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Gracilimanus obscurus
Taxonomy
Gracilimanus obscurus was named by Feldmann and Schweitzer (2014). Its type specimen is USNM 593562a and is a compression fossil. Its type locality is West flank of Big Horn Mountains, which is in a Bajocian open shallow subtidal limestone in the Gypsum Spring Formation of Wyoming. It is the type species of Gracilimanus.
Synonymy list
| Year | Name and author |
|---|---|
| 2014 | Gracilimanus obscurus Feldmann and Schweitzer p. 9 fig. 9,10 |
| 2016 | Gracilimanus obscurus Feldmann et al. p. 12 fig. 13.2 |
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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.
†Gracilimanus obscurus Feldmann and Schweitzer 2014
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class | |||||
| References: Turnsek 1997, Aberhan 1992 | |||||
Age range: Late/Upper Bajocian or 168.60000 to 168.20000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Bajocian | USA (Wyoming) | Gracilimanus obscurus (type locality: 155766) |