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The properties of buried soils reflect the paleoclimatic and ecological conditions of past eras. The study of these properties in pedo-chrono-sequences, the duration of functioning of which does not exceed several hundred years, allows reconstructing climate changes with the greatest possible accuracy for the studied period. The paleosols buried under burial mounds (kurgans) and surface soils were studied on the territory of the southeastern margin of the Russian Plain, in the Southern Cis-Urals (Orenburg region)....