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Soil erosion in relation to land-use changes in the sediments of Amik Lake near Antioch antique city during the last 4 kyr

dc.rights.licenseopenen_US
dc.contributor.authorEL OUAHABI, Meriam
dc.contributor.authorHUBERT-FERRARI, Aurélia
dc.contributor.authorLEBEAU, Héléne
dc.contributor.authorKARABACAK, Volkan
dc.contributor.authorVANDER AUWERA, Jacqueline
dc.contributor.authorLEPOINT, Gilles
dc.contributor.authorDEWITTE, Olivier
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.date.accessioned2024-05-29T11:22:24Z
dc.date.available2024-05-29T11:22:24Z
dc.date.issued2017-06-30
dc.identifier.issn0959-6836en_US
dc.identifier.urioai:crossref.org:10.1177/0959683617715702
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200130
dc.description.abstractEnThe Amik Basin in the Eastern Mediterranean region occupied since 6000–7000 BC has sustained a highly variable anthropic pressure culminating during the late Roman Period when the Antioch city reached its golden age. The present 6-m-long sedimentary record of the Amik Lake occupying the central part of the Basin constrains major paleoenvironmental changes over the past 4000 years using multi-proxy analyses (grain size, magnetic susceptibility, and x-ray fluorescence (XRF) geochemistry). An age model is provided by combining short-lived radionuclides with radiocarbon dating. A lake/marsh prevailed during the last 4 kyr with a level increase at the beginning of the Roman Period possibly related to optimum climatic condition and water channeling. The Bronze/Iron Ages are characterized by a strong terrigenous input linked to deforestation, exploitation of mineral resources, and the beginning of upland cultivation. The Bronze/Iron Age transition marked by the collapse of the Hittite Empire is clearly documented. Erosion continued during the Roman Period and nearly stopped during the early Islamic Period in conjunction with a decreasing population and soil depletion on the calcareous highland. The soil-stripped limestone outcrops triggered an increase in CaO in the lake water and a general decrease in ZrO2 released in the landscape that lasts until the present day. During the Islamic Period, pastoralism on the highland sustained continued soil erosion of the ophiolitic Amanus Mountains. The Modern Period is characterized by a higher pressure particularly on the Amanus Mountains linked to deforestation, road construction, ore exploitation, and drying of the lake for agriculture practices.
dc.language.isoENen_US
dc.sourcecrossref
dc.title.enSoil erosion in relation to land-use changes in the sediments of Amik Lake near Antioch antique city during the last 4 kyr
dc.typeArticle de revueen_US
dc.identifier.doi10.1177/0959683617715702en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalThe Holoceneen_US
bordeaux.page104-118en_US
bordeaux.volume28en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04592496
hal.version1
hal.date.transferred2024-05-29T11:22:26Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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