Oxidation rate of thiosulfate and elemental sulfur in the Black Sea

DOI

Oxidation rate of 35S-thiosulfate under simulated natural conditions and abundance of thiosulfate-oxidizing bacteria in a redox zone of the Black Sea are lower during winter and spring than in summer, especially in halistatic regions. Oxidation of thiosulfate under natural conditions is performed chiefly by lithotropic thionic bacteria, whose activity is limited by low temperatures. Adding thiosulfate and readily available organic matter to water samples from the redox zone and raising temperature of water stimulated activity of heterotrophic thiosulfate-oxidizing bacteria. Oxidation of elemental sulfur tagged with 35S apparently invovled two stages: abiotic oxidation of thiosulfate and subsequent bacterial oxidation of thiosulfate to sulfate.

Supplement to: Sorokin, Yury I (1992): Oxidation of thiosulfate and molecular sulfur in the redox zone of the Black Sea in winter and spring. Oceanology, 32(5), 600-605

Identifier
DOI https://doi.org/10.1594/PANGAEA.759302
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.759302
Provenance
Creator Sorokin, Yury I
Publisher PANGAEA
Publication Year 1992
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (30.889W, 41.805S, 41.032E, 44.497N); Black Sea
Temporal Coverage Begin 1991-02-11T00:00:00Z
Temporal Coverage End 1991-04-02T00:00:00Z