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
- J. I. Raine, A. G. Beu, A. F. Boyes, H. J. Campbell, R. A. Cooper, J. S. Crampton, M. P. Crundwell, C. J. Hollis, and H. E. G. Morgans. 2015. Revised Calibration of the New Zealand Geological Timescale: NZGT2015/1. GNS Science Report 2012(39) 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
- 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, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 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 | Permian-Jurassic of New Zealand | Permian Subages of Germany | Permo-Triassic Subages of Eastern Europe | Obsolete Carboniferous Ages of China | Permian of the Salt Range | Carboniferous Subepochs | ||||
---|---|---|---|---|---|---|---|---|---|---|---|
Jurassic | Late Jurassic | Tithonian | Oteke | Puaroan | 145 | ||||||
Kimmeridgian | 149.2 | ||||||||||
Kawhia | Ohauan | 150 | |||||||||
Heterian | 154.5 | ||||||||||
Oxfordian | 154.8 | ||||||||||
Middle Jurassic | Callovian | 161.5 | |||||||||
Temaikan | 164.3 | ||||||||||
Bathonian | 165.3 | ||||||||||
Bajocian | 168.2 | ||||||||||
Aalenian | 170.9 | ||||||||||
Early Jurassic | Toarcian | 174.7 | |||||||||
Herangi | Ururoan | 176 | |||||||||
Pliensbachian | 184.2 | ||||||||||
Aratauran | 188.9 | ||||||||||
Sinemurian | 192.9 | ||||||||||
Hettangian | 199.5 | ||||||||||
Triassic | Late Triassic | Rhaetian | Balfour | Otapirian | 201.4 | ||||||
Norian | Warepan | 208.5 | |||||||||
Otamitan | 217 | ||||||||||
Oretian | 221 | ||||||||||
Carnian | 227 | ||||||||||
Gore | Kaihikuan | 227.5 | |||||||||
Middle Triassic | Ladinian | 237 | |||||||||
Etalian | 238 | ||||||||||
Anisian | 242 | ||||||||||
Malakovian | 246 | ||||||||||
Early Triassic | Olenekian | Vokhmian | 247.2 | ||||||||
Nelsonian | 249 | ||||||||||
Induan | 251.2 | ||||||||||
DUrville | Makarewan | Kathwai | 251.5 * | ||||||||
Permian | Lopingian | Changhsingian | Meishanian | Buntsandstein | 251.902 | ||||||
252.4 * | |||||||||||
Chhidru | 252.9 * | ||||||||||
Waiitian | 253.2 | ||||||||||
Baoqingian | 253.4 * | ||||||||||
Wuchiapingian | Laoshanian | Late Vyatkian/Early Vyatkian | 254.14 | ||||||||
Puruhauan | 254.2 | ||||||||||
Kalabagh | 255 * | ||||||||||
Wargal | 256 * | ||||||||||
Laibinian | 257.7 * | ||||||||||
Guadalupian | Capitanian | Lengwuan | Aparima | Flettian | Ohre/Aller | Late Severodvinian/Early Severodvinian | 259.51 | ||||
Wordian | Kuhfengian | Leine | Late Urzhumian/Early Urzhumian | 264.28 | |||||||
265.3 * | |||||||||||
Barettian | 266 | ||||||||||
Amb | 266.1 * | ||||||||||
Roadian | Late Kazanian/Early Kazanian | 266.9 | |||||||||
270.7 * | |||||||||||
Cisuralian | Kungurian | Luodianian | 273.01 | ||||||||
Mangapirian | 276 | ||||||||||
Artinskian | 283.5 | ||||||||||
Telfordian | 285 | ||||||||||
Longlinian | 285.4 * | ||||||||||
288.5 | |||||||||||
Sakmarian | 290.1 | ||||||||||
Asselian | Zisongian | 293.52 | |||||||||
Carboniferous | Pennsylvanian | Gzhelian | Mapingian † | Late Pennsylvanian | 298.9 | ||||||
300.1 | |||||||||||
Kasimovian | 303.7 | ||||||||||
305.9 | |||||||||||
Moscovian | Middle Pennsylvanian | 307 | |||||||||
Bashkirian | Early Pennsylvanian | 315.2 | |||||||||
Mississippian | Serpukhovian | Late Mississippian | 323.2 | ||||||||
Visean | Middle Mississippian | 330.9 | |||||||||
Tournaisian | Early Mississippian | 346.7 | |||||||||
358.9 |