Ten Million Year Bins
The interval definitions in this timescale are derived from the following sources:
- J. A. Lillegraven and M. C. McKenna. 1986. Fossil mammals from the "Mesaverde" Formation (Late Cretaceous, Judithian) of the Bighorn and Wind River basins, Wyoming, with definitions of Late Cretaceous North American Land-Mammal "Ages". American Museum Novitates 2840:1-68 view
- J. Meng and M. C. McKenna. 1998. Faunal turnovers of Paleogene mammals from the Mongolian Plateau. Nature 394:364-367 view
- M. Freudenthal. 2006. Mammal Paleogene zones. personal communication view
- A. G. Sennikov and V. K. Golubev. 2006. Vyazniki Biotic Assemblage of the Terminal Permian. Paleontological Journal 40(suppl. 4):S475-S481 view
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
There are 56 timescales which overlap this one. show
This timescale is used in the definition of 2 collections
| International Chronostratigraphic Timescale | Ten Million Year Bins | Cretaceous North American Land-Mammal Ages | Paleogene Mammal Ages of Asia | Mammal Paleogene Zones | Permo-Triassic Subages of Eastern Europe | |||||
|---|---|---|---|---|---|---|---|---|---|---|
| Quaternary | Holocene | Meghalayan | Cenozoic 6 | 0 | ||||||
| Northgrippian | 0.0042 | |||||||||
| Greenlandian | 0.0082 | |||||||||
| Pleistocene | Late Pleistocene | 0.0117 | ||||||||
| Chibanian | 0.129 | |||||||||
| Calabrian | 0.774 | |||||||||
| Gelasian | 1.8 | |||||||||
| Neogene | Pliocene | Piacenzian | 2.58 | |||||||
| Zanclean | 3.6 | |||||||||
| Miocene | Messinian | 5.333 | ||||||||
| Tortonian | 7.246 | |||||||||
| Serravallian | Cenozoic 5 | 11.63 | ||||||||
| Langhian | 13.82 | |||||||||
| Burdigalian | 15.98 | |||||||||
| Aquitanian | 20.44 | |||||||||
| Paleogene | Oligocene | Chattian | Cenozoic 4 | Tabenbulakian | Hsandagolian | MP 30/MP 29/MP 28/MP 27/MP 26 | MP 25 | 23.03 | ||
| Rupelian | Kekeamuan | MP 24/MP 23/MP 22/MP 21 | 27.82 | |||||||
| Eocene | Priabonian | Cenozoic 3 | Houldjinian/Ergilian/Ulangochuian | MP 20/MP 19/MP 18/MP 17B/MP 17A | 33.9 | |||||
| Bartonian | Sharamurunian/Irdinmanhan/Arshantan | MP 16 | 37.71 | |||||||
| Lutetian | Cenozoic 2 | MP 15/MP 14/MP 13/MP 12/MP 11 | 41.2 | |||||||
| Ypresian | Bumbanian | MP 10/MP 8 + 9/MP 7 | 47.8 | |||||||
| Paleocene | Thanetian | Cenozoic 1 | Gashatan | MP 6 | MP 1 - 5 | 56 | ||||
| Selandian | 59.2 | |||||||||
| Danian | 61.6 | |||||||||
| Cretaceous | Late Cretaceous | Maastrichtian | Cretaceous 8 | Lancian/Edmontonian | 66 | |||||
| Campanian | Cretaceous 7 | Judithian/Aquilan | 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 | Vokhmian | 247.2 | ||||||
| Induan | 251.2 | |||||||||
| Permian | Lopingian | Changhsingian | Permian 4 | 251.902 | ||||||
| Wuchiapingian | Late Vyatkian/Early Vyatkian | 254.14 | ||||||||
| Guadalupian | Capitanian | Late Severodvinian/Early Severodvinian | 259.51 | |||||||
| Wordian | Late Urzhumian/Early Urzhumian | 264.28 | ||||||||
| Roadian | Permian 3 | Late Kazanian/Early Kazanian | 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 | 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 | ||||||||||