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
First, in regard to the vicissitudes of the living creation, all are
agreed that the sedimentary strata found in the earth's crust are
divisible into a variety of groups, more or less dissimilar in their
organic remains and mineral composition. The conclusion universally
drawn from the study and comparison of these fossiliferous groups is
this, that at successive periods distinct tribes of animals and plants
have inhabited the land and waters, and that the organic types of the
newer formations are more analogous to species now existing, than those
of more ancient rocks. If we then turn to the present state of the
animate creation, and inquire whether it has now become fixed and
stationary, we discover that, on the contrary, it is in a state of
continual flux--that there are many causes in action which tend to the
extinction of species, and which are conclusive against the doctrine of
their unlimited durability. But natural history has been successfully
cultivated for so short a period, that a few examples only of local, and
perhaps but one or two of absolute, extirpation can as yet be proved,
and these only where the interference of man has been conspicuous. It
will nevertheless appear evident, from the facts and arguments detailed
in the third book (from the thirty-seventh to the forty-second chapters,
inclusive) that man is not the only exterminating agent; and that,
independently of his intervention, the annihilation of species is
promoted by the multiplication and gradual diffusion of every animal or
plant. It will also appear, that every alteration in the physical
geography and climate of the globe cannot fail to have the same
tendency. If we proceed still farther, and inquire whether new species
are substituted from time to time for those which die out, and whether
there are certain laws appointed by the Author of Nature to regulate
such new creations, we find that the period of human observation is as
yet too short to afford data for determining so weighty a question. All
that can be done is to show that the successive introduction of new
species may be a constant part of the economy of the terrestrial system,
without our having any right to expect that we should be in possession
of direct proof of the fact. The appearance again and again of new
species may easily have escaped detection, since the numbers of known
animals and plants have augmented so rapidly within the memory of
persons now living, as to have doubled in some classes, and quadrupled
in others. It will also be remarked in the sequel (book iii. chap. 43),
that it must always be more easy if species proceeded originally from
single stocks, to prove that one which formerly abounded in a given
district has ceased to be, than that another has been called into being
for the first time. If, therefore, there be as yet only one or two
unequivocal instances of extinction, namely, those of the dodo and
solitaire (see ch. 41), it is scarcely reasonable as yet to hope that we
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account