Page images
PDF
EPUB
[blocks in formation]

218. net each.

THE

to

HE first volume of this important work, noticed in NATURE of January 19, 1905, and already in its second edition, dealt with geological processes and their results. In the two volumes now before us, which complete the work, geology is treated from the historical side, and we have a comprehensive review of the history of the earth on systematic lines. The treatment of these two formally separable branches of the science is, however, such as emphasise the essential unity of the whole. As geological processes were discussed with continual reference to the historical application of the principles laid down; so the evolution of the globe, which is the story of these latter volumes, is regarded consistently from the causal point of view. Indeed, some subjects already considered under the head of geological processes, such as the dynamics of deformation, the causes of glaciation, &c., are now more fully discussed in connection with the particular geological periods which most clearly exemplify the phenomena.

The part of the work which will be read with greatest interest is that which falls under the subtitle "Genesis." Considering geology as "the domestic chapter of astronomy," the authors devote much more space than is customary in geological treatises to the problem of the origin and primitive condition of the globe. This is, we think, amply justified by the fundamental place which cosmogony necessarily occupies in the construction of the science. It is evident that opinion concerning such questions as the causes of crust-movements, the essential mechanism of igneous action, the origin of the atmosphere and hydrosphere, the beginning of life, must be controlled by the view adopted, formally or tacitly, of the mode of origin of the earth as a planet. Less obviously, but not less surely, some theory of the earth's initial state is involved in numerous geological doctrines, the dependence of which on such considerations is liable to be overlooked; and the authors do good service in recalling this fact repeatedly in the historical record which follows. The clear recognition of cosmogony as the foundation of geology, by revealing an unsuspected element of hypothesis at various places in the superstructure, offers a warning which is perhaps in some quarters not wholly unnecessary.

The special interest of this part of the book, however, lies in the first complete exposition of the "planetesimal" theory, which the senior author has already propounded elsewhere. That our solar system has in some manner been evolved from a nebula of some kind is an assumption to which few will demur; but the particular theory associated with the name of Laplace, and generally known as the nebular hypothesis, starting from a gaseous nebula of extreme

tenuity, has for some time been felt to involve difficulties, which become more serious upon a closer examination. These difficulties are cogently stated by the authors, especial stress being laid on the great discrepancy which Moulton has pointed out from a consideration of the actual distribution of moment of momentum in the solar system. The meteoritic hypothesis, whether in Lockyer's or in Darwin's form, is held by the authors to be open to the same objections as the theory of a gaseous nebula, with which, indeed, it is practically identical as regards its more important consequences. According to the planetesimal hypothesis, the constituents of the system might be molecules or small masses of any kind moving in orbits about a common centre, the essential point being that their behaviour depended, not on mutual collisions (as on the meteoritic hypothesis), but on revolution in independent orbits. supposition there was, after the initial nebula was once formed, no fundamental change in the dynamics of the system, but only a progressive aggregation of the infinitesimal planetoids ("planetesimals") to form the planets and their satellites as they now exist.

On this

The original nebula postulated was not a gaseous one, but belonged to the type giving a continuous spectrum, and had, like most of these, the spiral form. There were also, as in such nebulæ in general, knots of denser aggregation which became the nuclei of the several planets, though the greater part of the material outside the central helioid was still widely scattered. The manner in which such a system may have been developed from an ancestral helioid by the near approach of another star is tentatively pictured; but this is no essential part of the hypothesis, which is concerned, not with the whole evolution of the solar system, but with the birth and subsequent history of the planets. Starting with the conception of an infinitude of small masses revolving in different elliptic orbits of considerable eccentricity, with a certain degree of clustering already pronounced, the authors discuss the manner in which these planetesimals became aggregated into planets, moving in orbits of only small eccentricity, and with rotation in the same direction as the orbital revolution.

