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NEW SERIES. eee VOLUME I. LONDON: SAMUEL HIGHLEY, 32, FLEET STREET. i 1853. FEB T2 \eas L1Q2a4RN LONDON: PRINTED BY W. CLOWES AND SONS, STAMFORD STREET. - 978.0642 RSS Sr —— xy! TRANSACTIONS OF THE MICROSCOPICAL SOCTETY OF LONDON. hess Lacinutaria sociaLis. A Contribution to the Anatomy and Physiology of the Rotvirera. By T. H. Huxtey, Esq., F.R.S., Assist.-“Surgeon R.N. (Read Dec. 31, 1851.) Tue leaves of the Ceratophyllum, which abounds in the river Medway, a little above Farleigh Bridge, are beset with small transparent, gelatinous-looking, globular bodies, about 1-5th of an inch in diameter. ‘These are aggregations of a very singular and beautiful Rotifer, the Lacinularia socialis of Ehrenberg. On account of their relatively large size, their transparency, and their fixity, they present especial advantages for microscopic observation ; and I therefore gladly availed myself of a short stay in that part of the country to inquire - somewhat minutely into their structure, in the hope of being able to throw some light on the many doubtful or disputed points of the organization of the class to which they belong. We are told by Ehrenberg (‘Infusions-Thierchen,’ p. 403) that Lacinularia socialis was discovered and described anonymously in Berlin in 1753. Miller bestowed upon it wheldony “4e5 ley al the name of Vorticella socialis, which was changed by o Schweigger to Lacinularia in 1820. Previously to the time — of Ehrenberg the genus appears to have become confounded with Megalotrocha ; and indeed Dujardin very reasonably, as it seems, altogether denies the propriety of their separa- tion. The extreme resemblance of the two forms is admitted by Ehrenberg himself; but he considers the attachment of the ova of Megalotrocha by a filament to the body—a circum- stance which does not obtain in Lacinularia—and the exist- ence of a gelatinous investment in the latter which is not found in the former, to be sufficient grounds of distinction. The matter is not one of much importance, but I call attention to the close alliance between Megalotrocha and Lacinularia for a reason which will appear in the sequel. The globular aggregations of which I have spoken are not VOL. I. i b 2 Hux ey on Lacinularia socialis. ramified animals like the freshwater Polyzoa, to which, at first sight, they have no small resemblance, but may be truly called compound animals, since each of the Lacinulari@ is a separate individual, which at one time swam about freely by itself,* which has voluntarily united itself with its fellows, and has taken its share in throwing out the gelatinous sub- stance which connects them into a whole. Each Lacinularia (Pl. I. fig. 1) has an elongated conical body, whose outer extremity is considerably the wider, and whose inner smaller end is truncated, and serves as a sucker or means of attachment to the stem on which the whole mass is seated; the outer third or fourth of the body contains the viscera, nothing but the muscular cords extending into the inner narrow elongated part of the animal. During con- traction the latter portion is thrown into sharp folds, while the visceral portion presents only three or four faint transverse constrictions. When the Rotifer is in a state of expansion and activity, its outer extremity is terminated by a large horseshoe-shaped wheel-organ, or “trochal disc” (figs. 2, 3), connected with the body by a narrowed neck. When contracted and at rest, the whole of this apparatus is drawn in, and the body takes on a more pyriform appearance (fig. 5). The mouth lies in the notch of the trochal disc (fig. 4 d) ; the anus is placed on the opposite side, at the lower part of the visceral portion of the animal (A). Anatomy of Lacinularia.—1 will now proceed to describe the various organs of the animal more minutely. The “trochal disc” is, as I have said, wide and horseshoe- shaped. It is seen in profile at figs. 1 and 2; from above at fig. 8. Its edges are richly beset with large cilia, which present a very beautiful wheel-like movement. Ehrenberg says that the ciliary organ is “as in Megalo- trocha,’ and in this he describes the disc as having a simple ciliated edge. I have not examined Megalotrocha, but I can say most decidedly that such is not the structure of La- cinularia.t In fact, the edge of the disc has a considerable thickness, and presents two always distinct margins—an upper (p) and * Or rather had the power of swimming about freely; for it does not appear that the young Lacinularic ever do leave the gelatinous envelope of the parent mass, unless aggregated together. + Leydig (Zur Anatomie und Entwickelungs-geschichte der Lacinu- laria socialis—Siebold and Kolliker’s Zeitschrift for February, 1852) says that ‘‘an elevated ridge runs along the lower surface of the wheel organ, not far from and parallel to its margin, whence there is a double edge and a groove, In which alone ciliary motion is observed.” Houxzey on Lacinularia socialis.- 3 a lower (p’), of which the former is the thicker and extends beyond the latter. The large cilia are entirely confined to the upper margin, and, seated upon it, they form a continuous horseshoe-shaped band, which, upon the oral side, passes entirely above the mouth (fig. 4). The lower margin (p’) is smaller and less defined than the upper, its cilia are fine and small, not more than 1-4th the size of those of the upper margin. On the oral _ side this lower band of cilia forms a V-shaped loop (fig. 4), which constitutes the lower and lateral margins of the oral aperture. About the middle of this margin, on each side, there is a small prominence, from which a lateral ciliated arch runs upwards into the buccal cavity, and, below, becomes lost in the cilia of the pharynx. The aperture of the mouth therefore lies between the upper and lower ciliary bands. It is vertically elongated, and leads into a buccal cavity with two lateral pouches, which give it an obcordate form; these lateral pouches contain the lateral ciliated arches. A narrow pharynx leads horizontally backwards from the lower part of the buccal cavity, and becomes suddenly widened to enclose the pharyngeal bulb in which the teeth are set. Where buccal cavity meets the pharynx, a sharp line of demarcation exists (fig. 2). In Meli- certa two curved lines are seen in a corresponding position, and evidently indicate two folds (PI. II. fig. 26), projecting upwards into the csophagus. In Brachionus these folds are stronger (fig. 31), while in Stephanoceros and Floscularia this partition between the cesophagus and what may be called the crop is still more marked. From the inner margin of the aperture in the partition two delicate membranes hang down into the cavity of the crop, which have a wavy motion, and it is to them I think that what Mr. Gosse describes as an appearance of “‘ water constantly percolating into the alimentary canal” is due. Dujardin had already noticed (1. c, p. 98) these “vibrating membranes” in Floscularia (‘ Infusoires,’ p. 611). Between the pharyngeal bulb and the mouth there lies on each side of the pharynx a clear, yellowish, horny-looking mass (f), which sometimes appears merely cordate, at others more or less completely composed of two lobes. A similar structure exists in Brachionus and Melicerta. 1 believe its function is to give strength to the delicate walls of the pharynx, and that it is therefore to be considered as a part of the horny skeleton.* * Leydig (loc. cit.) calls these bodies sacs, and considers them to be salivary glands. b2 4 Hoxtey on Lacinularia socialis. The general nature of the pharyngeal bulb and of its movements has been so often described that it is needless for me to refer to the subject here. With regard to the teeth, however, what I have seen is considerably at variance with the accounts of both Ehrenberg and Dujardin; the former calls the teeth of JZacinularia “reihenzaihnigen,” that is, having a stirrup-like frame, with many teeth set upon it; and the latter,in his general definition of the “ Melicertiens,” under which head he places Lacinularia, has “machoires en étrier” (‘ Hist. Nat. des Infusoires,’ p. 612).* As I have seen it (fig. 6), the armature of the pharyngeal bulb in this species—as in Stephanoceros—is composed of four separate pieces. ‘Two of these (which form the incus of Mr. Gosse) are elongated triangular prisms,} applied together by their flat inner faces ; the upper faces are rather concave, while the outer faces are convex, and upon these the two other pieces (the mallei of Mr. Gosse) are articulated. These last are elongated—concave internally, convex ex- ternally—and present two clear spaces in their interior; from their inner surface a thin curved plate projects inwards. At its anterior extremity this plate is brownish, and divided into five or six hard teeth, with slightly enlarged extremities. Posteriorly the divisions become less and less distinct, and the plate takes quite the appearance of the rest of the piece. This is essentially the same structure as that of the teeth of Notommata, described by Mr. Dalrymple (‘ Phil. Trans,’ 1849), and by Mr. Gosse (on the Anatomy of Notommata aurita, Mic. Trans. 1851), and very different from the true “ stirrup-shaped ” armature. A narrow oesophagus passes directly downwards from the posterior part of the cavity of the pharyngeal bulb, through the neck of the animal to the body, where it — into the wide alimentary canal, This is divided into three portions by an upper, a middle, and a lower constriction. The two upper parts are often not very distinctly divided. A wide oval or pyriform sac, whose wall contains many nu- cleated cells, opens into the upper portion on each side. This is the “ pancreatic” sac of Ehrenberg.t The middle dilatation frequently gives origin to several short cellular cceca. The lowest dilatation is globular, and has also several cel- * Leydig also finds Ehrenberg’s figures “‘ untrue to nature.” + Not described by Leydig. + According to Leydig there are four of these bodies, two smaller and two larger, and they do not open into the alimentary canal.—Loce, cit. .» p- 463. Houxtey on Lacinularia socialis. ae lular coeca projecting from its outer surface. Within it is clothed with very long cilia. The intestine is short and wide, and comparatively delicate ; it bends suddenly upwards on the side opposite the mouth, and terminates in a cleft of the integument, whose whole extent it did not seem to me to occupy. (Fig. 1 2) The Water Vascular System.—This system is thus loosely and confusedly alluded to—I cannot call it described—by Professor Ehrenberg :*—‘* The vascular system consists of transverse circular canals in the body, a vascular network at the base of the wheel-organ, with perhaps a broad circular canal at this part, and of trembling gill-like bodies’’—(loc. cit., p- 403). The vascular system is so obvious,{ that it is diffi- cult to understand how it can have been thus blurred over. The reader will bear in mind that the two bands which run up from the cloaca in many Rotifera, and are usually con- nected at their extremity with a “ contractile vesicle,” while they give attachment in their length to the “ trembling gill- like organs” of Ehrenberg, are considered by the latter to be the testes. He says that “ the trembling organs” appear to be within the sac in Hydatina, outside it in Notommata. Von Siebold (‘ Vergleichende Anatomie’) first pointed out that a vessel runs up in each of these bands, and that the ‘* trembling organs’’ are short branches of these vessels, each of which contains a vibrating ciliary band (Flimmer-lappchen), to which the trembling appearance is due. According to Von Siebold each of these vibrating bodies indicates an opening in the vessel. Oskar Schmidt (‘ Versuch einer Darstellung d. Organisation d. Raderthiere-—Erichsons Archiv, 1846) asserts that the ends of the water-vessels are closed, and that the vibrating body is within them. Dalrymple (loc. cit.) saw no testes in the lateral bands of Notommata, and considers that the “ tags”’ (the ‘ trembling organs” of Ehrenberg) are externally ciliated at their extre- mities. Mr. Gosse (‘ Microscopical Transactions,’ 1851) describes the water-vascular system in Motommata aurita, and states that the “ tags” of Ehrenberg are really pyriform sacs ; but he seems not to have distinguished the contained cilium, at least his description is ambiguous. ‘ When trembling mode- rately they are seen to be little oval bags attached to the tor- tuous vessel by a neck and sac at the other end. A spiral * “T can thus affirm, that what Ehrenberg describes as vessels in Lacinularia are in fact not vessels at all.”—Leydég, loc, cit., p. 468. t ‘Sehr aus-gepract,” Leydig, p. 465. 6 Huxtey on Lacinularia socialis. vessel, closed at the extremity, runs through most of its length, which maintains a wavy motion”—p, 98.* The following is what I have seen in Lacinularia :—There is no contractile sac opening into the cloaca as in other genera, but two very delicate vessels, about 1-4000th of an inch in dia- meter, clear and colourless (fig. 3 m), arise by a common origin upon the dorsal side of the intestine. Whether they open into this, or have a distinct external duct, I cannot say. The vessels separate, and one runs up on each side of sis body towards its oral side (fig. 2). Arrived at the level of the pharyngeal bulb, each vessel divides into three branches (fig. 3); one passes over the pharynx and in front of the pha- ryngeal bulb, and unites with its fellow of the opposite side, while the other two pass, one inwards and the other outwards, in the space between the two layers of the trochal disc, and there terminate as coeca. Besides these there sometimes seemed to be another branch, just below the pancreatic sacs. A. vibratile body was contained in each of the ceecal branches ; and there was one on each side in the transverse connecting branch. Two more were contained in each lateral main trunk, one opposite the pancreatic sacs, and one lower down, making in all five on each side. * M. Udekem (Annales des Sciences, 1851) has given a very elaborate, but I think not altogether correct, account of the water-vascular system of Lacinularia. He says that a vascular net-work exists at the base of the lobes of the wheel-organ; that these unite into gland-like ganglia (my ** vacuolar thickenings,” in the margin of the disc infra) ; that from these, vessels proceed to the central glands (vacuolar substance, in which the “band” of the water-vascular system terminates, mihz), from which three great vessels are given off. Of these, one “passes above the digestive tube, and anastomoses with its fellow from the opposite ganglion ; the second presents the same disposition as the first, but is placed below the digestive tube; the third passes directly downwards, skirting the digestive tube.” M. Udekem found it ‘‘impossible to trace it any further, but considers that it becomes lost on the digestive canal and ovaries.” He, therefore, has missed the external opening of the water-vascular system. What I have seen and described as ‘‘ vacuolar thickenings” in the peduncle, are described by M. Udekem as vascular ganglia, from which anastomosing vessels proceed. As M. Udekem’s instrument does not seem to have been good enough to define the vibratile cilium—for he speaks only of a ‘‘ vibratile or trem- bling movement”—I venture to think that he has been misled in describing these threads and vacuolar thickenings as forming any part of the true vascular system. Leydig’s opinion of M. Udekem’s results is, I find, much the same as my own. He says, ‘ Critically considered, then, we find that Udekem’s vascular system in Lacinularia is compounded of a multitude of the most heterogeneous parts of the animal—of structures which belong to the most different systems of organs, without one being a true blood-vessel.”—L. c¢., p- 465. Houxcey on Lacinularia socialis. ih. Each of these bodies was a long cilium (1-1400th of an inch), attached by one extremity to the side of the vessel, and by the other vibrating with a quick undulatory motion in its cavity (fig. 8). As Siebold remarks, it gives rise to an appearance singularly like that of a flickering flame. I particularly endeavoured to find any appearance of an opening near the vibratile cilium, but never succeeded, and several times I thought I could distinctly observe that no such aperture existed. Animals that have been kept for some days in a limited amount of water are especially fit for these re- searches. ‘They seem to become, in a manner, dropsical, and the water-vessels partake in the general dilatation. ‘The “ band” (fig. 7) which accompanies the vessel ap- peared to me to consist merely of contractile substance, and to serve as a mechanical support to the vessel. It terminates above, in a mass of similar substance, containing vacuole, attached to the upper plate of the trochal disc. I shall refer to this and similar structures below. I examined these structures so frequently that I have no doubt that the account I have given is essentially accurate, * and | am strengthened in this opinion by the account and figure of the corresponding vessels in Mesostomum given by Dr. Max Schulze, in his very beautiful monograph upon the Turbellaria (Beitrage zur Naturgeschichte d. Turbellarien). Through these the transition to the richly ciliated water- vessels of the Naidz, &c., is easy enough. Vacuolar Thickenings.—(figs. 2, 8 r). Under this head I in- clude a series of structures of, as I believe, precisely similar nature, which, on Professor Ehrenberg’s principles of interpre- tation, have done duty as ganglia, testes, &c., in short, have taken the place of any organ that happened to be missing. In various parts of the body the parietes have become locally thickened, and the prominences thus formed have * Leydig’s careful description coincides in all essential points with that given above. He particularly notices the fitness of Lacinulariz that have been imprisoned for some time, for the examination of the water-vascular system. The only discrepancy of importance in Leydig’s account is—firstly, that - he considers what I have called the ‘‘ vacuolar thickening on each side of the pharyngeal mass,” and what Ehrenberg calls a nervous centre, to be formed by convolutions of the water-vessel itself; and secondly, that he describes a cloacal vesicle as in other Rotifera. I looked particularly for such a vesicle, but could never see any ; in some cases, indeed, I could - trace the water-vessels distinct from one another, close to the anus. Beyond these particular cases, however, I will by no means venture to contradict so accurate an observer as M. Leydig. Leydig does not seem to have noticed the transverse anastomosing vessel over the pharynx. 8 Hox ey on Lacinularia socialis. developed many clear spaces, or vacuole—a histological pro- cess of very common occurrence among the lower invertebrata. Now these thickenings are especially obvious in two localities—Ist, in the prolongation of the body below the visceral cavity ;* and 2ndly, in the trochal disc. Of the former thickenings, the four uppermost are pro- moted by Professor Ehrenberg to be testes, for no other reason, apparently, than that, having missed the true water- vascular system with its bands, he knew not where else to find what he calls a male organ. Again, the thickenings (figs. 2, 37) in the trochal disc are mostly towards its lower surface and at its inferior margin ; they are generally four or five on each side, and are connected by branched filaments with that body on each side of the pharyngeal mass in which the band of the water-vascular system terminates. ~According to Professor Ehrenberg these are all ganglia, and the two yellowish bilobed or cordate bodies on each side of the pharynx are “ comparable to a brain!” Nervous System and Organs of Sense.{—On the oral side * Leydig (loc. cit., p. 467-8) regards the central vacuolar mass at the root of the tail as a peculiar gland, from which he says a duct runs down- wards to terminate at the extremity of the tail. The purpose of this organ is to secrete the gelatinous envelope. I must confess that I saw no grounds for this interpretation. The extremity of the tail always seemed to me to present a ciliated hemispherical cavity, closed above. + Leydig (1. c., p. 457 et seq.) criticises at length, and altogether re- pudiates, the mythical nerves and ganglions which Professor Khrenberg has ascribed to Lacinularia. He does not appear to have seen either the ciliated cavity, or the body which I still venture to think is the only true ganglion ; but describes a very peculiar nervous system, consisting of— 1. A ganglion behind the pharynx, composed of four bipolar cells, with their processes. 2. A ganglion at the beginning of the caudal prolongation, similarly composed of four larger ganglionic cells and their processes. The latter cells are what I have described as vacuolar thickenings; I could find no difference whatever between them and the thickenings in the disc, which Leydig allows to be mere thickenings. The former were not observed by me. I have not been able to repeat my investigations upon this point, as ] hope to do ; for the present I must offer as arguments against Leydig’s interpretation of the nature of the | structures which he observed— 1st. That the body which I describe as a ganglion is perfectly similar in appearance to the mass on which the eye-spots of Brachionus are seated. 2nd. That if such an arrangement of the nervous system as that which Leydig describes exists, the Rotifera are very widely different from their congeners, and, indeed, from all known animals. Leydig himself, however, says,—‘‘ That these cells, with their radiating processes, are ganglion-globules and nerves, is a conclusion drawn simply from the histological constitution of the parts, and from the impossibility of making anything else out of them, unless, indeed, organs are to be named according to our mere will and pleasure.”—L. c., p. 459. Huxtey on Lacinularia socials. Q - of the neck of the animal, or rather upon the under surface of the trochal disc, just where it joins the neck, and therefore behind and below the mouth, there is a small hemispherical cavity (fig. 40) (about 1-1400th of an inch in diameter), which seems to have a thickened wall, and is richly ciliated within. Below this sac, but in contact with it by its upper edge, is a bilobed homogeneous mass (figs. 2 and 4 2) (about 1-800th of an inch in diameter), resembling in appearance the ganglion of Brachionus, and running into two prolongations below, but whether these were continued into cords or not I could not make out. I believe that this is, in fact, the true nervous centre, and that the sac in connection with it is analogous to the ciliated pits on the sides of the head of the Nemertide, to the “ciliated sac” of the Ascidians, which is similarly connected with their nervous centre, and to the ciliated sac which forms the olfactory organ of Amphiozus. Mr. Gosse has described a similar organ in Melicerta ringens, and | have had an opportunity of verifying his obser- vations, with the exception of one point. According to this observer, the cilia are continuous from the trochal disc into the cup; so far as I have observed, however—and I paid par- ticular attention to the point—the cilia of the cup are wholly distinct from those of the disc. The interesting observations of the same careful observer upon the architectural habits of Melicerta would seem to throw a doubt upon the propriety of ascribing to the organ in question any sensorial function. But however remarkable it may seem that an animal should build its house with its nose, we must remember that a similar combination of functions is obvious enough in the elephant. No eyespots exist in the adult Lacinularia. In the young there are two red spots on the upper surface of the trochal disc, which are stated by Professor Ehrenberg to be seated upon “ medullary masses”? (Mark-Knétchen). I could not satisfy myself either of the truth of this statement or the contrary, in consequence of the difficulty of distinguishing the separate’ tissues in the young animal. I may be permitted here to say a word upon the nature of the “ calcar” or “ respiratory tube” of Ehrenberg, which exists in so many Rotifera. For his first notion, that it is connected with the reproductive system, Professor Ehrenberg has substituted the idea that it 1s a respiratory tube, through which currents of water are conducted into the cavity of the body, and bathe the “trembling organs” which he calls 10 Houxtey on Lacinularia socialis. “gills.” Professor Ehrenberg, however, has not produced any evidence of such in-going currents, and Dujardin has denied their existence. So far as has yet been observed, the calcar is in immediate connection with the nervous ganglion. Melicerta affords a very good opportunity for ex- amining the structure of the organs, of which in this genus there are two. It is a somewhat conical process of the in- tegument, containing a similar process of the internal mem- brane. This, however, stops short a little distance from the extremity, and forms a transverse diaphragm, from the centre of which a bunch of long and excessively delicate sete pro- ceeds (fig.29). I could observe no trace of any aperture with a power of 600 diam., though of course this is merely negative evidence. Is it not possible that, as the “ ciliated sac” of the Asci- dians has its analogue in the “ fossa” of the Rotifera, so the calcar may answer to the “ languet,’ which has a similar relation to both sac and ganglion ? In Notommata there is no calcar, but nervous cords proceed from the ganglion to the ciliated spots about the middle of the dorsal surface (Dalrymple). Reproductive Organs.—Considering Professor Ehrenberg’s determination of the male organs to be set aside, his descrip- tion of the reproductive organs extends only to the ovary, which, he says, in Lacinularia “ lies in the posterior cavity of the body, and has thus one and the same outlet with the intestine ” (p. 403). This seems to imply an oviduct; I could, however, see no such organ.* ‘l’he ovary consists of a pale, slightly granular mass ofa transversely elongated form (fig. 5 7), and somewhat bent round the intestine; it is enclosed within a delicate transparent membrane, which is hardly visible in the unaltered state, but becomes very obvious by the action of acetic acid, which contracts the substance of the ovary and throws the membrane into sharp folds. Pale clear spaces, which sometimes seem to be limited by a distinct membrane, are scattered through the substance of the ovary, and in each of these a pale circular nucleus is contained. ‘The nucleus is more or less opaque, but usually contains 1-3 clear spots (fig. 9). These are the germinal vesicles and spots of the future ova. Acetic acid, in contracting the pale substance, groups it round these vesicles, without, however, breaking it up into separate masses. It renders the nuclei more evident. * Leydig (1. ¢., p. 469) says that there is a wide oviduct which becomes folded when empty. I must leave the discrepancy until a further exami- nation decides which is right. Huxzey on Lacinularia socials. a = The ova are developed thus:—One of the vesicles in- creases in size, and reddish elementary granules appear in the homogeneous substance round it (fig. 10). This accumu- lation increases until the ovum stands out from the surface of the ovary ; but invested by its membrane which, as the ovum becomes pinched off as it were, takes the place of a vitellary membrane. In the mean while the germinal vesicle has increased in size, and its nucleus is no longer visible. In the ovum it appears as a clear space ; isolated by crushing the ovum it is a transparent, colourless vesicle. The perfect ova are oval, about 1-10th inch in diameter, and are extruded by the parent into the gelatinous connect- ing substance, where they undergo their development (fig. 11). The changes which take place after extrusion, or even to some extent within the parent, are—1, the disappearance of the germinal vesicle (as I judge from one or two ova in which I could find none); 2, the total division of the yolk, as described by Kolliker in Megalotrocha, until the embryo is a mere mass of cells, from which the various organs of the foetus are developed (figs. 12, 13, 14, 15, 16). The youngest fetuses are about 1-70th of an inch in length. The head is abruptly truncated, and separated by a con- striction from the body: a sudden narrowing separates the other extremity of the body from the peduncle, which is ex- ceedingly short and provided with a ciliated cavity, a sort of sucker, at its extremity. The head is nearly circular, seen from above, and presents a central protuberance in which the two eyespots are situated. The margins of this pro- tuberance are provided with long cilia—it will become the upper circlet of cilia in the adult. The margin of the head projects beyond this, and is fringed with a circlet of shorter cilia; this is the rudiment of the lower circlet of cilia in the adult. The internal organs are perceived with difficulty ; but the three divisions of the ali- mentary canal, which is as yet straight and terminates in a transparent cloaca, may be readily made out. ‘The water- vascular canals cannot be seen, but their presence is indicated by the movement of their contained cilia here and there (fig. 17). In young Lacinularie, 1-380th of an inch in length, the head has become triangular, the peduncle is much elongated, and thus it gradually takes on the perfect form (fig. 18). The young had previously crept about in the gelatinous investment of the parents ; they now begin to “swarm,” uniting together by their caudal extremities, and are readily pressed out as 12 Hoxtery on Lacinularia socialis. united free swimming colonies, resembling, in this state, the genus Conochilus. The process of development of these ova is therefore exactly that which takes place in all fecundated ova, and would lead one to suspect that spermatozoa should be found somewhere or other. Now, from the observations of Mr. Dalrymple, we should be led to seek a distinct male form with the ordinary sperma- tozoa. From those of Kélliker, on the other hand, we should equally expect to find each individual a hermaphrodite, with the very peculiar spermatozoon-like bodies which he has de- scribed in Megalotrocha. I must have examined some scores of individuals of Lacinu- laria with reference to the former case, without ever finding a trace of a male individual. All were similar, all contained either ova or ovarlum, nowhere was an ordinary spermatozoon to be seen. On the other hand, I found in many individuals singular bodies, which answered precisely to Kélliker’s descrip- tion of the ‘‘ spermatozoa” of Megalotrocha. ‘They hada pyri- form head about 1-1000th in. in diam, (fig. 19), by which they were attached to the parietes of the body, and an append- age four times as long, which underwent the most extraordi- nary contortions, resembling however a vibrating membrane much more than the tail of a spermatozoon; as the undulating motion appeared to take place in only one side of the append- age, which was zigzagged, while the other remained smooth. According to Kélliker again, these bodies are found only in those animals which possess ova undergoing the process of yolk division, while I found them as frequently in those young forms which had not yet developed ova, but only possessed an ovary. Are these bodies spermatozoa ?* Against this view we have * Leydig (loc. cit., p. 474) has observed, in several cases, what I de- scribe as probable spermatozoa, but considers them to be parasites. He does not notice the similarity of these bodies to those described by Kolliker in Megalotrocha ; but thinks that the l-tter has been misled by the vibratile organs. Leydig does not appear to be acquainted with the important observa- tions of Dalrymple, Brightwick, and Gosse; but brings forward as the true spermatozoon a tertium quid, whose description I subjoin in his own words :—‘‘ In almost every colony we meet with from one to four (in large colonies) individuals which are distinguishable from the rest at the first glance. By reflected light they appear quite white, which appearance arises from peculiar corpuscles which fill the cavity of the body more or less completely, and are driven hither and thither by the contractions of the animal, as well into the wheel-organ as into the caudal appendage. They are yellowish globular bodies, with sharp contours, 1-5000th to 1-1700th of an inch in diameter, with a double centre and a lighter peri- phery. The surface is covered by a mesh-work of bands projecting in- ~* Houx.ey on Lacinularia socialis. 13 the unquestionable separation of the sexes in Notommata, and the very great difference between these and the spermato- zoa of Notommata. Neither are the mode of development nor the changes undergone by the ovum any certain test that it requires or has suffered fecundation, inasmuch as the process closely resembles the original development of the aphides (see Leydig, Siebold and Kélliker, Zeitschrift, 1850). In the view that Kélliker’s bodies are true spermatozoa, it might be said—1. That the sexes are united in most Disto- mata, for instance, and separated in species closely allied (e.g. D. Ohenii). 2. That the differences between these bodies and the sperma- tozoa of Notommata is not greater than the difference between those of Triton and those of Rana. 3. That their development from nucleated cells within the body of Megalotrocha (teste Kolliker) is strong evidence as to their having some function to perform; and it is difficult to imagine what that can be if it be not that of spermatozoa. How- ever, it seems to me impossible to come to any definite con- clusion upon the subject at present.* Kolliker supposes that Ehrenberg has seen the ‘ spermato- zoa’’ and has taken them for the ‘ long vibratile bodies ;’’ while Siebold imagines that Kolliker has taken the long vibrating bodies for spermatozoa. No one, however, who has seen both struc- tures can be in any danger of confounding the one with the other. Asexual propagation of Lacinularia.—W hatever may be the nature of the process of reproduction just described, there exists another among the Rotifera, which has been noticed by almost every one, but not hitherto distinguished or understood. This is the production of the so-called “ winter ova,’ but which from their analogy with what occurs in Daphnia, I prefer to call *‘ ephippial ova.” Ehrenberg says that many ova of Hydatina have a double shell, and between the two shells there is a wide space. ‘¢ Similar ones occur in many Rotifera, in various often irre- gular forms: these have a much slower development, and [ call them thence winter ova” (p. 413). See also his account of Brachionus urceolaris (p.512). He does not notice the occur- rence of these ova in Lacinularia or Megalotrocha. ternally, which give the body a mosaic (parquettirtes) appearance. Im- moveable hairs, 1-1700th of an inch long, may be seen in isolated globules to radiate from the surface.” I have not observed any of these bodies. * T may mention here that I have found in Melicerta an oval sac lying below the ovary, and containing a number of strongly-refracting particles ey resembling in size and form the heads of the spermatozoa of Laci- nularia. 14 Houxtey on Lacinularia socials. Kélliker speaks of the ova of Megalotrocha acquiring a deep yellow investment, as if it were a further development of those ova whose yolk he saw divided. I am strongly inclined to be- lieve, however, that he was misled by the peculiar appearance of the winter ova, which look as if they had undergone yolk division. - Dalrymple gives a lengthened account of these peculiar ova in Motommata. He says that they are dark, and that their outer covering appears to consist of an aggregation of cells, under which is a second layer of cells containing pigment molecules. No distinct germinal vesicle, he says, is to be found in these ova ‘‘ from the want of general transparency ” (loc. cit., p.340). It will be observed that all these authors consider the winter ova or ephippial ova and the ordinary ova to be essentially ¢den- tical, only that the former have an outer case. The truth is, that they are essentially different structures, The true ova are single cells which have undergone a special development. The ephippial ova are aggregations of cells (in fact, larger or smaller portions—sometimes the whole—of the ovary), which become enveloped in a shell and simulate true ova. In a fully grown Lacinularia which has produced ova, the ovary, or a large portion of it, begins to assume a blackish tint (fig. 20) ; the cells with their nuclei undergo no change, but a deposit of strongly refracting elementary granules takes place in the pale connecting substance. Every transition may be traced from deep black portions to unaltered spots of the ovarium, and pressure always renders the cells with their nuclei visible among the granules. The investing membrane of the ovary becomes separated from the dark mass so as to leave a space, and the outer surface of the mass invests itself with a thick reddish membrane (fig. 21), which is tough, elastic, and reticulated from the presence of many minute apertures. This membrane is soluble in both hot nitric acid and caustic potass.* The nuclei and cells, or rather the clear spaces indicating them, are still visible upon pressure, and may be readily seen by bursting the outer coat. By degrees the ephippial ovum becomes lighter, until at last its colour is reddish brown, like that of the ordinary ova; but its contents are now seen to be divided into two masses—hemi- spherical from mutual contact (fig. 22). If this body be now crushed, it will be found that an inner structureless membrane exists within the fenestrated membrane, and sends a partition * Leydig (I. c., p. 453) says that the shells of the ova were not dis- solved by maceration in a solution of caustic soda (cold?) for twenty-four hours, and thence concludes that they may be composed of chitin. The above observation tends to the contrary conclusion. Huxuey on Lacinularia socials. 15 inwards, at the line of demarcation of the two masses (fig. 23). The contents are precisely the same as before, viz., nuclei and elementary granules (fig. 24). This, indeed, may be seen through the shell without crushing the case. I was unable to trace the development of these ephippial ova any further. Those of MNotommata, it appears, lasted for * some months without change (Dalrymple). It is remarkable that in Lacinularia these bodies eventually, like the ephippium of Daphnia, contain two ovum-like masses ; and there can, I think, be little doubt that the former, like the latter, are subservient to reproduction. There are then two kinds of reproductive bodies in Lacinu- laria :— 1. Bodies which resemble true ova in their origin and subsequent development, and which possess only a single vitellary membrane. 2. Bodies, half as large again as the foregoing, which re- semble the ephippium of Daphnia; like it have altogether three investments; and which do not resemble true ova either in their origin or subsequent development ; which therefore probably do not require fecundation, and are thence to be considered as a mode of asexual reproduction.* General Relations of the Rotifera.—It is one of the great blessings and rewards of the study of nature that a minute and laborious investigation of any one form tends to throw a light upon the structure of whole classes of beings. It supplies us with a fulcrum whence the whole zoological universe may be moved. I would illustrate this truth by showing how, in my belief, the structure of Lacinularia, as thus set forth, taken in conjunction with some other facts, gives us a clue to the solu- tion of the questio vexata of the zoological position of the Rotifera, and thence to the serial affinities of a large portion of the Invertebrata. * Leydig distinguishes particularly between the ordinary, and what I have termed, the ephippial ova. His description of the latter agrees essentially with that which has been given above; but he has not, I think, observed the genesis of the ephippial ova with sufficient care, and he thence interprets their structure by sup- posing that they are ordinarily fecundated ova, which have undergone a peculiar method of cleavage. The tendency of the observations de- tailed above, on the other hand, is to show that they are not ova at all in the proper sense, but peculiar buds like those of Aphis or Gyrodactylus, and as such are capable of development without fecundation. In the new edition of Pritchard’s ‘ Infusoria,’ it is stated (p. 620), that “‘in a recent paper by Mr. Howard on this species, he states that there are two kinds of reproductive bodies—one the ordinary ova, the other twice their size, representing gemmz.” No reference is given to Mr. Howard’s paper, and I have been at a loss to discover it, though desirous to do justice to him if possible. i Hextey on Lacinularia socialis. The curious analogy in form between the genus Stepha- noceros and the Polyzoa has, I believe, been the chief considera- tion which has led many naturalists, both in England and on the Continent, to arrange the Polyzoa and Rotifera together. This has been done in two ways, either by denying the affinity of the Rotifera with the Vermes, and so approximating them to the Polyzoa considered as organized on the molluscous type, or, as Leuckhart has done, by admitting the affinity of the Rotifera with the Vermes, but denying that of the Polyzoa with the Mollusca. I believe that there is a fundamental error in each case, namely, that of approximating the Polyzoa and the Rotifera at all. The resemblance between Sfephanoceros and a Poly- zoon is very superficial. No Polyzoon has the cilia on its tentacles arranged like those of Stephanoceros ; nor has any a similarly-armed gizzard: still less is there any trace of the water-vascular system which exists in all Rotifera. The relations between the Polyzoa and the Rotifera, then, are at the best mere analogies. On the other hand, the general agreement in structure be- tween the Rotifera and the Annuloida— under which term I include the Annelida, the Echinoderms, Trematoda, ‘lur- bellaria, and Nematoidea—is very striking, and such as to constitute an unquestionable affinity.* The terms of resemblance are these :— 1. Bands of cilia, resembling and performing the functions of the wheel-organs, are found in Annelid, Echinoderm, and Trematode larve. | 2. A water-vascular system, essentially similar to that of the Rotifera, is found in Monececious Annelids, in Trematoda, in Turbellaria, in Echinoderms, and perhaps in the Nema- toidea.} 3. A similar condition of the nervous system is found in Turbellaria. 4. A somewhat similarly armed gizzard is found in the Nemertidz ; and the pharyngeal armature of a Nereid larva may well be compared with that of Albertia. 5. The intestine undergoes corresponding flexures in the Echinoderm larve. There are, therefore, no points of their organization in which the Rotifera differ from the Annuloida ; * M. Milne Edwards, with his accustomed acuteness, pointed out (Annales des Sciences, 1845) the close affinity of the Rotifera with the Annelids, the Turbellaria, and the Nematoidea; but he did not include the Echinoderms in the group, doubtless because, at the time he wrote, sufficient was not known of the Echinoderm larve to demonstrate their truly annuloid nature. + To these may be added the Cestoidea and the Nemertide. Huxtey on Lacinularia socialis. 17 and there is one very characteristic circumstance, the presence of the water-vascular system, in which they agree with them. Now, with what Annuloida are the Rotifera most closely allied? To determine this point, we must ascertain what is the fundamental type of organization of the Rotifera. _ Suppose in Lacinularia a line to be drawn from the mouth ° to the anus, and that this be considered as the axis of the body ; suppose, again, that the side on which the ganglion lies is the dorsal side, the opposite being the ventral ; suppose, also, the mouth end to be anterior, the anal end posterior,—then it will be found that the lower circlet of cilia upon the trochal disc encircles the axis of the body, while the upper circlet of large cilia does not encircle the axis, but lies in the lower and an- terior region of the body. If the region behind that ciliary circlet which is traversed by the axis be called the post-trochal region, and that in front of it the pre-trochal region, we find that the circlet of large cilia is developed in the inferior pre-trochal region. Now compare this Rotifer with the larva of an Annelid. It will be immediately seen that the two are of essentially the same type, only that, while the Annelid larva is equally and symmetrically developed in all its regions, and has _ frequently no accessory ciliated bands, the Rotifer has its superior post-trochal and inferior pre-trochal regions de- veloped in excess ; so that the anus is thrown to the ventral, while the mouth is thrust towards the dorsal surface,* an accessory ciliated circlet being at the same time developed in the latter region. Meliceria ringens (compare figs. 26-28) resembles Lacinu- laria in the arrangement of its ciliated bands, only they are far more distorted from their normal circular form. Tubi- colaria closely resembles Melicerta, and there can be little doubt that Megalotrocha and Limnias are to be added to this division. In Brachionus, Philodina, Rotifer, Notommata, the same fundamental type obtains, but the deviation from symmetry takes place in a different way. In all these it is the ventral post-trochal region which is over-developed, and therefore the anus is thrown to the dorsal or ganglionic side. In Notommata the trocha appears to be simple and un- altered in most species, and there is no accessory circlet. * This over-development is not a mere matter of hypothesis. The young Lacinularia has the anus nearly terminal, and the “‘ peduncle” only subsequently attains its full proportions. Compare fig. 17 and fig. 18, pL. VOL. I. Cc 18 Hoxtey on Lacinularia socialis. In NV. aurita, however, as it appears from Mr. Gosse’s de- scription, and in Brachionus polyacanthus (figs. 30-33), several processes, three in the latter case, are developed from the superior pre-trochal region. They are richly ciliated, and appear to represent the accessory circlet of Lacinularia. Another distinct type is presented by Philodina (figs. 34- 37). In this the great trocha is bent upon itself, and the anterior divison of it, at first sight, simulates an accessory circlet developed in the superior pre-trochal region. It is not so, however, as the continuity of the band of cilia can be readily traced throughout. To this division of the Rotifera, viz. those which have the anus on the same side of the body as the ganglion, appear to belong the genera Stephanoceros and Floscularia—at least, if the ganglion be what I believe it to be, a granular mass, in connexion with the upper part of a large oval mass com- posed of clear cells, and having a pit in its centre exteriorly, which I believe to be the altered ciliated sac. These might then be considered as Notommate whose trochal circlet had become produced into long processes in Stephanoceros, while they remain as shorter knobs in Filos- cularia ; a tendency to which development may be traced in the little processes into which the trochal circlet is thrown around the mouths of Lacinularia and Melicerta, and perhaps in the three processes which, according to Mr. Dalrymple, arch over the mouth in Notommata. But Stephanoceros, Philodina, Notommata, Brachionus, and Lacinularia are the types of the great divisions of the Rotifera, and whatever is true of them will probably be found to be true of all the Rotifera. We may say, therefore, that the Rotifera are organized upon the plan of an Annelid larva, which loses its original symmetry by the unequal development of various regions, and especially by that of the principal ciliated circlet or trochal band; and it is curious to remark that, so far as the sexes of the Rotifera can be considered to be made out (approximatively), the dicecious forms belong to the latter of the two modifications of the type which have been described, while the moneecious forms belong to the former. | It is this circumstance which seems to me to throw so clear a light upon the position of the Rotifera in the animal series. In a Report in which I have endeavoured to harmonise the researches of Prof. Miller upon the Echinoderms,* I have shown that the same proposition holds good of the latter in * Annals of Natural History, 1851. Huxtry on Lacinularia socials. 19 their larval state, and hence I do not hesitate to draw the con- clusion (which at first sounds somewhat startling) that the Rotifera are the permanent forms of Echinoderm larve, and hold the same relation to the Echinoderms that the Hydriform Polypi hold to the Medusz, or that Appendicularia holds to. the Ascidians. The larva of Sipunculus might be taken for one of the Rotifera; that of Ophiura is essentially similar to Stephano- ceros; that of Astertas resembles Lacinularia or Melicerta. The pre-trochal processes of the Asterid larva Brachiolaria are equivalent to those of Brachionus. Again, the larve of some Asterid forms and of Comatula are as much articulated as any Rotifera. It must, I think, have struck all who have studied the Echi- noderms, that while their higher forms, such as Echiurus and Sipunculus, tend clearly towards the Dicecious Annelida, the lower extremity of the series seemed to lead no-whither. Now, if the view I have propounded be correct, the Rotifera furnish this wanting link, and connect the Echinoderms with the Nemertidz and Nematoid worms. At the same time it helps to justify that breaking up of the class Radiata of Cuvier, which I have ventured to propose elsewhere, by showing that the Rotifera are not ‘ radiate” animals, but present a modification of the Annulose type— belong, in fact, to what I have called the Annuloida, and form the lowest step of the Echinoderm division of that sub- kingdom. From our imperfect knowledge of the Nematoid worms it is difficult to form a definite scheme of the affinities of the Annuloida; but perhaps they may be sketched as in the Diagrams, pl. III. | These diagrams represent the arrangement of the ciliated bands with relation to the axis of the body in the Rotifera. Underneath each Rotifer is an Annelid or Echinoderm larva, with its ciliary bands represented in a like diagrammatic manner, to show the essential correspondence between the two. This paper is now printed exactly as it was read before the Micro- scopical Society on the 81st of December, 1851, with the exception of those notes which refer to the very excellent memoir of Dr. Leydig, pub- lished in February, 1852. Dr. Leydig must have been working at the subject at about the same time as myself, in the autumn of last year ; and if I refer to the respective dates of our communications, it is merely for the purpose of giving the weight of independent observation to those points (and they are the most important) in which we agree. — It is the more necessary to draw attention to this fact, since Professor Ehrenberg, in a late communication to the Berlin Academy, hints that the younger observers of the day are in a state of permanent conspiracy against his views. fy ic he July 9, 1852. e2 (1 BD i) On the Structure of the Rarnmes of Cactus ENNEAGONUs. By Joun Quexett, Esq., Professor of Histology to the Royal College of Surgeons of England. (Read Jan. 28, 1852.) Every living being that is made up of parts or organs, each having a definite structure, and performing a certain office, is termed an organized being; and the materials, however com- plicated, of which it is composed, are termed organic matter. The components of the Mineral Kingdom, on the contrary, possessing little or no structure, but generally being homoge- neous throughout, and having no adaptation of parts to per- form separate functions, are called inorganic or inorganized. If organic matter be subjected to chemical analysis, it will be found that in the first stage certain compounds, termed by some chemists proximate principles, or organic compounds or organizable substances by others, will be obtained; each of which principles, by further or ultimate analysis, will yield simple elements. ‘Thus, for instance, from the organized sub-_ stance termed muscle we obtain by analysis, first, fibrine, a proximate principle, which is its chief constituent; and, sub- sequently, by the analysis of fibrine, we get the principal elements—oxygen, hydrogen, carbon, nitrogen, and sulphur in certain proportions. If, however, a mineral, or inorganic matter of any kind be subjected to analysis, we get no proxi- mate principles, but only simple elements. Organic matter may be found in two states, viz., in that of life or in that of death. Living matter possesses the powers of growth and integrity, may select from surrounding materials, and appro- priate to its uses the inorganic elements; but in the state of death these powers are destroyed, and decay is the natural consequence. It is to the nature of this organic basis or matter of plants that I would now direct your attention, leaving that of animals for future consideration. In commencing our examination with the vegetable king- dom we shall find that inorganic or earthy matter exists in plants in two states, viz., Ist, as crystals, termed raphides, occurring in the interior of cells, and 2nd, in intimate con- nexion with the organic basis of the plant—ain this last state the inorganic element chiefly consists of silica. If we examine a portion of the layers of an onion or of a squill, or by taking a thin section of the stem or root of the garden rhubarb, we shall observe many cells in which either bundles of needle-shaped crystals or masses of a stellate form occur; these are termed raphides, from the Greek Pagis, a needle, the first crystals discovered being of this shape. Quexert on the Raphides of Cactus enneayonus. 21 Raphides were first noticed in Malpighi in Opuntia, and were subsequently described by Jurine and Raspail. According to the latter observer the needle-shaped or aci- cular are composed of phesphate, and the stellate of oxalate of lime. There are others having lime as a basis, combined with tartaric, malic, or citric acid. These are easily de- stroyed by acetic acid; they are also very soluble in many of the fluids employed in the conservation of objects: some of them are as large as the 1-40th of an inch; others are as small as the 1-1000th. They occur in all parts of the plant—in the stem, bark, leaves, stipules, sepals, petals, fruit, root, and even in the pollen, with few exceptions. They are always situated in the interior of cells, and not, as has been stated by Raspail and others, in the intercellular passages.* Some of the containing cells become much elongated, but still the cell-wall can be readily traced. In some species of Aloe, as for instance Aloe verrucosa, with the naked eye you will be able to discern small silky filaments. When these are magnified they are found to be bundles of the acicular form of raphides. In portions of the cuticle of the medicinal squill— Scilla maritima—several large cells may be observed, full of bundles of needle-shaped crystals. These cells, how- ever, do not lie in the same plane as the smaller ones belong- ing to the cuticle. In the cuticle of an onion every cell is occupied either by an octohedral or a prismatic crystal of oxalate of lime—in some specimens the octohedral form pre- dominates, but in others from the same plant, the crystals may be principally prismatic, and are arranged as if they were be- ginning to assume a stellate form. Those persons who are in the habit of examining urinary deposits must be familiar with the appearance of the crystals of oxalate of lime, and would readily recognise their close resemblance to those in the cells of the onion. Raphides of oxalate of lime are found in very great abund- ance in the medicinal rhubarb—the best specimens from Turkey containing as much as 35 per cent.; those from the East Indies 25 ; and the English, or that sold in the streets by men dressed up as Turks, 10 per cent. Buyers of this drug generally judge of its quality by its grittiness, that is by the quantity of raphides it contains ; and this is a curious fact, as the crystalline matter cannot be of any beneficial importance in the action of the medicine, for the * As as exception I may state that, many years ago, I discovered them in the interior of the spiral vessels in the stem of the grape-vine; but with some botanists this would not be considered as an exceptional case, the vessels being regarded as elongated cells. 22 Quexerr on the Raphides of Cactus enneagonus: tincture in which no raphides are contained is as efficacious as the powder. Some plants, as many of the cactus tribe; are made up almost entirely of raphides. In some instances every cell of the cuticle contains a stellate mass of crystals, in others the whole intericr is full of them, rendering the plant so exceedingly brittle that the least touch will occasion a fracture, so much so that some specimens of cactus senilis, said to be 1000 years old, which were sent a few years since to Kew from South America, were obliged to be packed in cotton, with all the care of the most delicate jewellery to preserve them during the transport, Raphides of peculiar figure are common in the bark of many trees. In the hiccory (Carya alba) may be observed masses of flattened prisms having both extremities pointed. Similar crystals are present in the bark of the lime-tree; they occur in rows, their pointed extremities nearly touching each other, their principal situation being in the cellular tissue close to the medullary rays. Other forms of crystals, as the rhom- bohedron and a small stellate form, are also found in the bark of the lime. In vertical sections of the stem of Eleagnus angustifolia nu- merous raphides of large size may be seen in the pith. Raphides are also found in the bark of the apple-tree, and in the testa of the seeds of the elm; each cell contains two or more very minute crystals. It is at present not known what office raphides perform in the economy of the plant: some have gone so far as to state that they are deposits to be applied towards the mineral part or skeleton of the plant; but the fact of their being insoluble in vegetable acids would prove this view of their use to be erroneous. The more rational supposition is, that they are generally accidental deposits formed by the union of vege- table acids with lime or other base existing in the plant or taken up from the soil. They may, however, be formed artificially, and my late brother succeeded in doing so in the following manner :—If oxalic or phosphoric acid be added to lime-water, the precipitate will be pulverulent and opaque. If, however, a vessel containing oxalate of ammonia in solution be connected by means of a few filaments of cotton with another vessel containing lime-water, crystals will be formed at the end of the fibres in contact with the lime-water. This led him to attempt to form them in the interior of cells: he selected for the purpose a portion of rice paper ; this substance was placed in lime-water under an alr-pump in order in fill the cells with the fluid ; the paper was then dried, QueKeEtTT on the Raphides of Cactus enneagonus. 23 and the process again and again repeated, until many of the cells were charged with lime-water; portions of the paper were then placed in weak solutions both of oxalic and phos- phoric acid, and at the end of three days crystals were found in the cells in both instances, those of the oxalic acid being of _ the stellate and those in the phosphoric acid being of the rhombohedral form. None of the acicular, however, were ever present, although the process was continued for ten days. One of these pieces of rice paper I now show you, and a stellate mass of crystals is very plainly to be seen in the centre of the field—each precisely resembles the raphides found in rhubarb. The above description, which is a modification of that given in my lectures, well applies to the raphides in most plants, but the case will appear to be a little different in those plants, such as the cacti, which live to a great age, and in which the crystalline matter is in the greatest abundance. Whilst working at this subject about twelve months since I was in- duced to examine the raphides of a species of Cactus termed enneagonus, a specimen of which had been given me by a friend as abounding in crystals. This specimen I have with me, just as I received it, the part containing the crystals being about thirty-nine years old; that they are very numerous, and at the same time very large, may be known by their being visible to the naked eye. If any of these raphides be examined in fluid with a power of at least 100 diameters, they will appear to be made up of crystals (as far as their external surface is con- cerned), which project outwards in the form both of sharp pointed and truncated prisms; and if the centre be brought into focus this part will be found more opaque than the rest, and to be of a circular figure like a nucleus. If the masses be mounted in Canada balsam before they are examined they will then present one or other of the appearances given in Plate III. figs. 1, 2, 3,4; some, as in fig. 1, will show a nucleus surrounded by concentric lamine of a brown colour ; others, as in fig. 2, will exhibit a spot like a nucleus, first surrounded by concentric lamine, but towards the margin the laminze become irregular, and the margin itself is composed of prismatic flattened crystals, not clear and transparent, but more or less granular, whilst some other specimens, as shown in figs. 3 and 4, are made up almost entirely of the prismatic crystals, with little or no trace of concentric lamination. Having found this to be the case I was anxious to ascertain the chemical com- position of these so-called raphides, and for the purpose I tried the action of various re-agents upon them, and noticed that the crystals were slowly dissolved in dilute hydro-chloric 24 QuvexeErr on the Raphides of Cactus enneagonus. acid, but I was much astonished to find that in many cases a basis or cast of the entire mass was left behind after the action of the acid had ceased ; and in most instances I could tell pre- cisely not only the spot where the crystals had been, but also form some general idea of the shape of the mass, and instead of their being, as I first imagined, a mass of crystals only, { found that there was some organic matter or basis connected with them. | When one of these raphides is crushed between two plates of glass, the outer crystals are readily detached ; some of these are represented by fig. 6: the part composing the nucleus is much the hardest, and exhibits a radiated and concentric laminated deposit, like the masses of carbonate of lime found in the urine of the horse. If portions of the cellular tissue of the cactus be examined, some cells will occasionally be found in which a more or less spherical mass, as shown in fig. 5, occurs in the centre of each: these masses correspond in every respect with the nuclei of the larger raphides: it would there- fore appear that in the early stages of development of these raphides the nucleus consisted of one of these spherical bodies, and the crystals on the exterior were formed subsequently. It may also happen that the bases of some of the crystals in process of time coalesce to form laminz, a condition not unlike that occurring in shell, as has been so well described by Dr. Carpenter, or rather like that which takes place in the formation of most of the laminated kinds of urinary calculi. My object in bringing the subject before the Society at this time is to ask those of our members who are chemists, and would be willing to look into the matter, if they could deter- mine the nature of the residuum or basis left after the destruc- tion of the earthy ingredient by means of the acid. They will find, as I shall presently have the opportunity of showing you, that there is something peculiar in the dissolution of the crystals—they are all, more or less, granular, as if the organic matter were not confined to the investing membrane, but int1- mately mixed up or incorporated with every atom of the lime. I have this day examined some sections of the Soap wood of China, in which stellate masses of crystals are very abundant. If these be acted on by dilute hydrochloric acid, the earthy constituent will disappear, but a cast of the original mass will be preserved in what may be termed organic matter. This point, however, is the one which requires to be carefully ex- amined by persons more skilled than myself in the science of organic chemistry. As far as my observations have hitherto gone, it would appear to be a rule that we rarely, if ever, find inorganic Quexetr on the Raphides of Cactus enneagonus. 25 material in the vegetable or animal kingdom, except in the crystalline state, without the existence of an organic basis. Since the above was written, my friend Dr. Lionel Beale has been kind enough to examine the raphides in question, . and the following is his report on the subject. “ A few of the white globular crystalline masses were treated with boiling distilled water, and the aqueous solution, after being filtered, was evaporated to a small bulk. Upon examining the residue by the microscope, numerous small colourless crystals, in the form of obtuse rhomboids, were observed. The residual solution was found to give precipi- tates insoluble in strong nitric acid, with solutions of nitrate of barytes and nitrate of silver, proving the presence of chlorine and sulphuric acid. Oxalate of ammonia gave a pre- cipitate insoluble in acetic acid, but soluble in strong nitric acid, showing the presence of lime. “* Hence boiling distilled water extracted a small quantity of soluble matter, which contained lime, chlorine, and sul- phuric acid, probably in the form of sulphate of lime and chloride of sodium. “« Acetic Acid.—The crystalline masses were not affected by boiling acetic acid. “‘ Potash.—No observable action was produced by boiling a few of the masses in solution of caustic potash. “ Nitric Acid—Upon the addition of strong nitric acid, effervescence occurred with some few of the bodies as they dissolved, but upon the majority this re-agent exerted little action in the cold. When the mixture was boiled, complete solution immediately took place. “The acid solution was evaporated to dryness; the dry residue was boiled in distilled water, and the filtered solution, after concentration, was allowed to remain in a still place for some time. Upon examining the residue with the microscope numerous well-formed octohedra of oxalate of lime were ob- served. “¢ Another portion of the original matter was incinerated :— the masses still retained their globular form, but became black, and the products of combustion burnt with a blue lambent flame. After exposure to a dull red heat for three or four hours, the crystals were perfectly decarbonized, and by the unaided eye could scarcely be distinguished from those which had not been incinerated. Upon microscopical examination, however, the crystalline fragments of which the crystalline masses were composed, were found to have acquired a dark granular uneven surface, and the sharpness of outline had been 26 QueEKETT on the Raphides of Cactus enneagonus. destroyed. The decarbonized residue was entirely dissolved in acetic acid with brisk effervescence ; and upon the addition of a solution of oxalate of ammonia to the acid solution, an abundant white precipitate was immediately produced; this was soluble in strong nitric acid, but insoluble in excess of acetic acld—oxa/ate of lime. In all probability, therefore, the crystalline masses consisted of— “ 1, A little organic matter ; “2. Sulphate of lime ; “ 3. A little of carbonate of lime ; ‘* 4. Traces of chloride of sodium ; “* 5. A vegetable salt of lime, containing a considerable pro- portion, or consisting entirely of oxalate of lime.” On the occurrence of a Membranous Cell or Cyst upon the Olfactory Nerve of a Horse, containing a large Crystal of Oxalate of Lime. By James B. Simonps, Esq. (Read April 28, 1852.) | Tue recent publication of Mr. Quekett’s lectures on the occur- rence of earthy salts in both animal and vegetable cells gives an unusual interest to these depositions, and more especially when they are met with in those parts of the organism of animals where we should scarcely anticipate their presence. For this reason, and as an addendum to his valuable papers now being read before the Society, I am induced to bring before you an interesting and novel fact which has lately come to my knowledge relating to a deposit of the oxalate of lime within a cell or small membranous cyst. : In the latter part of March a pupil of the Royal Veterinary College found, in dissecting the brain of a horse which had been procured from the slaughterhouse, a small transparent cyst, possessing a very bright or glistening aspect, attached to the bulbous portion of the right olfactory nerve. ‘The speci- men, together with a small portion of the nerve, was carefully removed, and a day or two afterwards it was kindly presented to me, he at that time believing it to be an hydatid. From having been kept in water I found that the nerve was somewhat decomposed, and very readily separated into a pulpy mass ; a circumstance which prevented any minute examina- tion of its structure being made. I observed, however, that its substance was partly absorbed, so as to form a cup-like con- cavity for the lodgment of the cyst; and I am led to infer from this circumstance that the sense of smell of the animal On a Cyst upon the Olfactory Nerve of a Horse. ie was greatly interfered with, and probably rendered very obtuse. But of this, as well as the existence or otherwise of pain from the pressure of the cyst, we are without means of ascertaining. On placing the specimen under the microscope, and viewing - it with a two-inch object-glass, I was surprised to find a large octohedral crystal of oxalate of lime, with beautifully de- fined facets freely floating in a limpid fluid which distended the walls of the cell. There appeared to be no obstacle to the passage of the crystal from side to side of the cavity or in any other direction when the specimen was placed in different posi- tions, its weight quickly carrying it to the most depending part. The walls of the cell have every indication of being composed of layers of areolar tissue spread out in a membranous form ; they are not, however, of uniform thickness throughout, although everywhere very translucent. Towards the circum- ference or periphery of the cell on one side there exists a bell-shaped spot (a Fig. 1, Pl. 1V.), which is thinly co- vered with membrane, but surrounded with many fibres, far more dense than in any other part. Beside the crystal within the interior there is a small mass of granular-like matter, which can also be made to vary its position; this mass is marked b. The occurrence of this deposition of the oxalate of lime in this situation is the more interesting from the circumstance that this salt of lime is very rarely met with in the urine of the horse, in which the carbonates, on the contrary, are very com- mon. Various forms of the carbonate of lime are noticed in the urine of the herbivora, produced by causes disturbing its ordinary mode of crystallization ; but none of these forms can be confounded with the octohedral arrangement of the oxalate. The priority of the formation of the cell or the crystal is not easy to be determined, it being possible that the blood of the animal, from impregnation with the oxalate of lime, deposited this salt in the place it was found, and that subsequently a cell enclosed it to prevent any serious ill consequences to the surrounding organism; or it may be that the cell was first formed, and then the salt was effused into its interior, where it led to the exudation also of fluid. Itis perhaps right to mention, in conclusion, that several capillary vessels are to be observed ramifying upon the walls of the cyst, and that it was firmly held in its place by fibres of areolar tissue. I may also add that the crystal has not been measured to ascertain its exact size, but that it can very readily be seen by unassisted Vision. C28) On the Development of Tubularia indivisa. By J. B. Mum- MERY, Esq. [Read May 26, 1852. | Havine found considerable difficulty in reconciling the accounts given by various naturalists of the development of Tubularia indivisa, | was gratified to have discovered a locality whence I could obtain by the dredge a regular supply of fresh speci- mens of that very interesting zoophyte; and during the past six months have made almost daily observations by the micro- scope upon its structure and development. The painstaking investigations of the late Sir John Graham Dalyell appear to have supplied much of the information pub- lished on the subject. It appeared however to me, on comparing the results of my own observations with the accounts and figures contained in the work of that indefatigable observer, that he had ever laboured under the disadvantage of employing a very imperfect microscope, and consequently misapprehended some of the phenomena to which he directed his patient attention. The general form of Tubularia indivisa has repeatedly been well described, but there are some portions of its structure re- specting which greater accuracy appears desirable. ‘The repro- ductive gemmules have usually been described as origimating at the base of the lower row of tentacules, and, owing to the pro- fusely crowded situation of these oviform bodies in the full- grown head, it is quite impossible to detect their real place of attachment to the body. It is however a well-known fact, that the full-grown head within three or four days drops from the stalk, and that in the course of six or seven days a new head is produced from the medullary pulp. On examining the newly-formed head, under a magnifying power of fifty diame- ters, the oviform gemmules are even at this early stage per- ceptible, arranged upon the outer surface of the body, and ex- tending vertically from the lower tentacules to the base of the oval tentacules in twelve equidistant lines ; two of the lower . tentacules originating in the space between each ovary, thus making the whole number twenty-four. In the early stages of their growth the capsules are attached to the ovary by a very short and somewhat thick stalk; the stalk gradually becomes elongated, having the capsules affixed alternately on each side throughout its length by a broad attach- ment, and the substance of the capsule is now of a pale rose- colour. As development advances the general rosy tint disappears, and the colouring matter appears concentrated in a well-defined organ of deep-red colour, which evidently supplies the connect- Mummery on the Development of Tubularia indivisa. 29 — ing link between the stalk and the enclosed embryo, and has been denominated the placental column. The pedicle, attach- ing the capsules to the stalk, having now become much smaller in proportion, the stalk, with its capsules, presents the appear- ance of a bunch of grapes. Sir John Dalyell declares his in- | ability to discover the ascending and descending currents con- veying granular matter, which have been observed in the stem of Tubularia by several naturalists. In addition to these, how- ever, I have distinctly noticed similar, though not equally ener- getic currents, in the stem supporting the reproductive gem- mules. The writer just named appears to have never detected more than one embryo in each cyst, but in some specimens I have found each cyst in the group to contain two, and occasionally even three embryos, distinctly perceptible through the sides of the cyst, which is sometimes quite transparent. While some clusters are fast approaching maturity, others, attached to the same ovary, are still in the very earliest stages of growth. As the contents of the capsules at length arrive at maturity, a bright red spot (which for some weeks past had become per- ceptible at the apex of the capsule) is observed slowly to expand in a quadrangular form, presenting the eppermce shown in fig. 3, Pl. 1V. The basal extremity of the nascent animal is now seen slowly emerging,—the drawing (in the particular instance illustrated) exhibiting the progress of development at intervals of an hour, commencing at 8 30 p.m., and concluding at 1 30 a.m., when the process of extrication was complete. The extremity which will form the future point of attachment in the fixed state of the young animal is always presented towards the aperture of the capsule, which appears to be dilated solely by the efforts of the animal. Slowly it emerges, withdrawing its tentacles in succession, until it has set itself free, when it crawls slowly upon the bottom of the vessel containing it, elevating itself on the extremities of its eight tentacles. After a period of time, varying from one to four days, the animal (which,.in its free condition, has never been remark- able for activity), having selected a suitable stone, or the surface of an old polypidon, reverses its position, and, with the mouth upwards, now attaches itself by the opposite ex- tremity, and remains rooted fast for life. In every instance that has come under my notice, the first animal that escapes is of an ellipsoidal form, not very greatly 30 Mummery on the Development of Tubularia indivisa. differing from the adult, excepting in the number of its ten- tacles, Within five minutes after the extrication of the animal already described, a second escapes through the dilated mouth of the capsule, but differing greatly from the former in con- figuration. It closely resembles, in miniature, a young spe- cimen of one of the star-fishes (Solaster papposa), presenting a discoidal form, surrounded by twelve obtuse tentacles. In the course of thirty-six hours this had greatly changed in form, and, within a few days after, the two varieties pre- sented but slightly different aspects, especially after they had fixed themselves. The empty capsule, or ovisac, with its contained placental column, remains dilated, exactly as when the young animals quitted it. After the lapse of about six weeks, the animals, which were previously colourless, gradually acquire a pale rose tint around the head, and eventually the ovaries are developed as it ap- proaches: the adult state. Much difficulty is experienced in preserving this zoophyte in a healthy state for examination, but it may be worth ob- serving that I at length succeeded tolerably well by connect- ing a syphon of gutta percha with a reservoir of salt water, and thus causing a small stream to fall from a height of several feet upon the surface of the water containing the specimens, and allowing the surplus water to overflow into a larger re- ceptacle. The agitation thus produced had the effect of retarding the fall of the heads. I trust I may be pardoned for referring to the highly in- teresting suggestion of Professor Forbes, in his admirable treatise on the naked-eyed Meduse, viz.: That possibly all the Medusz are, at one period of their life, fixed animals, as proved by Sars in the case of Cyanea aurita ; and that, con- versely, many of the zoophytes may be found to pass through a medium stage of existence, during which the germs are developed from which the zoophyte is reproduced,—as in the instances of Laomedea and Cyanea. As the latter zoophyte presents so close an affinity to the subject of my remarks, I have most carefully repeated my observations, and feel convinced that the animal which escapes from the pedunculated capsule is distinctly trace- able through all its stages, until, when fixed, it becomes the adult Z'ubularia, and that it undergoes no intermediate metamorphosis, or alternation in its mode of existence; I have thought it possible that the eight-armed creature might prove a Medusoid. Col.) Some Observations on the Structure and Development of VoLvox GLOBATOR, and its relations to other unicellular Plants. By Gro. Busk, Esq., F.R.S. (Read May 26, 1852.) THREE forms, or, as they are commonly regarded, species of Volvox are described and figured in Ehrenberg’s great work, and have been noticed by other observers. These are V. glo- bator, V. aureus, and V. stellatus. A fourth very similar or- ganism hasalso been described under the name of Spherosira Volvozx. . As I regard the three first named of these at all events, merely as forms or phases of one and the same species, the following observations will apply in some respects to all of them. They have more particular reference, however, to the common form of V. globator, which happens to be that most accessible to me. This beautiful and well known object, which was first noticed by Leeuwenhoek, received little satisfactory elucida- tion until it fell under the observation of Ehrenberg, whose account of its structure and notions respecting its nature have been adopted by most subsequent observers, and have been received with little opposition until very lately—ain fact until the beginning of last year. At that time Professor William- son read a paper on the subject before the Manchester Lite- rary and Philosophical Society, which is published in the 9th volume of their Memoirs. ~ Professor Williamson’s observations have led him to con- clusions in many points opposed to those arrived at by Ehrenberg, and especially are they confirmatory of Siebold’s original view of the vegetable nature of Volvor. With respect to some points of structure, however, concerning which Professor Williamson differs from the Prussian observer, I am inclined, from my own observations, to side with the latter, whose errors in the case of Volvox are not those of direct observa- tion ; but in this instance, as in very many others, itis obvious that Ehrenberg has allowed his imagination, working upon preconceived notions, to play the part of reason in the inter- pretation of correctly-observed phenomena; he has thence, in the explanation of what he has seen correctly, fallen occa- sionally into great and important errors. Whilst it cannot © be denied that the recent progress of knowledge with respect to the structure and nature of the lowest classes of organised beings, places an observer of the present day in a position so much more advantageous, that it is scarcely fair to institute a comparison between him and the great and laborious Prussian microscopist, at the time his principal works were written, VOL. I. d 32 Busk on Volvox globator. still it is much to be regretted that these modern lights, clear as they are, have not apparently been allowed to penetrate his mind, and that one to whom science is so much and so deeply indebted should retain views long since deservedly exploded by nearly all competent observers. The more common and best known form of Volvozx ghobdton, to the naked eye, or under a low power, appears as a trans- parent sphere, the surface of which is studded with numerous, regularly placed green granules or particles, and which con- tains in the interior several green globules, of various sizes in different individuals, though nearly always of uniform size in one and the same parent globe. These internal globes, which are the young or embryo Volvox, at first adhere to the wall of the parent cell, although the precise mode of connexion is not very apparent. When thus affixed, they are in a different concentric plane to the smaller green granules. Ata later period, and after they have attained a certain degree of development, these internal globes become detached, and frequently exhibit a rotatory motion, similar to that of the parent globe. In the form of Volvor, termed V. aureus by Ehrenbors, the outer sphere, or cell, exhibits precisely the same structure as the above, the only apparent difference between them con- sisting in the deeper green colour of the internal globules, These, however, soon exhibit a more important distinctive character in the formation of a distinct cell-wall of consider- able thickness around the dark green globular mass. ‘This wall becomes more and more distinct; and, after a time, the contents, from dark green, change into a deep orange-yellow ; and simultaneously with this change of colour the wall of the globule acquires increased thickness, and appears double. The third form, or Volvoz stellatus, differs in no respect from the two former, except in the form of the internal globules, which exhibit a stellate aspect, caused by the pro- jection on their surface of numerous conical eminences, formed of the hyaline substance, of which the outer wall of the globule is constituted. The deep green colour of the contents of these stellate embryos, and their subsequent changes into an orange colour, at once point out their close analogy with those of V. aureus. Ihave no doubt of their being merely modi- fications of the latter; and, in fact, the two ” forms are very frequently to be met with intermixed, and on several occasions I have observed smooth and stellate globules in the interior of one and the same parent globe. | The organism described and figured by Ehrenberg, Uaise the name of Spherosira volvox, also presents the appearance Busk on Volvox globator. Sanger of a transparent globe set with green spots, but it differs from the foregoing in two important respects. 1. In the absence of any internal globules or embryos. 