EON, Era, System, Series, Stages | Age (Ma) GTS 2004 |
Est. ±Ma |
Derivation of age | Principal correlative events | GSSP and location | Status | Publication |
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PHANEROZOIC Eon | |||||||
Cenozoic Era | |||||||
Neogene System | |||||||
QUATERNARY Sub-System | 2.588 | Quaternary is a formal Sub-System (Sub-Era) of the Cenozoic time scale. It is the interval of oscillating climatic extremes (glacial and interglacial episodes) that was initiated at about 2.6 Ma (set equal to base of Gelasian stage), therefore it encompasses the Holocene and Pleistocene epochs and the late Pliocene. | Equivalent to GSSP of Gelasian at Monte San Nicola, Gela, Sicily, Italy. Correlates with Marine Isotopic stage 103, and base of magnetic polarity chronozone C2r (Matuyama) | ICS formal recommendation to INQUA and ICS; Sept 2005. | Proposal in Episodes 28 (2), p.118-120, 2005 | ||
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base Holocene | 0.011784 | 0.00 | Annual layer counting in ice core ("ka" is relative to AD2000); counting uncertainy is 69 years | 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 | GSSP anticipated in 2005 | ||
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base upper Pleistocene Subseries | 0.126 | 0.00 | Astronomical cycles in sediments | base of the Eemian interglacial stage (= base of marine isotope stage 5e) before final glacial episode of Pleistocene | Amsterdam-Terminal borehole (63.5 m below surface; 52°22'45"N; 4°54'52"E), Netherlands | GSSP anticipated in 2006 | |
base middle Pleistocene Subseries | 0.781 | 0.00 | Astronomical cycles in sediments | Brunhes-Matuyama magnetic reversal | Candidate sections in Italy (Montalbano Jorica or Valle di Manche) and Japan (Chiba) | GSSP anticipated in 2007 | |
base Pleistocene Series | 1.806 | 0.00 | Astronomical cycles in sediments | Just above top of magnetic polarity chronozone C2n (Olduvai) and the extinction level of calcareous nannofossil Discoaster brouweri (base Zone CN13). Above are lowest occurrence of calcareous nannofossil medium Gephyrocapsa spp. and extinction level of planktonic foraminifer Globigerinoides extremus. | Top of sapropel layer 'e', Vrica section, Calabria, Italy | Ratified 1985 | Episodes 8 (2), p.116-120, 1985 |
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base Gelasian Stage | 2.588 | 0.00 | Astronomical cycles in sediments | Isotopic stage 103, base of magnetic polarity chronozone C2r (Matuyama). Above are extinction levels of calcareous nannofossil Discoaster pentaradiatus and D. surculus (base Zone CN12c). | Midpoint of sapropelic Nicola Bed ("A5"), Monte San Nicola, Gela, Sicily, Italy | Ratified 1996 | Episodes 21 (2), p.82-87, 1998 |
base Piacenzian Stage | 3.600 | 0.00 | Astronomical cycles in sediments | Base of magnetic polarity chronozone C2An (Gauss); extinction levels of planktonic foraminifers Globorotalia margaritae (base Zone PL3) and Pulleniatina primalis. | Base of beige layer of carbonate cycle 77, Punta Piccola, Sicily, Italy | Ratified 1997 | Episodes 21 (2), p.88-93, 1998 |
base Zanclean Stage, base Pliocene Series | 5.332 | 0.00 | Astronomical cycles in sediments | Top of magnetic polarity chronozone C3r, ~100 kyr before Thvera normal-polarity subchronozone (C3n.4n). Calcareous nannofossils -- near extinction level of Triquetrorhabdulus rugosus (base Zone CN10b) and the lowest occurrence of Ceratolithus acutus. | Base of Trubi Fm (base of carbonate cycle 1), Eraclea Minoa, Sicily, Italy | Ratified 2000 | Episodes 23 (3), p.179-187, 2000 |
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base Messinian Stage | 7.246 | 0.00 | Astronomical cycles in sediments | Astrochronology age of 7.251 Ma; middle of magnetic polarity chronozone C3Br.1r; lowest regular occurrence of the Globorotalia conomiozea planktonic foraminifer group. | Base of red layer of carbonate cycle 15, Oued Akrech, Rabat, Morocco | Ratified 2000 | Episodes 23 (3), p. 172-178, 2000 |
base Tortonian Stage | 11.608 | 0.00 | Astronomical cycles in sediments | Last Common Occurrences of the calcareous nannofossil Discoaster kugleri and the planktonic foraminifer Globigerinoides subquadratus. Associated with the short normal-polarity subchron C5r.2n. | Midpoint of sapropel 76, Monte dei Corvi beach section, Ancona, Italy | Ratified 2003 | Episodes 28 (1), p.6-17, 2005 |
base Serravallian Stage | 13.65 | 0.00 | Astronomical cycles in sediments | Near lowest occurrence of nannofossil Sphenolithus heteromorphus, within magnetic polarity chronozone C5ABr, and Mi3b isotopic event (global cooling episode) | GSSP anticipated in 2006 | ||
