■ I I - - /$yS$$P ■c*.-::>;* /:'-- : v- 1 / / K A ON THE ORIGIN OF SPECIES: OK, THE CAUSES OF THE PHENOMENA OF ORGANIC NATURE. % tipvm 4 $\* Statures to ftatorluiuj Pm BY THOMAS H. HUXLEY, F.R.S., F.L.S., rnoFESson of natural history in the jerjjyn street school of mines. NEW YORK: D. APPLETON AND COMPANY 443 & 445 BROADWAY. 1863. 6&W Sw s *£\fe r QDA4f Sr V fc/| LIBRARY I>- PREFACE TO THE AMERICAN EDITIOK The publication of Mr. Darwin's work on the u Origin of Species," whether we consider the import- ance of the questions it raises, the ability w T ith which he treats them, the boldness and originality of his speculations, or the profound and universal interest which the book awakened, must be looked upon as marking an era in the progress of science. But while it called forth a due share of candid discussion and intelligent criticism, it has been vehemently and per- sistently assailed by many who understood nothing of its real character ; and the subject has hence been so overloaded with prejudice and perversion that unscien- tific people hardly know what to think or believe about it. In these circumstances, those who disencumber the subject of its difficulties, simplify its statements, relieve it of technicalities, and bring it so distinctly within the horizon of ordinary apprehension that persons of com- mon sense may judge for themselves, perform an in- 4 PREFACE TO THE AMERICAN EDITION. valuable service. Such is the character of the present volume. Prefixed to the English edition, is the following note from Professor Huxley : " Mr. J. Aldous Mays, who is taking shorthand notes of my ' Lectures to Working Men,' has asked me to allow him, on his own account, to print those notes for the use of my audience. I willingly accede to this request, on the understanding that a notice is prefixed to the effect that I have no leisure to revise the Lectures, or to make alterations in them, beyond the correction of any important error in a matter of fact." The reader will not regret that the Lectures appear in this form. Taken from the lips of the distinguished naturalist, as he addressed an audience of ' Working Men,' they have a clearness, a directness, and a sim- plicity which belonged to the circumstances of their delivery. In this respect, the following Lectures are incomparable. Dealing w T ith the most abstruse and fundamental questions of mind and organization, these subjects are nevertheless presented in so lucid and at- tractive a manner as to impress vividly the commonest imagination. The gift of translating the high questions of science into popular forms of expression, without sacrificing ac- curacy and introducing error, is a very rare one among scientific men, but Professor Huxley possesses it in an eminent degree : his lectures are models of their class. CONTENTS. — • — NO. PAGE I. The Present Condition of Organic Nature ... 7 II. The Past Condition of Organic Nature . . . .29 III. The Method by which the Causes of the Present and Past Conditions of Organic Nature are to be Discov- ered. — The Origination of Living Beings . . .52 IT. The Perpetuation of Living Beings, Hereditary Trans- mission and Variation 80 V. The Conditions of Existence as affecting the Perpetua- tion of Living Beings 102 VI. A Critical Examination of the Position of Mr. Darwin's "Work, " On the Origin of Species," in relation to the complete Theory of the Causes of the Phenomena of Organic Nature 127 LECTUKE I. THE PPwESENT CONDITION OF ORGANIC NATURE. "When it was my duty to consider what subject I would select for the six lectures which I shall now have the pleasure of delivering to you, it occurred to me that I could not do better than endeavour to put before you in a true light, or in what I might perhaps with more modesty call, that which I conceive myself to be the true light, the position of a book which has been more praised and more abused, perhaps, than any book which has appeared for some years ; — I mean Mr. Darwin's work on the " Origin of Species." That work, I doubt not, many of you have read ; for I know the inquiring spirit which is rife among you. At any rate, all of you will have heard of it, — some by one kind of report and some by another kind of report ; the attention of all and the curiosity of all have been prob- ably more or less excited on the subject of that work. All I can do, and all I shall attempt to do, is to put before you that kind of judgment which has been formed by a man, who, of course, is liable to judge erroneously ; but at any rate, of one whose business and profession it is to form judgments upon questions of this nature. 