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Constraints on soluble aerosol iron flux to the Southern Ocean at the Last Glacial Maximum
Relief of iron (Fe) limitation in the Southern Ocean during ice ages, with potentially increased carbon storage in the ocean, has been invoked as one driver of glacial–interglacial atmospheric CO(2) cycles. Ice and marine sediment records demonstrate that atmospheric dust supply to the oceans increa...
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| Publicado en: | Nat Commun |
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| Autores principales: | , , , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Nature Pub. Group
2015
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4525188/ https://ncbi.nlm.nih.gov/pubmed/26204562 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms8850 |
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