ISO Albany Museum Records. 



I have much pleasure in naming the S. African species after 

 Mr. R. A. Albertyn. 



Gi/clot()sa\irus rohustiis occurs in the Upper Trias of Ger- 

 many, and it is probable that the S. African beds in which 

 C. A Ihertyni occurs, are of simitar age, since the Stormberg beds 

 immediately aljove are according to Seward, most probably of 

 Rhsetic age. 



On a new species of Oudenodori fO. megalo?^hinus) from the 

 Gough, S. Africa. By R. BROOM, M.D., &c. 



Close to Prince Albert Railway Station I recently found the 

 skull of a small Oudenodoti, which must be referred to a new 

 species. If the skull is mature, which the condition of the bones 

 would lead one to believe is not improbable, then it is the smallest 

 Oudenodon yet discovered. 



The upper surface of the skull and almost the whole of the 

 right side are practically perfect, but the left temporal arch and 

 the greater part of the left maxillary are lost. The main features 

 of the skull are the large size of the external nares, the narrow 

 interorbital region, with moderately broad parietal region, and the 

 great outward development of the squamosal bones. 



The posterior part of the skull resembles very closely that of 

 O, gracilis. The parietal foramen is, however, here situated in 

 an elevated portion of the skull roof. The preparietal bone is of 

 large size, and is supported on either side by the parietals. The 

 squamosal resembles considerably that of O. gracilis in the 

 peculiar outward development of the part which forms the tem- 

 poral arch. In this new species the outward process is much 



