Continental-shelf sediment as a primary source of iron for coastal phytoplankton
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/19511.pdf
Reference26 articles.
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3. Johnson, K. S., Gordon, R. M. & Coale, K. H. What controls dissolved iron in the world ocean? Mar. Chem. 57, 137–161 (1997).
4. Chavez, F. P. et al. Horizontal transport and the distribution of nutrients in the Coastal Transition Zone off Northern California: effects on primary production, phytoplankton biomass and species composition. J. Geophys. Res. 96, 14833–14848 (1991).
5. Hutchins, D. A. & Bruland, K. W. Iron-limited diatom growth and Si:N uptake ratios in a coastal upwelling regime. Nature 393, 561–564.
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