Dating of the hominid (Homo neanderthalensis) remains accumulation from El Sidrón cave (Piloña, Asturias, North Spain): an example of multi-methodological approach to the dating of Upper Pleistocene sites

6533b822fe1ef96bd127ceec

RESEARCH PRODUCT

Dating of the hominid (Homo neanderthalensis) remains accumulation from El Sidrón cave (Piloña, Asturias, North Spain): an example of multi-methodological approach to the dating of Upper Pleistocene sites

Ernestina Badal Vicente Soler Enrique Martínez Norbert Mercier Rainer Grün Ramon Julià Sergio Sanchez-moral M. De La Rasilla Antonio Rosas Javier Fortea David Santamaría Juan Carlos Cañaveras T. De Torres José E. Ortiz Nadine Tisnérat-laborde Carles Lalueza-fox Stephen Eggins Hélène Valladas Javier Lario

subject

010506 paleontology Archeology History Neanderthal Pleistocene 01 natural sciences Homo sapiens neanderthalensis Archaeological science law.invention 03 medical and health sciences Cave law biology.animal Amino acid dating Geología Radiocarbon dating 030304 developmental biology 0105 earth and related environmental sciences 0303 health sciences geography geography.geographical_feature_category Homo neanderthalensis biology Home de Neandertal Archaeology stomatognathic diseases Geology

description

The age of Neanderthal remains and associated sediments from El Sidrón cave has been obtained through different dating methods (14CAMS, U/TH, OSL, ESR and AAR) and samples (charcoal debris, bone, tooth dentine, stalagmitic flowstone, carbonate-rich sediments, sedimentary quartz grains, tooth enamel and land snail shells). Detrital Th contamination rendered Th/U dating analyses of flowstone unreliable. Recent 14C contamination produced spurious age-values from charcoal samples as well as from inadequately pretreated tooth samples. Most consistent 14C dates are grouped into two series: one between 35 and 40 ka and the other between 48 and 49 ka. Most ESR and AAR samples yielded concordant ages, ranging between 39 and 45 ka; OSL dating results permitted adequate bracketing of the sedimentary layer that contained the human remains. Our results emphasize the value of multi-dating approaches for the establishment of reliable chronologies of human remains. © University of Oxford, 2009.

year	journal	country	edition	language
2010-08-01

10.1111/arch.2010.52.issue-4/issuetoc https://oa.upm.es/4298/

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