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Crinerocrinus parvicostatus
Taxonomy
Crinerocrinus parvicostatus was named by Kolata (1982). Its type specimen is OU 8858 and is a 3D body fossil. Its type locality is East bank of Culley Creek, Criner Hills. 9-10 meters below Viola Limestone, which is in an Ordovician offshore ramp limestone/shale in the Bromide Formation of Oklahoma. It is the type species of Crinerocrinus.
Entered
by P. Wagner on 2019-05-26
Synonymy list
| Year | Name and author |
|---|---|
| 1982 | Crinerocrinus parvicostatus Kolata p. 190 figs. Plate 21, figures 7, 8; Figure 52 |
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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.
†Crinerocrinus parvicostatus Kolata 1982
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class, p = phylum | |||||
| References: Kiessling 2004, Aberhan 1992, Aberhan et al. 2004 | |||||
Age range: Middle Ordovician or 471.30000 to 458.20000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Middle Ordovician | USA (Oklahoma) | Crinerocrinus parvicostatus (type locality: 201757) |