GSSP Table - All Periods
Global Boundary Stratotype Section and Point (GSSP) of the International Commission on Stratigraphy
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Stage |
Numerical Age (Ma) |
GSSP Location |
Latitude, Longitude |
Boundary Level |
Correlation Events |
Status |
Reference |
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Phanerozoic Eon |
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Cenozoic Era |
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Quaternary System |
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Holocene Series |
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0.011784 |
NorthGRIP ice core, central Greenland |
75.1000°N 42.3200°W |
1492.45m depth in Borehole NGRIP2 |
Climatic -- End of the Younger Dryas cold spell, which is reflected in a shift in deuterium excess values |
Ratified 2008 |
Episodes 31/2, 2008; J. Quaternary Sci., Vol. 24 pp. 3-17, 2009 |
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Pleistocene Series |
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Upper Stage |
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Middle Stage |
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1.806 |
Vrica, Italy |
39.0385°N 17.1348°E |
base of the marine claystone overlying the sapropelic marker Bed ‘e’ (Mediterranean Precession Related Sapropel, MPRS 176) |
Magnetic -- ~15 kyr after end of Olduvai (C2n) normal polarity chron |
Ratified 1985 as base of Pleistocene; Ratified 2011 as base of Calabrian |
Episodes 8/2, p. 116 – 120, 1985; Episodes 35/3, p. 388-397, 2012 |
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2.588 |
Monte San Nicola, Sicily, Italy |
37.1469°N 14.2035°E |
base of marly layer overlying sapropel MPRS 250 |
Magnetic -- Matuyama/Gauss boundary (C2r/C2An) is 1m below GSSP. GSSP level is within Marine Isotope Stage 103. |
Ratified 1996 as base of Gelasian; Ratified 2009 as base of Pleistocene and Quaternary |
Episodes 21/2, p. 82–87, 1998; Episodes 33/3, p. 152-158, 2010 |
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Neogene System |
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Pliocene Series |
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3.6 |
Punta Piccola, Sicily, Italy |
37.2889°N 13.4933°E |
base of the beige marl bed of small-scale carbonate cycle 77 (MPRS 347) |
Magnetic -- Gauss/Gilbert (C2An/C2Ar) magnetic reversal is recorded immediately above the GSSP |
Ratified 1997 |
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5.333 |
Eraclea Minoa, Sicily, Italy |
37.3917°N 13.2806°E |
base of the Trubi Formation which corresponds to Insolation cycle 510 |
Magnetic -- base of the Thvera magnetic event (C3n.4n) is only 96 kyr (5 precession cycles) younger than the GSSP. |
Ratified 2000 |
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Miocene Series |
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7.246 |
Oued Akrech, Morocco |
33.9369°N 6.8125°W |
reddish layer of sedimentary cycle number 15 |
Planktonic foraminifer first regular occurrence of Globorotalia miotumida, and calcareous nannofossil FAD Amaurolithus delicatus |
Ratified 2000 |
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11.62 |
Monte dei Corvi Beach, near Ancona, Italy |
43.5867°N 13.5694°E |
mid-point of sapropel layer of basic cycle number 76. |
Calcareous nannofossil last common occurrence of Discoaster kugleri |
Ratified 2003 |
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13.82 |
Ras il Pellegrin section, Fomm Ir- Rih Bay, west coast of Malta |
35.9139°N 14.3361°E |
formation boundary between the Globigerina Limestone and Blue Clay |
Oxygen-isotopic event (global cooling episode) Mi3b; near calcareous nannofossil LAD of Sphenolithus heteromorphus |
Ratified 2007 |
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Langhian Stage |
15.97 |
Potentially in astronomicallytuned ODP core (Leg 154) or in Italy (Moria or La Vedova ) |
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Near planktonic foraminifer FAD of Praeorbulina glomerosa and top of magnetic polarity chronozone C5Cn.1n |
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Burdigalian Stage |
20.44 |
Potentially in astronomicallytuned ODP core |
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Near planktonic foraminifer FAD of Globigerinoides altiaperturus or near top of magnetic polarity chronozone C6An |
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23.03 |
Lemme-Carrioso Section, Allessandria Province, Italy |
44.6589°N 8.8364°E |
35m from the top of the section |
