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
Another general truth, obvious from the facts which have been already
collected, is the periodicity of introduction of species. They come
in by bursts or flood tides at particular points of time, while these
great life waves are followed and preceded by times of ebb in which
little that is new is being produced. We labour in our investigation of
this matter under the disadvantage that the modern period is evidently
one of the times of pause in the creative work. Had our time been
that of the early Tertiary or early Mesozoic, our views as to the
question of origin of species might have been very different. It is a
striking fact, in illustration of this, that since the glacial age no
new species of mammal, except, possibly, man himself, can be proved to
have originated on our continents, while a great number of large and
conspicuous forms have disappeared. It is possible that the proximate
or secondary causes of the ebb and flow of life production may be in
part at least physical, but other and more important efficient causes
may be behind these. In any case these undulations in the history of
life are in harmony with much that we see in other departments of
nature.
It results from the above and the immediately preceding statement,
that specific and generic types enter on the stage in great force,
and gradually taper off towards extinction. They should so appear in
the geological diagrams made to illustrate the succession of living
beings. This applies even to those forms of life which come in with
fewest species and under the most humble guise. What a remarkable
swarming, for example, there must have been of Marsupial Mammals in
the early Mesozoic, and in the Coal formation the only known Pulmonate
snails, five or six in number, belong to four generic types, while the
Myriapods and Amphibians alike appear in a crowd of generic forms.
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