PROCEEDINGS 



OF 



THE GEOLOGICAL SOCIETY OF LONDON. 

 Vol. II. 1838. No. 57. 



April 4.— Thomas William Maltby, Esq., M.A., of Turnham 

 Green, Middlesex; William Taylor, Esq., B.A., late of Queen's 

 College, Cambridge, now of New Ormond Street ; Mr. Isaiah Deck, 

 of Cambridge ; and Dr. Ainsworth, late Naturalist of Col. Chesney's 

 Expedition ; were elected Fellows of this Society. 



A paper was read, entitled, "A Description of Viscount Cole's 

 specimen of Plesiosaurus macrocephalus (Conybeare)," by Richard 

 Owen, Esq., F.G.S., Hunterian Professor in the College of Surgeons, 

 London. 



The author premises his description of the Plesiosaurus macroce- 

 phalus, by pointing out the characters of a species of Plesiosaurus, 

 which he regards as distinct from the Plesiosaurus dolichodeirus of 

 Mr. Conybeare ; and which, from the completeness of its skeleton in 

 the British Museum and other collections, he selects for a more im- 

 mediate comparison with the Plesiosaurus macrocephalus. 



He proposes to call the species thus selected, as a term of com- 

 parison, Plesiosaurus Hawkinsii, in honour of the gentleman to whose 

 remarkable skill and indefatigable labour, the beautiful and perfect 

 skeletons of it are exclusively due. The chief points in which the 

 Plesiosaurus Hawkinsii differs from the PI. dolichodeirus are, — that 

 the neck is a little longer than the trunk, instead of being fully equal 

 to the body and tail united ; — that it contains twent)''-nine cervical 

 vertebrae, bearing hatched-shaped ribs, instead of thirty-five; and that 

 the length of the head is equal to one-tenth part of the total length 

 of the skeleton, instead of one-thirteenth part as in the Dolichodeirus. 

 The PI. Hawkinsii differs also in the relative shortness and form of 

 the ulna and fibula, and in some other minor points. 



Having defined the species selected to illustrate the specific pecu- 

 liarities of the PL macrocephalus, Mr. Owen next offers some new 

 views respecting the elementary composition of a vertebra in the abs- 

 tract, suggested principally by a study of the vertebral column in 

 the Plesiosauri ; for having observed that the vertebral ribs, or the 

 elements termed by Geoffroy St. Hilaire paraaux, or para-vertebral 

 elements, are not bent down in the caudal region to form the protect- 

 ing laminae of the vascular trunks beneath the tail, but are continued 

 as shorter rib-like processes through a great part of the tail, co- 



3i 



