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
No doubt a prejudice has been excited against it in the minds of many
geologists, by its being thought to lead _necessarily_ to frequently
recurring glacial epochs throughout all geological time. But I have here
endeavoured to show that this is _not_ a necessary consequence of the
theory, because a concurrence of favourable geographical conditions is
essential to the initiation of a glaciation, which when once initiated has
a tendency to maintain itself throughout the varying phases of precession
occurring during a period of high excentricity. When, however, geographical
conditions favour warm Arctic climates--as it has been shown they have done
throughout the larger portion of geological time--then changes of
excentricity, to however great an extent, have no tendency to bring about a
state of glaciation, because warm oceanic currents have a {98}
preponderating influence, and without very large areas of high northern
land to act as condensers, no perpetual snow is possible, and hence the
initial process of glaciation does not occur.
The theory as now set forth should commend itself to geologists, since it
shows the direct dependence of climate on physical processes, which are
guided and modified by those changes in the earth's surface which geology
alone can trace out. It is in perfect accord with the most recent teachings
of the science as to the gradual and progressive development of the earth's
crust from the rudimentary formations of the Azoic age, and it lends
support to the view that no inportant[**important] departure from the great
lines of elevation and depression originally marked out on the earth's
surface has ever taken place.
It also shows us how important an agent in the production of a habitable
globe with comparatively small extremes of climates over its whole area, is
the great disproportion between the extent of the land and the water
surfaces. For if these proportions had been reversed, large areas of land
would necessarily have been removed from the beneficial influence of
aqueous currents or moisture-laden winds; and slight geological changes
might easily have led to half the land surface becoming covered with
perpetual snow and ice, or being exposed to extremes of summer heat and
winter cold, of which our water-permeated globe at present affords no
example. We thus see that what are usually regarded as geographical
anomalies--the disproportion of land and water, the gathering of the land
mainly into one hemisphere, and the singular arrangement of the land in
three great southward-pointing masses--are really facts of the greatest
significance and importance, since it is to these very anomalies that the
universal spread of vegetation and the adaptability of so large a portion
of the earth's surface for human habitation is directly due.
* * * * *
{99}
CHAPTER X
THE EARTH'S AGE, AND THE RATE OF DEVELOPMENT OF ANIMALS AND PLANTS
Public-domain text, read in full here on John Shaqi.
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