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Upper Cretaceous Deposits of the Volsk Structural Zone of the East European Platform: Turonian–Lower Campanian of the Kommunar Section: Paper 2. Macrofauna Review, Conclusions

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dc.abstract.enThe vertical ranges of inocerams, belemnites, ammonites, echinoids, sponges, and brachiopods from lithologically monotonous carbonate rocks have been studied in the Kommunar section. The results obtained in the study of macrofaunistic assemblages confirm and complement the benthic foraminifera research data of distinguished units of the middle–upper Turonian, Coniacian, lower and upper Santonian, and lower Campanian basal horizon. The stratigraphically full upper Coniacian–lower Santonian interval in the Kommunar section has been identified in the Volga region for the first time. The defined macro- and microfaunistic biostratigraphic units have been correlated and discussed. The Boreal–Tethyan magnetochronological correlation of the Santonian–Campanian makes it possible to conclude that the Santonian lower boundary in different regions differs by about a million years, which is comparable to the duration of the Santonian. © 2022, Pleiades Publishing, Ltd.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorKhudyakov, D. V.
dc.contributor.authorIl’inskii, E. I.
dc.contributor.authorGuzhikova, A. A.
dc.contributor.authorKalyakin, E. A.
dc.contributor.authorWalaszczyk, Ireneusz
dc.contributor.authorSel’tser, V. B.
dc.contributor.authorRyabov, I. P.
dc.contributor.authorPervushov, E. M.
dc.date.accessioned2024-01-26T11:21:20Z
dc.date.available2024-01-26T11:21:20Z
dc.date.issued2022
dc.description.financePublikacja bezkosztowa
dc.description.number2
dc.description.volume30
dc.identifier.doi10.1134/S0869593822030042
dc.identifier.issn0869-5938
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/124292
dc.identifier.weblinkhttps://link.springer.com/content/pdf/10.1134/S0869593822030042.pdf
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofStratigraphy and Geological Correlation
dc.relation.pages89-115
dc.rightsClosedAccess
dc.sciencecloudnosend
dc.subject.enammonites
dc.subject.enbelemnites
dc.subject.enbiostratigraphy
dc.subject.enbrachiopods
dc.subject.enCampanian
dc.subject.enConiacian
dc.subject.enechinoids
dc.subject.eninocerams
dc.subject.enmagnetostratigraphy
dc.subject.enSantonian
dc.subject.ensponges
dc.subject.enTuronian
dc.subject.enUpper Cretaceous
dc.subject.enVolga region
dc.subject.enVolsk structural zone
dc.titleUpper Cretaceous Deposits of the Volsk Structural Zone of the East European Platform: Turonian–Lower Campanian of the Kommunar Section: Paper 2. Macrofauna Review, Conclusions
dc.typeJournalArticle
dspace.entity.typePublication