Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
The plate-bearing ganoids of the Silurian and Devonian, at one time
supposed to be allied to Crustaceans, but whose dignity as "Forerunners
of the back-boned animals" is now generally admitted,[79] are clearly
true fishes, and of somewhat high rank, their strange bony armour being
evidently a special protection against the attacks of contemporary
sharks and gigantic crustaceans; and if we may judge by the Colorado
specimens, their existence dates back almost to the close of the
Cambrian, and they were probably contemporary with small sharks; while
as early as the Silurian and Devonian, if we regard the scaly ganoids
as a distinct type, we have already four types of fishes, and these
akin to those which in modern time we must regard as the highest of
their class.
[79] A. Smith Woodward, "Natural Science," 1892, and _Annals and Maga.
Nat. Hist._, October, 1890. This able naturalist, in introducing his
subject, remarks, from the point of view of an evolutionist:--"Whether
some form of 'worm' gave origin to the forerunners of the great
back-boned race, or whether a primeval relative of the King-crab
turned upside down and rearranged limbs and head these are questions
still admitting of endless discussion, no doubt fruitless in their
main object, but desirable from the new lines of investigation they
continually suggest."
One very little fish of the Devonian, of which specimens have been
kindly sent me by a friend in Scotland,[80] the Palæospondylus of
Traquair, may raise still higher hopes for the early vertebrates. It is
a little creature, an inch to two inches in length, destitute or nearly
destitute of bony covering, having a head which suggests the presence
of external gills, large eyes, and even elongated nasal bones,[81] a
long vertebral column composed of separate bony rings, more than fifty
in number, with possible indications of ribs in front and distinct
neural and haemal processes behind. One cannot look at it without the
suggestion occurring of some of the smaller snake-like Batrachians of
the Carboniferous and Permian; and I should not be surprised if it
should come to be regarded either as a forerunner of the Batrachians or
as a primitive tadpole.
[80] James Reed, Esq., of Allan House, Blairgowrie.
[81] I am aware that Woodward regards these parts differently.
However this may be, the upper part of the Devonian, though rich in
fishes and plants, has afforded no higher vertebrates than its lower
parts, and in the lowest Carboniferous beds we suddenly find ourselves
in the presence of Batrachians with well-developed limbs and characters
which ally them to the Lizards. True lizard-like reptiles appear in
the Permian, and then we enter on that marvellous reign of reptiles,
in which this class assumed so many great and remarkable forms, and
asserted itself in a manner of which the now degraded reptilian class
can afford no conception.
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