It is for the mathematician rather than the geologist to pass judgment upon this new treatment of the dynamical problems involved, but the geologist must be vitally interested in the verdict. The earth as built up on the planetesimal hypothesis will be a very different body from the earth as condensed from a gaseous spheroid, and must have passed through very different stages of evolution since it acquired individuality. The first-formed solid nucleus was probably devoid of any atmospheric envelope, its attraction being insufficient to control the rapidly moving molecules of gases. An appreciable atmosphere had probably been gathered when the growing globe had attained one-tenth of its present mass (being then comparable with Mars). The atmosphere would at first be collected from outside, but there was already a large quantity of occluded gases in the material built into the solid globe, which might eventually be

set free by extrusive agency, and continues to be a
source of supply to the present time. The nature of
the primitive atmosphere may be conjectured from the
known occluded gases in crystalline rocks and
meteorites, having regard also to a certain selective
effect depending on molecular weights. Carbon
dioxide was probably abundant and nitrogen only a
minor constituent, the latter, in virtue of its chemical
inertness, having accumulated progressively through-
out subsequent time. It is supposed also that the
oxygen in the present atmosphere has mainly been
set free by the agency of vegetable life. The
initiation of vulcanism is next considered, involving a-Huronian, Animikean, and Keweenawan.
discussion of the thermal conditions in the growing
globe. The heat produced by the infall of the planet-
esimals was probably important only in the earlier
stages of growth, and the chief source of the earth's
internal heat is ascribed to the progressive compression
of the central parts. It is estimated that this cause
alone would suffice to reach the melting temperature
of rock when the earth had acquired one-tenth of its
present mass. On account of the originally hetero-
geneous composition of the globe, local spots of fusion
would arise, the occluded gases presumably playing
a part in the process, and, aided by the varying differ-
ential attractions of the sun and moon, the molten
matter would gradually work its way outward. This
action is supposed to be facilitated by "selective
fusion," the more fusible materials encountered being
taken up and the more refractory of the old materials
deposited. In the general theory of igneous action
developed by the authors there is evidently much that
is debatable. In particular, the assumption that
minerals have their melting points raised without
limit by increased pressure, is one to which many
physicists will demur. The maximum melting point
found by Damien and others for various organic
bodies, and considered by Tamman to be a general
property, has led Arrhenius to very different con-
clusions concerning the actual condition of the earth's
interior.

offers most of novelty, but the larger portion of the
two volumes deals, on a more familiar model, with
the several geological periods in order. The Archæan
era is regarded as representing the climax of igneous
action (or, as it is confusingly styled, volcanic action),
and as being concurrently a time of intense crustal de-
formation. The Huronian and other pre-Cambrian
formations which follow the Archæan are grouped as
Proterozoic-an unfortunate choice, since the name
has already been used by Lapworth for the Lower
Palæozoic. The Lake Superior region is taken as the
typical area, and three distinct systems are recognised

Another part of our authors' system which fails to carry complete conviction is the explanation offered for the initiation of the ocean-basins. The cardinal fact to be accounted for is the lower density of the crust in the continental areas as compared with that beneath the ocean floor. The difference is here attributed to the weathering and leaching action on the land, as contrasted with the relative protection of the rocks under the sea. It is supposed that the selective action of degradation and transportation sets up in time an appreciable difference in composition between the average material of the continental and that of the suboceanic tracts, the former becoming more acid and so lighter, and the latter more basic and therefore denser. The effect would be cumulative, and the difference of density established would be permanent, not being obliterated by subsequent metamorphism. In this way there might be evolved, from an originally fortuitous disposition of the growing hydrosphere, a distribution of land and water having a high degree of relative permanence.

We have dwelt on that part of the work which

The

great fossiliferous systems are then dealt with in turn. the chief innovations as regards systematic arrangement being the division of the Carboniferous into two, Mississippian and Pennsylvanian, and the separation of the Lower Cretaceous as a distinct system under the name Comanchean. Under each head the development of the stratified sequence in the North American continent is described and its interpretation discussed, the probable geographical conditions of the North American area at different periods being illustrated by maps. The corresponding strata of other parts of the world are dismissed more summarily. This plan is natural in a work designed primarily for American students, and its inconvenience is felt only in certain cases where the American record is incomplete or inadequate, especially in the Permian and Jurassic periods. We have, however, as a digression, a good account of the widespread glaciation in the southern hemisphere in Permian times, with excellent figures (after Schwarz) of glaciated rock-surfaces and boulder deposits in South Africa. We think that the authors have succeeded in giving a fairly complete and wellproportioned sketch of the earth's history in its successive chapters. The only serious defect which we find is the slight notice accorded to igneous action, and especially the failure (except in the earliest chapters) to recognise this as an essential part of geological history, closely bound up with the tectonic development of the globe.

