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

Internet

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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