Ten Million Year Bins
The interval definitions in this timescale are derived from the following sources:
- 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
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 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, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- B. D. Webby. 1998. Steps toward a global standard for Ordovician stratigraphy. Newsletters in Stratigraphy 36:1-33 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 56 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 1 collections
International Chronostratigraphic Timescale | Ten Million Year Bins | North American Land Mammal Ages | Carboniferous Subepochs | Cenozoic Subepochs of Southern Europe | Ordovician of China | North American Mammal Subages/Zones | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Cenozoic 6 | Saintaugustinean | 0 | ||||||||
Santarosean | 0.0004 | ||||||||||||
Northgrippian | 0.0042 | ||||||||||||
Greenlandian | 0.0082 | ||||||||||||
Pleistocene | Late Pleistocene | Tarantian | Sheridanian | 0.0117 | |||||||||
Rancholabrean | 0.014 | ||||||||||||
Chibanian | Ionian | 0.129 | |||||||||||
Irvingtonian | Cudahyan/Sappan | 0.21 | |||||||||||
Calabrian | 0.774 | ||||||||||||
Blancan | Senecan/Rexroadian | 1.4 | |||||||||||
Gelasian | 1.8 | ||||||||||||
Neogene | Pliocene | Piacenzian | 2.58 | ||||||||||
Zanclean | 3.6 | ||||||||||||
Hemphillian | Late Hemphillian/late Early Hemphillian/early Early Hemphillian | 4.7 | |||||||||||
Miocene | Messinian | 5.333 | |||||||||||
Tortonian | 7.246 | ||||||||||||
Clarendonian | Late Clarendonian/Early Clarendonian | 9.4 | |||||||||||
Serravallian | Cenozoic 5 | 11.63 | |||||||||||
Barstovian | late Late Barstovian/early Late Barstovian/Early Barstovian | 12.5 | |||||||||||
Langhian | 13.82 | ||||||||||||
Burdigalian | 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 | ||||||||||
Aquitanian | 20.44 | ||||||||||||
Paleogene | Oligocene | Chattian | Cenozoic 4 | 23.03 | |||||||||
Monroecreekian | 23.1 * | ||||||||||||
Geringian | 24.7 * | ||||||||||||
Rupelian | 27.82 | ||||||||||||
Whitneyan | 29.5 | ||||||||||||
Orellan | 31.8 | ||||||||||||
Eocene | Priabonian | Cenozoic 3 | Chadronian | Late Chadronian/Middle Chadronian/Early Chadronian | 33.9 | ||||||||
Duchesnean | 37 | ||||||||||||
Bartonian | 37.71 | ||||||||||||
Uintan | Late Uintan/Early Uintan | 39.7 | |||||||||||
Lutetian | Cenozoic 2 | 41.2 | |||||||||||
Bridgerian | Twinbuttean/Blacksforkian/Gardnerbuttian | 46.2 | |||||||||||
Ypresian | 47.8 | ||||||||||||
Wasatchian | Lostcabinian/Lysitean/Graybullian/Sandcouleean | 50.5 | |||||||||||
Clarkforkian | Cf3/Cf2/Cf1 | 54.9 | |||||||||||
Paleocene | Thanetian | Cenozoic 1 | 56 | ||||||||||
Tiffanian | Ti6/Ti5/Ti4/Ti3/Ti2/Ti1 | 56.2 | |||||||||||
Selandian | 59.2 | ||||||||||||
Torrejonian | To3/To2/To1 | 60.9 | |||||||||||
Danian | 61.6 | ||||||||||||
Puercan | Pu3/Pu2/Pu1 | 63.8 | |||||||||||
Cretaceous | Late Cretaceous | Maastrichtian | Cretaceous 8 | 66 | |||||||||
Campanian | Cretaceous 7 | 72.1 | |||||||||||
Santonian | Cretaceous 6 | 83.6 | |||||||||||
Coniacian | 86.3 | ||||||||||||
Turonian | 89.8 | ||||||||||||
Cenomanian | Cretaceous 5 | 93.9 | |||||||||||
Early Cretaceous | Albian | Cretaceous 4 | 100.5 | ||||||||||
Aptian | Cretaceous 3 | 113 | |||||||||||
Barremian | Cretaceous 2 | 121.4 | |||||||||||
Hauterivian | 125.77 | ||||||||||||
Valanginian | Cretaceous 1 | 132.6 | |||||||||||
