•MB EARTH SCIENCES LIBRARY c. GIFT OF L. Camp KARTH ENCES THE PRIMARY FACTORS ORGANIC EVOLUTION E. D. COPE, PH. D. MEMBER OF THE U. S. NATIONAL ACADEMY OF SCIENCES; PROFESSOR OF ZOOLOGY AND COMPARATIVE ANATOMY IN THE UNIVERSITY OF PENNSYLVANIA CHICAGO THE OPEN COURT PUBLISHING COMPANY (LONDON: 17 JOHNSON'S COURT, FLEET ST., E. C.) 1904 EARTH S91ENCE3 LIBRARY COPYRIGHT BY THE OPEN COURT PUBLISHING Co. CHICAGO, ILL., 1896. -Osx^JO -»e ^w, R. R. DONNELLEY & SONS CO., CHICAGO. PREFACE. THE present book is an attempt to select from the mass of facts accumulated by biologists, those which, in the author's opinion, throw a clear light on the problem of organic evolution, and especially that of the animal kingdom. As the actual lines of descent can be finally demonstrated chiefly from paleontologic re- search, I have drawn a large part of my evidence from this source. Of course, the restriction imposed by limited space has compelled the omission of a great many facts which have an important bear- ing on the problem. I have preferred the paleontologic evidence for another reason. Darwin and the writers of his immediate school have drawn most of their evidence from facts which are embraced in the science of cecology. Weismann and writers of his type draw most of their evidence from the facts of embryology. The mass of facts recently brought to light in the field of paleon- tology, especially in the United States, remained to be presented, and the evidence they contain interwoven with that derived from the sources mentioned. Many of the zoologists of this country, in common with many of those of other nations, have found reason for believing that the factors of evolution which were first clearly formulated by La- marck, are really such. This view is taken in the following pages, and the book may be regarded as containing a plea on their behalf. In other words, the argument is constructive and not destructive. The attempt is made to show what we know, rather than what we do not know. This is proper at this time, since, in my opinion, a certain amount of evidence has accumulated to demonstrate the doctrine here defended, and which I have defended as a working hypothesis for twenty-five years. In the following pages I have cited many authors who have contributed to the result, but it has been impossible to cite all who M 2716 vi PRIMARY FACTORS OF ORGANIC EVOLUTION-. have written on one part or another of the subject. If some very meritorious essays have not been cited, it has been generally be- cause I have confined myself to those in which facts or doctrines were first presented, and have not had so much occasion to refer to those of later date. Mr. Romanes, in his posthumous book, Volume II. of his Dar- win, and After Darwin on Post- Darwinian Questions, expresses the following opinion of the position which has been taken by the Neo-Lamarckians of this country. He says that they do not dis- tinguish between the "statement of facts in terms of a proposition, and an explanation of them in terms of causality." Had Mr. Ro- manes been acquainted with the literature of the subject published in America and elsewhere during the last three years, he would have had reason to change this view of the case. I think he would have found in it demonstration "in terms of causality." At the outset it must be stated that a knowledge of the history of organic evolution rests primarily on the science of morphology, and secondarily on the kinematics of the growth of organic struc- tures. The phenomenon to be explained is the genealogical suc- cession, or phylogeny of organisms ; and the access to this subject is through the sciences of paleontology and embryology. The phe- nomena of the functioning of the organism, or physiology, are only incidentally referred to, as not the real object of inquiry. Since organic species are much more numerous than the tissues of which they are composed, organogenesis must claim attention more largely than histogenesis. It is true that histogenesis is fundamental, but it is a science as yet in its early infancy, and little space can be given to it. The exact how of organic evolution will never be finally solved, however, until our knowledge of histogenesis is com- plete. The research depicted in the following pages has proceeded on the assumption that every variation in the characteristics of organic beings, however slight, has a direct efficient cause. This assump- tion is sustained by all rational and philosophical considerations. Any theory of evolution which omits the explanation of the causes of variations is faulty at the basis. Hence the theory of selection cannot answer the question which we seek to solve, although it embraces an important factor in the production of the general re- sult of evolution. In the search for the factors of evolution, we must have first a knowledge of the course of evolution. This can only be obtained PREFACE. vii in a final and positive form by investigation of the succession of life. The record of this succession is contained in the sedimentary deposits of the earth's crust, and is necessarily imperfect. Advance in knowledge in this direction has, however, been very great of re- cent years, so that some parts of the genealogical tree are tolerably or quite complete. We hope reasonably for continued progress in this direction, and if the future is to be judged of by the past, the number of gaps in our knowledge will be greatly lessened. In the absence of the paleontologic record, we necessarily rely on the em- bryologic, which contains a recapitulation of it. The imperfections of the embryonic record are, however, great, and this record differs from the paleontologic in that no future discovery in embryology can correct its irregularities. On the contrary every paleontologic discovery is an addition to positive genealogy, if the present work has any merit, it is derived from the fact that the basis of the argu- ment is the paleontologic record. E. D. COPE. PHILADELPHIA, November i, 1895. CONTENTS. PAGE PREFACE v TABLE OF CONTENTS ix LIST OF ILLUSTRATIONS xiii INTRODUCTION . i PART I. THE NATURE OF VARIATION. PRELIMINARY 19 CHAPTER I. VARIATION. Preliminary 21 1. Variations of Specific Characters 25 a. Variations in Cicindela 25 b. Variations in Osceola doliata 29 c. Color- Variations in Cnemidophorus 41 d. Variations in North American Birds and Mam- mals in Relation to Locality 45 2. Variation of Structural Characters 58 3. Successional Relation 62 CHAPTER II. PHYLOGENY. 1. General Phylogeny 74 2. Phylogeny of the Vertebrata 83 a. Phylogeny of the Classes 83 b. The Line of the Pisces 99 c. The Line of the Batrachia ....'... 108 d. The Line of the Reptilia 113 e. The Line of the Aves 123 /. The Line of the Mammalia 126 g. Review of the Phylogeny of the Mammalia . 138 x PRIMARY FACTORS OF ORGANIC EVOLUTION. PAGE h. Phylogeny of the Horse 146 i. The Phylogeny of Man 150 3. The Law of the Unspecialized 172 CHAPTER III. PARALLELISM. Preliminary 175 1. Parallelism in the Brachiopoda 176 2. Parallelism in the Cephalopoda 182 3. Parallelism in the Vertebrata 192 4. Inexact Parallelism or Caenogeny 200 5. Objections to the Doctrine of Parallelism 205 CHAPTER IV. CATAGENESIS. . 211 PART II. THE CAUSES OF VARIATION. PRELIMINARY 225 CHAPTER V. PHYSIOGENESIS. Preliminary 227 a. Relation of Size of Mollusca to Environment . . 229 b. The Conversion of Artemia into Branchinecta . 229 c. Production of Colors in Lepidopterous Pupae . . 230 d. Effect of Light on the Colors of Flatfishes . . .238 e. Effect of Feeding on Color in Birds 238 f. Blindness in Cave Animals 241 CHAPTER VI. KINETOGENESIS. Preliminary 246 1. Kinetogenesis of Muscular Structure 249 2. Kinetogenesis in Mollusca 255 a. Origin of the Plaits in the Columella of the Gas- teropoda 255 b. Mechanical Origin of Characters in the Lamelli- branchiata 261 c. Mechanical Origin of the Impressed Zone in Cephalopoda 268 3. Kinetogenesis in Vermes and Arthropoda 268 4. Kinetogenesis in Vertebrata 275 i. Kinetogenesis of Osseous Tissue 275 a. Abnormal Articulations 275 CONTENTS. b. Normal Articulations 283 c. The Physiology of Bone Moulding 285 ii. Moulding of the Articulations 287 a. The Limb Articulations 287 b. The Forms of Vertebral Centra 302 iii. Increase of Size Through Use 304 a. The Proportions of the Limbs and their Segments 305 b. The Number of the Digits 309 c. The Horns 314 iv. Mechanical Origin of Dental Types 318 Preliminary 318 a. The Origin of Canine Teeth . 327 b. The Development of the Incisors 328 c. The Development of Molars 331 d. Origin of the Carnivorous Dentition .... 332 e. Origin of the Dental Type of the Glires .... 345 v. Disuse in Mammalia 352 a. Natatory Limbs 352 b. Abortion of Phalanges in Ungulata 353 c. Atrophy of Ulna and Fibula 355 d. Atrophy of Incisor Teeth 356 vi. Homoplassy in Mammalia 357 vii. Origin of the Divisions of Vertebrata 362 5. Objections to Kinetogenesis 375 CHAPTER VII. NATURAL SELECTION ..." 385 PART III. THE INHERITANCE OF VARIATION. PRELIMINARY 397 CHAPTER VIII. HEREDITY. 1. The Question Stated 398 2. Evidence from Embryology 401 a. Vertebrata 401 b. Arthropoda 404 3. Evidence from Paleontology 405 a. The Impressed Zone of the Nautiloids .... 405 4. Evidence from Breeding 422 a. Of Characters Due to Nutrition 423 b. Of Characters Due to Exercise of Function . . 426 c. Of Characters Due to Disease 430 xii PRIMARY FACTORS OF ORGANIC EVOLUTION. d. Of Characters Due to Mutilation and Injuries . 431 e. Of Characters Due to Regional Influences . . .435 5. The Conditions of Inheritance 438 6. Objections to the Doctrine of Inheritance of Acquired Characters 458 CHAPTER IX. THE ENERGY OF EVOLUTION. Preliminary 473 1. Anagenesis > 475 2. Bathmogenesis 484 CHAPTER X. THE FUNCTION OF CONSCIOUSNESS. 1. Consciousness and Automatism 495 2. The Effects of Consciousness 509 CHAPTER XI. THE OPINIONS OF NEO-LAMARCKIANS . . 518 LIST OF ILLUSTRATIONS. Fig. i. Horn on Cicindela 27 2. Osceola doliata triangula 32 3. Osceola doliata clerica 32 4. Osceola doliata collaris 34 5. Osceola doliata temporalis 34 6-7. Osceola doliata doliata 36 8. Osceola doliata syspila 38 9. Osceola doliata parallela 38 10. Osceola doliata annulata 40 11. Osceola doliata coccinea 40 12. Cnemidophorus tessellatus 42 13. Cnemidophorus gularis 43 14. Lacerta muralis 44 15. Shoulder-girdle of Phyllomedusa bicolor 64 16. Do. of Rana temporaria, tadpole with budding limbs. 64 17. Do., adult 64 18. Bufonidae 66 19. Scaphiopidae and Pelobatidae 66 20. Hylidas 67 21. Cystignathidae 67 22. Ranidae 67 23. Feet of Unia scoparia Cope, and Ptenopus garrulus Smith 72 24. Eusthenopterum foordii Whiteaves 90 25. Paired fins of Cladoselache Dean 92 26. Extremities of skeletons of caudal fins of fishes . . 96 27. Cricotus crassidiscus Cope, head and belly . . . . in 28. Cricotus crassidiscus Cope, vertebral column and pelvis 112 xiv PRIMARY FACTORS OF ORGANIC EVOLUTION. PAGE Fig. 29. Crania of Stegocephalia and Cotylosauria . . . .117 30. Diagrams of crania of Reptilia 118 31. Do 119 32. Archceopteryx lithographica Wagn 125 33. Ungulata, anterior feet 129 34. Ungulata, posterior feet 130 35. Ungulata, anterior and posterior feet 131 36. Phenacodus vortmanii Cope 134 37. Fore and hind limbs of Phenacodus primavi.s and Homo sapiens 137 38. Skull of Anaptomorphus homunculus Cope. Lower jaw of Anaptomorphus cemulus Cope 151 39. Tomitherium rostratum Cope, mandible 156 40. Tomitherium rostratum Cope, fore arm 157 41. Tomitherium rostratum Cope, ilium and femur . .158 42. Megaladapis madagascariensis Forsyth Major . . . 160 43. Skull of the man of Spy 161 44. Outlines of calvaria of the Neanderthal man, of the Spy men. . . . 162 45. Vertical sections of symphysis mandibuli of gorilla ; of orang ; of chimpanzee ; of Spy men .... 164 46. Sections of symphysis mandibuli of modern Liegois and of an ancient Parisian 166 47. Molar teeth of man .... 167 48. Parallelism in Brachiopoda .... . . . . 181 49. Circulatory systems 194 50. Succession of horns of Cervits elaphus L 197 51. Shoulder-girdles of Anura 198 52. Lernaa branchialis 212 53. Entoconcha mirabilis Mull 214 54. Mycetozoa 220 55- Typhlogobius californiensis Steind 245 56. Fusus parilis Con., displaying non-plicate columella. 257 57. Mitra lineolata Heilprin, showing the plications of the columella . - 259 58. Siphocyprcea problematica Heilprin, showing plica- tions of lips 260 59. Ostrea edulis, embryo 262 60. Mya arenaria 263 61. Modiola plicatula 264 LIST OF ILLUSTRATIONS. xv Fig. 62. Ostrea virginiana 264 63. Diagrammatic representation of the segments of the leech 270 64. Diagrammatic representation of the rings of a primi- tive crustacean 271 65. Diagrams of hand of Crangon and of Astacus . . . 274 66. Elbows of man and horse 280 67. Elbow of horse • . . 281 68. Periptychus rhabdodon Cope, showing foot .... 288 69. Hind foot of Poebrotherium labiatum Cope .... 290 70. Hind foot of three-toed horse 290 71. United first bones of two middle toes of deer-antelope 291 72. Wrist-joints at distal extremity of fore arm . . . 292 73. Elbow-joint of Crocuta maculata L 294 74. Elbow-joint of chimpanzee 295 75. Elbow -joint of Cervus elaphus 296 76. Cervus canadensis in motion 297 77. Cervus elaphus 298 78. Diagram of carpus of a Taxeopod, of a diplarthrous ungulate 299 79. Raccoon pacing 299 80. Rhinocerus unicornis carpus 300 81. Equus caballus fore foot 300 82. Gazella dorcas 301 83. Pes of Merychochcerus montanus and Bos taurus . . 307 84. Anterior feet of primitive Ungulata 308 85. Righ t posterior foot of Prothippus and Poebrotherium 310 86. Manus of Artiodactyla 312 87. Burrs on antlers of Cosoryx necatus Leidy .... 316 88. Diagram of excursion of lower jaw in mastication . 320 89. Cervus, molars 321 90. Cusps of superior premolars and molars 322 91. Two true molars of both jaws of a ruminant . . . 323 92. Sections of superior molar teeth 323 93. Chirox plicatus Cope, palate and molar teeth . . . 324 94. Meniscoessus conquistus Cope, last two superior mo- lars 325 95. Lemur collaris, dentition 326 96. Esthonyx burmeisterii Cope, dentition 328 xvi PRIMAR Y FA CTORS OF ORGANIC E VOL UT1ON. PAGE Fig. 97. Psittacotherium multifragum Cope, mandibular ra- mus 329 98. Diagrammatic representations of horizontal sections of tricuspidate molars of both jaws in mutual rela- tion 333 99. Deltatheriumfundaminis Cope, fragmentary skull . 336 100. Centetes ecaudatus, skull and molars 337 101. Inferior molar crowns representing transition from the simple to the quadritubercular 338 102. Stypholophus whitice Cope ; apposition of inferior and superior molars 339 103. Cynodictis geismarianus Cope ; skull 341 104. Aelurodon sizvus Leidy; coadaptation of crowns of superior and inferior molars in mastication . . . 342 105. Smilodon neogczus Lund ; skull 344 106. Sections of crowns of molars of Ungulata .... 345 107. Castorotdes ohioensis Foster ; skull 347 108. Castoro'ides ohioensis Foster ; skull from below . . 350 109. Ischyromys typus Leidy ; cranium and mandible . . 351 i jo. Balcena mysticetus ; fore limb 353 in. Feet of Amblypoda 354 112. Feet of Proterotheriidae 358 113. Dorsal vertebrae of merospondylous fishes .... 370 114. Vertebral column of Eryops megacephalus Cope . . 371 1 140 Sleeve of coat 371 115. Metatoceras cavatiformis Hyatt 406 116. Do 407 117. Temnochilus crassus 407 118. Metacoceras dubium Hyatt 408 119. Hyatt on Cephalopoda 410 120. Diagram explanatory of Diplogenesis 441 INTRODUCTION. THE doctrine of evolution may be defined as the teaching which holds that creation has been and is accomplished by the agency of the energies which are intrinsic in the evolving matter, and without the interference of agencies which are external to it. It holds this to be true of the combinations and forms of inorganic nature, and of those of organic nature as well. Whether the intrinsic energies which accom- plish evolution be forms of radiant or other energy only, acting inversely as the square of the distance, and without consciousness, or whether they be ener- gies whose direction is affected by the presence of con sciousness, the energy is a property of the physical basis of tridimensional matter, and is not outside of it, according to the doctrine we are about to consider. As a view of nature from an especial standpoint, evolution takes its place as a distinct science. The science of evolution is the science of creation, and is as such to be distinguished broadly from the sciences which consider the other operations of nature, or the functioning of nature, which are not processes of crea- tion, but processes of destruction. This contrast is especially obvious in organic evolution, where the two processes go on side by side, and are often closely in- 2 PRIMARY FACTORS OF ORGANIC EVOLUTION, termingled, as for instance in muscular action, where both destruction of proteids and growth of muscular tissue result from the same acts, or use. Physiology, or the science of functions, concerns itself chiefly with destruction, and hence physiologists are especially prone to be insensible to the phenomena and laws of progressive evolution. The building of the embryo, remains a sealed book to the physiologist unless he take into account the allied biological science of evo- lution, as resting on the facts of botany, zoology, and paleontology. In his reflections on the relations of mind to matter he is likely to see only the destructive functioning of tissue, and not the history of the build- ing of the same during the ages of geological time. J. B. P. A. Lamarck1 thus contrasts the theories of direct creation, and creation by evolution. The former asserts : "That nature or its author in creating animals has foreseen all possible kinds of circumstances in which they may have to live, and has given to each species a permanent organization as well as a prede- termined form, invariable in its parts ; that it forces each species to live in the place and the climate where one finds them, and to preserve there the habits which it has." He then states his own, or the evolutionary, opinion to be: "That nature in producing succes- sively all species of animals, commencing with the most imperfect or simple, and terminating its work with the most perfect, has gradually complicated their organization ; and these animals spreading themselves gradually into all habitable regions of the globe,— each species has been subjected to the influence of the circumstances in which it is ; and these have produced the habits which we observe, and the modifications of \Philosophie Zoologique, Paris, 1809, Vol. I., Chap. VII. INTRODUCTION. 3 its parts." On an earlier page of the same chapter, Lamarck thus formulates the laws of organic evolu- tion, to which his name has been attached. First law. " In every animal which has not passed the time of its development, the frequent and sustained employment of an organ gradually strengthens it, de- velops and enlarges it, and gives it power proportional to the duration of its use ; while the constant disuse of a like organ weakens it, insensibly deteriorates it, progressively reduces its functions, and finally causes it to disappear." Second law. "All that nature acquires or loses in individuals by the influence of circumstances to which the race has been exposed for a long time, and in con- sequence of the influence of the predominate employ- ment of such an organ, or of the influence of disuse of such part, she preserves by generation, in new indi- viduals which spring from it, providing the acquired changes be common to both sexes, or to those which have produced new individuals. " We have here a theory of the origin of characters ; viz., of the increased development or loss of parts as a result of use or disuse. We have also the theory that the peculiarities thus acquired are transmitted to the succeeding generation by inheritance. The next formal statement of the efficient cause of organic evolution was presented by Messrs. Charles Darwin and Alfred R. Wallace in I859.1 The cause assigned is natural selection, and Mr. Darwin thus states what is meant by this expression in his work The Origin of Species.'1 " If under changing conditions of life organic beings present individual differences 1 Proceedings of the Linnean Society of London. 2 Ed. 1872, p. 102. 4 PRIMARY FACTORS OF ORGANIC EVOLUTION. in almost any part of their structure, and this cannot be disputed ; if there be, owing to their geometrical rate of increase, a severe struggle for life at some age, season, or year, and this certainly cannot be disputed ; then considering the infinite complexity of the rela- tions of all organic beings to each other and to their conditions of life, causing an infinite diversity of struc- ture, constitution, and habits, to be advantageous to them, it would be a most extraordinary fact if no varia- tions had ever occurred useful to each being's own wel- fare, in the same manner as so many variations have occurred useful to man. But if variations useful to any organic being ever do occur, assuredly individuals thus characterized will have the best chance of being preserved in the struggle for life ; and from the strong principle of inheritance, these will tend to produce off- spring similarly characterized. This principle of pre- servation, or the survival of the fittest, I have called natural selection. It leads to the improvement of each creature in relation to its organic and inorganic condi- tions of life ; and consequently in most cases, to what must be regarded as an advance in organization. Nevertheless, low and simple forms will long endure if well fitted for their simple conditions of life." It is readily perceived that this statement makes no attempt to account for the origin of variations, but that it simply formulates, as observed by Mr. Darwin, the doctrine of survival of such variations as are most useful to their possessors. This fact is more distinctly pointed out in the same work (p. 63) where the author remarks: "Several writers have misapprehended or objected to the term natural selection. Some have even imagined that natural selection induces variabil- ity, whereas it implies only the preservation of such INTRO D UC TION. 5 variations as arise and are beneficial to the being under its conditions of life. No one objects to agriculturists speaking of the potent effects of man's selection, and in this case the individual differences given by nature, which man for some object selects, must of necessity first occur." It is evident then that Mr. Darwin did not attempt to account for the origin of variations, but that the service rendered by him and by Mr. Wallace to the doctrine of evolution consists in the demonstra- tion of the reality of natural selection. Darwin also assumes in the statement first quoted above, the in- heritance of acquired characters. In 1865 the Principles of Biology of Herbert Spen- cer appeared. In this work the attempt is made to set forth the laws of organic evolution, in a way which represents an advance beyond the positions of his predecessors. He adopts and harmonizes both the Lamarckian and Darwinian doctrines, and is at times more specific in his application of Lamarck's doctrine of the stimulus of the environment, and of use, than was Lamarck himself. Very often, however, Spencer contents himself with generalities ; or takes refuge in the "instability of the homogeneous," as an efficient cause. This phrase, however, like his other one, "the unknowable," is but a makeshift of temporary ignor- ance, and is neglected by Spencer himself, when he can see his way through it. He approaches the cause of the varied forms of leaves of plants in this language r1 "And it will also be remembered that these equalities and inequalities of development correspond with the equalities and inequalities in the incidence of forces." Language of similar significant but rather indefinite import is frequently used throughout this volume. 1 The Principles of Biology, by Herbert Spencer, Amer. Ed., 1873, II., p. 143. 6 PRIMARY FACTORS OF ORGANIC EVOLUTION. But in some cases Spencer is more specific. With reference to the inequality in the basal lobes of the erect leaves of Tilia and other plants, he says:1 "A considerable deviation from bilateral symmetry may be seen in a leaf which habitually so carries itself that the half on the one side of the midrib is more shaded than the other half. The drooping branches of the lime show us leaves so arranged and so modified. On examining their attitudes and their relations one to another, it will be found that each leaf is so inclined that the half of it next the shoot grows over the shoot and gets plenty of light ; while the other half so hangs down that it comes a good deal into the shade of the preceding leaf. The result is that having learned which fall into these positions, the species profits by a large development of the exposed halves ; and by survival of the fittest acting along with the direct effect of extra exposure, this modification becomes established." In his discussion of the origin of the characters of ani- mals, Spencer is also sometimes specific. Respecting the development of muscular insertions he remarks :2 "Anatomists easily discriminate between the bones of a strong man and those of a weak man by the greater development of those ridges and crests to which the muscles are attached ; and naturalists on comparing the remains of domesticated animals with those of wild animals of the same species, find kindred differ- ences. The first of these facts shows unmistakably the immediate effect of function on structure, and, by obvious alliance with it, the second may be held to do the same, both implying that the deposit of dense sub- stance capable of great resistance habitually takes I Op. cit., p. 143. ILoc. cit., p. 200. INTR OD UC TWN. 7 place at points where the tension is excessive." Quite as specific is his ascription of the forms of epithelial cells to definite causes, as follows:1 " Just the equal- ities and inequalities of dimensions among aggregated cells, are here caused by the equalities and inequalities among their mutual pressures in different directions ; so though less manifestly, the equalities and inequali- ties of dimensions among other aggregated cells, are caused by the equalities and inequalities of the osmatic, chemical, thermal, and other forces besides the me- chanical, to which their different positions subject them." In spite of this not infrequent definiteness, Mr. Spencer occasionally falls into the error of ascribing the origin of structures to natural selection, as in the case of the forms of flowers,2 and the armor-plates of paleozoic fishes.3 Spencer assumes the inheritance of acquired characters throughout. In 1866 Haeckel's Schopfungsgeschichte appeared. In this work the author presents a mass of evidence which sustains the doctrine of evolution, and he com- bines the views of Lamarck and Darwin into a general system. He says:4 "We should, on account of the grand proofs just enumerated, have to adopt Lamarck's theory of descent for the explanation of biological phe- nomena, even if we did not possess Darwin's theory of selection. The one is so completely and directly proved by the other, and established by mechanical causes, that there remains nothing to be desired. The laws of inheritance and adaptation are universally acknowl- 1 Op. cit., p. 260. 2 Op. cit., p. 153. 3<9/. cit., p. 288. *The History of Creation, Amer. Edition, II., p. 355. 8 PRIMARY FACTORS OF ORGANIC EVOLUTION. edged physiological facts, the former traceable to prop- agation, the latter to the nutrition of organisms." Apart from the statement that adaptation is traceable "to the nutrition of organisms," we find nothing in Haeckel's earlier writings which attempts the ex- planation of the origin of variations, beyond the gen- eral position assumed by Lamarck. The distinctive merit of Haeckel is his formulation of phylogeny. Much of this was speculative at the time he wrote, but so far as the Vertebrata are concerned, it has been largely confirmed by subsequent discovery. Up to this period, the form in which the doctrine of evolution had been presented, was general in its application ; that is, without exact reference to the structural definitions of natural taxonomic groups. No attempt was made to show the modes of the origin of any particular class, order, or genus, and only in the most general way in the case of a few species, by Mr. Darwin. Phylogeny was untried, except by Haeckel; and this distinguished author did not attempt to ac- count specifically for the origins of the divisions whose filiations he set forth. In the year in which Haeckel's work above cited appeared, Professor Hyatt of Boston and myself took the first step towards the formulization of a rational theory of the origin of variation, which should accord with specific examples of taxonomy. Quite indepen- dently, we selected the simple series presented by the characters of genera in their natural relations, Hyatt in the cephalopodous Mollusca, and I in the Batrachia Salientia. It is probable that Hyatt's l article was pub- lished shortly before mine. He says of the genera of Cephalopoda : "In other words, there is an increasing I Memoirs Boston Society Natural History, 1866, p. 193. INTR OD UC TION. 9 concentration of the adult characteristics in the young of higher species and a consequent displacement of other embryonic features which had themselves also previously belonged to the adult period of still lower forms." My own language is i1 "That the presence, rudimental condition, or absence of a given generic character can be accounted for on the hypothesis of a greater rapidity of development in the individuals of the species of the extreme type, such stimulus being more and more vigorous in the individuals of the types as we advance towards the same, or by a reversed im- pulse2 of development, where the extreme is charac- terized by absence or ' mutilation ' of characters." The phenomena of the aggregation of characters in pro- gressive evolution, and the loss of characters in retro- gressive evolution, were termed by me acceleration and retardation in an essay published in i86g.3 In these papers by Professor Hyatt and myself is found the first attempt to show by concrete examples of natural taxonomy, that the variations that result in evolution are not multifarious or promiscuous, but definite and direct, contrary to the method which seeks no origin for variations other than natural selection. In other words, these publications constitute the first essays in systematic evolution that appeared. By the discovery of the paleontologic succession of modifications of the articulations of the vertebrate, and especially mamma- lian skeleton, I first furnished an actual demonstration of the reality of the Lamarckian factor of use, or mo- 1 Transactions American Philosophical Society, 1866, p. 398; reprinted in The Origin of the Fittest, p. 92. 2 The expression " reversed " is unfortunate, diminished being the proper word to convey the meaning intended. 3 The Origin of Genera, Philadelphia, 1869. io PRIMARY FACTORS OF ORGANIC EVOLUTION. tion, as friction, impact, and strain, as an efficient cause of evolution.1 This demonstration led me to the necessary inference that when the agency directive of motion is consciousness, this also has been an impor- tant factor of evolution, in demonstration of the sup- position of Erasmus Darwin.2 Hyatt has demonstrated first on paleontologic evidence, the inheritance of a mechanically acquired character. Important contribu- tions to corresponding histories of the Mollusca have been made by Hyatt,3 Dall,4 Jackson,6 and Beecher.5 Many other contributions, into which the paleontologic evidence does not enter, have also been made by vari- ous authors in Europe and America. The authors quoted up to this point had all as sumed that the progress of evolution depends on the inheritance by the offspring of new characters acquired by the parent, and had believed that such is the fact in ordinary experience. In 1883, Weismann, in an essay on heredity, announced the opinion that charac- ters acquired by the body could not be transmitted to the reproductive cells, and could not therefore be in- herited. This doctrine rests on the relation of the germ-cells to those of the rest of the body, which is expressed in the following language of his predecessor Jaeger: "Through a great series of generations the l"The Origin of the Hard Parts of Mammalia," American Journal of Morphology, 1889, p. 137. 2 Origin of the Fittest, 1887, p. 357. 3"Phylogeny of an Acquired Characteristic," Proc. Amer. Philosophical Society, 1893, p. 349; "The Genesis of the Arietidae," Memoirs Mus. Compar. Zodlogy, Cambridge, Mass., 1889, XVI., No. 3. 4 Dall, W. H., "The Hinge of Pelecypods and Its Development, Amer. Jour. Sci. Arts, 1889, XXXVIII., p. 445. SJackson, R. T., " Phylogeny of the Pelecypoda, the Aviculidae, and Their Allies," Memoirs Boston Society Natural History, 1890, IV., p. 277. 6 American Journal Sci, Arts, 1893. INTRODUCTION. n germinal protoplasm retains its specific properties, dividing in every reproduction into an ontogenetic por- tion and a phylogenetic portion, which is reserved to form the reproductive material of the mature offspring. This reservation of the phylogenetic material I de- scribed as the continuity of the germ-protoplasm. . . . Encapsuled in the ontogenetic material the phyloge- netic protoplasm is sheltered from external influences, and retains its specific and embryonic characters." In other words, the reproductive cells are removed from the influence of those stimuli which affect and effect growth in the cells of the other parts of the body, so that no character acquired by the rest of the body can be inherited. The bearing of this theory on evolution is thus stated by Weismann : L "The origin of heredi- tary individual variations cannot indeed be found in the higher organisms, the metazoa and metaphyta, but is to be sought for in the lowest, the unicellular." "The formation of new species, which among the lower pro- tozoa could be achieved without amphigony (sexual union), could only be attained by means of this process in the metazoa and metaphyta. It was only in this way that hereditary individual differences could arise and persist. " In other words, variation in organic beings above the unicellular forms, has been and is, introduced only by sexual reproduction. The conclusions of Weismann were derived prin- cipally from embryologic research, and his disciples have been chiefly recruited from embryologists. These conclusions have been supported by extensive and ex- haustive investigations, which have added greatly to our knowledge of the subject. In order to account for 1 Essays, p. 296. For a complete account of Weismann's views, see The Germ-Plasm, 1893. 12 PRIMAR Y FA CTORS OF ORGANIC E VOL UTION. the appearance of characters in the embryonic succes- sion, through influences confined to the germ-plasma, Weismann invented a theory which requires the pres- ence of distinct molecular aggregates within it, which represent the potentialities or causes. To these he has given the names of ids, idants, determinants, etc. As Weismann's contribution to evolution has been con- fined to the department of heredity, I will consider it more particularly in the third part of this book, which is devoted to that subject. Weismann has, however, subsequently modified his views to a considerable extent. He has always admitted the doctrine of Lamarck to be applicable to the evolution of the types of unicellular organisms. His experiments on the effect of temperature on the production of changes of color in butterflies, showed that such changes were not only effected, but were sometimes inherited. This he endeavors to explain as follows. 1 ' 'Many climatic variations may be due wholly or in part, to the simultaneous variation of correspond- ing determinants in some parts of the soma and in the germ-plasm of the reproductive cells." This is an ad- mission of the doctrine which in 1890 I called Diplo- genesis,2 and which is adopted in the present work. It appears to have been first propounded by Galton in 1875. In the chapter on Heredity I hope to offer some reasons for believing that the suggestion of Galton embraces the true doctrine of heredity. From what has preceded, two distinct lines of thought explanatory of the fact of organic evolution may be discerned. In one of these the variations of organisms which constitute progressive and regressive 1 The Germ Plasm, Contemporary Science Series, 1893, p. 406. ^American Naturalist, Dec., 1889; published in 1890. INTRODUCTION. 13 evolution appear fortuitously, and those which are beneficial survive by natural selection, while those which are not so, disappear. Characters both benefi- cial and useless or harmless, which are acquired by the adult organism, are not transmitted to the young, so that no education in habit or structure acquired by the adult, has any influence in altering the course of evo- lution. This is the doctrine of Preformation. From this point of view the cause of the variations of organ- isms has yet to be discovered. The other point of view sees in variation the direct result of stimuli from within or without the organism ; and holds that evolution consists of the inheritance of such variations and the survival of the fit through nat- ural selection. This is the doctrine of Epigenesis. To this I would add that in so far as sensations or states of consciousness are present, they constitute a factor in the process, since they enable an organism to modify or change its stimuli. The position of each of these schools on each of the questions to which reference has been made, may be placed in opposition as follows : 1. Variations appear in defi- nite directions. 2. Variations are caused by the interaction of the organic being and its environment. 3. Acquired variations may be inherited. 4. Variations survive directly as they are adapted to changing environments. (Natural selec- tion.) i. Variations are promiscu- ous or multifarious. 2. Variations are "congeni- tal " or are caused by mingling of male and female germ-plas- mas. 3. Acquired variations cannot be inherited. 4. Variations survive directly as they are adapted to changing environments. (Natural selec- tion.) i4 PRIMARY FACTORS OF ORGANIC EVOLUTION. 5. Movements of the organ- ism are caused or directed by sensation and other conscious states. 6. Habitual movements are derived from conscious experi- ence. 7. The rational mind is de- veloped by experience, through memory and classification. 5. Movements of organism are not caused by sensation or conscious states, but are a sur- vival through natural selection from multifarious movements. 6. Habitual movements are produced by natural selection. 7. The rational mind is de- veloped by natural selection from multifarious mental activ- ities. It is not the object of the present book to present all the available evidence on both sides of each of the ques- tions above enumerated. I propose merely to submit certain facts, in support of the doctrines contained in the left-hand column of the above table. My aim will be to show in the first place, that variations of charac- ter are the effect of physical causes ; and second, that such variations are inherited. The facts adduced in support of these propositions will be necessarily prin- cipally drawn from my own studies in the anatomy, ontology, and paleontology of the Vertebrata. It will be my aim, moreover, to co-ordinate the facts of evo- lution with those of systematic biology, so that the re- sult may be as clearly presented as possible. The fail- ure to do this by the founders of evolutionary doctrine has given their work a lack of precision, which has been felt by systematic biologists. The detailed ap- plication of the principles of Lamarck and Darwin has been the work of their successors, and has necessarily thrown much new light on the principles themselves. In pursuing the object above stated, I shall be obliged INTR OD UCTION. 1 5 to consider briefly in the following pages, the validity of the general propositions on which the doctrine of evolution rests. Less space will be given, however, to those which are less relevant, than to those which are more relevant to the doctrine of neo-Lamarckism. PART I. THE NATURE OF VARIATION, PRELIMINARY. THE structural relations of organisms may be ex- pressed in the following canons : 1 1. Homology. — This means that organic beings are composed of corresponding parts ; that the variations of an original and fixed number of elements constitute their only differences. A part large in one animal may be small in another, or vice versa ; or complex in one and simple in another. The analysis of animals with skeletons, or Vertebrata, has yielded several hundred original elements, out of which the twenty-eight thou- sand included species are cpnstructed. The study of homologies is thus an extended one, and is far from complete at the present day. 2. Successional Relation. — This expresses the fact that species naturally arrange themselves into series in consequence of an order of excess and deficiency in some feature or features. Thus species with three toes naturally intervene between those with one and four toes. So with the number of chambers of the heart, of segments of the body, the skeleton, etc. There are greater series and lesser or included series, and mis- takes are easily made by taking the one for the other. 1 Origin of the Fittest, p. 6. The laws here stated are as expressive of the relations of plants as of animals. 20 PRIMA RY FAC TORS OF OR CAN 1C E VOL UTION. 3. Parallelism. — This states that all organisms in their embryonic and later growth pass through stages which recapitulate the successive permanent condi- tions of their ancestry. Hence those which traverse fewer stages resemble or are parallel with the young of those which traverse more numerous stages. This is the broad statement, and is qualified by the details. 4. Teleology. — This is the law of fitness of structures for their special uses, and it expresses broadly the general adaptations of an animal to its home and habits. The first and fourth of the laws above enumerated are taken for granted as generally accepted, and are not especially considered in the following pages. The second law, that of successional relation, is discussed and illustrated under the two heads of Variation and Phylogeny; the first expressing contemporary relations, and the second, successive relations in time. The third law, or that of parallelism, is considered in a chapter devoted to that subject. CHAPTER I— ON VARIATION. PRELIMINARY. «• , * «• • '- J * *•>"* A LL species are not equally variable. Some species jLJL vary little or not at all, even under domestication. Thus the varieties of the turkey (Meleagris gallopavd) and the guinea-fowl (Numida meleagris} are few, and are confined to albinistic or melanistic conditions. The barnyard fowl (Gallus j/.), on the other hand, varies enormously, as does also the pigeon (Columba livid). Among domesticated Mammalia the variations of cats (Felts domestica) are few as compared with those of dogs (Cam's sp.}. Variability is not peculiar to do- mesticated animals. A large proportion of animals and plants are, in a state of nature, variable, and some of these are much more so than others. The common garter-snake (Eut&niasirtalis} varies exceedingly, while the variations of the allied ribband snake (Eutania saurita) are minute or none. But little variation has been observed in the polar bear ([/rsus maritimus), while the common bear (17. arctos) presents many vari- eties. Similar conditions are found among fishes. Thus the larger species of pike, the muskallonge (Lucius nobi- lior), the pike (Z. estor), and the pickerel (L. vermicu- latus) are constant in their characters, whiIeTrie~small pickerel (L. vermiculatus) presents numerous varieties. 22 PRIMARY FACTORS OF ORGANIC EVOLUTION. Many of the varieties of the animals referred to in- habit the same territory, although some are restricted to particular regions. Of geographical varieties or races much is known. As a rule, all widely distributed species present them. Examples are the brown bear of the Northern Hemisphere ( Ursus arctos) ; the cobra di capello snake of the warmer parts of Asia {Naja tripu- dians}, and that of Africa {Naja haje}. In North Amer- ica the king-snake (Ophibolus getulus) and the milk- snake {Osceola -doliatd} are represented by distinct faces in different regions. On the other hand, the copperhead (Ancistrodon contortrix) and the Eastern rattlesnake (Crotalus horridus), which have a wide range, scarcely vary at all. The chub {Hybopsis bigut- tatus} is an example of a fish distributed everywhere east of the Rocky Mountains, which presents scarcely any variation. Variations are not promiscuous or multifarious, but are of certain definite kinds or in certain directions. Thus amid all their varieties, dogs never present black cross-bands on the back like those of the dog-opossum (Thylacinus cynocephalus} of Tasmania, nor do they present ocellated spots like those of the leopard, nor longitudinal stripes like those of certain squirrels. The same is true of the many varieties of cattle (Bos tau- rus), and of numerous other mammalia. Domestic fowls never vary to blue or green, colors which are common to many other birds ; nor are canaries known to produce blue or red natural sports. All variations are in the first place necessarily restricted by the ex- isting characters of the ancestor; but beyond this it is evident that other conditions determine the nature of the variation. It is not supposable, for instance, that the pale tints of animals which live in dry regions ON VARIATION. 23 originated by an accident or without a determining cause. The increased amount of dark pigment ob- served in animals which dwell in especially humid re- gions must have a corresponding cause, and it is nat- urally to be supposed, of a kind the opposite of that which produces the pale colors. I shall adduce some illustrations which show that color variations in species, as well as structural varia- tions in higher groups, have appeared in certain defi- nite series, and observe a successional relation to each other, which may or may not coincide with geograph- ical conditions. The same relation is observed in the order of appearance of variations on the body. Eimer and Weismann have shown that the grad- ual modification of color markings has originated in lizards and in caterpillars at the posterior end of the body and has gradually extended forwards. This has been discovered both by comparisons of the variations of the adults, and by studies of the order of their appear- ance in ontogenetic growth. Eimer shows that longi- tudinal bands have been produced in some animals by the confluence of spots placed in transverse series, which themselves are the remains of interrupted trans- verse bands. Thus he believes that the spots of the leopard group of the large cats were derived from the breaking up of transverse bands of the character of those now possessed by the tiger. The uniform colo- ration of the lion is the result of the obliteration of the spots. Traces of these spots may be distinctly seen in lions' cubs. In plants variation is said to be equally definite by Henslow. He says : "In 1847 Professor J. Buckman sowed the seed of the wild parsnip in the garden of the Agricultural College at Cirencester. The seeds 24 PRIMARY FACTORS OF ORGANIC EVOLUTION. began to vary, but in the same way, though in differ- ent degrees. By selecting seed from the best rooted plants the acquired ' somatic' characters of an en- larged root, glabrous leaves, etc. , became fixed and hereditary; and the ' Student,' as he called it, having been ' improved ' by Messrs. Sutton and Sons, is still regarded as ' the best in the trade. ' This is definite variation, according to Darwin's definition, for those weeded out did not differ from the selected, morpho- logically, except in degree, the variations towards im- provement not being quite fast enough to entitle them to survive.'* Finally I wish especially to point out that variation in animals, and probably in plants, (with which I am not so familiar,) gives no ground for believing that "sports "have any considerable influence on the course of evolution. This is apparent whether we view the serial lines of variations of specific, generic, or higher characters ; or whether we trace the phylogeny of the animal and vegetable types by means of the paleonto- logical record. The method of evolution has appar- ently been one of successional increment or decrement of parts along definite lines. More or less abruptness in some of the steps of this succession there may have been ; since a definite amount of energy expended in a given direction at a given point of history might pro- duce a much greater effect than the same amount ex- pended at some other period or point of evolution. This might be due to the release of stored energy, which could only be accomplished by a coincidence of circumstances. A simple illustration of the phenome- non of abrupt metamorphosis is to be found in the passage of matter from the gaseous to the liquid, and ON VARIATION. 25 from the liquid to the solid state. I have stated the case in the following language : 1 "As one or more periods in the life of every spe- cies is characterized by a greater rapidity of develop- ment " (ontogenetic) " than the remainder ; so in pro- portion to the approximation of such a period to the epoch of maturity or reproduction is the offspring liable to variation. During the periods corresponding to those between the rapid metamorphoses, the char- acters of the genus would be preserved unaltered, though the period of change would be ever approach- ing. Hence the transformation of genera may have been rapid and abrupt, and the intervening periods of persistency very long. Thus, while change is really progressing, the external features remain unchanged at other than those points, which may be called ex- pression points. Now the expression point of a new gen- eric type is reached when its appearance in the adult falls so far prior to the period of reproduction as to transmit it to the offspring and their descendants. " i. VARIATIONS OF SPECIFIC CHARACTERS. a. Variations in the Coleopterous Genus Cicindela. Dr. George H. Horn has traced the variations in the color patterns of the elytra of the North American species of this abundant and well-known genus. He shows that they form series, in the following language :2 "Any one in glancing over this series will perceive that there is a great similarity of marking between many species. This similarity, which may be con- sidered as the type of marking, and is illustrated by 1 Origin of the Fittest, p. 79. 2 Entomological New s, Philadelphia, Feb., 1892, p. 25. 26 PRIMARY FACTORS OF ORGANIC EVOLUTION. No. i of the accompanying plate (Fig. i) is the under- lying pattern from which all the forms observed in our Cicindela have been derived. "Before going further it is well to present the fol- lowing propositions that the argument and the illus- trations may be understood. "i. The type of marking is the same in all our spe- cies. "2. Assuming a well-marked species as a central type the markings vary, a, by a progressive spreading of the white, b, by a gradual thinning t>r absorption of the white, *. Color- Variations in Cnemidophorus. Another illustration of the nature of color-variation is to be found in certain species of the lacertilian gen- era Cnemidophorus in America, and Lacerta in Eu- rope. In both genera the color-markings differ in the same individual at different ages, and the age at which the adult coloration is assumed, differs in different lo- calities. Some of the species, e. g., Cnemidophorus sexlineatus, never abandon the coloration of the young of other species and subspecies. The same condition is characteristic of the C. deppei of Mexico, the C. lem- niscatus of Brazil, and other species. The process of color-modification in the C. tessellatus and C. gularis of North America is, as I have pointed out,1 as follows : The young are longitudinally striped with from two to four stripes on each side of the middle line. With in- creasing age, light spots appear between the stripes in the dark interspaces. In a later stage these spots increase in transverse diameter, breaking up the dark bands into spots. In some of the forms these dark spots extend themselves transversely and unite with each other, forming black cross-stripes of greater or less length. Thus we have before us the process by which a longitudinally striped coloration is transformed into a transversely striped one. The large number of specimens of the C. tessellatus and C gularis in the National Museum collection show that the breaking up of the striped coloration appears 1 Proceeds. Amer. Philos. Soc., 1885, p. 283. Transac. Amer. Philos. Soc 1892, p. 27. 42 PRIMARY FACTORS OF ORGANIC EVOLUTION. v / ON VARIATION. 43 first at the posterior part of the dorsal region (i. e., the sacral and lumbar). The confluence of the spots ap- pears there first; and finally (C. gularis semifasciatus}, where the color markings disappear, leaving a uniform hue, this also appears first at the posterior part of the 44 PRIMARY FACTORS OF ORGANIC EVOLUTION, ON VARIATION. 