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Geological formation in Moray, Scotland From Wikipedia, the free encyclopedia
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]
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 | 57.7°N 3.3°W |
Approximate paleocoordinates | 34.0°N 0.9°W |
Region | Moray Firth |
Country | Scotland |
Type section | |
Named for | Lossiemouth |
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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