Berriasian | 139.8 | ||||||||||||
Jurassic | Late Jurassic | Tithonian | Jurassic 6 | 145 | |||||||||
Kimmeridgian | Jurassic 5 | 149.2 | |||||||||||
Oxfordian | 154.8 | ||||||||||||
Middle Jurassic | Callovian | 161.5 | |||||||||||
Bathonian | Jurassic 4 | 165.3 | |||||||||||
Bajocian | 168.2 | ||||||||||||
Aalenian | Jurassic 3 | 170.9 | |||||||||||
Early Jurassic | Toarcian | 174.7 | |||||||||||
Pliensbachian | Jurassic 2 | 184.2 | |||||||||||
Sinemurian | Jurassic 1 | 192.9 | |||||||||||
Hettangian | 199.5 | ||||||||||||
Triassic | Late Triassic | Rhaetian | Triassic 4 | 201.4 | |||||||||
Norian | 208.5 | ||||||||||||
Carnian | Triassic 3 | 227 | |||||||||||
Middle Triassic | Ladinian | Triassic 2 | 237 | ||||||||||
Anisian | 242 | ||||||||||||
Early Triassic | Olenekian | Triassic 1 | 247.2 | ||||||||||
Induan | 251.2 | ||||||||||||
Permian | Lopingian | Changhsingian | Permian 4 | 251.902 | |||||||||
Wuchiapingian | 254.14 | ||||||||||||
Guadalupian | Capitanian | 259.51 | |||||||||||
Wordian | 264.28 | ||||||||||||
Roadian | Permian 3 | 266.9 | |||||||||||
Cisuralian | Kungurian | Permian 2 | 273.01 | ||||||||||
Artinskian | 283.5 | ||||||||||||
Sakmarian | 290.1 | ||||||||||||
Asselian | Permian 1 | 293.52 | |||||||||||
Carboniferous | Pennsylvanian | Gzhelian | Carboniferous 5 | Late Pennsylvanian | 298.9 | ||||||||
Kasimovian | 303.7 | ||||||||||||
Moscovian | Carboniferous 4 | Middle Pennsylvanian | 307 | ||||||||||
Bashkirian | Early Pennsylvanian | 315.2 | |||||||||||
Mississippian | Serpukhovian | Carboniferous 3 | Late Mississippian | 323.2 | |||||||||
Visean | Carboniferous 2 | Middle Mississippian | 330.9 | ||||||||||
Tournaisian | Carboniferous 1 | Early Mississippian | 346.7 | ||||||||||
Devonian | Late Devonian | Famennian | Devonian 5 | 358.9 | |||||||||
Frasnian | Devonian 4 | 372.2 | |||||||||||
Middle Devonian | Givetian | Devonian 3 | 382.7 | ||||||||||
Eifelian | 387.7 | ||||||||||||
Early Devonian | Emsian | Devonian 2 | 393.3 | ||||||||||
Pragian | Devonian 1 | 407.6 | |||||||||||
Lochkovian | 410.8 | ||||||||||||
Silurian | Pridoli | Silurian 2 | 419.2 | ||||||||||
Ludlow | Ludfordian | 423 | |||||||||||
Gorstian | 425.6 | ||||||||||||
Wenlock | Homerian | 427.4 | |||||||||||
Sheinwoodian | 430.5 | ||||||||||||
Llandovery | Telychian | Silurian 1 | 433.4 | ||||||||||
Aeronian | 438.5 | ||||||||||||
Rhuddanian | 440.8 | ||||||||||||
Ordovician | Late Ordovician | Hirnantian | Ordovician 5 | Hirnantian | Xiaoxita †/Shikou | Wufeng † | 443.8 | ||||||
Katian | Chientangkiangian | 445.2 | |||||||||||
Neichianshanian/Hanjiang | 449.5 | ||||||||||||
Sandbian | Ordovician 4 | 453 | |||||||||||
Middle Ordovician | Darriwilian | Ordovician 3 | Darriwilian | Guniu †/Hulo | 458.4 | ||||||||
Hunjiang † | Dawan †/Daobaowan/Ningkuo | 466.3 * | |||||||||||
Dapingian | Ordovician 2 | Dapingian | 467.3 | ||||||||||
Early Ordovician | Floian | Yiyangian | 470 | ||||||||||
Tremadocian | Ordovician 1 | Xinchangian | 477.7 | ||||||||||
Lianghekou † | 477.9 * | ||||||||||||
Cambrian | Furongian | Stage 10 | Cambrian 5 | 485.4 | |||||||||
Jiangshanian | 489.5 | ||||||||||||
Paibian | 494 | ||||||||||||
Miaolingian | Guzhangian | Cambrian 4 | 497 | ||||||||||
Drumian | 500.5 | ||||||||||||
Wuliuan | Cambrian 3 | 504.5 | |||||||||||
Series 2 | Stage 4 | 509 | |||||||||||
Stage 3 | Cambrian 2 | 514 | |||||||||||
Terreneuvian | Stage 2 | 521 | |||||||||||
Fortunian | Cambrian 1 | 529 | |||||||||||
538.8 |