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Boeotiaspis longispinus
Taxonomy
Paleolimulus longispinus was named by Schram (1979). Its type specimen is UM 5559 and is a mold. Its type locality is MV 7106, Supercrop Quarry, Bear Gulch, which is in an Arnsbergian lagoonal/restricted shallow subtidal limestone in the Heath Formation of Montana.
It was considered an invalid subgroup of Paleolimulus by Lamsdell (2016); it was recombined as Boeotiaspis longispinus by Lamsdell (2020).
It was considered an invalid subgroup of Paleolimulus by Lamsdell (2016); it was recombined as Boeotiaspis longispinus by Lamsdell (2020).
Synonymy list
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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.
†Boeotiaspis longispinus Schram 1979
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class | |||||
| References: Jell and Adrain 2002, Bambach et al. 2007 | |||||
Age range: Arnsbergian or 327.00000 to 323.70000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Arnsbergian | USA (Montana) | Paleolimulus longispinus (90681 116654) |