Natural iron fertilization of the Atlantic sector of the Southern Ocean by continental shelf sources of the Antarctic Peninsula
In large parts of the Southern Ocean, primary production is limited due to shortage of iron (Fe). We measured vertical Fe profiles in the western Weddell Sea, Weddell‐Scotia Confluence, and Antarctic Circumpolar Current (ACC), showing that Fe is derived from benthic Fe diffusion and sediment resuspe...
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Veröffentlicht in: | Journal of Geophysical Research: Biogeosciences 2012-03, Vol.117 (G1), p.n/a |
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Sprache: | eng |
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