Permian of China
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
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- A. G. Sennikov and V. K. Golubev. 2006. Vyazniki Biotic Assemblage of the Terminal Permian. Paleontological Journal 40(suppl. 4):S475-S481 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
There are 16 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 42 collections
International Chronostratigraphic Timescale | Permian of China | Obsolete Carboniferous Ages of China | Permian of Western Europe | Permo-Triassic Subages of Eastern Europe | Permian Subages of Germany | |||
---|---|---|---|---|---|---|---|---|
Triassic | Early Triassic | Olenekian | Vokhmian | 247.2 | ||||
Induan | 251.2 | |||||||
Permian | Lopingian | Changhsingian | Meishanian | Buntsandstein | 251.902 | |||
Baoqingian | 253.4 * | |||||||
Wuchiapingian | Laoshanian | Zechstein | Late Vyatkian/Early Vyatkian | 254.14 | ||||
Laibinian | 257.7 * | |||||||
Guadalupian | Capitanian | Lengwuan | Rotliegendes | Late Severodvinian/Early Severodvinian | Ohre/Aller | 259.51 | ||
Wordian | Kuhfengian | Late Urzhumian/Early Urzhumian | Leine | 264.28 | ||||
Roadian | Late Kazanian/Early Kazanian | 266.9 | ||||||
Cisuralian | Kungurian | Luodianian | 273.01 | |||||
Artinskian | Autunian | 283.5 | ||||||
Longlinian | 285.4 * | |||||||
Sakmarian | 290.1 | |||||||
Asselian | Zisongian | 293.52 | ||||||
Carboniferous | Pennsylvanian | Gzhelian | Mapingian † | 298.9 | ||||
300.1 | ||||||||
Kasimovian | 303.7 | |||||||
305.9 |