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Constraints on soluble aerosol iron flux to the Southern Ocean at the Last Glacial Maximum.
TM Conway
,
EW Wolff
,
R Röthlisberger
,
R Mulvaney
,
HE Elderfield
OAI: oai:www.repository.cam.ac.uk:1810/248532
Published by:
Abstract
Iron
biogeochemistry
Antarctica
ice core
dust