FORAMINIFERS FROM THE SERPUKHOVIAN STAGE STRATOTYPE, THE ZABOR'E QUARRY SITE (MOSCOW REGION)

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dc.contributor.author Gibshman N.B.
dc.date.accessioned 2021-11-23T00:58:49Z
dc.date.available 2021-11-23T00:58:49Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=13436877
dc.identifier.citation Stratigraphy and Geological Correlation, 2003, 11, 1, 36-60
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/32428
dc.description.abstract Distribution of foraminifers in the Tarusa, Steshev, and Protva horizons of the Serpukhovian Stage stratotype has been studied in the Zabor'e Quarry. Boundaries of Pseudoendothyra globosa. Eostaffellina decurta, and Eostaffellina protvae zones distinguished here are defined at the first occurrence levels of zonal index species. As is established, boundaries between horizons and foraminiferal zones do not coincide. Neoarchaediscus postrugosus (Reitl.) and "Millerella" tortula Zeller, which appear at the boundary between the Visean and Serpukhovian stages, can be regarded as markers of that stratigraphic level. Species "Millerella" tortula Zeller, Janischewskina delicata Mal., and Brenckleina rugosa (Brazhn.), which are important for stratigraphic subdivision and correlation, have been identified for the first time in the Moscow region. It is shown based on the microfacies analysis that foraminifers populated calm settings of a shallow sea that was shoaling with time up to the appearance of algal banks.
dc.subject Serpukhovian
dc.title FORAMINIFERS FROM THE SERPUKHOVIAN STAGE STRATOTYPE, THE ZABOR'E QUARRY SITE (MOSCOW REGION)
dc.type Статья
dc.subject.age Paleozoic::Carboniferous::Mississippian::Upper::Serpukhovian
dc.subject.age Палеозой::Каменноугольная::Верхний::Серпуховский ru


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