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
In Australia, New Zealand, and many other parts of the southern
hemisphere, where the indigenous land quadrupeds are comparatively few,
and of small dimensions, the reptiles do not predominate in number or
size. The deposits formed at the mouth of an Australian river, within
the tropics, might contain the bones of only a few small marsupial
animals, which, like those of Stonesfield, might hereafter be discovered
with difficulty by geologists; but there would, at the same time, be no
megalosauri and other fossil remains, showing that large saurians were
plentiful on the land and in the waters at a time when mammalia were
scarce. This example, therefore, would afford a very imperfect parallel
to the state of the animal kingdom, supposed to have prevailed during
the secondary periods, when a high temperature pervaded European
latitudes.
It may nevertheless be advantageous to point to some existing anomalies
in the geographical development of distinct classes of vertebrata which
may be comparable to former conditions of the animal creation brought to
light by geology. Thus in the arctic regions, at present, reptiles are
small, and sometimes wholly wanting, where birds, large land quadrupeds,
and cetacea abound. We meet with bears, wolves, foxes, musk oxen, and
deer, walruses, seals, whales, and narwals, in regions of ice and snow,
where the smallest snakes, efts, and frogs are rarely, if ever, seen.
A still more anomalous state of things presents itself in the southern
hemisphere. Even in the temperate zone, between the latitudes 52° and
56° S., as, for example, in Tierra del Fuego, as well as in the woody
region immediately north of the Straits of Magellan, and in the Falkland
Islands, no reptiles of any kind are met with, not even a snake, lizard,
or frog; but in these same countries we find the guanaco (a kind of
llama), a deer, the puma, a large species of fox, many small rodentia,
besides the seal and otter, together with the porpoise, whale, and other
cetacea.
On what grand laws in the animal physiology these remarkable phenomena
depend, cannot in the present state of science be conjectured; nor could
we predict whether any opposite condition of the atmosphere, in respect
to heat, moisture, and other circumstances, would bring about a state of
animal life which might be called the converse of that above described,
namely, a state in which reptiles of every size and order might abound,
and mammalia disappear.
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