Discourses: Biological & Geological: EssaysHuxley, Thomas Henry
Science
Discourses: Biological & Geological: Essays
Huxley, Thomas Henry
Biology; Geology
The very remarkable results which have been brought to light by the
sounding and dredging operations, which have been carried on with such
remarkable success by the expeditions sent out by our own, the American,
and the Swedish Governments, under the supervision of able naturalists,
have a bearing in the same direction. These investigations have
demonstrated the existence, at great depths in the ocean, of living
animals in some cases identical with, in others very similar to, those
which are found fossilised in the white chalk. The _Globigerinoe_,
Cyatholiths, Coccospheres, Discoliths in the one are absolutely identical
with those in the other; there are identical, or closely analogous,
species of Sponges, Echinoderms, and Brachiopods. Off the coast of
Portugal, there now lives a species of _Beryx_, which, doubtless, leaves
its bones and scales here and there in the Atlantic ooze, as its
predecessor left its spoils in the mud of the sea of the Cretaceous
epoch.
Many years ago[1] I ventured to speak of the Atlantic mud as "modern
chalk," and I know of no fact inconsistent with the view which Professor
Wyville Thomson has advocated, that the modern chalk is not only the
lineal descendant of the ancient chalk, but that it remains, so to speak,
in the possession of the ancestral estate; and that from the Cretaceous
period (if not much earlier) to the present day, the deep sea has covered
a large part of what is now the area of the Atlantic. But if
_Globigerina_, and _Terebratula caput-serpentis_ and _Beryx_, not to
mention other forms of animals and of plants, thus bridge over the
interval between the present and the Mesozoic periods, is it possible
that the majority of other living things underwent a "sea-change into
something new and strange" all at once?
[Footnote 1: See an article in the _Saturday Review_, for 1858, on
"Chalk, Ancient and Modern."]
6. Thus far I have endeavoured to expand and to enforce by fresh
arguments, but not to modify in any important respect, the ideas
submitted to you on a former occasion. But when I come to the
propositions touching progressive modification, it appears to me, with
the help of the new light which has broken from various quarters, that
there is much ground for softening the somewhat Brutus-like severity with
which, in 1862, I dealt with a doctrine, for the truth of which I should
have been glad enough to be able to find a good foundation. So far,
indeed, as the _Invertebrata_ and the lower _Vertebrata_ are concerned,
the facts and the conclusions which are to be drawn from them appear to
me to remain what they were. For anything that, as yet, appears to the
contrary, the earliest known Marsupials may have been as highly organised
as their living congeners; the Permian lizards show no signs of
inferiority to those of the present day; the Labyrinthodonts cannot be
placed below the living Salamander and Triton; the Devonian Ganoids are
closely related to _Polypterus_ and to _Lepidosiren_.
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