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Oriocrassatella elongata
Taxonomy
Oriocrassatella elongata was named by Boyd and Newell (1968). Its type specimen is AMNH 28473, a shell (Articulated shell), and it is not a trace fossil. Its type locality is AMNH2010, Beaver Creek, which is in a Kungurian open shallow subtidal packstone in the Park City Formation of Wyoming.
Synonymy list
| Year | Name and author |
|---|---|
| 1968 | Oriocrassatella elongata Boyd and Newell p. 30 figs. 1,3,5,9,11-21 |
| 1984 | Oriocrassatella elongata Muromtseva and Guskov p. 87 figs. Pl 48, fig 10 |
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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.
†Oriocrassatella elongata Boyd and Newell 1968
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| valve height | 98 | 18.8 | 8.00 | 35.0 | 19.0 | 6.90 |
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| Source: c = class | |||||
| Reference: Aberhan et al. 2004 | |||||
Age range: base of the Kungurian to the top of the Wuchiapingian or 279.30000 to 254.17000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Kungurian | USA (Wyoming) | Oriocrassatella elongata (type locality: 81512) | |
| Wuchiapingian | Russian Federation | Oriocrassatella elongata (114420) |