an pea ene Banesae Vane ana OMA ; ; AANAAA Man MANY Alalalalal: eAPAAARAARAAARWAMAAY | : A A AAAAA AAA nw AAANACIAWA A ‘ AVA YIAAMAAARMAMAAMAAMANAANANYSN Rane 1M a aot 2 Oa ee £ | ‘ x % ae a aN = S i) se S BS 00 On t 7 N \ a, yn ue la WEES) Wi Bs =e 7 » Pe Aa 5 > ia “i 4 7 ore 7 ht 7) hie 0 i ys i uy i ir 7 7 a , re Ma +e i am of , } Tu i; Hl hin ; z Z ? ~ * ' if ‘ \ ‘ ¢ aint t i & A ; " ' by ral part bs ‘ Pen f a) hes i} » aj Wit i i yy 3 ‘ tals rm ; ers . : r aad » 5 a Pay : : on Pee “a Sy — ha oe - Die il 4 yy _ ANNALS OF THE Cr Me OR Naa ieee ES On ie es Bain PMC ae ah tatee na Varo f 4 } iat 3 | | To - ¢ ‘ainyae z Division at Rint viston Of Molhmsins A N N A Ty. S eC Onc? race OF THE LYCEUM OF NATURAL HISTORY OF NEW YORK. VOLUME X. NEW YORK: PUBLISHED FOR THE LYCEUM, NATURALISTS’ AGENCY, SALEM, MASS. 1874. vod ¢ 7 at |THE SALEM PRESS. F.W. PurnaM & Co., Proprietors. Bop f OPP TORS: Ob Th BLY Ce U Mt. 1873. President. JOHN S. NEWBERRY. Viee- Presidents, een Gre Be Se OpNe GE NOR YG = Mi OORT ON. Corresponding Secretary. RIOR EAR ee DREN Wr eDPIeE Recording Secretary. ROBERT H. BROWNNE. Treusurer. JOURN: GH. Hol N EON. Mi Dr Hibrarian. 1334 (Era ORE 1B, INP ID) Committee of Publication. TSESO Ss eB arAUN Dy. JOHN (Ss NEW BE DR Y: SH ON 2 da ASW REN CED ACN Tl Bis (Se NAC TEIN. H., CARRING TON, BOLT ON: cis oan eC sae Snes P Ba ah th i Al Yai ee CA) ee $i cA oii ‘Or 2 ees , q iy - Vehen b ' ta A Prats Ty ats iy reel! ¥ See or = Ik a) Lape * : ; is oak he Fi iy vA we (a ins joe > a A i ; ie ae a ; 7 { é ‘ Md @'; a il : ek shee “ teed ‘ie ale , J ta : a CT Ps b f Fi five, valdek ‘on On cay ee ioe Olengtaeh soy 3i6. CONTENTS OF THE Ee NEE Vv Ome ME BY THOMAS BLAND AND W. G. BINNEY. Notes on the Genus Pineria and on the Lingual Dentition of Pineria Viequensis, ES ipeerrcieiet ie iciatelerereictetelointelelalatalefoleialelwlotpiciclaterelatcfeluicla's/a\nlelalatelele'elacle’s hotlodaceonacnnsecas oe On the Lingual Dentition of Helix turbiniformis, Pfr., and other species of Ter- restrial Mollusca. (Plate I1.).0.......cceececceccs ccc cccscccccscccccccesccsencce On the Systematic Arrangement of North American Terrestrial Mollusks....... , On the Relations of Certain Genera of Terrestrial Mollusca of, or related to, the Sub-family Succinine, with Notes on the Lingual Dentition of Succinea ap- pendiculata, Pfr. (Plate 1X, UNINHO AN fia) epataratoielalerotelelnlatsielareteiaialets|vleleleleis/els/x(eielale(eistersisle 6 Description of Hemphillia, a new Genus of Terrestrial Mollusks. (Plate TEX®). 2. On the Lingual Dentition of Certain Terrestrial Pulmonata Foreign to the United States.....cccccsccccscnccsecee eloiatelaetacielsieloreiointelaicigrefate arele eiolieieleistalefelelelelsisieie(ate/alsiee[ein 0 On the Lingual Dentition of Gwotis. (With plate XI in part.)...+-.+-++++eee senses Note on a curious form of Lingual Dentition in Physa. (With plate XI.).......-- On Prophysaon, anew Pulmonate Mollusk, on Ariolimax, on Helix lychnuchus and other species. (With Plates XIII and XIV.)..... Gscabosonoos aratefatera Rereysiale 5 On the Lingual Dentition and Anatomy of Achatinella and other Pulmonata. (With Plates XV and XVI.)...---+-+--- platereletslalalaieiatelcleivieraialsielelale/ podacodconsactos arcobnoangEooonaadsouoKoc Descriptions of New Species of Birds of the Genera Icterus and Synallaxis...... Descriptions of Six Supposed New Species of American Birds............-...++ BY ALBERT LEEDS. SPeChroscopic MxamMIMaLilomiOf SULA LES orcleyareeiele sin clelcieis/ele\els/e\cicislereio(aiaicialeraieleieiele/s'stsisieiace BY PROFESSOR BENJAMIN N. MARTIN. Essay upon a Necessary Limitation of the Doctrine. of the Unity of the General LOE CSUO Le NAUIIN Cireletaysiatelateleteteleleleietatetelaiatevnratars mieiatetsieceiatelelcietalete inte releloleafeleteieteieietelersiersettle BY EDWARD S. MORSE. On the Tarsus and Carpus of Birds. (With Plates IV and V.).......-----...--0-- - BY A. 8. PACKARD, JR. Catalogue of the Pyralidz of California, with descriptions of new Californian EACELOP HOGG ce ratertsiateletetd alsr-tate otels a etelsiatale/stetereraisicters ie (siyieete nie obadbiovonse NOOB ARE ABPNE Notes on some Pyralide from New England, with Remarks on the Labrador SPECIES TO feu SPH aamliyete rela state etejalelsistelorereteretatelerelatelateletaiaetistataislste/. HMamophila sumichrasti. Female. The feathers of the back are pale rufous, broadly marked down their centres with dark brown, the rump is immaculate and the upper tail coverts bright rufous; the feathers of the crown have dark brown shaft-stripes, with their edges brighter rufous than those of the back, there is a narrow cinereous stripe from the bill over the centre of the crown to the hind neck; a broader stripe of ashy-white extends from the bill over the eye, along each side of the crown as far back as the central stripe; below, and bordering this, is a brownish- red postocular stripe, also one from the bill to the eye; sides of the head and of the neck, lower part of the throat and the breast, of a pale ashy color, upper part of throat and abdomen grayish-white, the latter washed with very pale rufous, flanks and under tail coverts light rufous; a short, narrow brown line extends back from the angle of the mouth, and another parallel to it down the side of the chin on each side; the two central tail feathers are of a rather bright rufous, and are crossed with dusky, nearly obsolete bars, the other tail feathers have their inner webs brownish-rufous, the outer webs colored like the central feathers, the outer feather very pale rufous; quills liver-brown, margined with dull pale rufous, smaller wing coverts deep bright rufous, the middle and greater coverts blackish-brown edged with very pale rufous; “ iris brownish-red ; upper mandible brown, the lower mandible and feet fleshy.” Length (skin) 53 in.; wing 24; tail 235 tarsi 3. Habitat. Tuchitan, Tehuantepec, Mexico. Collected by Prof. F. Sumichrast, September 8, 1868. Type in Mus. Smithsonian Institution, No. 54139. ~ Remarks. With the exception of the very different mark- ings about the head, this species in coloring much resembles my HH. melanotis ; but it is much smaller, and differs from it in there being no black on the crown or sides of the head, and in having two narrow stripes extending downwards from the bill, on each side of the throat. I found a single specimen of this species in a remarkably fine collection of birds made by Prof. F. Sumichrast, in Southwest- Mexico, Central America, and South America. 7 ern Mexico, belonging to the Smithsonian Institution, and sub- mitted to me for examination by Prof. Henry. It contains many species of much interest, but so far this is the only one I feel satisfied to describe as new. Since my determination of it as a new species, I have received a letter from Prof. Sumichrast, containing a full ‘description and an accurate drawing of the head, apparently of the same bird, which he writes he is tempted to con- sider new. It is, therefore, with much pleasure I dedicate it to him. 6 Pipilo carmani. Male. Whole upper plumage, head, throat, and upper part of the breast olivaceous brown, with a reddish cast; there is a spot of white on the centre of the throat (this last character varies in size in different individuals) ; tail blackish-brown, edged with olivaceous and crossed with almost obsolete dusky bars, the outer two feathers on each side with an irregular oval spot of white on their inner webs at the end; quills dark hair-brown, with grayish margins; the wing coverts blackish-brown, the greater and middle coverts, the scapulars and the tertiaries spotted with white at their ends; lower part of breast and middle of abdomen white, sides broadly marked with bright ferruginous, the under tail coverts pale ferruginous; upper mandible brownish-black, the under paler; tarsi and toes light fleshy- brown. Length 64 in.; wing 2%; tail 3; bill 4; tarsi 1 The female differs only in having the color of the upper plumage and that of the throat of a lighter brown; the coloring of the abdomen, and the sides are the same in both sexes. Habitat. Socorro Island, Mexico. Collected by Col. A. J. Grayson, June, 1865. Types in Mus. Smithsonian Institution, No. 50843, No. 39990. Remarks. As will be seen, this is quite a diminutive species ; its style of coloring is like that of P. erythropthalmus, P. 8 Description of New Species of Birds from arcticus, &c. It may readily be known from all others by its smaller size. Col. Grayson requested that this species might be named after his friend, Dr. B. I’. Carman, of Mazatlan, to whom he was under many obligations. With this request it gratifies me to be able to comply. Note by Col. Grayson. Tris reddish-hazel; bill black; tarsi and toes brown ; nails brown. “This is an abundant species, found in all the thickets of the Island; many of them took up their abode in our camp, picking up crumbs about our feet, as tame as domestic fowls. They de- lighted in bathing in the water we had placed in a basin on the ground for their use, and frequent combats took place between them for this privilege. It was through the agency of this species that water was discovered in a locality where we had not the remotest idea of finding it, and for this providential service he was a welcome visitor and a privileged character.” @. Attila cimmamomeus, Male. Upper plumage of a rather light reddish cinnamon, the rump and upper tail coverts pale yellowish-cinnamon, the coverts lightest in color; front, superciliary stripe and sides of the head clear light yellow, all the feathers having black shaft-stripes; the throat and breast are clear yellow, the centres of the feathers with dusky flammulations, abdomen and under tail coverts bright lemon-yellow, sides of the breast and flanks bright pale cinnamon, thighs yellow, tinged with cinnamon ; tail clear cinnamon, of a brighter color than the back; quills dark brown, the primaries edged with grayish, the secondaries with light cimmamon; the smaller wing coverts are the color of the back, the middle and larger are blackish-brown ending with cinnamon; under wing coverts bright yellow, axillaries tinged with cinnamon; bill brownish horn-color, both mandibles whitish at tip, the hook much elongated; tarsi and toes brown. Length (skin) 84 in.; wing 3; tail 33; bill 1; tarsi 1. Mexico, Central America, and South America. 9 The female differs in having grayish-white on the front, sides of the head, throat and breast, in place of the yellow of the male; the abdo- men is creamy-white, with a slight tinge of yellow on the lower part ; under tail coverts very pale yellow; under wing coverts light yellow. Habitat. Mazatlan, Mexico. Collected by Col. A: J. Gray- son. Types in Museum of Smithsonian Institute, $ No. 58231; 2 No. 58232. Lemarks. Three specimens are in Col. Grayson’s collection, two marked A. sclatert and one A. citreopygius, but I think it a very distinct species from both; its affinities are with A. e7t- reopygrus, from which it differs in its upper plumage being not at all tinged with brown, the light marking on the rump apparently more restricted, the yellow coloring below clearer and brighter, without any brown on the sides of the breast, and the under wing coverts yellow—not light cinnamon as in that species; the tail is lighter in color, not inclining to brown; the feathers overlying the pleura are brighter in color and more elongated ; it is larger than A. cttreopygius, the tail being half an inch more in length than that of the other; the bill is more slender, with the hook conspicuously longer, and much lighter in color. A. sclatert has not been found, I think, north of Costa Rica; it may be distinguished by the olive-green which prevails in its upper plumage, also on the neck and breast. 8. Todirostrum superciliaris. Crown and hind neck dark grayish-plumbeous, the front blackish ; a white stripe extends from over the eye quite forward on the bill; lores blackish; back and rump bright olive-green; tail black, mar- gined with olive-green; wing coverts black, the ends broadly marked with bright yellow; quills brownish-black, edged with bright yellow ; under wing coverts yellow ; the under-plumage is pearly-white, with the upper part of the breast light plumbeous ; a wash of pale yellow on the lower part of the abdomen and under tail coverts ; sides under the wings light olive-green ; bill black, whitish at the end; tarsi and toes pale brown. Length 3f in.; wing 2; tail 12; tarsi 3; bill 4. 10 Description of New Species of Birds from Habitat. Venezuela? Collected by Mr. Christopher Wood, of Philadelphia. Type in my collection. Leemarks. In general appearance this comes nearest to 7. schistaceiceps, Scl., but has the crown of a lighter shade; is much whiter below, the ashy coloring occupying only a small space on the upper part of the breast; the yellow markings on the wings are much broader and brighter ; the wings, tarsi and tail are longer; a very distinguishing character is the white stripe, which runs from over the eye to the nostrils, on each side of the crown, whereas 7. schistaceiceps has a white spot in front of the eye, not extending over it. 9, Elainea macilvainii. Upper plumage greenish-olive, yellowish-green on the rump; front and crown blackish-brown, with a crest of light sulphur-yellow; a line from the bill over the eye and circle round the eye grayish-white ; lores dusky; tail light umber-brown, edged with yellowish-green; the smaller wing coverts are colored like the back, the other coverts are dark brown, the middle ones ending with very pale yellow, forming a transverse band, and the larger edged with the same color; quills blackish-brown, the primaries narrowly and the secondaries rather broadly margined with pale yellow; under wing coverts light yellow ; chin and throat grayish-white, sides of the breast dusky olive-green, middle of the breast pale yellow, the feathers with ashy centres, the abdomen and under tail coverts are of a clear, rather pale yellow; bill and feet black. Length 42 in.; wing 24; tail 24; tarsi 3; bill 3. Habitat. Venezuela? Collected by Mr. Christopher Wood. Type in my collection. Remarks. This fly-catcher in coloring most resembles £. placens, Scl., but is much smaller, with the upper plumage of a darker shade; the wings and tail each measure half an inch less than those of that species; the top of the head is darker and the crest much paler; by these differences it is easily dis- tinguished. Mexico, Central America, and South America. 11 I have named this species in compliment to my friend, J. H. Mcllvain, Esq., of Philadelphia, an ethnologist as well as ornithologist, to whose liberality Mr. Wood is indebted for the opportunity to make the collection, from which I obtained this and the preceding species. Unfortunately, Mr. Wood lost a considerable portion of his collection by shipwreck. 10. Empidonmax fulvipectus. Male. The entire upper plumage is brownish-olive, the crown and lengthened crest are a little darker ; lores dusky gray ; a conspicuous circle of pale yellow around the eye; tail dark brown, the outer web of the outside feather dull white, the other feathers edged with olive ; the smaller wing coverts are the color of the back, the middle and larger are blackish-brown, ending with dull pale fulvous, forming two bars across the wing; quills blackish-brown, with olive-green margins ; under wing coverts pale tawny yellow; under plumage dull yellow, the chin grayish, the breast and upper part of the abdomen of an olivaceous brownish-fulvous, middle of abdomen light buffy yellow ; the upper mandible is brownish-black, the under pale yellow ; tarsi and toes brownish-black. Length 52 in.; wing 3; tail 22; bill 31; tarsi 2. The bill is very narrow and tapers regularly from the base, not the least bulging at the sides; the third quill is the longest, second and fourth nearly as long, first and sixth equal. Habitat. City of Mexico. Type in my collection. Remarks. This species in its peculiar coloring is somewhat like E. bairdii, Scl., but may readily be known by its more slender form, longer wings and tail, its general duller color, decided brownish breast, and slender bill, this last in E. bairdit being quite broad. The bill exceeds in length that of A. hammondi, while it is quite as narrow at the base. 11. Trogon eximius. Trogon viridis, Lawr., Ann. Lye. N. Y., Vol. vii., p. 290. Male. Crown and hind neck dark violet-blue, back of a shining 12 Description of New Species of Birds from dark green, more or less mixed with violet-blue, rump and upper tail coverts deep violet-blue; front, cheeks, chin, and throat black; breast fine vivlet-blue, connecting with the same color on the hind neck ; abdomen and under tail coverts very deep orange, sides dark grayish slate-color, thighs sooty black; two middle tail feathers green, with a decided wash of blue, the outer webs of the next two feathers are of the same color, the inner webs black—the ends of all these end nar- rowly with black, the outer three feathers are white, their concealed bases being black; wings black; the quill feathers have their bases white, the primaries are narrowly edged with white for two-thirds their length ; the upper mandible is whitish horn-color, with the base pale plumbeous, the under is dark plumbeous ; feet dark brown, the soles yellow. Mr. J. Galbraith, in his note of this species, says, “very common, light blue about the eyes, irides brown.” Length (fresh) 10} in.; wing 53; tail 6; tarsi 4. The female is of a plumbeous slate-color, grayish on the breast, the abdomen and under tail coverts orange; primaries of a rich dark brown; the wing coverts and smaller quills are black, crossed with very narrow undulating white lines, rather widely separated ; tail blackish-brown, with a purplish gloss, the three lateral feathers are white at their ends, the outer web of the outer feather is barred with white, and has a few irregular bars of the same color on the inner web, both webs of the next feather also have a few white bars. Tlabitat. Isthmus of Panama. Typés in my collection. Remarks. In my catalogue of birds from Panama, I in- cluded this species as Z. veridis, Linn.; but as it differs so materiatly from that species, I consider it to be distinct. In general coloration it somewhat resembles Z”. viridis, but is rather smaller; the back is mixed with violet-blue, and the rump is of a more intense violet-blue color; the wash of blue on the tail is more apparent, and the orange of the under parts is of a deeper shade; but the most distinguishing character is that of the outer tail feathers, which have a much greater ex- tent of white on their terminal portions, when the tail is closed, the under side appears entirely white, the black bases being Mexico, Central America, and South America. 13 quite concealed, whereas in 7. vridis the ends of the feathers only are white, the black basal portions showing conspicuously. Specimens referred to 7. venustus, Cab., by Mr. Cassin, are in Prof. Orton’s collection, from Archidona, Ecuador; they agree quite well with Cabanis’ description, except in being of the same size as 7. viridis, not ‘somewhat smaller,” and that the abdomen is deep orange; he says, “belly yellowish-orange ;” in deseribing 7. viridis, he has, “belly orange,’ but this is perhaps a variable character. Compared with examples of Z. viridis from Bahia, Prof. Orton’s specimens are more of an azure instead of violet-blue, the upper plumage more golden, the rump less violet, being mixed with green; the middle tail feathers are green, without any shading of blue, and the abdomen and under tail coverts of a deeper orange; in the extent of white on the end of the tail feathers, they agree with 7. viridis. These comparative differences with 7. viridis are very simi- lar to those pointed out by Dr. Cabanis; as he makes no allu- sion to the ending of the outer tail feathers, I infer they are the same in both. Specimens exactly corresponding with those from Archidona are in collections received by Prof. Orton from Mr. J. Haux- well, at Pebas on the Upper Amazon; also, I have an example from Bogota. The new species differs from the specimens above spoken of as 7’. venustus, in the head and breast being of a deeper blue, the rump intensely violet instead of greenish ; the middle tail feathers, instead of being green, are more blue even than those of 7. viridis; the greater extent of white on the outer tail feathers distinguishes it from this as well as from Z”. viridis ; the orange coloring below is of a deeper color than in either T. venustus or T. viridis. 12. Chiorostilbon caribzeus. Male. Crown of a glittering pale golden-green, upper plumage and wing coverts grass-green, somewhat golden; the entire under-plumage 14 Description of New Species of Birds from is of a brilliant uniform emerald-green, with a few white feathers on the flanks; tail steel-blue; wings brownish-purple; bill black; feet dark brown. Length about 34 in.; wing 12; tail 145 bill 2. FTabitat. Island of Curagao. Type in my collection. Remarks. Its nearest ally appears to be C. atala, but that species is entirely of a golden-green; the new species is only slightly golden above, not the least so in its under-plumage, where it is of a much darker shade of green, and more glitter- ing; the tail is strikingly larger and the feathers broader, the color of which is more blue, that of C. atala being more of a steel-black; the wings are longer, and the bill appears to be stouter than in that species. Three specimens were presented to me by my friend, Mr. T. Bland; he obtained them from Mr. Henry H. Raven, who brought them from the Island of Curagao. ‘I'wo of the speci- mens are immature males. 