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dc.rights.licenseopenen_US
dc.contributor.authorKAMOUN, Mohamed
dc.contributor.authorZAIBI, Chahira
dc.contributor.authorLANGER, Martin R.
dc.contributor.authorKHADRAOUI, Afef
dc.contributor.authorBEN HAMAD, Asma
dc.contributor.authorBEN KHALIFA, Khaoula
dc.contributor.authorKHALIFA, Khaoula Ben
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCARBONEL, Pierre
dc.contributor.authorBEN YOUSSEF, Mohamed
dc.date.accessioned2024-04-03T08:20:00Z
dc.date.available2024-04-03T08:20:00Z
dc.date.issued2020-06-01
dc.identifier.issn0077-7749en_US
dc.identifier.urioai:crossref.org:10.1127/njgpa/2020/0897
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/189141
dc.description.abstractEnA multi-proxy approach to infer the environmental evolution and coastal dynamics was conducted on four sediment cores with the aim to decipher forcing factors shaping the coastline of Acholla (Tunisia) over the last 2000 years. The data recorded from palaeontological and sedimentological studies combined with 14C dating suggest a progression of four successive phases: (1) the first Holocene marine transgression (183 A.D.), overlying Upper Pleistocene marine sandstones, resulted in a brackish shallow-water coastal environment characterized by a mixture of lagoonal/estuarine, marine/brackish and marine/lagoonal ostracod assemblages with high species richness, (2) a high-energy event marked by the deposition of coarse bioclastic sands, rich in molluscs, charcoal particles and Tyrrhenian lithoclasts (towards 417 A.D.), (3) progradation of the coast (between 417 and 1577 A.D.), where longshore current drifts and a period of flooding/detrital input resulted in the build-up of a sandspit and the deposition of coastal sand bars, as indicated by increasing abundances of predominantly lagoonal/estuarine ostracods and molluscs. The natural sedimentation pattern was impacted by the construction of a Roman pier that accelerated the formation of the sandspit from 1577 A.D. onward (4), ultimately resulting in the complete closure of the lagoon as recorded by the expansion of saltmarshes containing a monospecific ostracod fauna (Cyprideis torosa).
dc.language.isoENen_US
dc.sourcecrossref
dc.subject.enOstracods
dc.subject.ensandspit
dc.subject.ensediment dynamics
dc.subject.enlagoon
dc.subject.enHolocene
dc.subject.ensea-level
dc.title.enEnvironmental evolution of the Acholla coast (Gulf of Gabes, Tunisia) during the past 2000 years as inferred from palaeontological and sedimentological proxies
dc.typeArticle de revueen_US
dc.identifier.doi10.1127/njgpa/2020/0897en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalNeues Jahrbuch für Geologie und Paläontologie - Abhandlungenen_US
bordeaux.page217-235en_US
bordeaux.volume296en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue3en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04530406
hal.version1
hal.date.transferred2024-04-03T08:20:02Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Neues%20Jahrbuch%20f%C3%BCr%20Geologie%20und%20Pal%C3%A4ontologie%20-%20Abhandlungen&rft.date=2020-06-01&rft.volume=296&rft.issue=3&rft.spage=217-235&rft.epage=217-235&rft.eissn=0077-7749&rft.issn=0077-7749&rft.au=KAMOUN,%20Mohamed&ZAIBI,%20Chahira&LANGER,%20Martin%20R.&KHADRAOUI,%20Afef&BEN%20HAMAD,%20Asma&rft.genre=article


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