Image (left) and reconstruction (right) of the ilium of the holotype
The holotype of Metriacanthosaurus parkeri, specimen OUM J.12144, was discovered in 1871 by W. Parker at Jordan's Cliff, near Weymouth, Dorset, on the southwest coast of England.[1] The specimen includes an incomplete hip, a leg bone, and part of a backbone; the geologistJohn Phillips briefly commented on the specimen during the same year.[2] These bones were from the Oxford Clay Formation, which dates to the Upper Jurassic.[3]
In 1923, German paleontologist Friedrich von Huene wrote a paper on Jurassic and Cretaceous European carnivorous dinosaurs within Saurischia. In this paper, he examined OUM J.12144, assigning it to a new species of Megalosaurus: Megalosaurus parkeri.[1] The specific name honours W. Parker. In 1932, however, von Huene concluded it was a species of Altispinax, A. parkeri.[4]
In 1964, scientist Alick Walker decided these fossils were too different from Altispinax, as they lacked the long vertebral spines, and named the new genus Metriacanthosaurus.[5] The generic name is derived from Greek metrikos, "moderate", and akantha, "spine". Metriacanthosaurus thus gets its name from its vertebrae, which are taller than typical carnosaurs, like Allosaurus, but lower than other high-spined dinosaurs like Acrocanthosaurus.
Metriacanthosaurus was a medium-sized theropod with a femur length of 80cm (31in). Gregory S. Paul in 1988 estimated its weight at 1 tonne (1.1 short tons).[6] Thomas Holtz gave a length of 8 meters (26.2 feet).[7]Metriacanthosaurus was named for the height of its neural spines, which are actually not overly tall for theropods.[3] They are similar to other theropods such as Megalosaurus, Sinraptor, and Ceratosaurus in being 1.5 times the height of the centrum.[8]
Classification
Originally named as a species of Megalosaurus in Megalosauridae, Metriacanthosaurus has since been reclassified in Metriacanthosauridae. It is thought to be related to genera such as Yangchuanosaurus, and in 1988 Paul synonymized the two genera. However, a 2007 review of British dinosaurs by Darren Naish and David Martill defending keeping the two genera taxonomically separate.[3]Metriacanthosaurus is considered a member of the subfamily Metriacanthosaurinae.[9]
Metriacanthosaurus is the only known member of Metriacanthosauridae outside of Asia (other than possible fragmentary records from the geographically close Falaises des Vaches Noires locality of northern France, which is probably similar in age to Metriacanthosaurus[10]). The earliest records of metriacanthosaurids in Asia are from the early Middle Jurassic, with Metriocanthosaurus being nested within the diversity of Asian metriacanthosaurids. Metriacanthosaurus thus likely represents a dispersal event from Asia into Europe during the early Late Jurassic. Metriacanthosaurus appears to have lived alongside other large theropods belonging to the family Megalosauridae.[11] Other dinosaurs known from the Oxford Clay (which both spans the preceding Callovian and the Oxfordian) include the megalosaurid theropod Eustreptospondylus, the sauropod Cetiosauriscus, the stegosaurs Lexovisaurus and Loricatosaurus, the ankylosaur Sarcolestes, and the iguanodontian Callovosaurus.,[12] with the poorly known ankylosaur Cryptosaurus also being known from Oxfordian aged sediments in Britain.[13][14] During this time, Europe formed an archipelago of islands surrounded by shallow seas, explaining the findings of these dinosaurs in marine sediments.[10]
↑ von Huene, F. (1932). "Die fossile Reptil-Ordnung Saurischia, ihre Entwicklung und Geschichte". Monographien zur Geologie und Paläontologie. 1 (4): 361.
↑ Walker, Alick D. (1964). "Triassic reptiles from the Elgin area: Ornithosuchus and the origin of carnosaurs". Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences. 248 (744): 53–134. Bibcode:1964RSPTB.248...53W. doi:10.1098/rstb.1964.0009.
↑ Benson, R. B. J.; Radley, J. D. (2010). "A New Large-Bodied Theropod Dinosaur from the Middle Jurassic of Warwickshire, United Kingdom". Acta Palaeontologica Polonica. 55 (1): 35–42. CiteSeerX10.1.1.601.354. doi:10.4202/app.2009.0083. S2CID54680840.
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