2. In the irregular size of the green granules lining the wall, which, instead of being of a uniform size, are of various dimensions (fig. 13, Pl. V.). The different sized granules are irregularly disposed, although, in relation to the sphere itself, they, or rather the centres of them, are as regularly dis- tributed as in the three just-described forms. What is rather remarkable with respect to this form is the circumstance, that the larger granules are not disposed over the whole periphery of the sphere, rarely occupying more than two-thirds of it, towards one side. In the more minute description of the elements of the above-mentioned organisms, the investigation of which requires the higher powers of the microscope, it will be convenient to commence with the common Volvox globator; and as the tracing of the development of the internal embryonic globules affords the readiest road to a compre- hension of the true structure of the mature globe, I shall pro- ceed in that course. The internal embryonic globules are visible in the young Volvox while still within the parent; but as they are at first concealed by the density of the wall of the young Volvoz, the very earliest stage of formation of the embryo cannot be readily noticed. In the earliest state in which these bodies can be observed, they appear as a globular, or rather discoid, nucleated cell (fig. 3), which, besides its apparent central nucleus, contains a number of minute spherules placed towards the periphery. At this time no distinct wall can be detected, the whole embryo (to use a convenient though incorrect term) apparently consisting of a homogeneous substance, with a lighter nuclear-looking space in the centre, and the above- mentioned spherules towards the periphery. This nucleated cell, as it may be termed, although without a cell-wall, in- creases in size, and the solid or coloured contents appear to retreat from the centre, which becomes clearer and clearer towards the periphery, which gradually becomes more and more opaque. As the cell grows, the nucleus (?) seems to disap~ pear, or to be converted into the clear central space; or, it may be, broken up and confounded in the more opaque con- tents. ‘The number of spherules increases as the cell grows, and it is very soon apparent that the now very thick parietal deposit of cell contents is breaking up into small portions or lobular masses, the centre becoming clear, and apparently filled only with a clear aqueous fluid. When the cell has thus acquired a considerable size, the contents begin to un- d 2 34 Busx on Volvox globator. dergo segmentation, as pointed out in the case of Volvox—l believe first by Professor Williamson. This process com- mences and proceeds precisely as in the ova of animals—the contents dividing first into two, and then each of the halves into two, and so on, till the division becomes too minute to allow of the counting of the segments. It is to be remarked, moreover—and I think this has not been noticed before—that the bright spherical bodies multiply quite as rapidly, if not in a more rapid ratio, up to a certain point, than the segmenta- tion goes on, so that each segment of the still-dividing mass always exhibits two, three, four, or even more of these par- ticles (figs. 1, 2). Ultimately the segmentation ends in the formation of innumerable green bodies, which are closely packed round the periphery of the cell. These bodies, though perfectly defined, are not at first separated by any clear space, and each contains at least one of the bright spherules alluded to (fig. 3). By their mutual pressure, these soft corpuscles of course assume an hexagonal figure, and they are now about 1-4000th of an inch in diameter, or rather more. As soon as, or even before, the segmentation commences, a distinct though delicate membrane, surrounding the embryonic mass, is quite evident, as described by Mr. Williamson; and beyond this is usually to be observed a very delicate zone of apparently gelatinous matter, which is sometimes so delicate as to escape observation, but may, I believe, always be detected by the use of a solution of iodine. When the segmentation is completed, in the way above de- scribed, the embryo Volvoxz exhibits the appearance of a sphe- rical body composed of a transparent membrane lined with distinct, uniform-sized, contiguous hexagonal masses, It con- tinues to grow, and very soon clear lines become apparent between the green masses, which are thus very distinctly defined, retaining the same hexagonal form—each with an apparent nucleus, which is probably derived from the bright spherule contained in it, but as yet without brown spot, clear space (vacuole), or vibratile cilia. As the embryo continues to grow, the spaces between the green masses continue to in- crease ; the green bodies gradually lose the hexagonal form, and assume the appearance of the ciliated zoospore next to be described, ‘They are now about 1-3000th of an inch, or thereabouts, in diameter, and the embryo, detached from its parent, becomes a free Volvox in its interior. We have thus arrived at the complete Volvox, and from the mode of its for- mation it is apparent that it consists of a transparent wall lined with the green bodies, and hollow in the interior; and also that it is surrounded, at all events while within the Bus on Volvox globator. | 30 parent, with a delicate transparent areola, apparently of gela- tinous matter We have now to examine more minutely the structure and nature of the green granules, and the further changes they undergo. Upon examination of the wall of a full-grown V. globator with a sufficient magnifying power, it will be seen, upon view- ing the edges, as it were, of the image in the field, with the object so arranged as to bring the equatorial plane exactly into focus (fig. 5), that the green granules are, in fact, vesicular or semivesicular bodies of a flask-like or conical form, about 1-3000th of an inch in transverse diameter, and placed at uniform distances apart. Each of them is prolonged out- wardly into a sort of peak or proboscis of a transparent and colourless or hyaline material, and from which proceed two very long vibratile cilia, which in close contact at first, pass through the parent cell-wall, upon the outer side of which they separate widely and perform very active movements. The outer cell-wall presents a minute infundibuliform depression at the point of exit of the cilia. It will also be observed, that each ciliated cell or zoospore, as it may analogically be termed, contains a green granular mass or masses, composed, for the most part probably, of chlorophyll granules and a more trans- parent body, which I suppose may be regarded as a nucleus, and derived, as it would appear, from one of the bright sphe- rules which have been noticed before. Atan early period after the maturity or completion of the zoospores they exhibit a minute, circular, clear space, or sometimes, but I think rarely, more than one, which is worthy of very attentive considera- tion. This space is of pretty uniform size in all cases, and about 1-9000th of an inch in diameter. It may be situated in any part of the zoospore, or not unfrequently in the base, or even in the midst of one or other of the bands of protoplasm connecting it with its neighbours. Its most important charac- ter consists in its contractility—a property already known to be possessed by similar spaces or vacuoles in vegetable spores. But what appears to me a very curious, and as yet unnoticed peculiarity of this contraction, consists in the fact that it is very regularly rhythmical. In several cases in which I have watched the phenomenon in question, uninterruptedly, for some time, the contractions or pulsations occurred very regularly at intervals of about 38” to 41”. In one case, however, if I was not misled in the observation, the interval was about twice this, viz., 1’ 25”. The contraction, which appears to amount to complete obliteration of the cavity of the “vacuole,” takes place rapidly or suddenly, as it were, whilst the dilatation is slow and gradual, The interval above noted was measured 36 Busk on Volvox globator. between one sudden contraction and the next, and about half of it perhaps was taken up by the slow dilatation of the space. This contractile vacuole always reappears in precisely the same spot. It would seem to exist, or at all events to present a contractile property only for a limited period, and to disappear soon after the formation of the brown spot, when, as I con- ceive, the zoospore has reached its maturity. The most favourable cases in which this contractile space is to be sought for, are those in which the Volvox is in the most vigorous state, and especially in that variety in which, owing perhaps to the copious supply of nutritive matter, the amount of protoplasm is very abundant, and the zoospores consequently very numer- ous and connected to each other, not by slender filaments but by wide processes, as in figs. 26, 27, which latter shows a contractile space situated in the base of one of the connecting bands of protoplasm, With the exception of the small space occupied by this contractile spot, the zoospore at first appears to be quite solid, and no distinct wall can be perceived around the green matter, but it rapidly changes. Owing either to the _expansion of the vacuole, above described, after it has lost its contractile property, or to the formation of others ofa different nature, and also perhaps in some degree to the absorption or consumption of some of the colouring contents, the zoospore gradually becomes more and more transparent (fig. 7); till at last, the greater part of it is clear and colourless, and what remains of the green matter contracts into a small irregular mass, adherent to the bottom or sides of what is now a cell— primordial cell of Cohn. (Figs. 5, 6.) Each cell, when fully formed, usually presents a brown spot, which is adherent to one ade of the cell towards the narrow end (figs. 5, 6); and what is remarkable, it will be noticed in a perfect specimen, that the brown spots are placed in a corresponding situation in all the cells, that is to say, all the cells appear to look the same way. This is the so-termed eye-spot of Ehrenberg. When examined with a high power (800—900 diam.) it presents the form of a cup or disc, con- cave on the side which looks outward, and convex on the other. ‘Though placed quite on the side of the cell, and pro- jecting a little upon it, the brown spot is nevertheless always covered by a thin membranous expansion of protoplasm, or, in other words, it is always lodged within the substance of the zoospore. ‘Though most usually present, the brown spot does not appear, in all cases, to be at any period a necessary con- stituent of the zoospore. It is one of the most persistent however, remaining visible as long as any portion of the zoo- spore is discernible. Besides the above-described elements, the Busx on Volvox globator. 3 37 zoospore, when viewed from above, exhibits two highly refrac- tive spots placed side by side, white seerh to represent the insertions or origins of the two vibratile cilia. The periphery of the cell presents a clear line, and appears to be formed of a delicate membrane—although, in the earlier stages of the existence of the zoospore, that is, before the for- mation of the eye-spot, or disappearance of the contractile vacuole, the whole evidently consists of a homogeneous sub- stance, in which the above described parts are imbedded, From the periphery of the zoospore proceed six thread-like processes, connecting it with as many of its neighbours. These threads appear to be simply continuations of the quasi? cell- wall, and to be of the same nature chemically as it, as are also the vibratile cilia. The connecting threads are sometimes double, or even triple, between some one or more of the sur- rounding cells, and they are invariably continuous between the two cells. This description applies more particularly to the zoospores in situ. When the Volvox is ruptured, many appear to be- come immediately detached, and to be washed out, as it were, with the aqueous contents of the parent cell. Under these circumstances they lose some of their previous regularity of form, but not much; they become more globular and the beak less prominent, but in other respects they appear much the same as before. The two vibratile cilia remain in @on- nexion with them, and continue their active movements. This is opposed to Mr. Williamson’s statement, that ‘‘ when thus liberated they exhibit no traces of the two cilia, or probos- cides” of Ehrenberg, and agrees with that of the latter. Among the thus liberated ciliated zoospores will usually be found numerous detached cilia, which, as is observed by Mr. Williamson, are generally more or less coiled at one end into a ring. And besides these I have not unfrequently noticed some extremely delicate annular bodies, about 1-9000th of an inch in diameter, perfectly clear and colourless, which seem as if they had escaped from the interior of the ruptured zoospore: but of this and their true nature I am unable to speak posi- tively. Having thus described what I conceive to be the anatomy of the common form of Volvox globator, 1 will thus sum up the result of what my observations have led me to conclude as to its structure. 1. That it originates in an apparently nucleated, discoid cell, which is generated in the interior of the parent, and liberated in a perfect, though not fully matured form; within which are contained similar germs. 9 os Busx on Volvox globator. 2. That the contents of this apparently nucleated discoid cell, consisting of a grumous material and refractive amyla- ceous (?) spherules, after a time undergo segmentation, at the same time exhibiting a distinct wall, beyond which is a delicate areola, apparently of a gelatimous consistence. 3. That this segmentation, attended with a corresponding augmentation in the number of the refractive spherules, ter- minates ultimately in the formation of numerous contiguous particles or segments, 4. That these ultimate segments are gradually separated from each other, remaining connected only by elongated pro- cesses or filaments, and constituting the ciliated zoospores of the mature Volvoz. ). That these zoospores at first are simple masses of pro- toplasm, containing a transparent nuclear body, and _ that afterwards they present for a time clear, circular spaces, which contract rhythmically at regular intervals ; and are subsequently furnished with a brown eye-spot; and at a very early period with two long retractile cilia, which, arising from an elongated hyaline beak, penetrate the parent ‘cell-wall, and exert active movements external to it. 6. That in a concentric plane internal to these ciliated zoo- spores are placed the germs of future individuals destined to follow the same course. aving thus traced one form of Volvox through its course BE development, I will proceed much more briefly to the others. In V. aureus, as I have said, the constitution of the wall of the parent cell is exactly as above described. At its earliest appearance also the internal embryonic body cannot be dis- tinguished from that of the ordinary form, except in its deeper green colour. It afterwards, however, acquires a thick wall, changes its colour to yellow without material alteration in size, and acquires a second equally firm and distinct envelope, or rather, as I believe, the original contents contract somewhat, and then form a second coat around themselves. Eventually a considerable space exists between these two coats (figs. 10, 12), which space is occupied by a clear and apparently aqueous fluid, but upon the addition of a solution of iodine a granular Glomdinces 4s produced in this fluid. The contents of the inner cell consist chiefly of amylaceous grains mixed with a greenish material in the one case, and with a bright yellow apparently oily fluid in the other. The amylaceous particles are of an irregular botryoidal form, and far from uniform in size. As regards the future destination of this form of germ, I am as yet in total ignorance ; there can, however, I think, be little doubt but that it represents the ‘‘still” form of spore of Busx on Volvor globator. | 39 other Alga—that it may, in fact, be termed the “ winter spore” of Volvox, destined, owing to its more persistent vi- tality, to continue the species, when its course of development in the usual way is interrupted by surrounding circumstances. Of that form of Volvor termed V. stellatus, 1 would only here observe that it seems to me merely a modification of the one last described, and that it appears to follow the same course of change and doubtless of future development. With respect to Spherosira volvox, my observations have been very limited, and I by no means desire to express myself with certainty as to its relationship to the forms above de- scribed, I merely surmise that it may be found to represent a peculiar mode of development of one and the same species. In external aspect, except in the want of uniformity in the size of the ciliated zoospores, it appears to agree in all respects with V. globator. It however contains no internal embryonic bodies, and it is therefore only to the ciliated cells that any reference need here be made. The smaller ones appear to me to resemble in all respects those of Volvox globator, and each to possess two cilia, which is important if true, because the only distinction between Volvox and Spherosira in Ehren- berg’s classification depends upon the circumstance, that in Spherosira there is only a single cilium to each zoospore, whilst there are two in Volvoz. | My supposition that Spherosira volvox and V. globator are allied, is founded, it must be owned, not upon any direct ob- servation, but chiefly upon the fact, that in the water in which the specimens of Volvox I had under examination were con- tained, there was at first none of the Spherosira any more than of V. aureus observable, and that after some days both were very numerous. The difference I am about to describe in the after develop- ment of the ciliated zoospores, is not by any means a sufficient ground upon which they should be deemed distinct species, because much greater differences are known to exist in other of the lower Algz during their various forms of development without its being thence allowable to suppose that they are of different species. In Volvox spherosira then, as at all events it may be termed, the larger green granules are in fact the ciliated zoospores in a stage of further progressive development. In the same spe- cimen they will be seen in all stages of division or segmenta- tion (fig. 13)—first into two, then into four, and so on till, as in the case of the embryo Volvoz, the ultimate result of the segmentation constitutes numerous minute ciliated cells or bodies (fig. 14)—not, however, as in that case, lining the 40 Busx on Volvox globator. inner surface of the wall of a spherical case, but forming by their aggregation, a discoid body, in which the separate fusi- form cells are connected together at one end, and at the other are free, and furnished each with a single cilium, In this stage these compound masses become free and swim about in the water, constituting, in fact, a species of the genus Uvella, or of Synerypta of Ehrenberg. With respect to the chemical constitution of the above described parts, the following are the results at which I have arrived :—1. By the use of iodine and sulphuric acid, tried repeatedly and in various ways, I have never succeeded satis- factorily in eliciting any tinge of blue in the wall of the mature Volvox. I therefore conclude that it contains no cellulose. It is invariably coloured, by the above re-agents, of a deep brown colour, and when thus coloured, this outer wall presents no trace whatever of structure; it appears uniformly transparent and homogeneous. The ciliated zoospores, also, with the connecting filaments and cilia, are turned brown, but of a very deep brown, by the same re-agents, excepting usually one or more particles in the interior of each, which are apparently turned blue, I am not satisfied as to the chemical re-action of the brown spot; it appears to assume a blue colour, but from the intensity of its colour and consequent opacity I am not sure that this is the case. The embryo cell, when young, is turned a deep brown, but when older and fully formed, but before it has arrived at maturity, it will be found that it is only the green masses, or future ciliated zoospores, that are thus changed, the cell-wall acquiring scarcely any tinge of brown. But when a young cell thus tested with iodine and sulphuric acid is ruptured, I have occasionally noticed that the fluid contents contain an abundance of minute bluish flocculi—I use the word flocculi because the particles are light and flocculent, and not at all like any of the more ordinary and more solid forms of amylaceous matter. The quantity of this flocculent matter appears to be greater towards the periphery of the cell, and, in fact, it would seem that the green bodies are at this time imbedded as it were in an amylaceous matrix, which they not improbably assimilate, because in the mature cell nothing of the sort is apparent. In the embryonic bodies, however, or winter spores of V. aureus and stellatus, the presence of cellulose is rendered abundantly evident in the two coats forming the tunic of the spore by the blue colour produced in them by iodine and sul- phuric acid (fig. 11); nearly as distinctly, in fact, as it is in the tunic of Micrasterias and other Desmidiee. 'The appa- rently clear fluid between the two tunics is rendered brownish aa Busx on Volvox globator. 4] and turbid at the same time (figs. 11, 12), and the solid con- tents of the interior are shown to consist, for the most part, of amylaceous grains of the peculiar botryoidal form above noticed. (Fig. 9.) The yellow oil-like fluid in the ripe spore acquires a green tint under the action of the same re-agents. (Fig. 9.) ; ot AppENDIx.—( October, 1852.) The above are the observations read at the Microscopical Society. I am now satisfied that they afford an account of but one of the multiform varieties under which Volvoz occurs at different times and places. I must own also, that at the time my observations there detailed were made, I was unable to reconcile much of what I saw with some of the statements and figures in my friend Professor Williamson’s ingenious paper on the same subject. Subsequent investigation, how- ever, and some correspondence with him, have satisfied me that I was hasty in drawing conclusions from one form only of a very protean object. I freely confess, that in much, in respect to which I had conceived Professor Williamson had fallen into some error of observation, he has been quite right, though at the same time I must say that his explanations of the appear- ances described and figured by him, do not exactly accord with my notions respecting them. I still maintain that the structure of the wall of Volvor—upon which alone I think we are dis- agreed—is essentially such as I have described it, viz., that it is formed by acontinuous, external tunic, lined by the ciliated zoospores. Professor Williamson, on the other hand, as I understand him, conceives the globe to be ‘a hollow vesicle, the walls of which consist of numerous angular cells filled with green endochrome, &c., the intercellular spaces being more or less transparent.” The ciliated zoospore, therefore, according to him, is not a mass of vegetable protoplasm, without dis- tinct wall, and precisely analogous to a Huglena, or other naked zoospores, but represents the endochrome of a cell hav- ing two walls, an external and an internal, which latter is “a ductile cell-membrane, lining the interior of each cell and sur- rounding the cell-contents,” and which ‘‘ inner membrane be- comes separated from the outer cell-wall excepting at a few points, where it is retained in contact.” And he thus explains the mode of formation of the connecting filaments. In this case, therefore, these filaments would never pass directly from ‘one green mass to another, but. would of course be interrupted in their course by the walls of two contiguous cells. That this, 42 Busk on Volvox globator. however, is not the case in the form of Volvoz, which formed the subject of my paper, is sufficiently obvious. But it is nevertheless true, as I find from examination of Professor Wail- liamson’s specimens, that his representation is, in certain cases, equally correct, as I shall afterwards explain. Another cir- cumstance also noticed by Mr. Williamson, and which, till he pointed it out particularly to me, had, though not altogether unnoticed, been disregarded, is the existence of delicate lines between the green granules, and dividing the wall of the Vo/- vox into very regular hexagonal spaces, in the centre of each of which is placed one of the green granules. ‘The former of these conditions— which, though I have never met with it myself distinctly in specimens from any other locality, seems to be sufficiently abundant in the neighbourhood of Manchester—is represented in figs. 15, 16, 17, 18, 19, 20. In these it will be seen that the central green body is surrounded, at variable dis- tances, by a tolerably thick, distinct membrane or wall, and that numerous irregular filaments, where they exist at all, extend from the central mass to this wall, and there terminate, and do not pass from one green mass to another, as in the usual form. Now, I explain the way in which the zoospore is thus modified, in this way: I regard the external membrane merely as the boundary-wall of the original zoospore, and, like the entire body, as composed of vegetable protoplasm; and I believe that this peculiar appearance is produced by a great and unusual expansion of the interior of the zoospore (by endosmosis of fluid probably), by which the outer or periphe- ral layer is separated from the remainder and principal part of the mass, containing the chlorophyll and nucleus, or supposed nucleus, &c. Zoospores, in fact, in this condition might be said to be dropsical. ‘That this separation of the wall from the contents arises in this way, and not, as Mr. Williamson says, from the shrinking of contents, is, I think, sufficiently obvious from several considerations, and is rendered very clear, if we trace the progressive stages of the hydropical enlarge- ment in one and the same Volvoz, as I have done in the figures above cited. In this series it 1s easy to observe the earliest formation of the clear space up to the most extreme dilatation of which the cell is capable, owing to its contiguity with others. Of course when a number of cells are thus enlarged and mutually compressed, they assume an hexagonal form; but this hexa- gonal arrangement must not, as it appears to me, be con- founded with another, to which I have before alluded, and which I conceive to be due to a different circumstance alto- gether. In fig. 15 of this series, some cells will be obseved Busk on Volvox globator. 43 © little if at all altered, from what I assume to be the normal form, and it will be seen that these little altered cells are mutually connected by the usual continuous filaments. In fig. 16 the zoospores are more expanded, and being in con- tact in many points, the connecting threads are absent; fig. 17 shows a further degree of expansion, but more irregu- © lar, and with irregular connecting filaments. In fig. 18 the enlargement is nearly as great as it can be, and numerous threads or processes of protoplasma extend from the central mass to the wall, just as they do in almost any vegetable cell from the nucleus to the primordial utricle, which utricle, in fact, 1s represented by the cell-wall in the case we are dis- cussing. In fig. 19, the dilatation is complete, and, owing to the greater age of the specimen from which this figure was taken, the protoplasma is much wasted, and all the filamentary processes completely gone. A faint granular appearance occupies the cavity of the primordial cell. It is a curious fact, as showing perhaps that all the vital action in the cell resides in or around the nuclear mass, that not unfrequently the central mass after considerable expansion of the cell, and the formation in that way of one wall, will begin to throw off asecond. ‘This condition is represented in a more highly magnified drawing in fig. 20, Although I have not myself seen any natural specimens in which this condition of the zoospores was present, except those for which I have been indebted to Mr. Williamson, still I have repeatedly observed a partial appearance of the same kind to take place, when a specimen of Volvoz of the normal sort is kept for some hours under observation in the micro- scope. Figs. 21, 22, 23 show the series of changes that took place in a certain number of zoospores watched at intervals, and left undisturbed for about twenty-four hours. (Fig. 21,10 am., Oct. 4. Fig. 22, 1 p.w., Oct. 4. Fig. sia 8 A.M., Oct. 5. ) Now with respect to the other form a hexagonal areo- lation, for my knowledge of which, as I have stated, I am chiefly indebted to Professor Pluamecd and hee 1s represented in figs. 24, 25, I have already observed, that I regard it as quite distinct from that produced by the mutual pressure of contiguous dilated zoospores. Professor William- son appears, from what he has told me by letter, to consider that this appearance is invariably present, or at all events that it can be elicited in all cases by appropriate means. I must confess however, that I have not been successful in seeing it, or in producing it in very many instances, and that I believe it is occasionally impossible by any means to demonstrate its 44 Busx on Volvox globator. existence. At some periods not a single specimen from a given locality will exhibit it, whilst at another, every indi- vidual will show it at the first glance. Thus in the month of _August last, when, in a certain pond on Blackheath there was the most incredible abundance of Volvoz, so great in fact as to render the water at the lee side of the pond in certain spots of a deep green colour, and to cause it to afford, when collected, a very strong herbaceous or confervoid smell, the majority of the plants exhibited the stellate form of spores, or rapidly acquired spores of that character, and very many were in, or soon assumed, the form of V. aureus. ‘They seemed in fact to be entering upon their hybernating state. Many among them, however, though all small and starved-looking, were of the common kind ; in all these Mr. Williamson’s hexagonal areola- tion was very distinct. In the month of October, however, upon returning to the same pond, I was able to find very few Volvoces at all, and all of the usual kind ; in none of these could I detect the least appearance of the same arrangement. I there- fore conclude that the greater or less distinctness, or complete absence of this character, is to be referred to external condi- tions with which we are not fully acquainted. The appear- ance itself I explain in this way. It appears to me that each zoospore is imbedded in a distinct gelatinous or semi-fluid envelope of considerable thickness, and that the hexagonal areas are formed by the sides of these distinct masses of gelati- nous matter coming into contact. I am inclined to think that there is no distinct membrane containing this gelatinous matter : if there be, it must be infinitely thin, because the line of con- tact is extremely delicate and single. I conceive, in fact, that each ciliated zoospore is surrounded with a gelatinous or semi-fluid areola, of the same nature precisely as that which surrounds the embryo Volvox while within the parent, and in which also it is not I thmk possible to detect a distinct limitary membrane. This envelope of the ciliated zoospores contains a nitrogenous element, which sometimes, on the addi- tion of iodine, gives rise to the appearance of minute heads around the outer periphery of each gelatinous mass, or in the lines of the hexagonal areas as seen in fig. 25. It is to be observed also, that connecting filaments of protoplasma may occasionally be seen to pass from one zoospore to another across the line of junction of the two gelatinous envelopes (fig. 24). These zoospores therefore of Volvox would appear to represent the ‘‘encysted zoospore”’ of Cohn (Protococcus pluvialis, &c.), and his fig. 43, plate 67, may perhaps be taken as a fair representation of what I conceive to be the condition in these connected zoospores in Volvox. This ex- Wixiramson on Volvox globator. 45 planation of the hexagonal areolation, however, does not clash at all with that which I have given as to the structure of the -wall of Volvox. For in this case, as in all others, the collected mass of zoospores, and their envelopes, is enclosed by a con- tinuous external membrane, not in any way derived from them but from the parent cell in cwisch they were originally formed. There are several other interesting points relating to Volvox which have come under my observation ina prolonged atten- tion to the subject, including another form of development of the internal spore, in which it divides, not in the usual way, into what may perhaps not inappropriately be considered as macrogonidia, to use Braun’s expression, but into a much smaller and differently arranged sort, which may be considered as his microgonidia; but to enter fully upon this and other points would demand more space than is here at command. [Whilst this paper is passing through the press, I have found that a faint, but quite distinct, purplish blue tinge may be produced in the wall of Volvox globator by means of Schultz’s solution, The specimens of Volvox in which I have noticed this have been preserved in glycerine for two months.—G. B.] Further Elucidations of the Structure of Votvox GLoBATor. By Professor W.C. Wittiamson. (Read June 21, 1852.) In May, 1851, I had the honour of laying before the Philo- sophical Society of Manchester a memoir on the Volvox globa- tor,* containing the results of a series of observations, which brought to light in that elegant object, a cellular structure, hitherto unobserved. Since the existence of these cells affects the character and affinities of the organism, it is desirable that the fact should be established beyond the possibility of dispute. My friend Mr. Busk, in a recent communication made to the Microscopical Society of London, either doubts their existence, or rejects my idea of their cellular nature. This denial, coming from such a quarter, renders it incumbent upon me to make the matter more plain than was done in my previous memoir: I am enabled to do this, partly by new ob- servations on the living Volvoz, and partly by some changes which the specimens prepared last year have undergone, making their structure more obvious than it previously was. * Published in the Ninth Volume of its Transactions. 46 Wit.iamson on Volvox globator. No one who has seen these specimens can for a moment doubt that there exists immediately beneath the superficial pellicle, or common investing membrane of each Volvox, a layer of closely-packed translucent vesicles, within each of which is located one of the numerous green spots ornamenting its periphery. In the memoir referred to, I endeavoured to show that these vesicles are true cells, whilst the green spots are the inner cell-membranes and their contents, representing the internal utricles of Harting and Mulder, the primordial utricles of Mirbel. The appearance of these cells in their different stages of growth was described, and the mode of their development and multiplication examined. Mr. Busk, who has recently directed his attention to this subject, has arrived at a different conclusion from my own, respecting the structures in question. Not having, then, seen the hyaline vesicles, which I regard as true cells, in any of his own specimens, he concluded that the Volvox consists of a number of protoplasms, which have resulted from the suc- cessive segmentations or subdivisions of one primary pro- toplasm, in the way described in my memoir. On being afforded an opportunity of examining some of my preparations of Volvox made last year, and in which the vesicles are re- markably distinct, though the appearance they presented was wholly new to him, he was still disposed to maintain his pre- vious opinion. Instead of admitting them to be true cells, he concluded that they were merely the outer layers of the protoplasmic segments, which, after separating from the pro- toplasmic mass, had become dropsically distended, and as- sumed the appearance of a true cell. Since I believe this general conclusion to be incorrect, I am anxious to render more clear than I have hitherto done, what appears to be the true interpretation of the structures in ques- tion. In accomplishing this, it will not be necessary to reca- pitulate all the details of my preceding memoir, since the accuracy of the greater number of them, as well as my con- clusion respecting the vegetable nature of Volvox, are con- firmed both by Mr. Busk and by other observers: some points, however, require to be examined in detail, There is one point respecting which I was clearly in error ; my present correction of the mistake is due to the suggestions which I have received from Mr. Busk. I found that each young germ was developed from one of the peripheral stratum of cells, by the ordinary process of cell-division or segmenta- tion. Having ascertained that each protoplasm in its matured state was invested by a true external cell, in addition to a very thin inner one which held the granular mass together, I con- Wituiamson on Volvox globator. 47 cluded that, in the earlier stages of the process of segmentation and development of the germ, each protoplasmic segment would be invested by a similar external cell-membrane, as is the case with Hematococcus, Palmella, &c. I could not ascer- tain what became of these outer cells, as successive subdi- visions of their contained protoplasms multiplied their number, but hazarded the surmise, that the earlier cells might either have been re-absorbed, or that they still existed in the form of thin membranes, consolidated with and investing the newer cells which I supposed had been developed within their in- terior. It is now obvious that none of the protoplasmic seg- menis have secreted their external cell-membrane, until the entire number destined to compose the matured organism has been completed. This interpretation accounts for many ano- malous circumstances. It explains the very close contact in which we find the green protoplasms of the immature germ. No transparent spaces intervene ; these only appear when the young germ is matured and furnished with cilia. It also explains my want of success in searching for the layers of cellulose, the residue of the supposed earlier-formed cells, which must have existed had the organism been developed in exactly the same way as a Palmella or an Hematococcus. In these latter objects, each segmentation of the protoplasm ts followed by the secretion of a true cell, which invests each segment. The point now to be demonstrated is the existence of two mem- branes surrounding each mass of protoplasm. First an inner one, very thin, and in the living state, closely embracing the gra- nular protoplasm, and corresponding with the inner cell-mem- brane of the ordinary Conferve ; second, an outer cell-mem- brane secreted from the exterior of the first. To facilitate describing, we may term the former of these the protoplasmic membrane, and the latter the cell-membrane. The protoplasmic membrane is easily shown to exist. Fig. 6, Pl. VI. represents a very young gemma, or budding germ, which consisted of but few segments, as it appeared when sub- jected to pressure under water. Some of the protoplasmic seg- ments glided through an aperture made in the common vesicle, without becoming ruptured. They accommodated themselves to the size and form of the aperture, and, on escaping, regained their spherical form. On increasing the pressure, each seg- ment burst, all the granular and mucilaginous contents flowing out and mingling with the water (60'). Asthey did so the protoplasmic membranes (6c) were distinctly seen as thin hyaline spheres. In the subsequent development of Volvox this membrane always continues in existence. Its appearance VOL, I. e 438 ~Wiuramson on Volvox globator. in the matured organism will be described immediately. When the gemma has attained its full size, by the process of segmenta- tion described in my former memoir, further changes occur. Translucent spaces separate the green protoplasms, now be- come hexagonal by mutual pressure. These translucent out- lines mark the development of the external cells investing the protoplasmic membranes. At first the two are in close oppo- sition; they subsequently separate, as the cell increases in s1ze, excepting at certain points where they remain in contact. Before tracing out the further stages of this process I must observe that the Volvox exhibits two apparently distinct states, which are, nevertheless, mere varieties of one species. In the one, each ‘protoplasm assumes the appearance of fig. 1 5, being angular, and giving off thick, irregular and often dichotomons fovende (he) athe cximenniaes of which are attached to the cell-wall (1a). In this case, the radiating threads consist not only of the protoplasmic membrane, but also of its granular, mucilaginous contents. The other condition referred to is represented in fig. 10. Each protoplasm (10d) is perfectly spherical, and connected with its neighbours by delicate capil- lary threads, these being so fine as to be sometimes almost invisible. In this state the cells to be described are often invisible ; nevertheless, they exist. The changes undergone by the stellate variety were described in my previous memoir. The cell expands, and as the pro- toplasm is only attached to it at certain points, the latter is drawn out until it finally assumes the stellate contour deli- neated in fig. 1. Each of the radiating threads is attached to the cell-membrane by its peripheral extremity, at a point exactly opposite the corresponding threads of contiguous pro- toplasms. On rupturing a Volvox under water these threads become detached from the cell-wall, and passing through the stages represented in figs. 2 and 3, assumed that of fig. 4, which is precisely that of fig. 10, minus the connecting threads, a state which occasionally occurs in the living Volvox. In numerous examples of both these varieties of Volvox | found each protoplasm surrounded by an angular, usually hexagonal, areola, as represented in fig. 5 of my original me- moir. They appeared as dark outlines when the object was illuminated by transmitted light. On exposing these speci- mens for a while to the action of some re-agents, as glycerine, I soon found that each dark line was really double, and marked the boundaries of two cells. This was shown by the gradual separation of these cells at the angles of the areola, as repre- sented. in fig. 11, which is a faithful transcript of part of one of these specimens when mounted in glycerine. In this ex- WixiiamMson on Volvox globator. 49 ample no cells were at first visible ; but as I watched them, they came gradually into view in some parts of the organism, but not in others. Fig. 11 represents a portion of it, in the upper part of which the cells are visible, whilst in its lower part they cannot be traced; here the tissues were transparent and apparently quite structureless, as was the entire sphere in the first instance. The transition from the one condition to the other was gradual; the dark lines becoming less conspicuous and finally disappearing as we approached the opposite side of the Volvox to that on which they were most distinct. ‘This specimen illustrates thousands that have been examined, and proves that the apparent absence of the cells from so many of the objects is no proof that they do not exist, but merely shows that certain favourable conditions are required to bring them into view. We are justified in concluding that they exist alike in all the specimens of Volvox, and are not merely accidental developments in a few individuals. In my mounted preparations we obtain further evidence respecting the nature of these two membranes—the proto- plasmic and the cellular. We see that the wall of the sphere has an appreciable thickness, the inner margin being as definite as the outer one, and nearly parallel with it. Fig. 5 represents this as seen ina section of a Volvox. A moment’s Inspection of my preparations would convince the most sceptical that such is the case; several of these peripheral cells, as seen in the section, are more highly magnified in figs. 14 and 15. The thin investing pellicle (15 d) com- presses the outer wall of each cell into conformity with the peripheral curve of the sphere; laterally the septa (15 a) are straight and parallel to one another. Internally, each cell is a little turgid (15 a), the centripetal pressure at this point being obviously at the minimum, and allowing the primary tendency of the cell to assume a spherical form to manifest itself. The green protoplasm adheres firmly to the peripheral wall of each cell, through which the cilia are protruded. Between the true cell-wall and the protoplasm, we have the protoplasmic membrane (14 and 15 cc’) in variable conditions. Some- times it forms an oval cell (14 e’), sometimes it is oval at one end and flattened out at the other (14c, 15c’); at others it is not only flattened out at each extremity and in close opposi- tion with the cell-wall, but even at the two sides (as in the centre cell of fig. 15) the two membranes are closely ap- proximated. If we turn to a superficial view of the same specimens, we _ shall obtain similar results. It must be borne in mind that in the living Volyox, even where the cells are visible, we only e2 50 Wixtiamson on Volvox globator. see the true cells ; the protoplasmic membrane being in such close apposition to its granular and mucilaginous contents as to prevent its being identified as a separate tissue. But when the specimens have been mounted some time, we often find that a change takes place. The protoplasmic matter shrinks up into a small irregular mass (7 6), and thus becomes detached from the protoplasmic membrane (7 c¢, c') which forms a ring round it. When we succeed in compressing the object so as to force the cells into an oblique position (as is done in those to the left of fig. 7), we see that these circles are really iden- tical with figs. 14 and 15 c, c’ in the sections. The external cells (7 a) remain in mutual contact, excepting at their angles. There is a little discrepancy between this description and that of fig. 11 in my former memoir, and the explanation of its cause will do much to diminish the real difference between myself and Mr. Busk, whilst it tends to confirm my ideas respecting the cellular structure of Volvox. In many of my mounted specimens, the outer or cel/-membranes have either failed to become visible, or have disappeared again. On the other hand, in these examples, the protoplasmic membranes have separated from their protoplasms and become very con- spicuous. I formerly confounded the two, and imagined that in. the latter examples the incipient separation of the cells at the angles (seen in figs. 11 and 16) had been subsequently carried much further, causing a complete isolation of the cells, as is: apparently the case in fig. 17. My error was corrected by the specimen delineated in fig. 7, in one part of which both these tissues are seen as there represented, thus enabling me to iden- tify the inner protoplasmic membranes (7 c) of the one with the - only membranes seen (17 c) in the other. Numerous similar specimens have since confirmed the correctness of this explana- tion, which clears up many obscure points. I now find no difficulty in recognising the two structures; the protoplasmic membrane, whether seen in front or in profile, is always more granular, from the adhesion to its inner surface of some of the granular elements of the protoplasm, than is the case with the cell-membrane, the outlines of which are invariably clear and fine. Fig. 8 represents three cells from the same specimen as fig. 7, in which the protoplasmic membranes nearly fill the respective cells; such specimens, seen in section, exhibit the appearance of the centre cell of fig. 15. I conclude that if we could bring all these structures into view in a section of aliving Volvox, they would present the appearance of fig. 12, where a represents the cell-membranes, b the protoplasm and its contiguous membranes, d the common pellicle, and e the prolonged threads of the proto- Witiamson on Volvox globator. 5f plasm connecting it with the peripheral walls of its cell. Such a section however cannot be obtained until chemical re-agents have rendered the tissues rigid, which process alters their arrangement and aspects. The entire thickness of the cellular peripheral wall of the Volvox is about 1-1400th of an inch, in specimens that have been a few days mounted in glycerine. The superficial dia- meter of the cells in the living Volvox varies from 1-800th to 1-]000th of an inch. The next question relates to the nature of the threads that connect together the protoplasms of the two varieties of Volvox. These cannot be exactly the same in figs. 1 and 10. In fig. 1, the entire protoplasmic mass is drawn out into a stellate form. Each thread consists of the protoplasmic membrane, and a portion of its contents. In fig. 10, on the other hand, the threads contain little or none of the protoplasmic granules, but appear to consist solely of a portion of the membrane. Of course to produce such a result this membrane must be highly ductile, and consequently but partially organized. That the threads are ductile and capable of being drawn out is easily seen on compressing a Volvox between two glasses. The fluid distending the sphere is very viscid and probably consists of mucilage. ‘This must have been secreted by the protoplasms. When we remember that cellulose is but a modified form of gum, we ean’ readily conceive that the conversion of the one into the other may sometimes be imperfectly accomplished amongst these lower forms of vegetation. Such I believe to be the explanation of the ductility of the protoplasmic membrane, and of the threads into which it is drawn out. Fig. 16 throws a little additional light on this subject. We see from it that whilst the thread sometimes consists of the drawn-out membrane (16 a), at others the membrane has re- ceded from the outer cell-wall, leaving only a very faint line, thickened at its peripheral extremity, marking the former point of junction with the outer cell-wall. The same thing is seen in fig. 7. In both these examples the threads were ori- ginally of the stellate type seen in fig. 1. Whilst the points of contact with the outer cell-wall are still indicated, they have lost their irregular dichotomous character, and are reduced to straight, radiating, capillary threads, such as are seen in fig. 1. ‘The greater portion of the viscid membrane has receded towards the protoplasm, whilst a small part has in like manner accumulated at the point of attachment to the cell-wall, form- ing the peripheral dots seen in the above figures; similar appearances present themselves in the other variety, fig. 10. Near the centre of fig. 11, the threads uniting’ several of the 52 Wi iiamson on Volvox globator. protoplasms have become broken; those which remain have drawn their respective protoplasms towards the sides of the cells to which they are attached. All these circumstances in- dicate a degree of ductility in the protoplasmic membrane such as would scarcely exist supposing it to consist of per- fectly organized cellulose. In the young gemma, as already observed, the protoplasms are in close contact on all their sides ; but a is only at a few points that an actual junction is established corresponding with the extremities of the future threads. What has been the eclectic power leading to this result? It is not mere acci- dent. Reference to fig. 11 will show, that in passing from one _ protoplasm to another these threads always traverse the sides of the hexagonal cells, and never their angles. It is also ob- vious that these points of adhesion are chosen prior to the de- velopment of the outer cell-membrane. This is indicated by the unvarying continuity of the threads when they are single ; but still more so when they are double and treble, as is frequently the case (figs. 10 and lle, e'). Whatever the number pro- ceeding from a protoplasm to any one side of its cell, the same number proceeds to the proximate side of the adjoining cell: I have scarcely seen one exception to this rule. I think the explanation just given meets the case ; if so, it may be a ques- tion whether the cell-membrane is developed between the con- tiguous extremities of the two protoplasmic threads, or whether it is deficient there, admitting of an actual as well as an appa- rent continuity. I have already given one or two reasons for believing the former hypothesis; but even should the -latter prove the true one, we shall only have recurring in Volvox a phenomenon that is common enough amongst the perforated cells and ducts of the higher plants. In but one instance have I seen a specimen countenancing the latter idea. In it the peripheral layer of cells was very thin and compressed ; many of the cells appeared to be wholly detached from each other, as represented in fig. 9; nevertheless the threads proceeded from protoplasm to protoplasm, apparently traversing the intercel- lular spaces. This specimen is so entirely exceptional as to leave little doubt on my mind that is capable of being explained. I have no doubt that, owing to the thinness of the peripheral cells,a section of it would resemble fig. 13. If we suppose that the circumstances which render the majority of Volvox cells hyaline and invisible, still continue to affect the portions of those in question that are external to the dotted line 13 f, the remainder being visible, we should have precisely such an appearance as is presented in fig. 9; the only visible por- Witutamson on Volvox globator. 53 tions of the cells being those which were below the points of mutual contact. The direction taken by these threads frequently demonstrates the presence of invisible cell-walls midway between two pro- toplasms. We have already seen that when the threads are liberated their tendency is to become shortened ; hence they pursue the most direct course from one point to another. But we occasionally see examples of what is delineated in fig. 10 e’, where two threads run parallel for some distance and then suddenly diverge, proceeding to different protoplasms. This condition obviously indicates the existence of some invisible point dapput, where the divarication occurs. This, doubt- less, consists of the hyaline cell-wall. We obtain similar evi- dence from almost every example of Volvox, when we examine the protoplasms at one margin of the sphere in profile. This can readily be done with object-glasses of short focus, owing to the transparency of the tissues. We very frequently see that the threads, instead of being straight, dip inwards towards the centre of the sphere, and meet at a well-defined angle mid- way between the two protoplasms, as represented in fig. 12 e. This can only be explained in the way just suggested. Whatever may be the true nature of the objects which I re- gard as cells, they are obviously separated from the protoplasms before the latter assume their stellate forms, or develop their delicate connecting threads. I have had specimens of every age, from the gemma artificially liberated from the parent sphere, to the hyaline and matured individual, in all of which these cells exist. They are obviously developed immediately after the final process of segmentation has completed the re- quired number of protoplasms ; the development of these cells of the cilia and of the common pellicle apparently taking place about the same time. Names sometimes matter little; but here they are significant, since they involve the origin of the disputed structure. Mr. Busk regards it as the outer covering of the protoplasm dropsically distended; I believe that the outer covering (my protoplasmic membrane) remains in close connexion with the viscous protoplasm until the two are sepa- rated artificially, and that the cell is a secretion from the outer surface of the protoplasmic membrane. According to this ex- planation, the two bear the same mutual relations as exist between the outer and inner membranes of any other Confervoid cell. The beautiful stellate, spiral, and other forms which the inner membranes of many of these plants assume after their separation from the cell-wall, with which they were primarily in close contact, afford ready illustrations of the similar trans- formations in Volvox. 54 Wittramson on Volvox globator. The origin of the superficial pellicle (fig. 14d and 15 d)- remains to be considered. In my last memoir, I stated that each young gemma was developed within a large transparent vesicle (fig. 5 f and 6 f), which appeared to be the expanded cell-wall of the primary cell (a). My more recent investigations confirm this conclusion. When we detach a young gemma and its vesicle from the parent Volvox, the vesicle usually carries away with it a few of the contiguous protoplasms adhering to its outer surface (fig. 6 5), indicating the firm adhesion between this vesicle and the walls of the sphere, which we know to exist. This vesicle expands as the gemma increases in size. At first, the latter is closely invested by the former; but when the cilia are developed on the surface of the young organism, the vesicle becomes considerably distended, allowing the gemma to revolve freely within its prison house. (See fig. 5.) At this time the gemma is already invested by its proper superficial pellicle ; hence the latter cannot be the modified primary germ-cell, as supposed by Mr. Busk, but is a new growth developed on the surface of the gemma whilst enclosed within the enlarged germ-cell. The source of this pellicle must be sought for in the aggregated protoplasms. It appears to be an independent secretion thrown off by them, in the way that the epidermal celis of a leaf co-operate to produce the similar structureless superficial pellicle. If this be a true homology, it would countenance the opinions of Schleiden and Payen, rather than of Mohl and Henfrey, the latter of whom regards the superficial pellicle as composed of the altered primary walls of pre-existing cells, and not as an external secretion. Henfrey’s explanation is that which I applied to the pellicle of Volvox, until the suggestion of Mr. Busk, respecting the primary condition of the volvocine protoplasms, showed me that in this instance the hypothesis was untenable. The relative periods at which the cells, the superficial pellicle, and the cilia make their appearance is not easily determined. So far as I have been able to form an opinion, I am disposed to think that the cilia first make their appearance, the cells and the outer pellicle being subsequent growths. A priori, we should have expected this to be the case, since it would not have been easy for delicate, flexible cilia to force their way through one or two imperforate invest- ing membranes. When the cilia are first produced they are very short, but they gradually lengthen, apparently by addi- tions to the base of each, secreted by the respective proto- plasms. After their formation we can readily understand how the pellicle could be secreted from the mass of protoplasms between and round the roots of these cilia, no pellicle being Wiiiamson on Volvox globator. : a}4) produced where they were attached to the protoplasm. As subsequent additions were made to their length, they would readily push through the apertures so left. After the cilia have fallen off, these apertures can occasionally be seen . arranged in pairs, as described in my last memoir. [I have, in my cabinet, one specimen in which two large Infusorize have been developed within the Volvox, and have apparently eaten away many of the protoplasms without destroying the integrity of the sphere: the cilia have also fallen off: the remaining membranes confirm my previous description of the appearance and relative positions of these apertures. The fluid with which the sphere is filled is not mere water, but is apparently mucilage. In a preparation in which a number of these objects are mounted in dilute alcohol, this gummy matter has changed to a brown colour, and refused to mingle with the alcohol, as would be the case supposing it to be mucilaginous. This proves that it is a true secretion from the organism, and not merely water absorbed by endosmosis. We may possibly obtain from this source an explanation of the distension of the entire sphere, of the individual cells, and of the vesicles investing the germs. As this gummy secretion increased in quantity, each thin membrane investing the respective protoplasms from which the fluid was derived, would become distended for its reception, as the mere result of internal centrifugal pressure. The secretion itself is, perhaps, little more than a diluted condition of the same gum as that which is more or less completely converted into cellulose in the various investing membranes just enumerated. I cannot but think that the details now brought forward, resulting from a careful re-examination of the entire subject, will convince every unbiassed observer of the general accuracy of my previous conclusions, and especially those relating to the cellular structure of the walls of the sphere. In the memoir in which these conclusions were recorded, I pointed out the close analogy that existed between the development of Volvox and that of many of the lower Alge and Conferve. I also referred to the obvious resemblance of each protoplasm to the well- known Zoospores. It is only whilst the segmentation of the gemme is in progress that a real relation exists between Volvox and young growing Conferve. At a later peried every segment ofthe former becomes converted into a Zoospore: each Zoospore, in turn, having the power to cast off its cilia, and go through a new process of segmentation, in precisely the same way as the Zoospores of a Conferva or a Vaucheria. Only a few in each Volvox are selected for this purpose, but the potentiality 56 Wiuamson on Volvox globator. doubtless resides in all. The cell-walls in the Volvox re- semble the cells in which the Confervoid Zoospores are deve- loped, the only essential difference being, that in the former instance the cilia penetrate the cell-wall, instead of being retained within it, and the germination is carried on whilst the Zoospores maintain their connexion with the ane sphere, instead of being previously detached from it. All the facts brought to light by this inquiry confirm my previous conclusion (which conclusion receives, also, the effective support of Mr. Busk), that the affinities of Volvox are with the vegetable, and not with the animal kingdom. Since the above memoir was laid before the Society, Mr. Busk has supplied me with specimens of Volvo stellatus. I quite agree with him - in his view that V. stellatus, V. globator, and V. aureus are mere varieties of one species. In his specimens of V. stellatus the protoplasms were of the stellate form of fig. 1. The investing cells were obviously present in all the examples which I ecamined. The above generalisation by Mr. Busk does away with the possibility of the brilliant granules of the protoplasm being spores, and leads to the probability that the curious bodies either in V, stellatus or V. awreus are the true winter spores. In J. stellatus I have noticed that the ordinary power of gemmation appears to have worn itself out; since, though the gemmez often co-exist with the spores (7), they are small, colourless, and abortive. The curious stellate invest- ments of the spores (?) of V. stellatus appear to me to be homologous with my vesicles (fig. 5), within which the true gemma are developed, and consequently to be the modified primary germ-cells. These often exist without the stellate protuberances, when their resemblance to the vesicles of the gemme is very obvious. In the pond from which I chiefly obtained my specimens this year, they were all of the type represented in fig. 10. This was their character in April. In the beginning of September, all traces of the connecting threads had disappeared, each protoplasm then resembling my fig. 4. At the close of September nearly all the Volvoces disappeared. In the few that remained, the protoplasms had reverted to the stellate type of fig. 1. Oh Biber) On the Application of Puorocrarny to the Representation of Microscopic Objects. By JosErpu Dertves, Esq. Commu- nicated by Mr. Bowerbank. (Read Oct. 27, 1852.) At the present time, when the microscope is contributing valuable aid in nearly every department of science, and its uses as an instrument are more generally known, it becomes of the greatest importance to possess some method more truthful than those hitherto adopted for copying the beautiful images of the achromatic object-glass. The recent discoveries in photography render its appli- cation to the microscope a subject for much consideration, since only by its assistance can we hope to obtain trustworthy impressions of objects so delicate and minute. I would, there- fore, beg to submit to the consideration of the Society the method I have adopted for producig these copies; and as an illustration of the successful application of Photography to the microscope, I have the honour of presenting the specimens which I have recently obtained. I must, however, beg to state that others have an earlier claim than myself to this application; but with so little success had it previously been carried out, that I believe I am correct in saying it has been generally abandoned as a means of depicting microscopic objects. But for the satis- factory result it is only necessary to refer to plate VII. The only arrangement necessary for the purpose is the addition to the microscope of a dark chamber, similar to that of the camera obscura, having at one end an aperture for the insertion of the eye-piece end of the compound body, and at the other a groove for carrying the ground-glass plate. This dark chamber should not exceed 24 inches in length (the size which I have found best to adopt): if extended beyond this, the pencil of light transmitted by the object- glass is diffused over too large a surface, and a faint and unsatisfactory picture is the result. The specimens ex- hibited were taken at this distance, which has the additional advantage of producing a picture, in size very nearly equal to the object as seen in the microscope. The eye-piece must be removed from the compound body, and the object (being well illuminated by reflection from the concave mirror) must be adjusted and focused upon the ground-glass plate. In the production of positive pictures a slight difficulty here arises, dependent upon the “ over-correction” of the object-glass. The effect of this ‘“ over-correction” is to project the blue rays of light beyond the other rays of the spectrum, and as the chemical properties of light reside in the violet and blue VOL. I. ia Seemann ee essai, 58 On the Application of Photography. rays, it becomes necessary that the plane of the sensitive plate should coincide with the foci of these rays, and it must therefore be placed beyond the surface at which the best definition is seen; this amounts to some distance with the lower combinations, and decreases with the increase of mag- nifying power. For the production of negative pictures the ordinary illu- mination is not sufficient, and recourse must be had to the sunbeam, which should be reflected upon the object by the plane mirror when powers are used not exceeding the quarter of an inch combination. It is not necessary here (when pro- ducing negatives by the sunbeam) to allow for the “ over- correction” of the object-glass, but merely to focus the object carefully upon the ground-glass plate. With regard to the time required for the production of these photographs, unfortunately no precise rules can be given, since it must vary with the sensitiveness of the mate- rials‘employed. The larger group exhibited was produced by the “1 inch object-glass,” and the time given varied from ten seconds to one minute. The smaller group, representing ““scales of Lepisma saccharina by the quarter inch and one- eight inch glasses, was taken with a more sensitive collodion ; and the time from ten to fifteen seconds.” In the production of negative pictures (from which the paper specimens were obtained) a moment’s exposure to the sunbeam is sufficient when using the lowest powers, and with the highest I have varied the time from five to ten seconds. In conclusion, | beg to submit this method which I have found so simple and successful, in the hope that the com- munication may be the means of directing attention to a subject both useful and interesting, and in the confidence that most satisfactory results will yet be obtained. Some Observations on the Structure of the Starch-Granule. By Geo. Busx, Esq., F.R.S. (Read Dec. 29, 1852.) “‘ No substance has been more investigated, and yet of which there is less known, than starch. After the researches of ten years, in the course of which the most various views have been propounded on the nature of starch, and after all its character- istics as a proximate vegetable substance have been discussed, we are little or nothing in advance of the old point of view ; and although we may, perhaps, not be wholly without some addition toour knowledge in secondary points, we are still entirely without any sound reasons to suppose that we have arrived at the truth.” This passage, from Poggendorff’s Annal., 1837, vol. xxxii. Busk on Starch-Granules. : 59 is quoted by Professor Schleiden, writing eight years after- wards,* and he adds that these eight years, notwithstanding the publication of innumerable works by chemists and vegetable physiologists, had been equally thrown away in the investi- gation of this important vegetable element; but, strangely enough, asserting that this unsatisfactory result had arisen solely in consequence of neglect, or from superficial micro- scopic examinations. If our knowledge respecting the structure of the starch-grain were thus unsatisfactory in 1844, it can scarcely be said to have been much enlarged since, notwithstanding the investiga- tions of the learned and eminent Professor himself; and to which investigations—whatever he may be inclined to think or express with respect to the labours of others—he would not be the last to resent the imputation of superficiality. We cannot but believe that a subject, which has thus baffled the endeavours of so many and such competent inquirers, must - possess some inherent difficulty, for, in 1851, we find Dr. A. Braun,{ one of the most accurate and acute of recent vegetable physiologists, still lamenting, in the same terms as Schleiden, the want of accurate knowledge on the subject of the origin, forma- tion, and structure of starch, which he is of opinion demands a new and careful investigation, seeing that none of the views set up are sufficiently based upon direct observation. : Having lately been incidentally led to the investigation of the structure of the starch-granule, I have thought the results might be interesting to the Society, although they cannot be said to be altogether novel. In the numerous and very different modes in which it has been attempted to explain the structure of the starch-granule, only two really and essentially distinct views seem to be ex- pressed. ‘These views,” as Schleiden observes, “are de- cidedly opposed to each other, and on the assumption or rejec- tion of them, the chemical judgment passed upon this substance must essentially depend.” 1. According to the one view the starch-granule is a vesicular body, the wall of which differs, at all events in consistence, if not in chemical constitution from the contents. 2. In the other view the granule is considered as a solid body, constituted either of a homogeneous substance, or com- posed of concentric layers, deposited, according to one set of observers, around a nucleus, either differing in its chemical * ‘Principles of Scientific Botany.’ Translated by Dr. Lankester. 1849. p. 19. + ‘Betrachtungen iib, d. Erscheinung der Verjiivgung in der Natur.’ 1851. F 2 60 Busx on Starch-Granules. nature from the layers around it (Fritsche), or not essentially different in that respect (Endlicher and Unger). Schleiden, on the other hand, and many other observers, look upon the supposed nucleus as a minute cavity or indentation. Dr. A. Braun (/. c.), however, supposes that this cavity does not exist originally in the granule, but that it is of a secondary nature, arising in the disappearance of the nucleus. The laminated, or supposed laminated, appearance evident in many forms of starch, and demonstrable perhaps in many others by means of polarized light, has been variously explained according to the above views not" the essential constitution of the sranules. In accordance with the former of these views, Miunter,* Nageli,t and Link, suppose that the lamine are formed by an internal or centripetal deposition of matter in the interior of the cell, and, according to the latter, this deposition is con- ceived to take place from without, or, as it may be expressed, centrifugally. This notion appears to be that more generally adopted. Originally propounded by Fritsche, it is followed by Schleiden, and, more recently also, though with some hesi- tation, by Dr. A. Braun (2. c.) who considers it as much more probable than that advocated by Munter and Nageli, if the starch-grains are not themselves cells, but merely the product of secretion from the cell-contents, in the same way as the cell- membrane is, with which the starch is so closely allied. ‘The same view is also adopted by Focket and Schacht.§ The above is a very brief and imperfect summary of the views more generally entertained on the structure of starch, and, omitting all reference to what has been written respecting its mode of “origin (which, in fact, amounts to little) and its use in the vegetable economy, I will now proceed to notice what may be termed a modification of the former of the above described views, or of that which assigns a cellular structure - to the starch-granule, and the reception of which I am greatly inclined, from my own observations, to advocate. 3 Leeuwenhoeck,|| to whom we are indebted for the earliest notice of starch-granules, enters with considerable minuteness into a description of those of several plants, such as wheat, barley, rye, oats, peas, beans, kidney beans, buckwheat, maize, and rice, and very distinctly describes experiments made by * Minter, ‘Ub. das Amylon der Gloriosa superba,’ &c. (‘ Bot. Zeit.’ 1845, p. 198.) { Nageli, ‘ Zeitschrift.” 1847, p. 117. + Focke, ‘ Die Krankheit der Kartoffeln.’ Taf. ii. fig. 13, f. g. h. § Schacht, ‘ Die Pflanzenzelle.? 1852, p. 41. || Leeuwenhoeck, ‘ Epistole Physiologice,’ &c. Delphis. 1719, p. 236. Busx on Starch-Granules. : 61 him in order to investigate the structure of the starch-granule, He placed a certain. number of the grains upon a clean piece of glass, and added a minute drop of water, and, upon the grains thus separated from each other, he placed two more drops of water. The water was then dissipated by the apph- cation of heat for about a minute. He then noticed that the -starch-granules had lost their rotundity and degenerated into plane figures of unequal size. From this experiment he con- cluded that the starch-grains of wheat, and other plants examined by him, were covered, like the wheat-grains them- selves, by a cuticle. And he imagined that the incurvation of the starch-granule took place at that part only, where the cuticle, not being continuous, was joined by a sort of com- missure—whence, he conceived it arose, that the granules, being heated and moistened, dehisced, and sank down into a flat form. He gives numerous figures of various sorts of starch in different stages, from partial expansion to complete evolution. We have here apparently the basis of the cellular hypothesis of starch, afterwards more fully developed by Raspail and others. Leeuwenhoeck, however, does not appear to have re- garded the contents of the starch-cell as fluid; and in this he was obviously more correct than his modern followers. But as Raspail’s view, in its integrity, is no longer maintained, I believe, by any one, having been long ago given up even by his more immediate followers, and particularly by Payen and Persoz, it is needless further to advert to it. The later modi- fication also of it advocated by Minter and Nageli, though ' with more scientific pretensions, is still so diametrically opposed to what may perhaps now be considered the correct doctrine of vegetable cell-formation, as in my opinion to be totally inadmissible. Following in the footsteps of Leeuwenhoeck, Dr. S. Reissek* attempts to deduce the cell-nature of the amylum-granules from the phenomena presented during their decay or disso- lution, when left for some time in water. He says that, “‘ owing to the solution and exosmosis of their internal and more solid substance (in contradiction to Schleiden and Miinter), they become hollow, so that of the entire starch-granule only the outermost layer remains, which, having become soft and flexible, assumes the appearance of a closed sacculus, that is, of a cell.” He therefore regards the amylum-granule as a perfect cell. * Keissek, Haidinger’s ‘ Berichten tb. d. Mittheil. von Freunden d. Naturwissen. in Wien.” Mai—Oct. 1846. Wien, 1847, p. 84. 62 Busk on Starch-Granules. : M. Guibourt * says that the internal portion of the starch- grain breaks up in the form of flocculi, whilst the outer portion, the membrane, is lacerable, and occasionally exhibits the form of an empty pouch. The expansion and alteration in form of the starch-grain, under the influence of heat and of sulphuric acid and other re-agents, is a fact recognised also by Schleiden and those who adopt the view of its solid or homogeneous nature; it is, in fact, so obvious a phenomenon that it could not possibly escape observation. ‘They, however, and I believe nearly all who have adopted the cellular hypothesis, consider this to be owing simply to the expansion of the solid body or vesicle. Till very recently, Leeuwenhoeck only appears to have attri- buted this increase in size and change of form of the granule, not to a mere expansion, but to an opening out of the granule on one side, or to its evolution in other words, whence it assumes a flattened figure, and of course an increase in apparent diameter. Although not, in the precise sense, understood by Leeuwenhoeck, I believe that his notion, with some correction, represents more nearly the true doctrine of the structure of the starch-granule than that of any of his successors till a very recent period. | In the Philosophical Magazine for April last is a paper ‘On the Amylum Grains of the Potato,’ by A. G. C. Martin, Librarian of the Imperial Polytechnic Institute of Vienna, which appears to me to contain the germs at all events of a correct doctrine with respect to starch ; and as I was led to pretty nearly the same conclusions as himself, though from experiments of a different kind and instituted for a different purpose, I have the more confidence in his results. And as the procedure I was led, more accidentally than otherwise, to adopt is perfectly easy and simple, this paper may at all events serve to incite others to repeat the experiments, and thus we may hope that the verata questio of the structure of starch may in some degree be set at rest. M. Martin’s mode of experimenting is nearly as possible the same as that adopted by the illustrious Leeuwenhoeck, and his results are not in the main very dissimilar. As the observed results at which M. Martin and myself have arrived in the examination of potato starch appear to coincide in every particular, it is obvious that the reasoning applied to his is equally applicable to mine. These results have in both cases been arrived at by noticing the phenomena which take place in the amylum-granule during its expansion, and * “Journal de Pharmacie.’ 1846, p. 191. Busx on Starch-Granules. 63 not when it has nearly or completely terminated.* This ex- pansion or dissection of the granule is effected by M. Martin by means of heat applied in an ingenious but still incon- venient way, while the object is under the microscope. He thus employs it :— “ Between two very thin glasses, of the same size as the stage of the microscope, a little amylum, with a sufficient quantity of water, is to be put, and the former well spread out with the finger, to prevent as much as possible the formation of bubbles. The number of amylum grains in the field of view should not exceed ten or fifteen. The glasses should lie freely on the spring-piece, which must be raised by means of two pieces of cork introduced below it, so that while the two glasses are lying right upon the object-bearer, a current of cold air will ascend from below, or permit the little flame to continue burning in the hole of or below the stage. As the glasses are wide, they protect the microscope from too great a heat or other danger. The small flame is to be obtained from a common thread, doubled and slightly waxed. ‘This, when ignited, gives a flame quite sufficient to boil the amylum.” In the course of his experiments he discovered that the slightly iodizing of the starch-grains delayed, so to speak, the entire process of boiling, and rendered the result more certain and satisfactory, and he states that his process seems to succeed still better in a concentrated solution of alum, with as much tincture of iodine as will colour the grains of a steel blue. The same benefit arises also in my process from the addition of as much iodine as will render the starch a pale blue without destroying its transparency ; and the use of iodine in either case is attended with the further advantage that it renders the starch in its subsequently changed condition much more visible than it otherwise would be. Instead of heat I employ concentrated sulphuric acid, and in the following way :—A small quantity’-of the starch to be examined is placed upon a slip of glass and covered with five or six drops of water, in which it is well stirred about, and with the point of a slender glass rod the smallest possible quantity of solution of iodine is applied, which is to be quickly and well mixed with the starch and water. As much of the latter as may be must be allowed to drain off, leaving the moistened starch behind, or a portion of it is to be removed by inclination of the glass, and the starch is then to be covered with a piece of thin glass. ‘The object must then be placed in the * Vide Observations on the Structure of the Starch-granule in a paper on Valisneria spiralis, by E. J. Quekett, published in the third number of the ‘ London Physiological Journal’ in 1844. 64 Busx on Starch-Granules. microscope, and the object-glass i or $) brought to a focus close to the upper edge of the piece of thin glass, With a slender glass rod, a small drop of strong sulphuric acid is to be carefully placed immediately upon, or rather above the edge of the cover; care being taken that it does not run over it. The acid of course quickly insinuates itself between the glasses, and its course may be traced by the rapid change in the appearance of the starch-granules with which it comes in con- tact. The course of the acid is to be followed by moving the object upwards, and when, from its diffusion, the re-agent begins to act more slowly, the peculiar changes in the starch- granules, now also less rapid, may be readily witnessed. These changes in potato-starch are thus described by M. Martin.* “First, the amylum grain sinks in, in that place, where, according to Fritsche, the kernel (nucleus) is situated. On the surface minute fissures appear, two of which almost regularly diverge towards the thicker end of the grain. The grain continues to be depressed inwards until a cavity is formed which is surrounded by an elevated ridge. In pro- portion as the grain swells up, this ridge increases in circum- ference and decreases in breadth, that is, continues to get flatter until fissures, mostly of a stellated form, appear in the hitherto, little altered thicker part of the grain. ‘The process is not very rapidly developed, and it is very difficult for the eye to follow it. Suddenly something is torn off, the grain is extended lengthways, and in the next moment a wrinkled skin of a rounded, generally oval shape, lies on the glass. Middle sized and sina grains exhibit this shape most dis- tinctly ; and they have usually only one longitudinal wrinkle, the upper and lower ends of which are pointed. The constant appearance of this wrinkle is important for the development of my theory. The appearance of this disc,’ he goes on to say, ‘‘ demonstrates that it is perfectly flat, and has a slightly elevated edge which also becomes flat on pressure. The con- tour is rounded, but perfectly sharp. If the two glasses be violently moved from one side to the other whilst pressing the amylum, the disc is torn, and it is distinctly seen, especially in the blue-coloured ones, to consist of two layers, an upper and a lower one. Further examination shows that they are collapsed vesicular bodies, consisting of an extremely fine but strong and elastic membrane.” ‘‘The primary form, therefore, of the amylum grain,” ac- cording to M. Martin, ‘is aspherical or ovate vesicle. If this be considered as empty, and so contracted that one-half Pe. 2K, Busx on Starch-Granules. | 65 | lies in the other half, a watch-glass shaped basin is formed, which after boiling and pressure between the two glasses, appears, in consequence of the delicacy and elasticity of the membrane, as a flat, round-edged disc.” ; According to him, it follows, that the starch-granule, in its more usual form at least, is formed by the inrolling upon itself of this spherical or ovate vesicle. It is not very easy, at all events I do not find it so, to comprehend M. Martin’s expla- nation of the mode in which this inrolling or involution takes place, nor have my own observations as yet enabled me to express a very decided opinion with respect to this point. The appearances exhibited in the microscope, under the action of strong sulphuric acid, convey the idea rather of an unfolding of plaits or ruge, which have, as it were, in some kinds of starch (those with a long fissure-like or stellate hilum especially) been tucked in towards the centre of the starch grain, than of the unwinding of rolls. And I conceive that the apparent laminz are nothing more than the indications of the edges of such plicz or folds in the contracted state, upon which I shall say a few words presently. ‘The starch-grain of the horse-chestnut perhaps affords as good an example as any, and one readily obtainable, of the appearances which might be supposed to arise were the constitution of the granule such asI have just described ; that is, as far as the tucking in of the vesicle towards the centre is concerned, because in this grain I am not aware that the concentrically laminated appearance arising from folds of the vesicle is evident. Fig. 10, Pl. VIII, represents the usual forms and aspect of the unaltered starch of this fruit, and figs. 11, 12, 13, various granules in different stages of evolution under the use of strong sulphuric acid. If it be allowed that the starch-vesicle, as the ultimate product of the evolution of the grain might perhaps be termed, be elastic—which, in all probability, it is—it is easy to understand, as in fact is pointed out by M. Martin, that the portions which are folded into the interior must be more or less compressed, and thence denser ; 1n consequence of which inequality of tension the phenomena exhibited under polarised light might be explained. I have examined several varieties of starch, such, for instance, as of the Po- tato; the Arrow-root termed ‘Tous les mois,” which is, I believe, afforded by a species of Canna; two other kinds of arrow-root ; the starch of the Spanish Chestnut; of the Yam ; of aspecies of Curcuma, which seems to be identical with East Indian arrow-root; of Cycas circinalis; Zamia integrifolia ; Arum maculatum, and what is termed Tacca arrow-root; and find more or less distinctly in all, indications of a similar 66 Busx on Starch-Granules. structure, differently modified, however, in some respects, in each. Upon referring, moreover, to the figures of different kinds of starch given in Schleiden’s ‘ Botany,’ before quoted, a tolerably complete series of development, as it may be termed, of different forms of starch, will, I think, be suffi- ciently obvious. Fig. 13 of Schleiden, representing starch- grains from the rhizome of Anatherum iwarancusa,* and fig. those of Iris pallida, show, as I conceive, the simplest form of inversion or folding of the edges of the starch-vesicle. A further stage is apparent in fig. 12, the starch of Colchicum autumnale; and a further advance may be traced in fig. 14, the starch-granules of Arum maculatum, whence the tran- sition to the form presented by the starch of the horse- chesnut is sufficiently clear, and from these more or less open forms to the complete involution seen in the potato-starch, &c. The dissection of the starch-grain may be effected in several ways besides those I have noticed, and equally, if not more, conveniently. And as the dissection effected in any of these modes appears to yield the same result, the latter may be regarded perhaps as the more worthy of confidence. I have usually selected for my experiments the form of arrow-root called ‘‘Tous les mois.” It is a favourable subject for investigation, owing to its large size and regular con- formation, as seen in figs. 1, 2, 3, 4,5. The grains of Tous les mois are of various sizes and of different shapes,—some oval, some more expanded, with a sort of horn or shoulder on. each side, or on one side only. The grains, like those of most. kinds of starch, are not cylindrical, but flattened, and towards one end of each grain is a minute circular spot, the area of which appears granular; and concentric to this spot the surface of the grain—or rather one of the flat surfaces only and the sides—is marked with delicate concentric rings. It is these rings which have been described as indicating a laminated structure, and, consequently, corresponding lines or planes should be seen, under favourable circumstances, passing through the substance. This appearance has actually been described as existing by Schleiden and others, but I have looked for it in vain, and Mr. Quekett, in his Lectures on Histology, describes the markings as superficial. His ex- pressions, moreover, would plainly imply that this accurate observer entertains an opinion with respect to the structure of the starch-grain pretty nearly if not quite identical with that advocated in this paper, and that, as I suppose, the lines indicate the ruge or folds into which the starch-vesicle is * Miinter, however, denies the existence of starch-granules like those figured by Schleiden in the rhizome of A. wwarancusa. Busx on Starch-Granules. 