
 
		polygonal  when  viewed  from  the  front,  but  this  shape  
 disappears in posterior view. He therefore conduded that  
 J. hexagonus was unfounded. Given the variability of centra  
 with their position in the vertebral column, and the infrequency  
 with which  they  are seen end-on, his objection is  
 valid. 
 Ichthyosaurus  hüdesiensis Koken,  1883 
 This  species was  erected  on some vertebrae,  and  a tooth,  
 from the Lower Cretaceous of northern Germany (Koken,  
 1883:  761,  pi.  24,  figs.  1-3). The material is indeterminate. 
 Ichthyosaurus  indicus Lydekker,  1879 
 L ydekker  described  fifteen  assodated  vertebrae  from  a  
 Cretaceous horizon in India, which he considered equivalent  
 to the English Upper Greensand (Albian). By his own  
 admission he could not be “absolutely certain of the specific  
 distinctness  of  the  Indian  form.”  However,  he  still  
 thought it worthwhile to erect the new species to show the  
 geographical range of the genus. The material is indeterminate. 
 Ichthyosaurus kokeni BrOili,  1908 
 This spedes was based by Broili  (1908: 433,fig.  3,  pi.  14,  
 figs. 1-10) on a complete humerus (fig. 3), a partial humerus, 
   intermedium,  a  basiocdpital,  and  several  vertebrae.  
 The  complete  humerus  is  much  expanded  proximally,  
 probably due to a compression distortion. This indeterminate  
 material is from the Lower Cretaceous of Grodischt, in  
 the Carpathian Mountains  of Romania. 
 Ichthyosaurus  lacunosae Quenstedt,  1885(? ) 
 Kuhn (1934:43) dted Quenstedt (1867) as the authority for  
 this Early Jurassic  spedes, but  this  reference was not  in-  
 duded in the literature dted, nor is there an entry for 1867  
 in the Bibliography o f Fossil  Vertebrates. The  spedes I.  lacunosae  
 is  briefly  treated  in  Quenstedt  (1885:  207),  where  
 reference is made to some caudal vertebrae. It is not clear  
 whether  this  is  the  first  dtation  of  the  species,  but  the  
 material  is  indeterminate. 
 Ichthyosaurus  latifrons Owen,  1840 
 König used this name for a poorly preserved partial skull  
 -  presumably from the Lower Lias -  without any description, 
   making  I.  latifrons  K önig,  1825  a  nomen  nudum.  
 Owen  (1840:  122-123)  gave  a  very  brief  description  in  
 which he referred to its unusually large parietal foramen,  
 and noted that, “the articular surfaces of the bodies of the  
 vertebrae  present  a  flattened  circumference.”  The  name  
 accordingly  first became  available  in  1840.  Owen  subsequently  
 gave  an  extended  description,  figuring  König’s  
 partial skull (Owen, 1881:119, pi. 27, fig. 1). This same skull 
 (BMNH R1122) was figured by L ydekker  (1889A:  fig.  33),  
 but  he  confused  the  issue  by  figuring  a  second  skull  
 (1889A:  fig.  31)  that has  subsequently  been  identified  as  
 Leptonectes tenuirostris. L ydekker also included a specimen  
 which has now been  identified  as Eurhinosaurus  longiros-  
 tris. Owen’s  (1881) description referred  to a second specimen, 
   an incomplete  skeleton,  “lacking both  ends,  but  including  
 the trunk, with chief part of the skull  .... ”. However, 
   much  of  his  description was  based  upon  the  partial  
 skull, which he figured in dorsal view. The skull exhibits a  
 broad expanse of the  frontals, but this is because the posterior  
 margins  of  the  nasals,  and  medial margins  of  the  
 postfrontals,  are  incomplete.  If  these  elements were  not  
 damaged  they would  overlie more  of  the  frontals,  as  in  
 Ichthyosaurus communis. The only unusual feature cited by  
 Owen  in his description was the shortness of the angular,  
 which,  “disappears  parallel with  the  hind  border  of  the  
 orbit.”  The  incomplete  preservation  of  the  skull  makes  
 adequate comparisons with other  taxa difficult. 
