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Seasonality, palaeoecology and migration of fauna from the Gravettian sites

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    0316132 - ARÚB 2009 PL eng A - Abstract
    Nývltová Fišáková, Miriam
    Seasonality, palaeoecology and migration of fauna from the Gravettian sites.
    [Sezonalita, paleoecologie a migrace fauny z gravettských lokalit.]
    Paleontological Conference /9./ - Abstracts. Varšava: Polish Academy of Sciences, Institute of Paleobiology, 2008 - (Pisera, A.; Bitner, M.; Halamski, A.). s. 63-64. ISBN 978-83-61236-01-6.
    [Paleontological Conference /9./. 10.10.2008-11.10.2008, Warszawa]
    R&D Projects: GA AV ČR KJB800010701
    Institutional research plan: CEZ:AV0Z80010507
    Keywords : Pleistocene * Geochemistry * migration * Gravettien * Seasonality
    Subject RIV: AC - Archeology, Anthropology, Ethnology

    The seasonality of the Gravettian sites could be studied by using the animal dental cement microstructures. Dolní Věstonice, Přerov-Předmostí and Moravany-Lopata II Gravettian sites were full-year settlements. The sites Jarošov, Spytihněv, Lubná I, Trenčianské Bohuslavice, Willendorf II (layer 8 and 9) and Krakow-Spadzista were on the other hand occupied only seasonally (from spring to autumn). Based on the strontium isotopes ratio it was find out that the large gregarious animals, such as reindeers or horses did not migrate in the north-south direction. Stable isotope values of the Palaeolithic animal bones showed the floral change close to the OIS 3-2 transition, when was the expansion of grass initiated, i.e. to the extension of tundra.

    Zvířecí kosti z gravtských lokalit byly podrobeny geochemickým analýzám a analýze přírůstku zubního cementu na kořenech zubů. Byla potvrzena hypotéza velkých celoročních sídlišť (Dolní Věstonice, Přerov-Předmostí and Moravany-Lopata II) a malých sezóních sídlišť (Jarošov, Spytihněv, Lubná I, Trenčianské Bohuslavice, Willendorf II (layer 8 and 9) and Krakow-Spadzista). Na základě geochemických analýz byla potvrzena migrace mamutů, ale vyvrácena migrace sobů. Ostatní analýzy ukázaly změny ve vegetaci na hranici OIS3 a OIS2.
    Permanent Link: http://hdl.handle.net/11104/0166145

     
     
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