The Geographical Distribution of Animals, Volume 1: With a study of the relations of living and extinct faunas as elucidating the past changes of the Earth's surfaceWallace, Alfred Russel
Science
The Geographical Distribution of Animals, Volume 1: With a study of the relations of living and extinct faunas as elucidating the past changes of the Earth's surface
Wallace, Alfred Russel
Paleontology; Zoogeography
_Eocene fauna of South America._--The few remains yet discovered in the
Tertiary deposits of the Pampas which are believed to be of Eocene age, are
exceedingly interesting, because they show us another change in the scenery
of the great drama of life; there being apparently a considerable
resemblance, at this epoch, between South America and Europe. They consist
of a large extinct feline animal, _Eutemnodus_; of _Palæotherium_ and
_Anoplotherium_, the well-known extinct Ungulates of the European
Tertiaries, and which have never been found in North America; and of three
genera of Rodents,--_Theridromys_, allied to _Echimys_, and found also in
the Eocene and Miocene of France; _Megamys_, allied to the living
_Capromys_ of the Antilles, and also to _Palæomys_, an extinct form of the
French Miocene; and a very large animal referred to _Arvicola_, a genus
found also in the Pliocene deposits of South America, and abundant in the
northern hemisphere. No Edentates have been found.
The resemblances of this fauna to that of Europe rather than to any part of
America, are so strong, that they can hardly be accidental. We greatly
want, however, more information on this point, as well as some
corresponding evidences as to the condition of West and South Africa about
the same epoch, before we can venture to speculate on their bearing as
regards the early migrations of organic forms.
_General Remarks on the Extinct Mammalian Fauna of the Old {149}and New
Worlds._--Leaving the more special applications of palæontological evidence
to be made after discussing the relations of the existing fauna of the
several regions, we propose here to indicate briefly, some of the more
general deductions from the evidence which has now been laid before our
readers.
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