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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10284165%21RIV15-MSM-11310___
rdf:type
skos:Concept n20:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.1016/j.quaint.2013.08.058
dcterms:description
The 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. The 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.
dcterms:title
Geoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic Geoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic
skos:prefLabel
Geoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic Geoarchaeology of Upper Palaeolithic loess sites located within a transect through Moravian valleys, Czech Republic
skos:notation
RIV/00216208:11310/14:10284165!RIV15-MSM-11310___
n3:aktivita
n15:I n15:P
n3:aktivity
I, P(EE2.4.31.0032)
n3:cisloPeriodika
11
n3:dodaniDat
n7:2015
n3:domaciTvurceVysledku
n17:5189063
n3:druhVysledku
n12:J
n3:duvernostUdaju
n19:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
18187
n3:idVysledku
RIV/00216208:11310/14:10284165
n3:jazykVysledku
n13:eng
n3:klicovaSlova
Czech republic; Central Europe; precipitation; geochemistry; microstratigraphy; sedimentology; Upper Palaeolithic loess
n3:klicoveSlovo
n5:Czech%20republic n5:precipitation n5:Upper%20Palaeolithic%20loess n5:sedimentology n5:microstratigraphy n5:Central%20Europe n5:geochemistry
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[0D2B2666678B]
n3:nazevZdroje
Quaternary International
n3:obor
n18:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:projekt
n10:EE2.4.31.0032
n3:rokUplatneniVysledku
n7:2014
n3:svazekPeriodika
351
n3:tvurceVysledku
Matys Grygar, T. Vandenberghe, D. Bajer, A. Hošek, Jan Lisá, Lenka
n3:wos
000345521100004
s:issn
1040-6182
s:numberOfPages
13
n6:doi
10.1016/j.quaint.2013.08.058
n16:organizacniJednotka
11310