A history of land mammals in the western hemisphereScott, William Berryman
History
A history of land mammals in the western hemisphere
Scott, William Berryman
Mammals; Mammals, Fossil
[Illustration: FIG. 218.—Skull of _†Leptomeryx evansi_, White River.
(After Matthew.)]
The third phylum, that of _†Leptomeryx_, had about the same range in
time as the preceding one, though it has not yet been found in the
John Day, and the genus is assuredly known only from the White River
beds, in which it is not uncommon. _†Leptomeryx_ comprised a number of
species, all very small animals, and none larger than a jack-rabbit. (See
Fig. 277, p. 563.) In size, proportions and appearance, these dainty
little creatures must have been very like the existing chevrotains or
“mouse-deer” of Asia and the Malay islands, and by many writers they have
been classed in the same suborder, the Tragulina. The upper incisors had
been suppressed and the upper canine reduced to very small size, while
the lower canine had become functionally one of the incisors. The skull
had a very long and slender facial region, but had a less llama-like
appearance than in _†Hypertragulus_. The neck was short and the fore
limbs much shorter than the hind, so that the back sloped downward from
the rump to the shoulders, as in the chevrotains. There was a remarkable,
indeed quite unparalleled, difference between the fore and hind limbs and
feet, the hinder extremity being not only much longer, but also much more
specialized, while the anterior one retained in very large degree its
primitive characteristics. Thus, in the fore-arm the ulna was complete
and separate from the radius, but in the lower leg the fibula was reduced
to its minimum. In the manus there were four entire and functional
digits, in the pes only two, which were joined in a cannon-bone.
Finally, there was a fourth phylum, that of _†Hypisodus_, which was
confined to the White River stage and is still incompletely known. This
was a tiny creature, much smaller than any of the preceding ones, and
is the only known White River ungulate with fully hypsodont grinding
teeth. Another very exceptional peculiarity of its dentition was that in
the lower jaw it had ten incisor-like teeth; not only the canine, but
the first premolar as well, had assumed the character of the incisors.
This same peculiarity is found in the lower Miocene †gazelle-camel,
_†Stenomylus_ (see p. 394), but in no other mammal.
A considerable assemblage of genera belonging to this family occurs in
the upper Eocene, but the material yet obtained is too fragmentary to
permit the assignment of these forms to the different phyla, though it is
very probable that among them are to be found ancestors of all the White
River and subsequent genera.
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