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
- 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
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- P. L. Gibbard, M. J. Head, and M. J. C. Walker. 2010. Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma. Journal of Quaternary Science 25(2):96-102 view
- A. D. Barnosky, M. Holmes, R. Kirchholtes, E. Lindsey, K.C. Maguire, A.W. Poust, M.A. Stegner, J. Sunseri, B. Swartz, J. Swift, N.A. Villavicencio and G. Wogan. 2014. Prelude to the Anthropocene: Two new North American Land Mammal Ages (NALMAs). The Anthropocene Review I(3):225-242 view
- W. B. Harland, R. L. Armstrong, A. V. Cox, L. E. Craig, A. G. Smith and D. G. Smith. 1990. A Geologic Time Scale 1989. view
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- Z.-X. Qiu and Z.-D. Qiu. 1995. Chronological sequence and subdivision of Chinese Neogene mammalian faunas. Palaeogeography, Palaeoclimatology, Palaeoecology 116(1-2):41-70 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
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 128057 collections
International Chronostratigraphic Timescale | Ammonite Chrons of Northwest Europe | Permian of North America | Permian of Western Europe | Cenozoic Subepochs of Southern Europe | North American Land Mammal Ages | Cenozoic Subepochs | Neogene Mammal Ages of China | Permian of the Salt Range | European Faunal Units | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Saintaugustinean | 0 | ||||||||||
Santarosean | 0.0004 | |||||||||||||
Northgrippian | 0.0042 | |||||||||||||
Greenlandian | 0.0082 | |||||||||||||
Pleistocene | Late Pleistocene | Tarantian | Late Pleistocene | Nihewanian | 0.0117 | |||||||||
Rancholabrean | 0.014 | |||||||||||||
Chibanian | Ionian | Middle Pleistocene | 0.129 | |||||||||||
Irvingtonian | 0.21 | |||||||||||||
Calabrian | Early Pleistocene | 0.774 | ||||||||||||
Blancan | 1.4 | |||||||||||||
Gelasian | 1.8 | |||||||||||||
Neogene | Pliocene | Piacenzian | Late Pliocene | Yushean | Villanyian | 2.58 | ||||||||
Ruscinian | 3.1 * | |||||||||||||
Zanclean | Early Pliocene | 3.6 | ||||||||||||
Hemphillian | 4.7 | |||||||||||||
Baodean | 4.9 | |||||||||||||
Miocene | Messinian | Late Miocene | Turolian | 5.333 | ||||||||||
Tortonian | 7.246 | |||||||||||||
Vallesian | 8.7 | |||||||||||||
Clarendonian | 9.4 | |||||||||||||
Tunggurian | 11.1 | |||||||||||||
Serravallian | Middle Miocene | Astaracian | 11.63 | |||||||||||
Barstovian | 12.5 | |||||||||||||
Langhian | Shanwangian | 13.82 | ||||||||||||
Burdigalian | Early Miocene | Orleanian | 15.98 | |||||||||||
Hemingfordian | 16.3 | |||||||||||||
Xiejiaan | 16.9 | |||||||||||||
Arikareean | 18.5 | |||||||||||||
Agenian | 20 | |||||||||||||
Aquitanian | 20.44 | |||||||||||||
Paleogene | Oligocene | Chattian | Late Oligocene | 23.03 | ||||||||||
Rupelian | Early Oligocene | 27.82 | ||||||||||||
Whitneyan | 29.5 | |||||||||||||
Orellan | 31.8 | |||||||||||||
Eocene | Priabonian | Chadronian | Late Eocene | 33.9 | ||||||||||
Duchesnean | 37 | |||||||||||||
Bartonian | Middle Eocene | 37.71 | ||||||||||||
Uintan | 39.7 | |||||||||||||
Lutetian | 41.2 | |||||||||||||
Bridgerian | 46.2 | |||||||||||||
Ypresian | Early Eocene | 47.8 | ||||||||||||
Wasatchian | 50.5 | |||||||||||||
Clarkforkian | 54.9 | |||||||||||||
Paleocene | Thanetian | Late Paleocene | 56 | |||||||||||
Tiffanian | 56.2 | |||||||||||||
Selandian | Middle Paleocene | 59.2 | ||||||||||||
Torrejonian | 60.9 | |||||||||||||
Danian | Early Paleocene | 61.6 | ||||||||||||
Puercan | 63.8 | |||||||||||||
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 | 145 | |||||||||||
Kimmeridgian | 149.2 | |||||||||||||
Oxfordian | 154.8 | |||||||||||||
Middle Jurassic | Callovian | 161.5 | ||||||||||||
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 | ||||||||||
180.1 | ||||||||||||||
Serpentinum/Falciferum/Tenuicostatum | 182 | |||||||||||||
Pliensbachian | Spinatum/Margaritatus/Davoei/Ibex/Jamesoni | 184.2 | ||||||||||||
Sinemurian | Raricostatum/Oxynotum/Obtusum/Turneri/Semicostatum/Bucklandi | 192.9 | ||||||||||||
Hettangian | Angulata/Liasicus/Planorbis | 199.5 | ||||||||||||
Triassic | Late Triassic | Rhaetian | 201.4 | |||||||||||
Norian | 208.5 | |||||||||||||
Carnian | 227 | |||||||||||||
Middle Triassic | Ladinian | 237 | ||||||||||||
Anisian | 242 | |||||||||||||
Early Triassic | Olenekian | 247.2 | ||||||||||||
Induan | 251.2 | |||||||||||||
Kathwai | 251.5 * | |||||||||||||
Permian | Lopingian | Changhsingian | 251.902 | |||||||||||
252.4 * | ||||||||||||||
Chhidru | 252.9 * | |||||||||||||
Wuchiapingian | Zechstein | 254.14 | ||||||||||||
Kalabagh | 255 * | |||||||||||||
Wargal | 256 * | |||||||||||||
Guadalupian | Capitanian | Capitanian | Rotliegendes | 259.51 | ||||||||||
Wordian | Wordian | 264.28 | ||||||||||||
265.3 * | ||||||||||||||
Amb | 266.1 * | |||||||||||||
Roadian | Roadian | 266.9 | ||||||||||||
270.7 * | ||||||||||||||
Cisuralian | Kungurian | Leonardian | Cathedralian | 273.01 | ||||||||||
Hessian | 281.9 * | |||||||||||||
Artinskian | Autunian | 283.5 | ||||||||||||
Wolfcampian | Lenoxian | 286.1 * | ||||||||||||
Sakmarian | 290.1 | |||||||||||||
Asselian | Nealian | 293.52 | ||||||||||||
298.9 |