Strontium and oxygen isotopes to trace mobility routes during the Bell Beaker period in the north of Spain
dc.contributor.author | Ortega Cuesta, Luis Ángel | |
dc.contributor.author | Alonso Fernández, Carmen | |
dc.contributor.author | Guede Sagastizabal, Iranzu Laura | |
dc.contributor.author | Zuluaga Ibargallartu, María Cruz | |
dc.contributor.author | Alonso Olazabal, Ainhoa | |
dc.contributor.author | Jiménez Echevarría, Javier | |
dc.date.accessioned | 2021-11-16T08:59:38Z | |
dc.date.available | 2021-11-16T08:59:38Z | |
dc.date.issued | 2021-10-01 | |
dc.identifier.citation | Scientific Reports 11(1) : (2021) // Article ID 19553 | es_ES |
dc.identifier.issn | 2045-2322 | |
dc.identifier.uri | http://hdl.handle.net/10810/53770 | |
dc.description.abstract | [EN]Strontium and oxygen isotopes of individuals from El Hundido and Valdescusa (north of Spain) sites, corresponding to the Bell Beaker culture, were analysed in order to determine mobility patterns and provenance areas. Strontium and oxygen isotope ratios in three teeth from two individuals at El Hundido and two teeth from the five individuals at Valdescusa were studied. The analyses were performed in both dentine and enamel fractions. Sr-87/Sr-86 ratios of El Hundido individuals indicate one was of foreign origin and the other was local whereas at Valdescusa were all of foreign provenance. Calculated delta O-18(w) values of El Hundido suggest a provenance from the geographical area close to the site while the Valdescusa would come from a warmer region. The comparison of oxygen and strontium isotope signatures indicate the west of the Iberian Peninsula (Zamora or the east of Leon regions) as the provenance area for the foreign individual at El Hundido and southwest France (Garonne basin) as the region of provenance for the Valdescusa. | es_ES |
dc.description.sponsorship | This work has been supported financially by Research Group IT1193-19 and PIBA 2018_1_0053 research projects of the Government of the Basque Country. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Nature Research | es_ES |
dc.rights | info:eu-repo/semantics/openAccess | es_ES |
dc.rights.uri | http://creativecommons.org/licenses/by/3.0/es/ | * |
dc.subject | element concentrations | es_ES |
dc.subject | bronze-age | es_ES |
dc.subject | bone | es_ES |
dc.subject | diagenesis | es_ES |
dc.subject | diet | es_ES |
dc.subject | reconstruction | es_ES |
dc.subject | France | es_ES |
dc.subject | ratios | es_ES |
dc.subject | carbon | es_ES |
dc.title | Strontium and oxygen isotopes to trace mobility routes during the Bell Beaker period in the north of Spain | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.holder | This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. | es_ES |
dc.rights.holder | Atribución 3.0 España | * |
dc.relation.publisherversion | https://www.nature.com/articles/s41598-021-99002-8 | es_ES |
dc.identifier.doi | 10.1038/s41598-021-99002-8 | |
dc.departamentoes | Geología | es_ES |
dc.departamentoeu | Geologia | es_ES |
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