13. Conurus holochlorus var. brevipes, Baird, M.S. Male. The general plumage is grass-green; the abdomen is lighter and has a yellowish cast; ends and inner margins of quills biackish; inside of quills and under-surface of the tail dull yellowish; bill yellowish-white ; feet light yellow. There is no difference in the plumage of the sexes. Length (fresh) 124 in.; wing 62; tail 64; tarsi 3. Habitat. Socorro Island, Mexico. Collected by Col. A. J. Grayson, “Spring of 1865.” Type in Mus. Smithsonian Insti- tution, No. 39971. Remarks. Six specimens before me, compared with two ex- amples of C. holochlorus from Salvador, have the toes uniformly shorter; the wings of the Socorro Island bird are half an inch shorter than in. those from Salvador; in plumage there is no perceptible difference in the two forms. Mexico, Central America, and South America. ab) The toes of the two forms measure as follows :— C. holochlorus—Outer toe 13; middle 1$; inner 2; hind C. brevipes— ce $; af 7a eat Color cleo 1ofe . 6s p) Note by Col. Grayson. “Socorro Parrot. Iris reddish-brown ; bill yellowish-white, dark or black at point ; feet pale yellow, with brownish scutelle ; nails dark brown. Contents of the stomach, kernels of nuts. “This Parakeet is quite abundant and evidently belonging to this locality, which it never leaves ; they are to be met with in flocks or in pairs. In the mornings they left the cove in which we were encamped, for the higher regions of the interior, to feed, returning again in the evening to roost; this cove, in which the trees are larger and the shade more dense than in other parts of the Island, seems to be their favorite resort. J saw them at times walking about on the ground beneath these trees, apparently picking up clay or gravel. They are remarkably tame, exhibiting no fear in our presence; three cages were soon filled with them, which were caught by hand, and their con- stant whistling for their mates brought many of them into camp, perching upon the cages and elsewhere. They feed upon a hard nut which they find in the mountain-gorges, and on ac- count of the inaccessible localities where this fruit grew, I was unable to find it; the powerful jaws of this Parakeet would indicate the fruit to be very hard.” 14. Leptoptila bonapartii. Male. Above of a light brownish-olive, a little browner on the wings and more olivaceous on the lower back and upper tail coverts, hind neck grayish, with a bluish tinge; front whitish, with a slight roseate tint, crown plumbeous-blue, grayish on the forward part and darker towards the occiput; throat white, sides of the head light brownish-vinaceous, this color extending somewhat on the hind neck ; breast and upper part of abdomen of a pale roseate color, lower part of abdomen and under tail coverts white, sides under the wings light 16 Description of New Species of Birds from cinnamon-brown ; four middle tail feathers colored like the back, the others purplish-black, terminating in white; under wing coverts dark bright cinnamon; the inner webs of the primaries light cinnamon, the larger quills are of a fine dark brown, the exposed portions of the others colored like the back ; bill black; feet yellow. Length 103 in.; wing 59; tail 4; bill 14; tarsi 1,3. Habitat. Mexico (A. Sallé). Type in Mus. Smithsonian Institution, No. 29693. Remarks. This specimen was received from Mr. Sallé and labelled by him ‘ Z. albifrons, Bp.;” the reverse side of the lable is marked “ ¢ P. V. Juin, ’59.” It no doubt was super- vised by Bonaparte, as Salle’s birds mostly were; it is very distinct from the species, which is now admitted to be entitled to bear that name, viz., the bird for some time known as JZ. brachyptera, Gray. I found this specimen in the collection of the Smithsonian Institution (where there are numerous specimens of the true L. albifrons) about two years ago, and hesitated to describe it as new, fearing to add to the confusion attached to the name of albifrons. In general coloration it somewhat resembles that species, which differs in being of a lighter olive above and more roseate on the breast, it has a much longer tail, with no plumbeous on the crown, and may be known from all its allies by the inner webs of the primaries being just edged with pale cinnamon. L. plumbeiceps, Scl. & Salv. (P. Z. 8., 1868, p. 59), differs in being dark brown above, in having the plumage of the breast somewhat darker, and the under-lining of the wings of a more intense color; in the new bird the plumbeous is confined to the crown, and does not extend on the hind neck, as in Z. plumbeiceps. It really comes nearest to LZ. rufaxilla, from South America, in general coloration, but that species has the breast more roseate, the blue of the head lighter and more restricted, the sides of the head cinnamon color, and the feet smaller. Mexico, Central America, and South America. 17 Under the circumstances I consider the name conferred a very appropriate one. 15. Zenaidura graysoni, Baird, M.S. Male. Entire plumage above olivaceous-brown, with a rufescent tinge, the crown of a darker brown; front, sides of the head, and the whole under-plumage dark cinnamon red, except the chin, which is paler; auricular spot black, but not very distinct; the sides under the wings grayish-plumbeous; the two central tail feathers are of the same color as the back, with their centres blackish-plumbeous; the next feather on each side has the outer web and end colored like the back, with a rather indistinct subterminal black bar on the inner web, below which the inner web is dark plumbeous, the next pair on each side are grayish-plumbeous, the outer webs broadly margined and tipped with brown, and having the subterminal black bar more distinct, the next two on each side of a light plumbeous-gray, just margined with brown on the outer webs, and with the black bars still darker, the outer feather has its end and the outer web pale bluish- white, the inner web dark plumbeous, the black spot mostly contined to the inner web; the tail feathers underneath are brownish-black, except the outer web of the lateral one, the end of which and those of the next two are light plumbeous, the ends of the others becoming darker towards the central ones, and more or less tinged with brown; primary and secondary quills blackish-brown, the outer primaries just edged with white; wing coverts and tertiaries of a rather lighter reddish-brown than the back, and marked with oval black spots, most conspicuous on the tertiaries; under wing coverts grayish- plumbeous; bill dark brown, base of under mandible yellowish; feet reddish. Length (fresh) 12 in.; wing 53; tail 5; bill 12; tarsi 1. Habitat. Socorro Island, Mexico. Collected by Col. A. J. Grayson. Type in Museum Smithsonian Institution, No. 50855, There is no difference in the plumage of the sexes. Three specimens are in the collection, one of which is rather more oli- vaceous on the back; otherwise all are alike. FEBRUARY, 1871. 2 Ann, Lyc. Nat. HisT., Vou. X. 18 " Description of New Species of Birds from The tail consists of fourteen feathers, as in the two others of the genus; the shape of the tail is like that of Z. yucatanen- sis, the feathers not pointed as in Z. carolinensis. Remarks. It bears no resemblance to Z. carolinensis ; com- pared with Z. yucatanensis, they are somewhat alike in color- ing below, but in Z. graysoni the color is more uniform and much darker; it differs from both species in the absence of metallic coloring on the neck. Note and observations by Col. Grayson. “ The Solitary Dove. Iris dark brown; bill dark brown, with a slight tinge of red; base of under mandible reddish- purple, as also the base of the gape; tarsi and toes reddish flesh-color, posterior portion of which is paler, nails brown- ish-black; bare space extending from base of bill to and around the eye plumbeous; second and third primary quills longest; tail graduated, with fourteen feathers, outer ones 14 inches shorter than the central. Not abundant. “Of all the birds I met with in the Island, this seemed to be the most lonely; not a flock or even a pair were ever seen together. They are remarkably tame, perhaps more so than any bird of this order; one was captured by hand as it came into our camp, and perched upon the rude table on which I was at work. Its melancholy look appeared to be in keeping with the solitude of, and its sombre plumage corresponding with the gray brush and brown voleanic rock composing its wild home. In form and appearance, when alive, it resembles the common Turtle Dove. “The first specimen seen and captured was by my son, Edward Grayson, whose name this evidently new species should bear—not for this discovery alone, but for the as- sistance often rendered, in making my collections, and more particularly on this expedition, in which he was indefatigable, even to enthusiasm, in aiding its progress, as well as the advancement of science, in the cause of which he came to an untimely death!” Mexico, Central America, and Svuth America. i) 16. Note on fallus longirostris, Boddaert. I received a specimen of /ea/lus in a collection from Bahia, which I was unable to determine and was inclined to consider undescribed; from the stoutness of its bill, I named it pro- visionally 2. crassirostris. In 1868 Messrs. Sclater and Salvin gave a most valuable and complete ‘Synopsis of the American Rails” (Proc. Zool. Soe., p. 442). Not being able to make it agree satisfactorily with any of the species therein enumerated, and an opportunity offering to send it to them, as they had lately so fully investigated the Rallide, I did so. On returning it, Mr. Sclater wrote, “is true dongirostris, figured Pl. En]. 849.” I infer from this (although not dis- tinctly so stated) that they consider it different from erepitans ; the two birds are very unlike, and no one with the two before him could confound them. If right in my inference, this would be a change of opinion since the publication of the Synopsis, wherein crepitans is put as a synonym of longirostris 5 this view has also been taken by other recent writers, adopting Mr, Cassin’s suggestion of their probable identity. I find it agrees with Buffon’s plate (which is of reduced size) in the apparent color of the back, also in the form and stout- ness of the bill; but they differ in the coloring below, which in the plate is more like ecrepitans, being of an ashy-fulvous, instead of uniform light rufous; they differ also in the bars on the flanks. The only characters, then, on which it can assume the name of dongirostris, are the shape of the bill and the color of the back, if these are deemed sufticient to overrule the coloring below, in which the plate resembles crepitans. My specimen differed so much from crepitans, as well as from all others, that I considered it undescribed at the time, taking for a settled fact that crepitans and longirostris were the same; if the Bahia bird is to take the name of longtrostris, it being certainly distinct from ecrepitans, the latter name must be restored to full specific rank. 20 Description of New Species of Birds from The bird from Bahia is grayish-olive above, flammulated with blackish-brown ; the under-plumage is light rufous, the throat white ; a stripe of dull rufous extends from over the eye to the bill; the sides and under wing coverts are brown, with transverse narrow white bars; the upper mandible is brown on the ridge and at the end, the remaining part and the lower mandible dark yellow; feet yellow. Length 12 in.; wing 54; tail 24; bill 24 to rictus; tarsi 13. It is smaller in all its measurements than erepitans, and has the bill fully twice as deep as in that species, the tarsi are shorter, the feathers of the back are bordered with grayish- olive instead of light bluish-cinereous, and the color below of a clear light rufous instead of an ashy-fulvous; the colors are more like those of /2. eleyans, but are lighter; its smaller size, shorter and stouter bill, distinguishes it also from that species. The description of R. dongirostris in Messrs. Sclater and Salvin’s Synopsis is evidently taken from United States speci- mens of erepitans. I have seen no description at all applicable to my Bahia specimen, and if the evidence is not considered sufficient for it to assume the name of dongirostris, it may then bear that of crassirostris. The new species of Vireo, described below, is added to my paper by request of Professor Baird. The description and remarks are his, without alteration by me. Vireosyivia magister, Barr, n. s. Habitat. Belize, Br. Honduras. Bill stout and lengthened. Wings considerably longer than the nearly even, though rather short and decidedly rounded tail; the Ist quill about equal to the 6th, or very little longer; the 3d longest ; the 2d and 4th a little shorter. No spurious primary. Upper parts olive-green, brightest on rump and tail; the head above, and to a less degree the back, with a slight gloss of ashy, but without forming acap. Beneath dull olivaceous-white, the belly (and Mexico, Central America, and South America. 21 the tibiz somewhat) rather buffy yellow; the sides of neck and body olivaceous. Axillars and inner wing coverts sulphur yellow; the crissum similarly colored, but duller. Quills almost black, edged internally with grayish-white, externally with olive; tail feathers more olive-brown, edged internally with greenish-yellow, externally with bright olive. A broad stripe of pale yeilowish from bill over and behind eye to nape, becoming paler when it reaches the eye, and with a faint indication of a dusky border above it; a dusky brown, well-marked stripe from bill to eye, and a small spot of the same behind it. The bill is almost black, except the basal half of lower mandible, which appears to have been nearly white. The legs are blackish-plumbeous. “ Iris brown” ( Wood) ? Total length, 6.00; wing, 3.00; tail, 2.50; difference between 9th and longest quills, .60; exposed portion of Ist primary, 1.90, of 2d, 2.15, of longest (measured from exposed base of Ist primary), 2.24 ; length of bill from forehead, .80, from nostril, .46, along gape, .90 ; tarsus, .83; middie toe and claw, .70, claw alone, .24; hind toe and claw, .56, claw alone, .27. This interesting new species of Vzreo is among the largest of the genus, considerably exceeding in size V. olivacea, and fully equal to V. calidris of Jamaica. In general appearance it closely resembles the latter, but there is even less of the grayish cap, and the dusky mandibular stripe is wanting; the under parts are rather more olivaceous ; the bill is of about the same size. The much rounded wings constitute an important char- acter of the species. The much larger size, almost black bill and feet, absence of ashy cap, more olivaceous under-parts, will readily distinguish the species from V. olivacea. The wings, also, are much more rounded ; the first quill about equal to the sixth, instead of being but little shorter than the fourth. The wing formula is much the same as that of V. agilis, but the size and coloration are very different. This species is one of several new species of birds in a col- lection made at Belize, British Honduras, for Dr. Henry Bryant, by Mr. Christopher Wood. 22 Notes on the Genus Pineria, and on the IL.—Wotes on the genus Pinerta, and on the lingual dentition of Pixerta Virquensis, Pfeifer. By Tuomas Branp anp W. G. Binney. Read March 20, 1871. Tue genus Pineria was established by Poey in 1854 (Me- morias, I., 428), and thus characterized :-— T. bulimiformis, imperforata, turrita, apertura rotundata, peris- toma simplex, rectum, undique acutum. Animal nudipes tentaculis duobus retractilibus instructum, apice oculatis ; labrum rotundatum ; reptatio sinuosa. Poey described two species, P. terebra and Beathiana, both from the Isle of Pines, of which figures are given (Jlemorias, lL. c., tab. 34, f. 12-18). He remarks that he had examined the living animal of P. Beathiana with great care, but could detect no trace of “ in- ferior tentacles,” and Dr. Gundlach had satisfied himself of their absence in 1. terebra. Observing that the form of shell (columella excepted) and sculpture of the former species was somewhat like that of Macroceramus turricula, Pfr., Poey studied its soft parts and found such tentacles existing. In 1856 Pfeiffer (Malak. 51. IL. p. 46) described Bulimus Viequensis, from Viéque, and suggested its alliance with Pineria. The species is figuredin Wotit. Conch. Fasc. xxxi. t. 93, f. 39-41. The late Rev. H. Parkinson, in 1857, discovered P. Viequen- sis in Barbados. In 1858 Fischer (Jowrn. Conch. vii. 184, t. 7, f. 7-8) described Helix Schrammi, from Guadaloupe. Pfeiffer (J/on. vi. 343) adopts the genus Pneria, for B. Viequensis, H. Schrammi, and Poey’s two species, and re- marking on the evident affinity of Fischer’s species with Vee- Lingual Dentition of Pineria Viequensis, Pfeiffer. 23 quensis, asks whether both should not be transferred to Macro- ceramus. . H. and A. Adams (en. ii. 163) place Poey’s species in Maero- ceramus, While Pineria is adopted by v. Martens (Albers, 2d, ed) as a subgenus of Pupa. We have compared specimens of J/elix Schrammi, received from M. Crosse, Pineria Viequensis from Barbados, and also of P. Schrammé trom Anguilla, St. Martin, and St. Bartholomew, and are satisfied that all are of one and the same species, which, by priority, is entitled to the specific name, Viequensis. We obtained the jaw and odontophore from a dead specimen of this species, collected at the east end of St. Martin, by Dr. van Rijgersma, for which we are indebted to Mr. Robert Swift, but no living example has at present been received to enable us to form an opinion as to the presence or absence of the “ in- ferior tentacles.” With respect to the alleged absence of those organs in Pineria, the following is a copy of a note by Poey, published in 1865, with a Catalogue of the Terrestrial and Fluviatile Mollusks of Cuba by Arango (/epertorvo, I. 145); “ En las altas regiones de la filosofia natural, tendran probablemente razon los que suprimen mi género Pineria, el cual he separado de los Macrocéramos por la razon, de que el animal no muestra ni vestigios de tentaculos inferiores. Los principios formolégicos nos obligan 4 considerar que existen virtualmente; por lo que no me opongo 4 que se suprima.” Before the commencement of the late Earopean war, we sent to M. Crosse, unfortunately without previous examination, the odontophore from a dead specimen of P. terebra, as to which we hope to have a report at no distant day. It will be seen from what has been stated above, that an opinion has been generally entertained in favor of placing the species of Pneria in the genus Macroceramus. Crosse and Fischer, in a late interesting paper (Journ. de Conch, xviii. 1, Jan. 1870) fully discussed the lingual dentition 24 Notes on the Genus Pineria, and on the of various groups of Cylindrella and Macroceramus, and con- sider that they constitute a natural family, characterized by the presence, Ist, of a jaw of extreme thinness, and with folds chevroned on the median line; and 2d, of lateral teeth, more or less palm-leaf shaped, disposed in very oblique rows, which family they designate as Cylindrellide. The authors proposed the following classification :— FAMILY CYLINDRELLID 4. 1. Group A. CYLINpRELLA (sensu stricto). Two lateral teeth on either side of the rachidian tooth; mar- ginal teeth of a very different form, varying in number, according to the species. This group comprises the sections Apoma, Beck, or Casta, Albers (including the sinistral species, C. gracilis, Wood, C. elongata, Chemn., C. Agnesiana, C. B. Ad.); Trachelia (C. Brooksiana, Gundl, &c.), and Mychostoma, Albers (C. costata, Guilding, C. Bahamensis, Pfr. &e.). 2. Group B. Cattonta, Crossk AND FiscHEr. Rachidian tooth with a very long cusp; lateral teeth more than two; marginal teeth arranged obliquely in a continuous line with the laterals, and not distinctly characterized. Only one species known, C. /liotte. 3. Group C. THaumasia, ALBERS (partim), Lateral teeth more than two; marginal teeth similar to the laterals, and not to be distinguished from them. This group includes the large species of Jamaica and Hayti, and some of those of Cuba, but none of the species of Hucalo- diune. 4. Group D. Lia, Arsers (emend.) Lateral teeth very numerous; marginal teeth of the same type as the lateral teeth, and not to be distinguished from Lingual Dentition of Pineria Viequensis, Pfeiffer. 25 them ; inner cusp simple and pointed, instead of semi-circular, as in the preceding groups. This group includes L. Maugeri, Wood, zebrina, Blandiana, macrostoma, Paivana, flexuosa, Gossei, and tricolor, all of Ja- maica, and L. virginea of Hayti. 5. Grourp E. Macroceramus, Guinprna. Lateral teeth very numerous, as in the preceding group; marginal teeth of the same type also ; two inner cusps. This includes forty-eight species, of which only four are found on the continent of America; the balance belong to the Antilles, particularly to Cuba, which alone has thirty-four. The other species formerly referred to the genus Cylindrella, are placed by Crosse and Fischer in the genera Hucalodium, Berendtia and FHolospira, of the family Helicide ; their lin- gual membranes resembling those prevailing in that family. The limits of the present paper preclude our entering further on this part of the subject. The authors remark that the three above-named genera of flelicide are localized in a relatively small portion of the American continent (Texas, Lower California, Mexico, and Guatemala), where there are very few representatives of Cylin- drella proper, while the family Cylindreilidw is largely de- veloped in the Antilles (Cuba, Jamaica, and Hayti especially), with an entire absence of the Cylindrelliform genera belonging to [elicide. From the subjoined descriptions of the jaw and lingual denti- tion of Pineria Viequensis, it will be seen that it belongs to the family Cylindrellide as restricted by Crosse and Fischer. If form of shell be considered, the species may be placed in the above-mentioned group E (d/acroceramus), but from the char- acter of the dentition it is rather a member of group A (Cylin- drella). ‘The resemblance of the dentition of P. Viequensis to that of Cylindrella Trinitaria, Pf. (Amer. Jour. of Oonch., iv., 187) is very striking. 