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
(8) The limb-bones increased in thickness until they became extremely
massive, to carry the immense weight of the body, and they eventually
lost the marrow-cavities, which were filled up with spongy bone, a
great gain in strength. As is generally, though not universally, true
of the large and heavy mammals, there was no coössification between the
limb-bones and no great increase in their proportionate length. The
thigh-bone, or femur, lost the cylindrical shape of the shaft, becoming
flattened and very broad, and acquiring something of the appearance of
the same bone in the elephants.
[Illustration: FIG. 166.—Right manus of †titanotheres. _A._,
_†Titanotherium_, White River (after Marsh). _B._, _†Palæosyops_,
Bridger, Princeton University Museum.]
(9) There was no loss or coössification of elements in wrist (carpus)
or ankle (tarsus) and _no reduction of digits_ within the limits of the
family. In the latest, largest and most specialized genera, as well as
in the earliest, smallest and most primitive, there were four toes in
the front foot and three in the hind. We have the most cogent reasons
for assuming that all mammals were derived from ancestors which had
five toes in each foot, neither more nor less. If this be true, then
the most ancient known †titanotheres, which were small and light, had
already suffered the loss of the first digit in the fore foot and of the
first and fifth digits in the hind foot, but there reduction ceased.
With the growing body-weight, long, narrow and slender feet would have
been a detriment, whereas in swift-running animals, like horses and
deer, long and very slender feet are a great advantage. The contrast is
both striking and instructive, showing the importance of a short, broad,
polydactyl and pillar-like foot to very large and heavy mammals, all of
which have feet of this character.
(10) The hoofs, as shown by the terminal bones (ungual phalanges) which
formed their bony cores, were reduced in size until they became mere
nail-like excrescences around the border of the massive foot.
3, 4. _Tapiridæ and †Lophiodontidæ. Tapirs and †Lophiodonts_
The history of the tapir family is not at all satisfactorily known,
partly because tapirs are comparatively rare as fossils in all of the
Tertiary formations, and still more for the reason that the specimens so
far collected are so fragmentary, not a single half-complete skeleton
among them. Had these animals actually been as rare in North America
as the fossils would seem to indicate, they could not possibly have
maintained themselves for so long a time, throughout nearly the whole of
the Tertiary and Quaternary periods. For some reason, probably because
they have always been forest-haunting animals, their habits must have
kept them in places remote from the areas where the accumulation of
sediments was in progress, and thus only occasional stragglers were
buried and preserved.
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