45 body. In the C. tessellatus rubidus the dark spots dis- appear first on the anterior regions. According to Eimer,1 among many color-variations of the Lacerta muralis there exists a series of types closely similar to those observed by me to characterize the two species of Cnemidophorus mentioned. I give figures of these series in all three species. It will be observed that in the second and third forms (B and C) of the L. muralis, the pale portions of the dark stripes do not'assume the very light hue of the ground color as they do in the corresponding phase of the Cnemido- phorus tessellatus (C and D, Fig. 12), but this interme- diate condition is exactly paralleled by the subspecies mariarum of the Cnemidophorus gularis. The corre- spondences are represented in the table on page 46. There are some color forms in the Lacerta muralis which are not repeated in the North American Cnemi- dophori, particularly those whidh result in a strong contrast between the dorsal colors as a whole and the darker lateral colors, as a band. The color variety, No. 7, of the Cnemidophori is not reported by Eimer as occurring in the Lacerta muralis. The variations from one to four form a direct series, and so do those represented by Nos. i, 2, 3, and 5. Such variations cannot be regarded as promiscuous, especially when the same process of change is to be observed in three different species, one of which in- habits a continent remote from the other two. d. Variations in North American Birds and Mammals in Relation to Locality. The distinguished zoologist, Dr. J. A. Allen of New York, has made a thorough study of this subject with \ArchivfUr Naturgeschichte, 1881, p. 239. 46 PRIMARY FACTORS OF ORGANIC EVOLUTION. ^1 O> Ln 4^ OJ M M 1 ? i. ? s s | s- s i. ? ? ~ PT* o ?r* CD >-*• ^ 1-1 x* o ^>* ^* P J2 " £ °* » 3 to 7 »-. g- rl •§• ?•§ si ! I rt> ,3 r-t- (-> CO CO ^ w ^WS0 ^^ Longitudinal • "rS ^ S o P S £;* • P o o^loa oS ^C : § 5 fl a .| | s 8 ¥1 :S | -s^S ll p S- T3 3 -* 5. n i P« « P Cb rt- a, w : § S ff S g S. a O cT n p J^ : p ^ P - * o- g. rr* DJ ^ CD ^ : 3 « I K g s: : < sr o oo JL oo • P H : ? £T ^ 2" • C ^ n • £ C P > rs |: 5, ^ S. 5. ^^ £ •5 • I 1 1 1 i 1 i v^ ~C^ S ' ? r> r^ r> 0, c^ Ci .***• &<3 0^ O'o Cr^ ? ^ S *\ Co ' ft 5.' a ' > ? ? ^> r~j Oj Oj C"j § ^ ^ a" §. 1^1 C ? 0 P ^ ft ^ <-Xi a' a1 ^ 1 1: | -10' 1 1 1 R ^ N hi ' ' h» CN hi fN a 5! •** r* g- •** .** g ? g |- s. £. £ ^ 1 p> 21 5j ^ | ? | ' 1 II 1 S ^ 1. 1 1 ?' Si- R ON VARIATION. 47 ample material at his disposal. Following lines al- ready laid down by Prof. Spencer F. Baird, Dr. Allen has shown that variations in form, size, and color are directly related to latitude, and that they are not pro- miscuous or multifarious, but are definite and graded. I make the following extract from a summary of the subject published by him in The Radical Review (New Bedford, Mass.) for May, 1877: "Geographical variation, as exhibited by the mam- mals and birds of North America, may be summarized under the following heads, namely : (i) variation in general size, (2) in the size of peripheral parts, and (3) in color ; the latter being subdivisible into (a) vari- ation in color with latitude, and (/£) with longitude. As a rule, the mammals and birds of North America increase in size from the south northward. This is true, not only of the individual representatives of each species, but generally the largest species of each genus and family are northern. There are, however, some strongly marked exceptions, in which the increase in size is in the opposite direction, or southward. There is for this an obvious explanation, as will be presently shown ; the increase being found to be almost invari- ably toward the region where the type or group to which the species belongs receives its greatest numer- ical development, and where the species are also most specialized. Hence the representatives of a given spe- cies increase in size toward its hypothetical center of distribution, which is in most cases doubtless also its original center of dispersal. Consequently there is fre- quently a double decadence in size within specific groups, and both in size, and numerically in the case of species, when the center of development of the group to which they belong is in the warm-temperate or trop- 48 PRIMARY FACTORS OF ORGANIC EVOLUTION. ical regions. This may be illustrated by reference to the distribution of the higher classes of vertebrates in North America. Among the species occurring north of Mexico there are very few that may not be supposed to have had a northern origin ; and the fact that some are circumpolar in their distribution, while most of the others (especially among the mammals) have congeneric Old World allies further strengthens the theory of their northern origin. Not only do individuals of the same species increase in size toward the north, but the same is true of the species of different genera. Again, in the exceptional cases of increase in size southward, the species belong to southern types, or, more correctly, to types having their center of development within or near the intertropical regions, where occur, not only the greatest number of the specific representatives of the type, but also the largest. "For more detailed illustration we may take three families of the North American Carnivora; namely, the Canidae (wolves and foxes), the Felidae (lynxes and wild cats), and the Procyonidae (raccoons). The first two are to some extent cosmopolitan, while the third is strictly American. The Canidae have their largest specific representatives, the world over, in the temperate or colder latitudes. In North America the family is represented by six species,1 the smallest of which (speaking generally) are southern, and the larg- est northern. Four of them are among the most widely distributed of North American mammals, two (the gray wolf and the common fox) being circumpolar spe- cies ; another (the Arctic fox) is also circumpolar, but IThe gray wolf (Cam's lupus], the coyote (C. latrans), the Arctic fox (Vul- pes lagopus) , the common fox (V. alopex], the kit fox (V. velox], and the gray fox {V. cinereoargentatus). ON VARIATION. 49 is confined to high latitudes. The three widest-rang- ing species (the gray wolf, the common fox, and the gray fox) are those which present the most marked variation in size. Taking the skull as the basis of comparison, it is found that the common wolf is fully one-fifth larger in the northern parts of British Amer- ica and Alaska than it is in Northern Mexico, where it finds the southern limit of its habitat. Between the largest northern skull and the largest southern skull there is a difference of about thirty-five per cent, of the mean size! Specimens from the intermediate region show a gradual intergradation between these extremes, although many of the examples from the upper Mis- souri country are nearly as large as those from the ex- treme North. "The common fox, though occurring as far north as the wolf, is much more restricted in its southward range, especially along the Atlantic coast, and presents a correspondingly smaller amount of variation in size. The Alaskan animal, however, averages about one- tenth larger than the average size of specimens from New England. In the gray fox, whose habitat ex- tends from Pennsylvania southward to Yucatan, the average length of the skull decreases from about five inches in Pennsylvania to considerably less than four in Central America — a difference equal to about thirty per cent, of the mean size for the species. "The Felidae, unlike the Canidae, reach their great- est development, as respects both the number and the size of the species, in the intertropical regions. This family has but a single typical representative — the panther (Felis concolor} — north of Mexico, and this ranges only to about the northern boundary ot the United States. The other North American represen- 50 PRIMARY FACTORS OF ORGANIC EVOLUTION. tatives of the family are the lynxes, which, in some of their varieties, range from Alaska to Mexico. They form, however, the most northern, as well as the most specialized or ' aberrant/ type of the family. While they vary greatly in color, as well as in the length and texture of the pelage, at different localities, they afford a most remarkable exception to all laws of variation in size with locality; for a large series of skulls, repre- senting localities as widely separated as Louisiana, Northern Mexico, and California, on the one hand, and Alaska and the Mackenzie River district on the other, as well as various intermediate localities, reveals no ap- preciable difference in size throughout this wide area. The true cats, however, as the panther and the ocelots, are found to greatly increase in size southward, or to- ward the metropolis of the family. The panther ranges from the Northern States southward over most of South America. Skulls from the Adirondack region of New York have an average length of about seven and a half inches, the length increasing to eight and three- quarters in Louisiana and Texas, from beyond which points there is lack of data. The ocelot (Felis parda- lls) finds its northern limit near the Rio Grande of Texas, and ranges thence southward far into South America. The average size of Costa Rican examples is about one-fifth greater than that of specimens from the Rio Grande. Instances of increase in size northward among the Carnivora of North America are so generally the rule that further space need not be taken in recounting ex- amples, in detail. It may suffice to state that the badger (Taxidea americand}, the marten (Mustela ame- ricana], the fisher (M. pennanti}, the wolverine {Gulo luscus}, and the ermine {Putorius ermineus} — all north- ON VARIATION. 51 ern types — afford examples of variations in size strictly parallel with that already noticed as occurring in the foxes and wolves. "To refer briefly to other groups, it may be stated that the Cervidae (deer family) are mainly rather north- ern in their distribution ; that the largest species occur in the colder zones, and that individuals of the same species increase rapidly in size toward the north. Some of the species, in fact, afford some of the most striking instances of northward increase in size ; among which are the Virginia deer and its several representa- tives in the interior of the continent and on the Pacific Slope. It is also noteworthy that the most obviously distinctive characteristic of the group — the large, an- nually deciduous antlers — reaches its greatest devel- opment at the northward. Thus all the northern spe- cies, as the moose, the elk, and the caribou, have branching antlers of immense size, while the antlers are relatively much smaller in the species inhabiting the middle region of the continent, and are reduced to a rudimentary condition— a simple, slender, sharp spike, or a small and singly forked one — in the tropical spe- cies; the antlers declining in size much more rapidly than the general size of the animal. This is true in individuals of the same species as well as of the species collectively. "The Glires (the squirrels, marmots, spermophiles mice, and their affines) offer the same illustrations in respect to the law of increase in size as the species already mentioned, the size sometimes increasing to the southward, but more generally to the northward, since the greater number of the species belong decid- edly to northern types. There is no more striking in- stance known among mammals of variation in size 52 PRIMAR Y FA CTORS OF ORGANIC E VOL UTION. with locality than that afforded by the flying squirrels, in which the northern race is more than one-half larger than the southern ; yet the two extremes are found to pass so gradually the one into the other, that it is hardly possible to define even a southern and a north- ern geographical race, except on the almost wholly arbitrary ground of difference in size. The species, moreover, is one of the most widely distributed, rang- ing from the Arctic regions (the northern limit of for- ests) to Central America. "Among birds the local differences in size are al- most as strongly marked as among mammals, and in the main, follow the same general law. A decided increase in size southward, however, or toward the warmer latitudes, occurs more rarely than in mam- mals, although several well-marked instances are known. The increase is generally northward, and is often very strongly marked. The greatest difference between northern and southern races occurs' as in mammals, in the species whose breeding-stations em- brace a wide range of latitude. In species which breed from Northern New England to Florida, the southern forms are not only smaller, but are also quite different in color and in other features. This is eminently the case in the common quail {Ortyx virgim'anus), the meadow-lark (Sturnella magna~), the purple grackle (jQuiscalus purpurcus), the red- winged blackbird (Age- laeus phaeniceus}, the golden- winged woodpecker (Co- laptes auratus^y the towhee (Pipilo erythrophthalmus}, the Carolina dove (Zenczdura macrura), and in nu- merous other species ; and is quite appreciable in the blue-jay (Cyanurus cristatus}, the crow {Corvus ameri- canus}, in most of the woodpeckers, in the titmice, numerous sparrows, and several thrushes and war- ON VARIATION. 53 biers, the variation often amounting to from ten to fifteen per cent, of the average size of the species. "As a general rule, certain parts of the organisms vary more than does general size, there being a marked tendency to enlargement of peripheral parts under high temperature, or toward the tropics, — hence south- ward in North America. This is more readily seen in birds than in mammals, in consequence, mainly, of their peculiar type of structure. In mammals it is manifested occasionally in the size of the ears and feet, and in the horns of bovines, but especially and more generally in the pelage. At the northward, in individ- uals of the same species, the hairs are longer and softer, the under fur more abundant, and the ears and the soles of the feet better clothed. This is not only true of individuals of the same species, but of northern species collectively as compared with their nearest southern allies. Southern individuals retain perma- nently, in many cases, the sparsely clothed ears and the naked soles that characterize northern individuals only in summer, as is notably the case among the dif- ferent squirrels and sphermophiles. "In mammals which have the external ear largely developed — as in the wolves, foxes, some of the deer, and especially the hares, — the larger size of this organ in southern as compared with northern individuals of the same species is often strikingly apparent. It is more especially marked, however, in species inhabit- ing extensive open plains and semi-desert regions. The little wood hare, or gray rabbit {Lfyus sylvaticus), affords a case in point. This species is represented, in some of its varieties, across the whole breadth of the continent, and from the northern border of the United States southward to Central America, but in 54 PRIMARY FACTORS OF ORGANIC EVOLUTION. different regions by geographical races or subspecies. In addition to certain differences of color and general size, the ears vary still more strongly. In the form inhabiting tire Great Plains, commonly known as the little sage-brush hare (Z. sylvaticus nuttalli}, the ears are considerably longer than in the eastern variety, and increase in size from the north southward, reach- ing their greatest development in Western Arizona and the desert region further westward and southward, where the variety is characterized mainly by the large size of its ears, which are in this race nearly_twice the size they attain in the eastern variety. In the long- eared ' jackass' hares of the plains, the ear likewise increases in size to the southward. In Lepus callotis, for example, which ranges from Wyoming southward far into Mexico, the ear is about one-fourth to one- third larger in the southern examples than in the north- ern. The little brown hare of the Pacific Coast (Z. trowbridgei) presents a similar increase in the size of the ear southward, as does, to a less extent, the prairie hare (Z. eampestris). Not only are all of the long- eared species of American hares confined to the open plains of the arid interior of the continent, but over this same region is the tendency to an enlargement of the ear southward stronger than elsewhere. It is also of interest in this connection that the largest-eared hares of the Old World occur over similar open, half- desert regions, as do also the largest-eared foxes. On our western plains, the deer are represented by a large- eared species. Among the domestic races of cattle, those of the warm temperate and intertropical regions have much larger and longer horns than those of north- ern countries ; as is shown by a comparison of the Texan, Mexican, and South American breeds, with ON VARIATION. 55 the northern stock, or those of the South of Europe with the more northern races. In the wild species of the Old World, the southern or sub-tropical are re- markable for the large size of their horns. The horns of the American prong-horn {Antilocapra americand} are also much larger at southern than at northern locali- ties.1 Naturalists have also recorded the existence of larger feet in many of the smaller North American Mammalia at the southward than at the northward, among individuals of the same species, especially among the wild mice, in some of the squirrels, the opossum and raccoon, as well as in other species. "In birds, the enlargement of peripheral parts, es- pecially of the bill, claws, and tail, is far more obvious and more general than in mammals. The bill is par- ticularly susceptible to variation in this regard, — in many instances being very much larger, among indi- viduals of unquestionably the same species, at the southward than at the northward. This accords with the general fact that all the ornithic types in which the bill is remarkably enlarged occur in the intertropical regions. The southward enlargement of the bill within specific groups may be illustrated by reference to al- most any group of North American birds, or to those of any portion of the continent. As in other features of geographical variation, the greatest differences in the size of the bill are met with among species having the widest distribution in latitude. Among the species inhabiting eastern North America we find several strik- IThe deer tribe, in which the antlers increase in size toward the north, offer an apparent exception to the rule of increase in size of peripheral parts toward the tropics. The antlers of the deer, however, are merely seasonal appendages, being annually cast and renewed, and are thus entirely different physiologically from the horns of bovines, which retain a high degree of vitality throughout the life of the animal. 56 PRIM 'A R Y FA CTORS OF OR CAN 1C E VOL UTION. ing examples of this enlargement among the sparrows, black-birds, thrushes, crows, wrens, and warblers, in the quail, the meadow-lark, the golden-winged wood- pecker, etc. Generally the bill, in the slender-billed forms, becomes longer, more attenuated, and more de- curved (in individuals specifically the same) in pass- ing from the New England States southward to Flo- rida, while in those which have a short, thick, conical bill there is a general increase in its size so that the southern representatives of a species, as a rule, have thicker and longer bills than their northern relatives, though the birds themselves are smaller. There is thus not only generally a relative, but often an abso- lute, increase in the size of the bill in the southern races. The species of the Pacific Coast and of the in- terior afford similar illustrations, in some cases more marked even than in any of the eastern species. More rarely, but still quite frequently, is there a similar in- crease in the size of the feet and claws. "The tail, alsq, affords an equally striking exam- ple of the enlargement of peripheral parts southward. Referring again to the birds of the Atlantic Coast, many of the above-named species have the tail abso- lutely longer at southern localities than at northern, and quite often relatively longer. Thus while the gen- eral size decreases, the length of the tail is wholly maintained, or decreases less than the general size ; but, in some cases, while the general size is one-tenth or more smaller at the south, the tail is ten to fifteen per cent, longer than in the larger northern birds. Some western species are even more remarkable in this respect ; and in consequence mainly of this fact the southern types have been varietally separated from the shorter-tailed northern forms of the same species. ON VARIATION. 57 "Variations in color with locality are still more ob- vious, particularly among birds, in which the colors are more positive, the contrasts of tints greater, and the markings consequently better denned than is usu- ally the case in mammals. The soft finely-divided covering of the latter is poorly fitted for the display of the delicate pencilings and the lustrous, prismatic hues that so often characterize birds. Mammals, how- ever, present many striking instances of geographical variation in color. "As already stated, geographical variations in color may be conveniently considered under two heads. While the variation with latitude consists mainly in a nearly uniform increase in one direction, the variation observed in passing from the Atlantic Coast westward is more complex. In either case, however, the varia- tion results primarily from nearly the same causes, which are obviously climatic, and depend mainly upoi the relative humidity, or the hygrometric conditions of the different climatal areas of the continent. In re- spect to the first, or latitudinal variation, the tendency is always toward an increase in intensity of coloration southward. Not only do the primary colors become deepened in this direction, but dusky and blackish tints become stronger or more intense, iridescent hues become more lustrous, and dark markings, as spots and streaks or transverse bars, acquire greater area. Conversely, white or light markings become more re- stricted. In passing westward a general and gradual blanching of the colors is met with on leaving the wooded regions east of the Mississippi, the loss of color increasing with the increasing aridity of the cli- mate and the absence of forests, the greatest pallor occurring over the almost rainless and semi-desert re- 58 PRIMARY FACTORS OF ORGANIC EVOLUTION, gions of the Great Basin and Colorado Desert. On the Pacific Slope, north of California, the color again increases, with a tendency to heavy, sombre tints over the rainy, heavily-wooded region of the Northwest Coast."1 2. VARIATION IN STRUCTURAL CHARACTERS. Modifications of structural characters may appear quite independently of variation of specific ones. In- deed, generic characters have at times changed completely without the appearance of corresponding changes in the more superficial characters which de- fine the species. Thus changes in the dentition of some of the Mammalia appear within the limits of species, which, should they become permanent, would entitle the two sets of individuals which display the different dentitions to be placed in different genera. Some striking examples of how generic characters may undergo metamorphosis without corresponding changes in specific characters, have been brought to light by Dr. William H. Dall among the Brachiopo- dous Mollusca. Some of the species of different gen- era can scarcely be distinguished, except by compari- son of their generic characters. I have cited the axolotls as illustrative of this phenomenon. Here the same species may reproduce as a permanent larva, or as an adult. Dume"ril has shown that the North Amer- ican salamander (Amblystoma tigrinuni} can lay and fertilize eggs before the metamorphosis is passed. I have since observed that the females of the allied spe- cies of Amblystomidae, the Chondrotus tenebrosus B. and G., of California contain mature eggs ready for de- 1 The Radical Review, May, 1877. ON VARIATION. 59 posit, and have supposed that this species has also the same power.1 The difference between such larvae and the adult which has passed the metamorphosis is great. It extends not merely to the branchial processes, but to the splenial teeth, which are shed, and to the palato- pterygoid arch, which is absorbed, and to the pos- terior ceratobranchial and epibranchial cartilages, which are absorbed. In the larva of the C. tenebrosus the palatopterygoid arches and epibranchials are ossified, so that the probability of its being able to maintain an independent existence as a larva is greater than in the case of the A. tigrinum. In this type, then, each spe- cies displays variations concomitant with reproductive maturity, which are not only of generic, but of family significance. In a third species, the Siredon mexica- num, no metamorphosis has yet been shown to take place, so that it is probable that it reproduces ordina- rily while in the branchiferous stage. Yet it is only specifically different from the larva of the Amblystoma tigrinum. Excellent illustrations of the serial appearance of generic characters may be seen in the family of the dogs (Canidae). In the true genus Canis, the dental formula is, I. |; C. \\ P. m. f ; M. f . The inferior sec- torial (m. i) has a metaconid, and the second inferior true molar has two roots. It not unfrequently hap- pens, however, that the last inferior molar (m. 3) is wanting ; and in some cases the inferior m. 2 has but one root. When in addition to this, as in some of the black-and-tans, in the Mexican naked dog, and in the pug, the inferior m. i loses its metaconid, we have the genus Synagodus. Occasionally the pug dog, and fre- quently the Mexican dog, loses one of its premolars IBatrachia of North America, 1888, p. 113, PI. xxii, xxiii. 60 PRIMARY FACTORS OF ORGANIC EVOLUTION. from both jaws. The Japanese spaniel goes still fur- ther, and usually loses also its second superior true molar and frequently another premolar from each jaw; and we then have a dentition which indicates a third genus, which has been called Dysodus. Its dental formula is I. $ ; C. \ ; P. m. \-\ ; m. J. Transitions between this and the normal dentition of Canis, in all respects can be found in the smaller domesticated dogs. And these modifications are not pathological, but simply express a rapid metamorphosis of the den- tition towards the reduced formula which is charac- teristic of the cats. And while the most characteristic dentitions belong to particular species (or races) of dogs, many of the single modifications are both absent and present in dogs of the same species or race. And these are the kind of characters which are observed to mark the slow progress during long geologic ages, of mammals of various other groups. These modifications are not promiscuous, but are in the di- rect line of change which has characterized all Mam- malia during geologic time; i. e., the reduction of the numbers of the molar teeth. And in greater detail, the loss of metaconid of the inferior sectorial, and loss of posterior true molars, are the exact losses which the carnivorous type has undergone in the evolution of the cats. A significant modification of the third superior pre- molar has been observed by Dr. Horace Jayne to be occasionally met with in the domestic cat. Sometimes an internal cusp (deuterocone), with a corresponding root is developed, giving rise to a tritubercular crown. Similar observations have been made on the denti- tion of man, which presents two phenomena of varia- tion of opposite phylogenetic significance. I have ON VARIATION. 61 shown1 that most of the Indo-European race, together with the Esquimaux, present a reversion to a lemu- rine form in the second and third superior molars, and sometimes, in the case of the Esquimaux, in the first superior molar also. I have also shown,2 after a study of the dentition of the extinct Mammalia, that the more complex molars of later placental orders, have been derived from a tritubercular type, which prevailed throughout the earth just before the opening of the Eocene period. In the line of human and quadruma- nous phylogeny, the lemurs of the Eocene period pre- sented this type of molar in the upper jaw, and mostly continue to do so to the present time. The true mon- keys, however, added the fourth tubercle or hypocone, in accordance with the developmental law in Mamma- lia generally, and the apes and men of the lower races present the same characteristic. Now, in the yellow race the hypocone of the last molar is generally want- ing, while in the white race it is usual to find it absent from both the second and third molars. In this we have a case of reversion. The reduction of the third (last) superior molar, and of the inferior as well, has gone further in the white race, since the tooth is frequently abnormally small, abortive, or totally wanting. The external su- perior incisor has a similar history, although its reduc- tion and loss is not nearly so frequent as that of the last molars. These losses from the dental series are not of the nature of reversions, since the number of teeth is more and more numerous as we recede in time along the line of human ancestry. It is, on the contrary, the continuation of a process which has been, 1 American Journal of Morphology , 1888, p. 7. 2 American Naturalist, 1884, p. 350; Origin of the Fittest, 1887, p. 347. 62 PRIMARY FACTORS OF ORGANIC EVOLUTION. as already remarked, common to all the Mammalia, of reduction in the number of teeth. Thus men with fewer teeth are more advanced than those with more numer- ous ones ; while people with tritubercular superior molars have reverted to an ancient type ; and both re- sults are probably attained by the same physiologic process, i. e. defect of nutrition. It is to be remem- bered also, in connection with our argument, that these dental variations are modifications of generic charac- ters, and that they are in definite directions, and are not promiscuous. With regard to the question as to whether dental variations in man are promiscuous or not, we have better opportunities of investigation than in the case of the lower animals generally. It may be safely asserted that the dental variations above cited are by far the most frequent in man, and that all others put together are relatively insignificant. 3. SUCCESSIONAL RELATION. As the biologic types are variations become perma- nent, it is important to examine how the former stand related to each other. These relations express the direction which variation has taken, and throw a great deal of light on the nature of the process. That exist- ing types of all grades are the result of the isolation of variations of species, is shown by the frequent exam- ples of incomplete isolation, which follows inconstancy of the definitive characters. Groups of individuals which display this partial isolation are termed sub- species. As an illustration of the mingling of isolated groups of individuals (species) with imperfectly isolated groups (subspecies), in a single genus, I refer to the American ON VARIATION. 63 garter-snake (genus Eutaenia B. and G.). An exami- nation of several hundred individuals of this genus yielded the following results : I found seventeen groups of individuals, which could be said to be completely isolated in characters, with very few exceptions. Eight other groups (species) are probably isolated, but they are not represented by a sufficiently large number of specimens to yield a satisfactory demonstration. Of the seventeen, four species embrace fifteen non-isolated geographical forms (subspecies), besides the typical forms (eight of which are included under the E. sirta- lis); and two others include three color forms easily recognizable, besides the typical ones. Similar phe- nomena are presented in every part of the animal and vegetable kingdoms. One of the most instructive natural divisions for the study of taxonomic relations as the result of varia- tion, on account of the simplicity of the relations pre- sented, is the Batrachia Salientia, or the order of Ba- trachia to which belong the toads, frogs, etc. Omitting the very restricted suborders of the Aglossa and Gas- trechmia, the Batrachia Salientia fall into two divi- sions, which differ only in the structure of the lower portion of their scapular arch, or shoulder-girdle. In the one the opposite halves are capable of movements which contract or expand the capacity of the thorax ; in the other the opposite halves abut against each other so as to be incapable of movement, thus pre- serving the size of the thoracic cavity. But during the early stages, the frogs of this division have the mova- ble shoulder-girdle which characterizes those of the other division, the consolidation constituting a modifi- cation superadded in attaining maturity. Further- more, young Salientia are toothless, and one section of 64 PRIMARY FACTORS OF ORGANIC EVOLUTION. the species with embryonic shoulder-girdle never ac- quire teeth. The suborder with embryonic shoulder- girdle is called the Arcifera, and that which is ad- vanced in this respect is the Firmisternia. Now the frogs of each of these divisions present nearly similar scales of development of another part of the skeleton, viz., the bones of the top of the skull. We find some in which one of these bones (ethmoid) is represented Fig. 17- Fig. 16. SHOULDER-GIRDLES OF "ANURA." Fig. 15. — Of the Arciferous type (Phyllomedusa bicolor}. Fig. 16, Rana temporaria, tadpole with budding limbs. Fig. 17, do., adult. Figs. 16 and 17 from Parker. by cartilage only, and the frontoparietals and nasals are represented by only a narrow strip of bone each. In the next type the ethmoid is ossified ; in the next, we have the frontoparietal completely ossified, and the nasals range from narrow strips to complete roofs ; in the fourth station on the line, these bones are rough, with a hyperostosis of their surfaces ; and in the next set of species this ossification fills the skin, which is thus no longer separable from the cranial bones ; in ON VARIATION. 65 the sixth form the ossification is extended so as to roof in the temporal muscles and inclose the orbits behind, while in the rare seventh and last stage, the tympanum is also inclosed behind by bone. Now all of these types are not found in all of the families of the Salien- tia, but the greater number of them are. SMC principal families, four of which belong to the Arcifera, are named in the diagram below, and three or four others might have been added. I do not give the names of the genera which are defined as above described, re- ferring to the explanation of the cuts for them, but in- dicate them by the numbers attached in the plate, which correspond to those of the definitions above given. A zero mark signifies the absence or non-dis- covery of a generic type. Sternum embryonic. Arcifera. Sternum complete Toothless. Toothed. Firmisternia. Bufonidae. Scaphiopidae. Cystignathidae. Hylidae. Ranidae. 1 10 I I O 2 — C 2 2 2 O 3—30 333 4—4 4 4 44 5—5 5 ° 55 6—6 6 6 66 7 — 70 o o o It is evident, from what has preceded, that a per- fecting of the shoulder-girdle in any of the species of the arciferous columns would place it in the series of Firmisternia. An accession of teeth in a species of the division BufonidceviQ>\A<\ make it one of the Scaphiopid(z\ while a small amount of change in the ossification of the bones of the skull would transfer a species from one to another of the generic stations represented by the numbers of the columns from one to seven. Fig. 19- SCAPHIOPID-E AND PELOBATID.*. Fig. 20. HYLID.*. Fig. 21. CYSTIGNATHID.S. 68 PRIMARY FACTORS OF ORGANIC EVOLUTION. That the above generic divisions have been actually developed from each other is demonstrated by the oc- currence of occasional intermediate forms. Thus no generic distinction can be maintained between types third and fourth in the family of toads (Bufonidae), so complete is the transition between them. In Hylidae and Cystignathidae occasional transitions between types second and third occur. In the Scaphiopidae the sub- species Spea hammondii intermontana sometimes has the frontoparietal fontanelle open, sometimes closed. I have seen some adult specimens of Rana virescens au- stricola from Central America with the ethmoid bone unossified above, as in the genus Ranula. The rugose cranium is only acquired in old age of some of the spe- cies of Polypedates of India. Yet these genera are as EXPLANATION OF CUTS OF CRANIA OF SALIENTIA. The numbers in each column correspond with the types of ossification mentioned in the text, and are the same as those in the table of families given in the same connection. The power numbers attached to No. 4, represent the degree of ossification of the nasal bone, except -l, which signifies unossified ethmoid. Most of the cuts are original. Fig. 18. — BUFONIDAE. — No. i, anterior part of skull of Chelydobatrachus gouldii Gray, from Australia. No. 4, do. of Schismaderma carens Smith, South Africa. No. 5, 'top of head of Peltaphryne peltacephala D. and B., Cuba. No. 7, top of head of Otaspis empusa Cope, Cuba. Fig. 19.— SCAPHIOPID.E AND PELOBATiD^E.— No. 2, diagram of top of cranium of Didocus calcaratus Micahelles, Spain. No. 5, skull of Scaphiopus holbrookii Harl., United States. No. 6, skull of Cultripes provincialis, from France, after Duges. Fig. 20. — HYLID-E. — No. I, Thoropa miliaris Spix., Brazil. No. 2, Hypsi- boas doumercii D. and B., Surinam. No. al, Hypsiboas punctatus Schn., Brazil. No. 4^, Scytopis venulosus Daudin, Brazil. No. 5, Osteocephalus planiceps Cope, E. Peru. No. 6, Trachycephalus geographicus D. and B., after Steindachner. Fig. 21. — CYSTIGNATHID.*. — No. i, Eusophus nebulosus Gir., Chili. No. 2, Borborocoetes tasmaniensis Gthr., Tasmania. No. 3, Elosia nasus Licht., Bra- zil. No. 4, Hylodes oxyrhynchus D. and B., West Indies. No. 6, Calyptocepha- lus gayi D. and B., Chili. Fig. 22. — RANID.E. — No. 4- 1, Ranula ckrysoprasina Cope, Costa Rica. No. 4!, Rana clamata Daud., N. America. No. 48, Rana agilis Thomas, Europe. No. 48, Rana hexadactyla Less., India. No. 5, Polypedates quadrilineatus D. and B., Ceylon. ON VARIATION. 6g well defined as closely allied genera in most natural divisions. It is seldom that so many stages of developmental series survive so as to be contemporaries, as in this case of the Batrachia Salientia. In order to obtain such series we usually have to explore the ages of the past. In the higher groups this is also the case, but here we have also occasional examples of the persis- tence of fairly complete series. Such a one is pre- sented by the suborder Artiodactyla of the Diplarth- rous Ungulate Mammalia. I give the definitions of the succession of the existing families. I. Molars bunodont (tubercular) ; superior incisors generally pres- ent. No cannon or naviculocuboid bones. Lateral toes well developed ; Hippopotamida. Lateral toes rudimental ; Suidtz. II. Molars selenodont (crescent-bearing). (Lateral toes rudimental or wanting). A. Premolars with one row of lobes. No naviculocuboid bone ; one superior incisor ; a can- non bone ; Camelidce. A naviculocuboid bone ; no superior incisor ; (cannon bone variable) ; Tragulida. AA. Premolars with two rows of tubercles ; a naviculocuboid and cannon bones ; no incisors above. Premolar iii with only one row of lobes ; canine teeth, no horns ; Moschida. Premolar iii with two rows of lobes ; fixed horns ; no canines above ; Bovida. Premolar iii with two rows of lobes ; horns decidu- ous ; Cervidtz. In this suborder we see a gradual complication of the structure of the molar teeth, and a loss of the in- cisors. In the limbs we observe the successive loss of the lateral digits, and the fusion of elements, — as the metapodials into cannon bones, and the elements of 7o PRIMAR Y FA CTORS OF OR GANIC E VOL UTION. the tarsus, and, what is not stated in the above table, of the carpus also. Finally there is the remarkable development of horns on the head. When we come to examine the phylogeny of this order we will find how completely these characters are the result of the fixation of variations which have appeared in past geo- logic ages, and how various are the combinations and modifications presented by the extinct types. Few natural groups permit of representation of their subdivisions in linear series. The only correct representation is in the form of a branching tree, and this cannot be well done in flat projection on the pages of a book. Each branch taken by itself, however, yields itself for a longer or shorter space to linear treatment. For an example of such linear series in higher groups I turn again to the Batrachia Salientia. Here the two suborders of the Arcifera and Firmisternia pre- sent the following interesting parallels : ARCIFERA. FIRMISTERNIA I. Without teeth. a. With sacral diapophyses dilated. Brevicipitidae. Bufonidae J Engystomidse. [ Phryniscidae. aa. Sacral diapophyses cylindric. Dendrophryniscidae. Dendrobatidae II. With premaxillary and maxillary teeth only. a. With sacral diapophyses dilated. Pelod>"iranchii— Acanthodii Agi atha Tunicata Acrania Enteropneusta The Vertebrata exhibit the most unmistakable gra- dation in the characters of the circulatory system. It has long been the custom to define the classes by means of these characters, taken in connection with those of the skeleton. Commencing in the Leptocardii with the simple tube, we have two chambers in the Marsi- pobranchii and fishes ; three in the Batrachia and Rep- tilia ; and four in the Aves and Mammalia. The aorta- roots commence as numerous pairs of branchial arter- ies in the Leptocardii ; we see seven in the Marsipo- branchi, five in the fishes (with number reduced in some) ; four and three in Batrachia, where they gen- erally cease to perform branchial functions ; two and one on each side in Reptilia ; the right-hand one in birds, and the left-hand one in Mammalia. This order is clearly an ascending one throughout. It consists of, first, a transition from adaptation to an aquatic, to 94 PRIMARY FACTORS OF ORGANIC EVOLUTION. an aerial respiration ; and, second, an increase in the power to aerate and distribute a circulating fluid of in- creased quantity, and of increased calorific capacity. In other words, the circulation passes from the cold to the hot-blooded type coincidentally with the changes of structure above enumerated. The accession of a ca- pacity to maintain a fixed temperature while that of the surrounding medium changes, is an important ad- vance in animal economy. The brain and nervous system also display a gen- eral progressive ascent. Leaving the brainless Acrania, the Marsipobranchs and fishes present us with small hemispheres with thin cortex, larger optic lobes, and well-developed cerebellum. The hemispheres are really larger than they appear to be, as Rabl Riickard has shown l that the supposed hemispheres are only corpora striata. But the superior walls are membranous, and support on their internal side only a layer of epithelial cells, as in the embryos of other Vertebrata, instead of the gray substance. So that, although we find that the cerebellum is really smaller in the Batrachia and most Reptilia than in the fishes, the better development of the hemispheres in the former gives them the pre- eminence. The Elasmobranchii show themselves su- perior to many of the fishes in the large size of their corpora restiformia and cerebellum. The Reptilia con- stitute an advance on the Batrachia. In the latter the optic thalami are, with some exceptions, of greater diameter than the hemispheres, while the reverse is generally true of the reptiles. The crocodiles display much superiority over the other reptiles in the larger cerebellum, with rudimental lateral lobes. The greater development of the hemispheres in birds is well known, \Biologisches Centralblatt, 1884, p. 449. PHYLOGENY. 95 while the general superiority of the brain of the living Mammalia over all other vertebrates is admitted. The consideration of the successive relations of the skeleton in the classes of vertebrates embraces, of course, only the characters which distinguish those classes. These are not numerous. They embrace the structure of the axis of the skull ; of the ear-bones ; of the suspensors of the lower jaw ; of the scapular arch and anterior limb, and of the pelvic arch and posterior limb. Other characters are numerous, but do not enter into consideration at this time. The persistence of the primitive cartilage in any part of the skeleton is, embryologically speaking, a mark of inferiority. From a physiological or functional standpoint it has the same significance, since it is far less effective both for support and for movement than is the segmented osseous skeleton. That this is a prev- alent condition of the lower Vertebrata is well known. The bony fishes and Batrachia have but little of the primitive cartilage remaining, and the quantity is still more reduced in the higher classes. Systematically, then, the vertebrate series is in this respect an ascend- ing one. The Acrania are membranous ; the Marsi- pobranchii and most of the Elasmobranchii cartilagi- nous ; the other Pisces and the Batrachia have the basicranial axis cartilaginous, so that it is not until the Reptilia are reached that we have osseous sphenoid and presphenoid bones, such as characterize the birds and mammals. The vertebral column follows more or less inexactly the history of the base of the skull, but its characters do not define the classes. As regards the suspensor of the lower jaw, the scale is in the main ascending. We witness a gradual change in the segmentation of the mandibular visceral arch of 96 PRIMARY FACTORS OF ORGANIC EVOLUTION. the skull, which clearly has for its object such a con- centration of the parts as will produce the greatest ef- fectiveness of the biting function. This is accom- plished by reducing the number of the segments, so as to bring the resistance of the teeth nearer to the power, that is, the masseter and related muscles, and their base of attachment, the brain-case. This is seen in PHYLOGENY. 97 bony vertebrates in the reduction of the segments be- tween the lower jaw proper and the skull, from four to none. In the fishes we have the hyomandibular, the symplectic, the inferior quadrate, and the articular. In the Batrachia, reptiles and birds, we have the quad- rate and articular only, while in the Mammalia these elements also are wanting. The examination of the pectoral and pelvic arches reveals a successive modification of the adaptation of the parts to the mechanical needs of the limbs. In this regard the air-breathing types display wide di- versity from the gill-bearing types or fishes. In the latter, the lateral elements unite below without the in- tervention of a median element or sternum, while in the former the sternum, or parts of it, is generally pres- ent. Either arrangement is susceptible of much me- chanical strength, as witness the siluroid fishes on the one hand, and the mole on the other. The numerous segments of the fishes' pectoral arch must, however, be an element of weakness, so that from a mechanical standpoint it must take the lowest place. The pres- ence of sternal elements, with both clavicle, epicora- coid, and coracoid bones on each side, gives the Rep- tilia the highest place for mechanical strength. The loss of the bony coracoid seen in the tailed Batrachia, and loss of coracoid and epicoracoid in the Mammalia, constitute an element of weakness. The line is not then one of uniform ascent in this respect. The absence of pelvis, or its extremely rudimental condition, in fishes, places them at the foot of the line in this respect. The forward extension of the ilium in some Batrachia and in the Mammalia, is to be com- pared with its backward direction in Reptilia, and its extension both ways in the birds. These conditions 98 PR t MAR Y FA CTORS OF ORGANIC E VOL UT1ON. are all derived by descent from a strictly intermediate position in the Batrachia and Reptilia of the Permian epoch. The anterior direction must be regarded as having the mechanical advantage over the posterior direction, since it shortens the vertebral column and brings the grip of the posterior nearer to the anterior feet. The prevalence of the latter condition in the Mammalia enables them to stand clear of the ground, while the Reptilia move with the abdomen resting upon it, excepting the higher Dinosauria, where the arrange- ment is as in birds. As regards the inferior arches of the pelvis, the Mammalia have the advantage again, in the strong bony median symphysis connecting the ischium and pubis.1 This character, universal among the land Vertebrata of the Permian epoch, has been lost by the modern Reptilia and birds, and is retained only by the Mammalia. So the lines, excepting the mam- malian, have degenerated in every direction in the char- acters of the pelvis. The limbs-of the Pisces are as well adapted to their environment as are those of the land Vertebrata ; but, from an embryological standpoint, their structure is inferior. The primitive rays are less modified in the fin than in the limb ; and limbs themselves display a constantly increasing differentiation of parts, com- mencing with the Batrachia and ending with the Mam- malia. The details of these modifications belong to the history of the contents of the classes, however, rather than to the succession of the Vertebrata as a whole. In review, it may be said that a comparison of the characters which define the classes of the vertebrates shows that this branch of the animal kingdom has IThis is an advantage as a protection during gestation. PHYLOGENY. 99 made with the ages successive steps of progress from lower to higher conditions. This progress has not been without exception, since, as regards the construction of the scapular arch, the Mammalia have retrograded from the reptilian standard as a whole. In subsequent pages I shall take up^the lines of the classes separately. b. The Line of the Pisces. The fishes form various series and subseries, and the tracing of all of them is not yet practicable, owing to the deficiency in our knowledge of the earliest or ancestral forms. Thus the origins of the three sub- classes, Holocephali, Dipnoi, and Elasmobranchii, are lost in the obscurity of the early Paleozoic ages. The genus Paleospondylus of Traquair from the Carbonife- rous probably represents an Agnathous type from which all fishes may have sprung, although the genus, as now known, has not sufficient antiquity to claim this place. It may be a near descendant of the amphi- oxus. A comparison of the four subclasses of fishes shows that they are related in pairs. The Holocephali and Dipnoi have no distinct suspensory segment for the lower jaw, while the Elasmobranchii and Teleostomata have such a separate element. The latter, therefore, present one step in the direction of complication be- yond the former. It is, however, asserted by Huxley1 that the absence of suspensorium is due to its appro- priation by the hyoid arch in the Holocephali, and its rudimental condition in the Dipnoi. If this be the case, the Holocephali and Dipnoi are peculiar speciali- 1 Proceedings Zoological Society, London, 1876, p. 45. ioo PRIMARY FACTORS OF ORGANIC EVOLUTION. zations at one side of the main line of descent of the fishes. We look then for the ancestral type of the true fishes among the Elasmobranchii, and of these the Ichthyotomi display the greatest resemblances to the Teleostomata in all respects.1 Too little is known of the history of the subclasses, excepting the Teleostomata, for us to be able to say much of the direction of the descent of their contained orders. On the sharks much light is shed by the dis- covery of characters of the genus Cladodus Agass., in which the support of the paired fins consists of a meta- pterygium, which is enclosed in a lateral fold of the body wall, and which gives rise to simple external basilar rods only. Of the Teleostomata a much clearer history is accessible. It has four primary divisions or tribes which differ solely in the structure of the sup- ports of the fins. In the first division, the Crossopte- rygia, the anterior limbs have numerous basilar bones which are supported on a peduncle of axial bones. The posterior limbs are similar. In the second divi- sion, or Podopterygia (the sturgeons, etc.), the pos- terior limbs remain the same, while the anterior limbs have undergone a great abbreviation in the loss of the axial bones and the reduction of the number and length of the basilar bones. In the third group, or Actino- pterygia, both limbs have undergone reduction, the basilar bones in the posterior fin being almost all atro- phied, while those of the fore limb are much reduced in number. In the fourth superorder, the Rhipido- pterygia, the axial supports of the median fins are greatly reduced in number, presenting a marked con- trast to the other superorders ; while the axial elements 1 See Proceedings American Philosophical Society, 1884, p. 572, on the genus Didymodus. PHYLOGENY. , _joj of the paired fins are present and primitive, and re- semble those of one of the suborders of sharks. The phylogeny of the Teleostomata, as indicated by the fin-structure, will commence with the Crosso- pterygia. From this group the Podopterygia may be theoretically derived, and from these the Actinoptery- gia. The Rhipidopterygia appear to be a side group, not in the main piscine line. But the oldest known Crossopterygia are from the Carboniferous, while the Rhipidopterygia are abundant in the Devonian. More- over, the superorder Actinopterygia, with its contracted fins, may have appeared in the Carboniferous, while the Podopterygia (Palaeoniscidae) certainly did so. The descent of the fishes in general has witnessed, then, a contraction of the limbs to a very small com- pass, and their substitution by a system of accessory dermal radii. This has been an ever-widening diver- gence from the type of the higher Vertebrata, and from this standpoint, and also a view of the "loss of parts without complementary addition of other parts," may be regarded as a process of degeneration. Taking up the great division of the Actinopterygia, which embraces most of the species of living fishes, we can trace the direction of descent largely by ref- erence to their systematic relations when we have no fossils to guide us. The three subtribes adopted by Jordan represent three series of the true fishes which indicate lines of descent. The Holostei include the remainder of the old ganoids after the subtraction of the Rhipidoptery- gia, the Crossopterygia, and the Podopterygia. They resemble these forms in the muscular bulbus arteriosus of the heart, in the chiasm of the optic nerves, and in the greater distinctness of the metapterygium. The FACTORS OF ORGANIC EVOLUTION two former characters are complexities which the two other divisions do not possess, and which, as descend- ants coming later in time, must be regarded as inferior, and therefore to that extent degenerate. Of these di- visions the Malacopterygia approach nearest the Ho- lostei, and are indeed not distinctly definable without exceptions. The third division, or Acanthopterygia, shows a marked advance beyond the others in : (i) the obliteration of the primitive trachea, or ductus pneu- maticus, which connects the swim-bladder and oeso- phagus ; (2) the advance of the ventral fins from the abdomen forward to the throat ; (3) the separation of the parietal bones by the supraoccipjtal ; (4) the pres- ence of numerous spinous rays in the fins ; and (5) the roughening of the edges of the scales, forming the cten- oid type. There are more or less numerous excep- tions to all of these characters. The changes are all further divergencies from the other vertebrate classes, or away from the general line of ascent of the verte- brate series taken as a whole. The end gained is spe- cialization ; but whether the series can be called either distinctively progressive or retrogressive, is not so clear. The development of osseous spines, rough scales, and other weapons of defense, together with the generally superior energy and tone which prevail among the Acanthopterygia, characterize them as su- perior to the Malacopterygia, but their departure from the ascending line of the Vertebrata has another ap- pearance. The descent of the Acanthopterygian fishes has probably been from Holostean ancestors, both with and without the intervention of Malacopterygian forms. This is indicated by increase in the number of basilar PHYLOGENY. 