The Deseado Formation of PatagoniaLoomis, Frederic Brewster
Science
The Deseado Formation of Patagonia
Loomis, Frederic Brewster
Paleontology -- Patagonia (Argentina and Chile)
The astragulus is a very characteristic bone. The trochlea is
asymetrical, the external condyle rising higher than the internal, and
the median groove being wide and shallow. On the nearly vertical outer
face of the astragulus, there is a semicircular band-like facet for the
fibula. The trochlea extends well around the top of the bone, allowing
a wide movement of the foot. The neck of the astragulus is long and
wide, carrying a broad flattened head, with its convex facet for the
navicular, covering the entire end. On the plantar side are the most
marked features. The ectal facet is in two planes, the anterior portion
being bent down to nearly right angles with the posterior, which seems
to be characteristic of this _Diadiaphorus_ series. The sustentacular
facet also is characteristic, being gently rounded and extending
clear to the navicular facet on the head, in _Diadiaphorus_ becoming
actually confluent with the navicular facet. Just at the edge of this
sustentacular facet is a tiny surface where the astragulus rubs on the
cuboid, the only case, as far as I am aware, where this occurs in any
_Litopterna_.
[Illustration: Fig. 11. Left astragulus plantar side: _a_, ectal
facet—½ natural size; _b_, sustentacular facet; _c_, facet for cuboid.]
The calcaneum is long and slender, the tuber being but slightly
enlarged, its sustentacular facet being a broad oval surface, while the
ectal facet is in two planes to correspond to that on the astragulus.
The facet for the cuboid is at the distal end, but is unusually
oblique, its inner margin sloping up almost to the sustentacular facet.
It is this slope which brings the cuboid in contact with the astragulus.
The navicular is broad and low, with a prominent hook behind. On its
upper face there is only the broad facet for the astragulus head; on
the lower face are three facets, externally, a large, more or less
triangular area, for the ectocuneiform; medianly a smaller similar
facet for the mesocuneiform; and on the internal side, sloping up onto
the internal face, a small facet for the reduced endocuneiform. On the
external face of this bone there is a tiny beveled facet for the cuboid.
The endocuneiform is a large scale-like ossicle articulating on the
lateral internal face of the navicular, and overlapping markedly the
inner surface of Metatarsus II.
The mesocuneiform is considerably reduced in size, carrying a broad
flat facet on the upper surface for the navicular, and a shallow
saddle-like one below for Mt. II, which is entirely carried by this
bone.
The ectocuneiform is considerably larger than the mesocuneiform,
resting above on the navicular, and carrying below the whole of Mt.
III. On its inner side are two facets which rub against the upper end
of Mt. II.
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