Magnetic -- base of Chron C6Cn.2n; planktonic foraminifer FAD of Paragloborotalia kugleri; calcareous nannofossil near LAD Reticulofenestra bisecta (base Zone NN1); Oxygen isotopic event Mi-1. |
Ratified 1996 |
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Paleogene System |
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Oligocene Series |
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Chattian Stage |
28.1 |
Possibly Monte Cagnero, Umbria-Marche region, Italy |
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Potentially extinction of planktonic foraminifer Chiloguembelina (base Foram Zone P21b); or an isotopic/climatic event |
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33.9 |
Massignano, near Ancona, Italy |
43.5328°N 13.6011°E |
base of a 0.5m thick greenishgrey marl bed 19m above base of section |
Foraminifer LAD Hantkenina and Cribrohantkenina |
Ratified 1992 |
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Eocene Series |
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Priabonian Stage |
38.0 |
Alano section, Piave River; Veneto Prealps, Belluno province, N. Italy |
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Tiziano Bed |
Calcareous nannofossil near FAD Chiasmolithus oamaruensis (base Zone NP18) |
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Bartonian Stage |
41.3 |
Contessa highway section near Gubio, Central Apennines, Italy |
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Calcareous nannofossil near LAD Reticulofenestra reticulata |
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47.8 |
Gorrondatxe section, Basque Country, Spain |
43°22'46.47"N, 3°00'51.61"W |
dark marl at 167.85 m in Gorrondatxe sea-cliff section |
LO of calcareous nannofossil Blackites inflatus (CP12a/b boundary); middle of polarity Chron C21r |
Ratified 2011 |
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56.0 |
Dababiya, near Luxor, Egypt |
25.5000°N 32.5311°E |
Base of Bed 1 in DBH subsection |
Carbon Isotope Excursion base, initiation of basal Eocene Thermal maximum (“PETM”) |
Ratified 2003 |
Micropaleontology 49/1, p.41 – 59, 2003; Episodes 30/4, p. 271 - 286, 2007 |
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Paleocene Series |
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59.2 |
Zumaia section, northern Spain |
43.3006°N 2.2594°W |
30.5m above the base of Itzurun Formation |
Magnetic -- Base of Chron C26n |
Ratified 2008 |
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61.6 |
Zumaia section, northern Spain |
43.3006°N 2.2594°W |
base of the red marls of Itzurun Formation |
2nd radiation of the calcareous nannofossil group Fasciculithus and sea-level fall |
Ratified 2008 |
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66.0 |
Oued Djerfane, west of El Kef, Tunisia |
36.1537°N 8.6486°E |
reddish layer at the base of the 50cm thick, dark boundary clay |
Iridium geochemical anomaly. Associated with a major extinction horizon (dinosaurs, ammonites, foraminifers, etc.) |
Ratified 1991 |
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Mesozoic Era |
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Cretaceous System |
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Upper Cretaceous Series |
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72.1±0.2 |
Tercis les Bains, Landes, France |
43.6795°N 1.1133°W |
level 115.2 on platform IV of the geological site at Tercis les Bains |
Mean of 12 biostratigraphic criteria of equal importance. Closely above is FAD of ammonite Pachydiscus neubergicus. Boreal proxy is FAD of belemnite Belemnella lanceolata. |
Ratified 2001 |
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Campanian Stage |
83.6±0.2 |
candidates are in southern England and in Texas |
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Crinoid LAD Marsupites testudinarius |
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Santonian Stage |
86.3 ± 0.5 |
Olazagutia, Navarra, Spain |
94.4 m in the Cantera de Margas quarry section |
the FO of the inoceramid bivalve Platyceramus undulatoplicatus |
Ratified 2013 |
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Coniacian Stage |
89.8 ± 0.3 |
candidates are in Poland (Slupia Nadbrzena), USA (Pueblo, Colorado), and Germany (Salzgitter-Salder Quarry) |
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Inoceramid bivalve FAD Cremnoceramus rotundatus (sensu Tröger non Fiege) |
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93.9 |
Pueblo, Colorado, USA |
base of Bed 86 of the Bridge Creek Limestone Member |
