↑ 1 blocks not present in 1866 1869 1872; present in 1859 1860 1861 |
If the climate, since the Glacial period, has ever been in any degree warmer than at present (as some geologists in the United States believe to have been the case,
chiefly from the distribution of the fossil Gnathodon),
then the arctic and temperate productions will at a very late period have marched a little further
north, and subsequently have retreated to their present homes; but I have met with no satisfactory evidence with respect to this intercalated slightly warmer period, since the Glacial period.
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→ moved first southward and afterwards backwards to the north, in unison with the changing climate, they will not 1866 1869 1872 |
during their long southern migration and re-migration northward, will 1859 1860 1861 |
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→ during their long migrations to any great diversity of temperature, 1866 |
to nearly the same climate, 1859 1860 1861 |
during their long migrations to any great diversity of temperature; 1869 1872 |
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→ they will all have migrated 1866 |
is especially to be noticed, they will have kept 1859 1860 1861 |
they all migrated 1869 1872 |
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→ this we find has been the case; 1859 1860 1861 1866 1869 |
they have been modified; 1872 |
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→ one with another, though 1866 1869 1872 |
though very 1859 1860 1861 |
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→ or sub-species, and some as certainly 1866 1869 |
and some few are 1859 1860 |
and many are 1861 |
or sub-species, and some as 1872 |
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→ each other on the several ranges. 1866 1869 1872 |
species. 1859 1860 1861 |
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→ illustrating what, as I believe, actually took place during the Glacial period, I 1859 1860 1861 1866 |
the foregoing illustration I have 1869 1872 |
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