The DOI matches its Crossref record; 32 of the 32 references it cites were found in a registry or an index.
The flux of iron from continental shelf sediments: A missing source for global budgets
Abstract
The flux of dissolved iron from sediments to the water column was measured with flux chambers along the California coast over a five‐year period. High fluxes were observed from sediments on the continental shelf. The measured fluxes were an average of 75 times larger than flux values derived from pore‐water iron gradients. The iron flux was significantly correlated with the oxidation of organic matter, which allows an extrapolation to the global shelf. The input from shelf sediments is at least as significant as the global input of dissolved iron from aerosols, which has been presumed to be the dominant external iron source. Evidence of this input is seen 100's of kilometers offshore where it can enable the high productivity of broad coastal regions seen in satellite images.
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Citations
Cites
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What controls dissolved iron concentrations in the world ocean?
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Self-citationShaw, T. J., Gieskes, J. M., & Jahnke, R. A. (1990) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(90)90149-f · Cited by 686
Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogen
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Iron cycling and nutrient-limitation patterns in surface waters of the World Ocean
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The Biogeochemistry of Iron in Seawater
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Cited by
The biogeochemical cycle of iron in the ocean
Boyd, P. W., & Ellwood, M. J. (2010) · Nature Geoscience · doi:10.1038/ngeo964 · Cited by 992
The organic complexation of iron in the marine environment: a review
Gledhill, M. (2012) · Frontiers in Microbiology · doi:10.3389/fmicb.2012.00069 · Cited by 631
A critical look at iron paleoredox proxies: New insights from modern euxinic marine basins
Lyons, T. W., & Severmann, S. (2006) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2006.08.021 · Cited by 630
Controls of Trace Metals in Seawater
Bruland, K. W., Middag, R., & Lohan, M. C. (2014) · Treatise on Geochemistry · doi:10.1016/b978-0-08-095975-7.00602-1 · Cited by 502
How well do global ocean biogeochemistry models simulate dissolved iron distributions?
Tagliabue, A., Aumont, O., DeAth, R., Dunne, J. P., Dutkiewicz, S., Galbraith, E., Misumi, K., Moore, J. K., Ridgwell, A., Sherman, E., et al. (2016) · Global Biogeochemical Cycles · doi:10.1002/2015gb005289 · Cited by 371
Metadata
- Authors
- Elrod, V. A., Berelson, W. M., Coale, K. H., & Johnson, K. S.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2004-06
- Volume
- 31
- Issue
- 12
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2067961116
- Cited by
- 485
- References
- 32
- FWCI
- 8.72
- Type
- journal article
- Language
- en
- Open access
- closed
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- Elrod, V. A., Berelson, W. M., Coale, K. H., & Johnson, K. S. (2004). The flux of iron from continental shelf sediments: A missing source for global budgets. Geophysical Research Letters. https://doi.org/10.1029/2004gl020216
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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