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Oobardjidama foulkesi
Taxonomy
Oobardjidama foulkesi was named by Salisbury et al. (2016). It is considered to be a form taxon. Its type specimen is WAM 12.1.6, cast of UQL-DP45-8, a footprint, and it is a trace fossil. Its type locality is Reddell Beach tracksite (UQL-DP45), which is in a Valanginian/Barremian lagoonal sandstone/siltstone in the Broome Sandstone Formation of Australia.
Synonymy list
| Year | Name and author |
|---|---|
| 2016 | Oobardjidama foulkesi Salisbury et al. p. 43 |
| 2020 | Oobardjidama foulkesi Moreau et al. p. 10 |
| 2021 | Oobardjidama foulkesi Poropat et al. p. 29 |
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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.
†Oobardjidama foulkesi Salisbury et al. 2016
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| S. W. Salisbury et al. 2016 | Trackway: weakly heteropodous (30–45%), variably medium- to wide-gauge trackways (sensu Romano et al., 2007 Romano, M., M. A. Whyte, and S. J. Jackson. 2007. Trackway ratio: a new look at trackway gauge in the analysis of quadrupedal dinosaur trackways and its implications for ichnotaxonomy. Ichnos 14:257–270.
[Taylor & Francis Online], [Google Scholar] ), with inner trackway width of 30–50 cm; manual tracks positioned midway between fore and aft pedal tracks, and in line with the rear half of contralateral pedal tracks; manual tracks situated relatively medially, within pedal trackway width. Pedal impressions: large-sized (craniocaudal length: 70–85 cm), near-piriform shape, but broadest across mid-track region, and with a lobed medial margin due to intersection of an asymmetrical heel pad crease; hallucal imprint widened medially by a bulbous cranial pad callosity; external outline of heel region semicircular as a result of occupation by a mediocaudal heel pad callosity; heel pad callosity medially offset and partitioned from fore-heel region of track by well-defined oblique ridge (∼45–75° to the horizontal); acute fore-heel caudal margin of internal track exclusive of heel pad; pedal track angulation between 90° and 100°. Manual impressions: marginally wider than long (∼115%); manual track angulation between 69° and 74°. |
Measurements
No measurements are available
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| Source: infrao = infraorder | |||||
| Reference: Marsh 1875 | |||||
Age range: base of the Valanginian to the top of the Barremian or 139.80000 to 125.00000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Valanginian - Barremian | Australia (Western Australia) | Sauropoda indet. (type locality: 61671) |