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Vidrioceras irregulare
Taxonomy
Stacheoceras (Vidrioceras) irregulare was named by Böse (1919). It is a 3D body fossil. Its type locality is Wolf Camp, Glass Mountains, which is in a Gzhelian carbonate limestone in the Gaptank Formation of Texas.
It was recombined as Vidrioceras irregulare by Plummer and Scott (1937), Bogoslovskaya (1990).
It was recombined as Vidrioceras irregulare by Plummer and Scott (1937), Bogoslovskaya (1990).
Synonymy list
| Year | Name and author |
|---|---|
| 1919 | Stacheoceras (Vidrioceras) irregulare Böse p. 152 figs. Pl 7, figs 62-73 |
| 1937 | Vidrioceras irregulare Plummer and Scott p. 133 figs. Pl 30, figs 18-20 |
| 1990 | Vidrioceras irregulare Bogoslovskaya p. 72 |
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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.
†Vidrioceras irregulare Böse 1919
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| shell height | 2 | 10.6 | 9.40 | 12.0 | 10.7 | 1.84 | |
| shell diameter | 2 | 21.5 | 19.7 | 23.5 | 21.6 | 2.69 | |
| shell inflation | 2 | 1.90 | 1.90 | 1.90 | 1.90 | - |
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| Source: o = order, c = class | |||||
| References: Kiessling 2003, Kiessling 2004 | |||||