. "Biostratigraphic evaluation of the Flysch Western Carpathians and Carpathian Foredeep according to study of calcareous nannoplankton has been performed for the geological map-sheet 24-431 \u0160lapanice. Sediments were sampled from the isolated localities during the geological research and mapping. The relative age of the flysch deposits was stated from the upper Middle Eocene up to the Oligocene-Miocene boundary within the zone interval NP16\u2013NN1. Sediments provided stratigraphic nannoplankton markers Cribrocentrum reticulatum, Isthmolithus recurvus, Chiasmolithus oamaruensis, Ch. altus, Pontosphaera enormis, Cyclicargolihus abisectus and Helicosphaera carteri. The cooling in the uppermost Eocene is marked by the occurrence of large and broadly elliptical placoliths of Reticulofenstra umbilicus and by the absence of discoasterids. The sea-level fluctuation and the specific development of depocentre during the Oligocene are reflected in the quantitative rise in genus Pontosphaera and by the bloom of Dictyococcites bisectus and Cyclicargolithus abisectus in its upper part. The Lower Miocene, NN1\u2013NN4 zone interval is characterized by the poor autochthonous nannofossil record. Shallow epicontinental sea enabled the development to genus Helicosphaera (H. carteri, H. ampliaperta, H. mediterranea), small specimens of genus Reticulofenestra and in its upper part by the occurrence of Sphenolithus heteromorphus. The Middle Miocene marine ingression is reflected by the nannoflora input. The lower part of zone NN5 is delimitated by the short horizon with Helicosphaera waltrans. The overlying strata are usually rich in nannoflora with high numbers of Helicosphaera vedderi and Coccolithus sp."@en . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F karpatsk\u00E9 p\u0159edhlubn\u011B a fly\u0161ov\u00E9ho p\u00E1sma Z\u00E1padn\u00EDch Karpat v okol\u00ED \u0160lapanic na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED" . . . "Western Carpathians, Carpathian Foredeep, Paleogene, Neogene, calcareous nannofossils, biostratigraphy"@en . . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F fly\u0161e Z\u00E1padn\u00EDch Karpat a karpatsk\u00E9 p\u0159edhlubn\u011B na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED bylo p\u0159ipraveno pro sestaven\u00ED geologick\u00E9 mapy 24-431 \u0160lapanice. Vzorky byly z\u00EDsk\u00E1ny z izolovan\u00FDch odb\u011Br\u016F a z m\u011Blk\u00FDch vrt\u016F p\u0159i geologick\u00E9ho v\u00FDzkumu a mapov\u00E1n\u00ED. Relativn\u00ED st\u00E1\u0159\u00ED fly\u0161e bylo stanoveno v intervalu od svrchn\u00ED \u010D\u00E1sti st\u0159edn\u00EDho eoc\u00E9nu a\u017E po hranici oligoc\u00E9n-mioc\u00E9n, z\u00F3ny NP16-NN1 na z\u00E1klad\u011B p\u0159\u00EDtomnosti stratigrafick\u00FDch marker\u016F Cribrocentrum reticulatum, Isthmolithus recurvus, Chiasmolithus oamaruensis, Ch. altus, Pontospohaera enormis, Cyclicargolithus abisectus a Helicosphaera carteri. Ochlazen\u00ED v nejvy\u0161\u0161\u00EDm eoc\u00E9nu je vyzna\u010Deno p\u0159\u00EDtomnost\u00ED velk\u00FDch a \u0161iroce ov\u00E1ln\u00FDch plakolit\u016F Reticulofenestra umbilicus a absenc\u00ED diskoasterid\u016F. Kol\u00EDs\u00E1n\u00ED mo\u0159sk\u00E9 hladiny a specifick\u00FD v\u00FDvoj depocentra v oligoc\u00E9nu je dokumentov\u00E1no kvantitativn\u00EDm rozvojem rodu Pontosphaera a rozkv\u011Btem druh\u016F Dictyococcites bisectus a Cyclicargolithus abisectus ve svrchn\u00ED \u010D\u00E1sti oligoc\u00E9nu. Spodn\u00ED mioc\u00E9n, NN1-NN4 je charakterizov\u00E1n chud\u00FDmi spole\u010Dstvy nanofosili\u00ED. M\u011Blk\u00E9 epikontinent\u00E1ln\u00ED mo\u0159e umo\u017Enilo rozvoj rod\u016F Helicosphaera (H. carteri, H. ampliaperta, H. medirerranea), mal\u00FDch exempl\u00E1\u0159\u016F rodu Reticulofenestra a ve svrchn\u00ED \u010D\u00E1sti se objevuje Sphenolithus heteromorphus. Transgrese ve st\u0159edn\u00EDm mioc\u00E9nu umo\u017Enila rozvoj nanofl\u00F3ry. Spodn\u00ED \u010D\u00E1st z\u00F3ny NN5 je vyzna\u010Dena kr\u00E1tk\u00FDm horizontem s Helicosphaera waltrans. V nadlo\u017En\u00EDch sedimentech se vyskytuj\u00ED bohat\u00E1 spole\u010Denstva s hojn\u00FDm v\u00FDskytem Helicosphaera vedderi a Coccolithus sp."