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
- 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. 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
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 126849 collections
International Chronostratigraphic Timescale | Cambrian of Australia | Permian of the Russian Platform | Devonian of Germany | Cambrian of North America | European Faunal Zones | |||||
---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Gelasian | MN 17 | 1.8 | ||||||
Neogene | Pliocene | Piacenzian | MN 16 | 2.58 | ||||||
MN 15 | 3.2 | |||||||||
Zanclean | 3.6 | |||||||||
MN 14 | 4.2 | |||||||||
MN 13 | 4.9 | |||||||||
Miocene | Messinian | 5.333 | ||||||||
Tortonian | MN 12 | 7.246 | ||||||||
MN 11 | 7.75 | |||||||||
MN 10 | 8.7 | |||||||||
MN 9 | 9.7 | |||||||||
MN 7 + 8 | 11.1 | |||||||||
Serravallian | 11.63 | |||||||||
MN 6 | 12.8 * | |||||||||
Langhian | MN 5 | 13.82 | ||||||||
Burdigalian | MN 4 | 15.98 | ||||||||
MN 3 | 16.9 | |||||||||
MN 2 | 20 | |||||||||
Aquitanian | 20.44 | |||||||||
MN 1 | 22.4 | |||||||||
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 | 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 | 251.902 | |||||||
Wuchiapingian | 254.14 | |||||||||
Tatarian | Vyatkian | 256.8 * | ||||||||
Guadalupian | Capitanian | Severodvinian | 259.51 | |||||||
Wordian | Urzhumian | 264.28 | ||||||||
Roadian | Kazanian | Povolzhian | 266.9 | |||||||
Sokian | 270.7 * | |||||||||
Cisuralian | Kungurian | Kungurian | Irenian/Ufimian | 273.01 | ||||||
Filipovian | 276.5 * | |||||||||
Saraninian | 280.1 * | |||||||||
Artinskian | Artinskian | Sarginian | 283.5 | |||||||
Irginian | 285.9 * | |||||||||
Burtsevian | 287.8 * | |||||||||
Sakmarian | Sakmarian | Sterlitamakian | 290.1 | |||||||
Tastubian | 291.7 * | |||||||||
Asselian | Asselian | Shikhanian | 293.52 | |||||||
Uskalykian | 294.8 | |||||||||
Surenian | 297.5 | |||||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | |||||||
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 | Givetian | 382.7 | |||||||
Eifelian | Eifelian | 387.7 | ||||||||
Early Devonian | Emsian | Emsian | 393.3 | |||||||
Pragian | Siegen | 407.6 | ||||||||
Lochkovian | Gedinnine | 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 | Datsonian | Franconian †/Dresbachian/Millardan | 485.4 | |||||
Payntonian | 486.8 * | |||||||||
Sunwaptan | 487.5 | |||||||||
Jiangshanian | Iverian | 489.5 | ||||||||
Steptoean | 493 * | |||||||||
Paibian | Idamean | 494 | ||||||||
Miaolingian | Guzhangian | Mindyallan | Marjumian | Albertian † | 497 | |||||
Boomerangian | 499 | |||||||||
Drumian | Undillan | 500.5 | ||||||||
Floran | 503 | |||||||||
Wuliuan | Templetonian | Topazan | 504.5 | |||||||
Delamaran | 506.5 | |||||||||
Ordian | 507.8 * | |||||||||
Series 2 | Stage 4 | Waucoban † | 509 | |||||||
510.8 * | ||||||||||
Dyeran | 511 * | |||||||||
Stage 3 | 514 | |||||||||
Montezuman | 514.8 * | |||||||||
Begadean | 519.9 * | |||||||||
Terreneuvian | Stage 2 | 521 | ||||||||
Fortunian | 529 | |||||||||
538.8 |