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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| 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 |