PALAEOCLIMATE CHANGES IN THE AFYON PROVINCE, SW-TURKEY, DURING THE MIDDLE-LATE PLEISTOCENE: SIGNALS FROM CALCAREOUS TUFA POLLEN AND STABLE ISOTOPE RECORDS

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Published: 2021-10-20
Keywords:
Calcareous tufa, palynology, palaeoenvironment, palaeoclimate, Afyon, SW-Turkey

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Ezher Tagliasacchi
Pamukkale University, Geology Engineering Department, Kınıklı, Denizli, Turkey
Mine Sezgül Kayseri-Özer
Dokuz Eylul University, Institute of Marine Science and Technology, Haydar Aliyev Bul, İnciraltı-Izmir, Turkey

Abstract

The calcareous tufas of Sarıkavak located in the northern part of NE-SW trending Acıgöl Graben in SW-Turkey are investigated in detail. For this aim, various analyses (stable isotopes, U/Th dating, palynology) have been carried out on samples obtained from both outcrops and drilling logs in and surrounding Sarıkavak Village. U/Th dating shows that these carbonates precipitated from 400 ka up to 80 ka. Preliminary pollen data, document climatic variability between MIS 11 and MIS 8 in the studied area.

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Vol. 31 (2018): "Quaternary: Past, Present, Future - AIQUA Conference 2018"

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Articles
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How to Cite

Tagliasacchi, E., & Kayseri-Özer, M. S. (2021). PALAEOCLIMATE CHANGES IN THE AFYON PROVINCE, SW-TURKEY, DURING THE MIDDLE-LATE PLEISTOCENE: SIGNALS FROM CALCAREOUS TUFA POLLEN AND STABLE ISOTOPE RECORDS. Alpine and Mediterranean Quaternary, 31, 161-164. https://amq.aiqua.it/index.php/amq/article/view/208