Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/300
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dc.contributor.authorMoreno García, Davinia-
dc.contributor.authorFalguères, Christophe-
dc.contributor.authorPérez-González, Alfredo-
dc.contributor.authorVoinchet, Pierre-
dc.contributor.authorGhaleb, Bassam-
dc.contributor.authorDespriée, Jackie-
dc.contributor.authorSala, Robert-
dc.contributor.authorCarbonell, Eudald-
dc.contributor.authorBermúdez de Castro, José María-
dc.contributor.authorArsuaga, Juan Luis-
dc.date.accessioned2018-05-10T14:36:10Z-
dc.date.issued2015-10-
dc.identifier.citationQuaternary Geochronology, 2015, 30, Part B, 535-540es_ES
dc.identifier.issn1871-1014-
dc.identifier.issn1878-0350-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/300-
dc.description.abstractAges based on independent methods, such as combined ESR-U series, luminescence, and magnetostratigraphic analyses have been obtained for the upper stratigraphical section of Gran Dolina site (TD6 to TD11 levels). However, the chronostratigraphical framework of this European Paleolithic key site remains incomplete because of its great antiquity and the lack of reliable methods. This paper provides new radiometric dates by electron spin resonance applied to optically bleached quartz grains for the whole stratigraphic sequence. The results agree with the previous chronostratigraphical framework for the upper part of the stratigraphical sequence. The ages for the Homo antecessor remains from TD6 layer range between 800 and 900 ka. The lowest layers attributed to endogenous sediments (TD1) could be contemporaneous with the Sima del Elefante TE9 human bearing layer dated to 1.2 Ma. The results suggest a human occupation of possibly more than 1 Ma at the Gran Dolina site. This study confirms moreover the potential of ESR dating method applied on quartz in karstic environment.es_ES
dc.description.sponsorshipThis research has been funded by the Ministerio de Ciencia e Innovación Project (ref. CGL2006-13532-C03-01) and D. Moreno was beneficiary of an FPI grant from MICINN. The authors wish to thank T. Garcia and JM. Dolo (Commissariat à l’Energie Atomique, Paris, France) for the alanine irradiation, the Conseil Régional d'Ile-de-France for the assistance for the acquisition of a ESR EMX Bruker spectrometer and the Ministère de la Culture, sous-direction de l’Archéologie, Service Régional de l’Archéologie of the Region Centre (France) for the financial support and assistance for the acquisition of a portable gamma spectrometer.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.subjectGran Dolinaes_ES
dc.subjectAtapuercaes_ES
dc.subjectESR datinges_ES
dc.subjectBleached quartzes_ES
dc.subjectKarstic sedimentses_ES
dc.subjectPleistocenees_ES
dc.titleNew radiometric dates on the lowest stratigraphical section (TD1 to TD6) of Gran Dolina site (Atapuerca, Spain)es_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quageo.2015.05.007-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quageo.2015.05.007es_ES
dc.date.available2018-05-10T14:36:10Z-
Appears in Collections:Arqueología
Datación por Resonancia Paramagnética Electrónica
Geocronología y Geología
Paleobiología



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