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Chlupacites uralensis
Taxonomy
Agoniatites uralensis was named by Bogoslovsky (1969). Its type specimen is PIN 1447/64, a shell, and it is a 3D body fossil. Its type locality is Bobrovka river, Pokrovskoye, which is in an Emsian/Eifelian carbonate limestone in the Russian Federation.
It was recombined as Chlupacites uralensis by Korn and Klug (2002).
It was recombined as Chlupacites uralensis by Korn and Klug (2002).
Synonymy list
| Year | Name and author |
|---|---|
| 1969 | Agoniatites uralensis Bogoslovsky p. 146 figs. Pl 4, figs 1-3 |
| 2002 | Chlupacites uralensis Korn and Klug p. 76 |
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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.
†Chlupacites uralensis Bogoslovsky 1969
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | minimum | maximum | median | s.d. | |
|---|---|---|---|---|---|---|---|
| shell height | 3 | 18.9 | 17.8 | 21.2 | 18.0 | 1.91 | |
| shell diameter | 3 | 41.4 | 38.6 | 46.5 | 39.5 | 4.32 | |
| shell inflation | 3 | 10.8 | 10.0 | 12.5 | 10.2 | 1.39 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Kiessling 2003, Aberhan et al. 2004 | |||||
Age range: base of the Late/Upper Emsian to the top of the Eifelian or 399.50000 to 387.95000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Emsian - Eifelian | Russian Federation (Sverdlovsk) | Agoniatites uralensis (171999) |