 Ichthyosaurus  leucopetraeus Burmeister  et  Giebel,  1862 
 This  species was  erected  upon  a  single  vertebra  and  rib  
 fragment, from the Jurassic of Rio de Copiapo, Chile (Burmeister  
 &  Giebel, 1862:123). The material is indeterminate. 
 Ichthyosaurus  nasimowii  Fahrenkohl,  1856 
 This Early Jurassic species was erected upon two vertebral  
 centra  (Fahrenkohl,  1856:  pi.  2).  Both  are  unusual.  The  
 first  (Fahrenkohl,  1856:  pi.  2,  fig.  1)  is remarkable for its  
 tapering shape, whereby one of its articular surfaces, probably  
 the posterior, has  a smaller diameter  than the other.  
 The other is unusual for the enormous depression on either  
 side,  for articulation with the  ribs. These paired rib facets  
 extend  from  the  anterior  to  the  posterior  surfaces  of  the  
 centrum, and are reminiscent of those of plesiosaurs. However, 
  the neural arch is unfused (and lost), and there are no  
 ventral facets for the chevrons. The tapered first  centrum  
 resembles the  terminal caudals of a plesiosaur, but, again,  
 there  are  no  chevron  facets,  and  there  are  no  lateral  rib  
 facets. The centra are probably best regarded as pathological. 
 Ichthyosaurus  normanniae Valenciennes,  1861B 
 This  species was based  on some  cranial bones,  including  
 the  basisphenoid  and  basiocdpital,  from  the  Kimmerid-  
 gian  of  Normandy,  France  (Valenciennes,  1861B:  1001).  
 The basiocdpital (Lennier,  1870:  pi.  6, fig.  7) appears  typical  
 of Ophthalmosaurus.  Bardet  et  al.  (1997)  referred  this  
 largely indeterminate material to  Ophthalmosaurus  sp. 
 Ichthyosaurus  numismalis  Fraas,  1892 
 Fraas  (1892:  30, pi.  1) founded this species upon a rostral  
 segment, 0.25 m long, from the Lower Lias (Lower Jurassic: 
 lower Pliensbachian) of Kirchheim, Germany. The material  
 is inadequate for diagnostic purposes. 
 Ichthyosaurus  ovalis  Phillips,  1871 
 Erected  for  some  “anterior  dorsal,  posterior  dorsal,  and  
 anterior caudal” vertebrae whose centra were said to have  
 “an  oval  outline  of  face” which was  higher  than  broad  
 (PHILLIPS,  1871:  339).  Such laterally compressed centra are  
 typical of apical and post-flexural vertebrae (see above  in  
 descriptive  section;  Fig.  12).  From  the  Kimmeridge  Clay  
 (Upper  Jurassic:  Kimmeridgian)  of  Swindon  (Wiltshire)  
 and  Shotover  (Oxfordshire), England. 
 Ichthyosaurus planartus  Theodori,  1854 
 Named for the relative flatness of the dorsal articulations  
 of  the  vertebral  centra,  this  species was  erected  upon  a  
 rather fragmented and scattered partial skeleton. The skeleton, 
   from  the Upper  Lias  (Toarcian)  of  Banz,  Germany  
 was  distributed  over  three  separate  slabs,  believed  to  be  
 associated. The first slab  contained many scattered vertebrae, 
   ribs,  and  a  humerus;  the  second  a  vertebral  series  
 with rib fragments; and the third a number of large mandibular  
 fragments,  cranial  elements,  teeth,  vertebrae, many  
 complete  ribs,  a  scapula  and  coracoid.  The  teeth  were  
 described as being indistinguishable from those of L. tenuirostris, 
  and the scapula and humerus resembled those of I.  
 trigonodon.  However,  the  dorsal  vertebrae  were  said  to  
 differ from all other Banz species by the roundness of their  
 centra. 
 The  incompleteness-of  the  holotype,  and  the  minor  
 differences of the vertebral centra, undermine the validity  
 of the species. 
