z. (based on Leg 171 projected 114.2 Ma relative to 114.0 for FAD H. albiensis).   But, LAD on Leg 207 table was assigned as 3/4th up in D. furcata zone (based on projected placement of 117.3 Ma in Leg 207 table)
	Nannoconus steinmannii	122.31		20% up in D. grandis s.z., which would be 60% up in D. deshayesi Zone.  SEPM'98 had assigned as Top of I. giraudi Z.
	Retecapsa angustiforata	123.35		60% up in D. weissi Zone
	Conusphaera rothii	123.76		20% up in D. weissi (J. Bergen assignment).  SEPM'98 has assigned as Probably equivalent to C. mexicana of some nannofossil wokers (J. Bergen, pers. commu., 2005).  Not on SEPM chart; but Leg 207 table implies an age about 0.5 myr older than FAD of E. floralis.
	NANNOCONID CRISIS	124.69		Uncertain calibration.  SEPM'98 has assigned as Just below (0.1 myr) the FAD of R. angustus
	Calcicalathina oblongata	129.19		35% up in Chron M3r (merger of Bralower's and Bergen's placements).  SEPM'98 had assigned as Base of Chron M3r; but LAD was middle of H. caillaudianus Z. in France.
	Lithraphidites bollii	130.99		Middle of Chron M5r [Bralower].  SEPM'98 had assigned LAD as 6/10 up in P. angulicostata auct. Z.
	Speetonia colligata	132.75		70% up in P. ligatus Zone.  SEPM'98 had also assigned LAD as 7/10 up in P. ligatus Z.
	Crucielipsis cuvillieri 	133.27		90% up in S. sayni Zone.  SEPM'98 had assigned as Middle of S.sayni Z.
	Tubodiscus verenae	133.53	dashed	DASH approximation in mid-Hauterivian (arbitrarily put at middle of S. sayni Zone here to avoid overlap with NC5).  Defines base of NC4, but difficult to pinpoint LAD.  SEPM'98 had assigned as Middle of H. trinodosum s.z. (of N. pachydicranus Zone).  With revised zonal scheme, this essentially is base of C. furcillata subzone.
	Eiffellithus striatus	133.85		Base of S. sayni Zone.
	Eiffellithus windii	136.12		Middle of A. radiatus Zone
	Rucinolithus wisei	138.44		40% up in S. verrucosum Zone (Bergen, but assumed to be former S.verr. version, hence including N. peregrinus s.z.)
	Eiffellithus primus, C. deflanderi	139.35		Middle of B. campylotoxus Zone.
	Haqius noelae	145.14		10% up in Chron M17r (Bralower); but Bergen correlated to coeval with FAD of his N. steinmannii or about 50% up in B. jacobi s.z. (used here).  SEPM'98 had assigned FAD as 1/4 up in B. jacobi Z., P. grandis s.z.
	Polycostella beckmanni	145.51		50% up in Chron M19n.2n.  On SEPM1998 chart, LAD is 55% up in Durangites Z.
	Stephanolithion bigotii bigotii	148.99		LAD is 95% up in Chron M22n.  On SEPM1998 chart, LAD is 80% up in Semiformiceras semiforme Z.
	Triscitum beaminsterense	153.23		Middle of C. divisum Zone. 
	Crepidolithus perforata	154.14		LAD is base of A. hypselocyclum Zone.  Formerly "M. perforata".  On SEPM1998 chart, LAD is 70% up in S. platynota Z.
	Lotharingius crucicentralis	158.79		LAD is 70% up in P. plicatilis Zone.  On SEPM1998 chart, LAD is base of P. (D.) antecedens subzone of P. plicatilis Zone.
	Stephanolithion bigoti maximum	159.61		LAD is base of P. pllicatilis Zone.  On SEPM1998 chart, LAD is 20% up in C. praecordatum s.z. of Q. mariae Zone
	Ansulasphaera helvetica	161.69		LAD is 40% up in L. lamberti.  On SEPM1998 chart, LAD is 25% up in Q. (L.) lamberti zone.
	Stephanolithion hexum	162.28		DASH -- LAD is 20% up in P. athleta Zone.  On SEPM1998 chart, LAD is base of R. anceps Zone.
	Lotharingius velatus	163.92		LAD at 30% up in M. gracilis Zone.  DTS1995 had this FAD is 20% up in M. (D.) gracilis zone, but not in SEPM chart.
	Stephanolithion speciosum	164.23		LAD at base of M. gracilis Zone.  On SEPM1998 chart, LAD is 55% up in B. (K.) bullatus Zone.
	Carinolithus magharensis	167.97		DASH at middle of P. parkinsoni (according to Erba).  But, SE France has reported LAD in middle of S. subfurcatum (middle of S. niortense zone).  On SEPM1998 chart, LAD is 45% up in P. densicostata s.z.  of P. parkinsoni Z., 
	Discorhabdus striatus (acme)	169.05		Top of Acme is 75% up in S. subfurcatum (S. niortense) Zone.  Also known as Biscutum striatum.  DTS1995 had the LAD at 35% up in schroederi s.z. of S. niortense zone; but not on the SEPM chart.
	Carinolithus superbus	169.25		Middle of S. subfurcatum (S. niortense) Zone.  J. Bergen's sections suggest a lower LAD at 25% up in this zone.  DTS1995 had this LAD at 50% up in G. baculata s.z. of S. niortense zone; but not in the SEPM chart.
	Biscutum constans	170.23		Base of S. humphriesianum zone.  Also called D. constans.  On SEPM1998 chart, LAD is base of hebridica s.z. of S. propinquans zone.
	Triscutum sullivani	170.42		LAD in middle of Sauzei Zone (now middle of S. propinguans Zone).  DTS1995 had this LAD at 30% up in hebridica s.z. of S. propinquans zone, but not the SEPM chart.
	Triscutum tiziense	171.21		Base of W. laeviuscula Zone.  On SEPM1998 chart, LAD is 70% up in H.(H.) discites s.z. of the H. discites zone.
	Bussonius prinsii	172.49		LAD is Base of G. concavum Zone.  On SEPM1998 chart, LAD is the base of G. formosus s.z. of the G. concavum zone.
	Axopodorhabdus atavus	175.16		J. Bergen will revisit the calibration.  On SEPM1998 chart, LAD is 50% up in L. opalinum s.z. of L. opalinum zone .
	Crepidolithus cavus	176.03		J. Bergen will revisit the calibration.  DTS1995 had this LAD is 15% up in fluitans s.z. of P. aalensis zone,  but not in the SEPM chart.
	C. cantaluppii	177.27		DASH at 30% up in "Menegini Zone" (= D. pseudoradiosa Zone).  On SEPM1998 chart, LAD is 80% up in levesquei s.z. of D. pseudoradiosa zone.
	Lotharingius hauffii (acme)	180.50		Base G. thouarsense Zone.  On SEPM1998 chart, LAD is the base of G. thouarsense zone.
	Orthogonoides hamiltoniae	181.28		95% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is the base of sublevisoni s.z. of H. Bifrons zone.
	Palaeopontosphaera grande	181.50		80% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Similiscutum finchii	181.80		60% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 70% up in H. falciferum s.z. of H. falciferum zone.
	Calcivascularis jansae	182.63		5% up in H. serpentinum Zone.  On SEPM1998 chart, LAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Crucirhabdus primulus	182.88		40% up in D. tenuicostatum Zone.  DTS1995 had this LAD at base of D. tenuicostatum s.z. of D. (O.) tenuicostatum zone, but not the SEPM chart.
	Parhabdolithus liasicus liasicus	185.44		55% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  DTS1995 had this LAD at 50% up in cornacaldense s.z. of lavinianum, but not in the SEPM chart.
	Crepidolithus pliensbachensis	188.14		40% up in T. ibex.  On SEPM1998 chart, LAD is 40% up in beirense s.z. of T. ibex.
	Prinsiosphaera triassica, Eoconusphaera ziambachensis, Crucirhabdus minutus, Archaeozygodiscus koessenensis 	199.60
	Orthopithonella misurinae,  Obliquipithonella prasina, Carnicalyxia tabellata, Cassianospica curvata	216.53
FAD
	Emiliania huxleyi (acme in Mediterreanean)	0.05
	Gephyrocapsa caribbeanica to E. huxleyi shift of dominance  [in "transitional" waters]	0.07		Same chron-age scaling as Berggren et al. (1995) = O-18 stage 4; 0.075 Ma; [b,d] = C1n.91
	Gephyrocapsa caribbeanica to E. huxleyi shift of dominance  [in tropical and subtropical waters]	0.09		Same chron-age scaling as Berggren et al. (1995) = O-18 stages 5a-5b; 0.09 Ma; [b,d] = C1n.88
	Emiliania huxleyi	0.29		Astronomically tuned in Pacific (ODP Legs 111 & 138) and Atlantic (Leg 154, Sites 925 & 926) -- Refs 1, 2, 9 & 10; in GTS2004 Neogene nannofossil appendix.  Age is recorded slightly younger (0.27 myr) in Mediterranean (refs. 17 & 18).  Berggren et al. (1995) placed similarly= O-18 stage 8; 0.26 Ma; [b,d] = C1n.67.
	Gephyrocapsa sp.3	1.02		Astronomically tuned in Pacific (ODP Legs 111 & 138) -- Refs 1-5; in GTS2004 Neogene nannofossil appendix.  FAD is recorded slightly later (0.97 Ma) in Mediterranean (refs. 17, 18 & 21).  Berggren et al. (1995) have same = O-18 stage 25 (above Jaramillo); 0.96 Ma; [b] = C1r.1r.15. 
	medium (over 4 microns) Gephyrocapsa spp. reentrance (reemG event)	1.04		Astronomically tuned in Pacific (ODP Legs 111 & 138) -- Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  FAD recorded slightly later (1.01 Ma) at Atlantic Leg 154, Sites 925 & 926, and later (0.96 Ma) in Mediterranean (refs. 11, 17-19 & 21).  Berggren et al. (1995) have same = O-18 stage 29 (within Jaramillo); 1.03 Ma; [a] = C1r.1n.5.
	Reticulofenestra asanoi (common)	1.14		Astronomically tuned in Atlantic Leg 154, Sites 925 & 926 -- Refs 9-11; in GTS2004 Neogene nannofossil appendix.  FAD is recorded slightly later (1.08 Ma) in Mediterranean (refs. 18, 19 & 21).
	small Gephyrocapsa spp. dominance	1.24		Astronomically tuned in Pacific (ODP Legs 111 & 138) --Refs 1-5, 9-11; in GTS2004 Neogene nannofossil appendix.  
	large (over 5.5 microns) Gephyrocapsa spp.	1.62		Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.  This FAD is recorded slightly later (1.46 and 1.56 Ma) in Pacific ODP Legs 111 & 138 (Refs 1-5) and in Atlantic Leg 154, Sites 925 & 926 (Refs 9-11), respectively.  Berggren et al. (1995) assign FAD slightly younger, as upper O-18 stage 48 [e]; 1.46-1.48 Ma; [a] = C1r.3r.55.
	medium (over 4 microns) Gephyrocapsa spp. (=bmG event)	1.73		Astronomically tuned in eastern Mediterranean -- Refs 11, 22-24; in GTS2004 Neogene nannofossil appendix.  This FAD is recorded slightly later (1.67 and 1.69 Ma) in Pacific ODP Legs 111 & 138 (Refs 1-5) and in Atlantic Leg 154, Sites 925 & 926 (Refs 9-11), respectively.  Pleistocene Nanno FAD of this Gephyrocapsa species was called "medium-o" by Berggren (early version of 1995 GSA paper) and "oceanica s.l." by Leg 145 -- both lists give "Rio et al, in press" as source, and have same age.  Berggren et al. (1995) assign as transition O-18 stages59/60 [e] (above top of Olduvai); 1.67-1.70 Ma; [a] = C1r.3r.15.
	Discoaster triradiatus -- (acme)	2.22		Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix.  This Acme onset is recorded slightly later (2.14 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs 9 & 10).  Pliocene nannofossil 'Discoaster triradiatus' (onset acme) occurs at 2.25 Ma in Mediterranean [ref. c], in Berggren et al. (1995) compilation = early Matuyama; 2.18 Ma [g]; but 2.25 in Medit. [d] = C2r.2r.6.
	Discoaster asymmetricus (FCO)	4.13		Lourens et al (GTS2004) referred to this FCO as a "subbottom".  Astronomically tuned in Pacific (ODP Legs 111 and 138) and in eastern Mediterranean (as 4.12 Ma) -- Refs 5-7, 22 & 25; in GTS2004 Neogene nannofossil appendix.  Pliocene nannofossil 'Discoaster asymmetricus' (FCO) occurs in upper Gilbert (4.15 Ma) in Mediterranean [ref. d], in Berggren et al.'s (1995) compilation =  near top of Cochiti; 4.2 Ma; [d] = C2n.1n.8.
	Reticulofenestra pseudoumbilica, Discoaster ovata	4.91		Lourens et al. (GTS2004 table) call both FADs in Mediterranean as a "subbottoms" in their calibration.  Astronomically tuned in eastern Mediterranean -- Refs 22 & 25; in GTS2004 Neogene nannofossil appendix.
	Ceratolithus rugosus	5.12		Astronomically tuned in Pacific (ODP Legs 111 and 138) -- Refs 5-8; in GTS2004 Neogene nannofossil appendix. This FAD is reported later (5.05 Ma) in Atlantic Leg 154, Sites 925 & 926 (refs. 13 & 14).  in Berggren et al.'s (1995) compilation => diachronous among regions -- Pliocene nannofossil Cerotolithus rugosus (FAD) occurs near top of Nunivak (4.5 Ma) in Mediterranean [ref. c,d].  Berggren et al. (1995) place within Thvera; 5.0-5.23 Ma; [c,i] = C3n.4n.5.
	Ceratolithus larrymayeri (sp.1)	5.34		Tabulated in Lourens et al (2004), and would be a regional marker for base of Pliocene.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix
	Ceratolithus acutus	5.35		Base C. acutus is a marker for base of Pliocene; not tabulated in Berggren et al. (1995).   Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  This FAD is calibrated at essentially same age (5.32 Ma) in Pacific (ODP Legs 111 & 138; refs. 5-8).  Berggren et al. (1995) assigned to uppermost part of C3r in Gilbert; 5.34 Ma [j,k] or 5.68 Ma [i] = C3r.85.
	Nicklithus amplificus	6.91		Genus for amplificus was "Amaurolithus" in Berggren's table; and had been used for a Subzone NN11c (and "CN9c") of their zonal scheme.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.  This FAD occurs later (6.68 Ma) in eastern Mediterranean (refs. 27-29).  Berggren et al. (1995) placed this FAD slightly higher (by 0.3 myr) -- base C3An.2n; 6.6 Ma [l,k,y]; or 6.02 [a] or 6.48 Ma [h] = base C3An.
	Amaurolithus primus	7.42		LAD of Amaurolithus primus is also LAD of genus Amaurolithus.  Astronomically tuned in eastern Mediterranean -- Refs 28 & 30-35; in GTS2004 Neogene nannofossil appendix.    This FAD is recorded slightly later (7.36 Ma) in Atlantic (Leg 154, Sites 925 & 926; refs 10 & 13).  Berggren et al. (1995) summarized: C3Br.2r; 7.2 Ma [l,k.y]; or 6.70 [a], 6.42 [f] or 6.80 Ma [h] = C3Br.2r.7.
	Discoaster surculus FCO	7.79		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.
	Discoaster quinqueramus	8.11		From Leg 145 compilation; not in Aubry's synthesis in Berggren et al. (1995) = C4; 7.46 Ma [b] or 8.12 Ma [h] = base C4n.2n (for older FAD estimate).
	Discoaster berggrenii	8.29		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 13; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had this FAD as slightly older by 0.3 myr = lower C4r; 8.6 Ma [l,k,y]; or C4; 8.00 [a], 7.5 Ma [g], or 8.16 [h] = C4r.2r.2.
	Discoaster loeblichii	8.77		Same chron-age scaling as Berggren et al. (1995) = base C4r; 8.7 Ma [l,k,y] = base C4r.
	Reticulofenestera pseudoumbilicus FCO	8.79		Lourens et al (2004) tabulate this "paracme" event with astronomical tuning in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Nearly simultaneous (8.71 Ma) in eastern Mediterranean (refs. 28, 33 & 35), where is defines base of MNN11.  Berggren et al. (1995) did not include it.
	Discoaster pentaradiatus (FCO)	9.37		Astronomically tuned in eastern Mediterranean -- Refs 28, 33 & 35; in GTS2004 Neogene nannofossil appendix.  LAD may be 0.3 m.y. earlier in Indo-Pacific [l,k,y].
	Minylitha convallis	9.75		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs slightly younger (9.61 Ma) in eastern Mediterranean (refs. 28, 33 & 35).  Berggren et al. (1995) place as C4Ar.2r.5, 9.5 Ma [l,y], or C4A, 8.9 Ma [a]; near Discoaster hamatus LAD, and indicate that this FAD in Pacific may be 0.2 m.y. later [ref. l,k,y] = C4Ar.2r.3.
	Discoaster bellus	10.40		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Discoaster neohamatus	10.52		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs much younger (9.87 Ma) in eastern Mediterranean (refs. 35 & 36).  Leg 145 compilation (not in Berggren et al., 1995) had placed in Chron C5, 8.96 Ma [b] or 9.62 [h] = base C4Ar.3r; which had put that FAD much higher by 0.8 myr.
	Discoaster hamatus	10.55		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs much younger (10.18 Ma) in eastern Mediterranean (refs. 35 & 36).  Berggren et al. (1995) note that this is "Controversial" and inconsistent datum, with reported ages of C5r.2r; 11.2 [l,u]; or C5;10.5 [b] or 10.9 [h]; therefore C5r.2r.7 (11.2 myr) was used as lowest FAD in a previous version of this chart.  More checks on this calibration is needed.
	Helicosphaera stalis (FCO)	10.71		Astronomically tuned in eastern Mediterranean -- Refs 35 & 36; in GTS2004 Neogene nannofossil appendix
	Discoaster brouweri	10.76		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs simultaneously (10.73 Ma) in eastern Mediterranean (refs. 35 & 36).
	Catinaster calyculus	10.79		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  Berggren et al (1995) note that correlations are disputed: C5n.2n, 10.7 Ma, [l,t,k,y]; or C5, 10.0 Ma [c] or 10.5 [h]; therefore, C5n.2n.2 seems best chron assignment.
	Catinaster coalitus	10.89		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 13 & 14; in GTS2004 Neogene nannofossil appendix.  FAD occurs slightly later (10.73 Ma) in eastern Mediterranean (refs. 35 & 36).  Very poorly constrained age, and Atlantic may be 0.4 m.y. before Pacific -- Berggren et al. (1995) give C5r.2r (Atl.); 11.3 Ma [l,h,t] or 11.1 Ma [b]; therefore an older placement (by 0.4 myr) of C5r.2r.5 was used on previous versions of this chart.
	Discoaster kugleri	11.90		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 14 & 15; in GTS2004 Neogene nannofossil appendix;  and simultaneous (11.90 Ma) in eastern Mediterranean (refs 35 & 36).  This "FCO" of Lourens et al (2004) seems to correspond in calibration to the "FAD" of Berggren et al (1995), which they summarized as C5r.3r; 11.8 Ma [l,r]; or C5A; 12.2 [b],12.7 [d],12.8 [h] or 12.0 Ma [i] = C5r.3r.3.
	Calcidiscus macintyrei (FCO)	12.46		FCO is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 15 & 16; in GTS2004 Neogene nannofossil appendix
	Reticulofenestra pseudoumbilicus	12.82		Assumed same chron-age scaling as Leg Berggren et al (1995) = C5A ; 12.7 [d] = base C5Ar.2r
	Triquetrorhabdulus rugosus	13.28		Miocene Nanno 'Triquetrorhabdulus rugosus FAD' is estimated as 12.5 Ma in Leg 145 table, but 13.2 Ma  (0.7 m.y. older) in Aubry's synthesis (in Berggren et al., 1995), based on Hole 608 (ref. r); which is used here = C5AAn;13.2 Ma [l,r] or C5A ;12.5 Ma [d] = C5AAr.5.
	Calcidiscus macintyrei	13.37		From Leg 145 compilation; not in Lourens et al (2004) synthesis = base C5An [h] = base C5An.
	Discoaster signus	15.85		Assumed same chron-age scaling as Leg 145 synthesis (not in Aubry's synthesis in Berggren et al., 1995) = C5B; same as Top-Acme of D.defl. [a] = C5Br.15.
	Sphenolithus heteromorphus	17.71		Lourens et al (2004) assign this event as a first-common occurrence (FCO) that is astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Refs 10 & 15; in GTS2004 Neogene nannofossil appendix.  However, based on coincidence with earlier calibrations, this is probably essentially the FAD as compiled by Berggren et al (1995) = lower C5D; 18.2 Ma [l,r; b,h,i] = C5Dr.1.
	Sphenolithus belemnos	19.03		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15; in GTS2004 Neogene nannofossil appendix.  Berggren et al. (1995) had similar assignment -- C6n; 19.2 Ma [d,h; l,r,t] or 19.7 [i] = C6n.9.
	Helicosphaera ampliaperta	20.43		Suggested as primary marker for base of Burdigalian.  Genus spelled as "Helicopontosphaera" in Lourens et al, 2004 table.  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix.
	Helicosphaera carteri (FCO)	22.03		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix
	Sphenolithus disbelemnos	22.76		Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 15 & 41; in GTS2004 Neogene nannofossil appendix.  This species was not recognized in other schemes.
	Discoaster druggi	22.82		Astronomically tuned in eastern Mediterranean (based on projecting astronomical tuning of long-period minima  to base-Miocene; Ref. 40; in GTS2004 Neogene nannofossil appendix), which is consistent with Leg 154.  However, smaller forms appear earlier, at end of Oligocene? (J. Bergen and E. de Kaenel, pers. commun., 2005).  Miocene Nanno 'Discoaster druggi' FAD has been assigned to C6Cn in Leg 145 compilation [ref. b,h], but Aubry (in Berggren et al., 1995) assigns 0.5 m.y. higher (in C6Br); so earlier chart had used C6Br; 23.2 Ma; [l,o] = C6Br.5.
	Sphenolithus delphix	23.21		Oligocene Nanno 'Spenolithus delphix FAD' may be similar to its 'onset of acme' (Leg 145 table).  Astronomically tuned in Atlantic (Leg 154, Sites 925 & 926) -- Ref. 10 & 15; in GTS2004 Neogene nannofossil appendix.  This FAD placement is nearly 1 myr higher than Leg 145 and Berggren et al. (1995) = upper C6Cr; 24.3 Ma; [a,f,t] = C6Cr.7.
	Triquetrorhabdulus carinatus (acme)	25.49		Same chron-age scaling as Leg 145; [not used by Aubry in Berggren et al. (1995)] = base C8n.1r; 26.0 Ma; [a,f] = base C8n.1r.
	Sphenolithus umbrellus	27.27		Scaling by Berggren et al. (1995); revised by Leg 145 = C9n; 26.3 Ma; [j,t] = C8n.2n.5.
	Sphenolithus ciperoensis -> S. distentus (abundance shift)	28.27		Same chron-age scaling as Leg 145 [ not used by Aubry in Berggren et al. (1995)] -- upper C10n; 28.3 Ma; [a,f] = C10n.1n.7.
	Sphenolithus ciperoensis	30.04		Oligocene Nanno 'Sphenolithus ciperoensis FAD' is assigned by Aubry (in Berggren et al., 1995) to Subchron C11n.2n, implying an age of 29.9 Ma.  This is about 1.3 m.y. older than estimate in Leg 145 table.  Used same chron-age scaling as Berggren et al. (1995) -- C11n.2n; 29.9 Ma; [j;a,b] = C11n.2n.5.
	Sphenolithus distentus	33.27		Diachronous -- Oligocene Nanno 'Sphenolithus distentus FAD' is "a very inconsistent datum which may occur as low as Nanno Zone NP21 ... or as high as in Zone NP23" (Aubry, in Berggren et al., 1995).  Age estimates in her table range from 31.5 to 33.1 Ma; and the oldest age (33.1 Ma) is used here.  This is approx. 1 m.y. older than the Leg 145 table.  Oldest FAD implies "CP18" begins before "CP17"!  Youngest FAD is ~31.5 Ma  Scaling used here is C12r; 33.1 Ma; [j,y,ee;a,b] = base C12r.
	Clausicoccus subdistichus (base of acme)	33.50		Oligocene Nanno 'Clausicoccus subdistichus' (Aubry, in Berggren et al., 1995) has alternate names of 'Ericsonia subdisticha' (Leg 145 table) and 'Ericsonia obrata' (Massignano section, Premoli Silva et al., 1988).  Same chron-age scaling as Berggren et al. (1995) = lower C13nr; 33.3 Ma; [z] = C13n.5.
	Isthmolithus recurvus	35.17		Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.2n; 36.0 Ma; [k,ll,oo] = C15r.65.
	Reticulofenestra oamaruensis	35.49		Restricted to high latitudes.  Same chron-age scaling as Berggren et al. (1995); revised by Leg 145 = C16n.1n; 35.4 Ma; [kk] = C16n.1n.5.
	Chiasmolithus oamaruensis	36.84		Same chron-age scaling as Berggren et al. (1995) = C17n.1n; 37 Ma; [a,b,cc] = C17n.1n.55.
	Reticulofenestra bisecta	37.69		Same chron-age scaling as Berggren et al. (1995) = C17n.3n; 38 Ma; [k,z,cc] = C17n.3n.
	Reticulofenestra hesslandii	39.61		Leg 145 [not used by Aubry in Berggren et al. (1995)] = uppermost C18r; 40.4 Ma; [a,d] = C18r.85.
	Reticulofenestra reticulata	41.13		Same chron-age scaling as Berggren et al. (1995) = mid C19r; 42 Ma; [k,dd,gg,ii] = C19r.5.
	Reticulofenestra umbilicus (>14 _m)	41.22		Eocene Nanno 'R. umbilica' FAD is latitude dependent; and occurs as early as basal C20r in Contessa section (Italy).  Used same chron-age scaling as Berggren et al. (1995) = mid C19r; 42.2 Ma; [a,d] = C19r.4.
	Reticulofenestra umbilicus	42.66		Same chron-age scaling as Berggren et al. (1995) = basal C20n; 43.7 Ma; [k,d,u,w] = C20n.1.
	Chiasmolithus gigas	45.35		Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = base C20r; 46.1 Ma; [a,b,n,mm] = base C20r.
	Nannotetrina fulgens	46.57		Same chron-age scaling as Berggren et al. (1995) = mid C21n; 47.3 Ma; [a,b,c,u] = C21n.35.
	Nannotetrina spp.	47.14		Leg 145 [not used by Aubry in Berggren et al. (1995)] = base C21n; 47.8 Ma; [a,c] = C21n.05.
	Blackites inflatus	47.92	dashed	Poor calibration.  Used same chron-age scaling as Berggren et al. (1995) = upper C21r; 48.5 Ma; [b,u] = C21r.5.
	Discoaster sublodoensis	49.43		Same chron-age scaling as Berggren et al. (1995) = lower C22n; 49.7 Ma; [a,b,c,u] = base C22n.
	Discoaster lodoensis	53.23		Same chron-age scaling as Berggren et al. (1995) = C24n.2r; 52.85 Ma; [a,b,c,n] = C24n.2r.5.
	Sphenolithus radians	53.76		Leg 145 [not used by Aubry in Berggren et al. (1995)] = base C24n.; 53.2 Ma; [a,c] = C24n.3n.1.
	Tribrachiatus orthostylus	54.15		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.64 Ma; [i,j] = C24r.88.
	Tribrachiatus contortus  (Morphotype B)	54.46		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.93 Ma; [i,j] = C24r.77.
	Discoaster diastypus	54.52		No firm magnetochronologic calibration (ref.k).  Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 53.9 Ma; [a,c] = C24r.75.
	Rhomboaster spp.	54.66		Leg 145 [not used by Aubry in Berggren et al. (1995)] = upper C24r; 54.0 Ma; [a,c] = C24r.7
	Tribrachiatus contortus  (Morphotype A)	54.95		Used relative chron-age scaling as Berggren et al. (1995) = upper C24r; 54.37 Ma; [i,j] = C24r.6.
	Tribrachiatus bramlettei	55.67		Paleocene Nannofossil Zone NP10 base (FAD of T. bramlettei) is a marker for the Paleocene/Eocene boundary.  Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55 Ma; [h,i] = C24r.35
	Rhomboaster cuspis	55.81		Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.16 Ma; [h,i] = C24r.3
	Cruciplacolithus eodelus	56.24		Also known as Campylosphaera eodela.  FAD of C.eodelus closely precedes C-13 excursion in many DSDP sites.  Used relative chron-age scaling as Berggren et al. (1995) = lower C24r; 55.5 Ma; [a,b,n] = C24r.15.   NOTE: Paleocene Nanno 'C. eodela' FAD listed by Leg 145 as "58.2 Ma" in Berggren et al. (1985), then converted; but I could not find this event given in Berggren et al. (1985) tables.
	Discoaster multiradiatus	56.97		Same chron-age scaling as Berggren et al. (1995) = mid C25n; 56.2 Ma; [a,c,p] = C25n.4.
	Discoaster okadai	57.60		Same chron-age scaling as Berggren et al. (1995) = upper mid-C25r; 56.8 Ma; [a,c,j] = C25n.65.
	Discoaster nobilis	57.66		Same chron-age scaling as Berggren et al. (1995) = upper mid-C25r; 56.9 Ma; [a,c,j] = C25r.6.
	Heliolithus riedelii	58.14		Paleocene Nanno 'H. riedeli' FAD age estimated from it's placement 0.6 m.y. before FAD of D. nobilis in Berggren et al. (1985)  table.  Chron-age scaling = lower C25r; 57.3 Ma; [j] = C25r.2
	Discoaster mohleri	58.32		Same chron-age scaling as Berggren et al. (1995) = basal C25r; 57.5 Ma; [a,j] = C25r.05.
	Sphenolithus anarrhopus	59.17		Same chron-age scaling as Berggren et al. (1995) = uppermost C26r; 58.4 Ma [j] = C26r.85.
	Heliolithus kleinpelli	59.17		Paleocene Nanno 'H. kleinpelli' FAD placed "slightly above mid-point of C26r", or 0.6 m.y. older than LAD 'D. danicus', by Berggren et al. (1985), but Leg 145 table has these as coeval events (citing Backman, 1986).  Same chron-age scaling as Berggren et al. (1995) = uppermost C26r;58.4 Ma;[a,c,j] = C26r.85.
	Heliiolithus cantabriae	59.76		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.3 Ma; [a,c] = C26r.65.
	Chiamolithus consuetus	60.48		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [j] = C26r.4.
	Fasciculithus tympaniformis	60.48		Same chron-age scaling as Berggren et al. (1995) = mid C26r; 59.7 Ma; [j] = C26r.4.  Coeval with FAD Neochiastozygus perfectus (North Sea) -- Ref.g.
	Fasciculithus ulii	60.69		Same chron-age scaling as Berggren et al. (1995) = lower C26r; 59.9 Ma; [j] = C26r.33.
	Fasciculithus spp.	60.78		Same chron-age scaling as Berggren et al. (1995) = lower C26r; 60.6 Ma; [a,c] = C26r.3.  Approx. FAD of Chiasmolithus bidens followed by FAD of Sphenolithus primus (North Sea) -- Ref.g.
	Sphenolithus primus	61.36		Same chron-age scaling as Berggren et al. (1995) = lowermost C26r; 60.6 Ma; [j] = C26r.1.  Approx. FAD of Neochiastozygus saepes in high latitudes -- Ref.g.
	Chiasmolithus bidens	61.45		Same chron-age scaling as Berggren et al. (1995) = lowermost C26r; 60.7 Ma; [j] = C26r.07.
	Sphenolithus spp.	61.50		Same chron-age scaling as Berggren et al. (1995) = basal C26r; 61.4 Ma; [a,c] = C26r.05.
	Ellipsolithus macellus	62.82		Paleocene Nanno 'E. macellus' FAD assigned to lower C27r by Berggren et al. (1985; 1995); but Leg 145 places higher (basal C26r) by about 1.6 m.y., citing Backman (1986).  Berggren et al. indicate that this is a solution susceptible taxon; so a lower FAD may be more appropriate?  I used Berggren's (Aubrey's) placement = lower C25r; 62.2 Ma; [j] = C27r.25.  Defines NP4 base.
	Chiasmolithus danicus	64.28		Same chron-age scaling as Berggren et al. (1995) = mid C28r; 63.8 Ma; [a,b,j] = C28r.5.
	Cruciplacolithus tenuis	64.91		Defines NP2 base.  Same chron-age scaling as Berggren et al. (1995) = lower C29n; 64.5 Ma; [a,b,j] = C29n.3.
	Cruciplacolithus primus	65.19		Same chron-age scaling as Berggren et al. (1995) = uppermost C29r; 64.8 Ma; [j] = C29r.9.
	Hornibrookina teuriensis	65.27		Same chron-age scaling as Berggren et al. (1995) = upper C29r; 64.9 Ma; [j] = C29r.8.
	Biantholithus sparsus	65.50		Same chron-age scaling as Berggren et al. (1995) = upper C29r; 65.0 Ma; [j] = C29r.7.
	Micula prinsii	65.90		Leg 207 assigned as 0.4 myr before end-Cretaceous.  Diachronous (p.16, ODP Leg 171B Expl. Notes); with Boreal FAD later than Tethyan (Von Salis, 1998, SEPM chart).  Assigned previously (1998) as simply 1 myr prior to end of Cretaceous (ODP Leg 171B assignment, and average of Tethyan/Boreal of von Salis).
	Cribrosphaerella daniae	66.30		Assigned here as synchronous with N. frequens, following von Salis SEPM98.  Boreal marker, approx. synchronous with FAD of N. frequens in Boreal realm (see Note on N. frequens).
	Nephrolithus frequens (low-lat.)	66.30		Leg 207 assigned as 0.8 myr before end-Cretaceous (used here) => closer to Boreal placement on SEPM98.  Boreal FAD is significantly (~1 myr) younger, as suggested on SEPM98 chart.  Low-lat shown on SEPM98 as mid-Chron C31n; but Leg 171B places ~1 myr younger.
	Cribrocorona gallica	68.73		SEPM98 shows as synchronous FAD with M. murus
	Micula murus	68.73	dashed	DASH:  Leg 207 assigned as 1.2 myr before end-Cretaceous (arbitrary equal-spacing of FADs of M. murus, N. frequens, and M. prinsii); ;but SEPM98 placement used in GTS04 and here (base Chron C31n).  DASHED -- Diachronous (p.16, ODP Leg 171B Expl. Notes). 
	Lithraphidites quadratus	68.98		SEPM98 shows as 0.1 myr after M. murus (used here).  However, GTS04 diagram (Fig.19.1) places Before (mid-way between M. murus and LAD of R. levis) -- used here for "GTS04".
	Uniplanarius trifidum	76.38		Also known as Quadrum trifidum.  Bralower et al. (1995) suggest this is coeval with FAD of foraminifer G. calcarata (about 0.8 myr younger), which may indicate uncertainty in Campanian inter-correlations.  SEPM'98 had assigned FAD as base of Late Campanian (base D. nebrascense zone).
	Uniplanarius sissinghii	77.38		Also known as Quadrum sissinghii.  Seems an arbitrary 1 myr below FAD of U. trifidum in Leg 171/207 tables.
	Ceratolithoides aculeus	78.92		FAD (from ODP 171/207) coincides with mid-B. perplexus (late) zone.
	Misceomarginatus pleniporus	80.00		Leg 207 listed (but not B. hayii LAD), and is a Boreal marker as "base of UC15".  Seems, from Leg 207 relative placement, to be essentially coeval with LAD of B. hayii.
	Ceratolithoides verbeekii	82.10		SEPM'98 had assigned FAD is ~0.1 myr above base of S.hippocrepi II zone in SEPM.
	Aspidolithus parcus constrictus	82.55		Also called "Broinsonia parca constricta" in some schemes.  FAD assigned here as middle of S. hippocrepis I zone (Leg 207 approximate age coincidence, but they essentially placed it an even 1 myr above FAD of A. parcus).
	Aspidolithus parcus parcus	83.53		FAD placed at base of Campanian.  Also called "Broinsonia parca parca" in some schemes.  BUT, base of preceeding A. parcus expansus is probably the one just above the boundary, and parca-parca occurs higher (J. Bergen 2005 pers. Commun.)
	Calculites obscurus	83.99		Leg 207 places at essentially Late/Middle Santonian boundary (base of D. bassleri zone)
	Lucianorhabdus cayeuxii	84.94		Estimates (SEPM, Leg 171/207) seem to converge on placement at Middle/Early Santonian boundary (base of C. vermiformis zone)
	Lithastrinus grillii	85.85		SEPM'98 had assigned Same age as FAD of R. anthorphorus
	Reinhardtites anthophorus	85.85		Leg 171B assigns to base of Santonian
	Micula decussata	86.96		Same as "Micula staurophora".  FAD is Late/Middle Coniacian boundary in Leg 171 and Tethyan SEPM column; BUT placed at Middle/Early Coniacian in Boreal SEPM column.  
	Lithastrinus septenarius	88.68		SEPM'98 had assigned as Just below (0.1 myr) the Middle/Early Coniacian boundary in Tethyan column.
	Marthasterites furcatus	89.63		SEPM'98 had assigned FAD as base of S. nigricollensis
	Eiffellithus eximius, Lucianorhabdus maleformis	91.23		SEPM'98 had assigned FADs as middle of P. percarinatus Z.
	Kamptnerius magnificus	92.05	dashed	DASH:  Not in Leg 207 table or SEPM chart; but highlighted by Bralower-Leckie as base of NC14 with assigned age of 91.8 Ma (using Gradstein et al., 1994 scale), which projects as 5% up in C. woollgari Zone.  However, FAD ranges as low as lower-Lower Turonian and as high as lower-Middle Turonian (Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI]
	Quadrum gartneri	92.70	dashed	DASH:  Base of M. nodosoides Zone [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI].  This is higher than the base of Turonian (Leg 171/207 placements) by 0.8 myr.
	Lithraphidites acutus, Microrhabdulus decoratus	95.56		SEPM'98 has assigned both as Middle of A. granerosense zone (used here); but Leg 207 projects age as base of Middle Cenomanian (~1 myr below)
	Corollithion kennedyi	97.93		SEPM'98 assigned FAD as middle of N. americanus Z.
	Eiffellithus turriseiffelii	102.93		Coeval with FAD of foraminifer R. ticinensis (Bralower-Leckie, 1997).  SEPM'98 assigned as Just below (0.15 myr) the base of H. orbignyi subzone.
	Eiffellithus monechiae	106.42		Coeval with FAD of foraminifer B. breggiensis by Bralower-Leckie (but see note on calibration of that datum).  Called E. cf. E. eximius in Bralower-Leckie chart.  Age assigned as 105 Ma in Leg 207 table (note on SEPM chart) => assigned as mid-A. intermedius ammonite subzone
	Axopodorhabdus albianus	109.06		Base of nannofossil A. albianus (called "P." albianus in Grippo et al., in press) is 23.3 long-eccentricity cycles below top of Albian (9.5 myr) => 109.1 Ma.  This projects to base of P. steinmanni ammonite subzone, rather than to 7/10 up in D. mammillatum Z., P. steinmanni s.z. of SEPM98 column.
	Tranolithus orionatus  (=T. phacelosus)	109.77		Nomenclature is "phacelosus" in older literature, but others seem to be using "orionatus" now (e.g., Bralower, Burnett).  Bralower-Leckie charts places this FAD in middle of T. primula Foram Zone, but this would be inconsistent with cycle-scaling of overlying FAD of A. albianus (base of next higher NC zone), therefore placed at 25% up in this table.  SEPM'98 had assigned Tranolithus "phacelosus" FAD as 7/10 up in D. mammillatum Z., P. steinmanni s.z., or at same level as FAD of Axopodo. albianus.
	Cribrosphaerella ehrenbergii	110.35		70% up in Nanno Zone NC8b.  SEPM'98 had assigned FAD as middle of L. tardefurcata Z., L. schrammeni s.z.
	Hayesites albiensis	111.69		Middle of H. planispira Foram Zone (LAD of T. bejaouensis to FAD of T. primula) on Bralower-Leckie (GSA Bull., 1997) chart.  SEPM'98 had assigned FAD as top of N. nolani Z., D. nodosocostatum s.z.
	Prediscosphaera columnata	112.02		Base of nannofossil P. columnata is 30.6 long-eccentricity cycles below top of Albian (12.4 myr) => 112.0 Ma = working definition for base of Albian.  (Primary control on Aptian-Albian interval!)    SEPM'98 has assigned as FAD is 2/10 up in L. tardefurcata Z., L. schrammeni s.z.
	Acaenolithus viriosus	113.00		30% up between Niveau Pacquer and Niveau Jacobi [J.Bergen], therefore about base of H. jacobi Zone.
	N. regularis	114.00		Bergen did not check calibration on this one.  SEPM'98 had assigned FAD as top of N. nolani Z., D. nodosocostatum s.z.
	Rhagodiscus hamptonii	116.00		Was a potential datum for base of "NC7c" zone; but not that widespread (only SE France and India -- [Bown and Kennedy, 2000].  Coeval with LAD of Foram G. algeriana (base of H. trocoidea Foram Zone, called H. gorbachikae Foram Zone on this chart).   [Note (by J. Bergen): Bralower called this base-NC7c marker as Rhagodiscus achylostaurion.  But true R. acy. Ha its FAD in Barremian.]  Not in SEPM chart.  Assigned as base of N. nolani zone (based on projected placement of 115.2 Ma in Leg 207 table)
	Nannoconus truitti (acme)	120.01		Uncertain calibration (J. Bergen); so used SEPM for now =  ~1/3rd up in C. martinoides Zone (= 1/3rd up in E. subnodosocostatum Zone).
	Radiolithus planus	121.36		60% up in T. bowerbanki (D. furcata) Zone.
	Braarudosphaera africana	121.41		55% up in T. bowerbanki (D. furcata) Zone.  SEPM'98 had FAD projected to 4/10 up in D. deshayesi Zone; but with new FAD of E. floralis (control age point in GTS2004), then it is near middle of D. furcata Zone)
	Eprolithus floralis 	121.90		Base E. floralis (base NC7A) fixed at 121.9 Ma  (was 119.0 Ma in Leckie's chart), which sets base of D. furcata Zone.  Time-control point for scaling E. Aptian.  SEPM'98 had FAD projected to 8/10 up in D. forbesi Zone (= D. weisi)  on SEPM chart; but now projects much higher (base of D. furcata Zone)
	Rhagodiscus angustus	122.93		Base of D. deshayesi.  SEPM'98 had assigned FAD assigned as base of D. weissi Zone
	Stoverius achylosum	124.03		80% up in Nanno Zone NC6a (Bralower with Leckie), or in upper-third of OAE1a event.  SEPM'98 has assigned as Same level as FAD B. africana (see its Note).
	Rhagodiscus gallagheri	124.59		40% up in D. tuarkyricus (D. oglanlensis) Zone.   [NOTE: New scaling for E. Aptian makes the interval between FADs of R. angustus and E. floralis as 2 myr, instead of only 1 myr.]  
	Hayesites irregularis 	125.11		Also called Rucinolithus irregularis.   95% up in Chron M1n.   SEPM'98 had assigned as just below (0.1 myr) the base of Aptian.
	Flabellites oblongus (consistent)	126.12		50% up in Chron M1n (Bralower, 1993).  SEPM'98 had assigned FAD is 1/10 up in A. vandenheckii Z.
	Rhadodiscus achlyostaurion 	126.92		Middle of H. feraudianus Zone.  SEPM'98 had assigned as Base of I. giraudi Z.
	Rucinolithus terebrodentarius, Rucinolithus windleyae	132.02		Middle of Chron M7r (J. Bergen), which is slightly lower (0.4 myr) than placement on SEPM chart.  The two taxa are combined by some specialists.  Bralower subdivides NC5 with this datum.  SEPM'98 had assigned as Base of Chron M6r when correlated with Italian magnetostratigraphy or just below the top of B. balearis Z. when correlated with French ammonites (which are similar placements, when using the GTS2004 time scale).
	Zeugrhabdotus scutula	133.69		25% up in S. sayni Zone.
	Lithraphidites bollii	135.47		25% up in C. loryi Zone.  Bralower uses this to subdivide NC4, but it seems that base of NC4 (LAD of T. verenae) is ABOVE this L. bollii FAD.  SEPM'98 had assigned LAD as 2/10 up in C. loryi Z.
	Nannoconus bucheri	136.54	dashed	DASH at SEPM placement = Just below (0.1 myr) the base of Hauterivian
	Eiffellithus striatus	137.27		Middle of H. trinodosum s.z. (of N. pachydicranus Zone).  With revised zonal scheme, this essentially is base of C. furcillata subzone.
	Zeugrhabdotus trivectis	139.27		60% up in B. campylotoxus Zone.
	Eiffellithus windii	139.68		10% up in B. campylotoxus Zone.  SEPM'98 had assigned FAD as 8/10 up in T. pertransiens Zone.  Note:  "SEPM98" age is different than actual SEPM chart, due to change in extent of T. pertransiens.
	Micranthololithus speetonensis, R. dekaenelii	139.77		Base of B. campylotoxus Zone.
	Calcicalathina oblongata	140.24		20% up in Chron M14r.  SEPM'98 had assigned FAD as 7/10 up in T. otopeta Zone, which would shift to Berriasian, due to working-group change in boundary.
	Rucinolithus. wisei	140.80		75% up in T. alpillensis Zone (Bergreen, 1994).  SEPM'98 had assigned FAD as base of B. picteti subzone.
	Tubodiscus verenae	140.95	dashed	DASH at Middle of T. alpillensis (about 2 ammonite zones LOWER than on SEPM chart), poorly constrained.  SEPM'98 had assigned FAD as 4/10 up in S. verrucosum Z.
	Percivalia fenestrata	141.25		Base of T. alpillensis Zone.  This FAD is used to subdivide NC2 (called NK2) to 2a/2b in scheme of Bralower et al. (1995).  SEPM'98 had assigned FAD as base of T. alpillensis subzone
	Rhaqodiscus nebulosus, Diadorhombus rectus	143.32		Rh. nebulosus FAD is Middle of S. subalpina s.z. (Bergen).  Diado. rectus FAD is 60% up in Chron M17r (Bralower).  SEPM'98 had assigned FAD of Rh. nebulosus as base of M. paramimounum subzone.  SEPM'98 had assigned FAD of Diado. rectus is base of S. subalpina subzone
	Assipetra infracretacea	143.92		10% up in Chron M17r (Bralower).  SEPM'98 assigned FAD as 1/4 up in B. jacobi Z., P. grandis s.z.
	Markalius circumradiatus	144.04		Base Chron M17r (Bralower).  SEPM'98 had assigned FAD just above (0.1 myr) the base of B. jacobi Z., P. grandis s.z.
	Retecapsa augustiforata	144.82		Base of P. grandis subzone (J. Bergen's calibration).    SEPM'98 had assigned FAD as 8/10 up in T. occitanica Z., D. dalmasi s.z.  Alternate name was C. angustiforatus.
	Cruciellipsis cuvillieri, Manivitella pemmatoldea	145.03		Middle of Chron M19n.1r.  Therefore, basal Berriasian instead of uppermost Tithonian (using top-Durangites working definition).  On SEPM1998 chart, FADs are 90% up in Durangites Z.
	Nannoconus kamtneri, Nannoconus steinmannii	145.14		30% up in Chron M17r (Bralower), which would be AFTER base of CC1; but Bergen correlated to about 50% up in B. jacobi s.z. (used here).  However, Bergen's version might be N. steinmanii minor of Bralower.  SEPM'98 had assigned FAD as middle of B. jacobi Z., P. grandis s.z.
	Speetonia collgata	145.15		90% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 85% up in Durangites Z.
	Rotelapillus laffittei	145.24		80% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 75% up in Durangites Z.
	Rhagodiscus asper	145.68		30% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 54% up in Durangites Z.  
	Nannoconus globulus	145.80		10% up in Chron M19n.2n.  On SEPM1998 chart, FAD is 51% up in Durangites Z.
	Lithraphidites carniolensis	145.95		Base of Chron M19n.  DTS1995 had this FAD is 30% up in Durangites Z., but not on the SEPM chart.  Ask J. Bergen to check.
	Umbria granulosa minor	146.66		FAD is middle of Chron M20n.  On SEPM1998 chart, FAD is 40% up in P. transitorius Z.one.
	Hexalithus noelae, Helenea chiastia	147.47		FAD are 50% up in Chron M20r.  On SEPM1998 chart, FADs are 40% up in M. ponti/B.peroni Z.
	Nannoconus compressus, Polycostella beckmannii	148.47		FAD are 10% up in Chron M21n.  On SEPM1998 chart, FADs are 45% up in S. admirandum/S. biruncinatum Zone.
	Conusphaera mexicana mexicana	149.31		FAD is 70% up in Chron M22n.  On SEPM1998 chart, FAD is 20% up in Semiformiceras semiforme Z.
	Conusphaera mexicana minor	149.95		FAD is 20% up in Chron M22n
	Zeugrhabdotus embergeri	150.47		mid-Chron M22r (based on Bralower).  DTS1995 had this FAD at 50% up in H. beckeri Z. , but not on SEPM chart.
	Faviconus multicolumnatus	155.50		FAD is 90% up in E. bimammatum Zone.  On SEPM1998 chart, FAD is base of T. hauffianum s.z. (upper E. bimammatum Z.one).
	Helenea quadrata	157.10		FAD is middle of B. bifurcatus Zone.  Former name was "M. quadratus".  On SEPM1998 chart, FAD is 25% up in P.(D.) stenocycloides s.z. (lower P. bifurcatus Zone).
	Stephanolithion bigotii maximum	161.61		FAD is 50% up in L. lamberti.  On SEPM1998 chart, FAD is 60% up in Q. (L.) lamberti zone.
	Stephanolithion bigotii bigotii	163.92		FAD at 30% up in M. gracilis Zone.  On SEPM1998 chart, FAD is the base of the M. (D.) gracilis zone.
	Crepidolithus perforata	164.02		FAD at 20% up in M. gracilis Zone
	Triscutum expansus	164.35		FAD at 75% up in B. bullatus Zone.  DTS1995 had this FAD is 60% up in herveyi Z., terebratus s.z.; but not in SEPM.
	Stephanolithion hexum	165.57		FAD is 25% up in O. aspidooides (which is equivalent to 25% up in H. retrocostatum zone).  On SEPM1998 chart, FAD is base of blanazense subzone of H. retrocostatum Zone.
	Axopodorhabdus rahla	165.72		Base of H. retrocostatum Zone (FAD in Tethyan realm),  DTS1995 had this FAD at 5/10 up in fortecostatum s.z. of C. bremeri Z., ;  but not in SEPM.
	Stephanolithion speciosum octum	168.24		FAD is 5% up in P. parkinsoni (upper Bajocian, rather than lower Bathonian as on SEPM chart).  On SEPM1998 chart, FAD is 20% up in recinctus s.z. of P. aurigerus Zone.
	Ansulasphaera helvetica	168.86		Base of G. garantiana Zone (which is much older than its FAD in Boreal realm as reported by Bown).  DTS1995 had this FAD at base of G. (G.) garantiana zone; but not on the SEPM chart.
	Stephanolithion speciosum speciosum	169.93		Middle of S. humphriesianum zone.  DTS1995 had this FAD at 50% up in S. humpriesianum s.z. of S. humpriesianum zone,  but not in the SEPM chart.
	Ellipsagelosphaera britannica (consistent)	171.40		Base of consistent E. britannica is middle of H. discites Zone.  On SEPM1998 chart, FAD is 30% up in the G. formosus s.z. of the G. concavum zone.
	P. grassei	171.60		On SEPM1998 chart, FAD is the base of H. (H.) discites Zone.
	Ellipsagelosphaera britannica (rare)	171.78		Base of Rare for E. britannica is 80% up in G. concavum Zone.  On SEPM1998 chart, FAD is 30% up in the G. formosus s.z. of the G. concavum zone.
	C. margarelii	173.11	dashed	DASH - 30% up in B. bradfordensis Zone (Aalenian, instead of in Toarcian on SEPM chart).  De Kaenel and Erba put this FAD much higher -- up to base of Bajocian!  On SEPM1998 chart, FAD is 20% up in walkeri s.z. H. (H.) discites zone
	Pseudoconus enigma	173.38	dashed	DASH -- Estimated as base of B. bradfordensis Zone.  DTS1995 had this FAD at the base of B. bradfordensis zone; but not in the SEPM chart.
	Triscutum sullivani	174.18		FAD is 40% up in L. murchinsonae Zone.  On SEPM1998 chart, FAD is 90% up in L. haugi s.z. of L. murchinsonae zone.
	Carinolithus magharensis	174.80		FAD is 90% up in L. opalinum Zone.  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Triscutum tiziense	175.16		middle of L. opalinum Zone.  (J. Bergen will revisit the calibration).  On SEPM1998 chart, FAD is 25% up in bifidatum s.z. of L. opalinum zone.
	Lotharingius contractus	175.38		FAD is 25% up in L. opalinum Zone.  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Retecapsa incompta	177.17		70% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is 7/10 up in L. opalinum s.z. of L. opalinum zone.
	Watznaueria fossacincta	177.56		50% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is the base of  levesquei s.z. of D. pseudoradiosa zone.
	Axopodorhabdus depravatus	178.15		20% up in "D. levesque Zone" (combined P. dispansum-D. pseudoradiosa).  On SEPM1998 chart, FAD is 40% up in grumer s.z. of P. dispansum zone.  
	Biscutum intermedium	178.54		Base "D. levesquei" (= base P. dispansum Zone).  On SEPM1998 chart, FAD is the base of P. dispansum zone.
	Discorhabdus criotus	181.28		95% up in H. serpentinum Zone.  On SEPM1998 chart, FAD is 50% up in lusitanicum s.z of the H. bifrons zone.  Formerly called "B. criotum" (genera change).
	Biscutum striatum	181.35		90% up in H. serpentinum Zone.  On SEPM1998 chart, FAD is 65% up in H. falciferum s.z. of H. falciferum zone.
	Carinolithus superbus	182.63		Assigned as 5% up in H. serpentinum Zone (but disagreement in placement among workers).  On SEPM1998 chart, FAD is 45% up in H. pseudoserpentinum s.z of H. serpentinum zone. 
	Lotharingius crucicentralis	182.94		20% up in D. tenuicostatum Zone.  On SEPM1998 chart, FAD 95% up in P. paltus s.z. of D. (O.) tenuicostatum zone.
	Lotharingius sigillatus	183.00		Base D. tenuicostatum Zone (in Tethys).  On SEPM1998 chart, FAD is base of D. (O.) tenuicostatum zone.
	Axopodorhabdus atavus	184.48		90% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  On SEPM1998 chart, FAD is 40% up in acuratum s.z. of algovianum zone.
	Lotharingius hauffii	185.30		60% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  On SEPM1998 chart, FAD is 5% up in acuratum s.z. of algovianum zone.
	Biscutum novum, Biscutum profundum	186.68		10% up in A. margaritatus (= combined Tethyan portisi through acuratum subzones).  Called D. novus on SEPM chart.  On SEPM1998 chart, FAD is the base of cornacaldense s.z. of lavinianum zone.
	Lotharingius spp.	187.35		mid-P. davoei Zone (Tethyan).  DTS1995 listed FAD as base of A. capricornus s.z. of P. davoei zone, but not in the SEPM chart.
	Bussonius prinsii	188.71		75% up in E. jamesoni Zone  (much lower than SEPM chart).  In DTS1995 FAD is the base of solare s.z. of emaciatum zonet.
	Similiscutum cruciulus	189.00		middle of U. jamesoni Zone.  On SEPM1998 chart, FAD is 55% up in U. jamesoni s.z. U. jamesoni zone.
	Similiscutum precarium	189.92		80% up in E. raricostatum Zone.  On SEPM1998 chart, FAD is 50% up in P. brevispina s.z. of U. jamesoni zone.  Taxa may be synonymous with D. orbiculatus (event on SEPM chart at same level).
	Crelaidolithus granulatus	190.41		50% up in E. raricostatum Zone (J. Bergen).  On SEPM1998 chart, FAD is base of A. maculatum s.z. of P. davoei zone.
	Orthogonoides hamiltoniae	192.40		70% up in A. obtusum Zone.  On SEPM1998 chart, FAD is 55% up in A. obtusum s.z. of A. obtusum zone.
	Parhabdolithus robustus	192.62		On SEPM1998 chart, FAD is 55% up in A. stellare s.z. of A. obtusum zone.
	Crepidolithus crassus	192.77		40% up in A. obtusum Zone.  On SEPM1998 chart, FAD is 55% up in A. obtusum s.z. of A. obtusum zone.
	Schizosphaerella punctulata	199.60
	Obliquipithonella rhombica (calcisphere)	203.64
	Crucirhabdus primulus	208.58
	Crucirhabdus minutus (coccolith), Archaeozygodiscus koessenensis (Ioxolith)	209.58
	Eoconusphaera ziambachensis (nannolith, Incertae sedis)	210.08
	Prinsiosphaera triassica (nannolith, Incertae sedis)	213.92
	Orthopithonella geometrica (calcisphere)	216.53
	EARLIEST NANNOFOSSILS = Orthopithonella misurinae and Obliquipithonella prasina (calcispheres), Carnicalyxia tabellata and Cassianospica curvata (nannoliths, Incertae sedis)	225.36



