THE GREAT SEA-LIZARDS AND THEIR ALLIES. 59 



bottom of the sea, was preyed upon by some carnivorous animal 

 (perhaps sharks). It seems, he says, as if a bite of the neck had 

 pulled out of place the eighth to the twelfth vertebrae. Those at 

 the base of the neck are scattered and dispersed as if through 

 more "tugging and riving." So with regard to its body, pro- 

 bably some hungry creature had a grip of the spine near the 

 middle of the back, and pulled all the succeeding vertebras in the 

 region of the hind limbs. Thus we get a little glimpse of scenes 

 of violence that took place at the bottom of the bright sunny 

 seas of the period when the clays and limestones of the Lias 

 rocks were being deposited in the region of Lyme-Regis. 



As time went on, these curious reptiles increased in size, until, 

 in the period when our English chalk was being formed (Creta- 

 ceous period), they reached their highest point (see p. 147). After 

 that they became extinct whether slowly or somewhat suddenly 

 we cannot tell. 



Until more is known of the ancient life of the earth, it will not 

 be possible to say with certainty what were the nearest relations 

 of the long-necked sea-lizards. They first appear in the strata 

 of the New Red Sandstone, which is below the Lias. Certain 

 little reptiles, about three feet long, from the former rocks, known 

 as Neusticosaurus and Lariosaurus, seem to be rather closely 

 related to the creatures we are now considering, and to connect 

 them with another group, namely, the Pliosaurs. They were 

 partly terrestrial and partly aquatic ; but it is not easy to say 

 whether their limbs had been converted into true paddles or not. 

 At any rate, there is every reason to believe that the long-necked 

 sea-lizards were descended from an earlier form of land reptile. 

 They gradually underwent considerable modifications, in order to 

 adapt themselves to an aquatic life. We noticed that the same 

 conclusion has been arrived at with regard to the fish-lizards. 

 Both these extinct groups, therefore, present an interesting analogy 

 to whales, which are now considered to have been derived, by a 

 like series of changes, from mammals that once walked the earth. 