base Langhian Stage | 15.97 | 0.00 | Calibrated magnetic anomaly scale | Near first occurrence of planktonic foraminifer Praeorbulina glomerosa and top of magnetic polarity chronozone C5Cn.1n | GSSP anticipated in 2008 | ||
base Burdigalian Stage | 20.43 | 0.00 | Calibrated magnetic anomaly scale | Near lowest occurrence of planktonic foraminifer Globigerinoides altiaperturus or near top of magnetic polarity chronozone C6An | Guide event is undecided. GSSP anticipated in 2008 | ||
base Aquitanian Stage, base Miocene Series, base Neogene System | 23.03 | 0.00 | Astronomical cycles in sediments | Base of magnetic polarity chronozone C6Cn.2n; lowest occurrence of planktonic foraminifer Paragloborotalia kugleri; near extinction of calcareous nannofossil Reticulofenestra bisecta (base Zone NN1). | 35 m from top of Lemme-Carrosio section, Carrosio village, north of Genoa, Italy | Ratified 1996 | Episodes 20 (1),p. 23-28, 1997 |
Paleogene System | |||||||
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base Chattian Stage | 28.4 | 0.1 | Calibrated magnetic anomaly scale relative to base-Miocene and C24n. Arbitrary 100 kyr uncertainty assigned. | Potentially extinction of planktonic foraminifer Chiloguembelina (base Foram Zone P21b); or an isotopic/climatic event | Possibly Monte Cagnero (Umbria-Marche region, Italy) | GSSP anticipated in 2006 | |
base Rupelian Stage, base Oligocene Series | 33.9 | 0.1 | Calibrated magnetic anomaly scale relative to base-Miocene and C24n. | Planktonic foraminifer, extinction of Hantkenina | Base of marl bed at 19m above base of Massignano quarry, Ancona, Italy | Ratified 1992 | Episodes 16 (3), p.379-382, 1993 |
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base Priabonian Stage | 37.2 | 0.1 | Calibrated magnetic anomaly scale relative to base-Miocene and C24n | Near lowest occurrence of calcareous nannofossil Chiasmolithus oamaruensis (base Zone NP18) | Tiziano Bed, Alano section (Piave River; Veneto Prealps, Belluno province, N. Italy) | ||
base Bartonian Stage | 40.4 | 0.2 | Calibrated magnetic anomaly scale relative to base-Miocene and C24n | Near extinction of calcareous nannofossil Reticulofenestra reticulata | |||
base Lutetian Stage | 48.6 | 0.2 | Calibrated magnetic anomaly scale relative to base-Miocene and C24n | Planktonic foraminifer, lowest occurrence of Hantkenina | Leading candidate is Agost section, Murcia province, Betic Cordilleras, Spain | GSSP anticipated in 2007 | |
base Ypresian Stage, base Eocene Series | 55.8 | 0.2 | Astronomical cycles in sediments scaled from base-Paleocene | Base of negative carbon-isotope excursion | Dababiya Section near Luxor, Egypt | Ratified 2003 | Micropaleontology v.49 (Suppl. 1), 2003. Episodes article in preparation |
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base Thanetian Stage | 58.7 | 0.2 | Astronomical cycles in sediments scaled from base Paleocene, using base of magnetic polarity chronozone C26n. Arbitrary 0.1 (2 precession cycles, plus the base-Paleogene radiometric) uncertainty assigned to all estimates. | Magnetic polarity chronozone, base of C26n | Leading candidate is Zumaya section, northern Spain | GSSP anticipated in 2007 | |
base Selandian Stage | 61.7 | 0.2 | Astronomical cycles in sediments scaled from base Paleocene, using magnetic polarity chronozone placement of C27n.9 | Undecided; 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) | Leading candidate is Zumaya section, northern Spain | Guide event is undecided. GSSP anticipated in 2007 | |
base Danian Stage, base Paleogene System, base Cenozoic | 65.5 | 0.3 | Ar-Ar and U-Pb age agreement | Iridium geochemical anomaly. Associated with a major extinction horizon (foraminifers, calcareous nannofossils, dinosaurs, etc.); | Base of boundary clay, El Kef, Tunisia (but deterioration may require assigning a replacement section) | Ratified 1991 | |
Mesozoic Era | |||||||
Cretaceous System | |||||||
Most Cretaceous substages also have recommended GSSP criteria | |||||||
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base Maastrichtian Stage | 70.6 | 0.6 | Estimated placement relative to Ar-Ar calibrated Sr-curve | Mean of 12 biostratigraphic criteria of equal importance. Closely above is lowest occurrence of ammonite Pachydiscus neubergicus. Boreal proxy is lowest occurrence of belemnite Belemnella lanceolata. | 115.2 m level in Grande Carrière quarry, Tercis-les-Bains, Landes province, SW France | Ratified 2001 | Episodes 24 (4), p.229-238, 2001; Odin (ed.) IUGS Spec. Publ. Series, v.36, Elsevier, 910pp. |
