4-7 1 3 PROCEEDINGS c 1^- or scuati^ i3o6tau 0ocictu of Natural l)uitorn. VOL. VI. 1856 TO 1359. BOS T O N : PRINT EI) FOR THE SOCIETY. 1859. /^/fl'-l i; r \ 1 :i; SI 1> I-; C \ M r, Ri ix; K : I'l.iNri.K i:v H. <>. nni(,nT(iN am) iomi-any. PROCEEDINGS OF THE BOSTON SOCIETY OF NATURAL HISTORY. TAKEN FROM THE SOCIETY'S RECORDS. My 2, 1856. Prof. Jeffries Wyman in the Chair. Dr. Wyman, on taking the chair, announced to the Society his acceptance of the office of President, to which he had been elected at the last meeting, and entered upon his duties as presiding officer. The Committee appointed to take into consideration the expediency of making summer excursions, asked for further time to report ; which was granted. A ninth letter was read from Mr. E. Samuels, giving a list of specimens collected in California for the Society. Two letters were read from Dr. James Lewis, of Mohawk, N. Y., dated June 18th and June 21st, pre- senting eighty-seven species of shells from his own neighborhood and twenty-five species from Georgia, Alabama, and Ohio, with the following list of PROCEEDINGS B. S. N. H. VOL. VI. 1 OCTOBER, 1856- '1 SHELLBEARING SPECIES OP MOLLUSCA OBSERVED IN POR- TIONS OF HERKIMER AND OTSEGO COUNTIES, NEW YORK. BY JAMES LEWIS, MOHAWK, N. Y. ]. Unio complanatus. Lea; rivers and canals. 2. U. cari- osus, Say ; Mohawk River ; very rare. 3. U. luteolus, Lam. ; Mohawk River ; very rare. 4. U. ochraceus, Say ; Mohawk River ; very rare. 5. U. radiahis, Lam. ; lakes ; abundant. 6. Alasmodon rugosa, Barnes ; canal and river, Mohawk. 7. A. marginata, Say ; canal and river ; rare. 8, A. undulata, Say ; lakes ; not abundant. 9. Anodon Jliwiatilis, J^ea. ; canal; very rarely seen. 10. A. ; new species ; lakes ; abundant. IL A. Lewisii, Lea; canal. 12. A. edentula, Say ; canal and mill-ponds ; rare. 13. A. Ferussaciana, Lea ; canal ; rare. 14. A. imhecilis, Say ; canal ; rare. 15. A. subcylindracea, Lea ; mill races ; rare. 16. Cyclas similis, Say ; lakes. 17. (7. modesta. Prime ; canals and streams. 18. C. transversa, Sa,y ; canals and river; Mohawk. 19. C. partumeia, Say ; ditches. 20. C. occidentalis, Prime, (pvalis, Pr., formerly.) 21. C. ovata, Lewis ; undescribed . very rare. 22. C. crocea, Lewis; very rare; outlets of lakes. 23. Pisidium dubium, Gould ; river. 24. P. ahditum, Hald. (Prime), P. zonatum, Pr. ; ditches. 25. P. vai'iahile, Pr., ditches. 26. P. compressum, Pr. ; canal, river, lakes, &;c. 27. P. altile? Nutt. ; still waters. 28. P. ventricosum, Pr. ; stagnant waters ; rare. 29. Palndiria integra, Say ; canal and river ; 30. P. decisa, Say; canal, river, and lakes. 31. P. ritfa, Haldeman ; canal and river ; rare. 32. Melania acuta, Lea ; canal and river. 33. M. (2 species ?) ; canal. 34. Amnicola lustrica ? Hald. ; canal, river, and lakes. 35. A. pallida? Hald.; lakes; rare. 36. A. limosa? Hald.; canal and river. 37. Valvata tricarinaia, Say ; canal, river, and lakes. 38. V. hicarinata, Lea ; lakes ; rare. 39. V. sincera, Say ; lakes. 40. Lymncpa elodes, Say ; stagnant water. 41. X. desidiosa, Say ; stagnant water. 42. X. humilis, Say ; stagnant water. 43. L. umhilicata, Adams ; stagnant water ; (with 48.) 44. L. gracilis, Jay ; lakes ; rare. 45. L. columella, Say ; lakes. 46. Physa heterostropha, Say ; ditches, &c., &c. 47. P. In- tegra ? Hald. ; rare ; river. 48. P. elongata, Say ; stagnant cold water. 49. Planorhis trivolvis, Say ; stagnant water. 50. P. hicari- natvs, Say; river. 51. P. armigerus, Say; stagnant water; rare. 52. P. dejlectus. Say ; lakes. 53. P. hirsutus, Say ; lakes. 54, P. parims, Say ; lakes and stagnant pools. 55. P. campaniilatus, Say ; lakes. 56. Ancylus rivularis'? lakes, on water plants. 57. A. ? Mohawk River ; very rare. 58. Helix alholabris, Say ; wooded sections generally. 59. H. alternata, Say ; wooded sections generally. 60. H. arborea^ Say ; old fallen timber, &c., &c. ; 61. ^ chersina, Say ; swampy grounds, under foliage. 62. H. concava, Say; swampy grounds, under leaves, &c. ()3. H. elecfriua, Gould ; moist places. Q4:. JI. fallax, Say (small var.) ; under rubbish in wooded sections. 65. ff.fuliginosa, Say; very rare ; habits little known. 66. If. hydrophila, Ingalls ; moist banks of rivers, in shade. 67. H. in- dentata, Say (with 63) ; quite rarely found. 68. H. intertexta, Binney ; woods. 69. H. lineata, Say ; under logs ; very rare. 70. H. lucuhrata, Say ; very rare. 71. H. minuta. Say ; damp places. 72. H. monodon^ Rackett ; under stones and sticks. 73. H.palliata, Say; woods. 74. H. Sayii, Binney; very rare. 75. H. striatella, Anthony; dry and moist localities. 76. If. thyroidus, Say ; shaded flats. 77. Succinea ohliqua, Say ; swampy flats, shaded. 78. S. ? {campestris of DeKay) ; hills. 79. S. vermetus, Say; shady banks of river. 80. *S'. avara, Say ; shores of lakes. 81. S. ovalis, Say; margins of ditches, &c., &c. 82. S. , similar to ovalis ; animal entirely black ; shores of lakes. 83. Bulimus luhricus, Brug. ; moist, shady places. 84. Pupa modesta. Say ; very rare. 85. P. exigua, Say ; damp places. 86. P. contracta, Say ; damp places. 87. P. milium, Gould ; rare. NOTES. No. 17, Cyclas modesta, Prime, may be the same as O. eden- iula. Say. Mr. Prime is of a different opinion, however. No. 30 probably embraces two species, one of which is decisa. No. 33 probably embraces two species, one of which is M. exih's, Hald. Nos. 34, 35, 36 are given on the authority of Prof. Haldeman, through Dr. ShurtlefF, of Westfield, Mass. No. 38 seems to be only a variety of 37. No living specimens of 38 have yet been detected. No. 39 has a more elevated spire than either 37 or 38, and was found associated with dead shells of 38 in the sediment of a small lake in the south part of Her- kimer County. No. 47 needs confirmation. I may yet secure specimens this season, so as to be able to send them. No. 64 occasionally presents a perfectly white shell; I have found only one, however, in which the animal was alive. I have also found an occasional specimen of 48 and 79 with a white shell. No. 48 appears to be the shell DeKay calls P. glabra. No. 58, H. albolahris, Say. DeKay appears to have named the young of this H. rufa. No. 70. I have some doubts if this be not H. inornata, Say. No. 75 presents two varieties. Those growing on dry localities are of a rufous brown, and have a very clean shell. Those grow- ing on flat lands, near the river, ai'e coated with mud, which seems to have the effect to bleach the shell somewhat. No. 82 may be only a variety of oralis. I observe the animals are exposed fully to the direct rays of the sun, which may have an influence in modifying the color, so as to cause the animals to become wholly black, — No. 81 being usually mottled with irregu- lar light and dark bands. Dr. Brewer called the Society's attention to the interesting fact, that a nest of the Nashville Warbler ( Verinivora ruhri- capilla) had been found in Lynn, in this State, by Mr. George Wells, an observing and enthusiastic naturalist of that town. This is a rare bird in this State, and, so far as is now known, its nest and eggs have never been met with by any ornithologist. It was included in Mr. Peabody's catalogue of the Birds of Massachusetts on the strength of a single specimen obtained by Dr. Samuel Cabot, .Jr. A year or two since, Mr. Charles S. Paine, of East Randolph, Vermont, observed a pair of these birds who evidently had their nest within a certain locality. He had no doubt that it was placed on the ground, but though carefully sought for, it was not discovered. Though not an uncommon bird in certain sections of the country, the Nashville Warbler has escaped the observation of most of our naturalists. Mr, Audubon never obtained but three or four specimens. Richardson and Swainson obtained only a single specimen, Wilson only three, and Mr. Nuttall mentions only one, seen near Salem. It is a rather common bird in Wisconsin, and by no means an uncommon bird in Vermont. It is quite possible that more attention to its localities may show it to be not so rare in this State as has been supposed. The nest found by Mr. Wells contained young birds, and a single egg. The nest was placed on the ground, in a dry place, among fallen leaves, and in the shelter of a thicket of young oak trees. The egg is ^f in length by ^ an inch in breadth, and in its shape is very nearly spherical, with one end more pointed than the other. The ground color is white, delicately tinged with pink, and spotted over the entire surface with dark purple and purplish-brown spots ; these are larger around one end, and are there gathered into a beautiful ring or wreath of confluent markings of various shades of purplish-brown. The nest was not taken, but left for the benefit of its occupants. Dr. Brewer also stated that he was indebted to the same gen- tleman for the nest and eggs of the Sylvicola pardalina, or Canada Flycatcher. This is by no means a common bird, nor are its nest and eggs known to have been obtained before with any certainty. Mr. Audubon speaks of having seen its nest in the great pine forest of Pennsylvania ; but he described it as found in a location quite different from the present instance. Mr. Wilson never met with its nest, or even with a female bird. Mr. Nuttall knew nothing of its breeding habits, and Richardson and Swain- son met with no specimens of it in the fur region. Several years since, Dr. Brewer received an egg from northern Vermont, the parents of which were so well described that he had no difficulty in recognizing them as this bird, and the eggs from Lynn con- firm the correctness of his supposition. The nest was found in low swampy ground, and was built at the foot of a tussock of thick grass, on the ground. It was constructed almost entirely 6 of leaves of the white pine, so loosely arranged that it was found necessary to sew them together in order to preserve it. The eggs, five in number, in shape are an oblong ovoid, ^ of an inch in length by y^g in breadth ; their ground color is a bluish white, irregularly marked with dots and small blotches of reddish brown. In the same locality, the present summer, there have been found, by Mr. Wells, the nest and eggs of the Prairie Warbler, Sylvicola discolor; the Chestnut-sided Warbler, S. icterocephala ; the Black-throated Green Warbler, S. viretis ; and the Black and White Creeper, Mniotilta varia. Mr. Wells has also observed a pair of the Solitary Vireo, V. soUtarius, which were evidently breeding in the vicinity. This is a rare bird, and is not given in Peabody's Birds of Massa- chusetts. Prof. Agassiz stated that, for several months past, he had been engaged in an investigation into the Geographical Distribu- tion of the Turtles in this country. For a correct determination of specific differences, it became necessary to collect specimens from all parts of the country as extensively as possible, and he had succeeded in obtaining specimens of nearly all the species existing in North America, and had been able to trace their geographical distribution very completely. Ample materials for a thorough survey had been placed in his hands through the ready assistance of his friends and correspondents, and by the officers of the Smithsonian Institution, who have put at his dis- posal their valuable collection. He had examined the specimens obtained by the government surveying expeditions of the several Rocky Mountain I'outes, and had received numerous specimens from the States in general, including Texas and California. He believed he had, at the present time, all but three species to be found in the United States proper, alive in his yard. The results to which he had arrived establish the fact, that several species, which have been supposed identical throughout their whole geographical range, are really distinct ; whilst others which have been described as different species, the young alone in some instances having served for description, have been found to be one and the same. He particularly called attention to the danger of describing species solely on theoretical grounds as dif- ferent, because they inhabit different parts of tlie world, or as identical from general resemblances. Dumeril and Bibron, in their work on Herpetology, and others, have attempted to identify marine turtles of different waters without sufficient authority. He had himself taken particular pains to inquire about the Sphargis or Leather-backed Turtle, which is found from the West Indies, northward, and which has been taken at Cape Cod. This animal has been said to inhabit the Mediterranean ; but the most thorough investigation shows only seven or eight in- stances on record of its having been found there. The museum at Salem furnishes an opportunity for distinguishing between the imbricata of the West Indies and that of the Indian Ocean, which have been considered the same. Holbrook describes the Trionyx of Georgia as existing in the Northern Lakes, and he traces the exact course by which it could ascend along the coast and up the Mississippi River to the lakes. Prof. Agassiz was satisfied that there are four different species of Trionyx in the United States, three of which are included in the one species of Holbrook ; and that each species has its own limited locality. The Chelidra or Snapping Turtles have the most extensive geographical range of any of the Chelonians. The Snapping Turtle of Massachusetts is found in South Carolina, Alabama, Louisiana, Missouri, and even at the head waters of the Osage. Of the family of Emydie, E. Blandingii is the true type. The swimming Emyda3 are either Southern or Western species ; there are none in New England except those which have but a limited power of swimming. Emys Oregonensis was described by Nuttall as existing west of the Rocky Mountains. Prof. Agassiz doubts its existence west of the Rocky Mountains, because no turtles have been found in those high regions lying between that range and the Sieri'a Nevada. Upon the Alleghanies, turtles have been found at a height of eleven hundred feet only, and there are no indications of their existence above this height. He had received two specimens from localities east of the Rocky Mountains, one of which was brought him by Mr. James M. Barnard, from Min- nesota. Mr. Nuttall's specimen, he thought, must have come from this side of the mountains. 8 Prof. Agassiz concluded that there is no general law regulat- ing the distribution of the Chelonians of North America. They are distributed through four grand divisions of the country, a northeastern, a southern, a western, and a Pacific range. The facts of their geographical distribution are now well established, but the reasons are by no means evident at present. The proba- bility is, that different individuals of the same species of animals are adapted, by peculiar organizations, to different climacteric influences, and that there is no general law of distribution for which physical agents can account. Dr. Storer asked what was the northern geographical limit of Cistudo Blandingii. In 1842, he presented to the Society a specimen from Bradford, Mass., until which time it had not been observed by naturalists north of South Carolina. Prof. Agassiz replied that he had found the eggs in Massachu- setts, and raised the animal from them. There is no evidence of its existence between Massachusetts and Illinois, where it is again found. It has a circle of distribution in the Northwestern States, and another disconnected range in Massachusetts. He thinks the animal may have originated in the two different localities. The President exhibited some Fossil Bones and Teeth, discovered by Mr. J. W. Foster, in Iowa. They consisted of remains of an animal belonging to the natural family of SuidaB, and appeared closely allied to, if not identical with the Euchserus of Dr. Leidy. A complete series of teeth was exhibited, in which the milk and permanent molars were all represented. A large portion of the skeleton, as well as the germs of the teeth of a very young animal, belonging to the same species, were ex- hibited, indicating that they were derived from an indi- vidual which had been born but a short time, or even from a foetus. Dr. Durkee exhibited a potato infested with a parasitic insect, a species of Acarus. A new generation is pro- duced every few weeks. The gentleman who gave him 9 the specimen informed him that the stem of the plant was likewise covered, and that he was disposed to think this might be the cause of the " potato disease." The late Dr. T. W. Harris believed the malady to be caused by parasitic fungi. Dr. C. T. Jackson was of the same opinion as Dr. Harris, and he supposed the presence of the insect in this case to be purely accidental. Messrs. F. W. Putnam, J. L. Hun ne well, and J. M. Hayward were elected Resident Members. July 16, 1856. The President in the Chair. Prof. Agassiz stated that, a few years since he had described a new family of fishes, Emhiotocoidce, in which the mode of re- production is viviparous. He had now to announce the fact, that, in another family, and one well known, there is likewise viviparous reproduction. He had recently been examining the ovary of the common haddock, and had found the ova already passed the stages of segmentation. He had not yet been able to examine them during the latest periods of development, but he had no doubt that the embryos were developed within the ovary. He thought, however, that the young might be brought forth in some kind of an envelop, and thus escape observation. In the Cod, Whiting, and American Hake, the ova likewise undergo development in the ovary. Prof. Agassiz was informed by the fisherman who had supplied him with the specimens in which this discovery was made, that he had for a long time supposed that the young were formed in the parent. Prof. Agassiz had been endeavoring to find homologies of development in all animals of the vertebrated type, and had 10 succeeded in tracing them so far as to be able to distinguish between vertebrata and invertebrata in the earliest stages of development of the egg. The President remarked that every new instance of ovarian impregnation was of great importance. The most recent re- searches go to prove that the seminal fluid comes in direct con- tact with the ovum, and perhaps enters into its substance ; but in Anableps, the ovum is surrounded by a membrane which would tend to prevent any such entrance. Prof. Agassiz observed that he considered fecundation as a series of acts rather than a single act. In Chelonians, the cir- cumstances under which the eggs are developed, would lead to the inference that an impulse is first received from the male, and then that four successive copulations in four successive years, twice a year, are necessary before segmentation takes place in the egg. In the Haddock, ovarian gestation has this physiologi- cal import, that it shows that what is a normal condition in one animal of a certain type, may be abnormal, and occur only ex- ceptionally in another animal of the same type, as in man and other of the higher forms of vertebrata. Dr. Gould inquired how ovarian impregnation took place in fishes. Prof. Agassiz replied that he had seen certain fishes place themselves in such a position that there was close approxima- tion of the abdomens of each, whilst in the female the entrance to the ovary was open to a very considerable extent. Mr. Bouv^, in behalf of the Committee appointed to consider the subject of summer excursions, reported in favor of the project, and proposed that the first excur- sion should be made to Hingham and the neighboring country. It was voted to assemble on board the Hing- ham steamboat at 9 o'clock, A. M., on Wednesday, July 23, and it was understood that the Committee would make arrangements for proper conveyances at Hingham when the company should arrive. Dr. C. T. Jackson read an extract from a letter of Mr. Roswell Field, of Greenfield, Mass., in which he says 11 he thinks he has discovered an entirely new footprint of a biped web-footed animal, two and a half inches long, with a stride of about ten inches, and with an impression of a tail. He regards it as much more perfect than the one described by Prof. Hitchcock, and thinks it may even prove that the latter was not made by a web-footed animal. This letter was referred to the President. Dr. A. A. Gould presented the following descriptions of shells : — Helix repercussa. T. sinistrorsa, discoidea, supra plan- ulata, infra concava, plicato-striata et lineis volventibus superne insculpta, castanea ; anfract. utroque 6-|-, ultimo vix angulato, prope aperturam deflecto : apertura despiciens, oblique lunata, peritremate reflexo, postice callo angulato juncto ; lamellis pala- tinis diiabus Intro volventibus, quarum una ad angulum incon- spicuu. Diam. 1 ; alt. j^j poll. From Tavoy and Mergui. Rev. J. Benjamin. Compared with //. anguina, it is less distorted, more elevated, concave beneath only, whorls more numerous and moi'e closely coiled, obtuse at periphery, not marbled in coloring. Helix ramentosa. T. suborbicularis, depressa, tenuis, per- forata, fulva fascia fusca albo marginata ad peripheriam cincta, lineis incrementalibus et sulcis decussantibus pariter obliquis granulata ; anfr. 5^ convexiusculis, ultimo obtuse angulato ; su- tura valdc impressa : apertura oblique oblongo-ovata ; peritre- mate postice acuto, sensim versus umbilicum reflexo, albo; fauce rufescente. Axis half an inch ; diameter f inch. California ; from the cabinet of Dr. W. Newcomb. Agrees well with H. zonata, Pfr., in which the umbilicus is larger, and no allusion is made to the rasp-like surface. Helix damascenus. T. conico-globosa, imperforata, solidula, dilute prunina ad apicem violacea subtus cinerascens, rudis et 12 lineis tenuibus interruptis numerosis cincta ; anfr. 5 rotundatis ; sutura irapressa : apertura subcircularis ; peristomate anguste reflexo, pallido, extremitatibus approximatis ; fauce livida ; col- umella incrassata, rotundatu. Axis Yi5- ; diam. -^^ poll. Desert region east of California. From the collection of Dr. W. Newcomb. The texture and coloring is much like that of H. alauda, Fer., but the shell is smaller and more elevated. BuLiMUS LEPiDUS. T. parva, plerumque sinistrorsa, vix per- forata, ovato-conica, elevata, polita, citrina ; anfr. 6 convexis, ultimo ventricoso ; sutura bene impressa : apertura subcircularis; peristomate albo, reflexo, ad columellam dilatato, extremitatibus approximatis. Axis 1^ ; diam. ^ poll. Mergui Islands. Rev. J. Benjamin. A pretty shell, grouping with Iceinis, Adamsii, and moniliferiis, but smaller, proportionally shorter and more ventricose, and dif- fering entirely in coloring, texture, and the broadly rounded form of the aperture. BuLiMUS LAUTUS. T. subperforata, oblique ovato-triangu- laris, tenuis, eburnea longitudinaliter rufo-lineata ; suturis palli- dis ; anfr. 6, ultimo ad peripheriam in carinam compresso, subtus versus umbilicum declivi et plicato : apertura oblique triangularis, ad angulura latero-basalem canaliculata ; peritremate expanso, intus incrassato, albo, rosaceo vivide submarginata. Length, one inch ; breadth, half an inch. From the mountains of Equador, near Quito ; by Joseph P. Couthouy, Esq. A most remarkable and beautiful shell, belonging to the peculiar group of Bulimi, with angulated apertures, found on the Andes, near Chimborazo. The basal angle stands off further from the axis in this than in any other species yet figured. B. semiclausus is banded, the basal angle rounded, the spire less acute. B. Knorri is more elongated, and the basal angle nearly axial. B. murrinus and B. fabref actus are also allied. Streptaxis prostrata. T. pupoidea, valde distorta, tenuis, dilute cornea ; anfr. 6, posticis lateraliter appositis, ad periphe- riam acute angulatis, antico subtus glabrato : apertura longior 13 quarn lata, lamina palatali instructa ; peristomate reflexo ; um- bilico crescentico, satis magno- Long. ^ poll. ; lat. I poll. Found by Dr. G. A. Perkins, at Cape Palmas, and at Rock- bookay, twenty miles in the interior, under dead leaves. He says " the animal is beautiful red, yellow, and orange." It is of" the size of *S'. aberrans, but is more eccentric and more compressed. Streptaxis elisa. Testa modica, valde secunda et compressa, supra tenuiter striata, infra glabrata et late perforata ; spira dis- coidea ; anfi*. 7 -|- juxta suturam profundam angulatis, ultimo lateraliter valde protenso : apertura transversa, subquadrata, peritremate everso, intus denticulis quatuor cruciatim dispositis armato, quinto minimo interdum posticc addito. Length, half an inch ; height, \ inch. From an island in the Mergui Archipelago ; Rev. J. Benjamin. In size and form most like aS*. Soideyetana, but is even larger and more depressed ; aperture much as in S. pyriformis, but more elongated, and the posterior denticle is very small and marginal ; the shell is double in size. Streptaxis exacutus. T. grandis, omnino dislocata, late umbilicata, pallide cornea, supra acute lirata, infra polita : spira discoidea, lateralis ; anfr. G -j- penultimo postice valde protruso, exacuto, apicalibus convexiusculis, bene discretis : apertura sub- quadrata ; peristomate albo, reflexo, postice angustato et sinuato ; palato lamina subcentrali et altera inconspicua ad angulum munito. Length, ^ ; breadth, -^^^ poll. Found by Rev. F. Mason, in Burraah. More solid and compressed than S. elisa, with no denticles on the peritreme, and with the edge of the penult whorl forming the posterior end of the shell very sharp. Clausilia vespa. T. solida, sinistrorsa, vespaeformis, de- flecta, la3vis, intense rufa ; anfr. 6, anteriori raptim attenuate, proximo corpulento, apicalibus cito decrescentibus ; sutura im- pressa, vix marginata : apertura ovata ; columella biplicata ; peritremate late reflexo, rufo. 14 Long. 1 ; lat. -^^ poll. Inhabits Tavoy. Eev. Francis Mason. This very singular, wasp-like shell is allied to C. insignis, Philippii, Cochinchinensis^ &;c., but distinguished from all by its peculiar form. I Cyclostoma pollex. T. polliciformis, distorta, suburabili- cata, rufescens ; anfr. 6, ultimo ventraliter planulato, dorsaliter gibboso ; anfract. posticis nonconformibus, rotundatis, dexti'orsum nutantibus ; sutura profunda, marginata : apertura circularis, postice truncata ; peritremate duplici, modice reflexo. Long li ; lat. f poll. Tavoy, British Burmah. Rev. Francis Mason. This singular shell may possibly be Cyclostoma chrysalis, Pfr., but is larger, destitute of lines and indentations. That shell is said to come from Arva, (probably Ava.) Megalomastoma My- ersii, Haines, is another species of the same type, but less distorted and more cylindrical. These shells, coming from the same region, to which many others will doubtless hereafter be added, I regard as constituting a natural group, probably generic, for which I would propose the name Pollicaria. Shell subperforate, chrysalidiform, ven- trally flattened, spire secund ; apertui'e subcircular, truncate posterioi'ly within the periti'eme. Cyclostoma cucullata. T. umbilicata, depresso-conica, soliduhv, lineis incrementi et lineis volventibus tenuibus superne insculpta, straminea ferrugineo tessellatim marmorata, et infra lineata, apice nigro ; anfr. 5 rotundatis ; sutura profunda": aper- tura (genuina) elliptica ; peritremate reflexo, et cucullo lato unicolori oblique truncato vakle protracto ; fauce flava. Diameter, exclusive of false lip, y^g- inch ; projection of hood- lip ;|^ inch ; axis ^ inch. From an island in the Mergui Archi- pelago ; Rev. Judson Benjamin. With the exception of the aperture, the shell is much like small specimens of C. linguiferum^ov still more like C. irroratum, Sowb. Its remarkable hood is sufficiently characteristic. MiTRA FLORIDA. T. ovato-fusiformis, solidula, albida ferru- gineo nubeculata et lineis numerosis fuscis interruptis interdum albo articulatis cincta, quoad rostrum plicata et oblique lirata ; anfractibus 7-|- ultimo spiram ter excedente, antice angustato: 15 apertura angusta, postice acuta ; labro acuto : columella sexpli- cata, plica postrema proximam bis superante ; intus alba. Axis If ; greatest diam. f ; length of aperture, 1-^ inch. Re- ceived from Dr. Edmund Ravenel, of Charleston, as from Florida. Another specimen, in the possession of Dr. Jay, was supposed to have come from the Philippine Islands. Its characters are intermediate between Mitra and Voluta. It most resembles in form and coloring a small Vol. antiqiiata, but the markings are much more crowded and delicate. Unio lepidus. T. transversa, elongato-ovata, tenuis, ventri- cosa, valde inequilateralis ; umbonibus tumidis, leviter undulatis, dilute viridibus ; disco olivaceo, vix radiato ; latere antico rotun- dato, superne angulato; latere postico ovato, marginibus arcuatis ; dentibus cardinalibus erectis, lamellatis, fimbriatis ; dentibus lateraHbus, rectis, acutis ; margarita argentata, postice iridescente ; cicatricibus anticis sejunctis. Long. 2f ; lat. 1; alt. 1^ poll. From a creek near Lake Monroe, P'lorida ; Dr. Henry Bryant. Very closely allied to U. trossulus, Lea, but is larger, more fragile, and the cardinal teeth are more compressed. Unio coruscus. T. parva, solida, transverse ovata, ad dor- sum lata, deorsum cuneata; umbonibus anticis valde erosis ; latere antico rotundato ; latere postico acuminato ; margine dorsali valde declivi ; margine ventrali lente arcuato ; epidermide piceo, nitente ; dentibus cardinalibus obliquis, validis ; dentibus lateralibus curtis, rectis; cicatricibus anticis sejunctis; margarita vivide cupreo- purpurea. Long. If; alt. |; lat. f poll. River St. John's, near Lake Beresford, Florida ; Dr. Henry Bryant. Of the same type as U. Buckleyi, and might be thought the young ; but it is more solid, less angular, is much darker colored, has a much more brilliant nacre and a stronger hinge ; trossnlus is less cuneate and has a white nacre, as has also U. Brumbyanus. Teredo thoracites. T. magna, solida, subequilateralis alba ; valvis trilobatis ; area anteriori maxima, antice truncata, obtuse lanceolata, concentrice insculpta ; area intermedia uncinata, ad apicem obtusa, apophysi valido intus sufFulta ; area posteriori 16 minima, lunata, superne emarginata, incrassata ; tuberculis car- dinalibus magnis, uncinatis ; apophysi subumbonali compresso, geniculate ; ossicula siphonalia pulpito mediano instructa, altero latere subulate, altero ligulato. Length and height, ^ inch ; breadth f inch. Tavoy, British Burmah ; Rev. F. Mason and Rev. J. Benjamin. In size and solidity this exceeds any species yet described. It is chiefly characterized by the great size of the anterior area when compared with the posterior ; the stilt-like form and great length of the pallets is also quite peculiar. Dr. C. T. Jackson gave a brief description of the bituminous coal formation of Elk County, Pennsylvania, which he had been engaged in exploring during the month of June last. He ob- served that the great bituminous coal basin or trough extends from the Northwestern border of Pennsylvania to Tuscaloosa, Alabama, as indicated on Mr. Jules Marcou's Geological Map of the United States. The northern portion of this basin is of great economical value, on account of its being the nearest to Lake Erie, one of the greatest markets for coals, which are required for steam navi- gation on all the great lakes, and for the furnaces and gas works, as well as for domestic use for fuel, on both the United States and Canada sides of these lakes. He remarked that statistics showed a larger amount of tonnage on the lakes than exists on the Atlantic coast of this country, and that steam rw^^ation would certainly greatly increase upon the lakes when coals coth^ be obtained at a reasonable cost, as will soon be the case, when the western portion of the Sunbury and Erie Railroad, now under contract, is completed, which would be done in the course of two years. Since the recent explorations were made into the extensive coal formation of Elk County, Pa., the Directors of this im- portant railroad have ordered the road to be laid amid those coal fields, and the consequences of this movement will soon be felt in the augmented value of the coal lands. The particular region explored by Dr. Jackson, is known as the Ridgeway Land and Coal Company's property, some 27,000 acres of land, all situated in the coal region. Five or six beds of 17 coal underlie this soil, and they generally dip only from two to five degrees from the horizon, and are from two to six feet in thickness. Most of the large beds are undisturbed, and only the small upper ones are here and there denuded by valleys of excavation. The deep ravines, or runs, expose some of the outcrops of the larger beds on the southeast sides of the hills ; on the northwest they are still deeply covered with rocks, the sandstones, and bituminous sliales. Each of these coal beds is overlaid with a stratum of eight or ten inches of slaty cannel coal, and they all rest on fire-clays. Iron ores, namely, carbonate of iron and brown hjematite, abound ; the former in the fire-clays, and tlie latter in the superincumbent shales. But few fossil plants are found in these shales, and only the scales, fins, and tails of fishes in the slaty cannel coal, which appears to have been a fine aqueous sediment of water-logged vegetable matter. A bed of buff-colored limestone occurs beneath the principal bed of coal, and is nine or ten feet thick. This limestone con- tains small fossil bivalve shells not yet named. The Ridgeway lands, then, contain coal, iron ores, limestone, and sandstone, with an abundance of clay suitable for fire-proof bricks. All the facilities for the reduction of iron exist on the spot, and soon the means of transportation of the coals and metal to mar- ket will be supplied. The county is elevated about 1,600 feet above the sea, and is in Lat. 41 '^ 25' N. and Lon. 1" 40' W. of Washington, and is remarkably healthful. The following analyses of the coals, iron ore, and limestone have been made by Dr. Jackson since his return to Boston. Specimen from the six feet bed : — Fixed carbon ...... 52.38 Gas expelled by heat . ... . . 40.00 Ashes of coke ...... 7.62 The ashes analyzed yielded — Silica . ...... Alumina and oxide of iron . Lime ....... 7.52 PROCEEDINGS B. S.N. II. — VOL, VI, 2 OCTOBER, 1S66. 100.00 6.20 1.10 0.22 18 The slaty cannel gives — Fixed carbon ...... 32 Gas 24 Earthy matter ...... 44 100 The limestone yielded — Carbonate of lime 95.75 Insoluble silica ...... 3.00 Peroxide of iron ...... 1.25 100.00 Analysis of the balls of carbonate of iron : 100 grains of this ore yielded — Peroxide of iron .... G1.50 = iron 43. Carbonic acid .... 31.50 Silex 7.00 100.00 In smelting iron ores with these coals, it will be necessary to convert the coal into coke, and the small coals may thus be dis- posed of on the spot. No better gas-making coals are found in the United States, and but one better variety in the British Pi'ovince of New Brunswick — namely, that of Albert County. Dr. Jackson spoke in high terms of admiration of a series of fossil fishes now at the Smithsonian Institution undergoing de- scription by Dr. Newberry. He stated that these fossils appear like fishes cast in brass, the scales of the ganoids being covered with a film of iron pyrites ; and expressed the hope that Dr. Newberry might soon exhibit some of them to the Society. They were found in the Diamond County coal mine in Ohio. Dr. A. A. Gould exhibited a specimen of the common Lumhricus ascaris, an intestinal worm, which was vomited alive by a person, by whom, and by whose friends, the worm was called a snahe. Dr. Gould referred to two or three other and similar cases, and observed that science could do much to disabuse the public of the incorrect idea that animals could live for any considerable 19 length of time in the human body, unless they belonged to some of the parasitic forms. Some discussion ensued as to the possibiUty, under any circum- stances, of a foreign animal living in the human stomach. The President narrated a case of a living toad, which was swallowed by an insane man, having been vomited, soon after, dead ; and the results of some experiments, in which worms were taken into the stomach in perforated tubes, where the worms lived but a short time. Dr. C. T. Jackson presented, in the name of Mr. Addi- son Gott, of Rock port, some Parasitic Crustaceans, com- monly known as Salve Bugs. Prof. Agassiz remarked that these animals contain an apparently oily matter, which, after immersion in alcohol, is changed into a substance resembling wax, and which is so hard as not readily to be cut with a knife. The specimens were referred to Dr. Jackson for chemi- cal examination. Mr. Robert Kennicott, of West Northfield, Cook Co., 111., was elected a Corresponding Member, and the fol- lowing named gentlemen Resident Members, viz : James E. Mills, Thomas W. Clarke, John Green, Edwin A. Gibbens, J. Henry Safford, Joseph Worcester, John Dean, David F. Weinland, Augustus J. Perkins, Samuel Ham- mond. July 23, 1856. EXCURSION MEETING. In pursuance of a plan adopted at the last meeting, the Natu- ral History Society met on board the steamer Mayflower, for an excursion to Hindiam and the neighborhood. There were 20 present about tliirty of its active members, several of (hem being among its founders or the earliest enrolled upon its list. After a beautiful sail down the harbor and among the islands, the com- pany found ample arrangements made for them at Ilinghara by the committee, and were conveyed in carriages along tlie new road in the direction of Nantasket Beach. This road, opened two years since, presents a number of interesting features to the student of nature. Mr. Thomas T. Bouve, the Chairman of the Committee of Arrangements, and to whom the Society were indebted for the complete success of the occasion, was most earnest in his en- deavors to call attention to every object of interest and instruction upon the route. Upon passing through the woods, not far from the Old Colony House, he pointed out several nests of the Night Heron, (^Ardea nycticorax,) built of sticks, high up in the trees. He remarked that these were the only Night Herons to be found anywhere in the vicinity of Boston, with the exception of those at Fresh Pond, and that tl)ere was danger of their complete extermination, if the young were taken and destroyed by people in the neighborhood, as has been done lately. Some distance further on, were seen the remains of submerged trees, supposed to be cedars, which had been imbedded in the peat, and which were exposed in the construction of the road. The President gave' some account of these remains, consisting of large stumps and roots, buried in salt-water peat. The swamp in which the trees grew, was somewhat below tide water, and in consequence of the breaking down of the barriers, the communi- cation with tlie ocean had been made ; and the whole tract, consisting of many acres, formerly covered with trees, is now regularly flowed by the high tides. This is one of several in- stances in which the ocean has made its inroads upon the shore in this neighborhood. The most recent breach occurred a few years since, near Pleasant Beach, during the great storm which carried away the Minot Lighthouse ; the sea barrier was broken through, and every tract of fresh water was invaded, and, unless soon reclaimed, will become permanently a part of the domain of the sea. He also called attention to an Indian cemetery, on the south- eastern slope of Atlantic Hill, near Nantasket Beach. 21 An examination of severul of the graves had been made by Mr. Francis Boyd, by whom attention was first called to them by Mr. F. Burr, one of the proprietors of the land, and Drs. M. and J. Wynian. Portions of the remains of four adults and orie child had been found. The cranium of one of the adults was sufficiently well preserved to exhibit the unequivocal anatomical characters of the North American Indians. Generally, the bones were too much decomposed to be removed, except in fragments. The original position of the bodies, as shown by that of the bones, was on one side, with the knees drawn up, and not in a sitting attitude. The articles buried with them consisted of fragments of pottery, composed of clay and pounded clam shells, of stone pestles, and a clay pipe, all of Indian manufacture ; also of an iron hatchet, a brass kettle, some beads of brass, and others of glass, which must have been obtained from the white settlers. These latter articles, of course, bring down the date of the ceme- tery to a period subsequent to the settlement of the country. Mr. Boyd invited the members of the Society to his house, where they had an opportunity of examining such of the remains and relics as were in his j^ossession, and at the same time were provided with a most generous and hospitable entertainment. After a ride a short distance upon the beach, the carriages were left, and the party wandered along the rocks and sea-shore towards Cohasset, where those interested in shells, fish, marine plants, minerals, &c., had opportunities of collecting specimens. Here remarks were made by those particularly versed in special subjects, amongst others, by Dr. David F. Weinland, who called attention to the ovaries of the Whiting, in which were eggs in process of embryonic development ; a fact which Prof. Agassiz has recently noticed in this fish, the cod, the haddock, and the American hake, our most common fishes, and which have hitherto been supposed to be oviparous and not viviparous. Meeting at a certain rendezvous, and resuming seats in the carriages, a pleasant drive was taken along the ridge road ; stop- ping to view the famous trap dyke upon the sea-shore, and its striated markings, indicative of glazier action according to some, or of drift action accoi'ding to others ; the prominent features of the dyke and surrounding rocks being pointed out by Dr. C. T. Jackson, Mr. Francis Al";er, and Mr. Bouve. 22 At about three o'clock, the company arrived, by special invita- tion, at the beautiful mansion of Mr. Bouvc, where, after exam- ining his magnificent mineralogical and geological cabinet, the Society sat down to a handsome banquet provided by him. After dinner, and a song from the accomplished Curator of Botany, a portion of the party scattered themselves for the col- lection of specimens, whilst the remainder assembled under the trees to listen to some remarks upon what had been seen during the morning. Some observations were made by the President, upon the man- ner in which the Limidus (the Horseshoe Crab) casts its shell. Unlike that of the crabs and lobsters, this is cast entire. The first step towards the formation of a new shell, is the separation of the soft parts from the old integument ; the new covering, at first quite soft, is everywhere minutely convoluted, in order to accommodate its increased surface. The old shell splits around the convex border of the head and thorax, and the Limidus escapes, withdrawing its legs, gills, and tail. The animal imme- diately expands, the convolutions of the new shell are drawn out, it hardens, and the growth is finished until the period of the next moulting. Dr. Wyman had found the horseshoe in the stage preliminary to shedding the skin, and in the act of leaving it ; in the latter case, the animal was not yet freed from the old shell, but its growth was already complete. From observations made on many shells, he had ascertained that at each moulting the increment was by one third to one half of the dimensions of the animal. Growth takes place at no other time than during the moulting period. The cuticle which lines the oesophagus and stomach is withdrawn at the time the external shell is cast, and comes away in connection with it. Mr. Francis Alger spoke of the great Beryl formation in the town of Grafton, New Hampshire, describing its crystals of gigantic dimensions which had been discovered there. One of these crystals, which he had caused to be removed and conveyed to Boston, weighed nearly 2^ tons, and was five feet in length. Another, the largest single crystal in the world, as far as is known, is nine feet in length, being a six-sided prism, the several faces of which measure respectively in width through the greatest diameter of the crystal, 2 feet 8 inches, 2 feet, 1 23 foot 11 inches, 1 foot 10 inches, 1 foot 6 inches, and 1 foot 9 inches — thus giving it a circumference of 12 feet. This crystal yet remains at the locality, but the quartz and feldspar sur- rounding it have been carefully removed by chisels, so that its position in its native bed can be readily observed. Three weeks labor of two men was expended in this process, as ordinary blast- ing by gunpowder would have destroyed the crystal. Its weight is probably not less than five tons. Dr. C. T. Jackson, at tlie request of Mr. Alger, gave a descrip- tion of the Geology of Alger s Bertjl Hill, in Grafton, N. H., where the above-mentioned crystals are found. They occur in a very largely crystallized vein of Granite, which traverses the hill of mica slate. In extracting the crystals of beryl, large quantities of orthose or potash feldspar, suitable for making the finest porcelain ware, were obtained, and this is now exported to England for that purpose. Plates of mica, a foot or more square, are also obtained, and are useful for making windows to stove doors, &;c. Dr. Jackson next proceeded to give an account of the Trap Dykes., and of the rocks altered by fire which were observed by the Society upon the coast of Cohasset, stating that the rocks were originally stratified, and were of aqueous deposition, and have since their deposit become metamorphosed by the agency of trap rocks which underlie them and have burst through them, in dykes running generally nearly east and west, with occasional crossing dykes having a north and south course. The minerals produced in the metamorphosed rocks, by the influence of the trap, are amygdules of feldspar, invested with a thin layer of Epidote, and of nodules of Epidote, like those of the Nahant rocks. Boulders of quartz occur in an unaltered state, in the metamorphic rocks, in considerable abundance. Dr. Jackson then extended his remarks to the trap rocks of different ages, and explained the remarkable influence they have exerted on limestones, slate-rocks, and sandstones, showing their agency in producing crystallized minerals and metalliferous ores of various kinds. In Nova Scotia and on Lake Superior, the trappean rocks, passing through the new red sandstone strata, combine with the ingredients of that rock, and also form an abundance of most beautiful minerals of the Zeolite family. 24 Native copper is also produced, in masses and in veins, both in Nova Scotia and on Lake Superior; this metal being found in large and regular veins in very great abundance in the Amygda- loidal trap of Keweenaw Point, Ontanagon, and Isle Royale districts, on Lake Superior. When trap rocks act upon slate rocks, they produce iron pyrites, and occasionally silver ores, and with silurian limestones they form lead and silver ores almost exclusively ; while, as before stated, native copper generally results from their influence upon the new red sandstone strata. Hence, the miner and the min- eralogist are guided in their researches by a knowledge of these geological laws, which seem to be universal in their application. Dr. D. F. Weinland gave an account of the Reproduction of Parasitic Animals, and explained the phenomena of Alterna- tion of Generation in the parasitic Trematoda of the Freshwater Snails. The first generation of this animal exists, in the form of " Distoma," in the intestines or lungs of Vertebrata, as a perfect animal with genital organs producing eggs ; the next generation exists as a yellow worm in the liver of the snails mentioned above, with or without an intestine, their bodies being filled with the third generation of the animal, viz : little worms with long tails — the so-called Cercarians — which originate in the body of the yellow worm by a kind of budding. In the third generation, these Cercarians are brought forth by the mother, swim for a while free in the water, and then become a kind of pupa ; form- ing a cyst around themselves, and in this state seeming to wait till, by chance, they are swallowed by a vertebrated animal in which they become, in a few days, as is shown by experiment, a perfect Distoma. Dr. Weinland had found a new species of Cercaria, the first known in this country, in the liver of the Physa heterostropha, and he concludes, from further investigations, that this Cercaria belongs as a larva to a blackish-spotted Distoma, which he has found frequently in the lungs of frogs and toads, and once in the intestine of a turtle, and which he proposes to describe under the name of Distoma atrlventre. He added that a similar alternation of generation takes place in another order of Helminthes or Parasitic worms, viz : the order of Cestoda. The investigations of Kuchenmeister and 25 SieboW have shown that the cysts in the flesh of the hog, causing the condition known under the name of " measly pork," are pupa? of the human tapeworm, and that they develop themselves into the latter when taken into the human intestine ; and that the human tapeworm, when eaten by a hog, produces in this animal these cysts. In three instances, in which he had seen tapeworms in Americans, these worms were identical with the Tcenia solium, the tapeworm of the English and Germans, the same species upon which the experiments of Kuchenmeister were made, — not the Botriocephalus latus, the tapeworm of the French and Swiss, which seems to have a different kind of development. He had found a larva of a tapeworm, a so-called Scolen, with two large red spots behind the head, in the intestine of the common Alewife, (^Alosa Americana,) provided with four large suckers, (acetabula,) but not having an articulated body, nor genital organs. This larva was destined, as he supposed, to become a perfect tapeworm only in the body of another vertebrated animal by which the alewife might be swallowed, — perhaps in a shark. He had found another larva of a tapeworm, the Tetra- rliynchus 3Iorrhiice, Rud., {T. corollatus, Siebold,) in a cyst near the heart of the common codfish. He had found the larva of tapeworms, known under the name of Cysticercus, in the pelvic region of the American hare, (Lepus Americanus,) and in the liver of the rat, {Mus decumanus.) After a careful comparison, he found them identical, one with the Cysticercus of the European hare, and the other with that of the European rat; which be- come, according to the experiments of the same Helminthologist, Kuchenmeister, the first, the tapeworm of the dog, and the second that of the cat; a fact likewise noticed by the American hunters. Dr. Weinland supposed that this Cysticercus of the American hare came from the European dog ; the eggs of the tapeworm having been swallowed by the hare, perhaps with vegetable food. In another and new species of tapeworm, the Tcenia punctata. Weinl., found in the gold-winged woodpecker, he had observed the embryo just hatching. The shell of the egg of this worm has two processes, each terminating in a large ball ; tlie embryo is provided with six spines. Some years ago. Dr. Hein and Dr. Meissner found pupa; of tapeworms in cysts in a land- 26 snail, {Helix pomatia,') and in a beetle, {Tenebrio molitor,) and in the cyst were found six little spines thrown off by the embryo. Thus, we have reason to believe that that hatching embryo, with its six spines, penetrates into an insect or a mollusk, forms there a pupa, loses its spines, and waits in this state till the snail or the insect is swallowed by a vertebrate ; for in vertebrata only we find pei'fect tapeworms. In the case of Taenia punctata., we may suppose that the embryo enters an insect, forms there a pupa, which afterwards is eaten with the insect by the wood- pecker, and then is developed into a tapeworm. Thus, the intimate I'elations existing between the woodpecker, its tape- worm, and the insects in which the latter lives as a pupa, and upon which the woodpecker feeds, must be intimately concerned in the preservation of the species of this worm ; and if we con- sider how infinitely small is the chance of a single egg's per- fecting its development in that bird, we see why one tapeworm should furnish millions of eggs in a year. The Psorosperraia, discovered first by Johannes Miiller, which may be another larval state of a worm, Dr. Weinland had found by thousands attached to the hind part of the eye bulb of the American Haddock, {Gadus aeglefinus.) To a question proposed by Dr. Gould, " Whence come the parasitic worms of the Foetus in Utero ? " Dr. Weinland an- swered, that only two or three such instances are known ; and from the f;ict that he once witnessed an Ascaris penetrating a membrane in such a manner, that, after it had traversed it, there was not to be seen any perforation in the membrane, (the worm having separated the fibres of the tissue without tearing it,) he thought that he could explain the presence of the worms, found in the embryo, by a passage from tlie abdomen of the mother and through the walls of the womb, and thence into the body of the embryo ; a movement which, according to this observation in Ascaris, could be effected without wounding the tissues. Mi\ Charles J. Sprague exhibited a beautiful specimen of a parasitic fungus growing upon the body of a beetle, a species of Sphoeria.. He said he supposed that the insect more or less com- pletely buries itself in the eartli, and then the plant attaches itself to its surface, and sooner or later destroys it. Mr. Sprague 27 had been making a special study of these peculiai' and little known growths the past year. Mr. Bouve made a few remarks upon the origin of Tgneous Rods, comparing specimens of the igneous rocks of New Hamp- shire and lava from Vesuvius, to illustrate the resemblances and differences between quick and slow crystallization. After these interesting and instructive observations, followed by the interchange of much general information in a more private manner, and after passing votes of thanks to Mr. Bouve for his untiring exertions throughout the day, and to Col. Boyd for his most welcome hospitality, the Society took the cars for Boston, and returned Avell satisfied that a day could not have been more agreeably and more instructively passed ; and the hope was uni- versally expressed that this excursion might be the first of a series, which would inevitably tend to augment the usefulness and prosperity of the Society. Avgust 6, 1856. The President in the Chair. Prof, William B. Rogers exhibited to the Society several specimens of rock, containing casts of portions of a large Trilobite lately obtained by him from a locality on the north edge of Braintree, about ten miles south of Boston. Prof. Rogers adverted to the great interest of this discovery as furnishing the first clear evidence yet obtained as to the geologi- cal age of any of the extensive series of altered rocks which occupy a large part of eastern Massachusetts and the neigliboring States. Hitherto, geologists have not been aware of the existence of any fossil forms in these strata, as none are referred to in the Geological Report of Prof. Hitchcock, or in any of the subse- 28 quent publications relating to the rocks of tliis region. The present discovery, therefore, will be a matter of surprise as well as gratification to those who have given attention to this obscure, and hitherto unproductive, portion of our geology. It is true, that in view of the lithological characters of these altered roclis, and their relation in strike and position to tlie car- boniferous strata adjoining them towards the southwest, in the contiguous parts of Massachusetts and Rhode Island, they have of late been considered as probably belonging to parts of the Paleozoic series, inferior to the coal measures, and including por- tions of the Devonian and Silurian systems. But the want of any positive evidence derived from fossils has, until now, left us without a clue to the actual Paleozoic age of any part of the group, and has indeed given a character almost purely conjectural to speculations in regard to the epoch of the group at large. In respect to the zoological relations of the Braintree Trilobite, Prof. Rogers remarked, that from the imperfect examination he bad as yet given these fragmentary specimens, lie was dis[)Osed to consider it as closely allied to the forms of Paradoxides, de- scribed by Green, in his monograpli of North American Trilo- bites. Of the two species described by Green, viz: P. Harlanl and P. Boltoni, only the latter has been recognized by Prof. Hall among our Appalachian fossils. This, under the generic head of Platynotus, and more recently of Lichas, he describes as a characteristic form of the Niagara group. Leaving the pre- cise affinities of our fossil for future examination, there can be no hesitation, from its general facies, in referring it and the in- cluding strata to a date among the more ancient of the Paleozoic formations. The rock in which these fossils occur is a ratlier fine-grained? bluish-gray, siliceous slate or slaty sandstone, forming part of a narrow belt of siliceous and argillaceous slates and grits ranging along the northern edge of Braintree. The fossiliferous layers are exposed in a quarry, vvhicli has been wrought for several years past to obtain ballasting material for some of the wharves in Boston, within which no doubt many of these fossils might be found among the piles of stone. The fossil casts occur not only on the parting surfaces of the strata, which are covered by a somewhat argillaceous and ochreous coating, but also in the 29 interior of the mass, whence, however, they are less readily spparated for examination. It appears that the proprietor of the quarry, Mr. E. Ilayward, and his family, have for some time been familiar with the occur- rence of these so-called images in the rock, without a suspicion of their having any scientific value. But it is to the kindness of Peter Wainwright, Esq., a member of this Society, who resides in the neighborhood, that Prof. Rogers has been indebted for the first suggestion which led to tlie investigation of this unique and most interesting locality. Tlie range or strike of the fossiliferous belt is about N. 70 E., and the dip in the quarry N. 20 W., at an angle of about 45 degrees. Adjoining it on the northwest side, are exposures of a more argillaceous and indurated slate, greatly broken up by joints and irregular cleavage planes, and at a short distance further on in the same direction, these altered sediments give place to tiie granitoid and sienitic masses so extensively quarried in the town of Quincy. In crossing the strata towards the south, we meet with slaty and gritty rocks, becoming more and more indu- rated as we proceed, which, passing into beds of a semi-crystalline character, are quickly followed by another range of Sienite. Thus the fossiliferous belt is actually included, in this part of its range at least, between large masses of igneous rock ; and it is not a little surprising that, under conditions so favorable to meta- morphic action, the fossil impressions should have been so well preserved. This discovery of well-marked fossils among the rocks of eastern Massachusetts, where hitherto their existence could scarcely have been suspected, may well lead us to hope that careful research in other parts of this region of altered sedi- ments will bring to light fossil organisms not less interesting in their scientific bearings than the Braintree Trilobite. Dr. C. T. Jackson observed that Mr. Fi-ancis Alger had a fossil, apparently identical with these and imbedded in a similar rock, which was obtained at the sale of the old Columbian Museum, in this city. Its origin was unknown. Dr. Hayes remai-ked, that it was with the deepest interest that he had listened to the announcement of the discovery made by 30 Prof. Rogers. The new and important facts, now made known by that gentleman, throw a clear light on what was obscure, and enable us to generalize many isolated observations made in this vicinity, which without them had no scientific basis ; and it must be the wish of all, that Prof. Rogers would give his attention further to this subject. Incidentally connected with the discovery of Prof. Rogers, are some observations he had himself made, while pursuing a research on the origin of the saline matter found in the waters which tra- verse the rocks and drift of this part of the State. These rocks, in the simplest form of expression, are broken down granite, the resultina: sand being recemented to form aoforregates, to which we mineralogically apply different names. It is to the material of this cement that he would call attention, as numerous experi- ments have shown that it is the source fiom which the waters take their saline matters, when percolating these rocks. Not only are the chlorides of the metals forming alkalies when oxidized present often, but we find salts of lime, which did not probably preexist in the sand or original rock. The sulphate, phosphate, carbonate, and crenate of lime are thus found, and when the aggregate reposes on other rocks, these salts are imparted to them in considerable amount. Thus, the Argillite of Charlestown is an example of quite a collection of lime salts, associated with the proto-persilicate of iron. In other parts of New England, when the argillite passes into roofing slate, and again where the metamorphic changes have occurred, we find either these salts, or the minerals into which they have passed. Now these lime salts are foreign matters of interest, for they most commonly claim an organic origin, and associated as they generally are with iron salts, which have retained some portion of protoxide, in consequence of the pres- ence of organic matter or carbon itself, they afford indicative evidence of the presence of organic matter, earlier in geological age than the organized forms which abound in other rocks. Dr. Charles T. Jackson read the following paper on the coal formation of Deep River, North Carolina : — During the month of May last, I had an opportunity of re- examining the coal fields on Deep River, North Carolina, and of 31 tracing llie out crop of the coal bed some miles further to the southwestvvard and across Deep River from Murchinson's to Forsliee and Street's Plantations. I had also the satisfaction of descending into the shaft sunk in the plain of Egypt, wliere two years since I directed borings to be made, by which the occurrence of coal beneath that plantation was discovered, and its extent under the table lands demon- strated. This shaft, sunk under the immediate direction of Mr. Wm. McLean, is admirably constructed, is 8 feet by 15 square, and penetrates to the depth of 4G2 feet, where it traverses the coals. At the bottom of this shaft I measured the following section : Coal .... Black band iron ore Coal .... Fire clay Coal .... Fire clay and shale at bottom. The strata and coal beds dip from 16 to 20° S. 10'' W. The aggregate thickness of the coal that can be taken out together in the ciiambers, is 5 feet 11 inches in thickness. These coals are quite free from sulphur, and are highly esteemed by the superin- tendent of the Brooklyn, N. Y., Gas Works, as good gas-making coals. They are also particularly valuable in the forges, since they make a perfectly hollow fire by coking readily. They also will serve for steam-engine and other fuel. On chemical examination, this coal was found to yield per cent — Fixed carbon . . . . . .63.6 Illuminating gas ..... 34.8 Red-brown ashes . . . . .1.6 16 inches 22 u 6 a 7 u 100.0 When converted into coke, it was found to produce 65^^^ per cent, of good solid coke. The black band iron ore is too sulphurous to admit of its being converted into good iron, it retaining 0.89 per cent, of sulphur even after thorough roasting. . 31.30 . 47.50 . 8.81 . 3.39 . 9.00 32 It yielded on analysis, per cent. — Coal Peroxide of iron .... Carbonic acid and moisture Sulphur ...... Siliceous .matter .... The oxide of iron was originally a protoxide iron ore, but was separated as a peroxide. At one time, the geological age of the Deep River coal for- mation was a subject of dispute among geologists; some main- taining that it belonged to the New Red, and others to the OoUiic or Lias group. Through the researches of Prof. Emmons, State Geologist to North Carolina, this question is likely to be finally settled ; and it appears from his geological map, a copy of which he kindly gave me, and from his fossils which I have inspected, that the lower portion of this formation is Triassic or of the New Red Sandstone group, and the Upper Liassic. Among the fossils discovered in the Deep River coal-bearing rocks, are numerous teeth and bones of saurian reptiles, coprolites of saurians and of fishes, and an abundance of scales of ganoid fishes resembling Catopterus of Redfield. Several species of Zamias, both the trunks and leaves, are also found. These will all be described in Prof. Emmons's Report, and will be repre- sented by wood-cuts. I understand that this Annual Report is now in press at Raleigh, N. C. CHEMICAL ANALYSIS OF A VARIETY OF AGALMATOLITE. BY C. T. JACKSON. A remarkable rock, supposed until now to be soapstone or talcose rock, was discovered a few years since on the borders of the Deep River coal-field, and was quarried as soapstone, but found unsuitable for lining stoves and furnaces, on account of its ready exfoliation when heated. Lately, other uses have been found for this beautiful material, for when ground it is a delicate white satin-like substance, and is similar to China clay. It is ground and bolted, and sold in New York at $40 per ton. I suppose it is employed to mix with 33 white lead, and it is said to be used also for the adulteration of fancy soaps, and also for glazing or satining wall-papei*. By chemical analysis, I find this rock is composed of, in 100 grains — Silica . . 75.00 Alumina . . 18.75 Potash . , . , , . 2.00 Water . . 3.50 Traces only of oxide of iron . 99.25 It is therefore Agalraatolite. Remarks upon the Deep River Coal Formation were also made by Prof W. B. Rogers. Dr. Hayes asked what chemical evidence Dr. Jackson had that the North Carolina or Deep River coal is a gas coal. Dr. Jackson replied, that his experiments were made in the usual manner, in covered platinum crucibles, (which represent very perfectly the gas retorts,) and that he found the North Carolina coal to produce Si-^^ per cent, of coal gas, which burned with a brilliant yellow and highly illuminating flame, without smoke, and did not give any sulphurous acid, or other disagreeable products, while the coke resulting from torrefaction of the coal was found to be of superior quality, giving less than two per cent, of ashes when burned. Practical trials, made with this coal at the Brooklyn, N. Y., Gas Works, had fully proved its excellence as a gas coal. To this Dr. Hayes added, that an experiment thus made hardly demonstrated, in his opinion, that the coal was a gas coal. The amount of volatile matter given off from any coal, varies with the rapidity or slowness of heating it, and may be made up of vapor of water formed from the constituents of the coal, and heavy vapors producing coal tar, together burning with a bright flame, from a coal wholly unfit for making gas. The coals of our Western States, and those of Scotland, offer fine illustrations of the error which might be committed in an experiment of this kind ; some affording a large volume of rich gas under a small PROCEEDINGS B. S, N. H. VOL. VI. 3 DECEMBER, 1856. 34 percentage of volatile matter, and others with a large amount of volatile matter burning brilliantly, but producing very little gas. The distinction between gas coal and bituminous coal, can be learned by more complete processes only, and his own experience on this coal, soon after it attracted public notice, and with strong hopes that it would prove a gas coal, did not lead to such a con- clusion. Dr. D. F. Weinland called the attention of the Society to a question now discussed in the European journals of Ornithology, viz : The cause of the change of color in the feathers of birds, and in the hairs of Mammalia, and the manner in which this change is effected. It is a well known fact that many birds, particularly the males, have a very differently colored plumage in ditferent sea- sons ; for instance, that the male of many singing birds has a far more beautiful plumage in the reproductive season than during the rest of the year ; furthermoi'e, that many northern birds and mammalia become pure white in winter, while they are yellow, red, brown, gray, or of a still darker color in summer. Till within the last few years, this change of color was sup- posed to be effected simply by the production of a new feather or hair ; but there are on record several instances which are entirely at variance with this supposition ; and Dr. Weinland was of the opinion, that, although this change is generally produced by molting, many instances are proved, by past and recent obser- vations, in which it has taken place without loss of the feather. Human Pathology has shown many cases, in which the hair of men, from sudden terror or from grief, has turned gray or white in so short a time (sometimes in one night) that there was no possibility of a change of the hair itself. A case is known in Ornithology, in which a starling in one day became white all over, after being rescued from the claws of a cat. These facts, however, seemed to be exceptions only, till quite recently some distinguished Ornithologists — Schlegel in Leyden, and Martin in Berlin — at the same time affirmed that many birds get their wedding plumage without molting. Experiments were made by many Ornithologists; some affirmed 35 the new statement, others denied it. But the most striking ob- servation which had come to the knowledge of Di-. Weinland, was made by a friend of his, Mr. Junghaus, of Berlin, on a Blue- throated Warbler, (Sylvia suecica,) which he had in a cage. From June, 1854, till the middle of February, 1855, the throat of this bird, from the bill down to the breast, was pure white ; over the breast ran three bands, blue, black, and yellow, the black one being the narrowest. In the middle of February, the blue band became darker, and spots of the same color appeared all over the white throat, with the exception of a small spot in the centre. On the 21st of February, all the throat was blue except that spot, which remained pure white till the 23d, when it became reddish. On and after the 24th, this reddish color also changed to blue ; but on the 1st of March there appeared again, in the midst of this blue, a lighter spot of beautiful silvery appear- ance ; and it is worth remarking, that this new color began at the basis of the feather, and proceeded outwards. Meanwhile, the black band on the breast had become larger, and shaded insensibly into the blue, while the yellow band remained un- changed through all these mutations. Thus the bird had got its wedding-plumage, without losing one feather, and this it kept through all the reproductive season. At the same time, Dr. Gloger, of Berlin, showed that a very similar observation had been previously made in this country by Audubon, on a male gull, which changed the color of its head, in a fortnight, from gray to the purest black, and, as he supposed, without changing a feather. There can be no longer any doubt about the fact ; but the question is, how can a feather change its color, when its blood- vessels and nerves are dried and dead, as is the case with every feather soon after it has reached its full growth. Dr. Weinland had only heard of one explanation, viz : that the wearing away of the fine laminae of the veins of the feather, the so-cqlled pinnul^e, might produce the change of color. This seemed to him not only an unphysiological view of the subject, that a bird should get its wedding-plumage by such a kind of decay of the feather, but, in the cases which he had observed, the changed feathers showed no traces of such a wearing process. The fol- lowing explanation of the fact seemed to him the most natural : 36 Conservators of museums very frequently notice that certain birds in the collections bleach, particularly Avhen exposed to light. A red-breasted Merganser {Mergus merganser) which Dr. Weinland saw, when just shot, with a red breast, and which, after having been deposited in the museum for some time, pre- sented a pale whitish breast, showed this very remarkably. He afterward obtained a bird of the same kind, and, when fresh, examined its breast-feathers with a high power of the micro- scope, and found all the pinnulte filled in spots with lacunes of a reddish fluid, which, from the dark appearance of their margins, seemed to be of an oily character. Some weeks afterwards the same feathers, having been exposed to the light, had become nearly white, and he found in the pinnulje, instead of the reddish lacimes, only air-bubbles, which it is known produce a white color, as in the case of the lily, which is rendered white by the air in its cells. This observation led him to the conclusion, that in this case the evaporation of the reddish fluid, and the filling of the spaces with air, produce the change of color. If this fluid is an oily matter, as there is reason to suppose, it will be readily admitted, physiologically, that it may be furnished by the organ- ism, by imbibition through the tissues, in consequence of a certain disposition of the nerves leading to the skin and to the sac of the feather in the skin, (even if the vessels and the nerve in the feather itself should be dried,) for fat goes through all tissues without resistance, and also through horn. Thus the fat coloring matter may flow out into the feathers during the time of reproduc- tion, which is the richest season in every living organism ; and then again, from want of food, cold temperature, weakness, decrepitude, or from strong emotions of the central nervous system, from sudden terror or grief, — the same coloring fat may be called back to furnish the suffering organism. This process, effected by different physiological conditions of the organism, seems to be a reasonable explanation of the fact, that many northern mammalia and birds become white in winter, while they ai'e dark-colored in summer ; that the hair of men or mamraaha, or the feathers of birds, may become suddenly gray or white from sudden terror, hard labor, or debility, while they are dark colored in mature life or in the more vigorous sea- sons of the organism. And if we add the hypothesis, that in the 37 oily fluid there may take place still other chemical processes, efl^ected by difFerent conditions of the nervous system, such as oxidation or deoxidation, we may explain in this way still other changes^of color; for instance, from yellow, through red, to black ; which, from observations made during the last winter, seems to be really the case in certain turtles (^Emys picta and marginata). Mr. Charles J. Sprague exhibited specimens of the Phallus duplicatus, Lin., in its immature as well as mature condition, and read an account of its structure and mode of growth. In conclusion, he remarked that this fungus is not common, though it is found from time to time after rains in shady places. Its odor is intolera- bly strong and disagreeable ; but the strangeness as well as beauty of its structure will repay an examination, which may particularly offend the sense of smell. It is common in Europe, and has been described and figured by most of the writers upon Mycology. Prof. Agassiz remarked that he was not aware that this fungus is rare in this country. He had observed it in his garden at Cambridge. He thought the American had a different shade of green from the European, though this had not been noticed by Mr. Sprague. He had a large specimen preserved in alcohol, which he should like to compare with the European plant. Prof. Agassiz stated that Dr. Augustus Miiller had recently pubHshed a paper on the Embryology of Petromyzon, (the Lamprey,) presenting facts hardly to be credited if they had not emanated from such authority. In the family of Cyclostome Fishes, thei^e have been placed two characteristic genera, viz : Petromyzon and Ammocetes. From the egg of Petromyzon, Miiller says he has raised Ammocetes, and he has likewise seen the latter become a Petromyzon. It is now well established, that fishes undergo a form of metamorphosis as well as insects. Prof. Agassiz had himself, within a few weeks, had an opportunity of studying the embryology of a species of shark {Acantheus Ameri- 38 canus). He had found the yolk, not surrounded by an amnios, but resting in the centre of an area vasculosa, and presenting, in its early development, other peculiarities only known to exist in the egg-laying vertebrata. He considered Plagiostomes a dis- tinct class of animals from fishes, and he thought it probable that Cyclostomes should also be separated as a class. He could not refer to one class animals developed in such different modes. The number of classes into which the animal kingdom is divided — into six by Linnteus, into sixteen by Cuvier, and into twenty- nine by Ehrenberg — shows that anatomical differences are in- sufficient for a proper determination of classes. He proposed that the general plan of structure be a test for types, and the manner in which this plan is developed the test for classes. Prof. Agassiz, in alluding to the probability of a fecundation of the egg whilst in the ovary, a question discussed at the last meeting, stated that Dr. Weinland had found, in the viviparous Zoarces anguillaris, that the ovarian bag (Graafian Vesicle) of the mature eggs was not a simple sac, but a double one ; and further, that this double sac was not continuous over the com- plete circumference of the egg, but that a disc of considerable size remained uncovered at the upper part, where the spermatozoa might come in contact with the yolk membrane. Dr. Weinland had also found the same condition in the skates and turtles. Pi'of. Agassiz thought that the same organization would be found in all Vertebrata. Mr. Charles Stodder informed the Society that Mr. Samuels, the Society's Collector, had returned from California. Mr. Samuels reports that he arrived at Petaluma, California, December 1, 1855, and left, in consequence of ill health, on the 4th of July, 1856. He explored the country, and collected specimens, in the distance of twenty miles east, north, and west of Petaluma, being portions of the two counties of Sonoma and Marine. He has sent to the Smithsonian Institution eleven large boxes, containing between 900 and 1000 species, and many thousand specimens. 39 He has received important and valuable assistance from his brother, Mr. Uriah Samuels, who collected while he was sick or engaged in putting up and preparing the specimens, besides giving him a home for the whole time, without which it would have been impossible to have accomplished so much, with the small funds pro- vided. It was voted that the thanks of the Society be pre- sented to Mr. Uriah Samuels for his kindness, and for the valuable assistance rendered the Society. Mr. Whittemore read a letter from Mr. J. A. Conrad, of Philadelphia. Mr. C. desires to collect specimens of shells and fossils in the Western States for the Society or for individuals. It was voted that a report of the late excursion of the Society to Hingham be entered upon the records of the Society. The Corresponding Secretary acknowledged the re- ception of the following letters, viz : From Robert Ken- nicott and James C. Parkinson, returning thanks for election as Corresponding Members, and offering to transmit communications ; from the Madison, Wiscon- sin, Historical Society, requesting an interchange of pub- lications ; from Edward Charles worth, requesting an exchange of the Journal for the publications of the York- shire Philosophical Society ; two communications from the Royal Academy of Sciences at Madrid. 40 September 3, 1856. The President in the Chair. A letter was read from M. Alexis Perry, of Dijon, France. A letter was read from Dr. Samuel Kneeland, Jr., notifying the Society of his resignation of the office of Curator of Ichthyology, and presenting a catalogue of the Comparative Anatomy Cabinet, a portion of the catalogue of the vertebrata which he had undertaken to complete. A communication was read from the city authorities, inviting the Society to unite in the ceremonies of the inauguration of the statue of Franklin. It was voted to accept the invitation, and a com- mittee, consisting of Messrs. Stodder, Jackson, and Whit- temore, was appointed to make the proper arrangements. Dr. Durkee, in behalf of the committee appointed to consider the question of purchase of the Entomological Cabinet of the late Dr. Harris, reported, that the com- mittee had examined the collection and found it in perfect preservation ; containing between four and five thousand species of American, besides a collection of foreign insects. The committee proposed that a sum of money should be raised, by subscription, for the purchase of the cabinet. Messrs. Amos Binney and James M. Barnard were added to the committee. The Secretary read the following communication from Prof. William B. Rogers : — So far as I have yet explored the quarry in the Quincy and Braintree belt, containing the remarhahle fossil Trilobites to 41 which I referred at the preceding meeting of the Society, I find that they belong chiefly, if not altogether, to one species, which, on the authority of Agassiz, as well as my own comparison with Barrande's descriptions and figures, is undoubtedly a Paradoxides. Of its specific affinities I will not now speak, further than to remark that the specimens agree more closely with Barrande's P. sphiostcs than with any other form. As the genus Paradoxides is peculiar to the lowest of the paleozoic I'ocks in Bohemia, Sweden, and Great Britain, marking the Primordial division of Barrande, and the lingidar flags of the British survey, we shall probably be called upon to place the fossiliferous belt of Quincy and Braintree on or near the horizon of our lowest paleozoic group, that is to say, somewhere about the level of the Primal rocks, the Potsdam Sandstone and the Pro- tozoic Sandstone of Owen, containing Dikelocephalus in Wis- consin and Minnesota. Tims for the flrst time we are furnished with data for fixing conclusively the paleozoic age of any portion of this tract of ancient and highly altered sediments, and what is more, for defining in regard to this region the very base of the paleozoic column, and that too hy the same fossil inscriptions which mark it in various parts of the old world. One of the most curious facts relating to the Trilobite of the Quincy and Braintree belt, is its seeming identity with the Para- doxides ffarlani, described by Green, in his monograph of North American Trilobites. This description, which is quite imperfect, was made out from a specimen of unknown locality procured some twenty-five years ago, thi'ough Dr. Harlan, from the collection of our well-known mineralogist, Mr. Francis Alger. The identity is, I think, established by the comparison of a nearly complete specimen of the Braintree fossil with the cast of P. Harlani taken from Mr. Alger's specimen, the original never having been returned. Considering the perfect agreement in lithological character of the matrix as described by Green with that of the Quincy fossils, and the immediate recognition of this agreement in mineral features by Mr. Alger on seeing my Quincy speci- mens, we can hardly doubt that the original specimen of P. Harlani come either directly, or through the drift scattered in the vicinity, from the same fossiliferous belt. 42 Dr. C. T. Jackson presented to the Society a cast of a very perfect specimen of the Trilobite (Paradoxides Tessini, or Harlani.) mentioned in Prof. Rogers's paper, which was obtained by him from the slate quarry at Braintree, on the 9th of August last. He also exhibited a cast of the specimen referred to by Prof. Rogers, which, from the character of the rock, he thought was undoubt- edly obtained from the same ledge, and which was pur- chased by Mr. Francis Alger, at the breaking up of the old Columbian Museum of Boston, some twenty-five years ago, and was originally presented to that museum by some one residing in this vicinity. Mr. Alger's specimen is in a sharj), angulai", prismatic mass of rock, having all the appearances of having been broken from the rocks in place, and certainly was not a boulder. From the existence of this specimen, and also from the frequent discovery of fragments of Trilobites in the erratic rocks on George's Island, geologists were prepared for the discovery of them in some of the ledges of this neighborhood, but no one ever thought of looking among the pinched up and metamorphic slates between the Quincy and Braintree Sienito hills for any fossils, until they were actually disclosed by the quarrying opera- tions of the Messrs. Haywood at Braintree ; and one of our members, Peter Wainwright, Esq., recognized them as trilobites, and as subjects of great scientific interest, and called the atten- tion of professed geologists to the locality. About five years ago, Mr. Eliphas Haywood first observed these fossils on opening his stone quarry for the purpose of obtaining underpinning and ballast stones. Without knowing their nature, he still looked upon them as interesting curiosities, and laid aside the specimens which have lately been brought before this Society. He showed them to Mr. Wainwright, who at once recognized them as trilobites, and brought them to Boston for the inspection of geologists, and presented two specimens to our associate. Prof. Wm. B. Rogers, to whom the Society is indebted for the first notice of these remarkable fossils, so important in the determina- 43 tion of our geognostic horizon. A few days after Prof. Rogers's visit to the quarry, Dr. Jackson, by invitation of Mr. Wainwright, visited it, and made a minute examination of all the geological phenomena which it presents, and obtained specimens of the trilobites through the kindness of Mr. Haywood, and by search at the quarry in company with Mr. Wainwright. Two speci- mens were obtained, one entire, which is 8^ inches long and 4 inches wide. The other, of which only the head and half the body was obtained is 6 inches wide, and its hood is 7-^ inches across by the base of the head ; hence the length of this specimen must have been 12^ inches at least, which is about the size of the largest specimens of the Paradoxides Tessini discovered in Sweden. The smaller individual has twenty-one articulations, but none in the tail beyond the lateral appendages, and in this respect differs from the P. Tessini, its nearest analogue, which has, according to Brongniart, four faintly marked depressions or folds crossing the tail transversely. They may have been oblit- erated in our specimen by the changes the rock has undergone. These Trilobites of Braintree occur in a blue gray argillaceous slate, containing silicate of lime, but no carbonate, and some disseminated iron pyrites. The stratification of the rock, as indicated by its grain and cleavages, dips to the north 50'', and runs east and west. It is but slightly altei'ed by heat in those portions where the trilobites are found, but near the Sienite rocks it is filled with nodules of Epidote, and closely resembles the altered slates of Nahant. There is a small vein of quartz, bear- ing iron pyrites in it, which cuts through the slate strata at right angles. There are also slickensides surfaces on some of the cleavages or joints in the quarry, indicating, as is supposed, the polishing effects of rapid earthquake movements at the period of disturbance of the strata at the time of their disruption by in- truded Sienite. These are all the marks discoverable of meta- morphic action of igneous rocks on their sedimentary strata, though the slate rocks are hemmed in by the Sienite rocks on both sides, and the belt of slate is quite narrow. On a hill near the quarry. Dr. Jackson could see the tall steeple of the Baptist Church in Somerset Street, Boston, and on taking its bearings with the compass, it was found to be 44 N. 10° W. ; and Nahant would be a little to the east of north. The Braintree rocks would then dip under those of Nahant, unless the same formation extends across the bay ; in which case, the Nahant series would form its upper strata. The existence of these Paradoxides in the argillaceous slates of Braintree, proves them to belong to the lowest of the fossil- iferous Silurian rocks, and that they are the geological equivalents of the argillaceous slates of Sweden, which are in a similar manner disrupted by the intrusion of Sienite. It is certainly interesting to find the base of the silurian system resting within the limits of old Massachusetts. The President stated that he had recently examined the electric apparatus in the tail of one of our common skates {Raia Icevis). The electric organs have been noticed by several anatomists, but have been fully described in Raia hatis and other species by Robin. . In the species dissected by Dr. Wyraan, the organs were more largely developed, extended further up into the base of the tail, and were more uncovered by the muscles, posteriorly, than in the ones examined by Robin. Thus far, no positive proof has been adduced to show that the organs in question really constitute an electric apparatus. Structurally they resemble those of the Torpedo and Gymnotus, but have not been observed to evolve electricity, though it has been stated that if a living skate is held by the tail, an electric shock is felt. The President also stated that he had seen the horny shell of the egg of the skate in the process of formation. He had found one in each oviduct, surrounded by the glandular enlargement which is visible near its middle. That portion of the duct was very much thickened, and mainly consisted of long tubular follicles, opening into its cavity. Although the shells were partially formed, the yolks had not yet descended into the duct; many of them were nearly mature. If this be a normal state of things, then we have, thus far, an unobserved example of the shell being formed previous to the descent of the ovum. The shell forms a pocket, open at the upper extremity, and through this opening, which is never wholly closed, the egg probably descends into its cavity. 