Kazan (Volga region) Federal University, KFU
KAZAN
FEDERAL UNIVERSITY
 
MULTIDISCIPLINARY STUDY OF THE MECHETLINO QUARRY SECTION (SOUTHERN URALS, RUSSIA) ? THE GSSP CANDIDATE FOR THE BASE OF THE KUNGURIAN STAGE (LOWER PERMIAN)
Form of presentationArticles in international journals and collections
Year of publication2020
Языканглийский
  • Balabanov Yuriy Pavlovich, author
  • Batalin Georgiy Aleksandrovich, author
  • Gareev Bulat Irekovich, author
  • Kotlyar Galina Vasilevna, author
  • Nurgalieva Nuriya Gavazovna, author
  • Sungatullin Rafael Kharisovich, author
  • Sungatullina Guzal Marsovna, author
  • Boyko Maksim Sergeevich, author
  • Ivanov Aleksandr Olegovich, author
  • Isakova Tatyana Nikolaevna, author
  • Kutygin Ruslan Vladimirovich, author
  • Mizens Gunar Andreevich, author
  • Mychko Eduard Vagifovich, author
  • Filimonova Tatyana Valerievna, author
  • Chernykh Valeriy Vladimirovich, author
  • Chuvashov Boris Ivanovich, author
  • Bibliographic description in the original language Chernykh, V.V., Kotlyar, G.V., Chuvashov, B.I., Kutygin, R.V., Filimonova, T.V., Sungatullina, G.M., Mizens, G.A., Sungatullin, R.K., Isakova, T.N., Boiko, M.S., Ivanov, A.O., Nurgalieva, N.G., Balabanov, Y.P., Mychko, E.V., Gareev, B.I., Batalin, G.A. Multidisciplinary study of the Mechetlino Quarry section (Southern Urals, Russia) - The GSSP candidate for the base of the Kungurian Stage (Lower Permian)//Palaeoworld. - 2020. - Vol.29, Is.2. - P. 325-352.
    Annotation The Mechetlino Quarry section is a potential candidate for the Global Section Stratotype and Point (GSSP) for the base of the Global KungurianStage on the International Stratigraphic Chart. In 2017, the Mechetlino Quarry section became the part of the First Geopark in Russia, thereforeexcavation work was carried out to clear it, a road was laid, and infrastructure was developed. Recent evidence to justify the base Kungurian boundaryin the Mechetlino section was obtained. Additional conodonts confirmed the data of V.V. Chernykh on the Artinskian–Kungurian transition. BesidesNeostreptognathodus pnevi Kozur and Movshovitsch, the second marker (N. lectulus Chernykh) of the base-Kungurian was established. TheArtinskian–Kungurian transition of the Mechetlino Quarry section is characterized by the richest associations of small foraminifers, ammonoids,and other groups. The occurrence of mass Clausiuraloceras above the Kungurian boundary, which changed the representative Artinskian association,was identified. Small foraminifers of the Artinskian–Kungurian transition are numerous and include sufficient species to provide a correlation withWestern Tethys, Svalbard and Australia. Data on isotopic ratios of 13C and 18O, 13Corgvalues and the magnetic susceptibility were obtained forthe first time.
    Keywords Mechetlino section; Artinskian Stage; Conodonts; Ammonoids; Foraminifera; GSSP of Kungurian Stage
    The name of the journal Palaeoworld
    URL https://www.scopus.com/inward/record.uri?eid=2-s2.0-85067196996&doi=10.1016%2fj.palwor.2019.05.012&partnerID=40&md5=fb26d7546b2b218922b9c406121ddda4
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