NATURAL MOULD OF THE BRAIN CAVITY OF A CAMBRIDGE ORNITHOSAURIAN [U] . (Cast.) All corrections listed in the "Errata" have been made in the text. Linking text for the plates has been added to the "Contents". AN ELEMENTARY STUDY OF Cambridge: PRINTED BY G. J. CLAY, M.A. AN ELEMENTARY STUDY OF AND BY OF ST. JOHN'S COLLEGE, CAMBRIDGE. "And when the appointed end comes, they lie not dishonoured in Cambridge: [All Rights reserved.] This memoir is a portion of the Catalogue of the Woodwardian Museum which has been made at Professor Sedgwick's request and at his cost. When the Professor laid upon me his commands to prepare a Catalogue of the Museum, it was planned in three distinct works. First, a series of indexes to the specimens in the great divisions into which the Museum is arranged; secondly, a series of memoirs upon the orders and classes of animals concerning which new knowledge is given by fossils in the Museum; and, thirdly, memoirs descriptive of those species contained in the arranged collections which are at present unknown in scientific writings. For the convenience of students the Catalogue is made in parts. The Syndics of the University Press printed last autumn as an example of the "Indexes to the Museum," an Index to the Pterodactyles, Birds, and Reptiles from the Secondary Strata. And this memoir is an example of the second kind of Catalogue, which explains the structures of the Pterodactyles of the Cambridge Greensand. In its progress questions have arisen which necessitated an examination both of the method, of research in comparative anatomy and of its results in classification. And in so far as the views here advanced differ from those commonly taught, the discrepancy is due to the writer's imperfect faith in the results of the inductive method of research, as commonly used by modern writers on PalÆontology. It has not been consistent with the plan of this little work to do more than scatter through it a few hints upon method, a subject which will more fitly be discussed with a part of the Catalogue which forms a synopsis of the osteology of the fossil animals usually named Reptiles. The views here urged have however but little of novelty. The name Ornithosauria was proposed by the distinguished naturalist Prince Charles Bonaparte in 1838. The group as an order was recognized by Von Meyer in 1830. The affinities of the brain appear to have been detected by Oken, and the bird-like character of the respiratory system was expounded by Von Meyer. And most of whatever this memoir contains has been already thought or discovered by the German philosophers, who have had the Pterodactyles as fossils of their fatherland, though my own conclusions were arrived at separately and from different materials. The oldest Ornithosaurians are from the Muschelkalk of Germany. In England the oldest are from the Lias,—several species of Dimorphodon—a genus in some respects nearly resembling the Pterosaurians of the Cambridge Upper Greensand. In the Oolite of Stonesfield are several species of Rhamphorhynchus or a similar genus. The great PÆlolithic period from the Oxford Clay to the Kimeridge Clay, has yielded in its several divisions small Pterodactyles of new species. And the Psammolithic period from the Portland Sand to the Lower Greensand has afforded many excellent remains both of true Pterosaurians in the Purbeck, Wealden, and Potton Sands, and of animals which indicate a new order of Ornithosauria having affinities with Von Meyer's thick footed saurians, the Dinosauria. In the Cretaceous series, Galt, Upper Greensand, and Chalk all have representatives of the Pterosauria; but no English stratum has hitherto yielded so many as the Cambridge Upper Greensand. From this formation the collection accumulated during Prof. Sedgwick's long professoriate is unequalled; though, excepting a few fine bones from the Chalk and the Purbeck Limestone, the Woodwardian Museum is as yet deficient in Ornithosaurians from the other Secondary Rocks. Until descriptions of these animals shall have been published a classification of the Ornithosauria must necessarily be provisional. And it cannot be expected that descriptions of the structure of Cretaceous Pterosaurians here given will hold good for all the Ornithosaurian sub-class. Finally, I have gratefully to express my thanks to the many friends, English and German, who have aided me with specimens and with their writings; to the chiefs and officers of the English museums, especially Prof. Owen, Prof Humphry, Prof Newton, Prof Phillips, Prof Flower, and Prof. Huxley; to the officers of the University Library, especially Mr Bradshaw, and Mr Crotch, for aid in consulting books; but chiefly to Prof Sedgwick, who while employing me as his paid Assistant to aid him in his Museum work, has generously encouraged me to carry on for several years, without restraint and as part of my daily labour, an investigation of which this treatise is the first fruit. Prof. Sedgwick has placed at my disposal an ample number of copies for distribution among those who take an interest in the Museum; and especially among those who have contributed to the Ornithosaurian collections, and aided me in my work. January 3, 1870.
