FORAMINIFER ZONES OF THE CALLOVIAN STAGE IN THE LOWER VOLGA REGION

dc.contributor.author	Saltykov V.F.
dc.date.accessioned	2024-10-23T07:16:03Z
dc.date.available	2024-10-23T07:16:03Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512620
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 356-360
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46169
dc.description.abstract	Callovian stratigraphy is usually based on ammonites, while foraminiferal assemblages are correlated with the ammonite scale. Precisely this approach was used for elaborating the Callovian stratigraphic scale for the Russian Platform based on the foraminifer group of microorganisms, which was proposed by a team of paleontologists at meetings in Vilnius (1982) and Tbilisi (1984). During recent decades, the lower Callovian ammonite scale was subjected to some changes, which makes it necessary to revise stratification of this substage in the Russian Platform.
dc.subject	Callovian
dc.title	FORAMINIFER ZONES OF THE CALLOVIAN STAGE IN THE LOWER VOLGA REGION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030032
dc.subject.age	Mesozoic::Jurassic::Middle::Callovian
dc.subject.age	Мезозой::Юрская::Средний::Келловейский

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