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Rhynchosauroides rectipes
Taxonomy
Rhynchosauroides rectipes was named by Beasley (1911) [named in Maidwell 1911]. It is a trace fossil. Its type locality is Daresbury Quarry, which is in an Anisian terrestrial sandstone in the Helsby Sandstone Formation of the United Kingdom. It is the type species of Rhynchosauroides.
Sister species lacking formal opinion data
Synonyms
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Synonymy list
| Year | Name and author |
|---|---|
| 1911 | Rhynchosauroides rectipes Beasley |
| 1911 | Rhynchosauroides membranipes Maidwell |
| 1963 | Rhynchosauroides rectipes Kuhn p. 61 |
| 1966 | Rhynchosauroides rectipes Demathieu p. 483 |
| 1972 | Rhynchosauroides rectipes Demathieu and Haubold p. 804 |
| 2003 | Rhynchosauroides membranipes Tresise p. 136 |
| 2003 | Rhynchosauroides rectipes Tresise p. 136 |
| 2010 | Rhynchosauroides rectipes Klein et al. p. 8 |
| 2011 | Rhynchosauroides rectipes Klein et al. p. 226 |
| 2021 | Rhynchosauroides rectipes Klein and Lucas p. 81 |
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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.
†Rhynchosauroides rectipes Beasley 1911
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Invalid names: Rhynchosauroides membranipes Maidwell 1911 [synonym]
Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| H. Klein et al. 2010 | Broad quadrupedal trackways. Manus positioned medially to the pes or being overstepped by the latter at normal gait. Depending on the velocity of movement, the pace angulation of the pes varies between 70◦ and 125◦. The pes is slender and digitigrade, the smaller manus more stout and plantigrade. Digits increase in length from I to IV, V is much shorter, I–IV can be curved inward. Drag marks of the tail occasionally present. |