Extinct Monsters: A Popular Account of Some of the Larger Forms of Ancient Animal Life — John Shaqi
Extinct Monsters: A Popular Account of Some of the Larger Forms of Ancient Animal LifeHutchinson, H. N. (Henry Neville)
Science
Extinct Monsters: A Popular Account of Some of the Larger Forms of Ancient Animal Life
Hutchinson, H. N. (Henry Neville)
Paleontology
But air and water have a way of penetrating into all sorts of places,
so that in nature they are almost everywhere. Water can slowly filter
through even the hardest rocks, and since it contains dissolved air,
it causes the decay of animal or vegetable substances. Take the case
of a dead leaf falling into a lake, or some quiet pool in a river. It
sinks to the bottom, and is buried up in gravel, mud, or sand. Now,
our leaf will stand a very poor chance of preservation on a sandy or
gravelly bottom, because these materials, being porous, allow the
water to pass through them easily. But if it settles down on fine mud
it may be covered up and become a fossil. In time the soft mud will
harden into clay or shale, retaining a delicate impression of the
leaf; and even after thousands of years, the brown body of the leaf
will be there, only partly changed. In the case of the plants found in
coal, the lapse of ages since they were buried up has been so great
(and the strata have been so affected by the great pressure and by the
earth's internal heat) that certain chemical changes have converted
leaves and stems into carbon and some of its compounds, much in the
same way that, if you heat wood in a closed vessel, you convert it
into charcoal, which is mostly carbon. The coal we burn in our fires
is entirely of vegetable origin, and every seam in a coal-mine is a
buried forest of trees, ferns, reeds, and other plants.
The reader will understand how it is that rocks composed of hardened
sand or gravel, sandstones and conglomerates, contain but few fossils;
while, on the other hand, such rocks as clay, shale, slate, and
limestone often abound in fossils, because they are formed of what was
once soft mud, that sealed up and protected corals, shell-fish,
sea-urchins, fishes, and other marine animals. Had they been covered
up in sand the chances are that percolating water would have slowly
dissolved the shells and corals, the hard coats of the crabs, and the
bones of the fishes, all of which are composed of carbonate of lime;
and we know that is a substance easily dissolved by water.
Public-domain text, read in full here on John Shaqi.
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