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
It may, perhaps, be inquired whether there is any evidence for the
existence of a tail-fin, such as is shown in our illustration. To this
it may be replied that the presence of such an appendage is as good as
proved by a certain flattening of the vertebræ at the end of the tail,
detected by Owen. The direction of this flattening is from side to
side, and therefore the tail-fin must have been vertical, like that of
a fish. In one specimen Sir Richard Owen has detected as many as 156
vertebræ to the whole body.
Our description of the fish-lizard has, we trust, been
sufficient--although not couched in the language used by men of
science--to give a fair idea of its structure and habits.
In conclusion, a few words may be said about the ancestry and
life-history of these ancient monsters. Palæontologists have good
reason to believe that they were descended from some early form of
land reptile. If so, they show that whales are not the first land
animals that have gone back to the sea, from which so many forms of
life have taken their rise.
During the long Mesozoic period fish-lizards played the part that
whales now play in the economy of the world; and they resembled the
latter, not only in general shape, but in the situation of the
nostrils (near the eye), and in their teeth and long jaws. But these
curious resemblances must not be interpreted to mean that whales and
fish-lizards are related to each other. They only show that similar
modes of life tend to produce artificial resemblances--just as some
whales, in their turn, show a superficial resemblance to fishes.
With regard to the particular form of reptile from which the
fish-lizard may have been derived, no certain conclusion has at
present been arrived at. This is chiefly from want of fuller knowledge
of early forms, such as may have existed in the previous periods known
as the Carboniferous and Trias (see Appendix I.). But there are
certain features in the skulls, teeth, and vertebræ that suggest a
relationship with the Labyrinthodonts, or primæval salamanders that
flourished during the above periods, or at least from amphibians more
or less closely allied to them. They cannot by any possibility be
regarded as modified fishes; for fishes have gills instead of lungs.
The fish-lizards played their part, and played it admirably; but their
days were numbered, and the place they occupied has since been taken
by a higher type--the mammal. As reptiles, they were eminently a
success; but, then, they were only reptiles, and therefore were at
last left behind in the struggle for existence, until finally they
died out, at the end of the Cretaceous period, when certain important
geographical and other changes took place, helping to cause the
extinction of many other strange forms of life, as we shall see later
on (see p. 147).
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