Iron Biogeochemistry in the High Latitude North Atlantic Ocean-Reference-Cited by-同舟云学术

Iron Biogeochemistry in the High Latitude North Atlantic Ocean

Published:2018-01-19 Issue:1 Volume:8 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Achterberg Eric P.,Steigenberger Sebastian,Marsay Chris M.,LeMoigne Frédéric A. C.,Painter Stuart C.,Baker Alex R.^ORCID,Connelly Douglas P.,Moore C. Mark,Tagliabue Alessandro,Tanhua Toste^ORCID

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41598-018-19472-1.pdf

Reference99 articles.

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2. Wu, J., Sunda, W., Boyle, E. A. & Karl, D. M. Phosphate Depletion in the Western North Atlantic. Ocean. Science 289, 759–762, https://doi.org/10.1126/science.289.5480.759 (2000).

3. Nelson, D. M., Brzezinski, M. A., Sigmon, D. E. & Franck, V. M. A seasonal progression of Si limitation in the Pacific sector of the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography 48, 3973–3995, https://doi.org/10.1016/S0967-0645(01)00076-5 (2001).

4. Martin, J. H. & Fitzwater, S. E. Iron deficiency limits phytoplankton growth in the northeast Pacific subartic. Nature 331, 341–343 (1988).

5. Coale, K. H. et al. A massive phytplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean. Nature 383, 495–501 (1996).

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