{"title":"A new locality of chondrichthyan fishes from the Upper Paleocene on the right bank of the Don river (Volgograd region)","authors":"V. A. Lopyrev, E. Popov","doi":"10.18500/1819-7663-2022-22-2-140-152","DOIUrl":null,"url":null,"abstract":"An assemblage of chondrichthyans is described from the new locality near Serafimovich town (the western part of Volgograd region). More than 2500 fossils were collected from the basal gravel-pebble bed and phosphorite-bearing layer from the lower part of the Buzinovka formation (upper Paleocene). There are reworked Cretaceous and Paleocene chondrichthyans (6 species) and synchronous 21 species of sharks and 2 species of chimaeroids. The presence of synchronous Gluekmanotodus heinzelini, Odontaspis winkleri, Paraorthacodus eocaenus, Xampylodon loozi allows correlating the described lower part of the Buzinovka formation with NP8 – NP9 nannoplankton zones or Alisocysta margarita – Axiodinium augustum dinocyst zones (Thanetian – basal Ypresian).","PeriodicalId":193038,"journal":{"name":"Izvestiya of Saratov University. Earth Sciences","volume":"288 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-05-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya of Saratov University. Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18500/1819-7663-2022-22-2-140-152","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
An assemblage of chondrichthyans is described from the new locality near Serafimovich town (the western part of Volgograd region). More than 2500 fossils were collected from the basal gravel-pebble bed and phosphorite-bearing layer from the lower part of the Buzinovka formation (upper Paleocene). There are reworked Cretaceous and Paleocene chondrichthyans (6 species) and synchronous 21 species of sharks and 2 species of chimaeroids. The presence of synchronous Gluekmanotodus heinzelini, Odontaspis winkleri, Paraorthacodus eocaenus, Xampylodon loozi allows correlating the described lower part of the Buzinovka formation with NP8 – NP9 nannoplankton zones or Alisocysta margarita – Axiodinium augustum dinocyst zones (Thanetian – basal Ypresian).