67 thrown in the contracted state, and that this is the case seems to be shown by the immediate effects of re-agents. The first change, after a slight swelling of the starch-grain, consists in the appearance of minute transparent elevations around the edge of the grain, as shown in fig. 6, each of which, I con- ceive, represents the edge of a fold or ruga ; a further stage of expansion is shown in fig. 7, and a still farther one in fig. 8; whilst the full expansion of the vesicle in Tous les mois is shown in fig. 9. I believe, also—but of this I would speak very doubtfully — that each starch-vesicle has an opening which corresponds with the central spot or hilum. With respect to the contents of the vesicle, some appearances lead me to suppose that, occasionally at all events, it contains a flocculent or grumous material—amorphous starch, which is equally coloured by iodine, as is the wall itself of the vesicle. There is sometimes also an appearance of a transparent colourless wall around these grumous contents, in a form of arrow-root I have examined; but an outline of this kind is often a very deceptive phenomenon, and I do not wish to be understood positively to assert its existence even in the case alluded to. Two additional modes, which I have found convenient in the examination of starch, consist:—Ist. In the previous roasting of the grain till it acquires a light-brown colour, and is, in fact, converted into British gum; while in this state, if it be moistened with a very weak solution of iodine, the grain gradually unfolds itself in the most beautiful manner. 2. The iodized solution of chloride of zinc, proposed by Pro- fessor Schultz, may also be very advantageously employed. This solution, if quite concentrated, does not at first colour the- starch at all, but, on the addition of a little water, the blue colour is elicited, and the starch-graims gradually swell out and evolve themselves in the same way as they do under the previously described treatment. I make the iodized so- lution of chloride of zinc by dissolving 1 ounce of fused chloride of zinc in about half an ounce of water, and adding to the solution (which amounts to about an ounce fluid mea- sure) 3 grains of iodine dissolved, with the aid of 6 grains of iodide of potassium, in the smallest possible quantity of water. Since the above paper was read, I have noticed appear- ances in the amylaceous corpuscles which occur in the wall of the primordial utricle of Hydrodictyon utriculatum, which lead to the opinion that the starch—in this case at least, 68 Smitu on Asteridia. and probably in all the similar forms and situations in which it occurs in the lower Conferve, &c.—is deposited around a nitrogenous nucleus. In Hydrodictyon the fact is very clear, that the central portion of the amylon-corpuscle is turned of a deep brown by iodine, or pink, by sulphuric acid and sugar (as was first pointed out to me by Mr. Huxley), and that at one time it exhibits no trace of starch in its composition, but that subsequently this nitrogenous nucleus becomes sur- rounded, not with an entire wall of starch, but apparently by a cup-shaped deposit of that substance in which the nucleus les imbedded, or from which it projects on the external aspect. Further observation of this and analogous pheno- mena may perhaps in time lead to a more satisfactory ex- planation of the genesis of starch than can at present possibly be given. It does not, at all events, contradict the notion of the vesicular nature of the starch-grain, but rather, as it seems to me, tends to confirm it; for we have only to imagine the entire removal—as we may often witness the partial—of the central nucleus, when what remains, viz. the cup in which it was lodged, will very closely resemble some of the more open forms of starch-vesicles I have noticed in the paper. On the Stellate Bodies occurring in the Cells of FREsH-wWATER “Aues. By the Rev. Wittiam Smirtu, F.L.S. Tue third volume of the ‘Transactions of the Microscopical Society,’ containing, at p. 165, ef seq., two papers by G. Shad- bolt, Esq., ‘ On the Sporangia of some of the Filamentous Fresh-water Algez,’ has just been placed in my hands. The subject discussed in these papers having attracted my attention at various times, and being in possession of ad- ditional facts, some corroborative of Mr. Shadbolt’s state- ments, and others which lead me to a conclusion widely different from that to which he has arrived, I have gladly embraced the opportunity, which the Society has accorded me, of bringing the following details under the attention of its members :— | The accurate observations of one of the earliest and most successful students of this department of botany, M. Vaucher, of Geneva, have established the correct nature of the oval body, formed by conjugation in the filamentous Algz, which this author has shown to be a true spore, each such body, formed by the union of two cells, giving birth, upon germina- Smitu on Asteridia. | 69 tion, to a single cell, which subsequently, by the ordinary method of self-division, becomes elongated into a filament (‘ Histoire des Conferves d’Eau douce,’ Geneva, 1803, p. 66, et seq., PI. IV. 5, V. 3, VI. 4). [have been able, by personal. observation, fully to confirm the observations of M. Vaucher in reference to one species of the Conjugate (‘ Ann. Nat. History,’ 2d5., vol. viii., p. 480), and have no hesitation in accepting the facts as of general import in reference to the entire family. | have alluded to the circumstance, not only as having a direct bearing upon the subject of this paper, but also that I may explain my reason for not employing the term “ Sporangium ” in reference to the bodies in question, it being evident that this designation is not applicable to a body which is in itself a single germ. With regard to the stellate bodies to which your attention is now more particularly requested, their true character being for the present doubtful, it will be better to employ a desig- nation which does not involve any reference to their nature, and has regard merely to their form, I shall therefore speak of them as Asteridia, their general appearance being that of circular, star-like bodies. The presence of asteridia is by no means confined to the family of the Conjugate. I have frequently noticed them in the Desmidiee, and occasionally in the Diatomacee, though in these tribes the presence of spinous processes is by no means a constant character. I have always found (and Mr. Shad- bolt’s experience seems to be confirmatory, /. ¢., p. 166) that, if present in a gathering when first made, the numbers of asteridia rapidly increased when the Alge were retained in vessels for future examination, and as more or less of change and decay almost invariably attends the attempt to preserve such organisms in a limited space, and removed from their natural habitats, I have hitherto regarded the presence of asteridia as indicative of disease, as being, in fact, a parasitic, perhaps a fungoid growth, consequent upon the degeneration of the cell- contents. x I am not prepared to put forward this as the true character of asteridia, but I am prepared to dispute a view of their nature which confounds them with the reproductive germs, and shall proceed briefly to state the reasons why such a character and function are altogether inadmissible. It is well known that conjugation in the Alge implies the union of the entire contents of two cells, which contents inter- mix and become condensed into the reproductive spore, and that this union is effected by the amalgamation of the contents of two contiguous cells in the same filament, or by the same 70 Smitu on Asteridia. process occurring in two cells belonging to different fila- ments. The mode in which this amalgamation takes place is either by the breaking down of the walls at the contiguous extremities of the cells, as in the Vesiculifere, or by the production of connecting tubes, which form channels of com- munication between the conjugating cells, whether in the same or different filaments. ‘These connecting tubes are shown in the drawings which accompany this paper, Pl. [X., fig. 2 3, fig. 46, &c.: and it is worthy of notice that, although one mode of effecting the union of the cells seems to be pretty general in the same Alga, it is by no means constant, as tubes connecting contiguous cells of the same filament, or uniting apposed cells of different filaments, will be found in con- nexion with the same species: an example is given in fig. 6.* Now it will be seen by a reference to the figures I have given, and more particularly to figs. 4, 5, 6, which are drawn with the camera lucida from mounted specimens of Zygnema quadratum kindly supplied by Mr. Shadbolt himself, that the circumstances, as stated above, which accompany the process of conjugation, altogether negative the opinion that the asteridia are products of such a process, as the cells contain- ing these bodies always contain with them a portion of the original endochrome or cell-contents, which must have been entirely absorbed had conjugation been effected. Nor are there, in any case, to be found the connecting tubes which are necessary to the process in the species we have selected. It is, therefore, evident that the asteridia are not modified or matured spores, as the cells containing them have not under- gone the process necessary to the formation of the repro- ductive body. An inspection of fig. 1 will also show the incorrectness of the conclusion to which Mr. Shadbolt has arrived, viz., that the asteridia are spores in a more advanced stage. We have here a portion of a filament of Zygnema quininum, in the cells of which the gradual formation of the asteridia may be dis- tinctly traced. Cell @ presents the ordinary and healthy ap- pearance of the plant ; in cell 6 degeneration has commenced, and a faint appearance of several aggregations of the cell- contents may be detected ; these aggregations in cell ¢ assume the character of perfect asteridia, which in cell d are no longer in contact with the endochrome, among which they have been generated. But in no case do we perceive any * This fact throws some doubt upon the propriety of placing (as Kutzing has done in his genus Rhynchonema, and Hassall in a sub-genus) species, which conjugate by tubes connecting contiguous cells, apart from those in which the conjugation takes place between cells in different filaments. Smitu on Asteridia. ) (al semblance of the process of conjugation, or of that mingling of the contents of different cells so essential to this function of vegetable life ; and instead of only one body, which is the invariable result of the conjugating process between two cells, we have each cell containing several asteridia, the number of which I have noticed to vary from two to six in a single cell. Figs. 2 and 3, which are drawn from specimens supplied by R. Hodgson, Esq., exhibit phenomena which are equally irreconcilable with the hypothesis I controvert. ‘These sketches represent portions of filaments of Mesocarpus scalaris. In this species the reproductive spore is lodged in the inflated tubes which connect the conjugating cells, while the asteridia, which were exceedingly numerous in the specimens I examined, were invariably contained in cells from which no connecting tubes had been projected. To the above considerations let me add the fact already referred to, viz. that germination has in several species of the Conjugate been observed to take place in the oval or elliptical spore which results from the process of conjugation, without any previous change in the form of this body. The figures, given in the plate which accompany Mr. Shad- bolt’s paper, bear out to their fullest extent the facts I have now stated, and might, indeed, have sufficed as illustrations of my views had I not been desirous of giving as many examples as possible of a singular, and far from common, monstrosity, in a curious and interesting class of plants; but I cannot forbear calling attention more particularly to Mr. Shadbolt’s fig. 4. This drawing, which represents Lyngbya floccosa with aste- ridia, is surely sufficient to prove that such bodies have no essential connexion with the reproductive spore, for in this case there are no traces whatever of the conjugating process, and each cell, whether with or without asteridia, has its full proportion of endochrome, though in a disturbed and degenerate condition, the breaking down of the cell-walls in the neigh- bourhood of the asteridia being a further evidence of the diseased condition of the filament. On the whole, while I feel unable to assign a positive character to these singular parasites, I feel no difficulty in withholding from them the important office ascribed to them by the gentleman upon whose communication I have commented. ‘The writer of that paper will allow me to thank him for the interest he has excited in a subject which has long caused me no little per- plexity, and for the very lucid manner in which he has stated his opinions. Lewes, Jan. 12, 1853. 72 QueEKETT on Fungus. Note.—Since the above was read before the Society, I have met with a brief notice of the Stellate Bodies, to which this paper refers, in a communication from Mr. G. H. K. Thwaites to the ‘Annals of Natural History,’ vol. xvii. p. 262, and dated March 19, 1846. It is satisfactory to find that the observations and conclusions of this eminent algologist coin- cide, as far as they extend, with mine. Mr. Thwaites asks whether the stellate bodies in the cells of Mesocarpus scalaris may not be an abnormal growth of the nucleus, or perhaps an internal parasite; describes them as formed from a small spherical cell, containing an oily-looking fluid; and states, as I have done, that they are not developed, in the manner of spores, at the expense of the endochrome of the cells which contain them.—W. S. On the Presence of a Funeus and of Masses of CRrysTAatLine Marter in the Interior of a living Osx Trex. By Joun QuEKETT, Resident Conservator of the Museum and Pro- fessor of Histology to the Royal College of Surgeons of England. (Read January 26, 1853.) In the month of August of the past year I formed one of a pic-nic party to visit the well known King Oak, in Marl- borough forest. ‘The day was stormy at intervals, but there was little or no wind. Whilst we were all assembled under a large ornamental shed, erected for the convenience of visitors to this much-frequented spot, a sudden loud snap- ping noise was heard, which was followed by a still louder crash of broken timber. This we found was not occasioned (as we first imagined) by the fall of a lofty oak, but, as it subsequently turned out, of only a large limb. Our fears at the moment were prdatly excited lest this fall might have been occasioned by one of the junior members of our party swinging on the limb, but it appeared that he had climbed into the interior of the King Oak, and, looking out of a hole, was the nearest spectator of the aecident; his attention having been directed to it by the noise of the snapping of wood, and the crash produced by the fracture of the branches of numerous trees in the neighbourhood, upon which the limb in question fell. As soon as our fears were allayed by knowing that our young friend was safe, some of the more venturesome of the party, myself amongst the rest, sallied forth to see what had happened. We found that the King Oak was uninjured, but that a tree about fifty yards from it, and of very large size, QuEKETY on Fungus. : 73 had lost one of its finest limbs, and some idea may be formed of the size of it when I tell you that, at the fractured part, it was nearly three feet in diameter, and its length, to the first bifurcation, just twenty-seven paces. On examining the frac- tured surface, I was surprised to perceive that in the very centre there was a white flocculent mass, about a foot in diameter, which at once reminded me forcibly of the appear- ance presented by a thin layer of cotton wool cemented to the surface of wood by gum or glue. I looked at it very carefully, and considered that it must be a filamentous fungus; and, on examining it with my pocket-glass, I dis- tinctly saw some sparkling crystals amongst the filaments ; some of these were very minute, others sufficiently large to be visible to the naked eye. The wood, at a cursory glance, appeared perfectly sound, was very moist from the quantity of sap present, and had a powerful acid smell, like that of vinegar, which was very perceptible on approaching the fractured portion. Having satisfied myself of the pre- sence of a fungus, I turned my attention to the examination of the fractured surfaces, both of the tree itself and of the limb, and I could discover no hole or trace of a hole, or any dead wood leading from the circumference to the centre, either of the tree or of the limb, but still there was a peculiar appearance in those parts of the wood itself near the white filamentous mass above-mentioned, which was due to the separation of those woody fibres, that were involved in the fracture. This appearance is still present in a speci- men of wood I brought away at the time, but which has now become hard and dry. All its surfaces exhibit a very remark- able kind of roughness different from that of any oak wood that has been split by artificial means, and I have tried in vain to get a surface at all like it by splitting. Having removed as much of the wood covered with the white mass as I well could with the aid of a pocket-knife, I took it home for microscopical examination, and the structure most com- monly exhibited is that shown in fig. 7, pl. IX. The woody fibres were much separated in parts, and the spaces between them occupied by a filamentous fungus and rather large pris- matic crystals. ; An idea may be formed of the size of some of the crystals by the power under which the drawing, fig. 8, was made— viz. 00 diameters. On removing a portion of the filamentous mass for examination with higher powers, I found the fila- ments intimately mixed up with the crystals ; the former were on an average 1-500th of an inch in diameter, whilst some of the latter were 1-8th of an inch square ; most of the filaments Wy) 74 QuEKETT on Fungus. had numerous globular bodies, about 1-800th of an inch, adherent to them, but many were scattered about irregularly ; these I concluded might be the spores—they are shown in fig. 8. It now becomes a question whether this fungus is of the same nature as that termed Merulius lachrymans, which is said to be the cause of dry-rot. I have tried in vain to get any fungus resembling it in specimens of dry-rot taken from wood employed in building, and I never recollect seeing any- thing at all like it in the interior of any specimen of wood, either living or dead. ‘The crystals are very peculiar, they may be readily seen by the naked eye studding the surface of some of the sections; some of them are so intimately mixed up with the filaments of the fungus that the crystalline matter appears to have been deposited upon them. A large crystal is shown in fig. 9, having fungi in its interior ; one of these is represented in fig. 10. It would appear, therefore, that the fungi were in a great measure auxiliary to the fall of the limb in question, if not the entire cause of it, the effect of the growth of the filaments being the separation of the woody fibres and a destruction of the channels through which the sap flowed; this last, being diverted from its usual course, no doubt lost a great portion of its watery part by absorption, and the solid matter held in solution then began to crystallize. The parts most thickly coated with the fungi are free from crystals; in fact, the fungi are so numerous as to form a perfect coating over the wood, some of the filaments being still white, but the majority of a light-brown colour. In those pieces of wood in which a cavity or cavities have been formed by the separation of the woody fibres, the crystals are most numerous. ‘They are generally of a tabular form, and so transparent that the filaments of the fungi over which they have formed may be readily seen within them. I have not yet been able to ascertain the exact chemical composition of the crystals, but they are soluble in dilute acids, and probably consist of some vegetable acid, with lime asa base. ‘The occurrence of fungi, visible to the naked eye, within a living oak tree, is a fact which few, if any, persons have yet described ; but the fungus of the dry-rot in wood which has been exposed to circumstances favourable to its de-. velopment is far from being uncommon. The fungus now in question would appear to differ from the Merulius lachrymans in growing in the interior of a living tree, whilst that is stated in books to commence growth in the sap-wood on the exterior. It would be interesting to ascertain whether a similar fungus exists in other parts of the same tree; and I shall endeavour to enlist the owner of it in the cause of science, in order that, QuEKETr on Fungus. : 75 when the time comes for this ancient inhabitant of the forest to be cut down, some competent person may be allowed to examine it. It may happen that fungi are more frequently present in wood than has been imagined, and when such tim- ber is made a part of a ship or building it may be the first to show symptoms of decay. The ravages of fungi are very remarkable. At one of the early meetings of this Society we had two papers on the decay of fruit, in which Dr. Hassall showed that the rottenness in bruised or over-ripe apples, pears, &c. depended upon the growth of fungi. We have now another instance of it in the oak, and I think that the further investigation of this subject would be well worthy the attention of microscopists. It was a fortunate thing, perhaps, that a microscopical observer hap- pened to be present when the limb of the tree in question fell, for, as it was beginning to rain heavily at the time, all trace of the filaments would either soon have been washed away, or they would have become so much injured as not to have attracted notice, and thus the observations contained in this paper (valueless as they may at first sight appear) would not have been recorded. ot saad REPORT OF THE THIRTEENTH ANNUAL MEETING OF THE MICROSCOPICAL SOCIETY. The Microscopical Society of London held their Thirteenth Annual Meeting, February 11th, 1853,—GeroreEr Jackson, Esq., President, in the Chair,—when the following Reports were read :— 1. Report of Council—According to annual custom the Council have to make the following Report on the state and progress of the Society during the past year. The number of members reported at the last anniversary was 183, including six associates and honorary members. Since that time there have been elected thirty: making the number 213. This number must, however, be reduced, by three deceased and nine withdrawn, giving a total of 201 as the present number of members, and showing an increase of nineteen upon the number reported at the last anniversary. The Council have also to report that a proposal having been made by the Editors of a new Microscopical Journal to publish the Transactions of the Society in that work, the Council have acceded to that proposal; and the first two parts of the ‘ Quarterly Microscopical Journal’ have been published, containing the Transactions. ‘These, if required, may be obtained separately by members of the Society with- out charge; and the whole publication may be had by the payment of 4s. per annum extra. Several new works have been added to the Library, as well as many new objects to the Cabinet; and there are also in the possession of the Society various drawings and diagrams, relating principally to the papers read before the Society, to- gether with copies of the several parts of the Transactions. 2. Report of Auditors——The receipts and payments have been as follows :— Thirteenth Report of 78 "pUlo}}¥ 0} 91GB JOU SVM IOJIPNY 190 oY, ‘“ANVEC AYNAH *4001100 W9y} puNoj puv ‘yoo S.loINsvoL], oy} WIM wey) pereduoo pue ‘sJUNODDW 9A0Ge oY} POULUeXe oAvY [—'SGRT ‘YITT Auvonugag OL # OGIF L 8 69 => * © Sdeyarg@ye soueleg 6 9 LSTF O-6ES we et SS © | 10198] [(00 a) WOLsSrUMIOs Tome Col ec et 8, 8 ee aire ‘Surpurg ‘Aydeisouyy ‘sytodexy pue suoryoesuely, Suyuitg TL. OP * “la 8° op“ onemiepeostisog “Areuorterd 6 8 0L 2.5 = son” et 09 TIO ae Aon sy uOMTSoneny Gao Se Ss oe te IlO ‘sey ‘ssueey{ 3% eouvpue Vy a0 1G a * + reyoloeg JUBISISSY es OU0L de 2 st a” ek OT Jo-Aruyeg © 0 06 - * 3. 42° 3 Bee Wee su0-00Y yo Auer ‘Ds “Fg "SLNEWAV ————s OL F O6TF 3: 0-1 D's "5 “BOSOOSTCOOD ou i By 4 SS. gramme PLE $2 “10g fo Puspryaes wok Fey “ai (* Se pjos SuONoRsuET |, . e eS8T . ° ce e ° ZGST . . 14 . . TS8T ° . ce. e ° OSST . e 14 " * 6P8T ° ° syueurteg penuuy > SSg81. : ‘ * Zggt ‘slequioy Jo oouvlyuq 10,7 "+ + + geak snotaeid wo. souepeg "SLdIGOAY "SSST “MITT Arensqag 07 “Zogt “yI™T Arensqa,q worg SdOLIGNV HO LAOdAat the Microscopical Society. : 79 The President delivered the following Address :— GENTLEMEN,—It has been customary on the recurrence of the anniversary of this Society for the President to make some observations, in addition to the reports of the Auditors and Council, on the progress made during the past year. In compliance with that custom I have first to congratulate you on the accession to our ranks of no less than thirty new members ; a greater number, I believe, than have been elected in any one year since the formation of the Society. That our members, both new and old, take an interest in our proceed- ings, is evinced by the increased attendance at our ordinary meetings; while the subjects brought forward, and the discus- sions which have taken place on them, sufficiently prove that a large proportion of us are working microscopists. By the Auditors’ Report at the last anniversary we were informed that the funds in the Treasurer’s hands, which at the previous audit amounted to 85/., had become reduced to the small sum of one pound and eight pence. At the same time the publication of our Transactions was considerably in arrear ; and to add to our difficulties, the Horticultural Society, whose rooms we have hitherto occupied at a rent proposed by them- selves, gave us to understand that this rent would be increased by ten pounds a year. The ground assigned for the increase was the large amount of accommodation afforded to us; and inasmuch as the occupation of the council-room every Wednes- day by our curator was not contemplated when the rent was originally fixed, there was some show of justice in the de- mand. It was found also that very few of our members availed themselves of the opportunity afforded them of coming here in the daytime to use the microscopes. The Council, therefore, judged it proper, in accordance with the economy which the state of our funds so peremptorily obliged us to exercise, to discontinue the Wednesday attendance of the curator, by which they hoped not merely to save his salary, but also to remove the ground assigned for the proposed in- crease of our rent. In this latter expectation they have been disappointed. The Horticultural Society persist in their determination ; and it has therefore been resolved to remove our meetings to No. 5, Cavendish Square, where the Chemical Society will afford us the use of very eligible rooms, together with light and fire, for the rent which we have hitherto paid without these accommo- dations. By the Auditor’s Report, just now read, you will perceive 80 Thirteenth Report of that, although we have brought up our arrears of publication to the month of June last, and have paid all our debts, we have now a balance in hand of 32/., which the economical measures adopted by the Council will, I hope, increase during the next year. In order that the members may not be deprived of the opportunity of using the microscopes, examining the objects in our cabinet, and consulting and exchanging books, the Council has engaged a curator to attend at six o’clock on the evenings of our ordinary meetings, which, it is hoped, will be found more convenient than the day attendance that has been dis- continued. : The necessity for the prompt publication of our Transac- tions has been adverted to by more than one of my prede- cessors, and must be sufficiently obvious to all of us; for when a man has observed a new fact, or suggested an im- provement in the mode of observing, and has determined to bring the matter before the public, he is seldom contented with the notice which the mere reading of his paper may attract, but is anxious to see it disseminated in print, so that his claim, either of discovery or invention, may rest on a firm basis. Unless, therefore, we can offer these advantages, we must expect that many interesting papers which might other- wise have come to us will be taken elsewhere, and be sub- mitted to the public through some more expeditious channel. In accordance with these views, the Council has made an arrangement with two of our members, who have commenced a Quarterly Journal of Microscopical Science, for the regular printing of our Transactions in that periodical ; so that authors will not only see their papers promptly published, but will also enjoy the benefit of the large circulation which the Journal has obtained. Our members, also, in addition to a copy of the Transactions, will obtain all the other matter which the Journal contains for one shilling per number. On the value of this matter, as two numbers have been already published, it is needless for me to expatiate at any length. Besides interesting original communications from observers in our own country, by means of translations and extracts from foreign journals and reviews of foreign works it affords to the mere English reader the knowledge of what is ~ being done by microscopists in all parts of the world; and by thus giving a starting point to his inquiries, prevents his wasting his time and energy in re-discovering what has been already observed. | The publication in full of our Transactions up to the end of June last, and the abstracts in the Journal of the papers read before us in October, November, and December, render the Microscopical Socrety. he 81 it unnecessary for me to go so deeply into the contents of these communications as has been usual at former anniversaries. Mr. Shadbolt’s paper, containing a variety of useful prac- tical information on the habitats and mode of collection of a number of beautiful microscopical objects, was listened to with much attention, and elicited many remarks and inquiries, and, had it not been already published in the Journal, would have demanded from me a more extended notice. The paper of Mr. Simonds records an interesting patho- logical fact. As a medical man, I cannot help regretting that pathology is a subject on which we have very few communica- tions; for I feel assured that the investigation of the products of disease is one of the most 7mmediately useful purposes to which the microscope can be applied ; and I believe that such communications would be well received, not merely by those of my own profession, but by the members generally. The paper of Mr. Mummery on the development of Tubu- laria indivisa, and those of Mr. Busk and Mr. Williamson on Volvox globator, contain a vast amount of well-illustrated microscopical observations. The same praise is due to Mr. Busk’s paper on Starch, _ which also teaches us the useful lesson, not to be satisfied with examining things in their natural state, but, by applying re- agents under the microscope, to combine chemical research with microscopical observation. The subject of Microscopical Photography, on which Mr. Delves has favoured us with a communication, accompanied by some beautiful specimens, is one of great interest. That it will attain a high degree of perfection no one who knows the persons engaged in its cultivation can reasonably doubt. There is, however, a difficulty in its application, which, I fear, will materially limit its use. Those who have been in the habit of using the microscope since the first introduction of achromatic lenses must have noticed that in proportion as the object-glasses have increased in aperture and improved in definition they have lost the power of penetrating to any depth; and this has now been carried to such an extent that when we examine with a high power any but the thinnest objects lying in an almost mathe- matical plane, we can only do so effectually with the finger on the fine adjustment to regulate the focus for the particular point on which the eye is fixed. This precision of focus, which is a necessary consequence of precision of definition, must have the effect of confining pho- tography (except with low powers) to the representation of the class of objects above described; or of only allowing us the 82 Thirteenth Report of alternative of having portions of them well delineated while the rest is indistinct. Other difficulties attending Micro- scopical Photography have been pointed out in Mr. Hodgson’s paper, on which it is not necessary for me to dilate. In spite of these obstacles, I venture to prophesy that this beautiful art will flourish; for its want of universal appli- cability need not prevent its use in the numerous cases to which it is appropriate. The paper of the Rev. William Smith on the Stellate Bodies occurring in the cells of fresh-water Algze gives some further details of these plants, which may hereafter assist us in forming a more correct theory of their physiology. Our Secretary, to whom we have formerly been so much indebted for valuable contributions, has recently read a very interesting account of some observations he has made on the presence of a fungus, and of masses of crystalline matter, in the interior of a living oak tree ; a circumstance which does not appear to have been previously noticed, and which hardly admits of a satisfactory explanation in the present state of our knowledge. It is not, however, less worthy of record on that account ; for all sound theory must be based upon carefully- observed facts; and the first fact of a kind is at least as valuable as those which may hereafter follow it. The very large demand for first-class microscopes, which has increased rather than diminished during the past year, has stimulated the makers to use every exertion to extend to the utmost the apertures of their object-glasses. Messrs. Smith and Beck have produced a 4-10th inch of upwards of 90°, chiefly valuable for the examination of opaque objects. Mr. Ross has lately made some objectives of 1-8th inch focal length, and 155° of aperture, which, by permitting very oblique illumination, bring out the markings on the most difficult test objects in a highly satisfactory manner. Mr. ‘Wenham, in following up his experiments to ascertain the limits of useful aperture, has constructed a glass of 170°, and 1-12th inch focus ; but is still of opinion that nothing is gained beyond 150°. From a very brief examination of his object- glasses, I am inclined to differ with him, and to think that for the purpose of merely discovering the existence of very close lines or dots the aperture cannot be too great. For the useful application of the microscope to minute anatomy and physi- ology a much smaller aperture will suffice, which, from not requiring such careful adjustment, and such close proximity to the object, is far more convenient in use. When we consider that the real aperture of an object-glass is the chord of the angle at which light is admitted, and that the the Microscopical Society. | 83 chord of 170° is more than ‘996 of the diameter of a circle, we may be certain that if the extreme limit has not already been reached, its further extension will scarcely be appreciable. To correct the aberration of these glasses as far as possible, and to bring them to the neatness of definition that has been attained in those of more moderate aperture, must now be the aim of our scientific opticians. A very useful addition to the mechanical arrangements of the microscope has been contrived by Mr. Brooke. In former days, when our objectives were single lenses, it was usual to set four or six of them in a wheel, by turning which the power could be changed in a moment. Our present object- glasses, consisting generally of three achromatic combinations, requiring to be set in tubes of some length and thickness, cannot be compressed into so small a space. Mr. Brooke has, however, effected the same purpose to the extent of two powers. To the nozzle of the microscope an arm is screwed, projecting in front, and carrying a pin on which a bar revolves, to each end of which an object-glass is screwed, Either of these, by rotating the bar, can be brought under the body of the instru- ment, while the other is carried beyond the stage so as to be quite out of the way. Object-glasses of one inch and one- quarter inch mounted in this way are found to be very con- venient when pursuing microscopical researches; the one to take a general view, and the other a particular one, of the object under inspection. - Mr. Brooke also exhibited a neat little contrivance for con- verting a pocket eye-glass into a table microscope. ‘Two straight square pieces of brass are halved into each other, and the pillar on which the eye-glass slides screws into the inter- section, the straight pieces forming the foot. The whole makes a useful stand, and packs into something smaller than an ordinary spectacle-case. Mr. Ross has constructed a very comprehensive microscope- stand, furnished with right-lined and circular motions, not merely to the stage but to what may be called the sub-stage, or that part which carries the different illuminators for trans- parent objects. All these motions being effected either by pinions or screws, the various adjustments are made with great comfort to the observer. ‘The instrument is heavy, and the quantity of excellent work in it necessarily renders it somewhat costly. Messrs. Smith and Beck have adopted an improved method of attaching the object-glass to the body for the purpose of preventing the excentricity which is frequently caused by the imperfection of the screw. They have also carried the same 84 Thirteenth Report of principle into the construction of the eye-piece by attaching the cells to the tubes by cylindrical fittings. Here, Gentlemen, I would willingly conclude; but I have still the melancholy duty remaining of recording the death of three of our members, a duty from which my predecessor was last year happily exempted. Of Mr. Edward Stokes I had no personal knowledge ; but I have been informed that he was a zealous cultivator of science. | Mr. Dalrymple and Dr. Mantell have both left names which will not speedily be forgotten, and which merit a much more extended notice than it is in my power to give. John Dalrymple was the eldest son of William Dalrymple, a highly distinguished surgeon at Norwich, under whom he received the early part of his professional education. He afterwards studied at the University of Edinburgh, and in 1827 became a member of the Royal College of Surgeons in London, and settled in the city. In 1832 he was elected Assistant-Surgeon to the Royal Ophthalmic Hospital, and Surgeon in 1843. In 1847 he retired from that office on account of ill health, and was appointed Consulting Surgeon. In 1851 the Fellows of the Royal College of Surgeons elected him a Councillor, He published a work on the Anatomy of the Eye in 1834; and a splendid one on the Pathology of that organ he only just lived to complete. In fact, he revised the last number but a few days before his death. His style is clear and concise ; and the soundness and precision of his views, and the accuracy of his delineations, are universally acknowledged by the profession. In 1839 he removed from the city to the west end of London, where his practice in- creased, and latterly had become greater than was compatible with the state of his health. In addition to his own peculiar department of surgery, in which he had attained the highest eminence and the full confidence of the profession, he suc- cessfully prosecuted the delicate and interesting science of microscopical anatomy, both human and comparative. He was an original member of this Society, and one of our first council ; and he contributed a valuable paper ‘‘ On the Ar- rangement of the Capillary Vessels of the Allantoid and Vitel- line Membranes in the incubated Egg” to the first volume of our Transactions. Until illness obliged him to spend bis evenings at home, he was a frequent attendant at our meet- ings; and his remarks, when he took a part in our discus- sions, were characterised not less by clearness and precision than by the modest and gentlemanly tone in which they were delivered. | the Microscopical Society. 85 Soon after the death of Dr. Gideon Mantell a brief memoir of him appeared in the Athenzeum, from which I shall extract a few particulars. Although a member of the medical pro- fession, he was not a graduate in medicine, but derived his title from the degree of LL.D. conferred by a foreign uni- versity. He commenced his career as a general practitioner at Lewes; removed to Brighton in 1835, and to London in 1839, residing first at Clapham, and afterwards in Chester- square. He was naturally an enthusiast, and, gifted with quick observation, he would have distinguished himself in almost any branch of science. ‘Ihe accident of his position made him a geologist; for little was then known of the Wealden formation, or of the fossils which it contained. Sel- dom has an observer had a richer field for the exercise of his powers, and seldom has an opportunity been better seized. In the course of a few years he collected together a museum of specimens from the Wealden and the chalk which now forms a portion of the British Museum, the trustees of that institu-_ tion having purchased it for 5000/. His first paper, published in 1813, was on the organic remains discovered in the en- virons of Lewes ; and from that period almost to the time of his death his literary labours were unceasing ; for on the sub- jects of Zoology and Botany no less than sixty-seven papers and works have been enumerated. When it is remembered that during all this time he was pursuing the active practice of his profession, contributing papers to the medical journals, and occasionally writing on other subjects, we may form some idea of his indefatigable industry. Dr. Mantell had also the satisfaction of making known the important discovery, by his son, of the remains of the gigantic birds of New Zealand, of which he possessed many very fine specimens, and on which he wrote several papers. Of his talents as a popular lecturer I can speak from my own observation. Possessed of a rapid and even flow of appro- priate language, sometimes rising into eloquence, and being enthusiastically fond of his subject, he managed to inoculate his audience with the same enthusiasm, and therefore had no difficulty in keeping up their attention even when he tres- passed considerably beyond the accustomed hour. He was an occasional but not frequent attendant at our meetings. Permit me, Gentlemen, in conclusion to thank you for the kind indulgence with which you have received my very im- perfect endeavours to fulfil the duties of your President. Of their imperfection no one can be more sensible than myself; but at the same time no one can more sincerely desire the con- tinued prosperity of the Society, or strive more to promote it. 86 Thirteenth Report of the Microscopical Society. Resolved unanimously—That the Reports of the Council and Auditors be received; and that they and the President's Address be printed in the Transactions of the Society. The law relating to the election of officers was then read ; and the Society proceeded to ballot for the officers and four new members of council for the year ensuing. The ballot having been taken, the following were declared elected :— Officers. President: Wes ek. 2s GeEoRGE Jackson, Esq. Treasurers nic 98 4 N. B. Warp, Esq. Seorétarysds. 26. 24 JoHN QUEKETT, Esq. Assistant Secretary. . Mr. Joun WI iis. New Members of Council. W. Gitiert, Esq. Joun Les, Esq., LL.D. Rogert WaArineTON, Esq. F. H. Wenuam, Esq. In the room of M. S. Leae, Esq. M. Marsuatt, Esq. ALFRED Ros.ine, Esq. J. B. Stmonps, Esq. Resolved unanimously—That the thanks of the meeting be given to the President, Treasurer, Secretary, and Members of Council, for their services on behalf of the Society during the past year. | b ABE) On the Minute Structure of a Species of Fausastna. By Pro- fessor W. C. Wittiamson. Communicated by Matthew Marshall, Esq. (Read June 22, 1851.) In the last memoir on the Foraminifera which I laid before the London Microscopical Society, I pointed out the existence of a curious system of tubes and canals, penetrating the parietes and septa of several species of Foraminiferous shells. In Polystomella crispa these chiefly presented themselves in the form of large canals passing through the calcareous umbilical regions. In some species of Nonionina and Amphistegina they existed as a dense network of minute canals, having their external orifices at the peripheral margins of the discoid shells. In the latter examples the canals were of small diameter, and their use in the economy of the living animal very dubious. On making a number of sections of a species of Faujasina (D’Orb.) from Manilla I discovered the existence of a much larger and more interesting arrangement of tubes than any that I had previously seen. ‘This shell is constructed on the inequilateral plan of the common Truncatulina tuberculata. Its inferior surface is flat, the corresponding extremities of the segments being arranged on a nearly uniform plane. As successive convolutions have been added to the antecedent ones, they have assumed the arrangement of a series of hollow cones placed over one another, the additions to the length of each new segment being confined to its upper extremity. Hence, whilst inferiorly all the convolutions are visible, on the upper surface we only see the outermost one presenting the aspect of a truncated cone. Fig. 1, Pl. X., is an enlarged representation of the lateral appearance of the shell, viewed as an opaque object. Whilst the vertical septal lines (1 d) are translucent, the intervening parietes of the segments (1 9), in which the minute foramina exist, is of an opaque gray colour. The inferior peripheral margin (1 f), and its continuation at the flat inferior surface, constituting the spiral septum (fig. 2 ¢) separating the con- volutions, exhibit the same translucent aspect; as does also the truncated apex of the cone (1 d'), towards which all the vertical septa converge. In nearly all the Foraminifera a translucent line appears to mark the existence of a subjacent septum. The segments, which do not extend to the summit of the shell, communicate with one another by one very ee oral aperture (1 e). Along each of the vertical septal lines (1 d) there exists an irregular double row of very distinct pits or depressions (fig. 6 f). Similar pits are seen inferiorly in the radiating septa VOL. I. h 88 WILLIAMSON on Faujasina. which divide the different segments of each convolution (fig. 2 b andd), but they do not occur in the peripheral margin (1 f and 6 e), or in the spiral septum (fig. 2 e). At the upper ex- tremity of the shell similar, but larger, pits are seen both on the flat truncated surface (1 da’) and on the sides intervening be- tween it and the upper portions of the segments (6 6). On making a series of sections of the shell we learn that these pits are the external orifices of a curious system of intra-septal canals and spaces, ramifying in its interior. Fig. 2 represents a thin superficial section of the inferior flat surface, viewed as a transparent object. _Thus examined, the conditions are reversed. ‘The foramina in the parietes of the hollow segments tend to intercept the light and look dark, whilsti'the solid calcareous septa are translucent and transmit it freely. ‘This section was made a little below the peripheral margin and parallel with the points a,a in fig. 1. The walls of the segments (2 a) exhibit the ordinary forami- nated aspect, and the segments themselves are arranged in the usual spiral manner. The spiral contour is lost in the centre of the section, owing to the circumstance that it there becomes very thin, and passes under the central cells which are placed a little above the level of those which surround them. In the radiating septal lines are seen numerous small orifices (2 b), which open by means of short canals (fig. 5h, h’) into the interseptal spaces immediately above them. As already observed, these orifices do not exist in the spiral sep- tum (2 e), but here and there even this superficial section ex- hibits traces of deep-seated canals passing through the septum and uniting the orifices belonging to contiguous convolutions (2.c). In this portion of the shell the apertures are usually in single rows ; but towards the exterior of the outer segments we sometimes see them arranged in pairs (2d). It is of course the external surface of the base of the shell that is re- presented in the drawing. On making a second section parallel to the last, but a little above the peripheral margin, in the plane of the points 1 4, d, we have the appearance presented by fig. 3. The drawing represents this section as seen when viewed in the opposite direction to the last, viz. looking at its upper or inner surface, and towards the base of the shell—some of the foraminated parietes of which are still preserved. We now perceive that there exists a number of large branch- ing intra-septal tubes and passages, which commence at the innermost segments and proceed in a radiating manner towards the periphery. As each of these tubes emerges from the septum separating two contiguous segments, and reaches the spiral one intervening between two convolutions, it exhibits a WILuraAMson on Faujasina. 89 marked tendency to divide into two branches (fig. 3a, 6), one of which is usually ina plane a little above thefother. On tracing back these tubes as they proceed from the outermost to the inner convolutions, we perceive that the bifurcations, which at one time marked the outer extremities of each series, serve two purposes: they are designed, primarily, to multiply the number of the external orifices ; but in addition to this, they subsequently facilitate the establishment of a free communica- tion hetween the internal intra-septal spaces and those of the newer convolutions, in which the septa are much more nu- merous ; but though a lateral divergent communication is thus maintained, I have only seen one instance in which a direct lateral communication was established between two transverse septa of the same convolution, parallel with the spiral septum. The exception is seen at fig. 3c. In this respect the species under consideration differs materially from the forms described in my preceding memoirs. The small circular apertures which appear along the course of these tubes, mark the points where the section has traversed the orifices of the canals descending to the inferior surface of the shell. Fig. 4 represents a third section made across the points fig. lec. This section has cut through the shell a little above the superior extremities of the cells belonging to the central convolutions ; a few of those belonging to the second spiral being seen at 4a. The outermost convolution, on the other hand, has been intersected across its large oral (?) apertures (fig. 1 e), revealing the nature of the connection (40) that exists be- tween contiguous segments. We now see that the portions, which in the section fig. 3 had the appearance of large radiating tubes, are really the lower borders of vertical intra-septal spaces (fig. 4 ¢ c’), which also give off true divergent cylindrical canals from their external margins, pene- trating the thick parietes of the shell. These spaces extend from the top to the bottom of each septum, and only assume the form of canals when they approach the peripheral shell walls. The connecting branches which unite the spaces of different convolutions (fig. 3 5) are also tubular. The septa of the second convolution in this section exhibit similar intra-septal spaces (4 d), which communicate exter- nally, as just described, with those of the outermost convo- lution, and also open internally into a large and very irregular central cavity (fig. 4 e and 5q). The true nature of this cavity will be better understood on referring to fig. 5, which repre- sents a vertical section of this instructive object, passing nearly through its centre. I am not quite certain whether it has actually traversed the primordial cell, but if not, it has cer- h 2 90 WILLIAMSON on Faujasina. tainly crossed the second one (see fig. 3), which is seen at a, along with four others, 6, c, d, and é, in the order of their suc- cessive development. "Whilst their inferior portions of the seg- ments are nearly on an uniform level, the upper extremites of those belonging to successive convolutions become rapidly elongated, leaving between them a large, irregular, conical space (fig. 5 g, g), the inverted apex of which rests upon the most central segment (5 a) and communicates with the inferior surface by means of the canals fig. 5’. Similar canals are also seen at 5 h, passing upwards into the inter-septal spaces ; whilst at 572’, corresponding ones proceed inwards through the respective septa of the cells c and d—in the translucent walls of the latter of which their direction, and the extent of the inter-septal space may be traced. I have not in any one instance found these spaces, or their divergent canals, communicating with the interiors of the seg- ments, though at the first glance many of them appear to do so, as is the case with the inner margin of the large segment fig. 5d. But from the examination of a considerable number of sections, [am satisfied that where such an appearance exists, it is either the result of an accidental fracture or an optical illusion; and that the only direct communications existing between the two parts of the organism, are through the pseu- dopodian foramina, many of which open into the tubular por- tions of these passages (figs. 3d and 4f); but never, as far as I have observed, into the intra-septal spaces. But the section now under consideration, in common with several of the others just described, presents a new and curious feature. The cavities in the translucent calcareous shell are thickly lined with a dark olive-brown substance, apparently the residuum of the soft animal. ‘This substance not only exists in the interior of all the segments, closing up the oral aper- tures, as at 5 f, but also occupies the intra-septal spaces and their respective canals, as well as the irregular cavity in the umbilical centre of the shell. If this substance is really the desiccated soft animal—and of this we should not have enter- tained a doubt, had it existed only in the interior of the seg- ments—it is evident that in this species the gelatinous tissue has not only filled the true chambers but has also occupied the intra-septal canals and passages. The specimen from which the section, fig. 4, was prepared, exhibited the same appearance, and traces of it oecut in all; hence it appears most probable that this brown substance is really the desiccated soft animal. If this should prove to be a correct conclusion, it is curious that the only medium of communication bétween the soft tissues inhabiting the spiral segments of the shell and those ~ Witaramson on Faujasina. | 91 occupying the intra-septal and central passages, should have been the minute pseudopodian foramina. ‘The structure is so very different in this respect, from anything that has been previously observed, that I am afraid to speak with too much certainty on the subject, though I entertain but little doubt respecting it. On examining the external contours of young examples of this species, we ‘often find the apex occupied by a deep and irregular depression, surrounded by the projecting upper extremities of the segments constituting the external convolu- tion. This depression, which is really identical with the irregular central cavity (fig. 59,9), subsequently becomes arched over by a calcareous layer (fig. 1d), derived from the upper portions of the newer convolutions. The roof thus formed is perforated by large apertures (fig. 65), through which a free communication is maintained between the external medium and the enclosed space. The nature of the latter varies considerably. Sometimes it exists in the form of a large irregular cavity, as already described, and at others as an intricate network of large canals. ‘The character of the external orifices also varies. In some examples they are large and patent, as in fig. 66; in others, numerous smaller tubes, ascending from the subjacent network, converge at some super- ficial depressions which occupy the position of the larger orifices. Fig. 6 represents a thin superficial section made in the plane of the oblique sides of the conical shell and exhibits three septa (6c), with the large orifices of their intra-septal canals (6 f), part of the external parietes of four segments (6d), densely perforated with minute pseudopodian foramina, part of the inferior peripheral margin (6 e), and a small lateral portion of the dome-like apex of the shell (6a). The preceding facts are sufficient to show that the subject of this brief memoir presents a very different structure from any of the Foraminifera hitherto described. Whether or not my supposition as to the probable occupation of the intra- septal canals and spaces by the gelatinous soft animal be established, it is obvious that this organism supports the con- clusion at which I arrived in a preceding memo1, viz. that the soft animal had the power of extending itself externally far beyond the limits of any individual segment, and would thus be able to secrete calcareous matter in other situations than the mere parietes of its own segment. It is only in this way that we can explain the production of the dome-like covering which encloses the central umbilical cavities and their ramifying canals. But if it should be ultimately proved that the soft tissues have occupied all these irregular cavities, we shall then have a form of organization which, from its great variability 92 Wixiramson on Faujasina. of contour, will approach much more closely to the calcareous sponges than any hitherto described. I am well aware that, to many, these dry details will appear unnecessarily and tediously minute; but it must be remem- bered that, until we are accurately familiar with all the lead- ing types of structure existing in this interesting group of organisms, we cannot be in a condition to arrive at final con- clusions respecting their nature and zoological position. Manchester, May 21st, 1851. Notice of a Diatomaceous Earth found in the Isle of Mull. By Witttam Grecory, M.D., F.R.S.E., Professor of Chemistry in the University of Edinburgh. Communicated by Pro- fessor Joun E. Quexetr. (Read March 23rd, 1853.) , Tuts earth was discovered, about two years ago, by the Duke of Argyll, who gave a short account of its geological position to the Royal Society of Edinburgh. It constitutes a bed, resembling marl in appearance, lying in a rough piece of ground, at Knock, near Aros, between Loch Baa, a fresh-water lake, 3 miles long and 1 mile broad, and the sea. The lake is about 30 feet, the land about 40 feet, above the sea-level, and the lake is surrounded with high mountains on all sides except the west, where its waters flow towards the sea, passing through the rough district, boggy in parts, above mentioned, which is about a mile broad. The marl-bed, as it is called on the spot, lies within 50 yards of the lateral granite rock, and half-way from the lake to the sea. The surface of the land between the lake and the sea is very uneven, covered with large stones, gravel, and sand. At one part there is a hollow, which in winter used to become a small loch, in summer only a stagnant pool, and in draining this the bed of marl was discovered. It was filled in summer by a small stream unconnected with the lake. The bed rests on the gravel, which again rests on the granite of which the whole district is formed. As there is no formation of an epoch be- tween those of the granite and of the gravel, we cannot, from | its position, ascertain precisely the geological period at which the bed was deposited. The Duke of Argyll regards the gravel as belonging to the Diluvium, and the Infusorial de- posit as comparatively of very recent origin. But there is reason to think, from the character of the species, that the deposit may belong to a more remote epoch. Ehrenberg, to whom I sent a portion of it, writes to me, that he thinks it probably connected with the Tertiary, or at all events, with “ GREGORY on Diatomaceous Earth. | 93 the Quaternary period, but he had only been able to make a partial examination of it at the time he wrote. This deposit must not be confounded with the Leaf-bed, also discovered in Mull by the Duke of Argyll; for that bed, which also contains a large number of Diatomaceous remains, occurs at a place 20 miles from the deposit now under con- sideration, and is found between two beds of volcanic trap, showing that the Dicotyledonous trees—remains of which abound in it—must have lived before the eruption which gave rise to the upper trap-bed, whatever may have been the period of that eruption. To return to the Infusorial deposit. The Duke of Argyll thinks it possible that the waters of Lock Baa, which now pass to the sea at a distance from the deposit, may, at one period, have flowed through the hollow where the deposit is found. Mr. Campbell Paterson, a gentleman residing on the spot, thinks that the sea at one time communicated with Loch Baa, and that the present barrier is the result of some geolo- gical change or convulsion. The gravel and sand, he says, exactly resemble those now forming in the neighbouring sea ; and although he has not observed any marine shells in the gravel, he thinks that the rocks at a higher level bear marks of the action of the sea. ‘These are points on which I cannot speak without a personal knowledge of the locality, but the deposit appears to contain only fresh-water organisms. The Duke of Argyll kindly gave me a small portion of the earth first discovered, which happened to be very pure, and which he stated to contain Naviculacee. On examining it, | was struck with tle variety of forms, and resolved to study it more closely ; this I have only been able recently to do, and I think the results may prove not uninteresting to the Micro- scopical Society. The Mull earth is, in the purest specimens, when dry, almost white, and much resembles chalk, being light, friable, and adhering to the fingers. But more commonly it has a pale fawn colour, and it is frequently strongly tinged with iron. The lightest and whitest specimens contain hardly anything besides siliceous organic remains, for the most part entire, but with some fragments. Other portions, which are denser, contain also many fragments of quartz of various sizes, and vast numbers of comminuted fragments of lorice. In the densest and worst, the quartz or sand and the fragments en- tirely predominate, and these can hardly be cleaned. ‘The specimens of middling quality, as well as the inferior ones which I at present possess, contain a great many minute fragments of lorica, often exceeding half or three-fourths of 94 GREGORY on Diatomaceous Earth. the mass. These ‘fragments form an excellent polishing powder, which may be had of various degrees of fineness. I find it best, except in the case of the very purest specimens, first to ignite the earth over the spirit-lamp in a platinum capsule, till the black colour first caused by the action of the heat on the organic matter present is burned off, and the earth is again nearly white. I then digest it for some hours in strong nitromuriatic acid, which removes the iron, and, after washing away the acid, press the lumps in water gently with the finger till the whole is diffused in the water. It is then elutriated as usual, to separate on the one hand the coarse sand, if any be present, and, on the other, the com- minuted fragments. The slides now offered to the Society were prepared in this way from earth of but middling quality, my supply of the purest having been very small and long ago exhausted ; while the deposit being at present, and for months past, flooded, it is impossible to procure a fresh supply of the purest earth. In endeavouring to identify the species present in ists earth, I found the greatest difficulty from the want of any work containing figures of all the known species. The only figures I could procure were those of Ehrenberg’s Atlas, 1838, and those of the last edition of ‘ Pritchard’s Infusoria.’ The former, of course, does not contain the very numerous species added to the list since 1838, and the latter has sel- dom more than one or two species in each genus. I had also Kiitzing’s ‘Species Algarum,’ without any figures. But I was able, after studying a good many slides of excellent quality, to distinguish somewhere about 65 forms, although I could not with any confidence name above one half of the number, Under these circumstances, I ventured to apply to the Rev. W. Smith, to whom I was fortunately able to send an excel- lent specimen of the earth. That distinguished naturalist had the very great kindness, in spite of his absorbing occupa- tions, to examine the earth, and to send me the following list of species which he has detected in the specimens sent. The names are those adopted in his forthcoming synopsis :-— Pinnularia major Pinnularia gracilis ‘5 acuminata + lata its oblonga ap alpina p viridis Navicula serians fr divergens nm rhomboides oe acuta £ ovalis ¥ radiosa ig dicephala S| mesolepta eA firma — st interrupta geese angustata * Tabellaria Gomphonema acuminatum a gibba 3 cruciatum GREGORY on Diatomaceous Earth. | Q5 Gomphonema Vibrio Himantidium gracile, Kutz. - capitulatum a bidens, W. Sm. Amphora ovalis * pectinale, Kutz. Stauroneis Phoenicenteron > arcus, Kutz. e gracilis af major, W.Sm. if linearis undulatum, Ralfs. anceps Tabellaria frustrata, Kiitz. Gymatopleura elliptica 2 ventricosa, Kutz. 3 apiculata Epithemia turgida Cocconeis Thwaitesii * gibba Bs Placentula ~ EKunotia gracilis Surirella Brightwellii » retrorsum ‘~ biseriata ; ,Wiadema Cymbella Helvetica Synedra capitata ee maculata os A Ice pS e sativa Fragillaria capucina, Kutz. ms affinis Orthoseira viridis, W. Sm. ™ cuspidata ing ouchalcea, W. Sm. It will be perceived that Mr, Smith has found, in the speci- mens sent to him, 59 species of fresh-water Diatomacee. As I] had made sketches of all those forms which I could not name, I was easily able to identify Mr. Smith’s species. I have stated that I had distinguished about 65 forms. I believe that some of these were side-views of species un- known to me at the time, and others, in all probability, accidental varieties. But I also think it probable that there may be a few species in the deposit which do not occur in the portion seen by Mr. Smith. At least, I am quite certain that that portion differs remarkably in some points from that which I had under examination at the same time. For ex- ample, in Mr. Smith’s specimen, of which he kindly sent me two slides as I had not tested it myself, I find that there are numerous and fine lorice of Epithemia turgida—a species which I had indeed observed in mine, but which I had found remarkably scarce. I have reason to think that hardly any two specimens will be found exactly to agree, and it is quite natural that different parts of the deposit should differ in the prevailing forms. Among the forms which I thought I had observed, but which Mr. Soa iedad) caoiindest with, are Melo- siera distans, and possibly MM. nummuloides ; Eunotia Triodon, and EL. Pentodon; possibly E. fabra, and one or two more. But most of these, if they do occur, are very scarce ; and therefore I do not venture to add any names to Mr. Smith’s list until I shall be confirmed by him or by some other experienced authority. There are several other forms, also doubtful, which I thought I had seen, but I need not name them. The Mull earth is characterised by several peculiarities. _ First, by the abundance of very fine specimens of the Navi- 96 GREGORY on Diatomaceous Earth. culacez, especially of the genera Pinnularia (14 species), Navicula (6 species), and Stauroneis (4-species). There are many splendid individuals of Pinnularia major (some 1-50th of an inch in length), oblonga, virides, divergens, and others ; and a few, but these very fine ones, of. P. data, and of the rare and beautiful P. alpina. Navicula rhomboides and N. serians are particularly frequent and fine, as is also Stauronets Phenicenteron. 2ndly. It is characterized by the abundance of Cymbelle of which there are 5 species. drdly. There is a remarkable development of the Eunotie, as LHunotia Tetraodon, E. Diadema, Himantidium Arcus, H. bidens, and the 4 other Himantidia and Epithemia turgida. Athly. There is a great abundance of Tabellaria fenestrata in every stage of development, some specimens being 10 or 12 times as long as others, but not broader, and of T. ventricosa which, how- ever, occurs almost always short. OSthly. There is a remark- able abundance of fine specimens of Gomphonema coronatum, and fine individuals of G. acuminatum also occur. ‘The genera Amphora, Cymatopleura, Cocconeis, Surirella, and Nitzschia occur less abundantly, and in some cases are very scarce. Fragilaria capucina, Kiitz., Orthoseira viridis, W.Sm., and O. ouchalcea, W.Sm., are abundant, as is Synedra biceps. I have observed the variety 6 recta, Kiitz., of this species. Besides the 59 species named by Mr. Smith (and I would again remind the Society that the names in the above list are those of Mr. Smith’s daily expected Synopsis), there is one form, to which I directed his attention, and which he cannot with certainty refer to any known genus. This form is abundant in all specimens of the earth, and is therefore an additional characteristic of it. It varies from 1-600th to 1-470th of an inch in length, and has usually the form of a plano convex lens, with two notches near the ends of the plane or very slightly concave side. It is broadest in the middle, and has sharp apices (fig. 1). At other times the apices are less sharp and the ends broader (fig. 2). It is finely cross striated, and Mr. Smith has ascertained the number of strie to be 44 in 1-1000th. It requires a very good glass to make out the striz, and it 1s possible that this form, from its abundance in the Mull earth, may be found available as a test object. For a long time I could not make out the striz (although I felt sure of their existence from the resemblance or aspect to other forms known to be striated) with a glass which had sufficed for all the other forms. But with a first-rate object glass, and good management, the striz may be shown and counted. It is possible that this form GreEGoRY on Diatomaceous Earth. | 97 may be an immature one, but to what are we to refer it? It differs from Himantidium Arcus and Eunotia gracilis in the number of striz, and Mr. Smith thinks it must stand near Eunotia Arcus, Kitz. Navicula Arcus, Ehr. It is not, how- ever, that species, nor is Mr. Smith sure that it is of that genus. He is to examine it more fully, and the matter is therefore in good hands. I may add, that while it has a general resemblance to small specimens of Himantidium Arcus, or of other allied species, it does not commonly occur where these are abundant. I have looked at a number of Diatomaceous earths, in many of which there were all the common species of Hunotia and Himantidium, but have only seen this form in one, namely, in a slide prepared by Mr. Topping, and labelled ‘‘ from the banks of the Spey.” This slide has many things in common with the Mull earth. Any of the slides sent with this paper will exhibit numerous examples of this form. I have further to add, that an average specimen of the Mull earth, on being analysed, was found, after being dried at 212°, to be composed of — Silica ~ - - - - - 70°75 Protoxide of iron, containing traces of phosphoric acid and manganese - — - - - 18°04 Organic matter = - = - - - 12°36 Loss, chiefly water - - - - Ue 5) 100-00 The iron is here stated as protoxide, but if calculated as peroxide, would amount to 16°69 per cent. Some of it cer- tainly is in the latter form from the action of the air, and the brown colour, and this diminishes the loss, but I have stated it as protoxide, because I believe it to be in that state before the air has access to it. ‘The presence of phosphoric acid, which was easily detected in the oxide of iron, by the use of molybdata of ammonia, is interesting. It is most probably derived from the organic matter of the Diatomacee, but I am not aware that its presence has been yet ‘observed in any in- fusorial earth. Ihave not determined the proportion of phos- phoric acid, which, although small, is appreciable. The earth contains neither lime nor magnesia. It is probable that this earth may be useful as a manure from the finely divided silica, the organic matter, and the phosphoric acid it contains. Professor Bailey ascribes the fertility of certain districts in America to the abundance of infusorial remains on the soil, so that the experiment is worth trying. 98 GREGORY on Diatomaceous Earth. I find I have omitted to notice that, besides the Diato- maceous organisms, the Mull earth contains abundance of the long spicules, and also of the gemmules of Sponyilla fluviatilis and S. lacustris, also a considerable number of siliceous forms, apparently Phytolitharia, more particularly Lithostylidium clepsammedium, and similar forms. ‘There are also some silicified forms much resembling certain deposits in the cuticle of Graminee, &c., besides occasionally silicified pollen grains, belonging both to grasses, and as I believe to Conifer. I have also seen some fragments of woody fibre and cells, probably silicified ; but I have not the means of determining with any accuracy these various organisms. Probably many members of the Society will be able easily to do this. I think I have seen some forms which resembled very much the Desmi- diaceze, such as Huastrum, Staurastrum, and Cosmarium; but on these points I will not venture to assert anything, although, as Desmidiacez occur in flint, and often contains a little silica, this occurrence is possible. In conclusion, even the imperfect examination to which the Mull deposit has been subjected, proves it to be richer in Diatomaceous species, and I think also in genera, than any other known deposit, so far as I am acquainted with them. I have heard that the deposit at Santa Fiora contains 39 species, and that found near Peterhead, and described by Dr. Dickie, contains 40, but I know of no others which equal these two, whereas in the Mull earth we have at least 60 species and 16 genera. ‘This will of course be interesting in reference to the geographical distribution of fossil Diato- macee, and I may add that Ehrenberg, who is preparing to publish a great work on this part of the subject, has been very much interested in the Mull earth, as being the first he had been able to obtain from the Hebrides, and thus filling up a great blank in his work. It is not, however, the first that has been discovered in the Hebrides, as there is a Diato- maceous earth at Raasay, also in the Hebrides. This I have not yet examined, but I presume it has been described. I beg to offer to the Society a few slides made, as I have stated, from a specimen of only middling quality, such as alone has been in my possession of late, and also a specimen of earth, not yet examined, in its natural state, which may possibly turn out good. I have added a portion of prepared earth in water, which cannot be cleaned from quartz fragments, but certainly contains a good many fine examples of the rare and beautiful Pinnularia alpina. . The subjoined figures are rough sketches of the doubtful Grecory. 0% Diatomaceous Earth. | 99 form in the Mull deposit. They are represented with a power of 400 diameters. I a : find the length to vary from 1-470 to 1-600 of an inch. There are, as Mr. Smith first ascertained, 44 striz in 1-1000 of an inch. It always exhibits the two notches towards the ends of the plane or slightly concave side. Fig. 1 is by far the most usual form; fig. 2 is, however, not unfrequent. The form is very abundant in the Mull deposit, and I have only seen it in one other, also from Scotland, namely in a slide labelled ‘“‘ From the banks of the Spey,” which, J had from Mr. Topping: Himantidium Arcus, which, when small, has some slight resemblance to the above form, has only 22 strizin 1-1000 of an inch and its striz are consequently, ceteris paribus, quite easily seen, when those of the doubtful form cannot be made out. Mr, Smith thinks its place must be near Hunotia Arcus, Kiitzing—Navicula Arcus, Ehr.; but that it cannot be referred to that species. Indeed it is only very immature specimens of EH. Arcus (Kiitz.) that at all resemble this form, since the mature /. Arcus (Kiitz.) has a bend or rounded angle in the middle. The doubtful form may be an immature one, but what is its aspect when mature ? On the Binocular Microscope, and on Stereoscopic Pictures of Microscopic Objects. By Professor C. Wueatstong, F.R.S. Communicated by Dr. Lankester, F.R.S. (Read April 27, 1853.) In Section 11 of my first Memoir on Binocular Vision, pub- lished in the Philosophical Transactions for 1838, I have alluded to the illusions to which microscopic observers are liable, from their inability to judge correctly the relief of objects when one eye only is employed. This indetermination of the judgment exists whenever a shadowless object is re- garded with a single eye. Frequently an elevation appears as a depression, a cameo as an intaglio, a hollow pyramid (as a crystal of muriate of soda) as a pyramid in relief, &c., and vice versa; but this indecision is entirely removed when the object is viewed with both eyes simultaneously. No mistake, if the object be a near one, can then be made with regard to t % 100 Wueatstone on the Binocular Microscope, &c. its relief; and the relative positions of every point, in depth as well as in length and breadth, can be correctly determined. The stereoscope affords a convincing proof that the two pro- jections of an object presented to the two eyes, suggest the real object far more effectively to the mind than a single projection to one eye does; and those who have paid much attention to the ap- pearance of binocular pictures in the stereoscope, will not have failed to remark, that not only is double vision of importance to enable us more accurately to judge of the relief of bodies, but it also occasions us to perceive things which pass entirely unnoticed when monocular pictures alone are regarded. Fully impressed with these views, and convinced, from the reasons above stated, that a binocular microscope would possess great advantages over the present monocular instrument, I, shortly after the publication of my first memoir, called the attention both of Mr. Ross and Mr. Powell to this subject, and strongly recommended them to make an instrument to realize the anticipated effect ; their occupations, however, pre- vented either of these artists from taking the matter up. The year before last, previous to the publication of my second memoir, I again urged Mr. Ross, and subsequently Mr. Beck, to attempt its construction, and for a short time they interested themselves in the matter, but ultimately relinquished it for want of time, and in my opinion over-estimating the difficulties of the undertaking. It appears, however, from a communication in the ‘ Ame- rican Journal of Science’ of January, 1853, which has been reprinted in the last number of the ‘ Microscopical Journal,’ that such an instrument has been actually constructed by Professor J. L. Riddell of New Orleans, and the results expected have been obtained. ‘The method Mr. Riddell employs is similar to the one I recommended to Mr. Beck. After the rays from the object pass through the compound object-glass in the usual manner, he deflects them by means of a system of rectangular prisms into two directions parallel to the original, and suff- ciently separated for the images to be seen by each eye. As in this arrangement there must be a considerable loss of light, I have proposed another which will not have this disadvantage, and which I will shortly submit to the Society. A binocular microscope is, however, by no means a novelty, and its invention dates nearly two centuries back. I have found, in the library of the Royal Society, a work entitled ‘La Vision parfaite, ou les Concours des deux Axes de la Vision, en un seul point de V’Objet. Par le P. Cherubin d’ Orléans, Capucin” This work was published at Paris in 1677, and in it eight chapters and a plate are devoted to a Wueatstone on the Binocular Microscope, &c. 101 minute description of the instrument, which he informs us he constructed, and presented to the Dauphin. The following is an extract from the Preface :— “< Some years ago I resolved to effect what I had long before premedi- tated, to make a microscope to see the smallest objects with the two eyes conjointly ; and this project has succeeded even beyond my expectation, with advantages above the single instrument so extraordinary, and so surprising, that every intelligent person to whom I have shown the effect, has assured me that inquiring philosophers will be highly pleased with the communication. For this reason I have determined to make it the principal subject of the present work.” And the second part, which contains a description of the in- strument, is thus headed :— ** Section the first, in which is taught the method of constructing a newly-invented microscope to see the smallest objects very agreeably and conveniently, represented entire to the two eyes conjointly, with a magni- tude and distinctness which surpasses everything which has been hitherto seen in this kind of instrument.” In the Pere d’Orléans’ binocular microscope, two object- glasses have their lateral portions cut away so as to allow of close juxta-position, and these nearly semi-lenses are so arranged, that their axes correspond with the two optic axes passing through the tubes containing the eye-pieces.. The author’s aim in its construction was solely the reinforcement of the impression by presenting an image to each eye, for he assumes, according to the then prevalent error, that vision by the two organs conjointly is naturally and necessarily unique, from the perfect conformity of all the homonymous parts of the two images of the object on the two retine. The real ad- vantage of such an instrument entirely escaped his attention ; viz., that of presenting to the two eyes the two dissimilar microscopic images of an object, under precisely the same cir- cumstances as the two unlike images of any usual object is presented to them when no instrument is employed, by which simultaneous presentment the same accurate judgment as to its real solid form, and the relative distances of all its points, can be as readily determined in the former case as in the latter. In the construction of a binocular microscope there is one thing especially to be attended to—viz., that the images be both direct, for in this case only a true stereoscopic representation will be obtained. If the images, on the contrary, be inverted, a pseudoscopic effect would be produced which will give a very erroneous idea of the real form. The reason of these effects is fully explained in Sections 5,10, 22, 23, of my Memoirs. The reversal of the images by reflection from mirrors or reflecting prisms, will produce the same result as to the stereoscopic and pseudoscopic appearances as their inversion by lenses. The binocular microscope constructed by the Pere d’Orleans was SO anal ate 102 Wueatstone on the Binocular Microscope, &c. pseudoscopic, though he describes one which, had it been made, would have been stereoscopic; he was, however, quite unaware that there would be any difference of this kind between them. ‘The pseudoscopic effects when inverted images are presented, and the natural appearances when erecting eye- pieces are employed, have not escaped the observation of Mr. Riddell. Besides actual inspection by means of the binocular micro- | scope, there is another way in which the advantages of bino- cular vision may be applied to microscopic objects. The beautiful specimens of photography, reproducing the highly magnified images of objects, inserted in a recent number of the Microscopic Journal, makes one regret that they were not accompanied by their stereoscopic complements. A very simple modification of the usual microscope would fit it for producing the two pictures at the proper angles; all that is necessary is to cause the tube of the microscope to move inde- pendently of the fixed stand round an axis, the imaginary pro- longation of which should pass through the object. A motion of 15° would include every difference of relief which it would be desirable to have, and it is indifferent in what direction this motion is made in respect to the stand. ‘The pair of stereo- scopic pictures may be obtained by a still simpler method, which requires no alteration in the microscope ; the object itself may be turned round on an imaginary axis within itself, from 7° to 15°. But this method is inapplicable unless the light be perfectly diffused and uniform so as to avoid all shadows, the presence of which would give rise to false stereo- scopic appearances. In the former case, where the object remains stationary and the tube moves independently of the frame, the arrangement of the light so as to cast single shadows might be an advantage, and assist the visual judgment. DESCRIPTION OF THE PLATES. The letters throughout have the same signification :—a, trochal disc ; b, body ; ¢, tail of peduncle; d, mouth; e, pharynx; f, “‘ yellow mass ;” g, gizzard; h, “‘pancreatic sacs;” 7, rectum; #4, anus; J, ovary; m, water-vessels ; n, ganglion; 0, ciliated sac; p, upper circlet of cilia; p/, _ lower circlet of cilia; 7, vacuolar thickenings. PLATE I.—JZLactrularia socialis. mA 09 OMOIAD NBO De . A single individual from the side. Lateral view of the trochal disc. . Trochal disc from above. . Aperture of the mouth—ciliated sac and ganglion. . Animal retracted. . Armature of the gizzard, viewed laterally. . Termination of a water-vessel in the trochal disc. . Water-vessel much magnified, showing the long flickering cilium. . A portion of the ovary much magnified, showing the germinal vesicles with their spots scattered through its substance. 10, 11. Stages in the growth of the ovum. 12-18. Stages in the development of the embryo. 19, Spermatozoon ? PLATE II. 20. A portion of the ovary undergoing the change into an ephippial ovum. 21, 22. Ephippial ova, the latter having its contents divided into two portions. 23. Ephippial ovum burst. 24. Its contents. 25. Muscular fibre—relaxed, a; contracted, 0. Melicerta ringens. 26. Viewed laterally. 27. From the ganglionic side. 28. From the mouth side. 29, Extremity of the calcar, showing its apparent closure and the bundle of cilia. Brachionus polyacanthus. 