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@article{1402947, author = {Poukarová, Hedvika and Weiner, Tomáš}, article_location = {WARSAW}, article_number = {3}, doi = {http://dx.doi.org/10.7306/gq.1301}, keywords = {Tetrapodomorpha; "Osteolepiformes"; cosmine; Famennian; Moravo-Silesian Basin; Moravian Karst}, language = {eng}, issn = {1641-7291}, journal = {GEOLOGICAL QUARTERLY}, title = {The first “osteolepiform” tetrapodomorph (Sarcopterygii) from the Paleozoic sequences of the Moravian Karst (Czech Republic)}, url = {https://gq.pgi.gov.pl/article/view/25353}, volume = {60}, year = {2016} }
TY - JOUR ID - 1402947 AU - Poukarová, Hedvika - Weiner, Tomáš PY - 2016 TI - The first “osteolepiform” tetrapodomorph (Sarcopterygii) from the Paleozoic sequences of the Moravian Karst (Czech Republic) JF - GEOLOGICAL QUARTERLY VL - 60 IS - 3 SP - 737-745 EP - 737-745 PB - Polish Geological Institute SN - 16417291 KW - Tetrapodomorpha KW - "Osteolepiformes" KW - cosmine KW - Famennian KW - Moravo-Silesian Basin KW - Moravian Karst UR - https://gq.pgi.gov.pl/article/view/25353 L2 - https://gq.pgi.gov.pl/article/view/25353 N2 - The first tetrapodomorph specimen from the Paleozoic sequences of the Moravian Karst (Moravo-Silesian Basin, Bohemian Massif, Czech Republic) is described. The well-pre served, cosmine-covered lateral extrascapular bone comes from the Upper Devonian (Famennian) hemipelagic Křtiny Limestone of the Líšeň Formation. The affinity to the “osteolepiforms” is inferred from the cosmine histology and morphological features of the bone. As signment to the Megalichthyiformes seems most probable. The associated fauna, e.g., clymenids, orthocone nautiloids, thin shelled bivalves, trilobites and crinoids, clearly demon strate a marine environment. ER -
POUKAROVÁ, Hedvika a Tomáš WEINER. The first “osteolepiform” tetrapodomorph (Sarcopterygii) from the Paleozoic sequences of the Moravian Karst (Czech Republic). \textit{GEOLOGICAL QUARTERLY}. WARSAW: Polish Geological Institute, 2016, roč.~60, č.~3, s.~737-745. ISSN~1641-7291. Dostupné z: https://dx.doi.org/10.7306/gq.1301.
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