International Chronostratigraphic Timescale
The interval definitions in this timescale are derived from the following sources:
- K. M. Cohen, S.C. Finney, P.L. Gibbard and J.-X. Fan. 2023. The ICS International Chronostratigraphic Chart v2023/09. view
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- J. I. Raine, A. G. Beu, A. F. Boyes, H. J. Campbell, R. A. Cooper, J. S. Crampton, M. P. Crundwell, C. J. Hollis, and H. E. G. Morgans. 2015. Revised Calibration of the New Zealand Geological Timescale: NZGT2015/1. GNS Science Report 2012(39) view
- F. F. Steininger, W. A. Berggren, D. V. Kent, R. L. Bernor, S. Sen and J. Agusti. 1996. Circum-Mediterranean Neogene (Miocene and Pliocene) marine-continental chronologic correlations of European mammal units. The Evolution of Western Eurasian Neogene Mammal Faunas (eds. R. L. Bernor, V. Fahlbusch, and H.-W. Mittmann) view
- M. Freudenthal. 2006. Mammal Paleogene zones. personal communication view
- J. Palfy, P. L. Smith, and J. K. Mortensen. 2000. A U-Pb and 40Ar/39Ar time scale for the Jurassic. Canadian Journal of Earth Sciences 37(6):923-944 view
There are 59 timescales which overlap this one. show
Interval boundaries marked with * have been interpolated based on the differences between the ages for international timescale boundaries quoted in the source and the currently accepted ages for those boundaries.
Interval names marked with † are no longer in current use.
This timescale is used in the definition of 126844 collections
International Chronostratigraphic Timescale | Permian of Western Europe | Permian-Jurassic of New Zealand | European Faunal Units | Mammal Paleogene Zones | Ammonite Chrons of Northwest Europe | Devonian Subages | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Neogene | Pliocene | Piacenzian | Villanyian | 2.58 | ||||||||
Ruscinian | 3.1 * | |||||||||||
Zanclean | 3.6 | |||||||||||
Miocene | Messinian | Turolian | 5.333 | |||||||||
Tortonian | 7.246 | |||||||||||
Vallesian | 8.7 | |||||||||||
Serravallian | Astaracian | 11.63 | ||||||||||
Langhian | 13.82 | |||||||||||
Burdigalian | Orleanian | 15.98 | ||||||||||
Agenian | 20 | |||||||||||
Aquitanian | 20.44 | |||||||||||
Paleogene | Oligocene | Chattian | MP 30/MP 29/MP 28/MP 27/MP 26 | MP 25 | 23.03 | |||||||
Rupelian | MP 24/MP 23/MP 22/MP 21 | 27.82 | ||||||||||
Eocene | Priabonian | MP 20/MP 19/MP 18/MP 17B/MP 17A | 33.9 | |||||||||
Bartonian | MP 16 | 37.71 | ||||||||||
Lutetian | MP 15/MP 14/MP 13/MP 12/MP 11 | 41.2 | ||||||||||
Ypresian | MP 10/MP 8 + 9/MP 7 | 47.8 | ||||||||||
Paleocene | Thanetian | MP 6 | MP 1 - 5 | 56 | ||||||||
Selandian | 59.2 | |||||||||||
Danian | 61.6 | |||||||||||
Cretaceous | Late Cretaceous | Maastrichtian | 66 | |||||||||
Campanian | 72.1 | |||||||||||
Santonian | 83.6 | |||||||||||
Coniacian | 86.3 | |||||||||||
Turonian | 89.8 | |||||||||||
Cenomanian | 93.9 | |||||||||||
Early Cretaceous | Albian | 100.5 | ||||||||||
Aptian | 113 | |||||||||||
Barremian | 121.4 | |||||||||||
Hauterivian | 125.77 | |||||||||||
Valanginian | 132.6 | |||||||||||
Berriasian | 139.8 | |||||||||||