Ammonite FAD Watinoceras devonense |
Ratified 2003 |
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100.5 |
Mount Risou, Hautes-Alpes, France |
44.3925°N 5.5119°E |
36 meters below the top of the Marnes Bleues Formation on the south side of Mont Risou |
Planktonic foraminifer FAD Rotalipora globotruncanoides |
Ratified 2002 |
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Lower Cretaceous Series |
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Albian Stage |
~113.0 |
Southeastern France |
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Candidates include: (1) calcareous nannofossil FAD of Praediscosphaera columnata (= P. cretacea of some earlier studies), (2) carbon-isotope excursion (black-shale episode), (3) ammonite |
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Aptian Stage |
~125.0 |
candidate is Gorgo a Cerbara, Piobbico, Umbria-Marche, central Italy |
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Magnetic -- base of Chron M0r; near FAD of Paradeshayesites oglanlensis ammonite zone |
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Barremian Stage |
~129.4 |
candidate is Río Argos near Caravaca, Murcia Province, Spain |
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Ammonite FAD Spitidiscus hugii – Spitidiscus vandeckii group |
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Hauterivian Stage |
~132.9 |
candidate is La Charce village, Drôme Province, southeast France |
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Ammonite FAD of genus Acanthodiscus (especially A. radiatus) |
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Valanginian Stage |
~139.8 |
candidates are near Montbrunles- Bains (Drôme province, SE France) and Cañada Luenga (Betic Cordillera, S. Spain) |
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Calpionellid FAD Calpionellites darderi (base of Calpionellid Zone E); followed by ammonite FAD “Thurmanniceras” pertransiens |
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Berriasian Stage |
~145.0 |
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Candidates include: (1) Magnetic -- base of Chron M18r, (2) Base of Calpionellid zone B, (3) ammonite FAD of Berriasella jacobi |
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Jurassic System |
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Upper Jurassic Series |
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Tithonian Stage |
152.1 ± 0.9 |
candidates are Mt. Crussol or Canjuers (SE France) and Fornazzo (Sicily, S. Italy) |
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Near base of Hybonoticeras hybonotum ammonite zone and lowest occurrence of Gravesia genus, and the base of magnetic polarity Chron M22An |
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Kimmeridgian Stage |
157.3 ± 1.0 |
candidate is Flodigarry (Isle of Skye, NW Scotland) |
57.6000°N 6.2000°W |
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Ammonite near base of Pictonia baylei ammonite zone of Boreal realm |
Anticipated 2009 |
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Oxfordian Stage |
163.5 ± 1.0 |
candidates are Redcliff Point (Dorset, SW England) and Savouron (Provence, SE France) |
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Ammonite Cardioceras redcliffense Horizon at base of the Cardioceras scarburgense Subzone (Quenstedtoceras mariae Zone) |
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Middle Jurassic Series |
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Callovian Stage |
166.1 ± 1.2 |
candidates are Pfeffingen (Swabian Alb, SW Germany) and in Russia |
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Ammonite FAD of the genus Kepplerites (Kosmoceratidae) (defines base of Macrocephalites herveyi Zone in sub-Boreal province of Great Britain to southwest Germany) |
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168.3 ± 1.3 |
Ravin du Bès, Bas-Auran area, Alpes de Haute Provence, France |
43.9606°N 6.3153°E |
base of limestone bed RB07 |
Ammonite FAD Gonolkite convergens (defines base of Zigzagiceras zigzag Zone) |
Ratified 2008 |
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170.3 ± 1.4 |
Murtinheira Section, Cabo Mondego, Portugal |
40.1992°N 8.9042°W |
base of Bed AB 11 |
Ammonite FAD Hyperlioceras mundum, Hyperlioceras furcatum, Braunsina aspera, and Braunsina elegantula |
Ratified 1996 |
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174.1 ± 1.0 |
Fuentelsaz, Spain |
41.1708°N 1.8333°W |
base of Bed FZ 107 |
Ammonite FAD Leioceras opalinum and Leioceras lineatum |
Ratified 2000 |