103 bones1 in the fins of families which have pectoral ven- tral fins, and in the extinct genus Dorypterus.2 The Malacopterygia display three or four distinct lines of descent. The simplest type is represented by the order Isospondyli, and paleontology indicates clearly that this order is also the oldest, as it dates from the Trias at least. In one line the anterior dorsal verte- brae have become complicated, and form an interlock- ing mass which is intimately connected with the sense of equilibrium in the water. This series commences with the Characinidae, passes through the Cyprinidae, and ends with the Siluridae. The arrangements for equilibration constitute a superadded complication, and to these are added in the Siluroids defensive spines and armor. Some of this order, however, are distinctly degenerate, as the soft purblind Ageniosus, and the parasitic Stegophilus and Vandellia, which are nearly blind, without weapons, and with greatly reduced fins. The next line (the Haplomi, pike, etc.) loses the precoracoid arch and has the parietal bones separated, both characters of the Acanthopterygia. This group was apparently abundant during the Cretaceous period, and it may have given origin to many of the Acantho- pterygia. Another line also loses the precoracoid, but in other respects diverges totally from the Acanthopterygia and all other Malacopterygia. This is the line of the eels. They next lose the connection between the scapular arch and the skull, which is followed by the loss of the pectoral fin. The ventral fin disappeared sooner. The palatine bones and teeth disappear, and the suspensor 1 See Cope " On the Homologies of the Fins of Fishes " ; American Nat- uralist, 1890, p. 401. 2 See Proceedings of the American Association for the Advancement of Sci- ence, 1878, p. 297. 104 PRIMARY FACTORS OF ORGANIC EVOLUTION. of the lower jaw grows longer and loses its symplectic element. The opercular bones grow smaller, and some of them disappear. The ossification of most of the hyoid elements disappears, and some of their cartila- ginous bases even vanish. These forms are the marine eels or Colocephali. The most extraordinary example of specialization and degeneracy is seen in the abyssal eels of the family Eurypharyngidae. Here all the de- generate features above mentioned are present in ex- cess, and others are added, as the loss of ossification of a part of the skull, almost total obliteration of the hyoid and scapular arches, and the semi-notochordal condition of the vertebral column, etc. The Acanthopterygia nearest the Malacopterygia have abdominal ventral fins, and belong to several or- ders. It is such types as these that may be supposed to have been derived directly from Holostean ances- tors. They appear in the Cretaceous period (Derce- tidae), along with the types that connect with the Ma- lacopterygia (Haplomi). Intermediate forms between these and typical Acanthopterygii occur in the Eocene (Trichophanes, Erismatopterus), showing several lines of descent. The Dercetidae belong apparently to the order Hemibranchi, while the Eocene genera named belong apparently to the Aphododiridae, the immediate ancestor of the highest Physoclysti, the Percomorphi. The order Hemibranchi is a series of much interest. Its members lose the membrane of their dorsal spinous fin (Gasterosteidae), and then the fin itself (Fistularia, Pegasus). The branchial apparatus has undergone, as in the eels, successive deossification (by retarda- tion), and this in direct relation to the degree with which the body comes to be protected by bony shields, reaching the greatest defect in the Amphisilidae. One PHYLOGENY. 105 more downward step is seen in the next succeeding order of the Lophobranchii. The branchial hyoid ap- paratus is reduced to a few cartilaginous pieces, and the branchial fringes are much reduced in size. In the Hippocampidae the caudal fin disappears and the tail becomes a prehensile organ by the aid of which the species lead a sedentary life. The mouth is much con- tracted and becomes the anterior orifice of a suctorial tube. This is a second line of unmistakable degen- eracy among true fishes. The Acanthopterygia with pectoral ventral fins pre- sent us with perhaps ten important ordinal or subordi- nal divisions. Until the paleontology of this series is better known, we shall have difficulty in constructing phylogenies. Some of the lines may, however, be made out. The accompanying diagram will assist in understanding them. The Anacanthini present a general weakening of the organization in the less firmness of the osseous tissue and the frequent reduction in the size and char- acter of the fins. The caudal vertebrae are of the diphycercal type. As this group does not appear early in geological time, and as it is largely represented now in the abyssal ocean fauna, there is every reason to regard it as a degenerate type.1 The Heterosomata (flounders) found it convenient to lie on one side, a habit which would appear to result from a want of mo- tive energy. The fins are very inefficient organs of movement in them, and they are certainly no rivals for swift-swimming fishes in the struggle for existence, excepting as they conceal themselves. In order to see the better while unseen, the inferior eye has turned in- IThe general characters of the deep-sea fish-fauna are those of degen- eracy. 106 PRIMARY FACTORS OF ORGANIC EVOLUTION. ward, i. e., upward, and finally has penetrated to the superior surface, so that both eyes are on one side. This peculiarity would be incredible, if we did not know of its existence, and is an illustration of the extraordinary powers of accommodation possessed by nature. The Heterosomata (flatfishes) can only be considered a de- generate group. The scyphobranch line presents a PHYLOGENY. 107 specialization of the superior pharyngeal bones, which is continued by the Haplodoci (Batrachidae). This cannot be called a degenerate line, although the fin- rays are soft. The double bony floor of the skull of the distegous percomorph fishes is a complication which places them at the summit of the line of true fishes. At the sum- mit of this division must be placed the Pharyngogna- thi, which fill an important role in the economy of the tropical seas, and the fresh waters of the Southern Hemisphere. By means of their powerful grinding pharyngeal apparatus they can reduce vegetable and animal food inaccessible to other fishes. The result is seen in their multifarious species and innumerable individuals decked in gorgeous colors, and often reach- ing considerable size. This is the royal suborder of fishes, and there is no reason why they should not con- tinue to increase in importance in the present fauna. Very different is the line of the Plectognathi. The probable ancestors of this division, the Epelasmia (Chaetodontidae, etc.), are also abundant in the tropi- cal seas, and are among the most brilliantly colored of fishes. One of their peculiarities is seen in a shorten- ing of the brain-case and prolongation of the jaws downward and forward. The utility of this arrange- ment is probably to enable them to procure their food from the holes and cavities of the coral reefs, among which they dwell. In some of the genera the muzzle has become tubular (Chelmo), and is actually used as a blow-gun by which insects are secured by shooting them with drops of water. This shortening of the basicranial axis has produced a corresponding abbre- viation of the hyoid apparatus. The superior pharyn- geal bones are so crowded as to have become a series io8 PRIMARY FACTORS OF ORGANIC EVOLUTION. of vertical plates like the leaves of a book. These characters are further developed in the Plectognathi. The brain- case is very small, the face is very elongate, and the mouth is much contracted. The bones sur- rounding it in each jaw are coossified. The axial ele- ments (pubes) of the posterior fins unite together, be- come very elongate, and lose the natatory portion. In one group (Orthagoriscidae) the posterior part of the vertebral column is lost, and the caudal fin is a nearly useless rudiment. In the Ostraciontidae (which may have had a different origin, as the pharyngeal bones are not contracted) the natatory powers are much re- duced, and the body is inclosed in an osseous carapace so as to be capable of very little movement. The en- tire order is deficient in osseous tissue, the bones be- ing thin and weak. It is a marked case of degeneracy. There are several evident instances of sporadic de- generacy in other orders. One of these is the case of the family of the Icosteidae, fishes from deep waters off the coast of California. Although members of the Percomorphi, the skeleton in the two genera Icosteus and Icichthys is unossified, and is perfectly flexible. Approximations to this state of things are seen in the parasitic genus Cyclopterus, and in the ribbon-fishes, Trachypteridae. Thus nearly all the main lines of the Acanthopte- rygii are degenerate ; the exceptions are those that terminate in the Scombridae (mackerel), Serranidae, and Scaridae (Pharyngognathi). c. The Line of the Batrachia. We know Batrachia first in the Coal Measures. They reach a great development in the Permian epoch, and are represented by large species in the Triassic PHYLOGENY. 109 period. From that time they diminish in numbers, and at the present day form an insignificant part of the vertebrate fauna of the earth. The history of their succession is told by a table of classification such as I give below : I. Supraoccipital, tabular, and supramastoid bones present. Pro- podial bones distinct. STEGOCEPHALI. Vertebral centra, including atlas, segmented, one set of segments together supporting one arch ; Rhachitomi. Vertebrae segmented, the superior and inferior segments each complete, forming two centra to each arch ; Embolomeri. Vertebral centra, including atlas, not segmented, one to each arch; Microsauri. II. Supraoccipital and supramastoid bones wanting. Frontal and propodial bones distinct ; URODELA. a. An os tabulare. A palatine arch and separate caudal vertebras ; Proteida aa. No os tabulare. A maxillary arch ; palatine arch imperfect ; nasals, pre- maxillaries and caudal vertebrae distinct ; Pseudosauria.1 ' No maxillary or palatine arches ; nasals and premaxil- liary, also caudal vertebrae, distinct ; Trachystomata. III. Supraoccipital, tabular, and supramastoid bones wanting. Frontals and parietals connate ; propodial bones and caudal vertebrae confluent ; SALIENTIA. Premaxillaries distinct from nasals ; no palatine arch ; astragalus and calcaneum elongate, forming a distinct segment of the limb ; Anura. The probable phylogeny of these orders as imper- fectly indicated by paleontology is exhibited in the diagram on the following page. An examination of the above tables shows that there has been in the history of the batrachian class a reduction in the number of the elements composing 1 Includes the Gymnophiona. no PRIMARY FACTORS OF ORGANIC EVOLUTION. the skull, both by loss and by fusion with each other. It also shows that the vertebrae have passed from a notochordal state with segmented centra, to biconcave centra, and finally to ball-and-socket centra, with a great reduction of numbers. It is also the fact that the earlier forms (those of the Permian epoch) show the most mammalian characters of the tarsus and of the pelvis. The later forms, the salamanders, show a more generalized form of carpus and tarsus and of pelvis also. In the latest forms, the Anura, the carpus and tarsus are reduced through loss of parts, except Salientia Traphystomata that the astragalus and calcaneum are phenomenally elongate. We have then, in the batrachian series, a somewhat mixed kind of change ; but it principally consists of concentration and consolidation of parts. The question as to whether this process is one of pro- gression or retrogression may be answered as follows • If degeneracy consists in "the loss of parts without complementary addition of other parts," then the ba- trachian line is a degenerate line. This is only partly true of the vertebral column, which presents the most primitive characters in the early, Permian, genera (Rhachitomi). If departure from the nearest approx- PHYLOGENY. in imation to the Mammalia is degeneracy, then the changes in this class come partly under that head. The scapular and pelvic arches of the Rachitomi are more mammalian than are those of any of their successors ; Fig. 27. — Cricotus crassidiscus Cope, parts of individual represented in Fig. 28; one-third natural size. From Permian of Texas, a, head from above; b, part of belly from below. From Cope. the carpus and tarsus are less so than that of the Anura. There are several groups which show special marks of degeneracy. Such are the reduced maxillary bones PHYLOGENY. 113 and persistent gills of the Protei'da ; the absence of the maxillary bones and the presence of gills in the Trachystomata ; the loss of a pair of legs and feeble- ness of the remaining pair in the same ; and the ex- treme reduction of the limbs in Amphiuma, and their total loss in the Caeciliidae. Such I must also regard, with Lankester, the persistent branchiae of the sire- dons. I may add that in the brain of the protei'd Nec- turus the hemispheres are relatively larger than in the Anura, which are at the end of the line. It must be concluded, then, that in many respects the Batrachia have undergone degeneracy with the passage of time. d. The Reptilian Line. As in the case of the Batrachia, the easiest way of obtaining a general view of the history of this class is by throwing their principal structural characters into a tabular form. As in the case of that class, I commence with the oldest forms and end with the latest in the order of time, which, as usual, corresponds, with the order of structure. I except from this the first order, the Ichthyopterygia, which we do not know prior to the Triassic period : I. The quadrate bone united with the adjacent elements by suture. A. Temporal region of skull with a bony roof ; no postorbital bars. Supramastoid bone present ; an interclavicle ; limbs ambulatory ; Cotylosauria. AA. Cranium with one postorbital bar ; no sternum. (Sy- naptosauria.) a. Paroccipital bone distinct. A supramastoid bone ; ribs two-headed on centrum ; carpals and tarsals not distinct in form from meta- podials ; Ichthyopterygia. ii4 PRIMARY FACTORS OF ORGANIC EVOLUTION. No supramastoid ; sub- and postpelvic ossifications ; in- terclavicle and clavicles separated from and below scapular arch ; ribs one-headed on centrum ; coracoid large, free posteriorly ; Testudinata. aa. Paroccipital bone not distinct. Ribs one or two-headed, capitulum intercentral ; clav- icles and interclavicles forming part of shoulder- girdle ; scapula simple ; pubis and ischium plate-like with small or no obturator foramen ; no sub- or post-pelvic bones ; no supramastoid ; Theromora. Supramastoid present ; ribs one-headed ; scapula trira- diate ; no sternum ; pubis and ischium plate-like ; no sub- or postpelvic bones ; Plesiosauria. AAA. Cranium with two postorbital bars ; a sternum. (Archo- sauria. ) Paroccipital bone not distinct ; no supramastoid. Ribs two-headed ; no interclavicle ; external anterior digits greatly elongate to support a patagium ; Ornithosauria. Ribs two-headed ; no interclavicle ; acetabulum per- forate ; limbs ambulatory ; Dinosauria. Ribs two-headed ; an interclavicle ; acetabulum closed ; feet ambulatory ; Crocodilia. Ribs one headed ; an interclavicle ; acetabulum closed ; feet ambulatory ; Rhynchocephalia. II. The quadrate loosely articulated with the adjacent elements, and only proximally. (Streptostylica. ) One postorbital bar, when present ; a paroccipital ; su- pramastoid not distinct ; ribs one-headed; Squamata. An inspection of the characters of these ten orders, and their consideration in connection with their geo- logical history, will give a definite idea as to the char- acter of their evolution. The history of the class, and therefore the discussion of the question, is limited in time to the period which has elapsed since the Per- mian epoch inclusive, for it is then that the Reptilia enter the field of our knowledge. During this period two remarkable orders of reptiles inhabited the earth, PHYLOGENY. those of the Cotylosauria and of the Theromora. The important character and role of these types may be inferred from the fact that the Cotylosauria are struc- turally nearer to the Batrachia and the Theromora to the Mammalia than any other, and the former presents characters which render it probable that all the other reptiles derived their being from them. The phylogeny may be thus expressed : MAMMALIA Pterosauria Dinosauria Crocodilia X Squamata ! Icbth Sauropterygia Anomodonta Testudinata ylosauri; It is extremely probable that the characters of the posterior parts of the cranium of reptiles, as seen in the osseous bars posterior to the orbit, were derived by a kind of natural trephining of the cranial roof of the primitive order of the Cotylosauria. This order has left remains in the Permian beds of North Amer- ica, South Africa, and Germany. This is the theory of Baur,3and I have rendered it probable by researches on the Permian genera of North America.4 1 Some unknown type of Pythonomorpha will represent the ancestor of the Ophidia, while it is uncertain whether this order originated from the Theriodonta or the Rhynchocephalia. 2 The Theromora include the Pelycosauria, Theriodonta, Anomodonta, and other suborders. 3 American Journal of Morphology , 1889, p. 471. 4 Trans. Amer. Philos. Society, 1892, p. 13 ; American Naturalist, 1892, p. 407. n6 PRIMARY FACTORS OF ORGANIC EVOLUTION. The diagrams on pages 117-119 illustrate the suc- cessive changes in the structure of the posterior region of the skull in the types mentioned. The orders and suborders Pseudosuchia, Rhynchocephalia, Ichthyo- pterygia, Dinosauria, Crocodilia, Sauropterygia, and Testudinata commence at the beginning of Mesozoic time, after the Permian had closed. The Squamata (lizards and snakes) commence, so far as is certainly known, in the later Mesozoic, in the Cretaceous period. The line which terminated in the Lacertilia and Ophidia (Squamata) may have originated directly from the Theriodonta, or it may have descended from the Rhynchocephalia. It departs from the former type in two respects : First, in the loss of the capitular articulation of the ribs, and, second, in the gradual elongation and final freedom of the suspensory bone of the lower jaw (the os quadratum). In so departing from the Theromora, it also departs from the mammalian type. The ribs assume the less perfect kind of attachment which the mammals only exhibit in some of the whales, and the articulation of the lower jaw loses in strength, while it gains in extensibility, as is seen in the develop- ment of the line of the eels among fishes. The end of this series, the snakes, must therefore be said to be the result of a process of creation by degeneration, and their lack of scapular arch and fore limb and usual lack of pelvic arch and hind limb are confirmatory evidence of the truth of this view of the case. Secondly, as regards the ossification of the anterior part of the brain-case. This is deficient in some of the Theromora, the ancestral series, which resemble in this, as in many other things, the contemporary Ba- trachia. The late orders mostly have the anterior walls PHYLOGENY. 117 n8 PRIMARV FACTORS OF ORGANIC EVOLUTION. PHYLOGENY. 119 120 PRIMARY FACTORS OF ORGANIC EVOLUTION. membranous, but, in the streptostylicate series at the end, the skull in the snakes becomes entirely closed in front. In this respect, then, the latter may be said to be the highest or most perfect order. As regards the scapular arch, including the ster- num, no order possesses as many elements as thor- oughly articulated for the use of the anterior leg as the Permian Theromora (excepting in the suborder Pelyco- sauria). In all the orders there is loss of parts, except- ing only in the Ornithosauria and the Lacertilia. In the former the adaptation is to flying. The latter re- tain nearly the theromorous type. An especial side development is the modification of abdominal bones into three pairs of peculiar elements to be united with part of the scapular arch into a plastron, and the in- clusion of the coracoid above them, seen in the Testu- dinata. The pelvic arch has a more simple history. Again, in the Theromora we have the nearest approach to the Mammalia. The only other order which displays sim- ilar characters is the Ornithosauria (Dimorphodon, according to Seeley). In the Dinosauria we have a side modification which is an adaptation to the erect or bipedal mode of progression, the inferior bones be- ing thrown backward so as to support the viscera in a more posterior position in birds. This is an obvious necessity to a bipedal animal where the vertebral col- umn is not perpendicular. And it is from the Triassic Dinosauria that I suppose the birds to have arisen. The main line of the Reptilia, however, departs from both the mammalian and the avian type and loses in strength as compared with the former. In the latest orders, the Pythonomorpha and Ophidia, the pelvis is rudi- mental or absent. PHYLOGENY. 121 As regards the limbs, the degeneracy is well marked. No reptilian order of later ages approaches so near to the Mammalia in these parts as do the Permian Thero- mora. This approximation is seen in the internal epi- condylar foramen and well-developed condyles of the humerus, and in the well-differentiated seven bones of the tarsus. The epicondylar foramen is only retained in later reptiles in the rhynchocephalian Sphenodon (Dollo); and the condyles of the Dinosauria and all of the other orders, excepting the Ornithosauria and some Lacertilia, are greatly wanting in the strong charac- terization seen in the Theromora. The posterior foot seems to have stamped out the greater part of the tar- sus in the huge Dinosauria, and it is reduced, though to a less degree, in all the other orders. In the paddled Plesiosauria, dwellers in the sea, the tarsus and carpus have lost all characterization, probably by a process of degeneracy, as in the mammalian whales. This is to be inferred from the comparatively late period of their appearance in time. The still more unspecialized feet and limbs of the Ichthyosaurus (Ichthyopterygia) can not yet be ascribed to degeneracy, for their history is too little known. At the end of the line, the snakes present us with another evidence of degeneracy. But few have a pelvic arch (Glauconiidae Peters), while very few (Peropoda) have any trace of a posterior limb. The vertebrae are not introduced into the definitions of the orders, since they are not so exclusively distinc- tive as many other parts of the skeleton. They never- theless must not be overlooked. As in the Batrachia, the Permian orders show inferiority in the deficient ossification of the centrum. Many of the Theromora are notochordal, a character not found in any later or- 122 PRIMARY FACTORS OF ORGANIC EVOLUTION. der of reptiles excepting in a few Lacertilia (Gecconi- dae). They thus differ from the Mammalia, whose characters are approached more nearly by some of the terrestrial Dinosauria in this respect. Leaving this order, we soon reach the prevalant ball-and-socket type of the majority of Reptilia. This strong kind of articulation is a need which accompanies the more elongated column which itself results at first from the posterior direction of the ilium. In the order with the longest columrt, the Ophidia, a second articulation, the zygosphen, is introduced. The mechanical value of the later reptilian vertebral structure is obvious, and in this respect the class may be said to present a higher or more perfect condition than the Mammalia. In review it may be said of the reptilian line, that it exhibits marked degeneracy in its skeletal structure since the Permian epoch ; the exception to this state- ment being in the nature of the articulations of the vertebra?. And this specialization is an adaptation to one of the conditions of degeneracy, viz., the weaken- ing and final loss of the limbs and the arches to which they are attached. The history of the development of the brain in the Reptilia presents some interesting facts. In the dia- dectid family of the Permian Cotylosauria it is smaller than in a Boa constrictor, but larger than in some of the Jurassic Dinosauria. Marsh has shown that some of the latter possess brains with relatively very narrow hemispheres, so that in this organ those gigantic rep- tiles were degenerate, while the existing streptostyli- cate orders have advanced beyond their Permian an- cestors. There are many remarkable cases of what may now be safely called degradation to be seen in the contents PHYLOGENY. 123 of the orders of reptiles.1 Among tortoises may be cited the loss of one or two series of phalanges in sev- eral especially terrestrial families of the Testudinidae. The cases among the Lacertilia are the most remark- able. The entire families of the Pygopodidae, the Anniellidae, the Anelytropidae, and the Dibamidae are degraded from superior forms. In the Anguidae, Te- idae, and Scincidae, we have series of forms whose steps are measured by the loss of a pair of limbs, or of from one to all the digits, and even to all the limbs. In some series the surangular bone is lost. In others the eye diminishes in size, loses its lids, loses the folds of the epidermis which distinguish the cornea, and finally is entirely obscured by the closure of the oph- thalmic orifice in the true skin.2 Among the snakes a similar degradation of the organs of sight has taken place in two suborders, which live underground, and often in ants' nests. The Tortricidae and Uropeltidae are burrowing-snakes which display some of the earlier stages of this process. One genus of the true colubrine snakes even (according to Gunther) has the eyes ob- scured as completely as those of the inferior types above named (genus Typhlogeophis.) e. The Avian Line. The paleontology of the birds not being well known, our conclusions respecting the character of their evo- lution must be very incomplete. A few lines of suc- cession are, however, quite obvious, and some of them are clearly lines of progress, and others are lines of re- 1 Such forms in the Lacertilia have been regarded as degradational by Lankester and Boulanger. 2A table of the degenerate forms of Lacertilia is given in the chapter on Catagenesis. 124 PRIMARY FACTORS OF ORGANIC EVOLUTION. trogression. The first bird we know at all completely, is the celebrated Archeopteryx of the Solenhofen slates of the Jurassic period. In its elongate series of caudal vertebrae and the persistent digits of the anterior limbs we have a clear indication of the process of change which has produced the true birds, and we can see that it involves a specialization of a very pronounced sort. The later forms described by Seeley and Marsh from the Cretaceous beds of England and North Amer- ica, some of which have biconcave vertebras, and all probably, the American forms certainly, possessed teeth. This latter character was evidently speedily lost, and others more characteristic of the subclass be- came the field of developmental change. The parts which subsequently attained especial development are the wings and their appendages ; the feet and their envelopes, and the vocal organs. Taking all things into consideration, the greatest sum of progress has been made by the perching birds, whose feet have be- come effective organs for grasping, whose vocal organs are most perfect, and whose flight is generally good, and often very good. In these birds also the circula- tory system is most modified, in the loss of one of the carotid arteries. The power of flight, the especially avian charac- ter, has been developed most irregularly, as it appears in all the orders in especial cases. This is apparent so early as in the Cretaceous toothed birds already mentioned. According to Marsh, the Hesperornithidae have rudimental wings, while these organs are well developed in the Ichthyornithidae. They are well de- veloped among natatorial forms in the albatrosses and frigate pelicans, and in the skuas, gulls, and terns, and are rudimental in their allies, the auks. They are PHYLOGENY. 125 developed among rasorial types in the sand-grouse, and, among the adjacent forms, the pigeons. Then w x Fig. 32. — Archteopteryx lithographica, from the middle Oolite of Bavaria. among the lower Passeres, the humming-birds exceed all birds in their powers of flight, and the swifts and 126 PRIMARY FACTORS OF ORGANIC EVOLUTION. some of the Caprimulgidae are highly developed in this respect. Among the higher or true song birds, the swallows form a notable example. With these high specializations occur some remarkable deficiencies. Such are the reduction of the feet in the Caprimulgidae, swifts, and swallows, and the foetal character of the bill in the same families. In the syndactyle families, represented by the kingfishers, the condition of the feet is evidently the result of a process of degenera- tion. A great many significant points may be observed in the developmental history of the epidermic struc- tures, especially in the feathers. The scale of change in this respect is in general a rising one, though vari- ous kinds of exceptions and variations occur. In the development of the reetrices (tail-feathers) there are genera of the wading and rasorial types, and even in the insessorial series, where those feathers are of prim- itive structure (Menuridae), are greatly reduced, or absolutely wanting. These are cases of degeneracy. There is no doubt that the avian series is in gen- eral an ascending one. f. The Mammalian Line. Discoveries in paleontology have so far invalidated the accepted definitions of the orders of this class that it is difficult to give a clearly cut analysis, especially from the skeleton alone. The following scheme, there- fore, while it expresses the natural groupings and affin- ities, is defective, in that some of the definitions are not without exceptions : * IThis classification of the Mammalia was first published by the writer in the American Naturalist for 1885 ; was improved in the same, 1889 (October;; and appeared in a Syllabus of Lectures of the University of Pennsylvania, July, 1891. PHYLOGENY. 127 I. A large coracoid bone articulating with the sternum. An inter- clavicle (Prototheria). Epicoracoid and marsupial bones ; fibula articulating with proximal end of astragalus : i. Monotremata. II. Coracoid a small process coossified with the scapula (Eutheria). a. Marsupial bones ; palate with perforations (uterus divided ; placenta and corpus callosum rudimental or wanting ; cere- bral hemispheres small and generally smooth). But one deciduous molar tooth : 2. Marsupialia aa. No marsupial bones ; palate generally entire (placenta and corpus callosum well developed). j8. Anterior limb reduced to more or less inflexible paddles posterior limbs wanting (Mutilata). Elbow-joint fixed ; carpals discoid, and with the digits separated by cartilage ; lower jaw without ascending ramus : 3. Cetacea. Elbow-joint flexible ; carpals and phalanges with normal articulations ; lower jaw with ascending ramus : 4. Sirenia. ,3(3. Anterior limbs with flexible joints. Ungual phalanges compressed and pointed1 (Unguiculata). ; . Feet taxeopodous (with exceptions in the carpus), d. Teeth without enamel ; generally no incisors. Limbs not volant ; hemispheres small, smooth : 5. Edentata 66. Teeth with enamel ; incisors generally present. No postglenoid process ; mandibular condyle not trans- verse ; limbs not volant ; hemispheres small, smooth : 6. Glires Anterior limbs volant ; hemispheres small, smooth : 7. Chiroptera A postglenoid process ; mandibular condyle transverse ; limbs not volant ; no scapholunar bone2; hemi- spheres small, smooth : 8. Bunotheria? A postglenoid process ; limbs not volant, with a scapho- lunar bone ; hemispheres larger, convoluted : 9. Carnivora. 1 Except Mesonychiidae. 2 Except Erinaceus and Talpa. 3 With the suborders Pantotheria, Creodonta, Insectivora, and Tillodonta 128 PRIMARY FACTORS OF ORGANIC EVOLUTION. yy. Feet diplarthrous. Limbs ambulatory; a postglenoid process ; molars qua- dri tubercular : 10. Ancylopoda. PPfl. Anterior limbs with flexible joints and distinct digits ; ungual phalanges not compressed and acute at apex l (Un- gulata2). e. Tarsal bones in linear series ; carpals generally in linear series. Limbs ambulatory; teeth with enamel : n. Taxeopoda? ££. Carpal series alternating ; tarsal series linear. Limbs ambulatory ; median digits longest ; teeth with enamel : 12. Toxodontia. £E£. Tarsal series alternating ; carpals linear. Cuboid bone partly supporting navicular, not in contact with astragalus : 13. Proboscidia. eeee. Both tarsal and carpal series more or less alternating. Os magnum not supporting scaphoides; cuboid sup- porting astragalus ; superior molars tritubercular : 14. Amblypoda. Os magnum supporting scaphoides ; superior molars quadritubercular : 4 15. Diplarthra* 1 Except the Hapalidae. 2 Lamarck, Zoologie Philosophique, 1809. 3 This order has the following suborders : Carpal series linear ; no intermedium ; tibia not interlocking with astraga- lus ; no anapophyses ; incisors rooted ; hallux not opposable : Condylarthra, Carpal series linear; an intermedium; tibia interlocking with astragalus; hallux not opposable : Hyracoidea. An intermedium; fibula not interlocking; anapophyses; hallux opposable; incisors growing from persistent pulps : Daubentonioidea. An intermedium; fibula not interlocking; anapophyses; hallux opposable; incisors rooted ; carpus generally linear : Quadrumana. No intermedium ; 6 nor anapophyses ; carpal rows alternating ; incisors rooted : Anthropomorpha.1 The only difference between the Taxeopoda and the Bunotheria is in the unguliform terminal phalanges of the former as compared with the clawed or unguiculate form in the latter. The marmosets among the former division are, however, furnished with typical claws. 4 Except Trigonolestes. fi This order includes the suborders Perissodactyla and Artiodactyla. It is the Ungulata of some authors. 6 Except in Simia and Hylobates. 7 Includes the Anthropoid apes and man. PHYLOGENY. 129 i3o PRIMARY FACTORS OF ORGANIC EVOLUTION. PHYLOGENY. 132 PRIMARY FACTORS CF ORGANIC EVOLUTION. The characters of the skeleton of the order Mono- tremata show that it is nearest of kin to the Reptilia, and many subordinate characters, especially of the extrem- ities, point to the Theromora as its ancestral source.1 In the general characters the Marsupialia naturally follow in a rising scale, as proved by the increasing perfection of the reproductive system. The Monodel- phia follow with improvements in the reproductive system and the brain, as indicated in the table above given. The oldest Monodelphia were, in respect to the structure of the brain, much like the Marsupialia, and some of the existing orders resemble them in some parts of their brain-structure. Such are the Condylar- thra and Amblypoda of extinct groups, and the Buno- theria, Edentata, Glires, and Chiroptera, recent and extinct. The characters of the brains of Amblypoda and some Creodonta are, in their superficial char- acters, even inferior to existing marsupials. The di- vided uterus of the recent forms named, also gives them the position next to the Marsupialia. In the Carnivora, Hyracoidea, and Proboscidia, a decided ad- vance in both brain-structure and reproductive system is evident. The hemispheres increase in size, and they become convoluted. A uterus is formed, and the testes become external, etc. In the Quadrumana and An- thropomorpha the culmination in these parts of the structure is reached, excepting only that, in the lack of separation of the genital and urinary efferent ducts, the males are inferior to those of many of the Artio- dactyla. This history displays a rising scale for the Mammalia.2 1 Proceedings American Philosoph. Society, 1884, p. 43. Antea, p. 87. 2 See the evidence for evolution in the history of the extinct Mammalia Proceedings of the American Association for the Advancement of Science, 1883. PHYLOGENY. 133 Looking at the skeleton, we observe the following successional modifications : First, as to the feet, and (A) the digits. The Con- dylarthra have five digits on both feet, and they are plantigrade. This character is retained in their de- scendants of the lines of Anthropomorpha, Quadru- mana, and Hyracoidea, also in the Bunotheria, Eden- tata, and most of the Glires. In some of the Amblypoda and in the Proboscidia the palm and heel are a little raised. In the Carnivora and Diplarthra the heel is raised, often very high, above the ground, and the number of toes is diminished, as is well known, to two in the Artiodactyla and one in the Perissodactyla. (B) The tarsus and carpus. In the Condylarthra and most of the Creodonta the bones of the two series in the carpus and tarsus are opposite each other, so as to form continuous and separate longitudinal series of bones. This continues to be the case in the Hyracoi- dea and many of the Quadrumana, but in the anthro- poid apes and man the second row is displaced inwards so as to alternate with the first row, thus interrupting the series in the longitudinal direction, and forming a stronger structure than that of the Condylarthra. In the bunotherian, rodent, and edentate series, the tar- sus continues to be without alternation, as in the Con- dylarthra, and is generally identical in the Carnivora. In the hoofed series proper it undergoes change. In the Proboscidia the carpus continues linear, while the tarsus alternates. In the Amblypoda the tarsus alter- nates in another fashion, and the carpal bones are on the inner side linear, and on the outer side alternating. The complete interlocking by universal alternation of the two carpal series is only found in the Diplarthra. (C) As to the ankle-joint. In most of the Condylarthra PHYLOGENY. 135 it is a flat joint or not tongued or grooved. In most of the Carnivora, in a few Glires, and in all Diplar- thra, it is deeply tongued and grooved, forming a more perfect and stronger joint than in the other orders, where the surfaces of the tibia and astragalus are flat. (D) In the highest forms of the Rodentia and Diplar- thra the fibula and ulna become more or less coossified with the tibia and radius, and their middle portions become attenuated or disappear. Secondly, as regards the vertebrae. The mutual articulations (zygapophyses) in the Condylarthra have flat and nearly horizontal surfaces. In higher forms, especially of the ungulate series, they become curved, the posterior turning upward and outward, and the an- terior embracing them on the external side. In the higher Diplarthra this curvature is followed by another curvature of the postzygapophysis upward and out- ward, so that the vertical section of the face of this process is an S. Thus is formed a very close and se- cure joint, such as is nowhere seen in any other Verte- brata. Thirdly, as regards the dentition. Of the two types of Monotremata, the Tachyglossus, and the Platy- pus, the known genera of the former possess no teeth, and the known genus of the latter possesses only a single corneous epidermic grinder succeeding two de- ciduous molars, like those of certain extinct forms, in each jaw. As the theromorous reptiles from which these are descended have well-developed teeth, their condition is evidently one of degeneration. We prob- ably have their ancestors in the Multituberculata, which range from Triassic to lower Eocene time in both hemispheres. In the marsupial order we have a great range of dental structure, which almost epito- 136 PRIMARY FACTORS OF ORGANIC EVOLUTION. mizes that of the monodelph orders. The dentition of the carnivorous forms is creodont ; that of the kan- garoos is perissodactyle, and that of the wombats is rodent. Other forms repeat the Insectivora. I there- fore consider the placental series especially. I have already shown that the greater number of the types of this series have derived the characters of their molar teeth from the stages of the following succession. First, a simple cone or reptilian crown, alternating with that of the other jaw. Second, a cone with an- terior and posterior lateral denticles. Third, the den- ticles rotated to the inner side of the crown below, and outer side above forming with the principal (median) cone a three-sided prism, with tritubercular apex, which alternates with that of the opposite jaw. Fourth, development of a heel projecting from the posterior base of the lower jaw, which, in mastication, meets the crown of the superior, forming a tubercular-sec- torial inferior molar. From this stage the carnivorous and sectorial dentition is derived, the tritubercular type being retained. Fifth, the development of a pos- terior inner cusp in the superior molar, and the eleva- tion of the heel in the inferior molar, with the loss of the anterior inner cusp. Thus the molars become qua- dritubercular, and opposite. This is the type of many of the Taxeopoda, including the Quadrumana and In- sectivora as well as the inferior Diplarthra. The higher Taxeopoda (Hyracoidea) and Diplarthra add various complexities. Thus the tubercles become flattened and then concave, so as to form V's in the section pro- duced by wearing ; or they are joined by cross-folds, forming various patterns, of which the most special- ized is that of the horse. In the Proboscidia the latter PHYLOGENY. 137 Fig- 37-— A Phenacodus primervus, fore and hind limbs ; B, Homo sapiens, fore and hind limbs. 1 38 PR I MAR Y FA CTORS OF OR GANIC E VOL UTION. become multiplied so as to produce numerous cross- crests. . The molars of some of the Sirenia are like that of some of the Ungulata, especially of the tapirine group, while in others the teeth consist of cylinders. In the Cetacea the molars of the oldest (Eocene and Miocene) types are but two-rooted and compressed, having much the form of the premolars of other Mammalia. In ex- isting forms a few have simple conical teeth, while in a considerable number teeth are entirely wanting. g. General Review of the Phytogeny of Mammalia. In the accompanying table some of the characters of the mammalian skeleton above described are thrown into a tabular form. They are exhibited in the order of their appearance in geological time, beginning with the oldest horizon at the bottom of the left-hand col- umn. Continued primitive types are enclosed in brack- ets. These relations were pointed out by me in 1883, ! and every discovery made since that date has confirmed their correctness. Some characters of the Mesozoic Mammalia are now added. Paleontology has cleared up the phylogeny of most of the mammalian orders, but some of them remain as yet unexplained. This is the case with the Cetacea, the Sirenia, and the Edentata. The Marsupialia can be supposed with much probability to have come off from the Monotremata, but there is but little paleon- tological evidence to sustain the hypothesis. Little progress has been made in unravelling the phylogeny 1 Proceedings American Assoc. Adv. Science, p. 40. The successional gra- dation in the limbs and teeth was announced by me in 1873 (Proceeds. Acad- emy Philadelphia, p. 371, and Journal of 'the Academy, 1874, p. 20), and that in the size of the hemispheres of the brain by Marsh in 1874 (American Journal Sci. Arts, p. 66). PHYLOGENY. 139 z" i Hemispheres larger, convo- luted. Hemispheres larger, convo- luted. Hemispheres small ; and larger. Hemispheres small. Hemispheres small ; mesen- cephalon some- times exposed. Meaencephalon exposed ; hemi- spheres small and smoother. CO c "o > c I C | > c | | 2 >> >i >, *** 3 "M "ac x> M c C bC N 0 Q C 35 _a 0 Q 33 ja ft cd C E 35 E T3 T3 •d C G c ! « . •o cd cd cd « T3 nU, m cd - SUPERIO MOLARS ibercles, ested an imented. ibercles, 1 (U ibercles, ested. ibercles. ibercles, ested. ill "o o S « S ° ^ J2 ^ il O U jne crest tubercul tubercul conodon todont. %. u u 4 o • ^- " -r V ° 2 3 «2 £i G H *• w S RADIUS. UNGU- LATA. Faceted. Faceted. Smooth. Smooth. Faceted. Smooth. O 0 E en Smooth. o < 6£ &c (C be si 5 M H C ^ C c c c < s •< en 5 J g!§ IS § aj 8 1 1 to '~r. IM u o 2? 'in O 8 3SI t-i n R- 0 CU o ft, OJ g.1 8, 0 D ^ 0 c G — C ^c S3 ex O < TJ •a T3 — •s O CU CD o > > •^ > > '^ 0 H J X ed g O cd s £ ^j ^j < (4 O E O O C ES E E , same, oblique view, displaying the large cerebral hemispheres. Fig. c, superior view of skull, natural size. Fig. d, inferior view, three-halves natural size. Lower figs, a, b, and c, left branch of lower jaw of Anaptomorphus eemu- lus Cope, twice natural size; a, from left side; b, inner side; c, from above. more or less fused together. These now well-known characteristics of human dentition constitute one of the examples of transition from a simian to a human 1 52 PRIMARY FACTORS OF ORGANIC EVOLUTION. type. I have pointed out a corresponding modifica- tion in the structure of the crown of the superior true molars, viz. : the transition from a quadritubercular to a tritubercular structure in passing from the lower to the higher races. As this point has some interesting im- plications in the earlier phylogeny of man, and as its value has been disputed, I give it a little attention. The facts of the case are as follows : I have dem- onstrated1 the fact that all forms of dentition exhibited by the eutherian mammals have been derived from a primitive tritubercular type. Professor Osborn says that he expects to be able to do the same for the multi- tuberculate (? Prototherian) dentition. I have also shown that man exhibits a tendency to revert from his primitive quadritubercular molar to this tritubercular type.2 As to the significance of these facts, I have expressed the view that this acquisition of a tritubercu- lar molar is a reversion to the lemurine type. This conclusion is necessary because the lemurs are the last of the families in the line of the ancestry of man which present this dentition. The monkeys and anthropoid apes are all quadritubercular, except a few limited col- lateral branches of the former, which still retain the lemurine type. There are also a few collateral types of lemurs which have acquired one or more quadri- tubercular molars, but they are not typical. In many tritubercular mammals, a precocious form or two can be found, which has acquired the fourth tubercle. But the further back we go in time, the fewer they become, until, in the Puerco fauna, of eighty-two species of I Proceeds. Amer. Philos. Soc., Dec., 1883 ; Origin of the Fittest > 1887, pp 245. 347, 359- "^American Journal of Morphology, II., i8B3, p. 7. PHYLOGENY. 153 eutherian mammals, but four have true quadritubercu- lar superior molars. I take this opportunity of saying, however, that re- version is not necessarily a result of heredity. It may be simply a retrogression on a line of advance already laid down. What influence lemurine heredity may have had in the case of man, it is not easy to know. But it must be borne in mind that various forms of degeneracy of molar teeth are possible other than the resumption of the tritubercular type, yet the normal reduction generally presented is just this lemurine and primitive eutherian condition. The simplicity of the elements involved, has something, but not everything, to do with this reversion. Dr. Paul Topinard has made an investigation l of the characters of the crowns of the molars in man, and has reached general conclusions identical with my own. He remarks (p. 665): "It is demonstrated, in conclu- sion, that the teeth of man are, at present, in process of transformation, and that in some future which is re- mote the inferior molars shall certainly be quadri- cuspid, and the superior molars tricuspid. It will be curious to have the statistics as to prehistoric man; unfortunately, their crania are rare, and their molars generally much worn." In the details of his examina- tion, there are some divergencies from my results. Thus he finds the quadritubercular second and third superior molar relatively of more frequent occurrence in Europeans than I did. But the absence of Europeo- Americans from his tables reduces the percentage of trituberculars in the Indo-Europeans. He makes no report of Esquimaux. Had he observed this type, he would have found a higher per cent, of tritubercular ZL'Anthropologze, 1892, p. 641 (Nov., Dec.). i54 PRIMARY FACTORS OF ORGANIC EVOLUTION. upper molars than in any race that he has recorded. He confirms my conclusion as to the high percentage of quadritubercular superior molars in the Malays, Polynesians, and Melanesians. The relation of this fact to phylogeny is to confirm Haeckel's hypothesis of the lemurine ancestry of man. I have advanced the further hypothesis that the An- thropomorpha (which include man and the anthropoid apes) have been derived directly from the lemurs, with- out passing through the monkeys proper. This close association of man with the apes, is based on various considerations. One of them is that the skeleton of the anthropoid apes more nearly resembles that of man in the most important respects than it does that of the monkeys. This is especially true of the verte- bral column, where the anapophyses are wanting in the Anthropomorpha (insignificant rudiments remain- ing on one or two vertebrae, as pointed out by Mivart), while they are well developed in the monkeys and lemurs. The molar teeth of the apes and man resem- ble each other more than either do those of the mon- keys, since they lack the crests which connect the cusps, which are general in the latter. The frequent presence of the tritubercular molar in man suggests the superior claim of the lemurs over the monkeys to the position of ancestor. Another signifi- cant fact pointing in the same direction is the existence of large-brained lemurs with a very anthropoid denti- tion (Anaptomorphidae) in our Eocene beds, which have the dental formula of man and the Old World monkeys and apes. This resemblance is very remarkable, much exceeding that lately observed by Ameghino in certain extinct forms of monkeys in Patagonia, which appear to be ancestors of the existing South American mon- PHYLOGENY. 155 keys (Cebidae), and possibly of the Old World monkeys also. The superior molars of the Anaptomorphus are tritubercular, while the premolars, canines, and in- cisors are essentially anthropomorphous, and rather human than simian. Anaptomorphus is probably at the same time the ancestor of the Malaysian lemurine genus Tarsius, and M. Topinard remarks that Tarsius has as good claims to be regarded as ancestral to Homo as Anaptomorphus. But M. Topinard must be aware that in the existing genus the character of the canine and incisive dentition is very unlike that of the Anaptomorphus and Homo. It is specialized in a different direction. The dentition of Anaptomorphus being so generalized as compared with Tarsius, I sus- pect that its skeleton will be found to present corre- sponding characters. Of course, if it be found here- after to have the foot structure of Tarsius (which I do not anticipate), it cannot be included in the ancestry of the Anthropomorpha. It must be further observed that the ancestral line of the Anthropomorpha cannot be traced through any existing type of Lemuridae, but through the extinct forms of the Eocene period.1 This is on account of the peculiar specialization of the inferior canines, which are incisor-like, and because of the peculiar character of the incisors themselves, in the modern lemurs in the restricted sense. But we have numerous lemurine types of the Eocene of both America and Europe which satisfy the conditions exactly, so far as the den- tition is concerned. These are mostly referable to the family Adapidae. Unfortunately, we do not know the entire skeletons 1 On the Primitive Types of the Orders of the Mammalia Educabilia, 1873, p. 8. 