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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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Detalles Bibliográficos
Autores principales:	Sun, Jimin, Ni, Xijun, Bi, Shundong, Wu, Wenyu, Ye, Jie, Meng, Jin, Windley, Brian F.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group 2014
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4264005/ https://www.ncbi.nlm.nih.gov/pubmed/25501388 http://dx.doi.org/10.1038/srep07463

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