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
- 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
- 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
- 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
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 126701 collections
International Chronostratigraphic Timescale | Ordovician of Australia | Carbo-Permian of the Russian Platform | European Faunal Units | Devonian Subages | Carboniferous of Western Europe | North American Land Mammal Ages | ||||
---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Saintaugustinean | 0 | ||||||
Santarosean | 0.0004 | |||||||||
Northgrippian | 0.0042 | |||||||||
Greenlandian | 0.0082 | |||||||||
Pleistocene | Late Pleistocene | 0.0117 | ||||||||
Rancholabrean | 0.014 | |||||||||
Chibanian | 0.129 | |||||||||
Irvingtonian | 0.21 | |||||||||
Calabrian | 0.774 | |||||||||
Blancan | 1.4 | |||||||||
Gelasian | 1.8 | |||||||||
Neogene | Pliocene | Piacenzian | Villanyian | 2.58 | ||||||
Ruscinian | 3.1 * | |||||||||
Zanclean | 3.6 | |||||||||
Hemphillian | 4.7 | |||||||||
Miocene | Messinian | Turolian | 5.333 | |||||||
Tortonian | 7.246 | |||||||||
Vallesian | 8.7 | |||||||||
Clarendonian | 9.4 | |||||||||
Serravallian | Astaracian | 11.63 | ||||||||
Barstovian | 12.5 | |||||||||
Langhian | 13.82 | |||||||||
Burdigalian | Orleanian | 15.98 | ||||||||
Hemingfordian | 16.3 | |||||||||
Arikareean | 18.5 | |||||||||
Agenian | 20 | |||||||||
Aquitanian | 20.44 | |||||||||
Paleogene | Oligocene | Chattian | 23.03 | |||||||
Rupelian | 27.82 | |||||||||
Whitneyan | 29.5 | |||||||||
Orellan | 31.8 | |||||||||
Eocene | Priabonian | Chadronian | 33.9 | |||||||
Duchesnean | 37 | |||||||||
Bartonian | 37.71 | |||||||||
Uintan | 39.7 | |||||||||
Lutetian | 41.2 | |||||||||
Bridgerian | 46.2 | |||||||||
Ypresian | 47.8 | |||||||||
Wasatchian | 50.5 | |||||||||
Clarkforkian | 54.9 | |||||||||
Paleocene | Thanetian | 56 | ||||||||
Tiffanian | 56.2 | |||||||||
Selandian | 59.2 | |||||||||
Torrejonian | 60.9 | |||||||||
Danian | 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 | |||||||||
Permian | Lopingian | Changhsingian | Melekhovian | 251.902 | ||||||
Wuchiapingian | 254.14 | |||||||||
Guadalupian | Capitanian | 259.51 | ||||||||
Wordian | 264.28 | |||||||||
Noginskian | 264.9 * | |||||||||
Roadian | 266.9 | |||||||||
Cisuralian | Kungurian | 273.01 | ||||||||
Pavlovoposadian | 276.8 * | |||||||||
Artinskian | 283.5 | |||||||||
Rusavkinian | 287.6 * | |||||||||
Sakmarian | 290.1 | |||||||||
Asselian | 293.52 | |||||||||
Kuzel | 297.7 | |||||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | |||||||
Stephanian | Stephanian C | 300.3 * | ||||||||
Stephanian B | 300.9 * | |||||||||
Stephanian A | 301.4 * | |||||||||
Kasimovian | Dorogomilovian | 303.7 | ||||||||
Khamovnikian | 304.8 | |||||||||
Cantabrian | 305 * | |||||||||
Krevyakinian | 305.8 * | |||||||||
Moscovian | Myachkovian | 307 | ||||||||
Westphalian | Westphalian D | 307.4 * | ||||||||
Podolskian | 308.9 * | |||||||||
Westphalian C | 309.8 | |||||||||
Kashirian | 311.4 * | |||||||||
Vereian | 313.8 | |||||||||
Westphalian B | 314.6 | |||||||||
Melekessian | 314.8 | |||||||||
Bashkirian | 315.2 | |||||||||
Cheremshanian | 316.9 * | |||||||||
Westphalian A | 317 * | |||||||||
Prikamian | 318.6 * | |||||||||
Namurian | Yeadonian | 318.8 * | ||||||||
Severokeltmian | 319.9 * | |||||||||
Marsdenian | 320.2 * | |||||||||
Krasnopolyanian | 321.2 * | |||||||||
Kinderscoutian | 321.5 * | |||||||||
Voznesenian | 321.9 * | |||||||||
Alportian | 322 * | |||||||||
Chokierian | 323.1 * | |||||||||
Mississippian | Serpukhovian | Zapaltjubian | 323.2 | |||||||
Arnsbergian | 324 * | |||||||||
Protvian | 324.4 * | |||||||||
Steshevian | 326.8 * | |||||||||
Pendleian | 327.4 * | |||||||||
Tarusian | 329 * | |||||||||
Visean | Venevian | Warnantian | Brigantian † | 330.9 | ||||||
Mikhailovian | 331.9 * | |||||||||
Aleksinian | 333.7 * | |||||||||
Tulian | 335.8 * | |||||||||
Livian | Asbian † | 336.3 * | ||||||||
Bobrikian | 339.9 * | |||||||||
Moliniacian | Holkerian †/Arundian/Chadian | 340.2 * | ||||||||
Radaevkian | 343.4 * | |||||||||
Tournaisian | Kosvian | Ivorian | 346.7 | |||||||
Kizelian | 350.7 * | |||||||||
Cherepetian | 351.9 * | |||||||||
Hastarian | 353.7 * | |||||||||
Karakubian | 354.4 * | |||||||||
Upinian | 356.3 * | |||||||||
Malevkian | 357.6 * | |||||||||
Gumerovian | 358 * | |||||||||
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 * | |||||||||
Silurian | Pridoli | 419.2 | ||||||||
Ludlow | Ludfordian | 423 | ||||||||
Gorstian | 425.6 | |||||||||
Wenlock | Homerian | 427.4 | ||||||||
Sheinwoodian | 430.5 | |||||||||
Llandovery | Telychian | 433.4 | ||||||||
Aeronian | 438.5 | |||||||||
Rhuddanian | 440.8 | |||||||||
Ordovician | Late Ordovician | Hirnantian | Bolindian | 443.8 | ||||||
Katian | 445.2 | |||||||||
Eastonian | 449 * | |||||||||
Gisbornian | 452 * | |||||||||
Sandbian | 453 | |||||||||
Middle Ordovician | Darriwilian | Darriwilian | 458.4 | |||||||
Dapingian | Yapeenian | 467.3 | ||||||||
Castlemainian | 468.5 * | |||||||||
Early Ordovician | Floian | Chewtonian | 470 | |||||||
Bendigonian | 471.8 * | |||||||||
Lancefieldian | 473.5 * | |||||||||
Tremadocian | 477.7 | |||||||||
Warendian | 482.8 * | |||||||||
485.4 |