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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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