LETTERS TO THE EDITOR [The Editor does not hold himself responsible for opinions expressed by his correspondents. Neither can he undertake to return, or to correspond with the writers of, rejected manuscripts. No notice is taken of anonymous communications. [The Editor urgently requests correspondents to keep their letters as short as possible. The pressure on his space is so great that it is impossible otherwise to ensure the appearance even of communications containing interesting and novel facts.] The Gulf-Weed (Sargassum bacciferum) a Means of Migration for Fishes and Marine Invertebrates OWING to the October number of NATURE having been mislaid, I have not had an opportunity until lately of seeing Mrs. Merrifield's remarks upon Gulf-weed which appear in vol. xviii. p. 708, where the Bermudas are alluded to as a locality where this species grows in situ. Having during my several visits to those islands of late years paid some attention to the Sargassum and its inhabitants, perhaps the few facts I am in possession of may prove interesting to botanists, and those who study the geographical distribution of marine animals. The Bermudas, being situate within that somewhat circular area of the North Atlantic, formed by the currents of the Gulf Stream, the North African, and equatorial currents, within which exists that vast accumulation of weed known from the time of Columbus to the present day as the "Sargasso Sea," afford excel lent opportunities for studying the plant in its floating condition, and also adherent in its natural state to the reef. During the winter months the prevailing gales, which are generally from south-east to south-west, bring to the islands large fields, as well as isolated patches, of the Gulf-weed, which prove a great boon to Bermudan farmers, who, but for this ocean waif, would often be minus manure sufficient to raise their root-crops with. To an observer a field of weed coming in from sea presents a somewhat variegated surface as regards colour, the major portion of it being of a dark brown, interspersed with spots and patches of light yellow. On closer inspection, these masses of floating weed are found to be inhabited by various species of pelagic and littoral crustaceans, particularly a small light brown crab, having a blotch of white on the carapace. Here and ❘ there the eye rests on a little pearly-white object, the well. known shell of that almost unknown cephalopod, Spirula prototypus, of Peron. The pretty purple shell of Ianthina communis is also to be seen, as are the singular forms of those truly oceanic acalephs, Valella communis and Physalia pelagica, which occasionally occur in large numbers, as they did during a heavy southerly gale on April 16, 1861, when countless myriads were literally wrecked upon the shores, together with the shells and rafts of Ianthine. About the margins of these floating fields, which are of some depth, may be seen various species of fishes, most of which have, no doubt, accompanied the fields, and lived in them, as game would do in a preserve where food and shelter are found. There is one species of fish which, above all others, seems to belong to the Sargassum, viz., the Marbled Angler (Antannarius marmoratus), which, from its peculiar arm-like pectorals, is specially fitted to rest upon the weed. Here it makes its wonderful nest amidst the mass, suspended by means of those silk-like fibres, which prove amply strong enough to support the large bunches of eggs, which hang like grape clusters within their orbicular case. These nests are occasionally to be found, but cannot be considered common; and only a few have been obtained from the weed on the Bermudan shore. There is hardly a doubt that it is from this fish-preserve in mid-Atlantic that those tropical and semi-tropical forms which occur incidentally at the Bermudas, Azores, Canaries, Madeira, and also on the east coast of America, come, for I have frequently obtained from these masses of gulf-weed, species which are not recognised as Bermudan, and would probably never have visited the island waters unless under the friendly shelter of the weed. Moreover, I have observed even in heavy storms that the sea never breaks throughout these floating fields, but although heaving and swelling to the usual height, ght, remains unruffled just if oil floated on the surface. This absence of disturbance would of itself commend the field of weed to the fishes; but when we consider other suitable adjuncts, such as supply of food, and shelter from enemies, we cannot fail to realise the excellent means of migration which this common possession affords, not only to fishes, but to all kinds of those lower invertebrate forms, as many of which have most certainly been brought to the shores of the Bermudas by this means. The isolated patches of weed, which