Osteological collection illustrative of modifications of Ornithosauria in the Cambridge Greensand, pp. 28-94.
For epipubic bone read prepubic bone, pp. 61, 102, 109, 110, 111, and pl. 8. TO THE The Cambridge Upper Greensand has yielded to collectors bones which illustrate nearly every part of the skeleton of the animals that are commonly named Pterodactyles. Large collections have been acquired for the Woodwardian Museum. A series of more than 500 bones have been arranged to exemplify the osteology and organization of the Ornithosauria in the area when the Cambridge Greensand was deposited. And this memoir is written to explain briefly some of the structures of the soft and hard parts of those animals which are exhibited or demonstrated by these relics. Another collection of nearly 400 bones has been arranged, which displays in association, as they were found entombed in the old Greensand sea-bed, the remains of the skeletons of thirty-three animals of the Pterodactyle kind. The whole of the remains from this formation hitherto gathered cannot be computed to have pertained to fewer than 150 individuals, which indicate a new sub-class of animals, two new genera and at least twenty-five new species. The bones were mostly of a paper or card-like thinness, and were originally hollow like the thin bones of birds. In the jaws of other animals, and in the sea, they were easily fractured, so that proximal ends and distal ends and shafts and split bones abound, while perfect bones are almost unknown. Even those bones like the carpals, which almost retain their entirety, invariably show indications of having been rolled on the sea-shore among the nodules of phosphate of lime with which they now occur, in their angular margins being rounded, and in the removal of slender processes. The rock in which these fossils are found is a thin bed of chalky marl which is heavily charged with dark-green grains of Glauconite, and is quarried largely, and entirely dug away to be deprived of the dark-brown nodules of phosphate of lime with which it is stored. In digging and in the subsequent washing, the workmen, stimulated by an ample reward, pick out the fossils as they are discovered. They are separated easily from the matrix of investing marl, so that every aspect of each bone is seen, except for the occasionally adherent oysters and the masses of phosphate of lime, with which material the bones are also filled. Hence these remains afford facilities for the study of the joints such as no other specimens have presented; and from their large size and comparatively great numbers, render easy the labour of the student who seeks to contrast them with the bones of other animals. The osteological collection has been formed without regard to species or genera, and arranged to exhibit the structure and organization of the tribe of animals. So far as possible each bone, as humerus, femur, &c., has its variations of structures and form contrasted on a single tablet. The series comprises the following bones: Fore-part of sternum. They are exhibited in Compartments a, b, c of the Table-case of Cabinet J. The letter F in a circle is placed against figured specimens. The Cambridge Pterodactyles first attain prominence in scientific literature in the year 1859. Professor Owen had figured (plate 32, fig. 6-8) fragments of bones in the PalÆontographical Society's Monograph for 1851; the distal end of a large ulna (fig. 6); the shaft of a phalange of the wing-finger, probably the first (fig. 7); and the upper portion of the shaft of a small humerus showing part of the radial crest (fig. 8). Inadvertently the last specimen was referred to the Lower Greensand. But although fragments of humerus of Pterodactyle and vertebrÆ of Pterodactyloid animals have in the last few years been gathered from the Potton Sands, those deposits were believed to be barren of fossils when Prof. Owen wrote; and all the Pterodactyles yet made known from near Cambridge were collected from the Cambridge Upper Greensand. Among the earliest successful collectors were Mr James Carter, the Rev. H. G. Day, St John's Coll.; Prof. G. D. Liveing, St John's Coll.; the Rev. T. G. Bonney, St John's Coll.; and Mr Lucas Barrett, Trin. Coll.; and the Rev. Prof. Sedgwick, Trin. Coll., on behalf of the Woodwardian Museum. Mr Day and Mr Bonney both presented every specimen from their cabinets which could enrich the University collection. And in the last ten years the Woodwardian Museum has acquired, through the skillful collecting of the Messrs Farren, the present materials. The associated sets of bones were formed by William and Robert Farren, who, obtaining the specimens from day to day as they were discovered, were enabled to put together such parts of the skeleton as remained together on the sea-bottom. These collections will hereafter be used for the