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
- 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
- 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
- M. Harzhauser and W. E. Piller. 2004. Integrated stratigraphy of the Sarmatian (Upper Middle Miocene) in the western Central Paratethys. Stratigraphy 1(1):65-86 view
- M. O. Woodburne. 1987. A prospectus of the North American Mammal Ages. In: Woodburne, M. O. (ed.), Cenozoic Mammals of North America. University of California Press, Berkelery, CA 285-290 view
- J. Alroy. 2000. New methods for quantifying macroevolutionary patterns and processes. Paleobiology 26(4):707-733 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 128315 collections
International Chronostratigraphic Timescale | Ammonite Chrons of Northwest Europe | Permian of North America | Cenozoic Subepochs | Central Paratethys Stages | North American Mammal Subages/Zones | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Late Pleistocene | Late Pleistocene | Sheridanian | 0.0117 | |||||||
Chibanian | Middle Pleistocene | 0.129 | ||||||||||
Cudahyan/Sappan | 0.21 | |||||||||||
Calabrian | Early Pleistocene | 0.774 | ||||||||||
Senecan/Rexroadian | 1.4 | |||||||||||
Gelasian | 1.8 | |||||||||||
Neogene | Pliocene | Piacenzian | Late Pliocene | 2.58 | ||||||||
Zanclean | Early Pliocene | 3.6 | ||||||||||
Late Hemphillian/late Early Hemphillian/early Early Hemphillian | 4.7 | |||||||||||
Miocene | Messinian | Late Miocene | 5.333 | |||||||||
Tortonian | Pannonian | 7.246 | ||||||||||
Late Clarendonian/Early Clarendonian | 9.4 | |||||||||||
Serravallian | Middle Miocene | Sarmatian | 11.63 | |||||||||
late Late Barstovian/early Late Barstovian/Early Barstovian | 12.5 | |||||||||||
Badenian | 12.8 * | |||||||||||
Langhian | 13.82 | |||||||||||
Burdigalian | Early Miocene | 15.98 | ||||||||||
Late Hemingfordian/Early Hemingfordian | 16.3 | |||||||||||
late Late Arikareean/early Late Arikareean/late Early Arikareean/early Early Arikareean | Harrisonian | 18.5 | ||||||||||
Aquitanian | 20.44 | |||||||||||
Paleogene | Oligocene | Chattian | Late Oligocene | 23.03 | ||||||||
Monroecreekian | 23.1 * | |||||||||||
Geringian | 24.7 * | |||||||||||
Rupelian | Early Oligocene | 27.82 | ||||||||||
29.5 | ||||||||||||
Eocene | Priabonian | Late Eocene | Late Chadronian/Middle Chadronian/Early Chadronian | 33.9 | ||||||||
37 | ||||||||||||
Bartonian | Middle Eocene | 37.71 | ||||||||||
Late Uintan/Early Uintan | 39.7 | |||||||||||
Lutetian | 41.2 | |||||||||||
Twinbuttean/Blacksforkian/Gardnerbuttian | 46.2 | |||||||||||
Ypresian | Early Eocene | 47.8 | ||||||||||
Lostcabinian/Lysitean/Graybullian/Sandcouleean | 50.5 | |||||||||||
Cf3/Cf2/Cf1 | 54.9 | |||||||||||
Paleocene | Thanetian | Late Paleocene | 56 | |||||||||
Ti6/Ti5/Ti4/Ti3/Ti2/Ti1 | 56.2 | |||||||||||
Selandian | Middle Paleocene | 59.2 | ||||||||||
To3/To2/To1 | 60.9 | |||||||||||
Danian | Early Paleocene | 61.6 | ||||||||||
Pu3/Pu2/Pu1 | 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 | Parkinsoni/Garantiana/Subfurcatum/Sauzei/Laeviuscula/Discites | 168.2 | ||||||||||
Humphresianum | 168.4 | |||||||||||
Aalenian | Concavum/Murchisonae/Opalinum | 170.9 | ||||||||||
Early Jurassic | Toarcian | Levesquei/Variabilis/Bifrons | Thouarsense | 174.7 | ||||||||
180.1 | ||||||||||||
Serpentinum/Falciferum/Tenuicostatum | 182 | |||||||||||
Pliensbachian | Spinatum/Margaritatus/Davoei/Ibex/Jamesoni | 184.2 | ||||||||||
Sinemurian | Raricostatum/Oxynotum/Obtusum/Turneri/Semicostatum/Bucklandi | 192.9 | ||||||||||
Hettangian | Angulata/Liasicus/Planorbis | 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 | |||||||||||
Guadalupian | Capitanian | Capitanian | 259.51 | |||||||||
Wordian | Wordian | 264.28 | ||||||||||
Roadian | Roadian | 266.9 | ||||||||||
Cisuralian | Kungurian | Leonardian | Cathedralian | 273.01 | ||||||||
Hessian | 281.9 * | |||||||||||
Artinskian | 283.5 | |||||||||||
Wolfcampian | Lenoxian | 286.1 * | ||||||||||
Sakmarian | 290.1 | |||||||||||
Asselian | Nealian | 293.52 | ||||||||||
298.9 |