Akademik Veri Yönetim Sistemi
Forams 2018, Edinburgh, Birleşik Krallık, 17 Haziran 2018 - 22 Ocak 2020, ss.1
The Upper Paleocene sequence in the Sinop Basin, eastern part of Sinop Basin, is investigated to determine the benthic and planktonic foraminiferal biozones. The studied sequence belongs to the Upper Paleocene Atbasi Formation.
A section was measured from the formation. The succession includes benthic and abundant planktonic foraminifera. The benthic foraminiferal assemblages are made up of 27 species belonging to 22 genera, namely Ammodiscus, Anomalina, Bolivinopsis, Cibicides, Cribrostomoides, Dentalina, Haplophragmoides, Gavelinella, Globulina, Glomospira, Gyroidina, Lagena, Lenticulina, Nodosaria, Nodosariella, Pararotalia, Planulina, Pullenia, Pulvinulinella, Robulus, Spirillina, Textularia. The sequence also contains benthic foraminifera with hyaline calcareous, calcareous and agglutinated cosmopolitan deep sea genera.
An Upper Paleocene Lower planktonic foraminiferal Zone P4c was distinguished by using 15 species belonging to 6 genera, consisting of Acarinina, Chiloguembelina, Globanomalina, Morozovella, Parasubbotina, Subbotina. This biozone is represented by a Acarinina soldadoenssis-Globanomalina pseudomenardii biozone.
The Upper Paleocene sequence in the Sinop Basin, eastern part of Sinop Basin, is investigated to determine the benthic and planktonic foraminiferal biozones. The studied sequence belongs to the Upper Paleocene Atbasi Formation.
A section was measured from the formation. The succession includes benthic and abundant planktonic foraminifera. The benthic foraminiferal assemblages are made up of 27 species belonging to 22 genera, namely Ammodiscus, Anomalina, Bolivinopsis, Cibicides, Cribrostomoides, Dentalina, Haplophragmoides, Gavelinella, Globulina, Glomospira, Gyroidina, Lagena, Lenticulina, Nodosaria, Nodosariella, Pararotalia, Planulina, Pullenia, Pulvinulinella, Robulus, Spirillina, Textularia. The sequence also contains benthic foraminifera with hyaline calcareous, calcareous and agglutinated cosmopolitan deep sea genera.
An Upper Paleocene Lower planktonic foraminiferal Zone P4c was distinguished by using 15 species belonging to 6 genera, consisting of Acarinina, Chiloguembelina, Globanomalina, Morozovella, Parasubbotina, Subbotina. This biozone is represented by a Acarinina soldadoenssis-Globanomalina pseudomenardii biozone.