- — Fao a a b - ee CED idee ‘D a eae ae Dw 3 Jamas BES), Zae ; =< y Scptenrb {399 bess e Fi — - - 4 - £& a = = * > <. all - J - i - 7 “es oe . ; * 4 i > . be Z Re » : + . : ae - ae 5 oa ie 4 , ’ “a = 5 c 7 " t a a. : ; es Poa : a" ae Fy 7 ’ sy a E We 7 é : ¢ ~ , a, - ~ — : 7 s . 7 =a = aL a ' a : be e — : 7 5 < P- ab di « r - 7 : vat . THE MONTHLY MICROSCOPICAL JOURNAL: TRANSACTIONS OF THE ROYAL MICROSCOPICAL SOCIETY, AND RECORD OF HISTOLOGICAL RESEARCH AT HOME AND ABROAD. EDITED BY HENRY LAWSON, M._D., M.R.C.P., F.R.MS., Assistant Physician to, and Lecturer on Physiology in, St. Mary’s Hospital. VOLUME XVII. 1B RAR gs we REW YORK BOTANICAL ~ Carpe’ LONDON: HARDWICKE ann BOGUE, 192, PICCADILLY, W. MDCCCLXXVII, The MonthlyMicroscopieal Journal.Jan.1.1 877. bs & CLXV. Foams vt ietilt (EEL ANN ———————— EO W West& Co lithe. Identity of N.crassinervis. F. Saxonica and N rhomboides. q = = _ a fo The Monthly Microscopical Journal.Jan.1.1377. Pl Cis ee i ee a GS ay oy a =. nn . E . | W.HDoallinger dd ad nat. 7 WWest& Co. ith. © Identity of N .crassinervis. F Saxonica and N rhomboides. RA Vie eR > REW YORK THE BOTANICAL MONTHLY MICROSCOPICAL JOBRNAL. JANUARY 1, 1877. ” I.—On “ Navicula crassinervis,” “ Frustulia Saxonica,” and Navicula rhomboides, as Test-objects. By Rev. W. H. Datiincer, V.P.R.M.S. (Read before the Royvau Microscopican Society, December 6, 1876.) Puates CLXV. anp CLXVI. Amonest competent authorities there appears to be no longer any dispute as to the true relations of the diatoms that have hitherto received the separate designations in the above title. Professor H. L. Smith of America, and Mr. Kitton of our own country, doubtless two of the most competent living authorities, are agreed that they are but three names for the same species ; for both “ N. crassinervis” and “ F'. Saxonica” have no real existence, being but forms of NV. rhomboides.* But the vicissitudes through which opinion and conviction have passed, in less than two years, as precursive of this valuable conclusion, are interesting. In May, 1875, Mr. Hickie, without the slightest doubt, declared F. Saxonica and N. crassinervis to be distinct species; and his conviction was reached not hastily, but after a study of the literature of the subject, after a careful investigation of his own collection of F. Sazxonicas, which was “a pretty extensive one,” and after ex- amining it, as a form properly entitled to its name, in company with Dr. Rabenhorst, “ both the discoverer and namer of the diatom in question.” + Besides which, he gives evidence, then clearly satisfactory to his own mind, that these three diatoms must be different, from the fact that to properly resolve them, they must be each placed differently in relation to the source of light.t But the great end he had in view was, to correct what he held to be a misconception on the part of Dr. Woodward as to the exist- — ence of longitudinal strie on “F'. Saxonica”; which Dr. Woodward © considered to be illusory, and which Mr. Hickie declared to be Le real; and the reality of which he contended was not only assured r+ by the evidence he brought, but by their having been perfectly i photographed by Herr Seibert. c» Lo this, with his usual thoroughness, and the aid of his match- Lu] CG * ‘M.M. J? vol. xv. pp. 278-281. + Ibid. vol. xiv. p. 33. t Ibid. p. 35. VOL. XVII. B 2 Transactions of the Royal Microscopical Society. less skill in micro-photography, Dr. Woodward replied ;* reaffirming his conviction that the “longitudinal strie of Dippel,’ and, in addition, those announced to have been seen by Mr. Hickie, were due to diffraction and interference; the spurious lines produced by which, he declared and proved, could be as readily photographed as real ones. Some beautiful photographs in support of this were sent ; and certainly to the skilled observer there can be no question that in the case of the frustules photographed by Dr. Woodward (and excellently reproduced in this Journal +) the lines photographed are spurious. Further, whoever has taken note of Dr. Wood- ward’s skill in manipulating test and other difficult objects, will want no assurance, that in reference to the frustules in the photo- graphs, if they could not be developed by Dr, Woodward, the probability is that they could not be developed at all. But this observer adds a note of extreme significance in this relation ; for he says, “ At the same time I shall be very glad if he (Mr. Hickie) can convince me, by satisfactory evidence, that this belief is erroneous, for analogy inclines me towards the opinion that in both Frustulia Saxonica and Amphiplewra pellucida the striz are really rows of beads, as is so easily to be seen in Navicula rhomboides, and that consequently we ought to be able to see longitudinal strize when the illuminating pencil has the proper direction, if only our glasses had the requisite defining power.” The italics are mine, but they show the sound and unbiassed view of the writer. A rejoinder is now given by Mr. Hickie.} In this occurs a letter from Dr. Rabenhorst, declaring the longitudinal striz of F, Saxonica to be real, and affirming that “if Dr. Woodward main- tains that Frustulia Saxonica is identical with Navicula eras- sinervis we must suppose that he is ignorant of one or other of them.” At the same time Herr Seibert’s photographs of the longitudinal as well as the transverse striz of a reputed “ #. Saa- onica” were presented to this Society for inspection. At the discussion which followed the reading of this paper it was affirmed that the photographs were simply indistinguishable from “ coarse Rhomboides,’ § and in both the paper and the discussion Mr. Hickie retracted “a previous erroneous statement,” and confessed that he was unable to ‘‘ state where Frustulia Saxonica ends and ‘ small’ Rhomboides begins.” || They were in fact identical. But he still maintained that ‘‘there was a very great difference between them and Crassinervis.” 4] After this, in a subsequent paper,** Dr. Woodward definitely proved that Herr Seibert’s photograph, purporting to be “ F. Saa- * ‘M. M. J.’ vol. xiv. pp, 274-281. f Ibid. + Ibid. vol. xy. p. 122. § [bid. vol. xv. p. 103, || Ibid. p. 127. | Ibid. p, 104. ** Thid. p. 209. On “ Navicula crassinervis,” &e. By W. H. Dallinger. 3 onica,” was, what it had been by some competent judges affirmed to be, ‘a coarse form of Rhomboides.”’ Mr. Charles Stodder then adds a concise note,* giving reason and authority for believing that both N. crassinervis and F. Sawonica are but forms of N. rhomb- otdes; and Dr. H. L. Smith’s most valuable and conclusive letter follows ;¢ and in this it is shown that not only is there identity between the three diatoms in question, but that all important authorities, Rabenhorst excepted, are agreed in the admission of that identity. To this letter Mr. F. Kitton, who had been requested by Professor H. L. Smith to revise the proofs, takes the opportunity of stating that he fully agrees “that the genus Frustulia should be abolished ;” and he is also of opinion “that Navicula cras- sinervis 1s only a form of N. rhomboides.” He adds, “ I may also state that my friend Mr. Hickie is of the same opinion.” Clearly therefore Mr. Hickie’s conviction of the “very great dif- ference” existing between N. rhomboides (into which F. Saxonica had now been fused) had been overcome. The reasonings or facts which accomplished this in Mr. Hickie’s case are not given us; but his frankness and candour are sufficient evidence of the scientific spirit in which his inquiries were conducted. So far, it is clear, that these three diatoms are, on the best authority, accepted as mere conditions of the one form, N. rhomb- otdes. ‘The reasons for this decision have relation to morphology and development, quite as much as to the characteristics of the silicious skeleton with which the microscopist is more generally concerned. With the former of these reasons I may not concern myself, but receive them thankfully from competent authority. But with the latter facts I will venture briefly to deal. Nothing up to this time is finally before us, as to what kind of “resolution ” these various conditions of Rhomboides may be expected to yield, or what their real value, as tests, is. My first acquaintance with this diatom was made some eight or nine years since. It had lain in my cabinet for some years before this: but some exquisite specimens prepared and mounted by L. Hardman, Esq., were courteously given me by him, and I did my best at that time with them. They were what I presume have been called ‘‘ small Lhomboides” ; for the largest of them taxed the power I then possessed, to develop their transverse striz sharply and well, with a good English 1th, and the smaller of them were so fine, as to resist all the manipulative skill I then possessed with a ysth, and some of the minute ones, even with Powell and Lealand’s y';th (dry). Coming from so excellent an authority on diatoms as Mr. Hardman, I accepted these as normal specimens of the species ; and as my manipulative skill increased with practice, and my * “M.M. J? vol. xv. p. 265. + Ibid. p. 279. B 2 4 Transactions of the Royal Microscopical Society. battery of lenses became improved, I was enabled to resolve into hemispheres all the larger, and most of the medium-sized ones, and eventually to consider myself master of the resolution of this diatom ; a work which I accomplished not for its own sake, but merely to have a given set of marked tests, of known value to myself, for the sake of future comparison. When therefore the value of “ F. Saxonica,” as a test for high powers, was announced, I proceeded at once to procure it. My first specimens were got from London ; but to my surprise the forms sent under this name were neither more nor less than the medium-sized frustules of my now well-worked specimens of N. rhomboides. I of course con- cluded that there was an error in naming, and at once wrote off to two other sources for the form I required. ‘To my great vexation, these were merely repetitions of what I had received before, one of them containing really coarser specimens than any I could find on Mr. Hardman’s slides of N. rhomboides. Determined to obtain the right frustules, I wrote to an English friend, then in Germany, — and was favoured with specimens, slightly smaller, but in every sense identical with those supplied from English sources. I failed to discover a single difference between them. I could striate, or resolve them into dots, precisely as I did my N. rhomboides. Their midribs—a very characteristic feature—were precisely like Rhomb- oides, and their general contour varied, as N. rhomboides varies, some frustules having an inclination to an obtuse angle in the centre of the margin, while others preserve in their margin a continuous curve. I had never made the natural history of diatoms a study; so the inference I was obliged to make was, that there must be some morphological or developmental difference between these diatoms which justified the difference of name: but as tests I determined that there was certainly no difference between them. When I first obtained N. crassinervis, my difficulty was almost as great; for although the frustules on the slides so named were certainly much smaller than the majority of frustules on my speci- mens of Lhomboides, still I could find some almost, if not quite, as small; and I could detect, in an examination of a number of specimens, nothing that had not its complete equivalent in the frustules of Rhomboides. I felt therefore bound to conclude that, as test-objects, these three separately named diatoms were merely Rhomboides of various sizes, and therefore, generally speaking, of greater or less difficulty in “ resolution.” I reached this conclusion nearly three years since, but as it was an opinion formed on the silicious frustules alone, and had no connection with the natural history of the form, I merely set it aside for what I considered it worth. But as competent authorities have now—fully knowing the nature of the plant—determined that the three forms in On “ Navicula erassinervis,’ &e. By W. H. Dallinger. 5 question are but conditions of the one form (Ahombozdes), it appears to me that some interest attaches to the fact that proofs of this may be obtained by a serial study of the silicious frustules, from the smallest or most dwarfed, to the largest or most developed ; and that such a study brings out plainly what value should be attached to this diatom as a test-object. I have now a very considerable collection of these forms, gathered from many sources, and through the courtesy of many friends; but I rarely find, amongst the very finest and minutest of them, any frustules that will not yield complete resolution into hemispheres, with Powell and Lealand’s “new formula” }-inch objective (immersion), with one or other of the methods of illu- mination I now employ; using as the source of light a broad- wicked paraffin lamp with the flame turned edgeways to the con- denser. Unfortunately time has never been sufficiently at my disposal, to enable me to make micro-photography my servant in study. But as the objects I have concerned myself with during the greater part of my life as a microscopist, have been swiftly moving vital ones, in the portrayal of which even photography could have been of no service, I have been obliged for some years to cultivate, with as much care as I could exercise, an accurate and delicate use of the pencil, in fixing permanently the images of objects which the microscope revealed. I believe in this instance its aid may be called in with some service. Having satisfied myself of the absolute similarity, in ultimate structure, of all the modifications of what we shall hereafter know as N. rhomboides, it appeared to me advisable to take one of the smallest of the forms hitherto labelled “ N. crassinervis,” and find the least magnifying power that would perfectly resolve it, and then employ the same power, and the same mode of illumination, on a series of the increasingly larger forms, until the extremely coarse ones were reached. In this way the identity of the ultimate structure in every developmental condition would be seen. The power necessary to resolve completely the smaller forms of the “ N. crassinervis” in my cabinet was 800 diameters (obtained with the }th above referred to). The figure marked A, Plate CLXV., represents the result. The brilliant definition obtained by the lens, rendered much more apparent the “resolution” than the most delicate drawing or photograph could do; but the drawing given is a careful rendering of the effect. It will be seen that some portion of the striae (transverse) are seen on the left-hand side of the midrib: but they are seen perfectly on the right-hand side; and in the upper half of it, resolution into dots, or hemispheres, placed in rectangular rows, is, in a good light, clearly visible. Of course, it is not pretended that enumeration of striz, and so forth, could be effected from this or the following drawings, as 6 Transactions of the Royal Microscopical Society. from a photograph. But they accurately represent the general facts. I next took a frustule of the same (reputed) form (“ N. crass¢- nervis”) which was of an average size, and placed it under the same lens, with the same illumination. The result is given at B, which represents the frustule magnified as before—800 diameters. Precisely the same “resolution” is given; but faint longitudinal lines are seen, in addition to the far more plainly visible hemispheres, placed precisely as in A. An average specimen of what was then labelled “ F’. Sawonica,” was now made to replace the above, all the conditions remaining intact. The drawing C, magnified 800 diameters, represents the result.. I have obtained more general “ resolution” into hemi- spheres than is here shown; but the specimen is typical, and I preferred to retain it. Transverse striz will be seen to be uni- versal; longitudinal striz are here and there faintly visible, and the rectangular rows of hemispheres are unmistakably manifest. Finally, a fair specimen of what I had long known as N. rhomb- oides was placed on the stage of the instrument, and, everything remaining as before, was examined. The result — magnified as before—is given at D. What was now aimed at was not to get the largest surface of hemispheres, but to get such a general result as would show the exact correspondence, in ultimate structure, of the preceding forms with this. The transverse striz, the longitu- dinal striz, and the rectangularly placed rows of hemispheres, are all most distinctly seen. But during the last three years some remarkable specimens of Rhomboides have come into my hands—specimens in which the frustules reach an immense proportional development ; and in which the striz, or rows of hemispheres, are very much coarser in rela- tion to Mr. Hardman’s coarsest frustules than the -latter are in relation to the finest and smallest of the forms so recently called “ N. crassinervis.” The largest of these have been found by me in some mountings received from a friend, and marked as having come from “Cherryfield, America.” The variation in their sizes, on the same slide, is very great, and the consequent difficulty of resolution ; but I selected one of the larger forms, and employing the same illumination as in the instances given above, put on the 4th immersion of Powell and Lealand (new formula) in place of the 4th, and worked up to 600 diameters. The result is given at E, Plate CLXYVI., which may be taken at once as the interpreter of all the rest, and the witness of their oneness. The striation in this case is every- where resolved into rows of hemispheres, placed in rectangular order ; and I know of few more beautiful objects in “still” micro- scopy than this. The frustule is of exquisitely perfect form, slightly tinted with yellow-brown : the hemispheres are everywhere On “ Navicula crassinervis,” &e. By W. H. Dallinger. 7 sharply and clearly separate, and the continuity of this is unbroken from end to end. If this form be studied with a good } (dry) of an angle of aperture of about 95°, and if the stage of the microscope be moderately thin, and all sub-stage gear be taken away, and the light from a good lamp condensed by a “ bull’s-eye” of about 5-inch focus be sent in at an angle of about 30° with the under surface of the slide, and the image of the flame be focussed on the centre of the object, this specimen of Rhomboides can be exquisitely resolved, on a black ground, with a third, or even a fourth eye- piece; the frustule itself, especially if seen amongst brilliantly white diatoms, assumes a pale sapphire tint, and the hemispheres with skilful management are beautifully developed. Taking these facts together, then, and guided by the decision announced by Professor H. L. Smith and Mr. Kitton, we may safely conclude that N. rhomboides is a diatom very permanent in its general form and characteristics, but eatremely variable in its size, and the tenwty of the ultimate structure of its silictous Srustules. But from this, a corollary inevitably follows. N. rhomboides ig a most uncertain and unreliable test. Unless the same mount- ing, and in many instances the same frustule, be used, in testing the capacity of a given lens, the most incongruous issues may result. To be told that a certain glass will resolve “ N. rhomb- oides,” may mean that it will resolve E, Plate CLXVL., or that it will resolve A, Plate CLX V.—quite a different result, and no guide as to whether A’s or B’s lens 1s better or worse than mine of the same power, unless the same slide of frustules be employed. To those accustomed to the use and comparison of diatomaceous test-objects for practical purposes, this is no new inference, as Mr. Kitton has recently so profitably told us.* But it is so palpable an instance that it may carry conviction. DESCRIPTION OF PLATES CLXY. AND CLXVI. Fig. A.—WNavicula crassinervis x 800 diameters, showing rectangularly placed hemispheres. B.—Ditto, ditto, a larger form similarly magnified. C.—Frustulia Saxonica, magnified by the same power, and showing similar structure. D.—A small form of N. rhomboides, also magnified 800 diameters, revealing the same structure. : E. —-A very large form of NV. rhomboides from “ Cherryfield,’ America, showing a corresponding structure, with a magnification of 600 diameters. * of an inch in diameter, and when more than yoyo we usually obtain the faint reds and greens of high orders or merely white light, distinguished from the bluish white of the first order by not giving the comple- mentary brown. When examined in water all doubt can be re- moved by observing the action of dilute hydrochloric acid, which dissolves calcite and arragonite with effervescence, and leaves quartz and many other minerals unchanged. Mica.—tThis is best recognized by its occurring as thin plates haying a laminar structure. When in water or mounted in balsam the flat surfaces lie parallel to the supporting glass, and it may be somewhat difficult to appreciate their thickness and to distinguish them from flat plates of quartz. If they cannot be made to turn round, so that their edges may ‘be seen, the only course that can be adopted is to illuminate carefully and observe the efiects of slight changes in focal adjustment, which may suffice to prove that the fragments are flat and have a laminar structure, with no cleavage in any other direction. The occurrence of small granules or crystals of red oxide of iron between the lamin may sometimes greatly assist in forming a satisfactory conclusion, since a perfectly flat thin layer of any such material is not at all likely to occur in quartz. Advantage may also be taken of the difference in refractive power, as described below when treating on glassy felspar. Hornblende, &e.—What I have said when describing the horn- blende and schorl in decomposed rocks will, I think, sufficiently explain the methods I have employed in identifying them in deposits. Perhaps the most decided difference between coloured hornblende and schorl is the intense dichroism of the latter, so that in certain positions no light passes through it. Felspars.—As a general rule the difference between the felspars in granitic and in volcanic rocks is so great that it may be con- venient to consider them separately. Those in granitic rocks are almost or quite free from cavities, or at most contains only a few fluid cavities, whereas the glassy sanidin of volcanic rocks often con- tains many well-marked glass cavities. It also differs greatly from other felspars in various ways. Thus, whilst the orthoclase oj L 2 130 Transactions of the Royal Microscopical Society. granitic rocks shows with polarized light coloured bands due to twin plates, and abite, oligoclase, and labradorite give more or less well-marked evidence of their cleavage, the sanidin of modern voleanic rocks often occurs as clear transparent fragments, having a simple optical structure, and showing no more lines of cleavage than a piece of glass. On the whole, fragments of unaltered felspar constitute but a very small part of our British stratified rocks, and glassy felspar is probably almost or quite absent; but when we come to study the modern deposits formed at great depths in the Atlantic and Pacific oceans, we find that it plays a most important part. For some time I feared that no ready means could be discovered to distinguish between it and quartz. Both break up into irregular transparent fragments, having a vitreous fracture, and, when of the same size, give with polarized light the same tints, so that these minerals cannot be distinguished by that means. At length, however, it occurred to me that perhaps there might be sufficient difference in their refractive power to cause them to appear different with suitable illumination. As previously named, the refractive power of quartz is almost absolutely the same as that of moderately fresh Canada balsam, but I find that it is decidedly less than that of very hard balsam. On the contrary, the refractive power of glassy felspar is equal to that of this very hard balsam, and greater than that of new and soft. Hence when both minerals are mounted in soft balsam, transmitted light passes so evenly through the quartz as to show little or no dark outline, whereas in passing through the glassy felspar it is somewhat bent, and if the apertures of both the condenser and object-glass are sufficiently small, the fragments show a dark outline. The difference is, however, scarcely so well marked as is desirable, and it is therefore better to make use of a different illumination. By using a condenser with a central stop, so as to get a black background, the oblique rays pass through the quartz without there being any light reflected, and the outline is invisible, or only shown by means of any superficial coating of some other material which may be present. There is, however, seldom any difficulty in distinguishing this from true surface reflexion. On the contrary, the glassy felspar having a somewhat higher refractive power than the soft balsam, reflects part of the light, and causes the fragment to show a well-marked bright outline. As far as I have been able to judge, this method gives satisfactory results, which are confirmed by other facts. Thus, for example, on examining some of the sandy matter washed from the deep ocean clays brought back by the ‘ Challenger,’ I came to the conclusion that certain particles were quartz and others glassy felspar, and on examining these with a much higher power I saw that what Anniversary Address of the President, H. C. Sorby, F.RS. 131 I had thus found to be quartz contained the usual fluid cavities, with moving bubbles, whilst what I had concluded must be felspar contained the well-marked glass cavities of modern volcanic rocks. There is little chance of confounding felspar and quartz in studying British stratified rocks. The only fear is of mistaking for one another fragments of decomposed felspar and portions of stratified rocks formed of thoroughly decomposed felspar, consoli- dated after deposition as separate granules. Kaolin, &e.—The principal characters of this substance have been already described. It may in general be identified by the more or less elongated and flattened shape of the particles, and by its strong depolarizing action, which, with crossed Nicols, suffices to give a pale bluish white, even when the particles are p3}o5 of an inch in diameter. There is no chance of confounding them with minute particles of quartz, which to give such a tint must be about four times that diameter. There is also no difficulty in distin- guishing kaolin from decomposed or comminuted pumice and some other analogous modern volcanic products, since the form of these particles is very different, and they have little or no action on polarized light. There is also no difficulty in distinguishing be- tween true kaolin and the minute short needle-like crystals met with abundantly in some decomposed volcanic rocks, since their shape is so different. Application of similar Principles to thin Sections of Rocks. As an almost universal rule thin sections of stratified rocks should be cut in a plane perpendicular to the stratification. In this case the thin flat plates of quartz or mica are almost always seen in transverse section, and the fact of their being thin and flat is at once apparent. There is also little difficulty in distinguishing between the thinnest pieces of quartz and the flakes of mica. These latter are usually thinner and of more uniform thickness, and with proper illumination and a sufficiently high magnifying power the laminar structure of the mica may be easily seen. Its colour and dichroism are also important characters, and observed to the greatest advantage in transverse sections. The identification of the various other minerals may be accomplished in the manner already described, and the only point that needs special attention is the recognition of the very minute granules of kaolin or micaceous substances disseminated amongst the larger fragments, which may, however, be accomplished by carefully regulating the aperture of the condenser, which must be small. 132 Transactions of the Royal Microscopical Society. Application of the above-described Principles to Special Cases. The practical application of the general principles already explained will, I think, be more readily understood if I describe a few characteristic examples of various uatural deposits. Millstone Grit of South Yorkshire.—It would be difficult to find a better example of a coarse-grained sandstone, almost entirely derived from granite, than the above-named rock. Some of the beds can easily be broken up into loose sand, and the structure of the grains observed when mounted in balsam. With very few exceptions they are extremely angular, as shown by Fig. 13, and in every respect identical with grains of quartz derived from decomposed granite. Grains of unchanged felspar do sometimes occur, but the greater part has been decomposed into clay, which has been squeezed into the spaces between the grains of quartz. In some few cases portions of felspar may still be seen adhering to quartz, as shown by Fig. 14, which may therefore be said to be actual grains of granite. The quartz is on the whole very free from fluid cavities, and more like that from the granites of Norway than from any British variety which 1 have examined, and certainly very unlike that from the Cornish granites. These conclusions agree admirably with other facts. In the associated pebble beds portions of undoubted granite may be found. It is of coarse grain, with comparatively clear felspar, quite unlike the usual varieties met with in Scotland or Cornwall, but closely like those from Norway. ‘The current structures of the rock clearly show that the material was drifted from the north-east, and it was probably derived from granitic rocks lying at no great distance in that direction. Even the much finer grained quartzose sand beds, like the gaunister, have apparently been mainly derived from granitic rocks. We need not go far.to find the other constituents of the granite. Mica abounds in some beds, and the decomposed felspar has no doubt largely contributed to the material of the associated shales and indurated clays. Nearly all the grains of quartz are as angular as if never subjected to attrition ; but a few are so much worn that they may have had a different history— they may have been exposed longer to wear, or may have been de- rived from dunes of blown sands. Sand of the Egyptian Desert,—This is a splendid example of a sand which has been very much worn by attrition, as shown by Fig. 15, all angles being removed. Ordinary dune sand shows the same kind of wearing in a less degree. When blown about by the wind the friction of the grains one on another is necessarily much greater than when they are to a considerable extent buoyed up in water, and there is thus no difficulty in understanding Anniversary Address of the President, H. C. Sorby, F. B.S. 138 why so many have been far more worn and rounded than the grains met with in subaqueous deposits. Both in them and the sand of the Desert, other things being equal, the amount of wearing is greater in the case of the larger than in the case of the smaller grains, which is easily explained, since their weight and the amount of friction would necessarily increase in higher pro- portion than their diameters. The contrast between this sand of the Desert and equally coarse sand from the Millstone Grit is most striking, as will be seen on comparing Figs. 13 and 15, and points most clearly to a very different history, although the materiak was in both cases originally derived from granite. Sand derived from Schists—On the sides of the valley of the Tay, north of Dunkeld, occur terraces of sand at some eleva- tion above the river. This sand is fine-grained, the common size of the grains being about st> of an inch. ‘There is no difficulty whatever in seeing that a very large proportion are flat plates, either by making them turn round in water, by care- fully studying their appearance when the focus is slightly changed, or by examining their action on polarized light, when mounted in balsam. Fragments of dark green hornblende are common. Since we cannot examine sections of the mica in the proper direction, its dichroism cannot be observed, but some of the darker flakes may have been derived from granitic rocks or highly altered schists. On the whole, the microscopical characters clearly indicate that the great bulk of the deposit was derived from schists; and, considering the geological character of the surrounding country, there can be little doubt about the accuracy of this conclusion. In the neighbourhood of Moffat and of Bangor occur hard slate rocks without cleavage, which can easily be cut into thin sections perpendicular to stratification. These show alternating layers of coarser and finer grain, and of red or pale green colour. The erains of quartz sand in the coarser layers are seldom y}5 of an inch in diameter. Those of 335 to s}y are common, and many are yoyo or less. A large proportion of these are flat plates, like those derived from schists, and in some cases they enclose plates of mica parallel to their longer axis, as shown by Fig. 16, the shaded part being the mica. Such a grain may be looked upon as a fragment of mica schist. The quartz is usually broken up into such small fragments that only a few show complex structure. Well-marked grains of green hornblende occur, and a good deal of green dichroic mica. ‘There are, however, a few which are dark dichroic, and in the very fine- grained layers are many minute granules, having all the characters of those derived from felspar or other minerals of granite rocks 134 Transactions of the Royal Microscopical Society. which decompose into similar material. Taking all these facts into consideration, there can be no reasonable doubt that a very large portion of these rocks has been derived from schists, which has been deposited along with a little mica and many very fine granules, derived from perhaps more distant granitic rocks. lt appears to me scarcely necessary to describe any other special cases. As far as I have been able to ascertain from an examination of sandy deposits belonging to nearly every period of our British stratified rocks, I think we may conclude that, as a general rule, the coarser-grained sands are mainly derived from granitic, and the finer from schistose rocks; which is no doubt because the separate solid fragments of quartz in granite are usually much larger than those in schists. Even the oldest slates which I have examined thus furnish evidence of the existence of still earlier strata, subsequently metamorphosed. One thing which may appear somewhat surprising is that on the whole the grains of sand are very little worn, and hence the finer-grained sands have not resulted from the wearing down of larger grains, but consist of particles which were originally small, separated from the larger by the action of currents. That part of the quartz worn off from the rounded grains is probably met with in the clays mixed with the true kaolin. It seems scarcely possible that the larger solid grains could be reduced to smaller by simple fracture, by the action of currents. The microscopical structure of the quartz enables us to form some idea of the general character of the granitic rocks which have yielded so large a part of the coarser sands met with in British strata. They must certainly have been very unlike the Cornish granites, since the quartz of these latter contains a far greater number of fluid cavities. They must have been much more like the granites of the Scotch Highlands or those of Norway, and perhaps we should not be far wrong if we were to conclude that they be- longed to a type intermediate between these, which formerly occurred in an area now no longer dry land. The difference in the colour of different sands depends on the amount and condition of the oxide of iron, forming as it were a superficial varnish. This is easily seen when the grains are mounted in balsam. ‘The quartz itself is the same, and since the state of the oxide might be so soon changed, there is no difficulty in understanding why sands of such very different colours may be associated together. The green grains of glauconite cannot as a general rule have been derived from pre-existing rocks, and ought rather to be attributed to chemical action occurring either during or soon after deposition, like the minute crystals of gypsum met with in some of the dredgings from the Pacific Ocean. Anniversary Address of the President, H. C. Sorby, F.R.S. 135 Clays, &e.—The chief portion of the fine-grained clays cannot be distinguished from the products of the decomposition of felspars and other minerals which can be changed in a similar manner; but mixed with this is a very variable amount of fine sand, in all probability transported in the compound granules already de- scribed. Since the sorting of the material depends upon its amount, and on the conditions of the current, there seems reason to hope that a further study of the ultimate character of clays may throw much light on these questions. Some of these indicate that they were rapidly deposited from very muddy, shallow water, and others that they were deposited from much clearer and deeper water. Volcanie Ash Beds in British Strata.—Extensive masses of rock have been often described as ash beds, but, when we come to examine the detailed structure, their true nature becomes very doubtful. Some of them may really have been true ashes, but they have undergone so much subsequent change that they are now totally unlike the ashes of modern volcanoes. The whole question requires much more examination, and the study of the subsequent alterations becomes the principal consideration, and it would lead me into far too wide a field of inquiry to enter upon it now. ‘That true but much altered ashes do exist is, however, clearly shown by some beds found at Bathgate, near Linlithgow. These show a structure which seems to indicate that they were originally a pumice ash, but the vesicles have been filled with infiltered mineral matter, and the whole greatly altered by chemical changes taking place after deposition. Conclusion. Leaving then out of consideration such cases, and confining our attention to by far the greater bulk of our British non-calcareous stratified rocks, we see that a most careful microscopical investiga- tion shows that the material was originally derived mainly from the chemical decomposition and mechanical breaking up of various granitic and schistose rocks, the products having been afterwards separated and sorted by the action of currents, and more or less con- solidated and changed by subsequent mechanical and chemical action. When we come to study the detail, it is also possible to form a satis- factory conclusion respecting the share which each of the above- named classes of rocks contributed to the formation of each particular stratum, and also to answer several questions of great interest in connection with the geological history of a very important group of stratified rocks, which hitherto have not been supposed capable of yielding any such information. Though these conclusions are 136 Transactions of the Royal Microscopical Society. in perfect harmony with well-known geological facts of an entirely independent character, yet some at least could not have been established in a satisfactory manner without tasking the utmost powers of the microscope, which are often required to see and identify the extremely small or larger particles of which the rocks are composed. EXPLANATION OF PLATE CLXXIV. Fics. 1, 2, 3—Grains of quartz from decomposed granite. Fic. 4.—Grain of quartz from schist. Fies. 5, 6.—Grains showing the contrast between simple and complex structure when seen with polarized light. Fic. 7.—Fragment of hornblende. » 8.—Fragment of felspar. ,, 9—Fragment of felspar seen with polarized light. , 10.—Fragment of decomposed felspar. ,, 11.—Granule of kaolin in various positions, very highly magnified. ,, 12.—Fragment of pumice. ,, 13.—Grain of quartz sand from Millstone Grit. , 14.—Fragment of granite from the Millstone Grit. ,, 15.—Grain of sand from the Desert. ,, 16.—Fragment of mica schist from the slate rocks near Moffat. GoLeia) Il.—Measurements of Rulings on Glass. By Evwarp W. Mortey, Western Reserve College, Hudson, Ohio, U.S.A. Puate CLXXV. In November 1875, Mr. Rogers, while employed in perfecting the details of his engine for ruling lines on glass, asked me to measure the intervals between the lines on a plate which he ruled for the purpose and sent to me. It contained a hundred heavy lines ruled twenty-four hundred to the inch, forty heavy lines ruled four hundred and eighty to the inch, forty light lines ruled like the last, ten lines ruled twenty-four to the inch, and a hundred light lines ruled twenty-four hundred to the inch. My attention was given to the detecting and measuring any periodic errors occasioned by periodic errors in the screw of the ruling engine, by eccentricity of the screw head, and by other causes producing similar results. To determine this kind of inequality with the smallest probable error, it was obviously proper to measure, not intervals produced by a hundredth of a revolution of the screw, but intervals ten or twenty times as large. ‘Twenty-three intervals of the hundred and twen- tieth of an inch as nearly consecutive as possible were therefore measured. After several preliminary trials with objectives of foci ranging from two inches to the sixteenth of an inch, a nominal inch objective, whose focal length is really eight-tenths of an inch, was selected for the work. It had been found that the same care with this objective gave results with a less probable error than any other tried. Mr. Rogers afterwards suggested that even a quarter- inch objective was too low a power to afford the required accuracy. While I cannot undertake to say what instrumental appliances are best suited to the habits, methods, and predilections of another ob- server, the fact remains that for myself the work in hand could be done with this objective so that a given amount of care made the probable error of results less than when the work was done with either a half, quarter, eighth, or sixteenth. The fine adjustment of the stand was screwed hard down and left untouched throughout the measurements. ‘The micrometer employed was a cobweb mi- crometer by Troughton, having two movable wires. The screw heads have each a hundred divisions; the fourth part of a division was read by estimation. Two readings were taken for each interval measured, between which the screw heads were both moved several divisions. ‘The wires were brought to the edges of the images of the lines of the glass plate, till the minimum visible bright line between the image and the wire was the same for each wire. As each interval was measured only twice, one can hardly compute the 0 Ee ee = , s =— 138 Measurements of Rulings on Glass. By E. W. Morley. Upper Curve: Upper Curve: Lower Curve: Lower Curve: Abscisse. Ordinates. Abscisse. Ordinates. Millim. Millim. | Millim. Millim. 0 — 4:2 0 + 0:8 5 + 5:1 6 +08 10 + 2:4 | 12 — 12 15 — 6°7 18 + 1:4 20 — 1:0 24 — 14 25 — 0°3 30 + 0°2 30 + 8°6 36 — 0°2 35 + 0°8 | 42 a 40 - 6:1 | 48 — 07 473 — 78 | 54 + 2°0 523 413 | 60 ah, 574 + 3°6 66 — 0°3 623 — 5°8 72 — 1-2 673 — 4:2 78 + 0'7 764 + 4:1 84 — 1:7 814 + 5:1 90 + 1:4 864 + 0:5 96 — 07 912 — 4:7 102 + 0:2 964 + 1:2 1014 + 5:8 | 1062 + 5°4 | 1112 + 0:3 | 1164 — 4:1 Horizontal scale, 10 millim. = ;}, inch. Vertical scale, 10 millim. = z5355 inch. Monthly Microscopical Journal, March 1, 1877. PLATE CLXXV. WACK VA oe 3/100,000 77, Y/10,000 tn. i) B) Luilinitiuitui! fila Measurements of Rulings on Glass. By E.W. Morley. 141 probable error of a mean. But the probable difference of the two measurements of one and the same interval will afford a convenient and, for the purpose, sufficient means of estimating the degree of confidence which may be felt in the result. The differences between two measurements of the same interval were one-fourth of a diyi- sion in seven cases, two-fourths in five cases, three-fourths in three cases, one division in two cases, one division and one-fourth in four cases, and one division and two-fourths in two cases. From this it appears that the probable difference of the two measurements of the same interval is fifty-six hundredths of a division of the screw head. Now the value of one revolution of the screw in the given circum- stances was the fourteen hundred and seventy-sixth of an inch, or 0-0006775. Hence the probable difference of two measurements for the same interval was the two hundred and sixty-one thousandth of an inch. It will be seen that this degree of accuracy was amply sufficient for the purpose. It will be noticed that twelve of the actual differences were smaller than the probable difference, and eleven were larger. In Figure a, Plate CLXXV., the measurements are plotted by making the abscissze proportional to the distance of the initial line of each measurement from the line where the measurements began, while the ordinates are proportional to the differences between the successive measurements and a constant subtrahend. It will be seen that an error whose period is five times the measured interval is clearly indicated. If the shortest interval of each of these five cycles is subtracted from the longest, the differences are successively seventy, eighty- six, fifty-five, fifty-eight, and fifty-eight: the unit being the four hundredth part of the revolution of the micrometer screw. Half of the mean of these differences is that part of the periodic error which corresponds to the fifth part of the circumference of the screw of the ruling engine, or to an are of seventy-two degrees. This quantity is eight and seventeen hundredths divisions of the screw head of the micrometer. If this be multiplied by the ratio of the diameter of the circle to the chord of the arc or seventy-two degrees, we have a tolerable approximation to the whole periodic error of those threads of the screw which produced these lines, as the screw was at the time adjusted. This quantity is the ten thousand six hundredth of an inch, or 0000094 inch. This quantity represents the greatest possible displacement of a line from its true place, as far as the displacement is periodic and not accidental; the greatest possible difference between two professedly equal intervals is double this quantity. ' If doubt is felt as to the propriety of assuming that the errors for a fifth ofa revolution and for a half revolution are proportional to the chords of the ares, the total displacement of a line by periodic 142 Measurements of Rulings on Glass. By EH. W. Morley. error may be computed in another way. If we subtract the mean of the whole twenty-three measurements from the successive mea- surements, we get the following column of residuals. If now we add all the successive residuals which have the same sign, we get the total measured displacement of the last line before the change of sign. In this way we obtain the column of displacements. ate Mean. Residuals. Displacements, 12,237 12,299 =) (92 12,375 a ae. ae 12,335 . + 36 i se os 12,200 _ Log 12,285 ” - U4 — 117 12,295 e He 12 425 ” + 126 | 12,312 f ti. i} +389 12,210 ~ merce) 12,185 < = ANd i = ae 12,320 99 + .21 | 12,352 m1 Eee: \ + 74 12,215 Pa me | 12.237 | ee 12,360 a5 + 61 | 12,375 + + 76 |$ +4 145 12,307 if 4a 12,230 % =; S| dae 12,317 a BY ati | hm 12,385 » + 86 | | 12,880 z + 8i + 191 12,305 | - eer 12,240 » — 59 | — 121 aT The mean displacement, without regard to sign, is thirteen divisions and two-tenths ; this quantity is the eleven thousand two hundredth of an inch, or 0°000089 inch. This quantity is twenty- four times as large as the probable difference of two measurements of the same interval. It is identical with the previous value. This agreement shows that the error is proportional to the chord of the arc of the screw which corresponds to the measured interval. It may be said that since the measured intervals were not all absolutely consecutive, the first method probably is the more accurate. Mr. Rogers, who did not for a time admit the conclusiveness of the foregoing measurements, thought that the periodicity shown in my results was most probably due to periodicity in the micro- meter screw employed. But it is obviously impossible to suppose that to such a cause could be due inequalities amounting to a fifth part of its pitch. And further, the measurements were so made that the effect of periodic errors in the micrometer could per- Measurements of Rulings on Glass. By EH. W. Morley. 1438 ceptibly affect only the accuracy of the reduction of the differences to fractions of an inch, while such errors could not affect the relative magnitudes of these differences except by quantities which may be neglected. A plate ruled by Mr. Rutherford, of New York, was afterwards measured in the same way, but with less care in making contacts. Kighteen intervals were measured ; the differences of the two mea- surements of the same interval were nothing in two cases, one in five cases, two in three cases, three in three cases, four in one case, seven in one case, and eight in three cases; the unit is the four hundredth of a revolution of the screw head. The probable differ- ence of the two measurements of the same interval is sixty-seven hundredths of a division. If the measurements be plotted, as in the former case, the result is seen in Figure b. If the shorter interval in each cycle is subtracted from the longer, half the mean of these remainders is the greatest observed displacement of a line by periodic error. This quantity is the seventy-six thousandth of an inch. This is but four and one-half times as large as the probable difference of the two measures of the same interval. The measure- ments therefore cannot be used to give the amount of periodic error in Mr. Rutherford’s screw, while they conclusively show that it is much smaller than in the former case-—Lead before the American Association for the Advancement of Science, August 1876, VOL. XVII. M (1444) NEW BOOKS, WITH SHORT NOTICES. The Microscope and its Application.*—The appearance of a second edition of Professors Nigeli and Schwendener’s Handbook of the Microscope (on the merits of which there is but one opinion abroad) will be hailed with interest by many in thi& country. Nor will this interest be diminished by the circumstance that the text-books which respectively represent foreign and English micrography differ so widely in subject, plan, and treatment. Our English manuals scarcely enter. upon that optical ground which is supposed to be specially reserved for the practical optician, whose authority as the designer and constructor of microscope combinations is accepted without question. On the other hand, they give full play to the fancy which dictates preferences for variety in size, shape, and mechanical arrangement of the instrument; in which respects the only gujding principle of any value—namely, that the instrument should be as little as possible encumbered with mechanical appliances, and that as much as possible should be left to the skilled manipu- lation of the observer—is too often neglected. But the English manual is chiefly distinguished by its fullness of detailed directions “how to work with the microscope,” and naturally blends with these directions a great amount of information regarding the various sub- jects of microscopic research as well as their technical manipulation. And thus it happens that the most important chapters of the English treatise are not those in which the optical construction of the micro- scope is explained, but rather such as treat of “its revelations.” But in the foreign handbooks, treating professedly of the theory and construction of the microscope, no place is made for disquisitions upon subjects of natural history, histology, or the special sciences of anatomy, pathology, &e. Firstly, because the theory of the micro- scope is treated in Germany as a physico-mathematical problem, in the demonstration of which the physicist and mathematician have equal if not superior rank with the mechanical constructor. And secondly, because the establishment of various schools of microscopy in the several university towns, and the issue of various scientific journals by professors connected therewith, as well as the frequent publication of special monographs, render every facility for micro- graphic literature, without trenching upon the volume specially devoted to the theory of the microscope and its manipulation. In the present phase of microscopic science another motive to study of the optical conditions under which appearances seen through the microscope must be interpreted, comes strongly into play: a motive which ought to be felt equally by all who profess to look a step or two beyond the mere amusement found in observing toy * ‘Tas Mikroscop: Theorie und:Anwendung desselben,’ von Carl Nageli, Pro- fessor in Miinchen, und 8S. Schwendener, Professor in Basel. Zweite verbesserte Auflage, mit 302 Holzschnitten, Leipzig: Verlag von Wilhelm Engelmann. 1877. NEW BOOKS, WITH SHORT NOTICES. 145 objects. For the surprising diversity—not to say antagonism—of view entertained by different observers who have over and over again examined the same object and yet have interpreted so differently the appearances observed, could not but lead to the conclusion that the microscopic image itself is not always the same unaltered transcript of the same light and shadow picture. The more difficult therefore the problem placed before the microscope for solution, the more needful should it seem that the theory of the compound microscope .be again strictly revised, if the difficulties of interpretation which increase with every fresh strain put upon the instrument are to be overcome. By Teutonic minds the relegation of so congenial a labour into the hands of the optician was not likely to be tolerated ! and as little would they be content that such knowledge should lie outside the recognized sphere of scientific investigation. The physico-mathematical investigation of the theory of the micro- scope has thus naturally fallen into the hands of those for whom this subject possessed special attraction. But it may also be fairly expected that all who are interested in microscopic research generally, should desire to hear of any new discovery that might come to light, or of any fresh aspect in which what was already known might appear after renewed examination. A second edition of a well-accredited work has therefore real significance, and appears opportunely for the lovers of microscopic science at a period when the limit of the powers of the microscope seems to have been reached, and, in default of adequate explanation and rational guidance, a certain misdirection of energy in any further efforts to add to its powers becomes imminent. The work of Professors Nigeli and Schwendener, of which we here propose to give a short account, brings down to the end of the year 1875 the latest summary of the optical questions connected with the theory of the microscope and of the conditions under which the various objects submitted to microscopic analysis are seen. Petty: Cash) 20 Wa. acceso m0 mn », Soiree Expenses .. 914 6 », Cash paid for 227. 5s. 7d. Consols... ae Ol 10) », Book Shelves a5. se Hye alias 5 (0) » Slate and Stand .. 212 6 | » Instruments and Repairs 819 0 | »» Stamped Cheque-book Oye: (2 | || » Balance remaining 31st | Dec. 1876 os joe) mao emo O , £41 17 3) £741 17 3 Jan. 29, 1877. Examined and found correct, CHARLES JAMES FOX. F. W. GAY. Liprary, APPARATUS, AND COLLECTIONS. The additions made to the library, apparatus, &., since the last Report are given below. The Council had much pleasure in responding to the request made by the Government for aid to the Loan Collection at South Ken- sington, and sent thereto a selection of instruments of historical interest. The books and collections are in as satisfactory a condition as the limited space and means at the disposal of the Society have permitted. PROCEEDINGS OF SOCIETIES. 165 The following are the more important works presented during the year: Transactions of the Linnean Society. Transactions of the Royal Irish Academy. The Application of Photography to Micrometry, with special reference to the Micrometry of Blood in Criminal Cases. Illustrated with Photographs. By Dr. J. J. Woodward. Medical and Surgical History of the War of the Rebellion, Part 2. From the Surgeon-General, U.S.A. Quinology of the East Indian Plantations. By John E. Howard. Memoire sur les Caracteres Mineralogiques et Stratigraphiques, &e. Par MM. Poussin et A. Rénard. Six sets of Photographs, with Pamphlets. By Dr. J. J. Woodward. Books PuRCcHASED, Quarterly Journal of Microscopical Science. Annals of Natural History. Proceedings of the Royal Society. Mycographia [cones Fungorum. Parts 2 and 3. APPARATUS, SLIDES, &C., PRESENTED. Three Slides of Minerals, from F. Rutley, Esq. Four Sections of Coal Fossils, from Mr. Norman. Three Slides of Diatoms, from Mr. F. Kitton. PAPERS READ BEFORE THE SOCIETY DURING THE PAST SESSION. Optical, Instrumental, and Technical. “ On the Characters of Spherical and Chromatic Aberration arising from Excentrical Refraction, and their Relations to Chromatic Dis- persion,” by Dr. Royston-Pigott. “ Ona New Arrangement for Illuminating and Centering with High Powers,” by Rev. W. H. Dallinger, March Ist, 1876. “Measurements of Méller’s Diatomaceen-Probe-Platten,’ by E. W. Morley, March 1st, 1876. “ A New Microscopic Slide,” by HE. V. Broeck, April 5th, 1876. “On a New Form of Pocket Spectroscope,” by H. C. Sorby. “ A Stage Incubator,” by H. A. Reeves, December 6th, 1876. “ Notes on Micro-photography,’ by Surgeon-Major Gayer, May drd, 1876. “On a New Process of Preparing and Staining Fresh Brain for Microscopical Examination,” by Bevan Lewis. “ Observation on Professor Abbe’s Experiments illustrating his Theory of Microscopic Vision,” by J. W. Stephenson, January 3rd, LST. Observations upon Mr. William Rogers’ Paper on a Possible Explanation of the Method employed by Nobert in Ruling his Test- Plates,” by W. Webb. “On the Present Limits of Vision,” by Dr. Royston-Pigott, October 4th, 1876. “On a New Method of Measuring and Recording the Bands of the Spectrum,” by Thomas Palmer, B.Se., October 4th, 1876. 