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Deep ocean carbonate ion increase during mid Miocene CO(2) decline

Characterised by long term cooling and abrupt ice sheet expansion on Antarctica ~14 Ma ago, the mid Miocene marked the beginning of the modern ice-house world, yet there is still little consensus on its causes, in part because carbon cycle dynamics are not well constrained. In particular, changes in...

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Detalles Bibliográficos
Autores principales:	Kender, Sev, Yu, Jimin, Peck, Victoria L.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group 2014
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3935200/ https://www.ncbi.nlm.nih.gov/pubmed/24569646 http://dx.doi.org/10.1038/srep04187

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