A. Bakaev, V. V. Bulanov, I. Ilaltdinov, D. Kozhanov, G. Ponomareva, I. Khopta
{"title":"The Problem of Dating the Kuyeda-Klyuchiki Section – a Unique Locality of Permian Vertebrates (Perm Region, Russia)","authors":"A. Bakaev, V. V. Bulanov, I. Ilaltdinov, D. Kozhanov, G. Ponomareva, I. Khopta","doi":"10.26907/2542-064x.2021.3.444-465","DOIUrl":null,"url":null,"abstract":"The Kueda-Klyuchiki locality of Permian vertebrates located in the south of the Perm Region in the Kuedinsky District was discovered in 2005 and quickly became known among paleontologists. The locality contains a rich complex of exceptionally preserved plants and vertebrates (fish, amphibians, and reptiles). Their remains are confined to limestones of various textures, which form two bone-bearing beds in the section of the quarry. However, the age of rocks remains a controversial issue. This research aims to analyze and compare various stratigraphic markers and discuss a number of existing stratigraphic inconsistencies in an attempt to arrive at a general conclusion about the age of the locality. According to geological survey data on a scale of 1:200 000, the Buraevo Sequence (Sheshmian Formation, Ufimian Stage) was identified in the territory of the quarry. At the boundary of the Sheshmian and Belebey Formations, a mineralogical “boundary” is observed, which is manifested in a decrease","PeriodicalId":23418,"journal":{"name":"Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki","volume":"12 1","pages":""},"PeriodicalIF":0.4000,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26907/2542-064x.2021.3.444-465","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MULTIDISCIPLINARY SCIENCES","Score":null,"Total":0}
引用次数: 2
Abstract
The Kueda-Klyuchiki locality of Permian vertebrates located in the south of the Perm Region in the Kuedinsky District was discovered in 2005 and quickly became known among paleontologists. The locality contains a rich complex of exceptionally preserved plants and vertebrates (fish, amphibians, and reptiles). Their remains are confined to limestones of various textures, which form two bone-bearing beds in the section of the quarry. However, the age of rocks remains a controversial issue. This research aims to analyze and compare various stratigraphic markers and discuss a number of existing stratigraphic inconsistencies in an attempt to arrive at a general conclusion about the age of the locality. According to geological survey data on a scale of 1:200 000, the Buraevo Sequence (Sheshmian Formation, Ufimian Stage) was identified in the territory of the quarry. At the boundary of the Sheshmian and Belebey Formations, a mineralogical “boundary” is observed, which is manifested in a decrease