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Eanus laevissimus
Taxonomy
Paranomus laevissimus was named by Wickham (1916). It is a compression fossil. Its type locality is Florissant, Station 14, which is in a Chadronian lacustrine - large shale in the Florissant Formation of Colorado.
It was recombined as Ludius laevissimus by Wickham (1920); it was recombined as Eanus laevissimus by Kundrata et al. (2021).
It was recombined as Ludius laevissimus by Wickham (1920); it was recombined as Eanus laevissimus by Kundrata et al. (2021).
Synonymy list
| Year | Name and author |
|---|---|
| 1916 | Paranomus laevissimus Wickham p. 521 figs. Pl 6, fig 10 |
| 1920 | Ludius laevissimus Wickham p. 354 |
| 2021 | Eanus laevissimus Kundrata et al. p. 25 |
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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.
†Eanus laevissimus Wickham 1916
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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 | |||||
Age range: Chadronian or 37.00000 to 33.90000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Chadronian | USA (Colorado) | Paranomus laevissimus (type locality: 106381) |