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dc.rights.licenseopenen_US
hal.structure.identifierInstitut national de recherches archéologiques préventives - Centre de recherches archéologiques de Bègles [Inrap, Bègles]
dc.contributor.authorBERTRAN, Pascal
hal.structure.identifierDurham University
hal.structure.identifierDepartment of Archaeology [Durham University]
dc.contributor.authorANDRIEUX, Eric
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLELEU, Sophie
IDREF: 104909641
hal.structure.identifierDe la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
dc.contributor.authorSICARD-DELAGE, Zoe
hal.structure.identifierLaboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
dc.contributor.authorOUCHAOU, Rachid
hal.structure.identifierMorphodynamique Continentale et Côtière [M2C]
dc.contributor.authorWEILL, Pierre
hal.structure.identifierUniversité de Lille
hal.structure.identifierLaboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
dc.contributor.authorREYNAUD, Jean-Yves
dc.date.accessioned2025-04-10T08:58:27Z
dc.date.available2025-04-10T08:58:27Z
dc.date.issued2024-10-29
dc.identifier.issn0169-555Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/206078
dc.description.abstractEnThe architecture and chronology of Late Pleistocene to Holocene alluvial deposits in the lower Garonne have been studied in details based on data (boreholes, trenches, ground-penetrating radar profiles, numerical dating) collected in quarries and during archaeological surveys. The preserved alluvial bodies, dated between ca. 38 ka and present, show that the river retained a meandering or anabranching pattern throughout this period, associated with the formation of lateral accretion packages and scroll bars in the convexity of meanders. Valley incision in connection to the LGM low sea level reached up to 19 m in the study area, and occurred between ca. 26 and 18 ka. Since ca. 18 ka, the lateral migration of meanders widened the plain without any significant incision of the Oligocene marl bedrock. The Early-Middle Holocene was characterized by the development of highly sinuous meanders, while sinuosity decreased in a late phase including the Little Ice Age. Comparison with other lowland European rivers shows that the persistence of a meandering or anabranching pattern during MIS 2 is not an isolated case. The documented examples are associated with rivers typified by low valley slope, or situated in southern regions unaffected by permafrost and characterized by dense vegetation. The latter conditions would not have led to a drastic change in river discharge and bedload transport during the Last Glacial, as was the case for more northerly rivers where braiding seems to have been common.
dc.language.isoENen_US
dc.subject.enfluvial morphology
dc.subject.enriver pattern
dc.subject.enGaronne
dc.subject.ensouthwest France
dc.subject.enLast Glacial
dc.subject.enHolocene
dc.title.enThe Late Pleistocene - Holocene meandering lower Garonne River, southwest France: Architecture of the valley fill and chronology, comparison with other European rivers
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.geomorph.2024.109469en_US
dc.subject.halPlanète et Univers [physics]en_US
bordeaux.journalGeomorphologyen_US
bordeaux.page109469en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04765395
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geomorphology&rft.date=2024-10-29&rft.spage=109469&rft.epage=109469&rft.eissn=0169-555X&rft.issn=0169-555X&rft.au=BERTRAN,%20Pascal&ANDRIEUX,%20Eric&LELEU,%20Sophie&SICARD-DELAGE,%20Zoe&OUCHAOU,%20Rachid&rft.genre=article


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