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Shenmuichnus wangi
Taxonomy
Shenmuichnus wangi was named by Xing et al. (2016). It is considered to be a form taxon. Its type specimen is DLS1-RP1-RM1–DLS1-RP3-RM3, a footprint, and it is a trace fossil. Its type locality is Dalishu tracksite I, which is in a Sinemurian lacustrine sandstone in the Lufeng Formation of China.
Synonymy list
Year | Name and author |
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2016 | Shenmuichnus wangi Xing et al. p. 723 fig. 3–7 |
2017 | Shenmuichnus wangi Xing et al. p. 8 |
2023 | Shenmuichnus wangi Abrahams et al. p. 9 |
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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.
†Shenmuichnus wangi Xing et al. 2016
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Diagnosis
Reference | Diagnosis | |
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L. Xing et al. 2016 | Narrow gauge trackways (WAP/ML 1⁄4 0.94) showing large heteropody (1:1.48). Pes tracks tridactyl, large (22–23 cm long and 20–24 cm wide), with robust digits and weak mesaxony. Divarication between digits II and IV ranging 67–73°. Manus tracks pentadactyl and symmetrical along digit III, wider than long, with a length/ width ratio of 0.6. Manus tracks aligned with antero-lateral margins of pes tracks formed by digits III and IV. Pes tracks rotated inward (22°), manus tracks rotated outward (35°), relative to trackway midline. Average pace angulation of manus tracks 92°, of pes tracks 125°. Short steps with pace length being 2.0–2.7 £ footprint length. |
Measurements
No measurements are available
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Source: subo = suborder, o = order | |||||
References: Marsh 1875, Kiessling 2004, Benton 1983 |
Age range: Sinemurian or 199.50000 to 192.90000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Sinemurian | China (Yunnan) | Shenmuichnus wangi (type locality: 220069) |