. "Kraft, P." . . "Graptolitov\u00E1 spole\u010Denstva a stratigrafie spodn\u00EDho siluru mr\u00E1kot\u00EDnsk\u00E9ho souvrstv\u00ED v hlinsk\u00E9 z\u00F3n\u011B, SV \u010D\u00E1st \u010Cesk\u00E9ho mas\u00EDvu (\u010Cesk\u00E1 republika)"@cs . "2"^^ . "RIV/67985831:_____/09:00324021" . "1"^^ . . "Graptolitov\u00E1 spole\u010Denstva a stratigrafie spodn\u00EDho siluru mr\u00E1kot\u00EDnsk\u00E9ho souvrstv\u00ED v hlinsk\u00E9 z\u00F3n\u011B, SV \u010D\u00E1st \u010Cesk\u00E9ho mas\u00EDvu (\u010Cesk\u00E1 republika)"@cs . . . . "1214-1119" . . "24"^^ . . . . "Graptolite assemblages and stratigraphy of the lower Silurian Mr\u00E1kot\u00EDn Formation, Hlinsko Zone, NE interior of the Bohemian Massif (Czech Republic)" . . "\u010Ctrn\u00E1ct graptolitov\u00FDch bioz\u00F3n zn\u00E1m\u00FDch z oblasti Barrandienu bylo identifikov\u00E1no v siln\u011B tektonizovan\u00E9m, kontaktn\u011B metamorfovan\u00E9m a nedostate\u010Dn\u011B odkryt\u00E9m vrstevn\u00EDm sledu \u010Dern\u00FDch b\u0159idlic a silicit\u016F mr\u00E1kot\u00EDnsk\u00E9ho sozvrstv\u00ED hlinsk\u00E9 z\u00F3ny. Graptolitov\u00FD mater\u00ED\u00E1l byl z\u00EDsk\u00E1n p\u0159ev\u00E1\u017En\u011B z izolovan\u00FDch blok\u016F z nich\u017E ka\u017Ed\u00FD p\u0159edstavoval jeden objemov\u00FD vzorek. Na z\u00E1klad\u011B korelace s vrstevn\u00EDmi sledy Barrandienu a Durynska s bohat\u00FDmi a dob\u0159e datovan\u00FDmi graptolitov\u00FDmi faunami byl z izolovan\u00FDch blok\u016F a ojedin\u011Bl\u00FDch v\u00FDchoz\u016F zrekonstruov\u00E1n vrstevn\u00ED sled a litologick\u00FD v\u00FDvoj mr\u00E1kot\u00EDnsk\u00E9ho souvrstv\u00ED. Bylo zji\u0161t\u011Bno 112 druh\u016F graptolit\u016F a pops\u00E1n nov\u00FD druh Pseudorthograptus finneyi sp. nov. Mezi graptolitov\u00FDmi faunami hlinsk\u00E9 z\u00F3ny a Barrandienu jsou mal\u00E9 rozd\u00EDly, ale litologick\u00FD v\u00FDvoj je odli\u0161n\u00FD. V hlinsk\u00E9 z\u00F3n\u011B je cel\u00E9 llandovery vyvinuto v podob\u011B \u010Dern\u00FDch b\u0159idlic a silicit\u016F kter\u00E9 se z\u0159ejm\u011B ukl\u00E1daly v prost\u0159ed\u00ED bl\u00EDzk\u00E9m stejn\u011B star\u00FDm souvrstv\u00EDm sasko-durynsk\u00E9 oblasti a Z\u00E1padn\u00EDch Sudet."@cs . "Graptolite assemblages and stratigraphy of the lower Silurian Mr\u00E1kot\u00EDn Formation, Hlinsko Zone, NE interior of the Bohemian Massif (Czech Republic)"@en . "P(IAA3013405), Z(AV0Z30130516)" . "Fourteen of the graptolite biozones, previously recognised in the Llandovery succession of the Barrandian area of central Bohemia, have been identified in the heavily tectonized and poorly exposed, epizonal and contact metamorphic black slates and silicites of the Mr\u00E1kot\u00EDn Formation of the Hlinsko Zone. Graptolites were collected by bulk sampling of loose boulders. The sedimentary succession of the Mr\u00E1kot\u00EDn Formation has been reconstructed, in particular by detailed correlation with the biostratigraphically well dated, graptolite-rich successions in the Barrandian area and Thuringia. 112 graptolite species have been recorded, Pseudorthograptus finneyi sp. nov. was described. There is little difference between the graptolite faunas of the Hlinsko Zone and the Barrandian area, but the lithological successions of the two areas differ. Mr\u00E1kot\u00EDn Formation was deposited near the depositional site of the coeval formations of Saxo-Thuringia and West Sudetes, rather than near the Barrandian area." . . . "\u0160torch, Petr" . "316663" . . "Bulletin of Geosciences" . "[5DF7B84DE203]" . "graptolites; stratigraphy; Llandovery; Hlinsko Zone; Bohemian Massif"@en . "1" . . "CZ - \u010Cesk\u00E1 republika" . "RIV/67985831:_____/09:00324021!RIV09-AV0-67985831" . . "Graptolite assemblages and stratigraphy of the lower Silurian Mr\u00E1kot\u00EDn Formation, Hlinsko Zone, NE interior of the Bohemian Massif (Czech Republic)"@en . "Graptolite assemblages and stratigraphy of the lower Silurian Mr\u00E1kot\u00EDn Formation, Hlinsko Zone, NE interior of the Bohemian Massif (Czech Republic)" . . . . "84" . "Fourteen of the graptolite biozones, previously recognised in the Llandovery succession of the Barrandian area of central Bohemia, have been identified in the heavily tectonized and poorly exposed, epizonal and contact metamorphic black slates and silicites of the Mr\u00E1kot\u00EDn Formation of the Hlinsko Zone. Graptolites were collected by bulk sampling of loose boulders. The sedimentary succession of the Mr\u00E1kot\u00EDn Formation has been reconstructed, in particular by detailed correlation with the biostratigraphically well dated, graptolite-rich successions in the Barrandian area and Thuringia. 112 graptolite species have been recorded, Pseudorthograptus finneyi sp. nov. was described. There is little difference between the graptolite faunas of the Hlinsko Zone and the Barrandian area, but the lithological successions of the two areas differ. Mr\u00E1kot\u00EDn Formation was deposited near the depositional site of the coeval formations of Saxo-Thuringia and West Sudetes, rather than near the Barrandian area."@en .