166 PROCEEDINGS OF SOCIETIES. “On the Measurements of the Angle of Aperture of Object- glasses,” by F. H. Wenham, November Ist, 1876. Natural History and Mineralogy. “The Identification of Liquid Carbonic Acid in Mineral Cavities,” by W. N. Hartley, F.C.S., March Ist, 1876. “On some Structures in Obsidian, Perlite, and Leucite,” by Frank Rutley, F.G.S., March Ist, 1876. - “Note on the Markings of Navicula rhomboides,” by Dr. J. J. Woodward, April 5th, 1876. “Some Results of a Microscopical Study of the Belgian Plutonic Rocks,” by A. Rénard, §.J., April 5th, 1876. “ On the Markings of the Body-scale of the English Gnat and the American Mosquito,” by Dr. J. J. Woodward, May 3rd, 1876. “On Remulina Sorbyana,” by J. F. Blake, May 3rd, 1876. “On the Rotifer Conochilus volvox,” by Henry Davis, June 7th, 1876. “On the Microscopical Structure of Amber,’ by H. C. Sorby and P. J. Butler, October 4th, 1876. “ A Curious Fact in connection with certain Cells in the Leaves of Hypericum Androsemum,” by W. Hinds, M.D. “ Experiments with a Sterile Putrescible Fluid exposed alternately to an Optically Pure Atmosphere,” &c., &c., by Rev. W. H. Dallinger, November Ist, 1876. “ Bastian and Pasteur on Spontaneous Generation” (translation), by H. J. Slack. “The Markings of Frustulia Saxonica,’ by Samuel Wells. “Qn Navicula crassinervis, Frustulia Saxonica, and Navicula rhomboides, as Test-Objects,” by Rev. W. H. Dallinger, December 6th, 1876. “On the Relations between the Development, Reproduction, and Markings of the Diatomacee,” by Dr. G. C. Wallich, January 38rd, 1877, Twelve gentlemen have been elected Fellows, and two have been elected Honorary Fellows of the Society during the year, and the Society have to regret the loss of seven ordinary and one Honorary Fellow. OBITUARY. CuristTIAN Gorrrreip Eprensere was born on the 19th of April, 1795, at Delitzsch, in Saxony, of which town his father was what we may perhaps call “town regent” (Stadtrichter), Even at the early age of fifteen he evinced a strong taste for the study of natural . history; but being destined by his father for the Church, he was sent to study theology at the University of Leipzig. He, however, soon resolved to devote himself to a profession more closely connected with his favourite subject, and applied himself to the study of medicine, thinking it impossible to earn his living by devotion to pure science. In 1819 he commenced practice, but abandoned it in the course of a PROCEEDINGS OF SOCIETIES. 167 year, and fairly commenced a career of scientific research, which was continued uninterruptedly for more than half a century. His early papers were chiefly on botanical subjects, and his first great discovery, made in 1820, was that fungi are developed from spores, and not by spontaneous generation. The minute anatomy of animal tissues also attracted his attention, but his fame chiefly rests on the many brilliant discoveries which he made in connection with living and fossil Fora- minifera, Polycistine, and Infusoria, using this term in the sense employed by him, which included many organisms now regarded as plants. The earliest paper connected with these subjects was published in 1829, and from that date until 1875 there appeared a constant suc- cession of valuable papers, or separate works, relating to minute animal or vegetable forms. His last was on marine and fresh-water dredgings from all countries, published in 1875, when eighty years of age. At the commencement of Ehrenberg’s splendid researches the achromatic microscope was quite in its infancy ; and, if we may rely on the conclusions to be drawn from a careful examination of the older microscopes in the late Loan Collection at South Kensington, something like one-half of Ehrenberg’s work must have been done with microscopes which nowadays would be looked upon as scarcely good enough for toys, much less for research. When we reflect on what he did with such imperfect instruments, and what many of our present microscopists do with their splendid apparatus, one cannot but feel that the eye at one end of the tube is, after all, the most important part of the whole optical arrangement. We all know very well that Ehrenberg was led into many errors, but, considering the means at his command and the extreme novelty and difficulty of some of his investigations, we may be surprised more by the truths dis- covered than by the mistakes made. What strikes us most is the vast extent and continuance of Ehren- berg’s researches. Independent of his great works on the Infusoria, on Microscopic Geology, and other kindred subjects, the number of separate memoirs published between 1820 and 1873 was no less than 293; being, therefore, an average of five or six, continued over a period of no less than fifty-three years. We must forbear to notice in detail even a mere fraction of these publications. We can scarcely over-estimate the effect of all this work on the advancement of micro- scepical science. Perhaps one of the most important conclusions was that minute organisms have contributed very much to the formation of thick masses of stratified rocks, and that such deposits as our chalk are—or, perhaps, still more correctly, were originally—most closely similar to deposits now being formed in modern oceans. He was elected an Honorary Fellow of our Society in 1840, and died on June 27, 1876, at the age of eighty-one years. Epwarp Newmay, F.L.S., &c., was born at Hampstead, on May 13, 1801. At a very early age he evinced a taste for natural history, which was fostered and encouraged by both his father and mother. After his school days were passed he resided with his father at 168 PROCEEDINGS OF SOCIETIES. Godalming, carrying on the business of a wool-stapler, but all the while devoting himself to the study of his favourite subject. In 1826 he removed to Deptford, where he engaged in the business of a rope manufacturer. It is said that in his garden there he specially culti- vated such flowers as attract many insects, and devoted much time to the study of their habits. He was one of the original members of the Entomological Club; and when this club started the ‘ Entomological Magazine, he was chosen to be its first editor; and for upwards of forty years the collection of the club was under his personal care. Towards the end of 1840 he became connected with a publishing firm, and conducted the business until 1870, during which interval were brought out several valuable works on insects and ferns, to the study of which plants he had devoted much attention. Amongst other pub- lications may be mentioned the ‘ Zoologist, of which no less than thirty-three annual volumes were published under Mr. Newman’s supervision. In 1858 he became the natural history editor of the ‘ Field, and continued to fill that post until his death. Amongst his papers in this periodical may be specially named those on economic entomo- logy, being perhaps the first to point out to agriculturists the true way to deal with their insect enemies. Mention may also be made of his two valuable works on British Moths and British Butterflies, which latter was written by him when in his seventieth year. He died on the 12th of June, 1876, at the age of seventy-five, having by his many separate works and very numerous original memoirs, and by means of the Journals published under his editorship, largely contri- buted to advance and disseminate a knowledge of various important branches of natural history. He was elected a Fellow of our Society in 1840. Though Dr. Francis Srpson, F.R.S., was elected a Fellow of the Microscopical Society in 1853, his scientific investigations were only indirectly connected with microscopical research, and had more special reference to general human anatomy and to the practical application of remedial measures. He was born in 1815, near Maryport, in Cum- berland, and received his medical education in Edinburgh and London. For thirteen years he was resident surgeon to the Nottingham Hos- pital, after which he removed to London. The subjects to which he directed his attention were chiefly more or less closely connected with the physiology and pathology of respiration ; but he was also the author of a valuable work on medical anatomy. He died suddenly at Geneva, on the 7th of September, 1876, aged about sixty, from the bursting of an aneurism, when almost in the act of telegraphing to say when he would arrive at his residence in London. Wuttram Detrertier, born December 23, 1800, died July 15, 1876. Joined the Microscopical Society in 1847. For more than twenty-five years he was an enthusiastic worker with the microscope, and in- terested himself in its optical and mechanical improvement. He acquired great skill in the display of difficult objects and in testing glasses, and when Messrs. Powell and Lealand contemplated the im- provements carried out in their first-class microscope, he entered OO ee ee eee PROCEEDINGS OF SOCIETIES. 169 warmly into their plans, and the first instrument of the new pattern was made for him. Joun Newton Tomurns, born 1812, died 1876. Joined the Society in 1857. He studied surgery under Joseph Henry Green, and passed with distinction through the medical curriculum of St. Thomas’s Hospital. He was for many years Inspector of the National Vaccine Institution, and was a Fellow of the Royal College of Surgeons, and of the Royal Botanical and Zoological Societies. He formed an ex- tensive collection of microscopes, apparatus, and objects, and for many years promoted microscopical pursuits by scientific gatherings at his house in Fitzroy Street, which afforded opportunities for examining novelties and for friendly discussion. The Secretaries have not been able to obtain any biographical information concerning the following : Chas. Gilbertson, elected Feb. 13, 1861, died Dec. 10, 1876. Henry Hopley White, elected April 1841, died Dec. 10, 1876. Andrew Yeates, elected March 1854, died Feb. 16, 1876. Donations to the Library since January 3, 1877: From Nextt Camm WV COKLY iia, oi, chi nacam occu atone! adem Manu Rae eamora! nced idan aoe nen Mantors JANe Tei, ACCA 55a oot Comme nog ior mcd EHOmy tam neo Ditto. Society of Arts Journal . «es, SOCIELY. Annuaire de L’Observatoire de Montsouris pour ‘VAn 1877 7. Memoir of the Life and Works of Edward Newman. By his Son.. Author. Bulletin de la Societé Botanique de France, 1876 .. .. .. «. Society, Annales de la Société Belge de Microscopie, 1875-6 Ae x Ditto. Bulletin des Seances de la Société Belge de Microscopie, 1874-5 oa, 1 Detto: Transactions of the Linnean cugre: “Two parts: ) <6) Uae ney a aitos Set of Photographs .. pegs Se dls Rit RT Oliver, Chicago. Popular Science Review. "No. 1 ' Now Gericd =. Mas! i. 20Rs .. Publisher. Dr. John Habirshaw, and Frederick Habirshaw, Esq., of New York, were elected Fellows of the Society. Water W. Reeves, Assist.-Secretary. Mepicat Microscopicant Society. Annual General Meeting, January 19,1877. Dr. J. F. Payne, President, in the chair. This was the first meeting held in the new rooms of the Society, 6, Pall Mall Place, W.; and the additional comforts and advantages offered over the old room seemed to be fully appreciated by those present. The Secretary’s Report for the year 1876 was read. The following are the names of the communications read before the Society during the past year :—President’s Address, Dr. Payne. Development of New Blood-vessels, Dr. Thin. Browning’s Triplet Mr. Jabez Hogg. Modification of Pritchard’s Microtome, Mr. Giles. Hints on the Systematic Study of Histology, Dr. Woodman. Cirr- hosis of Liver in Child, Mr. Needham. Freezing Microtome, Mr. R. 170 PROCEEDINGS OF SOCIETIES. Williams. Microscope for Viewing Circulation in the Frenum Lingue, Dr. U. Pritchard. Carcinonia of Liver simulating Cirrhosis, Dr. Goodhart. Myeloid Sarcoma, Mr. Needham. Organ of Corti in Mammals, Dr. U. Pritchard. Rodent Ulcer, Mr. Golding-Bird. The soirée of the Society was held on June 80. Of the fifty-four microscopes exhibited, twenty-four were devoted to a series of typical tumours ; besides these, a variety of instruments and photographs was shown. The number of members of the Society in December 1876 was 129. Several presents during the past year both of books and specimens were received ; and upwards of seventy different preparations besides apparatus were exhibited at the close of the meetings, in the same period. The Treasurer’s Report showed on December 31, 1876, a balance of 301. 9s. 3d. against one of 201. 9s. at the same time in the previous year. The soirée expenses amounted to 197. The actual increase in the income of the Society was therefore nearly 301. The retiring President then delivered his address. He congratulated the Society upon its numbering 122 paying members, and thought that just at this time it might be said to be passing through a crisis; it had outgrown its developmental stage, and now hoped for something better. Originally designed to be of service to medical students, it soon found its sphere of action among those far senior to students; and he would say that in his opinion this Society offered a more congenial field for the investigation of histological pathology than any other in London. One function he deemed specially belonging to the Society, i.e. to study the influence of histology—normal or pathological—in every- day medical practice; this included a very large but very important field if we include its relation to hygiene. A clearer knowledge of tissues had helped us to understand more of pathological conditions ; gave also a clearer precision in diagnosis, and sometimes even a general hint as to prognosis and treatment, Such a subject as “ degeneration,” how different was its aspect now to that of the prehistological period! Fatty infiltration was now easily distinguished from “ fatty degeneration,’ while the practical bearing of this was found in the recognition now of sudden death from a fatty heart—a condition proved by histological investigation, and even admitted sound in courts of law. Again, with regard to tumours, what numbers of varieties were classed under the one head malignant or even cancer, now known to be perfectly distinct from each other, and how usual was it to appeal to the microscope ere the surgeon gave an opinion as to the recurrence of the disease. Several other instances of the use rendered to practice by the microscope were quoted, particular stress being laid upon the help it had been in elucidating the intricacies of Bright’s disease. Chorea was brought forward as showing what yet remained to be done, for till its histological pathology were determined, who could say that it was not the expression of several diseases ? PROCEEDINGS OF SOOIETIES. 1 ipa In conclusion, the President remarked that this anatomical know- ledge was after all but the beginning of medicine. Still it was an improvement upon the time when the physician walked on air, so to speak—having nothing but symptoms to guide him—and given an anatomical basis, it would for most diseases at least be a histological one. The difficulties of investigation were great, and the slowness of discovery was not the fault but the misfortune of the histologist. LIvERPOOL Microscoproan Soctrety. The ninth ordinary meeting of this Society was held at the Royal Institution, Friday, December 1, the Rev. H. H. Higgins, A.M.,, in the chair. Captain Jno. H. Mortimer, of the U.S. ship ‘ Hamilton Fish,’ an associate member of the Society, exhibited a number of marine specimens which he had presented to the Free Public Museum. He also communicated some interesting facts in connection with the Physalia pelagica, known as the Portuguese man-of-war, the tentacles of which are of great length, consisting of a muscular band studded on its margin by rows of beads, each bead being a mass of small spherical cells, each of which contains a small spiral stinging thread, coiled up inside. Portions of the tentacles had been mounted for microscopic examination, and under a power of 500 diameters the cells and spiral contents were easily seen. Captain Mortimer stated that he had frequently witnessed the discharge of the stinging threads from the cells, and that the stinging power was perceptible some days after the death of the animal. He believed that the above facts were new to science. The paper for the evening was on “ Lines of Animal Life,” by the Rev. H. H. Higgins. The paper was illustrated by diagrams, especially by one of large size representing a Stammbaum des Thier- reichs, or genealogical tree of animals, enlarged from ‘ Grundriss der Zoologie, by Professor G. v. Koch, published in part, during the present year. \ A short and interesting discussion followed, after which the meeting concluded with the usual conversazione. San Francisco Microscorican Society, A meeting of the San Francisco Microscopical Society was held December 21. Mr. Isaac Lea donated to the cabinet a sheet of Phlogopite Mica from Canada, and another of Muscovite Mica from Chester County, Pennsylvania. Mr. Lea also exhibited a new micaceous mineral known as Hallite, a film of which he placed on the stage of the microscope and called attention to its characteristics, Mr. Hanks presented a sample of diatomaceous earth from a newly discovered deposit in Ione Valley, Amador County, California, 172 PROCEEDINGS OF SOCIETIES. A small portion hastily prepared showed several forms, mostly Dia- toma and Navicula. Four slides, being sections made in different directions of a hard deposit showing woody structure, found in the body of the Mount Diablo coal vein, and termed “Nigger Head” by the miners, were donated by Mr. 8. B. Christy. On examination, the wood fibres were clearly shown, and their general appearance was that of the oak. Mr. Hanks handed in a report on a sample of (so-called) silver mud from Oregon. Mr. Kinne exhibited several slides of diatoms mounted by Professor H. L. Smith, of Hobart College, Geneva, New York, which had been received in the way of exchange, and called the especial attention of the members to the preparations of Professor Smith and his authentic series of diatoms. - Mr. J. P. Moore handed in a new fungus, which he described at length, and has named Lentinus aurantius. tae. bth W.Wes Thrary e3~ del acd nat WH, Ded = ofa sinervis CALE S e frus |= CPs LULOTL iS pS AS Gigs c ped ft ere Th rkK ana | onica THE MONTHLY MICROSCOPICAL JOURNAL. APRIL 1, 1877. 1.—Additional Note on the Identity of Navicula crassinervis, Frustulia Saxonica, and N. rhomboides. By Rev. W. H. Dauuinearr, V.P.R.M.S. (Read before the Royau Microscopican Society, March 7, 1877.) PuaTE CLXXVI. Ir would have been a matter of much interest to me to have been present at the discussion which followed upon the reading of my paper upon the above subject in December last. I might have been able to afford or to evoke explanation that would have served to further elucidate the subject. it The only report of the discussion I have access to is that given in the January number of the ‘M. M. J.,’ which doubtless is sub- stantially correct. In the interests of science, and with a simple desire to elicit truth, | may be permitted the privilege of this note upon some of the statements it contains. And first, of course my paper did not aim at proving, or, on my own authority, even asserting, the ¢dentity of the diatoms in question. I simply accepted this on the authority of Professor H. L. Smith and Mr. Kitton, which to myself was, and still is, per- fectly competent. But accepting the identity of these forms thus established, I sought to augment its value by a fact—in itself of some optical interest—that all these forms were in ultimate struc- ture precisely alike; so that, using the lowest power that would reveal the beaded arrangement on the surface of the smallest forms, we could, by using successively larger forms, with the same power, see precisely the same arrangement with increasing clearness and ease. DESCRIPTION OF PLATE CLXXVI. Fic. 1, A, B, C, D.—Four forms of NV. rhomboides in a gathering from “ Cherry- field,” showing modifications of outline, with the existence of the links uniting the two extremes (A and D). @ in A shows that the striation was that belonging to N. rhomboides. Fic. 2.Similar examples from specimens taken in the living state at Llyn- cum-Bychan. — ‘ ; Fic. 3.—Similar evidences of change of form in the smaller frustules known as IV. crassinervis. en Fic. 4.—Different modifications occurring in the apexes A, B, C, of the mid- ribs of these diatoms. VOL. XVII. O 174 Transactions of the Royal Microscopical Society. Now the report of the discussion affirms that “ Mr. Ingpen suggested that, after all, the question of genus and species depended upon difference in shape, and not upon the absolute number or fineness of the lines.”* From which I should gather that the identity of ultimate structure which I pointed out, taken together with the opinion of the authorities named, had left the speaker unconvinced of the identity of the forms in question; since there were palpable though minute differences of shape in the drawings submitted. Now I have not the slightest desire to defend or seek to sustain the identity. This is in far better hands; and the facts I presented remain the same, whether the three forms be identical or not. But the position taken by Mr. Ingpen involves a biological question of large importance. Every possessor of a microscope knows that if there be one thing that is permanent in Navicula and Pleurosigma, it is not necessarily the tenuity or coarseness of the striation, but its arrangement; and it was to this that I specially called attention in the forms in question. On the other hand, I am prepared amply to prove that the “ shape” of these diatoms is subject to almost infinite variation: small in any given case, doubtless, but occurring in every conceivable direction. Nor am I alone in this affirmation. I number amongst my friends and acquaintances many amateur, and several profes- sional, mounters of diatoms; through whose hands, and under whose eyes, millions of certain forms pass every year; and with- out a single exception they assure me that between any two con- trasted and comparatively unlike forms of the “same species” they can find almost every intermediate grade or link. Now the point in question is, are we to establish a species upon a variable or an invariable characteristic ? Is specific identifica- tion to depend upon that which is always changing in indefinite ways, or upon that which practically never changes ? My first great lesson in biology was learned, incidentally, many years ago, from Professor W. K. Parker, who dispelled for ever my hard-and-fast view of species in Foraminifera by showing me every conceivable link between two species. The meaning of it never left me; and supplied by him with a rich store of foraminiferal material from almost every part of the world, I quietly worked over hun- dreds of thousands of forms; and, so far as the mere shell was con- cerned, proved to myself clearly that many so-called species were merely extreme modifications of the “species ” to their right or left, and that every intermediate modification could be found; a truth which has had ample illustration from Professor Rupert Jones in our recent ‘ Transactions.’ + But years of study have convinced me further, that this mutability is not confined to this group of the Protozoa. It is * (M.M. J.’ January 1, 1877, pp. 52, 53. + ‘M.M. J.’ vol. xy. 61. Identity of Navicula crassinervis, &e. By W.H. Dallinger. 175 everywhere manifest, where from their extreme minuteness and multitude, large numbers of microscopic organisms can be con- stantly compared. It is pre-eminently true, for example, of the desmids and the diatoms. Of course I need not remark that the mere study of mounted specimens is utterly incompetent for proof in such an investigation. One might as well attempt to generalize upon the osteological characteristics of a given skeleton by the observation of a limited number of specimens seen through the glass fronts of museum cases. It can only be done, as the Fellows of this Society well know, by the careful examination of unmounted material in every variety of condition. I have already said that my knowledge of the Diatomaceze does not extend much beyond the silicious frustules ; whilst I have spent comparatively little time in endeavouring to accomplish difficult feats with test-objects. But a working microscopist must have a set of crucial standards, thoroughly known to himself, to serve for comparison ; and N. rhomboides in its several varieties was very early adopted as mine: hence I have had an interest in this frus- tule which has extended over years ; and especially since the pro- minence given to “F', Saxonica” and “N. crassinervis” I have examined very large quantities of material derived from both England and America. It is my habit to make a drawing of any fact of moment in any of my observations; and I invariably do this in relation to variations of form in any well-known object or objects. Since reading the rule given by Mr. Ingpen, on which the determination of genera and species is said to depend, I have turned over the leaves of my folio, and have found some singularly suitable cases of variation in the “shape” of N. rhomboides (of course including F. Saw. and N. crass.), which are of considerable service; all the more indeed that some of them have been drawn for years, and all were drawn in entire independence of the question in hand. In Fig. 1, Plate CLXXVI., are the outlines of four frustules taken from a gathering of “ Cherryfield” rhomboides. They were of course drawn at different times, and from different “dips” of the material, and are doubtless not commonly to be found ; but whoever is supplied with sufficient material and patience might, I am con- vinced, select and arrange frustules precisely in the order in which they stand in the Plate. Apart then from the general symmetry, if the ends of the frustules drawn be examined, it will be seen that between A and D there is a remarkable difference; but if B and C be inserted in order between them, we have comparatively easy steps from the one to the other. Now the only diatom that I know of that in all respects comes near to A and B is Navicula cuspidata; but (1) as a rule the 02 176 Transactions of the Royal Microscopical Society. apexes of the frustules of this form have no constrictions as seen in A and B, and never, so far as my knowledge goes, a constriction so great as in A; and (2) although the striation is, in a general sense, the same as in N. rhomboides, anyone thoroughly familiar with both could never mistake the one for the other; and to show that the character of the beading is distinctively that of rhomboides, a portion has been carefully drawn at 8, A, Fig. 1. This was done with a magnification of 450 diams., and reduced; while the same nature and arrangement precisely of hemispheres or beads were demonstrated in each of the other three forms in Fig. 1. The point is, if “shape” be the characteristic on which the determination of “ genus and species” depends, then surely A, B, C, and D are each of them separate species! Moreover, at times it happens that the two ends of a given frustule are not absolutely like each other. In Plate CLXV., belonging to my paper published in the last Journal,* it will be seen that in Fig. C the right end of the frustule is not like the left one. This is strictly true to nature. A constriction is found at one end and not at the other ; does this make it, and similar forms, specifically different? It was stated in the discussion that the drawing of the large specimen which I had sent to the Society had not the “rhomboidal outline”; but if I had considered that “outline” of the slightest moment, it would have been an easy matter to find one that had. Do I rightly understand that such a specimen, if found and presented, would have to be considered a distinct species from the one drawn ; and which one of the speakers (Mr. Ingpen) declared “he should hardly eall a rhomboides at all”? If this be true, I can only say that there is, in what is now known as N. rhomboides, plenty of work for those who desire to engage in the labour of describing and naming species, But it appears to me that this canon for determining the generic and specifie differences of diatoms cannot hold good. It certainly must be rejected by the biologist. The differences be- tween A and D, Fig. 1, are not greater than those seen in many of the varieties of several species of fern ; nay, they certainly are not greater than the difference existing between a bulldog and a grey- hound, or between a “ pouter” and a rock-pigeon. And I think that we should therefore have no right to consider them specifically different, even 2f the intermediate links could not be found; which they certainly can. But whilst we have all this variation in form, there is one characteristic that is practically unchangeable; it is the character of the “striation.” It is perfectly true that, although it is the rule that the smallest frustules have the most delicate striation, it ig not (so far as my experience goes) invariably so. Small frustules * The present paper was sent to the Secretary in January, but could not be read until March, the Presidential Address intervening. Identity of Navicula crassinervis, &e. By W.H. Dallinger. 177 may have relatively coarse striation. But the arrangement of the hemispheres is, in frustules of all sizes, unalterably the same. Now as we do not select the variable but the invariable characteristics of the dog to define it specifically, on what principle should we ignore an énvariable characteristic of N. rhomboides (and all other Naviculz), and attempt to determine it specifically upon characteristics which are found, when large numbers are examined, to be constant only in their variability ? That this variation is ever recurring, I may further illustrate. I have lately been examining a fine gathering of N. rhomboides from Llyn-cum-Bychan, North Wales. The frustules are very large, and the beading or striation comparatively coarse. They were taken in the living state, and only cleaned for examination, and not for mounting. Fig. 2, A, B, C, gives the outlines of forms of frustules found repeatedly. I need not point out the varieties of form or “shape” which they present; they are sufficiently obvious. But I may remark that in all the “striation” was identical. Now I would ask, do these varieties of “shape” con- stitute specific differences? or rather, are they held to do so? Because, if they are, we should have a distinct and scientific method for their detection. Again. In an examination of a good-sized pocket-collecting bottle full of “ material,” in a well-cleaned state, of smaller forms, such as have been called F. Saxonica and N. crassinervis, I have detected and drawn the forms seen in Fig. 3, A, B, C, no less than five times, quite independently of each other ; but the striation was alike in all. Finally, the “nodules” were commented on as exhibiting variety, In my drawings; and this was taken as, apparently, important, and the form of the nodule combined with the “ shape ” of the whole frustule was suggested as the basis of specdfic de- markation. I can only say that it would have been by no means impossible to have selected “nodules,” in every case, alike; and however unlike any two frustules may be, it would be possible to find the intermediate links. In Fig. 4 are the midribs of three forms, occurring in the Llyn-cum-Bychan and “ Cherryfield ” gatherings not infrequently; and the same are also to be found in “Lancashire” and “Bennis Lake” cleaned material. These special varieties were drawn from the Llyn-cum-Bychan speci- mens, and it will be seen that B is simply a link between the extremes A and ©. And whilst it is not invariably so, I find a tendency towards the association, in the frustules, of such a nodule as C, Fig. 4, and such a termination or apex as A, Fig.1; whilst a midrib terminating as in A, Fig. 4, is associated with such an apex as C, Fig. 1. This tendency is (quite accidentally) depicted in the drawings sent with my last paper, and still preserved in the Plates. So far am I from seeing the need of multiplying species on 178 Transactions of the Royal Microscopical Society. what, in the light of the facts I submit, appear mistaken grounds, that I am the rather inclined to see how very many of them might be shown to glide insensibly into each other, having no rigid line between. But this of course would not be enough, unless the developmental history in all the said cases were coincident or nearly approximate—a matter on which I cannot speak. But when, on good authority, three Navicule, called separately by specific names, are affirmed to be capable of being considered one species, so far as their life-history is concerned; and when it is further shown that the “striation”—a permanent feature—is the same in each; in consideration of the fact that both the “shape” of the outline of the frustule and the form of the “nodules” are constantly subject to minute variations, it appears to be a case, fairly made out, of specific identity. This, however, is, comparatively speaking, a side issue ; the great point is, whether it is possible to make what are shown to be the variable features of a diatom—taken in entire independence of its life-history—the elements for determining its species ? There are three things in most Navicule that vary: (1) the general outline of the frustule, (2) the midrib as a whole (although, so far as my examination goes, it is much less variable than the outline of the frustule), and (3) the tenwity of the beading or striation. There is one thing (broadly speaking) which is in- variable—it is the character or arrangement of the beading.* * T write thus guardedly because I am convinced, as I have already hinted, that with a complete knowledge of the life-histories of all the forms of the Navi- cules there might be an immense reduction of what are now known as specific forms. ‘Take, for example, such a prominent form as NV. granulata and compare with it WV. latissima, N. humerosa, and N, brevis on one side, and NV, marina, N. pusilla, and J, carassivs on the other side, and I suspect that complete search would find all the intermediate forms. In like manner there can be but little question that in either old or living forms the intermediate steps between JV. rhomboides and N. cuspidata might, although perhaps with difficulty, be found. The transition forms between Pleurosigma fasciola and P, macrum and P. pro- longatum are almost at hand without searching; and I imagine that many of us who have examined a large number of slides or “ material” of the forms P. angu- latum, P. quadratum, and P. elongatum have often wondered at what point the one ceased and the other began. Of course if their life-histories are essentially different from each other, then their remarkable similarity and blending into each other must be regarded merely as coincidence, or in some sense “mimicry.” But if their developmental histories only differ enough to account for their differences of form, then I think such forms extremely instructive and well worthy the care- ful study of those who seek for direct and living proof of developmental changes in existing organisms: a matter much more readily discovered in minute forms, seen together in enormous numbers, and subject to critical investigation in their entirety, than in the larger and more complex organisms, which, when taken in the greatest numbers in which they can be found, for critical examination, are but, relatively, few indeed. In fact, therefore, in saying that even the arrangement of the beading in the diatoms, chiefly discussed in the above “ Note,” is permanent, I merely mean that it is so relatively to the other parts; but in all probability this permanence is only, in reality, an indefinite persistence, a feature, that is to say, immensely jess liable to change or vary than others. Gu, 1798") I—The Exhibitor: a Novel Apparatus for showing Diatoms, &e. By the Hon. and Rey. the Lord 8. G. Osnornz, B.A., F.R.M.S. Witx you kindly permit me to introduce to your readers a little addition to the apparatus of a microscope, which I am sure will well repay its cost, and the little practice in its manipulation, required for its perfect success. In nearly thirty years’ enjoyment of the microscope—using it for many hours on the greater proportion of my days, applying it to all kinds of investigation—I always coveted some simple means of getting a good oblique light for illuminating, under the higher powers. I have bought and borrowed a good many ingenious in- ventions for the purpose, and have generally succeeded in getting fair results, but always with more trouble than was quite agree- able, to say nothing of the expensive nature of the means used. After a great deal of experiment, and much hard work, with very indifferent tools, I am at last quite satisfied. I have for the last few months had more enjoyment from the microscope than I ever had before, and this from a very simple contrivance. The Dia- tomacez I had observed under other modern inventions, but until now I never saw their real beauty, or got such satisfactory informa- tion as to their construction. I will now give the plainest description I can of “ the Exhibitor.” I take a “Darker” stage, as used for polarizing. I have two counter-sinkings made on its stage front in the revolving ring; one, the top one, rather larger in circumference and shallower than the lower one. Into the lower “sinking” I drop a disk of blackened metal with a small kettledrum lens mounted in the centre. Into the upper “sinking” I place metal disks with certain apertures made in them; the front of these disks is just level with the face of the stage, the back close to the front of the disk holding the small lens. I have a fine screw-worm cut into the back part of the re- volving ring, coming up just below the lower counter-sinking. Into this screws a ring of brass carrying a bull’s-eye or kettledrum lens, of about the diameter of a shilling. The screw movement having a milled edge, it can thus be focussed as required with the small upper one. It will be at once seen that the Exhibitor is thus nothing more complex than a Darker stage with two kettledrums, the larger receiving the light from the lamp, transmitting it to the small one, which latter then delivers it at the back of the metal disk which is flush with the front of the stage, the screw movement enabling the observer to focus the two drums. As to the apertures to be cut in the metal disks, after a great 180 The Exhibitor. By the Hon. and Rev. the Lord 8. G. Osborne. deal of study I have arrived at the conclusion four such apertures will meet all that can be desired. No. 1, a fine “slit,” in length about the diameter of the upper “drum,” i the centre. No. 2,a similar aperture, a little way, say not quite its own length, from the centre. Nos. 3 and 4, a pin-hole and triangle, also a little out of the centre; these may all be cut in one disk. On the stage I have two steel springs for holding the slides, giving the means of shifting them in any direction. . Now for the modus operandi. Having screwed the lower drum home to the extent of the screw, drop in the disk with small drum (I have three of different diameters and projection); on this place the aperture disk; place and cramp the Darker on the stage; turn the mirror, and place the lamp so as to get the aperture lighted up, but not with the brightness as with direct illumination ; put on a slide, say of Angulatum (I prefer those of “ Moller”); adjust the mirror until you get a rather red appearance on the slide at the side farthest from the lamp. Focus down on this: when you come on a bright clear light, like that obtained from ordinary sub-stage illumination, by moving the stage laterally you will arrive at a portion of the slide with darker and darker background as you con- tinue to move it. It will now depend upon manipulation of the mirror to bring the object on this ground to its best definition. A little practice soon makes this easy. Supposing you have got an “ Angulatum” well shown—i.e. on dark ground—clear and erisp ; turn the milled head of the Darker stage and you will thus intensify or moderate the light. Having found with any one aperture good definition of any one object in a slide, with your fingers you can bring any specimen in the slide over this spot. I have thus brought every single object in the Typen-Platte of Moller successively in view, developing their respective beauty in a way I had hardly thought possible. I rarely use a mirror, infinitely preferring the Abraham’s achro- matic prism adjusted to the mirror bar; I can by my hand so alter the direction and amount of light with this, 1 desire nothing better. I use the ordinary Bockett lamp and condenser, with a small flame edgeways to the prism. I have worked of late chiefly with a },th of Zeiss, which I find quite capable of resolving almost every test on which I have tried it: it brings out both sets of lines on the Rhomboides, showing where they intersect. A 4 inch of Andrew Ross also gives me wonderful definition. The 4 and 1 inch of the same maker, with binocular, the objects on pitch-black ground, bring out many with a distinctness I have failed to get any other way. I prefer objects mounted dry, but seldom fail with any; asa proof of the way I now get definition; having dissected and mounted the gizzards of the Rotifers, 1 thought I knew their The Phytoptus of the Vine. By Prof. Giovanni Briosi. 181 mechanism well; I now find I had never before seen a row of teeth, shown clearly under the Exhibitor. I use it now for white- light illumination ; indeed, I scarcely use any other illuminator. It requires practice and patience to master its manipulation, but well repays it. p I have placed my models in the hands of Mr. Baker, of High Holborn, Mr. Curties having been here to see me work the instru- ment, and having lent me great assistance in getting lenses, &c., made for me. He has fitted one for me exactly as described above, and I find it perfect in use. I have no doubt but he will have them constructed at a moderate price, and show their use to anyone who may apply to him. I shall be more than satisfied if any of our Fellows get a tenth part of the pleasure I have had in the use of this little affair. That it may be capable of improvement I can conceive, and shall be most glad if it is so improved. by those who are more scientific than myself. SIDMOUTH. III.—On the Phytoptus of the Vine (Phytoptus vitis, Landois).* By Professor Giovanni Briost, of Palermo. Pirates CLXXVII. anp CLXXYVIII. Marcetio Matpieut has been the first to investigate scientifically this evil, which attacks many other plants besides the vine. This disease consists in a kind of protuberance which is formed on the leaves, which in consequence assume a characteristic speckled aspect. These protuberances, galls, or cecidii,t have, for the most part, a roundish or oblong, sometimes an irregular form, especially when through spreading they run one into another, assuming in conse- quence various sizes, so that leaves are found (at least at Favara) * Translated from the Italian by W. R. + Professor Targioni Tozzetti proposes for this disease the name of Zrinosy (it was he at least who did, I believe), but to me the name of Phytoptosy seems more appropriate from the moment that it has been proved not to be due to a fungus (Zrinewn), as it was once thought, but to a mite (acarus), the Phytoptus. t{ As the word gal/ could probably be only applied to pathological products of more or less roundish form, Thomas, to whom we are indebted for most accurate researches about this disease, proposed ultimately to designate by the Greek word cecidium every abnormal formation (in which the plant takes part) of the plants, caused by parasites; hence diptera-cecidium, acaro-cecidium, myco-cecidium, &e., according to whether the galls are due to diptera, acari, or fungi, &e. Besides grouping in two large categories all these varieties, viz. those caused by attacks of parasites with negative cones, and those due to attacks in other parts of the plants, he called the first acrocecidii and the second pleurocecidii, and lastly ceecidozoids the animals, cecidophyti the plants producing parasitism. Beitrige z, Kennt. d. Milbg. n.d. Gallm. in Giebel’s Zeitsch. f. d. gesammten Naturwissen- schaften, vol. xlii. p. 517. 182 The Phytoptus of the Vine. By Prof. Giovanni Briosi. which, thus attacked, have not a single spot left healthy and uncovered. Convex on the upper and concave on the under side of the leaves, these parasites present themselves covered with minute hairs, whitish in spring, later on reddish, or of a more or less dark tobacco colour. Fig. 1 represents a vine leaf slightly diseased, seen from beneath where the galls appear concave. : On the upper side the galls retain in the beginning the green colour of the leaf, turn yellowish later on, and become even brown, according to the force of the disease or the variety of the vine. Malpighi thought that the galls were caused by the drops of a liquid which he saw deposited by insects on the leaves together with eggs, and to which liquid he ascribed a fermenting action. Afterwards Malpighi’s explanation did not seem satisfactory, and many naturalists studied the phenomenon of the galls of the plants, amongst whom Persoon, Fries, Réaumur, Unger, Schlech- tendal, Fée, Lacaze-Duthiers, Vallot, Pagenstecher, &c.; and also, in the past few years, Landois, Thomas, and Sorauer published most important works on this subject.* Most of them at first saw in the contents of the galls parasitic fungi, and thus were created the genera Taphrina, Hrinewm, and Phyllerium. Palissot de Beauvais believed them algx, and Unger enlarge- ments of the leaf cells; others, directly enlarged hairs. * Publications —Malpighi, On the Excrescences and Tumours in Plants; Persoon, Sinops fungor, 1809; Fries, Observat. mycolog. 1815; Idem, Syst. mycologicum, 1825; Schlechtendal, Denkschrift der botan. Gesellsch. in Regens- burg, t. ii. 1822; Idem, Botan. Zeitung, t. xxiv.; Réaumur, Mémoires pour servir a 'Histoire des Insectes, 11. Mem. ix.; Vallot, Med. Acad. Dijon, 1832, part. d. scienc.; Unger, Die Exantheme der Pflanzen, 1833; Duges, Annales des Sciences naturelles, 2™¢ série, t. ii. 1834; Fée, Mémoire sur la Groupe des Phylleriées de Fries, 1834; Lacaze-Duthiers, Recherches pour servir 4 Histoire des Galles, Annales des Science. nat. 3° série, Bot. t. xix. 1853 ; Dujardin, Annales des Sciences nat. 8° série, t. xv. 1857; A. Scheuter, Troschl’s Archiv fir Naturgeschichte, Jahreang 23, t. i. p. 104, 1857; Pagenstecher, H. A., Ueber Milben, besonders die Gattung Phytoptus, in Verhandl. d. nat.-med. Vereins zu Heidelberg, t. i. 1857-59 ; Landois, H., Eine Milbe (Phytoptus vitis mihi) als Ursache des Trau- benmisswachses, in Zeitschrift fiir wissenschaftliche Zoologie von Siebold und Kolliker, t. xiv. p. 353, and following ones, 1864; Landois and Roese, Bot. Zeit. 1866, No. 38, p. 293; Thomas, Fr., Ueber Phytoptus Duj. und seine grossere Anzahl neuer und wenig gekannter Missbildungen, welche diese Milben an Pflanzen hervorbringen, con. I. Tay. in Prog. d. Realschule zu Ohrdurf, 1869 ; Idem, Schweizerische Milbengallen, Verhandlungen der St. Gallischen naturw. Gesellschaft, 1870-71; Idem, Milbengallen und verwandte Pflanzenauswiichse, in Bot. Zeit. 1872, No. 17, p. 282, and following ones; Idem, Entwicklungs- geschichte zweier Phytoptus-Gallen an Prunus, in Giebel’s Zeitschr. f.d. ge- sammten Naturwissenschaften, t. xxxix. p. 193, and following ones, 1872; Idem, Beitriige zur Kenntniss der Milbengallen und der Gallmilben; Idem, Die Stellung der Blattgallen an den Holzgewachsen und die Lebensweise von Phy- toptus (Zeitschrift f.d. gesammt. Naturwiss. t. xlii. pp. 513-537, 1873) ; T. Moritz, in Frauendorfer Blatter, p. 30, 1873; Sorauer, P., Handbuch der Pflanzenkrank- heiten, Berlin, 1874, p. 165, and following ones, > PY ee slee aig Rb ios As a ‘ hi j i sit | inns 63: Oo tan) ? = 5" C) 199) 9) & is The Mon thly, o The Phytoptus of the Vine. By Prof. Giovanni Briosi. 183 At present, however, after the observations of Fée, and the researches of Landois, Sorauer, Thomas, and others, it is ascer- tained beyond doubt that these cecidia are due to the punctures and irritation produced in the texture by the acarz, who lodge in it and live on the leaves. Cutting a very thin lamina across a gall of a vine leaf, and placing it under the microscope, there presents itself, as nearly as possible, a picture such as drawn in Fig. 14, viz. a forest of hairs of various sizes and shapes, and between these minute animals with elongated bodies, with four legs above, with small antenne, and segments precisely as Fée saw them in 1833.* These are mites (acar?), of which there has been formed a species for itself, called Phytoptus, which name was given to them in 1851 by Dujardin (who observed them on the linden and hazel), in order to express that they are really and solely parasites of living plants. These pathological plagues are thus produced. When the animal has found a favourable spot in the leaf, it pricks its texture, and sucks the moisture of the perforated cells. The plant now remedies on its part these punctures and prolonged irritation by supplying the wounded spot with fresh nourishment ; hence an afilux of substance (which can be ascer- tained under the microscope), and consequently an increase in the wounded cell or cells, which in consequence swell and extend externally and cause the formation of elevations. This process is clearly shown in Fig. 14, where f, e, d, are cells in various stages of such transformation. The cells participating in this work are solely the epidermoid cells. Professor Landois, of Heidelberg, to whom we are indebted for the most important and complete work on the Phytoptus vitis,t however, attributes these projections to the underlymg parenchy- matic cells, and says that the epidermoid cells are never trans- formed into projections (f), which is inexact.t These hairs or projections can attain a length four or five times the size of the leaf to which they belong; in fact, I found some of 0°85mm., 0°90 mm. (the average diameter of which was 0:03 mm.), on a leaf which only had a thickness of 0°20 mm. They are generally club-shaped, that is, are thicker towards the upper end, especially when young ; they are more or less irregular, often crooked or curved in various ways, presenting protuberances * Feée attributed the formation of the galls “ to an elongated larva with four legs terminating in little tufts of hair, attached to the upper and fore part of the body, which has transverse rings, and is covered with hairs.” See Targioni Tozzetti, in the Bulletin of the Entomological Society of Italy, 1870, p. 283, and following ones. + Summing up of Targioni in the Bulletin of the Italian Entomological Society, 1870, p. 283. t “ Die Epidermiszellen des Blattes wachsen nie zu Féden aus, sondern die Milbe sticht mit thren stiletartigen Mandibeln durch die Oberhaut die Parenchymzellen des Blattes an.’—Landois’ work, cited amongst the Publications, 184 The Phytoptus of the Vine. By Prof. Giovanni Briosi. and angles. ‘They are unicellular, that is, not presenting divisions, of which I at least saw none. Landois, on the contrary, found them to be formed of a row of elongated cells, which, to my mind, seems a mistake; and fig. 7 of his plate xxxi.* must probably have been taken from a normal hair of the vine (just as one of the hairs of my Fig. 14, which owing to a lithographic error in some plates doesnot reach out of the parenchyma), and not one of those pathological hairs of which we are speaking. These hairs contain a granulated transparent protoplasm, colourless or slightly yellowish when young, and more or less opaque or yellowish-brown when old. ‘Towards their base there is almost invariably found (toward the end of summer) an abundant quantity of starch, in form of very fine granules, similar to that gathered by me in the vessels of the higher plants. Now and then (not always, as Landois says) I also found small - crystals in the hairs, but not in the needle form of the raphides, so abundant in almost all the normal textures of the vine. These hair crystals are in such small quantity that it does not bear out what Landois says of the great waste of tartrate of potash caused by it. The same may be said of the chlorophyll, which I found very rarely even in the young hairs, where, on the other hand, he found it in abundance. Starch I found often abundant in the primary parenchymic strata lying beneath the hairs, which unusual accumulation of material in those cells is due to the abnormal and extraordinary development of organic substance required for the formation of the hairs. The texture of the parts of the leaf corresponding with the galls (harder than the surround- . ing healthy one) is seen more or less changed; the protoplasma of the cells frequently lost its transparency and became dark, either orange or brown. . These changes extend frequently, with various interruptions, throughout the thickness of the lamina up to the cellular stratum, which is bordered off by the opposite side of the leaf (g, Fig. 14). The plant loses, therefore, not only a considerable quantity of plastic substance which produces the pathological texture, but also organs which should produce this matter, grains of chlorophyll, of which the cells, whose protoplasm changes, are full; and it is easily understood that the harm done to the respiration organs must be hardly less than that done at the same time to the assimilation ones. The raising of the texture towards the upper side of the leaf, that is, on the opposite one to the wounded spot, Thomas + * Landois, Eine Milbe (Phytoptus vitis), &c., see Publications. + He says, verbatim: “ Der Intracellulardruck wird dadurch einseitig vermindert werden und muss folglich eine Riichwirkung ausiiben. Der nicht compensirte Druck, welchen der fliissige Zelleninhalt auf die der ausgesogenen Stelle diametral gegentiber- liegende Wand ausiibt, bewirkt die Forthewegung der Zelle selbst und des thr im Wege stehenden Theiles, der Blattspreite.’—Bot. Zeit. 1872, No. 17, p. 286. The Phytoptus of the Vine. By Prof. Giovanni Briosi. 185 explains by a partial diminution of the intercellular pressure, in the wounded and emptied cells, and Sorauer * by a hardening and perhaps a cuticularization of the cells due to the action of the atmosphere, which penetrates into the structure of the wounded cells. Now, without wishing to set these causes entirely aside, I think that the same forces which produce the hairs also cause this phenomenon. In fact, the afflux of the substance which takes place towards that spot of the leaf, where a gall begins to be formed, must extend by endosmosis and exosmosis more or less to all the strata of the texture lying in the thickness of the leaf, thus offering to all the cells of the lamina in the region correspond- ing with the wounded spot a more than usual nourishment. Whilst therefore the cells of the under side of the leaf discharge so much material, owing to the hair production, those underlying, up to the epidermis growth of the upper side, participating in this increased nourishment must of course grow and swell, which they (to my mind at least) cannot do without producing an incurvement of the lamina of the leaf, since the texture which compasses the gall in its normal state cannot grow with the same force and rapidity on account of the lesser nourishment. We now come to the mite, or acarus, the cause of the disease, This animal, belonging to the species Phytoptus Dujardin (Phytoptus vitis, Landois), is invisible to the naked eye, and its extreme smallness renders the study of the same, even with the microscope, most difficult. This explains why, notwithstanding the most painstaking researches of distinguished scientific men, there is still some doubt about its formation. The body is long, flexible, almost cylindrical, tapering off at the two extremitiés, which are slightly inclined towards the belly (Figs. 2, 3, 11, 12). In front it has two pairs of legs, which, when extended, project a little (about 0°01 mm.) beyond the extremity of the head. It is covered with transversal rings, which extend on one side to the insertion of the hinder pair of legs, and on the other to within a short distance of the anal opening. The cephalo-thoracic region is smooth, viz. without rings, whilst a very small depression, which, however, can always be distinctly recognized, separates it from the abdominal region. Above, nothing distinguishes the head from the thorax (which is common indeed to all arachnida, they having a cephalo-thorax), one superficies continues on both the segments, and the front part, which is turned down, terminates in a conical trunk. The proboscis communicating with the head is hollow, open in front (Fig. 12, m), and behind terminating at the cesophagus (Fig. 5, 2). On the abdominal side, that is, the one opposite to the dorsal, this cavity opens longitudinally, and shows an almost * Handbuch der Pflanzenkrankheiten, p. 171. 186 The Phytoptus of the Vine. By Prof. Giovanni Briosi. triangular fissure ; the smaller and hindmost side is represented by the under and triangular lip (Fig. 12, 2) of the mouth. © This opening is not always open, as the animal can bring the lateral sides so near as almost to touch one another, and also the sides of the angle projecting from the lower lip (Fig. 3), thus forming a tube which it uses for sucking, This cavity seems to enclose two very small mandibles &, 7, lamellary, and terminating in a pointed manner, which sometimes are placed on one another in such a manner as almost to resemble a single point (Fig. 5). The animal can draw in or lengthen these mandibles at pleasure (indeed they are seen in various lengths, and sometimes not even the smallest point of them projects or can be distinguished), and they can reach up to the front end of the opening, and perhaps even beyond. With these the mite must prick the leaves in order to suck the juice afterwards with the cephalic or buccal extremity which is transformed into a tube. The length of the thoracic region, from the point where the rings end to the extremity of the head, measured on the average 0°0265 mm., in animals whose whole length was 0°09 mm., viz. about one quarter of the total length of the body. ‘The development, however, of the curved upper or dorsal line of the cephalo-thorax of the same animals, from the spot where the dorsal bristles are inserted up to the top of the head, was on the average 0°0306 mm. ‘The skin of the abdomen, as said before, is externally covered with ring-like elevations, which are found flat and nearly level with the axis of the body, and cease all of a sudden at a short distance from the anal opening, leaving a small part of the belly (about 0-0085 mm.) perfectly smooth. I never counted more than seventy rings, generally only from sixty to sixty-six; their size in already developed animals varies from 0°00111 mm. to 0°0017 mm. Sorauer in the Phytoptus piri found, however, from fifty to eighty rings; and Landois in the Phytoptus vitis counted from 120 to 180, each measuring 0°0013mm. But as, according to Landois, the average size of the longest (female) animals is 0°13 mm., with a diameter of 0°035mm., the numbers of the rings must necessarily be a mistake, as otherwise the length of that part of the body which is covered with rings would exceed that of the whole body. Under great enlargement I observed that these rings are not smooth or uniform, but that each of them result from a series of raised corpuscles, just as Sorauer saw them in the Phytoptus piri. The anal opening is placed at the lower end, in the middle of a kind of disk which is a little hollowed out, in which the body terminates. On the body I found six pairs of bristles, two on the dorsal surface (one on the first, the other on the last ring), and four on The Phytoptus of the Vine. By Prof. Giovanni Briost. 