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Greenhouse- and orbital-forced climate extremes during the early Eocene
The Palaeocene–Eocene Thermal Maximum (PETM) was a significant global warming event in Earth's deep past (56 Mya). The warming across the PETM boundary was driven by a rapid rise in greenhouse gases. The event also coincided with a time of maximum insolation in Northern Hemisphere summer. There...
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| Udgivet i: | Philos Trans A Math Phys Eng Sci |
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| Main Authors: | , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
The Royal Society Publishing
2018
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6127382/ https://ncbi.nlm.nih.gov/pubmed/30177566 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2017.0085 |
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