The Geographical Distribution of Animals, Volume 2: 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 2: 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
_Marine Shells._--We go out of our usual course to say a few words about
the marine shells of this region, because their distribution on the two
sides of the continent is important, as an indication of the former
separation of North and South America, and the connection of the Atlantic
and Pacific Oceans. It was once thought that no species of shells were
common to the two sides of the Central American Isthmus, and Dr. Mörch
still holds that opinion; but Dr. Philip Carpenter, who has paid special
attention to the subject, considers that there are at least 35 species
absolutely identical, while as many others are so close that they may be
only varieties. Nearly 70 others are distinct but representative species.
The genera of marine mollusca are very largely common to the east and west
coasts, more than 40 being so named in the lists published by Mr. Woodward.
The West Indian Islands being a rich shell district, produce a number of
peculiar forms, and the west coast of {21}South America is, to some extent,
peopled by Oriental and Pacific genera of shells. On the west coast there
is hardly any coral, while on the east it is abundant, showing a difference
of physical conditions that must have greatly influenced the development of
mollusca. When these various counteracting influences are taken into
consideration, the identity or close affinity of about 140 species and 40
genera on the two sides of the Isthmus of Panama becomes very important;
and, combined with the fact of 48 species of fish (or 30 per cent. of those
known) being identical on the adjacent coasts of the two oceans (as
determined by Dr. Günther), render it probable that Central America has
been partially submerged up to comparatively recent geological times. Yet
another proof of this former union of two oceans is to be found in the
fossil corals of the Antilles of the Miocene age, which Dr. Duncan finds to
be more allied to existing Pacific forms, than to those of the Atlantic or
even of the Caribbean Sea.
NEOTROPICAL SUB-REGIONS.
In the concluding part of this work devoted to geographical zoology, the
sub-regions are arranged in the order best adapted to exhibit them in a
tabular form, and to show the affinities of the several regions; but for
our present purpose it will be best to take first in order that which is
the most important and most extensive, and which exhibits all the peculiar
characteristics of the region in their fullest development. We begin
therefore with our second division.
_II. Tropical South-America, or the Brazilian Sub-region._
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