Formation of Holocene paleosols in a relict sand dune sequence at Kıyıköy, Türkiye

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dc.authorid0000-0003-2024-0565
dc.authorid0000-0002-3112-5258
dc.authorid0000-0003-2837-5771
dc.authorid0000-0002-4273-9175
dc.contributor.authorErginal, Ahmet Evren
dc.contributor.authorBozcu, Mustafa
dc.contributor.authorYakupoglu, Nurettin
dc.contributor.authorAkbas, Abdullah
dc.contributor.authorKaya, Hakan
dc.contributor.authorTunc, Ismail Onur
dc.date.accessioned2026-02-03T12:03:22Z
dc.date.available2026-02-03T12:03:22Z
dc.date.issued2025
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThe paleoclimatic indicators from a relict dune and paleosol sequence observed south of K & imath;y & imath;k & ouml;y Port, NW T & uuml;rkiye, provide insights into the variable paleoclimatic conditions in the western Black Sea coastal zone over the last 4700 yrs BP. The relict dunepaleosol sequence consists of reddish-brown coarse sands with abundant shells and overlying paleosol. Radiocarbon dating of Donax trunculus shells collected from the lowest part of the relict dune revealed the onset of sand deposition 4689 +/- 123 yrs ago. The dark-colored paleosol layer, with an Rb/Sr ratio of 0.008, yielded an age of 287 +/- 32 yrs cal BP. These findings indicate that the paleosol developed around the 1700s, during one of the coldest phases of the Little Ice Age. This layer is followed by a brown-colored buried soil, indicating a short-lived humid and rainy period, as evidenced by an Rb/Sr ratio of 0.42.
dc.description.sponsorshipTUBITAK [112Y217]
dc.description.sponsorshipThis work was supported by TUBITAK (project number: 112Y217) . AEE would like to thank the Turkish Academy of Sciences for the support provided under the TUEBA-GEB & Idot;P program.
dc.identifier.doi10.55730/1300-0985.1976
dc.identifier.issn1300-0985
dc.identifier.issue4
dc.identifier.scopus2-s2.0-105007342841
dc.identifier.scopusqualityQ2
dc.identifier.trdizinid1333796
dc.identifier.urihttps://doi.org/10.55730/1300-0985.1976
dc.identifier.urihttps://search.trdizin.gov.tr/tr/yayin/detay/1333796
dc.identifier.urihttps://hdl.handle.net/20.500.12428/35055
dc.identifier.volume34
dc.identifier.wosWOS:001500660000007
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakTR-Dizin
dc.language.isoen
dc.publisherTubitak Scientific & Technological Research Council Turkey
dc.relation.ispartofTurkish Journal of Earth Sciences
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WOS_20260130
dc.subjectRelict dune
dc.subjectpaleosol
dc.subjectRb/Sr ratio
dc.subjectLittle Ice Age
dc.subjectpaleoclimate
dc.titleFormation of Holocene paleosols in a relict sand dune sequence at Kıyıköy, Türkiye
dc.typeArticle

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