156 PRIMARY FACTORS OF ORGANIC EVOLUTION. of these Eocene lemurs, but as far as we have them (genera Tomitherium and Adapis) they are monkey- like. But we have what is almost as useful, the skel- eton of their Eocene and Puerco ancestors, the Con- dylarthra. I long since pointed out that the latter order (not the genus Phenacodus, as Lydekker has ae pe Fig- 39- — Tomitherium rostratum Cope, one of the Adapidae, mandible, natural size; a, from left side; b, from above. Original, from Report U. S. Geol. Survey Terrs., Vol. III. represented me as saying) must be the ancestors of the lemurs, basing my views expressly on the general structure of the Phenacodus, Periptychus, and Menis- cotherium. The structure of the ungual phalanges of Periptychus is very significant, and even more so is that in Meniscotherium, as recently shown by Marsh, PHYLOGENY. 157 who adopts (without credit) my hypothesis of lemurine affinities of the Condylarthra (which he renames the Mesodactyla). From Condylarthra back to Creodonta is an easy transition, and I have always assumed that the Creodonta were derived from generalized polypro- todont Mursupialia. This view has been entirely confirmed by the recent discoveries of Ame- ghino in Patagonia, where he has found forms whose remains may be referred with equal pro- priety to the one group or the other. M. Topinard has been rather hasty in reaching the marsupial ancestry in suppos- ing that Phenacodus belongs to that order. All the evidence shows that Phenacodus is a generalized ungulate placental. To return to the more im- 1 Jl^ mediate ancestry of man. I ^J fflV m have expressed,1 and now main- tain as a working hypothesis, Jl MV *^at all the Anthropomorpha AH b^B were descended from the Eo w^j^ Cj0 cene lemuroids. In my sys- tem2 the Anthropomorpha in- cludes the two families Homi- nidae and Simiidae. The sole difference between these families is seen in the struc- ture of the posterior foot; the Simiidae having the 1 American Naturalist, 1885, p. 467. 2 Origin of the Fittest, 1887, p. 346, from American Naturalist, 1885, p. 34^, where the classification of the Taxeopoda should be in a foot-note; loc. cit., 1880, October. Fig. 40. — Tomitherium ros- tratum Cope, fore arm, five- sixths natural size. Original, b, ulna; c, radius. 158 PRIMARY FACTORS OF ORGANIC EVOLUTION hallux opposable, while in the Hominidse the hallux is not opposable. This is not a strong character, since it de- pends on a slight differ- ence in the form of the entocuneiform bone. In some vertebrates, as the tree-frogs, the same and similar characters (ge- nus Phyllomedusa) are not regarded as of fam- ily value. It is then highly probable that Homo is descended from some form of the Anthropomorpha now extinct, and probably unknown at present, al- though we do not yet know all the charac- ters of some extinct supposed Simiidae, of which fragments only remain to us. It cannot now be determined whether man and the Simiidae were both de- scended from a genus with opposable hallux, or without opposable , Or Whether from um rostratum Cope, five-sixths natural size; a, ilium; b, femur a genus presenting an original. PHYLOGENY. 159 intermediate character in this respect. This genus was, in any case, distinct from either of the two existing genera of Simiidae, Simia and Hylobates, since these present varied combinations of anthropoid resem- blances and differences, of generic and specific value. Professor Virchow in a late address1 has thrown down the gage to the evolutionary anthropologists by asserting that "scientific anthropology begins with living races," adding "that the first step in the con- struction of the doctrine of transformism will be the explanation of the way the human races have been formed," etc. But the only way of solving the latter problem will be by the discovery of the ancestral races, which are extinct. The ad captandum remarks of the learned professor as to deriving an Aryan from a Negro, etc., remind one of the criticisms directed at the doctrine of evolution when it was first presented to the public, as to a horse never producing a cow, etc. It is well known to Professor Virchow that hu- man races present greater or less approximations to the simian type in various respects. Such are the flat coossified nasal bones of the Bushmen ; the qua- dritubercular molars of the Polynesians ; the flat ilia and prognathous jaws of the " Negro ; the flat shin- bones of various races ; the divergent hallux of some aborigines of farther India, etc. Professor Virchow states that the Neanderthal man is a diseased subject, but the disease has evidently not destroyed his race characters; and in his address he ignores the important and well-authenticated discovery of the man and wo- man of Spy. These observations are reinforced by recent discovery of a similar man by DuBois at Trinil I Popular Science Monthly, January, 1893, p. 373, translated. 160 PRIMARY FACTORS OF ORGANIC EVOLUTION. in the island of Java. To these ancient people I will now devote some space. What had been long suspected is now established, Fig. 42. — Megaladapis madagascariensis Forsyth Major, yz natural size; lemuroid from Plis tocene bed of Madagascar, with tritubercular superior molars. From Forsyth Major. through the discovery and descriptions of Messrs. Fraipont and Lohest of Liege ; viz. that there dwelt in Europe during Paleolithic times a race of men which PHYLOGENY. 161 possessed a greater number of simioid characteristics than any which has been discovered elsewhere. The important discovery in the grotto of Spy of two skele- tons, almost complete, served to unify knowledge of this race, which had previously rested on isolated frag- ments only. These skeletons proved what had been previously only surmised, that the lower jaws of Nau- lette, and of Shipka, and probably the skeleton of Neanderthal, belong to one and the same race. The Fig. 43.— Skull of the man of Spy. From Prof. G. F. Wright's Man and the Glacial Period. From a photograph. simian characters of these parts of the skeleton are well known. These are the enormous superciliary ridges and glabella ; the retreating frontal region ; the thickness of the cranial wall ; the massive mandibular ramus with rudimentary chin, and the large size of the posterior molars. Messrs. Fraipont and Lohest have added other characters to these, viz. : the tibia shorter than in any other known human race ; the sigmoid flexure of the femur ; the divergent curvature of the bones of the fore-arm, and most important, a very 162 PRIMARY FACTORS OF ORGANIC EVOLUTION. peculiar form of the posterior face of the mandibular symphysis, already pointed out by Topinard in the jaw of Naulette. On these characters the following re- marks may be made.1 I. The prominent superciliary crests, which are 1 Archives Beiges de Biologie, VII., 1886, p. 731, Gand. PHYLOGENY. 163 characteristic of the Neanderthal race. No existing race presents such a development, neither the Papu- ans, Australians, nor Negroes of any race. But we find the superciliary crests and underlying sinuses identical in adult female orangs and chimpanzees and young male gorillas. In the female chimpanzees the crests are almost inferior in size to those of the man of Spy. II. The retreating forehead of the two crania of Spy is not found in any existing human race, while it is typical of that of Neanderthal. It is characteristic of female orangs and gorillas and of the young males of both species, and of adult males and female chim- panzees. It appears in existing men in rare and iso- lated cases; [probably as survivals]. III. The prominent transverse superior semicircu- lar crest of the occipital bone is found in existing races among the Fellahs of Africa and the Nigritos. It is characteristic of the Neanderthal skulls, and presents exactly the same characters as the young male and female orang and gorilla and young male and adult female of the chimpanzee. IV. No human race presents the characters of the lower jaw exhibited by those of Spy, Naulette, and Shipka. In this part of their osteology the anthro- poids depart widely from man, the most conspicuous point in the latter being the presence of a chin. Ac- cordingly, the angle formed by the anterior face of the symphysis with the inferior border of the horizontal ramus, is less than a right angle in man, and much more than a right angle in the anthropoids. According to Topinard, this angle in fifteen Parisians is 71.4°; in fifteen African Negroes, 82.2°; in fifteen Neocaledo- nians, 83.9°; in the jaw of Naulette, 94°. In the best 164 PRIMARY FACTORS OF ORGANIC EVOLUTION. preserved jaw of Spy the angle is 107°, if measured from the inferior symphysial border, or 90° if meas- C n M Fig. 45. — Vertical sections of symphysis mandibuli of gorilla (Fig. A), and orang (Fig. B], of chimpanzee (Fig. C), of Spy man No. i (Fig. D), and Spy man No. 2 (Fig. E). From Fraipont and Lohest. ured from the inferior border of the ramus. There is no chin in the jaw of the Spy race, and the large angle approaches without nearly equaling that of the PHYLOGENY. 165 anthropoids. But the posterior face of the symphysis presents the most remarkable peculiarity. In the symphysis of the apes (Fig. 54, A, B, C} the posterior border is a continuous slope from the alveolar border to the inferior margin, interrupted by a slight concav- ity below the middle. In the human jaw this line slopes backward to near the middle, where are situated the small tuberosities for the insertion of the genio- glossal muscles. (B in the accompanying figures.) The surface then slopes rapidly forward to pass into the narrow inferior border of the chin (Fig. 46, Pt G). In the jaws Naulette and Spy the structure is exactly in- termediate between the two, and quite different from both (Fig. 45, D, £). It commences above with a pos- terior slope similar to that of the apes, exhibiting what is called by Topinard " internal prognathism," as it appears in the lower human races. The surface then descends abruptly, forming a vertical concavity, which is bounded a considerable distance below by another protuberance, the insertion of the genioglossal muscles. This concavity is not present in the human symphysis, while it is less developed in the simian. The surface then slopes forward, as in the human sym- physis, but this portion is shorter than in human jaws generally. It is represented by a convex face in the simian jaw. This character, taken in connection with the others cited, goes a long way toward justifying the separation of the Neanderthal race as a distant species, as has been done by some author under the name of Homo neanderthalensis. This name is objectionable but must be retained. To these observations Messrs. Fraipont and Lohest add the following. V. The curvature of the ulna and radius, which T 66 PR IMA RY FAC TORS OF OR G A NIC E VOL UTION. produces a wide interosseous space, is not found in any human race, but is common to the apes. On the con- trary, the shortness of these bones is entirely human. VI. The anterior convexity of the femur, with its round section, is only found among living races among the Nigritos of the Philippine Islands. It is seen in a less degree in femora of Neolithic men, and occasional instances are seen among existing Europeans. It is the normal condition in the apes. VII. The tibia is shorter in its relation to the femur than in any human race, and is more robust than in M Fig. 46. — Sections of symphysis mandibuli of modern Liegois (Fig. F) and of an ancient Parisian (Fig. G). From Fraipont and Lohest. . most of them. This character, with the oval section, while not identical with what is seen in the apes, forms an approximation to it. Messrs. Fraipont and Lohest have pointed out the general characters of the dentition of the man of Spy. They show that the molars increase in size posteriorly to the same extent that they do in the apes, which is the reverse of what is usual in man, where they dimin- ish posteriorly, or, in a few lower races (Australians, etc.), remain equal. They show that the superior mo- lars are all quadritubercular, and that the internal root 168 PRIMARY FACTORS OF ORGANIC EVOLUTION. is distinct in all of them. Through the kindness of M. Lohest I received casts and photographs of these teeth, and I give here figures of the former (Fig. 47), which are more satisfactory than those in the memoir from which I have already quoted so fully, where, in- deed, the grinding faces are not represented at all. The figures accompanying1 show the large size of the last superior molar, which exceeds in its propor- tions those of the corresponding tooth in the chimpan- zee. The fourth tubercle, or hypocone, is especially large. In the male the crowns are more produced posteriorly than in man generally, and remind one of the character seen in the orang. The strong divergence of the internal root of the last molar is shown in No. 2 a, and the corresponding character in a Maori and a Fan from tropical Africa is shown in Nos. 3 and 5 a. The quadritubercular crown of the last superior molar of a Tahitian is shown in No. 4 a ; and the roots, which are exceptionally fused nearly as much as in the typi- cal Indo-European, are shown in No. 4. Dr. Eugene Dubois of the Army of the Netherlands has recently published in Batavia, Java, in a brochure in quarto, an account of some bones of an interesting quadrumanous mammal allied to man, which were found in a sedimentary bed of material of volcanic ori- gin of probably Plistocene age, near a village called Trinil. The remains consist of a calvarium which in- cludes the supraorbital ridges and a part of the occi- put ; a last superior upper molar, and a femur. The tooth was found close to the skull and belongs probably to the same individual as the latter, while the reference of the femur is more uncertain, as it was found some fifty feet distant. IFrom The American Naturalist, April, 1893. PHYLOGENY, 169 The characters of the skull are closely similar to those of the men of Neanderthal and of Spy, but the walls are not so thick as those of the former, and more nearly resemble those of the latter. The frontal region is, therefore, much depressed, and it is also much con- stricted posterior to the postorbital borders. The su- tures are obliterated. Dr. Dubois states that the cranial capacity is just double that of the gorilla, and two-thirds that of the lowest normal of man, bridging the gap which has long separated the latter from the apes. Thus the capacity of the former is 500 cubic centime- tres, and the latter is 1500 cubic centimetres. In the Java man the capacity is 1000 cubic centimetres. The last upper molar has widely divergent roots, as in apes and inferior races of man, and the crown is large, with the cusps not clearly differentiated, showing a character commonly observed in the lower molars of the gorilla. The femur is. long, straight, and entirely human. This discovery of Dr. Dubois adds to our knowledge of the physical characters of the Paleolithic man, and espe- cially to his geographical range. As regards the proper appellation of this being, Dr. Dubois is not happy. He proposes for him a new genus Pithecanthropus (after Haeckel), and even a new family, Pithecanthropidae, without having shown that he is not a member of the genus Homo. It is not certain that he is not an individual of the species Homo ncanderthalensis. His cranial capacity is less, it is true, than that of the man of Spy, but Virchow has pointed out that some of the Nigritos possess a remark- ably small cranial capacity, as little as 950 cubic centi- metres, and an inhabitant of New Britain only 860 cubic centimetres, a capacity even smaller than that of the man of Trinil. Until we learn the characters of 170 PR f MARY FACTORS OF ORGANIC EVOLUTION. the lower jaw of the latter we shall be in doubt as to whether this individual pertains to the Homo sapiens or the Homo neanderthalensis. The characters of the dentition, cranium, and limbs which have been observed in the Paleolithic man, are not without parallel in existing races, though the char- acters do not generally occur together in the latter. The supposition that all the Paleolithic men so far found are all pathological subjects is not a probable solution of the question, although this type was no doubt subject to pathological conditions such as have been found in the leg-bones of the men of Neanderthal and Trinil. The characters of the symphysis of the lower jaw are quite sufficient to separate the Neander- thal man as a distinct species of the genus Homo.1 This character is not pathological but it is zoological, and places that species between Homo sapiens and the apes. In conclusion, it may be observed that we have in the Homo neanderthalensis a greater number of simian characteristics than exist in any of the known races of the Homo sapiens, although, so far as known, he be- longs to the genus Homo. The posterior foot, so far as preserved, indicates this to be the case. The foot- character, which distinguishes the genera Homo and Simia still remains. There is still, to use the language of Fraipont and Lohest, " an abyss " between the man of Spy and the highest ape ; though, from a zoological point of view, it is not a wide one. The flints which were discovered in the stratum of cave deposit containing the human remains, are of the Paleolithic type known as Mousterien in France, which IThis view was first insisted on in an article on the Genealogy of Man in the American Naturalist, 1893, p. 331. PHYLOGENY. 171 are of later origin than the Chelle"en or older Paleo- lithic. The older Paleolithic man is not yet known. It is interesting to observe that these flints (Mouste- rien) are of the same form as the obsidian implements which I collected at Fossil Lake, in Oregon, with the bones of extinct llamas, horses, elephants, sloth, etc. The animals which accompanied the man of Spy are, Ccelodonta antiquitatis (wooly rhinoceros), Equus ca- ballus, Cervus elaphus, Cervus tarandus, Bos primigenius, Elephas primigenius, Ursus spelceus, Meles taxus, Hyaena spelcea ; five extinct and four existing species. As the evidence now stands, the most primitive and simian of human races inhabited the Old World. No trace of the Homo neanderthalensis has been found in America. As, however, Paleolithic implements are found in all continents, we may anticipate that this or some similar species of man will be discovered there also. The genealogy of man may be then represented as follows : CLASS & BRANCH Mammalia Reptilia Batrachia Pisces ORDER AND FAMILY. Hominidae Simiidae Adapidae Condylarthra Creodonta Marsupialia polyprotodontia Monotremata Theromora Batrachia Stegocephali Teleostomi Rhipidopterygia Elasmobranchii Ichthyotomi GEOL. SYSTEM Plistocene Neocene Eocene Cretaceous Jurassic Triassic • Carbonic Carbonic Agnatha Cephalochorda Leptocardii Vermes x Coelenterata * Protozoa * 1 Subordinate type not specified. 1 72 PRIMARY FACTORS OF ORGANIC EVOLUTION. 3. THE LAW OF THE UNSPECIALIZED. The facts cited in the preceding parts of this chap- ter show that the phylogenetic lines have not been continuous, but that they may be represented by a system of dichotomy. Jn other words, the point of departure of the progressive lines of one period of time has not been from the terminal types of the lines of preceding ages, but from points farther back in the series. Thus it is not the highly developed or spe- cialized plants which have given origin to the animal kingdom, but the lowest forms or Protophyta, which are not distinguishable from the Protozoa. Among animals it is not the specialized Arthropoda or Mol- lusca which present the closest affiliations with the Vertebrata, but the simple Vermes or Tunicata, from which the origin of the latter may be traced. In the Vertebrata it is not the higher fishes (Actinopterygia) which offer the closest points of affinity to the succeed- ing batrachian class, but that more generalized type of the Devonic period, the Rhipidopterygia, which probably occupies that position. The modern types of Batrachia (Urodela, Salientia) have plainly not fur- nished the starting-point for the reptiles, but the an- cient order of the Stegocephali, which are also fish- like, is evidently their source. The Reptilia of the Permian present us with types with fish-like vertebrae (Cotylosauria, Pelycosauria), from which the class Mammalia may be distinctly traced. The later reptiles diverged farther and farther from the mammalian type with the advance of geologic time. The same prin- ciple has been found to be true in tracing the history PHYLOGENY. 173 of the subdivisions of the great classes, in the preceding section. Agassiz and Dana pointed out this fact in taxon- omy, and I expressed it as an evolutionary law under the name of the "Doctrine of the Unspecialized." This describes the fact that the highly developed, or specialized types of one geologic period have not been the parents of the types of succeeding periods, but that the descent has been derived from the less spe- cialized of preceding ages. No better example of this law can be found than man himself, who preserves in his general structure the type that was prevalent dur- ing the Eocene period, adding thereto his superior brain-structure. The validity of this law is due to the fact that the specialized types of all periods have been generally in- capable of adaptation to the changed conditions which characterized the advent of new periods. Changes of climate and food consequent on disturbances of the earth's crust have rendered existence impossible to many plants and animals, and have rendered life pre- carious to others. Such changes have been often espe- cially severe in their effects on species of large size, which required food in large quantities. The results have been degeneracy or extinction. On the other hand plants and animals of unspecialized habits have survived. For instance, plants not especially restricted to definite soils, temperatures, or degrees of humidity, would survive changes in these respects better than those that have been so restricted. Animals of om- nivorous food-habits would survive where those which required special foods, would die. Species of small size would survive a scarcity of food, while large ones would perish. It is true, as observed by Marsh, that 174 PRIMARY FACTORS OF ORGANIC EVOLUTION. the lines of descent of Mammalia have originated or been continued through forms of small size. The same is true of all other Vertebrata. It is not to be inferred from the reality of the law of "the unspecialized" that each period has been de- pendent on the simplest of preceding forms of life for its population. Definite progress has been made, and highly specialized characters have been gradually de- veloped, and have passed successfully through the vicissitudes of geologic revolutions. But these have not been the most specialized of their respective ages. They have presented a combination of effective struc- ture with plasticity, which has enabled them to adapt themselves to changed conditions. In a large number of cases in each geologic age forms have been successful in the struggle for existence through the adoption of some mode of life parasitic on other living beings. Such habits reduce the struggle to a minimum, and the result has been always degen- eracy. In other cases it is to be supposed that ex- tremely favorable conditions of food, with absence of enemies, would have occurred, in which the struggle would have been almost nil. Degeneracy would fol- low this condition also. On the other hand, extreme severity of the struggle cannot have been favorable to propagation and survival, so that here also we have a probable cause of degeneracy. Degeneracy is a fact of evolution, as already remarked, and its character is that of an extreme specialization, which has been, like an overperfection of structure, unfavorable to sur- vival. In general, then, it has been the "golden mean" of character which has presented the most favorable condition of survival, in the long run. CHAPTER III.— PARALLELISM. IT IS now generally recognized that the successive types of organic beings present characters which are traversed in the embryonic life of those which at- tain the greatest complexity of development, and which occupy the highest places in the scale of life. This fact was observed by the early embryologists, as Von Baer and Agassiz, who did not admit its bearing on the doctrine of evolution. But Darwin and Spencer understood its significance, and Haeckel, Hyatt, and the writer applied it directly to the explanation of phy- logeny. At the present time one of the chief aims of the science of embryology is to discover the record of the history of the past, recapitulated in the stages of embryonic life, and to unravel the phylogenesis of plants and animals by this method. The utility of these researches is attested by the results which they have attained, though for obvious reasons, these are not as definite and conclusive as those which are de- rived from paleontology. The general conclusion is however justified, i. e., that the records of embryology and paleontology are closely similar, and that any dis- cordance between them may be explained on compre- hensible principles. 176 PRIMARY FACTORS OF ORGANIC EVOLUTION. A number of illustrations of the parallelism be- tween taxonomy, ontogeny, and phylogeny may now be given. i. PARALLELISM IN THE BRACHIOPODA. For the following abstract I am indebted to Mr. C. E. Beecher of New Haven, whose excellent work in this field is well known. The parallelism between the ontogeny and phy- logeny in the Brachiopoda has been worked out in numerous instances.1 To illustrate these, some more or less familiar genera may be taken as characteristic ex- amples. Lingula has been shown by Hall and Clarke (Pa/. New York, Vol. VIII., 1892) to have had its inception in the Ordovician. In the ontogeny of both recent and fossil forms, the first shelled stage has a straight hinge line, nearly equal in length to the width of the shell. This stage may be correlated with the more ancient genus Paterina from the lowest Cambrian. Subsequent growth produces a form resembling Obolella, a Cam- brian and Ordovician genus. Then the linguloid type of structure appears at an adolescent period, and is completed at maturity. Thus, Lingula has ontogenetic stages corresponding to (i) Paterina, (2) Obolella, and (3) Lingula, of which the first two occur as adult forms in geological formations older than any known Lin- gula. Paterina represents the radicle of the brachiopods. 1C. E. Beecher, "Development of the Brachiopoda," Part I., Introduc- tion, Amer. Journ. Sci., Vol, XLI., April, 1891 ; " Development of the Brachio- poda," Part II., Classification of the Stages of Growth and Decline, Amer. Jour. Sci., Vol. XLIV., August, 1892 ; "Development of Bilobites," Amer. Jour. Sci., Vol. XLII., July, 1891 ; " Revision of the Families of Loop-bearing Brachiopoda," Trans. Conn. Acad. Sci., Vol. IX., May, 1893. PARALLELISM. 177 It shows no separate stages of growth in the shell, is found in the oldest fossiliferous rocks, and corresponds to the embryonic shelled condition (protegulum) of other brachiopods. The genus Orbiculoidea of the Discinidae first ap- pears in the Ordovician and continues through the Mesozoic. The early stages in the ontogeny of an in- dividual are as in Lingula, first a paterina stage, fol- lowed by an obolella stage. Then from the mechan- ical conditions of growth a Schizocrania-like stage follows, and completed growth results in Orbiculoidea. The elongate form of the shell in Lingula, as well as in many other genera, is determined by the length of the pedicle and freedom of motion. The discinoid or discoid of Orbiculoidea and Discinisca among the brachiopods, and Anomia among pelecypods, is deter- mined by the horizontal position of the valves, which are attached to an object of support by a more or less flexible, very short organ, a pedicle or byssus, without calcareous cementation. This mode of growth is char- acteristic of all the discinoid genera, but, as already shown, the early stages of Paleozoic Orbiculoidea have straight hinge lines and marginal beaks, and in the adult stages of the shell the beaks are usually subcen- tral and the growth holoperipheral. This adult disci- noid form, which originated and was acquired through the conditions of fixation of the animal, has been ac- celerated in the recent Discinisca, so that it appears in a free-swimming larval stage. Thus, a character ac- quired in adolescent and adult stages of Paleozoic spe- cies through the mechanical conditions of growth, ap- pears by acceleration in larval stages of later forms before the assumption of the condition of fixation which first produced this character. 178 PRIMARY FACTORS OF ORGANIC EVOLUTION. The two chief subfamilies of the Terebratellidae undergo complicated series of metamorphoses in their brachial structure. Generic characters are based upon the form and disposition of the brachia and their sup- ports. The highest genera in one subfamily, which is austral in distribution, pass through stages correlated with the adult structure in the genera Gwynia, Cistella, Bouchardia, Megerlina, Magas, Magasell, and Terebra- tella, and reach their final development in Magellania and Neothyris. The higher genera in another subfam- ily, boreal in distribution, pass through metamorphoses correlated with the adult structures of Gwynia, Cistella, Platidia, Ismenia, Miihlfeldtia, Terebratalia, and Dal- lina. The first two stages in both subfamilies are re- lated in the same manner to Gwynia and Cistella. The subsequent stages are different except the last two, so that the Magellania structure is similar in all respects to the Dallina structure, and Terebratella is like Tere- bratalia. Therefore Magellania and Terebratella are respectively the exact morphological equivalent to, or are in exact parallelism with Dallina and Terebratalia. The stages of growth of the genera belonging to the two subfamilies Dallininae and Magellanimae are further correlated in the accompanying tables. The simplest genus Gwynia, as far as known, passes through no brachial metamorphoses, and has the same structure throughout the adolescent period, up to and including the mature condition. In the ontogeny of Cistella the gwyniform stage, through acceleration, has become a larval condition. In Platidia, the cistelliform structure is accelerated to the immature period, and in Ismenia (representing an ismeniform type- of struc- ture in the higher genera), the gwyniform and cistelli- form stages are larval, and the platidiform represents ? — R 5 c 7 v K a i O S f r; ^ 2 1 CO B- S" o M § i M n n 3Q §: S* ^ c *< CO ft; ~ 5. H ? 0s O n d B CO 1 n S a ora H CO H ^ c"' o" •-! O s- i 3 en |! — a 0 TO ^ a — £. *3 CO | ^ i. II' O = 3 3 S E ^ 3 f 2. " ^ - <§ E 2L *3 • CO «i 2. p Ei S^ H 5' o" a |i O n en ^t B ^ - s — 2. TO $ w S 0»5 39 o B O £. *3 ^ cL ^ — K 1 i 1 B* a § ^ o H CO B i ^ 533 — n orq W sa « en' ^ 35 JQ 3XJ - - - n ~ re "g CO S g H-. pg 5 §•' H ?. o1 H. SB q 3 3 H. z = O *i i3 O H en n 333 ~ n STQ * I p w re u; O. i S O — |'| CO re re — ET. a If O — ? 3 ? — 3 s s o" E i — r i S z. P 5 c_ •"- ^d 3 1 E, PI n 5 o o I 1 gwynifoi T; CO o B i ft *£ o -" 3 $ &" | 5 o i B s S 2. S "9 | R* 2_ 1 STAGES Ismenia platidifo cistellifo i CO I E i B n CD 1 E g o ~ 3 *• n CO ^ r_ a ^, 1 i i ^ B | 5 E -: B- ~ n S* OQ 1 •T ~ E.' ~ g_ CO ^. E! c5 ? ~' ^ Jj 1 i B i E o S E £ 5: § terebra mUhlfe 5* = 9 B Ei cistellil ?" = CO ^ a ? •T z' x ^ i E i E o 3 E E i8o PRIMARY FACTORS OF ORGANIC EVOLUTION. an adolescent condition. Similar comparisons may be made in the other genera. Progressively through each series, the adult structure of any genus forms the last immature stage of the next higher, until the highest member in its ontogeny represents serially, in its stages of growth, all the adult structures, with the larval and immature stages of the simpler genera. It is evident that in the identification of specimens belonging to the Terebratellidae, whether recent or fossil, the strict specific characters must be given first consideration. Species, therefore, must be based upon surface orna- ments, form, and color, within certain limits, and gen- era only upon structural features developed through a definite series of changes; the results of which are per- manent in individuals evidently fully adult. In each line of progression in the Terebratellidae, the acceleration of the period of reproduction, by the influence of environment, threw off genera which did not go through the complete series of metamorphoses, but are otherwise fully adult, and even may show re- versional tendencies due to old age ; so that nearly every stage passed through by the higher genera has a fixed representative in a lower genus. Moreover, the lower genera are not merely equivalent to, or in exact parallelism with the early stages of the higher, but they express a permanent type of structure, as far as these genera are concerned, and after reaching ma- turity do not show a tendency to attain higher phases of development, but thicken the shell and cardinal pro- cess, absorb the deltidial plates, and exhibit all the evidences of senility. 182 PRIMARY FACTORS OF ORGANIC EVOLUTION. 2. PARALLELISM IN THE CEPHALOPODA. Among Mollusca it is well known that the Cepha- lopoda form a number of series of remarkable regular- ity, the advance being, in the first place, in the com- plication of the folds of the external margins of the septa, and, in the second place, in the degree of invo- lution of one or both extremities of the shell to the spiral ; third, in the position of the siphon. Alpheus Hyatt, in an important essay on this sub- ject,1 points out that the less complex forms are in many cases identical with the undeveloped conditions of the more complex. He says: " There is a direct connection between the position of a shell, in the com- pleted cycle of the life of this order, and its own de- velopment. Those shells occupying the extremes of the cycle" (in time), "the polar forms, being more embryonic than the intermediate forms. The first epoch of the order is especially the era of rounded, and, in the majority of the species, of unornamented shells with simple septa ; the second is the era of or- namentation, and the septa are steadily complicating; in the third the complication of the septa, the orna- mentation, and the number of species, about twice that of any other epoch, all combine to make it the zenith of development in the order ; the fourth is dis- tinguishable from all the preceding as the era of re- trogression in the form, and partially in the septa. "The four periods of the individual are similarly arranged, and have comparable characteristics. As \Metnoirs of the Boston Society for Natural History, 1866, p. 193. Hyatt was followed by WQrtenberger in Ausland, 1873, who entirely confirmed his conclusions. PARALLELISM. 183 has been previously stated, the first is rounded and smooth, with simple septa ; the second tuberculated, and the septa more complicated; the third was the only one in which the septa, form, and ornamentation simultaneously attained the climax of individual com- plication; the fourth, when amounting to anything more important than the loss of a few ornaments, was marked by a retrogression of the whorl to a more tabu- lar aspect, and by the partial degradation of the septa." I am indebted to Professor Hyatt for the following more detailed account of the results of his researches in this interesting field. The evidence as to the na- ture of evolution derived from the Cephalopoda is more complete than that obtained from any other source. "Every group of nautiloids passes through, during its evolution in time, either a part or the whole of a certain series of changes. These modifications con- sist : first, of a straight or nearly straight cone, ortho- ceran ; second, a curved cone, cyrtoceran ; third, a coiled cone, gyroceran, which does not come in con- tact at any point; fourth, a coiled cone, nautilian, which does come in contact at the termination of the first vo- lution and then during further growth remains in about the same condition, all of the internal whorls being visible as in a flat coil of rope ; fifth, a coiled cone, involute-nautilian, which also comes in contact like the fourth but then the whorl growing with greater rapidity spreads internally, covering up more or less of the internal volutions sometimes to such an extent that even the centre is concealed from view. The ex- amples which I have myself seen of the fifth kind range from the Silurian to the Nautili of the existing fauna, some being present in every period, and of other kinds, the first, second, and third kinds die out gradually, 184 PRIMARY FACTORS OF ORGANIC EVOLUTION. diminishing in the Devonian and Carboniferous and ultimately ceasing their existence altogether in the Trias. The fourth ceases in the Cretaceous, and the fifth alone survives in the Tertiaries and is still living in the Nautilus umbilicatus and pompilus, and two other species. "Wherever found, the young of shells of the fifth kind are at first orthoceran or cyrtoceran like the first and second kind, then gyroceran in curvature like the third class, and then they become more or less rapidly nautilian like the fourth class in succeeding stages. In Silurian, Devonian, and Carboniferous forms this suc- cession is so marked that about all of the young shells of the fifth class may be described as palingenetic, that is as cyrtoceran, gyroceran, nautilian, and then involute-nautilian in their individual or ontogenetic development. In the Trias, Jura, Cretaceous, Ter- tiary, and present, as the fifth class increases in num- bers, there is a decided tendency to shorten and su- persede the gyroceran or third stage and introduce the fourth kind or the tendency to spread by growth in- wards, at earlier stages. "The characteristics of the sutures are correlative with these stages of development, and it may be said in a general way, that all other characteristics corre- late more or less when studied comparatively in dif- ferent series with the differences in the curvature and coiling of the whorls. The curvature and amount of involution is therefore the most important single char- acteristic of the nautiloids, so far as the comparative study of change by evolution is concerned, whether the whole order be considered statistically as above, i. e. with reference to the existence or non-existence of certain forms orthoceran, cyrtoceran, etc., or gen- PARALLELISM. 185 etically, i. e. with sole regard to the evolution of dis- tinct series which may be traced from their origin to their termination in time. "Of these last there are some in every period trace- able with more or less completeness by gradations of adults back to orthoceran or cyrtoceran ancestors. Of these series of adults, some pass through only the or- thoceran and cyrtoceran modifications, others have the orthoceran, cyrtoceran, gyroceran, and nautilian, but those having the latter and the nautilian- involute are of extreme rarity until the Carboniferous is reached. After this the nautilian shells begin to predominate in every series, ultimately becoming the sole representa- tives of genetic series. "Such series are, of course, frequently so closely parallel that it is possible to follow them, and show they are distinct only by means of certain genetic char- acters, the apertures, the structure of the siphuncle, the sutures and septa, and sometimes, although very rarely, all of these internal characters may show dif- ferences peculiar to some one genetic series in which the regular gamut of forms is passed through in the usual succession. Neglect of the comparative study of the stages of development and decline, and of the obvious parallelisms between these and adults of an- cestral forms, have caused naturalists, notably Bar- rande, to make artificial classifications in which about all straight forms, with the exception of some in which the siphuncles were notably distinct to be classed as Orthoceras, most of second kind as Cyrtoceras, most of the third kind as Gyroceras, most of the fourth and fifth kinds as Nautilus. "To such authors the involute-nautilian forms of the Silurian and the existing fauna were considered to i86 PRIMARY FACTORS OF ORGANIC EVOLUTION. be only specifically distinct, although any prolonged study and comparison of the young would have shown that they were widely separated in development and really only morphic equivalents evolved from entirely distinct ancestors. "A good example of this is the Eudoceratidae1 in- cluding the Silurian and Devonian Eudoceras and Trip- teroceras, and probably gyroceran form Edaphoceras of the Carboniferous and the close-coiled nautilian shells of Endolobus of the Carboniferous. The pe- culiar forms of this series and their remarkable sutures enable the observer to follow the line both in the grada- tions of the adults and by means of the parallelisms of the development. "Another good series easily distinguished by the re- markable sculpture of the shells is Zittelloceras of the Silurian with cyrtoceran forms, and the gyroceran and nautilian Halloceras of the Devonian. "One of the best is Thoraceras, a rough spinous cone of the Silurian, Devonian, and Carboniferous, which has straight and cyrtoceran shells ; the gyroceran Triboloceras of the Carboniferous, and the nautilian shells of Vestinautilus and its allies in the same period. "There is no possible explanation of the parallel- isms of development of these nautilian shells and the adult stages of others except heredity in the same gen- etic series. It is useless to waste time in discussion unless the facts are specifically denied after having been properly reexamined. "When the ammonoids are taken up, it is easy to demonstrate2 by the study of the young of the Gonia- 1 " Genera of Fossil Cephalopods," Proc. Bost. Soc. Nat. Hist,, p. 287. 2 See " Genera of Fossil Cephalopods," Proc. Bost, Soc. Nat. Hist., XXII., 1883, p. 303. PARALLELISM. 187 titinae that they had straight forms among their ances- tors and that these forms have a central siphuncle and suture as among nautiloids. The Devonian Goniati- tinae and some of the Carboniferous forms had also gyroceran forms and loosely coiled nautilian forms, in- dicating an ancestry with similar cones, but at these stages the siphuncle is invariably ventral as in the adults. The young of all of the Ammonitinae, however involute the shell may afterwards become, have an in- variably straight or curved cyrtoceran cone in the apical part, and when they come in contact by growth, the first whorl or whorls are equally invariably open coils like the coils of the fourth grade in nautiloids. The fifth kind of shell, the involute-nautilian, follows in precisely similar succession to what it does in the ontogeny of nautiloids. Farther than this the degree of involution increases according to the species, with age, and the amount of this involution is often an im- portant part of the specific diagnosis. "Among Ammonitinae one finds at once that there are no orthoceran or cyrtoceran shells except among the large group designated by the author as Bactrites. This genus begins early in the Silurian with shells that are not distinguishable from true Orthoceras except by having the siphuncle in adults and later stages close to the venter. Some of these forms have no bulb or protoconch and have a large scar on the apex as in true Orthoceras, others have a calcareous bulb or protoconch on the apex as in true Ammonitinae. There are also open or gyroceran shells in the adults of the genus Mimoceras which are repeated in the young of Anarcestes and other genera of Goniatitinae figured in my 'Embryology of Fossil Cephalopods.'1 1 Bull. Mus. Comp. Zodl., III. 1 88 PRIMARY FACTORS OF ORGANIC EVOLUTION. The shells of the Ammonitinae, however, are of the fourth and fifth kinds almost exclusively, and in fol- lowing out the separate genetic series one has to dis- tinguish the progressive gradations by means of the greater or less amount of involution even in the Go- niatitinae of the Devonian and Carboniferous. "There are also some very remarkable facts show- ing that the coiling is closer in the Mesozoic than in the Paleozoic forms as a matter of hereditary derivation. The young of the Silurian and Devonian forms have the open, slowly coiling whorls figured by Sandberger and Barrande and repeated by myself as referred to above, but the young of all Mesozoic forms are close coiled so far as known. This is shown in the centre of the umbilicus by the perforation or central opening which is extremely large in most of the Paleozoic Go- nititinae but becomes almost obliterated in the true Ammonitinae of the Jura. "In tracing parallels between development of the individual and the series among Ammonitinae it has been found by Branco and the author, that in orna- mented shells the young are first like a nautilus in the sutures, then have a goniatitic stage like the first rep- resentatives of the order of ammonoids in the Paleo- zoic, and that during these stages it is invariably smooth and similar in general form to these same an- cestors. After this nepionic stage is passed through the sutures and the characteristics alter with greater or less rapidity, but the stages show decisive parallel isms with the immediate ancestors of the same genetic series. Some of the best examples of palingenetic de- velopment of this kind, where the later stages of growth present parallels with proximate ancestors, are cited in PARALLELISM. 189 my « Genesis of the Arietidae ' 1 and others have been given by Buckman and Wiirtenburger. "Some of the most remarkable occur in the least expected quarters. As usual, when one has a true law, it leads him into conclusions that are, perhaps, more surprising to himself than to his readers, or to any subsequent investigator. This was certainly my own case in being led to recognise the perfect examples of parallelisms in retrogressive series. Quenstedt and all students since his time agree that the so-called genera Crioceras, Hamites, Ancyloceras, Baculites, forms that are successively more and more uncoiled until in Baculites they are absolutely straight cones, were derived from normal, close-coiled, involute-nau- tilian shells of the Ammonitinae. Their young have been repeatedly shown to be close-coiled and they grade into the normal progressive shells by all of their adult characters. "The ultimate fact in this demonstration has been added by Dr. Amos Brown in the discovery of a close coiled nepionic stage in the straight Baculites of the Cretaceous, the only form whose development had not been ascertained and whose exact relations had not been determined. "It is now admitted by all students of Ammonitinae that these retrogressive groups are not true genera; but that as first demonstrated by Quenstedt, Baculites, Crioceras, etc., are retrogressive stages in the evolu- tion of distinct genetic series and that they do not ex- ist as natural groups of species. In other words, dif- ferent genetic series of the Ammonitinae die out by passing through a series of modifications which are parallel and which are just the reverse of the parallel 1 Smitlison. Contrib., 673, p. 41 et seq. igo PRIMARY FACTORS OF ORGANIC EVOLUTION. series of the orthoceran, cyrtoceran, gyroceran shells with which each distinct complete genetic series of nautiloids arose in time. "While the nautiloids coil up in their progressive evolution and the Ammonitinae increase this coiling up tendency in the primitive and progressive forms of each genetic series, the latter in becoming retrogres- sive reverse the processes of progressive evolution. They become more and more uncoiled, each complete retrogressive series ending with a straight cone. All other characters correlate with this uncoiling and in a general way may be said to degenerate in greater or less proportion to the amount of the uncoiling. To make this extraordinary picture complete it is only necessary to add that these retrogressive series followed out to their ultimate development are distinctly parallel with changes or stages of modification taking place in the senile stages of individuals of the same genetic group. "In old age the highly ornamented shell gradually parts with its spines and other ornaments, the whorls slowly diminish, the involution decreases and even- tually in extreme age it becomes separated from the spiral and completely rounded and smooth. The aper- ture becomes correlatively modified, and also the su- tures. If an old ammonite could have its life pro- longed, it would become Baculites, and the full-grown part of the shell would, in some forms of Lytoceratinae be very similar to the minute nepionic shell of the Ba- culites as described and figured by Dr. Brown. If now the coiled adult part of this imaginary shell were broken off and lost, the straight senile fragment would be re- ferred to the old genus Baculites. The morphic char- acters of the gerontic or old-age stage of ontogeny are PARALLELISM. 191 therefore parallel with the forms evolved in the para- plastic or retrogressive stage of evolution of the phy- lum. In other words, the morphic modifications which may occur as permanent, specific, and generic charac- ters in the adults of retrogressive descendants of any progressive individuals may be predicted from the study of the similar changes that take place in the senile stages of the progressive individuals. As it has been stated by the writer on several occasions, the embryonic, nepionic, and later stages of development up to the adult repeat with greater or less clearness in proportion to their removal in time and organization from the point of the origin of the genetic group to which they belong the permanent characteristic of their ancestors ; the adult gives the existing essential differentials acquired by its own species, genus, and group, being the index according to the time of its oc- currence of the progression or retrogression of its group; the old, in its invariably retrogressive course, indicates the path that must be followed by degraded series after the acme of the group to which the indi- vidual belongs has been reached. This, of course, is a generalized statement of the correlations of the on- togenic cycle and the phylocycle when they occur as in the Ammonitinae, but it will be found eventually that this law is true of all animals to some degree. It is obvious from all past experience that every law of correlation of structures cannot be true in any one group without being found more or less in all organ- isms. I have therefore ventured upon the basis of this and Beecher's, Clarke's, and Schuchert's re- searches among Brachiopoda, corals, and trilobites, Dr. Jackson's among pelecypods, and after the con- firmations by the independent researches of Wurten- i92 PRIMARY FACTORS OF ORGANIC EVOLUTION. burger and Buckman among Ammonitinae, and those of Bather among crinoids, to designate the complete study of the correlations of the ontocycle and phylo- cycle as Bioplastology. Bioplastology is easily sepa- rable from the study of growth, and from that of hered- ity, for which last I have proposed the term Genesi- ology,1 and from that of Ctetology or the study of the origin of acquired characteristics. By properly denn- ing these different branches of research it is practicable to see that bioplastology includes the results of the ac- tion of growth, the laws of growth, as well as those of genesiology and ctetology, but has a field entirely dis- tinct from all of these in so far as it deals essentially with the study of parallelism in all its phases. " The parallelism of the gyroceras with an early stage of all coiled Cephalopoda is represented in Fig. 119 page 410, as illustrative of the inheritance of an ac- quired character. 3. PARALLELISM IN THE VERTEBRATA. Parallels between the ontogeny and phylogeny are well known in the Vertebrata. The primary relations of the Vertebrata are discernible in the successive types of structure of the nervous system, and of the skeleton, but most clearly in those presented by the circulatory system. It is well known that the central organ — the heart, is, in the amphioxus, a straight tube. In the next higher group, the Marsipobranchii (lampreys), it is a bent tube, with a constriction which divides it into two chambers. In the Pisces (fishes) the heart is composed of two chambers related to each other in a reversed longitudinal direction. In the Ba- 1 See Proceedings of the Boston Society of Natural History, 1893, p. 59. PARALLELISM. 