Synchronous turnover of flora, fauna and climate at the Eocene–Oligocene Boundary in Asia

The Eocene–Oligocene Boundary (~34 million years ago) marks one of the largest extinctions of marine invertebrates in the world oceans and of mammalian fauna in Europe and Asia in the Cenozoic era. A shift to a cooler climate across this boundary has been suggested as the cause of this extinction in...

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Veröffentlicht in:	Scientific reports 2014-12, Vol.4 (1), p.7463-7463, Article 7463
Hauptverfasser:	Sun, Jimin, Ni, Xijun, Bi, Shundong, Wu, Wenyu, Ye, Jie, Meng, Jin, Windley, Brian F.
Format:	Artikel
Sprache:	eng
Schlagworte:	639/33/445/209 704/2151/413 Animals Asia Biological Evolution Climate Climate Change Ecosystem Fossils Geologic Sediments Humanities and Social Sciences Ice ages Marine environment multidisciplinary Oceans Oceans and Seas Phylogeny Science Seasons
Online-Zugang:	Volltext
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