When we see a species first appearing in
the middle of any formation, it would be rash in the extreme to infer
that it had not elsewhere previously existed. So again when we find a
species disappearing before the uppermost layers have been deposited,
it would be equally rash to suppose that it then became wholly
extinct. We forget how small the area of Europe is compared with the
rest of the world; nor have the several stages of the same formation
throughout Europe been correlated with perfect accuracy.
With marine animals of all kinds, we may safely infer a large amount
of migration during climatal and other changes; and when we see a
species first appearing in any formation, the probability is that it
only then first immigrated into that area. It is well known, for
instance, that several species appeared somewhat earlier in the
palaeozoic beds of North America than in those of Europe; time having
apparently been required for their migration from the American to the
European seas. In examining the latest deposits of various quarters of
the world, it has everywhere been noted, that some few still existing
species are common in the deposit, but have become extinct in the
immediately surrounding sea; or, conversely, that some are now
abundant in the neighbouring sea, but are rare or absent in this
particular deposit. It is an excellent lesson to reflect on the
ascertained amount of migration of the inhabitants of Europe during
the Glacial period, which forms only a part of one whole geological
period; and likewise to reflect on the great changes of level, on the
inordinately great change of climate, on the prodigious lapse of time,
all included within this same glacial period.
Pages:
333
334
335
336
337
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
356
357