187 the belly. The first pair of the latter are placed between the ninth and twelfth ring (counting from the side where the head is), the second pair between the twentieth and twenty-second, the third pair towards the thirty-eighth ring, and the last pair invariably at the last but five rings. The hairs of the first dorsal pair are generally upright, diverging, and turned down at the end. The hairs of the last pair are nearly parallel with the axis of the body, turned towards the anus, the shortest and the closest placed towards one another (f, in Figs. 2,5). Landois, however, counts on the belly only six or seven large bristles; and Sorauer on the Phytoptus pert counts also six pairs, only slightly differently placed, as I found them on the Phytoptus vitis. The legs, colourless and nearly transparent, seem to be com- posed of six joints; the first, by which the leg is inserted on the thorax, corresponding with the coaa of insects, carries always a long bristle (Fig. 18); the second, which is the longest and most robust of all, shows two ring-like elevations, on the side of one of them being attached a second bristle; then follow three rather short divisions, the second last having a third bristle or hair pointed forward, and of such length as almost to reach to the extremity of the joint, which forms the fifth division, and on this is _ Seen a kind of strong and pointed style in the centre, bearing five appendixes or lateral bristles, so as nearly to resemble the form of a feather. There is also a small cylinder (through a lithographic error in the Plate ending in a point) bent forward and downward, which covers, so to say, the feather or thorn, and seems to protect it. The small cylinder is a little longer than the feather, and larger (the average of three which were measured was 0° 0066 mm. length, 0-00085 mm. diameter). The length of the legs in animals whose bodies measured on the average 0°90 mm. was 0°025 mm., and the diameter 0: 00225 mm. at the coxa. Neither description nor drawing given by Sorauer of the tarsus of the Phytoptus pir correspond with those of the Phytoptus vitis described in the foregoing, and also drawn by Landois, who, how- ever, changes the small cylinder into a bristle. The legs are compressed at the sides, and therefore if seen sideways appear larger than seen in front. Landois distinguishes in the legs three divisions only, but says that there are in the middle one (corresponding to our second one) two slight elevations, and in the third, two or three kind of loops or ring-like indentures. I agree that the first ones may be simple elevations, but the second ones appear to me true divisions of parts, and because of them I count five, which added to the tarsus, form therefore six parts or divisions for each leg. The animal walks very quickly notwithstanding the distribution of the moving organs, which is little suited to the shape of the VOL. XVII. P 188 The Phytoptus of the Vine. By Prof. Giovanni Briosi. body. It generally moves (raises or lowers) two legs at once, the right fore leg and left hind leg, or wice versd, and sometimes (for instance, when tired) it assists with its body, putting on the ground the anal extremity, which seems to act as a venthole (ventosa). In this case the body, bending semicircularly, shortens itself by draw- ing in as a leech, and the anus, whilst now nearly approaching the head, becomes fixed to the ground (or leaf), whilst the animal, using it as a support, lengthens itself by advancing the fore part of its body, and repeating the manceuvre. This cecidozoid when walking seems to put on the ground first the tarsus with its small cylinder, which, contrary to what Sorauer assumes (who believes it to be immovable), appears to me to be articulated and endowed with vertical motion, which allows the animal to assume a quasi normal position in that part on which the tarsus itself is inserted, and it is on this that the animal supports itself. The feather-like process too is articulated, and endowed with a lateral motion. The legs as well as the hind part of the body must be furnished with, relatively speaking, very strong muscles in order to allow of such a rapid motion. Under the line of insertion of the second pair of legs at the beginning of the abdomen, exactly after the second or third ring, are the genital organs, which outwardly appear as a kind of valve or sucker, whichever you may call it, smooth, attached to the skin of the body, above, and free below, and terminating in a (circular) arc-like curve. This valve, sometimes shut, sometimes open, covers the genital organs, hiding them almost always from the observer's eye. Once only, out of thousands of observations, I happened to see under it an oblong slit, around which ran a strong muscular ring, which had the aspect of a vagina. This detail has not been drawn, because the preparation was spoiled ; however, it resembled nearly fig. 6 of Sorauer.* In one pair of animals I saw in the region of the genital organs a fissure turned upwards. Of the male organs I know nothing whatever, outwardly the sexual organs present one and the same form in all animals. The male, however, appears to be smaller than the female, I having several times found two animals closely stretched together on their bellies, which I retained in state of copulation (in alcohol), of which one invariably was smaller than the other. If, however, one does not wish to take into account this difference in size, a very uncertain distinction, since even amongst the small animals there are some found with eggs, then I would presume to say that the male cannot be distinguished from the female with certainty, * Handbuch der Pflanzenkrankheiten, Tay. 1%, p. 122, The Phytoptus of the Vine. By Prof. Giovanni Briosi. 189 unless pronouncing males all animals in which no eggs can be discovered. Sorauer, and before him Scheuten, found in the Phytoptus pore animals of two distinct forms, that is, besides those cylindrical ones described here, others larger in front and round like egg ‘tops (Spitzeirunde), which were supposed to represent the male form in complete development. On the vine, however, I never could see any other but the variety of the cylindrical form, and Landois too seems only to have found this one, as he does not speak of an other. The animal of Figs. 11, 12 (laterally and in front), with valve entirely shut, may be to my mind either male or female, in which no eggs can be discovered. Once I had the opportunity of observing very closely the esophagus, the beginning of which is seen in n, Fig. 5; it is a tube with a very thin coat, which, as it descends, is enlarged to a kind of small bladder or bag, which is seen at the back part, towards the dorsal (at the same height about as the genital organs), which must take the place of the stomach. The intestines, how- ever, are lost below the stomach, and sometimes only the last part, ending at the anus, reappears. In the abdominal region there are often found oval corpuscles of various sizes, the largest in front, the smallest behind ; all con- tained in an oblong tube or bag, which ends in the genital valve on one side, and extends towards the anus on the other. The first are eggs in various stages of development, the second the ovary. The eggs are discharged by the opening of the valve (a, Figs. 2, 3), and I believe I have caught an animal in the very act of ex- pelling matured eggs, pretty far out already, as seen in Figs. 2, 3, representing the said animal laterally and in front. The ovary occupies the abdominal region, viz. nearer the abdominal surface than the dorsal (contrary to the intestines), and in the fore part, where the most developed eggs are, it seems to fill up nearly all the internal cavity of the animal. In the cecidozoid of Figs. 4, 5, the ovary was seen partly hanging out of the body, which was torn from above. The eggs when leaving the body are covered with a glutinous substance, on account of which they adhere to the objects on which they fall. Thus they are often found laterally suspended from the hairs C, where the mother must have deposited them. The egg has a somewhat elongated shape, and its contents when leaving the body of the mother appear uniform and finely granulated (Fig. 6). As it increases in volume one begins to distinguish in the interior a centre line (Fig. 8), afterwards the roundish shape of the outline of the embryo (Fig. 7); and even before breaking the vitelline membrane one can perceive inside already the animal rolled up in p 2 190 The Phytoptus of the Vine. By Prof. Giovanni Briosi. itself, with the outlines of the head already sketched and distinct, and with the traces of the rings on the body (Fig. 9). In Fig. 10 an animal is represented which scarcely left the vitelline mem- brane a, to which it is still adhering (attached). In this stage no hair could be seen as yet, neither were the legs all formed. The smallest animals I found measured 0°045 mm., and there I saw already the posterior dorsal hairs (which seem to be formed first) and the small cylinders of the ¢ars¢. The largest animals I found reached 0:1513 mm. in length, and between these two limits I found every size. I have said that this mite (acarus) has four legs only. Landois, however, found under these well-developed legs, two other rudimentary pairs. He relates that these acari, before they have reached their complete development and are fit to generate, pass through at least four changes: the first taking place when they leave the egg and get the tarsus projections; in the second they become simply larger; in the third they get the first pair, and in the fourth the second pair of rudimentary legs. Thus, he adds, the general rule, that all the acarzi when fully developed possess four pairs of legs, is fully confirmed.* I believe that Landois is mistaken; the four rudimentary legs, represented by four small appendixes, each terminating with a bristle, I have been unable to perceive. ‘There are, it is true, sometimes found animals who might easily give rise to such an idea, because on the spot where he puts the rudimentary legs there is an elevation terminating in a bristle; but under close observation one sees that this is due to the genital valve, which is found more or less raised by the action of the body under it, which seems to prepare itself for the expulsion of eggs. ‘Thus the bristles do not form part of the raised appendixes, but are attached to the hairs of the body, nearly at the margin of the genital aperture, as seen in Figs. 2 and 3, from which I conclude that these animals do really constitute a special genus of acart, which have only four legs. These arachnida seem to possess a most extraordinary tenacity of life. Sorauer saw them moving the legs after being twenty, and Landois after twenty-four hours in glycerine.t From the fact of their being able to live so long in a liquid like glycerine, Landois argues that their respiration is neither pulmonary nor tracheal, that it cannot even be cutaneous, and concludes that they must breathe through the anal opening. These acart are found on the vine at whatever season of the year it is examined, and Landois is in error when he affirms that they all die at the first diminution of temperature, that the eggs only remain between the hairs of the leaves, which fall in autumn, * Kine Milbe als Urs. d. Traubenmiss, p. 357. + Frauendorfer Blatter, 1873, No. 30. (Sorauer.) The Phytoptus of the Vine. By Prof. Giovanni Briosi. 191 eggs destined to produce in spring the young phytoptus, who climb up upon the new vine shoots. In autumn, on the contrary, these animals emigrate from the leaves, in order to nestle under the bracts which cover the winter buds, and perhaps to the roots where Moritz found them in the months of January and February, and on which they would cause the same alterations similar to those caused by the Phylloxera vastatriz. Between buds, gathered in January (in the midst of the cylindrical and very long hairs which are found under the scales or exterior bracts for the pro- tection of the buds), I found a large number of these cecidozoids, a little lethargic, but alive, and disposed to activity when exposed to heat. In one bud I counted more than 200 animals, in another 212, in a third 112, and in a fourth 72, and I do not think I have seen them all. Analogous observations have been made by Thomas * on the buds of Pirus communis, Prunus domestica, Sorbus aucu- paria, Tilia grandifolia, Alnus glutinosa, Acer campestre, &c. ; and Sorauert found them alive between buds of trees which shortly before had been exposed to a cold of —18° R. At the first mild breezes in spring, and the swelling of the buds, the animals regain breath, and begin again to lay eggs, which they deposit direct on the young leaves of the developing bud; thus the young ones are scarcely born, when they find already within reach the food which nourishes them. With the first young leaves of the vine, indeed, are discovered the first galls under the form of small spots of a colour little different from the parenchyma of the leaf, scarcely raised on the upper sides, and which can be specially well discovered by examining the young vine leaf by holding it between you and the sun. The distribution of the galls on the plant is also regulated by certain rules, which particularly depend on the conditions of nourishment of the animal, that is to say, on the one hand, of the faculty and force of the organs taking the nourishment, and on the other, of the mode of production and development of the latter. Thus it is that one can observe in May, on the stems attacked by the Phytoptus (when the vines are in full force of development), 1st, shoots which only present galls on the original and exterior leaf of the bud, which produced the branch and remained at its base; 2nd, shoots in which the galls, besides on the base leaf, reappear along the branch in two or three spots, leaving long intermediate spaces with perfectly un- hurt leaves; 3rd, shoots at last, in which the galls have left unhurt almost all the principal leaves, that is, those directly attached to * Beitrage z. Kennt. d. Milbg. u, Gallm. Giebel’s Zeitschr., &c., vol. xlii, p. 517, and following ones. + Hand. d, Pflanzky. p. 177. 192 The Phytoptus of the Vine. By Prof. Giovanni Briosi. the branch, and are found instead on the small leaves of the lateral small branches, growing out of the axils of the principal leaves, besides on the extreme end-bud of the shoot itself. This proves that the animal goes to lodge on the young textures which are still growing, probably because when the leaves are fully developed, their texture hardens so much, that the animal’s mandibles can pierce it no longer. And we owe probably to this circumstance, taken together with the other that the development of the plant in spring particularly seems to proceed more rapidly than the multiplication of the animal, that the disease does not cause all the harm to the vine which might be expected. In fact, we see that before the animal has multiplied to such a degree as to have to emigrate, for instance, to a lateral bud, the principal leaves of the stem are already developed in such a manner and way as no longer to allow the animal to rest thereon, and it leaves them, in fact, untouched, and goes higher up in search of a new bud. The invasion must be very strong if the plant cannot save a good part of its leaves. Thus, in fact, whilst in some vineyards in Favara the number of stems attacked by the galls was very large, there were very few in which the disease had spread to all the leaves. And where the evil was compassed within a certain limit, the plant did not seem to suffer much from it, whilst, however, on the stems which were almost totally invaded, the damage was so serious as to check the development of the fruit, the fruit buds having always remained so small that they could not arrive at maturity. The fundamental functions of the vine plant, as shown, that is, ass¢milation and respiration, are disturbed, and the sad consequences can, of course, not astonish us. However, the assertion of Landois,* that this disease is not less damaging to the vine than the renowned fungoid growth Ozdiwm Tuckeri, Berk., appears to me exaggerated. Certainly, if in one vineyard every year this disease should extend and augment in intensity, the products would be not a little dimimished. However, it is a fact in Italy (at least) where the disease is old, that (as far as I know) there are few examples of excessive damage. With regard to the remedies, Landois, assuming that at the end of autumn the animals die, suggests collecting and burning the leaves which fall in autumn and get dry under the plants, which leaves harboured the eggs from which are produced the animals in next spring; but after what has been said before, this remedy is insufficient, and perhaps is not worth anything (in dry leaves, gathered in December, I did not find any eggs, but only husks and dead animals, deformed and shrivelled in every case), * Memoir cited, p. 353. NY : eS ’ — G 9 A jek QO f (2) n e 13) ert = tan) » [= ie) — The Phytoptus of the Vine. By Prof. Giovanni Briosi. 193 since these cecidozoids not only do not die, but take their winter quarters on the plant itself, and develop with it. If the animals are in the buds, a large number will then be taken away with the pruning, and therefore the stems which showed the disease in the preceding summer should be kept as short as possible, the cut twigs carefully gathered, carried away out of the vineyard, and burnt. As to those portions of the branch which remain on the stem, as the remaining buds cannot be cut away under pain of almost losing the whole of the next harvest, one should in spring, when the first shoots have reached a certain length, and the galls have become apparent, cut off the leaves which are attacked most, and also the top of the most infested branches, carry them out of the vineyard, and throw all in the fire. This operation should be undertaken during the sunny hours, walking towards the sun, because the galls which at that epoch are still very small and almost green, can be easier seen by light which comes through the leaves. And this operation—easily carried out in the majority of the vineyards, where the vine is low and within reach of hand—repeated, conjointly with the short pruning, for some time, would, in my opinion, in a few years result in the destruction of this unwelcome visitor. EXPLANATION OF PLATES CLXXVII. AND CLXXVIII, Fic. 1.—A slightly attacked leaf seen from beneath. Fies. 2, 3.—Phytoptus laterally and belly upward, with genital valve a raised, and eggs b, which are about to emerge. (Enlargement 850 diameters.) Fiaes. 4, 5.—Phytoptus same position as above, with eggs, and part of ovary m, which projects out of the body torn above. (Enlargement 850 diameters.) Fies. 6, 7, 8.—Eggs in various stages of development. (Hnlargement 850 diameters.) Fig. 9.—An egg, much developed, which shows the embryo, with the traces of rings and the appendages of the head and the legs already distinct. The embryo detached itself from the vitelline membrane under repeated treatment with solution of potash and acetic acid. (Enlargement 850 diameters.) Fic. 10.—Phytoptus scarcely come out of the egg a. (Enlargement 850 diameters.) Fas. 11, 12.—Phytoptus lateral and front views, with genital valve lowered and shut, mandibles, &c. (Enlargement 850 diameters.) Fic. 13.—A leg much enlarged. Fic. 14.—Section across a gall, b; Phytoptus and eggs; f,e,d,A, hairs in various stages of development. Fic. 15.—Head of Phytoptus, seen across. ( aere9 IV.—On the Extrusion of the Seminal Products in Limpets. By W. H. Datz, Smithsonian Institution, U.S.A. In a paper published in the American Journal of Conchology, Part 3, 1871, I brought together a summary of the various details published from time to time by various naturalists, upon the anatomy and physiology of this group. In that paper it was shown that the manner in which the seminal products were freed from the ovary and testis, and the passage by which they reached the exterior, were unknown, and from the investigations of Lankester and myself, that the existence of the oviduct figured by Cuvier,* if not actually disproved, was at least a matter of grave doubt, and had not been confirmed by any subsequent examination. Lankestert had suggested that the passage of the ova to the exterior was made through two orifices first de- scribed by him and termed “capitopedal orifices.” These were said to open, “one on each side of the head in the angle formed by its junction with the muscular foot, and (internally) opening into the blood sinus surrounding the pharyngeal viscera. He also described an opening communicating between the “ peri- cardium and the supra-anal articulated sac,’ or accessory renal organ. The latter I have never been able to demonstrate to my own satisfaction, but I do not assume to dispute its possible exist- ence. Instead of opening externally in the angle formed by the head and the foot, the “capitopedal orifices,” if I have correctly identified them, are situated on the back of the neck, so to speak, or more properly on the transverse portion of the integument above the head and in front of the main pericardial chamber in the angle formed by the neck and the inferior surface of the mantle over the head. Mr. Lankester found them in Patella vulgata, but I have never been able to detect them in the few alcoholic specimens of that species which I have been able toexamine. In fresh specimens of Acmexa patina and testudinalis, I have generally been able to find them, and in the living animal they are of an orange colour. In Ancistromesus Mezxicanus they are quite prominent in some cases and almost imperceptible in others. They also differ in character. In Ancistromesus (one of the Patellide), they appear as true orifices, in the acmaas they present the appearance of an elongate, narrow, glandular mass, from which, internally, a duct is not always traceable. In some individuals they appear entirely absent or abortive. My own opinion of their function is, that they are aquiferous pores, such as are common to many mollusks, through which water passes into the circulation directly in the * “Mem. sur Jes Moll.’ 15, 1817. + ‘Ann. Mag. N. H.’ xx, p. 334, 1867. Seminal Products in Limpets. By W. H. Dall. 195 Patellide and by a process of straining through the glandular mass in the Acmeide. Whatever their office, it can hardly be of fundamental importance, or they would not be so frequently found in an abortive condition. Whether in some cases they may be indirectly in communication with the renal sac is of little conse- quence, as, in the paper alluded to, I have shown that in some genera the pericardium is so situated that there can hardly be any such communication, and in so homogeneous a group as the limpets it is unlikely that such an anatomical character, if important, should be inconstant. Moreover, through the intricate channels alluded to, the ova which are of considerable size could hardly be propelled without some special muscular arrangement which does not seem to be present in any case examined. Anxious to set at rest a question of so much interest, and which for so many years had puzzled anatomists, I have lost no opportunity of dissecting animals of this group, especially the large species in which the characters might be supposed to be more evident. The opacity of the shell and the impossibility of getting at even the external orifices of the viscera without destroying the life of the individual, proved effectual obstacles to the study of these functions in the living animal. While in the field, from 1871 to 1874 inclusive, I made dissections of many hundreds of acmzeas with no definite result, except that of finding that the sexual products appeared ripe in only a small portion of the ovary at any one time, and in the acmeas the portion most usually in that condition was the extreme right-hand part of the anterior end, immediately below the floor of the larger renal sac. No oviduct or opening was in any case demonstrated. Somewhat discouraged by repeated failure, on leaving the field- work in which I had been engaged, the matter was deferred until a better opportunity should arise. Some time since, a large number of specimens of the giant limpet of Central America, Ancistromesus Mewicanus, were obtained by the Museum of Comparative Zoology from the naturalists of the ‘Hassler’ expedition. By the courtesy of Professor Alex. Agassiz a number of these were turned over to me for dissection. In this species the right supra-renal sac is quite large, covering the entire superior surface of the animal between the muscular attachments.. The viscera are coiled below it in the usual manner, except that in ripe individuals the upper outer edge of the ovary or testis extends rather more beyond the peripheral coil of the intestine than in most species. A section then discloses the mem- branes in the following order from above. First, the external delicate layer of the mantle covering every- thing else, and very intimately bound together by tough connective tissue, with 196 Seminal Products in Limpets. By W. H. Dail. Second, the superior wall of the right-hand (and only fully developed) renal sac. By means of delicate, but tough columnar walls of tissue, forming connected cellular cavities, overlaid with semi-glandular tissue for the elimination of the renal secretions, the upper wall of this sac is connected with, _ Third, the floor of the sae, of similar constitution and tough- ness. ‘The two are readily separated owing to the greater delicacy of the connecting tissues, but the upper wall and the mantle, and the lower wall and the tissues below it, are very intimately connected by membranous fibres of such toughness as to render their separa- tion without injury very difficult. A muscular band or mesentery of considerable strength, having, in the specimens of Ancistromesus examined, a width equal to nearly one-twenty-fifth of its length; extends completely around the internal viscera which are compactly bound together by similar tissue. From the floor of the renal sac similar but short mesenteric bands extend downward to the peripheral band, radiating from the apex of the shell, and having, when in their natural position, a somewhat triangular form; the short sides of the triangles cor- responding to the distal ends of the radii, and their plane surfaces being nearly vertical to the horizontal plane of the visceral mass. In the specimen under consideration there were one posterior and ten lateral bands of this nature, five on each side. In details of form and dimensions these vary in different individuals. They widen at their junction with the tissues above and below, and send off numerous fibres in all directions, and especially to the peripheral band. We thus have as it were the entire visceral mass suspended in the perivisceral cavity, free of the floor and sides of the latter (except a delicate anchoring membrane, lying vertically in the median line and connecting the median line of the visceral mass with that of the muscles of the foot), but in contact or close con- nection with its roof which is composed of the floor of the larger renal sac. This sac opens externally by a prominent papilla to the right of the anal papilla, while the smaller (and usually almost abortive) left renal sac, opens by a proportionally smaller papilla to the left of the anal. The specimens were examined by cutting away the solid mus- cular foot, and thus exposing the perivisceral cavity without in any way lacerating its contents, sides, or upper surface. A number of individuals were dissected without coming any nearer to the object in view. At last, however, a specimen was taken up which appeared to solve the difficulties and afford the long-sought-for explanation. It wasa male. The surface of the viscera with one exception was perfectly normal. On the right-hand posterior portion of the periphery of the testis, covered with its usual delicate Seminal Products in Limpets. By W. H. Dall. LOT investing membrane, for the space of an inch from the posterior end of the median line, forward, the ducts were swollen and enlarged. They projected in a marked manner from the smooth and evenly rounded normal surface, like “‘ varicose veins,” except that the ducts are nearly parallel. In the ripest portions the delicate investing membrane of the testis had become ruptured or perforated, and the seminal matter exuding from these punctures had been solidified by the alcohol in little rounded grains or particles, which had not been disturbed by the careful manipulation of dissection. At those points where the congested or enlarged ducts were in mechanical contact with the roof of the perivisceral cavity, that is to say, the floor of the renal sac, numerous minute, but plainly visible, oval perforations appeared. These were oblique to the general plane of the membrane, the opening on the side adjacent to the testis being usually directed somewhat backward instead of vertically downward. They had also something of a funnel shape, being larger on the side toward the testis, and some of them were twice as large as others. The largest had a diameter of ‘015 inches, and would admit the passage of a fine bristle into the renal sac. On applying slight pressure from above, the fluids contained in the renal sac passed through in a minute jet. They were irregularly distributed, corresponding in locality to the ripeness of the ducts of the testis. Except where the testis in its ripe con- dition was in immediate proximity or actual contact with the membranes of the renal sac, no such orifices or pores were to be found. In the other specimens in which the testis or ovary showed none of these signs of maturity, no such orifices could be detected. The membranes in such cases presented a smooth and practically impervious surface in every part. It would seem as if these facts gave a final solution to the diffi- culty as follows: When the ovary or testis is ready to discharge its products, that portion of it which is ripe evinces its condition by an en- largement of the ducts, continuing until dehiscence takes place. Coincidently, the superincumbent membranes of the renal sac (whether by sympathy with the congestion of the seminal organ or otherwise) become lax and perforations make their appearance immediately adjacent to the dehiscent ducts. Through these orifices the seminal products make their way. A contraction of the pedal muscles would be sufficient to cause the ejection. After reaching the renal sac, the question of the extrusion of the ova or semen presents no difficulties. ‘The same agency which empties the sac of its secretions through the renal papilla would suffice to eject the seminal products, which floating in the water would cause the fertilization of the ova as in the case of Chiton. 198 Notes on “ Inclusions” in Gems, &e. By Isaae Lea. The rarity of individuals in a ripe condition in collections may be due to their repairing below tide marks at such times, and hence avoiding the collector. The method above suggested is paralleled in numerous other in- vertebrates, and even some fishes, with non-essential differences of detail. ‘The specimen referred to has been submitted to several naturalists who agree as to the facts. While additional evidence is desirable in corroboration, I feel tolerably confident of the correctness of the inferences drawn from the above facts, which furnish an explanation at once simple and in accordance with experience in other cases, of a very puzzling question. I may add, that the localized turgidity or swelling of the ripe seminal ducts had been previously observed by me on other occa- sions among specimens of Acmxa patina; but having dissected them in most cases from above, removing the membranes not con- nected by tissue with the ovary, and looking more particularly for a permanent duct or passage, the perforations of the renal mem- branes were likely to, and did, entirely escape my notice.—Proceed- ings of the Academy of Natural Sciences of Philadelphia. V.—Notes on “ Inclusions” in Gems, &e. By Isaac Lua, LL.D. In a communication on microscopic crystals contained in gems, which the Academy of Sciences of Philadelphia did me the favour to publish in its ‘ Proceedings’ * a few years since, I gave some figures of these crystals, which I have frequently since verified. I then observed that, beside these intercrystalline forms, there were in most gems cavities frequently so numerous that they amounted to tens of thousands. Since the period of the publication of my paper, I have made very large additions to my cabinet of gems, and particularly those of the Corundum group, sapphires, rubies, and the so-called Oriental topaz, Oriental amethyst, Asteria, &c. In the numerous fine blue sapphires of my collection, I have rarely explored one without finding numerous cavities, and ordinarily also finding the beautiful microscopic acicular crystals, which, when the specimen is cut cabochon, cause the three bands, and these by crossing form the star in Asteria. The cuneate microscopic crystals are also quite common. Cavities, with or without the fluids, are so frequent in crystals, from the soft calcite to the hard corundum, that little may be said as to their occurrence, as they are so common. * February and May 1869. Notes on “ Inclusions” in Gems, &e. By Isaac Lea, 199 Cavities in quartz crystals enclosing fluids have been observed by the older mineralogists, but the kind of fluid, and gas or air, was not ascertained by them. Sir Humphry Davy, in 1822,* investigated the contents of these cavities, and found them generally pure water. The gas-bubbles were sometimes found to be “ azote.” Sir David Brewster, in 1823, + published a memoir of great research and value. He first had his attention called to the examination of fluid in cavities by the explosion of a crystal of topaz when heating it. He found cavities and air-bubbles in nearly twenty different substances, and these inclusions were carefully examined by him. In some of these cavities he observed two fluids { and crystals, and these are figured in his plates. Subsequently, Mr. Sorby pub- lished a long and admirable paper § on fluid cavities and crystals in minerals, with numerous and interesting figures. He con- sidered that the cubic crystals were probably chloride of sodium. In his investigation he proved, by forming artificial crystals, that, in a natural state, the fluid cavities, with their “ inclusions,” must have been formed by aqueo-igneous forces. He gives a figure of fluid in mica, but I have never seen any in that mineral, although many hundreds have passed under my microscope in looking after crystals of magnetite, &c. Mr. Sorby also published a paper on cavities in quartz in the ‘ Phil. Mag.’ vol. xv. p. 158; also with Mr. Butler in ‘ Proc. Roy. Soc. London,’ vol. xvu. p. 299. Kirkel on “ Microscopic Minerals,” Neues Jahrbuch, 1870, p. 80, mentions bubbles and cubic crystals in quartz. He found iron glance and fluid in Eleeolite = Nephelite. In emery, from Naxos, he found fluid in cavities. In 1872, || Mr. Sang published an account of water in cavities of calcite. Very recently, Professor Hartley, King’s College, London, has published a very able paper on the subject of the fluid in quartz, &c.4] He says that Simmler in 1858, offering an inter- pretation of Brewster's observations, concluded that the expansible liquid was carbon dioxide. Professor Hartley states that in many cases the liquid in quartz is water, but that in some cases he found the two fluids; and his very satisfactory and careful experiments show conclusively that the most volatile of the two fluids is car- bonic dioxide. He found in every experiment that the fiuid dis- appeared when exposed to 31° C., and reappeared on cooling. Professor Hartley accords with Mr. Sorby in his reasoning that * ¢Phil. Trans.’ 1822. + ‘Trans. Roy. Soc. Edin.’ 1823. $ These two fluids Professor Dana without any analysis has called Brewster- linite and Cryptolinite. § ‘Journ. Geol. Soe.’ vol. xiv., 1858, “‘ Micro-structure of Crystals,” || ‘ Proc. Roy. Soc. Edin.’ p. 126. q ‘Journ, of the Chem, Soc. London,’ February 1876. 200 Notes on “ Inclusions” in Gems, &e. By Isaae Lea. “at the time of its assuming the solid state, the solution endured a high temperature.” Calcite has been found to contain nearly a quart of this fluid,* but it is not as common to be found in small cavities as it is in quartz. Fluorite.—Cavities in this mineral are rarely found, but they are sometimes seen with fluid and air-bubbles. Apatite.—I have never observed cavities in this mineral, but I have not given it much attention in microscopic examinations. Feldspar Growp.—In a former papert I gave the result of the examination of many specimens of various species. Since then I have examined numerous specimens of Labradorite, and found no cavities, but the black crystals were very numerous. In the moon- stone of this country I have not observed cavities or crystals; but in two specimens, out of about one hundred from Ceylon, I have seen a series of very regular quadrate cavities or crystals which do not appear to have any fluid. Tourmaline-—This interesting mineral is found beautifully crystallized, and of almost all colours, white, brown, green, red, black, &c. The finest are found at Mount Mica, near Paris, Maine.t Some of these specimens have small internal elongate crystals, which are terminated. A red specimen (Rubellite) in my collection has many irregular cavities. One green one from Ceylon has cavities with fluid, and another has very minute black acicular crystals in one direction. In brown crystals from Lower Dianburg, Carinthia, there are rough objects in the interior, evidently another mineral enclosed, which do not require the microscope to detect them. Cyanite.—Of the white and the blue varieties I have not ob- served any well-defined cavities or crystals; but in the grey-bladed cyanite, found at Cope’s Mills, near West Chester, Pennsylvania, there are always, I believe, small black masses which do not take a regular form, but are usually elongate. These may easily be detected by splitting a crystal along its eminent cleavage, and examining the cleavage face with a lens of small power; but a higher power is preferable. Quartz takes upon itself many colours. In it are found cavities in very great numbers, particularly in the clear fine crystals. Those which exist in such an abundance in Herkimer County, New York, and which are so limpid, and finely and doubly terminated, are sometimes furnished with thousands of cavities, even in small specimens, and these are of many various forms, frequently con- * Specimen in the collection of the late Dr. Chilton, of New York. + ‘Proc. Acad. Nat. Sci.’ May 11, 1869. } Dr. Hamlin has published a beautiful little work on the Tourmaline, with illustrations, Notes on “ Inclusions” in Gems, &c. By Isaae Lea. 201 taining fluid. In some cases the fluid may be seen to move by the unaided eye. In these Herkimer crystals, carbon in the form of anthracite is of very common occurrence, and in one of my speci- mens a small portion moves in the fluid of a cavity. These cavities often exist in an entire sheet, almost across the prism of a crystal. * In smoky quartz these cavities are much rarer, as also in ~ amethyst and wine-colour and green quartz. The amethyst is frequently penetrated with crystals of rutile, and these are often very large, sometimes one to four inches long. The Chester County specimens usually have numerous curved filamentous crys- tals, easily detected with a common lens. In Way’s Feldspar Quarry, near Dixon’s, Delaware, there is a very peculiar form of quartz, which is nearly transparent, but somewhat clouded. The fragments of all sizes, from that of a pin’s head to that of a small walnut, are enclosed in a mass of Deweylite. These fractured pieces are of indefinite forms. They are evidently cryptocrystal- line, and look as if they may have been heated and suddenly cooled, and thus fractured. When these pieces are subjected to a high power, there may be detected in them very minute oval cavities in great numbers, and the major axes usually placed in one direction I have never seen cavities in milky quartz or blue quartz. Sir David Brewster found many cavities in rock crystal from Quebec with “ water and mineral oil.” t Topaz.—tIn the various beautiful crystals which this mineral presents, there are frequently found cavities with fluid, and some- times in this fluid may be seen the cuboid crystals described by Sir David Brewster. He found a single fiuid in some cavities, and in others two fluids with “air-bubbles.” He says the fluid does not expand with heat. The Saxony transparent white crystals some- times have cavities, as well as those of pale wine-colour. The Bra- zilian gold-yellow specimens have these cavities very frequently. The clear pinkish are more free from them. I have never observed any microscopic acicular crystals in topaz. Emerald, Aquamarine, and Beryl—constitutionally the same— differ very much in regard to their possession of cavities and their commercial value. So far as I have been able to examine fine specimens of emerald, it is rare to see one without cavities. One which I have, of very fine colour, has many cavities of various forms, in which are included a fluid enveloping generally two per- fect cubic crystals of an unknown mineral. In all cases in this specimen, the second crystal is much the smaller. In aquamarine, cavities are not frequent, and in beryl I have * Sorby, ‘Journ. Geol. Soc.’ 1858, found many cavities, and thinks that the cubic crystals enclosed are probably chloride of sodium, as mentioned above. + The smoky quartz of Pike’s Peak has hexagonal spangles, which may be mica. t ‘ Trans. Roy. Soc. Edin.’ vol. x. 202 Notes on “ Inclusions” in Gems, &c. By Isaae Lea. detected them only in a specimen from Unionville, Penn. In this there is a biangular cavity with a small cubic crystal at an inner angle. Throughout the mass there are small suboval cavities. Garnet.—As a precious stone this is by no means rare, but it is lustrous, and of a fine colour. Cavities and microscopic crystals are very common in this gem.* The cavities are usually irregular and rough, and never to my knowledge have fiuid. On a polished surface of a piece of garnet from North Carolina, nearly an inch long, the reflexion of these crystals covered the whole surface with prismatic colours. Cinnamon Stone.—This beautiful variety of garnet, from Ceylon, as far as I have been able to observe it, and I have some twenty cut specimens, and numerous rolled pieces, has irregular cavities and some crystals, as I have stated in a former paper. Zircon.— With its high refractory power, this is used frequently as a gem, and sometimes sold as a diamond when white and per- fectly transparent. One of the numerous specimens which I have examined has cavities t and microscopic crystals, and a specimen from Ceylon has remarkable dark brown, elongate, fusiform spots, with numerous dotted ones intervening. Chrysoberyl.—The few specimens I have of this beautiful gem have neither cavities nor microscopic crystals, but Brewster ob- served “strata of cavities and both the fluids.” Chrysolite = Olivine.—In some of my specimens I have observed small cavities with fluid. Brewster met with them con- taining “ fluid and bubbles of air.” Spinel.—This gem occurs of several colours. The Spinel ruby, so called, sometimes is very close in colour to the true ruby, but it has not by any means the depth nor brilliancy of the true ruby. In a pale-green specimen of great beauty which I have received recently from Ceylon, I have not been able to detect cavities or crystals. In my former papers I have expressed uncertainty in this matter.f Jolite—This gem is inferior in hardness, colour, and specific gravity to sapphire, but is valued for its peculiar change of colour, being dichroic. One of my specimens is without any inclusions. The other is filled with blue four-sided prismatic crystals, which are long, and enclosed in a nearly white subtransparent mass, These erystals are sometimes broken and their parts prolonged in the mass, and they are all lying in nearly the same direction. Turquoise, with its peculiar and agreeable blue, is never trans- parent, and neither cavities nor microscopic crystals are found in it, * ¢Proc. Acad. Nat. Sci.” February and May 1869. + In a specimen in Dr. Leidy’s fine cabinet there are anastomosing cavities. + ‘Proc. Acad. Nat. Sci.’ February and May 1869, Notes on “ Inelusions” in Gems, &e. By Isaac Lea. 203 Opal.—This exquisite gem, which displays such brilliant colours, is very highly valued. It is but little harder than glass, and is indeed considered as volcanic glass. Its remarkable flashes of colour are attributed to fissures, in accordance with the theory of Newton’s coloured rings. I have never been able to detect either cavities or minute crystals in this beautiful gem, except in two cases. One of my specimens has a brown, terminated crystal, a six-sided prism of an unknown substance, about one-fifth of an inch long, and terminated by a single oblique plane; the other has several smaller ones. Lapis-lazuwli.—This was used by the ancients as a favourite gem, but it 1s not now valued as such. I have not been able to detect cavities or minute crystals in any specimen in my possession. Corundum.—This very interesting mineral, when in perfect transparent crystals, is highly valued as a gem, under the name of sapphire, ruby, &c., according to colour. When yellow, it is called Oriental topaz; when purple, Oriental amethyst. When purely white it is sometimes sold as a diamond. In this country we have two localities only of corundum where any large quantity has been found, that of Chester County, Pennsylvania, and Frank- lin County, North Carolina. From the mines in Chester County, several hundred tons have been taken, but no transparent crystals. Some opaque ones are bluish and some pinkish. The North Carolina locality has produced some very large crystals, and nu- merous small ones. Of the latter there have been found many quite pure and transparent, and these are sometimes blue and sometimes red. But none of them yet found are of value as gems. The fine sapphires and rubies are chiefly from Ceylon, and they form some of the most beautiful objects in nature. I have many of these in the form of worn pebbles, and some in fine hexagonal form, as well as hundreds of cut specimens. I have examined carefully more than one thousand specimens, with a view to discover whatever “ inclusions” they might possess. In a communication to the Academy* I described and figured some microscopic crystals in these and other gems. Since then I have added a very large number to my collection, and among these several hundred large and small transparent crystals. In a careful microscopic examination of these, I found a large number which contain cavities and minute crystals, the former sometimes scat- tered irregularly through the mass, and sometimes forming a sheet or film. These cavities are of all forms, but usually sub- elliptical ; sometimes tubular, and these tubes frequently anasto- mose in a very beautiful manner. ‘These cavities are so numerous that they frequently give a cloudiness to the specimen, which is less valuable as a gem, but most interesting in a scientific point of * «Proc, Acad. Nat. Sci.’ 1869, VOL. XVII. Q 204 Notes on “ Inclusions” in Gems, &e. By Isaac Lea. view. In some specimens these cavities exist by tens of thousands, and Sir David Brewster stated that in a specimen under his obser- vation there were about 37,000 of these cavities. I am sure that in one of my large cut specimens there must be more than double that number. It is a very common thing to see hundreds at a time of these cavities in the Ceylon specimens, partly filled with the fluids previously alluded to in these notes. But it is quite rare that they are found in the specimens from North Carolina. Still I have seen them in the transparent small fragments of deep blue crystals, and sometimes in the transparent light-coloured ones. In one specimen of the latter I discovered some most in- teresting cavities, which contained, beside the fluid, each a single cubic crystal. I had never observed an included crystal in any eavity in the numerous Ceylon specimens which I have examined. These cubic crystals have the exact form and appearance of those in the emerald described herein. In regard to the microscopic crystals in sapphire, having described and figured them in the papers before alluded to, I have little to add now. Further observation has confirmed what I then stated regarding the radii of Asteria. Very recently I have received a number of these Asteria of various colours, blue, purple, white, red, and dove colour ; several three-quarters of an imch in diameter. ‘The red and purple specimens are of peculiar beauty, and when examined in the sun, or any strong light, they both exhibit the microscopic acicular crystals with peculiar beauty, dis- played as they are in hexagonal form, and reflecting the spectral colours. The ruby Asteria is certainly among the most beautiful objects in nature, and the purple are very little less so. In some crystals of corundum there is a strong bronze reflexion, and this is the case with some of the large hexagonal crystals which were imported by Mr. 8. 8. White from India for commercial pur- poses, and which he distributed with so much liberality to our mineralogists. These bronze crystals have also been found at the Black Horse and Village Green localities in Delaware County, Pennsylvania. When examined with a good power, these bronze reflexions are at once seen to be caused by minute acicular crystals, and these may sometimes be seen in bunches. A pale ruby, “ Rubicelle,” which I lately received from my friend Hugh Nevill, Esq., Ceylon, about three carats, is a most interesting and beautiful gem. It has the depth and brilliancy almost of the diamond. It is nearly of a rose colour, and is per- fectly transparent. It is cut with a top table and not entirely symmetrical. Its refractive power is unusually great. Yet when this brilliant transparent gem is examined with a high power and strong light, the whole mass may be seen to be filled with long acicular crystals in three directions, parallel to the prismatic A Mode of altering the Focus of a Microscope. By M.Govi. 205 planes, and interspersed are numbers of very minute and delicate cuneiform crystals.* It has also a small cloud of exceedingly small cavities. Another remarkable specimen may be mentioned here, which has small cavities and minute microscopic crystals. It is of a pale yellow or straw colour, and of a depth and brilliancy scarcely exceeded by the diamond. During the examination, about two years since, of some hun- dreds of small crystals of sapphire, perfectly transparent to dark blue, I discovered one which had very singular plumose impressions on the planes of the prism. This induced me to examine carefully all those which I subsequently procured, and I have now over a dozen specimens which exhibit this very singular character. I am entirely at a loss to discover the cause of this form of minute impressions on so hard a substance. It evidently has been formed by some collateral mineral substance, against which the molecules in crystallization have been arranged. Diamond.—The hardest of all substances stands first among gems. It has not, however, much interest to the microscopist, as no cavities with fluid have been, so far as known, observed; nor has it included crystals of foreign substances. They are often very imperfect, containing rifts and discolorations. Some of my speci- mens have beautiful triangular impressions on the surface of the planes. My friend Dr. Hamlin, of Bangor, Maine, is engaged on an extended work on the diamond. Such a work is much needed, and I know no one as capable as he to accomplish it. This gem sometimes occurs of various colours. In my cabinet I have six different colours.—Proceedings of the Academy of Natural Sciences, Philadelphia, VI—A Mode of altering the Focus of a Microscope without altering the Position of either the Objective or the Object. By M. Govt. In working with the microscope, above all when we utilize it for comparing measures of length, it often happens that after having focussed it upon the first object, it is necessary to apply it to the observation of a second one, which is not absolutely at the same distance from the objective as the first. Then it becomes necessary to alter the focus of the instrument in order to have a clear image of the object, and this is done either by a movement of the whole microscope (i. e. the tube), or by an alteration of the eye-piece or the objective, or by a movement forwards or backwards of an inter- * Proc. Acad, Nat. Sci” May 11, 1869. Q 2 206 A Mode of altering the Focus of a Microscope. By M. Govi. mediate lens (as in the parfocal meroscope of Porro). In all these cases, no matter how much care may have been taken in the con- struction of the apparatus necessary for these alterations, it is almost impossible to avoid very slight deviations of the optical axis of the microscope, and hence we cannot count on the perfect exacti- tude of comparisons which demand an absolute invariability of the direction of this same axis. If instead of changing the focus by means of altering the optical apparatus we obtain the alteration by elevating or depressing the object itself, it may happen, and it does occur often enough, that the masses to be displaced being con- siderable, the displacements occur irregularly by a series of jerks, with flexion of the object, and hence with an uncertainty or an alteration of the length to be measured. Moreover, one can hardly focus one of the extremities of a scale without at the same time altering the focus of the other end, which causes a loss of time, and prolongs beyond measure operations which ought to be rapidly performed. It was therefore desired to find a means of altermg promptly the vertical focus of the microscope within certain limits, without having to fear either a change of direction of the optical axis of the instrument or any alteration whatever in the length to be measured. It was then necessary to consider how this could be done without interfering either with the optical part of the instrument or with the object. And it seemed almost impossible. But on reflecting, it appeared that the interposition between objective and object of a medium more refractive than air, bounded by plane and parallel faces normal with the axis of the microscope, would affect the object. Thus there is an apparent raising of the object : where d is the amount of elevation produced, e the thickness of the medium introduced, and n its index of refraction compared either with the air or a vacuum. It will suffice in fact to place beneath the objective a plate with plane and parallel surfaces, and of variable thickness, to bring readily into the focal plane of the eye-piece the image of objects situated at different distances in front of the object-glass without altering the position of either the objective or the object. But it was, if not impossible, at least extremely difficult to obtain solid plates with plane and parallel faces and with a thickness which could be altered at will, which withal were perfectly homogeneous throughout, and maintained their perpendicularity in their initial inclination in relation to the optical axis of the microscope. Fortunately a well-known property of liquids—that of leaving their surface during equilibrium perfectly horizontal—permits us A Mode of altering the Focus of a Microscope. By M. Govi. 207 to obtain with them what we could hardly hope to get with solids. Hence it is only necessary to employ a liquid layer placed, in a sort of cup with a transparent bottom, beneath the objective. or here we have a refractive plate whose thickness we can increase or diminish, and whose surfaces keep up constantly the same relation with each other and with the optical axis of the microscope. If then one establishes between the objective and the object a reservoir sufficiently large (in order to avoid capillary attrac- tion), closed below by a plate of glass with horizontal surfaces sufficiently parallel, and if then one introduces a liquid of the index m, which one may vary the level of at will by aid ofa plongewr, or by means of a communicating vessel filled with the same liquid, one may always by variations in the weight of the refractive layer bring to the same vertical distance objects whose real distances differ by quantities more or less considerable. The limit of these accommodations is given by the value of d, calculated from the formula already given. And as one hardly has recourse to liquids whose index of refraction is less than 1+3335 or more than 2°000 this limit would always be comprised between about a quarter and a half of the maaimum thickness of the liquid contained in the cup. It must be understood that it is not requisite to take account, in this valuation of d, of the constant displacement produced by the layer of glass and by a layer of liquid which it is well to have above it in order that the variations of thickness may take place in the same refractive substance. In cases where the objects to be observed are directly plunged in a liquid, this liquid might be made to serve the focalization of their images. The extreme mobility of most liquids demands great steadiness in the “cup” which carries them; without this the agitation of their surfaces would prevent the proper formation of images, just as it not unfrequently happens in the mercury baths that are used for astronomical purposes. If there are no trepidations, the observation of transparent or opaque objects is conducted as easily through the liquid layers as through the air, and the loss of light which results from successive reflexions does not materially affect the clearness of the images. A slight defect of parallelism between the inferior surface of the “cup” and the upper surface of the liquid should not affect the exactitude of the focus, whilst perfect horizontality of this latter gives this slight defect a constant value, whatever be the thickness of the liquid layer interposed. It produces only in this case a slight lateral displacement of the images, which, being the same for all, alters in nothing the value of their relative distances.—A Paper read before the French Academy, February 19, 1877. ( 208 ) PROGRESS OF MICROSCOPICAL SCIENCE. The Structure of the Echinoids,—It seems that M. 8. Lovén has published at Stockholm an essay on the above subject, which is of some importance. It is illustrated by fifty-three plates, and is likely to be of interest not only to the naturalist, but also to the paleon- tologist. The ‘ American Naturalist’ (February) says that it is chiefly zoological in its character, the text and plates are mostly devoted to a discussion of the homologies of the shell of the sea-urchins, parti- cularly those forms related to extinct genera of Echinoids. Com- parisons are also instituted with the classes of Asteroids (star-fish) and Crinoids, which will, if we mistake not, be found of much use to paleontologists. Especial attention is devoted to certain organs called Spherides, grouped around the mouth of sea-urchins, for the discovery of which naturalists are indebted to Professor Lovén. But the most interesting portions of the work are the exquisite drawings illustrating the anatomy and distribution of the nervous system and the water system of vessels. We have here for the first time, clearly shown, the more intimate relations of these organs. The plates are abundant and beautifully executed, the lithographs rivalling in clearness and delicacy the best steel engravings. The Position of Sponges.—Professor A. Hyatt, who lately read a paper on this subject before the Boston Society of Natural History, stated that he considered they formed the type of a new sub-kingdom of animals. He treated at some length on their mode of development. The paper will be published in the Society’s ‘ Transactions.’ The Oscillatoria and Bacteria formed the subject of a recent paper before the Boston Natural History Society, by Professor W. G. Farlow. Development of Scleroderma verrucosum.—In the ‘Annales des Sciences’ (1876, p. 30) an important memoir is published on the above subject by M. N. Sorokine, which is thus well abstracted by the ‘Journal of Botany’ (January). It says that attention is first directed to the two states, thread-like and lash-like, of the mycelium, upon which no organs of fecundation were discovered. In a very early state the mycelium consists of a cushion of short interlaced dichotomous filaments, which afterwards become still more interlaced, so that it has somewhat of a spongy structure consisting of masses of interlacing fibres with frequent cavities. Fine branches are now given off from the filaments which direct themselves into the nearest cavity, and when there bifurcate at their extremity, one of the bifurcations twining round its fellow; this is the commencement of the hymenium, which increases quickly by the formation of other filaments from the original one, and the young plantule now consists of a great number of hymenial masses contained in a darker-coloured common envelope, the intervals between the former being occupied by filaments which give origin to the capillitium. The filaments of the capillitium become transversely partitioned, and some of the segments are thickened, while PROGRESS OF MICROSGOPICAL SCIENCE. 209 others remain thin and transparent, and during the time the spores are ripening the latter are converted into mucilage, the simple or branched thickened segments remaining. The origin of the basidia is as follows: Immediately after the development of the hymenial masses, some of the filaments of which they are composed bear branches which direct themselves towards the centre of the mass; these branches divide transversely, and the terminal cell becomes elongated and is soon seen to carry four round pedicellate spores, the nucleus of the basidium disappearing before the spores make their appearance, as Woronine has already observed in Exobasidium. M. Sorokine cannot share the opinion of Berkeley and Tulasne that the spores do not arrive at their full development while attached to the basidia, but that they fall off and draw elements of nutrition from the nidus in which, when free, they find themselves. On the contrary, he thinks that the spores do not fall until their development is complete. He believes also that, contrary to what has already been held, there is no regularity in the order of local maturation of the hymenial masses. ‘I'he so-called “nucleus” of the spores is shown to be of oleaginous nature, since it dissolves in alcohol. Haperimental Observations on Mosses.—Some experiments of a very interesting nature were conducted lately at Strasburg in regard to the “artificial production of a protonema on the sporogonium of Mosses,” by Professor Dr. Stahl. They are described at some length in the ‘Journal of Botany’ for January, by a writer who signs himself G. R. M. M. He says, among other things, that as Brefeld’s views on the alternation of generations of the Ascomycetes take the relations existing in Vascular Cryptogams as a point of departure, it was first of all the question whether the production of the sexual generation was necessarily bound up with the formation of spores, or whether perhaps, under normal conditions, other parts of the spore-bearing plant were not in a position to produce the sexual plant. To settle this question by experiment no better object could be found than the sporogonium of Mosses, and after much searching Dr. Stahl found — that of Ceratodon purpureus to be the most suitable for conducting the necessary investigations. The experiments were instituted thus. The sporogonia were partly extracted from their mother-plants—a process which can usually be effected without injury—and partly cut off directly above the point of their connection; all were placed on damp earth under a bell-jar, and exposed to diffused daylight. Nota few soon showed clear signs of decay; others again remained green and unaltered in shape, with the exception of some deformations of the capsule. After two or three months, however, dense protonema- formations, on which leaf-bearing Moss-plants were already formed, proceeding from the cut surface of the seta, extended over the earthy substratum. From microscopic examination it appeared that the protonema-threads owed their origin to the chlorophyll-containing cells within the seta, longitudinal sections of which showed the way they arise. After a lapse of three months the contents of most of the seta-cells had died in both the forms of cultivation, but here and there were found, extending along the whole length of the seta, 210 PROGRESS OF MICROSCOPICAL SCIENCE. between the dead thin-walled cells of the fundamental tissue, cells which not only retained their protoplasm and chlorophyll, but had increased the volume of the latter in particular in a striking degree. These occurred in the decayed tissue, sometimes isolated and some- times in groups, the individual cells arranged beside or above each other. Even from cells in the wall of the capsule Dr. Stahl found protonema filaments to proceed. From Pringsheim’s observations, as well as from those here communicated, the conclusion is clearly arrived at that the transition from the spore-bearing generation to the sexual generation is not necessarily bound up with the formation of spores, but that, under conditions injurious to the formation of spores, different cells, both of the seta and the capsule, are capable of producing a protonema. The Origin of Pycnidia.—A difficult research is that which has been made by Dr. H. Bauke, and which is recorded in the ‘ Nova Acta’ (Band 36), Dresden, 1876. The original paper is abstracted at considerable length in the ‘ Journal of Botany’ (January), from which the following conclusions may be taken as stated by the author :—“ As to the question whether the Pycnidia are independent organisms, or whether they belong to the Ascomycetes, these researches prove the second of these alternatives to be correct. The cultivation of the Ascospores of Pleospora polytricha, Cucurbitaria elongata, and Lepto- spheeria (Pleospora) Doliolum regularly yielded Pycnidia—in the first of the three species named such bodies were up till now unknown; in this case the direct connection between the sown Ascospores and the Pycnidia was each time established. From Pleospora herbarwm, in spite of numerous cultivations instituted for the purpose of studying specially the development of the Perithecia and the Pleomorphism of this fungus, I obtained only twice Pyenidia. . . . In the cultivation of Melanomma (Spheria) Pulvis-Pyrius and of Pleospora pellita a dense mycelium was regularly produced, on which in the latter species the Conidia drawn by Tulasne appeared in masses, but no Pyenidia, which were indeed never found on either, &c. From Cucurbitaria Laburni and Pleospora Clematidis the same results were obtained, namely, no Pyenidia. Pycnidia appear as parasites on other Ascomycetes (as in the case of Cincinnobolus and Erysiphe) only as distinct exceptions.” Tubular Degeneration of the Medullary Nerve Sheath. — The ‘American Journal of Insanity’ (January 1877) says that in partial softening of the spinal cord, and in grey degeneration, Professor Arndt observed—by examining transverse sections, coloured with car- mine—the medullary sheath to consist of concentric layers. As the medullary substance showed an inflated condition, there was no doubt of a pathological alteration; but still, Arndt believes that it also establishes the true structure of the sheath, which normally, very probably, grows by forming concentric layers. Are Volvox globator and Sphcerosira volvox distinct Species ?—This question has at length been answered in the negative by Mr. W. H. Gilburt, who has a short but important paper on this question in the ‘Journal of the Quekett Club’ (February 1877). The relationship PROGRESS OF MICROSCOPICAL SCIENCE. 211 was suspected years ago by Mr. Busk, but it is now clearly defined. Mr. Gilburt says that he lately obtained some water from a pond in Epping Forest, near Walthamstow, containing Volvox globator in great numbers. On first looking at them, nothing particular was observed, save that many were decaying, and were occupied by one or more rotifers and their eggs. Making a more careful examination, he found that in some of the vigorous and more active ones, a difference between the macro-gonidia existed—some of them being smaller in size, lighter in colour, and the disposition of their gonidia less regular. Using a higher power, the difference became more marked, and under a power of 350 diameters those which departed from the supposed normal character appeared as the author has represented them in the drawing which accompanies the paper, a sphere as an ordinary Volvowx, but that some of the gonidia were missing, and their places occupied by compound bodies, in this and every other respect agreeing with the figures of Spherosira as given both by Ehrenberg and Busk. Submitting them to pressure so as to rnpture the cell-wall, he found that the compound bodies referred to escaped; and then appeared discoid in form, and composed of about thirty cells, flask-shaped, having a nucleus, being attached to each other by the smaller end, and furnished with abundant vibratile cilia, which can be seen in both aspects as figured. The action of the cilia imparts a slow, revolving, wheel-like motion to the group, but with very little progression. This motion can sometimes be seen while they are still within the containing sphere. In a single Spherosira as many as fifty-five of these compound bodies have been found. One most remarkable feature is, that while the Volvow globator may contain from two to seven macro-gonidia, yet in only two instances has he found more than one Spherosiva among them; though a very large number have been examined for this special purpose. The Formation of Spores in Lichens and Fungi.—A valuable essay on this subject has been translated from the French of M. Strasburger into ‘Grevillea’ for March. We can only abstract a few of the observations, more especially with reference to Physica ciliaris. The author says with regard to this species his own special researches show that the primitive nucleus really exists, and is found in the upper portion of the claviform ascus before the production of the spores. The ascus is filled with a protoplasm nearly uniform in density, and possesses a thick and very turgescent wall. The nucleus is spherical, especially dense and refractive in its upper part, as the examination of preparations preserved in alcohol demonstrates. The ascus augments in volume, the primitive nucleus disappears, and eight spores simultaneously arise in the superior part of the ascus. These spores approach each other closely, and absorb for their formation nearly all the superior protoplasm of the ascus. The spores appear complete. In the centre of each of them we observe a denser, although badly circumscribed spot. The young spores are at first solid, and surround themselves very rapidly with a colourless membrane of cellulose, which quickly increases in thickness. At the same time they increase in size, and their protoplasmic contents retire towards their walls. The denser, and at first central portion, which is an 212 PROGRESS OF MICROSCOPICAL SCIENCE. irregular or stellate granule, becomes equally parietal, and appears to be equivalent to a nucleus, for it immediately doubles itself, and displays between its two moieties a partition of protoplasm, by means of which the spore, which has become ellipsoid, is divided along its smaller axis, into two equal parts. But this nucleus is so small that we are unable to observe the details of its division. In the partition of protoplasm, there is formed at the same time a new wall of cellu- lose, which speedily acquires a great thickness. The two small nuclei which generally are at first fixed near the new wall, cannot be dis- tinguished from the other granular contents of the spores, until these acquire a greater age. Finally, the membranes of the spores which have become bicellular, rapidly acquire a colour, which becomes deeper and deeper, from grey to brown. The small quantity of pro- toplasm which surrounds the spores becomes tinted always, by iodine, of a yellow-brown. The Blood-globules of different Races of Man.—Dr. J. G. Richardson, of Philadelphia, has sent us an important paper which he has published on this subject in the ‘American Journal of Medical Sciences.’ He determined to obtain from the several individuals of different parts of the world who went to the American Exhibition last autumn, specimens of their blood. And he thus describes the results :—“ The samples were each procured by myself from the individuals mentioned (sometimes only through much persuasion), by puncturing a finger with the quick stab of a cataract needle, pressing out a small amount of blood, applying a clean slide to the apex of the drop, and then spreading out the portion of fluid which adhered to the glass, with the end of another slide, according to Professor Christopher Johnson’s ex- cellent method. The measurements were all made with a ,';th immer- sion objective and by the aid of a cobweb micrometer eye-piece, giving when thus combined a power of 1800 diameters. The value of the degrees of the eye-piece micrometer with this objective, at the cover correction employed, was determined by a stage micrometer kindly com- pared for me by my friend Col. J. J. Woodward, of Washington, D.C., with one carefully tested by the standard in the U.S. Coast Survey Office, and which he has pronounced practically correct. Instead of measuring all corpuscles, deformed or otherwise, in two directions, as proposed by Dr. Woodward,* I prefer to determine the size of un- altered, i.e. circular corpuscles only. By this plan, which I believe is that of our highest authority upon the subject, Professor Gulliver, we obtain the dimensions of nearly normal cell elements, such as are exhibited in Dr. Woodward’s beautiful photograph of fresh blood,} where, as in fluid preparations, but little variation in size exists among the corpuscles; and escape being misled by pathological specimens similar to those displayed in photograph No. 836, of the same in- valuable series. Since the chief cause of marked variation in magni- tude as well as of distortion in shape among blood-disks spread out upon glass is, I think, their mutual attraction and repulsion during * ¢ Phila. Med. Times,’ vol. vi. p. 457. + ‘Army Med. Museum,’ No. 861, New Series. PROGRESS OF MICROSCOPICAL SCIENCE. 213 the process of drying, my investigations were made upon portions of . slides where the corpuscles were very sparsely disseminated, and then, to secure the most infallible accuracy for my deductions, as the pre- paration was moved along, I measured every isolated circular red disk which came into the field of the microscope. In doing this I cautiously avoided recording those which manifested even slight departures toward an oval form, and by several experiments learned that the deviation corresponding to a transverse diameter of 5,),, and a conjugate of 5,!;, of an inch was recognizable by a single glance. One hundred corpuscles in each specimen were measured and the dimensions as I read them off in millionths of an inch noted down generally by an assistant. These memoranda, with the preparations to which they refer, are carefully preserved for examination by any experts who may desire to convince themselves respecting the sub- stantial foundation of fact whereon I base my conclusions.” Here follow the several results, which have been put in a more convenient form by the editor of the ‘American Naturalist’ (March 1877) than they have in the original paper : ~ if re aga 2 3/8 & tS) = ra og SEs od NATIONALITY OF & | Le SE | Ag Az leu8| sto lecs SUBJECT. oa og oe g B g& | e888] on8| 088 S | tel i irshies a5 = | wo | wa Gilat, (ee: tars lalieo. ue suns S eae el sare F sinlgtl oe 4 vines | g57| 33 e GeaPnes cpaer stank Japanese Sel LOO Esa eon e 23787) eS ele so ag Spanish .. .. | 30| 100 |1-3296/1-2777|1-3571/ 6 | 89 5 Belgian .. .. | 88] 100 | 1-8203/1-2777|1-3846| 7 | 88 5 Swiss .. .. .. | 40 | 100 | 1-3203/1-2857|1-4000| 7 | 82 | 11 Turkish .. .. | 29 | 100 |1-8197|1-2777|1-3846| 4 | 80 | 16 Danish .. .. | 25| 100 | 1-3257|1-2857|1-4000; 12 | 82 6 RUSstane ee altel On I—St9Oy 1 ~2857 | 1-3971 Ae oy 7 Norwegian .. .. | 35 | 100 | 1-8252 | 1-2857| 1-4000; 10 | 86 4 Swedish .. .. | 33| 100 | 1-8254/1-2777/1-8737/ 13 | 82 5 Italian .. .. | 35 100 |1-3272|1-2777|1-4000| 10 | 83 7 French .. 67 | 100 | 1-3239 | 1-2777| 1-8737| 12 | 80 8 al 52 | 100 |1-3229|1-2857|1-3856| 11 | 83 | 6 Cherokee Indian;\) 4g | 400 | 1-3215|1-2857/1-4000/ 10 | 83 | 7 born in U.S. .. f| | English parent- 9791 | 1.9777 | 1_294@ | Le ere | 40 | 100 |1-8191|1-2777|1-3846| 6 | 85 9 Total .. | .. | 1400 | 1-3224 | 1-2777|1-4000} 8 83 9 “ Combining these deductions, we find that of the wae 1400 cor- puscles each separately measured, the SEE Was s5'sy (°007878 mm.), the maximum ;,/,,, and the Sen FO00, of an inch; 1158 or 83 per cent. measured between 7,5 and x9 of an inch in diameter, and consequently under a power of 200 would appear about 214 PROGRESS OF MICROSCOPICAL SCIENCE. the same magnitude; 118 or about 8 per cent. were less than 34x, and 124 or nearly 9 per cent. were more than .,),, of an inch in diameter. The total number of corpuscles ;,5 of an inch across was 6, or less than one-half of 1 per cent. The total number 57,7 of an inch in diameter was 10, or less than 1 per cent. 'The somewhat smaller averages of the Italian, Swedish, and Norwegian specimens are perhaps due to slight accidental variations in spreading out the layers of blood for examination, and cannot be accepted, at least without further research, as indicative of either personal or national peculiarities.” MicroscoricAL Contents oF ForEIGN JOURNALS. The following brief notices of foreign journals of interest to the microscopist are taken partly from ‘Nature’ and the ‘Journal of Botany’ (for March) : Morphologisches Jahrbuch, vol. ii. part 4.—On the Development of the Auriculo-ventricular Valves of the Heart, by A. C. Bernays.—On the Segmentation of the Ovum and Formation of the Blastoderm in Calyptrea, by A. Stecker.—On the Primitive Groove in the Chick, by A. Rauber. Revue des Sciences Naturelles, vol. v.. No. 8, December 1876.— Contributions to the Natural History and Anatomy of the Ephemeride, by N. and E. Joly; an important paper.—On Parthenogenesis in Bombyx mori, by Carl von Siebold.—On the Histology of the Egg, by A. Villot, dealing with theoretical views on the germinal vesicle and its history. Bot. Zeitung, January 1877.—H. de Vries, “On the Expansion of Growing Cells from Turgescence.”—M. W. Beyernick, “On Plant- galls.” Flora, January.—L. Celakovsky, “On the Morphological Struc- ture of Vincetoxicum and Asclepias” (tab. 1).— C. Kraus, “ On Relations of Turgescence to Growth-phenomena.’—A. Batalin, “ Me- chanism of Movements of Insect-eating Plants.’—V. A. Poulsen, “A New Locality for Rosanoff’s Crystals.” (Esterr. Bot. Zeitschr.—* On the Occurrence and Origin of Etiolin and Chlorophyll in the Potato.” Bull. Bot. Soc. France, 1873, pt. 8.—E. Mer, “ Vegetative Pheno- mena preceding and accompanying the fall of Leaves.’— Ripart, “On New or Rare Cryptogams for Centre of France.’—E. Prillieux, * Formation and Development of some Galls.”—E. Mer, “ Nature and Functions of Evergreen Leaves.”—Id., “ Effect of Immersion on Aérial Leaves.” . Nuovo Giorn. Bot. Ital.—G. Briosi, “ On the Phytoptus Disease of the Vine” (tab. 1). [This article we have had translated, and repro- duced in the present number of the ‘ M. M, J.’ |—Id., ‘‘ On the Function = NOTES AND MEMORANDA. 205 of Chlorophyll in the Vine.’—G. Archangeli, “Ona Disease of the Vine ” (tab. 3).—G. Cugini, “ On the Hairs of Species of Plantago” (tab. 4—6). Zeitschrift fiir Wissenschaftliche Zoologie, vol. xxvii. part 4, 1876.— On the Anatomy of the Ophiuroid, Ophiactis virens, by H. Simroth, seventy pages, five plates.—On the Structure of the Brain in Arthro- pods, a Memoir describing the brains of Apis mellifica, Gryllus cam- pestris, Gryllotalpa vulgaris, Carabus viol., and Astacus fluviatilis, by M. J. Dietl, of Innsbruck, thirty pages, three plates. Reale Istituto Lombardo di Scienze e Lettere, Rendiconti, vol. x. fasc. 1—On Helminthosporium vitis (Lev.), a Parasite of the Leaves of the Vine, by M. Pirotta.—On the Phenomena which accompany the Expansion of Liquid Drops, by M. Cintolesi. Ofversigt of the Stockholm Acad. of Sciences, 1876, No. 6.— Dr. Nordstedt and Dr. Wittrock have published a paper in this on the Desmidice and Afdogonia of the Tyrol and Italy. Two excellent plates display the several novelties. In Naturforscher (January 1877) we note the following papers :— On the Germination of the Fruits of Mosses, by P. Magnus.—On the Preparation of Pure Alcohol Yeast, by Moritz Traube.—New Re- searches on Bacteria, by E. v. M.—On the Exhalation of Carbonic Acid and the Growth of Plants, by L. Rischawi.i—Researches on Assimila- tion in Plants, by A. Stutzer. The Memoirs of the St. Petersburg Society of Naturalists, vol. vii., contains a series of valuable physiological contributions, the most im- portant of which are :—On the Comparative Anatomy and Metamor- phology of the Nervous System of the Hymenoptera, by E. K. Brandt. —QOn Changes in the Hye produced by the Section of the nervus trigeminus, by M. Chistoserdotf.—On the Nucleus of the Red Globules of the Blood, by A. F. Brandt. NOTES AND MEMORANDA. Death of Dr. Bowerbank.—It is with great regret that we have to announce the death of one of our most distinguished Fellows, J. S. Bowerbank, LL.D., F.R.S., which occurred at his residence at St. Leonards-on-Sea, on March 8, and which we believe was caused by an attack of bronchitis. He had lived beyond the time that is generally allotted to us; that is to say, he had more than completed his threescore and ten years, being in fact eighty at the period of his death. He has not of late communicated anything to the Society, but he was not on that account idle. On the contrary, he was at work almost till his decease. Indeed, it is but a few months since a paper of his on the Spongiade was read before the Zoological Society. Besides his 216 NOTES AND MEMORANDA. various papers on zoology, communicated from time to time to the different associations, the great work by which his name will be remembered is the ‘ Monograph of the British Spongiadex, a book published in 1864 by the Ray Society, and which has been admirably illustrated by Mr. Lens Aldous. Mr. Bridgman’s Mode of Polishing a Speculum. — In a paper published in the February number of the ‘Quekett Club, Mr. Bridg- man gave an interesting account of a new universal reflecting illu- minator, which we regret that we cannot condense, as without the illustrations our remarks would be unintelligible. However, he also appended some observations on the above subject which are worthy of being recorded here. He says :—Having obtained the silver plate, and had it soft-soldered to a brass back and cut to the size, let a piece of sealing-wax or a small block of thick plate glass be attached to its back as a handle and to prevent flexure. Now procure a common writing-slate with a flat and smooth surface, and grind the silver with water until all scratches have disappeared, and a level face has been produced. If the surface be now well burnished with a straight burnisher it will add greatly to the brilliancy and durability of the polish. Next, take two pieces of thick plate glass, not less than three or four inches square, and upon the surface of one melt some pieces of clean pitch until soft enough to be spread evenly with a hot knife to about the thickness of a sixpence. Let the surface of the other glass be smeared with soap and water, and then pressed upon the soft pitch until the latter shall have acquired a flat and highly polished surface, when it may be slid off, and the pitch left to harden. Obtain at the chemist’s a pennyworth of “ precipitated carbonate of iron” (the softest and finest “rouge” possible), and mix with a few drops of water to the consistence of cream, and let the metal be lightly worked with this over all parts of the pitch in small circles, carefully avoiding all dirt or grit until the polish, commencing in the centre, shall have spread to the edges, and have a deep and brilliant lustre that will reflect objects with the utmost sharpness of definition. A New Microtome for cutting a series of sections was recently described to the Boston Society of Natural History, by Mr. C. 8. Minot. We have not yet seen any description of the instrument. Mr. Spencer’s Objective.—In our last number we described an objective of Mr. Charles A. Spencer, on the authority of the ‘Cin- cinnati Medical Journal.’ We now learn from that Journal that the object-glass referred to was not made by the veteran Spencer, but by his son, who, it states, with his father, and brother-in-law, O. T. May, is engaged in the manufacture of microscopes, under the “firm name” of Charles A. Spencer and Sons, in connection with the Geneva Optical Company. The immediate work of making these fine lenses is done by Mr. Herbert R. Spencer. The glass alluded to is a three-system lens, and is of 170° angle of aperture, instead of 160° as stated. CORRESPONDENCE. MicroscoprcaAL CENTENNIAL HixHIBITIon. To the Editor of the ‘ Monthly Microscopical Journal. 7, WiemMorr STREET, CAVENDISH SQUARE, February 20, 1877. Sirn,—The January number of the ‘ Monthly Microscopical Journal’ contains a review of the microscopes in the Centennial Exhibition at Philadelphia, in which the writer, Dr. Ward, while giving a most favourable notice of our exhibit, and expressing himself in a handsome manner as to the style and finish of our instruments, makes a remark which we fear may possibly bear a wrong inter- pretation. Referring to our objectives on Wenham’s new formula, Dr. Ward states that they were “ understood to have been entered for competition and then permanently removed from the Exhibition and the country.” This would imply that they were taken away before being examined, but this was not the case, as the judges tested the whole series critically on several occasions, and it was not until they informed our representative that their examinations were com- pleted that the glasses were removed from the building. We may add, that the judge’s Report is now in our possession, and that it is highly commendatory to both our microscopes and new objectives. We are, Sir, yours obediently, Ross anp Oo. ON THE MEANS OF CENTRING OBJECTIVES AND Roratina STAGES. To the Editor of the * Monthly Microscopical Journal.’ February 28, 1877. Si1r,— All who work with high powers, and use high-angled achro- matic condensers, have, no doubt, felt the inconvenience of the con- centric rotating stage being eccentric, not only with different objectives, but even, very often, with the one to which it may have been adjusted; and they may also have observed that the achromatic condenser, not- withstanding that it may have been carefully centred, will sometimes become eccentric. These defects are, of course, much less apparent in the very best workmanship. The means of “accurately centring the stage to the highest power objective” was introduced in 1875,* and later in the same year {+ the “concentric rotating stage having rectangular mechanical adjust- ments” was brought before the Royal Microscopical Society. Both these plans are based on nearly the same principle, and the result aimed at is to render the rotation of the stage concentric with any * «Science-Gossip, September 1875, p. lxvii.; and ‘M. M. J.’ No, Ixxxi. September 1875 (cover). + ‘M.M. J.’ No, Ixxxv. p. 54, January 1876. 218 CORRESPONDENCE. objective that the observer may wish to employ. But neither plan is of any use for centring objectives to the achromatic condenser when it is eccentric; moreover, the above-adjustments are cumbersome, because they must be fixtures, and their use is limited. The “new centring nose-piece” is, in my opinion, a great boon to observers who work with high powers on ¢est objects. Test work may not be very instructive, but it is undoubtedly the cause of the great improvements made on some of the modern objectives; it is also fashionable, not only among amateurs, but even among savants; and therefore any new apparatus that facilitates the attainment of accuracy should be welcomed. The centring nose-piece is made by Mr. Swift, and it figures in ‘Science-Gossip’ for February, page xv. The rectangular adjust- ments act in the same manner as those of the sub-stage, and the objective is thereby adjusted to the optical axis of the instrument. This nose-piece has the following advantages, namely: Ist, it is not a fixture, and it works with any microscope fitted with the “ universal screw”: 2nd, it may be used to rectify the eccentricity of the achro- matic condenser caused either by the “spring” of the fine adjustment when moving the screw-collar of the objective, or by the unsteadiness of the sub-stage; and also to centre any objective to the achromatic condenser fitted to a microscope without any under-stage adjustments: 8rd, it may also be used to render the rotating stage concentric with any objective. The only drawback is that this nose-piece may slightly strain the fine adjustment. It must be taken into consideration that neither the centring of the stage, nor that of the objective, is obtained “instantaneously ” nor “with the greatest facility ”: in either case the adjustments must be made very carefully. I am, Sir, yours obediently, A. DE SouzA GUIMARAENS. Nore ON THE STRUCTURE oF THE TEest IN ARCELLA. To the Editor of the ‘ Monthly Microscopical Journal. Sir,—In the ‘ Quarterly Journal of Microscopical Science’ for January last, p. 79, the following statement appeared : “For the first time seemingly a correct description of the structure of the peculiar test of the somewhat variously and otherwise pretty well known and at least common species Arcella vulgaris (Ehr.), is given by Hertwig and Lesser. Two plates, an outer forming the superficies of the test, an inner applied to the body of Arcella, are united in a honeycomb-like structure, whose hexagonal cavities form prismatic spaces standing vertically on the surface. Hertwig and Lesser conclude that the appearance of the markings on the Arcella test is not due to granulation as Dujardin supposed, or Claparéde and Lackmann as well as Carter assumed. Wallich indeed spoke of symmetrical reticulation and of hexagonal interspaces ; still Hertwig and Lesser doubt if he altogether correctly appreciated the structure, PROCEEDINGS OF SOCIETIES. 219 as how otherwise could he come to the conclusion that Arcella vulgaris could be but a sub species or even a species of Difflugia ?” What on earth my conclusions regarding the limitation of species in these lower forms of animal life have to do with the correctness or incorrectness of my published description and figures of the structure of the Arcelline test I am at a loss to conceive. The one is a matter of opinion ; the other a matter of fact. I am quite ready, however, to allow that in my humble opinion our knowledge of the biological re- lations of the Protozoa and Protophyta is much more likely to be increased by taking into due consideration the causes on which divergence is mainly dependent, than by seizing upon every trivial variation from an assumed type as evidence of specific distinctness. How far it is admissible to say that “a correct description ” of the structure of the test of Arcella was given “for the first time) by Messrs. Hertwig and Lesser,” and that I merely “spoke of sym- metrical reticulation and hexagonal interspaces,” the subjoined extract will at once show. I may mention that it is taken from the explana- tory references which accompany the plates illustrating my memoir ‘On the Extent and Causes of Structural Variation among the Dif- flugian Rhizopods;’ and that a detailed figure is there furnished of the structure as it exists in Arcella. “Fig, 87. Front view of D. arcella. Fig. a shows the invariably hexagonal pitting or reticulation of D. arcella (Arcella vulgaris). This can only be made out, however, in a mounted and crushed test, under a high power.” * I remain, Sir, your obedient servant, G. C. Watuico, M.D., &c. PROCEEDINGS OF SOCIETIES. Royat Microscorican Society. Kine’s Coutuece, March 7, 1877. H. C. Sorby, Esq., F.R.S., President, in the chair. The minutes of the preceding meeting were read and confirmed. A list of donations to the Society since the previous meeting was ie by the Secretary, and the thanks of the Society were voted to the onors. The President had great pleasure in announcing that there was every reason to believe that arrangements would be made with Sir John Lubbock to deliver the first Quekett lecture to the Society on May 2. The subject would in all probability be “The Microscopie Characters of Ants in connection with their Habits and Instincts.” The Quekett medal, which had recently been struck for the purpose, would be presented to Sir John Lubbock at the close of the lecture. F eee and Mag. Nat. Hist.’ March 1864. Explanation to plate xvi- g- . VOL. XVII. R 220 PROCEEDINGS OF SOCIETIES. Tickets would be issued to the Fellows for the admission of them- selves and one friend, and the use of the large theatre of the College had been obtained for the purpose. He added, the Council had arranged to have another scientific evening meeting on Wednesday, April 18, of which due notice would be given. The Secretary read a letter which had been received from Mr. Frederick Ebsworth, of Australia, describing a method of estimating and recording the dimensions of small objects, or the fineness of wool. An explanatory diagram accompanied the letter. The thanks of the meeting were voted to the writer for his com- munication. A paper by the Rev. W. H. Dallinger was read by the Secretary, entitled “ Additional Note on the Identity of Navicula crassinervis, Navicula rhomboides, and Frustulia Saxonica.” (The paper will be found at p. 173.) The President, in proposing a vote of thanks to Mr. Dallinger, said that the subject was one to which he had himself paid little or no attention, and therefore it would be out of place for him to say any- thing about it; but he thought it must be plain to everybody present that the method adopted by Mr. Dallinger could not fail to be the right one. He was sure that they would all be very glad to hear that Mr. Dallinger was about to receive considerable help in making his very interesting and important investigations—the sum of 100/. having been voted to him by the Royal Society from the Government Grant Fund of 40002. in order to further the progress of the observations upon which he was engaged. A vote of thanks to the Rev. W. H. Dallinger for his paper was unanimously carried. Mr. Ingpen said he was hardly in a position at a moment’s notice to make remarks upon the subject of the paper which were of sufficient value to be worth their attention. The points of his former observa- tions were directed to the use that should be made of generic names rather than to the identity or otherwise of the forms themselves, and the question of making use of one name for a large number of apparently different forms. He could not help fancying, however, that in a certain group there were collected together a number of diatoms in which, although there was the same arrangement of mark- ings, and therefore a good generic character, there were differences in other respects, and that these differences had been made use of for purposes which were not legitimate. For instance, the Rhomboides was put forward by one maker as a test for a particular objective, and another maker would produce a glass which would resolve a coarser form, also called Rhomboides. This would not be a fair test. He quite agreed with Mr. Dallinger that out of a great number of slides it was possible to find every intermediate variety between two forms, but what they really wanted was the establishment of something like type species. In the case before them they had three distinct forms and many varieties between them, and he quite agreed that the generic term of Frustulia was totally unnecessary. Yet which were they to take as their type form—as a test? He thought they had PROCEEDINGS OF SOCIETIES. 221 something like a starting point in the original Navicula rhomboides —they had its shape, its markings, and its median line, it was figured in “Smith,” and would be a very good one to start from. Then in the same book they had also N. crassinervis, or crassinervia, which had distinctly different ends, was round at the sides, and had the ends of the median line terminating in distinct nodules, compared with which N. rhomboides had its sides straighter, was more generally rhomboidal, and its median line terminated in blunted lancet-shaped points. Between these two they could easily get every variation leading from one to the other, and he thought it was most important from amongst these varieties to get a well-established typical Rhomboides and a typical Crassinervis. What had happened was that for some time they had one form only, after that a coarser form was brought forward as a test for a+ inch; it was much rounder at the sides, and there was a difference in the centre and ends of its median line, which were flattened and battledore-shaped; and then after this they got another form from the Cherryfield diatoms. On the same slide they might see the original Rhomboides and the new specimen. He thought that in this respect Moller had done a great deal towards creating this confusion, for on his type slide they found Rhomboides; but it was the big form, and nothing at all like the Rhomboides of Smith, whilst next to it was what he called Crassinervis—exactly the same as the original Rhomboides, but nothing at all like the Crassinervia of Smith. He should be one of the last to increase the number of genera and species upon insufficient data, but thought they ought not to group together forms which differed so greatly from the type given as that of the species. They wanted at least to know what they were talking about, instead of getting one so mixed up with another that as test-objects they might be used for what might be called illegitimate purposes and so became of little value. Mr. Slack said the paper raised a very wide practical question, and one which was not confined to diatoms. When a botanist was able to show that certain extreme forms were connected by a series of intermediate gradations, he was justified in placing them together in the same group notwithstanding their differences, just as a greyhound and a bulldog were both classed as dogs. In order to know what they were talking about, where there were a great number of so-called species in the question, it was well to retain distinctive names for them for purposes of identity even long after it had been shown that they had no claim to be spoken of as belonging to different genera or species. Mr. Charles Brooke said it appeared to him as a general question that it was quite impossible to assign two individuals to different genera when there was a series of intermediate forms which might be found passing from one to the other. It might be desirable to know the various forms by different names—as in the case of dogs already mentioned—but they should not be known as distinct species, and this should never be done where such gradations existed. This gradation of form had been traced throughout the whole class of the Foramini- fera to a far greater extent than amongst the diatoms, and amongst R 2 222, PROCEEDINGS OF SOCIETIES. them they found immense differences out of all proportion to those of the diatoms, but all unquestionably belonging to the same species, and amongst which it would be impossible to draw any lines if they tried to make them into distinct species. The President said the subject was one which certainly was not confined merely to diatoms, but which equally belonged to every department of science, only that it happened in the case of diatoms that they had the opportunity of examining so great a number of individuals that the variety would be in a measure proportionately great. Donations to the Library and Cabinet since February 7, 1877: From Nature. “Weekly 2.) 5 se Gee ee sib ny ae oie ret Atheneum. Weekly .. SE tale he Voom oc Ditto, Society of Arts Journal. Weekly POI osc) pp) SECU Quarterly Journal of the Gealbaical Society val | (lea a emperor nO Bulletin de la Société Botanique de France... Teloysh hou MRED CRE Enumeracion de los Vertebra dos Fosiles de Espatia. “Par Don C. Calderon, 1877 .. toe ane Cnn .. Author, Journal of the Quekett Club. No. 33 : .. «= Chub. Micro-photographs from the Diatomaceze. ‘By x Redmayne .. Author. Some Remarkable Forms of Animal Life from the Great Deeps off the Norwegian Coast. Part 2. By George O.Sars .. .. Ditto. On the Practical Application of Autography in Zoology, and ona New Autographic Method. By G.O.Sars_.. Ditto. Eleven Stained Preparations, &c., peer abe: Dr. Christopher Johnstone, of Baltimore ae we — Ditto, Twelve Slides ‘of whole Insects .... va aes cele) ER EEEDC ee REESC « G. H. Jones, Esq., was elected a ‘Fellows of the Society. Watrer W. ReEevss, Assist.-Secretary. Meprioat Mioroscorioan Soolety. February 16, 1877.—Henry Power, Esq., President, in the chair. Hyperemia of the Brain from Hanging.—Dr. Browning exhibited some interesting specimens illustrative of this subject. Two were taken from executed criminals, and were prepared by Surgeon-Major Roth, of Berlin, and one was from one of the lower animals that had been hanged for experiment. The brains were, in all cases, injected with carmine. In his remarks upon these specimens Dr. Browning stated that whereas most medico-legal writers describe only a medium amount of vascularity in the brain and that of venous character, and extravasations as very rare, he had found the congestion most intense : the capillaries being so distended in some parts that scarcely any nerve substance was to be seen: however, he had not found any extra- vasations of blood. As cause for the vascularity, the speaker suggested that the knowledge of his fate might, in the case of the criminal, cause some hypercemia at last, though this could not hold with the lower animals. The cerebellum he had found more vascular than the cerebrum. The President suggested that the vascularity was owing to pressure PROCEEDINGS OF SOCIETIES. 723 on the veins, while the arteries could, from not being so compressed, still force up more blood, He thought that the knowledge of his fate would rather make the criminal’s brain ancemic than hypercemic. The lower part of the spinal cord was undoubtedly congested, as shown by the frequency of priapism in these cases. After some further remarks from various members, the meeting resolved itself into a conversazione to exemine the specimens. Liverroot MicroscoricaL Society. The annual meeting of this Society was held on Friday, January 19, at the Royal Institution, the Rev. H. H. Higgins, M.A., in the chair. The annual report of the Committee stated that the number of members on the books of the Society was much the same as last year, and that the financial position of the Society was satisfactory. Important donations have been made of valuable slides to the So- ciety’s cabinet during the session; and also a further number of books have been added by donations and purchase to the library. The Committee congratulated the Society on the fact of the Presi- dent, the Rev. H. H. Higgins, having consented to retain the office of president for another year, in consequence of his prolonged absence, occasioned by his having, on the nomination of the Library, Museum, and Arts Committee of the Town Council, joined the ‘Argo’ scien- tific expedition to the West Indies, which has resulted in some very valuable additions to our local collections. The President delivered his inaugural address. In the course of it he said: Your kind reception of my paper on “Lines of Animal Life,’ consisting chiefly of remarks on the Stammbaum des Thier- reichs of Professor Koch, induces me to hope that a similar attempt to illustrate the vegetable kingdom may be acceptable, and the sub- ject of my address this evening is “Lines of Vegetable Life.” Thanking you for the favour of occupying during the second year the honourable position which I hold as your President, my best apology for so very brief a preface may be the interest and magnitude of my subject.” In concluding the address, the President said: “To appreciate these facts in nature it is not necessary to regard the theory of evolution as if evolution were unconditioned or of universal application ; at the same time it must, I think, be admitted that in the absence of that theory the facts themselves would be in- comprehensible, or would possess comparatively little interest.” The second ordinary meeting of the ninth session was held on Friday, February 2, at the Royal Institution, Colquett Street; the Rev. H. H. Higgins, M.A., President, in the chair. The Hon. See. (Mr. Chantrell), in announcing the donations, read a letter he had received from Mr. G. B. Rothera, of Nottingham, who was present as a visitor at the annual meeting, and heard the President’s inaugural address, the subject of which was “Lines of Vegetable Life.” To show his appreciation of the address, and his desire to see it pub- lished, he enclosed 5/. as a donation to the Society’s funds. Mr, 224 PROCEEDINGS OF SOCIETIES. Joseph Birdsale Jones and Dr. J. Birkbeck Nevins were elected ordinary members. The Rev. W. H. Dallinger, F.R.MLS., gave a practical “ Note on the Ultimate Limit of Vision,” as applied to our modern micro- scopical lenses. Reasoning on certain data more or less theoretical, mathematicians of the first order, notably Helmholtz, had concluded that the limit of vision had been reached; that the optician could practically aid us no further; that, in short, the limits of possibility had been arrived at, since light itself is too coarse to reveal objects smaller than those visible to our finest and most powerful lenses. The limit marked out was about the one hundred and eighty thousandth of an inch. But Mr. Dallinger gave instances of a re- markable kind—the result of his personal investigation—directed specially to this point, which were proved by a method of measure- meut employed specially for the purpose to carry the power of our most delicately constructed lenses considerably further than the mathematician considered possible ; revealing, indeed, smaller objects than those mathematically indicated ; and Mr. Dallinger did not by any means believe that he had wholly exhausted the utmost power of visibility by these experiments. A discussion followed, which was chiefly concerned in eliciting more in detail the method employed in these delicate measurements. The meeting concluded with the usual conversazione, at which there was a good display of microscopes and many interesting objects exhibited. Ml BRUROsnteen i | H q No pyr d oO THE MONTHLY MICROSCOPICAL JOURNAL. MAY-1, 1877. I.—The various Changes caused on the Spectrum by different Vegetable Colowring Matters. By Taos. Patumr, B.Sc. (Read before the Royau Microscoricau Society, April 4, 1877.) Puate CLXXIX. Tue kind reception that I met at your hands on a former occasion has encouraged me to trespass this evening for a short time on your forbearance, while I lay before you the result of some observa- tions that I have lately been making on the variability of the chlorophyll band in the spectrum. Chlorophyll, Fxcula viridis, or leaf green, is the name gene- rally given to the green colouring matter of vegetables ; it is found in nearly all plants growing in the light, with the exception of fungi and the true parasites, covering either the cell-walls or the spiral bands, as in Spirogyra, or the granular contents of the cells, which are composed of starch, or other similar bodies. If plants that have been grown in the light are placed in the dark, the leaves fall; and if others are produced, they have a whitish colour : again, if the plants that have been thus grown in the dark are removed to the light, the leaves soon lose their white hue, and eventually assume their natural colour; the rapidity with which they become green, and the intensity of their colour, will be in proportion to the amount of light to which they are exposed. The different rays of the spectrum have a varying influence in pro- moting the formation of chlorophyll, and some difference of opinion exists as to which rays are the most active in this respect, but the majority of experimenters agree that the yellow rays are those which are the most essential, because they have the greatest effect in promoting the decomposition of carbonic acid. EXPLANATION OF PLATE CLXXIX. Fic. 1.—Chlorophyl!1 normal. Fic. 7.—Petals of red Cineraria. », 2.—Chlorophyll acid. Hil 8! »» 3.—Leaves of Lobelia. » 9. ¢ Litmus. (Figs. in text.) » +4.—Petals of blue Cineraria. syn LOE », 0.—Leaves of Shumac. », 11.—Hypericene normal. » 6.—Tradescantia. 5, 12.—Hypericene acid: Note.—Class 1 isa symmetrical band. Class 2 is an unsymmetrical band. VOL, . XVII. g 226 Transactions of the Royal Microscopical Society. Mr. Fremy investigated the nature of this agent, and has ascertained that it is composed of two colouring principles, one a yellow, the other a blue; the former he has called phylloxanthin, and the latter phyllocyanin. Both these principles have been isolated by Mr. Fremy, who has also endeavoured to show that the yellow colour of blanched and very young leaves is due to the presence of a body which he has termed phylloxanthein, and which is coloured blue by the vapour of acids. The same result occurs in the discoloration of phyllocyanin; hence it would seem that this phyllocyanin is not an immediate principle, but that it is formed by the alteration of phylloxanthein, and indeed the spectroscopic observations that have of late years been carried on in relation to this subject, I am sure I may say by Mr. Sorby, tend to show that chlorophyll is more complex than Mr. Fremy considered, as the substances he treats of were probably only products of decomposi- tion by acids. The various shades of green seen in the organs of plants depend upon very different causes; partly upon the nature of the chlor- ophyll, whether it is pure, or more or less mixed with the yellow, blue, or brown products of its decomposition—see Mr. Sorby’s paper “On the Colours of Leaves at different Seasons of the Year;” partly upon the quantity of chlorophyll in the individual cells, partly on the thicker or looser arrangement of those cells, as on the under sides of leaves, which are generally of a lighter green, depending on the intercellular spaces which are there present, and which reflecting the light, white, thus mix with and diminish the intensity of the green. When any form of chlorophyll is treated with ether or alcohol, the colour is abstracted, while the organized forms, the corpuscles, &e., remain, so that true chlorophyll is really only a soluble sub- stance, dyeing the bodies called chlorophyll granules, &.; but the various degrees of solubility depend greatly on the presence of other substances, for instance, in the case of such evergreens as laurel, ether takes hardly any effect, but alcohol thoroughly dis- colours the leaves, whilst pyrethrum, a perennial, is hardly acted upon at all by alcohol, but ether takes great effect. If these solutions are evaporated to dryness, under the ex- hausted receiver of an air-pump, a green fatty matter is left, which forms soaps in combination with the alkalies. If this is again dis- solved in ether, and mixed with water, and the ether evaporated, small greasy globules are obtained, and similar globules are sepa- rated from the alcoholic solution at a freezing temperature. If the alcoholic tincture be mixed with water, and the alcohol evaporated by heat, part of the fatty substance is precipitated; the remaining solution is coloured a brown yellow, and has a characteristic smell, like that of black tea. It is soluble in the volatile and fixed oils, Changes caused on the Spectrum, &e. By T. Palmer. 227 but when treated with sulphuric acid it is either not changed or else carbonized. With regard to the second point or the colouring matter of plants, the green colour, which forms the most extensive class, has been treated upon in our primary consideration on chlorophyll; the red and yellow colours, as assumed by the leaves in autumn, are due to a chemical metamorphosis of the chlorophyll, and consequently the discoloration of the cellular tissue: see also Mr. Sorby’s paper “On the Various Tints of Autumnal Foliage.”* But independent of all this, there are the colours of the red cabbage, copper beech, and similar plants, all of which depend upon the existence of a special colouring liquid in the usually colourless epidermal cells, obscuring the chlorophyll which lies beneath. The bright colours of plants, and other parts of the inflorescence, as also on the lower surface of many leaves, Begonix Victoriz, for instance, as well as numerous herbaceous shoots, arise from the presence of matters of a different kind, almost always dissolved in the watery cell-sap. The colour of petals is ordinarily found to depend upon a certain number of the cells subjacent to the epidermal layer being filled with a coloured fluid, and the depth of the colour is proportionate to the number of superimposed layers of such cells, which act like so many layers of a pigment: each cell is usually filled with one colour when fully developed, but adjacent cells are often seen in variegated petals to contain distinct colours, the line of demarcation being accurately fixed by the cell-walls, through which the colours do not transude unless injured by pressure. In young tissues the colour has often a granular appearance in the cells, but this is a deception, arising from the mode in which it is developed. The colourless protoplasm, originally filling the cells, becomes excavated as it were by water bubbles, and the watery contents of the excavations become coloured ; they gradually enlarge, as the proto- plasm applies itself more completely to the walls of the cell, until they become confluent, and the coloared liquid fills the whole cell- cavity. ‘The isolation of the coloured juice in each particular cell seems to depend upon the primordial utricle, or parietal layer of protoplasm ; when this is injured by pressure or other external causes, endosmose is set up, and the integrity of the cell destroyed. In some cases the liquid colouring matter of flowers has been found to contain solid corpuscles; the red-colour cells of Salvia splendens and the blue ones of Strelitzia regina contain globules, and according to Von Mohl this is still more commonly the case with the yellow colours. In the yellow, perigonal leaves of Strelitzia regina, the colour is said to depend on the presence of crescentic filaments, floating in the cell-sap ; the white patches also on variegated and spotted leaves, such as those of Aucuba, Holly, * “Quart. Journal Se.’ vol. i. p. 64. 9 8 228 Transactions of the Royal Microscopical Society. variegated mint, Begonia, Argyro stigma, &c., arise from the absence of chlorophyll in the cells subjacent to the epidermis at those parts, which produces the same effect as we see in leaves that have been mined by caterpillars. Now it follows that the colouring agent which is found in vegetables is in several states of combination; first, with the extractive principle; secondly, with the resinous principle ; and thirdly, with a starchy or gummy principle, and it is these states which indicate the means of extracting them. Firstly, when, as in the case of logwood, madder, &c., the receptacle of the colour is of the nature of extracts, water is capable of dissolving it. Secondly, certain of the resinous colouring matters are soluble in alcohol, spirits of wine, or ether, and form in many cases the pharmaceutical tinctures: the other principle will be left, as it is hardly in connection with our subject. We will take as a standard the two solutions of chlorophyll, viz. that in oil normal, and that also in oil acid. In chlorophyll No. 1 we have a spectrum made up of four bands, two of which are definite, and one shaded, while the other is a general absorption of the blue end. Compared with this, we have chlorophyll No. 2, or that to which a small quantity of acid has been added ; we find on examination that a general displacement towards the blue end has taken place, which result, as shown by Mr. Sorby,* is due to a true decomposition of the original sub- stance, obtained when acid is added,{ though it is not regained when the acid is neutralized, as the normal action has gone too far for subsequent recovery; a material transformation has, however, taken place in the whole spectrum, the bands are constant though displaced, while their ratios are almost identical; this will be more clearly seen on reference to Fig. 2. We deduce that the acid has transformed an original sub- stance, which had the power of absorbing the rays of light, beyond » 652°0; still another band is produced at » 662-0, and though the bands 2 and 8 are proportionately shifted towards the blue, and have likewise gained in intensity, the general absorption is constant, and has sustained no apparent change: does it not appear possible that, in the case of solutions contaiming more acidity, this general absorption might be carried still farther into the blue, as, for instance, in other of the colouring agents of plants ? and if so, then in the event of an alkaloid form being also present in combination, the same spectrum as Fig. 2 may be still maintained, while the general absorption, &c., will be more nearly approached * ‘Roy. Micro. Jour.’ vol. xiii. + See Mr, Sorby’s paper “On Comparative Vegetable Chromatology,” ‘ Royal Society Proceedings,’ vol, xxi. p. 406, ‘Changes caused on the Spectrum, &c. By T. Palmer. 229 towards the red: take, for example, two vegetable colouring matter spectra; first, leaves of Lobelia; secondly, petals of blue Cineraria, for which I must refer you to Figs. 3 and 4. Fig. 1.—CHLOROPHYLL IN O1L NoRMAL. M. A. Observations. 1 | 23°955 | Centre .. .. | 652°0 | Class 1. Very black; size -510. 2 | 22-700 59 car pedal O0GrO » 1. Centre dark, ends shaded; size * 200. 3 | 21°700 x ob on ae 7(OPar » 1. Very shaded ; size °400. 4 | 20°500 | Commencement | 515°5 | Shaded at first, terminating in a very black absorption. Fic. 2.—CHLOROPHYLL IN Orn AcID. | 1 | 23°85 | Centre 662°0 | Class 1. Very black; size °5. NOSES Sete een | OUSwe » 1. Shaded; size 3. Si 295 a vo co | BBL » 1. Black; ends shaded; size °3. 4 | 20°5 Commencement | 515°5 | Shaded at first, terminating in a very | black absorption. Condition. | A. | A. | A. | Ratio.4 IharGybl Vac be 652°0 598°5 547-25 if 8 OGL ET ACIGY tere 662°0 608°0 537°0 Ios) °9188 Fic. 3.—LEAVES OF LOBELIA IN ETHER. M. A. Observations. 1 | 23:892 | Centre .. .. | 658°0 | Class 1. Very black; size °415. 2 | 22-650 5 sco, |) CULE », 1. Centre dark, ends shaded ; size °3. 