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
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
EH - Ecology - communities
OECD FORD branch
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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
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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
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