trasmas. 171 



48733. A canine ; from Brixham Cave, near Torquay. This spe- 



(Fig.) cimen is figured by Busk in the Phil. Trans, for 1873, and 



is provisionally referred to the present species. 



Brixham-Cave Collection. Presented, 1876, 



44926. The glenoidal extremity of the left scapula ; from the Pleis- 

 tocene of Ilford, Essex 1 . This specimen is No. B. 4 of 

 Davies's ' Catalogue of the Brady Collection ' (1874). 



Brady Collection. Purchased, 1878. 



21287. The left humerus ; from the Pleistocene of Grays, Essex. 



Purchased, 1848. 



21288. The distal extremity of the right humerus ; from the Pleis- 



tocene of Grays. This specimen is of unusually large 

 dimensions. Purchased, 1848. 



38512. The left ulna ; from the Pleistocene of Ilford. 



Purchased, 1848. 



24361. The left ulna ; from Pleistocene beds in a railway-cutting 

 near Kew Bridge. This specimen is of very large size, 

 but in its slender form agrees with the last example. 



Presented by T. Layton, Esq., 1849. 



47683. The proximal half of the left ulna ; from a cavern in Wind- 



(Fig.) mill Hill, Gibraltar. This specimen is figured by Busk in 



the Trans. Zool. Soc. vol. x. pi. vi. fig. 1; its specific 



reference is provisional. Brome Collection. Presented, 1876. 



44927. The distal extremity of the right radius; from the Pleis- 

 tocene of Ilford, Essex. This specimen is No. B. 5 of 

 Davies's ' Catalogue of the Brady Collection.' 



Brady Collection. Purchased, 1878. 



16852. The right radius : from Kent's-Hole Cavern, Torquay. The 



reference of this specimen is provisional; but it differs 



from the radius of U. spelceus by its more elongated form. 



McEnery Collection. Purchased, 1842. 



24961. The left scapho-lunar ; from the Pleistocene of Grays, Essex. 

 Presented by D. Sharpe, Esq., 1850. 



1 This and the other specimens of Ursine remains from the Ilford brick-earth 

 are only provisionally referred to the present species, as it is said that Ursus 

 arctos also occurs there. The complete tibia noticed below agrees so closely with 

 that of U. horribilis, that on this account, as well as from the circumstance of 

 the common occurrence of that species in the Pleistocene of Grays, the Ilford 

 remains are provisionally referred to U. horribilis rather than to U. arctos. 



