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
The grinding teeth underwent much more radical and striking changes.
At first (_†Mœritherium_) they were small, very low-crowned and of
simple pig-like or quadritubercular pattern, making two interrupted
cross-crests; all were in use simultaneously and the succession of
milk-teeth and premolars was by vertical replacement, as in normal
mammals generally. In _†Palæomastodon_ there were three pairs of
tubercles on the molars and in _†Gomphotherium_ these coalesced into
ridges, but in all the †mastodons there was more or less distinctness
of the conical tubercles. In one or more phyla the three-ridged plan
persisted for a long time, one such phylum terminating in the Pleistocene
_†Mastodon americanus_. In the other series the number of ridges
increased, first to four, then to five, six and more (_†Stegodon_); the
crowns of the teeth became much larger and higher, and the ridges, as
their number increased, became much thinner, and the valleys between
them were filled with cement, and finally, in the true elephants, with
their fully hypsodont, many-crested teeth, were thickly covered all over
with cement. The vertical succession of milk-teeth and premolars was
retained in _†Gomphotherium_, at least in some species, but the large
molars, which could not find room to be exposed while the premolars were
in place, came in successively from behind. This horizontal mode of
succession is the only one to be seen in the true elephants, in which but
one tooth, or parts of two, on each side of each jaw are in simultaneous
use and the premolars have entirely disappeared, but the milk-teeth are
retained.
The changes in the skull, which amounted to a reconstruction, were
very largely conditioned by the great increase in the length and
consequent weight of the tusks, in the size of the grinding teeth and the
development of the proboscis. In the earliest known type (_†Mœritherium_)
the skull had little about it that would, at first sight, suggest
proboscidean affinities; it was long and narrow, with sagittal crest
and occiput of normal type, very long cranial and very short facial
region. The nasal opening was directed forward and the nasal canal was
relatively long and horizontal in direction, but the nasal bones were
already much shortened, indicating that the proboscis was probably in
an incipient stage. The symphysis of the lower jaw was procumbent and
somewhat elongated, but to only a comparatively slight degree.
While the skull of _†Mœritherium_ was not obviously proboscidean, that
of its successor, _†Palæomastodon_, was unmistakably so, yet retained
several primitive features, which were lost in all of the subsequent
genera, such as the sagittal crest, the relatively low cranium and
moderate thickening of the cranial bones, the forward direction of the
nasal opening, etc.; the symphysis of the lower jaw was very greatly
prolonged.
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