Utilize este identificador para referenciar este registo: http://hdl.handle.net/10451/25686
Título: Distribution and chronological framework for Iberian variscite mining and consumption at Pico Centeno, Encinasola, Spain
Autor: Odriozola, Carlos P.
Villalobos García, Rodrigo
Burbidge, Christopher I.
Boaventura, Rui
Sousa, Ana Catarina
Rodríguez-Ariza, Oliva
Parrilla-Giraldez, Rubén
Prudêncio, M. Isabel
Dias, Maria Isabel
Palavras-chave: Variscite
Mining
OSL
14C-AMS
Iberia
Pico Centeno
Data: 8-Jan-2016
Editora: Elsevier
Citação: ODRIOZOLA, C. P.; VILLALOBOS GARCÍA; R.; BURBIDGE, C. I.; BOAVENTURA, R.; SOUSA. A. C.; RODRÍGUEZ-ARIZA, O.; PARRILLA-GIRALDEZ, R.; PRUDÊNCIO, M. I.; DIAS, M. I. (2016) - Distribution and chronological framework for Iberian variscite mining and consumption at Pico Centeno, Encinasola, Spain. Quaternary Research, 85, p. 159–176
Resumo: AMS radiocarbon and OSL dating, and profiling were used to directly delimit periods of variscite production at Pico CentenoMine 2. These resultswere integratedwith analysis of otherwell-dated periods of variscite production to establish an Iberian-wide chronological framework. Variscite production at Pico Centeno Mine 2 began at ~5200 BC, coincident with alpine jade production or Casa Montero Iberian flint production. Variscite was only used occasionally, together with other greenstones, during the 5th and 6th millennia BC. During the 4thmillenniumBC, variscite use began to increase to its apogee in the first half of 3rd millenniumBC when it appeared in nearly every Iberian burial site. This increase in variscite production and use coincided with decline in the popularity of alpine jade. By the end of the 3rd millennium BC, new resources began to be valued such as Asian and African Ivory, Baltic and Sicilian amber, and copper-based metal products. The variscite cycle thus started with the decline of jade in the 5th–4th millennium BC, and ended with the appearance of copper, ivory and extra-peninsular amber by the end of the 3rd millennium BC.
Peer review: yes
URI: http://hdl.handle.net/10451/25686
DOI: http://dx.doi.org/10.1016/j.yqres.2015.11.010
ISSN: 0033-5894
Versão do Editor: http://www.sciencedirect.com/science/article/pii/S0033589415001222
Aparece nas colecções:UNIARQ - Artigos em Revistas Internacionais

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