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Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event

The Miocene Climatic Optimum (MCO, 14–17 Ma) was ~3–4 °C warmer than present, similar to estimates for 2100. Coincident with the MCO is the Monterey positive carbon isotope (δ(13)C) excursion, with oceans more depleted in (12)C relative to (13)C than any time in the past 50 Myrs. The long-standing M...

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Detalles Bibliográficos
Autores principales:	Sosdian, S. M., Babila, T. L., Greenop, R., Foster, G. L., Lear, C. H.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group UK 2020
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6952451/ https://www.ncbi.nlm.nih.gov/pubmed/31919344 http://dx.doi.org/10.1038/s41467-019-13792-0

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