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1859
1860
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but likewise denuded condition. 1861 1866
condition. 1859 1860
and denuded condition. 1869 1872

namely— that though we find in our geological formations many 1861
namely our not finding in the successive formations infinitely numerous transitional 1859 1860
namely— that, though we find in our geological formations many 1866 1869 1872

and have existed, 1861 1866
or have existed; 1859 1860
and which formerly existed, we do not find infinitely numerous fine transitional forms closely joining them all together;— 1869 1872

we do not find infinitely numerous fine transitional forms closely joining them all together;— the 1861 1866
the 1859 1860 1869 1872

beneath the Silurian strata,— 1861
beneath the Silurian strata, 1859 1860
rich in fossils beneath the Silurian strata,— 1866
rich in fossils beneath the Cambrian strata,— 1869 1872

OMIT 1861 1866 1869 1872
plainest manner by the 1859 1860

I have reason to believe that one great authority, 1859 1860 1861
it is evident from the recent works of 1866
OMIT 1869 1872

from further reflection entertains grave doubts on this subject. 1861
from further reflexion entertains grave doubts on this subject. 1859 1860
that he now almost gives up this view; and some other great geologists and palæontologists are much shaken in their confidence. 1866
now gives the support of his high authority to the opposite side; and most other geologists and palæontologists are much shaken in their former belief. 1869
now gives the support of his high authority to the opposite side; and most geologists and palæontologists are much shaken in their former belief. 1872

think the natural 1859 1860 1861
believe that the 1866 1869 1872

and who do not attach much weight to the facts and arguments of other kinds given in this volume, 1859 1860 1861
OMIT 1866 1869 1872

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
bare
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
silurian
Cambrian
Silurian
epoch in a completely metamorphosed but likewise denuded condition.
The several difficulties here discussed, namely— that though we find in our geological formations many links between the
many
....
species which now exist and have existed, we do not find infinitely numerous fine transitional forms closely joining them all together;— the sudden manner in which
whole
several
several whole
groups of species
appear
first appear
first appeared
in our European
formations;
formations;—
the almost entire absence, as at present known, of
fossiliferous
fossiliferous
formations beneath the Silurian strata,— are all undoubtedly of the
gravest
most serious
nature. We see this in the OMIT fact that
all
....
the most eminent palæontologists,
namely,
namely
Cuvier,
Owen,
....
Agassiz, Barrande,
Falconer,
Pictet, Falconer,
E. Forbes ,
&c.,
&c,
and all our greatest geologists, as Lyell, Murchison, Sedgwick,
&c.,
&C
have unanimously, often vehemently, maintained the immutability of species. But I have reason to believe that one great authority, Sir Charles
Lyell
Lyell,
from further reflection entertains grave doubts on this subject. I feel how rash it is to differ from
these great
the foregoing
these
authorities, to whom, with others, we owe all our knowledge. Those who think the natural geological record
is in
in
any degree perfect, and who do not attach much weight to the facts and arguments of other kinds given in this volume, will undoubtedly at once reject
the
my
theory. For my part, following out
Lyells
Lyell's
metaphor, I look at the
natural
natural