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
- A. D. Barnosky, M. Holmes, R. Kirchholtes, E. Lindsey, K.C. Maguire, A.W. Poust, M.A. Stegner, J. Sunseri, B. Swartz, J. Swift, N.A. Villavicencio and G. Wogan. 2014. Prelude to the Anthropocene: Two new North American Land Mammal Ages (NALMAs). The Anthropocene Review I(3):225-242 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
- 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
- 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
- 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. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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 | North American Land Mammal Ages | North American Mammal Subages/Zones | Central Paratethys Stages | Ammonite Chrons of Northwest Europe | Cenozoic Subepochs | Silurian Ages of Europe | Permian of the Salt Range | European Faunal Units | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Saintaugustinean | 0 | ||||||||||
Santarosean | 0.0004 | |||||||||||||
Northgrippian | 0.0042 | |||||||||||||
Greenlandian | 0.0082 | |||||||||||||
Pleistocene | Late Pleistocene | Sheridanian | Late Pleistocene | 0.0117 | ||||||||||
Rancholabrean | 0.014 | |||||||||||||
Chibanian | Middle Pleistocene | 0.129 | ||||||||||||
Irvingtonian | Cudahyan/Sappan | 0.21 | ||||||||||||
Calabrian | Early Pleistocene | 0.774 | ||||||||||||
Blancan | Senecan/Rexroadian | 1.4 | ||||||||||||
Gelasian | 1.8 | |||||||||||||
Neogene | Pliocene | Piacenzian | Late Pliocene | Villanyian | 2.58 | |||||||||
Ruscinian | 3.1 * | |||||||||||||
Zanclean | Early Pliocene | 3.6 | ||||||||||||
Hemphillian | Late Hemphillian/late Early Hemphillian/early Early Hemphillian | 4.7 | ||||||||||||
Miocene | Messinian | Late Miocene | Turolian | 5.333 | ||||||||||
Tortonian | Pannonian | 7.246 | ||||||||||||
Vallesian | 8.7 | |||||||||||||
Clarendonian | Late Clarendonian/Early Clarendonian | 9.4 | ||||||||||||
Serravallian | Sarmatian | Middle Miocene | Astaracian | 11.63 | ||||||||||
Barstovian | late Late Barstovian/early Late Barstovian/Early Barstovian | 12.5 | ||||||||||||
Badenian | 12.8 * | |||||||||||||
Langhian | 13.82 | |||||||||||||
Burdigalian | Early Miocene | Orleanian | 15.98 | |||||||||||
Hemingfordian | Late Hemingfordian/Early Hemingfordian | 16.3 | ||||||||||||
Arikareean | late Late Arikareean/early Late Arikareean/late Early Arikareean/early Early Arikareean | Harrisonian | 18.5 | |||||||||||
Agenian | 20 | |||||||||||||
Aquitanian | 20.44 | |||||||||||||
Paleogene | Oligocene | Chattian | Late Oligocene | 23.03 | ||||||||||
Monroecreekian | 23.1 * | |||||||||||||
Geringian | 24.7 * | |||||||||||||
Rupelian | Early Oligocene | 27.82 | ||||||||||||
Whitneyan | 29.5 | |||||||||||||
Orellan | 31.8 | |||||||||||||
Eocene | Priabonian | Chadronian | Late Chadronian/Middle Chadronian/Early Chadronian | Late Eocene | 33.9 | |||||||||
Duchesnean | 37 | |||||||||||||
Bartonian | Middle Eocene | 37.71 | ||||||||||||
Uintan | Late Uintan/Early Uintan | 39.7 | ||||||||||||
Lutetian | 41.2 | |||||||||||||
Bridgerian | Twinbuttean/Blacksforkian/Gardnerbuttian | 46.2 | ||||||||||||
Ypresian | Early Eocene | 47.8 | ||||||||||||
Wasatchian | Lostcabinian/Lysitean/Graybullian/Sandcouleean | 50.5 | ||||||||||||
Clarkforkian | Cf3/Cf2/Cf1 | 54.9 | ||||||||||||
Paleocene | Thanetian | Late Paleocene | 56 | |||||||||||
Tiffanian | Ti6/Ti5/Ti4/Ti3/Ti2/Ti1 | 56.2 | ||||||||||||
Selandian | Middle Paleocene | 59.2 | ||||||||||||
Torrejonian | To3/To2/To1 | 60.9 | ||||||||||||
Danian | Early Paleocene | 61.6 | ||||||||||||
Puercan | 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 | |||||||||||||
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 | 298.9 | |||||||||||
Kasimovian | 303.7 | |||||||||||||
Moscovian | 307 | |||||||||||||
Bashkirian | 315.2 | |||||||||||||
Mississippian | Serpukhovian | 323.2 | ||||||||||||
Visean | 330.9 | |||||||||||||
Tournaisian | 346.7 | |||||||||||||
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 | Gleedonian | 427.4 | |||||||||||
Whitwellian | 429.7 * | |||||||||||||
430.5 |