3 | 21:450 os Bo no | Eawe 3, 1. Very shaded; size °3. 4 | 20°050 s oe, | aa2rO » 1. Black; size °3. 5D | 26°6 Commencement | 512°0 | Very black; general absorption. Fic. 4.—Buivur CINERARIA IN OIL. 1 | 22°44 | Centre .. .. | 615°0 | Class 1. Centre dark, shaded at ends; size *435. 2 | 21°135 = co io || ore » 1. Centre dark, shaded at ends; size 630. 3 | 20°0 + ss Ooo: O » 1. Very shady; size °4. 4 | 19°25 = «» « | 490°0 | Same as No. 1; size °d. D> | 16°0 Commencement | 426°0 | General absorption. a 230 Transactions of the Royal Microscopical Society. In the former specimen, which is prepared in ether, we have almost a facsimile of Fig. 2, though band No. 4 has disappeared ; where it began however, a general absorption is evident, bands 1 and 2 are brought nearer the blue end, while No. 3 is farther from it. The spectrum from the petals of blue Cineraria, Fig. 4, is perhaps more striking, as the bands are all nearer the blue end, while their symmetry with the preceding spectra is considerably altered, still owing, no doubt, to the presence of an acid, though comparison is hardly admissible, as the former specimens are prepared from the green leaves, while the latter is extracted from the blue petals of the flower. We will now pass on to consider the spectrum of Shumac. This substance contains a considerable percentage of tannic acid ; Mul- ligan and Downing give 24°37 per cent. Having procured some of the leaves of this plant from Palermo, I pulverized them, and after due preparation the following solution in oil was the result ; the spectrum, which will be seen on reference to Fig. 5, 18 curious enough to attract our notice, inasmuch as it almost agrees with Fig. 2, though the bands are all more or less nearer the blue end, yet the general absorption is increased towards the red. In this case we have a distinct proof of an existing acid in con- nection with the fluid; still there are differences, though to a less extent than in the previously considered specimens; may we not assume from this that the chlorophyll in the case of specimens Nos. 3 and 5 is in combination with some alkaline base, while the colour which is predominant in the case of No. 4, is of an acid construction? At the same time I must acknowledge there is every reason to think that an alkaline form is also present, though to a much less extent. It must, however, be borne in mind that this solution of Shumac is prepared from the dried leaves, and therefore I doubt whether the spectrum from living leaves would not be rather different from the one I have brought before your notice. Fic. 5.—SHumac. M. A. Observations. 1 | 23°857 | Centre .. .. | 661-0 Class 1. Very black; size °485. 2 | 22°60 _ sey ae | 0000 » 1. Centre shaded, ends very shaded ; size *20. SWOT Bad, San ee ees DoOND 5, 1. Indistinct; size °3. 4 | 20-005 is .. .. | 5385°0 | Same as band No. 2; size 33. 5 | 20°465 | Commencement | 517°0 | Very black; general absorption. But before leaving a subject which appears of some importance, there is one more solution, that of Tradescantia, Fig. 6, which is well worthy of our attention, as I think it bears especially on a Changes caused on the Spectrum, &c. By T. Palmer. 231 point which I wish to make quite clear. You will notice in this instance that band No. 1 is considerably more shaded than those hitherto mentioned, besides being nearer the blue end; this same effect occurs with bands Nos. 2 and 3, but unlike the other spectra they are dark and well defined, though of Class 2, or unsymmetri- cal, their terminations towards the blue being shaded, Fic. 6.—TRADESCANTIA. M. A. Observations. iL || Bets} Centre .. .. | 611:0 | Class 1. Shaded; size -3. 2 | 21-175 a go on) || BLEW » 2. Black, shaded to the left; size *7. 3 | 20°05 ‘5 532°0 » 2 Same as No. 2, though lighter; size °5. 4 | 19:2 Bs SH ob. | eke nlots » 1. Shaded as No. 1, centre darker ; size °6. Band No. 4 will be seen to agree with the corresponding one in Fig. 4, while the general absorption, which we have noticed forms so characteristic a feature in all the previous spectra, is entirely absent. Now it is just this fact which appears to me so curious, for here we have a spectrum which, if I may use the term, includes the whole of the other spectra, and yet it is so dif- ferent, though to an extent. it is accounted for I think, when con- sidered in connection with blue Cineraria, another part also of the inflorescence, in which the chlorophyll is only disseminated in a small degree, as compared with the leaves, &c.: then, with regard to the comparison of blue Cineraria, Tradescantia is certainly more astringent, but time and experience alone will answer these ques- tions, and we will now pass on to consider the second part of my subject. ; . Part IT. You will doubtless have perceived that hitherto I have only taken those forms of plants which have some similarity to the chlorophyll itself; we will now proceed to consider briefly the totally different colours, such as red and yellow. First we have red Cineraria, which for the sake of comparison is prepared in the same way as the blue, and it is to this Jatter, as compared with the former, that I wish to call your special atten- tion. The spectrum, as will be seen on reference to Fig. 7, differs from Fig. 4 in a notable degree; but as most present, no doubt, recollect the inference our worthy President, in vol. xiii, of our researches, drew between this colouring matter and that of Lobelia speciosa, | need hardly pursue my investigation further, ag the change here is almost identical, though the general absorption, 232 Transactions of the Royal Microscopical Society. which to a degree is evident in the blue specimen, is entirely wanting in the red. I annex the ratios of Mr. Sorby’s two read- ings and my own, to show how nearly they agree, and Mr. Sorby has since told me that his specimens were dissolved in a strong solution of sugar, which quite accounts for the slight displacement I have recorded. Fic. 7.—Rep Crneraria. ) M. A. | Observations. | 1 | 22-95 | Centre =. «. 585° | Class 1. Ends shaded, centre dark; size *5. 2 | 21°86 + aac 541° », 1. Same as No. 1; size *465. Bi e2029> 45 a ee 499° », 1. Shaded evenly ; size -455. Condition, A. Ae} |r A. Ratio. Blue Cineraria.. 615: 575° 535° 490°1 9265 Red ¥, es 585° 541° 499° a 1 3. -9234 55 59 % 594° 550° 509° is £29258 Lobelia speciosa 619° 573° 529° DS 29257 There may, I think, be found in this alteration of colour some similarity to the chemical effect caused in litmus, when that sub- stance has, through the intervention of an acid or alkali, been turned red or blue, as the case may be; and perhaps I may be per- mitted to add that I have employed the spectroscope in many cases where the determination of an acid or alkaline base has been necessary in chemical analysis. A glance at Figs. 8, 9, and 10 will suffice to show what takes place when the litmus is no more alkaline or acid, as the case may be: the moment at which the change occurs is the saturating point, and it is at times extremely curious to observe the sort of conflict which takes place between the two agents, till,.when subsidence occurs, we have either a normal, acid, or alkaline result ; the only point necessary is, that the original solution of litmus be made of a definite strength, and must naturally represent the normal state; that employed in these ex- periments is of 1 per cent. Now this seems to imply that the red colour of a fresh plant is more especially acid than the blue ; still the conditions of variation are so exceedingly numerous, that to fix anything like a definite why or wherefore as to the cause is quite out of the question, at least so far as my own short experience of nature and natural selection is concerned, I therefore must be pardoned if I shade myself under the following extract, taken from Mr. Darwin's admirable work, entitled ‘The Origin of Species.’ He there says: “ When a variation is of the slightest use to any being, we cannot Changes caused on the Spectrum, &e. By T. Palmer. 233 tell how much to attribute to the accumulative action of natural selection, and how much to the definite action of the conditions of life.” But to pursue the point somewhat further, and still to keep to our author, Mr. Darwin, in his new work, under the heading of “ Uniform colour of the flowers on plants self-fertilized, 22 el 20 19 Ey es a / 16 15 14 13 23 Fic. 8. Litmus normal. =| Fra. 10. Litmus ilkaline, Fic. 8.—Lirmus NorMau. M. | | A. Observations, ° 21°3 Centre 25). 565°5 | Class 2. Very black. 20°7 indies cctin ats 509°0 | Shaded to this point; size 2:5. Fic. 9,—Lirmvus Acrp. 21°2 Commencement a0} Shaded gradually to very black, 20°0 3 % 039°0 general absorption of blue, &c. Fic. 10.—Lirmus ALKALINE. | some \e@entrel ss ia 570°0 ‘. : . pice .on a Ta ee Re 5190 \ Same as in Fig. 8; size 2°25. NRE and grown under similar conditions for several generations.” ‘Time will not, however, permit me to give you his exact words, but I should strongly advise all my hearers to invest in that charm- ing book, which has now been out for some time, and is entitled ‘Cross and Self Fertilization of Plants.’ Mr. Darwin, after-having 234 Transactions of the Royal Microscopical Society. quoted a few cases of experiments, performed with Mimulus luteus, LIpomeea purpurea, Dianthus caryophyllus, and Petunia violacea, says :—‘‘ These few cases seem to me to possess much interest. We learn from them that new and slight shades of colour may be quickly and firmly fixed, independently of any selection, if the conditions are kept as nearly uniform as possible, and no inter- crossing be permitted. With Mimulus, not only a grotesque style of colouring, but a larger corolla and increased height of the whole plant were thus fixed; whereas with most plants which have been long cultivated for the flower garden, no character is more variable than that of colour, excepting perhaps that of height. From the consideration of these cases we may infer that the variability of cultivated plants in the above respects is due, firstly, to their being subjected to somewhat diversified conditions, and secondly, to their being often intercrossed, as would follow from the free access of insects.” “I,” says Mr. Darwin, ‘‘ do not see how this inference can be avoided, as when the above plants were cultivated for several generations, under closely similar conditions, and were intercrossed in each generation, the colour of their flowers tended in some degree to change, and to become uniform. When no intercrossing with other plants of the same stock was allowed, that is, when the flowers were fertilized with their own pollen in each generation, their colour in the later generations became as uniform as that of plants growing in a state of nature, accompanied at least m one instance by much uniformity in the height of the plants. But in saying that the diversified tints of the flowers on cultivated plants, treated in the ordinary manner, are due to differences in the soil, climate, &c., to which they are exposed, I do not wish to imply that such variations are caused by these agencies in any more direct manner than that in which the most diversified illnesses may be said to be caused by exposure to cold. In both cases the con- stitution of the being which is acted on is of preponderant im- portance.” In this last example, viz. Hypericene, I think you will see this verified ; the juice obtained from Hypericum is, as you know, of a reddish orange colour, turning red when treated with acid, but retaining its natural colour to a certain extent when prepared with oil. Our first spectrum, as shown in Fig. 11, represents this latter form. Fic. 11.—HYPERICENE IN OIL. | M. A. Observations. 1 | D8. entros | 2.4 wa. 590° Class 1. Shaded; size °5. 2 | 21°55 os ao) 60 554° Same as No. 1; size °5. 3 | 19°00 | Commencement | 498- | General absorption. | Changes caused on the Spectrum, &e. By T. Palmer. 235 On examination it will be found to be not unlike that of red Cineraria, though the blue end in this case is absorbed. I now added a few drops of acid to the solution, stopping immediately that the change of colour took place. This addition has, as will be Seen on reference to Fig. 12, had a contrary effect on the first two bands; they are, however, increased in definition, though their shapes are of Class 2 or unsymmetrical, while in the case of Fig. 11 they are of Class 1 or symmetrical, and the general ab- sorption in Fig. 12 has advanced towards the red. Fig. 12.—Hyprricense Actp. M. | Ar. Observations. Bsa Riek) Sa 8 . l 22°92 | Centres a, see: aay Class 2. Very black, shaded to the Peeks iy Bind v2 ai" §La0 |) S6b 5's right, mec set | entre: .toeee || 4320 : ‘ 2 { 90:2 Bates (et noe \ » 2. Black, shaded to the right. 3 | 20°6 | Commencement | 512:0 | General absorption. Through the kindness of Mr. Sorby, whom I now take the opportunity of most sincerely thanking, I am enabled to say that the first of these two spectra is not the usual one given by the colouring matter of normal hypericene. He lent me a tube of pure hypericene, the spectrum of which nearly accorded with that of my acid form, though the centres of the bands were different. My first solution, Fig. 11, we are therefore inclined to think is due to the presence of a yellow substance very common in plants, which is made deeper by the addition of an alkali, and much paler by an acid, in which latter case the intensity of the absorption would be increased ; the effect of this is that my solution is yellower than Mr. Sorby’s, and would be made more red by acid. Perhaps it would interest you to know the coloured oil is not unlike that of the solution in water, and like this has no fluorescence. This example now closes my remarks. I think I have brought suffiaent evidence, if not of proof, to substantiate what I have said, at least enough to open up a field for an immense amount of research. The conclusion which I draw from these few specimens is, that any plant, colouring matter, or substance may be so acid that the limit of the band of total absorption may be extended beyond one’s vision into the violet, or that the contrary effect ma be produced on the red by an alkali in excess. That both these states may be present, and that they both may affect the spectrum in their own particular way at the same time, is evident. 236 Transactions of the Royal Microscopical Society. IIl.—Microscopic Aspects of Krupp’s Silicate Cotton. By H. J. Stack, F.G.8., Sec. R.M.S. (Read before the Royau Microscoricat Soctery, April 4, 1877.) Pratrs CLXXX. anp CLXXXI. | SizicaTE cotton is the name under which blast-furnace slag reduced to a fibrous condition is now sold as a non-conducting substance for covering steam boilers, pipes, ice-houses, safes, &e. It is manufactured at the works of Herr Krupp, at Sayn, in Germany, by forcing a blast of steam, water, or air through molten slag, in the viscous state in which it runs from the furnace. Having obtained a specimen through the kindness of Messrs. Jones, Dade, and Co., the English agents, it was found when lightly compressed to be much like cotton wool, but of finer fibre. Amongst the fibres are to be seen a number of bulbs of various forms and sizes, seldom, however, exceeding the magnitude of an ordinary pin’s head, and usually less. The fibres vary in thick- ness from that of common spun glass to an extreme tenuity repre- sented by fractions of a thousandth of an inch. They are easily blown about as a fine dust, and from their material, and forms, as shown in some of the sketches, Figs. 1 to 4, must be very mis- chievous if introduced into the lungs. It is said that special pre- cautions have to be taken to prevent workmen engaged in the manufacture from being seriously, or fatally, injured. - The bulbs present some interesting appearances. They vary in shape and size as Figs. 5 to 17 show, and also in internal structure, though they may be generally described as solid bodies containing more or less numerous vesicles and hollows. Considering the sudden and violent explosive action by which they are formed, little regularity might be expected in their markings, but a considerable number exhibit a very beautiful and symmetrical ornamentation. A spherule, for example, one- thirtieth of an inch in diameter is thickly covered with compound vesicles (see Fig. 18), consisting of a central clear glass film sur- rounded by numerous minute bubbles, the whole when lit up under the microscope having an elegant jewelled appearance. When broken, the bulbs exhibit a conchoidal fracture diversified with small cavities and vesicles. In some cases the symmetrical arrangement last mentioned is found in the vesicles occupying the centre of a bulb. In some spherules obtained from a Yorkshire furnace by Mr. Sorby, numerous groups of crystals could be seen composed of minute prisms arranged in rectangular patterns. To test the mode in which such regular patterns as in Fig. 18 could be formed by explosive action upon a viscous substance, an The Monthly Mierc ee | x 300 | ' | | i , 18 | | } i "Wiest Selo lth Silicate Cotton bulbs. Microscopie Aspects of Silicate Cotton. By H. J. Slack. 237 ounce or two of common rosin was melted in an iron ladle, and when it began to boil suddenly thrown into cold water. An irregular brittle mass was obtained, exhibiting here and there small white patches. These when examined with 3-inch power showed some compound vesicles like Fig. 18, and others as it were in process of formation. It seemed as if the first action of the explosive steam was to produce an immense number of minute vesicles, and that those in the centre had a greater tendency to coalesce than those at the margin. Some centres were composed of a single clear vesicle, others of two, three, and so on. The general character of the silica cotton threads is much like the volcanic product known as “ Pele’s hair”; the bulbs resemble volcanic bombs. In some specimens the bulbs are like common white glass; in others they glow with the iridescent tints of Venetian work, and constitute objects of considerable beauty when illuminated with a side silver reflector. Iron slags producing this material are compounds of silica, alumina, &c. The following analysis from Percy’s ‘ Metallurgy’ may be taken as an illustration of their composition. The specimen was from South Staffordshire, and crystallized in well-defined translucent square prisms * : SHUIET ip? ok se eG pp ede ce LCOS NOMINARy Osho. so ssha- sl) Gaee sce LAUT IDTTIREN Rod as) Soles ote gas eo orl! Miatonesine gag cas ea as se ea RSG Protoxide of manganese .. .. .. 0°40 Protoxide of iron Se 0 ee as) ICH Potash@ «as. tee a Ga ee Se OSD Sulphide ofcaleium.. .. .. .. 0°82 99°81 The spun glass condition of slag is mentioned by Percy, who says,t “owing to some accidental condition the melted slag has actually been spun as it were by the blast, just as glass is spun by a wheel. I have received beautiful specimens of this kind from my friend Mr. Levick of the Blaina and Cwm Celyn Iron Works, and also from Prussia.” The fine threads of silicate cotton fuse readily into beads in the flame of a spirit lamp, but they are unchanged by a full red heat. The substance is not a pleasant one to handle, and no doubt numbers of sharp, and often curved and barbed particles entering the skin would produce great irritation. On this account it is supplied * Percy’s ‘ Metallurgy,’ vol. i. p. 23. t Ibid, p. 27. 238 Transactions of the Royal Microscopical Society. in the form of mattresses 2} inches thick, made up ready for use. Those who must handle it ought certainly to be provided with thick gloves, and great care should be taken not to inhale its fine dust. The rapid cooling of this silicate cotton in its process of forma- tion might be expected to give it polarizing properties, but it only possesses them in a feeble degree. TheMonthlyMicroseopical Journal Mayl.1877. lilt CLXXT. | ( 239 ) TII.—On the Lower Silurian Lavas of Eycott Hill, Cumberland By J. Currron Warp, Assoc. R.S.M., F.G.S., of Her Majesty's Geological Survey. (Read before the Royau Microscoricau Society, April 4, 1877.) PLaTE CLXXXYVII. CONTENTS. Introduction. 1. Examination in the Field. 2. Microscopical Examination. 3. Chemical Examination. Introduction. Tue series of lavas which I propose to describe belong to the northern extension of the volcanic series of Borrowdale, Cumber- land. This series has been treated of in my memoir on the Keswick district, and touched upon in various papers communi- cated to the Geological Society. My object in the present paper is to point out the value of microscopic research to the field- geologist both from a practical and a theoretic point of view, and at the same time to illustrate somewhat in detail the microscopic structure of a fine succession of ancient Silurian lava-flows. Eycott Hill lies in the north-eastern part of the Lake district, just outside the range of the mountains, and a mile and a half north of Troutbeck station on the line of railway from Penrith to Keswick. The hill is often locally known by the name of Berrier Nittles, and its highest point, through which the section (Plate CLXXXII.) runs, is 1131 feet above the sea. 1. Hxamination in the Field. The horizontal section, on the scale of six inches to a mile, Plate CLXXXIL., shows the series now to be described, dipping at a tolerably regular angle of from 35° to 40°. The interstratifica- tion of a thin band of Skiddaw slate (No. 4), near the base, would indicate that these are some of the lowest beds of the whole volcanic series, and although at this particular spot the junction between the Skiddaw slate and the volcanic rocks is a faulted one, there is abundant evidence farther north (given in Survey Reports) of the gradual passage from the one series into the other, or, in other words, of the submarine character of the earlier volcanic deposits, though at a later period the volcanoes became wholly or almost wholly sub-aérial. Whether the entire thickness of more than 2500 feet, shown in the section, represents submarine volcanic deposits is doubtful; from analogy with other parts of the district this is probably noé the case. VOL. XVII. v 240 Transactions of the Royal Microscopical Society. With the exception of four or five thin bands of bedded ash, the whole thickness here given is made up of a succession of lava- flows. The thickness of the highest bed of ash is uncertain, since the ground is obscured by superficial deposits and the unconformably overlapping carboniferous limestone soon hides any further suc- cession eastwards. It is not always easy to determine the thickness of the separate lava-flows, though in many cases they differ somewhat in character from each other, and are frequently highly vesicular in their upper and lower portions. In some cases the vesicles have been most markedly drawn out in the direction of flow. On the whole, the varying character of the beds has given rise, by weathering, to a general step-like form of the hill side, reminding one of the origin of the word trap (¢appa, Swedish, a stair). The ash varies in character from a very fine close fragmentary rock to one made up of large angular fragments, and therefore more properly called a breccia. The colour is often a fine purple, though sometimes the finer ash has the same grey-blue colour as the lava. The latter is also sometimes of a rich purple, but is more generally some shade of green or dark blue. The various lava-flows are of all degrees of texture, from a very compact flinty rock to a finely crystalline and porphyritic one, in which the crystals of plagioclase are sometimes an inch in length. The band of Skiddaw slate interstratified among these lavas, and lying imme- diately beneath a finely porphyritic flow, is not more than six or eight feet thick, and is considerably hardened. 2. Microscopie Examination. Perhaps the most satisfactory method of treating this part of my subject will be to take the various beds in succession, as given in the section, and describe the microscopic structure of each, where necessary. (1) Purple Ash.—This rock calls for no especial microscopic notice, being clearly fragmentary, and sometimes coarsely so. Such ashes when viewed under the microscope, in a thin slice, frequently show broken crystals and fragments of lava or previously formed ash-rocks imbedded in a fine dusty base, which last, under polarized light, with crossed prisms, usually appears dark with scattered points of light. (2) Lava.—Lithologically this rock presents a compact green base with yellowish or greenish tinge and small dark spots. It probably represents more than one flow, as it is about 300 feet thick, and has vesicular portions. Microscopically, the base consists of a mesh-work of minute felspar needles mingled with chlorite and magnetite, and a good Lower Silurian Lavas of Eycott Hill. By J.C. Ward. 241 deal of quartz in cavities. There seems to be scarce any unaltered augite, but, to judge from analogy, much of the chlorite must re- present that mineral. Some of the green mineral has a trans- versely fibrous structure when seen with crossed prisms. (8) Skiddaw Slate Band. (4) Lava (porphyritic) —This highly interesting and beautiful bed is about 100 feet in thickness, and in lithological structure shows a compact greenish-blue base containing dark-green spots of a soft mineral, and large porphyritically imbedded felspar crystals, many of them an inch long. Its microscopic character I have already described in the ‘Keswick Memoir’ (p. 20), and in my paper on “The Microscopic Structure of some Ancient and Modern Volcanic Rocks.” * In both cases coloured drawings are given. That in the ‘Survey Memoir,’ fig. 10, plate ii, shows a fine augite twin imbedded in the base of acicular felspar prisms, the spaces between which are filled up with a dirty green and brown pseudomorphic mineral (chlorite and chlorophzite) and numerous crystals of magnetite. The figure in the Quarterly Journal (fig. 6, pl. xvii.) shows a part of the same more highly magnified, and that in the Plate illustrating this paper (Fig. 1) shows the character of the crystalline base, one of the green pseudomorphs, and a portion of one of the large plagioclase crystals. These last are much cracked, and contain glass cavities, portions of the base, and grains of magnetite; they present very finely the banded structure peculiar to this group of felspars when viewed with polarized light. Augite, in crystals and grains, occurs pretty plentifully; much is in the form of pseudomorphs however (the soft dark spots before mentioned). The large twin spoken of above as figured else- where, contains an interesting example of a glass cavity with a bubble and two magnetite grains, with the following dimensions : Glass cavity +525, of an inch in diameter. Bubble =, of an inch in diameter. Tao i 21 1 1 i Magnetite grains the 3,5 and ~53¢5 Of au inch. Some of the green pseudomorphs seem to be after olivine, pre- senting the form and much-fissured appearance of that mineral. I have detected grains of olivine in an unaltered condition in some of these lavas, and therefore I think there can be no doubt that both it and augite were common constituents at one time, though both have been so much replaced by pseudomorphic minerals through subsequent alteration. The top of this lava is beautifully vesicular in parts, the vesicles being drawn out along the line of flow, and filled with chlorite, chalcedony, and calcite. * “Quart. Journ. Geol. Soc.’ vol. xxxi. p. 406. 7 2 242 Transactions of the Royal Microscopical Society. (5) Ash (100 to 120 feet thick).—This bed serves as a good instance of the value of microscopic examination. It is of so fine-grained a texture that I had originally taken it to be one of the more compact lava-flows, and had no suspicion of its ashy character until examining it under the microscope together with the other rocks in the same series. Unlike most of the fine ash- beds it is free from bedding, and evidently consists of closely com- pacted fine volcanic dust. Microscopic examination shows that the fragments are pretty uniform in size, and that many consist of lava. Next above this ash comes a great thickness of lava-flows, between 700 and 800 feet. They are numbered on the section 6 to 13. A little farther north than our line of section a band of ash and breccia occurs among these flows, but dies out southwards. (6) Lava.—Lithological: a very compact and dark base, with small felspar crystals. Microscopically the base is minutely crystalline, with small felspar needles, very small magnetite grains, and disseminated chloritic matter. Larger crystals of plagioclase felspar very much altered. Very little unaltered augite. Some pseudomorphs, ap- parently after olivine. ‘Small vesicles filled with calespar and chlorite. (7) Lava.—Lithological: compact greenish-grey base, with small felspar crystals and dark spots; breaking with conchoidal fracture. The microscopic structure of this bed is shown in Fig. 2, Plate CLXXXII. The base consists of the usual mesh-work of minute felspar prisms with chlorite and magnetite, and in it are larger imbedded crystals of felspar, all highly altered. There are many chloritic pseudomorphs, but no unaltered augite. (8) Lava.—tLithological: fine-grained base, with a reddish tinge, and containing small crystals and spots. Microscopical: a crystalline mixture of small felspar prisms and small grains and crystals of altered augite (?), with sparsely scattered magnetite. Some larger, but highly altered, felspar crystals, and many small vesicles filled with chlorite and calcite and haying a crystalline edging. (9) Lava—A compact form. (10) Lava.—Lithological: a compact greenish base, with small felspar crystals. Microscopical: fine crystalline base of felspar needles, mag- netite, and chloritic (altered augitic) matter, with porphyritically imbedded crystals of plagioclase felspar, and perhaps some ortho- clase pseudomorphs, after augite and olivine. (11) Lava.—-On the whole, similar to the preceding, but very vesicular. Lower Silurian Lavas of Eycott Hill. By J.C. Ward. 243 (12) Lava.—Lithological: purplish crystalline base, with many small porphyritically imbedded crystals. Microscopical: plagioclase crystals of various sizes imbedded in minutely crystalline base. Magnetite and chlorite, and many brownish-red specks of iron peroxide. Many of the larger crystals of felspar, besides having numerous reddish specks and _ lines scattered throughout them, are permeated by slender veins filled with chlorite. Portions of the base are also sometimes enclosed (or partially so) within the large crystals. No unaltered augite is dis- cernible, but in other respects the general crystalline appearance is quite that of the basaltic class of rocks. For a chemical analysis of this rock, see p. 246, No. 3. (13) Lava.—Lithological: compact dark-blue base. Microscopical: consists wholly of a minutely crystalline mixture of felspar needles, augite grains (a good deal altered), and mag- netite, together with chlorite. For a chemical analysis of this rock, see p. 246, No. 4. A thin band of ash and breccia parts this thick series of lavas just described from the following. (14) Lava.—A vesicular form; small vesicles in a compact greenish base. (15) Lava.—Lithological: grey-blue and highly crystalline base, slightly effervescing with acid. Microscopical: highly crystalline ; plagioclase crystals from the size of the ordinary needles up to those of + inch in length, show- ing the banded structure remarkably well. The larger crystals frequently enclose portions of the base. Magnetite, chlorite, and calcareous matter disseminated. For a chemical analysis of this rock, see p. 246, No. 5, (16) Lava.—Much the same as the last. (17) Lava.—Lithological: compact grey base, with small obscurely-defined crystals and wavy reticulated lines. Microscopically this is perhaps one of the most interesting rocks of the whole series. ‘The base is minutely crystalline, in- numerable small felspar needles all setting parallel to one another, and having a well-marked flow around larger and porphyritically imbedded crystals, much altered. Among the needles is much chloritic matter, and magnetite in fine grains. The crystalline flow is shown in plain light in Fig. 3, and under polarized light in Fig. 4. There are also certain darker bands, roughly parallel to one another, along which the chloritic matter seems to have been converted into a dark-brown or reddish product; these bands sometimes slightly cross the direction of flow. In the example shown in Fig. 3, the porphyritically imbedded plagioclase crystals often contain parts of the base enclosed within them, and portions of their outline are very indistinct, with 244 Transactions of the Royal Micrescopical Society. margins frequently indented by the base running far into the crystals, The quantity of magnetite grains in this sliced specimen is unusually large, and imparts a very dark character to the base. General Remarks on Microscopic Structure. The examination of this series of lavas, and the lavas of the district in general, proves conclusively that the minutely crystalline base of small felspar needles is the prevalent form, though fre- quently much obscured by subsequent alteration. These needles are undoubtedly in many cases triclinic felspar, but in some they may be orthoclase twins of the Carlsbad type. The larger crystals are generally plagioclase, though orthoclase seems to occur some- times. ‘They are replaced both by chlorite and serpentine, but owing to the great number of pseudomorphs of green minerals after both augite and felspar, it is by no means always easy—unless distinctly aided by the crystalline form—to distinguish between the various original constituents. Some of the chloritic pseudomorphs have curious little yellowish granules disposed in irregular lines along them, as seen in Fig. 2. In yet other cases the replacement has been such that in polarized light the whole of the crystal shows a mosaic of different colours, as seen in one case in Fig. 4. The many examples in which the porphyritically imbedded crystals either contain portions of the base shut up within them, or show it running far into their sides, like inlets and bays, clearly indicate that such crystals were formed previously to the consolida- tion of the base. The frequent enclosure of grains of magnetite within the glass cavities of the augite also points to the same fact, and to the very early crystallization of the magnetite. Indeed, the order of formation would seem to be, first the magnetite, next the larger crystals of augite and felspar, and lastly the base, so largely composed of minute needles of felspar, which frequently assume a well-marked flow around the larger crystalline masses. With regard to the augite crystals, it is striking how many slices may be examined, and yet none but pseudomorphs after the mineral be met with, while in other cases—though rather ex- ceptional— most of the larger crystals appear almost unaltered, and frequently exhibit well-marked twins. If this alteration be so prevalent among the larger crystals, there is but little wonder that the finer augitic matter which probably once existed throughout the base, in many or most cases should have been all completely changed, its place being taken by chloritic minerals. In Fig. 4 examples may be seen of partially altered augite crystals, under polarized light. The great quantity of pseudomorphic chloritic matter which prevails among these old lavas entitles many of them to be classed Lower Silurian Lavas of Eycott Hill. By J.C. Ward. 245 as diabases, and it becomes a question whether the term diabase may not thus be best employed to denote a rock belonging to the doleritic or basaltic class, in which the doleritie characters are much obscured by the presence of chlorite, or its more unstable ally delessite or chloropheite, changing to a brownish colour on ex- posure. Zirkel remarks, under the head of diabase,* that the diffused greenish mineral seems to be chlorite, and probably a decomposition product of augite. With regard to the accidental minerals, as they may be called, of these ancient lavas, it should be remarked that excessive altera- tion carried on through such exons of time could scarcely leave them untouched, when the prevailing constituents have undergone so much change; nevertheless both olivine and apatite may be occasionally observed, and there are few characters common to modern basalt which may not be recognized either in full or in part among some of these ancient Lower Silurian lava-flows. It now remains to be seen how far chemical analysis supports the idea of the basaltic character of some of these rocks. 3. Chemical Examination. Having previously had several analyses made of the lavas occurring in the Keswick district, and found their composition to agree with those of a generally intermediate group between the basic and acidic series, I became anxious to test some of these more northern lavas in the same way, and especially some of those which both lithologically and microscopically appeared more truly basaltic in character. I therefore selected three samples from the series described in this paper, of varying texture and appearance, and Mr. John Hughes, F.C.S., has made me the careful analyses which will be found in the table on next page under the third, fourth, and fifth columns. No. 3 analysis is that of the lava described as (12) in our series, and is microporphyritic in character. No. 4 is a very compact variety, and described as (13) in our section, and No. 5 answers to (15), and igs more like a modern basalt both lithologically, and in some respects microscopically, than any others. A comparison of these analyses with a mean analysis of rocks of the doleritic class shows clearly a general correspondence, so that chemically there can be no reason against considering some at any rate of these old lavas as representing ancient basalts. On comparing these three analyses with two of lava from the Keswick neighbourhood, it is seen that the latter are markedly less basic. In my previous papers I have stated my belief that many of the old Cumberland lavas represent the intermediate group answer- * *Mikroskopiche Beschaftenheit,’ p. 407. 246 Transactions of the Royal Microscopical Society. ing to the modern “ greystones” of Scrope or trachy-dolerites, and now I think there is equal reason to believe that at that very remote geological period, the Lower Silurian, there were erupted some lavas also of a basaltic type, and therefore that the idea formerly held of the specific distinctness of the ancient from the modern voleanic rocks is one that cannot be sustained. Mr. Allport has already shown the specific identity of Carboniferous dolerites and basalts with those of modern date, and I think that the microscopic, chemical, and field evidence which I have been able to collect among the volcanic rocks of the Lake district almost as clearly proves the existence of doleritic and trachy-doleritic lavas among the Lower Silurians. ' ANALYSES OF CUMBERLAND LAVAS. (1) (2) (3) (4) (5) ‘ Brown | tron Cr ag Dolerite. Knotts (Keswick Eycott Eycott Eycott Mean Sortie District). Hill. Hill. Hill. Analysis. Silica... .. .. «. | 60°718 | 59°511-| 53°300 | 52°600 | 51-100 | 51-00 Alumina .. .. .. | 14°894 | 17°460 | 20°990 | 17°315 | 22-051 | 16°06 OLA ies! ess ieee 2°354 | 3°705 °926 | 1°486 | 1-022 “84 Soda .. ; 2°843 | 3°093 | 2°456 | 2-622) 2-216 2°66 1 LTC Le rae Pe Oe 6°048 | 5°376 | 8°512 | 7-728 | 11:424 9°53 Magnesia... <5 0% 1:909 |} 1°801 | 3°964 | 3°252 | 2°346 5°18 Ferrous oxide .. 6°426 | 4°926 | 6°343 | 12-043} 5-885 14°75 Ferric oxide .. .. | 1°405 | 1°271| 1:°660| 1°722| 1-210 \ ? Bisulphide of iron .. *395 “604 Phosphoric acid ., "281 "115 *102 +153 “179 Subphuricacid.. .. 103 "086 | trace trace trace Carbonic acid .. .. 1-660 | 1°569 *320 -140 | 1:°820 Loss on ignition .. 964 °483 | 1-120} 1-160 -710 1-42 100°000 |100°000 |£00-000 |100-000 |100-000 Nos. 1 and 2 have been already published in the memoir on the Keswick dis- trict (sheet 101 8. E). Nos. 3, 4, and 5 are new, and unpublished in any paper or memoir. 7 ‘ The Monthly Microscopical Journal, May 1.1877 . , “qyby pazuojod ur =F SDA] AAV )f B Ol-bL'EI-9'b'S soN oyu f 02 sayour 12Aa'7 vag 8 ‘Lben vey -y bat — "Lf on eae -¢ bar — “pon every ¢ bur —-p a exoy +) “bag és UMA A(T PUN) AO QWN?) Cag) Ly 97.0 oA f? SO NTT UDIMNIIS AOMOT % | | “emolg MoppIAS 2 'C SN SP8q YST eum -4/ B 9) ,E1'S'L oN Peer | 9 795 — “WI HookzT Yo syd0", erunaj0, ey. Yybnouy2 Uomo iSlenes LE a> J AT | | ( 247 ) IV.—The Modifications which the Egg of the | Hooded-eyed| ~ Medusa undergoes before Fecundation. By M. A. Grarp. WE may take as a type the egg of Rhizostoma Cuviert. This medusa is found in great abundance, during autumn, along the shore of Wimereux, along with Chrysaora hyoscella and some other Acalephs. The smallest eggs in the ovary are formed of a transparent vitellus, enclosing a germinal vesicle and a nucleolus. One does not recognize any enveloping membrane at this stage. In pro- portion as the ovum increases in size, its transparency diminishes. The vitellus is charged with deutoplasm, and the germinal vesicle becomes more indistinct; at the same time one may distinguish on the periphery a very delicate vitelline membrane closely applied ,against the vitellus. At a further stage the egg presents on its surface a series of spherules equally spread over the whole. These are filled with a perfectly transparent substance, and are separated from the external membrane by a thin layer of granular proto- plasm, identical with that which occupies the centre and covers over the germinal vesicle. An optical section of the egg may then be compared roughly with that of a young vegetable stem at the moment the first circle of vascular bundles appears, which then divides the parenchyma into three parts: one central, one peri- pheral, and a third radial, uniting the two. The hyaline spherules rapidly increase till they touch each other, and at the same. time they attack the vitellne membrane. With a slight magnification it seems as if the vitellus was surrounded by a layer of cells which projected from its surface at right angles. More highly magnified one sees that the central granular protoplasmic mass is connected with the vitelline membrane by an immense series of little columns widened at both their extremities like the stalactitic columns we sometimes find in a cavern, uniting the two masses of stalagmite, that of the ceiling and that of the floor. These columns are con- stituted of a protoplasm less granular than that of the interior of the ovum. Finally, at the moment when the egg arrives at matu- rity, the columns break and leave only very slight thicknesses of the vitelline membrane at their former points of attachment. Then we have a central granular mass in which the germinal vesicle is not directly observable, and around this mass a transparent zone, which separates it from the vitelline membrane. Professor Harting has seen in the eggs of Cyanea Lamarekii and C. capillata the stage in which the columns appear,* but not * Harting, “Notices Zoologiques” (‘ Niederlandisches Archiv,’ Band [r, Heft IIL). 248 Modifications in Egg of the Medusa, &c. By M. A. Giard. having completely followed the preliminary phases he has given a false interpretation of the appearances observed. He considered that the ova of Cyanea were provided with a vitelline membrane of a considerable thickness, and pierced by a very large number of pores leading from without inwards, such, said he, as we find in the ovum of certain mammals—perhaps in all—and also in the ovum of many Teleostean fishes, where these pores have a much more considerable dimension. It is evident that these pretended pores are nothing else than columns of a clearer protoplasm to which we have already referred. Thus equally fall to the ground Harting’s supposition regarding the physiological function of these pores, that they may serve as channels for the respiration of the ovum, and also perhaps for the passage of the spermatozoa inwards. The preceding observations were conducted at Wimereux during September 1875. They were part of a series of researches not yet completed on the development of Medusz, and I decided to” publish them now because they seem to me to acquire a generality and an importance much greater than I at first supposed, thanks to the magnificent investigations of Weismann upon the ovum of the Daphnoidz (Clodocera).* Weismann has observed a process very like that which we have described, in the formation of what he calls the shell (schale) of the winter egg, in the genera Polyphemus Sida and Daphnella. It is remarkable that in this case, as in that of the Meduse, the egg underwent a tolerably long incubation in a special medium fur- nished by the maternal organism. The excretion of hyaline vesicles, which takes place from the entire surface of the vitellus in the ovum of Rhizostoma, may in other animals be limited to a portion of the surface. The pheno- menon then will have the appearance of a sort of excreted globules. One may—in the presence of this process—ask if the phenomena frequently pointed out, of rejection of a certain part of the vitellus at the moment of the maturation of the egg, should be regarded as equivalents in all animals in which they have been observed. Biitschli has in the clearest manner shown that the corpuscles de direction of the egg of Lymnzxus, Succinea, Nephelis vulgaris, and of Cucullanus elegans, arise by the process of cellular division. I may add that it is the same in Sulmacina Dysteri and in Spirorbis. In these various animals the excreted corpuscles have the value of rudimentary cells, having an atavic signification, and cannot be suitably styled refuse corpuscles (corpuscles de rebut). This term may, on the other hand, be applied to non-cellular * Weismann, “ Zur Naturgesch. der Daphnoiden” (‘ Zeitschrift fiir Wiss. Zoologie,’ XX VILL. Band, 1 and 2 Heft). Modifications in Egg of the Medusa, &c. By M.A. Giard. 249 materials, which, rejected by the vitellus, serve in the formation of accessory organs of the egg, for example of the shell (a coque) or the vitelline membrane. Such are the hyaline vesicles of the ovum of Rhizostoma Cuvieri. Errata in the President’s Address.—At page 129, in the bottom line, for orthoclase read oligoclase. At page 130, in the second line from the top, for abite read albite, and for oligoclase read orthoclase. At page 134, in second line from bottom, omit the words of gypsum. ( 250 ) PROGRESS OF MICROSCOPICAL SCIENCE. " Recent Researches on Kélliker’s Dieyema.—Professor Van Beneden has made some very important researches recently on the peculiar worms that bear the above name, and which appear to be parasitic on the renal (?) organs of various Cephalopods. These researches have been fully reported by (we suppose) the. younger Packard in the ‘American Naturalist. He says that Van Beneden claims of these species that they have no general body-cavity. The body is formed (1) of a large axial cylindrical or fusiform cell, which extends from the anterior extremity of the body, enlarged into a head, to the caudal extremity ; (2) of a single row of flat cells forming around the axial cell a sort of simple pavement epithelium. All these cells are placed in juxtaposition like the constituent elements of a vegetable tissue. There is no trace of a homogeneous layer, of connective tissue, of muscular fibre, of nervous elements, nor of intercellular substance. There is only between the cells a homogeneous substance, as between epithelial cells. The axial cell is regarded as homologous with the endoderm of the higher animals. He designates as the ectodermic layer the cells surrounding the large, single axial cell. There exists no trace of a middle layer of cells. We discover no differentiated apparatus; all the animal and vegetative functions are accomplished by the activity of the ectodermic cells and of the axial cell. On account of these characteristics Van Beneden regards these organisms as forming the type of a new branch of the animal kingdom which he distinguishes as Mesozoa. Hach species of Dicyema comprises two sorts of individuals differing externally, one (the Nemuatogene) pro- ducing vermiform embryos, the other (Rhombogene) infusoriform young. The Nematogenes produce germs which undergo total seg- mentation, and assume a gastrula condition. After the closure of the blastopore the body elongates, and the worm-like form of the adult is finally attained, as they pass through the body-walls of the parent. The germs of the Rhombogenes arise endogenously in special cells lodged in the axial cell and called “germigenes.’ The germ-like cells undergo segmentation, and then form small spheres which become infusoriform embryos. The worm-like young is destined to be developed and live in the Cephalopod where it has been born, while the infusorian-like young probably performs the office of dis- seminating the species; it transmits the parasite of one Cephalopod to another. This work is also an important contribution to histology, particularly to the subject of cell-division. Says Van Beneden, “ the recent researches of Auerbach, of Biitschli, of Strasburger, of Hert- wich, and those that I have published, have established the fact that the division of a cellule, that is to say, the multiplication of the cellular individuality, is the resultant of a long series of complex phenomena, accomplished in a determinate order, and having their seat as much in the nucleus as in the substance of the cell.” Finally, Van Beneden places in his branch of Mesozoa the hypothetical Gastreades, which PROGRESS OF MICROSCOPICAL SCIENCE, 251 term he applies to (gastrula-like) organisms formed of two kinds of cellules, some ectodermic, others endodermic, in which the endoderm is formed by invagination. He calls Planulades, those hypothetical Mesozoa which are formed from a many-celled sphere constituted like a Magosphera (Haeckel) and in which the two cellular layers are developed by delamination. He therefore divides the animal kingdom into three primary groups, that is, the Protozoa, the Mesozoa, and the Metazoa. i A curious New Sponge, Kallispongia.—Professor E. Perceval Wright describes * a beautiful little sponge found growing on the fronds of some species of red seaweeds from the coasts of Australia. _ The largest specimens measure not three millimeters in height. The sponge consists of three distinct and well-marked portions: firstly, a small basal disk; secondly, an elongated stem, on the summit -of which expands the third portion, or capitulum. The disk is button- shaped, flat, and is formed of an irregular horny framework, twice to three times as broad as the stem. The stem varies in height, and presents the appearance, in some cases, of a series of margined rings, some twenty in number, fastened together one on the top of the other; in others the margins of the rings will be more prominent, and the bodies of the rings will be, as it were, more deeply sunk. In both these cases the horny framework is of a more or less evenly latticed character, the longitudinal lines of the lattice being very prominent. The head portion, in its natural state, probably presents a more or less spherical form, perhaps slightly flattened on the summit, with an in- dication of being divided into four nearly equal parts, the open space between these leading into the body-cavity of the sponge. In some of the specimens the head portion nearest to the stem seems to have been formed of a somewhat denser framework than the upper portion, so that while being pressed this upper portion has been fractured across. The framework here is of a densely reticulated kind, in appearance reminding one of the reticulated network of the intracapsular sarcode in Thalassolampe, or of the tissues met with in some Echinoderms. This sponge has been called Kallispongia Archeri. The wonderful mimetic resemblance which it bears to some Crinoid forms can scarcely be overlooked. Leaving the texture and composition of the skeleton mass for the moment out of view, and simply looking at its outline—the circular disk-like base, the stem—the profile of which is absolutely the same, except as to size, as that of the pentacrinoid stage of Antedon rosaceus, and the slightly cleft head, the resemblance is very great. The Microscopic Anatomy of Vaccination.—Messrs. Braidwood and Vacher have published a very lengthy report on this subject in the ‘British Medical Journal.’ In this they state the following con- clusions :—a. The principal local changes excited by the vaccine contagium affect the rete mucosum, and consequently the hair- follicles. 6b. They consist in corpuscular infiltration of this tissue. c. The corpuscles to be most distinctly seen during the earlier days * ¢ Proc. R. Irish Acad.’ vol. ii. ser. 2, part 7. 252 PROGRESS OF MICROSCOPICAL SCIENCE. after inoculation, infiltrating this tissue, are oval or round nucleated cclls, deeply tinged by carmine. d. On successive days, these cor- puscles are to be seen in the crypts or hair-follicles budding or throwing off minute, round, highly refractive bodies. e. During the later stages, when the pock has nearly matured, these corpuscles elongate into fibres, or shrink up. jf. In becoming fibres, they encroach on the hair-shafts and hair-follicles. In none of the pre- parations examined by us have we observed any bacteria, fungoid forms, or allied organisms. Dr. Klein’s Observation on Small-pox.—We regret that this has not been noticed earlier, but it is of so much importance that we cannot allow it to remain absolutely nnnoticed. It is this. Dr. Klein has been convinced by Dr. Charles Creighton that his observations published in the ‘ Philosophical Transactions’ (vol. 165, part 1) are in part incorrect. He there described certain structures in the lymphatics of the skin as the mycelium of a fungus which he termed Oidium variole. He has, since Dr. Creighton published his paper, re- called his former observations. With an honesty of purpose for which it is hard to praise him too much, Dr. Klein says:—“ A comparison of the two kinds of specimens convinced me that the appearances re- presented in my figs. 18 and 19 are not due, as I supposed, to a mycelium in the cavities of the primary pustules, but are products of coagulation of some albuminous or kindred material by the reagent that had been employed for hardening the object in question (dilute chromic acid and spirit). The vegetable nature of the other structures —viz. those represented in figs. 9, 10, and 11 (i.e. the supposed mycelium in the lymphatics of the skin of the pock), as well as those in figs. 16 and 17 (i. e. the mycelium in the cavities of the secondary pustules)—becomes therefore very doubtful. My doubt as to these being also produced by coagulation is based partly on the similarity between the last-named features and those undoubtedly non-vegetable objects in Dr. Creighton’s specimens and also in my figs. 18 and 19, and partly on the following circumstances :—(1) I have lately ascer- tained that blood, especially in febrile conditions, which is contained in blood-vessels of tissues that had been subjected, in a fresh con- dition, to the hardening fluid (e. g.c hromic acid), presents appearances very similar to branched mycei:ium-threads to which are attached numerous conidia; the presence of more or less unaltered blood- corpuscles proves their true character. (2) I have likewise seen that blood-plasma containing globulin or parts of blood-corpuscles, when in lymphatic vessels or kindred spaces, show sometimes in the course of coagulation similar appearances. Whether the greater number of the thread-like structures is due to fibrin or to blood-corpuscles I cannot determine as yet; but it seems to me that both is the case.” Mr. Sorby on the Red Clays of the Ocean-bottom.—The President of the Royal Society, in his late address, makes the following observa- tions on this subject :—‘“ Before leaving this subject, I must mention the endeavour of our Fellow, Mr. Sorby, to determine the nature of the Red Clays of the ocean-bottom, of which we have heard so much. PROGRESS OF MICROSCOPICAL SCIENCE. 253 He informs me that, though any conclusions now to be drawn from his observations must be provisional, it is safe to consider that many specimens of the Red Clay are so entirely analogous to what the Gault must originally have been, that those specimens might almost be looked upon as being as truly modern Gault as the Globigerina-ooze is modern Chalk. In the Gault the grains of fine sand are chiefly quartz derived from the decomposition of schistose rocks. But the Pacific and Atlantic muds from great depths contain, besides quartz fragments, others of glassy felspar, pumice, and other volcanic pro- ducts; and Mr. Sorby has not been able to detect any difference between the main mass of the Gault and other rocks which are com- posed of very minute granules like those derived from felspar or other minerals which, in a similar manner, easily undergo complete chemical decomposition. Independent, therefore, of the presence of different organic remains, and of the modern volcanic products, there is little or no difference between the Red-Clay deposits and some of the earlier stratified rocks.” Empusca musce.—On this subject a paper was lately read before the Quekett Club, and appears in the last number of the Journal, by Mr. T. Charters White. He said, among other things, that the characteristic appearance of a fly affected with this disease is best detected when the fly, in its last moments, settles on a window; it then may be recognized by a zone of white deposit surrounding the fly like a halo—the fly maintains its living attitude, and will be found attached solely by the lips of its proboscis. Its legs are not crossed under it as is the case with all dead insects, but distended, as in the live state. Examining the fly now externally, you will find the hairs covered with minute white globules. These are the spores of the fungus, and are scattered also round the fly for some distance, in a very curious manner; in some cases almost as if they had been squirted out of regular points of the body. ‘The abdominal rings are separated by about their own breadth from each other, while they seem bursting from over-distension. 'The thorax and head do not seem so much affected as the abdomen. On opening the fly in a little glycerine and water, the cause of this over-distension is soon discovered by the appearance of a dense mass of mycelium threads, that emerge as soon as an opening is made in the abdomen, On the termination of Mr, White’s paper, a few very sensible observations on it were made by Mr. W. W. Reeves, which we quote as follows. He suggested that Mr. White might have carried the subject further with greater ad- vantage, for if they wished to follow up the growth of this fungus they must not be content merely to watch it as found upon dead flies, this being only half its history. Let them drop the fly into water, and then see what would take place. In a short time they would see the fungus grow out and develop in a very beautiful manner. It never fully developed upon a window pane for want of sufficient moisture, but if this were supplied much more could be seen of its history. Very little was known about it, but if anyone wanted to become better acquainted with it, by placing a fly thus attacked in a little water its further growth might be readily studied. Like many of this 254 PROGRESS OF MICROSCOPICAL SCIENCE. class of fungi it assumed different forms under different cireum- stances. It might be that the fly got into a diseased state, and settled upon the moist window pane—for it was only to be observed in damp weather. In the fifth volume of the ‘Quarterly Journal of Microscopical Science,’ p. 154, some account of it would be found ; and in vol. iii. p. 55, of the early Transactions of the Microscopical Society, it was described and figured by Mr. Cornelius Varley. Mr. Reeves added that the fungus was not confined to the house-fly—it was found also on the blow-fly and several other insects. Early Development of Sponges.