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Rapid short-term cooling following the Chicxulub impact at the Cretaceous–Paleogene boundary
The mass extinction at the Cretaceous–Paleogene boundary, ∼66 Ma, is thought to be caused by the impact of an asteroid at Chicxulub, present-day Mexico. Although the precise mechanisms that led to this mass extinction remain enigmatic, most postulated scenarios involve a short-lived global cooling,...
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| Auteurs principaux: | , , , , , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
National Academy of Sciences
2014
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| Sujets: | |
| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4040585/ https://ncbi.nlm.nih.gov/pubmed/24821785 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1319253111 |
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