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Marine phytoplankton and the changing ocean iron cycle
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“Iron is a micronutrient critical to fundamental biological processes including respiration and photosynthesis, and it can therefore impact primary and heterotrophic productivity.”
From Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth (2021) · cites this paper as Hutchins & Boyd, 2016
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Metadata
- Authors
- Hutchins, D. A., & Boyd, P. W.
- Venue
- Nature Climate Change
- Published
- 2016-11-24
- Volume
- 6
- Issue
- 12
- Pages
- 1072-1079
- ISSN
- 1758-678X
- 1758-6798
- Cited by
- 196
- References
- 4
- Language
- en
- Licence
- www.springer.com/tdm (tdm)
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