14 ANOMODONTIA. 



Seeley in the 'Quart. Journ. Geol. Soc' vol. xxxiv., pi. xxxii. 

 figs. 1-3, as the type of P. griersoni does not appear to 

 be specifically distinct from the present specimen ; the 

 parietal foramen being, if anything, larger than the latter. 

 The narrowness of the bone figured as the quadrate is 

 apparently due to imperfection. 



Presented by W. G. Atherstone, Esq., M.J). 



R. 794. The imperfect skull, much concealed by matrix ; from 

 Tafelberg. This specimen appears to be identical in size 

 and contour with the preceding. Purchased, 1886. 



R. 518. A smaller and less imperfect skull ; from Tafelberg. This 

 specimen cannot apparently be specifically distinguished 

 from the type ; neither is it apparent how the skull 

 figured by Seeley in the ' Quart. Journ. Geol. Soc' 

 vol. xxxiv. pi. xxxii. figs. 7-8, as the type of P. cuneiceps, 

 differs from this specimen. 



By exchange with the Blomfontein Museum, 1884. 



R. 795. An imperfect skull, with traces of other bones, much con- 

 cealed by matrix ; from Tafelberg. This specimen seems 

 to agree exactly with the preceding. Purchased, 188(5. 



Procolophon minor, Owen \ 



Founded upon a skull which, if adult, indicates a smaller species 

 than the preceding. This skull appears to be somewhat more 

 depressed than that of P. trigoniceps, with a relatively wider inter- 

 orbital bar, and without a lateral expansion of bone in the qua- 

 dratic region. 



Hah. South Africa. 



R. 1727. The somewhat imperfect skull ; from the Karoo system of 



{Fig.) the Tafelberg. The type ; figured by Owen in his 



' Catalogue of the Fossil Reptilia of S. Africa,' pi. xx. 



figs. 8-12. Since the specimen was figured part of the 



left side of the occiput has been cleared from matrix. 



Presented by W. G. Atherstone, Esq., M.D., 1875. 



Cat. Foss. Rept. S. Africa, p. 26 (187G). 