follow the course of the Gulf Stream, and become broken into lesser fragments, are also accompanied by those tropical and semi-tropical fishes which are found almost every summer on the coast of Nova Scotia; and even as far north as Newfoundland; and it is evident that without some such agency we could never account for the abundance of certain southern pelagic fishes which annually occur in our high latitude. In regard to the original habitat of S. bacciferum, as also the origin of that vast mass of floating weed which exists in midAtlantic, and is wholly composed of this species, I fear we must await further oceanic exploration. Although I am well aware that it grows in certain places on the Bermuda shores, those shores, even if they were wholly clothed with it, could not supply a tithe of the material which forms the vast accumulation of the weed existing in the Sargasso Sea. As to the allusion in Mrs. Merrifield's paper (quoting Agardh), made concerning the S. bacciferum being an inhabitant of the banks of Newfoundland, and other parts of the coast of north-east America, I can safely say that it is wholly unknown on this coast, save occasional sprays, which are brought north by the Gulf Stream, as are the fishes I have before alluded to. Halifax, Nova Scotia, January 25 J. MATTHEW JONES The Highest Tide on Record IN Lyell's "Principles of Geology," tenth edition, 1867, vol. i. p. 494, occurs a statement, given on the authority of Admiral Sir F. Beaufort, to the effect that the tides at Chepstow on the Wye sometimes rise to 69 and even to 72 feet. The statement is familiar to all who have read Lyell's work. If it be correct then this tide of 72 feet at Chepstow is apparently the greatest in the world, that in the Bay of Fundy being given as 70 feet in the extreme. I can find no authority for a tide so great as 72 feet at Chepstow other than that above cited. The old "Bristol Channel Pilot" books of 1821 and 1839 say nothing of the matter, as I am informed by Capt. Tizard, R.N., and the latest published "Pilot" gives 56 feet as the extreme rise of tide at Chepstow. There is thus no official knowledge of so high a tide as 72 feet, and I can find no published account of Admiral Sir F. Beaufort's observations; Sir C. Lyell refers to none such. I should be extremely obliged to any reader of NATURE who can refer me to any certain record of exceptionally high tides at Chepstow and confirmation of Sir C. Lyell's statement. There seems to be some uncertainty as to whether the highest tides on record occur in the British Islands or not. H. N. MOSELEY Exeter College, Oxford The Glacial Period and Geographical Distribution PROF. ASA GRAY, in his very interesting lecture on the distribution of the forest trees of the northern temperate region (NATURE, vol. xix. p. 327), after pointing out the remarkable differences that exist between the forests of the eastern and western sides both of North America and the Old World, suggests that the great poverty of the European as compared with the Japan-Manchurian region in this respect was caused by the Mediterranean cutting off the retreat of the flora which then occupied Europe, as it retired, at the approach of the glacial epoch, before the ice from the north. This explanation derives considerable support from some other facts in geographical distribution. The most characteristic Alpine and Arctic butterflies of the Palearctic region belong to the three genera, Parnassius, Chionobas, and Erebia. Of Parnassius, Dr. Staudinger, in his latest catalogue (1871) enumerates fourteen Palæarctic species, of which three occur in North and Central Europe, ranging as far south as the Balkans, but always in or near high lands, about a dozen occur in temperate Asia, ranging as far east as the Amur, and probably as many in North America, where they also are truly Alpine butterflies. Of Chionobas one species (C. aêllo, confined to the Alps) occurs in Central Europe, whilst six or seven others range from Lapland over Russia and Siberia, Mongolia, &c., to the Amur, and there are numerous species in Arctic and Alpine North America. Of Erebia there are fortyfive Palearctic species enumerated by Staudinger, and of these no less than twenty-five occur in the central Alpine chains of Europe. The genus likewise ranges all over temperate Asia, going as far south as the Himalayas and Moupin, and in North America is represented by a dozen or more species. Now, though an Erebia (E. Tyndarus, var.) occurs as far south in Europe as the Sierra Nevada, not a single species of any of these three genera occurs in North Africa, although the Atlas Mountains would seem eminently well suited for such Alpine insects. In this case, then, it seems clear that the same cause the barrier of the Mediterranean-which in the case of the miocene flora of Europe prevented