30. Viewed laterally. 31. From the mouth side. 32. From the ganglionic side. 33. From above. Philodina, sp. ? 34. Trochal disc from above. , laterally. 36. From the mouth side. 37. From the ganglionic side. PLATE III. The Diagrams illustrate Mr. Huxley’s paper of Adult Rotifera, and of Larval Annelids and Echinoderms. Fig. 1. Raphides from Cactus enneagonus, showing a nucleus surrounded by concentric lamine. 2. The same, with irregular lamine. 3 & 4, The same, without concentric lamination. 5. Nuclei of raphides. 6. Separated crystals of compound raphides. Trans ee FLT w Sy, ) Syn » eae sili : wlll Ml es T Horley, del. Tuffen West ,sctilp Ford & West, Imp. 54) Hatton Garden. LACINULARIA Ae ihe ee. % lee Trans. Soir Soe. PLM T Hetey del. Tuffen West , sculp. Ford & West, inp 54,Hatem Carden Pa ew ARIA BI MELICERTA, €C. BRACHIONUS. Dy Poi ODINA. Sines ae ie i Grant Noor: te LL Lacinularia. Melrcerta Philodina Brachionis Stephanoceros Larval Annelids & Echinoderms. if ia ‘Tutten West, scaip. Ford & West, Emp 54 Hatton Garden ‘ a ag # airs) <4 g 4 ¥ Fa well ‘ ; meek \ A - ‘ = ¥ - . 1 £ DESCRIPTION OF PLATE IV. On a Cyst upon the Olfactory Nerve of a Horse, by J. B. Simonds, Esq. a 1. The cyst containing a crystal of oxalate of lime.—a, Bell-shaped spot in interior of cyst.—b, A moveable mass of granular matter. On the Development of Tubularia indivisa, by J. R. Mummery, Esq. 16, 17. Fully developed head of Tubularia indivisa, loaded ) repro- ductive capsules. 13. Newly-formed head. 14, The same, showing arrangement of ovaries. 12. Internal surface of head (the oral tentacles removed), exhibiting twelve lines radiating from base of cavity, and corresponding with external ovaries. 15. Base of two marginal tentacles, 18. A group of reproductive capsules from the full-grown head, in several co-existing stages of development. 2, 3, 4, 5, 6. Progress in the extrication of young Tubularia, at intervals of one hour. 8. A young animal of the ellipsoidal form. 7a. Ditto, of the discoidal variety. 7s. The same, thirty-six hours after emerging from the capsule. 7c. The empty capsule. 10. The specimen, fig. 8—three days after—still free. 9. Ditto, on the fifth day, having affixed itself at base. 11. The young animal at the expiration of six weeks; the head having now acquired a pale rose tint, and the peripheral tentacles increased to sixteen. DESCRIPTION OF PLATE V. On the Structure and Development of Volvox globator, by Geo. Busk, Esq. 1. 7 3. Embryo Volvox, in which the contents are divided into four segments. Ditto, in which segmentation has proceeded to the formation of numerous segments, each furnished with several amylaceous spherules. Ditto, after segmentation is completed, but before the appearance of cilia. 3.* Portion of the edge of an embryo Volvox viewed in the equatorial oa > 27. plane, showing the cilia perforating the outer tunic, but not passing beyond the external gelatinous (?) envelope. . The same when tested by solution of iodine, . Portion of the edge of mature Volvox (var. vulgaris) viewed in the equatorial plane and representing three zoospores im situ. The faint lines between indicate the limits of the gelatinous envelope of each zoospore, the junctions of which are indicated by the hexagonal areas of Mr, Williamson. (‘These intermediate lines have been added to the figure since the original production of the paper.) . Mature zoospores, undergoing “‘ deliquescence.” . Zoospores in which the contractile vacuole is still present. “Winter spores” of V. awreus. a, in the earlier state; 6, when matured. . Contents of mature winter spore, affected by solution of iodine. a, amylaceous granules ; ; 5, yellow oil. . More highly magnified view "of a winter spore compressed, to Sow the double aoe. . The same crushed, and treated with iodine and sulphuric acid. . A portion of the edge, to show the granular fluid (as rendered so by iodine) between the outer and inner tunics. a, granular fluid; b, interior of spore. . Portion of wall of Spheerosira Volvox. p . Zoospores in different stages of development. a, one fully divided, seen on the side; b, the same viewed from above ; c, one in which segmentation has proceeded only to the second division. Series of changes occurring in the hydropical condition of zoospores. . More highly magnified view of the same—where there is apparently a second coat in process of being thrown off from the central mass of protoplasm. twenty-four hours. Fig. 22 shows the paral dropsy of the cell, but which did not proceed further. | A series of changes undergone by the same ZOOSpores in the course of . Professor Williamson’s hexagonal areolation. . Ditto under iodine. . Appearance assumed by the zoospores in the early state, where, owing to abundant nutrition, the quantity of protoplasm is very abundant. This form gradually passes into the ordinary, and it is in this state that the contractile spaces are most advantageously to be sought. Shows the situation of the contractile vacuole in a connecting band. Tuffen West sculp. (aa) A OD. 777 j yg oS, Ge paw / SIGNE. KWOK IIS SULYV. ie (ies Ford & West, Imp. London. oo A Cp ai PD) iS Inq Nov Foe LuV — GaP \ pee e ft sf . en BT a ONG x + * ( oso } , = j 0 fl. WP 7 aos) on ae Sg rN = i - wait A a \ i ul J cs Loy eer ‘J GBusk,del. Iuffen West, hth. Ford & West, inp. 54, Hatton Garden ‘ \ \ t ina - { ror 2 * OUR 99 NO DESCRIPTION OF PLATE VI. On the Structure of Volvox globator, by Professor W. C. Williamson. The same letters of reference are employed throughout to indicate the same structures. Cells of the stellate var. of Volvow in different stages of the con- traction of the protoplasmic threads. a, outer cell-wall; 5, pro- toplasm ; e, connecting threads; g, cilia. . Section of Volvox, with its ciliated parietal cells. /, vesicles in which the ciliated gemme are developed. Two of the gemmzx seen out of focus. 6. Young gemma ruptured by pressure. 06, detached protoplasms ; J, vesicles within which the gemma is developed ; c, protoplasmic membranes of three segments of the gemma. 0, granular and mucilaginous matter escaping from the ruptured segments. 7. Portion of a Volvox mounted in glycerine and viewed obliquely. a, cell-walls ; 6, protoplasms ; cc, protoplasmic membranes ; e, col- lapsed connecting threads. 8. Similar cells, in which the protoplasmic membrane is more distended. References as before. 9. Specimen in which the threads appear to traverse the intercellular spaces. References as before. 10. Ordinary appearance of the var., with spherical protoplasms. 11: Specimen of the same mounted in glycerine. 12. Probable section of living Volvow. d, superficial pellicle. 13. Probable section of fig. 11. 1 | Sections of figs. 1-4, after being mounted in glycerine. 16. Detached cells.from the same, viewed superficially. 17. Similar specimen, in which the cells are invisible—the protoplasmic membranes alone being seen. ut Ae Pee sf / UV 4 eS): GX . if ae ¢ IGN Hou Te Ford & West, imp. 54, Harton Garden. WCW.del. Tuffen West, sculp. ‘DESCRIPTION OF PLATE VIL. ; These Positive Photographs from Collodion Negatives, taken by _ J. Delves, Esq., illustrate that gentleman’s, Mr. Shadbolt’s, and Mr. & eae papers on Photography. Fig. ing Spimale and Trachem of the Siliswolin, magnified 60 diameters, exhi- biting the elastic spiral fibre between the layers of the air vessels. ze 2. Proboscis of the Fly, magnified 180 diameters, showing the divided Bet absorbent tubes. DESCRIPTION OF PLATE VIII. On the Starch-granule, by G. Busk, Esq. ig. rE 2,3, 4,5. Various forms of starch-granules in ‘* Tous les mois” Arrowroot. 6. Granules beginning to expand. 7, 8, 9. Farther progressive stages of expansion of the granule of ‘‘ Tous les mois.” 10. Various forms of starch obtained from the Horse-chestnut (sculus hippocastanum). 11, 12, 18. Granules of the same starch acted upon by sulphuric acid, DESCRIPTION OF PLATE IX. On Asteridia in Conferve, by the Rev. W. Smith. 1, Filament of Zygnema quininum, Ag., containing Asteridia in various stages of development. lie Scotian of Mesocarpus scalaris, Hass., var. 8, in conjugation, and 3 containing Asteridia. 4, Filament of Zygnema quadratum, Hass., in conga s 5. Filament of the same containing an Asteridiwm, and another a repro- ductive spore. 6. Filament of the same, showing a double mode of conjugation in the same species. On a Fungus in an Oak Tree, by Prof. E. J. Quekett. 7. A portion of an oak tree, showing a fungus and masses of crystals, in situ. 8. Fungus magnified 150 diameters. 9. Large crystal, having fungi in its interior. 10. A portion of fungus seen within a crystal. Ford & West, Imp. 4 Hatton Garden, sh . = ne , ‘ 7 rns 2 ’ ou ‘ ‘ PARE STO, e s~ ay My wis WEL, Af Lf, Dron M01 Dn Ford & West, Inp 54, Hatton Garden. Tuffen West,sc. - 7 Z = 7 et fea) y 7 1 c t 4% t ~ F, XS om x Ad DESCRIPTION OF PLATE X. Fig. 1. Lateral aspect of the Faujasina. Magnified 30 diameters. 2. Superficial section of the flat base of the shell. Mag. 60 diameters. 3. Horizontal section parallel to the last, across the points b 0, in fig. 1. Mag. 60 diameters. . Horizontal section across the points ¢ c in fig. 1. Mag. 60 diameters. . Vertical section across the points dd in fig. 1. Mag. 60 diameters. _ 6. Superficial section from the oblique side of the shell. Mag. 80 dia- meters. Ou He VOL. T. a . > “20, 43 bs * \ 4 b; i = ’ : 7 i re wud? iehin! . ~ - ~ . ~ W.C Williamson del. Tuffen West sc hai May Ford & West Imp INDEX TO TRANSACTIONS. VOLUME I. A. Aloe verrucosa, raphides in, 21. Amphistegina, 87. Asteridia, in Alge, Rev. W. Smith on, 68. B. Beale, Dr. L., analysis of raphides of Cactus enneagonus, 25. Binocular microscope, Prof. Wheat- stone, 99. Brachionus, 8. Busk, G., on the structure and de- velopment of Volvox globator and its relations to other unicellular plants, 31. on some observations on the structure of the starch granule, 58, C. Cactus enneagonus, Quekett on ra- phides of, 20. » senilis, Quekett on raphides of, 22. Chara vulgaris, 21. Cladophora glomerata, 21. Cocconema lanceolatum, 21. Cordylophora lacustris, 21. Cyst, membranous, containing a crys- tal of oxalate of lime, on the olfac- | tory nerve of a horse, J. B. Simonds on, 26. D. Delves, Joseph, on the application of photography to the representation of microscopic objects, 57. Diatomaceous earth found in the Island of Mrll, Prof. W. Gregory, 9z. K. Eleagnus angustifolia, raphides in, 22. Epithemia turgida, 95. Eunotia Triodon, 95. », Pentodon, 95. ge baorda, 95. F. Fauwjasina, minute structure of, by Prof. Williamson, 87. Floscularia, vibrating membranes in, 3. Fresh-water Alge, stellate bodies oc- curring in the cells of, Rev.W.Smith on, 68. G. Gosse, P. H., on water vascular sys- tem in WVotommata aurita, 5. Gregory, Prof. W., on Diatomaceous earth found in the Island of Mull, 92. H, Huxley, T. H., on Zacinularia so- cialis, 1. Hydrodictyon utriculatum, amyla- ceous corpuscles of, 67. K. Kolliker on division of the yolk in Megalotrocha, 11. L. Lacinularia socialis, anatomy and physiology of, by T. H. Huxley, LR sino) Leydig, Anatomie u. Entwick.-gesch. d. Lacinularia socialis, &c., 2, 8, 12. Lyngbya floceosa, 71. M. Megalotrocha, 1, 12. Melicerta, 2. Merulius lachrymans, 74. Mesostomum, 7. Mesocarpus scalaris, 71. Mummery, I. R., on the development of Tubularia tndivisa, 28. Mull earth, 95. Index to Transactions. N. Naviculacee, 93. Notommata aurita, teeth of, 4. os water vascular sys- tem in, P. H. Gosse on, 5. NNonionina, 87. * N. Opuntia, raphides in, 21. P; Philodina, 17. Photography, on the application of, to the representation of microscopic objects, by J. Delves, 57. Polyzoa and Rotifera, analogy be- tween, 16. Potatoe, amylum grains of, 62. Polystomella crispa, 87. Q. Quekett, on the structure of the ra- phides of Cactus enneayonus, 20. +3 on the presence of a Fungus and of masses of crystalline matter in the interior of a living oak tree, 72, R. Raphides, Quekett on, of various plants, 20. Rhubarb, raphides in, 21. S. Scilla maritima, raphides of, 21. Simonds, J. B., on a membranous cell or cyst upon the olfactory nerve of a horse, coutaining a large crystal of oxalate of lime, 26. Smith, Rev. W., on the Asteridiz or stellate bodies occurring in the cells of Fresh-water Alge, 68. Spheroplea crispa, 21. Spherosira Volvor, 32, 39. Spongilla fluviatilis, 21. Starch, granule, observations on the structure of, by G. Busk, 58. Stephanoceros, 4. Surirella ovata, 21. Synedra fasciculata, 21. T. Tous le mois, starch of, 65, 66. Truncatulina tuberculata, 87. Tubularia indivisa, development of by I. R. Mummery, 28. Turbellaria, 16. U. Udekem, on the water vascular sys- tem of Lacinularia, 6. V. Volvox globator, Busk, G., on the struc- ture and development of, 31. i further elucidations of the structure of, by Prof. W. C. Wil- liamson, 45. V. aureus, 40. V. stellatus, 40. W. Williamson, Prof. W. C., further eluci- dations of the structure of Volvor globator, 45. . Williamson, Prof. W. C., on the mi- nute structure of Fawasina, Wheatstone, Prof., on the binocular microscope and stereoscopic pic- tures of microscopic objects, 99. Z. Zygnema quadratum, 70. >» «= quintnum, 70. . TRANSACTIONS OF THE MICROSCOPICAL SOCIETY LONDON. NEW SERIES: Ww VOLUME II, LONDON: SAMUEL HIGHLEY, 32, FLEET STREET. 1854. LONDON : PRINTED BY W. CLOWES AND SONS, STAMFORD STREET. TRANSACTIONS OF THE MICROSCOPICAL SOCIETY OF LONDON. On the Application of Brnocutar Vision to the Microscope. By F. H. Wenuam. (Read May 25, 1853.) On viewing objects by the unassisted eyesight there are two conditions which enable us to appreciate or judge their various distances. Firstly, the object is observed by each eye from a separate point of view, and the consequent difference of outline, light, and shade between the images formed on each retina allows us to form an accurate idea of their various sizes and positions. ‘The angle of stereoscopic vision has been stated somewhat definitely to be about 18 degrees, but this must be subject to considerable variations, as whether the ob- server is long or short-sighted, the difference of distance between the eyes, and also the bulk, form, and position of the object. I may state that I have obtained a very good perspec- tive of minute objects when the angle of vision has exceeded 50 degrees. If we perforate a card with a pin, and examine the articles in a room illuminated by candle-light, with one eye looking through this aperture, we shall be able to judge of distance only from the relative intensity with which the objects are illuminated, the nearest receiving and giving off the greatest quantity of light, and the farthest being in comparative darkness. I make these preliminary observations because, in viewing the greatest portion of objects under the microscope, the con- ditions here referred to, which give us the faculty of judging of bulk and distance, do not exist in the same degree, if at all. In the first place, in viewing an object, as a transparency, with a single lens of short focus, we see it under such circum- stances as seldom happen to such surrounding objects as come under our daily observation, and in the illumination of trans- parent objects by direct transmitted light, the effect is the reverse of that which is necessary for us to Judge of distance VOL. I, Z WenuamM on Binocular Vision. by the relative intensity of the light, for that portion of the object farthest from the lens will receive the greatest share. This objection may probably be removed by a different sys- tem of illumination, but of this I shall treat hereafter. If the single lens is provided with a proper stop, what is known as the angle of aperture will be so exceedingly small that a series of uniform opaque particles lying behind each other in an object will be only seen by the direct light that they intercept, and the underlying ones will be invisible. These are the reasons why most microscopic objects, which we know must have a visible thickness, appear so perfectly thin, that we might almost imagine that they were painted on the glass slide upon which they are mounted. This illusion may be attributed to the natural effects of monocular vision, and in this case the only remedy is to view the object from different points at the same time with each eye, under equal magnify- ing power. I shall now enter into various methods of effect- ing this. One of the most simple and obvious is to employ two lenses, one to each eye, only differing from an ordinary pair of spectacles in the foci being shorter and the optic axes converging till the points where the foci intersect become coincident. Binocular vision may also be obtained through a single lens, if the diameter is sufficiently large to allow both eyes to see through it at the same time as in the common reading- glass. In these instances we cannot well use glasses of shorter focus than four or five inches; and in cases where higher magnifying powers are required it becomes necessary to adopt some method which shall produce the effect of bringing the two eyes proportionately closer together, to suit the diminished diameter and shorter focus of the lens. This may be accom- plished by means of a system of four plane reflectors, inclined at an angle of 45 degrees, and fixed behind the lens in a line at right angles to its axis, or else by four rectangular prisms in the same position; both these can be made to adjust to suit the diameters of various 3 lenses and difference of ; | Meee) §€6 clistance between the “LLL, ESSsanv” eyes. 2 The arrangement that / I have tried for lenses of short focus is repre- sented by fig. 1: aa is a plano-convex lens, be- hind which is placed the usual stop) b. c¢ ¢ are two rhomboidal Fig. 1. Wenuam on Binocular Vision. | 3 prisms of glass, with the reflecting ends inclined at an angle of 45 degrees. All the four surfaces of both prisms should be well polished, and their combined length when placed together should be such that the distance between the centres of the external diagonal reflecting planes should be the same as that between the eyes. I prefer the two solid prisms to a combination of four rectangular ones, as there is less loss of light, and error arising from external reflection. This com- bination makes a remarkably fine hand magnifier, giving such a depth and substance to objects as cannot be obtained with a single eye; the field of view is also large, as we are able to see the object obliquely through the lens. For lenses of low power, as from one to two inches focus, the prisms would require to be separated to some extent, or we should not ob- tain a sufficient angle for stereoscopic vision; in fact, we must consider this merely as a method of bringing the eyes closer together, that we may be enabled to see through a lens of small diameter with both of them at the same time, in a similar way as with the ordinary reading-glass before re- ferred to. On looking through the prisms, fig. 1, without the magni- fier, a singular illusion is produced, for the vision with the two eyes is brought so nearly to a state of parallelism that they are in effect blended into one, and we so far lose the power of appreciating distance, that we appear able to grasp objects several feet away from us, as the deceptions arising from monocular vision are increased by seeing with the two eyes from the same position as with one. In obtaining binocular vision with the compound achromatic microscope, in its complete acting state, there are far greater practical difficulties to contend against, and which it is highly important to overcome, in order to correct some of the false appearances, arising from what is considered the very perfec- tion of the instrument. All the object-glasses from the one inch upwards are possessed of considerable angular aperture, consequently images of the object are obtained from a differ- ent point of view, with the two opposite extremes of the margin of the cone of rays; and the resulting effect is, that there are a number of dissimilar perspectives of the object, all blended together upon the single retina at once. For this reason, if the object has any considerable bulk, we shall have a more accurate notion of its form by reducing the aperture of the object-glass. Select any object lying in an inclined position, and place it in the centre of the field of view of the microscope, then, with a card held close to the object-glass, stop off alternately b 4 Wenuam on Binocular Vision. - the right or left hand portion of the front lens, it will be seen: that, during each alternate change, certain parts of the object will alter in their rela- Ye. tive position. To il- te lustrate this, figs. 2 and 3 are enlarged drawings of a portion of the egg of the com- mon bed-bug (Cimex lecticularis), the oper- culum which covers the orifice having been forced off at the time the young was hatched. The figures exactly represent the two positions that the inclined orifice will occupy when the right and left hand portions of the object-glass are stopped off. It was illuminated as an opaque object, and drawn under a two-thirds object-glass of about 28° of aperture. If this experiment is repeated, by holding the card over the eye-piece, and stopping off alternately the right and left half of the ultimate emergent pencil, exactly the same changes and appearances will be observed in the object under view. The two different images thus produced are just such as are required for obtaining stereoscopic vision. It is therefore evident, that if, instead of bringing them confusedly together into one eye, we can separate them, so as to bring figs. 2 and 3 into the left and right eye, in the combined effect of the two projections we shall obtain all that is necessary to enable us to form a correct judgment of the solidity and distances of the various parts of the object. I shall. now explain some plans for effecting this. The most obvious method is to have two microscopes placed side by side, and converging towards the object, each tube to be furnished with a similar objective and eye-piece. For very low powers this would, no doubt, be the most perfect form of binocular microscope, but it is liable to objection, firstly, on account. of its expense, and, secondly, from the difficulty, if not impossibility, of using the higher powers. I do not think that it would be practicable to use anything beyond the half- inch object-glass; but I believe where vision is assisted by the use of both eyes together, it would be of advantage to employ objectives of smaller angular aperture, in this case, the focus would then fall at a greater distance from the front lens. I should also mention that a microscope of this description would require the two tubes to be placed at a different angle of convergence for every pair of object-glasses employed, of either longer or shorter focus. Bigs 1b te Fig. 2. OS TT WenuaM on Binocular Vision. 5 It has also been proposed to bisect the whole combination, of which our best objectives are composed, and separate the semi-lenses a sufficient distance asunder to obtain the effect of stereoscopic vision, each half being made to serve the purpose of a distinct combination; but this, I believe, would not answer at all, for if we escaped the total destruction of the object-glass during the operation of sawing it through, we should render it useless for all the ordinary purposes of inves- tigation, and also because any separation of the semi-lenses is quite unnecessary; for the angle of aperture of all the object-glasses by our best makers now exceeds that which is requisite for obtaining stereoscopic vision; and the methods that I have now to explain refer to the principle of obtaining two images of the object through the same object-glass, which is in all cases of the usual construction. In the last ‘Quarterly Journal of Microscopical Science’ there appeared a notice of a binocular microscope by J. L. Rid- dell, from Silliman’s Journal. According to his description, fig. 4 will represent the ar- rangement ; a is the objective provided at the back with the usual stops. The pencil of rays emergent from the ob- ject- glass is bisected and re- flected in opposite directions, by means of the internal surfaces of the rectangular prisms 6 b, which surfaces are inclined at an angle of 45°. The rays are again re- flected in a vertical direction, by means of two similar prisms, cc, the distance be- tween which must be regu- lated by the position of the eyes. The last prisms must be placed upon a lower level, as from the direction in which the rays are incident upon ) the first reflecting surfaces of the prisms b b, they have a down- ward tendency. The rays, after crossing each other, are received by two Huygenian eye-pieces, dd. In the diagram I have shown the prisms no larger than necessary for collecting all the rays from any of the object-glasses to be used; but it must be evident that Mr. Riddell makes use of prisms of b 6 WenuaAM on Binocular Vision. a larger size, as he states that “The outer prisms can’ be cemented to the inner by Canada balsam.” This amounts to the same thing as using a pair of prisms of solid glass, such as is represented by cc, fig. 1. I have carefully tried both of these methods, and find that the prisms alter the chromatic correction of the object-glass, and also materially injure the definition; for in making arrangements of prisms of this description we must always bear in mind that they produce a similar kind of aberration as a piece of glass of the same thickness as the distance which the ray passes through, Fig. 5. both before and after its reflection. There is also great difficulty in getting a per- fectly flat surface to the small reflecting planes. All these defects will be greatly magnified by the eye-piece. I have also tried what effect could be produced by means of plane reflectors, as Mr. Riddell says, “I use, for lightness and economy, four pieces of common looking-glass instead of prisms.” My experiment was not tried with common looking-glass, but with thin microscopic covering-glass, silvered at the back. The definition with the lower powers was to- lerably good, but the loss cf light very great. In order to remove the illusion of ele- vations appearing as depressions, Mr. Riddell proposes the “additional use of erecting eye-pieces ;” but I am afraid that when the microscope is taxed with this | addition, the loss of light and defining power will become very great, and that even easy test-objects will appear so ob- scure as to preclude all hope of our making any additional discovery relative to their structure. I must remark, that I have made these last observations and experiments merely for the sake of arriving at the truth, and not with the view of detracting in the slightest degree from the merits of Mr. Riddell’s invention; for very great credit is no doubt due to him for leading the way to the practical application of a principle, in the absence of which the microscope still remains an imperfect instru- ment; and, for my own part, I may, in all probability, shortly WenuaM on Binocular Vision. 7 see the day when my own designs for effecting the same end may be rendered obsolete by the march of improvement. In the plan just referred to, the error arising from the leneth or thickness of the prisms may be diminished by making the two mi- croscope bodies converge towards b 6, fig. 3, and adopting two rectangular prisms with the reflecting surfaces at the proper inclination for directing the rays of light from the object-glass, up the centre of each tube: by this means _ we can much reduce the substance of glass that the rays will have to pass through. Figs. 5 and 6 represent another method that I have contrived for using only two prisms, which can be made of the smallest possible size, and also at the same time do away with one re- flecting surface, which is one of the principal sources of error. Fig. 5 is the plan, and fig. 6 the elevation. a, fic. 6, is the object-glass, over which are two right-angled prisms bb, placed side by side with the reflecting sur- faces, at an angle of 45°. ce, fig. 5, are two Huygenian eye-pieces, placed a sufficient distance asunder to suit the eyes, and converging towards the vertical axis of the object-glass. The contact sides of the prisms must be equally ground away, till their two emergent surfaces are in a plane at right angles to the axes of their respec- tive eye-pieces. This method in- volves the necessity of having the object-glass at right angles to the : two bodies of the microscope, and is therefore just suited to some of the foreign form of stands, but is of course inap- plicable to the English ones, unless, indeed, we mount the bodies after our usual fashion, and allow the object-glass to point upwards in an inclined direction, and pass through the bottom of a stage, on the upper surface of which the objects can be placed, and which surface should be parallel to the axes of the bodies. This would give great facility for direct illumination ; for whether we used a superposed achromatic condenser or not, we should not require a mirror either by Fig. 6. 8 WenuaM on Binocular Vision. day or candle-light. I have not yet tried this arrangement of prisms, but intend to do so, as I have a favourable opinion of the method, although the one next to be described is pro- bably better. . If we consider the relative position of the two reflecting surfaces of the prisms 56, figs. 5 and 6, they will form the same angle represented by the es top line of fig. 7. It is there- Vig 7 fore evident, that if a rectan- gular plate of speculum metal is KAAKRF>RDDHRKRC Souta and oldie so as to form two reflecting facets in- clined to each other at the re- quired angle, as represented by fig. 7; and this being placed at an angle of 45°, with the division of the facets intersecting the axis of the object-glass, we shall divide the rays, and reflect them horizontally, just in the same way as represented in figs. 5 and 6, merely by means of one single reflection. Any other direction than a right angle, with respect to the axis of the object-glass, may of course be given to the rays, by inclining the reflector more or less. From the simplicity of this contrivance, and the facility with which it may be constructed, I shall take an early opportunity of giving it a trial. The only question I have is, whether a material may not be found that will reflect more light than even speculum metal: I have heard an alloy of cast-steel and platinum well spoken of, but have never seen any of it. In considering the aberrations which the thickness of glass contained in the reflecting prisms must inevitably produce when placed immediately behind the object-glass, it occurred to me, that if the same prisms were placed close to the top lens of the eye-piece, these errors, not being magnified, would be less sensibly felt. I have before mentioned, that the final image of an object, when it leaves the eye-piece, is compounded of several different images or perspectives of the object, all blended together, and which are as equally capable of separation there as be- hind the object-glass itself, as exemplified by figs. 2 and 3, which bear exactly the same appearance when under view, with the alternate sides of either the object-glass or eye-piece stopped off. Fig. 8 represents the methods that I have contrived for ob- taining the effect of bringing the two eyes sufficiently close to each other to enable them both to see through the same eye- plece together. aaa are rays converging from the field lens of the eye-piece. After passing the eye lens b, if not inter- cepted, they would come to a focus at c, but they are arrested ee WennaM on Binocular Vision. 9 by the inclined surfaces d d, of two solid glass prisms. From the refraction of the under incident surface of the prisms the focus of the eye- plece becomes elongated, and falls within the substance of the glass at e. The rays then diverge, and, after being reflected by the second inclined surface f, emerge from the upper side of the prism, when their course is rendered still more divergent, as shown by the figure. The reflecting angle that I have given to the prisms was 471°. I also find it is requisite to grind away the contact edges of the prisms as represented, as it prevents the extreme margins of the reflecting surfaces from coming into operation, which can seldom be made very perfect. The definition with these prisms is good, but they are liable to objection, on account of the extremely small portion of the field of view that they take in, and which arises from the distance that the eyes are of necessity placed beyond the focus of the eye-piece, where the rays being divergent, the pupil of the eye is incapable of taking them all in; also there is great nicety required in the length of the prisms, which must differ for nearly every different observer. I have constructed an adjusting binocular eye-piece, not differing in principle from the last. The first reflection is performed by means of a triangular steel prism, with the two inclined facets very highly polished; this is represented by the dotted outline gg, fig.8. The rays, after having been reflected at right angles, are taken up by two rectangular glass prisms, shown by the dotted lines at ff. The loss of light in this is much greater than in the former instance, and the ficld of view more contracted; for the rays from the eye-piece, after being reflected from the surface of the steel prism, fall to their natural focal distance, instead of being elongated, as in the solid prism, consequently the eye is still further removed from the focus. I had chosen hard steel for the reflector, on account of the property this material pos- sesses, of allowing the figure of a small flat surface to be retained, or even perfected, during the operation of polishing. I have also tried a combination of prisms over the field-glass, using two eye lenses, but with no good result. The best effect that I have yet produced in the way of Fig. 8. 10 WenuaM on Binocular Vision. binocular vision applied to the microscope, is that next to be described, in which I have altogether dispensed with reflecting surfaces, merely using three refracting prisms, which, when placed together, are per- fectly achromatic. aa, fig. 9, is a single prism of dense flint glass, with the three surfaces well polished. 66 are two prisms of crown glass, of half the length of the under flint prism, to the upper inclines of which they are cemented with Canada balsam. The angle of inclina- tion to be given to the prisms must depend upon the dispersive power of the flint and crown glass employed. In the combina- tion that I have worked out, I have used, for the sake of sim- plicity, some flint and crown that Mr. Smith kindly furnished me with, in which the dispersive powers are exactly as two to one, consequently I have had to make the angle of the crown just double that of the flint, in order to obtain perfect achro- matism, The refractive power of each must also be known, that we may determine the angles of the prisms suitable for refracting the rays from the object-glass into the two eyes, at a distance of nine inches. cc, fig. 9, represents a ray of light incident at right angles upon the under surface of the flint prism. On leaving the second surface and entering the crown prism it is slightly bent.inwards, and on finally emerg- ing it is refracted outwards, in the direction required. On looking through this prism I could not discover the slightest colour or distortion ; itis almost like looking through a piece of plain glass, and the loss of light is so inappreciable, that it is difficult to distinguish any difference between an object and its refracted image. The base of the compound prism should not be larger than is sufficient to cover the stop of the lowest object-glass, in order that they may be made very thin. The method of applying the prism to the binocular micro- scope is shown by fig. 10. aa is the object-glass, b the prism, placed as close behind it as the fittings will admit. The prism is set in an aperture ina flat disc of brass, which has an horizontal play in every direction, in order that it may be adjusted and fixed in such a position that the junction of the prisms may bisect the rays from the object-glass, and at the same time be at right angles to the transverse centres of the eye-pieces., cc are the two bodies of the microscope, provided with Fig. 9. J is Wennam on Binocular Vision. 11 draw tubes and the usual eye-pieces, dd. The distance between them should be rather less than the average distance asunder of the eyes, and in cases where these are very wide apart we can pull out the draw tubes, which will increase the distance between the eye-pieces. With this apparatus I obtain the whole of the field of view in each eye, which circumstance I was not pre- pared to expect, as this must in some measure depend upon the cor- rection of the oblique pencils of the object-glass, for we cannot expect to look obliquely through the ob- jective of a compound achromatic microscope in the same way as in the single lens arrangement, fig. 1, but can only avail ourselves of such oblique pencils of rays as are cor- rected for passing through the axis of the microscope. The arrange- ment represented by fig. 10 certainly gives a larger and better field than any other that I have yet tried; and on examining a globule of mercury I could not discover any aberration or inward or outward coma when viewed by the eyes, either separately or together. I should here mention that the same illusion is occasionally produced in the appearance of some objects with the instru- ment last described, as mentioned by Mr. Riddell, the vision being to some eyes pseudoscopic, or projections appearing as depressions, et vice versa. Probably habit would enable us to judge of their true form without our being under the necessity of resorting to a special expedient for the removal of the de- ception. ‘T have not yet tried a binucular polariscope applied to this instrument, but I have reason to expect some curious effects from it. I have thus far announced the progress of my experiments towards the attainment of complete binocular vision with the microscope, and | cannot too strongly insist on the importance of striving to arrive at a perfect result, particularly with the highest powers, for I feel convinced that it will be the means of settling many disputed points of structure. Whether it will require objectives of a peculiar construction I am not at present _ able to determine, but I may observe that the high power Fig. 10. 12 WenuaM on Binocular Vision. object-glasses, as now constructed, are best suited for viewing very thin objects. We obtain far more pleasant vision of bulk and depth with a smaller aperture. I have no doubt that the defects of the larger aperture arise from the confused medley of stereoscopic images blended together in one eye, and which confusion must increase with increase of aperture ; but if, on the other hand, we can divide these images between both eyes, then I admit that the aperture cannot be too great, as the largest portion of microscopic objects, from the way in which they are mounted, would be all the better shown under an exaggerated perspective, if I may so express it. The binocular microscope has already explained to me some of the false appearances arising from oblique illumina- tion. I refer particularly to what is known as the diffracting spectrum ; for example, if we illuminate the Podura by very oblique light, we see a kind of overlying shadow, upon which the markings of the scale are also visible. As I can- not reconcile this appearance to the known laws of the dif- fraction of light, I think that it is miscalled, and appre- hend that the phenomenon merely arises from the oblique light illuminating one of the perspective images partly as an opaque, and the other as a transparent object, and that they are, consequently, so far separated as to give the appearance of a double image. In illuminating objects under the binocular microscope with the ordinary concave mirror some management is required in order to get both images equally intense, for we can readily get one brilliantly illuminated, while the other is in compara- tive darkness, appearing on a black ground almost as an opaque object, exactly resembling in their combined effect on the eyes what is known as the diffracting spectrum. It also occasionally happens that the angle of light from the mirror is not sufficient to illuminate both images at the same time. These appearances lead me to conjecture that the mstrument will require a particular kind of illumination, but I am hardly yet in a position to express a decided opinion on the subject, but will investigate the matter shortly. This is the sum and substance of my present experience with respect to binocular vision applied to the microscope, and I do not think that mere enthusiasm has led me to over- rate the importance of the subject, but hope that what has already been done is only the commencement of a new era in the advancement of this useful and important instrument. I believe that there is yet much to be looked for in the way of improvement by the investigation of unexplored optical com- binations and principles. Wennam on Binocular Vision. | 13 - In conclusion I must express my thanks to Messrs. Smith and Beck for the prompt assistance that they have afforded me in the construction of the instrument, and also for the free use of such apparatus, selected from their stock, as might be useful to me in conducting my experiments. A Short Description of some New Forms of Diaromacrx from Port Natal. By Geo. Suappotr. (Read May 25, 1853.) THE constantly increasing interest evinced in the examination of the elegant forms of the Diatomacee has recently received an additional impetus from Messrs. Smith and Beck’s publi- cation of the first volume of the long expected ‘Synopsis of the British Species,’ by the Rev. W. Smith, F.L.S. A work of the kind alluded to will supply a want that has been much felt by microscopists, both as a record of what has already been accomplished in this branch of study, and also as a foundation for a general system of classification and nomenclature, for not 6nly is the latter in the most deplorable state of confusion, but by far the greater number of the foreign species are only capable of being referred to by their “ local habitation,’ being destitute of the other appendage generally considered so necessary. | Under these circumstances I propose conferring a provi- sional name on such new species as [am about to describe, trusting to the indulgence of any prior claimant to this right, whom I may unintentionally supplant, and promising to with- draw such name on cause being shown. About twelve or fifteen months back I was supplied, by the kindness of Mr. Geo. Busk, with a gathering of Diatomacez from ‘ Port Natal” so rich that I shall not attempt to give a detailed account of the forms already known, but, merely noticing a few of the most prominent of these, describe more particularly those species that are, so far as [ am aware, entirely new, endeavouring by the respective designations to recall them to the mind, by fixing upon some prominent peculiarity of appearance in each as the foundation for such distinction. From the prevalence of certain forms (although I am not at all acquainted with the facts of the case) I should be inclined to pronounce the locality whence they are derived as subject to marine influence, and at the same time probably not far from the mouth of some river, and it is also evident that the specimens are undoubtedly recent. Mixed with the Diatomee are some other bodies, which are scarcely capable of being classed with them, although, like 14 SHADBOLT on New Forms of Diatomacee. the spicula of many of the sponges (of which there is a goodly proportion), they are of a siliceous character, such as the Dictyocha, and also a form to which my attention was directed by Mr. Busk, and which I purpose identifying by the name of Bacteriastrum, from Baxrngia, a stick, and Aorgov, a star. By the kind assistance of another of our members, Mr. Capron, I am enabled to lay before you drawings of these most interesting bodies (of which may he distinguished three species), as also of most of the other novelties. From the tenuity of their structure the various Bacteriastra are better observed without being mounted in balsam ; they consist of a central irregular annular portion (not unlike the connecting membrane which may be observed in the Diatomee during self-division), surrounded by from eight to twelve rays, each many times longer than the diameter of the central por- tion, and the construction of these rays affords a good specific distinction, viz. lst, B. furcatum (fig. 1), the marginal rays forked ; 2nd, B. curvatum (fig. 2), marginal rays entire and curved in one direction; 3rd, B. nodulosum, marginal rays entire, straight, and covered with small protuberances like a knotted stick. This last species is by far the most rare.” A form tolerably abundant and quite distinct from anything I have ever met with from any other locality I propose to call Euphyllodium, from ev, and @vAdaov, having somewhat the outline of a spathulate leaf (fig. 3). It 1s characterised as follows: viz. valve symmetrical, convex, divided by a median rectilinear rib, reticulations of an irregular oblong form, dis- posed in regular and elegant curves around centres formed by the terminations of the median rib. I have noticed but one species, which I have called C. spathulatum. There was at first some doubt in my mind whether this might not belong to the genus Cocconeis, but the very distinct appearance of the median line, and the absence of anything that could possibly represent the inferior valve, which in the latter genus is generally (I believe always) somewhat different from the superior one, and likewise the marked character of the outline, satisfied me that this supposition was incorrect. It is not unlike the aspect of the genus Podosphenia, but here again there are differences so distinct as to satisfy me that it cannot be referred to it with propriety; for instance, there is no re- flexure of the valve, and the markings are not moniliform striz, but rather tessellate in character. * Since writing the above, I have made out most unquestionably that this pseudo-annular portion is a distinct cell, and not a mere annulus. Srapsott on New Forms of Diatomacee. 15 Of the genus Triceratium there are no less than five new species, one old, and one doubtful, making seven in all. The first I shall notice is of moderate size, and is distin- guished by peculiarly delicate markings somewhat obscurely disposed about three equidistant pseudo-nuclei— Tr. sculptum (fig. 4). Next we have one in which the markings appear like minute dots, closely crowded together, but disposed in a very regular manner from the axis of the valve; this is about the same size as the preceding, but the outline differs materially, each margin being arcuate with the concave surface outwards — Tr. arcuatum (fig. 5). Another species of medium size is in form nearly the con- verse of the preceding, the margin being so inflated as to cause the triangular outline to approach that of the circle; hence Tr. orbiculatum as its specific designation (fig. 6). This species exhibits a structure similar to that of Coscinodiscus radiatus: the reticulations, however, are not so regularly hexagonal, but they are largest at the centre, and diminish in size gradually towards the margin of the valves. - | have noticed also a single specimen of what appears to be Tr. alternans, but, as it presents only its front view, it is difficult to determine. The next I shall allude to is, however, the most important, being very remarkable and especially interesting from the front view exhibiting the disposition of the horn-like append- ages (figs. 7a@ and 75) and the mode of dividing. On the lateral view of the valves the most striking peculiarity is a sort of twistedness in the angles (fig. 7a), which is very marked: the specific name proposed is to note this fact, viz. Tr. contortum. The surface of each valve is adorned with short spines arranged in a tri-radiate double row, and at the termination of each double row is one very long one, being about one- third of the length of aside of the valve. These long spines are independent of and placed nearer to the axis than the horn-like processes from which the genus derives its name. Fig. 7b shows a specimen undergoing self-division. _ Another new species, much smaller than the last, is charac- terized by the reticulations being coarse and irregular in form, and the horns very large as compared with the size of the valve— Tr. crassum. Another species is, I believe, a variety only of the T. favus, which has been called gibbosus. The genus Pleurosigma has no less than five species, two being quite new, and both having the markings arranged dia- 16 SuaDBott on New Forms of Diatomacee. gonally, that is, with (what the Rev. W. Smith considers) cells placed alternately in contiguous rows. The outline of the largest (fig. 8) is very clumsy and the ends obtuse, and the median line but slightly flexed—this | call * validum ;” the other, P. inflatum, on the contrary, is of a graceful out- line, the apices acute, the flexure of the median line con- siderable, and is broad in proportion to its length (fig. 9). A third species is, I believe, also new; it was observed by Mr. Capron when making the drawings; but as I have not had an opportunity of examining it, I have not further no- ticed it. Specimens of P. formosum and P. Hippocampus are also found. There are two new species of Amphitetras, viz. A. ornata and._A. tessellata ; the former (fig. 10) is of small size, the mar- gins of the valves being considerably hollowed or emarginate and folded over so that each valve is not unlike in form to a collegian’s cap. The surface is elegantly but somewhat irre- gularly ornamented with delicate markings. A. tessellata (fig. 11) is of larger size, and the markings coarse and resembling - a tessellated pavement. There is a very striking and beautiful discoid valve, toler- ably abundant, of the same genus as one commonly found in the guano from Callao, but which, I conceive, has never yet had a generic name. It differs in essential characters both from the Coscinodiscus and Actinocyclus, and its position would probably be midway between them. It is possessed of a pseudo nucleus, is minutely embellished with delicate markings similar to those seen in Pleurosigma anyulatum, &c., but in segments radiating from the centre, so that, in all probability, the front view would exhibit slight undulations. ‘The absence of any distinct division between the segments, however, separates it from Actinocyclus. 1 propose for this form the generic name Actinophenia, from axtiv, aray, and Qaeios, glittering, with the specific designa- tion splendens. Fig. 12 is a new species of Hupodiscus, having four pro- cesses arranged regularly, and with the markings of a some- what similar character to those in the last described species, forming an elegant cross; I have, therefore, named it £. crucifer. Fig. 13 represents a Campylodiscus latus, also new, the cana- liculi being wide apart and few in number. Moderately abundant in this gathering are specimens of a highly interesting nature, on which the generic name of As- terolampra has been conferred by Professor Baily, of New York: one species, A. marilandica, has been figured in ‘the SHADBOLt on New Forms of Diatomacec. 17 American Journal of Science and Art,’ vol. xlviil.; a copy of the paper is in the library of this Society, it having been pre- sented by the late Mr. Edwin Quekett. The Port Natal species differs in many respects from A. marilandica, as the following description will show :— Frustules disciform, slightly convex, cellular (?), elegantly marked around the margin with 7 or 11 segments of an elliptical or parabolic outline, radii proceeding from the centre to the apex of each segmental curve, and strength- ened with bracket-like projections. The aspect is not unlike an ornamental wheel, the radii forming the spokes, The seg- ments are regularly and minutely divided into dots or cells (?), but it is necessary to use a high power and careful manipula- tion to display them: when properly shown, however, nothing can well be more exquisitely beautiful. ‘There is a very no- ticeable peculiarity in the number of the segments ; in every specimen I have seen, being either 7 or 11 (a few only of the latter number), and in the normal state the two valves, as far as my observation extends, are, without exception, disposed alternately, that is, that a segment of the superior valve always corresponds to an interspace of the inferior one, and vice versa. I have named this species A. impar, from the odd number of segments. Fig. 141s a representation of this beautiful frustule. A species of another genus, established by Professor Baily, Cliimacosphenia, is shown at figs. 15a and 156, b being the lateral view, and a the front view, in which the ladder-like divisions more resemble the links of a chain than in the only other species I have seen: I have consequently called it Cl. catena. Two very interesting forms, by no means rare in this very rich gathering, belong to a genus that has been described. under the names of Zygoceros and Denticella, the latter by Professor Baily, and as they clearly differ from the former, as may be seen by the most casual observer on inspecting fig. 16, which is a single frustule of a true Zygoceros, moderately common in this collection, I shall adopt the latter designation. I have only seen them either single or in pairs, having just completed the process of self-division, having a somewhat persistent connecting membrane. Front views are shown of the two new species in figs. 16 and 17. The side view is more or less elliptical in outline at the junction of the two valves, but sections in almost every other plane parallel to this would present a different figure, owing to the protuberances shown m the front view. In both species there arise from the cen- tral inflations two slightly curved spines from each valve, which, as in Triceratium, &c., in the process of self-division, VOL, II. c 18 SHADBOLT on New Forms of Diatomacee. are arranged across each other. The smaller of the two spe- cies (fig. 16), D. s¢mplex, has but one central inflation, and the lateral expansions are symmetrically placed so as to give each valve the appearance of a sort of mitre or head-dress. It is marked with numerous well-defined dots or cells (?). The second species, D. margaritifera (fig. 17), has, besides the two lateral expansions, three intermediate inflations, the cen- tral one being considerably the largest, and the whole is covered by numerous pearl-like eminences similar in aspect to those so common in Cosmarium and other Desmidiee. In both species the union of the two valves is marked by a sort of projecting band, which completely encircles the frustule. In addition to those I have described there are very many other forms already familiar to observers of the Dvratomee, and doubtless some new forms which I have overlooked. I am well aware that the present is a most imperfect sketch of a highly interesting gathering, containing, as will be shown by the following summary, no less than 55 species, of which 20 are certainly new, and in addition 4 forms of Sponge spicula. Species. Species. Bacteriastrium : . 38 of whichare certainly new 3 Calophyllum ‘Triceratium Pleurosigma Amphitetras . Actinopheenia Eupodiscus Asterolampra . Denticella Campylodiscus Climacospheenia _ Navicula Stauroneis Pinnularia Nitzschia, Grammatophora Tabellaria Striatella Zy goceros Acnanthes Cocconeis Doryphora Podosphenia . Synedra Coscinodiscus . Tryblionella Meloseira Biddulphia Epithemium . Dictyochas Ne) Be [piu po. eee oan. And 4 forms of Sponge Spicules. Ou St | eS ee tok pH WR Re NOR wr Noe ana Lee on Sponge Sand. 19 Observations on the Examination of SPONGE Sand, with Remarks on Collecting, Mounting, and Viewing FORAMINIFERA as Microscoric Oxssects. By M. 8. Lece, A.L.A. (Read June 22, 1853.) Various papers on the structure of the Foraminifera have been brought before the Society by Mr. Williamson and others, but the impression conveyed by those communications has been that the shells in question are not very easily obtained, and consequently they are likely to be passed over by micro- scopists from the want of specimens by which to study them, Although the matter of this paper has no pretension to originality, I am induced to offer these remarks in compliance with a suggestion thrown out by a Member of our Council, that if Members would occasionally communicate facts, appa- rently unimportant in themselves, or new modes of manipu- lation under the general title of ‘ Microscopic Memoranda,’ such remarks would contribute to diffuse a taste for the pursuit by facilitating the labours of those whose time and inclination admit of such researches. Under this impression I now lay before the Society the result of my experiments on sponge sand, and the methods employed to bring the specimens more immediately within my reach without the labour of picking them out from an in- discriminate sample of the sand itself. Having observed that there was some degree of uniformity in the magnitude of certain species of the Foraminifera, it occurred to me that by sifting the mass of sand through wires of different gauges important results would follow, and I therefore obtained some specimens of wire-gauze of 10, 20, 40, 70, and 100 wires to the inch, and, having also procured from a sponge merchant about a peck of the rubbish arising in sorting the sponges, I proceeded to separate the sand into parcels of different degrees of fineness, In the first process (employing a gauze with 10 wires to the inch) I cleared the mass of clippings of sponge, small pebbles, &c., without obtaining any specimens of shells worth retaining. In the second (20 wires to the inch) I obtained some very nice specimens of the Orbiculina adunca and complanata, but scarcely anything else; these specimens, of which the Mem- bers may recollect that Dr. Carpenter exhibited a series of very beautiful drawings at one of our soirées, were thus brought together, instead of being, as before, scattered through the mass, at intervals few and far between. c 2 20 Lee on Sponge Sand. By means of the third gauge of wire-gauze, specimens of Peneroplis, and smaller specimens of Orbiculina, were brought together, with other species of Foraminifera of considerable variety of beauty and form, the result here obtained being very decided and characteristic of particular species; for, although the quantity retained after this process was compara- tively small in relation to the original mass, yet the specimens were such as to afford an ample reward for the time and trouble incurred in obtaining them. But the most surprising result was obtained by using the next quality of wire-gauze (that of 70 wires to the inch), the amount retained being much larger in quantity, and the pro- portion of shells to sand and other débris being such that sliders mounted indiscriminately from it yielded several very good objects in every instance. From the above samples I was enabled to select, without difficulty, shells for microscopic observation; in the first two by the naked eye, and in the latter by using a hand magnifier, and removing them with the moistened point of a camel’s-hair pencil. ‘Lhe remaining portion of sand, forming probably 19-20ths of the original mass, will contain, as may easily be imagined, a very small comparative quantity of shells; but, nevertheless, it must not be thrown away. I again passed some of it through a gauze of 100 wires to the inch: the sample then retained yielded a fair quantity of shells by washing it in water, and thus other species characterized by their size were brought out by adopting the following process: having selected a dish of sufficient size and depth, and spread at the bottom of it a quantity of the sand, as much water was poured on it as would cover the whole to the depth of half an inch; after allowing the floating particles to settle, the dish was slightly raised at one end and gently agitated, so as to produce little eddies in the water. Inashort time it was observed that small channels were formed in the sand of a whiter aspect than the other portions ; allowing the water to settle gradually, the dish was slowly tilted at one end until the surface of the sand was exposed: the whiter particles being then carefully removed by means of a camel’s-hair pencil, they were found to consist almost entirely of very minute shells; and the process being repeated a few times a large amount (microscopically speak- ing) was obtained for future examination. In connexion with this subject I may venture a few remarks upon collecting, mounting, and viewing specimens of the Fo- raminifera as far as my experience has enabled me to speak. When about four years ago I was staying at Weymouth Lxee on Sponge Sand. 21 with my friend Mr. Woodward, in walking over the Small- mouth Sand, which is situate on the north side of Portland Bay, we observed the surface of the sand to be distinctly marked with white ridges, extending many yards in length, and parallel with the edge of the water. Upon examining portions of these we found that they consisted of Foraminifera in considerable abundance, and, upon scraping up a quantity of it carefully with a card, we obtained in a short time a bottleful of material which contained thousands and probably millions of these minute shells. My friend Mr. Cocken, during a recent residence at Brighton, was very successful in obtaining a considerable quantity of the Foraminifera from the surface of the mud exposed by the receding tide in Shoreham Harbour; and here also the surface only should be taken, in order to have a large proportion of shells. It is very well known to many of our Members that the ouze from the oyster beds yields a very fair proportion of Foraminifera and other materials for microscopic examination, and I am inclined to think from these evidences that the sur- face, and the surface alone, of sand or mud banks will yield satisfactory results. And I should recommend to all those who contemplate collecting for themselves, or employing others to do so for them, to take only the surface, being convinced that a few spoonfuls obtained in this way will yield more than a spadeful taken indiscriminately. My view of this is also confirmed by the large amount of shells in the sponge sand, for being taken from the sea-shores, that which is gathered up with them is such as occurs only on the surface. I think it also very probable that a locality sheltered from the direct action of the sea would be more favourable for finding these organisms than a bold shore exposed to all the violence of the wind and waves. If these conjectures should be borne out by experience, it is to be hoped that the increased facilities of finding their habitats will lead to extended obseryations on their living economy, a subject rendered extremely interesting by the papers of Mr, Williamson and the writings of Dr. Carpenter and others, where the subjects of their structure and zoological position are very ably discussed. The species of Foraminifera are so numerous that the mere mention of 575 species described by D’Orbigny as peculiar to the torrid zone, 350 species to the temperate zone, and 75 species to the frigid zone, sufficiently attests their abundance, and the samples of sand which have come under my own observation from the Caramatta Strait in the China Sea, from 22 Luee on Sponge Sand. Australia, and other localities, afford ample proof of numerous and beautiful forms. After collecting these minute shells, two very important points are, mounting them for future examination, and viewing them so as to obtain their true structure. Much depends on the different genera, as to the most eligible mode; the simplest and most natural is that adopted by Mr. Marshall of placing them in cells made of perforated card, putting a piece of thin glass over and sealing it down, so that the objects roll about loosely, and are viewed as opaque objects by a side light; another mode, also adopted by the same gentleman, is placing the shells on a glass slip with a little very dilute gum water, which causes the shells to adhere sufficiently to the glass as to admit of the air being exhausted from them when mounted in Canada balsam. They may then be viewed either as opaque or transparent objects, but it will be observed that the texture of the shell which invests the segments of the animal is (as observed by M. d’Orbigny) very variable, but it almost always follows the different mode of growth upon which the orders of that author are founded. When the segments are closely packed together, the shell is opaque, of a close texture like porcelain, and without any indications of external porosity ; when the segments are alternate without a spire, and when the spire is oblique, the shell is porous, and pierced over the last cells with a great number of little mouths, through which proceed the filaments, but which become obliterated when the animal no longer needs them; when the segments are in a straight line, when they are coiled upon the same spiral plane, or when they are alternate, and the shell inequilateral, their texture is almost as transparent as glass. From the above description it will be evident that one single mode of illumination will not suffice for duly developing ‘hel structure of these shells, and I should therefore recommend that some be mounted loosely in a cell, so that all parts may be viewed as they roll over; and others ‘be mounted in Canada balsam, and viewed by means either of the annular condenser of Mr. Shadbolt or the parabolic reflector of Mr. Wenham. By these means the difference in structure between the upper and under surfaces of the same species of shell is brought out, and that confusion avoided which occurs when direct light is transmitted. —~ ees eae et ee ieee ee ot ee Rainey on Artificial Light. | 23 A Method of employing Artimciat Lieut for the ILLumina- TION Of TRANSPARENT Oxsects, by which it is so deprived of Glare and Colour as to be equal in its Illuminating Power to the best Daylight. By Gro. Rainey, M.R.C.S., Demon- strator of Anatomy atSt.Thomas’s Hospital. (Read June 22, 1853.) Tue principal disadvantages attending the use of gas and lamp light, as they are ordinarily employed for microscopic illumination, are the disagreeable and somewhat painful glare and the unnatural colour which is given to all objects thus illuminated. These inconveniences are not felt so much where only a plane or concave mirror is used, as when the light is concen- trated upon the object by an achromatic condenser ; and, in the former case, they are partially remedied by transmitting the light through a piece of ground glass, either common or coloured ; or by dulling the surface of the mirror; but in the latter one, these means, by cutting off too much light, are productive of more harm than benefit, especially where the markings upon an object are very delicate and require a parti- cular kind of illumination to render them distinctly visible, as, for instance, the dots on the Pleurosigma angulatum. Hence, unless some other plan be adopted for moderating the intensity of all artificial light and correcting its colour, the employment of the achromatic condenser must either be limited to the hours of a good daylight, or the observer be in danger of materially injuring his eyesight. Mr. Gillett’s apparatus for producing the effect of a white cloud does, 1 am informed, remedy all the defects of lamp- light, but, from some difficulty or other in constructing or in applying it, its employment has not become general. The plan to which I have to call your attention is especially applicable to Mr. Gillett’s condenser, and may at a compa~ ratively small expense be made a part of that most useful instrument. Before proceeding further I may observe that the principle upon which my apparatus is constructed is one which has been of general adoption for the preservation of the eyes of those who use glasses, and therefore so far has no claim to originality ; but its precise construction and application to the microscope, and its effect in rendering artificial light equal if not superior to the very best daylight, are admitted by those who have seen it, and, to the best of my knowledge, are also new. But my motive has not been novelty but utility, in bringing this subject under the notice of this Society. 24 Rainey on Artificial Light. Now that which gives the peculiar burnish or glow to all objects when highly illuminated, whether by the direct rays of the sun, or by light proceeding from ignited matter, is due to the heating portion of the spectrum and certain coloured rays. In the former case we make use of light for microscopic illu- mination which has been deprived of this burnish by its having passed through the clouds; and in the latter this can be equally well effected by passing the light emanating from gas or a lamp through such transparent coloured media as will stop the calorific rays, and at the same time furnish the kind and amount of colour necessary to form, with the coloured rays of the flame, white light. The combination which I find to answer best is the fol- lowing :— One piece of dark blue glass, free from any tint of red, one of a very pale blue with a slight shade of green, and two of thick white plate glass, all cemented together with Canada balsam, This combination so completely stops the calorific rays, that when the direct rays of the sun are concentrated by a bull’s eye of the ordinary size upon a lucifer-match with this medium intervening, it does not become ignited ; and when this medium is used with Gillett’s condenser, objects illuminated by the light of a camphine lamp appear as if they were seen by a bright daylight. Boswe tt on Actinophrys Sol. 25 - Remarks on Acttnorurys Sot. By R.S. Boswett, Spring Hill Cottage, Charmouth, Dorset. (Read Oct. 26, 1853.) In an interesting paper in the ‘ Journal,’ of a description of Actinophrys Sol, by A. Kolliker, &c., (Vol. L., pp. 25 and 98,) the author, after entering into a very minute descrip- tion of this curious animalcule, says:—‘‘ The creature also seems to be capable of altering its entire form to a certain extent, and to be able to expand and again contract itself in toto. More extensive and more energetic movements do not occur at all, and I am consequently altogether ignorant as to how locomotion of the animal is effected.” My object in sending this short notice is to give him that information which he seems to want, though perhaps by this time he may have made the same discovery as myself, if not, it cannot but be interesting, not only to him, but also to others, who take an interest in these minute wonders of creation. The “ Sun animalcule” is very common in this part of Dorsetshire ; it abounds in pools where Desmidiee are found: they are ravenous feeders, not only upon the Desmidiee, but also upon all kinds of minute spores and animalcules. It was on examining some beautiful Desmidiee, a few evenings back, that my attention was arrested by the curious appearance of two or three very small Actinophrys floating very lightly upon the surface of the water in the form of a ball, with their delicate tentacular filaments perfectly erect all over their bodies ; in fact, they seemed to be floating upon these delicate filaments. This beautiful and curious appearance, so different from what I had generally observed, induced me to request Mrs. Boswell to look at it, but, while she was rising from her seat, I exclaimed, ‘ You are too late, the little creature has given a leap, and I have lost it!’ but upon moving the slide in the direction of the leap, I found the creature composedly resting in the usual manner upon the surface of the water— that is, in a flat position. This was not a solitary instance, for about five minutes after another gave a similar leap: the dis- tance must have been very great considering the size of the animal, as it was in the centre of the disc under Messrs. Smith and Beck’s 2-3rd object-glass with the second eye-piece, and I had to travel full an inch beyond the radius. These are the only two instances I have met with at present, not having made the little creature my peculiar study. I have frequently mounted the Actinophrys Sol with Des- midiee, but they generally burst at the edge of the sphere owing to the pressure of the glass cover, although they are to VOL, Il. 26 Busk on Avicularia. all appearance considerably thinner than Micrastorias denti- culata. Remarks on the Structure and Function of the AvICULARIAN and Vipracutar Oreans of the Potyzoa; and on their value as diagnostic characters in the classification of those creatures. (Read Nov. 23, 1853.) Tue Polyzoa, or, more properly speaking, one class of the Polyzoa characterized by the possession of a movable semi-cres- centic lip, furnished with a corneous rim, at the mouth of the cell,—the cheilostomata as | have elsewhere termed them, or Celleporina of Ehrenberg,—are, many of them, distinguished by the presence of appendicular organs affixed to one part or another of the cells of which the polyzoarium is composed. These organs are of two kinds, the one a sort of pincers, and the other consisting of a long, slender, movable seta. To the former set of organs, of whatever form, the term avicularium is here applied, and the latter are designated as vibracula. With respect to the structure of these organs of either class it is sufficient to remark that, however diverse their appearance may be, they are all constructed upon the same general type, that is to say, the organ consists of a hollow cup or receptacle containing two sets of muscles for the movements of its motile portion, the mandible, as I term it in the one case, and the seta in the other. Beyond this general conformity in type, however, my knowledge of the more intimate structure and contents of the cup in the vibracular organs, does not allow me to approximate them to the avicularia. The avicularia, besides the movable mandible, it may be observed, always have a corresponding fixed beak, the opponent as it were of the mandible, and necessary to constitute the organ, what I presume it to be, an instrument of prehension. This beak is needless, and is therefore wanting in the vibra- cula, and its absence in cases where the movable part is detached, would serve to distinguish one kind of organ from the other. I. The avicularia.— The first notice we have of the existence of these organs or rather of one form of them, is contained in Ellis’s account of what he terms the “ Bird’s-head coralline,” (Nat. Hist., Zooph., p. 36, pl. 20,) where he says, ‘On the outside of each cell we discover, by the microscope, the appearance of a bird’s head, with a crooked beak opening very wide.” Busk on Avicularia. ) 27 Mr. Darwin, in the ‘ Voyage of the ‘Adventure’ and ‘ Beagle,’ adverts at some length to these organs, and de- scribes their actions in the living state very graphically. They have also been described with great care by Dr. Van Beneden and the late Professor John Reid, and also by Nordmann and Krohn, the latter (as I extract from Dr. Johnston’s ‘ Hist. Brit. Zooph.’) classifying them under three different forms: 1, those which have the figure of the crab’s arms; 2, those which resemble pincers; and 3, those which are formed like bristles or hairs; the last corresponding to what are here termed the vwibracula. In a paper read before this Society, October 27, 1847, and published in the ‘ Transactions,’ I have described more particu- larly the structure of the curious and unique form presented by this organ in Notamia bursaria, pointing out, I believe for the first time, that the muscles were divisible into two distinct sets, one for the closure and the other for the opening of the mandible, with other minute particulars of their mecha- nical arrangement previously unnoticed; I also stated that the muscles not only in this organ but throughout, in this and other Polyzoa, are of the striped kind, or resembled those of the Brachiopoda more than of any other class in the Mollusca. I also indicated that the mandible and the beak of the cup were differently constituted to the rest of the organ, being com- posed of a horny instead of calcareous substance ; and that besides the two sets of muscles above noticed, the cup con- tained a “ peculiar body of unknown nature.” I believe that up to the present time our knowledge of these organs is pretty nearly limited to the above particulars. With respect to their homologies and functions, nothing but con- jectures have been offered; in fact, as regards the homo- logies of these organs with any existing in animals belonging to the same or any other class, no conjectures beyond the most vague have been offered. They may, perhaps, be regarded as analogous in function with the Pedicellarie of the Echino- derms, as well as with the little accessory cups filled with prehensile filaments, or thread cells, which are found in the Plumulariz and Campanulariade ; but, I conceive that any homology with these organs is quite out of the question. They are as nearly related to the claws of a lobster or the feet of a Pygnogonum.* * Mr. Huxley has pointed out to me several points of resemblance be- tween the avicularia, especially as to their mechanical and muscular ar- rangements, and the shells of the. Brachiopoda. An ingenious idea, and calculated to lead to the more serious consideration of the relationship between the Polyzoa and Brachiopoda, as suggested by Mr. Hancock d 2 28 Busk on Avicularia. Their structure so obviously indicates their aptitude for pre- hension, that the supposition of such being their function has been long entertained: and I have myself : no doubt whatever as to its being so; for, as Dr. Johnston observes, ‘ although they are too short to hand the prey to the mouth, yet, retained in a certain position, and enfeebled or killed by the grasp, the currents set in motion by the ciliated tentacula may then carry it within reach.” (‘ Brit. Zooph.’ p. 334.) Some time in the last year, a specimen of Scrupocellaria scruposa, if I remember right, was exhibited at one of our meetings, with a minute vermicule, retained in the grasp of its avicularia ; and the same thing seems to have been repeatedly noticed. An instance of the kind occurred to me when at the sea-side this autumn, and [ have made a figure to represent the occurrence (Plate IT. fig. 12). It 1s ofa portion of Scrupocellaria seruposa, two of the avicularia on which have, apparently simulta- neously, caught a minute vermicule which they retained with a most tenacious grasp. I kept the zoophyte under observa- tion for several days, in the living state, and during that time, in fact, till the whole died, the grasp of these organs was not relaxed ; and, although the movements of the captive were very active and apparently energetic, it was unable to liberate itself from the grim hold of its tiny but persevering antagonist. Another instance of the grasping propensity of these organs is exhibited in fig. 10, where two of them appear to be engaged in deadly combat. This figure is also intended to show the disposition of the muscles when thus employed. Considering, therefore, the conformation of the avicularia, and the instances in which objects of prey of different kinds have been noticed engaged by them, I think it is impossible to avoid the conclusion that they are for the prehension of ob- jects, either for the purpose of using them for food when dead and powerless, as suggested by Dr. Johnston; or it may be for purposes of defence. With respect to the structure of the avicularium, I aie already stated what is known; and have, in addition, only to remark that it hag occurred to me to notice a cirewmatamne hitherto overlooked, and which may eventually serve to throw some light upon the “ peculiar body” contained in the cell to which I adverted in my observations on Notamia. — It was in (‘ Ann. Nat. Hist.,’ 2nd Ser., vol. v. p. 198), than has hitherto been given to it. And with regard to this, it should be borne in mind, though per- haps the character is of no great importance, that all the Brachiopoda have striped muscular fibres, whilst for the most part the other classes of Mollusca, with some exceptions—Pecten, for instance—all te muscles of the unstriped kind, Busk on Avicularia. 29 that species, also, that I first noticed (in 1852) the fact that when the mandible is thrown back, or, in other words, when the avicularium is open, a slight prominence comes into view, covered with delicate setose hairs, which do not seem to be of - the nature of cilia, because they exhibit no motion. These minute sete appear to be seated’on the “ peculiar body ” above adverted to, and which again seems to be so connected with the muscles by which the mandible is closed, or rather, perhaps, to a membrane by which they are covered, or by which the opening of the cell is closed, when the mandible is thrown back, as to be protruded, simply by the throwing back of that process; so that the sete are then made to project beyond the level of the cup, and are withdrawn as the man- dible closes. Fig. 2 represents this apparatus in Wotamia. Fig. 7, the same thing in Bugula plumosa, and fig. 9, in Bugula avicularia. ‘These are the only three species in which, up to the present time, | have been able to perceive this arrangement; but not having had an opportunity of ex- amining the avicularia of any other, except Scrupocellaria seruposa, for the purpose, and in which I was unable to detect it (fig. 13), I am not prepared to say that it obtains univer- sally. It is probable, however, that in a modified form it may do so. I am inclined to the opinion that itis atactile organ, the object of which is to apprize the occlusor muscles of the contact of any minute floating object, upon which the muscles immediately contract, and either close the avicularium against the invasion of a foe or capture the appropriate prey. A second point that I have also observed in these organs, and which, I believe, has not been before noticed, is that the portion of the cup in which the muscles and the greater part of the peculiar organ (which might probably be regarded as a nervous ganglion) are placed, is closed in by a delicate mem- branous tympanum, which has a central perforation, through which the conjoined tendon of the occlusor muscles passes, and also a second smaller opening (at all events in B. avicularia), the object of which I do not know. This tympanic mem- brane is shown in fig. 8. So much for the structure and conjectural function of the avicularia ; and to proceed to consider the vibracula in the same particulars. 1. As to the structure of these organs, I have nothing new to offer. ‘They consist, as I have said, of a cup containing the muscular apparatus, and of a movable seta, articulated to the cup, and which appears to be moved in the same way as the mandible of the avicularia. This seta is in most cases simple and terete ; in others, as, for instance, generally in the genus 30 Busx on Avicularia. Caberea, it is toothed on one side; and in others, as in the species forming the family Selenariade, of which we have no British representative, the seta is very variously and curiously formed, in some being trifid or bifid at the extremity, and in one, Selenaria maculata, it is spirally contorted and minutely annulated, so as very closely to resemble the proboscis of a butterfly. As to the function of the vibracula, it would appear, in most cases, to be simply defensive. ‘The seta may be observed in almost constant motion, sweeping slowly and carefully over the surface of the polyzoary, and removing what might be noxious to the delicate inhabitants of the cells when their _tentacula are protruded. Another circumstance often to be observed with respect to these organs, is this, that each presents inferiorly a rounded perforation, as in Scrupocellaria and Canda, sometimes chan- nelled as in Caberea, which indicates the point of attachment of a radical tube or fibre. That this connexion with a radical tube, however, is not an essential attribute of the vibracular organ is sufficiently obvious from the circumstance that those tubes are frequent where no such organs exist; but where there are vibracula, the tubes invariably enter them, and not the cell itself. This is especially evident in the genus Canda, of which the British species, Canda (Cellularia) reptans, affords an instance. In the case of the Selenariade or Lunulites, 1 think it not improbable that the vibracula may be subservient to loco- motion. These organs, both avicularian and vibracular, appear to me to be of very considerable importance in a systematic point of view ; and, although from our imperfect knowledge of them, and in fact of the Polyzoa in general, the supposition can only be regarded as problematical, it seems not improbable that the presence or absence, especially of the avicularium, may be connected more directly with the intrinsic nature of the species upon which they are found, than has hitherto been supposed. It may, for instance, be the case, that those furnished with these offensive weapons live upon a kind of food different from that of the others who do not require such an aid in the capture or weakening of their prey. The Polyzoamay, per- haps, thus be divided into vegetable and animal feeders, or into feeders upon dead, and those which feed upon living organisms. One thing, however, is certain, that these organs afford, in many cases, excellent and available systematic characters ; and this part of the subject I will now proceed briefly to discuss. I have already stated that the accessory organs we are now Busk on Avicularia. 31 considering are divided into two kinds, apparently with dis- tinct functions—avicularia and vibracula; the one, probably prehensile, the other defensive. Of these, the avicularia are found by far the most extensively ; in fact, they are wanting in but few of the genera constituting the cheilostomatous class of Polyzoa. In employing them for the purpose of classification, it is necessary to subdivide them into three classes. 1, the pedunculate. 2, the sessile; and 3, the immersed, The two latter classes, however, run insensibly into each other, whilst the pedunculate form is obviously quite distinct, inasmuch as it presents an additional member, in the form of a basal joint. It is this form of avicularium to which the term “ birds,” or “ vultures’ heads,” is more pro- perly applied. It is well known in this form, as it occurs in Bugula avicularia, B. plumosa, and B. flabellata: it is also found in Bugula tridentata (Krauss), a South African species ; and in Bicellaria ciliata; whilst it is wanting altogether in Bugula neritina, Bicellaria grandis, and Bicellaria gracilis. A second modification of pedunculate avicularium, where it assumes the form of a long trumpet-shaped or infundi- buliform tube, exists in Bicellaria tuba. So far as I know then, at present, the pedunculate form of avicularium is restricted to the genera Bugula and Bicellaria, though it does not exist in every species of either genus, and in one, assumes a form quite different from the ordinary. All that can be said about it, therefore, in those two genera, is that where the avicularia exist, they are of the pedunculate variety. The true ‘“ bird’s-head” avicularia are always placed on the an- terior aspect of the cell, on one side below the level of the aper- ture, whilst the tubiform variety arises on the back of the cell. The sessile form of avicularium, as I have observed, may be subdivided into the projecting and the immersed. Of these, the latter is much the more extensively distributed : it is placed either at the angles or margin of the cells, or on some other part, usually of their anterior aspect, but some- times on the posterior: instances of the latter are presented in Caberea nuda, where the vibracular organs, so characteristic of the other species in the same genus, are replaced by what may be termed avicularia, though, in fact, they should more properly be referred to the vibracular type, inasmuch as the radical tubes enter their bases. The genus Retepora, also offers an instance of the posterior position of true avicularia ; but, with these exceptions, I am not acquainted with any other in which the avicularia are not on the sides or front of the body, as indeed, if our surmises with respect to their func- tion be well founded, might be expected. 