The Pamphlet Collection of Sir Robert Stout: Volume 53
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he lectures recently delivered by Mr. W. Denton have excited some little interest in the science of Geology, and more particularly in the associated science which is now known under the general title of Biology. We confess to a feeling of surprise that these lectures should have provoked the controversy which appears to have arisen in our Southern cities, for there was very little in the entire series, either by way of argument or illustration, that is not tolerably familiar, not merely to the scientific student, but to the reader of the ordinary magazine literature of the day; and the elementary facts which formed the staple of the geological lectures have been taught in our schools for the last twenty years. It is hardly a subject of complaint, however, that in explaining a science like geology Mr. Denton has been unable to submit much that is new to his audiences, for the details of the constant additions to our stock of knowledge of this science are of too technical and trivial a kind to interest a miscellaneous audience. And it must be said of Mr. Denton that even to scientific listeners he made ample amends for the familiarity of his materials by the freshness which he imparted in their preparation for the public. Scientific study is too little engaged in by the people for us to undervalue in any way such a course of lectures, and we heartily wish they had been better attended.
While saying so much, however, we are not to be interpreted as implying that exception might not be taken to some of the geological positions which Mr. Denton has laid down. In the face of the serious demurrers that have been entered by high authorities against the theory of a wholly fluid interior, Mr. Denton's definition of the earth's crust, as not exceeding 100 miles in thickness, was too positive. And there are even stronger objections to the stress he placed on the Whitney skull. It is worthy of remark that Professor Boyd Dawkins (whose right to speak with authority on such a subject Mr. Denton will hardly gainsay) has discussed this very question in a lecture during the current term at Owen College, Manchester. He examined the
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claims put forward by Professor Whitney, State geologist of California, on behalf of the Calaveras skull, and also those which have been made with respect to the skull found in the railway cutting at Olmo and the remains found by Professor Cappellini in Italy. Having considered fairly all the circumstances connected with these discoveries, Professor Dawkins declared emphatically that "the evidence of pliocene man fell to the ground equally in Europe and in the United States."
We are not disposed to cavil at the view which an enthusiastic geological student—as Mr Denton undoubtedly is—may choose to take of questions that are still undetermined, and on which diversity of opinion is allowable, though in such cases it is desirable to avoid dogmatism. We have, however, a more serious charge to make against his exposition of the present position of the doctrine of evolution in its relation to the origin of men. Few scientific believers in the Darwinian theory have ever claimed that the theory has reached the point of absolute demonstration. One of its most uncompromising champions, writing very recently, candidly acknowledges that" there are vast chasms to be filled up) by future observation," and while speaking of the theory merely as "doing as much as any other ingenious theory has done," contends for it as only plausible escape from an admission of the miraculous. The same writer roundly abuses Professor Owen as "a trimmer," for admitting even a thought of God into the calculation, by his expressed belief in the existence of an innate "tendency" animating nature towards a certain form of future development in accordance with the predestinated purpose of the Deity. Nor does Darwin escape censure from him for a similar weakness.*
* "The Doctrine of Descent and Darwinism," by Oscar Schmidt, Professor in Strasburg University, 1876.
† "Professor Hutton's Address on Biology," Canterbury College, March, 1882.
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* Lyell's "Manual of Elementary Geology,"
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* Huxley's "Man's Place in Nature."
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So also in the "testimony of the rocks." It is not deniable that, in the preparation of the earth for the support of man and the higher mammalia, there is disclosed by the fossil remains of the geological strata, a succession of life that has been generally, though by no means invariably, from lower forms to higher forms, but it is scarcely pretended by anyone that there is satisfactory proof of a traceable relationship between the types that have disappeared and those that succeeded them. The exceptions to this statement are as rare as the readiness to seize and parade them is eager among the evolutionists. What standard of evolutionary perfection are we to adopt? Taking size as the measure of progressive development, the animals, reptiles, and birds now existing, are puny and degenerate representatives of those that once roamed the earth.
If the geological record and the facts of natural history had told the story of evolution, its acceptance would not have been delayed until the publication of Darwin's speculations. But the observations of the chiefs of the scientific world were almost universally against it. Early in the century Lamarck and Geoffroy St. Hilaire had hazarded the theory, in conjunction with spontaneous generation, as a plausible explanation of the origin of life; but Cuvier, the greatest naturalist the world has produced, confuted them. Lamarck, relying mainly upon the variations produced upon animals in a state of domesticity, hoped for the discovery of the remains of some of these creatures nearer the time when they were taken from their native habitats. The proof came; not merely in fossil remains, but in preserved bodies of dogs and cats found among the mummies of Egypt. Cuvier demonstrated that 2000 or 3000 years of domesticity in every variety of climate had made no
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perceptible change in the anatomy of these animals as we know them. The labours of Cuvier, therefore, which closed with his death in 1832, tended only to confirm the observations of his great predecessor Linnaeus, who even declared that genera like species are primordial creations.* The work was taken up by Agassiz, one of the most careful observers of the century, who early declared his conviction that "the revelations of science unequivocally indicate the direct intervention of creative power,"† and who remained an inveterate opponent of the theory of descent up to the time of his death in 1873. Coming to the observers in the department of geology, we pass over Hugh Miller's defence of the Mosaic account of the creation, only to find Sir Charles Lyell, so late as 1855, with the whole geological record laid bare before him, writing vigorously against the doctrine of transmutation of species. It is true that since the publication of the "Origin of Species," in 1858, he has embodied in his "Principles of Geology" and "Geological Evidences of the Antiquity of Man," Mr Darwin's theory as a suggestive and plausible one; but the evidences of transmutation of species have remained in every material respect just as they were before Darwin's book appeared, despite the advent of the little Orohippus and the so-called lizard-tailed bird, over which the Darwinians have shed tears of rapture. It is a sufficient indication of the general tenor of the teachings of geology, that a most industrious personal search among the rocks, extending over thirty years, during which he had completely systematized the whole science of geology, left Sir Charles Lyell an active opponent of the doctrine of transmutation of species. Truly, if, as Mr Denton averred, it be a token of ignorance to express a doubt about the doctrine of descent we have the consolation of being in good company even among the Darwinians, to say nothing of the vast number of thinkers, scientific and philosophical, who still defend the theory of special creations, not excepting that American scientist who, in a certificate to Mr Denton's status, made a special reservation against committing himself to that gentlemen's views on this subject.
* Lyell's "Principles of Geology.'
† Agassiz and Gould's "Comparative Physiology."