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
It is here that natural science meets with theology, not as an
antagonist, but as a friend and ally in its time of greatest need;
and I must here record my belief that neither men of science nor
theologians have a right to separate what God in Holy Scripture has
joined together, or to build up a wall between nature and religion, and
write upon it, "no thoroughfare." The science that does this must be
impotent to explain nature, and without hold on the higher sentiments
of man. The theology that does this must sink into mere superstition.
In conclusion, can we formulate a few of the general laws, or perhaps I
had better call them the general conclusions, respecting life, in which
all Palæontologists may agree. Perhaps it is not possible to do this at
present satisfactorily, but the attempt may do no harm. We may, then, I
think, make the following affirmations:--
1. The existence of life and organization on the earth is not eternal,
or even coeval with the beginning of the physical universe, but may
possibly date from Laurentian or immediately pre-Laurentian ages.
2. The introduction of new species of animals and plants has been a
continuous process, not necessarily in the sense of derivation of
one species from another, but in the higher sense of the continued
operation of the cause or causes which introduced life at first. This,
as already stated, I take to be the true theological or Scriptural as
well as scientific idea of what we ordinarily and somewhat loosely term
creation.
3. Though thus continuous, the process has not been uniform; but
periods of rapid production of species have alternated with others in
which many disappeared and few were introduced. This may have been an
effect of physical cycles reacting on the progress of life.
4. Species, like individuals, have greater energy and vitality in
their younger stages, and rapidly assume all their varietal forms, and
extend themselves as widely as external circumstances will permit. Like
individuals also, they have their periods of old age and decay, though
the life of some species has been of enormous duration in comparison
with that of others; the difference appearing to be connected with
degrees of adaptation to different conditions of life.
5. Many allied species, constituting groups of animals and plants, have
made their appearance at once in various parts of the earth, and these
groups have obeyed the same laws with the individual and the species in
culminating rapidly, and then slowly diminishing, though a large group
once introduced has rarely disappeared altogether.
6. Groups of species, as genera and orders, do not usually begin with
their highest or lowest forms, but with intermediate and generalized
types, and they show a capacity for both elevation and degradation in
their subsequent history.
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