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
- F. M. Gradstein, J. G. Ogg, M. D. Schmitz and G. M. Ogg. 2020. Geologic Time Scale 2020 view
- M. Kretzoi. 1942. Necroteuthis n. g. (Ceph. Dibr., Necroteuthidae N. F.) aus dem Oligozän von Budapest und das system der Dibranchiata. Földtani Közlöny 72:125-238 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
- 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
- J. A. Lillegraven and M. C. McKenna. 1986. Fossil mammals from the "Mesaverde" Formation (Late Cretaceous, Judithian) of the Bighorn and Wind River basins, Wyoming, with definitions of Late Cretaceous North American Land-Mammal "Ages". American Museum Novitates 2840:1-68 view
- M. Freudenthal. 2006. Mammal Paleogene zones. personal communication view
- F. M. Gradstein, J. G. Ogg, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 view
- M. O. Woodburne. 1987. A prospectus of the North American Mammal Ages. In: Woodburne, M. O. (ed.), Cenozoic Mammals of North America. University of California Press, Berkelery, CA 285-290 view
- J. Alroy. 2000. New methods for quantifying macroevolutionary patterns and processes. Paleobiology 26(4):707-733 view
- B. D. Webby. 1998. Steps toward a global standard for Ordovician stratigraphy. Newsletters in Stratigraphy 36:1-33 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 126973 collections
International Chronostratigraphic Timescale | Ordovician of North America | Ordovician of the Baltic | |||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Ordovician | Late Ordovician | Hirnantian | Cincinnatian | Gamachian | Harju | Porkuni | 443.8 | ||||||||||||
Katian | Pirgu | 445.2 | |||||||||||||||||
Richmondian | 446 * | ||||||||||||||||||
Vormsi | 449.6 * | ||||||||||||||||||
Maysvillian | Rocklandian †/Shermanian/Ashbyan/Kirkfieldian/Blackriveran/Wildernessian/Trentonian/Franklinian | 449.8 * | |||||||||||||||||
Nabala | Johvi † | 450 * | |||||||||||||||||
Edenian | 450.4 * | ||||||||||||||||||
Viru | Rakvere | 450.6 * | |||||||||||||||||
Mohawkian | Chatfieldian | 451.1 * | |||||||||||||||||
Oandu | 452 * | ||||||||||||||||||
Sandbian | Keila | Idavere † | 453 | ||||||||||||||||
Turinian | 453.7 * | ||||||||||||||||||
Haljala | 453.9 | ||||||||||||||||||
Kukruse | 456.4 * | ||||||||||||||||||
Whiterockian | Canadian † | Chazyan †/Marmor | 457 * | ||||||||||||||||
Uhaku | Aluoja † | 457.5 * | |||||||||||||||||
Middle Ordovician | Darriwilian | 458.4 | |||||||||||||||||
Lasnamagi | 458.9 * | ||||||||||||||||||
Aseri | 460.4 * | ||||||||||||||||||
Oeland | Kunda | 462.9 * | |||||||||||||||||
Valaste †/Hunderum | 464.3 * | ||||||||||||||||||
Volkhov | Langevoja †/Vaana/Saka | 467.1 * | |||||||||||||||||
Dapingian | 467.3 | ||||||||||||||||||
Rangerian | 469.1 * | ||||||||||||||||||
Billingen | 469.3 * | ||||||||||||||||||
Early Ordovician | Floian | Ibexian | Blackhillsian | Jeffersonian † | Cassinian † | 470 | |||||||||||||
Latorp † | 470.1 * | ||||||||||||||||||
Hunneberg | 473.7 * | ||||||||||||||||||
Tulean | 473.9 * | ||||||||||||||||||
Tremadocian | 477.7 | ||||||||||||||||||
Stairsian | 480.3 * | ||||||||||||||||||
Varangu | 481.3 * | ||||||||||||||||||
Skullrockian/Demingian | 482 * | ||||||||||||||||||
Pakerort | 482.2 * | ||||||||||||||||||
485.4 * | |||||||||||||||||||
486.3 | |||||||||||||||||||
486.5 | |||||||||||||||||||
487.5 |