Carbo-Permian of the Russian Platform
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
- 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
- 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
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 492 collections
International Chronostratigraphic Timescale | Carbo-Permian of the Russian Platform | Permo-Triassic Subages of Eastern Europe | Obsolete Carboniferous Ages of China | Permian-Jurassic of New Zealand | ||||
---|---|---|---|---|---|---|---|---|
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 | 251.5 | ||||||
Permian | Lopingian | Changhsingian | Melekhovian | 251.902 | ||||
Waiitian | 253.2 | |||||||
Wuchiapingian | Late Vyatkian/Early Vyatkian | 254.14 | ||||||
Puruhauan | 254.2 | |||||||
Guadalupian | Capitanian | Late Severodvinian/Early Severodvinian | Aparima | Flettian | 259.51 | |||
Wordian | Late Urzhumian/Early Urzhumian | 264.28 | ||||||
Noginskian | 264.9 * | |||||||
Barettian | 266 | |||||||
Roadian | Late Kazanian/Early Kazanian | 266.9 | ||||||
Cisuralian | Kungurian | 273.01 | ||||||
Mangapirian | 276 | |||||||
Pavlovoposadian | 276.8 * | |||||||
Artinskian | 283.5 | |||||||
Telfordian | 285 | |||||||
Rusavkinian | 287.6 * | |||||||
288.5 | ||||||||
Sakmarian | 290.1 | |||||||
Asselian | 293.52 | |||||||
Carboniferous | Pennsylvanian | Gzhelian | Mapingian † | 298.9 | ||||
Kasimovian | Dorogomilovian | 303.7 | ||||||
Khamovnikian | 304.8 | |||||||
Krevyakinian | 305.8 * | |||||||
305.9 | ||||||||
Moscovian | Myachkovian | 307 | ||||||
Podolskian | 308.9 * | |||||||
Kashirian | 311.4 * | |||||||
Vereian | 313.8 | |||||||
Melekessian | 314.8 | |||||||
Bashkirian | 315.2 | |||||||
Cheremshanian | 316.9 * | |||||||
Prikamian | 318.6 * | |||||||
Severokeltmian | 319.9 * | |||||||
Krasnopolyanian | 321.2 * | |||||||
Voznesenian | 321.9 * | |||||||
Mississippian | Serpukhovian | Zapaltjubian | 323.2 | |||||
Protvian | 324.4 * | |||||||
Steshevian | 326.8 * | |||||||
Tarusian | 329 * | |||||||
Visean | Venevian | 330.9 | ||||||
Mikhailovian | 331.9 * | |||||||
Aleksinian | 333.7 * | |||||||
Tulian | 335.8 * | |||||||
Bobrikian | 339.9 * | |||||||
Radaevkian | 343.4 * | |||||||
Tournaisian | Kosvian | 346.7 | ||||||
Kizelian | 350.7 * | |||||||
Cherepetian | 351.9 * | |||||||
Karakubian | 354.4 * | |||||||
Upinian | 356.3 * | |||||||
Malevkian | 357.6 * | |||||||
Gumerovian | 358 * | |||||||
358.9 |