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
"May it not therefore be concluded (since, in addition to these
circumstances, its respiration must have required frequent access of
air) that it swam upon or near the surface, arching back its long neck
like the swan, occasionally darting it down at the fish which happened
to float within its reach? It may, perhaps, have lurked in shoal-water
along the coast, concealed among the sea-weed, and, raising its
nostrils to a level with the surface from a considerable depth, may
have found a secure retreat from the assaults of dangerous enemies;
while the length and flexibility of its neck may have compensated for
the want of strength in its jaws and its incapacity for swift motion
through the water, by the suddenness and agility of the attack which
they enabled it to make on every animal fitted for its prey, which
came within its extensive sweep."
More than twenty species of long-necked sea-lizards are known to
geologists.
Professor Owen, in his great work on _British Fossil Reptiles_, when
describing the huge Plesiosaurus dolichodeirus from Dorset, suggests
that the carcase of this monster, after it sank to the bottom of the
sea, was preyed upon by some carnivorous animal (perhaps sharks). It
seems, he says, as if a bite of the neck had pulled out of place the
eighth to the twelfth vertebræ. Those at the base of the neck are
scattered and dispersed as if through more "tugging and riving." So
with regard to its body, probably some hungry creature had a grip of
the spine near the middle of the back, and pulled all the succeeding
vertebræ in the region of the hind limbs. Thus we get a little glimpse
of scenes of violence that took place at the bottom of the bright
sunny seas of the period when the clays and limestones of the Lias
rocks were being deposited in the region of Lyme-Regis.
As time went on, these curious reptiles increased in size, until, in
the period when our English chalk was being formed (Cretaceous
period), they reached their highest point (see p. 147). After that
they became extinct--whether slowly or somewhat suddenly we cannot
tell.
Public-domain text, read in full here on John Shaqi.
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