Antarctic glacio-eustatic contributions to late Miocene Mediterranean desiccation and reflooding

The Messinian Salinity Crisis (MSC) was a marked late Neogene oceanographic event during which the Mediterranean Sea evaporated. Its causes remain unresolved, with tectonic restrictions to the Atlantic Ocean or glacio-eustatic restriction of flow during sea-level lowstands, or a mixture of the two m...

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Detalles Bibliográficos
Autores principales: Ohneiser, Christian, Florindo, Fabio, Stocchi, Paolo, Roberts, Andrew P., DeConto, Robert M., Pollard, David
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4659931/
https://www.ncbi.nlm.nih.gov/pubmed/26556503
http://dx.doi.org/10.1038/ncomms9765

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4659931/
https://www.ncbi.nlm.nih.gov/pubmed/26556503
http://dx.doi.org/10.1038/ncomms9765

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