193 trachia and Reptilia the cephalad (auricular) division is divided into two chambers by a septum ; while in the birds and Mammalia the caudad division (ventricle) is also so divided, making four chambers in all. The sources of the great vessels which distribute the blood to the body and return it to the heart, dis- play the same successional relation of types. In the Acrania (amphioxus), the Marsipobranchii, and most of the fishes, the vessel (truncus communis) which receives the blood from the central organ, gives off several branches on each side, which are distributed to skeletal bars or arches which are in immediate con- tact with water, which aerates the blood. They then return, and, first sending the carotids anteriorly, unite dorsad to the heart, and form the aorta posteriorly. In the Batrachia, where aerial respiration succeeds to an aquatic one during the life of the animal, the number of the vessels contributing to form the aorta is re duced from five to three in the sucessive types. One of the arches is aborted as an arch, and sends the cir- culating fluid to the modified swim-bladder of the fish, or lung, where it is aerated. This aerated blood is returned to the heart with non-aerated blood from other organs, and the mixture is sent throughout the body. In the reptiles we have essentially the same system, but the aorta-origins are reduced to two, and one, on each side. Next a division of the truncus com- munis ensues, which corresponds functionally with that in the ventricle, so that the impure blood from one auricle is sent into the ventricle (right) which com- municates with the lung ; and the aerated blood is then returned to the other auricle, which pours its contents into the left auricle, which drives it into the aorta, and thus throughout the body. Thus pure or Fig. 49. — Circulatory systems; 1-2, fish; 3-4, batrachian; 5, reptile; 6, bird; all from Gegenbaur. Figs. 7-8, human foetus, from His. PARALLELISM. 195 aerated blood is distributed to the organs, and all but one of the old roots of the aorta have ceased to function as such. This evolutionary succession is preserved with much fidelity in the ontogeny of the respective classes of Vertebrata. The representatives of each class pass through the stages which are permanent in the classes below them in the series. The Mammalia, as the highest class, pass through all the stages. (Fig. 49.) This series coincides also with phylogenetic succes- sion. The order of appearance in time of the Verte- brata is, first Agnatha, then Pisces, Batrachia, Rep- tilia, and Mammalia. In all the details of structure the same relation may be observed. Referring to the illustrations of phylogeny and variation of character described in the preceding pages, many of the characters definitive of natural divisions have been observed to appear in the course of the embryonic life of those types which pos- sess them. Those of greater systematic significance appear earlier, and those of less importance in a tax- onomic sense, later. I select some illustrations of this principle. I have shown that the primitive type of superior molar in the placental Mammalia is tritubercular, the fourth tubercle being added internally and posteriorly in the later forms. Dr. Taeker has recently observed that in the development of the superior molars in the horse, at an early stage the crown is tritubercular, and that the fourth cusp or hypocone is subsequently added, as in the phylogenetic history. As the horse presents the most complex molar among Mammalia, this sur- vival of the record is interesting. In the Artiodactyla and Edentata which lack su- 196 PRIMARY FACTORS OF ORGANIC EVOLUTION. perior incisor teeth, rudiments of them can be found in the early stages. We now know early extinct forms of both of these types where these teeth are permanent throughout life. In the toothless whalebone whales the same phenomenon has been observed. It is well known that the highest deer (Cervidae) add an antler to the simple spike horn in the third year, and an additional antler with each successive year for several years. Also they develop a basal snag of the antler (see Cuvier, Ossem. Fossiles ; Gray, Catal. Brit. Mus.) at the third year. Now a majority of those of the New World (genera Cariacus, Coassus) never develop it except in "abnormal" cases in the most vigorous maturity of the most northern Cariacus (C. virginianus); while the South American Coassus retains to adult age the simple horn of the second year of Cervus. Among the higher Cervidae, Rusa and Axis never assume characters beyond an equivalent of the fourth year of Cervus. In Dama the characters are on the other hand assumed more rapidly than in Cervus, its third year corresponding to the fourth of the latter, and the development in after years of a broad plate of bone, with points, being substituted for the addition ot the corresponding snags, thus commencing another series. Returning to the American deer, we have Blasto- cerus, whose antlers are identical with those of the fourth year of Cariacus. The oldest known deer (Palaeomeryx) have no horns, or they are undivided. Among Batrachia excellent illustrations are fur- nished by the two series of Salientia, the Arcifera and the Firmisternia. PARALLELISM. 197 The'firmisternial structure is a modification of the arciferous, which comes later in the history of growth, and probably also in geological time. During the early stages the Firmisternia have the movable shoul- •is! 3 IS IE! b 1 " Cog \J *< JJ ^ Z$2 o- -s 1 s SL ?? _^ *i» .- M o rs fe £ c ^ &r3. der girdle which characterizes those of the arciferous division, the consolidation constituting a modification superadded in attaining maturity. Furthermore, young Salientia are toothless, and one section of the species of Arcifera never acquire teeth. In these (the Bu- ig8 PRIMARY FACTORS OF ORGANIC EVOLUTION. fonidae) we have a group which is imperfect in two points instead of one. The genera of these salientian suborders exhibited on a preceding page as forming indentical series in five different families (pp. 66-67) are related to each other as developmental stages in the history of the genera that attain the extreme development on each line. For example we select the family Hylidae of* which the terminal genus is Trachycephalus. Nearly allied Fig. 51. — Shoulder girdles of Anura ; a, of the arciferous type (Phyllomedusa bicolor) ; b, Rana temporaria, tadpole with budding limbs; c, do., adult, firrais- ternial type ; b and c from Parker. to it is the genus Osteocephalus, which differs in the normal exostosis of the cranium not involving the derm, as it does in the former. Close to this is Scy- topis, where the fully ossified cranium is not covered by an exostosis. Next below Scytopis is Hyla, where the upper surface of the cranium is not ossified at all, but is a membranous roof over a great fontanelle. Still more imperfect is Hylella, which differs from Hyla in the absence of vomerine teeth. Now, the genus Trachy- cephalus, after losing its tail and branchiae, possesses PARALLELISM. 199 all the characters possessed by the genera Hylella and Hyla, either at or just before the mature state of the latter, as the ethmoid bone is not always ossified in advance of the parietals. It soon, however, becomes a Scytopis, next an Osteocephalus, and finally a Tra- chycephalus. It belongs successively to these genera, for an exhaustive anatomical examination has failed to reveal any characters by which, during these stages, it could be distinguished from these genera. The same succession in development of the genera of the other families is well known, the genus Otaspis of the Bu- fonidse attaining a point beyond any of the others, in the enclosure of its membranum tympani posteriorly by dermoossification. Finally reaching in our review the relations of spe- cific characters, the readers will call to mind that the species of the lacertilian genus Cnemidophorus (page 41) are either striped, spotted, or cross-banded, and that the Lacerta muralis agrees with them in this re- spect. It was also shown that the young of all the species are striped, and that the cross-banded forms pass through not only a striped, but an intermediate spotted stage, before attaining the adult coloration. The young of spotted salamanders are without spots (genera Amblystoma and Salamandra e g.) ; so that unspotted species resemble the young of the spotted. In many species of birds of more or less uni- form patterns of coloration, the young are spotted. In some of these the females remain spotted throughout adult life. In some other species both sexes retain the spotted coloration of the young. The young of most deer are spotted. In the fallow-deer (Axis) the adults retain the spotted coloration, thus resembling the young of most of the species. 200 PRIMARY FACTORS OF ORGANIC EVOLUTION. 3. INEXACT PARALLELISM OR C^ENOGENY. When the early or transitional stage of a higher form is exactly the same as a permanent lower form, the parallelism is said to be "exact." Such is the re- lation of a Cnemidophorus gularis scalar is to a Cnemido- ^phorus gularis gularis as to color characters ; and of an Amblystoma tigrinum to a permanent breeding Siredon lichenoides in characters of higher structural value. When the transitional stage of the higher only re- sembles the lower form in some one or more features, but not in all, the parallelism is said to be "inexact." It is evident that "exact parallelism " can only exist between ancestor and descendant in the same re- stricted line, and can be therefore only demonstrated in the case of the nearest relatives, between which a perfect phylogeny is known. So soon as new subordi- nate characters are assumed, or a change in the order of appearance of characters supervenes, the parallel- ism becomes "inexact," and such is the kind of paral- lelism usually observed. And it is more inexact the more widely removed in relationship are the forms compared. Thus the parallelism between the embryo man with five branchial slits, and the adult shark, is very inexact ; but that between a true fish and a shark is much less inexact. That between a higher and a lower shark is still more exact, and so on. Exact par- allelism in growth is called by Haeckel palingenesis or palingeny. The growth which has, through changes introduced subsequent to the origin of a line of de- scent, become inexact, or "falsified," is termed by the same author caenogenesis or caenogeny. PARALLELISM. 201 The superposition of characters which constitutes evolution, means that more numerous characters are possessed by the higher than the lower types. This involves a greater number of changes during the on- togenetic growth of each individual of the higher type. In other words, characters acquired during the phylo- genetic history are continually assumed by the pro- gressive form at earlier and earlier periods of life. This process has been metaphorically termed by Pro- fessor Alpheus Hyatt and myself "acceleration." All progressive organic evolution is by acceleration, as here described. Retrogressive evolution may be ac- complished by a retardation in the rate of growth of the taxonomic characters, so that instead of adding, and accumulating them, those already possessed are gradually dropped ; the adults repeating in a reversed order the progressive series, and approaching more and more the primitive embryonic stages. This pro- cess I have termed "retardation." Retardation is not however, always exact, even in retracing a true phylo- genetic line, whence in such instances the process may not be correctly described as retardation. Professor Hyatt has applied to such types the term "senile," and gerontic ; and to the resulting condition, the term "senility." His observations on this subject have been made on Mollusca, and principally on the Cephalo- poda, and are of fundamental importance in this con- nection. The history of a type which has passed through a full cycle of life, from its earliest appearance to its ex- tinction, is divided by Haeckel into three stages, viz.: those of its rise ; full vigor, as displayed by predomi- nance of variations and numbers ; and decadence. For these stages he uses the expressions Anaplasis, 202 PRIMARY FACTORS OF ORGANIC EVOLUTION. Metaplasis, and Cataplasis. For the processes which bring about the first and last of these conditions, Pro- fessor Hyatt has used the terms Anagenesis and Cata- genesis. Catagenesis is equivalent to degeneracy and has played an important part in organic evolution. I had used the term previously to Professor Hyatt for the same process, but with a wider application ; ex- tending its use to inorganic nature as well.1 (See Chapter IV. of this book.) Embryology has, however, revealed another series of phenomena which in many instances obscure the simplicity of the problem of ontogeny as presented in the preceding pages. It was the merit of Haeckel to generalize from the facts brought to light by this sci- ence, so as to present the relations which subsist be- tween the primitive stages of all multicellular animals. This is known as the Gastraea theory. He showed that the primitive gastric cavity of all such animals is produced by an invagination of a portion of the sur- face of a primitive sphere or morula, which results from the segmentation of the oosperm. This hollow half-sphere he termed the gastrula, and the theoretical primitive animal which corresponds to it he called the Gastraea. Marine animals very similar to this Gas- traea have been discovered. Haeckel showed, how- ever, that gastrulas are not all alike, since they differ in the extent to which the segmentation of the oosperm may be carried, and the rate of segmentation of differ- ent parts of it. Thus early do inexact parallelisms arise. From this point onwards special peculiarities of the various developmental lines appear, some of which have especial reference to the necessities of em- bryonic life. Hence the trochosphere stage of so many \Origin of the Fittest , p. 422. PARALLELISM. 203 invertebrate forms, and the nauplius and zoaea of the Crustacea. Such are the statoblasts which are resting-stages for the embryos of fresh-water sponges and Polyzoa, and the glochidia of the Unionidae, which are wanting in the marine forms of the same orders. Such are the amnion and allantois of certain Vertebrata and the placenta of certain Mammalia, which have no refer- ence to any structures but their own residua, found in the adults of those animals. A remarkable instance of this state of things ap- pears in the history of the evolution of the insects. It is quite impossible to understand this history without believing that the larval and pupal states of the high- est insects are the results of a process of degeneracy which has affected the middle periods of growth, but not the mature results. The earliest insects are the Orthoptera, which have active aggressive larvae and pupae, undergoing the least changes in their meta- morphosis (Ametabola), and never getting beyond the primitive mandibulate condition at the end. The meta- morphosis of the jawed Neuroptera is little more marked, and they are one of the oldest orders. The highest orders with jaws undergo a marked metamorphosis (Coleoptera, Hymenoptera), the Hy- menoptera even requiring artificial intervention in some instances to make it successful. Finally, the most specialized orders, the suctorial Diptera and Lepidoptera, especially the latter, present us with very unprotected more or less parasitic larval stages, both active and inactive. These animals have evidently de- generated, but not so as to prevent their completing a metamorphosis necessary for purposes of reproduction. As is well known, many imagines (Saturniidae, CEstridae) 204 PRIMARY FACTORS OF ORGANIC EVOLUTION. can perform no other function, and soon die, while in some Diptera the incomplete larvae themselves repro- duce, so that the metamorphosis is never completed. This history is parallel to that proposed by Dohrn to account for the origin of the Ammocoetes larval stage of the Marsipobranchii. He supposes this form to be more degenerate than the corresponding stage of its probable ancestral type in the ancestral line of the Vertebrata. An inactive life in mud is supposed by Dohrn to have been the effective cause. An inactive life on the leaves of plants, or in dead carcases, has probably been the cause of the same phenomenon in the Lepidoptera and Diptera. Thus we have developed an ontogeny within an ontogeny, and a phylogeny within a phylogeny. These facts do not, however, affect the general result in the least. They only show us that the persistent larvae of those animals which possess them, have a history of their own, subject to the same laws of evolution as the adults. It results that in many cases the phy- logeny can only be determined by the discovery and investigation of the ancestors themselves, as they are preserved in the crust of the earth. In all cases this discovery confirms and establishes such definite con- clusions as may be derived from embryology. It is also clear that on the discovery of phylogenetic series it becomes at once possible to determine the nature of defective types. It becomes possible to ascertain whether their rudimental parts represent the begin- nings of organs, or whether they are the result of a process of degeneration of organs once well devel- oped. An excellent illustration of inexact parallelism is to be found on comparison of man with the lower Ver- PARALLELISM. 205 tebrata. I have pointed out1 that in the structure of his extremities and dentition, he agrees with the type of Mammalia prevalent during the Eocene period (cfr. Phenacodus). Hence in these respects he re- sembles the immature stages of those mammals which have undergone special modifications of limbs and ex- tremities, such as Ungulata in which caenogeny has not obliterated the early stages from the embryonic record. These forms are probably extinct. I have also shown2 that in the shape of his head man resem- bles the embryos of all Vertebrata, in the protuberant forehead, and vertical face and jaws. In this part of the structure most Vertebrata have grown farther from the embryonic type than has man, so that the human face may be truly said to be the result of a process of retardation. Nevertheless, in the structure of his ner- vous, circulatory, and for the most part, of his repro- ductive system, man stands at the summit of the Ver- tebrata. It is in those parts of his structure that are necessary to supremacy by force of body only, that man is retarded and embryonic. 5. OBJECTIONS TO THE DOCTRINE OF PARAL- LELISM. An objection to the theory of parallelism in its full sense has been recently put forward by Mr. C. Her- bert Hurst.3 He says, "My object now is to show that in neither case can a record of the variation at any one stage of evolution be preserved in the ontog- eny, much less can the ontogeny come to be a series of 1 " The Relation of Man to the Tertiary Mammalia," Penn Monthly, 1875; Origin of the Fittest, 268. 2 " The Developmental Significance of Human Physiognomy," American Naturalist, June, 1883 ; Origin of the Fittest, 1887, p. 281. ZXatural Science, 1893, p. 195. 206 PRIMARY FACTORS OF ORGANIC EVOLUTION. stages representing in proper chronological order some of the stages of adult structure which have been passed through in the course of evolution." Again: "The early stages of the fish embryo are very like those of the bird embryo. These two do correspond to each other. The statement that the embryonic structure of a bird follows a course which is from beginning to end roughly parallel with, but somewhat divergent from, the course followed by a fish, is borne out by the actual facts. A bird does not develop into a fish and then into a reptile, and then into a bird. There is no fish-stage, no reptile-stage, in its ontogeny. The adult resembles an adult fish only very remotely. Every earlier stage resembles the corresponding earlier stage of the fish more closely. There is a parallelism be- tween the two ontogenies. There is no parallelism be- tween the ontogeny and the phylogeny of either a bird or any other animal whatever. A seeming parallelism will fall through when closely examined." " The promise that this theory gave of serving as the guide to knowl- edge of past history without the labor involved in pale- ontological research, was indeed tempting : and where the royal road to learning has been shown by it, it is not surprising that some zoologists should have entered for the race along this road. To what goal that road has led may be learned by a comparison of the nu- merous theories as to the ancestry of the < Chordata ' which have been put forward by those who have adopted the theory without enquiring as to its valid- ity." I have made this quotation as showing the point of view from which the doctrine of parallelism when in- correctly stated may be assailed. There is truth in the author's accusation that embryologists who have PARALLELISM. 207 not used their results with proper caution, have been frequently led to incorrect and even absurd results. The errors of this class of biologists are mainly due to their ignorance of species in the adult state, and their ignorance of systematic biology or taxonomy. They profess to regard this branch of the science as only suitable for beginners, and as comparatively unim- portant, as compared with their own ; yet one might as well attempt the study of philology without a knowl- edge of alphabets, as to study phylogeny without the knowledge of natural taxonomy. The correct discrim- ination of species, genera, etc., imposes much greater burdens on the faculty of judgment, than does any- thing to be found in any science which includes obser- vation and record only. But Mr. Hurst's statement is somewhat overdrawn, and he does not give embryolo- gists the credit which is due to their theory of recapitu- lation. I think he will find the following, which I wrote in I8721 to be a correct statement of the facts, and a fair induction as to principles. "The smaller the number of structural characters which separate two species when adult, the more nearly will the less complete of the series be identical with an incomplete stage of the higher species. As we compare species which are more and more differ- ent, the more necessarily must we confine the asser- tion of parallelism to single parts of the animals, and less to the whole animal. When we reach species as far removed as man and a shark, which are separated by the extent of the series of vertebrated animals, we can only say that the infant man is identical in its nu- merous origins of the arteries from the heart, and in the cartilaginous skeletal tissue, with the class of / IPenn Monthly, 1872. Origin of the Fittest, 1887, p. 8. 208 PRIMARY FACTORS OF ORGANIC EVOLUTION. sharks, and in but few other respects. But the im- portance of this consideration must be seen from the fact that it is on single characters of this kind that the divisions of the zoologist depend. Hence we can say truly that one order is identical with an incomplete stage of another order, though the species of the one may never at the present time bear the same relation in their entirety to the species of the other. Still more frequently can we say that such a genus is the same in character as a stage passed by the next higher genus ; but when we can say this of species, it is because their distinction is almost gone. It will then depend on the opinion of the naturalist as to whether the repressed characters are permanent or not. Parallelism is then reduced to this definition : that each separate charac- ter of every kind, which we find in a species, repre- sents a more or less complete stage of the fullest growth of which the character appears to be capable. In proportion as those characters in one species are contrasted with those of another by reason of their number, by so much must we confine our comparison to the characters alone, and the divisions they repre- sent; but when the contrast is reduced by reason of the fewness of differing characters, so much the more truly can we say that the one species is really a sup- pressed or incomplete form of the other The denial of this principle by the authorities cited has been in consequence of this relation having been assigned to orders and classes, when the statement should have been confined to single characters, and divisions char- acterized by them. There seems, however, to have been a want of exercise of the classifying quality or power of ' abstraction ' of the mind on the part of the objectors." PARALLELISM. 209 It is nevertheless true that the records brought to light by embryologists are very imperfect, and have to be carefully interpreted in order to furnish reliable evi- dence as to the phylogeny of the species examined. An illustration of this is the fact that the species char- acters appear in many embryos before those which de- fine the order or the family, although it is certain that the latter appeared first in the order of time. Most of the important conclusions as to the phylogeny of Ver- tebrata demonstrated by paleontology have never been observed by embryologists in the records of the spe- cies studied by them. Thus I have shown that it is certain that in the amniote vertebrates the intercen- trum of the vertebral column has been replaced by the centrum ; yet no evidence of this fact has been ob- served by an embryologist. If we could study the em- bryonic development of the vertebral column of the Permian and Triassic Reptilia, the transition would be observed, but in recent forms caenogeny has progressed so far that no trace of the stage where the intercentrum existed can be found. Again I have demonstrated by paleontological evi- dence that the lines* of the ungulate Mammalia origi- nated from a bunodont pentadactyle plantigrade an- cestor ; but embryonic research has failed to discover the preservation of a record of this fact in the ungu- lates at present existing. The embryo of the horse is not pentadactyle, nor even tridactyle, although tri- dactyle horses persisted late in geologic time. Nor has embryonic research demonstrated a four-toed stage in the Bovidae (oxen, etc.), although there is no doubt that they descended directly from an ancestor so characterized. Any number of similar cases might be cited to show the prevalence of inexact parallelism 210 PRIMARY FACTORS OF ORGANIC EVOLUTION. or caenogeny. If we could study the embryology of the many extinct forms of life, the missing stages would all be found, but as we have not the opportun- ity of pursuing this important research, we have to rely on paleontology for our phylogeny. Paleontology is and always will be imperfect, but all that we get is palingeny, or the phylogeny itself, and not an inverted and distorted record of it. CHAPTER IV.— CATAGENESIS. WE HAVE been principally occupied so far with progressive evolution or anagenesis. Reference has, however, been made to retrogressive .evolution or degeneracy, in Chapter III., in describing the evolution of the Vertebrata, and will be in Chapter V., under the caption "Disuse in Mammalia." Degeneracy has, how- ever, played a more important part in creation than would be suspected from these references, and I pro- pose in the present chapter to go more fully into its phenomena, which, in the broadest sense, I have called collectively Catagenesis. As evidence for degeneracy as a factor in evolution we naturally appeal first to examples in the life histo- ries of plants and animals which are known to us; and then examine the records of the past, in the light thus gained, for evidence of degeneracy in vegetable and animal phylogeny. In both directions we are met by an embarras de richesse, and a few conspicuous cases will have to suffice. The parasitic copepod Crustacea undergo a retro- grade metamorphosis, which commences at different periods of the growth history of different genera. Says Claus : "Many parasitic Copepoda, however, pass 212 PRIMARY FACTORS OF ORGANIC EVOLUTION. over the series of nauplius forms [which are traversed by other copepods] and the larva, as soon as hatched, undergoes a moult, and appears at once in the youngest Cyclops form with antennae adapted for adhering, and mouth -parts for piercing. From this stage they under- go a retrogressive metamorphosis, in which they become attached to a host, lose more or less completely the seg- mentation of the body, which grows irregular in shape, cast off their swim- ming feet, and even lose the eye, which was originally pres- ent (Lerndapodd). The males, how- ever, in such cases often remain small Fig. v.-Lerna>abranchialis;a, male ; *, non- and dwarfed, and degenerate female; c, female after fertilization adhere undergoing metamorphosis ; d, do. with egg sacs, , natural size. From Claus. more than One, firmly to the body of the female in the region of the genital opening. In the Lerncea such pigmy males were for a long time vainly sought for upon the very peculiarly shaped body of the large female (Fig. 52), which carries egg-tubes. CA TA GENESIS. 2 1 3 At last it was discovered that the small Cyclops -like males lead an independent life and swim about freely by means of their four pairs of swimming feet, and that the females in their copulatory stage resemble the males, and that it is only after copulation that they (the females) become parasitic and undergo the con- siderable increase in size and modification of form which characterizes the female with egg-tubes." A degeneracy of the females of a remarkable char- acter occurs in the insects of the order Strepsiptera. Here the female during the larval stage, bores its way into the body of a hymenopterous insect and soon un- dergoes a moult. At this time they shed their three pairs of well-developed legs, and become a parasitic maggot, which lives on the body of the host. The males do not undergo this degeneracy but retain the six legs and two pairs of wings common to the class Insecta. A notorious example of degeneracy among the Mol- lusca is offered by the Entoconcha mirabilis. Says J. S. Kingsley : " So greatly has parasitism altered the form of the body, and all of the organs, that the proper position of this form among the gastropods is far from certain, some placing it near Natica. Indeed, were it not for the characters afforded by the young, its posi- tion among the Mollusca would not be suspected. Some thirty years ago [before 1885] Johannes Miiller found in some specimens of Synapta digitata an inter- nal worm-like parasite, attached by one extremity to the alimentary canal, while the other end hung free in the perivisceral cavity." " In one specimen of Syn- apta out of one or two hundred this strange form oc- curs. It is a sac, the upper part bearing the female, and the lower the male reproductive organs, while the 214 PRIMARY FACTORS OF ORGANIC EVOLUTION. centre of the body serves for a while as a broodpouch, the embryos later passing out from an opening at the free end of the body of the parent. The eggs undergo a toler- ably regular develop- ment, producing a velum, shell, andoper- culum, the later stages being found free in the body -cavity of the host." The preceding ex- amples illustrate the degenerating or cata- genetic effect of a parasitic life. We will now observe the cor- responding effect of a sedentary life, which may be called earth- parasitism. As an ex- ample of this I select the well-known case of the lowest of the Vertebrata, the Tuni- cata Fig- 53- — A Synapta digitata with para- sitic Entoconcha ; B, a portion of Synapta, The embryo ascid- with Entoconcha (F) enlarged ; a, point of • i .1 r r attachment ; b, blood vessels ; /, female por- tion ; *', intestine; m, male portion ; me, me- a tadpole-like larva sentery. From Kingsley. actiyely through the sea by vibrating its long tail. After a short free-swimming existence the fully developed, tailed larva fixes itself by its anterior adhering papillae CA TA GENESIS. 2 1 5 to some foreign object, and then undergoes a remark- able series of retrogressive changes, which convert it into the adult ascidian. The tail atrophies, until noth- ing is left but some fatty cells in the posterior part of the trunk. The adhering papillae disappear and are replaced functionally by a growth of the test over neigh- boring objects. The nervous system with its sense- organs atrophies, until it is reduced to the single small ganglion placed on the dorsal edge of the pharynx, and a slight nerve-cord running for a short distance posteriorly. Slight changes in the shape of the body and a further growth and differentiation of the branchial sac, peribranchial cavity, and other organs now pro- duce gradually the structure found in the adult ascid- ian (Herdman). It is, however, to be noted that in the order Larvacea, this retrograde metamorphosis does not take place. It embraces the single family Appendiculariidae, which includes Tunicata which pre- serve the tail, notochord, and other larval features, and lead a free-swimming existence in the ocean. On the Tunicata, Herdman makes the following general observations. " (i) In the ascidian embryo all the more important organs (e. g. notochord, neural canal, archenteron) are formed in essentially the same manner as they are in amphioxus and other Chordata. (2) The free-swimming tailed larva possesses the es- sential characters of the Chordata, inasmuch as it has a longitudinal skeletal axis (the notochord), separat- ing a dorsally placed nervous system (the neural canal) from a ventral alimentary canal (archenteron) ; and therefore during this period of its life history the ani- mal belongs to the Chordata. (2) The Chordata larva is more highly organized than the adult ascidian, and therefore the changes by which the latter is produced DlPLOGLOSSA LEPTO Pygopodidae Zonuridae Anguidae Teidse Gerrhosauridae I. Limbs, two pair a. Digits 5-4 Tejus b. Digits 4-5 Tretioscineus Micrablepharus Gymopthalmus c. Digits 4-4 Sauresia Scolecosaurus Saurophis d. .Digits 4-3 • e. Digits 3-4 /. Digits 3-3 Microdactylus g. Digits 3-2 Herpetochalcis h. Digits 2-4 /'. Digits 2-3 >. Digits 2 2 £. One or both monodactyle Chamaesaura Panolopus Cophias Ophiognomon Caetia II. Fore limbs only Propus (digits o> III. Hind limbs only Pygopus Cryptodelma Delma Pletholax Aprasia Lialis Mancus Pseudopus Opheodes Hyalosaurus IV. No limbs Opheosaurus Dopasia Anguis GLOSSA ANNIEL- LOIDEA ANNULATI Scincidae Acontiidae Dibamidae Anelytropsidae Anniellidae Hagria Heteropus Ristella Menetia Gongyloseps Chiamela Rhinoseineus Tetradactylus Miculia Chalcidoseps Blepharactisis Sphenops Zygnopsis Allodactylus Tridentulus Chalcides Hemiergis Siaphus Phaneropis Sepomorphus Sphenoscineus Sepsina Nessia Hemipodium Anisoterma Lerista Eumecia Heteromeles Dimeropus Chelomeles Brachystopus Oncopus Brachymeles Anomalopus Coloscincus Furcillus Dicloniscus Evesia EuchirotK.ae (di- gits 3-5) Ollochirus Dumerlia Scelotes Soridia Podoclonium Dibamus Opheoscincus Herpetosaura Sepophis Herpetoseps Opheomorus Acontias Typhlacontias Anelytropsis Feylinia Typhlosaurus Anniella Amphisba:na Rhineura Lepidosternum Trogonophidae 218 PRIMARY FACTORS OF ORGANIC EVOLUTION. from the former may be regarded as a process of de- generation. The important conclusion drawn from all this is, that the Tunicata are the degenerate descend- ants of a group of the primitive Chordata " (=Verte- brata). The degeneracy of the Tunicata follows imme- diately their assumption of the sessile condition. Some of the degenerate forms which are not sessile, are sup- posed to be the free descendants of sessile forms. Among the craniate Vertebrata, most conspicuous examples of degeneracy are to be seen in the reduction and loss of limbs in certain Batrachia and in many Reptilia. In both classes successive loss of phalanges and digits form series in several groups of salamanders and lizards, and in both these orders there are forms with the limbs rudimental or altogether wanting. In Batrachia, the genus Amphiuma displays rudimental limbs with minute digits numbering two or three on each limb. In the Caeciliidae, the limbs are wanting. Both types are subterranean in their habits. I give the annexed table of the Lacertilia with degenerate limbs, which it will be observed are found in eleven distinct families. (Pp. 216-217.) Finally, in the snakes (Ophidia) the limbs have totally disappeared, rudiments only remaining in the boas and pythons and their allies. Paleontology renders it clear that this reduction is a case of degeneracy, since both the Ophidia and La- certilia can be traced to Reptilia of the Permian epoch, which have well-developed limbs. This degeneracy is allied to subterranean or terrestrial habits. It is prob- able that the primitive snakes sought concealment in cavities of the earth and beneath rocks and logs, and spent much of their time in narrow quarters, where CA TA GENESIS. 2 19 limbs would be of no use to them. Some of them, the Angiostomata, are now subterranean in their habits, and most of them are blind, or nearly so. These forms present rudiments of limbs, which leads to the supposi- tion that they are near to the ancestral types. From such forms they developed a type which has proved competent to compete successfully with other verte- brates on the ground, in the water, and in the trees of the forest. From what has gone before it is now clear that while kinetogenesis is a factor in progressive evolu- tion, the reverse process, or akinetogenesis, is as defi- nite a factor in degeneracy. The evidence derived from parasitism and sedentary modes of life is conclu- sive in this direction. I now cite another example of catagenesis which throws much light on the origin of the vegetable king- dom. I have advanced the hypothesis1 that plants are the degenerate descendants of protozoan animal ancestors, and I will now produce some of the evi- dence on which the hypothesis rests. The Myxomy- cetes or Mycetozoa occupy debatable ground between the vegetable and animal kingdoms. They seem at one period of their history to pertain to the former and at another to the latter. These organic beings are claimed by both botanists and zoologists, the former placing them with the Fungi, the latter including them in the Protozoa. The fact is that in their mature form they enter the Fungi, while in their early stages they are Protozoa. They have distinct reproductive structures, which pro- duce spores. From each spore issues a "flagellula," which is a simple cell with a flagellum, not apparently 1 Origin of the Fittest, pp. 431-432. 220 PRIMARY FACTORS OF ORGANIC EVOLUTION. different from a monad. The flagellum is early lost, and the cell is then termed an amcebula, since it does not differ materially from an amoeba. Its movements are similar, and it puts forth short pseudopodia. When these amcebulae come in contact with each other they Fig. 54. — Mycetozoa (from Lankester after Du Bary). 1-6, Germination of spore (i) of Tricheavaria, showing the emerging flagellula ; (4-5) and its conversion into an amcebula (6). 7-18, Series leading from spore to plasmo- dium phase of Chondrioderma. dijfforma ; 7, spore ; 10, flagellula ; 12, amoe- bula ; 14, apposition of two amcebulae ; 15-17, fusions; 18, plasmodium. 19- 20, Spore-fruit (cyst) of Physarum leucoph&um X 25 ; the former from the sur- face, the latter in section with the spores removed to show the sustentacular network or capillitium. 21, Section of the spore-cyst of Dydymium squamulo- sum, with the spores removed to show the radiating capillitium x, and the stalk. fuse, often in large numbers, forming a continuous gelatinous sheet, the plasmodium (Fig. 54), which may have several square inches, and even feet of sur- face. At the proper time reproductive organs form on this surface in the form of capsules (sporangia), which may or may not be supported on peduncles, and CA TA G£N£SfS. 22 1 which are filled with minute cyst-like masses of proto- plasm, or spores. As already stated, these spores give issue to flagellula. We have in the life of the Mycetozoa, if not the actual origin of the vegetable from the animal king- dom, a case closely similar to it in a collateral phylum. The process is one of degeneracy through the assump tion of a sessile life, or earth-parasitism ; an example of akinetogenesis. The paleontology of animals has ab- solutely established the fact that the predecessors of all characteristic or specialized types have been un- specialized or generalized types, "neither one thing nor another." It may then be regarded as almost cer- tain that the ancestors of the present higher types of plants were more animal-like than they; that the forms displaying automatic movements were more numerous, and the difficulty of deciding on the vegetable or ani- mal nature of a living organism greater than it is now. Hence it may be concluded that "animal" bathmism has from time to time undergone retrograde meta- morphosis producing as a result the permanent form of life which we call vegetable. Given spontaneous movement (i. e. growth) and surrounding conditions, and the resultant product must be structures adapted to their surroundings, just as the plastic clay is fitted to its mould. And this is essentially the distinguishing character of vegetable teleology as compared with ani- mal. In the average plant we see adaptation to con- ditions permitted by unconscious nutrition and repro- duction ; in the animal, adaptation to a greater variety of conditions, due to the presence of sensation or con- sciousness. In closing Part I. of this book, I desire to point out the conclusion which has, I think, been reached. 222 PRIMARY FACTORS OF ORGANIC EVOLUTION. It has been proved, as it appears to me, that the vari- ation which has resulted in evolution has not been multifarious or promiscuous, but in definite directions. It has been shown that phylogeny exhibits a progres- sive advance along certain main lines, instead of hav- ing been indefinite and multifarious in direction. It is not denied that many lines of variation have been at one geologic period and another discontinued. It is also true that certain divergences from the main lines have appeared, and that minor and secondary variations have occurred. Such variations do not seem to have had any material effect on the general course of evolution. In many cases such variations from main lines might be compared to the undulations in the course of a stream, which nevertheless seeks its lowest level in spite of all temporary obstacles. Pro- fessor Scott has termed these temporary variations "nu- tations," in an able article on the subject.1 "Sports" seem to have been of no importance in evolution what- ever. I American Journal Set. Arts, Vol. XLVIII., 1894, p. 355. PART II. THE CAUSES OF VARIATION, PRELIMINARY. IN Part II., which treats of the causes of variations, I propose to cite examples of the direct modifying effect of external influences on the characters of indi- vidual animals and plants. These influences fall nat- urally into two classes, viz., the physico-chemical (molecular), and the mechanical (molar). The modi- fications so presented are supposed to be the result of the action of the causes in question, continued through- out geologic time. To the two types of influence which thus express themselves in evolution, I have given the names Physiogenesis1 and Kinetogenesis. The inheritance of character is assumed in this sec- tion, and the reason for so doing will be considered later, in the third section of this book. In the animal kingdom we may reasonably suppose that kinetogenesis is more potent as an efficient cause of evolution than physiogenesis. In the vegetable kingdom it is quite evident that evolution is more usually physiogenetic than kinetogenetic. Atmospheric and terrestrial conditions play a major role in the 1 " The Energy of Evolution," American Naturalist, March, 1894. " The Origin of Structural Variations " in New Occasions, Chicago, May, 1894. C. H. Kerr & Co. 226 PRIMARY FACTORS OF ORGANIC EVOLUTION. determination of plant-structure, but motion has also had an important influence. The motion, however, has originated in small degree in the plant itself, but has been derived from without. Some importance must be ascribed to the effects of winds, but the prin- cipal source of the especial strains to which plants have been subjected, has been the insect world. In- sects have been inhabitants of land-plants since their origin in early Paleozoic ages, and the mutual relations of plants and insects have ever been intimate. As has been insisted by Muller and Henslow, the uses to which the floral organs have been put by hymenopte- rous and other insects have been probably a principal cause of the forms assumed by the former. From this direction has been derived the kinetogenetic influence in plant evolution. The few independent movements displayed by plants may have had some influence on the evolution of their structure. We have no reason as yet to suppose that such movements have any other than purely physical factors. CHAPTER V.— PHYSIOGENESIS. T)OTANISTS and gardeners are familiar with the JJ effects of physical causes in producing modifica- tions in the characters of plants. That modifications so produced have become hereditary is known to be the fact, and we may therefore infer that the evolution of plant forms has been produced in large degree by similar agencies in past geological ages. Says Hens- low:1 "M. Carriere raised the radish of cultivation, Raphanus sativus L. , from the wild species, R. rapha- nistum L., and moreover found that the turnip-rooted form resulted from growing it in a heavy soil, and the long-rooted one in a light soil. Pliny records the same fact as practised in Greece in his day, saying that the male (turnip form) could be produced from the female (long form) by growing it in a " cloggy soil. " The rule may be laid down that a species [of plant] may be constant as long as its environment is constant, but no longer. I have changed the spiny Ononis spinosa L., the rest-harrow, both by cuttings and by seed into a spineless form, undistinguishable from the species O. repens L. in two years ; but it would have, I doubt 1 Natural Science ; 1894, pp. 259-260. 228 PRIMARY FACTORS OF ORGANIC EVOLUTION. not, at once reverted to the O. spinosa if I had re- planted it on the poor soil from which I took it. It seems, therefore, to be a very hazardous and fallacious method of testing the value of specific or other char- acters by cultivation. A wild plant may or may not change at once. Thus the carrot, Daucus carota L., proved refractory with Buckman, but not with Vilmo- rin, who converted this annual into a hereditary bien- nial by sowing the seed late in the season, till the character of flowering in the second season became fixed." The prevalence of spinous plants in dry and desert regions has often been described.1 The same is true of reptiles, although spines appear on some species in fertile regions. Spines of plants are believed to be twigs, petioles, leaves, etc., partially aborted under the influence of drought, or the absence of the water neces- sary to the tissues of the parts in question. Wallace points out, however, that there are spinous plants in humid climates, citing the Gleditschia (honey locust) as an example. The spines of such plants may be sur- vivals of periods of drought in previous geologic ages. Or desiccation of certain parts of a plant might be a form of abortion of those parts, a phenomenon which is confined to no region, and is evidently due to causes other than drought in some cases. Henslow (/. in Metazoa in the tegumentary sheath of the body. " c, They consist first either of muscle-cells, or muscle-fibers, from which develop man- tle muscle-cells and mantle muscle-fibers. Mantle muscle-fibers compose the other- wise highly developed striped muscles of l"Die Entstehung und Ausbildung des Muskelgewebes, insbesondere der Querstreifung desselben als Wirkung der Thatigkeit betrachtet." Zeit- schrift ftir wissenschaftliche Zoologie, LIII., Suppl., 1892, p. 67. KINE TO GENESIS. 253 Arthropoda, and some Vertebrata (Batra- chia). And when the entire muscle-fiber is divided into fibrillae, there can appear an external layer of muscular threads. "(4) That muscle cells and fibers first appear in the external stratum of the active body of animals, is due to the especially active movements necessary to this part of the body. This is a simple mechanical consequence of the fact, that in a more or less longi- tudinally extended body of protoplasm, whether it be Protozoon or worm, or muscle-cell or muscle-fiber, that its movements must be more vigorous on the external than the internal portion of it. Therefore, the former would first display muscular structure. " (5) If the first stage is the development of masses of plasma, which display contraction in definite direc- tions, the next step is the division of such masses into muscle-threads or fibrillae. These threads must be re- garded as a result of contractions, whose inequality produces subdivisions of the original mass. A com- pound structure is also more effective than a simple one in effecting contractions. "(6) The next stage of evolution of muscular tissue consists of the appearance of the cross-striping. The mechanical effect of the cross-striping is to distribute the contractility equally throughout the length of the fiber. The contractions of the unstriped muscular fiber are less vigorous, and also less uniformly dis- tributed than those of the striped fiber. The cross- striping is a result of contractions. It commences as simple undulations of the surface of the fiber. The contraction of the plasma is wave-like and is propa- gated rapidly through the fiber, and is not due to a flow and return of the contained protoplasm. The 254 PRIMARY FACTORS OF ORGANIC EVOLUTION. frequent repetition of these local contractions and en- largement of the fiber have resulted in a permanent difference in its intimate structure, the alternate wavee becoming fixed as cross-bands." As evidence of the truth of this proposition, (6), Eimer cites many facts. In the muscles of the Mol- lusca, striped fibers occur in those forms, as Pecten, where the closing of the shell is especially vigorous, this being their mode of progress through the water. In other forms, where the muscles have no such vigo- rous use, the fibers are smooth. In Arthropoda, the muscles of the legs of swiftly running forms are striped, while those of the alimentary canal are smooth. It is a general law that muscles which have energetic con- tractions are striped, while those in which the con- tractions are slow or feeble, are smooth. In the com- mon house-fly, Eimer records some remarkable obser- vations. Flies examined in winter, during the period of torpidity, were found to have the fibers of the tho- racic muscles smooth. With advance of the spring the striping gradually made its appearance, and in the summer it was fully developed. An artificial imitation of winter, by refrigeration in an ice-cellar, caused the cross-striping to disappear. The striping in some other animals is shown by Eimer to be strongly in- fluenced by physical conditions. In fact, muscular tissue is highly plastic, and as it is directly under the control of nervous or equivalent stimuli, the effect of the latter in building structure is evident. That the motion communicated to the hard parts through the agency of the muscular system is effective in building the hard structures will be shown in a subsequent section. K2NE TO GENESIS. 255 2. KINETOGENESIS IN MOLLUSCA. a. The Origin of the Plaits in the Columella of the Gastropoda. Mr. W. H. Dall has developed the mechanics of evolution in the Gastropoda, and I quote extracts from one of his papers to show the harmony of his views with those of other Neo-Lamarckians.1 "The question which first arises is as to the origin of the columellar plications and their function. In considering the dy- namic relations of the animal to its shell we may ob- tain satisfaction on this point. In the fusiform Rha- chiglossa an anatomical difference exists to which I believe attention has not hitherto been called. In- deed, unless the principles of dynamic evolution are granted, it is a difference which would appear to have little or no significance. These principles, however, afford a key which seems to unlock this and many other mysteries. In the recent forms of this sort the adductor muscle, which in all gastropods is attached to the columella at a certain distance within the aper- ture, is attached deeper within the shell than in non- plicate forms. The point of attachment may be an entire turn, or even more, behind the aperture, while in short globose few-whorled shells and in the non- plicate forms it is, as a general rule, little more than half a turn behind the aperture. ' ' Now let us consider the dynamics of the case. We have, reduced to its ultimate terms, a twisted, shelly, hollow cone, subangulate or even channelled at two ex- 1 Transactions of the Wagner Free Institute of Science, Philadelphia, Aug., 1890, p. 58. 256 PRIMARY FACTORS OF ORGANIC EVOLUTION. tremes corresponding to the canal and the posterior commissure of the body and outer lip. Inside of this we have a thin, loose epithelial cone, the mantle, of which the external surface, especially toward the mar- gin, is shell-secreting ; lastly, inside of the mantle- cone we have a more or less solid third cone, consist- ing of the foot and other external parts of the body of the animal, which can be extended beyond the mantle- cone outwardly, as the mantle-cone can be beyond the shell- cone. The body-cone and the mantle-cone are attached at one of the angles of the shell-cone some distance within the opening of the spiral of the latter. The two outer cones constitute a loose, flexible funnel within a rigid, inflexible funnel, while the body-cone forms a solid, elastic stopper inside of all. " What will happen according to mechanical prin- ciples (which can be tested by anybody with the sim- plest apparatus) when the mantle-cone is withdrawn into a part of the shell-cone too small for the natural diameter of the contracted mantle-cone ? It must wrinkle longitudinally. Where will the wrinkles come? They will come at the angles of the shell-cone first ; they will be most numerous toward the aperture, since toward the aperture the mantle-cone enlarges dispro- portionately to the caliber of the shell, owing to its processes, the natural fold of the canal, etc., etc.; the deepest and strongest wrinkles will be on the pillar, owing to the fact that the attachment of the adductor prevents perfect freedom in wrinkling and the groove of the canal will mechanically induce the first fold in that vicinity. The most numerous small wrinkles will be near the aperture opposite the pillar, because of the mantle-edge this is the most expanded part, and there will be a tendency to a ridge near the angle of KINE TO GENESIS. 