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Pliocene reversal of late Neogene aridification

The Pliocene epoch (5.3–2.6 Ma) represents the most recent geological interval in which global temperatures were several degrees warmer than today and is therefore considered our best analog for a future anthropogenic greenhouse world. However, our understanding of Pliocene climates is limited by po...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Sniderman, J. M. Kale, Woodhead, Jon D., Hellstrom, John, Jordan, Gregory J., Drysdale, Russell N., Tyler, Jonathan J., Porch, Nicholas
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2016
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC4776468/
https://ncbi.nlm.nih.gov/pubmed/26858429
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1520188113
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