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
Of ultimately Old World origin, but through a considerable line of
descent in America, were the typically American deer (_Odocoileus_)
of which the Virginian and Black-tailed species are familiar modern
instances. Whether or not the Old World types, the Caribou (_Rangifer_)
and Wapiti (_Cervus canadensis_) had reached the western hemisphere,
is a matter of some doubt; if present at all, they must have been
comparatively rare. The Moose (_Alce americanus_), on the other hand,
had already appeared, but seems to have been confined to the western
half of the continent, its presence in the east being questionable. The
mistakenly named “Rocky Mountain Goat” (_Oreamnos montanus_), which is
an antelope of the chamois group, was an apparently late arrival in the
Pleistocene, while the peculiar Prong-Buck (_Antilocapra americana_),
which is very different from any of the Old World antelopes, was
present in the early part of the epoch. The descent of this remarkable
animal is still a problem, but not improbably it was derived from the
“deer-antelopes” of the Miocene and Pliocene, the last of which occurred
in the early Pleistocene. Mr. Gidley has announced the surprising
discovery in Maryland of a large antelope hardly distinguishable from the
African Eland (_Taurotragus_). Other late arrivals from the Old World
were several forms allied to the existing Musk Ox (_Ovibos_), at least
two genera of which (_†Preptoceras_ and _†Euceratherium_) have been found
in California. A surprising number of species of _Bison_ occurred in the
Pleistocene, no less than seven of which are recognized as distinct,
ranging from Florida to Alaska. It is not likely that all these species
coexisted at the same time, but we cannot yet determine their order of
succession, though the modern species, _B. bison_, was probably the
latest to arise. Most of these species were much larger than _B. bison_,
and some were gigantic, such as _B. †latifrons_, which had a spread of
horns of 6 feet and is found through the Mississippi Valley, and _B.
†crassicornis_ of Alaska.
[Illustration: FIG. 116.—Restoration of _†Preptoceras_, a musk-ox like
animal from the Californian Pleistocene. (From a skeleton in the museum
of the University of California.)]
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