a ~ 
== 
Parr IV. Secr. i, § 2.] EOCENE, 843 

With these animals there coexisted large and small carnivores and 
some lemuroid monkeys.’ 


———e 
— 
i eae 

Fic. 406.—Dernoceras (Marsn) (5). Restoration of SKELETON BY Proressor Marsu. 
§2. Local Development. 
Great Britain.?—Entirely confined to the south-eastern part of 
_ England, the British Eocene strata occupy two synclinal depressions in 
1 The restoration of Deinoceras in Fig. 406 has been kindly supplied Ly Professor 
Marsh. 
2 See Conybeare and Phillips, Geology of England and Wales; Prestwich, Q. J. 
Geol. Soc. vols. iii., vi. viii., x., Xi., xiii.; Edward Forbes, “Tertiary Fluvio-marine 
Formation of the Isle of Wight,” Mem. Geol. Surv. 1856; H. W. Bristow, “ Geology of 
the Isle of Wight,” Mem. Geol. Surv. 1862; Whitaker, “Geology of London Basin” in 
