Extinct Monsters: A Popular Account of Some of the Larger Forms of Ancient Animal LifeHutchinson, H. N. (Henry Neville)
Science
Extinct Monsters: A Popular Account of Some of the Larger Forms of Ancient Animal Life
Hutchinson, H. N. (Henry Neville)
Paleontology
Before this discovery the food of the Mammoth was unknown, and all
sorts of theories were devised in order to account for its remains
being found so far north. Some thought that the Mammoth lived in
temperate regions, and that the carcases were swept down by great
floods into higher and colder latitudes. But it would be impossible
for the bodies to be hurried along a devious course for so many miles
without a good deal of injury, and probably they would fall to pieces
on the way. But, as Professor Owen has so convincingly argued, there
is no reason why herds of Mammoths should not have obtained a
sufficient supply of food in a country like the southern part of
Siberia, where trees abound in spite of the fact that during a great
part of the year it is covered with snow. And this is his line of
reasoning. The molar teeth of the elephant show a highly complicated
and peculiar structure, and there are no other quadrupeds that feed to
such an extent on the woody fibre of the branches of trees. Many
mammals, as we know, eat the leaves of trees; some gnaw the bark; but
elephants alone tear down and crunch the branches. One would think
there was but little nourishment to be got from such. But the hard
vertical plates of their huge grinders enable them to pound up the
tough vegetable tissue and render it more or less palatable. Of
course, the foliage is the most tempting, but where foliage is scarce
something more is required.
Now, in the teeth of the Mammoth the same principle of construction is
observed, only with greater complexity, for there are more of these
grinding plates and a larger proportion of dense enamel. Hence the
inference seems unmistakable that the extinct species fed more largely
on woody fibre than does the elephant of to-day. Forests of hardy
trees and shrubs still grow upon the frozen soil of Siberia, and skirt
the banks of the Lena as far north as the sixtieth parallel of
latitude.
If the Mammoth flourished in temperate latitudes only, as formerly
suggested, then its thick shaggy coat becomes superfluous and
meaningless; but if it lived in the region where its body has been
found, then the argument from its teeth, and the fir-spikes found in
its stomach, is confirmed by the nature of its skin, and all the old
difficulties vanish. Professor Owen considers that we may safely infer
that, if living at the present day, it would find a sufficient supply
of food at all seasons of the year in the sixtieth parallel, and even
higher. Perhaps they migrated north during the summer; and, judging
from the present limits of arboreal vegetation, they may have been
able to subsist even in latitude 70° north, for at the extreme points
of Lapland pines attain a height of sixty feet.[66]
[66] Sir Henry Howorth, in his _Mammoth and the Flood_, suggests
another theory, and gives some valuable information.
Public-domain text, read in full here on John Shaqi.
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