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Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
The Earth underwent a major transition from the warm climates of the Pliocene to the Pleistocene ice ages between 3.2 and 2.6 million years ago. The intensification of Northern Hemisphere Glaciation is the most obvious result of the Plio-Pleistocene transition. However, recent data show that the oce...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5337981/ https://www.ncbi.nlm.nih.gov/pubmed/28252023 http://dx.doi.org/10.1038/ncomms14376 |