Boreal UC,BC,NJ,NT Nanno Zone (E.Cret-Carnian)	block	45	149/205/210	notitle	off	Late CRETACEOUS = mainly Burnett (1998); Early CRETACEOUS = mainly Bown et al. (1998); JURASSIC = Bown and Cooper (1998); TRIASSIC = Bown (1998).
	TOP	65.50
	UC20	68.60
	UC19	69.72
	UC18	69.83
	UC17	70.14
	UC16	71.12
	UC15	80.64
	UC14	81.47
	UC13	83.21
	UC12	84.94
	UC11	87.45
	UC10	88.58
	UC9	91.22
	UC8	92.24
	UC7	92.51
	UC6	93.41
	UC5	93.84
	UC4	93.98
	UC3	96.01
	UC2	97.72
	UC1	99.19		Mortimer's NK19 base is LCO of S. primitivum and B. ellipticum; but these are not tabulated by Bown'98, SEPM or Jim Bergen. Put arbitrarily here at base of Cenomanian -- need to eventually find calibrations.
	BC27	101.49
	BC26	103.13
	BC25	107.07
	BC24	108.62	dashed
	BC23	111.41	dashed
	BC22	114.00
	BC21	121.90	dashed
	BC20	122.42
	BC19	122.98
	BC18	125.00
	BC17	125.16
	BC16	126.88
	BC15	128.60
	BC14	128.97
	BC13	129.97
	BC12	130.71
	BC11	132.66
	BC10	132.99
	BC9	133.46
	BC8	134.86
	BC7	136.41
	BC6	136.65
	BC5	137.97
	BC4	139.92
	BC3	140.04
	BC2	140.18		BC2 is a very brief range-zone.
	BC1	141.66	dashed
	NJ18	148.39		This is Bown's definition for base of NJ18, and others confusingly, has a different NJ18 (and marker) that has nothing to do with this Boreal succession.
	NJ17b	148.66
	NJ17a	150.37
	NJ16b	150.63
	NJ16a	151.01
	NJ15b	156.30
	NJ15a	159.61
	NJ14	161.61
	NJ13	163.37
	NJ12b	164.25
	NJ12a	165.50
	NJ11	168.24
	NJ10	170.20
	NJ9	171.15
	NJ8b	174.18
	NJ8a	177.17
	NJ7	181.35
	NJ6	182.63
	NJ5b	184.08		The set of FADs of A. atavus, C. impontus and L. sigillatus and maybe B. prinsii (but see comments on its FAD about 5 myr below) are markers for base of NJ5b.
	NJ5a	185.30
	NJ4b	188.22
	NJ4a	189.07
	NJ3	191.87
	NJ2b	194.19
	NJ2a	196.69
	NJ1	199.60
	NT2b	210.08
	NT2a	213.92
	NT1	225.36

Boreal UC-BC Nanno Subzone	block	30	149/205/210	notitle	off
	TOP	65.50
	d	66.62
	c	67.85
	b	68.19
	a	68.60
	TOP	70.14
	d	70.27
	c	70.36
	b	70.77
	a	71.12
	e	72.16
	d	72.58
	c	78.38
	b	80.07
	a	80.64
	b	81.38
	a	81.47
	b	82.89
	a	83.21
	TOP	84.94
	c	86.96
	b	87.20
	a	87.45
	TOP	88.58
	c	89.07
	b	90.25
	a	91.22
	b	91.61
	a	92.24
	TOP	92.51
	b	93.27
	a	93.41
	c	93.62
	b	93.76
	a	93.84
	b	93.88
	a	93.98
	e	94.08
	d	94.25
	c	94.51
	b	95.53
	a	96.01
	c	96.91
	b	97.27
	a	97.72
	c	98.93
	b	99.11
	a	99.19		Mortimer's NK19 base is LCO of S. primitivum and B. ellipticum; but these are not tabulated by Bown'98, SEPM or Jim Bergen. Put arbitrarily here at base of Cenomanian -- need to eventually find calibrations.
	c	99.82
	b	99.96
	a	101.49
	TOP	103.13
	b	106.15
	a	107.07
	TOP	130.71
	b	132.56
	a	132.66
	TOP	133.46
	c	133.77
	b	134.42
	a	134.86
	TOP	137.97
	b	139.40
	a	139.92
	b	139.98
	a	140.04

Boreal NK Nanno zones	block	45	149/205/210	notitle	off	Ages mainly from Burnett (1998)
	TOP	65.50
	NK1 - 2	68.19
	NK3 - 5	69.72
	NK6	69.83
	NK7	70.14
	NK8	72.16
	NK9 - 12A	85.95
	NK13B	88.83
	NK14 A-C	92.24
	NK14 D	92.51
	NK16 - 17	93.76
	NK18	94.25
	NK19	99.19		Mortimer's NK19 base is LCO of S. primitivum and B. ellipticum; but these are not tabulated by Bown'98, SEPM or Jim Bergen. Put arbitrarily here at base of Cenomanian -- need to eventually find calibrations.


Boreal KN Nanno zones	block	45	149/205/210	notitle	off	Ages mainly from Burnett (1998)
	TOP	65.50
	KN1 - 5	69.72
	KN6 - 7	70.14
	KN8 - 9	70.36
	KN10 - 13	72.16
	KN14 - 19	79.67
	KN20	81.38
	KN21	81.47
	KN22 - 24	84.94
	KN25 - 29	88.58
	KN30 - 34	92.24
	KN35 - 38	93.41
	KN39	93.76
	KN40	95.53


Boreal Nanno Zone Marker	event		167/206/210		off	Late CRETACEOUS = mainly Burnett (1998); Early CRETACEOUS = mainly Bown et al. (1998); JURASSIC = Bown and Cooper (1998); TRIASSIC = Bown (1998).
FAD
	Nephrolithus frequens (oldest possible)	68.19		Burnett'98 states that N. frequens has a well-documented diachronous FO", which is youngest at northern high latitudes.  Burnett'98 schematically shows as about 40% up in B. argenta / junior Belemnite Zone (NW Europe).   SEPM'98 assigned FAD as 3/10 up between top of J. nebrascensis Z. and end of Maastrichtian
	Lithraphidites quadratus	68.60		Burnett'98 schematically shows as about 85% up in B. junior / tegulatus Belemnite Zone (NW Europe).
	Misceomarginatus pleiniporus, Misceo. quaternarius	80.64		Burnett'98 shows schematically as base of B. obtusus Zone of N. Amer. (= base of Middle Campanian)  SEPM'98 assigned FAD as 6/10 up in S. hippocrepis II Z.  These two taxa are quite similar (and may be synonymous).
	Broinsonia parca parca	81.47		Burnett'98 schematically shows as about 40% up in S. hippocrepis III Zone of N. Amer.  SEPM'98 assigned FAD as 3/10 up in S. hippocrepis I Zone.  Subzone UC14a is very brief.
	Arkhangelskiella cymbiformis	83.21		Arkhangelskiella cymbiformis (sensu Burnett'98b) FAD is schematically by Burnett'98 shown as middle of S. leei III Zone of N. Amer.
	Calculites obscurus	85.95		Burnett'98 notes that "consistent occurrence of rare to frequent Calculites obscurus has been recorded in this zone (UC11c), but cannot be relied on as a datum since the form has been observed to occur well below this level, albeit sporadically and very rarely (as has Calculites ovalis)."  Placed here as "FCO" and arbitrarily in middle of Zone UC11c.  SEPM'98 assigned FAD much higher, as top of C. choteauensis Zone.
	Lithastrinus grillii	87.45		Schematic diagram in Burnett'98 suggests about 40% up in G. margae ammonite Zone.
	Micula stauropora	88.58		Burnett'98 assigns as essentially at base of P. tridorsatum Zone.
	Lithastrinus septenarius	91.22		Same as L. "moratus" of Varol, 1992.  Schematic diagram in Burnett'98 suggests about 20% up in R. ornatissimum subzone of C. woollgari Zone.
	Kamptnerius magnificus (FCO)	92.24		Burnett'98 "FO of consistently-occurring K. magnificus lies areound the FO of E. eximius."
	Eiffellithus eximius	92.24		Schematic diagram in Burnett'98 suggests about 80% up in M. nodosoides Zone.   SEPM'98 assigned FAD at about 1 myr higher.
	Quadrum gartneri	92.51		Schematic diagram in Burnett'98 suggests about 1/3rd up in M. nodosoides Zone.  In contrast, Boreal column in SEPM'98 had placed Q. garneri FAD as Cenomanian (!!) at 4/10 up in N. juddii Z.
	Cylindralithus biarcus	93.98		Schematic diagram in Burnett'98 suggests about 10% up in M. geslinianum Zone.
	Lithraphidites acutus	96.01		Burnett'98 assigns as base of C. inerme Zone.  SEPM'98 assigned FAD as slightly higher (by about 0.3 myr) as 25% up in T. costatus subzone of A. rhotomagense Zone.
	Gartnerago segmentatum	97.72		Called "G. obliquum" by some authors; but Burnett'98  indicates that true "obliquum" comes in within mid-UC2c, or about 1 myr higher.  Burnett'98 assigns as basal (but not base) of M. dixoni ammonite zone, so set as 5% up here.
	Corollithion kennedyi	99.19		40% up in N. carcitanense subzone (Jackie Lee).  SEPM'98 assigned FAD as 8/10 up in [blank] Z.
	Eiffellithus turriseiffelii	101.49		90% up in M. inflatum Zone.  SEPM'98 assigned FAD as 7/10 up in E. loricatus Z., E. meandrinus s.z.
	Eiffellithus monechiae	103.13		60% up in M. inflatum Zone
	Axopodorhabdus albianus	107.07		Just below top (95%) of E. loricatus Zone.  SEPM'98 assigned FAD as 7/10 up in D. mammillatum Z., P. steinmani s.z.
	Tranolithus orionatus  (=T. phacelosus)	108.62	dashed	DASH at 25% up in H. dentatus Zone.  SEPM'98 assigned FAD as 7/10 up in D. mammillatum Z., P. steinmani s.z.
	Prediscosphaera columnata	111.41	dashed	DASH at middle of L. tardefurcata Zone (uncertainty ranges through entire zone).  SEPM'98 assigned FAD as top of L. tardefurcata Z., L. regularis s.z.
	Lithraphidites moray-firthensis	122.42	dashed	DASH at Middle of D. deshayesi Zone
	Farhania varolii	122.98	dashed	DASH at 95% up in D. forbesi Zone.  SEPM'98 assigned FAD as 3/10 up in D. deshayesi Z.
	Rhagodiscus gallagheri	125.00		Base of P. fissicostatus Zone (base of Aptian)
	Zeugrhabdotus scutula (acme)	128.60		Just above base (5%) of P. elegans Zone.
	Nannoconus borealis	128.97		Base of H. fissicostatum Zone.
	Nannoconus abundans	129.97		Base of P. rarocinctum Zone.  SEPM'98 assigned FAD as 3/10 up in S. hugii Z.
	Tegulalithus septentrionalis	133.46		25% up in M. speetonensis Zone
	Eprolithus? antiquus	136.41		60% up in E. amblygonium Zone.  SEPM'98 assigned FAD as 1/10 up in A. radiatus Z.
	Micranthololithus speetonensis	139.92		Base of P. heteropleurum subzone (middle of Polyptyhites Zone).  SEPM'98 assigned FAD as 8/10 up in T. pertransiens Z.
	Sollasites arcuatus	140.18		25% up in P. albidum Zone.  SEPM'98 assigned FAD as 8/10 up in T. otopeta Z.
	Retecapsa augustiforata	141.66		DASH at Base of S. icenii Zone (uncertain ranges through entire Ryazinian!).  Alternate name was C. angustiforatus.  SEPM'98 assigned FAD as 8/10 up in T. occitanica Z., D. dalmasi s.z.
	Stephanolithion atmetros	150.37		Base of P. scitulus Zone  (Bown and Cooper, 2000).  SEPM chart had FAD in middle of P. pectinatus Z.
	Stephanolithion brevispinus	151.01		30% up in A. autissiodorensis Zone (Bown and Cooper, 2000).  Former name was S. helotatus.  SEPM chart had FAD at base of A. autissiodorensis Z..  ANOTHER COMMENT AT CELL: This genus extends downward to the Aulacostephanus (Pseudomutabilis) eudoxus. Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Stephanolithion bigotii maximum	161.61		50% up in Q. lamberti Zone (Bown and Cooper, 2000).  SEPM chart also had FAD at base of Q. lamberti s.z. (mid-Q. lamberti Zone) 
	Stephanolithion bigotii bigotii	163.37		50% up in S. caloviense Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of galilei s.z. (P. koenigi Z.one)
	Ansulasphaera helvetica	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had FAD Just above (0.05 myr) base of O. orbis Zone.
	Pseudoconus enigma	168.24		5% up in P. parkinsoni Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of P. acris s.z. of lower P. parkinsoni Z.   ANOTHER COMMENT AT THIS CELL:  This genus extends downward to the Strenoceras (Garantiana) garantiana zone (tetragona s.z.). Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982.
	Stephanolithion speciosum	170.20		5% up in S. humphriesianum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 3/10th up in romani s.z. (lowermost S. humphriesianum Zone).
	Ellipsagelosphaera britannica	171.15		10% up in W. laeviuscula Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of W. laeviuscula Z.
	Lotharingius contractus	174.18		40% up in L. murchinsonae Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 1/10 up in upper L. haugi s.z. (middle of L. murchinsonae Z.).  ANOTHER COMMENT AT THIS CELL:   This genus extends downward to Leioceras opalinum zone (bifidatum s.z.).
	Retecapsa incompta	177.17		70% up in D. levesquei Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of D. pseudoradiosa Zone
	Discorhabdus striatus	181.35		90% up in H. faclciferum Zone.  Also called Biscutum striatum.   (Bown and Cooper, 2000).  SEPM chart had FAD at 8/10 up in H. falciferum s.z. (upper H. falciferum Zone)
	Carinolithus superbus	182.63		5% up in H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 3/10 up in H. exaratum s.z. H. exaratum s.z. (= strangewaysi s.z.; lower H. falciferum Zone)
	Crepidolithus impontus	184.08		10% up in P. spinatum Zone (called "C. cavus" in earlier zonations and SEPM chart). (Bown and Cooper, 2000).  Not on SEPM chart in Boreal columns, but Tethyan FAD was approximate middle of meneghini s.z.   ANOTHER COMMENT AT THIS CELL:   This genus extends downward to the Amaltheus margaritatus zone (Amaltheus gibbosus s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Lotharingius hauffii	185.30		60% up in A. margaritatus Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 8/10 up in cornacaldense s.z. (upper lavinianum Zone).
	Similiscutum cruciulus	189.07		Middle of U. jamesoni Zone (Bown and Cooper, 2000).  SEPM chart had FAD at approximate base of U. jamesoni s.z. (upper U. jamesoni Zone)
	Crepidolithus crassus	191.87		20% up in O. oxynotum Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of A. stellare s.z. ( A. obtusum Zone).   ANOTHER COMMENT AT THIS CELL:   The Nannofossil "Crepidolithus" genus extends downward to the E. raricostatum zone (Crucilobiceras densinodulum s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Parhabdolithus liasicus	196.69		75% up in S. angulata Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of Sinemurian stage. 
	Schizosphaerella punctulata	199.60		Base of Hettangian, but Bown indicates FAD might be as high as mid-Hettangian (Bown and Cooper, 2000).  SEPM chart had FAD at base of Jurassic  ANOTHER COMMENT AT THIS CELL:   This genus extends to the end of the Jurassic period.  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Obliquipithonella rhombica (calcisphere)	203.64
	Crucirhabdus primulus	208.58
	Crucirhabdus minutus (coccolith), Archaeozygodiscus koessenensis (Ioxolith)	209.58
	Eoconusphaera ziambachensis (nannolith, Incertae sedis)	210.08
	Prinsiosphaera triassica (nannolith, Incertae sedis)	213.92
	Orthopithonella geometrica (calcisphere)	216.53
	EARLIEST NANNOFOSSILS = Orthopithonella misurinae and Obliquipithonella prasina (calcispheres), Carnicalyxia tabellata and Cassianospica curvata (nannoliths, Incertae sedis)	225.36
LAD
	Cretaceous taxa	65.50	
	Reinhardtites levis	69.72		Burnett'98 schematically shows as about 85% up in B. sumensis Belemnite Zone (NW Europe).  SEPM'98 assigned LAD as top of H. ricolleti Zone of N.Amer., which is about 1 myr Higher.
	Tranolithus orionatus  (=T. phacelosus)	69.83		Called "phacelosus" by most older publications, but Burnett and Leg 207 use "orionatus".  Burnett'98 schematicaly shows this LAD at about 1/3rd up in B. sumensis Belemnite Zone of NW Europe.  SEPM'98 assigned FAD as 6/10 up in B. grandis Zone of N.Amer., which is nearly same timing.
	Broinsonia parca constricta	70.14		Burnett'98 schematically shows as base of B. obtusa Belemnite Zone (NW Europe).  Jim Bergen shows as mid-Early Maastrictian (and LAD of "parca parca" as mid-Late Campanina).
	Tortolithus caistorensis	70.36		Burnett'98 schematically shows as base of B. pseudobtusa Belemnite Zone (NW Europe).  SEPM'98 assigned LAD as 4/10 up in B. eliasi Z.
	Eiffellithus eximius	71.12		Burnett'98 schematically shows as about 70% up in B. langei Belemnite zone of NW Europe (used here), or about middle of B. reesidei Zone of N. Amer.  SEPM'98 assigned LAD as 2/10 up in B. compressus Z.
	Orastrum campanensis	72.16		Burnett'98 schematically shows as about 70% up in B. langei Belemnite zone of NW Europe (used here), or at about middle of B. compressus Zone of N. Amer.  Problem is how the NW Europe belemnites correlate to N.Amer. ammonites.  HOWEVER, Jim Bergen assigned O. campanensis LAD as ABOVE E. eximius LAD.
	Lithastrinus grillii	79.67		Burnett'98 schematically shows as about 85% up in B. asperiformis Zone of N. Amer., but notes that LAD is partially paleolatitude dependent.
	Lithastrinus septenarius	84.94		Same as L. "moratus" of Varol, 1992.  Schematic diagram in Burnett'98 suggests about base of Uintacrinus socialis CRINOID Zone (in Chalk); so I've arbitrarily put this at base of Middle Santonian.
	H. turonicus	88.83		Burnett'98 "LO of H. turonicus is here (Zone UC9c); so arbitrarily put in middle.
	Helenea (=Microstaurus) chiastia	93.41		Same as "Microstaurus chiastius" of other authors.  Burnett'98 assigns LAD to middle of W. devonense Zone (or, about 1/6th up in super-zone of W. coloradoense); but J. Bergen puts down to base of this zone (base of Turonian), and below LAD of R. asper.
	Axopodorhabdus albianus	93.76		Schematic diagram in Burnett'98 suggests about 85% up in M. geslinianum Zone.  This switches the "usual observed" sequence of LAD of A. albianus occurring AFTER the LAD of R. asper (which is the basis of separate NK zones)
	Lithraphidites acutus	93.84		Schematic diagram in Burnett'98 suggests about 60% up in M. geslinianum Zone.
	Gartnerago nanum	94.25		Schematic diagram in Burnett'98 suggests about 2/3rds up in C. guerangeri Zone.
	Gartnerago theta	95.53		Schematic diagram in Burnett'98 suggests about 25% up in A. rhotomagense Zone.
	Farhania varolii	114.00		Top of N. nolani subzone
	Lithraphidites moray-firthensis	121.90	dashed	DASH at Base of T. bowerbanki Zone
	Nannoconus borealis	125.16		Just above base (5%) of P. bidentatum Zone.
	Zeugrhabdotus scutula (acme)	126.88		Just above base (5%) of A. inexum Zone.
	Clepsilithus maculosus	130.71		25% up in S. variabilis subzone.
	Tegulalithus septentrionalis	132.66		Middle of C. gottschei Zone.  SEPM'98 assigned LAD as 5/10 up in P. ligatus Z.
	Eiffellithus striatus	132.99		75% up in M. speetonensis Zone
	Eprolithus? antiquus	134.86		30% up in E. regale Zone.  SEPM'98 assigned LAD as 8/10 up in C. loryi Z.
	Triquetrorhabdulus shetlandensis	136.65		Base of E. amblygonium Zone
	Micranthololithus speetonensis	137.97		Base of Dichotomites spp. Zone.
	Sollasites arcuatus	140.04		75% up in P. albidum Zone.  SEPM'98 assigned LAD as 1/10 up in T. pertransiens Z.
	Stephanolithion atmetros	148.39		90% up in fittoni Zone.  This is Bown's definition for base of NJ18, and others confusingly, has a different NJ18 (and marker) that has nothing to do with this Boreal succession.
	Stephanolithion bigotii bigotii	148.66		20% up in P. rotunda Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of P. pallasiodes Z. 
	Anfractus harrisonii	150.63		Base of elegans Zone.
	Lotharingius crucicentralis	156.30		95% up in A. regulare Zone (high-Boreal) (Bown and Cooper, 2000).  SEPM chart had LAD at base of A. rosenkrantzi Zone.
	Stephanolithion bigotii maximum	159.61		Base of P. plicatilus Zone (Bown and Cooper, 2000).  SEPM chart had LAD is near top (80% up) of C. cordatum s.z.  [uppermost C. cordatum Zone].
	Pseudoconus enigma	164.25		95% up in M. herveyi Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of P. koenigi Zone.
	Parhabdolithus robustus	188.22		Coeval with FAD of C. pliensbachensis (40% up in T. ibex Zone) (Bown and Cooper, 2000).  Not on SEPM chart in Boreal column, but Tethyan column has FAD (but this LAD is approximate base of P. brevispina s.z. (middle of U. jamesoni Zone)
	Parhabdolithus marthae	194.19		90% up in A. semicostatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10 up in E. sauzeanum s.z. (upper A. semicostatum Zone)
	Prinsiosphaera triassica, Eoconusphaera ziambachensis, Crucirhabdus minutus, Archaeozygodiscus koessenensis 	199.60		Base of Hettangian (Bown and Cooper, 2000).
	Orthopithonella misurinae,  Obliquipithonella prasina, Carnicalyxia tabellata, Cassianospica curvata	216.53

Boreal Nanno Subzone and other markers	event		167/206/210		off
EVENT
	Zeugrhabdotus noeliae (acme), Micrantholithus (acme)	132.56		Base of S. marginatus subzone
FAD
	Cribrosphaerella daniae (oldest possible)	66.62		Burnett'98 schematically shows as about middle of B. baltica / danica Belemnite Zone (NW Europe).  SEPM'98 assigned FAD as 3/10 up between top of J. nebrascensis Z. and end of Maastrichtian
	Arkhangelskiella maastrichtiana	67.85		Burnett'98 schematically shows as about 85% up in B. argenta / junior Belemnite Zone (NW Europe).
	Prediscosphaera stoveri	72.58		Burnett'98 schematically shows as about 50% up in B. minor Belemnite zone of NW Europe (used here), or about middle of B. stevensoni Zone of N. Amer.   SEPM'98 assigned FAD as nearly 5 myr Older at 4/10 up in B. sp. (smooth) Z.
	Reinhardtites levis, Lithraphidites praequadratus	72.63		Burnett'98 implied that apparent FAD is much later in Boreal realm than in Tethyan/temperate; and assigned schematically shows as about 50% up in B. minor Belemnite zone of NW Europe (used here), or as equivalent to base of D. stevensoni Zone of N.Amer (but, these don't correlate  using SEPM'98).  She notes that L. praequadratus first occurs with R. levis in this subzone in N. Germany.  SEPM'98 assigned FAD as nearly 5 myr Older at top of B. sp. (smooth) Z.
	Heteromarginatus bugensis	78.38		Burnett'98 schematically shows as about middle of "B. perplexus" Zone of N. Amer., so that "perplexus" trio is combined here.
	Broinsonia parca constricta	81.38		Burnett'98 schematically shows as about 60% up in S. hippocrepis III Zone of N. Amer. 
	Broinsonia magnum	81.92		Burnett'98 shows schematically as middle of S. hippocrepis II Zone of N. Amer.  SEPM'98 had assigned FAD as base of S. hippocrepis I Zone.
	Orastrum campanensis (FCO)	82.89		Burnett'98 shows schematically as base of S. hippocrepis I Zone of N. Amer.  SEPM'98 assigned FAD as just above base of Campanian.
	Lucianorhabdus cayeuxii	86.96		Schematic diagram in Burnett'98 suggests about base of P. serratomarginatus ammonite Zone.   In contrast, Boreal column in SEPM'98 assigned FAD nearly 2 myr Higher -- just below top of C. saxitonianus-I. undulatoplicatus Zone in mid-Santonian !!  Subzone UC11a is very brief.
	Reinhardtites anthophorus	88.01	dashed	DASH:  SEPM'98 assigned FAD as 1/10 up in C. saxitonianus -I. undulatoplicatus Z.  However, Burnett'98 notes that "FO of Reinhardtites anthophorus is an unreliable datum.  Its inception, which is widely believed to be in the Coniacian, is somewhat obscure.  (etc).  Therefore, assigned here as mid-Zone UC10 (Burnett's placement of its discussion) with a Dash.
	Broinsonia parca expansa	89.07		Burnett'98 assigns as essentially at base of F. petrocoriensis Zone.  Same as "B. lacunosa" and "Aspidolithus parcus expansus" of some authors.
	Zeugrhabdotus biperforatus	90.25		Schematic diagram in Burnett'98 suggests about 1/6th up in "super" S. neptuni Zone (version used in GTS04 includes "overlying" Prionocyclus germari Zone".
	Lucianorhabdus quadrifidus	91.61		Schematic diagram in Burnett'98 suggests about 25% up in R. kallesi subzone of C. woollgari Zone.
	Lucianorhabdus maleformis	92.51		Burnett'98 assigned this FAD at same level as Q. garneri FAD.  SEPM'98 assigned FAD at about 1 myr higher.
	Marthasterites furcatus	92.89		Burnett'98 "Marthasterites furcatus first occurs here (Zone UC6b) at higher paleolatitudes." AND, notes that "Personal observations have shown that this event is unreliable, the FO lying stratigraphically much lower at higher latitudes."  Arbitrarily placed in middle of Zone UC6b.  SEPM'98 assigned FAD nearly 3 myr higher, at top of S. whitfieldi Z, which is where Crux'92 found it in South England.
	Eprolithus moratus	93.27		Same as "E. eptapetalus" of Varol '92.  Base of subzone corresponds to extinction of Ceratolithina spp. In 'austral' province.  K. magnificus has its local FAD here in N. England. Burnett'98 assigns LAD to middle of W. devonense Zone (or, about 1/3rd up in super-zone of W. coloradoense)
	Quadrum intermedium	93.62		This is the 5-element Q. intermedium. Schematic diagram in Burnett'98 suggests about 50% up in N. juddii Zone.
	Cylindralithus sculptus	96.91		Schematic diagram in Burnett'98 suggests about 50% up in M. dixoni Zone.
	Kamptnerius magnificus (rare), Helicolithus anceps	98.89		Schematic diagram in Burnett'98 suggests about 75% up in N. carcitanense subzone.  These taxa may not occur (or are too rare) until later in more oceanic or southern locations.
	Calculites anfractus (rare)	99.82		80% up in S. dispar Zone.  Was suggested as datum for a base of Zone "BC27c", but probably too rare to be useful [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI]
	Tequlalithus tessellatus, Gartnerago praeobliquum	104.78		30% up in M. inflatum Zone
	Ceratolithina hamata	106.89		20% up in E. lautus Zone.
	Ceratolithina bicornuta, Owenia hillae	107.01		Base of E. lautus Zone.
	Crucicribrum anglicum	108.62	dashed	DASH at 25% up in H. dentatus Zone; uncertainty spans lower 2/3rds of Zone.
	Seribiscutum primitivum, Acaenolithus viriosus	112.30		90% up in H. jacobi Zone
	Nannoconus truitti (acme)	119.35		55% up in C. martinoides Zone.  SEPM'98 assigned FAD as 3/10 up in C. martinoides Z.
	Eprolithus floralis, Braarudosphaera africana, Radiolithus planus	121.90		Base of T. bowerbanki Zone.  SEPM'98 assigned FAD of E. floris is 4/10 up in D. deshayesi Z.; FAD of B. africana is 1/10 up in D. deshayesi Z.
	Hayesites irregularis, Flabellites oblongus	123.97		Base of D. forbesi Zone.  But, F. oblongus FAD is completely out-of-sequence compared to Tethyan (maybe Bown meant the LAD?), and H. irregularis FAD is nearly 1 myr after its Tethyan FAD.
	Acaenolithus sp. 1	127.91		Just above base (10%) of P. denckmanni Zone.
	Nannoconus pseudoseptentrionalis	128.60		Just above base (5%) of P. elegans Zone.
	Rucinolithus terebrodentarius	130.12		85% up in S. variabilis subzone.  Also called Assipetra terebrodetarius.
	Cretarhabdus inaequalis	133.09		65% up in M. speetonensis Zone
	Zeugrhabdotus scutula, Perissocyclus plethotretus	133.77		85% up in S. inversum Zone.  P.Bown uses Peri. plethotretus FAD to define base of brief BC8c subzone.
	Rucinolithus windleyae	133.94		Middle of S. inversum Zone.
	Tegumentum octiformis	134.86		30% up in E. regale Zone
	Repagulum parvidentatum	135.70		Middle of E. noricum Zone
	Conusphaera rothii	136.63		Base (5% up) of E. amblygonium Zone.  Secondary marker for base of BC6.  SEPM'98 assigned FAD as 5/10 up in N. pachydicranus Z., H. trinodosum s.z.
	Eiffellithus striatus	136.86		DASH at base of densicostatus Zone (probably equivalent to base of Olcostephanus spp. Zone.
	Zeugrhabdotus diplogrammus, Zeug. trivectis	137.97		Base of Dichotomites spp. Zone.
	Eiffellithus windii	139.40		Base of P. clarkei subzone (middle of Polyptychites Zone)
	Influx of Crucielipsis cuvilleri & Speetonia colligata	139.77		Base of Polyptychites Zone
	Triquetrorhabdulus shetlandensis	139.95		Middle of P. robustum subzone (lowermost Paratollia Zone).  Used to subdivide BC3 into very-brief a/b subzones.
	Rhagodiscus asper, Crucielipsis cuvilleri, Bukrylithus ambiguus, Crucibiscutum salebrosum, etc.	141.66	dashed	DASH at base of S. icenii Zone (uncertain ranges through entire Ryazinian!)
	Crepidolithus perforata	163.20		Base of K. jason Zone (Bown and Cooper, 2000).  Not on SEPM chart.  But DTS2000 (Source of information?) had FAD as 7/10 up in K. enodatum s.z. (uppermost S. calloviense Zone). 
	Triscutum expansus	164.23		Base of P. koenigi Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 1/3rds up in gowerianus s.z. (basal P. koenigi Zone)
	Axopodorhabdus rahla	164.74		Base of M. herveyi Zone (Bown and Cooper, 2000).  SEPM chart also had FAD at base of M. herveyi Zone (base of Callovian)
	Stephanolithion hexum	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of O. orbis Zone
	Stephanolithion speciosum octum, Hexapodorhabdus cuvillieri, T. shawensis	168.24		Set of FADs at 5% up in P. parkinsoni Zone (coeval with FAD of P. enigma) (Bown and Cooper, 2000).  J. Bergen suggests the FAD of S. speciosum octum would be a preferable marker for base of Zone NJ11.   SEPM chart had FAD at base of P. parkisoni Zone
	Biscutum intermedium	177.17		FAD is coeval with R. incompta FAD (70% up in D. levesquei Z.)  (Bown and Cooper, 2000).  SEPM chart had
	Discorhabdus criotus	180.70		Base of H. variabilis Zone.  Also called Biscutum criotum.   (Bown and Cooper, 2000).  SEPM chart had FAD in middle of H.variabilis Z.
	Lotharingius sigillatus	183.60		Middle of P. spinatum Zone (Bown and Cooper, 2000).  SEPM chart had FAD is just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. The set of FADs of A. atavus, C. impontus and L. sigillatus and maybe B. prinsii (but see comments on its FAD about 5 myr below) are markers for base of NJ5b.
	Axopodorhabdus atavus	184.08		Coeval with FAD of C. impontus (10% up in P. spinatum Zone) (Bown and Cooper, 2000).  SEPM chart had FAD at just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. The set of FADs of A. atavus, C. impontus and L. sigillatus and maybe B. prinsii (but see comments on its FAD about 5 myr below) are markers for base of NJ5b.
	Biscutum novum	185.58		50% up in A. margaritatus Zone (Bown and Cooper, 2000).  Also known as D. novus.   SEPM chart had FAD in middle of E. raricostatum Z. 
	Biscutum finchii	185.85		40% up in A. margaritatus Zone  (Bown and Cooper, 2000).  Not on SEPM chart (at least not in Boreal column).  FAD is 6/10 up in A. capricornus s.z. (P. davoei Z.one)
	Bussonius prinsii	189.60	dashed	DASH -- FAD is poorly constrained, and may be as low as base of Pliensbachian  (Bown and Cooper, 2000).  SEPM chart had FAD as just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. ANOTHER COMMENT AT THIS CELL:   This genus extends downward to the Amaltheus margaritatus zone (Amaltheus gibbosus s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982.
	Orthogonoides hamiltoniae	191.87		Coeval with FAD of C. crassus  (Bown and Cooper, 2000).  SEPM chart had FAD is 4/10 up in O. simpsoni s.z. (lower O. oxynotum Zone)
	Parhabdolithus robustus	193.66		Middle of C. turneri Zone (Bown and Cooper, 2000).  SEPM chart had
	Crepidolithus pliensbachensis	195.28		Base of A. semicostatum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 7/10 up in  charlesi s.z. (lower A. semicostatum Zone)
	Mitrolithus elegans	196.69		Coeval with P. liasicus  (Bown and Cooper, 2000).  SEPM chart had FAD in middle of A. bucklandi s.z.(upper A. bucklandi Zone)
	Parhabdolithus marthae	195.89		Middle of A. bucklandi zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of C. rotiforme s.z. (middle A. bucklandi Zone) 
	Tubirhabdus patulus	196.89		Middle of S. angulata Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of S. complanata s.z. (upper S. angulata Zone)
	Crucirhabdus primulus	199.21		DASH -- Bown and Cooper (2000) give it a vague placement within NJ1 zone.  Not on SEPM chart in Boreal column, but Tethyan FAD is given as approximately base of C. johnstoni s.z. (middle of P. planorbis Zone).
LAD
	Monomarginatus quaternarius	70.27		Burnett'98 schematically shows as about 40% up in B. pseudobtusa Belemnite Zone (NW Europe).  HOWEVER, Jim Bergen inverts this sequence, with this M.quarternarius LAD BELOW T. caistorensis LAD (hence, at end of Campanian).
	Uniplanarius gothicus	70.48		Burnett'98 schematically shows as about middle of B. lanceolata Belemnite Zone (NW Europe)
	Heteromarginatus bugensis	70.77		Burnett'98 schematically shows as about 90% up in B. langei Belemnite zone of NW Europe.  SEPM'98 assigned LAD as top of B. jenseni Z.
	Reinhardtites anthophorus	71.12		Burnett'98 puts simultaneous with LAD of E. eximius.  SEPM'98 assigned both LADs as 2/10 up in B. compressus Zone.  HOWEVER, Jim Bergen distinquished a "var. A" R. anthrophorus, and assigned this LAD to be ABOVE E. eximius LAD; and a "var.B" with LAD much earlier (in mid-Campanian).
	Cylindralithus biarcus	80.07		Burnett'98 schematically shows as about 80% up in B. maclearni Zone of N. Amer. 
	Eprolithus floralis (rare)	82.20		Burnett'98 shows schematically as base of S. hippocrepis II Zone of N. Amer.  HOWEVER, both Bralower and Bergen have LAD of Eprolithus floralis in late Coniacian = LCO?
	Zeugrhabdotus noeliae	84.13		A datum that occurs in both Boreal and Tethyan realm.  Burnett'98 schematically shows as about 85% up in Middle Santonian (U/M Santonian boundary at LAD of Marsupites testudinarius Crinoid.)
	Quadrum gartneri	87.20		Schematic diagram in Burnett'98 suggests about 70% up in G. margae ammonite Zone.  Subzone UC11a is very brief.
	Rhagodiscus asper	93.72		Burnett'98 assigns as base of B. clydense Zone.  This provides a tie to Tethyan zonations; although J. Bergen assigned this LAD in lower Turonian (above LAD of M. chiastius).
	Cretarabdus striatus	93.88		Called "loriei" by some authors.  Schematic diagram in Burnett'98 suggests about 45% up in M. geslinianum Zone.
	Corollithion kennedyi	94.08		Schematic diagram in Burnett'98 suggests about 90% up in C. guerangeri Zone.
	Staurolithites gausorhethium	94.51		Schematic diagram in Burnett'98 suggests about 1/3rd up in C. guerangeri Zone.
	Zeugrhabdotus xenotus	97.27		"Shelf-preferring form, therefore subzone might not be determinable in oceanic sequences".  Schematic diagram in Burnett'98 suggests about 30% up in M. dixoni Zone.
	Gartnerago chiasta	98.93		Schematic diagram in Burnett'98 suggests about 70% up in N. carcitanense subzone.  Zone UC1c is very brief.
	Watznaureria britannica	99.11		Schematic diagram in Burnett'98 suggests about 50% up in N. carcitanense subzone.
	Hayesites albiensis	99.96		Bown shows as 30% up in S. dispar Zone, but found higher [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI], therefore assigned here as 70% up.
	Ceratolithina bicornuta	106.15		Near base (5% up) in M. inflatum Zone
	Braloweria boletiformis	107.07		Just below top (95%) of E. loricatus Zone.
	Nannoconus truitti (acme)	115.15		95% up in P. nutfieldiensis Zone.  SEPM'98 assigned LAD as top of P. nutfieldiensis.
	Micrantholithus hoschulzii	115.30		90% up in P. nutfieldiensis Zone
	Rhagodiscus asper	116.50		Middle of P. nutfieldiensis Zone
	Nannoconus abundans	125.00		Base of P. fissicostatus Zone (base of Aptian)
	Conusphaera rothii	126.10		DASH at base of S. stolleyi Zone
	Diazomatolithus lehmanii (boreal)	127.97		Just above base (5%) of P. denckmanni Zone.
	Rhagodiscus pseudoangustus	128.97		Secondary marker for base of BC14.  Base of H. fissicostatum Zone.
	Speetonia colligata	130.96		Base of S. variabilis subzone.
	Tubodiscus verenae	132.71		25% up in C. gottschei Zone.
	Crucielipsis cuvillieri	132.76	dashed	DASH at Base of C. gottschei Zone.  SEPM'98 assigned LAD as 5/10 up in P. ligatus Z.
	Crucibiscutum salebrosum	133.23		Middle of M. speetonensis Zone
	Stradnerlithus silvaradius	134.06		25% up in S. inversum Zone.
	Cyclagelosphaera margerelii (acme)	134.42		75% up in E. regale Zone.  P.Bown uses to define base of brief BC8b subzone.
	Nannoconus oviformis, Kokia borealis	139.98		Base of Paratollia Zone
	Nannoconus sp. (discs)	140.24	dashed	DASH at base of P. albidum Zone.  SEPM'98 assigned LAD as 4/10 up in T. otopeta Z.
	Hexapodorhabdus cuvillieri	150.90		50% up in A. autissiodorensis Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of A. autissiodorensis Z..   Another marker for base of NJ16.
	Crepidolithus perforata	154.97		Base of R. cymodoce Zone (Bown and Cooper, 2000).  Formerly called M. perforata.
	Ansulasphaera helvetica	161.69		40% up in Q. lamberti Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of Q. lamberti s.z. (mid-Q. lamberti Zone) . Another marker for base of NJ14.
	Stephanolithion hexum	162.60		DASH at 75% up in E. coronatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of K. jason Zone.
	Lotharingius velatus	163.37		50% up in S. caloviense Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 6/10 up in K. enodatum s.z. (uppermost S. calloviense Zone).
	Stephanolithion speciosum octum, Steph. spec. speciosum	163.88		50% up in P. koenigi Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of curtilobus s.z. of P. koenigi Z.
	Tetrapodorhabdus shawensis	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of O. orbis Zone
	Carinolithus magharensis	168.89		95% up in S. niortense Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 6/10 up in S.niortense Z., schroederi s.z.
	Carinolithus superbus	170.17		10% up in S. humphriesianum Zone (Bown and Cooper, 2000).  SEPM chart had LAD in middle of humpriesianum s.z. (middle of S. humpriesianum Zone).
	Biscutum constans	170.25		95% up in S. propinquans Zone (E. sauzei Zone) (Bown and Cooper, 2000).  Also called D. constans.  SEPM chart had LAD at 6/10 up in hebridica s.z. of E. sauzei Z.
	Bussonius prinsii	172.49		Base of G. concavum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of G. concavum Zone.
	Crepidolithus impontus	173.51		90% up in L. murchinsonae Zone.  Also called C. cavus.   (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10ths up in B. bradfordensis s.z. (lower B. bradfordensis Z.,)
	Lotharingius hauffii (acme)	180.50		Top of Acme is at base of G. thouarsense Zone (Bown and Cooper, 2000).
	Orthogonoides hamiltoniae	181.35		90% up in H. faclciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD in middle of H. pseudoserpentinum s.z. (H. falciferum Zone)
	Biscutum finchii	181.95		Middle of H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD t 9/10 up in H. exaratum s.z. (= stranewaysi s.z.; lower H. falciferum Zone)
	Calcivascularis jansae	182.63		 This is another marker for base of NJ6.  LAD at 5% up in H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 3/10 up in H. exaratum s.z. H. exaratum s.z. (= strangewaysi s.z.; lower H. falciferum Zone). 
	Crucirhabdus primulus	182.94		20% up in D. tenuicostatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10 up in P. paltus s.z. of D. tenuicostatum Z.
	Crepidolithus pliensbachensis	188.22		40% up in T. ibex Zone (Bown and Cooper, 2000).  SEPM chart had LAD is approximately at base of beirense s.z. (T. ibex Zone).