As re

For reasons connected with the curriculum of American universities, the history of life is treated in great measure apart from the physical history of the earth, a plan not without practical disadvantages. No attempt is made to give a complete "roll-call of the flora and fauna of each period, but attention is directed especially to the main lines of biological development from the evolutionary standpoint. gards the evolution of life in general, it is supposed that more than half of the complete history antedate> the first fair record, offered by the Cambrian strata, in which we have abundant evidence of a development already far advanced. For this reason the Cambrian faunas are dealt with at some length. Similarly, in the Carboniferous we have for the first time a large mass of material bearing on the evolution of plant life, and this receives due notice, with a digression discussing the origin of coal and the climatic conditions implied in the profusion of vegetable life at that epoch.

The arrangement of the book is in most respects

well adapted to the requirements of students, and the presentation of the subject-matter is always clear. In the biological sections Transatlantic freedom of style is sometimes carried so far as to savour of the evening Press, paragraphs being headed, for example, "New Devices of the Bryozoans" and "The Protozoans make a Record." The abundant figures are well chosen, and, within the limitations of black and white, usually well executed, but the glazed paper, on which the whole is printed, is an offence to the sensitive eye. The work as a whole is one which will find a welcome in England as well as in America. The planetesimal theory, too, whatever its ultimate fate, is at least a spirited protest against any narrow limitation of geological time, and may serve to fortify timid geologists against the thunders of certain mathematicians, too apt to forget the precarious basis upon which their calculations are built. A. H.

THE GENESIS OF THE INVENTOR. Erfindung und Erfinder. By A. du Bois-Reymond. Pp. vi+284. (Berlin J. Springer, 1906.) 5 marks.

IN

Price

N his opening chapter, Herr du Bois-Reymond gives an historical survey of the development of the Patent Laws in civilised countries. They date from the Act of Parliament passed in the year 1623, which in its first clause abolished the long-standing grievance known as monopolies, by which favoured individuals had the exclusive right to sell such things as salt and coal; the second clause established a new variety of monopoly, out of which patent rights had their origin. Little has been altered in principle since that date. Even down to the term of fourteen

years the system still holds good, rights being granted to "any new manufactures." Other countries, adopting the idea at much later dates, attempted a more formal definition of invention, and legal logic has constantly tried to define the admissible and the inadmissible. Herr du Bois-Reymond shows that in Germany, since the year 1889, the number of patents granted has varied between 29 per cent. and 45 per cent. of the number of applications filed, and, therefore, assuming the quality of the inventions to be on an average the same from year to year, it would seem that the official mind is not yet certain in its workings.

The author's analysis of the nature of invention and inventors leads to the conclusion that neither need, nor chance, nor the lack of necessaries in surrounding life suffices to draw out the inventor. Instead of solving the problem by philosophic deductions from generalities, he descends to the particulars of the Patent Office, and concludes that inventors can be subdivided into three classes :-first, the intuitive genius, or, as Herbert Spencer would have said, the man who can do with little trouble that which cannot be done by the ordinary man with any amount of trouble; secondly, the technical man, well acquainted with his work, who follows in the wake of the intuitive genius, and is largely inspired by him; thirdly, the layman, whose special province

seems to be feeding-bottles. We are inclined to think that too much stress can be laid on the existence and qualifications of the first class. A long series of inductive reasonings, followed generally by equally laborious experiment, is the usual course of a successful invention. Helmholtz and Darwin were not inventors, but their methods were the same. Helmholtz said that in his work he could only liken himself to the mountaineer, painfully and slowly climbing, often obliged to turn backwards, lighting later on new traces leading forward, and finally reaching the goal, only to find to his confusion that a plain road led thither, if he had only had the eyes to see. Darwin said he thought he was superior to the common run of men in noticing things which easily escape attention, and in observing them carefully. "My industry has been nearly as great as it could have been in the observation and collection of facts. Herein lies the real spirit of the pioneer. Nothing is more useful than the quality on which Darwin naively lays stress, viz. that of noticing things which escape attention; and those who hope to reach the promised land without wandering in the wilderness are probably doomed to disappointment.

