Late Palaeolithic cave art and permafrost in the Southern Ural
Autor: | Yuri Dublyansky, Lawrence R. Edwards, Gabriella Koltai, Yuri Lyakhnitsky, Hai Cheng, Gina E. Moseley, Christoph Spötl, Denis Scholz |
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Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
Marine isotope stage
010506 paleontology lcsh:Medicine Hiatus 010502 geochemistry & geophysics Permafrost 01 natural sciences Article law.invention chemistry.chemical_compound Cave law Radiocarbon dating Stadial lcsh:Science 0105 earth and related environmental sciences Calcite geography Multidisciplinary geography.geographical_feature_category lcsh:R Archaeology Cave art chemistry lcsh:Q Geology |
Zdroj: | Scientific Reports, Vol 8, Iss 1, Pp 1-7 (2018) Scientific Reports |
ISSN: | 2045-2322 |
Popis: | Shulgan-Tash (also known as Kapova) cave located on the western slope of the Ural Mountains (Russia) is the easternmost European cave art monument of late Palaeolithic age. Radiocarbon dates from cultural layers in the cave suggest an age of about 16.3 to 19.6 ka (cal BP), but dates directly on the paintings were not obtained. In order to constrain the age of this art using an independent method, we performed detailed 230Th-U dating of calcite flowstone underlying and overgrowing the paintings at 22 sites in three halls of the cave. The youngest age for the underlying calcite (i.e., the maximum age of the cave art) is 36.4 ± 0.1 ka, and the oldest overlying calcite (constraining the minimum age of the cave art) is 14.5 ± 0.04 ka. The ca. 21.9 ka-long hiatus in calcite deposition during which the paintings were made is attributed to regional permafrost conditions and sub-zero temperatures inside the cave during Marine Isotope Stage (MIS) 2. This is supported by samples of cryogenic cave calcite, which document seven episodes of freezing and thawing of permafrost associated with stadials and interstadials of MIS 3, respectively. |
Databáze: | OpenAIRE |
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