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Carbon Gas Fluxes in Re-Established Wetlands on Organic Soils Differ Relative to Plant Community and Hydrology

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Abstract

We measured CO2 and CH4 fluxes for 6 years following permanent flooding of an agriculturally managed organic soil at two water depths (~25 and ~55 cm standing water) in the Sacramento–San Joaquin Delta, California, as part of research studying C dynamics in re-established wetlands. Flooding rapidly reduced gaseous C losses, and radiocarbon data showed that this, in part, was due to reduced oxidation of “old” C preserved in the organic soils. Both CO2 and CH4 emissions from the water surface increased during the first few growing seasons, concomitant with emergent marsh establishment, and thereafter appeared to stabilize according to plant communities. Areas of emergent marsh vegetation in the shallower wetland had greater net CO2 influx (−485 mg C m−1 h−1), and lower CH4 emissions (11.5 mg C m−2 h−1), than in the deeper wetland (−381 and 14.1 mg C m−2 h−1, respectively). Areas with submerged and floating vegetation in the deeper wetland had CH4 emissions similar to emergent vegetation (11.9 and 12.6 mg C m−2 h−1, respectively), despite lower net CO2 influx (−102 g C m−2 h−1). Measurements of plant moderated net CO2 influx and CH4 efflux indicated greatest potential reduction of greenhouse gases in the more shallowly flooded wetland.

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Acknowledgments

We owe great thanks to the California Department of Water Resources for funding this long-term study, and special thanks to Lauren Hastings for her hard work and dedication getting the site established and leading the study in the first years of the project. We also thank Susan Trumbore, Stanley Tyler, and Andrew McMillan for their help with C isotope sampling and analyses. Finally, we thank all the reviewers of this paper, who made some welcome and helpful suggestions.

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  1. United States Geological Survey, California Water Science Center, 6000 J Street, Placer Hall, Sacramento, CA, 95819, USA

    Robin L. Miller

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Correspondence to Robin L. Miller.

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Miller, R.L. Carbon Gas Fluxes in Re-Established Wetlands on Organic Soils Differ Relative to Plant Community and Hydrology. Wetlands 31, 1055–1066 (2011). https://doi.org/10.1007/s13157-011-0215-2

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