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Lower Jurassic Series |
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Toarcian Stage |
182.7 ± 0.7 |
Peniche (Portugal) |
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Ammonite near FAD of a diversified Eodactylites ammonite fauna; correlates with the NW European Protogrammoceras paltus horizon. |
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190.8 ± 1.0 |
Wine Haven, Robin Hood's Bay, Yorkshire Coast, England |
54.4069°N 0.4975°W |
base of Bed 73b |
Ammonite association of Bifericeras donovani and Apoderoceras sp. |
Ratified 2005 |
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199.3 ± 0.3 |
East Quantoxhead, SW England |
51.1909°N 3.2364°W |
0.90 m above the base of Bed 145 |
Ammonite FAD Vermiceras quantoxense, Vermiceras palmeri |
Ratified 2000 |
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Hettangian Stage |
201.3 ± 0.2 |
Kuhjoch section, Tyrol, Austria |
47.4839°N 11.5306°E |
5.80 m above top of Koessen Formation |
FO of ammonite Psiloceras spelae tirolicum, FO of palynomorph Cerebropollenites thiergartii |
Ratified 2010 |
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Triassic System |
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Upper Triassic Series |
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Rhaetian Stage |
~208.5 |
Key sections in Austria, British Columbia (Canada), and Turkey |
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Near FAD of ammonite Cochloceras, conodonts Misikella spp. and Epigondolella mosheri, and radiolarian Proparvicingula moniliformis |
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Norian Stage |
~227 |
Candidates are Black Bear Ridge in British Columbia (Canada) and Pizzo Mondello, Sicily (Italy) |
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Base of Stikinoceras kerri ammonoid zone and near FAD of Metapolygnathus echinatus within the M. communisti conodont zones |
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~237 |
Prati di Stuores, Dolomites, Italy |
46.5269°N 11.9303°E |
base of marly limestone bed SW4, 45m from base of San Cassiano Formation |
FAD of the ammonoid Daxatina canadensis; just below FO of conodont Paragondolella polygnathiformis and base of normal-polarity magnetic zone S2n |
Ratified 2008 |
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Middle Triassic Series |
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~242 |
Bagolino, Province of Brescia, Northern Italy |
45.8193°N 10.4710°E |
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 |
Ammonite FAD Eoprotrachyceras curionii (base of the E. curionii zone). Conodont FAD Budurovignathus praehungaricus is in the uppermost Anisian. |
Ratified 2005 |
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Anisian Stage |
247.2 |
Candidate section at Desli Caira (Dobrogea, Romania); significant sections in Guizhou Province (China) and South Primorye (Russia) |
45.0742°N 28.8022°E |
In Section B, the GSSP level will be either the FAD of conodont Chiosella timorensis at the base of Bed GR7 at ca. 7 m; OR the base of magnetozone MT1n at the 5.7 m level. |
Conodont FAD Chiosella timorensis or Magnetic -- base of magnetic polarity MT1n |
Anticipated 2009 |
Albertiana 36, 2007. |
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Lower Triassic Series |
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Olenekian Stage |
251.2 |
Candidate GSSP Mud (Muth) village, Spiti valley, northwest India |
31.9654°N 78.0246°E |
base of Bed 13A-2, about 4.8m up in Mikin Formation., Section M04 (~4000 m elevation |
Conodont FAD Neospathodus waageni, just above base of Rohillites rohilla ammonite zone, and below lowest occurrence of Flemingites and Euflemingites ammonite genera. Within a prominent positive Carbon-13 peak, and just above widely recognizable sequence boundary. |
Anticipated 2009 |
Albertiana 36, 2007 |
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252.17 ± 0.06 |
Meishan, Zhejiang Province, China |
31.0798°N 119.7058°E |
base of Bed 27c in the Meishan D Section |
Conodont FAD Hindeodus parvus |
Ratified 2001 |
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Paleozoic Era |
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Permian System |
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Lopingian Series |
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254.14 ± 0.07 |
Meishan, Zhejiang Province, China |
31.0819°N 119.7064°E |
base of Bed 4a- 2, 88 cm above the base of the Changxing Limestone at the Meishan D Section |
