Yildiz, AysegulToker, Vedia2019-08-012019-08-0120061367-9120https://dx.doi.org/10.1016/j.jseaes.2005.07.010https://hdl.handle.net/11480/5480Pseudoemiliana 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. (c) 2005 Elsevier Ltd. All rights reserved.eninfo:eu-repo/semantics/closedAccessbiostratigraphynannofossilPleistocene-HoloceneSea of MarmaraTurkeyArticle27683584610.1016/j.jseaes.2005.07.0102-s2.0-33748066677Q1WOS:000240883900007Q2