Biogeochemical Controls and Feedbacks on Ocean Primary Production
Abstract
Changes in oceanic primary production, linked to changes in the network of global biogeochemical cycles, have profoundly influenced the geochemistry of Earth for over 3 billion years. In the contemporary ocean, photosynthetic carbon fixation by marine phytoplankton leads to formation of ∼45 gigatons of organic carbon per annum, of which 16 gigatons are exported to the ocean interior. Changes in the magnitude of total and export production can strongly influence atmospheric CO 2 levels (and hence climate) on geological time scales, as well as set upper bounds for sustainable fisheries harvest. The two fluxes are critically dependent on geophysical processes that determine mixed-layer depth, nutrient fluxes to and within the ocean, and food-web structure. Because the average turnover time of phytoplankton carbon in the ocean is on the order of a week or less, total and export production are extremely sensitive to external forcing and consequently are seldom in steady state. Elucidating the biogeochemical controls and feedbacks on primary production is essential to understanding how oceanic biota responded to and affected natural climatic variability in the geological past, and will respond to anthropogenically influenced changes in coming decades. One of the most crucial feedbacks results from changes in radiative forcing on the hydrological cycle, which influences the aeolian iron flux and, in turn, affects nitrogen fixation and primary production in the oceans.
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Algae efficiently use CO2 and are responsible for more than 40% of global carbon fixation, with the majority of this productivity coming from marine microalgae.
“Algae efficiently use CO2, and are responsible for more than 40% of the global carbon fixation, with the majority of this productivity coming from marine microalgae [14,15].”
From Biofuels from algae: Challenges and potential (2010) · cites this paper as [14]
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De Riso, V., Raniello, R., Maumus, F., Rogato, A., Bowler, C., & Falciatore, A. (2009) · Nucleic Acids Research · doi:10.1093/nar/gkp448 · Cited by 305 · see citing works
Cyanobacteria and eukaryotic algae use different chemical variants of vitamin B12
Helliwell, K. E., Lawrence, A. D., Holzer, A., Kudahl, U. J., Sasso, S., Kräutler, B., Scanlan, D. J., Warren, M. J., & Smith, A. G. (2016) · Current Biology · doi:10.1016/j.cub.2016.02.041 · Cited by 250 · see citing works
Wang, J., Chen, D., Yan, D., Wei, H., & Xiang, L. (2012) · Chemical Geology · doi:10.1016/j.chemgeo.2012.03.005 · Cited by 192 · see citing works
Genomic Insights into Marine Microalgae
Parker, M. S., Mock, T., & Armbrust, E. V. (2008) · Annual Review of Genetics · doi:10.1146/annurev.genet.42.110807.091417 · Cited by 182 · see citing works
Diatom cultivation and biotechnologically relevant products. Part I: Cultivation at various scales
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Kranz, S. A., Dieter, S., Richter, K.-U., & Rost, B. (2009) · Limnology and Oceanography · doi:10.4319/lo.2009.54.2.0548 · Cited by 128 · see citing works
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The cryptochrome/photolyase family in aquatic organisms
Oliveri, P., Fortunato, A. E., Petrone, L., Ishikawa-Fujiwara, T., Kobayashi, Y., Todo, T., Antonova, O., Arboleda, E., Zantke, J., Tessmar-Raible, K., et al. (2014) · Marine Genomics · doi:10.1016/j.margen.2014.02.001 · Cited by 90 · see citing works
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African desert dust influences migrations and fisheries of the Atlantic skipjack-tuna
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“Of special importance are the limiting/co-limiting nutrients (Moore et al., 2013), both macronutrients, like N and P (Falkowski, 1998; Moore et al., 2013), and micronutrients such as iron (Fe), manganese (Mn), cobalt (Co), zinc (Zn) or nickel (Ni) (Rees and Bekheet, 1982; Price and Morel, 1990;…”
- Authors
- Falkowski, P. G., Barber, R. T., & Smetacek, V.
- Affiliations
- Rutgers, The State University of New Jersey (US)
- Corresponding author
- Falkowski, Paul G.
- Venue
- Science
- Published
- 1998-07-10
- Volume
- 281
- Issue
- 5374
- Pages
- 200-206
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2105796581
- Cited by
- 2,848
- References
- 99
- Citations by year
- 2026: 165 · 2025: 151 · 2024: 178 · 2023: 155 · 2022: 195 · 2021: 170 · 2020: 153 · 2019: 136 · 2018: 122 · 2017: 121 · 2016: 111 · 2015: 110 · 2014: 125 · 2013: 123 · 2012: 97
- FWCI
- 33.37
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Helmholtz-Zentrum für Polar-und Meeresforschung (Alfred-Wegener-Institut) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
- Keywords
- ocean primary productivity, phytoplankton, export production, biogeochemical cycles, carbon cycle, atmospheric CO2, mixed layer depth, nutrient fluxes, food web structure, nitrogen fixation, radiative forcing, water cycle, climate feedbacks, sustainable fisheries, paleoceanography
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