Methane fluxes in tidal marshes of the conterminous United States

Global Change Biology
By: , and 

Metrics

Cited by publications in Crossref
Web analytics dashboard Metrics definitions

Links

Abstract

Methane (CH4) 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 CH4 emissions, yet the magnitude and factors controlling CH4 fluxes in tidal wetlands remain uncertain. We synthesized CH4 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 CH4 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 CH4 m−2 year−1, with a median of 3.9 g CH4 m−2 year−1, and only 25% of sites exceeding 18 g CH4 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 CH4 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 CH4 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 CH4 flux changes, while the opposite was observed at the seasonal scale. Water levels influenced the timing and pathway of diel CH4 fluxes, with pulsed releases of stored CH4 at low to rising tide. This study provides data and methods to improve tidal marsh CH4 emission estimates, support blue carbon assessments, and refine national and global GHG inventories.

Suggested Citation

Arias-Ortiz, A., Wolfe, J., Bridgham, S.D., Knox, S., McNicol, G., Needelman, B.A., Shahan, J., Stuart-Haëntjens, E.J., Windham-Myers, L., Oikawa, P., Baldocchi, D.D., Caplan, J.S., Capooci, M., Czapla, K.M., Derby, R.K., Diefenderfer, H.L., Forbrich, I., Groseclose, G., Keller, J., Kelley, C., Keshta, A.E., Kleiner, H.S., Krauss, K., Lane, R.R., Mack, S., Moseman-Valtierra, S., Mozdzer, T., Mueller, P., Neubauer, S.C., Noyce, G., Schäfer, K.V., Sanders-DeMott, R., Schutte, C.A., Vargas, R., Weston, N.B., Wilson, B., Megonigal, J.P., and Holmquist, J.R., 2024, Methane fluxes in tidal marshes of the conterminous United States: Global Change Biology, v. 30, no. 9, e17462, 23 p., https://doi.org/10.1111/gcb.17462.

Study Area

Publication type Article
Publication Subtype Journal Article
Title Methane fluxes in tidal marshes of the conterminous United States
Series title Global Change Biology
DOI 10.1111/gcb.17462
Volume 30
Issue 9
Publication Date September 05, 2024
Year Published 2024
Language English
Publisher Wiley
Contributing office(s) Southwest Regional Director's Office
Description e17462, 23 p.
Country United States
Other Geospatial conterminous United States
Additional publication details