Number of the records: 1  

Geoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic

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    SYSNO ASEP0438582
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleGeoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic
    Author(s) Lisá, Lenka (GLU-S) RID, SAI, ORCID
    Hošek, J. (CZ)
    Bajer, A. (CZ)
    Matys Grygar, Tomáš (UACH-T) RID, SAI, ORCID
    Vandenberghe, D. (BE)
    Source TitleQuaternary International. - : Elsevier - ISSN 1040-6182
    Roč. 351, 17 November 2014 (2014), s. 25-37
    Number of pages13 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsregenerative-dose protocol ; Dolní Věstonice ; error limits ; record ; coversands ; community ; sequence ; paleosol ; impacts
    Subject RIVAC - Archeology, Anthropology, Ethnology
    Subject RIV - cooperationInstitute of Inorganic Chemistry
    Institutional supportGLU-S - RVO:67985831 ; UACH-T - RVO:61388980
    UT WOS000345521100004
    EID SCOPUS84884782507
    DOI10.1016/j.quaint.2013.08.058
    AnnotationThe Middle and Upper Palaeolithic sites situated within the system of Moravian and South Silesian valleys are key localities for understanding the patterns of seasonal mobility that enabled humans to exploit the North European Plain, and a possibility to distinguish the importance of the weather and climate for their subsistence practises. Loess accumulations that have covered the best preserved open air Palaeolithic sites in Central Europe display the climatic record covering at least 30,000 years. The sedimentological, microstratigraphical and geochemical record of three studied Upper Palaeolithic loess sites show significant changes, documenting increased precipitation towards the north. A progressive coarsening of the loess deposits during the Upper Pleniglacial, contrasting with the progressive fining toward the North European glaciation was detected. This methodological approach explains more precisely the context of formation processes connected also with human activity within the corridor between the North European Plain and the Danube Basin, through which a wide range of organisms, including humans and their prey species, were channelled.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2015
Number of the records: 1  

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