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
There is one other unsolved problem in the study of life by the
geologist to which it is still necessary to advert. This is the
inability of palæontology to fill up the gaps in the chain of being.
In this respect we are constantly taunted with the imperfection of the
record, a matter so important that it merits a separate treatment; but
facts show that this is much more complete than is generally supposed.
Over long periods of time and many lines of being we have a nearly
continuous chain, and if this does not show the tendency desired,
the fault is as likely to be in the theory as in the record. On the
other hand, the abrupt and simultaneous appearance of new types in
many specific and generic forms and over wide and separate areas at
one and the same time, is too often repeated to be accidental. Hence
palæontologists, in endeavouring to establish evolution, have been
obliged to assume periods of exceptional activity in the introduction
of species, alternating with others of stagnation, a doctrine differing
very little from that of special creation, as held by the older
geologists.
The attempt has lately been made to account for these breaks by the
assumption that the geological record relates only to periods of
submergence, and gives no information as to those of elevation. This
is manifestly untrue. In so far as marine life is concerned, the
periods of submergence are those in which new forms abound for very
obvious reasons, already hinted; but the periods of new forms of land
and fresh-water life are those of elevation, and these have their own
records and monuments, often very rich and ample, as, for example, the
swamps of the Carboniferous, the transition from the great Cretaceous
subsidence, when so much of the land of the Northern Hemisphere
was submerged, to the new continents of the Tertiary, the Tertiary
lake-basins of Western America, the Terraces and raised beaches of
the Pleistocene. Had I time to refer in detail to the breaks in the
continuity of life which cannot be explained by the imperfection of the
record, I could show at least that nature in this case does advance
_per saltum_--by leaps, rather than by a slow continuous process. Many
able reasoners, as Le Conte, in America, and Mivart and Collard in
England, hold this view.
Here, as elsewhere, a vast amount of steady conscientious work is
required to enable us to solve the problems of the history of life. But
if so, the more the hope for the patient student and investigator. I
know nothing more chilling to research, or unfavourable to progress,
than the promulgation of a dogmatic decision that there is nothing to
be learned but a merely fortuitous and uncaused succession, amenable
to no law, and only to be covered, in order to hide its shapeless and
uncertain proportions, by the mantle of bold and gratuitous hypothesis.
Public-domain text, read in full here on John Shaqi.
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