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
Published in:Nature Communications
Main Authors: Conway, T. M., Wolff, E. W., Röthlisberger, R., Mulvaney, R., Elderfield, H.
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2015
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/3527/
http://eprints.esc.cam.ac.uk/3527/1/ncomms8850.pdf
http://eprints.esc.cam.ac.uk/3527/2/ncomms8850-f1.jpg
http://www.nature.com/doifinder/10.1038/ncomms8850
https://doi.org/10.1038/ncomms8850