An introduction to the study of mammals living and extinctLydekker, Richard
Science
An introduction to the study of mammals living and extinct
Lydekker, Richard
Mammals
_Chœropotamidæ._—In this family the molars are intermediate in
structure between those of the _Suidæ_ and the next family. The upper
ones have very broad crowns, with the five columns arranged as in
_Anthracotherium_; while the premolars are not secant, and may be
very large. The best known forms are the small _Cebochœrus_ of the
Phosphorites of Central France; _Chœropotamus_ of the Upper Eocene, the
type species of which was of the size of a large Pig, with the dental
formula _i_ ³⁄₃, _c_ ¹⁄₁, _p_ ⁴⁄₃, _m_ ³⁄₃, and no distinctly selenodont
structure in the molars; the much larger _Elotherium_, from the Upper
Eocene and Lower Miocene of both the Old and New Worlds, which presents
the very rare feature of the absence of a third lobe to the last lower
molar; and the equally large _Tetraconodon_ of the Pliocene of India,
in which this third lobe was present and the premolars were of enormous
size. The remarkable North American Eocene genus _Achænodon_ should
perhaps also be placed here.
[Illustration: FIG. 112.—A right upper molar of _Merycopotamus pusillus_,
Pliocene, India. (From the _Palæontologia Indica_.)]
_Anthracotheriidæ._—The genera _Anthracotherium_ and _Hyopotamus_, of
the upper Eocene and Miocene, have the typical Eutherian dental formula;
the upper molars (Fig. 111) carrying three columns on the anterior and
two on the posterior half of the crown, all of which are of a more or
less decidedly selenodont structure. The mandible has a descending
flange at the angle. The figured tooth (in which the antero-internal and
antero-median columns are imperfect) may be compared with the diagram
given in Fig. 5, p. 32, when the homology of the columns or tubercles
will be at once apparent, the broken antero-median column representing
the protoconule. Some of the species are of large size, while others are
comparatively small.
_Merycopotamus._—The genus _Merycopotamus_ of the lower Pliocene
of India may be regarded as an Anthracotheroid which has lost the
antero-median column to the upper molars (Fig. 112), so that these teeth
are consequently quadrituberculate; and may thus be regarded as typical
examples of the brachy-selenodont modification of molar structure.
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