2016
DOI: 10.1002/9781119286448.ch1
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Morphology, phylogeny and taxonomy of osteolepiform fish

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Cited by 13 publications
(17 citation statements)
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“…Although we find a basic conservation of extraosseous replacement within early sarcopterygians our results also reveal previously unrecognized diversity in replacement processes both between tooth types, and between teeth and denticles. In the lingual maxillary and dentary rows of Eusthenopteron and Tiktaalik , and the anterior tooth row (ectopterygoid) of Onychodus , teeth were replaced in an almost alternating pattern similar to other onychodontiforms and osteolepiforms [19,20]. This alternating replacement within distinct rows, or fang pairs (in the case of Eusthenopteron and Tiktaalik ), was traditionally used to infer the presence of a dental lamina [5,37].…”
Section: Discussionmentioning
confidence: 99%
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“…Although we find a basic conservation of extraosseous replacement within early sarcopterygians our results also reveal previously unrecognized diversity in replacement processes both between tooth types, and between teeth and denticles. In the lingual maxillary and dentary rows of Eusthenopteron and Tiktaalik , and the anterior tooth row (ectopterygoid) of Onychodus , teeth were replaced in an almost alternating pattern similar to other onychodontiforms and osteolepiforms [19,20]. This alternating replacement within distinct rows, or fang pairs (in the case of Eusthenopteron and Tiktaalik ), was traditionally used to infer the presence of a dental lamina [5,37].…”
Section: Discussionmentioning
confidence: 99%
“…Specimens were obtained from the Natural History Museum, London, United Kingdom (NHM UK), Naturhistoriska Riksmuseet, Stockholm, Sweden (NRM), Nunavet Fossil Vertebrate collection (NUFV), Canadian Museum of Nature, Ottawa, Ontario, Canada (NMC); tomographic data were obtained from the Muséum National d'Histoire Naturelle, Paris, France (MNHN). Scan data of the following specimens were used: a left maxilla, left dentary, left ectopterygoid and parasymphyseal tooth whorl of Onychodus jandemarrai (NHMUK PV P63570, Frasnian, Gogo Formation, Western Australia) [18]; an anterior right dentary fragment of Eusthenopteron foordi (NRM-PAL P.35; Frasnian, Escuminac Formation, Miguasha National Park, Canada) [20,23,24]; a left anterior dentary fragment of Tiktaalik roseae (NUFV666; Frasnian, Fram Formation, Nunavut territory, Canada); and a coronoid 2 of Latimeria chalumnae (MNHN-ZA-AC-2012-26, caught in Domoni, Comores) [25].…”
Section: Methodsmentioning
confidence: 99%
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“…More specifically, Hay (1902) was the first to coin the term “Megalichthyidae”, after which Long (1985) suggested synapomorphies to define this particular “osteolepidid” clade, but the first full familial description was not provided until Young, Long & Ritchie (1992) . This was later revised by Fox et al (1995) , Borgen & Nakrem (2016) , and again most recently by Downs & Daeschler (2020) .…”
Section: Introductionmentioning
confidence: 98%
“…Aside from Cladarosymblema , there are several other genera commonly recognised within the Megalichthyidae: Megalichthys ( Agassiz, 1835 ) contains several species found in Devonian-Carboniferous deposits across North America ( Cope, 1882 ; Downs & Daeschler, 2020 ), Morocco ( Janvier & Martin, 1979 ), and the UK ( Thomson, 1964 ); Ectosteorhachis nitidus ( Cope, 1882 ) is known from the Lower Permian of the USA ( Thomson, 1964 ); Sengoerichthys ottoman —considered by some as the earliest megalichthyid—from the Frasnian of Turkey ( Janvier, Clément & Cloutier, 2007 ); Palatinichthys laticeps described from the Lower Permian of Germany ( Witzmann & Schoch, 2012 ); and the most recently described megalichthyid genus, Askerichthys heintzi, comes from the Late Carboniferous of Norway ( Borgen & Nakrem, 2016 ). However, Downs & Daeschler (2020) considered that the “unusual combinations of characters” in S. ottoman and P. laticeps precluded them from being megalichthyids.…”
Section: Introductionmentioning
confidence: 99%