The Story of the Earth and ManDawson, John William, Sir
Science
The Story of the Earth and Man
Dawson, John William, Sir
Human beings -- Origin; Paleontology
If we turn now to these latter rocks, and inquire as to their
conditions on our two great plateaus, we shall find a repetition of
changes similar to those which occurred in the times preceding. The
sandy shallows of the earlier part of this period give place to wide
oceanic areas similar to those of the Lower Silurian; In these we find
vast and thick coral and shell limestones, the Wenlock of England and
Niagara of America, as rich in life as the limestones of the Lower
Silurian, and with the generic and family forms similar, but the
species for the most part different. In America these limestones were
followed by a singularly shallow condition of the plateau, in which
the surface was so raised as at times to be converted into separate
salt lakes in which beds of salt were deposited. On both plateaus
there were alternations of oceanic and shallow conditions, under which
the Lower Helderberg and Ludlow beds, the closing members of the
Silurian, were laid down. Of the Atlantic beds of this period we know
little, except that the great limestones appear to be wanting, and to
be replaced by sandy and muddy deposits, in some parts at least of the
margins of the area. In some portions also of the plateaus and their
margins, extensive volcanic outbursts seem to have occurred; so that
the American plateau presented, at least in parts, the aspect of a
coral sea with archipelagos of volcanic islands, the ejections from
which became mixed with the aqueous deposits forming around them.
Having thus traced the interesting series of geographical conditions
indicated by the Silurian series, we may next take our station on one
of the submerged plateaus, and inquire as to the new forms of life now
introduced to our notice; and in doing so shall include the life of
both the Lower and Upper Silurian.
[Illustration: Fig. 9.--Fragment of Lower Silurian Limestone, sliced
and magnified ten diameters, showing the manner in which it is made up
of fragments of corals, crinoids, and shells. (From a paper oil the
Microscopic Structure of Canadian limestone, "Canadian Naturalist.")]
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