257 the posterior commissure. Repeated dragging of a shell secreting surface, thus wrinkled, over a surface fitted to receive such secretion, will result in the ele- vated shelly ridges which on the pillar we call plica- tions ; and on the outer lip lirae, if long, or teeth, if short. The commonly existing subsutural internal ridge on the body of the shell near the posterior com- missure will mark the spe- cial conditions in that part of the aperture. "When the secreting sur- face is thus wrinkled or cor- rugated longitudinally, the wrinkles and the concave folds between them will be directed in the sense or di- rection in which the body moves in emerging from or withdrawing to the whorl. The summits of the convex wrinkles will be appressed more or less forcibly against the shell -wall exterior to them in which they are con- fined. The semi-fluid, limy body ..whorl °pen*d' ^spiayinR J non-nhratft rohimftlla. From Dall. secretion of which the shell- lining is built up, exuding from the whole surface of the mantle, will be rubbed away from the lines of the summits of the wrinkles and tend to accumulate in lines corresponding to the concave furrows between the wrinkles. This secretion hardens rapidly and these lines would become somewhat elevated ridges which would by their presence (when once initiated) Fig. 56. — Fusus far His Con. the y whorl opened, displaying non-plicate columella. From Dall. 258 PRIMARY FACTORS OF ORGANIC EVOLUTION. tend to maintain the furrows and wrinkles in the same place with relation to the thus-initiated lirae, as these elevated lines are called when on the outer lip ; or plaits, when situated on the pillar. "The modification referred to generally takes place during resting stages of the animal's growth, since while the animal is rapidly extending its coil the se- cretions seem to be directed toward the extreme mar- gin, and the general mantle-surface resumes its secre- tive function (or the latter becomes active) somewhat later, after the formation of a definite varix, or thick- ened margin ; indicating a resting stage in the animal's career. It is probable also that during rapid growth there is less compression of the tissues than during the resting-stages. The external sculpture and some of the modifications of the aperture are connected with the functions of the extreme edge of the mantle ; those we are at present considering relate more especially to the function of its general surface by which the layer which lines the whorls, the pillar, plaits, and lirae are solely secreted and deposited. " In species with the abductor attached to the pillar near the aperture, the wrinkles would be fewer, and their action, if any, confined to the vicinity of the mar- gin of the aperture. The deeper the attachment, the greater will be the compression of the secreting sur- face and the distance over which it is constantly dragged back and forth, and the consequent length of the ridges of shelly matter deposited. If the inner or mantle-cone had the whole cavity to itself, it is evident that it could and would infold itself in a manner which might not appress its folds against the inner surface of the rigid outer or shell-cone. But there the mass of the solid and elastic foot and external body comes KINETOGENESIS. 259 into play, and by its withdrawal inward forces the wrinkled mantle-cone against the shell. The mantle is thus confined between a rigid outer and an elastic inner surface, with the result that it cannot recoil from the former and that a certain uniformity of size and direction is imposed upon the wrinkles, except where the re- cess of the canal allows them to become more emphatic, or to a less degree the posterior angle permits a slight expansion. The mechanical principles involved may be readily illustrated by the experiment of pulling a hand- kerchief through the neck of a bottle, or funnel, followed by a cork in the center. Of course, the more nearly the apparatus conforms to the form and twist of a spiral shell, the more nearly the results will approximate those of nature. It is difficult, however, to find any artificial tissue which will correspond in elasticity, or capacity for partial self-contraction, to the living tis- sues concerned in nature. Hence, an exact conformity is not to be expected, though the mechanical principles may be reasonably well illustrated. "A comparison of specimens will show that the results exhibited agree with marvellous precision with the results called for by the preceding hypothesis, based on the dynamical status of the bodies concerned, Fig. tfl.—Mitra lineolata Heilprin, the body- whorl opened, showing the pli- cations of the columella. From Dall. 260 PRIMARY FACTORS OF ORGANIC EVOLUTION. their motions and secretions. The agreement is so complete as to amount to a demonstration, though in certain cases there may be complications which need additional explanation. "A point which may- be noted in regard to the Vo- lutidae, to which my attention was called by Mr. Pils- bry, is that in this group the mantle is greatly ex- tended, and there would be more of it to be wrinkled than in such forms as Buccinum, etc. It may be added that the forms in which we note the beginning of plaits for this family, many of them, such as Liopeplum and Volutomorpha, had the mantle so extended as to deposit a coat of enamel over the whole shell, as in the modern Cypraea, so that here we have an additional reason why plica- tion should be emphasized in this group. "Of course, as before noted, the Fie. &.-Sifihocypr«a mechanical principles are the same prooletnatzca Heilprin ; body -whorl opened, in any group of gastropods, but showing plications of among those - which the wrinkling lips. From Dall. is confined to the region of the aper- ture, or those shells which are lirate or dentate, as opposed to plicate, several other principles come into play which may be briefly referred to in passing. In the first place, those species which have a very ex- tended mantle, with hardly an exception have a lirate aperture (Oliva, Olivella, Cypraea, Trivia, etc.). With species in which there is a widely expanded mantle and yet no lirations, it will usually be found that the mantle is not entirely withdrawn into the shell in such forms, or is permanently external to the shell (many KINETO&ENESIS. 261 Opisthobranchs, Marseniidae, Sigaretus, Harpa, etc.). In a group like the Cypraeidae, where nearly all the species are lirate on both lips, there are a few which want these lirae, and these are species which have a wider aperture in the adult than most of the genus, and in which we should expect the wrinkles to be less emphatic." b. Mechanical Origin of Characters in the Lamelli- branchs (Pelecypoda). Dr. Robert T. Jackson has pointed out1 the history of the characters of the retractor muscle and some of those of the list, of bivalve Mollusca. I take the fol- lowing abstract of his conclusions: "In the develop- ment of pelecypods we find in a late embryonic stage (the phylembryonic) that the shell has a straight hinge- line. This is characteristic of Ostrea (Fig. 59), Car- dium, Anodonta, and so many widely separated genera that it apparently represents a primitive ancestral con- dition common to the whole class. Embryology shows that the bivalve shell doubtless arose from the split- ting on the median line of a primitive univalvular an- cestor. If that ancestor had a saddle-shaped2 or a cup-shaped3 shell, as is probable, the first result of the introduction of a hinge in the median line would have been to straighten the shell on the hinge-line. This is a simple problem in mechanics, for if one tries to break by flexion a piece of metal which is saddle- shaped or cup-shaped, it will tend to form a straight line on the axis of flexion. A parallel case is seen in the development of a bivalve shell in ancient crus- \Memoirs of the Boston Society of Natural History, Vol. IV., No. 8, p. 277 July, 1890; American Naturalist, 1891, p. n. 2 Characteristic of young Dentalium. 3Characteristic of the extreme young of cephaious molUibka. 262 PRIMARY FACTORS OF ORGANIC EVOLUTION. taceans. The ancient Ostracoda, Leperditia, Aristo- zoe, etc., have a straight hinge-line and subcircular valves, which are united dorsally by a ligament. The resulting form of the early condition of the bivalvular shell in these two distinct classes is so strikingly simi- lar, that it lends weight to our supposition that the form is induced by the mechanical conditions of the case. " I think that the adductor muscles which close the valves may also be demonstrated to be the necessary consequence of the bivalvular condition. In the phyl- embryo stage (Fig. 59) the valves are closed by a single adductor muscle, which is the simplest condition mechan- ically possible to effect the desired end.1 This muscle does not seem homologous with any muscle in other classes of mollusks, and is probably developed from the Fig- y).—Ostrea edulis, embryo; a ad, anterior adductor muscle; mantle mUSCleS as a COnS6- m, mouth; a, anus ; z/, velum; h, quence of the Conditions of hinge of shell. (After Huxley.) . ... the case. In support of this view, bivalvular crustaceans may again be cited. They have an analogous adductor muscle, developed, of course, on an entirely different line of descent, but under closely similar mechanical conditions. At the completed prodissoconch stage in all pelecypods, as far as known, there are two adductor muscles, a second one having developed in the posterior portion of the body. In later life the anterior, the posterior, or both adductors iThis early adductor appears in the same position in many genera, and is apparently characteristic of the class. It is the anterior of the two adductors found in the later stages ; but it may be retained or lost in the adult. KINE TO GENESIS. 263 may be retained, reduced, or lost, according as the persistence or changes in correlated anatomical fea- tures retain in use or bring into disuse the muscles in question. "Let us look at examples of the retention or loss of the adductors. In typical dimyarian pelecypods, as in Mya (Fig. 60) or Venus, the adductors lie toward either end of the longer axis of the shell. As the hinge occupies a position on the borders of the shell about midway between the adductors, both muscles are nearly or quite in a position to be equally functional in clos- Fig. 60. — Mya arenaria. Lettering: ap ax, antero- posterior axis; hax?. hinge axis; a ad, anterior, and pad, posterior adductor muscle; m. mouth; //, palps ; a, anus ; g, gills ; pd, pedal muscle ; f, foot ; b, byssus ; A, heart. ing the valves. As a result, both muscles are of about the same size. The condition described is that existent in the completed prodissoconch stage in all pelecy- pods, as far as known. In later life, however, a revo- lution of the axes of the soft parts may take place, so that the antero-posterior axis (represented by a line drawn through the mouth and middle of the posterior adductor muscle), instead of being parallel to the hinge-axis (the axis of motion of the valves) as in dimyarians, may present a greater or less degree of divergence from the parallel. In progressive series, 264 PRIMARY FACTORS OF ORGANIC EVOLUTION. as in Modiola (Fig. 61), Perna, etc., as the adductor muscle is brought nearer and nearer to the hinge-line, Fig. 61. — Modiola plicatula. Lettering same as in Fig. 60. where its mechanical action is less and less effectual in closing the valves, we find that it is more and more reduced until it finally dis- appears, from disuse and atrophy, as in Ostrea (Fig. 62), and Pecten. Con- versely, the posterior ad- ductor in the same series in the revolution of the axes is pushed farther and farther from the hinge -line and nearer to the central plane of the valves, where its me- chanical action is most ef- fectual in closing the valves. With its increase in func- tional activity the muscle increases in size. The revolved position of the axes, and the consequent reduction or loss of the anterior adductor and increase of the posterior adductor, is Fig. 62. — Ostrea virginiana. Let- tering same as in Fig. 60. KINETOGENESIS. 265 found in many widely separated genera of pelecypods, as Ostrea, Mulleria, and Tridacna ; thus proving the development of the same features on different lines of descent.1 In Aspergillum the two valves have con- cresced so as to form a truly univalvular, tubular shell, so that the adductors would evidently be f unctionless if existent. The posterior adductor has disappeared and the anterior is reduced to a few disconnected shreds (Fisher), though evidently existent in the young, as attested by the form of the shell in the nepionic stage. " Ordinarily there are two posterior retractor- mus- cles of the foot in pelecypods, one situated on either side. In adult Pecten either the left retractor alone exists, or both retractors are wanting (the left doubtless al- ways exists in the young). In studies of young Pecten ir radians, I found that the animal always crawled while lying on the right side, with the foot extended through the notch in the lower valve and pressed against the surface of support. It is evident that while crawling in this position the left retractor is in the plane of traction, and it is retained ; on the other hand, the right retractor would not be in the plane of trac- tion, and it has disappeared through disuse and atro- phy.2 A similar disappearance of the right retractors of the foot is seen in Anomia glabra, and is explained on similar bases of argument. < ' In My a arenaria we find a highly elongated siphon. In the young the siphon hardly extends beyond the borders of the valves, and then the animal lives at or IDr. B. Sharp and I published almost simultaneously closely similar views on the mechanical aspect of the relative size of the adductors. See Proceeds. Phila. Acad.^ 1888, p. 122, and Proceeds. Boston Soc. Nat. Hist., Vol. XXIII., 1888, p. 538. 2 Both retractors doubtless exist in the prodissoconch stage of Pecten and allies. 266 PRIMARY FACTORS OF ORGANIC EVOLUTION. close to the surface. In progressive growth, as the animal burrows deeper, the siphon elongates, until it attains a length many times the total length of the valves. The ontogeny of the individual and the pale- ontology of the family both show that Mya came from a form with a very abbreviated siphon, and it seems evident that the long siphon of this genus was brought about by the effort to reach the surface, induced by the habit of deep burial. " The tendency to equalize the form of growth in a horizontal plane in relation to the force of gravity act- ing in a perpendicular plane, or the geomalic tendency of Professor Hyatt,1 is seen markedly in pelecypods. In forms which crawl on the free borders of the valves the right and left growth in relation to the perpendic- ular is obvious, and agrees with the right and left sides of the animal. In Pecten the animal at rest lies on the right valve, and swims or flies with the right valve lowermost. Here equalization to the right and left of the perpendicular line passing through the center of grav- ity is very marked (especially in the Vola division of the group) ; but the induced right and left aspect cor- responds to the dorsal and ventral sides of the animal, — not the right and left sides, as in the former case. Lima, a near ally of Pecten, swims with the edges of the valves perpendicular. In this case the geomalic growth corresponds to the right and left sides of the animal. "The oyster has a deep or spoon-shaped attached valve and a flat or flatter free valve. This form, or a modification of it, we find to be characteristic of all 1" Transformations of Planorbis at Steinheim, with Remarks on the Ef- fects of Gravity Upon the Forms of Shells and Animals." Proceeds. A. A. A. S., Vol. XXIX., 1880. KINETOGENESIS, 267 • pelecypods which are attached to a foreign object of support by the cementation of one valve. All are highly modified, and are strikingly different from the normal form seen in locomotive types of the group. The oyster may be taken as the type of the form adopted by attached pelecypods. The two valves are unequal, the attached valve being concave, the free valve flat ; but they are not only unequal, they are often very dissimilar, — as different as if they belonged to a distinct species in what would be considered typ- ical forms. This is remarkable as a case of acquired and inherited characteristics finding very different ex- pression in the two valves of a group belonging to a class typically equivalvular. The attached valve is the most highly modified, and the free valve is least modified, retaining more fully ancestral characters. Therefore, it is to the free young before fixation takes place and to the free, least-modified valve that we must turn in tracing genetic relations of attached groups. Another characteristic of attached pelecy- pods is camerated structure, which is most frequent and extensive in the thick attached valve. The form as above described is characteristic of the Ostreidae, Hinnites, Spondylus, and Plicatula, Dimya, Pernos- trea, Aetheria, and Mulleria; and Chama and its near allies. These various genera, though ostreiform in the adult, are equivalvular and of totally distinct form in the free young. The several types cited are from widely separated families of pelecypods, yet all, under the same given conditions, adopt a closely similar form, which is strong proof that common forces acting on all alike have induced the resulting form. What the forces are that have induced this form it is not easy to see from the study of this form alone ; but the 268 PRIMARY FACTORS OF ORGANIC EVOLUTION. ostrean form is the base of a series, from the summit of which we get a clearer view." c. Mechanical Origin of the Impressed Zone in Cepha- lopoda. Prof. Alpheus Hyatt has shown that the groove on the dorsum or inside of each coil of the Cephalopoda is due to the pressure exercised by contact with the ventral side of the coil within it. He has shown that this groove persists in cases where the shell in the course of evolution has become more or less unwound, and he regards this as an example of the inheritance of a mechanically acquired character. This subject is presented in greater detail in the part of this book de- voted to heredity. 3. KINETOGENESIS IN VERMES AND ARTHROPODA. It is believed with good reason that the Arthropoda have descended from some of the forms included in the branch Vermes, and perhaps Peripatus furnishes the nearest living approach to that type. The ances- tor, whatever it may have been, developed limbs from processes of the body-wall, and used them to aid in progression. Peripatus has soft flexible limbs, and a non-chitinous integument generally. With the begin- ning of induration of the integument, segmentation would immediately appear, for the movements of the body and limbs would interrupt the deposit at such points as would experience the greatest flexure. The muscular system would initiate the process, since flexure depends on its contractions, and its presence in ani- mals prior to the induration of the integuments in the order of phylogeny, furnishes the condition required. It is a matter of detail how the diverse segmentations KINETOGENESIS. 269 of existing forms were produced. We can believe, however, that, as in Vertebrata, there has been a gradual elimination of less important segments of the limbs, until the highest mechanical efficiency was at- tained. We well know how the segments of the head and body have been modified by fusion, etc. Prof. B. L. Sharp has shown the mechanical con- ditions of segmentation in Arthropoda as follows:1 "It occurred to me that if the theory [of kineto- genesis] had a general application, some additional proofs could be shown to exist among the inverte- brates, where we have the action of muscular force upon hard and resisting parts of the skeleton. Those which present the best study for this purpose appear to be the crustaceans, where we find an immense va- riety of articulations in the body and in the limbs; highly complicated locked joints, others allowing mo- tion in but one plane, as well as loose joints, where the hard parts scarcely come in contact with one another, and cases of degeneration of the hard parts, leading to total disappearance of a previously existing joint. "In the Anneiides, from which, there is no doubt, the arthropod branch sprang, we find no deposit of inorganic salts in the epidermis. The outer layer of the body is generally of a horn-like character, adher- ing closely to the secretive cells of the epidermis, very flexible, and thrown into folds by the vermicular mo- tion of its possessor. In the leeches the body consists of a flexible cylinder, made up of two sets of muscles, an outer longitudinal cylinder and an inner cylinder of circular fibers* the contraction of which causes the animal to increase in length, while shortening is ef- 1 American Naturalist, 1893, p. 89. 270 PRIMARY FACTORS OF ORGANIC EVOLUTION. fected by the contraction of the longitudinal layer. The external surface of the medicinal leech, for exam- ple, is thrown into a regular series of very fine folds, extending across the longitudinal axis of the body. These folds do not correspond in numbers to the so- mites of the body, which are not indicated externally, five, six, or more of them belonging to one somite. When the animal shortens its length, these folds are deepened and the segments thrown closely to- gether ; when extension takes place, the folds are flattened, spread open, although not wholly disappearing, as they are a fixed quantity, so to speak. I believe these folds are due to mechanical action ; by the disposition of the different fibers of the longitudinal series, in being in- serted in a series of planes bounded by the valleys between the folds, this being aided by some of the circular fibers which pass through Fig. 63.-Diagraminatic the longitudinal sheath, and find representation of the seg- . ments of the leech, show- their attachment to the bases of the ing the folds, valleys, and valleys, muscular fibers. ' Starting from this point, and supposing the regularity of the folds to have become established from preexisting folds by the regularity and stress of muscular action, we can conceive that when deposits of calcareous matter took place, rings simi- larly formed by a folding of a soft skin would receive that deposit at the most prominent portion of this fold, the convex face, and not in the protected valleys, as there would be more friction or pressure from external KINE TO GENE SIS. 271 causes, and no deposits would take place in the val- leys themselves, because they would not be subject to external friction, and their continual flexion would prevent any such deposits. Should such a deposit take place in the valleys, there would be a stiffening of the whole surface, which would defeat motion. In fact, in the leech the cuticle is already much thicker on the crests of the folds than in the valleys. * ' In the more primitive Crus- tacea, we find the animal made up of rings extending over the whole length of the body, similar to the rings of the leech, save that there is but one ring to one somite, and instead of a perpendicular valley between the folds, this valley has an inward and a forward direction, allowing the anterior edge of a caudad ring to fit into the posterior edge of a cephalad ring. . "In the higher Crustacea, sev- eral of the anterior rings have co- alesced and form a solid shield which is known as the carapace. This has no doubt arisen by the lessening of the action between the anterior rings when the posterior portion of the body became the moie active propelling organ. As the ac- tion ceased forward the valleys came to rest, and be- came exposed to friction and pressure, and conse- quently a deposit of calcareous matter took place pro- ducing the stiffening above hinted at. "The formation of jointed appendages from para- podic paddles of the annelids can be followed out in Fig. 64. — Diagram- matic representation of the rings of a primitive crustacean, showing the action of the muscles. 272 PRIMAKV FACTORS OF ORGANIC EVOLUTION, the same manner, since the manner of mutual relation of the segments is the same as in the case of the body- segments. " It has been stated that in the leech the folds do not correspond in number to the somites of the body, while they do in the Crustacea. All annelids do not move by means of a muscular system built upon the plan found in the leech. In many the circular layer has to a large extent disappeared, for the longitudino-circular plan is undoubtedly ante-annelidan. The movement of the free medusoid forms, and of the Ctenophora, is the result of a modified arrangement of this plan. "With the disappearance of the circular layer, we find a peculiar modification of the longitudinal layer. This layer becomes broken up and the fibers act in moving the setae, which answer to limbs. In a seg- ment of a setiferous annelid, we may observe that the longitudinal muscles of the somite in section at the po- sition of the seta are arranged like the letter 'V in the fork of which the seta lies, the fibers to the left (anterior) pull the seta externally backward, those on the right (posterior) pull the seta forward. The in- troduction of the setae, the origin of which I do not here attempt to explain, has no doubt been, together with the establishment of the external segmentation, a strong factor in causing the breaking up of the muscu- lar tube into sections (myotomes), which by use and consequent increase have extended each arm of the 'V into the segment on each side, while the insertion of the end of the seta has caused a break in the muscle by the formation of an aponurosis. This gives us the peculiar disposition of a myotome to extend across the union of two somites. "If we examine the segments of the so-called ab- KINETOGENESIS. 273 domen of the macrurous Crustacea, as the lobster, we will find that the anterior face of one abdominal ring is pulled into the posterior orifice of the ring lying an- terior to it, forming a kind of tubular ball and socket- joint, but with a flexible part of the integument with no calcareous deposit, folded upon itself, and acting physiologically as a tubular ligamentum teres. On ex- amining the different joints, we will find that com- mencing at a fixed point, as at the base of the thorax, the movable ring of the first abdominal somite is pulled into the fixed part. Then the first abdominal somite be- comes the fixed point for the movable ring posterior to it, and so on, so that we find that as the rings proceed away from the thorax, each is pulled into the opening of the one in advance. This is true of all those forms where the abdomen is well formed, strong, and an ac- tive organ in the economy of the animal ; when this organ, the abdomen, ceases to be an active organ of motion, as in the burrowing forms, as in Callianassa, Gebia, some of the Squillidae, etc., or where it is folded upon the sternum of the thoracic region, the muscles becoming weaker through disuse, the rings are not subject to the powerful muscular strain, and they as a rule overlap but little, if at all, but lie so that the edge of one ring rests upon the edge of another. In those forms where degeneration of the abdomen has pro- ceeded so far as not to have even the usual deposit of calcareous matter, as in the hermit crabs, there are simply indications of rings on the abdomen, and this organ is but little more than a fleshy sac containing some of the viscera, and supplied with a few muscles which act together, with the form of the organ, to keep the abdomen curled so that it may hold as a hook, the 274 PRIMARY FACTORS OF ORGANIC EVOLUTION. animal within the molluscan shell which it habitually inhabits. "When the limbs are examined, the same rule will be found to hold good, viz. : that the movable part is pulled into the fixed part. A modification of this is well illustrated in the evolution of the large chelae. In some forms, take for example Ibacus, the first pair, and in fact all of the thoracic limbs end in a sharp- pointed segment, there being not the slightest sugges- tion of a chela. In Crangon, on the other hand, the terminal segment is pulled against the broad face of the penultimate one thus making a shift for a chela. In the Stomatopoda this step has been developed, for the last segment can be drawn against the whole length of the pen- ultimate one (which is some- times grooved to protect the points of the spines of the latter) and forms with it a very effective grasping or- gan. The continual use of the terminal segment, the increase of the muscular power will tend to draw this terminal segment backward (into) on the penultimate which enlarges with the increase of bulk of muscle, so that a well-developed chela, as in the lobster is found, where the ultimate segment is pulled backward to about the middle of the penultimate segment." Fig. 65.— Diagrams of, a, hand of a form of Crangon ; b, hand of a form of Astacus. KINE TOGENESIS. 275 4. KINETOGENESIS IN THE VERTEBRATA. I have already adduced the evidence in support of the doctrine that the structures of the hard parts of invertebrates have been produced by muscular move- ments. In turning to the Vertebrata we shall find that the evidence indicating that the details of their hard parts have had a similar origin, is quite convincing. This branch of the animal kingdom presents two dis- tinct advantages for this study. First, we have a more complete paleontologic series than in any other. Sec- ond, we have the best opportunity for observation and experiment on their growth processes, since we our- selves, and our companions of the domesticated ani- mals, belong to this branch of the animal kingdom. I shall show first, the conditions under which ab- normal articulations of the skeleton have been formed ; and then the process involved in the formation of normal articulations. I shall then apply these facts to the phylogeny of the Mammalia as we know it, and then in a more general way to the Vertebrata as a whole. i. KINETOGENESIS OF OSSEOUS TISSUE. a. Abnormal Articulations. Hiitter, from whom I have quoted under the head of " Kinetogenesis of Muscle," thus describes the effect of abnormal conditions of joints on the articular sur- faces of the bones which form them. He says: "We have abundant opportunity to investigate the change of condition which the joints undergo during a year of fixed muscular contraction. "The ligaments and bursae undergo similar changes 276 PRIMARY FACTORS OF ORGANIC EVOLUTION. to those described for the muscles concerned. They elongate at points where the articular surfaces are spread apart, and correspondingly shorten where the flexure produces a folding. These changes proceed more slowly than those of the muscles and tendons. Very remarkable are the changes undergone by the articular cartilages. When a joint is permanently flexed, a part of the extremity of each bone is separated from contact with the other, and the articulation is finally destroyed at this point, because the cartilage begins to vanish. One must conclude that the exist- ence of the articular cartilages is dependent on their mutual contact ; for dislocated articular surfaces which remain in contact with soft tissues only, lose their car- tilaginous covering. . . . Finally it is possible by a consideration of the etiology of the effects of joint con- tractions to reach some hitherto unnoticed conclusions regarding the changes of articular surfaces, and bone forms. The results of joint-contraction are most con- spicuous when the latter occurs in childhood. During maturity, a dislocation which causes an articular bor- der or prominence to rest abnormally on the opposed articular face in the act of walking, will be followed by the penetration of the former into the latter, and a de- formation of the articulation ; but the corresponding changes under like conditions in the growing skeleton are much more conspicuous." Hutter thus describes the formation of new artic- ular surfaces as a consequence of dislocation of joints. " If the head of the femur or humerus leaves its socket, and rests on the side of the ilium or the scapula, the periosteum of the bone which receives the new impact is excited to active bone-production, and the result is the deposit of new osseous tissue. The thin bones KINETOGENESIS. 277 become thicker, not uniformly, but in correspond- ence with the periphery of the head of the humerus or femur, rather than with the point of contact of the latter. This point is irritated, but the contact of the ball restrains osseous deposit. So it occurs that grad- ually a new socket is developed, whose mechanical relations correspond exactly with those of the articu- lating bone. The head also acquires a strictly spher- ical shape, by such contractions and atrophies as are necessary to produce that result. Further, cartilage appears in the place of the periosteum of the socket, which functions like the primitive articular cartilage. It is characteristic of both connective and periosteal tissue to develop cartilage under the stimulus of con- tinued friction of hard surfaces, such as occurs in dis- locations and fractures." These observations of Hutter have been confirmed by Henke, Reyher, Moll, and Lesshaft. Henke and Reyher state that the artificial prevention of flexure of articulations in young dogs renders them immobile, and their restraint of flexure to one direction, results in a curving of the articular faces in that direction. I cite here two examples of modifications of struc- ture under abnormal conditions which imposed new impacts and strains on the parts. I have described these cases, which are examples of false elbow-joints in man and in the horse, in the Proceedings of the Amer- ican Philosophical Society for 1892. In the first case, that of the human elbow, the cubitus was luxated posteriorly, so that the humeral condyles articulate with the ulna anterior to the coro- noid process. The head of the radius is in contact with the external epicondyle on its posterior inferior face. The results are as follows. A new coronoid 278 PRIMARY FACTORS OF ORGANIC EVOLUTION. process was developed in front of the abnormal posi- tion of the humeral condyle to an elevation above the shaft of the ulna exceeding that of the normal coro- noid. Between it and the normal coronoid was devel- oped a perfectly functional cotylus which embraces the humeral condyle like the normal cotylus. The latter has its articular surface, buried under osseous deposit, so as to be no longer visible. The region of contact between the head of the radius and the external epicondyles, lias developed in the latter a large artic- ular cotylus which permits of both rotary and ver- tical movement of the former. The articular surface of the humeral condyles, except where in articulation with the ulna, is roughened, and partially overgrown with exostoses, so as to alter its form to a great extent. The opportunity of examining this specimen I owe to Provost Pepper of the University of Pennsylvania, in whose museum it is preserved. In the case of the horse's elbow, the luxation of the cubitus is inward, so that the olecranon articulates with the external epicondylar surface, and the humeral condyles are not adapted to the head of the radius ; their internal border falling considerably internal to the inner border of the radius. The horse from which this specimen was derived lived for two years after the luxation took place, and became able to use the limb in some degree. The effect on the articulation is as follows. A large part of the inferior extremity of the poste- rior rib of the shaft of the humerus, which is the place of insertion of the extern ^ flexor metacarpi muscle, has been removed, so as to present a wedge-shaped out- line with the apex downward. This removal permits the close articulation of the inner face of the olecranal KINETOGENESIS. 279 process with the epicondyle, which has developed a considerable articular face, on which movement takes place in extension and flexion. The posterior border of this face has developed a ridge which borders the facet behind, and retains the olecranon in place. Two other facets are developed on the humeral condyles, and two on the head of the radius. The most impor- tant of the latter is a bevel of the external part of the surface to the border, due to the contact of the ex- panded internal humeral condyle. The articular face of the olecranon is much depressed in consequence of its articulation with the external epicondyle of the humerus. Besides these new and changed facets, the effect of the luxation is seen in the development of os- seous crests at the points of insertion of the articular ligaments. One of these on the humerus has been al- ready referred to. Another is concentric with and posterior to the internal humeral facet of the olecranar process, and serves as a guide to the humeral crest above described. A third is an extensive osseous de- posit on the internal face of the head of the radius, which partially builds an extension of the head of the radius, which if completed would articulate with the overhanging portion of the internal humeral condyle. A third modification of normal structure is similar to that observed in the human elbow. It consists of os- seous deposit beneath the synovial bursa at points where the luxation causes a gaping of the surfaces. This occurs at the trochlear groove of the head of the radius, which is partially filled up with exostosis. The preceding observations lead to the following conclusions : First. Continued excessive friction removes osse- ous tissue from the points of contact until complete 282 PRIMARY FACTORS OF ORGANIC EVOLUTION. adaptation is accomplished and the friction is reduced to a normal minimum. Then a normal articular sur- face is produced. Second. Where the normal friction is wanting, and an inflammatory condition is maintained by a pull- ing stress on the investing synovial membrane, excess of osseous deposit is produced. Third. Stress on the articular ligaments and ten- dons stimulates osseous deposit at their insertions, which deposit may be continued into their substance. This is a pulling stress. These observations therefore show that osseous de- posit is produced by different forms of mechanical stimulus. EXPLANATION OF FIGURES 66 AND 67. 1-5, Homo sapiens, luxated elbow joint (one-half natural size) ; i, luxated elbow joint, from within ; 2, luxated elbow joint, from outer side; 3, humerus, posterior view of distal region; 4, humerus, distal view; 5, ulna and radius, anterior (superior) view ; 6-n, bones of abnormal left elbow joint of horse (one-half natural size) ; 12, 13, normal bones of elbow joint of horse (one-half natural size); 6-12, humerus, distal views; 7-13, cubitus, proximal views ; 8, humerus, external view of distal extremity; 9, humeral articulation of cubi- tus, from above; 10, cubitus, internal view ; n, cubitus, external view. Let- tering.— Ht humerus ; U, ulna ; R, radius ; C, coronoid process ; Czt second (abnormal) coronoid process ; O, olecranon ; En, entepicondyle ; EC, ectepi- condyle ; Eno, entepicondylar exostosis ; Eco, ectepicondylar exostosis ; Co, condylar exostosis ; Cos, superior condylar exostosis ; Cot, inferior condylar exostosis ; Hf, humeral facet ; Rf, radial facet ; Uf, ulnar facet ; Op, olecranar process of ulna ; Cp, coronoid process of ulna; Og, olecranar groove of hu- merus ; Tc, trochlear crest of humerus ; Tg, trochlear groove of humerus ; Ehc, external humeral facet of coronoid process ; Ihc, internal humeral facet of coronoid process ; la, abnormal facet for coronoid process of ulna ; ib, do. for internal roller of humerus; ic, do. for abnormal facet of humerus; id, do. for internal border of radius; le, do. for olecranar process of ulna ; if, do. for trochlear crest of humerus; 2a, 2b, 2c, exostoses of radius and ulna to fill vacuity between humerus and radius and ulna, ja, abnormal crest which serves as a guide to the olecranar process of the humerus ; jb, abnormal crest which serves as a guide to abnormal crest 30. ; jc, exostosis extending head of radius inwards to equalize its width with inward luxation of humerus ; 3d, exostoses of external epicondyle of humerus, to equalize its width with outward luxation of radius; je, abnormal exostosis of insertion of external tfexor metacarpi muscle ; jf, 3g, abnormal crest at insertion of external ar- ticular ligament on olecranar process of ulna. KINETOG&NESIS. 283 b. Normal Articulations. The origin of condyles and their corresponding cotyli has been made the subject of investigation by several German anatomists. L. Fick1 expressed the opinion that the concavo-convex surfaces were pro- duced by a wearing away of the surface which became concave, by the free action on it of the surface which became convex, the former being fixed, and the latter free. He found the conditions of muscular insertions to correspond with the conditions of fixity and free- dom required ; for the insertions are always nearer to the concave surface than to the convex surface. He constructed plaster models of joints, and by moving one on the other obtained a convex surface on the moving, and a concave surface on the fixed extremi- ties. These observations were confirmed by Henke,'2 but he very properly does not regard the result as due to wearing, but to the stimulation of metabolic action in the required directions. R. Fick3 has confirmed these positions in an extended memoir, and recently Dr. E. Tornier has devoted a still more thorough re- search to the same subject.4 R. Fick applied his ob- servations to the question of the phylogeny of the ar- ticulations, but did not see in it proof of the operation of mechanical causes, but ascribed it to "inheritance and natural selection " in accordance with the mean- ingless formula usual at the time he wrote. W. Roux,5 however, in reviewing Fick's article saw in the obser- 1 Ueber die Ursachen der Knochenformcn , Experimental- Untersuchung, 1859, Gottingen, G. Wiegand. 2 Anatomic und Mechanik der Gelenke, Leipsic, 1863, p. 57. SArchivfiir Anatomie und Physiologic, 1890, p. 391. 4 Archii> filr Entiuickelungsmechanik, I., 1894, p. 157. 5 Biologisches Centralblatt, 1891, p. 188. 284 PRIMARY FACTORS OF ORGANIC EVOLUTION. vations of Fick proof of a direct mechanical cause of the structure. I have pointed out the phylogeny of the articulations in the Mammalia in various papers from 1877! to i88g,2 and in 1881 I advanced the view that their successive evolution was due to impacts and strains {American Naturalist, July, 1881 ; Origin of the Fittest, p. 373). The opinion of Roux entirely sup- ports my position, and it is further established by the elaborate memoir of Tornier just cited. This author adopts the view that bone- development is controlled by Druck und Zug or impact and strain, and he adds some important considerations to those previously ad- vanced. Reasserts that "in all existing Vertebrata true bones may appear as secondary structures, since all of these animals possess bands and threads of con- nective tissue which possess the latent capacity to be changed wholly or in part into cartilage. " Thus is accounted for the development of sesamoid bones in tendons, in which category is included the patella. Tornier also shows that the concave articular face (cotylus) is that to which the flexor and extensor mus- cular insertions are nearest, while the convex face (condyle) is the one most remote from the muscular insertions. It must be observed that Tornier adopts the lan- guage of the American Neo-Lamarckians in using the expression "impact and strain." Impact and strain are different modes of motion. "Impact" implies pressure, while "strain " implies a pulling stress, either direct or torsional. It is therefore alleged by Tornier, as it has been by myself, that opposite modes of mo- \Report U. S. Geol. Survey W. of jooth Meridian, 1875, Vol. IV., p. 277- 279. Proceeds. Amer. Philosoph. Soc., 1884, p. 44. 2 Amer. Journal Morphology, 1889, p. 163. KINETOGENESIS. 285 tion may produce metabolic changes in osseous tissue. For this reason it is possible to account for the length- ening of the limb-bones in heavy animals, as an effect of impact, while the astragalus of bats may have been elongated by a stretching strain. c. The Physiology of Bone Moulding. Dr. Koelliker has summarized the results of the observations made by himself and his predecessors on the processes of the growth and absorption of bone, which determine the forms of the elements of the skel- eton.1 Bone is deposited through the agency of uninuclear cells, or osteoblasts, which may under peculiar condi- tions become enlarged and multicellular, when they are termed osteoclasts. These osteoclasts produce an absorption or destruction of the bone or dentine with which they are in contact, the bone or dentine being passive under the operation. How this is done is not known. Pieces of ivory which have been used to re- place bone removed by surgical methods, have been found to be both corroded by osteoclasts, and overlaid by layers of living bone by osteoblasts. In explanation of the causes which induce the for- mation and action of the osteoclasts, Koelliker remarks that : " the totality of changes of the jaws during the development of teeth appears to show that it is pres- sure by the soft parts which causes the absorption of bone. One can admit in the case of the jaw that the dental sacs in process of growth produce by their en- largement a state of irritation in the layer of osteo- blasts which originally border the alveolar edge, and 1 " The Normal and Typical Absorption of Bones and Teeth," Verhandl. der Phys. Med. Ges. ran M'iirzburg, II., III., 1872. 286 PRIMARY FACTORS OF ORGANIC EVOLUTION. that in consequence of this irritation the cellules trans- form themselves into osteoclasts, and acquire a new power, that of absorbing bone. The function will cease as soon as the teeth are formed, by the termina- tion of pressure, and then the formative action of the cellules adjacent to the bone will repair it as a conse- quence of a retransformation of these elements into osteoblasts. "I will not push further this first attempt at an explanation of the normal absorption of bone, but I content myself with observing, that in any case, pres- sure exercised by the soft parts counts for much in this phenomenon. Who does not remember in the face of these facts, numerous cases of pathological absorption of bone due to aneurisms, tumors, and hypertrophied organs? Who will not admit the great effect of the disappearance or arrest of development of organs on the size of their osseous surroundings ; as Pick, for- merly professor of anatomy at Marburg, has shown to take place in the orbit after the extirpation of the eye? It is possible to go a step further in the proposition, that external pressure has much to do with absorp- tion. Thus the growth of the brain and spinal cord produce the resorption seen in the interior of the skull and of the spinal canal ; that of the eye and of the nasal mucosa, and of the cranial vessels and nerves, have resulted in the enlargement of their cavities ; and in the case of foramina, in their wider expansion. . . . The medullary cavities of bones are produced in the process of growth by the corrosive activity of osteo- clasts." It is then pressure which produces the excavations which form new cotyli in the construction of new ar- ticulations due to dislocations. By such excavations KINETOGENESIS. 287 elevated portions remain adjacent to them. Other elevations, as already described, are due to deposit of bone stimulated by the absence of accustomed pres- sure, as in the filling up of the old ulnar cotylus in the human subject above described. Other elevations or osseous deposits such as occur at muscular and ligamentous insertions appear to follow a pulling stress. Many other examples of the abnormal production of articulations might be cited, but the above are suf- ficient to show the plasticity of osseous tissue. It is also evident that if such results follow the stimulus of the parts during a short period of months or years, the continuance of the appropriate mechanical stresses through geologic ages must have been quite sufficient to produce all the characters which we observe in the articulations of the vertebrate skeleton. I will now present the inferences which may be de- rived from consideration of the facts hitherto presented in this chapter. We have not been witnesses of the process of evolution, yet we believe that it has been in active operation. We have not been able to observe its modus operandi, but we may safely infer what it has been from the facts which are before us. Kineto- genesis having been observed in both the soft sarcode (muscle) and in the hard parts of animals, the law of uniformity obliges us to believe that similar changes have taken place in past ages whenever the necessity arose, and the energy at nature's disposal was suffi- cient. il. MOULDING OF THE ARTICULATIONS. a. The Limb Articulations. This part of the subject has the advantage of many facts of paleontology in our possession. We have 288 PRIMARY FACTORS OF ORGANIC EVOLUTION. now discovered the outlines of the phylogeny of many mammalian types, and many detailed histories of spe- cial lines of descent are known. Our knowledge is most complete in the unguiculate and ungulate pla- centals, while it is least as regards the Mutilata, and the implacentals. We have excellent series of skeletal parts, and I have given the successional modifications of some of them on page 139. In the first place, I will select an illustration of the effects of use on the articulations of the limbs and feet of the Mammalia. I take first the ankle and wrist-joints. In the ruminating animals (ox, deer, camel, etc.) and in the horse, among other living species, the ankle- joint is a very strong one, j j -, r ^nd yet admits of an CX- tensive bending of the foot ing pentadactyle plantigrade foot with- ., i j . treU]e out groove of astragalus, as in the C probable ancestor of the Diplarthra. tOngUC-and-grOOVC joint ; that is, two keels of the first bone of the foot, the astragalus, fit into two grooves of the lower bone of the leg, the tibia, while between these grooves a keel of the tibia descends to fill a cor- responding groove of the astragalus. Such a joint as this can be broken by force, but it cannot be dislocated. Fig. 68. — Periptychus rhabdodon Cope, a condylarthrous genus of the Puerco epoch of New Mexico; poste- rior foot, one-half natural size, show- KINE TO GENESIS. 289 Now, in all bones the external walls are composed of dense material, while the centers are spongy and com- paratively soft. The first bone of the foot (astragalus) is narrower, from side to side, than the tibia which rests upon it. Hence the edges of the dense side-walls of the astragalus fall within the edges of the dense side-walls of the tibia, and they have pressed into the more yielding material that forms the end of the bone, and causing bone absorption, pushed it upward, thus allowing the side-walls of the tibia to embrace the side-walls of the astragalus. Now, this is exactly what would happen if two pieces of plastic dead material, similarly placed, should be subjected to a continual pounding in the direction of their length. And in view of the facts already cited we cannot ascribe any other immediate origin to it in the living material. The same active cause that produced the two grooves of the lower end of the leg produced the groove of the middle of the upper end of the astragalus. Here we have the yielding lower end of the tibia resting on the equally spongy material of the middle of the as- tragalus. There is here no question of the hard ma- terial cutting into soft, but simply the result of con- tinuous concussion. The consequence of concussion would be to cause the yielding faces of the bones to bend downward in the direction of gravity, or to re- main in their primitive position while the edges of the astragalus were pushed into the tibia. If they were flat at first they would begin to hollow downward, and a tongue above and groove below would be the result. And that is exactly what has happened. This inclu- sion of the astragalus in the tibia does not occur in the reptiles, but appears first in the Mammalia, which de- scended from them. See Figs. 68-69. I have shown 2go PRIMARY FACTORS OF ORGANIC EVOLUTION. that without exception, every line of Mammalia com- menced with types with an astragalus which is flat in the transverse direction, or without median groove. n IN W 1® w r Fig. 69. Fig. 70. Fig. 69. — Hind foot of primitive cameloid Poebrotherium labiatum Cope, showing grooved astragalus and first toe-bones without keel in front at lower end. (From Colorado.) Fig. 70.- — Hind foot of three-toed horse (Prothippus sejunctus Cope; (from Colorado), showing grooved astragalus, and trace of keel on front of lower end of first bone of middle toe. KINETOGENESIS. 