OSL dating of the Middle Palaeolithic Hotel California site, Sierra de Atapuerca, north-central Spain

被引:83
|
作者
Arnold, Lee J. [1 ]
Demuro, Martina [1 ]
Navazo, Marta [1 ,2 ]
Benito-Calvo, Alfonso [1 ]
Perez-Gonzalez, Alfredo [1 ]
机构
[1] CENIEH, Ctr Nacl Invest Evoluc Humana, Burgos 09002, Spain
[2] Univ Burgos, Area Prehist, Burgos 09001, Spain
关键词
FINE-GRAINED QUARTZ; EL CASTILLO CAVE; SINGLE GRAINS; DOSE DISTRIBUTIONS; HUMAN OCCUPATION; MULTIPLE GRAINS; CHINESE LOESS; COSMIC-RAY; TT-OSL; LUMINESCENCE;
D O I
10.1111/j.1502-3885.2012.00262.x
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Arnold, L. J., Demuro, M., Navazo, M., Benito-Calvo, A. & Perez-Gonzalez, A. 2013 (April): OSL dating of the Middle Palaeolithic Hotel California site, Sierra de Atapuerca, north-central Spain. Boreas, Vol. 42, pp. 285-305. 10.1111/j.1502-3885.2012.00262.x. ISSN 0300-9483. In this study we present optically stimulated luminescence (OSL) dating results obtained at one of the most important open-air Middle Palaeolithic sites in the Sierra de Atapuerca foothills Hotel California. We also assess the possibility of obtaining extended-range OSL chronologies for a nearby Middle Pleistocene fluvial deposit using several novel methods, namely OSL dating of individual quartz supergrains', multi-grain aliquot thermally transferred OSL (TT-OSL) dating and the first application of a single-grain TT-OSL dating procedure. Four single-grain OSL ages constrain the Middle Palaeolithic occupation of Hotel California to between 71 +/- 6 and 48 +/- 3ka. The Hotel California single-grain equivalent dose (De) distributions are highly overdispersed and contain several dose populations, which are probably attributable to post-depositional sediment mixing, partial bleaching and intrinsic scatter. The reliability of multi-grain aliquot OSL dating is compromised by the complex underlying De dispersion affecting these samples, as well as by biasing multi-grain averaging effects. Extended-range OSL and TT-OSL chronologies for the nearby Pico River terrace are consistent with each other and with broad independent age control. These experimental approaches yield a weighted average age of 348 +/- 16ka for terrace TA9 of the Arlanzon River sequence. Our results highlight the benefits of comparing ages obtained using several OSL methodologies to improve the robustness of luminescence chronologies. They also demonstrate the potential that single-grain OSL techniques offer for establishing improved age constraints on the many other Middle Palaeolithic sites found at Atapuerca and elsewhere across north-central Spain.
引用
收藏
页码:285 / 305
页数:21
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