The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
Mr. Croll has, in his valuable work "Climate and Time" and in various
memoirs, brought forward an ingenious astronomical theory to account
for changes of climate. This theory, as stated by himself in a recent
paper,[FB] is that when the eccentricity of the earth's orbit is at a
high value, and the northern winter solstice is in perihelion, agencies
are brought into operation which make the southeast trade-winds stronger
than the northeast, and compel them to blow over upon the northern
hemisphere as far as the Tropic of Cancer. The result is that all the
great equatorial currents of the ocean are impelled into the northern
hemisphere, which thus, in consequence of the immense accumulation of
warm water, has its temperature raised, so that ice and snow must to a
great extent disappear from the arctic regions. In the prevalence of
the converse conditions, the arctic zone becomes clad in ice, and the
southern has its temperature raised.
[FB] "Cataclysmic Theories of Geological Climate," "Geological Magazine,"
May, 1878.
At the same time, according to Croll's calculations, the accumulation
of ice on either pole would tend, by shifting the earth's centre of
gravity, to raise the level of the ocean and submerge the land on the
colder hemisphere. Thus a submergence of land would coincide with a cold
condition, and emergence with increasing warmth. Facts already referred
to, however, show that this has not always been the case, but that in
many cases submergence was accompanied with the influx of warm equatorial
waters and a raised temperature, this apparently depending on the
question of local distribution of land and water; and this in its turn
being regulated not always by mere shifting of the centre of gravity,
but by foldings occasioned by contraction, by equatorial subsidences
resulting from the retardation of the earth's rotation, and by the excess
of material abstracted by ice and frost from the arctic regions, and
drifted southward along the lines of arctic currents. This drifting must
in all geological times have greatly exceeded, as it certainly does at
present, the denudation caused by atmospheric action at the equator,
and must have tended to increase the disposition to equatorial collapse
occasioned by retardation of rotation.[FC]
[FC] Croll, in "Climate and Time," and in a note read before the British
Association in 1876, takes an opposite view; but this is clearly contrary
to the facts of sedimentation, which show a steady movement of _débris_
toward the south and southwest.
While such considerations as those above referred to tend to reduce
the practical importance of Mr. Croll's theory., on the other hand
they tend to remove one of the greatest objections against it--namely,
that founded on the necessity of supposing that glacial periods recur
with astronomical regularity in geological time. They cannot do so if
dependent on other causes inherent in the earth itself, and producing
important movements of its crust.
Public-domain text, read in full here on John Shaqi.
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