any further retreat south, has operated to prevent any similar southerly spread amongst the victorious invaders from the north which pressed on the retiring host. With regard to the general similarity in facies and richness between the East American and East Asiatic tree-flora, certain facts pointing in the same direction will at once occur to the zoologist. Thus the Menopomas of the Ohio and Alleghany have their only near relations in the gigantic Sieboldias of north-east Asia, one species of these occurring in Japan, the other being one of Père David's discoveries in Moupin. Similarly with the genus Polyodon amongst ganoids. Only two species of this genus are at present known, P. folium, inhabiting the Mississippi, P. gladius the Yang-tse-kiang. The recent discovery of at least two species of Scaphi rhynchus in Turkestan makes it probable that ere long species of that Americo-Asian genus will be found in the Chinese rivers as well. The parallelism in the case of the salamanders is particularly interesting, when one remembers the celebrated Andrias Scheuchzeri of the Eningen beds, and it tends to favour the view that at that time practical identity in the forms of animals and plants reigned throughout the northern temperate zone. W. A. FORBES Cambridge, February 14 P.S.-The reported discovery (NATURE, vol. xix. p. 351) of a true alligator in the Yang-tse-kiang, will, if confirmed, add a still more remarkable case to those mentioned above. Leibnitz and the Royal Society THE experience of "P." as given in NATURE, vol. xix. p. 315, is physiologically interesting, and by no means usual. Before attempting an explanation it may be as well to assume that only one of "P.'s" ears was affected by the disorder, as by this hypothesis we get the greatest possible divergence from the healthy state. It would have been easy to ascertain which was the faulty organ at the time by requesting a musical friend to listen while "P." vocalised the note of the tuning-fork as conveyed to him by each ear separately. The discordant ear would then have been revealed. The fault of hearing must have been due either to some mechanical misadjustment of the auditory apparatus, by which a wrong sensation was conveyed to the brain, or else to some deep-seated brain or nerve lesion, which led to a faulty conception of the original sound. Let us consider briefly the first of these cases. From the exceedingly scanty description of his disorder given by "P." I gather that the discord was mostly conspicuous when the note was high pitched (such as when whistled). Now it sometimes happens from paralysis of the chorda tympani nerve, or even from occlusion of the Eustachian tube, that the tension of the ear-drum is preternaturally increased. Such affections, as aurists well know, frequently intensify to a distressing degree the hearing of high pitched notes, whilst they correspondingly diminish the sound of the lower tones of the chromatic scale. This result is probably obtained by the fact that the tense membrane responds more readily to the rapid vibrations of the higher tones than it does to those of a slower rate. We must also remember that the power of lessening the tension of the membrane is in such cases very seriously impaired, and, as a consequence, the power of adjustment also. I do not suppose that in PROF. TAIT and myself ought not to be at issue on this ques- p's" case there was any actual paralysis of the tympanic tion. I suppose we both want to get at the facts; and, for my part, I have no more desire to whitewash a foul reputation than he can have to blacken a fair one. Where we differ appears to be, as to how far Leibnitz's reputation can stand the test of facts. The question, however, is not whether Leibnitz acted disingenuously in respect to Gregory's series, or any other subordinate matter, but whether he was indebted to something of Newton's, surreptitiously imparted to him, for his differential calculus. If the grounds upon which that charge was made are swept away, there is an end of it. But if, on the other hand, that is not found feasible, and evidence to character becomes a factor in the final decision, then it is right to examine into those subordinate matters. Till then, I, for one, decline to touch them. At the same time let me say that I never undertook to be bail for Leibnitz's impeccability. All I said or say is, that on the published facts I believe that Leibnitz was led to the calculus by his own honest speculations, and had not the means of stealing from Newton, had he been that way disposed. But there are so many relative papers still unpublished, but publishable, that it is impossible to arrive at a true decision till at least some of them have been submitted to an authorised tribunal. Prof. Tait recommends me to repeat the fruitless attempt of Dr. Slowman. I