{"refrec":{"BRefID":38465,"RR":"<b>Lein, A.; Pimenov, N.; Guillou, C.; Martin, J.-M.; Lancelot, C.; Rusanov, I.; Yusupov, S.; Miller, Y.; Ivanov, M.</b> (2002). Seasonal dynamics of the sulphate reduction rate on the north-western Black Sea shelf. <i>Est., Coast. and Shelf Sci. 54(3)</i>: 385-401. <a href=\"https://dx.doi.org/10.1006/ecss.2000.0654\" target=\"_blank\">https://dx.doi.org/10.1006/ecss.2000.0654</a>","BEntID":38465,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Est., Coast. and Shelf Sci. 54(3)</i>: 385-401. <a href=\"https://dx.doi.org/10.1006/ecss.2000.0654\" target=\"_blank\">https://dx.doi.org/10.1006/ecss.2000.0654</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lein, A.; Pimenov, N.; Guillou, C.; Martin, J.-M.; Lancelot, C.; Rusanov, I.; Yusupov, S.; Miller, Y.; Ivanov, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lein, A. <i>et al.</i>","Englishabstract":"The microbial sulphate reduction rate (SRR) in the surface layer (0-30 cm) of shallow water sediments of the north-western Black Sea shelf has been measured using the <sup>35</sup>S radioisotopic technique. It was shown that SRR is accompanied by changes of salt composition of porewaters and isotopic (d<sup>34</sup>S) composition of sulphate. The hydrogen sulphide-derived minerals are formed in the solid phase of sediments. An expected exponential dependence of the isotopic composition of reduced sulphur compounds on the SRR was observed. In near-shore sediments, terrestrial organic carbon (d<sup>13</sup>C = - 26) as well as marine phytoplankton organic carbon (d<sup>13</sup>C = - 22) are associated with the SR processes. In August 1995 and May 1997-1998, anoxic conditions in near-bottom waters of coastal areas were not detected. The average value of H<sub>2</sub>S production in nearshore sediments varied from 3·62 mmol S m<sup>-2</sup> day<sup>-1</sup> in spring to 8·89 mmol S m<sup>-2</sup> day<sup>-1</sup> in summer 1995; these fluxes were twice as high as those measured in spring 1997 and 1998.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Seasonal dynamics of the sulphate reduction rate on the north-western Black Sea shelf","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-23 01:31:50.876729","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"sulphate reduction; sulphur isotopes; carbon isotopes; sediments; Black Sea","OtherDescriptors":null,"Notes":null,"AnaPub":2002,"MonPub":null,"DateUpdate":"2021-02-23","DateCreate":"2003-08-19","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000176333400008","VABBcode":null,"OpenAcc":0,"DOI":"10.1006/ecss.2000.0654"},"refs":null,"anarec":{"AnaID":38465,"PubliDate":2002,"Pagination":"385-401","XtraPublOfAnaID":null,"ISBN":null,"Volume":"54","Issue":"3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":44109,"SerRR":"Estuarine, Coastal and Shelf Science. 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