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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...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2017
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| 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 |