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
- 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
- Z.-X. Qiu and Z.-D. Qiu. 1995. Chronological sequence and subdivision of Chinese Neogene mammalian faunas. Palaeogeography, Palaeoclimatology, Palaeoecology 116(1-2):41-70 view
- 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
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 126610 collections
International Chronostratigraphic Timescale | Cambrian of China | Cambrian of West Avalonia | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Cambrian | Furongian | Stage 10 | Niuchehean | Taoyuanian † | 485.4 | |||||||
Jiangshanian | Jiangshanian | 489.5 | ||||||||||
Paibian | Paibian | 494 | ||||||||||
Waergangian †/Youshuanian | 494.9 * | |||||||||||
Miaolingian | Guzhangian | Guzhangian | Wangcunian † | 497 | ||||||||
Arcadian | 498.4 | |||||||||||
Drumian | Drumian | 500.5 | ||||||||||
Wuliuan | Wuliuan/Taijangian | 504.5 | ||||||||||
Series 2 | Stage 4 | Duyunian | Branchian | 509 | ||||||||
Stage 3 | Nangaoian | 514 | ||||||||||
Placentian | 517.1 | |||||||||||
Terreneuvian | Stage 2 | Meishucunian | 521 | |||||||||
Fortunian | 529 | |||||||||||
Jinnigian | 530.7 | |||||||||||
538.8 |