Articles | Volume 17, issue 8
https://doi.org/10.5194/bg-17-2219-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-2219-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA
Jonas Nycander
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Andy Ridgwell
Department of Earth Sciences, University of California–Riverside, Riverside, CA 92521, USA
School of Geographical Sciences, Bristol University, Bristol BS8 1SS, UK
Kevin I. C. Oliver
National Oceanography Centre, Southampton, University of Southampton, Southampton SO14 3ZH, UK
Carlye D. Peterson
Department of Earth Sciences, University of California–Riverside, Riverside, CA 92521, USA
Johan Nilsson
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
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Cited
12 citations as recorded by crossref.
- Glacial deep ocean deoxygenation driven by biologically mediated air–sea disequilibrium E. Cliff et al. https://doi.org/10.1038/s41561-020-00667-z
- Toward Determining the Spatio-Temporal Variability of Upper-Ocean Ecosystem Stoichiometry From Satellite Remote Sensing T. Tanioka et al. https://doi.org/10.3389/fmars.2020.604893
- Physiological and metabolic effects of glyphosate as the sole P source on a cosmopolitan phytoplankter and biogeochemical implications C. Wang et al. https://doi.org/10.1016/j.scitotenv.2022.155094
- Ensemble simulation of the Last Glacial Maximum marine biogeochemistry and atmospheric pCO2 drawdown due to the soft-tissue biological carbon pump C. Chien et al. https://doi.org/10.5194/esd-17-1277-2026
- Carbon Export Buffering and CO2 Drawdown by Flexible Phytoplankton C:N:P Under Glacial Conditions K. Matsumoto et al. https://doi.org/10.1029/2019PA003823
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al. https://doi.org/10.1038/s41598-024-67391-1
- Estimating Three‐Dimensional Carbon‐To‐Phosphorus Stoichiometry of Exported Marine Organic Matter E. Kwon et al. https://doi.org/10.1029/2021GB007154
- C:N stoichiometry and the fate of organic carbon in ecosystems of the northwest Pacific Ocean C. Zhang et al. https://doi.org/10.1016/j.pocean.2024.103372
- Diagnosing the causes of AMOC slowdown in a coupled model: a cautionary tale J. Gérard & M. Crucifix https://doi.org/10.5194/esd-15-293-2024
- Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using δ13C A. Morée et al. https://doi.org/10.5194/cp-17-753-2021
- Stoichiometric modulation of zooplankton grazing on ocean organic matter biogeochemistry: Results from idealized food web modeling K. Matsumoto et al. https://doi.org/10.1016/j.ecolmodel.2025.111423
- Linkages Between Dynamic Phytoplankton C:N:P and the Ocean Carbon Cycle Under Climate Change K. Matsumoto et al. https://doi.org/10.5670/oceanog.2020.203
12 citations as recorded by crossref.
- Glacial deep ocean deoxygenation driven by biologically mediated air–sea disequilibrium E. Cliff et al. https://doi.org/10.1038/s41561-020-00667-z
- Toward Determining the Spatio-Temporal Variability of Upper-Ocean Ecosystem Stoichiometry From Satellite Remote Sensing T. Tanioka et al. https://doi.org/10.3389/fmars.2020.604893
- Physiological and metabolic effects of glyphosate as the sole P source on a cosmopolitan phytoplankter and biogeochemical implications C. Wang et al. https://doi.org/10.1016/j.scitotenv.2022.155094
- Ensemble simulation of the Last Glacial Maximum marine biogeochemistry and atmospheric pCO2 drawdown due to the soft-tissue biological carbon pump C. Chien et al. https://doi.org/10.5194/esd-17-1277-2026
- Carbon Export Buffering and CO2 Drawdown by Flexible Phytoplankton C:N:P Under Glacial Conditions K. Matsumoto et al. https://doi.org/10.1029/2019PA003823
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al. https://doi.org/10.1038/s41598-024-67391-1
- Estimating Three‐Dimensional Carbon‐To‐Phosphorus Stoichiometry of Exported Marine Organic Matter E. Kwon et al. https://doi.org/10.1029/2021GB007154
- C:N stoichiometry and the fate of organic carbon in ecosystems of the northwest Pacific Ocean C. Zhang et al. https://doi.org/10.1016/j.pocean.2024.103372
- Diagnosing the causes of AMOC slowdown in a coupled model: a cautionary tale J. Gérard & M. Crucifix https://doi.org/10.5194/esd-15-293-2024
- Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using δ13C A. Morée et al. https://doi.org/10.5194/cp-17-753-2021
- Stoichiometric modulation of zooplankton grazing on ocean organic matter biogeochemistry: Results from idealized food web modeling K. Matsumoto et al. https://doi.org/10.1016/j.ecolmodel.2025.111423
- Linkages Between Dynamic Phytoplankton C:N:P and the Ocean Carbon Cycle Under Climate Change K. Matsumoto et al. https://doi.org/10.5670/oceanog.2020.203
Saved (final revised paper)
Latest update: 03 Oct 2026
Short summary
In glacial periods, ocean uptake of carbon is likely a key player for achieving low atmospheric CO2. In climate models, ocean biological uptake of carbon (C) and phosphorus (P) are often assumed to occur in fixed proportions.
In this study, we allow the ratio of C : P to vary and simulate, to first approximation, the complex biological changes that occur in the ocean over long timescales. We show here that, for glacial–interglacial cycles, this complexity contributes to low atmospheric CO2.
In glacial periods, ocean uptake of carbon is likely a key player for achieving low atmospheric...
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