ON THE LATE PALEOCENE STRATIGRAPHY OF THE SARATOV VOLGA REGION: MICROPALEONTOLOGICAL CHARACTERISTICS OF THE KAMYSHIN FORMATION, DYUPA GULLY SECTION

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dc.contributor.author Aleksandrova G.N.
dc.contributor.author Radionova E.P.
dc.date.accessioned 2025-06-10T10:13:40Z
dc.date.available 2025-06-10T10:13:40Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=13530566
dc.identifier.citation Paleontological Journal, 2006, 40, Suppl. 5,
dc.identifier.issn 0031-0301
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/49364
dc.description.abstract This paper presents the results of the integrated study of dinocysts and diatoms from the Kamyshin Formation, Dyupa Gully section. The Kamyshin Formation is shown to have been formed in the Late Thanetian-initial Eocene and to include the IETM interval. The Dyupa Gully section is comprised of the deposits of two transgressive-regressive cycles. The section is comprehensively characterized by micropaleontological finds (dinocysts, radiolarians, and diatoms) and proposed as a key section of the Middle Volga Region. © Pleiades Publishing, Inc. 2006.
dc.subject DIATOMS
dc.subject DINOCYSTS
dc.subject EARLY EOCENE
dc.subject LATE THANETIAN
dc.subject STRATIGRAPHY
dc.subject VOLGA RIVER REGION
dc.subject Eocene
dc.subject Thanetian
dc.title ON THE LATE PALEOCENE STRATIGRAPHY OF THE SARATOV VOLGA REGION: MICROPALEONTOLOGICAL CHARACTERISTICS OF THE KAMYSHIN FORMATION, DYUPA GULLY SECTION
dc.type Статья
dc.identifier.doi 10.1134/S0031030106110013
dc.subject.age Cenozoic::Paleogene::Eocene
dc.subject.age Кайнозой::Палеоген::Эоцен
dc.subject.age Cenozoic::Paleogene::Paleocene::Thanetian
dc.subject.age Кайнозой::Палеоген::Палеоцен::Танетский


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