Conodont FAD Clarkina wangi |
Ratified 2005 |
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259.8 ± 0.4 |
Penglaitan, Guanxi Province, South China |
23.6953°N 109.3211°E |
base of Bed 6k in the Penglaitan Section |
Conodont FAD Clarkina postbitteri postbitteri |
Ratified 2004 |
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Guadalupian Series |
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265.1 ± 0.4 |
Nipple Hill, SE Guadalupe Mountains, Texas, U.S.A |
31.9091°N 104.7892°W |
4.5m above the base of the outcrop section of the Pinery Limestone Member of the Bell Canyon Formation |
Conodont FAD Jinogondolella postserrata |
Ratified 2001 |
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268.8 ± 0.5 |
Guadalupe Pass, Texas, U.S.A |
31.8658°N 104.8328°W |
7.6m above the base of the Getaway Ledge outcrop Section of the Getaway Limestone Member of the Cherry Canyon Formation |
Conodont FAD Jinogondolella aserrata |
Ratified 2001 |
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272.3 ± 0.5 |
Stratotype Canyon, Texas, U.S.A |
31.8767°N 104.8768°W |
42.7m above the base of the Cutoff Formation |
Conodont FAD Jinogondolella nankingensis |
Ratified 2001 |
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Cisuralian Series |
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Kungurian Stage |
283.5 ± 0.6 |
candidates are in southern Ural Mtns. |
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Near conodont FAD Neostreptognathus pnevi - N. exculptus |
Anticipated 2009 |
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Artinskian Stage |
290.1 ± 0.26 |
candidates are in southern Ural Mtns. |
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Conodont FAD Sweetognathus whitei |
Anticipated 2009 |
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Sakmarian Stage |
295.0 ± 0.18 |
candidate is at Kondurovsky, Orenburg Province, Russia. |
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Near conodont FAD Sweetognathus merrelli |
Anticipated 2009 |
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298.9 ± 0.15 |
Aidaralash Creek, Kazakhstan |
50.2458°N 57.8914°E |
27m above the base of Bed 19, Aidaralash Creek |
Conodont FAD of isolated-nodular morphotype of Streptognathodus "wabaunsensis" |
Ratified 1996 |
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Carboniferous System |
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Pennsylvanian Subsystem (series Classification Approved In 2004) |
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Upper Pennsylvanian Series |
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Gzhelian Stage |
303.7 ± 0.1 |
candidates are in southern Urals or Nashui (south China). |
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Conodont FAD Idiognathodus simulator (s.str.). Close to FAD of ammonoid Shumardites. |
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Kasimovian Stage |
307.0 ± 0.1 |
candidates are in southern Urals, southwest USA and Nashui (south China). |
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Fusulinid FAD Protriticites, which is near ammonoid FAD Eothalossoceras. Alternative (higher) base is fusulinid FAD Montiparus montiparus, which is near conodont FAD Idiognathodus sagittalis. Age given here is the higher version; the lower one is about 1 myr older. |
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Middle Pennsylvanian Series |
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Moscovian Stage |
315.2 ± 0.2 |
candidates are in southern Urals or Nashui (south China). |
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Either conodont FAD Idiognathoides postsulcatus or Declinognathodus donetzianus. |
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Lower Pennsylvanian Series |
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323.2 ± 0.4 |
Arrow Canyon, Nevada |
36.7333°N 114.7778°W |
82.9m above the top of the Battleship Formation in the lower Bird Spring Formation |
Conodont FAD Declinognathodus noduliferus |
Ratified 1996 |
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Mississippian Subsystem |
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Upper Mississippian Series (series Classification Approved In 2004) |
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Serpukhovian Stage |
330.9 ± 0.2 |
candidates are Verkhnyaya Kardailovka (Urals) or Nashui (China) |
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Conodont FAD Lochriea ziegleri |
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Middle Mississippian Series |
