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
- 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
- P. L. Gibbard, M. J. Head, and M. J. C. Walker. 2010. Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma. Journal of Quaternary Science 25(2):96-102 view
- J. Meng and M. C. McKenna. 1998. Faunal turnovers of Paleogene mammals from the Mongolian Plateau. Nature 394:364-367 view
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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 | Cenozoic Subepochs | European Faunal Zones | Cenozoic Subepochs of Southern Europe | Paleogene Mammal Ages of Asia | Obsolete Carboniferous Ages of China | Permian of the Salt Range | European Faunal Units | ||||
---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Late Pleistocene | Late Pleistocene | Tarantian | 0.0117 | ||||||
Chibanian | Middle Pleistocene | Ionian | 0.129 | ||||||||
Calabrian | Early Pleistocene | 0.774 | |||||||||
Gelasian | MN 17 | 1.8 | |||||||||
Neogene | Pliocene | Piacenzian | Late Pliocene | MN 16 | Villanyian | 2.58 | |||||
Ruscinian | 3.1 * | ||||||||||
MN 15 | 3.2 | ||||||||||
Zanclean | Early Pliocene | 3.6 | |||||||||
MN 14 | 4.2 | ||||||||||
MN 13 | 4.9 | ||||||||||
Miocene | Messinian | Late Miocene | Turolian | 5.333 | |||||||
Tortonian | MN 12 | 7.246 | |||||||||
MN 11 | 7.75 | ||||||||||
MN 10 | Vallesian | 8.7 | |||||||||
MN 9 | 9.7 | ||||||||||
MN 7 + 8 | 11.1 | ||||||||||
Serravallian | Middle Miocene | Astaracian | 11.63 | ||||||||
MN 6 | 12.8 * | ||||||||||
Langhian | MN 5 | 13.82 | |||||||||
Burdigalian | Early Miocene | MN 4 | Orleanian | 15.98 | |||||||
MN 3 | 16.9 | ||||||||||
MN 2 | Agenian | 20 | |||||||||
Aquitanian | 20.44 | ||||||||||
MN 1 | 22.4 | ||||||||||
Paleogene | Oligocene | Chattian | Late Oligocene | Tabenbulakian | Hsandagolian | 23.03 | |||||
Rupelian | Early Oligocene | Kekeamuan | 27.82 | ||||||||
Eocene | Priabonian | Late Eocene | Houldjinian/Ergilian/Ulangochuian | 33.9 | |||||||
Bartonian | Middle Eocene | Sharamurunian/Irdinmanhan/Arshantan | 37.71 | ||||||||
Lutetian | 41.2 | ||||||||||
Ypresian | Early Eocene | Bumbanian | 47.8 | ||||||||
Paleocene | Thanetian | Late Paleocene | Gashatan | 56 | |||||||
Selandian | Middle Paleocene | 59.2 | |||||||||
Danian | Early Paleocene | 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 | ||||||||||
Kathwai | 251.5 * | ||||||||||
Permian | Lopingian | Changhsingian | 251.902 | ||||||||
252.4 * | |||||||||||
Chhidru | 252.9 * | ||||||||||
Wuchiapingian | 254.14 | ||||||||||
Kalabagh | 255 * | ||||||||||
Wargal | 256 * | ||||||||||
Guadalupian | Capitanian | 259.51 | |||||||||
Wordian | 264.28 | ||||||||||
265.3 * | |||||||||||
Amb | 266.1 * | ||||||||||
Roadian | 266.9 | ||||||||||
270.7 * | |||||||||||
Cisuralian | Kungurian | 273.01 | |||||||||
Artinskian | 283.5 | ||||||||||
Sakmarian | 290.1 | ||||||||||
Asselian | 293.52 | ||||||||||
Carboniferous | Pennsylvanian | Gzhelian | Mapingian † | 298.9 | |||||||
Kasimovian | 303.7 | ||||||||||
305.9 |