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Correlated terrestrial and marine evidence for global climate changes before mass extinction at the Cretaceous–Paleogene boundary

Terrestrial climates near the time of the end-Cretaceous mass extinction are poorly known, limiting understanding of environmentally driven changes in biodiversity that occurred before bolide impact. We estimate paleotemperatures for the last ≈1.1 million years of the Cretaceous (≈66.6–65.5 million...

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Autors principals: Wilf, Peter, Johnson, Kirk R., Huber, Brian T.
Format: Artigo
Idioma:Inglês
Publicat: The National Academy of Sciences 2003
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Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC141042/
https://ncbi.nlm.nih.gov/pubmed/12524455
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0234701100
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