2020
DOI: 10.1016/j.gr.2019.11.008
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The first record of redfieldiiform fish (Actinopterygii) from the Upper Triassic of Korea: Implications for paleobiology and paleobiogeography of Redfieldiiformes

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Cited by 4 publications
(5 citation statements)
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“…The Amisan Formation is known to 1,000 m thick and consists of the lower sandstone units, the lower shale unit, the middle sandstone units, the middle shale unit, and the upper sandstone unit (Yang, 1999). Diverse fossils have been documented from the Amisan Formation, including plants (Kim, 1976, 1990, 2001; Kimura and Kim, 1984; Kim et al, 2002; Kim and Roh, 2008), bivalves (Kim et al, 2015), conchostracans (Kim and Lee, 2015), insects (Nam and Kim, 2014; Nam et al, 2017), and fishes (Kim et al, 2020). Of these, plant and conchostracan fossils have been used for age-dating the Amisan Formation.…”
Section: Geological Settingmentioning
confidence: 99%
“…The Amisan Formation is known to 1,000 m thick and consists of the lower sandstone units, the lower shale unit, the middle sandstone units, the middle shale unit, and the upper sandstone unit (Yang, 1999). Diverse fossils have been documented from the Amisan Formation, including plants (Kim, 1976, 1990, 2001; Kimura and Kim, 1984; Kim et al, 2002; Kim and Roh, 2008), bivalves (Kim et al, 2015), conchostracans (Kim and Lee, 2015), insects (Nam and Kim, 2014; Nam et al, 2017), and fishes (Kim et al, 2020). Of these, plant and conchostracan fossils have been used for age-dating the Amisan Formation.…”
Section: Geological Settingmentioning
confidence: 99%
“…3 c–e), it is reasonable to consider this structure as the crystalline lens. The possible crystalline lens is also recognizable in a specimen of Hiascoactinus 16 .…”
Section: Discussionmentioning
confidence: 82%
“…The Amisan Formation is interpreted as alluvial-fan to lacustrine-delta environments 13 , and its depositional age is generally considered Late Triassic or Late Triassic-Early Jurassic based on fossil records 14 , 15 . A single specimen of Redfieldiiformes, Hiascoactinus boryeongensis , was reported from the Amisan Formation, and it is distinguished from Megalomatia mainly by a single plate-like branchiostegal ray and the caudally positioned dorsal and anal fins in near opposition to each other 16 . Accordingly, Megalomatia represents a new taxon, not different ontogenetic stages of Hiascoactinus .…”
Section: Introductionmentioning
confidence: 99%
“…Redfieldiiformes Berg, 1940 Redfieldiiformes are a clade of actinopterygians formed by at least 17 genera, known from the Lopingian to Early Jurassic, mostly in non-marine environments of Australia, Africa (Morocco, South Africa, Zambia and possibly Madagascar), Asia (South Korea), South America (Argentina), North America (USA) and putatively Europe (England, Germany, Ireland, Poland and Switzerland, see Gibson, 2018, Gouiric-Cavalli et al, 2017, Hutchinson, 1973a, Kim et al, 2020, Lombardo, 2013, Schaeffer, 1984, Schaeffer and Mc Donald, 1978, Sytchevskaya et al, 2009. Their general features include an elongated body covered with ganoid scales, the dorsal and anal fins located posteriorly, and a hemi-heterocercal caudal fin.…”
Section: Palaeontological Systematics Actinopterygii Cope 1887mentioning
confidence: 99%