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Rapid ocean acidification and protracted Earth system recovery followed the end-Cretaceous Chicxulub impact
Mass extinction at the Cretaceous–Paleogene (K-Pg) boundary coincides with the Chicxulub bolide impact and also falls within the broader time frame of Deccan trap emplacement. Critically, though, empirical evidence as to how either of these factors could have driven observed extinction patterns and...
Autores principales: | Henehan, Michael J., Ridgwell, Andy, Thomas, Ellen, Zhang, Shuang, Alegret, Laia, Schmidt, Daniela N., Rae, James W. B., Witts, James D., Landman, Neil H., Greene, Sarah E., Huber, Brian T., Super, James R., Planavsky, Noah J., Hull, Pincelli M. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
National Academy of Sciences
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6842625/ https://www.ncbi.nlm.nih.gov/pubmed/31636204 http://dx.doi.org/10.1073/pnas.1905989116 |
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