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...

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Detalles Bibliográficos
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.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2019
Materias:
Physical Sciences
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

Internet

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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