The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
The earliest suggestion on the subject known to the writer is that of
Prof. Asa Gray, in 1867, with reference to the probable northern source
of the related floras of North America and eastern Asia. With the aid
of the new facts disclosed by Heer and Lesquereux, Gray returned to
the subject in 1872, and more fully developed this conclusion with
reference to the Tertiary floras,[EE] and he has recently still further
discussed these questions in an able lecture on "Forest Geography and
Archæology."[EF] In this he puts the case so well and tersely that we may
quote the following sentences as a text for what follows:
[EE] Address to American Association.
[EF] "American Journal of Science," xvi., 1818.
"I can only say, at large, that the same species (of Tertiary fossil
plants) have been found all round the world; that the richest and
most extensive finds are in Greenland; that they comprise most of
the sorts which I have spoken of, as American trees which once lived
in Europe--magnolias, sassafras, hickories, gum-trees, our identical
southern cypress (for all we can see of difference), and especially
_Sequoias_, not only the two which obviously answer to the two
big-trees now peculiar to California, but several others; that they
equally comprise trees now peculiar to Japan and China, three kinds of
gingko-trees, for instance, one of them not evidently distinguishable
from the Japan species which alone survives; that we have evidence, not
merely of pines and maples, poplars, birches, lindens, and whatever
else characterise the temperate zone forests of our era, but also of
particular species of these, so like those of our own time and country
that we may fairly reckon them as the ancestors of several of ours. Long
genealogies always deal more or less in conjecture; but we appear to
be within the limits of scientific inference when we announce that our
existing temperate trees came from the north, and within the bounds of
nigh probability when we claim not a few of them as the originals of
present species. Remains of the same plants have been found fossil in our
temperate region as well as in Europe."
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