ISOTOPIC COMPOSITION OF BIOGENIC CARBONATES AND HOLOCENE PALEOGEOGRAPHIC RECONSTRUCTIONS OF THE WESTERN CASPIAN SEASHORE

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dc.contributor.author Vonhof H.
dc.contributor.author Kasatenkova M.S.
dc.contributor.author Kasimov N.S.
dc.contributor.author Lychagin M.Yu.
dc.contributor.author Slobodyan V.Yu.
dc.contributor.author Kroonenberg S.B.
dc.date.accessioned 2022-07-18T05:29:15Z
dc.date.available 2022-07-18T05:29:15Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13451885
dc.identifier.citation Doklady Earth Sciences, 2004, 394, 1, 145-147
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38242
dc.description.abstract Paleo-reconstruction of one new-Caspian transgression stage was carried out on the base of analysis of oxygen and carbon stable isotopes' content as well as of some metals in bivalve mollusk shells. Dynamics of δ18C values in mollusk shells upon their growth provides information on the temperature conditions and salinity of paleo-basins. The δ13C value characterizes intensity of organic substance accumulation in seawater. Cyclic changes of Sr and Ba concentration in mollusk shells imply the possibility of using these elements as indicators of basin paleoconditions.
dc.subject Holocene
dc.title ISOTOPIC COMPOSITION OF BIOGENIC CARBONATES AND HOLOCENE PALEOGEOGRAPHIC RECONSTRUCTIONS OF THE WESTERN CASPIAN SEASHORE
dc.type Статья
dc.subject.age Cenozoic::Quaternary::Holocene
dc.subject.age Кайнозой::Четвертичная::Голоцен ru


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