The Cambridge natural history, Vol. 08 (of 10)Gadow, Hans
Science
The Cambridge natural history, Vol. 08 (of 10)
Gadow, Hans
Animals
The eggs, having been deposited during the Southern summer, from November
to January or February, in holes on a sunny and sandy spot, contain nearly
ripe embryos in the following August. They are, however, not hatched until
about thirteen {300}months old. In the meantime they seem to undergo a kind
of aestivation. The nasal chambers become blocked with proliferating
epithelium, which is resorbed shortly before hatching.
I have kept half-a-dozen specimens in a green-house for several years, and
have come to the conclusion that they are dull, not companionable
creatures, in spite of their imposing, rather noble appearance when, with
their heads erect, they calmly look about with their large, quiet eyes.
Each dug its own hole in the hard ground underneath and between large
stones. At dusk they sat in front of the holes or walked leisurely to the
pan with the earthworms which formed their principal food. Meat they did
not touch, but they killed and chewed up lizards and blind-worms. Sometimes
they soaked themselves for many hours in the shallow, warm water. The skin
is shed in flakes. I never found them basking in the sun, and the pineal
eye, still so well developed in these strange creatures, caused them no
distress when bright light was thrown upon it. They grew tame enough not to
run away when found roaming about at night, but they did not like being
handled, and they inflicted the most painful bites when taken up
carelessly. The biggest, a male, was rather quarrelsome, grunted much, and
worried the others.
_SUB-CLASS III.–THEROMORPHA._
The Theromorpha comprise a great number of extraordinary, extinct reptiles,
which as a group had a wide range in space and time. The earliest known
occur in the Lower Red Sandstone of Thuringia and Bohemia, and in the
middle Permian strata of Russia. The majority have been found in strata
transitional between the Permian and the Triassic age, notably in the
Karroo sandstone of South Africa and in corresponding levels of North
America. Closely allied to them are those of the Triassic sandstone of
Elgin in Scotland, and of India. They seem to have died out with the
Muschelkalk or Middle Trias.
The various genera exhibit such a diversity of structure, shape, and size,
and many are still so imperfectly known, that {301}any diagnosis is liable
to be faulty, even assuming that they are a homogeneous group. To avoid
confusion, we characterise the Theromorpha as _Reptiles with a firmly fixed
quadrate, a single temporal arch, an interparietal foramen, and a pelvis in
which the pubes and ischia form one stout, ventral symphysis_.
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