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dc.contributor.author
Tribolo, Chantal  
dc.contributor.author
Mercier, Norbert  
dc.contributor.author
Dumottay, Charles  
dc.contributor.author
Cantin, Nadia  
dc.contributor.author
Banks, William E.  
dc.contributor.author
Stratford, Dominic  
dc.contributor.author
de la Peña, Paloma  
dc.contributor.author
Backwell, Lucinda Ruth  
dc.contributor.author
Wadley, Lyn  
dc.contributor.author
d'Errico, Francesco  
dc.date.available
2023-11-16T12:38:53Z  
dc.date.issued
2022-11  
dc.identifier.citation
Tribolo, Chantal; Mercier, Norbert; Dumottay, Charles; Cantin, Nadia; Banks, William E.; et al.; Luminescence dating at Border Cave: Attempts, questions, and new results; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 296; 107787; 11-2022; 1-17  
dc.identifier.issn
0277-3791  
dc.identifier.uri
http://hdl.handle.net/11336/218281  
dc.description.abstract
Border Cave hosts a rare Middle and Early Later Stone Age sequence of deposits that extends as far back as ca. 250 thousand years (ka). The site's chronology has been built mainly on Electron Spin Resonance (ESR) ages obtained from teeth, conducted at the end of the 1990s, and on radiocarbon dating for the more recent layers. In order to refine the sequence's chronology, several materials were selected for luminescence dating, including 34 siliceous lithic artefacts, and quartz and feldspar grains extracted from 10 sediment samples. Since the radioisotopic contents of the cave sediments are abundant in the volcaniclastic host rock (about 2% K, 10 ppm 232Th, 2 ppm 238U in the sediments) and the ages for the lower layers are over 40 ka, high (>150 Gy) equivalent doses (De) were expected for most samples. The saturated thermoluminescence (TL) signals of the lithic artefact samples suggested either that they had not been heated in the past, or that they were already too old to be dated. The presence in the sediments of 40–63 μm quartz grains dominated by the fast Optically Stimulated Luminescence (OSL) component and with apparent high D0 values (200–1000 Gy) suggested, a priori, that they could be appropriate for measuring high Des. However, a systematic drop of the De values for these high D0 grains was observed and could not be fully understood and corrected accordingly. The recently proposed pIT protocol, together with a global growth curve (GGC) approach, was applied to 63–80 μm feldspar grains extracted from the sediment samples. The data suggest that the IR225 signal was likely not fully bleached at the time of deposition. Nonetheless, two age estimates, assumed to bracket the target age, have been calculated for each sample. These estimates are consistent with the previous ESR ages and the ESR/C14-based Bayesian models. Further improvements can be considered in the future with the pIT - GGC method, which would allow both increased accuracy and precision.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Pergamon-Elsevier Science Ltd  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/  
dc.subject
Luminescence dating  
dc.subject
MIDDLE STONE AGE  
dc.subject
Border Cave  
dc.subject
Feldspar  
dc.subject.classification
Arqueología  
dc.subject.classification
Historia y Arqueología  
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HUMANIDADES  
dc.title
Luminescence dating at Border Cave: Attempts, questions, and new results  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2023-11-15T15:52:43Z  
dc.journal.volume
296  
dc.journal.number
107787  
dc.journal.pagination
1-17  
dc.journal.pais
Países Bajos  
dc.journal.ciudad
Amsterdam  
dc.description.fil
Fil: Tribolo, Chantal. Université Bordeaux Montaigne; Francia  
dc.description.fil
Fil: Mercier, Norbert. Université Bordeaux Montaigne; Francia  
dc.description.fil
Fil: Dumottay, Charles. Université Bordeaux Montaigne; Francia  
dc.description.fil
Fil: Cantin, Nadia. Université Bordeaux Montaigne; Francia  
dc.description.fil
Fil: Banks, William E.. Universite de Bordeaux; Francia. University Ks Natural History Museum; Sudáfrica  
dc.description.fil
Fil: Stratford, Dominic. University of the Witwatersrand; Sudáfrica  
dc.description.fil
Fil: de la Peña, Paloma. University of Cambridge; Estados Unidos. Universidad de Granada; España. University of the Witwatersrand; Sudáfrica  
dc.description.fil
Fil: Backwell, Lucinda Ruth. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Estudios Sociales. Universidad Nacional de Tucumán. Instituto Superior de Estudios Sociales; Argentina. University of the Witwatersrand; Sudáfrica  
dc.description.fil
Fil: Wadley, Lyn. University of the Witwatersrand; Sudáfrica  
dc.description.fil
Fil: d'Errico, Francesco. Universite de Bordeaux; Francia. University of Bergen; Noruega  
dc.journal.title
Quaternary Science Reviews  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.quascirev.2022.107787  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0277379122004188