Geochemical Evidences of Paleoenvironmental Changes in Late Quaternary Lacustrine Sediments of the Konya Closed Basin (Konya, Turkey)

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dc.authoridSayin, Ulku/0000-0002-5098-1578
dc.authoridOZMEN, Ayhan/0000-0003-0370-9915
dc.authoridKaraaslan, Hulya/0000-0003-0045-7943
dc.contributor.authorOrhan, Hukmu
dc.contributor.authorDelikan, Arif
dc.contributor.authorDemir, Ahmet
dc.contributor.authorKapan, Sevinc
dc.contributor.authorOlgun, Kemal
dc.contributor.authorOzmen, Ayhan
dc.contributor.authorSayin, Ulku
dc.date.accessioned2025-01-27T20:29:06Z
dc.date.available2025-01-27T20:29:06Z
dc.date.issued2019
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description1st Springer Conference of the Arabian-Journal-of-Geosciences (CAJG) -- NOV 12-15, 2018 -- Hammamet, TUNISIA
dc.description.abstractImportant geochemical evidence reflecting Quaternary climatic changes was obtained by evaluating geochemical data from 51 samples and datings from 3 samples by ESR method from sediments of a 7-m-deep trench in Great Konya lake area at the southwest of Adakale village (Konya, Turkey). The geochemical data indicate that the study area was influenced, four times, by a climate having strong precipitation, which caused strong erosion and high detrital input between 25,276 +/- 1732-year BP and approximately 50,000-year BP. These periods correspond to climatic changes during the last glacial periods, the warm climate of D-O-2, D-O-5, D-O-6 and D-O-14 events and the cold climate of H2, H3, H4 or H5 and H6 events.
dc.description.sponsorshipArabian Journal Geosciences,Springer
dc.description.sponsorshipTUBITAK [114Y237]
dc.description.sponsorshipThis study was supported by the TUBITAK project no 114Y237.
dc.identifier.doi10.1007/978-3-030-01599-2_17
dc.identifier.endpage76
dc.identifier.isbn978-3-030-01599-2
dc.identifier.isbn978-3-030-01598-5
dc.identifier.issn2522-8714
dc.identifier.issn2522-8722
dc.identifier.scopus2-s2.0-85092471218
dc.identifier.scopusqualityQ2
dc.identifier.startpage73
dc.identifier.urihttps://doi.org/10.1007/978-3-030-01599-2_17
dc.identifier.urihttps://hdl.handle.net/20.500.12428/22822
dc.identifier.wosWOS:000623519900017
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer International Publishing Ag
dc.relation.ispartofPatterns and Mechanisms of Climate, Paleoclimate and Paleoenvironmental Changes From Low-Latitude Regions
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectKonya Closed Basin
dc.subjectQuaternary climate
dc.subjectGeochemical proxies
dc.subjectLast glacial maximum
dc.titleGeochemical Evidences of Paleoenvironmental Changes in Late Quaternary Lacustrine Sediments of the Konya Closed Basin (Konya, Turkey)
dc.typeConference Object

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