In accordance with these facts the law may be stated, that, in
butterflies at least, all the individuals of a species respond to the
same external influences by similar changes, and that, consequently,
the changes brought about by climatic influences take a fixed
direction, determined by the physical constitution of the species.
When, however, new climatic forms of butterflies, in which natural
selection is completely excluded, and the nature of the species itself
definitely determines the direction of the changes, nevertheless show
variability from the very beginning, we may venture to conclude that
every transformation of a species generally begins with a fluctuation
of its characters. But when we find the primary forms of butterflies
always far more constant, this shows that the continued crossing of the
individuals of a species to a certain extent balances the fluctuations
of form. Both facts taken together confirm the law formerly enunciated
by me,[54] that in every species a period of variability alternates
with one of (relative) constancy--the latter indicating the
culmination, and the former the beginning or end, of its development.
I here call to mind this law, because the facts which I advanced at
that time, viz., Hilgendorf’s history of the phyletic development of
the Steinheim fossil shells, having since become somewhat doubtful, one
might easily be inclined to go too far in mistrusting them and refuse
to give them any weight at all.[55]
In the essay just indicated I traced the origin of a certain class
of local forms to local isolation. I attempted to show that when a
species finds itself in an isolated district in a condition (period)
of variability, it must there necessarily acquire somewhat deviating
characters by being prevented from crossing with the individuals
of other regions, or, what comes to the same thing, a local form
must originate. This production of local forms results because
the different variations which, for the time being, constitute the
variability of the species, would always be in a different numerical
proportion in the isolated district as compared with other regions;
and further, because constancy is produced by the crossing of these
(isolated) varieties among themselves; so that the resultant of
the various components is (local) variation. If the components are
dissimilar the resultant would also be different, and thus, from a
theoretical point of view, there seems to me no obstacle in the way
of the production of such local forms by the process of ‘amixia.’ I
believe that I have further shown that numerous local forms can be
conceived to have arisen through this process of preventive crossing,
whilst they cannot be explained by the action of climatic influences.
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