is it possible that an animal having, for instance,
the structure and habits of a bat, could have been formed by the
modification of some animal with wholly different habits? Can we
believe that natural selection could produce, on the one hand, organs
of trifling importance, such as the tail of a giraffe, which serves as a
fly-flapper, and, on the other hand, organs of such wonderful structure,
as the eye, of which we hardly as yet fully understand the inimitable
perfection?
Thirdly, can instincts be acquired and modified through natural
selection? What shall we say to so marvellous an instinct as that which
leads the bee to make cells, which have practically anticipated the
discoveries of profound mathematicians?
Fourthly, how can we account for species, when crossed, being sterile
and producing sterile offspring, whereas, when varieties are crossed,
their fertility is unimpaired?
The two first heads shall be here discussed--Instinct and Hybridism in
separate chapters.
ON THE ABSENCE OR RARITY OF TRANSITIONAL VARIETIES.
As natural selection acts solely by the preservation of profitable
modifications, each new form will tend in a fully-stocked country to
take the place of, and finally to exterminate, its own less improved
parent or other less-favoured forms with which it comes into
competition. Thus extinction and natural selection will, as we have
seen, go hand in hand. Hence, if we look at each species as descended
from some other unknown form, both the parent and all the transitional
varieties will generally have been exterminated by the very process of
formation and perfection of the new form.
But, as by this theory innumerable transitional forms must have existed,
why do we not find them embedded in countless numbers in the crust of
the earth? It will be much more convenient to discuss this question in
the chapter on the Imperfection of the geological record; and I will
here only state that I believe the answer mainly lies in the record
being incomparably less perfect than is generally supposed; the
imperfection of the record being chiefly due to organic beings not
inhabiting profound depths of the sea, and to their remains being
embedded and preserved to a future age only in masses of sediment
sufficiently thick and extensive to withstand an enormous amount of
future degradation; and such fossiliferous masses can be accumulated
only where much sediment is deposited on the shallow bed of the sea,
whi
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