M. Djakovic, G. Ćulafić, M. Milić, Damjan Ćađenović, N. Radulović
{"title":"黑山南部Budva地区Mide地区白垩纪-古近纪复理石的鱼化石","authors":"M. Djakovic, G. Ćulafić, M. Milić, Damjan Ćađenović, N. Radulović","doi":"10.2298/GABP1802011D","DOIUrl":null,"url":null,"abstract":"Cretaceous-Paleogene flysch represents the youngest formation in the Budva Zone. Although the Maastrichtian-Lower Eocene age of these rocks has been well documented in the literature, trace fossils areonly mentioned as abundant and not described. In the present paper, only a small number of ichnotaxa fromMide locality has been described, including Lorenzinia carpathica (ZUBER), Nereites irregularis (SCHAFHAUT), Scolicia plana KSIĄŻKIEWICZ and Paleodictyon latum VIALOV & GOLEV. They confirm deepsea environment.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"152 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-12-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Ichnofossils from Cretaceous-Paleogene flysch of Mide locality (Budva zone, Southern Montenegro)\",\"authors\":\"M. Djakovic, G. Ćulafić, M. Milić, Damjan Ćađenović, N. Radulović\",\"doi\":\"10.2298/GABP1802011D\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Cretaceous-Paleogene flysch represents the youngest formation in the Budva Zone. Although the Maastrichtian-Lower Eocene age of these rocks has been well documented in the literature, trace fossils areonly mentioned as abundant and not described. In the present paper, only a small number of ichnotaxa fromMide locality has been described, including Lorenzinia carpathica (ZUBER), Nereites irregularis (SCHAFHAUT), Scolicia plana KSIĄŻKIEWICZ and Paleodictyon latum VIALOV & GOLEV. They confirm deepsea environment.\",\"PeriodicalId\":263923,\"journal\":{\"name\":\"Geoloski Anali Balkanskog Poluostrva\",\"volume\":\"152 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-12-21\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoloski Anali Balkanskog Poluostrva\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2298/GABP1802011D\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoloski Anali Balkanskog Poluostrva","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2298/GABP1802011D","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Ichnofossils from Cretaceous-Paleogene flysch of Mide locality (Budva zone, Southern Montenegro)
Cretaceous-Paleogene flysch represents the youngest formation in the Budva Zone. Although the Maastrichtian-Lower Eocene age of these rocks has been well documented in the literature, trace fossils areonly mentioned as abundant and not described. In the present paper, only a small number of ichnotaxa fromMide locality has been described, including Lorenzinia carpathica (ZUBER), Nereites irregularis (SCHAFHAUT), Scolicia plana KSIĄŻKIEWICZ and Paleodictyon latum VIALOV & GOLEV. They confirm deepsea environment.