Drilling and core data from the Gulf of Gemlik (SE Sea of Marmara): Holocene fauna and flora assemblages

dc.authorid0000-0002-5975-3678
dc.authorid0000-0003-0658-0416
dc.authorid0000-0001-7996-7430
dc.authorid0000-0003-0853-3912
dc.authorid0000-0002-9440-4561
dc.authorid0000-0003-2678-3907
dc.authorid0000-0003-4823-3594
dc.authorid0000-0002-5042-7227
dc.contributor.authorMeriç, Engin
dc.contributor.authorYümün, Zeki Ünal
dc.contributor.authorNazik, Atike
dc.contributor.authorSa?ular, Enis Kemal
dc.contributor.authorYokeş, Mehmet Baki
dc.contributor.authorBüyükmerıç, Yeşim
dc.contributor.authorYıldız, Ayşegül
dc.contributor.authorYavuzlar, Gülin
dc.date.accessioned2021-06-09T07:45:06Z
dc.date.available2021-06-09T07:45:06Z
dc.date.issued2020
dc.departmentMühendislik Fakültesi
dc.description*Yıldız, Ayşegül ( Aksaray, Yazar )
dc.description.abstractThis study was conducted to determine fauna and flora assemblages of Holocene sequences from Gemlik Gulf (SE Marmara Sea) and to obtaine their similarities and differences between the assemblages of Gemlik and İzmit Bays. Total of 201 dark gray colored, fine to medium grained sandy clay samples were studied. In the drilled samples, 22 genera and 38 species were identified from the foraminifera characterizing the infralittoral zone. 40 genera and 58 species of foraminifera characterizing the upper circalittoral zone were identified. In addition, Black Sea originated Ammonia parasovica was found for the first time in cores taken from Gemlik Gulf. Nannofossil species characterizing the open-shallow marine environment Emiliania huxleyi, Reticulofenestra parvula, Coronosphaera spp., Syracosphaera spp., Helicosphaera spp. beside Gephyrocapsa oceanica, small Gephyrocapsa spp., Scyphosphaera porosa were obtained. A total of 27 genera and 37 species from ostracods were defined in the samples from gulf. Moreover, the quite abundant mollusc assemblage characterizing the shallow marine environment and fewer genera and species of diatoms were identified. The studied sequence is represented by NN21 Emiliania huxleyi biozone at the Holocene. Foraminifers and ostracods of the Gemlik Gulf are observed as Mediterranean-Aegean Sea originated assemblages. The mollusc shows the shallow marine community.
dc.identifier.doi10.19111/bulletinofmre.581537
dc.identifier.endpage150en_US
dc.identifier.issn0026-4563
dc.identifier.issue-en_US
dc.identifier.scopusqualityQ3
dc.identifier.startpage121en_US
dc.identifier.urihttps:/dx.doi.org/10.19111/bulletinofmre.581537
dc.identifier.urihttps://hdl.handle.net/20.500.12451/8100
dc.identifier.volume161en_US
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakTR-Dizin
dc.language.isoen
dc.publisherGeneral Directorate of Mineral Research and Exploration (MTA)
dc.relation.ispartofBulletin of the Mineral Research and Exploration
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectDiatome
dc.subjectForaminifer
dc.subjectGemlik Gulf
dc.subjectMollusc
dc.subjectNannoplankton
dc.subjectOstracod
dc.titleDrilling and core data from the Gulf of Gemlik (SE Sea of Marmara): Holocene fauna and flora assemblages
dc.typeArticle

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