32 Busx on Avicularia. Of angular imbedded avicularia, the numerous species of the genus Catenicella afford examples. ‘This organ, in fact, in that genus, often furnishing very satisfactory specific characters. In some, as C. plagiostoma, it is of gigantic size, in others very minute, and in one it seems to be aborted, being replaced by channelled processes, C. carinata. In several other species it is in some cells replaced by long ascending cornua or hollow spines, as in C. cornuta and C. taurina. The genera Menipea, Canda, Scrupocellaria, and Cellularia, are respectively distinguished by the presence or absence of avicularian and vibracular processes. The former are always of the sessile kind, either zmmersed, and at the superior and outer angle of the cell, or projecting and placed on the front of the cell, below the level of the aperture. In the genus Menipea, there is an angular, superior, imbedded ayicularium in many of the cells, and a projecting sessile organ on the front of the cell below the aperture, and no vibracula. The British species, Menipea ternata, affords an instance ; the other species similarly characterized, are—WM. cirrata, M. fuegensis, M. triseriata, M. ornata, M. patagonica, and M. multiseriata. The genus Canda, differs from Scerupocel- laria, mainly in the want of any avicularian process at the superior and outer angle; but the cells sometimes have a sessile avicularium in front, below the aperture. ‘This is particularly the case with Canda arachnoidea, in which the avicularia appear to occupy an unusual position: they do not seem to be seated on the fronts of the cells themselves, but to form a series affixed to the median septum between the two rows of cells ; and, what is very curious with regard to them in this species, they are apparently developed long after the completion of the cells, seeing that they are totally wanting in the upper and younger portions of the branches of the polyzoary, and gradually increase in size towards the inferior portion. In Scrupocellaria, we arrive at, the full development of these accessory organs; the species in this genus being all distinguished by their being furnished with both avicularia and vibracula. Of the former, one is always imbedded in the superior and outer angle, as in Scrupocellaria scrupea, S. scruposa, and S. Macandret ; whilst in others, such as S. ferox, and S. cervicornis, there are superadded to these, sessile avicularia on the front of the cell below the aperture, in the former species, of colossal dimensions. The genus Cellularia, again, is distinguished by the entire absence of both avicularia and vibracula. The British form Cellularia Peachit, affords an instance. The genus Caberea, except in the single species Hewett re- Busk on Avicularia 33 ferred to, and which might, perhaps, on that account, almost be regarded as the type of a separate genus, is distinguished, and very remarkably so, by the extraordinary size and curious arrangement of the vibracula on the back of the branches, which thence derive a very close resemblance to an ear of barley. It is in this genus that the vibracular organ acquires its ex- treme development. A British example is afforded in Caberea Boryi, a not uncommon denizen of the Channel coasts. In the genus Hmma, we have afforded an instance, in which the position of the organ may be used in the generic character. In the species belonging to this genus, the sessile, lateral avicularium is situated on a level below the aperture. £. ¢., Emma crystallina and E. tricellata. | The peculiar disposition and form of the avicularia, in Notamia, have been sufficiently adverted to in this and my previous communication to the Society. It would require too much of your time and too much space to enter very particularly into all the instances in which I have found the form, position, and existence of avicularia and vibracular processes useful in the classification of species. The above remarks, hasty as they are, will serve to give an idea of the extent to which they may be so employed ; and I would only observe, in addition, that a similar atten- tion to these organs will be found indispensably requisite for the due appreciation of specific and even generic distinctions, in the difficult and hitherto much confused families of the Flustrade, Membraniporide, and especially of the Celleporide, Escharade, and Selenariade. In Lepralia, particularly, in which genus I have placed nearly 60 species, I have found the use of these organs of the utmost importance, and easily avail- able. In fact without them it would have been a most difficult task to marshal into due order such an irregular and mutinous host. For the mode in which I have so employed this character, | must refer you to my ‘ Catalogue of Marine Polyzoa,’ just published by the British Museum, and will conclude by saying, that the names of the Polyzoa here em- ployed are those by which they are distinguished in that work, in which the appropriate synonyms will be found. d4 Structure of a peculiar Combustible Mineral, On the Minute SrructureE of a peculiar CompustiBte MineE- RAL, from the Coal Measures of TorRBANE-HILL, near Batu- GATE, LintirHGowsHIRE, known in Commerce as BoGHEAD CannEL Coat. By Joun Quexerr, Professor of Histology to the Royal College of Surgeons of England. (Read Nov. 23 and Dec. 21, 1853.) Tue substance in question has lately excited the greatest interest in the scientific world ; and_a trial, second to few in importance, has recently taken place in Edinburgh, having for its object the determination whether the Torbane-hill mineral should be called a coal or not, and whether it should be included in the missive of agreement for a lease, and let as coal. Those of my hearers who may wish for a particular account of the matter in dispute, and a statement of the facts brought forward, both by the pursuer and defender, or, with us in England, plaintiff and defendant, I would beg to refer to Mr. A. W. Lyell’s Report of the trial, published by Messrs. Bell and Bradfute of Edinburgh. ° Upon this trial no less than seventy-eight witnesses were examined—thirty-three for the plaintiff, and forty-five for the defendant. They might be classified as geologists, mineralo- gists, chemists, microscopists, and practical engineers, such as gas managers, miners, &c. With four of these classes of scientific witnesses I have no immediate concern, and will, therefore, leave them to settle their own differences ; but not so with the microscopists, with many of whom my opinions are entirely at variance. In order that you may all fairly understand the nature of this question, as far as the microscopical observers are concerned, I will, in the first place, give you a detailed account of the minute structure of the Mineral itself. Secondly, I will give a brief description of the minute structure of Coal. Thirdly, I will lay before you the whole of the evidence given by the microscopists on the part of the pursuer as well as the defender; and lastly, make a few remarks upon the conflicting testimony of some of the witnesses. I wish that the matter had fallen into abler hands than mine; but having been intimately acquainted with the mineral in dispute for some time past, and as two of the oldest members of this society, Mr. Bowerbank and myself, have had their competency called in question, and have been repre- sented by the Judge as no botanists, and, therefore, “are not, as [ understand, conversant or skilful in fossil plants,” and the society itself not having escaped his ridicule, the jury being from the Coal Measures of Torbane-hill. 39 informed that the Microscopical Society of London is “a learned body, who make it their object to pry into all things,” I cannot be silent; but I would have you keep in mind that my sole motive in now appearing before you, is, the cause of truth, and in this cause I come forward fearlessly, but honestly, to state that the Torbane-hill mineral is not, micro- scopically speaking, a Coal ; that it is not like any of the combus- tible substances used in this country as Coal ; and that, althouyh possessing some of the properties of Coal, it is, notwithstanding, a mineral sui generis, having avbasis of clay which is strongly impregnated with a peculiar combustible principle, and that when plants are found in it, they are accidental, and have no more been concerned in the formation of the mineral than has a fossil bone in that of the rock in which it may be imbedded. 1. External characters of the Mineral.—Of these you will have a good general idea from the specimens on the table before you. It frequently occurs in seams of some considerable thickness, and always in the neighbourhood of coal, some- times in immediate contiguity with it, but at other times, according to Mr. Ansted, separated from it by a layer of fire- clay. The colour is generally a dark brown or black, without lustre, but varies according to its position in the seam; its specific gravity is 1%, or 1,%, water being as 1. When scratched with a knife it exhibits a brown streak, in which particular it is said to differ from all the known coals with one or two exceptions. It is tough and not so brittle, but that very thin sections may be made of it, and when struck with a hammer, it emits a dull sound; the remains of plants, espe- cially Stigmaria, are of constant occurrence, and can be dis- tinguished by the naked eye without difficulty. 2. Characters exhibited under the Microscope.-—When a small chipping or fragment, about half an inch square, is examined as an opaque object under a power of 40 or 50 diameters, it will be found to consist of masses of a yellow material, some being of irregular figure, others more or less rounded, imbedded in a granular matrix, varying in colour from a yellowish-brown, almost to black. The whole of the mineral appears to be composed of granules of various sizes, and although the part which has been termed the matrix is black, this also will become brown if the surface be scraped. The scraping can readily be done under the microscope whilst the fragment is being inspected ; and, curiously enough, both the surface of the mineral, and the minute particles scraped off, assume a light-brown colour. Portions of plants imbedded in the mineral can, by the process of scraping, be readily distinguished from the impressions of plants ; the former are 36 Structure of a peculiar Combustible Mineral, always black and do not alter in colour, whereas the latter become brown, the same as other parts of the mineral. 3. Characters exhibited by sections under the Microscope— ‘There appear to be two principal varieties of this mineral, one of a yellowish-brown colour, the other nearly black, these differences, however, are chiefly dependent upon the position the particular fragment selected for section occupied in the block. When the first variety is reduced sufficiently thin to be transparent, which can be done without much difficulty, it will be seen to consist of a tolerably uniform, yellow mass, whilst the darker variety is either of a rich brown, or of a pale-yellow colour, minutely spotted with black granules. When the first or yellow variety is examined with a power of 50 or 100 diameters, it exhibits an appearanee of being made up of a mass of transparent rounded particles or spherules of a rich yellow or amber colour, varying in size from the zyg,th to the s}5th of an inch (as shown in Plate III, fig. 1), whilst the darker variety (fig. 2) is composed of two essential ele- ments, one in the form of the transparent rounded particles, the other minutely granular, but black and opaque, and occupying the spaces between the yellow particles. In the first variety of this mineral, or that which is of a yellowish- brown colour in section, the yellow particles above alluded to are so very abundant, that they appear almost to make up the entire mass, whilst the dark granular element is small in quantity. In the second, or dark variety, the strictly granular opaque element is much more abundant; it sometimes occurs in large patches, having none of the yellow particles with it, but more frequently it is found in the form of a coating to the particles themselves. When the yellow particles are of large size, they always exhibit more or less of a radiated structure internally: this appearance, which is well represented in figs. 1 and 2, very much resembles that of a radiated frac- ture, or a species of crystallization. I shall now, for the sake - of distinction, call all these yellow particles, or spherules, the bitumenoid or combustible portion of the substance, and the dark, granular part, I shall consider as the strictly mineral, or earthy ingredient. In some specimens there is a tolerable regularity in the size of the yellow particles, and in the disposition of the black mineral ingredient around them, so much so that an unprac- tised eye might, at first sight, consider its structure to be cel- lular: that such mistakes have actually been made you will very soon have an opportunity of learning. Having told you what is the usual structure of the substance in question, [ must beg you to understand that it matters little from the Coal Measures of Torbane-hill. — 37 in what direction the sections are taken; whether cut verti- cally, horizontally, or obliquely, there is no perceptible difference in the structure, and I say it without fear of con- tradiction, that no one, however skilled in microscopical observation could, from the imspection of a single specimen, state the direction in which the section had been made. Such is not the case with coal, as will hereafter be shown; a single inspection is sufficient to enable a practised microscopist to determine the actual direction of the section, whether trans- verse or longitudinal. Examination of portions of the Mineral having Plants imbedded in their substance—I have already stated that plants and the impressions of plants are not uncommon in this mineral ; of these | have made numerous sections and chip- pings, and most instructive they all are. The plants appear to be principally Stigmarie, and exhibit more or less of the three tissues known to botanists as the cellular, the woody, and the vascular ; and should one or more of these be present in any section, the minutest fragment even of a cell or vessel can be readily recognised by a practised observer; they, as it were, stand out boldly from the mineral matter in which they are imbedded, and (as shown in figs. 3 and 4) can be distinguished in all cases by their rich brown colour; but such plants I not only consider as extraneous and not forming the bulk of the mineral, but such plants my investigations lead me to conclude rarely if ever form coal; at all events no coal that [have yet examined has ever exhibited the least trace of being made up of such plants as are so commonly seen imbedded in this mineral. Even the coal lying upon this mineral, and running through it in every possible direction, is composed principally of woody tissue, and not of plants such as these. Examination of sections of the Mineral having Coal in juxta- position.—The first specimen of this kind which I had the opportunity of examining was brought by Mr. Bowerbank himself from one of the Torbane-hill pits. From this speci- men several sections were taken; one of them slightly mag- nified, is represented in Plate V., fig. 1. I regret I cannot show you the specimen itself, it being lodged in the Court of Session, in Edinburgh ; but [ have been favoured with a some- what similar one through the kindness of Mr. Gratton. As the block lay in the pit, the coal was situated below the mineral in the position I now hold it, and you will readily be able to distinguish the one from the other by the naked eye; but when viewed with a power of at least 50 diameters (as shown in Plate III., fig. 5), the smallest fragment of the coal that may happen to be mixed up with the mineral may be 38 Structure of a peculiar Combustible Mineral, readily traced ; even a part so minute as a single woody fibre can easily be recognised. In some specimens, the line of demarcation between the coal and the mineral is not very decided, owing to the coal and the plants found in connexion with it being so intimately blended ; in all such cases recourse should be had to the streak, as the best guide to distinguish them. In every part of the block containing coal and coal plants, the streak is black ; but in the smallest portions of the mineral it is brown. It is a curious fact, however, that in the specimen now before you, three kinds of structure are visible to the naked eye: Ist, true coal; 2nd, a mixture of coal with a few coal plants, principally Stigmarie ; 3rd, the mineral. When sections are made through the block in two directions at right angles to each other, the coal and the mixture of coal and plants will exhibit a structure corresponding with longitudinal and trans- verse sections of wood, but the mineral is the same in both sections. The yellow particles occupy all the interstices in the coal, and vary in shape, according to the spaces they have to fill (as shown in fig. 5); but whether they be elongated or of circular figure, more or less of the radiated structure is present in every particle. In such sections the vegetable tissues may be distinguished from the earthy ingredient by their rich brown colour. Examination of the Powder.—W hen the Torbane-hill mineral is reduced to powder, and examined either in water or in Canada balsam, the combustible and incombustible portions can be well seen; the one occurring in the form of the yellow or amber coloured particles before noticed, and constituting full two-thirds of the mass (as shown in Plate IIL, fig. 6), whilst the remainder is made up of minute opaque granules, having occasionally amongst them some which are quite transparent, and probably siliceous. Characters of the so-called Coke and of the Ash.—Three por- tions of the coke of the Torbane-hill mineral, each about 4 inches square, obtained from a gas-retort by Mr. Gratton, were of a greyish colour, and when scraped became perfectly black. The remains of plants were very visible throughout the substance of each, and were even more distinctly seen in the specimens of coke than in the mineral itself before being subjected to heat, for every part, however minute, had assumed a silvery appearance. When a flat piece of the coke, about half an inch square, is examined as an opaque object under a power of 50 or 100 diameters, it presents a peculiar sponge-like structure ; and when contrasted with a portion of the mineral, it will be noticed that all the yellow particles from the Coal Measures of Torbane-hill. 39 have disappeared, and a pitted appearance is produced, the pits being nothing more than the cavities in which the yellow particles were lodged, and the walls of the pits being the granular earthy ingredient which at one time surrounded the yellow particles. When small fragments of the coke are scraped off and subjected to a power of 250 diameters, none of the yellow combustible principle is present, the entire bulk being made up of dark granular masses. If the mineral be burnt in anopen fire, the ash will be nearly white; and when examined microscopically, no trace of the yellow com- bustible matter will be seen, and the granules (as shown in fig. 7) will be very minute, and of a light colour. These appearances will be constant, if care be taken to select a part of the mineral in which no traces of plants are visible to the naked eye; but if portions of plants be present, they will be readily recognised by their woody and vascular tissues. The principal distinction, therefore, between the coke of the gas- works and the ash is, that in the former the granules are larger and blacker than they are in the latter. From these and numerous other observations, I con- clude that the mineral in question is a clayey substance, im- pregnated with a combustible material occurring in the form of rounded particles of a rich yellow or amber colour, but whether these particles be bituminous or not the chemists must decide. What I have already stated refers exclusively to the Torbane-hill mineral, and no mention has yet been made of the structure of coal. Under this head I could enter into a detailed account of most of the well-known varieties of British coal, my knowledge of which has been principally derived from a careful investigation of sections made by myself and by my friend Dr. James Adams, of Glasgow; and I am happy in having this opportunity of bearing testimony to the correctness of the observations of Dr. Adams, upon which his opinions had been formed prior to my having the pleasure of his acquaintance. Were I now to describe these, I fear you would be kept here many hours; but it is the intention of Dr. Adams and myself, at no very distant period, to read a paper on the minute structure of the principal kinds of British coal, before the Geological Society, as we deem that the most fitting place for such a subject. For our present purpose, therefore, it will be merely necessary for me to give, in as con- cise a manner as possible, the results of the investigations of Dr. Adams and myself on this point ; but I would have you understand that although I give youa general description of the structure of coal, | have with me the specimens from which you will be enabled to judge for yourselves whether my state- 40 Structure of a peculiar Combustible Mineral, ments be correct. I am fully aware that the prevalent opinion with geologists and botanists is, that coal is made up of fossilized vegetable matter, and that this vegetable matter may consist of stigmariz, ferns, mosses, &c.; in short, of a great variety of vegetable substances. My investigations, however, lead me to believe that the basis of coal is essentially a peculiar kind of wood, and that when ferns, stigmariz, lepidodendra, and other plants occur in coal or its neighbourhood, they should be considered foreign to the coal, as these plants, before noticed, are to the Torbane-hill mineral. However contrary this may be to our preconceived notions, yet all the sections on the table before you, on a careful examination by an unpre- judiced observer, can lead to no other conclusion. I believe that there are in this room at the present time more sections of coal than any private individual has ever yet produced before a scientific assembly, and it is from these specimens, and from the study of these alone, that I am warranted in making this assertion. ‘The botanist will remember that most of the plants generally considered as forming coal, are such as on section will exhibit more or less of the cellular, woody, and vascular tissue: now it is a remarkable fact, that most of the plants visible to the naked eye in the ‘Torbane-hill mineral, as well as those lying in the strata above and below coal in general, are those which may contain spiral or other vessels; but, judging from all the sections of coal now before you, as well as chippings of others too numerous to mention, I am forced to the conclusion that such plants rarely if ever form coal, the basis of coal being essentially wood, of what kind, however, I will not at the present stage of the inquiry venture to mention, but I will state thus far, that it approaches more nearly to that of the Coniferee than any other wood ; because in the Conifer, as we know them in this country, there are few if any vessels or ducts in the woody part of the trunk, but occasionally cellular tissue in what are called the turpentine vessels, the entire bulk being woody fibre. Such is the case in coal. In all the sections that I have examined of undoubted coal, I have as yet found no trace of a spiral vessel or a dotted duct, but in one or two instances where the woody structure has been very evident, as shown in Plate V., fig. 3, the fibres were evidently dotted. External Appearances of Coal.—These must be so well known to most of you, that I need not dwell further upon them than to particularise one or two kinds which approach nearest to the Torbane-hill mineral in general appearance. The most remarkable of these is from Methil, in Fifeshire, and known as the Brown Methil. So peculiar is it, that when scratched with a knife, the streak is brownish-black From the Coal Measures of Torbane-hill. 41 in colour, somewhat resembling that of the mineral. There is also another variety of coal, termed the Black Methil, but in this the streak is black, as in all other coals. _Yet the microscopic characters of both these varieties are very similar, and differ in no respect from coals generally. A curious fact, however, I learnt from the chemists in Edinburgh, that the composition of the Brown Methil came nearer to that of the Torbane-hill mineral than any of the other known coals did ; a fact which is borne out by the similarity in their external appearance, Examination of Coal by the Microscope.—If a small cubical block of any kind of coal be examined under a power of 50 diameters, four of its six sides will exhibit more or less of a fibrous structure, precisely like that of wood ; the other two sides, if perfectly flat, will appear bright and polished, and show very little structure: these correspond to the transverse sections of wood. ‘Treat the Torbane-hill mineral in the same way, and how very different are the results! Nearly the same structure will be found on all its sides, but in none is there the least trace of a fibrous arrangement. Examination of Sections of Coal by the Microscope.—lf a section of any well-known coal, cannel or otherwise, be reduced sufficiently thin to be transparent, a work sometimes of considerable labour and difficulty, it will be found to ex- hibit one of two structures, according to the direction in which the section has been made. These, for the sake of distinction, may be called the cellular and the fibrous; the first corre- sponding with a horizontal section, the second with a vertical section, of wood. If it so happen that a section taken at random from any specimen of coal should exhibit one of these structures above named, by cutting at right angles, the other will be found. Thus, for instance, if the first section should correspond to a horizontal section of wood, the cut at right angles to it will correspond with the vertical one; and, of course, if the section be an oblique one, an intermediate structure would be observed. ‘This remarkable fact is con- stant in all the coals I have examined, and a knowledge of it enables the observer to tell at once whether any section taken at random was a horizontal or a vertical one. How strangely different this from the Torbane-hill mineral! Cut that mineral in any way you please, and there will be little or no difference in appearance. The structure of the transverse sections of coal is so very peculiar and so characteristic, that I must briefly _ point out the means it affords of distinguishing coal from any other modification of vegetable tissue. The peculiarity con- sists in this,—that, in the midst of a black opaque ground, VOL. I. e 42 Structure of a peculiar Combustible Mineral, numerous brown transparent rings, each having a black dot in the centre, are interspersed ; they appear like transverse sections of thick-walled cells or of woody fibres. In some coals they occur in close proximity to each other, as in woods generally: in other cases they are more or less separated, either by the black material before alluded to, or by a network of rather smaller rings, in which the central dot is absent, There are many coals, especially some of the common domes- tic kinds, in which it is difficult to recognise this structure in every part of the section; in these-coals a rich brown struc- tureless material—bituminous or not I cannot say—seems to be in excess, and so obscures the characteristic appearances of the rings. In longitudinal sections the woody fibres are generally well seen, and a tendency to split in the direction of their length (as shown in Plate V., fig. 5), may always be observed. Amongst the fibres may be noticed certain elon- gated cells, of a rich brown colour, having a dark line running down through the centre: these are constant in all coals, and when divided transversely, appear as the rings before noticed. Their size is tolerably uniform in many coals (as shown in Plate V., fig. 2). Mr. Witham was acquainted with the differences between a longitudinal and a transverse section of coal, as may be seen on referring to the 2nd edition of his work on the “ Fossil Vegetables of the Carboniferous and Oolitic Deposits ;” both the rings and the elongated cells are well figured, and his remarks on the value of investigating the microscopic structure of coal, are very excellent. ‘The absence of vascular tissue in the numerous sections of coal, made both by Dr. Adams and myself, would lead to the supposition that the wood of which it is composed must approach very near to that of the Conifere. Examination of the Powder of Coal.—When coal is reduced to a fine powder, and examined either in water or in Canada balsam, it will be found to consist principally of short opaque cylinders or fibres, occurring singly or in bundles, and of angular dark-brown plates of various sizes, probably composed of bituminous matter (as shown in Plate V., fig. 7); the remainder of the mass is made up of minute transparent particles of silica, with an occasional mixture of fragments of cells and fibres. Many blocks of coal have a fine dull black powder on two of their outer surfaces, which will make the fingers very black: this I call the charcoal layer, and in it will be found fragments of woody tissue of cells, and even of vessels. My investigations lead me to believe that this layer is derived from plants which existed at the same time as the coal-wood, but were not capable of being converted from the Coal Measures of Torbane-hill. _ 43 into true coal, but having been subjected to a great heat, their remains are left as a species of charcoal. Some speci- mens of the Torbane-hill coal have a large amount of this charcoal upon their upper and under surfaces, and in it, vessels of various kinds will occasionally be found, although such vessels do not occur in the solid coal itself. Examination of the Ash of Coal—TVhe brown ash of coal, with the exception of particles, probably of silica, is almost wholly composed of vegetable remains, some of which pro- perly belong to the coal itself, whilst others are derived from extraneous plants which have been mixed up with it. Every kind of tissue which has been described as proper to the coal may be met with in the ash, when not too much burnt. The remains of woody fibres and cells are the most common con- stituents, but flat, very opaque, irregular masses, such as are shown in Plate V., fig. 4, and which evidently correspond to portions of transverse sections of wood, are frequently found. Portions of siliceous cuticle, probably of grasses, as shown in fig. 6, from a drawing by Dr. Adams, are far from being uncommon. In short, when the indications of the woody structure of coal are very faint in sections, they are well ex- emplified in the ash. Sections of Welsh Anthracite (which I believe to be a fossil coke) are most difficult to obtain, and when made, afford very unsatisfactory evidence of vegetable structure: when, however, the ash is examined, the presence of woody tissue is unquestionable. The Torbane-hill mineral has been most carefully examined by my friend Dr. Adams, and as his investigations were car- ried on independently of mine, it will be satisfactory that you should be made acquainted with the conclusions he has ar- rived at after a laborious series of examinations. They are as follow :— ‘¢ The most interesting example which could be adduced, illustrative of the differences in essential characters, as demonstrated by the microscope, between substances supposed by commercial men to be identical, is found in the Torbanehill mineral, known also by the name of Boghead coal. In the lawsuit previously alluded to, much of the scientific evidence regard- ing this mineral was of a very conflicting character, so much so that the court virtually set aside the scientific evidence, and decided on the legal merits of the commercial bargain. “The importance of the interests involved, and the high character of the witnesses examined, have made this trial very celebrated ; and it is from an excusable desire that the grounds of the opinion I expressed at the trial should be understood, that I now seek to place them on record. I will, however, confine my remarks to a very short summary of my observations made upon the Torbanehill mineral, leaving a fuller detail with my friend, Professor Quekett, who gave joint evidence with me, and with whom I have discussed and investigated the whole subject of my ee 44 Structure of a peculiar Combustible Mineral, present communication with a most pleasing and perfect accordance of observation and opinion. ‘¢ The following are the principal results :— “¢T, A very thin section of the 'Torbanehill mineral, when viewed by transmitted light, has a pale-yellow colour, is semi-transparent, and, with the exception of very slight variations in the depth of the colour, probably dependent on the varying thickness of the section, it appears to be a uniform homogeneous mass. The same appearance is constantly presented notwithstanding that the sections are taken in various directions. While this is the usual appearance of what may be termed the average specimens, viz., of portions taken from the centre of the block (or seam), yet, in sections taken from near the outside, or lower portion of the seam, I find a, quantity of small opaque particles (evidently earthy matter) in the form of a fine powder, scattered through the yellow-coloured medium forming the mineral. In such specimens the transparent yellow substance forms irregular rounded granules, and the opaque powder is either sparingly diffused over, or forms an outline or partition, more or less perfect, around the exterior of the yellow granules. These granules vary much in size, being as small as 1-4000th of an inch, and of every intermediate size from that up to 1-200th of an inch in diameter. *¢ In sections taken from the outside, as above described, I have observed oceasional patches of opaque material of every irregular form, and which I could not liken to any other substance, unless I spoke of them simply as specks of dirt. In the same sections I have also found stalks of plants and fragments of wood. ‘These opaque patches and vegetable fragments are always distinctly isolated ; that is, they do not in any way resemble or form part of the substance of the mineral, otherwise than by being involved or contained in it, and their presence, therefore, can only be considered accidental. ‘‘ IJ. When reduced to a fine powder, and examined under water, all the particles of the mineral have a clear, and generally a sharp outline, are of an irregularly rounded form, and may be described as of a uniform granular appearance. About 7-10ths of the granules are very translucent, and of a light amber or yellow colour. About 2-10ths of the particles (also translucent) partake more of a flat, angular shape, and are quite colourless, probably consisting of siliceous matter. The remainder of the powder consists of dark semi-opaque particles. ‘ ‘*¢ In specimens of powder taken from an outside portion of the mineral, there is observed a larger proportion of the semi-opaque particles, together with the occasional appearance of vegetable stalks, rough fibrous frag- ments, and delicate fibrils of microscopic plants. With these special exceptions, the powder gives no trace whatever of organic structure. “ TII. The ash of the mineral, when examined under water, presents a considerable quantity of the colourless particles already described, lying at the bottom of the fluid, while a filmy particle of transparent particles floats on the surface. No trace whatever of organic structure is here observed. “« Polarised light does not in any way affect the appearances of the mineral. I have, in consequence of these investigations, a firm conviction of the non-identity of the Torbanehill mineral with coal, setting aside those differences which may be found to exist under mineralogical, geological, or chemical investigation. JI cannot conceive how the evidence of Amorphisin in the one case, and of intimate vegetable composition and of regular structure in the other, can be explained away, or any other view than that of non-identity of physical structure. In coal we find a well- characterized organization, or regular arrangement of its component parts from the Coal Measures of Torbane-hill. 45 so distinctly peculiar, that I should question the competency, at Jeast, of any party who, after comparing the microscopic appearances of the two substances in question, could hint at a resemblance. The Torbanehill mineral, on the other hand, is as thoroughly devoid of organic structure, or of any rezular arrangement of its component parts, as is a mass of jelly or a conglomerate of masons’ mortar.” I will now, in the third place, proceed to read the evidence given by the witnesses for the pursuer and the defender. Professor QUEKETT.—LHxamined by Mr. MACFARLANE. You are one of the Professors in the Royal College of Surgeons in London ?—Yes. What chair do you occupy ?—The chair of Histology. What is the object of that study?—An examination of the minute tissues or structure of plants and animals. I believe you have devoted a great deal of study and attention to that subject ?—Yes, for the last twenty years. You have published a catalogue of the preparations in the College of Surgeons of London, descriptive of the various tissues ?— Yes. And you have yourself a very extensive collection ?—Yes, I believe the largest in Europe. 3 You conduct your investigations with the aid of the microscope ?—Yes. And have you made careful investigation into the structure of the various coals, as well as other minerals P—Yes. Have you in this way had occasion to examine the most of the known coals in England and Wales ?—Yes, about seventy varieties. Have you also examined varieties of Scotch coal >—Yes. What have you discovered to be the tissue of coals ?—They show us a woody tissue. Have you found structure of that description in all the varieties to which you have referred >—AlIl the varieties of coal. More or less distinct, I suppose >—Yes. Now, have you examined the Torbanehill mineral ?—Yes, in every possible way microscopically. Were specimens of the mineral delivered to you ?—Yes, some time ago. By whom ?—By Mr. William Forbes and a Mr. Rettie. I have the specimens here. Now, did you subject those specimens to a very careful examination ?— Yes, very careful. You tried them in every possible way, and repeatedly ?—Yes, and repeatedly. Did you make a great many sections out of them ?—Yes, an immense number. eo as to give you every possible opportunity in tracing their structure ? —Yes. What result did you come to?—That the Torbanehill mineral is dif- ferent from anything that I ever saw in my life before. Did you discover any trace of organic structure P—Yes, when plants are accidentally mixed with it. You were enabled to ascertain when it was so ?—Yes. Perfectly ?—Perfectly. But in the substance itself ?—No structure—that is, what the micro- scopists would term an organic structure. Is it different in that respect from all the varieties of coal you have examined ?—Decidedly so. 46 Structure of a peculiar Combustible Mineral, Did you get illustrations P—Yes, I have illustrations. (Produces same.) I think you will come to a better understanding of the thing from those illustrations than from the specimens. ’ Explain what that is (referring to illustration shown to the jury).—This is a section of the Torbanehill mineral, or rather a granular section, and in it you will observe some yellow matter that burns—whether bituminous or resinous you must go to the chemists for. The black part is the strictly mineral part. What is the mineral matter to which you refer ?—It is the dark granular matter. Lord-President,—I understand that these illustrations show the bitumen and the mineral at different places ?-—Yes, my Lord. » Mr. Macfariane.—Now, then, do the illustrations of your coal investi- gations exhibit a different appearance ?P—Decidedly. Now, you say the mineral substance there is granular, is it so in the coal?—Not at all, except when visible to the naked eye. In coal, you can see mineral structure by the naked eye, but to that I do not allude; but under the microscope you can tell that is a totally distinct thing from the coal itself. What I mean is, that in specimens of coal you can often see crystallized matter with the naked eye. Is that extraneous P—I would say so. But when subjected to the microscope ?—It exhibits a totally different structure. It is not granular; it depends entirely on which way the specimen of coal is cut. If cut in one direction you will either see a cellular or fibrous appearance. Indicative of what >— Woody tissue. You have, I suppose, made sections in all the specimens of the Torbane- hill mineral—in all the various ways you have made sections of the coal ? —Yes. And you have found in all the different sections a decided difference, showing them in your mind to be different substances ?-—Certainly. Then, judging from all your experience and investigation, do you con- sider this Torbanehill mineral to be a description of coal or not ?—Certainly not. Have you any illustrations of coal there ?—Yes, I have a most remark- able illustration—perhaps the jury will understand better by this than anything else. JI have here a section of the mineral and coal in juxta- position ; this has been cut by Mr. Bryson, lapidary, and you will be enabled to see whether coal or mineral. The woody section is shown by the dark colour, the mineral by the other. Are those illustrations of longitudinal, or transverse sections, or what sections P—That of coal is longitudinal, and of the mineral it is supposed to be the same, because they are in juxtaposition. Suppose a transverse section—what differencer—In the Torbanehill mineral a section at right angles would present precisely the same cha- racter, but the coal would present another character, that character being shown in this lower drawing (exhibiting it to the jury). You will notice that the coal runs through that mineral. You can trace it by its minute tissue. You examined some of the Scotch varieties of coal?—Yes, many varieties. Did you examine the Methil?—Yes, of two kinds, I believe known by the names of the brown and the black. Did you discover vegetable structure there ?— Yes. Decidedly in both ?—Decidedly in both. And in that respect different from this Torbanehill mineral ?—Certainly. from the Coal Measures of Torbane-hill. Aq You mentioned at one time that you had observed the presence, in some of those coal specimens, of fossil plants ?—Certainly. Could you see them with the naked eye?—Yes, in those specimens of the Torbanehill. Have you seen them. in coal in the same oa ?—Yes, but I consider them extraneous or isolated examples. Cross-examined by Mr. Neaves.—Is the structure of coal uniform in general?—It is so tar uniform that the various transverse sections are uniform, and so are longitudinal. Equally visible in all places of the coal ?—Yes, in all places, except, as 1 have stated before, where you have mineral that is foreign to the coal. What mineral matter do ie allude toP—The chemists must decide that. You only speak to appearances rP—Yes, And the same formation in all?—Yes; the plants differ; I believe there are two kinds of plants or tissue that essentially form coal, But they present the same appearance ?—Yes, but those plants are not traceable in the same specimens of coal. ‘That in the neighbourhood of Glasgow may be different from the coal found in the neighbourhood of Edinbur gh. Can you distinguish the one plant from the other?—Yes, in the longi- tudinal section. And you never found any portion of any coal without exhibiting the same permanent structure ?—Certainly not. Where did you get that specimen you showed us of the two coals together ?—That was taken by Mr. Bowerbank from the mine two or three days ago, and the drawing was taken from a magnified representation of one of the sections. Lord President.—Let us take down what those specimens are if they are to go in, but I thought they were to be taken away by the witness. Dean of Faculty.—No. 25 represents that yellow matter of which the witness spoke; No. 26 is the drawing of that highly-magnified section ; Nos. 28 and 29 are the specimen and the drawing; and No. 27 is the appearance presented by the two different sections of coal itself, the one longitudinal and the other transverse. Witness.—There is one thing I would wish to state, this—I came here to speak the truth, and it may be testimony for or against my evidence, when I say that all that which may be supposed like vegetable structure in the Torbanehill mineral disappears when the structure is thin. Dean of Faculty.—When you speak of that which appears as vegetable structure, you mean those isolated fossil plants?—Yes. I would also allude to the fact that a book was published in this city twenty years avo, by Mr. Witham, of specimens made by Mr. Nicol; and this was the first representation of this vegetable structure. Dr. JAMES ApAMs.—ZHaxamined by Mr. MAcrarLane. You practise as a medical man in Glasgow P—I do. Have you devoted a good deal of time ‘and study to observations by the microscope ?—I have. For a considerable time back ?—For many years. re you subjected to examination by the microscope various minerals ? —I have. Extensively ?—Extensively. Varieties of Scotch coal P—Yes, a great many. Most of the known varieties ?—-Most of the known varieties. Have you examined the Torbanehill mineral ?—I have. 48 Structure of a peculiar Combustible Mineral, Recently ?—Recently. And did you subject it to a very careful investigation ?—Very careful. In various forms ?—Yes. Now, will you tell me what those Nos. of process are, No. 259 to 263, both inclusive ?—259 represents sections of various specimens of the Tor- banehill mineral, as seen under the microscope. From the centre of the same, from the outside or bottom, and also from the outside of block P—Yes. What is the next No. ?—260, representing two sections of coal, termed to me cannel coal—Duke of Hamilton’s cannel coal; the one represents what I have termed a longitudinal section, and the other a transverse section, drawn by myself. The next No.?—Is 261. This represents a drawing of what was termed to me Lesmahagow, Ferguson’s cannel coal—two sections drawn from specimens made by myself; but the drawing made by an artist named Donald, of Glasgow, under my eye. And you have no doubt they are correctly done ?—No aouths very faithfully made. The next No. ?—262, representing sections of—1st, what is termed Jordanhill cannel coal. The one is longitudinal of Jordanhill, the other is a transverse section of a coal called Cowdenhead, given tome. This one, 263, which represents three drawings—two transverse and one longi- tudinal; a transverse section of Jordanhill cannel coal, drawn by a medical gentleman of the name of Risk, under my eye, a faithful delinea- tion ; the other is a drawing of cannel coal procured from the Glasgow Gas Works, called Knightwood coal; and there is also a longitudinal drawing of Knightwood. Those three drawings were made under my eye by Mr. Risk. Did you subject the powder of the Torbanehill mineral to the micro- scope ?>—I did. Having applied a little water ?—Yes. What did you discover to be the particles?—Those particles have a clear granular shape, they are of an irregular rounded form, and I say may be described as exhibiting an uniform granular appearance. Any further description ?—About 7 of those granules are very translu- cent, and of a light-amber colour. About #%, also translucent, partake more of a flat or angular shape in their outline, and are quite colourless ; and there are a few particles of a dark or semi-opaque matter. Now have you examined coal specimens in the same way ?—I have. What were the results ?—They differed very materially ; the particles of cannel coal which I took as being the more compact coal, are found of various sizes, and in form generally flat, angular, or oblong, with fibrous character; the edges generally rough and as darkly opaque as in the centre. Have you examined the ash of the Torbanehill mineral ?—I have. When you said that the coal particles were of different sizes, were the particles of Torbanehill mineral of various or the same size When I examined them under a high power I found the Torbanehill to be also of various sizes. You examined them with the aid of a microscope carefully ?—Yes. What results?—I found it very difficult to describe the appearance, because it seemed to consist of a film or congeries of structureless particles. I got nothing tangible almost to lay hold ‘of. Iconsider most of those consisted of the colourless particles which I have mentioned as having been found in the powder, viz., the flat, angular, and perfectly transparent particles. from the Coal Measures of Torbane-hill. 49 I understand, Doctor, when you say perfectly structureless, that there was no organization ?—No organization ; they have form. No trace of vegetable origin >—None. Nor the coal ash?—In the coal ash examined under water, I found abundant remains of vegetable structure, examined in the same way. Woody tissues in the coal ?—Yes. Did you conduct your investigation of the ash of the Torbanehill mineral and of the coal both in direct and transmitted lights >—By both. And with the results which you have described P—Yes. Were they the best, most approved instruments ?—They were. I have used various instruments of all kinds, but I have used the best and most recent construction. What were those ?—Those were prepared by two of the most eminent London opticians, Mr. Ross and the firm of Smith and Beck. What conclusion do you arrive at in regard to this Torbanehill mineral, keeping in view your investigation of the sections, of the powder, and of the ash ?>— That the two substances are totally dissimilar. That the Torbanehill is a different substance from any coal with which you are acquainted r—Yes. - Cross-ecamined by Mr. Neaves.—Are you in practice in Glasgow as a physician P—I am. Have you marked the magnifying power of the instruments used on those specimens P—I have. . When did you first see this mineral?—I think on 15th January last ear. q Had you never seen it before -—Never to my knowledge. You had previously been in the habit of examining coals p—I had. And had seen all the cannel coals P—Not then. Ihave since examined them. What coal had you seen when in the practice of examining before >— Chiefly domestic coal. For many years ?—For several years. With any particular view ?—None. The body and ash of domestic coal ?—Yes. You always see the woody structure in the ash ?—Always; I have never failed. And in the coal ?—Do you mean the sections ? Yes.—I have never met with a piece of coal that had not those appearances. Do you give it a name ?—I call it a fibrous section, from appearing like a bundle of fibres in one direction. I give it longitudinally, because it gives me the idea of length, and annular, that is, composed of rings, when seen in a cross cut with a longitudinal. But are equally distinct in the same coal always?—Not equally distinct. Not equally distinct in all coals nor in the same coal ?—No, but remain always distinct in every coal. Re-examined by Mr. Macfarlane.—Have you been at Torbanehill ?—Yes, And made specimens ?—Yes. Did you examine from those specimens ?—Yes. Fair or average specimens of the mineral ?—I took them just as they were raised from the pit, and examined them from the centre, outside, and every way I could possibly conceive. Your observations have been more recently directed to cannel coal p— Yes. Can you give me the names ?—I believe I have examined about forty or 50 Structure of a peculiar Combustible Mineral, fifty different specimens, as far as I know, but I can give the names of different coals that I tested. Just give us a few ?—These were Capeldrae, Wemyss, and Pirniehill, wc. Your investigations had been previously chiefly directed to the ordinary coals ,—Yes. Is it more difficult to trace the organic structure in the cannel coal than in the ordinary domestic coal ?—It is. Perhaps requires more skill and practice ?—Yes, in conducting the investigation into the cannel coal. What is the reason of that?—The reason I believe to be, that the structure is much more compact in the cannel coal, and the section requires to be made exceedingly thin, and it is very difficult to procure that con- dition, from the excessive brittleness of the material, and also intense opacity, and containing particles of hard matter, which frequently tear out the specimens. Mr. BowERBank.—Lxamined by Mr. MACFARLANE. Mr. Bowerbank, you live in London P—I do. You have given a good deal of your time and attention to microscopical observations ?—I have for these twenty-five years past. You are a fellow of the Royal Society ?—I am. You were lately president of the Microscopical Society of London ?— I was. And you have written on the subject, I believe ?—I have. Have you made a great many examinations, with the aid of the micro- scope, of mineral substances P—I have. Of various descriptions of coal ?—I have. For many years, the subject, simply as a natural-history subject, was much inquired into. And you have turned your attention to it >—I have. And have for several years been taking observations, with the micro- scope, of coal substances P—Yes. Have you been at Torbanehill ?—I have. Recently ?—Yes, recently. And you obtained specimens of the mineral that is working there ?—I And subjected them to examination Pp—I have. Did you give a specimen last week to Professor Quekett P—I showed him a specimen, and he desired to possess it for examination. And did you give some specimens to Dr. Adams ?—I did. What has been the result of your examination of coal substances ?— Every coal which I have examined, either bv sections, or by external characters, or by the examination of the ash, has convinced me that it is an essential character of coal that it should be composed principally of organized vegetable substances and bitumen. Lord President.—Of what, did you say ?—Of organized vegetable carbon and bitumen principally. Mr. Macfarlane.—With a little earthy matter p—Yes. I think you said these examinations were of the sections of the sub- stance, and of the ash as well ?—Of the sections of the coal matter, and of the ash as well. The practice generally adopted in examination is, first to observe its ordinary characters, and next its sections, so as to develop its structure. Have you pursued the same mode of investigation in regard to the Torbanehill mineral ?— Exactly. And with what result ?-—I have found no organic structure in it, from the Coal Measures of Torbane-hill. 51 although I have examined it by powers varying from 40 or 50, up to very nearly 700 linear. I have also examined the ash with great care ; and I may say that as to almost every specimen that has passed through my hands identified, and others as well, in no case have I found any indications of vegetable structure in the ash. Then the results of your examination of the coal, and of this mineral, are very different ?—Quite opposite. I suppose, Mr. Bowerbank, you have used the best instruments p—Yes, Sir, I believe there are no better to be procured. Indeed, unless they were instruments of a high optical character, they would not develop the minutest portions of the tissue satisfactorily. Who are the great London makers ?—Ross, Bowell and Smith, and Bett (or Beck). You have examined, I suppose, different varieties of shales, have you ? —To a very considerable extent. Any traces of organic structure in them ?—Not in the body of the shale itself, but a oreat intermixture of isolated plants. In fact, in coal shales isolated plants form a considerable portion of them. We have had the word ‘ amorphous’ used frequently, Mr. Bowerbank. Can you explain its meaning ?—I understand an amorphous mass of that description to be a mass without crystallization—a mass which would cleave in any direction without any determinate arrangement. For instance, I would say a sandstone, although formed of granulated masses, is still an amorphous mass, as there is no determinate arrange~ ment. Where there is organic structure, the word amorphous would not, of course, apply ?—Not to the structure itself, but it may apply to ‘the medium in which that structure is imbedded. Cross-ecamined by Mr. Neaves.—Where did you get your specimens ? —Some from Torbanehill pits, which I visited within the last week. And adjoining properties ?—And some from the adjoining properties as well. What property was that ?—Bathgate pit, and another pit. I also received verified specimens sent from the country to request an examina- tion of them. You first saw the mineral there ?>—I first saw the mineral at Queen- wood College, some time ago. Some months ago ?—About three months ago. Re-examined by Mr. Macfarlane _—Among other coals have you examined various cannel coals ?—Frequently. And the statements you have made have had reference to them as well as to others ?—The specimens which I have examined of the cannel coals, vary very considerably in character from this new mineral from Tor- banehill. You discovered the vegetable origin of the structure in them ?—Oh, yes. This closes the evidence of the microscopists on the pursuer’s side. I will now proceed to read that given on the side of the defender. Professor J. H. BALFour.—Haxamined by My. NEAVEs, You are Professor of Botany in the University of Edinburgh ?—Yes. And [ understand that you have. devoted attention not only to the sub- ject of botany as concerns existing plants, but also to fossil botany ?—Yes. 52 Structure of a peculiar Combustible Mineral, Is that a part of the course that you teach P—Yes. In the course of teaching that class, are you in the habit of examining mineral substances with a view to noticing their structure ?—I examine fossil plants. I have a large collection of specimens of fossil plants. Have you been in this case shown some specimens of different minerals with a view of examining them ?—Yes. What were they ?—I have seen specimens of the 'l’orbanehill coal, the Methil coal, the Capeldrae coal, the Lesmahagow coal, and several other parrot and other common coals. Did you visit the ground at Torbanehill >—Yes, I went to the pits and examined the coal, and brought specimens from the place. Did you visit the Methil pit ?—Yes. And got some specimens from Methil ?—Yes, out of the pit. And where did you get the other specimens that you refer to?—I got them from various sources. Some were sent me authenticated by Mr. Russel, some were given me by Dr. Maclagan, also by Dr. Redfern, Dr. Aitken, and Professor Harkness. Did you make sections of these minerals with a view to a microscopical investigation of them r—Yes. Did you make such a variety of sections as to enable you to judge in all directions P—Yes, so as to judge fully of the structure. Now, from that examination, are you able to say whether you dis- covered in these specimens traces of organic structure -—Certainly organic structure. In all the specimens ?—In all the specimens more or less. Now, in the Torbanehill mineral did you find marks of organic struc- ture ?—Certainly. And in the Methil ?—And in the Methil. Was there any difference, or any resemblance, between the appearance of the Torbanehill mineral and the Methil mineral?—A remarkable similarity. Was there some Lesmahagow coal ?P—Yes. And some Capeldrae also ?— Yes. And I think some Kinneil coal ?—Some Kinneil. Which is a cannel also P—Yes. Did you take the assistance of Dr. Greville ?—I took his assistance in delineating what we saw under the microscope. Did you see his delineations ?— Yes. Did they appear to you to be successful ?—Most correct, I think. You believe coal generally to be a vegetable formation, I suppose ?— Certainly. Of what species of plants is it generally supposed to be composed ?—The coal plants are numerous. We have, in the first place, a mass of ferns, stigmarias, sigillarias, lepidodendrons, calamites, and various other genera. The ferns supposed to form coal-beds are very gigantic ferns compared with the present ferns ?—They are tree ferns. Is it a cryptogamic plant Pp—Yes. In such plants, what is the particular appearance or structure you would expect to find ?—In all these plants, as well as in other plants of a woody stem, we have cells and vessels; but in the tree ferns we have a structure which may be said to be pretty regular, which is called scalari- form, or ladder-like, from the bars visible upon it. They are vessels or tubes. Did you see in the Torbanehill coal appearances that seemed to you to indicate cellular structure p—Certainly. : No doubt of that >—No doubt of that. And also some appearances indicative of scalariform structure ?—Yes. from the Coal Measures of Torbane-hill. 53 The cellular appearances more generally diffused than the other ?—Yes, much more generally. Do you consider you have in that way evidence of the vegetable compo- sition of the Torbanehill mineral ?—Yes, certainly. And of the same character generally as the other cannel coals that you examined ?—Precisely. [Here several drawings were handed to the witness, and he was asked to explain them. In the first drawing, which was of the Torbanehill mineral, witness stated the sections showed the vegetable structure, and also the scalariform vessels, with the bars upon it, very distinctly.] Is that the kind of structure that is seen in modern tree ferns >—Yes. The next drawing exhibits three sections,—the Lesmahagow, the Capel- drae, and the Torbanehill coal,—showing precisely similar structure. They are a little different in colour, but the same in structure. There are also sections of the Torbanehill and Methil in the drawings, showing the same appearance and structure in both these. Another drawing of the separate individual shales shows distinctly the appearance of separate cells, both in the Torbanehill coal, in the Lesmahagow coal, and in the Capeldrae coal. And, in fact, we find these in various other coals. The cell is the base of the organic structure of these vegetables P—Yes. It is the accumulation of cell upon cell that builds up the structure p— Yes. Judging microscopically, then, and also with your knowledge of fossil botany, would you draw the inference that the Torbanehill was of the same, or of a different class of substances from the other cannel coals that you have mentioned P—The same class as of the cannel coals I have seen. The only difference, I understand you to say, is the difference in the tinge of colour ?—Yes, and that occurs in many coals. You don’t think that essential in deciding the question P—I do not. - Cross-ecamined by the Dean of Faculty.—These observations are made upon a thin section ?—Yes. Who made the sections ?>—They were made by Professor Harkness, Dr. Aitken, Dr. Redfern, and Mr. Glen. Would you mark upon each the name of the gentleman who did them ? —Yes, to the best of my recollection. {Here witness marked each section as requested. | Have you yourself been accustomed to make such sections P—I have made sections for the microscope. Have you much practice with the microscope ?—Yes, it is part of my course. In reference to existing plants ?—Yes, and also to fossil plants. I have a large collection of fossil sections. With regard to this drawing here [holding up one of those previously described by witness], that represents the impression of an individual fossil plant ?—That represents only a portion of a plant, the vascular part of the vascular tissue of a plant, approaching nearly to the scalariform tissue. Do you mean that the tissue is there, or the impression on the plant ?— The tissue is there. In this other portion of the seam, then, which is coloured brown, you do not observe any structure ?—I did not examine particularly. But does this represent what you saw on that occasion ?>—Yes. Then there is no appearance of structure there P—I cannot say. There is no structure represented there >—No. All that you found in this particular section is the representation of part of a fossil plant p—Yes. 54 Structure of a peculiar Combustible Mineral, Part of an individual plant apparently P—Part of an individual plant probably. Do you know from what portion of this seam of Torbanehill mineral this slice representing the upper drawing is taken P—I do not know the portion of the seam. Do you know the portion of the seam from which any of them were taken r—I have only seen the specimens. They seem to be the ordinary appearance of the Torbanehill mineral, and quite the usual appearance of the coal, so far as I saw. Here the Dean of Faculty took up another drawing, and asked witness if he saw anything similar to that ?—I saw appearances similar to that. Have you represented them ?—Represented them so far in some of these sections, only the dark colour between makes a difference in the appear- ances. Lord President.—Is that in the Torbanehill mineral P—Yes. Dean of Faculty.—Did you see anything like that [showing witness another drawing, No. 25]?—Something approaching to this. It wants, in some respects, the regularity of the structure I have seen in the other. Shown No. 26, another drawing, and asked if he had seen anything like that ?—This also approaches to what I observed, but wants the definiteness and regularity of the structure I saw. Did you see anything like that [showing No. 28, another drawing] ?— Yes, the yellow part is more like what we saw in the general structure. What power did you use in making these observations ?—They are marked in diameters ; two of them were 200, and the other 70. Have you ever examined shales in this way ?—I have looked at one or two shales. It is not so much in my way as plants. Do you find marks of fossil plants in them ?—Yes, they occur; but the structure is different in them. They have not the same marked definite form I have seen in the others. I understand that in these you represent both the transverse and the parallel sections ?—Yes, we have taken them in two directions. Which are the transverse P—The three upper are the longitudinal, and the lower the transverse or horizontal. What do you mean by horizontal ?—By horizontal we mean cutting off the ends of the vessels. That is to say, you learned that from the gentlemen who made them ?— I have examined sections. You did not see the sections made ?—No. Then, of course, you could only get the information from those gentle- men who made them ?—Yes. Are the three upper cut along the stratum, as it were, off the top of the stratum as it lies?—I am talking of them as regards the appearances we see in the microscope. Judging from ordinary structure, in the one case we cut the ends of the vessels ; in the other, we cut along the line longi- tudinally. Lord President.—The three upper are cut along the line of the vessels, and the three others are cut across the line of the vessels. Dean of Faculty.—Do I understand you to say that you were told they were cut in this way, and that that is the ground of your saying so; or do you form your opinion by the appearance they present ?—I was of course told so; and on looking at them, I should say they are so cut. Then it is from both these reasons that you say so ?—Yes. Did you examine any part of the ashes of this mineral with the micro- scope P—No. ; Did you ever examine the ashes of coal with the microscope ?—No. from the Coal Measures of Torbane-hill. 5d Did you use direct or transmitted light in these examinations P—I used ec aaa transmitted light, but I also viewed some specimens by direct light. Re-examined by Mr, Neaves.—There are several drawings here. Did you examine a great many more cuttings than these drawings ?—A great, number. : How many more, do you know ?—I cannot tell the number of the sec- tions of Torbanehill ; at all events, some eight or ten, besides sections of other coal. And then made a drawing of these P-—-Yes, as being average specimens. Did you see some of these sections made P—Yes, these were the sections made under my direction by Mr. Glen. The Methil section?—I cannot say I saw it made in the sense that I saw the whole process gone through, but it was done for me, by my di- rection, from a piece of Methil coal. Lord President.—Did you see Mr. Glen make some of the sections ?—I should rather say that the sections I allude to were made under my direc- tion, and were authenticated by me at the time. Mr, Neaves.—In the other sections of the Torbanehill mineral which you have examined besides this, did you find the same appearances r—The same appearances. - I forget what you said as to this yellow part of No, 28 P—I considere that to be a cellular structure. The yellow part included ?—Yes. This cellular tissue is a magnified appearance of the separate individual cells P—Yes. With the view of showing that they were at larger power ?—These are cells which occur in these coals, and they are separated the one from the other. We took magnified drawings of them. Occurring at Boghead ?—Yes, and on the others. And besides showing those things, you formed an opinion of what they were ?— Yes. That they were the indications of vegetable cellular structure P— Certainly. Lord President.—That is, the appearances in the mineral seams P—Yes. Mr, Neaves.—Including the Torbanehill P—Yes. And of that yellow part of the representation of the Torbanehill mineral ?—I believe it to represent vegetable cells. In these plants I suppose the structure is but imperfectly understood ? —I may say we do not know it so completely as we know all the plants of the present day. The cells may be longer or shorter p—Yes. They vary in their form rp—Yes. And that may affect the longitudinal appearance of the cells ?—Yes. I do not understand you to say that this is the mere impression of a foreign fossil, but the actual structure of the mineral at that place ?— Certainly. Dean of Faculty.—The individual plant is there lying in the mineral ? —The structure of the plant—not the entire plant. A part of a fossil plant is seen there ?—Yes. Mr. Neaves.—Forming a part of the coal ?—Yes. Dean of Faculty.—I understand, Dr. Balfour, that there is a part of the fossil plant here lying imbedded in something or other P—It is a quite dissimilar part as regards the appearance. The plant must be there in order to give it that appearance P—It must be the structure appearing so distinctly as to be seen there. 56 Structure of a peculiar Combustible Mineral, Very well; a plant is lying here upon another thing, which is here represented by a dull-brown colour ?—Yes, a part of the plant. Mr, Neaves.—What did you say ?—That that is part of the Sisetdaxe of a plant which is lying there in the mineral. When you make a section of the mineral you come upon this, showing you that there was a plant. At that part the mineral consists of that plant >—Yes. Dean of Faculty.—You have seen fossil plants in stone quarries ?—Yes. Mr, Neaves.—You do not consider that an example of such an appear- ance ,—No. Dr. ReprERN.—Haxamined by Mr. NEAvEs. Dr. Redfern, you lecture on subjects connected with the microscope in connexion with the University ?—Yes; and teach the use of the micro- scope. You are a Fellow of the College of Surgeons of London ?—Yes. Have you been accustomed to the examination of substances by the microscope ?—Yes. Principally of vegetable substances for some years ?—I have for many years been in the practice of examining vegetable structure by the micro- scope. Both in recent vegetables and in fossil substances ?—I have. Did you lately receive some specimens of different minerals, including some of the Torbanehill mineral ?—I did. From whom did you get the Torbanehill mineral ?—I got some specimens from Dr. Fyfe, and some others from the Aberdeen Gas Works, in the presence of Mr. Leslie, the manager. Did you subject these specimens of the Torbanehill mineral to micro- scopical examination ?—I did so. How many sections of it did you take ?—Eighteen. From the same piece, or from different pieces ?—From eight different pieces. Did you or did you not find vegetable structure in these sections ?>—I found vegetable structure in every section. Have you examined different cannel coals with the same view ?—I have. What cannel coals ?—I have examined Lesmahagow cannel coal, Capeldrae cannel coal, Wigan cannel coal, Methil cannel coal, and Halbeath parrot coal; and also the Kinneil coal from Bo’ness. In what way would you speak of the examination of these minerals, and of the examination of the Torbanehill mineral, in reference to the vegetable structure ?—I am quite convinced, that in the sections of these different coals there are parts which cannot be distinguished from each other. Vegetable structure in all ?—In all. And in some parts this mineral undistinguishable from the others ?— Certainly. The Boghead mineral has considerable varieties of aspect in itself 2—It has. Different shades of colour?—There are black, brown, and spotted pieces—black pieces with brown spots. In the lightish-colour portions of the Boghead mineral, what is that you saw ?—I saw vegetable cells in these portions. The structure that you saw is cellular structure ?—Yes. Besides the cells that you saw, what else did you notice ?—I noticed also woody fibre, or woody tissue. From the Coal Measures of Torbane-hill. oT Are there some yellow spots in this light-coloured portion of the mineral ?—'There are. What do you think these yellow spots indicate ?—They indicate the existence of vegetable cells. Have you applied any test to endeavour to find out whether they were vegetable or not ?—I have, Sir; I have many reasons for concluding that they are vegetable cells. Would you mention your reasons?—lI find that they can be perfectly isolated—they project upon the edges of all sections of the mineral—they are rounded—they are as uniform in size as the cells of other vegetable structures—the general appearance of the section is that of a piece of vegetable cellular tissue—the yellow spots do not act upon polarised light, or act upon it very feebly. Generally speaking, do you consider that the Torbanehill mineral exhibits the same appearances of structure and position microscopically as the other cannel minerals ?—It does. Did you see Dr. Greville’s drawings P—I not only saw the drawings, but I saw him make them. You had long previously examined the minerals ?—I had; long and carefully. Do these drawings appear to you to represent the general character of the mineral P—They do. ; And you believe these drawings to represent cellular tissue P—I do. Your sections were taken at random from the general specimens that you had P—Certainly. As fair specimens that you thought the mineral would exhibit ? —That was my chief object in obtaining them from the Aberdeen Gas Works. I took the specimens for as fair average specimens of the Torbanehill mineral as I could obtain. And they would have supplied similar representations as those Dr. Greville has given, in your opinion ?—I am satisfied of that. Cross-ecamined by the Dean of Faculty You say Dr. Greville’s drawings represent the same thing that you saw ?—They do. Did you examine the ash of this coal ?—Yes. With the microscope ?—Yes. I consider the examination of the ash as liable to great sources of fallacy, and place no dependence upon it. Your reasons?—I should not look upon the ash to make out the structure it contains. That is not your reason, but a repetition of your opinion. What is your reason r—Because I would expect the greater portion of vegetable structure, if it existed, to be destroyed by the process of combustion. Did you ever examine the ash of ordinary coal with the microscope P— I have not. Dr. R. K. Grevitte.—Huamined by Mr. NEAVEs. Dr. Greville, I believe you have devoted a good deal of your attention to the study of botany ?—Yes, it has been the principal study of my whole life. And in connexion with that to the use of the microscope P—I may say, without exaggeration, that for many years I have used the microscope almost every day. Among other branches of the vegetable kingdom, you have studied and written upon the cryptogamic family, which includes the ferns ?—Yes. And which requires particular use of the microscope in order to illustrate its fructification?—Yes. I may add that 1 have made the drawings of everything I have published from my own microscopical investigations. a 58 Structure of a peculiar Combustible Mineral, | made drawings of the outline and structure of two or three hundred ferns alone, Were you asked to assist some gentlemen using the microscope to represent the appearance of some sections of minerals ?—Yes. These are the drawings you made ?—Yes. Did you yourself look at various sections of the minerals besides those that you have represented ?—I did, especially with regard to the Boghead mineral. {examined under the microscope eighteen different slices made from eight different specimens of the substance. Were these Dr. Redfern’s specimens ?—Yes. Did you discover vegetable structure in these ?—Unquestionably, in the whole of them. Did you examine some other minerals—some cannel coals that this gentleman had?—I examined all those coals of which the names are appended to the drawings. There is the Methil, Lesmahagow, and Capeldrae coals. Now these are correct representations, to the best of your ability, of what they present -—They are; they might be more minutely finished, but they give, I hope, a fair representation “of the structure. Did it appear to you, from your examination of these different things, that they were the general structure of the mass, or any incidental structure ?—I have no hesitation in saying that it was the general structure of every specimen, not incidental. JI should consider it to be quite impossible it could be incidental. . Do you consider that there is a material difference or a substantial identity between these different bodies, as represented in these different minerals ?—I do not. I examined the specimens of the three upper- most sketches, and the structure was so similar, that I considered them to be identical. ‘There is a difference, but nothing amounting to any- thing essential in the structure. The Lesmahagow, Capeldrae, and Torbanehill are essentially the same. I may be allowed to add, that in each slice there is a difference in every part of that slice, so that you must be guided by the general view. From your botanical knowledge, have you any doubt that these repre- sentations exhibit vegetable cells ?—I have no more doubt of that than of my own existence at this moment. Will you explain what that paper is?—[handing witness one of the drawings spoken to by Professor Balfour|—That drawing represents vegetable cells in an isolated state, scattered throughout the substance, and observable, I believe, in most coals—certainly in most coals that I have examined. It is difficult to say what they may be, but I have no doubt that they are vegetable cells, solitary cells. They may possibly be transverse segments of cells, but I would not venture to say anything more than that. I believe them to be vegetable cells. Found in this mineral ?—We have found these vegetable cells in the Boghead as well as in others. . Will you explain what these two drawings represent °—{ handing witness two of the drawings spoken to by Professor Balfour |—The uppermost one represents cellular tissue in the Torbanehill mineral; and, upon the whole, I consider that as one of the most satisfactory specimens which I examined ; the cellular tissue is so unequivocally marked, and so regular, that it may be compared to that of a recent plant. It is exceedingly well defined. What I have represented in the drawing is not in the least exaggerated. No person accustomed to botanical sections would hesitate in believing that to be cellular tissue. The lower drawing represents a beautiful specimen, but whether that is general in the mineral I could not from the Coal Measures of Torbane-hill. d9 say. It represents a modification of the vascular structure of plants called technically the scalariform structure. I can compare it best by comparing it with an old basket. It is an unequivocal vegetable structure. What occurs in its neighbourhood in the rest of the section ?—'This was the whole that I saw. The other portion was not ground so thin, and I could not see what it consisted of ; but judging from the traces of these vessels at the extreme edges, I have no reason whatever to doubt, that if the remainder of the section had been ground sufficiently thin, we would have seen the continuation of that structure. But the other cells that you described here are diffused through the entire mass of the substance ?—In all the specimens I examined it was uniform throughout the whole. It was exceedingly well marked in the one that represents the transverse section of the cells. You get the width of the cells more distinctly when you cut the transverse section ?—You get the area more distinctly shown. Cross-examined by the Dean of Faculty.—Can you explain to me what are infusoria ?—Infusoria represent minute animals invisible to the naked eye—visible only to the microscope. Where do you find them P—It is very difficult to say where you do not find them. Generally they are sought for in fluids. You find them in minerals also?—I am not prepared to answer that question. Iam not sufficiently acquainted with the subject to venture to answer it. Then you cannot tell me what appearance they present when found in minerals when examined under the microscope ?—No, I am not aware of their occurring. Professor HaArKNEsS.—Hxamined by Mr. Youna. Professor Harkness, you are Professor of Geology in Queen’s College, Cork ?—Yes. You succeeded Dr. Nicol ?—About six months ago. You have devoted considerable attention to the study of geology ?—I have. And also to the examination of objects by the microscope ?—Yes, so far as relates to fossil plants. You have visited Torbanehill ?—I have. You went down one of the pits >—I was down two of them. And examined the mineral as it lay in the earth P—Yes. And made yourself acquainted with its geological composition ?—I found it to occur in the proper coal measures. Exactly in the position you would expect to find coal ?—Decidedly so. You found nothing whatever in its geological composition to lead you for a moment to doubt that it was coal?—Nothing; on the contrary, everything to induce me to believe that it was coal. Did you form any opinion upon the mineral itself ?—-I formed the opinion, that from the appearance of the mineral it was a coal. Did you take some specimens of the mineral away ?P— Yes, I did, for the purpose of making a more careful examination. And after that examination you retained your opinion ?—I did. And your opinion now is that it is a coal?—Decidedly so, without any manner of doubt. Did you make some sections of the mineral which you took away with the view of microscopic examination ?—So far as regarded fossil plants. Did you find the structure familiar ?—I found the structure peculiar, and the fossils characteristic of the coal formation. How many structures are there in coal and coal plant P—There are two 60 Structure of a peculiar Combustible Mineral, or three distinguishing characteristics, first the woody fibre, the scalariform tissue, and the cellular tissue. Is this upon the examination of a great many sections?P—Yes. That was generally, not mere accidental structure of particular pieces. You saw a drawing made by Dr. GrevilleP—I was present when that drawing was made. Sah ‘that gave a sufficiently distinct idea of the course of examination ? —Yes Of the Torbanehill and some other coals p—Yes ; and the Lesmahagow, Kinneil, Capeldrae, and some other cannels. I believe the drawing was made from a section furnished by your— That is a most beautiful ; specimen of cellular tissue. This is the most beautiful specimen you have seen of woody fibre ?—I distinguish woody fibre from cellular on account of the more regular formation of the cells. You have no doubt that this is a vegetable product P—Not the least. { Witness was shown the drawings illustrative of cellular tissue and woody fibre, and distinguished each with great precision. | You know what shales are >—Yes. Do shales ever exhibit vegetable structure P—As shales they do not. How would you describe a shale ?—There are several forms of shales. Supposing the coal to be so mixed with earthy matter as to be incapable of being used for fuel, then that would be called a coaly shale. And when the coaly matter is so great in proportion to the earthy mat- ter that it will burn ?—I should consider this a coal. And more or less pure according to the admixture of earthy matter ?— All coals contain more or less of earthy matter, and accordingly the coals run into shales as the earthy matter increases. When you come to a substance beyond which a substance will not burn, you would call it a coaly shale ?—Yes, It is very difficult to draw the line at the exact place?—Very difficult. Has this mineral anything of the character of a shale P—Not the least, so far as I have been able to detect. You have seen specimens of Methil coal, and examined them with the microscope ?>—Yes. And did you find anything to distinguish the Boghead mineral ?— So far as external appearance went, I could scarcely distinguish the one from the other, and there was also a great similarity in internal structure. There are a variety of cannels which approach each other very closely ? —In regard to the distinction between the two there is not a more com- mon one than this, the capability of burning and being used for the purposes of fuel. If the substance would burn, and could be used as fuel, you would say it was a coal ?—Yes, I would. If any substance ‘is sold in the market as a coal, is it a coal?—Yes, I should think so. There is no science against this >—None that I am aware of. Cross-ecamined by the Dean of Faculty.—I suppose whatever comes out of the coal measures and burns by itself is coal?—No; I would not say that. You might get a fragment of bitumen, which would not be coal, and that burns by itself. Is that the only exception >—I am not prepared to say that there are any other exceptions. Fragments of bitumen would be an exception ?—Yes. The way by which you distinguish a coal from a shale, or a shale from from the Coal Measures of Torbane-hill. 61 a coal, I understand is, that the one will burn, and that the other will not ?—The one will burn without the mixture of any extraneous matter. It will burn by itself ?—Yes. There are other distinctions ; but this is the distinction upon which you rested ?>—Yes. You were going to tell us that there were a number of kinds of shales. Tell me some of these ?—There are some which are absolutely devoid of coaly matter—clay shales, which have no coal in them at all. Any other distinction ?>—Yes; there are shales which I should charac- terize as bituminous shales. How do they differ from coaly shales >—They differ inasmuch as they give a bituminous smell when struck by the hammer; and they yield bitumen to chemical solvents. Do they burr ?p—Yes, they burn in some cases. Where do you find most bituminous shales P—You find them in Cam- bridge and in Dorsetshire, in the higher beds of the oolite. Do you find the Methil coal to be of a laminated and slaty structure p— I found some fragments that were laminated; but others present the conchoidal structure that you have in the Boghead, and is compost. The Boghead is compost ?—It is. Is the Methil coal so ?