Articles | Volume 14, issue 5
https://doi.org/10.5194/gmd-14-2713-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-14-2713-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model description paper
| 
18 May 2021
Model description paper |
| 18 May 2021
| 18 May 2021
Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21)
Sebastiaan J. van de Velde
CORRESPONDING AUTHOR
Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA
current address: Bgeosys, Geoscience, Environment & Society, Université Libre de Bruxelles, Brussels, Belgium
current address: Operational Directorate Natural Environment, Royal Belgian Institute of Natural Sciences, Brussels, Belgium
Dominik Hülse
Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA
Christopher T. Reinhard
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
Andy Ridgwell
Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA
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Cited
15 citations as recorded by crossref.
- Inclusion of a suite of weathering tracers in the cGENIE Earth system model – muffin release v.0.9.23 M. Adloff et al. 10.5194/gmd-14-4187-2021
- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al. 10.1038/s41586-022-05018-z
- Nonlinear and Nonmonotonic Effect of Ocean Tidal Mixing on Exoplanet Climates and Habitability M. Di Paolo et al. 10.3847/2041-8213/adbca3
- Stabilising millennial oscillations in large-scale ocean circulation with a delayed feedback due to a circumpolar current A. Keane et al. 10.1016/j.physd.2025.134680
- The History of Ocean Oxygenation C. Reinhard & N. Planavsky 10.1146/annurev-marine-031721-104005
- CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al. 10.5194/gmd-15-7593-2022
- ForamEcoGEnIE 2.0: incorporating symbiosis and spine traits into a trait-based global planktic foraminiferal model R. Ying et al. 10.5194/gmd-16-813-2023
- Bioturbation and the δ56Fe signature of dissolved iron fluxes from marine sediments S. van de Velde et al. 10.1098/rsos.220010
- The response and ecological implications between various sulfur forms and environmental factors in acid mine drainage M. Gao et al. 10.1016/j.envres.2025.121425
- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al. 10.5194/gmd-17-1729-2024
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al. 10.1038/s41598-024-67391-1
- Impacts of bioturbation on iron biogeochemistry and microbial communities in coastal sediment mesocosms under varying degrees of hypoxia J. Beam et al. 10.1016/j.ecss.2022.108032
- Hydrothermal vent fluid-seawater mixing and the origins of Archean iron formation N. Tosca & B. Tutolo 10.1016/j.gca.2023.05.002
- Modeling the impact of explosive volcanism on biogeochemical cycling at the peak of the Late Paleozoic icehouse L. Pfeifer et al. 10.1016/j.gloplacha.2025.104801
- Microbes in mass extinction: an accomplice or a savior? G. Luo et al. 10.1093/nsr/nwad291
15 citations as recorded by crossref.
- Inclusion of a suite of weathering tracers in the cGENIE Earth system model – muffin release v.0.9.23 M. Adloff et al. 10.5194/gmd-14-4187-2021
- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al. 10.1038/s41586-022-05018-z
- Nonlinear and Nonmonotonic Effect of Ocean Tidal Mixing on Exoplanet Climates and Habitability M. Di Paolo et al. 10.3847/2041-8213/adbca3
- Stabilising millennial oscillations in large-scale ocean circulation with a delayed feedback due to a circumpolar current A. Keane et al. 10.1016/j.physd.2025.134680
- The History of Ocean Oxygenation C. Reinhard & N. Planavsky 10.1146/annurev-marine-031721-104005
- CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al. 10.5194/gmd-15-7593-2022
- ForamEcoGEnIE 2.0: incorporating symbiosis and spine traits into a trait-based global planktic foraminiferal model R. Ying et al. 10.5194/gmd-16-813-2023
- Bioturbation and the δ56Fe signature of dissolved iron fluxes from marine sediments S. van de Velde et al. 10.1098/rsos.220010
- The response and ecological implications between various sulfur forms and environmental factors in acid mine drainage M. Gao et al. 10.1016/j.envres.2025.121425
- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al. 10.5194/gmd-17-1729-2024
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al. 10.1038/s41598-024-67391-1
- Impacts of bioturbation on iron biogeochemistry and microbial communities in coastal sediment mesocosms under varying degrees of hypoxia J. Beam et al. 10.1016/j.ecss.2022.108032
- Hydrothermal vent fluid-seawater mixing and the origins of Archean iron formation N. Tosca & B. Tutolo 10.1016/j.gca.2023.05.002
- Modeling the impact of explosive volcanism on biogeochemical cycling at the peak of the Late Paleozoic icehouse L. Pfeifer et al. 10.1016/j.gloplacha.2025.104801
- Microbes in mass extinction: an accomplice or a savior? G. Luo et al. 10.1093/nsr/nwad291
Latest update: 30 May 2025
Short summary
Biogeochemical interactions between iron and sulfur are central to the long-term biogeochemical evolution of Earth’s oceans. Here, we introduce an iron–sulphur cycle in a model of Earth's oceans. Our analyses show that the results of the model are robust towards parameter choices and that simulated concentrations and reactions are comparable to those observed in ancient ocean analogues (anoxic lakes). Our model represents an important step forward in the study of iron–sulfur cycling.
Biogeochemical interactions between iron and sulfur are central to the long-term biogeochemical...