26 Notes on the Genus Pineria. An examination of the lingual teeth of the various forms of Macroceramus, and of Pineria from the Isle of Pines, is ex- tremely desirable, and also of the soft parts of the latter, in order to settle the question raised by Poey as to the tentacles. In the meanwhile we continue to use the generic name Pineria. The following is a description of the jaw and lingual denti- tion of P. Viequensis : Jaw so extremely thin and delicate that it curls or folds over upon itself along the edges, and at the extremities ; pale horn-color, translu- cent ; strongly arched, subcircular; of nearly equal height throughout, the ends slightly attenuated and blunt; entire, but with the appear- ance of being divided perpendicularly into about twenty-eight sepa- rate sections or folds, the outer margin of each defined by a thicken- ing of the substance of the jaw; the sections curve strongly out- wards, excepting at the upper centre of the jaw, where they are arranged en chevron upon the central line; either margin serrated by the extreme outer edges of the sections or folds ; generally resembling the jaws of Macroceramus and Cylindrella* as figured in Ann. Lye. vill. 162.3; Am. Jour. Conch. iv. 187, v. pl. xi.3; Journ. de Conch. xviii. 1, pl. iii. and v., Jan. 1870. Lingual membrane very long and narrow, composed of numerous rows of teeth arranged obliquely from below upwards en chevron ; teeth arranged in quincunx 2. 1. 2 in eachrow, with several additional rudimentary marginal teeth; central teeth small, long, slender, crowded between the first laterals, its apex recurved into a rounded cusp ; first lateral broad, bicuspid, base of attachment subquadrate, lower cusp very large, broader than the base, subcircular, upper cusp very small, seated on a long, slender neck, which curves gracefully outward and upward beyond the apex of the central tooth; second lateral of the same shape as the first lateral ; marginal teeth five or six, arranged in a crowded row running obliquely upward and outward from near the base of the outer lateral, decreasing rapidly in length * Crosse and Fischer, in their description of the jaw of Cylindrella, remark that it is furnished with very fine ribs, which are shown under the microscope to be nothing less than a complete folding of the substance of the jaw. Genres des Poissons. QT as they pass outward, long, narrow, simple, with irregularly curved apices. On some portions of the lingual membrane the cusp of both central and lateral teeth are much more produced than on others, the lower cusp being quite spoon-shaped. With respect to the habits of Cylindrella and Macroceramus, we are indebted to Mr. C. P. Gloyne, of Jamaica, for the infor- mation that they feed on lichens growing on walls and rocks— he has found their stomachs and intestinal canals filled with such matter. He also remarks that the sinistral species (C. gracilis, etc.) appear to be viviparous, as he had frequently found four or five young shells, with several whorls, within living adults, but that while he had never detected eggs, he had not seen such embryo shells in the group to which C. sanguinea, etc., belong (Zhaumasia, Cr. and Fisch.). Il.— Genres des Poissons dela Faune de Cuba, appartenant a la Kamille Percipm, avec une Note @introduction par J. Carson Brevoort. By FELIPE POEY. Read March “th, 1871. INTRODUCTORY NOTE, [The difficulty in establishing a permanent generic group of animals defined by truly natural characters, is well known to naturalists, and to those more especially, who, as in the case with fishes, have to study preserved, and therefore shrunken and faded specimens. The want of a complete series of all the species and varieties, taken at all seasons and at all ages, and in both sexes, together with accurate data concerning their habits, geographical range, rarity of occurrence and appearance when fresh, causes insuperable difficulties in properly 28 Genres des Poissons defining the genera and characterizing the species. On this account we take especial pleasure in presenting the following paper by our esteemed corresponding member, Professor Poey, of Havana, on the great group which stands at the head of the Order of Fishes, the perplexing characters of which he has sought to more clearly define and describe. Well known as a careful observer and able anatomist, he is also a diligent and indefatigable collector of specimens and of information, qualities rarely found combined in the older naturalists. He has sought to become thoroughly acquainted with the entire Fauna of the tropical island which he inhabits, and his studies have thus a peculiar and abiding value. Hxamining, as in the case before us, specimens of every age and at all seasons, he learns their habits and native characteristics, so as to surely fix the species and mark the genus. His generic descriptions in the following paper are so thorough, that they can hardly be disputed or misunderstood. His bibliographical knowledge withal is most extensive, enabling him to present the history of each genus and criticise the labors of his pre- decessors. The paper is published as it was received, for were a translation of it to be attempted, the sense might be slightly altered, and the true meaning of the author be lost. J.C. B.] CLASSIS PISCIUM. Les Poissons sont des animaux vertébrés ovipares, a circula- tion double et compléte, & respiration bronchiale, et par con- séquent incomplete, ce qui fait baisser la température du sang. Le cceur est veineux, 4 deux cavités, s¢paré du sinus aortique. La plupart ont le corps couvert d’écailles. La locomotion s’éffectue par le moyen des nageoires, prin- cipalement par la caudale, Les nageoires pectorales représen- tent les membres thoraciques, et les ventrales les abdominaux. Oes nageoires sont soutenues par des rayons, tantot épineux, tantot mous, articulés, et le plus souvent branchus. Les dents sont implantées sur les machoires. Il peut y en avoir encore att vomer, aux palatins, aux ptérygoidiens in- ternes, sur Ja langue et sur les os pharyngiens; les ares branchiaux sont hérissés de tubercules épineux, de la Faune de Cuba. 29 Los hyoide est trés-compliqué: il soutient la membrane branchiostége, pourvue de rayons, placée sous les os opercu- laires, et formant avee ces derniers ’ouverture des ouies. Les narines Wont pas de communication avec Varriére- bouche. Pei a wn cristallin globuleux et trés-dur: il manque Vhumeur aqueuse. Poreitle est réduite & un sac qui représente le vestibule, et aux canaux semi-circulaires: on y trouve des otolithes. Les vertebres sunissent par des surfaces concaves: elles se divisent en abdominales et caudales. Les os de la téte, com- parés a ceux de Vhomme, se divisent presque toujours en plusieurs pieces, qui répondent aux points d’ossification des derniers. Les parties ordinaires dw cerveaw sont placdes & la suite les unes des autres. Le pylore est presque toujours entouré de coecums, qui remplacent le paneréas. Les reins sont fixés le long de l’épine. Les testicules et Jes ovaires sont doubles ; les premiers prennent le nom de laites. Presque tous les poissons osseux ont une vessie aérienne, dont toutes les fonctions ne sont pas bien connues, mais qui est pourvue d’une mem- brane musculaire, pour diminuer, au besoin, le volume du corps dans l’acte de la natation. La plupart des poissons n’ont pas d’accouplement. Ce qui vient d’étre dit présente quelques exceptions ou modifications chez les chondroptérygiens, qui, Vossification a part, sont supérieurs dans la série animale. (’) 1 Dans les divisions qui viennent 4 la suite du tableau ci-joint, j’ai souvent profité des travaux de Mr. Gill. J’ai consulté aussi, entr’autres matériaux, Varticle de J. Miiller, inséré dans Wiegmann’s Archiy. I., p. 292. Quant aux caractéres génériques, il faut avouer que les auteurs les plus renommés n’en ont employé qu’un nombre bien borné, et en ont négligé plusieurs de premiére importance. Ce reproche ne s’adresse pas 4 Mr. Gill, qui a donné l’exemple de diagnoses génériques plus étendues: c’est sous cette impulsion que je présente les miennes.—Quant & la nomenclature des os, j’ai adopté celle de Mr. Richard Owen. 30 Genres des Poissons CLASSIFICATIO PISCIUM VIVENTIUM ex Artedi, Linné, Cuvier, Agassiz, Miller, Owen, Bonaparte, C. Duméril, Bleeker, Gill, Poey. Subciassis. Sectio. Ordo. ~ Subordo. Series. Familie, v. ¢. =j { choripharyngodon- { thoracici. .. .Percide. w | Acanthopteri, Art. Tes BIER os s:o ss abdominales. Sphyrzenide. ie 1 amphipharyngodontes,P......... Malacanthidi. a f ee ( ctenoidei .. .Pomacentridi. a pe dae Sle a acanthopterygii... 1 cycloidei... . Scaridi. 2 4 : malacopteryeiis st i... AAA eh Scombresocidi. : : thoracici...Gobidi. 3 ; Gobiosomi, -P {-... | jugulares ,. Blennidi. Teleostei, M....4 1 | Subacanthopteri, P..4 Pediculati,l..................-- Lophidi. H Woe ulatio Mls minaret ameter Gadidi. Heterosomiiy Dir. cnet 213 wsteciaaiete Pleuronectidi. (ivestacapeerte’ Art. Abdominales, C Cyprinidi. rH INTO Wie nog dupopaousnoonsaconpecuuatacde Murzenidee. Q. nell pNematopnatiniy Gill eyem Rare ciccu teatieihelere see Sic ee race Siluridi. Sey A : WrryanOCON bse Cinsrsrtclele tciteeiee recite Diodontidi, ce Plectognathi, C..... ) Sclerodermi, C........s0.sc00ce. Balistidi. OD" |Meophobranchiiy© vem ii iclectere cieloisisictecine nit sieleyateietorectoeie ite Hippocampidi. bia OLE Stele Ms arc mm ielsreep ieee vidj ta; «ole ge olevarereimrsi> scereteaelsi axele sas Lepidosteidi. SOE Bho oc os { (CHOBATOSLSIN IM syectajate tafe teleleLelolelelcfetarelnls/slelofale/areveiayaicistaye eters Acipenseridi. ETOLODECETS FO waa as cierto taraiays ocls eicsotateican: esiatene Ratatek taepnvatelaiapeiesatelolsies oie Eis lo afoastelejeisveinints Lepidosirenidz. J Placiost D (PElenrobrerniy De s./ ao) *jae clots = Squalidi. Elasmobranchii, Bon... Ese Rest gan goot eb puree ION Con sPonocoadescde Rajidee. Aolocephalli, (MEST LIAT . Anes edd tae etotiben A bleis)< tet bet bere Chimeridze 3 EDV erOAT DS Meat ctatelelelasierelsiote oi Petromyzontidi, Dermopteri, Ow....... Cyclostomt, Doo. +0. l Hyperotreti, Mi soc citsisia beer: Myxinide. Men Locardliiliicr 1c sevacistacic einer tsisdsicleraciciatsicleicicerace coeie Amphioxidi. 1. Les Sympharyngodontes de Bleeker sont les Pharynyognathi de Miiller. 2. Miller place la famille des Chromides parmi les Pharyngognathes ; cependant, le Nandopsis tetracanthus de Cuba, a les os pharyngiens inférieurs unis seulement en apparence; car ils se séparent avec un léger effort. 3. Je n’ai pas nommé avec Miller Anacanthini mon ordre des Subacanthopteri, parceque Vauteur limite cette dénomination aux Gadidi, Pleuronectidi, Ophididi. 4, Je ne me suis pas occupé des Leptocephali de Bonaparte, ou Lemniscati de Kaup, parcequ’on ignore encore si ce sont des poissons adultes, ou des embryons. SUBCLASSIS I.—TELEOSTEI. Le nom de cette sous-classe est di & Miiller en 1845 ; il fait allu- sion a Vossification plus ou moins parfaite du sqiteletta! Elle répond aux poissons osseux de Cuvier, sauf les Lépidostéides. Branchies libres sur leur contour; ouverture branchiale simple de chaque cote, et placée au-devant des pectorales. Nerfs optiques croisés ; deux valvules opposées 4 entrée du bulbe aortique. Corps écailleux; les écailles sont ctenoides ou cycloides. de la Faune de Cuba. 31 Sectio 1.—TELEOCEPHALI. Le nom indique que la téte est parfaite. Cette coupe était nécessaire, etsa dénomination est due a Mr. Gill, qui l’a appliquée i un ordre. Elle embrasse les Acanthoptérygiens de Cuvier, ainsi que ses Malacoptérygiens abdominaux et subbrachiens, ex- cepté les Silurides. Les maxillaires et les prémaxillaires existent séparément, ainsi que les sous-orbitaires; l’os sous-operculaire existe, sauf chez les Notoptérides. Branchies pectinces. Ordo 1.—ACANTHOPTERI. Une partie des rayons dorsaux et quelques-uns de l’anale sont épineux, simples, non-articulés, ainsi que le premier de la ventrale. Ares branchiaux au nombre de quatre, portant les branchies entiéres, 4 double lame suivies d’une fissure, et ordi- nairement une fausse-branchie. Des appendices pyloriques 4 la branche montante de V’estomac. Vessie atrienne sans conduit pheumatique. Subordo 1.—CHoriPHARYNGODONTES. Os pharyngiens inféricurs sépares. Serves 1,—THoracict. Os pelvien en relation avec l’arcade scapulaire: ventrales tho- raciques. ' Familia 1.—Prrcw a. Corps plus on moins allongé; anus arrieré. Ventrales 1, 5. Sept rayons aux branchies; ouverture branchiale bien fendue ; la fausse-branchie existe, excepté dans les genres Lates et (’ni- 32 Genres des Poissons don. Quelques pieces operculaires épineuses on a bords dente- lés, excepté chez les Apsiles. Yeux latéraux ; overtures nasales doubles de chaque cété, ’antérieure a bord tubulaire, la posté- rieure simple. Bouche fendue a lextrémité du museau; ré- gime carnivore; machoires plus ou moins protractiles. Dents en velours, le plus souvent accompagnées dun rang externe de dents pointues, plus fortes et solides, avec ou sans canines. Dents au vomer et aux palatins. Une ou deux dorsales, avec ou sans sillon sur le dos, pour loger les rayons épineux; la par- tie molle moins étendue que la partie épineuse ; rayons mous branchus. eailles cténoides: ligne latérale continue, finis- sant sur la base de la caudale. Joues non-cuirassces. Le conduit osseux semi-circulaire latéral de lVouié com- mence sur Valisphénoide, pénctre dans le mastoidien, et revient par Vexoccipital, aprés avoir traversé ces trois os; le conduit vertical postérieur traverse l’exoccipital, pénetre dans le parocci- pital, et termine par une ouverture supérieure de ce dernier. C’est ce qui arrive chez les adultes; car dans les jeunes le canal membraneux latéral entre et sort par le mastoidien, par des ou- vertures rendues complétes au moyen d’une échanerure de !’alis- phénoide et de Vexoceipital ; Pautre pénétre par une échancrure de Vexoccipital. Le pectoral osseux et tout-a-fait superficiel, n’entre pas dans la formation de la capsule auditive. La premiere névrapophyse chevauche, c’est-a-dire quelle est mobile sur la premicre vertebre abdominale. Vertebres 10—14. Surtemporaux au nombre de deux. Ap- pendices pyloriques généralement peu nombreux; intestins a deux replis, sauf quelques légéres modifications. Vessie aéri- enne simple. Observations.—Cette coupe répond a la famille des Per- coides de Cuvier, Regne Animal, 2° édition; sauf les genres qui ont plus ou moins de sept rayons aux branchies, et les sous- familles du Dr. Giinther, Catalogue, I., p. 57, qui ont pour types les genres Pentaceros, Apogon, et Grystes. J’en ai détaché aussi les genres Centropomus et Rhypticus, comme types de familles de la Faune de Cuba. 33 distinctes; et les genres anomaux de Giinther (1. ¢., p. 51), Pogonoperca et Prionodes, ainsi que mon genre Gramma, non moins anomal. Voyez les observations de Mr. Gill, Proc. Phil., 1861, p. 46. Subfamilia 1.—SERRANINI. Une seule dorsale, la partie épineuse non-logée dans un sillon du dos. Opercule épineux, préopercule dentelé. Un rang de dents extérieures, solides et plus fortes que les intérieures qui les accompagnent, et qui sont ordinairement couchées et mobiles. Des canines sur le devant des machoires. Le premier sous-orbitaire, peu développé, ne recouvre pas la partie postéri- eure du maxillaire, excepté dans le genre Mentiperca. Pecto- rale arrondie. Dernier rayon de la ventrale attaché 4 l’abdo- men par une membrane axillaire. Il n’y a pas de lobule écailleux au-dessus de la base de la ventrale; mais il y a sou- vent une pli cutané écailleux au-dessus de Vaxille pectorale. Les écailles sont petites; le limbe préoperculaire en est cou- vert. L’os surscapulaire ne perce pas en dehors. Le post- frontal, saillant et aplati en dessus, porte un os caverneux post-orbitaire solidement encaissé, faisant continuation a la chaine d’osselets sous-orbitaires. La fosse paroccipito-mastot- dienne est plus ou moins profonde, couverte en partie par une cote parieto-mastoidienne, excepté cependant dans le genre Brachyrhinus. ly aun os labial, placé au-dessus du maxil- laire. On ne trouve pas dans les chairs, au-devant de la premiére épine internévrale, les trois fausses internévrales qui se présentent chez les Lutjaninz; tout au plus y voit-on dans les premiers groupes, un os de la nuque, incliné en sens contraire et moins ossifié. Les deux derniers groupes de cette sous-famille, appartenant aux genres [Haliperca et Hypoplectrus, forment une transition aux Leutjanini, par Vos surscapulaire ‘visible en dehors, lapo- physe post-frontale sans osselet post-orbitaire, la fosse paroccipito- MARCH, 1871. 3 ANN. Lyc. NAT. HIST., VOL. X. 34 Genres des Poissons mastoidienne limitée et non-recouverte, le défaut d’os labial et absence de fausses épines internévrales ; mais ils appartiennent aux Serraniné par tous les autres caractéres, qui sont les plus im- portants. La caudale est échancrée. Le limbe préoperculaire est nu. Ils different encore de tous les Percides par la ventrale sans frein membraneux. On pourrait former de cette coupe la sous-famille des Hypoplectrini. Voici dans quel ordre je place les genres de Cuba qui se p quoaano.yans cette sous-famille. a. 1. Trisotropis.—Species : Cardinalis, V al.—petrosus, Poey.— brunneus, Poey.—Bonaci, Poey.—171, Poey.—Aguaji, Poey. —camelopardalis, Poey.—429, Poey.—tigris, Val.—calliurus, Poey.—181, Poey.—interstitialis, Poey.—chlorostomus, Poey. —dimidiatus, Poey.—falcatus, Poey. 2. Lpinephelus.—Species: striatus, Bl.—morio, V al.—flavo- limbatus, Poey.—niveatus, Val.—impetiginosus, M. et Tr.—- lunulatus, Bl.—Cubanus, Poey. 3. Lioperca.—Species: mermis, Val. 4. Promicrops.—Species: Guasa, Poey. 5. Schistorus.—Species: mystacinus, Poey. 6. Prospinus.—Species: chloropterus, Cuv.—7T12, Poey. b: 7. Brachyrhinus.—Species: furcifer, Val. C. 8. Petrometopon.—Species: guttatus, L.—apiarus, Poey. 9. Enneacentrus.—Species : punctulatus, Gm.—224, Poey. 10. Menephorus.—Species : dubius, Poey.—809, Poey. d. 11. Centropristis.—Species: Merus, Poey. e. 12. Haliperca.—Species: Phebe, Poey.—fuscula, Jacome, Poey.—prestigiator, Poey.—bivittata, Val. 13. Diplectrum.—-Species: radians, Q. et G. 14, IMentiperca.—Species: luciopercana, Poey. de la Faune de Cuba. 35 ie 15. Hypoplectrus.—Species : puella, Cuv.—vitulinus, Poey. —indigo, Poey.—bovinus, Poey.—gummigutta, Poey.—gutta- varius, Poey.—pinnavarius, Poey.—maculiferus, Poey.—aber- rans, Poey.—nigricans, Poey.—accensus, Poey.—affinis, Poey. 16. Gonioplectrus.—Species: hispanus, Ouv. GENUS TRISOTROPIS. Historique.—Ce genre a été établi par Mr. Gill, dans les Pro- ceed. Acad. Philad., 1865, p. 104, dans la famille Percida, sous-famille Serranine. Voyez en entier cette description, dont le type est le 7. guttatus, Gill ex Bloch, le méme que le Serranus cardinalis de Valenciennes. C’est un démembrement du grand genre Serranus de Cuvier, appartenant a la division des Mérous de Cuv. et Val., et comprenant parmi ces der- niers ceux qui joignent & onze piquants de la dorsale la cau- dale coupée carrément, et Panale 3, 11. Ltymologie.—zrpeis, tres 3 tpomss, carina. Caractere du genre. AGS ps oblong, ceil haut; ouvertures nasales rapprochées, plus prés de I’ oeil ie du bout du museau. La bouche est trés-fendue; le maxillaire termine, dans les su- jets de 12 pouces, sous le milieu de l’ceil; mais dans les grands sujets, il dépasse l’orbite. La machoire inférieure est beaucoup plus avancée que la supérieure. L’opercule a trois pointes ; celle du milieu bien saillante, la supérieure émoussée, l’inféri- eure peu visible en dehors. Le préopercule finement dentelé, arrondi, presque sans sinuosité, sauf dans le groupe qui porte le nom vulgaire de Abadejo, ou Vangle inférieur se dé- tache et porte quelques grosses pointes; il n’est pas denticulé en dessous. La langue est pointue, lisse, retenue par un frein, logée en partie sous un voile membraneux. Dents.—Il y a une dent canine, robuste, courte, au-devant de chaque machoire ; elle est snivie d’une rangée externe de dents coniques, aigués, crochues, plus petites, solidement implantées. 36 Genres des Poissons En dedans, soit en arriére de cette premicre série, se trouve une bande de dents en cardes, gréles, aigués, les antérieures en plus grand nombre et plus longues, toutes mobiles, ordinairement couchées; celles de la machoire inférieure plus nombreuses. Les dents de la votite palatine sont aussi en cardes; celles du vomer, sur un chevron angulaire ; celles des palatins, sur une ligne étroite. Les os pharyngiens ont des dents en velours. Les ares branchiaux ont de courtes ratelures et de gros tuber- cules hérissés d’épines. Nageotres.