Water Reptiles of the Past and PresentWilliston, Samuel Wendell
Science
Water Reptiles of the Past and Present
Williston, Samuel Wendell
Aquatic reptiles; Aquatic reptiles, Fossil
It has been thought that these nothosaurs, so intermediate in structure
between the true plesiosaurs and land reptiles, were the actual
ancestors, but this is rather doubtful. It is probable that they were
only very closely akin to the real ancestors, since in some ways they
had become specialized too much, and, as we have already explained,
highly specialized characters or organs can never go back to their
earlier condition. The nothosaurs do prove beyond all possibility of
doubt that the plesiosaurs were at least the descendants of animals
closely allied to them, so closely, indeed, that it is doubtful whether
we could distinguish external differences were all of them actually
living at the present time.
[Illustration: FIG. 49.—_Lariosaurus balsami_.]
We have repeatedly seen that all aquatic animals have some or all the
bones of the limbs shortened, and it is of interest to observe that the
early plesiosaurs had longer forearm and foreleg bones than the later
ones, just as we have seen was the case with the early ichthyosaurs.
It would seem probable that all the early plesiosaurs had long necks,
though some of the late ones in Cretaceous times had relatively short
necks, shorter even than the known nothosaurs possessed.
The nothosaurs doubtless lived about the shores of the ancient seas,
spending much of their time in the water, leaving it perhaps when hard
pressed by their enemies, as do some modern reptiles, or to rear their
young. The teeth of the nothosaurs are long and slender in front,
shorter behind. The animals must therefore have been carnivorous in
habit, feeding probably upon such fishes as they could catch, and the
various invertebrates which live in shallow water. The structure of the
jaws and their attachments are quite as in the plesiosaurs, proving
that they could not have swallowed large objects; but the skull is
broader and flatter than that of most plesiosaurs, indicating habits
not unlike those of the modern alligators and crocodiles.
Some time we shall doubtless find remains of nothosaurs or nearly
allied animals elsewhere than in Europe, but probably not from later
deposits than the Triassic. So far as we now know, their geological
range and geographical distribution were much restricted; they
evidently wholly died out shortly after the plesiosaurs appeared.
CHAPTER VII
ANOMODONTIA
LYSTROSAURUS
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