 Ichthyosaurus polyptychodon Koken,  1883 
 Koken (1883:737, pi. 23, fig. 1) based this species on a skull  
 fragment  that  extended  from  the  anterior margin  of  the  
 orbit to the posterior boundary of the  external naris. This  
 indeterminate material  is  from  the  Lower  Cretaceous  of  
 northern  Germany. 
 Ichthyosaurus  posthumus W agner,  1852B 
 Erected upon a single and quite unremarkable tooth from  
 the Upper Jurassic of southern Germany (Wagner,  1852B:  
 702, pi.  4, figs. 4-5). 
 Bauer  (1898: pi. 2 7 ) figured the tail region of an ichthyosaur  
 which he  referred  to  as  Ichthyosaurus  trigonus  var.  
 posthumus  (in modern  taxonomic  practice,  this would be  
 considered as a subspecies). This material, like W agner’s,  
 is  clearly indeterminate. 
 Ichthyosaurus  psilonoti  Fraas,  1891 
 Fraas  (1891:  41) briefly described  this Early Jurassic species, 
   based  on  some  teeth, which he  said were  similar  to  
 those of Ichthyosaurus  communis.  Such  teeth  are not diagnostic. 
 Ichthyosaurus  quenstedti Zittel,  1890 
 Zittel (1890:  4 5 8 ,  fig. 4 2 7 )  erected  this Early Jurassic species  
 upon  a  small  segment  of  the  rostrum.  The material  
 lacks  any particular distinguishing features. 
 Ichthyosaurus  rheticus Sauvage,  1876 
 This was the second Rhaetian species that Sauvage (1876)  
 described on the basis of vertebral features, in his one-page  
 note  on  ichthyosaurs  from  Saone-et-Loire,  France. As  in  
 I. carinatus,  the material is not determinate. 
 Ichthyosaurus  saladensis Rusconi,  1949 
 Although most of the ichthyosaurs Rusconi  (1949)  treated  
 in this paper were from the Late Jurassic, he also described  
 some material from the Cretaceous. Ichthyosaurus saladensis  
 was erected upon some jumbled bones and teeth that Rusconi  
 (1 9 4 9 :7 0 -7 2 , fig. 11) interpreted as parts of the maxilla  
 and  mandible.  The  material,  which  is  indeterminate,  is  
 Early Cretaceous  (Berriasian) in  age. 
 ?Ichthyosaurus  sanjuanensis  Rusconi,  1949 
 This  species  was  erected  upon  two  vertebrae  from  the  
 Lower Jurassic of the Quebrada Honda, San Juan Province,  
 Argentina (Rusconi, 1949:  90,  figs.  1-2). The generic designation  
 was  in  some  doubt.  In  any  event,  the material  is  
 indeterminate. 
 Ichthyosaurus  sinuatus  Theodori,  185 4 
 Kiprijanoff  (1881:  8 7 ,  8 9 )  cited  Theodori  (1 8 5 4 )  as  the  
 authority of this species, from the Lias of Banz,  Germany.  
 This is because Theodori (1854: 5 0 ) had used it as a variety  
 name for I. tenuirostris. Little information was given for the  
 species, but Kiprijanoff  (1881:  pi.  18)  figured a tooth. This  
 material  is  indeterminate. 
 Ichthyosaurus steleodon Bogolubow, 1909 
 Bogolubow  (1909:  5 0 ,  figs.  1-2; pi.' 2,  figs.  6 -1 0 ) based this  
 species  upon  the  anterior  portion  of  a  rostrum  with  a  
 fragmentary left mandibular ramus, a second mandibular  
 segment,  and  a  vertebra.  The  teeth  are  fairly  long  and  
 robust,  without  any  indication  of  reduction,  which  suggests  
 the material might be referable to Platypterygius. This  
 material,  from  the  Lower  Cretaceous  (Hauterivian-Bar-  
 remian) of the Ul’yanovsk Region of Russia, is clearly too  
 incomplete for the erection of a new species.