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dc.contributor.authorSalihoğlu, Rana
dc.contributor.authorDinçer, Feyza
dc.contributor.authorDarbs, Güldemin
dc.date.accessioned2020-11-20T14:42:34Z
dc.date.available2020-11-20T14:42:34Z
dc.date.issued2019
dc.identifier.issn1464-343X
dc.identifier.issn1879-1956
dc.identifier.urihttps://doi.org/10.1016/j.jafrearsci.2018.12.017
dc.identifier.urihttps://hdl.handle.net/20.500.12809/1085
dc.descriptionGül, Murat/0000-0003-1555-6426; Salihoğlu, Rana/0000-0003-3277-2446en_US
dc.descriptionWOS: 000459841400015en_US
dc.description.abstractThis study was carried out in Iztuzu Spit (IS, Mugla-SW Turkey), which is a special environmental protection zone due to the presence of a loggerhead turtle breeding area. The aims of this study are: (1) to determine surface sediment content, (2) to investigate the Iztuzu Spit spatial changes using Google-earth images, and (3) to figure out the controlling factors in the spit development. The main shore of the Iztuzu Spit is predominantly composed of medium-grained sands that contain dominantly ophiolitic rock fragments. Five types of ostracods, sixteen types of benthic foraminifera, gastropods, mollusc, and bivalve shell fragments were identified from the sediment sample taken from coastal part of the IS. The main coastal area of the Iztuzu Spit attached to mainland initially decreased from 67.4 ha (2004) to 56.8 ha (2013) then increased to 58.5 ha in 2016. Significant erosion of the main beach of Iztuzu Spit was observed in the north-western edge. A small coastal region separated from the Iztuzu Spit by the Dalyan river mouth shows significant change. The northern side of this region acted as a new sedimentation area, while the southern side was affected by erosion. The reason of these changes is variation in the flow direction of the Dalyan River mouth due to the building of piers in the lagoon side of the Iztuzu Spit. The main coastal part of the Iztuzu Spit has recently been under the effect of waves, tides, and summer tourism clients, while the river flow direction and anthropogenic effects are the main controlling mechanisms in the development of the NW edge. Therefore, the Iztuzu Spit must be monitored continuously and protected as this region is the breeding zone of the loggerhead turtle.en_US
dc.item-language.isoengen_US
dc.publisherPergamon-Elsevier Science Ltden_US
dc.item-rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectSpiten_US
dc.subjectBeach Sedimenten_US
dc.subjectAnthropogenic Factoren_US
dc.subjectLoggerhead Turtleen_US
dc.subject&Idoten_US
dc.subjectZtuzu-Dalyanen_US
dc.subjectSW Turkeyen_US
dc.titleCoastal geology of Iztuzu Spit (Dalyan, Mugla, SW Turkey)en_US
dc.item-typearticleen_US
dc.contributor.departmentMÜ, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümüen_US
dc.contributor.departmentTempGül, Murat
dc.contributor.institutionauthorGül, Murat
dc.contributor.institutionauthorSalihoğlu, Rana
dc.identifier.doi10.1016/j.jafrearsci.2018.12.017
dc.identifier.volume151en_US
dc.identifier.startpage173en_US
dc.identifier.endpage183en_US
dc.relation.journalJournal of African Earth Sciencesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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