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
Let us then consider what are the main facts we have to account for.--1. In
Continental Africa, more especially in the south {286}and west, we find,
along with much that is peculiar, a number of genera showing a decided
Oriental, and others with an equally strong South American affinity; this
latter more particularly showing itself among reptiles and insects. 2. All
over Africa, but more especially in the east, we have abundance of large
ungulates and felines--antelopes, giraffes, buffaloes, elephants, and
rhinoceroses, with lions, leopards, and hyænas, all of types now or
recently found in India and Western Asia. 3. But we also have to note the
absence of a number of groups which abound in the above-named countries,
such as deer, bears, moles, and true pigs; while camels and
goats--characteristic of the desert regions just to the north of the
Ethiopian--are equally wanting. 4. There is a wonderful unity of type and
want of speciality in the vast area of our first sub-region extending from
Senegal across to the east coast, and southward to the Zambezi; while West
Africa and South Africa each abound in peculiar types. 5. We have the
extraordinary fauna of Madagascar to account for, with its evident main
derivation from Africa, yet wanting all the larger and higher African
forms; its resemblances to Malaya and to South America; and its wonderful
assemblage of altogether peculiar types.
Here we find a secure starting-point, for we are sure that Madagascar must
have been separated from Africa before the assemblage of large animals
enumerated above, had entered it. Now, it is a suggestive fact, that all
these belong to types which abounded in Europe and India about the Miocene
period. It is also known, from the prevalence of Tertiary deposits over the
Sahara and much of Arabia, Persia, and Northern India, that during early
Tertiary times a continuous sea from the Bay of Bengal to the British Isles
completely cut off all land communication between Central and Southern
Africa on the one side, and the great continent of the Eastern hemisphere
on the other. When Africa was thus isolated, its fauna probably had a
character somewhat analogous to that of South America at the same period.
Most of the higher types of mammalian life were absent, while lemurs,
Edentates, and Insectivora took their place. At this period Madagascar was
no doubt united with Africa, {287}and helped to form a great southern
continent which must at one time have extended eastward as far as Southern
India and Ceylon; and over the whole of this the lemurine type no doubt
prevailed.
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