Half Hours With Modern Scientists: Lectures and EssaysTyndall, John
Philosophy
Half Hours With Modern Scientists: Lectures and Essays
Tyndall, John
Science
Thus we see the order already pointed out to be true, and to be an
ascending one. This is the more evident as each type or class passes
through the conditions of those below it, as did the mammal; each
scale being shorter as its highest terminus is lower. Thus the
crocodile passes through the stage of the lamprey, the fish, the
batrachian and the reptile proper.
_b. In Time._ We have thus a scale of relations of existing forms of
animals and plants of a remarkable kind, and such as to stimulate
greatly our inquiries as to its significance. When we turn to the
remains of the past creation preserved to us in the deposits
continued throughout geologic time, we are not disappointed, for
great light is at once thrown upon the subject.
We find, in brief, that the lowest division of the animal kingdom
appeared first, and long before any type of a higher character was
created. The Protozoön, Eozoön, is the earliest of animals in
geologic time, and represents the lowest type of animal life now
existing. We learn also that the highest branch appeared last. No
remains of Vertebrates have been found below the lower Devonian
period, or not until the Echinoderms and Molluscs had reached a
great preëminence. It is difficult to be sure whether the Protozoa
had a greater numerical extent in the earliest periods than now, but
there can be no doubt that the Cœlenterata (corals) and Echinoderms
(crinoids) greatly exceeded their present bounds, in Paleozoic time,
so that those at present existing are but a feeble remnant. If we
examine the subdivisions known as classes, evidence of the nature of
the succession of creation is still more conclusive. The most
polyp-like of the Molluscs (brachiopoda) constituted the great mass
of its representatives during Paleozoic time. Among Vertebrates the
fishes appear first, and had their greatest development in size and
numbers during the earliest periods of the existence of the
division. Batrachia were much the largest and most important of land
animals during the Carboniferous period, while the higher
Vertebrates were unknown. The later Mesozoic periods saw the reign
of reptiles, whose position in structural development has been
already stated. Finally, the most perfect, the mammal, came upon the
scene, and in his humblest representatives. In Tertiary times
mammalia supplanted the reptiles entirely, and the unspiritual
mammals now yield to man, the only one of his class in whom the
Divine image appears.
Thus the structural relations, the embryonic characters, and the
successive appearance in time of animals coincide. The same is very
probably true of plants.
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