Локальная стратиграфия и палеоэкология стоянки поздней поры верхнего палеолита Дивногорье 1 в бассейне среднего Дона

Верхнепалеолитическая стоянка Дивногорье 1 расположена на низкой террасе реки Тихая Сосна, сложенной перигляциальным аллювием, который перекрыт пролювиально-делювиальными отложениями. В позднеледниковой толще фиксируются два уровня слабого педогенеза, два уровня мерзлотных и эрозионных нарушений, а также культурный слой стоянки с радиоуглеродным возрастом 13 800–13 300 л. н. Проведенные междисциплинарные геоархеологические исследования показали смену перигляциальной флювиальной обстановки субаэральной – вначале перигляциальной (в позднеледниковье), а затем межледниковой – лесостепной и периодически степной (в голоцене). Очень динамичный характер климата и ландшафтов был характерен для начала голоцена и особенно ярко выражен для позднего ледникового периода.

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