Articles | Volume 16, issue 13
https://doi.org/10.5194/bg-16-2573-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-2573-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Shifting mineral and redox controls on carbon cycling in seasonally flooded mineral soils
Rachelle E. LaCroix
CORRESPONDING AUTHOR
School of Earth & Sustainability and Stockbridge School of
Agriculture, University of Massachusetts, Amherst, MA, USA
Malak M. Tfaily
Soil, Water and Environmental Science Department, University of
Arizona, Tucson, AZ, USA
Menli McCreight
School of Earth & Sustainability and Stockbridge School of
Agriculture, University of Massachusetts, Amherst, MA, USA
Morris E. Jones
School of Earth & Sustainability and Stockbridge School of
Agriculture, University of Massachusetts, Amherst, MA, USA
Lesley Spokas
School of Earth & Sustainability and Stockbridge School of
Agriculture, University of Massachusetts, Amherst, MA, USA
School of Earth & Sustainability and Stockbridge School of
Agriculture, University of Massachusetts, Amherst, MA, USA
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- How does soil water status influence the fate of soil organic matter? A review of processes across scales C. Védère et al. 10.1016/j.earscirev.2022.104214
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- Quantifying mineral-associated organic matter in wetlands as an indicator of the degree of soil carbon protection A. Mirabito & L. Chambers 10.1016/j.geoderma.2023.116327
- Mineral Protection and Resource Limitations Combine to Explain Profile‐Scale Soil Carbon Persistence E. Lacroix et al. 10.1029/2021JG006674
- Water‐Soluble Organic Matter From Soils at the Terrestrial‐Aquatic Interface in Wetland‐Dominated Landscapes K. Wardinski et al. 10.1029/2022JG006994
- Mineralogic Controls are Harbingers of Hydrological Controls on Soil Organic Matter Content in Warmer Boreal Forests M. Patrick et al. 10.2139/ssrn.4072453
- Salinity increases under sea level rise strengthens the chemical protection of SOC in subtropical tidal marshes H. Xu et al. 10.1016/j.scitotenv.2024.176512
- Trade‐offs in soil carbon protection mechanisms under aerobic and anaerobic conditions W. Huang et al. 10.1111/gcb.15100
- Espacialização dos atributos do solo e suscetibilidade magnética em ambiente de inundação sazonal no Nordeste do Brasil H. De Oliveira Monteiro et al. 10.26848/rbgf.v17.4.p2795-2807
- Molecular Nature of Mineral-Organic Associations within Redox-Active Mountainous Floodplain Sediments C. Anderson et al. 10.1021/acsearthspacechem.3c00037
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- Ecosystem-specific patterns and drivers of global reactive iron mineral-associated organic carbon B. Zhao et al. 10.5194/bg-20-4761-2023
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- Theoretical Constraints on Fe Reduction Rates in Upland Soils as a Function of Hydroclimatic Conditions S. Calabrese et al. 10.1029/2020JG005894
- Spatiotemporal dynamics in soil iron affected by wetland conversion on the Sanjiang Plain G. Chi et al. 10.1002/ldr.4069
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Latest update: 26 Dec 2024
Short summary
Organic carbon (C) stocks within seasonal wetlands are vulnerable to increased severity and duration of droughts in response to climate change. Here we examined the mechanistic controls on C cycling in seasonally flooded mineral wetland soils. We found that different mechanisms preserve C in surface layers (oxygen limitations) compared to subsurface layers (mineral protection and lack of root C inputs).
Organic carbon (C) stocks within seasonal wetlands are vulnerable to increased severity and...
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