Science from an Easy ChairLankester, E. Ray (Edwin Ray), Sir
History
Science from an Easy Chair
Lankester, E. Ray (Edwin Ray), Sir
Natural history; Science
[Illustration: FIG. 20.—The heraldic basilisk, also called the
Amphysian Cockatrice. Observe the second head at the end of its tail—a
feature due to perversion of the observation that there are some
snake-like creatures (Amphisbena) with so simple a head that it is at
first sight difficult to say which end of the creature is the head and
which is the tail.]
Without looking further into the strange and fantastic catalogue of
imaginary monsters, one must recognise that it is a matter of great
interest to trace the origin of these marvellous creations of human
fancy, and the way in which they have first of all been brought into
pictorial existence, and then variously modified and finally stereotyped
and maintained by tradition and art. It has not infrequently been
suggested, since geologists made us acquainted with the bones of huge
and strange-looking fossil reptiles dug from ancient rocks, that the
tradition of “the dragon” is really a survival of the actual knowledge
and experience of these extinct monsters on the part of “long-ago races
of men.” It is a curious fact, mentioned by a well-known writer, Mrs.
Jameson, that the bones of a great fossil reptile were preserved and
exhibited at Aix in France as the bones of the dragon slain by St.
Michael, just as the bones of a whale are shown as those of the mythical
Dun-cow of Warwick in that city.
There are three very good reasons for not entertaining the suggestion
that the tradition of the dragon and similar beasts is due to human
co-existence with the great reptiles of the past. The first is that the
age of the rocks known as cretaceous and jurassic (or oölitic), in which
are found the more or less complete skeletons of the great
saurians—many bigger in the body than elephants, and with huge tails in
addition, iguanodon, megalosaurus, diplodocus, as well as the winged
pterodactyles (see Plate II., where a representation is given of what we
know as to the form and bearing of two species of pterodactyle) and a
vast series of such creatures—is so enormously remote that not only man
but all the hairy warm-blooded animals like him, did not come into
existence until many millions of years after these rocks had been
deposited by water and the great reptiles buried in them had become
extinct. The cave-men of the Pleistocene period are modern, even close
to us, as compared with the age when the great saurians flourished. That
was just before the time when our chalk-cliffs were being formed as a
slowly growing sediment on the floor of a deep sea. No accurate measure
of the time which has elapsed since then is possible, but we find that
about 200 ft. thickness of deposit has been accumulated since the date
of the earliest human remains known to us—whilst over 5000 ft. have
accumulated since the chalk began to be deposited, and the great
saurians ceased to exist. If we reckon, in accordance with the most
moderate estimate, a quarter of a million years for the upper 200 ft. of
Public-domain text, read in full here on John Shaqi.
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