—In a recent report of a meeting of the Société Vaudoise des Sciences Naturelles, ‘ Nature’ says that Pro- fessor Forel spoke on an interesting occurrence of an early develop- ment of sponges in the Lake of Geneva, due to the unusually mild winter of this year. The fluviatile sponge of the lake consists of a horny skeleton with very fine siliceous spiculs, covered with a sheet of soft, perforated animal matter. Usually, in autumn, this soft matter leaves the exterior ramifications and condenses under the form of small gemmule, half a millimeter in diameter, in the deepest interior parts of the horny skeleton. There it remains until the spring, when it expands anew upon the ramifications, and covers them with a sheet of living animal matter. But this year M. Forel observed on February 2, besides many sponges in their hibernal state, a colony of other sponges which had already reached their full summer de- velopment, differing only by a somewhat paler colour from the usual summer appearance. The occurrence is perfectly explained by the circumstance that the temperature of water in the Lake of Geneva was this year higher by two degrees than the average temperature for many years, which is 6°°3 Cels. for December and 4°°9 for January. The Structure of Itacolumite has been recently described to the Academy of Natural Sciences of Philadelphia,* by Professor W. P. Blake. The specimens, which were obtained in California, were un- usually fine, some being over 30 inches in length, and only 2 square inches in section. The colour and the structure appear to be the same as in flexible sandstone from other localities.. Thin and small scales of silver mica are abundant. It bends with little re- sistance up to a certain point, and without elasticity, but is rigid beyond that point. When held up by one end and shaken, the motion is transmitted in wave-like vibrations as in a cord, but the limit of movement is sensibly felt like a blow or shock. A specimen 32 inches in length may be bent 73 inches to one side or the other of a straight line. The freedom of movement is greatest at right angles to the plane of lamination. The specimens are also capable of being sensibly extended when pulled. In a specimen 82 inches long the extension amounted to about half an inch. The freedom of movement up to a certain point and the rigidity beyond that point indicate that there is a tolerably uniform distance between the grains of sand and a certain amount of movement possible among them, and that by bend- ing, the grains are brought into contact with each other. The theory * December 3, 1876, PROGRESS OF MICROSCOPICAL SCIENCE. 255 of the late Professor C. M. Wetherill that the grains of sand are shaped like dumb-bells was referred to with a doubt of its correct- nes. The part which the scales of mica play can only be shown by the examination under a microscope of carefully ground sections of the stone, which might perhaps be prepared for cutting by solutions of soluble glass. On concluding his remarks, Professor Blake was followed by Professor Leidy, who stated that he had examined Itacolu- mite microscopically without being able to detect anything like the dumb-bell structure described by Dr. Wetherill. He supposed that the intermingling of grains, differing in translucency and colour, gave rise to the impression of a dumb-bell arrangement. Thus a pair of adherent translucent grains surrounded with smaller coloured ones would give rise to such an impression. Circulation in a Fungus.—Mr. A. Lister recently exhibited a very interesting microscopic object at the Linnean Society. It was a bit of a lowly organized fungus known as Oldhamia utricularis, and there was seen to be a definite current running along spaces which had certainly the appearance of vessels. This current was of a clearish liquid, having numerous corpuscular elements in it. It was kept up for a considerable space of time. Mr. Lister promised to exhibit it at the Royal Microscopical Society, but unfortunately the approach of cold weather absolutely destroyed it. Botanischer Jahresbericht—We learn that the first part of the third volume of this admirable work has appeared, and we take this oppor- tunity of recording the fact. We received the two earlier volumes some years since, and we have found them very valuable résumés of the work done in previous years, not only in general botany, but in physiological and microscopical work. The Reproduction of Ulothrix zonata.—An important memoir of considerable length has been published on this subject in ‘ Prings- heim’s Jahrbiicher’ (vol. x. part 4), by Dr. Arnold Dodel, and there is an abstract of it as follows in ‘Silliman’s Journal’ for February. The genus Ulothrix belongs to the order Zoosporez, in which the re- production takes place by means of the macrozoospores and micro- zoospores, the former having four cilia and one germinative spot (the name given to the reddish-coloured dot found on one side), the latter having only two. The former bodies have for some time been con- sidered non-sexual, while the latter have been supposed to represent sexual organs which by their union form a body with four cilia, and distinguished from the macrozoospores by having two germinative spots instead of one. This body, which is called the zygospore, cor-_ responds to the organ of the same name in the Desmidez and Con- jugate proper. Dodel confirms the views of Areschoug, Cramer, and others, that the macrozoospores do not conjugate, but, after losing their cilia and coming to rest, grow at once into a new plant. He also agrees, in the main, with Areschoug as to the conjugation of the microzoospores, aud besides has been able to give a more exact ac- count of what becomes of the zygospores. He finds that they remain for a considerable time unchanged, and finally divide into a number VOL. XVII. U 256 PROGRESS OF MICROSCOPICAL SCIENCE. of zoospores, which soon come to rest and grow into new plants, as in the case of the macrozoospores. The latter it appears are more common in winter and spring, and were produced abundantly on thawing tufts which had been frozen, while the microzoospores are more common in summer. The most curious fact observed by Dodel is that those microzoospores which, for any reason, do not succeed in conjugating, grow at once into new plants just as in the case of the macrozoospores. In other words, the sexual process is reduced to the direct union of two bodies so similar that it is impossible to dis- tinguish one as male and the other as female, and furthermore these bodies, if not placed in conditions favourable for conjugating, can at once grow into new plants. It would be difficult to find sexuality of a lower grade than this, where each sexual organ is also capable of re- producing the plant by non-sexual growth. We would recall the case of Eurotium herbariorum mentioned by De Bary, where, of the several male organs (pollinodia) only one succeeds in coming in contact with the female organ, yet all, after the fertilization has taken place, continue to grow and take part in the formation of the sac which eventually encloses the spores. With very rare exceptions in the Thallogens, the male organ at once atrophies after fertilization has been accomplished. A New Parasitic Green Alga.— Nature, of March 8, says that not very long since it was thought that the want of chlorophyll deter- mined the parasitism of plants, and it is still true that the want of this green colouring substance serves to distinguish between fungi and alge. It is also true that the former need already-formed carbon compounds, but it is still thought that chlorophyll-bearing plants not only do not require to find these compounds ready formed, but that they are absolutely unable to assimilate them. It was therefore a fact of great interest when Professor Cohn described some years since (1872) a perfectly new chlorophyllaceous alga,* which he found living as a bright emerald green parasite in the thallus of duck-weed gathered at Breslau. For this the genus Chlorochytrium was esta- blished, and C. lemne was the only species until at a late meeting of the Dublin Microscopical Club, Professor E. Perceval Wright ex- hibited and described a second species found growing and developing itself in the mucilaginous tubes of a species of Schizonema, collected on rocks at Howth, near Dublin, between high and low water marks. There can be no question as to the parasite on the diatom bein different from that on the duck-weed, while there is but little difficulty in placing it in Cohn’s genus. Smaller in size its emerald lustre is scarcely if at all less than the fresh-water species, and like it its development has not been traced farther than the production of ZOOSpores. The Structure of Distoma sinense.—This is very fully given in a paper by Dr. W. Macgregor, of Fiji, which appears in the ‘ Glasgow Medical Journal’ (January 1877), and to which is appended a note by * “ Ueber parasitische Algen,” in ‘ Beit. zur Biol. der Pflanzen,’ Bd. I. Heft 2. PROGRESS OF MICROSCOPICAL SCIENCE. ZT Dr. Spencer Cobbold, fully confirming the author’s views. There is an excellent plate too, representing the natural size (half-inch), and also showing its minute anatomy, of which the following is an abstract :—1. Oral extremity. There is a deep, circular, cup-shaped cavity, having the proper opening of the mouth at its base. From the mouth proceeds a tube that dilates almost immediately to form a pharynx, directly beyond which the tube bifurcates, sending a division along each side to the caudal extremity, where they terminate in ceecal ends without any branching or subdivision. These tubes are no doubt the stomach. The contents are small, granular, usually refractive particles. 3. The water-vascular system. It commences at the extremity of the broad or caudal end, and after coming nearly in a line with the blind extremities of the stomach tubes, it dilates a little, and proceeds onwards in a slightly crooked course as far as nearly one-third the length of the animal. It then divides into two branches, which proceed one to each side until they traverse the stomach tubes, when they subdivide into two branches, one of which proceeds forwards and the other backwards, just external to the stomach. The contents are small, highly refractive particles. The organs concerned in reproduction occupy the greater part of the animal. 4. The ovary —a dark oval-shaped body lying obliquely with regard to the long axis of the parasite, and almost entirely to one side of the median line, from a little beyond which it extends to the stomach tube. It varies in size and shape according to the quantity of its contents. Attached to its end next to the oral extremity of the animal, is an irregular saculated pouch. It would appear to retain the miniature eggs until they are sufficiently developed for extrusion into the uterus. 6. Ducts of the yelk-forming glands. They proceed straight from the uterine pouch one to each side of the animal, and spread out into two beautifully formed bodies, the yelk- forming glands, situated between the stomach tube and the outer edge of the animal, on both sides, as far forwards as the neutral acetabulum and as far backwards as the ovary. Their contents are of a dark brown, but after being treated for some time with a solution of caustic soda, they become of a light red colour. 8. The uterus. A long irregularly branched tube occupying nearly the whole space between the gastric tubes from the uterine pouch behind to the neutral sucker in front. In every specimen it has a dark brown colour from the multitudes of contained eggs. It opens externally upon the surface of a small papilla. 10. The two testes. They are situated the one behind the other in the posterior third of the animal. They present a beautiful dendritic appearance that varies in its details of form in different individuals. It is very difficult to trace the course of the vasa deferentia. They seem to form a common duct, the end of which is modified to serve as an intromittant organ; but my observations on this point are not quite satisfactory. The eggs are very small; they have a brown colour, which is due not to the shell or covering of the egg, but to the yelk-granules. The operculum of the egg is colourless. It is situated at one end of the egg, and seems to be easily detached, as it is not seen on many eggs, even u 2 258 PROGRESS OF MICROSCOPICAL SCIENCE. before extrusion from the uterus. The secretions of the ovary, testes, and yelk-glands seem to meet in the uterine pouch, and to form by their union a fully developed egg, which passes thence into the uterus. The outer covering of the animal has a tuberculated appear- ance under the microscope, but has no cellular formation. Microscopic Changes in the Brain of the Insane-—This is not a subj:ct from which we can hope for much results at present. Still it is necessary to record any results that are arrived at. Therefore a paper that originally appeared in the ‘Dublin Journal of Medical Science, and which has been abstracted in the ‘Medical Record’ (March 15, 1877), is of interest. The author, Dr. Atkins, after referring to the elementary histology of the cortex of the brain, em- braces under three heads the morbid changes he observed in insanity, affecting—Ilst, the nerve-cells; 2nd, the neurogla; 3rd, the nerve- fibres. With regard to the former, the writer first alludes to the fuscous degeneration, and apparently does not hesitate to regard it as identical in its nature with the fatty degeneration of Blandford, and the granular degeneration of Major. The stages of pathogenesis are grouped under the heads of infiltration, precipitation, and disintegra- tion. The chemical nature of the change is regarded as pigmentary rather than fatty. To the pathology of simple atrophy Dr. Atkins adds nothing fresh, and he does not appear to appreciate the fact that the so-called “ giant-cells” are found, when searched for, in all brains. Under the morbid changes of the neuroglia, the coarse fibrillar ap- pearance seen often in epilepsy is regarded as a form of sclerosis. Disseminated and miliary sclerosis are then dealt with, and the pre- sence of colloid and amyloid bodies referred to. With regard to the nerve-fibres, Dr. Atkins appears dubious upon the significance of appearance, which (from his description) must be regarded as the varicose condition artificially produced, and which certainly does not approach the description of Mr. Hamilton’s artificially induced myelitis. The Circulatory System in Magelona.—The anatomy of this curious annelid has been gone into very carefully by Dr. McIntosh, who says of the circulatory system that the blood is a densely corpusculated fluid, the corpuscles having a pinkish colour. There are two large dorsal vessels which arise, near the tip of the tail, from the bifurca- tion of the ventral trunk. They pass forward along the dorsal arch of the alimentary canal, receiving in each segment a large branch from the ventral trunk and numerous capillaries from the intestinal wall, until the posterior border of the tenth segment is reached. At this part their dilated walls are supplied with powerful muscles, which, on the relaxation of the great muscles of the ninth segment, enable them to perform the functions of contractile chambers or “hearts,” and by vigorous systole send the blood forward in a swift stream along the single dorsal vessel of the anterior region. On arriving at the base of the snout the vessel ends in the efferent branch to the tentacle on each side. The current rushes along the latter (nearly at right angles to the dorsal trunk) to the tips, sending off in _ —— a a ee PROGRESS OF MICROSCOPICAL SCIENCE. 259 each a web of circumferential capillaries throughout the greater part of its length, and terminating in the afferent vessel, which proceeds backward, collecting, as it goes, the capillary streams, and then ends by turning forward at the base of the snout as the efferent cephalic vessel. The latter has no evident capillaries, but bends round at the tip of the flattened organ to terminate in the afferent cephalic vessel. A curious change takes. place in the majority of those Magelons which are provided with convoluted lateral organs of the body, in autumn. The cephalic vessels are much abbreviated, and the direc- tion of the current at the base of the snout is somewhat modified. The blood from the head and anterior region collects into a series of large vascular meshes which occur in the anterior region of the body, and in which the current is for the most part under the control of the greatly developed muscles of the body-wali. Thus it happens that the contraction of the latter, and of the special muscular apparatus which closes the communication with the posterior region at the ninth segment, drives the blood forward to unroll the proboscis. This niuscular arrangement in the anterior region and the muscular walls of the vessels themselves at the posterior part of the same division of the body send the current through the relaxed barrier at the ninth segment into the muscular ventral blood-vessel of the posterior region, and onward to the tail, where the trunk ends by bifurcating into the two dorsal vessels. In each segment a lateral branch leaves the ven- tral trunk at the anterior dissepiment, turns round and _ proceeds backward to the next dissepiment, and terminates in the branch to the dorsal vessel. Further, as first observed by Dr. Fritz Miiller, a sac- like dilatation takes place shortly after the commencement of the latter, and it fills at intervals, the distention being followed by a contraction which sends the blood onward by the branch to the dorsal vessel. In vigorous specimens, the currents of the blood are as swift and beautiful as in the tails of young salmon and other translucent vertebrates. When examined in the liquor sanguinis of the living animal a distinct nucleus can be seen in the blood-corpuscle. Professor Leidy on Rhizopods.—Professor Leidy, whose observa- tions on those animals we have from time to time recorded in these pages, has lately read a paper containing further results, before the Philadelphia Academy. This paper is abstracted in ‘Silliman’s Journal’ for March. It seems that Professor Leidy stated that last July, in the sphagnum swamps of Tobyhanna, Pocono Mt., Monroe Co., Pa., he noticed an abundance of a Rhizopod which he thought he had not previously seen, and which he at first supposed to be an un- described species, but which he now viewed as a variety of Hyalo- sphenia ligata. From this, as previously described, it differs in the test being of a pale sienna colour, and perhaps of greater thickness, but otherwise is like it. The test is compressed pyriform, with the length and breadth nearly or about equal, and the thickness one-half. The lateral borders are obtusely rounded. The mouth is transversely oval. The sarcode is colourless, and attached to the inside of the test by diverging threads. The pseudopods are usually from two to three. Measurements, ‘08 mm. long and broad, and ‘036 thick, with 260 PROGRESS OF MICROSCOPIOAL SCIENCE. the mouth ‘02 broad and ‘008. Others varied from ‘06 long and ‘08 broad, to 092 long by :064 broad. In observing the Pocono variety of Hyalosphenia ligata, and the beautiful and well-marked species Hyalosphenia papilio, he detected an important point of structure which previously had escaped his notice. In the active condition of these, and other Difflugians, they are seen with one or more pseudopods extended from the mouth of the test, to the margin of which the sarcode is attached, as well as by diverging threads to various points of the interior of the test. The interval between the body of the sarcode and the interior of the test is occupied with water. The extent of the interval increases with the increase in number and extent of protrusion of the pseudopods, and also varies according to the degree of emptiness or repletion with food of the sarcode body. When the pseudopods are withdrawn into the mouth of the test, the mass of the sarcode expands in a corre- sponding ratio, and the threads of attachment to the inside of the test contract in length. The intervening water appears to be dis- placed through small apertures of the lateral borders and fundus of the test, which exist in numbers usually from two to half a dozen or more. While speaking of Rhizopods, he would ask the attention of the Academy to some remarks on recent observations on the habits of several species of Amceba. One of the species of Amceba which he had most commonly seen, he took to be the Ameba verrucosa of Ehrenberg, with which the A. natans of Perty, and the A. terricola of Greef, appeared to him to be synonymous. ‘This species he had found in many places: in the crevices of the brick pavement in the yard attached to his residence, in brick ponds, in the ooze of the rocky shores of the Schuylkill River, in sphagnum swamps, in marsh mud, &e. It is remarkable for its sluggish character ; and in appearance reminds one of a little pile of epithelial scales, or fragment of dandruff from the head. Appearing quadrately oval or rounded, transparent, and more or less wrinkled, or marked with delicate wavy lines; the pseudopods rise in short obtuse mammillary eminences or wave-like ridges, the sum- mits of which are composed of transparent ectosare, while the central portion of the body is occupied by a thin, pale, diffused, and finely granular entosare. This contains one or more vesicles, usually one, which very slowly enlarges, and then less slowly collapses. In addition, as part of the structure, an oval granular nucleus is some- times visible. The food contents generally appear not to be abundant, and often the creature appears to be empty of food altogether. The character of its food is the same as with other species of Amceba. It not unfrequently feeds on Difflugians. In a specimen from sphagnum water, from Vineland, N.J., last August, he observed an individual, about the 1, of a millimeter, containing a Difflugia and a Trinema together. As observed by him, the species ranges from 51; to 1 of a millimeter in diameter. On the morning of August 27, from some mud adhering to the roots of Sparganium, obtained the day previously in a nearly dried-up PROGRESS OF MICROSCOPICAL SCIENCE. 261 marsh, at Bristol, Pa., he obtained a drop of material for examination with the microscope. After a few moments he observed an Ameba verrucosa, nearly motionless, empty of food, with a large central con- tractile vesicle, and measuring ;!; of a millimeter in diameter. Within a short distance of it, and moving directly towards it, was another and more active Amceba, the species of which he was not positive. It was perhaps the one described by Dujardin as A. limax, by which name, for the present purpose, it may be called. As first noticed, this Amoeba was limaciform, } of a millimeter long, with a number of conical pseudopods projecting from the front broader end, which was zg of a mm. wide. The creature contained a number of spherical food vacuoles with sienna-coloured contents, a large diatom filled with endochrome, besides several clear vacuoles, a posterior con- tractile vesicle, and the usual granular entosarc. The A. limax approached and came into contact with the motionless A. verrucosa. Moving to the right, it left a long finger-like pseudopod curved around its lower half, and then extended a similar one around the upper half until it met the first pseudopod. After a few moments the ends of the two pseudopods actually became connate (the second time he had observed this phenomenon), and the A. verrucosa was enclosed in the embrace of the A. limax. The latter assumed a per- fectly circular outline, and after awhile a uniformly smooth surface ; but the central contractile vesicle remained in the same condition, nor did he once observe it enlarge or collapse. The A. limax now moved away with its new capture, and after a short time what had been the head end contracted, became wrinkled and villous in appearance, while from what had been the tail end a number (ten) of conical pseudopods projected. The A. verrucosa assumed an oval form, and the contractile vesicle became indistinct, without collapsing. Moving on, the A. limax became more slug-like in shape, measuring about 4 mm. long, by = mm. broad. The A. verrucosa now appeared enclosed in a large oval clear vacuole, was constricted so as to be gourd- shaped, and had lost all traces of its contractile vesicle. Subsequently, the A. verrucosa was doubled upon itself; and at this period the A. limax discharged from one side of the tail end, the siliceous case of the diatom, which now contained only a shrivelled cord of endochrome. Later the A. verrucosa was broken up into five spherical granular balls, and these gradually became obscured and apparently diffused among the granular contents of the entosare of the A. limaz. At one moment the five granular balls derived from the A.° verrucosa appeared to be contained in three vacuoles, and the A. limax had amore contracted and radiate form, and then measured 5 mm. in diameter. The observation, from the time of the seizure of the A. verrucosa to its digestion, or disappearance among the granular matter of the entosare of the A. limax, occupied seven hours. From naked Amcebe, the test-protected Rhizopods were no doubt evolved, and it is a curious sight to observe them swallowed, home and all, to be digested out of their home, just as the contents of dia- toms are digested. It was also interesting to observe the cannibal 262 PROGRESS OF MICROSCOPICAL SCIENCE. Amceba swallowing another, and appropriating its structure to its own, just as we might do a piece of flesh, completely, without there being any excrementitious matter to be voided. The Pollen of the Conifere.—The ‘Journal of Botany’ (Feb- ruary) states that in the recently published ‘Atti del Congresso Internazionale Botanico tenuto in Firenze, there is an interesting paper by M. Tchistiakoff on Coniferous pollen, illustrated by two plates. Whether the grains be deprived of or provided with an air- chamber, in both cases the extine is composed of two layers, which are formed simultaneously, by transformation of the two-layered pri- mordial utricle, where the air-chamber is absent; while in the other condition the layers appear successively, the primordial utricle being here very thin, and the inner portion of the extine being laid down from a peripheral layer of plasma which appears after the formation of the thin outer portion. At each point where an air-chamber is destined to appear is seen an interspace between the two layers of the extine, filled with a small quantity of a gelatinous hygroscopic sub- stance. By expansion of the elastic outer extine-layer the interspaces are converted into vesicles; these are seen to be filled with a watery fluid which soon disappears, and the air-chamber is complete. Mean- while the several-layered intine has been formed by a secretion of cellulose. ‘he internal changes are precluded by the dissolution of the starch, the contents of the grain becoming transformed into the fovilla; at this time the outer and inner layers of the intine appear more pronounced, and the intermediate ones more or less hygroscopic. The periphery of the fovilla then becomes organized as a new primordial utricle, composed sometimes of a dense, shining, prismatic, pavement-like plasma (of a number of crystalloids, in fact), which is very well seen in Sequoia, Cryptomeria, and Cunninghamia ; but in other cases the prismatic structure is less pronounced, or is found only locally on the circumference of the uncrystallized plasma. MicroscoricAL ConTENTS oF FOREIGN JOURNALS. The Journal de l Anatomie, publié par MM. Robin et Pouchet. No. 2, 1877. Paris: Germer Baillicre.—The first paper in this number of the Journal is one of considerable length, on a subject known to most of us. It is on the Demodex folliculorum, and is by M. Megnin. It deals -very exhaustively with the subject, going into the minute anatomy of the different forms of Demodex, of which four distinct woodeuts are given. The plate which accompanies the paper gives the entire structure, the magnification used varying from 300 to 1200. diameters. In one case a hair-follicle of a dog is represented which displays the hair, and almost within the hair-sac are to be seen more than twenty Demodices. The author traces the complete development of the animal through three of its larval stages, from the condition in which it is footless to its regular eight-footed stage. He also describes the different species of Demodex, and deals at some length with their habits. The article is specially remarkable for the attack which it NOTES AND MEMORANDA. 263 makes on Mr. Erasmus Wilson, who wrote a paper on the subject of this arachnid, which is published in the ‘ Philosophical Transactions of the Royal Society ’ for 1842. It is pointed out that Mr. Wilson has fallen into the most terrible errors in his description of the animal. —A paper by M. Poincarré is also of interest to the histologist. It is upon the “ History of the Thyroid Body.” The author states that he has examined more than seventy glands, and these have been in all vertebrate animals, and he states that there is a general resem- blance of all to each other. But he remarks that while the presence of closed vesicular spaces is undoubtedly a characteristic feature in most thyroids, yet that man’s thyroid body is to some extent an excep- tion. He found that in human glands cysts were extremely common. Out of 106 specimens examined, no less than forty-three bore cysts within them.—Another paper, which is of some interest to the micro- scopic anatomist, is that upon “ The Origin of the Cranial Nerves,” by M. Duval. This is the conclusion of a series. The magnifying power employed is, of course, extremely low. Archiv fiir Mikroskopische Anatomie, herausgegeben von La Valette St. George und W. Waldeyer. 13 Band, 4 Heft. Bonn, 1877.— This number contains some very valuable and exquisitely illustrated papers. First in order is a long disquisition on the general structure of glands, by Dr. M. Nussbaum. This paper is illustrated by a plate containing many magnified representations of sub-maxillary and other salivary glands, of the glands of the pyloric end of the stomach, of the cesophageal glands, &c., &e. The most interesting paper in the entire number is that of Herr F. E. Schultze, on Spongicola fistularis. This is illustrated by three plates, in which we see the difficulty that the author must have had in referring the animal either to the Spongiade or to the Hydrozoa. It is exceedingly like the animals of both classes, and is really a connecting link of an extraordinary kind. We shall notice the rest of the contents in our next number. NOTES AND MEMORANDA. Angle of Aperture, Increase or Diminution of.—On this point there appears to be a considerable divergence of opinion at the present moment. We therefore publish a portion of a letter which has been addressed by Mr. Carl Reddots to the editor of the ‘ American _ Journal of Microscopy.’ He says :—* I find the following in the report of proceedings of the Dunkirk Microscopical Society, in this Journal for January 1877: «“¢ Professor Smith took a position radically opposed to many of the received ideas, and in favour of lenses of the widest angle of aperture for all kinds of work, even going so far as to express his * opinion that most of the work in histology and pathology done with the so-called ‘ working lenses’ of narrow angle, would require further 264 CORRESPONDENCE. attention, and with wide-angled objectives, which recent advances of the optician had put at our command,’ “This question about the comparative utility of lenses of wide or narrow angle is one of the greatest importance to all engaged in, or intending to engage in, any of the branches of the study of pathology, histology, or biology; to all who own lenses, or who are intending to own more... . Now, as is said in the report, there is a wide divergence of opinion among microscopists on this subject. While a few support Professor Smith, the great majority advocate and recommend the use only of small-angle lenses. . . . Dr. W. B. Carpenter has the credit of being one of the most influential advocates of the small angles. The writer of this is in possession of informa- tion that, within a few months, an objective of the highest possible air-angle was shown to Dr. Carpenter at his own house, and he asserted that he saw a certain histological subject better than ever before. Rev. Mr. Dallinger, of Liverpool, and his associate, Dr. Drysdale, have been for some years making the most important con- tribution to biology ever made. The writer has seen a letter from Mr. Dallinger that the flagella of a certain monad had been invisible to all objectives save two, both of the highest attainable angular air- aperture. Here we have one case of more and one of better. Will our American histologists contribute their facts ? ” Death of Professor Pancerii—We have to announce the death of this distinguished anatomist, which occurred quite recently. He was suddenly attacked whilst in the act of addressing his class at the University of Naples, and died in a few moments. It is supposed that the cause was disease of the heart. CORRESPONDENCE. Ture MicroscoricAL EXAMINATION OF Bioop STAINs. To the Editor of the ‘ Monthly Microscopical Journal.’ No. 1835, CurstNutT STREET, PHILADELPHIA, PENN., March 14, 1877. Dear Sir,—I fear you and your readers are almost as tired of the blood question as you are of the angle of aperture controversy ; yet I hope you will, in simple justice, allow me to make one remark, in reply to your severe editorial comment, in your February number, upon my views. Permit me to say, that you have been entirely misinformed respecting the claim I advance, which is not that we can distinguish human blood from that of the guinea-pig or dog, as photographed by Dr. Woodward, but only that in regard to stains containing cor- puscles within the range of human blood-dises (3359 to g¢op), and PROCEEDINGS OF SOCIETIES. 265 falsely alleged by a criminal to be those of some domestic animal slaughtered for food, we can aid the cause of justice, by testifying positively that the blood never came from an ox, pig, or sheep, the corpuscles of which, unfortunately for rogues, measure less than avo Of an inch in average diameter. In this respect I am so far from being “unquestionably wrong,” that I will undertake to prove my position, to the satisfaction of any honest inquirer of good stand- ing, who desires to test the question, by sending me unmarked fair specimens of blood-stains, under the conditions mentioned above.* Very respectfully yours, &ce., Jos. G. RicHARDSON, PROCEEDINGS OF SOCIETIES. Royat Mrioroscopican Society. Kina’s CoL.ece, April 4, 1877. H. C. Sorby, Esq., F.R.S., President, in the chair. The minutes of the preceding meeting were read and confirmed. A list of donations to the Society was read, and the thanks of the meeting were voted to the donors. The attention of the Fellows was particularly called to a donation of 150 slides of various objects, included in the list, presented by the Rev. R. H. Nisbett Browne, and a special vote of thanks to that gentleman was unanimously passed. The President announced that arrangements had been made to hold a scientific evening meeting on the 18th inst.; also that leave had been obtained to use the lecture theatre for the first Quekett lecture by Sir John Lubbock on May 2. That being an ordinary meeting day, there would be a little formal business to transact at the commencement of the proceedings, and when this had been done, the remainder of the evening would be occupied by Sir John Lubbock. At the end of the meeting the Quekett medal would be presented to the lecturer. Tickets of admission would be issued in due course, when every Fellow would receive one personal ticket, not transferable, and one transferable ticket for the admission of a friend. He had also been requested to intimate that a new list of Fellows of the Society was in course of preparation, and to ask that any alterations or cor- rections might be at once forwarded to the Assistant-Secretary, Mr. W. W. Reeves. Mr. Thomas Palmer read a paper “On the Variability of the * We do not doubt the accuracy of Dr. Richardson’s remarks in his new and qualified position. But so long as it is impossible to distinguish human blood from that of the dog, we think that the medical jurist cannot place much reliance on the microscope in his investigations. Still we think Dr, Richardson must be complimented upon the importance of bis researches. 266 PROCEEDINGS OF SOCIETIES. Chlorophyll Bands in the Spectrum.” The subject was illustrated by drawings, and the paper will be found printed at p. 225, The President, in proposing a vote of thanks to Mr. Palmer, said he was very glad to find that others beside himself had taken up the question of the spectra of the colouring matters of plants. The subject was one which he had worked at for some years, and it had proved so extensive that he felt he was only just beginning the in- quiry. These colouring matters are much more complex than is generally supposed, most of them are undoubtedly mixtures of two or three kinds of matters, and even the chlorophyll—the green colouring matter alone, is composed generally of two green matters, which exist separately in certain plants, and yet these facts had been overlooked by all observers excepting Professor Stokes and himself, and certainly they had been entirely ignored by all the Continental observers. The line it would be most important to carry out would be what were the chemical differences which gave rise to these changes in the spectra ? This was a line of inquiry which would necessarily take a very long time, and would involve an immense amount of work on the part of an observer. There was a great deal yet remaining to be done, and he was extremely pleased to find that the subject was being now taken up. The thanks of the meeting were unanimously voted to Mr. Palmer for his paper. Mr. Palmer said he had noticed a curious effect some time ago when examining a red solution of litmus; he found that when very bright light was obtained by using an angular prism as the reflector, instead of the spectrum going off quite black towards the violet end, he could see the line H, through the dark band. Mr. Hawkins Johnson inquired whether the absorption bands shown by a fluid under the spectroscope indicated any more than the difference in the colours of fluids, and whether the instrument was capable of distinguishing between colourless solutions, for example, between chloride of potassium and carbonate of soda ? The President said that though there might be in some cases dif- ferences observed between solutions which appeared to have scarcely any colour, the spectroscope was not competent to distinguish the difference in the chemical qualities of two such solutions as those named. He had, however, little doubt that there were many sub- stances which appear colourless, which would give definite spectra if our eyes enabled us to see farther into the red or the blue ends of the spectrum than they are able to do. The President said they had a paper that evening by the Abbé Rénard, which was of much interest in a geological point of view. The Abbé was present, but although he spoke English well, he felt he would rather not read the paper himself, though he was quite willing to address them in French. That course, however, being unusual, at his request Mr. Ingpen had kindly undertaken to read a résumé of the paper, the whole of which would be printed in the Journal. Mr. Ingpen then read a résumé of a paper by M. ’ Abbé Rénard, of Louvain, “ On the Mineralogical Constitution and Microscopical Characters of the Whetstones of Belgium.” land PROCEEDINGS OF SOCIETIES. 26/ A vote of thanks to the Abbé Rénard for his communication was carried by acclamation. The President said that the subject of the mineralogical consti- tution of these rocks was most important, and they were of much interest to English geologists, seeing that there were none at all like them to be found in this country. The occurrence of garnets in them, however, need not surprise, because they were frequently found in the slate rocks of our own lake districts, though perhaps not quite in so great a quantity. He thought that the slates of this character must be looked upon as thoroughly metamorphic, although they were not generally considered so; and therefore he regarded it as highly desirable to work out the subject in order to make out if possible what changes had taken place in the substances composing them. He might mention that the Abbé Rénard was the author of some of the very beautiful illustrations of the microscopical structure of rocks which were exhibited at the Loan Collection at South Kensington. A paper by Mr. H. J. Slack (who was unfortunately prevented by indisposition from being present at the meeting), “On Krupp’s Silica Cotton,” was taken as read, the President giving a summary of the general results, and explaining that it referred to the minute fibrous particles produced when a powerful blast was directed upon a quantity of melted glassy furnace-slag. Many of the little particles so pro- duced were like small shots, with one or more fine thread-like tails attached to them, and when the process was carried on in the open air, the whole place became filled with these minute particles, which were, from their hardness and sharpness, extremely detrimental to the lungs of persons who inhaled them. Mr. Slack’s paper had reference to the various shapes of the little spheres, and to the remarkable regularity which existed amongst them, as well as their curious markings. The President said that these spheres are of great interest in connection with the structure of meteorites, and might explain the formation of a number of round glassy particles which he had often found in those bodies. Nearly all the peculiarities of the artificial product may be referred to the tendency of a liquid to collect into spheres and of a viscuous glass to be drawn out into fibres. Mr. Slack’s paper was accompanied by some illustrative drawings; and a slide, in further illustration of the subject, was exhibited in the room. The thanks of the meeting were unanimously voted to Mr. Slack for his communication. The President said that they had received another paper to be read that evening ; 1t was from Mr. Clifton Ward, “ On the Lower Silurian Lavas of Eycott Hill, Cumberland.” The paper was rather too long to read in extenso at that late hour of the evening, but Mr. Stewart would read the introduction and the general conclusions. The whole paper would be printed in the Journal (at p. 239). Mr. Charles Stewart then read so much of the paper as explained the leading results. The President proposed a vote of thanks to Mr. Clifton Ward for his paper. The subject was one of considerable importance, because at one time it was thought that there was a great deal of difference between the composition of the ancient and modern lavas. This was 268 PROCEEDINGS OF SOCIETIES. due, in part, to the fact that these old lavas had undergone a great change since their first formation; in fact they were really meta- morphic in a very legitimate sense ‘of the term. Mr. Ward’s paper showed that originally they were in composition very much the same as some modern lavas. Mr. Ward had worked out the subject in a most admirable manner, and the results of his investigations would be found to be set out in his paper in a very complete and satisfactory way. He thought the Fellows might congratulate themselves in having such a subject, so ably treated, in the course of their transactions. A vote of thanks to Mr. Ward was then unanimously carried, and the meeting was adjourned to May 2. Donations to the Library and Cabinet since March 7, 1877: From Nature. “Weekly eis. °F 7 63° ce! eer 2 ea Athenzsums > Weekly :)i..)) sot) 2220 Os.> (aS. en cee Ditto. Society,of Arts Journal <;- 2; ) as lpetoy SeeeeOptips Archivos do Museu Nacional do Rio de ‘Janeiro... .. Le Directeur-Général, Reports of the Juries, Exhibition 1851 Be .. Frank Crisp, Esq. Micro-Chemistry of "Poisons. By Theo. G. Wormley, M.D. New York, 1867 a ; Ditto. One hundred and fifty slides (various) ... we) deo oe oe tops DRO eels eiemNesp ele Browne, M.A, Dayid Bogue, Esq., was elected a Fellow of the Society. Watter W. REEvEs, Assist.-Secretary. Scientific Evening of the Royal Microscopical Society. A scientific evening was held at King’s College on Wednesday, April 18, of which a detailed account, too late for the present number, will be given in the next one. We may mention that the upper set of rooms of this Institution were thrown open, and were filled by members who exhibited a vast variety of objects—many of them living —and apparatus of novelty. Tea and coffee were served in an ad- joining apartment, and altogether the meeting was a most pleasant and successful one. THE MONTHLY MICROSCOPICAL JOURNAL, JUNE 1, 1877. I.—On the Mineralogical Composition and the Microscopical Structure of the Belgian Whetstones. By Rev. A. Rénarp, 8.J., F.R.MLS. (Read before the Royau Microscopicau Soctety, April 4, 1877.) Amone the rocks used as fine whetstones, there are none, I think, more justly celebrated in Europe than those found in the neigh- bourhood of Viel-Salm, in the province of Liege, Belgium. They are in shape parallelopipeds, composed of a stratum more or less deeply coloured yellow, and of a stratum coloured blue-violet ; and are exported to every country in Europe and the Orient. Although I intend to direct attention chiefly to their constitu- tion as found from their study under the microscope, and to the light which this method of study throws upon the origin of those rocks and upon their physico-chemical constitution, yet I shall briefly notice some of the interesting geological considerations relative to their bearing and to their relations with the adjacent strata. The hones of the neighbourhood of Viel-Salm are found among the rocks which Dumont called Salmien, but which seem to resemble very much the English Cambrian, and to be the equivalent of the schist of Tremadoc. They form veins in the Cambrian slate of from one to two centimeters thick, but whose direction is so irregular, and whose composing strata are so winding and tortuous, that many geologists have mistaken them, and they have been not seldom described as real veins; whilst I have shown, supported, moreover, by Baur and Dumont, that they are regularly intercalated in the stratification, and form real strata in the slate, with which it is intimately united. The facts upon which I base my deductions and the macro- scopical descriptions, are given at length in a memoir which I devoted to this question. Before touching upon the microscopical study, let me say a word or two on the relations between the whetstone and slate, as by that means I may be more readily understood in the description of the whetstone as it appears under the microscope. When one sees a hone haying one layer of a yellowish white VOL. XVII. % 270 Transactions of the Royal Microscopical Society. material, and another of bluish slate distinctly separated by a straight line, sometimes of perfect regularity, there is a tendency to suppose that they are two fragments of different rocks fastened together one above the other, the juxtaposition being due rather to art than to nature; but when these stones are seen in the place which they occupy in the strata, one readily observes that the vein of whetstone is intimately united to the slate, and that the work- man has nothing else to do than to square the fragments. In certain exceptional cases, however, art is made to imitate nature ; and the workman sometimes, by fastening together fragments of different colours, gives to the market a hone that differs not in appearance from those formed by nature. Although this line of demarcation is usually found very distinct between the two layers and marking the direction of stratification, it also happens frequently that the whetstone passes imperceptibly into the slate, in such a way that at a certain point it is no longer possible to distinguish whether slate or whetstone is in question. It might be said there was a sort of mutual penetration of the two layers. : There is one character, common to the veins and the incasing layers, to which special attention should be given. It is this: the foliation, oblique to the stratification, is prolonged from the slate into the whetstone. Sometimes this foliation is but faintly charac- terized in the compact varieties, but it is always present in a latent state, and if the slate be broken, the lamina comes off, passing across the whetstone, and the fissure is prolonged with a regularity and constancy of angle which shows evidently that the two rocks have a common cleavage. I have proved that there is also present in these two rocks a second cleavage, not so easy, but, like the first, clearly distinct from the stratification. The existence of this cleavage shows, first, that the layers of whetstone existed before the uplifting of the strata; and the coexistence of the two cleavages obliges us to admit that the rocks of this group have been subjected on two different occasions to a pressure, brought to bear in two different directions, as contended in similar cases by Mr. Sorby. The easier cleavage must have been produced while the rocks were still in the plastic state, the second when they were already more solidified. I have dwelt upon the characters common to the two rocks, because they are in close relationship with the details of microscopical analysis which follow. To sum up, the whetstones are contemporary layers with the incasing slates, and have been subjected to the same mechanical actions as all of the phylladic rocks of this group. After this exposition, belonging rather to geology, let us inquire what are the minerals that constitute the whetstone of the neigh- bourhood of Salm. It should be remarked that this question cannot a On the Belgian Whetstones. By Rev. A. Rénard. 271 be answered by macroscopical examination alone, since the compact- ness of the rock and the fineness of its grain is such that, even with the aid of the magnifying glass, it is impossible to individualize the mineral species which make up the whetstone. It appears in general as a homogeneous substance of clear colour, and the geolo- gists who have occupied themselves with this rock have limited themselves to giving the description of some of its physical pro- perties and the details relative to its bearing, touching only inci- dentally on its composition. This, however, is not surprising when it is remembered that these skilful observers had not at their disposal microscopical analysis, which I have been able to use. Still, on examining with attention the lamine or the fractures, peculiarities may be seen at their surface which give a glimpse of the elements that microscopical analysis makes known. With the naked eye phylladic plates, closely aggregated, may be perceived. This phyllite has not the silvery or pearly aspect of sericite ; neither has its pyrognostic characters. It is these lamella which make up the fundamental mass of the rock. By the reflexion of a strong light there may be seen on these phylladic membranes a glistening due to crystalline granules of infinitesimal dimensions. These shining grains would naturally be attributed to quartz, were it not that study at the microscope discovers in them optical properties and crystalline forms which put aside this supposition. The micro- scopical dimensions of the elements mingled with the phyllite never determine the structure which we have called by the name of gneissic in our study of the rocks of the French Ardennes; at least, it does not appear to the naked eye nor under the magni- fying glass. Among the accidental elements visible to the naked eye should be counted iron glance, hydroxid of manganese, which often impregnates whetstone, quartz, and pyrophyllite. Let us pass now to the study of the ultimate constitution of the whetstone, as shown by microscopical analysis. In order to come at the results given in this paper, I have cut and polished more than seventy thin sections of this rock. ‘To have a general idea of the ultimate structure of the whetstone, we should study it first with the help of weak magnifying powers. There is then perceived a colourless micaceous substance which seems to make up in great measure the fundamental mass. These phylladie fibres, generally elongated and colourless, appear peppered with a black dotting, owing to a numberless quantity of granules which have the appearance of opaque points. There are seen also in- numerable microliths, some like simple dashes, and others of larger dimensions, but much more rare, showing a light bluish tint. Finally, with the help of a polarizing apparatus, it may be seen that one part of the mass belongs to an isotropic substance. Commonly the phyllite is completely covered by the prodigious x 2 272 Transactions of the Royal Microscopical Society. number of particles, more or less circular, scattered along the surface of the filaments. The elongated microliths are in line, and grouped with their greater axis parallel to the direction of the micaceous lamine. Clearer regions are also remarked in this mass, almost without interpositions, the arrangement of which contrasts with the general disposition of the elements. These veins, having a thickness of less than a millimeter, advance irregularly across the rock. They are made up chiefly of micaceous substance, and do not seem to be fissures filled up later on, but rather to have been formed at the same time that the rock took its distinctive petrographic character. They are found to contain, though in small proportions, all the elements which we discover as constituent parts of the whetstone. A fissure, filled later on, would not be filled with all the substances identical with those which form the rock. This kind of micro- scopical primary veins does not cross the whole of the thin section. They often form lenticular regions in it, of the same structure and composition as the little veins of which we have just spoken. None of the microscopical characters by themselves allow of a cer- tain identification of the lamelle with a determined phyllite. I give up, however, the opinion of Dumont, who considered, without sufli- cient proof, pyrophyllite to be the constituent principle of the phyllas of the Ardennes ; and I would bring these phyllitous fibres into con- nection with Damourite, a mineral which the chemical analyses of Messrs. Davreux and de Koninck, jun., have shown to exist in a garnet-bearing rock of Salm, that presents, as will be seen, many analogies with the whetstone. Still it is very difficult to decide this point with certainty, since it is impossible to isolate the lamellae for a separate analysis, and they are dotted with foreign minerals. On the other hand, the optical reactions are unsatis- factory ; for, as is known, one of the problems the most difficult of solution in the microscopical analysis of rocks is the specific deter- mination of the different micas, especially when they are found without distinguishable crystalline forms, and with extremely small filaments, as is here the case. Let us now pass to a more minute study of the different elements contained in that rock. For this we must use a magnifying power of from 400 to 600 diameters. With such aid we may perceive the innumerable granules, scattered over the surface of the lamine, become clearly and distinctly individualized, and the rock, at certain points, appears to be composed of globular forms whose agglomera- tion almost completely veils the micaceous element. The mean dimensions of these circular forms rarely exceed 0°02 mm. ; and, according to an approximative calculation, some parts are so beset with them, that a millimeter cube of rock contains over 100,000. These globules, for the most part rounded, sometimes also elongated, are, in some cases, terminated by crystallographic forms. They Se — On the Belgian Whetstones. By Rev. A. Rénard. 