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The Oligo–Miocene closure of the Tethys Ocean and evolution of the proto-Mediterranean Sea
The tectonically driven Cenozoic closure of the Tethys Ocean invoked a significant reorganization of oceanic circulation and climate patterns on a global scale. This process culminated between the Mid Oligocene and Late Miocene, although its exact timing has remained so far elusive, as does the subs...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7427807/ https://www.ncbi.nlm.nih.gov/pubmed/32796882 http://dx.doi.org/10.1038/s41598-020-70652-4 |