| OCR Text |
Show 1902.] DR. 0. I. FORSYTH MAJOR ON PLIOCENE VOLES. 105 West Runton type occurs together with the Crag types. The larger of the Crag-forms is besides represented by specimens from Bramerton (text-fig. 14, nos. 14 ft, b) and from Kyson in Suffolk. Text-fig. 14. Teeth of Tertiary Voles, enlarged. Figs. 10-17. Views of first lower molars. a=outer aspect, &=inner aspect (except 14J=upper view).-Fig. 10. Mimomys neivtoni, sp. n., same specimen as fig. 7.-Fig. 11. Mimomys intermedins (Newt.), same specimen as fig. 1.- Fig. 12. Mimomgs intermedins (Newt.), same specimen as fig. 21-Fig. 13. "Mimomys intermedins (Newt.)," same specimen as fig. 26, right side; West Runton (B. M . No. 6968 e, from Savin Coll. No. 1705).-Fig. 14 a. Mimomys plioccenicus (Maj.), Norwich Crag, Bramerton (Norwich Castle Mus. No. 728, from Reeve Coll.).-Fig. 14 b. The same, upper view.-Fig. 15. Same specimen as fig. 20, Mimomys plioccenicus (Maj.), Norwich Crag, Thorpe (Norwich Castle Mus. No. 971).-Fig. 16. Mimomys newtoni (?), East Runton Forest Bed (B. M . No. 6967 b, from Savin Coll. No. 464).-Fig. 17. Mimomys plioccenicus (Maj.), same specimen as fig. 5. For the present I content myself with three specific names, calling (1) plioccenicus the larger Crag-form, which I identify with the one from the Val d'Arno; (2) newtoni, a smaller rooted |