273 may be perceived to be bounded by regular lines, and one may dis- cover their lozenge-shaped faces, which are to be referred to the rhombo= dodecahedron. The dimensions of these crystals are ordi- narily so minute that they are not attacked in the polishing process, and thus they are preserved to us in the integrity of their form. They are therefore, in general, complete on all sides. It is difficult to judge of their optical properties, as they are set in a double refractive substance ; but by observing those of larger size that protrude on both sides of the micaceous lamin, or those isolated at the extremities of the thin sections where the thickness is least, they may be seen to be dark between the Nicols’ crossed risms. i Their perfect isotropism and their crystalline form place them amongst the minerals of the first crystallographic system. Seen by transmitted light they appear completely devoid of colour, bordered by zones of deep black, which diminish in intensity toward the centre of the crystal, where the colourless part sparkles with ex- ceeding briliancy. I have found these crystals in great numbers in all the various kinds of whetstones of the Salm formation. At one time they are gathered together at one point, at another they form lines or chaplets, and again they are isolated. With this ensemble of characteristics one may ask to what mineral species we are to refer these globular-formed crystals. However strange the conclusion may appear, I refer them to the garnet. In support of this I may show that the interpretation making it a garnetiferous rock is in no way opposed to any of the details of the micrographic description I have given, that it explains naturally all the facts that I have mentioned as well as the physical properties of the whetstone of Salm. The rhombo = dodecahedral forms, or globular crystals, which, however, now and then present a rhombic face, point out a mineral of the first system. The single refraction on which I before insisted now comes to support my interpretation. The high index of refraction of the garnet (4 = 1°772) shows itself by the unusual brilliancy displayed by the crystals when observed by trans- parency. * The high specific gravity of the rock (= 3°223) is also explained by the density of the garnet, which forms a great part of it. The specific gravity of garnet, as is known, reaches to 3°4 and even 4°3. Hitherto it has been frequently asked what the sub- stance could be that enabled these whetstones to wear even steel, and it was the supposition up to the present time that the element * To explain this fact, it is to be remembered that luminous rays penetrating a refracting body by a point, and forming at the point of incidence a hemispheric pencil, form in refraction a cone whose angle at summit is given by the equation sin. 7 =—- This angle diminishes in proportion as n increases. n 274 Transactions of the Royal Microscopical Society. was no other than quartz finely divided and dispersed through the stone. My researches prove, however, that they contain scarcely any quartz. Hence it is to the garnets that we are to attribute this hardness of the rock, for we know that the specific hardness of garnets is comprised between 6°5 and 7°5 of the scale of Mohs. The discovery of garnets in the slates of Recht by my friend Dr. Zirkel, Professor at the University of Leipsic, is another support of this interpretation, as the slates of Recht belong to the same formation as the rocks of Salm, of which they are the con- tinuation in Germany. The largest garnets of our preparations show inclusions which are found so often in this mineral when studied under the micro- scope; we observe also in the largest those irregular fissures which are so characteristic of garnet. But how is the yellow colour of the whetstone explained if we admit that this rock is, as we have said, almost exclusively com- posed of garnet? In our endeavours to explain this colouring, we have succeeded in determining the sort of garnet to which this mineral belongs. We place it in the variety called Spessartine, and we shall soon see that another kind of proof confirms us in this classification. In considering spessartine as the principal element of the whetstone, we see that the union of a very great number of infinitely small crystals of this mineral should produce, when regarded ‘ ensemble,” a yellowish-white tint; for the purest spessartine is in little transparent crystals of a pale yellow, im the island of Elba, at St. Marcel, in the diamond sands of Brazil, and in Maine in the United States. We thus easily understand, in admitting that spessartine is present here, how an agglo- meration of small garnets of this variety can produce the yellow tint of the whetstone. But what indicates still more certainly the manganese garnet is chemical analysis. M. von-der-Mark has found as much as 21-71 per cent. of MnO, and M. Pufal has found 17°54 per cent. in a specimen he has had the kindness to analyze for us. This large quantity of manganese should not cause sur- prise, since it is known that the spessartine of Haddam, in Connec- ticut, analyzed by Rammelsberg, gave 33 per cent. of MnO. Let us also bear in mind that the presence of manganese manifests itself in a remarkable manner when tested by a bead of borax. Let us also remark that all the surrounding rocks are as it were impregnated with manganese; it is found in the form of veins, or combined in the remarkable metamorphic minerals (ottrelite, de- walquite, &c.) of that region. And it is near veins of whetstone that MM. de Koninck and Davreux discovered the beautiful little garnet crystals of which they have given the description,* and whose composition approaches * *Bulletins de PAcadémie Royale de Belgique, 1873. On the Belgian Whetstones. By Rev. A. Rénard. 275 more nearly that of the typical variety of spessartine than that of any specimen of which an analysis has been published up to the present. I may add, that some specimens of whetstone have lost their colour through an impregnation of hydroxid of manganese. These became completely black, but in thin sections there imme- diately appeared all the essential elements of the rock, coloured, however, a faint brown by the foreign matter. A third element of the whetstone of Salm is schorl. This mineral is far less widely spread than the two which I have just made known. ‘The principal microscopic characters which this mineral offers in the rock are the following: the form of the sections is that of a parallelogram whose great axis may have on an average from 0:07 mm.to 0'08mm. In width it reaches 0°01 mm. Ordinarily the sections of the mineral are terminated at one extre- mity by planes intersecting each other at an angle more or less open; the opposite side being terminated by an almost straight line. They are traversed by crevices which are sensibly parallel to the base, and often appear notched. Their tint is not homogeneous ; it is pale green, blue, greyish, sometimes growing stronger at one extremity of the section. ‘This mineral is birefringent, and is strongly dicroscopic. The sections are often filled with black and opaque little spots. It is known, moreover, that M. Angor has discovered this mineral in a great number of slates and schists. We find again in our thin section a most perfect resemblance between the mineral he considers to be schorl and those which we have been led to consider as the same. The forms of that mineral, we have said, show a difference of development for the two extremities: this difference is the very same as that which affects schorl; which presents us so frequently with the most classic examples of enantiomorphism. We have said that certain sections show two different tints at the two extremities; this difference of tint is a well-known fact in the case of this mineral. Indeed, we know that the transparency of the tourmaline varies in the same crystal with the direction relative to the axis of the rhombohedron. It is more sensible in a perpendicular, and feebler in a parallel section, a fact which must be referred to its dicroscopism. But besides this phenomenon it is not uncommon to find that the same crystal presents different colours at the two extremities, or at least a tint of unequal intensity. According to M. von Lasaulx, the same thing is noticeable in the microscopic tourmalines enclosed in the garnets of the granulites of Saxony. We have just said that these crystals of schorl sometimes appeared as if broken; that they had undergone certain deformations. We remark, indeed, that these small sections of schorl appear broken, and that their various fragments lie at a short distance. M. Rosen- busch observes that those which are seen by the microscope are 276 Transactions of the Royal Microscopical Society. ordinarily curved, a fact we have remarked ourselves. As we have said, it is not rare to find the sections of schorl furrowed by fissures more or less parallel to the base. It was believed by some micro- scopists that this fissure represented a cleavage. Now, the best mineralogical works make no mention of a cleavage in this direction. Dana, Naumanm, and Des Cloizeaux mention cleavages only follow- ing R, o P2; besides this, these cleavages are not easy. We are therefore inclined to admit that these ruptures are the effect of mechanical action, as, for example, the stretching of the beds at the moment of foliation. The rupture in these little prisms must neces- sarily be made parallel to the base, where the points of more feeble resistance are found. I add that M. Zirkel and myself have been able to prove that these prisms belong to the hexagonal system. Tn a research that I made with him, we have found that in a thin section of a schist of the Ardennes a hexagonal section of this dicroscopic mineral was dark between the crossed Nicols’ prisms. This fact wholly confirms our interpretation as to the crystalline system of these little prisms. In the few pages devoted by M. Zirkel to a microscopic de- scription of the slates of Recht, he pointed out the presence of a prismatic mineral of a greenish yellow colour. High powers of the microscope are needed to observe this mineral, the prisms not being more than 0°03 mm. in length and 0°005 mm. in thickness, so that it is difficult to determine all the faces of the crystals, which, though complete, have not very well defined edges. Irregular aggregations are often found composed, sometimes of one or two individuals, sometimes of twins in the form of a knee. As none of the characteristics of these small crystals are opposed to those of augite,* M. Zirkel believed that he could class it with that mineral. Such are, in brief, the micrographic details he gives upon these microliths. We find them again in great abundance in the whetstone, and there under a great variety of very interesting crystalline forms, which have not as yet been pointed out by any micrographer. These prisms, which are identical with those remarked by M. Zirkel, are scattered through the whetstone sporadically, and are dis- tinguished from the prisms of schorl by their form, by the way they are grouped, by their tint, and also by their exiguity. At different times these prisms are ranged in lines, verge towards each other, and interlace, maintaining the while almost constant angles in their superposition. In some sections it is remarked that the prisms follow the undulations of the micaceous substance. We shall add nothing to the excellent description which M. Zirkel has * On this subject M. Zirkel remarks that our friend C. A. Lossen, of Berlin, has found in inferior Devonian, near Winterburg, some crystalline schists in which the macroscopic augite appears as an essential element. On the Belgian Whetstones. By Rev. A. Rénard. 277 given of the simple crystals of this kind. We find, however, in our sections, remarkable examples of grouping and of twins, of which we shall speak more in detail. When there is a certain quantity of these microliths gathered together, one is sure to remark, for some among them, a certain manner of adhesion or of superposition, which is too regular and constant in its repetition not to be subject to some crystallographic law (Fig. a). Wy ha Among these little crystals those of simpler form show the geniculated twins with an angle of about 60°, and in general it is with this angle that the crossings or superpositions of the minute prisms take “place. Oftentimes it isa granule of spessartine that serves asa point of attachment. The prisms do not preserve the same thickness through their entire length. In the upper part, for example, they appear a simple line, and toward the middle they suddenly bulge or swell out. Finally, im many cases they give rise, by their ramified disposition, to forms that may be considered as the skeletons of crystals that I have discovered in the whetstone of Sart, and of which I am now about to speak. In the thin sections of this whetstone there are to be observed triangular compound crystals, yellow, less transparent, and whose dimensions reach even to 0-05 mm. (Fig. b). These groups may be reduced to a single fundamental type, namely, a heart-shaped twin haying an angle of 60° at the summit. These crystals are formed of minute prisms that adhere to one another very perfectly, of which I have spoken above. ‘These sections are covered with parallel striz on both sides of the triangles, producing very dis- 278 Transactions of the Royal Microscopical Society. tinctly those striae which erystallographers generally call osec/- latory. it is not the microliths of Sart, however, that show the most remarkable crystalline forms. Some specimens of the whetstone of Ottrez exhibit, with a microscope of 600 or 700 diameters magni- fying power, a multitude of minute triangular crystals of the utmost delicacy and perfection (Fig. ¢). It has been shown that these little geometric solids are to be classed, on account of their angular measure and their form, with the geometrically disposed microliths of Sart and with the geniculated twins. But, on the other hand, inasmuch as the fundamental character seems to point them out as belonging to those regular aggregations, even in so much do they differ from them by their perfect transparency. They are not formed by the gathering together of a number of minute prisms, as is the case in the specimens from Sart, and are perfectly colourless. ‘They are exceedingly small, the base often not measuring more than the thousandth of a millimeter. That some idea may be had of their delicacy, it may suffice to state that it is not rare to find two or three of them superposed. If the observer turn the micro- metric screw he can readily convince himself that they occupy different planes even in the extremely minute thickness of the thin sections. Thanks to the delicacy and the perfection of their forms, one may attempt, with some chance of success, to determine the crystalline type in which the mineral is to be classed. The minuteness, however, of its dimensions, and the impossibility of isolating it, impose the necessity of pronouncing with great reserve ‘on the mineralogical nature of these remarkable microscopic twins to which I now for the first time call attention. By the inspection of the outline and of the extremely delicate line that joins the summit with the obtuse angle opposed the ob- server may readily recognize hemitropical forms; and the two halves polarizing with complementary colours prove in their turn that these two parts have their optical axes placed as they should be in the case of a hemitropy similar to that which we find in the ereater number of these twins. This mineral constitutes, in the great majority of cases, twins by juxtaposition ; however, some are found which are twins by pene- tration ; those, for example, which cling together by their summits, recalling what one sees in certain twins of tridymite, mentioned by Vom Rath. The angles of these rhomboids, to judge them by approximate valuations, such as can be made by the microscope, are of 60°, 90°, and 120°. In other terms, these are the angles given by the hemitropies of the crystals of the rhombic system which have an edge of about 120°, and for which the hemitropy is made following the rule = Plane of hemitropy = a face of the prism of about 120°, that is to say, a dome, 3 P oo for example, the principal axis of the two individuals forming together an angle of about 60°. On the Belgian Whetstones. By Rev. A. Rénard. 279 This interpretation explains the heart, or geniculated, twins which are presented to us in the little prisms contained in almost every thin section of the whetstone, and of the regular groupings of the rocks of Sart. In spite of all the details resulting from a minute study of these remarkable crystals, we must, however, confess that they are not sufficient to determine to what species of mineral they belong. We are here before one of the most difficult problems of petro- graphy, that of identifying with a macroscopic species, crystals of such small dimensions as those which we have discovered, and which besides show characteristics which seem to bring them near to known minerals. Yet there is nothing to prove that these microliths are not a new species. The abundance of material that we have at hand, and the extraordinary development of these forms in certain specimens that we have endeavoured to analyze with a scrupulous care, authorize us to think that they ought not to be referred to augite ; in truth, epidote offers points of resemblance for the colour and the twin; for we know that Kokscharow has found hemitropies of epidote resembling these we have here ; but the other characteristics of epidote are too different to permit us to ascribe to it these little twinned prisms. In order to dissipate the doubts raised on this point, I have examined the analogous forms given us by the mineralogists for the minerals of the class of silicates, and I have been struck with the resemblance between the twins of chrysoberyl and our little twin crystals. What, besides, adds a certain value to this con- sideration is, that chrysoberyl is found in crystalline schist, as, for example, at Tarakoja in the Ural Mountains, and Marschen in Moravia. Stratigraphical and petrographical studies, moreover, lead us in like manner to consider the whetstone that we are describing as belonging to the series that we designate as crystal- line schists. In terminating this micrographical part of the article relative to the whetstone, let me remark that the oligiste iron appears but rarely, and even then sporadically, in this rock, and that it appears more generally, and especially, in contact with oligistiferous slate, whose relations with the rock we have just described we will now briefly study. At the commencement of this paper I drew attention to the fact that the whetstone appears almost constantly associated with the oligistiferous phyllade, in which it forms regularly intercalated strata. We have seen that these two rocks are perfectly adherent, as also that the foliation of the one is common to the other; now it remains to inquire whether their mineralogical composition and micro-structure cannot throw some light on the relations that exist between them. Let us see therefore what data the microscopical analysis gives 280 Transactions of the Royal Microscopical Society. us for the oligistiferous phyllades. Here we have as guide M. Zirkel, who examined some thin sections of the phyllade of Recht, which is definitively the same as that associated with the Belgian whetstones. My observations on the oligistiferous phyllade of Ottrez, Bihain, Viel-Salm, &c., agree in every point with those of M. Zirkel. . M. Zirkel finds that the red grains scattered throughout this rock are in fact, as Dumont had admitted, oligiste iron; that under the microscope they appear of a red colour, and the sections, though generally irregular, are, however, sometimes hexagonal. M. Zirkel attributes the red colour of the phyllade to the accumulation of lamellz of this mineral. These lamella, as well as the other con- stituents of this rock, are enclosed in a micaceous substance, which constitutes the fundamental mass of the schist. The third con- stituent recognized by M. Zirkel is garnet, which appears in his preparations with the same characteristic marks that we have already seen in the whetstone. We would remark, however, that this mineral is far more abundant in this rock than in the slate. He makes mention besides of prismatic microscopical crystals, some of which are geniculated twins, and a fifth mmeral composed of granules generally flattened, black and opaque, irregularly termi- nated, and which are less than 0°'015 mm. He is inelined to regard them as carbonaceous particles so often found in black or blue schist. . We have but little to add to this excellent description of oligis- tiferous slate; the only additional element that we have yet recog- nized in plates of this rock is schorl, whose sections appear here like the sections of this mineral which we have examined in describing the whetstone of Salm. If now we compare the results which M. Zirkel has obtained for the composition of the oligistiferous slate and those which we have noted in this communication, we shall remark striking analogies in these two rocks, which we were far from suspecting, but which per- fectly explain the phenomena presented by their microscopic study. In both cases a micaceous substance constitutes the fundamental mass; there is the same structure, both contain garnet and small prisms quite identical, and in both schorl is present. The difference consists only in the fact that the slate contains lamelle of oligiste iron and carbonaceous granules, while these two minerals are rare in the whetstone. There yet remains an important geological question to be dis- cussed: it has reference to the origin itself of the rocks. Let it suffice to renrark that I have not met there any elements with traces of clasticity. On the contrary, everything seems to show that its essential elements are crystalline, formed cn situ. Resting on the ensemble of facts which I have observed, stratigraphic as On the Belgian Whetstones. By Rev. A. Rénard. 281 well as petrographic, I am inclined to admit that the bands or zones of the whetstone are real layers imbedded in the Cambrian formation of the province of Liege, and that they were deposited in the same way as the adjoining slates, in the Cambrian sea, with the proper characteristics that make them differ, from the very moment of their deposition, from the sediments that furnish phyllades. Without denying that a metamorphic action has affected this mass, in a general way, I am inclined to think that this phenomenon alone has not been able to effect the concentration of the mineralo- gical elements that constitute the whetstone. In conclusion, I add that this rare rock of Salm and the neigh- bourhood presents a mineralogical composition such as I have never found in any of the rocks ordinarily designated as razor-stones. I may be permitted here to thank MM. Richter and Dana for the information and specimens of whetstones they have forwarded to me. ( 282 ) II.—Observations on the Structure of the Red Blood-corpuseles of a young Trout. By W. H. Hammonp, Esq. THe circulation of the blood in a young trout may be so plainly viewed under the microscope, owing to the great transparency of the fish, that it occurred to me it would be a very good subject for experimenting on to ascertain if the red blood-corpuscles contain a nucleus in their living state as they flow in the vessels. By get- ting the little fish in a suitable position, as it swam in a cell full of water, I was able to use an objective giving an amplification of over 300 diameters; with this power I could see the corpuscles where they flow, slowly and singly, very distinctly in the smallest veins. When the red corpuscles presented their broad surfaces, they had the appearance represented in Fig. 1, a central spot or nucleus, and a rim round the margin. I also had good side views of the corpuscles in the small veins, just at the point where they branch out of the larger ones; here the corpuscles were continu- ally turning over, and at times one remained stationary for a little while ; when the edge was exactly opposite to me, they had the appearance shown in Fig. 2, the central spot or nucleus clearly projecting on both sides of the blood-disk. I could also see, as the corpuscles rolled over, that their outer part is a cylindrical ring; a section of one would have the appearance shown in Fig. 3. These observations were repeated many times on young trout varying from a day to three weeks old. Fiaq. 1. Fig. 2. Fig. 3. The question is\ important, for Professor Gulliver, F.R.S., in his paper entitled “Observations on the Sizes and Shapes of the Ked Corpuscles of the Blood of Vertebrates,” * says, “In every animal, without any known exception, of this great divi- sion (Pyrenemata), the red blood-corpuscle is characterized by the presence of a nucleus, which is plainly demonstrable in the majority of the corpuscles when examined on the object-plate under the microscope. Nor is the taxonomic value of this fact at all * «Proc. Zool. Soc., June 15, 1875. S < Poe Le), a ALDorsucdir ad nee bet Heterotrichus inzequarmetus, Donn. A New Acarite. By M. A. L. Donnadieu, DSc. 283 affected by the old and still vexed question, as to whether the nucleus exists distinctly or at all in the corpuscle while it circu- lates within the living blood-vessels, or is formed only after its exposure to the atmosphere or chemical reagents. Many years ago De Blainville, Valentin, Henle, and others, and more recently Savory, supported the latter view; and the former was adopted by Mayer and Kolliker, to which Brunke has lately conformed. The subject cannot be entertained here ; only it may be noted that I have satisfied myself of the substantial accuracy of Mr. Savory’s observations on the blood-disks of some British Batrachians, but not of the validity of his conclusions therefrom, and that I have plainly seen in certain fishes the projections on the corpuscles, indicative of a nucleus, while they were flowing within the living blood-vessels.” The facts, described above, were shown in the living fish at a late scientific meeting, at Canterbury, of the East Kent Natural History Society, and were regarded with much interest by the members present. IIL—A New Acarite. By M. A. L. Donnaninv, D.Sce., Professor at the Lyceum of Lyons. Puate CLXXXIILI. In the month of April, 1873, in emptying into a plate full of weak acetic acid * the contents of a collection from a sweeping net, I found an acarite which appeared to me to be quite new. It is diffi- cult for me to give any exact idea as to its origm. The glass was full of acarites of all kinds, Scirus, Trombidium, Gamasus, &e., and with them a great many insects, among which the Diptera were most numerous, more especially those allied to the common fly. With regard to the specimen which I found, which, in spite of EXPLANATION OF PLATE CLXXXIII. Fic. 1.—AHeterotrichus inequarmatus. Entire animal seen from behind. The left half is represented without the numerous hairs which cover the body, in order to show the tubercles which support these hairs. Fic. 2.—A tubercle very much enlarged, and showing the two kinds of hairs. a. Long and pointed hairs divided into segments. 6. Short hairs with the peculiar spherical swelling. Fic. 3.—Extremity of one of the feet. a. Tarsus. 6. Edge of the cupuliform membrane deprived of hooklets. c. Two large internal hooklets. d. Nine small spatuliform hooklets. jf. The three large external hooklets. g. hairs, Fic. 4.—Acarite magnified twice. * See, for an explanation of this process of research, ‘ Recherches sur les Tétramiques,’ par A. L, Donnadieu, 1875, p. 27. VOL. XVII. Y 284 A New Acarite. By M. A. L. Donnadieu, D.Se. all my search for others, was but that of a single individual, I believe that it is an undeveloped form (hypopiale) of Gamasus, which might very well have proceeded from one of the Diptera which I shall refer to. ‘The mouth, too badly defined to have any significant value, the general form of the body, and, above all, the absence of reproductive organs, seem to me to confirm this idea. I would observe that my description refers to the actual form of the individual, without in the slightest degree indicating what the ultimate appearances may be. I have called it Heterotrichus inequarmatus, which name can be applied to the complete form when I am fortunate enough to obtain it. The body, which is very transparent, is ovate; the rostrum makes a very slight bend forwards, through which one distinguishes only that which should be the palpx. The inferior surface is, flattened, the upper one is swelled out (bombée). ‘The skin on the entire region of the body is granular, and presents grooves in the neighbourhood of the feet and rostrum. On the dorsal face one sees a series of rounded elevations like little tubercles. At their level the skin is slightly brownish ; they serve to support the hairs which by their nature justify the generic name that I have given the animal. These hairs are, in fact, of two kinds. The one spiny at their ends seem formed of a series of joints, which fit one into the other. They are twice to three times the length of the body. They are comparatively slender, but are nevertheless rigid enough to give the animal the appearance of a body covered with sharp spines. ‘The others are short, and terminate in a slender point; almost in the middle they present a very large vesicular swelling filled with a mucous-like fimd, which by its transparence contrasts vividly with the brownish tint which fills the rest of the hair. The disposition and number of each of these hair-like processes on their little elevations of the surface are unimportant; but these latter are so abundant that the whole body disappears beneath the mass of hairs which cover it. The feet, eight in number, are short and decidedly conoid. They differ very slightly in length, the anterior pair being slightly shorter than the others. ‘Two pairs are directed in front, and two Betas At the point of origin they sensibly approach each other. Their mode of termination is the most remarkable point about them. The conical tarsus is terminated by a wide membrane capable of forming a cupuliform caruncula, on the lower border of which are placed hooklets. The latter are of two forms, and their appearance led me to give the specific qualification to the animal of imequarmatus. The first are freely bent, as is the case in the majority of the species. They thin away from base to extremity, The Action of Chlorophyll in the Vine. By Giovanni Briosi. 285 and their curvature forms a more or less marked semicircle. Two are directed to the front and the external border (le bond externe). Three others are seen in the outer border, but they are directed backwards. Between these two series are placed the hooklets of the second form (les crochets de la deuaieme forme). The latter are placed regularly upon the inferior borders of the tarsal ex- tremity, and are nine in number. They are short, and their initial part assumes up to the point of its insertion a more or less spatular form. Towards their summit they curve brusquely upwards, and terminate in a very short conical point. They are all equal in their length, which does not exceed a third of the preceding ones. Finally, the feet are covered with hairs analogous to the long ones on the body, but much shorter and more transparent. By all the characters that I have pointed out, this acarite appears to belong to the Gamasidx, to which certainly belong the adult forms represented in the present state of our knowledge by the undeveloped stage of certain Gadflies—Journal de l Anatomie, December 1876. 1V.—On the Action of Chlorophyll in the Vine. By Giovanni Briost, Engineer and Director of the Agricultural Station in Palermo.* One of the grandest conquests in the realm of modern botanical physiology, since it concerns the most fundamental phenomenon of life, is, without doubt, the discovery of the assimilating function of chlorophyll by which it forms starch out of the carbonic acid of the atmosphere and water, under the action of the light. As is known, it was the work of Mohl, Gris, Bohm, Sachs, Nageli, Kramer, Kraus, &¢., which led to this discovery, which has often since been confirmed. Consequently it is at present generally admitted that the starch is, at least amongst the vegetable sub- stances which are known to us, the primary form of the organic material of plants, out of which the laboratory of nature derives by transformations partly understood, and partly unknown to the chemist, all other physiological allied substances, as sugar, dextrine, inulin, cellulose, fat, &e. In another work,j I have pointed out that the product of the assimilation process of chlorophyll in some plants cannot be starch, * Translated from the Italian by W. R. + Briosi, “ Ueber normale Bildung von fettartiger substanz im Chlorophyll” (‘ Botanische Zeitung,’ 1873, No. 20 and following ones); also ‘ Nuovo Giornale Botanico,’ April 1875. eta 286 The Action of Chlorophyll in the Vine. By Giovanni Briosi. and demonstrated in fact that in the chlorophyll of the Strelitziz and Musce, instead of starch, oil or fat is constantly formed, and that in these plants afterwards, out of those substances, the cellulose, and the starch itself (which, too, is found in some of their organs), &c., originate. And these Musacex and the Allium cepa, in whose chlorophyll- grains Sachs could never detect starch, and where it is suspected that glucose is formed, are the only plants in which (to my know- ledge at least) it is certain that no hydrocarbon is formed. Since 1872, whilst studying what substances are formed in the vine, and what transformations they undergo, I often had occasion to observe, that in the chlorophyll-grains of this plant no starch is found, but the knowledge that this well-known and important plant had already formed the subject of the researches of the most dis- tinguished scientific men deterred me from prosecuting my labours; and since then I had no opportunity of taking them up again, as during the last few years [ have almost been taken away entirely from my studies. Having been called upon towards the end of last autumn, by His Excellency the Minister of Agriculture, to oceupy myself with a new disease of which we were warned in some vineyards at Favara (which disease has shown itself at present in the neighbourhood of Palermo as well, in a vineyard of Count Tasca, and which seems to threaten serious disaster to our wild vine), I recommenced my re- searches on the vine, of which, for the moment, I will state the following facts : Up to the present, I have never been able to detect even the slightest trace of starch in all the vine leaves I have examined, either young or old, in different vineyards and different varieties. The chlorophyll-grains of the vine, when treated with alcohol, potash, acetic acid, or iodine (usual method), appear more or less with hollows, but there never is the slightest indication of a starch reaction. Holes and little gutters are also formed in the chlorophyll- grains, either under treatment with alcohol, or even with distilled water. When dry, and without applying any reagent, the chloro- phyll-grains appear (uniform) without any holes or cavities. The chlorophyll-grains, which are for several days placed in a saturated solution of bichromate of potash, appear mostly without holes, but have lost their homogeneousness, and often show in their interior more or less dark spots. On the other hand, I never found starch in the mesophyll of the vine leaves hitherto examined by me, with exception of the enclosure-cells of the stomata, where it is never wanting. A small quantity of starch only is found in the vast crivellati and in the strati amilacei of Sachs, and in the ordinary fibro-vascular bundles. * ————— The Action of Chlorophyll in the Vine. By Giovanni Briost. 287 Glucose, too, I have been unable up to the present to ascertain microscopically in the vine leaves, since I, once only, had precipi- tated some red grains of oxide of copper in but two cells; if afterwards there was found glucose, it was in such small quantity as to be totally insignificant. Of oil or fatty matter, either nothing, or an insignificant proportion, is found. The only substance, however, amongst those determinable by the microscope, which is met with in abundance in the vine leaves, is tannin. It is found not only in the epidermal cells without chlorophyll, on both sides of the leaf, but also in all the cells with chlorophyll ; nay, in the substance of the palissade (palizzata) cells of the upper part of the leaf, where, by the direct action of the light, the influence of the chlorophyll must be more energetic than anywhere else, tannin is most abundant. From this, and other observations, I will not conclude as yet that tannin is formed in the chlorophyll-grains of the vine leaf, well knowing how daring such a conclusion might appear, in- asmuch as the greater number of researches made with regard to the share held by the tannin substances in the vegetable economy, lead us to regard the tannin more than anything else as a secondary and lesser product, and one of those which, when once formed, change no more, and remain as inert substances in the cells in which they originated, without having any share in the formation of fresh organic substance. At any rate, from researches now undertaken, I hope soon to be able to say something more positive on this subject. One more observation: It is at present generally admitted that the libro tenero is made up of the texture which is destined for the carriage of the protein substances, whilst the hydrocarbons and the fatty matters would be conducted through the parenchyma. This theory originated with Professor Sachs (to whom vegetable physio- logy owes so much), and rests mainly on the fact that in the elements of the first texture only albuminoid substances are found, and because chemists never have been able to find starch, other- wise than in an exceptional manner, notwithstanding that the degree of these triple (threefold) substances can be so very easily ascertained. On another occasion * I have shown that in the libro tenero, and specially in the cribriform vessels, starch scarcely ever is want- ing, and even that this starch, on account of its most minute formation, and of the peculiar construction of the said organs, seems well adapted to be carried from one part of the plant to another. At present, it is not without interest to know that, in * Briosi, “Ueber allgemeines Vorkommen yon Starke in den Siebréhren” (‘ Botanische Zeitung,’ 1873, No. 15 and following ones); also ‘ Nuovo Giornale Botanico Italiano, April 1875. 288 On Corpuscles of the Cornea, de. By G. I. Dowdeswell. the libro tenero of the vine, and particularly in the cribriform vessels, there is undoubtedly found besides starch, also tannin, and this in great abundance; this fact will help also to account for the physiological action exercised by this substance in the plant. I shall soon publish the particulars of the researches alluded to in the present preliminary communication. V.—On the Changes of the Fixed Corpuscles of the Cornea in the Process of Inflammation. By G. F. Dowprswent, B.A. Puiate CLXXXIV. Srvce the discovery by Von Recklinghausen of the immigration of pus-corpuscles into the substance of the cornea in inflammation, several observers have alleged that proliferation of the fixed cor- puscles of that tissue also occurs; in other words, that the so- termed leucocytes are not entirely immigrant, but that some of them are formed in the inflamed tissues. It is stated by those who take this view of the process, that in a few hours after the establish- ment of inflammation the fixed corpuscles begin to alter, that their processes are partially retracted and thickened, their outline be- coming more distinct, and that at a later period small spherical bodies appear in their substance by a process of endogenous cell- EXPLANATION OF PLATE CLXXXIV. Group I. Corpuscles of the Normal Cornea. Fic. 1.—T wo corpuscles, isolated, of a vacuolated appearance; nucleus indis- tinct, processes much anastomosing. Fic. 2.—Two similar corpuscles. Fic. 3.—A single corpuscle, showing reduplication of nucleus and nucleolus, and what might be taken for segmentation of its substance. Fic. 4.—T wo typical normal forms. Fic. 5.—A single corpuscle, with very large and strongly defined nucleus. Group II. Corpuscles of a Cornea forty-eight hours after commencement of inflammation by application of Nitrate of Silver. Fia. 6—A group of fixed corpuscles (c) and wander cells (wv). The latter are seen to be of diversified form and in an active state of cell-division. ‘The appear- ances which the fixed corpuscles present are all paralleled in the figures of normal pene and, notwithstanding the activity of the inflammation, as evidenced y the state of the wander cells, there is no appearance of proliferation nor of any- thing abnormal in these. Fic. 7.—A corpuscle with conspicuous nucleus and two wander cells (~) cling- ing to its processes, Fic. 8.—Two corpuscles, the one vacuolated and with nucleus distinct, the other similar to Fig. 3, Group I. On Corpuscles of the Cornea, de. By G. F. Dowdeswell. 289 formation ; that with the progress of inflammation these changes increase, the corpuscles losing their stellate form, and assuming the character of endogenous mother-cells which divide by fission. These observations have all apparently been made upon corneas excised and examined in serum or other fluid, or upon lamine of corneas prepared by the gold method. Cohnheim and others have denied that the changes are objective, and attribute all the appearances to an active immigration of leuco- cytes. A principal objection to this conclusion has been founded on the grounds that the observations commenced too late, when the asserted changes had already occurred. In the ordinary methods of preparation, the appearances pre- sented during the second and third day of the inflammation are such as might readily be conceived to arise from proliferation of the elements of the tissue ; and it is unquestionably matter of great difficulty to determine with certainty whether this does occur or not. ‘The purpose of the present note is to describe a mode of in- vestigating these appearances, by the employment of which satis- factory evidence may be obtained that the process essentially consists in the penetration of colourless corpuscles (migratory cells), in a state of active cell-division, into the cell-spaces of the cornea, where they overlie and obscure the cornea-cells in such a way that, in preparations made by the usual methods, they appear to be incorporated with them. If, however, a method is employed by which the ground-substance can be destroyed (as e. g. by potash) and the corpuscles separated by teasing, it is shown that they are perfectly unaltered, the migratory or wander cells only undergoing cell-division ; so that it is by the presence of the latter alone that the difference between a normal and an inflamed cornea can be recognized. The appearances presented by these corpuscles in corneas pre- pared by the ordinary methods, when supposed to be undergoing proliferation, have been so often described and figured that they need not be further referred to here. Methods adopted in these Haperiments.—Inflammation was induced either by touching the surface with a fine point of nitrate of silver in the usual way (in which case the ensuing process arrives at its height in about forty-eight hours,.and then gradually sub- sides, so that by the fourth or fifth day its effects have disappeared), or (when it was desired that the process should be of longer dura- tion) by a seton of silk thread. The animal having been killed at the proper period, and its cornea excised and immersed in half per cent. solution of gold chloride for sixty minutes, and exposed in a light warm place, when sufficiently coloured a small portion of the inflamed part is placed in a solution of potash till the ground- substance 1s completely dissolved. Care is requisite to hit off the 290 On Corpuscles of the Cornea, de. By G. F. Dowdeswell. exact point for this, a few minutes too much or too little rendering the preparation useless. If the time of exposure is too short, obviously the ground-substance is not wholly dissolved, and nothing is seen; if it is too long, the potash begins to act upon the pro- toplasm, and the corpuscles cannot be separated nor distinguished. It was found that, if the cornea was put into a 20 per cent. solution of pure potash cold, and then subjected to a temperature of 40° C., fifty minutes was the proper time required for the action of the potash. When sufficiently acted upon, the cornea is transferred to slightly acidulated water, to stop any further action of the potash, then placed on a slide, if necessary teased out lightly, and pre- served in glycerine. Ina preparation made by the above methods, a number of migra- tory cells will be apparent under the microscope, some of which are entangled amongst the processes of the fixed corpuscles. All these are in a state of active cell-division and assuming diversified forms, but are very readily distinguished from the fixed corpuscles by their being devoid of processes, of somewhat darker colour, and by their presenting a more opaque and solid appearance.* The fixed corpuscles, with their processes, show no alteration whatever. As may be seen from the Figures (Plate CLXXXIV., Group II.), the processes radiate from the bodies in a natural and symmetrical manner, and the ramifications are as perfect as ever. This would certainly not be so if segmentation had occurred; for in that case one side at least of each newly divided corpuscle would be devoid of processes. Nothing approaching to such a condition is ever seen. In inflamed preparations, as in normal ones, fixed corpuscles are occasionally met with containing two nuclei or a double. nucleus; but this appearance is not often seen, and not more fre- quently in later than in earlier stages. In conclusion, it may be stated that in the whole number of successful preparations of corneas which have been examined (amounting to upwards of twenty), no single instance has occurred in which any distinct appearance of segmentation can be made out. The most careful scrutiny of the preparations fails to detect any difference whatever, as regards their forms or aspects, between the fixed corpuscles of inflamed corneas and those of normal corneas — prepared in a similar way; nor would it be possible to distinguish preparations of the two classes from each other, were it not for the presence of migratory cells in the inflamed structure. In the drawings representations are given both of normal pre- parations (Plate CLXXXIV., Group I.) and of others at the most active period of inflammation (Group IJ.). These have all been most carefully drawn under the camera, each fibre and line being * This is not adequately shown in the drawings. TheMonthlyMicroscopical Journal June 1.1877. Pl. CLXXXIV. Group I ~~ West & Co lith, Corneal corpuscles. Group],normal,— group Zintlammatory. “ On the Teeth of certain Ruminants. By M. V. Pietkiewicz. 291 actually copied as they appeared in setw in the field of view of the microscope, some processes and other bodies being omitted for the sake of clearness, and the peripheral members of the group sometimes brought nearer to the centre to save space. Numerous other preparations were made at all stages of inflammation, com- mencing with five hours, when little or no change was observable, up to five and seven days, when, in the case of inflammation induced by nitrate of silver, the effects had passed off, leaving no recognizable traces.—Proceedings of the Royal Society, No. 177.* VI.—Goodsir’s Arguments on the Development of the Teeth of certain Ruminants. By M. Y. Prerximewicz. In a communication made to the British Association in 1839 Goodsir announced that he had discovered in the jaw of the calf and sheep the germs of incisor and canine teeth, and even of a molar, intermediate between an abortive canine and the ordinary molars which exist in these animals. Geoffroy Saint-Hilaire had already described abortive dental germs in the lower jaw of the baleen whale (Balena mysticetus). Naturalists, partisans of the theory of Lamarck, and of Evolution, Darwin particularly, seized hold of this idea; and thus associating the discoveries of compara- tive anatomy and paleontology, this embryological discovery per- mitted the association of groups of animals which had before been separated. Everyone knows the difference which exists between the dental formula of ordinary ruminants, as the ox and sheep, whose formula is 1} C$ M &, and the formula of the omnivorous pachyderms, the hippopotamus and the wild boar (le Sanglier),I13C1Mz. But all authors have found the presence of superior canines in two or three genera of ruminants, the deer and the goat, which have a formula of I$ C+ M €, and the existence of a pair of very distinct upper incisors in the camel (chameau) and lama (Jamas), giving the formula 1} C} M&. According to M. Paul Gervais these latter had even two pairs of upper incisors, one of which disappeared in the adult, but was present in young animals, so that they would have this formula 1? C+ M&; this author does not doubt either ~ that if the animal was examined at a younger age stili, one would find a third pair of incisors in them, and thus that their dental formula would be related to that of pachyderms minus one molar: I3C{}Mé&. Then, on the other side, the study of fossil species has shown that the Dinotheriwms and the Amphitragalus, con- sidered as ruminants of the group of Chevrotins, have seven molars * Professor Huxley has kindly given permission for its reproduction here.— Ep. ‘M.M.J.’ 292 On the Teeth of certain Ruminants. By M. V. Pietkiewiez. as the wild boars (Sangliers) have, that is to say the same number as the pachyderms. Thus, among the ruminants, we already know of fossil species having the same dental formula as the pachyderms, and of living species whose formula is almost identical; the dis- covery of Goodsir, by giving to ordinary ruminants, such as the ox and sheep, at a certain period at least of their lives, the same for- mula as that of pachyderms, permits us to associate these two groups. One set of naturalists sees in this one of the results of their hypothesis upon the unity of plan in nature. Another set sees in it a confirmation of their transformist theories, and explains the abortion of these organs by their non-usage, and the successive confirmation of this anomaly by “ adaptation” and “ heredity.” I was therefore surprised when, in endeavouring to verify an opinion which was so creditable to science, I found nothing what- ever to justify it. In a long series of preparations made upon the embryos of the ox and the sheep from the earliest period of em- bryonic life to the period when the foetus is 30 centimeters long in the sheep, not only have I never found the presence of follicles, but I have not even found a trace of the epithelial lamina, the beginning of all follicular development. Goodsir’s error was conceived through the false notion he had formed of the development of the follicles, and in the commence- ment of my investigations I had the same idea. In sections made properly at the anterior part of the upper jaw of the ox or sheep one finds in fact on each side of the median line an epithelial sac, which detaches itself from the buccal mucous membrane to bury itself in the jaw. The mucous layer of Malpighi uninterrupted forms itself an external lamina, whilst on its interior is found a polyhedric epithelium like that of the middle layers of the buccal epithelium. Thus formed this little sac appears to constitute the commencement of the follicle as Goodsir imagined it. But in continuing to make on the same jaw a series of sections going farther and farther from the anterior part, one sees the little sac lose its relations with the buccal mucus, and take the form of a circular canal for the mucus of the nasal fosse. Soon appears around this canal a cartilaginous belt, then at its upper part is a pad (bourrelet) containing vessels, and then one has before him Jacobson’s organ as Gratiolet described it. There is then nothing that can be compared even distantly to the germs of canines and incisors. If it is possible to conceive of Goodsir’s error in face of the little epithelial sae pro- duced by section of the buccal extremity of Jacobson’s organ, one finds nothing to justify him in affirming the presence of three incisors, of one canine, and of one molar tooth in this region.— Comptes Rendus, March 12, 1877. PROGRESS OF MICROSCOPICAL SCIENCE. The Structure and Origin of Meteorites—It may perhaps seem very strange to speak of the microscopical structure of the sun; but if meteorites have been formed in the manner suggested in Mr. Sorby’s lecture, published in ‘Nature’ for April 5, such an expression may not be unreasonable. He there shows that the microscopical structure of meteorites, though in some cases analogous to that of melted lavas, is yet in a greater number of cases more like that of consolidated vol- canic ashes. They have, however, some remarkable characters not yet found in any terrestrial rock, which indicate that they were formed under very special conditions. They frequently contain what were apparently originally small glassy spherules, which subsequently be- came more or less crystalline and devitrified. A large portion of some of these spherules is, however, still a true glass. The author shows that they are analogous to certain artificial furnace-products, but differ in such a way as to indicate that a melted glassy spray was projected into an atmosphere heated so nearly to its melting point that the par- ticles could collect into spheres without being drawn out into long fibres, as happens when the spray is blown into a cool atmosphere, so as to form the natural Pele’s Hair, or the analogous artificial furnace- product. Many other remarkable structures occur in meteorites, some requiring high magnifying powers ; and the general conclusion deduced from them is, that meteorites were formed when the surrounding at- mosphere was highly heated and subject to intense mechanical dis- turbances. Nearly all these remarkable peculiarities could be explained if they were formed under conditions like those now proved to cecur near the surface of the sun, and the chief question is whether they are portions of solid matter, perhaps now projected into space during the intense disturbances known to occur on the surface of the sun, or are remnants of matter subjected to similar influences at a remote epoch when the conditions now met with only near the sun extended much farther out into planetary space. If this be the case, it is perhaps not too much to say that the microscope was never applied to a question of greater magnitude, and the important bearing of very minute on immensely great objects made more apparent. Mr. Dallinger’s Lecture on Monads at the Royal Institution—On the first Friday evening of last month (May), the Rev. W. Dallinger, V.P.R.M.S., delivered a most important lecture on monads before the Royal Institution. The illustrations were given by means of the electric lamp so familiar to those who go to the Albemarle theatre, and they were in every respect admirable. The lecture, however, was in substance similar to Mr. Dallinger’s excellent article in one of last year’s numbers of the ‘ Popular Science Review.’ He proved the mar- vellous changes of form seen in some of these species of monads to be continuous alterations which invariably ended in the production of the original type. This he did by the most wonderfully patient observations. He also proved—a most important poit—that there 294 PROGRESS OF MICROSCOPICAL SCIENCE. was a difference in the power of resisting high temperatures exhibited between the mature and young forms of monads. This fact is of in- finite importance, as it tends to overthrow Bastian’s notions. The Diatom Earth of Richmond, U.S.A.—This subject has been discussed in an opening article (by Mr. C. L. Peticolas) in a late number of the ‘ American Journal of Microscopy.’ It says that to the microscopist this deposit is a source of unfailing interest, whilst the most inexperienced in such matters, upon being shown the wonderful forms found in it, are struck with surprise and delight. In looking at these different forms, one is struck with the wonderful resemblance which they bear to things of every-day use, as among them may be found models of almost all the implements used by savages, whether for war, the chase, or in domestic life; witness, for instance, his stone hatchets, arrow and spear heads, knotted clubs, boomerangs, &c.; a catalogue of such matters used by civilized people would embrace plates, dishes, cups, saucers, gridirons, pins, balls, tops, spectacles, watches, anchors, dumb-bells, cannon, coin, musical notes, and many other articles—the investigator being constantly startled by the strange resemblance which hundreds of these ancient natural forms bear to articles used in our houses and workshops. Certain varieties, however, predominate, and their distribution varies with level and locality, the upper portion of the stratum being compa- ratively poor in forms, while they increase in number and variety as we descend to the middle, falling off again towards the bottom. The genus Coscinodiscus seems to characterize this earth, and of it there are dozens of varieties varying from the (microscopically) enormous C. gigas to the minute and elegant C. subtilis, which resembles closely a finely polished opal, requiring a lens of wide aperture and consider- able power to show its revelations. Orthosira marina is abundant, whilst many beautiful forms of Navicula are found in every gathering. Amongst these we may note two kinds of Pleurosigma, one of which, P. angulatum, is a favourite test-diatom, and the other, which it is pro- posed to call P. Virginica (as it is the most common form of Plewrosigma in the Virginia earths), is remarkable for the beauty of its contour, which exactly copies a willow leaf, and the want of uniformity in its strie, which are much coarser in the middle than at the ends of the valves. It is easily resolved with a }-inch objective, without the aid of oblique light. The genus Triceratium is also well represented by many beautiful varieties, the most interesting of which is T. obtusum, which can be resolved as easily as P. Virginica. Isthmia enervis, Bid- dulphia Turmegti, Terpsinoe, Musica, Aulacodiscus crux, Navicula lyra, Gonphonema, Heliopelta, Asterolampra concinna, Asteromphalus Brooketi and Synedra are comparatively rare. From the great variety of its species, and the wide range in the character of their markings, the Richmond earth forms one of the best and most interesting tests for the performance of objectives of almost every power. On some, for instance, the areolations may be seen with a simple triplet, magni- fying 25 linear; on others a first-class twelfth or sixteenth of wide angular aperture, aided by all the modern refinements of illumination, is needed to show them. PROGRESS OF MICROSCOPICAL SCIENCE. 295 Starch in Granules of Chlorophyll.—According to a contemporary, Bohm asserts that if light is sufficiently intense to induce assimilation in green leaves, it has the power to cause an immediate transfer of starch from the stem, where elaborated matters may be stored, to the chlorophyll granules. For this reason he believes that many observa- tions hitherto made in regard to the immediate production of starch from carbonic dioxide in chlorophyll are untrustworthy. Such experi- ments should be made upon plants which have no starch already stored up, or upon detached leaves which contain no starch. Reproduction in the Ascomycetes Fungi.—A paper on this subject has been contributed by M. Maxima Cornu to the ‘ Annales des Sciences’ (1876, page 53), and it is given in lengthy abstract in a recent number of the ‘Journal of Botany.’ It states that the term “ sper- matia” has hitherto been applied to conidia-like bodies collected in special cavities, and thought to be incapable of germination. Tulasne had in some instances observed germination of bodies similar to sper- matia, but where budding did not result, instead of doubting the perfection of his cultural methods, he believed he had to do with sexual elements, and to these he applied the special term. By adopt- ing a system of culture somewhat similar to that made use of by Van Tieghem and Le Monnier in their researches on Mucorini, M. Cornu has succeeded in causing germination of many spermatia. The most satisfactory results were obtained when the nutritive liquid consisted of distilled water with 1 per cent. of sugar and 0-4 per cent. of tannin, though in a few instances simple water was the most ad- vantageous medium of growth. With these results in hand, M. Cornu thinks it permissible to suppose that all spermatia are capable of germination if a suitable liquid can be found for each case ; it becomes necessary, therefore, to consider the relations of spermatia to the similar reproductive bodies known as stylospores and conidia. Their main point of difference from stylospores resides in the fact that the membrane of the latter is usually double, while, unlike conidia, spermatia are collected in special cavities. MM. Cornu thinks that terminology is here too exuberant, and he proposes the elimination of the term “ conidium,” referring thick-membraned conidia to a place among stylospores, and thin-membraned to spermatia. He also, following out Bonorden’s suggestions, expresses his belief that certain Mucedines—e. g. Verticillium, Acrostalagmus, Dendrochium, &c.—are spermatia-bearing forms of Ascomycetous genera near Hypomyces ; other Mucedines he would refer to Peronosporeee and Mucorini. With regard to the function of spermatia, M. Cornu shows that, being very small and produced in great numbers, they are capable of causing wide diffusion of the species, the difficulty of germination being an additional advantage in diffusion, since the chances are considerable that before they reach a suitable nidus some time must elapse, during which they may be transported by the agency of winds, birds, &e. The Lymphatics of the Joints.