All Boreal Nanno Datums Combined	event		167/206/210		off
LAD
	Cretaceous taxa	65.50
	Reinhardtites levis	69.72		Burnett'98 schematically shows as about 85% up in B. sumensis Belemnite Zone (NW Europe).  SEPM'98 assigned LAD as top of H. ricolleti Zone of N.Amer., which is about 1 myr Higher.
	Tranolithus orionatus  (=T. phacelosus)	69.83		Called "phacelosus" by most older publications, but Burnett and Leg 207 use "orionatus".  Burnett'98 schematicaly shows this LAD at about 1/3rd up in B. sumensis Belemnite Zone of NW Europe.  SEPM'98 assigned FAD as 6/10 up in B. grandis Zone of N.Amer., which is nearly same timing.
	Broinsonia parca constricta	70.14		Burnett'98 schematically shows as base of B. obtusa Belemnite Zone (NW Europe).  Jim Bergen shows as mid-Early Maastrictian (and LAD of "parca parca" as mid-Late Campanina).
	Monomarginatus quaternarius	70.27		Burnett'98 schematically shows as about 40% up in B. pseudobtusa Belemnite Zone (NW Europe).  HOWEVER, Jim Bergen inverts this sequence, with this M.quarternarius LAD BELOW T. caistorensis LAD (hence, at end of Campanian).
	Tortolithus caistorensis	70.36		Burnett'98 schematically shows as base of B. pseudobtusa Belemnite Zone (NW Europe).  SEPM'98 assigned LAD as 4/10 up in B. eliasi Z.
	Uniplanarius gothicus	70.48		Burnett'98 schematically shows as about middle of B. lanceolata Belemnite Zone (NW Europe)
	Heteromarginatus bugensis	70.77		Burnett'98 schematically shows as about 90% up in B. langei Belemnite zone of NW Europe.  SEPM'98 assigned LAD as top of B. jenseni Z.
	Eiffellithus eximius	71.12		Burnett'98 schematically shows as about 70% up in B. langei Belemnite zone of NW Europe (used here), or about middle of B. reesidei Zone of N. Amer.  SEPM'98 assigned LAD as 2/10 up in B. compressus Z.
	Reinhardtites anthophorus	71.12		Burnett'98 puts simultaneous with LAD of E. eximius.  SEPM'98 assigned both LADs as 2/10 up in B. compressus Zone.  HOWEVER, Jim Bergen distinquished a "var. A" R. anthrophorus, and assigned this LAD to be ABOVE E. eximius LAD; and a "var.B" with LAD much earlier (in mid-Campanian).
	Orastrum campanensis	72.16		Burnett'98 schematically shows as about 70% up in B. langei Belemnite zone of NW Europe (used here), or at about middle of B. compressus Zone of N. Amer.  Problem is how the NW Europe belemnites correlate to N.Amer. ammonites.  HOWEVER, Jim Bergen assigned O. campanensis LAD as ABOVE E. eximius LAD.
	Lithastrinus grillii	79.67		Burnett'98 schematically shows as about 85% up in B. asperiformis Zone of N. Amer., but notes that LAD is partially paleolatitude dependent.
	Cylindralithus biarcus	80.07		Burnett'98 schematically shows as about 80% up in B. maclearni Zone of N. Amer. 
	Eprolithus floralis (rare)	82.20		Burnett'98 shows schematically as base of S. hippocrepis II Zone of N. Amer.  HOWEVER, both Bralower and Bergen have LAD of Eprolithus floralis in late Coniacian = LCO?
	Zeugrhabdotus noeliae	84.13		A datum that occurs in both Boreal and Tethyan realm.  Burnett'98 schematically shows as about 85% up in Middle Santonian (U/M Santonian boundary at LAD of Marsupites testudinarius Crinoid.)
	Lithastrinus septenarius	84.94		Same as L. "moratus" of Varol, 1992.  Schematic diagram in Burnett'98 suggests about base of Uintacrinus socialis CRINOID Zone (in Chalk); so I've arbitrarily put this at base of Middle Santonian.
	Quadrum gartneri	87.20		Schematic diagram in Burnett'98 suggests about 70% up in G. margae ammonite Zone.  Subzone UC11a is very brief.
	H. turonicus	88.83		Burnett'98 "LO of H. turonicus is here (Zone UC9c); so arbitrarily put in middle.
	Helenea (=Microstaurus) chiastia	93.41		Same as "Microstaurus chiastius" of other authors.  Burnett'98 assigns LAD to middle of W. devonense Zone (or, about 1/6th up in super-zone of W. coloradoense); but J. Bergen puts down to base of this zone (base of Turonian), and below LAD of R. asper.
	Rhagodiscus asper	93.72		Burnett'98 assigns as base of B. clydense Zone.  This provides a tie to Tethyan zonations; although J. Bergen assigned this LAD in lower Turonian (above LAD of M. chiastius).
	Axopodorhabdus albianus	93.76		Schematic diagram in Burnett'98 suggests about 85% up in M. geslinianum Zone.  This switches the "usual observed" sequence of LAD of A. albianus occurring AFTER the LAD of R. asper (which is the basis of separate NK zones)
	Lithraphidites acutus	93.84		Schematic diagram in Burnett'98 suggests about 60% up in M. geslinianum Zone.
	Cretarabdus striatus	93.88		Called "loriei" by some authors.  Schematic diagram in Burnett'98 suggests about 45% up in M. geslinianum Zone.
	Corollithion kennedyi	94.08		Schematic diagram in Burnett'98 suggests about 90% up in C. guerangeri Zone.
	Gartnerago nanum	94.25		Schematic diagram in Burnett'98 suggests about 2/3rds up in C. guerangeri Zone.
	Staurolithites gausorhethium	94.51		Schematic diagram in Burnett'98 suggests about 1/3rd up in C. guerangeri Zone.
	Gartnerago theta	95.53		Schematic diagram in Burnett'98 suggests about 25% up in A. rhotomagense Zone.
	Zeugrhabdotus xenotus	97.27		Shelf-preferring form, therefore subzone might not be determinable in oceanic sequences.  Schematic diagram in Burnett'98 suggests about 30% up in M. dixoni Zone.
	Gartnerago chiasta	98.93		Schematic diagram in Burnett'98 suggests about 70% up in N. carcitanense subzone.  Zone UC1c is very brief.
	Watznaureria britannica	99.11		Schematic diagram in Burnett'98 suggests about 50% up in N. carcitanense subzone.
	Hayesites albiensis	99.96		Bown shows as 30% up in S. dispar Zone, but found higher [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI], therefore assigned here as 70% up.
	Ceratolithina bicornuta	106.15		Near base (5% up) in M. inflatum Zone
	Braloweria boletiformis	107.07		Just below top (95%) of E. loricatus Zone.
	Farhania varolii	114.00		Top of N. nolani subzone
	Nannoconus truitti (acme)	115.15		95% up in P. nutfieldiensis Zone.  SEPM'98 assigned LAD as top of P. nutfieldiensis.
	Micrantholithus hoschulzii	115.30		90% up in P. nutfieldiensis Zone
	Rhagodiscus asper	116.50		Middle of P. nutfieldiensis Zone
	Lithraphidites moray-firthensis	121.90	dashed	DASH at Base of T. bowerbanki Zone
	Nannoconus abundans	125.00		Base of P. fissicostatus Zone (base of Aptian)
	Nannoconus borealis	125.16		Just above base (5%) of P. bidentatum Zone.
	Conusphaera rothii	126.10		DASH at base of S. stolleyi Zone
	Zeugrhabdotus scutula (acme)	126.88		Just above base (5%) of A. inexum Zone.
	Diazomatolithus lehmanii (boreal)	127.97		Just above base (5%) of P. denckmanni Zone.
	Rhagodiscus pseudoangustus	128.97		Secondary marker for base of BC14.  Base of H. fissicostatum Zone.
	Clepsilithus maculosus	130.71		25% up in S. variabilis subzone.
	Speetonia colligata	130.96		Base of S. variabilis subzone.
	Zeugrhabdotus noeliae (acme), Micrantholithus (acme)	132.56		Base of S. marginatus subzone
	Tegulalithus septentrionalis	132.66		Middle of C. gottschei Zone.  SEPM'98 assigned LAD as 5/10 up in P. ligatus Z.
	Tubodiscus verenae	132.71		25% up in C. gottschei Zone.
	Crucielipsis cuvillieri	132.76	dashed	DASH at Base of C. gottschei Zone.  SEPM'98 assigned LAD as 5/10 up in P. ligatus Z.
	Eiffellithus striatus	132.99		75% up in M. speetonensis Zone
	Crucibiscutum salebrosum	133.23		Middle of M. speetonensis Zone
	Stradnerlithus silvaradius	134.06		25% up in S. inversum Zone.
	Cyclagelosphaera margerelii (acme)	134.42		75% up in E. regale Zone.  P.Bown uses to define base of brief BC8b subzone.
	Eprolithus? antiquus	134.86		30% up in E. regale Zone.  SEPM'98 assigned LAD as 8/10 up in C. loryi Z.
	Triquetrorhabdulus shetlandensis	136.65		Base of E. amblygonium Zone
	Micranthololithus speetonensis	137.97		Base of Dichotomites spp. Zone.
	Nannoconus oviformis, Kokia borealis	139.98		Base of Paratollia Zone
	Sollasites arcuatus	140.04		75% up in P. albidum Zone.  SEPM'98 assigned LAD as 1/10 up in T. pertransiens Z.
	Nannoconus sp. (discs)	140.24	dashed	DASH at base of P. albidum Zone.  SEPM'98 assigned LAD as 4/10 up in T. otopeta Z.
	Stephanolithion atmetros	148.39		90% up in fittoni Zone.  This is Bown's definition for base of NJ18, and others confusingly, has a different NJ18 (and marker) that has nothing to do with this Boreal succession.
	Stephanolithion bigotii bigotii	148.66		20% up in P. rotunda Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of P. pallasiodes Z. 
	Anfractus harrisonii	150.63		Base of elegans Zone.
	Hexapodorhabdus cuvillieri	150.90		50% up in A. autissiodorensis Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of A. autissiodorensis Z..   Another marker for base of NJ16.
	Crepidolithus perforata	154.97		Base of R. cymodoce Zone (Bown and Cooper, 2000).  Formerly called M. perforata.
	Lotharingius crucicentralis	156.30		95% up in A. regulare Zone (high-Boreal) (Bown and Cooper, 2000).  SEPM chart had LAD at base of A. rosenkrantzi Zone.
	Stephanolithion bigotii maximum	159.61		Base of P. plicatilus Zone (Bown and Cooper, 2000).  SEPM chart had LAD is near top (80% up) of C. cordatum s.z.  [uppermost C. cordatum Zone].
	Ansulasphaera helvetica	161.69		40% up in Q. lamberti Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of Q. lamberti s.z. (mid-Q. lamberti Zone) . Another marker for base of NJ14.
	Stephanolithion hexum	162.60		DASH at 75% up in E. coronatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD is base of K. jason Zone.
	Lotharingius velatus	163.37		50% up in S. caloviense Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 6/10 up in K. enodatum s.z. (uppermost S. calloviense Zone).
	Stephanolithion speciosum octum, Steph. spec. speciosum	163.88		50% up in P. koenigi Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of curtilobus s.z. of P. koenigi Z.
	Pseudoconus enigma	164.25		95% up in M. herveyi Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of P. koenigi Zone.
	Tetrapodorhabdus shawensis	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of O. orbis Zone
	Carinolithus magharensis	168.89		95% up in S. niortense Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 6/10 up in S.niortense Z., schroederi s.z.
	Carinolithus superbus	170.17		10% up in S. humphriesianum Zone (Bown and Cooper, 2000).  SEPM chart had LAD in middle of humpriesianum s.z. (middle of S. humpriesianum Zone).
	Biscutum constans	170.25		95% up in S. propinquans Zone (E. sauzei Zone) (Bown and Cooper, 2000).  Also called D. constans.  SEPM chart had LAD at 6/10 up in hebridica s.z. of E. sauzei Z.
	Bussonius prinsii	172.49		Base of G. concavum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at base of G. concavum Zone.
	Crepidolithus impontus	173.51		90% up in L. murchinsonae Zone.  Also called C. cavus.   (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10ths up in B. bradfordensis s.z. (lower B. bradfordensis Z.,)
	Lotharingius hauffii (acme)	180.50		Top of Acme is at base of G. thouarsense Zone (Bown and Cooper, 2000).
	Orthogonoides hamiltoniae	181.35		90% up in H. faclciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD in middle of H. pseudoserpentinum s.z. (H. falciferum Zone)
	Biscutum finchii	181.95		Middle of H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD t 9/10 up in H. exaratum s.z. (= stranewaysi s.z.; lower H. falciferum Zone)
	Calcivascularis jansae	182.63		 This is another marker for base of NJ6.  LAD at 5% up in H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 3/10 up in H. exaratum s.z. H. exaratum s.z. (= strangewaysi s.z.; lower H. falciferum Zone). 
	Crucirhabdus primulus	182.94		20% up in D. tenuicostatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10 up in P. paltus s.z. of D. tenuicostatum Z.
	Parhabdolithus robustus	188.22		Coeval with FAD of C. pliensbachensis (40% up in T. ibex Zone) (Bown and Cooper, 2000).  Not on SEPM chart in Boreal column, but Tethyan column has FAD (but this LAD is approximate base of P. brevispina s.z. (middle of U. jamesoni Zone)
	Crepidolithus pliensbachensis	188.22		40% up in T. ibex Zone (Bown and Cooper, 2000).  SEPM chart had LAD is approximately at base of beirense s.z. (T. ibex Zone).
	Parhabdolithus marthae	194.19		90% up in A. semicostatum Zone (Bown and Cooper, 2000).  SEPM chart had LAD at 7/10 up in E. sauzeanum s.z. (upper A. semicostatum Zone)
	Prinsiosphaera triassica (nannolith, Incertae sedis), Eoconusphaera ziambachensis (nannolith, Incertae sedis), Crucirhabdus minutus (coccolith), Archaeozygodiscus koessenensis (Ioxolith)	199.60		Base of Hettangian (Bown and Cooper, 2000).
	Orthopithonella misurinae,  Obliquipithonella prasina, Carnicalyxia tabellata, Cassianospica curvata	216.53
FAD
	Cribrosphaerella daniae (oldest possible)	66.62		Burnett'98 schematically shows as about middle of B. baltica / danica Belemnite Zone (NW Europe).  SEPM'98 assigned FAD as 3/10 up between top of J. nebrascensis Z. and end of Maastrichtian
	Arkhangelskiella maastrichtiana	67.85		Burnett'98 schematically shows as about 85% up in B. argenta / junior Belemnite Zone (NW Europe).
	Nephrolithus frequens (oldest possible)	68.19		Burnett'98 states that N. frequens has a well-documented diachronous FO", which is youngest at northern high latitudes.  Burnett'98 schematically shows as about 40% up in B. argenta / junior Belemnite Zone (NW Europe).   SEPM'98 assigned FAD as 3/10 up between top of J. nebrascensis Z. and end of Maastrichtian
	Lithraphidites quadratus	68.60		Burnett'98 schematically shows as about 85% up in B. junior / tegulatus Belemnite Zone (NW Europe).
	Prediscosphaera stoveri	72.58		Burnett'98 schematically shows as about 50% up in B. minor Belemnite zone of NW Europe (used here), or about middle of B. stevensoni Zone of N. Amer.   SEPM'98 assigned FAD as nearly 5 myr Older at 4/10 up in B. sp. (smooth) Z.
	Reinhardtites levis, Lithraphidites praequadratus	72.63		Burnett'98 implied that apparent FAD is much later in Boreal realm than in Tethyan/temperate; and assigned schematically shows as about 50% up in B. minor Belemnite zone of NW Europe (used here), or as equivalent to base of D. stevensoni Zone of N.Amer (but, these don't correlate  using SEPM'98).  She notes that L. praequadratus first occurs with R. levis in this subzone in N. Germany.  SEPM'98 assigned FAD as nearly 5 myr Older at top of B. sp. (smooth) Z.
	Heteromarginatus bugensis	78.38		Burnett'98 schematically shows as about middle of "B. perplexus" Zone of N. Amer., so that "perplexus" trio is combined here.
	Misceomarginatus pleiniporus, Misceo. quaternarius	80.64		Burnett'98 shows schematically as base of B. obtusus Zone of N. Amer. (= base of Middle Campanian)  SEPM'98 assigned FAD as 6/10 up in S. hippocrepis II Z.  These two taxa are quite similar (and may be synonymous).
	Broinsonia parca constricta	81.38		Burnett'98 schematically shows as about 60% up in S. hippocrepis III Zone of N. Amer. 
	Broinsonia parca parca	81.47		Burnett'98 schematically shows as about 40% up in S. hippocrepis III Zone of N. Amer.  SEPM'98 assigned FAD as 3/10 up in S. hippocrepis I Zone.  Subzone UC14a is very brief.
	Broinsonia magnum	81.92		Burnett'98 shows schematically as middle of S. hippocrepis II Zone of N. Amer.  SEPM'98 had assigned FAD as base of S. hippocrepis I Zone.
	Orastrum campanensis (FCO)	82.89		Burnett'98 shows schematically as base of S. hippocrepis I Zone of N. Amer.  SEPM'98 assigned FAD as just above base of Campanian.
	Arkhangelskiella cymbiformis	83.21		Arkhangelskiella cymbiformis (sensu Burnett'98b) FAD is schematically by Burnett'98 shown as middle of S. leei III Zone of N. Amer.
	Calculites obscurus	85.95		Burnett'98 notes that "consistent occurrence of rare to frequent Calculites obscurus has been recorded in this zone (UC11c), but cannot be relied on as a datum since the form has been observed to occur well below this level, albeit sporadically and very rarely (as has Calculites ovalis)."  Placed here as "FCO" and arbitrarily in middle of Zone UC11c.  SEPM'98 assigned FAD much higher, as top of C. choteauensis Zone.
	Lucianorhabdus cayeuxii	86.96		Schematic diagram in Burnett'98 suggests about base of P. serratomarginatus ammonite Zone.   In contrast, Boreal column in SEPM'98 assigned FAD nearly 2 myr Higher -- just below top of C. saxitonianus-I. undulatoplicatus Zone in mid-Santonian !!  Subzone UC11a is very brief.
	Lithastrinus grillii	87.45		Schematic diagram in Burnett'98 suggests about 40% up in G. margae ammonite Zone.
	Reinhardtites anthophorus	88.01	dashed	DASH:  SEPM'98 assigned FAD as 1/10 up in C. saxitonianus -I. undulatoplicatus Z.  However, Burnett'98 notes that "FO of Reinhardtites anthophorus is an unreliable datum.  Its inception, which is widely believed to be in the Coniacian, is somewhat obscure.  (etc).  Therefore, assigned here as mid-Zone UC10 (Burnett's placement of its discussion) with a Dash.
	Micula stauropora	88.58		Burnett'98 assigns as essentially at base of P. tridorsatum Zone.
	Broinsonia parca expansa	89.07		Burnett'98 assigns as essentially at base of F. petrocoriensis Zone.  Same as "B. lacunosa" and "Aspidolithus parcus expansus" of some authors.
	Zeugrhabdotus biperforatus	90.25		Schematic diagram in Burnett'98 suggests about 1/6th up in "super" S. neptuni Zone (version used in GTS04 includes "overlying" Prionocyclus germari Zone".
	Lithastrinus septenarius	91.22		Same as L. "moratus" of Varol, 1992.  Schematic diagram in Burnett'98 suggests about 20% up in R. ornatissimum subzone of C. woollgari Zone.
	Lucianorhabdus quadrifidus	91.61		Schematic diagram in Burnett'98 suggests about 25% up in R. kallesi subzone of C. woollgari Zone.
	Kamptnerius magnificus (FCO)	92.24		Burnett'98 "FO of consistently-occurring K. magnificus lies areound the FO of E. eximius."
	Eiffellithus eximius	92.24		Schematic diagram in Burnett'98 suggests about 80% up in M. nodosoides Zone.   SEPM'98 assigned FAD at about 1 myr higher.
	Quadrum gartneri	92.51		Schematic diagram in Burnett'98 suggests about 1/3rd up in M. nodosoides Zone.  In contrast, Boreal column in SEPM'98 had placed Q. garneri FAD as Cenomanian (!!) at 4/10 up in N. juddii Z.
	Lucianorhabdus maleformis	92.51		Burnett'98 assigned this FAD at same level as Q. garneri FAD.  SEPM'98 assigned FAD at about 1 myr higher.
	Marthasterites furcatus	92.89		Burnett'98 "Marthasterites furcatus first occurs here (Zone UC6b) at higher paleolatitudes." AND, notes that "Personal observations have shown that this event is unreliable, the FO lying stratigraphically much lower at higher latitudes."  Arbitrarily placed in middle of Zone UC6b.  SEPM'98 assigned FAD nearly 3 myr higher, at top of S. whitfieldi Z, which is where Crux'92 found it in South England.
	Eprolithus moratus	93.27		Same as "E. eptapetalus" of Varol '92.  Base of subzone corresponds to extinction of Ceratolithina spp. In 'austral' province.  K. magnificus has its local FAD here in N. England. Burnett'98 assigns LAD to middle of W. devonense Zone (or, about 1/3rd up in super-zone of W. coloradoense)
	Quadrum intermedium	93.62		This is the 5-element Q. intermedium. Schematic diagram in Burnett'98 suggests about 50% up in N. juddii Zone.
	Cylindralithus biarcus	93.98		Schematic diagram in Burnett'98 suggests about 10% up in M. geslinianum Zone.
	Lithraphidites acutus	96.01		Burnett'98 assigns as base of C. inerme Zone.  SEPM'98 assigned FAD as slightly higher (by about 0.3 myr) as 25% up in T. costatus subzone of A. rhotomagense Zone.
	Cylindralithus sculptus	96.91		Schematic diagram in Burnett'98 suggests about 50% up in M. dixoni Zone.
	Gartnerago segmentatum	97.72		Called "G. obliquum" by some authors; but Burnett'98  indicates that true "obliquum" comes in within mid-UC2c, or about 1 myr higher.  Burnett'98 assigns as basal (but not base) of M. dixoni ammonite zone, so set as 5% up here.
	Kamptnerius magnificus (rare), Helicolithus anceps	98.89		Schematic diagram in Burnett'98 suggests about 75% up in N. carcitanense subzone.  These taxa may not occur (or are too rare) until later in more oceanic or southern locations.
	Corollithion kennedyi	99.19		40% up in N. carcitanense subzone (Jackie Lee).  SEPM'98 assigned FAD as 8/10 up in [blank] Z.
	Calculites anfractus (rare)	99.82		80% up in S. dispar Zone.  Was suggested as datum for a base of Zone "BC27c", but probably too rare to be useful [Sudeep Kanungo, UCL thesis, June 2005; and pers. commun., Oct 2005 at EGI]
	Eiffellithus turriseiffelii	101.49		90% up in M. inflatum Zone.  SEPM'98 assigned FAD as 7/10 up in E. loricatus Z., E. meandrinus s.z.
	Eiffellithus monechiae	103.13		60% up in M. inflatum Zone
	Tequlalithus tessellatus, Gartnerago praeobliquum	104.78		30% up in M. inflatum Zone
	Ceratolithina hamata	106.89		20% up in E. lautus Zone.
	Ceratolithina bicornuta, Owenia hillae	107.01		Base of E. lautus Zone.
	Axopodorhabdus albianus	107.07		Just below top (95%) of E. loricatus Zone.  SEPM'98 assigned FAD as 7/10 up in D. mammillatum Z., P. steinmani s.z.
	Tranolithus orionatus  (=T. phacelosus)	108.62	dashed	DASH at 25% up in H. dentatus Zone.  SEPM'98 assigned FAD as 7/10 up in D. mammillatum Z., P. steinmani s.z.
	Crucicribrum anglicum	108.62	dashed	DASH at 25% up in H. dentatus Zone; uncertainty spans lower 2/3rds of Zone.
	Prediscosphaera columnata	111.41	dashed	DASH at middle of L. tardefurcata Zone (uncertainty ranges through entire zone).  SEPM'98 assigned FAD as top of L. tardefurcata Z., L. regularis s.z.
	Seribiscutum primitivum, Acaenolithus viriosus	112.30		90% up in H. jacobi Zone
	Nannoconus truitti (acme)	119.35		55% up in C. martinoides Zone.  SEPM'98 assigned FAD as 3/10 up in C. martinoides Z.
	Eprolithus floralis, Braarudosphaera africana, Radiolithus planus	121.90		Base of T. bowerbanki Zone.  SEPM'98 assigned FAD of E. floris is 4/10 up in D. deshayesi Z.; FAD of B. africana is 1/10 up in D. deshayesi Z.
	Lithraphidites moray-firthensis	122.42	dashed	DASH at Middle of D. deshayesi Zone
	Farhania varolii	122.98	dashed	DASH at 95% up in D. forbesi Zone.  SEPM'98 assigned FAD as 3/10 up in D. deshayesi Z.
	Hayesites irregularis, Flabellites oblongus	123.97		Base of D. forbesi Zone.  But, F. oblongus FAD is completely out-of-sequence compared to Tethyan (maybe Bown meant the LAD?), and H. irregularis FAD is nearly 1 myr after its Tethyan FAD.
	Rhagodiscus gallagheri	125.00		Base of P. fissicostatus Zone (base of Aptian)
	Acaenolithus sp. 1	127.91		Just above base (10%) of P. denckmanni Zone.
	Zeugrhabdotus scutula (acme)	128.60		Just above base (5%) of P. elegans Zone.
	Nannoconus pseudoseptentrionalis	128.60		Just above base (5%) of P. elegans Zone.
	Nannoconus borealis	128.97		Base of H. fissicostatum Zone.
	Nannoconus abundans	129.97		Base of P. rarocinctum Zone.  SEPM'98 assigned FAD as 3/10 up in S. hugii Z.
	Rucinolithus terebrodentarius	130.12		85% up in S. variabilis subzone.  Also called Assipetra terebrodetarius.
	Cretarhabdus inaequalis	133.09		65% up in M. speetonensis Zone
	Tegulalithus septentrionalis	133.46		25% up in M. speetonensis Zone
	Zeugrhabdotus scutula, Perissocyclus plethotretus	133.77		85% up in S. inversum Zone.  P.Bown uses Peri. plethotretus FAD to define base of brief BC8c subzone.
	Rucinolithus windleyae	133.94		Middle of S. inversum Zone.
	Tegumentum octiformis	134.86		30% up in E. regale Zone
	Repagulum parvidentatum	135.70		Middle of E. noricum Zone
	Eprolithus? antiquus	136.41		60% up in E. amblygonium Zone.  SEPM'98 assigned FAD as 1/10 up in A. radiatus Z.
	Conusphaera rothii	136.63		Base (5% up) of E. amblygonium Zone.  Secondary marker for base of BC6.  SEPM'98 assigned FAD as 5/10 up in N. pachydicranus Z., H. trinodosum s.z.
	Eiffellithus striatus	136.86		DASH at base of densicostatus Zone (probably equivalent to base of Olcostephanus spp. Zone.
	Zeugrhabdotus diplogrammus, Zeug. trivectis	137.97		Base of Dichotomites spp. Zone.
	Eiffellithus windii	139.40		Base of P. clarkei subzone (middle of Polyptychites Zone)
	Influx of Crucielipsis cuvilleri & Speetonia colligata	139.77		Base of Polyptychites Zone
	Micranthololithus speetonensis	139.92		Base of P. heteropleurum subzone (middle of Polyptyhites Zone).  SEPM'98 assigned FAD as 8/10 up in T. pertransiens Z.
	Triquetrorhabdulus shetlandensis	139.95		Middle of P. robustum subzone (lowermost Paratollia Zone).  Used to subdivide BC3 into very-brief a/b subzones.
	Sollasites arcuatus	140.18		25% up in P. albidum Zone.  SEPM'98 assigned FAD as 8/10 up in T. otopeta Z.
	Retecapsa augustiforata	141.66		DASH at Base of S. icenii Zone (uncertain ranges through entire Ryazinian!).  Alternate name was C. angustiforatus.  SEPM'98 assigned FAD as 8/10 up in T. occitanica Z., D. dalmasi s.z.
	Rhagodiscus asper, Crucielipsis cuvilleri, Bukrylithus ambiguus, Crucibiscutum salebrosum, etc.	141.66	dashed	DASH at base of S. icenii Zone (uncertain ranges through entire Ryazinian!)
	Stephanolithion atmetros	150.37		Base of P. scitulus Zone  (Bown and Cooper, 2000).  SEPM chart had FAD in middle of P. pectinatus Z.
	Stephanolithion brevispinus	151.01		30% up in A. autissiodorensis Zone (Bown and Cooper, 2000).  Former name was S. helotatus.  SEPM chart had FAD at base of A. autissiodorensis Z..  ANOTHER COMMENT AT CELL: This genus extends downward to the Aulacostephanus (Pseudomutabilis) eudoxus. Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Stephanolithion bigotii maximum	161.61		50% up in Q. lamberti Zone (Bown and Cooper, 2000).  SEPM chart also had FAD at base of Q. lamberti s.z. (mid-Q. lamberti Zone) 
	Crepidolithus perforata	163.20		Base of K. jason Zone (Bown and Cooper, 2000).  Not on SEPM chart.  But DTS2000 (Source of information?) had FAD as 7/10 up in K. enodatum s.z. (uppermost S. calloviense Zone). 
	Stephanolithion bigotii bigotii	163.37		50% up in S. caloviense Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of galilei s.z. (P. koenigi Z.one)
	Triscutum expansus	164.23		Base of P. koenigi Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 1/3rds up in gowerianus s.z. (basal P. koenigi Zone)
	Axopodorhabdus rahla	164.74		Base of M. herveyi Zone (Bown and Cooper, 2000).  SEPM chart also had FAD at base of M. herveyi Zone (base of Callovian)
	Ansulasphaera helvetica	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had FAD Just above (0.05 myr) base of O. orbis Zone.
	Stephanolithion hexum	165.50		5% up in O. orbis (O. aspidoides) Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of O. orbis Zone
	Pseudoconus enigma	168.24		5% up in P. parkinsoni Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of P. acris s.z. of lower P. parkinsoni Z.   ANOTHER COMMENT AT THIS CELL:  This genus extends downward to the Strenoceras (Garantiana) garantiana zone (tetragona s.z.). Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982.
	Stephanolithion speciosum octum, Hexapodorhabdus cuvillieri, T. shawensis	168.24		Set of FADs at 5% up in P. parkinsoni Zone (coeval with FAD of P. enigma) (Bown and Cooper, 2000).  J. Bergen suggests the FAD of S. speciosum octum would be a preferable marker for base of Zone NJ11.   SEPM chart had FAD at base of P. parkisoni Zone
	Stephanolithion speciosum	170.20		5% up in S. humphriesianum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 3/10th up in romani s.z. (lowermost S. humphriesianum Zone).
	Ellipsagelosphaera britannica	171.15		10% up in W. laeviuscula Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of W. laeviuscula Z.
	Lotharingius contractus	174.18		40% up in L. murchinsonae Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 1/10 up in upper L. haugi s.z. (middle of L. murchinsonae Z.).  ANOTHER COMMENT AT THIS CELL:   This genus extends downward to Leioceras opalinum zone (bifidatum s.z.).
	Retecapsa incompta	177.17		70% up in D. levesquei Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of D. pseudoradiosa Zone
	Biscutum intermedium	177.17		FAD is coeval with R. incompta FAD (70% up in D. levesquei Z.)  (Bown and Cooper, 2000).  SEPM chart had
	Discorhabdus criotus	180.70		Base of H. variabilis Zone.  Also called Biscutum criotum.   (Bown and Cooper, 2000).  SEPM chart had FAD in middle of H.variabilis Z.
	Discorhabdus striatus	181.35		90% up in H. faclciferum Zone.  Also called Biscutum striatum.   (Bown and Cooper, 2000).  SEPM chart had FAD at 8/10 up in H. falciferum s.z. (upper H. falciferum Zone)
	Carinolithus superbus	182.63		5% up in H. falciferum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 3/10 up in H. exaratum s.z. H. exaratum s.z. (= strangewaysi s.z.; lower H. falciferum Zone)
	Lotharingius sigillatus	183.60		Middle of P. spinatum Zone (Bown and Cooper, 2000).  SEPM chart had FAD is just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. The set of FADs of A. atavus, C. impontus and L. sigillatus and maybe B. prinsii (but see comments on its FAD about 5 myr below) are markers for base of NJ5b.
	Crepidolithus impontus	184.08		10% up in P. spinatum Zone (called "C. cavus" in earlier zonations and SEPM chart). (Bown and Cooper, 2000).  Not on SEPM chart in Boreal columns, but Tethyan FAD was approximate middle of meneghini s.z.   ANOTHER COMMENT AT THIS CELL:   This genus extends downward to the Amaltheus margaritatus zone (Amaltheus gibbosus s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Axopodorhabdus atavus	184.08		Coeval with FAD of C. impontus (10% up in P. spinatum Zone) (Bown and Cooper, 2000).  SEPM chart had FAD at just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. The set of FADs of A. atavus, C. impontus and L. sigillatus and maybe B. prinsii (but see comments on its FAD about 5 myr below) are markers for base of NJ5b.
	Lotharingius hauffii	185.30		60% up in A. margaritatus Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 8/10 up in cornacaldense s.z. (upper lavinianum Zone).
	Biscutum novum	185.58		50% up in A. margaritatus Zone (Bown and Cooper, 2000).  Also known as D. novus.   SEPM chart had FAD in middle of E. raricostatum Z. 
	Biscutum finchii	185.85		40% up in A. margaritatus Zone  (Bown and Cooper, 2000).  Not on SEPM chart (at least not in Boreal column).  FAD is 6/10 up in A. capricornus s.z. (P. davoei Z.one)
	Similiscutum cruciulus	189.07		Middle of U. jamesoni Zone (Bown and Cooper, 2000).  SEPM chart had FAD at approximate base of U. jamesoni s.z. (upper U. jamesoni Zone)
	Bussonius prinsii	189.60	dashed	DASH -- FAD is poorly constrained, and may be as low as base of Pliensbachian  (Bown and Cooper, 2000).  SEPM chart had FAD as just above (0.03 myr) base of acuratum s.z. (middle of algovianum Zone. ANOTHER COMMENT AT THIS CELL:   This genus extends downward to the Amaltheus margaritatus zone (Amaltheus gibbosus s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982.
	Crepidolithus crassus	191.87		20% up in O. oxynotum Zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of A. stellare s.z. ( A. obtusum Zone).   ANOTHER COMMENT AT THIS CELL:   The Nannofossil "Crepidolithus" genus extends downward to the E. raricostatum zone (Crucilobiceras densinodulum s.z.).  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Orthogonoides hamiltoniae	191.87		Coeval with FAD of C. crassus  (Bown and Cooper, 2000).  SEPM chart had FAD is 4/10 up in O. simpsoni s.z. (lower O. oxynotum Zone)
	Parhabdolithus robustus	193.66		Middle of C. turneri Zone (Bown and Cooper, 2000).  SEPM chart had
	Crepidolithus pliensbachensis	195.28		Base of A. semicostatum Zone (Bown and Cooper, 2000).  SEPM chart had FAD at 7/10 up in  charlesi s.z. (lower A. semicostatum Zone)
	Parhabdolithus marthae	195.89		Middle of A. bucklandi zone (Bown and Cooper, 2000).  SEPM chart had FAD in middle of C. rotiforme s.z. (middle A. bucklandi Zone) 
	Parhabdolithus liasicus	196.69		75% up in S. angulata Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of Sinemurian stage. 
	Mitrolithus elegans	196.69		Coeval with P. liasicus  (Bown and Cooper, 2000).  SEPM chart had FAD in middle of A. bucklandi s.z.(upper A. bucklandi Zone)
	Tubirhabdus patulus	196.89		Middle of S. angulata Zone (Bown and Cooper, 2000).  SEPM chart had FAD at base of S. complanata s.z. (upper S. angulata Zone)
	Crucirhabdus primulus	199.21		DASH -- Bown and Cooper (2000) give it a vague placement within NJ1 zone.  Not on SEPM chart in Boreal column, but Tethyan FAD is given as approximately base of C. johnstoni s.z. (middle of P. planorbis Zone).
	Schizosphaerella punctulata	199.60		Base of Hettangian, but Bown indicates FAD might be as high as mid-Hettangian (Bown and Cooper, 2000).  SEPM chart had FAD at base of Jurassic  ANOTHER COMMENT AT THIS CELL:   This genus extends to the end of the Jurassic period.  Source: G.B. Hamilton, "A Stratigraphic Index of Calcerous Nannofossils", edited by A.R. Lord, The British Micropaleontological Society, 1982
	Obliquipithonella rhombica (calcisphere)	203.64
	Crucirhabdus primulus	208.58
	Crucirhabdus minutus (coccolith), Archaeozygodiscus koessenensis (Ioxolith)	209.58
	Eoconusphaera ziambachensis (nannolith, Incertae sedis)	210.08
	Prinsiosphaera triassica (nannolith, Incertae sedis)	213.92
	Orthopithonella geometrica (calcisphere)	216.53
	EARLIEST NANNOFOSSILS = Orthopithonella misurinae and Obliquipithonella prasina (calcispheres), Carnicalyxia tabellata and Cassianospica curvata (nannoliths, Incertae sedis)	225.36




Dinoflagellate cysts (N.Atl.)	:	Dinocyst Zone	Dinocyst Subzone	Dinocyst Zone Marker and selected major FAD/LAD	Dinocyst Other FAD/LAD	All N.Atl. Dinocyst Datums Combined	_METACOLUMN_OFF		CENOZOIC = mainly J. Powell in GTS2004 (Neogene and Paleogene figures). CRETACEOUS = mainly mainly J.-C. Foucher and E. Monteil (in Hardenbol et al., SEPM charts, 1998).  JURASSIC = Poulsen and Riding (2003)

Dinocyst Zone	block	45	214/235/182	notitle
	TOP	0
	D21	4.13
	D20	7.53
	D19	11.40
	D18	14.78
	D17	19.04
	D16	24.36
	D15	30.26
	D14	33.00
	D15	33.62
	D12	37.16
	D11	38.79
	D10	42.66
	D9	50.53
	D8	52.15
	D7	53.76
	D6	54.34
	D5	56.23
	D4	59.47
	D3	61.72
	D2	63.21
	D1	65.50
	TOP	85.56
	S. rot.	92.13
	F. fer.	94.75
	L. siph.	100.94
	C. int.	106.42
	S. cret.	108.77
	P. ali.	111.12
	(un-named)	125.00
	O. oper.	129.93
	S. terr.	132.76
	D. nan.	139.63
	S. ram.	139.96
	P. pell.	140.70
	DSJ39	145.63
	DSJ38	146.32
	DSJ37	147.41
	DSJ36	147.71
	DSJ35	148.00
	DSJ34	148.66
	DSJ33	148.92
	DSJ32	149.37
	DSJ31	150.37
	DSJ30	150.63
	DSJ29	153.16
	DSJ28	154.97
	DSJ27	155.65
	DSJ26	156.27
	DSJ25	157.15
	DSJ24	158.06
	DSJ23	158.69
	DSJ22	159.61
	DSJ21	160.66
	DSJ20	161.21
	DSJ19	162.52
	DSJ18	164.23
	DSJ17	165.13
	DSJ16	166.50
	DSJ15	167.68
	DSJ14	169.64
	DSJ13	170.23
	DSJ12	171.60
	DSJ11	174.71
	DSJ10	178.54
	DSJ9	181.20
	DSJ8	182.75
	DSJ7	183.00
	DSJ6	186.95
	DSJ5	187.35
	DSJ4	189.60
	DSJ3	193.25
	DSJ2	195.16
	DSJ1	203.64

Dinocyst Subzone	block	30	214/235/182	notitle
	TOP	0
	c	0.44
	b	2.39
	a	4.13
	b	5.00
	a	7.53
	b	8.77
	a	11.40
	c	12.82
	b	13.23
	a	14.78
	b	15.97
	a	19.04
	c	21.99
	b	23.03
	a	24.36
	c	27.60
	b	29.19
	a	30.26
	b	30.87
	a	33.00
	TOP	33.62
	c	34.36
	b	36.25
	a	37.16
	b	38.22
	a	38.79
	b	39.42
	a	42.66
	e	46.29
	d	46.67
	c	47.05
	b	49.64
	a	50.53
	c	51.18
	b	51.69
	a	52.15
	c	52.77
	b	53.36
	a	53.76
	b	54.09
	a	54.34
	b	55.73
	a	56.23
	c	56.97
	b	57.78
	b	58.74
	a	59.47
	b	60.92
	a	61.72
	b	62.26
	a	63.21
	c	64.54
	b	64.91
	a	65.50
	TOP	125.00
	P. cret.	128.32
	P. ana.	129.82
	V. mag.	129.93
	N. vet.	130.00
	C. ret.	132.76
	B. long.	135.15
	K. sim.	139.63
	TOP	140.70
	c	142.03


Dinocyst Zone Marker and selected major FAD/LAD	event		220/235/198
LAD
	Tectatodinium pellitum	0.44
	Invertocysta tabulata	2.39
	Reticulatosphaera actinocoronata	4.13
	Barssidinium evangelinae	5.00
	Hystrichosphaeropsis obscura	7.53
	Palaeocystodinium golzowense	8.77
	Palaeocystodinium sp. A (Costa & Downie 1979)	11.40
	Achomosphaera alcicornu	12.82
	Unipontidinium aquaeductum	13.23
	Cousteaudinium aubryae	14.78
	Apteodinium spiridoides	15.97
	Exochosphaeridium insigne	19.04
	Deflandrea phosphoritica	21.99
	Membranophoridium aspinatum	23.03
	Distatodinium biffii	24.36
	Svalbardella cooksoniae	27.60
	Enneadocysta pectiniformis	29.19
	Rhombodinium draco	30.26
	Enneadocysta arcuata	30.87
	Spiniferites sp. 1 (Manum et al. 1989)	33.00
	Glaphyrocysta semitecta	34.36
	Heteraulacacysta porosa	36.25
	Rottnestia borussica	37.16
	Heteraulacacysta? leptalea	38.22
	Areoligera tauloma	39.42
	Cleistosphaeridium diversisphinosum	42.66
	Wetzeliella articulata brevicornuta	46.29
	Dracodinium pachydermum	47.05
	Charlesdowniea columna	49.64
	Membranilarnacia compressa	50.53
	Dracodinium simile	51.18
	Dracodinium politum	51.69
	Dracodinium solidum	52.15
	Deflandrea oebisfeldensis	52.77
	Cerodinium wardenense	53.36
	Phelodinium magnificum	54.34
	Apectodinium augustum	55.73
	Areoligera gippingensis	57.78
	Palaeocystodinium bulliforme	58.74
	Isabelidium? viborgense	59.47
	Damassadiniium californicum	60.92
	Spiniferites cf. supparus	61.72
	Alisocysta reticulata	62.26
	Senoniasphaera inornata	63.21
	Spongodinium delitiense	64.54
	Carpatella cornuta	64.91
	Palynodinium grallator	65.50
	Hystrichodinium pulchrum	69.34
	Odontochitina operculata	69.99
	Palaeoperidinium cretaceum	70.74
	Litosphaeridium siphoniphorum	92.70
	Epelidosphaeridia spinosa	94.68
	Cribroperidinium intricatum	96.01
	Ovoidinium verrucosum verrucosum	99.11
	O. scabrosum	99.60
	Systematophora cretacea, Pterodinium aliferum	104.02
	Muderongia staurota	121.90
	Heslertonia heslertonensis	122.93
	Pseudoceratium pelliferum	125.00
	Batioladinium longicornutum	127.53
	Pseudoceratium anaphrissum	128.08
	Kleithriasphaeridium corrugatum group	128.20
	Canningia cf. reticulata (of Duxbury 1977)	130.00
	Gonyaulacysta teicha, A. eilema, Nelchinopsis kostromiensis	131.44
	Lagenorhytis delicatula, M. macwhaei	136.45
	Egmontodinium torynum	139.94
	Dichadogonyaulax culmula, D. boresphaera, S. arbustum	140.24
	Rotosphaeropsis thula	142.03
	Egmontodinium polyplacophorum, Dingodinium tuberosum	145.63
	Glossodinium dimorphum, Dichadogonyaulax? pannea	146.32
	Scriniodinium inritibile	147.71
	Occisucysta balios	148.00
	Perisseiasphaeridium pannosum	148.66
	Oligosphaeridium patulum	148.92
	Oligosphaeridium patulum (LCO), Cribroperidinium longicorne	149.37
	Subtilisphaera? paeminosa	150.37
	Endoscrinium luridum	150.63
	Aldorfia dictyota pyrum, Stephanelytron scarburghense, Stephanelytron spp.	153.16
	Scriniodinium crystallinum, Nannoceratopsis pellucida,Gonyaulacysta eisenackii	154.97
	Ctenidodinium ornatum	155.65
	Gonyaulacysta jurassica adecta, Atopodinium prostatum	156.66
	Compositosphaeridium polonicum	157.15
	Trichodinium scarburghensis, Rigaudella aemula	158.06
	Lithodinia caytonensis group	158.69
	Wanaea thysanota	159.85
	Liesbergia liesbergensis, Ctenidodinium continuum (rare)	160.66
	Ctenidodinium combazii, Aldorfia aldorfensis	164.23
	Valvaeodinium spinosum	165.13
	Carpathodinium predae	166.50
	Cribroperidinium crispum, Nannoceratopsis senex, Nannoceratopsis gracilis	167.68
	Mancodinium semitabulatum, Durotrigia daveyi, Phallocysta eumekes, Nannoceratopsis gracilis (common), Nannoceratopsis senex (common)	169.64
	Scriniocassis priscus	170.23
	Scriniocassis weberi	171.60
	Ovalicysta hiata, Susadinium knertene, Reutlingia cardobarbata, Susadinium scrofoides, Parvocysta spp. (bullula, nasuta, cracens)	174.71
	Luehndea spinosa	182.75
	Maturodinium inornatum, Valvaeodinium armatum	183.00
	Liasidium variabile	189.60
	Dapcodinium priscum	195.16
	Rhaetogonyaulax rhaetica, Suessia swabiana, Beaumontella? caminuspina, Sverdrupiella mutabilis	200.10
	W. listeri, R. wigginsi, Rhaetogonyaulax rhaetica (LCO)	200.27
	Arctic: Sverdrupiella spp., Noricysta spp., Heibergella spp.	205.71
FAD
	Spiniferites elongatus	0.44
	Spiniferites pachyderma	2.39
	Spiniferites cf. pseudofurcatus	4.13
	Operculodinium tegillatum	5.00
	Selenopemphix armageddonensis	7.53
	Barssidium evangelinae	8.77
	Amiculosphaera umbraculum	11.40
	Gramocysta verricula	12.82
	Achomosphaera andalousiensis	13.23
	Unipontidinium aquaeductum	14.78
	Labyrinthodinium truncatum	15.97
	Sumatradinium druggi	19.04
	Sumatradinium soucouyantae	21.99
	Invertocysta tabulata	23.03
	Tuberculodinium vancampoae	24.36
	Pentadinium laticinctum imaginatum	27.60
	Saturnodinium pansum	29.19
	Apteodinium spiridoides	30.87
	Wetzeliella gochtii	33.00
	Chiropteridium galea	33.62
	Thalassiphora reticulata	34.36
	Thalassiphora fenestrata	36.25
	Rhombodinium perforatum	37.16
	Wetzeliella simplex	38.22
	Rhombodinium porosum	38.79
	Rhombodinium draco	39.42
	Glaphyrocysta intricata	42.66
	Enneadocysta arcuata	46.29
	Phthanoperidinium regalis	46.67
	Dracodinium pachydermum	49.64
	Areosphaeridium diktyoplokum	50.53
	Charlesdowniea aff. clathrata	51.18
	Ochteodinium romanum	51.69
	Charlesdowniea coleothrypta	52.15
	Dracodinium varielongitudum	52.77
	Dracodinium solidum	53.36
	Dracodinium simile	53.76
	Wetzeliella meckelfeldensis	54.09
	Wetzeliella astra	54.34
	Apectodinium augustum	56.23
	Apectodinium homomorphum	56.97
	Rottnestia borussica	57.78
	Areoligera gippingensis	58.74
	Alisocysta margarita	59.47
	Cerodinium depressum	60.92
	Alterbidinium circulum	61.72
	Palaeocystodinium bulliforme	62.26
	Spiniferites cryptovesiculatus	63.21
	Xenicodinium lubricum	64.54
	Tectadodinium rugulatum	64.91
	Carpatella cornuta	65.50
	Palynodinium grallator	66.99
	Triblastula utinensis	69.92
	Ceratiopsis diebelii	73.55
	Areoligera senonensis	74.30
	Palaeoperidinium cretaceum	83.25
	Senoniasphaera protusa	85.56
	Florentinia buspina	90.89
	Senoniasphaera rotundata	92.13
	Florentinia ferox	94.75
	Ovoidinium verrucosum verrucosum	100.40
	Litosphaeridium siphoniphorum	100.94
	Carpodinium obliquicostatum	105.05
	Cribroperidinium intricatum	106.42
	Systematophora cretacea	108.77
	Pterodinium aliferum	111.12
	Hapsocysta peridictya	113.00
	O. scabrosum	116.30
	Endoceratium turneri	121.00
	Ovoidinium diversum	121.90
	Palaeoperidinium cretaceum	128.32
	Pseudoceratium anaphrissum	129.82
	Odontochitina operculata	129.93
	Muderongia staurota	132.56
	Subtilisphaera terrula	132.76
	Batioladinium longicornutum	135.15
	Nelchinopsis kostromiensis, Muderongia crucis	139.49
	Discorsia nanna	139.63
	Spiniferites ramosus group	139.96
	Gochteodinia villosa multifurcata, Systematophora palmula, Muderongia tabulata, Kleithriasphaeridium corrugatum group, Kleithriasphaeridium fasciatum, Ctenidodinium elegantulum, Tehamadinium daveyi, C. speciosum, D. boresphaera, Phoberocysta neocomica 	140.40
	Pseudoceratium pelliferum	140.70
	Endoscrinium pharo, Stiphrosphaeridium arbusum	142.03
	Gochteodinia villosa (consistent)	146.32
	Perisseiasphaeridium insolitum, Dingodinium spinosum	147.41
	Dichadogonyaulax culmula (consistent)	148.00
	Muderongia simplex (consistent) (sp. A of Davey, 1979)	148.92
	Rotosphaeropsis thula, Kleithriasphaeridium porosispinum	149.37
	Systematophora daveyi, Egmontodinium polyplacophorum	150.63
	Perisseiasphaeridium pannosum	152.11
	Cribroperidinium longicorne, Oligosphaeridium patulum	154.97
	Senoniasphaera jurassica (rare)	155.65
	Dingodinium tuberosum, Occisucysta balios	156.27
	Glossodinium dimorphum, Scriniodinium inritibile, Cribroperidinium globatum gr.	158.69
	Endoscrinium luridum	159.61
	Leptodinium subtile, Systematophora areolata gr., Endoscrinium luridum (rare)	160.66
	Wanaea fimbriata	161.21
	Liesbergia liesbergensis, Wanaea thysanota, Trichodinium scarburghensis, Limbodinium absidiatum, Scriniodinium crystallinum	162.52
	Compositosphaeridium polonicum (consistent)	163.20
	Compositosphaeridium polonicum	164.40
	Sirmiodinium grossii, Impletosphaeridium varispinosum	165.13
	Atopodinium prostatum	167.15
	Carpathodinium predae	168.86
	Cribroperidinium crispum, Valvaeodinium spinosum	170.23
	Durotrigia daveyi	171.60
	Nannoceratopsis dictyambonis, Phallocysta elongata, Susadinium scrofoides,	178.54
	Parvocysta nasuta, Phallocysta eumekes, Scriniocassis priscus, S. scrofoides	181.20
	Luehndea spinosa, Nannoceratopsis gracilis, Mancodinium semitabulatum, Valvaeodinium armatum, Maturodinium inornatum	186.95
	Nannoceratopsis senex	187.35
	Liasidium variabile	193.25
	Valvaeodinium koessianum	202.29
	Dapcodinium priscum, Suessia swabiana, B. langii, Beaumontella? caminuspina	203.64
	Arctic: Sverdrupiella spp., Noricysta spp., Hebecysta spp.	207.57
	Rhaetogonyaulax rhaetica, Heibergella spp.	216.53

Dinocyst Other FAD/LAD	event		220/235/198
LAD
	Selenopemphix dionaeacysta	1.62
	Melitasphaeridium choanophorum	3.60
	Spiniferites splendidus	4.13
	Labyrinthodinium truncatum	7.86
	Unipontidinium aquaeductum	12.31
	Ectosphaeropsis burdigalensis	13.73
	Hystrichokolporna cinctum	16.77
	Tityrosphaeridium cantharellus	19.43
	Thalassiphora pelagica	20.54
	Chiropteridium galea	22.27
	Deflandrea phosphoritica	23.03
	Wetzeliella gochtii	26.21
	Areoligera semicirculata	26.60
	Phthanoperidinium amoenum	28.42
	Achilleodinium biformoides	30.52
	Corrudinium incompositum	31.55
	Areosphaeridium diktyoplokum	33.50
	Glaphrocysta intricata	33.95
	Areosphaeridium michoudii	35.30
	Thalassiphora delicata	37.77
	Cerebrocysta bartonensis	39.90
	Phthanoperidinium distinctum	41.18
	Diphyes pseudoficusoides	43.67
	Phthanoperidinium clithridium	44.32
	Diphyes ficusoides	44.50
	Cerebrocysta magna	45.14
	Eatonicysta ursulae	48.05
	Membranilarnacia glabra	48.60
	Dracodinium varielongitudum	48.76
	Dracodinium condylos	51.90
	Alisocysta margarita	58.14
	Palaeoperidinium pyrophorum	58.88
	Fibradinium annetorpense	59.61
	Thalassiphora cf. delicata	61.21
	Alisocysta circumtabulata	61.92
	Spongodinium delitiense	64.22
	Triblastula utinensis	68.11
	Gillina hymenophora	69.34
	Raetiaedinium truncigerum, Aldorfia  deflandrei, Odontochitina costata, Trichodinium castanea	69.99
	Palaeohystrichophora infusorioides	70.74
	T.? spinosa	80.00
	Senoniasphaera protrusa	80.93
	Canningia senonica, Dinopterygium cladoides	83.44
	Ellipsodinium rugulosum	84.86
	Florentinia tenera	85.71
	Florentinia? torulosa	86.41
	Adnatosphaeridium tutulosa, Carpodinium obliquicostatum	93.87
	Dapsilidinium laminaspinosum, Leberidocysta defloccata, Apteodinium granulatum	93.87
	A. perforatum, Canningia torulosa, Disphaeria munda	98.67
	Protoellipsodinium spinocristatum, P. spinosum, Chlamydophorella nyei, Acanthaulax? tenuiceras, Subtilisphaera terrula, Litosphaeridium arundum, Gonyaulacysta helicoidea	100.94
	Carpodinium granulatum	101.62
	Carpodinium granulatum, P. polymorphum	112.00
	Gardodinium trabeculosum	112.70
	Cerbia tabulata	113.00
	Lagenadinium? membranoidium, Achomosphaera? neptuni	118.00
	Callaiosphaeridium tricheryum	121.40
	Ctenidodinium elegantulum	122.31
	Sirmiodinium grossii	122.93
	T. speetonensis, Valensiella magna, C.? cornutum	125.00
	Druggidinium spp., Hystrichosphaeridium arborispinum, Druggidium jubatum	126.65
	Aprobolocysta neistosa, Exiguisphaera plectilis	126.76
	Gonyaulacysta fastigiata, Spiniferites? dentatus	128.32
	Nexosispinum vetusculum	128.66
	Muderongia crucis	128.83
	T. ciliatum	129.32
	Hystrichodinium furcatum	129.37
	Muderongia tabulata, Cribroperidinium confossum	130.00
	Ophiiobolus sp. A of Davey (1979), Oligosphaeridium abaculum	130.37
	Muderongia simplex, Muderongia tetracantha	132.76
	Nematosphaeropsis scala	133.69
	C. validum, Exiguisphaera phragma	133.74
	I. distincta	134.18
	Batioladinium varigranosum	135.59
	Gochteodinia villosa multifurcata	136.24
	Foucheria modesta	139.21
	Systematophora palmula	139.26
	S. primaevus, Kleithriasphaeridium porosispinum	139.77
	C. compta, Tubotuberella apatela, C. speciosum	139.82
	Tehamadinium daveyi	139.90
	Gochteodinia villosa, Endoscrinium pharo	139.96
	Dingodinium? spinosum	139.98
	Batioladinium radiculatum	140.70
	Stiphrosphaeridium dictyophorum	141.71
	Amphorula expirata	142.16
	Senoniasphaera jurassica (rare)	146.32
	Muderongia sp. A of Davey (1979), Senoniasphaera jurassica (consistent)	147.03
	Kleithriaspaeridium telaspinosum	148.39
	Perisseiasphaeridium ingegerdae	149.79
	Subtilisphaera spp., Gonyaulacysta jurassica (rare), Protobatioladinium westburiensis	150.37
	Rhynchodiniopsis cladophora (consistent)	150.50
	Gonyaulacysta jurassica, Perisseiasphaeridium pannosum (LCO)	150.63
	Tubotuborella dangeardii	151.17
	Endoscrinium galeritum	154.97
	Clathroctenocystis asapha	156.78
	Evansia deflandrei, Chytroeisphaeridia cerastes	158.43
	Gonyaulacysta centriconnata, Limbodinium absidiatum	159.61
	Wanaea spp.; Wanaea thysanota	159.85
	Pareodinia prolongata (rare)	160.66
	Wanaea acollaris (rare), C. thullum, Pareodinia prolongata, Lagenadinium callovianum	161.21
	Reutlingia gochtii, Wanaea acollaris	162.01
	Chytroeisphaeridia hyalina	162.86
	Impletosphaeridium varispinosum, L. planoseptata	163.20
	Nannoceratopsis spiculata (rare)	163.54
	Lithodinia reticulata, Rhynchodiniopsis regalis	164.74
	Nannoceratopsis spiculata (common)	165.17
	Hapsidaulax margarethae	165.58
	Atopodinium polygonalis	165.99
	Dissiliodinium willei	166.62
	Lithodinia valensii	167.15
	Bradleyella adela	167.68
	N. ambioni, Nannoceratopsis triceras, Nannoceratopsis dictyambonis, Phallocysta elongata (rare)	170.62
	Moesiodinium raileanui (rare)	171.24
	Phallocysta  elongata (common)	171.60
	Nannoceratopsis plegas, Moesiodinium raileanui (consistent)	174.71
	Cantulodinium protuberatum, Nannoceratopsis triangulata, Valvaeodinium punctatum, Parvocysta spp. (LCO)	175.60
	sphaeromorph acritarchs	180.70
	Nannoceratopsis triceras (common)	182.70
	Luehndea spinosa (consistent)	182.93
	Beaumontella langii	186.95
	Liasidium variabile (LCO)	191.22
	Beaumontella langii (LCO)	195.28
	Valvaeodinium diacrorhaetium	197.28
FAD
	Impagidinium aculeatum	14.95
	Membranilarnacia? picena	21.37
	Max. abundance of Chiropteridium spp. (over 80% of total dinocyst association)	23.03
	Ectosphaeropsis burdigalensis	23.23
	Distatodinium biffii	28.42
	Chiropteridium lobospinosum	31.16
	Heteraulacacysta campanula	34.78
	Polysphaeridium congregatum	38.22
	Corrudinium incompositum	38.79
	Phthanoperidinium comatum (consistent)	49.95
	Pentadinium laticinctum	52.15
	Charlesdowniea crassiramosa	54.24
	Apectodinium parvum	56.47
	Phthanoperidinium crenulatum	57.98
	Deflandrea oebisfeldensis	58.14
	Deflandrea denticulata	58.56
	Cerodinium striatum	63.12
	Alisocysta reticulata	63.79
	Danea californica	65.25
	Spongodinium delitiense	73.55
	Canningia senonica	84.64
	Cannosphaeropsis utinensis	85.04
	Florentinia tenera, T.? spinosa	88.58
	Raetiaedinium truncigerum	89.78
	Florentinia? torulosa	91.88
	Heterosphaeridium difficile	92.13
	Florentinia clavigera	92.70
	Adnatosphaeridium tutulosa	94.20
	Canningia torulosa, Palaeohystrichophora infusorioides	99.90
	Dapsilidinium pumilum, Prolixosphaeridium conulum, Oligosphaeridium prolixispinosum, Kleithriasphaeridium readei, Achomosphaera sagena, Cyclonephelium hughesii, Leberidocysta defloccata, Rhiptocorys veligerum, Odontochitina costata, Endoceratium dettmanniae, Microdinium ornatum, Florentinia deanei	100.94
	Spiniferites? pterotus	106.42
	Xiphophoridium alatum, Psaligonyaulax deflandrei, Wallodinium anglicum, Histiocysta palla, Pervosphaeridium truncatum, Epelidosphaeridia spinosa	106.79
	Ellipsodinium rugulosum, Cyclonephelium membraniphorum	107.01
	A. perforatum	108.33
	Dinopterygium cladoides, Surculosphaeridium? longifurcatum	109.06
	Litosphaeridium arundum	110.90
	Apteodinium granulatum, Xenascus ceratioides	111.12
	Kleithriasphaeridium loffrense	112.00
	Ellipsoidictyum imperfectum	118.00
	Leptodinium cancellatum	121.00
	Surculosphaeridium trunculum, Gonyaulacysta cassidata	122.93
	Muderongia asymmetrica	123.97
	P. spinocristatum, P. polymorphum	125.00
	Carpodinium granulatum, C.? cornutum	127.86
	T. speetonensis, C. parva, P. solocispinum	128.17
	Kleithriasphaeridium? sarmentum, C. tabulata, Exiguisphaera plectilis	128.32
	Stiphrosphaeridium antophorum	128.32
	C. trycherium	131.92
	Florentinia mantellii	132.56
	Coronifera oceanica, Cribroperidinium confossum	132.76
	Gonyaulacysta teicha, Oligosphaeridium abaculum, Subtilisphaera perlucida, Ophiobolus sp. A of Davey (1979)	133.69
	Canningia cf. reticulata (of Duxbury, 1977)	133.74
	Exochosphaeridium phragmites group	134.10
	C. asymmetricum	134.18
	Nexosispinum vetusculum, A. neistosa	135.15
	Gonyaulacysta fastigiata	135.80
	P. spinosum	136.24
	Spiniferites? dentatus, Hystrichosphaeridium arborispinum	136.47
	Batioladinium varigranosum, Nematosphaeropsis scala	139.63
	Exiguisphaera phragma, Kleithriasphaeridium simplicispinum	139.84
	S. primaevus, H. schindewolfii, Muderongia macwhaeli forma B	139.91
	Oligosphaeridium complex, C. validum	139.96
	Achomosphaera neptunii, Heslertonia heslertonensis, Lagenorhytis delicatula, Muderongia simplex	140.22
	Oligosphaeridium diluculum	141.94
	Gochteodinia villosa (rare)	146.71
	Leptodinium deflandrei,  Amphorula expirata	149.76
	Kleithriasphaeridium telaspinosum, Cribroperidinium sp. A Davey (1982)	150.37
	Gochteodinia mutabilis	150.63
	Gochteodinia mutabilis (rare)	151.17
	Subtilisphaera? paeminosa, Perisseiasphaeridium pannosum (FCO)	152.38
	Subtilisphaera? inaffecta, Perisseiasphaeridium pannosum	153.93
	Dichadogonyaulax chondrum (FCO)	157.15
	Gonyaulacysta jurassica jurassica	161.21
	Reutlingia gochtii, Stephanelyron caytonense, Clathroctenocystis asapha, Gonyaulacysta centriconnata, Evansia deflandrei	162.52
	Stephanelytron spp.	164.23
	Chytroeisphaeridia hyalina, Mendicodinium groenlandicum, Gonyaulacysta jurassica (consistent), L. planoseptata, Rhynchodiniopsis cladophora, Reutlingia gochtii (rare), Ctenidodinium ornatum (rare)	164.74
	Pareodinia prolongata	166.21
	Lithodinia reticulata	166.40
	Hapsidaulax margarethae	167.01
	"Complex" skolochorate cysts	167.68
	Atopodinium polygonalis	167.97
	Kalyptea stegasta, Aldorfia aldorfensis, Ctenidodinium spp., Sentusidinium spp. (common), Gonyaulacysta jurassica (rare), Nannoceratopsis pellucida, Sirmiodiniopsis orbis, Ctenidodinium cornigerum	168.86
	Lithodinia valensii	169.64
	Wanaea acollaris, Rhynchodiniopsis? regalis	170.23
	Carpathodinium sp. A, Dissiliodinium giganteum	172.49
	Pareodinia ceratophora, Sentusidinium spp.	174.71
	Nannoceratopsis plegas	175.60
	Wallodinium cylindricum	178.54
	Parvocysta spp. (FCO), Nannoceratopsis triangulata	178.54
	Nannoceratopsis spiculata, Moesiodinium raileanui, Parvocysta spp.	181.20
	Nannoceratopsis triceras (FCO)	183.00
	sphaeromorph acritarchs	183.00
	Nannoceratopsis triceras	186.95
	Valvaeodinium punctatum	187.35
	Mendicodinium reticulatum	189.60
	Liasidium variabile (FCO)	192.04


