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...

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Bibliographic Details
Main Authors: Conway, Tim M., Wolff, E. W., Röthlisberger, R., Mulvaney, R., Elderfield, H. E.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2015
Subjects:
Online Access:https://digitalcommons.usf.edu/geo_facpub/1490
https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2529&context=geo_facpub