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Guizhouniscus microlepidus
Taxonomy
Guizhouniscus microlepidus was named by Liu (2003). Its type specimen is Guizhou Stone Cultural and Artistic Palace 1, a skeleton, and it is a compression fossil. Its type locality is Wusha, Xingyi (NIGP collection), which is in a Longobardian marine horizon in the Falang Formation of China. It is the type species of Guizhouniscus.
Synonymy list
| Year | Name and author |
|---|---|
| 2003 | Guizhouniscus microlepidus Liu p. 347 figs. Pl 1, fig 1; pl 2, fig 1; pl 3, fig 1 |
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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.
†Guizhouniscus microlepidus Liu 2003
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, subp = subphylum | |||||
| References: Carroll 1988, Hendy et al. 2009 | |||||
Age range: Longobardian or 242.00000 to 235.00000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Longobardian | China (Guizhou) | Guizhouniscus microlepidus (type locality: 146379) |