All N.Atl. Dinocyst Datums Combined	event		220/235/198		off
LAD
	Tectatodinium pellitum	0.44
	Selenopemphix dionaeacysta	1.62
	Invertocysta tabulata	2.39
	Melitasphaeridium choanophorum	3.60
	Spiniferites splendidus	4.13
	Reticulatosphaera actinocoronata	4.13
	Barssidinium evangelinae	5.00
	Hystrichosphaeropsis obscura	7.53
	Labyrinthodinium truncatum	7.86
	Palaeocystodinium golzowense	8.77
	Palaeocystodinium sp. A (Costa & Downie 1979)	11.40
	Unipontidinium aquaeductum	12.31
	Achomosphaera alcicornu	12.82
	Unipontidinium aquaeductum	13.23
	Ectosphaeropsis burdigalensis	13.73
	Cousteaudinium aubryae	14.78
	Apteodinium spiridoides	15.97
	Hystrichokolporna cinctum	16.77
	Exochosphaeridium insigne	19.04
	Tityrosphaeridium cantharellus	19.43
	Thalassiphora pelagica	20.54
	Deflandrea phosphoritica	21.99
	Chiropteridium galea	22.27
	Deflandrea phosphoritica	23.03
	Membranophoridium aspinatum	23.03
	Distatodinium biffii	24.36
	Wetzeliella gochtii	26.21
	Areoligera semicirculata	26.60
	Svalbardella cooksoniae	27.60
	Phthanoperidinium amoenum	28.42
	Enneadocysta pectiniformis	29.19
	Rhombodinium draco	30.26
	Achilleodinium biformoides	30.52
	Enneadocysta arcuata	30.87
	Corrudinium incompositum	31.55
	Spiniferites sp. 1 (Manum et al., 1989)	33.00
	Areosphaeridium diktyoplokum	33.50
	Glaphrocysta intricata	33.95
	Glaphyrocysta semitecta	34.36
	Areosphaeridium michoudii	35.30
	Heteraulacacysta porosa	36.25
	Rottnestia borussica	37.16
	Thalassiphora delicata	37.77
	Heteraulacacysta? leptalea	38.22
	Areoligera tauloma	39.42
	Cerebrocysta bartonensis	39.90
	Phthanoperidinium distinctum	41.18
	Cleistosphaeridium diversisphinosum	42.66
	Diphyes pseudoficusoides	43.67
	Phthanoperidinium clithridium	44.32
	Diphyes ficusoides	44.50
	Cerebrocysta magna	45.14
	Wetzeliella articulata brevicornuta	46.29
	Dracodinium pachydermum	47.05
	Eatonicysta ursulae	48.05
	Membranilarnacia glabra	48.60
	Dracodinium varielongitudum	48.76
	Charlesdowniea columna	49.64
	Membranilarnacia compressa	50.53
	Dracodinium simile	51.18
	Dracodinium politum	51.69
	Dracodinium condylos	51.90
	Dracodinium solidum	52.15
	Deflandrea oebisfeldensis	52.77
	Cerodinium wardenense	53.36
	Phelodinium magnificum	54.34
	Apectodinium augustum	55.73
	Areoligera gippingensis	57.78
	Alisocysta margarita	58.14
	Palaeocystodinium bulliforme	58.74
	Palaeoperidinium pyrophorum	58.88
	Isabelidium? viborgense	59.47
	Fibradinium annetorpense	59.61
	Damassadiniium californicum	60.92
	Thalassiphora cf. delicata	61.21
	Spiniferites cf. supparus	61.72
	Alisocysta circumtabulata	61.92
	Alisocysta reticulata	62.26
	Senoniasphaera inornata	63.21
	Spongodinium delitiense	64.22
	Spongodinium delitiense	64.54
	Carpatella cornuta	64.91
	Palynodinium grallator	65.50
	Triblastula utinensis	68.11
	Gillina hymenophora	69.34
	Hystrichodinium pulchrum	69.34
	Raetiaedinium truncigerum, Aldorfia  deflandrei, Odontochitina costata, Trichodinium castanea	69.99
	Odontochitina operculata	69.99
	Palaeohystrichophora infusorioides	70.74
	Palaeoperidinium cretaceum	70.74
	T.? spinosa	80.00
	Senoniasphaera protrusa	80.93
	Canningia senonica, Dinopterygium cladoides	83.44
	Ellipsodinium rugulosum	84.86
	Florentinia tenera	85.71
	Florentinia? torulosa	86.41
	Litosphaeridium siphoniphorum	92.70
	Adnatosphaeridium tutulosa, Carpodinium obliquicostatum	93.87
	Dapsilidinium laminaspinosum, Leberidocysta defloccata, Apteodinium granulatum	93.87
	Epelidosphaeridia spinosa	94.68
	Cribroperidinium intricatum	96.01
	A. perforatum, Canningia torulosa, Disphaeria munda	98.67
	Ovoidinium verrucosum verrucosum	99.11
	O. scabrosum	99.60
	Protoellipsodinium spinocristatum, P. spinosum, Chlamydophorella nyei, Acanthaulax? tenuiceras, Subtilisphaera terrula, Litosphaeridium arundum, Gonyaulacysta helicoidea	100.94
	Carpodinium granulatum	101.62
	Systematophora cretacea, Pterodinium aliferum	104.02
	Carpodinium granulatum, P. polymorphum	112.00
	Gardodinium trabeculosum	112.70
	Cerbia tabulata	113.00
	Lagenadinium? membranoidium, Achomosphaera? neptuni	118.00
	Callaiosphaeridium tricheryum	121.40
	Muderongia staurota	121.90
	Ctenidodinium elegantulum	122.31
	Sirmiodinium grossii	122.93
	Heslertonia heslertonensis	122.93
	T. speetonensis, Valensiella magna, C.? cornutum	125.00
	Pseudoceratium pelliferum	125.00
	Druggidinium spp., Hystrichosphaeridium arborispinum, Druggidium jubatum	126.65
	Aprobolocysta neistosa, Exiguisphaera plectilis	126.76
	Batioladinium longicornutum	127.53
	Pseudoceratium anaphrissum	128.08
	Kleithriasphaeridium corrugatum group	128.20
	Gonyaulacysta fastigiata, Spiniferites? dentatus	128.32
	Nexosispinum vetusculum	128.66
	Muderongia crucis	128.83
	T. ciliatum	129.32
	Hystrichodinium furcatum	129.37
	Muderongia tabulata, Cribroperidinium confossum	130.00
	Canningia cf. reticulata (of Duxbury, 1977)	130.00
	Ophiiobolus sp. A of Davey (1979), Oligosphaeridium abaculum	130.37
	Gonyaulacysta teicha, A. eilema, Nelchinopsis kostromiensis	131.44
	Muderongia simplex, Muderongia tetracantha	132.76
	Nematosphaeropsis scala	133.69
	C. validum, Exiguisphaera phragma	133.74
	I. distincta	134.18
	Batioladinium varigranosum	135.59
	Gochteodinia villosa multifurcata	136.24
	Lagenorhytis delicatula, M. macwhaei	136.45
	Foucheria modesta	139.21
	Systematophora palmula	139.26
	S. primaevus, Kleithriasphaeridium porosispinum	139.77
	C. compta, Tubotuberella apatela, C. speciosum	139.82
	Tehamadinium daveyi	139.90
	Egmontodinium torynum	139.94
	Gochteodinia villosa, Endoscrinium pharo	139.96
	Dingodinium? spinosum	139.98
	Dichadogonyaulax culmula, D. boresphaera, S. arbustum	140.24
	Batioladinium radiculatum	140.70
	Stiphrosphaeridium dictyophorum	141.71
	Rotosphaeropsis thula	142.03
	Amphorula expirata	142.16
	Egmontodinium polyplacophorum, Dingodinium tuberosum	145.63
	Senoniasphaera jurassica (rare)	146.32
	Glossodinium dimorphum, Dichadogonyaulax? pannea	146.32
	Muderongia sp. A of Davey (1979), Senoniasphaera jurassica (consistent)	147.03
	Scriniodinium inritibile	147.71
	Occisucysta balios	148.00
	Kleithriaspaeridium telaspinosum	148.39
	Perisseiasphaeridium pannosum	148.66
	Oligosphaeridium patulum	148.92
	Oligosphaeridium patulum (LCO), Cribroperidinium longicorne	149.37
	Perisseiasphaeridium ingegerdae	149.79
	Subtilisphaera spp., Gonyaulacysta jurassica (rare), Protobatioladinium westburiensis	150.37
	Subtilisphaera? paeminosa	150.37
	Rhynchodiniopsis cladophora (consistent)	150.50
	Gonyaulacysta jurassica, Perisseiasphaeridium pannosum (LCO)	150.63
	Endoscrinium luridum	150.63
	Tubotuborella dangeardii	151.17
	Aldorfia dictyota pyrum, Stephanelytron scarburghense, Stephanelytron spp.	153.16
	Endoscrinium galeritum	154.97
	Scriniodinium crystallinum, Nannoceratopsis pellucida,Gonyaulacysta eisenackii	154.97
	Ctenidodinium ornatum	155.65
	Gonyaulacysta jurassica adecta, Atopodinium prostatum	156.66
	Clathroctenocystis asapha	156.78
	Compositosphaeridium polonicum	157.15
	Trichodinium scarburghensis, Rigaudella aemula	158.06
	Evansia deflandrei, Chytroeisphaeridia cerastes	158.43
	Lithodinia caytonensis group	158.69
	Gonyaulacysta centriconnata, Limbodinium absidiatum	159.61
	Wanaea spp.; Wanaea thysanota	159.85
	Wanaea thysanota	159.85
	Pareodinia prolongata (rare)	160.66
	Liesbergia liesbergensis, Ctenidodinium continuum (rare)	160.66
	Wanaea acollaris (rare), C. thullum, Pareodinia prolongata, Lagenadinium callovianum	161.21
	Reutlingia gochtii, Wanaea acollaris	162.01
	Chytroeisphaeridia hyalina	162.86
	Impletosphaeridium varispinosum, L. planoseptata	163.20
	Nannoceratopsis spiculata (rare)	163.54
	Ctenidodinium combazii, Aldorfia aldorfensis	164.23
	Lithodinia reticulata, Rhynchodiniopsis regalis	164.74
	Valvaeodinium spinosum	165.13
	Nannoceratopsis spiculata (common)	165.17
	Hapsidaulax margarethae	165.58
	Atopodinium polygonalis	165.99
	Carpathodinium predae	166.50
	Dissiliodinium willei	166.62
	Lithodinia valensii	167.15
	Bradleyella adela	167.68
	Cribroperidinium crispum, Nannoceratopsis senex, Nannoceratopsis gracilis	167.68
	Mancodinium semitabulatum, Durotrigia daveyi, Phallocysta eumekes, Nannoceratopsis gracilis (common), Nannoceratopsis senex (common)	169.64
	Scriniocassis priscus	170.23
	N. ambioni, Nannoceratopsis triceras, Nannoceratopsis dictyambonis, Phallocysta elongata (rare)	170.62
	Moesiodinium raileanui (rare)	171.24
	Phallocysta  elongata (common)	171.60
	Scriniocassis weberi	171.60
	Nannoceratopsis plegas, Moesiodinium raileanui (consistent)	174.71
	Ovalicysta hiata, Susadinium knertene, Reutlingia cardobarbata, Susadinium scrofoides, Parvocysta spp. (bullula, nasuta, cracens)	174.71
	Cantulodinium protuberatum, Nannoceratopsis triangulata, Valvaeodinium punctatum, Parvocysta spp. (LCO)	175.60
	sphaeromorph acritarchs	180.70
	Nannoceratopsis triceras (common)	182.70
	Luehndea spinosa	182.75
	Luehndea spinosa (consistent)	182.93
	Maturodinium inornatum, Valvaeodinium armatum	183.00
	Beaumontella langii	186.95
	Liasidium variabile	189.60
	Liasidium variabile (LCO)	191.22
	Dapcodinium priscum	195.16
	Beaumontella langii (LCO)	195.28
	Valvaeodinium diacrorhaetium	197.28
	Rhaetogonyaulax rhaetica, Suessia swabiana, Beaumontella? caminuspina, Sverdrupiella mutabilis	200.10
	W. listeri, R. wigginsi, Rhaetogonyaulax rhaetica (LCO)	200.27
	Arctic: Sverdrupiella spp., Noricysta spp., Heibergella spp.	205.71
FAD
	Spiniferites elongatus	0.44
	Spiniferites pachyderma	2.39
	Spiniferites cf. pseudofurcatus	4.13
	Operculodinium tegillatum	5.00
	Selenopemphix armageddonensis	7.53
	Barssidium evangelinae	8.77
	Amiculosphaera umbraculum	11.40
	Gramocysta verricula	12.82
	Achomosphaera andalousiensis	13.23
	Unipontidinium aquaeductum	14.78
	Impagidinium aculeatum	14.95
	Labyrinthodinium truncatum	15.97
	Sumatradinium druggi	19.04
	Membranilarnacia? picena	21.37
	Sumatradinium soucouyantae	21.99
	Invertocysta tabulata	23.03
	Max. abundance of Chiropteridium spp. (over 80% of total dinocyst association)	23.03
	Ectosphaeropsis burdigalensis	23.23
	Tuberculodinium vancampoae	24.36
	Pentadinium laticinctum imaginatum	27.60
	Distatodinium biffii	28.42
	Saturnodinium pansum	29.19
	Apteodinium spiridoides	30.87
	Chiropteridium lobospinosum	31.16
	Wetzeliella gochtii	33.00
	Chiropteridium galea	33.62
	Thalassiphora reticulata	34.36
	Heteraulacacysta campanula	34.78
	Thalassiphora fenestrata	36.25
	Rhombodinium perforatum	37.16
	Wetzeliella simplex	38.22
	Polysphaeridium congregatum	38.22
	Rhombodinium porosum	38.79
	Corrudinium incompositum	38.79
	Rhombodinium draco	39.42
	Glaphyrocysta intricata	42.66
	Enneadocysta arcuata	46.29
	Phthanoperidinium regalis	46.67
	Dracodinium pachydermum	49.64
	Phthanoperidinium comatum (consistent)	49.95
	Areosphaeridium diktyoplokum	50.53
	Charlesdowniea aff. clathrata	51.18
	Ochteodinium romanum	51.69
	Charlesdowniea coleothrypta	52.15
	Pentadinium laticinctum	52.15
	Dracodinium varielongitudum	52.77
	Dracodinium solidum	53.36
	Dracodinium simile	53.76
	Wetzeliella meckelfeldensis	54.09
	Charlesdowniea crassiramosa	54.24
	Wetzeliella astra	54.34
	Apectodinium augustum	56.23
	Apectodinium parvum	56.47
	Apectodinium homomorphum	56.97
	Rottnestia borussica	57.78
	Phthanoperidinium crenulatum	57.98
	Deflandrea oebisfeldensis	58.14
	Deflandrea denticulata	58.56
	Areoligera gippingensis	58.74
	Alisocysta margarita	59.47
	Cerodinium depressum	60.92
	Alterbidinium circulum	61.72
	Palaeocystodinium bulliforme	62.26
	Cerodinium striatum	63.12
	Spiniferites cryptovesiculatus	63.21
	Alisocysta reticulata	63.79
	Xenicodinium lubricum	64.54
	Tectadodinium rugulatum	64.91
	Danea californica	65.25
	Carpatella cornuta	65.50
	Palynodinium grallator	66.99
	Triblastula utinensis	69.92
	Ceratiopsis diebelii	73.55
	Spongodinium delitiense	73.55
	Areoligera senonensis	74.30
	Palaeoperidinium cretaceum	83.25
	Canningia senonica	84.64
	Cannosphaeropsis utinensis	85.04
	Senoniasphaera protusa	85.56
	Florentinia tenera, T.? spinosa	88.58
	Raetiaedinium truncigerum	89.78
	Florentinia buspina	90.89
	Florentinia? torulosa	91.88
	Senoniasphaera rotundata	92.13
	Heterosphaeridium difficile	92.13
	Florentinia clavigera	92.70
	Adnatosphaeridium tutulosa	94.20
	Florentinia ferox	94.75
	Canningia torulosa, Palaeohystrichophora infusorioides	99.90
	Ovoidinium verrucosum verrucosum	100.40
	Litosphaeridium siphoniphorum	100.94
	Dapsilidinium pumilum, Prolixosphaeridium conulum, Oligosphaeridium prolixispinosum, Kleithriasphaeridium readei, Achomosphaera sagena, Cyclonephelium hughesii, Leberidocysta defloccata, Rhiptocorys veligerum, Odontochitina costata, Endoceratium dettmanniae, Microdinium ornatum, Florentinia deanei	100.94
	Carpodinium obliquicostatum	105.05
	Cribroperidinium intricatum	106.42
	Spiniferites? pterotus	106.42
	Xiphophoridium alatum, Psaligonyaulax deflandrei, Wallodinium anglicum, Histiocysta palla, Pervosphaeridium truncatum, Epelidosphaeridia spinosa	106.79
	Ellipsodinium rugulosum, Cyclonephelium membraniphorum	107.01
	A. perforatum	108.33
	Systematophora cretacea	108.77
	Dinopterygium cladoides, Surculosphaeridium? longifurcatum	109.06
	Litosphaeridium arundum	110.90
	Pterodinium aliferum	111.12
	Apteodinium granulatum, Xenascus ceratioides	111.12
	Kleithriasphaeridium loffrense	112.00
	Hapsocysta peridictya	113.00
	O. scabrosum	116.30
	Ellipsoidictyum imperfectum	118.00
	Endoceratium turneri	121.00
	Leptodinium cancellatum	121.00
	Ovoidinium diversum	121.90
	Surculosphaeridium trunculum, Gonyaulacysta cassidata	122.93
	Muderongia asymmetrica	123.97
	P. spinocristatum, P. polymorphum	125.00
	Carpodinium granulatum, C.? cornutum	127.86
	T. speetonensis, C. parva, P. solocispinum	128.17
	Palaeoperidinium cretaceum	128.32
	Kleithriasphaeridium? sarmentum, C. tabulata, Exiguisphaera plectilis	128.32
	Stiphrosphaeridium antophorum	128.32
	Pseudoceratium anaphrissum	129.82
	Odontochitina operculata	129.93
	C. trycherium	131.92
	Muderongia staurota	132.56
	Florentinia mantellii	132.56
	Subtilisphaera terrula	132.76
	Coronifera oceanica, Cribroperidinium confossum	132.76
	Gonyaulacysta teicha, Oligosphaeridium abaculum, Subtilisphaera perlucida, Ophiobolus sp. A of Davey (1979)	133.69
	Canningia cf. reticulata (of Duxbury 1977)	133.74
	Exochosphaeridium phragmites group	134.10
	C. asymmetricum	134.18
	Batioladinium longicornutum	135.15
	Nexosispinum vetusculum, A. neistosa	135.15
	Gonyaulacysta fastigiata	135.80
	P. spinosum	136.24
	Spiniferites? dentatus, Hystrichosphaeridium arborispinum	136.47
	Nelchinopsis kostromiensis, Muderongia crucis	139.49
	Discorsia nanna	139.63
	Batioladinium varigranosum, Nematosphaeropsis scala	139.63
	Exiguisphaera phragma, Kleithriasphaeridium simplicispinum	139.84
	S. primaevus, H. schindewolfii, Muderongia macwhaeli forma B	139.91
	Spiniferites ramosus group	139.96
	Oligosphaeridium complex, C. validum	139.96
	Achomosphaera neptunii, Heslertonia heslertonensis, Lagenorhytis delicatula, Muderongia simplex	140.22
	Gochteodinia villosa multifurcata, Systematophora palmula, Muderongia tabulata, Kleithriasphaeridium corrugatum group, Kleithriasphaeridium fasciatum, Ctenidodinium elegantulum, Tehamadinium daveyi, C. speciosum, D. boresphaera, Phoberocysta neocomica 	140.40
	Pseudoceratium pelliferum	140.70
	Oligosphaeridium diluculum	141.94
	Endoscrinium pharo, Stiphrosphaeridium arbusum	142.03
	Gochteodinia villosa (consistent)	146.32
	Gochteodinia villosa (rare)	146.71
	Perisseiasphaeridium insolitum, Dingodinium spinosum	147.41
	Dichadogonyaulax culmula (consistent)	148.00
	Muderongia simplex (consistent) (sp. A of Davey, 1979)	148.92
	Rotosphaeropsis thula, Kleithriasphaeridium porosispinum	149.37
	Leptodinium deflandrei,  Amphorula expirata	149.76
	Kleithriasphaeridium telaspinosum, Cribroperidinium sp. A Davey (1982)	150.37
	Systematophora daveyi, Egmontodinium polyplacophorum	150.63
	Gochteodinia mutabilis	150.63
	Gochteodinia mutabilis (rare)	151.17
	Perisseiasphaeridium pannosum	152.11
	Subtilisphaera? paeminosa, Perisseiasphaeridium pannosum (FCO)	152.38
	Subtilisphaera? inaffecta, Perisseiasphaeridium pannosum	153.93
	Cribroperidinium longicorne, Oligosphaeridium patulum	154.97
	Senoniasphaera jurassica (rare)	155.65
	Dingodinium tuberosum, Occisucysta balios	156.27
	Dichadogonyaulax chondrum (FCO)	157.15
	Glossodinium dimorphum, Scriniodinium inritibile, Cribroperidinium globatum gr.	158.69
	Endoscrinium luridum	159.61
	Leptodinium subtile, Systematophora areolata gr., Endoscrinium luridum (rare)	160.66
	Wanaea fimbriata	161.21
	Gonyaulacysta jurassica jurassica	161.21
	Liesbergia liesbergensis, Wanaea thysanota, Trichodinium scarburghensis, Limbodinium absidiatum, Scriniodinium crystallinum	162.52
	Reutlingia gochtii, Stephanelyron caytonense, Clathroctenocystis asapha, Gonyaulacysta centriconnata, Evansia deflandrei	162.52
	Compositosphaeridium polonicum (consistent)	163.20
	Stephanelytron spp.	164.23
	Compositosphaeridium polonicum	164.40
	Chytroeisphaeridia hyalina, Mendicodinium groenlandicum, Gonyaulacysta jurassica (consistent), L. planoseptata, Rhynchodiniopsis cladophora, Reutlingia gochtii (rare), Ctenidodinium ornatum (rare)	164.74
	Sirmiodinium grossii, Impletosphaeridium varispinosum	165.13
	Pareodinia prolongata	166.21
	Lithodinia reticulata	166.40
	Hapsidaulax margarethae	167.01
	Atopodinium prostatum	167.15
	Complex skolochorate cysts	167.68
	Atopodinium polygonalis	167.97
	Carpathodinium predae	168.86
	Kalyptea stegasta, Aldorfia aldorfensis, Ctenidodinium spp., Sentusidinium spp. (common), Gonyaulacysta jurassica (rare), Nannoceratopsis pellucida, Sirmiodiniopsis orbis, Ctenidodinium cornigerum	168.86
	Lithodinia valensii	169.64
	Cribroperidinium crispum, Valvaeodinium spinosum	170.23
	Wanaea acollaris, Rhynchodiniopsis? regalis	170.23
	Durotrigia daveyi	171.60
	Carpathodinium sp. A, Dissiliodinium giganteum	172.49
	Pareodinia ceratophora, Sentusidinium spp.	174.71
	Nannoceratopsis plegas	175.60
	Nannoceratopsis dictyambonis, Phallocysta elongata, Susadinium scrofoides,	178.54
	Wallodinium cylindricum	178.54
	Parvocysta spp. (FCO), Nannoceratopsis triangulata	178.54
	Parvocysta nasuta, Phallocysta eumekes, Scriniocassis priscus, S. scrofoides	181.20
	Nannoceratopsis spiculata, Moesiodinium raileanui, Parvocysta spp.	181.20
	Nannoceratopsis triceras (FCO)	183.00
	sphaeromorph acritarchs	183.00
	Luehndea spinosa, Nannoceratopsis gracilis, Mancodinium semitabulatum, Valvaeodinium armatum, Maturodinium inornatum	186.95
	Nannoceratopsis triceras	186.95
	Nannoceratopsis senex	187.35
	Valvaeodinium punctatum	187.35
	Mendicodinium reticulatum	189.60
	Liasidium variabile (FCO)	192.04
	Liasidium variabile	193.25
	Valvaeodinium koessianum	202.29
	Dapcodinium priscum, Suessia swabiana, B. langii, Beaumontella? caminuspina	203.64
	Arctic: Sverdrupiella spp., Noricysta spp., Hebecysta spp.	207.57
	Rhaetogonyaulax rhaetica, Heibergella spp.	216.53




Dinoflagellate Cysts (Tethyan)	:	Tethyan Dinocyst Zone	Tethyan Dinocyst Zone Markers and other major FAD/LAD	Other Tethyan Dinocyst FAD/LAD	All Tethyan Dinocyst Datums Combined	_METACOLUMN_OFF		E. Monteil (in Hardenbol et al., SEPM charts, 1998)

Tethyan Dinocyst Zone	block	45	214/235/182	notitle
	TOP	129.47
	K. corr.	137.23
	V. mag.	138.48
	M. aust.	139.77
	M. mac. B	140.21
	M. mac. A	140.89
	F. mod.	141.93
	D. ben.	144.36
	B. john.	148.98

Tethyan Dinocyst Zone Markers and other major FAD/LAD	event		220/235/198
LAD
	Epelidosphaeridia spinosa	92.79
	Cribroperidinium intricatum	93.67
	Litosphaeridium siphoniphorum	93.94
	O. scabrosum	100.24
	Palaeohystrichophora cf. infusorioides	100.48
	Endoceratium turneri	103.95
	Cerbia tabulata	111.85
	Subtilisphaera terrula	119.50
	Lithodinia stoverii	120.00
	Rhynchodiniopsis aptiana	122.67
	Prolixosphaeridium parvispinum	124.12
	Druggidium spp.	125.00
	Pseudoceratium pelliferum	126.10
	Muderongia staurota	126.48
	Valensiella magna	129.47
	Kleithriasphaeridium corrugatum	129.80
	Muderongia macwhaei	131.95
	Aprobolocysta eilema	132.35
	Nelchinopsis kostromiensis	134.07
	Biorbifera johnewingii	137.65
	Druggidium apicopaucicum	137.83
	Dichadogonyaulax bensonii	139.85
	Kleithriasphaeridium fasciatum	140.14
	Cirrusphaera dissimilis	141.93
	Valensiella pygmaea	143.03
	Prolixosphaeridium basifurcatum	143.20
	Lanterna spp.; Lanterna bulgarica	145.73
	Protobatioladinium lunare, Leptodinium mirabile	148.24
	Leptodinium subtile, Dingodinium scabratum	148.61
	Gonyaulacysta jurassica, Protobatioladinium westburiensis, Subtilisphaera? paeminosa	149.89
	Endoscrinium luridum	150.84
	Tubotuberella dangeardii	151.52
	Stephanelytron spp.	152.59
	Scriniodinium crystallinum	153.06
	Surculosphaeridium cribrotubiferum	154.53
	Gonyaulacysta eisenackii, Ctenidodinium ornatum	155.35
	Compositosphaeridium polonicum	156.81
	Wanaea thysanota	158.43
	Wanaea digitata	159.61
	Ctenidodinium combazii	164.35
	S. Hemisphere:  H. balmei	205.71
	S. Hemisphere:  S. ottii	234.56
FAD
	Subtilisphaera pontis-mariae	92.36
	Odontochitina costata, Palaeohystrichophora infusorioides	100.48
	Ovoidinium verrucosum verrucosum, Endoceratium dettmanniae	100.80
	Epelidosphaeridia spinosa	101.08
	Litosphaeridium siphoniphorum	103.27
	Palaeohystrichophora cf. infusorioides	103.95
	Ellipsodinium rugulosum	105.05
	O. scabrosum	117.40
	Palaeoperidinium cretaceum	124.22
	Prolixosphaeridium parvispinum	127.99
	Subtilisphaera terrula	129.47
	Odontochitina operculata	129.84
	Rhynchodiniopsis aptiana	130.61
	Aprobolocysta eilema	133.61
	Muderongia staurota	136.12
	Subtilisphaera perlucida	138.17
	Kleithriasphaeridium corrugatum	137.23
	Valensiella magna	138.48
	Muderongia australis	139.77
	Druggidium apicopaucicum	140.14
	Muderongia macwhaei forma B	140.21
	Muderongia macwhaei forma A	140.89
	Pseudoceratium pelliferum	141.25
	Foucheria modesta	141.93
	Cirrusphaera disimilis	143.03
	Valensiella pygmaea	144.30
	Dichadogonyaulax bensonii	144.36
	Spiniferites ramosus group	144.88
	Warrenia californica	145.73
	Prolixosphaeridium sp. A of Monteil (1993)	147.00
	Biorbifera johnewingii, Cometodinium habibii	148.98
	Lanterna sportula	150.84
	Subtilisphaera? paeminosa	152.59
	Cribroperidinium longicorne, Subtilisphaera? inaffecta	152.83
	Occisucysta balios, Amphorula spp.	153.39
	Glossodinium dimorphum	158.43
	Impletosphaeridium varispinosum	164.23
	Compositosphaeridium polonicum	164.74
	Nannoceratopsis triceras	176.58
	Parvocysta spp., Scriniocassis priscus	180.50
	Mancodinium semitabulatum, Nannoceratopsis gracilis, Scriniocassis weberi, Luehndea spp.	186.95
	Mancodinium spp.	189.60
	Dapcodinium priscum	191.22
	S. Hemisphere:  H. balmei	211.30
	S. Hemisphere:  W. listeri	216.53
	S. Hemisphere:  Suessia swabiana	218.66
	S. Hemisphere:  R. wigginsii	219.81
	S. Hemisphere:  S. ottii	240.00

Other Tethyan Dinocyst FAD/LAD	event		220/235/198
LAD
	T. oblongata	94.38
	Disphaeria munda	94.45
	Gonyaulacysta helicoidea	100.01
	Apteodinium maculatum grande	103.27
	P. polymorphum	111.85
	Oligosphaeridium? asterigerum	124.74
	Druggidium deflandrei, Heslertonia heslertonensis	125.00
	Druggidium rhabdoreticulatum	126.92
	Batioladinium longicornutum	129.47
	Dapsilidinium warrenii	129.80
	Muderongia crucis	130.94
	Cribroperidinium confossum	131.82
	S. primaevus	136.23
	Tehamadinium dodekovae	138.56
	Foucheria modesta	139.64
	Prolixosphaeridium sp. A of Monteil (1993), D.? deflandrei	139.77
	Warrenia californica; S. palmula	140.16
	Diacanthum hollisteri	140.21
	Systematophora areolata	140.61
	Amphorula metaelliptica	141.40
	Muderongia longicorna (acme)	141.67
FAD
	Disphaeria munda, Canningia torulosa	100.05
	Carpodinium obliquicostatum	100.27
	Psaligonyaulax deflandrei	103.27
	Xiphophoridium alatum	103.95
	Apteodinium maculatum grande	105.05
	Protoellipsodinium spinocristatum	121.05
	Cribroperidinium? tenuiceras	121.09
	Ovoidinium diversum	124.22
	C. tabulata	125.27
	P. spinosum	128.08
	P. polymorphum	128.30
	Druggidium rhabdoreticulatum	129.97
	Coronifera oceanica	133.53
	C. parva	136.23
	Lithodinia stoverii	137.17
	Batioladinium longicornutum, Hystrichodinium furcatum	137.23
	S. primaevus	137.52
	Heslertonia heslertonensis	138.48
	Nelchinopsis kostromiensis, Druggidium deflandrei, Discorsia nanna	139.77
	Gardodinium trabeculosum	139.81
	Oligosphaeridium complex	140.10
	Kleithriasphaeridium fasciatum	140.66
	Systematophora sp. A of Monteil (1993)	141.40
	D. aerlicum	141.55
	Muderongia longicorna (acme)	141.78
	Muderongia longicorna, Ctenidodinium elegantulum	144.36


All Tethyan Dinocyst Datums Combined	event		220/235/198		off
LAD
	Epelidosphaeridia spinosa	92.79
	Cribroperidinium intricatum	93.67
	Litosphaeridium siphoniphorum	93.94
	T. oblongata	94.38
	Disphaeria munda	94.45
	Gonyaulacysta helicoidea	100.01
	O. scabrosum	100.24
	Palaeohystrichophora cf. infusorioides	100.48
	Apteodinium maculatum grande	103.27
	Endoceratium turneri	103.95
	Cerbia tabulata	111.85
	P. polymorphum	111.85
	Subtilisphaera terrula	119.50
	Lithodinia stoverii	120.00
	Rhynchodiniopsis aptiana	122.67
	Prolixosphaeridium parvispinum	124.12
	Oligosphaeridium? asterigerum	124.74
	Druggidium spp.	125.00
	Druggidium deflandrei, Heslertonia heslertonensis	125.00
	Pseudoceratium pelliferum	126.10
	Muderongia staurota	126.48
	Druggidium rhabdoreticulatum	126.92
	Valensiella magna	129.47
	Batioladinium longicornutum	129.47
	Kleithriasphaeridium corrugatum	129.80
	Dapsilidinium warrenii	129.80
	Muderongia crucis	130.94
	Cribroperidinium confossum	131.82
	Muderongia macwhaei	131.95
	Aprobolocysta eilema	132.35
	Nelchinopsis kostromiensis	134.07
	S. primaevus	136.23
	Biorbifera johnewingii	137.65
	Druggidium apicopaucicum	137.83
	Tehamadinium dodekovae	138.56
	Foucheria modesta	139.64
	Prolixosphaeridium sp. A of Monteil (1993), D.? deflandrei	139.77
	Dichadogonyaulax bensonii	139.85
	Kleithriasphaeridium fasciatum	140.14
	Warrenia californica; S. palmula	140.16
	Diacanthum hollisteri	140.21
	Systematophora areolata	140.61
	Amphorula metaelliptica	141.40
	Muderongia longicorna (acme)	141.67
	Cirrusphaera dissimilis	141.93
	Valensiella pygmaea	143.03
	Prolixosphaeridium basifurcatum	143.20
	Lanterna spp.; Lanterna bulgarica	145.73
	Protobatioladinium lunare, Leptodinium mirabile	148.24
	Leptodinium subtile, Dingodinium scabratum	148.61
	Gonyaulacysta jurassica, Protobatioladinium westburiensis, Subtilisphaera? paeminosa	149.89
	Endoscrinium luridum	150.84
	Tubotuberella dangeardii	151.52
	Stephanelytron spp.	152.59
	Scriniodinium crystallinum	153.06
	Surculosphaeridium cribrotubiferum	154.53
	Gonyaulacysta eisenackii, Ctenidodinium ornatum	155.35
	Compositosphaeridium polonicum	156.81
	Wanaea thysanota	158.43
	Wanaea digitata	159.61
	Ctenidodinium combazii	164.35
	S. Hemisphere:  H. balmei	205.71
	S. Hemisphere:  S. ottii	234.56
FAD
	Subtilisphaera pontis-mariae	92.36
	Disphaeria munda, Canningia torulosa	100.05
	Carpodinium obliquicostatum	100.27
	Odontochitina costata, Palaeohystrichophora infusorioides	100.48
	Ovoidinium verrucosum verrucosum, Endoceratium dettmanniae	100.80
	Epelidosphaeridia spinosa	101.08
	Litosphaeridium siphoniphorum	103.27
	Psaligonyaulax deflandrei	103.27
	Palaeohystrichophora cf. infusorioides	103.95
	Xiphophoridium alatum	103.95
	Ellipsodinium rugulosum	105.05
	Apteodinium maculatum grande	105.05
	O. scabrosum	117.40
	Protoellipsodinium spinocristatum	121.05
	Cribroperidinium? tenuiceras	121.09
	Palaeoperidinium cretaceum	124.22
	Ovoidinium diversum	124.22
	C. tabulata	125.27
	Prolixosphaeridium parvispinum	127.99
	P. spinosum	128.08
	P. polymorphum	128.30
	Subtilisphaera terrula	129.47
	Odontochitina operculata	129.84
	Druggidium rhabdoreticulatum	129.97
	Rhynchodiniopsis aptiana	130.61
	Coronifera oceanica	133.53
	Aprobolocysta eilema	133.61
	Muderongia staurota	136.12
	C. parva	136.23
	Lithodinia stoverii	137.17
	Kleithriasphaeridium corrugatum	137.23
	Batioladinium longicornutum, Hystrichodinium furcatum	137.23
	S. primaevus	137.52
	Subtilisphaera perlucida	138.17
	Valensiella magna	138.48
	Heslertonia heslertonensis	138.48
	Muderongia australis	139.77
	Nelchinopsis kostromiensis, Druggidium deflandrei, Discorsia nanna	139.77
	Gardodinium trabeculosum	139.81
	Oligosphaeridium complex	140.10
	Druggidium apicopaucicum	140.14
	Muderongia macwhaei forma B	140.21
	Kleithriasphaeridium fasciatum	140.66
	Muderongia macwhaei forma A	140.89
	Pseudoceratium pelliferum	141.25
	Systematophora sp. A of Monteil (1993)	141.40
	D. aerlicum	141.55
	Muderongia longicorna (acme)	141.78
	Foucheria modesta	141.93
	Cirrusphaera disimilis	143.03
	Valensiella pygmaea	144.30
	Dichadogonyaulax bensonii	144.36
	Muderongia longicorna, Ctenidodinium elegantulum	144.36
	Spiniferites ramosus group	144.88
	Warrenia californica	145.73
	Prolixosphaeridium sp. A of Monteil (1993)	147.00
	Biorbifera johnewingii, Cometodinium habibii	148.98
	Lanterna sportula	150.84
	Subtilisphaera? paeminosa	152.59
	Cribroperidinium longicorne, Subtilisphaera? inaffecta	152.83
	Occisucysta balios, Amphorula spp.	153.39
	Glossodinium dimorphum	158.43
	Impletosphaeridium varispinosum	164.23
	Compositosphaeridium polonicum	164.74
	Nannoceratopsis triceras	176.58
	Parvocysta spp., Scriniocassis priscus	180.50
	Mancodinium semitabulatum, Nannoceratopsis gracilis, Scriniocassis weberi, Luehndea spp.	186.95
	Mancodinium spp.	189.60
	Dapcodinium priscum	191.22
	S. Hemisphere:  H. balmei	211.30
	S. Hemisphere:  W. listeri	216.53
	S. Hemisphere:  Suessia swabiana	218.66
	S. Hemisphere:  R. wigginsii	219.81
	S. Hemisphere:  S. ottii	240.00



Dinoflagellate cysts (North Sea)	:	N-Sea Dinocyst Zone	Dinocyst events	_METACOLUMN_OFF		Morton Smelror (2005; via Felix Gradstein; measured from NORGES charts)

N-Sea Dinocyst Zone	block	120	214/235/182	notitle
	TOP	0
	Un-named 	0.44
	Melitasphaeridium choanephorum	1.46
	Amiculosphaera umbracula	1.95
	Reticulatosphaera actinocoronata	2.68
	Selenopemphix brevispinosa	4.05
	Operculodinium piaseckii	5.26
	Cristadinium diminutivum	6.81
	Decahedrella martinheadii	7.53
	Labyrinthodinium truncatum	8.77
	Palaeocystodinium golzowense	10.89
	Cannosphaeropsis passio	13.65
	Unipontidinium aquaeductum	15.97
	Distatodinium paradoxum	17.80
	Cribroperidinium tenuitabulatum	19.43
	Cordosphaeridium cantharellum	21.49
	Caligodinium amiculum	22.03
	Chiropteridium spp.	24.36
	Distatodinium biffii	27.07
	Spiniferella cornuta	31.15
	Areoligera semicirculata	31.77
	Deflandrea granulata	32.51
	Schizophacus cooksoniae	33.50
	Areosphaeridium dictyoplokus 	36.25
	Heteraulacacysta porosa	39.98
	D. colligerum	44.50
	Dapsilidinium ficusoides	48.05
	Eatonicysta ursulae	48.76
	Dracodinium varielongitudum	52.15
	Deflandrea oebisfeldensis	55.73
	Apectodinium augustum	58.14
	Alisocysta margarita + P. pyrophorum	59.47
	Isabelidinium? viborgense + S. magnifica	63.21
	Senoniasphaera inornata	65.50

Dinocyst events	event
LAD
	Melitasphaeridium choanephorum, L. parviconvexa	0.44
	Tuberculodinium  vancampoae	1.04
	Amiculosphaera umbracula	1.46
	Reticulatosphaera actinocoronata, Operculodinium janduchenei	1.95
	Selenopemphix  brevispinosa, Piccoladinium fenestratum	2.68
	Invertocysta lactymosa	3.07
	Edwardsiella sexispinosum	3.60
	Operculodinium piaseckii	4.05
	Cristadinium diminutivum	5.26
	Decahedrella martinheadii	6.81
	Hystrichosphaeropsis obscura, Labyrinthodinium truncatum, Cristadinium cristatoserratum	7.53
	Palaeocystodinium golzowense	8.77
	Cerebrocysta poulsenii, Cordosphaeridium minimum	10.07
	Cannosphaeropsis passio	10.89
	Palaeocystodinium sp. A, Lophocysta sulcolimbata	11.40
	Unipontidinium aquaeductum, P. laticinctum, Systematophora placacantha	13.65
	Apteodinium spiridoides, Distatodinium paradoxum/craterum	15.97
	Apteodinium australiense	17.19
	Cribroperidinium tenuitabulatum	17.80
	Cordosphaeridium cantharellum	19.43
	Leptodinium sp. III	20.74
	Caligodinium amiculum	21.49
	Deflandrea phosphoritica, Chiropteridium galea, Chiropteridium spp.	22.03
	Distatodinium biffii, Membranophoridium aspinatum	24.36
	Chiropteridium lobospinosum	25.49
	Spiniferella cornuta	27.07
	Wetzeliella symmetrica group, Thalassiphora pelagica	28.10
	Phtanoperidinium spp.	29.48
	Rhombodinium draco, Corrundinium incompositum 	30.26
	Areoligera semicirculata 	31.15
	Deflandrea granulata 	31.77
	Schizophacus cooksoniae, Samlandia chlamydophora, Achilleodinium biformoides 	32.51
	Areosphaeridium  dictyoplokus 	33.50
	Areosphaeridium michoudii 	35.30
	Heteraulacacysta porosa	36.25
	Rhombodinium momboideum	39.98
	Phtanoperidinium distinctum	41.18
	Dapsilidinium pseudofiscusoides	43.67
	Cerebrocysta magna, S. placacantha	45.14
	Hystrichosphaeropsis costae	46.14
	Eatonicysta ursulae	48.05
	Dracodinium condylos	48.37
	Dracodinium politum	48.60
	Dracodinium varielongitudum	48.76
	Deflandrea oebisfeldensis	52.15
	Cerodinium speciosum, Phelodinium magnificum, Alisocysta sp. 2	54.34
	Apectodinium augustum	55.73
	Alisocysta margarita	58.14
	Isabelidinium? viborgense	59.47
	Cerodinium diebelii	59.90
	Alisocysta reticulata	62.26
	Senoniasphaera inornata	63.21
	Carpatella cornuta	64.91
	Palynodinium grallator	65.50





North Sea Microfossil Zones (Cenozoic)	:	North Sea Zone	North Sea Event	_METACOLUMN_OFF		Gradstein and Backstrom (1996); Gradstein et al. (1999), Kaminiski and Gradstein (2005) as summarized on NORGES chart series.

