
 
        
         
		ENALIOSAURS. 
 deep  continuous  furrow,  and  retained  by  slight  ridges  extending,  
 between the teeth, along the sides  and  bottom  of  the furrow  (PI.  73*  
 fig. 9),  and by the gum and the organized membranes  continued  into  
 the-groove and upon the base of the teeth. 
 The germs of the  new  teeth  are  developed  at  the  inner side of  
 the  base  of  the  old  ones.  Mr.  Conybeare  has  given a figure  of  a  
 transverse section across the jaw-bone, (reproduced at  PI.  73,  fig.  7)  
 in which the new tooth  (c)  has  penetrated  the  osseous  substance of  
 the  base  of  the  old  tooth  (b), and  its  point  has  nearly entered the  
 remains of the pulp-cavity which has continued  open in the  crown  of  
 the tooth (a). 
 From  the  circumstance  of  the  consolidation of  the base  of  the  
 teeth  in  the  Ichthyosaur  Mr.  Conybeare  infers  that  they  were  
 retained  longer  in  the  jaw than  are  the  hollow teeth  of  the  crocodiles  
 ;  but the analogy of  other  Saurians,  and the observation of two  
 new  teeth  at  successive  stages  of  formation  at  the  base of  an  old  
 tooth,  prove  that  the  succession  of  new sets  of  teeth was repeated  
 more  than  once,  though  probably  not  so  frequently  as  in  the  
 crocodile. 
 1 2 1 .  Plesiosaurus.—The teeth of the  Plesiosaur are conical, long,  
 slender,  curved  and  sharp-pointed;  they  appear  to  retain  their internal  
 cavity,  as  in  the  teeth  of  a  crocodile;  they  have a very long  
 round  fang  or  implanted  base, which,  in  old  teeth,  contracts, as it  
 sinks into the jaw,  and terminates almost in a point. 
 The chief  distinction, which the dental system offers between the  
 present and the preceding genus of  Enaliosaur, is the loose  implantation  
 of  the  teeth  of  the  Plesiosaur  in  separate  alveoli.  'In  thus  
 deviating from the Ichthyosaur,  the Plesiosaur proportionally approximates  
 to  the crocodilian type, and  this affinity is likewise manifested  
 in the unequal size of the teeth, and  the  development of some  of the  
 anterior ones into large tusks. 
 The  teeth  are  composed,  as  in  the  Ichthyosaur,  of  a  body of  
 hard  and simple  dentine,  covered  at  the  crown by a coat of enamel,  
 and,  at  the  base,  by a coat  of  cement;  but  the  latter  is  relatively  
 thinner than in the Ichthyosaur, and is not inflected into the substance  
 of the dentine.  The  crown  is  characterized  by well-defined  narrow 
 elevated  longitudinal  ridges,  terminating  abruptly  at  different  distances  
 from the apex, to which, however, none of them extend. 
 In the lower jaw of the Pies,  macrocephalus  there  are  twenty-six  
 teeth on each premandibular  bone:  the  crown  of  one  of the  large  
 anterior tusks,  in  a  lower jaw,  ten  inches  in  length,  measured  one  
 inch  and a half  in  length  and one  third of  an  inch  in  breadth;  its  
 transverse  section  was  nearly  circular.  The  premandibular  piece  
 of . the  lower  jaw  of  the  Pies,  arcuatus  contains  fifty-four  teeth,  or  
 twenty-seven  on  each side,  the six anterior teeth on  each  side being  
 larger  and  longer  than  the  rest.  In  the  lower  jaw  of  the  Pies,  
 dolichodeirus there are  twenty-five teeth on each side,  the four anterior  
 of which are the largest. 
 The disposition  of  the  calcigerous  tubes  is  shown  in a longitudinal  
 section of  the  apical  third part  of  a tooth  of  the  Plesiosaurus  
 Hawkinsii in PL  74.  In their  general course they bear a considerable  
 resemblance to the same parts  in  the  Ichthyosaurus,. but  the primary  
 curvature presents a more graceful sigmoid line,.from the inclination of  
 the peripheral extremities of the tubes towards the apex.  The diameter  
 of the tubes near their origin is -^„th of an inch; their interspaces equal  
 five or six of their diameters ;  the secondary undulations are relatively  
 wider than in the Ichthyosaurus, and the secondary branches are longer  
 and  more  bent;  the  tubes  divide  dichotomously  several  times  in  
 their course ;  the divisions,  after a slight divergence proceeding in the  
 same parallel line with each other and with the main stem.  The finer  
 secondary  branches  dilate  into  extremely  minute  cells  along  tracts  
 which run parallel  with  the  contour  of  the  tooth itself,  and occasion  
 the apparent alternation of opaque  and  clear  layers observable in the  
 section by transmitted light,  as  represented in  the  figure;  the  mode  
 of termination  of  the  calcigerous  tubes  is  shown  at  fig.  2,  PI.  74.  
 The  enamel  presents  the  same  fine  fibrous  structure  as  in  the  
 Ichthyosaurus. 
 The  mode  of  succession  of  the  teeth  of  the  Plesiosaur differs  
 from that of  the Ichthyosaur  in  the  growing  tooth  being  developed  
 in  a  cell  at  the  inner  side  of the  old  socket,  and  affecting  by  its  
 pressure  the  bone  of  the  jaw,  rather  than  the  tooth  about  to  be  
 displaced.