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Archaeology of the Pleistocene-Holocene transition in Portugal : Synthesis and prospects

2020Artigo científico Acesso aberto
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dc.contributor.authorGameiro, Cristina
dc.contributor.authorAubry, Thierry
dc.contributor.authorAlmeida, Francisco
dc.contributor.authorDimuccio, Luca
dc.contributor.authorGabriel, Sónia
dc.contributor.authorGaspar, Rita
dc.contributor.authorGomes, Sérgio
dc.contributor.authorValcarce, Ramón Fábregas
dc.contributor.authorFigueiredo, Sofia
dc.contributor.authorManzano, Carmen
dc.contributor.authorMarreiros, João
dc.contributor.authorOliveira, Cláudia
dc.contributor.authorSantos, André Tomás
dc.contributor.authorSilva, Maria João
dc.contributor.authorTereso, João Pedro
dc.contributor.authorXavier, Pedro
dc.date.accessioned2020-08-24T13:47:33Z
dc.date.available2020-08-24T13:47:33Z
dc.date.issued2020
dc.description.abstractThe Tardiglacial of Portugal has been associated with the Magdalenian culture and lithic industries characterized by tool miniaturization, a diversity of microlith types, and the absence of a intentional blade production. The technological characterization, the chronology and the phasing of the Portuguese Magdalenian have been defined based on data recovered from open-air sites of the Estremadura region (Central Portugal). This paper presents an overview of the research undertaken over the last twenty-five years, including results from research and preventive archaeology fieldwork outside this region, namely in the Côa, Sabor and Vouga Valleys (northern Portugal), as well as in the Guadiana Valley and Algarve regions (southern Portugal). Our chronological boundaries are the Greenland Stadial 2-1b and the 8.2 ka event, from Early Magdalenian to Early Mesolithic. Regarding vegetation, deciduous Quercus underwent expansion during the warm phases of the Tardiglacial and retracted during cold ones, when pines increased. After the Solutrean, the faunal assemblages show a decrease in the variability of the represented species and an increase in fish, birds, small mammals and rabbits (Oryctolagus cuniculus). Concerning the cultural sequence, the Middle Magdalenian remains uncharacterised. After the Upper Magdalenian, and thenceforward, the use of local raw materials and of cores-on-flakes (burin or carinated endscraper type) for bladelet production gradually increased. In terms of lithic armatures typology, a four-stage sequence can be discerned: 1) Upper Magdalenian with axial points rather than backed bladelets, quite common in previous phases; 2) Final Magdalenian with an increase in the diversity of armature types; 3) Azilian with geometric microliths, curved backed points (Azilian points) and Malaurie points, and 4) Early Mesolithic without retouched bladelet tools or at best a persistence of Azilian armature types. There were some changes in the Palaeolithic rock art of the Douro basin between phase 3 (Final Magdalenian) and phase 4 (Late Azilian): figurative animal representations give place to animal depictions characterized by their geometrical bodies, often filled-in, and red deer becomes the best-represented animal.pt_PT
dc.description.versioninfo:eu-repo/semantics/acceptedVersionpt_PT
dc.identifier.citationGameiro, C., Aubry, T., Almeida, F., Dimuccio, L., Gabriel, S., Gaspar, R., Gomes, S., Valcarce, R. F., Figueiredo, S., Manzano, C., Marreiros, J., Oliveira, C., Santos, A. T., Silva, M. J., Tereso, J. P., & Xavier, P. (2020). Archaeology of the Pleistocene-Holocene transition in Portugal: Synthesis and prospects. Quaternary International. doi: 10.1016/j.quaint.2020.03.018pt_PT
dc.identifier.doi10.1016/j.quaint.2020.03.018pt_PT
dc.identifier.urihttp://hdl.handle.net/10451/44237
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.relation.publisherversionhttps://www.sciencedirect.com/science/article/pii/S1040618220301038pt_PT
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/pt_PT
dc.subjectTardiglacialpt_PT
dc.subjectChronostratigraphypt_PT
dc.subjectPalaeoenvironmentpt_PT
dc.subjectLithic technologypt_PT
dc.subjectArtpt_PT
dc.titleArchaeology of the Pleistocene-Holocene transition in Portugal : Synthesis and prospectspt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.titleQuaternary Internationalpt_PT
person.familyNameGameiro Gonçalves
person.familyNameaubry
person.familyNameDimuccio
person.familyNameGabriel
person.familyNamePinto da Silva e Conceição Santos
person.familyNameTereso
person.givenNameCristina Maria
person.givenNamethierry
person.givenNameLuca Antonio
person.givenNameSónia
person.givenNameAndré Tomás
person.givenNameJoão
person.identifierF-3481-2013
person.identifier.ciencia-id0C12-6F51-8131
person.identifier.ciencia-id641B-2C54-561F
person.identifier.ciencia-id1B1C-D535-FD7F
person.identifier.ciencia-id371E-A140-146D
person.identifier.ciencia-id6917-91ED-3295
person.identifier.ciencia-id5811-814C-0E01
person.identifier.orcid0000-0003-3521-3594
person.identifier.orcid0000-0003-0071-3361
person.identifier.orcid0000-0002-3889-2492
person.identifier.orcid0000-0001-9457-8695
person.identifier.orcid0000-0001-9937-6523
person.identifier.orcid0000-0003-0871-8255
person.identifier.ridM-2381-2013
person.identifier.scopus-author-id15739577500
person.identifier.scopus-author-id36450290200
person.identifier.scopus-author-id55222024200
person.identifier.scopus-author-id26656227900
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
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