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The acheulean of the upper Guadiana river basin (central Spain). Morphostratigraphic context and chronology

dc.contributor.authorSantonja, M.
dc.contributor.authorPérez-González, A.
dc.contributor.authorBaena, J.
dc.contributor.authorPanera, J.
dc.contributor.authorMéndez-Quintas, E.
dc.contributor.authorUribelarrea, D.
dc.contributor.authorDemuro, M.
dc.contributor.authorArnold, L.
dc.contributor.authorAbrunhosa, Ana
dc.contributor.authorRubio-Jara, S.
dc.date.accessioned2022-12-15T11:24:18Z
dc.date.available2022-12-15T11:24:18Z
dc.date.issued2022-08
dc.description.abstractIn the upper basin of the Guadiana River, especially in the sectors drained by its right-bank tributaries, the Bullaque and Becea rivers, important concentrations of Acheulean and Mousterian industries can be found in a superficial position. These industries have provided series containing tens of thousands of pieces. Deposits in stratigraphic position have also been identified, related to the fluvial terraces of the Guadiana and Jabalon rivers and some tributaries. Within the sector studied, in the province of Ciudad Real, the position of these deposits is related to alluvial fans developed on the slopes of the immediate reliefs. These fans, mainly composed of Lower and Middle Ordovician quartzite gravel, were eroded in their distal positions by the Bullaque and Becea rivers, forming very low terraces on which large concentrations of Acheulean and Mousterian lithic industry can be found. El Sotillo, the only known stratigraphic site in the area, was excavated in 2017-2019 and consists of several levels with Mousterian and Acheulean industry. We present the technological characteristics of the main Acheulean assemblage recognised at this site, for which numerical dates have been obtained placing its chronology in the second half of the Middle Pleistocene. The location of these sites, in surficial position and El Sotillo, allows us to recognise a territorial space with specific geographic characteristics and a very significant human impact.pt_PT
dc.description.sponsorshipGrant PGC 2018-093612-B-100
dc.description.sponsorshipMCIN/AEI/10.13039/501100011033
dc.description.sponsorshipSBPLY/17/180801/000018
dc.description.sponsorshipPID2019-103987GB-C33
dc.description.sponsorshipSBPLY/18/180801/000071
dc.description.sponsorshipSBPLY/19/180801/000006
dc.description.sponsorshipED481D-2022/023
dc.description.sponsorship2018-093612B-100
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.3389/feart.2022.912007pt_PT
dc.identifier.eissn2296-6463
dc.identifier.urihttp://hdl.handle.net/10400.1/18640
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherFrontiers Media SApt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectIberian Peninsulapt_PT
dc.subjectGuadiana basinpt_PT
dc.subjectLower Palaeolithicpt_PT
dc.subjectAcheuleanpt_PT
dc.subjectLithic technologypt_PT
dc.subjectMiddle Pleistocenept_PT
dc.subjectLuminescence datingpt_PT
dc.subjectPalaeo-landscapept_PT
dc.titleThe acheulean of the upper Guadiana river basin (central Spain). Morphostratigraphic context and chronologypt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.titleFrontiers in Earth Sciencept_PT
oaire.citation.volume10pt_PT
person.familyNameAbrunhosa
person.givenNameAna
person.identifier.ciencia-id4713-BBB4-BE73
person.identifier.orcid0000-0002-9720-2623
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationa78e90e5-fdde-4695-85b5-16d7aba3263a
relation.isAuthorOfPublication.latestForDiscoverya78e90e5-fdde-4695-85b5-16d7aba3263a

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