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dc.contributor.author Xu L.
dc.contributor.author Reddy C.M.
dc.contributor.author Farrington J.W.
dc.contributor.author Frysinger G.S.
dc.contributor.author Gaines R.B.
dc.contributor.author Johnson C.G.
dc.contributor.author Nelson R.K.
dc.contributor.author Eglinton T.I.
dc.date.accessioned 2021-02-12T05:10:11Z
dc.date.available 2021-02-12T05:10:11Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=604118
dc.identifier.citation Organic Geochemistry, 2001, 32, 5, 633-645
dc.identifier.issn 0146-6380
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/24798
dc.description.abstract We report the identification of a novel long-chain ketone in Holocene Black Sea sediments. Based on chemical properties, and chromatographic and mass spectrometric characteristics, this compound has been identified as a di-unsaturated C36 ethyl ketone. Further analyses indicated the position and configuration of the double bonds, and the novel alkenone was determined to be hexatriaconta-(16E,21E)-dien-3-one. While this compound is present in only trace quantities in Unit I sediments, it is the most abundant alkenone in portions of Unit II. Its presence thus apparently pre-dates the invasion of Emiliania huxleyi in the Black Sea. The down-core profiles and isotopic compositions suggest that the precursor for the C36:2 alkenone may be distinct from that of the C37-39 alkenones, however the biological origin of this novel compound is presently unknown.
dc.subject ALKENONE
dc.subject STRUCTURE CHARACTERIZATION
dc.subject SEDIMENT
dc.subject BLACK SEA
dc.subject HOLOCENE
dc.subject HAPTOPHYTES
dc.title IDENTIFICATION OF A NOVEL ALKENONE IN BLACK SEA SEDIMENTS
dc.type Статья
dc.subject.age Cenozoic::Quaternary::Holocene en
dc.subject.age Кайнозой::Четвертичная::Голоцен ru


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