| Lossiemouth Sandstone | |
|---|---|
| Stratigraphic range: Carnian–Rhaetian ~ | |
| Type | Geological formation | 
| Unit of | New Red Sandstone Supergroup | 
| Underlies | Stotfield Cherty Rock Formation | 
| Overlies | Burghead Sandstone Formation or unconformably on Devonian beds | 
| Thickness | up to 30 m (98 ft) | 
| Lithology | |
| Primary | Sandstone | 
| Location | |
| Coordinates | 57°42′N3°18′W / 57.7°N 3.3°W | 
| Approximate paleocoordinates | 34°00′N0°54′W / 34.0°N 0.9°W | 
| Region | Moray Firth | 
| Country | Scotland | 
| Type section | |
| Named for | Lossiemouth | 
The Lossiemouth Sandstone is a Middle to Late Triassic (Ladinian to Norian) age geological formation. It is exposed on the south side of the Moray Firth near Lossiemouth and near Golspie in Sutherland. [1] Dinosaur remains are among the fossils that have been recovered from the formation. [2]
| Vertebrates reported from the Lossiemouth Sandstone | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images | 
| Dasygnathoides | D. longidens | Nomen dubium | ||||
| Brachyrhinodon | B. taylori | A rhynchocephalian |   | |||
| Erpetosuchus | E. granti | A Pseudosuchian |   | |||
| Hyperodapedon | H. gordoni | A rhynchosaur |   | |||
| Leptopleuron | L. lacertinum | A procolophonid |   | |||
| Ornithosuchus | O. woodwardi | An ornithosuchid |   | |||
| O. taylori | Junior synonym of O. woodwardi | |||||
| Saltopus [3] | S. elginensis [3] | "Partial postcranial skeleton" [3] | A dinosauriform previously classified as a specimen of Leptopleuron |   | ||
| Scleromochlus | S. taylori | A possible avemetatarsalian |   | |||
| Stagonolepis | S. robertsoni | An aetosaur |   | |||
| Telerpeton | T. elginense | Junior synonym of Leptopleuron | ||||
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