Barová (Sobolova) Cave, Moravian Karst (Czech Republic). Upper Pleistocene fosiliferous in-cave sediments, instructive paleontological excavations

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Barová (Sobolova) Cave, Moravian Karst (Czech Republic). Upper Pleistocene fosiliferous in-cave sediments, instructive paleontological excavations

Popis výsledku v původním jazyce

Since the discovery of Barová Cave in 1947, three periods of excavations in the inner part of the cave had been done until present, in context with both caving activities connecting distant parts of the cave and archeological/paleontological research projects proceeded within the cave entrance. Fossil bone remains of typical Upper Pleistocene fauna (Weischelian glaciation) were excavated, especially bone remains of the cave bear (Ursus ex gr. spelaeus). These activities followed by intensive speleological work led to the filling up all the entrance parts with huge slag deposits. Then the locality became unclear and taken as paleontologically completely excavated. As the consequence of the underlying sediments slide succession in the northwest part of the ?Shaft II?, new layers of bone rich sediments were opened in the basis of the old excavation sites and their surroundings. Subsequently, new restoration of old excavation sites was done, the terrain had been cleaned, newly topographica

Název v anglickém jazyce

Barová (Sobolova) Cave, Moravian Karst (Czech Republic). Upper Pleistocene fosiliferous in-cave sediments, instructive paleontological excavations

Popis výsledku anglicky

Since the discovery of Barová Cave in 1947, three periods of excavations in the inner part of the cave had been done until present, in context with both caving activities connecting distant parts of the cave and archeological/paleontological research projects proceeded within the cave entrance. Fossil bone remains of typical Upper Pleistocene fauna (Weischelian glaciation) were excavated, especially bone remains of the cave bear (Ursus ex gr. spelaeus). These activities followed by intensive speleological work led to the filling up all the entrance parts with huge slag deposits. Then the locality became unclear and taken as paleontologically completely excavated. As the consequence of the underlying sediments slide succession in the northwest part of the ?Shaft II?, new layers of bone rich sediments were opened in the basis of the old excavation sites and their surroundings. Subsequently, new restoration of old excavation sites was done, the terrain had been cleaned, newly topographica

Druh

D - Stať ve sborníku

CEP obor

AC - Archeologie, antropologie, etnologie

OECD FORD obor

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Projekt

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Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název statě ve sborníku

16th International congress of speleology

ISBN

978-80-87857-07-6

ISSN

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e-ISSN

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Počet stran výsledku

6

Strana od-do

133-138

Název nakladatele

Czech Speleological Society

Místo vydání

Praha

Místo konání akce

Brno

Datum konání akce

21. 7. 2013

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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