--D. 11, 16 ; A. 3, 11. Le dernier rayon épineux de la dorsale est au moins aussi long que celui qui le précede, et rapproché du premier rayon mou; la partie molle est nota- blement moins étendue que la partie épineuse. La candale est coupée carrément, présentant souvent deux pointes trés-peu saillantes; il est trés-rare de la trouver légérement arrondie vers les pointes, et je ne l’ai vue bien échanerée que chez le T. falcatus. Les épines anales ne sont pas fortes; et il y aun repli cutané au-dessus de la base de la pectorale. Ecailles.—Les écailles sont petites ; car lear nombre, sur la ligne latérale, passe ordinairement de 100: elles doivent se ranger sous la division des Cténoides de Mr. Agassiz, a cause de Péventail qu’elles ont toujours a leur racine; mais leur bord libre, quoique ponctué, n’est pas toujours cilié ; il est souvent couvert par l’épiderme, ce qui empéche de les compter avec ex- actitude, et de les sentir sous les doigts. Celles de l’opercule sont un peu plus petites que celles du trone; celles du dessus de la téte et des joues sont encore plus petites; il y en a sur le limbe du préopercule et sur l’interopercule ; celles qui s’éten- dent sur le bout du museau et sur la machoire inférieure sont trés-petites ; et celles qui couvrent le maxillaire le sont a tel degré qu’on ne peut les distinguer qu’avec une forte loupe. La partie molle des nageoires verticales est en partie couverte par la peau, qui montre a la loupe de petites écailles ; il y en a méme a la base des interstices que laissent entr’elles les épines dorsales. On trouve souvent, soit entre deux écailles, soit a la base d’une de la Faune de Cuba. on seule, de tres-petites écailies, qui se montrent comme des tuber- cules microscopiques, formés par l’épiderme sous laquelle elles se cachent. Squelette.—Crane élargi en arriére. Espace interorbitaire large et enfoncé. La créte suroccipitale est basse, terminant postérieurement en angle obtus; les autres crétes sont hautes ; il n’y a pas de ecréte frontale. L’orbite est placé sur la moitié antérieure du crane. L’apophyse préorbitaire est tres-saillante, et portant la téte qui s’articule avec le premier sous-orbitaire ; Papophyse post-orbitaire est tres-prononcée. La lame antérieure de Valisphénoide avance beaucoup; le trou postérieur qui donne passage au nerf trijumeau est trés-arri¢ré. La convexité oto- cranienne ne se montre pas au dehors. La base esphénoidale du crane est droite ; la fosse paroccipito-mastoidienne est pro- fonde. Voici comment Mr. Gill décrit le crane: “ Distinguished by the petrous-like convexity between the supra-orbital grooves, and its triangular sinus behind, into the angles on each side of which the lateral crests terminate; the crests are parallel, and the surface between flat or scarcely convex.” Cing sous-orbitaires et un osselet cavernenx solidement en-. caissé sur ’apophyse post-orbitaire. Prétympanal pourvu d’une lame apophysaire plate. Lessix premiéres vertebres abdominales sans apophyses transverses, les deux derniéres paires formant l’an- neau. Les premieres névrapophyses de la colonne vertébrale sont larges, courtes, plus obliques que les normales. Jes cétes sont dans Vordre suivant, de chaque cété: 2 épines épinévrales, 8 pleur- apophyses, 7 épipleurales. La premiére épine internévrale ne porte qu’un seul aiguillon de la dorsale. I] n’y a pas sur le devant, entre les chairs, de fausses internévrales ; on y trouve seulement un osselet peu durci, saus téte épineuse, disposé obliquement en sens contraire, en arriére de la créte occipi- tale; on pourrait le nommer los de la nuque. L’os pelvien n’a pas son apophyse interne ascendante. Visceres.—Lintestin est ferme ; il revient deux fois sur lui- 88 Genres des Poissons méme, et se pelotonne avant le premier pli. Les ccecums sont au nombre de 12 a 18, ordinairement 15; ils sont longs et fermes. La vessie aérienne est 4 parois minces et transparentes. I] nest pas rare de trouver au milieu des viscéres des helminthes enkystés, bleuatres 4 lextérieur. Couleurs.—Les couleurs, chez les espéeces de Cuba, sont d’un fond violet, plus ou moins couvert de taches d’un brun rouge- dtre: le rouge se présente parfois sur le fond du dos et sur les taches. Les nageoires verticales ont un fin liséré blanc, qui se perd avec l’age. Variétés—Les changements apportés par lage ne se bornent pas a la petitesse de l’ceil et au raccourcissement des nageoires; mais encore aux couleurs du corps, et surtout a celle des nageoires pectorales, qui dans le premier age sont presque d’une teinte uniforme, et plus tard bordées d’une maniére tranchée d’orangé ou de blane. fistoire.—La plupart de ces poissons deviennent trés-grands ; leur chair est bonne 4 manger. Ceux de grand taille sont suspects, parce que parfois et bien rarement ils ont été péchés malades, et ont causé l’indisposition que dans le pays on nomme ciguatera. GENUS EPINEPHELUS. Historique.—Ce genre a été établi par Bloch, Ichthyologia, Pars 10, p. 9; abandonné par Cuvier et Valenciennes, rétabli par Mr. Gill, Proceed. Philad., 1862, pp. 286, 237 ; 1863, p. 80; dans la famille Percide, . sous-famille Serranine. C'est un démembrement du grand genre Serranus de Cuvier, appartenant a la division des Mérous de Cuv. Val., et com- prenant parmi ces derniers ceux qui joignent 4 onze piquants de la dorsale la caudale ordinairement arrondie, et les nombres de l’anale 8, 9; jamais plus, quelquefois 3, 8. Etymologie.—taweperes, obnubilus. Voici les caractéres assignés par Bloch: “ Pisces capite toto squamoso, operculo anteriore serrato, posteriore aculeis de la Faune de Cuba. 39 armato;” & quoi il ajoute une seule dorsale et des écailles ciliées. La premiére espéce décrite est le /. afer, dont ila fait plus tard le type de son genre Alphestes, et dont je m’oc- cuperai au sujet du Prospinus chloropterus: ce type de Bloch a la caudale arrondie, et l’anale 3, 9. Ce genre, négligé par Cuvier et Valenciennes, a été repris par Mr. Gill, qui y a ajouté un caractére remarquable, savoir, des dents en cardes et mobiles dans Vintérieur des machoires. En 1865, Proceed. Philad., p. 105, il l’a distingué du genre Trisotropis par la forme du crane; et par le seul fait d’avoir accordé a ce dernier genre J’anale 3, 11, il a Jaissé dans le genre Epinephelus les especes qui ont l’anale 3, 9; il n’a rien dit de la caudale, mais celle de 7risotropis n’est pas pour lui arrondie. Bloch a nommé ces poissons Epinépheéles, parce que, dit-il, “ils ont les yeux couverts d’une membrane, ou d’une taie;” ce qui ferait croire qwils ont sur ceil une membrane adipeuse. Tout au plus voit-on chez les adultes une prolongation de Ja paupicre supérieure, qui est loin de pouvoir étre nommée une taie. Le nom reposerait alors sur une erreur, et mériterait d’étre changé. En ce cas le groupe Mérow de Cuv. Val., fixé par sa premiere espéce Serranus gigas, pourrait y étre sub- stitué, en Latin Jerws. Quant aux Mérous de 9 épines dor- sales, ilsen ont été détachés par Mr. Gill, qui en a fait ses genres Petrometopon et Hnneacentrus. Le genre Crom ileptes de Swainson, Nat. Hist. of Fishes, &*., 11, pp. 168, 201, doit aller a la synonymie du genre “pinephelus, Caractéres du genre.—Pour étre bref dans les caractéres du genre, je me bornerai a& dire qwil a tous ceux qui ont été assignés au genre 7risotropis, sauf Vanale 3, 9, et la forme du crane; la caudale est ordinairement arrondie. Le crane est étroit entre les deux orbites; la créte mastoidienne forme un arc descendant. La langue n’est pas toujours si pointue. Les écailles du trone sont ciliées et découvertes, sans mélange d’autres plus petites ; les nageoires verticales n’ont pas toujours un liseré, et portent quelquefois une lanicre vers les pointes 40 Genres des Poissons épineuses de la dorsale. La vessie natatoire est a parois minces, mais ordinairement renforcée sur sa partie antérieure; le nombre des ccecums varie, mais il n’est pas trés-considérable. La chair est toujours saine. GENUS LIOPERCA. Historique.—Ce genre a été établi par Mr. Gill en 1862, dans les Proceed. Philad., pp. 236, 287, famille Percidae sous-famille Serranine. Il se trouve dans la division de: *“ Dorsale entiére ou presque entiére, caudale enticre ou simple- ment échanerée; corps oblong, écailles petites; dents non- couchées en arriére des canines; écailles douces au tact et glissantes; onze rayons épineux a la dorsale; type: Serranus anermis C. et V.—L’auteur dit en 1865, dans le méme ouvrage, p. 105: “que les genres de cette sous-famille établis par lui pour les espéces des Indes occidentales, peuvent se distinguer par la forme du crane, méme le genre Lioperca, qui offre cependant le plus de doutes.” Etymologie.—r«ies, levis ; Perca, nom propre. Ce qui peut- étre fait allusion a la faiblesse des pointes operculaires. Caracteres du genre.—Corps oblong, machoires a-peu-prés @égale longueur. Trois pointes 4 Vopercule ; celle du milieu forte, les autres plates. Préopercule finement dentelé.a la branche montante, fortement a Vangle, nullement au’ bord inférieur. Narines rapprochées de Veil. Langue lisse, libre et pointue. Dents.—l.es dents des machoires sont en cardes; les plus intérieures, quoique petites, sont mobiles, et il y en a quel- ques-unes de plus grandes sur le devant; les canines ne sont bien remarquables que dans un age avancée. Les dents du vomer et des palatins sont en cardes, sur un seul chevron. Nageoires.—D. 11, 19; A. 3, 9. La partie molle de la dorsale est trés-élevée ; la caudale arrondie, excepté dans un age fort avancé. de la Faune de Cuba. 41 Ecailles.—Environ 100 sur une ligne longitudinale ; celles de la joue trés petites ; il y en a sur toutes les piéces operculaires et sous le dentaire. Il n’y en a pas sur les apophyses mon- tantes du prémaxillaire, sur le devant de l’ceil, ni sur le maxil- laire. ly en asur la base de toutes les nageoires, principale- ment sur les verticales médianes, qui sont couvertes d’une peau épaisse. Squelette—Le crane est étroit postérieurement, ainsi que Vespace interorbitaire ; la créte suroccipitale peu relevée, se continuant avec une créte frontale tres basse et courte; la mastoidienne est descendante. L’orbite est avancé, les apo- physes orbitaires saillantes ; le trou du nerf trijumeau arriéré ; Ja convexité otocranienne nulle en dehors; la base esphenoidale un peu courbe. Sous-orbitaires an nombre de 4, sans compter Vosselet solidement encaissé sur l’apophyse post-orbitaire ; pré- tympanal pourvu dune apophyse laminaire. Les apophyses latérales des vertebres abdominales commencent sur la 6° et vont en augmentant, les deux dernicres paires formant l’anneau. Les premieres névrapophyses forment un are renforcé sur le devant; 2 épines épicentrales antérieures, 8 pleurapophyses, 6 épipleurales (peut-étre 8). Le premier internévral ne soutient quwune seule épine du dos; il n’y a pas sur le devant de fausses épines internévrales. Visceres.—Estomac court, branche montante trés-courte ; ceecums assez nombreux, divisés, les divisions sont dans le type au nombre de 60. L’intestin est trés-ferme et trés-gréle, faisant les circonvolutions ordinaires, mais se pelotonnant un peu avant le premier pli. Vessie a¢rienne 4 parois minces et transparentes. Observations.—J’ai adopté ce genre dans ma Synopsis, en 1868, par déférence pour Vopinion de Mr. Gill, en qui j’ai toujours reconnu un tact stir, soit un don particulier pour la classification. Un des caracteres par lui donnés, a cependant disparu ici; ¢’est celui qui se fonde sur l’absence de dents couchées en arriére des canines: on voit que les machoires sont 49 Genres des Poissons armées dans le sens de celles de Zrisotropis ; ce n’est quwune question de plus ou de moins entre les deux genres. C'est peut-étre moi qui ai induit en erreur Mr. Gill; car en 1851, époque a laquelle j’ai décrit Vespéce-type dans mes Mémoires, je n’avais pas encore les connaissances que j’ai retirées plus tard de mes études et des savants articles de Vichthyologiste améri- cain, mon digne correspondant durant le cours de plusieurs années ; et j’ai commis alors quelques erreurs: ainsi, je me suis trompé en écrivant que les dents sont en velours ras; ce qui ne peut paraitre ainsi que chez de jeunes individus; et que la créte suroccipitale est haute. Tel qu'il est, le genre Lioperca peut étre séparé de Triso- tropis et de Epinephelus par un corps un peu bossu, a cause de | Vaffaissement de la téte, la peau plus mucilagineuse, deux épines plates qui accompagnent une épine plus robuste de lopercule, bout du museau dépourvu d’écailles, sauf le dentaire ; ececums nombreux et divisés, défaut complet de fausses épines inter- névrales. Une autre particularité bien remarquable est celle que lage introduit dans la forme des nageoires verticales, surtout dans la caudale, qui, @abord arrondie, devient dans l’dge adulte légérement échancrée. GENUS PROMICROPS, Listorique—Ce genre a été établi par Mr. Gill, qui n’en a pas encore donné au public les caractéres; mais il a eu la bonté de me lindiquer avant Vimpression de ma Synopsis, ayant pris pour type le Serranus Guasa de mes Mémoires. Etymologie.—Je crois que le nom se rapporte a la briéveté de la partie antérieure du créne; ce qui est di au grand avancement de l’orbite. Caracteres du genre.—Ce genre a les caractéres des Epine- pheli, sauf le crane, qui se rapporte a celui des Zrisotropi par la grande distance interorbitaire. On y remarque l’wil trés- de la Faune de Cuba. 43 avancé, et le trou du nerf trijumean tres-arriéré. Il en differe de plus par les dents et par Pextréme division des appendices pyloriques. Les dents sont en cardes sur une large bande, un peu plus étroite &la machoire inférieure; le bord externe offre une rangée de dents un peu plus fortes, surtout les deux premiéres, mais on ne voit pas s’y détacher de vraies canines; la rangée tout-a-fait interne, sur le devant, offre aussi quelques dents plus fortes. La bande des palatins et le chevron du vomer sont en cardes plus fines. Les ccecums et leurs divisions sont in- nombrables. GENUS SCHISTORUS. LTistorique-—Genre établi par Mr. Gill, Proceed. Philad., 1862, pp. 236, 237, ou il en donne les caractéres suivants, servant 4 le distinguer des autres genres de Cuba: “ Famille des Percide, sous-famille Serranine ; une seule dorsale sans échancrure, caudale enticre, corps oblong, écailles petites, des dents couchées derriére les canines, préopercule ayant vers le bas des épines tournées en avant; D. 11, 14; cceeums nom- breux et divisés.” Type: Serranus mystacinus, Poey. Caractéeres du genre.—Je crois qwil faut faire peu d’attention aux pointes de l’angle du prévpercule, telles que les présente cette espéce, lesquelles sont peu nombreuses et variables; ce qui, outre la taille et la dentition, Véloigne du groupe des Plectropome, Laissant a part ce faible caractére, tout ce que m’a appris l’étude de cette espéce, n’ayant pas examiné le squelette, en fait un véritable Apinephelus, avec la seule difference que présentent les appendices pyloriques. J’ai indiqué ce dernier caractere, bien mieux prononcé chez le Promicrops Guasa; et on le retrouve, tel que le présente le Schistorus mystacinus, chez le Hpinephelus niveatus et chez le Lioperca inermis. L’étude du crane peut seule nous dire si le genre doit étre conservé, ou s'il faut le considérer comme un 44 Genres des Poissons Epinephelus ou comme un Promicrops. Mon respect pour Popinion de Mr. Gill m’a fait adopter son genre dans ma Synopsis, en 1868. Etymologie.—exiSw, diviser; pes, humeurs. Par allusion aux coecums. GENUS PROSPINUS. Historique.—Les auteurs du genre Plectropomus (Cuy. et Val., Poiss., IL, p. 887) ont eux-mémes qualifié de fort léger le caractére tiré de la dentelure autour et au-dessous de l’angle préoperculaire. C’est cependant sur les modifications de ce caractére qwont été fondés, parmi les Percidw, sous-famille des Serranina, plusieurs genres, qui ne mériteraient pas d’étre conservés, si lon n’avait pas trouvé a leur appui quelques autres particularités plus importantes. Le genre Plectropomus est de 1828: il a été subdivisé en trois groupes, selon le nombre de dentelures, et le bord mon- tant du préopercule entier ou finement dentelé. La premiere espéce nommeée, et qui doit par conséquent servir de type dans le premier groupe, est le Bodianus melanoleucus de Lacépéde. Le corps est allongé. Le bord montant du préopercule est entier; D. 8, 11; A. 2, 8. Les écailles sont petites; il y en a sur le bout du museau, sur le maxillaire, sur les nageoires; les pectorales sont arrondies, la caudale a-peu-prés coupée carré- ment. Le genre [Hypothrodus (on lit Hyporthodus, mais je crois que cest une faute d’impression) a été établi par Mr. Gill, Proce. Phil., Mai de 1861, p. 98. Type: ZZ. flavicauda, Gill. L’oper- cule, la joue, les os surmaxillaires sont couverts d’écailles, la mdachoire inférieure nue. Le préopercule porte a l’angle une forte épine, elle-mémne denticulée, aussi que le bord montant ; il y a encore des dentelures au bord inférieur. D. 11, 14; A. 3, 10. Le genre Prospinus a été nommé dans mes Mémoires, I. p. de la Faune de Cuba. 45 364. Type: Pl. chloropterum C. V., fondé, p. 888, sur la force et le petit nombre de dents sous-préoperculaires. Il a été adopté par Mr. Gill, Proc. Acad. Phil., 1862, pp. 236, 237, dans la division de ‘Dorsale entiére ou presque entiere, eaudale enticre ou simplement échanerée, corps oblong, écailles petites, dents couchées en arriére des canines, préopercule pourvu en dessous d’une on de deux pointes dirigées en avant ; D. 11, 18-19. Ccecums 8.” Le genre Alphestes de Bloch, Systema, p. 2386, en 1801, ayant pour type le Apinephelus afer de Bl., Ichth., tab. 327, lequel est le méme que le P/. chloropterum de C. et V., ala priorité sur le genre Prospinus; mais je crois qwil doit tomber: 1°. parce quwil n’est pas fondé sur Vépine préoper- culaire, que l’auteur n’a pas apercue; 2°. parce que le caractcre donné a une étendue trop-considérable, savoir: Sguame oper- cult posterioris duplo majores quam anterioris. C’est tout ce qwil en dit; et c’est ce qui pourrait étre appliqué a une foule de genres. Le genre Acanthistius a été proposé par Mr. Gill, Proce. Acad. Phil., 1862, p. 236, pour le Pl. serratwm, Cuv. et Val., qui doit servir de type. Cette espéce, placée dans le 2° eroupe de C. et V., a le corps gros et court, les deux machoires @éeale longueur, des écailles au maxillaire et & la machoire inférieure ; préopercule fortement dentelé; et prés de langle, deux grosses dents dirigées en avant, dont Vantérieure plus forte. D. 13,16; A. 3,9. Lcailles petites. Le genre Hypoplectrodes a été proposé par Mr. Gill, Proceed. Acad. Phil., 1862, p. 236, pour le Pl. nigro-rubrum, C. et V. Il est plus allongé que le PU. serratwm ; les dentelures du bord montant du préopercule sont plus fines; il n’y a au bord inférieur que deux pointes dirigées en avant, dont lune a anole 107 A8, 8: Genre Gonioplectrus, Gill.—V oyez ci-dessous. Genre //ypoplectrus, Gill.—V oyez ci-dessous. Genre Schistorus, Gill.—Voyez ci-devant. 46 Genres des Poissons Etymologie.—Prospinus, épine tournée en avant. Caractere du genre Prospinus.—U differe du genre Lpine- phelus par Vépine préoperculaire et quelques menus détails : ainsi, les canines sont trés-petites ; on n’en voit pas a la machoire infé- rieure. La ligne latérale porte 70 écailles; celles de l’opercule sont grandes; elles sont petites sur les jones; ily en a sur Des- pace interorbitaire et sur l’os turbinal, mais non pas sur le bout du museau ni sur le maxillaire. L’épine unique sous-préopercu- laire est trés-forte, couverte dans le frais par la peau: elle parait elle-méme finement subdivisée en arriere, parce qu’elle porte la terminaison de la roue formée par l’angle. Genus BracuyrHINvus. LHistorique.—Ce genre a été établi par Mr. Gill, dans les Proced. Acad. Philad., 1862, p. 236, dans la famille des Per- cide, sous-famille Serranine ; type, Serranus creolus, C. et V. Il y est placé dans la division de ‘ Dorsale enticre ou presque entiere ; caudale bifurquée, a lobes aigus; dorsale basse et uniforme ; formule radiale 9, 18-19.” C’est pour Cuvier et Va- lenciennes un Serran du groupe des Anthias. J’ai adopté ce genre dans ma Synopsis, en 1868. Plus tard, Mr. Guichenot, dans un travail intitule Zndew Generum et Specierum Anthiadido- rum, inséré dans le 9° volume des Annales de la Société Lin- néenne de Maine et Loire, a fait de ’espéce que je viens de citer le type de son genre Paranthias, dont il a donné les caracteéres suivants: “Corpus oblongum subelongatum, squamis minimis vestitum. Caput breve curvatum, omnino squamosum. Preeo- perculum tantum denticulatum. Oculi parvi. Pinna dorsi simplex absque incisa, simul ac analis et caudalis in parte squamosa.” Etymologie.—fpaxvs, brevis; pv, nasus. Caractéres du genre-—Corps élégamment oblong, museau court, ceil médiocre ; narines rapprochées, occupant le milieu entre l’ceil et le prémaxillaire; préopercule finement ‘dentelé, de la Faune de Cuba. 47 sinueux vers le bas; opercule a trois pointes, l’inférieure pres- que aussi forte que celle du milieu; bouche petite, machoire inferieure un peu plus avancée que la supérieure. Langue lisse. Dents.—Les dents des machoires sont courtes et pointues sur un rang extérieur, précédées de deux canines petites et fortes ; a lintérieur il y a une bande de petites dents en cardes, tres-étroite ala machoire inférieure. Celles du vomer sont sur une plaque triangulaire, et celles des palatins forment une plaque apre. Les dents pharyngiennes supérieures sont en cardes, les inférieures en velours. Le premier are porte de longues rate- lures. Nageotres.—D. 9,19; A. 3,9. La partie molle de la dor- sale est plus basse que l’épineuse, et moins étendue; les épines anales sont courtes, mais fortes; la pectorale est arrondie, for- mant cependant un prolongement aigu; caudale bifurquée ; ventrale retenue par une membrane axillaire. Le dernier rayon des nageoires médianes est filamenteux. Leailles.