291 From early Tertiary times to the present day, we can trace the gradual development of this groove in all the lines which have acquired it. The upper surface became first a little concave ; the concavity gradually became deeper, and finally formed a well- marked groove. The history of the wrist-joint is similar. The surface of the fore- arm bones which joins the fore- foot is in the early Tertiary Mam- malia uniformly concave. In the ruminating mammals it is divided into three fossae, which are sep- arated by sharp keels. These fos- sae correspond with the three bones which form the first row of the carpus or palm. The keels correspond to the free sutures be- tween them. The process has been evidently similar to that which has been described above as produc- ing the side-grooves in the end of the tibia. The dense walls of the sides of the three bones imping- ing endwise on the broad yielding surface of the fore-arm (radius) bones of' two middle toes have gradually, under the influence °f deer-antel°P* <&**?* ' Jurcatus Leidy), showing Of COUntleSS bloWS, impressed extension of keel on front themselves into the latter. On of lower end (From Mio- cene of Nebraska. the contrary, the surface above the weaker lines between the bones not having been subject to the impact of the blows, and influenced by Fig. 71. — United first 292 PRIMARY FACTORS OF ORGANIC EVOLUTION. gravity, remains to fill the grooves, and to form the keels which we observe. (See Fig. 72.) There is another striking instance of the same kind in the feet of Mammalia ; that is, in the development of the keels and grooves which ap- pear at the articulation of the first set of bones of the toes (metapodials)with the bones of the second set (phalanges). These keels first appear on the posterior side of the end of the first set of bones, pro- jecting from between two flexor tendons. These ten- dons, in many mammals, con- tain two small bones, one on each side, each of which acts like the knee-pan, and resem- bles it in miniature, which are called sesamoid bones. These tendons and bones exercise a constant pressure on each side of the middle line, when the animal is running or walking, and this pressure, together with the concussion with the ground, appears to have permitted the protru- sion of the middle line in the form of a keel, while the KINETOGENESIS. 293 lateral parts have been supported and even com- pressed. The reptilian ancestors of the mammals do not possess these keels. Now, I have shown that the lines of mammalian descent displayed by paleontology are characterized, among other things, in most instances, by the gradual elevation of the heel above the ground, so that the animal walks on its toes. It is evident that in this case the concussion of running is applied more directly on the ends of the bones of the foot than is the case where the foot is horizontal. As a consequence we find the keel is developed farther forward in such ani- mals. But in many of these, as the Carnivora, hip- popotamus, and the camels, there is developed under the toes a soft cushion, which greatly reduces this con- cussion. In these species the keel makes no further progress. In other lines, as those of the horse, the pig, and of the ruminants, the ends of the toes are ap- plied to the ground, and are covered with larger hoofs, which surround the toe, and the cushion is nearly or quite dispensed with. These animals are especially distinguished by the fact that their metapodial keels extend entirely round the end of the bone, dividing the front, as well as the end and back (Fig. 71) ; since the front of the metapodial is out of the reach of the sesamoid bones, its keel would seem to be a mould- ing to the groove of the first phalange, which is itself moulded by the middle and posterior part of the meta- podial keel (Wortman.) A third and similar example is furnished by the elbow-joint of the Quadrumana and Diplarthra. In the lower Mammalia, including the Carnivora (Fig. 73), the distal end of the humerus presents a subme- dian groove, which receives the ulna, and on the inner 294 PRIMARY FACTORS OF ORGANIC EVOLUTION. side of it, a more or less convex surface, which is ap- plied to the head of the radius. The coronoid process of the ulna is narrow, and its dense bounding walls impinge on the broad face of the humeral condyle in flexion and extension, and transfers to it the force of impact when the foot strikes the ground. In either case strong pressure has been brought to bear on the humeral condyle, and it has yielded to the denser body of the ulna, thus forming the groove in question. In such Mammalia the effect of impact of the limb on the ground has been to impress the head of the radius on the humeral condyle upwards. The dense edges of the former have im- pressed themselves on the latter, while the unsupported middle portion has yielded in the direc- tion of gravity, and the result is what we find, i. e., a cup-shaped surface of the head of the radius, and a convexity of the humeral condyle adapted to it. Among specializations of the elbow-joint, I call attention to two. In Quadrumana the head of the radius, probably owing to continued supination of the manus, occupies a position at the external side of the coronoid process of the ulna, and impinges on the outer part of the condyle of the humerus. The con- cavity of its head, and the convexity of the humeral condyle, are visible as before, but a prominent tongue or keel, which has been called the intertrochlear crest, hyena) seen from behind ; h, humerus ; r, radius ; «, ulna. Original. KINETOGErNESIS. 295 separates the ulnar and radial surfaces of the humerus (Fig. 74). This keel occupies the groove or interval which separates the head of the radius from the coro- noid process of the ulna. It is plain that we have here another tongue and groove-joint, produced by the mu- tual adaptation of parts under strain, pressure, and impact. The other extreme of elbow-joint is found in that of the diplarthrous Ungulata (Fig. 75). Here the head of the radius, while retaining its normal position on the inner side of the fore-arm, is extended to the external side of the ulna and even beyond it, adapting it- self to the entire width of the humeral condyles. The same structure is found in the spe- cialized forms of both series of Diplarthra, the Perisso- dactyla and Artiodactyla. This expansion of the head of the radius appears to be in di- rect relation to the duration through long geologic ages Fig. 74.— Elbow-joint of chim- of the impacts which have Panzeefrombe affected the limbs of these, the swiftest of the Mam- malia. That the head of the radius should be spread so as to fit the entire surface of the humerus, under all circumstances, seems to be a mechanical necessity. But in addition to this we find a tongue- and-groove adaptation, in which the crest (which I have called the trochlear crest) articulates with a groove in the head of the radius. The internal articulation of the humerus with the radius has the usual form, convex and con- cave distad. The trochlear crest marks the external border of the olecranar groove of the humerus. But 2g6 PRIMARY FACTORS OF ORGANIC EVOLUTION. the external part of the humeral condyles is converted into a roller which is set off from the trochlear crest by the abrupt contraction of its diameter ; while the cor- responding part of the head of the radius projects to fit it exactly. A probable explanation of the form of this roller may be derived from a consideration of the almost identical structure of the meta- podio-phalangeal articulation of the Artiodactyla. The internal and external sides of the distal metapodial condyles are not sim- ilar, the external being more strongly impressed than the in- ternal (Fig. 77D). This is simply due to the unequal pressure ex- erted on the two extremities of the condyle by the phalanges, owing to the divergent direction of the digits when serving as a support. In the distal end of } the humerus the same effect is Fig. ys.-Efbow-oim of seen> the external part of the con- eiaphus (red deer) dyle nearly resembling the corre- sponding part of the metapodial bones. This is traceable to the same cause, viz. : the divergent position assumed by the fore arm on the hu- merus, when the weight is supported on one fore leg only. This brings the line of pressure through the ex- ternal part of both the head of the radius and the hu- meral condyle (Fig. 77 A). That the higher ungulates are "knock-elbowed" may be readily observed by watching their gaits (Fig. 76). KINE TOGENESIS. 297 A distinct consequence of combined impact and strain is seen in the evolution of the carpus and tarsus of the Diplarthra. In primitive Mammalia, as in most Unguiculata, the bones of the carpus and tarsus succeed each other in such a way that the principal lines of separation be- tween the elements coincide in the two rows, thus producing a linear relation be- tween the former. In the Diplarthra, on the other hand, the ele- ments of the two rows alternate with each other so as to produce a strong interlocking. I have shown that in the primitive Ungu- lata, the Taxeopoda, the linear arrange- ment is observed, while in three orders of ungulates, the Pro- boscidea, Toxodontia, and Amblypoda, there are various degrees of alternation intermediate between the linear type of the Taxeopoda and the completely interlocked condition of the Diplarthra. It has been already pointed out in the chapter on phylogeny that the taxeopodous type Fig. 76. — Cervus canadensis in motion : from Muybridge's Animal Motion ; showing the " knock-elbow" position of the fore leg, in both plantation and recover. 298 PRIMARY FACTORS OF ORGANIC EVOLUTION. of foot preceded the diplarthrous in time. Besides the alternation mentioned, it is quite general in both types for the metapodial bones to possess a facet for con- tact with that element of the carpus and tarsus next exterior to the one to which they have their principal articulation. From these facts it is evident that the bones of the second carpal and tarsal rows have, in Fig. 77. — Cervus elaphus; A, B, C, humero-radial articulation ; A and B, with the radius in position; C, with radius twisted; D. £, metatarsophalan- geal articulation ; D, front ; E, distal view, twisted. the process of evolution, assumed a position interior to their primitive position, with reference to the first row proximad to them, and the metapodials distad to them. The cause of this shifting of position is to be found in the movements of the limbs in progression, and especially in rapid progression (Fig. 78). If we observe the movements of the limbs in a KINE TO GENESIS. 299 diplarthrous ungulate, we shall see that as the foot is planted on the ground the prominent flexures of the limbs, the elbow and gambril joints, are turned in- follex Index X&JA -inn? Mininf Index Sled* Fig. 78. — Diagram of carpus of a Taxeopod (A) and (B) of a diplarthrous ungulate. From Osborn. wards, so that the limb, were it free from the ground, would be twisted or rotated on its long axis from within, forwards and outwards. As the foot rests on Fig- 79- — Raccoon pacing, showing right fore foot just before recovery. From H. Allen. the ground, the limb experiences a torsion strain in the directions mentioned. This throws the weight on the interior bones of the lower legs, the radius and the tibia. Thus these bones have acquired a great supe- 300 PRIMARY FACTORS OF ORGANIC EVOLUTION. riority in dimensions over the external elements (ulna and fibula) in all the Diplarthra. The bones of the inner side of the first carpal and tarsal rows have thus transmitted an ever-increasing share of the impact, as the radius and tibia have developed, and have grown Fig. 80. Fig. 81. Fig. 80. — Rhinocerus unicornis carpus. Arrow ending in P, line of impact in plantation ; do. ending in A', line of strain in recover. Fig. 81. — Eguus cabaUus forefoot. Sc, scaphoid; L, lunar; Cu, cunei- form; Toz, trapezium and trapezoideo ; Un, unciform ; ing., magnum-. with their growth at the expense of the external ele- ments, the cuneiform in the carpus, and the calcaneum in the tarsus, which have become very narrow elements in the higher Diplarthra. As the pressure has been obliquely from within outwards, the growth of the proximal elements, the scaphoid and lunar in front, 302 PR IMA RY FAC TORS OF OR GA NIC E VOL UTION. and the astragalus behind, has been in the same direc- tion. It has been shown by Dr. H. Allen that just before the recover of the foot, the latter is directed outwards from a line parallel with the axis of the body, so that the weight falls on the inner part of the sole of the former. This naturally causes the bones of the foot to press inwards on the heads of the metapodials, so that the latter tend to grow outwards on the second tarsal row. In this way were produced the facets on the external side of the heads of the metapodials. Thus is accounted for, on simple mechanical princi- ples, the phenomenon of carpal and tarsal displace- ment exhibited in its highest development, by the Dip- larthra. It is significant that diplarthrism has not appeared in mammals which possess an elastic pad of connec- tive tissue on the soles, as in Unguiculata generally, and especially in the Carnivora. Diplarthrism is pres- ent in the camels, which have a pad, but I have shown that this pad did not appear until a comparatively late geologic epoch, and long after diplarthrism had be- come established in the camels' ancestors, the Poe'bro- theriidae. The faceting of the head of the astragalus as the result of impacts, is seen on comparison of the astra- gali of Phenacodus and Hyracotherium in Ungulata (Figs. 33-35), and of Dissacus and Mesonyx among the Creodonta. In this last genus we have the only faceted astragalus among carnivorous mammals, but this genus is at the same time subungulate. b. The Forms of Vertebral Centra. The mutual articulations of the vertebral column are those of the centra and of the zygapophyses. Many KINETOGENESIS. 303 important modifications in these articulations are to be seen in Vertebrata, the Reptilia presenting the great- est variety, excepting in the zygapophyses, which are tolerably uniform in that class. In the Mammalia, modifications of the central articulations are not more striking than are those of the zygapophyses. The forms of central articulation are four, viz. : the amphicoelous, the ball-and-socket, the plane, and the saddle-shaped. The first type is only seen in a very imperfect degree in Mammalia and in but very few vertebrae, where it is indeed but a modification of the plane. The ball-and-socket is chiefly found in the neck of the long-necked Mammalia, as the higher Diplarthra, and to a less degree in their lumbar re- gions, while the dorsal vertebrae present an approach to the same type in the same groups. The saddle- shaped centrum is only found in Mammalia in the necks of certain genera of monkeys. The majority of Mammalia present the plane articulation of all the ver- tebral centra. In Mammalia in which movement of the vertebrae on each other has become impossible, the centra co- ossify, as for instance in the sacrum. In this region the number of vertebrae coosified is directly as the length of the iliac bone, which supports and holds them im- movable. Such is their condition throughout the dorsal region in the extinct Edentata of the family Glyptodontidae, where the carapace is, as in the tor- toises, inflexible, and which therefore limits the possi- bility of motion of the vertebral column. Another illustration is seen in the necks of the balaenid Ceta- cea, and to some degree in the Delphinidae and Physe- teridae. The lack of present mobility of this part of the column is due to its extreme abbreviation, a char- 304 PRIMARY FACTORS OF ORGANIC EVOLUTION. acter which has been gradually developing during Ce- nozoic time ; since the earliest Cetacea had consider- ably longer necks than the later ones, and had their vertebral centra distinct. It appears to me probable that the shortening was the result of disuse. This disuse would arise from gradually increasing powers of locomotion through the water, a progress, which, judging from the character of the limbs of the Zeuglo- don, was evidently made after the time of the Eocene. The increase of speed would enable the animal to over- take and capture its prey, without the necessity of using a long prehensile neck in seizing it in the pur- suit. The ball-and-socket articulation of the vertebrae is well known to be the predominant condition in the Reptilia, and the fact that it is necessarily associated with the flexibility of the column is equally well under- stood. The flexibility is directly as the weakness of the limbs, for in the large and long-limbed terrestrial Reptilia of the order Dinosauria, the vertebral articu- lations of the dorsal region, at least, are plane. That it is chiefly confined to, and best developed in, the most flexible regions, i. e., the cervical and lumbar, of the column of the Mammalia, also shows this neces- sary connection. There can be no doubt but that the ball-and-socket vertebral articulation has been pro- duced by constant flexures of the column in all direc- tions, as has been suggested by Marsh. iii. INCREASE OF SIZE THROUGH USE. Under this head I enumerate examples where the mechanical causes in operation are less self-evident than those included under the preceding section. They KINE TO GENESIS. 305 are, however, probably due to the same process, viz., impact and strain. a. The Proportions of the Limbs and of Their Segments. The length of the legs of terrestrial Mammalia has increased with the passage of time. The inferior types of Mammalia now existing, as Marsupialia, Glires, Insectivora, Edentata, have short legs, with a few cases of extreme specialization as exceptions, such as kangaroos, rabbits, and jerboas (hiad legs only), the Dolichotis patachonica, the Rhynchocyonidae, and the sloths. In the orders which stand at the summit of the series, as the Diplarthra, Proboscidia, Carnivora, and Anthropomorpha, the legs are much increased in length, and this is especially marked in certain forms which stand in all respects at the summit of their re- spective orders. Thus in Diplarthra, the deer, ante- lope, and horse are distinguished for length of limb ; in the Proboscidia, the elephant ; in the Carnivora, the large cats and hyaenas ; in the Anthropomorpha, the fore limbs are long in all, the hind ones especially so in man. The cause of this elongation is apparently use. It is the hind legs that are elongated in a straight line in animals that walk on them, as man ; and both, in those that walk on both, as the elephant. In animals that leap with the hind legs these are still more elongated, and are folded when at rest, and rapidly extended when in motion. In animals that climb with the fore legs, these are elongated, as in the Anthropomorpha, except man. In those that climb with all fours, all are elongate, as in the sloths. It must be remembered that these elongations are the sum of increments added one to the other through long ages of use in geologic 306 PRIMARY FACTORS OF ORGANIC EVOLUTION. time. The mechanical character of that use has not been identical. It is of two principal kinds, viz. : im- pact and longitudinal strain. These two forms of en- ergy move in directions opposite to each other ; the one as compression in the direction of the length of the bone ; the other, as a stretching in the direction of the length of the bone. Both processes alike appear to have stimulated growth in the direction of the length of the bone. The increase in the length of the legs has not been always due to increase in length of the same segment. In a majority of the higher mammals, the increase has been principally in the foot, and especially in the meta- podials and digits, producing digitigradism. In the forms which have remained plantigrade, the femur (Proboscidia), or femur and tibia (Quadrumana), or all three segments (Tarsius), have been the seat of the elongation. We can again trace these especial elonga- tions to special uses. In animals which leap, the dis- tal segments of the limbs are elongated ; in those which do not leap, but which merely run or walk, it is the proximal segments of the limbs which are elon- gated. Animals which run by leaping are divided into those which run and leap with all fours, as Diplarthra ; and those which run and leap with the posterior limbs only, as the jerboas and kangaroos. In both types, the distal segments of the hind limb are elongated, and in the Diplarthra, those of the fore limb also. , Animals which do not leap in progression (ele- phants, Quadrumana, bears) are always plantigrade, and have very short feet, but elongate thighs, and, mostly, tibias. These facts show that those elements which receive KINE TOGENESIS. 307 the principal impact in progression are those which increase in length. In digitigrade animals it is the feet which receive the impact of the repeated blows on the Mb i Fig. 83. — Pes of (A) Merychochcerus montanus from Scott ; (B] Bos taurus, much reduced. Co., Calcaneum ; As, Astragalus; Na, Navicular; Neb, Na- viculocuboid ; Cu,Mec, Ecto-mesocuneiform ; Mt, Metatarsals (cannon bone); Enc, Entocuneiform. earth while in progression, while supporting the weight of the body at every stage of the process. In planti- grade animals it is the soles of the feet, and the bones of the leg in line with them, which receive the impact, 3o8 PRIMARY FACTORS OF ORGANIC EVOLUTION-. KINETOGENESIS. 309 while the feet beyond this point receive none, and do not support the body, except very partially at the mo- ment of leaving the earth. b. The Number of the Digits. The reduction in the number of toes is supposed to be due to the elongation of those which receive the greater number of strains and impacts in rapid pro- gression, and the complementary loss of material available for the growth of those not subject to this stimulus. This is rendered probable from the fact that the types with reduced digits are dwellers on dry land, and those that have more numerous digits are inhabitants of swamps and mud, or are more or less aquatic. That this inequality is due to these mechan- ical causes is still further indicated by the fact that in those forms where the soles are thickly padded (Car- nivora, Proboscidia) the reduction has either not taken place, or has made little progress, amounting to the loss of only one digit. (An apparent exception in the case of the camels will be mentioned later.) A still more important body of evidence which shows that the inequality in size and number of digits is due to impacts and strains unequally distributed, has been brought forward by Ryder. He points out that defi- nite results are to be observed in those limbs of a given type of animal which experience correspondingly defi- nite influences ; while in the limbs where the strains are equal, the modifications do not appear. Examples of this kind are to be found in the unguiculate Mam- malia and in the Marsupialia. Thus in the jerboas which use the hind limbs in leaping, these only dis- play reduced digits, the fore limbs remaining of prim- 310 PRIMARY FACTORS OF ORGANIC EVOLUTION. itive character. The same is true of the kangaroos. In digging genera, the fore limbs experience the modi- 0 Fig. 85. — A, Right posterior foot of Prothippus sejunctus Cope, from Colo- rado, about one-half natural size. From U. S. Geological Survey of Territo- ries, F. V. Hayden, IV. B, Right posterior foot of Poebrotherium labiatum Cope, from Colorado, three-fifths natural size. From Hayden's Report, IV., Plate CXV. fications, while the hind limbs are more normal, as in Chrysochloris and various Edentata. KINETOGENESIS. 311 Ryder sums up the evidence in two propositions, as follows : l "I. The mechanical force used in locomotion dur- ing the struggle for existence has determined the digits which are now performing the pedal function in such groups as have undergone digital reduction. "II. When the distribution of mechanical strains has been alike upon all the digits of the manus or of the pes, or both, they have remained in a state of ap- proximate uniformity of development." The application of the impact, or strain, or both, in progression, is easily understood. In recover (see p. 299), the leg is bent on the foot as it rests on the ground, and those digits which then leave the ground last, sustain greater strain than those which leave it sooner. In replacing the foot on the ground (planta- tion), those digits which strike it first experience greater force of impact than those which strike it later. Sup- posing the five primitive digits to have been of equal length, the distribution of the impact and of the strain will depend on the angle at which the foot is directed with reference to the direction of motion. If the feet are pointed forwards, the middle digits will experience strain and impact ; if outwards, the inner digits bear the weight ; if inwards, the external digits receive it. Observation on five-toed plantigrade mammals shows that their feet are turned neither inwards nor outwards in progression, but straight forwards. It is probable that the primitive Mammalia moved in the same manner. This is also to be inferred from the fact that they were plantigrade, so that the leverage transversely in or out which results from the elevated heel of the digitigrade leg was very much less in them. ^American Naturalist, 1877, p. 607. 3i2 PRIMARY FACTORS OF ORGANIC EVOLUTION. In progression of this type, the middle digits of course leave the ground last and strike it first. Thus the middle toes have been stimulated at the expense of the lateral ones, so that in the Diplarthra, either the mid- die one (Perissodactyla) alone remains, or the middle two (Artiodactyla). In the kangaroos the external toes have been chiefly used, so that the fourth and fifth digits have been principally developed. In man, who KINETOGENESIS. 313 now turns his feet out when using them as bases of re- sistance to muscular labor, the inner digit has become most robust. The mechanical history of the human great toe is however yet unknown. As regards the equal development of the third and fourth digits in the Artiodactyla, as distinguished from the development of the middle digit of the Perisso- dactyla, I have advanced the following hypothesis. I have supposed that the primitive members of this for- mer division sprung from pentadactyl plantigrades who dwelt in swamps and walked on very soft ground. The effect of progression in mud is to spread the toes equally in all directions and on each side of the me- dian line. Such feet remain in the mud-loving hippo- potamus, and to a lesser degree in the true pigs. From such ancestry the cloven-footed Diplarthra derived their characters. The Hyracotheriinae, the ancestors of all Perissodactyla, display on the other hand evi- dence of a life on harder ground, especially in the pos- terior foot, where articulations are already rigidly de- fined, and the third digit is longer than the others. Some of their descendants love swamps, as one or two species of tapirs and rhinoceroses, but others live on the dryest ground, as the Andean tapir and the African rhinoceros. As to the highest members of both even and odd toed groups, the Bovidae and the Equidae, their habitat is in the vast majority of cases the dry land (Figs. 80-81). Continued and excessive prehensile strain with weight on the longest digits, must be assigned as the cause of the especial elongation; and disuse as the cause of the loss of the external and shorter digits, of the sloths ; so that there remain but two and three (Cholrepus and Bradypus), and in the climbing ant- 3i4 PRIMARY FACTORS OF ORGANIC EVOLUTION-. eater (Cycloturus) but one principal toe and two rudi- ments. The excessive strain and impact experienced by certain digits in leaping, accounts for the digital reduction in the hinder foot of the kangaroos and jer- boas, precisely as in the perissodactyle ungulates. c. The Horns. Horns are developed in Mammalia and other Ver- tebrata on similar parts of the skull, principally on the posterior lateral angles, as in various Batrachia, Rep- tilia, and Mammalia, and on the nose, as in a few Mammalia and several reptiles, recent and extinct. These parts are the ones which are especially brought into contact with resisting bodies ; the nose in pushing a path or way for the head and body; the lateral occi- pital region in defence and assault, when the sensitive nose and eyes are protected by being held near the ground. In the latter position the posterolateral an- gles, when present, receive more frequent collision with, and vigorous stimulation from, a body attacked or resisted, and in accordance with the observed re- sults of irritation on dermal and osseous tissues, addi- tional matter has been deposited. In Lacertilia and Batrachia Salientia there are distinct posteroexternal cranial angles ; in Batrachia Urodela such angles are less prominent. In unguiculate Mammalia and in all others with a sagittal crest there are no such angles ; hence this type of skull has never developed posterior horns. The rhinoceros has developed the dermal nasal horn, and the Elasmotherium, a median osseous horn, since posterolateral angles of the skull are want- ing or close together. In the Dinocerata and the Ar- tiodactyla, where the temporal crests are lateral, leav- ing a wide fronto-parietal plane with posterior lateral KINETOGENESIS. 315 angles, horns are developed. In members of both groups horns have been developed over the orbits also (Fig. 87), and in the Dinocerata on the extremities of the nasal bones as well. These growths are all on parts which are subject to especial irritation by contact with other bodies, animate and inanimate. Among Artiodactyla, the deer (Cervidae) are espe- cially distinguished by the periodical shedding of all but the bases of their horns. Extinct forms found in the Upper Miocene of the United States and France (the Loup Fork series) furnish the explanation of the origin of this remarkable peculiarity. In the genus Cosoryx we find that the horns may or may not pos- sess a burr near the base of the beam, like that of the deer ; the same species being indifferently with it or without it. This observation has been made on three species, — the C. necatus, C. furcatus and C. ramosus. The following explanation of these facts has been pro- posed by myself.1 "From the facts of the case the following inference may be derived, premising that it is very probable that a genus allied to the present one has given origin to the family of the deer. It is ob- vious that the horns of (Dicrocerus) Cosoryx did not possess a horny sheath as in the Bovidae, from the fact of their being branched. As the sheath grows by ad- dition at the base, the presence of branches which necessarily obstruct its forward movement, would be fatal to the process. There is much to be said in favor of the view that the horns were covered with an integu- ment, probably furred, as in the giraffe and young stage in the deer. Thus there are grooves in the sur- face of the beam for superficial blood-vessels, which 1 U. S. G. G. Survey West of the tooth Mer., G. M. Wheeler : IV., Paleon- tology, 1877, p. 348. 316 PRIMARY FACTORS OF ORGANIC EVOLUTION. must have been protected by skin (I do not observe these grooves on the beam of C. teres}. The retention of the broken extremity of an antler, so as to be re- united, as described (Fig. 87, C), could not have been accomplished without an integument. The presence of the burrs cannot be accounted for on any other supposition, as there are no foramina to give exit to nutrient vessels at the point where they exist; the irregularity of those positions also forbids the latter idea, and adds to the probability that the arteries which furnished the deposit of phosphate of lime were contained in a super- ficial dermal coating. The supposition is also strengthened by the fact that the only existing ruminants (the giraffes) Cosoryx ramosus Cope; C, antler broken with permanent u. s. GO-V. Geoi. Expi. tooth Mer., G. M. without horny sheaths have them covered with hairy skin. " It appears that in the antlers of the Cosoryx the deposit of a burr was immediately associated with the death of the portion of the horn beyond it, so that it disintegrated and disappeared. This was not the case with the beam in the specimens observed. Neverthe- KINETOGENESIS. 317 less it is probable that the death of the horn would be associated with the deposit of the burr in this case also, were the conditions the same. What those con- ditions were we can only surmise. It was very prob- ably the death of the integument which invested and nourished the horn that produced that result ; and this would more readily occur in the exposed antlers than in the more protected basal portion of the beam. It is very probable that this result would follow blows and laceration of the surface received during combat, or accidental contact with hard substances. The in- tegument would be stripped up to near the junction of the antlers with each other, or of the beam with the cranium, and the arteries would be constricted or closed at those points. It is near these junctions that all of the burrs are found. But as such lesion would be necessarily less complete at the point where the horn has greatest circumference, so the entire death of the horn might be less usual than that of the branches. Should such lesions have occurred for a long period at the breeding season, nature's efforts to repair by redeposit of bony tissue might as readily be- come periodical as the increase in size and activity of the reproductive organs and other growths which char- acterize the breeding season in many animals. The subsequent death of the horn would be at some time followed by its shedding by the ordinary process of sloughing." Cosoryx is not the true ancestor of the Cervidae, as its teeth have already attained the prismatic type of the higher Bovidae. But Blastomeryx is most prob- ably the ancestor of the deer. The remains of this genus occur with those of Cosoryx, but the burr has not yet been observed on its horns. 318 PRIMARY FACTORS OF ORGANIC EVOLUTION. IV. THE MECHANICAL ORIGIN OF DENTAL TYPES. In investigating the origin of dental types it is necessary to become acquainted with the nature of the mutual movements of the series of the opposing jaws. I have classified them as follows : * I. Inferior molars work within superior molars, but not between them. Psalidodect mastication. 1. The inferior molars shear on the interior side of the su- perior : Triconodontidce. II. Part or all of inferior molars work alternately to and between superior molars. Amoebodect mastication. 2. The inferior molar shears forwards on the superior mo- lar. Proterotome mastication : Creodonta; Carnivora. 3. The inferior molars shear posteriorly against the superior molars. Opisthotome mastication : Coryphodontidcz, Uintatheriidce. III. Molar teeth of both jaws oppose each other. Antiodect mas- tication. 4. The movement of the lower jaw is vertical. Orthal mas- tication : Suo'idea, Tapiridce. 5. The movement of the lower jaw is from without inwards. Ectal mastication : many Peris sodacty la. 6. The movement of the lower jaw is from within outwards. Ental mastication : most Artiodactyla; some Perrissodactyla. 7. The movement of the lower jaw is from before backwards. Proal : some Monotremata Multituberculata and most Glires. 8. The movement of the lower jaw is from behind forwards. Palinal : Proboscidea (Ryder). The distinction of teeth into incisors, canines, and molars appears independently at various points in the line of Vertebrata. Incisors and molars are distin- IMechan. Origin Hard Parts of Mammalia, 1889, p. 226. KINETOGENESIS. 319 guished in sparoid fishes, and in placodont and dia- dectid reptiles. Canine-like teeth, or pseudo-canines, appear in clepsydropid and crocodilian reptiles, and in saurodont fishes. Canine-like incisors appear in the Clepsydropidae. The variety of character in these structures presented by the Mammalia to be consid- ered is great, and the principles deduced from obser- vation of them are applicable to the Vertebrata in general. As mechanical causes of the origin of dental modi- fications, I have enumerated the following : 1. Increase of size of a tooth, or a part of a tooth, is due to increased use, within a certain maximum of capacity for increased nutrition. 2. The change of direction and use of a tooth take place away from the direction of greatest, and in the direction of least resistance. 3. It follows, from their greater flexibility, that crests of crowns of teeth yield to strains more readily than do the cusps. 4. The increase in the length of crests and cusps in all directions, and therefore the plications of the same, is directly as the irritation from use to which their apices and edges are subjected, to the limit set by the destructive effects of such use, or by the re- cuperative energy of nutrition. 5. The direction of growth of the branches of a V, or of the horns of a crescent, will be the direction of movement of the corresponding parts of the opposite jaw. Before giving a review of the various dental types of Mammalia, I wish to describe some special exam- ples where the effect of mechanical causes is most ob- vious. I therefore first repeat the observation of Ryder 320 PRIMARY FACTORS OF ORGANIC EVOLUTION. as to the origin of the selenodont molars of the Artio- dactyla ; and my own as to the origin of a similar structure in the molars of certain multituberculate Pro- totheria. In the former the mastication is ental ; in the latter it is proal, as shown by Osborn. In the accompanying figure from Ryder the move- ments of the lower jaw in mastication of lophodonts, are diagrammatically represented, a represents the movement in Carnivora, and in the orthal bunodonts, as the pigs, b shows a slight lateral movement be- lieved by Ryder to exist in the wart hog (Phacochoa- a t> Fig. 88. — Diagram of excursion of lower jaw in mastication; from Ryder; a-b, orthal ; c-f, ental. rus). c represents the movement in kangaroos, pha- langers, and tapirs. In d a theoretical intermediate movement is represented, such as Ryder supposed to have characterized the Anchitherium. In e the usual movement among ruminants is depicted, as is seen in the deer, etc. In / the wider excursion of the jaw is that seen in the giraffe, camel, and ox. In these move- ments from b to/, the lower jaw is moved transversely across the upper jaw from one side to the other. Some of the Diplarthra masticate on one side of the jaw when performing this movement, and some on the other. That is, in passing the lower jaw across the face of the upper, some masticate the food on the side KINE TO GENESIS. 321 where the external face of the lower jaw crosses the upper jaw from within outwards (ental); while in other types the food is masticated on the side where the lower jaw passes the external edge of the upper jaw from without inwards (ectal). While masticating with one side of the jaws, the opposing dental series of the other side are not in contact. All mutual effect of the teeth of one jaw on the other could therefore appear on the side temporarily used for mastication only. Among recent Un- gulata the rumi- nants present the ental mastication ; the rhinoceros and horses, the ectal ; and rodents, the proal. Ryder is of the opinion that the mastication of the Proboscidia is pali- nal, but I have not been able to satisfy myself of this. When the crests of the inferior molars were devel- oped, their relation to the crests of the superior molars was always anterior in mastication. That is, the in- ferior crest, in the closing of the jaw, collides with the crest of the upper molar, with its posterior edge against the anterior edge of the latter. This is because : first, as to position, the two anterior cusps of the lower molar are the remains of the anterior triangle which fit originally between two superior molars, and be- cause, in the closing of the jaw, these cusps continue to hold that position ; and second, as to function, be- Fig. 89.— Cervus, molars : a, superior, exter- nal view ; b, do. inferior view; c, inferior molars, superior view ; from Ryder. 322 PRIMARY FACTORS OF ORGANIC EVOLUTION. cause the canine in the ungulate series diminishes in size, and does not, therefore, draw the inferior molars forwards by wedging on the superior molar, as in the Carnivora, but allows free scope to the posterior trac- tion of the temporal muscle in its exercise on the lower jaw. In those forms which masticate from the inside out- wards (the ental type), the cusps of the inferior molars, passing between those of the superior molars, would tend to flatten the sides on which they exerted fric- tion, and to extend those sides outwards beyond the median apex of the cusp. (Fig. 90.) The result would be, and taking into view the yielding of the tissue to Fig. 90. — Cusps of superior premolars and molars : «, external cusps of molar of Sarcothraustes ; b, of Phenacodus ; c, of Anthracotherium ; d, of Oreodon ; e, half of inferior molar of Cervus;/", superior premolar of Cory- phodon ; from Ryder. such strain, has been, to modify the shape of the cusp by pushing its side walls, so that a horizontal section of it would become successively more and more cres- centic. The effect on the inferior teeth would be to produce the same result in their external cusps, but in the opposite direction. The sides of the cusps would be pushed inwards, past the apex, giving a crescentic section more or less perfect, as the operation of the cause had been of long or short duration. The result of the lateral movement in mastication may be under- stood by reference to the accompanying cut, Fig. 91. The external crescents of the inferior molars (<£) are seen to pass between the internal crescents of the K1NE TOGENESIS. 323 superior molars (a). The mutual interaction and effect on the form of the crescents may be readily under- stood. In Fig. 90 the successive stages of this effect Fig. 91 — Two true molars of both jaws of a ruminant : a, superior molars, their inner crescents ; b, inferior molars, their external crescents ; the arcs show directions of motion of jaws in mastication; from Ryder. on one or two cusps may be seen, beginning with a cone (#) and terminating with crescents (ef). Thus is the origin of the selenodont dentition of the highest Fig. 92. — Transverse vertical sections of superior molar teeth, showirg transition from bunodont (A) type to lophodonts (B, C). A, Sus erymanthius. B, Ovis amaltheus. C, Bos taurus. From Gaudry. Letters : d, dentine ; e, enamel ; c, cementum. artiodactyle explained by Ryder, and, I believe, cor- rectly. Kowalevsky and I have shown that the types with selenodont (crescent-bearing) molars, have descended 324 PRIMARY FACTORS OF ORGANIC EVOLUTION. from tubercle-bearing (bunodont) ancestors. This de- scent has witnessed an increased depth of the infold- ing of the crown, as represented in the accompanying figure. Now, in the table of masticatory types above given it is shown that in the bunodont type of the Suoidea the mastication is orthal, and a gradual in- crease in the length of the lateral excursions of the lower jaw has been shown to have resulted in the ental mastication. Thus has structure kept pace with func- tion in the evolution of the selenodont dentition. Fig. 93.— Chirox plicatus Cope, palate and molar teeth from below, three- halves natural size. From Puerco bed of New Mexico. From American Nat- uralist, 1887, p. 566. The general structure of the dentition in the Proto- theria Multituberculata is similar to that of the Glires. The incisors in the Plagiaulacidae, Chirogidae, and Poly- mastodontidae have structure and functions generally similar to those of that order. The result in the form and function of the molar dentition has been sim- ilar to that observed in the Glires. The postglenoid process is probably absent in these animals ; in any case the mandibular condyle is rounded, and is not transverse. Prof. H. F. Osborn has pointed out to me that mastication was performed by a fore-and-aft K1NE TO GENESIS. 325 movement of the inferior molars on the superior in Plagiaulacidae. This was no doubt the case in the oth^r families named. The molar teeth of the lower types, as Tritylodon from the Trias, present conical tubercles in longitudinal series, two in the lower and three in the upper jaw. The two series of the lower jaw alternate with the three in the upper jaw, moving in the grooves between the latter, while the three se- ries of the upper molars reciprocally embrace the two of the lower molars. This is demonstrated by the mutual wear of the tubercles seen in Ptilodus and Chirox (Fig. 93). The trituration was probably the same in Tri- tylodon, but in Polymastodon the increased thickening of the tubercles prevented their interlocking action in masti- cation. In this genus the tu- bercles Slid OVer each Other, f\^.g^.— A, Meniscoessus conquis- and truncated the apices ^ cope, last two superior molars. from the Laramie of Wyoming, Until in Old Specimens they twice natural size. B, Meniscoessus, were entirely worn away. In second species' from Osborn' Meniscoessus (Fig. 94) and Stereognathus we have an interesting illustration of the effect of the action of cusps on each other when under prolonged mutual lateral thrust. Their external sides have been drawn out into angles in the direction of thrust, converting their transverse sections from circles to crescents. As the thrust is in the Multituberculata longitudinal, the crescents are transverse to the axis of the jaw. In the selenodont Artiodactyla, where the thrust is transverse to the line of the jaw, the crescents are longitudinal. That similar effects should accompany similar move- 326 PRIMARY FACTORS OF ORGANIC EVOLUTION. ments in two groups of Mammalia so widely separated as these two is strong evidence in favor of the belief that the two facts stand in the relation of cause and effect. I now present an example of the effect of strain, as shown by the direction of the inferior incisors of the lemurine Quadrumana. These teeth project horizon- tally from the extremity of the mandible, so as not to oppose the superior incisors, in consequence of which they are useless as organs of prehension. But they Fig- 95- — Lemur collaris, dentition from below and above ; natural size ; original. are used by their possessors as a comb for the fur, drawing them from below upwards when thus employ- ing them. The strain is always in one direction, and must have resulted in developing the procumbent posi- tion which they now display (Fig. 95). This is a di- rect deduction from the fact that the incisor teeth are similarly displaced by the pressure of the tongue in cases of the abnormal enlargement of that organ in man. I now describe the general character of mammalian dentition, with the view of pointing out how strong, in KINETOGENESIS. 327 the light of the facts already cited, is the evidence of their origin through mechanical strains and impacts. a. The Origin of Canine Teeth. The origin of canine, pseudo-canine, and canine- like incisor teeth is due to the strains sustained by them on account of their position in the jaws at points which are naturally utilized in the seizing of prey, or the fighting of enemies. In some reptiles (Dimetro- don) the end of the muzzle has been utilized ; in croco- diles, the side of the jaw ; while the intermediate position has been most used by Mammalia. The rea- son why the canine instead of the incisor teeth have been selected by carnivorous Mammalia for prehensile purposes is not at present clear to me. In accordance with Rule I., its increased size has been due to the especial and energetic strains to which it has been subjected while in use as a prehensile or offensive weapon, when buried in the body of its prey or enemy. The superior canine would acquire larger size earlier in time than the inferior canine, since it bears the greater part of such strain, as attached to the more fixed head and body of its possessor. The anterior teeth of the lower jaw would be less available for use, since they offer weaker and less fixed resistance to the opposing body. That the first tooth behind the canine was not generally enlarged is (under I.) due to the fact that its posterior position prevents it from having the same amount of use, and experiencing the strain that a tooth more anteriorly placed necessarily re- ceives. It is excluded from considerable use by the projecting muzzle above and in front of it. That it was not drawn out into a horizontal position was due to the presence of teeth anterior to it. 328 PRIMARY FACTORS OF ORGANIC EVOLUTION. That the increased size of canine teeth is due to strains is strongly indicated by the huge development of these teeth in the walrus. This animal uses its ca- nines for the breaking of ice, and for lifting itself from the water on to the edge of strong ice. The fact that canines and not incisors have been thus developed is a necessary result of the fact that the walrus is a de- scendant of a line of animals which had already re- duced "incisors and larger canines. b Fig. 96. — Esthonyx burmeisterii Cope, dentition: «, profile; b, superior; c, inferior dentition, grinding faces. Reduced. b. Development of the Incisors. The history of the incisor teeth of the Mammalia exhibits three processes, viz. : hypertrophy (e. g. Glires), specialization (e. g. Galeopithecus, Lemur- idae), and atrophy (e. g. Booidea, Phacochcerus, Glos- sophaga, etc.). KINE TOGENESIS. 329 Of hypertrophy we have two types : the first repre- sented by the Glires, Multituberculata, Tillodonta and their ancestors; and second, by the Proboscidia, the narwhal and certain Sirenia. As the uses of the inci- sors present two types corresponding with their struc- ture, we have ground for believing the uses in question to have been the efficient agent in producing the lat- ter. Esthonyx furnishes us with an example (Fig. 96) where all the incisors are present in the lower jaw, and a Fig. yj.—Psittacotherium multifragum Cope, mandibular ramus, one-half natural size ; a, profile ; b, from above. where the function of one pair of them (the second) has evidently been partially rodent in character; that is, it has served as a scraper and gouger of food sub- stances. Persistent use has apparently developed the size of this pair of teeth, until we find in Psittacothe- rium (Fig. 97) they have reached a greater efficiency, and that the external incisors of the lower jaw have disappeared. This disappearance can be accounted for on the ground of disuse, a retirement from service due to position, and the increased growth of incisor 330 PRIMARY FACTORS OF ORGANIC EVOLUTION. No. 2. In Calamodon the first incisor has become ru- dimentary from the same cause, and in Anchippodus it has disappeared altogether, leaving a truly rodent incisor dentition, consisting of the second incisors only, in the lower jaw. Continued use as chisels has developed these teeth to the great proportions seen in such Glires as Castoroides, etc. (Fig. 107). The use which the Proboscidia and Sirenia (Hali- core) give their incisors, is, from a mechanical point of view, like that which the Carnivora give their ca- nines ; that is, it consists of impacts in the long axis, and strains transverse to the long axis of the tooth. The elephants use their tusks for prying up the vege- tables on which they feed, or for pushing aside the vegetation through which they wish to pass. The an- cestors of the Proboscidia are not certainly known, but they possessed incisors of enlarged proportions, such as we find in the Toxodontia and other late rep- resentatives of some of the primitive Ungulata. Use of such teeth in the manner referred to, without oppo- sition from the inferior incisors, will account for the tremendous proportions which they ultimately reached in some of the species of Elephas. The use made by the narwhal of its single huge superior incisor, that of an ice-breaker, indicates the origin of its large dimensions. So with the straight incisors of the hippopotamus; use as diggers has straightened them to a horizontal from their primitive vertical direction, a change which is also partially ac- complished in the true pigs (Sus). In the Sirenian genus Halicore the upper incisors have been used in excavating vegetable growths from the banks and bottom of shallow seas. The transition from three incisors (Prorastomus) to two (Dioplothe- KINETOGENESIS. 