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Loss of fixed nitrogen causes net oxygen gain in a warmer future ocean
Oceanic anoxic events have been associated with warm climates in Earth history, and there are concerns that current ocean deoxygenation may eventually lead to anoxia. Here we show results of a multi-millennial global-warming simulation that reveal, after a transitory deoxygenation, a marine oxygen i...
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| Gepubliceerd in: | Nat Commun |
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| Hoofdauteurs: | , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Nature Publishing Group UK
2019
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6594934/ https://ncbi.nlm.nih.gov/pubmed/31243270 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-10813-w |
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