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Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering
Authigenic clay minerals formed on or in the seafloor occur in every type of marine sediment. They are recognized to be a major sink of many elements in the ocean but are difficult to study directly due to dilution by detrital clay minerals. The extremely low dust fluxes and marine sedimentation rat...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5635029/ https://www.ncbi.nlm.nih.gov/pubmed/29018196 http://dx.doi.org/10.1038/s41467-017-00853-5 |