base Campanian Stage | 83.5 | 0.7 | Spline fit of Ar-Ar ages and ammonite zones. | Crinoid, extinction of Marsupites testudinarius | Leading candidates are in southern England and in Texas | ||
base Santonian Stage | 85.8 | 0.7 | Spline fit of Ar-Ar ages and ammonite zones. | Inoceramid bivalve, lowest occurrence of Cladoceramus undulatoplicatus | Leading candidates are in Spain, England and Texas | ||
base Coniacian Stage | 89.3 | 1.0 | Spline fit of Ar-Ar ages and ammonite zones. | Inoceramid bivalve, lowest occurrence of Cremnoceramus rotundatus (sensu Tröger non Fiege) | Base of Bed MK47, Salzgitter-Salder Quarry, SW of Hannover, Lower Saxony, northern Germany | GSSP anticipated in 2006 | |
base Turonian Stage | 93.5 | 0.8 | Spline fit of Ar-Ar ages and ammonite zones | Ammonite, lowest occurrence of Watinoceras devonense | Base of Bed 120, Rock Canyon Anticline, east of Pueblo, Colorado, west-central USA | Ratified 2003 | Episodes 28(1), p. 93-104, 2005 |
base Cenomanian Stage | 99.6 | 0.9 | Spline fit of Ar-Ar ages and ammonite zones, plus monitor standard correction. Then cycle stratigraphy to place foraminifer datum relative to ammonite zonation. | Planktonic foraminifer, lowest occurrence of Rotalipora globotruncanoides | 36 m below top of Marnes Bleues Formation, Mont Risou, Rosans, Haute-Alpes, SE France | Ratified 2002 | Episodes 27 (1), p.21-32, 2004 |
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base Albian Stage | 112.0 | 1.0 | Cycle-stratigraphy of FAD of P. columnata relative to base of Cenomanian, with large uncertainty due to lack of GSSP criteria | Candidates include: (1) calcareous nannofossil, lowest occurrence of Praediscosphaera columnata (= P. cretacea of some earlier studies), (2) carbon-isotope excursion (black-shale episode), (3) ammonite | Guide event is undecided. GSSP anticipated in 2008 | ||
base Aptian Stage | 125.0 | 1.0 | Base of M0r, as recomputed from Ar-Ar age from MIT guyot | Magnetic polarity chronozone, base of M0r; near base of Paradeshayesites oglanlensis ammonite zone | Leading candidate is Gorgo a Cerbara, Piobbico, Umbria-Marche, central Italy | ||
base Barremian Stage | 130.0 | 1.5 | Pacific spreading model for magnetic anomaly ages (variable rate), using placement at M5n.8. | Ammonite, lowest occurrence of Spitidiscus hugii Spitidiscus vandeckii group | Leading candidate is Río Argos near Caravaca, Murcia province, Spain | ||
base Hauterivian Stage | 136.4 | 2.0 | Pacific spreading model for magnetic anomaly ages (variable rate), using placement at base M11n | Ammonite, lowest occurrence of genus Acanthodiscus (especially A. radiatus) | Leading candidate is La Charce village, Drôme province, southeast France | ||
base Valanginian Stage | 140.2 | 3.0 | Pacific spreading model for magnetic anomaly ages (variable rate), using placement at M14r.3 (base T. pertransiens). | Calpionellid, lowest occurrence of Calpionellites darderi (base of Calpionellid Zone E); followed by the lowest occurrence of ammonite Thurmanniceras pertransiens | Leading candidates are near Montbrun-les-Bains (Drôme province, SE France) and Cañada Luenga (Betic Cordillera, S. Spain) | ||
base Berriasian Stage, base Cretaceous System | 145.5 | 4.0 | Pacific spreading model for magnetic anomaly ages (variable rate), assigning to base of Berriasella jacobi zone (M19n.2n.55) | Maybe near lowest occurrence of ammonite Berriasella jacobi | |||
Jurassic System | |||||||
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base Tithonian Stage | 150.8 | 4.0 | Pacific spreading model for magnetic anomaly ages (variable rate), assigning to base M22An | Near base of Hybonoticeras hybonotum ammonite zone and lowest occurrence of Gravesia genus, and the base of magnetic polarity chronozone M22An | Guide event is undecided. GSSP anticipated in 2007 | ||
base Kimmeridgian Stage | 155.7 | 4.0 | Pacific spreading model for magnetic anomaly ages (variable rate), assigning to base M26r.2 (Boreal ammonite definition) | Ammonite, near base of Pictonia baylei ammonite zone of Boreal realm | Candidate is Flodigarry (Isle of Skye, NW Scotland) | GSSP anticipated in 2006 | |
base Oxfordian Stage | 161.2 | 4.0 | Pacific spreading model for magnetic anomaly ages (variable rate), assigning to base M36An | Ammonite, Brightia thuouxensis Horizon at base of the Cardioceras scarburgense Subzone (Quenstedtoceras mariae Zone) | Leading candidates are Savouron (Provence province, SE France) and Redcliffe Point (Dorset, SW England) | GSSP anticipated in 2006 | |
