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Eoanomoepus latus
Taxonomy
Eoanomoepus latus was named by Lockley et al. (2018). It is considered to be a form taxon. Its type specimen is Trackway T3 (replica MGL 12), a footprint, and it is a trace fossil. Its type locality is Moab North tracksite (UCM Loc. 30), which is in a Triassic terrestrial horizon in the Rock Point Formation of Utah. It is the type species of Eoanomoepus.
Synonymy list
Year | Name and author |
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2018 | Eoanomoepus latus Lockley et al. p. 424 |
2021 | Eoanomoepus latus Klein and Lucas p. 61 |
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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.
†Eoanomoepus latus Lockley et al. 2018
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Diagnosis
Reference | Diagnosis | |
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H. Klein and S. G. Lucas 2021 | Transverse tridactyl tracks only two thirds as long as wide, hence more transverse than typical Anomoepus with digit traces little connected, and digit divarication wide but variable. Step short, trackway very wide, with low pace angulation, and outward rotation of pes. Eoanomoepus differs from Anomoepus in length/width ratio (0.60-0.70 vs. ~1.08) and lack of obvious inward rotation characteristic of the latter, well-known ichnogenus. The trackway width of Eoanomoepus differs from Anomoepus in being unusually wide, also with usually an irregular step and stride dimensions. Eoanomoepus also differs from Anomoepus in lacking evidence of a hallux (digit I) trace and being more digitigrade. |
Measurements
No measurements are available
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Source: subo = suborder, o = order | |||||
References: Benton 1983, Marsh 1875 |
Age range: Late/Upper Triassic or 237.00000 to 201.40000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Late/Upper Triassic | USA (Utah) | Eoanomoepus latus (type locality: 219952) |