Articles | Volume 12, issue 1
https://doi.org/10.5194/bg-12-209-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-209-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Variable C : N : P stoichiometry of dissolved organic matter cycling in the Community Earth System Model
Earth System Science, University of California, Irvine, CA, USA
J. K. Moore
Earth System Science, University of California, Irvine, CA, USA
Y.-C. Teng
Earth System Science, University of California, Irvine, CA, USA
F. Primeau
Earth System Science, University of California, Irvine, CA, USA
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- Modeling the impact of riverine DON removal by marine bacterioplankton on primary production in the Arctic Ocean V. Le Fouest et al. 10.5194/bgd-11-16953-2014
53 citations as recorded by crossref.
- Modelling the impact of riverine DON removal by marine bacterioplankton on primary production in the Arctic Ocean V. Le Fouest et al. 10.5194/bg-12-3385-2015
- Calibration of a simple and a complex model of global marine biogeochemistry I. Kriest 10.5194/bg-14-4965-2017
- Efficient dissolved organic carbon production and export in the oligotrophic ocean S. Roshan & T. DeVries 10.1038/s41467-017-02227-3
- Estimating Three‐Dimensional Carbon‐To‐Phosphorus Stoichiometry of Exported Marine Organic Matter E. Kwon et al. 10.1029/2021GB007154
- Natural aerosols explain seasonal and spatial patterns of Southern Ocean cloud albedo D. McCoy et al. 10.1126/sciadv.1500157
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- Global distribution and surface activity of macromolecules in offline simulations of marine organic chemistry O. Ogunro et al. 10.1007/s10533-015-0136-x
- Microbial Physiology Governs the Oceanic Distribution of Dissolved Organic Carbon in a Scenario of Equal Degradability A. Mentges et al. 10.3389/fmars.2020.549784
- Evaluation of the accuracy of an offline seasonally-varying matrix transport model for simulating ideal age A. Bardin et al. 10.1016/j.ocemod.2016.07.003
- Size Fractionation of Dissolved Organic Nitrogen in Peatland Fluvial Systems D. Edokpa et al. 10.1021/acs.est.8b01417
- Dynamics of the Marine Dissolved Organic Carbon Reservoir in Glacial Climate Simulations: The Importance of Biological Production M. Gilchrist & K. Matsumoto 10.1029/2022PA004522
- Global Patterns of Surface Ocean Dissolved Organic Matter Stoichiometry Z. Liang et al. 10.1029/2023GB007788
- Mesoscale Effects on Carbon Export: A Global Perspective C. Harrison et al. 10.1002/2017GB005751
- Inverse-model estimates of the ocean's coupled phosphorus, silicon, and iron cycles B. Pasquier & M. Holzer 10.5194/bg-14-4125-2017
- Phosphorus as an integral component of global marine biogeochemistry S. Duhamel et al. 10.1038/s41561-021-00755-8
- Annual Net Community Production of Particulate and Dissolved Organic Carbon From a Decade of Biogeochemical Profiling Float Observations in the Northeast Pacific W. Haskell et al. 10.1029/2020GB006599
- Calibrating a global three-dimensional biogeochemical ocean model (MOPS-1.0) I. Kriest et al. 10.5194/gmd-10-127-2017
- Convergent estimates of marine nitrogen fixation W. Wang et al. 10.1038/s41586-019-0911-2
- The Angola Gyre is a hotspot of dinitrogen fixation in the South Atlantic Ocean T. Marshall et al. 10.1038/s43247-022-00474-x
- Metagenomic analysis reveals global-scale patterns of ocean nutrient limitation L. Ustick et al. 10.1126/science.abe6301
- Sensitivity of Steady State, Deep Ocean Dissolved Organic Carbon to Surface Boundary Conditions K. Matsumoto et al. 10.1029/2021GB007102
- A simple method for the quantification of amidic bioavailable dissolved organic nitrogen in seawater R. Letscher & L. Aluwihare 10.1002/lom3.10622
- On the influence of “non‐Redfield” dissolved organic nutrient dynamics on the spatial distribution of N2 fixation and the size of the marine fixed nitrogen inventory C. Somes & A. Oschlies 10.1002/2014GB005050
- Microbial community composition and nitrogen availability influence DOC remineralization in the South Pacific Gyre R. Letscher et al. 10.1016/j.marchem.2015.06.024