@cs . . "1"^^ . . . . . "Zpr\u00E1vy o geologick\u00FDch v\u00FDzkumech v roce 2013" . "1"^^ . "I" . "RIV/00025798:_____/14:00000152!RIV15-MSM-00025798" . . "\u0160v\u00E1benick\u00E1, Lilian" . "0514-8057" . "Biostratigraphic evaluation of the Carpathian Foredeep and Flysch Carpathian deposits in the vicinity of \u0160lapanice, calcareous nannofossils."@en . . . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F karpatsk\u00E9 p\u0159edhlubn\u011B a fly\u0161ov\u00E9ho p\u00E1sma Z\u00E1padn\u00EDch Karpat v okol\u00ED \u0160lapanic na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED"@cs . "5494" . "podzim" . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F karpatsk\u00E9 p\u0159edhlubn\u011B a fly\u0161ov\u00E9ho p\u00E1sma Z\u00E1padn\u00EDch Karpat v okol\u00ED \u0160lapanic na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED" . "RIV/00025798:_____/14:00000152" . . "[3D592949DA6E]" . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F fly\u0161e Z\u00E1padn\u00EDch Karpat a karpatsk\u00E9 p\u0159edhlubn\u011B na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED bylo p\u0159ipraveno pro sestaven\u00ED geologick\u00E9 mapy 24-431 \u0160lapanice. Vzorky byly z\u00EDsk\u00E1ny z izolovan\u00FDch odb\u011Br\u016F a z m\u011Blk\u00FDch vrt\u016F p\u0159i geologick\u00E9ho v\u00FDzkumu a mapov\u00E1n\u00ED. Relativn\u00ED st\u00E1\u0159\u00ED fly\u0161e bylo stanoveno v intervalu od svrchn\u00ED \u010D\u00E1sti st\u0159edn\u00EDho eoc\u00E9nu a\u017E po hranici oligoc\u00E9n-mioc\u00E9n, z\u00F3ny NP16-NN1 na z\u00E1klad\u011B p\u0159\u00EDtomnosti stratigrafick\u00FDch marker\u016F Cribrocentrum reticulatum, Isthmolithus recurvus, Chiasmolithus oamaruensis, Ch. altus, Pontospohaera enormis, Cyclicargolithus abisectus a Helicosphaera carteri. Ochlazen\u00ED v nejvy\u0161\u0161\u00EDm eoc\u00E9nu je vyzna\u010Deno p\u0159\u00EDtomnost\u00ED velk\u00FDch a \u0161iroce ov\u00E1ln\u00FDch plakolit\u016F Reticulofenestra umbilicus a absenc\u00ED diskoasterid\u016F. Kol\u00EDs\u00E1n\u00ED mo\u0159sk\u00E9 hladiny a specifick\u00FD v\u00FDvoj depocentra v oligoc\u00E9nu je dokumentov\u00E1no kvantitativn\u00EDm rozvojem rodu Pontosphaera a rozkv\u011Btem druh\u016F Dictyococcites bisectus a Cyclicargolithus abisectus ve svrchn\u00ED \u010D\u00E1sti oligoc\u00E9nu. Spodn\u00ED mioc\u00E9n, NN1-NN4 je charakterizov\u00E1n chud\u00FDmi spole\u010Dstvy nanofosili\u00ED. M\u011Blk\u00E9 epikontinent\u00E1ln\u00ED mo\u0159e umo\u017Enilo rozvoj rod\u016F Helicosphaera (H. carteri, H. ampliaperta, H. medirerranea), mal\u00FDch exempl\u00E1\u0159\u016F rodu Reticulofenestra a ve svrchn\u00ED \u010D\u00E1sti se objevuje Sphenolithus heteromorphus. Transgrese ve st\u0159edn\u00EDm mioc\u00E9nu umo\u017Enila rozvoj nanofl\u00F3ry. Spodn\u00ED \u010D\u00E1st z\u00F3ny NN5 je vyzna\u010Dena kr\u00E1tk\u00FDm horizontem s Helicosphaera waltrans. V nadlo\u017En\u00EDch sedimentech se vyskytuj\u00ED bohat\u00E1 spole\u010Denstva s hojn\u00FDm v\u00FDskytem Helicosphaera vedderi a Coccolithus sp." . "Neuveden" . "Biostratigrafick\u00E9 vyhodnocen\u00ED sediment\u016F karpatsk\u00E9 p\u0159edhlubn\u011B a fly\u0161ov\u00E9ho p\u00E1sma Z\u00E1padn\u00EDch Karpat v okol\u00ED \u0160lapanic na z\u00E1klad\u011B studia v\u00E1pnit\u00FDch nanofosili\u00ED"@cs . "Biostratigraphic evaluation of the Carpathian Foredeep and Flysch Carpathian deposits in the vicinity of \u0160lapanice, calcareous nannofossils."@en . . . "7"^^ . . . "CZ - \u010Cesk\u00E1 republika" .