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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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| Pubblicato in: | Proc Natl Acad Sci U S A |
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| Autori principali: | , , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2016
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| Soggetti: | |
| Accesso online: | 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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