Articles | Volume 14, issue 5
Geosci. Model Dev., 14, 2713–2745, 2021
https://doi.org/10.5194/gmd-14-2713-2021
Geosci. Model Dev., 14, 2713–2745, 2021
https://doi.org/10.5194/gmd-14-2713-2021
Model description paper
18 May 2021
Model description paper | 18 May 2021

Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21)

Sebastiaan J. van de Velde et al.

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Cited articles

Adloff, M., Ridgwell, A., Monteiro, F. M., Parkinson, I. J., Dickson, A., Pogge von Strandmann, P. A. E., Fantle, M. S., and Greene, S. E.: Inclusion of a suite of weathering tracers in the cGENIE Earth System Model – muffin release v.0.9.10, Geosci. Model Dev. Discuss. [preprint], https://doi.org/10.5194/gmd-2020-233, in review, 2020. a, b
Alcott, L. J., Mills, B. J. W., and Poulton, S. W.: Stepwise Earth oxygenation is an inherent property of global biogeochemical cycling, Science, 366, 1333–1337, https://doi.org/10.1126/science.aax6459, 2019. a
Balistrieri, L. S., Murray, J. W., and Paul, B.: The cycling of iron and manganese in the water column of Lake Sammamish, Washington, Limnol. Oceanogr., 37, 510–528, 1992. a
Balzano, S., Statham, P. J., Pancost, R. D., and Lloyd, J. R.: Role of microbial populations in the release of reduced iron to the water column from marine aggregates, Aquat. Microb. Ecol., 54, 291–303, https://doi.org/10.3354/ame01278, 2009. a, b
Beam, J. P., Scott, J. J., McAllister, S. M., Chan, C. S., McManus, J., Meysman, F. J. R., and Emerson, D.: Biological rejuvenation of iron oxides in bioturbated marine sediments, ISME J., 12, 1389–1394, https://doi.org/10.1038/s41396-017-0032-6, 2018. a
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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.