—It is generally so. But portions are slaty and laminated p—Yes. Will you explain what infusoria are >—I have not given any opinion as concerning infusoria. : But you can give one ?—They are minute microscopic animals. Where are they found ?—I generally find them in water. Are they not to be found in mineralsP?—I have not found them in minerals, But are they not to be found in minerals ?—They are found in certain mineral beds, but I have not found them in mineral beds. Dr. Witu1am AiTKeN.—LHxamined by Mr. PENNEY. You made some sections of the Torbanehill mineral, and of some other coals P—Yes. Were they for your own examination, or some that Dr, Greville drew ? —TI did some, and also for my own. You got the returns from Torbanehill ?—I did. From the pit mouth p—Yes. You made the sections fairly for the purpose of testing °—Yes. Mr. Neaves then stated that they would not require to examine Mr. Glen, as his sections were also admitted. Having now read to you the evidence given by the micro- scopists on both sides of the question, I cannot refrain from making a few remarks on some of the statements of the defender’s witnesses. ‘The subject to me is a painful one, for it is always with feelings of regret that I venture to differ in opinion from any scientific observer ; but, however contrary to my inclination, I have a public duty to perform, to say nothing of the character I have to sustain amongst you as a member of this society. I sincerely hope, however, that those gentlemen will take it all in good part, and believe that it is only for the reasons above assigned, and not from any 62 Structure of a peculiar Combustible Mineral, public or private feeling of opposition to their opinions that I appear before you this night. I will not dwell long upon the subject, as it must be very clear to you all—first, that the specimens examined by these gentlemen must have had more or less of plant structure im- bedded in them; secondly, that they have evidently mistaken the peculiar arrangement of the combustible and earthy por- tions of the mineral for vegetable cellular tissue. Thirdly, they can certainly never have examined sections of many coals microscopically, as one and all tell you that they saw the same structure in the mineral as they did in coals. Had they made sections of coal in two directions, at right angles to each other, they could hardly have failed in seeing, almost at a glance, how much the sections differed in structure the one from the other. That such is really the case, even in the coals which they state in their evidence they have examined, may be shown by reference to Plate IV. In fig. 1 is repre- sented a transverse section of the so-called brown methil ; and in fig. 2, a longitudinal section of the same. ‘The two structures are so different in appearance, that, had such sections been made, I feel confident there could not have been a second opinion on the subject. In fig. 3 is shown a transverse section of the black methil, and im fig. 4 a longi- tudinal section. ‘The differences, if anything, are even more striking than in the brown methil. But what will be said of figs. 5 and 6, which represent a transverse and longitudinal section of Lesmahagow cannel coal? That anything at all resembling such a structure as this, can be found in sections of the mineral in question, except when coal is present, I emphatically deny. Now, granting for a moment that the structure of the mineral be cellular, what plants, I would ask, could the cells have belonged to? Can any botanist produce a single instance of a recent or fossil plant of the same thicknesssas a seam of the Torbanehill mineral, which shall be made up of a mass of cellular tissue, that is, without vessels or woody fibres being present with the cells? Again, if the structure be cellular, we should expect to find the most durable part of the cell—the cell wall—always pre- sent, which is not the case. If this view be correct, the yellow particles being solid must be the contents of colt they cer- tainly cannot be cells. ‘The cell-wall also, as far as we know it, in recent and fossil plants, always presents on section a more or less uniform thickness and a homogeneous appear- ance; whereas the structure around the yellow particles in all cases, except where plants are present, is minutely granular, from the Coal Measures of Torbane-hill. 63 being in reality the clayey or earthy ingredient of the mineral, None of the defender’s witnesses, it appears, ever examined the ash of coal; and one witness in particular, Dr. Redfern, stated that the examination of ‘ash in general was liable to great sources of fallacy, and placed no dependence upon it ;’ whereas, it subsequently appeared that he had never examined the ash of ordinary coal with the microscope. Were I disposed to be hypercritical, I could mention many other points in the evidence that I entirely dissent from; but I trust I have already said enough, and will therefore sum up my remarks by stating that I consider the mineral in ques- tion is not a coal, being structurally different from all un- doubted coals, including those with which it appears it has been compared by the microscopists engaged by the defender. In order, therefore, that the scientific world in general may have an opportunity of judging for themselves whether this statement be correct or not, I have put specimens of the mineral and of these coals into the hands of the preparers of microscopic objects, and in a short time sections will be on sale by them and by the principal opticians in this metropolis. I might by some persons be accused of unfairness in making even these few remarks upon the evidence of the wit- nesses for the defence, when they are all located in different parts of Great Britain, and therefore not able to be present this evening to answer for themselves. I wish, however, that they could have been here, and more especially if they could have brought with them the sections upon which their opinions were formed, and the drawings which were produced in court. They might say, perhaps, that it would not be fair play to send their specimens, their drawings, and their remarks into an enemy’s camp; on my own part, however, | can ven- ture to state that | am ready to appear before any tribunal of scientific men in this kingdom, and my drawings and speci- mens shall be open to all who may be interested in the subject, to examine for themselves. I beg it may be expressly under- stood, that should there be any one point in this paper which on subsequent investigation may turn out to be incorrect, I shall be as ready to come forward and acknowledge myself in error as | now am to express an opinion not hastily formed : my only object, as I said before, is truth ; and by truth I will abide. There is one other point that I would briefly allude to before drawing my remarks to a conclusion, and this is a portion of the Lord President’s address to the Jury, in which, 64 Structure of a peculiar Combustible Mineral, as before stated, Mr. Bowerbank and myself are placed in no very enviable position ; it is as follows :— “* Besides those gentlemen who were examined as geologists and che- mists, and who differ so widely, there was examined another class of men, and possessed of great attainments—lI refer to the microscopists. One of them was the late President of the Microscopic Society of London—a learned body, who make it their object to pry into all things. Three of these gentlemen were examined for the pursuer, and four for the defender. The pursuer’s witnesses told you that there was no trace of organic struc- ture, no woody fibre or tissue, in short, no trace of vegetable matter in this substance, although occasionally there might be the incidental pre- sence of vegetable remains. The witnesses of this class on the other side told you, on the contrary, that in every part of it there was the most clear vestiges of vegetable structure. I do not know, when I have so many geologists, and so many microscopists telling me that it is not coal, and so many on the other side telling me the opposite, I say Ido not know that I feel myself much the wiser, or further advanced in the inquiry. But if you have, in addition, a great number of chemists, and speaking with equal authority and equal contrariety, it is difficult to know what to make of the controversy. Ido not know that I have anything to say against the skill of the microscopists, or the skill of any of those gentle- men ; but one general remark may be made on the microscopic testimony, - and it is, that there are those who see a thing, and also those who do not see it—those who do see it, cannot see it unless it is there, and those who cannot see it do not see it at all. But very skilful persons looking for a thing and not seeing it, creates a strong presumption that it is not there. But when other persons do find it, it goes far to displace the notion that it is not there. But there is another observation on the microscopic evidence that occurred to me. Ido not know whether I am under any misappre- hension, but I think that three, certainly two, of those examined by the defenders, are botanists also; and I do not think that any of those exa- mined for the pursuer, two of them from London, represented themselves as botanists. Now, the defender’s witnesses are accustomed to look for plants, and can understand them when they see them. The gentlemen on the other side again, looking for woody fibre or tissue, are not, as I under- stand, conversant or skilful in fossil plants. But finding such a difference of opinion, and such opposite conclusions arrived at by those persons, I do not know, unless you think that some gave their reasons more satisfac- torily than others—I say I do not know that I feel my mind much relieved from the difficulties of this case by listening to all that evidence. It is very interesting no doubt, and if they were all standing on one side, and nobody standing on the other side, it might be very satisfactory to one’s mind to listen to such evidence.” To such remarks I would briefly reply that, however severe a counsel may be in his cross-examination, and how- ever strong his language in addressing the jury may be, I think it to a certain extent excusable, as he is endeavouring to do the best for his client; but I must confess my great surprise that a learned judge should see fit to single out one set of scientific witnesses from the pursuer’s side, and hold them up, I would say, almost to ridicule; that he did so on from the Coal Measures of Torbane-hill. _ 65 the present occasion, the part of the address which I have just read to you will show. I think it will eventually turn out that the two members of the Microscopical Society of London, *‘ that learned body who make it their object to pry into all things,” are accustomed to look for plants, and can under- stand them when they see them; nay, I will assert that they can do more, for they can tell when a particular structure is not a plant. Had his Lordship been silent on the point, he would not have laid himself open to these truly justifiable remarks, I would now, gentlemen, in conclusion, leave the matter in your hands. [ think that the subject in question is one of the most important ever brought before the notice of this Society, and one which no set of men in this or any other country are so competent to investigate. Most of the members of this society are, as stated in the certificate for suspension, ‘‘ attached to scientific pursuits,” and most of them are in possession of the best instruments, and are accustomed to use them; let them, therefore, study the subject for themselves, and give independent testimony. Where, I might ask, can be found a correct definition of coal? I believe, at present, no such definition is extant, and it is on this account that I look upon the trial of Gillespie versus Russel, as one of the greatest importance to the geologist, the chemist, the mineralo- gist, and the microscopist ; and | am of opinion that from it will spring, not only a perfect definition of coal, but of other combustible substances found in connexion with it, and, therefore, it is to be hoped that such contradictory statements as were made by the different scientific witnesses on the trial in question may in future be avoided. It remains, then, for the microscope, ‘‘ that most valuable of all scientific instru- ments (to quote the words of Mr. Ross) ever yet bestowed by art upon the investigator of nature,” to assist in deciding the true structure of coal, as it has already done that of many other organic substances of a previously-doubtful nature. q o~ ie) CO — *JINJONIIS I[QeIISIA Jo sooe1} SMOYS skeaye yse oy} pue ‘souvrvodde snoiqy @ Jo Sset IO a10UL sjuesaid pur ‘pUNos dIT[eJoUL B s}IUIe BYOD *yuosoid souITjoUIOS 103} eur Ayyee $ Mojoo uMOIG Yor v Jo soyed azepnsue peueyey GI poxtu A]yeuoisevo00 aie asey} : S2IQ JO Soypunq 10 seiqy jo Ajediourid posodu0d “INO[OO TMOIQ You BJO st moNs10d prouswiNnitq sq} sosvo ysoUT UT ynq ‘sseut oy} Ysno1y} AjAVNSe111 po19}ye0s oe soporyied prousunziq Mopjos Moz B “TINIOTT UWMOIG oy} Sse ‘[eoo oUlOS UL ‘“poulwexo useq oAey Yor STVod oy} [je JO OysliojoVreyo oie ‘1094RT oq} Ul salqy oy} pue sTjoo poyesuoja uMOIq YOU oy} pure ‘LUIZ OY} Ul SUIT pornojoo-Joquue pe[20-os 94} JO vouaseid ayy, “poo Jo suoTjOeS Sutpuodsai100 YY Sulosise Yoq ynq “yuoLOF -jtp A]][e}0} SUOT}OOS [VUIPNIISUOT pu ss1OASUBLT, *poom Jo UOTOVS [CUIPNIISUO] v Oy] ‘oouUvIvodde snoiqy eB JIQIYXS [LM ‘s}SI] UTeZIO0 UL ‘SOpIS XIS S}I JO MO] *“SNOI}SN] puv UMOIG Yep “IIe, UMOIG oy} Ut ‘Sno1jsny pur yoryq yes ‘opyyaq “yovy~q iMojog “"TVOO ‘vols Jo ATqeqoud ‘sgoord aepnSue Jo pue ‘1033eu AYJAva Jo setnueas yrep jo AjerMUe sjsisuoo yse oy} ‘Suruing Aq poaoulal useq oAvy saporyied MOT[eA oy} YouTA wo ‘soutavo 10 syd jo soles @ Surjuosoid ‘yonijs useyA punos {np ‘ASuods pue yySI, ‘axog ‘snosorpis ATqeq -oid pue “Guoredsuen 031nb sisyj0 ‘enbedo autos ‘royeu AyzIvo JO sopnuess JO a1n}XTUL [euoIsvo00 YUIA ‘soporyaed moyjed ay} Jo ATpedtoutid pesodmog *SONSSI} ITY} JO wAIOF oY} Aq sv To“ se ‘IMojoo UAOIG Yor 1104} Aq postusooe1 Ajtsea oq Avut Loy} ‘yuasoad oq syuetd Jo suonsz0d Jo ‘sjuvjd Jy ‘ope si uoTjOes oy} ABM JOAO -YOIYA 91NJONI}S UL VOUIIEHIP ou f YOVa Jo a1yU80 ay} Ul yuosoid st oIMjoNIYs pozeIpel & ‘adIRT 18 soponied oy} uoyM ‘SIseq sepnuesd-ATONUTUT e Aq popunoiins sasvd suOS Ul ‘mMoToo JequIe pus ‘oinsy AemMoiio Jo ‘sazis snoLIvA JO seporTed "SSVUL OY} WOT 41 sutstea Aq 10 Sutderos Aq J0y}10 ‘aAoIq euI000q [1M ‘yorTq oaomoy “aed Aue : ssvur [el9ued 34} WOIZ poyovjop oie YOM ‘ANOTOO UMOIQ-I.SI] jo Suleq sopraed 10 sajnueis asoy} ‘1epnUeLy *Qa}SN] WOT ‘UMOIG Yvoijs ‘Ysno, ‘yorTq IO UMOIG “INOTOD "IVGANIN TIIH-ANVEYOL “yse pue ayoo ay} Jo siojowreyD ‘¢ JopAod oy} Jo s1djoereyO “+ “9doo0s -O10IUE oY} Jopun suoryoes fq payiqryxa 2 Aq poliqryxa siojovreyQ °Z sIoyoeleyQ “e "S1aJIWILIp OS Jo 1oMoOd & Jepun ‘yoafqo onbedo ue se PoMoIA “UOseIZ TeoIqnD S19JOVIVYO [VUIO}IXY *T ‘IVOQ pue IVUANI] TIH-INVaUOT, OY} useMjoq AONAAAATIGG JO SLNIOG 'IVdIONING Oy} JO MATA AVINAY Roper, on the Diatomacee of the Thames. _ 67 Some Observations on the Diatomacex of the Thames. B F.C. S. Rover, F.G.S. (Read January 25th, 1854.) In the year 1843 M. Ehrenberg, read before the Academy of Sciences of Berlin a paper on the microscopical marine infu- soria of the deposits of the Elbe,* in which he established the remarkable fact that at Gliickstadt, a distance of forty miles, and even above Hamburg, upwards of eighty miles, from the mouth of the river, marine siliceous-shelled Infusoria were found alive, and their skeletons deposited in such abundance in the mud of the river, that at the former locality they form one quarter to one-third of the entire mass, and that the pro- portion is still about half that amount at Hamburg, as far as the flood-tide extends. All his observations gave a great pre- dominance of marine over fresh-water species, even when the salt taste of the water was no longer perceptible. In the lists which accompany this paper, M. Ehrenberg enumerates thirty-four marine species, under the style of siliceous-shelled Polygastrica, the whole of which would now be classed as Alge@, under the order Diatomacee. The local distribution of these organisms is a point of some interest ; and as well-authenticated lists of species from the different localities in Great Britain have still been only partially attempted, I am induced to lay before the Society the results of some observa- tions on the deposits of the river Thames, which accord in a great degree with those made by Ehrenberg in the Elbe, though the proportion of marine to fresh-water species is more equal at corresponding distances from the sea. The abundance of the Diatomacee, and the facility with which the different species have been collected at Hull, Poole Harbour, and other well-known localities, where they may be gathered alive, and offer such advantages for acquiring an intimate acquaintance with their habits and modes of growth, has tended, in a great measure, to divert attention from those which are deposited by the Thames water; and, with the exception of some species of Triceratium, Eupo- discus, and a few other forms, the greater part of the list I shall hereafter mention has been hitherto, so far as I am aware, altogether unnoticed, or at all events no special detail of them has been given Romi that locality. The chief cause, I imagine, for this neglect of the Diato- macee of the Thames and other rivers, has arisen from the fact, that observers have endeavoured to pursue the same plan * Verhandl. der Konigl. Preuss. Akad. der Wissenschaften zu Berlin, 1848. VOL. IT. h 68 Roeer, on the Diatomacee of the Thames. which meets with such success in the localities I have before alluded to, that is, to examine them in a living state; but, as far as I can judge from ny own experience, this affords a most unsatisfactory result ; and after a careful examination of the mud deposited at different points in the Thames, any one might easily arrive at the conclusion that the varieties to be met with were comparatively few, and, except for the exami- nation of some of the larger species, not worth the time neces- sary for extended observation. Having, some months back, brought home a bettleful of the black mud from the extremity of the Isle of Dogs, taken about half-way between high and low water mark, and for several nights successively submitted it to a careful examina- tion, the only species of Diatomacee I met with were a Trice- ratium favus, and several specimens of Coscinodiscus radiatus and Surirella splendida. 1 had laid it aside for some time, when it occurred to me that the same course of proceeding which is necessary to bring out the siliceous frustules from guano might prove equally efficacious with this Thames mud. Acting on this idea, I boiled a portion of it for some time in hydrochloric and afterwards in strong nitric acid, until the whole was perfectly clean: and, on mounting it, the result far exceeded my expectations ; for though impossible to form an accurate conclusion, I should imagine that, excluding the coarse sand, nearly one-fourth of the finer part of the residuum was entirely composed of the siliceous valves of different species of Diatomacee ; and the prevalence of marine forms also proves that, at the distance of nearly forty miles from the mouth of the Thames, their distribution is very similar to that previously described by M. Ehrenberg in the Elbe. The only observations on this point of the inquiry, as regards British rivers, that I have met with, are notices of the species which occur in the Humber, and in a paper by Mr. T. F. Bergin,* read before the Microscopical Society of Dublin in 1842, who, from a careful examination of the deposits of the Liffey, after a perusal of Ehrenberg’s paper on the Mud Banks in the Harbour of Wismar, was led to a different con- clusion; and stated it as his opinion that a few species of Navicula, not comprising 1-1000th part of the mass, were the only organized forms that occurred in the mud deposited by that river. The cause of this he attributes to the fact of the source of the river being so short a distance from the sea, and, having its rise in the mountains of Wicklow, the rapidity * Microscopic Journal, vol ii., p. 68. Roprr, on the Diatomacee of the Thames. | 69 of the current is so great, that the germs of these minute organisms have not time to increase and multiply as they do in more sluggish streams, flowing for a long distance through alluvial deposits. A similar occurrence of marine Diatomacee at a considerable distance from the sea has, however, been noticed by Professor Bailey, in America, who, in his ‘ Microscopical Observations on South Carolina and Georgia,’ published by the Smithsonian Institution, expresses the surprise with which he found in Lake Monroe, 200 miles from the mouth of the St. John’s river, specimens of Amphiprora constricta, Odontella poly- morpha, and Navicula elongata, which he considered decidedly: marine, and which had often occurred to him on the shores of the Atlantic. I now proceed to give lists of the species from different localities in the Thames, placing those from the Isle of Dogs first, and comparing them with the forms from Hammersmith and near Gravesend ; and though I have been unable at pre- sent to examine the deposits of the two latter localities so as to give more than a general view of the species, yet these are sufficiently well marked to show the distribution of those peculiar to marine and fresh water. In all the localities many species of Melosira, Odontidium, and other genera occur, which, from the want of good figures, I have been unable to name. The well-marked frustules of those figured in the first volume of the Rev. William Smith’s valuable synopsis have been easily recognized, from the ex- tremely accurate figures there given. In all cases where any doubt existed, I have referred to slides of the species authen- ticated by Mr. Smith himself. In some few instances I am indebted to his kind assistance, and also to his able coadyjutor, Mr. West, for the determination of forms I was unable satisfactorily to identify, and in a few others I have depended on the figures of Kiitzing’s work on the Diatomacee. One if not two species of Dictyocha occur in the mud from the Isle of Dogs, but I have excluded them from the list, as there appears some doubt if they can be correctly referred to the same order. Marine and Brackish Water Species from the Isle of Dogs. 1. Epithemia sorex 9. Eupodiscus argus 2. se musculus 10. “5 fulvus 3. Amphora affinis li. a radiatus 4, - hyalina Zs ss sculptus 5. Cocconeis scutellum 13. Actinocyclus undulatus 6 N diaphana 14, aa sedenarius ? 7. Coscinodiscus radiatus 15. Triceratium favus 8 A eccentricus Care, ie striolatum ? h 2 70 Roper, on the Diatomacee of the Thames. 17. Triceratium undulatum 18. alternans 19. Cyclotella Kutzingiana 20. Campylodiscus cribrosus 21. bi-costatus 22. Surirella Brightwellii 23. 5 ovata 24. Fs gemma 25 * fastuosa, 26. a salina 27. Tryblionella marginata 28. 9 punctata 29. an acuminata 30. 5 gracilis 31. Nitzschia sigma 32. - angularis 33. » parvula 34. ig, dubia 35. Amphiprora alata 36. Navicula elliptica 37. MP didyma 38. 3 punctulata 39. Navicula Jennerii 40. bs pusilla 41. - elegans 42. Pinnularia directa 43. Bs distans 44. 5 peregrina 45. Stauroneis pulchella 46. Pleurosigma hippocampus 47. as strigilis 48. Synedra gracilis 49. » erystallina 50. » superba 51. » tabulata 52. Doryphora amphiceros 53. ss Boéckii 54. Odontella aurita . Podosira Montagnei . Grammatophora marina . Zygoceros rhombus . Melosira nummuloides . Achnanthes (a spec.) Fresh-water Species. . Epithemia turgida . Amphora ovalis . Cocconeis placentula 10. Campyllodiscus costatus 11. Surirella biseriata 1 2 - alpestris 3. argus 4, Cymbella Ehrenbergii D. re maculata 6. 55 cuspidata 7 i‘ helvetica 8 9 12. . pinnata 13. Cymatopleura solea 14. 4 elliptica 15. Nitzschia sigmoidea 16. Bs linearis 17. Navicula ovalis 18. a: producta Sys nA rhyncocephala 20. 55 inflata 21. “ gibberula 22. amphisboena 23. Pinnularia acuta 24, Pinnularia viridis 25. e oblonga 26. 9 major 27. “a radiosa 28. Stauroneis linearis 29. ”» Pheenicenteron 30. io anceps 31. Pleurosigma attenuatum . Synedra radians . Cocconema lanceolatum a parvum ‘ts cistula . Gomphonema acuminatum a capitatum 9 curvatum 3 constrictum a cristatum dichotomum . Odontidium hyemale . Fragillaria capucina _ Tabellaria ventricosa . Diatoma vulgare From this list it appears that out of one hundred and four species, fifty-nine are peculiar to marine and brackish water, of which thirty are decidedly marine. The following six species are, however, all that are identical with those included in M. Ehrenberg’s lists from Gliicksiadt and Hamburg, viz. : Coscinodiscus radiatus and eccentricus, Triceratium favus, Surirella gemma, Eupodiscus argus, identical with Tripodiscus Roperr, on the Diatomacee of the Thames. 71 germanicus and Actinocyclus undulatus, probably identical with Actinoptychus senarius. This would seem to show that though the general results were similar, yet from some peculiarity, either in the water or the distribution of these minute organisms, the species abounding in the rivers of the north of Europe are marked with a distinctive character from those found in the Thames. The prevailing form in the Elbe ap- pears to be the Actinocyclus, and its allied genus Actinoptychus of Ehrenberg, of which he enumerates no less than fourteen species out of the thirty-four marine forms that he recognised. On comparing with the foregoing list from the Isle of Dogs, the species which occur in the mud at Hammersmith and near Gravesend, it appears, that though a few marine forms are still found at the former locality, yet the preponderance of fresh-water species is very great ; whilst at the latter the marine and brackish water species, with a few exceptions, alone occur. The following lists include all I have at present met with from those localities :— Marine and Brackish Water Species from the Thames near Gravesend. 1. Epithemia musculus | 21. Nitzschia angularis 2. Cocconeis scutellum | 22. Amphiprora alata 3. Coscinodiscus eccentricus 23, Navicula Jennerii 4, — radiatus 24, Py didyma 5. marginatus ? 25 5 punctulata 6. Eupodiscus areus 26. Pinnularia cyprinus ce 5 crassus 27. Stauroneis salina 8. Actinocyclus undulatus 28, Pleurosigma angulatum u. a sedenarius ? 29. a hippocampus 10. Triceratium favus 30. Balticum LW 45 alternans 31, Doryphora amphiceros 12. Campylodiscus cribrosus 32. Achnanthes brevipes 13. Surirella ovata ood. Grammatophora marina 14, i gemma 34, Podosira Montagnei Ld. # fastuosa 35. Melosira nummuloides 16. Tryblionella acuminata 36. as sulcata 17. ne marginata 37. eA salina, US; As punctata 38. Odontella aurita 19. Nitzschia sigma 39. Orthosira marina 20. i dubia Fresh-water Species from Gravesend. 1. Cocconeis placentula 5. Navicula minutula 2. Coseinodiscus minor 6. Synedra ulna 3. Nitzschia sigmoidea ‘7. Cocconema cistula 4, Navicula cuspidata 8. Cyclotella rotula Marine and Brackish Water Species from the Thames near Hammersmith, 1. Amphora membranacea 2. Coscinodiscus eccentricus 3. Actinocyclus undulatus 4, eo Surirella Brightwellii Tryblionella gracilis a acuminata 72 Roper, on the Diatomacee of the Thames. 7. Nitzschia sigma 11. Pleurosigma hippocampus 8. Nitzschia parvula 12. Doryphora amphiceros 9. Navicula elliptica 13. Gomphonema marinum 10. Pinnularia directa 14. Odontella aurita Fresh-water Species from the same Place. 1. Epithemia turgida 16. Pinnularia viridula 2. Cymbella Ehrenbergii 17. He stauroneiformis o. Amphora ovalis 18. Pleurosigma attenuatum 4. Cocconeis placentula 19. Synedra ulna 5. Campylodiscus costatus 20. Cocconema cymbiforme 6. Surirella biseriata 21. ip cistula 7. Cymatopleura solea 22. Gomphonema acuminatum 8. 5 elliptica 23. - constrictum 9. i apiculata 24. Fragillaria virescens 10. Nitzschia sigmoidea 25. Diatoma vulgare 11. Navicula amphisbeena 26. Melosira arenaria Alas ms crassinervia 27. y varians 13. fe inflata 28. Fragilaria capucina 14, ‘5 cuspidata 29. Coscinodiscus minor 15. x amphirhynehus From these lists it appears that at Gravesend, out of forty- seven species, eight only are decidedly peculiar to fresh water ; whilst at Hammersmith we find there are twenty-nine fresh- water species out of a total of forty-three ; showing, however, that the influence of the flood-tide, even at that distance from the sea, gives a decided character to the Diatomacee deposited by the water. The following ten species are all that are common to the three localities :— Coscinodiscus eccentricus, Actinocyclus undulatus, Tryblionella acuminata, Nitzschia sigma, Pleurosigma hippocampus, Doryphora amphiceros, Odontella aurtta, Cocconets placentula, Nitzschia sigmoidea, and Cocconema cistula, of which the three latter alone are peculiar to fresh water. These are all forms which more extended observation on the deposits of other river and estuary deposits will pro- bably prove to be most universal in their distribution. I have found most of them in the mud of the Avon from Bristol, and also in that deposited at Pembroke Harbour; but it will re- quire a careful examination of many other deposits to prove that any have a purely local habitat, or are entirely confined to sea or fresh water. The following species which occur in the Thames have also been found by Professor Bailey in America, recorded in ‘Sil- liman’s Journal of Sciences’ for 1845, vo]. xlviii. p. 837 :— Iu the Mud from Charleston Harbour. Actinocyclus senarius Rhaphoneis amphiceros Coscinodiscus eccentricus Ne rhombus Eupodiscus argus Triceratium favus Pinnularia didyma | Zygoceros rhombus Pleurosigma Balticum Roper, on the Diatomacee of the Thames. 73 And in the Mud from Newhaven Harbour. Actinocyclus senarius Pinnularia peregrina Coscinodiscus eccentricus - didyma Gallionella sulcata Rhaphoneis rhombus Grammatophora marina | A proof of the widely-extended distribution of these species. From the first of the foregoing lists I have selected a few species for more particular notice, and annex drawings of the most interesting, on the scale adopted by Mr. Smith, namely, 400 diameters. There is:a large species of Cocconeis (Pl. VI. fig. 1), elliptical in form, and marked longitudinally with undulating striz, and also with faint transverse lines, concentric with the extremities of the valve, but only visible with a high power and oblique light. The perfectly elliptic form and peculiarity of the cross strie seem to distinguish it:from the C. placentula of Mr. Smith ; but I am doubtful whether it may not be a variety of that species, Of the four species of EHupodiscus, the most plentiful is EF. radiatus, which, from one specimen, in which three frustules were conjoined, may probably sometimes occur concatenated, in a similar way to Odontella aurita. EE. sculptus, the most peculiar in its markings, is rarely met with; and L. fulvus and argus are sparingly distributed. The latter shows the delicate hexagonal reticulations alluded to by Professor Quekett as marking the Tripodiscus Rogersii of Professor Bailey. ‘The star-shaped cells appear, when seen by direct light, to be placed in the centre of small bosses or protuberances, in which it differs from all other Diatomacee that I am acquainted with. The Actinocyclus undulatus of Mr. Smith’s Synopsis occurs abundantly. This species appears to include the Acti- noptychus senarius of Ehrenberg and Kiitzing ; but after a careful examination of many specimens, I have been unable to make out any undulations similar to those of fig. 4, in Plate V. of the Synopsis, in the large species that occur in the Thames and elsewhere; and although a multiplication of species is a point carefully to be avoided without good grounds, it appears to me that the appellation undulatus should be confined to a small form, in which these undula- tions distinctly occur, and the large and well-known species retain the name originally applied to it by M. Ehrenberg, namely, A. senarius. Sparingly distributed, I have another large and beautiful disc (fig. 2), with sixteen septa, the surface of which is covered with faint cross-stria, similar to those of Pleurosigma ; and in * See Histological Catalogue, p. 212. 74 Roper, on the Diatomacee of the Thames. that respect it resembles the valves from Natal, for which . Mr. Shadbolt proposed the name of Actinophenia ; but I find this striation is no distinctive character, as all the specimens of A. undulatus (or senarius) that 1 have examined have the same peculiarity, and the septa are plainly discernible, espe- cially with the parabolic condenser. In the lists I have ap- plied to it provisionally the name of Actinocyclus sedenarius, as it approaches very nearly to Ehrenberg’s figure of that species in the ‘ Berlin Transactions’ for 1839, tab. 4, p. 2. The septa appear to have their origin from the smooth central portion or pseudo-nodule, and to terminate at slight eleva- tions or openings at the margin of the disc, and in perfect specimens those on one valve are opposite to the interspaces on the other. The front view exhibits slight traces of undu- lations, as in fig. 13, not in continuous waved lines, but rising to points at the extremities of the rays, giving the side view an appearance similar to that of a ridge-and-furrow roof. The diameter varies from 1-288th to 1-187th of an inch. Of the genus Triceratium four species occur. A small one, by no means uncommon, is represented by fig. 3, which I consider the J. striolatum of Ehrenberg; it has convex sides, small horn-like processes at the angles, which are rather obtuse, and is marked with minute dots or cells, radiating from the centre. In the determination of this species I am, after a careful examination, compelled to differ from Mr. Brightwell, who, in his monograph of this genus in a late Number of the ‘ Microscopical Journal,’ refers to a Paper by M. Ehrenberg in the ‘ Berlin Transactions’ for 1839, in which there is a figure of 7. striolatum, and the following description of the species: —“ Testule lateribus triquetris convexis, angulis sub-acutis, superficie subtilissime punctato-lineata, dorsi cin- gulo medio levi; and yet Mr. Brightwell describes it as with ‘concave ends,” and figures it with concave sides; and in the frustules I have seen of his species, the central band on the front view is punctate or cellular, whereas it is described by Ehrenberg as smooth. ‘The cellular structure of the side view is also so plainly apparent, that it would hardly have been described as ‘ subtilissime punctato-lineata ” by so careful an observer. Looking, therefore, at Ehrenberg’s figure and description, I should conclude that the species figured by Mr. Brightwell cannot be the JT. striolatum, but should re- ceive some other appellation. The concave sides would seem to refer it to T. pileus of Ehrenberg; but I have not seen a figure or full description of that species. Triceratium alternans of Bailey is rarely met with; and I have only one specimen of JT. undulatum, in which the peculiar Roper, on the Diatomacee of the Thames. 75 projection of the posterior valve beyond the undulating sides of the upper, as noticed by Mr. Brightwell in his Paper before alluded to, is plainly shown. | Campylodiscus costatus and cribrosus are frequently met with. Another small species is represented by fig. 4, which Mr. Smith informs me he has named 67-costatus, and that he will give a figure of it in the addenda to his second volume. In appearance it so much resembles C. clypeus, that 1 had applied that name to it, especially as that species is included in Ehrenberg’s lists as occurring at Gliickstadt, Hamburg, and some localities in Holland, and was found by Professor Bailey in Lake Monroe. The valve is nearly circular, saddle-shaped, canaliculi about forty, distinct, length at the sides about half the radius, at the ends much shorter. The central portion has two narrow bands of coste parallel with the terminations of the side canaliculi. Diameter is about 1-384th of an inch, The most abundant species in all the slides | have examined is represented by figs. 7 to 10, which I believe would all be included as varieties of Doryphora amphiceros by Mr. Smith, and as different species of Rhaphoneis by Ehrenberg and Kiitzing. ‘The difference of form is so great, and the peculiarity of the cellular markings so apparent, that they appear to furnish data for specific distinction quite as good as are afforded in many species of Navicula and Plewrosigma. Not having Ehrenberg’s figures or descriptions to refer to, I am guided solely by the “species Algarum” of Professor Kiitzing. Fig. 7, from its lanceolate form, strong granular markings, and well-marked median line, might probably be referred to Rhaphoneis gemmifera. The length varies from 1-319th to 1-3820th of an inch; breadth, about 1-1090th of an inch; it occurs but sparingly. Fig. 8 is rarely met with, but is readily distinguished by its more robust form, the greater delicacy of its striz, and the slightly marked and nearly parallel sides of its median line. The length is 1-349th of an inch, and breadth 1-779th of an inch. It would be referred to Rhaphoneis fasciolata. Fig. 9 is exceedingly common, and in the size of its markings resembles fig. 7, but differs in being more concentric, and nearly obliterating the median line at the acute extremities of the valve. The breadth of the valve is also much greater in proportion to the length. ~The length is 1-600th of an inch, and breadth 1-1224th of an inch. It agrees with Rhaphoneis pretiosa. Fig. 10 is widely different from any of the preceding, and is by no means abundant. ‘The valves are very diaphanous, the mark- ings faint, median line obscure, and form ‘sub-orbicular, the 76 Rorer, on the Diatomacee of the Thames. apices being very short; the length is 1-588th to 1-779th of an inch, and breadth 1-1034th to 1-968th of an inch. I should refer it to Rhaphoneis rhombus. The only point of distinction between this genus and the Doryphora of Pro- fessor Kiitzing appears to be the presence of a stipes; and it would be a point of some interest to determine whether these forms are attached in a similar manner, or whether, as I imagine from the abundance with which they occur, and the absence of any direct negative observations, the frustules are free as in Navicula. A large and well-marked species is represented by fig. 5, which has not, I believe, been hitherto figured as British. I have been unable to obtain a front view of a perfect frustule, though the single valves are by no means uncommon. By a comparison with some specimens of Zygoceros rhombus from Petersburg, Virginia, kindly lent me by Professor Quekett, I have little doubt that it can safely be referred to that species,* as the only difference is, that in the Thames spe- cimens, the side view of the valves is rather broader in proportion to the length. The valves are nearly rhomboidal, slightly produced at the extremities, and terminate in a pro- jecting tubular horn or spine. The surface is minutely punctate with small hexagonal cells, radiating from the centre, and has from three to six small spinous processes at the sides, with two rather longer at the extremities of the valve... The length varies from 1-300th to 1-188rd of an inch, and breadth from 1-375th to 1-260th of an inch. Figs. 11 and 12 are, I believe, front and side views sie Zygoceros surirella of Ehrenberg. I have only met with one specimen of the perfect frustules, represented by fig. 14, which agrees in form with the figure given by him in the ‘ Berlin Transactions’ for 1839, tab. 4, fig. 12, and shows the smooth central band and striations, which distinguish the side view. Fig. 16, which I consider the side view of a larger specimen, somewhat resembles the genus Ahaphoneis, but differs, in the markings being nearly parallel, and though granular, so confluent as almost to appear as lines; the central smooth portion terminates in two lobes, corresponding with the pro- jections, which appear at the extremities when the front view — is obtained. ‘The length is 1-714th to 1-1240th of an inch, and breadth 1-1500th to 1-2500th of an inch. I have met with the same species in the deposits of Pembroke Harbour. Fig. 6 a and b represents a small cross-shaped valve that occurs sparingly, which Mr. Smith, from a drawing, thought * The genus Zygoceros is included by Mr. Smith in that of Biddulphia ; this will, therefore, be the Biddulphia rhombus of the ‘Synopsis.’ Roper, on the Diatomacee of the Thames. — At might be referred to his Odontidium tabellaria: it is peculiar, from the strongly-marked cross stri@, which occur on each side of the valve; the length is 1-1385th and the breadth 1-1750th of an inch. The form of the valve is similar to Ehrenberg’s figure of Staurosira construens,* which he describes ‘‘as a four-angled Fragilaria, separated from the nearly allied genus of Amphitetras, by the absence of openings at the four angles,+ but without authentic specimens for comparison, it is im- possible, from the small outline figure he gives, to refer it with certainty to this genus. Mr. West informs me he has met with it from many other localities.{| From the Thames near Gravesend [ have lately obtained a large and fine spe- cimen of Coscinodiscus, about the 1-107th of an inch in diameter. It has a smooth spot in the centre of the valve, and with that exception is covered with hexagonal cells, radiating towards the circumference. Mr. Smith informs me it is quite new to him, but approaches somewhat to C. marginatus, but differs from the descriptions given of that species. I have at present no other forms, either from this locality or at Hammer- smith, that call for special notice. From the foregoing observations it appears that at ee distance of at least fifty miles from the sea, the deposits of the Thames are still, to a certain extent, influenced by marine forms of life, and that at Greenwich, which is about forty miles from the mouth of the river, a most distinct marine character is shown by the examination of the species of Diatomacee which occur there. I think it very probable that many species are only brought up by the flood-tide, and being unable to exist in the slightly-brackish water, the siliceous skeletons are merely deposited in those parts of the river least subject to disturbing causes, and that they would rarely be met with in a living state. That they have a per- ceptible influence on the formation of shoals and mud-banks in the bed of the river there can be no doubt; and the great abundance and general distribution of species serve to illus- trate the occurrence of similar deposits in a fossil state, at localities now far removed, by alterations in the earth’s surface, from the streams or harbours in which they were originally deposited. Another point, probably worthy of attention, is the in- fluence these organisms have in the formation of deltas at the * See Berlin Academy Transactions, 1847, tab. 1, fig. 44. t See Berlin Academy Proceedings, 1843, p . 45. { From specimens I have lately seen of Ae Harrison, W.S., I am inclined to believe that this may be a small form of that species rather than O. tabellaria. As it is a doubtful form I have not included it in the lists. 78 Roper, on the Diatomacee of the Thames. mouths of large and slowly-flowing rivers, such, for instance, as the Mississippi, in which the mean velocity of the current at New Orleans is only about one mile and a half per hour for the whole body of water. Sir Charles Lyell, from expe- riments on the proportion of sediment carried down by the river, has calculated that, taking the area of the delta at 13,600 square miles, and the quantity of solid matter brought down annually at 3,702,758,400 cubic feet, it must have taken 67,000 years for the formation of the whole.* Now, as the siliceous frustules of the Diatomacee are secreted from the water alone, and would most probably be extremely abundant in so sluggish a stream (especially as Professor Bailey has found both marine and fresh-water species abundant in the rice- grounds), there can be little doubt that, without taking the larger proportion noticed by Ehrenberg in the Elbe, even if it were considerably less, it would reduce the above period by several thousand years, and the same cause would probably apply with equal force to the Ganges and Nile. M. Ehren- berg considered that at Pillau there are annually deposited from the water from 7,200 to 14,000 cubic metres of fine microscopic organisms, which in the course of a century would give a deposit of from 720,000 to 1,400,000 cubic metres of infusory rock or Tripoli stone. My principal object in the foregoing paper has been to direct the attention of microscopists more particularly to the Diatomacee deposited by rivers and in tidal harbours, not only in those localities where they occur in overwhelming abun- dance, on the surface of quiet estuary waters, but in the mud itself, in which many of the rarer forms, and doubtless many new species, are yet to be found. That such an examination is still a desideratum is, I think, shown by the fact that out of the 279 species described by Mr. Smith in the first volume of his ‘Synopsis,’ only six are given as inhabitants of the Thames, and a very limited number to the Avon, Orwell, and some other rivers; whilst the Severn, the Mersey, and many of our tidal harbours are altogether unnoticed. That examinations of this nature may sometimes prove useful in an economical point of view is very probable, parti- cularly as it has been noticed that the best samples of guano contain the greatest number of these siliceous skeletons, which doubtless serve to replace the large amount of silica ab- stracted from the soil by the cereal crops. Hence it is pro- bable that the deposits of many of our rivers would have a beneficial effect if applied to the land, and it rests with the microscopist to point out the most favourable localities for * Lyell’s Principles of Geology, 8th edit., p. 219. Roper, on the Diatomacee of the Thames. — fat obtaining it. Ehrenberg notices an instance where this has been done in Jeverland, where a blue sand, abounding in cal- careous and siliceous shells, is collected, and greatly increases the fertility of the arable soil to which it.is applied; and Professor Bailey also states that the mud of Newhaven har- bour is used as a fertilizer, and is found to contain 58°63 per cent. of silica. The distribution of the lower forms of Alge, particularly the Diatomacee, is probably more extended, both in point of time and geographical range, than any other class of or- ganized beings. Thus we see associated with gigantic reptiles and other extinct forms, several existing species of Diatomacee occurring in the chalk formation before the deposition of the tertiary strata, proving that the Eocene group is not strictly entitled to that designation, but that the dawn of the world in which we live extends much further back in the history of our planet.* And with respect to their local distribution, Dr. Hooker, in alluding to the deposits of the Victoria Bar- rier in the Atlantic Ocean, remarks,+ “‘There is probably no latitude between Spitzbergen and Victoria Land where some of the species of other countries do not exist. Iceland, Britain, the Mediterranean Sea, North and South America, all possess antarctic Diatomacee. ‘The siliceous coats of species only known living in the waters of the South Polar Ocean have during past ages contributed to the formation of rocks, and thus they outlive several successive generations of organized beings. The Phonolite stones of the Rhine, and the Tripoli stone, contain species identical with what are now contri- buting to form a sedimentary deposit (and perhaps at a future period, of rock), extending in one continuous stratuin for 400 miles.” | With the distribution of these forms in our own country we are only at present partially acquainted, and the prepara- tion, therefore, of carefully-compiled lists of species from different localities is still a point to be desired, and might probably lead to some interesting generalizations. In conclusion, I have only to hope that this slight attempt to bring before the Society the results of a careful examination of the Thames deposits may induce other and more expe- rienced observers to take up the same subject in other locali- ties. The facts I have brought forward are sufficient to afford, in the words of an excellent observer and late member of this Society, “‘a striking proof of the important part which * Humboldt’s Cosmos, p. 265. t Dr. Hooker, Flora Antarctica, vol. ii., p. 505. { Mr. Edwin J. Quekett, in London Physiol. Journ, Feb. 1844, p. 145. — 80 Roper, on the Diatomacee of the Thames. these minute organisms were created to perform in the depo- sition of materials for the earth’s surface, and stamp upon reflecting minds that no creature, even the most minute, is formed without special purposes ; and that the least in size of all, by the organization given to them by the great Architect of the Universe, have been employed to carry out his un- fathomable intentions.” wl POm P OF THE FOURTEENTH ANNUAL MEETING OF THE MICROSCOPICAL SOCIETY. Tue Microscopical Society of London held their Fourteenth Annual Meeting, February 15th, 1854,—Grorce Jackson, Esq , President, in the Chair. The Assistant Secretary read the following Reports :— Report of Council.— According to annual custom, the Council have to make a Report on the state and progress of the Society during the past year. The number of members at the last anniversary was—ordi- nary members 198, associates and honorary 5, giving a total of 203. Since that time there have been elected 28, making the total number 231. This number must, however, be re- duced by 3, who have retired, making a final total of 228, and being an increase of 25 upon the number at the last anniversary. ; The cabinet of objects and the library have been increased by various donations ; and there are also in the possession of the Society various drawings and diagrams relating chiefly to papers read at the meetings of the Society, together with copies of the several parts of the Transactions and of the Journal. The Council have also to state that, in consequence of the great inconvenience of the present rooms, they have decided upon removing from them. The Society will return to the rooms of the Horticultural Society in Regent-street, if possible, by the meeting on the 29th March. VOL. I. D Fourteenth Report of 84 “DL “Sh "169% AOU SI AJOLIOg oY} 0} SUISUOTEq S[OSUOH *7U2;) Jad ¢ Jo JUNOMIG ONT, x “HA TAOd “V “MA ‘rormne “TVORUAd “H ‘pqgT ‘Areniqag WET sty} poacidde pue pourmexg OL L OSGF OO = | PURy UL couTlee On Gn Cre a eee x%S[OSUOD “PZ ‘SBT ‘28h JO esByoin z O38 fen oI | oF ae SOM OUR ISOg “AOUQH UES 0 916 Fe ee ee 4 4 © g0q09T]09 0} WorssTUTUTO, 0 0 gL ° ‘0% ‘Aqdetsouyry ‘syrodoy ‘stuoloRsURI], SUULIG o: ef ie eo ce BL opmogne “929 “ST UOULYSeTJoyy tole eo ee OOO 9 ‘SOUIJOOTT 7B SOUBPUOTTV 6: 0l'Z eS eS Genego O20. 12h oe > + Azeyo100g JURISISSy a 023 ay oe ay eee Se ALOT CAO) JO Acre 0 8 02 ey See tS * SuLOOY JO JOY JOT “p38 *# "SENUNA V OL T O9aF 0-0 6 yf Ff fs 8 QOMOIABT “IJ, WO, UOTeUCG OT L Sv6F OSCE GlGe =i ZO . = oe a = pesl Arenupy.o9 sjos “WOO “PLT “89 “201% Uo spuepralq om, @ O Zia 3 Pio suo NOUS], jo sardop Or “h 36ce ee ae PSST pure “EgsT ‘SEs ‘TS81 srvok out IO} syueuded jenuuy 0 & & "+ (osquos wad se po1SdAUI Usaq OABY YOIYM) suor1sod uo) 0 8LT09 ° ° ° ° = StequteyT Jo souenUy 10,7 Ds °F Igoe: * 7 * ¢ * aves snorserd oy} wor courpeg DSF “SLAG RY, "PEST ‘IGT Arenaqay 09 ‘eegT ‘eT Avenaqoag wor ‘SUOLIGAV THE 40 LHOdda the Microscopical Society. | 85 The President delivered the following Address :— GENTLEMEN,—I have much pleasure in again congratu- lating you on the state of our finances; for, although the balance in hand is only twelve pounds more than that of last year, yet we have been enabled to pursue our usual course of investing the compositions received from life-members, and have thus increased our funded property from 2102. 5s. 11d. to 2591. 4s. 1d. It is the opinion of some who have had ex- perience in these matters, that a society which judiciously expends its yearly income is in a more healthy condition than one which hoards a large portion of it, and that therefore we ought carefully to avoid becoming rich. Until, however, our dividends form a much larger proportion of our annual assets than they do at present, we need entertain no fears on this head ; while the possession of a reserve fund to fall back upon in case of need cannot be regarded as an evil. By the arrangement which has been made with the editors for the supply of the ‘ Microscopical Journal ’ gratuitously to all our members, and by the prompt publication of our trans- actions, which have been brought down to the end of the year, a steady increase both of members and papers may be reason- ably expected; of which I trust the experience of the past year is but the commencement. Twenty-eight new members have been elected, and twelve papers, many of them of con- siderable interest, have been read. That of Professor Wheatstone, on the application of bino- cular vision to the microscope, has pointed out the advantages we may expect to derive from this principle, when certain optical difficulties have been overcome; and Mr. Wenham, by his ingenious contrivances and admirable workmanship, has vanquished some of these difficulties, and given us a glimpse of the benefits in store for us. The modification of artificial light by the intervention of coloured glasses has often been attempted, but it has generally been found to impair definition. The combination proposed by Mr. Rainey, for the purpose of stopping the heating rays, although it sensibly diminishes the light, appears to answer remarkably well. Dr. W. Gregory, Mr. Shadbolt, and Mr. Roper have con- tributed papers on Diatomacee. The latter, on those of the Thames, is particularly interesting, as opening a field of research in our own vicinity, the specimens being obtained from localities with which we are all acquainted. Mr. Legg’s paper on sponge-sand contains many hints 86 _ Fourteenth Report of which collectors and mounters of objects will find useful in their pursuits. Mr. Boswell has communicated an interesting fact on the mode of progression of Actinophrys Sol. His subsequent paper on the bird’s-head processes in Polyzoa had been anticipated by the accurate and more extended observa- tions of Mr. Busk, read two months before. The valuable paper of Professor Quekett, on “‘ a combustible mineral from the coal measures of Torbane Hill,’ clearly demonstrates the presence, not merely of the remains of plants, but of a peculiar woody structure in every description of coal, and the absence of this peculiar structure in the mineral in question. In microscopic botany we have been favoured with two interesting communications: one by Dr. Hobson, on the development of tubular structure ; and the other on the disease affecting the vine, by Mr. T. West. As mostoof shese papers have been already published, a more extended analysis of them would only be tedious. I would rather occupy a few minutes in considering how far this Society, during the fourteen years of its existence, has accom- plished the objects which its founders had in view at its formation. On turning back to our “ History, Constitution, and Laws,” we find it recorded that one of these objects was the ‘¢ promo- tion of improvements in the optical and mechanical construc- tion of the microscope.’ With the improvements which have been made in the construction of object-glasses, the Society for many years had but little to do; although, by promoting the use of the instrument, and by keeping alive a spirit of rivalry between the different makers, it was not altogether without influence. Recently, however, an amateur among our own members has demonstrated the possibility of getting good definition with an angular aperture that admits of no appreciable increase; and has thrown out suggestions, which, if carried into effect, will be productive of still further advantages. In the mechanical construction of the instrument, and in the different methods of illumination, so many improvements have been made by our members, that [ should take up too much of your time were I to attempt to enumerate them. The next object proposed for the Society, “ the communi- cation and discussion of observations and discoveries,” has constituted the principal occupation of our hours of meeting; and for the interest and variety of the subjects, I need only refer to the volumes of our ‘ ‘Transactions.’ These observations have been altogether the result of indi- vidual and self-directed researches ; but it is worthy of con- the Microscopical Society. | 87 sideration whether more might not have been done had we adopted the co-operative and systematic mode of proceeding recommended by our first President. ‘That Professor Owen’s suggestions may not altogether be lost sight of, I will, with your permission, quote a paragraph or two from his Address at our Second Anniversary ! After remarking on the importance of conceiving clearly the aim of our researches, and giving a right direction to our exertions, he says: “ A slight glance even at the classes of natural objects, of which the intimate structure remains but partially, if at all, known, will suffice to show us how many are the subjects that might be profitably selected by an indi- vidual or a committee for a systematic series of microscopical observations. In the animal kingdom, for example, how little we know of the modifications of the microscopical structure of shells recent and fossil, of the stony habitations of the nume- rous class of polypes, of the crustaceous coverings of the annulose animals, of the calcareous coverings of the Echino- dermata, or of the bones in different classes of animals, and in different parts of the skeleton of the same animal ! “‘In Mineralogy how much remains to be done in the microscopical investigation of different classes of rocks, as of oblites, of sands, flints, &c. ‘If committees were appointed to take different subjects of minute research under their respective care, in how short a time might a vast body of microscopical facts be accu- mulated !” Selecting a few subjects from the Professor’s list, let us see what the systematic researches of three individuals, quite dis- tinctly carried on, have effected. The structure of shells has been ably investigated both by Dr. Carpenter and by Mr. Bowerbank ; the structrue of flints and agates also by the latter ; and that of bones, developing general views of much importance, by our indefatigable Secretary. Had committees been appointed, as Professor Owen sug- gested, and had their members worked with half the zeal and -assiduity displayed by these three gentlemen, what a vast body of microscopical facts might by this time have been accumulated ! The “ formation of an arranged collection of microscopical objects” was another of the ends proposed to be effected by the Society; but, considering the number of our Members, and that many of them are dextrous manipulators, frequently engaged in mounting specimens, the progress made in stocking our cabinet is by no means a subject of congratula- tion. The last object proposed to be attained was “ the esta- 88 Fourteenth Report of blishment of a library of standard microscopical books.” Here also, although something has been done, we have no cause for boasting. But if every Member who wishes to refer to such works, and cannot find what he wants in our library, were to address a note to the Council, giving the title of the book needed, we should gradually have these deficien- cies supplied. There are one or two subjects of microscopical investigation that do not appear to have attracted our attention so much as might be wished. Some communications from the Rey. J. B. Reade, in the early days of the Society, served to show that the microscope might be made of great utility in delicate chemical re- searches; and a paper by Dr. Bird Herapath, in the Fifth Number of the ‘ Microscopical Journal,’ strongly confirms this view ; but, with the exception of some incidental notices of the application of chemical tests to determine the nature of organic structure, very little of chemical microscopy has come before this Society. For this there may be a sufficient reason; the subject is a special one, and chemists may prefer bringing their microscopical observations before the Chemical Society, to the alternative of submitting chemical matters to the Microscopical. How far they are right I will not determine. When we look over the list of our Members, and observe the number of medical men included in it, we may well be surprised that our ‘Transactions’ have been enriched with so few papers on Animal Pathology. Had this been the case only since the institution of the Pathological Society, a reason similar to that above assigned might account for it; but even now it may fairly be questioned whether the accuracy of dis- coveries in microscopical pathology would not be better tested by a body of men accustomed to use the instrument, and to examine matters of all kinds with it, than by those who have not had these advantages, however well they may be acquainted with the general subject. A physician in a neighbouring country some years ago announced that, by the aid of- the microscope, he had disco- vered a pathognomonic symptom of pulmonary consumption in a peculiar egg-shaped body occurring in the sputa. It was afterwards found that in the hospital to which he was attached the consumptive patients breakfasted on arrow-root, and the peculiar bodies were some of the unbroken starch granules that had stuck to their mouths. In both the addresses of Professor Bell this want of papers on Animal Pathology is noticed ; and his ideas are so just, and the Microscopical Socrety. | 89 his language so clear and forcible, that 1 cannot better con- clude the subject than by quoting the last paragraph from his Address at our Sixth Anniversary: ‘Let us remember,” said he, “ that the instrument which we employ is capable of elucidating subjects of far more importance than the distinc- tion of species of animalcules, and the demonstration of the structure of a zoophyte. The relief of suffering, and the sal- vation of life itself, are amongst the legitimate objects of microscopic research. Let not our medical members, then, be satisfied with the mere amusement, or even the bare scien- tific information to be derived from it; but let them employ it as an important means of carrying out the great objects of their profession, in determining the nature of diseased struc- tures, the distinctions between the healthy and morbid states of the tissues, and, consequently, in enlarging our means of restoring health to the sick, ease to the suffering, and life to the dying.” It only remains, Gentlemen, for me to express the satisfac- tion which I feel in resigning this Chair to one whose inti- mate knowledge of physiology in both its branches, no less than his general scientific attainments, so eminently qualify him to preside at our meetings. It was unanimously resolved—That the Reports of the Council and Auditors be received ; and that the Reports, with the President's Address, be printed. The election of officers took place ; when the following were declared elected :— Officers. MESUUCHE ss Dr. CarrENTER. PCUSUPCT ek N. B. Warp, Esq. RGEC ks JOHN QUEKETT, Esq. New Members of Council. Dr. Lions, BEALE. JosH. Gratton, Esq. M. MarswHa tt, Esq. Sami. C. WHITBREAD, Esq. In the place of WarreEN De La Rug, Esq. W. Giiert, Esq. Joun Ler, Esq., LL.D. Rosert Warineron, Esq. Hoae, on the Water-Snail. oT Observations on the DevELopmMENT and GrowtH of the WaTER- Swart (Limneus stagnalis). By Jasez Hoee, M.R.CS.. &e. (Read March 29th, 1854.) In submitting the observations which I have the honour of bringing to the notice of the Fellows of the Microscopical Society this evening—on the Development. and Growth of the Water-snail (Limneus stagnalis)—I do so with considerable diffidence. When I first gave the subject my special atten- tion, and began to jot down the remarks that occurred to me as growing out of my experiences, I was not fully aware of the extent to which many able investigators had traversed the same ground before me. So far back as 1754, precisely a century since, Baker, in his book entitled, ‘ Employment for the Microscope’ (p. 325), was the parliestito sdeserihe ‘a small water-snail and its spawn, or eggs, fastened in little masses, against the sides of the glass,” in which he kept them. It also engaged the attention of the illustrious Swammerdam; and, more recently, that of Reaumur and Dr. Grant. Mr. Bowerbank’s very interesting and careful observations on the ‘ Structure of the Shells of Mollusca and Conchifera,’ and the scientific researches of Dr. Carpenter, have thrown great additional light upon this subject. A brief record of my own personal investigations, with regard to this department of microscopic observation can, therefore, present no signal feature of interest beyond that of confirming and enforcing the experience of the talented and eminent micro- scopists who have preceded me. It is with this view that I venture to lay before the Microscopical Society the few remarks which I have now the privilege of reading, happy if I shall have contributed, in however slight a degree, to add in any way to the store of knowledge already accumulated. Into a glass vase, where my stock of Chara, Vallisneria, &c., is growing, | introduced last Autumn a single Limneus, for the purpose of observing its habits; I was then more espe- cially curious to see its mode of creeping along, under the surface of the water, by means of its fleshy foot. Upon one occasion, as I sat watching the movements of the animal, attached as it then was to the side of the vase, near the surface of the water, it suddenly became uneasy, moving to and fro, and im a short time it began to deposit very slowly, through a fissure near its ventral aperture, a small gelatinous sac, filled with transparent specks, at the same time firmly gluing it to the glass. This sac I examined with a pocket magnify- ing-glass, and found it contained fifty-six ova. Each egg was VOL. II. OZ Hoge, on the Water-Snail. of an ovoid form, and consisted of a pellucid membrane filled with a transparent fluid, having a very minute yellow spot, the yolk, adhering to one side of the cell-wall. Seen with the sunlight falling upon it, it had all the brilliant colours of the soap-bubble. Viewing it again on the second day, I observed that the yolk had a central spot, or nucleolus, rather deeper coloured than the rest. On the fourth day the yolk had changed its position, and doubled in size, as shown slightly magnified (Plate VII. fig. 1). Upon a closer examination, a central depression, or transverse fissure, could be seen, which, on the sixth day, plainly indicated the line of demarcation in the little mass, as represented at fig. 2. From this time it commenced to move round the whole interior of the cell, with a very slow rotatory motion ; the motion was increased when the sunlight shone upon it, from which I concluded, that, as it received more heat, its movements were thereby accelerated. The increase in size of the two parts of the animal appeared to be uniform up to the sixteenth day, when the shell apparently occupied the larger portion, represented at fig. 3; and the spiral axis, around which the calcareous lamelle were being deposited, had a much darker colour than the soft, or cephalic extremity. On the eighteenth day the tentacle was visible, with a small black speck at its root, the eye; this was seen to be protruded with the movement of the tentacle. Upon closely watching it, a fringe of cilia could be seen surrounding the tentacle and oral aperture ; and, from observing the direc- tion of the currents, I am led to believe that the earliest rotatory motion is in a great degree, if not wholly, dependent upon the action of the cilia. A constant current being kept up in the cell-contents, we may conclude, that with this motion, we have the conversion of the cell-contents into the several tissues ; and probably the whorl-shape of the shell is likewise due to the same formative process. The rotation was, on every occasion of my observing it, from the right to the left, and this always combined with a motion around the egg ; the embryo performing a circuit, as represented magnified at fig. 4, and forcibly reminding me of M. Wichura’s scientific investigations into the curious property possessed by the leaves of plants, of winding generally in a particular direction. He observes :— ‘¢ It is a very remarkable phenomenon, that the circularly or heliacally acting forces of nature follow an unchanging, definite, lateral direction in their course. In cosmical nature the planets describe heliacal lines, wind- ing to the right in space, by virtue of their circulation from west to east ; since this is combined with the advance, in company with the sun, towards a point in the northern hemisphere. In the department of physics we meet with allied phenomena in the circular polarization of light, and in Hoga, on the Water- Snail. | 93 the course of electro-magnetic spirals. Organic life exhibits the same laws in the circulation of the blood, in all cases starting from the left side of the animal body ; and in the heliacal windings of the shells of Mollusks, which follow a direction determinate for every species. But plants, above all, give evidence of a wonderful obedience to such laws, in the direction of the spiral vessels, the heliacally winding trunks of trees, winding stems and leaves, and probably also in the circulation of their saps.” * Professor Quekett has directed attention to this subject, especially with regard to plants, in his ‘ Histological Lec- tures. ‘To proceed :— From the twenty-sixth to the twenty-eighth day the little animal was actively engaged in making its way out of the egg, in the advanced stage represented at fig. 5, leaving its _ shell behind it in the ova-sac, and immediately attaching itself to the side of the glass. The ciliary motion is then better seen ; each tentacle being surrounded at the extreme edge by a row of cilia kept in motion by bands of muscular fibre : the cilia are protruded from beneath the shell, and kept incessantly at. work, in conjunction with those surrounding the opening to the mouth; thus bringing a constant current of water for the gration of the branchiz, situated above the oral aperture ; and at the same time a due supply of nourishment for the growth of the little animal. And it is a remarkable fact, that, as soon as the gastric teeth are properly matured to enable it to cut the vegetable substances growing in the water, the cilia being no longer required, then disappear, and drop off, from the tentacles. ‘The tentacles and oral fringe of cilia are represented magnified, in the drawing, at fig. 6. But if, on the other hand, the young animal be kept in fresh water alone, without vegetable matter of any kind, it still retains its cilia, and attains only to a small size; it then acquires gastric teeth, but of a very imperfect character, which never attains to perfection in form or in size. If at the same time it is confined to a small narrow cell, it will only grow to such a size as will enable it to move about freely; thus adapting itself to the necessities of its existence. Dr. Grant, I believe, first pointed out the ciliary motion in the embryo of some salt-water species of Gasteropoda. In examining the embryos of Buccinum undatum and Purpura lapillus, which are also enclosed in groups within transparent sacs, he was struck with an incessant motion of the fluid in the sac towards the fore-part of the embryo; and he then noticed that this motion was produced by cilia placed around two funnel-shaped projections on the fore-part of the young * M. Wichura, ‘“‘On the Winding of Leaves,” translated by Arthur Henfrey, F.R.S., ‘ Scientific Memoirs,’ 1853. hk 2 94 Hoee, on the Water-Snail. animal, which form the borders of a cavity, in which he per- ceived ‘a. constant revolution of floating particles. He also observed these circles of cilia in the young of the species of Trochus, Nerita, &c., in which the embryo was seen revolving round its axis. He met with the same appearance in the naked Gasteropoda, as the Doris, Eolis, &c. The embryo of these revolve round its centre, and swims rapidly forward by means of its cilia, when it escapes from the ovum, Dr. Grant assigns various uses to these motions, but does not connect them with respiration or nourishment, although there can be little doubt that they are so. In some six weeks, or two months, the flattened form of the shell becomes gradually changed into that of the conical form of the full-grown animal (fig. 7).* That this little creature is hermaphrodite, like the common snail, is proved by my having only this solitary animal in my vase; and yet nearly all the eggs deposited by it arrived at maturity. Like the common snail it is also copulative, as I have seen two animals mutually pass a thin tongue-like organ into a fissure between the body and upper surface of the pos- terior portion of the foot. I observed in the few eggs that did not come to maturity that the yolk only slightly increased in size, and then remained in that state until all the others were hatched, when the ova- sac became the prey of other animals. This one snail deposited two and three of these ova-sacs in the course of the week; and in two months I calculated that upwards of 800 young would result therefrom; thus it will be seen, that the number of eggs deposited by each individual is very great; fully explaining the rapidity with which this class of animals increases, either on land or in the water. The shell, as we have before seen, is begun at a very early stage in the formative process. It is first observed to have the shape of minute ovoid cells, which are deposited side by side around the axis, or central cell; and this may be described as a cytoblast, enclosing a certain quantity of colour- ing matter, just sufficient to give it a distinctive appearance, from the previously-formed basement membrane. ‘The sides of one cell being in close contact with those of other cells, a gradual compression, or elongation, takes place, and we have, finally, resulting divisional ribs, hardened by the deposition of calcareous matter into a shelly covering. Subsequently all trace of the earliest cells and cytoblasts are lost. 7 * In warm weather the eggs arrive at maturity in a much shorter time, especially when exposed to the light and warmth of the sun. Hoag, on the Water-Snail. ob My own observations upon the Zimneus, in many important particulars, coincide with those of Mr. Bowerbank, made in 1843, and published in the Transactions of this Society, upon the Structure of Shells of Mollusca, &c. Mr. Bowerbank thus explains the development of the shells of these animals :— ‘‘ Let us suppose the rudiment of the future shell to have been the result of the excretion of some mucus or lymph (properly, albumen) ; it would then be nothing more than a very thin transparent membrane, with a determinate figure dependent upon the figure of its species. In this membrane organizing cytoblasts and cells are produced and multiplied in rapid succession, until, by their increase and opposition, a cellular struc- ture is formed in it. On their first appearance the cells are transparent and globular, but pushed on by the law of growth, which regulates their development, they very soon begin to secrete, from their inner surfaces, carbonate of lime. The cells being filled with it, a solid structure is the result of their close aggregation ; the pattern being modified only by the form and degree of condensation of the caleigerous cells, in which it has been secreted. ‘i * % * A layer or stratum of shell being thus formed, another is produced from its inner surface by the same means, and then others, until the normal set is completed: the whole being kept together as one by the living tissues.” Mr. Bowerbank believes that the truth of this mode of formation is proved, not only by the structures he has dis- covered, but also by the phenomena which occur in its repa- ration of injuries; for he says :— ** This reparation is not made by a coat of calcareous matter, spread over the wound by the collar or mautle of the animal, as has been main- tained, but by an effusion of coagulable lymph, in which cytoblasts are produced in the first instance, and quickly succeeded by a cellular struc- ture, in which the earthy basis of the shell is secreted, and by which the scar is filled up, or the fracture cemented together,.”’ This I have repeatedly verified, and always found that after an injury to the shell of either an embryonic, or more perfectly- formed animal, in a few hours subsequently the process of repair has been commenced by a deposition of cells, less in size, and somewhat more irregular in form than the first. Upon breaking off an eighth of an inch from the edge of the shell of a full-grown animal, I observed that it first threw out a series of exudations of plasma, or albuminous matter; which, after some days, became hardened by a calcareous deposit, corresponding in appearance to the lines of growth of the old shell, but only to the extent required to convert the edge into a smooth and strong margin of about one-half the breadth broken off; and, ultimately, new lines of growth were thrown out beyond the edge of the mantle; this I clearly ascertained by scraping it with a fine knife. In reference to this part of my inquiry I may be pardoned for directing 96 Hoge, on the Water-Snail. attention to the very interesting observations of Professor Paget :— “That the reparative power in each perfect species, whether it be higher or lower in the scale, is in an inverse proportion to the amount of change through which it has passed in its development from the embryonic to the perfect state. And the deduction to be drawn is, that the powers for development from the embryo are identical with those exercised for the restoration from injuries : in other words, that the powers are the same by which perfection is first achieved, and by which, when lost, it is recovered. Indeed, it would almost seem as if the species that have least means of escape or defence from mutilation were those on which the most ample power of repair has been bestowed ; an admirable instance, if it be only true, of the beneficence that has provided for the welfare of even the least of the living world, with as much care as if they were the sole objects of the Divine regard.” Dr. Carpenter differs in some particulars from Mr. Bower- bank, more especially with reference to the vascularity of ‘the shell, which, I believe, he entirely denies, and somewhat inclines to the more generally received opinion of Reaumur ; who, after careful examinations of the shells of Gasteropoda, came to the following conclusions :— ‘‘ That these calcareous defences are mere excretions from the surface of the body, absolutely extra-vital and extra-vascular, their growth being carried on by the addition of calcareous particles deposited in consecutive layers. The dermis, or vascular portion of the integument, is the secreting organ, which furnishes the earthy matter, pouring it out apparently from any part of the surface of the body, although the thicker portion, distin- guished by the appellation of the mantle, is more especially adapted to its production. The calcareous matter is never deposited in the areole of the dermis itself, but exudes from the surface, suspended in the mucus which is copiously poured out from the muciparous pores, and gradually hardened by exposure ; this calciferous fluid forms a layer of shell, coating the inner surface of the pre-existent layers to increase the size of the original shell, or else in furnishing at particular points for the reparation of injuries which accident may have occasioned.” * Now, if it be a mere excretion from the surface of a mem- brane, and neither vital nor vascular, how does Reaumur account for the deposit of the calcigerous cells, and subse- quent formation into shell, so early seen in the embryo; and that long before these cells can become consolidated by exposure to air? Mr. Bowerbank has seen, as well as myself, that at a very early stage of embryonic life, calcareous matter is deposited, and hardened into shell ; and this can be readily proved, by simply breaking up the egg, and submitting a portion of the contents to the action of a drop of very dilute acetic acid, when the carbonate of lime will be very quickly * ¢ Article Gasteropoda.’ By Professor Rymer Jones. ‘ Cyclopedia of Anatomy and Physiology.’ Hoee, on the Water-Snail. 97 dissolved out, with a brisk effervescence; the basement mem- brane only remaining, as in the older shell. _ If the young animal be viewed under a power of 150 diameters, the whole mass is sufficiently transparent, to show that the shell is an important part of the whole structure, and not “ suspended in mucus ;” but has a hardened and definite form long before it issues from the egg, or comes in contact with the external air, to produce any hardening effect upon it. Mr. Bowerbank has observed, that in the fully-formed shell “the mode of effecting repairs in the periostracum, affords evidence of a high degree of vitality.” As to the term extra- vital, | know not what it means; and, I believe, no one who has bestowed care and attention in the investigation of the works of the Great Creator, will for one moment assume the smallest speck to be an extra-vital production, or addition. Indeed, it appears to me that it would be as reasonable to deny the vitality of bone, or the growth of the lower organized cartilage, as to deny it to the shell of the pectinibranchial and pulmonated Mollusks. Dr. Carpenter says :— ““ It may now, however, be stated as an ascertained fact, that shell always possesses a more or less distinct organic structure ; this being, in some instances, of the character of that of the epidermis of higher animals, Ne in others having more resemblance to that of the dermis, or true skin.” From repeated examinations, I believe, with Mr. Bower- bank :-— “‘ That the structure of shell is analogous to bone in some respects, and is formed much in the same manner as in particular kinds of bony matter, by the deposition of carbonate of lime within the cells of the membranes, which enter into the composition of the shell, or by the aggregation and coalescence of the calcigerous cells when the membrane is very sparingly produced ; and that it is made up of three strata. Hach stratum being formed of innumerable plates, composed of elongated cellular structure ; each plate consisting of a single series of cells parallel to each other. These plates of cellular structure are deposited alternately in contrary directions, so that each series of cells intersects the one beneath it, at nearly right angles.” If to a portion of the periostracum a small quantity of very dilute acetic acid be added, to dissolve out the calcareous matter, and it be then viewed under a magnifying power of 250 diameters, it will be seen to be composed of oval cyto- blasts, exhibiting distinct nuclei, beneath which will be found a fine membrane studded with minute spots, apparently the escaped contents of the cells. This membrane has a regular series of corrugations or folds arranged throughout its whole extent, which gives to the shell in certain positions an 98 Hose, on the Water-Snail. iridescent lustre. Immediately beneath this is placed the transparent basement membrane of an even texture and very light amber colour, this is the albuminous or animal mem- brane ; which with the layer before referred to, and above this, appears to me to be traversed by tubes, that no doubt run from the inner to the outer portion of the shell substance, and probably this net-work of pores have assigned to them similar duties to those in the human skin, viz., that of throwing off effete particles of matter, &c. The very small proportion of animal matter contained in this shell is a marked characteristic ; after the removal of the calcareous matter by dilute acid, we have the small residuum of a grain or two only ; from this cause the shell is very brittle at all times. The shell of the fully-formed animal is ovate, whorls five or six, elongated and dextral; thus favouring, as before observed, the notion that the circular motion of the embryo when in the egg determines the whorl.* The mantle of the animal partakes of the same character and structure as that of mucous membrane generally, more especially that portion of it lining the internal surface of the shell; thence itis reflected over the body, and forms a direct communication with the external shell and internal soft parts. Its other important use, besides that of depositing carbonate of lime, is the secretion of plasma, or a glazing fluid, which it spreads over the internal portions of the shell, and with which it lubricates the whole of the external parts, thus pre- venting any irritation that might arise from a drying up of | the coarser particles of calcareous matter. Another use I have particularly noticed, is that of converting a large part of it, beneath the greater whorl of the shell, into an air-bag, or receptacle for holding a bladder of air, which must have consi- derable influence in rendering the shell buoyant and light, as by suddenly discharging it, the animal instantly sinks to the bottom. The animal is often seen to rise to the surface of the water for the purpose of taking in a supply of fresh air, which it does by opening a small valvular aperture, situated about the eighth of an inch above the ventral outlet. If the animal be removed from the water it immediately squeezes out this supply of air, at the same time it presses out the water from the body, for the purpose of enabling it to recede * For further information and much interesting matter upon this sub- ject I must refer to Mr. Bowerbank’s researches upon the ‘ Structure of Molluscous and Conchiferous Animals,’ most accurately and carefully illustrated, published in the Transactions of this Society, 1843. Also Dr. Carpenter’s researches, published in the Reports of the British Association, 1844 and 1847; and his ‘ Principles of General and Comparative Phy- siology.’ Hoaa, on the Water- Snail. 