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
The inner trochlea differs from that of the Scelidothere in having a
greater relative antero-posterior extent, and in forming, in place of an
uniform convex surface, a trochlea similar in structure to that on the
outer side. The extent of rough surface on the upper part of the
astragalus intervening between the articular surface for the bones of
the leg, and that for the scaphoides is extremely small in the Megathere
and Mylodon(?); it is relatively greater in the Scelidothere; it is
still more extensive in the Armadillo; but is the longest in the Sloth.
The anterior extremity of the astragalus which is entirely occupied by
the scaphoid articular surface is very peculiar in the Scelidothere (Pl.
XXVI. fig. 2.): it presents one convex and two concave facets, which,
however, form part of one continuous articular surface: the convex facet
forms the internal part of the surface, and presents a rhomboidal form
with the long axis vertical. The concave facets (_c_ and _d_) are
extended transversely and placed one above the other; they are slightly
concave in the transverse, and nearly flat in the vertical directions.
In the Megatherium (fig. 1.) the scaphoid surface of the astragalus is
divided only into one concave and one convex portion, both continuous
with each other: the concave facet (_c_) corresponds with the upper
concavity in the Scelidothere, but is a pretty uniform subcircular
depression, fourteen lines in depth: the convex facet, _d_, is continued
across the whole breadth of the under part of the scaphoid surface and
corresponds with both the inner convex, and lower concave surfaces of
the scaphoid articulation in the Scelidothere.
In the Mylodon(?) (Pl. XXVIII. fig. 3.), the articular facet,
corresponding with that marked (_c_) in the astragali of the Megathere
and Scelidothere, is simply flattened, instead of being concave; the
rest of the scaphoid surface corresponds with that in the Megatherium.
In the Armadillo the scaphoid articular surface is undivided and wholly
convex: in this part of the astragalus, therefore, we find the
Scelidothere deviating from the Armadillo further than does the
Megathere; while the Mylodon or Megalonyx(?) most resembles the
Armadillo in the configuration of this part of the astragalus.
If we compare the outer surfaces of the astragalus in these quadrupeds,
we shall find, however, that the Scelidothere and Armadillo closely
agree: the outer facet of the fibular trochleæ, above described, is
continued in the Scelidothere (Pl. XXVIII. fig. 2.), upon the fibular
side of the astragalus reaching nearly half-way down the posterior part,
and down nearly the whole of its anterior.
In the Armadillo, it extends over the whole of the anterior part of the
outer side of the astragalus. In both animals the lower boundary of this
articular surface describes a strong sigmoid curve.
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