Let us consider, in the first place, the chances for the preservation
of remains of the present fauna and flora of a country. The surface of
the land may be densely clothed with forest and abundantly peopled
with animal life. But the trees die and moulder into soil. The
animals, too, disappear, generation after generation, and leave few or
no perceptible traces of their existence. If we were not aware from
authentic records that central and northern Europe were covered with
vast forests at the beginning of our era, how could we know this fact?
What has become of the herds of wild oxen, the bears, wolves and other
denizens of primeval Europe? How could we prove from the examination
of the surface soil of any country that those creatures had once
abounded there? The conditions for the preservation of any relics of
the plant and animal life of a terrestrial surface must obviously be
always exceptional. They are supplied only where the organic remains
can be protected from the air and superficial decay. Hence they may be
observed in (1) the deposits on the floors of lakes; (2) in
peat-mosses; (3) in deltas at river-mouths; and (4) under the
stalagmite of caverns in limestone districts. But in these and other
favourable places a mere infinitesimal fraction of the fauna or flora
of a land-surface is likely to be entombed or preserved.
In the second place, although in the sea the conditions for the
preservation of organic remains are in many respects more favourable
than on land, they are apt to be frustrated by many adverse
circumstances. While the level of the land remains stationary, there
can be but little effective entombment of marine organisms in littoral
deposits; for only a limited accumulation of sediment will be formed
until subsidence of the sea-floor takes place. In the trifling beds of
sand or gravel thrown up on a stationary shore, only the harder and
more durable forms of life, such as gastropods and lamellibranchs,
which can withstand the triturating effects of the beach waves, are
likely to remain uneffaced.
Public-domain text, read in full here on John Shaqi.
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