Cenozoic Subepochs
The interval definitions in this timescale are derived from the following sources:
- 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, and A. G. Smith. 2004. A Geologic Time Scale 2004 1-589 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. F. Steininger, W. A. Berggren, D. V. Kent, R. L. Bernor, S. Sen and J. Agusti. 1996. Circum-Mediterranean Neogene (Miocene and Pliocene) marine-continental chronologic correlations of European mammal units. The Evolution of Western Eurasian Neogene Mammal Faunas (eds. R. L. Bernor, V. Fahlbusch, and H.-W. Mittmann) view
- F. J. Prevosti, C. O. Romano, A. M. Forasiepi, S. Hemming, R. Bonini, A. M. Candela, E. Cerdeño, M. C. Madozzo Jaén, P. E. Ortiz, F. Pujos, L. Rasia, G. I. Schmidt, M. Taglioretti, R. D. E. MacPhee, and U. F. J. Pardiñas. 2021. New radiometric 40Ar–39Ar dates and faunistic analyses refine evolutionary dynamics of Neogene vertebrate assemblages in southern South America. Scientific Reports 2021(11):9830 view
- J. J. Flynn and C. C. Swisher, III. 1995. Cenozoic South American Land Mammal Ages: correlation to global geochronology. Geochronology Time Scales and Global Stratigraphic Correlation, SEPM Special Publication 54:317-333 view
There are 13 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 13391 collections
International Chronostratigraphic Timescale | Cenozoic Subepochs | Neogene Mammal Ages of China | European Faunal Zones | South American Land Mammal Ages | ||||
---|---|---|---|---|---|---|---|---|
Quaternary | Pleistocene | Late Pleistocene | Late Pleistocene | Nihewanian | Lujanian | 0.0117 | ||
Chibanian | Middle Pleistocene | 0.129 | ||||||
Ensenadan | 0.3 * | |||||||
Calabrian | Early Pleistocene | 0.774 | ||||||
Sanandresian | Uquian † | 1.7 * | ||||||
Gelasian | MN 17 | 1.8 | ||||||
Neogene | Pliocene | Piacenzian | Late Pliocene | Yushean | MN 16 | Vorohuean | 2.58 | |
Chapadmalalan | 2.9 * | |||||||
MN 15 | 3.2 | |||||||
Zanclean | Early Pliocene | 3.6 | ||||||
Montehermosan | 3.7 * | |||||||
MN 14 | 4.2 | |||||||
Baodean | MN 13 | Huayquerian | 4.9 * | |||||
Miocene | Messinian | Late Miocene | 5.333 | |||||
Tortonian | MN 12 | 7.246 | ||||||
MN 11 | 7.75 | |||||||
Chasicoan | 7.9 * | |||||||
MN 10 | 8.7 | |||||||
MN 9 | 9.7 | |||||||
Mayoan | 9.9 * | |||||||
Laventan | 10.9 * | |||||||
Tunggurian | MN 7 + 8 | 11.1 | ||||||
Serravallian | Middle Miocene | 11.63 | ||||||
MN 6 | 12.8 * | |||||||
Colloncuran | 13.7 * | |||||||
Langhian | Shanwangian | MN 5 | 13.82 | |||||
Friasian | 15.4 * | |||||||
Burdigalian | Early Miocene | MN 4 | 15.98 | |||||
Santacrucian | 16.2 * | |||||||
Xiejiaan | MN 3 | 16.9 | ||||||
Colhuehuapian | 17.4 * | |||||||
MN 2 | 20 | |||||||
Aquitanian | 20.44 | |||||||
Deseadan | 20.9 * | |||||||
MN 1 | 22.4 | |||||||
Paleogene | Oligocene | Chattian | Late Oligocene | 23.03 | ||||
Rupelian | Early Oligocene | 27.82 | ||||||
Tinguirirican | 28.9 * | |||||||
Eocene | Priabonian | Late Eocene | 33.9 | |||||
Divisaderan | 35.9 * | |||||||
Bartonian | Middle Eocene | 37.71 | ||||||
Lutetian | 41.2 | |||||||
Mustersan | 41.9 * | |||||||
Ypresian | Early Eocene | 47.8 | ||||||
Casamayoran | 47.9 * | |||||||
Paleocene | Thanetian | Late Paleocene | Riochican | 56 | ||||
Itaboraian | 56.9 * | |||||||
Peligran | 58.9 * | |||||||
Selandian | Middle Paleocene | 59.2 | ||||||
Danian | Early Paleocene | 61.6 | ||||||
Tiupampan | 62.4 * | |||||||
66 |