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

Kód výsledku v 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>

Nalezeny alternativní kódy

RIV/00216224:14310/16:00093834

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

—

Projekt

<a href="/cs/project/GA13-11193S" target="_blank" >GA13-11193S: Holocenní dynamika ekosystémů Hornomoravského úvalu jako klíč k poznání procesů, které ovlivnily tvorbu současné krajinné mozaiky</a><br>

Návaznosti

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

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název periodika

Holocene

ISSN

0959-6836

e-ISSN

—

Svazek periodika

26

Číslo periodika v rámci svazku

9

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

10

Strana od-do

1345-1354

Kód UT WoS článku

000381283200001

EID výsledku v databázi Scopus

—