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Late Middle Pleistocene malacofauna of the Acheulean site of Valdocarros II, Jarama river valley, Madrid, Spain

dc.contributor.authorAparicio Alonso, María Teresa
dc.contributor.authorPanera Gallego, Joaquín
dc.contributor.authorRubio Jara, Susana
dc.contributor.authorUribelarrea Del Val, David
dc.contributor.authorPérez González, Alfredo José
dc.date.accessioned2023-06-18T00:07:01Z
dc.date.available2023-06-18T00:07:01Z
dc.date.issued2017
dc.description.abstracting to its geographical position relative to northwestern Europe, the Iberian Peninsula was a refuge for many species during periods of harsh environmental conditions in the Quaternary. Despite this, the Pleistocene history of non-marine molluscs in Spain has been scarcely addressed. In this study, we examine the malacofauna of Valdocarros II, a site within the Complex Terrace of Arganda in the Jarama river valley tributary of the Tagus River in central Spain. This large, minutely-excavated site consists of five flood sequences identified in five archaeological levels and has been dated to the late Middle Pleistocene (end MIS 8–beginning MIS 7). Specimens of twelve freshwater and eighteen land mollusc taxa were identified. The most abundant species observed was Xerotricha madritensis, a land snail endemic to the Iberian Peninsula that today inhabits exposed surfaces with scarce plant cover. The most abundant freshwater species found was Anisus spirorbis, which currently thrives in tributaries of the Jarama River. This malacofauna assemblage features different ecological components, though dry, open-ground terrestrial species predominate. A correspondence analysis of the most frequently appearing land animals and the archaeological levels revealed a slight separation of level 2 from the other levels, indicative of its mesophilous character. However, few differences among these levels were identified in three correspondence analyses performed on the land or freshwater species datasets. Our observations of the malacofauna assemblage of Valdocarros II indicate a site characterized by a temperate climate and open areas with riverside vegetation. Furthermore, we propose the assignment of this site to an interstadial given the observed malacofauna of the five levels.
dc.description.departmentDepto. de Prehistoria, Historia Antigua y Arqueología
dc.description.facultyFac. de Geografía e Historia
dc.description.refereedTRUE
dc.description.sponsorshipDirección General de Patrimonio Histórico
dc.description.sponsorshipDirección General de Investigación de la Comunidad de Madrid
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/70359
dc.identifier.doi10.1016/j.quaint.2018.04.011
dc.identifier.issn1040-6182
dc.identifier.officialurlhttps://doi.org/10.1016/j.quaint.2018.04.011
dc.identifier.urihttps://hdl.handle.net/20.500.14352/19274
dc.journal.titleQuaternary International
dc.language.isoeng
dc.page.final71
dc.page.initial64
dc.publisherElsevier
dc.relation.projectID(PR170/04-13244; PR42/05-14071; 1962/ 2006/00)
dc.relation.projectID(06/123/2003)
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.cdu902(460.27)
dc.subject.keywordCentral Spain
dc.subject.keywordFreshwater Mollusca fossils
dc.subject.keywordLand snail fossils
dc.subject.keywordJarama River
dc.subject.keywordMalacofauna
dc.subject.keywordPleistocene
dc.subject.ucmPrehistoria
dc.subject.unesco5504.05 Prehistoria
dc.titleLate Middle Pleistocene malacofauna of the Acheulean site of Valdocarros II, Jarama river valley, Madrid, Spain
dc.typejournal article
dc.volume.number520
dspace.entity.typePublication
relation.isAuthorOfPublicationa238bfd0-b5c1-4b5e-b81d-5ab3beee5526
relation.isAuthorOfPublication21120521-f3fb-45a0-9c00-aa26c0df93a7
relation.isAuthorOfPublication886f9834-0fc0-47bc-bbe9-aa4957e062dd
relation.isAuthorOfPublicationa928f5ad-f505-4a04-a6da-796bac5f18d0
relation.isAuthorOfPublication.latestForDiscovery21120521-f3fb-45a0-9c00-aa26c0df93a7

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