Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
These views may be thus briefly stated. From the earliest period at
which plants and animals can be proved to have existed, there has been a
continual change going on in the position of land and sea, accompanied
by great fluctuations of climate. To these ever-varying geographical and
climatal conditions the state of the animate world has been unceasingly
adapted. No satisfactory proof has yet been discovered of the gradual
passage of the earth from a chaotic to a more habitable state, nor of
any law of progressive development governing the extinction and
renovation of species, and causing the fauna and flora to pass from an
embryonic to a more perfect condition, from a simple to a more complex
organization.
The principle of adaptation to which I have alluded, appears to have
been analogous to that which now peoples the arctic, temperate, and
tropical regions contemporaneously with distinct assemblages of species
and genera, or which, independently of mere temperature, gives rise to a
predominance of the marsupial or didelphous tribe of quadrupeds in
Australia, of the placental or monodelphous tribe in Asia and Europe, or
which causes a profusion of reptiles without mammalia in the Galapagos
Archipelago, and of mammalia without reptiles in Greenland.
_Recent origin of man._--If, then, the popular theory of the successive
development of the animal and vegetable world, from the simplest to the
most perfect forms, rests on a very insecure foundation; it may be
asked, whether the recent origin of man lends any support to the same
doctrine, or how far the influence of man may be considered as such a
deviation from the analogy of the order of things previously
established, as to weaken our confidence in the uniformity of the course
of nature.
Antecedently to investigation, we might reasonably have anticipated that
the vestiges of man would have been traced back at least as far as those
modern strata in which all the testacea and a certain number of the
mammalia are of existing species, for of all the mammalia the human
species is the most cosmopolite, and perhaps more capable than any other
of surviving considerable vicissitudes in climate, and in the physical
geography of the globe.
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