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Pseudovidrioceras girtyi
Taxonomy
Vidrioceras girtyi was named by Miller and Cline (1934). Its type specimen is USGS 1726 and is a 3D body fossil. Its type locality is USGS 988i, Raymond Canyon, Sublette Range, which is in a Roadian offshore shale in the Phosphoria Formation of Wyoming. It is the type species of Pseudovidrioceras.
It was recombined as Pseudovidrioceras girtyi by Bogoslovskaya (1990), Leonova (2002).
It was recombined as Pseudovidrioceras girtyi by Bogoslovskaya (1990), Leonova (2002).
Synonymy list
| Year | Name and author |
|---|---|
| 1934 | Vidrioceras girtyi Miller and Cline p. 290 figs. Pl 39, figs 15-17 |
| 1990 | Pseudovidrioceras girtyi Bogoslovskaya p. 72 |
| 2002 | Pseudovidrioceras girtyi Leonova p. S80 |
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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.
†Pseudovidrioceras girtyi Miller and Cline 1934
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| shell height | 2 | 8.00 | - | - | 8.00 | - | |
| shell diameter | 2 | 15.5 | 15.2 | 15.8 | 15.5 | 0.389 | |
| shell inflation | 2 | 1.00 | - | - | 1.00 | - |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Kiessling 2003 | |||||