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Chronology of the MIS 3 megafauna in southeastern West Siberia and the possibility of late survival of the Khozarian steppe mammoth (Mammuthus trogontherii chosaricus) A. V. Shpansky, Y. V. Kuzmin

By: Shpansky, Andrey VContributor(s): Kuzmin, Yaroslav VMaterial type: ArticleArticleContent type: Текст Media type: электронный Subject(s): хазарский степной мамонт | мегафауна | радиоуглерод | Западная СибирьGenre/Form: статьи в журналах Online resources: Click here to access online In: Radiocarbon Vol. 63, № 2. P. 575-584Abstract: We report a new series of radiocarbon (14C) dates on the MIS 3 megafauna for a previously poorly studied region of southeastern West Siberia. Some species, like woolly mammoth and woolly rhinoceros, and Pleistocene bison and horse, existed throughout the MIS 3 (ca. 29–59 ka cal BP); cave hyaena is dated to ca. 46,400 cal BP. The very late 14C dates on Khozarian steppe elephant (Mammuthus trogontherii chosaricus), ca. 45,100–45,400 cal BP, may indicate the survival of this species in Siberia up to MIS 3. More work is needed to confirm or reject this suggestion. Previously, Khozarian steppe elephant was known in Siberia only at the beginning of the Late Pleistocene (MIS 5e).
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Библиогр.: c. 582-584

We report a new series of radiocarbon (14C) dates on the MIS 3 megafauna for a previously poorly studied region of southeastern West Siberia. Some species, like woolly mammoth and woolly rhinoceros, and Pleistocene bison and horse, existed throughout the MIS 3 (ca. 29–59 ka cal BP); cave hyaena is dated to ca. 46,400 cal BP. The very late 14C dates on Khozarian steppe elephant (Mammuthus trogontherii chosaricus), ca. 45,100–45,400 cal BP, may indicate the survival of this species in Siberia up to MIS 3. More work is needed to confirm or reject this suggestion. Previously, Khozarian steppe elephant was known in Siberia only at the beginning of the Late Pleistocene (MIS 5e).

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