Yıldız, AyşegülToker, Vedia13.07.20192019-07-1613.07.20192019-07-1620061367-9120https://dx.doi.org/10.1016/j.jseaes.2005.07.010https://hdl.handle.net/20.500.12451/2938Pseudoemiliana lacunosa, Gephyrocapsa oceanica and Emiliania huxleyi (Ionian) (Pleistocene-Holocene) calcareous nannoplankton zones were identified from 82 samples of 14 cores taken from 8 locations in the northeastern Sea of Marmara. The investigation indicates that the identified biozones have been alternated by tectonic activity in the 1, 5 and 6 core locations. The study area has been affected three times by tectonic activity during the Pleistocene-Holocene time interval. The first activity occured during the Early Pleistocene and the others during Holocene. © 2005 Elsevier Ltd. All rights reserved.eninfo:eu-repo/semantics/closedAccessBiostratigraphyNannofossilPleistocene-HoloceneSea of MarmaraTurkeyArticle27683584610.1016/j.jseaes.2005.07.010Q1