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, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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
- 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 128028 collections
International Chronostratigraphic Timescale | Carboniferous of North America | 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 | Late Pleistocene | Nihewanian | 0.0117 | |||||
Rancholabrean | 0.014 | ||||||||
Chibanian | 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 | 168.2 | ||||||||
Aalenian | 170.9 | ||||||||
Early Jurassic | Toarcian | 174.7 | |||||||
Pliensbachian | 184.2 | ||||||||
Sinemurian | 192.9 | ||||||||
Hettangian | 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 | 254.14 | ||||||||
Kalabagh | 255 * | ||||||||
Wargal | 256 * | ||||||||
Guadalupian | Capitanian | 259.51 | |||||||
Wordian | 264.28 | ||||||||
265.3 * | |||||||||
Amb | 266.1 * | ||||||||
Roadian | 266.9 | ||||||||
270.7 * | |||||||||
Cisuralian | Kungurian | 273.01 | |||||||
Artinskian | 283.5 | ||||||||
Sakmarian | 290.1 | ||||||||
Asselian | Bursumian † | 293.52 | |||||||
Carboniferous | Pennsylvanian | Gzhelian | Virgilian | 298.9 | |||||
Kasimovian | Missourian | 303.7 | |||||||
Desmoinesian | 305.9 * | ||||||||
Moscovian | 307 | ||||||||
Atokan | 312.7 * | ||||||||
Bashkirian | 315.2 | ||||||||
Morrowan | 318.4 * | ||||||||
Mississippian | Serpukhovian | Chesterian | 323.2 | ||||||
Visean | 330.9 | ||||||||
Meramecian | 335.8 * | ||||||||
Osagean | 343.1 * | ||||||||
Tournaisian | 346.7 | ||||||||
Kinderhookian | 351.9 * | ||||||||
358.9 |