The Story of the Earth and ManDawson, John William, Sir
Science
The Story of the Earth and Man
Dawson, John William, Sir
Human beings -- Origin; Paleontology
The London clay is lower Eocene; but in the beds of the Isle of Wight
and neighbouring parts of the South of England, we have the middle and
upper members of the series. They are not, however, so largely
developed as in the Paris basin, where, resting on the equivalent of
the London clay, we have a thick marine limestone, the Calcaire
Grossier, abounding in marine remains, and in some beds composed of
shells of foraminifera. The sea in which this limestone was deposited,
a portion no doubt of the great Atlantic area of the period, became
shallow, so that beds of sand succeeded those of limestone, and
finally it was dried up into lake basins, in which gypsum, magnesian
sediments, and siliceous limestone were deposited. These lakes or
ponds must at some period have resembled the American "salt-licks,"
and were no doubt resorted to by animals from all the surrounding
country in search of the saline mud and water which they afforded.
Hence in some marly beds intervening between the layers of gypsum,
numerous footprints occur, exactly like those already noticed in the
Trias. Had there been a Nimrod in those days to watch with bow or
boomerang by the muddy shore, he would have seen herds of heavy
short-legged and three-hoofed monsters (Palæotherium), with large
heads and long snouts, probably scantily covered with sleek hair, and
closely resembling the Modern Tapirs of South America and India,
laboriously wading through the mud, and grunting with indolent delight
as they rolled themselves in the cool saline slime. Others more light
and graceful, combining some features of the antelope with those of
the Tapir (Anoplotherium) ran in herds over the drier ridges, or
sometimes timidly approached the treacherous clay, tempted by the
saline waters. Other creatures representing the Modern Damans or
Conies--"feeble folk" which, with the aspect of hares, have the
structure of Pachyderms--were also present. Creatures of these types
constituted the great majority of the animals of the Parisian Eocene
lakes; but there were also Carnivorous animals allied to the hyæna,
the wolf, and the opossum, which prowled along the shores by night to
seize unwary wanderers, or to prey on the carcases of animals mired in
the sloughs. Wading birds equal in size to the ostrich also stalked
through the shallows, and tortoises crawled over the mud.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account