240 TTNGULATA. 



M. 1432. The second left upper true molar ; from the Upper Eocene 

 of Caylux. Purchased, 1884. 



M. 75. Fragment of the left maxilla, containing portions of m. 1 

 and m. 2 ; from the Lower Miocene of Cadibona (Piedmont), 

 Italy. The teeth of this specimen agree precisely with 

 those of the palate figured by P. Gervais (op. cit.). 



Purchased, 1880. 



M. 75 a. Fragment of the right maxilla, containing the first true 

 molar, which agrees precisely with the corresponding tooth 

 of the last specimen ; from the Lower Miocene of Cadibona. 



Purchased, 1880. 



29593. Small fragment of the right maxilla 1 , containing m. 3 

 and the outer half of m- 2 ; from the Lower Miocene of 

 Cadibona. The teeth of this specimen agree in relative 

 size with those of M. 75 ; and it is probable that both 

 belong to the same species, whatever that species may really 

 be. The length of m. 3 is 0,043, which agrees with the 

 smallest form referred by Gastaldi to A. magnum. 



Presented by the Earl of EnnisMlen, 1855. 



11963. Cast of the symphysis and part of the right ramus of the 

 mandible, containing mm. 2, mm. 3, ram. 4, and mrnTi. The 

 original is the type specimen, and was obtained from the 

 Lower Miocene 2 of Lobsann, in Alsace. It is figured by 

 Cuvier in the ' Ossemens Fossiles,' 2nd ed. vol. iv. pi. xxxix. 

 fig. 5, and by De Blainville in the ' Osteographie,' Genus 

 Anthracotherium, pi. iii. 



Mantett Collection. Purchased, 1836. 



M. 2177. Fragment of the left ramus of the mandible of a young 

 individual, showing mm . 4 and mTT ; from the Upper Eocene 

 of Caylux. The teeth of this specimen agree precisely 

 with those of the last. The length of m . 1 is 0,028. 



Purchased, 1885. 



29907. The third right upper incisor of an Anthracotherium ; from 

 the Hempstead beds (Lower Miocene) of the Isle of Wight. 



1 This specimen has been hitherto referred to A. cuvieri (but without any 

 sufficient reason), and is so noticed by the present writer in the ' Palaeontologia 

 Indica,' ser. 10, TO!, ii. pp. 151, 153. The form of the loop connecting the two 

 columns, noticed on the latter page, appears to be due merely to wear. 



2 Teller (pp. cit. p. 57) correlates these beds with the Hempstead beds. 



