EVIDENCE FOR ANAEROBIC METHANE OXIDATION BY ARCHAEA IN EUXINIC WATERS OF THE BLACK SEA

dc.contributor.authorSchouten S.
dc.contributor.authorWakeham S.G.
dc.contributor.authorDamste J.S.S.
dc.date.accessioned2021-03-13T07:01:08Z
dc.date.available2021-03-13T07:01:08Z
dc.date.issued2001
dc.description.abstract13C-depleted archaeal-derived ether-bound cyclic biphytanes occur in particulate organic matter from the euxinic waters of the Black Sea. These strongly 13C-depleted biomarkers (up to -58%%) provide evidence that archaea are consuming methane in euxinic waters. 13C-depleted archaeal compounds were absent from surface sediments, suggesting that the responsible organisms are in low abundance and leave no characteristic fingerprint in the sedimentary record.
dc.identifierhttps://www.elibrary.ru/item.asp?id=791690
dc.identifier.citationOrganic Geochemistry, 2001, 32, 10, 1277-1281
dc.identifier.issn0146-6380
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26669
dc.subjectARCHAE
dc.subjectMETHANE OXIDATION
dc.subjectBLACK SEA
dc.subjectGAS HYDRATES
dc.subjectCYCLIC BIPHYTANES
dc.titleEVIDENCE FOR ANAEROBIC METHANE OXIDATION BY ARCHAEA IN EUXINIC WATERS OF THE BLACK SEA
dc.typeСтатья

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