8 THE PRESENT CONDITION And here, as it will always happen when dealing with an extensive subject, the greater part of my course — if, indeed, so small a number of lectures can be prop- erly called a course — must be devoted to preliminary matters, or rather to a statement of those facts and of those principles which the work itself dwells upon, and brings more or less directly before us. I have no right to suppose that all or any of you are naturalists ; and even if you were, the misconceptions and misunder- standings prevalent even among naturalists on these matters would make it desirable that I should take the course I now propose to take, — that I should start from the beginning, — that I should endeavour to point out what is the existing state of the organic world — that I should point out its past condition — that I should state what is the precise nature of the undertaking which Mr. Darwin has taken in hand ; that I should endeavour to show you what are the only methods by which that undertaking can be brought to an issue, and to point out to you how far the author of the work in question has satisfied those conditions, how far he has not satisfied them, how far they are satisfiable by man, and how far they are not satisfiable by man. And for to-night, in taking up the first part of this question, I shall endeavour to put before, you a sort of broad notion of our knowledge of the condition of the living world. There are many ways of doing this. I might deal with it pictorially and graphically. Following the example of Humboldt in his " Aspects of Nature," I might endeavour to point out the infinite variety of organic life in every mode of its existence, with refer- ence to the variations of climate and the like ; and such an attempt would be fraught with interest to us all ; OF ORGANIC NATURE. V but considering the subject before us, such a course would not be that best calculated to assist us. In an argument of this kind we must go further and dig deeper into the matter; we must endeavour to look into the foundations of living Nature, if I may so say, and discover the principles involved in some of her most secret operations. I propose, therefore, in the first place, to take some ordinary animal with which you are all familiar, and, by easily comprehensible and. obvious examples drawn from it, to show what are the kind of problems which living beings in general lay before us ; and I shall then show vou that the same problems are laid open to us by all kinds of living beings. But, first, let me say in what sense I have used the words " organic nature." In speaking of the causes which lead to our present knowledge of organic nature, I have used it almost as an equivalent of the word " living," and for this reason, — that in almost all living beings you can distinguish several distinct por- tions set apart to do particular things and work in a particular way. These are termed " organs," and the whole together is called " organic." And as it is universally characteristic of them, this term " organic " has been very conveniently employed to denote the whole of living nature, — the whole of the plant world, and the whole of the animal world. Few animals can be more familiar to you than that whose skeleton is shown on this diagram. You need not bother yourselves with this " Equus caballus " written under it ; that is only the Latin name of it, and does not make it any better. It simply means the common Horse. Suppose we wish to understand all about the Horse. Our first object must be to study 1* 10 THE PRESENT CONDITION the structure of the animal. The whole of his body is inclosed within a hide, a skiu covered with hair ; and if that hide or skin be taken off, we find a great mass of flesh, or what is technically called muscle, being the substance which by its power of contraction enables the animal to move. These muscles move«the hard parts one upon the other, and so give that strength and power of motion which renders the Horse so useful to us in the performance of those services in which we employ him. And then, on separating and removing the whole of this skin and flesh, you have a great series of bones, hard structures, bound together with ligaments, and forming the skeleton which is represented here. In that skeleton there are a number of parts to be recognized. This long series of bones, beginning from the skull and ending in the tail, is called the spine, and these in front are the ribs ; and then there are two pairs limbs, one before and one behind ; and these are what we all know as the fore-legs and the hind-legs. If we pursue our researches into the interior of this animal, we find within the framework of the skeleton a great cavity, or rather, I should say, two great cavities — one cavity beginning in the skull and running through the neck-bones, along the spine, and ending in the tail, containing the brain and the spinal marrow, which are extremely important organs. The second great cavity, commencing with the mouth, contains the gullet, the stomach, the long intestine, and all the rest of those internal apparatus which are essential for digestion ; and then in the same great cavity, there are lodged the heart and all the great vessels going from it ; and, be- sides that, the organs of respiration — the lungs ; and OF ORGANIC NATURE. 