Počet záznamů: 1  

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

  1. 1.
    SYSNO ASEP0438582
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevGeoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic
    Tvůrce(i) Lisá, Lenka (GLU-S) RID, SAI, ORCID
    Hošek, J. (CZ)
    Bajer, A. (CZ)
    Matys Grygar, Tomáš (UACH-T) RID, SAI, ORCID
    Vandenberghe, D. (BE)
    Zdroj.dok.Quaternary International. - : Elsevier - ISSN 1040-6182
    Roč. 351, 17 November 2014 (2014), s. 25-37
    Poč.str.13 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaregenerative-dose protocol ; Dolní Věstonice ; error limits ; record ; coversands ; community ; sequence ; paleosol ; impacts
    Vědní obor RIVAC - Archeologie, antropologie, etnologie
    Vědní obor RIV – spolupráceÚstav anorganické chemie
    Institucionální podporaGLU-S - RVO:67985831 ; UACH-T - RVO:61388980
    UT WOS000345521100004
    EID SCOPUS84884782507
    DOI10.1016/j.quaint.2013.08.058
    AnotaceThe 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.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2015
Počet záznamů: 1  

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