North Sea Zone	block	120	126/200/113	notitle
	TOP	0.00
	NSR 13 (Cass. teretis)	1.81
	NSR 12B (Cass. grossa)	2.85
	NSR 12A (Glob. inflata)	3.60
	NSR 11 (Neoglob. atlantica)	5.33
	NSR 10 (Bolbo. metsmacheri)	8.05
	NSR 9B (Ehren. variabilis)	12.26
	NSR 9A (Glob. praescitula)	17.06
	NSR 8B (Cat. unicavus)	23.03
	NSR 8A (Siliceous biofacies)	28.45
	NSR 7B (Turr. alsatica)	32.08
	NSR 7A (Ader. agterbergi)	34.16
	NSR 6B (Un-named)	37.24
	NSR 6A (Retic. amplectens)	40.44
	NSR 5B (Ammomarg. aubertae)	43.29
	NSR 5A (Retic. intermedium)	48.60
	NSR 4 (Sub. patagonia)	53.07
	NSR 3 (Fenestr. antiqua)	55.73
	NSR 2B (Retic. pauperum)	60.05
	NSR 2A (Ammoan. ruthvenmurrayi)	61.72
	NSR 1 (Moro. pseudobulloides)	65.50

North Sea Event	event		149/200/140
LAD
	Elphidium clavatum, Cassidulina teretis, Cassidulina scaldisiensis, Neogloboquadrina pachyderma	0.47
	Cassidulina grossa, Ammonia beccari	1.81
	Cassidulina grossa LCO, Sigmoilopsis schlumbergeri, Nonion affine LCO, Monspeliensis pseudotepida, Globorotalia inflata (pl. foram)	2.85
	S. North Sea: Hyalinea balthica	2.96
	PLANK. FORAMS = Neogloboquadrina atlantica, Globorotalia crassaformis, Globorotalia puncticulata, Neogloboquadrina humerosa 	3.60
	Bolboforma metzmacheri, Cibicides telegdi; PLANK. FORAMS = Neogloboquadrina atlantica (dextral), Globigerina bulloides, Neogloboquadrina acostaensis 	5.33
	Ehrenbergina variabilis, Cassidulina subglobosa, Martinottiella cylindrica, Bolboforma fragori (nanno), Bolboforma spiralis, Neogloboquadrina pachyderma (pl. foram)	8.05
	Globorotalia praemenardii, DWAF 	12.03
	Cibicidoides wuellerstorfi, Uvigerina semiornata; Neogloboquadrina continuosa (pl. foram), Globigerina praebulloides (pl. foram), 	12.26
	Spirosigmoilinella compressa; PLANK. FORAMS = Globorotalia praescitula/zealandica, Sphaeroidinellopsis disjuncta, Sphaeroidinellopsis seminulina	14.74
	Catapsydrax unicavus (pl. foram), Globigerinoides trilobus (pl. foram), Asterigerina guerichi	17.06
	Siliceous biofacies; S. NORTH SEA = Globigerina ciperoensis, Globoquadrina praedehiscens, Dentoglobigerina baroemoensis	20.43
	Siliceous biofacies LCO, Cibicidoides mundulus, Aulacodiscus insignis var. (sp.3,4,5) (diatom); S. NORTH SEA = Globigerina officinalis, Almaena osnabrugensis	23.03
	Turrilina alsatica LO, Spirosigmoilinella  compressa (pl. foram) LCO, Dorothia seigliei	26.94
	Turrilina alsatica LCO	28.45
	Adercotryma agterbergi, Annectina biedai, Rotaliatina bulimoides, DWAF LCO (rare); PLANK. FORAMS = Reticulophragmium acutidorsatum, Ammodiscus latus, Reticulophragmoides jarvisi	32.08
	S. North Sea = Subbolina linapoerta, Turborotalia pomeroli, Globorotalia cerroazulensis	33.88
	Ammosphaerodina pseudopauciloculata (pl. foram)	34.16
	Reticulophragmium amplectens (pl. foram); S. NORTH SEA = Marginulopsis decorata, Cibicidoides truncanus 	37.24
	Ammomarginulina aubertae (pl. foram), Karrerulina conversa, Karrerulina coniformis, Haplophragmoides kirki	40.44
	PLANK. FORAMS: Recticulophragmium intermedium, Recurvoidella lamella, Spiroplectammina navarroana	43.29
	S. North Sea = Turrilina robertsi, Acarinina pentacamerata, Acarinina sp.  	44.19
	Popovia spp., Subbotina patagonica (pl. foram);  S. NORTH SEA = Planorotolites planoconicus, Acarinina densa, Acarinina pseudotopilensis, Planorotalites australiformis, Morozovella formosa gracilis, Acarinina soldadoensis, Bulimina trigonalis  	48.60
	Fenestrella antiqua (diatom)	53.07
	DWAF (rare)	55.73
	Spiroplectammina dentata (S. North Sea)	56.52
	DWAF LCO, including Rzehakina minima, Hyperammina rugosa, Saccamina placenta, Reticulophragmium pauperu, Reticulophragmium garcilassoi (rare), Spiroplectammina spectabilis LCO	56.67
	Ammoanita ruthvenmurrayi (pl. foram), Hormosina excelsa, Labrospira pacifica (rare), Cystammina sveni, Conotrochammina voeringensis (rare), Ammoanita ingerlisae (rare)	60.05
	Cenosphaera lenticularis, Gavelinella beccariiformis, Remesella varians; PLANK. FORAMS = Morozovella pseudobulloides, Globanomalina cf. compressa, Subbotina triloculinoides, 'Globigerina' trivialis, Globoconusa daubjergensis, 'Globigerina' simplicissimum	61.72



Chitinozoa (N.Gondwana; Silurian)	:	Chitinozoa  Zone	_METACOLUMN_OFF		GTS2004 diagrams (Melchin et al., 2004)

Chitinozoa  Zone	block	120	214/216/167	notitle
	TOP	416.00
	Angochitina superba	417.08
	Margachitina elegans	418.03
	Fungochitina kosovensis	418.70
	Eisenackitina barrandei	420.13
	Eisenackitina phillipi	421.17
	Angochitina echinata	422.10
	Belonechitina latifrons	422.90
	Sphaerochitina lycoperdoides	424.22
	Conochitina pachycephala	426.50
	Cingulochitina cingulata	427.20
	Margachitina margaritana	428.60
	Angochitina longicollis	432.15
	Eisenackitina dolioliformis	436.68
	Cono. alargada	437.55
	Spinachitina maennili	439.24
	Conochitina electa	441.12
	Beloechitina postrobusta	441.82
	Spinachitina fragilis	443.70
	Tanuchitina oulebsiri	444.84
	Tanuchitina elongata	446.11
	Ancyrochitina merga	448.15
	Armoricochitina nigerica	449.17
	Acanthochitina barbata	450.19
	Tanuchitina fistulosa	451.21
	Belonechitina robusta	453.25
	Euconochitina tanvillensis	454.78
	(uncertain)	457.33
	Lagenochitina dalbyensis	458.10
	Lagenochitina deunffi	459.88
	Lagenochitina ponceti	460.90
	Linochitina pissotensis	462.34
	Laufeldochitina clavatai	463.06
	Armoricochitina amoricana - Cyathochitina jenkinsi	464.86
	Siphonochitina formosa	465.58
	Cyathochitina calyx - Cyathochitina protocalix	467.74
	Desmochitina bulla	468.66
	Belonechitina henryi	470.14
	Desmochitina ornensis	471.80
	Eremochitina brevis	474.18
	Eremochitina baculata	476.56
	Conochitina symmetrica	478.60
	Lagenochitina conifundus ? Lagenochitina destombesi	488.30




Radiolarians	:	Radiolarian Zone (Cenoz-Cret)	Triassic Zone (Kozur'03)	Low-lat Radiolarian zone (Permian)	Cis-Ural Radiolarian zone (Permian)	Radiolarian Zone Marker	Other Radiolarian datums (Cenoz)	All Radiolarian Datums Combined	_METACOLUMN_OFF		CENOZOIC = Sanfilippo and Nigrini (1998), Nigrini and Sanfilippo (2001).  MESOZOIC = partly from P. de Wever (in Hardenbol et al., SEPM charts, 1998), but Triassic includes some of Kozur (2003).

Radiolarian Zone (Cenoz-Cret)	block	50	248/148/16	notitle		CENOZOIC = Sanfilippo and Nigrini (1998), Nigrini and Sanfilippo (2001).  CRETACEOUS = partly from P. de Wever (in Hardenbol et al., SEPM charts, 1998).
	TOP	0.00
	RN17	0.18
	RN16	0.42
	RN15	0.61
	RN14	1.10
	RN13	1.71
	RN12b	2.40
	RN12a	2.76
	RN11b	3.42
	RN11a	3.82
	RN10	4.19
	RN9	6.90
	RN8	7.75
	RN7	8.84
	RN6	12.01
	RN5	15.66
	RN4	17.00
	RN3	17.77
	RN2	20.05
	RN1	22.84
	RP22	23.90
	RP21	28.77
	RP20	33.01
	RP19	35.00
	RP18	36.32
	RP17	37.43
	RP16	38.34
	RP15	38.93
	RP14	41.84
	RP13	43.52
	RP12	46.76
	RP11	47.94
	RP10	48.60
	RP9	50.14
	RP8	53.23
	RP7	57.71
	RP6c	58.43
	RP6b	59.99
	RP6a	60.95
	RP5	61.65
	RP4	63.38
	RP3	64.37
	RP2	64.99
	RP1	65.44
	TOP	65.50
	Amphipyndax tylotus	73.61
	Amphipyndax pseudoconulus	83.53
	Theocampe urna	85.85
	Un-Zoned	123.45
	G2	126.54
	Blank	127.53
	G1	129.13
	Blank	129.92
	F3	133.40
	Blank	133.63
	F2	135.02
	Blank	135.60
	F1	137.65
	E2	137.69
	Blank	137.98
	E1b	140.08
	Blank	140.30
	E1a	141.82
	Blank	142.27
	D2	144.95
	Blank	145.46

Triassic Zone (Kozur'03)	block	150	248/148/16
	TOP	199.60
	Laxtorum perfectum	201.62
	Praecitriduma mostleri	202.96
	Sqinabolella? trispinosa	203.64
	Betraccium deweveri	206.64
	TOP	222.70	dashed
	Tetraporobrachia haeckeli	226.94
	[un-named]	228.01
	Tritortis kretaensis	228.73
	Muelleritortis cochleata	231.68
	Muelleritortis firma	234.56
	[un-named]	235.78
	Ladinocampe multiperforata	240.17
	Spongosilicar. Italicus	241.00
	Spongosilicar. transitus	241.15
	Tetraspinocyrtis laevis	241.30
	(no dated radiolarians)	241.60
	Parasepsagon robustus	241.89
	Barantuna cristianensis	242.19
	Paroertlispongus diacanthus	243.68
	Hozmadia gifuensis	245.17
	Hozmadia ozawai - Parentactinia nakatsugaraensis	248.08
	RADIOLARIANS UNKNOWN	249.33
	Stigmosphaerostylus turkensis	250.38
	RADIOLARIANS UNKNOWN	251.40

Low-lat Radiolarian zone (Permian)	block	150	248/148/16			Kozur (2003)
	TOP	251.36
	Lacisus siphunculus - Cariver dorsoconvexus	252.40
	Neoalbaillella ornithoformis	253.80
	Cariver orthogonus - Ishigaconus hamatus	253.80
	Neoalbaillella optima s.s	260.07
	Follicucullus ventricosus - Ishigaeonus scholasticus	263.10
	Parafollicucullus convexus - Follicucullus porrectus	264.45
	Parafollicucullus monacanthus	265.13
	Parafollicucullus fusiformis - Parafollicucullus globosus	266.90
	Parafollicucullus globosus - Parafollicucullus longtanensis	268.00
	Parafollicucullus corniculatus	269.56
	Spinodeflandrella foremanae - Parafollicucullus cornelli	270.60
	Pseudoalbaillella rhombothoracata	272.48
	Parafollicucullus ornatus	275.60
	Parafollicucullus lomentarius	281.10
	TOP	289.50
	Pseudoalbaillella (Kitoconus) elegans	294.60
	Curvalbaillella uforma	299.00

Cis-Ural Radiolarian zone (Permian)	block	150	248/148/16			Kozur (2003)
	TOP	271.60
	Pseudolilthelius permicus - Ruzhencevisp. uralicus	273.35
	TOP	275.60
	Polyeudroent. lautitia	277.80
	TOP	281.10
	Pa. cataphracta	284.40
	C. monopt. - P. plumata	286.95
	F. circumfusa	289.50
	Holdsworthella perforata	292.56
	TOP	294.60
	Curvalbaillella uforma	299.00



Radiolarian Zone Marker	event		248/178/85			CENOZOIC = Sanfilippo and Nigrini (1998), Nigrini and Sanfilippo (2001).  MESOZOIC = partly from P. de Wever (in Hardenbol et al., SEPM charts, 1998), but Triassic includes some of Kozur (2003).
LAD
	Stylatractus universus	0.42
	Anthocyrtidium angulare	1.10
	Pterocanium prismatium	1.71
	Anthocyrtidium jenghisi	2.40
	Stichocorys peregrina	2.76
	Phormostichoartus fistula	3.42
	Phormostichoartus doliolum	3.82
	Didymocyrtis penultima	4.19
	Stichocorys delmontensis	6.90
	Diartus hughesi	7.75
	Diartus petterssoni	8.84
	Dorcadospyris dentata	15.66
	Theocyrtis annosa	20.05
	Tristylospyris triceros	28.77
	Lithocyclia aristotelis group	33.01
	Thyrsocyrtis (Pentalacorys) tetracantha	35.00
	Podocyrtis (Lampterium) mitra	38.93
	Podocyrtis (Lampterium) sinuosa	41.84
	Podocyrtis (Podocyrtoges) phyxis	43.52
	Theocotyle nigriniae	48.60
	Pterocodon (?) anteclinata	53.23
	Peritiviator (?) dumitricai	59.99
	T. pulchra, T. veneta, C. pulchrum, X. spicularius	94.08
	A. diaphorogona, A. irregularis, A. horridus	95.18
	A. dendroacanthos,  C. triangulare, D. gracilis	96.10
	D. obesa	97.54
	T. conica	104.85
	A. umbilicata	110.30
	Sphaerostylus lanceola	116.20
	P. boesii	121.00
	B. helenae, P. tythopora	121.90
	C. biopodium, C. infundibuliforme	125.44
	North Sea: Tricolocapsa sp.1 and sp.2, P. jonesi s.l., S. devorata, Cenosphaera sp.1, P. 'hispida'	140.55
	North Sea: O. mclaughlini, T. 'obesa'; and Highest prominent S. devorata, Cenosphaera sp.1 and P. 'hispida' 	142.84
	E. orea	145.46
	North Sea: End of Radiolarian influx, P. jonesi s.l. (prominent), Spondodiscus sp.4 (LCO)	146.32
	North Sea: Cenodiscus sp.3	147.43
	North Sea: Cenosphaera sp.1 (LCO), Cenodiscus sp.1 (LCO)	148.92
	North Sea: O. lowreyensis	149.26
	North Sea: P. hexagona (LCO), Cenosphaera sp.1 (prominent)	150.02
	Pantanellium riedeli	150.84
	North Sea: P. blowi (LCO), Cenosphaera sp.1 (LCO), P. jonesi (LCO)	153.16
	Pseudocrucella adriani, Tritrabs rhododactylus	154.40
	North Sea: Stichocapsa sp.1	162.52
	North Sea: O. iniqua	163.20
	Thetis bernouillii	163.37
	Mesosaturnalis tetraspinus	167.68
	Zartus dickinsoni	170.23
	B. deweveri, C. deweveri, P. spinosa	203.64
	C. triassica	211.24
	P. dercourti	216.53
	P. anisicus	234.56
	RADIOLARITE GAP of Earliest Triassic !!	250.38
FAD
	Buccinosphaera invaginata	0.18
	Collosphaera tuberosa	0.61
	Stichocorys peregrina	6.90
	Stichocorys delmontensis	7.75
	Diartus hughesi	8.84
	Diartus petterssoni	12.01
	Dorcadospyris alata	15.66
	Calocycletta (Calocyclissima) costata	17.00
	Stichocorys wolffii	17.77
	Cyrtocapsella tetrapera	22.84
	Lychnocanoma elongata	23.90
	Dorcadospyris ateuchus	28.77
	Lithocyclia angusta	33.01
	Calocyclas bandyca	36.32
	Cryptocarpium azyx	37.43
	Podocyrtis (Lampterium) goetheana	38.34
	Podocyrtis (Lampterium) chalara	38.93
	Podocyrtis (Lampterium) mitra	41.84
	Podocyrtis (Podocyrtoges) ampla	43.52
	Eusyringium lagena	46.76
	Dictyoprora mongolfieri	47.94
	Theocotyle cryptocephala	48.60
	Theocorys anaclasta	50.14
	Buryella clinata	53.23
	Bekoma bidartensis	57.71
	Stylotrochus nitidus,  Pterocodon (?) poculum	58.43
	Bekoma campechensis	60.95
	Buryella tetradica	61.65
	Buryella foremanae	63.38
	Stichomitra granulata	64.37
	Amphisphaera kina	64.99
	Amphisphaera aotea	65.44
	Amphipyndax tylotus	73.61
	Amphipyndax pseudoconulus	83.53
	Theocampe urna	85.85
	A. lirioides, D. multicostata	91.31
	A. superbum, Crucella cachensis, A. longipina	93.55
	C. pulchrum	97.54
	Pseudodictyomitra nakasekoi	98.54
	Dorypyle? anisa, Obesacapsula somphedia	99.64
	P. putahensis, D. formosa	100.27
	D. obesa, A. horridus, T. veneta	103.68
	A. dendroacanthos, C. triangulare, A. irregularis, T. pulchra, C. euganea, C. messinae, T. conica	104.85
	D. gracilis, R. euganeum, Pseudodictyomitra pseudomacrocephala	106.15
	Mita spoletoensis	108.59
	Mita gracilis	112.00
	T. conica, X. spicularius	117.70
	Pseudodictyomitra lodogaensis	116.20
	North Sea: Tricolocapsa sp.1 and sp.2	141.66
	A. helenae	145.46
	North Sea: P. hispita (FCO)	146.71
	Sethocapsa cetia	150.84
	Triactoma echiodes	154.40
	North Sea: Common Radiolaria	154.97
	Emiluvia pessagnoi	160.90
	Acanthocircus trizonalis	163.37
	North Sea: Stichocapsa sp.1	165.17
	Mirifusus dianae	165.91
	Emiluvia sedecimporata, Pantancilium riedeli	166.40
	Hsuum maxwelli, Eucyritidiellum ptyctum	167.68
	Andromeda depressa, Tricolocapsa plicarum, Mesosaturnalis tetraspinus	170.23
	L. validus	203.64
	P. dercourti, C. triassica, C. deweveri	228.01
	P. hellenica	240.00
	F. calcaneum	241.00
	RADIOLARITE GAP of Earliest Triassic !!	251.40

Other Radiolarian datums (Cenoz)	event		248/178/85
LAD
	Anthocyrtidium nosicaae	0.70
	Pterocorys campanula	0.80
	Lamprocyrtis neoheteroporos	1.28
	Anthocyrtidium michelinae	1.49
	Theocorythium vetulum	2.04
	Anthocyrtidium ehrenbergi	2.94
	Didymocyrtis avita	3.09
	Anthocyrtidium pliocenica	3.40
	Lychnodictyum audax	3.60
	Spongaster pentas	4.13
	Spongaster berminghami, Spongaster klingi	4.17
	Solenosphaera omnitubus procera, Soleno. omni. omnitubus	5.31
	Acrobotrys tritubus	5.55
	Siphostichartus corona	5.67
	Calocycletta (Calocyclior) caepa	6.14
	Acrobotrys tritubus	6.34
	Stichocorys johnsoni	6.79
	Calocycletta (Calocycletta) cladara	6.84
	Didymocyrtis antepenultima	7.75
	Dictyocoryne ontongensis	7.94
	Botryostrobus miralestensis	8.23
	Didymocyrtis laticonus	8.84
	Lithopera (Lithopera) neotera, Stichocorys wolffii	8.87
	Cyrtocapsella japonica, Lithopera (Glomaria) thornburgi	9.86
	Carpocanopsis cristata	10.67
	Lithopera (Lithopera) renzae, Cyrtocapsella cornuta, Cyrtocapsella tetrapera	12.13
	Calocycletta (Calocycletta) virginis, Dorcadospyris alata, Liriospyris parkerae	13.67
	Didymocyrtis mammifera	14.10
	Carpocanopsis bramlettei	14.68
	Calocycletta (Calocyclissima) costuta, Didymocyrtis tubaria, Didymocyrtis violina	15.00
	Dorcadospyris forcipata	15.66
	Eucyrtidium diaphanes	15.88
	Liriospyris stauropora	16.11
	Carpocanopsis favosa	16.33
	Didymocyrtis prismatica	16.55
	Carpocanopsis cingulata	16.78
	Lychnocanoma elongata	17.00
	Dorcadospyris ateuchus	17.77
	Calocycletta (Calocyclopsis) serrata	20.61
	Calocycletta (Calocycletta) robusta	21.17
	Artophormis gracilis	23.11
	Dorcadospyris papilio	23.64
	Lychnocanoma trifolium	24.88
	Lithocyclia angusta	27.80
	Theocyrtis tuberosa	29.16
	Lithocyclia crux	29.54
	Dorcadospyris pseudopapilio	30.31
	Centrobotrys petrushevskayae	30.70
	Centrobotrys gravida	31.47
	Artophormis barbadensis	31.85
	Dictyoprora pirum	32.62
	Cryptocarpium ornatum, Dictyoprora mongolferi, Lychnocanoma amphitrite	33.01
	Dictyoprora armadillo	33.51
	Lophocyrtis (Lophocyrtis) jacchia	34.01
	Calocyclas turris, Thyrsocyrtis (Thyrso.) bromia, Thyrsocyrtis (Thyrso.) rhizodon, Cryptocarpium azyx	34.50
	Thyrsocyrtis (Pentalacorys) lochites, Calocyclas bandyca, Calocyclas hispida, Lychnocanoma bellum, Podocyrtis (Podocyrtis) papalis	35.00
	Thyrsocyrtis (Pentalacorys) triacantha	35.27
	Eusyringium fistuligerum	35.80
	Podocyrtis (Lampterium) goetheana	36.06
	Podocyrtis (Lampterium) chalara	36.60
	Calocyclas hispida	37.15
	Spongatractus pachystylus	37.58
	Theocotylissa ficus	37.88
	Sethochytris triconiscus	38.04
	Lithocyclia ocellus group	38.34
	Podocyrtis (Lampterium) trachodes	38.64
	Phormocyrtis striata striata	38.93
	Podocyrtis (Podocyrtoges) ampla	40.39
	Eusyringium lagena, Podocyrtis (Lampterium) fasciolata, Podocyrtis (Lampterium) helenae	41.11
	Podocyrtis (Podocyrtoges) dorus	42.51
	Eusyringium lagena	42.85
	Theocotyle venezuelensis	43.52
	Podocyrtis (Podocyrtoges) diamesa, Theocotyle nigriniae, Theocotyle conica, Theocorys anaclasta, Lamptonium fabaeforme constrictum, Lamptonium fabaeforme chaunothorax, Thyrsocyrtis (Thyrso.) hirsuta, Thyrsocyrtis (Thyrso.) robusta	45.68
	Thyrsocyrtis (Pentalacorys) tensa	46.76
	Lamptonium fabaeforme fabaeforme	47.16
	Theocotyle cryptocephala	47.55
	Calocycloma castum	47.94
	Podocyrtis (Lampterium) acalles	48.11
	Buryella clinata	48.60
	Spongatractus balbis	48.91
	Lamptonium sanfilippoae	49.22
	Phormocyrtis striata exquisita, Phormocyrtis cubensis	50.14
	Pterocodon(?) ampla, Bekoma bidartensis, Buryella tetradica, Thyrsocyrtis (Thyrsocyrtis) tarsipes	50.91
	Theocotylissa alpha	51.69
	Lamptonium pennatum	55.79
	Bekoma campechensis	57.07
	Buryella pentadica	59.21
FAD
	Pterocorys hertwegii	0.74
	Anthocyrtidium euryclathrum	0.91
	Lamprocyrtis nigriniae	1.15
	Anthocyrtidium angulare	1.81
	Pterocorys zancleus	1.85
	Cycladophora davisiana	2.58
	Lamprocyrtis neoheteroporus	2.65
	Theocorythium trachelium trachelium.	2.69
	Didymocyrtis tetrathalamus tetrathalamus	3.09
	Amphirhopalum ypsilon	4.01
	Spongaster tetras tetras	4.13
	Didymocyrtis avita	4.19
	Pterocanium prismatium	4.91
	Spongaster pentas	5.49
	Pterocorys campanula	5.67
	Solenosphaera omnitubus procera, Soleno. omni. omnitubus	7.41
	Didymocyrtis penultima	7.75
	Acrobotrys tritubus	7.94
	Spongaster berminghami	8.35
	Didymocyrtis antepenultima.	8.84
	Lithopera (Lithopera) bacca, Phormostichoartus doliolum	8.87
	Lithopera (Lithopera) neotera	12.13
	Calocycletta (Calocycletta) cladara, Cyrtocapsella japonica	13.67
	Didymocyrtis laticonus	14.10
	Lithopera (Lithoperu) renzae, Lithopera (Glomaria) thornburgi, Phormostichoartus corbula, Dictyocoryne ontongensis	15.00
	Liriospyris parkerae	16.11
	Carpocanopsis cristata	16.78
	Didymocyrtis mammifera	17.16
	Calocycletta (Calocyclior) caepa	17.31
	Dorcadospyris dentata	17.47
	Liriospyris stauropora	17.62
	Siphostichartus corona	17.77
	Didymocyrtis tubaria, Didymocyrtis violina, Stichocorys delmontensis, Carpocanopsis bramlettei	18.91
	Carpocanopsis favosa	21.73
	Cyrtocapsella cornuta	22.28
	Calocycletta (Calocyclopsis) serrata, Calocycletta (Calocycletta) virginis, Bottyostrobus miralestensis.	22.84
	Eucyrtidium diaphanes	23.37
	Curpocanopsis cingulata	23.90
	Dorcadospyris forcipata	24.88
	Calocycletta (Calocycletta) robusta	25.85
	Dorcadospyris papilio	26.83
	Theocyrtis annosa	29.16
	Lychnocanoma trifolium	29.93
	Didymocyrtis prismatica	30.31
	Centrobotrys thermophila	30.70
	Lychnodictyum audax	31.08
	Centrobotrys petrushevskayae, Dorcadospyris pseudopapilio	31.47
	Artophormis gracilis, Lithocyclia crux	31.85
	Centrobotrys gravida	32.24
	Phormostichoartus fistula	32.62
	Theocyrtis tuberosa	35.53
	Lychnocanoma amphitrite	36.87
	Calocyclas turris	37.15
	Thyrsocyrtis (Thyrsocyrtis) bromia	37.73
	Thyrsocyrtis (Pentalacorys) tetracantha, Dictyoprora pirum,	37.88
	Dictyoprora armadillo	38.19
	Lithocyclia aristotelis group	38.34
	Tristylospyris triceros	38.93
	Cryptocarpium ornatum	39.66
	Artophormis barbadensis, Thyrsocyrtis (Pentalacorys) lochites, Sethochytris triconiscus,	41.11
	Podocyrtis (Lampterium) trachodes	42.17
	Eusyringium fistuligerum	42.85
	Podocyrtis (Lampterium) fasciolata, Podocyrtis (Lampterium) helenae	43.18
	Eusyringium fistuligerum	44.60
	Podocyrtis (Podocyrtoges) phyxis	45.68
	Thyrsocyrtis (Pentalacorys) triacantha	46.76
	Podocyrtis (Podocyrtoges) dorus	47.16
	Theocotyle conica	47.55
	Podocyrtis (Lampterium) sinuosa	48.11
	Thyrsocyrtis (Thyrsocyrtis) robusta	48.27
	Theocotyle venezuelensis	48.44
	Spongatractus pachystylus	48.91
	Thyrsocyrtis (Thyrsocyrtis) rhizodon	49.53
	Podocyrtis (Podocyrtoges) diamesa	49.83
	Phormocyrtis striata striata, Lamptonium fabaeforme constrictum, Podocyrtis (Lampterium) acalles, Lychnocanoma bellum	50.14
	Theocotylissa ficus, Lithocyclia ocellus group, Thyrsocyrtis (Pentalacorys) tensa	51.69
	Calocyclas hispida	52.46
	Spongatractus balbis, Lamptonium sanfilippoae, Theocotyle nigriniae, Thyrsocyrtis (Thyrsocyrtis) hirsuta	53.23
	Theocotylissa alpha	53.87
	Lamptoniumfabaeforme chaunothorax	54.51
	Pterocodon(?) anteclinata,  Lophocyrtis (Lophocyrtis) jacchia	55.15
	Lamptonium fabaeforme fabaeforme, Calocycloma castum	55.79
	Podocyrtis (Podocyrtis) papalis	56.43
	Phormocyrtis cubensis	58.07
	Pterocodon(?) ampla	60.47



All Radiolarian Datums Combined	event		248/178/85		off
LAD
	Stylatractus universus	0.42
	Anthocyrtidium nosicaae	0.70
	Pterocorys campanula	0.80
	Anthocyrtidium angulare	1.10
	Lamprocyrtis neoheteroporos	1.28
	Anthocyrtidium michelinae	1.49
	Pterocanium prismatium	1.71
	Theocorythium vetulum	2.04
	Anthocyrtidium jenghisi	2.40
	Stichocorys peregrina	2.76
	Anthocyrtidium ehrenbergi	2.94
	Didymocyrtis avita	3.09
	Anthocyrtidium pliocenica	3.40
	Phormostichoartus fistula	3.42
	Lychnodictyum audax	3.60
	Phormostichoartus doliolum	3.82
	Spongaster pentas	4.13
	Spongaster berminghami, Spongaster klingi	4.17
	Didymocyrtis penultima	4.19
	Solenosphaera omnitubus procera, Soleno. omni. omnitubus	5.31
	Acrobotrys tritubus	5.55
	Siphostichartus corona	5.67
	Calocycletta (Calocyclior) caepa	6.14
	Acrobotrys tritubus	6.34
	Stichocorys johnsoni	6.79
	Calocycletta (Calocycletta) cladara	6.84
	Stichocorys delmontensis	6.90
	Diartus hughesi	7.75
	Didymocyrtis antepenultima	7.75
	Dictyocoryne ontongensis	7.94
	Botryostrobus miralestensis	8.23
	Diartus petterssoni	8.84
	Didymocyrtis laticonus	8.84
	Lithopera (Lithopera) neotera, Stichocorys wolffii	8.87
	Cyrtocapsella japonica, Lithopera (Glomaria) thornburgi	9.86
	Carpocanopsis cristata	10.67
	Lithopera (Lithopera) renzae, Cyrtocapsella cornuta, Cyrtocapsella tetrapera	12.13
	Calocycletta (Calocycletta) virginis, Dorcadospyris alata, Liriospyris parkerae	13.67
	Didymocyrtis mammifera	14.10
	Carpocanopsis bramlettei	14.68
	Calocycletta (Calocyclissima) costuta, Didymocyrtis tubaria, Didymocyrtis violina	15.00
	Dorcadospyris dentata	15.66
	Dorcadospyris forcipata	15.66
	Eucyrtidium diaphanes	15.88
	Liriospyris stauropora	16.11
	Carpocanopsis favosa	16.33
	Didymocyrtis prismatica	16.55
	Carpocanopsis cingulata	16.78
	Lychnocanoma elongata	17.00
	Dorcadospyris ateuchus	17.77
	Theocyrtis annosa	20.05
	Calocycletta (Calocyclopsis) serrata	20.61
	Calocycletta (Calocycletta) robusta	21.17
	Artophormis gracilis	23.11
	Dorcadospyris papilio	23.64
	Lychnocanoma trifolium	24.88
	Lithocyclia angusta	27.80
	Tristylospyris triceros	28.77
	Theocyrtis tuberosa	29.16
	Lithocyclia crux	29.54
	Dorcadospyris pseudopapilio	30.31
	Centrobotrys petrushevskayae	30.70
	Centrobotrys gravida	31.47
	Artophormis barbadensis	31.85
	Dictyoprora pirum	32.62
	Lithocyclia aristotelis group	33.01
	Cryptocarpium ornatum, Dictyoprora mongolferi, Lychnocanoma amphitrite	33.01
	Dictyoprora armadillo	33.51
	Lophocyrtis (Lophocyrtis) jacchia	34.01
	Calocyclas turris, Thyrsocyrtis (Thyrso.) bromia, Thyrsocyrtis (Thyrso.) rhizodon, Cryptocarpium azyx	34.50
	Thyrsocyrtis (Pentalacorys) tetracantha	35.00
	Thyrsocyrtis (Pentalacorys) lochites, Calocyclas bandyca, Calocyclas hispida, Lychnocanoma bellum, Podocyrtis (Podocyrtis) papalis	35.00
	Thyrsocyrtis (Pentalacorys) triacantha	35.27
	Eusyringium fistuligerum	35.80
	Podocyrtis (Lampterium) goetheana	36.06
	Podocyrtis (Lampterium) chalara	36.60
	Calocyclas hispida	37.15
	Spongatractus pachystylus	37.58
	Theocotylissa ficus	37.88
	Sethochytris triconiscus	38.04
	Lithocyclia ocellus group	38.34
	Podocyrtis (Lampterium) trachodes	38.64
	Podocyrtis (Lampterium) mitra	38.93
	Phormocyrtis striata striata	38.93
	Podocyrtis (Podocyrtoges) ampla	40.39
	Eusyringium lagena, Podocyrtis (Lampterium) fasciolata, Podocyrtis (Lampterium) helenae	41.11
	Podocyrtis (Lampterium) sinuosa	41.84
	Podocyrtis (Podocyrtoges) dorus	42.51
	Eusyringium lagena	42.85
	Podocyrtis (Podocyrtoges) phyxis	43.52
	Theocotyle venezuelensis	43.52
	Podocyrtis (Podocyrtoges) diamesa, Theocotyle nigriniae, Theocotyle conica, Theocorys anaclasta, Lamptonium fabaeforme constrictum, Lamptonium fabaeforme chaunothorax, Thyrsocyrtis (Thyrso.) hirsuta, Thyrsocyrtis (Thyrso.) robusta	45.68
	Thyrsocyrtis (Pentalacorys) tensa	46.76
	Lamptonium fabaeforme fabaeforme	47.16
	Theocotyle cryptocephala	47.55
	Calocycloma castum	47.94
	Podocyrtis (Lampterium) acalles	48.11
	Theocotyle nigriniae	48.60
	Buryella clinata	48.60
	Spongatractus balbis	48.91
	Lamptonium sanfilippoae	49.22
	Phormocyrtis striata exquisita, Phormocyrtis cubensis	50.14
	Pterocodon(?) ampla, Bekoma bidartensis, Buryella tetradica, Thyrsocyrtis (Thyrsocyrtis) tarsipes	50.91
	Theocotylissa alpha	51.69
	Pterocodon (?) anteclinata	53.23
	Lamptonium pennatum	55.79
	Bekoma campechensis	57.07
	Buryella pentadica	59.21
	Peritiviator (?) dumitricai	59.99
	T. pulchra, T. veneta, C. pulchrum, X. spicularius	94.08
	A. diaphorogona, A. irregularis, A. horridus	95.18
	A. dendroacanthos,  C. triangulare, D. gracilis	96.10
	D. obesa	97.54
	T. conica	104.85
	A. umbilicata	110.30
	Sphaerostylus lanceola	116.20
	P. boesii	121.00
	B. helenae, P. tythopora	121.90
	C. biopodium, C. infundibuliforme	125.44
	North Sea: Tricolocapsa sp.1 and sp.2, P. jonesi s.l., S. devorata, Cenosphaera sp.1, P. 'hispida'	140.55
	North Sea: O. mclaughlini, T. 'obesa'; and Highest prominent S. devorata, Cenosphaera sp.1 and P. 'hispida' 	142.84
	E. orea	145.46
	North Sea: End of Radiolarian influx, P. jonesi s.l. (prominent), Spondodiscus sp.4 (LCO)	146.32
	North Sea: Cenodiscus sp.3	147.43
	North Sea: Cenosphaera sp.1 (LCO), Cenodiscus sp.1 (LCO)	148.92
	North Sea: O. lowreyensis	149.26
	North Sea: P. hexagona (LCO), Cenosphaera sp.1 (prominent)	150.02
	Pantanellium riedeli	150.84
	North Sea: P. blowi (LCO), Cenosphaera sp.1 (LCO), P. jonesi (LCO)	153.16
	Pseudocrucella adriani, Tritrabs rhododactylus	154.40
	North Sea: Stichocapsa sp.1	162.52
	North Sea: O. iniqua	163.20
	Thetis bernouillii	163.37
	Mesosaturnalis tetraspinus	167.68
	Zartus dickinsoni	170.23
	B. deweveri, C. deweveri, P. spinosa	203.64
	C. triassica	211.24
	P. dercourti	216.53
	P. anisicus	234.56
	RADIOLARITE GAP of Earliest Triassic !!	250.38
FAD
	Buccinosphaera invaginata	0.18
	Collosphaera tuberosa	0.61
	Pterocorys hertwegii	0.74
	Anthocyrtidium euryclathrum	0.91
	Lamprocyrtis nigriniae	1.15
	Anthocyrtidium angulare	1.81
	Pterocorys zancleus	1.85
	Cycladophora davisiana	2.58
	Lamprocyrtis neoheteroporus	2.65
	Theocorythium trachelium trachelium.	2.69
	Didymocyrtis tetrathalamus tetrathalamus	3.09
	Amphirhopalum ypsilon	4.01
	Spongaster tetras tetras	4.13
	Didymocyrtis avita	4.19
	Pterocanium prismatium	4.91
	Spongaster pentas	5.49
	Pterocorys campanula	5.67
	Stichocorys peregrina	6.90
	Solenosphaera omnitubus procera, Soleno. omni. omnitubus	7.41
	Stichocorys delmontensis	7.75
	Didymocyrtis penultima	7.75
	Acrobotrys tritubus	7.94
	Spongaster berminghami	8.35
	Diartus hughesi	8.84
	Didymocyrtis antepenultima.	8.84
	Lithopera (Lithopera) bacca, Phormostichoartus doliolum	8.87
	Diartus petterssoni	12.01
	Lithopera (Lithopera) neotera	12.13
	Calocycletta (Calocycletta) cladara, Cyrtocapsella japonica	13.67
	Didymocyrtis laticonus	14.10
	Lithopera (Lithoperu) renzae, Lithopera (Glomaria) thornburgi, Phormostichoartus corbula, Dictyocoryne ontongensis	15.00
	Dorcadospyris alata	15.66
	Liriospyris parkerae	16.11
	Carpocanopsis cristata	16.78
	Calocycletta (Calocyclissima) costata	17.00
	Didymocyrtis mammifera	17.16
	Calocycletta (Calocyclior) caepa	17.31
	Dorcadospyris dentata	17.47
	Liriospyris stauropora	17.62
	Stichocorys wolffii	17.77
	Siphostichartus corona	17.77
	Didymocyrtis tubaria, Didymocyrtis violina, Stichocorys delmontensis, Carpocanopsis bramlettei	18.91
	Carpocanopsis favosa	21.73
	Cyrtocapsella cornuta	22.28
	Cyrtocapsella tetrapera	22.84
	Calocycletta (Calocyclopsis) serrata, Calocycletta (Calocycletta) virginis, Bottyostrobus miralestensis.	22.84
	Eucyrtidium diaphanes	23.37
	Lychnocanoma elongata	23.90
	Curpocanopsis cingulata	23.90
	Dorcadospyris forcipata	24.88
	Calocycletta (Calocycletta) robusta	25.85
	Dorcadospyris papilio	26.83
	Dorcadospyris ateuchus	28.77
	Theocyrtis annosa	29.16
	Lychnocanoma trifolium	29.93
	Didymocyrtis prismatica	30.31
	Centrobotrys thermophila	30.70
	Lychnodictyum audax	31.08
	Centrobotrys petrushevskayae, Dorcadospyris pseudopapilio	31.47
	Artophormis gracilis, Lithocyclia crux	31.85
	Centrobotrys gravida	32.24
	Phormostichoartus fistula	32.62
	Lithocyclia angusta	33.01
	Theocyrtis tuberosa	35.53
	Calocyclas bandyca	36.32
	Lychnocanoma amphitrite	36.87
	Calocyclas turris	37.15
	Cryptocarpium azyx	37.43
	Thyrsocyrtis (Thyrsocyrtis) bromia	37.73
	Thyrsocyrtis (Pentalacorys) tetracantha, Dictyoprora pirum,	37.88
	Dictyoprora armadillo	38.19
	Podocyrtis (Lampterium) goetheana	38.34
	Lithocyclia aristotelis group	38.34
	Podocyrtis (Lampterium) chalara	38.93
	Tristylospyris triceros	38.93
	Cryptocarpium ornatum	39.66
	Artophormis barbadensis, Thyrsocyrtis (Pentalacorys) lochites, Sethochytris triconiscus,	41.11
	Podocyrtis (Lampterium) mitra	41.84
	Podocyrtis (Lampterium) trachodes	42.17
	Eusyringium fistuligerum	42.85
	Podocyrtis (Lampterium) fasciolata, Podocyrtis (Lampterium) helenae	43.18
	Podocyrtis (Podocyrtoges) ampla	43.52
	Eusyringium fistuligerum	44.60
	Podocyrtis (Podocyrtoges) phyxis	45.68
	Eusyringium lagena	46.76
	Thyrsocyrtis (Pentalacorys) triacantha	46.76
	Podocyrtis (Podocyrtoges) dorus	47.16
	Theocotyle conica	47.55
	Dictyoprora mongolfieri	47.94
	Podocyrtis (Lampterium) sinuosa	48.11
	Thyrsocyrtis (Thyrsocyrtis) robusta	48.27
	Theocotyle venezuelensis	48.44
	Theocotyle cryptocephala	48.60
	Spongatractus pachystylus	48.91
	Thyrsocyrtis (Thyrsocyrtis) rhizodon	49.53
	Podocyrtis (Podocyrtoges) diamesa	49.83
	Theocorys anaclasta	50.14
	Phormocyrtis striata striata, Lamptonium fabaeforme constrictum, Podocyrtis (Lampterium) acalles, Lychnocanoma bellum	50.14
	Theocotylissa ficus, Lithocyclia ocellus group, Thyrsocyrtis (Pentalacorys) tensa	51.69
	Calocyclas hispida	52.46
	Buryella clinata	53.23
	Spongatractus balbis, Lamptonium sanfilippoae, Theocotyle nigriniae, Thyrsocyrtis (Thyrsocyrtis) hirsuta	53.23
	Theocotylissa alpha	53.87
	Lamptoniumfabaeforme chaunothorax	54.51
	Pterocodon(?) anteclinata,  Lophocyrtis (Lophocyrtis) jacchia	55.15
	Lamptonium fabaeforme fabaeforme, Calocycloma castum	55.79
	Podocyrtis (Podocyrtis) papalis	56.43
	Bekoma bidartensis	57.71
	Phormocyrtis cubensis	58.07
	Stylotrochus nitidus,  Pterocodon (?) poculum	58.43
	Pterocodon(?) ampla	60.47
	Bekoma campechensis	60.95
	Buryella tetradica	61.65
	Buryella foremanae	63.38
	Stichomitra granulata	64.37
	Amphisphaera kina	64.99
	Amphisphaera aotea	65.44
	Amphipyndax tylotus	73.61
	Amphipyndax pseudoconulus	83.53
	Theocampe urna	85.85
	A. lirioides, D. multicostata	91.31
	A. superbum, Crucella cachensis, A. longipina	93.55
	C. pulchrum	97.54
	Pseudodictyomitra nakasekoi	98.54
	Dorypyle? anisa, Obesacapsula somphedia	99.64
	P. putahensis, D. formosa	100.27
	D. obesa, A. horridus, T. veneta	103.68
	A. dendroacanthos, C. triangulare, A. irregularis, T. pulchra, C. euganea, C. messinae, T. conica	104.85
	D. gracilis, R. euganeum, Pseudodictyomitra pseudomacrocephala	106.15
	Mita spoletoensis	108.59
	Mita gracilis	112.00
	Pseudodictyomitra lodogaensis	116.20
	T. conica, X. spicularius	117.70
	North Sea: Tricolocapsa sp.1 and sp.2	141.66
	A. helenae	145.46
	North Sea: P. hispita (FCO)	146.71
	Sethocapsa cetia	150.84
	Triactoma echiodes	154.40
	North Sea: Common Radiolaria	154.97
	Emiluvia pessagnoi	160.90
	Acanthocircus trizonalis	163.37
	North Sea: Stichocapsa sp.1	165.17
	Mirifusus dianae	165.91
	Emiluvia sedecimporata, Pantancilium riedeli	166.40
	Hsuum maxwelli, Eucyritidiellum ptyctum	167.68
	Andromeda depressa, Tricolocapsa plicarum, Mesosaturnalis tetraspinus	170.23
	L. validus	203.64
	P. dercourti, C. triassica, C. deweveri	228.01
	P. hellenica	240.00
	F. calcaneum	241.00
	RADIOLARITE GAP of Earliest Triassic !!	251.40




Diatoms	:	Diatom Zone	Diatom Zone Marker FAD/LAD	Other Neogene Diatom FAD/LAD	All Diatom Datums Combined	_METACOLUMN_OFF		NEOGENE = mainly Maruyama (2000; Table 3).  PALEOGENE = partly from J. Barron (in Hardenbol et al., SEPM charts, 1998)

Diatom Zone	block	60	196/213/23	notitle
	TOP	0
	NPD12	0.31
	NPD11	1.21
	NPD10	1.99
	NPD9	2.65
	NPD8	3.75
	NPD7Bc	4.85
	NPD7Bb	5.55
	NPD7Ba	6.83
	NPD7A	7.67
	NPD6B	8.66
	NPD6A	9.24
	NPD5D	9.96
	NPD5C	11.58
	NPD5B	12.94
	NPD5A	13.14
	NPD4Bb	14.48
	NPD4Ba	14.88
	NPD4Ba	15.87
	NPD3B	16.28
	NPD3A	16.88
	NPD2B	18.16
	NPD2B	19.86
	NPD1	23.41
	R. gel.	25.76
	B. ven.	28.2
	R. vig. s.z. b	28.94
	R. vig. s.z. a	30.38
	C. ret.	33.27
	C. exc.	33.5
	B. brun.	34.43
	A. mary.	39.41
	B. imp.	41.15
	H. gond.	43.03
	H. ala.	44.34
	Py. c.a.	45.63
	T. kan.	48.64
	C. obl.	49.78
	C. und.	52.15
	P. grac.	54.58
	H. inc.	59.71
	H. per.	63.56
	H. ros. - T. hei.	65.5

Diatom Zone Marker FAD/LAD	event		201/213/80
LAD
	Proboscia curvirostris	0.31
	Actinocyclus oculatus	1.21
	Neodenticula koizumii	1.99
	Neodenticula kamtschatica	2.65
	T. insigna	4.85
	Rouxia californica (LCO)	6.83
	Thalassionema schraderi (LCO)	7.67
	Denticulopsis simonsenii (LCO)	8.66
	Denticulopsis dimorpha	9.24
	Denticulopsis praedimorpha (LCO)	11.58
	Denticulopsis hyalina (LCO)	13.14
	Gladius spp.	65.5
FAD
	Neodenticula koizumii	3.75
	Thalassiosira oestrupii	5.55
	Denticulopsis dimorpha	9.96
	Denticulopsis praedimorpha	12.94
	Denticulopsis simonsenii	14.48
	Denticulopsis hyalina	14.88
	Denticulopsis lauta	15.87
	Denticulopsis praelauta	16.28
	Crucidenticula sawamurae	18.16
	Crucidenticula kanayae	16.88
	Thalassiosira fraga	19.86
	Thalassiosira praefraga	23.41
	Rocella gelida	25.76
	Bogorovia veniamini	28.2
	Rocella symmetrica	28.94
	Rocella vigilans	30.38
	Cestodiscus reticulatus	33.27
	Coscinodiscus excavatus	33.5
	Baxteriopsis brunii	34.43
	Asterlampra marylandica	39.41
	Brightwellia imperfecta	41.15
	Hemiaulus gondolaformis	43.03
	Hemiaulus alatus	44.34
	Pyxilla caput avis	45.63
	Triceratium kanayae	48.64
	Craspedodiscus oblongus	49.78
	Craspedodiscus undulatus	52.15
	Pyxilla gracilis	54.58
	Hemiaulus incurvus	59.71
	Hemiaulus periterus	63.56

Other Neogene Diatom FAD/LAD	event		201/213/80			mainly Maruyama (2000; Table 3)
LAD
	Thallassiosira jouseae	0.35
	Rhizosolenia matuyamai	0.99
	Coscinodiscus pustulatus	1.8
	Pyxidicula horridus	1.89
	Pyxidicula pustulata	2.06
	Thalassiosira convexa	2.34
	Neodenticula kamtschatica (LCO)	2.65
	Thalassiosira marujamica	3.14
	Thalassiosira jacksonii	3.24
	Rouxia californica	6.04
	Thalassiosira miocenica	6.13
	Thalassiosira praeconvexa	6.66
	Cavitatus jouseanus	6.88
	Thalassiosira minutissima	8.45
	Denticulopsis katayamae	8.56
	Lithodesmium reynoldsii	8.98
	Nitzschia heteropolica, Medialia splendida	10.99
	Crucidenticula nicobarica	12.53
	Denticulopsis hustedtii (LCO)	13.19
	Thalassiosira praeyabei	13.48
	Crucidenticula kanayae	14.67
	Denticulopsis praelauta	15.35
	Rocella gelida	21.53
FAD
	Rhizosolenia matuyamai	1.07
	Proboscia curvirostris	1.58
	Thalassiosira antiqua	1.66
	Fragilariopsis doliolus	1.99
	Neodenticula seminae	2.68
	Actinocyclus oculatus	3.83
	Thalassiosira latimarginata	5.08
	Thalassiosira praeoestrupii	6.22
	Neodenticula kamtschatica (FCO)	6.57
	Thalassiosira miocenica	6.57
	Thalassiosira jacksonii	7.17
	Neodenticula kamtschatica	7.46
	Nitzschia reinholdii	7.55
	Thalassionema schraderi (FCO)	8.45
	Thalassiosira antiqua	8.56
	Thalassiosira marujamica	8.71
	Denticulopsis katayamae	9.35
	Thalassionema schraderi	9.58
	Thalassiosira minutissima	9.84
	Hemidiscus cuneiformis	11.88
	Thalassiosira brunii	11.98
	Proboscia barboi	12.32
	Denticulopsis simonsenii (FCO)	13.14
	Thalassiosira grunowii	13.73
	Thalassiosira praeyabei	14.67
	Actinocyclus ingens nodus	15.1
	Actinocyclus ingens	17.52


All Diatom Datums Combined	event		201/213/80		off
LAD
	Proboscia curvirostris	0.31
	Thallassiosira jouseae	0.35
	Rhizosolenia matuyamai	0.99
	Actinocyclus oculatus	1.21
	Coscinodiscus pustulatus	1.80
	Pyxidicula horridus	1.89
	Neodenticula koizumii	1.99
	Pyxidicula pustulata	2.06
	Thalassiosira convexa	2.34
	Neodenticula kamtschatica	2.65
	Neodenticula kamtschatica (LCO)	2.65
	Thalassiosira marujamica	3.14
	Thalassiosira jacksonii	3.24
	T. insigna	4.85
	Rouxia californica	6.04
	Thalassiosira miocenica	6.13
	Thalassiosira praeconvexa	6.66
	Rouxia californica (LCO)	6.83
	Cavitatus jouseanus	6.88
	Thalassionema schraderi (LCO)	7.67
	Thalassiosira minutissima	8.45
	Denticulopsis katayamae	8.56
	Denticulopsis simonsenii (LCO)	8.66
	Lithodesmium reynoldsii	8.98
	Denticulopsis dimorpha	9.24
	Nitzschia heteropolica, Medialia splendida	10.99
	Denticulopsis praedimorpha (LCO)	11.58
	Crucidenticula nicobarica	12.53
	Denticulopsis hyalina (LCO)	13.14
	Denticulopsis hustedtii (LCO)	13.19
	Thalassiosira praeyabei	13.48
	Crucidenticula kanayae	14.67
	Denticulopsis praelauta	15.35
	Rocella gelida	21.53
	Gladius spp.	65.50
FAD
	Rhizosolenia matuyamai	1.07
	Proboscia curvirostris	1.58
	Thalassiosira antiqua	1.66
	Fragilariopsis doliolus	1.99
	Neodenticula seminae	2.68
	Neodenticula koizumii	3.75
	Actinocyclus oculatus	3.83
	Thalassiosira latimarginata	5.08
	Thalassiosira oestrupii	5.55
	Thalassiosira praeoestrupii	6.22
	Neodenticula kamtschatica (FCO)	6.57
	Thalassiosira miocenica	6.57
	Thalassiosira jacksonii	7.17
	Neodenticula kamtschatica	7.46
	Nitzschia reinholdii	7.55
	Thalassionema schraderi (FCO)	8.45
	Thalassiosira antiqua	8.56
	Thalassiosira marujamica	8.71
	Denticulopsis katayamae	9.35
	Thalassionema schraderi	9.58
	Thalassiosira minutissima	9.84
	Denticulopsis dimorpha	9.96
	Hemidiscus cuneiformis	11.88
	Thalassiosira brunii	11.98
	Proboscia barboi	12.32
	Denticulopsis praedimorpha	12.94
	Denticulopsis simonsenii (FCO)	13.14
	Thalassiosira grunowii	13.73
	Denticulopsis simonsenii	14.48
	Thalassiosira praeyabei	14.67
	Denticulopsis hyalina	14.88
	Actinocyclus ingens nodus	15.10
	Denticulopsis lauta	15.87
	Denticulopsis praelauta	16.28
	Crucidenticula kanayae	16.88
	Actinocyclus ingens	17.52
	Crucidenticula sawamurae	18.16
	Thalassiosira fraga	19.86
	Thalassiosira praefraga	23.41
	Rocella gelida	25.76
	Bogorovia veniamini	28.20
	Rocella symmetrica	28.94
	Rocella vigilans	30.38
	Cestodiscus reticulatus	33.27
	Coscinodiscus excavatus	33.50
	Baxteriopsis brunii	34.43
	Asterlampra marylandica	39.41
	Brightwellia imperfecta	41.15
	Hemiaulus gondolaformis	43.03
	Hemiaulus alatus	44.34
	Pyxilla caput avis	45.63
	Triceratium kanayae	48.64
	Craspedodiscus oblongus	49.78
	Craspedodiscus undulatus	52.15
	Pyxilla gracilis	54.58
	Hemiaulus incurvus	59.71
	Hemiaulus periterus	63.56




Belemnite Zones	:	NW Europe Belemnite Zone	NW Europe subzone (Jur.)	Balto-Scandia (Lt. Cret.)	Tethyan (Oxf-Haut)	Tethyan subzone (Lt.Jur.)	Russian Platform (Lt. Cret.)	_METACOLUMN_OFF		R. Combemorel (in Hardenbol et al., SEPM charts, 1998)

