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Paleauletobius silenus
Taxonomy
Rhynchites silenus was named by Heer (1847). It is a compression fossil. Its type locality is Oeningen (unspecified collection), which is in a Sarmatian crater lake limestone in the Upper Freshwater-Molasse Formation of Germany. It is the type species of Paleauletobius.
It was recombined as Paleauletobius silenus by Poinar and Legalov (2015).
It was recombined as Paleauletobius silenus by Poinar and Legalov (2015).
Synonymy list
| Year | Name and author |
|---|---|
| 1847 | Rhynchites silenus Heer p. 180 figs. Pl 6, fig 8 |
| 1864 | Rhynchites silenus Heer p. 373 |
| 2015 | Paleauletobius silenus Poinar and Legalov p. 71 |
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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.
†Paleauletobius silenus Heer 1847
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: c = class, p = phylum | |||||
| References: Bush and Bambach 2015, Kiessling 2004 | |||||