Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum

The Middle Eocene Climatic Optimum (around 40 million years ago) was a roughly 400,000-year-long global warming phase associated with an increase in atmospheric CO(2) concentrations and deep-ocean acidification that interrupted the Eocene’s long-term cooling trend. The unusually long duration, compa...

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Detalles Bibliográficos
Autores principales: Krause, Alexander J., Sluijs, Appy, van der Ploeg, Robin, Lenton, Timothy M., Pogge von Strandmann, Philip A. E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10409649/
https://www.ncbi.nlm.nih.gov/pubmed/37564379
http://dx.doi.org/10.1038/s41561-023-01234-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10409649/
https://www.ncbi.nlm.nih.gov/pubmed/37564379
http://dx.doi.org/10.1038/s41561-023-01234-y

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