Iron from melting glaciers fuels the phytoplankton blooms in Amundsen Sea (Southern Ocean):Iron biogeochemistry
Dissolved iron (DFe) and total dissolvable Fe (TDFe) were measured in January-February 2009 in Pine Island Bay, as well as in the Pine Island and Amundsen polynyas (Amundsen Sea, Southern Ocean). Iron (Fe) has been shown to be a limiting nutrient for phytoplankton growth, even in the productive cont...
Published in: | Deep Sea Research Part II: Topical Studies in Oceanography |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2012
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Subjects: | |
Online Access: | https://hdl.handle.net/11370/bf3ba305-79f5-4e6d-8c9d-9ffd86d25f2e https://research.rug.nl/en/publications/bf3ba305-79f5-4e6d-8c9d-9ffd86d25f2e https://doi.org/10.1016/j.dsr2.2012.03.007 |