Distinct iron isotopic signatures and supply from marine sediment dissolution
Iron (Fe) inputs to the surface ocean may stimulate photosynthesis and have an impact on the uptake of carbon dioxide in the ocean on glacial to inter-glacial timescales of climate change1. Global ocean reservoir-flux models2 indicate that 90% of Fe used by marine phytoplankton in the present day su...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
2013-07-19.
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Subjects: | |
Online Access: | Get fulltext |