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Eastern Mediterranean Sea cold seep sediments provide pore-water and solid-phase data for modeling methane fluxes and anaerobic oxidation rates. The model constrains methane concentration and oxidation within a narrow 14-18 cm depth interval below the sediment-water interface. This dataset supports isotopic mass balance calculations indicating microbial biomass from methane oxidation constitutes about 20% of total organic carbon.
Primary data format is HTML, likely a published journal article or report, not a structured data file; license is not specified.