decline to follow the example of that ominously surnamed savant; for it is contrary to precedent that the pursuer should ask the defender to show his hand; and I am quite sure that "the proper authorities" abroad have too much sense to take the initiative. So I appeal to the Council of the Royal Society of 1879 (not that of 1712, as Prof. Tait gives it), and I do so for these two reasons : 1. The so-called Commercium of 1712, which was merely a statement, arriving at no decision on the principal question, contained several allegations (apparently inconsistent with known facts) which give colour to the charge against Leibnitz; it is then an obvious duty on the part of the Royal Society, who were on the occasion represented by the Committee, to give the proof, or make the reparation. 2. The first-published charge against Leibnitz, which was made by Wallis in 1695, was based on allegations said to have been derived from papers and letters in the possession of the Royal Society; it is but fair, then, that those papers and letters should be published. I therefore once more respectfully urge upon the Royal Society to reopen the main question, and publish such of the relative 66 muscles, but it is just possible that there may have been a certain degree of misadjustment of the drum of the affected ear due to a feeble and imperfect contraction of one or the other of the muscles referred to. If the disorder was, as I surmised, accompanied with great tenseness of the membrane, the laxator We might, I believe, tympani would be the faulty muscle. under such circumstances, expect the ear-drum to vibrate discordantly in response to a note, for Helmholtz's experiments with stretched strings would suggest that this is feasible within certain limits. As a matter of fact this discordance is rare, and therein rests the interest of "P.'s" case. I can scarcely believe that in his case any of the deeper structures of the ear were seriously implicated, otherwise he would hardly have made such a rapid and complete recovery as he did. Brighton, February 10 W. AINSLIE HOLLIS YOUR correspondent "P." (NATURE, vol. xix. p. 315) desires an explanation of the phenomenon of alteration in the pitch of sounds, which he has experienced in his own person whilst suffering from temporary deafness. Your second correspondent on this subject, Dr. Wallich (p. 340), was under my observation at the time of his experiencing the same peculiar and comparatively rare aberration, and I was able myself to verify his statements. I propose with your permission to give an explanation which appears satisfactory to myself, and hope it may be so to your correspondent "P." Persons suffering in this way find that sounds heard by the affected ear appear to be sharper or flatter than their true pitch as heard by the other ear, and hence a sound may even appear double. The internal ear, or labyrinth, must be the part affected, and in all probability it is the cochlea which is at fault. Now most authorities are agreed that the pitch of a sound is appreciated by the cochlea in the following manner. Each tone, or division of a tone, has its corresponding portion on the spiral lamina of the cochlea, which under ordinary circumstances can only be affected by that tone. So that the sound-wave produced by a certain tone passes along the keyboard (as it were) of the spiral lamina until it reaches its own key, which it strikes or so affects as to cause an impression to be sent from that portion of the lamina to the brain. Hence the appreciation of variation in the pitch of sounds. Feb. 20, 1879] NATURE This theory being accepted ccepted, for an explanation of the aberration in question we have only to suppose some slight physical alteration in the contents of the cochlea, which would cause the sound wave to strike or affect the wrong portion of the lamina spiralis, and thus a false impression would be carried to the URBAN PRITCHARD brain. Now attention is drawn to the above allow me to give another experience. On two separate occasions while playing the English concertina, and more particularly when single notes or simple chords were struck, I noticed that each was followed by a loud and distinct note an octave lower which appeared to be that of its fundamental tone. The musical tones of the voice of any person addressing me, also, had their deeper reverberations in a similar manner, these being numerous and of rapid succession; the confusion arising was very like that which is heard in a hall unsuitably constructed for sound. The nuisance, for such it amounted to, I was troubled with for a couple of days each visitation, the abnormal state of hearJOHN HARMER ing being peculiar to the left ear only. Wick, near Arundel Intellect in Brutes THE following case will perhaps interest those who believe that the reasoning faculty