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Macrostylocrinus wyomingensis
Taxonomy
Macrostylocrinus wyomingensis was named by Kolata (1976) [deposited in type collection at the Department of Geology, University of Illinois (UI), Urbana, Illinois]. Its type specimen is UI X-5190 and is not a trace fossil. Its type locality is Bighorn Formation Crinoids, which is in a Maysvillian deep subtidal limestone in the Bighorn Dolomite Formation of Wyoming.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1976 | Macrostylocrinus wyomingensis Kolata |
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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.
†Macrostylocrinus wyomingensis Kolata 1976
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: g = genus, c = class, p = phylum | |||||
| References: Aberhan et al. 2004, Kiessling 2004, Hendy et al. 2009, Aberhan 1992 | |||||
Age range: Maysvillian or 450.20000 to 449.60000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Maysvillian | USA (Wyoming) | Macrostylocrinus wyomingensis (type locality: 10446) |