45 Dr. Durkee exhibited specimens of Goliathus giganteus^ from the interior of Africa; a male and female Katy-did, {Platyphyllum concavum,) from Milton, Mass. ; and two male specimens of Spectrum femoratum, Say, commonly known as Walking Sticks, from Brookline. Dr. Keep presented a cast of a fourth molar tooth, occurring in the left side of the upper jaw of a human subject. The tooth was not of full size. The President observed that there was a fourth molar in the skeleton of the Chimpanzee in the Society's Cabinet. The following gentlemen were elected Corresponding Members, viz : Winthrop Sargent, of Natchez, Miss. ; Dr. John S. Newberry, of Cleveland, Ohio; William F. Robinson, of Ceres, McKean Co., Penn. ; and John R. Blake, of Greensboro', Ga. The following gentlemen were elected Resident Mem- bers, viz : Albert Fearing, S. H. Pearce, Augustine Shurt- leff, John S. Foster, and Frank D. Cobb. DONATIONS TO THE MUSEUM. July 2d. A collection of Shells, including eighty-seven species from Herkimer Co., N. Y., and twenty species from Georgia, Alabama, and Ohio; presented by Dr. James Lewis, of Mohawk, N. Y. ( Virle catalogue on p. 1, Vol. VI.) July 16th. Parasitic Crustaceans known as Salve Bugs ; by Mr. Addison Gott, of Rockport, Mass. A Serpent and Salamander, from St. Mary's, Elk Co., Penn. ; by Dr. C. T. Jackson. A Bat, from Cuba; by Dr. A. A. Gould. A Rattlesnake, Croialus dur'issits, killed in Milton, Mass.; by Dr. C. C. Holmes. Two specimens of Argus Pheasant, Argus giganteus, male and female, from Malacca; by Oscar Gassett, Esq. Salmo erylhrogaster, from Moosehead Lake ; two specimens of Salmo fonlinalis ; a specimen of a probably undescribed species from the Great Schoodic Lakes ; two Smelts ; and three specimens of different species of Alosa, from the Penobscot River and the sea near its mouth ; by Dr. S. Kneeland, Jr. August 6tb. A bottle of Fishes from the western coast of Africa; by Mrs. George S. Hillard. Sept. 3d. A collection of specimens from California, consisting of Birds, Mam- mals, Corals, and Molluscs; by James Tallant, Esq., of Concord, N. H. Two young Sea-Turtles, from Penang, E. Indies; by Capt. George E. Tyler, of Dor- 46 Chester. Three specimens of Prairie Massasanga, Crotahphorus tergeminus ; three Spotted Water-Adders, Nevodia sipedon ; Prairie Water- Adder, Rer/ina Gra- hamii; Eutamia proxima, E. radix, E. sirtalis ; Green Snake, Coluber vernalis ; received in exchange from Robert Kennicott, Esq., of Illinois. Two specimens of Hyla triseriata ; one of Hemidactylum scutatum ; one of Ameira sexlineata ; two of Salamandra symmetrica ; two of Salamandra of unknown species ; one of Amhystoma punctata ; two of Amhystoma lurida ; two of Cestudo Blandingii ; ten of Emys picta ; two of Heterodon 2)latyrrhinos ; by Dr. J. N. Borland. BOOKS RECEIVED DURING THE QUARTER ENDING SEPT. 30, 1856. Gliederung der Bevolkerung des Bayern. Von Hei-mann. 4to. Pamph. Miinchen, 1855. From the Author. The Red Sandstone Formation of Pennsylvania, and Genera and Species of Shells. Isaac Lea. 8vo. Pamph. Philadelphia, 1856. From the Author. American Geology. Bj^ Eben Emmons. Vol. I. 8vo. Albany, 1855. From the Author. Annual Report of the Trustees of the New York State Library. 8vo. Pamph. Albany, 1856. From the Trustees. Memoires de la Soci^t^ Royale des Sciences de Liege. Tome X. 8vo. Li^ge, 1855. From the Societe Royale. Plantse Kaneanse Grajnlandicce. By E. Dnrand. 4to. Pamph. 1856. -From the Author. Rede in der offentlichen Sitsung der Konigl. Akademie der Wissenschaften. Von Thiersch. 4to- Pamph. Miinchen, 1855. From the Author. History and description of the Skeleton of a New Sperm Whale in the Aus- tralian Museum. By Wm. S. Wall. 8vo. Sydney, 1851. From the Aulhoi: Thii'd supplement to Dana's Mineralogy. 8vo. Pamph. 1856. From the Author. Synopsis of Entozoa and some of their Ecto-congeners. By Joseph Leidy, M. D. 8vo. Pamph. Philadelphia, 1856. Descriptions of some Remains of Fishes from the Carboniferous and Devonian Formations of the United States. Also, Descriptions of some Remains of Ex- tinct Mammalia. By Joseph Leidy. 4to. Pamph. Philadelphia, 1856. From the Author. Memoirs of the American Academy of Arts and Sciences. Vol. V. New Series. 4to. Cambridge and Boston, 1855. Proceedings of the American Academy of Arts and Sciences. Vol. III. pp. 185-248. 8vo. 1855-6. From the Academy. Description of a New Genus of Crinoidea. By L. P. Yandell, M. D. 8vo. Pamph. 1856. Notice of a Fossil Genus, Blastoidea, from the Devonian Strata. Kentucky. 8vo. Pamph. By B. F. Shumard, M. D., and L. P. Yandell, M. D. 1856. From the Authors. Statistical Information relating to certain Branches of Industry of Massachu- setts. By Francis DeWitt. 8vo. Boston, 1856. Third Annual Report of the Secretary of the Massachusetts Board of Agricul- ture. 8vo. Boston, 1856. From C. L. Flint. 47 Proceedings of the American Philosophical Society. Vol. VI. No. 55. Phil- adelphia, 1856. Silliman's American Journal of Science and Arts. No. 64, for July, 1856. 8vo. New Haven. Gelehrte Antzeigen herausgegeben von Mitgliedern der K. Bayer. Akademie der Wissenschaften. Band 40, 41. Proceedings of the Royal Geographical Society of London, Nos. 1, 2. 8vo. Pamph. London, 1856. New York Medical Times. Nos. 10, 11, 12. New York Journal of Medicine. Vol. I. Nos. 1, 2. Proceedings of the Academy of Natural Science of Philadelphia. Vol. VIIL No. 3, pp. 101-138. 8vo. Philadelphia, 1856. Proceedings of the Essex Institute. Vol. I. 8vo. 1848-56. Salem, Mass. Received in Exchange. Annals and Magazine of Natural History. Nos. 102-105. London, 1856. Quarterly Journal of the Geological Society. Nos. 45, 46. London, 1856. Genera of Recent Mollusca. By H. and A. Adams. Part 26. London, 1856. Proceedings of the Zoological Society of London. Part 22, for 1854. Illus- trated. Monographia Auriculaceorum Viventium. Auct. L. Pfeiffer, Dr. 8vo. Pamph. CasseUis, 1856. Cj'clostomaceen. Zweite Abtheilung. Bearbeitet von Dr. L. Pfeiffer. 4to. Niirnberg, 1853. From the Courtis Fund. Life of George Washington. By Washington Irving. Vol. HI. 8vo. New York, 1856. History of Massachusetts — The Provincial Period. By J. S. Barry. 8vo. Boston, 1856. Narrative of the Expedition of an American Squadron to the China Seas and Japan in 1852-4, under the command of Commodore M. C. Perry, U. S. Navy. By F. L. Hawks, D.D., LL.D. 8vo. New York, 1856. History and Antiquities of Boston, from 1630 to 1770. By S. G. Drake. 8vo. Boston, 1856. Works of John Adams. With a life of the Author. By C. F. Adams. Vol. I. and X. 8vo. Boston, 1856. Deposited by the Rejmblican Institution. October 1, 1856. The President in the Chair. Dr. S. L. Abbot was chosen Secretary, pro tern. Prof. Agassiz called the attention of the Society to several living specimens of young Gar-pikes, from Lake Ontario. 48 They were remarkable, he said, as still preserving certain em- bryological characters. The most conspicuous of these vvas the prolongation of the vertebral column in the form of a fleshy filament, distinct from the caudal fin, which had at times a vibrat- ing motion, involuntary, and quite distinct from the motions of the tail itself, as is seen in some embryos. This singular formation shows that the caudal fin is properly an appendage to the lower surface of the dorsal column, a true second anal, and not the proper termination of the column. The specimens exhibited showed their affinity to reptiles, by their motions and attitudes ; the spine being more flexible than in ordinary fishes, and their position, when at rest, being frequently more or less bent, par- ticularly towards the tail ; peculiarities arising from the ball and socket joints of the vertebrae, — a proper reptilian arrangement. The manner of feeding also is unlike that of fishes, and resem- bles that of reptiles. Other fishes take their food with open mouth, and swallow it at once ; but this one approaches its prey slyly, sidewise, and suddenly seizing it holds it in its jaws, until, by a series of movements, it succeeds in getting it into a proper position for swallowing, as is the habit with alligators and lizards. The ball of food in the body of this fish is seen to move gradu- ally, as it distends the body in its progress, from one end to the other, as is seen in snakes. This fish is also remarkable for the large quantity of air which escapes from its mouth. The source of this Prof. Agassiz had not been able satisfactorily to determine. At certain times it approaches the surface of the water, and seems to take in air, but he could not think that so large a quantity as is seen adhering in the form of bubbles to the sides of the gills could have been swallowed, nor could he suppose that it could be secreted from the gills themselves. These differ- ent interesting facts were noticeable in the specimens exhibited, which were fed for the occasion on live minnows, the only food they could be persuaded to take. Dr. A. A. Hayes read by its title the following paper — ON THE STATE IN WHICH PHOSPHATE OF LIME EXISTS IN SEA-WATER. In a description given to the Society of a consolidated phos- phate of lime, arising from the action of atmospheric agents on 49 the arenaceous remains of the fish food of fowls of the Atlantic islands, I alluded to the chemical process by which this solid was formed. The solubility of the altered material, in water, was also pointed out, the experiments on which these statements were founded having been made two years earlier. At the time of exhibiting some remarkably pure depositions from sea-water, containing phosphate of lime, at a later meeting, want of time prevented me from showing how phosphate of lime exists in sea- water. When bones of fish and of quadrupeds are moistened with sea- water, or pure water, fermentation commences in the gelatinous parts of tissues present, and, under a disengagement of several of the volatile oily acids and ethers, a considerable mechanical change takes place in the bones. Similar etfects attend the changes when the bones are wholly immersed in water; and if the temperature of the sun^ounding air is 85*^ F., after the lapse of six or eight days, the turbid fluid, containing fatty and crenic acids, holds in solution a portion of phosphate of lime. A late chemical journal informs me that M. Wohler, has since made the same observations on ordinary water and water freed from carbonic acid, with the same results ; and he deems them important to agriculturists, who can dissolve their bones in water and apply the solution as a fluid fertilizer. Interesting as this fact of the solution of bones in sea and common water is, the explanation of how it takes place has called for numerous experiments, and the truths arrived at apply to the explanation of other phenomena of interest. Bones immersed in sea-water, ordinary water, or boiled water, dissolve to a very slight extent; rarely more phosphate of lime is present than is due to the simple solution of bone-phosphate of lime in gelatinous fluids. It is to a subsequent action that the increased quantity of bone-phosphate is owing, and this action arises from fermentation. The bones containing gelatine quickly enter into fermentation or putrefy, and the bone-phosphate of lime, consisting of three proportions of lime to one proportion of phos- phoric acid, is presented to the fluid containing carbonic and crenic acids. These acids unite to the lime of the bone-phosphate, and separate, forming carbonate and crenate of lime. By losing in this way one proportion of lime, the phosphate with two pro- PROCEEDINGS B. S. N. H. — VOL. VI. 4 JANUARY, 1857. 50 portions of lime is left, and this, much more soluble than bone- phosphate, remains in solution. As the fermentation proceeds, more lime is removed from the phosphate dissolved, until two proportions of the three usually found in bone-phosphate are actually combined with the other acids. In this fluid, bone- phosphate of lime dissolves to a greater extent than in water, and in the experiments we find it present, so long as excess of bone-phosphate remains. Some experiments have shown that the carbonic and crenic acids have the power of removing still more lime from the mono-phos2")hate remaining, so that the solu- tions approach the state of phosphoric acid dissolved and car- bonate and crenate of lime deposited. This complex action has heretofore escaped attention, probably from the fact that on add- ing solution of ammonia, bone-phosphate of lime falls, and this quantity of bone-phosphate was assumed to be the whole phos- phate dissolved. If, however, the liquor from which the bone- phosphate has been removed, be treated with solution of double chloride of calcium and ammonium, a much more voluminous pi'ecipitate is obtained, arising from the combination of free phos- phoric acid with the new proportion of lime added. There are other chemical relations of interest, but I advert to one only, — the solution containing the mono-phosphate, and even phosphoric acid, from the fermenting mass, is slightly alkaline, and it does not lose this character when heated to the boiling point ; — long boiling, ■with evaporation, gives rise to acidity, which manifests itself slowly but decidedly. We can now explain the solution of the phosphate of lime in the neutral fluids of the tissues in health, and in the secretions and excretions where its presence is indi- cated generally. In sea-water, and in bittern even, bones decompose and dis- solve, but the act is never one of simple solution after the organic changes commence. An elimination of lime by acids momentarily present, converts the bone-phosphate into mono- phosphate, which is a soluble salt, and can exist under the con- ditions in presence of carbonate of lime and magnesian salts. No difficulty attends the experiment of thus separating from sea-water a phosphate containing at least three proportions of phosphoric acid to one of lime, there being present at the same moment in solution, the ordinary tris-phosphate, and in this 51 mixed state the salt uniformly exists. In pi-ecipitates produced in boiling sea-water, and in our analyses, we estimate the phos- phoric acid as a bone-phosphate salt, which is not sti'ictly a coi-rect statement. The results here given allow us to readily explain by simple solution and evaporation the conversion of the granular and finely divided fish bones into a solid, compact rock, Avhere all traces of its granular form are lost. The President gave an account of some fossil bones collected in Texas. For these the Society is indebted to the liberality of Dr. Charles Martin, Surgeon U. S. Navy. They were pur- chased by him while attached to the Coast Survey dui-ing the winter of 1 855-5 G, at the mouth of the Brazos River. They were discovered in the bed of the river, during its low stage, about fifty miles from the coast. The collection is very valuable and interesting, not only as representing three distinct races of gigantic quadrupeds, but as indicating a new locality in the geographical distribution of the animals to which they belonged. It is not a little remarkable that three such genera as Mastodon, Elephant, and Megatherium, should be represented in a collection of no more than eight specimens taken at random. Six of the eight appear to have undergone similar changes of density and mineralization ; these are the Symphysis of the lower jaw, an ultimate Molar, and the Femur of an Elephant, the Tibia of Megatherium, and the two Molars of a Mastodon. The others are lighter colored, and much less dense. Coming as they do from the bed of a river, it is impossible to determine how far they were originally associated in the same geological formation. It is not impossible that those first mentioned were from the same locality. 1. Symphysis of the lower jaxo of cm Elephant. — The branches of the jaw were broken ofi" on both sides ; that of the right a little in advance of the alveolus, and that of the left just at the alveolus. The fragments of the branches now remaining form an open angle of about 112'^ to 115'^. The depth of the sym- physis on its inner face is about five inches. The channel or groove which is continued over the upper border of the jaw on the median line, and descends towards the chin in front, is quite short and reaches but little below the upper edge of the jaw. 52 The point of the symphysis is broken off at its base, but the fractured surface indicates that it was only very imperfectly developed. When compared with that of Elephas primigenius, the chin is less prominent and the point not so much depressed. 2. Upper Molar of Elephant. — This has been much injured by having been exposed in the bed of the river ; the fangs are all broken oif, and a portion of its anterior extremity has been destroyed, so that its original size cannot now be ascertained. What the entire number of plates was on this tooth previous to its coming into use it is also impossible to say. The fact, how- ever, that all but four have become abraded, indicates that it had been a long time in action. Its shape and proportions indicate that it was an ultimate molar from the upper jaw. The following table gives the dimensions and weight of the tooth as compared with those of a right and left corresponding molar discovered at Zanesville, Ohio, and now in the collection of the late Dr. J. C. Warren. Greatest length ..... Height when resting on the grinding surface Length of grinding surface Breadth of grinding surface Whole number of laminae Laminfe of grinding surface Weight in pounds and ounces . Zancsville right upper molar. 13i 13^1 lOJ. 11 8f 9 H H 29 30 18 18 15 17 14 8J lo' 19 15 19 J From the above comparisons, it will be seen that while the dimensions of the three molars vary but little, the number of plates is quite different in the specimen from the Brazos from what it is in those from Zanesville; there being from 10 to 11 more in the latter than the former. Is this a mere variation, or is it an indication of a specific ditFerence ? This question cannot be answered until we know more accurately than is now known, the normal range of variation in these animals. So great a variation as this in one and the same species has not as yet been noticed. 53 3. Femur of Elephant. — This comprises only the lower half. It is that of an animal fully adult, and belonged to an individual of small size ; the shaft of the bone is more round than that of Mastodon. Compared with that of the Cambridge skeleton, at corresponding parts, the transverse diameter of the latter is 5^ inches, and the antero-posterior 3 inches ; of the fossil, the first diameter is 4 and the second 2 J inches. The condyles examined from behind are longer in a vertical direction and of a more uniform width in the Mastodon than in the fossil elephant. This animal must have been of very small size — probably not ex- ceeding eight feet in height — and, as it is fully adult, must have been very much smaller than the individual from which the molar was derived. 4. Lower extremity of a Right Humerus of Mastodon 1 — This belonged to an animal of large size. The outer condyle is par- tially broken off; breadth across condyles 10 inches. 5. Ulna of the same. 6. An ultimate or sixth upper molar of Mastodon giganteus, as shown by its gradual contraction from before backwards. It is incomplete ; there are four ridges remaining, but the anterior extremity is fractured. It is thickly invested with crusta petrosa between the bases of the ridges. Its greatest breadth is 4^ inches. It diminishes in size from before backwards. 7. An idtimate loiver molar. — It is longer and naiTower than the preceding, as is usually the case with lower molars compared with upper. Length ....... 7f inches. Breadth 3f " These two teeth have a similar aspect, and may have both been derived from the same individual. 8. Tibia of Megatherium. — This was from the left side, and consists of the lower half. The inferior extremity is well pre- sei'ved. The inner tuberosity, which is thick, rounded, and in- dented for the attachment of ligaments, exhibits on its posterior face two grooves for the passage of the tendons of the flexor muscles of the foot. These are both much less deep than the groove seen on the corresponding portion of the tibia of the Mylodon. The outer border of the bone is thinner, and presents a rough, fractured surface, caused by the breaking off of the fibula, which, in Megatherium, is anchylosed with the tibial,. 54 The articulating surface corresponds with that of the same part in the Megatherium. It consists of two deep depressions, sep- arated by a sharp ridge ; the inner depression is a segment of a nearly spherical surface, and the outer forms a broad groove of considerable length, and traverses the end of the bone obliquely from before backwards and inwards. These surfaces correspond Avith the peculiar configuration of the astragalus, which in Mega- theroid animals is quite characteristic. The dimensions of the fragment are as follows: — Inches. Breadth at the lower extremity . . . .13 Thickness of do .... 8 Breadth of upper extremity, fractured ... 8 Thickness of do .... 4.5 Transverse diameter of spherical concavity . . 4 Antero-posterior diameter of do ... 4.7 Transverse diameter of elongated articular surface . 4.7 Antero-posterior (oblique) do . 9.5 The circumference of the bone around the lower extremity, without the fibula, is two feet seven inches ; that of the Madrid specimen with the fibula is 2 feet 6^ inches. The breadth of the Madrid specimen with the fibula is 12J- inches, and that of the specimen from the Brazos River, without the fibula, is 13 inches. The latter, therefore, must have belonged to a much longer animal than the former. In North America, the Megatherium has hitherto been found only in two localities, viz : Skiddaway Island, on the coast of Georgia, and on the banks of the Ashley River, in South Caro- lina. Dr. Leidy, in his Memoir on the Extinct Sloth Tribe of North America, gives a list of all the remains of the Megatherium which have been discovered in the United States ; the upper half of a tibia is described, but in no instance is the lower portion mentioned. Since the animals, whose structure is known, from North and South America, are of different species, he thinks the North American Megatherium forms a distinct species, which he calls M' mirabile. I have had no means of making a direct com- parison of the bone from the Brazos River with the correspond- ing part of the skeleton from South America ; and as the same portion of bone from the M. mirabile has not yet been discovered, 55 , I am unable to say whether the species is identical with either of the others or not. Mr. John Green read a paper entitled — SOME OBSERVATIONS ON THE STRUCTURK OF BONE IN FYTIION. The ribs of Python are hollow, without cancelli, except at the vertebral extrenaity, and in thickness they are about one fifth or one sixth of the diameter of the bone. In the macerated and dried bone, the cavity contains only adipocire and some remains of a lining membrane. The nutritious artery enters near the vertebral end of the rib, and passes directly through into the medullary cavity. The vertebra; are made up of a very dense osseous tissue, with' cancelli in the upper and posterior parts of the bodies, and in the interior of the spinous processes, and to a small extent in the arches on each side of the great foramen. The microscopic structure of the ribs is remarkable in the total absence of Haversian canals. The lacuna; and canaliculi are distinct, and the lamellar structure well marked. The laraellffi are arranged in two series, the first (fundamental lamellae of Kolliker) parallel to the external surface of the rib, and the second series concentric with the medullary cavity and cutting off many of the first series at an acute angle. This internal series of lamella; appears to be a secondary deposit, taking place after the formation (by absorption) of the central cavity, and is homologous with the lamella; of the Haversian canals in human bones, the medullary cavity itself corresponding to the Haversian canal. Under the microscope, the vertebra; present lamellie for the most part parallel with the exterior of the bone, with lacunae and canaliculi well marked, but with a few canals which in the bodies have an antero-posterior direction, and pass directly through the thickness of the bone. These canals vary consid- erably in size, do not branch or anastomose, and are generally not surrounded by lamellae, although, in a few canals, one or two lamellae have been observed. The lacunjE correspond in arrange- ment with the lamellar structure of the bone, and are entirely independent of the canals. 56 Dr. Weinland read a paper on the motions of animals as regarded from a psychological point of view. The President stated that, within a few days, he had made an experiment, upon a mouse, of the poisoning powers of one of the living Rattlesnakes belonging to the Society, The mouse when put in the case with the snakes showed no particular signs of fear, but occupied itself apparently in search- ing for the readiest way of escaping, in the course of which it repeatedly approached the reptiles, and sometimes crossed over them. After being repeatedly struck at, it was wounded by one of them, and died tetanic in the course of two minutes. It was then taken from the case for the purpose of making an examina- tion of the state of the blood. On being opened, the animal proved to be a female far advanced in pregnancy, and the inter- esting fact was noticed that the foetuses were alive for fourteen minutes after the mouse was wounded ; the poison acting much more promptly on the latter than the former, —a circumstance not easy to be accounted for; — ^in reality the arrest of the cir- culation was as likely to have been the cause of death in them as the poison. The Secretary inquired whether the arrest of the respiratory function by the tetanus might not have been the cause of death in the parent ; a cause which would not directly act upon the young ? Dr. "Wyman replied that he could not answer positively upon this point, — the tetanus was universal. After the body had been examined, it was returned to the case with the snakes, and was swallowed in due time by the one which had bitten it. The process of deglutition seemed to be per- formed entirely by means of the upper jaws. On the fourth day after being swallowed, the animal was voided entire, without having been digested. Prof. Agassiz spoke of a new work on Fishes by Duraeril, which was in process of publication in a costly and elegant man- ner. As to its scientific value it was entirely behind the present 57 day, and might as well have been written thirty years ago as now. Prof. Agassiz proceeded to notice in detail many defects in the system of classitication, pronouncing it a woi'k entirely unworthy of confidence as scientific authority, and quite incon- sistent with the reputation of its author. Dr. Henry W. Williams was elected a Resident Mem- ber. October 15, 1856. The President in the Chair. Dr. C. T. Jackson stated that at the meeting of April 2d, a communication was received from Mr. Edward Daniels of Illinois, upon a supposed conversion of human bones into phosphorus. Since that time the supposed bones had been shown to be the phosphorus of com- merce ; but they resembled the long bones of a child, having an enlarged extremity not unlike a condyle, and a central canal, which is not uncommon in stick phospho- rus, resembling the medullary canal. Dr. Weinland made the following remarks upon the Corrosion of the Shells of Freshwater Clams : It is generally believed and stated in the books, that the coi*- rosion of the shells of freshwater clams, which is observed upon the beak, and which frequently extends over the whole surface of the shell, as in Unio complanatus, Anodonta implicata, and Lampsilis radiata, for instance, is effected by the dissolving prop- erties of fresh water when irapi-egnated with carbonic acid. It is supposed that the carbonate of lime is converted into the bicarbonate, and in this state dissolved by the water. This pro- cess may sometimes take place, but it does not seem to be the commencement of the corrosion. In all the specimens of Ano- donta implicata which he had recently collected at Fresh Pond, 58 (about sixty) lie found little holes, or channels, from one to three lines in length, piercing the epidermis, and presenting sharp edges, such as would not have been likely to result from a chemi- cal process. Moreover, he found in many of these holes small worms, and therefore he was inclined to suppose that they com- mence the process of corrosion in the shell ; that they perforate the epidermis, and after the removal of this, the chemical process above alluded to may take place. How far the same supposition may prove true with regard to sea-shells he was not prepared to say. The President offered some remarks on the morphol- ogy of the urinary bladder of Batrachians. Fi'om observations which he had recently made, he thought it questionable whether they belonged to the group of Anallantoi- dians, with which they had been generally classed. He com- pared the urinary bladder of Frogs with that of Fishes and Scaly Reptiles, and showed that structurally it resembled that of the latter group. He was inclined to regard it as a rudimentary allantois, inasmuch as it had the same anatomical relations to the intestine and vascular system that the allantois has. Mr, C. J. Sprague exhibited specimens of Cyclomyces, recently collected by Mr. Denis Murray in the vicinity of Boston, and made some remarks upon the peculiarities of this genus of Fungi. There are three principal arrangements of the spore-bearing apparatus in the common table-formed fungi, which are so dis- tinct as to be generally known to unscientific observers ; viz : in radiating, thin plates, as in Agaricus ; in vertical pores, as in Pohjporits ; and in vertical spines, as in Hi/dnum. The genus Cyclomyces exhibits a series of narrow concentric plates from the stipe to the margin, like seats in an amphitheatre. The genus comprises but very few species, only one of which has been detected in America, the Cyclomyces Greeneii found by Mr. B. D. Greene in Tewksbury. A concentric arrangement of spines is sometimes observed in some Hydnums. Dr. Darkee exhibited a specimen of Goliathus gigan- 59 teus, from Africa. The wings, drawn out from beneath the elytrae, measured four and one half inches from tip to tip. The following named gentlemen were elected Resident Members, viz: Alfred E. Giles, 1. T. Talbot, of Boston ; Ambrose Wellington of Cambridge, A. T. Cummings of Roxbury, and Edwin Harrison of the Lawrence Scien- tific School. November 5, 1856. The President in the Chair. Dr. David F. Weinland read the following paper, entitled - OBSERVATIONS ON A NEW GENUS OF T^NIOIDS. In the middle of April, 1856, I found a single living sjiecimen of a new kind of tapeworm in the small intestine of our gold- winged woodpecker (Picus auratus). This Taenia is remarkable for the structure of its organs of reproduction. As in the human tapeworm {Tcenia solhini), so also in this, the genital openings alternate from one articulation to the next ; but in the former, and as seems generally to be the case in T^enioids, the testicles lie in the middle of each articulation. (See Von Siebold, Vergleichende Anatomic der wirbellosen Thiere, pri47 ; and the figure in Blanchard, Recherches sur Forganization des Vers, pi. 15; f. 4, 7.) They were placed, on the contrary, in the tapeworm of the woodpecker, in the anterior part of the articulation, just in front of the genital opening, fiUing up by a large mass of convolute spermatic canals all that part of the articulation, and thus excluding from it the uterus. Further- more, the uterus did not consist of branched, treelike canals, (see Blanchard, 1. c.) but on the contrary of a large number of balls, perhaps connected with each other by slender ducts. Von Siebold, 1. c. p. 146, and note 23, seems to speak of a similar 60 structure observed by liim or Delia Cliiaje in Taenia ocellaia, and Dujardin (Histoire naturelle des Helminthes, Paris, 1845) has observed exactly the same structure of the uterus in a tape- worm of the European Picas major. As in other tapeworms, the spermatozoa were very fine, fili- form, of one diameter throughout, without the so-called head or body of other spermatozoa. But what was very strange, these spermatozoa were of very different lengths; some twice, thrice, or even four times as long as others. Moreover, they would readily break into pieces, and were not so soft and pliable as they generally are. I saw several break into two pieces, (par- ticularly when coming out from the cirrus-bag,) and both pieces moved on. Whether this phenomenon occurred accidentally, or whether it was a natural characteristic of these spermatozoa, I am at a loss to say. No water was used in the examination, of the bad effects of which upon spermatozoa I am fully aware. In either case this is a subject worthy the investigation of physiologists ; for such a power of division would imply a nature in these sper- matozoa entirely different from what we have hitherto observed. Other spermatozoa present individual elements ; on the contrary, those of this tapeworm would be really dividual, at least virtually, as they have the faculty of dividing and thus multiplying them- selves. Not the slightest difference could be observed, in activ- ity, movement, or form, between the divided portions and the whole animals ; so that we may suppose, that each of the divided pieces had the fructifying power, as well as the others. Further- more, the motion of these spei-raatozoa was extraordinary. Whilst others move in a peculiar, quick, vibratory manner, these progi-Css much more slowly, in a succession of long curves, reminding one of the motion of an eel at the bottom of a river. This same tapeworm is also remarkable for the strange shape of its eggs. While the eggs of tapeworms generally are globular or oval, the shape of these was that of a large ball running out on both sides into tubes which terminated in balls, of about half the diameter of the central one. I found these eggs in all stages of development, some containing nothing but a clear yolk, while others presented embryos with six little spines. The yolk as well as the embryo was found only in the central ball, and there 61 also the yolk membrane terminated. Thus the lateral tubes of the egg, as well as the balls in which they terminated, are to be considered merely as excrescences and appendages of the outer (the third) coating of the egg. Similar appendages to the eggs of tapeworms have been met with previously by other observers ; namely, threads running out on two sides in Tcenia wfandibuli- formis and plaiiiceps by Von Siebold, (1. c. p. 148,) and Tcenia cyathiformis by Dujardin, (1. c. p. 568, and figured PI. 9, Fig. R. 2,) while Von Siebold (1. c.) describes the eggs of the same worm as provided at the pointed ends of their outer pear-shaped coatings, with two bladder-like appendages, which remind one more of the new form just described. Two delicate tufts, one on each side, have been observed by Meissner in Mermis nigres- cens (Beitraegc zur Anatomie und Physiologie der Gordiaceen, in Von Siebold and Kolliker's Geitschrift fur Wiss. Zool. VII. Taf. II., Fig. II.) and by Siebold, 1. c. in Tcenia variabilis. All these appendages belong to the third coating of the egg, adjoining the so-called chorion. Analogous appendages are found in the eggs of sharks and skates. Some of the embryos were hatched under my eyes, and, in spite of the greatly different organization of the adult worms, their organization was seen to be throughout identical with that of the embryos of the genuine Ta^nias, (those of man, dog, cat, etc.) namely, a roundish disk, containing smaller and larger granules, and provided with six little spines, disposed in three pairs, two lateral and one in front. We might ask here, is it only the simplicity of organization which causes this similarity of such incipient organisms, which are so distant from each other when adults ? or is it perhaps rather the real and material ex- pression of the ideal unity of such a type (that of Ttenioids, for instance) ? The embryos of all Dicotyledonous plants start with a little root and two leaflets, whatever difference they may ex- hibit, when full grown, in relation to the organs of nutrition, respiration, or reproduction ; they may have the complicated flowering of a rose, or the simple perigon of an oak. Thus every Dicotyledonous embryo exhibits materially the unity of that great diversified type. Again the simple cell, from which both ani- mals and plants originate, represents materially that j^deal unity which embraces all living beings. If this be so, the question arises, can we extend this principle, which has already laid open 62 or strengthened such natural divisions as Dicotyledonous and Monocotyledonous plants, over all natural groups ? Is it the stand- ard of every type or group ? Is it the proof of its foundation in nature, that its members exhibit materially their unity by iden- tity of organization at any time of their embryonic development? "We think that it is impossible to answer this question for want of embryological data, but in relation to the Tajnioids, which we will call a family, its truth is remarkably evident. We form a natural group of all those Tcenias, the embryos of which show that disk-like body with six spines. We might call them Hexe- chinidaj. Many genera with very different structure in relation to the reproductive organs, the number and disposition of the hooks, the form of the proboscis, &c. &c., are included in it. Even their forms when adult are not the same, but we have a doubt whether we ought not, in basing, as Agassiz has taught us, families upon foi'ms, to make, at least in the lower animals, this allowance, that the guiding form is often not exhibited in the adult animal, but only in a much earlier, perhaps in its embryonic state. We allude here particularly to all those animals in which an alternation of generation is observed, such as Cirripeds, etc. The neiv genus, which we found upon the structural peculiari- ties mentioned above, we will call Liga, and the species, from its many yellowish-brown dots, punctata. A full description of both genus and species, with drawings, will be given on some future occasion. Dr. Gould asked if there is around the mouth of the common tapeworm {^T., F. L. S. Description of Eight New Species of Birds from South America. P. L. Sclater. 8vo. Pamph. London, 1856. S3'nopsis of the Galbnlidaj. By the same. 8vo. Pamph. London, 1853. Draft Arrangement of the Genus Thamnophilus ( Vieillot). By the same. 8vo. Pamph. London, 1855. List of Specimens of Birds in the British Museum. Part IIL Section 1. Eamphastidoe. 12mo. Pamph. London, 1855. Birds received in collections from Santa F6 di Bogota. P. L. Sclater. 8vo. Pamph. London, 1855. Synopsis of the Fissirostral Family Bucconidas. By the same. 8vo. Pamph. London, 1854. Fro7n P. L. Sclater. Silliman's Amei-ican Journal of Science and Art. Nos. 65, 66. Journal of the Royal Geographical Society of London. Vol. XXV. Proceedings of the Royal Geographical Society of London. Nos. 3, 4, 5. 8vo. Pamph. 1856. Proceedings of the Zoological Society of London. Nos. 292-304. 8vo. Paraph. 1856. Wiirttembergische Naturwissenschaftliche Jahreshefte, Zwolfter Jahrgang. Zweiter Heft. 8vo. Stuttgart, 1856. Receuil des Actes de I'Academie Imperiale des Sciences, Belles Lettres, et Arts de Bordeaux. 17ieme ann^e. 1855. Trimestres 3, 4. Pamph. 8vo. Bordeaux. Delia Regione Vulcanica del Monte Vulture e del Tremuoto ivi avvenuto nel di 14 Agosto, 1851. Da L. Palmieri ed A. Scacchi. 4to. Napoli, 1852. New York Journal of Medicine. Vol. L No. 3. 8vo, New York, 1856. Bulletin de la Societe de Geographic. 4rieme serie. Tome X. 8vo. Paris, 1855. Rendiconto della Reale Accademia delle Scienze. Tome IL pp. 181-200. 4to. 1853. Proceedings of the Elliott Society of Natural History, pp. 25-46. 8vo. Pamph. Almanach der Kaiserlichen Akad. der Wissenschaften. Sechster Jahi-gang. 12mo. Wien, 1856. Bericht iiber die Oesterreichische Literatur der Zoologie, Botanik, und Paleon- tologie, aus den Jahren, 1850-3. 8vo. Wien, 1855. Verhandlungen des Zoologisch-botanischen Yereins in Wien. Band V. Oct. Dec. 1856. Wien. Memoires de la Socit5te de Physique et d'Histoire Naturelle de Geneve. Tome XIV. l^re partie. 4to. Geneve, 1855. Annales de la Socidte Linneenne de Lyon. 8vo. Tome IL Lyon, 1855. Annales des Sciences Physiques et Naturelles, d' Agriculture et d'Industrie, publi(5es par une Socictc; Imperiale d' Agriculture de Lyon. 2ieme. Serie VII. lere partie. 4to. Lyon, 1851. 96 Jahrbiicher der K. K. Central- Anstatt fiir Meteorologie und Erdmagnetismus. Von Karl Kroil. IV Band. Jahrgang, 1852. 4to. Wien, 1856. Abhandlinigen der Koniglichen Akademie der Wissenschaften zu Berlin. Aus deui Jalire, 1854. Erstes Supplement Band. Fol. 1856. Monatsbericht der Kcinig. Preuss. Akademie der Wissenschaften zu Berlin 8vo. July to Dec, 1855. Proceedings of the Academy of Natural Sciences of Philadelphia. Vol. III. Nos. 4, 5. 8vo. 1856. Atti della Reale Accademia delle Scienze, Sezione della Societa Eeale Bor- bonica. Vol. VI. 4to. Napoli, 1851. Rendiconto de la Societa Reale Borbonica. 10 Nos. 1852-4. 4to. Napoli. Relazione sulla malattia della vite apparsa nei contorni di Napoli ed altri luoghi della Provincia, fatta da una commissione e presentada all Reale Accad- emia delle Scienze. 4to. Napoli, 1852. Zeitschrift fiir die Gesammten Naturwissenschaften. 17 Nos. July to Dec, 1850, and Jan. to Dec. 1855. 8vo. Berlin, 1854-5. Verhandlungen des Naturhistorischen Vereins der Preussischen Rheinlande und Westphalens. Heft 1, 2, 3. Svo. Bonn. 1855-56. Bulletin de la Societ(^ de Geographic. 4vieme serie. XI. Paris. 8vo. 1856. Journal of the Academy of Natural Sciences of Philadelphia. III. Part 3. 4to. 1856. Annales des Sciences Physiques et Naturelles d' Agriculture et d'Industrie. Svo. Lyon, 1855. Memoires del' Academic Imperiale des Sciences, &c., de Lyon. Tomes IV. V. Svo. 1854-5. Denkschriften der Kaiserlichen Akademie der Wissenschaften. Band X. XL 4to. Wien, 1855-6. Sitzungsberichte der K. Akademie der Wissenschaften. Band XVIII. XIX. XX. Heft Band I. 9vo. Wien, 1856. Archiv fiir Naturgeschichte, Wiegman, Erichson. No. 6, 1852; 5, 1854; and 1, 3, 5, 1855. Svo. Berlin, 1854-5. Received in Exchange. Recherches sur les Vers a Soie. Guerin-Meneville. Svo. Pamph. Paris, 1854. Recherches sur les Maladies des Vegetaux et particulier^ment sur la Maladie de la Vigne. Guerin-Meneville. Svo. Pamph. Note sur un Precede cultural et efficace pour fiiire perir TEumolpe de la Vigne ou Ecrivain. Guerin-Meneville. 8vo. Pamph. Note sur une Larve d'Insecte observ^e dans les Tiges de Seigle provenant de la Champagne. Guerin-Meneville. Svo. Pamph. Memoire sur la necessit(5 d'etudier un moyen simple et applicable en grand de preserver les Bl(5s des attaques de I'alucite. Guerin-Meneville. Svo. Pamph. Observations sur I'lndustrie de la Soie. G. Meneville et E. Robert. Svo. Pamph. 1853. Archives du Museum d' Histoire Naturelle. Tome V^II. Liv. 3, 4; et VIII. 1, 2. 4to. Paris, 1855-6. Catalogue des Genres et Sous-Genres d'Oiseaux contenus dans le jMus^um Britannique. George R. Gray. 4to. Pamph. Paris, 1855. Conspectus Volucrum Anisodactylorum. Svo. Pamph. Conspectus Volucrum Zygodactylorum. Svo. Pamph. 1854. Tableau des Oiseaux de Proie. Svo. Pamph. 1854. Extrait de la Revue et Magasin de Zoologi.e. No. 2. 1855. Svo. Pamph. 97 Tableaux Synoptique de I'Ordre des Herons. 4to. Pampli. 1855. Excursions dans les divers mus($es d'AUemagne, d'HolIande et do Belgique; Paralleliques de I'Ordre des Echassiers. 4to. Pamph. 1856. Notes sur les Oiseaux des Isles Marquises. 4to. Pampli. The above list of pamphlets by C. L. Bonaparte. International Exchange by A. Vattemare. Annals and Magazine of Natural History. Nos. 106, 107. From the Courtis Fund. Encyclopaedia Britannica. Vol. XI. 4to. Boston, 1856. Arctic Explorations in 1853, 4, 5. E. K. Kane. 2 vols. 8vo. New York, 1856. Cyclopajdia of Anatomy and Phj'siology. Manual of United States History. Samuel Eliot. 8vo. Boston, 1856. Memoirs of Celebrated Characters. 12mo. Vol. III. New York, 1856. History of the Reign of Charles V. Wm. Robertson. Edited by W. H. Pres- cott. 3 vols. 8vo. Boston, 1855. Private Con-espondence of Daniel Webster. Edited by Fletcher Webster. 2 vols. Svo. Boston, 1856. Deposited by the Republican Institution. BINNEY LIBRARY. Albin's Birds. 3 vols. 4to. Full calf. London, 1738-40. Albin's Natural History of Spiders. 4to. Half calf. London, 1736. Albin's Natural History of English Insects. 4to. Full calf. London, 1749. Aldrovandi Opera Omnia. 13 vols. Folio. Old calf. Bonnvias, 1599-1668. Adelou, Phj'siologie de I'Homme. 4 vols. Svo. Sheep. Paris, 1823. American Philosophical Society's Transactions. Vol. IX. parts 1 and 2. 4to, Paper. Philadelphia, 1844-45. Archives du Museum D'Histoire Naturelle. Vol. III. 4to. Half calf. Paris, 1839-43. Archives du Museum d'Histoire Naturelle. Vol. IV. 4to. Paper. Paris, 1845. American Monthly Magazine, from May, 1817, to Oct. 1818. 3 vols. Svo. Half morocco. New York. Annales des Sciences Naturelles. 31 vols. Svo. (Including Table.) Half calf, and 1 in paper; and Revue. Annales Bibliographiques. 1829-31. Svo. Half mor. Paris, 1824-41. Annales BibHographiques. 1829-31. 20 vols, in 10. Half calf. Vol I. 3d series. Annales Bibliographiques. 4 1-2 vols, in Nos. Royal Svo. Paris, 1844-46. Annals of Natural History. 16 vols. Half mor. 17th and half 18th vols, in Nos. Svo. London, 1838-46. Anatomic des Systemes Nerveuses, Atlas. 4to. Pamph. Paris, 1825. Alger's Phillips' Mineralogy. Svo. Cloth. Boston, 1844. Anspach's History, of Newfoundland. Svo. Boards. London, 1827. Art of Angling. 12mo. Half sheep. London, 1740. Antediluvian Phytology. By Edmund T. Artis. London, 1838. Barbut, Genres des Insectes. 4to. Sheep. London, 1781. Back's NaiTative of Arctic Land Expedition. 4to. Half calf. London, 1836. PROCEEDINGS B. S. N. H. — VOL. VI. 7 MARCH, 1857. 98 Bell's British Quadrupeds. 8vo. Half calf. London, 1839. Bell's British Eeptiles. 8vo. Half calf. London, 1837. Bewick's British Birds. 2 vols. 8vo. Plalfcalf. New Castle, 1832. Bewick's British Quadrupeds. 8vo. 1790. Barbut, Genera Vermium. 4to. Sheep. London, 1783. Beche's Theoretical Geolog}'. ]2mo. Boards. London, 1834. Bennett's Fishes of Ceylon. Roj'al 4to. Half calf. London, 1834. Bingley's Animal Biography. 3 vols. 8vo. Half calf. London, 1805. Bingley's Useful Knowledge. 3 vols. 12mo. Sheep. London, 1821. Bonnet's Contemplations of Nature. 2 vols. 12mo. Sheep. London, 1766. Bloch, Histoire Naturelle des Poissons. 10 vols, in 5. 24mo. Half calf. Paris, 1830. Bohadsch, De Quibusdam Animalibus Marinis. 4to. Half calf. Dresds, 1761. Boitard, Manuel d'Histoire Naturelle. 2 vols. 24mo. Paris, 1827. Book of Butterflies, Sphinxes, and Moths. 2 vols. 24mo. Boards. Edin- burgh, 1832. Boreau et Lartique, Histoire Naturelle. 12mo. Paper. Paris, 1839. Bosc, Histoire Naturelle des Crustac^s. 2 vols. 24mo. Half calf. Paris, 1830. Bremser, Les Vers Intestinaux de I'homme. 8vo. Half sheep. Paris, 1824. Brisson's Ornithologia. 6 vols. 4to. Old calf. 260 plates. Paris, 1760. British Association for the Advancement of Science, Report of Meetings at York and Oxford, 1832. 8vo. Boards. London, 1833. British Naturalist. 2 vols. 12mo. Boards.' London, 1833. Brown's Natural History of Jamaica. Folio. Full calf. London, 1789. Brown's Zoologist's Text Book. 2 vols, 12mo. Boards. Glasgow, 1833. Brown's Zoology. 4to. Half mor. ; gilt edges. London, 1776. Bruguifere et Lamarck, Histoire Naturelle des Vers. 3 vols. 4to. Paris, 1792- 1832. Buffon's Natural History of Birds, Beasts, &c. 4 vols. 12mo. Boards. Lon- don, 1831. Buffon's Natural History, by Barr. 15 vols. 12mo. Sheep. London, 1792-8. Babbage on the Decline of Science in England. 8vo. Boards. London, 1830. Barton's Medical and Physical Journal. 3 vols. 8vo. Half calf. Philadel- phia, 1805-8. Blackwell's Researches in Zoology. 8vo. Boards. London, 1834. Bloch, Histoire Naturelle des Poissons. 3 vols. Royal folio. Full red mor. ; gilt edges. Berlin, 1785-87. Blumenbach, Manuel d'Histoire Natui-elle. 2 vols. 8vo. Sheep. Metz, 1803. Bomare's Dictionnaire d'Histoire Natm'elle. 8 vols. 4to. Sheep. Lyons, 1791. Bonaparte's Amei'ican Ornithology. 4 vols. Roj'al 4to. Half mor. Phila- delphia, 1825-33. Bonaparte's Birds of Europe and North America. 8vo. Cloth. Loudon, 1838. Bonaparte, Memoria sulla distribuzione degli Animali Vertebrati. 8vo. Half calf. Bologna, 1830. Boston Journal of Philosophy and the Arts, from May, 1823, to Dec, 1826. 3 vols. 8vo. Half Russia. Boston. Buffon's Histoire Naturelle. 17 vols. Supplement 7 vols. ; (1st and 2d A'ols. wanting) in all 24 vols. 4to. Old calf. Paris, 1749-89. 99 Bulletin d'Histoire Naturelle et Actes dc la Soci(5t($ Linn^enne de Bordeaux. 11 vols. (2d vol. wanting.) 8vo. Sheep. Bordeaux, 1826-39. Burmeister's Manuel of Entomology. 8vo. Boards. London, 1836. Bartram's Travels through Carolina, &c. 8vo. Sheep. Philadelphia, 1791. Bichat, Recherches Physiologiques. 8vo. Sheep. Paris, 1822. Bonnet, (Envres d'Histoire Naturelle ct dc Philosophic. 8 vols, in 10. Half calf. Neuchatel, 1799-1803. Bradford's History of Massachusetts. 8vo. Boards. Boston, 1825. Brard, Mineralogie Appliqut^ aux Arts. 3 vols. Svo. Boards. Paris, 1821. Bibliotheca Banksiana. 5 vols. 12mo. Calf. London, 1798. Bigelow, Jacob. Plants of Boston and Environs. 8vo. Boards. Boston, 1814. Bakewell's Introduction to Geology. Svo. Half Russia. New Haven, 1827. British Museum, Report on. 2 vols. Folio. Paper. London, 1836. Buffon, Nouvelles Suites a. 8vo. Paper. 9 odd vols. Paris. Cuvier, Anatomic Compar^e. 8vo. Paris, 1836-46. Cuvier, Elogcs Historiques. 3 vols. Svo. Half calf. Strasbourg et Paris, 1819-27. Cuvier's Memoires pour I'Histoire de Mollusques. 4to. Half calf. 35 plates. Paris, 1817. Cuvier's Animal Kingdom, by Latreille. 4 vols. 8vo. Half calf. Loudon, 1834-36. Cuvier, Dents des Mammiferes. Svo. Calf; gilt edges. Strasbourg, 1825. Cuvier, Histoire Naturelle des Cetacc's. Svo. Half calf. Paris, 1836. Cuvier, Ossemens Fossiles. 10 vols. Svo. Half calf. Paris, 1834-36. Cuvier, et Valenciennes, Histoire Naturelle des Poissons. 15 vols. 8vo. Half calf. 5 in paper (in all 20.) Paris, 1828-46. Cuvier's Theory of the Earth. Svo. Half Russia. New York, 1818. Cuvier's Anatomic Comparc^e. Svo. Half boards. Paris, 1805. Cuvier, Histoire de ses Travaux, par Flourens. 12mo, Half calf. Paris, 1S45. Cabinet of Natural History. 2 vols. 4to. Half calf. Philadelphia, 1830-32. Catesby's Natural History of Carolina, Florida, and the Bahama Islands. 2 vols. Royal folio. Half calf. London, 1731-43. Catalogue of Fossil Remains, &c., in the Museum of the Royal College of Sm-geons of England. 4to. Cloth. London, 1845. Charleton, De Diflferentiis et Nominibus Animalium. Small folio. Half calf. Oxford, 1677. Chevalier, Melanges Photographiques. Svo. Paper. 127 pp. Paris, 1844, Cabanis, Du Physique et du Moral de I'Homme. 2 vols. Svo. Boards. Paris, 1824. Camerarii Symbolse ex Quadrupedibus. Small 4to. Half calf. Nuremburg. Cicero's Orations translated into English, by Rutherford. 4to. Full calf. London, 1797. Cleaveland's Mineralogy. 2 vols . Svo. Half sheep. Boston, 1822. Combe's Phrenology. Svo. Boards. Philadelphia, 1822. Conversations on Mineralogy. 2 vols. 12mo. Boards. London, 1822. Carey on Political Economy. Svo. Sheep. Philadelphia, 1822. Dana's Notice of Dr. Blum's Treatise on Pseudomorphous Minerals. Svo. pp. 22. New Haven. 1845. 100 Dana on the Structure and Classification of Zoophytes. 4to. Boards. Phil- adelphia, 1846. Darwin's Researches in Geology and Natural History. 8vo. Cloth. London, 1839. Darwin's Zoology of the Beagle. 5 vols. Royal 4to. London, 1840-43. Davy's Consolations of Travel. 12mo. Boards. London, 1831. Description of the Island of St. Michael, by J. W. Webster. 8vo. Boards. Boston, 1821. Dictionnaire de I'Histoire Naturelle, par Herbigny. 3 vols. Calf. 18mo. Paris, 1755. Drury's Exotic Insects, French and EngHsh. 4to, Full calf. Plates. Lon- don, 1770. Drury's Exotic Entomology, enlarged by Westwood. 3 vols. 4to. Half mor. London, 1837. Dutrochet Memoires des Vegetaux et des Animaux. 2 vols. 8vo. Half calf. Paris, 1837. Deleuze, Histoire et Description du Museum Royale d'Histoire Naturelle. 2 vols. 8vo. Boards. Paris, 1823. Desmarest, Considerations sur la classe des Cn;stac^s. 8vo. Half calf. Paris, 1825. Dumeril et Bibron, Ei-petologie Generale. 8 vols. (6th and 7th vols, wanting.) 8vo. Half calf. Paris, 1834-46. Dumeril's Sciences Naturelles. 2 vols. Svo. Boards. Paris, 1825. Darwin's Zoonomia. 4to. Half sheep. Loudon, 1794. Ellis's Zoophytes. 4to. Full Russia. London, 1786. Enchiridion Historicte Natm-alis. 12mo. Sheep. London, 1797. Evelyn's Sylva. 2 vols. 4to. Half mor. York, 1812. Eyton's Rarer British Birds and Catalogue of British Birds. Svo. Half calf. London, 1836. Edwards's Essay upon Natiiral History, &c. Svo. Sheep. London, 1770. Edwards's Agens Physiques sur la vie. Svo. Boards. Paris, 1824. Ellis on Corralines. 4to. Calf. London, 1755. Edwards's (Milne) Histoire NatureUe des Crustac^s. 4 vols. (1 of plates.) Svo. Half calf. Paris, 1834-40. Fauna Japonica, Temminck and Schlegel. Folio; Half calf. London, 1833. Fishes of New York. By S. G. Mitchell. 4to. Without covers. Fisher's Description of the Small Pox, Varioloid, Cow Pox, and Chicken Pox. 4to. Boards. 13 plates. Boston, 1829. Fleming's British Animals. Svo. Half calf. Edinburgh, 1828. Forbes's British Star Fishes. Svo. Cloth. London, 1841. Forry's Climate of United States. 8vo. Cloth. New York, 1842. Fleming's Philosophy of Zoology. 2 vols. Svo. Boards. Edinburgh, 1822. Forskal, Descriptiones Animalium Itinere Orientale. 4to. Full calf. Hanniaj, 1775. Forster's Catalogue of British Birds. Svo. Boards. London, 1817. Forster's Natural History of Swallows. Svo. Paper. London, 1817. Fourcroy, Entomologica Parisiensis. 2 vols. 18mo. Paper. Paris, 1785. Fabricii Fauna Groenlandica. Svo. Half calf. Hafnite et Lipsise, 1780. 101 Good's Physiological Nosology. 8vo. Boards. Boston, 1823. Giraud's Birds of Long Island. 8vo. Cloth. New York, 1844. Gould's Invertebrata of Massachusetts. 8vo, Half calf. Cambridge, 1841. Grave's Ovarium Brittanicura. 8vo. Boards. London, 1816. Geoffrey, Histoire des Insectes. 2 vols. 4to. Old calf. Paris. Gesneri Historia Animalium. 5 vols, in 3. Folio. Old calf. Tiguri, 1551-58. Gesneri Historia Naturalis. 4 vols. Folio. Parchment. Tiguri, 1551-58. Goldsmith's Animated Nature. 8 vols. Post 8vo. Full calf. London, 1774. Gory and Percheron. Monographic des Cetoines. 8vo. Half calf. Paris, 1833. Geradin, Tableau Elementaire D'Ornithologie, with Atlas, 2 vols. 8vo. Half calf. Paris, 1806. Gouan, Histoire des Poissons. 4to. Old calf. Strasbourg,' 1770. Gray's Synopsis Reptilium. 8vo. Boards. London, 1831. Guerin, Bulletin Zoologique. 8vo. Half calf. Paris, 1835. Guerin, Magasin de Zoologie. 13 vols. 8ro. Half calf. And 3 nos. Paris, 1831-45. Guiana, Natural History of. 12mo. Half boards. London, 1769. Guide pour les Kechi^rches et Observations Microscopiques. 12mo. Pamph. Paris, 1836. Guide des Voyageurs en Em-ope, par Reichard. 3 vols. Half boards. Paris, 1824. Harlan's Fauna Americana. 8vo. Half Russia. Philadelphia, 1825. Harris's Insects injurious to Vegetation. 8vo. Half calf. Cambridge, 1841. Herbst, Versuch einer Naturgeschiclite der Krabben und ICi'ebse. 4 vols. 4to. (3 in paper, 1 full calf.) 1793-1804. Berlin und Stralsund. Hitchcock's Geology, Mineralogy, Botany, and Zoology of Massachusetts, with Catalogue of Animals and Plants. 8vo. Boards. Amherst, 1835. Hayden, Horace H., Geological Essays. Baltimore, 1820. Harlan's Medical and Physical Researches. Thick 8vo. Half mor. Philadel- phia, 1835. Hewitson's British Oology. 2 vols. 8vo. Cloth. Newcastle-upon-Tyne. Hill's History of Animals. Folio. Half calf. London, 1752. Hill's Natural History of Fossils. Folio. Half calf. London, 1748. Harris's Aurelian. By Westwood. Folio. Half red mor., gilt and gilt edges. London, 1840. History of Quadrupeds. 8vo. Sheep. New Castle, 1790. Hayes's Natm-al History of Birds. Royal folio. Old half calf. London, 1755. Historia Naturalis Brasilianse. Folio. Full green mor. Amsterdam, 1648. Histoire Naturelle, Generale et Particulaire. (Buffon.) 126 vols. 8vo. Paper covers. Paris. Au. IX. Histoire Naturelle des Oiseaux. (Buflfon.) 9 vols. 4to. Boards. Paris, 1790. Histoire Naturelle des Oiseaux. Supplement. 7 vols. Ditto. Histoire Naturelle des Torres. 4to. Parchment. Paris, 1755. Histoire Naturelle des Mammiferes. 4to. Half calf. Paris. Histoire Naturelle des Animaux, Articul^s, Insectes ; 3 vols. Crustac^s ; 1 vol. 8vo. Paper. Paris, 1844. Histoires Generales des Lepidopter^s. 26 nos. 16mo. Paris. 102 Holandre's Abr^ge d'Histoire Naturelle. 6 vols. Post. 8vo. (2 of plates.) Half calf. 1790. Howard's (Philip) History of the Earth and Mankind. 4to. Boards. Lon- don, 1797. Hughes's Natural History of Barbadoes. Folio. Old calf. London, 1750. Button's Book of Nature. 12mo. Half calf. London, 1821. Hammatt's Book on the Ashby Coal-Field. 4to. Ashby, 1836. Icthyologia Petri Artedi. 8vo. Half bound. Leyden, 1738. niustrations of Zoology of South Africa. By A. Smith. 28 nos. 4to. Lon- don, 1849. Johnston's British Zoilphytes. 8vo. Cloth. Edinburgh, 1838. Jardine and Selby's Hlustrations of Ornithology. 2 vols. 4to. Half mor. Edinburgh. Jesse. An Angler's Eamble. 8vo. Cloth. London, 1836. Jesse. Gleanings in Natural History. 2 vols. (1st wanting.) 12mo. Cloth. London, 1838. Jonstonus, Historia Naturalis. Folio. Parchment. Amsterdam, 1647. " Historia Naturalis, Quadrupetibus. Folio. Old calf. " Historia Natui-alis, Piscibus et Cetis. Folio. Old calf. Jefferson's Notes on the State of Virginia. Svo. Sheep. Boston, 1801. Jenyn's British Vertebrate Animals. 8vo. Half calf. Cambridge, Eng., 1835. Karnes's Elements of Criticism. 2 vols. 8vo. Sheep. New York, 1819. Kirwan's (Richard) Geological Essays. 12mo. Sheep. London, 1799. Klein, Dispositio Echinodermatum. 4to. Half calf. Gedani, 1734. Knorr, Deliciaj Naturas Selecta;. 2 vols. Imperial folio. Full sheep. Nu- remberg, 1754-67. Kalm's Travels in North America. 3 vols. Svo. Calf. Warrington, 1770-71. Le9ons d' Anatomic Comparee. Par Cuvier et Duvernoy. 8vo. Paper. 8 vols. in 9. Paris, 1846. Leuwenhoeck's Works. 2 vols. 4to. Half sheep. London, 1792. Linnffius, Animal Kingdom. 4to. Half calf. London, 1792. " Voyages in the Levant. 12mo. Calf. London, 1766. " on Insects. 8vo. Old calf. London, 1773. Linnsei Fauna Suecica. 8vo. Half calf. Stockholm, 1761. Liunrei Museum UlricEe. 8vo. Calf. Holmiaj, 1764. Linnaeus, Systema Natura. 8 vols. Svo. Calf. VindobonsB, 1767-70. Linnseau Society's Transactions. 16 vols. 4to. Full calf. London, 1791-1833. Lamarck, Systeme des Animaux sans Vertebras. Svo. Sheep. Paris, 1801. Lamarck's Philosophie Zoologique. 2 vols. Svo. Half blue calf. Paris, 1830. Latham's General Synopsis of Birds. 10 vols. 4to. Full Russia, gilt edges. London, 1781-1801. Latreille's Histoire Naturelle des Reptiles. 4 vols, in 2. 24mo. Half sheep. Paris, 1830. Leach's Crustacea. 4to. Half calf. London, 1817. Lessor's Insecto-Theology. Svo. Sheep. Edinburgh, 1799. Lesson, Manuel d' Ornithologie. 2 vols. 24mo. Paris, 1828. 103 Lewin's Birds of Great Britain. 8 vols, in 4. Koyal 4to. Full gi-een mor. London, 1795-1800. Lewin's Lepidopterous Insects of New South Wales. 4to. Half mor. Lon- don, 1822. Lister's Exercitatio Anatomica. 8vo. Old calf. London, 1694. Low's Funda Oreadensis. 4to. Half calf. Edinburgh, 1813. Lyonnet, Recherches sur les Insectes. 4to. Half calf. Paris, 1832. Lacepede, Histoire Naturelle. 5 vols. 8vo. Half calf. Paris, 1819. Latreille, Cours d'Entoniologie. 8vo. Half calf. Paris, 1831 . " Families Naturelles du Regno Animal. 8vo. Half calf. Paris, 1825. Leach and Nodder's Zoological Miscellany. 3 vols. Roj-al 8vo. Half calf. London, 1814-17. Lempriere's Lectures on Natural History. 8vo. Boards. London, 1830. Lesson, Manuel de Mammalogie. 24mo. Half calf. Paris, 1827. Le Vaillant, Voyage dans I'Afrique. 2 vols. Sheep. Paris, 1790. Le Vaillant, Deuxieme Voyage dans I'lnterieur de I'Afrique. 3 vols. 8vo. Sheep. Paris. Lewin's Birds of New Holland. Royal 4to. Half mor. London, 1838. Lewis and Clarke's Expedition. 2 vols. Svo. Sheep. Philadelphia, 1814. Lubbock's Fauna of Norfolk. 8vo. Cloth. Norwich, 1845. Loudon's Magazine of Natural History. 1st and 2d series. 13 vols. Svo. Half Russia. London, 1829-40. Marsham's Entomologia Bntannica. Svo. Half calf. London, 1802. Martyn's Dictionary of Natural History. 2vols.ini. P'olio. London, 1785. Memoires de la Soci^t^ d' Histoire Naturelle de Paris. 5 vols. 4to. Half calf. Paris, 1823-24. Memoires de la Socii?t(i d'Histoire Naturelle de Strasbourg. 2 vols, (and Vol. m. in paper, and 3 nos. 4to. Half calf. Paris, 1830-35. Memoires de la Societe de Physique et d'Histoii-e Naturelle de Geneve et Paris, 1821-42. Memoires de la Socit^t^ de Physique et d'Histoire Naturelle de Geneve et Paris. Vols. X. and XL Paper. Memoir of Lewis David von Schweinitz, P. D. 12mo. Pamph. Philadelphia, 1835. Michaux, Histoire des Arbres Forestiers de 1' Amerique Septentrionale. ; 3 vols. Royal Svo. Full Russia. Paris, 1800-13. Montagu's Ornithological Dictionary. By Rennie. Svo. Half calf. London, 1831. Mudie's British Birds. 2 vols. 8vo. Cloth. London, 1834. Miscellany of Natural History. Parrots. 12mo. Cloth. Edinburgh, 1833. Molina, Histoire Naturelle du ChiH. 12mo. Sheep. Paris, 1789. Museum Wormianum. Folio. Full calf. Amsterdam, 1655. Magazine of Zoology and Botany. Conducted by Jardine, Selby, and Dr. Johnston. 2 vols. Svo. Cloth. Edinburgh, 1837-38. Magendie, Anatomic des Systcmes Nerveuses. 2 vols. Half bound. Paris, 1825. Magendie, Precis de Physiologic. 2 vols. Svo. Boards. Paris, 1825. Mantell's Medals of Creation. 2 vols. Post Svo. Cloth. London, 1844. " Wonders of Geology. 2 vols. Post Svo. London, 1838. 104 Meckel, Anatomie Compar(5e. 6 vols. 8vo. Half sheep. Paris, 1828-30. Mammatt's Geological Facts. Royal 4to. Cloth. London, 1836. Marsham's Coleoptera Britannica. 2 vols. Halfmor. London. Minstrelsy of the Woods. 12mo. Cloth. London, 1832. Moufeti Inscctorum sive Minimorum Aniraaliura Theatrum. Small folio. Half calf. London, 1634, Monograph of Testudinata. By Thomas Bell. Folio. Paper. London. Miiller, Zoologica Danica. 2 vols. Folio. Boards. Havania;, 1788-89. Natural History. Birds. 12mo. Cloth. London, 1835. Natural History. Insects. (Family Library.) 2 vols. 12mo. Boards. New York, 1830. Natural History of Norway. Folio. Half Russia. London, 1845. Natural and Civil History of America. 2 vols, in 1. Folio. Calf. London, 1760. Nature Displaj'ed. Translated from the French. 7 vols. 12mo. Full calf. London, 1733. Naturalists' Miscellany. 19 vols. 8vo. Full calf. Neue Wirbelthiere von Dr. Ruppell. 2 vols. Folio. Paper covers. Frank- fort, 1836-40. Nuttall's Travels in Arkansas. 8vo. Boards, Philadelphia, 1821. Oliver's Recollections of Fly Fishing. 16ino. Cloth. London, 1834. Owen's History of British Fossil Mammalia' and Birds. 10 uos. 8vo. Lon- don, 1844-46. Owen's History of Serpents. 4to. Full calf. London, 1742. Owen's Description of the Skeleton of an Extinct Gigantic Sloth. 4to. Clotli. London, 1842. Parra, Descripcion de Historia Naturale mas del ramo Maritimo. Small 4to. Old calf. Havana, 1787. Pallas, Miscellauea Zoologica. 4to. Half calf. Parkinson's Organic Remains. 3 vols. 4to. Half calf. London, 1808-20. Parkinson's Outlines of Oryctology. 8vo. Half calf. London, 1G22. Patterson's Insects mentioned in Shakespeare's Plays. 12mo. Cloth. Lon- don, 1838. Pennant's Arctic Zoology. 3 vols. 4to. Old calf. London, 1792. Pennant's Indian Zoology. 4to. Half calf. 16 colored plates. London, 1790. Pennant's British Zoology. Imp. folio. Full Russia. 107 plates. Loudon, 1766. Pennant's British Zoology. 4 vols. Royal 8vo. Half calf. London, 1812. Pennant's Genera of Birds. 4to. Half calf. London, 1781. Pennant's Histoiy of Quadrupeds. 2 vols, 4to. Half calf, London, 1793, P^ron, Voyage aux. Tei-res Australes, 2 vols. 4to. Atlas, Folio. Half calf. Paris, 1807-16. Percheron, Bibliographic Entomologique. 2 vols. 8vo. Half calf. Paris, 1837, PhiUips's Mineralogy, 8vo. Boards. New York, 1818. Pisonis Indise utriusque de re Natural! et Medica. Folio. Parchment. Am- sterdam, 1658. Plinii Historia Naturalis. Folio. Old calf. 1615. 105 Pline, Histoire Naturelle. 12 vols. 4to. Sheep. Paris, 1771-82. Programme de I'lmperiale Soci(5t6 des Naturalistes. 4to. Pamph. Moscow, 1825._ Polehampton's Gallery of Nature and Art. 6 vols. 8vo. Full calf. London, 1817. Pultcney's Writings of LinniEus. 4to. Sheep. London, 1833. Rennie's Conspectus of Butterflies and Moths. 18mo. Boards. London, 1832. " Field Naturalists' Magazine, from January, 1833, to April, 1834. Svo. Half calf. London. Redi Opuscula Varia Physiologica. 3 vols. 24mo. Parchment. London, 1729. Report of Geological Reconnaissance of Virginia. By W. B. Rogers. 4to. Without covers. Rogers's Geology of New Jersey. 8vo. Cloth. Philadelphia, 1840. Richardson, Fauna Boreali-Americana. 4 vols. 4to. Half mor. London, 1829-37. Ross's Appendix to the Narrative of a Second Voyage in Search of a North- west Passage. Royal 4to. Cloth, London, 1835. Rusconi, Monografia del Proteo Anguino de Laurenti. 4to. Full calf. Pavia, 1819. Ruppell, Zoijlogische Atlas von Nord Afrika. Royal 4to. Half red mor. Frankfort a Main, 1826. Russell on Indian Serpents. Imp. folio. Full green mor. London, 1796. Rutherforth's (Thomas) Ordo Institutionum Physicorum. Cambridge, 1743. Reaumur, Histoire des Insectes. 6 vols. 4to. Old calf. Paris, 1734-42. Salmonia. 12mo. Boards. Plates. London, 1832. Samoulle's Entomologist's Compendium. Svo. Half calf. London, 1819. Saint-Hilaire, Histoire Naturelle des Maramiferes. Svo. Half calf. Paris, 1829. " Zoologie Generale. 8vo. Half calf. Paris, 1841. Salvianus Aquatilium Historic. Folio. Parchment. Rome, 1554. Scheuchzer's Histoire Naturelle de la Bible. 8 vols, in 5. Folio. Full Russia. Amsterdam, 1732-37. Schlegel, Essai sur la Physionomie des Serpens. 2 vols. Svo. Sheep. And Atlas. Haye, 1837. Schoolcraft's View of Mines and Minerals of Western United States. 8vo. Boards. New York, 1819. Seba Albertus, Locupletissimi Rerum Naturalium Thesauri. 3 vols. Large folio. Full sheep. Amsterdam, 1758. Sepp, Nederlandsche Vogelen. Imp. folio. Half calf. Amsterdam, 1770. Selby's British Ornithology. 2 vols. 8vo. Half mor. Edinburgh, 1833. Shaw, George, General Zoology. Vol. III. 2 parts. Svo. Boards. London, 1802. " " Zoological Lectures. 2 vols. Svo. Half calf (and duplicate, half bound.) London, 1809. Shepard's Mineralogy. 12mo. Cloth. New Haven, 1844. Shepard's Report of the Geological Survey of Connecticut. Svo, 188 pp. New Haven, 1837. 106 Shepard's Syllabus to Lectures on Chemistry. 8vo. 204 pp. Charleston, 1841. Smellie's Philosophy of Natural History. 4to. Half calf. Edinburgh, J790. Another copy. 8vo. Dover, 1808. Smith's Botany. Boston, 1814. Smith's (J. E.) Memoirs and Correspondence. Edited by Lady Smith. 2 vols. 8vo. Boards. London, 1832. Smith (J. E.) on the Sexes of Plants. 8vo. Half calf. London, 1786. Smith's (J. E.) Selection of the Correspondence of Linnaeus, &c. 2 vols. 8vo. Boards. London, 1821. Smith's Tracts on Natural History. 8vo. Old calf. London, 1798. Smith's (S. S.) Essay on the Human Species. 8vo. Sheep. New Brunswick, 1810. Smith's (J. V. C.) Fishes of Massachusetts. 12mo. Boards. Boston, 1833. Soemmerring (Thomas von) on the Elephant, Mastodon, &c. Specimen ArchsBologise Telluris. 4to. Pampli. Gottingen, 1803. Specimen Lithographiae Helvetica. Old calf. 24mo. Liguri, 1602. Spallanzani's Natural History of Animals and Vegetables. 2 vols. 8vo. Sheep. London, 1784. Spallanzani's Travels in the Two Sicilies. 4 vols. 8vo. Calf. London, 1798. Stark's Natural History. 2 vols. 8vo. Half calf. Edinburgh, 1828. Stillingfleet's Tracts relating to Natural History, &c. 8vo. Sheep. London, 1791. Storer's Fishes and Reptiles of Massachusetts. Svo. Half calf. Storer's Synopsis of Fishes of North America. 4to. Boards. Cambridge, 1846. Swainson's Birds of Brazil and Mexico. Svo. Half mor. gilt. London, 1841. Swaramerdam's History of Insects. Folio. Old calf. London, 1758. Syst^me Naturelle du Eegne Animal. 2 vols. 8vo. Calf. Pai'is, 1754. Schaeffer's Elementa Entomologica. 4to. Eatisbon, 1755. Tayloi-'s Report on the Washington Silver Mine. 8vo. 40 pp. Plates. Phil- adelphia, 1845. Temminck, Manuel d'Ornithologie. 4 vols. 8vo. Half calf. Paris, 1820-40. Thacher's American Medical Biography. Svo. Boards. London, 1827. Thompson's Zoological Researches. 4 nos. Svo. Pamph. Cork. Timb's Knowledge for the People. 5 nos. 24mo. Boston, 1831-32. Transactions of the Natural History Society of Northumberland, Durham and Newcastle-upon-Tyne. 2 vols. 4to. Half mor. Newcastle, 1831-1838. Transactions of the Geological Society of Pennsylvania. Vol. L 8vo. Cloth Philadelphia, 1835. Transactions of the Literary and Philosophical Society of New York. Vol. I 4to. Boards. New York, 1815. Temminck, Monogi-aphies de Mammalogie. . Tome L 4to. Old calf. Paris 1827. Tudor's Letters on the Eastern States. Svo. Boards. Boston, 1821. Vasari, Le Vite dei Pittori. 4to. Parchment. Fiorenza, 1568. Virey, Philosophic de I'Histoire Naturelle. Svo. Half calf. Paris, 1835. Voyage dans le Nord d'Hayti. 4to. Paper. (Imperfect.) ■ 107 Wallis on the True Age of the World. 8vo. Cloth. London, 1844. Wallace's Dissertation on the Number of Mankind. 12rao. Calf. Edinburgh, 1753. Wells on Dew. 8vo. Boards. London, 1815. Wernerian Natural History Society Memoirs. 7 vols. 8vo. Half calf. Edin- burgh, 1811-38. White's Journal of a Voyage to Nc\y South Wales. Eoyal 4to. Full calf. 65 plates. London, 1790. Whitehurst's Works. 4to. Old calf. London, 1792. Wiegmann, Archiv fur Natiirgeschichte. 9 vols. Half calf. 2 vols, iu nos., in all 11 vols. 8vo. Berlin, 1835-45. Willoughbeii Ornithologia. Folio. Old calf. London, 1676. Wilson's American Ornithology. 3 vols. 8vo. Half mor., uncut. New York and Philadelphia, 1828. Wilson's American Ornithology. 9 vols. 4to. Half bound. Philadelphia, 1812. Wilson's American Ornithology. Royal 4to. Half mor. New York, 1829. Wilson on Lisects. 4to. Boards. Edinburgh, 1835. Wilson's Natural History of Fishes. 4to. Boards. Edinburgh, 1838. Wilson's Natural History of Quadrupeds and Whales. 4to. Boards. Edin- burgh, 1838. Witham's Observations on Fossil Vegetables. Thin 4to. Boards. Edinburgh, 1838. Wood's Ornithological Guide. 8vo. Cloth. London, 1835. Wiegmann, Herpetologia Americana, fol. Beroliui. 1834. Wood's Catalogue of the Best Works on Natural History. 8vo. London, 1832. Webster's History of St. Michaels. 8vo. 1821. Yarrell's British Fishes. 2 vols. 8vo. Half calf. London, 1836. " British Fishes. Supplement. 8vo. Cloth. London, 1839. " British Birds. 3 vols. 8vo. Half calf. London, 1843. Zimmermann, Specimen Quadrupedum. 4to. Sheep. London, 1777. Zoological Journal. 6 vols. 8vo. (1 of plates.) Half Russia, London, 1825-29. — Deposited by 3Irs. Amos Binney, January 7, 1857. The President in the Chair. ' Mr. James E. Mills exhibited specimens of slate from Somerville, Massachusetts, and read the accompanying account of an analysis made by Mr. L. M. Dornbach, of the Lawrence Scientific School. 108 The following analysis of a variety of Slate, found in the town of Somerville, Mass., near Boston, was commenced upon the supposition that it was a Dolomite ; as the cleavage resembled, in many respects, that of rhombohedral carbonates. The angle which the plane in the direction of the dip makes with the plane of stratification is 102.*^ The angle which the other plane of cleavage makes with that of stratification is 112'*. The angle which the two planes inclined to the plane of strati- fication make with each other is llC, though this varies some- what in different specimens. The specific gravity is the same as that of Dolomite, being 2.8192. Analysis shows it to be a silicate of iron, alumina, lime, and magnesia, in which the lime forms less than one per cent, of the whole, as is shown by the following table : — Water 3.439 Sesquioxide of Iron 8.324 Sesquioxide of Alumina ,...*, 19.353 Lime ........ .625 Magnesia 4.944 Silica 63.238 99.923 The President exhibited the dilated vena cava of an Otter, {Lutra Canadensis,) recently taken in Massachu- setts, and explained the peculiar physiological condition of this animal in connection with its diving habits. He also pointed out some other interesting points in its anatomy. Prof. H. D. Rogers made some remarks upon Ameri- can and European Geology, in anticipation of a paper which he said he intended to bring before the Society. Dr. T. M. Brewer read the following paper on Vireo- sylvia : — In the Proceedings of the Academy of Natural Sciences of Philadelphia, (Vol. V. p. 153,) a description of a new species of 109 Vireosylvia is given by Mr. John Cassin of Philadelphia, from a single specimen obtained by him in Brigham's Woods, near that city. Its close resemblance to V. gilva, and the fact of its having been for some time an unique specimen, has led to the doubt whether it was a good species. Mr. Cassin described it as differing from the gilva, which it most resembled, in being smaller, in having a shorter and weaker bill, and a form gen- erally shorter and stouter, with colors more vivid, and the super- ciliary line more distinct. He named it Vireosylvia Philadel- phica. Two yeai's since, my attention was called by Thure Kumlien, Esq., a very accurate and careful ornithologist of Wisconsin, to a specimen of Vireosylvia obtained by him near Lake Kos- kouong, in the southwestern part of that State. He thought it a distinct species from any he had seen any description of, and quite distinct from the F. gilva. I gave the specimen to a friend, upon whose judgment I relied more than I could upon my own, who pronounced it a V. gilva. Mr. Kumlien was not satisfied with this decision, and still insisted that its habits, even more than its plumage and size, showed it to be a distinct species. The following year he sent me several specimens which I gave to Mr. Cassin, who had no doubt that they were of the species he had described as F. Philadelphica, though others to whom I showed them were still unconvinced. In answer to a letter in which I informed Mr. Kumlien that his birds were supposed to be the V. gilva in an unusually fresh plumage, he wrote me the answer which I give below. It proves, to my mind, conclu- sively his correctness, establishing the species to be a good one, distinct from V. gilva and identical with that described by Mr. Cassin as F. Philadelphica. I take the greatest pleasure in thus giving Mr. Kumlien the credit of having worked it out, unaided by any suggestion or help from any one, in view of the disadvantages under which he labors in the want of access to any text-books. His letter is interesting, as throwing the first light that has yet been given to the public upon the habits and distribution of this new and little known species. The following is the extract referred to : — " In regard to the Vireo which I sent you last being the Vireo gilvus ' in an unusually fresh plumage,' I beg your perusal of 110 the following remarks. You may think it bold in me, but so far as I read Wilson I am not satislied in regard to this vireo matter. " Vireo ffilvus, Wilson — in every respect agreeing with Wil- son's description — is common here from the 8th or 10th of May till September. It consequently breeds here. It is an excellent singer. I have a number of skins, and all agree in their mark- ings. There is very little difference between its spring and autumnal dress. It is found in openings more than in thick timber, and frequently near farm-houses. Its length varies from 5J- to 6 inches; I have one that measures full six. Vireo ? — that which I sent you, and which cannot be V. ffilvus if the pre- ceding is — is by no means so common as the other, and I have never observed it before May 15th, and only from the loth to the 25th of May and in September. I never heard this bird sing a note. It keeps in the most secluded thickets ; I never found it anywhere else. It is a smaller bird than the other. Its length is from 5 to H^ inches, which is the longest I have ever found. I admit that in general markings both birds are very much alike, but the ffilvus is a more slender bird than the other, which appears stouter. Between the spring and autumnal dress of the ffilvus, as I have said, there is but little difference in the markings, but the other, in autumn, is considerably tinged with yellow. Another point is the difference in the relative length of the primaries, which is as follows : — V. ffilvus. * Vireo ? First primary very short. First primary longer than Sth. Second do. longer than 6th. Second do. "> longest and of Third do. ~> longest and of Third do. ) the same length. Fourth do. j the same length. Fourth do. longer than the 1st. Fifth do. longer than 2d. Fifth do. shortest. Wing 3 inches. Wing 2^ inches. " This will, I think, separate them. This measurement was taken from several specimens. " But the question may arise, is not my F. ffilvus perhaps the V. Novehoracensis ? It is not ; the iris is hazel and not white, and moreover, on my ffilvus there are no yellow markings, except a very faint greenish-yellow on the breast. V. Novehoracensis is Ill 5-^ inches in length, and I never had a specimen of V. gilvus so small as that." I have given Mr. Kumlien's letter in nearly his own language, and in no instance have I varied from his meaning. I think it establishes his vireo to be a good species, and if so, it is the Vireosylvia Philadelphica of Mr. Cassin. President Hitchcock exhibited specimens of impres- sions, which he supposed to be those of a Myriapod, found at Turner's Falls on Connecticut River. President Hitchcock also presented specimens of de- pressions found in the Sandstone of the Connecticut Valley. They were of regular polygonal forms, gen- erally from five to eight sided, shallow, and about an inch in diameter. Similar depressions have been found in the Niagara Limestone of New York, of two or three feet in diameter. Mr. Hitchcock suggested that they might have been made by tadpoles. He had observed these animals in the water contained in the excavations, and had been informed by boys that they had seen tadpoles in the act of excavating them. In 1850, Prof. B. Silliman, .Jr., exhibited similar specimens to the American Asso- ciation for the Advancement of Science, and read a letter from a gentleman suggesting the same explanation of their forma- tion. This explanation Prof. H. had not heard of, until he had conceived the idea himself. Mr. Hitchcock further stated that he was now doubtful, if the tracks which he had supposed to have been made by birds, in the Connecticut Valley Sandstone, were really jjroduced by birds, since one great argument, viz : that of the number of phalanges in the toe, is lost. Tracks of an animal, which was certainly a quadruped, are now found, presenting the same number of pha- langes and toes as the dinornis. Specimens of Clay Stones were exhibited by Mr. Charles Stodder and Mr. Ambrose Wellington. The Committee appointed to memorialize Congress, 112 reported that they had prepared a memorial and for- warded it to Washington. Dr. Weinland read a paper on series in the animal kingdom, as follows: — ON SERIES IN THE ANIMAL KINGDOM. BY DAVID F. WEIN- LAND. The existence of certain Zoological Groups, namely, those of Classes, Orders, Families, and Genera, was first noticed by the father of Zoology, Aristotle. Two thousand years afterwards, these groups were again brought to light and named by Linnaeus. They have since been improved by Cuvier and Baer, and the idea of type has been added. But it was not till lately that the signification, at least of three of them, viz : of CLasses, Orders, and Families, was recognized and circumscribed by Agassiz. These ideas will henceforth stand and be acknowledged as founded in nature. But the question arises, whetlier there do not exist still other relations and I'eal afiinities of animals to each other, which are not included in these groupings, which have an equal right to be introduced into our zoological system. We think that this is in foct tlie case, and we shall endeavor to show in the following sketch, that there exist throughout the whole animal kingdom afiinities of the animals to each other, which we can comprehend under the name of " Series." About twenty years since, a German Naturalist, Kaup, spoke of series in the animal kingdom, but his ideas proving somewhat arbitrary, the subject received less attention than it deserved. Nevertheless, its truth, if rightly understood, has been since recognized by some distinguished naturalists. Oken, for instance, spoke of a scale among Articulata, in which he placed the worms lowest, next the Crustacea, and last the insects ; and Agassiz has illustrated this gradation fully in the development of the butter- fly, and has added still another amongst insects proper ; starting from the principle that chewing rank below the sucking insects. Another order of position has been recognized by Milne Ed- wards and by Dana among Polypi ; another by Leopold von Buch among Cephalopods ; another by Dana for Crustacea. We 113 have tried to trace out these gradations also, among the higher animals, and the success which we have met with, wherever we have had accurate information, has convinced us that such grada- tions, which might very properly be termed series, really exist throughout the animal kingdom. Thus, among Mammalia, Ave have recognized until now two natural series running parallel to each other, a carnivorous and a herbivorous series. The carnivorous begins with the whales, runs through the dolphin, seal, and Intra, to the marten, whence it divides into two branches, one Plantigradous, the other Digiti- gradous. The latter of these branches runs through the cat, leopard, and dog, where it ends ; the other, that of the planti- gradous, runs through Nasua, Procyon, (raccoon,) bear, to the cynocephalous monkey, and through the liigher monkeys to man. In this latter series, we would call the attention of naturalists particularly to the bear, as the intermediate link between carniv- orous animals and monkeys. When we consider the mixed animal and vegetable food of the bear, its manner of life, and general habits, its climbing and embracing propensities — for in the bear we find an atm capable of embracing as in the monkey — and when we ob^rve its manner of standing upright on its plantigradous feet, wtliich is evidently connected with the use of the fore legs as arms, there can be no doubt that the bear fills out that gap which seems to exist between carnivorous animals and monkeys. Such is the carnivorous series. Parallel to this, and analogous to it, runs a herbivorous series ; beginning with the Zeuglodons, and running through Sirenoids, Morse, Dinotherium to Anoplotherium. Here it divides into two, the Pachyderms and the Ruminants, and thus Owen was right when he said that the Anoplotherium includes the characters of Ruminants and Pachyderms. From Anoplotherium starts on one side the Ruminant series, running through camel, cow, ante- lope, deer, — and on the other side, the Pachyderm series, running from Anoplotherium to Palajotherium and Tapir. At this point we have another division into the series of horses, which culminates in our domesticated horse, — and the series of hogs, which embraces rhinoceros, elephants, and hogs. Among Birds, there are at least four series : one starting from the ostriches, and ending with the Gallinaceie ; — (I would re- PROCEEDINGS B. S. N. H. VOL. VI. 8 MARCH, 1857. \(ir 114 mark, in passing, upon the striking similarity which exists be- tween the ostrich and the young of the domestic fowl) — a second beginning with the pelican, and ending with the Gallinula, a wader; a third beginning with the hawks, and ending with the singing-birds ; a fourth beginning with Rhamphastos, and ending with the parrot ; another beginning with the Buceros, and ending with the swallow and humming-bird. In Reptiles, there seems to be but one series, — snakeS, lizards, and turtles ; the snakes moving by the dorsal column, and having head, neck, trunk, and tail united ui one 'continuous body, are analogous to the whales, and the Sirenoids. The lizards, pro- vided with a distinct neck, trunk, and tail, and with legs, are analogous, the lower ones, the Anguiformes, to the seals, the higher, to Lutra and Marten. In the turtles, the distinction of parts is carried still farther ; the head and neck are very free, the trunk which, in lizards, assists in locomotion, is scarcely used for this purpose, and the four legs are the locomotory organs. In the class of Batrachia we have again the same series. Cascilia is snake-like, and wholly analogous to the snakes and to whales. Icthyoids and Salamanders, provided with small or well-developed legs, are wholly analogous to lizards, and the frogs and toads to turtles.' In frogs and toads also, the four legs are the only organs of locomotion, but the neck and head are not as free as in turtles. This goes far to prove that the class of Batrachians ranks lower than that of Reptiles, January 21, 185T. The President in the Chair. Dr. Henry Bryant read the following paper, entitled — A LIST OF BIRI>S OBSERVED AT GRAND MANAN AND AT YAR- MOUTH, N. S., FROM JUNE 16 TO JULY 8, 1856. In the early part of last summer I made an excursion, in company with J. E. Cabot, Esq., to the island of Grand Manan 115 and to Yai'mouth, N. S. ; principally with the view of observing the habits of the birds breeding in those localities. The follow- ing species were seen by us ; those marked with an * only at Manan, and those marked with a f only at Yarmouth : — * Halicetus leucocephalus. A pair of full-plumaged birds were seen every day at low tide, apparently watching for an oppor- tunity of robbing the gulls of any thing worth the trouble. * Hypotriorchis columharms ? A bird which appeared to be of this species was seen at Duck Island. * OtMS Cassinn. A nest of this bird was found by Mr. Cabot in the midst of a dry, peaty bog. It was built on the ground, in a very slovenly manner, of small sticks and a few feathers, and presented hardly any excavation. It contained four eggs on the point of being hatched. A young bird, the size of a robin, was also found lying dead on a tussock of grass in another similar locality. Chordeiles Virginianns. Only a few individuals seen. Chcetura jyelasgica. Quite common. A number of these birds •were seen flying round the northeastern head of Green Island at Yarmouth, and were, without doubt, nesting there, as they were seen to fly in and out of the crevices of the rocks — the impos- sibility of ascending the face of the cliffs prevented an actual verification of the fact. Hirundo Americana. Not so common as either of the other two species of the genus. Hirundo bicolor. Very common ; breeding in hollow stumps. Incubation had generally commenced by the 2d of June. Hirundo rufa. By far the most common swallow, particularly at Manan. The nests were almost universally built without the projecting neck. Of late years, these birds, as they become more habituated to building in sheltered situations, have nearly discon- tinued their former habit of building their nests in a retort shape. Tyranmda Jlaviventris. This pretty little Flycatcher was more numerous at Manan than at Yarmouth. Though apparently unsuspicious, it was difficult to procure, in consequence of its restlessness and its frequenting almost exclusively the thickest clumps of alders and small firs. In its habits it approximates more nearly to the warblers, than does any other species of the genus that I am acquainted with. During our walks in the roads IIG and paths tlirougli the woods, it was never seen perched on a dry twig or overhanging branch, waiting for passing insects, as is the favorite habit of most of the genus; it procured its food ahnost entirely by diligently hunting in the thickest foliage, rarely venturing a short distance in pursuit of its prey. The note of this bird is also much softer than that of the other Tyrannulie. Setophaga rnticella. More numerous than I have ever before seen them. The young were hatched at Yarmouth before the 1st of July. Myiodioctes Canadensis. Particularly numerous at Yarraoutli among the small ferns and bushes on the edges of swamps. * Sylvicola icterocephala. Only one pair seen. Sylvicola cestiva. Common at Yarmouth, though not so much so as at Eastport. None were seen on any of the small islands. Sylvicola striata. Abundant in the alders. Sylvicola virens. This species was the most common warbler observed. The males could be seen and beard in every direc- tion ; the females were not so numerous, being probably engaged in incubation or feeding their young brood. Trichas Marilandica. Common everywhere in suitable local- ities. Mniotilta varia. Quite abundant. Pants atricapillits. Not so numerous as Avith us at the same season. t Parus Hu.dsonicus. Quite a number of these little titmice were seen on the Big Mud Island. A pair of old birds with their young brood were seen near Yarmouth on the 3d of July. Their habits seemed identical with those of the common species. Though the young were fully fledged and could fly with ease, the old ones were so solicitous for tlieir safety that I could almost catch them in my hands. A nest was found near by that proba- bly belonged to this family; it was built in a dead white-birch, in the same warm manner that the common Chickadee builds with us. The note resembles that of the common species, but is shai'per and more filing, and can readily be imitated by the syl- lables Tzee-dee -dee-dee uttered with the front teeth in juxtapo- sition. Tiirdus migratorius. This bird, so preeminently domestic with 117 us, confining itself almost entirely during the breeding season to the garden or orchard, was extremely numerous, but had appar- ently lost its desire for human society. We found it nesting everywhere, in the thickest woods and most secluded pastures, much oftener than in the neighborhood of houses. The eggs of the second brood were already laid, and incubation commenced by the 25ih of June. Tur^dus olivaceus. One specimen was seen at Long Island, Manan, and another at the Big Mud, Yarmouth. Its note differs entirely from that of the T. soUtarius ; it also differs very much in its habits, the latter species being generally seen on the ground, while the olivaceous Thrush prefers to procure its food among the branches. The one seen at Big Mud was perched on the top of a small dwarf-fir, and was hunting the passing insects, with all the dexterity of a typical ilycatcher. Tardus soUtarius. Very numerous. The plumage of the old birds was much worn by rubbing against the thick bushes that they principally inhabit; there was also much less of the yellow- ish tint on the breast than oil specimens procured at other locali- ties. The first brood had already left the parent birds. One procured on the 27th of June, was fully fledged, but so unlike the adult that I append a description of it : Wings, tail, and greater wing-coverts as in adult. Rump reddish-brown, with light yellowish-brown spots, most distinct towards the back. All the rest of the upper parts olive-brown, with a long lanceolate whitish spot in the centre of each feather, and the tip blackish-brown. Smaller wing-coverts ferruginous-brown, with spots of light yel- lowish-white, in the centre of each feather, occupying the greater part of the tip, and running to a point towards the base. Throat whitish in the centre, a black line on each side from the base of lower mandible to below the eye. All the under parts more yellowish than in the adult, with the sides of the neck, breast, and flanks spotted with blackish-brown — the spots being rounded on the centre of the breast, transvei'se on the upper part of the abdomen, and V-shaped on the side of neck and breast, most distinctly so on the latter. The general effect of the plumage is precisely the same as that of the DendrocolaptincE. Zonotrichia savanna. Particularly numerous on all the grassy islands ; incubation nearly completed by the 2oth of June. 118 Zonotrichia Pennsylvanica. On arriving at Manan, we were at first much puzzled by a note that we had never heard before ; the bird that made it was always perched on the top of some small tree or bush, and before being approached sufficiently near to identify it, would drop into the bushes beneath. On watch- ing the spot and shooting the bird, that we supposed had made the note, it proved to be a White-throated Sparrow ; but the note was so different from the soft warble made by that bird with us in spring, that for some time we supposed that we had shot the wrong bird. This note can readily be imitated by pro- nouncing the syllables Pee-pee-pee-peehody-peebody, rather slowly and in the same key. Few were seen in the neighborhood of houses, but wherever the woods were thin, with an undergrowth of bushes, or in bushy pastures, they were quite numerous. StrutMo nivalis. This common and neat-looking sparrow, as Dr. Brewer observes, takes the place occupied by the Emberizella socialis with us, and is, if any thing, more confiding and domestic in its habits. The young were universally hatched by the 25th of June. The note is almost exactly similar to that of the Chip- ping Sparrow. Oarduelis tristis. Not common. Erythrospiza purpurea. Not more numerous than in Massa- chusetts during the breeding season. Quiscalus versicolor. A few seen. * Gorvus corax. One pair seen. Gorvus Americanus. Very common ; more so at Manan than at Yarmouth. Garridus cristatus. Common. t Garridus Ganadensis. At Yarmouth, we saw more of this species than of the common Blue-jay. The name generally given it by the inhabitants is Cat-bird. The bird called Cat-bird with us, Mimus felivox, we did not see either at Manan or at Yarmouth. Some others of our common birds that were not seen by us were Mimus rufus, Tardus Wilsonii, Sialia Wilsonii, Dolychonyx ory- zivora, Fringilla graminea, Pipillo erythrophthalmus, Sturnella ludoviciana, Molothrus pecoris, Sterna argentea. Bomhycilla GaroUnensis, Not common. Picus puhescens. Several seen. * Picus arcticus. One pair seen at Manan. 