Archive image from page 169 of A descriptive catalogue of the. A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. descriptivecatal02brit Year: 1910 140 MAEINE EEPTILES OF THE OXFOED CLAY. larger; the two are separated by a well-marked oblique groove () running from front to back of the bone. The plane of the distal condyles makes an angle with that of the proximal expansion, but is not turned almost at right angles with it as in Steneosaurus. There is a well-marked deltoid prominence ().


Archive image from page 169 of A descriptive catalogue of the. A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. descriptivecatal02brit Year: 1910 140 MAEINE EEPTILES OF THE OXFOED CLAY. larger; the two are separated by a well-marked oblique groove () running from front to back of the bone. The plane of the distal condyles makes an angle with that of the proximal expansion, but is not turned almost at right angles with it as in Steneosaurus. There is a well-marked deltoid prominence (). The humerus in this genus is longer than the tibia and more than half as long as the femur: in Steneosaurus the reverse is the case. The radius and ulna, though similar to those of Test-fig. 54. Left humerus and left half of shoulder-girdle of Mycterosuclius nasutas : A, humerus from front: B, distal end of humerus ; 0, outer side of coracoid and scapula. (R. 2617, g nat. size.) , radial condyle; , ulnar condyle ; cor., coracoid; , deltoid crest; /., coracoid foramen : , glenoid fossa; h., head of humerus ; , intercondylar groove ; sc, scapula. Steneosaurus in form, are likewise proportionately larger. The difference of proportion between the fore and hind limb may be expressed by saying, that if the combined


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