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
One word may be said here as to use of fossil plants in determining
geological time. In this I need only point to the fact of my
having defined in Canada three Devonian floras, a Lower, Middle,
and Upper, and that Mr. Whiteaves, in his independent study of the
fossil fishes, has vindicated my conclusions. There are also in Nova
Scotia three distinctive sub-floras of the Lower, Middle, and Upper
Carboniferous.[111] I have verified these for the Devonian and
Carboniferous of the United States, and to some extent also for those
of Europe. To the same effect is the recognition of the Kootanie or
Lower Cretaceous, the Middle Cretaceous, Upper Cretaceous, Laramie and
Miocene in Western Canada. These have in all cases corresponded with
the indications of animal fossils[112] and of stratigraphy. Fossil
plants have been less studied in this connection than fossil animals,
but I have no hesitation in affirming that, with reference to the
broader changes of the earth's surface, any competent palæobotanist is
perfectly safe in trusting to the evidence of vegetable fossils.
[111] _Transactions Royal Society of Canada_, 1883 to 1891.
[112] Reports on Fossil Plants of the Devonian and Lower Carboniferous.
It may be objected that such evidence will be affected by the
migrations of plants, so that we cannot be certain that identical
species flourished in Greenland and in temperate America at the same
time. If such species originated in Greenland and migrated southward,
the specimens found at the south may be much newer than those in the
north. This, no doubt, is locally true, but the migrations of plants,
though slow, occupy less time than that of a great geological period.
It may also be objected that the flora of swamps, plains, and mountain
tops would differ at any one period. This also is true, but the same
difficulty applies to animals of the deep sea, the shore, and the land;
and these diversities of station have always to be taken into account
by the palæontologist.
References:--Report on the Erian or Devonian Plants of Canada,
Montreal, 1871. Article in Princeton Review on Genesis and
Migrations of Plants. "The Geological History of Plants," London
and New York, 1888 and 1892. Papers on Fossil Plants of Western
Canada, 1883, and following volumes of Transactions of Royal
Society of Canada.
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