→ local; and lastly, although each species must have passed through numerous transitional stages, it is probable that the periods, during which each underwent modification, though many and long as measured by years, have been short in comparison with the periods during which each remained in an unchanged condition. 1866 1869 1872 |
local. 1859 1860 1861 |
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→ OMIT 1866 1869 1872 |
must have tended to make the geological record extremely imperfect, and 1859 1860 |
must have made the geological record extremely imperfect, and 1861 |
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→ find many links— we do not find 1869 1872 |
not find 1859 1860 |
find 1861 1866 |
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→ interminable 1859 1860 1869 1872 |
many links between the members of the same group— we do not find interminable 1861 |
many links between the species of the same group— we do not find interminable 1866 |
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→ Cambrian 1869 1872 |
first bed of the Silurian 1859 1860 1861 1866 |
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→ We now know that at least one animal did then exist; but I 1869 1872 |
I 1859 1860 1861 |
We now know that animals, and probably plants, lived at an epoch immensely remote, long anterior to the primordial zone of the Silurian system, but I 1866 |
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→ OMIT 1866 1869 1872 |
as far as we can see, 1859 1860 1861 |
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→ extended for an enormous period, 1866 1869 1872 |
for an enormous period extended, 1859 1860 1861 |
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→ commencement of the Cambrian system; 1869 1872 |
Silurian epoch; 1859 1860 1861 |
commencement of the Silurian epoch; 1866 |
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→ only as remnants 1866 1869 1872 |
all be 1859 1860 1861 |
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→ agree admirably with 1872 |
seem to me simply to follow on 1859 1860 1861 1866 1869 |
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→ variation and natural 1872 |
natural 1859 1860 1861 1866 1869 |
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