FIRST DINOFLAGELLATE FINDS IN UPPER OLIGOCENE CONTINENTAL SEDIMENTS OF THE ZHURAVKA FORMATION (WESTERN SIBERIA)

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dc.contributor.author Kuz'mina O.B.
dc.contributor.author Volkova V.S.
dc.date.accessioned 2022-08-14T03:31:12Z
dc.date.available 2022-08-14T03:31:12Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=13472517
dc.identifier.citation Doklady Earth Sciences, 2004, 394, 1, 14-18
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38549
dc.description.abstract The first findings of dinocysts Pseudokomewuia in Western Siberia are analyzed from the viewpoint of their significance for solving the questions of stratigraphy, paleogeography and paleoecology of basins in Cenozoic era.
dc.subject Oligocene
dc.title FIRST DINOFLAGELLATE FINDS IN UPPER OLIGOCENE CONTINENTAL SEDIMENTS OF THE ZHURAVKA FORMATION (WESTERN SIBERIA)
dc.type Статья
dc.subject.age Cenozoic::Paleogene::Oligocene
dc.subject.age Кайнозой::Палеоген::Олигоцен ru


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