The Cambridge natural history, Vol. 10 (of 10)Beddard, Frank E. (Frank Evers)
Science
The Cambridge natural history, Vol. 10 (of 10)
Beddard, Frank E. (Frank Evers)
Animals; Mammals
In the mode of the articulation of the lower jaw to the skull the Mammalia
apparently, perhaps really, differ from other Vertebrates. In the Amphibia
and Reptilia, with which groups alone any comparisons are profitable, the
lower jaw articulates by means of a quadrate bone, which may be movably or
firmly attached to the skull. In the mammals the articulation of the lower
jaw is with the squamosal. The nature of this articulation is one of the
most debated points in comparative anatomy. Seeing that Professor
Kingsley[14] in the most recent contribution to the subject quotes no less
than fifty-two different views, many of which are more or less convergent,
it will be obvious that in a work like the present the matter cannot be
treated exhaustively. As, however, Professor Kingsley justly says that "no
single bone occupies a more important position in the discussion of the
origin of the Mammalia than does the quadrate," and with equal justice adds
that "upon the answer given as to its fate in this group depends, in large
measure, the broader problem of the phylogeny of the Mammalia," it becomes,
or indeed has long been, a matter which cannot be ignored in any work
dealing with the mammals. A simple view, due to the late Dr. Baur and to
Professor Dollo, commends itself at first sight as meeting the case. The
last-named author holds, or held, that in all the higher Vertebrates it is
at least on _a priori_ grounds likely that two such characteristically
vertebrate features as the lower jaw and the chain of bones bringing the
outer world {27} into communication with the internal organ of hearing
would be homologous throughout the series. He believed, therefore, that the
entire chain of ossicula auditus in the mammal is equal to the columella of
the reptile, since their relations are the same to the tympanum on the one
hand and to the foramen ovale on the other; and that the lower jaw
articulates in the same way in both. It follows, therefore, that the
glenoid part of the squamosal must be the quadrate which has become
ankylosed with it after the fashion of concentration in the mammalian skull
that has already been referred to. The fact that occasionally the glenoid
part of the squamosal is a separate bone[15] appeared to confirm this way
of looking at the {28} matter. But the hall-mark of truth is not always
simplicity; indeed the converse appears to be frequently the case. And on
the whole this view does not commend itself to zoologists at present. For
it must be borne in mind that the lower jaw of the mammal is not the
precise equivalent of that of the reptiles. Apart from the membrane bones,
which may be collectively the equivalents of the dentary of the mammal,
there is the cartilaginous articular bone to be considered, which forms the
connexion between the rest of the jaw and the quadrate in reptiles. Even in
the Anomodontia, whose relations to the Mammalia are considered elsewhere,
there is this bone.
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