Reconstruction of the Climate of the Medieval Epoch on the Basis of Soiland Geochemical Studies of Kurgans of the Srostki Culturein the South of Western Siberia
The environmental diversity of Altai region is of great interest for researchers. There are many monuments of cultural heritage in the region, which are still poorly studied by natural scientific methods. Paleosols and background soils of the large Srostki-I necropolis of the Early Medieval epoch have been examined by pedological and geochemical methods with the aim to trace changes in the soil properties over time and to apply these data for reconstruction of the paleoclimate. This kurgans group is located in Biysk district of the Altai region and, according to the radiocarbon method, dates back to 890 ± 105–975 ± 85 AD (calibration 1δ). Paleosols of the Medieval epoch are characterized by a weaker leaching of carbonates in the middle part of the profile, lower accumulation of biophilous elements (P, S, Co) in the upper horizons, and lower values of the weathering index Al<sub>2</sub>O<sub>3</sub>/(CaO + MgO + Na<sub>2</sub>O + K<sub>2</sub>O) in comparison with the background surface soils. Thus, in the period before the construction of the kurgans, these paleosols were formed under somewhat more arid climate in comparison with the present time. However, the similarity of these paleosols and background surface soils in their morphological properties, reconstructed humus content, and averaged values of weathering indices Al<sub>2</sub>O<sub>3</sub>/(CaO + MgO + Na<sub>2</sub>O + K<sub>2</sub>O) and Rb/Sr, as well as Mn/Sr, Mn/Al, and Mn/Fe indices characterizing the degree of biological activity attest to humidization of the paleoclimate during the period of construction of the kurgans. Among highly hazardous pollutants of the first toxicity class, the studied soils are enriched with As and Cd (in comparison with natural abundances of these elements in the lithosphere). In general, regional soils and parent materials are enriched in As, Ni, Zn, Ba, and Sn, though the concentrations of these heavy metals in the soil profiles remain below the corresponding maximum permissible concentrations. The accumulation of toxic substances under the impact of anthropogenic pollution in the profiles of studied soils does not exceed the permissible values. The concentrations of heavy metals in the background surface soils are no higher than those in the medieval paleosols. The application of GIS technology demonstrated that 21 settlements and 130 necropolises of the Srostki community (second half of the 8th–12th centuries AD) were localized on fertile soils of level areas near large lakes and rivers (the Ob, Katun, Biya, Aley, and other rivers) and within wide valleys at the confluence of small streams with them.