in man and animals differs in degree only, and is essentially the same in kind. Some years ago a plumber told me that he had, on several occasions, been called in to examine into the cause of leakage of water-pipes under the flooring of houses, and had found that the rats had gnawed a hole in the leaden pipe to obtain water, and that great numbers of them had made it a common drinking-place, as evidenced by the quantity of dung lying about. The plumber brought me a piece of leaden pipe, about inch in diameter and inch in thickness, penetrated in two places, taken by himself from a house on Haverstock Hill. There are the marks of the incisors on the lead, as clear as an engraving; and a few hairs and two or three of the rats' vibrissæ have been pinched into the metal in the act of gnawing it. This crucial proof of brute intelligence-a rat will not drink foul water-interested me so much, that I ventured to send an account of it to Dr. Chas. Darwin, asking his opinion on the means by which the rats ascertained the presence of water in the pipe. To this he replied: "I cannot doubt about animals reasoning in a practical fashion. The case of rats is very curious. Do not they hear the water trickling?" It may be conceded that this explanation is the most probable, and if it be the true one we have an example of an animal using his senses to obtain the data for a process of reasoning, leading to conclusions about which he is so certain that he will go to the trouble of cutting through a considerable thickness of lead. Obviously man could do no more under the same conARTHUR NICOLS ditions. OUR ASTRONOMICAL COLUMN The Companion OF ALGOL. There are grounds for suspecting that the light of the small star about 80" distant from Algol in the S.P. quadrant is also variable. Schröter in his letter to Bode, wherein he first drew attention to this object, mentions that he detected it with a 7-feet reflector on October 12, 1787, and although small it was distinctly seen. Soon afterwards he estimated its ness distance from Algol at 1' 30". On April 9, 1788, the star was not to be found, and he therefore concluded that it must be variable. In 1792, when he was in possession of a 13-feet reflector, which he describes as the most powerful instrument then available in Germany, he re-examined the vicinity of Algol, and on March 9 saw the companion much brighter than before, and compares its distinctness in the larger telescope with its faintness in the smaller one with which he had discovered it. But on April 5, in a state of atmosphere at least as favourable as on March 9, with the same instrument and magnifying power, not the slightest trace of the companion could be perceived; on increasing the power to 370, with the utmost straining of the eye, the faintest glimmering was now and then pected in its position. Schröter then, in this second com sus munication to Bode, expresses himself more confidently as to the variability of the small star. In the early part of the year 1874 the writer of these lines made several ineffectual attempts to observe the companion, using various powers on a 7-inch refractor; though the skies were favourable enough, nothing could be glimpsed in its place. It was not therefore without surprise that upon re-examining the vicinity under similar conditions on September 9 of the same year, the companion was caught at once, and seen with great distinctness. It was measured with Mr. J. G. Barclay's 10-inch found to be 194°4 and the refractor at Leyton, by Mr. Talmage, on October 2 following, when the angle was 1835 is recorded, but his distance distance 79" 02; the magnitude was estimated 11.12. An observation by Smyth in is much too small; it is not stated whether he found the companion himself or whether his knowledge of its existence was due to Schröter's communications to Bode. It does not occur amongst the objects in the "Bedford Cycle," which were re-measured by Secchi. While upon the subject of variable stars we may just mention that ، Andromedæ, to which attention is directed in the last number of the Monthly Notices of the Royal Astronomical Society as "a new variable star," is no novelty: we referred to the star as almost certainly entitled to insertion in the catalogues of such objects, four years since (NATURE, vol. xi. p. 308). "A MISSING STAR."