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. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- J. Meng and M. C. McKenna. 1998. Faunal turnovers of Paleogene mammals from the Mongolian Plateau. Nature 394:364-367 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. 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 126762 collections
International Chronostratigraphic Timescale | Cambrian of West Avalonia | Carboniferous of North America | Paleogene Mammal Ages of Asia | Cambrian of Britain | Permian of the Pamirs | Cambrian Epochs | European Faunal Units | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Neogene | Pliocene | Piacenzian | Villanyian | 2.58 | ||||||||
Ruscinian | 3.1 * | |||||||||||
Zanclean | 3.6 | |||||||||||
Miocene | Messinian | Turolian | 5.333 | |||||||||
Tortonian | 7.246 | |||||||||||
Vallesian | 8.7 | |||||||||||
Serravallian | Astaracian | 11.63 | ||||||||||
Langhian | 13.82 | |||||||||||
Burdigalian | Orleanian | 15.98 | ||||||||||
Agenian | 20 | |||||||||||
Aquitanian | 20.44 | |||||||||||
Paleogene | Oligocene | Chattian | Tabenbulakian | Hsandagolian | 23.03 | |||||||
Rupelian | Kekeamuan | 27.82 | ||||||||||
Eocene | Priabonian | Houldjinian/Ergilian/Ulangochuian | 33.9 | |||||||||
Bartonian | Sharamurunian/Irdinmanhan/Arshantan | 37.71 | ||||||||||
Lutetian | 41.2 | |||||||||||
Ypresian | Bumbanian | 47.8 | ||||||||||
Paleocene | Thanetian | Gashatan | 56 | |||||||||
Selandian | 59.2 | |||||||||||
Danian | 61.6 | |||||||||||
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 | Dorashamian | 251.902 | ||||||||
Wuchiapingian | Dzhulfian | 254.14 | ||||||||||
Guadalupian | Capitanian | Midian | 259.51 | |||||||||
Wordian | 264.28 | |||||||||||
Murgabian | 266.2 * | |||||||||||
Roadian | 266.9 | |||||||||||
Cisuralian | Kungurian | Kubergandian | 273.01 | |||||||||
Bolorian | 279.8 | |||||||||||
Artinskian | 283.5 | |||||||||||
Yakhtashian | 286 | |||||||||||
Sakmarian | Sakmarian | 290.1 | ||||||||||
Asselian | Bursumian † | Asselian | 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 * | |||||||||||
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 | 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 | 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 | Merioneth | Dolgellian/Trempealeauan | Late Cambrian | 485.4 | ||||||
Festiniogian | 489.2 * | |||||||||||
Jiangshanian | 489.5 | |||||||||||
Maentwrogian | 493.1 * | |||||||||||
Paibian | 494 | |||||||||||
Miaolingian | Guzhangian | St Davids | Middle Cambrian | 497 | ||||||||
Arcadian | 498.4 | |||||||||||
Drumian | 500.5 | |||||||||||
Wuliuan | 504.5 | |||||||||||
Series 2 | Stage 4 | Branchian | Caerfai | Early Cambrian | 509 | |||||||
Stage 3 | 514 | |||||||||||
Placentian | 517.1 | |||||||||||
Terreneuvian | Stage 2 | 521 | ||||||||||
Fortunian | 529 | |||||||||||
538.8 |