Abstract
Dinosaur tracks and other archosaur footprints from multiple stratigraphic levels in coastal exposures near Cardiff, and a site near Nottage, Porthcawl area, provide evidence of a diverse assemblage of trackmakers from the “marginal facies”; of the Mercia Mudstone Group (Late Triassic), that can be closely compared with other Pangaean ichnofaunas of the same age. The footprints, comprising at least 88 identified trackways from about 10 stratigraphie levels, can be assigned to the ichnogenera Grallator (Grallator), Grallator (cf. Anchisauripus), Chirotherium? or cf. Tetrasauropus, Pseudotetrasauropus? and Otozoum, most of which are new records for the Late Triassic of Great Britain. The ichnofauna indicates a relatively abundant and diverse archosaur‐dominated terrestrial vertebrate fauna in a semi‐arid setting subject to intermittent deposition by ephemeral streams. The numerically dominant track‐makers appear to have been small theropods with a lesser number of larger prosauropods and other archosaurs of...
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