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base Callovian Stage | 164.7 | 4.0 | Equal subzones scale Bajo-Bath-Callov | Ammonite, lowest occurrence of the genus Kepplerites (Kosmoceratidae) (defines base of Macrocephalites herveyi Zone in sub-Boreal province of Great Britain to southwest Germany) | Leading candidate is Pfeffingen, Swabian Alb, SW Germany | GSSP anticipated in 2006 | |
base Bathonian Stage | 167.7 | 3.5 | Equal subzones scale Bajo-Bath-Callov | Ammonite, lowest occurrence of Parkinsonia (G.) convergens (defines base of Zigzagiceras zigzag Zone) | |||
base Bajocian Stage | 171.6 | 3.0 | Equal subzones scale Bajo-Bath-Callov | Ammonite, lowest occurrence of the genus Hyperlioceras (defines base of the Hyperlioceras discites Zone) | Base of Bed AB11, 77.8 m above base of Murtinheira section, Cabo Mondego, western Portugal | Ratified 1996 | Episodes 20 (1), p.16-22, 1997 |
base Aalenian Stage | 175.6 | 2.0 | Duration of Aalenian-Toarcian from cycle stratigraphy | Ammonite, lowest occurrence of Leioceras genus | base of Bed FZ107, Fuentelsalz, central Spain | Ratified 2000 | Episodes 24 (3), p.166-175, 2001 |
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base Toarcian Stage | 183.0 | 1.5 | Duration of Aalenian-Toarcian from cycle stratigraphy | Ammonite, near lowest occurrence of a diversified Eodactylites ammonite fauna; correlates with the NW European Paltus horizon. | GSSP anticipated in 2006 | ||
base Pliensbachian Stage | 189.6 | 1.5 | Cycle-scaled linear Sr trend | Ammonite, lowest occurrences of Bifericeras donovani and of genera Apoderoceras ((defines base of Phricodoceras taylori subzone of Uptonia jamesoni ammonite zone) | Base of Bed 73b, Wine Haven section, Robin Hood's Bay, Yorkshire, England, UK | Ratified 2005 | Proposal in Eclogae Geol. Helv. 96, p.275-297, 2003. Episodes article in preparation |
base Sinemurian Stage | 196.5 | 1.0 | Cycle-scaled linear Sr trend | Ammonite, lowest occurrence of arietitid genera Vermiceras and Metophioceras | 0.9 m above base of Bed 145, East Quantoxhead, Watchet, West Somerset, SW England, UK | Ratified 2000 | Episodes 25 (1), p. 22-26, 2002 |
base Hettangian Stage, base Jurassic System | 199.6 | 0.6 | U-Pb age just below proposed GSSP for base-Jurassic | Near lowest occurrence of smooth Psiloceras planorbis ammonite group | Guide event is undecided. GSSP anticipated in 2007 | ||
Triassic System | |||||||
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base Rhaetian Stage | 203.6 | 1.5 | Magnetostratigraphic correlation to cycle-scaled Newark magnetic polarity pattern | Near lowest occurrence of ammonite Cochlocera, conodonts Misikella spp. and Epigondolella mosheri, and radiolarian Proparvicingula moniliformis | Key sections in Austria, British Columbia (Canada), and Turkey | Guide event is undecided. GSSP anticipated in 2008 | |
base Norian Stage | 216.5 | 2.0 | Magnetostratigraphic correlation to cycle-scaled Newark magnetic polarity pattern | Base of Klamathites macrolobatus or Stikinoceras kerri ammonoid zones and the Metapolygnathus communisti or M. primitius conodont zones | Leading candidates are in British Columbia (Canada), Sicily (Italy), and possibly Slovakia, Turkey (Antalya Taurus) and Oman. | Guide event is undecided. GSSP anticipated in 2008 | |
base Carnian Stage | 228.0 | 2.0 | Magnetostratigraphic correlation to cycle-scaled Newark magnetic polarity pattern | Near first occurrence of the ammonoids Daxatina or Trachyceras, and of the conodont Metapolygnathus polygnathiformis | Candidate section at Prati di Stuores, Dolomites, northern Italy. Important reference sections in Spiti (India) and New Pass, Nevada (USA). | Guide event is undecided. GSSP anticipated in 2007 | |
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base Ladinian Stage | 237.0 | 2.0 | U-Pb array by Mundil et al. on levels near Nevadites (= Secedensis) ammonite zone in Dolomites, plus placement relative to magnetostratigraphy corrlations to cycle-scaled Newark magnetic polarity pattern | Ammonoid, lowest occurrence of the Eoprotrachyceras curionii (base of the E. curionii zone; onset of the Trachyceratidae family. Above lowest Neogondolella praehungarica conodont | Top of "Chiesense groove", 5m above base of Buchenstein Beds, Caffaro river bed, Bagolino (Brescia province, N. Italy) | Ratified 2005 | |
