The Book of History (Vol. 1 of 18): A History of All Nations from the Earliest Times to the PresentVarious
History
The Book of History (Vol. 1 of 18): A History of All Nations from the Earliest Times to the Present
Various
World history
Now, plants obtain their nitrogen mainly from the minute proportion
of ammonia that exists in the atmosphere, and this ammonia is formed
by the union of the nitrogen of the air with the hydrogen of the
water-vapour under the influence of electric discharges--that is,
of thunderstorms. It is evident, then, that the required amount of
this essential compound will depend upon a due adjustment of the
quantities of nitrogen and aqueous vapour always present; while the
electric discharges seem to be due to the friction of various strata
of air with each other and with the earth’s surface, due to the winds
and storms; and winds are due to highly complex causes, involving
the rate of the earth’s rotation, the rise and fall of the tide, the
density of the atmosphere, the quantity of its aqueous vapour, and the
amount of solar heat which it receives. Unless all these very diverse
factors existed in their due proportion, some of the results might be
highly prejudicial if not quite inimical to the development of life.
To these various adaptations of our gaseous envelope we must add one
other. Carbonic acid gas in the atmosphere is absolutely essential
to vegetable life, while it is directly antagonistic to that of the
higher animals. Its quantity must, therefore, be strictly proportionate
to the needs of both; and that beneficial proportion must have been
preserved throughout the whole period of the existence of the higher
air-breathing animals.
These various considerations show us that our atmosphere, consisting
as it does mainly of two common gases mixed together, and therefore
seeming to most people one of the simplest things possible, is really a
wonderfully complex arrangement which is adapted to serve the purposes
of living organisms in a great variety of ways. But this by no means
exhausts the subject of its adaptation to support and develop organic
life, because its very existence on the earth in a suitable quantity
and composed of the essential elements can be shown to depend on other
and deeper relations which will now be pointed out.
The older writers on the subject of the habitability of the planets
took no account whatever of the importance of size, distance from the
sun, period of rotation, and obliquity of the ecliptic as determining
the possibility of organic life, but simply assumed that, because the
earth possessed an abundant life-development, all the other planets
must also possess it. But we know that the above-mentioned factors are
of very high importance, as we will proceed briefly to point out.
[Sidenote: Earth’s Envelope of Gas]
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