—Knviron 115 Je long de la ligne latérale, qui asa direction normale. I] y enasur toute la téte, excepté aux lévres, ainsi que sur les nageoires. Le préopercule n’a pas son limbe nu. Il] n’y a pas de lame surseapulaire. Squelette.—Le crane est aplati en dessus, concave dans l’es- pace interorbitaire, qui est assez large; Vorbite est rejeté vers Vextrémité antérieure ; la créte suroccipitale est basse, arrondie, et peu prolongée en arriére ; la paroccipitale est sinueuse; la fosse paroccipito-mastoidienne est ouverte antérieurement; le basi-occipital offre une ample ouverture qui conduit a la fosse sous-cranienne. Sous-orbitaires au nombre de quatre? Nul osselet solidement encaissé sur l’apophyse post-orbitaire. Pré- tympanal portant une lame apophysaire. Les apophyses laté- rales abdominales commencent ala 5° vertebre, les deux derniéres paires formant ’anneau. Les deux avant-premicres névrapo- physes sont courtes, fortes, et peu inclinées. I] parait que appa- reil des cOtes se compose de 2 épines épinévrales, 8 pleurapo- physes, 7 épipleurales. Le 1* internévral soutient une seule épine 48 Genres des Poissons du dos; il y a sur le devant deux, peut-étre trois fausses interné- vrales. L’os pelvien n’a pas d’apophyse interne ascendante. Visceres.—Ceecums, 8. GeENus PETROMETOPON. Historique.—Ce genre a été établi par Mr. Gill, dans les Proceed. Acad. Philad., 1865, p. 105, sur le nombre des épines dorsales et la construction du crane, famille des Percida, sous- famille Serranine ; ayant proposé pour type le Perca guttata de Linné, soit le Serranus coronatus de Valenciennes. En 1862, p- 236 du méme ouvrage, il Pavait placé dans le genre Lodi- anus de Bloch; mais en 1865, il a laissé ce dernier dans les Labride, type Bodianus bodianus de Bloch, soit le Labrus rufus de Linné. J’ai adopté ce genre dans ma Synopsis, en 1868. C’est un démembrement du genre Serranus de Cuvier, groupe des J/érous, dont il se distingue principalement par les neuf aiguillons de sa nageoire dorsale. Eiymologie.—merpe, petra; métamoy, frons; 4 cause de l’en- durcissement du crane sur la partie frontale. Caractéres du genre.—Corps oblong. Narines rapprochées, placées prés de l’eeil. Préopercule dentelé sur le bord poste- rieur seulement ; cpercules 4 trois pointes Gpineuses. Machoire inférieure plus avancée que la supérieure. Dents.—Les machoires ont une rangée extérieures de petites dents aigués, précédées d’une ou deux petites canines. La ma- choire supérieure a, derriére cette rangée, une bande d’aspéri- tés ; mais sur le devant il y a un groupe de dents en cardes, les plus internes trés-longues et gréles, couchées et mobiles. La machoire inférieure porte derriere la rangée externe une bande de dents en cardes, fines et allongées, également conchées et mo- biles. Le vomer porte un chevron triangulaire de petites dents, et les palatins un mince chevron. La langue est lisse. Les dents pharyngiennes sont en velours. de la Faune de Cuba. 49 Nageoires.—D. 9,14; A. 3,8. La derniére épine dorsale est égale a celle qui la précede. La partie molle de la dorsale a presque autant d’étendue que la partie épineuse. Les épines de Panale sont fortes. La caudale est arrondie. La ventrale est rete- nue par une membrane axillaire. Ecailles.—La ligne latérale est arquée. Les écailles sont ciliées, petites, environ 70 sur une ligne longitudinale ; celles de la joue sont petites. Il yen ade trés-petites sur toute la téte, méme sur le maxillaire, et sur la base des nageoires verticales. Un espace anteorbitaire qui conduit aux narines est cependant nu. Le surscapulaire ne perce pas en dehors. Squelette—Le crane a peu de largeur en arriére ; espace interorbitaire endurci, étroit, et convexe ; la eréte suroccipitale trés-basse, et les autres aussi. L’orbite est placé sur la partie antérieure. La fosse paroccipito-mastoidienne est profonde; les apophyses articulaires préfrontales sont verticales. Les sous- orbitaires sont au nombre de cing, et de plus il y a un osselet caverneux solidement encaissé dans Vapophyse post-orbitaire. Le prétympanal a une apophyse laminaire. Les six premiéres vertébres abdominales n’ont pas d’apophyses latérales, les trois derniéres paires formant l’anneau. Les premiéres névrapophyses sont robustes, dont les deux dernieres moins longues. On compte 2 épines épinévrales, 8 pleurapophyses, 7 épipleurales, dont la derniére est plut6t une épinévrale. Le premier inter- névral soutient une seule épine dorsale. L’os pelvien n’a pas d’apophyse ascendante. Viscéres.—Circonyolutions ordinaires, intestin gréle, un peu pelotonné avant le premier pli; ccoecums médiocrement nom- breux, longs, fermes. Vessie aérienne trés-solide. fistoire.—Ce sont des poissons de mer, carnivores, de taille médiocre ; ceux de Cuba se distinguent par un fond rougedtre parsemé de taches brunes; trois taches brunes le long du dos, de chaque céte. MARCH, 1871. | j 4 ANN, Lyc. NAT. Hist., Vou. X. 50 Genres des Poissons GeENus ENNEACENTRUS. Fistovique.—Ce genre a été établi par Mr. Gill, dans les Pro- ceed. Acad. Philad., 1865,p. 105, conjointement avec le genre /n- neacentrus, sur le nombre des épines dorsales et de la construe- tion du crane; famille des Percide, sous-famille Serranine ; ayant pour type le Serranus Ouatalibi de Valenciennes, soit la variété rouge du Perca punctulata de Gmelin. J’ai adopté ce genre dans ma Synopsis en 1868, II] appartient au méme groupe que le genre antérieur. Etymologie.—étvvix, novem ; xévzpev, aculeus. Caractéres dw genre.—Ce sont tous les caracteres du genre Pétrométopon, sauf ceux du crane, qui differe en ce qu’il est cannelé dans l’espace interorbitaire, et toute sa surface lisse, comme Mr. Gill, habile observateur des cranes, l’a déja fait remarquer. Le besoin de traduire au-dehors cette distinction anatomique, m’oblige d’ajouter un caractere tiré des couleurs: cest, pour Cuba, deux taches noires surcaudales, et une autre, de chaque coté, sur ’extrémité de la machoire inférieure. Jai trouvé dans le type un petit nombre de ccecums, dépassant 5, et la vessie aérienne a parois minces. Les mceurs et la taille sont ceux des Pétrométopons. Gernus MENEPHORUS. Le genre Menephorus ne differe du genre Enneacentrus de Mr. Gill, que par la caudale coupée en croissant, et le défaut de taches noires sur le pédicule caudal et a l’extrémité du menton ; il porte, comme le genre établi par Mr. Gill, des points bleus sur le corps. L’importance du premier de ces deux caractéres n’a pas été méconnu du savant classificateur que je viens de nommer; car il l’a fait heureusement entrer dans la description de ses genres. Il est certain que la caudale des Trisotropis se présente coupée carrément ; celle des Epinephela est arrondie; celle des Zutjanz est échancrée; celle des Caran- de la Faune de Cuba. 5 gide est bifurquée. Cependant, je mignore pas qu'il y a en cela de rares exceptions, comme par exemple chez mon Z7iso- troprs falcatus et chez le Kpinephelus morio ; et je waurais pas sur ce seul caractere établi un nouveau genre dans la coupe de Mr. Gill, si je n’avais pas été appuyé par un trait de coloration caractéristique qui se trouve chez les Hnneacentri, et qui man- que dans les deux espéces du genre que j’établis ici. Quant au caractere de coloration, il parait nul au premier abord, quand on considére que lVorganisation entiére n’est nul- lement changée par la disposition des couleurs; mais d’un autre coté, on observe que la nature est souvent constante dans sa maniere de peindre les animaux, suivant les groupes aux- quels ils appartiennent. Ainsi, les espéces de la race féline ont en général le poil fauve, parsemé de taches arrondies; les Colibris, parmi les oiseaux, ont le gosier aussi resplendissant que les pierres précieuses ; les Buprestes, parmi les Coléoptéres, sont couverts Wor; les Papillons du genre Coliade sont presque tous jaunes, et les Piérides, blanches ; les Satyres dérobent aux herbes des bois montagneux leurs traits cendrés et incertains. Hiibner a étrangément abusé de ce caractére dans sa classifica- tion lépidoptérique ; mais il n’en a pas été moins conduit 4 faire d@’heureux rapprochements. Les couleurs souvent n’aménent a rien; mais dans certains groupes elles semblent devoir faire nécessairement partie des descriptions génériques; ne fut-ce quwau dernier terme. Je prends pour type le Hnneacentrus dubius de mes Mémoires, LEtymologie.—riva, luna; 4épe, fero. Ce qui répond au mot latin Lunzfer, la caudale étant coupée en croissant. GENUS CENTROPRISTIS. Ce genre a été établi par Cuvier et Valenciennes, en 1829, dans Il’ Histoire des Poissons, ILI., p. 86, sous le nom de Centro- pristes. Dans le 2° volume du Régne animal, qui est posté- 52 Genres des Poissons rieur, quoique de la méme année, il a été changé en Centropris- tis, qui est plus acceptable. D’aprés les auteurs du genre, ils sont parmi les Perches 4 dorsale unique et 4 dents en velours, & peu-prés ce que sont les Serrans dans la division de dents canines, c’est-a-dire, qwils réunissent & un opercule épineux un préopercule dentelé en scie. Le museau, la machoire et la membrane des ouiés man- quent d’écailles; mais il y en a sur le crane, sur la joue, et sur les piéces operculaires. Type: Perea atraria, L. Le type nommé, a les dents en velours, la langue lisse ; D. 10,11; A. 3, 7. La caudale est trilobée; mais la forme de cette nageoire n’entre pas dans les caracteres du genre, tel que le présentent Cuv. et Val. Le Dr. Giinther, Catal. I., p. 82, indique les dents en velours, avec de tres-petites canines aux deux machoires. II ajoute que les dents du vomer sont sur une plaque triangulaire et que les nombres sont: D. 10, 12 (ou moins de 12); A. 8, 7 (parfois 6). Presque toutes les espéces citées dans dans cette partie de son catalogue, ont été plus tard portées par Mr. Gill 4 un nouveau genre, nommé par Ini //aliperca. Etymologie.—xévz per, aculeus ; *pir7¥s, serratus. Genus Hatiperca. Tistorique.—-Ce genre a été établi par Mr. Gill, dans les Proceed. Acad. Philad., 1862, p. 236, parmi les Percida, sous-famille Serranine ; type, Serranus bivittatus, C. et V., S. Phabe, Poey, Centropristis tabacarius,C. V.,&*. Il est placé dans la division de “ Dorsale enti¢re ou presque entiére, caudale enticre ou simplement échanerée, corps délié, écailles modé- reés (50-75) dents non conchées, machoires égales, préopercule dentelé.” Les especes de ce genre ont été distribuées par Ou- vier et Valenciennes parmi les Serrans proprement dits et les Centropristes. C’est dans ces derniers qu’elles ont été placées par le Dr. Giinther. Klein, Miss. V., p. 60, N°. 4, a placé une de la Fuune de Cuba. 53 de nos espéces dans son genre Prochilus, dépourvu de dents, qualifié de monstrueux par Cuvier et Valenciennes. Etymologie.—érs, mare ; *épxn, perche. Caractéres du genre.—Corps allongé, téte obtuse en dessus, ceil médiocre, ouvertures nasales rapprochées et placées pres de Veil; préopercule dentelé sur tous ses bords, opercules a trois épines rejetées en bas; bouche grande, machoire inférieure dépassant la supérieure. Langue lisse, libre, pointue. Voyez ce qui a été indiqué dans la sous-famille des Serranint. Dents.—Les machoires ont un rang extérieur de dents poin- tues, dont les deux ou trois premiéres en haut, une ou deux en bas, sont plus fortes et peuvent étre considérées comme canines ; en dedans, il y a en haut une bande de dents en velours, ainsi que sur le devant de la machoire inférieure. Parmi celles de devant de la machoire supérieure, il y en a une de chaque cdoté longue et forte, couchée en arriére, et qui parait étre mobile. Au milieu du rang externe de la machoire inférieure, s’élevent environ cing dents plus longues que les autres et écartées. Les dents du vomer sont sur un chevron triangulaire, et celles des palatins sur une bande étroite. Nageoires—D. 10, 12; A. 3, 7. La derniere épine dorsale est égale a Vavant-derniére. La partie molle ‘est a-peu-pres aussi étendue que la partie épineuse. La caudale est échancrée. Il n’y a pas de lanieres a la pointe des épines dorsales. Evcailles.—Les écailles sont au nombre de 50 a 70 le long de la ligne latérale, laquelle est parallele au dos. Celles des joues sont égales ou presque aussi grandes que celles de l’opercule ; tantot il y ena, tantot il n’y en a pas sur l’interopercule, dont le limbe est toujours nu; le crane et tout le musean en est dépour- vu; il yen aa la base des nageoires verticales. Squelette—Le crane est arrondi en-dessus ; les crétes courtes et basses, la suroccipitale rejetée en arriére ; espace interorbi- taire étroit ; une apophyse laminaire au prétympanal. Les apo- physes latérales des vertebres abdominales commencent a la 5°, les trois dernieres paires formant ]’anneau. La 1° et la 2° névra- 54 Genres des Poissons pophyses sont fortes et courbent leur pointe en avant. La 1° épine internévrale soutient deux rayons de la dorsale; 2 épines épicentrales, 8 pleurapophyses, 7 épipleurales. Viscéres.—L’intestin est mou, les eceecums au nombre de 5, la vessie aérienne a parois minces et transparentes. fistoire—On en connait plusieurs espéces, toutes de petite taille. Genus DreLectrRuM. Historique.—Ce genre a été établi en 1855, par le Dr. Hol- brook, dans son /ehthyology of South Carolina, p. 32. Type: Serranus fascicularis, Cuv, et Val. ila été accepté par Mr. Gill, Proceed. Acad. Philad., 1862, pp. 236, 237. Caractéres.—I) ne différe du genre /aliperca que par le préo- percule armé de deux faisceaux d’épines divergentes. Le JZ. b¢- vittatus peut servir de transition entre ces deux genres. Etymologie.—as, bis; *aaxrpev, plectrum, que Cuvier traduit éperon. Genus MENTIPERCA. Historique.—Ce genre a été établi par Mr. Gill, dans les Proceed. Acad. Philad., 1862, p. 236. Type: Serranus lucio- percanus, Poey. Caractéres.— Le genre Mentiperca parait bien établi, quoique Vauteur ne lait séparé des Haliperce que par un menton proéminent et le petit nombre de ccecums (deux seulement). - L’avancement de la machoire inférieure, chez les Halzper- c@, a été indiqué par moi; mais ce caractére n’est pas bien re- marquable. I] est bien prononcé chez les Mentiperce, ce qui leur fait un museau plus pointu; Vceil est plus grand. Le crane, au lieu d’étre arrondi, est plat en dessus. Le préorbitaire, trés-développé, couvre tout le milieu de l’os maxillaire, et touche au bord de la lévre. Ouvertures nasales extrémement petites, de la Faune de Cuba. 55 surtout lantérieure, qu’on peut a peine découvrir avec une forte loupe. Sauf ces différences, il a les caractéres des //al?- perce ; je ne suis pas certain cependant que l’on trouve der- riére les premieres dents de la machoire supérieure, la grosse dent qui de chaque cdté se couche en arriére. Ltymologie.—Mentum—Percea. Genus Hyporiectrvs. Fistorique.—Ce genre a été établi par Mr. Gill, Proce. Acad. Philad., 1862, pp. 236, 237 ; type, Plectropoma puella C. et V. Il yest placé dans la famille des Perczda@, sous-famille Serrani- nw. ‘* Dorsale entiere, caudale échancrée, corps oblong, écailles petites, dents couchées en arriére des canines, préopercule ayant en dessous des dentelures dirigées en avant, le dit préopercule denticulé en dessous en forme de scie. D. 16, 14-15. J’ai accepté ce genre dans ma Synopsis, en 1868. L’espéce citée par Mr. Gill est chez Cuvier et Valenciennes le type de leur 3° division des Plectropome, laquelle, outre les dentelures fines du bord montant du préopercule, en montre au bord inférieur de nombreuses, presque aussi fines, mais dirigées en avant. Litymologie.—ixe, sub; xajxzpov, plectrum. Caracteres du genre.—Corps court, comprimé ; cil médioere, haut ; narines rapprochées, plus prés de Veil que du bout du museau. Préopercule finement dentelé a son bord montant, sans échancrure, portant sur son bord inférieur 10 a 12 dente- lures dirigées en avant. Opercule armé de trois pointes épineuses. Bouche bien fendue, la machoire inférieure dépas- sant la supérieure. Langue lisse. Voyez ce qui a été indiqué dans la sous-famille des Serraniné. Dents.——Il] y a aux machoires un rang externe de petites dents coniques, crochues, précédées de deux courtes canines. En ar- riére, sur la machoire supérieure, il y a un rang de dents plus minces, plus nombreuses sur le devant, et qui paraissent cou- ‘ 56 Genres des Poissons chées et mobiles. A la machoire inférieure les dents couchées ne se trouvent que sur le devant. Les dents du vomer sont sur une plaque triangulaire. Nageoires.—D. 10,15; A. 3, 7. La derniére épine dorsale est aussi longue que l’avant derniére ; l’étendue de la partie molle égale, a peu pres, celle de la partie épineuse ; les épines anales sont fortes; la caudale est échanerée. I] n’y a pas de la- niéres membraneuses a Vextrémité des epines dorsales. Ecailles.—Les €cailles sont tortement ciliées, aussi longues que hantes, adhérentes, plus fortes sur les jones que sur les deux piéces postérieures operculaires ; les plus grandes du trone se trouvent sur les flanes, pres de la pectorale ; celles de la gorge sont petites ; il y en a aux tempes, mais non pas sur le crane, Vinteropercule, le limbe préoperculaire, ni le bout du musean, inclus le maxillaire et le dentaire. Il n’y ena pasa Ja mem- brane des ouiés. De tiés-petites écailles s’étendent sur la base des nageoires verticales; il n’y en a pas sur la base des pectorales, Squelette.—Le crane est arrondi a son sommet, |’espace inter- orbitaire médiocre, l’orbite plus rapproché de Vextrémité anté- rieure ; la créte suroccipitale basse et rejetée en arriére; la mastoidienne trés-basse; le nasal bas. Les cinq premiéres vertebres abdominales manquent d’apophyses latérales ; les trois derniéres paires forment l’anneau. Les premieres névrapophyses sont plus fortes et plus courtes que les autres. L’appareil des cdtes se compose de 2 épinévrales, 8 pleurapophyses, 6 épi- pleurales. Le 17 internévral sontient deux ¢pines dorsales. Le coracoidien est tres-échancré vers le bas. L’os pelvien n’a pas d’apophyse ascendante. Viscéres.—Lintestin fait les cireonvolutions ordinaires ; ap- pendices pyloriques au nombre de 5; vessie natatoire a parois minces, quoique opaques; vésicule du fiel allongé. Histoire.—Ce genre parait tres-naturel. Les espéces qui le composent sont assez nombreuses, et de petite taille: environ 5 pouces. de la Faune de Cuba. bye GENUS GONIOPLECTRUS. Historique.—Ce genre a été établi par Mr. Gill, Proceed. Acad. Philad., 1862, pp. 236, 237, parmi les Percida@, sous- famille Serranina, dans la division de ‘ Dorsale entiére, caudale entiére, corps oblong, écailles petites, dents couchées en arri¢re des canines, préopercule portant a son angle une dent plec- troidale dirigée enavant: D. 8. Type: Plectropoma hispa- num, O. V. Je Vai adopté dans ma Synopsis, en 1868. L’espéce citée par Mr. Gill est le type du 2° groupe de Plectropoma de Cuvier et Valenciennes, distingué par le bord montant du préopercule dentelé, n’ ayant au bord inférieur quwun petit nombre de dentelures. Les espéces renfermées dans cette division ne forment pas un groupe naturel, comme le dé- montrent le Pl. chloropterum, le Susuki, le Serratum, le nigro- rubrum, types aunjourd’hui de nouveaux genres. Etymologie.—vyava, angulus ; xaqxzpov, plectrum. Caractéres du genre.—Corps court, cil médiocre, placé haut ; préopercule finement dentelé a son bord montant, pourvu en des- sous d’une forte épine partant de langle et se dirigeant en avant; opercule a trois pointes, celle du milieu extrémement longue et forte. Dents.—Les dents des machoires sont en cardes; il y en asur le devant quelques-unes un peu plus longues, couchées et pro- bablement mobiles ; une seule canine en haut, forte; deux en bas longues et fortes, au milieu de la machoire. Les dents du vomer sur une plaque triangulaire; les palatines sur une bande étroite. Nageoires.—D. 8, 13; A. 3, 7. Les rayons épineux de la dorsale sont assez courts et forts, le dernier plus court que celui qui le précéde ; la partie molle a peu d’étendue relativement a la portion épineuse. Les épines anales sont trés-fortes. La pec- torale est plutot arrondie que pointue. Ventrale retenue par une membrane axillaire. Licailles.—Les écailles sont cili¢es. La ligne latérale se re- 58 Genres des Poissons léve et ne suit pas la direction paralléle au dos. I] y a des écailles sur toutes les pieces operculaires; celles des joues sont petites; il n’y en a passur le crane, qui est apre, ni sur le devant du museau; elles montent sur les nageoires médianes jusqu’aux deux tiers de leur hauteur; il y en'améme quelques-unes sur la membrane épineuse de la dorsale. L’ossurscapulaire envoit au dehors sa lame plate. Squelette.—Malegré la grande différence que présente, au pre- mier aspect, ce genre comparé avec les /ypoplectri, Vexamen du crane révéle entre eux une grande aflinité. Ainsi il est ar- rondi en dessus, la créte suroccipitale est au-dessous du niveau frontal ; les autres erétes sont basses ; la distance interorbitaire médiocre; mais le nasal n’est pas bas. J’ignore si le labial existe. Les apophyses latérales des vertebres abdominales se montrent a commencer de la 7°, les trois derniéres paires formant Vanneau. La 1° névrapophyse chevauche ; les trois qui suivent sont fortes et rejetées en arriére, les quatre autres sont courtes ; celles qui suivent sont normales. Je ne crois pas qwil y ait entre les chairs de fausses épines internévrales. Viscéres.—L’intestin est étroit, et fait les circonvolutions ordinaires. J’ai compté 8 appendices pyloriques, courts et fermes. J’ai trouvé des crustacés dans son estomac. Observations.—Si Von n’avait égard qwa Vépine sous-preé- operculaire, on placerait ce genre a cdté du genre Prospinus ; mais le nombre des épines dorsales et la forme du crane rap- proche ce dernier des Hpinepheli ; tandis que le genre Gonio- plectrus se rapproche davantage des //ypoplectri. Supramiia I].