A sauropod-dominated tracksite from Rubha nam Brathairean (Brothers' Point), Isle of Skye, Scotland
A sauropod-dominated tracksite from Rubha nam Brathairean (Brothers' Point), Isle of Skye, Scotland
Scottish Journal of Geology (May 2018) 54 (1): 1-12
- Archosauria
- Chordata
- depositional environment
- Diapsida
- dinosaurs
- Eubrontes
- Europe
- fossil localities
- Great Britain
- habitat
- Hebrides
- Highland region Scotland
- ichnofossils
- Inner Hebrides
- Inverness-shire Scotland
- Isle of Skye
- lagoonal environment
- morphology
- photogrammetry
- Reptilia
- Saurischia
- Sauropoda
- Sauropodomorpha
- Scotland
- Tetrapoda
- Theropoda
- tracks
- United Kingdom
- Vertebrata
- Western Europe
- Great Estuarine Group
- Duntulm Formation
- Lealt Shale Formation
- Breviparopus
- Rubha nam Brathairean
Middle Jurassic dinosaur fossils are exceedingly rare, but new discoveries from the Isle of Skye, Scotland, are beginning to fill this gap. We here describe a new dinosaur tracksite found in the Lealt Shale Formation (Bathonian) of the Great Estuarine Group at Rubha nam Brathairean (Brothers' Point) on Skye. The site preserves an abundance of small sauropod manus and pes prints and several isolated and broken medium-to-large tridactyl footprints. The main site occurs on a single horizon of shaley limestone that formed in a lagoonal environment. The sauropod tracks are tentatively assigned to the ichnotaxon Breviparopus due to the narrow gauge of the trackways, the digital characteristics of the pes, and the ratio of heteropody observed between the manus and the pes. A theropod trackmaker is inferred for some of the tridactyl impressions with several indicative of the ichnotaxon Eubrontes. This new site strengthens the inference, originally based on a previously discovered locality near Duntulm Castle (Duntulm Formation) in northern Skye, that sauropods habitually spent time in lagoons during the Middle Jurassic. Supplementary material: The photogrammetric model of track BP2_40 and associated metadata and photographs are available at https://doi.org/10.6084/m9.figshare.c.4046390