Cretaceous-Cenozoic of New Zealand
The interval definitions in this timescale are derived from the following sources:
- 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
- P. L. Gibbard, M. J. Head, and M. J. C. Walker. 2010. Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma. Journal of Quaternary Science 25(2):96-102 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
- M. Freudenthal. 2006. Mammal Paleogene zones. personal communication view
- J. Meng and M. C. McKenna. 1998. Faunal turnovers of Paleogene mammals from the Mongolian Plateau. Nature 394:364-367 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.
This timescale is used in the definition of 1251 collections
International Chronostratigraphic Timescale | Cretaceous-Cenozoic of New Zealand | Cenozoic Subepochs of Southern Europe | European Faunal Units | Mammal Paleogene Zones | Paleogene Mammal Ages of Asia | European Faunal Zones | ||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Quaternary | Holocene | Meghalayan | Wanganui | Haweran | 0 | |||||||
Northgrippian | 0.0042 | |||||||||||
Greenlandian | 0.0082 | |||||||||||
Pleistocene | Late Pleistocene | Tarantian | 0.0117 | |||||||||
Chibanian | Ionian | 0.129 | ||||||||||
Castlecliffian | 0.34 | |||||||||||
Calabrian | 0.774 | |||||||||||
Nukumaruan | 1.63 | |||||||||||
Gelasian | MN 17 | 1.8 | ||||||||||
Mangapanian | 2.4 | |||||||||||
Neogene | Pliocene | Piacenzian | Villanyian | MN 16 | 2.58 | |||||||
Waipipian | 3 | |||||||||||
Ruscinian | 3.1 * | |||||||||||
MN 15 | 3.2 | |||||||||||
Zanclean | 3.6 | |||||||||||
Opoitian | 3.7 | |||||||||||
MN 14 | 4.2 | |||||||||||
MN 13 | 4.9 | |||||||||||
Miocene | Messinian | Taranaki | Kapitean | Turolian | 5.333 | |||||||
Tongaporutuan | 7.2 | |||||||||||
Tortonian | MN 12 | 7.246 | ||||||||||
MN 11 | 7.75 | |||||||||||
Vallesian | MN 10 | 8.7 | ||||||||||
MN 9 | 9.7 | |||||||||||
Southland | Waiauan | 11.04 | ||||||||||
MN 7 + 8 | 11.1 | |||||||||||
Serravallian | Astaracian | 11.63 | ||||||||||
MN 6 | 12.8 * | |||||||||||
Lillburnian | 13.05 | |||||||||||
Langhian | MN 5 | 13.82 | ||||||||||
Clifdenian | 15.1 | |||||||||||
Pareora | Altonian | 15.9 | ||||||||||
Burdigalian | Orleanian | MN 4 | 15.98 | |||||||||
MN 3 | 16.9 | |||||||||||
Otaian | 18.7 | |||||||||||
Agenian | MN 2 | 20 | ||||||||||
Aquitanian | 20.44 | |||||||||||
Landon | Waitakian | 21.7 | ||||||||||
MN 1 | 22.4 | |||||||||||
Paleogene | Oligocene | Chattian | MP 30/MP 29/MP 28/MP 27/MP 26 | MP 25 | Tabenbulakian | Hsandagolian | 23.03 | |||||
Duntroonian | 25.2 | |||||||||||
Whaingaroan | 27.3 | |||||||||||
Rupelian | MP 24/MP 23/MP 22/MP 21 | Kekeamuan | 27.82 | |||||||||
Eocene | Priabonian | MP 20/MP 19/MP 18/MP 17B/MP 17A | Houldjinian/Ergilian/Ulangochuian | 33.9 | ||||||||
Arnold | Runangan | 34.6 | ||||||||||
Kaiatan | 36.7 | |||||||||||
Bartonian | MP 16 | Sharamurunian/Irdinmanhan/Arshantan | 37.71 | |||||||||
Bortonian | 39.1 | |||||||||||
Lutetian | MP 15/MP 14/MP 13/MP 12/MP 11 | 41.2 | ||||||||||
Dannevirke | Porangan | 42.6 | ||||||||||
Heretaungan | 45.7 | |||||||||||
Ypresian | MP 10/MP 8 + 9/MP 7 | Bumbanian | 47.8 | |||||||||
Mangaorapan | 48.9 | |||||||||||
Waipawan | 52 | |||||||||||
Paleocene | Thanetian | Teurian | MP 6 | MP 1 - 5 | Gashatan | 56 | ||||||
Selandian | 59.2 | |||||||||||
Danian | 61.6 | |||||||||||
Cretaceous | Late Cretaceous | Maastrichtian | Mata | Haumurian | 66 | |||||||
Campanian | 72.1 | |||||||||||
Santonian | Piripauan | 83.6 | ||||||||||
Raukumara | Teratan | 86.1 | ||||||||||
Coniacian | 86.3 | |||||||||||
Turonian | 89.8 | |||||||||||
Mangaotanean | 90.5 | |||||||||||
Arowhanan | 93.7 | |||||||||||
Cenomanian | 93.9 | |||||||||||
Clarence | Ngaterian | 95.2 | ||||||||||
Motuan | 99.5 | |||||||||||
Early Cretaceous | Albian | 100.5 | ||||||||||
Urutawan | 103.3 | |||||||||||
Taitai | Korangan | 108.4 | ||||||||||
Aptian | 113 | |||||||||||
117.5 | ||||||||||||
Barremian | 121.4 | |||||||||||
Hauterivian | 125.77 | |||||||||||
Valanginian | 132.6 | |||||||||||
Berriasian | 139.8 | |||||||||||
145 |