Jurassic | Late Jurassic | Tithonian | Oteke | Puaroan | 145 | |||||||
Kimmeridgian | 149.2 | |||||||||||
Kawhia | Ohauan | 150 | ||||||||||
Heterian | 154.5 | |||||||||||
Oxfordian | 154.8 | |||||||||||
Middle Jurassic | Callovian | 161.5 | ||||||||||
Temaikan | 164.3 | |||||||||||
Bathonian | 165.3 | |||||||||||
Bajocian | Parkinsoni/Garantiana/Subfurcatum/Sauzei/Laeviuscula/Discites | 168.2 | ||||||||||
Humphresianum | 168.4 | |||||||||||
Aalenian | Concavum/Murchisonae/Opalinum | 170.9 | ||||||||||
Early Jurassic | Toarcian | Levesquei/Variabilis/Bifrons | Thouarsense | 174.7 | ||||||||
Herangi | Ururoan | 176 | ||||||||||
180.1 | ||||||||||||
Serpentinum/Falciferum/Tenuicostatum | 182 | |||||||||||
Pliensbachian | Spinatum/Margaritatus/Davoei/Ibex/Jamesoni | 184.2 | ||||||||||
Aratauran | 188.9 | |||||||||||
Sinemurian | Raricostatum/Oxynotum/Obtusum/Turneri/Semicostatum/Bucklandi | 192.9 | ||||||||||
Hettangian | Angulata/Liasicus/Planorbis | 199.5 | ||||||||||
Triassic | Late Triassic | Rhaetian | Balfour | Otapirian | 201.4 | |||||||
Norian | Warepan | 208.5 | ||||||||||
Otamitan | 217 | |||||||||||
Oretian | 221 | |||||||||||
Carnian | 227 | |||||||||||
Gore | Kaihikuan | 227.5 | ||||||||||
Middle Triassic | Ladinian | 237 | ||||||||||
Etalian | 238 | |||||||||||
Anisian | 242 | |||||||||||
Malakovian | 246 | |||||||||||
Early Triassic | Olenekian | 247.2 | ||||||||||
Nelsonian | 249 | |||||||||||
Induan | 251.2 | |||||||||||
DUrville | Makarewan | 251.5 | ||||||||||
Permian | Lopingian | Changhsingian | 251.902 | |||||||||
Waiitian | 253.2 | |||||||||||
Wuchiapingian | Zechstein | 254.14 | ||||||||||
Puruhauan | 254.2 | |||||||||||
Guadalupian | Capitanian | Rotliegendes | Aparima | Flettian | 259.51 | |||||||
Wordian | 264.28 | |||||||||||
Barettian | 266 | |||||||||||
Roadian | 266.9 | |||||||||||
Cisuralian | Kungurian | 273.01 | ||||||||||
Mangapirian | 276 | |||||||||||
Artinskian | Autunian | 283.5 | ||||||||||
Telfordian | 285 | |||||||||||
288.5 | ||||||||||||
Sakmarian | 290.1 | |||||||||||
Asselian | 293.52 | |||||||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | |||||||||
Kasimovian | 303.7 | |||||||||||
Moscovian | 307 | |||||||||||
Bashkirian | 315.2 | |||||||||||
Mississippian | Serpukhovian | 323.2 | ||||||||||
Visean | 330.9 | |||||||||||
Tournaisian | 346.7 | |||||||||||
Devonian | Late Devonian | Famennian | Late Famennian | 358.9 | ||||||||
Middle Famennian | 365.3 * | |||||||||||
Early Famennian | 368.5 * | |||||||||||
Frasnian | Late Frasnian | 372.2 | ||||||||||
Middle Frasnian | 375.4 * | |||||||||||
Early Frasnian | 379.3 * | |||||||||||
Middle Devonian | Givetian | Late Givetian | 382.7 | |||||||||
Middle Givetian | 383.7 * | |||||||||||
Early Givetian | 385.9 * | |||||||||||
Eifelian | Late Eifelian | 387.7 | ||||||||||
Early Eifelian | 390.3 * | |||||||||||
Early Devonian | Emsian | Late Emsian | 393.3 | |||||||||
Early Emsian | 398.3 * | |||||||||||
Pragian | Pragian | 407.6 | ||||||||||
Lochkovian | Late Lochkovian | 410.8 | ||||||||||
Middle Lochkovian | 412.8 * | |||||||||||
Early Lochkovian | 415.6 * | |||||||||||
419.2 |