Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
INTRODUCTION xxix<br />
ments met with in the steins and vessels of plants, leaves, hairs, fruits, &c. ; in the nerves, the umbihcal cord, the<br />
cochlea of the ear, the ventricles of the mammahan heart, the stomach, bladder, uterus, &o. All these structures<br />
are spiral because of original endowment and bias.<br />
An outstanding argument in favour of Design and Original Purpose is to be found in the give-and-take movements<br />
or rhythms common alike to the inorganic and organic kingdoms. The physical universe gives to and takes<br />
from plants and animals light, heat, moisture, &c., during the day and laight, and the seasons. The importance<br />
of day and night and the seasons to plants and animals cannot be over-estimated. These changes ensure periods<br />
of activity and periods of comparative repose ; periods for feeding and growing ; periods for reproducing, &c. If<br />
there were no alternations of day and night and of the seasons, the whole economy of plants and animals would be<br />
changed. They would cease to be healthy, and would probably cease to exist.<br />
Day and night and the seasons are due to well-known cosmic changes ; namely, to the rotation of the earth<br />
on its axis every twenty-four hours, and to the earth revolving round the sun once in 365 days. The sun and light<br />
and the earth, and the earth's atmosphere, were necessarily created before plants and animals. The latter are<br />
parts of a designed whole.<br />
The unfailing recurrence of day and night and the seasons were all considered before plants and animals were<br />
formed. The inorganic and organic kingdoms were clearly made for each other, and form complemental parts of<br />
one great scheme.<br />
" Oldest of all the formations lonown to geologists, and representing perhaps the earliest rocks produced after<br />
our earth had ceased to be a molten mass, are the hard, crystalhne, and much contorted rocks, named by the late<br />
Sir W. E. Logan Laurentian, and which are largely developed in the northern parts of North America and Europe,<br />
and in many other regions. ... In the lower part of this great system of rocks which, in some places at least, is<br />
thirty thousand feet in thickness, we find no traces of the existence of any living thing on the earth. But in the<br />
middle portion of the Laurentian, rocks are found which indicate that there were already land and water, and that<br />
the waters and possibly the land were already tenanted by Uving beings. The great beds of limestone which exist<br />
in this part of the system furnish one indication of this. . . . The cUmate and atmosphere of the Laurentian may<br />
have been well adapted for the sustenance of vegetable life. We can scarcely doubt that the internal heat of the<br />
earth still warmed the waters of the sea, and these warm waters must have diffused great quantities of mists and<br />
vapours over the land, giving a moist and equable if not a very clear atmosphere. The vast quantities of carbon<br />
dioxide afterwards sealed up in Hmestones and carbonaceous beds must also have still floated in the atmosphere and<br />
must have suppUed abundance of the carbon, which constitutes the largest ingredient in vegetable tissues. Under<br />
these circumstances the whole world must have resembled a damp, warm greenhouse, and plants loving such an<br />
atmosphere could have grown luxuriantly. In these circumstances the lower forms of aquatic vegetation and those<br />
that love damp, warm air and wet soil would have been at home. .<br />
" It may fairly be assumed that in the present world, and in those geological periods with whose organic remains<br />
we are more familiar than with those of the Laurentian, there is no other source of unoxidised carbon in rocks than<br />
that furnished by organic matter, and that this has obtained its carbon in all cases, in the first instance, from the<br />
deoxidation of carbonic acid by hving plants. . .<br />
" In the later geological formations the limestones are mostly organic—that is, they consist of accumulated<br />
remains of shells, corals, and other hard parts of marine animals."<br />
Sir WiUiam Dawson, to whom I am indebted for the foregoing extracts, furnishes the annexed table indicating<br />
the order in which plants and animals appeared on the earth.i<br />
It will be seen from the table on p. xxx that plants and animals become more complex with the advance of<br />
time, there being what may be regarded as types of plants and animals, and an ascending series in both. Thus the<br />
Bozoic age furnished Protogens and Algae in plants, and Protozoa in animals ; the Palaeozoic age, Acrogens and<br />
Gymnosperms in plants, and Invertebrates, Amphibians, and Fishes in animals ; the Mesozoic age, Cycads and Pines<br />
in plants, and Reptiles in animals ; the Kainozoic age, Angiosperms, Palms, &c., in plants, and Mammals and Man<br />
in animals.<br />
It also shows that creation, considered from the geologic standpoint, is a progressive work, that is, a work which<br />
consists of stages and has been accomphshed at different times. This was a priori to be expected. The earth and<br />
its climate had to be prepared for the advent of plants and animals, and the plants and animals were created in<br />
succession and varied according to the condition of the earth and climate at particular periods. This accounts<br />
for the prevalence of rank vegetation and huge animals at one period of the earth's history, and for a less luxuriant<br />
vegetation and a more refined fauna at another. It also accounts for changes in the flora and fauna of different<br />
regions of the earth at different times, due to vicissitudes of climate ; the remains of temperate and tropical plants<br />
and animals being not unfrequently found in the same district.<br />
1 "The Geological History of Plants " {International Scicntilio Series, London, 1888, pp. 4 and 8).<br />
.