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Paracravenoceras barnettense
Taxonomy
Nuculoceras barnettense was named by Plummer and Scott (1937). It is a 3D body fossil. Its type locality is B.E.G. 205-T-24 upper, abandoned lime kiln SE of San Saba, which is in a Serpukhovian marine limestone in the Barnett Formation of Texas.
It was recombined as Syngastrioceras barnettense by Ruzhentsev and Bogoslovskaya (1971); it was recombined as Paracravenoceras barnettense by Gordon (1960), Korn and Titus (2015).
It was recombined as Syngastrioceras barnettense by Ruzhentsev and Bogoslovskaya (1971); it was recombined as Paracravenoceras barnettense by Gordon (1960), Korn and Titus (2015).
Synonymy list
| Year | Name and author |
|---|---|
| 1937 | Nuculoceras barnettense Plummer and Scott p. 108 figs. Pl 7, figs 15-18 |
| 1960 | Paracravenoceras barnettense Gordon p. 144 figs. Pl 28, figs 16-18,25-28; text-figs 1C-F |
| 1971 | Syngastrioceras barnettense Ruzhentsev and Bogoslovskaya p. 294 |
| 2015 | Paracravenoceras barnettense Korn and Titus p. 84 |
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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.
†Paracravenoceras barnettense Plummer and Scott 1937
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| shell height | 2 | 9.54 | 7.00 | 13.0 | 10.0 | 4.24 | |
| shell diameter | 2 | 16.7 | 12.3 | 22.7 | 17.5 | 7.35 | |
| shell inflation | 2 | 2.57 | 2.00 | 3.30 | 2.65 | 0.919 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2003, Kiessling 2004 | |||||
Age range: Pendleian or 330.30000 to 326.90000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Pendleian | USA (Texas) | Paracravenoceras barnettense (169951) | |
| Serpukhovian | USA (Texas) | Nuculoceras barnettense (type locality: 128624) |