119 Colaptes auratus. Not nearly as common as in Massachusetts. '\ Ectojristes migratorius. A dead female was found on Green Island, twelve miles from Yarmouth. It presented no appear- ance of having met a violent death. Totanus macularms. Very abundant on all the grassy islands. Incubation generally terminated by the 1st of July. t Totcmus semipahnatus. One pair seen. A nest was found by the boatman, containing, as usual, four eggs. This bird I do not think has been observed breeding on the New England coast north of Cape Cod. Charadnus melodus. Abundant ; breeding on all the sandy or gravelly beaches. The young were observed running about by the 25th of June. Charadrius semipahnatus. Only a few seen. t Anas obscura. One pair seen at the Big Mud Island. Somateria mollissima. During our stay at Manan we saw a dozen or two of these birds, and obtained two eggs at the inner Green Island. At the Mud Islands they were much more numer- ous. A number of females with their young broods were seen. The largest of the young were about a quarter grown. On ap- proaching them, they dived with as much apparent facility as the old ones, and did not rise till they were at a safe distance. t Sula hassana. On arriving at Yarmouth, we were informed that we should find plenty of Gannets on Gannet Rock. But it was with a feeling of surprise almost as much as satisfaction, that on approaching the rock sufficiently near, we first saw the birds. The rock itself is a miniature of the Gannet Rock of the Gulf of St. Lawrence, as described by Audubon, and is as difficult, probably more difficult, of access. On approaching it, the Gan- nets were seen to the number of some hundreds, covering the northern end of the summit ; they were quite shy, and had all left the rock before we had arrived within a hundred rods of it ; they flew round our heads a few times, and then gradually dis- appeared. The number of full-plumaged birds was greater than I expected, as, from this being probably their most southern breed- ing place, I had presumed, in accoi'dance with the common laws governing the migration of birds to the colder regions, that the majority would be in immature plumage. The number of brown birds was about one to three of the white, or adult birds. On 120 scrambling to the summit of the rock, we found the nests ranged all round its borders, most numerous on the northern aspect, where they formed a continuous row; they were very bulky, composed entirely of eel-grass, and were apparently used for more than one season, as several of thera had been recently repaired. The whole surface of the rock, as well as the outside of the nests, was white from the droppings of the birds, and the nests themselves, viewed from a short distance, looked more like petrifactions than any thing else, encrusted as they were with urea. The number of the nests, by count, was one hundred and fifty. Not a single egg was found in any of them, as they had been recently robbed. The same day we saw a fisherman at Green Island, who said that the Monday previous he had taken sixty eggs from the rock. Sterna hirundo. A dozen pairs were breeding on the inner Green Island at Manan, and many hundreds on Green Island at Yarmouth. In consequence of the facility of access to Green Island from Yarmouth, the birds are much disturbed. During the short time that we passed on the Island, two other parties landed for the purpose of egging. t Sterna arctica. We found several hundred pairs of these birds breeding on one of the Mud Islands. It was the first time that I had ever found them breeding apart from other species of the genus, and was therefore much pleased at being able to examine a large number of their eggs, the authenticity of which was positive. On comparing them with a number of the eggs of the common tern procured at Green Island, no specific difference could be discerned. Some of the nests were made in the short grass at the edge of the beach, others on the masses of sea-weed that had been driven up by storm above the ordinary reach of the w;ives, and others were mere excavations in the sand and gravel of the beach. On examining specimens the moment they are shot, the pearl-gray tint of the lower parts is frequently not readily perceived, except in certain lights, and if this color were the only specific character, it would frequently be impossible to distinguish them from the common tern. This color grows grad- ually deeper after death, and finally becomes nearly as dark as that of the upper parts. The length of the bill varies consider- ably in this as well as in some other species of tern, the difference 121 being more than a quarter part of the length of the shorter speci- mens. The long external tail-feathers are also very variable in length, being an inch and a half shorter in some specimens, with- out any appearance of having been broken or worn. The only diagnostic character that can be depended on in specimens of all ages is the comparative length of the tarsi which are always longer than the middle toe in the common species and never longer in the arctic. The following table gives the comparative length of the tarsus and middle toes of three specimens of each species taken at random : — S. Arctica. S. hirundo. 9 9 $ s c? 9 1 2 3 1 2 3 *15 15 14| 18^ 201 19 154 m 16 17 18 16 Tarsus IMiddle toe . Lams argentatus. The favorite breeding-places of this bird, at Manan and the neighboring islands, were the heaths, as they are called by the inhabitants — dry, peaty bogs, covered with coarse grass, scattered bushes, and dwarf firs. The nests were generally placed so as to be sheltered by the firs or bushes, seldom in the open heath. I should imagine, from Audubon's desci'iption, that the number of nests on trees was greater at the time of his visit than at present. This may be accounted for by the fact that the breeding-places having been protected for some time by the owners of the islands, the birds have not been so much disturbed as formerly. On the Big Mud Island, near Yarmouth, they were also found nesting on trees. More or less were found breeding on all the islands we visited ; but everywhere with the exception of the places mentioned, the nests were placed in the grass among the rocks, or on the rocks themselves. The eggs found in I)laces where the birds had probably not been disturbed were about half hatched by the sixth of July. Dr. T. M. Brewer states, in the 6th Vol. of the Journal, page 304, that the Larus leucopterus is occasionally found breeding on the island near Manan. As this bird is quite rare with us, and has always been supposed to breed only on the shores of the Arctic Ocean, it was an object of special search both to Mr. Cabot and myself ; but with * Millimetres. 122 the exception of a single pair of Saddle-backs, Larus marinus, no large gulls, other than the herring-gulls, were seen by either of us. All the inhabitants at Manan, with whom we conversed on this subject, stated that there was a bird, called by them Farmer Gull, larger than the herring-gull, with a dark head and shoul- ders, which was occasionally found breeding in solitary pairs on the rocky islands. This description of the farmer gull is proba- bly correct as far as it goes, more particularly as their attention had been called to a specimen, unfortunately destroyed before our arrival, which had been procured for Dr. Brewer. When at Manan, we were told that we should find this bird much more numerous at the Seal Islands, near Yarmouth. On ai'riving at Yarmouth, we still heard of the Farmer Gull, and the same description was given of it as at Manan, but we were told that it was seldom seen there, though quite abundant at the Bay Cha- leur. What species this bird may prove to be I do not know, but am inclined to think, if a described species, it is a black- backed gull in immature plumage, though the inhabitants who had been in the habit of seeing this gull, did not consider it the same as their so-called Farmer Gull. t Larus marinus. One pair seen at Big Mud Island. t Larus atricilla. Two pair seen at Green Island near Yar- mouth. Their nests were not discovered, but the birds were shot, and evidently, from the enlarged state of the oviducts of the females, had recently finished laying. This is another of the birds which are common on the shore south of Cape Cod, and mentioned by Richardson as inhabitants of the fur countries ; they are not known to breed between Cape Cod and the Bay of Fundy. * Lestris Richardsonii. One pair seen near Green Island. TItalassidroma Leachii. This bird was found breeding in the manner described by Dr. T. M. Brewer, on some of the small islands near Manan ; and also on the islands near Yarmouth, including the Mud Islands, mentioned by Audubon as the breed- ing places of the Wilson Petrel. Mormon Arcticus. Only one specimen of this singular bird was seen near Manan, but at the islands in the neighborhood of Yarmouth they are still quite abundant. The only place where we found them breeding was at Gi-een Island. One egg was found here laid in a crevice in the rocks. Several burrows were 123 seen, much too large for the Petrels, and were probably made by the PulRn, but neither eggs nor birds were found in them. TJria grylle. This bird was found breeding wherever the locality was suitable. On one of the islands near Manan, called the Inner Green Island, we purchased twenty from a man who had collected them there. From the number of inaccessible rocks in this vicinity, (the breeding-places by choice of this bird,) its number will not probably be much diminished for years. It breeds as far south as Mt. Desert on the coast of Maine. t Uria troille. Gannet Rock is nearly divided, by a deep chasm, into two portions. On scrambling up its sides, we saw a number of guillemots standing on the rocky shelves of the most precipitous part ; seven eggs could be seen within the space of three or four feet square ; these were procured with great difficulty and some danger, by the boatman. They were all light blue, with fewer marks than is generally the case. Incubation had commenced in five of them. The birds were quite tame, and would occasionally alight on the rocky shelves within thirty yards of where we were standing watching them. Most of the time they were flying through the fissure in the rock, always coming from the same side, and passing sometimes within a few feet of our heads. On Green Island, a single young one was procured, apparently a few days old. fAlca torda. A number of auks were seen at Gannet Rock and also at Green Island. Two eggs were found at the latter place, and an old female was caught alive by Mr. Cabot. A much greater number of the four last-mentioned birds was seen, than were apparently breeding in the neighborhood ; this might very probably be caused by the larger proportion of them being barren birds. This fact was not ascertained, as it might have been, by dissecting a number of the birds, as we did not feel inclined to aid in their fast approaching extirpation from this their most southern stronghold. Dr. Gould inquired how these birds compai-ed with those of Northern Europe, and the Northwest Coast of North America. The Arctic circle has been considered one uniform Zoological Region ; he had recently examined shells collected by Mr. Stinip- son in Behring's Straits and upon the northwest coast of North 124 America, and had found many of them to be identical with those found between us and Labrador. One shell in particular, iV^wci/Za thraciceformis, he alluded to ; one valve of this shell brought from Japan, exactly mated an opposite valve taken at Prov- incetown, Mass. At Hakodadi, Japan, the Arctic fauna exists, and some shells of our coast are found ; whilst at Simoda the shells are those of the China seas. Birds can traverse the ocean in the northern regions where the continents approach each other, but it is a question if mollusca can travel such distances. Dr. Bryant stated that the majority of our Arctic birds are identical with those of Europe ; and that the Arctic Ornithology of the Western Coast of North America differs more from that of the Eastern Coast than the latter does from that of Europe. He also stated that the migration of birds is an interesting subject bearing upon this question, the causes of migration being by no means fully understood. This present winter, one of our most common migratory birds, the Song Sparrow, (^Zonotrichia meloda,) is quite abundant in the vicinity of Boston, and two, which Dr. Bryant' killed for the purpose of examining them, were fat and in good condition, showing that they had not suf- fered from the severity of the weather, or the want of food, causes generally assigned for the autumnal emigration of birds from this region. Dr. T. M. Brewer stated that it had been ascertained that there is a greater diversity of species among the birds of the Eastern and "Western North Atlantic coasts than was formerly supposed. Several species, bearing close resemblance upon the two continents, have been established to be different — for ex- ample, the Velvet Duck, the Peregrine Falcon, and the Fish Hawk. It was interesting to observe that, for no apparent cause in their organization different from that common to both shores, many birds are found only on one or the other shore ; for in- stance, the INIanx Shearwater, the lesser Saddleback Gull, the European Scoter, (differing only in size from the American,) are found only in Europe. Between the birds of the Atlantic and Pacific coasts there is more diversity, and also there are observ- able differences of distribution. Thus, Brunnich's Guillemot, found by Dr. Kane in latitude 70° North, and rarely found so far south as Massachusetts Bay, in midwinter breeds in the harbor 125 of San Francisco, in latitude nearly corresponding with that of Ilichmond, Virginia. The Uri'a gryUe, whose extreme southern breeding-point on tiie Atlantic is the Bay of Fundy, breeds also near San Francisco. It may be, however, that the Eastern and the Western birds will yet be found to be of different species. Dr. Brewer believed that they would be. Dr. Pickering observed that the Song Sparrow lives all the year at Philadelphia. As to the passage of birds across the ocean, he could say that a flock of gulls kept company with the ship, in which he crossed the Atlantic some time since, the whole distance. Capt. Atwood remarked that, as to fishes, it is often the most delicate, and those having the thiiniest skins, which are the last to migrate. The President stated that he had recently an opportu- nity, through the kindness of Dr. Bartlett, of New Bed- ford, of dissecting the eye of a Sperm Whale, and the parts surrounding it. On examining the region of the eye, an enormous development of the muscles was inmiediately observed. The sclerotic coat of the eye was very thick, and likewise formed a very thick sheath around the optic nerve, imbedding the bloodvessels, and almost as hard as bone. It was found, however, to contain no ossific matter, and to be simply very dense fibrous tissue. Behind the globe of the eye, and occupying a large space, was a large venous plexus. The eyelids were thick, and the conjunctiva folded back in such a manner as to permit the eye to recede in the socket. The globe of the eye, together with the optic nerve, w^eighed three and a lialf ounces. The powerful retractor muscle, analogous to that of ruminants, weighed five and a half ounces. The other muscles seemed only indirectly connected with the globe, and their use seemed rather to be to open the lid than to move the globe. The muscles which were attached to the lids were of great size, and together weighed one and a half pounds. The object of such muscular power he could not divine. The vascular plexus distended would tend somewhat to force forward the eye, and a sphincter muscle behind the eye would have a 126 similar effect ; but these do not seem to demand such extensive muscular power. Mr. N. H. Bishop gave an account of the Zonda Wind of South America. The " Viente de Zonda" may be called a local wind, as it only blows, in the vicinity of San Juan, of the Argentine Republic, S. A. The town lies at the eastern base of the Andes, three or four leagues from the outer Sierra, South lat. 31° 4', (Molina,) long. 68° 57' West, (Arrowsmith.) Behind the first sierra, in the valley of the Andes, are four or iive farms which constitute the hanllet of Zonda, from which the wind is named. To all appear- ance, the wind is formed outside the range, and blows west upon the town ; but some old guides pretend that it comes from off the snowy caps of the main Cordillera. It blows at all seasons, though in the month of August (midwinter) it is most frequent. This wind is hot and parching to the skin, and brings with it clouds of dust and dirt, that fill the houses of the people with fine sand. All persons leave their work and seek refuge in their houses, while many of the huts of the gauchos are blown away 'by the force of the wind. Most persons are troubled with severe headaches ; those who have been suffering from diseases of the heart, find their complaints greatly aggravated, and frequently there are cases of sudden death. Three or four years since, five persons fell dead during Zondas in the month of August. The Zonda lasts sometimes but two or three hours, at other times more than forty-eight hours. While the Zonda is at its height, a few puffs of cold air from the south announce a change, and immediately the weathercock veers from east and west to north and south, and a cold wind, equally as strong as the hot Zonda, now prevails from the south; all nature is refreshed, and men return to their labors. Mr. Bishop stated that he had opened a communica- tion with a North American residing at the base of the Andes, in South America, and that, through him, he hoped to be enabled to obtain specimens of natural his- tory from that region. 127 The President exhibited the skeleton of a young South American Ostrich belonging to the Society, and pointed out some interesting anatomical features in the bones of the neck and leg. The President also exhibited the Cranium of a Digger Indian, brought by Mr. Samuels from California. Its internal capacity was about seventy-six cubic inches, nearly the same as that of the Australian and Hottentot. The forehead was very narrow, and the posterior part of the head very broad. The President likewise exhibited and pointed out the homologies of the cranial bones of a Python, the entire skeleton of which serpent belongs to the Society. Dr. J. P. Reynolds presented, in the name of Rev. Louis B. Schwarz, a Bulbous Root, from Africa (15° or 18° S. L.) together with a gum found in the sandy soil. In the rainy season these roots throw out a leaf a foot in length, and produce a most beautiful flower. A resinous substance exudes from the bulbs when cut, and probably this resin, found in the soil, comes from the plant. The thanks of the Society were voted to Mr. Schwarz for the donation. The plant was referred to Mr. Sprague, and the resin to Dr. Hayes, for examination. Messrs. L. M. Dornbach, B. C. Ward, Charles Kess- rnann, and Edward Habicht, were elected Resident Mem- bers. February 4, 1857. The President in the Chair. The Corresponding Secretary presented a communica- tion from Mr. Charles Whittlesey, of Cleveland, Ohio, 128 entitled " Remarks explanatory of a Section of the Drift or superficial Materials of the Northwest, from Lake Erie to the Lake of the Woods." Referred to the publishing committee. A communication was read from Mr. E. S. Morse, of Portland, Me., on Helix asteriscus, and specimens of the shell were presented. Helix asteriscus, Morse. Animal, short, bluish. Shell, small, orbicular, very much depressed ; whorls four, rounded above and below ; banded by twenty-five to thirty very thin, transparent, and prominent ribs, very oblique, inclined back- ward ; spire not rising above the last whorl ; suture deeply im- pressed ; umbilicus moderately large, showing all the volutions ; finely striated between the ribs ; in some specimens parallel lines may be observed. Color, light brown. Dimensions : breadth, J^^ in. ; height, ^^ in. Found at Bethel, Me., in company with Pupa pentodon and Pupa exigua, Sept. 28, 1856. Observations. This shell differs from N. annulata, Case, in being smaller, the umbilicus not so large, spire not elevated, intercostal space not marked with parallel lines, but finely stri- ated ; the color is also different. Its peculiar thin, transparent ribs, depressed spire, and deep umbilicus, are prominent features that can never confound it with other species. Mr. Amos Binney read the following communication from his brother, Mr. W. G. Binney, and presented the specimens referred to : — Philadelphia, December 27, 1856. Enclosed you will find a suite of the common American Snail, Helix thyroidiis, Say, for the Museum of the Society. Being engaged in a careful study of the land shells of the United States, I am paying particular attention to ihaiv geographi- cal distribution. In forming suites of all the species from every part of the Union, some interesting results have been reached. The snail in question has been found in nearly every section of 129 the country, and probably exists in all the States east of the Rocky Mountains, with the exception, perhaps, of the peninsula of Florida. In New England it is comparatively rare. In the Middle States it is much more abundant, and reaches its max- imum size. In the Southwestern States it is represented by the form which Dr. Gould considers as specifically distinct, and has described as Helix hucculenta. It is distinguished by its smaller size, the umbilicus being generally closed, and in many individ- uals it has a strong resemblance to H. clausa, Say. The speci- mens from Alabama are at once recognized by the greater quan- tity of calcareous matter in their shells, their larger size and peculiar yellowish tinge. Georgia specimens received from the lit. Rev. Bishop Elliott of Savannah, are furnished Avith a strong denticle on the inner portion of the peristome, near the umbilicus. St. Simon's Isle, on the coast of Georgia, has a very peculiar variety, which has been furnished by Mr. Postell. It is at once distinguished from those of the main land, by a smaller and more triangular aperture, and elevated, pyramidal spire. Another curious form is found only near Philadelphia. It is only one half and often not more than one third the size of the Ohio shell — has a very orbicular aperture, generally not furnished with the parietal denticle. It seems restricted to the immediate vicinity of the city, those from New Jersey, only ten miles distant, being of the common form. Its resemblance to If. bucculenta will at once be noticed — a curious fact, when we consider that one is found on the primary formations, while the other is peculiar to the limestone countries of the Southwest. When fresh, the Phil- adelphia variety is of a pretty pink color. Dr. A. A. Hayes read the following report: — ANALYSIS OF A SPECIMEN OP GUM PROM AFRICA, PRESENTED BY REV. MR. SCHWARZ. The specimen was transparent, of a fine red-brown color, externally hard and bx-ittle ; within, it was tough and slightly elastic. It dissolved in the mouth, becoming tough, like jujube paste, and gave the impression of agreeable sweetness ; after a PROCEEDINGS B. S.N. H. VOL. VI. 9 APRIL, 1857. 130 few minutes, a slightly acrid sensation followed, like that produced by unripe guavas. Its Spec. Grav. is 1.406. In cold water it dissolves wholly, and the solution bears the addition of its bulk of pure alcohol. More alcohol renders it turbid, and as an emulsion it long retains its opacity and uni- formity of diffusion. Alcohol does not dissolve it. 100 parts consist of — Moisture dissipated at 212'' F. . . . 3.46 Pure colorless Arabine ..... 83.42 Glucose 10.80 Salts and Earths 1.28 Coloring and acrid matter, and loss . . . 1.04 100.00 The coloring matter resembles a humate, having an alkaline base, and the salts obtained were carbonates of lime and potash, with silicate and phosphate of lime, and a trace of manganese oxide. All attempts to isolate the body giving the slightly acrid impression, failed, from its easy decomposition. It will be seen, that, as a natural mixture of arabine and glu- cose, this specimen differs from the known gums. Excepting the coloring matter, it is also remarkably pure, and the glucose does not crystallize. An examination of the bulb, which accompanied the specimen of gum, was made, so far as to prove that the bulb furnished a like body, apparently as an excretion. In the bulb, the gum is associated with a bitter principle, which seems to be lost as the gum matures. Economically considered, this gum has some importance. As presented, it has all the valuable qualities desired for uniting surfaces by gumming. Its color can be removed, to adapt it to cases where color would be objectionable. As a mixture of gum and glucose, having the peculiar elas- ticity found in jujube paste, it might be used with advantage in the manufacture of lozenges, and all preparations of a similar kind, into which gum and sugar enter in mixture, as well as in inks and water-colors. Being destitute of Bassorine, it cannot be substituted for other bodies for thickening mordant mixtures. 131 Mr. Sprague staled that he had been unable as yet to determine the species, or even genus of this bulb. In en- deavoring to obtain further information relative to this plant, Dr. Reynolds had ascertained that the missionary station, where it was obtained, was called Otymbingo amongst the Ovambo tribe, about three weeks' journey from Walfisch Bay, the nearest seaport. The bulbs are found in very great abundance around the mission, in a poor soil of reddish-looking clay. During the dry season they give no evidence of activity ; but when the average amount of water falls during the rainy season, they shoot out their leaves to the height of three or four feet. There is a kind of spiral turning of each leaf, and it is curved outward at the tip. The stem, which is four or five feet in height, bears several flowers. Mr. Schvvarz considers the plant allied to the Amaryllis tribe, and is inclined to place it amongst the Bruns- wigia. Dr. C. T.Jackson exhibited a very handsome specimen of Hematite Iron Ore, belonging to the Brandon Iron and Car Wheel Company. This iron is remarkable for its stalactitic character, and is probably of hydrous origin. It is composed of hydrated peroxide of iron, 85g per cent., water, 141 per cent., with a minute quantity of manganese and silica. This ore produces the very best kind of iron, and is easily smelted. It yields about fifty per cent. Dr. Hayes stated that he had proved, from careful analysis and examinations of pseudomorphs, as well as the more ordinaiy foi'ms of hematite, that the infiltration of an aqueous solution of silicates of proto-peroxides of iron and manganese, caused the production of hematite. The beautiful black, glossy coveriu"-, which confers so much beauty on the ores of iron not truly hem- atites, as well as the ore of manganese, is always composed of silicate of proto-peroxide of iron, with silicate of one or both oxides of manganese ; and the compact peroxides of manganese, often owe their density and hardness to this compound. Mr. T. T. Bouve, referring to a discussion on a previous even- 132 ing, upon the slide or fall of land upon the Presumpscot River, near Portland, Maine, some years since, in which discussion he had i)articipated, read documents from parties who visited the locality immediately after the event occurred, in order to show that the views maintained by him were correct, viz : that the phenomenon was due primarily to a partial washing out of the substrata by the action of the river ; — that it might be more truly described as a fall or sinking of the surface, attended with some sliding towards the river, which it croAvded from its course, rather than to a sliding action alone of the surface, occasioning a denudation of the substratum of dny. The presence of this clay to such an extent on the surface, he described as resulting from its being forced up by the crushing weight of the soil over it, through the fissures and divisions that occurred above when the fall took place. This spread over the disturbed area to a considerable extent, and formed numerous hillocks, Mr. Bouve then exhibited a fine series of conci'etions from the clay, most of which had a nucleus of some organic body. Among these nuclei were coprolites of fishes, fish-bones, joints of crabs, Balani, shells of the genera Mya, Bulla, Nucula, and Saxicava. These con- cretions, and those from other deposits of clay, are not, as has been supposed by some, mere balls or masses of clay which have become indurated by carbonate of lime imparted from the nucleus, but true segregations of carbonate of lime from the solution of this substance disseminated in the plastic clay. These bodies ordinarily contain about 50 per cent, of carbonate of lime. They do not always have a nucleus ; on the contrary, those from many localities very seldom have any. These seem by no means neces- sary for their production. Undoubtedly the carbonate of lime in the plastic clay, acted upon by elective affinity, was led to draw itself towards certain points, and to arrange itself more or less concentrically about a centre where might be or not a nucleus of some foreign body. Why the carbonate of lime did not in such cases crystallize, is more than is clearly understood. Probably, it might have something to do with the mechanical action of the clay as a disturbing element. In cases where the forms are flattened disks, or lenticular, as in some deposits, it may be supposed that the strata of clay were of diffex'ent density. This would account for the flattening, inas- 133 much as the force, acting in a radius from a centre, would be more free to exert itself horizontally than otherwise. Dr. Charles T. Jackson stated that he had several times, dur- ing his geological survey of the State of Maine, examined the slide on the Presumpscot River, in Westbrook, and had published a short description of it in his annual reports on that survey. He agreed with Mr. Bouve in opinion that an undermining of the strata of clay, by the action of the river, probably induced the slide, but he was satisfied that the strata of clay marl had slid forward toward the river as well as fallen from the original level of the remaining bank. Whether the frosts of winter cracked the clay at its junction with the bank now standing, and thus let in the water to the soft, plastic clay below, rendering it very slippery, or the desiccation of it had caused such a fissure, was unknown, but there cannot be a doubt that it was owing to the extreme plasticity of the under blue clay that the strata were enabled to slide toward the river, as they have done. The positions of the fir-trees upon the clay bed prove a sliding motion of the mass toward the river. With regard to the concretions found at the slide. Dr. Jack- son stated that the clay marl in which they are found contains about ten per cent, of carbonate of lime, while the concretions generally contain as much as 50 per cent. He considered the crystallizing force of the cai'bonate of lime to be the cause of the concretionary structure and form of these bodies, the foreign bodies occasionally found Avithin them serving as nuclei around which this semi-crystallization took place, the carbonate of lime segregating and carrying with it the inert particles of clay, the spheroidal form being that which would result from this action when the force was not adequate to the production of crystals. He illustrated this view by reference to the spheroidal struc- ture of hyalite and of various hydrous silicates which form from a gelatinous paste in which there is not sufficient freedom of motion to allow of the formation of perfect crystals. In case there were a larger proportion of carbonate of lime in solution as a bicar- bonate, the crystalline foi'ms would become more perfect, as in the well-known crystallized sandstone of Fontainbleau, in which grains of silicious sand are forced into the form of calcareous 134 spar by the energetic segregation of the crystalhzing carbonate of lime; the sand being inert matter which was forced by the calca- reous salt to enter into the crystalline form of the spar. Simihxr illustrations were adduced from chemical experiments and observations in which spheroidal forms result, and also in which foreign bodies are forced to enter into the structure of crystals. He quoted the experiments of Beudant, which he had repeated, in which Prussian blue was included in crystals of nitre and alum. He also alluded to the effects of different men- strua, in modifying the forms of crystals or totally changing their forms, instancing the crystallization of sea salt in the foi'ms of the regular octahedron in a solution of urea, whereas the cube is its usual form. Dr. A. A. Hayes followed Dr. Jackson, in remarking on the concretions called claystones. Having incpiired of Dr. J. how large was the proportion of sand in the Fontainbleau crystallized sandstone, and received for answer about fifty per cent., he said that he had often examined the spots where they were forming, and had noticed a growth equal to the size of a garden bean, to take place in the course of two or three weeks of wet, spring- time weather. To form a just conception of the conditions, the fact must be kept in view, that the beds containing them are composed of fine silts, and in the case immediately under view, these were arranged in planes of deposition of alternate courses, covered by much finer material, in layers of different thickness ; so that the mass was stratified ; the coarser layers being very permeable to water. The rounded forms, often strongly resem- bling organic remains, are found resting between these layers, and a condition necessary to their formation is, the presence in the layer or rock above them of abundance of carbonate of lime. The force exerted by some salts in their tendency to crystallize is brought into view only when we study their formation, and carbonate of lime is one of the constantly occurring salts which well illustrates, in a remarkable manner, this power of assuming regular forms. As has been stated, with fifty per cent, of its weight of sand, it forms regular rhomboids, but the more recent obser- vations of some African travellers, who found their progress im- peded by " stone plants," six or eight inches high, formed of 135 aggregates of spear-shaped crystals of sand, cemented by carbo- nate of lime, show, that this large proportion may be exceeded, while the foreign material is in a somewhat coarse state. In the formation of claystones, however, we are to consider the presence of finely-divided matter suspended in, or so mixed with water of infiltration in spring-time, or general saturation from position, that it has nearly a semi-fluid state. A saturated solution of bicarbonate, or more commonly crenate of lime, finds its way into the soft mass, by frost crevices, or channels left by roots, or even air bubbles, and at these points the concretions commence, when no nuclei of similar chemical composition exist. The finely-divided matter interposes an obstacle to the formation of crystals of carbonate of lime, far greater than an equal amount of coarser foreign matter would do ; and we observe, then, the influence of that beautiful law in accordance Avith which rounded forms are produced. In the laboratory similar forms daily occur, where the presence of finely-divided and diffused bodies, arrests the formation of crystals, and globular, or curved-surfaced solids are produced ; as in the animal frame, the cell structure causes the dissolved phosphate of lime to take the curvilinear form pertainnig to organization. The claystones which are pro- duced under the simple conditions here described, have no con- centric structure ; a slight conformity to this structure being observed, when a bubble of air, or a vacant space, marks the point of commencing deposition. In other cases, a shell in its calcareous composition offers a preferred nucleus, and as it con- tributes its lime salt, a concentric arrangement may be noticed in the forms resulting, especially after exposing them to heat. Rounded masses once formed become centres, or nuclei of second- ary occurring aggregates, one central mass being surrounded by spheres attached ; but in all it is easy to read the influence of the tendency of carbonate of lime to crystallize, and the opposition of the finely-divided silt, causing the particles of both to assume forms without straight bounding lines, as the polarizing force of crystallization is ai'rested in all directions. It may be added that a great number of bodies present rounded forms de[)endent on a modification of this law of restrained crys- tallization, such as numerous iron ores, bog manganese, and even 136 the more compact forms, where infiltrated solution?, forming part of the material, existed at the moment of aggregation. Dj". Hayes made some remarks on the formation of macle crystals, the true theory of which he stated that he had many vears since illustrated by numerous specimens and examples. Starting from the point where Beudant left the subject resting on a supposition, it occurred to him that the law was quite within the scope of a chemical demonstration, which would place this and similar instances of crystallization among known scientific facts. Without entering minutely into the matter, we may take as an example a salt exerting a strong tendency to crystallize from a hot solution on cooling, — ordinary saltpetre. A solution of this salt, in a pure state, slowly cooled, affords solid, six-sided prisms, or the crystals become solid if allowed to rest in the fluid, and we observe nothing but the result of ordinary crystal- lization. If the process has been carefully watched, — and it is a most interesting and instructive exhibition, — it will be observed that the particles of solid, so soon as tliey become visible, are rectangular, and that they are polarized. Motion may cause similar poles to approach within the limits of repulsion, when the particle turns and brings its opposite pole in contact, the union taking place at a certain angle, and the frame-work thus laid out becomes closed in by successive layers of polarized particles, forming a regular, solid crystal of a hexagonal form. The same operation going on in a solution of the same salt, mixed with a solution of common salt, exhibits for some time the same pi'ocess of construction ; but it soon becomes apparent that a solid prismatic crystal will not form, and time does not change the condition of the solution. A frame-work, or skeleton crystal is built up as before, and possibly the interstices may be solidly filled, but there will appear a hexagonal cavity in the centre, representing a considerable part of the volume of the crystal. If we carefully seal this cavity and remove the crystal, we find the fluid contents to be a strong solution of common salt, and the inte- rior of the crystal has quite finished surfaces. The suggestion at once arises that the crystal, having used in its structure all the saltpetre within reach, has completed its form with a strong solution of common salt. To test the correctness of this supposi- 137 tion, we may substitute a solid body, choosing one wliicli from its fineness can be diffused uniformly, ami we shall find that a pure salt will, by its polarizing action on this suspended matter, fill its cai-ity quite closely, and make u[) its true solid crystal in part of clay, Prussian blue, or other bodies. Ranging through the ordinary salts, cooling from solutions, or the melted state, made crystals will be obtained almost constantly, while in all cases of slow evaporation and avoidance of those conditions favoring the production of macles, solid transparent crystals only foi-m. Em- ploying thus many thousands of pounds, or only a few grains of salt, the operation of this law o^ polarization extended to contigu- ous matter is seen, and in the experiments alluded to, it was shown that its modified and more complex action gave beautiful results. Skeleton crystals, such as sublimates, and snow-flakes, and frost- work may be assumed to be solid crystals, at the instant of their formation : the vapor, or air, being polarized to fill the vacancies, which afterwards appear, gives the beauty and variety so strik- ingly presented by them. Mr. Charles Stodder stated that Professor Hitchcock, in his " Final Report on the Geology of Massachusetts," 1841, devotes several pages to the subject of claystones. He says : " They are undoubtedly concretions, formed by laws somewhat analogous to those of crystallization. I freely confess, however, that so far as my means of information extend, the subject of concretions is involved in great obscurity." — Report, p. 40G. " When broken, the concretion appears compact and perfectly homogeneous through- out, hi no case have I discovered a concentric or oolitic struc- ture ; nor did the application of strong heat develop it." p. 409. " In a very few cases I have met with a pebble, or a congeries of coarse sand, near the centre of the claystone, which appeared to have been the nucleus around which the particles collected ; but in ninety-nine cases out of a hundred, no such nucleus can be discovered ; although it is undoubtedly true, that there must have been something to determine the particles to a particular centre." p. 410. Since Professor Hitchcock's Report, Mr. Stodder was not aware that any observations had been made throwing any light on the origin or structure of these concretions. He exhibited two speci- mens, cut open, — one. No. 1014 of the State collection from Am- 138 herst, was, as Prof. H. found tliem, compact atul perfectly homo- geneous, and no nucleus was visible. The other, a very fine example of these claystones, from an unknown locality, was a de- pressed spheroid, almost a perfect circle in outline, presenting the markings which gave it the appearance of having been turned in a lathe, with an appendage on one side, apparently another spheroid attached to the principal one. On cutting this open and polishing the cut surface, it displayed a concentric structure with slight variations in color. There was no lamination ; the whole mass being perfectly compact, and the lines of colors not sharply defined, but fading almost impercepti- bly one into the other ; but the contrast of colors was sufficient, in a favorable light, to exhibit unmistakably the concentric ar- rano-ement of the material and the origin of ihe lines on the surface which give these concretions so much the appearance of works of art. There is a minute nucleus less than -J^ of an inch in diameter. The first concentric layer exhibits its arrangement about the nucleus in the form of an ellipse, assuming the spheroi- dal form at the outset ; the succeeding layers extend the long diameter more than they do the short one ; then a layer extends over the long diameter and one side only of the short ; on the other side of the now lenticular body, the layer terminates before reaching the centre, and its edge makes one of the lines, that so much resemble the marks of the turner's tool. Other layers are added to the long diameter, only increasing the compression of the spheroid, their edges making each a line on both sides. The lines of color in the appendage before referred to are concentric with the centre of the concretion, showing that that was not formed around an independent nucleus as might be supposed by the external appearance. The minute size of the nucleus, and its position outside of the centre, render it very difficult to be found without great care, and very liable to be destroyed by cutting or breaking the stone. No failure to find a nucleus is sufficient evidence that the concre- tion was formed without it. Mr. Stodder also called attention to another form of clay concretion or segregation, which he saw some years since in Windsor, Ct. 139 On the bank of the Farmhigton Tlivcr, was a bold, nearly per- pendicular bluft'of the Connecticut valley clay, stratified in hori- zontal layers of from half an inch to an inch, and perhaps two inches in thickness. The divisional planes between the strata were indurated, perhaps ^\ of an inch thick, and somewhat harder than the mass of the clay. Exposed to the elements the softer clay had been washed out between the hardened divisional planes, to the depth of one or two inches. Extending from one hardened plane to another, were cylindrical concretions of from ^ to f of an inch in diameter, at various distances apart. Tlie bluff, seen in front, presented the appearance of small shelves sup- ported by innumerable small columns, many of which had a small hole through the centre. They looked as if they might have collected about the rootlets of plants, but it is questionable whether roots would penetrate clay to the depth of ten or fifteen feet, or tlieir direction would always be vertical. The columns undoubtedly were not lime and clay like the clay- stones, but merely indurated clay, as none of them could be found at the base of the bluff, the follen ones having decomposed. Dr. Jackson referred to the Fossil from Lake Superior, which accompanied the collection of minerals presented by Dr. Kneeland at the last meeting, and which it was suggested by Mr. Stodder, might assist in determining the age of the copper-bearing rocks of that region. Dr. Jackson stated that the fossil was a Cyathophyllum, and undoubtedly came in the drift from the upper Silurian Rocks of the northern shore of the lake. Dr. Jackson exhibited specimens of Aluminium, consist- ing of a table-fork made of the metal, some wire, foil, and an ingot. Aluminium is now obtained in France at the cost of nine dollars a pound, and Dr. J. has been informed by a manufacturing chemist that it will soon .be pro- duced at the cost of only four dollars a pound in this country. The Corresponding Secretary read the following let- ters, viz : from the Regents of the University of New 140 York, January 15, 1857; the Royal Institution, Novem- ber 26, 1856, acknowledging the receipt of the Proceed- ings of the Society; from the Societe Imperiale d' Agri- culture, &c., de Lyon, July 9, 1856, the Societe Lin- n^ene de Lyon, July 9, 1856, the Academic Imperiale &c., de Lyon, July 14, 1856, the Acadejnie Royale des Sciences de Stockholm, August 1, 1856, presenting their various publications ; from Dr. John S. Newberry, Washington, Dec. 22, 1856, acknowledging -the receipt of his diploma as Corresponding Member; from Robert Kennicott, Esq., West Northfield, Illinois, January 15, 1857, acknowledging the donation of the Journal ; from Isaac Lea, Philadelphia, January 2, 1857, and M. L. A- Huguet Latour, Montreal, Jan. 3, 1857, requesting that missing numbers of the Proceedings may be sent to them ; from William Stimpson, Washington, Jan. 2d, 26th, and 29th, concerning his papers on the Crustacea of Califor- nia ; froni Charles Girard, New York, Jan. 19, con- cerning his descriptions of new California fishes : from Charles Whittlesey, Cleveland, Ohio, Jan. 25, accom- panying a geological paper, Mr. Leander Wetherell was elected a Resident Mem- ber. February 18, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. Prof..H. D. Rogers read the following paper entitled, — CLASSIFICATION OF THE METAMORPHIC STRATA OF THE AT- LANTIC SLOPE OF THE MIDDLE AND SOUTHERN STATES. The following is a concise sketch of the Geological composi- tion of the Atlantic Slope of the Middle and Southern States, 141 derived chiefly from a study of the formations of this portion of Pennsylvania. Discarding from our present survey tlie newer deposits of the region, or those long, narrow, superficial troughs of unconform- ably overlying red and gray shales and sandstones of mesozoic, or middle secondary age, which partially cover the older or crystalline, and semi-crystalline strata, and restricting our atten- tion to these, we shall find, — that when carefully studied, they rank themselves, so far as they admit of subdivision at all, into three natural physical groups. All the sedimentary mineral masses, without exception, are in a condition, more or less, of metaraorphism or transformation from the earthy to the crystal- line state by heat, and therefore using the term in a critical sense, all of them are Metamorphic Rocks. In the more current con- ventional application of this word, only some of them, however, pertain to the usually recognized Metamorphic or Gneissic series ; others belong unequivocally to the Paleozoic, or ancient life-rep- resenting system, while others again constitute an extensive, intermediate group, not typically gneissic or granitoid in their degree of crystalline structure or metamorphism on the one hand, nor yet fossiliferous on the other, at least so far as the closest scrutiny can discover. For a long while, indeed, from the commencement of geological researches in this district of the Atlantic slope, until the geological surveys of Pennsylvania and Virginia had unravelled the composition and structure of the region, all of these ancient, and more or less altered strata of the Atlantic slope, from its summit in the Blue Ridge and South Mountain, to its base at the margin of tide water, were regarded and designated alike as primary rocks, and were supposed to constitute but one group, and that the oldest known to geologists. Early, however, in the course of those surveys, it came to light that by tar the larger portion of the rocky masses of at least the middle and northwestern tracts of the Atlantic slope, including much of the Blue Ridge and of the Green Mountains, was of a different type and age from the oldest metamorphic, or true gneissic system. The evidence in support of this conclusion was, first, an obvious and verj^ general difference in the composition of llie two sets of strata; secondly, a marked difference in their conditions of metamorphism, and thirdly and more especially, a 142 striking contrast in their directions and manner of uplift, the pli- cations and undulations of the less metamorphic series, dipping almost invariably southeastward, while the gneiss presents in many localities, no symmetrical foldings, but only a broad out- crop, dipping to a different quarter. These structural dissimili- tudes imply essential differences in the direction and date of the crust movements, lifting and transforming the respective groups, and led the geologists of Pennsylvania and Virginia to a convic- tion, that over at. least many tracts, a physical unconformity, both in strike and dip, would be yet discovered. It was not, however, till a relatively late date in the prosecution of the geological sur- vey of Pennsylvania, that the geologists of that State detected there positive evidences of this physical break, and interval in time between the two groups of strata, and established by ocular proof the correctness of the previous induction. This unconform- ity, reflecting so much light on the whole geology of the Atlantic slope, was first clearly discerned in tracing the common boundary of the two formations from the Schuylkill to the Brandy wine, and the Susquehanna, but it was quickly afterwards recognized on the borders of the gneissic district, north of the Chester County limestone valley, and again, soon after, in the Lehigh Hills at their intersection with the Delaware. Prior to the suspension of the geological survey from 1843 to 1851, the true Paleozoic Age of the non-fossiliferous crystaUine marbles, and semi-crystalline talcoid slates, and vitreous sand- stones of the Chester and Montgomery Valley, had been clearly demonstrated by the State geologist, through a comparison of the strata with their corresponding formations in a less altered con- dition further north ; but it was not until the resumption of field research, upon the revival of the survey in 1851, that any dis- tinctive fossils were detected in these greatly changed rocks, ■which even in their original state seem to have been almost des- titute of their usual organic remains. Assembling all the evidence which we now possess, we have in the Atlantic slope by actual demonstration but one physical break or horizon of unconfoi'mity throughout the whole immense succession of altered crystalline, sedimentary strata, and within this region but one paleontological horizon, that, namely, of the already-discovered dawn of life among the American strata. 143 This latter plane or limit, marking the transition from the non- fossiliferous or azoic deposits to those containing organic remains, lies within the middle of the primal series or group, of the Penn- sylvania Survey, that is to say, in the Primal White Sandstone, Avhich even where very vitreous, and abounding in crystalline mineral segregations, contains its distinctive fossiL the ScolitJais linearis. The primal slates beneath the sandstone, and in im- mediate alternation with it, possess not a vestige of organic life, nor has any such been yet discovered anywhere within the limits of the Atlantic slope, or on the northern or western borders of the great Appalachian basin of North America, either in this lower primal slate, or in the other semi-metamorphic grits and schists physically conformable with it, and into which the true Paleozoic sequence of our formations physically extends down- ward. We have thus, then, two main horizons, subdividing the more or less metaraorphic strata of the Atlantic slope into three systems or groups ; the one, a physical break or interruption in the original deposition of the masses; the other, a life-limit or plane, denoting the first advent, so far as is yet discovered, of organic beings. As these two planes are not coincident, but include between them a thick group of sedimentary rocks, sepa- rated from the lower physically, from the upper ontologically, w^e are fully authorized, in the existing state of research, to employ a classification, which recognizes a threefold division of all these lower rocks. To the most ancient or lowest group, it is proposed to continue the name of gneiss, preferring, however, to call this division generically the Gneissic Series, em[)loyinr>- sometimes the technical synonyme Hypozoic, proposed by Profes- sor John Phillips, for these lowest of the metainorphic strata. To the great middle group, less crystalline than the gneissic, and yet destitute of fossils, the descriptive terms semi-metamorphic or Azoic are applicable. And to the third uppermost system, or entire succession of the American Appalachian strata from the primal, containing the earliest traces of life, to the latest true coal rocks, or last deposits of the Appalachian sea, it is here pro- posed to affix^ as for many years past, the well-chosen title, con- ferred on corresponding formations in Europe, of the Paleozoic, or ancient life-entombing system or series. Thus we have the Hypozoic rocks, or those underneath any life-bearing strata ; 144 Jzoic, or those destitute of any discovered relics of life ; and Paleozoic, or those entombing the remains of the earth's most ancient extinct forms of once living beings. The Atlantic slope of Pennsylvania includes all these three systems of strata. Where the azoic strata display their maxi- mum amount of crystalline structure or metamorphism, they often simulate the true ancient hypozoic or gneissic rocks so closely, and they are indeed so identical with them in mineral aspect and structure, that the observer is baffled in his attempts to distin- guish the two groups lithologically ; nevertheless, it clearly ap- pears, as the sections illustrating this country prove, that they are distinct systems, occupying separate zones, susceptible of inde- pendent definition on the geological map. At the time of the first construction of the general geological map of the State, the true limits separating the hypozoic or gneissic from the azoic or semi-metamorphic rocks were but vaguely understood, and the State geologist did not venture to define them on the map, but shaded the one system into the other, indicating, however, what he has since proved, that the true gneissic rocks, in their southwestward course, pass out of the State at the Susquehanna, only a short distance north of its southern boundary, while the azoic, or talco-micaceous group, as a genuine, downward extension of the primal, paleozoic series, widens progressively going westward, until, from a very narrow outcrop at the River Schuylkill, it occupies at the Susquehanna the whole broad zone south of the limestone valleys of the Conestoga and Codorus streams in Lancaster and York counties. Since the revival of the field work of the survey, the dividing limit of these two sets of metaraorphic strata has been traced and mapped with precision. To the southwest of the Susquehanna it has never, it is believed, been pursued through Maryland and the other southern States, though one may readily discern it in going north- Avard or westward from Baltimore, or ascending the Atlantic slope in Virginia. In Maryland it crosses the Baltimore and Susquehanna Railroad about twelve miles north of Baltimore, and it is intersected by the Baltimore and Ohio raih-oad a little east of Sykesville ; it crosses the Potomac above Georgetown, and the James River in Virginia, west of Richmond. The line of bound- ary is, however, not a simple one, but is intricately looped, in 145 consequence of numerous nearly parallel anticlinal foldings of the strata, sending promontories or fingers of the older rocks, within the area of the newer or semi-metamorphic, to the west of their average boundary, and causing, of course, corresponding troughs, or synclinal folds of the newer, to enter eastward of the average boundary, the general area of the older. The Atlantic slope has received hitherto so little exact geological study, that we are, as yet, without the data for determining with any precision, either the succession of its much broken and closely- plicated strata, or the geographical limits which separate even the larger sub-groups. It is sufficient, however, for our present purpose, to show the existence and the approximate range of two great metamorphic systems, separated by a physical break ; and the conformable relations of the later or upper of these to well known lower paleozoic formations of the Appalachian chain. Mr. T. T. Bouve said he was incredulous as to the matter of slates being so altered as to be mistaken for gneiss or altered into true gneiss ; he questioned whether gneiss ever were a deposited rock. Dr. C. T. Jackson made some remarks dissenting from Prof. Rogers upon certain points in the metamorphic theory, and adduced some observations upon the slates of Pequauket Mountain, in New Hampshire, in support of his views. Prof. Wm. B. Rogers supported the theory of Prof. H. D. Rogers. Dr. T. M. Brewer read the following LIST AND DESCRIPTIONS OF EGGS OBTAINED IN CALIFORNIA BY E. SAMUELS. Buteo montanus, Nuttall. The Western Red-tailed Hawk or White-throated Buzzard. This bird was first recognized as a distinct species by Mr. Nuttall, (Manual, 1840.) Its claims to this distinction have remained unrecognized until very recently. In the Proceedings of the Philadelphia Academy, Feb. 1856, PROCEEDINGS B. S. N. H. — VOL. VI. 10 APRIL, 1857. 146 Mr. Cassin, for the first time, refers to this hawk as a distinct species from the variety found in the eastern States. ( B. bcrealis.) Two eggs belonging to a bird of this species were obtained by Mr. Samuels near Petahnna, California, in 1856, one of which measures 2j^^ inches in length, by \\^ inches in its greatest breadth. The shape of the egg is an almost exact ovoid, slightly tending to a spheroid, one end being hardly perceptibly larger than the other. Its grovind color is a very light buff, the spottings and markings giving to it the effect of a yellowish-white. The egg is marked over the entire surface with blotches, dashes, and lines of a light tint of a brown tending to Vandyke. These are mixed with markings of a lighter purplish-brown. The mark- ings, of both shades, are chiefly oblong in shape, and run with the length of the egg. They bear no i-esemblance to any eggs of the B. horealis that I have ever seen, and are also quite unlike those of any other hawk, so far as I am aware. The nest was discovered by Mr. Samuels, not far from Peta- luraa, California, close to the Mission House, near Petaluma Flat. It was built on the top of a large evergreen oak, at least seventy feet from the ground, and was constructed entirely of large, coarse sticks, lined with a iew stray feathers. The eggs were two in number, and had been set upon a short time. The male bird was shot as it flew from the nest, which was so hidden by the thick branches that it would have escaped detection. Buteo calurus, Cassin. Black Red-tail Hawk. This hawk is comparatively a new species, having been met with for the first time by T. Charlton Henry, M. D., U. S. Army, in the vicinity of Fort Webster, New Mexico, and described by Mr. Cassin in the Proceedings of the Academy of Natural Sciences, Philadel- phia, February, 1855, p. 277. The specimen obtained by Mr. Samuels, with the egg, is the second that has been discovered at the j)resent time, so far as I am aware. In regard to its habits and specific peculiarities but little is known, and its geographical distribution can only be conjectured from the two points, about a thousand miles apart, where the two representatives of this spe- cies were obtained, — Fort Webster and Petaluma. The nest was found by Mr. Samuels on a hill north of Peta- luma, California. It was built near the top of an evergreen oak, 147 at the height of about sixty feet from the ground. The nest con- tained two eggs at the time it was discovered, which were just on the point of hatching. It was constructed of sticks, and was lined with moss. Both birds were about the spot. The male bird manifesting much more courage than his mate in resistance to the intruders, was shot. The female was wounded, but escaped. The egg of the B. calurus measures 2^-^ inches in length by ly\- in breadth. Its capacity is considerably less than that of the B. montanus ; its shape is a much more oblong oval ; one end is evidently more pointed than the other. Its ground color is a dirty cream-white. It is covered, chietly at the larger end, with blotches and smaller markings of a dark shade of a brown almost exactly corresponding with that known as Vandyke- brown, with smaller markings and spottings of a lighter shade of the same. The latter are distributed at intervals over its entire surface. Buteo insignatiis ? The Canada Buzzard or Brown Buzzard. In the collection of eggs obtained in California by Mr. Samuels, were two eggs of a hawk which he had no doubt belonged to a bird of this species. The parent was shot on the nest, but escaped into a deep ravine below, and was not obtained. The egg is different from that of any other hawk that I am acquainted with, and it has been assigned to this bird, on the strength of Mr. Samuels's impressions. It should be added, however, that his view of the bird was necessarily incomplete, and he may have been mistaken in regard to it. It is possibly the egg of Buteo Bah-dii, (a variety of -B. Sivainsoni,) or it may belong to the B.elegans, all of which bear sufficient resemblance to the B. insignatus to be confounded with it, without an opportunity of closer inspection than he pos- sessed. The nest was on a large white-oak, over a deep ravine, on San Antonio Creek, near Petaluma. It was very large, was constructed of coarse sticks, and was at least sixty feet from the ground. In regard to the habits and the geographical distribution of this hawk, but little is known to naturalists. It was first de- scribed from a specimen belonging to the Natural History Society of Montreal, and obtained in that vicinity. Specimens have since been met with in California ; but to what extent it is distributed 148 through the intervening country remains to be ascertained. It is not improbable that it is a more common species on the Pacific coast, and that it is of rare and accidental occurrence in the east- ern part of the continent. Dr. lieermann has ascertained that this hawk rears its young in California, where he met with both adult and young specimens. The egg supposed to be that of this hawk, measures 2y*^ inches in length by ly*^ in breadth. Its shape is an oblong oval, and neither end is perceptibly larger than the other. The ground color of the egg is a cream- white, but little obscured by markings or secondary colors. The egg is marked, chiefly at one end, with lines, dottings, and small blotches of a light reddish-brown. The lines with which one end of the egg is sparingly marbled are much darker, and are more nearly of a Vandyke-brown. The greater portion of the egg, especially that which corresponds with the smaller end, is free from any markings. This has no close resemblance to the egg of any other American hawk that I have ever met with, but most nearly approaches that of the Rough- legged Falcon from Labrador. Hirundo bicolor. White-bellied Swallow. Hirundo lunifrons. Republican or Cliff-Swallow. Mellisuga anna. Anna Humming-Bird. Two nests with the eggs of this bird were obtained by Mr. Samuels. They are not new, bat are probably to be found in few collections. The nest and eggs procured by Mr. S. correspond substantially with the descriptions and measurements given by Mr. Nuttall and quoted by Mr. Audubon. (Birds of America, Vol. X. p. 188.) Tyrannus verticalis. Arkansas Flycatcher. Scolecophacfus Mexicanus. Brewer's Blackbird, Audubon. This bird was first met with in the territory of the United States by Mr. Audubon, who found it in the country about Fort Union, near the confluence of the Yellow Stone and the Missouri. He called it, supposing it to be undescribed, Quiscalus Brewerii. It had, however, been previously given by Mr. Swainson as Mexicanus. Mr. Samuels was so fortunate as to meet with seve- ral of the nests, with the eggs of this bird. The egg measures 149 lj\ inches in length by J-| of an inch in breadth. It is an oblong oval, but pliglitly pointed at the smaller end, and, except in size, bears some resemblance to the egg of the common Song Spar- row, ( Zonoti'ichia melodia.) Its ground color is a greenish-white, over which are diffused, in most of the specimens, numerous blotches and markings of a ferruginous brown. The nests were in low bushes in wet places, and did not essentially vary from those constructed by the Red-winged Blackbird. Agelaius (juhernator. Crimson-winged Blackbird. The nests and eggs obtained by Mr. Samuels correspond with the descrip- tion given by Dr. A. L. Heermann in the Journal of the Phila- delpliia Academy. Cyanocorax Cah'fornicus. California Jay. This is probably the same bird given by Mr. Audubon as the Ultramarine Jay, Garrulus sordidus, of Swainson, and G. idtramarinus, of Bona- parte. Its eggs have been described by Dr. Ileerman StunieUa neglecta. Missouri Meadow Lark. Zonotrichia grammaca. Lark Bunting. Carpodaciis familiaris. California Purple Finch. Melanevpes formicivorus. California Woodpecker. Ectopistes GaroUneiisis. Carolina Turtle-Dove. Gallipepla Califormca. California Quail. The Secretary read the following communication from Dr. James Lewis, of Mohawk, N. Y., addressed to the Corresponding Secretary : I received yesterday the fourth sheet of Vol. VI. of the Pro- ceedings of the Boston Society of Natural History, in which I find some remarks by Dr. Weinland relative to the causes of erosions on fresh-water shells. This subject has atti'acted my attention to a considerable extent, and I am glad there are others who are similarly interested. 150 Although T assent to the propositions of Dr. Weinland as being sufficient to explain the subject in some instances, I have not regarded the presence of small worms on shells, nor the presence of carbonic acid in water, as sufficient to account for the great diversity of appearances presented by the same species in diffi^r- ent localities. From what information I have been able to obtain in relation to the geological characters of various regions in which shells are found, it appears that those bodies of Avater having large quan- tities of calcareous salts in solution produce shells very little liable to erosion ; while on the contrary, where there is very little lime, and the water holds in solution considerable quantities of saline alkalis and ferruginous salts, the shells are very liable to be eroded. Among the numerous specimens that I have, illustrating the above, are large numbers of shells from streams in Georgia, where the waters abound in saline alkalis. The shells are very generally eroded. I have also shells from other regions where the saliue alkalis are more abundant than lime, and they present the same character. I have also shells from Ohio, Illinois, Wisconsin, &c., which are from streams abounding in lime, and an eroded specimen is seldom to be seen among them, except, perhaps, a few aged shells that are evidently worn by long contact with abrading surfaces of other bodies, I have also shells from a lake in Herkimer county, N. Y., nearly all of which have perfect beaks, and the few that are eroded are by no means as chalky in their texture as some specimens I have seen from localities deficient in lime. The bottom of the lake, in the instance specified, is a bed of marl. But a more satisfactory proof that the freedom of shells from erosion depends on the relative proportions of various salts or alkalis in solution in the water, is presented in a limited body of water under my own immediate inspection. Near the village of Mohawk, is a slowly-moving body of water, in which considerable numbers of shells are found. In those por- tions of this body of water where the various salts bear their natural and proper relation to each other, the shells are very perfect, and generally very free from erosions. But at and be- low, where the refuse ashes from an ashery are drained or leached 151 into this body of water after every shower, a considei-able quan- tity of saline alkalis finds its way into the water, where, in con- sequence of its specific gravity, it falls to the bottom, and every shell within reach of the influence of this alkaline matter, is more or less eroded, and most of them very much so. But further down, the shells grow more perfect, probably in consequence of the dilution of the alkalis, and their more general diffusion in the whole body of the water, by the influence of the slight current in it. It may be thought strange that the presence of saline alkalis in water is urged as a cause of the erosion of shells, but it may be explained in this way. Wliere two or more alkalis are present in the food of an animal, and only one of them is necessary and proper to enable it to perform its healthy functions, the others may, in part, take the place of the proper substance, and if so, the shell formed under such circumstances w-ould be more or less liable to erosion, in proportion to the solubility of the substituted materials. We have now only to inquire respecting a locality producing eroded shells, — Is the water so highly charged with lime, that the presence of a more soluble alkali in small quantity can have no material influence in the formation of the shells ? If the answer be yes, then we may reasonably ascribe the eroded character of the shells of such a locality entirely to minute parasites ; but if there be a preponderance of saline alkalis in the water, they may be reasonably expected to enter into the organization of the shells, and a very slight abrasion of the epidermis of the shell from any cause, would expose the soluble alkalis to the solvent action ot water alone, and the remaining portion of the shell becoming less dense (and '"chalky") by a removal.pf a portion of its substance, would, of course, wear away very rapidly. It is easy to understand why the beaks of bivalves, and the apices of univalves are first attacked by the erosive process. Firstly, the epidermis is thin- ner at those points : secondly, those portions of the shell formed in early life may be presumed to contain more gelatinous, and less calcareous matter, than the parts formed at or near maturity. I do not know demonstratively that this is the case, but analogy teaches it. 152 Dr. Gould observed, that shells in limestone waters are less liable to erosion, not from any difference in their composition, but simply because there is less tendency in such waters to abstract lime from the shell. Prof. William B. Rogers suggested, that an analysis of shells from various waters should be made, to deter- mine any difference in their chemical composition. The Secretary read a letter from Dr. Samuel Kneeland on a supposed new species of Siredon from Lake Supe- rior. The following account was subsequently received : Siredon hyemalis, Kneeland. From 9 to 10 inches long ; color on back olive-green, with a few small blackish spots, arranged for the most part in longitudinal rows, and with a few smaller spots varying in color from bright to rufous-yellow. A line, more dis- tinct towards the tail, separating the olive-color of the back from the sides, which are of a purplish-brown, with more numerous yel- lowish spots sometimes coalescing into patches half an inch long and two lines broad; brightest on sides of head and tail. Under sur- face of body of an asby-brow^n color, with a more or less distinct median white line, or linea alba ; the yellow spots occur on the under surface of the jaw. From the nostrils, Avhich are situated at the extreme corner of the truncated muzzle, about half an inch wide, there I'uns a dark line through the centre of the eye back to near the external gills; upper and lower segment of the iris of a yellowish silvery color. Tail flattened laterally, ter- minating in a rounded thin edge, more mottled than any other part of the body. Gills, three in number on each side, exter- nal, provided with an immense number of exceedingly delicate fringes, of a deep red color when the animal is breathing ac- tively ; these gills are kept waving to and fro in a most grace- ful manner during active respiration ; when at rest they are shrunken, still, and colorless. Just behind these gills are the anterior extremities, about an inch in length, provided with four fingers, mottled like the sides of the body; under suifnce of the wrist and hand whitish, almost translucent, with the finger-tips black. About five inches further back are the posterior extrera- 153 ities, in size, color, and number of toes, like the anterior limbs. About three fourths of an inch behind the posterior limbs, is the vent, of a bright orange-red color, in some specimens surrounded with fringe-like projections. General shape and aspect of the head, snaky ; some specimens, between the eyes and gills are much broader than others ; average greatest width, just anterior the gills, 1^ inch, — slight constriction in region of gills, — behind the last the body is cylindrical and eel-like, about an inch in diameter, gradually tapering towards the tail. The mouth is provided with sharp conical teeth, and the palatine roof is studded with them. Besides the motions of the gills, the animals suck in water which passes out by the narrow openings at the base of the gills. I liave kept several of the animals for months, giving them nothing whatever to eat except what they got from the lake water, which I changed every day or two. The water of Por- tage Lake is very full of vegetable, and, probably, animalcular impurities, on which, doubtless, the creatures fed ; but their teeth indicate more substantial food than this. They have been kept for months in clear spring water, so that the preservation of life is probably due rather to the tenacity of the vital principle in reptiles, than to any thing they find to eat in the water. The animals in my possession, have been frozen under ice half an inch thick, every night for three months, without any apparent diminution of their activity; though the water around them was not entirely frozen. 1 kept one an hour out of the water, during which time it became quite sluggish, occasionally opening its mouth spasmodically, as if to swallow water or air ; at the end of the hour, on replacing it in the water, it soon regained its activ- ity. Removing one entirely from the water, all motions of life had ceased at the end of four hours. Their motions in the water are very lively, and performed by the motions of the body and tail ; they now and then come to the surface to take in or force out a globule of air ; the last they often do under water. Their feet serve them for a slow and difficult locomotion on the bottom ; when they move quickly in a jar their limbs are stretched at right angles, as if to steady the body ; perhaps in a larger space they would be applied close to the body. These animals are rarely if ever seen, except during the win- ter; those I obtained were sucked up through the pumps for the 154 supply of the water for the copper stumps ; they are never thus caught in the summer or autumn. They change their skin at this season ; I have had several with the old skin hanging to the new in shreds and patches, which are washed off by the water in two or three days, leaving the colors of the new skin very bright ; the edges of the tail are then so thin and transparent that the network of bloodvessels can be seen with the naked eye. The reason why they approach the shore at this season may be on account of this change in the skin, and possibly for breeding pur- poses. About once a week they pass from the anus a gelatinous mass, about the size of a pea, of a whitish color. I thought this might be possibly an egg, but the envelop soon becomes soft in the water, and its contents are lengthened out into a somewhat convoluted form. If this should not have been described, I would propose for it the name of Siredon hyemalis. The Secretary read a communication from Mr. Robert Kennicott, of Chicago, informing the society that he had several living specimens of the Great-tailed Fox-Squirrel, [Scivrus magnicavdatus, Harlan,) which he held at the disposal of the Society or its members. Mr. Kennicott also announced the organization of the Chicago Academy of Natural Sciences. President, Prof. J. V. Z. Blaney. Dr. T. M. Brewer announced the organization of the California Society of Natural History, at Stockton. President, R. K. Reid ; and presented its circular, which w^as referred to the Council. Messrs. James R. GatlifF, of Buenos Ayres, and Rus- sell Loring, of Valparaiso, were elected Corresponding members. Messrs. Edward S. Rand, Jr., and John P. Robinson, were elected Resident members. 155 March 4, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. Mr. Amos Binney presented, in the name of his brother, a Monograph on the group of American Helices repre- sented by H. fuliginosa. Referred to the Publishing Committee. Mr. Amos Binney also presented, in the name of his brother, the following paper : DESCRIPTIONS OF TWO SUPPOSED NEW SPECIES OF AMERICAN LAND SHELLS, BY WM. G. BINNEY. 