The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
Lastly, we sometimes have impressions or footprints representing the
locomotion of fossil animals, rather than the fossils themselves. In
this way some extinct creatures are known to us only by their footsteps
on sand or clay, once soft, but now hardened into stone; and in the
case of some of the lower animals the trails thus made are often not
easily interpreted (Figs. 12, 12_a_). It has been found that even
sea-weeds drifted by the tide make impressions of this kind, which, when
they occur in old rocks, are very mysterious. Even rain-drops are
capable of being permanently impressed on rocks, and constitute a kind
of fossils. Besides these we have many kinds of imitative markings which
simulate fossils, as those of concretions or nodules, which are often
very fantastic in shape, those of dendritic crystallisation giving
moss-like forms, and the complicated tracery produced on muddy shores
by the little rills of water which follow the receding tide (Fig. 13).
Such things are often mistaken by the ignorant for fossil remains, but
are easily distinguished by a practised eye.
[Illustration: FIG. 12_a_.—Footprints of modern _Limulus_, or
king-crab, in the sand, which enable us to interpret those in Fig. 12.]
The reader who has followed these, perhaps somewhat dry, details, will
be rewarded for his patience by having some conception of the conditions
in which we find fossil remains, and of the evidence by which we can
refer these to different periods in the history of the earth.
[Illustration: FIG. 13.—Current markings on shale, resembling a fossil
plant. Reduced from a photograph (Dawson’s _Acadian Geology_).]
Carrying this knowledge with us, and at the same time glancing at the
table of successive formations prefixed to this chapter, we shall be
prepared, without any additional geological study, to understand the
statements to be made in the following chapters, and to appreciate the
actual nature of the succession of life in so far as it is at present
known.
[Illustration: MAGNIFIED AND RESTORED SECTION OF A PORTION OF EOZOON
CANADENSE.
The shaded portions show the animal matter of the Chambers, Tubuli,
Canals, and Pseudopodia; the unshaded portions the calcareous
skeleton.]
CHAPTER II.
THE BEGINNING OF LIFE ON THE EARTH.
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