-From a letter addressed by Prof. C. H. F. Peters, Director of the Observatory, Clinton, New York, to the Superintendent of the Naval Observa tory, Washington, which Admiral Rodgers has communicated to the Astronomische Nachrichten (No. 2240), it appears that he has strangely misinterpreted a note with the above heading, which was lately printed in this column. We referred to an object observed at Washington, with Hygeia in 1850, and afterwards sought for at that observatory and elsewhere on the assumption that it might possibly have been a trans-Neptunian planet, and in view of the failure of a careful search on this hypothesis, we remarked: "the only likely explanation appears to be that there was a variable star in this position, and that the observations in right ascension were affected with greater error than might be expected, considering that on two of the days of observation several comparisons were made." Prof. Peters, however, explains the difficulty by referring several transits to the first instead of to the second wire of the movable plate of the micrometer employed, in which case the star is identified with Lalande 36613, and Prof. Hall has found, on examining the original observing-books, that Mr. Ferguson had altered several correct observations to correspond with erroneous ones, and Admiral Rodgers accepts the explanation as satisfactory. But Prof. Peters is alarmed about the matter now that NATURE "stirs it up again," and writes to the Superintendent of the Washington Observatory "in order that nobody thereby might be induced to spend months and years upon a renewed search," and to "stop any further perpetuation of the credence, that a trans-Neptunian planet is revealed by the Washington Observations." be seen that our suggestion was that a variable star might exist in the observed position, and was in no way connected with a renewed search for a trans-Neptunian planet. Prof. Peters must entertain rather odd notions as to the probable knowledge of his astronomical confrères respecting the contents of the ecliptical region of the sky, if he believes that any one would be induced, by remarks that we might offer, to undertake in these days a search for a distant planet close to the ecliptic amongst stars of the ninth magnitude! It will COMET 1871 V.-Dr. B. A. Gould, with his usual energy, has secured an excellent series of post-perihelion places of the comet discovered by Dr. Tempel on November 3, 1871, which in a fortnight's time sank below the European horizon. The discussion of these observations in conjunction with those made in the northern hemisphere, will lead to a much more precise knowledge of the orbit than we have at present. OLBERS' COMET OF 1815.-In a recent note upon this comet it should have been stated that, acting upon the wish expressed by Olbers at the time, Triesnecker printed his observed differences of right ascension and declination between the comet and comparison-stars in Zeitschrift für Astronomie, vol. ii. The Vienna observations, therefore, admit of a new reduction, in addition to those previously named. are referred to, which show marked differences in the diurnal variations of the barometer at places quite near to each other, as Greenwich, Kew, Oxford. It is remarked especially that the forenoon maximum in the months of May to July occurs near 9 A.M. at Greenwich, and near 8 A.M. at Kew; while at Falmouth and Valentia it is delayed to 11 A.M., or noon, and occurs in June as late as 2 P.M. at Helder. Having made several investigations relatively to these questions (which I have not been able to publish as yet in detail), I think it may not be without advantage to give at present conclusions relating to the results above noticed. It is obvious that it is of the highest importance with relation to the research as to the cause or causes of the remarkable semi-diurnal oscillations of the barometer, that we should have only real variations of atmospheric pressure to deal with, and not instrumental irregularities; and that, if there is any part of the mean diurnal variations which is due to local causes, we should be able to separate that part from any other which may be due to general or cosmic causes. When it is remembered that the range of the mean diurnal variation with us is from two to three hundredths of an inch of mercury, and that the epochs of maximum or minimum may be shifted an hour by a difference of one or two thousandths of an inch, it will be seen how essential it is that the instruments, the observations, and the corrections shall be the best, in order to be sure that we have real variations of atmospheric pressure before us. In order to obtain the best possible results, my investigations have been limited to observations made in firstclass observatories with standard instruments. From observations made during several years at Makerstoun, Dublin, Greenwich, and Brussels, I have sought by the harmonic analysis the functions of sines which represent them most accurately. I give here the equations for the means of the three months in question-May, June, and July. The variation, v, is in ten-thousandths of an inch of mercury; the origin for each of the four stations M, D, G, and B, is mean midnight (0 = 0): M, v = 56 sin (+ 355°) + 68 sin (2 + 1430) + 21 sin (39 + 1710) The terms on the right of each