1. SUCCINEA LINEATA. Testa oblongo-ovata, solidior, albida aut cinerea; spira elevata, acuta ; anfractus 3 convex!, lineis parallelis inter rugas incre- mentales volventibus ornati ; sutura impressa ; apertura orbiculata- ovata, oviformis, partem testae dimidiam tequans ; columella pli- cata, callo albo induta. DESCRIPTION. Animal not observed. Shell oblong-ovate, with three very convex whorls ; spire ele- vated, acute ; surface marked with irregular wrinkles of growth, between which are coarse parallel revolving lines, somewhat removed from each other. Aperture large, about as long as one half of the whole length of the shell, egg-shaped ; columella folded; a deposition of callus on the parietal wall of the aperture. Greatest diameter, 6 ; alt. 12 millimetres. Geographical Distribution. Collected in considerable quantity by Dr. F. V. Hayden,on high hills near Fort Union. Jiemarks. The specimens collected being dead and eroded, it is impossible to say what is the color of the shell when fresh. It is probably ashy white, I'esembhng the true S. campestris of the Southern States. The revolving lines which distinguish it at 156 once from every other described American species, are more apparent on the middle of the body whorL These are quite coarse, and placed at irregular intervals; — on some specimens scarcely discernible. The aperture is unlike that of any other of our species ; being correctly egg-shaped, — it is nearest in form to that of S. campestris, but is less expanded. The parietal wall of the aperture is unusually horizontal. In general aspect it resembles somewhat S. vermeta, but is distinguished from that shell by its more oval shape, and the greater convexity of the whorls. It is the heaviest American species. HELIX INTERCISA. Testa solidissiraa, luteo-cinerea, apice rufa, globoso-eonica ; spira brevis ; sutura impressa ; anfractus quinque, convexiusculi, lineis parallelis volvenlibus, valde demissis, strias incrementales distinctas intercidentibus notati ; anfr. ultimus globosus, supra peripheriam fascia union, rufa obscurissima ornatus ; apertura maxime obliqua, forma equi calcei, rotundata; labrum albo-cine- reum, incrassatum, subtus reflexiusculum, subunidentatum, umbil- icum totum tegens ; marginibus approximati:^', callo interjunctis. SYNOXYMS AND IlEFEREXCES. Helix Nlckliniana. Lea. var. Binney Terrestrial Molhisks, II. p. 120, III. pi. VI. f. 1. Ico7i in medio posita. DESCRIPTIOX. Animal wot observed. Sliell globose-conic, with five slightly-rounded whorls ; spire little elevated ; suture distinct ; upon the body whorl a dark revolving band, hardly discernible ; aperture very oblique, shape of a horseshoe ; peristome thickened, heavy, dirty white, slightly reflected at the umbilicus, which it entirely conceals near its junction with the columella, furnished with a tooth-like process, the extremities connected by a heavy ash-colored callus, which is spread more lightly over the whole parietal wall ; epidermis grayish yellow, apex rufous. The striae of growth are very numerous and distinct, crossed by numerous, regular, revolving lines, so deeply impressed as to entirely separate them into small sections ; thus the whole surface of the shell is divided into minute, 157 raised parallelograms, separated by the deep longitudinal and horizontal furrows. Greatest diameter, 22; less, 19 ; alt. 15 millimetres. Geographical Distribution. Found in Oregon Territory. Remarks. This shell I found in the collection of my father, Dr. Amos Binney. It was labelled H. Nickliniana, Lea. var., and as such is figured in the terrestrial moUusks. I cannot believe, however, that any species can admit of varieties differing so much as this does from NicMiniana. To Mr. Lea's figure and descrip- tion it bears no resemblance whatever, either in shape or sculp- turing. It may readily be distinguished among the Helices of the Pa- cific coast, by its grayish, heavy shell, its thickened lip, and above all, by the peculiar markings of the surface. Dr. A. A. Hayes exhibited a specimen of rock guano, from a lately-discovered deposit on an island not far dis- tant from the main land in the Atlantic Ocean. Dr. Hayes called attention to this substance chiefly, as an illus- tration offered of the solution and subsequent deposition of phos- phate of lime from decomposing bones. Eeferring to a paper which he lately read here, in explanation of the chemical action, he showed that the solution of bibasic phosphate, eliminated from tribasic phosphate of lime, had penetrated into and cemented not only the phosphate of comminuted bones, but had united a mass of bivalve shells ; in some cases actually i*emoving the excess of carbonate of lime, leaving a partly bibasic phosphate behind. He had examined a number of cases of this transference, and found sand and gravel aggregated by the phosphate which had been removed from bone-phosphate, through the agency of cai'- bonic and crcnic acids, formed in the humid decomposition of the animal matter present in the bird droppings, — so as to form a compound rock. The facts already observed prove that mineral masses contain- ing phosphate of lime, may be thus formed from animal phosphate of lime, and present all the characters which we recognize in the phosphate of lime engaged in the oldest slates. Additional inter- est has been given to this subject, by communications from Prof. 158 Booth of Philadelphia, and Dr. S. L. Snowden Piggott of Balti- more, who have analyzed specimens, in which the phosphoric acid had combined with both oxide of iron and alumina. Dr. Hayes stated that the economical value of this substance is great, as a mineral fertilizer, it dilFering in this respect from the common guano which derives its importance in agriculture from its organic elements. Dr. Hayes also gave an account of the formation of Monk's Island, with the probable changes that its surface had undergone. Dr. Bryant read the following communication on a supposed new species of Turkey recently described by Mr. Gould. In the January number of the Annals of Natural History, Mr. Gould describes a new species of turkey, from the mountains of Mexico. In the same article, he states that the domestic turkey did not originate from the common wild turkey, Meleagris gcdlo- pavo ; grounding this assertion principally on two facts, namely, the difference in the structure of the two birds, and their not readily breeding together. How far climate and other influences may have affected the domestic variety in England, I do not know, but with us neither of these statements is correct. If it were not for the difference of plumage it would be impossible in many cases to distinguish the two birds ; and even with this aid it is sometimes very difficult to decide with certainty when the specimen is a female. I can give no reason why the wild turkey should be unwilling to breed with the domestic variety in Eng- land, except that they are probably kept in confinement, to which even the domestic bird with us unwillingly submits. At any rate, this is not the case in the United States. The wild turkey breeds here with the tame variety quite as readily as could be expected ; whenever wild turkeys are numerous, it is an ordinary occurrence for the tame hen to prefer the wild gobbler to the domestic ones. I have had in my own possession wild hens that bred with a tame gobbler, a fact much stranger than that of the wild gobbler breeding with the tame hen. But the most satis- 159 factory proof of their specific identity is that the offspring of mixed blood is known to be both hardier and more prolific than the more domestic variety, — a fact which cannot be reconciled with the theory of specific difference. Dr. C. T. Jackson exhibited specimens of Aluminium and several of its most important alloys with other metals, and read a condensed resume of the various com- munications on the subject contained in the Comptcs Rendas of the French Academy of Sciences. The three most interesting alloys of aluminium are those with silver, copper, and zinc. "When five per cent, of aluminium is added to pure silver it increases the hardness of the metal and improves its quality for plate, since this alloy is capable of receiving a high polish, and is less liable to corrosion than the usual alloy of silver with copper. When ten per cent, of aluminium is fused with pure silver, a much harder alloy results, which is still quite malleable and takes a resplendent polish. This alloy also resists the action of sul- phide of hydrogen which at once blackens pure silver and its usual copper alloy. It is also well adapted, from its superior hardness and stiffness, for the manufacture of forks and knives, and plate made of it is less liable to be scratched and defaced by use. The effects of aluminium on copper are quite remarkable, and a very small proportion of aluminium is found to change the color of copper to that of gold, while the alloy is much softer and more ductile than pure copper. The whitening power of aluminium when alloyed with copper, is much greater than thaT possessed by zinc, and the alloys with aluminium are all malle- able both when hot and cold. A specimen of an alloy of one hundred parts by weight of cop- per and five parts by weight of aluminium was of the color of British gold coin, and was readily rolled out into sheets thin as letter paper, it working as easily as fine silver. It is stated in a communication published in the Gomptes Ren- das, that this alloy is not affected by sulphide of ammonium ; but tliis Dr. Jackson finds to be an error; for the moment a drop of 160 the sulphide is let fall on this alloy a deep red spot is produced, and this quickly changes to a perfect black stain. When larger proportions than 10 per cent, of aluminium are melted with copper, the alloys become hard, and ultimately, by increasing the proportion of aluminium, the alloy is made brittle. The alloy of 10 per cent, of aluminium and 90 of copper is malleable, ductile, and has a golden color, but it is not capable of withstanding the action of acids or of sulphide of ammonium. An alloy of 10 parts of aluminium and 90 of zinc is malleable, and takes a very brilliant polish with the lustre and color of highly-polished steel. Dr. Jackson remarked that we know, as yet, but little of the uses of aluminium and of its alloys, and that the introduction of the new metal, at moderate cost, into the workshops of our me- chanics and artisans, is likely to open a new field for enterprise in metallurgy. Numerous experiments are required, and larger quantities of the alloys should be made, so as to test their properties and value in a practical way, and the sacrifice of some hundreds of pounds of aluminium could well be afforded in view of the useful results that would be obtained by experiments with its numerous alloys. Were aluminium works erected in this country, it is prob- able that the first few years' production from them would be consumed in experiments by our practical artisans, or be sold for specimens to schools and colleges, or to private gentlemen. By manufacturing this metal on a large scale, the cost of its production can undoubtedly be made quite moderate. It is stated that it can now be made in Paris at a cost of nine dollars a pound. This is a considerable reduction from the former prices, for the speci- mens now before the Society cost one hundred and sixty doUai's per pound. The following paper was read at the meeting of Octo- ber 1st, 1856, by Dr. David Weinland. A PSYCHOLOGICAL VIEW OF THE MOTIONS OF ANIMALS, BY DR. DAVID "WEINLAND. There is hardly any part of the science of natural history which has been so little studied as the psychology of animals. 161 The ability to descend to the level of the mental constitution (ipvxv) of animals, to understand their feelings, thoughts, and desires, seems to have diminished in proportion to the progress of civilization ; or, at least, in proportion as cultivated minds of civilized nations have secluded themselves from free nature in cities and students' closets. Still, we think the psychology of animals is by no means the least interesting subject of human thought. It is acknowledged that man is the crowning work of creation, and this has been proved and illustrated often enough by comparison of the structure of his body with that of other ver- tebrates ; by showing that there exists an ideal series of develop- ment from the horizontally moving fish to the erect man. Now, may not this truth be as clearly, or more clearly traced, in fol- lowing out the degrees of development of the psychical element, from the low, feeding, and propagating fish, to man as made in the image of God — that is, thinking in the same categories with him. Undoubtedly such a series of psychical development exists, but its steps have never been marked out, though many materials have been collected in regard to the subject. In the effort to attain a method of studying this part of the science of nature, the following considerations have occurred to me. We know the condition of a man's soul, or of its representative in an animal, only by external manifestations. Thus, in order to have a standard of comparison for the difl^erent degrees of psy- chical development of animals, we may start from an analysis of what is called the characteristic of animals, in opposition to plants, namely, voluntary motion. In considering closely the motions of a dog, we recognize in them two entirely different kinds. One, and that by far the most common, serves only and immediately the animal itself as the means by which to obtain whatever it desires and enjoys, (food, for instance,) and to shun whatever it dislikes. This kind of motions we may call subjective ; that is, selfish motions ; be- cause they serve only the subject itself. But again, we see an- other kind of motions. Thus, the dog plays with other dogs, with other animals, and with man. It makes many movements with the head, eyes, ears, and tail, which serve no other purpose than to show to other animals, or to man, the present condition of its inner nature ; to show them what it feels, what it thinks, and what it PROCEEDINGS B. S.N. H. VOL. VI. 11 MAY, 1857. 162 seeks. These motions are not subjective ; they are made in re- lation to the inner natures of others, and therefore may be prop- erly called sympathetic motions. Which of these two kinds of motions is the higher? Undoubtedly the latter. All animals have the first ; the second are not common to all. Does an her- maphrodite worm, for instance, know that another being lives and feels ? If not, it has no sympathetic motions. Having considered how to view the motions of an animal, let us return to our problem, namely, to find a standard for the com- parison of the different degrees in which, in the series of animals, the mental constitution is developed ; and to show that the greater or less degree of development of the sympathetic motions in an animal, and of its organs to perform them, exhibits at the same time, the degree of its psychical development. That such is the case is because no degree of this development, beyond eating and drinking, can possibly exist, except in society with, and in regard to, fellow-beings. All those animals of higher mental organization, are social animals, or, at least, are connected by certain psychical relations, with other animals. Thus, among insects, the hymenoptera rank psychically very high. The greater part of them live in communities ; that is to say, each individual lives and cares not only for itself, but also for its fellow-citizens. It knows that it belongs to a certain community, has certain duties there, &c. ; and whenever we admire the sagacity of a bee or an ant, it is its working and thinking in relation to other beings that we admire. Moreover, only ani- mals which are social by their nature, can be domesticated ; that is, made friendly to man. Man himself becomes human only when in society with fellow-men. Children lost in forests when young, growing up there, resemble beasts. The higher the civil- ization of men, the closer and more complicated are the relations between them. Now if this be so ; if the social life is the only field where, in men or in animals, a higher growth of the spirit is possible ; and if with man the social life is far more developed than with any other member of the animal kingdom, we may draw our final conclusion, namely, that we can determine the psychical rank of any animal, from a knowledge of the degree of its ability to manifest itself to its fellow-beings, or, what is the same thing, of its organs for sympathetic motions. 163 An example may illustrate the truth more fully. Let us look at these organs in a fish, a lizard, and in man. The fish rests horizontally in the water ; the head, neck, and trunk form one bulky mass ; the dorsal column itself is the locomotatory oi-gan ; the four limbs, fins, are used for balancing the body ; the ears are rudimentary ; the eyes stiff, cold, without eyelids, and thus without expression, and from their position and slight mobility, of a very narrow horizon ; there is no voice with which to call a companion. What means has this animal, by which to show to another being what it feels ? Now as we see in fishes hardly any organs for sympathetic motions, or senses for sympathetic perceptions, we think we are justified in saying, that there must be also in them very little sympathetic feehng or thinking. Let us rise some steps further in the series of vertebrates, to the lizard, — that quick, lively, sagacious animal. While in fishes, the greater part of the body, and all four limbs, are used in loco- motion, we find here four developed legs, the body nearly exempt from the function of locomotion, and thus capable of further differentiation ; and the head, neck, trunk, and tail are distinct. With the distinct neck, and consequent ability to turn the head, are immediately connected, not only a larger horizon, but also many motions which manifest whatever moves or excites the animal. Together with the larger horizon, the eyes are very well developed, and the play of the eyelids (which are wanting in fishes and even in snakes) gives expression ; so much, indeed, that I have been able to tell from a glance at the eyes alone of some lizards which I once kept alive for a long time, and which were tame, whether they felt well or not. The ears, also, the organs of the real social sense, are well developed in lizards ; and though the animals themselves have no voice, still they seem to like music. The tongue, which rarely exists in fishes, and when present, is a mere organ for swallowing food, has here not only become an organ of touch, but a means of expressing sympathy, for I have seen them licking each other in play. In turtles, which are higlier than lizards, we find already a voice ; and even the fore feet are used as organs for sympathetic motions. Prof. J. Wyman, in observing two of our common pond turtles at the breeding season, saw the male gently stroke the head of the female for some minutes. 164 Rising a step higher, we find in birds the voice developed to a high degree, but yet confined to a narrow range of modulated sounds. In mammalia, the organs for sympathetic motions are more developed than in birds, except, perhaps, those connected with the voice, although even this point remains to be settled. In mammalia, we find the first hints of what shall come in man. The first idea of an arm, we find in the bear, — it embraces ; and this idea of an arm is connected with the ability to stand erect upon the flat of the foot. In mammalia, too, we first find the idea of a hand, hinted at already in the bear, but carried out more fully in the monkey. The features of the face we find remark- able in tlie dog, and still more so in the monkey. We could find a like series in the organs of reproduction, which from this merely natural view, must be considered organs of sympathy. It is interesting to consider hermaphroditism from this stand- point : it will be evident that it cannot occur in any animal of high psychical endowments. We will in addition, merely call attention to the fact that fishes have no organs of copu- lation, or very rudimentary ones, that in many species the male does not know the mother of the eggs which it fecun- dates, while on the other hand, some reptiles, many birds, and most mammalia live in pairs, or, at least, their males and females go together throughout life, helping and taking care of each other. All the family life, the only fountain of moral and intellectual beauty, rests in the distinction and voluntary union of the sexes, and this distinction and union only make possible the highest unity of two beings which exists. We will dwell no longer on these steps, but consider man him- self. If our principle of coincidence of the degree of psychical development, with the degree of the development of the organs of sympathetic motions, be true, we must find these latter in their highest condition in man. And so it is. Man, standing upright on his feet, has all his body free for sympathetic motions ; and the organs by which they are performed are here in perfection. What we saw in the fish as a balancing instrument, in the lizard as a mere locomotatory organ, is in man an arm which embraces the child, the friend. With the hand, of which we saw no sign in the fish, which is a foot and a locomotatory oi'gan in the lizard, and the same in all mammalia, even monkeys, man grasps the 165 hand of his fellow-man, and shows him what he feels, and with it, he emphasizes his language. Here are the features of the face, expressing by the most diversified play of motions, the varying conditions of the spirit, telling love and hate, joy and pain. Here are the eyes, the mirror of the soul. All these organs we find in a lower condition, in the higher mammalia, especially in monkeys. But there is one kind of sympathetic motions, which man alone enjoys, — those employed in language, — the power to express fully his4deas, his emotions to other men, by modulated sounds, produced by the complicated motion of the larynx, the tongue, the lips, &c. Many animals, it is true, have a voice, but none of them can express a series of thoughts or feelings. The cry of an animal is always the last concluding word of a sentence. It may be the result of a series of thoughts, but this series itself is never expressed. Men have also this kind of sounds — the sounds of laughing, crying, and many others : thus the war-cry of the Indian is no language ; it is an animal sound, like the cry of a wolf, when it calls others to help. But all men have, beyond these animal sounds, the free, flexible language. They not only show to each other, some of the points of their thinking, and feel- ing, and willing ; they show, or can show, all the process which goes on within ; that is, their inner natures can, by means of language, communicate with each other freely. We I'ecognize in language the highest kind of sympatlietic motions. Conclusions. Firstly, when trying to study the psychical en- dowments of animals, we have to start from the study of their mo- tions, as the only manifestation of their mental constitutions (fvxf/) which we can perceive. Secondly, There are to be distinguished in animals two kinds of voluntary motion, — the subjective and the sympathetic. The latter furnish the principal data for the study of the psychical rank ; for every higher endowment flows fi'om the sympathy of one feeling and thinking being with another. Sympathy is only a flowing forth of love, and love is the fountain of all moral and intellectual beauty in man. Mr. C. J. Sprague stated that he had been informed by a friend, who had recently visited Singapore, of a curious fact, viz : that many of the bodies of the natives 166 who are killed by the tigers, are left unconsumed, and that, upon an average, one body daily is found with the neck dislocated. Dr. Charles Pickering observed that undoubtedly many bodies are found, but probably a much larger number are carried off by the tigers into the thick jungles, and consumed at their leisure. Dr. A. A. Gould presented, in the name of J. P. Cou- thoy, Esq., specimens of corals taken in seventy feet of water from the well-known wreck near the Island of Magdalena. The vessel has been under water about forty years, and consequently these corals are not above that age. He supposed them to be the largest speci- mens found upon the wreck, and suggested that they might aid in determining the rate of coral growths. Capt. Atwood exhibited a bottle of oil, a specimen of a substance which is occasionally thrown up on the shore of Provincetown, and which is supposed to come from the remains of the brig Hollander, which was lost some twenty years since in that neighborhood, and which was probably laden with linseed oil. The specimen was referred to Dr. Hayes for exami- nation. Dr. Bryant exhibited several of the birds presented last year by the Victoria Society, at Melbourne, and a por- tion of Mr. Samuels's birds from California. Dr. Gould presented, according to the directions of the late Dr. Binney, the third volume of the Terrestrial Mollusks and Shells of the United States, described and illustrated by Dr. Binney, and edited by Dr. Gould. 167 March 18, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. Dr. A. A. Hayes reported that the specimen of linseed oil which was referred to him at the last meeting, had been tested. It was found to be slightly acid, in consequence of well-known reactions taking place between a minute quantity of fermentable matter expressed from the seed and the oil, resulting in the pro- duction of an oily acid. Tlie oil is not, however, in the state which it assumes on exposure to air, but closely resembles fresh- drawn oil, in all respects but odor and slight acidity. When boiled as usual, it becomes capable of forming the elastic film after exposure to air, and its useful properties have not been lost or impaired after its long submersion in sea water. In answer to a question from Mr. Mills, as to the composition of pudding-stone, Dr. Hayes replied that he had made a some- what extended examination of the cementing material of the Roxbury conglomerate, and found that it is silicate of lime gen- erally. There are cases where finely-divided slaty argillite forms, with silicate of lime, quite large quantities of cement, uniting pebbles of considerable size ; but these exhibitions are only another feature, referable to the action of the same silicious compound. The rock contains chlorine, and as chloride of calcium is readily decomposed by hydrous silica, it might be assumed that the silicate of lime was thus formed. But the con- glomerate is very frequently traversed by bold dykes of trap, which contain a large amount of sulphuret of iron, and the fissures in the conglomerate, being often filled with sublimed quartz, the more probable supposition is, that the silicate of lime was formed by the transportation of silica in the heated vapor of water. Such silica would combine with the lime and alumina of the comminuted slates, and form the cement at the points where we now find it. In reply to a question, Dr. Hayes expressed as his conclusions, 168 respecting the silicification and consequent preservation of organ- isms,— that the process proceeded, step by step, with the change of the organism into gaseous or aqueous matter. The mollusca may be considered as simply organized water, for one hundred parts by weight, often contain ninety-seven parts of water, vola- tile at 150° F. The cell walls of albumino-gelatinous matter are permeable, and the infiltration of aqueous solutions of silicate of lime, would displace the water, gradually depositing silica in a hydrous state, while the lime passed out with the water. As consolidation is hastened by the decomposition of the animal matter, the cell walls become changed, and the carbon or humus, in excess over that which can become gaseous or aqueous, remains ; retaining as a mere skeleton the forms of the walls. These silicified forms are always porous, and the flints contain the carbon of the organic matter, unevenly distributed. As a beautiful illustration of silicification, he referred to the specimens of trees from California, frequently found in the explorations for gold ; many of the specimens presenting the sap vessels entire in all their delicate organization and nearly natural color, while near by, on the same piece, may be seen black portions, in which the organized forms are lost, and the color is deep black. This striking diversity is due to the fact that the wood at some points had passed into the last stage of humus, — carbon and water, — before silicification took place, and hence the specimens present us with both silicified wood and silicified charcoal. He observed the same changes, though less obvious, while examining the highly interesting locality on the Island of Antigua, and at a ' future meeting will exhibit illustrative specimens. Dr. C. T. Jackson remarked that he had examined the mate- rials which enter into the composition and cementation of sand- stones and conglomerates, and had found the cements to be differ- ent in different cases. In some, carbonate of lime forms the principal cement, in others, oxide of iron composed a large propor- tion of the cementing matters, and in others, finer particles of the same I'ocks that composed the conglomerate had formed a paste, which had been hardened by the agency of heat and by the production of silicate of lime derived, undoubtedly, from the decomposition of chloride of calcium. He stated that when peb- 169 bles are moistened with a solution of chloride of calcium, and then placed in contact and heated, the chlorine of the chloride of calcium escapes, and the oxide of calcium or lime unites with the silex and forms silicate of lime. There could be no doubt that the chloride of calcium was derived from sea-water. Some- times in the vicinity of trap dykes, as at Purgatory, near New- port, Rhode Island, specular iron ore, evidently derived from sub- limation of oxide of iron from the chloride of iron, had invested the pebbles with a thin crystalline film, which served as a cement. He stated some experimental results of M. Gay Lussac, on subli- mation of specular iron ore, from chloride of iron, and his obser- vations on the production of this ore in the crater of Mt. Vesu- vius ; experiments and observations which Dr. Jackson had repeated and verified. The cementing materials of some sandstones are so largely calcareous, that on removal of the carbonate of lime by the action of acids, the stone crumbles into sand. In such sandstones the carbonate of lime was probably infiltrated as a bi-carbonate, and on losing one equivalent of carbonic acid, the carbonate of lime would solidify in crystalline form and firmly unite the sand, making it into a solid rock. If a sandstone, cemented by carbonate of lime, is exposed to a high temperature, silicate of lime would be produced by combi- nation of silex with the lime, and carbonic acid gas would be disengaged. Dr. Henry Bryant called the attention of the Society to some of the birds presented by the Royal Victoria Society of Melbourne, Australia. Among them was a pigeon resembling more nearly the Phaps elegans of Gould than any other species he had found described ; but differing sufficiently from Gould's description to lead him to believe that it might prove to be a new species. The dif- ference consists in the present specimen having a whitish line beneath the eye, not found in the P. elegans, and in the back being a greenish brown, with slight metallic reflections, instead of " deep, rich, lustrous chestnut," as described by Gould. One of the birds on the table did not belong to the Society, but 170 was placed there merely for exliibition. It was one of three belonging to a gentleman of this city, which had been mounted by the taxidermist. It was the Magnificent Trogon, ( Oalurus resplendens, Gould,) one of the most brilliant birds known, and though it would not, perhaps, bear a minute comparison with some of the humming-birds, yet, from its size and graceful plumage, it must be unsurpassed as seen in its native wood. Dr. Bryant also remarked, that, in consequence of the unusual mildness of the weather in February, the blue- birds and other of the earlier migratory birds, made their appearance this year by the 15th, nearly a month earlier than they ordinarily arrive from the South ; and that, although the weather had subsequently been quite severe, (the thermometer falling to near zero,) the blue- birds had remained with us, and were singing and ap- parently enjoying themselves at this low temperature. In reply to a question from Mr, Wetherell, as to the production of sugar from the Chinese Sugar-cane raised in this neighborhood, Dr. Jackson stated that crystallized sugar could not be profitably made, but that a syrup suitable for food or distillation could be obtained. The amount of crystallizable sugar in the plant increases the farther south the plant is raised. Dr. Jackson has ob- tained a certain quantity of crystallized sugar in the cane grown at Watertown, Mass. Dr. Durkee exhibited the Algse brought from Califor- nia, by Mr. Samuels, and Dr. Bryant exhibited some of the birds which had been recently mounted. The Corresponding Secretary announced the receipt of the following letters, viz : — From the Linnsean Society, London, Nov. 25, 1856, Entomo- logical Society, London, Dec. 3, 1856, Geological Society, London, Dec. 4, 1856, American Philosophical Society, March 13, 1857, and the Societe de Geographic, Paris, Feb. 7, 1857, acknowl- in edging the receipt of the publications of the Society ; Naturfor- schende Gesellschaft, in Eraden, Oct. 2, 1856, and the Acade- mic des Sciences, Paris, Feb. 14, 1857, presenting their pub- lications. Mr. A. M. Gay was elected a Resident Member. DONATIONS TO THE MUSEUM. January 7, 1857. Specimens of impressions in the Connecticut Valley Sand- stone, possibly made by tadpoles, by Prof. Edw. Hitchcock. (See printed Pro- ceedings, Vol. VI. p. Ill, for an account of these impressions.) Eviys marrnorata, Crotalus lucifer, and Rana longipes, from California, by E. Samuels. Begina Kirtlandii, from Illinois, by Robert Kennicott. January 21. Cranium of a Digger Indian, from California, by E. Samuels. A Bulbous Root, and a specimen of Gum from Africa, by Rev. Louis B. Schwarz, (For an analysis of this gum and an account of the plant, see printed Proceed- ings, Vol. VI. p. 129.) A white-throated Sparrow, {Fringilla Pennsylimnica, Aud.) a Rusty Blackbird, {Icterus pecoris, Aud.) and a Yellow-rumped Warbler, (Sylvia coronata, Aud.) together with a Black Squirrel, (Sciurus niger, Linn.) all from Lake Superior; by Dr. S. Kneeland, Jr. February 4. Specimens of a new minute species of Snail, Helix asteriscus, Morse, from Bethel, Maine; by E. S. Morse. A suite of Helix thyroidns, Say, from various localities; by W. G. Binney. Specimens of Red Gum Wood aud the Common Building-Stone of Australia, by 0. H. Holden. February 18. Four crania of birds ; a fragment of the jaw-bone of an alliga- tor, illustrating the development of the teeth; an egg-shell with a peculiar pro- tuberance; and some fossil shells from Georgia; by Dr. H. Bryant. A specimen of Silicified Wood from the Colorado Desert, California; by W. P. Blake. March 4. Corals, taken in seventj' feet of water from the Spanish wrecked vessel off the Island of Magdalena; by J. P. Couthoy. Two specimens of Downy Woodpecker, {Pints pubescens, Linn,) from Milton; by E. Sanmels. Min- erals from California and a neuropterous insect, CuirydaUs ccn-nuius, from Boston ; by S. Adams. March 18. The Saw of a Sawfish taken in the Persian Gulf and a Fossil, My- craster cor-anguinum, Agass. ; by Rev. J. P. Robinson. A Glossy Finch, {Ama- dina nitens); Beautiful Weaver-Bird, [Hyphantornis per-sonata ;) and an undeter- mined species of Hyphantornis ; by Dr. F. J. Bumstead. BOOKS RECEIVED DURING THE QUARTER ENDING MARCH 31, 1857. Terrestrial Air-Breathing MoUusks of the United States and adjacent Territo- ries of North America, described and illustrated by Amos Binney. Edited by Augustus A. Gould, M. D. 4to. Vol. III. Plates. Boston, 1857. From the Heirs of Amos Binney, 172 Descriptions of Terrestrial Shells of North America. 12mo. Pamph. By Thomas Say. Philadelphia. 1856. From W. G. Blnney. Animal Report of the Geological Survey of the State of Wisconsin. By J. A. Percival. 8vo. Pamph. Madison, 1856. Fi-om J. A. Lapham. On the Avoidance of Cyclones, with Notices of a Typhoon at the Bonin Is- lands. By J. Rodgers, U. S. N., and A. Schouborn. 8vo. Pamph. New Haven, 1857. Fmn W. C. Redfidd. First and Second Reports on the Noxious, Beneficial, and other Insects of the State of New York. By Asa Fitch, M. D. 8vo. Albany, 1856. From the Author. Notes on American Species of Cyclas. By Temple Prime, L. L. B. Part I. 8vo. Pamph. The Hague, 1857. From the. Author. Prodromus animalium evertebratorum quae in Expeditione ad Oceanum Pa- cificum Septentrionalem observavit et descripsit W. Stimpson. 8vo. Part I. pp. 1-13. Philadelphia, 1857. From the Author. Report of the Commissioner of Patents for 1835. Agriculture. 8vo. Wash- ington, 1856. From the Hon. Henry Wilson. Memoir of James Brown. By G. S. Hillard. 8vo. Boston, 1856. From, Messrs. Little, Brown if Co. Nachrichten von der Georg-Augusts-Universitat und der Konigl. Gesellschaft der Wissenschaften zu Gottingen, 1855. 12mo. Pamph. From the Society. United States Astronomical Expedition in 1849-52. Vol. VI. Under direc- tion of Lieut. J. M. Gilliss. 4to. Washington, 1856. From Lieut. J. M. Gilliss. Narrative of the Expedition of an American Squadron to the Chinese Sea and Japan, in 1852-4, under Commander M. C. Perry, U. S. N. 4to. Washington, 1856. Vols. I. III. Report of Commissioner of Patents for 1855. Arts & Manufactures. Vols I. II. 8vo. Washington, 1856. From the Hon. Chas. Sumner. Magnetical and Meteorological Observations at Lake Athabasca and Fort Simp- son. By Capt. J, H. Lefroy, and at Fort Confidence in Great Bear Lake, by Sir John Richardson. 8vo. London, 1855. Ichthyology. Article in Encycloptedia Britannica. 4to. Pamph. London, 1857. From Sir John Richardson. Quadrature of the Circle, &c. By A. Young. 8vo. Pamph. Burlington, Vt., 1853. Theory and Laws of Solar Attraction. By A. Young. 8vo. Pamph. St. Albans, Vt., 1856. Fro7n G. F. Houghton. Rendiconto della Societa Reale Borbonica. Anno, 1855. 2 Nos. Naples. Memoria suUo Incendio Vesuviano del Mese di Maggio, 1855,fatta per incarico della R. Accad. delle Scienze dai Socii, G. Guarini, L. Palmieri ed A. Scacchi. 4to. Pamph. Naples, 1855. From the Accademia delle Scienze. Canada at the Universal Exhibition. 8vo. Toronto, 1856. Tables of the Trade and Navigation of the Province of Canada, for 1855. 8vo. Toronto. Annual Reports for 1854 and 1855 of the Normal, Model, Grammar, and Com- mon Schools in Upper Canada. 8vo. Pamph. Toronto. Reports of the Superintendent of Education for Lower Canada. 8vo. Pamph. Toronto, 1850, 1851, 1865. 173 An Act to regulate the Militia of the Province. 8vo. Pamph. Quebec, 1855. Acte des Municipalit^s et des Chemins de 1856. 8vo. Quebec. Annual Reports (1830-1836) of the Natural History Society of Montreal. 18mo. Pamph. Montre.al. Catalogue de la Collection Envoy^e du Canada a I'Exposition TJniverselle de Paris, 1855. 12mo. Pamph. Paris, 1855. From L. A. Huguet-Latour. New York Journal of Medicine. Vol. II. Nos. 1, 2. 8vo. New York. Silliman's American Journal of Science and Arts, Nos. 67, 68. Schriften der in St. Petersburg Gestifteten Russisch Kaiserlichen Gesellschaft fiir die Gesammte Mineralogie, I. &vo. St. Petersburg, 1842. Notices of the Meetings of Members of the Royal Institution of Great Britain. Part VI. 8vo. July, 1855-6. London, 1856. Also, List of Members, &c. Pamph. London. Kongl. Vetenskaps-Akademiens Handlingen, fur 1853, 54, 55. 8vo. Stockholm. Proceedings of the American Philosophical Society. Vol. VI. No. 56. July- December, 1856. 8vo. Pamph. Philadelphia. Memoirs of the American Academy of Arts and Sciences. New Series. Vol. VI. Part. L 40. Cambridge, 1857. Proceedino;s of the Academy of Natural Sciences, pp. 1-16, and 87-94. 8vo. Pamph. Philadelphia, 1857. Bulletin de la Socit^te de Geographic. Tome XII. 8vo. Paris, 1857. Canada Naturalist and Geologist. Vol. II. No. 1. Montreal, 1857. Transactions of the Linnajan ' Society of London. Vol. XXII. Part. I. 4to, London, 1856. Journalof the Proceedings of the Limiffian Society. Botany. Vol.1. Nos. 1-3. Zoology. Vol. I. Parts 1-3. 8vo. London, 1856. List of the Members of the Linuasan Society of Loudon. 8vo. Pamph. 1856. Received in Exchange. Annals and Magazine of Natural History. Nos. 108, 109, 110, for Dec. 1856, and January and February, 1857. 8vo. London. From the Courtis Fund. Encyclopasdia Metropolitan a. Vol. XII. 4to. London, 1856. Also. Vol. I. Part 4, containing Dissertation 6th, Mathematical and Physical Science. 4to. Pamph. London, 1856. Deposited by the Rejmhlican Institution. April 1, 1857. Dr. D. H. Storer, Vice-President, in the Chair. Dr. A. A. Gould offered the following preamble and resolutions relative to the decease of Prof. J. W. Bailey, and they were unanimously adopted : — In addition to those immediate and corresponding members 174 who have been recently removed by death, — men of original research and large contributors to tlie extension of the bound- aries of science, — men equally notable for their blameless lives and scientific attainments, — Forbes, Johnston, Redfield, Thomp- son, Harris, Warren, — we have now to associate the name of Bailey, for a long time one of the professors at West Point. None who have had the good fortune to know him can fail to appreciate his truly philosophical spirit, his zeal, his accuracy, and his extreme modesty. With his early life I am unacquainted, and so far as I know, the first paper of any extent which he communicated, was one which he read to the Association of Geologists and Naturalists at their meeting in Boston in 1843, entitled " Sketch of the Infusoria of the family Bacillaria, with some account of the most interesting species which have been found in a recent or fossil condition in the United States." It extended to upwards of fifty pages, was illus- trated by six plates and gave him at once a high place among scientific men. Since then he has published numerous papers, mostly in Silliman's Joui'nal, on the microscopic forms of animal and vegetable life, to which, and to the perfection of the micro- scope as an optical instrument, he chiefly limited his investiga- tions. Prof. Harvey, in the introduction to his work on the Algae of North America, thus writes : " Well known in his own peculiar branch of science, he has found a relaxation from more wearing thought in exploring the microscopic world, and his various papers on what may be called ' vegetable atoms,' (Diatomacea^) are widely known and highly appreciated. From him I received the first specimens of United States Alg^e which I possessed ; and, though residing at a distance from the coast, he has been of essential service in diffusing a taste for this department of botany." I think none will gainsay me when I characterize him as the Ehrenberg of America, — and that in having been selected to preside at the next meeting of the American Association for Science, he had received but a merited honor. Resolved, That in the death of Prof. Jacob W. Bailey, we, in common with the numerous scientific associations with which he was connected, deplore the loss of a true philosopher, a laborious coadjutor, and a most amiable man. 175 Resolved, That we tender our sympathies to the deeply-afflicted survivors of his family left orphans by the sudden and heart- rending removal of a mother, and by the premature death of an endeared father. Captain N. E. Atvvood, of Provincetown, having been requested to favor the Society with some remarks upon fishes and their habits, related many interesting facts which had come to his knowledge during a life spent as a New England Fisherman. He first remarked upon the senses of taste, smell, sight, and touch. It has been said by eminent ichthyologists that taste and smell are very imperfectly developed in fishes; but this is not the fact. Many fish are very particular in the choice of food ; others, such, as the mackerel and blue-fish, and mid-water and top-water fish generally, seem to be governed by sight in their selection of food. He had often seen mackerel, when they were abundant around a vessel, take all the bait that was thrown over- board, but at the same time carefully avoid the baited hook. He had also noticed that tobacco thrown overboard was seized by mackerel but immediately rejected, showing as he thought a sense of taste. It is to be presumed, however, that taste must be imperfectly developed in animals which have a tongue more or less cartilaginous, and covered with recurved teeth ; being obliged unceasingly to open and close the jaws for the purpose of respira- tion, they cannot long retain food in the mouth, but are obliged to swallow it without mastication. The sense of smell seems to be well-developed in some fishes. For instance, the ground swimmers generally have a choice as to their food. Halibut and cod are attracted a great distance with certain kinds of bait. Herring, when fresh and in good condi- tion, will be very readily taken by cod, but when it has become stale from long keeping, it will be rejected. Crustaceans, also, as lobsters and crabs, are attracted by certain bait, which leaves no doubt that they likewise possess some sense of smell. Al- though the cod seems to swallow almost any thing that comes in his way, even stones, wood, and fragments of nearly every thing thrown overboard, Mr. Atwood had never seen an univalve mol- 176 lusk in its stomach. The bivalve shell is found, and the bank clam is very common in the stomach, the shells being placed within each other in the most compact manner, when there are several of them in that organ. In some other ground swimmers, both bivalve and univalve mollusks are found. The haddock, ling, catfish, and one species of flounder are great shell-eaters, and very frequently undescribed species of moUusca are taken in their stomachs. The cod lives mostly upon live fish. It is very greedy, and even when distended with food, it will bite briskly at the hook. It is frequently taken with a full-grown mackerel partly in its stomach and partly in its mouth, with the tail still projecting. At other times, when the alimentary sack is empty, it appears to have no desire to partake of food. When kept alive in the holds of vessels, no other nourishment is given the cod than the minute animalcules contained in the water. A very curious fact Mr. Atwood stated that he had observed, — the cod often swallows alive the tant or sand-eel and the pipe-fish, both having heads very much elongated anteriorly and pointed. These fish some- times pierce the stomach of the cod and escape into the abdomi- nal cavity, and there they are found in a perfect state of preser- vation, adherent to its walls, but changed in color to a dark red, and in substance so hard that they are not readily divided with a knife. They have to be cut away before the cod can be split open. The fish is always in good health apparently, and there are no marks of inflammation about the stomach or abdominal cavity, unless the material of attachment be considered as such. Fish migrate considerable distances in quest of prey, sometimes totally deserting localities where they have been very abundant. There is a species of crustacean called commonly by fishermen the sea-flea, which infests spots upon the Grand Banks, hun- dreds of square miles in extent, and which drives before it the cod and other fish. During his last voyage to the Banks, Capt. Atwood tried to fish with clam bait, which, however, came up untouched ; he then put on menhaden for bait and lowered to the bottom, but upon raising the hook nothing was found but the skeleton of the fish, the soft parts having been consumed by the sea-flea. 177 Dr. Chas. Pickering observed, witli reference to the sense of smell in fishes, that he had examined the brain of the shark, and that in this, as well as in cartilaginous fishes generally, the development of the olfactory nerve and the olfactory lobe of the brain was very considerable. The chairman, Dr. D. H. Storer, called attention to the last volume of the work on the Terrestrial Mollusca of the United States, by the late Dr. Binney, edited by Dr. A. A. Gould, a copy of which had been recently pre- sented to the Society. He stated that Dr. Binney was desirous, and left directions for the completion of the work, the charge of which was committed to Dr. Gould. It had taken ten years to complete it; but the duty had been nobly and admirably performed, and it was exceed- ingly gratifying to him to say that it would prove most creditable to the Society and to the country. Mr. Amos Binney said that ten years might seem a long period for the completion of the work, but any apparent delay was more than sufficiently accounted for by the time occupied in collecting the materials, which, at the decease of his father, were very widely scattered. Dr. A. A. Hayes exhibited some fragments of iron and bronze vessels from the volcanic ashes of Pompeii, which had repassed from the state of a wrought metal to that of the original ore. Dr. J. B. S. Jackson exhibited an Intestinal Worm, (Ascaris lumbrico'ides,) which was passed from the rectum of a child, with about an inch of its body inserted through the eye of a common dress-hook. He observed that this example illustrated the singular tendency of this worm to crawl through perforations in the intestine, into the duct of the gall-bladder, or into the appendix coeci. PROCEEDINGS B. S. N. H. VOL. VI. 12 JUNE, 1857. 178 Dr. A. A. Gould presented, in the name of Lieut. Preble, U. S. Navy, a specimen of Dlpsas plicata, upon the inner surface of which were a number of beautiful elevated pearly figures, representing the god Boodh, pro- duced during the lifetime of the animal, upon nuclei placed within the shell. The following account of the process, by Dr. Magowan of Ningpo, accompanied it: — The introduction of the pearl nuclei is an operation of consid- erable delicacy. The shell is gently opened with a spatula of mother of pearl, and the free portion of the mollusc is carefully separated from one surface of the shell with an iron probe ; the foreign bodies are then introduced between the points of a bifur- cated bamboo stick, and placed in two parallel rows upon the mantle or fleshy surface of the animal. A sufficient number having been placed on one side, the operation is repeated on the other. Stimulated by the irritating bodies, the suffering animal spasmodically presses against both sides of its testaceous skele- ton, keeping the matrices in place. This being done, the animals are deposited one by one in canals, streams, or pools connected therewith, five or six inches apart, at depths of from two to five feet, in lots of from five to fifty thousand. If taken up a few days after the introduction of the moulds, they will be found attached to the shell by a membranous secretion, which at a later period becomes impregnated with calcareous matter ; and finally layers of nacre are found deposited around each nucleus, the process being analogous to the formation of calculous concretions in animals of a higher development. A ridge of nacre generally extends from one pearly tumor to another, connecting them all together. About six times in the coui'se of the season several tubs of night soil are thrown into the reservoir for the noui'ishment of the animals. Great care is taken to prevent goat manure falling in, as it is highly detrimental to the mollusc, preventing the seci'etion of good nacre, or killing them, according as the quantity is great or small. In November the shells are carefully collected by hand. Dr. Storer presented a specimen of the Trumpet Fish, {Centriseus scolopax.,) caught at Provincetovvn, the first 179' known to him to have been taken upon this eoast. It is common upon the European coast and in the Mediter- ranean. Messrs. James G. Shute, of Woburn, and Henry J. Clarke of Cambridge, were elected Resident Members. April 15, 1857. Dr. Chas. T. Jackson, Vice-President, in the Chair. Dr. A. A. Gould announced a bequest to the Society, by the late Professor Jacob W. Bailey, of West Point, N. Y., a Corresponding Member, dated February 11, 1857, communicated in a letter from his brother William M. Bailey, Esq., of Providence, as follows : — BEQUEST OF PROF. J. W. BAILEY. " First. A microscopic collection, contained in cases resembling books, together with said cases, and the index volumes thereunto belonging ; the whole bearing for titles, ' Microscopic Collec- tions.' " Second. The whole of my collection of Algce, or Sea-weeds, as contained in a set of portfolios, together with said portfolios. " Third. All my rough material for microscopic research, as contained in small boxes, paper, vials, and larger boxes, con- taining large masses marked with chalk, Richmond, Petersburg, Georgia, Florida, «fcc. " Fourth. I request said Society to retain the first and second of the foregoing bequests as a part of their collections, as long as said Society shall exist, making such uses as they please of the rough material in the third bequest." Also, in a codicil, dated February 24, 1857 : " A volume con- taining rough sketches, &c., of microscopic forms, and marked with title, 'Microscopic Memoranda.'" 180 Also, " All my other microscopic drawings, sketches, or micro- scopic memoranda, to be kept or destroyed, in any part, at the option of the Society." Also, " Such of the following books as are not possessed by the Society, viz : Ehrenberg's Microgeologie, and all my other German Scientific Books ; also, all my books, pamphlets, &c., relating to Algse, Diatomacese, Microscopic Botany, and His- tology ; also, Lindley and Hutton's Fossil Flora, and all my other Botanical Books." Also, " My ' Scientific Letters,' in packages so marked, with the privilege of destroying such as are of no value to the Society, as autographs, &c." " I desire that my Executor shall stipulate with the Boston Society of Natural History, to which I have made valuable be- quests, that such bequests shall be placed in a case or cases by themselves, and that my sons, who may be at college at Cam- bridge, may have such access to such case or cases, for the pur- pose of study or examination, as may be consistent with the rules of said Society." Dr. Gould, after remarking upon the great value of this bequest to the Society, upon its importance to science in the study of microscopic recent and fossil forms, offered the following resolutions, which were unani- mously adopted : — Resolced, That while acknowledging the receipt of the bequest of the late Prof Bailey, the Society would express its gratifica- tion at having been made the depository of collections containing original and authentic specimens of microscopic forms and Algje, which must ever remain the ultimate and standard objects of reference, in this country, in the study of those subjects ; i^ledg- ing itself to secure, as far as practicable, their preservation, and to make them as extensively useful as possible. Resolved, That a Committee be appointed to receive and report upon the bequest, and also to execute the expressed wish of Prof. Bailey, that his "bequests shall be placed in a case or eases by themselves." Resolved, That the request of W. P. Blake, Esq., be granted. 181 desiring that such papers as may be found rehiting to a Report on the Infusoria of California, may be given up to him for publi- cation, as originally intended. Resolved, That the thanks of the Society be presented to W. M. Bailey, Esq., for the prompt and complete manner in which he has executed the will of his brother, so far as concerns this Society. Dr. A. A. Gould, Prof. John Bacon, and Dr. Silas Durkee were appointed the committee referred to in the second resolution. The following communication was read from Mr. Charles J. Sprague, on the Botanical Position of the Chinese Sugar Cane: — The plant was called Holcus saccharatus by Linnaeus ; but when this genus underwent a subdivision by subsequent botanists, this species was placed by some in that of Andropogon, by others in that of Sorghum. These two genera are closely allied. Some of the best authorities consider the diflferences so slight as to warrant their union into one. Steudel arranges Andropogon, Sorghum, and Trachypogon all under one head — Andropogon. Lindley italicises Sorghum in the last edition of his " Vegetable Kingdom," and places it beneath Trachypogon, evidently consid- ering them equivalent. Dr. Gray retains Sorghum for our only native species (aS*. nutans) in his last edition of the Manual, con- sidering the genus a good one. It is between Andropogon and Sorghum, therefore, that we must choose in reference to this particular species. The differences between them are these — Andropogon. Sorghum. Inflorescence spicate. Inflorescence paniculate. Spikelets in pairs, only one Spikelets in twos or threes, cen- being fertile. tral one only being fertile. Glumes herbaceous or mem- Glumes hard, coriaceous or in- branaceous. durated. Eachis hairy. Rachis smooth. 182 If these differences shall eventually render the genera suffi- ciently distinct to establish a universally recognized separation, then this jilant must be placed under that of Sorghum. The specific name is a matter of some doubt. Both >S'. vulgare and S. saccharatiim are recorded as distinct species ; but there is frequently a query appended to the latter. Some of our best authorities incline to the opinion that these two are identical, the differences between them being due to the long cultivation which the plant has undergone. We know tliat some of the grasses have sported into numerous varieties ; and it is very probable that the Broom Corn, Doura or Guinea Corn, and the Chinese Sugar Cane are all descended from one and the same stock. If we accept this as a fact, then the plant should be called, Sorghum vulgare, Pers., var. saccharatum, L. ; but as the latter name is so extensively known, and as there is still some doubt as to the identity, it may be as well to continue the name Sorgli um saccharatum. The true Sugar Cane, Saccharum ojfficinarum, belongs to the same tribe of grasses, differing in the ample inflorescence, which is paniculate, and drooping with downy pedicels and florets. A letter was read from Robert Kennicott, Esq., of Illinois, accompanying a donation of Mammalia, Birds, and Shells. With reference to the Mammalia, Mr. Ken- nicott says : — " The Arvicola austerus is a prairie animal, and will interest any one studying mammals ; the A. riparius is pronounced a true species by Prof. Baird. The Hespei'omys Bairdii is a new species, which will be described by Dr. Hoy and myself soon. It comes near Audubon's and Bachman's Mas Michiganiensis, but it is readily distinguished upon comparing the two. I have sent your Society specimens of this species (^Bairdii) already, under the name of 3Ius Michiganiensis ; it is strictly a prairie animal. Dr. Hoy has found M. Michiganiensis near Racine, Wisconsin." Mr. N. H. Bishop presented the following list of Plants, most commonly met with daring a pedestrian tour across 183 the continent of South America, from Rosario, on the Parana, to Valparait^o, Chili: — Bolax, an umbelliferous plant, above the snow on mountains, collected 10,000 feet above level of sea. Capsicum, Red Pep- per (aji,) very common in the northern parts of the Republic. Prosopis Algaroba, White Algaroba, order Leguminosa3 ; also Black Algaroba is very common. Portulaca ; Verbena, several varieties ; Loasa, Tropceolum, Alstrcemeria, Chenopodium, ScM- zanthus pimiatus, Geranium, Lathyrus puhescens, Argemone Mex- icana, CEnothera, Liqypia, Acicarpha, QninchamaUum, Salpiglossis ; valleys and base of the Andes. Maloastrum, Supinus ; deserts at the eastern foot of the Andes. Medicago sativa, Alfafa, culti- vated for cattle ; M. maculata, weed refused by cattle, the common Aveed of clover fields. Scirpus, Solanum ; Lagoon near San Juan, on the desert. Tessaria ahsinthoides ; border of lagoon, San Juan, Argentine. Republic, October. Stromhocarpa strombulifera, Screw plant ; Traversia, San Luis to the Andes. Larrea divari- cata ; common; Traversia between Mendoza, and San Juan. Dr. C. T.Jackson gave an account of the Copper Mine, so called, at Elk Run, Fauquier County, Virginia. The copper is found in strata of the Triassic Age, in trap- dykes coming through Sandstone, containing a little of the yellow and gray sulphuret, and the carbonate of copper, azurite, chryso- colla, and malachite in thin films. Had quartz or cai'bonate of lime been the gangue-stone, he should have supjjosed the locality to have been of some economic value. He advised the company not to work it, and afterwards learned that an old mine, in which a shaft had been sunk 150 feet, situated near that place, had been abandoned many years before as unprofitable. Dr. Jackson made some further remarks in illustration of the view that the rock, through which the trap-dyke comes, exerts an influence upon its metallic contents, and refei-red to a previous communication to the Society upon this subject. (vSee report of the Excursion Meeting, printed Proceedings, Vol. VI. p. 24.) Prof. H. D. Rogers said that Geology was in a state of 184 great confusion as to the nomenclature of the superpo- sition of strata. He had felt the necessity of introducing some new terms, and he proposed the following, viz : — 1. Conformable Continuous. 2. Conformable Intei'rupted. 3. Unconformable Continuous. 4. Unconformable Interrupted. He illustrated the application of the terms by the aid of a dia- gram, representing three strata — Limestone below, Shale interme- diate, and Sandstone the uppermost, designating them by A, B, and C respectively. If we find a partial blending of organic remains, and partial intermingling of materials, with evidence of continuity in time of deposition, this condition may be expressed by the first term. If the strata A and C are together in superposition, without physical sign of bi'eak, and yet with abrupt omission in types of life, it should be designated in the second category. If the sequence of the strata is uninterrupted, and yet a displace- ment exists from some physical disturbance, the third term is applicable. The fourth term would designate C, unconformably upon A, and at the same time an exclusion of B. The recognition of such distinctive terms would much tend to promote the science of Geology. Dr. Jackson observed, that amongst other examples of the interrupted series, there is a fine illustration in the superposition of the Sandstones of the Connecticut River, upon the Gneiss, Granites, and Mica-Slate of New Hampshire, at Northfield, Mass.; where the whole PalsEOzoic Series is wanting. Dr. Jackson expressed himself in favor of the nomen- clature of Prof. Rogers, because it was both explicit and succinct. The Chairman announced the death of Prof. Michael Tuomey, of Alabama, one of the Corresponding Mem- bers of the Society, and requested Prof. W. B. Rogers to propose a resolution suitable to the occasion. 185 Prof. Rogers, in doing so, said that he had listened with pain- ful surprise to the announcement just made of the death of our associate, Prof. Tuomey. Last summer, when attending the Scientific Association in Albany, his apparently vigorous frame and look of quiet enthusiasm, gave promise of many more seasons of productive geological toil. Of the early life of Michael Tuomey, Prof. Rogers said he knew nothing, farther than that he was, he believed, a native of Ireland, and coming to this country quite young, became first a resident of the State of New York. As a cultivator of science, he early attracted notice by his study of the Tertiary deposits of the neighborhood of Petersburg, in Virginia, where for some years he resided in the capacity of a teacher. After this he was appointed to conduct the Geological Survey of South Carolina, and having completed the work as far as practicable with the means at his command, published, in 1848, a Report on the Geology of the State, which proved highly acceptable to geologists as well as useful to the community for whose practical benefit it was designed. Soon after this. Prof. Tuomey was elected to the Chair of Geology and Natural History in the University of Alabama, and placed at the head of the State Geological Survey then organ- izing ; in which truly interesting field he has ever since been steadily and actively employed. His paleontological studies in the Tertiary and Cretaceous deposits of the Southern Atlantic States proved a valuable introduction to the examination of those groups of formations as they are developed in middle and southern Alabama ; and we cannot doubt that had he lived to complete the survey, his additions to this branch of our geology, as well as his investigation of the structure and paleontology of the older rocks overspreading the northern part of the State, would have formed an important contribution to our knowledge of that rich and varied portion of our great geological field. His partial Reports of the Survey, of which two or three have been published, although intended mainly to indicate the progress of the v ork, contain many valuable details ; but of the nearness of the si/ vey to its completion, and of the extent and character of the raa/elials in reserve for a final Report, Prof. Rogers was without the means of judging. He could only say, that from the great rich- ness of this part of the geological field, and the known industry 186 and ability of Prof. Tuomey, we bad reason to anticipate from it much interesting matter, especially in the department of Paleon- tology. Besides his occasional descriptions of fossils from the Tertiary deposits, Prof. Tuomey had of late, in conjunction with Prof. Holmes of South Carolina, been engaged in publishing in quarto numbers a work on the " Fossils of South Carolina," which for the excellence of its material, and the faithfulness and beauty of its illustrations, may very favorably compare with any similar work published in this country. Prof. Rogers then offered the following resolutions, which were unanimously adopted : — Resolved, That we have heard with unfeigned regret of the death of Prof. Tuomey, of Alabama, an event which deprives the geologists and naturalists of our country of a zealous and active associate, whose labors had already won for him an hon- orable place among our scientific explorers, and whose knowledge and experience, in connection with the important survey in which he was engaged, gave earnest of still more extensive and valuable contributions. Resolved, further, that we offer to the family and friends of the deceased an expression of our sincere regret and sympathy. Prof. William B. Rogers having asked permission to make a few remarks in relation to the scientific services- of the late William C. Redfield, proceeded as follows : — Since the opening of the present year, the cultivators of sci- ence have been called on to lament the loss of two of their distinguished co-laborers, on this side the Atlantic, William C. Redfield, of New York, and Prof. Bailey, of West Point, the former eminent for his researches on the subject of storms, the latter for his microscopical discoveries. Our Society, claiming Prof. Bailey as one of its most valued members, has already accorded an appropriate memorial to his genius, labors, and virtues. We have also had the satisfaction of numbering Mr. Redfield among our associates, and we are all familiar with his reputation as a man of science, and some of us have known him as a friend. Feeling, therefore, the loss which the community of science, especially in this country, have sustained in his death, 187 we may not inappropriately claim a share in the general and deeply felt regret occasioned by this event, by placing on our records a brief tribute to the scientific- worth and manly excel- lences which marked his career. Mr. Redfield, it is stated, was but little favored in early life by opportunities of education. Even after his removal from his native State, Connecticut, to tlie city of New York, while yet a young man, he became immersed in business occupations such as are commonly thought incompatible with purely intellectual pur- suits, and which in most cases leave but little leisure and still less disposition for the studies and investigations of science. But his strong inclination for scientific inquiries was not to be re- pressed by these discouragements, and he early enrolled himself among the active students of Meteorology, Physical Geography, and Geology. In the first of these departments, which it is well known was the principal field of his investigations, his patience and sagacity in observing facts, and in collating and compai'ing the observa- tions made by others, bore their rich fruit in that remarkable generalization which, under the title of the Rotary Theory of Storms, is so commonly associated with his name. His earliest recognition of this law appears to have been suggested by the phenomena of the violent storm which, in the year 1821, swept over New England ; and it is not a little remarkable that it was a storm occurring the same year in Central Europe which led the German Meteorologists into a similar train of inquiry, and conducted Prof. Dove, of Berlin, to a theory founded like that of Mr. Redfield on the union of a progressive with a rotary move- ment of the disturbed column of air. It must not, however, be supposed that the fact of a revolving motion in some of the more violent storms had hitherto entirely escaped observation. Long before these systematic inquiries were thought of, navigators had recognized such a movement in some of the storms within the Tropics. As far back as 1G80, Capt. Langford, in a paper on West Indian hurricanes, printed in the Philosophical Transactions, described them as progressive whirlwinds ; and at the beginning of the present century. Col. Capper, Mr. Horsburg, and a French writer, Romme, speak of the hurricanes or typhoons of the India and China seas as revolving 188 storms. But these early observations and suggestions, pointing chiefly to local phenomena, and involving no clear conception of a general law, attracted little notice at the time of their publica- tion, and were almost, if not entirely forgotten when Redfield and Dove, without a knowledge of each other's labors, framed the great generalization of the progressive-rotary character of these atmospheric movements. Without detracting from Prof. Dove's share in the investigation, it must, I think, be admitted, that to Mr. Redfield is preeminently due the credit of having first given to this law a truly inductive character ; and I need hardly add that his analysis, year after year, of the data dili- gently collected by him, was a work involving no small amount of detailed labor, as well as of sagacity and skill. Although his investigations were directed pi-incipally to the storms of the Atlantic north of the Equator, he w^as early led on theoretical grounds to announce the proposition that in the southern hemisphere the motion of storms is the reverse of that presented by them in the northern one, both as regards progres- sion and rotation. This statement was soon after confirmed by Col. Reid, the author of the well-known work on the Law of Storms, in an elaborate investigation of those of the Southern Indian Ocean. These important generalizations in the discovery and develop- ment of which Mr, Redfield so largely shai'ed, although not universally accepted either at home or abroad, have been adopted by most of those who have devoted themselves to the practical study of the subject, and in particular have been advocated with much ability by Col. Reid, already named, and by Mr. Pidding- ton, author of the " Sailor's Horn-book for Storms," to both of whom we are indebted for extensive researches in this branch of Meteorology. Through the treatises of these gentlemen, and the numerous memoirs of Mr. Redfield, this theory is rapidly becom- ing familiar to the minds of navigators, many of whom have not only accepted but practically applied it. Even the general public have learned its language and its leading features, from the accounts of cyclones or revolving storms, so often repeated in the current news. It is but proper to add that the evidence in favor of this law has lately received an important accession from the publication by Mr. Poey of Havana, of a tabular description 189 of the gales of the West Indies and Atlantic, in which their pro- gressive rotary character, and the opposite directions of the movement on different sides of the equator is shown by an inves- tigation of between three and four hundred distinct storms, ex- tending over a period of about the same number of years. How far these laws are applicable to other than ocean storms, and what new laws or modifications of the rotary principle may obtain in the interior of continents, are questions which do not seem at present capable of a satisfactory answer. But however they may be decided by future investigations, we cannot, I think, fail to recognize in the generalizations of Redfield and his co- workers a valuable contribution to positive knowledge, and an induction which, even should it be found strictly applicable only to the oceans and their coasts, is fraught with great practical good as well as scientific interest. In saying thus much, I would not be considered as accepting the theoretical views which Mr. Redfield from time to time suggested in explanation of the origin of the revolving and pro- gressive motion which he labored to demonstrate. These specu- lations rarely put forth, and never very strenuously urged, appear to have had but little interest for him in comparison with the establishment of the Icnv of the plienomena. Indeed, they were so briefly, and I must in candor add, so indistinctly presented, as to attract but little attention from the scientific world. At the same time it should be considered that even had Mr. Redfield possessed a philosophical inventiveness and a command of the exact sciences beyond what we would claim, or his own modest self-appreciation would admit as his, we could hardly have hoped that, in the present stage of investigation, he could have furnished a really satisfactory solution of the complex problem of the dynamics of storms. His labors, together with the concurring or the conflicting views of other Meteorologists at home and abroad, mark a great and beneficent progress in this difficult inquiry, and encourage the hope that, along with a knowledge of the laws of the winds, we shall hereafter be able to grasp in our thoughts the mode of their origin and the physical forces by which they are produced. While giving his chief attention to the development of the Law of Storms, Mr. Redfield found time for many useful obser- 190 vations in geology, especially in relation to the fossil fishes of the so-called New Red Sandstone belt of New Jersey and Con- necticut, as well as those of the coal rocks of Eastern Virginia. In this inquiry, he had the valuable assistance of his son, Mr. John H. Redfield, to whom we ai'e indebted for descriptions and figures of several of these interesting fossils, as well as for im- portant suggestions, founded on zoological affinities, as to the age of the belt of rocks in which they are entombed. The continuation of this work had long, I believe, been a favorite plan with Mr. Redfield, and seems to have been one of the last subjects connected with scientific pursuits which engaged his attention ; for on his visit to Boston in the autumn, he spoke with much interest of having resumed the task of preparing, with the help, I think, of Prof. Agassiz, a comprehensive mono- graph of the fossil fishes of this group of strata. But alas, on the 12th of February, he was called on to relinquish this and all other labors. He died at the ripe age of 68 years, but with faculties unimpaired, leaving us to regret that he could not have lived to continue his useful career, and yet giving us, in what he had done, cause to rejoice that he was permitted to work so long and so successfully in extending science and promoting the in- terests of mankind. Such is a slight notice of the scientific labors of Mr. Redfield. The esteem in which they are held is best proved by the honoi*- able rank to which they raised him among the cultivators of positive science. Of his character as a gentleman, whether in society, or presiding at a meeting of the American Association of Science, I would gladly speak were it in my power to depict the gentleness and modesty of his discourse, and that union of amiable and manly qualities which won the affection and respect of so many of his associates in scientific pursuits. But I must leave such a tribute to other and more competent hands, and will now bring my remarks to a close by asking the Society to adopt the following resolutions : — Resolved, That the late William C. Redfield, by his sagacity and patience in philosophical researches, and by the importance of the conclusions which he assisted in demonstrating, has re- flected honor upon the progressive science of our country, and earned a title to the lasting recollection of his scientific brethren, and, 191 Resolved, further, that, in recording this mark of our regard for his memory, we wouUl tender to his family and friends an expression of our deeply felt regret and sympathy. The resolutions were unanimously adopted. The Chairman announced that the next meeting would oe the regular Annual Meeting for the election of OtH- cers, and Reports of Curators, and other business. Dr. A. A. Gould, Mr. James M. Barnard, and Dr. J. B. S. Jackson were appointed a committee to nominate officers for the ensuing year. ANNUAL MEETING. May 6, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. The records of the last meeting and of the last annual meeting were read and approved. The Treasurer, Librarian, and the several Curators presented their Annual Reports, which were read and accepted. Messrs. James M. Barnard and Charles J. Sprague were appointed to audit the accounts of the Treasurer. The Committee appointed to nominate officers for the ensuing year, reported a list of candidates, and the report was accepted. The following gentlemen were duly elected officers, viz : — 192 President, Jeffries Wyman, M. D. Vice-Presidents, Chas. T. Jackson, M. D. D. H. Storer, M. D. Corresponding Secretary, Samuel L. Abbot, M. D. Recording Secretary, Benj. Shurtleff Shaw, M. D. Treasurer, Nathaniel B. Shurtleff, M. D. Librarian, Cliarles K. Dillaway. Curators, Thomas T. Bouve, Of Geology. John Bacon, M. D. Mineralogy. Charles J. Sprague, Botany. Tliomas M. Brewer, M. D. Oology. Henry Bryant, M. D. Ornithology. Thomas J. Whittemore, ConcJiology. J. Nelson Borland, M. D, Herpetology. Silas Durkee, M. D. Entomology. Nathaniel E. Atwood, Ichthyology. Theodore Lyman, Crustacea and Radiala. John Green, Comparative Anatomy. Cabinet Keeper, Charles Stodder. Dr. J. N. Borland presented the following list of Rep- tiles collected in California, by Mr. E. Samuels, viz: — 193 CHELONIANS. Family— Elodites. Ernys marmorata. Baird and Girard, Proc. Ac. Nat. Sci. Philad. Oct. 1852, vol. 6, p. 177. OPHIDIANS. Family— Crotalid^. Grotalus lucifer. Baird and Girard, Proc. Ac. Nat. Sci. Philad. Oct. 1852, vol. 6, p. 177. Family — Colubrid^. Eutainia ordinoides, B. & S. Cat, N. Am, Rep. Pt. 1. p. 33, 1853 Bascanion vetustus, do. do. do. do. 97, do. Gontia mitis, do. do. do. do. 110, do. Ophibolus Boylii, do. do, do. do. 82, do. IXadopMs amahilis, do. do. do. do. 113, do. Pituophis Wilkesii, do. do, do, do, 71, do. SAURIANS. Sub-family — Chalcidien. Gerrhonotus multicarinaius, Blainville, Nouv. Ann. du musee d'histoire naturelle, tome 4, 1835, PI. 25, fig. 2. Sub-family— Lepidosaurien. Plestiodon Skiltonianum, B. & G., Stansbury's Report to Con- gress of Exploring Expedition to Utah, p. 349, PI. 4, fig. 4-6. Sub-family — Eunotes. Sceloporus occidentalis, B. & G. Proc. Ac. Nat. Sci. Phil, vol. 6, p. 175, 1852. . BATRACHIANS. Sub-order— Anoures. Rana longipes described as nigricans, Hallowell, Proc. Ac, Nat. Sci. Phil. vol. 8, p. 96, 1854. Byla regilla, B. & G. Proc. Ac. Nat. Sci. P}iil. vol. 6, p. 174, 1852. PROCEEDINGS B. S. N. H. — VOL. VI- 13 jpLT, 1867. 194 Sub-order — Urodela. Taricha torosa, Gray, Cat. llept. in British Museum. Taricha larvis, H. & G. Proc. Ac. Nat. Sci. Phil. vol. 6, p. 302, 1853. Aneides liiguhris, B. & G. Proc. Ac. Nat. Sci. Phil. vol. 4, p. 126. Heredia Oregonensis, Ch. Girard, Proc. Acad. Nat. Sci. Phil, vol. 8, p. 235, 1856. Batrachoseps attenuata, S. F. Baird, Journ. Acad. Nat. Sci. Phil. vol. 1, p. 288, 1849. Amhystonia Calif ornica, Gray, Cat. Rept. in Brit, Mus. Dr. A. A. Gould, in behalf of the committee appointed to receive and report upon the Bequest of Professor Bai- ley, submitted the following report, which was accepted. » The Committee appointed to receive and report upon the Bequest of the late Prof. Bailey, have attended to their duty, and state the following results :— The examination of the Books, Drawings, and Correspondence was submitted to the Chairman — the Microscopical Collection to Dr. Bacon — the Algce and preparations of organic tissues to Dr. Durkee. In presenting the Report, the order in which the several be- quests are specified will be followed. I. The Microscopical Collectiox. Dr. Bacon's Re- port, (A.) The Microscopic Collection, which comprises the most valu- able portion of the specimens mounted for the microscope, is contained in twenty-four boxes in the shape of octavo volumes. Five of the boxes contain specimens of Diatoms, &c. from the Atlantic Soundings, including two boxes from Lieut. Berry- man's Soundings between America and Ireland in 1856. Three boxes contain specimens from Soundings in the Arctic pnd Pacific oceans. Gulf of Mexico, and Para River, &c. in S. America. In four boxes are American and Foreign Diatoms ; Diatoms in Guano ; and Fossil Polycistlns and Diatoms from Barbadoes. 195 In three boxes are Fossil Diatoms from Virginia and Mary- land ; Bermuda ; Monterey, California ; Suisun Bay, &c. Nearly all the specimens in the above boxes were mounted by Prof. Bailey ; and they are accompanied by manuscript cata- logues, or by memoranda on slips of paper, in which the posi- tions of more than three thousand individual objects on the slides are noted with reference to Bailey's Universal Indicator for Microscopes ; thus enabling the actual specimens described by him to be readily found and identified at any future time. A part of the Collection is also accompanied by an alphabetic cata- logue of species, with references to the slides on which speci- mens may be found. Two boxes contain recent and fossil Vegetable Tissues ; and two others Test Objects and miscellaneous Organic Bodies, and a micrometer scale on a glass slide. The number of glass slides in these twenty-one boxes is five hundred and fifty. In addition to the selected specimens in the Microscopic Col- lection, there are more than eight hundred specimens mounted on glass slides, comprising many duplicates of those in the Col' lection, and a variety of miscellaneous microscopic objects. There are also two hundred specimens of Polythalamia mounted as opake objects and labelled. These are not dupli^ cates of the Polythalamia in the Microscopic Collection, which are in Canada balsam. A very valuable portion of the bequest consists of the original specimens of microscopic material, collected by various scientific and exploring expeditions, and an extensive series of specimens received from European correspondents, including Ehrenberg and other distinguished microscopists. Among the miscellaneous objects are three microscopic daguer^ reotypes, seven photographs on paper, nineteen drawings of microscopic objects, and two micrometer scales on small slips of glass. II. The Alg^, &c. Dr. Durkee's Report, (B.) These are contained in thirty-two portfolios. They are from almost every part of the globe, They are arranged and named in a manner to afford great ^.ssistance to the student, \yho m^y 196 be interested in the study of Marine Botany. In most instances, specimens of the same kind, but collected at different seasons of the year, or brought from different localities, and presenting dif- ferent appearances to the naked eye, are phiced side by side, upon the same sheet or within the same envelope, so that the work of comparing one specimen with another, and of ascertain- ing the names of doubtful ones, which the student may possess, is rendered easy. And the fact, that very niany of the speci- mens are those originally described, and that nearly every plant in the collection has attached to it the name of some distinguished algologist, as Bailey, Harvey, Binder, or Jolit, stamps upon it an important value. It makes it a type specimen. Upon the cover of each volume is an index of what is con- tained within ; that is, a synopsis of the series, sub-series, order or family, to which the enclosed specimens belong ; and even the individual names of the plants are written on the outside. The family of Florideae are the most numerous, and embrace nearly one half of the whole collection. They are contained in fifteen portfolios. The Diatomaceae are in one volume, and amount to four hun- dred and twenty-five. The whole number in the collection is about four thousand five hundred. Of this number about two hundred varieties belong to the FloridetB, The Committee have not had time to enter into further par- ticulars respecting this magnificent collection of Algae. Its value is beyond all price. It raises the department of Marine Botany to a preeminent position in our Cabinet. We hazard nothing in saying that no collection of the kind in the country is equal to it, and but few in Europe superior to it. The animal tissues are contained in the boxes or Nos. marked 4, 5, 6. No. 4, contains the tissues of some of the Vertebrata. J^o. 5, the tissues of some of the Articulata. J^^o. 6, the tissues of some of the Mollusca and Radiata. The whole number in the three boxes is sixty-nine ; all in good order excepting one. The slide containing this specimen is broken. 197 III. The Books. The whole number of bound volumes is eight)'-four, besides one hundred and fifty unbound volumes and pamphlets, and these latter are not the least valuable portion of the Library, consisting as they do of important monographs, a form in which much that has been done in Algology and Mi- croscopy is as yet only to be found. Among the works are the splendid Microgeologie of Ehrenberg, the works of Kiitzing, Queckett, Ralfs, Hassall, Smith, Agardh, Harvey, Lindley, and Hutton. Indeed, nearly every thing of importance relating to his favorite studies is here ; and they are rendered additionally valuable by important notes of his own. IV. The volume containing rough sketches of microscopic forms and marked " Microscopic Memoranda," is a most interest- ing volume. It consists of letter-sheets of sketches made by means of the camera lucida, under the microscope, or of more finished drawings on glazed cards and arranged on sheets. At the end is an alphabetical catalogue of the several objects deline- ated. There are four hundred and fifty sheets, and seven hun- dred different objects named in the catalogue. Of most of these, numerous attitudes are given, so that the whole number of sketches is probably not less than three thousand, and they are high- ly valuable as an illustrative accompaniment to the microscopical collection. They are all characteristic and instructive, and many of them exquisitely done. They date as far back as 1838 — twenty years ago — and being chronologically arranged, afford a graphic diary of the train of Prof. Bailey's investigations, as well as of his own wanderings ; for wherever he went his micro- scope or his collecting boxes and bottles went with him. From Quebec to Florida we trace out all his abiding-places during his vacations. This collection is curious as it shows how he was gradually led into the study of microscopic organic forms. His first observa- tions were of vegetable structure — then we have an Echinorhyn- chus — the ovipositor of an ephemera, &c. In January, 1839, in examining some aquatic plants he perceived a curious body, the nature of which he could not make out ; it afterwards proved to be a Gomphonema. This excited his curiosity in that direction, and his sketches of common Diatomaceae soon became frequent. March 11, 1839, he sketched an organism which Ehrenberg sub- 198 sequently named Stauronema Bayleyi. In 1843, his observa- tions had become so numerous that, at the meeting of the Asso- ciation of Geologists and Naturalists in Boston, he communicated his paper entitled, " Sketch of the Infusoria of the family Bacil- larige, found recent or fossil in the United States," extending to fifty pages and illustrated by figures ; a paper which attracted much attention everywhere, and placed him at once in the high- est rank as an investigator of microscopic forms. The volume is also instructive in showing how much industry and enthusiasm — what a patient and gradual accumulation of numberless facts — how many trials, and doubts, and difficulties a man must always surmount in arriving at solid fame and true eminence. V. The Scientific Letters, which he submitted to the Society to retain such as might be deemed desirable for auto- graphs or otherwise, and destroy the remainder at discretion, your Committee have found very interesting, and consider that, with very few exceptions, they ought to be preserved. In addi- tion to every man of scientific note in this country, he numbered among his correspondents all the most noted Microscopists and Algologists in Europe, such as Ehrenberg, Kiitzing, Queckett, Harvey, Greville, Smith, Williamson, Ralfs, Agardh, De Bre- bisson, Montague, Le Normand, and very many others. Their letters contain many interesting facts and discussions, and even now many of them contain drawings and specimens as they were sent, and which the Committee think should be transferred to their appropriate places. The history of Microscopy and Micro- scopists in this country, can never be so well learned elsewhere as from these letters. Indeed, time always renders the corre- spondence of original investigators of curious interest and of real value. As an index of the varied acquirements and world- wide reputation of our departed benefactor, Ave think they should be preserved. The thousand and one inquiries which were made of him respecting Microscopes — the little packages sent him by hundreds from beginners that they might be named, " if it would not be taxing him too much," show how much of his time he must have sacrificed, as every man of mark in science is called upon to do, to good nature, and to tasks that were profitless and vexa- tious so far as his own advancement is concerned. 