Lossiemouth Sandstone | |
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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 | ||||||
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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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