Island Life; Or, The Phenomena and Causes of Insular Faunas and FlorasWallace, Alfred Russel
Science
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Wallace, Alfred Russel
Biogeography; Glacial epoch; Island ecology
The great difference presented by the birds of these islands as compared
with those of the equally remote Azores and Bermudas, is sufficiently
explained by the difference of climatal conditions. At the Galapagos there
are none of those periodic storms, gales, and hurricanes which prevail in
the North Atlantic, and which every year carry some straggling birds of
Europe or North America to the former islands; while, at the same time, the
majority of the tropical American birds are {284} nonmigratory, and thus
afford none of the opportunities presented by the countless hosts of
migrants which pass annually northward and southward along the European,
and especially along the North American coasts. It is strictly in
accordance with these different conditions that we find in one case an
almost perfect identity with, and in the other an almost equally complete
diversity from, the continental species of birds.
_Insects and Land-shells._--The other groups of land-animals add little of
importance to the facts already referred to. The insects are very scanty;
the most plentiful group, the beetles, only furnishing about forty species
belonging to thirty-two genera and nineteen families. The species are
almost all peculiar, as are some of the genera. They are mostly small and
obscure insects, allied either to American or to world-wide groups. The
Carabidae and the Heteromera are the most abundant groups, the former
furnishing six and the latter nine species.[61]
{285}
The land-shells are not abundant--about twenty in all, most of them
peculiar species, but not otherwise remarkable. The observation of Captain
Collnet, quoted by Mr. Darwin in his _Journal_, that drift-wood, bamboos,
canes, and the nuts of a palm, are often washed on the south-eastern shores
of the islands, furnishes an excellent clue to the manner in which many of
the insects and land-shells may have reached the Galapagos. Whirlwinds also
have been known to carry quantities of leaves and other vegetable _debris_
to great heights in the air, and these might be then carried away by strong
upper currents and dropped at great distances, and with them small insects
and mollusca, or their eggs. We must also remember that volcanic islands
are subject to subsidence as well as elevation; and it is quite possible
that during the long period the Galapagos have existed some islands may
have intervened between them and the coast, and have served as
stepping-stones by which the passage to them of various organisms would be
greatly facilitated. Sunken banks, the relics of such islands, are known to
exist in many parts of the ocean, and countless others, no doubt, remain
undiscovered.
Public-domain text, read in full here on John Shaqi.
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