CRETACEOUS FORMATIONS. 11 



pneumatic foramina are at the back part of the base of the diapophysis, as I have seen 

 them in the cervical vertebra of a Dinornis. The articular surfaces of the centrum 

 retain the transversely extended form, and are simply concave before and convex 

 behind, which at once distinguishes the Pterosaurian hind-cervical vertebra from that 

 of the bird. 



In the dorsal region the vertebral centrum (fig. 24), retaining its shortness, gains 

 in depth, and presents the more usual proportions of cup-and-ball reptilian vertebrae. 

 The under surface (fig. 20) is smooth and even, very slightly concave lengthwise, 

 convex transversely. The parapophysis disappears, and the diapophysis, which 

 alone supports the rib, after the first or second dorsal, is sent off from a higher 

 position in the neural arch (fig. 25). 



Sacrum. 



Fig. 26, Tab. II, shows parts of the bodies of three anchylosed sacral vertebras, 

 the first being demonstrated by part of its anterior concave articular surface (a) 

 for the last lumbar vertebra. The groove for the passage of the nerve notches the 

 back part of the parapophysis, close to the line of suture with the second sacral. In 

 this vertebra the corresponding nerve-notch is more advanced, leaving a short sutural 

 surface behind, indicative of a position of the neural arch crossing for a short extent 

 the line of junction of the second with the third sacral centrum. The parapophyses 

 of the second and third are sent off almost on a level with the lower surface of the 

 centrum, which is flattened. 



The fore part of the sacrum of a much larger Pterodactyle, from the Cambridge 

 Green-sand, differing also in the less transverse convexity of the under part of the 

 first centrum, measures 1 1 lines across the shallow anterior articular concavity, and 

 14 lines from the lower part of the centrum to the fore part of the base of the neural 

 spine. The neural canal is circular and 2 lines in diameter ; above it the neural arch 

 rises like a vertical wall for 5 lines, where the spine has been broken off. 



Caudal Vertebra. 



From the number of elongated caudal vertebrae in the series of fossils from the 

 Cambridge Green- sand submitted to me — not fewer than seven — I believe the large 

 Pterodactyle from that formation to have had a long tail, but moveable, not stiff 

 through anchylosis of the vertebrae, as in Pter. (Ramphorhynclms) Gemmingi, V. 

 Meyer. 



The largest of these caudal vertebras measures 1^ inch in length; it is slightly 



