Exploring pre-neolithic environmental dynamics: paleoecology around the Göbekli Tepe based on a multiproxy approach in southeastern Türkiye

Paleoecological findings from soil samples recovered near the Göbekli Tepe indicate an environment that sustains a variety of multiproxy analyses, revealing prominent changes in ecological conditions.

Soil samples were collected in the vicinity of the pre-Neolithic site in the Göbekli Tepe. These sediment samples underwent comprehensive analysis utilizing a multiproxy approach, which included pollen analysis, total organic carbon (TOC) and total inorganic carbon (TOC) measurements, and X-ray fluorescence (XRF) elemental analysis.

Total organic carbon varied significantly in the SK-1 section, with lower levels at the bottom and higher levels at the top. The Ca/Ti ratio, which is indicative of weathering and moisture availability, typically increased in the early Holocene and briefly decreased at approximately 13,354 years BP. The Sr/Ti ratio, related to weathering and erosion processes, also suggests intensified weathering. The presence of deciduous forests and the increase in organic carbon values further support the notion of favorable environmental conditions during the early Holocene. In contrast, the lower levels of SK-1 show lower organic carbon values, lower Ca/Ti and Sr/Ti ratios, and greater abundances of herbaceous plants and steppes, indicating colder and drier conditions at 13,354 years BP.

A significant increase in organic carbon values and the presence of deciduous Quercus in the upper levels of the SK-3 section suggest a period of increased organic productivity and the existence of deciduous forests during the early Holocene at the Göbekli Tepe.