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dc.rights.licenseopenen_US
dc.contributor.authorROBIN, Nicolas
dc.contributor.authorBILLY, Julie
dc.contributor.authorNICOLAE-LERMA, Alexandre
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
dc.contributor.authorHESP, Patrick A.
dc.contributor.authorROSEBERY, David
dc.contributor.authorFAUNY, Corentin
dc.contributor.authorDEPARIS, Jacques
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARIEU, Vincent
dc.contributor.authorBOUCHET, Cedric
dc.contributor.authorMIOT DA SILVA, Graziela
dc.date.accessioned2023-11-06T13:55:12Z
dc.date.available2023-11-06T13:55:12Z
dc.date.issued2022-12-25
dc.identifier.issn1096-9837en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/184627
dc.description.abstractEnThe vast majority of coastal dunes in Europe have been stabilized by increasing vegetation cover since the mid-20th century. However, some systems may experience a remobilization phase, generally occurring locally and further propagating alongshore, the drivers of which remain poorly documented. This study investigates the evolutionary paths (stabilization/destabilization/remobilization) from 1945 to 2020 of a 2 km-long modern coastal transgressive dunefield located in southwest France with a holistic approach (GPR profiles, aerial photographs and LiDAR topographic data). Results show a landward migration of the transgressive dune by approximately 233 ± 7.5 m, through two distinct stages of rapid landward migration from 10 to 23 m/yr (Stage I: 1949–1959 and Stage III: 2000–2021) separated by an approximately 40-year stage of slow to no migration, but with substantial windward slope deflation (Stage II). The onset of Stage II is due to the fixation of vegetation by human action between 1950 and 1959. The onset of Stage III is hypothesized to be driven by long and sustained upper backshore/dune toe erosion beginning in 1968 due to a massive shoal welding that locally disturbed the longshore drift. It induced a destabilization of the dune and erosion of the vegetation cover over some decades. A non-synchronization is therefore observed between the start of the perturbation (1968), then the migration (2000), in line with the hysteresis concept of Tsoar (2005). This study shows that almost all of the sedimentary volume of the 1945 dune has been remobilized by translation to shape the dune system in its current form. The 2.2 km dunefield has grown by approximately 673 000 ± 190 000 m3 during the 2005–2020 period. Among this volume, there is a new foredune that was built from 2005 between the upper beach and the transgressive dune (volume in 2020 of about 394 000 ± 68 000 m3).
dc.language.isoENen_US
dc.title.enNatural remobilization and historical evolution of a modern coastal transgressive dunefield
dc.typeArticle de revueen_US
dc.identifier.doi10.1002/esp.5535en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalEarth Surface Processes and Landformsen_US
bordeaux.volumen/aen_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issuen/aen_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Earth%20Surface%20Processes%20and%20Landforms&rft.date=2022-12-25&rft.volume=n/a&rft.issue=n/a&rft.eissn=1096-9837&rft.issn=1096-9837&rft.au=ROBIN,%20Nicolas&BILLY,%20Julie&NICOLAE-LERMA,%20Alexandre&CASTELLE,%20Bruno&HESP,%20Patrick%20A.&rft.genre=article


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