NW Europe Belemnite Zone	block	150	204/153/186
	TOP	65.5
	No Zone	66.25
	Belemnitella baltica / danica	66.99
	Belemnitella danica / argenta	67.74
	Belemnitella argenta / junior	68.48
	Belemnitella junior / tegulatus	69.23
	Belemnella fastigata	69.46
	Belemnella cimbrica	69.68
	Belemnella sumensis	69.91
	Belemnella obtusa	70.14
	Belemnella pseudobtusa	70.36
	Belemnella lanceolata	70.60
	Belemnitella "langeli"	73.61
	Belemnitella "minor"	74.11
	Belemnitella mucronata	80.64
	Gonioteuthis quadratagracilis / Belemnitella mucronata	80.84
	Gonioteuthis quadratagracilis	81.03
	Gonioteuthis quadrataquadrata	82.28
	Gonioteuthis quadrataquadrata / Belemnitella praecursor	83.53
	Gonioteuthis granulata	84.40
	Gonioteuthis westfalicagranulata	84.69
	Gonioteuthis westfalica westfalica	85.85
	Gonioteuthis westfalica praewestfalica	87.20
	TOP	93.92
	Actinocamax plenus	94.12
	TOP	95.64
	Actinocamax primus	98.67
	Neohibolites ultimus	99.54
	Neohibolites praeultimus	103.68
	Neohibolites oxycaudatus	106.42
	Neohibolites minumus	109.80
	Neohibolites minor	111.12
	Neohibolites strombecki	112.00
	Neohibolites wollemani	115.00
	Neohibolites inflexus	118.00
	Neohibolites clava	120.00
	Neohibolites ewaldi	122.42
	[unnamed zone]	124.48
	Oxyteuthis depressa	125.73
	Oxyteuthis germanica	127.36
	Oxyteuthis brunsvicensis	128.63
	Aulacoteuthis spp.	128.97
	Praeoxyteuthis pugio	129.97
	Hibolites jaculoides	135.15
	Acroteuthis acmonoides	137.43
	Acroteuthis acrei	139.21
	Acroteuthis kemperi	140.18
	Pachyteuthis explanatoides	144.46
	Pachyteuthis souichii	150.63
	Pachyteuthis explanatus	155.65
	Cylindroteuthis obeliscus	161.21
	Rhopaloteuthis gillieroni 	164.74
	Duvalia disputabilis	167.68
	Megateuthis elliptica	171.60
	Homaloteuthis spinatus	174.71
	Brevibelus subaduncatus	175.60
	Brevibelus breviformis and Acrocoelites curtus	180.50
	Acrocoelites wrighti 	180.70
	Acrocoelites ilmintrensis	182.70
	Passaloteuthis bisulcatus 	183.00
	Passaloteuthis zieteni  	186.95
	Hastites clavatus	189.60
	Nannobelus acutus 	196.50
	TOP	198.44
	Schwegleria	199.60

NW Europe subzone (Jur.)	block	120	204/153/186	notitle
	TOP	144.46
	Pachyteuthis lateralis	148.92
	TOP	161.21
	Rhopaloteuthis gillieroni and Hibolites semihastatus	162.35
	TOP	163.20
	Dicoelites meyrati	164.74
	TOP	166.31
	Duvalia disputabilis and Belemnopsis fusiformis	167.68
	Belemnopsis apiciconus	170.23
	TOP	170.42
	Eocylindroteuthis trauscholdi	171.60
	TOP	173.38
	Belemnopsis brevicanalis	174.71
	Acrocoelites bobeti	177.56
	TOP	180.70
	Acrocoelites striolatus	181.20
	Acrocoelites trisulculosus	182.70
	TOP	186.95
	Passaloteuthis apicicurvatus	188.54
	Coeloteuthis dens and Coeloteuthis excavatus	189.60
	Nannobelus oppeli 	193.19
	Nannobelus acutus	196.50

Balto-Scandia (Lt. Cret.)	block	150	204/153/186
	TOP	70.33
	Belemnella lanceolota	70.60
	TOP	74.30
	Belemnitella mucronata	77.64
	Belemnellocamax balsvikensis	80.64
	Gonioteuthis quadratagracilis / Belemnitella mucronata / Belemnellocamax mamillatus	82.30
	Gonioteuthis quadrataquadrata / Belemnitella alpha	83.53
	Gonioteuthis granulata	84.40
	Gonioteuthis westfalicagranulata / Belemnitella propinqua	84.81
	Gonioteuthis westfalica westfalica / Belemnitella propinqua / Goniocamax lungreni	85.85
	Goniocamax lungreni	89.07
	TOP	93.92
	Actinocamax plenus	94.12
	TOP	95.62
	Actinocamax primus	98.67
	Neohibolites ultimus	99.54

Tethyan (Oxf-Haut)	block	120	204/153/186
	TOP	135.80
	Duvalia gervaisiana	136.75
	Duvalia emerici	139.21
	Duvalia lata	145.46
	Duvalia ensifer and Rhopaloteuthis strangulatus	150.84
	Hibolites semisulcatus	154.53
	Duvalia didayanus and Duvalia duvalianus	161.21


Tethyan subzone (Lt.Jur.)	block	120	204/153/186	notitle
	TOP	156.81
	Duvalia dumortieri and Rhopaloteuthis spissus 	159.61
	Rhopaloteuthis bzoviensis	161.21

Russian Platform (Lt. Cret.)	block	150	204/153/186
	TOP	65.50
	Belemnella casimirovensis	67.18
	Belemnitella junior	69.23
	Belemnella licharewi	70.60
	Belemnitella langeli najdini	71.30
	Belemnitella langeli langei	73.55
	Belemnitella langei minor	74.49
	Belemnitella mucronata	80.64
	Gonioteuthis quadratagracilis / Belemnitella mucronata	80.81
	Belemnitella alpha/ Belemnitella praecursor /Gonioteuthis quadrata quadrata 	82.39
	Gonioteuthis quadrataquadrata / Belemnitella praecursor	83.53
	Gonioteuthis granulata / Belemnitella praecursor	84.34
	Belemnitella propinqua / Goniocamax lundgreni uilicus	85.85
	Goniocamax lungreni	88.58
	Actinocamax plenus triangulus	93.55
	Actinocamax plenus	96.01
	Actinocamax primus / Neohibolites ultimus	99.54


Inoceramids (Lt.Cret.)	:	Central European/ Russian Platform Zones	Central European/ Russian Platform FAD/LAD	Western European Inoceramid FAD/LAD	Aquitaine Inoceramids	_METACOLUMN_OFF		A.V. Dhondt (in Hardenbol et al., SEPM charts, 1998)

Central European/ Russian Platform Zones	block	150	204/156/140	notitle
	TOP	65.5
	Tenuipteris argentea	68.00
	Spyridoceramus tegulatus	69.30
	TOP	82.30
	Cordiceramus muelleri / Sphenoceramus patootensiformis	84.34
	Sphenoceramus pinniformis	84.63
	Cordiceraumus undulatoplicatus / Sphenoceramus cardissoides	85.85
	Magadiceramus subquadratus	87.24
	Volviceramus koeneni	88.55
	Inoceramus schloenbachi	89.07
	Inoceramus costellatus	90.89
	Inoceramus cuvieri/ lamarcki	91.72
	Mytiloides hercynicus	91.88
	Mytiloides labiatus/ hercynicus	92.70
	Mytiloides labiatus	93.55
	Inocermaus pictus lineage	95.06
	Inoceramus crippsi	99.57

Central European/ Russian Platform FAD/LAD	event		204/170/159
LAD
	Tr. morgani. Spyridoceramus tegulatus, Tr. nahorianensis	69.23
	Sph. aff. ingua, Sph. angustus, Sph. patootensiformis	81.63
	Cordiceramus cordiformis. S.c. cardissoides, P. cyc. ahnesensis	84.34
	Cordiceraumus undulatoplicatus, S. p. reticulus	84.63
	M. s. crenistriatus, M. s. subquadratus, S. subcardissoides, V. koeneni, M. s. crenelatus, V. involutus, S. fasciculatus 	85.85
	C. kleini, V. percostatus, C. frechi, P. m. mantelli, P. m. subrheanus, V. incurvatissimus, P. m. beyenburgi	87.77
	C. ernsti, C. schloenbachi, I. lusatiae, I. rotundatus, C. i. lueckendorfensis, I. w. waltersdorfensis, I. w. hannovrensis	88.58
	Inoceramus c. costellatus, M. incertus, I. d. labiatoidiformis, I.[H.] hercules,  I. c. pietzschi, I. d. dresdensis, I. s. striatoconcentricus, I. striat. aff. carpathicus	89.07
	I. brevealatus, I.i. stuemckei, I. i. lamarcki, M. hercynicus, I. saxonicus, M. labiatus, I. cuvieri, I. apicalis, I. s. striatocostatus, M. subhercynicus, I. i. inaequivalvis	90.48
	Mytiloides mytiloides,  My. goppeinensis	92.13
	I. p. pictus	92.70
	I. atlanticus, Inoceramus crippsi hoppenstedtensis	94.75
	Inoceramus c. cripsi	95.23
FAD
	Tenuipteris argentea	69.23
	Tr. nahorianensis, Spyridoceramus tegulatus, Tr. morgani	69.71
	Cordiceramus muelleri, Cordiceramus haenleini, Sphenoceramus pinniformis, Spheno. cardissoides, Spheno. patootensiformis, Sph. angustus, Sph. aff. lingua 	84.34
	S.c. subreticulus	84.63
	Cordiceraumus undulatoplicatus, Sphenoceramus c. cardissoides, S. pachti pachti, S. p. reticulus, C. cordiformis, P. c. cycloides, P. c. ahnesensis	85.85
	Magadiceramus s. subquadratus, S. fasciculatus, M.s. crenelatus, M.s. crenistriatus, S. subcardissoides	87.77
	Volviceramus koeneni, P. m. mantelli, V. percostatus, V. involutus, P. m. beyenburgi, V. incurvatissimus, C. frechi, P. m. subrheanus, C. kleini	88.55
	C. ernsti, C. schloenbachi, I. w. hannovrensis, C. i. lueckendorfensis, I. rotundatus	89.07
	I. w. waltersdorfensis, I. c. costellatus, I.[H.] hercules, I. striat. aff. carpathicus, I. d. dresdensis, M. incertus, I. d. labiatoidiformis, I. lusatiae	90.48
	I. l. stuemckei, I. i. inaequivalvis, I. cuvieri, I. apicalis, I. s. striatocostatus, I. lamarcki lamarcki, I. saxonicus, I. brevealatus, I. c. pietzschi, I. p. bohemicus, Mytiloides hercynicus, My. subhercynicus	92.13
	I. p. bohemicus	93.56
	I. p. pictus, I.p. bannewitzensis, I. neocaledonicus,  I. p. concentricoundulatus, 	94.75
	I. atlanticus	95.23
	I. e. etheridgei, I. r. reachensis, I. schoendorfi	96.01
	I. tenuis	97.81
	I. vigatus virgatus, I. vigatus scalprum, Inoceramus crippsi hoppenstedtensis	98.67
	Inoceramus c. crippsi	99.57

Western European Inoceramid FAD/LAD	event		204/170/159
LAD
	Ca. regularis	70.60
	Sph. aff. lingua, Se. inflexus, Sph. aff. angustus, Sph. patootensiformis, Sph. nasutus, E. flexibaltica, Pl. adversus, Pl. rhomboides, Se. selenae	80.84
	Sph. ccardissoides subreticulus, S. pachtireticulus, S.c. cardissoides, 	84.34
	S. subcardissoides, Ma. s. subquadratus, Ma. subquadratus crenelatus, S. fasciculatus, P. mantelli undatus, P.  mantelli mantelli, V. involutus, V. koeneni	85.85
	Cr. kleini, Vo. percostatus, Pl. mantelli beyenburgi, Pl. mantelli subrheanus, Vo. incurvatissimus	87.77
	I. lusatiae	88.58
	I. striat. aff. carpathicus, I. d. dresdensis, I.c. costellatus, I.[H.] hercules, I. i. falcatus	89.02
	I. lamarcki lamarcki, Mytiloides hercynicus, I. cuvieri, I. apicalis, My. subhercynicus, I. i. inaequivalvis, M. goppelnensis, I. lamarcki stuemckei, M. mytiloides, My. labiatus	90.48
	Mytiloides submytiloides	92.13
	I. p. pictus, I.? pedalinoides, I.? tenuimbonatus	93.55
	I. prefragilis, I.? ginterensis	93.72
	I. f. flavus, Inoceramus c. crippsi, I. schoendorfi, I. atlanticus, I.? e. etheridgei, I. r. reachensis, I. anglicus conjugalis	94.75
	I. tenuis, I. vigatus scalprum, I. vigatus vigatus, Inoceramus crippsi hoppenstedtensis	95.06
	I. a. arvanus	95.23
FAD
	Ca. regularis, End. Pteroides	80.84
	End. b. baltica, End. flexibaltica, Pl. adversus, Pl. rhomboides, Se. selenae, Se. inflexus	83.53
	S. angustus, Sph. martinii, S. pinniformis, S. cardissoides, S. aff. lingua, S. patootensiformis, C. muelleri	84.34
	C. haenleini, C. cordiformis, C. cordiinitialis, C. brancoformis	84.63
	S. pachti pachti, P. cycloides cycloides, P. cycloides wegneri, S. pachti reticulus, P. cycloides ahnesensis, S. cardissoides subreticlus, S. cardissoides cardissoides, C. undulatoplicatus	85.85
	Sph. fasciculatus, Ma. subquadratus crenelatus, Ma. subquadratus subquadratus, Sph. subcardissoides	87.77
	Vo. incurvatissimus, Vo. percostatus, Vo. involutus, Pl. mantell beyenburgi, Vo. koeneni, Pl. mantell subrheanus, Cr. kleini, Pl. mantell mantelli, Pl. mantell undatus	88.58
	C. ernsti, C. schloenbachi, I. w. hannovrensis, I. w. waltersdorfensis, I. rotundatus, C. inconstans lueckendorfensis	89.02
	I.[H.] hercules, I. c. costellatus, I. d. dresdensis, I. striatoconcentricus aff. carpathicus	90.48
	I. lusatiae, I. inaequivalvis falcatus, I. lamarcki stuemckei, I. cuvieri, I. apicalis, I. inaequivalvis inaequivalvis, I. lamarcki lamarcki	92.13
	Mytiloides submytiloides, My. subhercynicus	92.70
	Mytiloides goppelnensis, My. hercynicus, My. mytiloides, My. labiatus	93.55
	I. p. bohemicus	94.01
	I. tenuimbonatus, I. pictus bannewitzensis, I.? pedalinoides	94.75
	I. ginterensis, I. prefragilis, I. p. pictus	95.23
	I. schoendorfi, I. atlanticus	96.01
	Inoceramus crippsi hoppenstedtensis, I.? e. etheridgei, I. f. flavus, I. a. arvanus, I. vigatus scalprum, I. vigatus vigatus	98.72
	Inoceramus c. crippsi, I. tenuis, I. r. reachensis, I. anglicus conjugalis	99.57

Aquitaine Inoceramids	event		204/170/159
FAD
	Tr. nahorianensis, Ca. pteroides	70.60
	Tr. tenuiplicatus	80.50
	E. flexibaltica, Pl. alaeformis	80.64
	Ca. goldfussianus, Pl. artigesi, Co. muelleri	83.53
	Pl. adversus, Pl. ezoensis, Co. cordiformis, Se. inaequabilis, Se. regularis, End. b. baltica, "I". borilensis	85.10
	C. cordiinitialis, C. bueltensis, C. brancoiformis	85.85
LAD
	Tr. nahorianensis	65.50
	End. b. baltica, Ca. pteroides, Tr. tenuiplicatus	69.23
	Pl. alaeformis, "I". borilensis, Pl. artigesi	70.60
	End. flexibaltica, Ca. goldfussianus, Pl. adversus, Co. muelleri	80.50
	Se. regularis, Se. inaequabilis	80.64
	Co. cordiformis, End. b. baltica	83.53
	C. cordiinitialis, C. brancoiformis, C. bueltenensis	84.63


Brachiopod	:	Tethyan Brachiopod zone (Early-Mid Jur)	Tethyan Brachiopod subzone	Boreal Brachiopod zone (Middle-Late Jur)	Boreal Brachiopod subzone	_METACOLUMN_OFF		B. Laurin (in Hardenbol et al., SEPM charts, 1998)

Tethyan Brachiopod zone (Early-Mid Jur)	block	120	152/133/193
	TOP	162.35
	Dorsoplicathyris dorsoplicata	163.20
	Robustirhynchia tenuiformis and Aromasithyris almerasi	164.23
	TOP	165.13
	Wattonithyris circumdata and Arceythyris dipthycha	165.33
	Burmirhynchia turgida and Tubithyris globata	166.11
	TOP	166.31
	Antiptychina bivallata	166.50
	TOP	166.89
	Formosarhynchia dumortieri	167.87
	TOP	168.86
	Lissajousithyris matisconensis	169.64
	TOP	170.23
	Monsardithyris cortonensis	171.21
	Conarothyris opima	172.49
	Pseudoglossothyris brebissoni and Monsardithyris trilineata	174.71
	Rhynchonelloidea ruthenensis and Globirhynchia prava	175.60
	Stroudithyris infraoolithica and Stroudithyris stephanoides	179.19
	TOP	180.60
	Sphaeroidothyris vari and S. decipiens	180.95
	Homoeorhynchia meridionalis and Telothyris jauberti	182.70
	Liospiriferina falloti and Aulacothyris iberica 	183.00
	Quadratirhynchia quadrata and Zeilleria (Z.) quadrifida	183.80
	Gibbirhynchia amalthei and Zeilleria (Z.) sarthacensis	185.58
	Rudirhynchia rudis	187.22
	Gibbirhynchia curviceps	189.60
	Spiriferina betacalcis, Piarorhynchia juvenis and Zeilleria (Cincta) cor	193.25
	Cuneirhynchia oxynoti and Zeilleria (Z.) vicinalis	196.50
	Zeilleria (Zeilleria) perforata	199.60

Tethyan Brachiopod subzone	block	120	152/133/193	notitle
	TOP	166.89
	Rugitela cadomensis and Tubithyris whatleyensis 	167.48
	Gnathorhynchia voultensis 	167.87
	TOP	170.23
	Morrisithyris phillipsiana 	170.62
	M. cortonensis and Cymatorhynchia gingensis 	171.21
	Loboidothyris perovalis 	171.60
	Rhynchonelloidea subangulata and C. opima	172.49
	Stroudithyris pisolithica	173.82
	Ferrythyris elianae	174.71
	TOP	175.60
	Homoeorhynchia cynocephala and Zeilleria (Z.) lycetti	177.07
	Stroudithyris infraoolithica and Stroudithyris stephanoides	179.19
	TOP	180.60
	Sphaeroidothyris vari and S. decipiens	180.70
	Sphaeroidothyris perfida	180.95
	Telothyris jauberti and Homoeorhynchia meridionalis	181.20
	Stolmorhynchia bouchardi	182.70
	Nannirhynchia pygmoea and Koninckella bouchardi 	182.93
	TOP	187.22
	Gibbirhynchia curviceps 	188.01
	Cuersithyris davidsoni and Cuersithyris radstockiensis 	189.60

Boreal Brachiopod zone (Middle-Late Jur)	block	120	128/156/201
	TOP	150.50
	Terebratula portlandica	150.63
	TOP	150.84
	Xestosina arguta	151.98
	Terebratula gr. subselloides	153.54
	Terebratula suprajurasensis	154.19
	Terebratula subsella	154.97
	Terebratula aff. lusitanica	155.65
	Zeilleria astartina	157.26
	Juralina bauhini	157.88
	Galliennithyris bourgueti	158.43
	Galliennnithyris galliennei	159.85
	Aulacothyris impressa	161.21
	Aromasithyris dreyfussi	162.18
	Septaliphoria orbignyana and Dorsoplicathyris dorsoplicata	163.20
	Rhynchonelloidella spathica	164.40
	TOP	164.74
	Burmirhynchia elegantula	165.13
	Wattonithyris circumdata	165.72
	Kallirhynchia concinna	166.50
	TOP	167.29
	Rugitela cadomensis	167.48
	Terebratula movelierensis 	167.87
	Aulacothyris carinata and Ferrythyris ferryi	168.86
	Lissajousithyris matisconensis	169.84
	Pavirhynchia parvula	170.23
	Monsardithyris cortonensis	171.21
	Conarothyris opima	172.49
	Pseuodoglossothyris brebissoni	174.71
	TOP	175.16
	Conarothyris conglobata	175.60
	Stroudithyris infraoolithica and Zeilleria (Z.) lycetti	179.19
	TOP	180.57
	Pseudogibbirhynchia jurensis	180.95
	Telothyris jauberti and Telothyris pyrenaica	182.93
	Quadratirhynchia quadrata and Zeilleria (Z.) quadrifida	183.80
	Zeilleria (Z.) sarthacensis	185.58
	Rudirhynchia rudis and Scalpellirhynchia scalpellum	187.13
	Zeilleria (Cincta) numismalis	189.60
	Piarorhynchia juvenis and Zeilleria (Cincta) cor	193.25
	Zeilleria (Z.) vicinalis and Spiriferina walcotti	196.50
	Zeilleria (Zeilleria) perforata	199.60

Boreal Brachiopod subzone	block	120	128/156/201	notitle
	TOP	155.77
	Postepithyris cincta	156.27
	Dorsoplicathyris subinsignis	156.89
	TOP	162.18
	Septaliphoria orbignyana and Dorsoplicathyris dorsoplicata	162.86
	Aromasithyris aromasiensis	163.20
	Aromasithyris almerasi and Septaliphoria mourdoni	164.23
	Cererithyris nutiensis	164.40
	TOP	164.74
	Burmirhynchia proteiformis	164.93
	Goniorhynchia boueti	165.13
	TOP	167.48
	Millithyris arvierensis	167.68
	TOP	169.64
	Goniothyris craneae	169.84
	TOP	170.23
	Cymatorhynchia pallas	170.62
	Monsardithyris cortonensis 	171.21
	Loboidothyris perovalis 	171.60
	Rhynchonelloidea subangulata and C. opima 	172.49
	TOP	173.82
	Ferrythyris elianae	174.71
	TOP	175.60
	Homoeorhynchia cynocephala	177.32
	TOP	181.70
	Stolmorhynchia bouchardi	182.70
	Koninckella bouchardi	182.93
	TOP	194.47
	Calcirhynchia calcaria	196.50


Siberian Pelecypod Zones (latest Tri.)	:	Pelecypod Zone	Pelecypod Subzone	_METACOLUMN_OFF		P. Van Veen (in Hardenbol et al., SEPM charts, 1998)

Pelecypod Zone	block	100	128/156/201	notitle
	TOP	199.60
	Tosapecten efimovae	203.64
	Monotis ochotica	205.71
	Monotis scutiformis	209.15
	Otapiria ussuriensis	210.01

Pelecypod Subzone	block	100	nocolor	notitle
	TOP	199.60
	Tosapecten efimovae	202.29
	Camptonectes nanus 	203.64
	Monotis subcircularis	204.67
	Monotis zabaikalika	205.71
	Monotis pinensis	207.43
	Monotis daonellaeformis	209.15 


Rudist Events	:	Western Europe rudists	Periadriatic rudists	_METACOLUMN_OFF		J.-P. Masse and J. Philip (in Hardenbol et al., SEPM charts, 1998)

Western Europe rudists	event
FAD
	P. leymeriei	67.87
	Hipuritella castrol	69.23
	H. radiosus	71.30
	Praeradiolites alatus, P. saemanni, P. haeninghausi	76.68
	Hippurites heberti, Hipuritella sulcatoides, H. variabilis, Vaccinites archiaci	83.53
	Hippurites bioculatus, Hipuritella carezi	84.05
	Hippurites sublaevis, Hipuritella toucasi, Vaccinites beaussetensis, V. dentatus, V. galloprovincialis, V. giganteus major	85.85
	Vaccinites giganteus, Hipuritella incisus, V. moulinsi	89.02
	Vaccinites petrocoriensis, V. praegiganteus	90.48
	V. rousseli, V. praepetrocoriensis, V. inferus, V. grossouvrei	92.13
	Durania arnaudi	92.91
	Vaccinites fontalbensis	93.55
	Caprina adversa	96.01
	Ichthysarcolithes triangularis	97.27
	Sphaerulites foliaceus	97.27
	D. pyrenaica, D. delphinensis	102.31
	C. choffati	107.01
	E. rousseli	109.06
	A.? darderi	113.00
	H. lamberti	115.00
	P. cantabricus, P. santanderensis P. verneuili	118.00
	E. plicatus	119.00
	E. katzeri	121.00
	H. almerae	121.45
	C. douvillei	124.48
	O. rhodanica	125.00
	M. virginiae, P. paradoxa, P. varians	126.10
	R. gryphoides, T. transversa, R. ammonia, M. varians, P. sulcata	128.97
	A.? marticensis, T. carinata	130.02
	A.? blumenbachi	132.95
	R. renevieri	133.18
	P. tubiconcha	136.46
	Lovetchenia sp.	136.75
	M. valangiensis, M. eurystoma, M. valdensis, V. tombecki	141.05
	M. rougonensis	142.50
	H. luci	142.67
LAD
	Hipuritella lapeirousei	66.50
	Praeradiolites haeninghausi	66.91
	D. cornupastois	89.02
	Caprinula boissyi, Sauvagesia sharpei, Radiolites lusitanicus	93.55
	H. lamberti	102.31
	A.? darderi, E. rousseli	103.68
	T. carinata	107.89
	E. plicatus, "P." cantabricus	110.53
	H. almerae	111.71
	E. katzeri	114.00
	O. rhodanica, T. transversa, R. grypholdes, A.? blumenbachi, A. marticensis, R. ammonia, P. paradoxa, C. douvillei, M. virginiae, M. varians, P. varians, P. sulcata	121.45
	R. renevieri	127.75
	P. tubiconcha	131.52
	Lovetchenia sp.	132.95
	H. luci, V. tombecki, M. valdensis, M. eurystoma, M. valangiensis	138.94
	M. rougonensis	140.18

Periadriatic rudists	event
FAD
	Hippurites cornucopiae	67.87
	V. ultimus, V. braciensis, Hippurites heritschi, H. colliciatus, Sabinia aniensi, Pironaea polystyla, P. milovanovici, 	71.30
	Vaccinites boehmi, V. anici, V. extremus, V. sulcatus	83.53
	Vaccinites atheniensis, V. gosaviensis, Gorjanovicia costata, V. oppeli	85.85
	Hippuritella incisus, V. giganteus	89.07
	Hippurites requieni	92.13
	Sphaerucaprina forojuliensis, Orthoptychus striatus,  N. gigantea, Schiosa carinatoformis, I. bicarinatus	97.27
	Caprina schiosensis, Sphaerucaprina forojuliensis, Neocaprina nanosi, Sauvagesi sharpei, Ichthyosarcolithes poljaki	99.57
	E. lyratus	108.77
	Sellaea spp., E. plicatus	110.83
	B. petersi, O. nicolinae, O. murgensis, Himeraelites sp.	125.00
	Lovetchenia sp.	126.65
LAD
	Bournonia adriatica	66.05
	Durania cornupastoris	89.07
	Caaprinula boissyi, Sauvagesia sharpei, Ichthyosarcolithes rotundus	93.55
	Lovetchenia sp., B. petersi, O. nicolinae,  O. murgensis, G. costatus	121.00




Ostracodes	:	Boreal Ostracodes	Tethyan Ostracodes	French Ostracode zone (Jur)	French subzone	French datum	_METACOLUMN_OFF		J.-P., Colin et al. (in Hardenbol et al., SEPM charts, 1998)

Boreal Ostracodes	event		178/181/175
LAD
	M. latimarginata parvipunctata	5.53
	C. moosi	16.39
	C. semipunctata	22.38
	H. montosa	28.45
	C. laticostata	33.46
	C. scrobiculoplicata, N. whitecliffensis	48.60
	M. gr. heiroglyphica	65.50
	C. lacertosa	70.60
	C. zygopleura	83.53
	P. calkeri	83.99
	N. vaneeni, M. harrisiana	95.62
	C. chapmani	100.94
	B. gualtina	106.42
	P. (K.) nodigera	108.77
	R. bekumensis	112.00
	S. tricostata	115.00
	P. intermedia	121.00
	S. hammi	123.97
	H. hechti, S. bilobata, P. triplicata	126.35
	S. praethorensis, C. frankei	135.37
	G. teres	139.98
	Galliaecytheridea polita	146.58
	Galliaecytheridea spinosa	146.83
	S.(Ektyphocythere) triebeli	151.96
	Galliaecytheridea dissimilis	152.38
	Nophrecythere cruciata oxfordiana	156.97
	Lophocythere interrupta	161.15
	Eudechacythere puncticava	162.86
	Praeschuleridea confossa	164.33
	Micropneumatocythere falcata	164.76
	Nophrecythere rimosa	164.97
	Eoschulderidea batei	165.58
	M. postangusta	167.04
	Glyptocythere scitula	169.65
	Glyptocythere polita	170.24
	Ektyphocythere triangula, Progonocythere carinata	170.64
	Progonocythere reticulata	171.25
	Kinkelinella gr. sermoisensis	172.51
	Trachycythere verrucosa	178.54
	Ektyphocythere debilis	180.60
	Ogmoconcha Ogmoconhella spp.	182.70
	Gramannella apostolescui	184.14
	K. foveolata, Wicherella semiora	185.16
	Pleurifera harpa, Gammacythere ubiquita	186.95
	Ektyphocythere moorei, Ogmoconchella aspinata	194.02
	Cytheretelloidea circumscripta	195.22
	Ogmoconcha moorei	199.60
	Ogmoconcha bristolensis	200.27
	K. germanica	222.70
	J. tsorfatia	228.01
	G. efforta prisca, S. alata levis	229.43
	T. fisheri	234.56
FAD
	M. latimarginata parvipunctata	15.77
	C. moosi	20.07
	L. scrobiculata	28.45
	C. semipunctata	29.45
	L. striatopunctata, H. hebertiana	33.46
	F. forbesi	36.92
	C. cellulosa, L. consobrina	45.00
	C. eoceanica	48.60
	N. whitecliffensis	50.30
	C. nerva nerva	59.90
	P. cirrusa	61.00
	K. montensis	61.92
	L. fissurata	64.71
	S. pseudoeximia, C. joergenseni	69.23
	C. major	67.32
	M. hieroglyphica	67.73
	M. macrophtalma, P. (D.) puncturata	68.14
	L. ornata, S. eximia, C. anorchidea 	70.60
	C. anorchidea, P. phylloptera	80.50
	P. lonsdaleianus	83.53
	C. lacertosa	84.69
	G. calkeri	87.77
	C. longaeva, C. zygopleura, I. gr. marssoni	89.78
	H, donzei, C. derooi	94.53
	D. inferangulata	95.62
	O. donzei	97.81
	R. gr. luermannae	107.01
	M. harrisiana	108.77
	R. reticulata	110.83
	P. (K.) nodigera	114.25
	S. tricostata	118.00
	B. gaultina	121.00
	R. bekumensis	123.97
	P. intermedia	125.00
	S. hammi	128.32
	V. blanda	129.97
	S. bilobata	131.52
	H. hechti, C. frankei, P. triplicata	136.32
	P. hannoverana	139.81
	S. praethroenensis, G. teres	141.05
	Macrodentina retirugata	146.58
	Galliaecytheridea polita	146.83
	Galliaecytheridea spinosa	147.65
	Macrodentina maculata	148.63
	Galliaecytheridea elongata	152.38
	M. (P.) proclivis 	153.93
	Galliaecytheridea dissimilis	157.25
	S. triebeli	160.48
	Nophrecythere cruciata oxfordiana	161.15
	Lophocythere interrupta	162.86
	Eudechacythere punctivata, Lophocythere scraba, L. cruciata	164.76
	Micropneumatocythere falcata	165.17
	Fossaterquemula blakeana	165.58
	Fastigatocythere juglandica	166.21
	Lophocythere propinqua, Praeschuleridea confossa	166.62
	L. ostreata	167.04
	M. postangusta	167.25
	Eoschulderidea batei, Progonocythere polonica	167.68
	Nophrecythere rimosa	168.07
	Glyptocythere scitula	170.24
	Glyptocythere polita	170.64
	Progonocythere carinata	171.25
	Progonocythere reticulata, Ektyphocythere triangula	171.64
	D. gallemanica	178.54
	E. vitilis, Otocythere callosa	180.70
	E. (Praeschuleridea) pseudokinkelinella	181.20
	K. gr. sermoisensis, Ektyphocythere intrepida	182.70
	Ektyphocythere intrepida, K. tenuicostata	183.03
	Wicherella semiora	187.12
	Gramannella apostolescui	188.01
	Ogmoconcha amalthei, K. multicostata, Gammacythere ubiquita	189.54
	Pleurifera harpa	191.14
	O. danica	194.02
	C. crassireticulata	195.22
	Cristacythere betzi	196.50
	Cytheretelloidea circumscripta	198.38
	Ektyphocythere moorei, Ogmoconchella aspinata	199.60
	A. kuhni	176.58
	Ogmoconcha moorei, O. bristolensis	200.95
	Ogmoconcha martini	201.62
	R. penshurtensis	202.29
	R. wicheri	203.84
	R. rueggeri	204.15
	R. gracilis	205.71
	K. germanica	224.18
	S. brotz. alpina	225.66
	L.(C.) rectagona	229.43
	S. alata levis	234.56
	T. fisheri, Triassellina ssp.	239.65
	G. subtilis	239.78
	S.(P.) petersbergensis	241.60

Tethyan Ostracodes	event		178/181/175
LAD
	O. plictatula, C. plannonica	5.53
	C. acuminata verrucosa	10.57
	N. helvetica	14.24
	C. tricostata	16.39
	S. delemontensis, P. pontonxensis	23.13
	H. oertlii, P. ventricosa, N. eoceanus	33.46
	L. striatopunctata, C. homoedwardsiana, P. moyesi	40.78
	H. praetexta	43.60
	D. volpensis	50.77
	C. infragilis, P. juncea, M. gr. canaliculata	56.67
	M. gr. canaliculata, C. infragilis, P. juncea	57.90
	L. astrei, M. gr. heiroglyphica	65.50
	I. marssoni, M. propinqua, K. petrocoriensis	70.60
	L. senonensis	81.63
	K. major, C. flexuosa	83.53
	M. cuvillieri	88.58
	L. grekoffi, S. ectypus, M. soriensis	89.78
	R. condemiensis	91.97
	V. ballonensis, P. taxyae, A. oertlii, D. strangulata	93.42
	N. gr. vanveeni	93.91
	C. aptensis, R. bartensteini, D. (P.) bosquetiana, C. rectangularis	99.57
	H. derooi	106.42
	P. bedoulensis	118.00
	P. inversa, S. bilobata, S. extranea, P. triplicata	128.30
	S. frankei, P. rodewaldensis	133.53
	K. humilis	136.49
	V. reicheli	137.69
	P. paquieri	140.08
	V. camberiensis	142.30
	P. revili	143.21
	M. decipiens	146.37
	M. (P.) ornata, M. (P.) steghausi	150.70
	Amphicythere confundens	153.23
	C. ovoidale	154.53
	C. index, Nophrecythere cruciata oxfordiana	158.38
	S.(Ektyphocythere) triebeli, L. cruciata	160.50
	NO PUBLISHED DATA IN Upper TOARCIAN to CALLOVIAN	161.63
	K. gr. sermoisensis	181.73
	O. ambo	182.85
	Gramannella apostolescui	183.84
	Gammacythere ubiquita	187.75
	Cytheretelloida circumscripta, K. praeluxuriosa	196.50
	C. buisensis	198.38
FAD
	S. contortus, A. woodwardi	0.61
	A. speyeri	1.39
	U. margaritifera	3.41
	C. carinata, C. simplex, A. convexa, A. emathlae	5.53
	C. acuminata acuminata	10.57
	A. (U.) oblonga, C. batei	16.39
	N. helvetica	21.12
	D. minor	23.13
	H. ornata	33.46
	L. pertusa, M. foveolata, U. striatopunctata	48.60
	P. ventricosa, E. gr. isabenaensis	53.58
	H. praetexta	57.02
	D. volpensis	59.90
	M. gr. canaliculata, P. juncea	65.50
	L. astrei	70.60
	K. petrocoriensis	81.63
	M. propinqua	83.53
	K. major	84.63
	M. gr. hieroglyphica	85.85
	I. marssoni, L. senonensis	89.07
	C. flexuosa, M. a. cuvilieri	89.78
	L. grekoffi, T. gr. geinitzi	93.42
	R. condemiensis	94.60
	P. taxyae, D. strangulata, V. ballonensis	95.78
	A. oertlii, M. soriensis, R. aquitanica	99.57
	C. aptensis	111.99
	S. jonesiana	118.00
	C. rectangularis	121.00
	H. derooi	121.90
	P. bedoulensis	126.37
	P. inversa	129.97
	S. bilobata	133.53
	S. extranea	133.85
	C. frankei, P. triplicata, P. rodewaldensis	136.86
	V. reicheli	139.10
	P. paquieri	140.66
	P. mazenoti	142.30
	K. humilis	144.19
	V. camberiensis, P. revili	144.53
	NO PUBLISHED DATA IN TITHONIAN	145.87
	M. retirugata, M. decipiens	150.84
	Cytherelloidea weberi, M.(P.) steghausi	154.14
	M?. pulchra	154.53
	Amphicythere confundens	156.45
	C. ovoidale	158.38
	C. index	161.13
	NO PUBLISHED DATA IN Upper TOARCIAN to CALLOVIAN	181.23
	K. gr. sermoisensis	182.70
	Gramannella apostolescui	186.95
	Gammacythere ubiquita	189.54
	K. praeluxuriosa	197.24
	Cytheretelloida circumscripta, Ogmoconchella aspinata	199.60


French Ostracode zone (Jur)	block	120	178/181/175
	TOP	148.66
	Protocythere bireticulata	150.84
	Fabanella prima, Macrodentina annulata, Metacytheropreton elegans	151.98
	Acanthocythere undata, Amphicythere semisulcata, Retocythere regularis	154.97
	Marcodentina intercostulata, Rectocythere iuglandiformis	155.65
	Macrodentina (P.) pulchra pulchra, Galliacytheridea postrotunda	156.89
	Schuleridea minuta	158.55
	Progonocythere multipunctata	160.66
	Terquemula oertlii	161.21
	Lophocythere scabra, Lophocythere interrupta interrupta	163.20
	Lophocythere cruciata franconica	164.23
	Nodophtalmocythere bicostata, Micropneumatocythere escovillensis	164.74
	Schuleridea trigonalis	166.11
	Kliena levis, Fabanella bathonica	167.68
	Pleurocythere regularis, Pleurocythere richteri	168.86
	Fuhrbergiella gigantea	170.62
	Ektyphocythere triangula, Praeschuleridea decorata	171.60
	Camptocythere media	174.27
	Camptocythere modesta	174.71
	Aphelocythere undulata, Praeschuleridea ventriosa, Camptocythere praecox, Aphelocythere kuhni	176.58
	TOP	177.07
	Praeschuleridea bernierensis	180.50
	Enktyphocythere bucki, Enktyphocythere rugosa	182.70
	Enktyphocythere cf. arcuatocostata, Kinkelinella tenuicostati	183.00
	Ogmoconcha gr. Amalthei	189.60
	Ogmoconcha hagenovi	196.50
	Ogmoconchella ellipsoidae	199.60

French subzone	block	120	178/181/175	notitle
	TOP	149.37
	Macrodentina rugulata	150.84
	TOP	155.65
	Macrodentina (M.) tenuistriata, Vernoniella sequana	156.89
	TOP	161.21
	Monoceratina calloevica	162.52
	TOP	164.74
	Terquemula blakeana, Micropneumatocythere falcata	165.52
	TOP	166.11
	Micropneumatocythere quasicitrella	167.29
	Nophrecythere bessinensis, Kinkelinella malzi, Pseudoprotocythere? bessinensis	167.68
	TOP	169.64
	Fuhrbergiella horrida	170.42
	TOP	170.62
	Pneumatocythere carinata	171.21
	Cytheropterina comica, Progonocythere reticulata	171.60
	Camptocythere pusilla	172.49
	TOP	173.16
	Camptocythere obtusa	173.38
	TOP	183.00
	Cytherelloidea anningi, Gramanella apostolescui	186.95
	Pleurifera? vermiculata, Gammacythere ubiquita, Trachycythere horrida	188.41
	Pleurifera harpa	189.60
	Pleurifera plicata	191.22
	Klingerella lotharingiae, Klingerella laneuvevillae, Klingerella? undata	193.25
	Lophodentina lacunosa	195.28
	Klingerella luxuriosa	196.50
	Klingerella praeluxuriosa	197.28
	Bairdiacypris? sartriensis, Kingerella translucens, Ptychobairdia? hettangica	198.44
	Cytherelloidea buisensis	199.60

French datum	event		178/181/175
LAD
	Protocythere bireticulata	148.66
	Macrodentina rugulata	149.37
	Fabanella prima, Macrodentina annulata, Metacytheropreton elegans	150.84
	Acanthocythere undata,  Amphicythere semisulcata, Retocythere regularis	151.98
	Marcodentina intercostulata, Rectocythere iuglandiformis	154.97
	Macrodentina (M.) tenuistriata, Vernoniella sequana, Macrodentina (P.) pulchra pulchra, Galliacytheridea postrotunda	155.65
	Schuleridea minuta	156.89
	Progonocythere multipunctata	158.09
	Terquemula oertlii	159.61
	Lophocythere scabra, Lophocythere interrupta interrupta, Monoceratina calloevica	161.21
	Lophocythere cruciata franconica	163.03
	Nodophtalmocythere bicostata, Micropneumatocythere escovillensis	164.23
	Schuleridea trigonalis, Terquemula blakeana, Micropneumatocythere falcata	164.74
	Kliena levis, Fabanella bathonica	165.52
	Micropneumatocythere quasicitrella	166.11
	Kinkelinella malzi, Pseudoprotocythere? bessinensis	166.99
	Nophrecythere bessinensis	167.29
	Fuhrbergiella gigantea, Pleurocythere regularis, Pleurocythere richteri	167.68
	Fuhrbergiella horrida, Glyptocythere scitula	169.70
	Glyptocythere polita	170.23
	Ektyphocythere triangula, Praeschuleridea decorata, Pneumatocythere carinata	170.62
	Camptocythere media, Cytheropterina comica, Progonocythere reticulata	171.21
	Camptocythere pusilla	171.34
	Camptocythere obtusa	173.16
	Camptocythere modesta	174.27
	Aphelocythere undulata, Praeschuleridea ventriosa, Camptocythere praecox, Aphelocythere kuhni	174.71
	Praeschuleridea bernierensis (rare)	176.09
	Praeschuleridea bernierensis	176.58
	Enktyphocythere bucki, Enktyphocythere rugosa	179.52
	Enktyphocythere cf. arcuatocostata, Kinkelinella tenuicostati	182.70
	Ogmoconcha gr.aAmalthei, Gramanella apostolescui	183.00
	Cytherelloidea anningi	183.12
	Trachycythere tubulosa, Trachycythere serratina	184.20
	Gammacythere ubiquita, Trachycythere horrida	185.58
	Pleurifera? vermiculata	186.68
	Pleurifera harpa	188.34
	Pleurifera plicata	189.30
	Ogmoconcha hagenovi (rare)	189.60
	Ogmoconcha hagenovi	190.01
	Klingerella lotharingiae, Klingerella laneuvevillae, Klingerella ? undata	191.22
	Lyubimovella? frequences, Lophocythere normaniae	191.95
	Lophodentina pumicosa	192.04
	Klingerella luxuriosa	194.67
	Lophodentina convergens	194.88
	Bairdia carinata	195.59
	Ptychobairdia? hettangica, Klingerella praeluxuriosa	196.50
	Bairdiacypris? sartriensis, Kingerella translucens	196.69
	Cytherelloidea buisensis	198.44
FAD
	Protocythere bireticulata, Macrodentina rugulata	150.84
	Fabanella prima, Macrodentina annulata, Metacytheropreton elegans	151.98
	Acanthocythere undata,  Amphicythere semisulcata, Retocythere regularis	154.97
	Marcodentina intercostulata, Rectocythere iuglandiformis	155.65
	Macrodentina (M.) tenuistriata, Vernoniella sequana, Macrodentina (P.) pulchra pulchra, Galliacytheridea postrotunda	156.81
	Schuleridea minuta	158.55
	Progonocythere multipunctata	160.66
	Terquemula oertlii	161.21
	Monoceratina calloevica	162.52
	Lophocythere scabra, Lophocythere interrupta interrupta	163.20
	Lophocythere cruciata franconica	164.12
	Nodophtalmocythere bicostata, Micropneumatocythere escovillensis	164.74
	Terquemula blakeana, Micropneumatocythere falcata	165.52
	Schuleridea trigonalis	166.11
	Micropneumatocythere quasicitrella	166.89
	Kliena levis, Fabanella bathonica, Kinkelinella malzi, Pseudoprotocythere? bessinensis	167.68
	Nophrecythere bessinensis	167.97
	Pleurocythere regularis, Pleurocythere richteri	168.86
	Glyptocythere scitula	170.23
	Fuhrbergiella horrida, Glyptocythere polita	170.42
	Fuhrbergiella gigantea	170.62
	Pneumatocythere carinata	171.34
	Ektyphocythere triangula, Praeschuleridea decorata, Cytheropterina comica, Progonocythere reticulata	171.60
	Camptocythere pusilla	172.58
	Camptocythere obtusa	173.38
	Camptocythere media	174.27
	Camptocythere modesta	174.71
	Praeschuleridea ventriosa, Camptocythere praecox, Aphelocythere kuhni	176.83
	Aphelocythere undulata	177.07
	Praeschuleridea bernierensis	180.30
	Enktyphocythere bucki, Enktyphocythere rugosa	182.70
	Enktyphocythere cf. arcuatocostata, Kinkelinella tenuicostati	183.00
	Cytherelloidea anningi, Gramanella apostolescui, Trachycythere serratina	186.95
	Trachycythere tubulosa	187.75
	Trachycythere horrida	188.34
	Pleurifera harpa, Pleurifera? vermiculata, Gammacythere ubiquita	189.60
	Ogmoconcha gr. amalthei	190.68
	Pleurifera plicata	191.22
	Klingerella lotharingiae, Klingerella laneuvevillae, Klingerella? undata, Lyubimovella? frequences, Lophocythere normaniae	193.25
	Lophodentina pumicosa	194.37
	Lophodentina lacunosa	195.28
	Lophodentina convergens	195.59
	Klingerella luxuriosa, Bairdia carinata	196.50
	Klingerella praeluxuriosa, Ogmoconcha hagenovi	197.28
	Ptychobairdia? hettangica	199.02
	Ogmoconchella ellipsoidae, Cytherelloidea buisensis, Bairdiacypris? sartriensis, Kingerella translucens	199.60




Ostracodes (Paleozoic)	:	Ostracode Zone (Silurian)	Ostracode subzone (Silurian)	_METACOLUMN_OFF		GTS2004 diagrams (Melchin et al., 2004)

Ostracode Zone (Silurian)	block	120	178/181/175	notitle
	TOP	359.20
	hemisphaerica/latior I.	360.73
	hemisphaerica/dichotoma	365.32
	intercostata	367.62
	serratostriata - nehdensis	372.21
	sigmoidale	374.50
	splendes/reichi schmidt /volki /materni /barrandei	378.28
	cicatricosa/barrandei I.	379.36
	cicatricosa	380.44
	cicatricosa/torleyi I.	383.14
	torleyi	387.90

Ostracode subzone (Silurian)	block	50	178/181/175	notitle
	TOP	360.73
	2	363.79
	1	365.32
	2	369.91
	1	372.21


Charophytes	:	Charophyte Zone	Charophyte LAD/FAD	_METACOLUMN_OFF		J. Riveline (in Hardenbol et al., SEPM charts, 1998),

Charophyte Zone	block	100	195/221/131	notitle
	TOP	0.00
	Nitellopsis (Tectochara) etrusca	13.78
	Nitellopsis (Tectochara) ginisburgi	21.12
	Stephanochara berdotensis	21.95
	Rantzieniella nitida	23.58
	Chara notata	26.05
	Stephanochara ungeri	28.01
	Chara microcera	29.32
	Rhabdochara major	32.46
	Stephanochara pinguis	33.91
	Stephanochara vectensis	34.93
	Harrisichara vasiformis tuberculata	35.95
	Gyrogona tuberosa	36.51
	Psilochara repanda	36.92
	Raskyella vadaszi	37.75
	Chara friteli	39.03
	Raskyella pecki	41.20
	Maedleriella embergeri	48.24
	Nitellopsis (Tectochara) thaleri	52.48
	Peckichara piveteaui	53.08
	Peckichara disermas	56.67
	Sphaerochara edda	57.02
	Dughiella bacillaris	64.23
	Peckichara llobregatensis	65.00
	Peckichara sertulata	66.00
	Peckichara sp. 1	67.32
	Microchara cristata	68.41
	Septorella ultima	70.95
	Peckichara cancellata	73.36
	Peckichara pectinata	79.68
	Peckichara baylensis	83.53
	Amblyochara media	83.76
	Microchara olmesensis	86.02
	Atopochara trivolvis multivoltis	96.01
	Atopochara trivolvis restricta	106.42
	Clypeator grovesii lusitanicus	121.00
	Axcidiella cruciata	126.65
	Atopochara trivolvis triquetra	130.07
	Globator maillardii steinhauseri	141.25
	Globator maillardii nurrensis	142.30
	Globator maillardii incrassatus	142.96
	Globator maillardii maillardii	145.80
	Dictyoclavator fieri ramalhoi	154.53
	Echinochara peckii	157.55
	TOP	202.29	dotted
	Auerbachichara rhaetica	216.53	dotted
	Stellatochara thuringia	230.27	dotted
	Stellatochara hoellvicensis	241.00	dotted
	Stellatochara dnjeproviformis	245.17	dotted
	Porochara triassica	248.92	dotted
	Porochara / Vladimiriella globosa ?	251.00

Charophyte LAD/FAD	event		203/221/158
LAD
	Nitellopsis (Tectochara) ginsburgi	6.58
	Harrisichara turberculata	32.46
	Gyrogona tuberosa	35.95
	Raskyella vadaszi	36.92
	Raskyella pecki	39.03
	Dughiella bacillaris	57.02
	Septorella ultima, P. sertulata	68.41
	Peckichara cancellata	70.95
	Amblyochara media	75.59
	Globator spp.	121.90
	H. neimongolensis	128.30
	Dictyoclavator spp.	141.55
FAD
	Nitellopsis (Tectochara) etrusca	13.78
	Nitellopsis (Tectochara) ginisburgi	21.12
	Stephanochara berdotensis	21.95
	Rantzieniella nitida	23.58
	Chara notata	26.05
	Stephanochara ungeri	28.01
	Chara microcera	29.32
	Stephanochara pinguis	33.91
	Harrisichara turberculata	34.93
	Gyrogona tuberosa	36.51
	Raskyella vadaszi	37.75
	Raskyella pecki	41.20
	Maedleriella embergeri	48.24
	Nitellopsis (Tectochara) thaleri	52.48
	Peckichara piveteaui	53.08
	Peckichara disermas	56.67
	Dughiella bacillaris	64.23
	Peckichara llobregatensis	65.00
	Peckichara sertulata	66.00
	Peckichara sp. 1	67.32
	Septorella ultima	70.95
	Peckichara cancellata	73.36
	Peckichara pectinata	79.68
	Peckichara beylensis	83.53
	Amblyochara media	83.76
	Microchara olmesensis	86.02
	M. fusiformis	89.07
	Atopochara trivolvis multivoltis	96.01
	Atopochara trivolvis brevicellis	100.94
	Atopochara trivolvis restricta	106.42
	Clypeator grovesii lusitanicus, Atopochara trivolvis trivolvis	121.00
	Embergerella cruciata, P. paucibracteatus	126.65
	A. triquetra, T. calcitrapa, G. m. trochiliscoides, A. trivolvis triqueta	130.07
	Cl. grovesii gautieri, P. adnatus, H. neimongolensis	138.87
	F. harrisii, E. stellata	140.18
	Globator maillardii steinhauseri	141.25
	Globator maillardii nurrensis	142.30
	D. fieri neocomiensis	142.63
	Globator maillardii incrassatus	142.96
	Atopochara trivolvis horrida, Globator maillardii praecursor, Clypeator grovesii discordis	145.46
	Globator maillardi maillardi	145.80
	Globator maillardi rectispirali	146.68
	P. subcylindrata	150.75
	Dictyoclavator fieri ramalhoi	154.53
	Echinochara peckii	157.55
	Porochara palmeri	166.84
	P. sublaevis	167.48
	Latochara durand-delgai	197.74

Calcareous Algae (E.Cret.)	:	W Europe horizons	Periadriatic horizons	_METACOLUMN_OFF		J.-P. Masse (in Hardenbol et al., SEPM charts, 1998),

