Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
It was for many years suggested that the marsupial order to which the
fossil animals of Stonesfield were supposed exclusively to belong
constitutes the lowest grade in the class Mammalia, and that this order,
of which the brain is of more simple form, evinces an inferior degree of
intelligence. If, therefore, in the oolitic period the marsupial tribes
were the only warm-blooded quadrupeds which had as yet appeared upon our
planet, the fact, it was said, confirmed the theory which teaches that
the creation of the more simple forms in each division of the animal
kingdom preceded that of the more complex. But on how slender a support,
even if the facts had continued to hold true, did such important
conclusions hang! The Australian continent, so far as it has been
hitherto explored, contains no indigenous quadrupeds save those of the
marsupial order, with the exception of a few small rodents, while some
neighboring islands to the north, and even southern Africa, in the same
latitude as Australia, abound in mammalia of every tribe except the
marsupial. We are entirely unable to explain on what physiological or
other laws this singular diversity in the habitations of living mammalia
depends; but nothing is more clear than that the causes which stamp so
peculiar a character on two different provinces of wide extent are
wholly independent of time, or of the age or maturity of the planet.
The strata of the Wealden, although of a later date than the oolite of
Stonesfield, and although filled with the remains of large reptiles,
both terrestrial and aquatic, have not yielded as yet a single marsupial
bone. Were we to assume on such scanty data that no warm-blooded
quadrupeds were then to be found throughout the northern hemisphere,
there would still remain a curious subject of speculation, whether the
entire suppression of one important class of vertebrata, such as the
mammiferous, and the great development of another, such as the
reptilian, implies a departure from fixed and uniform rules governing
the fluctuations of the animal world; such rules, for example, as appear
from one century to another to determine the growth of certain tribes of
plants and animals in arctic, and of other tribes in tropical regions.
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