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Eoasianites eximius
Taxonomy
Eoasianites eximius was named by Ruzhentsev (1950). Its type specimen is PIN 320/1874, a shell, and it is a 3D body fossil. Its type locality is Sakmara River, cut 165 km, bed 17, which is in a Gzhelian marine siliciclastic in the Russian Federation.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1950 | Eoasianites eximius Ruzhentsev p. 137 figs. Pl 9, figs 3,4; text-fig 53 |
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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.
†Eoasianites eximius Ruzhentsev 1950
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| shell height | 2 | 3.55 | 3.50 | 3.60 | 3.55 | 0.071 | |
| shell diameter | 2 | 10.7 | 10.4 | 11.0 | 10.7 | 0.424 | |
| shell inflation | 2 | 5.20 | 5.00 | 5.40 | 5.20 | 0.283 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Kiessling 2003 | |||||