KFU. Card publication. The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region, East-European Platform

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THE PARASTRATOTYPE OF THE URZHUMIAN STAGE IN THE VYATKA-KAZAN REGION, EAST-EUROPEAN PLATFORM

Form of presentation

Articles in international journals and collections

Year of publication

2018

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Authors, employees of KFU

Arefev Mikhail Pavlovich, author

Bakaev Aleksandr Sergeevich, author

Bulanov Valeriy Viktorovich, author

Ivanov Aleksandr Olegovich, author

Muravev Fedor Aleksandrovich, author

Silantev Vladimir Vladimirovich, author

Authors, postgraduates KFU

Zharinova Veronika Vladimirovna, postgraduate kfu

Urazaeva Milyausha Nazimovna, postgraduate kfu

Bibliographic description in the original language

Silantiev, V., Arefiev, M., Mouraviev, F., Bulanov, V., Ivanov, A., Urazaeva, M., Bakaev, A., Zharinova, V. (2018). The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region, East-European Platform / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 206-215.

Annotation

New multidisciplinary studies of the Urzhumian parastratotype confirm its reference status for the Vyatka-Kazan region of European Russia. The purely continental Urzhumian represents the upper unit of the Biarmian Series (Middle Permian) of the Geological Time Scale of Russia and is tentatively correlated with the Wordian of the International Chronostratigraphic Chart. The lower part of the parastratotype corresponds to the Sulitsa Formation and consists of lacustrine red-bed continental rocks containing rare conchostracans and fish scales. The upper part of the parastratotype corresponds to the Isheevo Formation and is composed of red-colored alluviallacustrine terrigenous and clayey rocks with interbeds of microbial limestones. The clayey rocks often include a large number of paleosols of differing maturity, among which vertisols and calcisols prevail. This part of the section contains a diverse fauna of non-marine ostracodes, bivalves, conchostracans, fishes and tetrapods.

Keywords

Middle Permian, Urzhumian, biostratigraphy, non-marine bivalves, ostracodes, conchostracans, fish, tetrapods

The name of the journal

IOP Conference Series: Earth and Environmental Science

URL

http://www.filodirittoeditore.com/index.php?route=product/product&product_id=160

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=181983&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Arefev Mikhail Pavlovich	ru_RU
dc.contributor.author	Bakaev Aleksandr Sergeevich	ru_RU
dc.contributor.author	Bulanov Valeriy Viktorovich	ru_RU
dc.contributor.author	Ivanov Aleksandr Olegovich	ru_RU
dc.contributor.author	Muravev Fedor Aleksandrovich	ru_RU
dc.contributor.author	Silantev Vladimir Vladimirovich	ru_RU
dc.contributor.author	Zharinova Veronika Vladimirovna	ru_RU
dc.contributor.author	Urazaeva Milyausha Nazimovna	ru_RU
dc.date.accessioned	2018-01-01T00:00:00Z	ru_RU
dc.date.available	2018-01-01T00:00:00Z	ru_RU
dc.date.issued	2018	ru_RU
dc.identifier.citation	Silantiev, V., Arefiev, M., Mouraviev, F., Bulanov, V., Ivanov, A., Urazaeva, M., Bakaev, A., Zharinova, V. (2018). The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region, East-European Platform / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 206-215.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=181983&p_lang=2	ru_RU
dc.description.abstract	IOP Conference Series: Earth and Environmental Science	ru_RU
dc.description.abstract	New multidisciplinary studies of the Urzhumian parastratotype confirm its reference status for the Vyatka-Kazan region of European Russia. The purely continental Urzhumian represents the upper unit of the Biarmian Series (Middle Permian) of the Geological Time Scale of Russia and is tentatively correlated with the Wordian of the International Chronostratigraphic Chart. The lower part of the parastratotype corresponds to the Sulitsa Formation and consists of lacustrine red-bed continental rocks containing rare conchostracans and fish scales. The upper part of the parastratotype corresponds to the Isheevo Formation and is composed of red-colored alluviallacustrine terrigenous and clayey rocks with interbeds of microbial limestones. The clayey rocks often include a large number of paleosols of differing maturity, among which vertisols and calcisols prevail. This part of the section contains a diverse fauna of non-marine ostracodes, bivalves, conchostracans, fishes and tetrapods.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Middle Permian	ru_RU
dc.subject	Urzhumian	ru_RU
dc.subject	biostratigraphy	ru_RU
dc.subject	non-marine bivalves	ru_RU
dc.subject	ostracodes	ru_RU
dc.subject	conchostracans	ru_RU
dc.subject	fish	ru_RU
dc.subject	tetrapods	ru_RU
dc.title	The Parastratotype of the Urzhumian Stage in the Vyatka-Kazan Region, East-European Platform	ru_RU
dc.type	Articles in international journals and collections	ru_RU