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. A. Lillegraven and M. C. McKenna. 1986. Fossil mammals from the "Mesaverde" Formation (Late Cretaceous, Judithian) of the Bighorn and Wind River basins, Wyoming, with definitions of Late Cretaceous North American Land-Mammal "Ages". American Museum Novitates 2840:1-68 view
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 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
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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
- M. Freudenthal. 2006. Mammal Paleogene zones. personal communication 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.
This timescale is used in the definition of 126884 collections
International Chronostratigraphic Timescale | Cretaceous North American Land-Mammal Ages | Silurian of North America | European Faunal Units | Carboniferous of China | Neogene Mammal Ages of China | Mammal Paleogene Zones | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Late Pleistocene | Nihewanian | 0.0117 | ||||||||
Chibanian | 0.129 | |||||||||||
Calabrian | 0.774 | |||||||||||
Gelasian | 1.8 | |||||||||||
Neogene | Pliocene | Piacenzian | Villanyian | Yushean | 2.58 | |||||||
Ruscinian | 3.1 * | |||||||||||
Zanclean | 3.6 | |||||||||||
Baodean | 4.9 | |||||||||||
Miocene | Messinian | Turolian | 5.333 | |||||||||
Tortonian | 7.246 | |||||||||||
Vallesian | 8.7 | |||||||||||
Tunggurian | 11.1 | |||||||||||
Serravallian | Astaracian | 11.63 | ||||||||||
Langhian | Shanwangian | 13.82 | ||||||||||
Burdigalian | Orleanian | 15.98 | ||||||||||
Xiejiaan | 16.9 | |||||||||||
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 | Lancian/Edmontonian | 66 | ||||||||
Campanian | Judithian/Aquilan | 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 | |||||||||||
Permian | Lopingian | Changhsingian | 251.902 | |||||||||
Wuchiapingian | 254.14 | |||||||||||
Guadalupian | Capitanian | 259.51 | ||||||||||
Wordian | 264.28 | |||||||||||
Roadian | 266.9 | |||||||||||
Cisuralian | Kungurian | 273.01 | ||||||||||
Artinskian | 283.5 | |||||||||||
Sakmarian | 290.1 | |||||||||||
Asselian | 293.52 | |||||||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | |||||||||
Xiaodushanian | 300 * | |||||||||||
Kasimovian | 303.7 | |||||||||||
Dalaun | 305.8 * | |||||||||||
Moscovian | 307 | |||||||||||
Bashkirian | 315.2 | |||||||||||
Huashibanian | 318.5 * | |||||||||||
Lousuan | 321.2 * | |||||||||||
Mississippian | Serpukhovian | Dewunian | 323.2 | |||||||||
Shangsian | 330.8 * | |||||||||||
Visean | 330.9 | |||||||||||
Jiusian | 335 * | |||||||||||
Tournaisian | Tangbagouan | 346.7 | ||||||||||
Devonian | Late Devonian | Famennian | 358.9 | |||||||||
Frasnian | 372.2 | |||||||||||
Middle Devonian | Givetian | 382.7 | ||||||||||
Eifelian | 387.7 | |||||||||||
Early Devonian | Emsian | 393.3 | ||||||||||
Pragian | 407.6 | |||||||||||
Lochkovian | 410.8 | |||||||||||
Silurian | Pridoli | Cayugan | 419.2 | |||||||||
Niagaran | 422.5 * | |||||||||||
Ludlow | Ludfordian | 423 | ||||||||||
Gorstian | 425.6 | |||||||||||
Wenlock | Homerian | Lockportian | 427.4 | |||||||||
Sheinwoodian | 430.5 | |||||||||||
Llandovery | Telychian | Ontarian | 433.4 | |||||||||
Aeronian | 438.5 | |||||||||||
Alexandrian | 438.7 * | |||||||||||
Medinan | Clinton | 440.1 * | ||||||||||
440.7 * | ||||||||||||
Rhuddanian | 440.8 | |||||||||||
443.8 |