IDENTIFICATION OF A NOVEL ALKENONE IN BLACK SEA SEDIMENTS
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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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