(Table 3) Rates of hydrogen sulfide formation due to bacterial sulfate reduction in the water mass of the lower portion of the pycnocline layer at different stations in the Black Sea in February-April 1991

DOI
Identifier
DOI https://doi.org/10.1594/PANGAEA.786995
Related Identifier https://doi.org/10.1594/PANGAEA.786996
Related Identifier https://doi.org/10.1134/S0001437011060166
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.786995
Provenance
Creator Sorokin, Yury I
Publisher PANGAEA
Contributor P.P. Shirshov Institute of Oceanology, Southern Branch
Publication Year 2011
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 16 data points
Discipline Earth System Research
Spatial Coverage (31.240W, 43.210S, 32.120E, 45.660N); Black Sea