100 The Committee would recommend that a selection should be made of such as contain valuable scientific facts, and that these be arranged alphabetically and bound ; the remainder to be kept in bundles, as they now are. In conclusion, the Committee would congratulate the Society in having been made the recipients of scientific treasures so rich and so rare. It becomes us to insure their preservation, and to make them profitable. In bestowing them here, he no doubt expected a better use would be made of them here than else- where. He was of too practical a turn to be satisfied with mere storage. He anticipated that some one would take up the sub- ject where he left it, make himself familiar with the collection, be able to refer to the individual objects of it, and to answer such inquiries as other investigators might seek to have settled from it. What a glorious opportunity for one or more young men of leisure and scientific tastes. Every thing which has been collected in this country relating to the Algae and to Microscopic forms is here embodied, together with all the books necessary for the study and further pursuit of those branches. Whoever shall make himself master of them must be the ultimate authority for America, Such an opportunity for distinction even Ehrenberg never had. Who shall be the man ? We would not close without one word of tribute to the memory of our benefactor. We knew him to be a man of conscience, amiable in his whole character, and of the highest order among men of science. But the revision of his labors has tended to raise him still higher in our admiration. He is an eminent example of what may be accomplished by constant application, and of the confidence which one may inspire in his fellowr-men by unwavering truthfulness. In the very prime of life, with all the necessary outlays and appliances for extensive and rapid strides in knowledge, it seems too great a loss to be submissively acquiesced in. We cannot refrain from quoting, as expressive of our own estimate of his worth and position, from the letter of one who could appreciate him justly. " I had seen that you are President of the Montreal meeting (Association for Science) next year. I am sure every one acquaint- ed with what you have done for the advancement of science, American science and American scientific character, will say, that 200 no appointment at the present time could be more appropriate or just. My dear sir, I hope the great Disposer of events, whose minute works you have done so much to place before our eyes in all their exquisite beauty of form, of workmanship, and of adaptation, will give you yet many years to enjoy the honors you have so honestly acquired, and to add many more discoveries to those you have already secured." At the last meeting, no distinct Resolution having been passed touching one of the stipulations accompa- nying the bequest of Prof. Bailey, the following was offered and unanimously adopted. Resolved, That the sons of Prof. Bailey have access to the books and specimens bequeathed by him, and be allowed to use them at their own pleasure ; that they also have the same use of the library and cabinet of the Society as members ; and, that in consideration of his priceless contributions, their names be placed on the list of Patrons. Dr. A. A. Hayes read a paper upon the kind of sugar developed in the Sorghum saccharatum, or Chinese Sugar-Cane, as follows : — The introduction of this interesting plant has led to many somewhat extravagant suggestions, in relation to its future bear- ing on the agriculture and commerce of our country, particularly in relation to its produce of sugar. I have therefore deemed it a subject worthy of chemical observation and experiments, to determine its claims as a sugar producer ; and have also chosen it to illustrate a uniformity of vegetable secretion, according with well-known natural laws. In order to give scientific precision to the remarks which follow, it is neces- sary that a brief definition of the terra sugar, should be given. So rapidly has chemical science progressed of late, that this well-known terra has now become a generic name for a class of bodies, individually presenting us with the most marked diver- sities of sensible characters and composition. We have sugars which are sweet, others which are slightly sweet, and some desti- tute of sweetness : some are fermentable, others do not undergo this change : some are fluid, more are solid. 201 In connoctlon with the present subject, adopting cane sugar as the most important kind commercially, and as an article of food from certain inherent qualities, if we examine into its sources, we find them abundant, but not numerous. So far as observation has extended, its production by a plant is definite ; a change of locality, even when accompanied by a marked change in the habit of the plant, does not alter essentially the nature of the sugar it produces. Thus the cane of Louisiana rarely matures and is an annual, while in the soil and climate of Cuba, it enjoys a life of thirty, or even sixty years. The juice of our southern plant always contains more soluble alkaline and earthy salts than is found in the cane of Cuba, but its sugar is secreted as cane sugar. The juice of the sugar beet, of watermelons, and a large number of tropical fruits, the sap of the maple and date palm, afford cane sugar. In these juices and saps, when concentrated by desicca- tion in the cells of the plants, it always appeai-s in regular, bril- liant crystals, of a prismatic form, clear and colorless ; distinctly indicating a vital force in the plant, separating it from other proximate principles and leaving it in its assigned place pure. The class of sugars next in importance, includes under the gen- eral term Glucose, a number of sugars having varied characters, which should be separately grouped. Among them are the sugars of fruits, seeds, and grasses : those produced in the ani- mal system, and the artificial sugars made from starch, grains, and sawdust. The varieties of glucose are both solid and semi- fluid. When solid they present aggregates of sub-crystalline form, in which the organic tendency to rounded surfaces, is gen- erally seen. The semifluid forms often manifest a disposition to become solid on exposure to air, and they then experience a molecular change, which produces crystals having new relations to polarized light and different physical and chemical characters. It is unnecessary to enter more minutely at this time, into a description of each variety of glucose, for the individuals of the class are easily distinguished from each other, and most clearly and remarkably from cane sugar. The plants producing the natural glucose sugars, mature their cells as perfectly as those producing cane sugar, and the secretion can be found as distinctly isolated from other principles as cane sugar is ; even when the glucose is semifluid. Hence we are able to determine by micro- 202 scopical observations, fiidetl by chemical tests, the presence and kind of sugar in the tissues, or sap of a plant, often without in- curring the risk of change of properties through the chemical means adopted for withdrawing the sugar. AVe have the authority of our associate, Mr. Sprague, for the conclusion, that the Sorghum vulgare, or saccharatum, belongs to the tribe including grasses, and we should therefore expect to find its saccharine matter the variety of glucose called sugar of grasses or fruit sugar. The unsuccessful attempts made to crys- tallize sugar from the juice of the Sorghum, produced in different cHmates of our country last year, indicated that it contained no cane sugar, or that the presence of some detrimental matter in the expressed juice, destroyed the crystallizable character of cane sugar, as can be artificially done. My observations com- menced after I had obtained several specimens of the Sorghum, and have been continued on the semifluid sugar, likewise from different parts of the United States, with uniform results. When a recent shaving of the partially dried pith of the matured stalks of the Sorghum, is examined by the microscope, we observe the sugar cells filled with semifluid sugar. After exposure to air it is often possible to distinguish some crystalline forms in the fluid sugar. These grains, after being washed, cease to present a clear crystalline character, and have the hard- ness and general appearance, of dry fruit sugar. By withdraw- ing the sugar without the aid of water, it is possible to obtain it colorless and neutral, as a semifluid glucose or fruit sugar, and no traces of crystals or crystalline forms can be seen. The glu- cose thus obtained, freely exposed to air, soon undergoes the molecular change which is exhibited by sugar of grapes, and we thus observe another character associating the whole product, with the sugar of grasses and fruits. Leaving the physical observations, and substituting the more exact processes of the laboratory, I found that the semifluid sugar of the Sorghum did not blacken in sulphuric acid, but was sensitive to the action of alkalies, and reduced the alkaline solution of tartrate of copper, thus conforming to the well-known characters of glucose. The most careful trials I could make, failed in detecting cane sugar in any samples of the Sorghum stalks, or in the samples of sugar, including one made by Col. Peters in Georgia, prepared under 203 the most careful management. I must therefore conclude, that the Sorghum cultivated in this country does not secrete cane sugar or true sugar ; its saccharine matter being purely glucose in a semifluid form. As a matter of science this result is interesting, in showing the integrity of character pertaining to the genus in which this plant is botanically placed ; the sweet grasses yielding fruit sugar, while the maize produces cane sugar only. In its economical bearings we might wish that the sorghum secreted cane sugar, for the values of cane sugar and glucose are very different. From the best authorities we learn that the power of imparting sweetness in cane sugar, is between two and one half and three times as great as that of dry glucose, and the semifluid sugar of the Sorghum containing water, nearly four pounds of this will be required, to equal one pound of sugar in ordinary use. As a raw material for the production of spirit, for which it seems well adapted, the glucose of the Sorghum may prove valuable, and as an addition to a forage crop, the plant may be found to possess a high agricultural importance. Dr. John Bacon made a statement confirmatory of the results arrived at by Dr. Hayes. He was unable to obtain any crystals of cane sugar. The Chairman, Dr. Jackson, said he had obtained crystals by evaporation of the syrup over sulphuric acid : "whether they were of cane or grape sugar he could not say. Cane sugar had been found in the plant by Euro- pean chemists. He had made extensive investigations into its chemical properties and economic value, for the United States Government, which would be published in the Patent-Office Report. Mr. N. H. Bishop exhibited some of the seed of the Chinese Sugar-cane, and remarked that it was imported from France and not China, as might be supposed. It was estimated by seedsmen that ten tons would be sold in Boston this season for planting, and that one pound would plant an acre. 204 Mr. N. H. Bishop presented a male and a female Bur- rowing Owl, [Athene cunicularia,) from South America, and read the following paper upon this bird : — THE BURROWING OWL OF SOUTH AMERICA. (Athene cunicularia. Molina.) I first met with this bird on the banks of the River San Juan, in the Banda Oriental, one hundred and twenty miles west of Monte- video, where a few pairs were observed devouring mice and insects during the daytime. From the river, travelling westward thirty miles, I did not meet a single individual, but after crossing the Las Vacas, and coming upon a sandy waste covered with scattered trees and low bushes, I again met with several. Upon the pampas of the Argentine Republic they are found in great numbers, from a fevv miles west of Rosario, on the Parana, Lit. 32 deg. 56 min. south, to the vicinity of San Luis, where the pampas end and a travesia or saline desert commences. On these immense plains of grass it lives in company with the bizcacha, (Lagostomics trichodactylus, Brookes,) an animal that bears resemblance to the rabbit and agouti, and undermines a great extent of country with its burrows. The habits of this owl are said to be the same as those of the species that inhabits the holes of the marmots upon the prairies of western North America, and one writer speaking of the latter bird remarks, " We have no evidence that the owl and marmot habitually resort to one burrow ; " and Say adds, " that they were either common though unfriendly residents of the same habitation, or that our owl was the sole occupant of a burrow acquired by the right of con- quest." Li this respect they differ from their South American relatives, who live in perfect harmony with the bizcacha, and during the day while the latter is sleeping, a pair of these birds stand a fevv inches within the main entrance of the burrow, and at the first sound, be it near or distant, they leave their station and remain outside of the hole, or upon the mound that forms the roof of the domicile. When man approaches, both birds mount above him in the air and keep up the alarm note, with irides dilated, until he passes, when they quietly settle down in the grass, or return to their former place. 205 While on the pampas I did not observe these birds taking prey during the daytime, but at sunset the bizcachas and owls leave their holes and search for food, the young of the former playing about the birds, as they alighted near them. They do not asso- ciate in companies, there being but one pair to each hole, and at night do not stray far from their homes. In speaking of the North American burrowing owl, a writer says that the species suddenly disappears in the early part of August, and also that it is strictly diurnal. The Athene cunicn- laria has not these habits ; it does not disappear during any part of the year, and it is both diurnal and nocturnal, for though I did not observe it preying by day on the pampas, I noticed that it fed at all hours of the day and night on the north shore of the Plata, in the Banda Oriental. At long. 66 degs. west, our caravan struck the great saline desert that stretches to the Andes, and during fourteen days' travel on foot, I did not see a dozen of these birds. While resid- inff outside the town of San Juan, at the eastern base of the Andes, I had an opportunity to watch their habits in a locality differing materially from the pampas. The months of September and October are the conjugal ones, and during the middle of the former month I obtained a male bird with a broken wing. It lived in confinement two days, refusing to eat, and died from the effects of the wound. A few days later a boy brought me a female owl, with five eggs, that had been taken from her nest, five feet from the mouth of a burrow that wound among the roots of a tree. The female bird was fierce in her cage, and fought with her wings and beak, uttering all the while a shrill prolonged note, resembling the sound pro- duced by drawing a file across the teeth of a saw. I supplied her with eleven full-grown mice, which were devoured during the first thirty-six hours of confinement. My object was to discover if this bird burrowed its own habita- tion, and my observations of eight months failed to imj^ress me with that belief. I have conversed with intelligent persons who have been famihar with their habits, and never did I meet one that beheved this bird to be its own workman. It places a small nest of feathers at the end of some deserted or inhabited burrow, as necessity demands, in which are deposited from two to five white 206 eggs, little larger than the domestic pigeon's. In the Banda Oriental, where the country is as fine, and the favorite food of the owl more plentifully distributed than upon the pampas, this bird is not common compared with the latter locality. The reason is obvious. The bizcacha does not exist in the Banda Oriental, and consequently these birds have a poor chance for finding habitations. On the pampas, where thousands upon thousands of bizcachas undermine the soil, there, in their true locality, the traveller finds thousands of owls. Again, along the bases of the Andes, w^here the bizcacha is rarely met with, we find only a few pairs. Does the hole from which this specimen w^as obtained, dug among the roots of a tree, appear to be the w^ork of a bird or quadruped ? The several works that I have consulted do not in one instance give personal observations relative to the burrowing propensities of this owl, from which fact it will be inferred that it never has been caught in the act of burrowing. Dr. Hayes presented, in the name of R. H. Eddy, Esq., some specimens of Native Borate of Lime from South America. They varied in size, were of a dirty appear- ance externally, but internally beautifully white and silky, and exhibited a tendency to crystallization. The thanks of the Society were voted for the gift. It was voted that during the summer months the meetings should commence at 8 o'clock P. M. May 20, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. In the absence of the Secretary, Mr. C. C. Sheafe was chosen Secretary pro. tem. Dr. Silas Durkee read a paper on the method by which the 207 common Earth Worm (Lumhricus terrestris) finds its way into vessels, such as tubs, barrels, pails, &c., and about the eaves and gutters of houses and sheds, which subject has occasionally been a topic of discussion at the meetings of this Society. It is well known that after a shower of rain, upon a warm summer's day, the lumbricus is frequently found in the places above named ; but by what means they arrive there is the ques- tion. Dr. Durkee had recently had an opportunity of watching some earth worms which were placed in glass jars standing in his office. At first there was a small quantity of water in the bottom of the jar, which seemed to prevent them from ascending any great distance ; but upon removing this they were repeatedly seen mounting along the sides of the vessel. The progression was at a more moderate rate, and by shorter strides or stages, when they attempted to climb in a vertical direction, than when their course was more inclined. In some instances they reached the top of the vessel, a distance of eighteen inches in eight min- utes. Generally their wanderings were quite irregular and cii'- cuitous, and they continued on the sides of the glass sometimes for the space of two hours, a part of the time in motion and a part of the time at rest. The worms drag themselves along by a few of their segments at a time, and the number of segments in motion at any one moment is less in their ascending course than when a horizontal or downward direction is taken. The abundant glu- tinous secretion with which they are' covered, together with their numerous seta? and segments, seems well adapted to aid them in their various motions. The following paper on the Zonda Wind, was read by Mr. N. H. Bishop :— At a former meeting of the Society, I offered some remarks relative to this peculiar wind. (See Proceedings, vol. vi. p. 126.) I now request the favor of ofi^ering some additional observa- tions upon this peculiar wind. In searching through the works of the very few authors who have visited the interior of the Argen- tine States, (all but one or two of whom are Europeans,) I find that one only mentions the existence of the above phenomenon, 208 and he did not probably visit the town where my observations were made, which locahty is considered by the natives the north- ern limit of the zondas. John Mier.s, author of an interesting work on the provinces o^ La Plata and Chili, remained a short time in Mendoza, a town nearly one hundred and fifty miles south of San Juan, and capi- tal of the province of Mendoza. He states that this southern locality is annoyed by winds that blow during the summer months from the valley of Zonda, and notes the fact that two dark clouds came from the northwest and hovered over the town during the greater part of the night, and in the morning everything exposed to the air was covered with fine sand, which was of a light-gray color, and slightly magnetic. It was Miers's opinion that " a souffriere, or active volcano," existed to the northward of San Juan, from which the hurricanes and showers of sand originated. Had Mr. Miers visited San Juan, his view of the position of the souffriere, or volcano, would undoubtedly have been changed ; for though the zondas sometimes reach Mendoza to the south, the direction of the wind when it strikes that place, differs from the line it follows when it rushes with violence upon the northern town. At San Juan, it comes due west from the Andes ; hence the starling-point of the zonda cannot be to the north of the town, as Miers conjectured. According to the account of the natives, the zonda of San Juan does not cover a broader space than ten or fifteen miles after it leaves the Sierra of Zonda. Taking this into consideration, in connection with Miers's state- ment that the Mendoza zonda comes from the northwest, differ- ing as it will be seen four points from the northern town, we may infer that the Mendoza and San Juan zondas do not blow at the same time. If this be true, it is an interesting fact, showing that this peculiar wind does not always follow the same track. I remained but a short time in Mendoza, and not being conver- sant with the language of the inhabitants at that time, could not have collected information relative to the zonda, as it affects that locality, even had I then been aware of its existence. Miers states that these are summer winds in Mendoza. From personal observation and reliable accounts of educated San Juan- inos, I found that they are more particularly the winter winds — at least they are more frequent during that season. Invalids 209 suffering from pulmonary diseases, and complaints aflf'eeting the heart and liver, anticii):ite the month of August (midwinter) with consternation; and their anxiety is not quieted until they have passed through the dreaded ordeal. While passing the winter in San Juan, I noted the courses of upwards of twenty zondas. Some were of short duration ; others lasted eighteen or twenty hours. During the latter part of August, 1855, while standing upon the saline desert, a few miles east of San Juan, my attention was attracted to a cloud of dust that appeared to roll through the air as it appi'oached me. I started for a sheltez", and had hardly reached it, when the zonda swept past, filling the air with fine yellow sand. The temperature of the previously sultry atmos- phere suddenly rose many degrees, and the occupants of the neighboring huts were affected with severe headaches. 1 noted with a compass the course of the wind, and found it to be west. All night, and through the following day and night, it continued blowing with undiminished force. Each hour the vane beside the hut was consulted, and the same course as at first was always observed. A few hours before the wind ceased the sand showers were exhausted. The greatest heat was during the first few hours : and this is always the case, whether the zonda commences during the daytime or night. After continuing for thirty-six hours, the change came. It was instantaneous. The hot wind seemed cut off at right angles by a cold wind from the south. The change could not have occu- pied more than forty seconds. The south wind lasted twenty hours, and was as violent as the hot zonda. In speaking of the Mendoza zondas, Miers does not mention the succession of the south wind. It is easy to comprehend that after so large a space has become filled with heated air, the effect will be felt in the cooler regions of the south, and a strong current from that direction will rush in to restore the atmospheric equilibrium. Hence the cause of the south wind succeeding the zonda. Miers believed that the origin of the zondas was volcanic, and for a precedent, I will state, upon the authority of Sir Woodbine Parish, that the volcano Penquenes, which is situated about one hundred miles southwest from Mendoza, and reaches an altitude of nearly fifteen thousand feet above the level of the PROCEEDINGS B. S. N. H. — VOL. VI. 14 AUGUST, 1857. 210 sea, emits clouds of ashes and pumice-dust. This dust is carried by the winds as far as Mendoza, but these clouds do not strike the town with the force of a San Juan zonda. The pumice- dust is borne along by variable winds. From this fact we may infer that the fine sand of the zondas comes from a similar source. The most important question is, " Where originates the hot and parching wind that always accompanies, and is peculiar to the zondas ? " The old guides, who are familiar with the valleys of the Andes, inform me that these winds blow from off the main snow-clad ridge of that great chain of mountains, and express their surprise at the fact, " that from a cold region comes a burn- ing wind." Strong and steady winds generally follow a direct line. This fact is peculiar to the zondas. If Miers's conjecture be true re- garding the origin of these winds, the position of the volcano or souffriere might be found by obsei'ving the following suggestion, bearing in mind that the Mendoza wind comes from the north- west, and the San Juan zonda from the west. That point where two lines — one running west from the northern town, the other northwest from the southern town — will intersect, is the starting- point of the sand clouds, if not of the accompanying hot wind. Looking upon the map of South America, we find in the Cor- dillera of the Andes, between the latitudes of San Juan and Men- doza, four peaks marked as doubtful volcanoes, — Limari, directly west of San Juan ; Chuapu, thirty miles further south ; and near the half-way point of the two towns, Ligua. To the north of west of Mendoza, stands prominent the lofty Aconcagua, that has been estimated by two English captains to have an elevation of 23,900 feet. The point of intersection of the west and north- west zonda lines is in the vicinity of Limari and Chuapu, and if not either of these, the zonda volcano is a near neighbor to them. Mr. Sprague exhibited specimens of a fungus which he had found upon young pear-trees, (Capnodium elong-a- tum,) and which had been recently found in great quan- tities on the stenns and leaves of young white pines grow- ing in Hingham, by Mr. T. T. Bouve. He also exhibited a drawing of the plant, showing the different forms of the peridia, some being merely rounded half-spheres, 211 while others had extended themselves into elongated and forked points. This fungus does not form in the tissues of the plants upon which it is parasitic, but is merely an incrusting growth, spreading over and entirely covering the surface of the stem and leaf. This compact envelope is highly injurious to the infested plant, as it prevents the access of air and light to its tissues. On removing a portion from the pine leaves, the normal green was found to have changed to a dull yellow, similar to that of the decaying leaves. Dr. A. A. Hayes exhibited some specimens, resembling Trachyte rock so closely, that most observers would have mistaken them for Trachyte. The specimens consisted of hand specimens, having the uneven fracture of trachyte, full of capillary passages, with some cavities ; there were fractured planes of brown and flesh-colored minerals, resembling feldspar, and some small red, brown-colored and black granules ; but the most characteristic mark was the occurrence of angular fragments and grains of yellowish green color, hardly distinguishable from epidote by the eye. The external surface was brown and uneven, like that of a weathered basalt, or trap. The island from which these specimens came has been examined by a geologist, and from the prevalence of this rock, it is said that he pronounced the island to be of volcanic origin. A mass was sent to Dr. Hayes, and he found it had structural planes, the divisions producing trapezoidal masses, their surfaces and the lines marked by darker colors, and, so far as could be determined, there was evidence of the mass being part of a rock formation of some extent. The chemical composition discloses the remarkable fact that this rock is composed essentially of fish bones and altered shells, which have passed through the alimentary canals of sea fowls. Referring to communications before made, Dr. Hayes stated that the organic matter of fish bones in the droppings of fowl, reacts on the bone phosphate of lime, to eliminate acid salts of phos- phoric acid, and these cement other portions, or decompose shells, which are cornposed of carbonate of lime and animal tissues. 212 The feldspar-like granules are generally compact, colored por- tions of converted shells, having a crystalline form, and there are aggregates of ferruginous and aluminous phosphates, arising from the same kind of action on ferruginous matter, which, in the form of a tine clay, or volcanic ash, has been brought within the sphere of the action of the acid phosphates. The cavities some- times present minute crystalline facets of phosphate of lime crystals, while the capillary channels and pores, which give the trachyte-like character, are really the passages through which the carbonic acid and other gases escaped, during the transformation of the organic matter, precisely as they occur in basalt and trap, where igneous action has been supposed to have been influential. This rock is covered more or less by Atlantic guano rock, presenting the variety which consists of compact, light-colored phosphate of lime, containing about twenty parts in one hundred of carbonate of lime, and in some parts is a consolidated shell- bank ; the recent shells and coral fragments being visible. Where, through time and favorable exposure, the bone remains have thoroughly decomposed the shells, hand specimens would be mistaken for the flesh-colored, massive phosphate of lime of New Jersey. These more or less well-cemented and altered rocks are also connected with still more recent deposits, retaining even the odorous animal remains of oily acids ; and the whole formation, above that of the trachytic form of rock, contains the remains of infusoria. Thus a small island of the Atlantic, lying about eighteen degrees north of the equator, presents us with an epitomized succession of rock strata, formed from materials which, once endowed with life, have served to nourish other living systems, and then given rise to chemical changes, resulting in the produc- tion of various mineral solids which remain. The trachyte-like rock forming the basis rock of this island, theoretically, may have received its geological and chemical characters in ocean water. A subsidence of the land, after its surface had been deeply covered with organic remains, would allow of that aqueous action of decomposition and cementation which we notice, and the subsequent desiccation would explain the natural divisions by rents. The formation of silicates of iron, manganese, and alumina from phosphates of lime, is a mineral- 213 izing process which can take phice in ocean water by infiltration, volcanic ashes, or divided materials of plastic rocks being present, as analysis shows them to be. The rock is hydrous, losing nearly ten per cent, of its weight by ignition, or Water with a little organic matter - - - - 10.00 Bone Phosphate of Lime, - 85.20 Carbonate of Lime, 3.00 Oxides L'on, Manganese and Alumina, - - - 5.22 Silicic Acid and Sand, 1.78 105.20 The excess of weight being due to the estimation of the phos- phoric acid united to lime as bone phosphate of lime, while truly part of it, with a portion of silica, is united to the oxides present. Dr. John Bacon exhibited some Calculi, six or seven hundred in number, taken from the bladder of an ox. They were amorphous, presenting no crystalline forma- tion, and containing only a small quantity of organic matter. This is one of the rarest forms of urinary stones. On motion of Mr. Charles Stodder, it was voted to appoint a Committee to take into consideration and report upon the subject of establishing a Microscopic Department of the Society. Messrs. Durkee, Jackson, Bacon, Shaw, Sprague, An- drews, and Barnard, were appointed this Committee. George Duncan Gibb, M. D., of London, was elected a Corresponding Member. 214 June 3, 1857, Prof. Wm. B. Rogers, in the Chair. DEPARTMENT OF MICROSCOPY. The following report was read and adopted : — The Committee to whom was referred the subject of establish- ing a new department for the investigation of microscopic nature, beg leave to oifer as a report the following Preamble and Reso- lutions. Whereas, The recent acquisition of the invaluable cabinet and library of the late Professor Bailey has awakened the Society to the necessity of giving a new impetus to the progress of micro- scopic science ; to the great usefulness which a special depart- ment for the development, record, and publication of observations on the minute structure of organic and inorganic bodies, would possess : Resolved, That this Society do hereby establish a department for microscopic investigation to be known as the DEPARTMENT OF MICROSCOPY ; to consist of members of the Society, specially interested in micro- scopic studies, who may desire to join it. No individuals, who are not members of this Society, shall be members of this depart- ment. Resolved, That a Curator of this department shall be chosen yearly at the Annual Meeting, whose duty shall be to take charge of all specimens and preparations belonging to the depax't- ment, and to preside at its meetings. The department may appoint sub-committees upon the different branches of the sci- ence, to whom shall be referred specimens for examination and report. The Recording Secretary of the Society shall be, ex officio, Secretary of this department. Resolved, That at the first regular meeting of the Society in each month, at the hour of nine o'clock, the presiding officer shall 215 call for microscopic reports, papers, remarks, or exhibitions, in the order here named ; and such reports, papers, remarks, or exhi- bitions shall be in order during the continuance of the meeting, provided that no business matter properly belonging to the Annual Meeting of the Society shall be thus superseded at the regular or adjourned Annual Meetings. Resolved, That this department shall have the use of the Library Room of the Society for its meetings when desired. Resolved, That the proceedings of this department shall be published in the Journal and Proceedings of this Society, subject to the decision of the Publishing Committee of the Society. A Committee, appointed to nominate a candidate for the office of Curator of the Department of Microscopy, reported the name of Dr. Silas Durkee, and he was accordingly chosen Curator of the Department. Prof. John Bacon exhibited a package of Bailey's Universal Indicators, received from Mr. Gavitt, of Al- bany, and intended for the use of the Society. Observers, making use of Prof. Bailey's mounted specimens, and being in possession of one of these indicators, may easily find any special object upon the slide which had been referred to or described by Prof. B. Mr. C. J. Sprague announced the Donation by Benja- min D. Greene, Esq., the first President of the Society, of his very extensive and valuable Herbarium. A Com- mittee, consisting of Messrs. Sprague and Durkee, was appointed to draw up a series of resolutions, expressive of the gratitude of the Society for the donation, and of its proper estimation of its value. The Curator of Crustacea and Radiata, Mr. Theodore Lyman, was empowered to loan Mr. Bowerbank of London, certain specimens of sponges, to aid him in the publication of a work upon this subject. 216 The Corresponding Secretary read the following list of letters recently received : — Elliott Society of Natural History, Charleston, S. C. ; Ethno- logical Society, London, January 31, 1857 ; K. Bayerische Akademie der Wissenschaften, February 4, 1857 ; Imperial Mineralogical Society of St. Petersbui-g, November 30, 1856; Verein fur Vaterlandische Naturkunde in Wurtemberg, January 20, 1857 ; Accademia, &c., di Bologna, May 29, 1856 ; Royal Geographical Society, London, November 29, 1856, acknowledg- ing the receipt of the Society's publications ; also from the last five above-named institutions, presenting various publications, as well as from the Naturforschende Gesellschaft zu Elmden, October 2, 1856. Messrs. Archelaus Wilson of Boston, and R. H. Barn- well of the Scientific School, were elected Resident Members. June 17, 1857. Dr. D. H. Storer, Vice-President, in the Chair. The Committee appointed to prepare Resolutions, expressive of the sentiments of the Society in recognition of the donation by Benjamin D.^ Greene, Esq., of his Botanical Collection, submitted the following, which were unanimously adopted : — Resolved, That this Society is deeply sensible of the active sympathy which has ever been exhibited in its welfare by its first President, Benjamin D. Greene, Esq., — -a sympathy which has led him to bestow upon the Society his extensive and valu- able Herbarium, the fruit of a long lifetime devoted to the culti- vation of botanical science, to a diligent accumulation of the 217 world's vegetable productions, and a critical study of our native flora, which his own frequent discoveries have enriched. Resolved, That the proffer of this rare collection of plants is gratefully and cordially accepted ; and the Corresponding Secre- tary is instructed to inform Mr. Greene of this acceptance, trans- mitting a copy of these resolutions. Mr. Sprague stated that the Herbarium is particu- larly rich in specimens collected by various Exploring Expeditions, both of this country and of Europe ; reports of some of which have not as yet been published. Very many of the plants are new to the Society's cabinet, and the collection altogether is very extensive and exceed- ingly valuable. Prof. Wm. B. Rogers made some remarks upon a peculiar geological condition which he had noticed in the Slate Rocks of Governor's Island, in Boston Harbor, and of which he had never seen any notice. At the landing near the fort, where the slate is exposed, he had observed a series of ledges of dark grayish-blue slate, in which is exposed a species o? fault known as horizontal heave. There are two lines of direction in the beds, and these are at right angles with each other. This phenomenon of horizontal heave, combined with the system of cross cleavage which is at right angles with the planes of bedding, creates some obscurity in some spots as to which are the original planes of bedding. In other localities, and especially in the Quincy and Braintree siliceous slate in which trilobites have been recently found, the same difficulty exists ; rendering it impracticable to obtain perfect specimens of that fossil in any amount, since the rock splits off in an opposite direction to that in which the animal was de- posited. This system of horizontal heave has been extensively studied in Europe, and has elicited much discussion from geologists and physicists upon the theory of the phenomena engaged in its pro- duction. It is supposed that a great pressure has been applied to the rocky mass, either before or after it had reached a com- 218 plete state of solidity, and that this pressure has produced such a structural arrangement as to develop particular planes of cleav- age where the adhesion was the slightest. This supposition has been sustained by experiment, recently instituted in England, in which it has been demonstrated that scales of mica and other material of flattened form, intermingled with plastic clay and sub- mitted to continuous and energetic pressure, assume approximate parallelism, and impart to the mass a laminar structure. Where cleavage shows itself in limestone containing mica scales and flattened particles of silica, the microscope has detected an ap- proximate degree of parallelism between these substances and the cleavage planes. Dr. S. Ivneeland, Jr., exhibited two specimens of Siredon, taken in Portage Lake, Michigan, which were described by him in the Proceedings of February, 1857, and which he had suc- ceeded in keeping alive. These animals are very hardy, the water in which they were contained having been frozen and thawed many times in succession during the last winter, when their only food was such minute matter as they might have found in the lake water. They have maxillary and palatal teetli, and though they are very much feared by the Indians, on account of the supposed poisonous nature of their bite, yet Dr. Kneeland has not known them to attack each other ; and he himself handles them very freely, without any attempt of the animal to bite. The heads of the two specimens are of different shape, and possibly they are of different sexes. Since they have been in Boston, they have been fed upon live worms by Dr. Durkee, of which they will consume several every day. Near the gills upon the surface of the body are a number of parasitic worms, rough dx'awings of which were exhibited by Dr. Durkee. Dr. H. R. Storer said he had been informed that an Albino of the Common Striped Squirrel of Massachu- setts {Sciurus striatus) had been taken at South Fram- ingham. It was perfectly white, with pink eyes, and a note like that of the common striped squirrel. The Secretary, at the request of Dr. T. M. Brewer, 219 exhibited specimens of a Gum from California, which was said to resemble in its properties Gum Arabic, and of a bark which was stated to have the mucilaginous charac- ter of Slippery Elm Bark. The specimens were samples of some presented to the California Society of Natural History by Dr. Thomas Payne, of Mariposa, Cal., and forwarded to Dr. Brewer by Dr. Holden ; they were re- ferred to Dr. Hayes for analysis. Mr. Thomas Hollis (after a moment's examination of it) stated that the bark bore considerable resemblance to the Wild Cherry Bark. It had a similar odor, but it was not so astringent. The mucilage from this is not imme- diately extracted in the mouth, but, as is the case with the Wild Cherry Bark, it may be developed after some hours maceration in cold water. The wild cherry like- wise exudes a gum similar to this. Dr. A. A. Gould presented, in the name of William M. Bailey, Esq., of Providence, a Photograph of his brother, the late Prof. Bailey of West Point. The thanks of the Society were voted for the gift. Messrs. Theodore Metcalf, George N. Davis, and Thomas D. Morris were elected Resident Members. ADDITIONS TO THE MUSEUM. April 15, 1857. Bequest of the late Prof. Jacob W. Bailey, consisting of his complete Microscopical Collection, Algse, &c., an inventory of which will be found in the Report of the Committee on page 194. A collection of Shells, Crustacea, and Corals ; presented by N. E. Atwood. A Trumpet Fish ( Centriscus scolopax) ; by Dr. D. H. Storer, the first known to have been taken on this coast. A collection of Algse; by J. C. Parkinson. A Double-collared Arracari {Ptero- gbssusbitm^quatus); a Field Yaxe.(Turdtis jiilaris); &.y^ oodiXaxk (Anthus arboreus); by Dr. F. J. Bumstead. AHobm (Turdus migratorius)-^ by E. Samuels. A speci men of Dipsas plicata, from the East Indies, with images encrusted by the nacre upon its internal surface; by Lieut. G. H. Preble, U. S. Navy; a Female Snow- Goose and a Shoveller Duck from Virginia; by Wm. Sohier. A Song Sparrow and a Robin; by E. Samuels. 220 May 20. Burrowing Owls (Athene cunicularia) male and female, from South America; by N. H. Bishop. Native Borate of Lime from South America; by R- H, Eddy. Fossils and Acorns; by Theodore Parker. Vitreous Copper Ore from South Carolina; by Di-. C. T. Jackson. Saw of a Saw Fish; by Geo. S. Wheel- wright. June 3. The extensive and valuable Herbarium of Benjamin D. Greene, Esq., the first President of the Society. Shells and Crustacea .from Hiltonhead, S. C. ; by J. S. P'ay, Esq. Sponges from Singapore, and Corals; by S. Durkee. Cast of the Brain of Spurzheim ; by Theodore Pax'ker. June 17. A Photograph of the late Prof. J. W. Bailey, presented by his brother W. M. Bailey, Esq., of Providence; Arvicola misterus, two specimens,^, riparius, Eesperomys Bairdii, Vireo soUtarius, Trichas PhiladeljMca, Vermivora chryso2}iera, V. peregrina, Rallus elegans, and a collection of Shells, all from lUinois ; by Thomas Kennicott. BOOKS RECEIVED DURING THE QUARTER ENDING JUNE 30, 1857. Description of New Fossil Crinoidea from the Palaeozoic Rocks of Western and Southern Portions of the United States. By B. F. Shumard, M. D. 8vo. Pamph. Philadelphia, 1857. Fi-om the Author. Synopsis Avium Tanagrinarum. By P. L. Sclater. 8vo. Pamph. Loudon. From the Author. Archiv fiir Naturgeschichte, gegiiindet von A. F. A. Wiegmann. Fortgesetzt von W. F. Erichson. Sechstes Heft pp. 1-486. 8vo. 3 nos. Berlin, 1855. From Br. F. H. Froschel. Annual Report of tbe Trustees of the New York State Library. 8vo. Pamph. Albany, 1457. Fi-om the Trustees. Seventeenth Annual Report of the Regents of the University of New York. 8vo. Pamph. Albany, 1857. From the Regents. Fourth Annual Report of the Secretary of the Massachusetts Board of Agri- culture. 8vo. Boston, 1857. From J. L. Flinty Esq., Secretary. Report of the Commissioners on tbe Artificial Propagation of Fish. Massa- chusetts Legislative Document. 8vo. Pamph. Boston, 1857. From N. E. At- wood, Esq. Proceedings of the American Association for the Advancement of Science. Tenth Meeting, Albany, N. Y., 1856. 8vo. Pamph. Cambridge. From the Association. Laws of Structure of the more disturbed Zones of the Earth's Crust. By Prof. H. D. Rogers. 4to. Pampb. Edinburgh, 1856. Geology and Physical Geography of North America. By the same. 8vo. Pamph. London, 1856. Edinburgh New Philosophical Journal. New Series. Nos. 6, 8, 9. 8vo. 1856-7. From Prof. H. D. Rogers. Rapport special sur les mesures qui ont (ii& adopts pour I'Etablissement d' une Ecole Nonnale. 12mo. Pamph. Montreal, 1847. 221 Regies et Reglements de I'Asseinbl^e Legislative. 18rao. Pampli. Toronto, 1856. Listes des Rapports ou Etats de la Legislature du Canada. Long 4to. Pamph. Toronto, 1856. Assemblde Legislative, 1856, Liste des Lois Expirantes. 4to. Pamph. Toronto. Sommaires des Deliberations de I'Assembl^e Legislative du Canada. Long 4to. Pamph. Toronto, 1856. Journal du Cultivateur et Proced^s du Bureau d' Agriculture du Bas-Canada. Vol. in. Nos. 1-12, and Vol. IV. Nos. 1-8. 4to. Pamph. Montreal, 1856. Journal de ITnstruction Publique. Vol. I. No. 3. 4to. Pamph. Montreal, 1857. Farmers Journal. 4to. Pamph. Vol. IV. No. 12. Montreal, 1857. Second Rapport sur I'Exploration des Lacs Sup(5rieur et Huron. Par le Compte de Rottermund. 8vo. Pamph. Toronto, 1857. Tables of Trade and Navigation of Canada for 1856. 8vo. Pamph. Toronto, 1857. Reports of Commissioners of Crown Lands of Canada for 1856. 8vo. Pamph. Toronto, 1857. From L. A. Huguet Latour. Transactions of the Academy of Science at St. Louis. No. 1. Vol. I. 8vo. Pamph. St. Louis, 1857. Silliman's American Journal of Science and Arts. No. 69, for May, 1857. 8vo. New Haven. Verhandlungen des Naturhistorischen Vereines der Pi-eussischen Rheinlande und Westphalens. DreizehnterJJahrgang. Drittes heft. 8vo. 2 nos. Bonn, 1856. Natural History Review. Nos. 9, 10, 11. 8vo. London, 1856. Proceedings of the Royal Geographical Society of London. Nos. 6, 7. 8vo. Pamph. 1857. Transactions of the American Philosophical Society. Vol. XI. Part 1. 4to. Philadelphia, 1857. Journal of the Royal Geographical Society. Vol, XXVI. 8vo. London, 1856. Transactions of the Cambridge Philosophical Society. Vol. IX. Part 4. Cambridge, (England,) 1856. Natural History Review. No. 1. January, 1857. 8vo. London. Canadian Naturalist. Vol. II. No. 2. May, 1857. 8vo. Pamph. Montreal. Conchological Miscellany. By S. Hanley. Nos. 2, 3. 4to. Pamph. London. Proceedings of the Academy of Natural Sciences of Philadelphia, pp. 17-100. 8vo. 1857. Catalogue of Human Crania in the Collection of the Academy of Natural Sciences at Philadelphia. By J. A. Meigs, M. D. 8vo. Pamph. 1857. Beitrage zur Kenntniss der Landplanarien nach Mittheilungen des Dr. Fritz Miiller in Brasilien und nach eigenen Untersuchungen von Dr. Max Schultze. 4to. Pamph. Halle, 1857. Jahrbucher des Vereins fiir Naturkunde im Herzogthum Nassau. Heft XI 8vo. Pamph. Wiesbaden, 1856. Wui'ttembergische Naturwissenschaftliche Jahreshefte- Zehnter Jahrgang Drittes Heft. Zwolfter .Jahrgang; Drittes Heft. Dreizehnter Jahrgang; Erstes Heft. Stuttgart. 8vo. 1856-7. Die Gewitten des Jahres 1855. Ein Beitrag zur Physiologic der Atmosphare von Dr. M. A. F. Prestel. 8vo. Pamph. Eraden. 222 Verhandlungen devEussisch-Kaiserlichen Mineralogischen Gesellschaft zu St. Petersburg. Jahrgang, 1855-6. 8vo. Pamph. 1856. Gelehrte Anzeigen der K. Bayer. Akad. der Wissenschaften. Band 42, 43. 4to. Miinchen, 1856. Theorie und Anweudung des Seitendruck-spirometers, von Dr. E. Harless. 4to. Pamph. Miinchen, 1856. Bemerkungen iiber den Zusammenhang zwischen demBildungs gesetze eines Jfettenbruches. Von L. Seidel. 4to. Pamph. Miinchen, 1855. Beitrage zu Einens Wissenschaftlichen Begriindung der Lehre von Mienenspiel. Von Prof. Dr. E. Harless. 4to. Pamph. Miinchen, 1855. Preussischen Staaten. Neuve Reihe. Dritte Jahrgang. 2 nos. .Juli, 1855, Juni, 1856. 8vo. Berlin. Memorie della Accademia delle Scienze dell' Istituto di Bologna. Tome VI. 4to. 1855. Rendiconto delle Session! dell' Accademia delle Scienze dell' Istituto di Bo- logna. 8vo. Pamph. 1850-55. New York Journal of Medicine. Vol. II. No. 3. 8vo. New York, 1857. Re- ceived in Exchange. Annals and Magazine of Natural History. Vol. XIX. Nos. 111-114. London, 1857. From the Courtis Fund. History of Massachusetts. The Commonwealth Period. By J. S. Barry. 8vo. Boston, 1857. Burke's Works. Vols. IV. V. VI. Also, his Speeches. Vols. I. II. 12mo. London, 1855-7. Arctic Adventures by Land and Sea. Edited by Epes Sargent. 12rao. Bos- ton, 1857. Biographical and Historical Sketches. By T. B. Macaulay. 8vo. New Yoi-k 1857. Testimony of the Rocks. By Hugh Miller. 8vo. Boston, 1857. My Last Cruise. By A. W. Habersham. 8vo. Philadelphia, 1857. Essays Biogi-aphical and Critical. By H. T. Tuckerman. 8vo. Boston, 1857. New Biographies of Illustrious Men. By T. B. Macaulay and others. 8vo. Boston, 1857. Life of George Washington. By Washington Irving. Vol. IV. 8vo. New York, 1857. Depositedhy the Republican Association. BEQUEST OF PROF. J. W. BAILEY. Agardh, C. A. Systema Algarum. 16mo. Lund. 1824. Agardh, Jacobus G. Algse Maris Mediterranei et Adriatici. Observationes in diagnosin Specierum et dispositionem Generum. 8vo. Paris, 1842. Agardh, Jacobus G. Species, Genera, et Ordines Algarum. 8vo. 2. Lund. 1848-51. Areschoug, J. E. Phycea Scandinavias Marinse. 4to. Upsal, 1850. Braun, Alexander. Algarum Unicellularium Genera nova et minus cognita, prcemissis Observationibus de Algis Unicellularibus in Genere. 4to. Lipsise, 1855. Postel, Alexander et Ruprecht, Franciscus. Illustrationes Algarum in Itinere circa Orbem. Atlantic fol. Petropoli, 1840. 223 De Buch, Leopold. Petrifactions receuilHes en Aniei'ique par A. de Humboldt, et par M. C. Degenhart. Imp. fol. Berlin, 1839. {Presentation Copy.) Busch, Wilhelm. Beobachtungen ueber Anatomie und Entwickelung einigcr Wirbellosen Seethiere. 4to. Berlin, 1851. Dana, J. D. Structure and Classification of Zoophytes. 4to. Philadelphia, 1846. Dujardin. Nouveau Manuel complet de P Observateur au Microscope. 18mo. Paris. Accompagn^ d' un Atlas renfermant trente planches gravet5s sur acier. Koyal 8vo. Paris, 1842. Ehrenberg, C. G. Verbreitung und Einfluss des Mikroscopischen Lebens in Sud und Nord Amerika. Fol. Berlin, 1843. Passat-Staub und Blut-Regen, ein grosses organischer unsicht- bares Wirken und Leben in der Atmosphiire. Fol. Berlin, 1849. ■ Microgeologie. Das Erden und Felsen schaffende wirken des unsichtbar kleinen selbstandigen Lebens auf der Erde. Imp. fol. Leipzig, 1854-6. Elliott, Stephen. Sketch of the Botany of South Carolina and Georgia. 8vo. 2 vols. Charleston, 1821-24. Endlicher, S. L. Mantissa Botanica altera. Sistens Generum Plantanim tertium. Roy. 8vo. Vindob. 1843. Harvey, W. H. Manual of the British AlgiB. With plates. 8vo. London, 1849. {Presentation Copy.) Nereis Australis; or Algffi of the Southern Ocean. 4to. Lon- don, 1847. {Presentation Copy.) Phycologia Britannica, or History of British Seaweeds. Col- ored Figures. 8vo. 4 London. 1846-51. Nereis Boreali- Americana, or Contributions towards a History of the Atlantic and Pacific Coasts of North America. Part I. Melanospemiese. Part II. Rhodospermese. 4to. Washington, 1851. Hassall, A. H. History of the British Fresh Water Alg£e. 8vo. London, 1845. Microscopic Anatomy of the Human Body in Health and Disease. 8vo. 2. New York, 1851. {Presentation Copy.) Hooker, W. J. English Flora of Sir James E. Smith. Class XXIV. Crypto- gamia, Vol. V. (or Vol. II. of Dr Hooker's British Flora, Part I.) containing the Mosses, Lichens, Hepatic^, Characese, and Algse. 8vo. London, 1838. Kittlitz, F. H. von. Vierundzwanzig Vegetations-Ansichten von Kiirtentan- dem und Inseln des Stillen Oceans. 4to. Siegen. Text. Krohn, August. Beitrag zur Entwickelungsgeschichte der Seeigellarven. 4to. Heidelberg, 1849. Kiitzing, F. T. Die Kieselschaligen Bacillarien oder Diatomeen. 4to. Nord- hausen, 1844. Species Algarum. 8vo. Lipsise, 1849. Leidy, Joseph. Ancient Fauna of Nebraska. 4to. Philadelphia, 1852, {Pre- sentation Copy.) Lindley, John. Introduction to Botany. 8vo. London, 1832. andHutton, W. Fossil Flora of Great Britain. 8vo. 3. Lon- don, 1831-7. The Vegetable Kingdom. 8vo. London, 1856. Mandl, L. Traits Pratique du Microscope et de son Emploi dans I'Etude des Corps Organises. 8vo. Paris, 1839. 224 Mohl, Hugo von. Principles of the Anatomy and Pliysiology of the Vege- table Cell. 8vo. London, 1852. Montagne, Camille. Cryptogamia Guganensis. Svo. Paris, 1855. Muhlenberg, D. H. Descriptio Uberior Graminum et Plantarum Calamari- narum Americi3e Septeutrionalis indigenarum et Cicurura. 8vo.. Philadelphia, 1817. Miiller, Johann. Ueber die Larven und die Metamorphose der Holothurien undAsterien. 4to. Berlini, 1850. Museum of the Royal College of Surgeons, England. Descriptive and Illus- trated Catalogue of the Histological Series. Vol. I. Elementary Tissues of Vegetables and Animals. (By Mr. Quekett.) 4to. London, 1850. Payer, J. Botanique Cryptogamique, ou Histoire des Families Naturelles des Plantes Inferieures. Roy. Svo. Paris, 1850. Peck, W. G. Botany of the Northern and Middle States. 12mp. Albany, 1833. Perty, Maximilian. Zur Kenntniss Kleinster Lebensformen nach Bau, Funk- tionem Systematik, rait Specialverzeichniss der in der Schweiz beobachten. Roy. 4to. Bern. 1852. Pritchard, Andrew. History of Infusoria, living and fossil. Svo. London, 1841. History of Infusiorial Animalculse, living and fossil. Svo. London, 1852. Quekett, John. Lectures on Histology. Illustrated by 159 woodcuts. 8vo. London, 1852. Rabenhorst, L. Die Siisswasser Diatomaceen (Bacilarien) fiir Freunde der Mikroskopie. 4to. Leipzig, 1853. Riess, P. T. Die Lehre von der Reibungselekluoitat. Svo. 2. Berlin, 1853. Roemer, F. Kriedebildungeu von Texas und ihre organischen Einschliisse. Roy. 4to. Bonn, 1852. Schacht, H. Das Mikroscop und seine Anwendung, insbesondere fiir Pflanzen- Anatomie und Pliysiologie. Svo. Berlin, 1851. Schultze, M. S. Ueber den Organismus der Polythalamien (Foraminiferen) nebst ueber die Rhizopoden im allgemeinen. Imp. Fol. Leipzig, 1854. Smith, Rev. W. Synopsis of the British Diatomaceje. Svo. 2. London, 1853-6. Stein, Dr. F. Die Infusiousthiere auf ihre Entwickelungsgeschichte. 4to. Leipzig, 1854. Sullivant, W. S. Musci and Hepaticis of the United States. Svo. New York. 1856. ToiTcy, John. Compendium of the Flora of the Northern and Middle States. 12mo. New York, 1856. Monograph of North American Cyperacece. Svo. New York, 1836. Van Beneden, P. J. R^cherches sur les Bryozoaires fluviatiles de Belgique. 4to. Bruxelles, 1847. Williamson, W. C. On some of the Microscopical Objects found in the Mud of the Levant and other Deposits. Svo. Manchester, 1847. PAMPHLETS. Gray, Asa. Notice of Dr. Hooker's Flora Antarctica. Svo. Pamph. New Haven, 1849. 225 Harvey, W. H. Botany consiilered in reference to the Art of Design. An Address. 8vo. Pamph. Dublin, 1849. Dickeson, M. W., and Brown, A. Report on tlie Cypress Timber of Jlississippi and Louisiana. 8vo. Pamph. Philadelphia, 1848. Br^bisson, A. de. Description de deux Nouveaux Genres d'Algues Fluviatiles. 8vo. Paraph. Montagne, C. Essai d'Organographie de la Famille des Hepatiques. 8vo. Pamph. Paris, 1845. Thwaites, G. H. K. On the Gonidia of Lichens. 8vo. Pamph. Ralfs, J. On the Genera Spirulina and Coleochcete. 8vo. Pamph. Dickie, G. Notes of Algte observed at various Altitudes in Aberdeenshire. 8vo. Pamph. Thwaites, G. H. K. On an apparently undescribed state of the Palmeteaj. 8vo. Pamph. Agardh, J. G. In systeraate Algarum hodierna Adversaria. 8vo. Lund. 1844. Louder, 0. G. Algse. (Title-page wanting.) 8vo. Pamph. Leidy, Joseph. Researches into the Compai-ative Structure of the Liver. 8vo. Pamph. Philadelphia, 1848. Morton, S. G. Catalogue of Skulls of Man and the inferior Animals in his Collection. 8vo. Pamph. 3d ed. Philadelphia, 1849. Bischofl", T. L. G. On the Periodic Maturation and Discharge of Ova. (Trans- lated by Gilman and Tellkampf) 8vo. Pamph. New York, 1847. Adams, C. B. Contributions to Conchologj'. Nos. 1, 2, 3. 8vo. Pamph. 1849. Morton, S. G. Letter to the Rev. A. Bachman, D D., on the Question of Hy- bridity in Animals, considered in reference to the Unity of the Human Species. 8vo. Pamph. Charleston, 1850. '- Hybridity in Animals considered in reference to the Question of Unity of the Human Species. 8vo. Pamph. New Haven, 1847. Observations on the Ethnography and Archeology of the American Aborigines. 8vo. Pamph. New Haven, 1846. Adams, C. B. Synopsis Conchyliorum Jamaicensium, &c. 8vo. Pamph. Boston, 1845. Haldeman, S. S. Account of some hitherto unnoticed Species of the Genus Hydrachna. Miiller. 8vo. Pamph. Report upon an Individual of the Bushman Tribe. 8vo. Pamph. New York, 1848. Gibbes, L. R. Description of a New Species of Salamander. 8vo. Pamph. Boston. Williamson, W. C. On the Structure of the Shell and Soft Animal of Poly- stomella crispa, &c. Pamph. Manchester, 1848. The Ocean, and its Meaning in Nature. 8vo. Pamph. Montagne, C. Prodromus Generum Specierumque Phycearum Novarum. 8vo. Pamph. Paris, 1842. Troost, Gerard. Description d'un Nouveau Genre de Fossiles. Pamph. 4to. Valentine, W. On the Existence of Stomata in Mosses. 4to. Pamph. 1838. Bowerbank, J. S. On the Organic Tissues in the Bony Structure of the Corallidse. 4to. London, 1842. ■ On the London and Plastic Clay Formations of the Isle of Wight. 4to. London, 1839. PROCEEDINGS B. S. N. H. — VOL. VI. 15 AUGUST, 1857. 226 Bowerbank, J. S. On the Siliceous BoJies of the Clialk, Greensamls, and OoMtes. 4to. Pamph. 1840. Quekett, E. T. Observations on the Ergot of Rye and some other Grasses. 4to. London, 1838. Mantel], G. A. Memoir of a Portion of the Lower Jaw of the Iguanodoh, &c. 4to. Pamph. London, 1841. On the Fossil Remains of Turtles discovered in the Chalk Formation of the Southeast of England. 4to. Pamph. London, 1841. Deane, James. Illustrations of Fossil Footprints of the Valley of the Con- necticut. 4to. Pamph. 1849. Le Conte, J. L. On Platygonus compressus, a new fossil Pachyderm. 4to. Pamph. 1848. Baird, S. F. Revision of the North American Tailed-Batrachia, with Descrip- tions of New Genera and Species. 4to. Pamph. 1849. Williamson, VV. C. On the Distribution of Fossil Remains on the Yorkshire Coast. 4to. Pamph. 1836. ■ On the Microscopic Structure of the Scales and Dermal Teeth of some Ganoid and Placoid Fish. 4to. Pamph. London, 1849. Lehmann, J. G. C. Novarum et minus cognitarum stirpium, pugillus Septi- mus. 4to. Pamph. Hamburgi, 1838. Mirbel et Spach. Notes pour servir a I'Histoire de I'Embryogenie V^g^tale. 4to. Pamph. 1839. Agardh, J. G. Ofrer de Capska Arterna af sKiglet Tridtea. 8vo. Pamph. 1847. Montague. Memoire conoernant les Organes Males du Genre Targionia. 4to. Pamph. 1838. Areschoug, J. E. Phycologia. Decas Tabularum prima. 4to. Gothoburgi, 1847. Translation of " Beitrage zur Lehre von der Befruchtung der Pflanzen." By A. J. C. Corda. 8vo. Pamph. New York, 1836. Gray, Asa. Remarks on Structure and Affinities of the Order CeratophylliB. 8vo. Pamph. New York, 1837. Bailey, J. W. Account of an Excursion to ]\It. Katahdin, in Maine. 8vo. Pamph. Croom, H. B. Catalogue of Plants, Native and Naturalized, in the Vicinity of Newborn, N. C. 8vo. Pamph. 1837. Decaisne, M. J. Plantes de I'Arabie Heureuse recueillies par M. P. E. Botta. 4to. Pamph. Agardh, C. A. Icones Algarum ineditse : fasciculi qui extant duo. 4to. Pamph. Lund. 1846. Chauvin, J. F. Recherches sur 1' Organisation, &c., de plusieurs Genres d'AIgues. Agardh, C. A. Essai d'une repartition des Polypiers Calcif^res de Lamouroux. 4to. Pamph. Ccen, 1842. Melanthacearum Americce Septentrionalis Revisio. 8vo. Pamph. New York, 1837. Torrey, J, Account of several new Genera and Species of North American Plants, 8vo. Pamph. Montague, C, Recherches sur la Structure du Nucleus des Genres SphcEro- phoron, &c. 8vo, Pamph. 1842. (With an autograph letter.) Arnott, G. A. W. On the Genus Torreya. 8vo. Pamph. 22 Bowerbank, J. S. On a New Variety of Vascular Tissue. 8vo. Pampli. London, 1840. Queliett, E. T. On the Development of the Vascular Tissue of Plants. 8vo. Pamph. London, 1840. On the Structure of some Tissues possessing Hygrometric Properties. 8vo. Pamph. London, 1840. Emerson, G. B. Notice of Prof. A. P. de Candolle. 8vo. Pamph. Boston, 1841. Gray, Asa. Notice of the Botanical Writings of the late C. S. Rafinesque. 8vo. Pamph. Southwick, E. W. Notes of a Tour to the White Hills. 8vo. Pamph. 1841. July 1, 1857. Dr. Chas. T. Jackson, Vice-President, in the Chair. The Report of the Committee appointed to audit the Treasurer's Annual Account was read and accepted. Dr. A. A. Hayes reported that a specimen of Gum from Cali- fornia, referred to him at the last meeting, had been examined chemically. It proved to be pure Arabine, or the colorless con- stituent of gums, which is soluble in cold water and forms a clear gum solution, without the character of emulsion. This gum is commercially valuable, the quality being fully equal to any im- ported. A specimen of Bark from California, also referred to him, was found to contain mucilage, analogous to that of the bark of the Ulmus fidva, (Slippery Elm.) It was not, however, so abundant, and it was less soluble in water. Besides mucilage, a small por- tion of one of the varieties of tannin gives astringency when the bark is chewed. These are not substances of value, and there is no reason for supposing that this bark will prove specially im- portant. Dr. A. A. Hayes exhibited a specimen of Octohedral Tin Ore rom the gold washings of Owen's River, on the way from Mel- 228 bourne to Sydney, Ani^tralia. The ore is accompanied by titan- iferous and chromiferous iron ores, garnets, and yellow quartz. In this connection, he stated that he had examined the black sands of many of tlie gold washings of California, in which, be- sides garnets and topazes, cinnabar is generally found, without detecting tin ore. Some of the titaniferous iron crystals yield the slight traces of oxide of tin, often found in the ore, but no crystals of pure oxide of tin have been found. Although, in general, a resemblance exists between the sands of Australia and those of California, the heavy ores found are not the same in both. Mr. F. H. Storer exhibited specimens of Lithium, Strontium, and Calcium, and described the process of their preparation. Dr. Jackson presented a specimen of Sugar obtained by Mr. Wray from the Sorghum saccharatum, or Ciiinese Sugar Cane, which was raised in Algeria. He likewise presented some of the dried juice of the Sorghum, which he had prepared from samples of the plant raised in Massachusetts. Dr. Hayes stated that the plant, when raised in Algeria, con- tained Cane Sugar, but that, when raised in this climate, it had been satisfactorily determined, by both microscopical and chemical examinations of the juice in the cells, that only Grape Sugar is produced. The specimens were referred to the Microscopical Department. MICROSCOPICAL DEPARTMENT. The Curator of the department announced the dona- tion, by Dr. John Bacon, of a handsome portable double Argand Gas Burner, together with the accompanying apparatus for connection with the gas pipes of the build- ing. These burners were used for the microscopical demonstrations of the evening, and found very convenient and effective. Dr. Durkee exhibited some living specimens of Vorticella cra^ teriformis, Ehrenberg. He stated that this infusorial animalcule first made its appearance upon a Gordim aqriaticiis, one of the so-called horse-hair worms, so commonly found in pools of water, 229 which he had alive at his office, and that the Vorticolla after- wards was propagated upon the skin of a Salamander, and upon a piece of cork, kept in the same glass vessel with the worm. The animalcule surmounts a flexible stem or pedicle, it is trans- parent, and its mouth is surrounded by numerous cilia, which are constantly in motion, and serve to keep the water in circulation and to bring food near it. The Vorticellte, assuming a great variety of elegant forms, with their pedicles at times partially coiled in a spiral form, and at other times elongated, and with the cilia in motion, producing a current carrying with it small particles of water into the alimentary sack, were beautifully seen upon the stand of the microscope. Dr. Bacon exhibited some very large and fine specimens of Cystine, from the spontaneous deposit of the urinary excretion of a person who has passed several Cystine Calculi within a few months. This substance is of extremely rare occurrence here. Dr. Bacon also exhibited some Crystals of the Sulphate of lodo-Quinine, a substance remarkable for its polarizing action, and some Zeolitic Crystals of Carbonate of Lime, from the urine of the horse. Dr. Durkee exhibited specimens of ValUsneria spiralis^ an aquatic plant, growing in great abundance in Fresh Pond and other waters. The circulatory fluid of the plant, running in channels around the cells of which it is composed, was plainly demonstrated by the microscope. Mr. Sprague exhibited specimens of an Alga which he found in a sulphur spring near Portland, Me. It grew in abundance, investing the neighboring grass, sticks, leaves, &c., with a soft flaccid, snow-white fringe. It was found to consist, under the microscope, of excessively slender, pellucid filaments, about a line or more long, filled with minute granules, arranged in no particular order. The filaments were simple, and attached firmly to the object on which they grew. Mr. Sprague supposed that it might be the Calothrix nwea, Ag. He also exhibited some of the minute fungi of the order Goni- omycetes — Sporlde^miiim concinmtm and Sporidesmivm epiphyl- lum. 230 Messrs. John S. Martin and Edwin Manley were elected Resident Members. July 8, 1857. MICROSCOPICAL DEPARTMENT. Dr. Silas Durkee, Curator, in the Chair. It was voted to appoint sub-committees, to whom should be referred specimens for microscopic examina- tion ; and the following were appointed, viz : — Anatomy. — Jeffries Wyman, Silas Durkee, A. A. Gould, O. W. Holmes, H. I. Bowditch, J. N. Borland, D. F. Weinland. Geology and Mineralogy. — A. A. Hayes, C. T. Jackson, W. B. Rogers, H. D. Rogers, Louis Agassiz, T. T. Bouve. Botany. — C. J. Sprague, S. Durkee, C. L.' Andrews. Pathology.— T>. S. Shaw, Calvin Ellis, H. J. Bigelow, C. D. Homans. Chemistry. — John Bacon, C. T. Jackson, A. A. Hayes, J. P. Cooke, F. H. Storer. Messrs. Bacon, Cooke, and Shaw were appointed a committee to examine the specimens of Sorghum saccharatum referred to the department at the previous meeting of the Society. July 15, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. The Committee of the Council to whom was referred the consideration o' the expediency of raising the Annual 231 Assessment from three to five dollars, presented a report, which was read and accepted. The Committee con- cluded their report with the recommendation that the Annual Assessment be five instead of three dollars. The consideration of this recommendation was postponed to the next meeting. The Chairman read a letter from Townend Glover, of Washington, returning thanks to the Society for his elec- tion as Corresponding Member, and accepting the same. Mr. Glover likewise wrote that he intended soon to send to the Society a number of plates of Insects Injurious to Vegetation, which he was preparing for publication. Mr. T. J. Whittemore read a letter from a gentleman in Germany, proposing to exchange a collection of Fossil Shells of Austria for those of North America, or a rare and costly work on fossils for the same. The letter was referred to the Curator of Geology. Dr. S. Kneeland, Jr., read the following paper : — ON THE BIRDS OF KEWEENAW POINT, LAKE SUPERIOR. BY S. KNEELAND, JR., M. D., BOSTON. Most of the birds mentioned in the following list were seen by me during a residence of nearly a year at Portage Lake, from August, 1856, to June, 1857. A few have been introduced on tlie authority of competent eye-witnesses. When there is any doubt concerning the occurrence of a bird, it is so indicated. In Ke- weenaw Point, I include that portion of the Upper Peninsula of Michigan which extends up into Lake Superior, embracing not only the Point proper, but the western portion as far as Ontona- gon, the region of Portage Lake and Entry, and the Anse of Ke- weenaw Bay — all of which localities I have visited. This region lies between 47° and 48° north latitude, and be- tween 88° and 90° longitude west from Greenwich, being the so-called " Copper Region " of Lake Superior. It is probable that many birds, especially among the warblers 232 and migratory species, will be added to this list hereafter ; and it is almost certain that many others inhabit the adjacent country, which has been very little explored. This, therefore, is only an approximation to a complete list of the birds of Upper Michigan. This district is, for the most part, heavily wooded with pines, spruces, firs, balsams, cedars, maples, and birches, and would be naturally supposed to be the favorite retreats of many more birds than are found in it. The stillness of the dark and virgin forests is most remarkable ; and it is only during the few warmer months that the woods lose this dismal character. Snow begins to fall about the middle of November, from which date to the middle of March, scarcely a day passes without a fall of snow some time during the twenty-four hours — hence only the hardier birds re- main during the winter. The numerous small lakes and water- courses are the favorite resorts of many water-birds, some of whom breed here. Of mammals, the small fur-bearing animals alone are common ; such as the fox, beaver, otter, fisher, marten, mink, and musk-rat — wolves are quite unknown ; deer scarce, and bears few. Por- cupines and squirrels are numerous. FALCONID^. 1. Golden Eagle. Aquila fulvus, Linn. This bird I have not seen, neither have I met with any one who has seen it beyond a doubt ; though, from the reports of hunters and Indians, I am inclined to think it is found here. 2. Bald Eagle. Halicetus leucocephalus. Linn. Breeds on the Point and near Portage Lake. 3. Fish Hawk. Pandion halieetus, Linn. 4. Gyr-Falcon. Falco Islandiciis, Brliim. I have heard of a white falcon, of large size, (measuring about five feet in the spread of his wings,) which was shot on the Point ; this, I think, must have been the gyr-falcon. 5. Great-footed Hawk. Falco peregrinus, Linn. 6. Pigeon Hawk. Hypotriorchis columharius, Linn. 7. Sparrow Hawk. Tinnunculus sparverius, Linn. 8. Common Buzzard. Buteo vulgaris, Bechst. 9. Red-shouldered Hawk. Buteo lineatus, Gmel. 10. Red-tailed Buzzard. Buteo borealis, Gmel. 233 11. Rough-legged Buzzard. ArcMbtiieo lagopifs, Bnm. 12. Goshawk, (doubtful ) Astur palumbarius, Linn. 13. Cooper's Hawk, (doubtful.) Accifiter Cooperi, Pr. Bonap. 14. Sharp-shinned Hawk. Accipiter fuscus, Gmel. 15. Common Harrier. Circus cyaneiis, Linn. STRIGID^. 1 6. Hawk Owl. Surnia funerea, Gmel. This owl is com- mon in the neighborhood of Eagle River and Harbor ; it is not found at Portage Lake. 17. Snowy Owl. Nyctea nivea, Thunb. 18. Acadian Owl. Athene Acadica, Temm. 19. Cinereous Owl. Syrnium cinereum, Gmel. 20. Barred Owl. Symium nehulosum, Gmel. 21. Great Horned Owl. Bubo Virginianus, Gmel. 22. Mottled Owl. Ephialtes asio, Linn. CAPRIMULGID^. 23. Whip-poor-will. Gaprimulgus vociferus, Wils. 24. Night-Hawk. Ghordeiles Virginianus, Briss. HIRUNDINID^. 25. Barn Swallow. Hirundo rufa, Vieill. 26. White-bellied Swallow. Hirundo bicolor, Vieill. ALCEDINID^. 27. Belted Kingfisher. Geryle alcyon, Linn. CEKTHID^. 28. Red-bellied Nuthatch. Sitta Canadensis, Lath. 29. Winter Wren. Troglodytes hyemalis, Vieill. LUSCINID^. 30. Blue Bird. Sialia Wilsoni, Swains. 31. Arctic Blue Bird. Sialia arctica, Swains. 32. Water Thrush. Enicocichla Noveboracensis, Gmel. 33. Black-capped Tit. Parus atricapillus, Wils. 34. Hudson's Bay Tit. Parus Hudsonicus, Mill. 234 35. Yellow-poll Warbler. Mniotilta (Estiva, Gmel. 36. Canada Warbler. Mniotilta Canadensis, Linn. 37. Yellow-rumped Warbler. Mniotilta coronata, Linn. 38. Black-poll Warbler. Mniotilta striata, Gmel. 39. Black and Yellow Warbler. Mniotilta maculosa, Gmel. 40. Black-throated Green Warbler. Mniotilta virens, Gmel. (Doubtful.) It is probable that many other warblers are found here ; and it is said that some are, on more or less good authority ; but where there is so little certainty, I prefer to leave the list of warblers to be filled up hereafter. 41. Wagtail. Anthus Ludovieianus, Gmel. TURDIDiE. 42. American Robin. Turdus migratorius, Linn. This bird appears in the latter part of April, a month before the snow leaves the ground. 43. Wood Thrush. Turdus mustelinus, Gmel. 44. Rufous-backed Thrush. Turdus fuscescens '? Shaw. 45. Olive-backed Thrush. Turdus solitarius ? Wils. 46. Cat-Bird. Mimus Caroline?isis, Linn. This bird is not found at Portage Lake, though it is said to occur in the more settled parts of the country. As this is one of the species which follow the course of agriculture, it is quite likely that it will soon become a general summer resident. MUSCICAPID^. 47. King Bird. Tyrannus intrepidus, Vieill. 48. Pewit Flycatcher. Myiohius nunciola, Wils. 49. Wood Pewee. Myiohius virens, Linn. 50. Redstart. Setophaga ruticilla, Gmel. 51. Red-eyed Vireo. Vireo olivaceus, Linn. 52. White-eyed Vireo. Vireo Noveboracensis, Gmel. AMPELID^. 53. Bohemian Wax-wing. Ampelis garridus, Linn. 54. Cedar Bird. Ampelis cedrorum, Vieill. LANIIDJE. 55. Great American Shrike. Lanius septentrionalis , Gmel. 235 CORVIDyE. 56. Canada Jay. Perisoreus Canadensis, Jj'inn. This bird is common in the winter, and a great pest to the trappers, from its propensity to steal their poisoned baits. Like the raven, it often falls a victim to its greediness, by devouring meat containing strychnine set for foxes and the fur-bearing animals. 57. Blue Jay. Cyanocorax cristatus, Linn. Not common on Portage Lake. 58. American Magpie. Pica Hudsonica, Sabine. I have seen a few specimens obtained near Eagle River. 59. American Raven. Corvus cacalotl,Wix^\. Very common at Portage Lake ; in the winter almost, if not entirely, to the exclusion of the crow. 60. American Crow. Corvus Americanus, Aud. Rare at Portage Lake, but common on the Point and in the Ontonagon district. STURNID^. • 6L Rusty Grrakle. Scokcophagus ferrugineus, Wils. Early in the spring these birds arrive in immense flocks, and exceed- ingly fat ; they remain till about the last of September. 62. Cow Blackbird. Molothrus pecoris, Gmel. 63. Red-winged Blackbird. Agelaius phoeniceus, Linn. 64. Bob-o'-link, (doubtful.) Dolichonyx oryzivorus, Linn. FRINGILLID^. 65. Rose-breasted Grosbeak. Guiraca ludoviciana, Linn. 66. American Goldfinch. Fringilla tristis, Linn. 67. Lesser Red-poll. Fringilla linaria, Linn. These birds are seen in flocks of twenty or thirty all through the winter, in the woods near the lake and in the beaten roads, in company frequently with the snow-birds. They show a singular propen- sity to pick in snow stained by human urine ; though the roads be full of the dung of cattle containing oats and pieces of corn, the linnets I have always seen in crowds about the spots in the snow discolored from the above cause ; whether this habit was from a desire to obtain fluid at a season when the snow does not melt even at mid-day, or some of the elements of this secretion, 236 I cannot say. Similar congregations of bees and wasps are often noticed about public urinals in the country. 68. Snow Bird. Fringilla hyemalis, Linn. 69. Pine Finch. Fringilla pinus, Wils. 70. Fox-colored Sparrow. Zonotrichia iliaca, Merr. 71. Sonf Sparrow. Zonotrichia melodia, Wils. 72. White-throated Sparrow. Zonotrichia albicoUis, Gmel. This bird is very abundant. Its beautiful and plaintive notes may be musically represented as follows : — as to interval and time in a flat key ; this should be written two octaves above, and the fourth interval (E flat) should be what is called a " flat fourth ; " sometimes the first two notes only are heai'd, at others, from one to the four triplets in addition ; instead of the triplets, an equivalent single note is often given for one or more of thera. I have heard its sweet song at all hours of the day and night in the spring and summer. 73. White-crowned Sparrow. Zonotrichia leucophrys, F'orst. 74. Bay-winged Sparrow. Zonotrichia graminea, Gmel. 75. Chipping Sparrow. Zonotrichia socialis, Wils. 76. Tree Sparrow. Zonotrichia monticola, Gmel. 77. Snow Bunting. Plectrophanes nivalis, Linn. 78. Lapland Lark Bunting. Plectrophanes lapponicus, Linn. 79. Shore Lark, (doubtful.) Otocoris alpestris, Linn. 80. Purple Finch. Carpodacus purpureus, Gmel. 81. Pine Grosbeak. Slrobilophaga enucleator, Linn. 82. Common Crossbill. Loxia Americana, Wils. 83. White-winged Crossbill. Loxia leucoptera, Gmel. The former of these crossbills occurs in large flocks during most of the winter, hopping about the houses with the familiarity of chipping sparrows. The white-winged species I have not seen ; but I am confident it is found here. PICID^. 84. Arctic Woodpecker. Picoides arcticrts, Rich, and Sw. 237 85. Three-toed Woodpecker. Picoides hirsutus, Vieill. The first of these species is common during the whole of the severe winters of Lake Superior. 86.. Hairy Woodpecker. Picus viUosus, Linn. 87. Downy Woodpecker. Picus pubescens, Linn. 88. Canada Woodpecker. Picus leucomelas, Bodd. 89. Pileated Woodpecker. Dryocopus pileatus, Linn. 90. Red-headed Woodpecker. Melanerpes- erythrocephalus, Linn. 9L Golden-winged Woodpecker. Colaptes auratus, Linn. COLUMBID^. 92. Passenger Pigeon. Ectopistes migratorius, Linn. I have seen them at Portage Lake as early as May 4. TETRAONIDiE. 93. Common Quail. Ortyx Virgimanus, Linn. This is an- other of the birds that follow man in his agricultural movements. A few years since quails were unknown in the Upper Peninsula ; now they are not uncommon on the Point ; as yet they have not been seen on Portage Lake. As more attention is paid to agri- culture for the support of the mining population, the quail will doubtless be common in the fields. 94. Canada Gi'ouse. Tetrao Canaderisis, Linn. 95. Ruffed Grouse. Bonasa umbelliis, Linn. The first species is comparatively rare ; I have never heai'd of one being seen on Portage Lake. The latter species is very common in the woods at all seasons of the year. 96. White Ptarmigan. Lagopus mutus ? Leach. There is a white grouse in this region, but whether it is the L. mutus, albus, or leucurus, I cannot positively say. CHARADRIAD^. 97. Black-bellied Plover. Squatarola Helvetica, Linn. 98. Golden Plover. Charadrius pluvialis, Linn. 99. American Ring Plover. Charadrius semipalmatus, Kaup. ARDEID^. 100. Sandhill Crane. Grus Americana, Linn. 238 101. Green Heron. Ardea virescens, Jjinn. 102. American Bittern. Botauriia lentiginosus, Mont. SCOLOPACID^. 103. Yellow-shanks Tatler. Totanus Jlavipes, Gmel. 104. Tell-tale Tatler. Totanus melanoleuc us, Grmel. 105. Solitary Tatler. Totanus chloropygius, Vieill. 106. Semipalmated Tatler, (doubtful.) Totanus semipalmatus, Gmel. 107. Spotted Tatler. Tringoides macularia, Linn. 108. Long-legged Sandpiper, Hemipalmamultistriata, Liclit. 109. Schinz's Sandpiper. Tringa Schinzn, Brehm. 110. Peep. Tringa pusilla, Wih. 111. Red-breasted Snipe. Macroramphus griseus, Gmel. , 112. Common Snipe. GaUinago Wilsonii, Temm. 113. Woodcock. Philohela minor, Gmel. 114. Wilson's Phalarope. Phalaropus Wilsonii, Sab. RALLIDiE. 115. Sora Rail. Ortygometra Carolina, Linn. This is not uncommon at Portage Lake in September and October. 116. American Coot. Fidica Americana, Gmel. The tatlers, sandpipers, snipes, coots, geese, ducks, and loons, begin to arrive at Portage Lake about the last of April, when only the small streams opening into the lake are free from ice ; from this time till the last of May, when the ice disappears, they are very numerous, and are shot in great numbers. ANATID^. 117. White-fronted Goose. Anser ergthropus, L'mn. 118. Snow Goose. Anser hgperboreus,Fa\\. These are rare, compared with the Canada Goose. 119. Canada Goose. Bernicla Canadensis, Linn. Quite com- mon at Portage Lake in the spi'ing. 120. Swan. Cygnus Americanus, Sharpless. These birds have been seen flying over, but I have never known of one alight- ing or being shot in this region. 121. Summer or Wood Duck. Aix sponsa, Linn. 239 122. American Widgeon. 3fareca Americana, Gmel. 123. Pintail Duck. Dajila acuta, Linn. 124. Mallard. Anas hoschas, Linn. 125. Dusky Duck. Anas ohscura, Gmel. 126. Green-winged Teal. Querquedula Carolmensis, Gmel. 127. Blue-winged Teal. Pterocyanea discors, Linn. 128. Gadwall Duck. Ohaulelasmus strepera, Linn. 129. Shoveller Duck. Spatula clypeata, Iawo.. 130. Ring-necked Duck. Fuligula collaris, Don. 131. Scaup Duck. Fidigida marila, Linn. 132. Canvas-back Duck. Nyroca valisneria, Wils. This duck is occasionally seen here during its migrations, but I could not ascertain that any had ever been shot. 133. Red-headed Duck. Nyroca Americana, Pr. Bonap. This species I have often seen and eaten at Portage Lake. 134. Golden-eye Duck. Glangula Americana, Pr. Bonap. 135. Buffel-headed Duck. Glangula albeola, Linn. 136. Goosander. Mergus castor, Linn. 137. Red-breasted Merganser. Mergus serralor, Linn. 138. Hooded Merganser. Mergus cucullatus, Linn. I have been, told by hunters here that there is at some seasons of the year, a nearly white merganser, or " saw-bill," as they call it, in the lakes of this vicinity. From the alleged improbability of. the occurrence of the smeiv {Mergellus albellus, Linn.) except as a very rare visitor from Arctic Europe, I have not included this bird in my list, though its occurrence is firmly maintained. by the Indians and hunters, who ought to know. The bird seen by them may be some white-plumaged duck ; though I must say I am inclined to believe that Audubon is wrong in excluding the smew from the. American continent, and that Wilson is right in making it not an uncommon bird here. COLYMBID^. 139. Common Loon. Colymhus glacialis, Linn. This is a very common species at Portage Lake, in the spring and summer, and is here possessed of all the shyness peculiar to it in more populous localities. The only way the gunner can approach it in the open lake, where it delights to sport and feed, is to conceal the bow of his boat or canoe with branches of evergreen, and 240 surmount the leafy covering with a bright flag; behind this screen he can paddle easily towards the bird, whose natural curi- osity prompts him to swim towards it to see what the strange object is. By keeping up a shrill whistle at the same time, it is not difficult to get within gun-shot. They are hunted considera- bly for their skins, of which the natives make bags, pouches, and knife-sheaths. 140. Red-throated Diver. Oolymhus septentrionalis, Linn. 141. Black-throated Diver. Colymhus arcticus, Linn. 142. Crested Grebe. Podiceps cristatus, Linn. 143. Horned Grebe. Podiceps cornutus, Gmel. 144. Pied-bill Dobchick. Podilymhus Carolinensis, Lath. LARID^. 145. Herring Gull. Larus argentatus, Briin. This bird is very common on the Great Lakes, following in the wake of steamers and vessels, and is not uncommon on Portage Lake. There is said to be a smaller black-headed gull there, but I have never seen it above the Saut St. Marie. This is undoubtedly the Larus Bonapartei, Rich. & Sw. 146. Common Tern. Sterna Wilsoni, Pr. Bonap. There are doubtless other species of terns here. PELECANID^. 147. White Pelican. Pelecanus trachyrhynchus, Lath. One of these bii'ds was seen and shot at on the Point a few years since. Synopsis of number of Species in the several Families. — FalconidaB, 15 ; Strigida?, 7 ; Caprimulgidaj, 2 ; Hirundinidaj, 2 ; Alcedinidfe, 1 ; Certhida^, 2 ; Luscinidse, 12 ; Turdidse, 5 ; Mus- cicapidaj, 6 ; Ampelida^, 2 ; Laniidas, 1 ; Corvida^, 5 ; Sturnidse, 4; Fringillida?, 19; Picida}, 8; Columbidas, 1; Tetraonidae, 4; Charadriadffi, 3 ; Ardeida^, 3 ; Scolopacidae, 12 ; Rallidse, 2 ; Ana- tidie, 22 ; Colymbida?, 6 ; Laridre, 2 ; Pelecanidte, 1. In all, 147 species ; of which 96 are land birds, and 51 are water birds. The birds of prey are numerous, and consequently the warblers, flycatchers, and finches are in the proportion neces- sary to supply them with food. The crow and woodpecker fara- 241 ilies preserve the usual ratio of cold climates ; while the ducks, divers, and beach birds are what we should naturally expect to find in the neighborhood of the largest and finest sheet of fresh water in the world. Dr. Silas Durkee exhibited two specimens of the Com- mon Glowworm, {Lampyris noctiluca,) which were found in Dedham, Mass. He remarked that the Glowworm is not the larva of an insect, but the perfect female of a winged beetle, from which it is so different that nothing but actual observation would lead one to infer that they are different sexes of the same insect. The specimens exhibited have a small flat head, furnished with antennae about half a line in length, and when examined with a common pocket magnifier, are seen to consist of two colors, white and chestnut, alternating. They do not appear to have the power of producing or extinguishing the light at will. Their brilliancy is less than that of the Elater noctilucus, two specimens of which Dr. D. exhibited several months since. Dr. Durkee said that he had watched these glowworms during an interval of about nine hours, commencing at eight o'clock in the evening. The pe- culiar faculty of producing light began to show itself between the segments of the body and at the large spiracles or stigmata, which may be seen in connection with the rings ; there being two of these spiracula to each segment, and twenty -four in all. From about eight o'clock to midnight, the light along the rings and at the spiracles was much more brilliant than it was through the segments themselves. But during the latter part of the nio-ht, the light was equally diffused throughout the entire length of the worm. This was the case in both specimens. And during this distribution of the luminous power, or property, nothing could be seen of the spiracula, or of the segments or joints. The worms appeax'ed as if they were two fused masses of beautiful phosphorescent light ; sometimes at rest, sometimes assuming a variety of shapes, according to their slow and graceful move- ments. The luminous properties were displayed at first through a few of the spiracula and a few of the joints, while all the rest were in a condition like that which is maintained during PROCEEDINGS B. S. N. H. — VOL. VI. 16 OCTOBER, 1857. 