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Clionites (Traskites) fairbanksi
Taxonomy
Clionites fairbanksi was named by Hyatt and Smith (1905). It is a 3D body fossil. Its type locality is Brock Mountain, 3 miles east of Madison's ranch (Trachyceras subzone), which is in a Tuvalian carbonate limestone in the Hosselkus Formation of California.
It was recombined as Clionites (Traskites) fairbanksi by Smith (1927).
It was recombined as Clionites (Traskites) fairbanksi by Smith (1927).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1905 | Clionites fairbanksi Hyatt and Smith p. 183 figs. Pl 40, figs 1-11; pl 41, figs 1-14 |
| 1927 | Clionites (Traskites) fairbanksi Smith p. 85 figs. Pl 40, figs 1-11; pl 41, figs 1-14 |
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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.
†Clionites (Traskites) fairbanksi Hyatt and Smith 1905
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | |||||
|---|---|---|---|---|---|---|---|
| shell height | 1 | 22.5 | |||||
| shell diameter | 1 | 65.0 | |||||
| shell inflation | 1 | 25.5 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Kiessling 2003 | |||||