FRILL-GILLED SHARK 
533 
teetli of the lower than in those of the upper jaw. With the occasional exception 
of some portions of the tail, the notochord persists throughout life. At the present 
day the range of the existing members of the genus includes most temperate and 
tropical seas, some of the species reaching as much as 15 feet in length. Whereas 
in the grey comb-toothed shark (Notidanus griseus), of the Atlantic and Mediter¬ 
ranean, the number of gill-clefts is six, in each of the other three species it is seven. 
Fossil species occur from the Pliocene to the middle Jurassic; many of these, like 
the one of which two teeth are shown in the illustration, being of much larger 
dimensions than any of the existing forms. As to the habits of these sharks, there 
appears to be practically no information. 
Friii-Giiied From the typical genus of the family the Japanese frill-gilled 
Shark. shark differs by the greatly elongated and slender form of the body; 
and by each of the six gill-clefts being protected by a frill-like flap of skin. The 
teeth are also of a somewhat simpler structure, being similar in both jaws, and each 
consisting of three slender, curved, and subconical cusps, separated by a pair of 
rudimentary ones; while there is an unpaired median series at the extremity of 
the lower jaw only, instead of in both the upper and the lower. Although mainly 
persistent, the notochord is in part replaced by ill-developed vertebrae of the type 
characteristic of the suborder. Fossil teeth from the European Miocene have been 
assigned to this genus. 
The Spiny Dog-Fishes and their Allies, —Family S'finacidje. 
Although the members of the present family approximate in their external 
conformation more to the typical sharks than to the rays, yet in the structure of 
their vertebrae they agree with the latter. Accordingly, both the spiny dog-fishes, 
rays, saw-fishes, and their kindred are regarded as forming a suborder (Tecto- 
spondyli) distinguished from the one including the preceding families by the 
following characters. In the bodies of the vertebrae, when fully developed, the 
concentric calcified plates are more numerous than those radiating from the centre; 