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346.7 ± 0.4 |
Pengchong, south China |
24.4333°N 109.4500°E |
base of bed 83 in the Pengchong Section |
Benthic Foraminifer FAD Eoparastaffella simplex |
Ratified 2008 |
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Lower Mississippian Series |
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358.9 ± 0.4 |
La Serre, France |
43.5555°N 3.3573°E |
base of Bed 89 in Trench E’ at La Serre, (but FAD now known to be at base of Bed 85) |
Conodont FAD Siphonodella sulcata IMPRECISE (GSSP discovered in 2006 to have biostratigraphic problems, and can not be correlated with precision.) |
Ratified 1990 |
Episodes 14/4, p. 331-336, 1991; Newsletters on Stratigraphy, 43/2, p. 195 - 205, 2009 |
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Devonian System |
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Upper Devonian Series |
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372.2 ± 1.6 |
Coumiac Quarry, near Cessenon, Montagne Noire, France |
43.4613°N 3.0403°E |
Base of Bed 32a |
Conodont FAD Palmatolepis triangularis, just above a major extinction horizon (Kellwasser Event) with conodont LADs Ancyrodella and Ozarkodina, and Goniatite LADs of Gephuroceratidae and Beloceratidae |
Ratified 1993 |
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382.7 ± 1.6 |
Col du Puech de la Suque, Montage Noire, France |
43.5032°N 3.0868°E |
base of Bed 42’ at Col du Puech de la Suque section E |
Conodont FAD Ancyrodella rotundiloba |
Ratified 1986 |
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Middle Devonian Series |
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387.7 ± 0.8 |
Jebel Mech Irdane, Morocco |
31.2374°N 4.3541°W |
base of Bed 123 |
Conodont FAD Polygnathus hemiansatus |
Ratified 1994 |
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393.3 ± 1.2 |
Wetteldorf, Eifel Hills, Germany |
50.1496°N 6.4716°E |
21.25m above the base of the exposed section, base of sample station WP30 |
Conodont FAD Polygnathus costatus partitus |
Ratified 1985 |
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Lower Devonian Series |
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407.6 ± 2.6 |
Zinzil'ban Gorge in the Kitab State Geological Reserve, Uzbekistan |
39.2000°N 67.3056°E |
base of Bed 9/5 |
Conodont FAD Polygnathus kitabicus |
Ratified 1995 |
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410.8 ± 2.8 |
Velká Chuchle, Prague, Czech Republic |
50.0147°N 14.3726°E |
base of Bed 12 in Velká Chuchle Quarry |
Conodont FAD Eognathodus sulcatus sulcatus and Latericriodus steinachensis Morph beta |
Ratified 1989 |
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419.2 ± 3.2 |
Klonk, near Prague, Czech Republic |
49.8550°N 13.7920°E |
within Bed 20 |
Graptolite FAD Monograptus uniformis |
Ratified 1972 |
IUGS Series A, 5, p. 96-109, 1977 |
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Silurian System |
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423.0 ± 2.3 |
Požáry Section, Reporyje, Prague, Czech Republic |
50.0277°N 14.3249°E |
within Bed 96 |
Graptolite FAD Monograptus parultimus |
Ratified 1984 |
Episodes 8/2, p. 101-103, 1985; Geol. Series, Nat. Mus. Wales, 9, p. 90 - 100, 1989 |
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Ludlow Series |
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425.6 ± 0.9 |
near Ludlow, UK |
52.3592°N 2.7772°W |
coincident with the base of the Leintwardine Formation |
Imprecise. May be near base of Saetograptus leintwardinensis Graptolite zone. |
Ratified 1980 |
Lethaia 14; Episodes 5/3, p. 21-23, 1982; Geol. Series, Nat. Mus. Wales, 9, p. 73 - 90, 1989 |
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427.4 ± 0.5 |
near Ludlow, UK |
52.3592°N 2.7772°W |
coincident with the base of the Lower Elton Formation |
Graptolite FAD Saetograptus (Colonograptus) varians |
Ratified 1980 |
Lethaia 14; Episodes 5/3, p. 21-23, 1982; Geol. Series, Nat. Mus. Wales, 9, p. 73 - 90, 1989 |
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|
Wenlock Series |
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430.5 ± 0.7 |
Sheinton Brook, Homer, UK |
52.6156°N 2.5647°W |
within upper part of the Apedale Member of the Coalbrookdale Formation |
Graptolite FAD Cyrtograptus lundgreni |
Ratified 1980 |
Lethaia 14; Episodes 5/3, p. 21-23, 1982; Geol. Series, Nat. Mus. Wales, 9, p. 51-73, 1989 |
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|
433.4 ± 0.8 |
Hughley Brook, UK |
52.5811°N 2.6389°W |
base of the Buildwas Formation |
