Evolution; Knowledge, Theory of; Philosophy and religion
Aggregates of living creatures illustrate the general truth in other
ways. If each species of organism be regarded as a whole, it displays
two kinds of rhythm. Life as it exists in all the members of such
species, is an extremely complex kind of movement, more or less distinct
from the kinds of movement which constitutes life in other species. In
each individual of the species, this extremely complex kind of movement
begins, rises to its climax, declines, and ceases in death. And every
successive generation thus exhibits a wave of that peculiar activity
characterizing the species as a whole. The other form of rhythm is
to be traced in that variation of number which each tribe of animals and
plants is ever undergoing. Throughout the unceasing conflict between the
tendency of a species to increase and the antagonistic tendencies, there
is never an equilibrium: one always predominates. In the case even of a
cultivated plant or domesticated animal, where artificial means are used
to maintain the supply at a uniform level, we still see that
oscillations of abundance and scarcity cannot be avoided. And among the
creatures uncared for by man, such oscillations are usually more marked.
After a race of organisms has been greatly thinned by enemies or lack of
food, its surviving members become more favourably circumstanced than
usual. During the decline in their numbers their food has grown
relatively more abundant; while their enemies have diminished from want
of prey. The conditions thus remain for some time favourable to their
increase; and they multiply rapidly. By and by their food is rendered
relatively scarce, at the same time that their enemies have become more
numerous; and the destroying influences being thus in excess, their
number begins to diminish again. Yet one more rhythm, extremely
slow in its action, may be traced in the phenomena of Life, contemplated
under their most general aspect. The researches of palæontologists show,
that there have been going on, during the vast period of which our
sedimentary rocks bear record, successive changes of organic forms.
Species have appeared, become abundant, and then disappeared. Genera, at
first constituted of but few species, have for a time gone on growing
more multiform; and then have begun to decline in the number of their
subdivisions; leaving at last but one or two representatives, or none at
all. During longer epochs whole orders have thus arisen, culminated, and
dwindled away. And even those wider divisions containing many orders
have similarly undergone a gradual rise, a high tide, and a
long-continued ebb. The stalked _Crinoidea_, for example, which, during
the carboniferous epoch, became abundant, have almost disappeared: only
a single species being extant. Once a large family of molluscs, the
_Brachiopoda_ have now become rare. The shelled Cephalopods, at one time
dominant among the inhabitants of the ocean, both in number of forms and
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