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- W2155169444 abstract "Organoclastic degradation and anaerobic oxidation of methane (AOM) are known to influence sulfate, methane and bicarbonate concentrations of sediment pore-waters. In this work we have analyzed the pore-fluid composition of three piston cores (36–39 m long) collected from water depths ranging from 1429 to 1691 m. We attribute the observed linear sulfate concentration profiles and (ΔCa + ΔAlk)/ΔSO42− ratios dominantly to anaerobic oxidation of methane (AOM) induced sulfate consumption. The gas rich layers just below the base of hydrate stability zone (BGHSZ) is the possible source of the enhanced diffusive flux of biogenic methane (δ13CCH4 ranging from −99.7 to −106.3‰ VPDB). Occurrences of disseminated gas hydrate in the Mahanadi Basin within the hydrate stability zone (210–220 m thick) supports the link between linear sulfate profile, high rate of AOM and hydrate occurrence." @default.
- W2155169444 created "2016-06-24" @default.
- W2155169444 creator A5033967484 @default.
- W2155169444 creator A5049047995 @default.
- W2155169444 creator A5050338368 @default.
- W2155169444 creator A5069721525 @default.
- W2155169444 creator A5084092241 @default.
- W2155169444 date "2014-01-01" @default.
- W2155169444 modified "2023-10-14" @default.
- W2155169444 title "Pore-water chemistry of sediment cores off Mahanadi Basin, Bay of Bengal: Possible link to deep seated methane hydrate deposit" @default.
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- W2155169444 doi "https://doi.org/10.1016/j.marpetgeo.2013.10.011" @default.