Interactive effects of salinity, redox, and colloids on greenhouse gas production and carbon mobility in coastal wetland soils

PLoS One. 2024 Dec 30;19(12):e0316341. doi: 10.1371/journal.pone.0316341. eCollection 2024.

Abstract

Coastal wetlands, including freshwater systems near large lakes, rapidly bury carbon, but less is known about how they transport carbon either to marine and lake environments or to the atmosphere as greenhouse gases (GHGs) such as carbon dioxide and methane. This study examines how GHG production and organic matter (OM) mobility in coastal wetland soils vary with the availability of oxygen and other terminal electron acceptors. We also evaluated how OM and redox-sensitive species varied across different size fractions: particulates (0.45-1μm), fine colloids (0.1-0.45μm), and nano particulates plus truly soluble (<0.1μm; NP+S) during 21-day aerobic and anaerobic slurry incubations. Soils were collected from the center of a freshwater coastal wetland (FW-C) in Lake Erie, the upland-wetland edge of the same wetland (FW-E), and the center of a saline coastal wetland (SW-C) in the Pacific Northwest, USA. Anaerobic methane production for FW-E soils were 47 and 27,537 times greater than FW-C and SW-C soils, respectively. High Fe2+ and dissolved sulfate concentrations in FW-C and SW-C soils suggest that iron and/or sulfate reduction inhibited methanogenesis. Aerobic CO2 production was highest for both freshwater soils, which had a higher proportion of OM in the NP+S fraction (64±28% and 70±10% for FW-C and FW-E, respectively) and organic C:N ratios reflective of microbial detritus (5.3±5.3 and 5.3±7.0 for FW-E and FW-C, respectively) compared to SW-C, which had a higher fraction of particulate (58±9%) and fine colloidal (19±7%) OM and organic C:N ratios reflective of vegetation detritus (11.4 ± 1.7). The variability in GHG production and shifts in OM size fractionation and composition observed across freshwater and saline soils collected within individual and across different sites reinforce the high spatial variability in the processes controlling OM stability, mobility, and bioavailability in coastal wetland soils.

MeSH terms

  • Carbon Dioxide / metabolism
  • Carbon* / analysis
  • Carbon* / metabolism
  • Colloids*
  • Greenhouse Gases* / analysis
  • Greenhouse Gases* / metabolism
  • Methane* / metabolism
  • Oxidation-Reduction*
  • Salinity*
  • Soil* / chemistry
  • Wetlands*

Substances

  • Soil
  • Greenhouse Gases
  • Carbon
  • Colloids
  • Methane
  • Carbon Dioxide

Grants and funding

This research was performed on project award 60097 from the Environmental Molecular Sciences Laboratory, a DOE Office of Science User Facility sponsored by the Biological and Environmental Research program under Contract No. DE-AC05-76RL01830. The samples used for this study were collected at field sites stewarded by COMPASS-FME, a multi-institutional project supported by DOE-BER as part of the Environmental System Science Program. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.