Imprecise. Between the base of acritarch biozone 5 and LAD of conodont Pterospathodus amorphognathoides. The current GSSP does not coincide with the base of the Cyrtograptus centrifugus Biozone, as was supposed when the GSSP was defined. Restudy recommends a slightly higher and correlatable level on condonts -- the Ireviken datum 2, which coincides approximately with the base of the murchisoni Graptolite Biozone |
Ratified 1980 |
Lethaia 14; Episodes 5/3, p. 21-23, 1982; Geol. Series, Nat. Mus. Wales, 9, p. 51-73, 1989 |
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Llandovery Series |
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|
438.5 ± 1.1 |
Cefn-cerig Road Section, Wales, UK |
51.9700°N 3.7900°W |
within the Wormwood Formation |
Just above Brachiopod LAD Eocoelia intermedia and below FAD of Eocoelia curtisi |
Ratified 1984 |
Episodes 8/2, p. 101-103, 1985; Geol. Series, Nat. Mus. Wales, 9, p. 36-50, 1989 |
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|
440.8 ± 1.2 |
Trefawr Track Section, Wales, UK |
52.0300°N 3.7000°W |
within Trefawar Formation |
Graptolite FAD Monograptus austerus sequens |
Ratified 1984 |
Episodes 8/2, p. 101-103, 1985; Geol. Series, Nat. Mus. Wales, 9, p. 36-50, 1989 |
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443.4 ± 1.5 |
Dob's Linn, Scotland |
55.4400°N 3.2700°W |
1.6m above the base of the Birkhill Shale Formation |
Graptolite FAD Akidograptus ascensus |
Ratified 1984 |
Episodes 8/2, p. 101-103, 1985; Silurian Times No. 14 (2006) |
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Ordovician System |
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Upper Ordovician Series |
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445.2 ± 1.4 |
Wangjiawan North section, N of Yichang city, Western Hubei Province, China |
30.9841°N 111.4197°E |
0.39m below the base of the Kuanyinchiao Bed |
Graptolite FAD Normalograptus extraordinarius |
Ratified 2006 |
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|
453.0 ± 0.7 |
Black Knob Ridge Section, Atoka, Oklahoma (USA) |
34.4305°N 96.0746°W |
4.0m above the base of the Bigfork Chert |
Graptolite FAD Diplacanthograptus caudatus |
Ratified 2006 |
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|
458.4 ± 0.9 |
Sularp Brook, Fågelsång, Sweden |
55.7137°N 13.3255°E |
1.4m below a phosphorite marker bed in the E14b outcrop |
Graptolite FAD Nemagraptus gracilis |
Ratified 2002 |
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|
Middle Ordovician Series |
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467.3 ± 1.1 |
Huangnitang section, Changshan, Zhejiang Province, SE China |
28.8539°N 118.4897°E |
base of Bed AEP 184 |
Graptolite FAD Undulograptus austrodentatus |
Ratified 1987 |
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|
470.0 ± 1.4 |
Huanghuachang Section, NE of Yichang city, Hubei Province, S. China |
30.8605°N 110.3740°E |
10.57 m above base of the Dawan Formation |
Conodont FAD of Baltoniodus triangularis |
Ratified 2007 |
Episodes 28/2, p. 105 - 117, 2005; Episodes 32/2, p. 96-113, 2009 |
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|
Lower Ordovician Series |
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|
477.7 ± 1.4 |
Diabasbrottet, Hunneberg, Sweden |
58.3589°N 12.5024°E |
in the lower Tøyen Shale, 2.1m above the top of the Cambrian |
Graptolite FAD Tetragraptus approximatus |
Ratified 2002 |
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|
485.4 ± 1.9 |
Green Point Section, western Newfoundland |
49.6829°N 57.9653°W |
at the 101.8m level, within Bed 23, in the measured section |
Conodont FAD Iapetognathus fluctivagus |
Ratified 2000 |
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Cambrian System |
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Furongian Series |
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Stage 10 |
~489.5 |
candidate section is Duibian (Zhejiang province, China) |
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|
Trilobite FAD of Lotagnostus americanus. An internal substage division might be FAD of Codylodus adesei conodont |
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|
~494 |
Duibian B section, Zhejiang province, China |
28°48.958'N 118°36.896'E |
28.2 m in Duibian B section |
FAD of agnostid trilobite Agnostotes orientalis and the FO of polymerid trilobite Irvingella angustilimbata |
Ratified 2011 |
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|
~497 |
Wuling Mountains, Huayuan County, NW Hunan Province, Chin |
28.3895°N 109.5257°E |
at 396 m in the Huaqiao Formation |
