. "4"^^ . "RIV/00025798:_____/12:00000296!RIV13-MSM-00025798" . . . "Paleokarst or tectonics? B\u0159ezina, Vysok\u00E1 site, Moravian Karst"@en . "Paleokras nebo tektonika? B\u0159ezina-Vysok\u00E1, Moravsk\u00FD kras" . . "Nov\u00E1 lokalita spodno-st\u0159ednovis\u00E9sk\u00E9 trilobitov\u00E9, goniatitov\u00E9, m\u011Bk\u00FD\u0161\u00ED, radiolariov\u00E9 a dal\u0161\u00ED fauny spolu se stejn\u011B star\u00FDmi rostlinn\u00FDmi zbytky a ichnofosiliemi byla pops\u00E1na z b\u0159ezinsk\u00FDch b\u0159idlic zcela obklopen\u00FDch svrchnodevonsk\u00FDmi v\u00E1penci frasnu maco\u0161sk\u00E9ho souvrstv\u00ED. D\u0159\u00EDv\u011Bj\u0161\u00ED, sp\u00ED\u0161e tektonick\u00E9 vysv\u011Btlen\u00ED situace bylo nahrazeno modelem p\u0159edpokl\u00E1daj\u00EDc\u00EDm svrchnodevonsk\u00FD v\u00FDzdvih, exhumaci a krasov\u011Bn\u00ED b\u011Bhem famenu a tournai. Krasovou periodu ukon\u010Dila spodnovis\u00E9sk\u00E1 transgrese. \u010Clenit\u00FD, siln\u011B diversifikovan\u00FD paleokrasov\u00FD povrch nab\u00EDzel vhodn\u00E9 prost\u0159ed\u00ED v n\u011Bm\u017E prosperovala \u0161irok\u00E1 \u0161k\u00E1la organizm\u016F. Pozd\u011Bji, ve svrchn\u00EDm karbonu b\u011Bhem varisk\u00E9 orogeneze byly b\u0159idlice spolu s v\u00E1pencov\u00FDm podlo\u017E\u00EDm zvr\u00E1sn\u011Bny. B\u0159idlice b\u0159ezinsk\u00E9ho souvrstv\u00ED p\u0159edstavuj\u00ED inici\u00E1ln\u00ED st\u00E1dium siliciklastick\u00E9 kulmsk\u00E9 facie Drahansk\u00E9 vrchoviny. Nen\u00ED pochyb o tom, \u017Ee ve v\u00E1penc\u00EDch maco\u0161sk\u00E9ho souvrstv\u00ED m\u016F\u017Eeme o\u010Dek\u00E1vat mnoho podobn\u00FDch projev\u016F paleokrasov\u00E9ho v\u00FDvoje." . . "2"^^ . "Otava, Ji\u0159\u00ED" . "157622" . "Paleokras nebo tektonika? B\u0159ezina-Vysok\u00E1, Moravsk\u00FD kras"@cs . "Nov\u00E1 lokalita spodno-st\u0159ednovis\u00E9sk\u00E9 trilobitov\u00E9, goniatitov\u00E9, m\u011Bk\u00FD\u0161\u00ED, radiolariov\u00E9 a dal\u0161\u00ED fauny spolu se stejn\u011B star\u00FDmi rostlinn\u00FDmi zbytky a ichnofosiliemi byla pops\u00E1na z b\u0159ezinsk\u00FDch b\u0159idlic zcela obklopen\u00FDch svrchnodevonsk\u00FDmi v\u00E1penci frasnu maco\u0161sk\u00E9ho souvrstv\u00ED. D\u0159\u00EDv\u011Bj\u0161\u00ED, sp\u00ED\u0161e tektonick\u00E9 vysv\u011Btlen\u00ED situace bylo nahrazeno modelem p\u0159edpokl\u00E1daj\u00EDc\u00EDm svrchnodevonsk\u00FD v\u00FDzdvih, exhumaci a krasov\u011Bn\u00ED b\u011Bhem famenu a tournai. Krasovou periodu ukon\u010Dila spodnovis\u00E9sk\u00E1 transgrese. \u010Clenit\u00FD, siln\u011B diversifikovan\u00FD paleokrasov\u00FD povrch nab\u00EDzel vhodn\u00E9 prost\u0159ed\u00ED v n\u011Bm\u017E prosperovala \u0161irok\u00E1 \u0161k\u00E1la organizm\u016F. Pozd\u011Bji, ve svrchn\u00EDm karbonu b\u011Bhem varisk\u00E9 orogeneze byly b\u0159idlice spolu s v\u00E1pencov\u00FDm podlo\u017E\u00EDm zvr\u00E1sn\u011Bny. B\u0159idlice b\u0159ezinsk\u00E9ho souvrstv\u00ED p\u0159edstavuj\u00ED inici\u00E1ln\u00ED st\u00E1dium siliciklastick\u00E9 kulmsk\u00E9 facie Drahansk\u00E9 vrchoviny. Nen\u00ED pochyb o tom, \u017Ee ve v\u00E1penc\u00EDch maco\u0161sk\u00E9ho souvrstv\u00ED m\u016F\u017Eeme o\u010Dek\u00E1vat mnoho podobn\u00FDch projev\u016F paleokrasov\u00E9ho v\u00FDvoje."@cs . "2"^^ . . . "Paleokarst, Moravian Karst, tectonics, Macocha Formation, B\u0159ezina shales, trilobite fauna."@en . . "Paleokras nebo tektonika? B\u0159ezina-Vysok\u00E1, Moravsk\u00FD kras" . . . . "[675E45AEB165]" . . "A new locality of Lower \u2013 Middle Vis\u00E9an trilobite, goniatite, mollusca, radiolaria and other fauna, together with plant remnants and ichnofauna has been described from B\u0159ezina Shales outcrops totally surrounded with limestones of Upper Devonian, Frasnian age (Macocha Formation). Earlier, rather tectonic explanation of the situation has been replaced by a model suggesting Famenian \u2013 Tournaisian local uplift, exhumation and karstification. The karst period was finished with Lower Vis\u00E9an transgression. Diversified paleokarst surface offered a suitable environment for wide range of organisms. Later on, in Upper Carboniferous during the Variscan orogeny, the fossiliferous shales were folded and faulted together with the limestone bedrock. Pelites of the B\u0159ezina Formation represent initial stage of the Upper Vis\u00E9an siliciclastic Culmian facies of the Drahany Upland. There is no doubt that abundant similar occurences of paleokarst phenomena could be expected within Upper Devonian limestones of the Macocha formation."@en . . "Paleokras nebo tektonika? B\u0159ezina-Vysok\u00E1, Moravsk\u00FD kras"@cs . . "Paleokarst or tectonics? B\u0159ezina, Vysok\u00E1 site, Moravian Karst"@en . "RIV/00025798:_____/12:00000296" . . . "1212-1134" . "I" . "2012" . "\u010Cern\u00FD, Jan" . . "CZ - \u010Cesk\u00E1 republika" . "Zpr\u00E1vy Vlastiv\u011Bdn\u00E9ho muzea v Olomouci" . . "303" . .