elucidation of species. They are the only materials which can give the proportions of the Cambridge Ornithosaurians, and the contrast of aspect which distinguished the living animals from those from other rocks. The other collections of these fossils are those of Mr William Reed and Mr J. F. Walker at York, the Museum of Practical Geology, and the British Museum. The Woodwardian specimens as collected were placed in the hands of Prof. Owen, and were first made known in the Professor's lectures on reptiles and birds delivered at the Museum of Practical Geology in 1858. In that year Prof. Owen communicated to the British Association for the Advancement of Science, and printed in their Report, the matter of the memoir which was published with plates by the PalÆontographical Society in 1859. In this latter year Prof. Owen communicated to the Royal Society an account of the vertebral column of Pterodactyles. In 1859 Prof. Owen also produced a classification of recent and fossil reptiles at the meeting of the British Association, in which the order Pterosauria appears with new characters—such as the pneumatic structure of most of the bones—drawn from Cambridge specimens. In 1860 Prof. Owen produced another memoir on Pterodactyles, which was published by the PalÆontographical Society. A brief account of the tribe appeared about the same time in the Professor's PalÆontology. In these writings are descriptions of the various parts of the vertebral column. Their procoelian centra are described, and the pneumatic foramina are noticed and supposed to have communicated with air-cells. They are compared with birds, and distinguished from birds; but although the order is classed with reptiles no contrast with reptiles is made. Other bones described are a basi-occipital, and a doubtful bone, then thought to be a frontal, but which is more like the neural region of the sacrum. The sternum is compared with the sternum of the birds Apteryx and Aptenodytes, is stated to be formed, in the main, on the Ornithic type, and to possess distinct synovial articular cavities for the coracoids such as only occur in birds. The inter-coracoid process of the sternum is compared with that of Bats, Birds, and Crocodiles. The mechanism of the framework of the wings is said to be much more bird-like than bat-like, the anchylosed scapula and coracoid being remarkably similar to those of a bird of flight. The coracoid is shorter and straighter in birds than in Pterodactyles, but no comparisons are made with reptiles. The humerus is known only by the proximal end. It is said to conform at its proximal end more with the Crocodilian than with the Avian type, but to have the radial crest much more developed than in either Crocodile or Bird. The bone is, however, chiefly compared with birds, and is figured between corresponding bones of a Vulture and a Crocodile. The pneumatic texture is said to be as well marked as in any bird of flight. Of the carpus it is said, the Pterodactyle, in the complete separation of the metacarpus from the antibrachium by two successive carpals answering to the two rows, adheres more closely to the reptilian type than to that of birds. But the row which was regarded as proximal is the distal row, while the supposed distal row is proximal. The claw-phalange and distal end of the wing-metacarpal, the mandible, teeth, and jaw are the other bones described, but their comparative osteology is not discussed. In the Professor's account of a fragment of a jaw it is said, "The evidence of the large and obviously pneumatic vacuities now filled with matrix, and the demonstrable thin layer of compact bone forming their outer wall, permit no reasonable doubt as to the Pterosaurian nature of this fossil. All other parts of the flying reptile being in proportion, it must have appeared with outstretched pinions like the soaring Roc of Arabian romance, but with the demoniacal features of the leathern wings with crooked claws, and of the gaping mouth with threatening teeth, superinduced." When the specimens on which Prof. Owen had founded the foregoing views of the osteology and classification of these animals were at length returned to the Woodwardian Museum, it became a duty of the present writer to arrange and name them. And in a Memoir on Pterodactyles which was communicated to the Cambridge Philosophical Society and read March 7 and May 2 and 16, 1864, a position was claimed for them, distinct from reptiles, as a separate sub-class of Sauropsida, nearly related to birds. In September of the same year a communication was made to the British Association "On the Pterodactyle as evidence of a new sub-class of vertebrata (Sauromia)," with enlarged drawings of the skull and some of the other bones, in which the conclusions arrived at were that, excepting the teeth, there is little in such parts of the head as are preserved to distinguish the Cambridge Pterodactyles from birds; and that the remainder of the skeleton gives a general support to the inference from the skull. Papers were communicated