Ten Million Year Bins
The interval definitions in this timescale are derived from the following sources:
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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
- 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
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.
This timescale is used in the definition of 1 collections
International Chronostratigraphic Timescale | Ten Million Year Bins | Cambrian of Australia | Cenozoic Subepochs of Southern Europe | North American Land Mammal Ages | Cambrian of West Avalonia | |||
---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Cenozoic 6 | Saintaugustinean | 0 | |||
Santarosean | 0.0004 | |||||||
Northgrippian | 0.0042 | |||||||
Greenlandian | 0.0082 | |||||||
Pleistocene | Late Pleistocene | Tarantian | 0.0117 | |||||
Rancholabrean | 0.014 | |||||||
Chibanian | Ionian | 0.129 | ||||||
Irvingtonian | 0.21 | |||||||
Calabrian | 0.774 | |||||||
Blancan | 1.4 | |||||||
Gelasian | 1.8 | |||||||
Neogene | Pliocene | Piacenzian | 2.58 | |||||
Zanclean | 3.6 | |||||||
Hemphillian | 4.7 | |||||||
Miocene | Messinian | 5.333 | ||||||
Tortonian | 7.246 | |||||||
Clarendonian | 9.4 | |||||||
Serravallian | Cenozoic 5 | 11.63 | ||||||
Barstovian | 12.5 | |||||||
Langhian | 13.82 | |||||||
Burdigalian | 15.98 | |||||||
Hemingfordian | 16.3 | |||||||
Arikareean | 18.5 | |||||||
Aquitanian | 20.44 | |||||||
Paleogene | Oligocene | Chattian | Cenozoic 4 | 23.03 | ||||
Rupelian | 27.82 | |||||||
Whitneyan | 29.5 | |||||||
Orellan | 31.8 | |||||||
Eocene | Priabonian | Cenozoic 3 | Chadronian | 33.9 | ||||
Duchesnean | 37 | |||||||
Bartonian | 37.71 | |||||||
Uintan | 39.7 | |||||||
Lutetian | Cenozoic 2 | 41.2 | ||||||
Bridgerian | 46.2 | |||||||
Ypresian | 47.8 | |||||||
Wasatchian | 50.5 | |||||||
Clarkforkian | 54.9 | |||||||
Paleocene | Thanetian | Cenozoic 1 | 56 | |||||
Tiffanian | 56.2 | |||||||
Selandian | 59.2 | |||||||
Torrejonian | 60.9 | |||||||
Danian | 61.6 | |||||||
Puercan | 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 | 298.9 | ||||
Kasimovian | 303.7 | |||||||
Moscovian | Carboniferous 4 | 307 | ||||||
Bashkirian | 315.2 | |||||||
Mississippian | Serpukhovian | Carboniferous 3 | 323.2 | |||||
Visean | Carboniferous 2 | 330.9 | ||||||
Tournaisian | Carboniferous 1 | 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 | 443.8 | ||||
Katian | 445.2 | |||||||
Sandbian | Ordovician 4 | 453 | ||||||
Middle Ordovician | Darriwilian | Ordovician 3 | 458.4 | |||||
Dapingian | Ordovician 2 | 467.3 | ||||||
Early Ordovician | Floian | 470 | ||||||
Tremadocian | Ordovician 1 | 477.7 | ||||||
Cambrian | Furongian | Stage 10 | Cambrian 5 | Datsonian | 485.4 | |||
Payntonian | 486.8 * | |||||||
Jiangshanian | Iverian | 489.5 | ||||||
Paibian | Idamean | 494 | ||||||
Miaolingian | Guzhangian | Cambrian 4 | Mindyallan | 497 | ||||
Arcadian | 498.4 | |||||||
Boomerangian | 499 | |||||||
Drumian | Undillan | 500.5 | ||||||
Floran | 503 | |||||||
Wuliuan | Cambrian 3 | Templetonian | 504.5 | |||||
Ordian | 507.8 * | |||||||
Series 2 | Stage 4 | Branchian | 509 | |||||
510.8 * | ||||||||
Stage 3 | Cambrian 2 | 514 | ||||||
Placentian | 517.1 | |||||||
Terreneuvian | Stage 2 | 521 | ||||||
Fortunian | Cambrian 1 | 529 | ||||||
538.8 |