Methane fluxes in tidal marshes of the conterminous United States
- Physics Department Universitat Autònoma de Barcelona Barcelona Spain, Ecosystem Science Division, Department of Environmental Science, Policy and Management University of California Berkeley California USA
- Smithsonian Environmental Research Center Edgewater Maryland USA
- Institute of Ecology and Evolution University of Oregon Eugene Oregon USA
- Department of Geography The University of British Columbia Vancouver British Columbia Canada, Department of Geography McGill University Montreal Quebec Canada
- Department of Earth and Environmental Sciences University of Illinois Chicago Chicago Illinois USA
- Department of Environmental Science and Technology University of Maryland College Park Maryland USA
- Earth System Science Stanford University Stanford California USA
- U.S. Geological Survey Water Resources Mission Area Menlo Park California USA
- Department of Earth and Environmental Sciences California State University East Bay, Hayward California USA
- Ecosystem Science Division, Department of Environmental Science, Policy and Management University of California Berkeley California USA
- Department of Architecture &, Environmental Design Temple University Ambler Pennsylvania USA
- Department of Plant &, Soil Sciences University of Delaware Newark Delaware USA
- Department of Environmental Sciences University of California Riverside Riverside California USA
- Maryland Department of Natural Resources Chesapeake Bay National Estuarine Research Reserve Annapolis Maryland USA
- Coastal Sciences Division Pacific Northwest National Laboratory Sequim Washington USA
- Ecosystems Center Marine Biological Laboratory Woods Hole Massachusetts USA, Department of Environmental Sciences University of Toledo Toledo Ohio USA
- Department of Oceanography and Coastal Sciences Louisiana State University Baton Rouge Louisiana USA
- Schmid College of Science and Technology Chapman University Orange California USA, Kravis Department of Integrated Sciences Claremont McKenna College Claremont California USA
- Department of Geological Sciences University of Missouri Columbia Missouri USA
- Botany Department, Faculty of Science Tanta University Tanta Egypt, Department of Environmental Science and Technology University of Maryland College Park Maryland USA
- U.S. Geological Survey Wetland and Aquatic Research Center Lafayette Louisiana USA
- Comite Resources Baton Rouge Louisiana USA
- Tierra Resources LLC Lafitte Louisiana USA
- Department of Biological Sciences University of Rhode Island Kingston Rhode Island USA
- Bryn Mawr College, Department of Biology Bryn Mawr Pennsylvania USA
- Institute of Landscape Ecology University of Münster Münster Germany
- Department of Biology Virginia Commonwealth University Richmond Virginia USA
- Earth and Environmental Science Dept Rutgers University Newark Newark New Jersey USA
- U.S. Geological Survey Woods Hole Coastal and Marine Science Center Woods Hole Massachusetts USA
- Department of Environmental Science Rowan University Glassboro New Jersey USA
- Department of Geography and the Environment Villanova University Villanova Pennsylvania USA
- Department of Biological Sciences Florida International University Miami Florida USA
Abstract
Methane (CH 4 ) is a potent greenhouse gas (GHG) with atmospheric concentrations that have nearly tripled since pre‐industrial times. Wetlands account for a large share of global CH 4 emissions, yet the magnitude and factors controlling CH 4 fluxes in tidal wetlands remain uncertain. We synthesized CH 4 flux data from 100 chamber and 9 eddy covariance (EC) sites across tidal marshes in the conterminous United States to assess controlling factors and improve predictions of CH 4 emissions. This effort included creating an open‐source database of chamber‐based GHG fluxes ( https://doi.org/10.25573/serc.14227085 ). Annual fluxes across chamber and EC sites averaged 26 ± 53 g CH 4 m −2 year −1 , with a median of 3.9 g CH 4 m −2 year −1 , and only 25% of sites exceeding 18 g CH 4 m −2 year −1 . The highest fluxes were observed at fresh‐oligohaline sites with daily maximum temperature normals (MATmax) above 25.6°C. These were followed by frequently inundated low and mid‐fresh‐oligohaline marshes with MATmax ≤25.6°C, and mesohaline sites with MATmax >19°C. Quantile regressions of paired chamber CH 4 flux and porewater biogeochemistry revealed that the 90th percentile of fluxes fell below 5 ± 3 nmol m −2 s −1 at sulfate concentrations >4.7 ± 0.6 mM, porewater salinity >21 ± 2 psu, or surface water salinity >15 ± 3 psu. Across sites, salinity was the dominant predictor of annual CH 4 fluxes, while within sites, temperature, gross primary productivity (GPP), and tidal height controlled variability at diel and seasonal scales. At the diel scale, GPP preceded temperature in importance for predicting CH 4 flux changes, while the opposite was observed at the seasonal scale. Water levels influenced the timing and pathway of diel CH 4 fluxes, with pulsed releases of stored CH 4 at low to rising tide. This study provides data and methods to improve tidal marsh CH 4 emission estimates, support blue carbon assessments, and refine national and global GHG inventories.
- Sponsoring Organization:
- USDOE
- Grant/Contract Number:
- AC05-76RL01830
- OSTI ID:
- 2439804
- Alternate ID(s):
- OSTI ID: 2484334
- Journal Information:
- Global Change Biology, Journal Name: Global Change Biology Journal Issue: 9 Vol. 30; ISSN 1354-1013
- Publisher:
- Wiley-BlackwellCopyright Statement
- Country of Publication:
- United Kingdom
- Language:
- English
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