242 the day ; that is, they yielded no light. This partial illumina- tion, however, soon gave place to the most charming diffusion of light along the whole length of the body, and the latter condition was preserved unbroken until the light of day broke the charm, and these fairy little creatures were transformed into mere worms. It is said that the light in the female is most brilliant in the season when the sexes are destined to meet. In some species the light is emitted only during the period for propagation. • The Curator of Crustacea and Radiata asked to be excused from the care of the Crustacea, or to have the department divided. He thought there was sufficient labor for two curators, and he could properly take charge of the Radiata only. The subject was referred to a com- mittee, consisting of Messrs. Abbot, Gould, and Whit- temore. James H. Slawson, of Houghton, Michigan, was elected a Corresponding Member. Messrs. Chas. V. Bemis, M. D., of Medford, and Oliver W. Peabody, of Boston, were elected Resident Members. August 5, 1857. Dr. Chas. T. Jackson, Vice-President, in the Chair. A communication was read from the Georgic Associa- tion of Cattaraugus County, N. Y., requesting dona- tions of Publications, Specimens, &c. Referred to the Publishing Committee. Mr. W. G. Dix, by invitation, read a paper upon Ecua- dor and its natural productions. Dr. Head, of the U. S. Army, exhibited a large Hair- ball, so called, six inches in diameter, taken from the 243 stomach of a healthy ox, on the banks of the Nueces, in Texas. Its surface was smooth, hard, and apparently calcareous. Dr. D. H. Storer remarked that balls of this character were occasionally found here ; not, however, so large as this. Quite a large one from the stomach of a hog, com- posed of bristles, was sent recently to the Society for Medical Improvement. The hairs are introduced into the stomach in the process of licking the skin. Dr. H. R. Storer presented specimens of a Smelt from Squam Lake, N. H., remarking on its peculiar interest, as affording an instance of a species originally migrating to fresh water from salt water, and now permanently resident in the former. Dr. Storer said that he had learned of its existence several years since, but had, until now, been unable to obtain it. When full groAvn the lake smelt seldom exceeds six inches in length and is extremely attenuated, but a careful examination leaves little doubt of its identity with our marine Osmerus viridescens. It is found throughout the year, in both Squam Lake and Winnipi- seogee, though more rarely in the latter. The modifications in shape referred to, would probably be found to exist also in the smelt of Jamaica Pond, near Boston, specimens of which had already been presented to the Society ; the conditions of life being much the same in both, the latter having been imprisoned artificially, while the former had become a permanent resident in fresh water from natural causes alone. It was once supposed that the salt water Cusk was found in the New Hampshire lakes, but Dr. D. H. Storer had proved, in the Journal of this Society, that the fishes in question were not only specifically but generically distinct. Dr. Storer also presented two species of Leuciscus, one of them probably undescribed, from the same locality. MARYLAND MARBLES AND IRON ORES. Dr. C. T. Jackson stated that he had recently examined the marble and limestone quarries of Texas, Maryland, for Mr. Wil- 244 liara Robinson, of Baltimore, and at the same time had visited the quarries in the same town where the marbles now employed in the extension of the General Post-Office and Patent-Office at Washington, wei'e obtained. The marbles at Mr. Robinson's quarries are identical in character with those from the United States quarries above mentioned. The Dolomite, which is the finer-grained marble, similar to that used in the Post-Office extension, has a density of 2.851, hence a cubic foot of it will weigh 178.187 pounds avoirdupois. On chemical analysis this stone is found to consist of Carbonate of lime -------- 59.4 Carbonate of Magnesia ------ 38.5 Carbonate of Manganese and Iron - - - 1.4 Insoluble siliceous matter ------ 0.7 100.0 The strength of a stone of the neighboring quarry, tested at Washington, was found to be equal to a resistance of 18,061 pounds per square inch. This marble is suitable both for monu- mental purposes and for architecture. The broken fragments of it make, when burned, a hot magnesian lime, which, when mixed with sand, forms a mortar with some hydraulic properties, so that it is very permanent, and resists the action of water after it is once hardened or set. The other marble is a coarse-grained white limestone, called by the quarrymen Alum Stone, on account of the large size of its crystals, and their great purity. A stone identical with this is employed in the extension of the Patent-Office buildings. This marble has a density of 2.697, and a cubic foot of it weighs 168.562 pounds. Its strength is equal to a resistance of 8.057 pounds per square inch, according to the experiments made at Washington on a stone identical with this which was taken from a neighboring quarry. This stone is largely burned for making lime, and furnishes the best quality of pure white lime for mortar and for plastering ceil- ings. The marble is also employed in building, though it is far inferior in strength to the dolomitic variety before described. On chemical analysis this limestone was found to consist of 245 Carbonate of lime, 97.9 Carbonate of Manganese and Iron, - - - 1,8 Insoluble Silica, 0.3 100.0 It does not contain any majjnesia, a remarkable fact, consider- ing its close contiguity to the Dolomite. Dr. Jackson stated he had on this same excursion examined a remarkable locality of Iron Ore, near Whitehall station on the Northern Central Railroad, about 20 miles north of Baltimore. This locality presented some interesting geological and miner- alogical phenomena. The rocks were Talcose rock or soapstone, chlorite slate, and masses of crystallized garnets so closely packed together in chlorite as to resemble a pudding stone in general ap- pearance. The garnets are regular rhombic dodecahedrons, and are generally of the size of grape shot, tliough some of them are as large as a turkey's egg. The chlorite slate is filled with an impurity of crystals of octahedral magnetic iron ore, and with veins of the granular ore of the same kind. The soapstone gen- erally underlies the iron ore, though it alternates with the chlorite slate in one instance at this mine. The iron ore with the chlorite slate and garnet rock are mined together, and the ore sells at a neighboring anthracite furnace at $3 per ton. Dr. Jackson said that no one would, on looking at the heaps of this ore, conceive it worth any thing for furnace purposes, but on analysis he found that an average sample of the ore yielded 41 per cent, of the per oxide of iron, which is equal to 28jo per cent of metallic iron. A certain proportion of garnets aids the smelting of the iron ore by their ready fusion and by preventing the absorption of any oxide of iron by the slag even if the garnet itself does not yield, as it probably does, a certain proportion of iron in the smelting furnace. Dr. C. T. Jackson presented, in the name of W. E. S. Whitman, Esq., of Gardiner, Me., specimens of the shells, [Alasmodonta arcuata) which are opened for pearls in that State. 246 Dr. J. A. Lamson was elected a Resident Member. The names of Professors W. B. and H. D. Rogers were added to the list of Resident Members. DEPARTMENT OF MICROSCOPY. An extract from a letter of C. A. Spencer, of Canas- tota, N. Y., to Dr. Dm-kee, was read to the Society. Mr. Spencer says that he is " manufacturing a new lens, which he calls the ' Orthoscopic Eyepiece.' It is more perfectly achro- matized than the old negative form, has a perfectly flat field, and is more luminous. Its cost, he says, is high, (fifteen dollars ;) still, he is satisfied it will meet a want long felt by microscopists." Alluding to some recent examinations of animal tissues with his lenses, in connection with Mr. Clark, Prof. Agassiz's assistant, Mr. Spencer says, ".one result of large angles of aperture in such investigations was a gratifying and complete answer to the objections made by some to such lenses. In studying tissues made up of several laminae or layers, varying, perhaps, inter se, in their textures, small angles of aperture give a confused mixture of all the layei's at once, and the specific characters of none. We found the large angles of aperture to insulate these beautifully and per- fectly,— an effect of course valuable in the highest degree." Dr. John Bacon exhibited specimens of Foraminifera, from South Carolina, and Polycistina from Barbadoes, belonging to the Bailey collection. These fossils belong to the same group, and agree in some of their essential characters. Tire calcareous carapaces of the for- mer are perforated with numerous openings through which the animal protrudes thread-like processes of its body for nourish- ment. In the latter, the carapaces are siliceous, and, with the exception of these, there are no organisms having siliceous coverings, which have been positively determined to be animal. They have been placed in the animal kingdom from their struc- ture and the albuminous character of their substance, (sarcode,) from their motion, and from the manner of obtaining nutriment, distinct from that of vegetables. 247 Dr. Bacon also exhibited specimens of Foraminifera and Polycistina found in deep soundings of the Atlantic Ocean. Mr. C. L. Andrews exhibited specimens of Algae. Mr. Chas. K. Stevens, of Lawrence, exhibited one of Spencer's microscopes, to which were adapted a second set of lenses made by Nachet of Paris, and embodying some recent improvements. A description of a new stand for the compound micro- scope was given, and the instrument exhibited by Dr. Oliver Wendell Holmes, as follows : — The more especial object of this mechanical arrangement is to facilitate the use of the direct light of a lamp placed close to the object. Many of our microscopists must have seen Mr. Spencer use a lamp in this way, holding it in his hand and varying the distance and obliquity so as to produce the particular effect de- sired. The advantages of direct light are its easy management, its brilliant eflPects, and the more perfect definition it gives of deli- cate objects. But, inasmuch as the heat and smoke of the lamp ascend, this method of illumination can only be used with the microscope-tube (or compound body) in the horizontal or moder- ately inclined position, unless the lamp be so far removed as to lose its peculiar advantages. It is evident that the lamp cannot be used at all with the tube vertical and directly over it. If an instrument is to be employed in the horizontal or slightly inclined position, it will require a stage movement ; otherwise both hands will be needed to move the object, and will even then find it awkward to do so, as the object must be secured to prevent its sliding. Again, if the stage is inclined, and the lamp close to it, it is evident that the broader the stage the more it overhangs the lamp, and the more it is exposed to its smoke and heat. By making the stage open at top, like a horseshoe, we get rid of this difficuhy entirely. An instrument that answers this special object alone, namely, the use of direct light, can Ijc made, on the general plan of the one I show the Society, with great ease, and at small expense. 248 But as it is sometimes necessary or convenient that the object should be placed horizontally and the microscope-tube vertically, — as in examining fluids with low powers, or opaque bodies, — certain additions have been made to this model to render it capable of being so used ; reflected light, or the use of the condensing lens being substituted for the mode of illumination for which it is specially adapted. This, of course, involves the expense of a mirror and lens with their adjustments, which is, however, tri- fling, if the plan here shown is followed. The instrument is represented in working order in figure 1. The base of the whole is a box made of black walnut, three quarters of an inch thick, having two uprights, of the same mate- rial and thickness, firmly screwed to the inner edges of the strips 249 which partly cover it. On each side of the uprights, over these partial covers, are screwed two thick pieces of black walnut, with holes for the eye-glasses on one side and the objectives on the other. This box is open at one end to receive a flat-iron or other weight, if required, and to admit the other parts when the in- strument is packed. Between the uprights is received the bearing semicircle, made of three pieces of black walnut glued together, the inner one hav- ing the grain directed lengthwise, the two outer ones vertically. This is provided with a " slot " partly vertical, partly horizontal, and several notches. A binding screw holds it at any angle and at various heights between the uprights. The microscope-tube, made heavy by a leaden tube inside, is laid upon two V-shaped supports cut out of the wood, being held solely by its weight when used in the horizontal or inclined posi- tion. The microscope-tube has a ring an inch wide, fitting tight, but becoming loose on pressing its handles, and having a little projec- tion, or spur on the side opposite its handles, as shown in fig- ure 2. The anterior V-shaped support is also shown in this figure. It has a piece of brass let into the wood for the s'pur on the ring to play against. As the posterior surface of this support is slanted about one sixteenth of an inch, it is evident that in turning the tube through a semicircle it will advance or recede that distance. This turning of the tube is performed by means of the black pasteboard disk clasped to the tube near the eye-piece, which makes a sufficiently delicate fine adjustment. The horseshoe stage consists of two pieces of brass, cast and planed, 4 inches across at the widest part, and 3 inches in height. The first, nearest the observer, turns on a screw at the centre of its semi-circumference against a brass plate screwed to the bear- ing semicircle. The second turns on a screw which unites one of its arms — the right — to the corresponding arm of the first horse- shoe. The first horseshoe therefore carries the other with it ; the second turning very easily, is moved independently of the first- The handles are flat, the one with the cross next the observer, the other projecting three quarters of an inch beyond it, so that a 250 slight change of the thumb determines whether one alone shall move, and the object be carried up and down, or both, and the object move from side to side. Figure 3 shows the principle of arrangement, and figure 4 the object-holder with its springs, which is held against the horseshoe by a piece of brass plate screwed upon the latter, as shown in figure 1 — the object-holder sliding between the two. The tray that holds the lamp is of sheet-iron, 5 inches by 3, with a ledge of half an inch in width at its remote edge. On this tray rests a thin piece of wood of the same size, covered with velvet. The lamp having its base covered with velvet also, cannot slide ofi', even when the microscope is much inclined, — but the lamp, with the piece of wood on which it rests, is easily slid from side to side. Fig. 5 represents the diaphragm with the achromatic condenser. This is arranged in place by sliding its foot under a spring upon the same piece of wood to which the tray for the lamp is fas- tened. The dimensions of various parts not yet given are as follows : Inside dimensions of the box, length 8 inches ; width 5 ; height 2 ; from bottom of inside of box to binding screw, 1 1 inches. Dis- tance between uprights 1|^ inch. Bearing semicircle same thick- ness. Radius of this semicircle Z^ inches. Object-holder 7 -[-2. Diaphragm 3 inches in diameter. If desired to use the microscope in the vertical position, the tube must be held firmly against the supports, the tray removed, and the mirror represented in figure 1 brought into its place. A loose ring of plate brass capable of being made fast to the bear- ing semicircle serves to fix the tube. The mirror is a plane one, set in an open frame. If a plano-convex lens is placed over it, it acts like a. concave mirror ; if the mirror is removed the same lens may be used as a condenser. In packing this instrument, the tray and diaphragm go at the bottom of the box, the bearing semicircle is held by the binding- screw between the uprights, and the pasteboard disk is held at the side of one of the uprights. The lamp and other accessions go into the box. The leading peculiarities and novelties of the instrument will now be indicated. 1. Union of stability and portability. The base gives a suflS.- 251 cient degree of steadiness for common purposes. But by sliding a couxmon Jlat-iron into its interior it becomes as firm as the most ponderous instruments of Ross, which are too heavy to be carried about with comfort. 2. The facility with which the heujht of the compound body, as w-ell as its inclination, may be varied by means of the " slots " and notches in the bearing semicircle. 3. The mode of focal adjustment by rotation of the tube, or compound body. This has a movable ring upon it with a pro- jecting spur, which bears against the slightly inclined posterior surface of the anterior V-shaped support of the tube. The disk which protects the eyes is used as a levei", and thus a very smooth and uniform motion without the smallest amount of " lost time " or " back lash " is obtained without rack and pinion, spring or screw. 4. The open horseshoe stage, with the movable object-holder received upon its remote (anterior or inferior) surface, the glass object-slide being itself pressed by springs against the remote surface of the object-holder. It follows from this arrangement, 1st. That if one object is in focus, all others mounted in a similar manner are in focus, or very nearly so ; 2d. That the thickness of the stage becomes practically reduced to nothing, as the glass slide is next the lamp, and behind, or below, every thing except the springs that press it forward against the remote face of the object-holdei". 5. The double radial stage-movement. The horseshoe piece next the observer turns from side to side on a screw passing through the lower or middle portion of its arc. The other horse- shoe piece turns on a screw fixing it to one arm of the first, so that it moves up and down. The arcs they follow form so small a part of a circle that the eye cannot distinguish their movement from a rectilinear one. The holt and crossbow flat handles, working singly or together, make the management of the stage movement very convenient. 6. The flat-wicked lamp, so mounted as to move freely without the possibility of slipping, at whatever angle the apparatus may be inclined. 7. The combination of mirror and lens in an open frame, so as, by slight alterations, to serve a triple purpose ; that of plane mirror, of a condenser, and of a substitute for the concave mirror. 252 8. The simple and elFective mounting of the achromatic con- denser and the diaphragm attached to it. It remains for others to determine if any or all of these inno- vations are improvements. August 19, 1857. Dr. Chas. T. Jackson, Vice-President, in the Chair. Dr. D. F. Weinland read a paper entitled — Some Points in the Zoology of Hayti, — as follows : — A few weeks since I returned from nearly half a year's so- journ on the southwestern neck of that beautiful mountain-island, (this is the meaning of the Indian name Hayti,) and I wish to communicate to my scientific friends some of my impressions and observations,-"^ whilst they are fresh in my mind, even if they should yet lack the stamp of elaboration. I shall speak first of the organic life of the sea-shore, and since this depends upon the geological formation of the coast, and upon the nature of the sea, these subjects will first be introduced. I. THE SEA-SHORE. The noiihern shore of the southwestern neck of Hayti is mostly cote de fer, that is, an iron-bound coast. There ai-e but few small sandy bays, which serve as landing-places for the fish- ing boats, and near them are generally found huts of fishermen, or a small village. The rock which bounds all the rest of the coast is a hard brit- tle limestone, formed very generally of a conglomeration of mad- repores and other corals, as AstrEcae, Mgeandrinas, Milleporse, etc. and of various kinds of shells, cemented with a mass of smaller and formless lime-particles, the powdered particles of the same corals and shells. This rock is full of pores and roundish cavi- 1 Most of these observations -were made in company with my friend Mr. Ed- ward Habich of Boston, a member of our Society, on our daily walks along the sea-shore, or during our excursions up the rivers or back in the forests of the interior. 253 ties with sharp edges, perhaps the places where softer shells or fragments of corals have been washed out by the erosion or attrition of the water, or knocked out by corals, thrown up in the stormy winter season of the furious north wind. The species of corals and shells which enter into the composition of this rock, I found nearly all alive in the adjoining sea. Some of them, how- ever, have disappeared from among the living ; others are dying out, and are now very rarely found, though common in the earlier portions of the present period ; for they exist in great quantities in the rock at the depth of a few feet. Such animal remains enclosed in rock, yet belonging to species now living, or to species now extinct, but which lived in the earlier ages of this period, together with species now living, we are accustomed to call modern fossils. They are the more interesting because they show how, without any remarkable revolution of our globe, cer- tain species of animals gradually die out. The same rock, composed of modern fossils and their detritus, I found in the interior mountain regions of the island, about thirty miles from the sea-shore, and at a height, as I should judge, of at le^st one thousand feet above the present level of the sea. In- deed, the whole first, that is, northernmost, ridge of mountains which runs along that northern sea-shore of Hayti, from east to west, is crowned with large layers or broken masses of this same kind of rock, which being, as stated above, a formation of the present geological period, goes far to show that this whole ridge has been raised in this present period. Thus the existence of the greater part, and the configuration of the whole of the southwest- ern neck of the island of Hayti is of a comparatively recent origin. Two questions at once suggest themselves here, whether the for- mation of the same roch, and whether the elevation of the land, are going on at the present time. That the former, the formation of the same limestone rock, is really in progress at the present day, seems to be evident in some places, where the whole bottom of the sea near the shore, at a depth of from one to five and six feet below low-water mark, is, as it were, a flat pavement of the same kind of rock. Crust-building corals, as Porites, Ma^andrinas, Sideras- trseas, etc. live upon it, and in the interstices of these are thrown up from below dead shells, broken Millepores, Madrepores, and 254 Astrseans. By the powerful action of the waves on the shallow bottom, these remains are broken and ground upon each other, and their form is lost. The lime powder which results from this pulverizing action furnishes the cement which fills the shells and unites the pieces into one solid mass, Magonnerie hon Dieu (God's Masonry) as the negroes of the French colonies call it. In consideration of these facts the first part of our question may be answered in the affii'm- ative. But whether the whole coast is constantly and gradually rising, (as we know is the case with the coast of Sweden,^) or whether those different layers of that submarine pavement have been thrown up at various periods, by sudden volcanic agencies, I am at a loss to decide from my own observations. I will only state that the layers which lie now just above low-water mark, are (for instance, in some places in the neighborhood of Jeremie) quite undisturbed banks, running in a plain parallel to the level of the sea. This seems rather to favor the idea of a gradual rising than of a sudden upheaving, and the latter would be more likely to fracture the layers and to change their original horizontal position into an angle towards the horizon. I conclude, from the information afforded me, that this lime- stone formation must extend over the whole northern part of Hayti, from its western cape (Tibouron) to the neighborhood of Port-au-Prince. Further, the rocky part of the sea-shore of Bar- badoes, Maria Galante, of Grand-terre in Guadaloupe, of An- tigua, St. Bartholome, St. Martin, Arguilla, and Santa Cruz, seems to be of the same composition and age. I should judge so, also, from an account of William Maclure, published just forty years ago in the Journal of the Academy of Natural Sciences of Pliila- delphia, vol. i. p. 134, et seq. Further also, the honeycomb limestone of Jamaica is the same rock, according to a communi- cation of my friend Dr. Hyde,^ who lived in that island for many years. 1 According to the observations of Leopold von Buch, Hallstroem, and Lyell, the whole northern coast of Sweden and that of Finland is continually rising at the rate of four feet in a century. See also Humboldt's Kosmos, I. p. 315 and p. 472, et seq. 2 Dr. J. S. Hyde, of New England, a zealous and experienced conchologist, by whom were collected many of the Jamaica land-shells, which were described by 255 1 have not yet had an opportunity to look for other geological reports of the Antilles. I suppose, however, that this is the same limestone formation, which the negroes in Guadaloupe very ap- propriately call " God's masonry," and which is so evidently a formation of modern time, since it encloses instruments made by man, and even those once celebrated, supposed fossil human skel- etons. If we want a name for the Haytian limestone described above, we might call it the modern " Coral-rag," for if it had not been for the difference in the fossil remains, I should have recognized it as exactly the same limestone, which forms those steep, porous rocks of the so-called rough Alps of Southern Germany, between the Danube and Rhine. Indeed, it was not a slight pleasure for me to see here clearly, how those old rocks of my home must have been formed in their time, millions of years. ago, when Southern Ger- many was yet an island not much larger than Hayti, having a wax-m climate, and surrounded by a warm ocean ; and presenting, all along the coast, the same banks of corals ; and in the cavities of these rocks the cidarites, which abounded then, and of which I found one species alive in Hayti. But this also is so scarce as to show that its days have passed. II. THE SEA OF NORTHERN HAYTI. Beyond the formation of the coast there are some features con- nected with the sea, which borders upon the northern side of that island, which are of the greatest importance to its animal and vegetable life. 1. The great respiration of the ocean, the ebbing and flowing of the tide, hardly touches that coast. Neither the native fishermen along the coast, nor the American captains in the harbor speak of high and low water there. The great tide wave is not only broken by the wall of islands in front of the Mexican Gulf, but, perhaps, is even neutralized by a continual current, which runs from east to west all along the northern shore of Hayti. the late Prof. Adams, tells me that he found this limestone, particulai-ly in the northern part of that island. He noticed it for its peculiar richness in Cyclos- tomas, which live in the cavities. 2 See Humboldt's Kosmos, I. p. 260. 256 2. All the motion of the sea on that shore depends upon the wind. Its agencies are twofold ; first, the daily change of sea and land wind, the former beginning to blow in the morning about eight o'clock, the latter in the evening between six and nine. The latter is much more constant, and being also more powerful, it depresses, every evening, the level of the sea all along the coast from one to two feet. But there is, secondly, another, a yearly change of the winds, viz : a prevailing northerly wind in winter, particularly in December, January, and February, and a prevail- ing southerly wind in summer. This great change produces this eiFect, that in the season of the North, as they call it there, the level of the sea is constantly, on the average, eight feet higher than in summer. How much this change bears, also, upon the organic life of the sea-coast, is evident. I will only state that during the last week of May and the first of June, in one place not larger than an acre, more than a hundred Actineaj and Holothurias died, because left upon dry land ; not to speak of the thousands of other ani- mals, fishes, echini, etc., and of sea-plants which died in those natural basins near the sea, where the water, cut off" from the refreshing ocean, was overheated by the nearly perpendicular rays of the tropical sun. The rising of the land from the waves, the same that we know took place repeatedly in the great epochs of the history of our globe, and which, as Dr. J. D. Dana once said, brought death among the sea tribes in one universal desolation, — the same we see now on the northern shore of this island, i-e- peated annually with the change of the winds ; and though on a smaller scale, yet destroying hosts of living organisms. More- over, in that stormy season of the North, the whole bottom of the ocean, all along the shore, at more than five fathoms depth, is swept, and not only all the dead remains but many living shell- fishes, and large blocks of corals, are dashed against the iron- bound coast and thrown up on dry land. This is the season dreaded equally by the Haytian coasters and tiie merchant vessel in the harbor. The former, when overcome by a dark, stormy night, without a compass, an instrument unknown to them, are driven helpless along the shore, and their small boats frequently thrown against the rocks. The latter, the merchant vessel, drags 257 its anchors on the moving bottom of the sea (called rade marec) and runs ashore.^ Besides the motion of the sea, there is one circumstance more worthy of notice, as bearing upon the organic life of this sea- shore. It is the chemical composition of the sea-water. The sea- water contains, at this distance (about eighteen degrees) from the equator, the greatest amount of salt in solution ; more than the water near New England, and a good deal more than the sea immediately under the equator. This remarkable fact has been shown by Linz, a German scientific traveller, on his voyage round the world.^ The rivers of the northern shore of Hayti are not large enough to exert an extensive influence upon the composition of the sea-water, even in the immediate neighborhood of their mouths, and, moreover, they are generally barred up by sand-banks during a great part of the dry season. These sand- bars prevent again a large pouring in of sea-water into the river, and thus the river water is quite fresh and sweet in the immediate neighborhood of the sea, so much so that vessels take in their drinking water there. But notwithstanding this, (and it is an interesting physiological fact,) I found relatively more sea-fishes going up annually from the sea into these rivers, than ascend the German rivers ; showing how flexible their nature must be to bear the sudden change in the saltness and density of the water, when passing from that deeply saline ocean into fresh water. The case is different with those sea-fishes of New England and Germany which enter rivers ; they have always to pass through brackish water, and thus the change is effected gradually. (To be continued.) Dr. C. T. Jackson said that he had found in analyses of sea-water from coral regions a greater amount of car- bonate of lime than is found in water from other parts of the ocean. He supposed it to be derived from the decom- 1 In the harbor of Jeremie, which is uot protected against this north wind, two vessels ran ashore at one time during one of the last winters. This occurs nearly every year. 2 See Humboldt's Kosmos, I. p. 320, where we find also the reason for this re- markable phenomenon. PROCEEDINGS B. S. N. H. — VOL. VI. 17 NOVEMBER, 1857. 258 posed corals, rather than a natural ingredient of the water and the source of coralline growth. Dr. Jackson exhibited the shells (Alasmodonta arcuata) which were presented at the last meeting by W. E. S. Whitman, Esq., of Gardiner, Me. This species is found in the rivers of Kennebec county, and being lined with a pearly secretion, the shells have been sought for in that neighborhood for pearls. The thanks of the So- ciety were voted for the gift. Dr. Weinland called attention to the fact that the outer surface of the shells, near the hinge, was considerably eroded, and he referred to a communication of Dr. James Lewis, of Mohawk, N.' Y., read to the Society February 18, 1857, in which the pres- ence of saline alkalis is assigned as the cause of erosion by that gentleman, contrary to an opinion expressed by himself in a paper read to the Society October 15, 1856. He disagreed with Dr. Lewis upon this point, for he believed that the animal absorbs from the water only such substances as ai'e suited to its nature. Dr. A. A. Hayes stated that where the composition of the water is changed at different seasons of the year, there is great liability to erosion. He attributed the effect to the presence of organic acids, as humic and ulmic acids or mixtures of the two, which he said were at certain times sufficiently strong to attack the epidermis of the shell. He referred to changes in the Con- necticut, Concord, and Schuylkill rivers, the last two of which have been so much altered in their composition by impurities introduced in mining operations or otherwise, as to render them more or less destructive to animal life. Dr. Weinland remarked that he could not believe any waters to be so strongly acid as to be capable of destroying the epider- mis. In his paper referred to above, which he had read to the Society, he had maintained that the first step of the erosive process vpas the destruction of the epidermis by a worm. Dr. Jackson thought from the appearance of the smallest per- forations that the destruction of the shell originally commenced with a worm. Mr. T. J. Whittemore observed that the shells in Fresh Pond 259 Cambi'idge, are ei-oded, whilst those in a stream near the pond are unaffected except in certain portions of it where there is a clay bottom. In the Middlesex Canal they are free from ero- sions, but in Concord River the opposite is the case. Dr. Weinland said that the observation ©f Mr. Whittemore sustained his view of the question. The worms which infest the shells do not live in sandy bottoms, and he had generally noticed the erosion of the shells to extend just so far only as they are im- bedded in the clay. Mr. C. J. Sprague called attention to the fact that the corroded surfaces are in some instances covered with epidermis, which may have been a new growth from the neighborhood of the hinge. Dr. Jackson said that he had frequently seen the animal taken out of the shell by the mink or musk-rat, the sun having previously killed the animal and expanded the shell. Mr. Whittemore said that the common belief, that the musk-rat brings out the mollusk from the water, and leaves it upon the shore in the heat of the sun for this object, is probably true. Mr. F. H. Storer exhibited crystals of Sulphide of Lead obtained by sublimation; one of the accidental pro- ducts of a smelting furnace in Germany. He remarked upon the exceedingly great volatility of this compound of lead, and upon the influence which its presence in the atmosphere, even at a great distance from the furnace, exerts upon the vegetation of the region. It has been shown by analysis that large spruce trees, six or eight inches in diameter, contain lead, even in their innermost parts, which had evidently been taken up by the roots. Dr. C. T. Jackson gave an account of the Sand-Sharks which are caught near Nantucket. While upon the island recently, he had seen some brought to the shore eight or nine feet in length. From the liver is extracted on an average a gallon of oil, which is used by curriers, and worth seventy-five cents a gallon. The body is used for manure. 260 Dr. Jackson presented, in the name of Amos Otis, Esq., a brick of peculiar shape, and apparently imperfectly- made, which was found at Monamet, near Sandwich. It came from a locality, interesting in a historical point of view, as having been the spot where the Pilgrims built a trading-house in the year 1627. The thanks of the Society were voted for the gift. Mr. C. K. Dillaway exhibited the tooth of a Narwhal, [Monodon monoceros, Lin.) It was about seven feet in length, and a very beautiful and perfect specimen. Messrs. Thomas R. Sullivan and Joseph Willard, Jr., were elected Resident Members. September 2, 1857. The President in the Chair. Mr. Theodore Lyman read the following paper on a new species of Coral : — In October, 1848, and April, 1849, Milne Edwards and Jules Haime published two monographs on the Astreida;, (Annales des Sciences Nat. S^""*^ Serie, torn. 10 et 11.) Under this name they included only a part of the Astra3ans of previous authors, namely, such only as had platforms or dissepiments between the lamellie, and these they call traverses. They further divided the family into two sub-families, Eusmilinos and AstreinjB ; the former com- prising those with smooth-edged lamellje ; the latter, those whose lamella3 bore teeth. Descending to genera, they subdivided these to a very great extent. Dana's Genus Euphyllia is sepa- rated into nine groups ; Lamarck's Genus Astrosa, as understood by Dana, is multiplied to nearly twenty ; and, in addition, there are added to the family some forty or fifty quite new genera, many of them comprising only fossils. To sum up ; the family 261 to which Dana, in 1847, apportioned thirteen genera, appeared, the year after, under tlie auspices of Edwards and Ilairae, with about eighty. Tlie comparison, philosophically conducted, of these two classifications, would be of the highest interest, but I speak of them now only in connection with a new species of Astrajan, recently fallen upon, in arranging the cabinet of this Society. Its discovery furnishes one more proof of the absolute necessity of some laws, plain and sure, by which classification may be determined. A description of the coral will show the difficulties under which a natui'alist must, in such a case, labor. AsTR^A DECACTis, Lymau. Polyps short and budding from the upper edge ; consequently the corallum takes the form of a thin plate, which, in this case, is somewhat wavy, and has a few swelhngs on its surface. A ground surface shows the corallum, between the calicles, to be solid, with a few very small pits, or vesicles ; this is generally the case, but, where the calicles are a good deal crowded, the intervening corallum is made up of a double row of vesicles. The calicles, when not crowded, are nearly round, but each is surrounded by a fence of grains, which takes the form of a more or less regular hexagon. These grains cannot be seen without a lens ; there are generally about five on a side, (in all about thirty,) and the fence, which they form, is situated midway be- tween each calicle and its neighbors. The calicles are from one half to three quarters of a line in diameter, and are remarkable, not only for their small size, but also from the fact of their hav- ing only te7i stout lamellfe. These laraelh^ are sensibly smooth on their sides and edges, (and the species would thus come under the Sub-Family Eusmilinai of Edwards,) they are considerably exsert, and extend outward a little beyond the edge of the cali- cle ; inwards, they run to a point nearly half-way to the centre, when they pitch suddenly downwards and become thinner ; at the centre they all join a solid columella, which has an oval form, and projects above the level of the lamellae, at their point of juncture with it. On examining a calicle with a strong lens, there may sometimes be seen, on the edge of the calicle and mid- way between the lamellfe, fine points, or grains, whose size does 262 not exceed that of the grains of the fence. Although these bear no sort of proportion, compared with the ten strong lamellfe, still, for reasons that it would take some time to tell, I am inclined to look on them as true lamella, in a rudimentary stage. In some calicles they cannot be discovered at all ; in others there are two, and, in rare instances, there are as many as ten, or one between each pair of large lamellae. A vertical section of a calicle shows the characteristic dissepiments {traverses, Edw.) of a true As- trsean, and a styliform columella, which continues nearly, or quite, to the bottom, though with a diminished size towards its lower extremity. In this species the columella gives the same indication of a bilateral symmetry that is shown in the elongated mouth of Actinia, and, among the Halcyonoids, in that of Renilla, &c. In a line with the longest diameter of the columella there are, almost always, two lamellie, and, on each side of the axis thus formed, four lamella? symmetrically arranged ; and it is to be further observed, that the calicle itself has a tendency to elon- gate itself in the direction of this axis. The corallum is covered underneath with a thin, slightly folded epitheca ; and above it has a rough look, under a lens, by reason of its crowded calicles, and stout, exsert lamella?. Now, as regards the place this species should occupy among Astreidffi, if we go by the system of Dana, it would come under the Genus Astrjea, and would be among the species of the Sub- Genus Orbicella, from which it differs only in the less numerous rays. If, on the other hand, we refer to Edwards and Haime, we find that it agrees with no living genus, but is \qyj near to, if not identical with, the Genus Astroccenia, which is entirely fossil, and, with the exception of one species, does not rise higher than the chalk. With this genus it agrees in growing in a plate; in having an epitheca a little folded ; in marginal budding ; in polyps soldered by their walls ; in a solid, styliform columella ; in having thick lamella*, and in having small calicles. If the genera of Edwards are really to be admitted, it would be curious to see this old habitue of the chalk once more among the living. A description of the genus will be found in the Annales des Scien. Nat. S*^™*^ Serie, tome x. page 296, and figures in the Paleonto- graphical Society Monograph on British Fossil Corals, 1850, Part I. Plate 5 ; and in Denkschriften der Akademie zu Wien, 263 vol.7. Reuss liber Kreideschichten, Plates 8 and 14. Of these, the A. magnijica, figured by Reuss, resembles most the present species. Considering, however, that the genera of Edwards have been looked on with some misgiving, by more than one good authority, and particularly in respect to the characters taken from the teeth of lamellte, and the so-called columella, I deemed it safer to leave this species, for the present, among the members of the Genus Astrasa, as received by Dana ; though, at the same time, I feel pretty sure it will have to be removed therefrom, as soon as the classification of polyps is better understood. The specimen from which this description was taken was growing on a sponge. The plate was about 2^ inches long, 1^ inches broad, and 3 lines thick, at the thickest part. The edges of the plate were in some places very thin. Dr. A. A. Gould thinks the sponge a West Indian species, and this, com- bined with the fact that it was in the same case with Mr. Bart- lett's Florida collection, makes it very probable that this species inhabits Florida. The President gave a brief account of some facts noticed during a recent visit to Surinam. The committee appointed to consider the expediency of dividing the Department of Crustacea and Radiata, reported in favor of the project, and the report was adopted. H. R. Storer, M. D., was elected Curator of Crustacea. Messrs. James H. Weeks and George N. Faxon were elected Resident Members. DEPAETMENT OP MICROSCOPY. Dr. John Bacon exhibited three different forms of oxalate of lime, occurring as a deposit in the urinary secretion, remarking that they were interesting in a pathological point of view, as well as from their chemical relations. They were, first, the ordinary, apparently octohoedral form ; secondly, the rare dumb-bell form ; 264 and, thirdly, crystals which he had now seen for the first time, six-sided tables, often very thin and transparent, and resembling cystine in appearance. They were accompanied in the speci- men by thicker rhombic tables, more or less modified, and he considered them all modifications of rhombohoedrons. He also exhibited crystals of oxalate of lime from the vege- table kingdom. Prof. Bailey called attention some time since to the large amount of oxalate of lime existing in the bark of certain trees, the {)rincipal ingredient of the ashes of which was carbon- ate of lime, a salt arising from the decomposition of the oxalate and other organic salts of lime. This excretion from the human body Dr. Bacon has noticed to be quite common in Boston, but it cannot be due to the use of water containing lime salts, for the Cochituate water is now almost universally used, and this, it is well known, is one of the purest of pond waters. He would not even consider a small amount of oxalate of lime deposited from the urine as a morbid indication, for this salt is so insoluble that a precipitation of it in a certain quantity may be regarded as not inconsistent with health. An ingenious instrument, in brass and steel, for mak- ing fine sections of "wood and other articles for micros- copic examination, was presented by Edward C. Cabot, Esq., and the thanks of the Society voted for the dona- tion. September 16, 1857. The President in the Chair. Mr. Charles Stodder read a paper on the vibrations caused by the falling of the water over the dam at Had- ley Falls, as follows : — A paper was read at the Montreal Meeting of the American Association for the Advancement of Science, on the vibration caused by the falling of the water over the dam at Hadley Falls, The same matter has been the subject of discussion in this 265 Society, by Messrs. Briggs and Desor in 1850, (Proc. vol. 3, p. 287,) and by Mr. Briggs in 1852, (vol. 4, p. 185.) The only cause for the phenomenon that I have seen assigned is the agitation of the air, behind tlie falling sheet of water. Tliis theory is effectually disproved — if there were no other reasons against it — by the fact cited by Mr. Briggs, of the dam at Lewis- ton, where the water falls over an inclined plane, leaving no space for air under it ; yet the vibrations are very decided. The case of Hadley Falls seems to have attracted more atten- tion than elsewhere, as probably the vibrations are moi-e power- ful, and have been noticed at greater distances than in other places. I expect to show that the causes of the vibrations are there found nearer a maximum, and the intensity and force of the vibrations, as well as the distance at which they are felt, ought to be greater there than at any of the other places which have been referred to. The dam at Hadley is 1,000 feet long, at nearly right angles to the current of the river, and causes a vertical fall of thirty or thirty two feet. The water does not fall in an even stream from the summit of the dam to the surface of the water below, but the upper surface in section presents to the eye a waved or curved outline. This appearance I have noticed at Hadley, Nashua, Lawrence, and at every other vertical fall which I have ever seen, when under the proper conditions to exhibit it. If we could see the under side of the sheet, we should find, undoubtedly, correspond- ing appearances on that side. This phenomenon is caused by the property of falling fluids, by which they assume the globular form, which may be seen in the Kauterskill Falls, on the Cats- kill Mountains, where the whole body of falling water is broken into spray and drops — in the fall of water from the jet of a foun- tain, and in water flowing from a vessel. In all cases, if the water falls a certain distance, proportioned to its mass, the whole will assume the globular form, and become drops. Applying this principle to the fall over an artificial dam, the water at the very commencement of its descent begins to assume that form, and the further it descends, the nearer it approaches it. In pass- ing over an artificial dam, like that at Hadley, the water presents a uniform depth throughout the whole length of the dam ; and if we imagine the current of water to be an infinitude of small 266 streams, of uniform depth, in contact with each other, each hav- ing the same tendency, the result must be to produce swelHngs and contractions throughout the whole extent of the dam. Now, when each of these waves strikes the bottom, it gives a blow pro- portioned in force to the body of water falling from the height of the dam. A certain depth of water running over the top of the dam must fall a certain distance before it would be entirely sepa- rated into globules. The smaller the quantity of water, the less distance is required ; consequently every variation in the depth of the water causes a variation in the size and distance of the waves, or tumors ; each of these causes a concussion propor- tionate in intensity to the weight of water in it, and proportionate in rapidity to their distance apart. These effects of falling water should be expected, in general, only in artificial falls, such as mill-dams. In natural falls, it is rare that a vertical face is presented for the water to fall over ; and even if such a fall is presented, it is usually formed of angu- lar rocks, causing various depths of water ; and as every varia- tion of depth alters the conditions, the space required to form the tumors in, there would be no coincidence among the tumors formed in different parts of the falling stream ; so that tlie waves of one part would strike the bottom, in the intervals of those of another part, and tlius the concussion of one neutralize the other. Ao-ain, to produce the vibrations, the stream should fall from an equal height throughout its width. If one part falls thirty feet, and another twenty-five feet, the same result is produced as by differ- ent depths of water. For this reason I conclude that vibrations are not conspicuous at Lawrence. There the dam is diagonal to the stream, and there is considerable difference in the height of the fall, at the two ends of the dam. At Hadley the conditions for causing vibrations are, if we cannot say at the maximum, at least the most favorable of any we know. The height of the fall is considerable — great for an artificial work — and so is the width of the stream. The height is uniform from side to side. The dam is one right line from bank to bank, the bed of the river is solid rock, an almost level floor, free from loose or piled up masses. The top of the dam is perfectly level. Conse- quently there is an uniform depth of water passing over the whole length, falling an uniform distance. The waves or tumors 267 of the falling water are uniform, and strike the bottom with syn- chronous concussion from one end of the dam to the other. It is not surprising that the earth should be felt to vibrate in Spring- field, seven miles in one direction, and in Amherst, fourteen miles in another. Another interesting line of inquiry arises here. Hadley Falls, Springfield, and Amherst, are all situated on the red sandstone of the Connecticut valley, I will venture to say that the vibra- tions have not been felt beyond the boundaries of that rock on either side of the valley. Further between Amherst and Hadley we have the intruded trap, forming Mount Holyoke. This trap is said by Prof. Hitchcock not to be a dyke, crossing the strata of sandstone, but to be interposed between the beds of sandstone. This of course is the interjiretation of such parts of the trap as can be examined, but the trap might have cut through the strata of sandstone at some great depth, and only be interposed between the strata near the surface. I believe the fact that these vibra- tions have been felt beyond the trap rock, indicates that it does not cut off" the strata of sandstone at any great depth — that, if it did so, it would cut off the vibrations. Now if the trap lies entirely be- tween strata of sandstone, it may not have been injected, but it may have been poured over the surface of the underlying stratum when that was the uppermost. Dr. C. T. Jackson, instancing the vibrations noticed at the Dam at Nashua, stated, that, in that place, the vibra- tions only take place when the wind is in such a direc- tion as to break the fall, and permit of the escape of air, which is evidently confined behind the sheet of water. Mr. Theodore Lyman read an extract from a letter of Mr. Bowerbank of London, acknowledging the reception of some sponges sent him by the Society, and promising to send a collection of sponges in return. Mr. B. is de- sirous of obtaining specimens of a spongilla which he says he learns is common in the Cochituate water-pipes of Boston. 268 Dr. Gould said that he had frequently seen a species of spongilla in these pipes. Dr. C. T. Jackson said that specimens could be ob- tained at the Brookline reservoir gates. They are of a yellowish green color. Dr. J. B. S. Jackson said that he had met with small specimens in the pipes of his house, perhaps two or three lines in diameter, and seven or eight in length. Dr. A. A. Gould said he had received a letter from Prof. Dawson of Montreal, stating that there had recently been a slide in the neighborhood of that city, by which many new species of tertiary fossils were exposed, and amongst them some spiculae of sponges. Dr. J, B. S. Jackson exhibited specimens of Dermestes and a block of wood, forming the support for an anatom- ical preparation, into which wood the insect had eaten. He was not aware before that this animal attacked wood. Dr. C. T. Jackson presented, in the name of Samuel Swan, Esq., some specimens of the common Water Lily, [Nymphcea odorata.) They were procured from a pond in Yarmouth, Mass., and were peculiar in this respect, that the flowers were of a delicate pink color, instead of being, as ordinarily, white. Dr. J. had noticed, several years since, in Mossy Pond, in Lancaster, this same lily with flowers of a deep red color. He suggested that they were probably only varieties of the same species pro- duced by ferruginous or other modifications of the soil in which they grew. The President exhibited some species of fishes from the Surinam River, and mentioned some conditions, here- tofore unnoticed, under which the eggs are developed. In a species of Bagrt^ called by the negroes " Ningi-ningi," 269 tlie eggs are carried during the whole period of development in the month. Dui'ing the month of June, the females have their mouths filled with eggs, and tiie young may he seen in all stages of formation, if a large number of individuals is examined. There are at least four species of Siluroids which have this liuhit. The Aspredos, or " trompettis," likewise have a peculiar mode of gestation, analogous to that found in Syngnathus. In Aspredo the eggs are attached, by means of pedicles surmounted by cups, to the under side of the abdomen, as far forwards some- times as the mouth, on the sides to the pectoral and ventral fins which they sometimes cover, and as far back as the mid- dle of the tail. Valenciennes describes the appendages which support the eggs of Trompetti, but nowhere expresses the opinion that they were destined to carry eggs. After the eggs are hatched the pedicles are absorbed. A specimen of Hylodes lineatus w^as also exhibited, showing the manner in which the young are carried upon the back of the parent. In Hylodes, we have one extreme of a series which commences with Pipa, where each egg is carried in a separate pouch in the back of the fiemale ; in Notodelphis, as shown by Dr. Weinland, all the eggs are carried in one dorsal pouch ; in Alytes, the eggs in strings are wound round the legs, and finally^ in Hylodes, the tadpoles adhere to the back of the parent without any protection. Though having all the organization of a tadpole, viz : gills and a tail adapted to swimming, they are found in the woods on the back of the parent at a distance from water. The early stages of development are unknown. The habits of Hylodes, as well as those of the fishes above referred to, are well known to the negroes of Guiana. DONATIONS TO THE MUSEUM. July 1, 1857. Nest and Eggs of Baltimore Oriole, Yphantes Baltimore; Bobo- link, Dolkhmiyx m-izivorus : Maryland Yellow-throat, Trichas Marilmidicus ; Bam Swallow, Hirundo rustica; Cedar Bird, Amjielis c/arrulus; Lesser Pewit Fly- catcher, Muscicapa fusca ; Wilson's Thrush, Twdus fuscescens ; Blue Jay, Cy- 270 anocorax cristatus ; Eggs of Spotted Tsitler, Totanus macularius ; Passenger 'P\ge.on, Ectopistes migratorius ; Nest of Chimney Swallow, Cypsebis pelasgius ; by Francis S. Williams, Esq. Scarlet Ibis, Ibis rubra ; by Mrs. Curtis B. Ray- mond. Petrified Wood and Bone; by S. A. Green, M. D. Geological Map of the United States ; by Jules Marcou. Shells from the Cape de Verde Islands, Cuba, and the Western Coast of Africa, and Volcanic Matter from the Cape de Verdes ; by Mr. N. H. Bishop. A Crawfish from North Carolina, Vitreous Cop- per Ore, and Argentiferous and Auriferous Galena from the same State ; by Dr. C. T. Jackson. July 15. Ripple Marks in Sandstone, Algee, and Parasitic Shells ; by Dr. S. Kneeland, Jr. A Horned Toad from Texas ; by Mr. Ainsworth. August 5. Specimens of the shell, Alasmodonta arcuata, which is opened for pearls in Maine ; by W. E. S. Whitman, Esq. Specimens of a Smelt, Osmerus viridescens, taken in Squam Lake, New Hampshire, and of two species of Leu- ciscus, one probably undescribed, from the same locality; by Dr. H. R. Storer. August 19. A Brick, interesting in a historical point of view, having been taken from the ruins of a trading house, built by the Pilgrims near Sandwich, in the year 1627; by Amos Otis, Esq. Samples of the Soils of Michigan, Mis- souri, Indiana, Minnesota, Wisconsin, and Iowa; by Dr. S. Kneeland, Ji-. September 2. A brass instrument for making fine sections of wood and other articles; by Edward C. Cabot, Esq. A collection of one hundred and forty Bird Skins forwarded by the Government National Museum of Melbourne, to the Boston Society of Natural History, viz : — Menura superba, Lj-re Bird ; Podiceps AustraUs, Australian Grebe ; Cacatua Leadbeaterii, Leadbeater's Cockatoo ; Ptilonorhynchus holosericeus, Bower Bird; Platycercus Barnars, Barnars Par- rakeet; (rj-zts ^MsiraZasiajiMs, Australian Crane; Cereopsis Noiub Hollandioe., Cere- opsis Goose ; Pedronomus iorquaius, Plain Wanderer ; Heinipodms pyrrhothorax, Chestnut-breasted Hemipode, three specimens; Liniosa melanui-oides, God wit; £nlomo2jhila jncta, Painted Honey-Eater; Recurvirostris rvbricollis, Red-necked Avocet ; Psophodes crepitans, Coach-whip Bird ; Platycercus Pennaniii, Pen- nant's Parrakeet; Fidica AustraUs, Australian Coot ; Plialacrocorax carboides, Australian Cormorant ; Athene strenua, Powerful Owl ; Casarca tadornoides, Mountain Duck; Porphyria melanosiis, Black-backed Porphyrio; Artamus super - ciliosus, White eyebrowed Wood-Swallow, two specimens; Gymnorhina organ- icum, Tasmanian Crow-Shrike; Anas punctata, Chestnut-breasted Duck; Nycti- corax Caledonicus, Nankeen Night-Heron ; Podiceps popicephalus. Grey-hooded Grebe, two specimens; Spheniscus minor, lAttie Penguin; Lobevanellus lobatus, Spur-winged Plover; Sterna melanauchen, Black-naped Tern ; Cacatua Eos, Rose-breasted Cockatoo; Biziura lobata, Musk Duck; Cinclosoma punctatum, Spotted Ground-Thrush ; Campephaga Jardinii, Jardines Campephaga, two spe- cimens; Artamus personatus, Masked Wood-Swallow; Petroica Goodenovii, Red- capped Robin ; Melithreptus melanocephahis, Black-headed Honey Eater, two specimens; Rhipidura j-jy^/rons, Rufous-fronted Fantail, two specimens; Hemi- podius velox. Swift-flying Hemipode, two specimens: Himantojnts leucocephalus, White-headed Stilt; Estrelda temporalis, Red-eyebrowed Finch, two specimens ; Amadina Lathamii, Spotted-sided Finch, two specimens; Eiaticula bicincta, Dou- ble-banded Dottrel; Anthochxra mellivm-a, Brush Wattle-Bird, two specimens; Climacteris picumnus, Vfhite-throated Tree-Creeper, two specimens; Acrocepha- lus AustraUs, Reed Warbler; Cysticola Uneocapilla, Black-striated Warbler, two specimens; Pardalotus striatus, Striated Pardalote, two specimens; Zosterops dorsalis, Grey-backed Zosterops, two specimens ; Dicceum hirundinaceum, Swal- 271 low Dicseum, four specimens; Glotiis glotloides, Green-Shank; Sericornis humilis, Sombre-colored Sericornis, two specimens; Malurus cyaneus, Blue Wren, two specimens; MeUphaga Australaskina, Tasmaniaii Honey-Eater; Ueliphriffa mys- tacalts, Moustached Honey-Eater, three specimens ; Collocalia arborea, Tree Mar- tin, two specimens; Clirysoccrys luckhis, Bronze-wing Cuckoo, two specimens; Trichofflossus rubriiorques, Stringy-bark Parrakeet, two specimens; Lathamus discolor, Swift Parrakeet, three specimens ; AcanOiiza chrysorrhma, Yellow- rumped Acanthiza; Erythrodryas rlwdinogaster, Flame-breasted Robin, two speci- mens; Acanthiza uropygialis, Chestnut-rumped Acanthiza, two specimens; Cln- cloramphus rvfescens, Rufous-tinted Cincloramphus, two specimens; Acanthiza lineata, Striated Acanthiza, four specimens; EjAhianura albifrons, White-fronted Epthianura, two specimens ; Calamanthus fuliffinosus. Reed Lark, two speci- mens; Fakunctdus frontatus, Tit Shrike; Eopsallria Australis, Yellow-breasted Robin, two specimens ; Acanthorhynchus tenui7'ost7'is, Slender-billed Spine-Bill, two specimens; Pachycephala pectoralis. Banded Thick-Head, two specimens; Petroica ?)jilum- bea, Plumbeous Flycatcher, two specimens; Anthus Australis, Australian Pipit; Silteta chrysoptera, Orange-winged Sittela, two specimens; Pachycejyiuda, ; Four Specimens of Acanthiza, of two different species; Smicornis brevirostris, Short-billed Smicornis; Two Species of Honey Eater; Cisticola magna, Great Warbler; Hiaticula ruficapilla. Red-capped Dottrel; Schaniclus albescens. Little Sandpiper; Schaniclus suburquatus, Curlew Sandpiper. The following birds, etc., obtained at Lake Superior in 1857, prepared and pre- sented by Dr. S. Kneeland, Jr.; Male and female Sharp-shinned Hawk, Ac- cipiter J'uscus, Gmel. ; Male Sparrow-Hawk, Tinnuncxdus spiarve.rius, Liim. ; Hawk Owl, Sicrnia Junerea, Gmel. ; Acadian Owl, male, Athene Acadica, Temm.; Male and female Kingfisher, Ceryle alcyon, Linn. ; Plicated Wood- pecker (young), Dryocopus pileatus, Linn.; Three-toed Woodpecker, male, Pi- coides fwc^icMs, Rich & Sw. ; Hairy Woodpecker, female, Picus villosus, Linn.; Male and female Downy Woodpecker, Picus pubescens, Linn. ; Golden-winged Woodpecker, male, Culaptes auratus, Linn.; American Raven, Corvus cacalotl, Wagl. ; Blue Jay, Cyanocorax cristatus, Linn. ; Canada Jay, two females, Peri- soreus Canadensis, Linn.; Rusty Grakle, male and female, Scolecophagus feri-u- gineus, Wils. ; Pine Grosbeak, female, Sirobilophaga enucleator, Linn. ; Snow Bird, two specimens, Plectrophanes nivalis, Linn.; Snow Finch, Fringilla hyemcdis, Linn.; Red-poll Linnet, two specimens, Fringilla linaria, Linn.; Cross-bill, Loxia Americana, Wils. ; Purple Finch, Carpodacus jmrpureus, Gmel. ; White-throated Sparrow, Zonotrichia albicollis, Gmel. ; Fox-colored Sparrow, two females, Zono- trichia iliaca, Merr. ; Olive Hermit Thrush, male and female, Tardus solitarius '? Wils.; Brown Hermit Thrush, male and female, TurdusJ'uscescensf Shaw; Sum- mer Duck, male, Aix sjjonsa, Linn. ; Dusky Duck, female. Anas obscura, Gmel. ; Common Snipe, female, Gallinago Wilsonii, Temm.; Red-breasted Snipe, female, Macroramphus griseus, Gmel. ; Tell-tale Tatler, Totanus melanoleucus, Gmel.; Wilson's Plover, Charadrius semipalmatus, Kaup.; Solitary Tatler, Tutanus chlo- ropygius, YieWX; Sora Rail, Ortygometra Carolina, Linn.; Red Squirrel, Sciurus 272 Httdsonius, Gmel.; Striped Squirrel, Tamias Lysteri, Rich. — American Magpie, Pica Hudsonica, Sabine; Cednr Bird, Ampelis cedvorum, Vieill; prepared aiTd pre- sented by J. H. Slawson, of Houghton, Michigan. September 16. Specimens of the common Water Lily, (Nymphcea odorata) of a pink color, from Yarmouth, Mass. ; by Samuel Swan, Esq. Two Crania of Albatross; by Di-. S. Durkee. • BOOKS RECEIVED DURING THE QUARTER ENDING SEPT. 30, 1857. Slemoirs of the Geological Society of India. Vol. 1. Tart I. 8vo. Calcutta, 1856. From die Governor-General oj' India. Prodromus descriptionis Aniraalium Evertebratorum quffi observavit et de- scripsit W. Stimpson. Pai't 2d. 8vo. Paraph. Philadelphia, 1857. Froiii the Author. Notice siir une nouvelle Esp^ce de Davidsonia. Par L. De Koniuck. From Prof. H. D. Rogers. Tableaux of New Orleans. By B. Dowler, M. D. 8vo. Pamph. From the Authm\ Lettres sin- les Eoches du Jura. Par Jules Marcou. 8vo. Premiere Livrai- son. 8vo. Paris, 1857. From the Author. Smithsonian Contributions to Knowledge. Vol. IX. 4to. Washington, D. C. 1857. Annual Reports of the Board of Regents of the Smithsonian Institution. 8vo. 2 vols. 1855-6. Washington, D. C. From the Smithsonian Institution. Journal de Tlnstruction Publique. Vol. I. Nos. 5-8. 8vo. Pamph. Mon- treal, 1857. Journal of Education. Vol. I. No. 4. 4to. Montreal, 1857. Farmer's Journal. Vol. V. No. 1. 8vo. Pamph. Montreal, 1857. From L. A. H. Latour. First Annual Report of the Secretary of the Board of Agriculture of Massa- chusetts. 2d Series. 8vo. Boston, 1853. Transactions of the Michigan State Agricultural Society. Vol. VII. 8vo. Lansing, 1856. Tenth and Eleventh Annual Reports of the Board of Agriculture of Ohio, for 1855-6. 2 vols. 8vo. Chillicothe, 1856-7. Twentieth Annual Report of the Board of Education. PamiDh. 8vo. Boston. 1857. Abstract of the Census of Massachusetts for 1857. Annual Reports relating to Births, Blamages, Deaths, &c., in Massachusetts, for 1855. 8vo. Pamph. Boston. Transactions of the Massachusetts Society for the Promotion of Agriculture for 1856. 8vo. Pamph. Boston, 1857. Synopsis of Communications on the Cause and Cure of the Potato Rot. 8vo. Pamph. Boston, 1852. From C. L. Flint, Secretary of the Board of Agri. culture. 273 History of Wisconsin. Vols. I. and III. By Wm. R. Smith. 8vo. Madison, 1854. Address .before tlie Regents of the TJniversity. Bj- D. Read, L.L. D. 8vo. Pamph. Madison, 1856. Charter of the City of Wisconsin. 8vo. Pamph. Madison, 1856. First Annual Report of the Executive Committee of the State Historical So- ciety of Wisconsin. 8vo. Pamph. Madison, 1855. Report of the Iron of Dodge and Washington Counties, Wisconsin. By J. G. Percival. 8vo. Pamph. Milwaukee, 1855. Annual Report of the Geological Sm-vey of Wisconsin. By J. G. Pei'cival- 8vo. Pamph. Madison, 1856. State Annual Report and Collections of the State Historical Society of Wis- consin for 1855. 8vo. Vol. H. Madison, 1856. Fro7n the Historical Society of Wisconsin. Bulletin de la Societe de Geographic. 4ieme Serie. Tome XHI. 8vo. Paris. 1857. Canadian Naturalist and Geologist. Vol. H. No. 3, July. No. 4, September, 1857. Montreal. Second Meteorological Report presented to Parliament. Long 4to. Pamph. Melbourne, 1856-7. Account of the Smithsonian Institution. By W. J. Rhees. 8vo. Pamph. Washington, 1857. Monatsbericht der Kciniglichen Preuss. Akademie der Wissenschaften zu Berlin. January to December, 1856. 11 Nos. 8vo. Mathematische Abhandlungen der Koniglichen Akademie der Wissenschaf- ten zu Berlin. 4to. 1855. Aus dem Jahre Physikalische Abhandlungen der K. Akademie der Wissenschaften zu Berlin. 4to. Bivalve Shells of the British Islands. By Wm. Turton. 4to. London. 1848. Index Testaceologicus. 8vo. London, 1818. By W. Wood. Genera of Recent Mollusca. Parts 27-30. 8vo. London. By H. and A. Adams. Catalogue of North American Mammals, chiefly in the Museum of the Smith- sonian Institution. By S. F. Baird. 4to. Pamph. 1857. Silliman's American Journal of Science and Art. July, September, 1857. New York Journal of Medicine. July, 1857. Proceedings of the Zoological Society of London. Part 23. 8vo. 1855. Proceedings of the Elliott Society, pp. 49-100. 8vo. 1857. Received in Exchange. Quarterly Journal of the Zoological Society. Vol. XIII. Part 3. 8vo. Lon- don, 1857. Annals and Magazine of Natural History. July, August, September, 1857. Svo. London. From the Courtis Fund. Historical Sketches of Eminent Statesmen. Brougham, Henry, Lord. 2 vols. 8vo. Philadelphia, 1854. Encyclopaedia Britannica. Vol. XIII. 4to. Boston, 1857. Deposited by the Republican Institution. PROCEEDINGS B. S. N. H. — VOL. VI. 18 DECEMBER 1857. 274 October 7, 1857. The President in the Chair. Mr. Theodore Lyman read a paper upon a new genus and species of Coral, Syndepas GouJdii. GENUS SYNDEPAS, (Lyiliail.) Derivation, avv, deTrac, (goblet.) Growing in tufts (or single ?) ; calicles cylindrical or turbi- nate ; striated on the outside with granulated ridges ; within deep ; walls solid ; larger lamelliB exsert, finely toothed on their edges ; budding from the side, low down, or from the coenen- chyma between tlie calicles. This genus is distinguished from Desmophyllura of Ehrenberg by the fact that the lamellae are toothed and not arranged in bundles ; from Culicia of Dana, by depth of calicle, external stria} and exsert lamelli^ ; from Cladocera of Ehrenberg by dif- ferent mode of growth and by internal dissepiments ; and from Dendrophyllia of Blainville, by different mode of growth and the solidity of the walls. The Garyophyllia solitaria (Lesueur) and the Caryophyllicp dUatata and j^ocillum of Dana will probably come under the genus. SYNDEPAS GOULDii, (Lyman.) The general appearance is that of a cluster of little goblets connected by a lime cement, which is often the resting-place of Serpulfe, Bryozoa, and boring shells. The zoophyte buds, either from the side, low down, or from the open space between the calicles, {ccenenchyma, Edwards.) The group begins with three or four cups, low, standing well apart, and connected at their bases by a thin sheet of ccenenchyma. New buds appear, and the whole growing upwards and outwards gradually makes a tuft of crowded though independent individuals. The calicles, though sometimes cylindrical, are normally turbinate ; within, 275 thej have a depth often as great as 3^ lines. Their height varies from 3^ to 9^ lines. The tallest are the oldest, and have continued growing with their younger neiglibors. The greater diameter is from 4 to 6 lines, and the difference between the longitudinal and transverse diameters is occasionally as great as 6 to 3^ ; at other times the calicles are nearly round. In the longitudinal axis there usually lie two lamella? of the first cycle, which shows a tendency to a bilateral symmetry. The larger calicles have from 48 to 74 lamella% so that there are four cycles, and sometimes part of a fifth. Those of the last cycle, however, are very small and thin, and can scarcely be seen without a lens. The six that make the first cycle are conspicuous for their size ; they are rounded at their upper ends, exsert, often as much as a line, and are thicker than the wall of the calicle. Their sides are covered with grains, arranged more or less regularly in curved lines, running from the wall to the edge of the lamella. Wherever one of these lines ends on the margin, it projects a little, and thus the edge of tlie lamella is toothed. The lamellae of the second and third cycles do not materially differ, except in size, from those of the first. The lamella? are not confined within the limits of the wall of the calicle, but appear on its outside, as vertical ridges or striaa, extending often from top to bottom ; in some instances, however, they are nearly covei-ed by marine in- crustation to within a line of the top ; and, again, they may be obliterated by the growth outwards of the wall. These ridges, which may properly be called the outer edges of the lamellae, are thicker than the inner edges, but present, to a greater or less degree, the same granular teeth. The smallest lamella? occa- sionally bend sidewise and join their neighbors, a feature observed in its perfection among the Eupsammidte, and, to some extent, in other families. The columella is frequently wanting, or repre- sented only by one or two lamellar teeth ; but, on the other hand, it may form, at the bottom of the calicle, a spongy mass, two or three lines in diameter. The wall, at its upper margin, is very thin and diaphanous ; outside, in the spaces between the lamellfe, it is slightly granulated. It is highly probable that the polyp, like the Garyophyllia solitaria, has the protruded, Caryophyllian mouth, and about twenty-two short tentacles, in two rows ; and farther, that it has the power of raising itself above the edge 276 of the calicle. It is evidently as successful a collector of Crus- tacea as its numerous kindred ; for, still wedged in the visceral cavity of one individual, was found part of a small crab. The specimens were got by Mr. J. P. Couthouy, from the wreck of the San Pedro, sunk, in 1814, in the bay of Cumana, on the northeast coast of South America, and were presented by him to Dr. A. A. Gould. Dr. Gould, after whom I have named the species, kindly put them all at my disposal to be described. Prof. Dana briefly notices three species of Caryophyllia, of which he says : " The following species have been observed only in the simple state, and may or may not be budding species." Dana, Zooph. p. 383. The first of these, C. solitaria, has been described by Lesueur, (Journal Acad. Nat. Scien. Philad. vol. 1, p. 179,) and is also spoken of by Lamarck. It comes very near to the present species, but differs as follows : it has fifteen to sixteen larger lamella?, alternating with smaller, while this species has, at the most, ten or twelve that can in any way be called larger. G. solitaria has the margin of the calicle nearly entire, while S. Gouldii has it rough with heads of lamella. Lesueur's figure represents the coi-allum partially buried in, or surrounded by, the substance to which it is attached, a mode of life quite different from the encrusting habit of the present coral. The second species, G. pocillum (Dana), is much broader than high, a proportion not met with in over 150 calicles, young and old, of aS'. Gouldii which I have examined ; and in which it is rare to find the breadth as great as the height. The species now under consideration has only six lamellas decidedly prominent ; while the other has " twelve larger, very broad and exsert," and " three intermediate, smaller and one half narrower ; an arrangement not found at all in the subject of this paper. The third, G. dila- tata (Dana), differs so strongly that no comparison is required. All three of these have the outward sti'iae stretching only part way down the wall, while, in almost all the specimens of S. Gouldii the striae reach quite to the bottom of the calicle. The most important distinction of all, however, is, that G. solitaria, pocillum, and dilatata, have only been seen solitary, while this species has invariably a grouping habit ; nor do I think a calicle could be broken off in such a way as to give the idea that it had grown single. Prof. Dana has been at the trouble of examining 277 a specimen I sent him, and lias written me, that in his opinion the polyp is new. This species would come under the family of Caryophyllida^ of Dana, though his description certainly seems inexact, or at least ambiguous, when he says ; " coralla within not transversely septate, surface not lamello-striate ;" for some of the genus Caryophyllia (e. g. Caryophyllia arhuscula) have dissepiments, and the exterior of some species is striate, (e. g. O. pocillum, &c.) This family is represented in the classification of Edwards and Haime by parts of the families, Eupsammidaj, Turbinolida?, Astreida', Oculinidte, and Cyathophyllida?. The jiresent genus has all the characters of the Turbinolida3, but cannot be put with them, on account of the toothed lamellae ; whereas Edwards expressly says : " The lamellar lines never separate at their exti'emities, either singly or in bundles, to form crenellations, teeth, spines, or lobes, and the free edge of the lamella remains always entire." This only shows how unphilosophical are the family characters given by some of the most eminent authorities. It must be pretty plain that this genus should make one of the natural group that in- cludes Turbinolia, Desmophyllum, Flabellum, Cyathina, &c.. yet it cannot be admitted there, according to Edwards, because the grains on the sides of the lamella3 are continued so as to project a little beyond the edge. This genus would fall under Dana's tribe of Caryophyllacea, which is characterized by " numerous tentacles in two or more series," inferior gemmation, when any, and many-rayed cells, and corresponds to parts of Edwards's Sections, Zoantliaria aporosa, perforata, rugosa, malacodermata, and tabulata. This Tribe and these Sections would be called, by some systematic writers. Sub- orders. These great discrepances between distinguished authors, and that, too, on the threshold of classification, may perhaps be accounted for by the fact that the classification of Dana is founded on the polyps themselves and their skeleton, while that of Edwards and Haime rests principally on the ultimate struc- ture of the skeleton or polypier. A single instance will put this difference in a clear light. Edwards puts Madrepores, Porites, and Dendrophyllige in the same Sub-order, (^Zoantliaria perfo- rata^ because they all have holes through their walls ; but then the Dendrophylliifi have numerous tentacles, in two rows, and a 278 protrutling mouth, while Porites and Madrepores have a mouth on a level with the edge of the calicle, a;nd only twelve tentacles. Dana therefore puts under Cavyophyllacea the Uendrophyllia;, and under Madreporacea the Madrepores and Porites. Dr. A. A. Hayes read a letter from Dr. C. F. Wins- low, of Troy, N. Y., and presented, in his name, a sup- posed fragment of a human cranium, found in California, 180 feet below the surface of Table Mountain. The thanks of the Society were voted for the gift. Dr. Winslow writes : " I sent by a friend, who was going to Boston this morning, a precious relic of the human race of earlier times, found recently in California, 180 feet below the surface of Table Mountain. As it is the first organic sign of human exist- ence preceding or coeval with a drift age, or a general or minor ' deluge,' that has been found in the earth, I have thought it would be interesting for the scientific gentlemen of Boston to discuss the subject, and for a portion of the fragment sent to me to be preserved in the cabinet of your Society of Natural History. My friend Col. Hubbs, whose gold-claims in the mountains seem to have given him much knowledge of this singular locality, writes that the fragment was brought up in ' pay dirt ' (the miners' name for the placer gold drift) of the Columbia claim, and that the various strata passed through in sinking the shaft consist of vol- canic formations entirely. Whether his knowledge is accurate touching the volcanic formations I have some doubt, and have written foi" more certain information. " The mastodon's bones being found in the same deposits, points very clearly to the probability of the appearance of the human race, on the western portions of North America at least, before the extinction of those huge creatures. As I have frag- ments of Mastodon and Eleplias primigenius, or a kindred spe- cies, taken between ten and twenty feet below the surface, among the upper placer gold deposits of the same vicinity, it would seem that man was probably contemporary, for a certain period, with the closing dynasties of these two formidable races of quadrupeds. This discovery of human and mastodon remains in the same locality gives also great strength to the possible truth of the old 279 Tndian tradition of tlie contemporary existence of the mammoth and aboriginals of this region of tlie globe." Dr. A. A. Hayes also read a letter from Mr. A. P. Davis, of Buchanan, Liberia, giving some farther par- ticulars in relation to the discovery of Native Iron in Africa. Mr. Davis, from whom the specimen analyzed by Dr. Hayes Avas received, in the present letter describes the mass found as " being as large as the crown of a man's hat, and like a rock, of a yellow color taken from the earth. From its appearance I supposed it would break into pieces ; but it resisted the repeated blows of a sledge-hammer of fifteen pounds weight ; and I could not separate it by breaking, as the hardest blows only flattened it. It was by these means we found out it was malleable. The huge bulk was put in the fire and blown to, until it became suffi- ciently hot to be cut. It was divided into many parts, and some of the same bulk was actually ore, not malleable at all. It had a very craggy appearance, with many cells in it. Where the ore is to be had, or the distance that the ore in question came from, is about four to six days' travel. I have none now, but will, with Div^ine help, get some as soon as possible." Dr. Hayes added that he was indebted to the efforts and kind- ness of Rev. Joseph Tracy, of the Colonization Society, for the letter from Mr. Davis, and other intei'esting facts in relation to the natural productions of the country bordering on the lands of the colony of Liberia. The President exhibited specimens of curiously inter- twining and intergrowing woods from Surinam ; they were referred to the Curator of Botany. The Curator of Crustacea exhibited the Crustacea collected in California by Mr. E. Samuels, together with other specimens presented by the Smithsonian Insti- tution. Among them are several new species described by Mr. Stimpson in the forthcoming number of the So- ciety's Journal. 280 The Curator of Ichthyology presented a Fish from the North Atlantic, a new species, and probably belonging to a genus new to North America. Dr. S. Kneeland presented about fifty specimens of Mammalia, Birds, and Reptiles from Lake Superior. Dr Kneeland remarked that, as yet, there wei'e no rats and common mice at Portage Lake, the place of these animals being filled by the Flying Sqnirrels which breed in the walls of the houses, and by the Field Mice. The reptile, described by him at a former meeting (Proceed- ings, Vol. VI. p. 152) as a Siredon, is a Menobranchus, but prob- ably a new species, as it does not answer to the descriptions of either M. maculatus or M. lateralis. If it is new, the specific name of M. hyemalis would hold good. The salamanders, trout, and tortoises vary somewhat from described species. Mr. F. H. Storer exhibited some proof-sheets of a work upon the Plants of Austria, by Ettingshausen and Pokor- ny, recently published at the Imperial Printing- Office in Vienna. The impressions, from which these prints were struck off, are obtained by the process known as " Na- ture's own Engraving," in which the dried plant to be copied is placed between a sheet of steel and another of very pure soft lead, and all together subjected to great pressure by passage between rollers. An impression of the plant, even in microscopic details of the most delicate Algae, is thus transferred to the soft lead — the plant being forced into it, — from which any number of copies may be taken by electrotyping. Examples of the application of this process in the delineation of other objects, such as small animals, agates, fossil impressions, sections of wood, lace, &c., were also exhibited. Dr. D. H. Storer stated that he had lately received a fine specimen of the Sting Ray from Dr. E. W. Carpen- ter, of Chatham. It proves to be the Paslinaca hastata 281 of Dekay. It measured nine feet from the snout to the extremity of the tail. It is described by Dekay as hav- ing three caudal spines ; this specimen, however, pre- sented but one, and the stump of a second, anterior to it. DEPARTMENT OP MICROSCOPY. The Secretary, Dr. B. S. Shaw, exhibited specimens of the larva of some species of Fly {Musca or (Estrus), which were found in the skin of the scalp, face, neck, and back of a child seven days old. The specimens were imbedded in pustules of about one eighth of an inch in diameter, resting upon an inflamed base half an inch or more in width. The only specimen preserved for examination was placed in alcohol. After it had been immersed in this fluid for sevei'al days, it was found to measure a quarter of an inch in length by a sixteenth in breadth. Color white. Body composed of eleven segments, exclusive of head ; anterior portion of each segment surrounded by a band of bristles or spines. Head armed with two black booklets ; no visible mouth. Cuvier speaks of the mouth of the cutaneous larvas as " being composed of fleshy lobes only, whilst that of the internal larvae is armed with two strong bent hooks." If this is true, the natu- ral nidus of these larvae would seem to be the internal organs rather than the skin. Humboldt, Rudolphi, Linnaeus, Gmelin, and others, speak of a species of Qilstrus as (Estrus hominis. This species, however, so far as is known, has only been met with in South America, and when thoroughly studied may prove to be identical with one of those better known. In endeavoring to ascertain what is known concerning the presence of maggots in the human body, the Secretary had met with a large number of cases where the mucous membranes had been infested with them, and with several cases where the skin had been chosen as the nidus for the larva or agg. Of the Coleopterous insects, such as beetles, mealworms, &c., he had collected between thirty and forty cases, where their larvai had been found in the stomach, intestines, urinary organs, nostrils, and inner canthus of eye. The larvai of Neuroptera and Lepidoptera have been found in 282 similar situations. Of the larvfe of Diptera, those of Musca and CEstrus seem to be most common ; those of Musca forming by far the largest number of any one genus, thirty-seven cases hav- ing been tabulated and reported by Mr. F. W. Hope, in the Transactions of the Entomological Society of London, Vol. II. The species of these maggots was generally unknown ; but many were recognized as belonging to M. vomitoria., M. carnaria, and M. domestica. The genus Oestrus seems to be that which most frequendy deposits upon the extei'nal surfjice of the human body. Of these cases he had met with Ivvo upon the scrotum, two in the skin of the abdomen, two in the scalp, and one in each of the following named situations, — leg, arm, scapula, ear, jaws, antrum, and stomach. These larvae were either called Oestrus hominis, or they were described without a specific name, with the exception of one, which was CEstrus bovis. A full account of this case was read before the Boston Society for Medical Improvement, and published in the Boston Medical and Surgical Journal of October 8, 1857. Mr. C. J. Sprague exhibited specimens of a new fun- gus, Glcsosporium crocosporum, Berk, and Curt, named from specimens collected by himself. This fungus is found very commonly in autumn upon various kinds of melon. It appears in orange spots upon the outer sur- face, and is generally found in places which seem to have re- ceived a blow. Sometimes, however, the fungus covers the whole fruit in a yellow and orange incrustation. It belongs to that numerous family of fungi which infest the leaves and bark of all plants, and the epidermis of fruits. There is no true peri- thecium, but the spores spring in myriads from a nucleus just beneath the epidermis, and then ooze forth through an aperture in irregular granular masses drying on the surface. They are elongated oval in shape, and of a clear yellow-orange color in mass. Mr. Sprague also exhibited the spores under a microscope. 