Such

Superficially, chance seems to play a large part; but Herr du Bois-Reymond maintains that chance only determines whether this or that individual shall do the deed, and has nothing to do with whether or not the deed shall be done. This is probably true in those cases in which attention is directed to a problem from various sides owing to a main directing cause. was the result of Moissan's discovery of the production of calcium carbide in the electric furnace. The acetylene generator seems to follow as a matter of course. Moissan had no heed for the commercial exploitation of such things, and many others, becoming aware of the existence of an obvious need, which appeared to be capable of being dealt with without the aid of the calculus, rushed in, left the relics of their labours in the files of the Patent Office, and discovered later that they were wholly unacquainted with the conditions of the problem. In this case mere inspiration leads nowhere; laborious experiment is much more to the point, and chance only comes in, having regard to the number of men at work on the task, in determining who shall lodge his application first. That cannot properly be called chance which is merely the outcome of some unlooked-for combination or slight variation of procedure; it is precisely for these things that the inventor toils, and when they come within his sight he merely recognises that for which he has patiently hoped.

Herr du Bois-Reymond concludes by considering the reaction on civilised life which is due to the existence of the inventor. The idea of protecting the inventor was only an indirect cause of the Patent Laws in most countries. A more direct impulse was probably given by the view that the prosperity of the State was likely to be increased by such encouragement as could be given to the creation of industries. Still, Faraday's commercial value has been incalculable, but he received little encouragement from Patent Laws, while

Watt was obliged to circumvent them in order to carry on his business. Moreover, the State undoubtedly profits directly. It is asserted by men competent to judge that the amount received in patent fees is greater than all the profits made by inventors. In other words, the average profit made on an invention is not sufficient to cover the charges made by the State. Herr du Bois-Reymond's book may be recommended to those who take an interest in the philosophic analysis of these questions, and they may also hope to find much worldly wisdom scattered throughout its pages, and a wealth of illustration, drawn from the experience of a busy life.

W. H. S.

BIOLOGICAL PHILOSOPHY.

The volume on Ethics has some excellences the discussion of the origin of morality, for example, with what the author regards as the most important proposition he has to offer, viz. that organic evolution. reproductive evolution, and moral evolution are interdependent. Some other things are not quite so convincing-the statement that there has been far more vicious than virtuous obedience in human history, or another that morality is æons of æons older than the oldest creed, the proof offered being that a cat cares for its kittens. Apparently morality began ages before man was ever heard of, though, in a different context, Dr. Saleeby describes a baby as non-moral, premoral, or if you like, immoral."

There is a hard saying on one page to the effect that historians of the (inaccurate and picturesque) school of Carlyle and Froude are no longer in request.

Psychology (pp. 124); Sociology (pp. 124); Ethics This comes with rather a bad grace from one (pp. 118). By Dr. C. W. Saleeby. Three vols. Scientific Series. (Edinburgh and London: T. C. and E. C. Jack.) Price 18. net each.

DR.

R. SALEEBY discusses the problems of philosophy from the Spencerian standpoint in an interesting fashion. Of the three volumes, that on Psychology appears much the best; it is the most serious, and though the author has there one bête noire in the person of Dr. Ward, who suffers vicariously for all the sins of "academic psychology," the reader is not wearied, as in the Ethics volume, by incessant declamation against Nietzscheanism, on the one hand, and what is politely called 'hell-fire morality" on the other.

