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Qingshania cercida

Osteichthyes - Parasemionotidae

Taxonomy
Qingshania cercida was named by Liu (2002). Its type specimen is Jurong City Museum J015, a skeleton, and it is a compression fossil. Its type locality is Qingshan quarry, Jurong, which is in a Smithian carbonate limestone in the Qinglong Formation of China. It is the type species of Qingshania.

Synonymy list
YearName and author
2002Qingshania cercida Liu p. 36 figs. Pl 4, figs 3,4; pl 5, fig 1
2006Qingshania cercida Tong et al. p. 154 fig. 8

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
classOsteichthyes
RankNameAuthor
subclassActinopterygii()
infraclassActinopteri()
NeopterygiiRegan 1923
infraclassHolostei(Müller 1846)
familyParasemionotidaeStensiö 1932
genusQingshania
speciescercida

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

Qingshania cercida Liu 2002
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: marinesubp
Locomotion: actively mobilec
Diet: grazerf
Diet 2: detritivoref
Created: 2014-02-08 20:11:11
Modified: 2014-02-08 20:11:11
Source: f = family, c = class, subp = subphylum
References: Hendy et al. 2009, Carroll 1988, Kiessling 2004, Neuman and Wilson 1985

Age range: Smithian or 249.90000 to 248.10000 Ma

Collections (2 total)


Time interval Ma Country or state Original ID and collection number
Smithian249.9 - 248.1China (Anhui) Qingshania cercida (117945)
Smithian249.9 - 248.1China (Jiangsu) Qingshania cercida (type locality: 117942)