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Preindustrial, historical, and fertilization simulations using a global ocean carbon model with new parameterizations of iron limitation, calcification, and N2 fixation
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“This idea is easily illustrated with iron, which is the most common metal co-factor and a limiting micronutrient in large regions of the oceans today, especially high-nutrient low chlorophyll (HNLC) regions (for reviews see Zahariev et al., 2008;Moore et al., 2013).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Zahariev et al., 2008
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Self-citation
Metadata
- Authors
- Zahariev, K., Christian, J. R., & Denman, K. L.
- Affiliations
- University of Victoria (CA)
- Fisheries and Oceans Canada (CA)
- Corresponding author
- Zahariev, Konstantin
- Venue
- Progress In Oceanography
- Publisher
- Elsevier BV
- Published
- 2008-04
- Volume
- 77
- Issue
- 1
- Pages
- 56-82
- ISSN
- 0079-6611 (ISSN-L)
- OpenAlex
- W1977892071
- Cited by
- 108
- References
- 91
- Citations by year
- 2026: 2 · 2025: 3 · 2024: 2 · 2023: 13 · 2022: 11 · 2021: 11 · 2020: 6 · 2019: 6 · 2018: 8 · 2017: 3 · 2016: 4 · 2015: 4 · 2014: 7 · 2013: 8 · 2012: 3
- FWCI
- 3.95
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Progress In Oceanography (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- ocean carbon cycle, iron limitation, iron fertilization, biological carbon pump, calcification, nitrogen fixation, air-sea CO2 flux, ocean alkalinity, dust deposition, glacial maximum, ocean carbon uptake, radiative forcing
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