—Lutsanint. Une seule dorsale, la partie épineuse presque entiérement logée dans un sillon du dos. Préopercule dentelé ; opercule sans épines ou n’en portant qu’une plate. Machoire in- férieure peu avancée. Un rang de dents extérieures, solides et plus fortes que les intérieures, qui plus ou moins les } de la Faune de Cuba. 59 accompagnent; des canines sur le devant des machoires. Le premier sous-orbitaire, tres-développé, recouvre en partie Vextrémité postérieure du maxillaire. Pectorale pointue ; dernier rayon de la ventrale attaché a ’abdomen par une mem- brane axillaire. I] n’y pas de lambeau cutané écailleux au- dessus de l’axille pectorale. Mais il y a toujours un lobule écailleux au-dessus de la base de la ventrale. La caudale est échanerée ou bifurquée. Les écailles sont grandes ou médiocres. Le limbe préorperculaire est nu; l’os surscapulaire perce en dehors. Le post-frontal n’a pas d’os caverneux solidement encaissé dans l‘apophyse post-orbitaire. Quand Vos existe, il y est lachement encaissé. La fosse paroccipito-mastoidienne est ouverte et se continue jusq’au frontal. Il n’y a pas d’os labial. Il ya dans les chairs, au-devant de la dorsale, trois fausses épines internévrales. On voit que cest a juste titre que Mr. Gill a formé cette sous-famille, qui se distingue assez nettement de l’antérieure ; en méme temps quelle se rapproche de la famille des Sparoida. Voyez la-dessus ce qu’en dit Mr. Gill, Proced. Acad. Philad., 1862, p. 446, d’aprés les vues de Mr. Troschel. Le genre Lutjanus est le type normal de cette coupe: ¢’est le genre Mésoprion de Cuvier. Voici les genres compris dans cette sous-famille :— 1. Ocyurus.—Species: chrysurus, Bl.—aurovittatus, Ag.— ambiguus, Poey.—lutjanoides, Poey. 2. Phomboplites.—Species : elegans, Poey. 3. Lutjanus.—Species: Caxis, Bl.—Jocu, Cuv.— Caballerote, Bl.— Cubera, Poey.— Buccanella, Cuv.—Aubrieti, Dem.— Ojanco, Poey—profundus, Poey—Campechianus, Poey—ana- lis, Cuv.—rosaceus, Poey. 4. Tropidinius.—Species : Arnillo, Poey. 5. Platyinius.—Species : voraw, Poey. 6. Htelis.—Species: oculatus, Val. 7. Verilus-—Species: sordidus, Poey. 60 Genres des Poissons Genus Ocyurts. fistorique.—Genre établi par Mr. Gill, Proceed. Acad. Philad., 1862, pp. 286, 237, ot il en donne les caractéres suivants, servant a le distinguer des autres genres de Cuba: “ Famille des Percide, sous-famille Lutjanine, caudale bifurquée a lobes trés-aigus.” Le type cité est le Mesoprion chrysurus de Cuvier et Valenciennes. LEtymologie.—axvs, celer ; spe, canda. Caractéres du genre. — Le genre Ocyurus, considéré dans son type, présente les caracteres qui suivent: Corps élégam- ment oblong. Opercule sans épines. Narines écartées, d-peu- prés a égale distance de l’cil que du bout du musean. Bouche petite, la machoire inférieure dépassant un peu la supérieure. Langue Apre. Dents.—Les machoires portent une rangée de petites dents aigues, écartées, sans canines remarquables; derriére cette rangée il y a en haut une bande d’aspérités, ainsi qu’en bas sur la partie antérieure seulement ; il y a des aspérités aux pa- latins et au vomer; ce dernier en présente une plaque rhom- boidale ; les os pharyngiens ont des dents en fin velours. Le premier are des branchies porte de longues ratelures. Nageoires.—D. 10, 18; A. 3, 9. L’étendue de la partie molle de la dorsale est un peu moindre que celle de la partie épineuse. Caudale bifurquée, a lobes trés-aigus, portée sur un pédoncule étroit. Leuwilles.—Elles sont assez grandes, environ 55 le long de la ligne latérale, qui est paralléle au dos; il y en a aux tempes, aux joues, et sur l’appareil operculaire, sauf le limbe du préoper- cule; le reste de la téte en est dépourvu. Squelette.—Le crane, vu en dessus, est large; l’espace inter- orbitaire assez grand et enfoncé; la créte suroccipitale trés- haute, et se continuant avec la créte frontale jusqu’a larticula- tion du nasal. Les apophyses latérales des vertébres abdomi- nales commencent a la 6° vertébre. Le 1° internévral ne soutient de la Faune de Cuba. 61 quw’une seule épine. L’appareil des cotes se compose de 2 épinévrales, 8 pleurapophyses, 6 épipleurales. Viscéres.—Circonvolutions ordinaires ; ccecums au nombre de 53 vessie aérienne longue, opaque, argentée. Genus RHOoMBOPLITES. fistorique—Ce genre a été établi par Mr. Gill, dans tes Proceed. Acad. Philad., 1862, pp. 236, 237; type: Centropristis aurorubens, Cuy. et Val. Il y est mis dans la famille des Per- cide, sous-famille Lutjanine, caudale échancrée, dents vomeé- riennes sur une plaque rhomboidale. Je Vai adopté dans ma Synopsis, en 1868, Etymologie. —feuBos, rhombus ; wares, armatura. Caractéres du genre.—Corps oblong, élégant; cil grand, peu élevé; narines rapprochées, aussi éloignées de lceil que de Vextrémité du museau; préopereule finement dentelé a sa branche montante, bien denté a l’angle et sur la branche infeé- rieure ; opercule 4 une seule pointe épineuse, plate. Bouche petite, machoire inférieure dépassant la supérieure. Langue apre. Dents. de dents aignes, écartées, plus grandes d’avant en arricre, Les michoires présentent extérieurement une rangée 2 mais sans canines prononcées. La rangée d’en haut est accom- pagnée intérieurement d’une bande de dents en cardes fines ; tandis que celle d’en bas n’en a que sur la partie antéricure. Dents vomériennes sur une plaque rhomboidale ; celles des pa- latins sur une large plaque. Pharynx 4 dents en velours. Pre- mier are des branchies a longues ratelures. Nageoires.—D. 12,11; A. 3,8. La partie molle de la dorsale est d’une étendue beaucoup plus courte que celle de la partie épineuse. Caudale bien échancrée. Ecailles. —Elles sont ciliées, de grandeur médiocre, environ 60 le long de la ligne latérale, qui est paralléle au dos. La téte en 62 Genres des Poissons montre jusqu’aux tempes ; la joue en est couverte, aussi grandes qua Vopercule ; il y en a a Vinteropereule, mais pas au limbe préoperculaire. Le reste de la téte en est dépourvu. Le sur- scapulaire laisse voir son bord postérieur en dehors. Squelette—Le crane, vu en dessus, est aplati, le diamétre postérieur grand, ainsi que Vespace interorbitaire. La créte sur- occipitale est haute, se continuant avec la frontale; les autres sont basses. Une large perforation basilaire conduit aux fosses sous-craniennes. L’orbite occupe un espace plus prés de l’extré- mité antérieure que de la postérieure. Sous-orbitaires au nom- bre de quatre. Prétympanal portant une apophyse laminaire. Les apophyses latérales de abdomen commencent 4 la 5° ver- tebre. Il y a de chaque cdté 2 épinévrales, 8 pleurapophyses, 6 épinévrales. La 1° épine internévrale supporte deux rayons épineux. L’os pelvien n’« pas d’apophyse ascendante. Viscéres—Circonvolutions ordinaires. Ccecums, 5. Observations.—On voit que ce qui distingue principalement ce genre de celui que Mr. Gill nomme Lutjanus, c’est le nombre 12 des épines dorsales ; car la plaque rhomboidale du vomer est un caractere commun a plusieurs Lutjans. J’ai pris pour type, quant aux caractéres du genre, le Rh. elegans de Vile de Cuba. Histoire.—Meeurs carnivores ; taille médiocre. Genus Lursanvs. Listorique—Ce genre a été établi par Bloch en 1797, dans son Ichthyologie, Pars 7, p. 324, sous les caractéres suivants: “téte nue antérieurement; préopercule dentelé, opercule sans épines ; museau aigu.” Ila pour premiere espéce son Latia- nus Luteanus du Japon, qui est le M/esoprion Lutjanus de Cuvier, dont les nombres sont: D. 10,13; A. 3, 8. Cuvier, en 1817, avait adopté ce genre; mais il ’a abandonné en 1828, et l’a remplacé par celui de J/ésoprion, parce qu il est de la Faune de Cuba. 63 mélé dans Bloch a des espéces d’autres familles, soit Se?énoides, soit Labroides, et a des Serrans du groupe des Mérous. Si cette raison pouvait étre admise, il faudrait supprimer bien d’autres genres. Mr. Gill, croyant sans doute que le poids d’un grand nom ne saurait nuire a la priorité, a rétabli le genre de Bloch dans les Proceed. Acad. Philad., 1862, pp. 236, 237, comme syno- nyme de Mesoprion, Cuv. Mr. Demarest Vavait déja accepté ; et avant lui, Lacépéde, en ajoutant le caractere de “ une seule nageoire dorsale.” Mr. Gill lui assigne: “ Lutjanine, caudal emarginated, profile straight ; occiput crested.” Son type est le Desoprion griseus, Cuv., qui est le méme que le Lutjanus Canis. Le Dr. Giinther a conservé le nom de Cuvier. Je crois avec Mr. Gill que le genre Liacope, Cuv., soit Genyroge de Cantor, doit étre confondu avec les Lutjani. Etymologie—Du mot Lutjang, que Bloch avait cru du Japon, et qui est malais, selon Cuvier. Bloch écrit en latin Lutianus. Caractéres du genre.—V oici comment je présente les carac- téres du genre Lutjanus, prenant pour type le Jesoprion Caxis, n’ayant pas en mon pouvoir le type cité par Bloch. Corps oblong, un peu élevé; museau aigu; machoire inférieure un peu moins avancée que la supérieure ; opercule finissant en angle mousse et non-épineux ; préopercule presque pas dentelé en dessous. Langue tantot lisse, tantot apre. Dents._-La machoire supérieure a une rangée externe de dents aigues, écartées, les dernicres plus petites ; elle est pré- cédée de deux canines tres-longues ; en dedans il y a une large bande d’aspérités. La machoire inférieure n’a pas de canines remarquables, mais seulement une rangée externe de dents aigues, plus longues que celles d’en haut, et les derniéres plus petites ; en dedans il n’y a quune plaque étroite d’aspérités sur le devant. Les dents du vomer sont tantdt sur un simple chevron triangulaire, tantot sur une plaque rhomboidale qui se 64 Genres des Poissons prolonge en arricre en angle trés-aigu. Les dents pharyngi- ennes inférieures sont en velours ; mais le bord interne en porte une rangée de plus grosses et crochues, ainsi que les os supérieurs. Le premier are des branchies a de longues ratelures. Nageotres.--D. 10, 14; A. 3,8. La caudale est échancrée, mais non pas profondément. Ecailles.—Elles sont ciliées, de 45 a 50 sur une ligne longi- tudinale. Il yen a aux piéces operculaires, aux tempes, aux joues ; mais non pas sur le crane, sur le museau, nisur le limbe du préopercule. Il y en a sur la base des nageoires verticales, partie molle; mais non pas sur la base des nageoires paires. Elles sont d’égale grandeur sur la joue et sur l’opercule. Squelette.—Le crane est étroit en arriére. La créte surocci- pitale plus ou moins élevée; Veil placé au milieu de la longueur cranienne; l’espace interorbitaire étroit; le trou qui livre passage au nerf trijumeau est presque marginal. L’ap- pareil sous-orbitaire porte en tout cing os, dont le dernier paraft articulé sur ’apophyse postorbitaire, mais trés-lachement. I] y a 2 épines épinévrales, 8 pleurapophyses, 7 épipleurales. Le 1* internévral porte deux épines du dos. Visceres.—L’intestin fait les circonvolutions ordinaires. La vessie aérienne est ordinairement solide ; quand ses parois sont minces, elles ne sont pas transparentes. La vésicule du fiel est longue et étroite. Les ccecums, au nombre de 5, mous et courts. Observations.—Ce genre admet quelques subdivisions: ainsi les espéces nommeées Caxis, Jocu, etc., ont de longues canines a la machoire supérieure, et de grosses dents a Vinférieure; en méme temps que les rayons mous des nageoires médianes sont plats, trés-divisés et contigus. D’autres ont les dents moins remarquables, surtout le Lutjanws Ojanco, et les rayons mous peu divisés. Il y a encore des différences a l’égard de la convexité otocranienne. de la Faune de Cuba. 65 Genus TRoprprnivs. Historique.—Ce genre a été établi par Mr. Gill, qui n’en a pas encore fait connaitre les caracteres. Je l’ai adopté dans ma Synopsis en 1868, d’aprés les renseignements manuscrits de auteur, savoir : “ Distinguished by the elevated occipital crest; strengthened by a subvertical rib behind, and the simple paroc- cipital process.” Type: Z. Arnillo, Poey. Etymologve.—rporis, carina; iver, nucula. Caracteres du genre-—Corps oblong. Narines rapprochées, plus prés de l’ceil que de Vextrémité du museau; une seule épine a l’opercule ; préopercule finement dentelé 4 la branche montante et a Vangle, sinueux en dessous; bouche médiocre- ment fendue, machoire inférieure un peu avancée. Langue lisse. Dents.—Les dents des machoires sont courtes et pointues, sur un rang externe; précédées de deux canines en haut et trois en bas. Intérieurement, il y aen haut une bande en velours ras, ainsi qu’en bas; mais ici il n’y en a que sur la partie antérieure. Celles du vomer sont sur un simple chevron transversal, et aux palatins sur une seule ligne. Les os pharyngiens ont des dents en velours en bas, en cardes fines en haut. Le premier are porte de longues ratelures. Nageowres.—D. 10, 10; A.3, 8. La caudale est échancrée ; la ventrale n’a pas de lobe écailleux au dessus de sa base. Eeailles—Environ 60 sur la ligne latérale, qui suit la courbure du dos; il yen a sur la joue, mais non pas sur le limbe du préopercule ; les autres pieces operculaires en sont pourvues ; on en yoit un groupe aux tempes: le reste de la téte est nu. Les nageoires verticales antérieures n’en ont pas. Squelette—Le crane est médiocrement élargi en arriére et sur l’espace interorbitaire; la créte suroccipitale commence vers le milieu de l’orbite; elle est haute, tronquée en arriére ; les deux autres sont basses. La convexité otocranienne ne se montre pas en dehors. L’opercule est arrondi et échaneré MARCH, 1871. 5 Ann. Lyc. NAT. Hist., Vou. X, — 66 Genres des Poissons vers le haut, son épine unique renforecée intérieurement. Cing sous-orbitaires; prétympanal sans apophyse laminaire. Les apophyses latérales abdominales commencent 4 la 5° vertébre, les trois derniéres paires formant Vanneau. Les quatre premiéres névrapophyses sont assez fortes. Le 1° internévral supporte deux épines du dos. L’os pelvien n’a pas d’apophyse interne ascendante. Viscéres.—Ccecums, 5. Observations.—Le nombre des rayons de la dorsale, et la base nue de cette nageoire, ainsi que de l’anale, distinguent principalement ce genre des Lutjani. L’écaille ventrale sur- axillaire manque. L’opercule et le prétympanal offrent encore des différences. Genus Puaryinivs. Ce genre a été établi par Mr. Gill, en 1862, dans les Proceed. Acad. Philad., pp. 236, 237, dans la sous-famille des Lutjanine ; ayant ‘la caudale échancrée, les dents du vomer sur une plaque triangulaire, le profil bossu, occiput plat.” Type: le Mesoprion vorax, Poey. Il rentre dans le genre Anthias de Bloch, ou Serrans barbiers de Cuvier et Valenciennes. Mr. Gill a cependant démontré dans son article sur le genre Litelis, Proceed. Acad. Philad., 1862, p. 447, que sa plus grande affinité est avec les Lutjans, ou Mesoprionsde Cuvier. Je Vai adopté dans ma Synopsis, en 1868. Etymologie.—x«r0s, latus ; iver, nucula. Caracteres du genre.—Malgré la dorsale sans échancrure, qui distingue ce genre, il est tellement rapproché du genre Etelis, que je crois devoir le décrire par simple comparaison (voyez ci-dessous). I] a les caractéres de ce dernier, savoir, la méme colonne vertébrale, les mémes pieces operculaires, l’ceil grand, la bouche bien fendue, le dentaire avancé, la caudale bifurquée, les écailles manquant au-dessus et au-devant de la téte, ainsi qu’aux nageoires, sauf le long des rayons de la de la Faune de Ouba. 67 caudale. Tl s’en distingue par la dorsale entiare et par les détails qui suivent. Le corps est oblong, sans étre élancé ; trongon de la queue plus court, lobes moins inégaux ; le museau plus bombé; l’ceil plus petit, le dentaire moins avancé; le maxillaire et le dentaire sans écailles; le préopercule plus dentelé a Vangle et en-dessous; la partie molle de la dorsale plus étendue; les épines anales plus fortes; le dernier rayon mou de cette nageoire non-divisé ; les écailles plus petites, 60 sur une ligne longitudinale; celles de la caudale plus nom- breuses. Les dents des machoires offrent quelques différences: je les décris minutieusement ici. En haut, il y a d’abord deux ou trois canines, puis vient la rangée externe de dents pointues, au nombre a-peu-pres de 12, et quelques-unes plus petites; dans Vintérieur il y en a une bande en velours ras, plus large sur le devant, ot les plus intérieures sont les plus longues. En bas, il y a d’abord 5 a 6 dents en crochets, plus petites que les canines d’en haut, et elles vont en augmentant de la premiére 4 la dernicre; immédiatement aprés vient larangée de dents externes, plus petites et plus nombreuses que celles d’en haut. Dans Vintérieur, le devant seulement est pourvu d’une bande de dents en cardes fines, dont les plus intérieures sont les plus longues, mais non pas mobiles. Le crane est construit sur le méme modeéle que celui de V Htelis ; il en differe cependant par un frontal plus prolongé, et les deux crétes latérales plus basses, ce qui détache un peu plus la créte suroccipitale. Genus ETELIs. Hlistorique.-—Ce genre a été établi en 1828, par Cuvier et Valenciennes, Poiss. II., p. 127, famille des Percoides; “ ayant tous les caractéres des Perches proprement dites, sauf une rangée externe de dents en crochets, et se distinguant du genre 68 Genres des Poissons Lucioperca par les palatins tout en velours et par ses opercules pourvus de deux pointes.” Le type est le Z. carbunculus, C. V. C’est un démembrement du genre Anthias de Bloch, qui peu-a-peu se trouyera réduit a une seule espéce, le Labrus Anthias, L., Anthias sacer, Bl., dont Rafinesque a fait le genre Aylopon: cette espéce a des particularités remarquables aux dents des machoires et au piéces operculaires; et surtout aux vertebres, qui sont 10-16. Swainson, en 1839, Nat. Hist. of Fishes, ete., I., pp. 168, 202, le présente sous le nom de /tc/les, en ajoutant le caractere de “caudale a lobes inégaux.” II établit en méme temps le genre Hlastoma, qui en differe, selon lui, par les lobes égaux et la nageoire dorsale profondément échancrée, sa partie épineuse plus étendue que la postérieure, l’ceil trés-grand; type, Serra- nus oculatus,C. V. On voit que les illustres auteurs de P Histoire générale et particuliére des Poissons n’ont pas connu la grande aflinité qui existe entre le carbunculus et le oculatus ; ni Swainson non plus. Le Dr. Giinther a suivi exemple de Cuvier et Valenciennes. Mr. Gill a démontré que ces deux espéces appartiennent au méme genre. Le nom de Swainson doit done passer a la synonymie. Il en est de méme du genre /fesperanthias de Lowe, Fishes of Madeira, 1843, puisqu’il prend pour type le S. ocuwlatus, ainsi que Swainson. CO’est encore le genre J/acrops, établi par Mr. Oh. Duméril en 1856, Ichth. analyt., p. 279. I] faut consulter sur ce sujet et sur les caractéres détaillés du genre un bon article de Mr. Gill, inséré dans les Proceed. Acad. Philad., 1862, p. 447, sous le titre de “ On the Synonymy and Systematic Position of the Genus Zéezis of Cuvier and Valenciennes.” Ltymologie.—Nom propre d’un poisson dans Aristote. Caracteres du genre.—J’ai profité du travail de Mr. Gill. j’y ai ajouté quelques autres particularités, principalement celles qui ont été prises sur le squelette. Corps oblong, élancé; racine de la queue longue. Dorsale de la Faune de Cuba. 69 unique, presque double a cause de son échancrure profonde ; Vespace entre les yeux plan, ainsi que Pocciput; museau court, bouche grande; ceil tres-grand ; narines rapprochées, beaucoup plus pres de Poeil que de l’extrémité du museau ; le préopercule n’a pas d’échancrure ; son bord montant est finement pectiné, Vangle et le dessous sont denticulés; lopercule est armé d’une pointe assez forte, Vinférieure n’éxistant pas, la supérieure tres- plate; maxillaire terminant sous le tiers postérieur de Vceil ; machoire inférieure plus avancée que la supérieure; langue lisse. Denis. en crochets, petites, écartées, les premieres d’en haut un peu Les machoires ont une rangée extérieure de dents plus fortes; parmi celles-ci on remarque une canine peu développée en haut, et une plus petite en bas. . liptical shape, in the greater expansion of the sides of the cara- pax, in the non-projecting front, in the concealment of the eyes beneath the orbital margin of the carapax, in the broader and fo) b) non-tapering exognath of the external maxillipeds, and in the ft 5 tes} ’ expanded penult joint and short dactylus of the ambulatory feet. The hepatic region is not distinetly defined, and is not oD e/ , toothed. Uhlias is an American, while Oreophorus is an East Indian genus. Uhlias ellipticus, nov. sp. Of this species I have seen only one specimen, a female, which may be described as follows: Carapax broad, regularly elliptical, rather depressed ; sides much expanded, laminiform; middle of the carapax elevated above the sides, which are depressed. Upper surface, with the exception of the central parts and the lateral expansions, covered with deep, rounded, or elongated pits. The posterior pits are the largest, and six of them, of a pentagonal or rounded shape, are situ- ated on the posterior part of the branchial regions, three on each side. , 5 c equals in width the two tar- FG. 6. Fie, 7. FIG. 8. : 4 : The intermedium in the three figures is saleio; whichrit finally, unites’ seprasented black) 0111 (ae ondo tO Pp eis : Fig. 6. Representing lower portion of To show still more plainly leg of Salamandra maculosa, Copied from : 3 3 Gegenbaur, with distal tarsals omitted. the reasons for believing that Fig. 7. Spizella socialis copied from fig. ae 1, plate iv, of this paper, with intermediwm the pretibial bone of Wyman introduced. Fig.8. Ideal figure showing true position represents the intermedium, Of erence in relation to proximal tar- the following diagrams are Pe pret presented. The intermedium ey eeae: is represented black. Figure 6 represents the intermedium and its associate tarsals in relation to the tibia and fibula of Salamandra maculosa, after Gegenbaur. UW fe 77 152 On the Tarsus and Oarpus of Birds. Figure 7 represents the tarsus of an embryo bird, with the pretibial bone introduced, bearing the same relation that it afterwards does to its own tarsals; and figure 8 repre- sents the pretibial bone and its actual relation to the two tarsals, as seen in Professor Wyman’s oldest specimen, the tibia now having widened so as to include the two tarsals within its lateral boundaries, and consequently including the pretibial bone also. That the tibia widens at its distal extremity in that way, so as to equal in width not only the two tarsals, but the three metatarsals, may be seen by re- ferring to plate 1v; and indeed to suppose that it would do so is reasonable, since the excessive reduction of the fibula naturally enhances the greater proportionate development of the tibia; and by this excess of growth, the pretibial bone, or intermedium, finds its anomalous position in front. of the tibia. ; In connection with this elongated cntermedium, it is inter- esting to note that in certain lizards where the intermedium is absent, the centrale takes on the elongated and slender form, and is wedged between the other tarsals. If further investigation should prove the correctness of this interpretation, we have an interesting stage in the con- ditions of this bone represented, namely, that in birds the intermedium is at first a separate bone, as in the lower rep- tiles, but finally it anchyloses with the astragalus, as in higher vertebrates, thus proving the correctness of Gegen- baur’s statement that the astragalus of higher vertebrates represents the ¢bzale and intermedium connate. Thus we must recognize in birds the presence of four tarsal bones, and at least four carpal bones. ConcLupiInG OBSERVATIONS. — At an early stage of the embryo the leg and the wing are almost precisely alike, and even after the principal bones have made their appearance the two appendages are remarkably alike in the form and proportion of their parts. This similarity was noticed by On the Tarsus and Carpus of Birds. 