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rses, the _fifth_ or "little" toe appears for the first time. As all the above-mentioned forms succeed one another in point of time, it may be regarded as probable that we shall yet be able to point, with some certainty, to some still older example of the _Equidoe_, in which the first digit is developed, and the foot assumes its typical five-fingered condition. [Illustration: Fig. 230.--Skeleton of the foot in various forms belonging to the family of the _Equidoe_. A, Foot of _Orohippus_, Eocene; B, Foot of _Anchitherium</>, Upper Eocene and Lower Miocene; C, Foot of _Hipparion_, Upper Miocene and Pliocene: D, Foot of Horse (_Equus_), Pliocene and Recent. The figures indicate the numbers of the digits in the typical five-fingered hand of Mammals. (After Marsh.)] Passing on to the Even-toed or _Artiodactyle Ungulates_, no representative of the _Hippotamus_ seems yet to have existed, but there are several forms (_Choeropotamus, Hyopotamus_, &c.) more or less closely allied to the Pigs (_Suida_); and the singular group of the _Anoplotheridoe_ may be regarded as forming a kind of transition between the Swine and the Ruminants. The _Anoplotheria_ (fig. 231) were slender in form, the largest not exceeding a donkey in size, with long tails, and having the feet terminated by two hoofed toes each, sometimes with a pair of small accessory hoofs as well. The teeth exhibit the peculiarity that they are arranged in a continuous series, without any gap or interval between the molars and the canines; and the back teeth, like those of all the Ungulates, are adapted for grinding vegetable food, their crowns resembling in form those of the true Ruminants. The genera _Dichobune_ and _Xiphodon_, of the Middle and Upper Eocene, are closely related to _Anoplotherium_, but are more slender and deer-like in form. No example of the great Ruminant group of the Ungulate Quadrupeds has as yet been detected in deposits of Eocene age. [Illustration: Fig. 231.--_Anoplotherium commune_. Eocene Tertiary, France. (After Cuvier.)] Whilst true Ruminants appear to be unknown, the Eocene strata of North America have yielded to the researches of Professor Marsh examples of an extraordinary group (_Dinocerata_), which may be considered as in some respects intermediate between the Ungulates and the Proboscideans. In _Dinoceras_ itself (fig. 232) we have a large animal, equal in dimensions to the living Elephants, which it further resembles in the s
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