equation represent the oscillations, whose superposition completes the whole diurnal variation. We find From the Ist term that the epochs of the maximum and minimum were the same within a few minutes at M, D, and B (as shown by the arguments 355°, 358°, and 354°), differing at Greenwich from the others by about 40m. From the 2nd term, that of the semi-diurnal oscillation, The exact agreement in the epochs of maxima and minima and the regularity of the variation of range with latitude in the semi-diurnal oscillation show that this oscillation obeys a general law. Dr. Lamont has supposed that the Ist term, or single oscillation, is due to variation of temperature; this, I believe, is not the case. When we compare the terms for different seasons of the year, we find that for the same place the epochs of maximum and minimum may vary twelve hours in the single oscillation, while the epochs deduced from the same term for the temperature variations do not differ one hour. Not only so, I have found on the South Indian Ghats that the epochs deduced from the Ist term of the barometric equations vary seven hours in ascending 6,000 feet; while those shown by the 2nd term are absolutely constant. For all these reasons I conclude that the semi-diurnal oscillation of the atmospheric pressure is due to a cosmic cause, independent of local influences, while the single diurnal oscillation shows that part of the solar action which is modified by atmospheric conditions yet to be determined. The results for the four stations just given are a few links in a long chain of facts which tend to prove that the semi-diurnal oscillation of the barometer is due to an action of the sun, which is repeated equally, twice in each day, like the solar oceanic tide. It will be seen, I think, from the results obtained from the Brussels, Greenwich, Dublin, and Makerstoun observations that the differences noticed at the beginning of this article cannot be allowed to enter as data into the domain of meteorology without much greater study of all the circumstances on which they depend. The facts of atmospheric variations are very difficult of explanation, but if we begin to admit results which may be purely instrumental among these facts explanation will become impossible. It is a fact that the true temperature of the mercurial columns has not always been obtained, and when we have to discuss observations with self-registering instruments, many sources of error, including those of temperature on the apparatus itself, have to be cared for. At stations near the sea, such as Helder, Valentia, and Falmouth, we have also to remember that in the varying height of the partial base of the atmosphere, through the solar oceanic tide, there is a real cause of diurnal barometric oscillation whose amount and epochs should be ascertained and deducted before exact comparisons can be made with observations inland. At the same time I would remark that of the stations here considered Dublin is near the sea, while the others are more or less distant from it. JOHN ALLAN BROUN MAROCCO AND THE ATLAS THE expedition of which an account is given in this most interesting volume was undertaken by Sir Joseph Hooker and Mr. Ball in the spring of 1871, and lasted a little over two months. Many causes comThe observations here studied at the four observatories are all made by the eye. 2 Journal of a Tour in Marocco and the Great Atlas." By Joseph Dalton Hooker, K.C.S.I., C. B., Pres. R.S., Director of the Royal Gardens, Kew; and John Ball, F.R.S., M.R.I.A. With an Appendix, including a sketch of the Geology of Marocco, by George Maw, F.L.S. (London: Macmillan and Co., 1878.) Feb. 20, 1879] NATURE bined to hinder the publication of this journal until now, but the delay will, we feel sure, not in the least detract from either the novelty or value of its contents. The coast-line of the territory of Marocco extends from the frontier line of Algeria on the Mediterranean, along through the Straits of Gibraltar to the Atlantic Ocean, nearly opposite to the Canary Islands. Inland it would seem to have no absolutely well-defined boundary-line except towards Algeria, but it is supposed to stretch far into the Great Desert on the southern side of the Great Atlas range. Of this great region, possibly as large in extent as Spain, and the chief ports of which are within a few days' steaming of Southampton, almost nothing, if we except the 'mere coast-line, is known; and a journey across the dark continent itself seems easier of accomplishment than one to the town of Tarudant, in the southern valley of the Great Atlas. The distance from Gibraltar to Tangiers is scarcely thirty-five miles. The five peaks of the Beni Hassan are seen from the Rock, yet we have no records of their having been investigated, and when the authors earnestly desired