153 Agassiz a long time ago, as well as the fact that in the embryo robin, the toes are webbed. In the early embryo the toes are always webbed, and for a long time in the embryo all the toes point forward; these are two characters highly characteristic of lower groups of birds. The turning back of the first toe is a subsequent modification. The first metatarsal appears last in development. The phalanges of the third and fourth toes appear first, and the others in regular succession. The phalanges of the foot appear before those of the hand. The metacarpals and phalanges are widely separated in the early embryo, and were it possible for the wing at this stage to make a track in the mud, the impression would be like that made by a tridactyle foot. In fact it is a tridactyle foot at this stage. The metatarsals are also separated at the same stage, but not so widely as the metacarpals. There is a difference of opinion among anatomists in their interpretation of the fingers of the wing. Gegenbaur, Huxley, Rolleston and others, regard the marginal finger on the radial side as representing the first finger, or pollex, while Wyman, Owen and Coues, believe this digit to repre- sent the index, or second finger. It seems more reasonable to believe that this latter interpretation is right; for when the number of fingers or toes is reduced in Mammalia and Reptilia, they are always taken away from the sides of the member, the thumb first disappearing and then the little finger. If we compare the leg and wing of Spizella (figs. 1 and 32, pl. rv and v) we shall see that in this early stage there are but three metatarsals and three metacarpals, and it seems reasonable to compare them together. As the first toe appears much later and is reduced to two phalanges, and has its metatarsal also greatly reduced, and as at the stage just cited the first toe is represented only by a few granules, it seems natural to infer that in the wing, the first finger never makes its appearance. 154 On the Tarsus and Carpus of Birds. In regard to the reptilian characters in birds, it seems that a nearer relation between birds and pterosaurians can be established, with the additional carpals pointed owt in this paper. At least one of the characters for separating the pterosaurians from the birds, as given by Owen, fails in the light of. these distal carpals. Owen says, in his “Fossil Reptiles of the Liassic Forma- hon, that. —— “A carpus with one large and one small bone in a proxi- mal row, and with a second large, and at least one small one in a distal row, is another character by which the ptero- sauria manifest their closer affinity to reptiles than to birds.” Now this is precisely the character of all those birds thus far examined. | EXPLANATION OF THE PLATES. Plate IV. THE TARSUS AND EMBRYOS. In every case the right leg and right wing are represented. For want of room on the plates I have been compelled to leave out the humerus and femur in most of the figures given. : All the embryos are represented of natural size, and by referring to them, an approximate idea may be formed of the size of the appendage drawn, as well as the age and condition of the embryo. Reference to the embryo preceded by the initial E, follows explanation of the figure, thus: Fig. 1, Spizella socialis. WH. 18. Fig. 1. Spizella socialis. HK. 18. The three bones separate, the jibulare being at the end of the jibula. The 2d, 3d and 4th metatarsals not complete, while the Ist metatarsal appears only as a few granules. Fig. 2. Spizella socialis. E. 19. Tarsal joint appearing, in separation of cartilage between proximal and distal tarsal bones. Fig. 3. Turdus fuscescens. E. 21. The tarsals separate. The distal end of tibia widening so as to in- clude the proximal tarsals. * Palxontographical Soc., Vol. XXIII, 1869. On the Tarsus and Carpus of Birds. 155 Fig. 4. Turdus fuscescens. Embryo not given. A later stage in which the proximal tarsals have already united with the tibia, and the distal tarsal has not yet united with the metatarsals. Fig. 5. Turdus fuscescens. Another view of the same. Fig. 6. Tyrannus Carolinensis. HK. 23. The tibiale and fibulare united with tibia, the centrale still free. Fig. 7. Dendreca estiva. KH. 24. The two proximal tarsals united. The centrale very large and capping the three metatarsals. Fig. 8. Dendreca estiva. Another view of the same, showing the tarsal bones more distinctly. Hig. 9. Dendreca estiva. Another view of same, showing centrale capping the metatarsals. Fig. 10. Quiscalus versicolor. EK. 25. The tibiale and jibulare united, but net yet anchylosed to the tibia. The centrale still free. Fig. 11. Quiscalus versicolor. An enlarged view of the tarsus. Fig. 12. Stalia sialis. HK. 31. The proximal tarsals united with the tibia. The distal tarsal united with the fourth metatarsal. Fig. 18. Stalia sialis. Another view of the same. Fig. 14. Cotyle riparia. HE. 27. A considerably advanced stage in which the three tarsal bones are distinctly separate. Fig. 15. Hirundo lunifrons. HE. 30. The ¢ibiale and jfibulare about uniting. The centrale already blended with third metatarsal. Fig. 16. Zringoides macularius. HK. 26. The tibiale and jibulare united forming an hour-glass shaped bone. The centrale flattened and capping the metatarsals but not yet united with them. Fig. 17. Zurdus migratorius. : Posterior portion of early embryo, showing the leg as a simple fin, and caudal vertebre. 156 On the Tarsus and Carpus of Birds. Fig. 18. Spizella socialis. 19. 66 66 20. ce oe 21. Turdus fuscescens. 22. Molothrus pecoris. 23. Tyrannus Carolinensis. 24, Dendroeca estiva. 25. Quiscalus versicolor. 26. Tringoides macularius. 27. Cotyle riparia. 28. ie a Several days from the egg. 29. Tringotdes macularius. Just ready to hatch. 30. Mirundo lunifrons. 31. Stalia sialis. EXPLANATION OF LETTERS. FE. Femur. Too LLOeGhe F. Fibula. ( t. TLibiale = astragalus. TARSUS. y f. Fibulare = caleaneum = os calcis. | ¢. Centrale = navicular = scaphoideum. I, U, Wu, 1v. Corresponding metatarsals. Plate V. THE CARPUS. Fig. 32. Spizella socialis. E. 18. Showing three carpals and three metacarpals. No indication of pha- langes. Fig. 383. Spizella socialis. EH. 19. The fourth carpale now formed; phalanges also formed, and fingers, at this stage widely spread. Fig. 34. Spizella socialis. EH. 20. Third and fourth carpal bones united, and third and fourth metacarpals united at distal and proximal ends. Fig. 35. Spizella socialis. Several days from the egg, and nearly capable of flight. On the Tarsus and Carpus of Birds. 157 Fig. 36. Turdus fuscescens. KE. 21. Showing four carpals. Fig. 37. Turdus fuscescens. A slightly more advanced stage, showing the third and fourth carpal bones about uniting. The fourth carpale sending out a process to third metacarpal. The wlrare apparently uniting with wna. Fig. 38. Turdus fuscescens. The same carpus under slight pressure. The wlnare separate again. Fig. 39. Quiscalus versicolor. EH. 25. Showing the minute third carpale and the elongated ulnare. Fig. 40. Molothrus pecoris. HK. 22. The third and fourth carpale united. Fig. 41. Sialia sialis. Third and fourth carpale about uniting, and fourth carpale sending out peculiar process to third metacarpal. Fig. 42. Sialia sialis. E. 31. A slightly more advanced stage, in which the distal carpals and base of metacarpals are all united. Fig. 48. Cotyle riparia. LE. 27. Anchylosis far advanced. Ulnare supposed to have united with ulna. Fig. 44. Dendreca estiva. EK. 24. Ulnare supposed to have united with the ulna. The carpal marked 7, supposed to be intermedium. Third and fourth carpale united. Fig. 45. Hirundo lunifrons. KE. 30. The four carpals all separate. Fig. 46. Tyrannus Carolinensis. KE. 23. Showing excessively long radiale. Fig. 47. Tyrannus Carolinensis. Another specimen under pressure, with a new carpal? supposed to be centrale. | Fig. 48. Tyrannus Carolinensis. Another specimen under pressure, in which the long wlnare readily separates, leading to the supposition that the second carpale is here present. The peculiar form of ware in Tyrannus, fig. 47, is seen also in Moloth- rus and Sialia, figs. 40, 42 and 48. APRIL, 1872. u ANN. Lyc. NAT. HIST., VOL. X. 158 On the Systematic Arrangement of EXPLANATION OF LETTERS. H. Humerus. vu. Ulna. r. Ltadius. (u. Ulnare = cuneiform. r. Ladiale = scaphoid = naviculare. | ce. Centrale = central. CARPUS. < i. Intermedium = lunar. {| z. Second carpale = trapezoid. 3. Third carpale = magnum. 4. Fourth carpale = unciform. 1, UI, 1v. Corresponding metacarpals. IX.— On the Systematic Arrangement of North American Terrestrial Mollusks. By THOMAS BLAND AND W. G. BINNEY. Read January 29, 1872. SINCE the publication of our work on the Land Mollusks of North America,* we have had the opportunity of examin- ing the animals and the lingual dentition of many additional American, as well as numerous foreign species. We have also carefully studied the various systems of classification which have been proposed both here and abroad. The re- sult of our researches is a considerable change in our views regarding the classification of terrestrial mollusca. Such of these changes as relate to the American families, we pur- pose stating here, referring always to the page of our work containing the description or statement to be modified. *Land and Fresh-water Shells of North America, Part I. Smithsonian Institution, Feb., 1869. , North American Terrestrial Mollusks. 159 We restrict our corrections and suggestions to the genera belonging to the fauna of North America, exclusive of that of Mexico and Lower California. The divisions A and B (p. 2) of Dr. Gray (founded on the head, eye-peduncles and tentacles being retractile under the skin, or contractile) cannot be retained, as the recent observations of Stoliczka have proved the eye-peduncles of Onchidium to be really retractile. The same may possibly be true of Veronicella. The sections 1, Vermivora and 2, Phyllovora are equally untenable. There is not the difference in food indicated by these names. For instance, no species can be more carnivo- rous than Stenogyra decollata, which is always placed among the herbivorous genera. Limax maximus, also, we have known to devour its kind, though it is ranked in the same section. The first instance shows how incorrectly the aculeate marginal teeth alone are called of carnivorous type, as they are entirely wanting in Stenogyra decollata. The presence or absence of a jaw is not a reliable char- acter to sustain the distinction of these sections. Helix tneequalis, for instance, has no jaw. The teeth are equally unreliable, inasmuch as all our species of Macrocyclis, placed in section 2, have teeth like those described in section 1. So have Helix inequalis, Hyalina Baudoni and Gonospira palanga. Moreover, some genera show a gradual change from the so-called herb- ivorous to the so-called carnivorous type of teeth. Thus in Glandina and Macrocyclis we find the carnivorous type only ; in Zonites, Vitrina and Limax the marginal teeth are carnivorous, and occupy the greater part of the membrane, but the few laterals are of the herbivorous type. In Zonites cellavius the latter are greatly’ modified and resemble closely the carnivorous type. The membranes of Vitrina limpida and Zonites chersinus, however, by the increased number of laterals and the bifurcation of the marginals, are more nearly related to the herbivorous type. Thus, instead of the differ- 160 On the Systematic Arrangement of ence of food, of the presence or absence of a jaw, of the aculeate or quadrate form of teeth, supposed to exist between the Vermivora and Phyllovora, we find these characters shared irregularly by both sections, and consequently we abandon them. OLEACINID (p. 13).—In the description of the teeth the term aculeate, rather than recurved, better expresses their thorn-shaped outline. In our descriptions of the lingual “membranes, we have often called these teeth wneini, and with less judgment used the same term for the quadrate marginal teeth of some of the elicide. It would be better in all cases to retain the names central, lateral and marginal for the three forms of teeth. CYLINDRELLID&.—We no longer consider this a distinct family. Even while our work was passing through the press the presence of a jaw was discovered by one of us.* We also misapprehended the character of the teeth, which have since proved to be simply a modification of the form usual in the Helicide. We propose, therefore, to place the species referred to Cylindrellide, and also of Macroceramus referred to Orthalicine, in the family Helicide, before the genus Bulimulus. Messrs. Crosse and Fischer (Jour. de Conch., January, 1870), after a thorough study of the jaws and lingual mem- branes of numerous species, proposed to separate the Cylin- drellide as a family, supporting their views entirely upon the jaw and teeth, both of which we have found unreliable. The kind of jaw supposed by them to be peculiar to the family has been detected by us in various species of Bulimu- (uss, and, inoue, Ofelia (see Amn. liye, IN. HoN)) Weex 79). The type of palmate teeth, also, which Messrs. Crosse and Fischer describe as characteristic of the family is not constant, as we find it entirely wanting in Macroceramus Gosset. (See American Journ. of Conch. vii, pl. 17, figs. SD salels, be) * Bland, Amer. Jour. of Conch. IV. 1868. North American Terrestrial Mollusks. 161 CYLINDRELLA (p. 22).—In dhs genus there is a jaw, thin, almost membranous, light horn color, semitransparent, arched, ends but little attenuated; in one single piece, but divided by delicate ribs into numerous oblique plates,* chevroned on the central line, with a median triangular plate at the top; cutting edge simple; no beak. The teeth are not joined two by two at their bases. They are distinct as in the other //elicidw. The centrals are small, long, narrow, with a broadly recurved, blunt, rounded and expanded apex; the laterals have a long, subquadrangular base of attachment, bearing, below, a large, bluntly rounded, greatly expanded, palmate cusp, representing the inner and central cusps of the laterals; and, above, a long, slender, graceful cusp, representing the external cusp of the other Helicide. This last is bluntly truncated, or bears a re- curved cusp, smaller but of same shape as that below; or it has a laterally extended, small, blunt point. In some species the laterals extend to the margin of the lingual membrane ; in others there are distinct marginal teeth, long, narrow, laminar, with bluntly recurved apices. A full description and figures of these various forms of teeth will be found in Journal de Conchyliologie, Jan., 1870. Houxospira (p. 24).— Messrs. Crosse and Fischer, in the article on Cylindrellide, referred to above, have shown that Holospira is a distinct genus from Cylindrella. The jaw is arcuate, about the same shape as in Cylindrella, thin, light horn colored, without separate plates or anterior ribs; with obsolete strie, transversal and vertical; cutting edge simple, without a median beak. The lingual membrane wants entirely the chevron-shaped rows of teeth and the palmate form of cusp, characteristic of Cylindrella. It resembles that usual in the //elicide, the lateral teeth not unlike those we have figured of Lulimulus pallidior (Ann. Lyc. N. H. of N.Y., ix., p. 282). * As in Helix turbiniformis, not as in Orthalicus. (See Ann.N.Y. Lyc., X., 79, pl. ii. fig. 2.) 162 On the Systematic Arrangement of The genus Holospira, with the two species H. Léemert and HH. Goldfussi, must be placed, together with Oylindrella and Macroceramus, as already mentioned with regard to those genera, in the family Helicide. Macrocreramus.— In this genus the jaw and lingual mem- brane are as in Cylindrella, and our description (page 219) must be cancelled. In MW. Gossez, however, the teeth are the same as in felix, with bluntly pointed denticles, one long and the other short, as shown in our above referred to figure. Henicipm (p. 25).—More recent investigations have satisfied us that the presence of a mucus pore is not in itself a character to warrant the separation of the Arionide as a family. It has been shown that the pore exists, with various modifications, in many species of Geophila where it was not before suspected, for instance in Helix pylaica, Glandina ligulata (Petenia, Crosse, Journ. Conch. 1869, p. 35), Glan- dina monilifera (Morelet, ibid., 1852). Unless, then, we are prepared to consider these species as belonging to a family distinct from //elix and Gilandina respectively, we cannot separate the Arzonide from the Helicide on account of the presence alone of the mucus pore. The description of the foot of Helicide (p. 25) should be modified by the addition of the following words: “or with a distinct locomotive disk,” and “ or with a caudal mucus pore.” To the description of the jaw must be added the words “or with one upper, accessory plate. Jaw sometimes want- ing.” The last reference is necessary to embrace such cases as Helix inequalis, a species, however, which may be proved to belong to another family. As a basis for grouping the large number of genera of Flelicide into subfamilies, we retain the characters of the jaw and teeth, but with some modifications, as shown in the following synopsis. The subfamily Pup7ne is entirely sup- pressed, as it has been shown that no reliance can be placed on the median beak-like prominence to the cutting edge of North American Terrestrial Mollusks. 163 the jaw, or on the presence or absence of striz or ribs on its anterior surface, at least as subfamily characters. We have recognized, therefore, at present three forms of jaw only, viz.: lst, simply in one piece; 2d, in one piece, with an upper accessory plate; 3d, in numerous separate, free, im- bricated pieces. Some modifications even in these distine- tions will, we believe, soon prove necessary, as several forms of accessory plate have already been noticed,* and the jaw of Punctum, figured by us on p. 222, is a modification of that of Orthalicus figured on p. 215. We admit two distinctions on the lingual membrane for the purpose of grouping the genera into subfamilies, viz. : marginal teeth conical, separate, aculeate; and marginal teeth crowded, quadrate, dentate or serrate. Based upon these characters we propose the following grouping of the North American genera of Helicidee :t VITRININE. Jaw in one piece. Marginal teeth separate, conical, aculeate.— Macrocyclis, Zonites, Hyalina, Vitrina, Limax. Hevicinm. Jaw in one piece. Marginal teeth crowded, quadrate, dentate or serrate.— Arion, Ariolimax, Binneia, Patula, Helix, Holospira, Cylindrella, Macroceramus, Buli- mulus, Cionella, Stenogyra, Pupa, Vertigo. ORTHALICINE. Jaw composite, in numerous, free, im- bricated pieces. Marginal teeth crowded, quadrate, dentate or serrate.— Orthalicus, Liguus, Punctum. SuccININ!. Jaw in one piece, with one upper accessory plate. Marginal teeth crowded, quadrate, dentate or serrate. — Succinea. Subfamily Virrinin® (p. 25).—The following description is to be substituted for that given : Jaw in one piece, smooth, usually striated, never ribbed, * See Eucalodium, Journ. de Conch., 1870, pl. v, fig. 1. + Gill, in fact, embraces in his section Holognatha, all the genera included in our sub- * families Vitrinine and Helicine with the exception of Bulimulus, regarding which he adopts the views of Albers and von Martens, placing it in the section Goniognatha, with Orthalicus. (Arrangement of the Families of Mollusks, Washington, 1871.) 