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
No representative of this series has yet been found in the upper
Oligocene; and it is not yet possible to say whether their absence
from the John Day beds, as in several other cases already referred to,
was due to an actual geographical difference in contemporary faunas,
or whether it is merely one of the accidents of preservation and
collecting. In the upper White River, however, was another most curious
animal (_†Protoceras_), a forerunner, if not a direct ancestor, of
_†Syndyoceras_. The exact relationship between the two forms can hardly
be determined, until the genera, one or more, which once connected them
shall have been recovered, though it is obvious that they belonged to the
same series. _†Protoceras_ was a smaller animal and, if anything, an even
more bizarre-looking object, for the anterior protuberances were broad,
prominent and everted plates of bone, not even suggesting horns in their
form, and the posterior pair were short and club-shaped; in the female
neither pair was more than indicated. The dentition was very similar
to that of _†Syndyoceras_, except that the upper tusk was considerably
larger and scimitar-shaped; the female had no tusks. In the fore-arm
the two bones were just beginning to coalesce, but in the lower leg the
fibula was completely reduced. The manus had four complete and functional
digits, the laterals not very much shorter and thinner than the median
pair; but the pes was already didactyl, though the metatarsals were
separate, not fused into a cannon-bone; two long and pointed splints
were the vestigial remnants of the second and fifth digits.
[Illustration: FIG. 217.—_†Protoceras celer_, skull of male. (After
Osborn and Wortman.)]
It is not yet possible to trace this phylum below the level of the
uppermost White River beds, yet that will very probably be accomplished
by future exploration.
The second phylum of the family was represented in the lowest Miocene
by _†Hypertragulus_, a genus of much smaller animals than those of the
preceding series, which went back to White River times without essential
change, and was abundant in the John Day stage. Despite this fact, the
structure of the genus is still incompletely known and much remains
to be learned, but enough has already been ascertained to justify
the association of this phylum with the _†Protoceras-†Syndyoceras_
series in one family as reasonable. The number of upper incisors in
_†Hypertragulus_ has not been ascertained, but the canines were enlarged
and tusk-like, the lower one not having gone over to the incisors, as it
had in the preceding group. The skull had much resemblance to that of the
contemporary camels, the sudden narrowing of the facial region giving it
a very llama-like appearance; the orbit was open and on the face in front
of it was a conspicuous vacuity. The ulna and radius were coössified and
there were four digits in the manus, two in the pes, but no cannon-bone
was formed.
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