base Anisian Stage | 245.0 | 1.5 | Proportional subzonal scaling | Conodont, lowest occurrences of Chiosella timorensis | Candidate section at Desli Caira (Dobrogea, Romania); significant sections in Guizhou Province (China) and South Primorye (Russia) | GSSP anticipated in 2007 | |
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base Olenekian Stage | 249.7 | 0.7 | Composite standard from conodonts scaled to base-Anisian and base-Triassic | Conodont, lowest occurrence of Neospathodus waageni; near lowest occurrence of Flemingites and Euflemingites ammonite genera | Chaohu (Anhui province, E. China). Important sections in Spiti | GSSP anticipated in 2006 | |
base Induan Stage, base Triassic System, base Mesozoic | 251.0 | 0.4 | U-Pb ages bracket GSSP (Bowring et al., 1998) | Conodont, lowest occurrence of Hindeodus parvus; termination of major negative carbon-isotope excursion. About 1 myr after peak of Late Permian extinctions. | Base of Bed 27c, Meishan, Zhejiang, China | Ratified 2001 | Episodes 24 (2), p.102-114, 2001 |
Paleozoic Era | |||||||
Permian System | |||||||
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base Changhsingian Stage | 253.8 | 0.7 | Permian-Carboniferous time scale is derived from calibrating a master composite section to selected radiometric ages | Conodont, near lowest occurrence of conodont Clarkina wangi | Base of Bed 4a-2, 88 cm above base of Changxing Limestone, Meishan D section (Zhejiang province, E. China) | ||
base Wuchiapingian Stage | 260.4 | 0.7 | Conodont, lowest occurrence of Clarkina postbitteri postbitteri | Ratified 2004 | |||
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base Capitanian Stage | 265.8 | 0.7 | Conodont, lowest occurrence of Jinogondolella postserrata | 4.5 m above base of Pinery Limestone Member, Nipple Hill, SE Guadalupe Mountains, Texas, USA | Ratified 2001 | Episodes article in preparation | |
base Wordian Stage | 268.0 | 0.7 | Conodont, lowest occurrence of Jinogondolella aserrata | 7.6 m above base of Getaway Ledge outcrop, Guadalupe Pass, SE Guadalupe Mountains, Texas, USA | Ratified 2001 | Episodes article in preparation | |
base Roadian Stage | 270.6 | 0.7 | Conodont, lowest occurrence of Jinogondolella nanginkensis | 42.7 m above base of Cutoff Formation, Stratotype Canyon, southern Guadalupe Mountains, Texas, USA | Ratified 2001 | Episodes article in preparation | |
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base Kungurian Stage | 275.6 | 0.7 | Near lowest occurrence of conodont Neostreptognathus pnevi - N. exculptus | Leading candidates are in southern Ural Mtns. | |||
base Artinskian Stage | 284.4 | 0.7 | Conodont, lowest occurrence of conodont Sweetognathus whitei | Leading candidates are in southern Ural Mtns. | |||
base Sakmarian Stage | 294.6 | 0.8 | Conodont, near lowest occurrence of conodont Sweetognathus merrelli | Leading candidate is at Kondurovsky, Orenburg Province, Russia. | |||
base Asselian Stage, base Cisuralian Series, base Permian System | 299.0 | 0.8 | Conodont, lowest occurrence of Streptognathodus isolatus within the S. "wabaunsensis" conodont chronocline. 6 m higher is lowest fusilinid foraminifer Sphaeroschwagerina vulgaris aktjubensis | 27 m above base of Bed 19, Aidaralash Creek, Aktöbe, southern Ural Mountains, northern Kazakhstan | Ratified, 1996 | Episodes 21 (1), p.11-18, 1998 | |
Carboniferous System | |||||||
Pennsylvanian Subsystem (series classification approved in 2004) | |||||||
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base Gzhelian Stage | 303.9 | 0.9 | Near 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. | Guide event is undecided. GSSP anticipated in 2007 | |||
base Kasimovian Stage | 306.5 | 1.0 | Near base of Obsoletes obsoletes and Protriticites pseudomontiparus fusulinid zone, or lowest occurrence of Parashumardites ammonoid | Guide event is undecided. GSSP anticipated in 2008 | |||
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base Moscovian Stage | 311.7 | 1.1 | Near lowest occurrences of Declinognathodus donetzianus and/or Idiognathoides postsulcatus conodont species, and fusulinid species Aljutovella aljutovica | Guide event is undecided. GSSP anticipated in 2008 | |||
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base Bashkirian Stage, base Pennsylvanian Subsystem | 318.1 | 1.3 | Conodont, lowest occurrence of Declinognathodus nodiliferus s.l. | 82.9 m above top of Battleship Wash Fm., Arrow Canyon, southern Nevada, USA | GSSP ratified 1996. Subsystem rank with Mississippian and Pennsylvanian names ratified 2000. | Episodes 22 (4), p.272-283, 1999 | |