[ocr errors]

On psychology our author has nothing very startling to say. He defines his subject as the science, not of consciousness, but of mind. He favours the Wundtian theory of psychophysical parallelism. He regards mind as a product and phenomenon of evolution; or rather, having boldly stated that life is prior to mind, he closes one of two chapters on the evolution of mind by maintaining that the responsiveness of the leucocyte to irritation points to sentiency on its part, and by withdrawing his bold statement in favour of a bolder, that life and mind are co-equal, co-extensive, and of common origin. That is to say, he levels up the leucocyte to man. In the latter part of his book he dwells much more on the will than on the intellectual functions, as he wishes, not to lead up to a text-book on logic, but to the consideration of conduct. The result is that many questions which one finds discussed in the ordinary handbooks are not even mentioned in this; but, of course, amid the multiplicity of cheap introductory works there is no reason why all should go in the same ruts.

In the volume on Sociology one notes that our author follows the Spencerian line that the State has no consciousness of its own, and therefore the welfare of the State never means anything more or other than the welfare of the citizens. He follows his master, too, very closely in his opposition to free education, which he thinks as bad as free breakfasts for the children. A later chapter is occupied with an indictment of the modern city, and others with a discussion of socialism, conservatism, and liberalism.

whose merits are probably-quanto intervallo !— much like those of the writers named; while his defects include an inadequate apprehension of the real issues involved and a stumbling knowledge of Greek. For logos does not mean science, nor is teleology derived from the word meaning "at a distance."

BIOLOGY OF THE FROG.

The Biology of the Frog. By Samuel J. Holmes. Ph.D. Pp. vii+370. (New York: The Macmillan Company; London: Macmillan and Co., Ltd., 1906.) Price 6s. 6d. net.

IN

N the vast literature that treats of the frog there is no comprehensive summary of its biology. Every natural history teacher has realised this want, which has increased in proportion with the great recent extension of instruction in elementary natural phenomena. No animal is more thoroughly known from the anatomical, histological, and embryological aspects, but on the side that appeals to teachers and commencing students, the study of habit and function, existing knowledge of the frog is scattered and often untrustworthy. This gap the author strives to fill. writing primarily for the student. His book is a compilation of what is known of the behaviour of the frog and of its several organs. Unfortunately it is not only this. Dr. Holmes has not freed himself sufficiently from formal and dogmatic zoology. He must have all the nomenclature and the anatomy of the medical school, as though we could never learn or teach zoology without a load of descriptive structural details. The new wine of comparative physiology has been poured into the old vessel and has burst it, leaking out now here now there, so that no good draught is obtainable. The wine, however, is good, and the more pity the framework was not better adapted to hold it and yield it to the thirsty soul.

The frog enters on p. 62, chapter ii. Here "we begin our study." Unfortunately there are two earlier chapters, with which most readers will begin. The first deals with the classification of Amphibia, and ought to have been simplified or postponed. The

chapter of the book an idea of the process of evolution.

Few misprints occur, but "Wiederscheim" for the distinguished anatomist of Freiburg is of irritating F. W. G.

second is the main ecological chapter, and involves
the use of many anatomical expressions that a young
student will not understand until later. The mode of
protrusion of the tongue by lymph pressure; the
changes in the liver, fat-body, and gonads; the form-frequency.
ation of new blood corpuscles and other difficult
topics, are referred to before so much as a brief refer-
ence to the chief features of the frog itself.

The succeeding chapters are arranged on the stereotyped anatomical plan. In reference to the external features, no remark is made of the prevalence or significance of the dark upper sides and light under sides of animals, or of the meaning of gradational shading. A green pigment is attributed to the frog at the close of the third chapter and denied on p. 192. Descriptions of the internal organs, of development, and of the histology of the different organic systems occupy the rest of the book. We have, however, admirable summaries of physiological action under each histological section, and for these teachers will be thankful. The treatment of the skin and of the blood, of digestion and respiration calls for praise. The seasonal metabolic changes in the tissues of the frog are well described under the various organs that are affected, and the references will enable one to find the original papers with ease.

