land Article Meta-Analysis of Geomorphodynamics in the Western Lower Bakırçay Plain (Aegean Region, Turkey) Fabian Becker 1,* , Daniel Knitter 2 , Moritz Nykamp 1 and Brigitta Schütt 1 1 Physical Geography, Department of Earth Sciences, Institute of Geographical Sciences, Freie Universität Berlin, 12043 Berlin, Germany;
[email protected] (M.N.);
[email protected] (B.S.) 2 Physical Geography I: Landscape Ecology and Geoinformatics, Institute of Geography, Faculty of Mathematics and Natural Sciences, Christian-Albrechts-Universität zu Kiel, 24098 Kiel, Germany;
[email protected] * Correspondence:
[email protected] Received: 17 August 2020; Accepted: 17 September 2020; Published: 22 September 2020 Abstract: The relation between human activities, climate variability, and geomorphodynamics in the Mediterranean region is widely discussed. For the western lower Bakırçay plain in the ancient Pergamon Micro-Region, geoarchaeological studies have shown changes in geomorphodynamics primarily on a site-basis. We reconstruct past geomorphodynamics in the area based on a meta-analysis of 108 14C-ages obtained from 25 sediment sequences mainly from colluvial and alluvial deposits by analyzing cumulative probability functions of the 14C-ages. Accounting for biases in the database, we applied different approaches and compared the empirical probability functions with simulated functions. Reconstructed geomorphodynamics in the western lower Bakırçay plain during the Holocene principally coincide with a trend of climate-driven sensitivity to erosion and population dynamics in the eastern Mediterranean, but are also related to the local settlement history. Our data analysis shows that transformations of the Pergamon Micro-Region between the Hellenistic and Roman Imperial times is contemporary to increasing geomorphodynamics that peak in Roman Imperial times.