to the Cambridge Philosophical Society on February 17, 1868, on indications of Mammalian affinities in Pterodactyles in the pelvis and femur, and February 22, 1869, on the bird-like characters of the brain and metatarsus in the Pterodactyls from the Cambridge Greensand. The other references to Cambridge specimens are in a paper "On the literature of English Pterodactyles" in the Annals and Magazine of Natural History for Feb. 1865, and in "An epitome of the evidence that Pterodactyles are not reptiles, but a new sub-class of vertebrate animals allied to birds," in the same magazine for May, 1866. In the meantime Prof. Owen's views have somewhat changed. In the first volume of the Comparative Anatomy and Physiology of the Vertebrata (1866), the Pterosauria are classed as the highest group of reptiles, and take rank above the Dinosauria. In the second volume of that work (1866), occurs the following passage: "Derivatively the class of birds is most closely connected with the Pterosaurian order of cold-blooded air-breathers. In equivalency it is comparable rather with such a group than with the Reptilia in totality, or with the Mammalia." Nearly every writer on Pterodactyles, who has expressed any opinion at all, has formed an estimate of his own of their organization. They have been assigned to almost all possible positions in the vertebrate province, by great anatomists who all had before them very similar materials. An account of these views is given by von Meyer in his monograph of the Pterodactyles of the Lithographic Slate. It will not be necessary to discuss these conclusions here, for the materials from the Lithographic Slate and those from the Cambridge Greensand are so different that no light would be thrown on the organization of the animals by an exposition of any fallacious inferences from German specimens. In England they are classed with Reptilia, chiefly through the influence of the discourse upon them given by Baron Cuvier in his Ossemens Fossiles[A]. It therefore may conduce to a clear view of the subject to quote in Cuvier's words the passages in that memoir which have been supposed to establish their position among reptiles. He says,—"Ayant encore portÉ mon attention sur le petit os cylindrique marquÉ g (i.e. os quadratum) qui va du crÂne À l'articulation des mÂchoires, je me crus muni de tout ce qui Étoit nÉcessaire pour classer ostÉologiquement notre animal parmi les reptiles." The exact relations of the quadrate bone are not seen in either Cuvier's or Goldfuss' or von Meyer's figures of this Pterodactyle, the P. longirostris; but in von Meyer's figures of P. crassirostris, P. longicollum, and P. Kochi it appears to be a free bone articulated to the squamosal and petrosal region of the skull and with the lower jaw. This is not the case with either Chelonians or Crocodiles, which have the quadrate bone firmly packed in the skull; nor is it paralleled even among those lizards and serpents which have the bone as free; while, on the contrary, it is characteristic of the whole class of birds. The form of the bone is not more Lacertian than Avian, while its direct attachment to the bone of the brain-case finds no parallel among lizards, but is exactly paralleled in all birds. [A] Tome V. Part a, pp. 358, 383. Edition, 1814. Cuvier then goes on to say, "Ce n'Étoit pas non plus un oiseau, quoiqu'il eÛt ÉtÉ rapportÉ aux oiseaux palmipÈdes par un grand naturaliste[B]." Which position he supports as follows:— [B] Blumenbach. (1) "Un oiseau auroit des cÔtes plus larges, et munies chacune d'une apophyse rÉcurrente[C]; son metatarse n'auroit formÉ qu'un seul os, et n'auroit pas ÉtÉ composÉ d'autanut d'os qu'il a de doigts." These, though they may not be characters which are those of birds, are certainly not eminently reptilian. The elongated form of the tarsals in birds is peculiar, but quite functional, as may be seen among the Penguins, where, when the so-called tarso-metatarsal bone is no longer erect, it becomes much shorter, and is nearly separated into three distinct bones. The cretaceous Pterodactyles appear to have this bone exactly like that of birds. [C] This shown in other specimens since figured, and in the specimen from Stonesfield in the Oxford Museum. (2) "Son aile n'auroit eu que trois divisions aprÈs l'avantbras, et non pas cinq comme celle-ce." This is a difference, but a difference of detail only, and not a reptilian character. The creatures have wings; and no reptile known, from recent or fossil specimens, has wings. The general plan of the wing, though very unlike, approximates to that of a bird. Most birds have two phalanges in the long finger, though some have three. One Pterodactyle is described as having only two phalanges in the wing-finger, while most of the German specimens appear to have four phalanges. In birds the longest finger appears to be the middle one, while in Pterodactyles it is the innermost one. (3) "Son bassin auroit eu une toute autre Étendue et sa queue osseuse un toute autre forme; elle seroit