99 into the interior of its shelly house for protection ; in this act it is greatly facilitated by the action of retractor muscles, having a strong tendinous attachment to the columella of the shell. Theshell of the young animal, and thin portions of the older shell, viewed by polarized light on the selenite stage, are interesting and beautiful objects. In the young animal the growth of the membranous part is effected by the gradual expansion of the vascular and cellular tissues, and we are soon enabled to define the expanded foot. This is a fleshy disc, broader anteriorly and divided into transverse segments ; by a particular arrangement of the longitudinal muscular fibres it is enabled to perform a series of undulatory move- ments, by which means the animal glides smoothly along; its under surface is likewise studded over with a number of small orifices, which assist in causing a vacuum to be formed, and thus it suspends itself in an inverted position from the surface of the water, moving about in any direction, The muscular fibres, by their interlacements, greatly assist the animal in its progression, and in the performance of rapid movements; at the outer edge it is, turned over, or returned upon itself, forming a smooth and strong margin of condensed tissue and muscular fibres, which take their course in broad fasciculi, and gradually taper off toa thin tendinous attachment on the pillar of the shell. The mouth is situated at the under and fore-part of the head ; it is a muscular cavity, enclosing a dental apparatus, semicircular in shape and provided with transverse rows of projecting spines, or teeth of a horny structure, or, more correctly, alternating rows of incisor and canine teeth, each being pointed with silica, and accurately fitted to cut against each other; they are thus admirably adapted for the scraping or stripping off the cuticle from the blades of Vallisneria, which the animal does without killing the plant, and leaves it more accurately divided, than at all possible to obtain by the usual mode of splitting for microscopic observation. The gastric teeth are immediately joined to the csophagus or gullet, and to this succeeds the gizzard, a strong muscular apparatus, a quarter of an inch in length, and having a rugose appearance, with transverse and longitudinal fibres, by means of which every movement requisite for the conversion of the food is effected, and passes into a small membranous sac, the stomach ; this is folded into longitudinal plice, and from it arises the large intestine of considerable length, having much of the appearance of intestine in the higher order of animals, excepting in colour ; a narrow longitudinal band passes down on either side of the external coat, and internally it is apparently 100 Hoee, on the Water-Snail. supplied with valves. In its course it takes a considerable turn around the inner whorls of the shell, terminating in a rectum which has its vent placed between a small portion of the mantle and the under edge of the last whorl of the shell. The liver is not nearly so large as it is in the land-snail ; it consists of two lobes, and is enclosed in a strong capsular covering ; it pours a pale-coloured bile into the stomach by more than one duct, and is provided with a proper hepatic system of vessels. The heart is a strong muscular apparatus, having both an auricular and ventricular cavity; it is surrounded by a very delicate membrane (the pericardium). In shape it is pyriform, with muscular cords stretching from side to side, of a highly elastic character, looking not unlike very fine bands of India- rubber alternately contracting and expanding ; these cords are, no doubt, analogous to the corde tendinee of the mammal heart. ‘The heart receives the erated blood from the respira- tory organs, and propels it through the vessels at the rate of sixty times a minute. It is placed far back in the superior portion of the shell, near to the axis, where itis securely fixed without reference to the movements of the mouth or body of the animal. Like others of this family of aquatic Gasteropoda, the breathing apparatus resembles the branchiz of fishes in struc- ture ; they are pectinated, and placed in three or four rows near the roof of a cavity under the integuments of the head, or rather above the oral opening, which is peculiarly arranged with retractor and other muscles, for the purpose of permitting an uninterrupted eration of the blocd as it is brought to the branchie. The nervous system consists of many gangliz, or nervous centres, in place of a distinct brain, but “each of these gangliz may be considered as a distinct brain of the hetero- gangliate form.’ They are freely distributed throughout the body, but connected with each other by cords of communica- tion ; the nervous mass appears to be granular, and is some- what yellow in colour, whilst the nerves themselves are white and smooth, and invested with a delicate membrane (neur?- lemma). Professor Jones observes that— ‘‘ One remarkable circumstance may be mentioned as peculiar to this class ; the changes of position of the nervous centres obey the movements of the mouth, with which they are intimately connected ; they are, in fact, pulled backwards and forwards by the muscles serving for the pro- trusion and retraction of the oral apparatus, and are thus constantly changing their relations with the surrounding parts. ‘“«' he ganglia, placed above the cesophagus, sends off branches to supply the muscles of the head, the tentacles, and give origin to the optic nerves ; Hoge, on the Water-Snail. . 1Or and from the sub-cesophagial ganglion, which fully equal the former in size, arise those nerves which supply the muscles of the body, and of the viscera.” * The singular adaptation of the eye must not be omitted ; this appears in the early embryonic stage to be situated within or on the tentacle, it is constantly retracted with it, which is due to the length of the pedicle, and to the retractile sheath of the optic nerve, enabling the animal to shorten it; at the same time the tentacle folds down over it, forming a protec- tive cover at all times. The eyes are situated at the base of the inner side of the tentacle, and resemble two very small black spots. When examined with a power of 100 diameters, they are seen to be transparent spherical lenses, surrounded by a black zone or iris, the pigmental layer is continued some distance down the pedicle. It is pear-shaped, and evidently the little animal is very quick-sighted, as he avoids every obstacle placed in his way, or quickly withdraws himself into his house if one attempts to touch him; although in avoiding obstacles he appears to make great use of his tentacles as true feelers. ‘The tentacles are composed of a dense elastic tissue, surrounded by a band of muscular fibre ; in shape they are triangular, with the base attached to the body of the animal. The Limnei are stated by Professor Forbes to have been found in the fossil state as far back as the Oolitic epoch; and the most ancient forms bear a striking resemblance to the common existing types. In England, at the present time, they are abundant in nearly all the waters where vegetable matter is growing, and in the slow running rivers, especially where the water-cress is found. The Limneus, like every other living thing, is infested with its parasite. Reaumur observed a sort of mite infesting the snail (Helix aspersa), they were securely lodged in the pul- monary cavity. Miiller also noticed in certain Gasteropods a worm; and Dr. Gould, examining a specimen of the Physa heterostropha, “found the neck of the animal beset with numerous little things, looking like short, minute, white lines, attached like leeches, and which derive their nourishment from the fluids of the animal without his having the power to dislodge them.” , M. Baer states that he discovered a Filaria in the abdomen of Limneus stagnalis; and in many of the same family of Mollusca he has met with a worm allied to the Naides, “‘ living in the respiratory cavity, or hanging like little tufts of threads from the sides of the abdomen; whence he named it Chelogaster.” Besides these, he says, “ a kind of Cercaria * Professor Rymer Jones, op. cit. 102 Hoae, on the Water-Snail. finds an appropriate nidus for their evolutions in the body of the lacustrine snails ; and the curious transmutations of form they undergo in the interior of the animals, and the circum- fluent water, afford one of the most striking illustrations of Steenstrup’s theory of alternating generations.” * Upon observing the Limneus in my glass rather closely, I noticed that its body was covered with the “ little white line- lookiny leeches,” described by Dr. Gould and M. Baer; upon carefully detaching one or two, and viewing them with a half- inch object-glass, it had the formidable appearance represented in the drawing at fig. 8. It has an anterior mouth, surrounded with minute teeth or spines, over which it possesses great power. Suddenly it may be seen to dart out its body, at the same time projecting its mouth to some distance apparently for the purpose of seizing its prey, when it as quickly retracts itself within the shell of the animal, where it securely attaches itself to its body by a posterior sucker. It is possessed of a great number of hooklets or feet, by these it creeps from one part of the body to another, but is always found adhering to those parts affording security in times of danger. Eventually they become so numerous that the animal’s life falls a sacrifice to its troublesome tormentors, having apparently no power to rid itself of them. In conclusion, I would offer a word or two on the cell ; the primordial wall of which does not enter into the formative process of the embryo. The cell contents only are required for the purpose of affording nourishment to the vital blastema of the nucleus, in which a cycle of progressive development once set up, goes on until the animal is sufficiently matured to break through the cell-wall,and escape from the ova-sac. At the same time it may be inferred, that this is in some way assisted by the process of endosmose, and in this way certain gases or fluids become drawn into the cell-interior, and thus mate- rially aid in the supply of nourishment for the growth of the animal. The cell-wall bears the same relation to the future perfect animal that the egg-shell of the chick does to it; it is but an external covering to a certain amount of gaseous and fluid matter, and for the purpose of placing the germ of life in a more favourable state for development, assisted as it is by an increase of temperature usually the result of a chemical action set up, or once begun, in an organism and a medium. The ovum, destined to become a new creature, originates from a cell enclosing a gemmule, from which its tissues are formed, and nutriment is assimilated, and which eventually enables * Avassiz and Gould’s ‘ Principles of Zoology.’ Hoae, on the Water-Snail. 108 the animal successively to renew its organs through a series of metamorphoses, which give it permanent conditions not only different but even directly contrary to those which it had primitively. — In this one fact are we not furnished with a well marked or broad line of demarcation between that of animal and vege- table life? In the development of the animal, the cell-wall takes no part in the formative process ; it is but an enveloping membrane required for a time, and then thrown off. On the contrary, in vegetable life it enters largely into the formative process, and ultimate development of all its tissues; it.is ever to be found growing with its growth, cell-wall upon cell-wall intact, with or without its earliest contents. Note.—June 6th, 1854. My attempt to arrest the development of some young animals is still continued with perfect success. They have remained in the same narrow glass-cell, at the stage of growth before referred to, viz., about the size the animal usually attains during the first two or three weeks of its existence. They are now siz months old, alive and well, the cilia are re- _ tained around the tentacles in constant activity ; whilst other animals of the same brood and age, placed in a situation favourable to growth, have attained their full size, and have now produced young, which are of the size of their elder relations, _ DESCRIPTION OF PLATE VII. Fig. 1.—A magnified representation of the increase and change of situation occurring to the yolk of egg of Limneus on the fourth day. 2.—The change observed on the sixth day, showing the transverse fissure or divisional line in the mass. 3.—The formation of the shell proceeding more rapidly, it appears on the sixteenth day as the larger portion of the embryonic mass. 4,—The embryo performing its heliacal windings around the shell. ore Tye or young animal, seen soon after it has issued from the shell. 6.—The tentacles, with cilia, seen under a 3-inch object-glass ; the arrows indicating the course of the current produced by the cilia. 7.--The natural size and form of the shell of a full-grown Limneus. 8.—Parasitic animal found on the body of Limmneus, magnified 100 diameters. 104 Greeoory, on Fossil Diatomacce. Observations on some Deposits of Fossil Diatomaces. By Witiram Grecory, M.D., F.R.S.E. (Read April 19th, 1854.) In the series of microscopic objects issued by the Zurich Microscopical Association, there occurs a specimen of Berg- mehl, stated to be from Lillhaggsjon in Lapland, which is very remarkable in several particulars. First, there is a very great abundance of Hunotia Triodon, exhibiting the most astonishing variations of outline, so that the extreme varieties in opposite directions, those, for ex- ample, which are short, compressed, and have strongly-marked prominences, and such as are long, flattened, the apices being lengthened out, while the prominences actually disappear, or can only be traced by a hardly-perceptible waviness in the dorsal outline, would hardly be supposed to belong to the same species, and yet a perfect and gentle gradation may be traced from the one extreme to the other. This remarkable tendency to vary in form is peculiar, among the Eunotie I have seen, to this species, EL. Trzodon and to E. begebba, Kiit- zing. Itis totally absent in the common fossil forms of £. Tetraodon and E. Diadema, which hardly vary at all, save in size. It appears to me that this fact, especially when we consider that all these species often occur together, as, for example, in the Mull deposit, where £. Triodon, though not frequent, is just as variable as in the Bergmehl under consideration, demonstrates that these species are really distinct, and not, as some have conjectured, varieties of one, which may present one, two, three, four, five, six, seven, or more prominences. If all belonged’to one species, all should be alike variable or alike constant, whereas some vary ad infinitum, others not at all, in form at least. Nor can it be said that such a form as E.. Triodon is developed, as a variety, only under certain cir- cumstances; for in the Mull deposit it occurs with all its peculiarities, and therefore the supposed circumstances must have occurred; and yet, in that deposit, HE. Tetraodon and E. Diadema are much more abundant, and show no tendency to vary inform. But these two last-named species are absent from this Lapland deposit, where EL. Triodon abounds, It seems to me that these facts settle the question as to the species named, which must be held to be true and well- marked species; one of the characters of EL. Triodon and of E. begebba being a tendency to vary in form, while fixity of form characterises H. Tetraodon and EL. Diadema. This Laponian deposit also contains E. serra, and I think Greeory, on Fossil Diatomacee. 105 I have seen LE. heptodon. E. serra seems to be confined to Scandinavian deposits. Although differing from the Mull deposit in regard to the forms I have named, and also some others, this Bergmehl agrees with it in many points, as in the abundance of Navicula rhomboides and JN. serians, that of many Pinnularie, of Gompho- nema coronatum, of several Cymbelle, Stauroneides, Tabellaria, Orthosire, and other forms, but especially in the presence of Funotia incisa, first observed by me in the Mull earth. The ’ variety 6 is here the more frequent. There is another form, common to these two deposits, which, so far as I know, has not been described. It is an aspect like a Synedra, long and narrow, straight in the middle, and having the ends curved opposite ways, which gives to it a sigmoid character. I am inclined, however, to suppose it to be a Mitzschia, for while 1 cannot make out the transverse strie of Synedra, I can see a row of puncta on each margin in some specimens. It is, however, quite distinct from NV. sigmoidea. In the Mull earth it is generally broken, so that we see only one-half; but I have found several entire ex- amples. In the Lapland deposit it is more frequent, and often entire, although from its slender proportions it is apt to be broken, and fragments also occur. As we have already Nitzschia sigmoidea and N. sigma, this form, if it be a Nitzschia, may be called N. sigmatella. I have still to notice a form occurring in this Lapland Berg- mehl, which, so far as I have been able to ascertain, is un- described. It is narrow and of considerable length, but bent into the form of a sickle, or nearly a semicircle. It is slightly attenuated at the rather acute apices, and has very strong and distinct, though rather fine, transverse strie. It approaches more nearly to Hunotia arcus, as figured by Smith, but differs entirely from it, in being much more curved, in the absence of the characteristic prominence in the so-called ventral surface, and in its having much stronger and more distinct strie, all of which characters combined give it an entirely peculiar aspect. Taking it, for the present, to be a Hunotia, I propose for it the name of Hunotia falz, or E. falcata. I would now direct attention to a deposit, of which speci- mens were sent to me by Mr. Norman, under the name of Liineburg. It is well known that there is an extensive de- posit on the Liineburg heath, in Hanover, and one part of it is known as the earth or Bergmehl of Oberrohe, near Liine- burg, another as that of the Limeburg heath. These I find to be quite distinct from the deposit of which I now speak, as obtained from Mr. Norman; for this, as I have found, has a 106 Greeory, on Fossil Diatomacee. composition absolutely identical with that of the Lillhaggsjon Lapland deposit I have described. Not only the species are the same, but they are in the same proportions. In both Eunotia triodon presents in abundance its strange variations ; in both the long sigmoid form, and also the sickle-like form, occur. In short, I can detect no difference between these two de- posits; besides the forms I have named, both contain Hunotia incisa, chiefly var. 8; and both alike contain such forms as Eunotia serra, Tetracyclus lucustris, and others, imasmuch that I think it more probable that one of them has been misnamed, than that two deposits, in places so distant as Limeburg in Hanover, and Lillhaggsjon in Lapland, should be identical in composition. Since all the specimens of earth from Oberrohe near Liineburg, and the Liineburg heath, that I have examined (and I have seen several different specimens in the natural state), differ from the Lapland earth, and since the Lapland earth is referred to its locality by the Zurich Association, | conclude that the earth in Mr. Norman’s hand is really not from Liineburg, but from Lapland. Perhaps there may be a place called Lineburg in Lapland, near Lillhaggsj6n ; but this I have not been able to ascertain. In the mean time, this so-called Liineburg deposit will supply observers with the two forms I have now described. I have noticed it in some other forms which I believe to be undescribed ; to these I shall return on some future occasion. TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE I. VOL. II. 1. Bacteriastrium furcatum. 2. — curvatum. 3. Euphyllodium spathulatum. 4. Triceratium sculptum. 5 6 — arcuatum. — arbiculatum. 7a. Triceratium contortum. *7b, —————— do. showing spine. 8. Pleurosigma vallidum. 9. ——-——-— inflatum. 10. Amphitetras arisata. 11. tessellata. 12. Hupodiscus crucifer. 13. Campylodiscus latus. 14, Asterolampra impar. 15a & 15b. Climacosphenia catena. 16. Denticella simplex. Ee. margaretifera. —_———— % Iran Mcr Joa Ulli [ Ee Corr cenet (Cer ee Cine D ueee woe 0 n0olvee A eLbeocueveney cecal UL ELEOC CLE ae COCDOG KCCULEL TL, We EOO BEL ECLELCTY Sion ~ 9, gos OR Ve i) ui P, OOON PECL aot rome evar 520005, Toh 5) aagis3 Tuffen West, ad nat seulp Ford & West Imp 54:Hatton Garden, TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE II. Figs. 1, 2, 3, 4, 5.—Avicularium of Notamia bursaria. L—Avicoleriam in the closed state. 2.—Avicularium open, exhibiting the tactile (?) brush. 3.—Avicularium viewed in front, to show an opening below the beak. 4.—Avicularium in the early stage of developement. 5.—Closed avicularium, more magnified, showing the muscular structure and the internal organ. Figs. 6, 7, 8.—Avicularium of Bugula plumosa. 6.—In the closed state. 7.—Open, showing the tactile (?) brush. 8.— Open, to show the diaphragm, Figs. 9, 10, 11.—Avicularium of Bugula avicularia. 9.—Open, to show the tactile (?) brush (more magnified). 10.—Two avicularia grasping each other, 11.—One partially open (less magnified). 12.—Avicularium of Scrupocellaria scruposa. 13.—A small vermicule captured by two avicularia in Scrupocellaria scruposa. 14.—Avicularium of Bugula plumosa, in the early stage of developement. DESCRIPTION OF PLATES IIL, IV., & V. Tllustrating Professor Quekett’s Papers on me Torbane-hill Mineral. PLATE III. Fig. food section of the yellow variety of the Torbane-hill Mineral, as seen under a magnifying power of 130 diameters. 2.—A section of the dark variety of the Torbane-hill Mineral, as seen under a power of 130 diameters. The yellow circular masses exhibit ~a radiated structure; they form the combustible portion of the mineral, whilst the dark matter is the earthy ingredient. 3.—A section of the Torbane-hill Mineral, in which a specimen of Stig- maria ficoides is imbedded : every part of this plant can be readily distinguished from the mineral by its rich brown colour. Mag- nified 6 diameters. 4,.—A portion of the same specimen magnified 50 diameters, showing how easily the smallest portion of vegetable tissue can be distinguished from the substance of the mineral. 5.—A section of the Torbane-hill Mineral, through which .a thin layer of coal ran, which may be readily recognised by its brown colour. The yellow particles of the mineral in contact with the coal are of more or less oval figure. 6.—The powder of Torbane-hill Mineral, showing the yellow bituminous particles, and fragments of vessels. 7.—Ash of the Torbane-hill Mineral. PLATE IV. 1.—Transverse section of the Brown Methil Coal. 2.—Longitudinal section of the same. 3.—Transverse section of the Black Methil Coal. 4.—Longitudinal section of the same. 5.—Transverse section of the Lesmahagow Cannel Coal. 6.—Longitudinal section of the same. PLATE V. 1.—A section showing the Mineral and Coal in juxtaposition ; magni- fied 3 diameters. 2.—Representations of the comparative sizes of the transverse sections of the brown elongated cells from various Coals, drawn by means of the camera lucida, by Dr. Adams, 70 diameters. 3.—Chippings of Newcastle Coal, showing dotted woody tissue. 4.—Ash of common domestic Coal, exhibiting the remains of a transverse section of wood. 5.—A. longitudinal section of Coal from Lochgelly, showing its identity with a similar section of wood, from a drawing in the possession of Dr. Adams. 6.—Ash of Coal, exhibiting portions of siliceous cuticle and other frag- ments of vegetable tissue foreign to the coal. 7.—Powder of Breadisholme Coal, from a drawing by Dr. Adams. Ley y Wadine See Ford. West 54.Hatton Garden QL ffl i Vd TELS LV. ) 7 Vib Ford & West Chromo Tap 7 WU ‘PA (40, Trant M S 8 8 s w& 3 Tuffen West Chromo, Lith. ad nat Srons Moir Leo aM LY A xX 770 Ford & West Imp. London Taffen West lth. . DESCRIPTION OF PLATE VI. 1.—Cocconeis placentula. 2.—Actinocyclus sedenarius ? 3.—Triceratium striolatum. 4.—Campylodiscus bi-costatus. 5.—Zygoceros Rhombus. 6 a.—Odontidium Harrisonii ? 6 b.— ee front view. 7.—Rhaphoneis gemmifera. 8.— oe fasciolata. 9.— Gs pretiosa. 10.— “ rhombus. 11.—Zygoceros Surirella; front view. 12,— 5 side view. 99 13.—Front view of Actinocyclus sedenarius, showing the undulations. 14.—Side view of the same, showing the cellular markings. rans Mowe Ste Vl LAM. ase fe al SO Mewar Aw, So TO GUGS® OOS”: over ERECT CON Og. cee eee inn aD, 0, [Fev reotie v0 Ch oRee pQpor Ce oen co o £ ooo! foe ouren oy oF Poon sen re 9 oc fo ng PP O69 Hi 00G ON Cpe CEP LOL nn gts phOOe Reoconcang Deer ott SOnHOH EOE ¢, S Pecorcvert | 1 CoveH C00 RO eewpe beef HECee CUCL eet pocceoucoctco soeHEC CEE oo L000 ELOUELCE Faeneo cele ens Rail ia ye aS 1000 I ths of an, Inch mange 400 cams Ford & West, imp, Hatton Garden £ *. . TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE VII. To illustrate Mr. Hogeg’s Paper on the Development and Growth of the Water-snail. Fig. | 1.—A magnified representation of the increase and change of situation occurring to the yolk of egg of Limneus on the fourth day. 2.—The change observed on the sixth day, showing the transverse fissure or divisional line in the mass. 3.—The formation of the shell proceeding more rapidly, it appears on the sixteenth day as the larger portion of the embryonic mass, 4.—The embryo performing its heliacal windings around the shell. 5.—The embryo, or young animal, seen soon after it has issued from the shell. 6.—The tentacles, with cilia, seen under a 4-inch object-glass; the arrows indicating the course of the current produced by the cilia. 7.—The natural size and form of the shell of a full-grown Limneus. 8.—Parasitic animal found on the body of JLimneus, magnified 100 diameters. BFE BDA ort ibe ane as % apg ty be 960s STERN Bil : = ~ se ~ : > . ¢ SJ 4 INDEX TO TRANSACTIONS. VOLUME TI. A. Actinophrys Sol, remarks on, by kh. 8. Boswell, 25. B. Binocular vision, on the application of to the microscope, by F. H. Wen- ham, 1. Boswell, R. "S., remarks on Actino- phrys Sol, 25. Busk, G., FRS., on the structure and function of the avicularian and vibracular organs of the Poly- zoa, 26. Diatomacez, new forms of, from Port Natal, description of, by G. Shad- bolt, 13. ie of the» Thames, some observations on, by F. C. S. Roper, F.G.S., 67. H. Hogg, Jabez, observations on the development and growth of the Water Snail (Limneus stagnalis), al: Lip Illumination of transparent objects, on a method of employing artificial light for, by G. Rainey, M.R.C S., 23. ie; Legg, M. S., A.I.A., observations on the examination of Sponge-sand, 19: Limneus stagnalis observations on the development and growth of the, by Jabez Hogg, M.R.C.S., 91. M. Microscopical Society, Report of the Fourteenth Annual Meeting of the, 81. Bs Polyzoa, remarks on avicularian and vibracular organs of, by G. Busk, F.R.S., 26. Q. Quekett, John, on the minute struc- ture of the Torbane Hill mineral, 34, R. Rainey, G., M.R.C.S., on a method of employing artificial light for the illumination of transparent objects, 23. Report of the Fourteenth Annual Meeting of the Sue So- ciety, 81. Roper, F. C. S., some observations on the Diatomacee of the Thames, 67, Ss. Shadbolt, G., description of some new forms of Diatomacee from Port Natal, 13. Sponge-sand, observations on the ex- amination of, &c., by M.S. Legg, A.I.A., 19. Tt: Torbane Hill mineral, or Boghead coal, on the minute structure of, by John Quekett, 34. Ww. Water Snail (Limneus Stagnalis), J Hogg, on the development and growth of the, 91. Wenham, F. H., on the application of binocular vision to the microscope, 1. th ae | ae ee ae. osiy oa , TRANSACTIONS OF THE MICROSCOPICAL SOCIETY LONDON. DA NEW SERIES. a, VOLUME IIL. LONDON: SAMUEL HIGHLEY, 32, FLEET STREET. 1855. LONDON: PRINTED BY W. CLOWES AND SONS, STAMFORD STREET, TRANSACTIONS OF THE MICROSCOPICAL SOCIETY OF 1; ON DON. —-——— Some Remarks on obtaining Puorocrarus of Microscopic: OsseEcts, and on the CoinciDENCE of the CHEMICAL and VisuaL Foct of the OBsect Giasses. By F. H. Wennam. (Read November 22nd, 1854.) In this communication it is not my intention to give a detailed description of the well-known methods of obtaining micro- photographs, which have already been explained in the papers of Messrs. Delves, Shadbolt, and others, but merely to point outa remedy for some of the difficulties that have hitherto been connected with the process. The main points in this paper were read at the last meeting of the British Association for the Advancement of Science, at Liverpool, but I have thought it proper to bring them forward again, as I believe that the principal number of those who have entered into the practice of this department of photo- graphy are members of the Microscopical Society. As it is now upwards of two years since the announcement was first made, and from the few specimens that have been produced since that period (many of which are in the hands of our Society), it may fairly be assumed that the practice of microscopic photography has not become by any means uni- versal, and, in fact, there are some amongst us who doubt whether the art can ever be usefully applied, or prove a sub- stitute for the camera lucida. I should regret to see this application of the microscope abandoned, while it is still under the march of improvement, and while science can furnish us with new facts to facilitate the process. The con- clusion that I have arrived at, derived from my own practice, is, that it is in general both easy with respect to manipulation, rapid in production, and faithful in delineation, and I have a favourable opinion of its utility. There are some exceptional cases, which I shall notice. How far the specimens that I herewith present to the Society will bear me out in this assur- VOL. III. b 2 Wenuam, on Microscopic Photography. ance, others will probably be better able to judge than myself. I have not worked at it with sufficient diligence to make a choice selection, but have taken them as they came. I should judge that the whole of them, to the number of twenty-two, had occupied about six hours of sunlight, of course including some failures. If the photographs are intended for illustration, it is re- quisite that they should each be included in a given space. The position of the sensitive surface must in consequence be made to vary, more or less, for every different object, accord- ing to its size. A range of from five to ten feet is oftentimes required. A box of this length is both inconvenient and cumbrous, and it is a matter of some difficulty to get access to the furthest end for the purpose of focussing the object accu- rately. For these and other reasons, I have altogether aban- doned the use of the microscope camera, and given the preference to the method herein described. In the first place, it may be proper to offer a few remarks on the subject of the illuminating source, as I have tried many experiments with the view of obtaining an artificial light suit- able for photographic purposes. A light may appear strongly luminous, and yet possess but a feeble degree of photographic intensity ; and [ have not yet succeeded in producing a satisfac- tory result from either gas, oil, or camphine lamps. Burning phosphorus will give a more rapid impression, but its use is both inconvenient and expensive. Fine zinc turnings, burnt in atmospheric air, equal or surpass this; a ball of about three- quarters of an inch in diameter will last a sufficient time to give a distinct impression. As it is of no consequence whether the light is intermittent or not, I have produced an image from a succession of electric sparks, arising from the spon- taneous discharge of a small Leyden jar, containing about thirty inches of coated surface, the discharging knobs being placed in the axis of the lenses for condensing the light upon the object. The electric spark contains a large proportion of the actinic rays ; I found that about one hundred discharges pro- duced a good impression. The electric light between charcoal points I have not yet tried. Ina few instances I have used the hydro-oxygen, or lime light, but I consider that it does not possess that degree of actinic intensity which its brilliancy and appearance would seem to indicate. It has been proved that the two latter may be successfully applied for obtaining photographic impressions, but they are both troublesome and too much out of the way of the micro- scopist to be generally useful. I have merely mentioned these experiments with the view Wenuam, on Microscopie Photography. : 3 of recording them for the guidance of other experimentalists, for I have a strong belief that such an investigation may end in a useful result. There can be no doubt that it is a desi- deratum to discover a composition for a photographic fusée, so to term it, that will burn for a sufficient period of time, and with the requisite actinic intensity for obtaining, not only microscopic impressions, but also nocturnal, or underground photographs. I trust, therefore, that this subject may be taken in hand by some one more practically conversant with the details of pyrotechnic chemistry than myself. - There is no light that has hitherto been found that will give results at all equal to those to be obtained by the use of sun- light. The method that I have adopted for applying it, is simply to use the ordinary table microscope as a solar one. A room is selected, to the window of which sunlight must have free access ; this is closed by a shutter, having an aperture at the lower end of about three inches in diameter; below this is placed a level table or bench at a convenient height, so that when the microscope body is in a horizontal position, its axis may coincide with the centre of the aperture in the shutter. Outside the latter is fixed a solar reflector, which may be adjusted from the inside, or more simply through a sleeve fastened around a hole in the shutter; in this case the mirror may be mounted entirely in a wooden frame. With this arrangement the course of proceeding is as fol- lows: having clamped and adjusted the object on the stage of the microscope, place it horizontally against the aperture in the shutter, remove the eye-piece, and throw sunlight through the object by means of the solar reflector ; lay a black cloth around the microscope so as to stop out all extraneous light ; then, by properly focussing, a distinct image may be obtained upon a paper screen held at various distances. The stand for supporting the collodion plate consists of a vertical piece of board with a heavy base; the excited plate is held on to this by means of two undercut fillets at right- angles to each other. The stand may be set at various dis- tances along the horizontal bench, which also serves as a support for the microscope. The operation of taking the photograph is, first to adjust the mirror for light, and then to focus the image on a card placed in the plane of the collodion surface ; next remove the card and lay it against the body of the microscope, so as to stop off all light ; then drop the sensitive plate into its place, snatch the card away, and quickly replace it again, so as to let the image of the object fall upon the plate: a fraction of a second is oftentimes sufficient. I prefer a rather slow collodion, and if b 2 4 Wenuam, on Microscopic Photography. the weather is warm develop with a half-grain solution of pyrogallic acid. For the lowest powers, it is oftentimes not necessary to use any arrangement for condensing the sunlight upon the object, the simple reflection from the plane mirror being sufficient ; but the half-inch object-glass, and upwards, requires a bull’s- eye lens of about three inches in diameter. If the objects are small and delicate, such as the Diatomacee, the achromatic condenser must be used in combination. _I should mention that a piece of yellow glass must be let into the upper portion of the shutter, transmitting enough light to manipu- late by. Having briefly described the method of operating, I will state what I consider to be its peculiar advantages. ‘The object is focussed with great facility and certainty. We are, in some cases, enabled to obtain an impression of an object mounted so as to be out of a flat plane ; in some instances, by the convenience afforded for inclining the sensitive plate at every angle relative to the optic axis, and in others by focus- sing two or more separate times. For example, suppose the object to be a Fly’s foot, one of the pads of which lies in a lower plane, and is consequently out of focus; while the im- pression of the first half is being taken, the next which is out of focus can be stopped off with a card; the second focus is then taken, and the first impressed portion of the object ob- scured: thus by a diversified series of paper stops, we may approximately represent the entire form of an object, the whole of which cannot be seen, except by a series of three or four focal adjustments. A very great number of microscopic preparations are so organized as to be composed of parts which require different periods of exposure to produce a perfect impression ; some parts will be barely defined, while others are utterly solarised and lost from over exposure. The method that I have ex- plained affords especial facilities for stopping off the most tender portions. As it is requisite for the purpose of ensuring quick and accurate focussing, together with the most distinct impressions, that the actinic and visual foci of the objective should be coin- cident, I give the result of my investigations on this point. For the highest powers the difference is sometimes so small as to render the correction a matter of trifling importance; but with the 4 inch, 1 inch and 1% inch, the distance is very considerable; in fact, the more perfect the object-glass for microscopic purposes, the less is it suited for a photographic lens. The object-glasses are invariably what is technically ae Wenuam, on Microscopic Photography. D termed ‘‘ over corrected ;” for the point of convergence of the chemical rays near the most refrangible or blue end of the spectrum, lies beyond the visual focus. I have an objective corrected specially for these rays, and though perfect for pho- tographic purposes, yet on account of its being non-achromatic, it is unsuited for microscopic investigation. The simplest and cheapest way of producing the required degree of “ under correction,” is to screw a biconvex lens into the place of the back stop of the object-glass, acting as part of its optical combination For Smith and Beck’s 14 inch, I have used a lens of 8 inches focus, and for the 2-3rd, one of 5 inches, which also serves for the 4-10th inch ; these bring back the actinic to the exact position of the visual focus. The combination used as an objective shows some colour, but the additional lens does not affect the spherical correction to any material extent, and the increase of distinctness in the photographs obtained by means of the application of this additional lens is most striking. It must not be supposed that the focal lengths that I have here given of the correcting lenses will in all instances serve for the objectives above named, for the correction will probably require a lens of a different focus for every different object- glass; it is, perhaps, best to be provided with several of them, as their cost is but trifling. Those that I have made use of have been selected from ordinary spectacle lenses, most care- fully centered and turned down to the required size. Some remarks have been published on the possibility of obtaining stereoscopic pictures of microscopic objects by means of the “binocular microscope,’ but the ordinary in- strument will answer every purpose without any optical addition whatever, for it has been shown* that if the object itself be viewed alternately with the right and left half of the object-glass without any altering of its position, the difference in form of the resulting images assimilates to the effect of a different angle of vision; and if two photographs of the object obtained by the separate halves of the object-glass be placed in the stereoscope, they will give an appearance of solidity to the object. The only addition that is required to produce this effect is to fix a sliding stop close behind the objective, having straight edges that will cut off either the right or left hand sides ; a photographic impression being taken at the two extremes. If the object-glass be one of considerable aperture, about one-third only of the diameter may be cut off, which will be sufficient to give the difference of form required for the stereoscopic image. * ¢ Quarterly Journal of Microscopical Science,’ for July, 1853. 6 Wenuam, on Microscopic Photography. It is most remarkable how an impression of the finest details of an object, or the markings on even the most difficult tests, may be obtained by means of the photographic microscope, and so definitely that I have used it for proving their struc- ture.* The application of photography to the delineation of microscopic objects is somewhat limited, not by any diffi- culties or defects in the process, but by occasional peculiarities . of colour, or transparency in the objects themselves. Many insect, animal, and vegetable structures, though sufficiently transparent to the eye, are absolutely opaque to the actinic rays. I possess a specimen of a parasitic insect of a dark red tinge, and in which a splendid internal tracheal system can be discerned. I have tried every means of obtaining a pho- tographic representation of this, but without success. With all periods of exposure the object appears as a mere blank space, or like a hole cut in a sheet of paper. Until further discoveries have removed these difficulties, the application of microphotography must be to some extent restricted, as many objects are for this reason excluded. All structures dependent upon outline or opacity, such as sections of bone and wood, vegetable fibres, &c., may be delineated with ease and certainty. In conclusion, I will enumerate the peculiar advantages of my method: first, the use of the ordinary microscope as a solar one, a dark room serving as a substitute for a camera ; the additional apparatus required will cost but a few shillings. Second, the method of obtaining the combination of the che- mical and visual foci, which I have found to be of great practical utility ; third, the mode of obscuring for a time the parts of the object either easily solarised and lost, or out of focus. I have not advanced these as mere speculations, but have submitted them successfully to the test of repeated trial. I may also remark that when sunlight is to be obtained, I have found the practice of microscopic photography to be one of particular certainty, for unlike other branches, the con- ditions of light are so favourable and definite, that an impres- sion may always be obtained ; and though the present state of the science in this department is admitted to be imperfect, yet there can be no question that it is still progressive, * Within the last few days I have succeeded in obtaining a photo- graphic impression of the P. angulatum, magnified about fifteen thousand diameters, showing the configuration of the markings perfectly black and distinct in a far greater degree than we can ever hope to see them through the compound microscope ; and it is my opinion, that if ever the structure of these difficult tests is to be proved it will be by the aid of photography. Rose, on Parasitic Borings in Fossil Fish-scales. 7 and in my proposals for removing some of the defects of pre- vious methods, I venture to hope that the results may here- after show that I have contributed my mite towards the advancement of the art. On the Discovery of Parasitic Borines zn Fossiz Fisu- scaLes. By C.B. Ross, F.GS., &c. (Read June 28th, 1854.) THE subject of the communication which I bring before the Microscopical Society, through the favour of my friend Pro- fessor Quekett, is the discovery of parasitical borings within the delicate structure of fossil fish-scales. The history of my detection of these workings is as follows: —In the winter of 1851, when examining fossil fish-scales from the chalk strata of this neighbourhood, it struck me— as many of them were thin and translucent, particularly those of cycloid fishes—that they might make interesting micro- scopic objects; and I sent up to Norman, in the City Road— a well-known preparer of specimens for the microscope—a small piece of chalk with scales adhering to it, requesting him to put a few upon glasses for me. In consequence of their thinness and brittle texture, he succeeded in affixing a por- tion of two scales only. Upon examining them, I observed that one of them exhibited elegant arborizations, extending over a large portion of the scale; in the other scale no such branching figures were visible; nothing, indeed, was seen but a yellowish, translucent substance, traversed by equidis- tant lines, evidently the lines of growth; similar lines were also seen traversing the portion of scale containing the beau. tiful arborizations. (See Plate L., fig. 1.) I at first thought the ramifications were on the surface of the scale, and imagined they might be minute coralloid bodies ; but upon applying to them a power of 1-8th, I became satis- fied that they were tubes of some kind within the texture of the scale; and by varying the focus, and passing in review different parts of the scale, I ascertained that they were situ- ated between its lamine. Still, I could not conceive their origin; for I was convinced they had nothing to do with the natural structure of the scale, from there being nothing of the kind to be seen in the other scale, and both of them cycloid scales (Osmeroides ?). Not very long after meeting with this interesting specimen, I was so fortunate as to receive from Mr. Wetherell, of High- gate, a paper, published in the ‘ Annals of Natural History,’ by Mr. Morris, of Kensington, entitled ‘ Paleontological 8 Ross, on Parasitic Borings in Fossil Fish-scales. Notes,” in which he described, under the name of Talpina, branching bodies, or rather the casts of branching tubes, met with in the Belemnite from the upper chalk, adding also ex- cellent lithographed figures of them. On the perusal of this paper, and inspection of the illustrations, I was instantly satisfied that the ramifying tubes I had found in the fish- scales were of the same nature as those met with in Belem- nites,* although the former are so much more delicate than the latter. The illustrations accompanying this communication will afford you a better idea of the course and configuration of these borings than any description which I can give; still, I may say, that they proceed between the delicate lamine of the scale in a graceful curve to their extremities, branching off on either side, and terminating in a symmetrically-formed dilatation or cell, and they do not frequently inoscolate. The beginnings of the tubes are occasionally confluent, as seen in fig. 1a, at c; im other instances they commence solitarily, and the parasite, having formed a few lateral branches, has appa- rently terminated its labours abruptly. It seems, also, that it has sometimes passed from one lamina into another; thus taking a transverse direction, or one perpendicular to the lamine, which is made manifest by the microscope, now and then detecting a transverse section of a bore. Fig. la@ ex- hibits a detached fragment of the original specimen; viz., the one in which the borings were first discovered ; upon it the lines of growth are well marked. The discovery of the above interesting fact led me to the examination of fossil scales from other fishes, and the next I selected were the scales of Prionolepis angustus, a ganoid fish, from the lower chalk. I was not long in meeting with the depredations of its parasite; but, you will observe, on ex- amining fig. 3, that its operations are of a very different character to those in the osmeroid scale exhibited in fig. 1; for, in this instance, the tubes proceed in a slightly wavy form, with the lateral branches passing off at a consider- able angle, and occasionally at right angles; they extend also toa greater length than those in the first specimen ; still, there cannot be a doubt of their having a similar origin. Proceeding with my researches, I took another scale from the lower chalk, of a thicker substance, therefore, possibly from a placoid fish, but being a very imperfect specimen I cannot say which it is, ganovd or placoid ; it is, at least, from a different genus to Prionolepis. Here, again, I met with * It is singular that no traces of them have been observed in the Belemnites of the Jurassic series.—Von Hagenow. Rose, on Parasitic Borings in Fossil Fish-scales. 9 borings, and so greatly resembling those in the last-examined scale (fig. 3), I must, therefore, consider its parasite but a variety of the one which infested that scale. This specimen is represented by fig. 4; the decussating lines shown are probably markings peculiar to that kind of scale. Pursuing this interesting inquiry, I next took a scale found in the shale of the Kimmeridge clay, and in it I met with another form of the parasitic workings; for, in the first place, they are of a larger calibre, and their form is more decidedly dichotomous. See fig. 5. The figures given from this scale clearly show that the parasite inhabited layers deeper than the external one ; indeed, this circumstance was manifest in some of my first specimens, With the view of determining whether similar depredations are committed upon the scales of living fishes, I have carefully examined numerous scales of several different marine and fresh-water fishes ; and I have not met with a vestige of borings of any kind in a single instance. To what form of organism, vegetable or animal, are we to attribute these remarkable operations? We are, I am aware, fully cognizant of the invasion of recent corals, shells, and bones, by boring sponges (Clionz) and Conferve.* But those intruders, although comparatively small, have their workings in most cases visible to the unassisted eye; whereas, in the instances which I have brought before you, most of them require a magnifying power of 1-4th to enable us to trace their course with any degree of distinctness. In my first specimen (fig. 1, Plate I.), the borings of which I took great pains to measure, I estimated their calibre at about one 2-1000th to 4-1000th of an inch. I learn from Mr. Morris’s paper, before referred to, that M. von Hagenow has, under the name of Talpina, “arranged certain problematical branching bodies, which traverse the spathose guard of the Belemnite, and whose position in the animal kingdom has not been defined, whether as belonging to the Annelides or to the boring-sponges.”’ From the mi- nuteness of the agent effecting the borings within the fish- scales, | am more disposed to attribute them to the operations of infusorial parasites, rather than to the growth of sponges or conferve ; particularly when I consider that the ocean de- positing the calcareous mud must have been the habitat of myriads of Infusoria of infinitesimal calibre. +} * See Professor Quekett’s Lectures on the Histology of Animals, vol. ii. pp. 42, 153, &c. + Since reading the above paper, I have found abundance of borings in a scale from the mud of the river Oran, in Algeria.—C, B. R. 10 Gregory, on a remarkable Group On a Remarkaste Groupe of Diatomaceous Forms, with Remarks on SHAPE or OUTLINE as a@ SPECIFIC CHARACTER an the Diatomacez. By Witittam Grecory, M.D., F.R.S.E., Professor of Chemistry. (Read October 28th, 1854.) AxourT a year ago I first noticed, in a gathering from Dud- dingston Loch, a Navicula of nearly an oval form, with broad, obtuse apices, which differed from all the Naviculaz known to me. ‘The striation was peculiar and strongly marked, the strie being about 16 in ‘001”, highly inclined everywhere, except just about the middle, where the inclined striz seemed to decussate, leaving, of course, a triangular space on each side of the centre, while in these triangular spaces the striz were parallel and transverse. This arrangement, as we shall see, occurs in several species of Navicula and Pinnularia. The form here alluded to was referred to different species, and even to different genera, by different friends whom I con- sulted ; some regarding it as a form of MNavicula semen, while others supposed it to be related to Pinnularia gracilis, or to P. radiosa. But its aspect was totally distinct from that of the species named, which, moreover, all have from 24 to 26 striz in ‘O001”. Meantime other forms occurred, with the same number and arrangement of the striz, and with the same peculiar aspect, but of different outline. Some were nearly rhombic, short, and rather broad; some were longer, also nearly rhom- bic, but with a contraction and subsequent expansion at the apices, thus becoming more or less subcapitate. Others were nearly linear, with obtuse ends ; others linear and subcapitate. Some were found with nearly straight sides, and acuminate, ending in small apiculi; while others had curved sides, con- tracted to narrow and produced ends. In some cases these produced ends terminated in round knobs; in others in acute points. Some again had straight sides, with contracted ends terminating in round heads. In the whole of the forms now mentioned, I observed the same characters, the same number and arrangement of the strie, and the same aspect. On examination it appeared that the striz were really moniliform, though not obviously so to the éye, having rather a smooth soft aspect than any appear- ance of granulation. During the whole year new forms, agreeing with those already mentioned in every point but that of outline, were from time to time observed. In another Duddingston Loch gathering, I found in abundance a very fine one, accompanied by others, such as those represented in figs. 1, 18, 28, Pl. IT. of Diatomaceous Forms. | ll In a gathering from the vicinity of Oban I found several ; one very near the original oval form, but with flattened apices, and a slight tendency to constriction just within them. These last, which closely resemble Pinnularia oblonga, shortened, and rather broader in proportion, are frequent in a Norfolk gathering sent me by Mr. Bleakley, in which occur also several others. The Oban gathering contains also various other forms of this group, one of which has precisely the form and size of Pinnularia acuta, and as that species occurs along with it, the two forms are easily compared and distinguished. Here also occur forms approaching nearly to that of Pinnularia pere- grina, although in a purely fresh-water gathering. In another similar gathering from a bog in Ayrshire, there is abundance of a form not to be distinguished from P. pere- grina, along with others of the outline of P. acuta, P. radiosa, &e. I now began to suspect that these forms might all belong to one species, for on close inspection I found a very large num- ber of intermediate or transition forms. I, therefore, named the supposed type Navicula varians, and continued to search for its modifications. : In the Glenshira sand, although not very abundant, it ex- hibits all the forms as yet enumerated, but chiefly those which have an outline allied to that of Pinnularia gracilis, but twice or thrice as large, and to that of P. peregrina. These forms and several others I have since found abundantly in the recent mud or sand deposited by the Dhu Loch, near the mouth of the Glenshira, the lake which when at a higher level in the valley, deposited the Glenshira sand described in the last number of this Journal. Having received from the Rev. Professor Smith, in Sep- tember, a slide, of fresh-water origin, in which Navicula varians, of the type of Pinnularia peregrina, was very abun- dant, I begged Mr. Smith to examine the form, which he found, as in all the other types of NV. varians which he had seen, to have moniliform striz. He then extended the inquiry to the typical Pinnularia peregrina, and found that it also had, at all events in many instances, moniliform striz. From this, I concluded, that in all probability Pinnularia peregrina was at all times only a type of N. varians. I believe Mr. Smith intends to change the generic name of P. peregrina to Navicula. It seems to me in the highest degree probable, that Pinnu- laria oblonga is nothing else than another type of UW. varians. For the form (fig. 1) does not differ from P. oblonga, except in length, every other detail being identical in the two forms ; 12 Grecory, on a remarkable Group and although I cannot say that I have seen the moniliform character of the striz either in fig. 1, or in P. oblonga, I believe that this has been seen in the former. If so, any one who compares the two forms which occur together, both in the Oban gathering, and in Mr. Bleakley’s gathering from Norfolk, will see that the latter can hardly fail to exhibit the same character. I have not myself been able as yet to attempt the resolution of these strize. with any refinement of appliances, and therefore I must leave this point for future examination. I have still to notice one more type, which I first observed in a gathering from Lochleven, where it is very scarce, but which is frequent in a second and distinct gathering of Mr. Bleakley’s from Norfolk. It is rather small, and either of a short and very broad oval form, or absolutely discoid, but has all the characters of the group. It is seen in fig. 17. At first I supposed it to be distinct, but I have since been led to suspect that it is only a form of the group I have described. This, however, is by no means certain. On the one hand, it seems to be certainly a Navicula, although in this point of view its orbicular form is very remarkable. It also varies to ovals of different proportions, and it has exactly the striation of the first observed form of WV. varians (fig. 25), to which, indeed, in shape, the oval varieties approach very closely. On the other hand its variations are, so far as I have yet seen, confined within rather narrow limits ; and its form is so striking, that I had named it at one time Navicula orbicularis. Since the preceding sentences were written, I have been informed that this species was some time since named by Mr. Smith Navicula scutelloides. So far as I know, it has only occurred as yet in the two localities I have mentioned ; namely, Norfolk and Lochleven. We have now mentioned most of the observed types of WV. varians, so far, at least, as they present the characteristic stria- tion and aspect; and although all the forms I have named may not be found to belong to it, yet it appears that there exists a large group, characterised by a very peculiar aspect and striation, the number of striz varying only from about 14 in -001” in the larger to 18 in :O001” in the smaller forms, the usual number being 16. This group seems to include several which have been con- sidered. as distinct species, such as Pinnularia (Navicula) peregrina, and other forms, referred to Navicula semen, N. rhyncocephala, Pinnularia gracilis, P. radiosa, &c., although in these three species the normal striation is 26 in -001”. But there are even more of the forms of this group which are undéscribed, such as the round and oval forms ; that which “3 ii i of Diatomaceous Forms. 13 resembles a shortened P. oblonga; that which occurs in Dud- dingston Loch; the subcapitate forms; the capitate forms with straight sides; that having the form of P. acuta; and various others. If these two classes of forms, the known and the unde- scribed, really constitute one group, we find in that group nearly every shape which is seen in the genera Navicula and Pinnularia ; and also transition forms, connecting together the various types. The question naturally arises: Can all these varied forms belong to one species? Now, at one time, certainly, each marked type of form would have been regarded as a distinct species. But the more extended observations of recent times have proved that form, shape, or outline, is not nearly so permanent a character as had been imagined. In a paper on the Mull Deposit (¢ Journal,’ January 1854,) I pointed out, and illustrated by some figures, the remarkable tendency to variety of form in three species, namely, Eunotia bigibba, Kitz: Pinnularia divergens, W. Smith, and Himantidium bidens. I alluded also to the same tendency in Eunotia triodon; and I again returned to the same point in this last species, ina short paper in the ‘ Journal’ for July, 1854. Other examples are not wanting ; and the more the Diatomacez are studied, the more do we perceive that, in many species at least, the shape or outline is subject to endless variations. It certainly appears at present as if, inmany species, the form were constant : but we must be cautious in affirming this, for in two species which I adduced as examples of constancy in outline, namely, Navicula rhomboides, and NV. serians, we have now good reason to believe that important variations of shape occur. Just as NV. peregrina seems to belong to the group of NV. varians, so it appears that WV. Crassinervia will prove to belong to N. rhomboides ; and that a form, apparently yet more widely differing from the latter, namely, that which I have lately described* under the name of WN. interrupta, which is linear, narrow and obtuse, may be found to be another modification of IV. rhomboides. The Revd. Professor Smith has also very recently detected a modification of NV. serians, most remarkably different in shape from the usual type. It will. probably be found necessary, looking to the uniformity of markings and aspect in the forms here described, and to the existence of such numbers of transition forms con- necting the various types of outline, to form a species, Navicula varians, including these forms as sub-species ; or * In a paper read to the Microscopical Society, 25th of October last, which will appear in the next Number of the ‘ Journal.’ 14 Grecory, on a remarkable Group else to form a subgenus, characterised by its markings, that is, by its structure, including, as species, the chief types of outline to be found in the group. Some system of sub- division must be employed, in order to avoid confusion. I dare not venture, in the present imperfectly investigated con- dition of these forms, to prepare a permanent nomenclature for them. I content myself with directing attention to the subject, merely using the name JN. varians as a convenient symbol for the group. I entertain no doubt that other analogous groups will be detected by careful examination. It is quite plain that in such groups form, shape, or outline cannot be. regarded as a trustworthy specific character, although it is probable that many species exist in which the form, being constant, may be safely used in this way. It is an important question how far other characters, such as the number of the striz, or their arrangement, or the general aspect, may be depended on as specific characters. In this case, as in that of form, there seem to be many examples in which the characters are constant. But yet other cases occur where the tendency to vary seems to extend to these characters also. Thus, I have more than once pointed out that Pinnularia divergens, W. Smith, which, as it occurs in the Premnay peat, has, according to W. Smith, 11 striz in 001”, occurs abundantly in the Mull deposit, and in many recent gatherings, with every detail, and especially the very peculiar arrangement of the striz, which have three centres of divergence, precisely as figured in the Synopsis, while the number of strie is from 24 to 26 in :001". I have now repeatedly met with both varieties, and although the number of striz seems never to fall so low as stated by Mr. Smith, yet there is a very marked difference. It would be out of place here to enter minutely on this question, which, however, is well worthy of attention. It will probably be found that in certain cases none of the characters above alluded to are constant ; while in many they appear to have a great degree of uniformity. But it is strictly within the scope of this paper to notice a group allied to that of WV. varians, and differing from it chiefly in the number of striz. I have already stated that some of the forms now figured had been referred to such species as NV. semen, NV. rhyncocephala, P. gracilis, and P. radiosa, in all of which the normal number of striz is from 24 to 26 in ‘001." Now, I find, occurring generally with those forms which I refer to the group of WN. varians, others, having, like them, all or most of the varied shapes I have alluded to, and yet having of Diatomaceous Forms. | 15 much finer stria; in fact, agreeing in this respect with the four species just named. To this group belong the form figured in my paper on the Mull deposit as Pinnularia exiqua ; that figured in the same paper as a doubtful form of P. radiosa, or between that species and P. peregrina, and a considerable number of other forms, which not only have the striz inclined and otherwise arranged exactly as in NV. varians, but pass into one another by intermediate forms, Their aspect is quite distinct from that of MN. vartans, because the strie, being much finer, cease to be conspicuous, as they are so remarkably in NV. varians. To this group belongs also a form I lately described * as WN. latiuscula, and I am inclined to. believe that the group includes WN. semen, N. rhyncocephala, P. gracilis, P. radiosa, and others, just as I suspect that the group of NV. varians includes WN. peregrina and P. (qy WN ?) oblonga. In favour of this supposition, | may mention that a friend informs me that the striz of P. gracilis have been found by him to be moniliform, although the fact may not yet be thoroughly established. This, it will be observed, corres- ponds to Mr. Smith’s observation on the strie of P. peregrina. It is well known that the strie in P. gracilis are somewhat obscure, and that in this, as well as in number, they differ from those of N. varians. .But we can now see how it was that several of the forms of WV. varians were referred to P. gracilis. The latter, with its normal striation, appears to belong to the second group which I have mentioned, and which, for convenience, may be called N. mutabilis. It will be observed that if, in the case of NV. varians, the two characters of variableness of outline and variableness in the number of striz should be found united, NV. varians and N. mutabilis would then constitute but one group, divided, in the first instance, into those with 16 striz in *001” or WN. varians, and those with 26 strie in '001,” or N. mutadilis, whether these divisions be regarded as species, or as subgenera. I have only farther to add, at present, that both these groups are widely distributed and often abundant, whether in the shape of the known species, such as P. peregrina, P. gracilis, &c., or in that of the types now first pointed out. I have named those gatherings or deposits in which they occur most abundantly ; but there are few mixed fresh-water gather- ings in which some of them do not occur. I have it, fortunately, in my power to supply observers with some of the most interesting gatherings, and I shall be happy to forward small portions of these, or slides, where the material is very scanty, to such microscopists as may wish to examine them. * In the paper already alluded to in a preceding nete. DESCRIPTION OF PLATE I. In illustration of Mr. Rose’s Paper on Parasitic Borings in Fossil Fish-scales. Fig. 1.—Borings in a cycloid scale (Osmeroides?), from the lower chalk of West Norfolk. 1a magnified 35 diameters. At c¢, in this figure, is shown the confluence of two tubes at their commencement. 1 b, a por- tion more highly magnified. 2.—Borings in another scale, magnified 1385 diameters. 3.—Borings in a svale of Prionolepis angustus, from the lower chalk ; magnified 135 diameters. 4.—A variety of the last, from another scale, perhaps placoid, obtained from the lower chalk. 5.—Borings in fragments of a Fish-scale, from shales of Kimmeridge clay. a,a. The specimen from which these are taken has lost the external lamina, therefore the borings lie between the two lamin, or in an inferior one. b,b. This specimen has the external lamina on it. c. The external lamina is in this figure situated at d. e Ford & West, Imp. Tuffen West. sc. CUE 4) On the DEvELopMENT of the Empryo of Purrura Lapittus, By Writtram B. Carpenter, M.D., F.R.S., F.G.S., Presi- dent of the Microscopical Society of London, &c. &c. (Read December 29th, 1854.) Nortwitustanpine the large amount of attention which has been given by Microscopists, during the last twenty years, to the development of the ova of Gasteropod Mollusks, and the completeness with which, in particular cases, its successive stages have been observed, much still remains to be learned respecting it. And this is more especially the case with re- gard to the Pectinibranchiate order, which includes not only a very large proportion of the entire class, but also comprehends those forms which, by general consent, would be regarded as its types. For nearly all the most complete series of observa- tions yet made, have had for their subjects either Nudibran- chiate or Pulmonated Mollusks; the ova of the former pre- senting peculiar facilities for examination, in virtue of their extreme transparency, and the rapidity with which they undergo some of their most important changes, so that these can be watched while in actual progress ;* and those of the latter having attracted the attention of that large class of naturalists, who, not having the opportunity of sojourning at the coast, are glad to avail themselves of the opportunities afforded by the universal diffusion of Helices, Li ymnei, &c., for the prose- cution of this kind of research.+ * On the embryonic development of Nudibranchiate and Tectibranchiate Gasteropods, see especially the admirable memoir of Vogt, on Address of the Present. 27 on the other hand, if the plasmatic division between the vacuoles should be unusually broad, a new vacuole forms in its substance. Now this mode of cell-development I believe to be altogether a new fact to physiologists; and although Mr. Wenham’s observation stands as yet unconfirmed, yet it accords so well, on the one hand, with the facts which I have stated with regard to the simpler Protophytes, and on the other, with appearances which I have myself observed in various animal structures, that I feel a strong couviction of its essential truth. If, now, we direct our attention to the Protozoa, or simplest forms of animal life, with a view to inquire whether there be among them any phenomena of a parallel kind, we are at once struck with the strong resemblance which their condition bears to that of the humblest Protophytes. Taking the well-known Actinophrys sol as a typical example, we find that it consists of a nucleated particle of “ sarcode” (the equivalent of the vegetable “ protoplasm”), whose destitution of anything like limitary membrane is evidenced by its extraordinary power of extending itself into filaments, which, when they happen to meet each other, undergo a complete coalescence. Yet this nucleated particle behaves, in many respects, as a true cell. It draws nutrient material into its interior, applies it to the augmentation of its own substance, and multiplies itself by duplicative subdivision. It has been supposed even to per- form the generative act by conjugation with other particles like itself; but recent observations upon Actinophrys and allied organisms, have rendered it very doubtful whether the fusion of two of these particles is a real conjugation ; since no special product has been observed to result from it; and not only two, but several, individuals have been seen thus to coalesce together, the composite mass afterwards resolving itself again into isolated particles not apparently differing in any respect from the originals. What is the true meaning of this act, therefore, we are at present unable to affirm ; but the fact, however we may interpret it, is in itself extremely significant, as affording an additional proof of the homogeneousness of the sarcode-body of the Actinophrys. I need scarcely stop to remark, that the same is true of the animal bodies of the Foraminifera generally ; for these, in so far as we are acquainted with them, are nothing else than homogeneous particles of sarcode, extending themselves into pseudopodia, whose coalescence, when they happen to encoun- ter one another, affords ample evidence of the non-existence of any limitary membrane. In Ameoba, the distinction between cell-wall and cell-contents begins. to show itself; the super- * 28 Address of the PRESIDENT. ficial portion of the sarcode having decidedly more consistence than the interior ; and the pseudopodia being much less freely extended. Still, however, the consistence of this external layer is not such as to present any obstacle to the reception of alimentary particles into the interior of the sarcode-body through any portion of its surface, or to interfere with the rejection of indigestible particles,—the temporary orifice, in either case, being at once closed by the coalescence of its edges ; so that there is obviously no definite limitary mem- brane, notwithstanding that the liquidity of a large part of the interior substance allows a free movement of granular particles in every direction, as I observed many years ago. Thus, the Ameba seems to me to represent that condition of the vege- table cell, in which the primordial utricle is distinguishable as the external more condensed layer of the protoplasmic mass, but does not possess the distinctness of a proper mem- brane. A more advanced stage is seen in the curious Gre- garina, which must be regarded as corresponding with the Protozoa in the simplicity of its organization, whilst it resem- bles the Entozoa in the peculiarity of its habitat. For here, the distinction between the cell-wall and the cell-contents is decidedly marked ; the former becoming more consistent, and the latter more liquid. The body undergoes great changes of form, but no pseudopodial extensions are sent forth; and the nutrient materials being imbibed in a liquid state by the whole surface, neither are solid particles introduced by an oral orifice extemporised in the superficial layer, nor are rejectamenta extruded through a like extemporised anus. Passing-on to the Infusoria, we find much reason to regard these simpler forms (at any rate) in the light of cells modified for an independent existence; and their essential difference from Actinophrys and Amoeba seems to lie in this, that the external layer of the sarcode is condensed into a more definite limitary membrane,—a change which involves other altera- tions. For, in the first place, the body can undergo compara- tively little change of form ; and no pseudopodia can be sent forth. And, secondly, as the alimentary particles can no longer be introduced through any point of the surface, a definite orifice is left in the membranous envelope, into which the nutrient materials are driven by the peculiar dis- position of the cilia; and, in many cases, a definite anal orifice is also provided, through which indigestible matters may be ejected. : Thus, among the Protozoa, as among the Protophyta, whilst we trace a gradual advance in the differentiation of the homo- geneous particle of sarcode into the true cell, we find vast Address of the PRESIDENT. 29 multitudes of beings passing their whole lives (so far, at least, as we are acquainted with them) in that earlier and simpler condition, in which no such differentiation has taken place, and in which, therefore, the structural constitution of a cell has not been attained. Now before I pass on to inquire how far this condition finds its parallel in the elementary parts of higher organisms, I wish to stop for a moment, to notice how strongly the differences between the Vegetable and Animal kingdoms are marked out, even in those lowest and simplest forms of both, which we have been just engaged in considering. For the Protophytes, like the most perfect Plants, draw their nutri- ment from the inorganic compounds which are everywhere within their reach,—water, carbonic acid, and ammonia; by decomposing carbonic acid, they give off oxygen; and they form for themselves the starch and the chlorophyll, the cellu- lose and the albumen, which they apply to the augmentation of their own substance. On the other hand, even those hum- blest Protozoa, the Rhizopoda, can only exist (so far as we can see) upon organic materials previously elaborated by other beings: these they receive ‘‘ bodily” into their interior ; and though mouth, stomach, intestine, and anus, all have to be extemporized every time that the animal feeds, yet the digestion which the alimentary particles undergo in its interior, is not less complete than that which is performed by the most elaborate apparatus which we anywhere meet with ; and the nutrient materials thus obtained seem to be appro- priated, without any further conversion, to the augmentation of the substance of the body. Thus, notwithstanding the remarkable analogy which these two orders of beings exuilpia I cannot see that any difficulty need be experienced in separating them, when we are acquainted with their mode of nutrition. The Gregarina constitutes no real exception; for although it imbibes its nutriment through its entire surface, like the Protophyte, yet that nutriment has been previously digested and prepared for it by the animal whose body it inhabits ; and in the absence of any oral orifice or digestive apparatus of its own, it corresponds with a far higher group of animals, the Cestoid Worms, which live under the same conditions. Some recent observations, it is true, would seem to invalidate this distinction, by showing that certain rhizopods and infusoria have their origin in undoubted plants ; but we must be permitted for the present to withhold our assent from conclusions so strange, and to question whether they may not be invalidated by some unsuspected fallacy. It has been well remarked, however, that ‘ there is no limit to the possibilities VOL. IV. d 30) Address of the PRESIDENT. of Nature ;” and | should be the last to attempt to set up as fixed laws what are merely the expressions of the present state of our knowledge, or to wish to throw discredit on the ob- servations of accomplished and careful microscopists, merely because they overthrow distinctions which I had imagined to be well founded. I would strongly recommend the observa- tions of Professor Hartig (Quart. Journ. of Microsc. Science, Vol. IV., p. 51) and of Mr. Carter (Ann. of Nat. Hist., Feb., 1856) to your attentive scrutiny; and hope that some of our members may be able, ere long, to furnish either a confirmation or a refutation of them. Turning, now, to some of those parts of the fabric of higher animals, in which a cellular organization has been described by some observers and denied by others, I think I shall be able to show that the discrepancy is capable of being recon- — ciled, by the application of the principle of progressive dif- ferentiation to the mass of sarcode in which any such organ originates. Thus having found, in various kinds of shells, certain instances in which a very definite cellular organization appeared to me to exist,—others in which this organization was less definite, though still (as I thought) unmistakeably present,—others in which it was only faintly indicated,—and others in which I could discern no traces of it ;—and having also met with gradations from one condition to another, even in the very same shells ;—I thought myself justified in con- cluding that the animal basis of the shell-substance must have been originally cellular in every case, but that the divisions between the cells must have been lost in some cases by a very early coalescence. Mr. Huxley, on the other hand, has recently expressed an opinion,* founded on an examination of my own preparations, that the whole of my interpretation is erroneous, and that no cellular structure can really be discerned in shell. Now in the justice of this verdict, | cannot say that I am pre- pared to coincide ; on the other hand, I am quite ready to admit that my original interpretation requires modification. Taking the general history of the first formation of a leaf from a layer ‘of protoplasm, as probably applicable to the formation of a lamina of shell from a layer of sarcode, I should now interpret the appearances which my preparations exhibit, as follows :—In those forms of shell-substance in which I can discern no structure whatever, and in which a continuous membrane is left after decalcification, I should be disposed to think that the entire layer of sarcode has undergone calcifica- tion, before any differentiation of parts had begun to take place in it. In those again in which (as in Mya and Thracia) a * ‘Cyclopedia of Anat. and Physiol.,’ Supplement, p. 489. Address of the PRESIDENT. dl cellular arrangement is more or less obvious in the section, but in which no distinctly-cellular residuum is left after decal- cification, I should infer that the processes of vacuolation and of consolidation had commenced, but had not proceeded far, when the calcification took place. Lastly, in those in which (as in Pinna) a very definite residuum, apparently cellular, is left after decalcification, the very striking resemblance which this bears to that stage in the vacuolation and consolidation of a layer of protoplasm about to form a leaf (as described and figured by Mr. Wenham) which immediately precedes the formation of distinct cells, induces me to think that such must have been the stage in which the sarcode-layer must have undergone calcification. Hence, whilst agreeing with Mr. Huxley that in few (or perhaps none) of the structures which I have described as cellular, are any complete cells ordi- narily formed, [| still believe that in all of them there has been a nisus more or less operative, towards the development of cells; their differences lying solely in the greater or less degree of differentiation, tending towards the production of perfected cells, which had manifested itself in the sarcode at the time of its calcification. I am strongly disposed to believe, that the same doctrine will apply to many other animal structures, in which the pre- sence of a cellular organization is affirmed by some and denied by others. If, for example, you look at the scale of an Eel, you observe that its otherwise homogeneous substance is marked out by ovoidal spaces, which suggest the idea of cartilage-cells with an intervening matrix. By Professor Williamson, who _ has carefully studied the structure of fish-scales,a layer of this kind has been shown to be of very general occurrence ; and he considers these ovoidal spaces to be “ botryoidal concre- tions” of calcareous matter, having no relation whatever to cells. And he puts the like interpretation on analogous appearances exhibited by various egg-shells, which have been regarded by Professor Quekett and others as indicative of a cellular organization. Now the microscopic appearance of the scale of the Eel so precisely resembles that of the leaf- forming layer of protoplasm, as figured by Mr. Wenham, that I can scarcely doubt that its ovoidal spaces are vacuoles formed with a view (as it were) of becoming cells; and that the regularity of the shape and disposition of the calcareous concretions is determined by that of the vacuolations. And the condition of such egg-shells as exhibit an appearance of cellular structure, so closely resembles that of many shells of mollusks, in which there is a cellular areolation without well- 32 Address of the PRESIDENT. defined membranous partitions, that 1 can scarcely hesitate in attributing to it a similar origin. The general doctrine, then, which seems to me best to express the facts I have stated, is that those essential endow- ments which we have been accustomed to attribute only to the typical cell, may exist in that comparatively-homogeneous substance which is commonly termed “ protoplasm”’ in the vegetable kingdom, and “ sarcode” in the animal; that iso- lated particles of this substance may comport themselves after the manner of true cells, although no distinction between cell-wall and cell-contents may have made itself apparent ; and that various organs and tissues among the higher plants and animals have their origin in larger extensions of the same substance, in which the process of ced/ulation may either pro- ceed to the complete evolution of an aggregate of perfect cells, or may be stopped at any point, so as to leave but faint traces of the tendency in question. I have already adverted to the belief which I have from the first entertained, that in the animal body, the fibrillation of the blastema may take place quite independently of cellulation; and I am much disposed to think that the formation of other tissues may take place by alike direct process of conversion. But I wish to take this opportunity of protesting against the assertion, that where no perfected cells can be demonstrated, there is not a tendency to a cellular organization, however incomplete may be its result. It would be just as unphilosophical, in my opinion, to assert that the white fibrous tissue does not mani- fest the tendency of the blastema to fibrillate, because it seldom exhibits isolated sharply-defined fibres like those of the yellow or elastic tissue. Some apology might, perhaps, seem due for thus occupy- ing your time in an abstract physiological disquisition ; but next to correct observation, is the right interpretation of what we see; and, in fact, it is often extremely difficult (as is obvious in the history of this very inquiry) to distinguish between the impressions which the objects themselves make upon our minds, and the ideas which we connect with those impressions. And I am desirous that those whom I have now the pleasure of addressing, should be put in the way of examining for themselves into the merits (1) of the cell- doctrine as commonly held, (2) of the opposite view put forward by Mr. Huxley, and (3) of the intermediate doctrine which I have this evening endeavoured to expound. Address of the PRESIDENT. 33 It now only remains for me, in resigning the chair to m successor, to thank you most gratefully for the kind indulg- ence which you have so constantly extended to me; and to express my regret that I have not been able to do more to promote the interests of the Society, by myself furnishing original communications to its meetings. It is known to many of you, that the small amount of time which I can spare for original research, has long been devoted to one special object, the elucidation of the structure and physiology of the Foraminifera; and the liberal assistance which has been afforded me by the Royal Society in the prosecution of my researches (whereby I have been enabled to procure the unrivalled series of microscopic drawings that I have exhi- bited from time to time at our meetings), makes me feel it but common gratitude, to place before that Society the systematic results of my researches. And further, the number and variety of demands upon my time have entirely precluded my making any such active exertions to obtain communications from others, as may not unreasonably be ex- pected from your President. I have the gratification of believing that my successor may be much more able than I have been, to contribute to your welfare in both these modes; and it is, therefore, with much satisfaction that I look for- ward to being replaced by one of the oldest members of the Society, who has given evidence of such extensive attainments in various departments of Microscopical Science, and who will, I feel confident, do the fullest credit to your choice. I have only to beg you to believe, that the warmest desire to promote the interests of the Society has never been wanting on my part, and that nothing but the coercion of circum- stances, which I could not control or resist, has prevented me from more fully manifesting the sincerity of that desire in labour for your benefit. x cs 2a ( Na avalite reas iy, hy oa a ede On the Post-rertiary Diatomaceous Sanp of GLENSHIRA. Part IT. Containing an account of a number of additional undescribed species. By Witi1amM Grecory, M.D.,F.R.S.E., M.R.I.A., &c.; Professor of Chemistry in the University of Edinburgh. Illustrated by numerous figures drawn from Nature, by R. K. Greviiiz, LL.D., F.R.S.E., &c., and engraved by Turren West, Esq. (Plate V.) (Read March 26, 1856.) In the first part of this communication * [ described the pecu- liar locality in which the Glenshira Sand occurs, and pointed out, that the remarkable mixture of marine and fresh water forms which it contains, was a proof that, when this sand or mud was deposited, the fresh-water lake, then filling the upper part of the valley, and standing, of course, at a higher level than it now does, must yet have occupied the same relative level, compared with the sea, which it now occupies, when it is confined to the lowest part of the valley, and being exactly at the level of half-tide, flows into the sea at low water ; while, at high water, the sea flows into the lake. This state of matter produces in the lake, at this moment, a mix- ture of marine and fresh-water species, not only of diatoms, but also of other tribes, both animal and vegetable. And as the. existence of a similar mixture in the sand now under ex- amination, deposited at the higher level, implies that at the period of its deposition the relative levels of the sea and of the lake were the same as now, while we see that the lake now stands at a lower level than formerly, we infer, that since that period the land has risen, or the sea has fallen; a con- clusion justified and supported by many other geological phe- nomena in the estuary of the Clyde, with which Loch Fine, the arm of the sea into which the Dhu Loch of Glenshira flows, communicates. In the same paper I gave a list of about 215 known species of Diatoms, and nearly 20 undescribed species, which I had found in the deposit ; a number of species far exceeding that hitherto found in any other similar deposit, so far as is known to me. This, I conceive, indicates that the circumstances which favoured the mixture and accumulation of species must have been of very prolonged duration. At the same time I stated that there remained about as many more undescribed forms as those I had been able at that time to figure, and that these should be figured and described on some later occasion. I now proceed to fulfil that promise. I must explain, however, that it is impossible for me to com- * ¢ Quarterly Journal of Microscopical Science,’ vol. iii., p. 30. VOL. IV. é - 36 Dr. Greeory, on the Post-tertiary plete the investigation in the present paper. In the first place, the sand is not yet exhausted ; for although I have ex- plored about 600 slides of it, new forniis are sf toes tae to time occurring. Secondly, it has been found impossible to finish the study even of the whole of those which I had ob- served in it in 1854, and to prepare figures of them. I pro- pose, therefore, only to describe and figure, at this time, such of the new forms as have been duly studied. This is, no doubt, the majority of them ; but it will require a third paper to complete the examination, more especially of the smaller forms, among which, as well as among those of the larger which have not yet occurred entire, much remains to be done. Before describing the new forms, I must add to the list of known species formerly given the following, many of which were accidentally omitted. Others have since occurred to me, and a few have been pointed out to me by Mr. Okeden, well known as a zealous observer. These I have also myself seen. Additional List of known Species. 