Dynamic Greenland ice sheet driven by pCO(2) variations across the Pliocene Pleistocene transition

It is generally considered that the perennial glaciation of Greenland lasting several orbital cycles began around 2.7 Ma along with the intensification of Northern Hemisphere glaciation (NHG). Both data and model studies have demonstrated that a decline in atmospheric pCO(2) was instrumental in esta...

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Detalles Bibliográficos
Autores principales: Tan, Ning, Ladant, Jean-Baptiste, Ramstein, Gilles, Dumas, Christophe, Bachem, Paul, Jansen, Eystein
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6232173/
https://www.ncbi.nlm.nih.gov/pubmed/30420596
http://dx.doi.org/10.1038/s41467-018-07206-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6232173/
https://www.ncbi.nlm.nih.gov/pubmed/30420596
http://dx.doi.org/10.1038/s41467-018-07206-w

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