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Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition

Rapid global cooling at the Eocene – Oligocene Transition (EOT), ~33.9–33.5 Ma, is widely considered to mark the onset of the modern icehouse world. A large and rapid drop in atmospheric pCO(2) has been proposed as the driving force behind extinctions in the marine realm and glaciation on Antarctica...

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Detalles Bibliográficos
Autores principales: Pound, Matthew J., Salzmann, Ulrich
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5324063/
https://www.ncbi.nlm.nih.gov/pubmed/28233862
http://dx.doi.org/10.1038/srep43386