Articles | Volume 11, issue 7
https://doi.org/10.5194/gmd-11-2649-2018
© Author(s) 2018. 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-11-2649-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
OMEN-SED 1.0: a novel, numerically efficient organic matter sediment diagenesis module for coupling to Earth system models
BRIDGE, School of Geographical Sciences, University of Bristol, Clifton, Bristol BS8 1SS, UK
Department of Earth Sciences, University of California, Riverside, CA 92521, USA
Sandra Arndt
BRIDGE, School of Geographical Sciences, University of Bristol, Clifton, Bristol BS8 1SS, UK
BGeosys, Department Geoscience, Environment & Society (DGES), Université Libre de Bruxelles, Brussels, Belgium
Stuart Daines
Earth System Science, University of Exeter, North Park Road, Exeter EX4 4QE, UK
Pierre Regnier
BGeosys, Department Geoscience, Environment & Society (DGES), Université Libre de Bruxelles, Brussels, Belgium
Andy Ridgwell
BRIDGE, School of Geographical Sciences, University of Bristol, Clifton, Bristol BS8 1SS, UK
Department of Earth Sciences, University of California, Riverside, CA 92521, USA
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Cited
15 citations as recorded by crossref.
- End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia D. Hülse et al. 10.1038/s41561-021-00829-7
- Model of Early Diagenesis in the Upper Sediment with Adaptable complexity – MEDUSA (v. 2): a time-dependent biogeochemical sediment module for Earth system models, process analysis and teaching G. Munhoven 10.5194/gmd-14-3603-2021
- What global biogeochemical consequences will marine animal–sediment interactions have during climate change? T. Bianchi et al. 10.1525/elementa.2020.00180
- A model for marine sedimentary carbonate diagenesis and paleoclimate proxy signal tracking: IMP v1.0 Y. Kanzaki et al. 10.5194/gmd-14-5999-2021
- Quantifying Importance of Macrobenthos for Benthic‐Pelagic Coupling in a Temperate Coastal Shelf Sea W. Zhang et al. 10.1029/2020JC016995
- Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21) S. van de Velde et al. 10.5194/gmd-14-2713-2021
- Trickle and Treat? The Critical Role of Marine‐Terminating Glaciers as Icy Macronutrient Pumps in Polar Regions J. Hawkings 10.1029/2021JG006598
- OMEN-SED(-RCM) (v1.1): a pseudo-reactive continuum representation of organic matter degradation dynamics for OMEN-SED P. Pika et al. 10.5194/gmd-14-7155-2021
- Microbial Controls on the Biogeochemical Dynamics in the Subsurface M. Thullner & P. Regnier 10.2138/rmg.2019.85.9
- Mitigation of Extreme Ocean Anoxic Event Conditions by Organic Matter Sulfurization D. Hülse et al. 10.1029/2018PA003470
- RADIv1: a non-steady-state early diagenetic model for ocean sediments in Julia and MATLAB/GNU Octave O. Sulpis et al. 10.5194/gmd-15-2105-2022
- The fate of organic carbon in marine sediments - New insights from recent data and analysis D. LaRowe et al. 10.1016/j.earscirev.2020.103146
- New insights into large-scale trends of apparent organic matter reactivity in marine sediments and patterns of benthic carbon transformation F. Freitas et al. 10.5194/bg-18-4651-2021
- Widespread energy limitation to life in global subseafloor sediments J. Bradley et al. 10.1126/sciadv.aba0697
- Are seep carbonates quantitative proxies of CH4 leakage? Modeling the influence of sulfate reduction and anaerobic oxidation of methane on pH and carbonate precipitation J. Blouet et al. 10.1016/j.chemgeo.2021.120254
15 citations as recorded by crossref.
- End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia D. Hülse et al. 10.1038/s41561-021-00829-7
- Model of Early Diagenesis in the Upper Sediment with Adaptable complexity – MEDUSA (v. 2): a time-dependent biogeochemical sediment module for Earth system models, process analysis and teaching G. Munhoven 10.5194/gmd-14-3603-2021
- What global biogeochemical consequences will marine animal–sediment interactions have during climate change? T. Bianchi et al. 10.1525/elementa.2020.00180
- A model for marine sedimentary carbonate diagenesis and paleoclimate proxy signal tracking: IMP v1.0 Y. Kanzaki et al. 10.5194/gmd-14-5999-2021
- Quantifying Importance of Macrobenthos for Benthic‐Pelagic Coupling in a Temperate Coastal Shelf Sea W. Zhang et al. 10.1029/2020JC016995
- Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21) S. van de Velde et al. 10.5194/gmd-14-2713-2021
- Trickle and Treat? The Critical Role of Marine‐Terminating Glaciers as Icy Macronutrient Pumps in Polar Regions J. Hawkings 10.1029/2021JG006598
- OMEN-SED(-RCM) (v1.1): a pseudo-reactive continuum representation of organic matter degradation dynamics for OMEN-SED P. Pika et al. 10.5194/gmd-14-7155-2021
- Microbial Controls on the Biogeochemical Dynamics in the Subsurface M. Thullner & P. Regnier 10.2138/rmg.2019.85.9
- Mitigation of Extreme Ocean Anoxic Event Conditions by Organic Matter Sulfurization D. Hülse et al. 10.1029/2018PA003470
- RADIv1: a non-steady-state early diagenetic model for ocean sediments in Julia and MATLAB/GNU Octave O. Sulpis et al. 10.5194/gmd-15-2105-2022
- The fate of organic carbon in marine sediments - New insights from recent data and analysis D. LaRowe et al. 10.1016/j.earscirev.2020.103146
- New insights into large-scale trends of apparent organic matter reactivity in marine sediments and patterns of benthic carbon transformation F. Freitas et al. 10.5194/bg-18-4651-2021
- Widespread energy limitation to life in global subseafloor sediments J. Bradley et al. 10.1126/sciadv.aba0697
- Are seep carbonates quantitative proxies of CH4 leakage? Modeling the influence of sulfate reduction and anaerobic oxidation of methane on pH and carbonate precipitation J. Blouet et al. 10.1016/j.chemgeo.2021.120254
Latest update: 03 Jun 2023
Short summary
We present a 1-D analytical diagenetic model resolving organic matter (OM) cycling and the associated biogeochemical dynamics in marine sediments designed to be coupled to Earth system models (ESMs). The reaction network accounts for the most important reactions associated with OM dynamics. The coupling is described and the OM degradation rate constant is tuned. Various observations, such as pore water profiles, sediment water interface fluxes and OM content, are reproduced with good accuracy.
We present a 1-D analytical diagenetic model resolving organic matter (OM) cycling and the...