{"title":"伊拉克东北部Bekhme地区Tanjero组(马斯特里赫特晚期)浮游有孔虫生物地层学","authors":"Majid M. Al-Mutwali, M. Ibrahim","doi":"10.33899/earth.2019.170035","DOIUrl":null,"url":null,"abstract":"The biostratigraphy of Tanjero Formation has been investigated within a wellexposed section at the northern limb of Perat anticline, Bekhme area, Northeastern Iraq. The studied section consists mainly of marl, marly limestone, and sandstone. The formation conformably overlies Shiranish Formation (Late Campanian-Maastrichtian) and it is overlain unconformably by the Kolosh Formation (Paleocene). The samples of the section under investigation yielded rich and well diversified planktonic foraminiferal taxa, where 69 planktonic species belonging to 21 genera have been recognized. The detailed foraminiferal investigation permits the recognition of four well defined zones. These are from older at the base: 4. Plummerita hantkeninoides Total Range Zone. 3. Pseudoguembelina palpebra Partial Range Zone. 2. Pseudoguembelina hariaensis Interval Zone. 1. Racemiguembelina fructicosa Interval Zone. The Planktonic zones were correlated with other zonal schemes inand outside Iraq. They are considered to be of Late Maastrichtian age.","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"46 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-05-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Planktonic Foraminiferal Biostratigraphy of Tanjero Formation (Late Maastrichtian) in Bekhme Area, Northeastern Iraq\",\"authors\":\"Majid M. Al-Mutwali, M. Ibrahim\",\"doi\":\"10.33899/earth.2019.170035\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The biostratigraphy of Tanjero Formation has been investigated within a wellexposed section at the northern limb of Perat anticline, Bekhme area, Northeastern Iraq. The studied section consists mainly of marl, marly limestone, and sandstone. The formation conformably overlies Shiranish Formation (Late Campanian-Maastrichtian) and it is overlain unconformably by the Kolosh Formation (Paleocene). The samples of the section under investigation yielded rich and well diversified planktonic foraminiferal taxa, where 69 planktonic species belonging to 21 genera have been recognized. The detailed foraminiferal investigation permits the recognition of four well defined zones. These are from older at the base: 4. Plummerita hantkeninoides Total Range Zone. 3. Pseudoguembelina palpebra Partial Range Zone. 2. Pseudoguembelina hariaensis Interval Zone. 1. Racemiguembelina fructicosa Interval Zone. The Planktonic zones were correlated with other zonal schemes inand outside Iraq. They are considered to be of Late Maastrichtian age.\",\"PeriodicalId\":371191,\"journal\":{\"name\":\"Iraqi National Journal of Earth Sciences\",\"volume\":\"46 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2019-05-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Iraqi National Journal of Earth Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33899/earth.2019.170035\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Iraqi National Journal of Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33899/earth.2019.170035","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Planktonic Foraminiferal Biostratigraphy of Tanjero Formation (Late Maastrichtian) in Bekhme Area, Northeastern Iraq
The biostratigraphy of Tanjero Formation has been investigated within a wellexposed section at the northern limb of Perat anticline, Bekhme area, Northeastern Iraq. The studied section consists mainly of marl, marly limestone, and sandstone. The formation conformably overlies Shiranish Formation (Late Campanian-Maastrichtian) and it is overlain unconformably by the Kolosh Formation (Paleocene). The samples of the section under investigation yielded rich and well diversified planktonic foraminiferal taxa, where 69 planktonic species belonging to 21 genera have been recognized. The detailed foraminiferal investigation permits the recognition of four well defined zones. These are from older at the base: 4. Plummerita hantkeninoides Total Range Zone. 3. Pseudoguembelina palpebra Partial Range Zone. 2. Pseudoguembelina hariaensis Interval Zone. 1. Racemiguembelina fructicosa Interval Zone. The Planktonic zones were correlated with other zonal schemes inand outside Iraq. They are considered to be of Late Maastrichtian age.