Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
It would be wrong to leave this subject without noticing that
remarkable feature in the southward movement of the later floras,
to which I believe Prof. Gray was the first to direct attention. In
those periods when a warm climate prevailed in the Arctic regions,
the temperate flora must have been, like the modern Arctic flora,
circumpolar. When obliged to migrate to the south, it had to follow the
lines of the continents, and so to divide into separate belts. Three of
these at present are the floras of Western Europe, Eastern Asia, and
Eastern America, all of which have many representative species. They
are separated by oceans and by belts of land occupied by plants which
have not been obliged to migrate. Thus, while the flora of the Eastern
United States resembles that of China and Japan, that of California
and Oregon is distinct from both, and represents a belt of old species
retained in place by the continued warmth of the Pacific shore, and the
continuous extension of the American continent to the south affording
them means of retreat in the Glacial age. Were the plants of China
and Eastern America enabled to return to the Arctic, they would then
reunite into one flora. Gray compares the process of their separation
to the kind of selection which might be made by a botanical distributor
who had the whole collection placed in his hands, with instructions
to give one species of each genus to Europe, to Eastern Asia, and to
Eastern America; and if there was only one species in a genus, or if
one remained over, this was to be thrown into one of the regions, with
a certain preference in favour of America and Asia. This remarkable
kind of geographical selection opens a wide field not only for thought,
but for experiment on the actual relationship of the representative
species. There is a similar field for comparison between the trees
of Georgia in latitude 30° to 35°, and the same species or their
representatives as they existed in Cretaceous times in the latitudes of
50° and 60°. The two floras, as I know from actual comparison, are very
similar.
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