Upper limits on the extent of seafloor anoxia during the PETM from uranium isotopes

The Paleocene Eocene Thermal Maximum (PETM) represents a major carbon cycle and climate perturbation that was associated with ocean de-oxygenation, in a qualitatively similar manner to the more extensive Mesozoic Oceanic Anoxic Events. Although indicators of ocean de-oxygenation are common for the P...

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Detalles Bibliográficos
Autores principales: Clarkson, Matthew O., Lenton, Timothy M., Andersen, Morten B., Bagard, Marie-Laure, Dickson, Alexander J., Vance, Derek
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7810695/
https://www.ncbi.nlm.nih.gov/pubmed/33452243
http://dx.doi.org/10.1038/s41467-020-20486-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7810695/
https://www.ncbi.nlm.nih.gov/pubmed/33452243
http://dx.doi.org/10.1038/s41467-020-20486-5

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