ESR Dating Ungulate Tooth Enamel from the Mousterian Layers at Pešturina, Serbia
Author(s): Gligor Dakovic; Bonnie A. B. Blackwell; Dušan Mihailovic; Mirjana Roksandic; Anne R. Skinner
Year: 2017
Summary
In southern Serbia, Pešturina contains three Mousterian layers, with late Pleistocene faunae. The site
overlooks a tributary to the Nišava River southwest of Niš near the Sičeva Gorge. In all three
sedimentological layers, the large mammalian faunae suggest a mixed environment with temperate forest,
rocky cliffs, and steppe within walking distance from the cave. Fragmentation patterns and butchering marks
plus the lithic tools indicate that some faunal remains were human kills. A depositional hiatus occurred
between Layers 4 and 3. From 14 ungulate teeth from the Mousterian layers, 50 enamel subsamples were
independently ESR dated. With < 0.1 ppm U in the enamel, and 1.0-3.5 ppm dentinal U, the ESR ages do not
depend on the U uptake rates used for the calculations. Nor does any potential Rn loss introduce any
uncertainty. To assess the external dose rates, bulk sediment samples and individual mineralogically distinct
components were analyzed by NAA, then volumetrically averaged, while time-averaged cosmic dose rates
were calculated using the ramped box method. At least two teeth had been reworked, likely associated with
the erosion event that removed part of Layer 4 before the deposition of Layer 3. ESR ages correlated with
Marine (Oxygen) Isotope Stages (MIS) 3-6.
Cite this Record
ESR Dating Ungulate Tooth Enamel from the Mousterian Layers at Pešturina, Serbia. Gligor Dakovic, Bonnie A. B. Blackwell, Dušan Mihailovic, Mirjana Roksandic, Anne R. Skinner. Presented at The 81st Annual Meeting of the Society for American Archaeology, Vancouver, British Columbia. 2017 ( tDAR id: 430392)
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Keywords
General
ESR dating; mammalian enamel; Charentian Mousterian; Denticulate Mousterian; Pešturina, Serbia.
Geographic Keywords
Europe
Spatial Coverage
min long: -11.074; min lat: 37.44 ; max long: 50.098; max lat: 70.845 ;
Record Identifiers
Abstract Id(s): 14979