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
While the facts above slightly sketched impress us with the grand
progress of the vegetable kingdom in geological time, they equally show
the persistence of vegetable forms as compared with that of the dead
continental masses and the decay of some forms of life in favour of the
introduction of others.
When we find in the glacial beds the leaves of trees still living in
North America and Europe, and consider the vicissitudes of elevation
and submergence of the land, and of Arctic and temperate climates
which have occurred, we are struck with the persistence of the weak
things of life, as compared with the changeableness of rocks and
mountains. A superficial observer might think the fern or the moss
of a granite hill a frail and temporary thing as compared with solid
and apparently everlasting rock. But just the reverse is the case.
The plant is usually older than the mountain. But the glacial age
is a very recent thing. We have facts older than this. As hinted in
a previous paper, in the Laramie clays associated with the Lignite
beds of North-western Canada--beds of Lower Eocene or early Tertiary
age--which were deposited before the Rocky Mountains or the Himalayas
had reared their great peaks and ridges, and at a time when the whole
geography of the northern hemisphere was different from what it is
at present--are remains of very frail and delicate plants which still
live. I have shown that in these clays there exist, side by side, the
Sensitive Fern, _Onoclea sensibilis_, and one of the delicate rock
ferns, _Davallia tenuifolia_.[108] The first is still very abundant
all over North America. The second has ceased to exist in North
America, but still survives in the valleys of the Himalayas. These two
little plants, once probably very widely diffused over the northern
hemisphere, have continued to exist through the millenniums separating
the Cretaceous from the present time, and in which the greater part
of our continent was again and again under the sea, in which great
mountain chains have been rolled up and sculptured into their present
forms, and in which giant forms, both of animal and plant life, have
begun, culminated and passed away. Truly God hath chosen the weak
things of the world to confound those that are strong.
[108] Report on 49th Parallel, 1875.
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