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. 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
- F. M. Gradstein, F. P. Agterberg, J. G. Ogg, J. Hardenbol, P. Van Veen, J. Thierry, and Z. Huang. 1995. A Triassic, Jurassic, and Cretaceous time scale. SEPM Special Publication 54 view
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- J. Palfy, P. L. Smith, and J. K. Mortensen. 2000. A U-Pb and 40Ar/39Ar time scale for the Jurassic. Canadian Journal of Earth Sciences 37(6):923-944 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.
This timescale is used in the definition of 126586 collections
International Chronostratigraphic Timescale | European Faunal Zones | Cenozoic Subepochs of Southern Europe | Neogene Mammal Ages of China | ||||
---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | 0 | ||||
Northgrippian | 0.0042 | ||||||
Greenlandian | 0.0082 | ||||||
Pleistocene | Late Pleistocene | Tarantian | Nihewanian | 0.0117 | |||
Chibanian | Ionian | 0.129 | |||||
Calabrian | 0.774 | ||||||
Gelasian | MN 17 | 1.8 | |||||
Neogene | Pliocene | Piacenzian | MN 16 | Yushean | 2.58 | ||
MN 15 | 3.2 | ||||||
Zanclean | 3.6 | ||||||
MN 14 | 4.2 | ||||||
MN 13 | Baodean | 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 | Tunggurian | 11.1 | |||||
Serravallian | 11.63 | ||||||
MN 6 | 12.8 * | ||||||
Langhian | MN 5 | Shanwangian | 13.82 | ||||
Burdigalian | MN 4 | 15.98 | |||||
MN 3 | Xiejiaan | 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 | ||||||
66 |