Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
Just as political geography sometimes presents boundaries not
in accordance with the physical structure of countries, so the
distribution of animals and plants shows many peculiar and unexpected
features. Hence naturalists have divided the continents into what
Sclater has called zoological regions, which are, so to speak, the
great empires of animal life, divisible often by less prominent
boundaries into provinces. In vegetable life similar boundaries may
be drawn, more or less coincident with the zoological divisions.
Zoologically, North America and Greenland may be regarded as one
great region, the Nearctic, or new Arctic, the prefix not indicating
that the animals are newer than those of the old world, which is by
no means the case. South America constitutes another region the
Neotropical. If now we turn to the greater Eurasian continent, with
its two prolongations to the south in Africa and Australia, we shall
find the whole northern portion, from the Atlantic to the Pacific,
constituting one vast region of animal life, the Palearctic, which also
includes Iceland and a strip across North Africa. Africa itself, with
Madagascar, whose allegiance is, however, only partial, constitutes
the Ethiopian region. India, Burmah, the south of China, and certain
Asiatic islands form the Oriental region. Australia, New Guinea, and
the Polynesian islands constitute the Australian region. All of these
regions may in a geological point of view be considered as portions of
old and permanent continental masses, which, though with movements of
elevation and depression, have continued to exist for vast periods.
Some of them, however, seem to have enjoyed greater immunity from
causes of change than others, and present, accordingly, animals and
plants having, geologically speaking, an antique aspect in comparison.
In this sense the Australian province may be regarded as the oldest of
all in the facies of its animal forms, since creatures exist there of
genera and families which have very long ago become extinct everywhere
else. Next in age to this should rank the Neotropical or South American
region, which, like Australia, presents many low and archaic forms
of animal life. The Ethiopian region stands next to it in this, the
Oriental and Nearctic next, and last and most modern in its aspect is
the great Palearctic region, to which man himself belongs, and the
animals and plants of which vindicate their claims to youth by that
aggressive and colonizing character already referred to, and which has
enabled them to spread themselves widely over the other regions, even
independently of the influence of man. On the other hand, the animals
and plants of the Australian and South American regions show no such
colonizing tendency, and can scarcely maintain themselves against those
of other regions when introduced among them. Thus we have at once
in these continental regions a great and suggestive example of the
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