"Badenian; parastratotype; multiproxy quantitative analysis; palaeoecology; climate"@en . "Hrabovsky, J." . "24510" . . . "I, P(GA205/09/0103), Z(MSM0021620855)" . . "Two shallow boreholes were drilled in 2010 into the Badenian (Langhian) parastratotype at Zidlochovice (Carpathian Foredeep, NN5 Zone, Czech Republic). Their profiles (26 m of sediment) were studied comprehensively (sedimentology, palaeontology-calcareous nannoplankton, red algae, palynology, Foraminifera, Bryozoa, Brachiopoda, Ostracoda, Mollusca, Teleostei and Elasmobranchii). The sedimentary succesion was biostratigraphically correlated with the NN5 Zone (14.9-13.9 Ma), namely with the initial time of the Middle Miocene Climatic Transition. Seven lithofacies representing multiple alternations of mudstone, sandstone and limestone facies were recognised within sedimentary succession. Fossils indicated a normal marine, warm to subtropical environment. The generally shallowing trend from the bottom (epibathyal/circalittoral) to the top (shallow infralittoral) of the sedimentary succession with repeated palaeobathymetric changes could be recognized in both boreholes."@en . "Dol\u00E1kov\u00E1, N." . . "000330540100004" . . . "Utescher, T." . . "Hladilov\u00E1, S." . . . . "Neues Jahrbuch Fur Geologie Und Palaontologie-Abhandlungen" . "The Badenian parastratotype at Zidlochovice from the perspective of the multiproxy study"@en . . "271" . "Seko, M." . "The Badenian parastratotype at Zidlochovice from the perspective of the multiproxy study" . . "Nehyba, S." . "Two shallow boreholes were drilled in 2010 into the Badenian (Langhian) parastratotype at Zidlochovice (Carpathian Foredeep, NN5 Zone, Czech Republic). Their profiles (26 m of sediment) were studied comprehensively (sedimentology, palaeontology-calcareous nannoplankton, red algae, palynology, Foraminifera, Bryozoa, Brachiopoda, Ostracoda, Mollusca, Teleostei and Elasmobranchii). The sedimentary succesion was biostratigraphically correlated with the NN5 Zone (14.9-13.9 Ma), namely with the initial time of the Middle Miocene Climatic Transition. Seven lithofacies representing multiple alternations of mudstone, sandstone and limestone facies were recognised within sedimentary succession. Fossils indicated a normal marine, warm to subtropical environment. The generally shallowing trend from the bottom (epibathyal/circalittoral) to the top (shallow infralittoral) of the sedimentary succession with repeated palaeobathymetric changes could be recognized in both boreholes." . . . . . "DE - Spolkov\u00E1 republika N\u011Bmecko" . "RIV/46747885:24510/14:#0001124" . "0077-7749" . . "2" . "RIV/46747885:24510/14:#0001124!RIV15-MSM-24510___" . "4780" . "The Badenian parastratotype at Zidlochovice from the perspective of the multiproxy study"@en . "Z\u00E1gor\u0161ek, Kamil" . "1"^^ . "Brzobohaty, R." . "10.1127/0077-7749/2014/0383" . "The Badenian parastratotype at Zidlochovice from the perspective of the multiproxy study" . . . "[948759770401]" . "Holcov\u00E1, K." . . "33"^^ . "9"^^ .