One other consideration is worth notice: with animals and plants that
can propagate rapidly and are not highly locomotive, there is reason
to suspect, as we have formerly seen, that their varieties are
generally at first local; and that such local varieties do not spread
widely and supplant their parent-forms until they have been modified
and perfected in some considerable degree. According to this view, the
chance of discovering in a formation in any one country all the early
stages of transition between any two forms, is small, for the
successive changes are supposed to have been local or confined to some
one spot. Most marine animals have a wide range; and we have seen that
with plants it is those which have the widest range, that oftenest
present varieties; so that with shells and other marine animals, it is
probably those which have had the widest range, far exceeding the
limits of the known geological formations of Europe, which have
oftenest given rise, first to local varieties and ultimately to new
species; and this again would greatly lessen the chance of our being
able to trace the stages of transition in any one geological
formation.
It should not be forgotten, that at the present day, with perfect
specimens for examination, two forms can seldom be connected by
intermediate varieties and thus proved to be the same species, until
many specimens have been collected from many places; and in the case
of fossil species this could rarely be effected by palaeontologists.
Pages:
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
356
357
358
359
360
361
362