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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Библиографические подробности
Опубликовано в: :Proc Natl Acad Sci U S A
Главные авторы: Sniderman, J. M. Kale, Woodhead, Jon D., Hellstrom, John, Jordan, Gregory J., Drysdale, Russell N., Tyler, Jonathan J., Porch, Nicholas
Формат: Artigo
Язык:Inglês
Опубликовано: National Academy of Sciences 2016
Предметы:
Physical Sciences
Online-ссылка: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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