Sir John Drummond Hay, the British Minister Plenipo- P Argan Trees. tentiary in Marocco, to assist them in exploring their recesses, he was reluctantly obliged to pronounce against the feasibility of any such excursion, and even when they started for a short excursion to Cape Spartel it was considered prudent to give them an escort of two soldiers. With this excursion the botanical interest of this journal begins. Plants of many sorts were seen and collected. Where a little slender stream ran through some damp meadows they were charmed by the delicate tint of a pale blue daisy that enamelled the green turf. It was merely a variety of the little annual daisy (Bellis annua) so common in many parts of Southern Europe; but the blue tint does not seem to have been noticed elsewhere. The botanical district to which this northern corner of Marocco belongs has been called that of the cistus and heath. One very interesting plant to be often seen living in the Botanical Gardens of Kew and Dublin is thus described: "The most singular of these is the Drosophyllum lusitanicum, a plant of the sun-dew tribe, whose branched stem bears several large yellow flowers. The numerous slender strap-shaped root-leaves, nearly a foot in length, that are gradually contracted to the thickness of whipcord, are beset with pellucid ruby-tipped glands, and present a peculiarity that appears to be unique in the vegetable kingdom. Any one who has remarked the growth of ferns must have seen that in the young state the leaves are rolled or curled inwards, so that in the process of unfolding the face or upper side of the leaf, which was at first concealed, is gradually opened and turned to the light. A similar process occurs in many other plants; but in Drosophyllum alone, so far as we know, the young leaf is rolled or curled the reverse way, so that the upper side of the leaf is that turned outwards. It appears to grow in many parts of Southern Portugal; reappears on the north side of the Straits of Gibraltar near Tarifa and Algeciras, and on the southern side about Cape Spartel and on the hills above Tetuan, where it commands a view of the opening of the Mediterranean, but extends no farther eastward." Tetuan was visited from Tangiers. The season (April 10) was scarcely far enough advanced for the flowering of many of the sea-side plants, "but there was more than enough to rejoice the heart of a botanist, especially one escaping from the ghastly spring season of the north, where, when the days grow longer, they become only the more dreary, and where the bitter east winds parch and blast the young leaves and blossoms that are tempted to unfold themselves to their own destroying by the mildness of the winter weather." At Tetuan, Beni Hosmar was ascended. It was about 3,000 feet high, and had not been ascended by any European since Barker Webb's time. The season was still too little advanced, and the botanist who will follow the travellers' profootsteps about the beginning of June is mised a much richer harvest. Ceuta, about thirty miles from Tetuan, was next visited, and in order to catch the steamer to Mogador, our authors had to cross over to Gibraltar, from whence they again departed on April 20, in the Vérité, landing for a brief moment at Casa Blanca. They were in the port of Mogador on the 26th. Arrangements were soon made, through the goodness of the late Consul Carstensen, for the excursion to the Great Atlas. Mules were bought, the question of costume was decided, the interpreter of the Consulate, Abraham by name, was lent for the trip. The necessary escort consisted of four soldiers under the command of a captain. The necessary dinner at the Governor's was eaten, and about Instead of 7 A.M. on the morning of April 29 the cavalcade took its departure from Mogador for Marocco. following the direct road, a detour nearly at right angles was made, to enable the botanists to gain a fuller acquaintance with the great Argan Forest. Their course was first through a sandy soil, but as it rose and receded a little from the coast, the tertiary calcareous rock that underlies the sand cropped out here and there, and the first Argan trees appeared. "As we advanced, the trees grew larger and nearer together, and as we approached our intended halt, at a place called Douar Arifi, they formed a continuous forest. "The Argan tree is in many respects the most remarkable plant of South Marocco; and it attracts the more attention as it is the only tree that commonly attains a large size, and forms a conspicuous feature of the landscape in the low country near the coast. In structure and properties it is nearly allied to the tropical genus Sideroxylon (Iron-wood); but there is enough of general resemblance, both in its mode of growth and its economic uses, to the familiar olive tree of the Mediterranean |