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Initial findings reveal occupation dynamics in the Volga River Delta, suggesting fluctuations in Caspian Sea levels may have influenced settlement.
In this article, we present the first results from radiocarbon dating of the Kirakle-Tobe settlement located in the central part of the Volga River Delta, southern Russia. Archaeological artifacts and 14 C measurements on charcoal indicate three stages of settlement development on the Kirakle-Tobe knoll. The oldest 14 C age corresponds to the Late Sarmatian period—early 4th century CE. The abundance of archaeological artifacts associated with the 6th–8th centuries CE indicates a long period of occupation. The youngest 14 C age presumably corresponds to the Khazarian period (9th century CE). These results suggest dynamic human activity in the central part of the Volga River Delta during the Great Migration Period. These initial results can be used to verify the impact of fluctuations in the Caspian Sea level on the Volga River Delta during the Great Migration Period.
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Soloviev et al. (2025) studied this question.
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