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Terrestrial cooling in Northern Europe during the Eocene–Oligocene transition
Geochemical and modeling studies suggest that the transition from the “greenhouse” state of the Late Eocene to the “icehouse” conditions of the Oligocene 34–33.5 Ma was triggered by a reduction of atmospheric pCO(2) that enabled the rapid buildup of a permanent ice sheet on the Antarctic continent....
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| Main Authors: | , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2013
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3651463/ https://ncbi.nlm.nih.gov/pubmed/23610424 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1210930110 |
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