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
- 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, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 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
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 | Silurian Ages of Europe | Carbo-Permian of the Russian Platform | Ammonite Chrons of Northwest Europe | Carboniferous of China | ||||
---|---|---|---|---|---|---|---|---|
Jurassic | Middle Jurassic | 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 | |||||||
Permian | Lopingian | Changhsingian | Melekhovian | 251.902 | ||||
Wuchiapingian | 254.14 | |||||||
Guadalupian | Capitanian | 259.51 | ||||||
Wordian | 264.28 | |||||||
Noginskian | 264.9 * | |||||||
Roadian | 266.9 | |||||||
Cisuralian | Kungurian | 273.01 | ||||||
Pavlovoposadian | 276.8 * | |||||||
Artinskian | 283.5 | |||||||
Rusavkinian | 287.6 * | |||||||
Sakmarian | 290.1 | |||||||
Asselian | 293.52 | |||||||
Carboniferous | Pennsylvanian | Gzhelian | 298.9 | |||||
Xiaodushanian | 300 * | |||||||
Kasimovian | Dorogomilovian | 303.7 | ||||||
Khamovnikian | 304.8 | |||||||
Krevyakinian | Dalaun | 305.8 * | ||||||
Moscovian | Myachkovian | 307 | ||||||
Podolskian | 308.9 * | |||||||
Kashirian | 311.4 * | |||||||
Vereian | 313.8 | |||||||
Melekessian | 314.8 | |||||||
Bashkirian | 315.2 | |||||||
Cheremshanian | 316.9 * | |||||||
Huashibanian | 318.5 * | |||||||
Prikamian | 318.6 * | |||||||
Severokeltmian | 319.9 * | |||||||
Krasnopolyanian | Lousuan | 321.2 * | ||||||
Voznesenian | 321.9 * | |||||||
Mississippian | Serpukhovian | Zapaltjubian | Dewunian | 323.2 | ||||
Protvian | 324.4 * | |||||||
Steshevian | 326.8 * | |||||||
Tarusian | 329 * | |||||||
Shangsian | 330.8 * | |||||||
Visean | Venevian | 330.9 | ||||||
Mikhailovian | 331.9 * | |||||||
Aleksinian | 333.7 * | |||||||
Jiusian | 335 * | |||||||
Tulian | 335.8 * | |||||||
Bobrikian | 339.9 * | |||||||
Radaevkian | 343.4 * | |||||||
Tournaisian | Kosvian | Tangbagouan | 346.7 | |||||
Kizelian | 350.7 * | |||||||
Cherepetian | 351.9 * | |||||||
Karakubian | 354.4 * | |||||||
Upinian | 356.3 * | |||||||
Malevkian | 357.6 * | |||||||
Gumerovian | 358 * | |||||||
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 |