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Statements

Subject Item
n2:RIV%2F00094862%3A_____%2F14%3A%230001774%21RIV15-GA0-00094862
rdf:type
skos:Concept n4:Vysledek
rdfs:seeAlso
http://www.quartaer.eu/pdfs/2014/2014_08_nerudova.pdf
dcterms:description
The excavations in the Kůlna Cave yielded a quantity of archaeological finds dating from MIS 6 to MIS 2; these represent an extraordinary information potential for the reconstruction of human behaviour in the context of the natural environment from the Middle Pleistocene to the beginning of the Holocene. Apart from the reconstruction of human activities that were under way in the cave, e.g. through GIS applications, the researchers analysed the seasonality and migration of the preserved fauna. Through the study of dental cement increments of selected individuals we tried to ascertain the season when the animals died. The results show that at various periods of time the cave served different purposes; while during the Magdalenian (layer 5) it was occupied in spring, during the Upper Micoquian (layers 6a, 6b) it was a spring and autumn seasonal settlement, and during the Lower Micoquian (layer 7a) it was inhabited from autumn to spring. We propose that the function of the cave gradually changed from an overwintering location in the Lower Micoquian (layer 7a) to a seasonal settlement locality (Upper Micoquian, Magdalenian). Strontium analyses have shown that the majority of the studied animal individuals came from the nearby surrounding area of the cave, most likely the Moravian Karst area, with the exception of two animals with values from beyond the karst region. From this we deduce that not only Neanderthals, but later on also Anatomically Modern Humans took advantage of the location of the cave at the boundary between two different ecosystems, i.e. an open landscape and the karst area, in their hunting strategies. The humans who occupied the cave at different periods made use of different biotopes to provide themselves with supplies. The ratios of C and N isotopes correlate with changes in the character of the natural environment of archaeological layers 7a - 4 and render more precise the information previously acquired by malacological and other faunal analyses. The excavations in the Kůlna Cave yielded a quantity of archaeological finds dating from MIS 6 to MIS 2; these represent an extraordinary information potential for the reconstruction of human behaviour in the context of the natural environment from the Middle Pleistocene to the beginning of the Holocene. Apart from the reconstruction of human activities that were under way in the cave, e.g. through GIS applications, the researchers analysed the seasonality and migration of the preserved fauna. Through the study of dental cement increments of selected individuals we tried to ascertain the season when the animals died. The results show that at various periods of time the cave served different purposes; while during the Magdalenian (layer 5) it was occupied in spring, during the Upper Micoquian (layers 6a, 6b) it was a spring and autumn seasonal settlement, and during the Lower Micoquian (layer 7a) it was inhabited from autumn to spring. We propose that the function of the cave gradually changed from an overwintering location in the Lower Micoquian (layer 7a) to a seasonal settlement locality (Upper Micoquian, Magdalenian). Strontium analyses have shown that the majority of the studied animal individuals came from the nearby surrounding area of the cave, most likely the Moravian Karst area, with the exception of two animals with values from beyond the karst region. From this we deduce that not only Neanderthals, but later on also Anatomically Modern Humans took advantage of the location of the cave at the boundary between two different ecosystems, i.e. an open landscape and the karst area, in their hunting strategies. The humans who occupied the cave at different periods made use of different biotopes to provide themselves with supplies. The ratios of C and N isotopes correlate with changes in the character of the natural environment of archaeological layers 7a - 4 and render more precise the information previously acquired by malacological and other faunal analyses.
dcterms:title
Palaeoenvironmental analyses of animal remains from the Kůlna Cave (Moravian Karst, Czech Republic) Palaeoenvironmental analyses of animal remains from the Kůlna Cave (Moravian Karst, Czech Republic)
skos:prefLabel
Palaeoenvironmental analyses of animal remains from the Kůlna Cave (Moravian Karst, Czech Republic) Palaeoenvironmental analyses of animal remains from the Kůlna Cave (Moravian Karst, Czech Republic)
skos:notation
RIV/00094862:_____/14:#0001774!RIV15-GA0-00094862
n5:aktivita
n16:I n16:P
n5:aktivity
I, P(GAP405/11/0406)
n5:dodaniDat
n9:2015
n5:domaciTvurceVysledku
n18:1047329
n5:druhVysledku
n13:C
n5:duvernostUdaju
n6:S
n5:entitaPredkladatele
n21:predkladatel
n5:idSjednocenehoVysledku
35612
n5:idVysledku
RIV/00094862:_____/14:#0001774
n5:jazykVysledku
n11:eng
n5:klicovaSlova
Micoquian; Magdalenian; Epi-Magdalenian; 13C/12C; 15N/14N; 87Sr/86Sr; seasonality analyses
n5:klicoveSlovo
n7:87Sr%2F86Sr n7:Magdalenian n7:seasonality%20analyses n7:Epi-Magdalenian n7:13C%2F12C n7:15N%2F14N n7:Micoquian
n5:kontrolniKodProRIV
[0FC83CA58B15]
n5:mistoVydani
Leidorf
n5:nazevEdiceCisloSvazku
Quartär: Internationales Jahrbuch zur Eiszeitalter- und Steinzeitforschung; Band 61
n5:nazevZdroje
Quartär: Internationales Jahrbuch zur Eiszeitalter- und Steinzeitforschung
n5:obor
n20:AC
n5:pocetDomacichTvurcuVysledku
1
n5:pocetStranKnihy
198
n5:pocetTvurcuVysledku
3
n5:projekt
n17:GAP405%2F11%2F0406
n5:rokUplatneniVysledku
n9:2014
n5:tvurceVysledku
Míková, Jitka Nývltová-Fišáková, Miriam Nerudová, Zdeňka
s:numberOfPages
11
n14:doi
10.7485/QU61_08
n12:hasPublisher
Hugo Obermaier Society for Ice Age and Stone Age Research
n15:isbn
978-3-86757-927-8