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
Whether, then, in questioning our proto-foraminifer, we have reference
to the vital functions of its gelatinous sarcode, to the complexity
and beauty of its calcareous test, or to its capacity for effecting
great material results through the union of individuals, we perceive
that we have to do, not with a low condition of those powers which we
designate life, but with their manifestation through the means of a
simple organism; and this in a degree of perfection which we, from our
point of view, would have in the first instance supposed impossible.
If we imagine a world altogether destitute of life, we still might
have geological formations in progress. Not only would volcanoes belch
forth their liquid lavas and their stones and ashes, but the waves and
currents of the ocean and the rains and streams on the land, with the
ceaseless decomposing action of the carbonic acid of the atmosphere,
would be piling up mud, sand, and pebbles in the sea. There might even
be some formation of limestone taking place where springs charged
with bicarbonate of lime were oozing out on the land or the bottom of
the waters. But in such a world all the carbon would be in the state
of carbon dioxide, and all the limestone would either be diffused in
small quantities through various rocks or in limited local beds, or
in solution, perhaps as chloride of calcium, in the sea. Dr. Hunt has
given chemical grounds for supposing that the most ancient seas were
largely supplied with this very soluble salt, instead of the chloride
of sodium, or common salt, which now prevails in the sea water.
Where in such a world would life be introduced? on the land or in the
waters? All scientific probability would say in the latter.[67] The
ocean is now vastly more populous than the land. The waters alone
afford the conditions necessary at once for the most minute and the
grandest organisms, at once for the simplest and for others of the most
complex character. Especially do they afford the best conditions for
those animals which subsist in complex communities, and which aggregate
large quantities of mineral matter in their skeletons. So true is this
that up to the present time all the species of Protozoa and of the
animals most nearly allied to them are aquatic. Even in the waters,
however, plant life, though possibly in very simple forms, must precede
the animal.
[67] A recent writer (Simroth) has, however, undertaken to maintain the
thesis that land life preceded that in the sea. It is unnecessary to
say that he is an evolutionist, influenced by the necessity laid upon
that philosophy to deduce whales, seals, etc., from land animals.
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