283 October 21, 1857. The President in the Chair. In the absence of the Recording Secretary, Mr. C. J. Sprague was chosen Secretary 7?ro tern. I ^\ Dr. A. A. Gould read a letter from Prof. Hubbard of Dartmouth College, giving an account of a fish which was seen to fall to the earth, during a sudden squall of wind and rain, in a town in Vermont. Dr. Gould thought the fact interesting, as corroborating several instances of the same kind which had previously been recorded, some of which had come to his own knowledge. Dr. Gould also stated that a letter had been sent to him through Prof. Lovering by Mr. George S. Blackie, written by Prof. Gregory of Edinburgh to the late Prof. Bailey. Dr. Gould read several passages of general interest regarding certain observations made by Prof. Gregory on the Diatomaceous Exuviae of the Post-Tertiary sand at Glenshira, near Inverary, the greater part of the letter being devoted to a close criticism on certain new forms. Several prepared specimens, and a number of pamphlets on the subject, were laid on the table, to be added to the collection of Prof. Bailey. On motion of Dr. Gould, it was voted that the receipt of the letter and specimens be acknowledged with thanks to Prof. Gregory. Dr. Kneeland presented a large number of specimens, collected by himself, illustrating the different forms in which the copper occurs, and the various rocks with which it is associated, in the Lake Superior district of Keweenaw Point. All the copper, with the exception of a small amount of car- bonate near the surface, which he liad seen over this extensive 284 district, was the pure metal ; — he showed its different forms of mass, leaf, and botrjoidal copper ; of rounded pieces, varying from a rifle ball to a small shot in size, scattered through the rock, called shot copjyer ; and also the metal in a crystalline form, in curiously contorted spiculae, and in the thinnest laminae. Associated with the metal were the various forms of granular and aniygdaloidal trap, tabular spar, quartz, epidote, prehnite, calc-spar, &c. ; crystals of dog-tooth spar, of calc-spar containing copi)er, of quartz, &c. Some of the specimens were blackened by the kiln-tires employed to facilitate the separation of the matrix. The specimens were from the Minntsota, Cliff, and Portage Lake districts. He also presented several specimens of native silver associated with copper ; of agates from the lake shore ; of chlorastrolites, found only on Isle Royale island ; of sulphuret of copper and rose quartz from the noi'th shore of the lake ; and of fossil corals from the drift. He thought the speci- mens of value, not only mineralogically, but especially as illus- trating this particular and almost unique copper deposit ; for such a series he had looked in vain Avhen wishing to study this subject, and he thought the present collection, with others he made last winter from the same localities, would be of great value to any one pursuing this study at so great a distance from the copper region. Dr. Bacon exhibited a calculus taken from the urethra of an ox. It consisted essentially of silica, with a little carbonate and phosphate of lime. It measured about four lines in diameter, and presented a rough or tubercu- lated surface. Dr. Wyman asked how common calculi of this chemi- cal composition are. Dr. Bacon said that very few cases are on record, but that probably many passed unnoticed. Dr. Gould asked whether the lime-salts were diffused throughout the mass or not. Dr. Bacon said that in this case they are uniformly diffused. The silica was amorphous, not crystalline. Dr. Kneeland, who brought the specimen from the 285 neighborhood of Lake Superior, said that the animal died from this obstruction. The calculus was perfectly impacted in the urethra, so as to prevent the egress of the bloody urine which distended the bladder.* Mr. John Green made some remarks upon the micro- scopic structure of certain fish scales he had recently been examining; he showed them to be of bony struc- ture, which he considered to have an important bearing on classification. Dr. Gould alluded to some recent observations in France in relation to the reproduction of Arachnides, or rather their power of producing fertile eggs, though com- pletely isolated from the male. Blanchard found that the genital apparatus of the female was composed of two ample tubes to which the ovarian crypts were attached. These serve as reservoirs in which the seminal fluid accu- mulates, through which the eggs pass and are impreg- nated ; but which is not exhausted by one ovulation, serving for many subsequent occasions. Blanchard therefore concludes that one coupling is necessary, and serves for several years. M. Delfraysse had in like man- ner invoked anatomy to settle the question. He like- wise finds the two tubes and the fecundating liquid ; but states that he has found two little glandular bodies be- tween the ovaries and tubes, which secrete the fertilizing fluid. He therefore concludes that the animals are her- maphrodite ; — that the seminal fluid is furnished at the time of laying eggs, and not kept in store ; and that no copulation is absolutely necessary. Dr. G. remarked that there was evidently room for further anatomical research, and did not see how the latter conclusion com- ported with the well-known organization of the Arach- nides as males and females. * In the account of Calculi from the bladder of an ox, upon page 213 of this volume, it should have been stated that their composition was nearly pure silica. Secretary. 286 Mr. Sprague laid on the table a package of AlgaB, pre- sented to the Society by Mr. B. D. Greene. They formed part of Prof. Harvey's collections, and came from Australia, Ceylon, and the Friendly Islands. They were beautifully prepared with printed labels, and fur- nished another instance of Mr. Greene's liberality to the Society. The Corresponding Secretary was instructed to make a fitting acknowledgment to Mr. Greene for the donation. The President made some remarks on the mode of reproduction of certain fishes in Surinam, and detailed some interesting points of structure in their eyes. Mr. Joseph Tillinghast and Mr. George H. Rogers, of Gloucester, were elected Resident Members. November 4, 1857. Dr. C. T. Jackson, Vice-President, in the Chair. Dr. Jackson exhibited crystals of sugar produced by the Sorghum saccharatum, or Chinese Sugar Cane. They were six-sided prisms, and rhombic prisms with angles of 103° and 77° — crystallographic proof, as he consid- ered, of their being cane sugar. Dr. Jackson stated that the young plant contains gum or dex- trine, and glucose. As the period of inflorescence is approached, large quantities of starch globules may be seen in the cells of the plant. If, at this period, the stalk is pressed, the fluid which exudes is found slightly milky, owing to the presence of starch globules, which subside after some time. When the seed ripens, the starch diminishes in quantity in the cane, and the expressed juice gives, upon evaporation, almost wholly cane sugai-. This is a point of interest in the manufacture of sugar. The presence of starch in the syrup prevents the ready formation of crystals of 287 cane sugar, and it should therefore be removed by decantation or filtration. Fermentation of the syrup and the conversion of the sugar into lactic acid and raannite takes place in warm weather. It should therefore be boiled before viscous fermen- tation takes place. Dr. Jackson expressed the opinion that the Sorghum would ripen in the Northern States in warm seasons, if planted early. Mr. Theodore Lyman read a paper upon a new spe- cies of Coral, as follows : — The genus Oculina, established in 1816 by Lamarck, includes the polyps distinguished by the solidity of their corallum through- out ; to this feature may be added, that they have generally a tendency to branching, and an abundance of solid tissue between the calicles. The animals themselves, so far as observed, have a well-marked central disk, and about twenty-four slender, tapering tentacles, alternating longer and shorter. Prof. Dana (1848) describes nine species under the genus Oculina, and six species under the genus Allopora, which was included by Lamarck's genus Oculina, and which includes Allopora (Ehrenberg, 1834) and Stylaster (Gray, 1831). Milne Edwards and Haime (Mon- ographie des Oculinides, Annales des Scien. Nat. 3^™<^ Serie, tome xiii. 1850,) have established a family of Oculinida;, which includes, besides new species, all species under the above-named genera. This family has twenty genera, principally character- ized by the modes of budding, the variations of the columella and paluli, the smoothness or roughness of the surface, and the shapes of the lamellae. Of these genei"a, several are fossil, and others have only new species. The species, according to Dana, are changed as follows, by Edwards, 0. diff'usa, varicosa, and pallens appear under the name diffusa ; 0. ocidata and virginea become oculata. 0. horrescens is transferred to the genus Acrhelia ; 0. prolifera to Lophelia ; 0. axillaris to Cyathelia ; and 0. hir- tella to Schlerhelia. And, finally, the Caryophyllia anilwphyllum of Dana is brought into this family and put in the genus Lophe- lia. It should be observed that these genera of Edwards and Haime are, as usual in their classification, founded entirely on the structure of the polyp frame, without reference to the soft parts. 288 OCULINA GLOMERATA, Lyman. Mass, encrusting a piece of sheet lead. In two or three places there are signs of" the beginnings of branchlets. Corallum solid, granulated slightly in the spaces between the calicles. Calicles in some places crowded, and with numerous buds among them ; generally 1^^ lines broad, and often f line high ; round, upright, striated and granulated outside ; a few much larger than the rest. LamelltB, in the full-grown calicles, 26, rarely less, and in a few instances as many as 38 ; a little exsert, rather delicate, every other one reaching the centre ; all toothed for their whole length, and the larger ones with two or three little lobes, the lower of which might be considered as paluli ; sides finely toothed. Colu- mella small generally, and inclined to be spongy. The specimen is a couple of inches long and an inch high. It was broughr by Mr. Couthouy from the wreck of the San Pedro, sunk in 1814 in the bay of Cumana ; and is now in the collec- tion of Dr. A. A. Gould. This species would come under the genus Oculina as defined by Edwards. The other species differ from it as follows : 0. virginea, Indian Ocean ; calicles far apart ; rarely more than 24 lamellas — calicles a little swelled at the base. 0. speciosa differs like the preceding, and has moreover two circles of distinct paluli. 0. Petiveri, calicles distant, strongly swelled at the base, and with furrows between. 0. Banhsii, cal- icles distant, liardly raised above the surface, surrounded by a depression. 0. Valenciennesi, calicles little prominent, sometimes even depressed. 0. Jissipara, fissiparous ; • lamellae irregular. O. varicosa, calicles farther apart ; lamella? stouter, less toothed ; cavity deeper ; only 24 lamella?. 0. diffusa, calicles farther apart ; lamellae stouter, little, or not at all, exsert, 24 in number. 0. pallens, calicles larger, deeper ; lamella? much stouter, and less toothed. There is but one Oculina known which is encrust- ing in its growth. This is the 0. conferta, (British Fossil Corals, p. 27, tab. 11, fig. 2, 1850,) which is an eocene fossil, and may, perhaps, with the present species, be only the young state of an arborescent form. Dr. Jackson read a communication from John Bachel- der, Esq., dated Monument, October 27, 1857, upon the 289 Ruins of a Trading House erected by the Pilgrims at that place. The communication was presented, upon motion of Dr. Jackson, to the Massachusetts Historical Society. Prof. Theophilus Parsons presented a section of an Elm, which exhibited a singular involuted growth ap- pearing after the falling of a large limb. The growth occurred at the edge of a hollow in the trunk, and presented the appearance of a curling inward of the edge of the cavity, — by which it was several times rolled upon itself, the bark following the curl to its termination. Prof. Parsons, in reply to a question from the Corresponding Secretary, stated that this curl, if unrolled, would more than span the gap on the edge of which it was found. Mr. Sprague thought that the curvature of the tree admitted of simple explanation. The falling of the large bough had car- ried with it a considerable portion of the heart wood of the tree, leaving the centre exposed to decay. As, year after year, this central portion disappeared, the outer, living shell became thin- ner and thinner, and began to assume a convolute form, from the growth being always on one surface only. The shrinking and drying of the internal part, joined to the swelling and increasing of the external part, had gradually curved the rim of wood, like the convolute estivation of some corollas. As the tree grew in height, the aperture left by the fallen bough, and increased by the subsequent decay, gradually became narrower by the shrink- age and inward growth of the margins. Prof. Parsons concurred with Mr. Sprague in this expla- nation. The Corresponding Secretary read the following letters, viz : From the Academy of Natural Sciences, Philadelphia, April 7 ; the Academy of Science of St. Louis, June 6, and September 11 ; the American Philosophical Society, Sept. 10 ; the Academic Royale, &c. de Belgique, Bruxelles, January 15, 1856, and Feb- ruary 6, 1857 ; K. Akademie der Wissensehaften, Wien, April 10, 1857; Royal Society of Sciences at Gottingen, April 18, PROCEEDINGS B. S. N. H. VOL. VI. 19 .TANITARY, 1858. 290 1857 ; Smithsonian Institution, June, 1857, acknowledging the receipt of the Proceedings of the Society ; Verein fiir Natur- kunde in Nassau, March 1, 1857 ; Cambridge Philosophical Society, February 26, 1857 ; K. Akademie der Wissenschaften, Wien, November 24, 1856, presenting their various publications. From Prof Joseph Lovering, July 20, presenting, in behalf of the American Association for the Advancement of Science, its Proceedings ; Academy of Natural Sciences, June 19, asking for a missing number of the Journal ; the Georgic Association, Ran- dolph, N. Y., July 21, asking for the publications of the Society ; Geological Museum, Calcutta, January, 1857, making the same request, and sending its own Memoirs ; and from James H. Slawson, Houghton, Michigan, acknowledging his election as Corresponding Member. DEPARTMENT OF MICROSCOPY. Mr. John Green exhibited a large number of thin sec- tions of the Bush Ropes, so called, — peculiar woods ob- tained by him in Surinam, and made some extended remarks upon their method of growth. He said he was preparing a paper upon the subject, which he should read when his examinations are completed. Dr. James C. White exhibited the Eggs of the Itch Insect, Sarcoptes ho7}iinis. He remarked that, as is now well known, it is the female only which burrows. She bores transversely downwards through the skin, but never to a great depth beneath the surface. Each day as she moves onward she leaves an egg behind her. After she has deposited fourteen, the larva of the first matures and creeps out upon the surface, there to ramble with the other young and males till maturity, when if a female, and after copulation with a male, also an outsider, it repeats the process above mentioned. Each day a young one emerges from the burrow, leaving behind the membranous walls of its cell. The acarus may thus extend its hole indefinitely, even to the extent of four inches, and its course may be traced by a white elevated line on the skin. It 291 never leaves its burrow ; but if a pustule should be formed above it, by the scratching of the patient, the larvse are destroyed ; but the mother cunningly emerges to the surface at the edge of the pustule, and commences a downward descent anew. The male is much smaller than the female, and has ten extremities. The female wants one of these posteriorly, and the young three. She is also armed with two saw-like claws, which cut a way through the tissues by a transverse motion over each other as the blades of scissors do. Hebra thinks the opening for the exit of the eggs is a fold or valve on the belly, which may be easily seen, though it has never been figured. The present specimen was snipped from the glans penis, a favorite and undisturbed lurking-place. It consists of a canal bored obliquely through the tissues, containing a series of twelve eggs, together with fcecal matter, strewn along the passage. When first cut out, the animal herself was seen at the lower ex- tremity with one egg in her body. The first two or three eggs were quite mature, so that the extremities of the young could be distinctly made out. She generates but one egg a day, though Bourgignon says he has seen four at once in her body. Hebra thinks this impossible, and he is probably correct, as he has made them an especial study, cultivating a colony on himself for two or three months. He once saw the two sexes in act of coition, belly to belly. The same species occurs on the lion, camel, and other animals. Dr. White showed also the spores of the parasitic plant of Pityriasis versicolor. The specimen was taken two or three days since from the back of a gentleman who was not aware of any cutaneous dis- ease. There were some dozen patches, the largest the size of a pea. They present a yellow appearance, are elevated, and con- sist of epidermal cells, between the layers of which the parasite is found. Some alkaline carbonate is added to make the epi- thelium transparent. It is still a mooted point whether the para- site is the cause of the disease, or merely a growth in an exuda- tive process. The fact that we sometimes fail to find the parasite tends to the latter conclusion. Microscopically, it consists of 292 spores, containing a fat-like nucleus, grouped together between the layers of the epithelial cells. Sometimes the cells, by union, form long branching tubes, with here and there a nucleus scattered along their course. The cells sometimes subdivide also. It does not appear to be very rare here, as Dr. White had seen three cases in as many weeks. Mr. C. J. Sprague exhibited five specimens of Artotro- g-us Asterophora, Fr., parasitic upon Nyctalis, and showed the copious echinulate spores under the microscope. He also exhibited specimens of a nearly allied fungus, Sepe- donium cei'vimmi, Fr., which is rare, and which in this case grew upon a matrix where it had not before been detected. This fungus has generally been associated with Peziza macro- pus^ and was imperfectly figured by Ditmar upon this plant in Sturm's Fl. Deutsch, where the species was first described under the name of 31ycogone cervimim. The specimens exhibited were found by Mr. Denis Murray upon Helvella ephippium Lev. The lower portion of the hymenial surface was clothed with a white, felty envelope, while the upper portion was brown with the copi- ous spores of the ripened parasite. The spoi'es were exhibited under the microscope in dilFerent stages of growth and maturity. Mingled with them were many spores of an entirely different character. They were linear, narrowed at each end, uniseptate, pellucid, nearly colorless, with a yellowish tinge. Mr. Sprague had detected their growth from the ends of long, slender fila- ments, much smaller than those of the Sepidonium. Bonorden mentions that other parasites are frequently found in company with the Sepedonium, such as Monosphorium and Sporotrichum ; but neither of these genera bear spores like those in question. Prof. Parsons, of Cambridge, exhibited and presented a specimen of Infusorial Earth, from the neighborhood of Bangor, Maine. Copper was said to have been de- tected in the silica of which the specimen was composed. Dr. J. C. White was appointed one of the Committee on Chemistry of the Department of Microscopy. 293 November 18, 1857. The President in the Chair. Dr. Hayes remarked that a specimen of Infusorial Earth, (which was afterwards identified as part of the specimen referred to in the proceedings of the last meeting,) given to him by Dr. A. A. Gould, had been submitted to chemical examination, with- out the detection of any compound of copper, either mixed or combined with it. The existence of copper, as part of the ma- terial of the Navicula, would be an interesting fact ; but in the present state of our knowledge, there is no evidence afforded by chemical analysis in support of such an opinion. Dr. Hayes stated, in connection with the reported presence of cane sugar in the expressed juice of the variety of sorghum cul- tivated somewhat extensively the last two years, that he had grave doubts of its production anywhere, as an immediate prin- ciple. One or two varieties of sorghum, which really pro- duce cane sugar, had doubtless been cultivated, and had afforded sugar directly. Without having had an opportunity offered for an analysis of the secretion in the stalk, as cultivated so far south as where the ordinary cane can be reared, his most careful in- quiries had resulted in the conclusion that there, as well as here, glucose alone is contained in the cells of the plant. In Georgia and South Carolina the utmost efforts to obtain sugar from the juice, both on the large scale of manufacture and Ik more refined and varied operations, have failed, and the most recent informa- tion includes the fact that the product, obtained in Louisiana, side by side with that of the ordinary cane, sent to St. Louis for refin- ing, did not prove to be sugar. Masses of crystaUine matter have been obtained by evaporating the syrup ; but when it is remembered that a gallon of the expressed juice of the fully ripened plant contains more than an ounce of salts of potash, lime, &c., the production of a compound of glucose and salts is not surprising. If the plant secreted cane sugar, we should not from analogy expect that a change of habitat, allowing the plant to perfect its 294 cells, would lead to the formation of glucose only. Nor should we, in view of the experience, especially in our Southern States, meet with the two or three doubtful cases recorded of sugar pro- duct ; but as in the beet, the maple, and the cane, sugar, as a constant jjroximate constituent, would be found in the sorghum juice. The President gave an account of some observations on the development of Anableps Gronovii, as compared with that of the Embiotocas of California. Prof. Agassiz has described these last as having a " true ova- rian gestation." This statement is true, but in a somewhat dif-. ferent sense from that in which the development of Anableps may be considered ovarian. In Embiotocas the ovary is divided internally into numerous compartments by folds of lining mem- brane which project into its cavity ; these folds are germ pro- ducing, as the young ova may be seen between their layers, even when the foetuses are being developed in the cavity of the ovary. Nothing has been determined as yet as to the period when the ovum of Embiotocas leaves the ovisac, whether before or after impregnation. Wherever it has been observed, the foetus has been found in the cavity of the ovary, enveloped in the long- itudinal folds of its lining membrane. In Anableps, the gesta- tion is carried on to its completion, or nearly so, in the ovisac ; this last grows as the foetus is developed, becomes quite vascular, and by its apposition with the vascular papillte of the yelk sac, carries on those interchanges between the parent and the foetus which are necessary for respiration and nutrition. Dr. C. T. Jackson exhibited to the Society a portion of the supposed meteoric stone from Marblehead, which was brought to him for analysis on the 14th November. He remarked that it bore so close a resemblance to the slag of a copper smelting furnace, that he at first hardly thought it worth the trouble of analyzing, but since it might become im- portant to record the real composition of this alleged meteoric matter,.he had made the analysis, with the following results per cent. : — 295 Per oxide of iron - =58.72=metallic iron, 41,12 Silica - - - 34.48 Alumina - - - 2.40 Magnesia - - 0.39 Sulphur (bj difference) 4.01 100.00 Search was made for nickel, copper, and chrome, but no trace of those metals was discovered. The proportions of iron and of silica were not different from those of meteoric stones, but per- haps the perfect oxidation and combination of the iron with the nitric acid was the strongest evidence of its terrestrial origin that the specimen presents ; for even had nickel been discovered in it, this would not alone prove its celestial origin, since the copper ores worked at Point Shirley often contain nickel, which would be likely to be found in some of the slags. Mr. Edwin Harrison, of Cambridge, reported the result of an analysis of two specimens of Magnetite, the first from the Iron Mountain, the second from the Pilot Knob, Missouri. IRON MOUNTAIN ORE. Iron 68.95 Oxygen 27.00 Sand and Silic. of Alum. - - - - 3.07 Manganese ------ (trace) Spec, grav., 3.997 at 13.°1 centigr. 99.02 PILOT KNOB ORE. Iron - 54.307 Oxygen ------ 26.720 Insol. subs, in H. CI. - - - - 17.509 Spec, grav., 3.137 at ll.°5 centigr. 98.536 296 Mr. Sprague read the names of a small collection of cryptogamous ])lants brought by Dr. Samuel Kneeland, Jr., from the Lake Superior region, as follows, namely : — Agaricus Orcdla, Bull. ; Lycoperdon ijyriforme, Schoeff. ; Polyporus perennis, Fr., hirsutus, Fr., Cetulinus, Fr., igniarius, Fr., applanatus, Pers. ; Tnbercularia pezizoidea, Scliw. ; Usnea longissiyna, Ach. ; Sticta pulmonaria, Acli. ; Nechera pennata, Hedw. These species are all common over a broad area of the United States. They are mainly interesting as defining their range, and showing how little change is exhibited in the growths of a region extending thousands of miles. The President announced the resignation of Patrick T. Jackson, Esq., as Trustee of the Courtis Fund. It was voted to present the thanks of the Society to Mr. Jackson for his able and efficient services, and Mr. James M. Barnard was chosen Trustee of the Courtis Fund in his place. December 2, 1857. The President in the Chair. Dr. C. T. Jackson observed that a question having been raised as to the variety of sorghum from which the crystallized cane sugar exhibited at the last two meetings was obtained, he now presented to the Society the panicle of the plant he had ope- rated upon, with the ripe seed attached, which the members would observe was the true Chinese variety of the sorghum, and such as grows in this vicinity. He also presented specimens of the fructification of that vai'iety of the sorghum from Caffraria, called there the Im- phee, which is suited only to warm climates, and will not ripen in New England, but which, in warm seasons, ripens in the Southern States. 297 He remarked that, after having both last year and this demon- strated that the Chinese sugar cane produces, when ri[)e, true cane sugar with its perfect crystals, having all the replacements and secondary forms belonging to cane sugar, and wholly incom- patible with the forms of grape sugar, or glucose, and having publicly made this demonstration before the Society, by aid of excellent microscopes, he could not consider the nature of the sugar an open or undecided question, about which members had a right to entertain different opinions. It was an absolute demonstrated fact, beyond question. He had shown that the unripe plant produces grape sugar, which is readily crystal- lizable by suitable operations, and the form of those ciystals is that of grape or fruit sugar, wholly incompatible with that of the cane sugar so abundantly found in the ripe plant. He stated that the ripe sorghum juice gives from 12 to 18 per cent, of saccharine matter, and, by the usual process of sugar-making in a practical way, nine per cent, of good crystallized cane sugar. He had operated also on the Implice, which, when unripe, gave also grape sugar, and, when ripe, good crystallized cane sugar. The failui-es alluded to by Dr. Hayes, as having taken place at the South, were from operations on the unripe Imphee in South Carolina. Dr. A. A. Hayes read the following paper, on a chem- ical change which takes place in the glucose of the sorghum : — In a paper communicated to this Society some months since, I alluded to the fact, that the glucose of the sorghum cultivated in New England, like fluid fruit sugar, passes to the condition of dry, or crystalline fruit sugar. The subsequent more careful investigation of this change led to the observation, that the action is continuous, proceeding indeed during many months, and resulting finally in the production from pure glucose of sugar having the higher grade of a variety of heet root, or cane sugar. In the account which follows, the experiments were made on the glucose of that variety of sorghum which has dark purple seed coverings, the variety generally cultivated in our northern States. 298 When we extract the saccharine matter of the stalk of the sorghum, either by expression, or through the aid of water, and purify the solution by means of animal charcoal, we obtain glu- cose, holding in solution some salts of potash, lime, and soda. This glucose does not afford crystals by evaporation in desiccated air, nor does alcohol, saturated with cane sugar, leave undis- solved any sugar. The perfectly formed cells of the plant, triturated with animal charcoal, afford to boiling alcohol the same substance. The dry glucose is abundantly soluble in alcohol of 86 per cent., and the dense syrup of the same dissolves without limit in it. After ex- posure in warm air, crystalline concretions, resembling dry grape sugar, form in isolated masses. Analysis shows a large proportion of saline matter, composed of phosphoric acid, chlo- rine, sulphuric acid, acetic acid and potash, soda, lime, and oxide of iron. This saline matter forms a compound with the glucose, and thus makes up the crystalline grains, which first appear in the dense syrup. These are constant results, in treating the plant which has been cultivated the two past seasons, and they present no remarkable feature, in comparison with those obtained on glucose from other soui'ces. After the lapse of several weeks, however, the pure glucose which has been withdi'awn from the foreign aggregates exhibits the production of crystalhne points, which, becoming numerous, soon assume the forms of regular crystals. These crystals in- crease in volume, but while forming in the glucose they present skeletons, rather than solid crystals, of a pure substance, and are often grouped. Crude syrup, remaining after the concentration of the juice by rapid boiling, undei'goes the same modification, and crystallized sugar slowly separates from samples which originally did not contain any. Slips of the pith of the plant, which had been carefully exam- ined under the microscope, without any traces of crystals being found, after some months, show their cells filled with voluminous, dry crystals. Repeated trials prove that the chemical change, resulting in the production of the crystals, from glucose, is not dependent on exposure to air and loss of water, but it takes place when the syrup is kept in closed bottles. As the glucose is abundantly soluble in alcohol of 90 per cent.. 299 this agent enables us to learn at any moment the production of sugar in a sample ; the sugar when formed being nearly insolu- ble in cold alcohol. Thus, when a certain number of crystals have formed, if we withdraw by solution in alcohol the unchanged glucose, and after dissipating the alcohol, allow it to repose, crystallization recommences in the portion removed, and repe- tition^ of this experiment may be made, until after about ten months, small portions only of unaltered glucose remain. Although the evidence of the conversion of the glucose, step by step, into sugar, aiForded by the action of alcohol, is impor- tant, the observations here recorded are based upon experiments made in a similar manner, with the alkaline solution of tartrate of copper, and acidulated alcohol saturated with cane sugar ; they leave no doubt that the normal saccharine juice of the plant be- comes, per se, converted into sugar, forming regular crystals of large size. These crystals, by solution in water, are easily puri- fied, losing their porous structure and becoming solid, transpar- ent, and colorless modifications of the rhombic prism from an aqueous solution. They are always apparently more volumi- nous than the crystals of cane sugar, formed under like circum- stances, but they have all the brilliancy of cane sugar. In chemical characters, the most pure crystals yet obtained show a diversity when compared with cane or palm sugar. They are less soluble in water ; in sulphuric acid they do not exhibit the same depth of coloration that cane sugar does. With the copper test, a partial I'eduction takes place, under the same conditions, where cane sugar does not produce change on this agent. The conclusion reached is, that this sugar, wholly unlike any variety of glucose or fruit sugar, belongs to a higher class, and probably will rank with beet sugar, in most of its characters. The present is the first instance, within my knowledge, of the conversion of any variety of glucose into a sugar of high grade, after its extraction artificially. Dr. Jackson remarked that the statements made by Dr. Hayes in his paper were so extraordinary, and so opposed to the expe- rience of both scientific and practical men, that those results should be verified by others before they could be believed. If Dr. Hayes had discovered that the juice of the sorghum, after it 300 was expressed, would change, per se, into cane sugar, it was a most important discovery ; for no chemist or practical operator had ever attained such a result. Dr. Jackson was aware that starch changes into dextrine, then into grape sugar, and lastly into cane sugar, in the living organism of the plant, and that some of these changes could be effected by chemical art, but thus far no one had ever known grape to change into cane sugar^ut of the living organisms, though the contrary operation was not un- common, namely, the conversion of cane sugar into glucose, or even mannite. Up to this time we are not aware that any authority states that glucose can, by the action of any salts, be changed into cane sugar. He remarked that the term cane sugar was not restricted to a species, but to a group or family, having a rhombic prism for the primary form, and that there was undoubtedly some slight difference to be found in the dimensions of their crystalline an- gles, all of which, however, fall within the limits of the general form known as that of cane sugar, and are incompatible with grape sugar, which belongs to the cubic system. The sugar of the ripe sorghum has the crystalline form, and all the physical and chemical properties of cane sugar, and cannot be classed with any other. It exists ready formed in the cells of the plant, and may be seen by aid of the microscope in them when the plant is dried rapidly. It is obtained immediately on expression of a few drops of the juice upon a plate of glass, on which per- fect crystals of cane sugar are seen by the microscope. Dr. David F. Weinland made some extended remarks upon the Parasites of man, giving an account of their early history, from the time of Aristotle to the present day. After alluding to the two genera of Tapeworms described by Bremser, and a third genus, a species of which has been described by Kuchenmeister, Dr. Weinland announced the discovery of a fourth genus, which he names Acanthotrias (three rows of hooks). Thus far he had seen it only in the cysticercus stage. It has fourteen hooks in each of the three rows, the uppermost row being 301 the shortest. The specimen came from a dissecting-room sub- ject, in one of the Southern States, which very probably may have been a Negro. The Tcenia solium is found in England, Germany, and America. The Botriocephalus latus is limited to Switzerland and Russia, or, in the exceptional cases where it has been found in Germany, the person from whom it was taken had been to Switzerland. It remained to be determined if the new genus was peculiar to the negro race. A discussion ensued as to the manner in which these worms are introduced into the human body, the degree of heat requisite to destroy their vitality in the j5rocess of cooking, and the action of salt upon them. Dr. Weinland suggested that they might be introduced into the human body with butter and other articles, which had been cut with the same knife as measly pork, which, it is well known, is a mass of the cysticercus stage of the tapeworm. Dr. J. C. White said, that, in Germany, the ova of tapeworms were frequently found upon the green vegetables used for salad. Mr. F. H. Storer said that raw ham and pork are frequently eaten in Germany. Dx'. Chas. Pickering said that it had been noticed, in the "Western States, that the tapeworm is much more frequently found in the immigrants from Europe than in the Americans. Mr. John Green said that John Hunter speaks of a worm which was found alive in a carp which had been boiled. Dr. Weinland said that, in the instances where worms were supposed to have been found alive in cod and other fish, their motion was, most probably, not one of vitality, but due to the elasticity of their tissue. Dr. A. A. Gould stated that several hundred hogs were lost in East Cambridge, during the last summer, from the measly disorder. Mr. N. H. Bishop exhibited a pair of Albino Rats, which were caught under a barn in Medford, near the Mystic River. The President, in reply to a question from Dr. Gould, said he 302 believed albinos always propagated albinos. They certainly do through several -generations. Dr. "Weinland said he had noticed that if one of the parents has a single dark spot, however small, the pigment shows itself first in the eye of the offspring. DEPARTMENT OF MICROSCOPY. Dr. S. Durkee exhibited some of the Red Snow {Pro- tococcus nivalis) from Greenland, belonging to the Bailey collection. Mr. John Green stated that he had found the same or a similar plant near Portland, Maine, growing in the hol- low of a rock. The plant contained in its cells nuclei of a greenish color. December 16, 1857. The President in the Chair. Mr. Charles Stodder read a report upon the substance known as Gum Lahoe, which was referred to him at the previous meeting for examination, as follows : — GUM LAHOE. The specimen is an amorphous mass, made up of foldings of two colors, shades of brownish drab with some very dark brown spots, which seem to be derived from bits of bark and wood. The two shades of drab appear to be identical in every respect except coloi'. It has a slight peculiar odor, is somewhat friable, as it breaks before a knife, and is non-electric. It bears no resemblance whatever to caoutchouc, or any of the varieties of the so-called gutta percha. Its external characters mostly resem- ble those of pitch. 303 It is insoluble in water, cold or hot, but softens with heat. In boiling water it is almost fluid, and particles of bai'k and wood separate, leaving the gum nearly clean. In this state it is very adhesive, tenacious, and may be drawn into threads and sheets of great tenuity. It may thus be rendered somewhat elastic, and nearly transparent. When cold it hardens very slowly, and is compact, homogeneous, and very adhesive. After exposure to a temperature of 32°, or, during one or two days, to a tempera- ture of from 40° to 60°, it acquires a little brittleness, but readily softens by the warmth of the hand and becomes plastic. It be- comes of a dark color upon working it in the hands a short time. It is insoluble in cold or hot alcohol. In boiling alcohol it behaves the same as in boiling water, except that, the tempera- ture being lower, it is not so fluid ; after boiling in alcohol it is more brittle than after boiling in water. Left in alcohol for sev- eral days after boiling, a white flocculent matter, heavier than alcohol, is separated ; upon boiling the alcohol with the flocculi and the gum, the former totally disappear, leaving the solution clear. It is soluble in cold oil of turpentine, naptha, and chloroform, more readily and in gi'eater quantity than gutta percha. It is also readily soluble in sulphuric ether. Solutions in oil of tur- pentine, naptha, and ether are heavier than the solvent ; those in chloroform are lighter. It burns with much flame and smoke ; immediately before burning, it melts into a transparent amber-colored fluid. Ex- posed to a temperature above that of boiling water, it melts, boils, and swells, with the rapid escape of gas. The amount of the resi- due is much less than that of the original, but it seems to possess nearly the same properties ; this point, however, was not fully examined. It is a vegetable product, intermediate with the resins and gutta tuban or percha. Dr. A. A. Gould read a communication from Dr. Skil- ton, of Troy, N. Y., upon Equus Major, as follows : — EQUUS MAJOR. The last summer, 1857, Col. Leonard McChesney found, in his ploughed field in Brunswick, one mile from the city of Troy, 304 a number of teeth of the Fossil Horse ; the spot of marshy ground where they were found had, by trenching, been converted into a fine soil for garden crops. Mr. McChesney has been so fortunate as to find two incisors, slender in form ; of the lower jaw, both the first molars, and three out of the next four molars on each side, viz : second, third, fourth, and fifth ; of the upper jaw, the left first molar, and three on each side of the next four molars, — embracing of this animal's teeth seventeen. Of all the Fossil Horse teeth we have seen, there is decayed out of them all the fangs and bony parts, some of the dentine, and in this instance more or less of the ends of the plates of enamel. The length of the enamel of the first upper molar still remaining is 1.9 in., ditto the first lower molar is 2.33 in. ; length of longest upper molar is 2.9 in., ditto longest lower molar is 3 in., ditto of incisors, 2 in. Dr. Dekay, at the time of the publishing of " The New York State Natural History," had not learned of the discovery of any fossil horse remains in this State. Some four or five years since, a lower first molar, in a fine state of preservation, was picked up by the writer's son, George S. Skilton, on the margin of one of the rivers near Troy. Dr. J. C. White read a paper on the development of Tapeworms, as follows : — GENERATION OF THE HELMINTHES. I thought it might not be uninteresting, after the interest evinced by the Society at the last meeting on the subject of the Helminthes of the human body, to give, in a few words, the ideas now prevalent in Germany in respect to their development. Let us take the joint or proglottis of a Tcenia solium, and watch it through its phases. We know that it is a perfect indi- vidual by itself, capable of reproducing, and that when mature and filled with eggs it becomes congested, sepai'ates itself volun- tarily from its next younger joint above, and is discharged. We will suppose now that by some means to be presently considered, the eggs regain entrance within the intestinal canal after their wanderings. Each ripe egg or embryo consists of a body armed 305 with three pairs of hooklets, by which it is able to burrow in tis- sues, and make its way to any j)art of the human system. After it has found its proper nidus, be it muscle, brain, eye, or other organ, and has become encysted, its hooklets drop off, and from its walls a protuberance grows inwards, which gradually changes into a head, neck, and body, or, in other words, becomes the sco- lex. This at first remains enclosed within the embryonic blad- der as a receptacle, but later the animal pushes itself free. Its head has now become that of the true Ttenia, and from it depends the former receptacle as a bladder. Siebold maintains that this cyst is only a joint of the scolex, which has become dropsical ; but Kuchenmeister (and his views are adopted by all modern pathol- ogists) insists that this is another stage of development, and the normal condition of the animal. Now, unless the encysted ani- mal is set free artificially, the genei-ation stops here ; but if, in any way, it escape, and again find entrance within the intestinal canal, it fastens itself by its head to the walls, its bladder drops off, leaving behind the marks of attachment on the oldest joint, and in its place the true joints of the Tjenia are developed, form- ing the animal with which we started. It is only by this method that a Taenia can be produced ; for the eggs or embryos of the proglottis either pass into the tissues, and become there encysted scolices or nurses, or else pass away with the fiBces, At all events, they are never converted pri- marily into Tainiae, else we should find tapeworms as plentiful as ascarides. To account for the production of Tgenite, therefore, we must admit the scolex within the intestinal canal, and this may be done more easily than we imagine. The head of the Cysti- cercus is but a mere mite, and it is not necessary that its bladder should accompany it, which, as above mentioned, drops off, leav- ing behind the mark of its former attachment. We know how general a disease this parasite forms among swine ; but it is not wholly confined to them ; for we find it also, though seldom, in the bear, deer, and ox, not to mention many other animals, so that nations who eat no pork may be infested by Ttenire. It is probable that many scolices may pass through the intestinal canal of man, and yet not generate the tapeworm, for it must attach itself to its walls before the joints are produced. PROCEEDINGS B. S. N. H. — VOL. VI. 20 APRIL, 1868. 306 Some authorities would have it that the embryo discharged from the proglottis is capable of an immediate conversion into the scolex by burrowing into the soft tissues of the same indi- vidual; but it is more probable that the eggs must first leave the intestine, and mature outside, since scolex seldom occurs together with Ta3nia, and then it is probably accidental. When the mature proglottis is discharged fi"om the intestine, it deposits its eggs in moist earth, on plants, in the water, and so on. These eggs are covered with a very thick membrane, which withstands much pressure between the glasses of a microscope, and they are capable of remaining a long time quiescent, like other pai'asitic ova, till a suitable menstruum is found for their development. That they may pass into the stomach of man and other animals with various articles of diet and drink is unquestioned ; for they are found in water, and on salads and other vegetables, which are eaten without being previously cooked, and sometimes not even washed. The genus Ta3nia still requires much study to remove the doubt which rests upon several species. Five or six are known, which find a habitation in man, ( T. solium ; nana ; mediocan- nellata ; ecMnococciis ; T. of Good Hope ; and T. or Bothrioce- phalus latus,) one of which wants the booklets peculiar to the rest. They may be found wanting also in T. solium, in some instances. Of these species the scolices are unknown, with the exception of Cysticercus and Echinococcus. The encysted form of Bothriocephalus may have been confounded with that of T. solium. The joints of this worm are thrown off in chains, and not singly, as with Taenia. Two varieties of the Cysticercus have been observed. Of course, after the adoption of the scolex theory, it became interesting to inquire where the Ttenia of the common Echino- coccus had been all this time. Siebold thought that the Ta3nia of the dog was the animal in question ; for he gave the Echino- coccus of animals, ^. veterinorum, to dogs, and at the end of twenty-two days found in their intestine a Taenia with but three joints ; the last one perfect, however, showing that the animal had arrived at maturity. This view was generally adopted till quite recently, when Kiichenmeister showed that the E. veterinorum differed from E. /lominis in the form of its booklets, and he gave 307 some of the latter in soup to a criminal condemned to be exe- cuted, and on dissection a Taenia very like T. solium was found, with but three joints, and bearing a head of Echinococcus. This T. ec/iinococcvs, as he calls it, had so long escaped observation only from its diminutive size, it being only three lines in length. The last proglottis of the three was perfect, and contained the sexual organs. This is a late discovery, and must not be con- founded with T. echinococcus of Siebold, who made the E. homi- nis and E. veterinorum the same species. In our study of these important and interesting parasites we notice three stages of development. First we see the proglottis leaving the intestine, and apparently seeking in the outer world of light and pure air some element, of which we are ignorant, for the development of the embryo. It possesses fibres capable of conti'acting after it has left the body, and finally discharges its eggs from the ovi-sac. These lead a nomadic life till by chance they once more gain admittance to their old haunts, where, in- stead of remaining contented, they burrow at once into the tis- sues, and then, after the formation of a head, leave them again, if possible, to resume their former quarters in the intestine, where the last stage of development is completed. We can but notice that the Taenia feeds upon matter which has not been oxygenized or converted into tissue ; whereas in its other state it exists upon the substance of animal life itself. Ivo- kitansky noticed in the bladder of a Cysticercus, found in the brain, shreds of nerve fibre ; and they must obtain from the hu- man tissues they prey upon the great amount of calcareous mat- ter found in their concentric corpuscles. What the object of these is no man knows ; but the advancement in this branch of observation within the last few years leads us to hope that light may be thrown upon many points in their history, now obscure. Dr. Gould read a communication from Mr. William Stimpson, upon a new form of parasitic gasteropodous moUusca, which he calls Cochliolepis parasiticus, as fol- lows : — In the spring of 1852, while investigating the marine fauna of the coast of South Carolina, in company with my friend, Lieut. T. D. Kurtz, U. S. A., I had the fortune to meet with a new form of parasitic gasteropodous mollusca, living under circum- stances quite unique in this order. We had succeeded in cap- turing some gigantic annelides of the Aphrodita family, (^Aco'etes lupi7ia,) which lived in thick leathery tubes, extending down two or three feet into the mud near low-water mark. Upon drawing one of these worms from its domicil, some bright blood- red objects were found concealed under its scales, which, upon examination, proved to be little shells, resembling in size and shape our common Plaiiorbis exacutus. These were placed in a watch-glass of sea-water, and drawings made of them, which are presented herewith. The publication of these figures has been delayed, in the hope that opportunity would occur for a more thorough investigation of the structure of the animal, with the view of determining its place in the system. It has not, however, since been met with ; and as the subject is one of great interest, I have been led to give at this time such information as could be collected from the specimens first discovered. For this curious animal, which evidently forms a new genus and species, I would propose the name COCHLIOLEPIS PARASITICUS. The animal was of a blood-red color ; foot oblong, tapering behind with a rounded extremity, slightly auricled before, ante- riorly bimarginate. Head small, rounded and notched in front, without veil. Tentacles slender, tapering, equalling in length the diameter of the shell. Eyes none. (?) A small supple- mentary plicated gill on the right side, projecting out freely be- 309 yond the aperture of the shell, and attached only at its constricted base. Two long cirri arise fi'oni the body on the right side, near the junction of the mantle ; these protrude like vibracula from the superior angle of the aperture, when the animal is in motion. Operculum thin, flexible, and pellucid. The shell is thin, discoidal, convex above, concave and um- bilicated below; the edge thin and sharp. Whorls three in number, rapidly enlarging. Surface smooth and glossy, indis- tinctly striated with lines of growth. Lip not thickened. Diam- eter one eighth of an inch. Hab. Harbor of Charleston, S. C. ; parasitic on Acoetes lupina. Dr. B. J. Jeffries exhibited the Atlas and Axis of a man about fifty-five years of age, and very muscular. The Odontoid Process was not united with the Axis. Mr. Edward Daniels, State Geologist of Wisconsin, and a corresponding member of the Society, presented a number of geological specimens from that State, and remarked as follows : — Occurring throughout an extensive district of Eastern Wis- consin and Northern Illinois, is a rock of Upper Silurian Age, clearly corresponding to the Clinton or Niagara groups of the New York Reports. In numerous localities, this rock contains cavities and thin seams filled with solid bitumen, which is fre- quently found in the digging of wells and cellars, and is commonly called coal. Near Chicago, is an outcrop of this rock, in which bitumen is very extensively found, in fluid form at ordinary tem- peratures, as well as in the solid state. The cavities sometimes contain half a pint. The rock is an Encrinal Limestone, the en- crinal forms being quite distinct in the northernmost portions of the district. From the walls of a church erected of this stone the bitumen has exuded and run down in streams, giving the building the appearance of some of the ancient ruins of Europe. The scale of bitumen peels ofl", however, after some time. Quar- ries have been opened in the limestone to the depth of fifteen 310 feet. A few corals are found in it, and occasionally some of tlio larger cor^s. Mr. Daniels also presented some minute Trilobites, and other fossils, from the base of the Potsdam Sandstone of Wisconsin. The localities were various : the valley of the Black River, in the northwestern part of the State, the mouth of Black River, and a spot sixty miles up the same river. He stated that they were interesting, being the oldest fossil forms yet found in this country, the sandstone resting directly upon the upturned edges of the Azoic rocks. Upon a small island in Black River he had found perfect impressions of Crustaceans, consisting of double rows of parallel tracks, precisely like those in Montreal. Mr. John Green — referring to a specimen of Silicious Infuso- rial Earth presented to the Department of Microscopy, Novem- ber 4, 1857, and which was at that time said to contain copper — stated that other samples of the earth had since been analyzed by Mr. Albert Gould, of the Lawrence Scientific School, with the following result, viz : — Organic Matter and Water - . - 14.48 Silicic Acid 82.03 Carbonate of Lime ----- 0.32 Oxide of Copper ----- 0.89 Sesqui-Oxide Iron and Alumina - - 1.47 Loss _-_---- 0.81 100.00 This result is the mean of two determinations. Mr. Gould stated that the specimens came from a pond in Beddington, Maine, between ten and fifteen feet in depth, and about eight or ten acres in extent. When treated with boiling chlorohydric or nitric acids concentrated, no copper was found by the sulphuretted hydrogen test. The same was the case with diluted aqua regia. When boiled with concentrated aqua regia for an hour, some copper was found; but when it was fused with carbonate of soda, which certainly was itself free from copper, nearly one per cent, of copper was obtained. Before the blow- pipe also, on charcoal, a spangle of metallic copper was seen. 311 From the action of alkalies it woulil a|)pear that the copper was combined with silica, and not an accidental ingredient. Dr. H. R. Storer exhibited a Porcupine, {Hystrix dor- sata, Lin.,) shot in New Hampshire, and belonging to the collection of Master Frederic Gilmore. He also exhib- ited, in connection with it, the representation of this ani- mal, figured by Audubon and Bachman, showing it to be extremely inaccurate. Messrs. John D. Philbrick and Edward P. .Jeffries were elected Resident Members. DONATIONS TO THE MUSEUM. October 7, 1857. A fragment of a Human Cranium, whicli was said to have been found in deposits coeval with the Mastodon, in California; by Dr. C. F. Winslow. Specimens of intergrowing and intertwining woods from Surinam ; by Dr. Jeffries \V.T,nnun. A collection of Radiata from the Gulf of St. Lawrence, and a Fish from the North Atlantic Ocean, which probably belongs to a genus new to North America; by Capt. N. E. Atwood. A collection of Crustacea made in California by Mr. E. Samuels, containing fifteen species, viz : Chiome- cetes Behrinyianus, Epiallus productus, Cancer gracilis, C procluctus, C. antenna- rius, Pachyrjrapsus crassipes, Pseudorjrapms Oregonensis, P. nmlus, Hippa analo- gica, Porcellana rupkola, Gebia Pugettensis, Calliannssa kmgimana, Astacus Trmo- bridgii, Crangon Franciscorum, C. nigricaud/i : by E. Samuels. Crustacea from the Northwest Coast of the United States; by the Smithsonian Institution. A collection of Animals in alcohol, made by Dr. S. Kneeland, .Jr., in the region of Lake Superior; by Dr. S. Kneeland, Jr. The Skin of a Ray; by Dr. D. H. Storer. October 21. Microscopic preparations of the Diatomaceous Exuviaa of the Post-tertiarj' Sand of Glenshira, near Inverary, Scotland ; by Prof. Gregory of Edinburgh. A collection of Minerals made in the mining districts of Lake Su- perior; by Dr. S. Kneeland, .Jr. A collection of Algas from Australia, Ceylon, and the Friendly Islands, prepared by Prof. Hai-vey ; by Dr. Benjamin D. Greene. A Red Phalarope, Phalarojms fuUcularius, Bonap. shot on Charles River; by C. W. Lovett, Jr. A Fish from Boston Harbor; by E. Samuels. November 4. A section of an elm exhibiting a singular curved growth ; by Prof. Theophilus Parsons. A living specimen of young Bald Eagle, nnt, wings, a large macula upon the pleui-a below the wing, and another be- tween the anterior and medial feet, dusky: antennae (9) 14- articulate, verticillate, slender, articulations separated, scapus rather thick, and with the pedicellum translucent ; $ about 24- articulate, slender ; palpi slender cylindric, 3=articulate, terminal articulation more slender and larger than the preceding ones : thorax with three large oval conspicuous dusky vitta? : abdomen 9-articulate, two basal articulations dusky above. This insect in the larva state feeds upon the leaves of the Rohinia pseud'ocacia, the margin of which it forms into a roll. Tlie larva is white, or pale orange, of 13 segments, the first of which receives the retractile head ; nine segments, from the fourth to the twelfth inclusive, with spiracles. The pupa does aiot foniu a cocoon, but lie^ without a covering. It can move itself by means of tho abdomen. The insect is not strictly a Ceci- PEOCEEDINGS R. S- N, H. — VOL. VI. 26 JANUARY, 1859, 402 (lomya, the posterior vein of the wing being interrupted, the basal portion sending a deflected filament (which does not seem to be hollow) to the middle of the posterior margin. The disrupted parts of the posterior vein pass and run parallel to each other for a short distance, the apical portion being the more anterior. Two species of minute parasitic Hymenoptera destroy a great many individuals of this insect, which, in conjunction with Odonta scutellaris, Oliv., has for several yeai's killed the foliage of Robinia in southeastern Pennsylvania, so that the trees present the appearance of having been destroyed by dry weather, the brown leaves remaining upon the tree. This happens chiefly in August. EKIOPHILUS. Hald. The new geijeric name (meaning wool-loving) is given in allu- sion to Eriosoma, upon which this insect is parasitic ; and the trivial name mali has reference to the apple-tree, upon which it is found. Observing the dead and black specimens of Eriosoma, with the body plump, but hollow, and a small perforation posteriorly, we examined other individuals without the perforation, and found them to contain the naked pupa of a minute hymenopterous in- sect, which, before it left the larva state, must have bored through the belly of the Eriosoma and aflixed it to the branch. This insect belongs to the family of Ghalcididce, and has the following generic characters : — Head free, transverse, eyes large, and set with short stiff hairs ; antennae with short pile, elbowed, with six articidations, the first long (in the male), the second subconical, the third and fourth short and equal, the fifth subcylindrical, and the sixth fusiform ; in the female the flagellura is fusiform, the second and fifth joints short, and the wings ample, the anterior on'e with the subcostal vein straight, the stigmal branch very short, and difficult to distin- guish ; basal portion of the disk without pile, anterior and ex- terior margin short ciliate ; posterior wing ciliate with long hairs. Feet slender, pentamerous, adapted for leaping ; medial tibial spine long, anterior one curved. Abdomen sessile, and rather long, having a sharp slender exsertile sting or ovipositor in the female. Pupa without a follicle. 403 E. malt. Length one twenty-fifth of an inch, expanse of the wings about twice this amount. Body shining black, with a few hairs ; front vertically impressed upon each side of the middle for the antennte, eyes violet, scabrous, short pilose ; antenncB (ex- cept the first and base of the second joint) lohile. Wings with two straight lines of pile running at an acute angle from the end of the subcostal vein across the disk, which is densely pilose ex- terior to them. Base of the abdomen yellow, followed above by several indistinct brownish transverse bands. Anterior feet wliite, the femora (except the apex) black ; medial femora black, base and apex white, tibice black, with the apex and the tarsi white. Posterior femora and tarsi (except the base) white. Leaps with agility. The genus seems to have some affinity with Agonioneurus. APHIS (pemphigus) stamineus. Hald. This name is proposed for a large species of Aphis, which forms follicles on the leaves of the silver-leaved maple, (Acer eriocarpum.) Male. — Black, feet long, slender, and rufous ; tarsi bi-articu- late ; wings slightly deflexed, translucent, pale ferruginous at the base, submarginal nervure conspicuous, black, and ending in a long stigma ; disk with four simple nervures ; posterior wings with three nervures ; mesonotum polished, with a deep Y-shaped impression ; abdomen without tubes ; pi'omuscis obsolete, anten- nas 6-ai"ticulate, the first two short, the third long, and the fourth, fifth, and sixth gradually lengthening ; length of the body, 1^ line ; or to the end of the wings, 2^. Female and pupa. — Apterous, dark-reddish brown, feet paler ; promuscis twice as long as the head, thickened near the apex ; length, 1^ lines. Dr. Gould observed, in relation to the food of the robin, which had been spoken of at the preceding meet- ing, that experiments, conducted since midwinter, show that its crop is found full of insects at night ; as many as 500 have been found in a single bird. It is difficult to understand how they get such a full supply in cold weather. 404 Mr. C. J. Sprague, exhibited a castor bottle contain- ing red pepper, which was completely riddled by the grubs and perfect insects of a little beetle, apparently the same as he had formerly found committing its ravages among the plants of the Society's herbarium. It was Ptinus fur, according to Dr. Pickering. Dr. J. C. White read a report on the parasites of the Orthag-oriscus mola (Sun-fish), referred to him at the last meeting. They consisted principally of female speci- mens of Pennella filosa. Dr. White gave an account of some interesting points in their structure. Attached to the Pennellce were numbers of Cineras vittata. Attached to the bodies of the Cineras and to the ovaries of the Pennella were numerous polyp stems, the Laomedea gelatinosa. On the skin of the same fish were other crustacean parasites, usually called " fish-lice," the Cecrops Latreilli. The tissue of the sun-fish, which is so elastic as to rebound to a considerable height when thrown upon the ground, was found by Dr. White, on microscopic exam- ination, to consist almost wholly of yellow elastic fibre, interlaced in an intricate manner, and presenting no ap- pearance of true muscle. There may be a little white fibrous tissue intermixed, but the alcohol had so inter- fered with the action of reagents as to render its detec- tion uncertain. Dr. Gould spoke of the great difficulty which he had recently found to exist in Europe in obtaining American works on Natural History, although they are eagerly sought for, especially in Germany. He alluded to the high prices charged for American books by the inter- ference of foreign booksellers, and mentioned one, the cost of which in America was $4, and in Europe $24. The President nominated as a Committee on the sub- 405 ject of Dr. Hayes's proposed Arctic Expedition, Prof. Theophilus Parsons, and Drs. A. A. Gould and S. Knee- land, Jr., and they were chosen. Jules Marcou, of Zurich, Switzerland, was chosen a Corresponding Member; and Dr. Daniel V. Folts, of East Boston, and Thomas Motley, Jr., of West Roxbury, Resident Members. DONATIONS TO THE MUSEUM. July 7, 1858. A fossil Asie7-ias from Lewiston, Me. ; by William W. Raker. A Scup, PcKjrus argyrops, Lian., from Lynn, Mass.; by Zaccheus Phillips. A young Gopher, Spermophilus tredecimUneahis, Mitch., and a specimen of Crys- tallized Iron Ore, from Minnesota; by Dr. S. Kneeland, Jr. September 1. A Trilobite, Pm-aJoxides Ilarlani, neai-ly perfect, from Brain- tree; and a specimen of rock containing native gold, from the Steele Mine, Montgomery Co., North Carolina; by Dr. C. T. Jackson. Two specimens of the Glow-Worm, from Cohasset; by Charles J. Sprague. Specimens of Crustacean Parasites from the Sun-Fish, 0 rthagoriscus mola, the jaws, and a portion of the flesh, from Cohasset; b}' Dr. S. Kneeland, Jr. Shells from Sweden, fossils from Maine, and alcoholic specimens of the internal organs of birds, and some Cirri- peds; by Dr. S. Cabot, Jr. September 15. European Shells, and a large Beetle; by Dr. D. F. Weiuland. Internal moulds of Ai-ca, and a fragment of fossil bone, probably cetacean, from New Jersey ; by Charles K. Landis. A portion of rock containing Encrinitss and fossil shells from Sharon Springs, N. Y. ; by C. B. Fairbanks. Specimens of Ophiui'a, taken from cods' stomachs, and crustacean parasites from their gills; by Dr. S. Kneeland, Ji-. Specimens of Motella, from Nahant; by C. Cooke. Three specimens of Ehotris (nov. sp.), one of Vomer Brownii, one of Ikemulon fonnosum, and four of Clupea, from Hayti, and one of Pelromyzon JlmmlUis, from Berlin; by Dr. D. F. Weinland. Specimens of Fundulus pisctdentus, Hydrargyra Jlavula, Cyprinodon variegatus, Poecilia laiipinna, and Heterandra Ilolbrookii ; by Prof. Holbrook, of Charleston, S. C. BOOKS RECEIVED DURING THE QUARTER ENDING SEPT. 30, 1858. Prodromus Descriptionis Animal iura Evertebratorum. Auct. W. Stimpson. Parts v., VI. 8vo. Pamph. Philadelphia, 1858. From the Author. Experiments on Sonorous Flames, with Remarks on the primary Source of their Vibration. By Prof. W. B. Rogers. 8vo. Pampli. New Haven. From the Author. 406 Essay on the Tapeworms of Man. By D. F. Weinland, P. D. 8vo. Pamph. Cambridge, 1858. From the Author. Keports on Railway and Electro-Magnetic Telegraph from Quebec to Halifax. 8vo. Pamph. Fredericton, 1847. From M. H. Perky. Notes pour servir a une description Geologique des Montagnes Rocheuses. Par J. Marcou. 12mo. Pamph. Geneve, 1858. From the Author. The Dudley Observatory and Scientific Council. Statement of the Trustees. 8vo. Pamph. Albany, 1858. From the Trustees. Notes on American Land Shells. By W. G. Binney. No. 8. 8vo. Pamph. Philadelphia, 1858. From the Author. London Geological Journal. Nos. 1, 2, 3. 8vo. London, 1846-7. 3 copies. From E. Charlesivorth, F. G. S. Natural History Review. Vol. V., No. 2. 8vo. London, 1858. Zeitschrift fiir die Gesammten Naturwissenschaften. Jahrgang, 1857. Zehn- ter Band. 8vo. Berlin. Canadian Journal of Industry, Science, and Art. No. 16. July. 1858. Toronto. Bulletin de la Soci^te de Geographic. Tome XV. 8vo. Paris, 1868. Jahrbuch der K. K. Geologischen Eeichsanstalt. Vols. 1-3 and 5-8. 8vo. Wien, 1850-58. Malakozoologische Blatter. V Band 1-2. Bog. 6 Taf. Genera of Recent Mollusca. By H. and A. Adams. No. 34. London, 1858. Conchological Miscellany. By S. Hanley. Parts 3-10. 4to. London. Sowerby's Thesaurus Conchyliorum. Part 18. London. Proceedings of Zoological Society of London. Part 25, for 1857. 8vo. London. New York Journal of Medicine. Vol. V., No. 2, for September, 1858. Archiv fiir Naturgeschichte. Drei-und-Zwanzigster Jahrgang. Viertes Heft. 8vo. Pamph. Berlin, 1857. Proceedings of the Royal Geographical Society of Loudon. Vol. 2. Nos. 1, 2. 8vo. London, 1858. Journal of the Royal Geographical Society. Vol. 27. 8vo. London, 1857. Silliman's American Journal of Science and Arts. No. 77, for September, 1858. Canadian Naturalist and Geologist. Vol. 3, No. 4. Montreal, 1858. Proceedings of American Philosophical Society. Vol. VL, No. 59. January to June, 1858. New York Journal of Medicine. Vol. VL, No. 1. July, 1858. Canadian Journal of Industry, Science, and Art. New Series. No. 17. Sept. 1858. WiirttembergischeNaturwissenschaftliche Jahreshef te. Dreizehnter Jahrgang. Drittes Heft. 8vo. Pamph. Stuttgart, 1857. Silliman's American Journal of Science and Arts. 2d Series. No. 76, for July, 1858. Received in Exchange. Annals and Magazine of Natural History. No. 7, Vol. 2. July, 1858. Lon- don. Quarterly Journal of the Geological Society. No. 55. Aug. 1858. Svo. London. Cyclopcedia of Anatomy and Physiology. By R. B. Todd, M. D., F. R. S. Parts 49 and 50. 8vo. London. 407 Annals and Magazine of Natural History. Vol. 2, No. 8, lor August, 1858. London. From the Courtis Fund. Encj'clopajdia Britannica. Vol. XVI. Memoirs of the Life of John Quincy Adams. By Josiah Quincy, LL. D. 8vo. Boston, 1S58. Deposited by the Ripiiblican Institution. October 6, 1858. Dr. C. T. Jackson in the Chair. Prof. Agassiz, as an introduction to the description of some new fishes from Lake Nicaragua, made some remarks on classification. He observed that as yet there is no natural ichtliyological sys- tem. The three principal ones which have attracted the attention of naturalists are the following, in chronological order. 1. That of Cuvier, remarkable for its precise divisions into natural fami- lies, founded on the consistence of the skeleton, and on the char- acters and situations of the fins. 2. His own system, based on the structure of the scales ; this, though placing too great stress on external characters, led to the discovery of many interesting affinities between the scales and the internal organs. 3. That of Johannes Miiller, deriving the characters from purely anatomical Structure, leading to combinations without regard to zoological differences. The fault of all these systems is their exclusiveness, attaching too great value to single characters. He thought a combination of the three systems would lead to a better appre- ciation of certain groups. The Nicaraguan fishes, collected by Julius Fi-oebel, are representatives of four genera of a single family, foreign to North America ; though much resembling Pomotis, they belong to the family of Chromids. In the family of Labroids, in which the Chromids were for- merly included, the last pharyngeal bones are united into a single odd bone, without trace of suture — there is no fissure between the fourth and fifth branchial arches ; the last gill is imperfectly de- 408 veloped ; the scales are cycloid, and the tubes of the lateral line branching. Ileckel separated the genera Cichla and Chromis, and with the Scicenoids having less than seven branchiostegal rays, formed a distinct family, the Chromids. Miiller found that the first of these differed from the latter, which have no suture in the last pharyngeal bone, and pseudobranchia on the inner surface of the operculum ; he called the latter Pomacentrini ; for the former he retained the name Chromids, uniting them, however, under the name of Phcu-yngognathi, and including with them the genera Belone, Scomheresox, and Exocetus, but which really are in no way allied to the Labroids, Pomacentrini, and Chromids. Eveiy Labroid is a marine fish ; all the Chromids are inhab- itants of fresh water, and peculiar to South and Central America, except one species in the Nile, and one in South Africa. Of the four genera from Nicaragua, one, were it not for the inter- rupted lateral line, would reseinble very closely Dentex ; Prof. Agassiz proposed to call it Parachromis gidosus. A second, re- sembling Chrysophrys, he called Hypsophrys unimacidatns. A third resembling Bodps, he named Baiodon fasciatus. The last he called Amphilophus Froehelii, which is peculiar in not having the ordinary fleshy lips, but a large triangular lobe projecting above the upper and below the lower jaw, like the nasal append- ages of some bats. Though the form of these Chromids varies from the elongated shape of the Pickerel to the roundness of the Bream, there is one character common to all — the second dorsal fin and the anal are pointed backward, extending over the caudal. Though coming from the same lake, and belonging to the same family, the disti'i- bution of the colors varies considerably ; yet it is derived from one pattern. Prof. A. showed how from the simple vertical bands of the sides, a longitudinal line was formed by the increase and union of the color in the centre of the bands, and its fading above and below ; and how in the H. unimaculatus a single spot was developed to the exclusion of the rest. Dr. C. T. Jackson exhibited some fine samples of to- bacco, Nicotiana tabacum, raised in the Connecticut valley, at Hatfield, Mass., by Mr. Dickinson. On drying it, the specimens were found to lose 88 per cent, of their 409 weight; on being bnrned, the stems decrepitate, indi- cating the presence of nitre ; the main stalks decay rapidly and form an excellent manure ; it is an exhausting crop, and requires rotation with others. As much as 2500 lbs. of the dried tobacco, worth between $400 and $500, have been raised to the acre. The leaves are thin, smooth, and wide, and are largely exported to Havana for the covers of cigars. Dr. A. A. Gould gave an account of a recent visit to some of the scientific institutions of Europe, confining his remarks to Great Britain. Mr. Charles T. Carney made the following commu- nication : — " In September, 1857, I was led to investigate the Sesquioxide of Chromium, with a view of decomposing the same without in- jury to any organic matter which might be pi-esent with it. The means usually employed for effecting the decomposition, by boil- ing sulphuric acid, &c. were of course unavailable, and I was much interested in observing a peculiar reaction which was new to me ; and I do not know that it has been before observed. I found that when the ignited sesquioxide was exposed to the action of the galvanic battery, in presence of a dilute solution of caustic alkali, it was decomposed, and the chromate of alkali formed in solution. Thinking it possible that a combination might occur with the caustic alkali and some soluble portion of the chrome oxide, I next subjected some freshly prepared and ignited sesquioxide to the action of caustic alkali for twelve hours ; then after being thoi'oughly washed and dried, submitted it to the action of the battery. The result was the same, and from the solution of chromate of alkali obtained, I formed the chromic salts of lead and silver." Stephen P. Leeds, of Brooklyn, N. Y., was chosen a Corresponding Member. Octavius Pickering, of Cambridge, and Dr. C. F. Win- slow, of West Newton, were chosen Resident Members. 410 October 20, 1858. Dr. Durkee in the Chair. Dr. A. A. Gould continued his remarks on the Euro- pean collections of Natural History, giving brief sketches of those of Paris, Florence, Vienna, Munich, Bonn, Am- sterdam, Leyden, and Glasgow. Mr. Theodore Lyman read a paper on the forms of birds, the object of which was to show how form, as depending on structure, may be recognized in this class, and may be expressed by meas- urements. He had compared, for this purpose, a hawk and an owl, and a duck and an auk, showing that the form is character- istic in each group, which may therefore be looked upon as a natural family in the animal kingdom. There is no essential difference between the bill and claws of the hawk and owl ; there are, however, very striking differences in the size and position of the eyes, the bulk of the lower body, and in the length of the tarsus. Owls have large, prominent eyes, turned to the front, a body bulky below, and (generally) a very short tarsus ; their abundant plumage is so arranged as to bring out these features ; the feathers of the head make a kind of face, in the midst of which appear a half-buried beak and a pair of round, staring eyes ; the body is large and heavy looking, growing larger below, and apparently ending in a partly concealed pair of feet ; the natural position is bolt upright, on account of the short tarsi and the weight of the body in front. Hawks have eyes of moderate size, rather sunken, and on the sides of the head ; the body is elegant and compact, and the tarsus generally long ; the plumage is commonly shorter and closer ; the ordinary position is with the body standing well up on the legs, and inclined at a small angle from vertical. The owl gives the idea of solemnity and gravity, the hawk that of alertness and vigor, but both share the expres- sion of ferocity. In the auks and ducks, both water-birds, the chief elements of difference are the plane of the bill with reference to that of the 411 head, the shape of the body, and the position of the legs. The ducks have the bill flattened in a horizontal and the head in a ver- tical plane, and the legs placed so far forward that they can move, though awkwardly, on land ; the neck is long and slender, and the body short and chubby. The auks have the head com- pressed in a horizontal and the bill in a vertical plane ; the body is very long and flattened vertically ; the legs are entirely be- hind, and the tibia is so bound down by the integuments, that the animal, on land, often tumbles forward, and assumes when stand- ing an upright position. The paper was accompanied by drawings, and by tables giving the proportions of the skulls and skeletons, and showing the characters of the families. Prof. Agassiz made some remarks on two Pomocentri- dcB from the Florida reefs, of the genera Glyphisodon and Pomacentrus, the latter being a new species called by him P. meleagris. The family of Discoboli, of which the Lump-fish is the chief representative, is very interesting both anatomically and zoologi- cally. Swainson arranged the lump-fish with the lamprey-eel, which is as bad as placing the bat among the bii'ds. Cuvier placed it with the malacopterygians, with the Gadidce and Pleura- nectidce. J. Miiller separated the Discoboli from malacoptery- gians, and placed them with the acanthopterygians, where they belong ; but from the fact that the ventrals are united into a disk, he erroneously placed them in a family Cyclopodi, with Go- bius, separating Eleotris from the family. The genus Echeneis, according to Prof. Agassiz, belongs among the scomberoids. He gave some of the characters of the genera Cyclopterus, Liparis, Gobiesox, and Lepadogaster, of the family Discoboli ; — in Lepado- gaster there are two pairs of pectorals and two pairs of ventrals, one pair of which consist each of folds of skin only, and are not true fins ; the membranous fold of the second pectorals contains fibrous rays, and is attached to the shoulder bone, the membranous ven- tral fold is attached to the styloid bone. These structural fea- tures render a separation of Lepadogaster and Cyclopterus as 412 distinct families necessary. He would place the Discoboli not at all with Gobius, but in the neighborhood of the sculpins. He pre- sented to the Society specimens of three new genera of this fam- ily, as follows : Crossognathus, Ag., from Charleston, S. Carolina ; Lobognathus, Ag., from Peru ; and Plychoclieilus, Ag., from Puget Sound. The following communication was received from Mr. William Stimpson : — Smithsonian Institution, Washington, D. C, Oct. 1, 1858. I wish to place on record in the Proceedings of the Society the existence of a remarkable new form of Brachyurous Crustacean on the coral reefs at Hawaii. It cannot be properly I'eferred to any known family, although having perhaps more resemblance to Pinnotheres than any other known genus, as its integuments ai-e soft, and the female abdomen of great size, — in fact larger than the carapax. Its place in the series is pi'obably between Pin- notheres and Hymenosoma. Four specimens only are in my possession, which are, unfortunately, all females. They were collected by the scientific corps of the U. S. North Pacific Sur- veying Expedition, under the command of Capt. John Rodgers. It may be called HAPALOCARCINUS MARSUPIALIS. The shell or general integument of the body is but little indu- rated, quite soft and flexible, such as occurs after moulting in other crabs. The feet however, particularly the chelipeds, are sufficiently firm. The carapax is leather depressed, smooth, and glabrous, suboval, longer than broad, narrower in front than be- hind, somewhat truncated at either extremity, and without teeth or spines on any part. Front horizontal, straight. Orbits small, excavated in the anterior margin. Eyes short, oblique, inclining to longitudinal, and scarcely retractile. Antennula3 very short and minute, placed at the inner angle of the orbit. The epis- tome is scarcely distinct, as the lamelliform maxiUipeds reach nearly to the eyes and antenna?. The buccal area occupies the whole breadth of the carapax anteriorly, the outer maxillipeds covering the subhepatic regions. The maxillipeds are loosely applied, as in some Anomoura, and those of the two sides are 413 separated from each other at the base by the triangular anterior extremity of the sternum, which is greatly prolonged. In the outer maxillipeds the ischium-joint is enlarged and dilated within, while the meros is very small, and slender like the last three joints or palpus ; the exognath is slender and palpigerous. The feet are slender and weak, smooth and shaped nearly as in Pinnotheres. The chelipeds are equal, and about as long as the ambulatory feet, and twice as thick. Fingers of the hand nearly straight, longitudinal, and shorter than the palm. Dactyli of the ambulatory feet all very short, and slightly uncinate. Sternum very broad and smooth, with the genital orifices rather wide apart. Abdomen of great size, larger than the rest of the animal, smooth, but with the segments distinct ; the sides much expanded and folded inward, forming a kind of pouch for the reception of the eggs. Color a dark blue-gray, or "neutral tint." Length of the carapax, 0.21 ; breadth, 0.165 inch. Found clinging to the branches of living madrepores, at the depth of one fathom, in the harbor of Hilo, Hawaii, March, 1856. They probably feed upon the coral-polypes. The Corresponding Secretary read the following let- ters, which had been recently received, viz : — From the Smithsonian Institution, June 23 ; the Royal So- ciety of London, March 13 ; the Lyceum of Natural History of New York, Februaiy 11, acknowledging the receipt of the So- ciety's publications ; from Charles Loosey, New York, August 19 ; the Royal Geographical Society, April 20, presenting vari- ous publications ; from William Sharswood, Philadelphia, accom- panying descriptions of insects; the same, August 26, proposing an exchange of publications with the Entomologischer Vei-ein zu Stettin ; the Societe du Museum d'Histoire Naturelle de Stras- bourg, March 1, 1857, proposing an exchange of publications. Joseph Hyrtl, of Vienna, was elected an Honorary Member of the Society. W. G. Binney, of Burlington, N. J., and E. S. Morse, of Portland, Me., were elected Corresponding Members. Dr. Richard H. Wheatland, of Salem, was chosen a Resident Member. 414 November 3, 1858. The President in the Chair. Dr. C. F. Winslow read a paper on certain facts bear- ing upon the coincident origin of the inhabitants of the Society and Sandwich islands ; it related principally to the custom of burying the placenta deep in the ground as near as possible to the spot where a child is born, with the idea of securing for the child a perpetual inheri- tance in the earth, an indisputable right to the soil, and an equality with other men. He had traced this custom in both the above groups of islands, far removed from each other, and thought it would be interesting to trace it, if possible, among the Malays, from whom the Poly- nesians are generally supposed to have originated. Mr. T. T. Bouve exhibited a thin, white, paper-like substance, found stretched over a quantity of meal con- tained in a box, in which a large number of grubs were concealed. Prof. Agassiz made some remarks on a catalogue of the fishes of Jamaica, by the Hon. Richard Hill, of Kingston. He regarded it as interesting for purposes of comparison with the species of North America and Europe. It is well known that the fishes of the two sides of the Atlantic are specifically dis- tinct, except a few northern ones, which are identical, not from crossing from one continent to another, but from migrating south- ward on both shores from the same arctic centre. As maps are usually drawn, the average temperature of the water for the year is taken as regulating the geographical distribution of fishes ; but, as Prof. Dana has shown in his report on the Crustacea of the U. S. Exploring Expedition, the average of the greatest cold has a more important influence in this distribution. From the Arctic, 415 Gulf-stream, and African currents, the modification of the zones of temperature in the Atlantic is very striking — for instance, the temperate zone on the American side extends only from Cape Hatteras to Cape Cod, about ten degrees of latitude, while on tlie Eux'opean it extends from the coast of Sweden to the Cape de Vei*d Islands, nearly five times as many degrees — on the contrary, the tropical zone, which extends in America from Cape Hatteras to 25° S. latitude, or sixty degrees, extends only about twenty de- grees on the African Guinea coast. The line of temperature established by the average of the thirty coldest days in the year, gives the clue to the distribution of the marine fauna ; in America this is essentially tropical, and in Europe essentially temperate. Of the families mentioned in this list, the Cottoids are essen- tially North American, and ther eare five in Jamaica ; the Scice- noids are tropical, Europe having but a few ; the Sparoids are essentially Mediterranean, where fifteen genera exist, and there are four in Jamaica ; the Squammipennce are tropical, and numer- ous in Jamaica ; the Scomberoids are cosmopolitan, and numerous everywhere ; the Mullets are tropical, and there are several in Jamaica ; the Lahroids, very rare here, are numerous in the tro- pics ; the Gyprinoids, though quite cosmopolitan, have never been found in South America, and there are none in Jamaica ; one Gentropomus is found in fresh water in Jamaica, which is unusual ; the Siluroids are few, those of America are few in comparison with those of Asia ; while a kindred family, the Goniodonts, are peculiar to this country ; the Pleuronectidce belong to the tem- perate zone, yet there are few here. J. M. Barnard, Esq., stated a fact in confirmation of the tropi- cal character of the American marine fauna ; he had lately received a keg of echinoderms from Zanzibar, in 5° S. latitude, which were almost identical with those from East Florida. Prof. Parsons stated some facts in regard to the ani- mals of the White Mountains, which he had learned from an experienced hunter, especially in respect to the abundance of the sable and deer. Prof. Agassiz remarked that the fauna of the Adiron- dac Mountains, 1500 feet above the sea, is essentially that of the fur countries. 