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Eryon perroni
Taxonomy
Eryon perroni was named by Étallon (1859). It is a compression fossil. Its type locality is Calmoutiers, chailles siliceuses, which is in an Oxfordian offshore ramp limestone in the Terrain à Chailles Formation of France.
Sister species lacking formal opinion data
Entered
by C. Schweitzer on 2012-02-04; modified by M. Clapham on 2022-06-17
Synonymy list
| Year | Name and author |
|---|---|
| 1859 | Eryon perroni Étallon p. 181 figs. Pl 4, figs 1-3 |
| 2010 | Eryon perroni Schweitzer et al. p. 43 |
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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.
†Eryon perroni Étallon 1859
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: infrao = infraorder, o = order, c = class | |||||
| References: Turnsek 1997, Aberhan 1992, Fearon and Clapham 2023 | |||||
Age range: Early/Lower Oxfordian or 161.50000 to 154.80000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Jurassic | France | Eryon perroni (139752) | |
| Early/Lower Oxfordian | France | Eryon perroni (type locality: 226086) |