<h2><span class="pagenum"><SPAN name="P21"></SPAN></span><SPAN name="chapV"></SPAN>V<br/> THE AGE OF THE COAL SWAMPS</h2>
<p>The land during this Age of Fishes was apparently quite lifeless. Crags and
uplands of barren rock lay under the sun and rain. There was no real
soil—for as yet there were no earthworms which help to make a soil, and
no plants to break up the rock particles into mould; there was no trace of moss
or lichen. Life was still only in the sea.</p>
<p>Over this world of barren rock played great changes of climate.
The causes of these changes of climate were very complex and they
have still to be properly estimated. The changing shape of the
earth’s orbit, the gradual shifting of the poles of rotation,
changes in the shapes of the continents, probably even fluctuations
in the warmth of the sun, now conspired to plunge great areas of
the earth’s surface into long periods of cold and ice and now
again for millions of years spread a warm or equable climate over
this planet. There seem to have been phases of great internal
activity in the world’s history, when in the course of a few
million years accumulated upthrusts would break out in lines of
volcanic eruption and upheaval and rearrange the mountain and
continental outlines of the globe, increasing the depth of the sea
and the height of the mountains and exaggerating the extremes of
climate. And these would be followed by vast ages of comparative
quiescence, when frost, rain and river would wear down the mountain
heights and carry great masses of silt to fill and raise the sea
bottoms and spread the seas, ever shallower and wider, over more
and more of the land. There have been “high and deep”
ages in the world’s history and “low and level”
ages. The reader must dismiss from his mind any idea that the
surface of the earth has been growing steadily cooler since its
crust grew solid. After that much cooling had been achieved, the
internal temperature ceased to affect surface
<span class="pagenum"><SPAN name="P22"></SPAN></span>conditions.
There are traces of periods of superabundant ice and snow, of
“Glacial Ages,” that is, even in the Azoic period.</p>
<p>It was only towards the close of the Age of Fishes, in a period of
extensive shallow seas and lagoons, that life spread itself out in
any effectual way from the waters on to the land. No doubt the
earlier types of the forms that now begin to appear in great
abundance had already been developing in a rare and obscure manner
for many scores of millions of years. But now came their
opportunity.</p>
<div class="fig"> <SPAN name="img-22"></SPAN> <ANTIMG src="images/img-22.jpg" alt="A CARBONIFEROUS SWAMP" width-obs="450" height-obs="634" /> <p class="caption">
A CARBONIFEROUS SWAMP
<br/>
<small><i>A Coal Seam in the Making</i></small></p>
</div>
<p>Plants no doubt preceded animal forms in this invasion of the land,
but the animals probably followed up the plant emigration
<span class="pagenum"><SPAN name="P23"></SPAN></span>very closely.
The first problem that the plant had to solve was the problem of
some sustaining stiff support to hold up its fronds to the sunlight
when the buoyant water was withdrawn; the second was the problem of
getting water from the swampy ground below to the tissues of the
plant, now that it was no longer close at hand. The two problems
were solved by the development of woody tissue which both sustained
the plant and acted as water carrier to the leaves. The Record of
the Rocks is suddenly crowded by a vast variety of woody swamp
plants, many of them of great size, big tree mosses, tree ferns,
gigantic horsetails and the like. And with these, age by age,
there crawled out of the water a great variety of animal forms.
There were centipedes and millipedes; there were the first
primitive insects; there were creatures related to the ancient king
crabs and sea scorpions which became the earliest spiders and land
scorpions, and presently there were vertebrated animals.</p>
<div class="fig"> <SPAN name="img-23"></SPAN> <ANTIMG src="images/img-23.jpg" alt="SKULL OF A LABYRINTHODONT, CAPITOSAURUS" width-obs="383" height-obs="468" /> <p class="caption">
SKULL OF A LABYRINTHODONT, CAPITOSAURUS
<br/>
<small><i>Nat. Hist. Mus.</i></small></p>
</div>
<p>Some of the earlier insects were very large. There were dragon flies
in this period with wings that spread out to twenty-nine inches.</p>
<p>In various ways these new orders and genera had adapted themselves
to breathing air. Hitherto all animals had breathed air dissolved
in water, and that indeed is what all animals still have to do.
But now in divers fashions the animal kingdom was acquiring the
power of supplying its own moisture where it was needed. A man
with a perfectly dry lung would suffocate to-day;
<span class="pagenum"><SPAN name="P24"></SPAN></span>his lung
surfaces must be moist in order that air may pass through them
into his blood. The adaptation to air breathing consists in all
cases either in the development of a cover to the old-fashioned
gills to stop evaporation, or in the development of tubes or other
new breathing organs lying deep inside the body and moistened by a
watery secretion. The old gills with which the ancestral fish of
the vertebrated line had breathed were inadaptable to breathing
upon land, and in the case of this division of the animal kingdom
it is the swimming bladder of the fish which becomes a new,
deep-seated breathing organ, the lung. The kind of animals known
as amphibia, the frogs and newts of to-day, begin their lives in
the water and breathe by gills; and subsequently the lung,
developing in the same way as the swimming bladder of many fishes
do, as a baglike outgrowth from the throat, takes over the business
of breathing, the animal comes out on land, and the gills dwindle
and the gill slits disappear. (All except an outgrowth of one gill
slit, which becomes the passage of the ear and ear-drum.) The
animal can now live only in the air, but it must return at least to
the edge of the water to lay its eggs and reproduce its kind.</p>
<div class="fig"> <SPAN name="img-24"></SPAN> <ANTIMG src="images/img-24.jpg" alt="SKELETON OF A LABYRINTHODONT: THE ERYOPS" width-obs="670" height-obs="243" /> <p class="caption">
SKELETON OF A LABYRINTHODONT: THE ERYOPS
<br/>
<small><i>Nat. Hist. Mus.</i></small></p>
</div>
<p>All the air-breathing vertebrata of this age of swamps and plants
belonged to the class amphibia. They were nearly all of them forms
related to the newts of to-day, and some of them attained a
considerable size. They were land animals, it is true, but they
were land animals needing to live in and near moist and swampy
places, and all the great trees of this period were equally
<span class="pagenum"><SPAN name="P25"></SPAN></span>amphibious in
their habits. None of them had yet developed fruits and seeds of a
kind that could fall on land and develop with the help only of such
moisture as dew and rain could bring. They all had to shed their
spores in water, it would seem, if they were to germinate.</p>
<p>It is one of the most beautiful interests of that beautiful science,
comparative anatomy, to trace the complex and wonderful adaptations
of living things to the necessities of existence in air. All
living things, plants and animals alike, are primarily water
things. For example all the higher vertebrated animals above the
fishes, up to and including man, pass through a stage in their
development in the egg or before birth in which they have gill
slits which are obliterated before the young emerge. The bare,
water-washed eye of the fish is protected in the higher forms from
drying up by eyelids and glands which secrete moisture. The weaker
sound vibrations of air necessitate an ear-drum. In nearly every
organ of the body similar modifications and adaptations are to be
detected, similar patchings-up to meet aerial conditions.</p>
<p>This Carboniferous age, this age of the amphibia, was an age of life
in the swamps and lagoons and on the low banks among these waters.
Thus far life had now extended. The hills and high lands were
still quite barren and lifeless. Life had learnt to breathe air
indeed, but it still had its roots in its native water; it still
had to return to the water to reproduce its kind.</p>
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