CRETACEOUS RESEARCH, vol.87, pp.296-311, 2018 (Peer-Reviewed Journal)
Article / Article
Science Citation Index Expanded, Scopus
Upper Cretaceous, Foraminifera, Calcareous nannofossils, Correlations, NORTHERN CALCAREOUS ALPS, RED BEDS, NIERENTAL FORMATION, CRETACEOUS CLIMATE, STABLE-ISOTOPES, NW TURKEY, FORAMINIFERA, EVOLUTION, TETHYS, PALEOCEANOGRAPHY
The Santonian-Campanian boundary interval close to the village of Goynuk in northwestern Turkey (Bolu province) was recorded and examined with respect to nannofossil and foraminiferal biostratigraphy, magnetic polarity and magnetic susceptibility. During the Late Cretaceous, the Mudurnu-Goynuk Basin was located on the Sakarya continent situated in the northwestern Tethyan Realm, north of the Neo-Tethys.