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Glabrocingulum wannense
Taxonomy
Phanerotrema wannense was named by Newell (1935) [Phanerotrema? wannense Newell 1935]. It is not a trace fossil. Its type locality is Wann, which is in a Missourian marine shale in the Wann Formation of Oklahoma.
It was recombined as Glabrocingulum (Glabrocingulum) wannense by Sturgeon (1964), Kues and Batten (2001); it was recombined as Glabrocingulum wannense by Wagner (2023).
It was recombined as Glabrocingulum (Glabrocingulum) wannense by Sturgeon (1964), Kues and Batten (2001); it was recombined as Glabrocingulum wannense by Wagner (2023).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1935 | Phanerotrema wannense Newell pp. 347 - 348 figs. pl. 36 f. 2a-c |
| 1964 | Glabrocingulum (Glabrocingulum) wannense Sturgeon p. 208 figs. pl. 33 f. 3-6; pl. 36 f. 20 |
| 2001 | Glabrocingulum (Glabrocingulum) wannense Kues and Batten p. 27 |
| 2023 | Glabrocingulum wannense Wagner p. 5107 |
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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.
†Glabrocingulum wannense Newell 1935
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, o = order | |||||
| References: Bambach et al. 2007, Hendy 2009 | |||||
Age range: base of the Desmoinesian to the top of the Virgilian or 312.80000 to 298.90000 Ma
Collections (14 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Desmoinesian | USA (Ohio) | Glabrocingulum wannense (64888 64901 64902 64913 64915 64918 64923 64925 64926) | |
| Missourian | USA (Texas) | Glabrocingulum wannense (217917) | |
| Missourian | USA (Oklahoma) | Phanerotrema wannense (157965 160139) | |
| Virgilian | USA (Texas) | Glabrocingulum wannense (217891 217894) |