Mississippian Subsystem | |||||||
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base Serpukhovian | 326.4 | 1.6 | Near lowest occurrence of conodont, Lochriea crusiformis | Guide event is undecided. GSSP anticipated in 2007 | |||
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base Visean | 345.3 | 2.1 | Foraminifer, lineage Eoparastaffella simplex morphotype 1/morphotype 2 | Leading candidate is Pengchong, south China | |||
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base Tournaisian, base Mississippian Subsystem, base Carboniferous System | 359.2 | 2.5 | Conodont, above lowest occurrence of Siphonodella sulcata | Base of Bed 89, La Serre, Montagne Noir, Cabrières, southern France | Ratified 1990 | Episodes 14 (4), p.331-336, 1991 | |
Devonian System | |||||||
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base Famennian Stage | 374.5 | 2.6 | Devonian time scale is a statistical fit of a composite biostratigraphic zonation (based on Figure 8 of Williams et al., 2000) to selected radiometric ages | Just above major extinction horizon (Upper Kellwasser Event), including conodonts Ancyrodella and Ozarkodina and goniatites of Gephuroceratidae and Beloceratidae | base of Bed 32a, upper Coumiac quarry, Cessenon, Montagne Noir, southern France | Ratified 1993 | Episodes 16 (4), p.433-441, 1993 |
base Frasnian Stage | 385.3 | 2.6 | Conodont, lowest occurrence of Ancyrodella rotundiloba (defines base of Lower Polygnathus asymmetricus conodont Zone) | Base of Bed 42a', Col du Puech de la Suque section, St. Nazaire-de-Ladarez, SE Montagne Noir, southern France | Ratified 1986 | Episodes 10 (2), p.97-101, 1987 | |
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base Givetian Stage | 391.8 | 2.7 | Conodont, lowest occurrence of Polygnathus hemiansatus, near base of goniatite Maenioceras Stufe | Base of Bed 123, Jebel Mech Irdane ridge, Tafilalt, Morocco | Ratified 1994 | Episodes 18 (3), p.107-115, 1995 | |
base Eifelian Stage | 397.5 | 2.7 | Conodont, lowest occurrence of Polygnathus costatus partitus; major faunal turnover | Base unit WP30, trench at Wetteldorf Richtschnitt, Schönecken-Wetteldorf, Eifel Hills, western Germany | Ratified 1985 | Episodes 8 (2), p.104-109, 1985 | |
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base Emsian Stage | 407.0 | 2.8 | Conodont, lowest occurrence of Polygnathus kitabicus (= Po. dehiscens) | Base of Bed 9/5, Zinzil'ban Gorge, SE of Samarkand, Uzbekistan | Ratified 1995 | Episodes 20 (4), p. 235-240, 1997 | |
base Pragian Stage | 411.2 | 2.8 | Conodont, lowest occurrence of Eognathodus sulcatus | Base of Bed 12, Valká Chuchle quarry, southwest part of Prague city, Czech Republic | Ratified 1989 | Episodes 12 (2), p.109-113, 1989 | |
base Lochkovian Stage, base Devonian System | 416.0 | 2.8 | base-Devonian from scale in Cooper (GTS 2004), which is 1 myr younger than Tucker et al (1998) estimate. | Graptolite, lowest occurrence of Monograptus uniformis | Within Bed 20, Klonk, Barrandian area, southwest of Prague, Czech Republic | Ratified 1972 | Martinsson (ed.), The Silurian-Devonian Boundary, IUGS Series A, no.5, 349 pp., 1977 |
Silurian System [Holland and Bassett (eds), A Global Standard for the Silurian System, Nat. Mus. Wales, Geol. Series No.10, Cardiff, 325 pp., 1989] | |||||||
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base Pridoli Series (not subdivided in stages) | 418.7 | 2.7 | Silurian and Ordovician time scales are from calibrating a CONOP composite graptolite zonation to selecte radiometric ages | Graptolite, lowest occurrence of Monograptus parultimus | Within Bed 96, Pozáry section near Reporje, Barrandian area, Prague, Czech Republic | Ratified 1984 | Episodes 8 (2), p.101-103, 1985 |
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base Ludfordian Stage | 421.3 | 2.6 | Imprecise. May be near base of Saetograptus leintwardinensis graptolite zone. | Base of lithological unit C, Sunnyhill Quarry, Ludlow, Shropshire, southwest England, UK | Ratified 1980 | Lethaia 14, p.168, 1981; Episodes 5 (3), p.21-23, 1982 | |
base Gorstian Stage | 422.9 | 2.5 | Imprecise. Just below base of local acritarch Leptobrachion longhopense range zone. May be near base of Neodiversograptus nilssoni graptolite zone | Base of lithological unit F, Pitch Coppice quarry, Ludlow, Shropshire, southwest England, UK | Ratified 1980 | Lethaia 14, p.168, 1981; Episodes 5 (3), p.21-23, 1982 | |