11 then the kidneys, and the organs of reproduction, and so on. Let us now endeavor to reduce this notion of a horse that we now have, to some such kind of simple expression as can be at once, and without difficulty, re- tained in the mind, apart from all minor details. If I make a transverse section, that is, if I were to saw a dead horse across, I should find that, if I left out the details, and supposing I took my section through the anterior region, and through the fore-limbs, I should have here this kind of section of the body (Fig. 1). Here would be the upper part of the animal — that great mass of bones that we spoke of as the spine (a, Fig. 1). Here I should have the alimentary canal (5, Fig. 1). Here I should have the heart ( the shore, x y the sea-level, then the coarser deposit will subside over the region B, the finer over A, while beyond A there will be no deposit at all ; and, consequently, no record will be kept, simply because no deposit is going on. Now, suppose that the whole land, C, D, which 36 THE PAST CONDITION we have regarded as stationary, goes down, as it does so, both A and B go further out from the shore, which Fig. 4. will be at y\ x 1 y\ being the new sea-level. The con- sequence will be that the layer of mud (A), being now, for the most part, further than the force of the current is strong enough to convey even the finest debris, will, of course, receive no more deposits, and having attained a certain thickness will now grow no thicker. We should be misled in taking the thickness of that layer, whenever it may be exposed to our view, as a record of time in the manner in which we are now regarding this subject, as it would give ns only an imperfect and partial record it would seem to repre- sent too short a period of time. Suppose, on the other hand, that the land (C D) had gone on rising slowly and gradually — say an inch or two inches in the conrse of a century, — what would be the practical effect of that movement ? Why, that the sediment A and B which has been already depos- ited, would eventually be brought nearer to the shore- level, and again subjected to the wear and tear of the sea ; and directly the sea begins to act upon it, it would of course soon cut up and carry it away, to a greater or less extent, to be re-deposited further out. OF ORGANIC NATURE. 37 "Well, as there is, in all probability, not one single spot on the whole surface of the earth, which has not been up and down in this way a great many times, it follows that the thickness of the deposits formed at any particular spot cannot be taken (even supposing we had at first obtained correct data as to the rate at which they took place), as affording reliable informa- tion as to the period of time occupied in its deposit. So that you see it is absolutely necessary from these facts, seeing that our record entirely consists of accumu- lations of mud, superimposed one on the other ; seeing in the next place that any particular spots on which accumulations have occurred, have been constantly moving up and down, and sometimes out of the reach of a deposit, and at other times its own deposit broken up and carried away, it follows that our record must be in the highest degree imperfect, and we have hardly a trace left of thick deposits, or any definite knowledge of the area that they occupied in a great many cases. And mark this! That supposing even that the whole surface of the earth had been accessible to the geolo- gist, — that man had had access to every part of the earth, and had made sections of the whole, and put them all together, — even then his record must of neces- sity be imperfect. But to how much has man really access ? If you will look at this Map you will see that it represents the proportion of the sea to the earth : this coloured part indicates all the dry land, and this other portion is the water. You will notice at once that the water covers three-fifths of the whole surface of the globe, and has covered it in the same manner ever since man has kept any record of his own observations, to say 38 THE PAST CONDITION nothing of the minute period during which he has cul- tivated geological inquiry. So that three-fifths of the surface of the earth is shut out from us because it is under the sea. Let us look at the other two-fifths, and see what are the countries in which anything that may be termed searching geological inquiry has been carried out : a good deal of France, Germany, and Great Brit- ain and Ireland, bits of Spain, of Italy, and of Russia, have been examined, but of the whole great mass of Africa, except parts of the southern extremity, we know next to nothing ; little bits of India, but of the greater part of the Asiatic continent nothing ; bits of the Northern American States and of Canada, but of the greater part of the continent of North America, and in still larger proportion, of South America, nothing ! Under these circumstances, it follows that even with reference to that kind of imperfect information which we can possess, it is only about the ten thousandth part of the accessible parts of the earth that has been exam- ined properly. Therefore, it is with justice that the most thoughtful of those who are concerned in these inquiries insist continually upon the imperfection of the geological record ; for, I repeat, it is absolutely necessary, from the nature of things, that that record should be of the most fragmentary and imperfect char- acter. Unfortunately this circumstance has been con- stantly forgotten. Men of science, like young colts in a fresh pasture, are apt to be exhilarated on being turned into a new field of inquiry, and to go off at a hand-gallop, in total disregard of heriges and ditches, losing sight of the real limitation of their inquiries, and to forget the extreme imperfection of what is really known. Geologists have imagined that they could tell OF ORGANIC NATURE. 