Hydrologic Controls of Methane Dynamics in Karst Subterranean Estuaries

• Published in: Global biogeochemical cycles 2018-12, Vol.32 (12), p.1759-1775
• Main Authors: Brankovits, D., Pohlman, J. W., Ganju, N. K., Iliffe, T. M., Lowell, N., Roth, E., Sylva, S. P., Emmert, J. A., Lapham, L. L.
• Format: Article
• Language: English
• Subjects: anchialine ecosystem; Anoxia; Aquifers; Bacteria; Brackish water; Carbon cycle; carbon cycling; Carbonates; Catchment area; Catchment basins; Caves; Chemical reactions; coastal aquifer; Coastal aquifers; Coastal waters; Consumption; Dry season; Dynamics; Ecosystems; Energy sources; Estuaries; Estuarine dynamics; Estuarine ecosystems; Estuarine environments; Food chains; Food webs; Foods; Fresh water; Freshwater environments; Greenhouse effect; Greenhouse gases; hydrobiogeochemistry; Hydrologic regime; Hydrology; Inland water environment; Karst; Marine ecosystems; Mass balance; Meteorology; Meteorology and hydrology; Methane; Methane budget; Microorganisms; Organic chemistry; Oxidation; Rain; Rainfall; Rainy season; Records; Seasonal variations; Seasons; subterranean estuary
• ISSN: 0886-6236; 1944-9224
• DOI: 10.1029/2018GB006026

Karst subterranean estuaries (KSEs) extend into carbonate platforms along 12% of all coastlines. A recent study has shown that microbial methane (CH4) consumption is an important component of the carbon cycle and food web dynamics within flooded caves that permeate KSEs. In this study, we obtained high‐resolution (~2.5‐day) temporal records of dissolved methane concentrations and its stable isotopic content (δ13C) to evaluate how regional meteorology and hydrology control methane dynamics in KSEs. Our records show that less methane was present in the anoxic fresh water during the wet season (4,361 ± 89 nM) than during the dry season (5,949 ± 132 nM), suggesting that the wet season hydrologic regime enhances mixing of methane and other constituents into the underlying brackish water. The δ13C of the methane (−38.1 ± 1.7‰) in the brackish water was consistently more 13C‐enriched than fresh water methane (−65.4 ± 0.4‰), implying persistent methane oxidation in the cave. Using a hydrologically based mass balance model, we calculate that methane consumption in the KSE was 21–28 mg CH4·m−2·year−1 during the 6‐month dry period, which equates to ~1.4 t of methane consumed within the 102‐ to 138‐km2 catchment basin for the cave. Unless wet season methane consumption is much greater, the magnitude of methane oxidized within KSEs is not likely to affect the global methane budget. However, our estimates constrain the contribution of a critical resource for this widely distributed subterranean ecosystem. Plain Language Summary Subterranean estuaries occur worldwide where fresh and marine‐derived waters mix within coastal aquifers, creating a chemical reaction zone that alters the composition of materials transported to the sea. According to a recent study, methane—a potent greenhouse gas—and the bacteria that feed on it form the basis of a complex food web restricted to cave networks flooded by the subterranean estuary. Questions about the seasonality and magnitude of this methane sink remain unclear. Unprecedented chemical records collected during this study with simultaneous meteorological and hydrological data reveal that methane accumulation is significantly greater during the dry season than during the wet season when rainfall is more prevalent and greater mixing in the coastal aquifer facilitates methane consumption. We estimate that ~1.4 t of methane are consumed during a 6‐month‐long dry period within the ~100‐km2 catchment region. This estimate constrains the