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base Homerian Stage | 426.2 | 2.4 | Graptolite, lowest occurrence of Cyrtograptus lundgreni (defines base of C. lundgreni graptolite zone) | Graptolite biozone intersection in stream section in Whitwell Coppice, Homer, Shropshire, southwest England, UK | Ratified 1980 | Lethaia 14, p.168, 1981; Episodes 5 (3), p.21-23, 1982 | |
base Sheinwoodian Stage | 428.2 | 2.3 | Imprecise. 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 define. 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 | Base of lithological unit G, Hughley Brook, Apedale, Shropshire, southwest England, UK | Ratified 1980 | Lethaia 14, p.168, 1981; Episodes 5 (3), p.21-23, 1982 | |
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base Telychian Stage | 436.0 | 1.9 | Brachiopods, just above extinction of Eocoelia intermedia and below lowest succeeding species Eocoelia curtisi. Near base of Monograptus turriculatus graptolite zone. | Locality 162 in transect d, Cefn Cerig road, Llandovery area, south-central Wales, UK | Ratified 1984 | Episodes 8 (2), p.101-103, 1985 | |
base Aeronian Stage | 439.0 | 1.8 | Graptolite, lowest occurrence of Monograptus austerus sequens (defines base of Monograptus triangulatus graptolite zone) | Base of locality 72 in transect h, Trefawr forestry road, north of Cwm-coed-Aeron Farm, Llandovery area, south-central Wales, UK | Ratified 1984 | Episodes 8 (2), p.101-103, 1985 | |
base Rhuddanian Stage, base Silurian System | 443.7 | 1.5 | Graptolites, lowest occurrences of Akidograptus ascensus, with FAD of Parakidograptus acuminatus occurring slightly higher | 1.6 m above base of Birkhill Shale Fm., Dob's Linn, Moffat, Scotland, UK | Ratified 1984 | Episodes 8 (2), p.98-100, 1985 | |
Ordovician System | |||||||
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base Hirnantian Stage | 445.6 | 1.5 | Graptolite, lowest occurrence of Normalograptus extraordinarius, base of major positive carbon-13 isotope excursion, and beginning of pronounced sea-level fall associated with onset of a major glaciation | 0.39 m below base of Kuanyinchiao Bed, Wangjiawan North section, 42 km N. of Yichang city (west Hubei province, China) | |||
base Katian Stage | 455.8 | 1.6 | Graptolite, lowest occurrence of Diplacanthograptus caudatus. Just below base of Guttenberg carbon-13 isotope excursion | 4 m above base of Bigfort Chert, Black Knob Ridge section, 5 km NE of Atoka town (S. Oklahoma, USA) | GSSP anticipated in 2005 | ||
base Sandbian Stage | 460.9 | 1.6 | Graptolite, lowest occurrence of Nemagraptus gracilis | 1.4 m below phosphorite in E14a outcrop, Fågelsång, Scane, southern Sweden | Ratified 2002 | Episodes 23 (2), p.102-109, 2000 (proposal; formal GSSP publication in preparation). | |
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base Darriwillian Stage | 468.1 | 1.6 | Graptolite, lowest occurrence of Undulograptus austrodentatus | Base of Bed AEP184, 22 m below top of Ningkuo Fm., Huangnitang, Changshan, Zhejiang province, southeast China | Ratified 1987 | Episodes 20 (3), p.158-166, 1997 | |
base of third stage (not yet named) | 471.8 | 1.6 | Conodont, potentially lowest occurrence of Protoprioniodus aranda or of Baltoniodus triangularis | Candidate sections at Niquivil (Argentina) and Huanghuachang (China) | |||
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Base Floian Stage | 478.6 | 1.7 | Graptolite, lowest occurrence of Tetragraptus approximatus | Just above E bed, Diabasbrottet quarry, Västergötland, southern Sweden | Ratified 2002 | Episodes 27 (4), p.265-272, 2004 | |
base of Tremadocian stage, base Ordovician System | 488.3 | 1.7 | Conodont, lowest occurrence of Iapetognathus fluctivagus;just above base of Cordylodus lindstromi conodont Zone. Just below lowest occurrence of planktonic graptolites. Currently dated around 489 Ma | Within Bed 23 at the 101.8 m level, Green Point, western Newfoundland, Canada | Ratified 2000 | Episodes 24 (1), p.19-28, 2001 | |
Cambrian System | |||||||
Overview of potential Cambrian subdivisions in Episodes 23 (3), p. 188-195, 2000 | |||||||
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Stage 10 | Trilobite, lowest occurrence of Lotagnostus americanus. An internal substage division might be lowest occurrence of Codylodus adesei conodont | ||||||
Stage 9 | Trilobite, lowest occurrence of Agnostotes orientalis | ||||||
