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Extreme sensitivity in Snowball Earth formation to mountains on PaleoProterozoic supercontinents
During the PaleoProterozoic 2.45 to 2.2 billion years ago, several glaciations may have produced Snowball Earths. These glacial cycles occurred during large environmental change when atmospheric oxygen was increasing, a supercontinent was assembled from numerous landmasses, and collisions between th...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2019
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6382813/ https://www.ncbi.nlm.nih.gov/pubmed/30787355 http://dx.doi.org/10.1038/s41598-019-38839-6 |