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
Let humble plants, then, be introduced in the waters, and they would
at once begin to use the solar light for the purpose of decomposing
carbonic acid, and forming carbon compounds which had not before
existed, and which, independently of vegetable life, would never have
existed. At the same time lime and other mineral substances present in
the sea water would be fixed in the tissues of these plants, either
in a minute state of division, as little grains or Coccoliths, or in
more solid masses like those of the Corallines and Nullipores. In this
way a beginning of limestone formation might be made, and quantities
of carbonaceous and bituminous matter, resulting from the decay of
vegetable substances might accumulate on the sea bottom. Now arises
the opportunity for animal life. The plants have collected stores
of organic matter, and their minute germs, along with microscopic
species, are floating everywhere in the sea. The plant has fulfilled
its function as far as the waters are concerned, and now a place is
prepared for the animal. In what form shall it appear? Many of its
higher forms, those which depend upon animal food or on the more
complex plants for subsistence, would obviously be unsuitable. Further,
the sea water is still too much saturated with saline matter to be
fit for the higher animals of the waters. Still further, there may
be a residue of internal heat forbidding coolness, and that solution
of free oxygen which is an essential condition of existence to the
higher forms of life. Something must be found suitable for this saline,
imperfectly oxygenated, tepid sea. Something, too, is wanted that can
aid in introducing conditions more favourable to higher life in the
future. Our experience of the modern world shows us that all these
conditions can be better fulfilled by the Protozoa than by any other
creatures. They can live now equally in those great depths of ocean
where the conditions are most unfavourable to other forms of life,
and in tepid unhealthy pools overstocked with vegetable matter in a
state of putridity. They form a most suitable basis for higher forms
of life. They have remarkable powers of removing mineral matters from
the waters and of fixing them in solid forms. So, in the fitness of
things, a gigantic Foraminifer is just what we need, and after it has
spread itself over the mud and rock of the primeval seas, and built up
extensive reefs therein, other animals may be introduced, capable of
feeding on it, or of sheltering themselves in its stony masses, and
thus we have the appropriate dawn of animal life.
Public-domain text, read in full here on John Shaqi.
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