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
I need not say to palæontologists that this is not what we actually
find in the primordial rocks. I need but to remind them of the early
and remarkable development of such forms as the Trilobites, the
Lingulidæ and the Pteropods, all of them highly complex and specialized
types, and remote from the embryonic stages of the groups to which
they severally belong. In the case of the Trilobites, one need merely
consider the beautiful symmetry of their parts, both transversely and
longitudinally, their division into distinct regions, the necessary
complexity of their muscular and nervous systems, their highly complex
visual organs, the superficial ornamentation and microscopic structure
of their crusts, their advanced position among Crustaceans, indicated
by their strong affinity with the Arachnidans or spiders and scorpions.
(See figures prefixed.)
All these characters give them an aspect far from embryonic, while, as
Barrande has pointed out, this advanced position of the group has its
significance greatly strengthened by the fact that in early primordial
times we have to deal not with one species, but with a vast and highly
differentiated group, embracing forms of many and varied subordinate
types. As we shall see, these and other early animals may be regarded
as of generalized types, but not as embryonic. Here, then, meets us at
the outset the fact that in as far as the great groups of annulose and
molluscous animals are concerned, we can trace these back no farther
than to a period in which they appear already highly advanced, much
specialized and represented by many diverse forms. Either, therefore,
these great groups came in on this high initial plane, or we have
scarcely reached half way back in the life-history of our planet.
We have, here, however, by this one consideration, attained at once to
two great and dominant laws regulating the history of life. First, the
law of continuity, whereby new forms come in successively, throughout
geological time, though, as we shall see, with periods of greater or
less frequency. Secondly, the law of specialization of types, whereby
generalized forms are succeeded by those more special, and this
probably connected with the growing specialization of the inorganic
world. It is this second law which causes the parallelism between the
history of successive species and that of the embryo.
Public-domain text, read in full here on John Shaqi.
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