Trilobite FAD Glyptagnostus reticulatus |
Ratified 2003 |
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Series 3 |
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|
~500.5 |
Louyixi, Guzhang County, NW Hunan Province, S. China |
28.7200°N 109.9647°E |
121.3 m above the base of the Huaqiao Formation |
Trilobite FAD Lejopyge laevigata |
Ratified 2008 |
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|
~504.5 |
Drum Mountains, Millard County, Utah, USA |
39.5117°N 112.9915°W |
at the base of a dark-gray thinly laminated calcisiltite layer, 62 m above the base of the Wheeler Formation |
Trilobite FAD Ptychagnostus atavus |
Ratified 2006 |
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|
Stage 5 |
~509 |
candidate sections are Wuliu-Zengjiayan (east Guizhou, China) and Split Mountain (Nevada, USA) |
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|
Trilobite, potentially FAD of Oryctocephalus indicus |
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Series 2 |
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Stage 4 |
~514 |
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|
Trilobite FAD Olenellus or Redlichia |
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Stage 3 |
~521 |
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|
Trilobites -- their FAD |
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|
Terreneuvian Series |
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Stage 2 |
~529 |
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|
|
Small Shelly Fossils, or Archaeocyathid species |
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|
541.0 ± 1.0 |
Fortune Head, SE Newfoundland, Canada |
47.0762°N 55.8310°W |
2.4m above the base of Member 2 in the Chapel Island Formation |
Trace fossil FAD Trichophycus pedum |
Ratified 1992 |
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Precambrian |
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Proterozoic Eon |
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Neoproterozoic Era |
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|
~635 |
Enorama Creek, Flinders Ranges, South Australia |
31.3314°S 138.6334°E |
base of the Marinoan cap carbonate |
(1) 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. |
Ratified 1990 |
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|
Cryogenian System |
850 |
Defined chronometrically; but will be replaced by GSSP. First glacial episode occurred after 750 Ma |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Tonian System |
1000 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Mesoproterozoic Era |
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Stenian System |
1200 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Ectasian System |
1400 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Calymmian System |
1600 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Paleoproterozoic Era |
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Statherian System |
1800 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Orosirian System |
2050 |
Defined chronometrically |
|
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Rhyacian System |
2300 |
Defined chronometrically |
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|
Ratified 1990 |
Episodes 14/2,1991 |
|
Siderian System |
2500 |
Defined chronometrically, but it will be replaced by GSSP |
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|
Ratified 1990 |
Episodes 14/2,1991 |
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Archean Eon |
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|
Neoarchean Era |
2800 |
Defined chronometrically |
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|
|
Subcomm. decision 1996, but not submitted to ICS |
Informally in Episodes 15/2, 1992 |
|
Mesoarchean Era |
3200 |
Defined chronometrically |
|
|
|
Subcomm. decision 1996, but not submitted to ICS |
Informally in Episodes 15/2, 1992 |
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Paleoarchean Era |
3600 |
Defined chronometrically |
|
|
|
Subcomm. decision 1996, but not submitted to ICS |
Informally in Episodes 15/2, 1992 |
|
Eoarchean Era |
4000 |
Base is not defined |
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|
|
Subcomm. decision 1996, but not submitted to ICS |
Informally in Episodes 15/2, 1992 |
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Hadean Eon |
~4600 |
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|
Formation of planet Earth. Informal term |
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