Lizards. 

 Table-case. 

 No. 3. 



26 Squa/mata Ijticertilia, Anguidcc, Varanidce, etc. 



rhombifer and P. depressus. Others are recorded from the 

 Miocene of CEningen and the Lignites of Bonn-on-the-Rhine, and 

 are exhibited in this case. 



SUB-ORDER 2. Lacertilia (Lizards). 



The earliest known member of the large group of existing 

 Lacertian reptiles is Macellodus (with which Saurillus is pro- 

 bably identical, or closely allied), mostly known by jaws and teeth 

 from the Purbeck beds of Swanage, Dorset, a small lizard with 

 pleurodont dentition, dermal scutes, and procoelous vertebrae. 



Coniasaurus, with expanded teeth, occurs in the Chalk of 

 Kent and Sussex. Several genera of lizards are represented in 

 the Tertiaries of France and America. Remains of a species of 

 Iguana occur in the Eocene Phosphorites of France, and the 

 Middle Eocene of Hordwell, Hampshire. 



FIG. 31. (A) Outer, and (B), inner views of the left dentary bone of an Anguoid 

 Lizard ; from the Eocene Phosphorites of Cay lux, France. . 



The Anguidce (Slow-worms) are represented by several 

 genera from Gers in France (Middle Miocene), and from Rott, 

 near Bonn (Lower Miocene); from Steinheim, Bavaria; and 

 from England and North America. 



FIG. 32. (A) Eight Maxilla; (B) Anterior, and (C) Posterior views of a dorsal 

 vertebra of Varanus bengalensis (Daudin), Pleistocene, Madras. |. 



The VaranidcB (Monitors) are represented by a very large 

 form Megalania, from Queensland, Australia, and by Varanus 



