The first record of osteolepiform sarcopterygian from the Moravian Karst (Famennian, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00074343" target="_blank" >RIV/00216224:14310/14:00074343 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The first record of osteolepiform sarcopterygian from the Moravian Karst (Famennian, Czech Republic)
Popis výsledku v původním jazyce
Devonian and Carboniferous sequences of the Moravian Karst were deposited in the Rheno-Hercynian basin at the southern margin of Laurussia. All the previously known sarcopterygian remains from these deposits belong to onychodontiform fishes (eg. Ginter in Hladil et al. 1991). Recently, a cosmine-covered dermal bone was found in a small abandoned pit-quarry near the road leading from Brno Líšeň to Ochoz u Brna, where the two meters thick section of the Famennian Křtiny Limestones (Líšeň Formation) is exposed. This specimen was obtained from darker grey biodetrital limestones close to the boundary of the Upper Palmatolepis rugosa trachytera and the Lower Palmatolepis perlobata postera conodont zones (the bed ?B? sensu Weiner & Kalvoda 2013). The dermal bone is subtriangular in outline and bears characters of the lateral extrascapular. The absence of overlapped area at the median margin suggests that the lateral extrascapulars overlapped the median extrascapular.
Název v anglickém jazyce
The first record of osteolepiform sarcopterygian from the Moravian Karst (Famennian, Czech Republic)
Popis výsledku anglicky
Devonian and Carboniferous sequences of the Moravian Karst were deposited in the Rheno-Hercynian basin at the southern margin of Laurussia. All the previously known sarcopterygian remains from these deposits belong to onychodontiform fishes (eg. Ginter in Hladil et al. 1991). Recently, a cosmine-covered dermal bone was found in a small abandoned pit-quarry near the road leading from Brno Líšeň to Ochoz u Brna, where the two meters thick section of the Famennian Křtiny Limestones (Líšeň Formation) is exposed. This specimen was obtained from darker grey biodetrital limestones close to the boundary of the Upper Palmatolepis rugosa trachytera and the Lower Palmatolepis perlobata postera conodont zones (the bed ?B? sensu Weiner & Kalvoda 2013). The dermal bone is subtriangular in outline and bears characters of the lateral extrascapular. The absence of overlapped area at the median margin suggests that the lateral extrascapulars overlapped the median extrascapular.
Klasifikace
Druh
O - Ostatní výsledky
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA14-18183S" target="_blank" >GA14-18183S: Sekvenční stratigrafie devonských bioeventů - výkyvy mořské hladiny na přechodu od klimatického režimu greenhouse k icehouse</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů