Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
Remains of this remarkable animal of the drift or gravel period
of this country have been found at Brentford and elsewhere near
London. Speaking of this animal, Professor Owen observes, that “it
is commonly supposed that the Lion, the Tiger, and the Jaguar are
animals peculiarly adapted to a tropical climate. The genus Felis (to
which these animals belong) is, however, represented by specimens
in high northern latitudes, and in all the intermediate countries
to the equator.” The chief condition necessary for the presence of
such animals is an abundance of the vegetable-feeding animals. It
is thus that the Indian tiger has been known to follow the herds of
antelope and deer in the lofty mountains of the Himalaya to the verge
of perpetual snow, and far into Siberia. “It need not, therefore,”
continues Professor Owen, “excite surprise that indications should
have been discovered in the fossil relics of the ancient mammalian
population of Europe of a large feline animal, the contemporary of the
mammoth, of the tichorrhine rhinoceros, of the great gigantic cave-bear
and hyæna, and the slayer of the oxen, deer, and equine quadrupeds that
so abounded during the same epoch.” The dimensions of this extinct
animal equal those of the largest African lion or Bengal tiger; and
some bones have been found which seem to imply that it had even more
powerful limbs and larger paws.
THE MAMMOTHS OF THE BRITISH ISLES.
Dr. Buckland has shown that for long ages many species of carnivorous
animals now extinct inhabited the caves of the British islands. In low
tracts of Yorkshire, where tranquil lacustrine (lake-like) deposits
have occurred, bones (even those of the lion) have been found so
perfectly unbroken and unworn, in fine gravel (as at Market Weighton),
that few persons would be disposed to deny that such feline and other
animals once roamed over the British isles, as well as other European
countries. Why, then, is it improbable that large elephants, with a
peculiarly thick integument, a close coating of wool, and much long
shaggy hair, should have been the occupants of wide tracts of Northern
Europe and Asia? This coating, Dr. Fleming has well remarked, was
probably as impenetrable to rain and cold as that of the monster ox of
the polar circle. Such is the opinion of Sir Roderick Murchison, who
thus accounts for the disappearance of the mammoths from Britain:
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