Late Holocene environment and climatic changes in Ameralik Fjord, Southwest Greenland - evidence from the sedimentary record.

H.S. Møller, K.G. Jensen, A. Kuijpers, S. Aagaard-Sørensen, M.-S. Seiedenkranz, M.A. Prins, R. Endler, N. Mikkelsen

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    Sedimentological and geochemical (XRF) data together with information from diatom and benthic foraminiferal records of a 3.5 m long gravity core from Ameralik Fjord, southern West Greenland, is used for reconstructing late-Holocene environmental changes in this area. The changes are linked to large-scale North Atlantic ocean and climate variability. AMS
    Original languageEnglish
    Pages (from-to)685-695
    JournalThe Holocene
    Volume16
    Issue number5
    DOIs
    Publication statusPublished - 2006

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