—Dr. Stirling states in the ‘ Medical Record’ that Herr H. Tilimanns contributes an essay on this subject to the ‘ Archiv. fiir Mikros. Anat.’ (Band xii.) It would seem that 296 PROGRESS OF MICROSCOPICAL SCIENCE. the lymphatics of tendons, fascie, and serous membranes can very conveniently be injected by flexing and extending these parts. The joint of a newly killed dog was filled with a coloured fiuid, and the limb flexed and extended, but no colouring matter entered the lymphatics. This would seem to show that absorption from the synovial surface takes place in a way different from that which obtains in the case of serous membrane. By the puncture method, however, Tillmanns easily succeeded in injecting with a 0°5 per cent. solution of silver or soluble Berlin blue, a very rich network of lymphatics lying immediately under the epithelium and also in the subsynovial connective tissue. This he did in the large joints of the ox and horse. The superficial lymphatics lie directly under the epithelioid layer, deeper than the finest capillaries, but superficially to the large arterial and venous branches. The author finds that the blood-capillaries do not project bare into the joint, but are covered by the epithelioid layer. No lymphatics were found in the villi of the joints. The superficial subepithelioid lymphatics communicate with very wide vessels lying in the subsynovial tissue, where the lymph-vessels are very numerous and not unfrequently surround the blood-vessels. The vessels can be most easily injected where the synovial membrane joins the base or cartilage. No lymphatics pass from the synovial membrane, either into the subjacent bone or carti- lage. The microscopic structure of the lymphatics was studied by Stirling’s method, viz. digestion in artificial gastric juice. It seems that the epithelioid lining of the lymphatics is directly continuous with the elastic tissue of the adjacent tissue, thus fixing the lym- phatics. The lumen of the vessels will thus be kept patent by the elastic fibres, and may even be dilated when the fibrous tissue becomes swollen. This bears out some suggestions already made by Ludwig under normal circumstances. Remarks on the Structure of Precious Opal.—Professor Leidy, according to ‘Silliman’s American Journal’ for April, has an article in the ‘ Proceedings of the Academy of Natural Sciences of Phila- delphia’ for 1876, p. 195, on the microscopic structure of the opal of Queretaro, Mexico. Structure of the Red Blood-corpuscle of Ovipara.—Mr. Gulliver sent a note on this subject to a late meeting of the Hast Kent Natural History Society. It is conceivable, he wrote, that there may be an essential difference between the corpuscles of batrachians and fishes ; so that, granting the truth of his own and Mr. Hammond’s obser- vations on the presence of the nucleus in the living corpuscles of this class, the validity of Professor Savory’s observations on the absence of the nucleus of the living corpuscles of frogs and newts would not be necessarily destroyed. And then the question would only be like that which was so much agitated upwards of a quarter of a century ago, concerning the structure of these corpuscles throughout the ver- tebrate sub-kingdom. At that time one party, following Hewson, declared that the nucleus is quite distinct; while another party, with PROGRESS OF MICROSCOPICAL SCIENCE. 297 Dr. Young, Dr. Hodgkin, and Mr. Lister, maintained that there is no nucleus. But the subsequent researches of Mr. Gulliver had proved that the disputants on both sides were, as in the fable of the chame- leon, both right and wrong; for the regular blood-disks of mammals are destitute of a nucleus, while those of the lower vertebrates are regularly nucleated. And hence his two great divisions of vertebrates —Apyrenemata and Pyrenemata. The Blyborough Tick.—At the above Society, referring to the plates and engravings of this tick, lately published with descriptions in the ‘Journal of the Quekett Microscopical Club,’ and in ‘ Science-Gossip,’ it was stated that specimens received from Blyborough had been for- warded from Canterbury to Oxford, and declared at that University to be identical with a species described and named Argas pipistrelle, by Professor Westwood, in the ‘ Proceedings of the Entomological Society of London,’ for the year 1872. The Microscopical Active Principle of the Cobra Poison.—An inter- esting paper in which the chemistry of cobra poison is exhaustively dealt with, appeared lately in a paper termed the ‘ Analyst, from the editor of which we have obtained the blocks used to print the figures over leaf. These representations are figures magnified 250 diameters of cobric acid, of which the following account is taken from an essay by Mr. W. Blyth, M.R.C.S., that appeared in the ‘ Analyst’:—“On the 1st of January of this year, I succeeded in obtaining a crystalline, acid, extremely poisonous substance, which appears to be contained in the venom to the extent of 10 per cent.; this substance, there is every reason to believe, is the sole and only active principle. It may be obtained by coagulating the albumen with alcohol, filtering, driving off the alcohol at a gentle heat, concentrating the liquid to a small bulk, precipitating with basic acetate of lead, collecting the precipi- tate, washing it, and subsequently decomposing it in the usual way by SH.,, removing the sulphide of lead, evaporating to a small bulk at a gentle heat, and finishing the evaporation spontaneously or in a vacuum, or it may~be obtained by coagulating and separating the albumen as before, shaking up in a tube with ether, removing the ether in the usual way, evaporating the ether off, redissolving in water and passing through a wet filter to separate fat, and evaporating as-before; in either case the result is microscopic needles, dissolving in water with an acid reaction and possessing highly poisonous pro- perties; they appear to be identical with the needles obtained by sublimation. “For this substance I provisionally propose the name of cobric acid. I have not been able to go as yet any farther in the investigation of this interesting substance, for the simple reason that my two very small supplies are now exhausted, and I must wait for a third packet, but it will not be uninteresting to pause for a moment to consider what a terribly active substance this cobric acid must be, for sup- posing Nicholson’s data are correct, and that the whole of the average quantity of the venom (that is 6 grains, containing 2 grains of solids) 298 PROGRESS OF MICROSCOPICAL SCIENCE. is injected into a man, it t!:en follows, since the solid residue contains 10 per cent. of cobric acid, that one-fifth of a grain would be fatal, so that we have here a rival to aconitia weight for weight in its power of destruction.” t \i | Cobric Acid magnified 250 diameters. The Blood-vessels of Muscle under the Microscope.—Mr. W. H. Gaskell has recently presented a paper on this subject to the Royal Society, in which he describes the results of observations made on the living blood-vessels of the mylohyoid of the frog. He says he found that the mylohyoid muscle was the most suitable one for his purpose, it being easy to prepare it for microscopic observation without da- maging the circulation through it, and, in fact, without even touching the muscle; whilst, owing to its thinness, the small amount of con- nective tissue in the neighbourhood of the vessels, and the absence of pigment-cells, it is possible here to measure with a micrometer eye- PROGRESS OF MICROSCOPICAL SCIENCE. 299 piece the diameter of vessels more accurately and easily than in any other preparation. Upon placing this muscle under the microscope, without having previously touched the nerve, it is seen that the cir- culation presents much the same character as in the web, the median red-corpuscle stream with an inert layer on each side being plainly visible, although, perhaps owing to the manipulation, the arteries at first are slightly fuller and more dilated than the corresponding vessels in the web. The calibre of the smaller arteries does nof, as a rule, remain for any length of time the same, variations taking place some- what similar to what has often been described in the vessels of the web, but with this difference, that whereas in the so-called “rhythmic contractions” of the arteries in the web the artery appears to contract to a certain point and then to return to its original calibre or beyond it, in the arteries of the muscle the vessel appears to dilate from the normal calibre, and then gradually to return to that calibre or below it. These dilatations vary considerably in extent and are abso- lutely irregular in time, being much less marked both in frequency and extent in some frogs than in others, and depend, so it seems to him, probably upon some chance stimulation of the vessels, such as exposure to the air, &e. Upon direct stimulation of the web by means of the interrupted current there occurs a most marked constriction, not only of the arteries between the electrodes, but extending over the whole web, both during the stimulation and for some little time after the stimulation is over. He goes on to say, ‘“ Whether the arteries immediately between the electrodes contract, I cannot yet say; I can, however, affirm positively that there is no contraction of the smaller arteries situated but a slight distance from the electrodes, or if there is, it must take place in the very short space of time necessary for refocussing on the artery under observation, as in every Case, as soon as I have been able to measure the calibre again, I have found it con- siderably dilated. Here, then, is a marked difference between the web and mylohyoid on direct stimulation. As to the effect of section of the nerve, I have always noticed that it is followed by a decided reddening of the corresponding muscle, the difference of colour being manifest, as previous to the section the two mylohyoid muscles are always equally pale. Upon closer examination, by first putting the muscle in position under the microscope and then cutting the nerve, it is seen that about five to six seconds after section the arteries dilate very rapidly, the dila- tation soon reaching a maximum, in perhaps twenty or thirty seconds, and then gradually diminishing until the original calibre is reached, some four or five minutes after section—that is, the dilatation caused by section of the nerve is not a lasting one, but is exceedingly similar to that caused by slight mechanical stimulation of the nerve ; for whether its peripheral extremity is pinched by a pair of forceps, or dipped into concentrated salt solution, or still more markedly when cut and torn by scissors and forceps, there always occurs after a brief latent period of a few seconds, during which there is no trace of constriction, a con- siderable rapid dilatation of the artery, which lasts but a short time, and then gradually gives way to a return to the original calibre, and is always accompanied by a more active very full stream, the inert VOL. XVII. Z 3800 PROGRESS OF MICROSCOPICAL SCIENCE. layer having wholly disappeared, and the red corpuscles being crowded together to the very edge of the vessel. Here, then, is another marked difference between the web and the muscle.” * Mr. Lewis’ Freezing Microtome.—The adjacent cut represents this instrument, which Mr. Bevan Lewis, F.R.M.S., has described at some length in the ‘Journal of Anatomy’ (vol. xi.), and which is not so novel as he seemed to think at first. In fact, he states at the conclu- sion of his paper that he then became aware of a previously described instrument by Mr. Hughes; but he says that in his (Mr. H.’s) micro- tome, the spray is not so directly brought to bear upon the tissue, which consequently requires from five to eight times as long a period to freeze, with, of course, a corresponding increase in the loss of ether : this is of material import when absolute anesthetic ether is em- ployed. He states that “the instrument consists of three portions: (1) an ordinary Stirling’s microtome; (2) a section plate; (3) a freezing and condensing chamber. The simplicity of the arrange- ment will, I trust, recommend its use amongst my fellow-workers in the department of cerebral histology. Reference to the accompanying woodcut will place the reader in possession of the plan upon which H this instrument has been constructed. The section plate (a) is riveted by a brass arm to the microtome (b). The freezing compartment (c) consists of a cylinder (d) and a condensing chamber (e), the latter being formed of brass with a sloping floor leading to the exit-tube, which is provided with a stop-cock (f). The cylinder is capped with tin-foil stretched across it, and has an orifice (d) through which the nozzle of the spray apparatus is introduced. In using this instru- ment it is only necessary to bring down the cap of the cylinder from one-fourth to three-eighths of an inch below the level surface of the section plate, and to place in it a section of brain of about the same thickness. The spray instrument is inserted at the orifice,and by the ordinary double elastic balls a free play of ether beneath the cap freezes the tissue in from twenty to thirty seconds or less. On with- drawing the spray instrument, the slight play of ether, still continuing from the remaining tension of the elastic ball, is utilized by being * “Proceedings of the Royal Society,’ No. 176. PROGRESS OF MICROSCOPICAL SCIENCE. 301 carried rapidly along the surfaces of the section blade, and then the finest possible sections may be cut with great ease. The consistence of nervous structures, when thus frozen, is really exquisite for section cutting, and the tissue remains rigidly adherent to the capped top of the cylinder. Perfect steadiness of the freezing chamber is ensured by soldering it to the microtome plug, and it can be readily removed from its position by throwing back the section plate, a movement allowed for by the hinge-joint (#).” The Siliceous-shelled Bacillarie in Diatomacee.—These are being described in the ‘American Journal of Microscopy’ (March and April),* from papers which originally appeared in the ‘ Lens,’ and which were translations by Professor Smith, of Kiitzing’s work on the Bacillarie. Strange to say, however, there is no notice of either author or translator attached to the paper itself. But in another part an editorial note explains this fact. To those who are unfamiliar with the original work, this translation must prove of interest. The last passages in the April number contain a very decided but well- merited attack on Ehrenberg for his habit of disregarding the work of others in establishing species. Reproduction of Rotifer vulgaris—An American, Mr. C. F. Cox, has been studying this subject with some success. He says that “My attention was called to the process of reproduction by seeing, in the larger rotifers, an extra ‘gizzard’ below the one to which each individual seemed properly entitled, and by observing the in- dependent movements of the imprisoned embryos. But a simple egg-shaped vacuole-like ovum is to be seen in every rotifer, even at its birth, I believe. Subsequently the embryo develops its ciliated lobes, its proboscis, its eyes, and its foot or leg, and for a short period before birth a slight ciliary movement may be seen, and a slow working of the gizzard. At this time its head is close to the gizzard of the parent, and the appearance is as if the fetal rotifer were actually sharing the food of the mother and remas- ticating it. This, however, finally ceases, and the foetus, generally with some difficulty, turns itself within the parent, in order to present its head first at the time of parturition. If the operation is inter- rupted, or the parent much disturbed, the foetus may turn back again, and this vacillation is in many cases repeated several times before birth is effected. Some writers state that the nascent rotifers ‘creep out of their envelopes, extend themselves, and put their wheels in motion, while within the ovary, but I am convinced that motion of the ‘ wheels’ is impossible at this time, both from the size and from the position of the young, and the rest of the statement quoted seems to me highly imaginary. The slight ciliary motion observable at this time is produced, I think, not by the large cilia upon the infolding head-lobes, but by a ciliary system lining the throat of the animalcule, analogous to the ciliary system which I have discerned in the throat * By the way, there appears to be some irregularity of publication about this journal. We have only to-day, May 8, received the number dated April. Is it published at the end instead of the beginning of the month? a2, 302 PROGRESS OF MICROSCOPICAL SCIENCE. of Floscularia. From this motion’s being seen so plainly in the nascent rotifer, I am inclined to believe that it is by this means that food is taken from the parent’s supply, as already suggested. The movements of the foetus do not seem to trouble the parent in the least degree, although she is, as usual, extremely sensitive to any external motion. The whirling of her cilia and the working of her gizzard are interrupted by the reproductive process only at the very instant of parturition. The ovarian sac opens into the cloaca, or rectum, of the rotifer, and the young is extruded from the anus, which is just at the lower edge of the upper segment of the foot-stalk or leg, and is what is rather indefinitely fermed, by some authors, the ‘ contractile vesicle.’ At the critical moment the parent draws herself violently together, so as to force the head of the young rotifer through the anus, and then the latter actively liberates itself and crawls away. At first it is somewhat awkward and undetermined in its movements, but, after creeping about for a few minutes, it attaches itself to some fixed object and opens out its ciliary wreaths, which it whirls as accurately and as gracefully as any old animalcule could do. Frequently a mother rotifer, containing a well-advanced embryo, also contains several partially developed ova, one of which may be seen to be ' undergoing a sort of segmentation or differentiation, the gizzard being about the first organ to make its appearance. I have several times seen a large rotifer, which had been killed in some way, lying drawn up into a rounded mass, in which a lively young one was making frantic but ineffectual efforts to break through the envelop- ing corpse and escape. This suggests the conclusion that the de- velopment of the foetus, after it has reached a certain point, is dependent upon the parent only for food; and this supports my belief, already expressed, that the foetal rotifer actually and actively feeds, and does not merely passively imbibe. On seeing so many rotifers containing young as I have happened upon in the last few days, I am astonished that their reproductive process has not been oftener the subject of observation and description than it seems to have been. All the rotifers I now see are in the interesting con- dition described, and yet, according to ‘ the authorities,’ no males of Rotifer vulgaris have ever been discovered. Analogy, however, seems to indicate that this rotifer, like Hydatina, Brachionus, Melicerta, Floscularia, &c., is dicecious. The earlier steps in its mode of repro- duction are, therefore, an inviting subject for investigation. By the way, why do Pritchard, Carpenter, and others, persistently describe and draw Rotifer vulgaris with spined or hooked margins to the segments of the foot-stalk or leg? I think I have never seen it with such segments. The foot-stalk, as far as I have observed, is simply telescopic, like that of Acéinurus, and consists of more segments than are usually drawn or described—probably six. Can it be that there is a difference in these respects between the common rotifer of England and that of this country ?” A Tape-worm in a Cucumber (/).—It is stated that at a recent meeting of the Academy of Sciences, at Philadelphia, Dr. Leidy exhibited a specimen of a tape-worm said to havé been taken from the ee PROGRESS OF MICROSCOPICAL SOIENCE. 303 inside of a large cucumber. This was the first time he had heard of one of these worms haying been found in a vegetable. It had all the characteristics of a true tape-worm, but belonged apparently to an unknown species. The ovaries, containing round yellow eggs, were confined to the anterior extremity of the segment. [The ova of the mature worm may have been deposited in the manure with which these plants are so freely surrounded, and it is remotely possible that some one of them may have got in through some crevice in the plant, and may then have begun its development as though it had got into a mammal’s stomach, It is certainly difficult to understand. | The Structure of the Brachiopoda.—This is very well given in a series of papers in the April and May numbers of the ‘ Geological Magazine, by our most distinguished Brachiopodist, Mr. Thomas Davidson, F.R.S. King’s, Hancock’s, Owen’s, Morse’s, Gratiolet’s, and Deslongchamps’ views are fully discussed by the author. Carboniferous and Permian Foraminifera.—The volume of the Monographs of the Paleontographical Society for 1876 contains an important essay by H. B. Brady, entitled “A Monograph of Car- boniferous and Permian Foraminifera,’ the genus Fusulina being excepted. This has been well reviewed by a most distinguished Foraminifer authority, Professor T. R. Jones, F.R.S., in the May number of the ‘Geological Magazine. We give here the portion of interest to the microscopist :—‘ The ‘ Zoological Con- siderations,’ of especial interest to the Rhizopodist, comprise a critical review of von Reuss’ and Carpenter's classifications of Foraminifera, and a general comparison of the generic forms known in the Car- boniferous strata with those now living. The conclusions arrived at are—l,. The prevalent forms (except Fusulina) in the Carboniferous and Permian limestones do not belong strictly to either of the two sub-orders (Imperforata and Perforata) into which Foraminifera have been divided, but to intermediate types (especially Trochammina, Valeulina, Endothyra, Nodosinella, and Stacheia), neither invariably arenaceous nor uniformly perforate in their shell-texture. 2. In the modifications of these primitive intermediate types there are some varieties conspicuously sandy and imperforate, others essentially hyaline and porous; and these varietal peculiarities seem to have been transmitted as permanent characters, thereby originating the two parallel isomorphic series. 38. The porcellanous imperforate group (Miliolida) is of later creation, judging from negative evidence. 4, The Permian Rhizopod-fauna is much more limited than the Car- boniferous, being confined to five generic types (Trochammina, Nodo- sinella, Nodosaria, Textularia, and Fusulina), representing, however, at least four distinct families of Foraminifera, which in the Car- boniferous rocks are represented by fifteen genera.” More than twenty genera and many species are described and figured, and after naming them in their order, Professor Jones concludes as follows :— “The exposition of the structure of Valvulina and Endothyra and their interesting subarenaceous allies, already noticed, and the discovery of the Rotaline (Truncatulina, Pulvinulina, Calcarina), and of the Num- 3804 PROGRESS OF MICROSCOPICAL SCIENCE. mulinide (Archediscus, Amphistegina, and Nummulina), m the Car- boniferous limestones, are some of the most important points in this excellent Monograph; and its value is greatly enhanced by eight elaborate Tables, special and general, showing in great detail the geological and geographical distribution of the fifty-eight species, according to their localities and stratal horizons in the many districts whence they were obtained. A perfect index for genera and species and their synonyms completes the volume.” British Fossil Bivalved Entomostraca of Post-Tertiary and Car- boniferous Dates.—These have been thoroughly worked out and figured in sixteen plates in the ‘ Monographs of British Fossils, * by Dr. G. 8. Brady and Messrs. H. W. Crosskey and Dr. Robertson. Of it the ‘ Geological Magazine’ (May) says:—‘ The classification of the Ostracoda (the special group of Bivalved Entomostraca treated of in this Monograph), according to the shape, texture, markings, and hinge- ment of the valves, and the synopsis of their genera, based upon the anatomical characters of the animal, will be highly acceptable to the students both of recent and of fossil specimens ; and indeed these admirable synopses are full of the latest information, derived from the researches chiefly of Dr. G. O. Sars, of Norway, and Dr. Brady himself. ‘Of the 182 species of Ostracoda described in this Mono- graph, 24 may be considered to have been inhabitants of fresh or slightly brackish water, the remaining 108 being strictly marine species. All except Limnicythere antiqua are known in the living state. Of the marine forms found in the Post-Tertiary beds there are lists given,—1. Of those now known as characterizing the Arctic seas and the northern coasts of Norway, Scotland, and America. 2. Those now extinct, or unknown in the living state. 3. Those found in the Glacial and Post-Glacial deposits of Norway. 4. Those found in the Glacial (and Post-Glacial ?) deposits of Canada.” The Carboniferous Entomostraca have been handled by Professor Rupert Jones, J. W. Kirkby, and G. 8. Brady, in the same volume, and their observations extend only to “the Cypridinade and their Allies.” “Some parts of the Mountain Limestones of various countries seem to abound in subglobular bivalve carapaces, and their loose valves, which approximate in character to various members of the Cypridinad group; some are also found in the Coal-measures; and others in the older Devonian, and even in the Silurian rocks. They are associated frequently with other Ostracodous valves, such as Beyrichia, Leperditia, Cytheride, and Cypride of various alliances. In this part of the Monograph we find 183 Cypridine (directly related to the existing Cypridina); 7 Cypridinelle, 9 Cypridellinee, 6 Cypri- delle, and 2 Sulcune, which are genera arranged artificially to receive several forms of carapace varying by gradational differences from the valves of the known Cypridina ; 2 Cyprelle ; 1 Bradycinetus ; 1 Philomedes ; and 2 Rhombine, of which much the same may be said as of the foregoing ; also 4 Entomoconchi, 1 Offa, and 3 Polycopes. The definition of the true Cypridine,—the true allocation of the * Published by the Paleeontographical Society, vol. xxviii. PROGRESS OF MICROSCOPICAL SCIENCE. 305 several species placed by De Koninck under Cyprella, Cypridella, and Cypridina,—and a more exact interpretation of M‘Coy’s Entomoconchus, are (besides many new species) the chief novelties of this memoir, which is illustrated by five plates (by George West) very full of excellent figures of these small fossils.” Reproduction of Ulothrix zonata.—In a series of most valuable abstracts of German botanical papers that Mr. 8. Le M. Moore is giving in the ‘ Journal of Botany’ (May), appears the following, which is taken from a paper by Dr. Arnold Dodel in ‘ Pringsheim’s Jahr- bucher fiir Wissenschaft. Botanik’ (vol. x. p.417):—Ulothrix zonata has spores of two kinds—viz. 4-ciliated macrozoospores produced either singly or two together in the mother-cell, and 2-ciliated microzoo- spores arising several together in each mother-cell. Sometimes the two spore-forms are found in neighbouring cells of a thread, but they usually have distinct periods of activity, autumn and winter being favourable to the formation of macrozoospores, and spring and summer to that of microzoospores. The latter copulate and form resting zygo- zoospores, a fact which sets Areschoug’s position beyond cavil; but the strangest thing of all is that those individuals which fail to copulate are like the macrozoospores in having the power of imme- diate asexual reproduction. This most remarkable observation, which its discoverer regards as furnishing a transition state between sexual and asexual generation, comes to some extent to the timely support of the Strassburg school, who deny that the fact of germination is suffi- cient proof of the asexuality of spermatia. Several figures are given showing polymorphism of the threads and of the zoospores; between the two forms of the latter there are all kinds of transition, the only absolute distinction being based on the number of cilia. Further, it has long been known that microzoospores sometimes germinate while still in the mother-cell, and Dr. Dodel has seen some of them dege- nerate in this position without budding. Dr. Dodel agrees with Pringsheim that copulation of microzoospores is the morphological type of sexual reproduction. As for the zygozoospore, which, germi- nating after its period of rest, produces, not a thread of cells but a variable number of zoospores from which the threads arise, it is regarded as an independent new sexual generation, so that we have in Ulothriz true alternation of generation. Dr. Dodel points out the affinity of Ulothrichee to Volvocinee and Hydrodictyee, but he is too prudent to dogmatize on the subject of classification. He holds, however, that the facts he has discovered afford strong support to the theory of evolution, as they show how (morphologically, of course) an asexual cell may become endowed with sexual properties. MicroscopicAL Contents oF ForEIGN JOURNALS. Archiv fiir Mikroskopische Anatomie, 13 Band, 4 Heft (continued from last number of ‘M. M. J.’)—On the Cell-formation which occurs in the Connective Tissue of Muscles, by Walther Flemming, This is a paper illustrated by three very good plates. It treats 306 NOTES AND MEMORANDA. exhaustively of the subject of the structure of the connective tissue. The author deals principally with molluscan structures, giving those of Mytillus edulis and Anodonta piscinalis very fully. He makes out connective tissue to be a far more complex structure than it is gene- rally believed to be, and his preparations, which are capitally drawn, bear him out. The preparations have been mounted in various ways. He has used, for example, alcohol, bichromate of potass, turpentine, glycerine, and osmium. For injections he has used Prussian blue and picro-carmine. The most important point he shows is that of the relation of the so-called schleim-cells. The memoir covers fifty pages. —There is also a short paper, by Herr Fr. Meyer, on preservative fluids for microscopic objects. Reichert and Du Bois-Reymond’s Archiv (January).—Carl Sachs describes and figures the terminations of nerve-fibres in certain ten- dons.—F. Boll’s article on the Savian vesicles found in the torpedo about the nasal orifices and between the external edges of the elec- trical organs and the limb-cartilages, is very interesting, because he demonstrates the existence in their epithelium of spindle-shaped cells corresponding in character to those so commonly found in special sense organs. The Zeitschrift fiir Wissenschaftliche Zoologie, vol. xxvi. part 2.—In this Herr Repiachoff continues his contributions on the Chilostomous Bryozoa, giving many interesting particulars about the development of the amphiblastic ovum of Lepralia and Tendra.—Herr Ludwig Graff describes the anatomy of the Sipunculoid Chetoderma nitidulum.— Dr. Hubert Ludwig writes on the interesting Gastrotrichous Rotifers, established as a separate order by Metschnikoff. NOTES AND MEMORANDA. Is Vision with the Microscope Finite or Unlimited 2—A paper on this subject appears in the ‘ Boston Journal of Chemistry, and is evidently written by one who is accustomed to microscopical re- search. We give it in full as follows:—The question of the limits of visibility is an eminently practical one, of great interest to all microscopists and physicists. On this question Mr. Sorby says: “ The highest powers of our best modern microscopes, he {Helmholtz ?] assumes, will enable us to see objects an eighty-thousandth part of an inch in diameter.” This sentence hardly represents Mr. Sorby’s posi- tion. After referring to Helmholtz’s principles of interference fringes, or diffraction, he says, “ It appears to me that we cannot do better than to adopt these principles in forming some conclusion as to the size of the smallest object that could be seen with a theoretically perfect microscope. Looked at from this point of view alone, with a dry lens this could not be less than one 80,000th of an inch.” This NOTES AND MEMORANDA. 307 passage, it will be at once seen, is limited to the “dry lens,” and while he says the “smallest object,” the context shows that he means the separation of lines, and nota single object, for he at once goes on to show that closer lines may be separated by the use of blue light and immersion objectives, and also says, “ The size of the smallest bright point that can be seen depends on entirely different considerations, and might be considerably less.” All these speculations of Sorby and Helmholtz (and Abbe may be included) are based on theoretically perfect microscopes. (In this case the ‘ microscope” means the objective, the all-important part of the instrument.) Now who ever saw a “theoretically perfect” microscope? Who can ascertain, that one is theoretically perfect? How can it be ascertained that one is perfect? The only possible way of measuring the approximation towards perfection is by the performance. So long as the per- formance of the best microscopes falls short of what a theory says is possible, the theory may be accepted as correct; but when the micro- scope has done more than theory says is possible, theory must be in fault. For years microscopes have been made, and are in use, that do more than Helmholtz’s theory will allow. The difficulty with Helmholtz and Abbe is that they had not seen and experimented, in 1872, 1875, and 1874, with all the microscopes that had been made at that time, but only with such German instruments as came in their way; and that made their theories to agree with the performance of those instruments. That the theories are wrong is proved by the fact that Nobert’s lines, finer than 112,000 to the English inch, have been seen repeatedly by numerous observers, whereas Helmholtz fixes the theoretical limit at 110,000. On the other hand, as yet no lines so fine as 114,000 to the inch have been seen. Nobert has ruled lines that he claims are 224,000 to the inch. Until something finer than 112,000 is actually seen, it must be an open question whether the failure is the fault of the microscope or of the ruling. Nobert him- self has not seen his own finer lines, and always pronounced it im- possible to see any finer than 80,000 to the inch, until he saw 95,000 to the inch with a Tolles’ immersion lens. The writer saw 90,000 to the inch with a dry lens more than ten years ago. As to the size of a single object which may be seen, there is but little known. The limit is undoubtedly in the perfection, or rather want of perfection, in the microscope. The best experiments in this direction have been made by Mr. W. A. Rogers, of the Cambridge observatory. Various writers have assigned different values to the angle at which an object can be seen, varying from 6” to 120”. This is, of course, a physio- logical matter. Mr. Rogers says, “ Even the smallest value named is much too large. I will at any time undertake to rule a single line one 30,000th of an inch in breadth, which can be seen the distance of seven inches from the eye. This corresponds to an angle of about 1”. Comparing minute particles of matter which can be seen under a Tolles’ ,1,th objective with those that can be measured, in the way indicated above, there is every reason to suppose that the limit of visibility falls beyond one 400,000th of an inch. But that light is of ‘too coarse a nature’ to enable us to see particles of matter as 308 CORRESPONDENCE, small as one 200,000th of an inch is a conclusion which can be re- futed without the slightest difficulty.” A few years ago Mr. Huxley said in substance, at a meeting of the London Microscopical Society, that if the opticians could not supply microscopes that would enable one to see spaces between objects one 100,000th of an inch apart, naturalists were at the end in that direction of their work. It was replied that American and London opticians had already supplied instruments that had separated lines but one 224,000th of an inch apart. CORRESPONDENCE. THe LATE Proressor Cu. G. Enrenpera’s RESEARCHES ON THE Recent AND Foss, FoRAMINIFERA. To the Editor of the ‘ Monthly Microscopical Journal.’ Srr,—The following observations on Dr. Ehrenberg’s researches may not be uninteresting to your readers.* Amongst the most enthusiastic observers and voluminous writers on microscopic organisms, Dr. Ehrenberg stands pre-eminent. By the end of the year 1838 he had reduced to order the multitudinous specimens of recent and fossil Microphytes and Microzoa which he had either collected, with Dr. Hemprich, in the East (Egypt, Dongola, Syria, Arabia, and Abyssinia), or had received from numerous corre- spondents. In the ‘Transactions of the Berlin Academy of Sciences’ for 1831, 1832, and 1838, Dr. Ehrenberg published the results of the researches made on Corals and associated animals by Dr. Hemprich and himself in 1823-25 among the islands and coral-banks, and along the coasts of the Red Sea. In this memoir, after reviewing the systems of classification adopted by his predecessors, he separated the Coral animals into Anthozoa (flower-animals) and Bryozoa (moss-animals) ; and the former he divided into Zoocorallia (comprising Polyactinia, Octactinia, and Oligactinia), and the Phytocorallia (comprising Poly- actinia, Dodecactinia, Octactinia, and Oligactinia). Altogether he enumerated 386 living species, of which 110 he had himself observed in the Red Sea. The range of Corals and their occurrence in the fossil were also noticed. The classification here alluded to has been superseded by others based on a still more intimate knowledge of the structure and phy- siology of the Celenterate groups—Hydrozoa and Actinozoa; whilst the classification of his “ Bryozoa” (Polythalamia,t Gymnocore, Thallopoda, and Scleropodia), mingling Foraminifera and Polyzoa, * These remarks are based on some critical notes on Ehrenberg’s species of Foraminifera in the ‘Annals and Mag. Nat. Hist.’ Ser. 4, vols. ix. and x. + Ebrenberg’s “ Polythalamia” (divided into Monosomatia and Polysomatia) consist of Forumimifera with some Polyzoa. CORRESPONDENCE. 309 could not greatly assist zoological investigation. Some interesting conclusions, however, were arrived at, valuable and true in the main,— namely, that the same kinds of Foraminifera occur both recent and fossil ; that, nevertheless, each set of strata has more or less decidedly its own special group of Microzoa ; and that Chalk in particular, and probably most limestones and calcareous marls, are largely composed of Foraminifera (Polythalamia, Ehrenb.). Thus these minute or- ganisms, with Coccoliths (Morpholites, Ehrenb., in part), appear to be the main constituents of the White Chalk. Although even recent forms of Microzoa are found in the Chalk, Ehrenberg warns us that these lowly creatures only go to prove that this, like many other calcareous rocks, is a “ Halibiolith,’ or marine deposit of organic origin; and not that the Cretaceous and Recent periods have been closely linked by identity and continuity of high grades of life.* Amplifying with his own increased knowledge the already published observations on the persistence of low orders of life, Dr. Ehrenberg, having studied some living Foraminifera of the North Sea, at Cuxhaven, contributed in 1839 an interesting memoir to the Berlin Academy, figuring two living species (Polystomella striato-punctata and Nonionina umbilicata) with great exactness, as well as some obscure forms, which he found in both the living and the fossil state} This memoir is given in English, with the original plates, in Taylor’s ‘Scientific Memoirs,’ vol. iii., art. xiii. In 1843 several highly magnified figures of minute recent Forami- nifera from America were treated of and illustrated by Ehrenberg in the Berlin Academy Transactions for 1841. Dr. Ehrenberg’s memoir “ On the muddy deposits at the mouths and deltas of various rivers in Northern Europe, and the Animalcules found in these deposits” { was noticed at large in the ‘ Quart. Journ. Geol. Soe.’ vol. i. p. 251, &c., as illustrative of the influence of microscopic life (chiefly Diatomacez) on recent and fossil stratified accumulations. Few can now recollect the astonishment with which geologists received in 1836 the assertion that large masses of rock, and even whole strata, are composed of the remains of microscopic animals and plants ;§ but this assertion has been confirmed and extended, largely by Ehrenberg’s further labours, and we now recognize many “ Halibiolithic” deposits and Diatomaceous earths. In the ‘ Abhandl. Berlin Akad.’ for 1847, many extremely minute Foraminifera, occurring in wind-dust on different occasions, in several parts of Europe, are described and figured. They form part of the curious gatherings of invisible things that wind-storms make and dis- perse in their whirlings over the surface of the earth,—sweeping the sea-shore, sand-bank, and dry river-bed, the volcano, the desert, and * ¢ Quart. Journ. Geol. Soc.’ vol. xxviii. pp. 122-124. + The late Mr. Thomas Weaver, F.R.S., in the ‘ Annals and Mag. Nat. Hist.’ 1841, and in the ‘ Philos. Mag.’ of the same year, gave a full abstract of two of Ehrenberg’s memoirs (read in 1838 and 1840) above mentioned, together with an appendix touching the researches of Alcide d’Orbigny on the Foraminifera of the Chalk of Paris. t From the ‘ Abhandl. k. preuss. Akad. Wissenschaft. Berlin’ for 1843. § ‘Proceed. Geol. Soc.’ vol. iii. p. 62. 310 CORRESPONDENCE. the ploughed field, for organic and inorganic particles, and winnowing its dusty harvest over distant and far different areas. These tiny Foraminiferal waifs, potent witnesses of the path and doings of the wind-storm, being figured by transmitted light only, like those of 1841, teach little as to genera and species. In these memoirs, and in shorter collateral notices in the ‘ Monats- berichte’ of the Berlin Academy of Sciences (namely, for 1838, 1840, 1844, 1858, &e.), Ehrenberg treated of numerous Diatomacee (“ Poly- gastrica”’*), Polycystina,} Foraminifera (“ Polythalamia”), Spongoliths, Geoliths, Phytoliths, and other microscopic organisms, which he had found, either recent (especially in the Red Sea, the Mediterranean, and the North Sea), or fossil in numerous deposits of various ages, such as the Mountain-Limestone, Oolite, Chalk, Tertiary, and Post-Tertiary strata. Some few of the recent and fossil species referred to in these memoirs were figured by him in the ‘ Abhandlungen’ for 1838 and 1839 ; but it was not until 1854 that Ehrenberg was enabled to fulfil his earnest and laudable desire to give to the world faithful and manifold portraits of the well-prepared and almost innumerable microscopic objects on which his published opinions had been founded. In 1854 the crowning of his favourite labour was accomplished in the publication of the ‘Mikro- geologie, with the recognition and aid of the State. In this grand work, beside multitudes of fossil Diatomacee, Polycystina, Spongoliths, &e., the long-looked-for Foraminifera were depicted, from his own drawings, with the best artistic skill, with loving care and right royal liberality. There are 4000 figures, in great part coloured, and all, except plate 40, magnified at least 300 times linear. With regard to the zoological determinations of Foraminifera, there is a great discordance between Ehrenberg and other Rhizo- podists; nevertheless, taking a broad view of the results of his labori- ous, if not accurately discriminative, work among the fossil and recent Foraminifera, we may fully acknowledge his having shown that several living species are also to be found fossil in Tertiary and Cretaceous deposits. Throughout the ‘Mikrogeologie’ there appear numerous persistent forms, belonging to the Cretaceous, Tertiary, and Recent periods, These his experienced eye readily detected; and in many instances his lists show their relationship ; but, for some occult reason, he failed generally to characterize them by description and nomencla- ture, though often grouped naturally on his plates. As with his classification of the Foraminifera among his “ Bryozoa” (1839), so with his ‘Mikrogeologie’ (1854), he failed to seize the clue to the right understanding and disentanglement of these many-featured Rhizopods. Ehrenberg’s truthful plates, however, supply the rhizo- podist with a storehouse of beautifully prepared specimens, mostly seen by transmitted light; and from these, for by far the most part, good and useful conclusions can be drawn, as from fresh specimens, except that, being viewed only as transparent objects, with but little * The “Polygastrica” of Ehrenberg, or “Infusoria,” comprise Jnfusoria, Diatomacee, Desmidiacee, and some Gromide. t+ Ebrenberg’s Polyeystina comprehend the Polycystina, Acanthometrina, and Thalassicollida of later authors, by whom the whole group is termed Radiolaria. CORRESPONDENCE. 311 perspective, and rarely with both faces of the shell, they too often fail to satisfy the student, though the artistic labour bestowed on them has been exact and conscientious. ( To be continued.) I remain, Sir, yours, &c., T. Rupgrr Jones. Mr. Arcuer’s Genus HyaLospHENta. To the Editor of the ‘ Monthly Microscopical Journal, READING, May 5, 1877. Sir,—Mr. Archer, in his “ Résumé of Recent Contributions to our Knowledge of Fresh-water Rhizopoda” in the current number of the ‘ Quarterly Microscopical Journal,’ refers “a lobose, monothalamian sarcodine” to the genus Hyalosphenia, instituted, with questionable propriety, by Stein, and accepted by Mr. Archer, though with obvious hesitation. Permit me to say that the so-called Hyalosphenia lata recently detected by E. Schultze is neither good as a genus nor new as a species, having been briefly described and correctly figured in your own Journal so far back as December 1870, under the name of Difflugia ligata by Yours truly, J. G. Tate. Lorp 8. G. Ossorne’s Exursrror. To the Editor of the ‘ Monthly Microscopical Journal.’ SIDMOUTH. Sir,—As I find that my former letter to you on the subject of an instrument to facilitate the exhibition of the Diatomacex, and other objects, requiring very oblique light when examined with high powers, has attracted the attention of some good observers, will you kindly permit me to offer a few more words on the subject, as I am anxious to prevent any disappointment to those who may try it. I find, and have informed Mr. Curteis, that all the apertures necessary, may be with ease cut on one disk. If a line is drawn through the centre of a disk, crossed by another at right angles, a good workman will with ease cut four apertures, one on each of these lines. They should be one-tenth of an inch from the point at which the lines intersect. If so cut, when the disk is revolved, each aperture will in turn come to the same position as regards the slide on the stage; they will not in any way interfere with each other. This plan saves a great deal of trouble, and enables the observer to try the effect of each aperture on any object, with the greatest ease, and no disturbance of any part of the instrument. I always now use four apertures so cut—a fine slit, and three triangles punched in different positions as regards the centre of the disk; in the case of each, taking care that their illuminated edge should be the one-tenth of an inch from the centre. It much facilitates the use of the Exhibitor, if, before this disk is 313 CORRESPONDENCE. put in over the small drum lens, the mirror is worked until it gives a reflexion of the lamp—strong on the edge of its diameter farthest from the lamp. I use as lamp, and most strongly recommend the following simple plan. On the sliding tube which carries the shade of an Acland lamp, I slide a tin shade blackened, covering the whole chimney. In this shade is a circular aperture opposite the flame, against which I fix an ordinary condensing lens; a tin cap slips over this with an aperture } inch in diameter, at the base of a cone projecting 2? inches ; at the mouth 1} inch in diameter. I have two small cones to pass into this, as diaphragms;-one with small circular aperture, the other a slit the size of the flame. I find it best to blacken all parts of the tinwork. I have given Mr. Curteis a drawing of the arrange- ment. I have, since I wrote to you, tested the power of the instrument in every possible way; it has never failed me. I can get diatoms bril- liantly illuminated on perfect black ground, and on any shade up to a soft grey light. With the 4 inch of Ross, the Type-Platten is a most beautiful study. With the highest objectives, I, with ease, get all the definition of which they are capable, with very little trouble. Let me add, I have arrived at the conclusion there are some— daily I read of more—individuals whose eyes must be constructed after a fashion very different from my own, and that of anyone I ever met with. Their crystalline lenses must have been by nature gifted with a power of correction which counteracts any and every short- coming in any object-glass. To them “the screw-collar” is a super- fluity ; they have a special visual power which adapts itself to the thickness of any covering glass. They have a peculiar power of penetration by their own eye-piece which supplements in the most extraordinary way the eye-pieces of the best opticians; to resolve a Pellucida into hemispheres with a + inch of Ross is an easy thing! IT must confess I envy these most highly gifted men. I have worked hard at Diatomacese with the best powers of the best makers. I have used good, expensive sub-stage illumination, as well as some months’ work with my own contrivance, I can make nothing of Pellucida beyond the beauty of its outline; I can with ease make out the longitudinal and transverse lines of the larger Rhomboides, with their intersection ; the small Rhomboides with some care gives me one set of lines well, the other faintly ; Crassinervis beats me. The best tests of good magnifying power with penetration for high powers, are, to my mind, good specimens of Versicolor and A. trilin- gulatus ; an object-glass which shows the full structure of these beautiful objects, I hold to be next to perfect, especially when seen on a black background. I shall be most glad if any of my brother microscopists are more successful than I have been with the Exhibitor; I shall be quite content if they meet with my own success. Nature has only given me the ordinary eye, now old; younger men of gifted eyes, may, for all I know, spot Pellucida with the Exhibitor; I shall hear of it with satisfaction, yet with envy. S. G. Osporne. Gezis.-) PROCEEDINGS OF SOCIETIES. Royat Microscorican Society. Kine’s CoLiece, May 2, 1877. H. C. Sorby, Esq., F.R.S., President, in the chair. The minutes of the preceding meeting were read and confirmed. A list of donations to the Society was read by the Secretary, and the thanks of the meeting were voted to the donors. The Secretary read the following letter, which had been received from C. J. Lambert, Esq. 3, QurEN SrreeT Puace, Upper Tuames STReet, Lonpon, April 24, 1877. Sir,—My father, by his will, left a sum of 25,0001, which he requested me to distribute among persons in his employ, and in gifts to scientific societies, in such manner as I should think fit. I have the pleasure to inform you that I propose appropriating to you, out of the legacy, a sum of 500/., and I enclose a legacy receipt, which I will thank you to sign and return to me, and I will then forward you a cheque for the amount. I remain, yours, &e., The Royal Microscopical Society, C. J. Lampert. King’s College, Strand, W.C. P.S.—I have been induced to appropriate this sum to your society at the suggestion of one of your Fellows, Mr. John Badcock. Co da He also stated that the money had been received by their Treasurer, and would be invested with the other property of the Society. He had only further to propose a special vote of thanks to Mr. Lambert for his munificent donation, and all would agree that their thanks were also due to Mr. Badcock for his very useful intervention. Votes of thanks were then put to the meeting, and carried by acclamation. The President said, that before proceeding to that for which they were more particularly assembled, it would be well for him to say a few words as to the origin of the series of lectures which they were about to inaugurate. It was something like two years ago that the Council of the Society resolved to institute a lecture, to be called the Quekett lecture, in honour of the late Professor John Quekett, and to be delivered from time to time by eminent microscopists; and it was thought that in memory of these occasions it would be “well to present to the lecturer the Quekett medal of the Society, for which dies had been some time ago prepared, but which had not hitherto been utilized. Various circumstances had intervened to pre- vent this arrangement from being carried out; but at length they were met together to hear the first Quekett lecture, which was to be 314 PROCEEDINGS OF SOCIETIES. delivered to them that evening by Sir John Lubbock, on whom he had great pleasure in calling. Sir John Lubbock, Bart., M.P., F.RS., &c., who was received with hearty applause, having expressed his sense of the honour conferred on him by the Council in selecting him as the first Quekett lecturer, proceeded to deliver his lecture “On some points in the Anatomy of Ants.” The subject was well illustrated by a number of coloured diagrams enlarged from microscopic sections and preparations, and also by a series of beautifully executed drawings, which were placed upon the table. The lecture will be printed in a future number. The President was quite sure he should express the wish of every one present in proposing a hearty vote of thanks to Sir John Lubbock for his very interesting and instructive lecture. He had himself listened to it with very great pleasure, and had no doubt that it had been listened to with equal pleasure by all who were present. He therefore proposed that they should all join in a vote of thanks for the very able lecture which they had been privileged to hear. Mr. Charles Brooke said that he also had been very much inter- ested by the lecture, and greatly pleased with the very able manner in which the anatomical structure of so minute an animal had been described. He hoped that, as time went on, their learned lecturer would be able still further to follow out his interesting subject, and that they might hope to hear some more of the results of his inves- tigations at a future date. He had very great pleasure in seconding the vote of thanks to Sir John Lubbock. The vote of thanks was then formally put to the meeting by the President, and carried by acclamation. The President said that he had now the pleasing duty to perform of presenting the Quekett medal to the lecturer of that evening ; and, addressing Sir John Lubbock, he expressed the very great pleasure he had in presenting it to him in the name of the Council and of the Fellows of the Society; and he could not help expressing also his gratification at the opportunity thus afforded of doing honour to one whom it was his privilege to regard both as a personal friend and as a man of science. Sir John Lubbock, in reply, assured the Council and the Fellows that he felt very highly the honour conferred upon him in having been requested to deliver this lecture. He should preserve the medal with some degree of pride, and his family would preserve it as a much-prized memorial of the proceedings of that evening; and he would further say, that if anything could enhance its value in his esti- mation, it would be the fact of his having received it from the hands of his highly esteemed friend, the honoured President of their Society. Scientific Evening, April 3, 1877. Exhibitors and Objects. The President, H. C. Sorby, Esq.: Specimens showing the appli- cation of the microscope to the determination of the index of refraction of minerals. Remarkable characters of double refracting crystals. PROCEEDINGS OF SOCIETIES. 315 Mr. J. W. Bailey: A folding microscope of new pattern. Mr. Charles Baker: Lord G. 8. Osborne’s new diatom exhibitor. Messrs. R. and J. Beck: Pleurosigma formosum upon a black ground, with an achromatic eye-piece and patent achromatic con- denser. Surirella gemma, with ;4, immersion with central stop and patent condenser. New form of small microscope, with concentric rotating stage, &c. Large portable microscope, with apparatus and objectives complete. Mr. Badcock: Megalotrocha albo-flavicans, &c. Mr. John Browning: Absorption spectrum of bromine. Mr. Charles Collins: Young hippocampi in four stages of develop- ment. Mr. Henry Crouch: Vegetable preparations double stained by Dr. J. G. Hunt, of Philadelphia. Mr. Encch: British trap-door spider, Atypus sulzeri, and spinnerets of spider. Mr. F. Fitch: Some very beautiful natural mounts of insects. Mr. W. H. Gilburt: Asplemium bulbiferum, stained. Mr. J. W. Goodinge: Pleurosigma angulatum, with .. Dr. Gray: Rare diatoms from Santa Monica. Mr. H. Hailes: Foraminifera, Spirillina vivipera var. Magaritifera and Chilostomella ozizeki, &e. Messrs. J. How and Co.: Dolerite intrusive in granite, trachytic lava, and carboniferous limestone. Mr. Thomas Howse: Peziza bicolor alive, and a section of the seed of Oollomia grandiflora, showing delicate spiral threads which surround the testa. Dr. Lawson: Transverse section of human spinal cord, and Mi- crosporon furfurans, a fungus that attacks the hair and skin. Mr. W. G. Lettsom: Decomposed glass from Pompeii, mounted by Sir David Brewster ; and a section of a Cornish mineral which shows the bands due to Didymium. Mr. R. T. Lewis: Rheea fibre under the microscope. Mr. 8. J. McIntire: Eye of drone-fly. Dr. Millar: Mylinsia Zittelli and M. Grayii, recent representations of ventriculites. Mr. Moginie: Living organisms. Mr. 8. Norman: Spicula of Dendrospongia Sturii, human brain, and precious opal. Mr. Thomas Palmer: Micro-spectroscope and chemical changes in substances. Mr. W. W. Reeves: Young crinoid larve of Antedon on Bugula flabellata from Torbay, lent by Major Lang. Mr. Sigsworth: Section of hoof of the horse, showing the papille. Mr. H. J. Slack: Section of fossil bone from Tilgate Forest, and bulbs of Krupp’s silicate cotton. Mr. Charles Stewart: Ovary of Dorocidaris papillata and Asper- gillus glaucus. Mr. Amos Topping: Injected drum of ear of frog ; ditto lung of frog; and ova of ditto, in different stages of development. VOL. XVII. Qa 316 PROCEEDINGS OF SOCIETIES. Mr. F. H. Ward: Section of corn from toe, cornea of pig, and Toenia grandis, stained. Mr. Tuffen West sent some very beautiful drawings of the fol- lowing objects. List of Drawings. Zoea, from Indian Ocean. Sarcopsylla, from fowl, Ceylon. Nyc- teribia, vampyre bat. Nycteribia, details. Nycteribia, winged, from Ceylon. Larva, Meloée. Acadus destructor. Acadus plumosus. vie os ‘4 287 = Sot ae, Gd = , ELIT