248 FROM OR OH I FPUS TO MIOHIPPUS chap. 



has a well-marked coracoid process. The radius and ulna are 

 separate ; so too are the tibia and fil)ula. EoM/ppus, belonging 

 to the same sub-family, is slightly more primitive ; for the hind- 

 feet have a rudiment of digit I. OroUipims is a little nearer to 

 the Horses in that the molar teeth have acquired a little further 

 advance towards the equine type. Instead of the tubercles of the 

 teeth remaining for the most part separate, they have fused into a 

 set of ridges, of which, however, the pattern is less complex than 

 in the modern Horses. In other respects Orohi^^pus is much like 

 Hyracotherium. Pachynoloplms seems to be but a synonym. 



The next stage is shown by Mesohijrpi'S, a Lower ]\Iiocene 

 form, usually referred to the neighbourhood of Palaeothcnmn. It 

 has nearly lost one of the toes of the fore-foot, a rudiment only 

 remaining ; the metapodials, at any rate of the fore-feet, seem to 

 be slightly increased in length. The orbit is not encircled by 

 bone, but there is a strong process from the frontal, wiiich nearly 

 meets the zygomatic arch. 



Anchiiheriiim, from the Upper jMiocene, is not far removed in 

 structure from the last-mentioned form ; it is a trifle nearer the 

 existing Horse in several points. The ulna is further reduced and 

 fused with tlie radius below ; the rudiment of digit V is still 

 more rudimentary ; the two lateral digits are smaller in proportion 

 to the central one than they are in Mcsohij^piis ; the fibula is 

 fused Ijelow with the til)ia. I'rom this form to Equvs is a small 

 series of steps, characterised by the still further reduction of all the 

 digits except III, l)y the still further reduction of the already 

 rudimentary ulna and fibula, and by the increasing depth of the 

 molar teeth, which are of course, in Equus, hypselodont. 



Another interesting conclusion may seem to follow when we con- 

 sider the geographical range of the ancestral Horses. Hyracotherium 

 and Pachynoloplms occurred both in the Old and New World. 

 From them may have arisen the Horses of both hemispheres. 

 After that point there is a division. Mrsohippus is American, 

 and we get at Equus in that continent through Desmatippus and 

 Protohippus. On the other hand there are no remains known of 

 Mesohippiis in Europe ; and unless subsequent researches prove 

 the existence of Mesohippus, we have to rely upon forms which 

 are placed with Anchitherium and Hiptparion. 



It seems that in America the next genus in the direct line 

 of equine descent to Mesohippus is Mioliippius. It is smaller in 



