Orhan, HukmuDelikan, ArifDemir, AhmetKapan, SevincOlgun, KemalOzmen, AyhanSayin, Ulku2025-01-272025-01-272019978-3-030-01599-2978-3-030-01598-52522-87142522-8722https://doi.org/10.1007/978-3-030-01599-2_17https://hdl.handle.net/20.500.12428/228221st Springer Conference of the Arabian-Journal-of-Geosciences (CAJG) -- NOV 12-15, 2018 -- Hammamet, TUNISIAImportant 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.eninfo:eu-repo/semantics/closedAccessKonya Closed BasinQuaternary climateGeochemical proxiesLast glacial maximumConference Object737610.1007/978-3-030-01599-2_17N/AWOS:0006235199000172-s2.0-85092471218Q2