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
- D. H. Erwin and S. A. Bowring. 2004. Cambrian time scale. view
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- F. M. Gradstein, F. P. Agterberg, J. G. Ogg, J. Hardenbol, P. Van Veen, J. Thierry, and Z. Huang. 1995. A Triassic, Jurassic, and Cretaceous time scale. SEPM Special Publication 54 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 126691 collections
International Chronostratigraphic Timescale | Mesozoic Subages | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Triassic | Late Triassic | Rhaetian | 201.4 | ||||||||
Norian | Sevatian | 208.5 | |||||||||
Alaunian | 213.2 * | ||||||||||
Lacian | 216.7 * | ||||||||||
Carnian | Tuvalian | 227 | |||||||||
Julian | 233.4 * | ||||||||||
Middle Triassic | Ladinian | Longobardian | 237 | ||||||||
Fassanian | 239.7 * | ||||||||||
Anisian | Illyrian | 242 | |||||||||
Pelsonian | 243.8 * | ||||||||||
Bithynian | 244.7 * | ||||||||||
Aegean | 245.5 * | ||||||||||
Early Triassic | Olenekian | Spathian | 247.2 | ||||||||
Smithian | 248.9 * | ||||||||||
Induan | Dienerian | 251.2 | |||||||||
Griesbachian | 251.4 * | ||||||||||
251.902 |