Spatial and temporal variability in carbon dioxide and methane exchange at three coastal marshes along a salinity gradient in a northern Gulf of Mexico estuary

• Published in: Biogeochemistry 2015-04, Vol.123 (3), p.329-347
• Main Authors: Wilson, Benjamin J, Mortazavi, Behzad, Kiene, Ronald P
• Format: Article
• Language: English
• Subjects: Aquatic ecosystems; biogeochemistry; Biogeosciences; Brackish; carbon; Carbon dioxide; Coastal zone management; Earth and Environmental Science; Earth Sciences; ecosystem respiration; Ecosystems; Environmental Chemistry; Estuaries; freshwater; Gas exchange; Life Sciences; Methane; net ecosystem exchange; Photosynthesis; Pore water; Salinity; Salt marshes; sea level; Sea level rise; sediments; temporal variation; Vegetation cover
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/s10533-015-0085-4

Carbon gas fluxes in tidal marshes vary spatially and temporally because of vegetation cover, subsurface biogeochemical processes, and environmental forcing. The objective of this study was to examine how ecosystem carbon gas exchange changes along an estuarine salinity gradient. We measured carbon dioxide (CO₂) and methane (CH₄) gas fluxes from three marshes representing a salinity gradient (0–32 ppt) in the Mobile Bay estuary, Alabama, USA. CH₄flux was relatively small with no significant differences across sites despite salinity differences. Interestingly, sediment porewater CH₄concentrations were significantly higher at the high salinity salt marsh and decreased with decreasing salinity. Midday net ecosystem exchange (where a positive rate indicates net carbon assimilated through photosynthesis) was greatest at the most fresh site (4.8 ± 0.3 µmol CO₂m⁻² s⁻¹), followed by the saline (2.8 ± 1.0 µmol CO₂m⁻² s⁻¹) and brackish (1.4 ± 0.6 µmol CO₂m⁻² s⁻¹) sites. However, net ecosystem exchange integrated diurnally revealed each marsh to be a net CO₂source to the atmosphere as a result of high ecosystem respiration with the freshwater marsh emitting more CO₂(−893.4 ± 187.9 g C m⁻² year⁻¹) than the brackish (−517.8 ± 85.2 g C m⁻² year⁻¹) and salt marsh (−410.2 ± 98.2 g C m⁻² year⁻¹). This finding leads to the conclusion that either the marshes are losing carbon or that they receive a subsidy of respirable carbon, possibly via tidal deposition. The extent to which sedimentation from tidal deposition contributes carbon to these ecosystems, however, remains unknown. Without such a subsidy, marshes in the study area will not be able to keep up with sea level rise.