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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Detalles Bibliográficos
Autores principales: Conway, T.M., Wolff, E.W., Röthlisberger, R., Mulvaney, R., Elderfield, H.E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4525188/
https://www.ncbi.nlm.nih.gov/pubmed/26204562
http://dx.doi.org/10.1038/ncomms8850

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4525188/
https://www.ncbi.nlm.nih.gov/pubmed/26204562
http://dx.doi.org/10.1038/ncomms8850

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