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 CO2 cycles. Ice and marine sediment records demonstrate that atmospheric dust supply to the oceans increase...
Published in: | Nature Communications |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Digital Commons @ University of South Florida
2015
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Subjects: | |
Online Access: | https://digitalcommons.usf.edu/geo_facpub/1490 https://doi.org/10.1038/ncomms8850 https://digitalcommons.usf.edu/context/geo_facpub/article/2529/viewcontent/ncomms8850.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2529/filename/0/type/additional/viewcontent/ncomms8850.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2529/filename/1/type/additional/viewcontent/ncomms8850_s1.pdf |