Eolianite and coquinite as evidence of MIS 6 and 5, NW Black Sea coast, Turkey

Basit Öğe Kaydı
dc.authorid0000-0002-3112-5258
dc.authorid0000-0001-8704-4935
dc.authorid0000-0002-9834-7680
dc.authorid0000-0003-4966-1208
dc.authorid0000-0002-8710-6232
dc.authorid0000-0002-3331-8205
dc.authorid0000-0001-8598-8596
dc.authorid0000-0002-1090-7146
dc.authorid0000-0003-3772-3096
dc.contributor.authorErginal, Ahmet Evrenen_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.contributor.authorSelim, Hamit Haluken_US
dc.contributor.authorBozcu, Mustafaen_US
dc.contributor.authorÖztürk, Muhammed Zeynelen_US
dc.contributor.authorEkinci, Yunus Leventen_US
dc.contributor.authorDemirci, Alperen_US
dc.contributor.authorElmas, Elmas Kırcıen_US
dc.contributor.authorÖztürk, Tuğbaen_US
dc.contributor.authorÇakır, Çağlaren_US
dc.contributor.authorKarabıyıkoğlu, Mustafaen_US
dc.date.accessioned2017-03-13T10:50:03Z
dc.date.available2017-03-13T10:50:03Z
dc.date.issued2017-04
dc.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.description.abstractThis paper discusses the implications of a lowstand carbonate eolianite and overlying transgressive sequence of coquinite at Şile on the Turkish Black Sea coast based on composition, depositional characteristics and optical age estimations. The cross-bedded eolianite is a mixed ooid quartz grainstone in composition, yielding a depositional age matching MIS 6. It formed at the backshore of the paleobeach with the supply of sediment the from the beach face and offering insights into the drift of mixed shallow marine carbonates and siliciclastics together with radial ooids by onshore winds from a subaerially exposed high- to low-energy ooid shoals and oolitic sand complexes which developed parallel to the shoreline on the shallow shelf margin. During this lowstand, a low-relief dune retaining a record of opposing paleowind directions than that of prevalent northeasterly winds of today appears to have been lithified to form dune rock (aeolinite) under drier conditions compared to the present. Coinciding with MIS 5e, shallow marine coquina beds resting unconformably on the eolianite indicate the occurrence of the Mediterranean transgression during the last interglacial, as confirmed by benthic foraminifera within the high-salinity tolerant coquina shells.en_US
dc.description.versionPublisher's Versionen_US
dc.identifier.citationDemirci, A., Güneç Kıyak, N., Ekinci, Y. L., Öztürk, M. Z., Bozcu, M., Çakır, Ç., Öztürk, T. . . . & Karabıyıkoğlu, M. (2017). Eolianite and coquinite as evidence of MIS 6 and 5, NW black sea coast, turkey. Aeolian Research, 25, 1-9. doi:10.1016/j.aeolia.2017.01.004en_US
dc.identifier.doi10.1016/j.aeolia.2017.01.004
dc.identifier.endpage9
dc.identifier.issn1875-9637
dc.identifier.issn2212-1684
dc.identifier.scopus2-s2.0-85012066535
dc.identifier.scopusqualityQ1
dc.identifier.startpage1
dc.identifier.urihttps://hdl.handle.net/11729/1194
dc.identifier.urihttp://dx.doi.org/10.1016/j.aeolia.2017.01.004
dc.identifier.volume25
dc.identifier.wosWOS:000402214000001
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.indekslendigikaynakScience Citation Index Expanded (SCI-EXPANDED)en_US
dc.institutionauthorGüneç Kıyak, Nafiyeen_US
dc.institutionauthorÖztürk, Tuğbaen_US
dc.institutionauthorid0000-0001-8598-8596
dc.language.isoenen_US
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.publisherElsevier B.V.en_US
dc.relation.ispartofAeolian Researchen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBlack Seaen_US
dc.subjectCoquiniteen_US
dc.subjectEolianiteen_US
dc.subjectLate Pleistoceneen_US
dc.subjectSea levelen_US
dc.subjectTurkeyen_US
dc.subjectRegenerative-Dose protocolen_US
dc.subjectSingle-Aliquoten_US
dc.subjectCosmic-Rayen_US
dc.subjectLevelen_US
dc.subjectStratificationen_US
dc.subjectLuminescenceen_US
dc.subjectAeolianitesen_US
dc.subjectEvolutionen_US
dc.subjectEventsen_US
dc.titleEolianite and coquinite as evidence of MIS 6 and 5, NW Black Sea coast, Turkeyen_US
dc.typeArticleen_US
dspace.entity.typePublication

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