Fluvial style change during the last glacial-interglacial transition in the middle Tisza valley (Hungary)

C. Kasse, S.J.P. Bohncke, J. Vandenberghe, G. Gabris

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    Sedimentary changes during the last ∼2500 years have been reconstructed from cored sedimentary records from the deltaic floodplain of the Lower Tagus Valley and the Tagus mudbelt on the continental shelf offshore Lisbon. We used a multi-proxy approach consisting of sedimentology, grainsize, pollen data and magnetic susceptibility. In the floodplain grainsize coarsened and sedimentation rate and magnetic susceptibility increased during the late Holocene due to an increased flooding frequency and/or intensity. On the Tagus shelf the mudbelt grainsize fined, together with a higher sedimentation rate and increased magnetic susceptibility. The fining grainsize is explained by an increased suspended sediment flux towards the shelf and subdued winnowing. Floodplain and shelf records were correlated by radiocarbon dating and changes in sediment characteristics. We identified four depositional phases (∼2300/∼1600/∼1100/∼670 cal BP) on the floodplain and the shelf. These are tentatively explained by land-use changes in the Tagus catchment. © 2009 The Geologists' Association.
    Original languageEnglish
    Pages (from-to)180-194
    JournalProceedings of the Geologists' Association
    Volume121
    Issue number2
    DOIs
    Publication statusPublished - 2010

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