The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
Dr. Andrews was travelling in Egypt some years ago, and joined a
party of officers of the great survey of Egypt in a visit to the
Great Western Desert, the rainless, sandy waste west of the Nile, not
very far from what is now called the Fayoum, and where in Roman days
was the great Lake Mœris, now dried up to a mere brine pool, in the
salt water of which the fresh-water fishes of the Nile still live.
The surveying party intended to determine the geological age of these
sands, which stretch for hundreds of miles, often rising into cliffs
which are cut sharp by the wind and show horizontal stratification.
The geologists determined that the sands of this region were of
Eocene and Miocene Age, and from them Dr. Andrews brought home
some very interesting bones. These included the remains of a more
primitive Mastodon than any as yet known, and of an animal which he
called Meritherium, which is a connecting link between elephants
and other mammals. The collection included also remains of great
flesh-eating beasts, and of sea cows, of tortoises, and of a snake
sixty feet long!
However, in regard to the history of elephants, the upshot of Dr.
Andrews' most important discoveries is that we find living here in
the Upper Eocene period (which is older than the age in which the
_Tetrabelodon Mastodon_ was found) an elephant ancestor of the kind
to which Dr. Andrews gave the name of _Palæomastodon_ or "ancient
mastodon." We thus arrive at an ancestral elephant-like creature
which serves to join the elephant stock on to more ordinary mammals.
This beast was not so very big, perhaps about the same size as an
ordinary cart-horse.
Dr. Andrews' further triumph was the additional discovery of the
rather smaller animal which he called the _Meritherium_, and which
was undoubtedly an elephant of sorts, though at first sight it has no
resemblance to one, and probably had no trunk at all. It certainly
had no big tusks; but its teeth make us certain that it belonged
to the elephant family. "Here, then," says Sir E. Ray Lankester,
"we have arrived at a form which undoubtedly was closely related
to the ancestors of all the elephants, if not actually itself that
ancestor, and in it we see the origin of the elephants peculiar
structure. From this comparatively normal pig-like _Meritherium_, the
wonderful elephant, with his upright face, his dependent trunk, and
his huge spreading tusks has been gradually, step by step, produced.
And we have seen some, at least, of the intermediate steps--the
lengthening of the jaws and the increase in the size of the teeth in
the _Palæomastodon_--carried still further on by the _Tetrabelodon_,
and then followed by a shrinkage of the lower jaw and final evolution
of the middle part of the face and upper jaw into the drooping,
wonderful, prehensile trunk."
Public-domain text, read in full here on John Shaqi.
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