Chronology and environmental changes from a sediment core spanning the last 485 ka from Lake Acıgo<spacing diaeresis>l (SW Anatolia)
Creators
- 1. Mugla Sitki Kocman Univ, Dept Geol Engn, Mugla, Turkiye
- 2. Kutahya Dumlupinar Univ, Dept Geol Engn, Kutahya, Turkiye
- 3. ITU, Eurasia Inst Earth Sci, EMCOL, Ayazaga, Istanbul, Turkiye
- 4. Univ Quebec, GEOTOP, Montreal, PQ, Canada
- 5. Univ Portsmouth, Sch Environm Geog & Geosci, Portsmouth, England
- 6. Leibniz Inst Balt Sea Res IOW, Rostock, Germany
Description
This study details the construction of an age-depth model for the uppermost 128 m of the 600 m long Ac & imath;gol2009-B03 sediment core, retrieved from the hypersaline Lake Ac & imath;gol in southwestern Anatolia. The model aligns the arboreal pollen record from Ac & imath;gol2009-B03 with the LR04 benthic delta 18O stack marine oxygen isotope record. Initial correlation was achieved using the Dynamic Time Warping algorithm, which was subsequently refined through manual tuning and finalized with Bayesian age-depth modeling to enhance precision and report the associated uncertainty levels. The model's accuracy incorporates multiple chronological constraints, including three radiocarbon dates, three U/Th dates, and the Kos Plateau Tuff, dated at 161.3 +/- 0.1 ka. According to this model, the upper 128 m of the Ac & imath;gol2009-B03 sequence spans approximately the last 485,000 years, encompassing Marine Isotope Stages (MIS) 1-12 and part of MIS 13. Our model serves as an update to the previously published, linearly constructed, age model as being used more anchor points and an efficient algorithm for similarity measurements which lies on a robust statistical foundation. In this period, arboreal pollen data suggest increasing (decreasing) arboreal vegetation input during interglacial (glacial) periods.
Files
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