Evolution and Classification of the Pocket Gophers of the Subfamily Geomyinae — John Shaqi
Evolution and Classification of the Pocket Gophers of the Subfamily GeomyinaeRussell, Robert J.
Science
Evolution and Classification of the Pocket Gophers of the Subfamily Geomyinae
Russell, Robert J.
Pocket gophers
In Pliocene Geomyinae the two columns of the molars tend to merge into
one. This is evident on the worn occlusal surface of the teeth; the
lateral re-entrant folds are shallow vertically and progressively
recede laterally until only a slight inflection remains. In the final
stages of attrition, the inflection disappears and the tooth is a
simple elliptical column. In the Pleistocene the monoprismatic pattern
appears at earlier stages of wear owing to the decrease in depth of
the re-entrant folds, and in Geomyinae of Recent time the initial
stages of wear on the enamel cap of infants erase the last vestiges of
two columns in the molar teeth.
The general trend in evolution, therefore, has been from a bicolumnar
to a monocolumnar pattern. The particular patterns of wear
characterizing each genus are described in detail beyond.
The third upper molar has evolved less rapidly than the first and
second and in one of the modern lineages (tribe Geomyini) tends to
retain at least a vestige of the primitive bicolumnar pattern in
the final stage of wear. Therefore, the loss of any trace of the
bicolumnar pattern in M3 is considered to be a much specialized
condition. Unfortunately, the fossil record of the third upper molar
is less complete than that for the first molar and second molar; the
tooth drops out of its alveolus more often than does any one of the
other molariform teeth and is seldom recovered.
_Character of Enamel Patterns_
In the primitive genera the enamel pattern is bilophate and the
enamel loop (see Fig. 4B) is continuous on the occlusal surface of
a worn molar. Concomitant with the union of the double columns, the
bilophodont pattern is reduced to a single loph, but the enamel still
completely encircles the dentine.
In the molars of modern geomyines, the enamel loop is not continuous
but is interrupted on the sides of the crown by vertical tracts of
dentine that are exposed at the occlusal surface of the tooth during
early stages of wear. Therefore, a continuous enamel band is to be
found only in a juvenal individual whose teeth have been subjected to
only slight attrition on the enamel cap. In molars lacking enamel on
the labial and lingual sides, anterior and posterior enamel plates, or
blades, are found on each molar. The premolar also has an enamel plate
on the anterior surface and another on the posterior surface, and in
addition both re-entrant angles are protected by a V-shaped investment
of enamel. One or the other of the various plates can be reduced or
lost accounting for the several distinctive tooth-patterns of the
modern geomyines. If loss occurs, it usually is the anterior plate in
the lower dentition and the posterior plate in the upper dentition,
including the upper premolar. When reduction of the posterior plate of
the upper cheek teeth occurs, enamel is first lost from the labial
side of the tooth, thus leaving only a short vestigial plate on the
lingual end of the crown.
_Grooving of Incisors_
Public-domain text, read in full here on John Shaqi.
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