- Biodiversity and Stoichiometric Plasticity Increase Pico‐Phytoplankton Contributions to Marine Net Primary Productivity and the Biological Pump R. Letscher et al. 10.1029/2023GB007756
- Characteristics of Using Feed Impact on Tilapia (Oreochromis niloticus) Culture Using a Dynamics System Approach A. Kurniawan et al. 10.20473/jafh.v12i3.43348
- Coccolithophore Growth and Calcification in an Acidified Ocean: Insights From Community Earth System Model Simulations K. Krumhardt et al. 10.1029/2018MS001483
- Does Marine Surface Tension Have Global Biogeography? Addition for the OCEANFILMS Package S. Elliott et al. 10.3390/atmos9060216
- Regionally Variable Contribution of Dissolved Organic Phosphorus to Marine Annual Net Community Production R. Letscher et al. 10.1029/2022GB007354
- A reevaluation of the magnitude and impacts of anthropogenic atmospheric nitrogen inputs on the ocean T. Jickells et al. 10.1002/2016GB005586
- Waste-based hydrothermal carbonization aqueous phase substitutes urea for rice paddy return: Improved soil fertility and grain yield H. He et al. 10.1016/j.jclepro.2022.131135
- Quantification of gene copy numbers is valuable in marine microbial ecology: A comment to Meiler et al. (2022) J. Zehr & L. Riemann 10.1002/lno.12364
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- Exploring the role of different data types and timescales in the quality of marine biogeochemical model calibration I. Kriest et al. 10.5194/bg-20-2645-2023
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- Long-term stability of marine dissolved organic carbon emerges from a neutral network of compounds and microbes A. Mentges et al. 10.1038/s41598-019-54290-z
- New nutrients exert fundamental control on dissolved organic carbon accumulation in the surface Atlantic Ocean C. Romera-Castillo et al. 10.1073/pnas.1605344113
- Marine phytoplankton stoichiometry mediates nonlinear interactions between nutrient supply, temperature, and atmospheric CO<sub>2</sub> A. Moreno et al. 10.5194/bg-15-2761-2018
- The Community Earth System Model Version 2 (CESM2) G. Danabasoglu et al. 10.1029/2019MS001916
- On the benefits of using cell quotas in addition to intracellular elemental ratios in flexible-stoichiometry Plankton functional type models. Application to the Mediterranean Sea M. Baklouti et al. 10.1016/j.pocean.2021.102634
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- Non-redfieldian mesopelagic nutrient remineralization in the eastern North Atlantic subtropical gyre B. Fernández-Castro et al. 10.1016/j.pocean.2018.12.001
- Dityrosine formation via reactive oxygen consumption yields increasingly recalcitrant humic‐like fluorescent organic matter in the ocean R. Paerl et al. 10.1002/lol2.10154
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- Subtropical Gyre Nutrient Cycling in the Upper Ocean: Insights From a Nutrient‐Ratio Budget Method Y. Xiang et al. 10.1029/2023GL103213
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- Southern Ocean carbon export efficiency in relation to temperature and primary productivity G. Fan et al. 10.1038/s41598-020-70417-z
- Nutrient uptake plasticity in phytoplankton sustains future ocean net primary production E. Kwon et al. 10.1126/sciadv.add2475
- Impact of the Elemental Composition of Exported Organic Matter on the Observed Dissolved Nutrient and Trace Element Distributions in the Upper Layer of the Ocean P. Quay 10.1029/2020GB006902
- Modelling marine DOC degradation time scales L. Polimene et al. 10.1093/nsr/nwy066
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Short summary
Marine DOM is known to exhibit stoichiometry depleted in N and P compared with POM, suggesting variable production and remineralization stoichiometry for C, N, and P within marine DOM cycling. We utilize marine DOM observations and an inverse tracer modeling framework to optimize DOM cycling parameters for the BEC biogeochemistry ocean model of the CESM, finding a variable stoichiometry with faster turnover of P > N > C superior to the commonly assumed Redfield stoichiometry for marine DOM.
Marine DOM is known to exhibit stoichiometry depleted in N and P compared with POM, suggesting...
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