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.
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
20 citations as recorded by crossref.
- Instability in the geological regulation of Earth’s climate D. Hülse & A. Ridgwell
- Inclusion of a suite of weathering tracers in the cGENIE Earth system model – muffin release v.0.9.23 M. Adloff et al.
- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al.
- Nonlinear and Nonmonotonic Effect of Ocean Tidal Mixing on Exoplanet Climates and Habitability M. Di Paolo et al.
- GEOCLIM7, an Earth system model for multi-million-year evolution of the geochemical cycles and climate P. Maffre et al.
- Stabilising millennial oscillations in large-scale ocean circulation with a delayed feedback due to a circumpolar current A. Keane et al.
- Editorial preface to special issue: Dynamics of Earth's climate system and biogeochemical cycles in deep time Y. Cui et al.
- The History of Ocean Oxygenation C. Reinhard & N. Planavsky
- NutGEnIE 1.0: nutrient cycle extensions to the cGEnIE Earth system model to examine the long-term influence of nutrients on oceanic primary production D. Stappard et al.
- CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al.
- ForamEcoGEnIE 2.0: incorporating symbiosis and spine traits into a trait-based global planktic foraminiferal model R. Ying et al.
- Bioturbation and the δ56Fe signature of dissolved iron fluxes from marine sediments S. van de Velde et al.
- The response and ecological implications between various sulfur forms and environmental factors in acid mine drainage M. Gao et al.
- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al.
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al.
- Impacts of bioturbation on iron biogeochemistry and microbial communities in coastal sediment mesocosms under varying degrees of hypoxia J. Beam et al.
- Hydrothermal vent fluid-seawater mixing and the origins of Archean iron formation N. Tosca & B. Tutolo
- Modeling the impact of explosive volcanism on biogeochemical cycling at the peak of the Late Paleozoic icehouse L. Pfeifer et al.
- Microbes in mass extinction: an accomplice or a savior? G. Luo et al.
- Microbes that breathe iron and eat sulfur B. Wan & M. Mansor
20 citations as recorded by crossref.
- Instability in the geological regulation of Earth’s climate D. Hülse & A. Ridgwell
- Inclusion of a suite of weathering tracers in the cGENIE Earth system model – muffin release v.0.9.23 M. Adloff et al.
- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al.
- Nonlinear and Nonmonotonic Effect of Ocean Tidal Mixing on Exoplanet Climates and Habitability M. Di Paolo et al.
- GEOCLIM7, an Earth system model for multi-million-year evolution of the geochemical cycles and climate P. Maffre et al.
- Stabilising millennial oscillations in large-scale ocean circulation with a delayed feedback due to a circumpolar current A. Keane et al.
- Editorial preface to special issue: Dynamics of Earth's climate system and biogeochemical cycles in deep time Y. Cui et al.
- The History of Ocean Oxygenation C. Reinhard & N. Planavsky
- NutGEnIE 1.0: nutrient cycle extensions to the cGEnIE Earth system model to examine the long-term influence of nutrients on oceanic primary production D. Stappard et al.
- CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al.
- ForamEcoGEnIE 2.0: incorporating symbiosis and spine traits into a trait-based global planktic foraminiferal model R. Ying et al.
- Bioturbation and the δ56Fe signature of dissolved iron fluxes from marine sediments S. van de Velde et al.
- The response and ecological implications between various sulfur forms and environmental factors in acid mine drainage M. Gao et al.
- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al.
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al.
- Impacts of bioturbation on iron biogeochemistry and microbial communities in coastal sediment mesocosms under varying degrees of hypoxia J. Beam et al.
- Hydrothermal vent fluid-seawater mixing and the origins of Archean iron formation N. Tosca & B. Tutolo
- Modeling the impact of explosive volcanism on biogeochemical cycling at the peak of the Late Paleozoic icehouse L. Pfeifer et al.
- Microbes in mass extinction: an accomplice or a savior? G. Luo et al.
- Microbes that breathe iron and eat sulfur B. Wan & M. Mansor
Saved (final revised paper)
Latest update: 06 May 2026
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...