39 us what was going on at all parts of the earth's surface during a given epoch ; they have talked of this deposit being contemporaneous with that deposit, until, from our jfittle local histories of the changes at limited spots of the earth's surface, they have constructed a universal history of the globe as full of wonders and portents as any other story of antiquity. But what does this attempt to construct a universal history of the globe imply ? It implies that we shall not only have a precise knowledge of the events which have occurred at any particular point, but that we shall be able to say what events, at any one spot, took place at the same time with those at other spots. Let us see how far that is in the nature of things practicable. Suppose that here I make a section of the Lake of Killarney, and here the section of another lake — that of Loch Lomond in Scotland for instance. The rivers that flow into them are constantly carrying down deposits of mud, and beds, or strata, are being as constantly formed, one above the other, at the bottom of those lakes. Now, there is not a shadow of doubt that in these two lakes the upper beds are all older than the lower — there is no doubt about that ; but what does this tell us about the age of any given bed in Loch Lomond, as compared with that of any given bed in the Lake of Killarney? It is, indeed, obvious that if any two sets of deposits are separated and discontinu- ous, there is absolutely no means whatever given you by the nature of the deposit of saying whether one is much younger or older than the other ; but you may say, as many have said and think, that the case is very much altered if the beds which we are comparing are 40 THE PAST CONDITION continuous. Suppose two beds of mud hardened into rock, — A and B are seen in section. (Fig. 5.) Well, you say, it is admitted that the lowermost bed is always the older. Very well ; B, therefore, is older than A. No doubt, as a tchole, it is so ; or if Fig. 5. any parts of the two beds which are in the same verti- cal line are compared, it is so. But suppose you take what seems a very natural step further, and say that the part a of the bed A is younger than the part b of the bed B. Is this sound reasoning ? If you find any record of changes taking place at b, did they occur be- fore any events which took place while a was being deposited ? It looks all very plain sailing, indeed, to say that they did ; and yet there is no proof of any- thing of the kind. As the former Director of this In- stitution, Sir II. De la Beche, long ago showed, this reasoning may involve an entire fallacy. It is extremely possible that a may have been deposited ages before b. It is very easy to understand how that can be. To return to Fig. 4 ; when A and B were deposited, they w T ere substantially contemporaneous; A being simply the finer deposit, and B the coarser of the same detritus or waste of land. Now suppose that the sea-bottom goes down (as shown in Fig. 4), so that the first deposit O'v ORGANIC NATURE. 41 is carried no farther than ogi«(!6 of the nation. It is a step towards the simplification of English History. By th« term Revolutions, the author intends to denote the great phases of change, through which both the government and people of England have passed, during the historical period of their existence. "A work of this kind," says Blackwood's Magazine, "cannot be superfluous, if it is worthily executed ; and the honorable position which Dr. Vaughan has earned for himself in both theology and literature, gives us a guarantee that this will be the case. The specimen before us we have read with interest and improvement. We should particularize the ecclesiastical portion of the history as being executed with special care, and as remarkable for the spirit of justice and liberality he displays. T& these pages we may honestly recommend the reader, as the fruit of steady and con- scientious labor, directed by a liberal and enlightened spirit" "This treatise," 6ays the London Athenaium, "or rather narrative, is deeply and variously interesting. Written plainly, but with all the characteristics of independent thought and accomplished scholarship, it may be pronounced a masterly survey of English civilization from the remotest epoch to the commencement of the fifteenth century. We have found this volume in every way excellent. It is at once a narra- tive and a disquisition, learned, genial, critical, and also picturesque. The spirit of English history animates it throughout. Dr. Vaughan, by completing such a work will have done good service to literature." 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