Shallow Marine Benthic Foraminifera Assemblage of the Early Eocene Succession in the Northern Arac (Kastamonu) and Paleoecological Interpretation

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dc.contributor.authorOzgen Erdem, Nazire
dc.contributor.authorCanbolat, M. Yasin
dc.contributor.authorSinanoglu, Derya
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:45:06Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:45:06Z
dc.date.issued2016
dc.department[Ozgen Erdem, Nazire] Cumhuriyet Univ, Jeol Muhendisligi Bolumu, TR-58140 Sivas, Turkey -- [Canbolat, M. Yasin] Nevsehir Haci Bektas Veli Univ, Jeol Muhendisligi Bolumu, TR-50300 Nevsehir, Turkey -- [Sinanoglu, Derya] Batman Univ, Jeol Muhendisligi Bolumu, TR-72000 Batman, Turkeyen_US
dc.description.abstractSoganli Formation of Early Eocene age in the northeastern of Arac (Kastamonu) has been investigated in order to determine their paleontology and palaeoecology. The sequence consists of gray, yellowish, clayey limestone, rich in larger benthic foraminifers. The lower parts of clayey limestone are dominated by porcellaneous foraminifera such as Alveolina and Orbitolites and by dascylad algae. The top of the section is characterized by hyaline calcareous foraminifers such as Assilina and Nummulites. Idalina sinjarica Grimsdale, Glomalveolina lepidula Schwager, A. cemali Sirel & Acar, A. rotundata kazancii Sirel & Acar, A. erki Acar, A. ankarensis Sirel, A. pieroi Sirel & Acar, Lockhartia conditi (Nuttall), L. tipperi (Davies), Orbitolites complanatus Lamarck, Cyclopertorbitolites tokerae Ozgen-Erdem, Assilina spinosa Davies & Pinfold, Nummulites sp., Cribrobulimina sp., Kathina sp., Neorotalia sp., Triloculina sp. have been decribed along the section. The distribution of the larger benthic foraminifera indicates Early Eocene age. According to these assemblages, we interpret that deposition of the unit started in a restricted shallower environment and continued in a shallow high energy environment.en_US
dc.identifier.endpage273en_US
dc.identifier.issn1016-9164
dc.identifier.issue3en_US
dc.identifier.startpage259en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12418/7253
dc.identifier.volume59en_US
dc.identifier.wosWOS:000443714500002en_US
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isotren_US
dc.publisherTMMOB JEOLOJI MUHENDISLERI ODASIen_US
dc.relation.ispartofTURKIYE JEOLOJI BULTENI-GEOLOGICAL BULLETIN OF TURKEYen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectArac (Kastamonu)en_US
dc.subjectbenthic foraminiferaen_US
dc.subjectearly Ypresianen_US
dc.subjectEoceneen_US
dc.titleShallow Marine Benthic Foraminifera Assemblage of the Early Eocene Succession in the Northern Arac (Kastamonu) and Paleoecological Interpretationen_US
dc.typeArticleen_US

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