416 The Treasurer announced that the entomological col- lection of the late Dr. Harris had been delivered to the Society, and that the money had been paid to Mrs. Har- ris. The Society for the Promotion of Agriculture, which had subscribed liberally, were very anxious that Dr. Harris's Report to the Legislature, now out of print, should be reprinted. On motion of Prof. Parsons, a committee of five was appointed to inquire into the best means of republishing the work, if possible with illus- trations ; the committee consisted of Prof. Parsons, J. M. Barnard, Dr. A. A. Gould, and Messrs. Agassiz and Charles Hale. Mr. Alexander Agassiz gave an account of the con- dition of the collection, which is for the most part in good order. The committee to whom was referred the letter of Dr. I. I. Hayes, announcing his intention of making another attempt to reach the north pole of the earth, reported as follows : — The Committee to whom was referred the letter of Dr. I. I. Hayes, announcing his intention of making another attempt to reach the north pole of the earth, would report :- — 1. That we regard the proposed expedition with no ordinary interest ; and receive assurance that it will be successfully prose- cuted, in view of the near approaches which have already been made in that direction ; — the reasons by wJiich it is shown that the obstacles hitherto encountered may be in a great measure evaded ; — the personal experiences of its conductor of the dan- gers and rigors to be met, and his ability to forestall them ; — and especially in his acquaintance with the residences and character of the natives on whom he must mainly rely for extra aid — an acquaintance probably superior to that of any other person. 2. That while the hopes of former expeditions may not liave been fully reaHzed, yet that in view of the additions made to hu- man knowledge as to the meteorology, geography, and other natu- ral features of our globe, as well as the proofs they have given of 417 the physical endurance, perseverance, and moral energies of our race ; enough has been attained to entitle tliem to be considered as any thing but unsuccessful ; and that we anticipate similar results from this, results in no way inferior to those attaching to previous expeditions. 3. That whatever of encouragement and countenance can be derived from this Society, we wish to tender to Dr. Hayes ; assuring him that our best wishes will accompany him — and of our confidence that his return will be fraught with fruits most valuable to science. All which is respectfully submitted. Augustus A. Gould, ") Samuel Kneeland, Jr. V- Committee. Theophilus Parsons. ) The Report and accompanying Resolutions were accepted and adopted as the sense of the Society, and the Corresponding Secretary was directed to communi- cate a copy of the same to Dr. Hayes. Messrs. William B. Gibson, and Albert Ordway, of Boston, were elected Resident Members. November 17, 1858. Dr. C. T. Jackson, Vice-President, in the Chair. Prof. Parsons, from the committee appointed at the last meeting to inquire into the best method of securing the reprinting of Dr. Harris's work on insects, made a report recommending immediate action in preparing a memorial to the Legislature, concurrently, if necessary, with other Societies. On his motion it was voted that a committee be appointed with full powers to take the steps necessary to procure a new edition. The subject was referred to the same committee by the Chair. PROCEEDINGS B. S, N. H. VOL. VI. 27 FEBRUARY, 1859. 418 Dr. Kneeland read a paper on the North American fur- bearing animals of the genus Mustela, exhibiting in illus- tration a skeleton and skins obtained by him at Lake Superior in the winter of 1856-7, and presenting and describing a skeleton of the fisher, Mustela Canadensis, Schreber. These animals, called martens, to distinguish them from the mink and weasels (of the genus Putorius), are two, the fisher or Pennant's marten, and the pine marten, or American sable — the mink is often erroneously called American sable by hunters and furriers. The length of the skeleton to end of tail was 33 inches, tail 13 inches, skull 4 inches, lower jaw 2^ inches — the dorsals are 14, lumbar 6, sacral 3, and caudal vertebra3 20 ; ribs 14 pairs, of which 10 appear to be true. The pine marten {Mustela Americana, Turton) is much more rare, and more valuable for its fur. A specimen of the rare plant, Sullivantia Ohionis, Torr. & Gray, was presented in the name of Mr. I. A. Lapham, of Milwaukee, found by him on wet sandstone cliffs at the dells of the Wisconsin river, where the La Crosse and Milwaukee railroad crosses. As far as he knew, this species had only been found previously on calcareous cliffs in Ohio by its discoverer, Mr. William S. Sullivant. Mr. Theodore Lyman exhibited specimens and en- larged drawings of the animal of Syndepas Gouldii, showing that this coral is different from the Caryophijllia solitaria, Lesueur. Dr, Borland exhibited two specimens of aggregated crystals of ferruginous quartz, from Valentia, Spain. Prof. Agassiz remarked tliat of the European species of Salmo, the S. salar, Linn., is found on both sides of the Atlantic ; while the S. eryox, Linn., called S. hamatus by Cuvier, remarkable for the hook in the lower jaw of the male, and differing from the 419 other in color and shape, has been hitherto considered as confined to Europe. But on the 29th of October a fish of the latter spe- cies was caught in the Merrimac River, and examined by him — another example of Arctic species coming down on the American as well as the European coast. In the family of Salmonida^, Cuvier unites the abdominal fishes with an adipose fin, and a peculiar structure of the upper jaw — the maxillary and intermaxillary forming a continuous arch. J. Mliller has more recently pointed out structural differences in this family. In those Salmonida3 having no pseudobranchia, he found some with complicated anterior vertebra;, and such he called Characini — others, with the maxillary and intermaxillary bones united side to side into an immovable arch, he called Sco- pelini. The true salmons belong entirely to Arctic and cold regions — the Characini are tropical and fresh-water species of America and Africa, being absent from Asia and Australia — the Scopelini are marine, and of the temperate and warm regions. The dentition of Characini is peculiar, varying much in different members of the family ; in a new genus Analcestis, Ag., from Rio Remak, Peru, resembling Chalceus, Cuv., there are no canines behind the multicuspidate grinders. He had ascertained by direct compai-ison that the species of different basins are dif- ferent, though belonging to the same genus ; many species con- sidered identical by Valenciennes will no doubt prove to be dis- tinct. The Chai'acini are now known to extend beyond South America into Texas and Cuba, and they are probably numerous in Central America. In the course of a discussion on the so-called migrations of fishes. Prof. Agassiz referred to the well-known return of the salmon to the rivers where they were born — and said that what has been called migration, as in the case of the shad, is only the successive arrival of diffei'ent individuals, (as the whole number is going northward to spawn,) in different latitudes and in different months, later according to the increase of latitude. Upon this subject very little is known ; but it is certain that fish do not always approach the shore to get into warmer water ; they may perhaps do so to be relieved from the pi-essure of great depths. Dr. Brewer observed that the European Widgeon, occasionally 420 seen in this country, had been found on Long Island, apparently breeding — also that the European Saxicola is found breeding in Labrador ; this had been called S. cenanthoides by Mr. Cassin, who considered it a different bird from S. cenanthe, Linn. Two small bones exhibited to the Society were pronounced by Prof. Agassiz to belong to the anterior portion of the anal fin of some GhcBtodon, pi-obably of the genus Platax. Dr. Green tendered the resignation of his office of Curator of Comparative Anatomy, which was accepted, and Messrs. Whittemore, Lyman, and Kneeland were appointed a committee to nominate a candidate to suc- ceed him. Messrs. Francis H. Brown, and Jacob Burckhardt, of Cambridge, were chosen Resident Members. December 1, 1858. Dr. C. T. Jackson, Vice-President, in the Chair. Dr. C. F. Winslow read a paper on " Comets and the curvature of their tails," in which he discarded the ma- terial theories heretofore entertained respecting the con- stitution of the tails of these bodies, and set forth a theory of luminous waves generated by the nucleus, which are arrested, decomposed, and swept back into space by the rays of light projected from the sun. Prof. Parsons read a memorial to be presented at the next session of the Legislature by the Boston Society of Natural History, the Massachusetts Historical Society, the Massachusetts Society for promoting Agriculture, and the American Academy of Arts and Sciences, re- questing the republication of Dr. T. W. Harris's work on the " Insects injurious to Vegetation," with illustrations. 421 The memorial was adopted, and, on motion of Prof. Parsons, committees were appointed to confer with those Societies : Prof. Parsons and Dr. Gould to confer with the Academy, and Messrs. Barnard and Binney with the other Societies. Mr. T. T. Bouve announced the donation of a valuable collection of the bones of Zeuglodon cetoides from C. S. Hale, Esq., of Burlington, New Jersey, and read the cor- respondence between the donor and himself on the sub- ject. With regard to this species he made the following statement : — In 1832, Dr. Harlan, of Philadelphia, first described a verte- bra of a supposed gigantic fossil saurian, for which he established the genus Basilosaurus. In 1835, Prof. Agassiz described a tooth of this animal, at the University of Cambridge, England, as belonging to a genus allied to the seal family, which he named Phocodon. In 18-40, M. Grateloup, from the examination of a fragment of the jaw containing teeth, at first uncertain whether to refer it to a cetacean or a saurian, finally placed it among amphibia, in a genus which he called Squalodon. In 1839, Prof. Owen, satisfied that the animal was a cetacean, proposed for it the name of Zeuglodon cetoides. In 1843, a great part of a skeleton, found in Alabama, was described in the American Jour- nal of Science. Soon after this the Hydrarchos Sillimani of Dr. Koch was exhibited, in a series of bones measuring 114 feet; this Prof. J. Wyman discovered to be made up of several indi- viduals, and the so-called head to be composed of bones some of which were not in their natural position. In 1845, Dr. R. W. Gibbes described, in the Proceedings of the Academy of Natural Sciences, some teeth which he referred to a new genus Dorudon, from the shape of the teeth ; he subsequently gave up this genus and referred his specimen to the Zeuglodon, making, how- ever, a new species, Z. serratus ; he also ascertained the identity of the genus Squalodon with Zeuglodon. He thinks that the original genus Basilosaurus should be restored, with the following species : B. cetoides, Owen ; B. serratus, Gibbes ; B. squalodon, Grateloup. 422 This collection consists of 36 vertebrae, and 26 fragments of ribs and other bones. Zeuglodon remains are found in abun- dance in the eocene deposits of Alabama ; they have also been found in Georgia and Louisiana. On motion of Dr. Gould, a committee was appointed to express to Mr. Hale the feelings of the Society for this valuable donation, which included also at some future time his entire cabinet of Natural History — Mr. Bouv^, Dr. Gould, and Prof. Agassiz were appointed the com- mittee. Dr. A. A. Gould presented the following descriptions of Shells collected in the North Pacific Exploring Expe- dition under Captains Ringgold and Rodgers : — SucciNEA LAUTA. Testa magna, tenuis, plerumque S. obli- qu£e similis, sed postice tumidior, ad apicem minus acuta. Long. Yjj ; lat. y^g- poll. On shrubbery at Hakodadi (I si. Jesso). A very large, thin shell, most like S. obliqua, Say. ViTRiNA iMPERATOR. T. niagnifica, fragilis, ventricosa, epi- dermide rigida fuscescente induta, obsolete spiraliter striata ; anfr. 3+. Apertura ampla subcircularis, ad columellam vix incras- sata. Axis f ; diam. 1^ poll. Inhabits Hong Kong in ravines near summits of hills. By far the largest species yet described ; approximates closely to H. ampulla, Bens. Helix l.eta. Testa tenuis, lucida, subglobosa, viridi-cornea, vitta rufa ad peripheriara et altera prope suturam ornata ; anfr. 5 ventricosis, striis volventibus tenuissimis. Apertura magna, sub- circularis, peristomate modico, e verso, ad umbilicum magis reflexo. Axis 1 ; diam. 1^ poll. Inhabits Hakodadi on bushes and shrubs. General outline not unlike If. pomatia. Helix labilis. T. parva, tenuis, nitida, succinea, depressa, lenticularis ; ad peripheriam acuta ; subtus convexa, polita, arete umbilicata ; anfr. 5 convexiusculis. Apertura transversa, anguste lunaris, columella verticalis. Axis y^j ; diam. ^ poll. 423 Inhabits HakocTadi, among dead leaves, in woods. Very nearly allied to H. miselld. Helix pdpula. T. minuta, ovato-conica, levis, succinea, infra convexa, indentata ; anfr. 6-|- tabulatis, ad peripheriam ob- tuse angulatis. Apertura transversa, lunata ; labro siraplici, colu- mella recta, reflexa. Axis ad ^ poll. Among dead leaves in woods, Hakodadi (Isl. Jesso). Very much like our chersina, or the European y'HZt'a. Helix pauper. T. parva, discoidea, rufo-cornea, striis in- crementi costulata, subtus calyculata ; anfr. 4^ convexiusculis ; sutura profunda. Apei'tura perobliqua, prona, rotundata ; peris- tomate simplici. Diam. y^g- ; axis -^ poll. On dead wood in thick- ets, Petropaulski, Kamtschatka, also Hakodadi (Isl. Jesso). Allied to ff. rotundata and perspectiva. Probably the same noted by Middendorff' as H. ruderata of Europe. Helix operculina. Testa tenuis, depressissima, rufo-cornea ; anfr. 5 concavo-convexis, ad peripheriam acutissime carinatis, marginatis ; subtus concava deinde convexa. Apertura angustis- sima, sigmoidea, peristomate vix reflexo. Axis -^^ ; diam. -/(j poll. Inhabits Peel Isl. (Bonin Is.) Mr. Wright. An exceedingly depressed species, looking much like the oper- cle of some Trochus. Helix squarrosa. Testa planorboidea, squarrosa, ochra- ceo-cornea, subtus pallidior, convexa, late umbilicata; anfr. 6 con- vexiusculis, ad peripheriam subangulatis. Apertura parva, an- gusta, lunata ; peristomate simplici, ad columellam reflexo. Diam. -^^ ; axis -^^ poll, (probably immature.) Ousima (Japan), among stones on hill sides. Well distinguished by its large deep umbilicus, ochreous color, and rough, scaly surface. Allied to Shanghaiensis. Nanina pisolina. Testa fragilis, vitrea, levis, raellita, orbi- cularis, subtus convexior, imperforata ; anfr. 3^ depressis, ad peripheriam rotundatis. Apertura lunata, labro ubique simplici. • Diam. \ ; axis ^ poll. Cape of Good Hope (?) 424 A small globular species unlike any one I have found de- scribed. Sub-gen. Gorilla, H. & A. Adams (eraendatus). Testa pla- norboidea, plerumque sinistrorsa, plus minusve distorta, arete spi- rata, subtus concava ; fauce in fundo denticulis compressis fere occluso, quorum uno sa^pe ad aperturam producto ; peristomate incrassato, refiexo. C. PULViNAUis. T. utrinque concava, cornea, striis incrementi conspicuis insculpta ; anfr. ad 7 (subtus 5) ultimo demum deflecto. Apertura lunata admodum campanulata, peristomate flexuoso, satis reflexo ; denticulis in fauce ad 9, baud productis. Diam. f ; axis ^ poll. Hong Kong, high up in the ravines ; also near Canton. Almost precisely of the size and shape of H. refiiga, Gould, but that is reversed and has a lamina running to the aperture. Stkeptaxis Sinensis. Testa obliqua, polita, virescens, spira depressa, ovoidea, anfr. 7 acutis, sutura profunda minute crenu- lata. Apertura obliqua, semi-ovalis, verticalis, lamella unica pala- tal! munita ; peristomate Hexuoso, reflexo ; columella recta ; um- bilico amplo. Axis ^-^ ; diam. ^ poll. Inhabits Hong Kong. Differs from S. Souleyetana in its smaller size, smooth surface, fiexuous lip, and more elongated aperture. Clausilia pr.eclara. Testa sinistrorsa, clavato-fusiformis ad apicem producta, dilute carnea, liris conspicuis clathrata ; anfr. 11 ultimo angustato, trientem long, testte adequante. Apertura pyriformis, antice sub-canaliculata ; peritremate albo satis reflexo ad anfr. ultimum baud coadnato ; lamina palatali elevata, tenui, 1. columellari conspicua, duplici, contorta, lamellis 4 tenuibus ad interspatium, extus apparentibus. Axis 1 ; diam. max. ^ poll. Inhabits Loochoo. Allied to valida, insignis, &c., but most like pluviatilis on account of its aperture. Alyc^us pilula. Testa parva, ovato-conica, imperforata, rufescens, striis numerosis (sub lente) cincta ; anfr. 4 rotundatis, ultimo constricto ; sutura profunda. Apertura circularis, anfrac- 425 turn proximum vix attigens ; faure valde contracto ; peristomate modice reflexo ; fistula suturali exili valde appressa. Operculum corneum, arete spirals, apice centrali. Axis ^ ; diam. ^ poll. Inhabits Ilong Kong, China. Cyclotus illotus. T. planorboidea, rudis, rubiginosa, sub- tus late et profunde umbilicata ; anfr. 4 rotundatis, sutura sim- plici, impressa. Apertura circularis, anfractum proximum haud amplectens ; labro simplici. Diam. 3 ; axis 1 poll. Inhabits Loochoo. In form and general aspect greatly resembling Cycl. suturalis, Sowb., but is smaller, and has a simple suture. Cyclostoma bakbata. T. parva, ovato-conica, rufo-cornea, liris numerosis volventibus et striis incrementi tenuibus lamellosis decussata, decussationibus barbara gerentibus ; anfr. 5 rotun- datis, sutura canaliculata. Apertura postice subangulata ; peris- tomate simplici, vix expanso ; umbilico modico, profundo. Diameters ^ inch. Inhabits Ousima. Two of the ridges on the outer whorl and one on the others are more conspicuous than the rest. Cyclostoma citharella. T. parva, subglobosa, tenuis, rufa, laminis incrementi tenuibus ornata, ad peripheriam prope aperturam biangulata, satis umbilicata. Apertura circularis, peristomate simplici anfractum proximum tantum attigente. Operculum subrotundum, paucespiratum, margine attenuate. Diameters -^ inch. Inhabits Ousima. Were it not for the operculum, it might be mistaken for Helix harpa, Say. Cyclostoma musiva. T. ovato-conica, cornea, radiatim rufo strigata, subtus ad peripheriam rufo tessellata, modice umbilicata, striis volventibus ad 5 arata, lineis incrementi conspicuis decus- sata ; anfr. 5 rotundatis, sutura canaliculata. Apertura rotun- data, peristomate simplici. Axis ^- ; diam. ^ inch. Inhabits — ? (probably Japan). The surface is conspicuously and beautifully relieved by the decussating lines. 426 The preceding three species form a peculiar group near to Cyclostoma proper, characterized by the thin paucispiral opercle with thinned edges, the globose conic form, free umbilicus, nearly circular peristome which barely touches the preceding Avliorl, and the projecting lamellar striai of growth decussating with revolv- ing ridges in some cases furnished with epidermal barbs. It may be called Japonia. Helicina verecunda. T. pyraraidato-lenticularis, spiraliter minutissime striata, luteo-virens ad apicem rubescens, ad peri- pheriam subangulata, subtus convexa, admodum callosa ; anfr. 4 planulatis. Apertura ovato-triangularis ; peristomate evaso, albido, ad columellam rectam angulariter juncto. Axis ^ ; diam. ^ inch. Inhabits Loo Choo. Belongs to the group of which H. striatida is a type. Mr. A. E. Agassiz made the following communication on the mechanism of the flight of lepidoptera : — The nervures of the wings of butterflies are so arranged as to give the greatest lightness and strength ; they are hollow, with their greatest diameter at the base of the wing, the point of great- est strain, their diameter gradually diminishing to the edge of the membrane. If a section be made across such a wing, parallel to the axis of the body, we find very much the arrangement which has been experimentally proved by Fairbairn and Stephenson as giving the greatest strength of beams, as exemplified in the tubu- lar bridge — in the insect nervure, as in the strongest beam, we find the most possible material thrown into the flanges, and the upright support as thin as practicable — in the insect wing we have a very thin membrane connecting two flanges, whose section is very great compai-ed to the membrane, with the additional advantage that these flanges are hollow, increasing their strength and diminishing their weight. In all Ave find the strongest ner- vure placed either directly on or near the anterior edge of the upper wing ; there is no such nervure in the lower wing, all being of nearly the same size, as such a one would have prevented the elasticity of the wing from assisting the flight to any considerable extent. The lower wing is always partially covered by the upper ; were this not the case, in the downward beat the resist- ance of the air would cause the lower wing to become separated 427 from the upper, and a current of air would rush through between the wings, and compel the butterfly to employ additional force to keep them together ; as thus arranged, the resistance of the air keeps the Avings together during the downward beat, and their elasticity during the upward. The curve in which any point of the wing moves during one beat is an arc of a hehx, and not an arc of an ellipse as Strauss-Durckheim supposes. The Corresponding Secretary read a letter from Dr. I. I. Hayes, acknowledging the receipt of notice of the So- ciety's action with reference to his proposed Arctic expe- dition, and requesting permission to publish the Report of the committee. It was voted that he be permitted to make such use of the Report as he may think for his advantage. The Corresponding Secretary also read the following letters which he had recently received, viz : — From the Smithsonian Institution, February 20 and May 19, 1858, acknowledging the receipt of publications of this Society ; from the Real Academia de Ciencias de Madrid, August 1, 1857, presenting its Memoirs, 3d Series, tomo 2% parte 2^^ ; Wilham Sharswood, Philadelphia, Nov. 11, concerning the proposed pub- lication of the descriptions of certain insects, «&;c. ; M. Auguste Le Jolis, Cherbourg, France, Nov. 15, 1858, in acknowledgment of his election as Corresponding Member ; Stephen P. Leeds, Rutherfordton, N. C, Oct. 28, and William G. Binney, Burling- ton, N. J., Nov. 17, also acknowledging their election. The committee to whom was referred the nomination of a candidate for Curator of Comparative Anatomy, reported the name of Dr. James C. White, of Boston — and he was chosen. A vote of thanks was passed to Mr. Daniel F. Hicks, of Wabashaw, Minn., for the donation of a sharp-tailed grouse, Tctrao ])hasianeUus, Linn. Hon. Richard Hill, of Kingston, Jamaica, was chosen a Corresponding Member; and Mr. Nathan Farrand, of Boston, a Resident Member. 428 December 15, 1858. Dr. D. H. Storer, Vice-President, in the Chair. Dr. James C. White exhibited specimens and figures of Stephanurus dentatus, Diesing, Sclerostomum denta- tum ? Rudolphi. These worms were found in the leaf-lard of an apparently healthy hog, in the adipose tissue near the kidney. They occu- pied a portion of the same about the size of a man's fist, and had burrowed through the mass in every direction, forming canals three or four millimetres (^ to ^ of an inch) in diameter, which terminated in cysts. On cutting open these cavities, which did not communicate with each other, they were found filled with pus, and in each were two worms, male and female. The female is nearly double the male in size, and bent upon herself so that the two extremities meet. The head and tail of both sexes are red, and the bodies are a pale yellow, mottled with black. The females, being filled with eggs, were darker. They are oviparous, and the eggs were found in all stages of segmentation. They belong undoubtedly to the nematoidea, and, so far as can be ascertained from the scanty descriptions given, to the above- named species. Whether the embryo inhabits another part or not is not ascertained, for the mature worm only is known, and mentioned as found in the liver of the hog. They were situated along the course of a large blood-vessel, and no doubt gained their situation by boring through the circulatory system while in the embryonic candition. Dr. Kneeland read the following communication on the breathing apparatus of the Menobranchus, showing the relative value of the branchial, pulmonary, and cuta- neous respirations : — In June last he put two of these reptiles into an aquarium with half a dozen minnows, varying in size from two to three inches. The fish were frequently seen nibbling at the expanded gills of the reptiles, which as often suddenly started from their ordinary 420 state of repose, attempting to seize the fish, which they never succeeded in doing. In about ten days the menobranchs had nothing left of the gills but the almost bare cartilaginous sup- ports, with only here and there a branchial fringe. The fish were then taken out, and the branchial fringes began to grow again, and in the course of six months had regained about half their normal size. He had watched these reptiles for two sum- mers, and no similar falling of the gills ever took place, so that it appears in the present instance that the fish actually eat them off, their loss being a pathological and not a natural phenomenon — in either case this fact seems interesting in a physiological point of view, as bearing upon the respiratory organs of these reptiles. He had ascertained (see page 153 of this volume) experimentally that they survive out of water about four hours, showing that their pulmonary sacs, or lungs, are not alone sufficient for the maintenance of respiration. In the present instance, though their pulmonary sacs were the principal respiratory organs, the animals did not apparently suffer. These lungs are two, one on each side, cylindrical, with thin transpai'ent walls like the air-bladder of fishes, with vessels ramifying through their thickness ; they open anteriorly by a common trachea into the oesophagus, and are about two inches long and one sixth of an inch in diameter. According to Dr. Gibbes, the branchiae are supplied with blood by the branchial artery coming directly from the ventricle, while no branch of this artery runs to the lungs, which are supplied from the aorta. These animals, even when their bi-anchia3 are in full play, occasionally come to the surface and swallow air, which they emit in the water with a faint squeak, by means of the vol- untary muscles with which the lungs are supplied. The question arises, why are these lungs apparently sufficient for respiration in the water, and not in the air, though the respired element be in both cases the same ? As there is no evidence of internal gills, the reason must be, that in the air, while the branchial tufts, from dryness are unfit for circulating the blood, the complementary respiration of the skin, so importiint in rep- tiles, cannot be carried on — the pulmonary sacs alone are in- sufficient for the aeration of the blood, and the animal dies. In the water, however, though the branchiae, as in this case, be useless, the cutaneous respiration is unimpeded, and with the pulmonary 430 is sufficient for the purification of the blood. This fact shows the importance of the cutaneous respiration and the insufficiency of the puhnonary, and that these reptiles cannot be considered truly amphibious, though probably approaching as near to this con- dition as any animals. Specimens of Pomotis and Esox, and of amphibians, were presented by Mr. H. D. Thoreau, from Concord, Mass. Mr. Putnam was of opinion that one of the Po- motis would prove a new species. There are with us two varieties of Esox, commonly known as the long or shovel-nosed pickerel, and the short or trout-nosed, to the last of which the specimens belonged. Mr. Putnam was inclined to think these were distinct species, unless the differences should prove to be sexual. Drs. D. H. and H. R. Storer considered them varieties of the same spe- cies ; Messrs. Baird and Girard think them distinct. Dr. Bryant made some remarks on the habits of two fly- catchers, Muscicapa acadica and M. JiaviveJitris ; the former is represented by writers on ornithology as exceedingly wild, and as inhabiting the most solitary places ; he had found it, on the con- trary, generally quite familiar, breeding near his house, at Co- hasset, Mass., and becoming so tame as to fly up to his hand to receive a moth. He also mentioned that he had seen last June two males of the white-crowned sparrow, a rare bird here even in winter. Mr. A. E. Agassiz exhibited colored drawings of the Salmo eri/ox, Linn., recently taken in the Merrimac River. DONATIONS TO THE MUSEUM. October 6, 1858. Bones of the head and scapular arch of Boras, from Buenos Ayres; and coleoptera from Lunenburg, Mass.; by T. J. Whittemore. Skull and skin of a new species of Antelope from South Africa; by Thomas Nelson. A piece of impure ambergris from St. Domingo; by Capt. E. H. Russell. October 20. Several European reptiles, as follows: Laceria viridis, L. agilis, 431 Zuoloca vivipara, Vipera berus, Tropidonolus natrix (2 varieties, one young in shell), Anguis frayilis, Bufo calnmita, B. viricHs, B. vnlf/aris, Rnna escidcnia, R. temporaria, Bombinator igneus, Triton cristatus, T. ir/neus, Pelobates fusais, Saln- mandra maculosa, and Hifla arborea; by Dr. D. F. Weinland. A pigeon-hawk, n. coluinbarius, L. ; by Samuel Rodman. Three new genera of Fishes; by Pro!'. Agassiz. Novembers. Shells from Mohawk, N. Y.; by Mr. Lewis. A gold and a sil- ver pheasant; by Dr. Charles G. Greene. A crawfish from the Mississippi River; by Dr. S. Kneeland, Jr. A large collection of Zeuglodon bones; by C. S. Hale. November 17. Skeleton of the fisher marten, Mustela Canadensis, Schreb. from Lake Superior; by Dr. S. Kneeland, Jr. Specimen of SuUivantia Ohionis, Torr. & Gray, from the dells of the Wisconsin River; by L A. Lapham. Specimens of Melania, and of calamine, from Mossy Creek, Tennessee; by Dr. C. T. Jackson. December 1. Sharp-tailed grouse, Tetrao phasianeUus, L. from Minnesota; by Daniel F. Hicks. A specimen of Brazilian cotton ; by W. H. Dennett. December 15. Specimens of young Fomotis, Esox, and frogs, from Concoivl, Mass. ; by H. D. Thoreau. Skull of young grisly bear and of a large beaver, from California; by E. S. Holden. Skull of young black bear from Lake Supe- rior; by Dr. S. Kneeland, Jr. BOOKS RECEIVED DURING THE QUARTER ENDING DEC. 31, 1858. Formation of Rotating Rings by Air and Liquids. By Prof. Wm. B. Rogers. 8vo. Pamph. From the Author. Remarks on certain Species of North American Helicidffi, with descriptions of new species. By Thomas Bland, F. G. S. 8vo. Pamph. New York, 1858. From the Author. Report of Exploration of the country between Lake Superior and Red River Settlement. 8vo. Pamph. Toronto, 1858. From Capt. Latour. Review of Marcou's Geology of North America. By J. D. Dana. 8vo. Pamph. From the Autlior. Phycologia Australica, or a History of Australian Seaweeds. By W. H. Har- vey, F. L. S. Nos. 1, 2, 3. 8vo. London. From the Author. Hints to Craniographers. By J. A. Meigs, M. D. 8vo. Pamph. Phil. 1858. From the Author. Catalogue of Birds in the Museum of the East India Company. Vol. 2. 8vo. London, 1856-58. Catalogue of Lepidopterous Insects in the Museum of the East India Com- pany. Vol. 1. 8vo. London, 1857. From the Birecioi-s of the East India Com- pany. Nereis Boreali Americana. By Wm. H. Harvey, M. D., &c. Part 3d. 4to. Washington, 1858. Annual Report of Regents of the Smithsonian Institution. 8vo. Washington, 1858. From Smithsonian Institution. Proceedings of the Academy of Natural Sciences of Philadelphia. Vol. X. Sigs. 10, 11, 12. 1858. 432 Memorias de la Real Academia de Ciencias de Madrid. Tomo 4. 5° serie — Ciencias Naturales. Tomo 2o. Parte 2. 1vol. 8vo. Madrid, 1867. Canadian Naturalist and Geologist. Vol. 3. No. 5. October, 1858. 8vo. Pamph. Montreal. New York Journal of Medicine. Vol. 5. No. 3. November, 1858. Receueil des Actes de I'Acad^mie Imperiale des Sciences, &c., de Bordeaux, igieme nnnde, 1857, 3e et 4<= Trimestre, et 20'«n'e ann^e, 1858, 1" Trimestre. 8vo. Bordeaux, 1858. Jahrbucli der K. K. Geologischen Reichsanstalt. 1857. VIII Jahrgang. N™ 4. October, November, December. 8vo. Wien, 1858. Silliman's Journal of Science and Ai'ts. Vol. XXVI. No. 78, for Novem- ber, 1858. Journal of the Royal Dublin Society. Vol.1. 8vo. 1858. Proceedings of the Royal Geographical Society of London. Vol. II. Nos. 3, 4, 5. 8vo. London, 1858. Berichte der Oberhessischen Gesellschaft fur Natur-und Heilkunde. 3 Nos. May 1854, October 1855, June 1857. 8vo. M(5moires de la Soci^t^ Royale des Sciences de Li^ge. Tomes XL and XIII. 8vo. Lic^'ge, 1858. Annales de la Society Linn^enne de Lyon. Tomes III. IV. 8vo. La'Oii, 1856-7. Natural History Review. Vol. V. No. 3. July, 1858. 8vo. London. Memorie della Reale Accademia delle Scienze. Vols. I. 11. 4to. Napoli, 1857. Continuazione del Rendiconto della Reale Accademia delle Scienze. Anno V. et VI. Napoli. Wiirtembergische Naturwissenschaftliche Jahreshefte. Vierzehnter Jahrgang. Zweites und drittes Heft. 8vo. Stuttgart, 1858. Neue Formen von Infusorien. Von L. K. Schraarda. 4to. Pamph. Wien, 1849. Nachrichten von der Georg-Augiists-Universitat und der K. Gesellschaft der Wissenschaften zu Gottingen. 1857. 12mo. Annales des Sciences Physiques, &c., de Lyon. 2'fni« Serie, Tome VIII. 3ieme Serie, Tome 1. 8vo. Lyon. Canadian Journal of Industry, Science, and Art. No. 18. November, 1858. 8vo. Toronto. Proceedings of the American Antiquarian Society. 8vo. Pamph. Boston, 1858. Received in Exchaiiffe. Annals and Magazine of Natural History. Vol. 11. No. 9, for September; No. 10, for October; No. 11, for November; No. 12, for December. 3d Series. Lon- don, 1858. Fossils of South Carolina. By Profs. M. Tuoraey and F. S. Holmes. 4to. Charleston, S. C. 1856. Quarterly Journal of the Geological Society. Vol. XIV. No. 56, part 4. No- vember, 1858. 8vo. London. Mammals of Australia. By J. Gould, F. R. S. Parts 3, 4. Folio. London. Monograph of Trochilidse, or Humming Birds. By J. Gould, F. R. S. Parts 4, 5, 6. Folio. London. Birds of Asia. By J. Gould, F. R. S. Parts 3, 4. Folio. London, 1851-3. From the Courtis Fund. INDEX TO VOL. VI. N. B. New genera and species are in italics. AcADEMYjChicago, of Natural Sciences, 154. Acantheus Americaniis, Embrj^ology of, 37. Acantlwtrias, nov. gen. Weinland, 300. Acarus of potato, 9. Acrocladia mammillatfl, 384. Africa, Native iron from, 279. African bulb, 127 ; gum, Analj-sis of, 129. Agalmatolite, Analysis of, 32. Agassi z's. Prof, notice of Johannes Miil- ler, 382. Agelaius gubemator. Egg of, 149. Alabama, Peculiarities of Helix thyroi- dus in, 129. Alasmodonta arcuata, cause of erosion of, Discussion on, 258. Albino rats from Medford, Mass., 301. Albino Sciurus striatus, 218. Alca torda, 123. Alcoholic bevei-ages and their falsifica- tions. Dr. A. A. Hayes on, 352. Alewife, Larvce of ttenia in, 25. Alga; from Australia, Ceylon and Friend- ly Islands, 286; from California, 170. Algeria, races of, M. Bodiclion on, 383. Alternation of generation in Treraatoda of Freshwater Snails, 24. Alum Stone from Texas, Maryland, Analysis of, 245. Aluminium, 139, 159. Alycseus 2)ilula, Gould, 425. Amaranthus pumilus, 66. American Fossils, Oldest, 310. American Helices, Monograph on, 155. American works on Natural History in Europe, 404. Ammodromus Samuelis, Baird, 379. Anableps Gronovii, development of, as compared with that of Embiotoca, Prof. J. Wyman on, 294. Analysis of Agalmatolite, 32 ; of Alum Stone from Texas, Maryland, 245; Deep River coal, 31 ; Black-band iron ore, 32 ; Dolomite from Texas, Mary- land, 244; Gum from Africa, 129; In- fusorial earth, containing copper, by Albert Gould, 310; Magnetite from Iron Mountain and Pilot Knob, Mis- souri, by Edwin Harrison, 295; Ridge- way Carbonate of iron, 18; Ridge- way Coal, 17; Ridgeway Limestone, 18 { Scales of Striped Bass, 374 ; Som- erville Slate, 108; Supposed Meteoric Stone from Marblehead, Mass., by C. T. Jackson, 294. Anas obscura, 119. Animal Kingdom, Series in, 112. Animals, Psychological view of their motions, bv David Weinland, 160. Annual Meeting, May 6, 1857, 191. May 5, 1858, 370. Aphis ( Pemphigus) siamineus^Hald., 403. Aquarium, 365. Arachnides, Reproduction of, 285. Arctic Expedition, proposed by Dr. I. I. Hayes, Action of Society on, 396; Report on, 416; Vote on, 427. Ardea nycticorax at Hingham, Mass. 20. Artotrogus asterophora, 292. Ascaris lumbricoides, 177. Aspredo, Manner of gestation of, 269; Aspredo levis, peculiar method of hatching its eggs, 328. Assessment, Ainuial, Report on, 230. Astacus Klamath ensis, Stimpson, 87. niyrescem, " 87. Trowbi'idgii, " 87. Astraea decactis, Lyman, 261. Athene cunicularia, N. H. Bishop on, 204. Atlantic slope of Middle and Southern States, Classification of Metamorphic Strata of, 140. Atlantic and N. Pacific shells identical, 124. Atlas not united to Odontoid Process, 309. Australia and California, sands of, Re- mark on, 228. Australia, Pigeon from, 169. Bagre, see Aspredo levis; Manner of hatching its eggs, 268. 424 Bailey, Prof. J. W., Decease of, 173; Bninnioh's Guillemot, Breeding habits Bequest of, 179; Photograph of, 219; of, 124. Report on bequest of, 194; Resolution Bulb from Africa, 127, 131. concerning his sons, 200; Resolutions Bulimns /a«^(/,s, Gould, 12. concerning, 174. kjmliis, " 12. Bailey's Universal Indicators, 215. BniT-owing of Echinoderms in Lime- Bark from California, 219, 227. stone, 368. Bairdii Ilesperomys, 182. Burrowing Owl, N. H. Bishop on, 204. Bass, Striped, Analysis of scales of, Bush Ropes from Surinam, Sections of, 374. 290. Batrachians, Morphology of bladder of, Buteo calurus, Egg of, 146 ; insignatus, 58. Egg of, 147 ; montanns, Egg of, 145. Beetle, Parasitic fungus on, 26. Bequest of Prof. J. W. Bailey, 179; Calculi, Urinary, of nearly pure Silica, Resolutions on, 180. from the ox, 213, 284. Beryl, EnoiTnous, at Grafton, N. H., 22. California and Australia, sands of, Re- Biniiey, Dr. Amos, Deposit of Library marks on, 228. witli the Society, 64; Notice of, 89. California Gum, 218, 227; Bark, 219, Binney Library, Catalogue of, 97 ; Reso- 227; Society of Natural History, 154; lutions concerning deposit of, 65. Birds" eggs, 145; New Crustacea from, Birds, change of color in, Cause of, 34; 279. Early appearance of, in 1857, 170; Caliianassa fow^imawn, Stimpson, 86. Forms of, as related to structui-e, 410; Callipepla Californica, 149. Four Series among, 113 ; Protection Calothrix nivea, 229. of, by law, 329; Of Grand Manan and Calurus resplendcns, 170. Yarmouth, N. S., 114; of Keweenaw Canada Flycatcher, Sylvkola pardalina. Point, List of, by Dr. Kneeland, 231; Nest and eggs of, found in Lynn, Mass., of Northeast and Northwest Coast 5. of America, Dr. Henry Bryant on. Cane Sugar in Sorghum saccharatum, 114. 286, 293, 296, 337. Birds' eggs from California, Descriptions Capacity of Cranium of Digger Indian, of, by Dr. T. M. Brewer, 145. 127. Birds' "tracks iu Connecticut River Sand- Capnodium elongatmii on Oranges, 378 ; stone. 111. on White pines, 210. Bitumen in Encrinal Limestone in Wis- Carbonate of Iron, Ridgeway, Analysis cousin, Edward Daniels on, 309. of, 18. Black-masked Ruddy Duck, from Lake Carduelis tristis, 118. Chamijlain, 375. Carpodacus familiaris, 149. Blanding's Cistudo, in Massachusetts, 8. Catalogue of Binney Library, 97. Blind Fish of Mammoth Cave, Anatomy Cayenne Pepper, Ptinus fur in, 404. of, 72. Cecidomya robinim, Hald., 401. Bombycilla Carolinensis, 118. Cecrops on Orthagoriscus mola, 396; C. Bone, "Structure of, in Python, 55. Latreilli on the same, 404. Bony structure of fish scales, 285. Cemetery, Indian, in Hingham, Mass., Borate of Lime, Native, 206. 20. Borneo, Orangs of, 71. Centriscus scolopax, from Province- Books bequeathed by Prof. Bailey, List town, Mass., 178. of, 222. ' Cervus Virginianus, Parasites of, 395; Botanical position of Chinese Sugar Filaria in,395; Distoma and Cysticer- Cane, C. J. Sprague on, 181. cus in, 395. Botany of Sorghum vulgare, C. J. Cercaria, new species iu liver of Phy- Sprague on, 321. sa heterostropha, 24. Brachyurous Crustacean, New form of, Chstura pelasgica, 115. 412." Charadrius melodus, 119; semipalma- Braintree, Mass., Trilobite from, 27, 40; tus, 119. Paradoxides Harlani from, 369. Chelydra serpentina from Winona, Min- Brazos River, Texas, Fossils from, 51; nesota, 382. Fossil Elephant from, 51 ; Mastodon Chemistry of alcoholic beverages and from, 53; Megatherium from, 53. their falsifications. Dr. A. A. Hayes Breeding habits of Uria Brunnichii, 124 ; on, 352. of U. grylle, J25. Chestnut sided Warbler, Sylvkola utei-o- Brick from a Pilgrim Trading-house, cephala, nest and eggs from Lynn, 260. ]\lass., 5, 425 Chicago Acailemv of Natural Sciences, 154. Chimpanzee, Brain of, 375 ; Supernume- rary mohir in, 45. Chinese Sugar Cane, 170; botanical position of, C. J. Spragueon, 181; its Sugar, Dr. A. A. Hayes on, 200. Chinese Yam, raised in Massachusetts, 335. ChioiKBcetes Behrirujianus, Stimpsoa, 84. Chordeiles Virginianus, 115. Chromium, SesquioKide of, New reaction of, under galvanic battery, 409. Cineras on Ortliagoriscus mola, 396; C. vittata on Pennellae, 404. Cistudo Blandingii in Massachusetts, 8. Claspevs of Skates, Function of, 377. Classification of Corals, 373; of Fishes, Prof. Agassiz on, 407; of the Meta- morphic Strata of the Atlantic slope of the Middle and Southern States, H. D. Rogers on, 140. Clausilia pratclara, Gould, 424. vespa, " 13. Clay concretions from Presumpscot K"iver, Me. 132. Clay Stones, 111; Discussion on 132, 137. Climbing power of Earth Worms, 206. Coal basin, Bituminous, of Pennsylvania, 16; Coal formation of Deep River, N. Carolina, 30; Analysis of coal from, 31 ; Age of, 32 ; is it a gas coal, 33. Coal, Ridgeway, Analysis of, 17. Cochituate water, Spongilla in, 267. Cochliolepis parasiticus, Stimpson, 307. Cod, Viviparous 9; Larva of taenia in, 25; Sand-eel and Pipe-fish in abdom- inal cavity of, 176. Cohasset, Mass., Trap dikes of, 23. Colaptes auratus, 119. Color of plumage in birds, Change of, 34. Comets, C. F. Winslow on, 420. Committee on Dr. Hayes's proposed Arc- tic Expedition, 405; Resolutions pro- posed bj', and adopted, 416. Communications, Verbal, by Agassiz, Louis, 6, 9, 37, 47, 56, 63, 364, 376, 382, 385, 407, 411, 414, 418. Alger, Francis, 22. Atwood, Capt. N. E., 71, 175. Bacon, John, 246, 263. Bishop, N. H., 126. Bodichon, M., 383. Bouv^, T. T., 131. Brewer, T. M.. 4, 419. Brown-Sequard, 67. . Bryant, Henry, 169, 170, 431. Cabot, S., Jr.", 375. Daniels, Edward, 309. Durkee, Silas, 228, 381. Gibson,X3apt. W. M., 71. Gould, A. A., 72. Green, John. 66. 342, 346, 362. Hayes, A. A., 30, 131, 136, 167, 227, 293, 352. Hitchcock, C. H., 330. Hitchcock, President, 111. Jackson, C. T., 16, 23, 42. 57, 159, 168, 170, 183, 259,286,296,341. Kneeland, S., Jr., 335, 396. Lvinan, Theodore, 374. Mills, James E , 63, 107. Parsons, Theophilus, 289, 415. Rogers, Henrv D., 108, 378. Rogers, William B., 27, 183, 217, 332, 333. Sprague, C. J., 37, 58, 66, 131, 165, 210,229,282,296, 378. Stodder, Charles, 138, 369, 381. Storer, D. H., 243. Storer, F. H., 259. Weinland, David P., 24, 57, 346,"%64, 1(385. White, .T. C, 290, 291, 428. Wvman, Jeffries, 8, 20, 21, 22, 44, 56, 58, 71, 72, 89, 108, 125, 263, 268, 294, 328, 336, 363, 376, 380, 395. Communications, Written, by Agassiz, A. E., 426. Baird, S. F., 370. Binney, William G., 128, 155. Bishop, N. H., 204, 207. Bouve, T. T., 391, 421. Brewer, T. M., 108, 145. Brvant, Henrv, 114, 158. Carney, Charles T., 409. Dix, W. G., 242. Dornbach, L. M., 107. Durkee, Silas, 206, 241. Edwards, William, 327, 337. Gould, Albert, 310. Gould, A. A., 11, 173, 422. Green, John, 55, 374. Haldeman, S. S., 401. Harrison, Edwin, 295. Haves. A. A., 48, 129, 200, 211, 297, .355.' Holmes, 0. W., 247. Jackson, C. T., 17, 30, 32, 243, 294. Kneeland, Samuel, 152, 218, 231, 371, 418, 429. Lewis, James, 2, 149. Lyman, I'heodore, 260, 274, 287, 410. Magowan, Dr , 178. Morse, E. S. , 127. Pickering, Charles, 326, 366. Rogers, Henry D., 140. Rogers, William B., 40, 184, 186, 339, 346. Shaw, B. S., 281. Skilton, Dr., 303. citharella, '' 425. jinisim, ' ' 425. cuaillata, " 14. jjolltx, ' ' 14. }tus, " 425. 426 Sprague, Charles J., 181, 282, 292, Crustacean, Brachyurous, New form of, 315, 321. 412. Stimpson, William, 84, 307, 412. Crustacean impressions on an island in Stodder, Charles, 264, 302. Black River, Wisconsin, 310. Storer, 1). H., 385. Cryptogamous plants from region of Treadwell, Daniel, 396. Lake Superior, List of, 296. Weinland, David F., 34, 56, 59, 112. Crystals of Sulphate of lodo-Quinine, 160,252. 229; Zeolitic of Carbonate of Lime, White, J. C, 304, 404. 229; Made, Theory of formation of, Whittlesey, Charles, 127. 136. Winslo\v,'^C. F., 414. Cui-ator of Comp. Anatomy, Dr. J. C. Wyman, JeflVies, 51, 73, 400. White chosen, 427; of Crustacea, H. R. Storer elected, 263. Composition of Sandstones and Con- Curatorship of Crustacea and Radiata, glomerates, C. T. Jackson on, 168. 242. Concretions, Clay, from Presumpscot Cyanocorax Californicus, 149. River, Me. 132; iMauner of formation Cyathophyllum, from Lake Superior, of, 132. 139. Conglomerates, Composition of, 168. Cyclomyces, 58. Congress, Memorial to, 111. Cyclopean pig. Prof. J. Wyman on, 380. Connecticut River Sandstone, Bird Cyclostoma barbata, Gould, 425. tracks in. 111. " Copper, from Lake Si^perior Mines, and rocks with which it is associated,283; Different forms in which the copper occurs, 284; Silver with minerals and Cyclotus illoius, fossils from the same locality, 284. Cj-perus esculentus, raised in Wash- Copper in infusorial Earth, "292, 293, ington, D. C, 337. 310. Cysticercus in Cervus Virginianus, 395. Copper Mine at Elk Run, Virginia, C. Cystine, 229. T. Jackson on, 183. Corals, Prof. Agassiz on, 373; Classifi- Dams, vibrations of water falling over, cation of, 373 ; forty years old, from a William Edwards on, 327; W. B. wreck, 166. Rogers on, S38. Coral growth. Prof. Agassiz on rate of, Deane, Dr. James, Decease of, 387; No- 364. tice of, by T. T. Bouve, 391. Coral, new species of, Theodore Lyman Deep River, N. C, coal formation, Geo- on, 287; lasso-cells of, Prof. Agassiz logical age of, 32; Fossils of, 32. on, 367; Madrepore, Rate of growth Dennestes in Wood, 268. of, 374. Digger Indian, Capacity of cranium of, Cordiceps gi-owing on a fly, 337. 127. Corilla, Sub-genus, 424. Dioscorea batatas, see Yam, Chinese. Corrosion of Shells of Freshwater Dipsasplicata, Process of forming pearly Claras, Cause of, 57. figures in, 178. Corvus corax, 118; C. Americanus, 118. Distoma in Cervus Virginianiis, 395. Courtis Fund, J. RL Barnard chosen Dolomite from Texas, Maryland, Analy- Trustee of, 296. sis of, 244. Cragin, Dr. F. W., Decease of, 400; Drift, from Lake Erie to Lake of the Notice of, by Prof. J. Wyman, 400; Woods, 128. Resolutions concerning, 401. Cranium, human. Supposed fragment Earlt appearance of Birds in 1857, of from California, 180 feet below 170. surface of Table Mountain, 278; of Earth Worm, Climbing power of, 206. Digger Indian, Internal capacity of, Ecliinoderms, Burrowing of in Lime- 127. stone, 368. Creeper, Black and White, Mniotilta Ectopistes Carolinensis, 149; E. migra- varia, nest and eggs from Lynn, Mass., torius, 119. 5. Ecuador, W. G. Dix on, 242. Crossognatbus, nov. gen. Agas. 412. Eggs of Aspredo levis carried in mouth Crustacea, Parasitic, 19; New species of parent fish, 328; of other species of, from Western N. America, 84 ; also, 328. from California, 279; H. R. Storer Eggs of Bagr(5 or Ningi-ningi, Manner chosen Curator of, 263, in which they are hatched, 268. 427 Ego;-case of Skates, Prof. J. Wyman's observations on its formation, 376. Egg of Slellisuga anna, 148 ; of Scoleco- pliagus Mexicanus, 148. • Electric apparatus of Raia batis, 44. Elephant Fossil, from Brazos River, 51. Elk Run, Va., Copper Mine at, 18.3. Elm, Involuted growth of, 289. Embryological characters of Garpikes, 48. Embryology of Acantheus Americanus, 37. Encrinal Limestone of Wisconsin con- taining Bitumen, 309. Engraving "Nature's Own," 280. Entomological Collection of Dr. T. W. Harris, its purchase for the Society, 416. Epidermis, from mouth of Pristis sagit- tata, 67. Equus major, from Brunswick, N. Y. , Dr. Skilton on, 303. Eriophilus, nov; gen. Hald., 402. mali, " 403. Erismatura Dominica from Lake Cham- plain, 343, 375. Erosion of Alasmodonta arcuata, Cause of, 258; of Freshwater shells, 57; Dr. James Lewis on, 149. Erythrospiza purpurea, 118. Esox, Varieties of, 430. Eupagurus, Samtielis, Stimpson, 86. turgidus, '' 86. European Widgeon from New Jersey, 376; breeds on L. Island, 419. Excursions, 10; to Hingham, 19. Exocetus, Dr. Weinland on, 385. Ej'e of Sperm Whale, 125. Eye piece, Orthoscopic, 246. Families of Turtles, Proper characters of, 64. Fecundation of Turtles, 10. Feeding and growth of American robin, 396. Filaria in Cervus Virginianus, 395. Fish, tlying. New division of, 385. Fishes, Prof. Agassiz on Classification of, 407 ; Habits of, Capt. N. E. Atwood on, 175; Blind, of Mammoth Cave, Anatomy of, 72. Fishes, European, Transplanting of, 369. Fishes, Fossil, from Ohio, 18. "-"^^ Fishes, Jamaica, Prof. Agassiz on Hill's Catalogue of, 414; Lophobranchious, method of locomotion in. Dr. D. F. Weinland on,'<346 ; Migration of, 125, 419; new species from Nicaragua, 408 ; ovarian impregnation in, 10 ; from Surinam, 328; fish from North Atlantic, probably a new species, 280 ; dropped on land during a show- er, 2^3: Fish Scales, of bony struc- ture, 285 ; Fluorine in, 366. Flight of Lepidoptera, Mechanism of, 426. Florida Pomocentridaj, New species of, 411. Fluorine in fish scales, 366. Flycatcher, Canada, Nest and eggs of, found in Lynn, Mass., 5. Fly, House, Parasitic plant on, 337. Flving fish. Proposed new division of them, by Dr. Weinland, 385. Foetus, liuman, of third week. Dissection of, by Prof J. Wyman, 336 ; Analogies of its transient conditions, 336; Para- sites in, 26. Foetal pigs. Remarks on, by Prof. J. Wyman, 363; foetal porpoise, 71. Food of Robin, Discussion an, 399, 403. Footprint, biped web footed. Fossil, 10. Foraminifera exhibited, 246. Forms of Birds, related to structure, 410. Fossil, biped webbed footprint, 10. Fossil crustacean impressions, in Wis- consin, 310. Fossil bones of Suidse from Iowa, 8 ; Fos- sils, American, Oldest, 310; Fossils, Proposed exchange of, 231 ; from Brazos River, Texas, 51 ; of Deep River Coal formation, 32; Fossil-Ele- phant from Brazos River, 51 ; Fossil fishes from Ohio, 18; ditto Starfish from Lewiston, Me., 394. Freshwater Shells, Cause of erosion of, 149. Fungi, New England, List of, by C. J. Sprague, 316. Fungus, Parasitic, on a Beetle, 26. Ganoids, a Natm-al group, 63. Gar-pikes, Embryological characters of, 48; Affinities of to reptiles, 48; and Sturgeons, Resemblances of, 63, Garrulus cristatus, 118; Canadensis, 118. Gas, burning jets of. Sonorous action of, 333, 339, 346. Generation, Alternation of, in Trematoda of Freshwater Shells, 24. Geographical distribution of North American Turtles, Prof. Agassiz on, 5. Geological Section, from Greenfield to Charlemont, Mass., Diagram of, 330; Description of Section, by C. H. Hitch- cock, 330; Remarks on, by Prof. W. B. Rogers, 332; on Map of Pennsyl- vania, 378; of New Mexico, 368. Georgia, Peculiarities of Helix thj'roi- dus in, 129. Gestation of Aspredos or Trompetti, 269. Glseosporium crocosporum, Berk, and Curt., 282. 428 Glowworm, Dr. Dnrkee on the, 241; from Cohasset, Mass. 396. Glucose of Sorghum, chemical change in, Dr. A. A. Haj-es on, 297 ; Dr. C. T. Jackson on, 299. Goliathus giganteus, 58. Goniobatis, nov. gen. Agassiz, 385. meleayris, " 385. Gould, Dr. A. A., Account of visit to Scientific Institutions of Europe, 409, 410. Governor's Island, IMass., Slate rocks of, Peculiar condition of, 217; Horizontal heave in, 217. Graafian vesicle of Zoarces anguillaris, 38. Grand Manan, Birds of, 114. Green, John, Resignation of ofliceof Cu- rator of Cftmparative Anatomy, 420. Greene, B. D., Donation to Herbarium, 215. Growth prol)ably rapid of ^ladrepora alcicornis, 364. Guano, Rock, from an island in the At- lantic Ocean, 157. Guillemot, Brunnich's, Breeding habits of, 124. Gum, African, Analysis of, by Dr. A. A. Hayes, 129 ; from California, 218, 227 ; Lahoe, C. Stodder on, 302. Habits of fishes, Capt. N. E. Atwood on, 175. of Muscicapa acadica and fla- viventris, 430. Haddock, viviparous, 9 ; Psorospermia in, 26. Htematite, 131 ; Manner of production of, 131. Hair ball, 242. Halisetus leucocephalus, 115. Hake, American, viviparous, 9. Hapalocarcinus marsupialis, Stimpson, 412. Harris, Dr. T. W., purchase of his En- tomological Collection by the Society, 416. Hayti, Chemical effect of Sea-water on Organic Life of, 257 ; some points in the Zoologv of, Dr. D. F. Weinland on, 252 ; Elevation of, 253 ; Sea of, 255. Heart's action, Brown-S^quardon influ- ence of respiration on, 67. Helices, American, Monograph on, by W. G. Binne}', 155. Helicina verecunda, Gould, 426. Helix asteriscus, Morse, 128. bucculenta, 129. clausa, 129. Bamascena, Gould, 11. intercisa, Binnev, 156. labiiis, Gould, 422. Imta " 422. Helix minixtissima, 72. operculina, Gould, 423. pauper, jmpulus, i^amentosn, 423. 423. 11. repercussa, 11. sqtiarrosa, 423. thyroidus. Geographical distribu- tion of, 128. " Peculiarities of, in Ala- bama, Georgia, St. Simon's Isle, and near Philadelphia, 129. Helminths, Nature's method of preserv- ing them, Dr. D. F. Weinland on, 343. Herbarium, Donation of, by Benjamin D. Greene, 215, Resolutions on, 216. Herbivora, Series among, 113. Hesperomys Bairdii, 182. Hingham,"Mass., Excursion to, 19; Sub- merged trees at, 20. Hippa analoya, Stimpson, 85. Hirundo Americana, 115; bicolor, 115, 148; lunifrons, 148; rufa, 115. Hog, Kidney of, Sclerostomum dentatura found in, 428. Hornet's nest, occupied three successive years, 329. Human and Mastodon remains found together, 278. Hylodes luieatus, 269. Hypotriorchis columbarius, 115. Ichthyology, Curator of, Capt. N. E. Atwood elected, 92. Idota;a resecata, Stimpson, 88. Impressions, Fossil crustacean, in Wis- consin, 310; Myriapod,in Connecticut River Sandstone, 111. Impressions, Polygonal, in Connecticut River Sandstone, 111. Indian Cemetery at Hingham, Mass. 20. Indian, Digger,' Capacity of cranium, 127. Infusorial Earth, Copper in, 292, 293; Analysis of, by Albert Gould, 310. Inhabitants of Sandwich and Society Islands, are they of common origin ? 414. Insects injurious to Vegetation, Report on republishing Dr. Harris's Work on, 417. Memorial to Legislature on, 420; Insects, Dr. Harris's Collec- tion of, 40. Instrument for making sections of wood, 264. lodo-Quinine, Sulphate of, Crystals of, 229. Iron, Carbonate of, Ridgeway, Analysis of, 18; Native, from Africa, 279; Iron, black-band ore. Analysis of, 32; ore from Maryland, 245; from New York with oolitic structure, 340; Remarks of W. B. Rogers on 340; Sand as 429 a nucleus of, 341; Mountain, Mo., Magnetite from, Analysis of, 295. Island Monk's, 158. Itch insect, Eggs of, 290. Jamaica, Fishes of, Prof. Agassiz's, re- marks on Hill's Catalogue of, 414. Japan, Shells from, 124. Japonia, Gould, nov. genus, 426. Journal, Sixth Volume completed, 335. Keweenaw Point, Birds of, List of, by Dr. Kneeland, 231. Kingdom, Animal, Series in, 112. Kneeland, Dr. S., Jr., elected Secretarv, 386. Labrador, European Saxicola breeds in, 420. Labrax lineatus. Analysis of scales of, 374 ; Section of scale of, 362. Lahoe Gum, 302. Lake Champlain, Erismatura Dominica from. 343, 375. Lake Superior, List of Cryptogamous plants from vicinity of, 296; Cya- thophyllum from, 139; Trap dikes of, 23. Lampyris noctiluca? 241. Landslide near Montreal, exposing ter- tiary fossils, 268; ditto on Presump- scot River, Me., 132; Cause of, T. T. Bouv«5 on, 132. Laomedea gelatinosa on Cineras and PennelljE, 404. Larus argentatus, 121; marinus, 122; atricilla, 122. Lasso cells of Coral, 367 ; Spermatozoa in, 873. Lead, Sulphide of, crystals, 259. Lepadogaster and Cyclopterus should be placed in distinct families, Prof. Agassiz's views, 411. Lepidoptera, Flight of, 426; mechanism of wing, 427. Lernsea on Orthagoriscus mola, 396. Lestris Richardsonii, 122. t^etter from Dr. James Lewis, present- ing shells, &c., 1. Library, Binney, Catalogue of, 97. Letters from, Academia,Real de Madrid,39, 387,427. Academic Imperiale, &c., de Lyon, 140. Academic Royale de Belgique, 289. Acad^mie Rovale des Sciences de Stockholm, 140, 358, Academic des Sciences, Paris, 171. Academy of Natural Sciences, 289, 290. Academy of Science of St. Louis, 289. Accademia di Bologna, 216. Akademie, K. Baverische, der Wis- senschaften, 70, 216, 387. Akademie, Kaiserliche, der Wissen- schaften, Wien, 92,289,290, 387. Akademie, K. Preussische,der Wissen- schaften, 92, 387. Association, American, for the Ad- vancement of Science, 290. Association, Dublin University Zo(5- logical and Botanical, 92. Association, Georgic, Randolph, N.Y., 242, 290. Association, Pottsville Scientific, 329. Batchelder, John, 288. Baird, Spencer F., 70. Binney, Mrs. M. A., 64. Binney, W. G., 128, 387, 428. Bowerbank, Mr., 267. Calonby, Stephen, 92. Chavlesworth, Edward, 39. Clarke, Robert, 92. Conrad, J. A., 39. Davis, A. P., 279. Davis, H., 358, 387. Dawson, Prof., 268. De Jolis, Auguste, 427. Georgic Association, 242, 290. Gesellscliaft Naturforschende in Em- den, 171. Gibbes, Dr. Lewis R., 92. Girard, Charles, 140. Glover, Townend, 231. Gregory, Prof., 283. Harvard College, Corporation of, 358. Hayes, Dr. L I., 396, 427. Howell, Robert, 387. Hubbard, Prof., 283. Institute, Essex, 140, 358. Institution, Roval, 358. Kennicott, Robert, 39, 140, 154, 182. Kneeland, Samuel, Jr., 49, 152. Kumlien, Thure, 109. Latour, L. A. Huguet, 140. Lawrence, George N., 92. Lea, Isaac, 140. Leeds, Stephen P., 428. Lewis, James, 1. Library, New York State, Trustees of, 92, 358. Loosey, Charles, 413. Loring, Russell, 329. Lycseum of Natural History, New York, 358, 413. Madison Historical Society, 39. Magowan, Dr., 178. Martin, Dr. Charles, U. S. N., 92. Morse, E. S., 66. Museum, Geological, Calcutta, 290. Naturforschende Gesellschaft zu Em- den, 216. Newberry, John S., 140. Parkinson, James C., 39. Perry, Alexis, 40. 430 Public Library of Boston, 358. Reale Accademia delle Scienze di Napoli, 70. Regents of N. Y. University, 70, 139. Roj'al Geographical Society, 70, 413. Royal Institution, 140, 358. Royal Society, 70, 358. Samuels, E., 1. Sargent, Winthrop, 92. Secretary of State, 70. Sharswobd, William, 401, 413, 428. Shurtleff, Simeon. 387. Slawson, James H., 290. Smithsonian Institution, 290, 413, 428. Society des Arts et des Sciences de Batavia, 387. Society de Geographie, 70, 170. 387. Society d'Histoire Naturelle du De- partement de la Moselle, 387. Soci(5t^ du Museum d'Histoire Natu- relle de Strasbourg, 413. Society de Physique, &c., de Geneve, 92. Socii5t6 des Sciences Naturelles de Neuchatel, 329. Society Imperiale, d' Agriculture, &c., de Lyon, 140. Societ^ Linn^ene de Lyon, 140. Society Royale, &c., de Li(?ge, 358, 369. Societ(5 Royale de Zoologie, Amster- dam, 387. Society, American Philosophical, 170, 289. Society, Cambridge Philosophical, 290. Society, Elliott, of Natural History, 216,'329. Societ}', Ethnological, 216. Society, Geological, 170, 358. Society, Imperial Mineralogical, of St. Petersburg, 216. Society, Leeds Philosophical and Lit- erary, 387. Society, Linnfean, 170, 387. Societ}', Royal Geographical, 216. Society, Royal, of Edinburg, 329. Society, Royal, of Sciences at Gottin- gen, 289. Spencer, C. A., 246. Stimpson, William, 91, 92, 140. Swallow, G. C-,369. Swan, A., 358. Toldervy, J. B., 329. Verein, Naturhistorischer, Bonn, 329. Verein,Naturwissenschaftlicher,Ham- burg, 329. Verein, Zoologisch-Botanischer, 92, 358. Verein fiir Naturkunde in Nassau, 290, 329. Verein fiir Vaterlandische Natur- kunde in Wurtemberg, 216, 387. Whittlesey, Charles, 140. Winslow, C. F., 278. Leuciscus from Squam Lake, N. H., 243. Library, Donations to, by Academia, Real, de Ciencias de Mad- rid, 432. Acad^mie des Sciences de Stockholm, 360. Academie Imperiale des Sciences, &c., de Lyon, 96. Academie Imperiale des Sciences de Bordeaux. 95, 362, 389, 432. Academy, American, of Arts and Sci- ences, 46, 173, 361, 390. Academy of Natural Sciences of Philadelphia, 47, 96, 173, 221, 361, 432. Academy of Science at St. Louis, 221, 390. Accademia delle Scienze dell' Istituto di Bologna, 222. Accademia Reale delle Scienze, 95, 172, 432. Adams, H. & A., 406. Akademie, K. Bayerische, 47, 221, 389, 390., Akademie, K. Preussische, 96, 273, 389, 406. Akademie, K. S. Vetenskaps, 173, 362. Akademie, Kaiserliche der Wissen- schaften, Wien, 95, 96, 313. Albany Institute, 360. Annales des Sciences Physiques de Lvon, 432. Archiv fiir Naturgeschichte, Erichson, 96, 389, 406. Association, American, for the Ad- vancement of Science, 220. Atwood, N. E., 220. Bache, A. D., 360. Bailey, J. W., 222, 223, 224, 225, 226, 227, 360. Bailey, J. W., Heirs of, 313, 389. Baird, S. P., 313. Binney, Amos, Heirs of, 166, 171. » BinneV, Mrs. A., 97. Binney, W. G., 172, 360, 406. Bland, Thomas, 431. Borland, J. N., 388. Boston, City of, 312. Brown- S^quard, M., 94. Canadian Naturalist and Geologist, 173, 221, 273, 362, 390, 406, 432. Carpenter, P. P., 361. Chadbourne, P. A., 388. Charlesworth, E., 406. Conchological Miscellany, 221. Courtis Fund, 47, 173, 222, 273, 314, 362, 390, 406, 433. Dana, James D., 46, 93, 388, 431. 431 Daniels, E., 360. Denny, H., 94, 313. Dowler, B., Dr., 272, 360. Durand, E., 46. East India Company, 431. Emmons, Eben, 46. Essex Institute, 47. Faxon, G. N., 360. Fischer, Dr. S.,94. Fitch, Asa, 172. Flint, C. L., 46, 220, 272. Frauenfeld, G., 361. Gebiete der Naturswissenchaften, 313. Gesellschaft in St. Petersburg fiir Mineralogie, 173, 222. Gesellschaft, K., der Wissenschaften zu Gottingen, 172, 313, 432. Gesellschaft Oberhessischer, 432. Gillis, Lieut. J. M., 172. Governor General of India, 272. Greene, B. D., 360. Gregory, William, 360. Hanley, S., 406. Harvey, W. H., 431. Hayes, A. A., 388. Hermann, 46. Hickcox, J. H., 93. Holden, E. S., 389. Holmes, F. S., 360. Houghton, G. F., 84, 192, 313. Hunt, T. S., 360. Institute, Albany, 361. Institution, Republican, 47, 173, 222, 273, 314, 362, 390, 391, 407. Institution, Smithsonian, 93, 272, 273, 432. Institution, Royal, 173, 389. Jordan, Alexis, 94. Journal, American, of Science and Art, 96, 193, 221, 273, 314, 361, 389, 406, 432. Journal, Canadian, of Industry, Sci- ence and Art, 389, 406, 432. Kneeland, Dr. S., Jr., 360. Lapham, I. A., 172, 312. Latour, L. A. Huguet, 173, 221, 272, 361, 431. Lea, Isaac, 46, 360. Leidv, Joseph, 46, 360. Library, Astor, 361. Little,"Bro\vn & Co., 172. Lyceum of Nat. History, Ne\v York, 361. Marcou, Jules, 93, 272, 406. McClelland, Dr. John, 95. Medicine, New York Journal of, 95, 173, 389, 406, 432. Meigs, J. A., 221, 431. Meteorologie, &c., K. K. Central An- stalt, 96. Natural History Review, 361,389, 406, 433. Naturforschender Gesellschaft in Em- den, 314. New York Journal of Medicine, 222, 273, 314, 361. New York Library, Trustees of, 46, 220. Olmsted, D.,313. Owen, Richard, 94. Palmieri, A., ed A. Scacchi, 95. Perley, M. H., 406. Prime, Temple, 172. Redfield, W. C, 172. Reichsanstalt Geologische, Wien, 406, 432. Review, Natural History, 221, 313. Richardson, Sir John, 172. Robell, F. von, 93. Rogers, H. D., 220, 272, 360, 388. Rogers, W. B., 405, 431. Royal Institution, 173. Scfimarda, L. K., 313,432. Schonbein, C. F., 94. Sclater, P. L., 95, 220. Shumard, B. F., 46, 220. Smith, F. G., 361. Smith, J. L.,94. Soci^t^ de Geographie, 95, 173, 273, 406. Society de Physique, &c., de Geneve, 95. Society des Sciences Naturelles de Neuchatel, 313. Soci^'t^ Imperiale d' Agriculture de Lyon, 95. Soci^t^ Linn^enne de Lyon, 95, 432. Society Royale de Li^ge,'46, 361,432. Society, American Antiquarian, 432. Society, American Philosophical, 47, 173, 221, 314, 361, 406. Society, Cambridge Philosophical, 221. Society, Elliott, of Natural History, 95, 273. Society, Geological, Dublin, 389. Society, Geological and Polytechnic, of Leeds, 389. Society, Historical, of Wisconsin, 273. Society, Leeds Literary and Philo- sophical, 94, 314, 389. Society, Linnsean, London, 173, 389. Society, Royal, Dublin, 432. Society, Royal Geographical, 47, 95 221, '313, 362, 390, 406, 432. Society, Zoological, London, 95, 273, 406. Society, Zoological, 313. Sprague, C. J., 388. Stimpson, William, 94, 172, 272, 405. Sumner, Charles, 172, 361, 389. Thiersch, 46. Troschel, F. H., 220, 362. University, New York, Regents of, 94, 220, 360. 432 Vattemare, A., Exchange with, 96, 97. Verein der Preussischeu Rheinlande uiul Westphalens, 313. Verein fiir Naturkunde, Nassau, 221. Verein Naturhistorischer, Bonn, 221. Verein Wiirtembergischer, 95, 221, 314, 362, 389, 406, 432. Verein Zoologisch-Botanischer, 95, 362. Vogel, A., Jr., 94. Wall, William S., 46. Warner, John, 313. Weinland, D. F., 406. Wells, D. A., 360. Wiegmann, A. F. A., 313. Wilson, Henry, 172. Yandell, L. P., 46. Liga punctata, Weinland, 62. Lime, Native Borate of, 206 ; Carbonate of, Zeolitic crystals of, 229; Oxalate of, 263 ; Phosphates of, effect of de- caying organic matter on. Dr. A. A. Hayes on, 355; Phospliate of. State in which it exists in Sea-water, 48. Limestone, Encrinal, of Wisconsin, con- taining Bitumen, 309; of Texas, Ma- ryland, 243 ; Ridgeway, Analysis of,18. Limulus, manner of casting its shell, 22. List of Mollusks of Herkimer and Ot- sego Counties, N. Y., by James Lewis, 2. Livoneca vulgaris, Stimpson, 88. Lobognnthus, nov. gen. Agassiz, 412. Locomotion of Lophobranchious fishes. Method of, 346. Lophobrancliious fishes, method of loco- motion of. Dr. D. F. Weinland on, 346. Loxorynchus, nov. gen. Stimpson, 84. granais, " 85. Lumb: icus ascaris, 18 ; terrestris, climb- ing power of. Dr. Durkee on, 206. LygiAdilatata, Stimpson, 88. Macle Crystals, Theory of formation of, 136. Madrepora alcicornis. Probably rapid growth of, 364. Madrepore Coral, Rate of growth of, 374. Magnetite from Iron Mountain and Pi- lot Knob, Missouri, Analysis of, by Edwin Harrison, 295. Maine, Fossil Starfish from, 394. Mammalia, Series among, 113. Mammoth Cave, blind fish of. Anatomy of, 72. Map, Geological, of Pennsylvania, 378. Marble of Texas, Maryland, 243. Mareca Penelope from New Jersey, 375. Maryland Limestone, 243; Marble, 243. Massachusetts, Eastern, Paleozoic rocks of, their age, 41 ; Salmo hamatus in, 418, 431 ; tobacco, 408. Mastodon and human remains found to- gether, C. F. VVinslow on, 278; from Brazos River, 53. Megalops, Structure of Scales of, 363. Megatherium from Brazos River, 53. Melanerpes formicivorus, 149. Mellisuga anna. Egg of, 148. Members, Corresponding, elected. Binnev, W. G., 413. Blake" John R., 45. Davis, H., 341. De Jolis, M. Auguste, 70. Dewey, C. P., 370. Gatliff, James R., 154. Gibb, George Duncan, 213. Hill, Richard, 428. Hoopes, Bernard A., 341. Kennicott, Robert, 19. Lawrence, George N., 72. Leeds, Stephen P., 409. Loring, Russell, 154. Marcou, Jules, 405. Morse, E. S., 413. Newberry, John S., 45. Robinson, William F., 45. Sargent, Winthrop, 45. Shurtleff, Simeon, 370. Slawson, James H., 242. Swan, Rev. Joshua A., 334. Member, Honorary, elected. Hyrtl, Joseph, 413. AIembers, Resident, elected. Agassiz, Alexander E. R., 370. Baker, W. W., 335. Barnwell, R. H., 216. Bemis, Cliarles V., 242. Brown, F. H., 420. Burckhardt, Jacob, 420. Carnev, Charles T., 335. Clarke, Henrv J., 179. Clarke, Thoni.as W., 19. Coale, William E., 370. Cobb, Frank D., 45. Cummings, A. L, 59. Davis, George N., 219. Dean, John, 19. Dornbach, L. M., 127. Farrand, Nathan, 427. Faxon, George N., 263. Fearing, Albert, 45. Folts, Dr. D. v., 405. Foster, John S., 45. Gaffield, Thomas, 388. Gay, A. M., 171. Gibbens, Edwin A., 19. Gibson, William B.,417. Giles, Alfred E., 59. Green, John, 19. Green, Dr. S. A., 266. 433 Habicht, Edward, 127. Hammond, Samuel, 19. Harrison, Edwin, 59. Havward, J. M., 9. Hill, P, C, 330. HunnewelJ, J. L., 9. Jeflries, Edward P., 311. Kessmann, Charles, 127. Kidder, Jerome G., 345. Lamson, J. A., 246. Lewis, Charles P., 394. Lovett, Charles W., Jr., 341. Manley, Edwin, 230. Martin, John S., 230. Metcalf, Theodore, 219. Miles, James E., 19. Morris, Thomas D., 219. Motlev, Thomas, 405. Ordway, Albert, 417. Otis, Dr. J. H., 388. Page, Kilby, 341. Peabody, Oliver W., 242. Pearce, S. H., 45. Perkins, Augustus J., 19. Philbrick, John D., 311. Pickering, Octavius, 409. Putnam, F. VV., 9. Rand, Edward S., Jr., 154. Robinson, John P., 154. Rogers, George H., 286. Rogers, Henrv D., 246. Rogers, William B , 246. Russell, Dr. Ira, 388. Safibrd. J. Henr.y, 19. Shurtleff, Augustine, 45. Shute, James G., 179. Stone, L. B., 330. Sullivan, Thomas R., 200. Talbot, I. T., 59. Tillinghast, Joseph, 286. Ward, B. C, 127. Weeks, James H., 263. Weinland, David F., 19. Wellington, Ambrose, 59. Wetherell, Leander, 140. -Wheatland, Dr. R. H., 413. Willard, Joseph, 260. Williams, Dr. Henry W., 57. Wilson, Archelaus, 216. Winslow, Dr. C. F., 409. Woodward, Samuel, 382. Worcester, Joseph, 19. Wright, Edwin, 379. Memorial to Congress, 111. Menobranchus from Portage Lake, Michigan, 152, 218; hyemalis, Knee- land, 280; Habits of, 371; relative value of branchial, pulmonary and cutaneous I'espiration in, Dr. Knee- land on, 429. Metamorphic Strata of the Atlantic Slope of the Middle and Southern States, Classification of, by H. D. Rogers, 140. Meteoric Stone, supposed, from Marble- head, Mass., Analysis of, by Dr. C. T. Jackson, 294. Microscope, Compound, Dr. 0. W. Holmes's new stand for, 247; Figure of, 248. Microscopic Stnicture of Orthagoriscus inola, 404. Microscopical Department, Committees of, 230, 213; Report of, 214. Microscopy, Curator of, 215. Migrations of Fishes, 125, 419. Millepora not a Polyp, 364. Mitra florida, Gould, 14. Mniotilta varia, 116; nest and eggs from Lynn, Mass., 5. Molar Supernumerary, in man and a Chimpanzee, 45. Mollusca, Terrestrial, Binney on, 177. Mollusks of Herkimer and Otsego Coun- ties, N. Y., List of, by James Lewis, 2. Monk's Island, 158. Mormon Arcticus, 122. Morphology of bladder of Batrachians, 58. • Mosquitoes infesting a limited locality, 381. Motions of Animals, Psychological view of, 160. Musca, Larva of, in human skin, 281. ^luscicapa acadica and flaviventris, hab- its of, Dr. Bryant on, 430. Museum, Donations to, by Adams. S"., 171. Ainsworth, Mr., 270. Agassiz, L., 388, 431. Andrews, C. L., 312. Atwood, N. E., 93, 219, 280, 311, 359. Bailev, J. W., 219. Bailey, W. W., 220. Baker, William W., 405. Balch, F., 388. Binnev, W. G., 171. Bishop, N. H., 219, 270. Blake, C. W., 93. Blake, W. P., 171. Borland, J. N., 46, 93, 359. Bryant, Henry, 171, 340, 359. Bumstead, F. J., 171, 219, 359. Cabot, Edward C, 264, 270. Cabot, S., Jr., 359, 405. Cooke, C, 405. Couthouy, J. P., 171. Curtis, D. T., 359. Dall, Mrs. C. W.,312. Davis, H., 359. Dennett, W. H., 431. Dexter, William P., 312. Durkee, Silas, 93, 220, 272. Eddy, R. H., 206, 220. 434 Fairbanks, C. B., 405. Farwell, 0. A., 93. Fay, .1. S., 220. Fesscnden, C. B., 388. Fletcher, Mr., 93. Forbes, .J. M., 3-59. Gassett, Oscar, 4.5. Glover, Towiicnd, 337, 359. Gott, Addison, 45, 359. Gould, A. A., 45, 312, 359, 388. Green, John Jr., 312, 328, 359. Green, S. A., 270. Greene, B. U., 220, 286, 311. Greene, C. G., 431. Hale, C. S., 421, 431. Ilalev, William, 93. Hayden, F. V., 93. Haves, A. A., 388. Hicks, D. F., 431. Hi Hard, Mrs. G. S., 45. Hitchcock, David, 111, 171. Holbrook, J. C, 405. Holden, E. S., 431. Holden, O. H., 171. Holmes, C. C, 45. Jackson, Charles T., 45, 220, 228, 270, 312, 337, 359, 405, 431. • .Tenks, J. W. 1'., 359. Kelloj,% E- 15- & K. C, 312. Keimicott, Robert, 46, 93, 171,220. Kneeiand, S., Jr., 45, 93, 171, 270, 271, 280, 283, 296, 311, 312, 359, 388, 406. Kollock, Cornelius, 93. Landis, C. K., 405. Lapham, I. A., 418,431. Lewis, James, 45, 431. Loring, Caleb, Jr., 359. Lovett, C. VV., Jr., 311. Lyman, Theodore, 388. Marcou, Jules, 270. Martin, Charles, 92. Morse, Henrv I)., 375, 388. Morse, E. S., 93, 171. Museum, National, Melbourne, 270. Nason, Samuel M., 311. National Museum, Melbourne, 270. Nelson, Thomas, 431. Otis, Amos, 260, 270. I'arker, U. G., 93. Parker, Theodore, 220, 359. Parkinson, J. C, 219. Parsons, Theophilus, 289, 292, 311, 312. Phillips, Zaccheus, 405. Pickering, Charles, 93. Preble, Lieut. G. H., 219. Raymond, Mrs. C. B., 270. Robinson, J. P., 171. Rodman, Samuel, 431. Russell, E. H., 431. Samuels, E., 93, 171, 219, 311, 312, 359, 386, 388. Sargent, L. M., .Ir. 359. Schwartz, Louis 15., 171. Slawson, J. H., 272. Sohier, William, 219. Sprague, Charles J., 405. Stodder, Charles, 369, 388. Storer, 1). H., 311, 312. Storer, H. R., 93, 219, 270, 312. Swan, Samuel, 268. Tallant, .James, 45. Thorcau, H. D., 430, 431. Tufts, Samuel, Jr., 388. Tyler, George E., 45, 92. Wallace, William M., 382, 388. Warren, J. M., 375, 388. Weinland, D. F., 405, 431. Wheelwright, George S., 220. Whitman, W. E. S., 245, 270. Whittemore, T. J., 359, 431. Williams, Francis S., 270. Winslow, C. F., 278, 311. Wyman, Jeffries, 311, 312. Miiller, Johannes, Prof. Agassiz's notice of, 382. Mustela, N. American species of. Dr. Kneeiand on, 418; Mustela Canaden- sis, 418. Mvcology of N.England, Contributions to, 315. Myiodioctes Canadensis, 116. Myriapod Impressions, in Connecticut River Sandstone, 111. Nanina pisolina, Gould, 423. Nantucket, Sand Sharks from, 259. Narwhal, Tooth of, 260. Natural Hisiory, American works on, rare and costly in Europe, 404. Nature's method of preserving Hel- minths, .343. Nest and eggs of Mniotilta varia from Lynn, Mass., 5; of Vermivora rubri- capilla found in Lynn, 4; Sylvicola discolor, ditto, 6; icterocephala and pardalina, ditto, 6; virens, do., 5. New England Fungi, List of, bj' C. .1. Sprague, 316. New England Mycology, Contributions to, by C. J. Spnigue, 315. New Hampshire, Porcupine from, 311. N. Jersey, Mareca Penelope from, 375. New Mexico, Geological Map of, by Jules Marcou, 368. Nicaraguan Fishes, New species of, 408. Ningi-ningi, Manner of hatching its eggs, 268. Nomenclature of Superposition of Stra- ta, H. D. Rogers on, 183. North American species of Mustela, 418. North American Turtles, Prof. Agassiz on the Geographical distribution of, 5. 435 North America, Western, New Crusta- Phosphate of Lime, 48, 355. cea from, 84. Phosphorus, Supposed conversion of North Athmtic, New fish from, 280. human bones into, 57. North Carolina Coal, Is it apis coal? 33. Photographs of microscopic objects, N. Pacific and Atlantic shells identical, 330. 124; Kxiiedition, Report of, 91. Photo-lithographic figures of microscop- Note of White-throated Sjjarrow, 236. ic objects, 358; Photo-lithograph pro- Nova Scotia, Trap dikes ot', 23. cess, 358. Nymphcea odorata. Pink, 208. Physa heterostropha. New species of Cercaria on liver of, 24. Objectives, Microscope, by Grunow, Physalia, Stinging power of, Dr. Charles 381. " Pickering on, .366. Octohedral tin ore, Australian, 227. Picus auratus. Taenia of, 59; pubescens, OcuUuA ylome.rata, Lj'man, 288. 118; arcticus, 118. Odontoid Process not united to Atlas, Pig, Cyclopean, Prof. J. Wyman on, 309. 380. Officers for 1857-8, 192; 1858-9, 370. Pigeon from Australia, 169. Ohio, Fossil fishes from, 18. Pilgrim Trading house at Monumet, Oil from a wreck twenty years old, 166, Mass., 289. 167. ' Pilot Knob, Mo., Magnetite from, Analy- Oldest American Fossils, 310. sis of, 295. Oranges, Capnodiumelongatum on, 378. Pines, White, Capnodium elongatum Orangs of Borneo, Capt. Gibson on, 71. on, 378. Organisms, Silicification of, A. A. Pink Nymphsea odorata, 268. Hayes on, 168. Pipe-fish in abdominal cavity of Cod, Orthagoriscus mola, Microscopic struc- 176. ture of its tissue, 404; Cecrops and Pityriasis versicolor. Parasitic plant Cineras on, 396; Parasites of, 404; from, 291. Lernaia on, 396; Pennella filosa on, Plagiostomes not fishes, 38. 404. Plants from S. America, List of, by Orthoscopic eyepiece, 246. N. H. Bishop, 182; Cryptogamous, Otus Cassinii, 115. from region of Lake Superior, List Ovarian impi-egnation in fishes, 10. of, 296. Owl, Burrowing, 204. Polycistina exhibited, 246. Ox, Urinary calculi of nearly pure Sil- Polygonal Impressions in Connecticut ica from an, 213, 284. River Sandstone, 111. Oxalate of Lime, 263. Pomacentrus melear/j-is, Agassiz, 411. PomocentridtE, new Florida species, Paleozoic age of rocks of Eastern 411. Massachusetts, 41. Pomotis, supposed new species of, 430. Pandalus Dana, Stimpson, 87. Pompeii, Vessels from, 177. Paper-like substance formed by meal- Porcupine from N. Hampshire, 311. worms, 414. Porcellana rupicoln, Stimpson, 85. Paradoxides Harlani, 41; from Brain- Porpoise, Fcetal, 71. tree, Mass. , 369. Potato acarus, 9. Parasites in the fcetus, 26; Human, 300; President, Acceptance of Election as, by Discussion on, 301. Dr. Jeffries Wyman, 1. I'arasitic plant on House fly, 337. Presumpscot River, Me., Clay concre- Parasitic plant of Pityriasis versicolor, tions from, 132 ; Landslide on, 132. 291 ; Parasitic wornis,Xature's method Pristis sagittata, Epidermis from mouth of preserving them. Dr. D. F. Wein- of, 67. land on, 343. Protococcus nivalis, 302. Parusatricapillus, 116j Hudsonicus,116. Provincetown, Mass., Centriscus scolo- Pastinaca hastata, 280. pax from, 178; Trumpet Fish from. Pearly figures in Dipsas plicata, how 178. formed, 178. Psorospermia in the Haddock, 26. Pennella filosa on Orthagoriscus mola, Psychological view of the motions of 404; Cineras vittata on, 404. animals, by David F. Weinland, 100. Pennsylvania Bituminous coal basin, Ptinus fur in Cayenne pepper, 404. 16; Geological Map of, 378. Ptychocheilus, nov. gen. Agassiz, 412. Phallus duplicatus, 37. Pudding-stone, Composition of, by A. A. Philadelphia, Peculiarities of Helix Hayes, 167. tliyroidus near, 129. Python, Structure of bone in, 55. 436 QuiscALUs versicolor, 118. Raia batis, Electric apparatus of, 44. BcmdalUa, iiov. gen., Stimpson, 85. ornatn, " 85. Kats, Albino, from Medford, Mass., 301. Rattlesnake, Experiment with, 56. Redfield, William C, Notice of, by W. B. Rogers, 186. Red Snow, 302. Report on Dr. 1. I. Hayes's proposed Arctic Expedition, 416; North Pacific Expedition, 91. Reproduction of Arachnides, 285. Reptiles, Series among, 114; collected in California, by E. Samuels, List of, 192. Resolutions on Deposit of Bimiey Libra- ry, 65. Respiration, Brown-S^quard on, 67; brancliial, pulmonary, and cutaneous, their relative value in Menobranchus. 429. Ridgeway Limestone, Analysis of, 18; Carbonate of iron. Analysis of, 18; Coal, Analysis of, 17. Robin, American, Feeding and growth of, 396; food of. Discussion on, 399. Rock Guano from an island in the At- lantic Ocean, 157. Saint Simon's Isle, Peculiarities of Helix thyroidus in, 129. Saline ma"tters in waters of Eastern Jlassaciiusetts, Origin of, 30. Salmo hamatus, found in ISIassacliu- setts, 418, 431. Salmonidse, Prof. Agassiz on, 418. Samuels, E., Collections in California, 38. Sand-Eel in abdominal cavity of Cod, 176. Sand-Sharks from Nantucket, 259. Sands of California and Australia, 228. Sandstone of Connecticut River, Bird tracks in. 111. Sandstones, Composition of, 168. Sarcoptes hominis, 290. Saxicola, Eui'opean, breeding in Labra- dor, 420. Scale of Striped Bass, (Labrax lineatus,) Section of, 362. Scales of Wegalops, Structure of, 363. Sciurus striatus. Albino, Specimen of 218. Sclero.stomura dentatura found near the kidney in a hog, 428. Scolecophagus Mexicanus, Egg of, 148. Scopelus, New species of, 71. Sea-water, Effect of, on organic life of Hayti, 257. Sepedonium cervinum, 292. Series in the Animal Kingdom, 112; among Herbivora, 113; JIanimalia, 113; Reptiles, 114. Sesquioxide of Chromium, New reaction of, under galvanism, 209. Setophaga ruticella, 116. Shaw, Dr. B. S., Resignation of, as Re- cording Secretary, 379; Vote of thanks to, 379. Shell of Limulus, Mode of casting off; 22. Shells, Freshwater, Erosions of, by Dr. James Lewis, 149; Shells, new species of, collected by N. Pacific Exploring Expedition, 422; New species of, 11; of freshwater Clams, Cai;se of cor- rosion of, 57, 258; of .Japan, &c., 124; of North Pacific and Atlantic identi- cal, 124. Silicification of Organisms, A. A. Haves on, 168. Skate, (Raia batis,) Electric apparatus of, 44; Egg-case of, Observations on its formation, by Prof. J. Wyman, S376; Claspcrs of, their use, 377. Skin, Tattooed, 91; Skin, human, Lai-va of Musca in, 281. Skunk, Stryclinine detected in, 342. Slate Rocks of Governor's Island, Bos- ton harbor, peculiar condition of, Prof. W. B. Rogers on, 217; Horizontal heave in, 217. Slate from Somerville, Mass., Analysis of, 108. Smelt, (Osmerus viridescens) from Squam Lake, N. H., 243 ; modified by residence in fresh water, 243 ; in Ja- maica Pond, Mass., 243. Society and Sandwich Islands, facts bearing on qui>stion of common origin of their inhabitants, 414. Society of Natural History, California, 154." Somateria mollissima, 119. Somerville, Mass., Analysis of Slate from, 108. Sonorous action of jets of burning gas, Prof. W. R. Rogers on, 333, 339, 346. Sorghum Halepense, 326 ; saccharatum, 326; vulgare, 326; saccharatum. Cane Sugar from, 286, 293, 296, 337 ; Chem- ical examination of, 342; Products of, 228; Sugar of. Dr. A. A. Hayes on, 200; vulgare. Botany of, C.J. Sprague on, 321 ; Varieties of. Dr. C. Picker- ing on, 326; Chemical change in Glu- cose of, 297. South America, List of plants from, by N. H. Bishop, 182. Sperm Whale, Structure of its eye, 125. Sphojroma ampUcauda, Stimpson. 89. Spongilla in Cochituate water, 267. Squam Lake, N. H., Leuciscus from, 437 243; Osmerus viridescens, Smelt, in, Terrestrial Mollusca, Binney on, 177. 243. Texas, Fossils from Brazos River in, 51. Starfish, Fossil, from Lewiston, Me., 394. Texas, Limestone of, 243 ; Marble, 243. Stepliaiiurus dentatus, found near the Thalassidroma Leachii, 122. kidney in a hog, 428. Tigers, People killed by, 16.5. Sterna arctica, 120; hirundo, 120. Tin Ore, Octohedral, from Australia, 227. Stinging power of Physalia, 366. Toad, Living, swallowed, 19. Strata, Superposition of. Nomenclature Tobacco raised in Massachusetts, 408. of, H. D. Rogers on, 184. Totanus macularius, 119; seniipalraa- Streptaxis, e//V;, Gould, 13. tus, 119. exacutd, '■ 13. Trachyte, Specimens resembling, from prostrala. " 12. guano rock, A. A. Hayes on, 211; Sinensis, " 424. Analysis of, 213. Striped Bliss, Analysis of Scales of, 374. Transplanting of European Fishes, 369. Struthio nivalis, lis. Trap dikes of Cohasset, 23; of Nova Strychnine detected in a Skunk, 342; Scotia and Lake Superior, 23. method of detecting, Dr. A. A. Hayes Trees submerged at Hingham, 20. on, 342 ; Dr. John Green on the "de- Trematoda, Alternation of Generation tection of, 346. in, 24. Sturgeons and Gar-pikes, Resemblances Trichas Marilandica, 116. of, 63. Trichophyton tonsurans, 379. Sturnella neglecta, 149. Trilobite from Braintree, Mass., 27, 40. Succinea lauta, Gould, 422. Trompettis, Manner of gestation of, 269. linenta, Binney, 155. Trumpet Fish from Provincetown, Sugar Cane, Chinese, Syrup and Sugar Mass., 178. from, 170; Botanical position of, 181; Tryblionella eWptica, Stodder, 381. Dr. A. A. Hayes on, 200; cane, from Tuomey, Prof Michael, Notice of, by VV^. Sorghum Saccharatuni, 286, 293, 296, B. Rogers, 184. 337; Chemical examination of, 342. Turdus migratorius, 116; Feeding and Suid«, Fossil bones of, from Iowa, 8. growth of, 396; olivaceus, 117; soli- Sula bassana, 119. tarius, 117. Sullivantia Ohionis from Wisconsin, Turkey, Gould's supposed new species 418. of, 158. Sulphide of Lead Crystals, 259. Turtles, Fecundation of, 10; Proper Sun-fish, See Oithagoriscus mola. characters of families in, 64; North Superior, Lake, Mines, Copper from, and American, Prof. Agassiz on the Geo- rocks with which it occurs, 283; Dif- graphical distribution of, 5. ferent forms of, 284; Silver with, 284. Tyrannula fiaviventris, 115. Supernumerary molar in Man and Tyrannus verticalis, 148. Chimpanzee, 45. Supra-renal Capsules, Brown-S^quard Unio comscus, Gould, 15. on, 69. lepidus, " 15. Surinam bush-ropes. Sections of, 290; tlria Brunnichii, Breeding habits of, woods, 279. 124; grylle, 123, 125; troille, 123. Surinam fishes, 328 ; Reproduction of, 286; unusual conditions of develop- Vallisneria spiralis, 229. ment of eggs of. Prof. Wyman on, Verraivora rubricapilla, nest and eggs 268. of, 4. Sylvicola discolor, nest and eggs found Vesicle, Graafian, Peculiarity of, in at Lynn, Mass., 6; icterocephala, 116; Zoarces anguillaris, 38. aestiva, 116; striata, 116; virens, 116; Vessels, Pompeian, 177. icterocephala and pardalina, nest and Vibrations in water falling over dams, eggs found in Lynn, Mass., 5; virens, William Edwards on, 327, 338; Prof nest and eggs from Lynn, Mass., 5. W. H. Rogers on, 338. Synckpas, nov. gen., Lyman, 274. Vireo Solitary, Vii-eo soliiarius, seen in Gimldii, " 274, 418. Lynn, Mass", 5. Vireosylvia Philadelphica, 109, Habits TiENiA of Picu« auratus, 59. of, 110; Compared with V. gilvus, Tcenioids, New genus of, 59. 110. Tapeworm, New species of, 300; Devel- Yitr'mix imperntor, Gould, 422. opment of, 304; Larvae of, in the Ale- Vorticella craterifornais, 228. wife. Cod, hare, and rat, 25. Teredo thoracites, Gould, 15. Warblek, Black-throated Green, Syl- 438 vicolavirens, nest and eggs from Lynn, Mass., 5; Chestnut-sided, S. ictero- cephala, 5; Nashville, Vennivora ru- bricapilla, ditto, 4; Prairie, Syldcola discolor, ditto, 6. Warren, J. C, List of his Scientific writings, 83 ; Notice of, by the Presi- dent, 73. Washington, D. C, Cyperus esculentus raised in, 337. Water, Vibrations of, falling over dams, 327, 338 ; at Hadley Falls, Charles Stodder on, 264 ; at "Nashua, 267. Water lily, Pink, 268. White Mountains, Prof. Parsons on the existence of the Sable on, 415. White-throated Sparrow, Zonotrichia albicollis. Note of, 236. Whiting, Viviparous, 9. Widgeon, European, breeding on Long Island, 419. Wind, Zonda, 126. Wisconsin, Sullivantia Ohionis from, 418. Wood, Dermestes in, 268. Woods from Surinam, 279. Wreck, Coral forty years old from, 166. Yam, Chinese, raised in Massachusetts, 335; chemical constituents of, 337. Yarmouth, N. S., Birds of, 114. Zeuglodon cetoides, deposited by C. S. Hale, 421; T. T. Bouv(5 on, 421. Zeus, ocellatus, Storer, 386. Zoarces anguillaris, peculiarity of Graaf- ian Vesicle of, 38. Zonda Wind, N. H. Bishop on, 126, 207. Zonotrichia albicollis. Note of, 236 ; grammaca, 149; savanna, 117; Pefln- sylvanica, 118. Zoology of Hayti, Dr. Weinland on, 252. ERRATA Page 11 last line but one, for Dnmascenus read Damascena. " 25 line 12, for Scolen read Scolex, " 152 " 14, " Sire(lo7i read menobranchm. " 154 " 15, " " " " " 218 " 14, " " " " " 385 last line but one, for 20th volume read 10th volume. h N^-'^ ^■^l*- ^ c.