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
[86] Saporata, "Ancienne Vegetation Polaire"; Hooker, Presidential
Address to Royal Society, 1878; Thistleton Dyer, "Lecture on Plant
Distribution "; Mr. Starkie Gardner, Letters in _Nature_, 1878, etc.
The basis of most of these brochures is to be found in Heer's "Flora
Fossilis Arctica."
The earliest suggestion on this subject known to the writer is that of
my old and dear friend, Professor 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 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,[87]
and still later he further discussed these questions in an able lecture
on "Forest Geography and Archæology."[88] In this he puts the case so
well and tersely that I may quote the following sentences as a text for
what follows:--
[87] Address to American Association.
[88] _American Journal of Science_, xvi., 1878.
"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 characterize 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 high 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."
Public-domain text, read in full here on John Shaqi.
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