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Darwin, Charles, 1809-1882

"The Origin of Species by means of Natural Selection, 6th Edition"

For
instance, it cannot be doubted that all the Cambrian and Silurian
trilobites are descended from some one crustacean, which must have lived
long before the Cambrian age, and which probably differed greatly from any
known animal. Some of the most ancient animals, as the Nautilus, Lingula,
etc., do not differ much from living species; and it cannot on our theory
be supposed, that these old species were the progenitors of all the species
belonging to the same groups which have subsequently appeared, for they are
not in any degree intermediate in character.
Consequently, if the theory be true, it is indisputable that before the
lowest Cambrian stratum was deposited long periods elapsed, as long as, or
probably far longer than, the whole interval from the Cambrian age to the
present day; and that during these vast periods the world swarmed with
living creatures. Here we encounter a formidable objection; for it seems
doubtful whether the earth, in a fit state for the habitation of living
creatures, has lasted long enough. Sir W. Thompson concludes that the
consolidation of the crust can hardly have occurred less than twenty or
more than four hundred million years ago, but probably not less than
ninety-eight or more than two hundred million years. These very wide
limits show how doubtful the data are; and other elements may have
hereafter to be introduced into the problem. Mr.


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