Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum

Understanding marine environmental change and associated biological turnover across the Palaeocene–Eocene Thermal Maximum (PETM; ~56 Ma)—the most pronounced Cenozoic short-term global warming event—is important because of the potential role of the ocean in atmospheric CO(2) drawdown, yet proxies for...

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Detalles Bibliográficos
Autores principales: Chang, Liao, Harrison, Richard J., Zeng, Fan, Berndt, Thomas A., Roberts, Andrew P., Heslop, David, Zhao, Xiang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6167317/
https://www.ncbi.nlm.nih.gov/pubmed/30275540
http://dx.doi.org/10.1038/s41467-018-06472-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6167317/
https://www.ncbi.nlm.nih.gov/pubmed/30275540
http://dx.doi.org/10.1038/s41467-018-06472-y

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