base Paibian Stage, base Furongian Series | 501.0 | 2.0 | Radiometric ages near primary marker level. Estimated age and uncertainty only | Trilobite, lowest occurrence of agnostoid Glyptagnostus reticulatus. Coincides with base of large positive carbon-isotope excursion | 369.06 m above base of Huaqiao Fm, Paibi section, NW Hunan province, south China | Ratified 2003 | Lethaia 37 (4), p.365-380, 2004 |
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Trilobite, lowest occurrence of Lejopyge laevigata | >Candidate sections are at Wangcun or nearby Luoyixi (NW Hunan province, S. China) | ||||||
Trilobite, lowest occurrence of Ptychagnostus atavus | Candidate section is Wangcun (NW Hunan province, S. China) | GSSP anticipated in 2006 | |||||
513.0 | 2.0 | Radiometric ages near primary marker level. Estimated age and uncertainty only | Trilobite, potentially lowest occurrence of Oryctocephalus indicus | Candidate sections are Wuliu-Zengjiayan (east Guizhou, China) and Split Mountain (Nevada, USA) | GSSP anticipated in 2007 | ||
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Trilobite, lowest occurrence of Olenellus or Redlichia | Guide event is undecided | ||||||
Trilobites -- their lowest occurrence | |||||||
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Small Shelly Fossils, or Archaeocyathid species | Guide event is undecided | ||||||
base Cambrian System, base Paleozoic Era, base Phanerozoic Eon | 542.0 | 1.0 | U-Pb age from Oman coinciding with the negative carbon excursion | Trace fossil, lowest occurrence of Treptichnus (Phycodes) pedum. Near base of negative carbon-isotope excursion | 2.4 m above base of Member 2 of Chapel Island Fm., Fortune Head, Burin Peninsula, southeast Newfoundland, Canada | Ratified 1992 | Episodes 17 (1&2), p.95-100, 1994. |
PROTEROZOIC Eon | |||||||
Pre-Cambrian eras and systems below Ediacaran are defined by absolute ages, rather than stratigraphic points. | |||||||
Neoproterozoic Era | |||||||
base Ediacaran System | 630 | Age suggested by Ediacaran Subcomm.; bracketed by radiometric ages of 600 and 635 Ma | Termination of Varanger (or Marinoan) glaciation. | "Base of the Marinoan cap carbonate (Nuccaleena Formation), immediately above the Elatina diamictite in the Enorama Creek section, Flinders Ranges, South Australia." | "Neoproterozoic III" (ratified 1990 with base defined chronometrically at 650 Ma) was formally replaced by Ediacaran Period and its GSSP in Feb 2004. | Summary in Science 305, p.621-622, 2004. Episodes article in preparation | |
Cryogenian System | 850 | Defined chronometrically; but will be replaced by GSSP | Base = 850 Ma | Ratified 1990. GSSP replacement planned for 2007 | Episodes 14 (2), p.139-140, 1991 | ||
Tonian System | 1000 | Defined chronometrically | Base = 1000 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Mesoproterozoic Era | |||||||
Stenian System | 1200 | Defined chronometrically | Base = 1200 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Ectasian System | 1400 | Defined chronometrically | Base = 1400 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Calymmian System | 1600 | Defined chronometrically | Base = 1600 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Paleoproterozoic Era | |||||||
Statherian System | 1800 | Defined chronometrically | Base = 1800 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Orosirian System | 2050 | Defined chronometrically | Base = 2050 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Rhyacian System | 2300 | Defined chronometrically | Base = 2300 Ma | Ratified 1990 | Episodes 14 (2), p.139-140, 1991 | ||
Siderian System | 2500 | Defined chronometrically; but will be replaced by GSSP | Base = 2500 Ma | Ratified 1990. GSSP replacement planned for 2007 | Episodes 14 (2), p.139-140, 1991 | ||
ARCHEAN Eon | |||||||
Neoarchean Era | 2800 | Defined chronometrically | Base = 2800 Ma | Subcomm. decision 1996, but not submitted to ICS | Informally in Episodes 15 (2), p.122-123, 1992. | ||
Mesoarchean Era | 3200 | Defined chronometrically | Base = 3200 Ma | Subcomm. decision 1996, but not submitted to ICS | Informally in Episodes 15 (2), p.122-123, 1992. | ||
Paleoarchean Era | 3600 | Defined chronometrically | Base = 3600 Ma | Subcomm. decision 1996, but not submitted to ICS | Informally in Episodes 15 (2), p.122-123, 1992. | ||
Eoarchean Era | ~4000 | Base is not defined | Oldest preserved rocks on Earth's surface | Subcomm. decision 1996, but not submitted to ICS | Informally in Episodes 15 (2), p.122-123, 1992 | HADIAN Eon | ~4650 | Base is not defined | Formation of planet Earth. Informal term |