Processes and patterns of oceanic nutrient limitation
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Iron is the most common metal co-factor and a limiting micronutrient in large regions of the modern ocean, especially HNLC regions.
“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 Moore et al., 2013
Moore et al. (2013) highlighted spatial heterogeneity on a global scale in surface waters for major limiting nutrients such as nitrate or phosphate, as well as trace metals.
“As well, Moore et al. (2013) have highlighted spatial heterogeneity on a global scale in surface waters with regards to both major limiting nutrients such as nitrate or phosphate, as well as trace metals.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Moore et al., 2013
The Peru Margin δ15N record broadly agrees with earlier reconstructions of water-column denitrification intensity and extent between glacial and interglacial periods, with lower δ15N in glacial stages and higher δ15N in interglacial stages.
“The δ 15 N record from the Peru Margin is broadly consistent with previously inferred changes in the intensity and/or extent of areas of water-column denitrification between glacial and interglacial periods, i.e., lower δ 15 N during glacial stages and higher δ 15 N during interglacial stages (Fig. 2c; see Galbraith and Kienast, 2013;Moore et al., 2013).”
From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Moore et al., 2013
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Marañón, E. (2015) · Annual Review of Marine Science · doi:10.1146/annurev-marine-010814-015955 · Cited by 514 · see citing works
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Self-citationAerosol Deposition Impacts on Land and Ocean Carbon Cycles
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“…among other elements) (Reid, 2003; P ´ erez García-Pando et al., 2016; Rodríguez et al., 2020) that stimulate the growth of phytoplankton in two ways: by direct nutrients supply (Moore et al., 2013) and by providing Fe and P that stimulate N fixation, alleviating N limitation (Mills et al., 2004).”
- Authors
- Moore, C. M., Mills, M. M., Arrigo, K. R., Berman-Frank, I., Bopp, L., Boyd, P. W., Galbraith, E. D., Geider, R. J., Guieu, C., Jaccard, S. L., Jickells, T. D., La Roche, J., Lenton, T. M., Mahowald, N. M., Marañón, E., Marinov, I., Moore, J. K., Nakatsuka, T., Oschlies, A., Saito, M. A., Thingstad, T. F., Tsuda, A., & Ulloa, O.
- Affiliations
- National Oceanography Centre (GB)
- Stanford University (US)
- Centre National de la Recherche Scientifique (FR)
- University of Tasmania (AU)
- McGill University (CA)
- University of Essex (GB)
- ETH Zurich (CH)
- University of East Anglia (GB)
- University of Exeter (GB)
- Cornell University (US)
- University of Pennsylvania (US)
- University of California, Irvine (US)
- Nagoya University (JP)
- GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
- Woods Hole Oceanographic Institution (US)
- University of Bergen (NO)
- Atmosphere and Ocean Research Institute, The University of Tokyo (JP)
- University of Concepción (CL)
- Corresponding author
- Moore, C. M.
- Mills, M. M.
- ORCID
- Venue
- Nature Geoscience
- Published
- 2013-03-31
- Volume
- 6
- Issue
- 9
- Pages
- 701-710
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2036677156
- Cited by
- 2,236
- References
- 100
- Citations by year
- 2026: 170 · 2025: 219 · 2024: 212 · 2023: 221 · 2022: 231 · 2021: 255 · 2020: 176 · 2019: 166 · 2018: 154 · 2017: 125 · 2016: 133 · 2015: 95 · 2014: 68 · 2013: 8
- FWCI
- 71.84
- Type
- journal article
- Language
- en
- Open access
- green
- escholarship.org
- Licence
- Locations
- Nature Geoscience (publishedVersion)
- Open Access at Essex (University of Essex) (acceptedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (submittedVersion)
- eCite Digital Repository (University of Tasmania) (submittedVersion)
- HAL (submittedVersion)
- BORIS (University Library Bern) (submittedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- eScholarship (California Digital Library) (submittedVersion, cc-by)
- Figshare (submittedVersion)
- Oskar-Bordeaux (Universite de Bordeaux) (submittedVersion)
- UEA Digital Repository (University of East Anglia) (submittedVersion)
- Funders
- Japan Society for the Promotion of Science (24121004, 20241003)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- phytoplankton, nitrogen limitation, iron limitation, phosphorus limitation, micronutrients, co-limitation, nutrient stoichiometry, upwelling zones, Southern Ocean, eastern equatorial Pacific, ocean primary productivity
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