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
- 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
- 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, 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
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 127057 collections
International Chronostratigraphic Timescale | Obsolete Names for ICS Units | Cretaceous North American Land-Mammal Ages | Devonian of Czechoslovakia | Permian of China | Devonian of Germany | Permian of Western Europe | Neogene Mammal Ages of China | Silurian of the Baltic | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Late Pleistocene | Nihewanian | 0.0117 | |||||||||
Chibanian | 0.129 | ||||||||||||
Calabrian | 0.774 | ||||||||||||
Gelasian | 1.8 | ||||||||||||
Neogene | Pliocene | Piacenzian | Tertiary † | Yushean | 2.58 | ||||||||
Zanclean | 3.6 | ||||||||||||
Baodean | 4.9 | ||||||||||||
Miocene | Messinian | 5.333 | |||||||||||
Tortonian | 7.246 | ||||||||||||
Tunggurian | 11.1 | ||||||||||||
Serravallian | 11.63 | ||||||||||||
Langhian | Shanwangian | 13.82 | |||||||||||
Burdigalian | 15.98 | ||||||||||||
Xiejiaan | 16.9 | ||||||||||||
Aquitanian | 20.44 | ||||||||||||
Paleogene | Oligocene | Chattian | 23.03 | ||||||||||
Rupelian | 27.82 | ||||||||||||
Eocene | Priabonian | 33.9 | |||||||||||
Bartonian | 37.71 | ||||||||||||
Lutetian | 41.2 | ||||||||||||
Ypresian | 47.8 | ||||||||||||
Paleocene | Thanetian | 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 | Meishanian | 251.902 | |||||||||
Baoqingian | 253.4 * | ||||||||||||
Wuchiapingian | Longtanian † | Laoshanian | Zechstein | 254.14 | |||||||||
Laibinian | 257.7 * | ||||||||||||
Guadalupian | Capitanian | Lengwuan | Rotliegendes | 259.51 | |||||||||
Wordian | Kuhfengian | 264.28 | |||||||||||
Roadian | 266.9 | ||||||||||||
Cisuralian | Kungurian | Luodianian | 273.01 | ||||||||||
Artinskian | Autunian | 283.5 | |||||||||||
Longlinian | 285.4 * | ||||||||||||
Sakmarian | 290.1 | ||||||||||||
Asselian | Zisongian | 293.52 | |||||||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | ||||||||||
300.1 | |||||||||||||
Kasimovian | 303.7 | ||||||||||||
Moscovian | 307 | ||||||||||||
Bashkirian | 315.2 | ||||||||||||
Mississippian | Serpukhovian | 323.2 | |||||||||||
Visean | 330.9 | ||||||||||||
Tournaisian | 346.7 | ||||||||||||
Devonian | Late Devonian | Famennian | Wocklum/Dasberg/Hemberg/Nehden | 358.9 | |||||||||
Frasnian | Adorf | 372.2 | |||||||||||
Middle Devonian | Givetian | Srbsko | Givetian | 382.7 | |||||||||
Eifelian | Chotec | Eifelian | 387.7 | ||||||||||
Early Devonian | Emsian | Daleje/Zlichovian | Emsian | 393.3 | |||||||||
Pragian | Pragian | Siegen | 407.6 | ||||||||||
Lochkovian | Lochkovian | Gedinnine | 410.8 | ||||||||||
Silurian | Pridoli | Ohesaare | 419.2 | ||||||||||
Kaugetuma | 421.7 * | ||||||||||||
Ludlow | Ludfordian | Kuressaare | 423 | ||||||||||
Paadla | 423.4 * | ||||||||||||
Gorstian | 425.6 | ||||||||||||
Wenlock | Homerian | Rootsikula | 427.4 | ||||||||||
Jaagarahu | 429.2 * | ||||||||||||
Sheinwoodian | 430.5 | ||||||||||||
Jaani | 431.8 * | ||||||||||||
Llandovery | Telychian | 433.4 | |||||||||||
Adavere | 434 * | ||||||||||||
Aeronian | 438.5 | ||||||||||||
Raikkula | 439.4 * | ||||||||||||
Rhuddanian | 440.8 | ||||||||||||
Juuru | 441.4 * | ||||||||||||
Ordovician | Late Ordovician | Hirnantian | 443.8 | ||||||||||
Katian | 445.2 | ||||||||||||
Sandbian | 453 | ||||||||||||
Middle Ordovician | Darriwilian | 458.4 | |||||||||||
Dapingian | 467.3 | ||||||||||||
Early Ordovician | Floian | 470 | |||||||||||
Tremadocian | 477.7 | ||||||||||||
Cambrian | Furongian | Stage 10 | 485.4 | ||||||||||
Jiangshanian | 489.5 | ||||||||||||
Paibian | 494 | ||||||||||||
Miaolingian | Guzhangian | Series 3 † | 497 | ||||||||||
Drumian | 500.5 | ||||||||||||
Wuliuan | Stage 5 † | 504.5 | |||||||||||
509 |