Élargie, et non pas grÊle et conique." The pelvis of Pterodactyle is not reptilian, and no living reptile has a pelvis like it. It is not unlike the pelvis of a Monotreme, but the ilium is more Avian. It resembles the pelvis of Dicynodon. And the discovery of a long-tailed bird-like the ArchÆopteryx shows that the tail is like that of old birds, even if it also presents some analogy in form to that of certain reptiles and mammals. (4) "Il n'y auroit pas eu de dents au bec; les dents des harles ne tiennent qu'À l'enveloppe cornÉe, et non À la charpente osseuse." This is not a reptilian character. Among reptiles some tribes have teeth, others want them; and among mammals some animals are without teeth, though they are so characteristic of the class. It is an anomaly that birds should all be toothless. And so, without citing the supposed teeth of ArchÆopteryx, it may be affirmed that it would be no more remarkable for some birds to have teeth than it is for some mammals and reptiles to be without them. (5) "Les vertÈbres du cou auroient ÉtÉ plus nombreuses. Aucun oiseau n'en a moins de neuf; les palmipÈdes, en particulier, en ont depuis douze jusqu'À vingt-trois, et l'on n'en voit ici que six ou tout au plus sept." This is a variation of detail such as, had it occurred among birds, would hardly have been deemed evidence of their affinities. When the variation of the neck-vertebrÆ ranges from 23 to 9, the further reduction of the number to 7 becomes insignificant, and does not show that the animal was a reptile. (6) "Au contraire, les vertÈbres du dos l'auroient ÉtÉ beau-coup moins. Il semble qu'il y en ait plus de vingt, et les oiseaux en ont de sept À dix, ou tout au plus onze." This modification is obviously the result of smaller development of the pelvic bones from front to back, and hence of the small number of vertebrÆ in the sacrum. It does not support the reference of Pterodactyles to the class of reptiles. Speaking of the teeth, it is said, "Elles sont toutes simples, coniques, et À peu prÈs semblables entre elles comme dans les crocodiles, les monitors, et d'autres lÉzards." The teeth of Pterodactyles are (in the skull) for the most part in the premaxillary bones, in which it is so characteristic for the teeth of animals to, be merely conical and simple. Therefore it would have been difficult to imagine the teeth to have been anything but what they are, whatever the affinities of the Pterodactyle might be. It is remarked, "La longueur du cou est proportionÉe À celle de la tÉte. On y voit cinq vertÈbres grandes et prismatiques comme celles des oiseaux À long cou, et une plus petite se montre À chaque extrÉmitÉ." This adds nothing to the evidence for its reptilian character. "Ce qui est le plus fait pour Étonner, c'est que cette longue tÉte et ce long cou soient portÉs sur un si petit corps; les oiseaux seuls offrent de semblable proportions, et sans doute c'est, avec la longueur du grand doigt, ce qui avoit determinÉ quelques naturalistes À rapporter notre animal À cette classe." Nor is this evidence that the animal was a reptile. And in many minor matters Cuvier is careful to show how their modifications resemble those of birds; and when this is not so, birds are the only animals from which he finds them varying. And the few suggestions which are thrown out respecting their affinities with lizards are upon points which are also common to birds. Thus what Cuvier did was to distinguish these animals from birds, and incidentally to show that their organization was a modification of that of the Avian class. And the legitimate inference would have been that their systematic place was near the birds, and not that they were reptiles. But in Germany Cuvier's views on Pterodactyles have by no means been submissively received; and great anatomists, since he wrote, have propounded and defended views as various as those of the anatomists who preceded him, and with no less confidence in the results of their science. In the brief space at my command it would be impossible to do justice to the works of this array of philosophers, and therefore I present in a somewhat condensed version the epitome of their conclusions given by Hermann von Meyer in his Reptilien aus dem Lithographischen Schiefer der Jura. They form a commentary on the casts of Solenhofen Pterodactyles contained in the Woodwardian Museum. regarded the Pterodactyle as an unknown kind of bat, and thought that Cuvier was misled by Collini's imperfect description. He believed that he found in them different kinds of teeth as in mammals; and regarded them as differing from bats chiefly in having larger eye-holes, a longer neck, four fingers and four toes, a longer metatarsus, and in having but one elongated finger; and found the closest analogue of the fingers in Pteropus marginatus of Bengal. And although inclined to place the Pterodactyle between Pteropus and Galeopithecus, he suspects from the bird-like characters of the head and feet that its true place is intermediate between mammals and birds. [D]. |