331 rium), and to one (Halicore), is identical with what has taken place in the Proboscidia and Glires, and has resulted in the production of an effective digging- tool. In other genera it ma)' be supposed that their habits of browsing on soft growing materials did not necessitate the use of digging incisors, hence these teeth became atrophied, as in the manatee and Rhy- tina. c. Development of Molars. In fishes and reptiles where teeth occasionally pre- sent very primitive conditions, the theory of the origin of particular types of molar teeth is more simple than in the case of Mammalia. The observations of Hiiter on the action of osteoblasts under stimulus show that under moderate irritation osseous tissue is deposited, while under severe pressure osseous tissue is removed. Koelliker has shown that the action of these bodies is the same in dentine as in true bone. Hence modifica- tions of dental structure must stand in close relation to the uses to which they are put. Thus severe pressure on a simple tooth crown would, if long continued, cause it to expand laterally, or in the direction of least re- sistance, and to grow but little in its vertical axis, i. e., in the direction of greatest resistance. The molar teeth have been subjected to much more severe direct irritation from use than any others in the jaws, and this will account for their increased diameters. In the case of the eutherian Mammalia, molar teeth are not traceable back to ancestral types of reptilian mo- lars, but to simple conic (haplodont) reptilian teeth. The process of the evolution of the complex mamma- lian molars from these, forms the subject of a paper in the American Journal of Morphology for 1889, from which I quote extensively in the present work. 332 PRIMARY FACTORS OF ORGANIC EVOLUTION. I have there shown that the greater number of the types of this series have derived the characters of their molar teeth from the stages of the following succes- sion. First a simple cone or reptilian crown, alternat- ing with that of the other jaw (haplodont type). Sec- ond, a cone with lateral denticles (the triconodont type). Third, the denticles to the inner or outer side of the crown, forming a three-sided prism, with tritu- bercular apex, which alternates with that of the oppo- site jaw (tritubercular type). Fourth, development of a heel projecting from the posterior base of the lower jaw, which meets the crown of the superior, forming a tuberculosectorial inferior molar. From this stage the carnivorous and sectorial dentition is derived, the tritubercular type being retained. Fifth, the develop- ment of a posterior inner cusp of the superior molar and the elevation of the heel of the inferior molar, with the loss of the anterior inner cusp. Thus the molars become quadritubercular, and opposite. This is the type of many of the Taxeopoda, including the Quadrumana and Insectivora as well as the inferior Diplarthra. The higher Taxeopoda (Hyracoidea) and Diplarthra, add various complexities. Thus the tu- bercles become flattened and then concave, so as to form V's in the section produced by wearing ; or they are joined by cross-folds, forming various patterns. In the Proboscidia the latter become multiplied so as to produce numerous cross-crests. d. Origin of the Carnivorous Dentition. The anterior cusplet of the triconodont crown is (Fig. 98 A), in the upper jaw, the paracone, and in the lower jaw the paraconid ; and the posterior cusplet is the metacone or metaconid, respectively. As the prin- KINETOGENESIS. 333 cipal cusps, or protocone and protoconid, alternate with each other, the cusplets stand opposite to them in the closing of the jaws, and a certain amount of interfer- ence results. As the lesser cusps are the less resistant to the wedging press'ure of such contact, their position would change under its influence, rather than the large central cusps. The lower jaw fitting within the upper, the effect of the collision between the major cusps of the one jaw, and cusplets of the other, would be to emphasize the relation still more ; that is, the cusplets of the upper jaw would be wedged outwards, while those of the lower jaw would be pressed inwards, the major cusps retaining at first their original alternate position. With increase of the size of the teeth the cusps would soon assume in each jaw a position more or less transverse to that of the other jaw, producing, as a result of the crowding, a crown with a triangular section in both. The process may be rendered clear by the following diagram : B C Fig. 98. — Diagrammatic representations of horizontal sections of tricuspi- date molars of both jaws in mutual relation ; the shaded ones represent those of the upper jaw: A, Triconodon ; B, Menacodon ; C, ideal tritubercular mo- lars, approached by Menacodon, B. It is supposed on the contrary by Rose and Kiiken- thal that mammalian molars which support more than one cusp have been formed by the fusion of several simple reptilian cones. So far as regards the higher Mammalia this hypothesis is in opposition to all the facts of paleontology and is not worthy of discussion. 334 PRIMARY FACTORS OF ORGANIC EVOLUTION. The only question that can arise is with reference to the origin of the multituberculate molar of the Proto- theria. It is further questioned by Forsyth- Major, whether the tritubercular molar has been derived from the tri- conodont. He believes, on the contrary, that it is de- rived from the multitubercular type by reduction. There are two objections to this view : (i) the cones of the tritubercular tooth or trigon should be subequal, were they derived from a multitubercular source. On the contrary, the two external cones of the upper, and the two inner cones of the lower series are in the earliest (Jurassic), as well as most of the tritubercular types, smaller than the single opposite cusp or proto- cone, precisely as are the anterior and posterior cones of the triconodont molar. (2) No paleontologic series from the multitubercular to the tritubercular types has been traced, while the series from the triconodont to the tritubercular is well known. Forsyth-Major's evi- dence that such a transition exists in the Glires, is better explained by tracing the moderate complexity he describes to a tritubercular origin. It is also alleged by Allen and Scott that the inter- nal cusps of the premolars, when present, originate by the development of internal cingula, and have no prim- itive tritubercular ancestry. The evidence at our dis- posal from paleontological sources is in favor of this view; hence it is reasoned that the history of the mo- lar teeth must have been identical. This however does not follow, especially as the paleontologic evidence points the other way. The history of the two series has been different. In the first place the premolars have been subjected to much less use than the true molars ; hence they retained the primitive reptilian KINETOGENESIS. 335 simplicity for a much longer period, a simplicity which they retain in the Carnivora, except the J-, which be- came the sectorial. Secondly, the premolars, instead of increasing in size, have in many types decreased ; the Diplarthra alone presenting an exception to this rule. That the internal cusps of the premolars may have arisen by growth of cingula in this order, is by no means improbable. We seem to have here an excel- lent illustration of the origin of two identical struc- tures by different evolutionary routes. The first modification of the tritubercular molar of the lower jaw is the addition of a low cingulum at the posterior base. This is seen in a rudimentary condi- tion in various living species of the Centetidae and Chrysochloridse of the insectivorous order (Fig. 100); but in these existing forms the superior molar has added a posterior cingulum also, which widens inter- nally, or towards the palate (Fig. 101). In the evolu- tion of the dentition, the inferior posterior cingulum, or " heel, "was developed first, as in the Deltatherium, Centetes, and Stypolophus (Figs. 99, 100, 102), where it is quite large ; while the superior cingulum is want- ing in Stypolophus and Didelphodus, but is present in a very rudimentary condition in Deltatherium fundami- nis. In all of these genera the external cusps of the superior series have been pressed inwards, and more or less together, and are therefore removed in this re- spect from the primitive condition. The more primi- tive state of the superior cusps is seen in some species of Mioclaenus, where, however, a posterior cingulum may be developed. The primitive type of tritubercular superior molar is that of Sarcothraustes, and in the same genus the inferior molar only differs from the primitive type in having a well-developed heel. Among 336 PRIMARY FACTORS OF ORGANIC EVOLUTION. recent Mammalia the carnivorous and insectivorous Marsupialia generally have the tritubercular lower mo- lar with heel. In the Chiroptera and many Insectivora the heel is largely developed, and supports two cusps, as it does in some Creodonta. - 99- — Deltatherium fundaminis Cope, fragmentary skull, two-thirds natural size ; from the Puerco bed of New Mexico. a,b, c, from one individ- ual; d, from a second animal; a, right side of cranium; b, palate from be- low ; c, mandible, part from above ; d, left ramus, outer side ; from the Re- port of the U. S. Geol. Surv. Terrs., Vol. III. From this point the evolution of the tritubercular molar must be considered from two standpoints. The first is the mechanical cause of the changes of its form ; and the second is the mechanical cause of its definite KINE TOGENESIS. 337 location in a particular part of the jaw. For it has been already stated that in the evolution of the secto- rial dentition of the Carnivora, the number of molars and premolars has considerably diminished, while those that remain have become relatively much larger. In the tritubercular dentition the crowns proper of one jaw alternate with those of the other (Fig. 100); but when heels are added in either jaw, they will op- pose such part of the crowns of the teeth in the oppo- Fig. loo.—Centetes ecaudatus: A, skull, side seen obliquely from below; B, superior molars from below ; C, inferior molars from above. site jaw as comes in contact with them when in use. The development of the heel in the inferior molars produced a type which is known as the tuberculosec- torial. This type characterizes the Creodonta and a few Carnivora. In the former there are generally three such teeth, in the latter but one. In the tuberculosectorial type of inferior molar the primitive tritubercular part of the crown (trigonid of Osborn) stands principally anterior to the posterior 338 PRIMARY FACTORS OF ORGANIC EVOLUTION. root of the tooth. It appears that the posterior root has been extended backwards, so as to occupy a posi- tion below the middle of the superior molar, while the tritubercular crown has been confined to the space be- tween the crowns of the superior molars. This would follow of necessity from the alternating action of the crowns of the opposite series, in connection with a general increase in size of the teeth. In the opening of ,/»fiir Mikroskopische Anatomte, 1880, XVII, pp. 241-243, PI. XXVII. Ryder, American Naturalist, 1888, p. 547. 404 PRIMARY FACTORS OF ORGANIC EVOLUTION. primitive Glires. The removal of the enamel from the apices of the tubercles and crests of their descendents is due to the abrasion consequent on ordinary use. On this Ryder (/. *•.) remarks : ' ' The great value which is to be attached to the fact that abrasions of the enamel of the adult, which have reacted upon the functional activity of the enamel organ of the embryo rat, so that such mechanically induced alterations could be inherited, does not consist so much in the proof it affords that mutilations can be inherited, as it does that mutilations incurred in the ordinary struggle for existence, may, under certain conditions in certain practically feral species, be transmitted." Having shown by these examples that acquired characters can be inherited, I offer some other illus- trations which are at hand. b. Arthropoda. It has been already rendered probable if not certain (p. 268) that the segments of the body and limbs of the Arthropoda were originally produced by the movements of definite tracts on each other, during the period that the external surfaces were becoming hardened by chi- tinous or calcareous deposits. It is well known that this segmentation is no longer produced by this mechanical cause during the adolescent or any other post-embry- onic stage of the life of the individual, but that it ap- pears during the various stages of embryonic life, and is therefore inherited. Thus segmentation of the body appears in the embryo while still attached to the yolk. During the larval life of many insects the process of segmentation is suspended, but during the repose of pupal life, it goes on with great rapidity. In this stage while protected from external mechanical stimuli, the HEREDITY. 405 limbs with their specialized segments are fully devel- oped, so that the individual is mature as it issues from its prison. This illustration of inheritance derives its point in the present connection from the fact that it presents an example of the inheritance of characters which were plainly acquired by mechanical stimuli during post-embryonic life of the primitive ancestors of the Arthropoda. 3. EVIDENCE FROM PALEONTOLOGY. a. The Impressed Zone of the Nautiloids. I have already quoted Professor Hyatt on the par- allelism which is characteristic of the various series of nautiloid Cephalopoda, as discovered by paleontologic research. (P. 182.) The impressed zone is a character which has been produced by mechanical causes (pres- sure), and Prof. Hyatt has observed cases where this acquired peculiarity has been inherited in instances where the mechanical cause which produced it no longer existed. He describes these instances as follows i1 "The characteristic dealt with in the paper of which this is an abstract, is of essential importance among nautiloids and ammonoids or all of the Cepha- lopoda having chambered shells and living within their shells. It consists mainly of an impression made on the inner side or dorsum of each outer whorl during the coiling up, as the whorl grows and is moulded over the venter or outer side of the next inner whorl. "This matter will be better understood, if a short description is given of the following figures. Fig. 115 shows an almost complete fossil cast of a full grown I American Naturalist, 1893. October, p. 865. Professor Hyatt has person- ally looked over and corrected these quotations. 406 PRIMARY FACTORS OF ORGANIC EVOLUTION, Metatoceras cavatiformis Hyatt, and some of the lines or sutures made in the external surface of the cast by the intersections of the partitions or septa that cut up the coiled tube of the living shell into air cham- bers. Fig. 116 shows a broken specimen of the same species, but with the outer and older whorls in large part removed. The innermost septum near the center of the coil was built across the interior after the animal had constructed the hollow apex or point. It then moved along, adding to the external wall of the tube, Fig. 115. which has been destroyed and removed from this cast, and built the second septum, and so on until it reached the tenth septum. By some freak of fossilization a number of the septa beyond this have been destroyed, so that if we were to remove the fragment of the ex- ternal whorl and take out the center which has just been described, this would have the exact aspect of a cast of a young shell with ten air chambers.1 The IThe shaded area in the center, shaped like a large inverted comma, was an open space in the living shell. This is almost invariably filled by the HEREDITY. 407 eleventh air space or chamber being open and without divisions would then appear to be the living chamber which the animal occupied when it built the tenth sep- t Is— Fig. 116. turn. Normally the shell really continued to progress from the tenth septum by additions to the outer wall and put in new septa behind it, together with the con- Fig. 117. necting tube until it reached s', and finally the las* septum, Is. This one, Is, was really the last one built rocky matrix in which the shells occur and is often, as in this specimen, al- lowed to remain. See also 4, 5, 6, of Fig. 119, which show the comma shaped umbilical perforations or openings left at the center through the crytoceran form of the young. 4o8 PRIMARY FACTORS OF ORGANIC EVOLUTION. and it formed the floor of a true living chamber, U, formerly occupied by the animal at the time of its death and burial in the sediment of the carboniferous period. Fig. 115 shows a similar fossil but with a longer, although still incomplete living chamber. If the external wall of shell had been preserved none of these structures could be seen. Fig. 117 shows a fossil Temnochilus crassus, a shell of the same family, with this external wall preserved, and all these internal structures covered up. The impressed zone is the reentrant curve shown in all these figures and especially marked in the lower outline of an outer whorl of another carboniferous species, Metacoceras dubium Hyatt, Fig. 118, im. z. "It is not necessary to go into a discussion of the details of internal structures and their relations to the impressed zone in this abstract, but it is essential to give a general description of the morphogeny of the order of nautiloids. "This group of chambered Cephalopods contains the following classes of forms : first, straight, conical shells, type Orthoceras, Fig. 119, No. i; second, curved cones, Cyrtoceras, Fig. 119, No. 2 ; third loosely coiled, open whorled cones, do., No. 3; fourth, coiled cones with the whorls more or less enveloping, do., No. 5. The fourth and fifth forms are usually included in the old genus, Nautilus. Practically, it is better to designate the first class as orthoceran, the second as cyrtoceran, the third as gyroceran, and the fourth and fifth as nautilian. In tracing genetic series through HEREDITY. 409 ? time they are found to diverge in their evolutibn, start- ing with the orthoceran and passing through jteirallel lines of forms, many of the genetic series havrng in succession cyrtoceran, gyroceran, and even nautilian forms of the fourth and fifth classes. Others, are not so perfectly parallel, stopping short with the\ cyrto- ceran class of forms or the gyroceran. Many also begin with cyrtoceran shells, while others diverge from the gyroceran, and still other series have only nautilian shells of different grades of close coiling and m\olu- tion. ''The application of the law of repetition in here ity to the chambered shell-covered cephalopods, shows that the straight orthoceran shells, Fig. 119, No. i, were repeated in the young of the curved cyrtoceran forms, Fig. 119, No. 2, and these forms in their turn in the young of the gyroceran forms, Fig. 119, No. 3 ; and this may be seen by comparing the young or api- cal part of each shell represented in outline with the full-grown shells of the preceding figures. The apex of No. 2, with the whole of No. i ; the apex of No. 3, with the whole of No. 2. It will be understood, of course, that the figures in outline represent full-grown shells, except when otherwise explained, and that they were built like the shells of Nos. 1-2, by an animal living in their interiors and adding band after band of shelly matter to the exterior, but in these outlines the shell is supposed to be perfect and the internal struc- tures concealed.1 The young of Fig. 119, No. 4, which represents the fourth class of forms repeats the cyrtoceran form, then curves more closely, and just before it comes in contact there is a short time when 1 Except in No. 9, in which a portion of the shell is broken away, showing the cast of the interior and the sutures. V/sOi Fig. 119.— Hyatt on Cephalopoda. HEREDITY. 411 EXPLANATION OF FIG. 119. LETTERING. a. Apex of shell. This usually bears a scar on the point, as shown in Nos. 14 and 15, but this has no bearing on the question discussed, and has not been described. This also represents the youngest (nepionic) or cyrto- ceran stage in the growth of the shell, No. 8 being a young shell with complete living chamber. This letter also indicates the location of the sections corre- spondingly lettered in the figures. b is used to indicate the section of the cyrtoceran stage in Nos. 11-13. b' is used to indicate the place of the sections, Nos. 4-5^', upon the whorls of Nos. 4-5. They were taken through the whorl in the gyroceran stage. c is used for the adolescent fneanic) stage of growth in the whorl and the corresponding sections. c' is used for the full-grown (ephebic) stage in the growth of the whorl and the corresponding sections. dior the first part of the senile (gerontic) stage. e for the final and most degenerative part of the senile stage. iz for the impressed zone. v venter or outer side of the shell, the dorsum being the inner side of the whorl. •w for the whorls, thus i w in Nos. 3 and 4 means the end of the first whorl, zwMhe beginning of the second whorl, 3 w that of the third whorl. These letters serve to show the progressive increase in numbers of the whorls in the different classes of forms. FIGURES. No. i. Outline of an orthoceran shell. No. 2. Outline of cyrtoceran shell. No. 3. Outline of gyroceran shell. No. 4. Outline of nautilian shell, having a larger umbilical perforation at (a) and fewer whorls at the same age, than in No. 5 ; in other words, it is less tightly and completely coiled up than the class of shells represented by that figure. No. 5. A nautilian shell with tighter coils than in No. 4 and the whorls coming in contact and the impressed zone beginning at an earlier stage. No. 6. Barrandeoceras bohemicum (sp. Barrande) Hyatt, showing the most involute of the Silurian shells so far as known ; No. 6 is reduced in size, but the section No. 7 is natural size. No. 8. A young shell of the same, natural size, with complete living chamber. Nos. 9-10. Coloceras globatum (sp. De Koninck) Hyatt, adult. No. 9 has a part of the outer shell broken off, showing the edges of the septal partitions (sutures) as lines on the strong cast of the interior. Nos. 11-13. Same to show the cyrtoceran stage and section, with its im- pressed zone. No. 14. Cenoceras clausum, Hyatt. Nos. 15-16. Nautilus pompiiius, to show the cyrtoceran stage with its im- pressed zone. 4i2 PRIMARY FACTORS OF ORGANIC EVOLUTION. it overlaps the ,apex without touching it. At this time it is plainly gyroceran, like the whole of No. 3. After it touches the first whorl just beyond the apex it re- mains in contact, and the inner side or dorsum of the second or overlapping whorl begins to show a flatten- ing as a result of this collision of the whorls. The sec- tions of the orthoceran, cyrtoceran, and gyroceran whorls show no such flattening in any of the speci- mens examined, although hundreds of different kinds have been studied. The sections are designated on the plate by the same letters as the supposed lines of the sections made through the tube, and although dia- grammatic figures, they give a sufficiently clear gen- eral explanation of the facts observed. More specific figures could have been given in abundance and will be given in the paper now in course of preparation.1 "Fig. 119, No. 5, shows the same phenomena as No. 4. The young is at first cyrtoceran like the adult whorl of No. 2, and open, then becomes gyroceran in curvature and finally overlaps the apex when it has arrived at the end of the first volution, but does not at first touch it. Then coming into contact it acquires a flattened area or faint impressed zone on the dorsum or inner side of the second volution, as is shown in the section No. 5^. This is similar to the section of No. 4 shown in No. 4*:', which represents a cut through an adult whorl of the fourth class of forms. It differs only in being smaller, on account of the younger stage of growth at which it occurs. "The entire series of forms from orthoceran to nau- tilian is more or less represented, even in the earliest period at which the nautiloids appear, namely, in the ISee "Phylogeny of an Acquired Characteristic," Hyatt, Proceed tugs, American Philosophical Society, Philadelphia, XXXII., No. 143. HEREDITY. 413 rocks of the Quebec group. There is, however, this qualification : the fifth class of forms, or the involute nautilian, are relatively rare and become more abun- dant in successive periods. The young of nautilian shells of the earlier periods are also apt to be less closely coiled, or, in other words, remain open and similar to cyrtoceras for a longer time during their growth. This is shown by the large size of the central hole, or um- bilical perforation, left in the center of full-grown shells. This perforation is much larger, as a rule, in Paleozoic than in the Mesozoic forms. ''In each period the genetic series or groups of nau- tilian forms have peculiarities of structure in the su- tures, ornaments, apertures, etc., by which they can be separated from each other, and these peculiarities are the same as those possessed by gyroceran, cyrto- ceran, and often orthoceran shells which occurred often earlier in time, so that one can trace each group of nautilian shells back to its ancestors through the par- allel stages of evolution above described. The groups, in other words, are parallel in their morphogenesis, like two individuals of the same parents in their de- velopment from youth to old age. "As a general rule the impressed zone originates, as described above, after the whorls come in contact, rarely before this time in the growth of any individ- uals. Barrandeoceras is one of the most involute shells known in the Silurian, and Fig. 119, No. 6, gives a true sketch of this species ; No. 7, shows a section of a full-grown shell with a decided impressed zone, and No. 8 is the young. This last is a purely cyrtoceran form with a compressed elliptical section like that of No. 7, but no impressed zone, the inner side being rounded like the diagram of Cyrtoceras, No. 2. The 4i4 PRIMARY FACTORS OF ORGANIC EVOLUTION. impressed zone is not present in the young of Ophidi- oceras, the closest coiled of all these forms, nor in the young of most species of the Silurian before the whorls touch, and all of the species likely to present this pecu- liarity have been investigated. "The impressed zone is also, as a rule, lost in the oldest stage of the whorl of every individual when the whorls cease to continue to grow in contact. This condition is represented in the last part of the outer- most whorl of Nos. 4 and 5 in sections, Nos. 4*?, 5 220. Chondrotus tenebrosus, 58, 59. Chordata, 86, 205, 215, 218. Chorology, 387. Chrysochloridae, 335. Chrysochloris, 310. Cicindela, variations in, 25. Ciona intestinalis, 456. Cladodus, 100. Clarke, 176, 191. Claus, 211. Clepsydropidae, 319. Climatius, 92. Cnemidophorus, 199 ; color-variation of, 41. Cnemidophorus deppei, 41 ; C. gra- 536 PRIMARY FACTORS OF ORGANIC EVOLUTION. hamii, 46; C. gularis, 41, 46, 200; C. costatus, 46; C. scalar is, 46, 200 ; C. semifasciatus, 43, 46 ; C. mariarunt, 41, 45 ; C. sexlineatus, 41, 46 ; C. ter- sellatus, 41, 46; C. melanostethus, 46 ; C". perplexus, 46 ; C. rubidus, 45, 46 ; C. septemvittatus, 46 ; C. vario- losus, 46. Coassus, 196. Cobitis, 363. Cobra de capello, 22. Coelacanthidae, gi. Cceleoterata, 79, 81, 82, 83, 250. Coelogasteroceras canaliculatum, 421. Cohesion, 484. Colaptes auratus, 52. Coleoptera, 203. Colocephali, 104, 106. Coloceras globatunt, 4, 16. Color changes, in Lepidoptera, 230; in cocoons, 440; in birds, 238: in fishes, 499; in tree-frogs, 499. Color variations, in the genus Cicin- dela, 25 ; in Osceola doliata, 29 ; in Cnemidophorus, 41. Colostethidae, 78. Columba livia, 21. ^-—Complementary growth-energy, 248. — Conditions of inheritance, 438. Condylarthra, 84, 85, 132, 133, 134, 135, 141, 143, 157, 356, 357. 359, 388. Coniferae, 77. ..^-Conscious energy, 507. Consciousness, 495, 505. Consciousness and automatism, 495. Conversion of Artemia into Branchi- ata, 229. Cope, E. D., 8, 528. Copepoda, 211. Cophylidae, 70. Copperhead, 22. Corvus amerzcanus, 52. Coryphodon, 354. Coryphodontidae, 318. Cosoryx, 315, 317. Cosoryxfurcatus, 315 ; C. necatus, 315; C. ramosus, 315 ; C. teres, 315. Cossus ligniperda, 237. Costa Rica, 50. Cotylosauria, 87, 88, 113, 115, 122, 172. Crangon, hand of, 274. Craniomi, 100. Creodonta, 336, 337, 338, 339, 341, 343, 388. Cretaceous, 139, 143, 184, 189, 419, 420, 421, 422. Cricotus crassidiscus, HI. Crioceras, 189. Crocodilia, 94, 114, 116. Crocuta ntaculata, 294. Crossopterygia, 100, 101. Crotalus horridus, 22. Crustacea, 211, 271, 273. Cryptopnoy, 494. Ctenophora, 272. Ctetology, 192. Cunningham, J. L., 238, 527. Cyanurus cristatus, 52. Cyclops, 212. Cyclopterus, 108. Cycloturus, 314. Cymatoceras elegans, 418. Cynodictis geismarianus, 341. Cynognathidae, 88. Cypraea, 260. Cypraeidae, 261. Cyprinidae, 103. Cyrtoceras, 185, 408, 413. Cystignathidae, 65, 70, 71. Cystignathus pachypus, 390. Dall. W. H., 10, 58, 255, 520, 530, 531. Dama, 196. Darwin, C., 3, 4, 5, 6, 7, 14, 231, 247, 248, 249, 385, 387, 398, 474, 48o. Darwin, E., 10, 505. Daubentonioidea, 128. Degeneracy, 247; in birds, 126; in plants, 76 ; in reptiles, 122 ; in crus- tacea, 211 ; in mollusca, 213; in vertebrata, 215. Delphinidae, 303. Deltatheriutn fundaminis, 335. Dendrobatidae, 70. Dendrophryniscidae, 70. Dentition modification, in Canidae, 59 ; in Felidae, 60 ; in Homo, 60, 61 ; in lemurs, 61 ; in lower placenta! mammals, 61 ; in monkeys, 61. Depuy, 430. Dercetidae, 104. ' Descartes, 498. INDEX. 537 Designed action in animals, 500. Devonic period, 77, 91, 101, 172, 184, 186, 188, 362, 415, 420, 422. Diadectidae, 89. Diadiaphorus, 359. Dibamidae, 123. Dicrocerus, 315. Didelphodus, 335. Didymium squamulosum, 220. Digits, number of, 309. Dimorphodon, 120. Dimya, 267. Dinocerata, 314, 315, 356. Dinosauria, 98, 114, 116, 120, 121, 122, 304, 372. Dioplotherium, 330. Diplarthra, 84, 128, 133, 136, 143, 144, 146, 293, 295, 297, 300, 302, 305, 306, 312, 313, 320, 332, 360, 403- Diplogenesis, 12, 441, 443, 470. Dipneusta, 89. Dipnoi, 89, 99. Diprodontidae, 143. Diptera, 203, 204. Dipus, 361. Disciniscus, 177. Dissacus, 302. Disuse in Mammalia, 352. Dog-opossum, 22. Dohrn, 204. Dolichotis, 361 ; D. patachonica, 305. Dollo, 121. Domestic fowls, 21. D'Orbigny, 417. Dorypterus, 103. Driesch, 457. DuBois, Dr., 159, 168, 169. Dume"ril, 58. Dynamical evolution, 524. Dyscophidae, 70. Dysodus, 59, 146. Echidermata, 368. Echinodermata, 80, 81, 82, 83. Echinus, 457. Ectal mastication, 318. Edaphoceras, 186. Edentata, 127, 132, 133, 138, 141, 143, 145, 186, 195, 303, 305, 310, 356, 360. Education, 505. Eels, 103. Effect of feeding on color in birds, 238. Effect of light on the colors of flat- fishes, 238. Effects of consciousness, 509. Efficient cause, 10, 497, 498. Eigenmann, C-, 244. Eimer, 23, 45, 252, 254, 527. Elasmobranchii, 91, 94, 95, 99. Elasmotherium, 314. Elbow-joint, of Cervus elaphus, 296; of chimpanzee, 295 ; of horse, ab- normal, 278 ; human, abnormal, 277. Elephas, 145, 330. Elliot, D. G., 531. Elosia nasus Licht, 68. Embolomeri, 88, 109, uc. Embryology, 202, 209, 401. Embryonic variations, 444. Emphytogenesis, 486. Endoceras, 186. Endolobus, 186; E. excavatum, 417. Energies, specific, 480. Energy, 448, 451, 506, 507, 512; synop- tic table of, 484; anagenetic, 478, 484 ; definition of, 473 ; of evolu- tion, 473 ; catagenetic, 479, 484 ; cor- relation of, 506 ; inorganic, 475, 484, 512 : composition of, 490. Engystomidae, 70. Enhydra, 352. Ental mastication, 318. Entoconcha mirabilis, 213. Environment, physical influences of, 436, 452, 475. Eocene, 61, 104, 135, 138, 139, 142, 143, 145, 147, 150, 154, 155, 173, 205, 304- 365, 377- Epigenesis, 13. Epihippus, 147, 148. Epilasmia, 107. Epilepsy in Cavia, 430. Equidae, 313. Equilibrium, 508. . Equus, 145, 149, 359 ; E. caballus^ 84, 300. Ergogenesis, 486. Erinaceus, 127. Erismatopterus, 104. Eryops megacepalus, 371. Esquimaux, 61, 153. 538 PRIMARY FACTORS OF ORGANIC EVOLUTION. Esthonyx, 329. Eudoceratidae, 186. Euprotogonia, 147. Europe, 55, 160, 426, 427. Europeans, 166. Europeo-Americans, 153. Eurypharyngidae, 104. Eusophus nebulosus Gir, 68. Eusthenopteronfoordii, 91. Eutaenia, 63 ; E. saurtta, 21; E. sirta- lis, 21, 63. Eutheria, 373. Evolution, science of, 22. Expression points, 25. Faxoe, 418. Feet of Chinese women, 399. Felidae, 48, 49, 145, 342. Felis, 339. Felis concolor, 49 ; F. dontestzca, 21 ; F. pardalis, 50. Fellahs, 163. Ferns, 77. Pick, R., 283, 284, 286, 377, 528. Firmisternia, 64, 70, 71, 196, 197, 389, 390. Fisher, 91, 99, 101, 104. Fishes, ancestral type of, 86, 91, 99. Fistularia, 104. Flatfishes, 238. Flexure, 368. Florida, 52, 56. Flossensaum, 243. Forel, 463. Forsyth-Major, 334, 469. Fraipont, 160, 161, 165, 166, 170. France, 83, 170, 315. Friction, 279, 519, 378, 490. Fuligo, 503. Functions of consciousness, 495. Fungi, 70, 219. Furcifer, 197. Fttsus parilis, 257. Gage, 363. Galeopithecus, 328. Gallinae, 391. Gallus sp., 21. Galton, Dr., 12, 471. Ganocephali, no. Garman, S., 241. Garter-snake, 21. Gasterosteidae, 104. Gastraea theory, 202. Gastrechmia, 63. Gastropoda, plaits in shell of, 255. Gazella dorcas, 301. Gebia, 273. Gecconidae, 73, 88, 122. Gegenbaur, 91, 366. Gelocus, 312. Genealogy, of man, 171 ; of the horse, 146. Genesiology, 192. Geomyidae, 352. Giard, 527. Glauconiidae, 121. Gleditschia, 228. Glires, 51, 127, 132, 133, 135. HI. *43, 305. 3i8, 324, 328, 329, 330, 331, 334. 345. 346, 360, 361, 404- Glochidia, 203. Glossophaga, 328. Glossophaginae, 356. Gloxinia, 384. Glyptodontidae, 303. Gobius, 499. Goethe, 247. Gonagenic variations, 444. Goniatitinae, 186, 187, 188, 422. Gravitation, 484. Growth-energy, 449, 473 ; G. force, 484. Gulick, 388. Gulo luscus, 50. Gunther, 123, 390. Gwynia, 178, 179. Gymnosperms, 79. Gyroceras, 185. Haeckel, E., 7, 8, 85, 88, 89, 154, 169, 175, 201, 202, 387, 448, 454. Halicore, 330, 336. Hall, 176. Halloceras, 186. Hamites, 189. Hapalidae, 141. Haplodoci, 106, 107. Haplomi, 103, 104, 106. Harpa, 261. Hawaiian Islands, 388. Heliotropism, 503. INDEX. 539 Hemibranchii, 104, 106. Hemimantis, 71. Hemiphractidae, 71. Henke, 277, 283, 528. Henslow, G., 23, 226, 227, 228, 383, 384, 527- Herdman, 215. Heredity, 398. Hering, 492. Hertwig, 456, 457. Hesperornithidae, 124. Heteroglossa, 71. Heterologous series, 71. Heteromorphosis, 455. Heterosomata, 105, 106. Hilgard, S. W., 433. Hinnites, 267. Hippocampidae, 105. Hippopotamidae, 69. Hippopotamus, 330, 402. Hippotherium, 84, 149, 359 ; H. medi- terraneum^ 84. H6ffding,498. Holocephali, 99. Holoptychiidae, 91. Holostei, 101, 102. Holostomi, 106. Hominidae, 157. Homo, 155, 158, 169, 170. Homogeneous series, 71. Homogeny, 72. Homologous, series, 71. Homology, 19. Homo neanderthalenszs, 170; H. sa- piens, 170 ; H. erectus, 169. Homoplassy in Mammalia, 72, 357. Homoplastic series, 71. Hoplobatrachus, 71. Horn, G. H., 25, 29. Horns, 314 ; of Cervus elaphus, 197. Horse, evolution of trotting, 426; H. phylogeny of, 146, 522. House-fly, 254. Hunger, '504. Hurst, C. H., 205, 207. Huter, 251, 275. 276, 331. Huxley, 89, 99, 476. Hyaenidae, 145, 342, 343. Hyaenodon, 343. Hyatt, A., 8, 9, 10, 175, 182, 183, 201, 202, 266, 268, 405, 420, 451, 520, 528, 529, 530, 531- Hybodus, 372. Hybopsis biguttatus, 22. Hydroids, 82. Hydrotropism, 501. Hyla, ii, 198, 199 ; H . carolinensis, 499; H. gratiosa, 499. Hylella, 71, 198, 199. Hylidae, 65, 70, 198. Hylobates, 159. Hymen, 399. Hymenoptera, 82, 903. Hyopotamus, 312. Hyperolius, 71. Hypothesis of the origin of the divi- sions of the Vertebrata, 362. Hypsiboas donmercii D. and B., 68; H. punctatus Schu., 68. Hyracoidea, 132, 133, 141, 143. 332. Hyracotheriinae, 313. Hyracotherium, 147, 148, 302. Hystricidae, 351. Ibacus, 274. Ichthyocephali, 106. Ichthyopterygia, 113, 116, 121. Ichthyornithidae, 124. Ichthyosaurus, 121. Ichthyotomi, 100. Icichthys, 108. Icosteus, 108. Iguanidae, 73. Impact, 277, 284, 287, 291, 302, 305, 311, 485- Impressed zone of the nautiloids, 405. Increase of size through use, 304. India, 159. Indo-Europeans, 153. Inexact parallelism, 200. Influence, of external stimulus on mo- tions of animals, 496 ; of the mental condition of the mother on the fos- tus, 434, 451 ; of mind on coloration, 499; of mind on matter, 498. Infusoria, 79, 511. Inheritance, of acquired characters, 401, 405 ; of characters due to dis- ease, 430; conditions of 438, 440, of exercise of function, 426; of mu- 540 PRIMARY FACTORS OF ORGANIC EVOLUTION. tilation and injuries, 399, 431 ; of nutrition, 423; of regional influ- ences, 435, 440. Insecta, 213, 226. Insectivora, 136, 140, 143, 305, 332, 336, 361. Intelligence, animal, 500, 504. Introduction, i. Ischyromystypus, Leidy, 351. Ismenia, 178, 179. Isolation, 387. Isospondyli, 103, 106. Jackson, R. T., 10, 191, 261, 520, 531. Jaeger, 10. Japanese spaniel, 60. Java, 160. Java man, 169. Jayne, H. Dr., 60. Jordan, Dr., 101. Joseph, Dr., 242. Judgment, 504, 506. Juglans m'gra, 466; J. regia, 466. Jura, 122, 139, 140, 142, 143, 184, 188, 417, 418, 419, 420, 421. Katabolism, 481. Kinetobathmism, 485. Kinetogenesis, 225, 246, 287, 375, 496 ; in Mammalia, 288 ; in Mollusca, 255; of muscle, 249; objections to the theory of, 375 ; of osseous tis- sue, 275 ; under impact and strain, 519; under use in Vermes and Ar- thropoda, 268 ; in Vertebrata, 275. Kingsley, J. S., 89, 213. Koelliker, Dr., 285, 331, 377, 381. Kowalevsky, 323. Kukenthal, 333. Lacerta muralis, 45, 195; L. m. albi- ventrtS) 46 ; L. m. campestris, 46 ; L. m. maculostrz'ata, 46; L. m. punctu- latofasciata, 46 ; L. nt. reticulata, 46 ; L. nt. strzatomaculata, 46 ; L. nt. tigrz's, 46. Lacertilia, 88, 116, 120, 121, 122, 123, 218, 314, 372. Lamarck, 2. 5, 7, 8, 12, 14, 241, 387, 497- Lamellibranchs, 261. Lankester, E. R., 71, 113. Laramie, 139. Larvacea, 215. Law of the unspecialized, 172. Law, Prof., 431. Lawrence, 426, 427. Laws of organic evolution, 3. Laws of structural relations, 19. Leidy, Professor, 351. Lemur collaris, 326. Lemuridae, 155, 328, 339, 356, 469. Lemuroids, 157. Lemurs, 61, 150, 154, 155, 156. Leperditia, 262. Lepidoptera, 203, 204, 237, 440, 441. Leporidae, 348. Leptodactylus pentadactylus, Laur., 390. Lepus, 351, 361 ; L. sylvaticus, 53. LerntEa. branchialis, 212. Lernaeapoda, 212. Lesshaft, 277. Lifege, 160. Life, definition of, 513. Light effect, of, on flatfishes, 238. Lima, 266. Limbs, moulding of articulations of, 287; vertebrate segmentation 01,367. Line of the pisces, 99. Lingula, 176, 177. Liocephalus, 391. Liopeplum, 260. List of papers by American authors on the law of kinetogenesis, 528. Litopterna, 357, 359. Lituites, 414 Loeb, 455. Lohest, 160, 161, 165, 166, 168, 170. Lophiodontidae, 355. Lophobranchii, 105, 106. Louisiana, 50. Loup fork, 139, 148, 315. Lucius estor, 21 ; L. nobilior, 21 ; L. vermzculatus, 21. Lytoceratinae, 190. Macacus, 391. Machrauchenia, 359. Mackenzie River, 50. Magas, 178, 179. Magasella, 179. INDEX. Magellania, 178, 179. Magosphaera, 102, Malacopterygia, 102, 103, 104. Mammalia, characters of, 93 ; line of the successional modifications of the feet and digits of, 133 ; verte- brae of, 135 ; dentition of, 135 ; phy- logeny of, 138 ; origin of, 87; brain and nervous system of, 144. Man of Spy, 161. Maori, 168. Marey, 491. Marseniidae, 261. Marsh, 122, 123, 156, 174, 304. Marsipobranchs, 94, 95, 192, 193, 204. Marsupialia, 127, 132, 138, 142, 143, 157, 305, 309, 336, 361, 374- Mastodonsaurus, 117. Maupas, 79, 459. Mead, T. H., 31. Mechanical, causes of dental modifi- cations, 319 ; conditions of segmen- tation in Arthropoda, 269; origin of characters in Pelecypoda, 261 ; origin of the impressed zone in Cephalopoda, 261. Megerlina, 178, 179. Melanesians, 154. Meldola, Prof., 231, 234. Meleagris ga Hop a vo, 21. Meniscoessus conquzstus, 325. Meniscotherium, 156. Menodontidae, 355. Mental, evolution, 510 ; degeneracy, 509; processes, 506. Menuridae, 126. Merospondyli, 106, 372. Merrifield, 230. Merychoch&rus montanus, 307. Mesohippus, 148. Mesonyx, 141, 302. Mesozoic age, 79, 116, 188, 413. Metabolism, 481. Metaplasis, 202. Metatoceras cavatifortne, 406; M. du- biitm, 408. Metazoa, 252. Mexico, 29, 48, 49, 388. Michahelles, 242. Microsauria, 109, no. Miles, M., 481. Milk-snake, 29. Mind, development of, 364; its rela- tion to matter, 507, 508. Mimetic analogy, 392. Mimoceras, 187, 421. Minot, C. S., 468. Miocene, 138, 139, 315. Mioclaenus, 335. Mississippi, 57. Mitchell, Dr. C., 455. Mitra lineolata, 259. Mivart, 154. Mixophyes, 71. Mnemogenesis, 492. Modiola, 264. Molar teeth, of man, 61, 152; of Es- quimaux, 153 ; of Fan, 168 ; of man and woman of Spy, 166 ; of Maori, 168 ; of Tahitian, 168. Moll, 277. Mollusca, 8, 80, 81, 82, 83, 172, 182, 213, 229, 254, 261, 368, 388, 523, 524. Moloch, 72. Monkeys, intelligence of, 500; in Patagonia, 157. Monocondylia, 87, 372. Monodelphia, 132, 142, 144, 374. Monotremata, 88, 127, 132, 135, 138, 140, 142, 143. Morphogeny from Gwynia to Dal- lina, 179. Morris, C., 363. Moschidae, 69. Moulding of the articulations in the Vertebrata, 287. Mousterien type, 170. MQhlfeldtia, 178, 179. Muller, Aug., 226, 383. Muller, Johannes, 213. Mulleria, 265, 267. Multituberculata, 135, 145, 318, 324, 325. 329. 388. Muscle, kinetogenesis of, 239; striped, 254. Mus decumanus, 403. Mustela, americana, 50 ; M. pennantt, 50. Mustelidae, 342. Mutations, 222. Mutilata, 143, 288, 290, 291, 374. Mutilations, 398, 431. 542 PRIMARY FACTORS OF ORGANIC EVOLUTION. Mya arenarta, 263, 265, 266. Mycetozoa, 219, 229. Myism, 484. Myrmecobius, 140. Myxomycetes, 75. 219, 501, 503. Nageli, 527, 528. Narwhale, 330. Natica, 213. Natural selection, 247, 385, 474. Nature of variations, 113, 115. Naulette, 161, 162, 163, 165. Nautili, 183, 184, 185, 186, 408, 413, 417, 418, 419, 420, 421, 422. Nautilinidae, 421. Nautiloids, 405, 415, 421. Neanderthal man, 159, 161, 163, 165, 169, 176. Necturus, 113. Negritos, 163, 166, 169, 154. Negro, 159, 163. Nematocarpa filamentaria, 526. Nematognathi, 106. Neocaledonians, 163. Neocene, 143, 148. Neo-Darwinians, 381. Neo-Lamarckians, 255, 284, 375, 389, 518. Neo-Lamarckism, 241, 518. Neolithic man, 166. Neothyris, 178. Nephryticeras, 415. Neurism, 484, 496. Neuroptera, 203. New Britain, 169. New England, 49, 52, 56, 437. New Granada, 29. Newton, 480. New York, 50, 402, 437." Nigritos, 154, 163, 166, 169. Normal articulations, 283. Norman horse, 423. North America, 10, 29, 47, 48, 53, 55, 73, 115, 124. Nutrition, 423. Objections, to the doctrine of inheri- tance of acquired characters, 458 ; to kinetogenesis, 375 ; to the doc- trine of parallelism, 205. Obolella, 176. Odessa, 224. (Ecology, v, 384. CEstridae, 102. Oliva, 260. Olivella, 260. Ononis repens, 227 ; O. spinosa, 227 228. Ontogeny, 444. OSphyta, 77. Opheontorphus tnintus, 29. Ophidia, 116, 120, 122, 218, 372. Ophidioceras, 414. Opinions of Neo-Lamarckians, 518. Opisthobranchs, 261. Opisthotome mastication, 318. Orbiculoidea, 177. Orconectes pellucidus, 241. Ordovician, 77, 83, 176. Origin, of the animal line, 514; of Batrachia, 89; of canine teeth, 327; of carnivorous dentition, 332; of the ' dental type of the Glires, 345; of divisions of the vertebrates, 362 ; of genera, 9 ; of the plaits in the col- umnella of the gastropods, 255 ; of plants, 514 ; and survival of the fit- test, 4; of hereditary individual variation, n. Ornithosauria, 114, 120, 121. Ornithostomi, 143. Orr, H. B., 531. Orthagoriscidae, 108. Orthal mastication, 318. Orthoceras, 185, 187, 408. Orthognathism, 248. Orthoptera, 203. Ortyx virginianus, 52. Osborn, H. F., 152, 320, 324, 337, 378, 379, 444, 470, 520, 521, 530. Osceola doliata annulata, 30, 35, 39; O. d. clerica, 31, 33, 39; O. d. cocci nea, 30, 37, 39 ; O. d. collaris, 31, 33, 39 ; O. d. conjuncta, 30, 39 ; O. d. doliata, 22, 29, 30, 33, 39 ; O. d. gcn- tilis, 30, 37, 39 ; O. d. parallela, 30, 35, 39 I O. d. polyzona, 30, 37, 39 ; O. d. syspila, 30, 35, 39 ; O. d. tempora- h's, 3i > 33. 391 O, d. triangula, 31, 33, 39- Osteocephalus, 198, 199. Osteolepididae, 91. INDEX. 543 Ostraciontidae, 108. Ostracoda, 262. Ostrea, 261, 264, 265. Ostrea edulis, 262 ; O, virginiana, 264. Ostreidae, 267. Otariidae, 353, 390. Otaspis, 199. Owen, 150. Oyster, 266, 267. Pacific, 29, 51, 56. Packard, 241, 521, 525, 530. Palaeomeryx, 196. Palaeoniscidae, 181. Palaeospondylus, 99. Palaeosyops, 377. Paleolithic, flints, 170 ; man, 169, 170 ; time, 160. Paleozoic, 188, 226, 413, 415, 417. Palinal mastication, 318. Palingenesis, 200. Paludicola, 71. Pangenesis theory, of Brooks, 454 ; of Darwin, 450. Pantodonta, 141. Pantolambda, 141, 354. Pantotheria, 388. Pantylus, 117. Papilio demoleus, 231 ; P. nz'reus, 231. Papuans, 163. Paradise-birds, 391. Parallelism, 20, 175 ; in the Brachio- poda, 176 ; in the Cephalopoda, 182 ; inexact, 200 ; objections to doctrine of, 205 ; in the Vertebrata, 192. Parasitism, 211, 214, 509. Pariotichus, 117. Parisians, 163. Passeres, 124. Patagonia, 157. Paterina, 176. Paurodon, 343. Pavlow, M., 84. Pea-fowls, 391. Pecten, 254, 264, 265, 266. Pediculati, 106. Pegasus, 104. Pelecypoda, 261. Pelobatidae, 70. Pelodytidae, 70. Peltaphryne peltacephala D. & B., 68. Pelycosauria, 87, 88, 120, 172. Pennsylvania, 49, 437. Pepper, Dr., 278. Percomorphi, 104, 106, 108. Perigenesis, 448, 454. Periptychus, 141, 156, 268. Perissodactyla, 133, 312, 313, 318, 355, 357, 359, 36o, 361, 390, 5i9- Permian, 87, 88, 98, 108, no, 114, 115, 121, 122, 172, 209, 218, 363. Perna, 264. Pernostrea, 267. Peropoda, 121. Perrier, E. , 527. Phacochoerus, 328. Phanerogamia, 77, 79. Pharyngognathi, 106, 107, 108. Phenacodontidae, 147, 150. Phenacodus, 146, 147, 156, 157, 205, 302. Phenacodus primcevits, 130, 137; P. vortntanzz, 134. Phillipine Islands, 166. Phocidae, 353. Phryniscidae, 70. Phrynocephalus, 73. Phrynosoma, 72. Phyllomedusa, 158. Phyllopod Crustacea, 229. Phylogenetic scheme of the Mamma- lia, 127. Phylogeny, general, 74, 444 ; of ani- mals, 79 ; of the Batrachia, 108; of the birds, 123 ; of the classes, 83 ; of the fishes, 99 ; of the horse, 146 ; of the Mammalia, 126, 138; of man, 150; of plants, 78; of the reptiles, 113 ; of the Teleostomata, 101 ; of the Vertebrata, 83 ; of the Actino- pterygia, 101. Physarum leucophceum, 220. Physeteridae, 303. Physiobathmism, 485. Physiogenesis, 225, 227, 435. Physiology, ii, 479; of bone mould- ing, 285. Physoclysti, 104. Pickerel, 21. Pieris, 230 ; P. brassicae, 230 ; P. ra- pae, 230. Pigeon, 21. 544 PRIMARY FACTORS OF ORGANIC EVOLUTION. Pike, 21. Pilsbry, 260. Pinnotheres holotkuriae, 242. Pipilo erythrophthalmus, 52. Pisces, 87, 95, 98, 192, 195. Plagiaulacidae, 324, 345. Plagiaulax, 142. Plant variation, 23. Plants, fossil, 77; evolution of, 515. Platidia, 178, 179. Platypus, 135. Plectognathi, 106, 107, 108. Plectospondyli, 106. Plesiosauria, 114, 121. Pleuracanthus, 372. Pleuronectidae, 238. Plicatula, 267. Pliny, 227. Pliocene, 387. Plistocene, 149, 168. Podopterygia, 100. Poebotheriidae, 302. Pollard, 89. Polygamy, 390. Polymastodon, 142. Polymastodontidae, 324. Polynesians, 154. Polypedates, 68 ; P. quadrilineatus D. & B., 68. Polyprotodontia, 140, 143. Poiypterus, 89. Polyzoa, 202. Porifera, 80, 81. Pouchet, 498. Poulton, E. B., 230, 237, 381, 392, 393, 439, 449, 461. Pre-Carboniferous age, 421. Pressure, 286, 292, 295, 340, 405, 519. Principle of improvement, 527. Proal mastication, 318. Proboscidia, 128, 132, 133, 136, 141,144, 297, 305, 306, 309, 318, 321, 329, 330, 33L 332, 345, 36o, 382, 519. Procolophonina, 87. 88. Procyonidae, 48. Production of colors in lepidopterous pupae, 230. Prognathism, 417. Proportions of limbs and of their seg ments, 305. Prorastomus, 330. Protective colors, 392. Proteida, 109, no, in. Proteles. 146. Proterotherium, 359. Proterotome mastication, 318. Proteus, 242. Prothallium, 455. Prothippus, 149, 359. Protodonta, 388. Protophyta, 75, 76, 77, 172. Protoplasm, composition of, 483. Prototheria, 88, 324 360, 374. Protozoa, 75, 79, 81, 83, 172, 219, 249, 252, 505. ProtozoOn, 459. Psalidodect mastication, 318. Pseudis, 71. Pseudosauria, 109. Pseudosuchia, 116. Psittacotherium, 329, 346, 351. Ptenophus garrulus Smith, 73. Pteridophyta, 77, 79. Pterosauria, 115. Ptilodus, 324. Puerco, 139, 140, 141, 147, 150, 156, 403. Putorius erntineus, 50. Pygopodidae, 123. Pythonomorpha, 120. Pyxicephalus, 71. Quadrumana, 132, 133, 136, 143, 293, 294, 3o6, 326, 332, 360, 361, 467. Quebec group, 413, 420. Quenstedt, 189. Quiscalus purpureus, 52. Rabl RQckard, 94. Raccoon pacing, 299. Rachitomi, 109, no, in, 372. Radiant energy, 484. Rana agilis Thomas, 68 ; R. catesbey- ana, 68 ; R. chrysoprasina, 68 ; R. clamata, 68 ; R. hexadactyla, 68 ; R. temporaries, 64. Ranidae, 65, 70, 71, 389. Raphanus raphanistrum L., 227; R. sativus L., 227. Recapitulation, 453, 492. Reduction of digits, 309. Regeneration, 455. Reptiles, degeneracy of the eye of INDEX. 545 219; degeneracy of the limbs of, 218; degeneracy in the skeletal structure of, 122 ; development of the brain of, 122 ; line of, 113 ; suc- cessive changes in the structure of the skull of, 1 16; vertebral articu- lation of, 121. Reptilia, 88, 94, 95, 98, no, 114, 116, 120, 122, 132, 172, 193, 195, 209, 2l8, 289, 303, 304, 363, 365, 366, 374, 388. Retardation, 9, 201. Retrogressive evolution in the Verte- brata, 145. Reyher, 277. Rhinoceros, 313. 314. Rhinocerus unicorm's, 300. Rhipidopterygia, 91, 100, 101, 172, 366. Rhizopoda, 249. Rhynchocephalia, 114, 116. Rhynchocyonidae, 305. Rhytina, 331. Riley, C. V., 531. Rodentia, 135, 519. Romanes, vi, 471. Rose, 333- Roux, W., 283, 284. * Rusa, 196. Ryder, J. A., 79, 309, 3", 3*9, 320, 321, 323, 346, 349, 366, 404, 455, 485, 486, 518, 519, 520, 521, 529, 530, 531, 532. Salamandra, 199. Salientia, 109, no, 172, 196, 197. Sandberger, 188. San Diego, 244. Sarcothraustes, 335. Saturnia, 466. Saturniidae, 203. Sauermann, Dr., 239, 240. Sauropterygia, 115, 116. Sauvage, Dr., 372. Scaphiopidae, 65. Scaphiopus holbrookii, 68. Scaridae, 108. Schisniadernta carens Smith, 68. Schizocrania, 177. Schmankewitsch, V., 230. Schools of evolutionary doctrine, 13. Schuchert, 191. Scincidae, 123. Sciuridae, 351. Scombridae, 108. Scott, W. B., 222, 334, 526, 531, 532. Scudder, S., 465. Scyphophori, 106. Scytopis, 198, 199. Sectorial teeth, 139. Sedgwick, 492. Seeley, 88, 120, 123. Segmentation of the external skele- ton of the Arthropoda, 269 ; origin of, 368. Segmentation of the vertebral col- umn, 368; origin of, 368. Selenodont dentition, 320; origin of, 323. Self-consciousness, 495. Semper, 228, 242, 527. Sense perception, 495. Sensation, 495, 513. Serranidae, 108. Sex, 516. Sexual selection, 389. Sharp, B., 269, 531. Shetland pony, 423. Shipka, 161, 163. Shoulder girdles of Anura, 64. Sigaretus, 261. Siluric, 77, 83, 183, 185, 186, 187, 413, 414. Siluridae, 103. Simla, 159, 170. Simiidae, 157, 158. Siphocyprcea problematica, 260. Siredon lichenoides, 200 ; 5. mexica- num, 59. Sirenia, 127, 142, 143, 145. 329, 33O, 352, 360. Skull, of man of Spy, 161 ; of Neander- thal man, 162. Smilodon neog&us, 344. Solenhofen slates, 123. Sonoran, 29. South America, 50, 154. Sloths, 305. Spain, 437. Spea hammondii interment ana, 68. Spencer, H., 5, 6, 7, 175, 367, 385, 466, 476, 517, 5i8, 527- Sphenodon, 121. Spinous plants, 228. Spondylus, 267. 546 PRIMARY FACTORS OF ORGANIC EVOLUTION. Sponges, 80. Sports, influence of, 24 Spy, 159, 161, 163, 164, 165, 166, 169, 170. Squainata, 114, 115, 116. Squillidae, 273. Stahl, EM 501. Starch, 481. Statogenesis, 485, 496. Stegocephali, 88, 109, 172. Stegophilus, 103. Stentor, 250. Stereognathus, 325. Stevenson, C., 432. Strain, 305, 311, 313, 319, 326, 327, 349, 281, 485, 519, 521. Strepsiptera, 213. Streptostylica, 114. Sturnella tnagna, 52. Stypolophus, 335. Stypolophus ivhitite, 339. Successional relation, 19, 62. Suidae, 69. Suoldea, 318, 324. Sus, 330. Symphysis mandibuli of a, chimpan- zee, 164; gorilla, 164; liegois, 166; orang, 164; Parisian, 166; Spy man, 164 ; Spy woman, 164. Synagodus, 59. Synapta digitata, 213. Systems of evolution, 13. Table of the characters of the mam- malian skeleton, 139. Tachyglossus, 135. Ta3ker, 195. Tahitian, 168. Tapir, 313. Tapiridae, 318. Tarsipes, 146. Tarsius, 155, 306. Taxeopoda, 128, 136, 146, 297, 357; car- pus of, Taxidea americana, 50. Teeth, evolution of, 318, 522. Teidae, 123. Teleology, 20. Teleostomata, 91, 99, 100, 101, 336. Tellkampf, Dr., 241. Terebratellidae, 178, 179, 180. Termites, 500. Tertiary, 184, 291, 421. Testudinata, 114, 115, 116, 119, 133. Texas, 50, 436. Theory of internal causes, 527. Theory of use and disuse, 3. Theriodonta, 115, 116. Thermochemistry, 483. Theromora, 88, 114, 115, 116, 120, i2i; 132. Thoatherium, 359. Thoraceras, 186. Thoropa miliaris Sphix, 68. Thylacinus cynocephalus, 22. Tillodonta, 140, 143, 145, 329, 360. Tomes, 381. Tontitherium rostratum Cope, 156. Topinard, P., 153, 155, 157, 168, 165. Tornier, E., 283, 284, 528. Tortoises, 114. Tortricidae, 123. Toxodontia, 128, 143, 297. 330, 360, 382. Trachycephalus, 198. Trachypteridae, 108. Trachystomata, 109, in. Tragulidae, 69. Traquair, 99. Trias, 108, 113, 135, 184, 209, 325, 417 Triboloceras, 186. Trichea van'a, 220. Triconodon Owen, 343. Triconodontidae, 318. Trichophanes, 104. Tridacna, 265. Trilobita, 83. Trimen, R., 231. Trinil, man of, 159, 168, 169, 170. Trionychidae, 303. Tripteroceras, 186. Tristichopteridae, 91. Trityloden, 325. Trivia, 260. Trotting horses, 426. Troglocaris, 242. Tubularia mesentbryantheniuntt 456, Tunicata, 172, 214, 218, 362. Turbot, 499. Tyndall, Prof., 476. Typhlogeophis, 123. Typhlogobius, 244. INDEX. 547 Unconsciousness, 494, 507. Uinta, 147. Uintatherium, 354. Uintatheriidae, 318. Uma, 73. Unguiculata, 140, 143, 374. Ungulata, 138, 140, 142, 143, 147, 205, 248, 295, 297, 302, 321, 330, 340, 353. 355, 357, 36i, 374, 39° ; origin of, 209. Unionidae, 203. United States, 49, 53, 315. Urochorda, 82. Urodela, 109, no, 172. Uropeltidae, 123. Uroplates, 88. Ursus arctos, 21, 22 ; U. maritintus, 21. Unspecialized, doctrine of, 173. Use and disuse, doctrine of, 9. Vandellia, 103. Vanessa to, 232 ; V. urticae, 232. Variation, 21. Variation, of basal lobes of leaves, 5; causes of, 225; in cicindela, 25; cnemidophorus, 41 ; embryogenic, 444 ; fortuitous, 444 ; gamogenic, 444; geographical, 47; gonagenic, 444 ; in North American birds and mammals, 45 ; origin of, 225, 497 ; ontogenetic, 444 ; in Osceola doliata, 29 ; phylogenetic, 444. Variations, of specific characters, 25 ; somatogenic, 444 ; structural char- acter, 58. Varigny, 229. Vermes, 80, 81, 82, 83, 172, 263, 268, 368, 437. Vertebral centra, forms of, 308. Vertebrata, brain and nervous sys- tem of, 94, 139 ; classification of, 93; circulating system of, 93, 192; origin of, 81 ; phylogeny of, 81. Vestinautilus, 186. Vilmorin, 228. Virchow, Prof., 159. 169, 467. Vise, 416. Vola, 266. Volutidae, 260. Volutimorpha, 260. Volvox, 79. Vom Rath, 470, 471. Von Baer, 175. Von Brunn, 403. Vulpes alopex, 48 ; V. cinereoargenta- tus, 48 ; V. lagopus, 48 ; V. velox, 48. Wallace, A. R., 3, 5, 228, 381, 383, 387, 391, 392, 466. Ward, L., 531. Wasatch, 139, 146. Weale, M., 231. Weismann, 10, u, 12, 23, 203, 399, 424 438, 450, 458, 459, 480. West Indies, 387. White River, 139. Wiedersheim, 366. Wilson, E. B., 457, 487. Wood, T. W., 230, 231, 233, 234. Woodward, A. S., 372. Wortman, 293, 402, 520. Wundt, 498. Wurtenburger, 189. 191. Yucatan, 49. Zeller, 242, 243. 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