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. Meng and M. C. McKenna. 1998. Faunal turnovers of Paleogene mammals from the Mongolian Plateau. Nature 394:364-367 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
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 126764 collections
International Chronostratigraphic Timescale | Paleogene Mammal Ages of Asia | Ordovician of China | ||||||
---|---|---|---|---|---|---|---|---|
Paleogene | Oligocene | Chattian | Tabenbulakian | Hsandagolian | 23.03 | |||
Rupelian | Kekeamuan | 27.82 | ||||||
Eocene | Priabonian | Houldjinian/Ergilian/Ulangochuian | 33.9 | |||||
Bartonian | Sharamurunian/Irdinmanhan/Arshantan | 37.71 | ||||||
Lutetian | 41.2 | |||||||
Ypresian | Bumbanian | 47.8 | ||||||
Paleocene | Thanetian | Gashatan | 56 | |||||
Selandian | 59.2 | |||||||
Danian | 61.6 | |||||||
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 | 168.2 | |||||||
Aalenian | 170.9 | |||||||
Early Jurassic | Toarcian | 174.7 | ||||||
Pliensbachian | 184.2 | |||||||
Sinemurian | 192.9 | |||||||
Hettangian | 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 | 259.51 | ||||||
Wordian | 264.28 | |||||||
Roadian | 266.9 | |||||||
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 | 427.4 | ||||||
Sheinwoodian | 430.5 | |||||||
Llandovery | Telychian | 433.4 | ||||||
Aeronian | 438.5 | |||||||
Rhuddanian | 440.8 | |||||||
Ordovician | Late Ordovician | Hirnantian | Hirnantian | Xiaoxita †/Shikou | Wufeng † | 443.8 | ||
Katian | Chientangkiangian | 445.2 | ||||||
Neichianshanian/Hanjiang | 449.5 | |||||||
Sandbian | 453 | |||||||
Middle Ordovician | Darriwilian | Darriwilian | Guniu †/Hulo | 458.4 | ||||
Hunjiang † | Dawan †/Daobaowan/Ningkuo | 466.3 * | ||||||
Dapingian | Dapingian | 467.3 | ||||||
Early Ordovician | Floian | Yiyangian | 470 | |||||
Tremadocian | Xinchangian | 477.7 | ||||||
Lianghekou † | 477.9 * | |||||||
485.4 |