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
Now, judging by the amount of organic and physical change that occurred
during and since the glacial epoch, and that which has occurred since the
Miocene period, it is considered probable that this maximum of excentricity
coincided with some part of the latter period; and Dr. Croll maintains that
a glacial epoch must then have {60} occurred surpassing in severity that of
which we have such convincing proofs, and consisting like it of
alternations of cold and warm phases every 10,500 years. The diagram also
shows us another long-continued period of high excentricity from 1,750,000
to 1,950,000 years ago, and yet another almost equal to the maximum
2,500,000 years back. These may perhaps have occurred during the Eocene and
Cretaceous epochs respectively, or all may have been included within the
limits of the Tertiary period. As two of these high excentricities greatly
exceed that which caused our glacial epoch, while the third is almost equal
to it and of longer duration, they seem to afford us the means of testing
rival theories of the causes of glaciation. If, as Dr. Croll argues, high
excentricity is the great and dominating agency in bringing on glacial
epochs, geographical changes being subordinate, then there must have been
glacial epochs of great severity at all these three periods; while if he is
also correct in supposing that the alternate phases of precession would
inevitably produce glaciation in one hemisphere, and a proportionately mild
and equable climate in the opposite hemisphere, then we should have to look
for evidence of exceptionally warm and exceptionally cold periods,
occurring {61} alternately and with several repetitions, within a space of
time which, geologically speaking, is very short indeed.
Let us then inquire first into the character of the evidence we should
expect to find of such changes of climate, if they have occurred; we shall
then be in a better position to estimate at its proper value the evidence
that actually exists, and, after giving it due weight, to arrive at some
conclusion as to the theory that best explains and harmonises it.
_Effects of Denudation in Destroying the Evidence of Remote Glacial
Epochs._--It may be supposed, that if earlier glacial epochs than the last
did really occur, we ought to meet with some evidence of the fact
corresponding to that which has satisfied us of the extensive recent
glaciation of the northern hemisphere; but Dr. Croll and other writers have
ably argued that no such evidence is likely to be found. It is now
generally admitted that sub-aerial denudation is a much more powerful agent
in lowering and modifying the surface of a country than was formerly
supposed. It has in fact been proved to be so powerful that the difficulty
now felt is, not to account for the denudation which can be proved to have
occurred, but to explain the apparent persistence of superficial features
which ought long ago to have been destroyed.
Public-domain text, read in full here on John Shaqi.
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