Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/248
Full metadata record
DC FieldValueLanguage
dc.contributor.authorArnold, Lee J.-
dc.contributor.authorDemuro, Martina-
dc.date.accessioned2018-04-24T14:39:13Z-
dc.date.issued2015-10-
dc.identifier.citationQuaternary Geochronology, 2015, 30, Part B, 472–478es_ES
dc.identifier.issn1871-1014-
dc.identifier.issn1878-0350-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/248-
dc.description.abstractSingle-grain thermally transferred optically stimulated luminescence (TT-OSL) dating has recently been applied to a number of the Atapuerca palaeoanthropological sites. As yet, however, there have not been any direct assessments of TT-OSL signal stabilities for specific grains used for dating. In this study, we undertake a series of TT-OSL suitability assessments on known-age samples from Gran Dolina and Sima del Elefante. Our results suggest that the Atapuerca samples contain populations or sub-populations of grains with suitably stable TT-OSL signals for dating over late-Early and Middle Pleistocene timescales. Equivalent dose (De) distribution analysis in combination with pulse-annealing assessments provides a useful means of identifying inter-grain and inter-sample differences in TT-OSL signal stabilities. We also show that obtaining De values using different preheat conditions may help to identify potentially problematic TT-OSL behaviours. Analyses of multi-grain aliquot TL curves for these samples reveal that 'bulk' TL signal loss experiments may provide limited insights into TT-OSL source trap lifetimes due to averaging effects, the dominance of grain populations that do not produce TT-OSL, and interference from slowly bleaching OSL components. Our results improve the robustness and precision of existing TT-OSL chronologies for units TD6-3 and TE16-TE17 at Gran Dolina and Sima del Elefante, and support the broader suitability of the single-grain TT-OSL approach at the Atapuerca sites.es_ES
dc.description.sponsorshipFinancial support for this research was provided by Australian Research Council Future Fellowship project FT130100195, grant CGL2010-16821 from the Ministerio de Economía y Competitividad de España, and Marie Curie International Reintegration Grant PIRG08-GA-2010-276810.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectLuminescence datinges_ES
dc.subjectThermally transferred optically stimulated luminescence (TT-OSL)es_ES
dc.subjectSingle-graines_ES
dc.subjectAtapuercaes_ES
dc.subjectEarly Pleistocenees_ES
dc.titleInsights into TT-OSL signal stability from single-grain analyses of known-age deposits at Atapuerca, Spaines_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quageo.2015.02.005-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quageo.2015.02.005es_ES
dc.date.available2018-04-24T14:39:13Z-
Appears in Collections:Datación por Luminiscencia
Geocronología y Geología



This item is licensed under a Creative Commons License Creative Commons