The zoology of the voyage of H.M.S. Beagle [vol. 1 of 5] : $b Fossil mammaliaOwen, Richard
Science
The zoology of the voyage of H.M.S. Beagle [vol. 1 of 5] : $b Fossil mammalia
Owen, Richard
Beagle Expedition (1831-1836); Mammals, Fossil; Paleontology -- South America; Zoology
In the Megatherium the upper articular surface of the astragalus is also
divided into two trochleæ, of which the one on the fibular side (fig. 3,
_a_), is of much greater relative size and extent than the tibial one
(_b_), and is raised nearly four inches above the level of the latter,
although in the oblique position in which the bone is naturally placed
in the skeleton, the highest part of each convexity is on the same
level. The fibular trochlea differs also from that in the Scelidothere
in being regularly convex in the transverse as well as the
antero-posterior direction. The tibial convexity resembles that in the
Scelidothere, save in its smaller relative size; its internal margin
likewise forms an angular projection below the internal malleolus.
The upper surface of the astragalus of the Mylodon, or Megalonyx(?) (Pl.
XXVIII. fig. 5.),[56] differs from that in the Megatherium in having a
narrower fibular trochlear ridge.
The astragalus of the Ai (_Bradypus tridactylus_) differs widely from
that of either the Megathere, Mylodon(?) or Scelidothere in having a
conical cavity on the upper surface, in place of the fibular convexity,
in which concavity the distal end of the fibula rotates like a pivot.
This mechanism is closely related to the scansorial uses of the inwardly
inflected foot of the Sloth.
If the astragalus of an Armadillo[57] were placed side by side with that
of the Megathere, it would be very difficult to determine the analogous
parts, especially of the upper surface, unless guided by the
intermediate structure presented by the Scelidothere. The upper surface
of this bone, in the Armadillo, is, however, divided into two
transversely convex trochleæ, separated by a much wider transversely
concave surface. The fibular trochlea resembles that of the Scelidothere
in having its upper and outer facets sloping away at an acute angle, but
without meeting at a ridge anteriorly; this surface is not more raised
above the tibial trochlea than in the Scelidothere.
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