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

dc.contributor.author	Schouten S.
dc.contributor.author	Wakeham S.G.
dc.contributor.author	Damste J.S.S.
dc.date.accessioned	2021-03-13T07:01:08Z
dc.date.available	2021-03-13T07:01:08Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=791690
dc.identifier.citation	Organic Geochemistry, 2001, 32, 10, 1277-1281
dc.identifier.issn	0146-6380
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26669
dc.description.abstract	13C-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.subject	ARCHAE
dc.subject	METHANE OXIDATION
dc.subject	BLACK SEA
dc.subject	GAS HYDRATES
dc.subject	CYCLIC BIPHYTANES
dc.title	EVIDENCE FOR ANAEROBIC METHANE OXIDATION BY ARCHAEA IN EUXINIC WATERS OF THE BLACK SEA
dc.type	Статья

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