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Ordosemys leios
Taxonomy
Ordosemys leios was named by Brinkman and Peng (1993). Its type specimen is IVPP V.9534-1, a partial shell, and it is a 3D body fossil. Its type locality is Laolonghuozi, Ordos Basin, which is in a Valanginian/Hauterivian fluvial sandstone/siliciclastic in the Luohandong Formation of China.
Synonymy list
| Year | Name and author |
|---|---|
| 1993 | Ordosemys leios Brinkman and Peng p. 2129 figs. 2-11 |
| 2000 | Ordosemys leios Sukhanov fig. 17.14 |
| 2004 | Ordosemys leios Tong et al. p. 3 |
| 2008 | Ordosemys leios Brinkman et al. p. 55 |
| 2008 | Ordosemys leios Danilov and Parham |
| 2014 | Ordosemys leios Perea et al. |
| 2014 | Ordosemys leios Puntener et al. |
| 2019 | Ordosemys leios Li et al. |
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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.
†Ordosemys leios Brinkman and Peng 1993
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: subo = suborder, c = class, subp = subphylum | |||||
| References: Carroll 1988, Kiessling 2004, Uetz 2005, Hendy et al. 2009 | |||||
Age range: Valanginian or 137.05000 to 132.60000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Berriasian - Valanginian | China (Shandong) | Ordosemys leios (47070) | |
| Valanginian - Early/Lower Hauterivian | China (Nei Mongol) | Ordosemys leios (type locality: 46931) |