W Europe horizons	event		201/213/80
LAD
	S.hasi	103.00
	M. elitzae	111.99
	A. fouryae, C. lyrata, T. marsicana, S. melitae, S. polyreme, P. fragilis, C. nigra, S. muehlbergi	121.00
	H. cylindrica	121.00
	H. urladana si, A. hispanica	121.90
	L.? danilovae	125.00
	S. genevensis, H.? paucicalcarea	128.30
	D. hauteriviana	128.71
	M. verae	133.21
	P. jurassica, S. annulata, S. johnsoni, C. marteli, R. piailensis, C. solkani	138.94
	M.? praturloni	139.56
	T.? neocomensis	139.77
	F. campanensis	140.02
	Z. embergeri	140.18
	O.? lemmensis	142.63
	C. jurassica	142.96
FAD
	H. lepina, D. undulata, T. tripolitanus	107.89
	S. hasi	116.50
	C. nigra, T. marsicana, C. lyrata	125.00
	H. cylindrica	125.00
	A. hispanica, H. urladanisi	127.20
	S. polyreme, S. muehlbergi	131.91
	S. genevensi, S. melitae, A. pouryae, L.? danilovae, P. fragilis, H.? paucicalcarea	132.56
	M. elitzae	133.85
	M. verae, D. hauteriviana	136.75
	Z. embergeri	142.15

Periadriatic horizons	event		201/213/80
LAD
	H. dinarica	119.05
	S.? somalica, S. melitae, C. lyrata, T. margicana, C. velici	121.45
	S. biokovensis	123.97
	H. catenaeformis	127.75
	S. melitae	130.26
	S. annulata, C. solkani	134.50
	T.? neocomiensis 	140.77
	C. jurassica	142.96
FAD
	C. somalica, C. lyrata, T. marsicana, C. velici	125.00
	H. urladanasi	127.20
	L.? danilovae, S. biokovensis	132.75
	H. catenaeformis	134.50
	H. dinarica	139.56
	C.solkani, T.? neocomiensis, S. annulata	145.27


Spores/ Pollen (Tri)	:	Spores/ Pollen (Alpine/Germanic)	Spores/ Pollen (Arctic)	_METACOLUMN_OFF		P.A. Hochuli (in Hardenbol et al., SEPM charts, 1998),

Spores/ Pollen (Alpine/Germanic)	event		194/216/99
FAD
	C. rhaeticus, Limbosporites lundbladii	202.29
	Q. anelliformis, Rhaetipollis germanicus	203.64
	Perinopollenites elatoides, M. fuscus, K. (Heliosporites) reissingeri	211.30
	G.(Corollina) zwolinska, Chasmatosporites spp., G. rudis (common)	216.59
	Corollina spp.	218.66
	R. tuberculatus	220.95
	T. verrucata	225.66
	G. (Corollina) meyeriana, Partitisporites quadruplices	225.66
	Patinasporites densus, Camarozonosporites rudis, V. ignacii	228.01
	Enzonalosporites vigens, Partitisporites spp.(common), Duplicisporites spp. (common)	229.97
	W. magnus	230.42
	Infernopollenites spp.	231.68
	Echinitosporites iliacoides, Ovalipollis pseudoalatus (common), C. insignis, T. verrucata	234.56
	Duplicisporites granulatus	236.76
	Camerosporites secatus	238.75
	Partitisporites spp., Ovalipollis pseuodoalatus, Staurosaccites quadrifidus	240.33
	Kuglerina meieri	240.33
	Aratisporites saturni, P. longdonensis	243.38
	Dyupetalum vicentinensis, C. nevesi	243.68
	I. chitonoides	244.27
	(Triadispora crassa, T. suspects, T. plicata) Angustisulcites spp., Stellapollenites thiergartii	245.17
	Triadispora crassa	245.53
	C. gunyalensis, J. conmilvinus, D. insolitus	247.72
LAD
	Limbosporites lundbladii, C. rhaeticus, R. tuberculatus, Ovalipollis pseudoalatus, Rhaetipollis germanicus	199.60
	G. rudis	200.95
	Enzonalosporites vigens, V. ignacii, Patinasporites densus	202.29
	Duplicisporites granulatus, Camerosporites secatus, T. verrucata	216.59
	Infernopollenites spp.	218.66
	Partitisporites novimundanus, Aulisporites astigmosus, Lagenella martinii, Praecirculina granifer, Staurosaccites quadrifidus	222.70
	Infernopollenites spp.	224.63
	Kuglerina meieri, A. klausii	225.66
	I. chitonoides, Echinitosporites iliacoides	228.01
	C. insignis, W. magnus	229.43
	C. nevesi	231.68
	Dyupetalum vicentinensis	239.35
	Stellapollenites thiergartii	240.00
	C. cristatus, I. kosankei, Microachrydites fastidioides, V. jenensis, K. apiculatus	241.60
	Triadispora (acme), (T.crassa, T. suspecta, T. plicata)	242.19
	Densosporites nejburgii, C. gunyalensis, J. conmilvinus, D. insolitus	243.68
	Alisporites cymbatus	244.72
	Densosporites nejburgii (common), D. (Triplexisporites) playfordii	245.17
	Cycloverrutriletes presselensis, L. brevicula, L. obsoleta	246.76
	C. chalasta	250.50

Spores/ Pollen (Arctic)	event		194/216/99
FAD
	Rhaetipollis germanicus, Perinopollenites elatoides	207.57
	Limbosporites lundbladii, R. tuberculatus	211.75
	Q. anelliformi, Kyrtomisporis spp. (common), Chasmatosporites spp.(common)	216.53
	Corollina spp.	217.59
	M. fuscus	219.81
	V. ignacii	228.01
	A. laevigatus	229.43
	T. (Patinasporites) toralis	230.76
	S. worsleyi	231.68
	Echinitosporites iliacoides	234.56
	Ovalipollis pseudoalatus, T. verrucata	238.00
	Partitisporites spp.	239.00
	Prodiploxipinus spp. (ornamented), Chasmatosporites spp.	239.65
	I. chitonoides	242.64
	C. gunyalensis, A. macrocavatus, Tridiaspora plicata	243.05
	S. (Cornutisporites) seebergensis, I. chitonoides, A. circumdatus	245.14
	A. spiniger	245.48
	J. punctispinosa	246.63
	A. robustus	247.72
	Lundbladispora spp. (common)	250.16
	U. imperialis, P. pococki	250.71
LAD
	Limbosporites lundbladii, R. tuberculatus, A. laevigatus                  	199.60
	G. rudis	200.95
	P. ornatus	202.29
	V. ignacii	203.64
	V. ignacii (common), G. rudis (common)	205.71
	Aulisporites astigmosus, F. laevigata	208.29
	P. mosellanum (common)	210.01
	Kyrtomisporis spp. (common), P.(Cerebrupollenites) macroverrucosus	211.30
	C. obvius	213.11
	T. verrucata, T. (Patinasporites) toralis, S. worsleyi	216.53
	I. rieberi, I. chitonoides	217.59
	Staurosaccites quadrifidius	219.81
	Echinitosporites iliacoides	228.01
	C. gunyalensis	231.68
	K. apiculatus	238.00
	J. punctispinosa, K. punctatus	239.65
	Densosporites nejburgii	244.01
	Densoisporites spp. (common), A. robustus, P. reticulatus, V. jenensis	245.14
	Kraeuseli saeptatus, L. variabilis, P. disertus, P. fungosus, N. striatus (common)	248.08
	Lundbladispora spp. (common), Pechorosporites spp. (common)	249.76
	S. richteri, P. pococki	250.16
	C. chalasta (common)	250.49


Flora (Paleozoic)	:	Flora Macro Zone (Carboniferous)	Flora Micro Zone (Carboniferous)	Spore Zone (Silurian)	Spore Datum (Devon.)	_METACOLUMN_OFF

Flora Macro Zone (Carboniferous)	block	60	194/216/99	notitle		GTS2004 diagrams (Davydov et al., 2004)
	TOP	299.00
	C-Pp1	301.45
	Pp10	302.92
	Pp9	303.90
	Pp8	305.72
	Pp7	307.28
	Pp6	308.06
	Pp5	309.10
	Pp4	311.70
	Pp3	312.66
	Pp2	313.94
	Pp1	318.10
	Mp5	319.76
	Mp4	324.33
	Mp3	330.18
	Mp2	349.47
	Mp1	359.20	dashed

Flora Micro Zone (Carboniferous)	block	60	194/216/99	notitle		GTS2004 diagrams (Davydov et al., 2004)
	TOP	294.60
	DS	299.00
	VC	301.45
	NBM	302.92
	ST	305.72
	OT	309.36
	SL	310.92
	NJ	312.66
	RA SS	313.94
	FR	314.58
	KV	316.18
	SO	321.01
	TK	324.33
	NC	327.35
	VF	330.18
	NM	331.13
	TC	335.85
	TS	340.58
	PU	346.69
	CM	348.08
	?	348.78
	PC	350.86
	BP	352.25
	HD	355.03
	VI	359.20

Spore Zone (Silurian)	block	150	194/216/99			GTS2004 diagrams (Melchin et al., 2004)
	TOP	416.00
	Synorisporites tripapillatus-Apiculiretusispora spicula	418.70
	Lophozonotriletes? poecilomorphus -Synorisporites libycus	420.91
	Sclya. downiei - Concen. sagittarius	422.90
	Artemopyra brevicostata- Hispanaediscus verrucatus	425.54
	Archaeozonotriletes chulus nanus - Archaeozonotriletes chulus chulus	431.36
	Ambitisporites avitus - Ambitisporites dilatus	436.25
	Pseudodyadospora sp. B - Segestrespora membranifera	443.70

Spore Datum (Devon.)	event		194/216/99
LAD
	Retispora lepidophyta	359.97



Vertebrates (Perm-Silur)	:	Vertebrate Zone	Vertebrate datum	_METACOLUMN_OFF		GTS2004 diagrams

Vertebrate Zone	block	150	246/187/102	notitle
	TOP	251.00
	endothiodontid/dicynodontid empire	263.10	dotted
	tapinocephalid empire	275.10	dotted
	edaphosaurid empire	299.00	dotted
	C-Pt1	301.45	dashed
	Pt 2	307.28	dashed
	Pt 1	313.94	dashed
	Mt 2	335.85	dashed
	Romer's Gap	355.03	dashed
	D - Mt1	361.20	dashed
	TOP	363.09	dashed
	Bothriolepis ciecere	366.09	dashed
	Bothriolepis ornata	367.62	dotted
	Phyllolepis	371.44	dashed
	Bothriolepis leptocheira	372.97	dashed
	(un-named)	376.66	dashed
	Bothriolepis maxima	378.82	dashed
	Bothriolepis trautscholdti	382.06	dashed
	Bothriolepis cellulosa	384.22	dashed
	Devononchus concinnus	388.23	dashed
	Diplacanthus gravis	391.80	dashed
	Coccosteus cuspidatus	394.08	dashed
	Pt. rimosum/ Ch. estonicustus	396.08	dashed
	Laliacanthus singularis	398.93	dashed
	(un-named)	403.68	dashed
	Gomphonchus tauragensis	407.00	dashed
	Lietuvacanthus fossulatis	413.60	dashed
	Nostolepis minima	416.00	dashed
	Katoporus timanicus lithuanicus, Poracanthodes punctatus	417.22	dashed
	Nostolepis gracilis	418.03	dashed
	Thelodus sculptilis	419.48	dashed
	Andreolepis hedei	420.78	dashed
	Phlebolepis elegans	421.94	dashed
	Phlebolepis ornata	422.42	dashed
	Paralogana martinssoni	425.05	dashed
	Loganellia grossi	426.80	dashed
	Loganellia avonia	428.60	dashed
	Loganellia sibirica /Loganellia scotica	438.86	dashed
	Valyalaspis crista	443.00	dashed
	(not zoned)	443.70



Vertebrate datum	event		246/187/102
FAD
	Eryops	301.45
	Edaphosauridae	307.28
	Nectridae	313.94
	Anthracosauria	335.85




North American Mammals	:	NALMA	NALMA Subzones	N.Amer. zonal and selected markers	Other N.Amer. Plio-Pleist events	All N.Amer. Mammal Datums Combined	_METACOLUMN_OFF		Woodburne (2004); and J. Hooker (GTS2004 diagrams)

NALMA	block	60	242/187/102
	TOP	0
	Rancholabrean	0.19
	Irvingtonian	1.80
	Blancan	4.91
	Hemphilian	9.07
	Clarendonian	12.53
	Barstovian	15.97
	Hemingfordian	18.50
	Arikareean (Geringian)	30.04
	Whitneyan	32.08
	Orellan	33.88
	Chadronian	37.24
	Duchesnean	39.21
	Uintan	46.20
	Bridgerian	52.24
	Wasatchian	55.73
	Clarkforkian	56.79
	Tiffanian	61.72
	Torrejonian	64.28
	Puercan	65.50
	Lancian	70.74
	"Edmontonian"	80.86
	Judithian	82.17
	Aquilan	85.17

NALMA Subzones	block	40	242/187/102	notitle
	TOP	0.19
	Ir 3	0.39
	Ir 2	0.89
	Ir 1	1.95
	Bl 5	2.60
	Bl 4	3.10
	Bl 3	4.10
	Bl 2	4.61
	Bl 1	4.91
	Hh 4	5.91
	Hh 3	6.88
	Hh 2	7.59
	Hh 1	9.07
	Cl 3	10.09
	Cl 2	12.06
	Cl 1	12.53
	Ba 2	14.78
	Ba 1	15.97
	He 2	17.34
	He 1	18.50
	Ar 4	19.09
	Ar 3	22.20
	Ar 2	27.86
	Ar 1	30.04
	TOP	33.88
	Ch 3	34.94
	Ch 2	35.85
	Ch 1	37.24
	Du 2	38.27
	Du 1	39.21
	late	42.18
	early	46.20
	late	46.95
	middle	50.21
	early	52.24
	Wa7	52.82
	Wa6	53.23
	Wa5	53.89
	Wa4	54.38
	Wa3 (Greybullian)	54.81
	Wa2	55.24
	Wa1	55.46
	Wa0	55.73
	Cf3	56.15
	Cf2	56.61
	Cf1	56.79
	Ti5	57.72
	Ti4	58.08
	Ti3	59.10
	Ti2	60.63
	Ti1	61.72
	To3	61.98
	To2	63.10
	To1	64.28
	Pu2/3	65.27
	Pu1	65.50

N.Amer. zonal and selected markers	event		242/203/144
FAD
	Platygonus compressus	0.08
	Bison	0.19
	Ondatara zibethicus	0.31
	Smilodon populator	0.78
	Microtus meadensis,  Lemmiscus curtatus	0.89
	Euceratherium	1.12
	Mammuthus	1.36
	Megalonyx wheateyi	1.57
	Phenacomys	1.72
	Platygonus vetus	1.95
	Glossotherium chapadmalense, Mictomys vetus	2.58
	Miracinonyx inexpectatus	3.03
	Pliolemmus	3.21
	Procastoroides	3.50
	Borophagus diversidens, Megalonyx leptostomus, Glyptotherium	3.60
	Pliopotamys	4.04
	Ogmodontomys poaphagus	4.68
	Ursus	4.80
	Nanippus peninsulatus, Ogmodontomys sawrockensis	4.90
	Eocioleus; carnivores (Lutra, Megantereon, Mustela, Sminthosinus, Trigonictis); arvicolines (Ogmodontomys, Protopliophenacomys) and Miopetaurista (flying squirrel) in Hh 4	5.91
	Agriotherium (carnivore), Castor (beaver), Felis (carnivore), Megalonyx (definition of the subdivision, a edentate), Ochotona (pika), Plesiogulo (carnivore), Pliozapus (zapodid), Prosomys (murid) in Hh 3	6.88
	carnivores (Enhydritherium, Eomellivora, Indarctos, Lutravus, Machairodus, Simocyon); Neotragoceras (bovid ungulate), Thinobadistes (definition of subdivision, a edentate) in Hh 2	7.59
	Crusafontina (soricid), Kansasimys (eomyid), Lemoynea (desmanine mole), Pliometanastes (definition of subdivison, a edentates), Paramicrotoscoptes (murid), Pliotomodon (murid) in Hh 1	9.07
	Actiocyon, Hoplictis, Platybelodon in Cl 3	10.09
	Barbourofelis is age marker of Cl 2 subzone.  Cormohipparion (hipparionines equine horses) in Cl 2	12.06
	Pseudoceras; plains taxa invade Great Basin	12.53
	Gomphotherium, Hesperolagomys, Lanthanotherium, Megasminthus, Pliogale, Pseudocyon, Russellagus, Untermannerix in Ba 2	14.78
	Plithocyon (hemicyonione bear), Zygolophodon (Proboscidean Datum)	15.97
	aceratherine rhinos (Aphelops, Peraceras), teloceratine rhino (Teleoceras); Copemys (cricetid), mustelids (Dinogale, Mionictis, Plionictis, Sthenictis); Eomys (an eomyid), Petauristodon (sciurid), Pseudaelurus (true felid) in He 2	17.34
	Ursavus (ursid); Aletomeryx (aletomerycine artiodactyl), Amphictis (procyonid), Amphicyon (amphicyonid), Antesorex (soricid), Brachypotherium (teleoceratine rhino), Floridaceras (aceratherine rhino), Caterogale, Desmatolagus and Oreolagus (rabbits), Edaphocyon (procyonid), Euroxenomys (casterine beaver),  Phoberocyon (hemicyonine), Plesiosorex (plesiosoricid), and mustelids (Leptarctus, Miomustela, Potamotherium) in He 1	18.50
	Barbouromeryx (cranioceratine dromomeryid), Cynelos (amphicyonine amphicyonid), Paracosoryx (merycodontine antilocaprid), Prablastomeryx in Ar 4	19.09
	Cephalogale, Menoceras (a rhino), Moropus, Ysengrinia (amphicyonine amphicyonid), Zodiolestes (a paleomustelid) in Ar 3	22.20
	Menoceras	23.31
	Entoptychus	24.74
	Parvericius, Caninae	27.33
	Meniscomys	28.52
	Palaeocastor, Erinaceidae, Talpinae, Kalobatippus, Dinohyus	30.04
	Diceratherium, Protoceras	32.08
	Hypertragulus calcaratus, Suoidea	33.88
	Cricetidae, Mustelidae	34.94
	Merycoidodon, Nimravidae	35.85
	Entelodontidae, Ursidae, Bothriodon, Poebrotherium	37.24
	Ischyromys	38.27
	Anthracotheriidae, Canidae, Amphicyonidae, Mesohippus, Rhinocerotidae	39.21
	Lagomorpha, Soricidae, Ruminantia	42.18
	Eobasileus cornutus, Hyracodontidae, Camelidae, Merycoidodontoidea	46.20
	Hyrachyus eximius	46.95
	Uintatherium anceps	50.21
	Omomys, Palaeosyops	52.24
	Brontotheriidae, Hyrachyidae, 	52.82
	Heptodon	53.23
	Chiroptera, Orohippus	53.89
	Oxyaena gulo	55.24
	Dipsalidictis transiens	55.46
	Primates, Artiodactyla, Perissodactyla	55.73
	Coryphodon, Rodentia	56.79
	Plesiadapis simonsi	57.72
	Plesiadapis churchilli	58.08
	Dinocerata, Oxyaenidae, Plesiadapis rex	59.10
	Plesiadapis anceps	60.63
	Plesiadapis, Phenacodus	61.72
	Pantolestidae, Nyctitheriidae	61.98
	Pantolambda, Deltatherium, Mixodectes	63.10
	Paromomys, Tetraclaenodon	64.28
	Purgatorius, Periptychus	65.27
	Catopsalis, Protungulatum	65.50
LAD
	Mictrotus meadensis, Microtus paroperarius	0.23
	Mictomys kansasensis/mel, Ondatra annectens, Meglonyx weatleyi	0.58
	Miracinonyx inexpectatus	0.78
	Stegomastodon	1.19
	Hypolagus, Ophiomys, Mictomys vetus	1.66
	Prodipodomys	1.95
	Procasteroides	2.15
	Dipoides rexroadensis, Ogmodontomys poaphagus, Pliopotamys, Pliolemmus	2.58
	Borophagus hilli, Platygonus pearcei	3.33
	Megantereon	3.60
	Ogmodontomys sawrockensis	4.63
	Nimravinae	23.03
	Poebrotherium	27.33
	Meniscomys	25.05
	Hyracodontidae	28.52
	Merycoidodon	30.10
	Pantolestidae, Ischyromys, Hypertragulus calcaratus, Bothriodon, Mesohippus	32.19
	Brontotheriidae	33.74
	Oromerycidae, Cylindrodontidae	33.88
	Multituberculata, Apatotheria	35.40
	Hyopsodus	35.85
	Plesiadapiformes, Nyctitheriidae	37.24
	Dinocerata, Omomys, Taeniodonta, Hyrachyidae	39.21
	Oxyaenidae, Hyrachyus eximius, Eobasileus cornutus	42.18
	Tillodontia, Orohippus, Phenacodus, Palaeosyops, Uintatherium anceps	46.20
	Heptodon, Coryphodon	50.21
	Eucosmodontidae	53.89
	Oxyaena gulo	54.38
	Dipsalidictis transiens	54.81
	Arfia junnei	55.46
	Arctostylopida, Plesiadapis	55.73
	Plesiadapis gingerichi	56.61
	Plesiadapis churchilli, Periptychus	57.72
	Plesiadapis rex	58.08
	Plesiadapis anceps	59.10
	Pantolambda, Catopsalis, Paromomys	60.63
	Tetraclaenodon, Mixodectes	61.72
	Deltatherium	61.98
	Protungulatum, Purgatorius	64.28

Other N.Amer. Plio-Pleist events	event		242/203/144
FAD
	Megalonyx jeffersonii	0.16
	Clethrionomys	0.84
	Microtus paroperarius	0.86
	Ondatra annectens, Microtus sp. (5T)	1.19
	Synaptomys	1.33
	Paramylodon harlani	1.75
	Lepus	1.91
	Northrotheriops, Mictomys kansasensis/mel, Allophaiomys pliocaenicus	1.97
	Onadatra idahoensis, Smilodon gracilis	2.44
	Sylvilagus	3.12
	Stegomastodon, Platygonus bicalcaratus	3.53
	Ophiomys, Platygonus pearcei, Dipoides rexroadensis	4.72
LAD
	Smilodon gracilis, Allophaiomys pliocaenicus	0.62
	Platygonus vetus	0.82
	Megalonyx leptostomus, Platygonus bicalcaratus, Ondatra idahoensis	1.72
	Nanippus peninsulatus, Borophagus diversidens, Glossotherium chapadmalense	2.13
	Paenemarmota	2.44


All N.Amer. Mammal Datums Combined	event		242/203/144		off
FAD
	Platygonus compressus	0.08
	Megalonyx jeffersonii	0.16
	Bison	0.19
	Ondatara zibethicus	0.31
	Smilodon populator	0.78
	Clethrionomys	0.84
	Microtus paroperarius	0.86
	Microtus meadensis,  Lemmiscus curtatus	0.89
	Euceratherium	1.12
	Ondatra annectens, Microtus sp. (5T)	1.19
	Synaptomys	1.33
	Mammuthus	1.36
	Megalonyx wheateyi	1.57
	Phenacomys	1.72
	Paramylodon harlani	1.75
	Lepus	1.91
	Platygonus vetus	1.95
	Northrotheriops, Mictomys kansasensis/mel, Allophaiomys pliocaenicus	1.97
	Onadatra idahoensis, Smilodon gracilis	2.44
	Glossotherium chapadmalense, Mictomys vetus	2.58
	Miracinonyx inexpectatus	3.03
	Sylvilagus	3.12
	Pliolemmus	3.21
	Procastoroides	3.50
	Stegomastodon, Platygonus bicalcaratus	3.53
	Borophagus diversidens, Megalonyx leptostomus, Glyptotherium	3.60
	Pliopotamys	4.04
	Ogmodontomys poaphagus	4.68
	Ophiomys, Platygonus pearcei, Dipoides rexroadensis	4.72
	Ursus	4.80
	Nanippus peninsulatus, Ogmodontomys sawrockensis	4.90
	Eocioleus; carnivores (Lutra, Megantereon, Mustela, Sminthosinus, Trigonictis); arvicolines (Ogmodontomys, Protopliophenacomys) and Miopetaurista (flying squirrel) in Hh 4	5.91
	Agriotherium (carnivore), Castor (beaver), Felis (carnivore), Megalonyx (definition of the subdivision, a edentate), Ochotona (pika), Plesiogulo (carnivore), Pliozapus (zapodid), Prosomys (murid) in Hh 3	6.88
	carnivores (Enhydritherium, Eomellivora, Indarctos, Lutravus, Machairodus, Simocyon); Neotragoceras (bovid ungulate), Thinobadistes (definition of subdivision, a edentate) in Hh 2	7.59
	Crusafontina (soricid), Kansasimys (eomyid), Lemoynea (desmanine mole), Pliometanastes (definition of subdivison, a edentates), Paramicrotoscoptes (murid), Pliotomodon (murid) in Hh 1	9.07
	Actiocyon, Hoplictis, Platybelodon in Cl 3	10.09
	Barbourofelis is age marker of Cl 2 subzone.  Cormohipparion (hipparionines equine horses) in Cl 2	12.06
	Pseudoceras; plains taxa invade Great Basin	12.53
	Gomphotherium, Hesperolagomys, Lanthanotherium, Megasminthus, Pliogale, Pseudocyon, Russellagus, Untermannerix in Ba 2	14.78
	Plithocyon (hemicyonione bear), Zygolophodon (Proboscidean Datum)	15.97
	aceratherine rhinos (Aphelops, Peraceras), teloceratine rhino (Teleoceras); Copemys (cricetid), mustelids (Dinogale, Mionictis, Plionictis, Sthenictis); Eomys (an eomyid), Petauristodon (sciurid), Pseudaelurus (true felid) in He 2	17.34
	Ursavus (ursid); Aletomeryx (aletomerycine artiodactyl), Amphictis (procyonid), Amphicyon (amphicyonid), Antesorex (soricid), Brachypotherium (teleoceratine rhino), Floridaceras (aceratherine rhino), Caterogale, Desmatolagus and Oreolagus (rabbits), Edaphocyon (procyonid), Euroxenomys (casterine beaver),  Phoberocyon (hemicyonine), Plesiosorex (plesiosoricid), and mustelids (Leptarctus, Miomustela, Potamotherium) in He 1	18.50
	Barbouromeryx (cranioceratine dromomeryid), Cynelos (amphicyonine amphicyonid), Paracosoryx (merycodontine antilocaprid), Prablastomeryx in Ar 4	19.09
	Cephalogale, Menoceras (a rhino), Moropus, Ysengrinia (amphicyonine amphicyonid), Zodiolestes (a paleomustelid) in Ar 3	22.20
	Menoceras	23.31
	Entoptychus	24.74
	Parvericius, Caninae	27.33
	Meniscomys	28.52
	Palaeocastor, Erinaceidae, Talpinae, Kalobatippus, Dinohyus	30.04
	Diceratherium, Protoceras	32.08
	Hypertragulus calcaratus, Suoidea	33.88
	Cricetidae, Mustelidae	34.94
	Merycoidodon, Nimravidae	35.85
	Entelodontidae, Ursidae, Bothriodon, Poebrotherium	37.24
	Ischyromys	38.27
	Anthracotheriidae, Canidae, Amphicyonidae, Mesohippus, Rhinocerotidae	39.21
	Lagomorpha, Soricidae, Ruminantia	42.18
	Eobasileus cornutus, Hyracodontidae, Camelidae, Merycoidodontoidea	46.20
	Hyrachyus eximius	46.95
	Uintatherium anceps	50.21
	Omomys, Palaeosyops	52.24
	Brontotheriidae, Hyrachyidae, 	52.82
	Heptodon	53.23
	Chiroptera, Orohippus	53.89
	Oxyaena gulo	55.24
	Dipsalidictis transiens	55.46
	Primates, Artiodactyla, Perissodactyla	55.73
	Coryphodon, Rodentia	56.79
	Plesiadapis simonsi	57.72
	Plesiadapis churchilli	58.08
	Dinocerata, Oxyaenidae, Plesiadapis rex	59.10
	Plesiadapis anceps	60.63
	Plesiadapis, Phenacodus	61.72
	Pantolestidae, Nyctitheriidae	61.98
	Pantolambda, Deltatherium, Mixodectes	63.10
	Paromomys, Tetraclaenodon	64.28
	Purgatorius, Periptychus	65.27
	Catopsalis, Protungulatum	65.50
LAD
	Mictrotus meadensis, Microtus paroperarius	0.23
	Mictomys kansasensis/mel, Ondatra annectens, Meglonyx weatleyi	0.58
	Smilodon gracilis, Allophaiomys pliocaenicus	0.62
	Miracinonyx inexpectatus	0.78
	Platygonus vetus	0.82
	Stegomastodon	1.19
	Hypolagus, Ophiomys, Mictomys vetus	1.66
	Megalonyx leptostomus, Platygonus bicalcaratus, Ondatra idahoensis	1.72
	Prodipodomys	1.95
	Nanippus peninsulatus, Borophagus diversidens, Glossotherium chapadmalense	2.13
	Procasteroides	2.15
	Paenemarmota	2.44
	Dipoides rexroadensis, Ogmodontomys poaphagus, Pliopotamys, Pliolemmus	2.58
	Borophagus hilli, Platygonus pearcei	3.33
	Megantereon	3.60
	Ogmodontomys sawrockensis	4.63
	Nimravinae	23.03
	Meniscomys	25.05
	Poebrotherium	27.33
	Hyracodontidae	28.52
	Merycoidodon	30.10
	Pantolestidae, Ischyromys, Hypertragulus calcaratus, Bothriodon, Mesohippus	32.19
	Brontotheriidae	33.74
	Oromerycidae, Cylindrodontidae	33.88
	Multituberculata, Apatotheria	35.40
	Hyopsodus	35.85
	Plesiadapiformes, Nyctitheriidae	37.24
	Dinocerata, Omomys, Taeniodonta, Hyrachyidae	39.21
	Oxyaenidae, Hyrachyus eximius, Eobasileus cornutus	42.18
	Tillodontia, Orohippus, Phenacodus, Palaeosyops, Uintatherium anceps	46.20
	Heptodon, Coryphodon	50.21
	Eucosmodontidae	53.89
	Oxyaena gulo	54.38
	Dipsalidictis transiens	54.81
	Arfia junnei	55.46
	Arctostylopida, Plesiadapis	55.73
	Plesiadapis gingerichi	56.61
	Plesiadapis churchilli, Periptychus	57.72
	Plesiadapis rex	58.08
	Plesiadapis anceps	59.10
	Pantolambda, Catopsalis, Paromomys	60.63
	Tetraclaenodon, Mixodectes	61.72
	Deltatherium	61.98
	Protungulatum, Purgatorius	64.28



Europe Mammals	:	ELMA	MN-MP Zones	Europe Paleogene events	_METACOLUMN_OFF		J. Hooker (GTS2004 diagrams)

ELMA	block	60	242/187/102
	TOP	23.03
	Arvernian	29.16
	Suevian	33.79
	Headonian	37.24
	Robiacian	42.77
	Geiseltalian	48.46
	Grauvian	50.83
	Neustrian	57.24

MN-MP Zones	block	40	242/187/102	notitle
	TOP	0
	un-named	1.95
	MN17	2.60
	MN16	3.40
	MN15	4.20
	MN14	4.70
	MN13	7.00
	MN12	8.20
	MN11	9.00
	MN10	9.50
	MN9	11.19
	MN7-8	12.51
	MN6	15.20
	MN5	17.00
	MN4	18.01
	MN3	19.99
	MN2	22.80
	MN1	23.03
	MP30	23.31
	MP29	23.94
	MP28	24.66
	MP27	25.59
	MP26	27.60
	MP25	29.16
	MP24	30.22
	MP23	30.90
	MP22	32.73
	MP21	33.79
	MP20	33.88
	MP19	34.78
	MP18	36.58
	MB17 b	36.80
	MB17 a	37.24
	MP16	40.44
	MP15	42.18
	MP14	42.77
	MP13	44.27
	MP12	45.97
	MP11	48.46
	MP10	50.83
	MP8-9	55.46
	MP7	55.73
	MP6	57.24
	MP1-5	65.50

Europe Paleogene events	event		242/203/144
FAD
	Issiodoromys bransatensis	23.31
	Issiodoromys pseudanoema	23.94
	Issiodoromys limognensis	24.66
	Issiodoromys quercyi	25.59
	Plesiosorex, Issiodoromys pauffiensis	27.60
	Blainvillimys blainvillei	29.16
	Issiodoromys minor, Soricidae	30.22
	Blainvillimys helmeri, Viverridae	30.90
	Blainvillimys gregarius, Issiodoromys medius	32.73
	Bothriodon	33.45
	Rhinocerotidae, Cricetidae, Entelodon, Castoridae 	33.79
	Palaeotherium m. medium	34.78
	Palaeotherium curtum villerealense	35.89
	Palaeotherium magnum, Isoptychus euzetensis, Talpidae, Anthracotheriidae	37.24
	Cainotheriidae, Palaeotherium castrense robiacense	39.40
	Leptolophus stehlini	40.20
	Lophiodon lautricense	40.44
	Pseudoltinomys cosetanus	42.18
	Propalaeotherium, isselanum	45.97
	Palaeotherium, Pseudosciuridae, Theridomyidae s.s., Amphimerycidae, Plagiolophus	44.01
	Quercygale, Lophiotherium	44.27
	Propalaeotherium hassiacum, Anoplotheriidae	48.46
	Choeropotamidae, Gliridae, Propachynolophus gaudryi	50.83
	Lophiodon	51.56
	Donrussellia, Propachynolophus levei	51.98
	Lophiodontidae	52.24
	Hyrachyidae	52.82
	Oxyaena gulo	54.81
	Dipsalidictis transiens	55.46
	Primates, Artiodactyla, Perissodactyla, Rodentia,  Oxyaenidae, Coryphodon	55.73
	Liotomus	57.24
	Pantolestidae, Arctocyon	58.50
	Adapisorex	59.61
	Plesiadapis	61.21
	Adapisoriculidae	61.98
	Hainina	65.50
LAD
	Theridomyidae	23.03
	Issiodoromys pseudanoema	23.31
	Issiodoromys limognensis	23.94
	Issiodoromys quercyi, Dichobunidae	24.66
	Issiodoromys pauffiensis, Anoplotheriidae	25.59
	Plagiolophus, Nyctitheriidae, Blainvillimys blainvillei	27.60
	Blainvillimys heimersheimensis	29.16
	Pseudosciuridae, Issiodoromys medius, Blainvillimys helmeri	30.22
	Blainvillimys gregarius, Entelodon, Plagiolophus ministri, Primates	30.90
	Bothriodon	32.84
	Palaeotherium	33.41
	Amphimerycidae	33.79
	Xiphodontidae, Palaeotherium m. medium	33.88
	Palaeotherium curtum villerealense	34.78
	Isoptychus euzetensis, Lophiotherium	36.19
	Lophiotherium, Quercygale	36.87
	Propalaeotherium	37.24
	Leptolophus stehlini	37.61
	Hyrachyidae, Lophiodontidae, Palaeotherium castrense robiacense, Pseudoltinomys cosetanus	38.22
	Lophiodon leptorhynchus	40.44
	Propalaeotherium isselanum	42.77
	Propalaeotherium hassiacum	45.97
	Phenacodus, Donrussellia, Propachynolophus gaudryi	48.46
	Propachynolophus levei	50.99
	Multituberculata	51.98
	Plesiadapis, Coryphodon, Oxyaenidae, Hyopsodus	52.31
	Oxyaena gulo	54.38
	Dipsalidictis transiens	55.24
	Adapisoriculidae	55.52
	Liotomus, Hainina, Neoplagiaulax, Adapisorex, Arctocyon	56.15

Asian Mammals	:	ALMA	Asian Mammal Subzones	_METACOLUMN_OFF		J. Hooker (GTS2004 diagrams)

ALMA	block	60	242/187/102
	TOP	23.03
	Tabenbulukian	24.79
	Hsandgolian	33.79
	Ergilian	35.10
	Ulangochuian	37.20
	Sharamurunian	40.39
	Irdinmanhan	46.20
	Arshantan	52.09
	Bumbanian	55.73
	Gashatan	56.90
	Nongshanian	62.94
	Shanghuan	65.50

Asian Mammal Subzones	block	30	242/187/102	notitle
	TOP	56.90
	(c)	58.08
	(b)	60.05
	(a)	62.94
	(b)	64.91
	(a)	65.50

South America Mammals	:	SALMA	_METACOLUMN_OFF		NEOGENE zonal ages are taken from The Paleobiology Database accessed Sept, 2005.  PALEOGENE zonal ages measured from J. Hooker (GTS2004 Figure 20.4, p.400)

SALMA	block	60	242/187/102
	TOP	0
	Lujanian	0.80
	Ensenadan	1.17
	Uquian	2.99
	Chapadmalalan	4.01
	Montehermosan	6.98
	Huayquerian	9.07
	Chasicoan	10.09
	Mayoan	11.89
	Laventan	13.82
	Colloncuran	15.49
	Friasian	16.28
	Santacrucian	17.43
	Colhuehuapian	20.44
	TOP	26.41
	Deseadan	27.90
	TOP	30.99
	Tinguirirican	32.08
	TOP	33.60
	Mustersan	34.21
	TOP	35.60
	Barrancan	36.80
	? Vacan ? (Casamayoran)	55.73
	Riochican	57.42	Dashed
	Itaboraian	59.03
	Tiupampan	60.19
	Peligran	61.07	Dotted



Regional Stages	:	North America Series (Cret, Permian, PreCamb)	North America Stage (Permian-Cambrian)	California (Cenozoic)	Europe Series (Cret, Perm-Carb, Camb)	Europe Stages (Perm-Carb, Ordov)	Europe Substages (Perm-Carb)	Baltic Regional Stages (Silurian)	Russia Series (Permian)	Russia Stages (Perm-Carb & Cambrian)	Russia Substages (Perm-Carb)	Tethyan Stages (Permian)	Kazakhstan (Cambrian)	New Zealand (Present-Perm.)	Australia (Cenozoic & Silur-Proterozoic)	China (Jurassic-Archean)	Japan (Neogene & Cret)	South Africa (PreCamb)	_METACOLUMN_OFF

North America Series (Cret, Permian, PreCamb)	block	100	234/201/201	notitle		CRET = GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	65.50
	Gulfian	99.60
	Comanchean	126.99
	Coahulian	145.46
	TOP	253.80	dashed
	Ochoan	260.40
	Guadalupian	270.60
	Leonardian	276.15	dashed
	Wolfcampian	298.34
	TOP	542.00	dashed
	Hadrynian	850
	Helikian	1600
	Aphebian	2500

North America Stage (Permian-Cambrian)	block	100	234/201/201			Cretaceous and Precambrian = GeoWhen (compiled by R. Rohde; at www.stratigraphy.org); Permian-Carboniferous from Davydov (1996; GTS2004), Silurian-Ordovician from GeoWhen (compiled by R. Rohde; at www.stratigraphy.org); Cambrian from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005))
	TOP	253.80	dashed
	Castile	260.40
	Capitanian	265.80
	Wordian	268.00
	Roadian	270.60
	Cathedralian	273.35
	Hessian	276.15	dashed
	Lenoxian	288.48
	Nealian	298.34
	Bursumian	299.98	dashed
	Virgilian	304.08	dashed
	Missourian	305.65	dashed
	Desmoinesian	308.71	dashed
	Atokan	313.94	dashed
	Morrowan	318.10
	Chesterian	333.02	dashed
	Meramecian	339.63	dashed
	Osagean	349.40	dashed
	Kinderhookian	359.20
	Chatauquan	370.06
	Senecan	388.03
	Erian	391.80
	Ulsterian	416.00
	Cayugan	421.30
	Niagaran	438.01
	Medinan	443.70
	Cincinnatian	451.01
	Mohawkian	461.98
	White Rockian	471.80
	Cassinian	473.02
	Jeffersonian	475.00
	Demingian	478.60
	Skullrockian / Ibexian	489.89
	Sunwaptan	495.20
	Steptoan	501.00
	Marjuman	506.50
	Delmaran	513.50
	Dyeran	518.20
	Montezuman	521.00
	[ no subdivisions ]	542.00	dashed


California (Cenozoic)	block	100	234/201/201			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	0.000
	Hallian	0.012
	Wheelerian	1.90
	Venturian	2.20
	Repettian	2.90
	Delmontian	7.51
	Mohnian	13.51
	Luisian	15.51
	Relizian	16.51
	Saucesian	21.99
	Zemorrian	33.50
	Refugian	34.99
	Narizian	48.03
	Ulatisian	51.02
	Penutian	53.02
	Bulitian	55.79
	Ynezian	61.51

Europe Series (Cret, Perm-Carb, Camb)	block	100	220/217/234	notitle		Cret = Traditional series-level divisions; Perm-Carb = Davydov (GTS2004) and German Stratigraphic Commission (2002); Cambrian from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005)
	TOP	65.5
	Senonian	89.27
	TOP	125.00
	Neocomian	145.46
	TOP	251.00
	Zechstein	260.40
	Rotliegend	301.21
	Silesian	326.40
	Dinantian	359.20
	TOP	488.30
	Merionethian [West Avalonia; no subdivisions]	501.80
	Arcadian [West Avalonia; no subdivisions]	510.00
	Branchian [West Avalonia; no subdivisions]	520.40
	Placentian [West Avalonia; no subdivisions]	542.00

Europe Stages (Perm-Carb, Ordov)	block	100	220/217/234			Perm-Carb = Davydov (GTS2004) and German Stratigraphic Commission (2002); GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	251.00
	Zechstein	260.40
	Saxonian	275.60	dashed
	Altunian	301.21
	Stephanian	307.12
	Westphalian	315.22
	Namurian	326.40
	Visean	345.30
	Tournaisian	359.20
	TOP	443.70
	Hirnantian	445.60
	Rawtheyan	446.52
	Cautleyan	447.64
	Pusgillian	448.97
	Streffordian	452.03
	Cheneyan	454.98
	Burrellian	457.02
	Aurelucian	460.90
	Llandeilian	464.00
	Abereiddian	471.80
	Fennian	473.50
	Whitlandian	475.00
	Moridunian	478.60
	Migneintian	485.97
	Tremadocian	488.30


Europe Substages (Perm-Carb)	block	100	220/217/234	notitle		Perm-Carb = Davydov (GTS2004) and German Stratigraphic Commission (2002)
	TOP	299.00
	Kuzel	301.21
	Stephanian C	303.90
	Stephanian B	304.68
	(A) Barruelian	305.72
	Cantabrian	307.12
	(D) Asturian	309.36
	(C) Bolsovian	311.70
	(B) Duckmantian	313.30
	(A) Langsettian	315.22
	Yeadonian	315.86
	Marsdenian	316.50
	Kinderscoutian	317.30
	Alportian	317.70
	Chokierian	318.10
	Arnsbergian	324.33
	Pendleian	326.40
	Brigantian	331.88
	Asbian	336.42
	Holkerian	339.91
	Arundian	343.41
	Chadian	347.39
	Courceyan	359.20

Baltic Regional Stages (Silurian)	block	100	220/217/234	notitle		GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	Ohesaare	417.08
	Kaugetuma	418.70
	Kuressaare	419.48
	Paadla	422.74
	Rootsikula	424.55
	Jaagarahu	427.00
	Jaani	428.20
	Adavere	436.68
	Raikkula	440.88
	Juuru	443.70

Russia Series (Permian)	block	100	230/217/234	notitle
	TOP	251.00
	Tatarian	265.80
	Biarmian	270.60
	Cisuralian	299.00

Russia Stages (Perm-Carb & Cambrian)	block	100	230/217/234			Permian = Kotlar and Pronina-Nestell (2005) with fusulinid-ages from Davydov (GTS2004); Carboniferous = Davydov (GTS2004); Cambrian from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005)
	TOP	251.00
	Vyatkian	257.10	dashed
	Severodvinian	265.80
	Urzhumian	268.00
	Kazanian	270.60
	Ufimian	273.10
	Kungurian	275.60
	Artinskian	284.40
	Sakmarian	294.60
	Asselian	299.00
	Orenburgian	301.21
	Gzhelian	303.90
	Kasimovian	306.50
	Moscovian	311.70
	Bashkirian	318.10
	Serpukhovian	326.40
	Visean	345.30
	Tournaisian	359.20
	TOP	478.60
	Tremadocian	488.30
	Mansian	491.13
	Ketyna	494.00
	Yurakian	496.00
	Ensyan	498.25
	Maduan	500.00
	Tavgian	501.20
	Nganasanyan	502.20
	Mayan	505.80
	Amgan	511.40
	Toyonian	516.30
	Botomian	518.60
	Atdabanian	521.00
	Tommotian	531.20
	Nemakit - Daldynian	542.00
	Vendian	567.00	dotted

Russia Substages (Perm-Carb)	block	100	230/217/234	notitle		Permian = Kotlar and Pronina-Nestell (2005) with fusulinid-ages from Davydov (GTS2004); Carboniferous = Davydov (GTS2004)
	TOP	251.00
	Upper	254.13	dashed
	Lower	257.10	dashed
	Upper	260.40	dashed
	Lower	265.80
	Upper	269.30
	Lower	270.60
	TOP	299.00
	Melekhovian	299.98
	Noginian	301.21
	Pavlovoposadian	302.43
	Rusavkian	303.90
	Dorogovilovian	304.68
	Khamovnichian	305.72
	Krevyakian	306.50
	Peskovian	307.12
	Myachkovskian 	308.06
	Podolskian	309.36
	Kashirian	310.14
	Tsninian	310.84
	Vereiian 	311.70
	Melekesian	312.66
	Cheremshanian	313.94
	Prikamian	314.90
	Severokeltmian	315.96
	Krasnopolyanian	317.04
	Voznesenian	318.10
	Zapaltjubian	319.84
	Protvian	322.17
	Steshevian	324.33
	Tarussian	326.40
	Venevian	330.18
	Mikhalovian	333.02
	Aleksian	335.85
	Tulian	339.63
	Bobrikovian	342.47
	Radaevian	345.30
	Kosvinian	348.08
	Kizelovian	349.40
	Cherepetian	350.86
	Karakubian	352.25
	Upinian	355.03
	Malevian	357.31
	Gumerovian	359.20

Tethyan Stages (Permian)	block	100	236/204/215			Davydov (GTS2004)
	TOP	251.00
	Dorashamian - Dzhulfian	256.44
	Laibinian	262.43
	Midian	264.45
	Murgabain	268.00
	Kubergandian	270.60
	Bolorian	275.60
	Yakhtashian	280.11
	Sakmarian	294.60
	Asselian	299.00
	Orenburgian	301.21
	Gzhelian	303.90

Kazakhstan (Cambrian)	block	100	230/217/234			from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005)
	TOP	483.45	dashed
	Ungurian	489.52
	Batyrbayan	491.63
	Aksayan 	495.40
	Sakian	501.00
	Ayusokkanian	503.00
	Zhanaarykian	504.93
	Tyesaian	507.03
	"Lenan" [ no subdivisions ]	513.50
	Lower Cambrian [no subdivisions]	542.00


New Zealand (Present-Perm.)	block	100	197/217/234			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	0.000
	Hawera	0.011
	Putikian	0.480
	Okehuan	1.10
	Nukumaruan	1.96
	Mangapanian	2.59
	Waipipian	3.60
	Opoitian	4.79
	Kapitean	6.00
	Tongaporutuan	9.99
	Waiauan	11.51
	Lillburnian	15.00
	Clifdenian	16.51
	Altonian	17.49
	Awamoan	19.98
	Hutchinsonian	21.00
	Otaian	23.03
	Waitakian	26.99
	Duntroonian	28.02
	Whaingaroan	33.88
	Runangan	37.24
	Kaiatan	39.99
	Bortonian	44.03
	Porangan	46.97
	Heretaungan	50.02
	Mangaorapan	52.02
	Waipawan	56.51
	Teurian	65.50
	Haumurian	70.60
	Piripauan	83.53
	Teratan	86.94
	Mangaotanean	92.95
	Arowhanan	95.06
	Ngaterian	99.60
	Motuan	103.95
	Urutawan	110.04
	Korangan	119.03
	Mokoiwian	145.46
	Puaroan	150.03
	Ohauan	151.95
	Heterian	156.02
	Temaikian	168.97
	Ururoan	187.95
	Aratuaran	199.60
	Otapirian	202.99
	Warepan	205.99
	Otamitan	218.01
	Oretian	224.98
	Kaihikuan	232.01
	Etalian	243.00
	Malakovian	248.00
	TOP	251.00
	Makabewan	253.80
	Waiitian	260.40
	Braxtonian	270.60
	Mangapirian	277.98
	Telfordian	288.99

Australia (Cenozoic & Silur-Proterozoic)	block	100	197/217/234			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org); Cambrian from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005)
	TOP	1.00
	Werrikooian	1.81
	Yatalan	3.40
	Kalimnan	4.29
	Cheltenhamian	5.00
	Mitchellian	10.51
	Bairnsdalian	15.00
	Balcombian	15.51
	Batesfordian	16.51
	Longfordian	27.47
	Janjukian	30.03
	Aldingan	36.00
	Johannian	52.02
	Wangerripian	61.72
	Danian	65.50
	TOP	416.00
	Melbournian	428.20
	Eildonian	433.02
	Keiloran	443.70
	Bolindian	449.99
	Eastonian	456.00
	Gisbornian	460.90
	Darriwillian	468.10
	Ypeenian	469.99
	Castlemanian	470.99
	Chewtonian	473.02
	Bendigonian	475.00
	Warendian - Lancefieldian	488.30
	Datsonian 	489.52
	Payntonian	492.00
	Iverian	496.00
	Idamean	501.00
	Mindyallan	502.20
	Boomerangian	503.00
	Undillian	504.93
	Late Templetonian - Floran	507.03
	Ordian - Early Templetonian 	513.50
	Lower Cambrian [no subdivisions]	542.00
	Adelaidean	1300
	Carpentarian	1800
	Nullaginian	2500

China (Jurassic-Archean)	block	100	208/217/215			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org); Cambrian from Shanchi Peng (chair of subcommission, to J. Ogg, Dec. 2005)
	TOP	145.46
	Penglaizhenian	149.04
	Suiningian	161.21
	Shaximioan 	167.00
	Xintiangouan	175.60
	Ziliujingian	199.60
	Erqiaoan	209.01
	Huobachengian	219.00
	Bananian	228.01
	Falangian	237.00
	Guanlingian	245.17
	Yongningzhenian	249.75
	Feixianguanian	251.00
	Changshingian	253.80
	Wujiapingian	260.40
	Maokovian	270.60
	Xixianian	299.00
	Mapingian	309.98
	Dalanian	312.98
	Huashibanian	318.10
	Dewuan	333.02
	Datangian	344.92
	Yanguan	349.47
	Shaodongian	359.20
	Xikuangshanian	374.50
	Shetianqiaoan	385.30
	Dongganglingian	391.41
	Yingtangian	397.50
	Sipaian	407.00
	Yujianian	409.98
	Nagaolingian	413.02
	Lianhuashanian	416.00
	Yulongsian	418.70
	Miaogoalingian	422.00
	Guandian	425.51
	Xiushanian	428.99
	Baishaean	433.02
	Shinulanian	438.01
	Longmaxian	443.70
	Wufengian	448.97
	Linxiangian	454.47
	Baotan	460.90
	Miaopoan	464.00
	Guniutanian	471.80
	Dawanian	472.00
	Honghuayuanian	478.60
	Ichangian	488.30
	Taoyuanian	496.00
	Paibian (Waergangian)	501.00
	Youshuian	501.80
	Wangcunian	504.93
	Taijianian	510.00
	Duyunian	515.25
	Nangaoan	521.00
	Meishuchuan	536.82
	Jinningian	542.00
	Sinian	799	dashed
	Jinningian	1750
	Luliangian	2350
	Wutaian	2700
	Fupingan	3100
	Qianxin	3800

Japan (Neogene & Cret)	block	100	208/217/215			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	0.78
	Yuzanjian	1.50
	Kechienjian	1.90
	Suchian	3.00
	Totomian	3.60
	Yuian	9.51
	Fujian	11.12
	Kaburan	13.51
	Tozawan	15.97
	Haranoyan	18.20
	TOP	65.50
	Hetonian	77.07
	Urakawan	89.27
	Gyliakian	96.64
	Miyakoan	125.00

South Africa (PreCamb)	block	100	198/217/174			GeoWhen (compiled by R. Rohde; at www.stratigraphy.org)
	TOP	542.00
	Namibian	900
	Mokolian	2050
	Vaalian	2500
	Randian	3000
	Swazian	4000

Italian Pleistocene Stages	:	Italian marine stage	Italian marine substage	_METACOLUMN_OFF		P. Gibbard (2004, and references therein; pers. commun. to J.Ogg, 2006)

Italian marine stage	block	100	211/217/206	notitle
	TOP	0.018
	Tarantian	0.126
	Ionian	0.96
	Calabrian	1.81
	Gelasian	2.588

Italian marine substage	block	80	211/217/206	notitle
	TOP	0.09
	Tyrrhenian	0.126
	TOP	0.96
	Sicilian	1.24
	Emilian	1.50
	Santomian	1.81


