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New information augmenting the picture of local environment at the LGM/LGT in the context of the Middle Danube region

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F16%3A43890968" target="_blank" >RIV/60076658:12310/16:43890968 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/16:00093834

  • Result on the web

    <a href="http://journals.sagepub.com/doi/abs/10.1177/0959683616640051" target="_blank" >http://journals.sagepub.com/doi/abs/10.1177/0959683616640051</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1177/0959683616640051" target="_blank" >10.1177/0959683616640051</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    New information augmenting the picture of local environment at the LGM/LGT in the context of the Middle Danube region

  • Original language description

    Records of occupation by humans in the period following shortly after the Last Glacial Maximum (LGM; 21 +/- 2 kyr cal. BP) are still very rare in Central Europe, since it is inferred that the extreme climatic conditions caused the decolonisation of previously settled areas. Our study focuses on the reconstruction of environmental conditions in the surroundings of the open-air Palaeolithic site, Brno-Styrice III, which falls within this period. The research concentrated on the study of malacological, pollen and anthracological samples to reconstruct the climate shortly after the LGM. C-14 dating places the chronostratigraphic position of the site more precisely at the end of the LGM, more specifically into Last Glacial Termination (LGT); analysis of chipped stone industry identifies the occupation with the Epigravettian settlement. The site represents a significant example of the recurrent habitation of a microclimatically favourable microregion near a watercourse in order to utilise available sources of livelihood. The results of the pollen, anthracological and malacological analyses documented a more or less treeless character of surrounding landscape. The vegetation was mostly formed by a mixture of shrub tundra and grassy loess steppe vegetation. Open woodland with birch, willow and bird cherry occurred in relatively moist river banks and the lower slopes of hills with more favourable microclimatic conditions. Malacological collection highlights the presence of cool temperate species (Pupilla loessica, Vallonia excentrica and Helicopsis striata). In the surroundings of the studied site, the pollen analysis provided a reconstruction of parkland forest-steppe vegetation (with lack of temperate deciduous trees) typical for a cold and dry climate.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    EH - Ecology - communities

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA13-11193S" target="_blank" >GA13-11193S: Holocene environmental dynamics in the Hornomoravský úval region: Key processes inducing the formation of recent landscape mosaic.</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2016

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Holocene

  • ISSN

    0959-6836

  • e-ISSN

  • Volume of the periodical

    26

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    10

  • Pages from-to

    1345-1354

  • UT code for WoS article

    000381283200001

  • EID of the result in the Scopus database