A history of land mammals in the western hemisphereScott, William Berryman
History
A history of land mammals in the western hemisphere
Scott, William Berryman
Mammals; Mammals, Fossil
The Edentata were more abundant and diversified than at any other time
in South American history of which the record is preserved. Two of the
modern subdivisions of this order have not been certainly identified
in the Santa Cruz collections, the arboreal sloths and the anteaters,
and though they may be found there at any time, it will only be as
stragglers from the warmer forested regions to the north, where these
forms had doubtless long been present. Unfortunately, however, nothing
is directly known concerning the life of those regions in Miocene
times. On the other hand, three groups of edentates, two of them now
extinct, were very copiously represented in the Santa Cruz formation,
the armadillos, †glyptodonts and †ground-sloths. Of the many armadillos,
some quite large, others very small, only a few can be regarded as
directly ancestral to those now in existence; the truly ancestral
forms were probably then living in the forests of Brazil and northern
Argentina, in the same areas as the ancestral tree-sloths and anteaters.
In comparison with the giants of the Pliocene and Pleistocene, the Santa
Cruz †glyptodonts were all small, the carapace rarely exceeding two
feet in length, and, what it is particularly interesting to note, they
departed much less widely from the armadillo type than did their gigantic
successors. The †ground-sloths were present in actually bewildering
variety and they also were very small as compared with the huge animals
of the Pleistocene, none of them exceeding the Black Bear in height or
length, though proportionally much more massive, and many were no bigger
than foxes. They had small heads, long bodies, heavy tails and short,
thick legs; their teeth show that they were plant-feeders, but their feet
were armed with long, sharp and formidable claws. Among this great host
of Santa Cruz †ground-sloths may readily be noted the probable ancestors
of the gigantic creatures which were such characteristic elements of the
Pliocene and Pleistocene faunas.
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