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Chauliodites nanshenghuensis
Taxonomy
Nivopteria nanshenghuensis was named by Lin (1978). Its type specimen is NIGP 51620, a forewing, and it is an impression. Its type locality is Nanshenghu, which is in a Triassic marginal marine mudstone in China.
It was recombined as Shurabia nanshenghuensis by Storozhenko (1997), Storozhenko (1998); it was recombined as Chauliodites nanshenghuensis by Zhang et al. (2022).
It was recombined as Shurabia nanshenghuensis by Storozhenko (1997), Storozhenko (1998); it was recombined as Chauliodites nanshenghuensis by Zhang et al. (2022).
Synonymy list
Year | Name and author |
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1978 | Nivopteria nanshenghuensis Lin p. 316 figs. Pl 1 fig 5 |
1997 | Shurabia nanshenghuensis Storozhenko p. 14 |
1998 | Shurabia nanshenghuensis Storozhenko p. 130 |
2003 | Nivopteria nanshenghuensis Aristov p. 37 fig. 3d |
2022 | Chauliodites nanshenghuensis Zhang et al. p. 4 fig. 2C,D |
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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.
†Chauliodites nanshenghuensis Lin 1978
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: c = class, p = phylum | |||||
References: Kiessling 2004, Bush and Bambach 2015 |
Age range: Middle Triassic or 246.70000 to 237.00000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Middle Triassic | China (Guizhou) | Nivopteria nanshenghuensis (type locality: 146281) |