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Sources and sinks of CO 2 and CH 4 in siliciclastic subterranean estuaries
Author(s) -
Pain Andrea J.,
Martin Jonathan B.,
Young Caitlin R.
Publication year - 2019
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.1002/lno.11131
Subject(s) - siliciclastic , alkalinity , methanogenesis , carbonate , environmental chemistry , methane , carbon dioxide , estuary , sulfate , halite , chemistry , environmental science , geology , oceanography , gypsum , geomorphology , facies , paleontology , structural basin , organic chemistry
Anthropogenic production of greenhouse gases (GHGs) has intensified the need to constrain estimates of natural atmospheric sources from both terrestrial and marine systems. Estuaries are known sources of carbon dioxide (CO 2 ) and methane (CH 4 ); however, less is known about GHG dynamics in subterranean estuaries (STEs). We evaluate CO 2 and CH 4 dynamics in three proximal STEs bordering Indian River Lagoon, Florida, where groundwater flows through siliciclastic sediments with minor carbonate mineral contents. Although the three STEs have similar mineralogical and flow characteristics, CO 2 and CH 4 concentrations vary by orders of magnitude. Nonconservative mixing of both gases is observed, and CH 4 is generally produced while CO 2 is sequestered. The extent of methanogenesis is linked to the redox potential of inflowing groundwaters, as well as degree of CH 4 oxidation, which results mostly from anaerobic oxidation of methane. Methane concentrations vary by orders of magnitude, and stable isotopic signatures suggest differences in the microbial production pathway between sites. CO 2 is sequestered due to the production of alkalinity relative to dissolved inorganic carbon, which occurs both through rapid CaCO 3 dissolution at the shoreline as low‐pH groundwater from the siliciclastic aquifer interacts with carbonate minerals in lagoon sediments, as well as redox reactions, particularly sulfate reduction and denitrification. These results demonstrate a high variability in CO 2 and CH 4 concentrations, and thus fluxes, even among geographically constrained and hydrogeologically similar STEs. Although STEs are sources of both CO 2 and CH 4 to surface waters, the variability of production and consumption complicates global estimates of GHG fluxes from STEs.