Sulfide and thiosulfate-oxidizing bacteria in anoxic marine basins

The occurrence of sulfide and thiosulfate-oxidizing bacteria was examined in waters and sediments of the Black Sea and the Caraco Trench. Isolates obtained by enrichment-culture techniques exhibited facultative autotrophic-growth characteristics and oxidized thiosulfate or sulfide. Acid was not formed during growth in mineral medium. Most of the isolates were facultatively anaerobic, using nitrate as the terminal hydrogen acceptor. Strictly aerobic bacteria were found only in oxygenated waters. Comparison of the metabolic capabilities of the isolates during growth in sulfide and thiosulfate media with chemical parameters measured in the Black Sea and Cariaco Trench waters suggests that the biological oxidation of thiosulfate is the rate-limiting step in the oxidative turnover of sulfur compounds in the basins. Evidence for the oxidation of sulfide in the anoxic waters is presented, and possible explanations for the occurrence of this process in the absence of suitable electron acceptors (O₂. NO₃) are discussed. A maximum dark assimilation of carbon dioxide was located just below the oxygen-sulfide interface in the Cariaco Trench. Problems of interpreting these data are considered.Contribution No. 2958 of the Woods Hole Occanographic Institution. Supported by the National Science Foundation Grants GA 29665 and GA 33405.