Nor should we be justified in assuming that if, for
instance, the bed of the Pacific Ocean were now converted into a continent
we should there find sedimentary formations, in recognisable condition,
older than the Cambrian strata, supposing such to have been formerly
deposited; for it might well happen that strata which had subsided some
miles nearer to the centre of the earth, and which had been pressed on by
an enormous weight of superincumbent water, might have undergone far more
metamorphic action than strata which have always remained nearer to the
surface. The immense areas in some parts of the world, for instance in
South America, of naked metamorphic rocks, which must have been heated
under great pressure, have always seemed to me to require some special
explanation; and we may perhaps believe that we see in these large areas
the many formations long anterior to the Cambrian epoch in a completely
metamorphosed and denuded condition.
The several difficulties here discussed, namely, that, though we find in
our geological formations many links between the species which now exist
and which formerly existed, we do not find infinitely numerous fine
transitional forms closely joining them all together. The sudden manner in
which several groups of species first appear in our European formations,
the almost entire absence, as at present known, of formations rich in
fossils beneath the Cambrian strata, are all undoubtedly of the most
serious nature.
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