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Liuzhinia parva
Taxonomy
Liuzhinia parva was named by Wei (1981). It is a 3D body fossil. Its type locality is Longmendong, Feixianguan Formation member 4, Emei Mountain, which is in a Dienerian marine horizon in the Feixianguan Formation of China.
Synonymy list
| Year | Name and author |
|---|---|
| 1981 | Liuzhinia parva Wei p. 502 figs. Pl 2, figs 1-9 |
| 2006 | Liuzhinia parva Crasquin-Soleau p. 62 figs. Pl 2, fig 19 |
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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.
†Liuzhinia parva Wei 1981
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| carapace height | 3 | 0.276 | 0.260 | 0.300 | 0.270 | 0.021 | |
| shell height | 1 | 0.460 | - | - | - | - |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Jell and Adrain 2002 | |||||
Age range: base of the Capitanian to the top of the Bithynian or 264.28000 to 244.24000 Ma
Collections (8 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Capitanian | Türkiye | Liuzhinia parva (47929) | |
| Griesbachian - Dienerian | Hungary | Liuzhinia parva (61369) | |
| Dienerian | China (Sichuan) | Liuzhinia parva (type locality: 120634) | |
| Spathian | China (Guangxi) | Liuzhinia parva (106644 106645 106646) | |
| Spathian | China (Sichuan) | Liuzhinia parva (120633) | |
| Bithynian | Romania | Liuzhinia parva (197722) |