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The role of marine sediment diagenesis in the modern oceanic magnesium cycle
The oceanic magnesium cycle is largely controlled by continental weathering and marine authigenic mineral formation, which are intimately linked to long-term climate. Uncertainties in the magnesium cycle propagate into other chemical budgets, and into interpretations of paleo-oceanographic reconstru...
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| Опубликовано в: : | Nat Commun |
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| Главные авторы: | , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group UK
2019
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6761265/ https://ncbi.nlm.nih.gov/pubmed/31554801 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-12322-2 |
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