235.* Cymbella sinuata, W. G, 250. Navicula Pandura, Bréb. (?) 236. Amphora membranacea. 251. Pinnularia megaloptera, Ehr. 237. a salina. 252. ‘4 biceps, W. G. 288. : hyalina. 20. ~, linearis, W. G. . 239. Amphiprora paludosa. 254, #3 subcapitata, W. G. 240. Campylodiscus Ralfsii. 255. »» + sracillina, WW. . 241. Actinocyclus undulatus. 256. Pleurosigma distortum. 242. Actinocyclus ? ate u, intermedium. 243, Actinocyclus duodenarius, Sm. | 258. Gomphonema subtile, Ehr. 244. Nitzschia bilobata. 259. Orthosira spinosa. 245. Navicula Westii. 260. ae mirabilis. 246. ns obtusa. 261. Grammatophora Balfouriana.t+ 247. 55 Hennedii. (See Synopsis, Vol. II. Pl. LXI. 248. 2s rostrata. fig. 383.) 249. Navicula varians, W. G. (in all its forms). On this list I would only remark, that the species marked W.G. have been lately described by me, as well as Nos. 248, 251, and 258, the two last as new to Britain;} that No. 249, Navicula varians, has been also fully desoneen by me elsewhere : § that No. 243, Actinocyclus duodenarius, appears -* These numbers are continued from Part I., in which J gave a list of 234 species. + Ihave given a figure of this form, as being little known as yet. At first it seemed to differ from the form ‘ficured by Dr. Greville, the inter- rupted vittz being less conspicuous, the striee more so ; : but I am now satisfied that it is essentially the same form, which varies, however, more than was at first supposed. The figure is not numbered, as it is not intended for engraving. + ‘ Quarterly Journal of Microscopical Science,’ vol. iv., p. 1. § ‘Trans. Micr. Soc., Quart. Journ. of Micr, Science,’ No. X., p. 10, Jan. Loop. a Diatomaceous Sand of Glenshira. 37 as a British form in Vol. II. of Smith’s Synopsis. I have found in Glenshira several forms of this kind, differing only in the number of septa, which varies from 7 or 8 to 14 or 16. I observe in Pritchard’s Animalcules, that Ehrenberg makes a species of each number of septa ; but to judge by the aspect of these forms in Glenshira, they are all of one species, which I have named duodenarius, because 12 is about the average of the septa in those I have seen there. No. 250, Navicula Pandura, was last year figured by De Brébisson as occurring at Cherbourg. I mark it with a query, because it is doubtful whether it may not be the same species as WV. nitida, Sm., (named in my former list,) and also because I have great doubts as to either of these forms being correctly named. They belong to a very striking group, in which the Glenshira sand is somewhat rich, and which I shall have presently to consider more fully. Of No. 247, Navicula Hennedii, I give a figure, because very fine specimens occur in this deposit, and the form has not yet been figured, though it will be described in Vol. II. of Pro- fessor Smith’s Synopsis. The two Orthosir@ are also new forms; O. spinosa having been found in Braemar by Drs. Greville and Balfour, and in Auvergne by Professor Smith, and figured both by Dr. Greville and Professor Smith ; and O. mirabilis having been found last summer in Wales by Mr. Okeden, but not yet figured. I may here mention, that I had observed and sketched both, in my earliest explorations of the Glenshira sand, fully three years ago; but from the number of new forms, T was compelled to postpone the study of them, and had not been able to resume it when the naturalists above named discovered them. But before the account of O. spinosa had appeared, I had again found both forms in three or four South American soils. I mention this here, because my ob- servations on these soils have led me to doubt whether O. mirabilis be not an abnormal state of O. spinosa. My reasons for thinking so are: 1. That inall the localities in which O. mirabilis occurs, it is accompanied by O. spinosa. 2. In the Glenshira sand and in the American soils, I was un- able to find any discoid or end view, or diaphragm, which I could suppose to be that of O. mirabilis, except that of O. spinosa; and I believe that Mr. Okeden has been equally unsuccessful. 3. I found one cylinder, one-half of which had the peculiar markings of O. mirabilis, narnely, two series of curved or sigmoid lines, decussating and crossing the cylinder transversely ; while the other half had all the characters of O. spinosa. 4. In no specimen of O. mirabilis have I seen any appearance of the usual septa, so strongly marked in e 2 38 Dr. Grecory, on the Post-tertiary O. spinosa, which leads me to suppose that the markings are due to the septa having been removed and replaced by some new internal arrangement. 9. In both forms, the ends of the cylinders exhibit the spines, or appearance of spines, from which OQ. spinosa is named. It was for these reasons that I did not earlier mention O. mirabilis as a species; and as for O. spinosa, I had postponed it with other forms, otherwise both might long ago have been known. Let us now turn to the new forms. Here I must premise that a few of those new figures were described and figured in my former paper. I have figured these again, in some cases, be- cause the former figures were accidentally erroneous ; or in others, on account of additional peculiarities, or because I now understand the forms better than I was at that time able to do. By far the greater part of the forms now given are figured for the first time. 1. Navicula rhombica, n. sp. In my former paper are two figures of this species, which is very frequent in the sand. I now give two more figures, to complete the history of it. Length from 0-001” to 0-0025”. Form rhombic, with somewhat acute apices as in the former figures, or elliptic lanceolate, with obtuse extremities, as in fig. 1. Stria fine, but easily seen with a good 1-4 or 1-5, about 45 in -O0O1”, but those near the middle of the valve much more distant, so as to be almost conspicuous ; the striz slightly inclined. Median line strong ; nodule large and well marked. Valve colourless, or pale yellow. The above characters sufficiently distinguish this species from WN. rhomboides, which, in the typical form, is always acutely rhombic, of a much darker colour, and has no definite central nodule, the two halves of the median line ending in sharp triangular points. The striz in WV. rhomboides are so fine, that I have never yet been able to see them with a 1-5 of extraordinary goodness, and they are indeed hardly to be resolved by the 1-8; they are also parallel. All these things unite to give to WV. rhombica an aspect so entirely different from that of WV. rhomboides, that it is impossible to confound the two forms, where, as in the present deposit, they occur together. I may add that the variations of NV. rhomboides, viz., WV. crassinervia and WN. interrupta, W. G., are quite distinct from those of NW. rhombica. I state this, because some who have only seen the figures of NV. rhombica in my former paper, have supposed that it is only WV. rhomboides. Those who have seen the forms will admit that it is not possible for two species of the same genus to differ more thoroughly; but it is im- Diatomaceous Sand of Glenshira. 39 possible, in all cases, to represent in drawing, characters which, in the forms, are perfectly satisfactory. Since writing the former paper, however, I have observed an additional mark of distinction, which has even led me to doubt whether the form under consideration be a Navicula at all; for it frequently occurs in what I may call packs, like packs of cards, in which six, eight, or more are laid flat and close on each other, I have represented one of these in fig. 1.* This is a character which | have not observed in any Navicula, although it is easy to imagine that some species of the genus may occur in such groups. From the fact of these packs being so frequent in a deposit like this, so long water-tossed, it may be inferred, that the forms composing them are very firmly attached together in the living state. I must leave to better authorities to decide whether this be a Mavicula or not, merely observing that it is a well-marked and beautiful species. I believe WV. rhombica to be a marine form, having seen it, with other marine species, in a recent gathering from the coast near Tantallan, Haddingtonshire. ‘There were also some fresh-water, or rather brackish-water forms, derived from the mouth of a small brook near the spot. If it be marine, this will be another point of distinction between it and WV. rhomboides. I have seen no trace of it in all the very numerous fresh-water gatherings I have studied, though NN. rhomboides is one of the commonest forms (222.)f 2. Navicula maxima, n. sp. This was also figured in my former paper, but I now give some additional figures of it, both because I have since found much finer specimens, and in order to show its usual varieties. Form linear, broad, usually a little incurved at the middle, with broadly acuminate apices, as in fig. 2. Also linear, narrow and long, without constriction, as in fig. 2*. Some of this variety are very long and narrow; and there are also forms intermediate between 2 and 2*, as in fig. 2**. Length from 0:0035” to 0°:0065”. Median line strong, usually some- what bent towards the central nodule, at least in the broader variety. Striz transverse, parallel, reaching the median line ; fine and close, about 50 in 0:O0OL” in the broader, consider- ably finer in the narrower variety. Colour of the valve in balsam, clear straw yellow. The valve is thick and convex, so that, when not lying quite flat, the edges become black. It is a very striking form, and frequent in the coarser densities of the prepared sand. From the figure formerly given, some have supposed it to be identical with MW. firma Bf, Sm. As that form was not + This is the number attached to the species in the list given in Part I. AO Dr. Grecory, on the Post-tertiary figured in the Synopsis, Vol. I., and I was at the time little acquainted with it, | was at first inclined to adopt this view. But a further examination of both forms has satisfied me that they are distinct. WV. firma f has, even in balsam, a strong brown colour; its striation is coarser, and far more conspicuous, and is also slightly inclined; and it forms several well-marked varieties, which have been: described and figured by Ehrenberg as distinct species, such as JV. dilatata, NN. amphigomphus, and others. Now, so far as I can see, N. maxima exhibits no other varieties than those here figured, which I give for the purpose of comparison. Moreover, while in N. firma, in all its forms, we have a side line on each side of the median line, WV. maxima bas usually two such lines on each side. Lastly, both forms occur in this deposit, and are easily distinguished by their general aspect, even under a low power. (225.)* 3. Navicula Hennedit, Sm. I give a figure of this beautiful species, because no figure of it has yet “been published, and because the finest specimens [ have seen occur in the Glen- shira sand. As it will be fully described in the Synopsis, Vol. IL, I need only say here, that fig. 3 represents a very fine one, although I have a specimen one-half larger even than this, (247. st 4. Navicula latissima, n. sp. This is another very ee species, which occurs very well developed in our deposit. Form very broadly elliptical, with very obtusely acuminate apices, having usually a very slight constriction before the extremities. The sides are occasionally parallel in the middle. Length from 0:002” to 0-005”, or even 0:006”. Some of the shorter individuals, from the great breadth, are nearly or- bicular. Nodule very large, median line doubly conical, the bases of the cones meeting at the nodule. This appearance is due to the striation, which does not reach the middle, and re- cedes farthest from it near the central nodule. Striz rather coarse, finely moniliform, bighly radiate, and not reaching the true inner median line. Colour of the valve, in balsam, a strong straw yellow, occasionally light brown. : I understand that some are disposed to refer this form to N. granulata, Bréb., which, as I stated in my former paper, also occurs here. But I cannes do this; for in WV. granulata, not only are the striz much less numerous, even though it is a considerably smaller form, but they are composed of large granules, so distant as to give a special character, from which Be name is taken. In J. latissima, the striz# are indeed * So numbered in Part I. + So numbered in the list of known forms, given at page 34. Diatomaceous Sand of Gilenshira. 41 moniliform, as in many other navicule, but this character is far from being conspicuous. Moreover, the invariable and decided colour of the valve distinguishes it from NV. granulata, which is colourless. Neither have I ever seen in UW. latissima the produced or apiculate apices of NV. granulata. I consider NN. latissima to have very well marked characters, and the aspect of the larger individuals to be entirely peculiar. Fig. 4 represents one of the shorter, and fig. 4* one of the longer forms of this fine species. (262. ) 5. Navicula quadrata, n. sp. (=. humerosa, Bréb. ) This form is allied to the preceding, and is equally frequent in the deposit. Form rectangular or nearly square, the ends suddenly con- tracted to short produced apices. Length from 0:0015” to 0-005” or even more, the breadth not increasing with the length in the longer individuals. The usual length is about 0:0025” or 0:003”. Striz radiate, much finer than in JW. latissima, minutely moniliform, coming nearer to the median line. Fig. 5 represents an example rather below the average size. When I first observed this form, and sent it to de Brébisson, he told me that he had then just found it at Falaise, and had named it NV. humerosa; but he preferred my name as having been the earlier, and as more characteristic. Subsequently, Professor Smith referred it to NV. granulata, Bréb., with which it agrees in form, while it differs from it remarkably in striation and aspect. De Brébisson, having found it quite un- mixed with WV. granulata, still, I believe, regards it as a dis- tinct species.* For this reason, | give it here as such, adding, however, that I think it probable that it may prove to be a variety, not indeed of WV. granulala, but of WN. latissima, from which it differs, indeed, both in form and in number of stria, but which it resembles considerably in general aspect. In my paper on Navicula varians,} 1 have shown that neither outline nor-number of striz are to be relied on, in certain cases, as specific characters, and [ shall take an early opportunity of directing attention to other tacts of the same kind which I have since observed. I may add that in this deposit there occur forms which, both as regards outline and striation, are intermediate between this one and the preceding, WN. latissima. _Even as a variety, however, it requires to be noticed and figured, in order to give a correct idea of the species as we find it. (263.) I may here state that all the three forms, NV. latissima, tor] _.™ It appears as such, I find, in Vol. II. of the Synopsis, p. 98, as N. humerosa. Of course I shall withdraw my name. and adopt that of de Brébisson, to avoid confusion. + ‘Quart. Journ. of Mier. Science, No. X., p. 10, Jan. 1855. 42 Dr. Grecory, on the Post-tertiary NN. quadrata, and N. granulata, are marine forms, and that they all occur in recent gatherings on our coasts. 6. Navicula formosa, n. sp. This is a very beautiful form, and is frequent in the coarser densities of the deposit. Form, an elegant linear elliptic, or elliptic lanceolate, with somewhat obtuse extremities. Nodules large and definite ; median line like that of many Pinnularie, such as P. viridis. Strie slightly inclined, about 35 in -001”, not reaching the median line. There is, on each side of the median line, a side line, parallel to it. Length from 0:003” to 0:0065.” ‘At one time I referred N. maxima f and this form to one species, but in WV. formosa the striae, besides being inclined, and not reaching the median line, are much more conspicuous, giving to the form a peculiar and well-marked aspect. I had also some doubts, whether it should not be referred to Pinnularia, rather than Wavicula, but I have preferred the latter, because I believe the striz to be moniliform, though very minutely so. Fig. 6 represents a specimen, nearly of the average size; it is, however, often considerably longer. 1 have not yet seen it elsewhere. (264.) 7. Navicula pulchra,n, sp. This very pretty form is not so frequent in the deposit as most of the preceding species. Form, elliptic lanceolate, almost rhombic, with a slight in- flexion towards the extremities; not very broad. Length about 0-003.” Striz not very fine, very highly radiate, and very strongly moniliform, which gives to it a very peculiar aspect. Fig. 7 represents what appears to be the typical form, which I have only seen in this deposit. (265.) 8. Navicula angulosa, n. sp. This very beautiful form is frequent in the medium densities of the sand. Form elliptic lanceolate, rather broad, with acute apices. Length from 0:0025” to 0:0045.” Strize conspicuous, marginal, and bounded, internally, by an angular, rhombic space. No- dules definite, median line sharp and distinct. It is repre- sented of the average size in fig. 8, I understand from Mr. Bleakley, that he has found this form on our eastern coasts. Var. 8. Rather smaller. Form linear, sides parallel, ends acuminate, striz more distant; otherwise agreeing with a. Represented in fig. 8*. This also seems to have occurred to Mr. Bleakley. Perhaps this species ought to be referred to ‘the genus Pinnularia, but it is not easy to define these two genera. We shall see presently that moniliform or costate striz are not always to be depended on, although Professor Smith distin- - guishes them by these characters. I was at one time persuaded to refer this form to N. palpebralis, but having carefully — studied authentic specimens of that species, I am satisfied that Diatomaceous Sand of Glenshira. 43 they are distinct. Indeed NV. palpebralis is a very small form, while WV. angulosa is generally large and conspicuous. But the angular space in the middle in both varieties of N. angu- losa, is a good and permanent mark of distinction. (266.) 9. Navicula Macula,n.sp. This is a very remarkable form, which is not rare in the lighter densities of the deposit ; but | have never seen it elsewhere as yet. Form elliptic in the middle, short, contracted, and again slightly expanding to very obtuse, almost truncate apices. In shape it is not unlike the larger specimens of Cocconeis fiexella ( Thwaitesi?, Sm.). Length, 0:0015” to 0-002”. Median line straight, abruptly terminating at two points some way on each side of the centre. ‘There is no central nodule, but only a large blank space, the length of which lies across the middle of the valve, and which looks like a stain. Beyond this, towards each end, the valve is very finely striated. Striz about 70 in 0001", transverse and parallel. The peculiar blank central space, which is not at all like an expanded nodule, differs from anything I have seen in any other form. I have examined not less than 100 specimens, and in none of them could I see any appearance of a central nodule, nor could I trace the median line farther than the margin of the blank, as we can do in so many forms where the nodule is expanded. Fig. 9 is a very accurate representation of this form, which is remarkably uniform in its characters. (267.) 10. Navicula solaris, n. sp. ‘This is a very pretty and well- marked form, frequent in the middle densities of the deposit. It is represented in fig. 10. ~_ Form rhombic, long and narrow, with obtuse extremities. Length from 0:0015”" to 0:0045”. The striation is fine, but very distinct, even conspicuous, very much inclined towards the ends, and in the centre, where there is a small circular blank spot, so highly radiate as to present the appearance of a sun with rays. Stria 36 in ‘O0L". The valve is usually of a brown colour, more or less deep, even in balsam, There is some resemblance between the shorter individuals and P. ra- diosa; but WN. solaris, besides having finer striz, and those more inclined, is usually much longer. As both forms occur in the deposit, they are easily seen to differ very materially in aspect. I have not yet observed it elsewhere. (268.) 11. Navicula Pandura, Bréb.? In the course of last year a very beautiful form was described and figured under this name by de Brébisson as occurring in sea water at Falaise. I have here given under this name, as a British form, that which is represented in fig. 11, although it does not appear to be in all points identical with that of de Brébisson. But the Glen- 44 Dr. Grecory, on the Post-tertiary shira sand is particularly remarkable for the occurrence in it of several different forms of the same general type, which I figure that they may be compared with others from different localities. That which I have named, doubtfully, W. Pandura, is in shape panduriform, very deeply constricted in the middle, with the extremities nearly triangular, broad, with somewhat acute apices. Nodule square; median line strong, double, straight, with two dark lines, parallel to it, and close to it on each. side, converging at the ends. These lines are shades, caused by elevations in the striae, and similar to those in N. elliptica, Kutz (ovalis, Sm.), and in NV. didyma. Length 0-004” to 0:005”. Striz coarse, very conspicuous, costate. Indeed, had not de Brébisson named his form Navicula, I should have called it Pinnularia, as the coste resemble those of P. alpina. It will be seen that the next form has the same character. (269.) 12. Navicula nitida, Sm.? I have named this form, repre- sented in fig. 12, also doubtfully, as no description of the species has yet appeared. It is represented in fig. 12. Form like that of the preceding, but less deeply constricted, and the ends longer in proportion. Length 0-003” or 0:004”. Striz not quite so coarse as in the last, costate. I have been re- peatedly informed that this is Professor Smith’s WV. nitida, but I cannot reconcile this with his definition of MNavicula as having moniliform, Pinnularia as having costate striae. (270.) 13. Navicula incurvata, n.sp. This form, which belongs to the same group, is a true Mavicula, if that generic name imply moniliform striation. Form approaching to that of the two preceding species, but much more gently constricted, narrower in proportion, and with the extremities very uniformly rounded, Median line straight, with the dark-shaded lines on each side. Striz much finer than in the two last, about 30 in -001", and minutely moniliform. It is perfectly uniform in its character, and a well-marked species. Length 0-003” to 0-004”. (271.) 14. Navicula splendida, n. sp. This very fine species is also a true Navicula, but still belongs to the same group. Form panduriform, much constricted, very broad at the shoulders, ends triangular and obtuse. Length 0-005" to 0-006.” Median line straight, nodule square. Strizv rather fine, compared with the two first forms of the group; but dis- tinctly moniliform ; not reaching the median line, and leaving on each side of it a long narrow blank space, whiel ‘adda to ite apparent breadth. The aspect of this form, as may be seen in the figures, is very different from that of the other forms of the group. It is the rarest of them in this deposit, and, as yet, has not occurred elsewhere. (272.) Diatomaceous Sand of Glenshira. 45 15. Navicula didyma, var. y. To the four preceding forms I add one more, which I do not venture to erect into a new species. It has the form and size of a very frequent form of N. didyma, but with the entire or costate striz of Nos. 11 and 12, This character would lead us to make it a Pinnularia, were it not that de Brébisson, and even Professor Smith him- self, who gives it as a character of Pinnularia, have referred, in N. pandura and WN. nitida, costate forms to the genus Navicula. At least I am so informed as to UN. nitida, for I have not seen Smith’s description of it, nor an authentic speci- men named by him. De Brébisson’s figure of N. pandura speaks for itself. | I. have figured the costate form, which, for these reasons, I refer for the present to N. didyma, in fig. 15. No detailed description of it is necessary, and I need only say here, that I frequently meet with it in the Glenshira sand, along with the other forms of this group, ,which I have figured, and that, besides the two common forms of WV. didyma, well figured by Smith, our deposit contains one, if not two other varieties which have moniliform striz, and which I refer also to NV. di- dyma, a species which, like NV. elliptica, Kiitz. (ovalis, Sm.) and W. elliptica, Sm. (Smithii, Bréb.), appears to vary much both in outline and general aspect. 16. One of these is represented in fig. 16. It is frequent in the deposit. I call it WV. didyma, 6. It is evident that all these constricted forms belong to one group, but how they are to be classified it is not easy to say. The following questions naturally occur :—1. Do the costate forms constitute one or more species? 2. Are the monili- form types of this group to be referred to one or more species ? 3. Is it possible that all these forms, whether moniliform or costate, belong to one and the same species? and if so, how is that species to be defined ? ) If we refer them all to one species, or even if the form, fig. 15, be referred to NV. didyma, or figs. 11 and 12 to Navi- cula, what becomes of Professor Smith’s definition of Pinnu- laria, and how is that genus to be distinguished from WNavicula? I do not pretend here to answer these questions ; but I may state, that the form fig. 15 has every appearance of being a variety of WN. didyma (agreeing precisely, as it does, in form and size with the commonest small form of that species, which is very abundant in the deposit); and if that be so, then we have moniliform and costate striz in the same species. I may add that I have made observations on N. elliptica, Kitz. (.N. ovalis, Sm.), a common fresh-water form, which tend to show that it passes into UW. didyma, 46 Dr. GreGory, on the Post-tertiary equally well known as a marine form.* And I have also observed, that WV. eldiptica, which varies remarkably in all obvious characters, sometimes acquires a nearly, if not a per- fectly costate striation, though usually strongly moniliform. . As I propose soon to lay these observations before the Society, I shall not here go farther into the subject. 17. Navicula clavata,n.sp. ‘This very fine form, represented in fig. 17, has at first sight some resemblance to N. Hennedii ; but on close inspection, it presents remarkable characters. Form elliptic, broad, with broad rounded projecting masses at the apices, which are the extremities of the median line. Striation marginal, asin WV. Hennedii, but the inner bounding line of the striated band, instead of being purely elliptic, as in that form, becomes towards the extremities, nearly straight, so as to form a kind of angle, giving to the included blank space between it and the median line, a very remarkable form. Median line complex. First there is in the middle, as in N. Hennedit, a narrow line proceeding from each end, and terminating on each side of the centre, and at a short distance from it, in long rounded expansions; the other extremities are also rounded, but larger. Between the two central knobs lies a rectangular white space, extending in its length at right angles to the median line, and rather narrow. It reaches beyond the general width of the middle part, that is, the striated portion now to be mentioned, expands at the middle. On each side of the proper median line is a transversely striated band, which, near the ends, touches the median line, but near the middle, recedes a little from it on both sides. The striated band expands into large round heads, projecting beyond the true elliptical outline of the valve, and it also ex- pands a little in the middle. The white blank across the centre appears to have at each end a small striated patch placed trans- versely to it. The large swollen ends of the complex median line, not only project, forming short snouts, but stand out strongly from the surface of the valve. The strize appear rather coarser than those of N. Hennedii, about 20 in -001", and are very distinctly moniliform. Length of the valve, 0:0034”. I may here mention that Dr. Greville has found in the same Trinidad sand which I have alluded to elsewhere in this * T observe that in Vol. II. of the Synopsis, Professor Smith gives, as N. elliptica, Kiitz. var. 8, the form which I found in Lochleven, and which resembles NV. didyma. I admit that it seems to be a variety of N. elliptica, Kiitz., but I cannot find any essential difference between it and certain forms of N. dydyma. Is it possible that N. elliptica, Kutz. may take the form of N. dydyma in sea water, and that some other local cause may have produced the same modification in the fresh water of Lochleven ? Diatomaceous Sand of Glenshira. | AT paper, and which has yielded so many fine new forms, a still larger and finer Navicula, to which he has paid me the com- pliment of attaching my name. In this form also, we find the projecting, rounded, club-like snouts to the valve, standing out from it in the same manner. It is quite distinct from the form here figured, although, no doubt, the two forms belong to the same group. I think I have seen, in the Glenshira Sand, indications of a tendency in the larger forms of Navicula Smithii, Bréb. (elliptica, Sm.), to pass into snouted varieties, with the snout rising in relief from the surface of the valve. 1 have not met with WV. clavata, except in this deposit. (273.) 18. Pinnularia longa, n. sp. This remarkable form, of which an. average example is represented in fig. 18, is not rare in the deposit, but, on account of its slenderness, is seldom found entire. Form rhombic, very long and narrow, with acute termina- tions. Coste very conspicuous, distant, inclined or radiate, about 12 in 0-001". Length from 0-004” to 0-008”, but usually about 0-006”. ‘The only known form to which it has any resemblance is P. directa, Sm. But in P. directa, the form is rather lanceolate than rhombic, while the striz are much more numerous, and are also parallel, reaching the median line, which those of P. longa, in the middle, at least, do not reach. Moreover, P. directa, so far as I have seen, is a much smaller form. PP. longa has another peculiarity, which is, that the median line, as seen in the figure, is gene- rally twisted. ‘The valve appears very thick. (274.) 19. Pinnularia fortis, n. sp. This is a very pretty little form, and frequent in the lighter densities of the deposit. It is well represented in fig. 19. Form nearly rhombic, or rhombic lanceolate, rather short, apices somewhat obtuse. Length from 0-002" to. 0:0035. Costz conspicuous, about 16 in -001, and apparently projecting from the surface of the valve, for on the edge view they seem to stand out, and the valve has, in consequence, a very pe- culiar aspect. The valve is also very convex towards the extremities, but concave in the middle, which gives to the F. V. a constricted form. There is a blank space at the centre, round which the cost radiate. There is something about the form very difficult to reproduce in a drawing. The coste appear very distant, yet when counted, we find them much more numerous than we expected; and if we give in the figure the real number, the whole character of the form is lost. This character is well represented in the figure, but there are fewer coste there than in the original. It is a very well-marked form. (275.) 48 Dr. Grecory, on Post-tertiary Sand of Glenshira. 20. Pinnularia inflexa,n. sp. This is a remarkably neat little form, well marked, and frequent in the lighter densities. Form elliptic lanceolate, ends acute. Striation conspicuous. Coste subdistant, highly radiate, leaving in the centre a rather large round blank space, about 26 in 0:001”. Near each apex is a strong black cross-bar across the valve, which I believe to be caused by a depression in the valve, and I have named it from this character. Length 0:0014". It is very uni- form in its characters, and is well represented in fig. 20. (276.) 21. Pinnularia acutiuscula, n. sp. This is another well- marked species, frequent in the finer densities. Form long, almost lanceolate, with the sides parallel in the middle, and slowly converging to the acute apices. See fig. 21. Length from 0:002"' to 0:0026”. Strize distinct and conspicuous in the middle part, from being more widely separated. They are also radiate, but less strongly so than those of the two preceding forms. ‘They are finer than in these forms, and are about 30 in ‘001’. The only form to which this one has any resemblance is P. acuta, but its peculiar form and aspect are quite sufficient to distinguish it. Both forms occur here, and when seen together appear quite different. (277.) 22. Pinnularia Ergadensis, n. sp. I have given this name, from Ergadia, Argyll, to the species represented in fig. 22. Form nearly linear, or linear elliptic, ends rounded, obtuse, almost truncate. Length from 0-002" to 0:0045", or more. Striation finer than in P. fortis, but conspicuous ; cost about 25 in 0:001", sub-distant, not quite reaching the median line, somewhat inclined. It is frequent in the lighter densities, and has a perfectly distinct aspect, so that it cannot be con- founded even with P. fortis, the form which it most resembles, but in which the character of the striation is totally different. As yet, I have met with none of the species of Pinnularia here figured, except in the Glenshira sand. (278.) 23. Stauroneis amphioxys, n. sp. This curious form is not un- frequent in the lighter densities, and is well represented in fig. 23. Form nearly rhombic, tending to lanceolate, with acute apices. Valve highly convex, so as very often to pre- sent the dark appearance of an air-bubble, and, even in the best position, showing the margin as a broad black line. Stauras broad, reaching the margin, very transparent, so as often to be seen with difficulty, if in the least out of focus. At other times it is black, from the general convexity. Striz fine, very nearly parallel, transverse, nearly 60 in 0-001”, not conspicuous, often apparently irregular, from the convexity of the valve. (279.) (To be continued.) HEnrrey, on some Fresh-water Alge. 49 Notes on some Fresu-waTER ConFERVOID Aca, new to Bri- TAIN. By Artruur Henrrey, F.R.S., Professor of Botany, King’s College, London. (Plate IV.) (Read March 26, 1856:) Panpvoritna Morum, “hr. Pandorina, Ehrenberg (Char. emend). Frond a microscopic, ellipsoidal, gelatinous mass, containing imbedded near the periphery, sixteen or more biciliated, permanently active gonidia, arranged in several circles perpendicular to the long axis of the frond. The gonidia, almost globose, with a short, beak-like process, a red spot, and a pair of cilia which pro- ject through the substance of the frond to form locomotive organs upon its surface. Reproduction—1l, by the conversion of each gonidium into a new frond within the parent mass ; and 2, by the conversion of the gonidia into encysted resting spores, which are set free, and (?) subsequently germinate to produce new fronds. P. Morum, Ebr. (P1. IV., figs. 1-25.) Fronds hyaline; from about 1-80” downwards. Gonidia either sixteen, and then arranged in four circles of 4, or thirty-two, and then in five circles, three at the poles of 4, and the intermediate three of 8 gonidia, which in the perfect form stand near the peri- phery and wide apart. In the forms which produce the resting spores, the gonidia are crowded together in the centre. The gonidia are green, but the contents of the resting spores, after they have become encysted, are converted into oily and. granular matter of a bright-red colour. The description of Pandorina given by Ehrenberg, is so incorrect, that no one would be able to determine the organism by its aid; but the figures in the ‘ Infusionsthierchen, al- though rude, are sufficient for identification. Pandorina Morum has been observed by Focke* and Alex. Braun in recent years, who pointed out the errors of Ehrenberg in stating that the gonidia had only one cilium and no eye-spot ; but we do not anywhere find a clear and satisfactory account of this creature. It was with much satisfaction that we re- ceived early in February of this year (1856), from H. Pol- lock, Esq., a bottle containing a vast quantity of Pandorina Morum, which he had found colouring the water in a pool at : Hatton, near Hounslow, Middlesex. * «Physiolog.’ Heft., ii. 1854, Pl. 1V. t+ ‘ Verjungung,” Ray Society’s Vol. for 1853, pp. 169, 209. 50 HeEnrrey, on some Fresh-water The forms presented by this organism are exceedingly varied, and nothing can be more beautiful than a number of them revolving slowly on their long axes in a drop of water, as seen under a power of about 100 diameters.* In the first place, the perfect form exhibits two patterns shown in figs. 1 and 3, and there are minute counterparts to these, remain- ing in that state, as in figs. 7 and 9; while in the water where the species is actively multiplying, all sizes between figs. 13 and 14, just emerged from the parent frond, and the full grown from figs. 1 and 3, &., occur. The form with 32 gonidia results from the cell-division going on one stage further than in the form with 16; but this difference is fixed during the earliest stages of development, as the form with 16 (fig. 1) never changes into that with 32 (fig. 3), after it has become free from the parent. In the perfect forms the gonidia are arranged near the periphery of the frond in circles, like the equator and parallels of latitude on a globe, so that Pandorina resembles Cohn’s Stephanosphera{ more closely than any of the other Volvocinee, that having a single equa- torial ring of gonidia in its globular frond. Among the forms with the isolated gonidia occur others almost equally numerous with the gonidia collected together into berry-like heaps (figs. 15-20); these are smaller than the others, but equally varied in dimensions ; their gonidia resemble those of the other form; they appear destined to form the resting spores. The gonidia are almost globular; they have no proper membrane, but consist of a gelatinous, granular substance which contains a thinner fluid in the centre, as it contracts strongly by exosmosis when strong saline solutions are ap- plied. There is a large, nucleus-like body (the chlorophyll- vesicle of A. Braun) at the posterior end of the gonidium (fig. 5), and at the opposite side is a short beak-like process, with a colourless space behind it; the pair of cilia arise here, and a little to one side and below these is the reddish-brown granule called the ‘ eye-spot. We have never been able to observe a pulsating vacuole, as described by Busk and Cohn in Volvox and Gonium. The gelatinous frond appears to be perfectly homogenous, without any boundary membrane. Jodine and sulphuric acid do not colour it blue. It is tolerably resistent, and appears solid, as it does not give way or become indented by exter- nal pressure, as is the case with the hollow frond of Volwoz. The fronds are multiplied by the conversion of the gonidia * A. Braun says they revolve constantly to the right; but they change the direction constantly. + ‘ Annals Nat. Hist.,’ 2nd Ser., x., p. 321, &c. Confervoid Alge. : D1 into new families. If they are viewed at night, many of the fronds may be found at rest at the bottom of the vessel (in the daytime they assemble at the side next the light), motionless, and with the gonidia rounded and deprived of their nucleus. By covering up the bottle from the light, the development of the new fronds, which naturally takes place very early in the morning, may be retarded so as to be followed during the morning until noon. Some of the fronds may be found with the gonidia converted into berry-like heaps (fig. 10), others with the gonidia already distinct (fig. 11), while many parent fronds present the young fronds more or less regularly arranged in the softened and expanded parent mass (fig. 12), which ulti- mately dissolves and sets them free (fig. 13,14). They then increase in size in proportion to the favourable conditions in which they are placed. I have never seen anything like what are described by Cohn in Stephanosphera as ‘ microgonidia.’* When kept for some weeks, an increasing quantity of fronds became accumulated at the bottom of the water, and these chiefly of the character shown in fig. 17, but devoid of cilia; and while many of them decayed, in others the gonidia be- came encysted so as to form globular cellules. Left for a fortnight, the water was found without a trace of green colour, with merely a brownish sediment at the bottom, upon ex- amining which, it was found to contain a large number of berry-like: forms (fig. 17), with the gonidia not only encysted, but with their contents converted into a red, oily, granular substance (figs. 21-25), as in the resting-spores of many Con- fervoids. The gelatinous frond was here almost dissolved away, and a slight pressure was sufficient to detach and separate the cellules, which are doubtless resting-spores, and destined to become subsequently developed into new fronds. This remains to be decided. The organism thus described is a well-marked and distinct species, very different from Volvoxz and Gonium, but approach- ing near to Stephanosphera. The form which produces the resting-spores, after losing its cilia, is Kutzing’s Botryocystis Morum, Ihave met with a form like this not unfrequently, but never before with the perfect Pandorina. Mr. Pollock tells me that he has collected trom the same pond for some years past, but never found Pandorina before, and yet it colours the water green this season. Volvox seems, in like manner, to come and go at intervals of years, its revivification from the resting-spores depending much on external conditions. * ¢ Ann. Nat. Hist.,? 1. c. In a letter received from Professor A. Braun since the above was written, he speaks of the forms with small gonidia (figs. 7—9) as the ‘microgonidial’ form. A. H., June, 1856. VOL. Iv. mi 52 HEnFrEY, on some Fresh-water Apiocystis Brauntana, Nageli. Aptocystis, Nageli. Frond a microscopic, hyaline, gela- tinous, sac-like body, attached by an attenuated base; contain- ing numerous green globular gonidia, multiplying, during the growth of the frond, by quaternate division, and finally breaking out by a lateral orifice as active, two-ciliated zoospores, each of which becomes encysted and grows up into a new frond. A. Brauniana, Nag. (PI.1V., figs. 26 and 27.) Frond pyriform, 1-600” to 1-25” high, the cavity filled up by gela- tinous matter, in which are embedded the gonidia, at first few, increasing in number with age as far as 1600, each about 1-2000" in diameter. Nigeli, ‘ Einz. Algen,’ p. 67, Pl. ii A; Kiitzing, ‘Spec. Alg.,’ p. 208. Fresh-water ditches, &c. A few young specimens of this little plant were observed in January of this year (1856) in a jar of water containing aquatic plants, brought from Wimbledon Common six months previously. ‘The whole collection was destroyed by frost soon after, so that the development was not followed. Nageli (0. c.) gives the following account of it:— “The young ‘ swarm-cells’ (zoospores) attach themselves by their ciliated point (especially to Cladophora fracta), and become invested with a club-shaped enveloping membrane. ‘The first division of the green body then takes place in the direction of the axis of the vesicular envelope, and is repeated, in A. Brauniana, alternately in each direction of space. During this the vesicle in which the cells (gonidia) lie, continually expands, and generally becomes very evidently pedunculated. Young vesicles contdin a regular number of cells, namely, 2,4, 8, 16, 32, &c. ; but the number afterwards becomes indefinite ; in largish vesicles, 1-50” long and 1-120” in diameter, I have counted about 800; in the largest, about 1-25" long and 1-50" thick, some 1600 cells. “‘ The cells (gonidia) are at first uniformly distributed over the whole cavity of the vesicle. Subsequently they generally become collected on the internal surface of the wall of the vesicle, where they lie in one or more strata. But the cell-division always takes place in all directions of space, the cells situated internally advancing outwards towards the periphery. In old vesicles the cells are sometimes arranged in rings of 8 upon the wall. “ When the family of cells is mature for ‘ swarming,’ which may occur at very different sizes and with very different numbers of gonidia, the cells begin to move at first slowly from their places, and then gradually to circulate more rapidly in and out about each other. The vesicle bursts and the gonidia emerge by the orifice which is formed. Sometimes the swarming is preceded by the state in which the cells are arranged in parietal rings. ; “The cells secrete an abundant gelatinous coating, which becomes ~ softened within the vesicle, and confluent into a structureless jelly. The vesicle sometimes appears merely as the boundary line of the jelly; in general, however, it may be distinguished as a distinct wall composed of denser gelatinous substance (PI. IV., fig. 25), the internal outline of which is always distinct and sharp, while the outer is frequently indistinct and partly dissolved.” Confervoid Alge. 53 The vesicle sometimes presents delicate ciliary processes on the outside. The zoospores have two cilia, according to Al. Braun.* They have no ‘ eye-spot.’ CLATHROCYSTIS AERUGINOSA. Clathrocystis, Nov. Gen. Frond a microscopic gelatinous body, at first solid, then saccate, ultimately clathrate, (frag- ments of the broken fronds occurring in irregularly-lobed forms,) composed of a colourless matrix, in which are im- bedded innumerable minute gonidia, which multiply by divi- sion within the frond as it increases in size. (No zoospores or resting-spores observed.) C. eruginosa. (PI. IV., figs. 283—36.) Fronds floating in vast strata upon fresh-water pools, forming a bright green scum, presenting to the naked eye a finely granular appear- ance ; when dried appearing like a crust of verdigris. Gonidia or green cells, with a distinct membrane, about 1-8000” in diameter, leaving a hyaline border at the surface of the fronds ; full-grown fronds, 1-50" to 15” in diameter. Microhalea eru- ginosa, Kiitzing. (‘ Linnea,’ viii, p. 371, Pl. 8, fig. 23.) Microcystis icthyoblabe, Kiitz., ‘Phyc. Gen. ex parte. Mene- ghini, ‘Monogr. Nostoch.’ p. 104. Microcystis eruginosa, ‘Tab. Phyc.’ i, Tab. 8. Polycystis eruginosa, Kiitz., ‘Sp. Alg.,’ p. 210. “ Flos Aque,” ‘Treviranus,’ Linnza, xvii., p- 51, Pl. 3. On fresh-water lakes. This remarkable form does not appear to have been ob- served hitherto in Britain. We found it in the autumn of 1855, forming a scum extending over a large portion of the surface of the lake in the Royal Botanic Gardens at Kew. A portion of it, brought home and preserved in a room ina bottle of water, continued to grow healthily until the middle of winter. It is very well described in the paper of Treviranus above referred to; but none of Kiitzing’s descriptions mention its remarkable mode of growth or its peculiar form when perfect. Apparently that author has only seen it in a dry state; it does not agree with the definitions of the genera Microcystis or Microhaloa ; and as the name Polycystis has been occupied in the Fungi, we have ventured to add to the already confusing synonymy, by giving it a distinctive and characteristic name. The smallest fronds met with are usually roundish or ellip- soidal, of the character shown in PI. IV., figs. 28 and 34. When quite young they appear to be solid, but as they grow by the multiplication of the internal gonidia, and the secretion of gelatinous matter, the expansion takes place chiefly near the * “Verjungung,’ &c., Ray Soc. Vol. 18538, p. 209. f 2 o4 HENFREY, on some Fresh-water Confervoid Alge. periphery, so that the frond becomes a hollow body (just as the stems of Grasses or Umbellifere become fistular). ‘The walls of the sac then give way, (figs. 29 and 30,) and as the expansion proceeds, orifices are formed in different parts, until the whole becomes a coarsely-latticed sac or clumsy net, of irregularly-lobed form (fig. 31). Then this becomes broken up into irregular fragments (figs. 32—34) of all shapes and sizes, (giving the stratum a granular appearance to the naked eye,) each of which recommences. the expanding growth, and becomes a latticed frond. The internal cells are very minute, but have a distinct margin with internal granules (figs. 35 and 36). They multiply by dividing into two or four. ‘The gela- tinous frond always presents a transparent border or peripheral stratum, destitute of green cells; but no boundary membrane exists, the surface exhibiting a softened or half-dissolved aspect. On the approach of winter the fronds ceased to in- crease, and by degrees most of the gelatinous masses faded to a light brownish tint, swelled up and settled to the bottom of the water in light flocculent clouds. They appear to become half dissolved, and to allow the green cells to become. free, as many of the latter were found free, adhering to the sides of the vessel ; perhaps these reproduce the fronds in the next season. No zoospores were ever detected. The verdigris-like appearance of this Alga when dead is most remarkable and characteristic. While growing, in its wet state, it is rather of a yellowish opaque green colour. As to the systematic position of the above species, Pando- rina belongs, of course, to the Volvocinee ; Clathrocystis is doubtless referable to the same group as Pulmella cruenta, and therefore to the family of true Palmellacee, which will require to ‘be kept apart from Protococcus, and similar forms, on account of the absence of zoospores. -Apiocystis must remain’ for the present in the heterogeneous assemblage which in- cludes Protococcus, Gleocapsa, &c., which require much more study before they can be satisfactorily classified. WenuaM, on Illuminating Opaque Objects. 1) On a Meruop of Ittuminatinc Opaque Ossects under the Highest Powers of the Microscore. By F. H. Wenuam. (Read March 26th, 1856.) REPEATED experiments have shown, that it is a matter of extreme practical difficulty to contrive any method of con- densing light directly down upon an object, when viewed under an eighth or twelfth object-glass of large aperture. In the first place, the close proximity of the front lens and its setting, will only allow a thin conical disc of light, to find a passage towards the object, at an angle of seldom less than 100°, or at an obliquity far too great to be practically useful ; and secondly, when the object is covered with thin glass, con- siderably more than half the light will be lost by the reflection from the surfaces, the rays from which enter the microscope, and occasion an amount of glare and fog sufficient to obscure the object; for these reasons I think that there is but little chance of obtaining any useful result in this direction.* The methods that I now bring before the Society are based upon an entirely different principle, which is not applicable to dry objects, but only to those mounted either in Canada balsam, fluid, or any other refractive medium. An experience of nine months warrants me in the assurance of its complete success, as a means of investigation—objects being brilliantly illuminated in a jet-black field, with an objective of 170° of aperture or more. The principle of operation consists, in causing rays of light to pass through the under side of the glass slip upon which the object is mounted, at the proper angle for causing total internal reflection from the upper surface of the thin cover, which is .thus made to act the part of a speculum, for throwing the light down upon the under-lying objects, immersed in the balsam or fluid. _ As there will be no total reflection from the planes of a parallel plate of a refractive material, it is necessary to adopt some method for allowing the rays to enter the medium at such an angle as to cause total reflection from the upper sur- face. There are many methods of effecting this; those which I now describe I have found to be the most practicable and useful: a,a, fig. 1, is a glass slide containing objects mounted in balsam; 6, thin glass cover; ec, is a right-angled prism * Since the above, Mr. Ross has shown me his ingeniously-contrived Leiberkuhn, applied to the highest powers for illuminating wncovered opaque objects, and which performs most admirably ; to my mind un- doubtedly proving the fact, that the minute scales from the wings of butterflies, &c., are perfect cellular structures. 56 Wenuam, on a Method of cemented on to the under surface of the slide with Canada balsam ; d, is an Amici prism for condensing and directing the rays into the prisin c; e, is a large bull’s-eye condenser placed with its convex side towards the lamp. Fig. 1. Making ample allowance for all possible differences of refraction in the slide, balsam, and cover, the angle of total reflection for the mean refrangible ray, will vary from 40° to 45° from the perpendicular—at any rate it will never exceed the latter degree ; consequently for this reason I consider the right-angle prism the most convenient for most purposes, as the rays may be passed perpendicularly through its surfaces with- out any trouble arising from refraction. The mode of action illustrated by the diagram is simply as follows: the rays from the luminous source are first collected and converged by the large bull’s-eye lens e, and then further condensed and directed upwards by the Amici prism d; they next enter the surface of the right angle prism e, and pass directly onwards till they reach the upper side of the thin cover, from whence they are totally reflected down again, forming a brilliant surface of light, which will of course illu- minate any small bodies immersed in the balsam just below. If the cover is clean and free from scratches, not the smallest portion of light from the luminous source will find its way through. The view of the objective will be unimpeded, and the field perfectly black. Another way of causing the light to enter the prism, is by means of a parabolic condenser, adjusted as under ordinary circumstances ; the light will in this case enter the two faces of the prism at the same time, which is some advantage ; it must be sufficiently small to have some Illuminating Opaque Objects. 57 play in the cavity at the apex of the paraboloid ; if the right- angled faces are one quarter of an inch square, it will perform very well. The objection to the plan just described is the necessity of having a separate prism for every object, which, though of advantage in some remarkable and peculiar cases, is not necessary for all. Fig. 2 is more universal in its appli- cations ; aa is a thin plate of brass, 5, a right angle prism let in exactly flush with the upper surface; any smal] objects Fig. 2. such as animalcules, Diatomacee, pollen, &c., must be laid upon the prism with water, and covered with thin glass; total reflection will then occur from the uppermost surface, in the same way as in fig. 1, and illuminate the objects in the fluid. Any ordinary plane slide containing objects mounted in balsam may be placed upon the plate and prism, first inter- posing a drop of water. It is almost unnecessary to remark that if this, or some other fluid is not interposed, the rays will all be reflected from the back of the prism itself, instead of passing onwards into the slide. Fig. 3 is another method ; aa is a glass slide—under this is cemented with Canada balsam a lens, 0}, nearly hemispherical, with a seg- ment removed so as to leave the thickness equal to about one-third the dia- meter of the sphere. The flat facet of the lens is blackened. The radius of curvature should be about two-tenths of an inch: the use of the blackened facet is to exclude all rays below the incident angle of total reflection. This lens is intended to be used in conjunction with the parabolic condenser, in the manner represented by the figure. The rays from the parabola pass through the surface of the lens in a radial direction without refraction, and proceed till they reach the upper surface of the thin glass cover, where they are totally reflected and converge upon the object; the Fig. 3. 58 Wennam, on a Method of cover in this instance acts precisely the part of a Leiberkuhn, with the advantage of more perfect reflection. A lens of this description may be. let into a thin plate of brass as in fig. 2, and used in the same, way as an aquatic holder, the parabolic condenser always being used for concen- trating the light. When a slide containing balsam-mounted objects is placed above the lens, instead of using water, it is preferable to employ turpentine, or oil of cloves; the refractive index of the latzer being nearly the same as crown glass. The reason for introducing this agent is because light impinging upon the polished plane between a greater and a less refractive medium, will always suffer total reflection at the surface of the former, at a given angle dependent upon the relative refrangibilities. If water is used, the angle of the illuminating pencil will be limited to about 160°; above this, all rays will be reflected down again by the flat surface of the lens, and lost, as shown by fig. 4; aa represents the glass slide, with Fig. 4. IN objects in balsam ; 0 is a hemispherical lens placed underneath the slide, with water interposed ; cc, rays which pass onwards to the top plane of the thin glass cover, to be reflected down again upon the object: the dotted lines, dd, are the portions of the illuminating pencil, that will be lost by being reflected from the flat surface of the Jens—of course if a medium of nearly the same refractive power as the glass is used, such as oil of cloves, all this light will be transmitted and rendered available. Another variation in this principle of illuminating opaque objects, is that illustrated by fig. 5: @ is a small paraboloid of solid glass with a flat top. A black stop, 6, of the same diameter as the apex, is fixed at the base of the parabola, for Illuminating Opaque Objects. 59 the purpose of stopping out direct rays. This paraboloid is set in a ring, which is screwed underneath a flat brass plate, Fig. 5. so as to bring the upper plane surface of the glass exactly level with that of the plate in the manner shown by the figure. The parabola must be sufficiently short to prevent any rays from passing within the angle of total reflection relative to the flat top—or the paraboloid may be cut off at the point in the curve intersected by an angle of 45° drawn from the focus. If a powerful series of parallel rays be sent into the base of this paraboloid, not any of the light will find its way through the upper flat surface. The whole will be reflected down again into the hody of the glass. If now a piece of thin glass is placed on the top, with a-drop of water, the greater portion of the illuminating pencil will be transmitted to the upper surface of the cover, and from thence totally reflected, illumi- nating any small objects contained in the fluid. Glass slides containing balsam objects may be placed on the apex of the paraboloid, using an intermedium of turpentine, camphine, or oil of cloves, in preference to water. This same reasoning also applies when small objects are viewed directly in fluid, by being laid on the flat top of the paraboloid, and covered with thin glass. When the nature of the substances will admit of it, for the purpose of obtaining greater intensity of illumina- tion, they should be placed in turpentine or oil of cloves; in _this case the whole of the light will be reflected from the top surface of the cover—no separate reflection taking place from the upper plane of the paraboloid, as with water. In using this instrument, all that is required is to throw direct light into the parabola, by means of the concave mirror. Having now described some modifications of this principle of illuminating opaque objects, as most especially adapted for the highest powers, numerous experiments will justify me in saying a few words as to the effect. The light may be ob- tained of any required degree of intensity, and the field per- 60 Wennam, on the Vegetable Cell. fectly black, with objectives of the most extreme aperture ; some Diatomace@ mounted in balsam, are shown with a degree of beauty and delicacy, that I have never seen equalled, and from the lights brilliantly illuminating the prominences on the surface, many of them wear an entirely different appearance to the same objects seen as transparencies, and from the absence of all irregular refraction and colour, and the purity of the vision, the mind is impressed with the fact, that we are viewing them under their true features, as cellular structures, and in some instances displaying such a singular arrangement and con- figuration of markings, in cases where I had not even suspected them to exist, that I shall on a future occasion give some illustrations of them. It must not, however, be expected that all the Diatomacee can be seen by these methods, for some of them, when mounted in balsam, are so exceedingly translucent, that they will not hold a sufficient quantity of light, to be viewed as strictly opaque objects. For this method of illumination, the greatest nicety is required in the adjustment of the object-glass, the slightest defect in this causing milkiness and indistinctness of vision— indeed so particular is the care required in this respect, that a different adjustment is sometimes necessary for various parts of the same object, in a case where it lies in an inclined position in the balsam. With regard to the relative merits of the three methods that I have mentioned; for those who are already possessed of a parabolic condenser, the preference is most decidedly to be given to the hemispherical lens, fig. 4, set in a very thin plate of brass, but the truncated paraboloid, fig. 5, is by itself a most convenient piece of apparatus, readily applied and easily managed, forming a most useful adjunct to the other. On the VEGETABLE Ceti. By F. H. Wennam. (Read May 28th, 1856.) In the ‘ Annals of Natural History’ for May, 1856, there is a notice, by Professor Henfrey, relating to my paper on ‘ Cell Development,’ published in the ‘ Quarterly Journal of Micro- scopical Science’ for Jan. 1856. I prefer making my reply through the medium of the same Journal, which is accessible to all whom the subject may concern. The notice commences by saying :—‘ The essay contains internal evidence of the author’s want of familiarity with the subject treated.” It does, in all probability, contain irregu- larities and omissions which may possibly be excused in an inexperienced writer on these particular subjects. I pretend Wennam, on the Vegetable Cell. 61 to be nothing more than a sincere searcher after the truth, uninfluenced by motives of ambition or notoriety ; and it is not fair that I should be criticised according to the same rigid rules which would be applicable to an established pro- fessor. As regards “‘ want of familiarity with the subject,” I can only say, that for years past I have examined the deve- lopment of the vegetable cell, and have been trying, without success, to reconcile the facts that I. have observed with the written statements of Mr. Henfrey; for it is to these, or such as have appeared under his sanction, that I have made the most particular reference. ‘This is my excuse for not viewing these things through the medium of Mr. Henfrey’s eyesight, and for falling back upon my own judgment; and I trust that I may be pardoned for so doing. Even to this hour the cell theory is by no means a settled question, and I would advise those engaged in this study to form their ideas less upon a groundwork of contending theories, and apply more diligently and directly to the book of nature for information, It is to be regretted that any remarks should give rise to this form of reply, so directly out of the course of correct scientific discussion. I will now proceed to notice Mr. Hen- frey’s objections, which are scanty enough. He first says, in reference to me:—“ The objects selected were unfavourable, and not favourable as he imagined ; for young leaves of most flowering plants, in the stages figured by him, are not flat plates, but cones, or at all events solids having more than one thickness of cells in all three dimensions ; therefore the view is confused by one layer lying behind another.” In reply to this I may say, that if Mr. Henfrey had condescended to read my paper before thus perverting my meaning, he would find these subjects described as “ cellular-cones,” or “ nodules of protoplasm filled with cell-cavities ;” so that this objection must at once fal] to the ground: and to avoid the delineation of that confusion he mentions, I had drawn directly with the camera lucida the top layer of cells only, and any error in form and position is a trifling one, occasioned by the object being slightly flattened in the compressor. Mr. Henfrey further remarks :—‘‘ But even in the leaves of Anacharis the application of dilute sulphuric acid and solution of iodine suffices to render the structures clearly dis- tinguishable, as quite different from what is represented in Mr. Wenham’s drawings.” No doubt of it! I believe that there are but few recent vegetable structures that would submit to such treatment unchanged. I have tried numerous experiments with these and other re-agents, but ceased to place much confidence in them for the investigation of very young 62 Wennam, on the Vegetable Cell. cells ; for, though they are most useful for testing the transi- tion stages between protoplasm, starch, and cellulose-layers; &e., they are extremely prone to develop an appearance of saan brawies and organisms that do not really exist. I much prefer, when the case will admit of it, to view the structure and note the successive stages of development under natural conditions. I am, however, far from wishing to disparage the valuable test referred to. The effect of sulphuric acid and solution of iodine, in the young cells in the cases in question, is to cause the cavities in the formative plasma to become more distinctly apparent, as perfectly clear spaces, containing nothing else but a watery fluid. The objection that I have sometimes found in using it is, that in the boundary of a consolidated plasma, known to be homogeneous, it is apt to develop the appearance of layers, or zones, not arising from cellulose deposits, but caused by the grades of chemical action of the test. When young cells contain but a small quantity of contents, another fallacy may arise, from the application, for they become drawn together in the centre of the cavity, appearing as a ball of nucleus, As a further explanation, which must be considered supple- mentary to my former paper, I have now some additional remarks to make on vegetable cell development. The basis of a cellular structure in its first stage,—consist- ing of a membranous sac filled with an uniform plasma, or mass of formative material,—may be termed by some, “ the primordial cell ;” but in my view improperly, for the external membrane is merely protective, it exerts no active influence upon, and is unconnected with the subdivision, or cellulation of the contents, and, taken as a whole, has none of the func- tions of an individual cell.* Now we have here a vesicle filled with formative material, ready to break up into a group of cells. Those who have examined for themselves with the requisite degree of care must recognize a simultaneous development,t numerous rudi- * When the cuticular envelope, containing the uniform plasma, is ruptured under water, the protoplasm sometimes escapes as a globule, which speedily becomes filled with vacuoles. ‘These rapidly enlarge and increase in number, till the whole becomes spread out and diffused in the fluid. The tunic, or envelope of young cells, does not at first, in all cases, possess an uniformity of surface; for, in many plants it is spinous, or covered with tubercules, at its earliest. stage ; these are the rudiments of hairs. It is remarkable at what an early - period they are perfectly deve- loped, even before a definite or complete cellulation of the plasma, that they have sprung from, has taken place; some of the hairs being already jointed, and showing sap-currents in their cells. + When the bark is stripped’ from the growing branches of exogenous plants, early in the spring, the surface of the wood is covered with a slimy WenuaM, on the Vegetable Cell. 63 mentary cell-cavities appearing spontaneously throughout the mass at the same time, and increasing independently of each other; in every one the inner lining of each space in the formative protoplasm becoming hardened into a membranous layer, which may be readily proved, as the unconnected cell- sacs can be washed out of the containing plasma and isolated. The ‘ vacuoles” are rather apt to take their rise from the larger particles contained in the plasma, but I believe that this is only a mechanical and not a vital condition, for it is equally certain that a large number of them form themselves apparently without any starting point whatever. In Anacharis, and many other plants, these cells, in the first stage of their existence, are simple membranous sacs, containing nothing else but a limpid, watery fluid, and a few very minute granu- lar bodies adhering to the cell-wall—and here is a point at issue. It is maintained that cells, even in their very earliest stage, contain an active nitrogenous layer lining the interior of their cavities—the so-termed “ primordial utricle.’ My own observations cannot confirm this; and, indeed, reasoning independently of the evidence of eye-sight, it seems an anomaly to expect a detached portion of a material to be enveloped in a cavity of its own substance, before any limitary membrane is completely formed to prevent their coalescence. Neither can it be set down as a general rule, that new cells are commenced singly around a collection of solid contents, for *‘ vacuoles” are to be seen of the minutest size, which are afterwards expanded, so as to become perfect cells in all respects; unless in this case it is assumed that the formation takes place around invisible contents. As I have before stated, it is not until the rmeHAbIRTD of the sac is completely formed, that protoplasm is found within the cell; this is rapidly followed by the deposit of internal film of protoplasm, in a free state; if this is scraped off it will be found to contain transitional cambium cells, dotted ducts, &c., in all stages of development. The formative plasma is mostly deposited in the form of strips, in the grooved surfaces of the bark and wood, and there rapidly resolves itself into a row of cells, or hardens into a fibr e, according to the influences of local conditions, or ‘the size of the matrix. These cells are not formed by the division of older ones, but arise directly from the simultaneous cellulation of the formative plasma, in the manner that I have explained in other instances. From the light colour of the substance it is a difficult matter to investi- gate the young cellular deposit, as an opaque object ; but after the surface has dried, an impression may be taken with black sealing-wax, which will also sometimes bring away some of the young cells in course of formation, and afford a more satisfactory view of the cell stages and arrangement, using a Leiberkuhn for illumination. 64 Wenuam, on the Vegetuble Cell. secondary layers, and the appearance of other constituents, as starch, chlorophyll, &c. The sooner the term ‘ primordial utricle,” as applied to the active nitrogenous Jluid, or protoplasm, flowing round the interior ofthe cell-cavities, is discarded the better, for a clear understanding of its all-important properties as the formative principle. If even a viscid fluid can be endowed with the properties of a membrane, it is not at all times so in this case, as it frequently collects in the form of clots, or nuclei (as some might term them); thus changing its name and appearance perhaps several times during the course of a day. The specimens drawn for illustrating my last paper origin- ated in a plasma so homogeneous and free from all extraneous matters, that the cell-cavities were clear from first contents ; in fact, this is mostly the case with Anacharis and some other aquatic plants ; the cellulation occurring in a mass of proto- plasm nearly pure ; but this is not so in other instances. What I have already said of cellular formation might serve as a guide to the principle to which my investigations have led me, but it may now be proper to notice some frequent variations, which at first sight might not appear reconcilable to my views: I refer to tissues originating in a mass of cells, not hollow at their commencement, but with their cavities completely filled with contents (and hence I have always hesitated in making use of the general term “ vacuoles”). This condition is easily observable in some leaves and germi. nating seeds, where the formative substance contains a larger quantity of extraneous matter; under such circumstances the process of cellulation is in no way different, for relieving the mind from the task of attempting to reconcile the theory of the subdivision of an unity (and the relationship of “ mother and daughter cells”), and admitting the principle of a simulta- neous development of cells, the denser granulated material of the original plasma, in its first stage of cellulation, is shown to arrange itself in the form of irregular squares, trapeziums, or oblong figures, partitioned off by thick divisions of more transparency and consistency. This is the true protoplasm, which has separated from its solid admixtures, or expanded from centres, as it were, to form the cell walls, a process to which Dr. Carpenter has so appropriately applied the term ‘¢ differentiation ;”’* but it must not be supposed that these * This term is also explanatory of the formation of the simplest types of shell, which have arisen from a plasma containing calcareous matter. The “sarcode” (analogous in vital properties to vegetable protoplasm) having separated into somewhat irregular divisions, and formed a mem- brane between the nucleated and consolidated calcareous matter, producing a rude cellular structure. In some more perfect developments of shell Wenuam, on the Vegetable Cell. 65 rudimentary walls, or rather septa, become one uniform and continuous solid—the true cell wall is still formed in the interior of each cavity, with the appearance of being moulded upon the mass of contents, and when the membrane has acquired consistency, the proper cell constituents arise within, from external absorption as in former instances. The cells may now be washed out from the intervening plasma in which they are imbedded, as separate sacs just in the same way as | have described before. The expanding action of the living protoplasm, may be seen in actual operation during the conjugation of the Desmidiee—a process that Ihave always watched, with never- failing interest. When the two masses of endochrome are ejected, they are not bounded by any limitary membrane as some seem to suppose, but unite at first oftentimes in the form of a rugged mass. All the intervening protoplasm now separates from the general mixture, and forms an external sheath, which hardens into a membrane—the cell wall of the unicellular sporangium.* I bring this forward again, because the expansive effect of the protoplasm, as seen to take place here, will illustrate the action in the associated cells in question, when filled with contents, by considering each cell in the formative plasma for the time being, as a separate and independent organ. If now one system of cells are first formed with empty cavities, and another with more or less of primary contents, the question arises, what ought to be the physiological differ- ence in favour of the subsequent vital welfare and develop- ment of the latter? As far as my investigations have gone I cannot say that the full cells appear to differ much in growth, or derive after benefit from the circumstance of their first replete condition, the well-doing of the cell still depending upon external conditions ; but without going so far as to state structure, there seems to be a beautiful combination of this vital action, in conjunction with definite chemical arrangement, or a crystallization of the calcareous deposit, giving rise to very regular and perfect cellular forms, and prismatic structures. It would be a very interesting inquiry to ascer- tain how far these two forces act together in harmony, in forming regular cell arrangements in other departments of the animal and vesetable king- dom. ‘This would be an investigation in which the polariscope would be extremely serviceable. * In some of the Desmidiece and Algce, when the endochrome or con- tents of one cell are forced out, by the application of gentle pressure, into the water, the first action is somewhat similar to that which takes place during conjugation. The protoplasm separates from the other consti- tuents, and is determined outwards as a complete envelope, the mass ac- quires a spherical shape, and remains so for many hours, but no consis- tent exterior membrane is ultimately formed ; all vital action ceasing at this point, the mass always proving barren. 66 Wenuaw, on the Vegetable Cell. that the primary contents are useless for the purposes of nutrition, | will merely mention that some recent and most valuable practical researches, made by an independent ob- server (and which [ trust he will shortly bring before the public), have proved that extraneous matters may be conveyed into the mass of the formative plasma, and substituted for the contents of the primary cells, without interfering’ with the growth, and of such a nature as to afford no nutriment to their tissues. In conclusion I beg to inform the Society, that though the microscope has led me to take up particular views of cell development, | do not profess to write a complete essay on the subject. 1 will, however, remark, that it is still quite a new field for investigation, for all the controversies and con- tending theories that for years past have appeared on this theme have done but little towards the enunciation of a simple system of laws. As cell formation undoubtedly takes. place, in various grades of complexity, the lowest and highest being widely different in their mode of production, in order to simplify this most important branch of science, I would venture to suggest, with all due deference, the possibility of classifying the subject, by arranging it in heads or depart- ments, or to make myself understood, say as follows :— 1. Spontaneous appearance of membranous cavities in a primitive plasma, or simple differentiation. 2. Cell formation by self-division, or the conjunction of definite membranes or utricles. 3. Cells requiring special organs for their production. 4, Allied phenomena, &c. If this were accomplished it would save some amount of confusion; much of what is already known might be arranged under such heads as these. In the most highly organised plants, it is probable, that all these modes of cell formation separately exist, in varlous organisms. It is to after influences, or vascular bundles arising from the parent stem, that the proportions of symmetry and form are conveyed to the embryo cellular mass, dividing, distribut- ing, or increasing it according to its destined condition. At the time that these vessels and ducts begin to force their way through the young assemblage of cells, these differ so much in both individual form and arrangement, as to be typical in nearly all cases of the most excessive irregularity (the embryo leaves of the vine may be taken as an average example), and is utterly irreconcilable with the idea that the cavities or cells originate from the regular division and subdivision of pri- mordial cells. TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE I., Vou. IV. Illustrating Mr, Wenham’s Paper on the Vegetable Cell. Fig. 1.—End of stalk of Anacharis alsinastrum. 6, b. Germs of future leaves. 2.—Primitive cell-formation of leaf of Anacharis. 3o.—Primitive cell-formation of Arabis albida, with the rudiments of cells appearing at the apex. 4.—Leaflet of Arabis, with cells in a more advanced stage. 5.—Malformed stellate hair with the protoplasm at the apex, showing a tendency to cell-formation. 6.—Leaflet of Reseda burst at the apex. The exuded mass of protoplasm having become filled with cavities. 7.—Primitive cell-formation of leaf of Anethum Feniculum. 8.—Cells of Anacharis in succeeding stage to Fig. 2. 9,—Cells of Anacharis in more advanced stage. a. a. Septa of protoplasm dividing cells too much elongated into two parts. 10.—Cell excessively elongated with an intermediate mass of protoplasm, a. Cavity formed in protoplasm which expands and divides the original cell-space into three parts. 11.—Cells of Anacharis in latest stage of growth. 12.—Group of embryo flowers of Arabis albida. a. b. c. d.e. f. g. Succes- sive stages of development. h. Cell prolongations or rudiments of stellate hairs. es ee E Reet Lf Frans Mio he Vd MAL FHW del. Taffen West sc Ford & West Imp. N & Ss, Pe Prices H " sie, ‘ ’ 4 - 0% \ ) 5 ay > ~~ "\ a 1 om ( ry oT sy ‘ ' i eis Beer grees ay) ae Tale a nae TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE IV., Illustrating Professor Henfrey’s paper on some Fresh-water Con- fervoid Algee, new to Britain. Bye Figs, 1—25, Pandorina Morum, Ebr. Fig. & 1 —Perfect form, with 16 gonidia, side view. 2.—Ditto, polar view. 3.—Perfect form, with 32 gonidia, side view. 4,—Ditto, polar view. 5.—A gonidium, side view. 6.—Ditto, from above. 7 and 8.—Side and end view of a small onc with 16 gonidia. 9.—Side view of a small frond, with 32 gonidia. 10.—A frond, with the gonidia dividing. i1.—A more advanced frond. 12.—A frond, with the young ones nearly perfect. 13 and 14.—Young fronds free. 15 to 20.—Side and end views of fronds, with the gonidia pushed close together. 21.—Side of a frond, like fig. 15, with the gonidia encysted, their contents turned red, and the gelatinous envelope nearly dissolved. 22.—HEind view of the same. 23.—Side view of one with 32 gonidia, more magnified. 24.—Resting-spores (encysted gonidia) free. 25.—One more magnified, to show the membranous coat. Figs. 26 and 27, Apiocystis Brauniana, Nageli. 26.—A half-grown frond. 27.—Green conidia from the interior, the lower ones dividing. Figs. 28—36, Clathrocystis ceruginosa, Henfrey. 28 to 31.—Successive stages of development of a frond. 32 to 834.—Fragments of a broken-up frond, like fig. 31. 35.—Green cells from the interior of the ‘gelatinous fronds, some under- going division. 36.— One more peemicd, to show the membranous coat. : Fran Micr ec VA. GUM. AUenfrey adnat. Tuffen West sc. WWest chromo Imp. ‘ » é 4 : ? ‘ . ree : os 4 a 2 j ” ‘ ‘ ( . ; Py Rs z oun wk 4! : + ‘ pa 2 A \ mo 5 i ad rh TRANSACTIONS OF MICROSCOPICAL SOCIETY. DESCRIPTION OF PLATE V., Illustrating Dr. Gregory’s paper on the Glenshira Sand. Fig. 1.—WNavicula rhombica, n. sp. A frequent variety ; 8. V. *— ,, sy Front view, showing several grouped in a pack. 2.—N. maxima, n.sp. 2*.—Ditto, narrow variety. 2**.—Intermediate form of NV. maxima. 3.—LN. Hennedyi, Sm. (Not figured in Synopsis, vol. ii.) 4.—N. latissima, n. sp. 4*.—Ditto, longer variety. 5.—WN. quadrata, n. sp. (= N. humerosa, Bréb.) 6.—. formosa, n. sp. 7.—N. pulchra, n. sp. 8.—N. angulosa, n. sp. 8*.— 6 B. 9.—N. Macula, n. sp. 10.—W. solaris, n. sp. 2 figures. 11.—WN. ? Pandura, Bréb, (?). 12.—N. ? nitida, Sm. 12*.— ? 13.—WN, incurvata, n. sp. 14.—N. splendida, un. sp. 15.—WN. didyma, y. Costate striz. 16.— - , 5. A new variety. 17.—N. clavata, n. sp. 18.—Pinnularia longa, 0. sp. 19.—P. fortis, n. sp. 20.—P. inflexa, n. sp. 21.—P. acutiuscula, n. sp. 22.—P. Hrgadensis, n. sp. 23.— Stwuroneis amphioxys, ni. sp. The figures in this plate represent, for the most part, full-sized or large individuals under a power of 400 diameters. No. 9, Navicula Macula, is represented under a somewhat higher power; but I believe there are individuals of equal size under 400 diameters. ’ The remainder of the new forms which I have described in the Glenshira Sand, and several of which are very curious, will be figured in the next Number of the Journal. Wa A = RC EIEIO C((\\ | svi ALD 0. SSW SS ; 3 SLUG ETA LY PIR a : CU | i, di eG 2 : PPPeESEEL TES : ahh < YY ANY me eats ct | RY 2 Ld Mla Z WM 0 ig \' Ct, TOO WT TI LUM MM NWN AE AA =raoth DANN WW TM mal a) Ford & West Teap DY Grealle del. Tiffen West sculp, s tant INDEX TO TRANSACTIONS. VOLUME IV. A. . Address of the President of the Microscopical Society, 17. Algee new to Britain, 49, ‘iB. Beale, Lionel, M.B., on a simple form of portable microscope, with lever adjustment, 13. C. Cell, vegetable, Mr. Wenham on, 60. -" D. Diatomaceous sand of Glenshira, 35. G. Greville, Dr. R. K., drawings of dia- tomacee, 35, Gregory, Dr. W., on the post- tertiary diatomaceous sand of Glenshira, 35. Glenshira, diatomaceous sand of, 35. H. Henfrey, Arthur, Notes on some fresh-water Confervoid Algee, new to Britain, 49. 16 Illuminating opaque objects, Mr. Wenham, on, 55, M, Microscope, portable, on a simple form, with lever adjustment. By Lionel Beale, M.B., 13. Microscopical Society, Address of the President, 17. - Report of the Sixteenth Annual Meeting of the, 15. R. Report of the Sixteenth Annual Meeting of the Microscopical So- ciety, 15. S. Sand, diatomaceous, of Glenshira, 35. WV. . Vegetable cell, on the formation and development of the; By F. H. Wenham, 1. W. Wenham, F. H., on the formation and development of the vegetable cell, 1. ‘s oa on a method of illuminating opaque objects, 55. si ea on the vegetable cell, 60. ' LONDON: PRINTED BY WILLIAM CLOWES AND SONS, STAMFORD STREET AND CHARING CROSS, AS vs) PORES Pp ys beag re : , NY ve ve rw j ! 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