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Sir Richard Owen KCB FRMS FRS (20 July 1804 – 18 December 1892) was an English biologist, comparative anatomist and palaeontologist. Owen is generally considered to have been an outstanding naturalist with a remarkable gift for interpreting fossils .
Chondrosteosaurus (meaning "cartilage and bone lizard") was a sauropod dinosaur from the Early Cretaceous Wessex Formation of England.. Holotype specimen of C. gigas. The type species, Chondrosteosaurus gigas, was described and named by Richard Owen in 1876. [1]
Dinosaur classification began in 1842 when Sir Richard Owen placed Iguanodon, Megalosaurus, and Hylaeosaurus in "a distinct tribe or suborder of Saurian Reptiles, for which I would propose the name of Dinosauria." [1] In 1887 and 1888 Harry Seeley divided dinosaurs into the two orders Saurischia and Ornithischia, based on their hip structure. [2]
Images Cardiodon. Nomen dubium. Sir Richard Owen, UK; Possible subjective synonym of Cetiosaurus. Cetiosaurus. Valid Sir Richard Owen, France Switzerland Morocco UK; A European Sauropod Cetiosaurus. Cladeiodon. Misidentification Sir Richard Owen, Germany; Dubious non-dinosaurian archosaur. Suchosaurus. Nomen dubium. Sir Richard Owen England ...
Dinodocus (meaning "terrible beam") is a genus of sauropod dinosaur, named by Richard Owen in 1884. The name is now usually considered a nomen dubium.The only species, D. mackesoni, a name given to some fossil bones from the Lower Greensand Group (Lower Cretaceous) of Hythe, Kent, England, were formerly placed in the genus Pelorosaurus (Mantell, 1850 [1]), but a review by Upchurch et al. (2004 ...
In 1842, Megalosaurus was one of three genera on which Richard Owen based his Dinosauria. On Owen's directions a model was made as one of the Crystal Palace Dinosaurs, which greatly increased the public interest for prehistoric reptiles. Subsequently, over fifty other species would be classified under the genus, originally because dinosaurs ...
Holotype of Dacentrurus armatus (NHMUK OR 46013), from Owen's 1875 monograph. On 23 May 1874, James Shopland of the Swindon Brick and Tyle Company reported in a letter to Professor Richard Owen that their clay pit, the Swindon Great Quarry below Old Swindon Hill at Swindon in Wiltshire, had again produced a fossil skeleton that he was willing to donate to the British Museum of Natural History.
Owen had noticed that many fossils showed a downward bend in the rear tail. At first, he explained this as a post mortem effect, a tendon pulling the tail end downwards after death. However, after an article on the subject by Philip Grey Egerton , [ 27 ] Owen considered the possibility that the oblique section could have supported the lower ...