The book is one that will prove useful to every teacher of elementary biology, and its usefulness would have been enhanced by a thorough-going biological treatment and simplification of the anatomical details. Few biological writers realise what a stimulus to teachers and to taught lies in a new mode of presentation of a well-worn subject. In the writing of a biology of the frog a superb opportunity has presented itself of boldly embarking on the physiological method and of subordinating anatomy to the working out of function and response. Moreover, the biology of the frog is not well worn. It is, in contrast with anatomical knowledge, inaccessible and scattered, and with much labour it has been brought together for the first time. With so much novelty at his disposal one cannot help regretting that the author has adopted an arrangement for his work that puts biology into a subordinate place, with the result that he has made a useful but not an illuminating work.

It is in no carping spirit that we point out a few suggestions and corrections for a second edition. Chiefly we should advise the deletion of the experiments and experimental results dealing with severe lesions. The chapter on the nervous system is one that no sensitive student could read without shuddering, and a recapitulation of the revolting experiments made by certain writers was wholly unnecessary in such a work as this. It is with regret that

we notice this serious drawback.

The description of the tadpole, and, indeed, of the life-history generally, while fairly careful in cellular detail, is lacking in any broad suggestiveness that

will remain after the anatomical detail has faded from the mind. The mode of hatching, the meaning of food-yolk, the fish-like character of the larva are not touched upon, nor is there given in this or any other

OUR BOOK SHELF.

Morphologie und Biologie der Algen. By Dr. Friedrich Oltmanns. Zweiter Band, Allgemeiner Theil. Pp. vi+443. (Jena: Gustav Fischer, 1905.) Price

12 marks.

IT is difficult to say of this much-wished-for and longexpected fruit of Dr. Oltmanns's industry more than that it meets all these wishes and hopes. There is one respect in which a fault may be found, the last to be thought of, viz. the arrangement, but it is cured by the provision of an excellent index. Detailed criticism of a work of this size in the pages of NATURE is out of the question, and the present writer confesses that he has attempted such a task several times, but always with the result that his effort not only left no satisfaction to himself, but kept a fear before him that his judgment might easily be misunderstood.

In a word, the book is invaluable to all workers at this subject, and well worthy of the great reputation of Dr. Oltmanns as a researcher and teacher. If any faults were to be found in a detailed criticism they would be, not with Dr. Oltmanns, but with the fate that has prevented his access to our great collections. This short notice of so great a work must not, from its brevity, seem to lack in the heartiness the reviewer wishes to express in his welcome to it. The volume has been long needed by those who are earnestly at work, and no one values it more than the writer of this brief note of thanks for it, and for the industry of the author of it.

GEORGE MURRAY.

Atlas colorié de la Flore alpine. By J. Beauverie and
L. Faucheron. Pp. 98. (Paris: J. B. Baillière and
Son, 1906.) Price 7.50 francs.

THE recollections of botanising expeditions in the
High Alps must ever remain a source of pleasure to
those who have had such enjoyable experiences. Not
only the botanist, but anyone endowed with a spark
of latent appreciation for the beauties of nature can-
not fail to be aroused to enthusiasm when for the first
time he has the good fortune to behold patches of
Anemone vernalis in the spring, or to discover clumps
of Ranunculus glacialis on the snow-line. It is
natural, therefore, that there should be a demand for
floras of the Alpine regions adapted to amateurs, and
nature of this volume, which contains excellent illus-
also worthy of professed botanists. Such is the
trations combined with simple descriptions of the
flowers and references to localities where they may
be found. To confine the book to reasonable com-
pass, only fairly common Alpine plants are included,
and preference is given to the denizens of the higher
Alps. So far as the selection is concerned, there is
little to note except that the orchids have received
rather scant measure, and the thistles are entirely
omitted. Some of the plants,
plants, e.g. Douglasia
vitaliana and Androsace villosa, are interesting for
their association with the French Alps, while, on the
other hand, several species are included that are
absent from French territory. The compilation re-
flects credit on the authors for their clear and pithy
descriptions, and on the publishers for the manner
in which the plates are produced.

« PreviousContinue »