Eurasian Quaternary (terrestrial) Stages	:	NW European stages	NW European substages	British stages	British substages	Russian Plain stages	Russian Plain substages	_METACOLUMN_OFF		P. Gibbard (2004, and references therein; pers. commun. to J.Ogg, 2006)

NW European stages	block	100	220/225/234
	TOP	0.018
	Weichselian	0.09
	Eemian	0.126
	Saalian	0.38
	Holsteinian	0.41
	Elsterian	0.46
	Cromerian Complex	0.86
	Bayelian	1.12
	Menapian	1.38
	Waalian	1.60
	Eburonian	1.76
	Tiglian	2.44	dashed
	Praetiglian	2.56	dashed
	Reuverian C	2.63	dashed
	Reuverian B	2.70	dashed

NW European substages	block	100	220/225/234	notitle
	TOP	0.126
	Warthe	0.16	dashed
	Drenthe	0.19
	Wacken / Domnitz	0.335	dotted
	Fuhne	0.38
	TOP	0.46
	Noordbergum (Interglacial IV)	0.50
	Glacial c	0.55
	Rosmalen (Interglacial III)	0.62
	Glacial b	0.68
	Westerhoven (Interglacial II)	0.71
	Glacial a	0.77
	Waardenburg (Interglacial I)	0.86
	Dorst	0.93
	Leerdam	0.96
	Linge	1.055
	Bavel	1.12
	TOP	1.78
	C5-6	1.87
	C4c	1.92
	A, B, C1-3	2.44

British stages	block	100	195/225/234
	TOP	0.018
	Devensian	0.09
	Ipswichian	0.126
	Wolstonian	0.38
	Hoxnian	0.41
	Anglian	0.46
	Cromerian	0.86
	Beestonian	1.76
	Pastonian	1.87
	Pre-Pastonian / Baventian	1.92
	Bramertonian / Antian	2.12
	Thurnian	2.27
	Ludhamian	2.48
	Pre-Ludhamian	2.61	dashed
	Waltonian	2.70	dashed

British substages	block	100	195/225/234	notitle
	TOP	0.126
	"Tottenhill"	0.19
	[un-named]	0.38

Russian Plain stages	block	100	230/217/234
	TOP	0.018
	Neopleistocene	0.86
	Eopleistocene	1.76
	Late Pliocene	2.588

Russian Plain substages	block	100	230/217/234	notitle
	TOP	0.018
	Valdaian	0.09
	Mikulinian	0.126
	Moscovian	0.16
	Dnieper	0.19
	Likhvinian	0.41
	Okian	0.46
	Muchkapian	0.55
	Donian	0.68
	Ilynian	0.71
	Pokrovian	0.77
	Petropavlovian	0.86
	Krinitsa	1.38	dashed
	Tolucheevka	1.76
	Khapry	2.16	dashed
	Verkhodon	2.61	dashed



North American Quaternary (terrestrial) Stages	:	North America stages	North America substages	_METACOLUMN_OFF		P. Gibbard (2004, and references therein; pers. commun. to J.Ogg, 2006)

North America stages	block	100	234/201/201
	TOP	0.018
	Wisconsinian	0.09
	Sangamonian	0.126
	Illinoian	0.19
	Pre-Illinoian	2.72	dashed

North America substages	block	40	234/201/201	notitle
	TOP	0.19
	A	0.38
	B	0.46
	C	0.55	dashed
	D	0.68	dashed
	E	0.77	dashed
	F	0.93	dashed
	G	1.38	dashed
	H	1.76	dashed
	I	1.88	dashed
	J	1.92	dashed
	K	2.72	dashed

New Zealand Quaternary Stages	:	New Zealand stages	_METACOLUMN_OFF		P. Gibbard (2004, and references therein; pers. commun. to J.Ogg, 2006)

New Zealand stages	block	100	197/217/234	notitle
	TOP	0
	Haweran	0.34
	Castlecliffian	1.65
	Nukumaruan	2.44
	Mangapanian	2.63	dashed

Chinese Loess	:	Chinese Loess Sequence	_METACOLUMN_OFF		An Zhisheng et al. (1990) [measured from their diagram]

Chinese Loess Sequence	block	60	208/217/215	notitle
	TOP	0.00
	S0	0.010
	L1	0.121
	S1	0.155
	L2	0.222
	S2	0.27
	L3	0.31
	S3	0.33
	L4	0.38
	S4	0.41
	L5	0.49
	S5	0.58
	L6	0.67
	S6	0.69
	L7	0.74
	S7	0.77
	L8	0.79
	S8	0.82
	L9	0.93
	S9	0.95
	L10	0.97
	S10	0.98
	L11	1.00
	S11	1.02
	L12	1.04
	S12	1.07
	L13	1.12
	S13	1.14
	L14	1.16
	S14	1.19
	L15	1.34
	WS1	1.47
	WL1	1.56
	WS2	1.63
	WL2	1.77
	WS3	1.98
	WL3	2.20
	WS4	2.34
	WL4	2.52
	RS	2.63


Loess Mag Susc	point				off
nopoints	line		0	230
	0.000	100
	0.004	90
	0.011	125
	0.015	120
	0.019	92
	0.026	97
	0.030	32
	0.038	36
	0.045	40
	0.053	55
	0.057	59
	0.062	70
	0.068	80
	0.075	75
	0.083	75
	0.090	78
	0.094	92
	0.101	90
	0.105	70
	0.109	45
	0.116	40
	0.120	30
	0.128	32
	0.135	50
	0.143	42
	0.150	140
	0.158	184
	0.165	195
	0.173	150
	0.180	55
	0.188	20
	0.195	28
	0.203	35
	0.210	38
	0.218	25
	0.225	20
	0.229	29
	0.237	89
	0.240	70
	0.248	49
	0.255	40
	0.263	55
	0.270	180
	0.278	150
	0.285	55
	0.289	49
	0.297	112
	0.300	90
	0.308	65
	0.315	40
	0.323	50
	0.330	52
	0.338	52
	0.345	70
	0.349	180
	0.353	161
	0.357	130
	0.360	140
	0.364	158
	0.368	140
	0.372	162
	0.375	120
	0.383	20
	0.391	20
	0.398	32
	0.406	38
	0.413	30
	0.421	35
	0.424	60
	0.428	80
	0.436	105
	0.443	160
	0.451	180
	0.458	149
	0.462	70
	0.466	89
	0.469	113
	0.473	40
	0.477	20
	0.481	25
	0.488	35
	0.496	35
	0.503	35
	0.511	40
	0.518	57
	0.526	62
	0.533	60
	0.541	210
	0.544	248
	0.548	230
	0.556	205
	0.563	182
	0.571	119
	0.578	130
	0.586	100
	0.590	80
	0.593	111
	0.601	95
	0.608	80
	0.616	30
	0.623	32
	0.631	32
	0.638	28
	0.646	21
	0.650	19
	0.653	24
	0.661	35
	0.668	44
	0.676	50
	0.683	42
	0.687	38
	0.691	40
	0.698	15
	0.706	61
	0.713	38
	0.721	68
	0.728	90
	0.736	60
	0.739	40
	0.743	48
	0.747	62
	0.751	70
	0.758	95
	0.766	110
	0.770	118
	0.773	40
	0.781	25
	0.784	39
	0.788	49
	0.794	72
	0.801	105
	0.808	128
	0.814	116
	0.821	81
	0.828	13
	0.834	15
	0.841	13
	0.848	20
	0.854	21
	0.861	20
	0.868	17
	0.874	17
	0.881	30
	0.888	45
	0.891	52
	0.895	52
	0.901	48
	0.908	24
	0.915	25
	0.918	27
	0.921	26
	0.928	24
	0.931	38
	0.935	82
	0.941	122
	0.945	129
	0.948	125
	0.955	56
	0.961	70
	0.965	96
	0.968	88
	0.975	68
	0.978	77
	0.981	95
	0.988	86
	0.994	85
	1.000	105
	1.006	111
	1.012	130
	1.018	90
	1.024	82
	1.030	70
	1.036	72
	1.048	90
	1.060	98
	1.066	109
	1.072	90
	1.077	58
	1.082	96
	1.087	64
	1.091	90
	1.096	42
	1.101	54
	1.106	28
	1.111	28
	1.116	28
	1.121	34
	1.130	32
	1.135	100
	1.140	135
	1.150	172
	1.155	179
	1.160	90
	1.165	50
	1.169	51
	1.174	42
	1.179	88
	1.189	72
	1.194	102
	1.199	85
	1.205	20
	1.210	70
	1.213	15
	1.218	15
	1.228	16
	1.238	15
	1.247	14
	1.257	12
	1.267	18
	1.276	22
	1.286	42
	1.291	55
	1.296	80
	1.306	82
	1.311	68
	1.315	80
	1.320	72
	1.325	30
	1.330	19
	1.340	28
	1.345	29
	1.354	41
	1.364	58
	1.374	100
	1.379	109
	1.384	95
	1.393	75
	1.403	65
	1.413	105
	1.423	85
	1.427	79
	1.432	85
	1.437	70
	1.442	70
	1.452	98
	1.462	60
	1.466	123
	1.471	32
	1.481	60
	1.486	50
	1.496	52
	1.500	98
	1.510	59
	1.520	40
	1.530	44
	1.535	64
	1.539	50
	1.549	40
	1.559	50
	1.561	70
	1.564	35
	1.574	52
	1.578	71
	1.588	92
	1.598	78
	1.603	95
	1.612	80
	1.617	88
	1.622	85
	1.632	94
	1.637	80
	1.647	56
	1.656	50
	1.666	45
	1.671	30
	1.676	51
	1.681	48
	1.685	54
	1.695	49
	1.705	34
	1.715	40
	1.724	35
	1.729	28
	1.734	30
	1.739	79
	1.744	70
	1.754	61
	1.763	40
	1.773	34
	1.778	35
	1.785	40
	1.799	90
	1.813	71
	1.827	60
	1.834	115
	1.841	120
	1.855	125
	1.868	95
	1.882	70
	1.889	88
	1.896	81
	1.910	90
	1.924	79
	1.931	105
	1.938	105
	1.945	100
	1.952	88
	1.959	95
	1.965	82
	1.979	70
	1.986	32
	1.992	46
	1.999	28
	2.006	30
	2.019	35
	2.033	60
	2.046	70
	2.060	55
	2.074	36
	2.087	29
	2.101	29
	2.114	30
	2.128	50
	2.134	71
	2.148	69
	2.155	58
	2.168	58
	2.182	49
	2.195	26
	2.209	49
	2.216	35
	2.222	42
	2.236	88
	2.249	45
	2.263	56
	2.277	90
	2.290	59
	2.297	80
	2.304	69
	2.317	79
	2.331	55
	2.337	68
	2.344	39
	2.358	30
	2.371	40
	2.385	85
	2.398	52
	2.412	22
	2.419	34
	2.425	26
	2.439	50
	2.452	80
	2.466	60
	2.480	52
	2.493	35
	2.500	56
	2.507	32
	2.520	55
	2.534	51
	2.547	161
	2.554	195
	2.561	170
	2.567	91
	2.581	115
	2.588	108
	2.601	130
	2.615	92
	2.628	60


Antarctic delta-Deuterium (per-mil)	point				off	Jouzel et al. (2004).  Accessed from NCDC Paleoclimatology Program.
nopoints	line		-450	-360
	0.00007	-391.20
	0.00014	-396.49
	0.00022	-398.19
	0.00029	-398.11
	0.00037	-400.07
	0.00046	-398.49
	0.00055	-397.83
	0.00064	-394.86
	0.00073	-400.54
	0.00082	-392.33
	0.00092	-398.81
	0.00101	-396.96
	0.00111	-396.37
	0.00121	-393.51
	0.00131	-394.30
	0.00141	-395.44
	0.00152	-396.86
	0.00163	-397.49
	0.00174	-397.54
	0.00185	-396.51
	0.00197	-397.89
	0.00209	-396.96
	0.00222	-396.97
	0.00234	-402.41
	0.00247	-397.01
	0.00260	-395.10
	0.00273	-393.74
	0.00285	-393.96
	0.00297	-396.33
	0.00309	-395.95
	0.00322	-399.50
	0.00335	-397.56
	0.00348	-394.81
	0.00360	-393.87
	0.00372	-393.87
	0.00385	-396.24
	0.00398	-394.44
	0.00412	-395.27
	0.00425	-395.20
	0.00438	-395.00
	0.00452	-396.20
	0.00465	-396.91
	0.00479	-395.27
	0.00493	-396.07
	0.00506	-394.10
	0.00520	-395.53
	0.00534	-399.23
	0.00548	-396.94
	0.00562	-395.29
	0.00575	-393.10
	0.00589	-397.51
	0.00603	-396.41
	0.00617	-397.56
	0.00632	-397.54
	0.00646	-400.19
	0.00661	-398.03
	0.00675	-396.24
	0.00690	-398.96
	0.00705	-402.01
	0.00720	-398.90
	0.00735	-402.39
	0.00750	-395.30
	0.00764	-397.46
	0.00779	-398.07
	0.00794	-400.49
	0.00809	-404.27
	0.00825	-400.67
	0.00840	-401.09
	0.00855	-398.37
	0.00870	-398.94
	0.00885	-398.61
	0.00900	-396.29
	0.00915	-398.83
	0.00930	-394.07
	0.00944	-392.28
	0.00959	-394.63
	0.00973	-391.67
	0.00987	-391.30
	0.01001	-393.06
	0.01015	-392.03
	0.01029	-389.14
	0.01043	-393.50
	0.01057	-392.61
	0.01071	-388.41
	0.01086	-392.41
	0.01101	-392.94
	0.01116	-394.27
	0.01131	-392.01
	0.01146	-391.79
	0.01161	-391.80
	0.01176	-390.56
	0.01191	-393.01
	0.01207	-392.40
	0.01222	-398.23
	0.01239	-401.76
	0.01257	-407.20
	0.01276	-409.31
	0.01295	-412.14
	0.01315	-415.66
	0.01336	-415.10
	0.01357	-414.10
	0.01377	-410.77
	0.01397	-413.57
	0.01417	-414.96
	0.01438	-411.74
	0.01458	-407.67
	0.01478	-402.99
	0.01496	-404.94
	0.01516	-410.74
	0.01538	-412.16
	0.01558	-410.93
	0.01579	-413.19
	0.01601	-418.67
	0.01624	-418.26
	0.01647	-418.99
	0.01671	-423.57
	0.01697	-423.94
	0.01723	-428.26
	0.01750	-433.73
	0.01779	-433.81
	0.01809	-438.79
	0.01840	-439.89
	0.01873	-441.44
	0.01906	-441.93
	0.01939	-440.89
	0.01972	-442.46
	0.02005	-439.79
	0.02039	-443.77
	0.02073	-441.41
	0.02106	-441.40
	0.02138	-442.01
	0.02171	-442.31
	0.02204	-441.83
	0.02237	-441.11
	0.02269	-440.20
	0.02302	-443.51
	0.02335	-440.17
	0.02369	-442.79
	0.02402	-439.33
	0.02434	-439.47
	0.02467	-443.17
	0.02501	-442.99
	0.02535	-443.47
	0.02569	-444.50
	0.02603	-445.16
	0.02638	-444.66
	0.02672	-443.97
	0.02706	-444.24
	0.02740	-444.60
	0.02774	-443.81
	0.02807	-439.00
	0.02839	-437.79
	0.02872	-443.73
	0.02905	-437.46
	0.02937	-440.43
	0.02968	-435.89
	0.02998	-437.13
	0.03029	-439.87
	0.03062	-442.47
	0.03096	-440.91
	0.03129	-438.43
	0.03162	-444.04
	0.03196	-441.71
	0.03227	-435.11
	0.03257	-437.73
	0.03289	-441.66
	0.03322	-438.54
	0.03353	-434.86
	0.03385	-438.40
	0.03419	-442.99
	0.03452	-438.61
	0.03483	-434.80
	0.03514	-433.37
	0.03544	-435.43
	0.03576	-436.67
	0.03608	-437.91
	0.03640	-435.79
	0.03672	-436.70
	0.03703	-431.80
	0.03733	-429.71
	0.03761	-422.69
	0.03789	-429.23
	0.03818	-427.01
	0.03846	-428.13
	0.03875	-429.96
	0.03906	-436.94
	0.03940	-439.01
	0.03974	-435.83
	0.04007	-436.29
	0.04043	-439.01
	0.04078	-433.14
	0.04111	-436.27
	0.04146	-440.27
	0.04182	-437.61
	0.04216	-435.24
	0.04247	-430.01
	0.04280	-431.91
	0.04315	-434.80
	0.04350	-438.20
	0.04383	-437.13
	0.04416	-435.38
	0.04448	-431.54
	0.04478	-427.74
	0.04507	-425.20
	0.04534	-422.31
	0.04562	-421.87
	0.04589	-420.64
	0.04617	-426.87
	0.04646	-426.75
	0.04676	-428.57
	0.04708	-434.26
	0.04741	-433.10
	0.04773	-434.46
	0.04806	-432.60
	0.04839	-434.55
	0.04872	-430.93
	0.04904	-431.63
	0.04935	-430.34
	0.04967	-431.57
	0.04999	-431.76
	0.05031	-428.62
	0.05061	-428.11
	0.05091	-424.26
	0.05121	-426.90
	0.05151	-423.52
	0.05180	-424.31
	0.05208	-418.60
	0.05237	-426.33
	0.05267	-425.17
	0.05297	-425.59
	0.05329	-432.05
	0.05361	-427.04
	0.05392	-428.69
	0.05425	-431.83
	0.05459	-434.26
	0.05492	-430.36
	0.05525	-429.02
	0.05556	-424.81
	0.05586	-423.65
	0.05616	-424.34
	0.05646	-425.10
	0.05676	-420.24
	0.05704	-419.97
	0.05733	-421.63
	0.05762	-421.59
	0.05792	-424.48
	0.05823	-423.76
	0.05855	-428.73
	0.05887	-427.67
	0.05920	-428.02
	0.05953	-429.61
	0.05987	-431.78
	0.06022	-434.73
	0.06059	-437.01
	0.06097	-438.30
	0.06137	-442.67
	0.06177	-437.38
	0.06214	-434.30
	0.06252	-438.53
	0.06292	-440.55
	0.06331	-438.62
	0.06371	-441.40
	0.06413	-443.41
	0.06455	-442.02
	0.06496	-441.36
	0.06538	-442.33
	0.06578	-439.38
	0.06619	-441.25
	0.06659	-436.18
	0.06700	-443.29
	0.06741	-439.67
	0.06781	-434.37
	0.06817	-430.15
	0.06851	-423.40
	0.06884	-424.84
	0.06919	-427.79
	0.06954	-428.49
	0.06990	-431.37
	0.07028	-437.10
	0.07067	-434.60
	0.07104	-429.00
	0.07139	-427.48
	0.07173	-422.76
	0.07205	-419.96
	0.07236	-416.41
	0.07268	-422.97
	0.07301	-426.08
	0.07337	-430.70
	0.07374	-431.23
	0.07411	-430.37
	0.07447	-429.55
	0.07482	-425.94
	0.07518	-430.18
	0.07554	-428.44
	0.07589	-427.48
	0.07623	-423.49
	0.07658	-426.17
	0.07692	-421.66
	0.07724	-421.75
	0.07757	-420.89
	0.07789	-420.97
	0.07822	-418.95
	0.07854	-421.57
	0.07886	-419.69
	0.07918	-416.01
	0.07948	-415.48
	0.07979	-413.18
	0.08009	-414.90
	0.08038	-411.50
	0.08067	-410.00
	0.08097	-412.04
	0.08126	-410.35
	0.08156	-412.31
	0.08186	-413.74
	0.08217	-414.84
	0.08249	-417.42
	0.08281	-416.03
	0.08314	-419.54
	0.08348	-420.22
	0.08384	-422.67
	0.08420	-425.36
	0.08459	-430.66
	0.08499	-429.29
	0.08538	-427.58
	0.08578	-427.21
	0.08616	-424.30
	0.08654	-423.40
	0.08691	-422.76
	0.08727	-419.24
	0.08764	-422.06
	0.08803	-424.30
	0.08842	-425.32
	0.08881	-426.13
	0.08921	-425.75
	0.08960	-425.38
	0.08998	-419.45
	0.09035	-422.52
	0.09073	-421.55
	0.09111	-422.90
	0.09148	-420.75
	0.09185	-420.03
	0.09222	-420.48
	0.09258	-415.33
	0.09294	-419.21
	0.09330	-420.84
	0.09367	-419.07
	0.09405	-422.13
	0.09442	-421.43
	0.09480	-418.89
	0.09516	-421.43
	0.09554	-418.70
	0.09591	-420.55
	0.09628	-418.34
	0.09665	-420.79
	0.09703	-420.05
	0.09741	-420.95
	0.09779	-418.80
	0.09815	-416.96
	0.09851	-416.20
	0.09888	-417.28
	0.09925	-419.42
	0.09964	-421.79
	0.10003	-421.08
	0.10043	-421.72
	0.10083	-426.82
	0.10125	-430.78
	0.10166	-426.00
	0.10207	-423.74
	0.10250	-419.54
	0.10292	-422.03
	0.10335	-419.20
	0.10379	-417.05
	0.10423	-412.14
	0.10467	-417.44
	0.10512	-421.95
	0.10558	-425.39
	0.10604	-431.09
	0.10651	-429.59
	0.10697	-430.45
	0.10743	-425.65
	0.10789	-424.45
	0.10833	-424.11
	0.10877	-423.09
	0.10922	-425.13
	0.10966	-424.80
	0.11009	-422.07
	0.11050	-421.39
	0.11090	-417.61
	0.11129	-415.69
	0.11167	-411.36
	0.11204	-410.71
	0.11241	-408.17
	0.11276	-407.57
	0.11312	-407.38
	0.11347	-407.14
	0.11380	-402.56
	0.11412	-400.69
	0.11444	-399.75
	0.11475	-396.96
	0.11507	-398.33
	0.11539	-392.03
	0.11570	-385.01
	0.11600	-390.98
	0.11631	-393.74
	0.11663	-393.92
	0.11694	-390.35
	0.11724	-392.11
	0.11755	-388.04
	0.11786	-390.83
	0.11816	-387.06
	0.11846	-387.93
	0.11876	-386.71
	0.11906	-385.96
	0.11935	-389.20
	0.11964	-381.30
	0.11994	-386.73
	0.12024	-385.13
	0.12054	-386.45
	0.12084	-385.52
	0.12114	-383.31
	0.12143	-384.48
	0.12171	-379.21
	0.12201	-388.45
	0.12232	-387.82
	0.12263	-386.26
	0.12294	-386.62
	0.12326	-389.74
	0.12358	-387.31
	0.12390	-388.38
	0.12421	-385.40
	0.12451	-381.58
	0.12480	-379.03
	0.12509	-381.74
	0.12537	-375.92
	0.12564	-371.95
	0.12590	-370.66
	0.12615	-364.29
	0.12639	-366.68
	0.12664	-367.92
	0.12690	-369.51
	0.12716	-371.18
	0.12743	-370.95
	0.12770	-371.99
	0.12798	-374.89
	0.12827	-376.11
	0.12858	-383.51
	0.12890	-386.35
	0.12924	-386.42
	0.12959	-392.06
	0.12997	-398.14
	0.13037	-399.17
	0.13081	-405.20
	0.13128	-413.88
	0.13178	-411.61
	0.13231	-418.40
	0.13288	-423.30
	0.13352	-432.18
	0.13420	-433.24
	0.13491	-436.27
	0.13563	-434.47
	0.13634	-435.18
	0.13708	-440.71
	0.13785	-440.43
	0.13861	-437.05
	0.13936	-440.53
	0.14012	-438.64
	0.14087	-436.46
	0.14161	-435.20
	0.14234	-436.97
	0.14308	-437.25
	0.14383	-435.92
	0.14455	-435.89
	0.14526	-430.74
	0.14598	-435.28
	0.14671	-433.21
	0.14743	-436.00
	0.14813	-429.40
	0.14882	-430.65
	0.14950	-430.22
	0.15020	-433.21
	0.15091	-431.70
	0.15164	-435.65
	0.15241	-437.71
	0.15320	-441.06
	0.15401	-438.98
	0.15482	-441.16
	0.15562	-439.72
	0.15641	-438.65
	0.15714	-427.36
	0.15783	-426.93
	0.15854	-432.05
	0.15929	-435.77
	0.16004	-423.84
	0.16077	-427.55
	0.16153	-434.04
	0.16232	-436.78
	0.16315	-438.67
	0.16397	-437.62
	0.16476	-435.09
	0.16551	-430.53
	0.16624	-425.53
	0.16696	-428.55
	0.16771	-430.86
	0.16851	-434.18
	0.16932	-437.51
	0.17010	-424.97
	0.17086	-432.57
	0.17168	-431.98
	0.17252	-436.32
	0.17335	-434.80
	0.17419	-439.17
	0.17504	-433.04
	0.17589	-427.72
	0.17677	-427.52
	0.17767	-435.78
	0.17855	-437.10
	0.17945	-439.06
	0.18039	-442.53
	0.18134	-440.56
	0.18228	-440.06
	0.18322	-441.63
	0.18414	-437.97
	0.18501	-431.09
	0.18580	-423.05
	0.18650	-412.80
	0.18718	-424.91
	0.18793	-427.70
	0.18873	-431.79
	0.18952	-430.54
	0.19028	-422.80
	0.19105	-425.52
	0.19187	-430.66
	0.19266	-427.36
	0.19339	-419.90
	0.19409	-420.01
	0.19477	-408.39
	0.19541	-411.57
	0.19601	-408.11
	0.19661	-406.02
	0.19721	-405.71
	0.19782	-402.69
	0.19844	-406.53
	0.19908	-406.02
	0.19976	-412.28
	0.20050	-417.43
	0.20128	-422.11
	0.20208	-421.09
	0.20286	-418.58
	0.20362	-411.55
	0.20434	-411.35
	0.20504	-410.23
	0.20573	-410.78
	0.20641	-407.59
	0.20708	-404.57
	0.20775	-405.64
	0.20841	-399.73
	0.20905	-400.91
	0.20970	-402.12
	0.21034	-402.78
	0.21101	-406.27
	0.21169	-403.34
	0.21238	-407.72
	0.21307	-403.20
	0.21373	-399.75
	0.21439	-402.01
	0.21508	-406.30
	0.21583	-412.35
	0.21664	-418.00
	0.21748	-420.45
	0.21837	-422.68
	0.21934	-429.18
	0.22042	-437.22
	0.22157	-437.48
	0.22276	-440.76
	0.22395	-437.53
	0.22503	-425.86
	0.22603	-425.91
	0.22712	-436.18
	0.22825	-430.28
	0.22935	-433.92
	0.23047	-430.62
	0.23156	-428.80
	0.23260	-423.71
	0.23359	-420.26
	0.23453	-416.12
	0.23541	-411.20
	0.23625	-409.06
	0.23709	-409.96
	0.23792	-407.09
	0.23874	-406.63
	0.23952	-401.12
	0.24025	-396.51
	0.24092	-387.87
	0.24154	-381.26
	0.24214	-384.36
	0.24276	-385.35
	0.24341	-387.30
	0.24412	-399.38
	0.24494	-407.63
	0.24589	-417.21
	0.24697	-427.62
	0.24810	-423.59
	0.24925	-427.42
	0.25049	-434.25
	0.25180	-434.31
	0.25313	-435.16
	0.25444	-432.52
	0.25575	-434.48
	0.25704	-430.15
	0.25829	-427.73
	0.25957	-433.03
	0.26088	-431.53
	0.26221	-434.76
	0.26350	-426.80
	0.26475	-428.06
	0.26604	-431.98
	0.26742	-435.29
	0.26888	-438.37
	0.27039	-439.64
	0.27196	-442.44
	0.27356	-441.30
	0.27514	-438.86
	0.27670	-439.77
	0.27826	-439.33
	0.27975	-432.66
	0.28116	-431.21
	0.28255	-430.95
	0.28390	-426.63
	0.28519	-425.24
	0.28643	-420.35
	0.28763	-419.53
	0.28882	-418.91
	0.28996	-412.24
	0.29113	-419.88
	0.29244	-426.58
	0.29388	-432.52
	0.29535	-429.20
	0.29679	-427.91
	0.29828	-430.76
	0.29976	-426.19
	0.30123	-429.87
	0.30272	-426.73
	0.30415	-422.51
	0.30555	-420.07
	0.30705	-430.52
	0.30865	-429.03
	0.31023	-430.09
	0.31177	-425.82
	0.31322	-420.33
	0.31457	-414.11
	0.31583	-411.95
	0.31708	-410.13
	0.31840	-418.41
	0.31983	-423.24
	0.32125	-416.72
	0.32257	-411.47
	0.32378	-406.05
	0.32490	-399.26
	0.32597	-397.41
	0.32700	-394.31
	0.32801	-394.86
	0.32902	-393.33
	0.33001	-392.25
	0.33098	-390.83
	0.33196	-392.95
	0.33292	-387.97
	0.33380	-377.78
	0.33458	-369.07
	0.33533	-369.24
	0.33615	-378.23
	0.33710	-391.48
	0.33825	-403.29
	0.33960	-413.06
	0.34129	-430.03
	0.34336	-442.39
	0.34558	-439.96
	0.34774	-436.94
	0.34979	-432.98
	0.35174	-431.52
	0.35377	-436.45
	0.35594	-440.49
	0.35823	-441.79
	0.36050	-439.09
	0.36268	-434.65
	0.36477	-431.92
	0.36685	-432.18
	0.36894	-433.05
	0.37095	-426.45
	0.37283	-422.39
	0.37482	-432.15
	0.37691	-429.58
	0.37891	-426.19
	0.38077	-418.74
	0.38257	-419.59
	0.38439	-420.60
	0.38617	-414.89
	0.38808	-426.10
	0.39011	-422.48
	0.39200	-414.63
	0.39368	-404.32
	0.39520	-399.12
	0.39665	-396.35
	0.39808	-394.83
	0.39946	-390.92
	0.40079	-388.52
	0.40208	-385.26
	0.40336	-385.39
	0.40462	-382.96
	0.40587	-383.34
	0.40712	-382.98
	0.40839	-384.31
	0.40971	-386.61
	0.41110	-390.62
	0.41254	-391.78
	0.41403	-393.15
	0.41554	-392.29
	0.41710	-395.56
	0.41876	-400.21
	0.42053	-402.62
	0.42230	-397.19
	0.42430	-414.82
	0.42696	-434.75
	0.43019	-443.04
	0.43363	-442.95
	0.43693	-435.37
	0.44000	-432.53
	0.44306	-433.59
	0.44608	-429.91
	0.44921	-438.89
	0.45241	-433.10
	0.45552	-434.73
	0.45837	-418.64
	0.46096	-420.09
	0.46357	-420.98
	0.46611	-414.38
	0.46851	-411.36
	0.47079	-406.11
	0.47303	-406.39
	0.47534	-410.29
	0.47775	-411.30
	0.48023	-413.64
	0.48281	-416.90
	0.48546	-416.91
	0.48815	-417.94
	0.49100	-424.33
	0.49397	-423.04
	0.49686	-418.90
	0.49964	-416.41
	0.50234	-413.20
	0.50502	-413.56
	0.50781	-418.34
	0.51073	-419.35
	0.51373	-420.59
	0.51706	-431.16
	0.52064	-429.67
	0.52431	-433.02
	0.52810	-434.28
	0.53188	-432.21
	0.53542	-424.74
	0.53860	-416.07
	0.54166	-418.03
	0.54502	-427.17
	0.54847	-420.96
	0.55169	-415.23
	0.55466	-407.86
	0.55743	-405.20
	0.56013	-403.08
	0.56276	-400.84
	0.56538	-400.96
	0.56802	-401.98
	0.57067	-400.97
	0.57337	-403.50
	0.57615	-404.53
	0.57893	-402.97
	0.58170	-403.22
	0.58442	-398.73
	0.58746	-414.07
	0.59121	-427.39
	0.59518	-423.63
	0.59899	-421.74
	0.60281	-423.15
	0.60669	-421.89
	0.61034	-413.49
	0.61354	-402.79
	0.61645	-399.16
	0.61939	-403.16
	0.62250	-403.90
	0.62637	-425.56
	0.63133	-438.68
	0.63648	-432.07
	0.64138	-431.67
	0.64644	-435.95
	0.65186	-441.38
	0.65716	-432.93
	0.66198	-427.54
	0.66651	-424.38
	0.67096	-425.19
	0.67521	-416.91
	0.67909	-411.95
	0.68279	-409.67
	0.68630	-404.39
	0.68966	-403.41
	0.69304	-403.47
	0.69655	-406.20
	0.70015	-405.53
	0.70388	-410.34
	0.70783	-413.07
	0.71193	-413.19
	0.71650	-424.46
	0.72156	-428.37
	0.72649	-422.73
	0.73100	-415.60
	0.73533	-415.08
	0.73997	-433.65



Antarctic CO2 (ppmv)	point				off	0-11 ka = Taylor Dome (Indermuhle et al, 1999a);  11-27 ka = Taylor Dome (Smith et al, 1999);  27-60 kyr = Taylor Dome (Indermuhle et al, 1999b).  64-417 kyr = Vostok (Barnola et al., 2003);  417-649 kyr = Dome C (Siegenthaler, 2005).  Accessed from NCDC Paleoclimatology Program, and spliced together.
nopoints	line		180	300
	0.00039	282.9
	0.00049	279.7
	0.00057	276.1
	0.00067	277.4
	0.00074	280.7
	0.00083	280.8
	0.00092	282.2
	0.00102	283.6
	0.00113	283.5
	0.00122	285.0
	0.00132	284.0
	0.00141	279.4
	0.00151	278.4
	0.00162	278.3
	0.00175	282.9
	0.00185	278.5
	0.00197	279.4
	0.00208	279.4
	0.00220	278.2
	0.00230	281.4
	0.00245	279.4
	0.00258	276.7
	0.00274	278.2
	0.00284	275.9
	0.00291	276.9
	0.00302	277.3
	0.00312	277.3
	0.00322	274.1
	0.00332	275.4
	0.00344	274.4
	0.00353	276.1
	0.00365	275.8
	0.00376	276.9
	0.00389	274.7
	0.00399	273.4
	0.00412	274.6
	0.00424	274.1
	0.00437	271.6
	0.00448	273.1
	0.00458	271.2
	0.00476	272.9
	0.00491	270.2
	0.00503	273.5
	0.00519	271.6
	0.00533	271.9
	0.00549	272.4
	0.00562	270.4
	0.00577	270.9
	0.00594	269.9
	0.00611	268.3
	0.00627	266.0
	0.00644	266.5
	0.00659	266.2
	0.00675	266.4
	0.00691	265.1
	0.00707	264.6
	0.00723	263.0
	0.00734	262.1
	0.00745	261.0
	0.00761	261.3
	0.00788	260.3
	0.00815	259.9
	0.00851	261.0
	0.00879	261.1
	0.00899	264.1
	0.00956	262.0
	0.01016	265.8
	0.01069	266.6
	0.01110	265.4
	0.01151	264.0
	0.01159	266.9
	0.01169	260.4
	0.01188	251.4
	0.01232	247.6
	0.01261	254.1
	0.01327	241.6
	0.01343	237.1
	0.01454	237.6
	0.01500	244.7
	0.01566	229.4
	0.01647	219.4
	0.01652	219.4
	0.01697	218.0
	0.01801	189.7
	0.02015	190.5
	0.02147	189.1
	0.02174	189.0
	0.02235	187.7
	0.02367	195.2
	0.02389	194.1
	0.02456	196.1
	0.02524	194.0
	0.02577	191.1
	0.02647	193.5
	0.02704	196.8
	0.02753	199.6
	0.02803	199.1
	0.02848	200.4
	0.02927	200.2
	0.02973	200.1
	0.02995	201.6
	0.03020	200.9
	0.03056	203.6
	0.03104	205.3
	0.03258	208.8
	0.03283	213.0
	0.03308	211.3
	0.03325	212.6
	0.03380	213.6
	0.03397	210.8
	0.03413	209.9
	0.03429	210.6
	0.03472	210.3
	0.03483	207.8
	0.03506	205.7
	0.03526	198.6
	0.03543	196.4
	0.03587	197.5
	0.03634	198.2
	0.03673	201.4
	0.03688	198.9
	0.03747	201.4
	0.03770	201.6
	0.03791	202.2
	0.03811	201.9
	0.03919	199.9
	0.03968	201.7
	0.04002	205.0
	0.04055	210.0
	0.04085	214.0
	0.04126	216.2
	0.04181	214.6
	0.04219	215.7
	0.04267	210.6
	0.04344	206.6
	0.04465	203.1
	0.04524	200.0
	0.04555	199.1
	0.04636	202.1
	0.04687	206.9
	0.04738	206.9
	0.04838	212.3
	0.04883	214.3
	0.04919	218.0
	0.05035	216.9
	0.05148	211.7
	0.05214	210.8
	0.05297	208.0
	0.05378	211.5
	0.05539	218.2
	0.05708	220.4
	0.05775	215.0
	0.05830	214.9
	0.05886	212.5
	0.05983	204.6
	0.06156	197.4
	0.06207	203.6
	0.06369	195.4
	0.06570	191.4
	0.06688	195.0
	0.07285	227.4
	0.07536	229.2
	0.07900	217.1
	0.08006	221.8
	0.08286	231.0
	0.08493	241.1
	0.08573	236.4
	0.08632	228.1
	0.08718	214.2
	0.08805	217.0
	0.08936	208.0
	0.09169	224.3
	0.09246	228.4
	0.09535	232.1
	0.09984	225.9
	0.10083	230.9
	0.10183	236.9
	0.10337	228.2
	0.10521	236.9
	0.10620	230.7
	0.10831	238.2
	0.10899	245.7
	0.11025	251.3
	0.11146	256.8
	0.11258	266.3
	0.11347	261.4
	0.11408	274.6
	0.11474	273.3
	0.11618	262.5
	0.11752	267.6
	0.11840	273.8
	0.11927	272.0
	0.12000	265.2
	0.12065	277.7
	0.12196	272.2
	0.12261	276.3
	0.12382	268.7
	0.12386	266.6
	0.12431	266.3
	0.12457	279.8
	0.12472	273.0
	0.12488	277.2
	0.12575	273.8
	0.12602	267.1
	0.12648	262.5
	0.12681	262.6
	0.12745	275.4
	0.12781	275.6
	0.12830	274.1
	0.12840	287.1
	0.12865	286.8
	0.12901	282.7
	0.12941	264.1
	0.12976	263.4
	0.13011	257.9
	0.13017	259.0
	0.13099	264.6
	0.13166	245.0
	0.13179	240.4
	0.13207	228.9
	0.13282	223.5
	0.13333	224.0
	0.13337	220.3
	0.13364	210.6
	0.13421	208.9
	0.13436	203.7
	0.13500	204.6
	0.13517	200.4
	0.13527	198.0
	0.13568	198.1
	0.13598	201.8
	0.13610	200.7
	0.13636	202.5
	0.13666	195.9
	0.13674	201.1
	0.13738	194.4
	0.13769	193.4
	0.13799	194.2
	0.13823	190.2
	0.13945	192.3
	0.13985	196.5
	0.14126	195.6
	0.14131	196.5
	0.14236	190.4
	0.14544	197.0
	0.14916	203.0
	0.15030	191.9
	0.15042	188.9
	0.15185	200.6
	0.15447	189.0
	0.15530	185.5
	0.15571	187.5
	0.16049	204.4
	0.16104	196.5
	0.16300	191.6
	0.16352	190.1
	0.16434	186.7
	0.16528	183.8
	0.16630	196.5
	0.16987	197.9
	0.17260	197.8
	0.17462	196.0
	0.17544	190.3
	0.17603	189.4
	0.17627	190.1
	0.17855	207.7
	0.18078	213.2
	0.18162	217.7
	0.18245	198.1
	0.18336	199.8
	0.18506	203.5
	0.18720	210.7
	0.18934	231.4
	0.19106	231.5
	0.19159	220.3
	0.19263	218.0
	0.19512	226.5
	0.19563	220.1
	0.19757	226.4
	0.19844	241.2
	0.19903	242.6
	0.20221	251.0
	0.20319	239.1
	0.20428	247.7
	0.20515	244.4
	0.20544	231.9
	0.20572	232.2
	0.20612	228.7
	0.20667	226.3
	0.20703	229.4
	0.20741	231.4
	0.20799	238.2
	0.20818	237.2
	0.20879	230.0
	0.20907	240.5
	0.20941	242.2
	0.21002	244.6
	0.21023	243.9
	0.21083	247.3
	0.21101	252.0
	0.21148	246.9
	0.21193	239.5
	0.21228	257.4
	0.21301	243.4
	0.21415	251.2
	0.21504	241.4
	0.21559	240.3
	0.21588	242.7
	0.21646	247.5
	0.21701	251.7
	0.21727	251.2
	0.21757	245.3
	0.21768	245.4
	0.21834	240.5
	0.21968	214.1
	0.21968	212.2
	0.22004	216.1
	0.22018	216.2
	0.22076	203.7
	0.22076	207.2
	0.22105	208.9
	0.22161	205.7
	0.22296	203.4
	0.22345	215.7
	0.22463	236.9
	0.22530	234.5
	0.22551	233.1
	0.22589	224.5
	0.22671	232.4
	0.22738	233.9
	0.22784	241.7
	0.23070	245.2
	0.23138	252.1
	0.23199	241.4
	0.23257	247.4
	0.23310	243.1
	0.23365	239.2
	0.23413	245.7
	0.23447	245.9
	0.23478	247.4
	0.23521	252.9
	0.23624	259.8
	0.23685	263.2
	0.23783	279.0
	0.23820	280.3
	0.23894	263.8
	0.23925	252.4
	0.23955	249.9
	0.23987	236.7
	0.24020	230.4
	0.24058	219.4
	0.24207	214.7
	0.24365	200.2
	0.24422	213.9
	0.24486	195.4
	0.24548	196.7
	0.24609	195.4
	0.24745	199.0
	0.24809	201.9
	0.24898	204.0
	0.25046	203.9
	0.25152	209.7
	0.25217	205.7
	0.25296	208.9
	0.25388	214.7
	0.25523	228.2
	0.25605	199.9
	0.25650	211.7
	0.25725	188.7
	0.25779	187.2
	0.25848	194.2
	0.25923	198.9
	0.25996	184.7
	0.26075	190.4
	0.26160	193.9
	0.26241	194.2
	0.26321	198.4
	0.26405	193.2
	0.26483	202.2
	0.26570	204.5
	0.26649	211.0
	0.26743	215.4
	0.26868	223.7
	0.27068	231.4
	0.27228	228.0
	0.27301	226.4
	0.27391	231.4
	0.27445	230.4
	0.27522	231.0
	0.27730	234.9
	0.27793	220.4
	0.27860	217.2
	0.27954	207.7
	0.28036	206.0
	0.28120	206.7
	0.28230	212.7
	0.28349	213.2
	0.28530	217.1
	0.28622	224.4
	0.28710	231.0
	0.28785	236.2
	0.28849	239.0
	0.28943	236.0
	0.29057	240.2
	0.29177	240.7
	0.29247	250.2
	0.29300	248.6
	0.29368	244.9
	0.29462	225.9
	0.29585	227.9
	0.29638	226.2
	0.29713	233.2
	0.29805	237.9
	0.29902	239.0
	0.29988	241.9
	0.30065	251.7
	0.30150	256.8
	0.30246	257.2
	0.30333	246.9
	0.30395	272.7
	0.30459	251.7
	0.30530	245.2
	0.30531	244.7
	0.30713	255.9
	0.30810	249.2
	0.31004	257.2
	0.31004	256.3
	0.31093	260.4
	0.31177	260.3
	0.31267	260.6
	0.31349	266.3
	0.31437	264.0
	0.31514	266.2
	0.31594	270.2
	0.31668	271.9
	0.31745	275.2
	0.31898	265.0
	0.31975	271.8
	0.32038	272.7
	0.32139	273.2
	0.32211	282.4
	0.32258	289.2
	0.32283	288.4
	0.32349	298.7
	0.32419	278.2
	0.32499	285.8
	0.32553	278.7
	0.32624	270.5
	0.32711	255.7
	0.32810	241.9
	0.32927	239.7
	0.33021	234.2
	0.33229	250.2
	0.33363	200.7
	0.33529	205.2
	0.33697	204.9
	0.33828	211.9
	0.34017	220.4
	0.34300	221.2
	0.34474	216.2
	0.34611	209.5
	0.34761	209.2
	0.35077	193.0
	0.35241	186.2
	0.35437	185.8
	0.35684	201.2
	0.35969	206.4
	0.36277	201.9
	0.36450	200.0
	0.36622	214.7
	0.36812	224.6
	0.36956	229.7
	0.37301	227.0
	0.37456	240.0
	0.37676	239.1
	0.37819	246.9
	0.37963	245.9
	0.38350	258.1
	0.38491	264.7
	0.38658	259.3
	0.39059	255.2
	0.39245	250.2
	0.39463	266.3
	0.39671	274.7
	0.39855	277.1
	0.40039	278.0
	0.40584	279.7
	0.40902	281.2
	0.40902	283.7
	0.41083	276.3
	0.41409	285.5
	0.41543	286.9
	0.41716	277.6
	0.41740	273.8
	0.41833	268.6
	0.41883	266.4
	0.41938	270.6
	0.42040	267.7
	0.42091	268.3
	0.42136	270.8
	0.42169	270.0
	0.42194	265.4
	0.42226	255.3
	0.42274	252.1
	0.42323	248.2
	0.42343	242.5
	0.42443	219.7
	0.42500	227.2
	0.42583	211.5
	0.42610	207.6
	0.42696	209.8
	0.42793	207.5
	0.42895	200.3
	0.42995	201.7
	0.43093	201.3
	0.43194	202.0
	0.43297	199.1
	0.43441	201.1
	0.43544	203.5
	0.43644	208.1
	0.43729	201.7
	0.43814	201.2
	0.43901	204.9
	0.43992	201.9
	0.44078	198.4
	0.44166	193.3
	0.44256	192.5
	0.44308	199.1
	0.44345	204.3
	0.44396	203.3
	0.44433	208.3
	0.44520	202.4
	0.44600	195.5
	0.44685	190.7
	0.44777	194.4
	0.44874	199.9
	0.44939	205.2
	0.44973	210.0
	0.45068	208.1
	0.45158	204.4
	0.45246	203.4
	0.45342	205.5
	0.45401	206.5
	0.45441	215.5
	0.45497	218.7
	0.45537	229.2
	0.45591	232.7
	0.45628	243.7
	0.45686	243.9
	0.45712	245.6
	0.45786	241.2
	0.45856	233.1
	0.45934	232.8
	0.46019	236.6
	0.46098	239.1
	0.46137	236.5
	0.46166	231.3
	0.46207	220.8
	0.46237	218.8
	0.46317	223.8
	0.46397	223.4
	0.46473	227.3
	0.46545	231.4
	0.46616	231.4
	0.46686	231.2
	0.46757	233.0
	0.46828	232.9
	0.46897	231.3
	0.46963	237.1
	0.47028	242.0
	0.47064	240.9
	0.47091	252.8
	0.47132	249.3
	0.47153	242.6
	0.47215	243.3
	0.47278	246.7
	0.47343	243.7
	0.47410	239.7
	0.47477	239.1
	0.47546	238.3
	0.47615	238.5
	0.47685	237.6
	0.47753	236.4
	0.47823	236.5
	0.47893	232.8
	0.47965	230.6
	0.48036	230.8
	0.48110	228.2
	0.48185	230.8
	0.48261	231.2
	0.48338	232.0
	0.48413	232.2
	0.48488	234.1
	0.48562	233.9
	0.48639	235.5
	0.48718	236.0
	0.48794	238.2
	0.48870	237.0
	0.48953	240.3
	0.49039	233.4
	0.49127	236.4
	0.49213	235.2
	0.49298	242.0
	0.49384	238.2
	0.49470	239.2
	0.49556	241.5
	0.49641	243.0
	0.49723	247.2
	0.49804	246.2
	0.49886	245.5
	0.49964	245.3
	0.50042	247.7
	0.50120	245.5
	0.50197	243.5
	0.50424	241.9
	0.50499	236.8
	0.50575	235.8
	0.50656	233.7
	0.50738	230.3
	0.50822	227.8
	0.50907	224.7
	0.50992	222.7
	0.51074	221.2
	0.51158	220.3
	0.51238	220.7
	0.51284	214.5
	0.51318	211.4
	0.51368	204.4
	0.51404	200.0
	0.51465	195.1
	0.51498	193.8
	0.51555	190.5
	0.51597	199.8
	0.51700	199.4
	0.51806	205.0
	0.51910	206.4
	0.52013	212.9
	0.52115	211.2
	0.52218	205.0
	0.52326	203.6
	0.52434	208.1
	0.52539	210.3
	0.52648	209.6
	0.52757	209.7
	0.52874	204.6
	0.52992	202.5
	0.53059	208.8
	0.53106	213.6
	0.53218	215.2
	0.53322	219.9
	0.53418	221.7
	0.53477	222.3
	0.53517	226.3
	0.53586	222.1
	0.53622	220.3
	0.53720	223.6
	0.53811	224.3
	0.53895	226.7
	0.53973	233.9
	0.54053	241.0
	0.54102	243.0
	0.54138	249.1
	0.54191	244.0
	0.54229	250.5
	0.54295	245.6
	0.54327	240.4
	0.54428	238.1
	0.54538	234.5
	0.54601	229.7
	0.54644	230.2
	0.54746	230.3
	0.54845	228.3
	0.54941	231.6
	0.55036	231.9
	0.55129	234.6
	0.55204	234.1
	0.55310	240.1
	0.55393	242.3
	0.55474	245.7
	0.55556	245.8
	0.55636	247.6
	0.55717	251.4
	0.55796	252.4
	0.55873	252.6
	0.55951	251.4
	0.56029	253.7
	0.56105	254.3
	0.56181	253.9
	0.56255	254.5
	0.56330	253.2
	0.56403	253.9
	0.56481	252.8
	0.56556	253.0
	0.56631	250.2
	0.56708	251.3
	0.56784	250.0
	0.56861	251.3
	0.56936	251.8
	0.57012	251.8
	0.57087	249.6
	0.57164	251.6
	0.57242	250.3
	0.57320	246.3
	0.57399	247.7
	0.57480	249.2
	0.57561	248.7
	0.57643	251.8
	0.57723	251.9
	0.57801	252.1
	0.57880	248.9
	0.57960	252.5
	0.58042	252.9
	0.58124	251.3
	0.58205	251.3
	0.58281	251.1
	0.58355	249.1
	0.58426	252.9
	0.58498	251.5
	0.58549	244.1
	0.58575	243.8
	0.58623	236.2
	0.58659	230.3
	0.58712	225.2
	0.58752	219.4
	0.58811	215.4
	0.58857	209.9
	0.58932	206.7
	0.58973	210.6
	0.59281	224.0
	0.59334	226.0
	0.59415	234.4
	0.59457	238.8
	0.59522	246.3
	0.59569	250.2
	0.59627	248.1
	0.59669	243.6
	0.59720	237.4
	0.59847	225.7
	0.59885	229.4
	0.59950	233.2
	0.59989	238.1
	0.60053	238.0
	0.60095	232.9
	0.60152	221.2
	0.60197	216.4
	0.60271	216.3
	0.60312	219.0
	0.60383	226.0
	0.60434	229.4
	0.60554	232.5
	0.60669	237.9
	0.60781	239.1
	0.60889	244.5
	0.60992	248.5
	0.61096	254.6
	0.61190	259.2
	0.61281	257.7
	0.61366	259.6
	0.61450	258.0
	0.61533	256.0
	0.61613	252.5
	0.61694	252.4
	0.61772	252.3
	0.61859	247.9
	0.61946	245.4
	0.62032	243.0
	0.62117	238.6
	0.62204	237.3
	0.62255	234.3
	0.62290	227.8
	0.62339	214.9
	0.62375	205.0
	0.62434	198.7
	0.62467	199.9
	0.62544	199.5
	0.62583	195.6
	0.62679	192.1
	0.62729	193.9
	0.62814	193.0
	0.62882	194.3
	0.62982	187.7
	0.63039	189.1
	0.63142	190.2
	0.63196	190.4
	0.63296	194.1
	0.63353	194.6
	0.63441	188.6
	0.63501	190.5
	0.63597	192.1
	0.63644	194.8
	0.63737	187.8
	0.63785	192.0
	0.63877	185.8
	0.63924	185.3
	0.64007	191.3
	0.64067	193.2
	0.64156	198.4
	0.64206	198.7
	0.64293	191.3
	0.64339	189.2
	0.64427	182.4
	0.64479	183.9
	0.64565	186.6
	0.64629	189.8
	0.64729	187.8
	0.64784	189.0
	0.64885	189.1
	0.64938	185.8