164 On the Systematic Arrangement of with a beak-like median projection to its cutting edge. Lin- gual membrane, with separated, conical, aculeate marginal teeth. Genus Hyauina (p. 29).—We have already stated our views relative to the value of the caudal mucus pore as a family character, and in consequence unite the Arionide to the Flelicide. This brings the genus Zonites next to the genus Hyalina. The two genera are very nearly allied, their only distinction, so far as known to us, being in the presence in Zonites of a distinct locomotive disk to the foot, and of longitudinal furrows along the side of the animal near its base, rising over the top of the tail and uniting above a ter- minal mucus slit or pore. (See fig. 524, p. 292.) This difference is considered of generic value by most authors,* among others by Albers and v. Martens, whose descriptions of genera we adopted in our work. They place, however, in the genus //yalina many species which are known to possess the mucus slit (or some modification of it), as /7. olivetorum and H. nitida (see Moquin Tandon), and ZH. JSuliginosa, levigata, inornata, suppressa (see Terr. Moll. U.S., ii). We have ourselves observed it in the following additional species, 77. cellaria, viridula, indentata, intertexta, ligera, demissa, capsella, lasmodon and multidenta, and in Zonites kopnodes, sculptilis and gularis. Its having been overlooked by many European authors in so common a species as cellariat leads to the supposition that it really exists also in other species now referred to Hyalina. We propose, therefore, to place in the genus Zonites the species in which the caudal mucus pore or slit has been actually observed, restricting /Zyalina to those without it. We have not had an opportunity of examining all the species, but have failed to discover any pore in Tennessce specimens, * But not by Messrs. Fischer and Crosse in their magnificent work ‘‘ Etudes sur les Mollusques Terrestres et Fluviatiles du Mexique et du Guatemala” (page 150), where Zonites and Hyalina are considered generically identical. + No mention of the caudal mucus gland in Z. cellarius is made in the monographs of Draparnaud, Moquin-Tandon, Reeve, Forbes and Hanley, Gray or Gwyn Jeffreys. North American Terrestrial Mollusks. 165 received from Miss Law, of H. interna; it may, however, have escaped our notice, being often difficult of detection. The orifice of generation in the genus Zonztes is said to be at the base of that of respiration, below the collar, and not below the right eye-peduncle as in Helix. It may be much doubted, however, whether this be a constant generic charac- ter, as it is found in some species of the former much nearer to the head than the collar. The dart sac and dart were observed by us in specimens of Zonites demissus and Z. Hiliotti. They have also been noticed by Mérch (Moll. Dan.) in Zonites ( Oxychilus) nitidus. The description of Albers and v. Martens must therefore be modified, as well as Moquin Tandon’s assertion that no species of Zonites has the dart.* Subfamily Hericrxa.—The following description is to be substituted for that given at p. 67. Jaw in one piece, either smooth, striated, or ribbed, with or without a median beak-like projection to its cutting edge. Lingual membrane with crowded, quadrate marginal teeth, either dentate or serrate. The ribs are found in every degree of development, pass- ing quite across the jaw and denticulating one or both margins, or only developed on the lower portion of the jaw, and crenellating the lower margin. The ribs are often al- most obsolete, or represented by wrinkles or coarse striz. They are present on the anterior surface of the jaw only, or on both anterior and posterior surfaces. They are distant, narrow, stout, few, or crowded, broad, stout and numerous. Their number is inconstant in the same species. They some- times are very broad, and seem like separate plates soldered to the anterior surface of the jaw, or to be formed by a folding of the jaw upon itself. When this appearance of folding into plaits is given it will generally be found that the plait-like sections are actually separated by distinct, but * Hence, probably, Draparnaud correctly reports its presence in Helix algira. 166 On the Systematic Arrangement of delicate ribs. When by this form of ribs the jaw is divided into separate compartments, these compartments or plates are either vertical or inclined obliquely towards the median line of the jaw. Sometimes this last arrangement is de- veloped to such a degree that the oblique lines of separation, or delicate ribs, of the plates meet before reaching the bottom of the jaw, and a triangular plate is left at the upper centre of the jaw, its base being upward. This form of jaw is usually thm and membranous. It has been considered the characteristic of the subfamily Orthalicine, or of the Goni- ognatha by most authors. We, however, can treat it only as a modification of the usual form of ribbed jaw, inasmuch as we find it in various degrees of development in Bulimulus, Bulimus, and even in Helizx.* It will be seen below that we restrict the Orthalicine to those genera whose jaw is in actu- ally free, imbricated pieces. When the jaw is striated and not ribbed, the striz are vertical, or they converge towards the median line, as do the plates in Macroceramus and Cylindrella. There are often transverse striz also. The upper margin of the jaw is often extended into a stout membranous attachment, apparently of the same mate- rial and consistency as the jaw itself, and showing the same continuity of structure by the striz of the jaw extending into it without interruption. The jaw is found in every degree of consistency, very thick in most species of Helix, quite membranous and almost transparent in some of Bulimulus, in Macroceramus and Cylindrella. The cutting margin of the jaw is smooth, crenellated, or denticulated. It is simply concave, or furnished with a more or less developed beak-like median projection. In shape the jaw ranges from scarcely arcuate, long, low, to horse-shoe shaped, short, high. * See our notes on Helix turbiniformis in Ann. N. Y. Lyc. x, pl. ii, fig. 2. North American Terrestrial Mollusks. 167 We have not noticed in any of the Helictde the vertical median carina to the jaw, often present in the Vitrinine. PatuLa (p. 71).—We propose to recognize this as a genus, following the more recent decision of von Martens (Preuss. Exp. p. 258). It will take precedence of the genus Helix. To the description of the shell and animal already given, we may add that in the American species the jaw cannot be said to be ribbed, as usual in Helix. On that of several species, however, there are subobsolete ribs or wrinkles near the cutting edge, which they sometimes crenel- late. The prevailing type of jaw seems to be such as we have figured for P. alternata (p. 75). Lingual membrane as figured on p. 75. The marginals, however, are serrate in P. asteriscus. In the other species they have one long, inner, oblique, blunt denticle, and one or more short, side denticles. For the description of the jaw and lingual membrane of the genus Helix (p. 69) may be substituted the descriptions given by us above for the jaw and lingual membrane of the subfamily HHelicine. We have noticed in the genus Helix, as now constituted, every form of jaw which we have de- seribed at length above, except that having angular upper median plates. With the exception of Patula, we still retain the genus Helix in the sense in which it is used by Albers and von Martens. With all those who have studied the genus, we are aware that it contains numerous natural groups, many of which appear to be sufficiently well marked to warrant their being recognized as distinct genera; space, however, does not permit of our considering this part of the subject. Genus BuLimuLus (p. 191).—To the description of the jaw must be added, ‘‘ often presenting the appearance of separate plates, sometimes arranged obliquely towards the central line, so as to form an upper triangular plate, as in Cylindrella.” This last form is usually thin and almost transparent. 168 On the Systematic Arrangement of Subfamily Orruanicina (p. 212).—The following de- scription of the subfamily must be substituted for the one given. Jaw composite, in numerous free, imbricated pieces, usually with oblique sutures towards the centre of the jaw, leaving an upper, angular, median piece. No median pro- jection to the cutting edge, which is. serrated by the lower angles of the separate pieces. Lingual membrane with mar- ginal teeth crowded, quadrate, usually broadly dentate. It will be observed that we include only in this subfamily the genera whose jaw is actually in separate pieces, not those in which the jaw is in one single piece, though in plates formed by the ribs being arranged so as to give the appear- ance of separate pieces. We do not, moreover, use the term Orthalicine in the same sense as Goniognatha of some authors to comprise all the genera whose jaw has an upper angular, median plate. This last form of jaw is found in Cylindrella, Macroceramus, Pineria, and in some species of Bulimulus, but not in Punctum. We do not recognize it as of value in dividing the Helicide into subfamilies. We base this subfamily (Orthalicinew) solely on the free, imbri- cated pieces of its composite jaw. The description of the genus Achatina (p. 212) is to be entirely omitted. We adopt Liguus as a genus, and add the following description of the jaw and lingual membrane. Jaw arcuate, ends attenuated, pointed; composite, being in numerous separate, free, imbricated, triangular pieces, with sutures inclined obliquely to the centre of the jaw, so as to leave an upper median, angular piece. Cutting edge with no median projection, serrated by the lower angles of the oblique pieces. Lingual membrane with long, quadrate teeth, pointed or simply with a broad, recurved cusp. OrtHaLicus.—The following description of the lingual membrane must be substituted for that given at p. 215. Long, broad, with numerous rows of long, four-sided, North American Terrestrial Mollusks. 169 narrow, uniform teeth, bearing a broad, expanded, recurved, gouge-shaped cusp. Genus STENOGYRA (p. 228).—Central teeth of the lingual membrane very small, tricuspid ; laterals large, subquadrate, tricuspid, middle cusp very large; marginals subquadrate, obtusely denticulated. Subfamily Sucornmy® (p. 255).—To our description of the lingual teeth must be added, ‘* marginal teeth quadrate, crowded, dentate or serrate.” ; ? Note on Helix inversicolor Fer. and other species from Mauritius. While the foregoing paper was being printed, we had, through the kindness of Mr. J. G. An-hony, of the Museum of Comparative Zoology, Cambridge, and of Mr. J. H. Thomson, the opportunity of examining the animals of //elix enversicolor Fer., FH. leucostyla Pfr., HZ. rufozonata H. Ad. and HT. militaris Pfr., received from Mr. Pike, the United States Consul at Mauritius. The results of such examination are so interesting that we now publish them. H. inversicolor and H. militaris are placed by v. Martens in fHelicacea, genus Helix, the former in the section Caraco- lus, and the latter in Stylodon, but both, as well as ZH. rufozonata and leucostyla, rather belong to Vitrinea, genus Nanina of that author’s classification. Indeed oug figure of the lingual dentition of Manina cabias, Benson (Am. Jour. of Conch. vii, pl. 17, fig. 6), almost equally well applies to the species under consideration, as will be seen from the following description of their dentition. The jaws stout, arcuate, high, ends slightly attenuated, blunt; anterior surface with no ribs; cutting edge with a decided, blunt, median projection. t Lingual membrane long, broad. Central and lateral teeth in horizontal rows, in shape as usual in the Helicide. Mar- ginal teeth in oblique rows, aculeate, bluntly bifid, decreas- 170 Monographie des Poissons de Cuba ing in size as they pass off laterally. In Helix militaris there is about an equal number of laterals and marginals. The resemblance of these species to the genus WVanina holds good also in the external characters of the animal. The tail is long, gradually tapering towards a blunt extrem- ity, which is bifid, being separated into two distinct pro- cesses by a transverse, triangular, deeply-seated, mucus pore. There is a distinct locomotive disk to the foot. Down the centre of the back of the foot is a distinct line, from which the granulations run obliquely down to a horizontal line of furrows bordering the edge of the foot. This horizontal line rises over the extremity of the tail, above the process which overhangs the mucus pore. These species must certainly be removed from the genus FHlelix, and even from the Helicine, and placed among the Vitrinine in the genus Vanina. X.— Monographie des Poissons de Cuba compris dans la sous-famille des Sparini. PaR FELIPE POERY, PROFESSEUR D’ HISTOIRE NATURELLE A WUNIVERSITE DE LA HAVANE. ET MEMBRE CORRESPONDANT DU LYCEE D’HISTOIRE NATURELLE DE NEW YORK. = Présenté le 29 Janvier, 1872. FPaMinga SPARIDI. La famille des Spares est fondée sur le genre Spars d’Artédi, Genera, p. 35; adopté par Linné et caractérisé principrlement par des molaires rondes en forme de pavés sur les edtés des machoires. C’est proprement la premiere tribu de Cuvier, Regne Animal II, p. 181, qui répond aux groupes Pagrina et Sargina du Dr. Gunther, Catalogue, I, p. 412. Ce genre a été conserve par Bloch et par Lacépéde, compris dans la sous-famille des Sparini. 171 qui y ont fait entrer un grand nombre d’espéces qui ne lui appartiennent pas, surtout le dernier. F Cependant, Cuvier place dans la méme famille d’autres tribus qui n’ont pas de molaires arrondies, et qui forment principalement le groupe Cantharina du Dr. Gunther. [la done fallu exclure les dents des caracteres essentiels et eénéraux de cette famille. Les Sparidi sont des poissons a corps oblong et comprimé ; ventrales 1, 5; trois épines anales; piéces operculaires sans armure; bouche non protractile, palais sans dents: écailles cténoides de médiocre grandeur, n’en ayant pas aux na- geoires ; queue sans bouclier; les os de la téte sans caverno- sités ; coecums peu nombreux. Je passe sous silence d’autres caractéres importants, parce qwil y a des exceptions dans quelques sous-familles ; je m’étendrai davantage dans celles de Cuba. C’est a tort que Linné accorde a ces poissons des pectorales arrondies. Observations. —Je sépare des Sparidi le groupe Pimelep- terina du Dr. Giinther, parce quwil a sept rayons branchios- teges, et des écailles aux nageoires verticales. Le régime herbivore et les nombreux appendices pyloriques, le rap- prochent des Chétodons, pres desquels Cuvier l’a place. Sous-familles de Cuba.—1. Sparini; 2. Sargini. SuBFAMILIA SPARINI. Cette sous-famille répond au groupe Pagrina du Dr. Gin- ther; caractérisé par des dents coniques sur le devant des michoires, suivies en dedans d’un groupe de dents en cardes ; des molaires rondes sur les cétés. Le préorbitaire, tres développé, couvre en partie le maxillaire ; “la langue est lisse. Dorsale unique, dont la partie épineuse peut se loger dans un sillon du dos. Il y asix rayons branchiosteges. Caudale fourchue, pectorale pointue. Régime carnivore. 172 Monographie des Poissons de Cuba Nous pouvons diviser cette sous-famille ainsi qu’il suit : . J. Premier interhémal non taillé en forme de bec de plume a écrire. 1. Plusieurs rangs de dents molaires. a. Des dents coniques fortes sur le devant des machoires. ft» Maxillaire'nonrenile:.Wt. yoni) Seeareer tos Ame Snonrusa hae Tie Maxillaire renilé,). 2.0402 (a6) ob.20-) ia) A dithognathus, Swe b. Des dents coniques faibles sur le devant des machoires , Pagellus, Cuv. 2. Deux rangs de molaires, canines fortes . . . . . Pagrus, Cuv. 3. Un seul rang de molaires, canines médiocres AO OUCSHECAILEUSES mm) isl enn lnen le eS DCEO doOnal GEhite b. Joues sans écailles . . . ‘ Se oe een co COMMING (Oliv. II. Premier interhémal taillé en forme de bec de plume a écrire. 1. Plusieurs rangs de dents molaires, pectorales longues, dépassant l’anus, canines plus ou moins fortes . Calamus, Sw. 2. Unrang de moins aux molaires, pectorales courtes, ’ natteignant pas lanus, canines faibles . Grammateus, Poey. Les genres Chrysoblephus et Argyrops de Swainson restent, le premier parmi les Spares, le second parmi les Pagres. Le genre Sparus a été établi en 1738, quoique avec une signification plus étendue, par Artédi, Genera, p. 35; ayant pour type le Sparus aurata de Linné. Accepté par Linné, avec la méme ¢étendue, il a depuis servi de type 4 une famille divisée en plusieurs genres, dont aucun n’a conservé le nom primitif, .contre Tusage des classificateurs; excepté chez Swainson, qui la bien a tort appliqué, en 1839, a un groupe de Sparoides sans molaires arrondies. C’est aujourd’hui pour tous les auteurs le genre Chrysophrys de Cuvier, Regne Animal, IT, p. 181, 1829; nom que la loi de la priorité nous oblige a faire passer sous le joug de la synonymie. Cuvier et Valenciennes ont fait entrer dans le genre Pagel- lus les especes des Antilles, qui sont toutes pourvues de plume, du moins celles de Cuba; mais Mr. Guichenot, dans sa Févision du génre des Pagels, les en a séparé pour les placer dans le genre Calamus de Swainson. De méme que les Sparint sans plume ont été divisés en plusieurs genres, d’aprés le nombre et la forme de leurs dents, compris dans la sous-famille des Sparini. 173 il parait que nous devrions aussi diviser les Sparini 4 plume d’aprés les différences analogues et non moins remarquables de leur dentition. Mais malgré ces différences chez les pois- sons 4 plume -de Cuba, je ne me trouve pas disposé & intro- duire de nouvelles coupes génériques aux dépens du genre Calamus; ayant toutes le désavantage de ne pouvoir traduire au dehors le caractere général, qui consiste dans une modifi- cation de Vinterhémal, servant d’entonnoir a la vessie nata- toire. On verra cependant que j'ai fait une exception. Genus CALAMUS. Historique. —Ce genre a été établi par Swainson, en 1839, dans The Nat. Hist. of Fishes, Amphibians and feptiles, UU, p-..221, comme sous-genre de Chrysophrys, ayant pour type le Pagellus calamus de Valenciennes, dans Cuv. et Val. His- toire des Poissons, VI, p. 206, pl. 152; sous les caractéres suivants: “Head very large; profile abruptly oblique ; dor- sal fin slightly emarginate in the middle; the second anal spine hollow and shaped as a pen; pectoral large.” La seconde épine anale est sans doute un dapsus de Vauteur, qui a voulu dire le deuxiéme interépineux, lequel soudé au pre- mier, est creusé en entonnoir pour recevoir la vessie aérienne. Mr. Guichenot (1868) adopte ce genre dans sa Révision du genre des Pagels, et lapplique, sans distinction de dents, & tous les Sparoides & plume de la sous-famille des Sparini. Etymologie. — Calamus, plume & écrire. Caracttres du genre. — Corps élevé vers la nuque, ceil haut, museau oblique, anus arrieré; bouche petite, machoire inférieure un peu arriérée ; symphyse sans pores, membrane branchiostege narrivant pas a. Varticulation de la machoire inférieure; narines pres de Veil, rapprochées, Pouverture postérieure sur une fente longitudinale, oblique, Pantérieure tres petite. Le maxillaire prolonge 4 son angle antérieur une éminence, qui forme une corne a l’extérieur. Dents. — Le devant des machoires porte un groupe de May, 1872. 12 ANN. LYC. NAT. HIST., VOL. X. 174 Monographie des Poissons de Cuba dents en cardes, qui avec lage deviennent grenues; le rang extérieur est toujours plus robuste, et se compose de dents plus ou moins coniques et crochues, quelquefois trés fortes, comme des dents canines, et alors en petit nombre. Les dents latérales sont arrondies en pavé, sur trois rangées principales en haut et deux en bas; la seconde d’en haut est formée de tubercules plus petits. Celles du troisieme rang, en haut, et du second en bas, sont les plus grosses, surtout celles du fond de la bouche. Il y a encore une ou deux courtes rangées de tubercules plus internes, qui deviennent plus nombreux dans lage adulte, mais qui existent toujours. Les premieres molaires de la rangée externe ont leur cou- ronne un peu conique, quoique courte. Le nombre de séries dentaires donne a la bouche un diamétre plus grand que dans le genre qui suit. Les dents pharyngiennes sont en cardes fortes et courtes. Nageotres.— La dorsale a onze piquants, sa portion molle a peu d’étendue ; l’anale est beaucoup plus longue que haute , la ventrale est sans membrane axillaire, et porte au-dessus de sa base une écaille lancéolée; la pectorale est longue et pointue, atteignant l’anale. Ecailles.— Les écailles ont leur bord libre presque entier. La téte en est dépourvue, sauf aux pieces operculaires; il y en a un groupe étroit sur la joue, et non pas sur le limbe du préopercule ; il n’y ena pas aux nageoires. L’écaille sur- scapulaire, extrémement amincie, est a peine visible en de- hors; de la part une série d’écailles qui remontent oblique- ment sur la nuque, et qui sont fortement striées. Squelette.—Je prends pour type de cette déscription le Calamus Bajonado. Le crane, vu en dessus, est médiocre- ment élargi en arriére et entre les deux orbites. La eréte suroccipitale est haute, et son angle est aigu: les deux autres crétes sont tres-basses. L/’orbite, rejeté en arriere, laisse un espace tres court pour la cavité encéphalique. L’apophyse préfrontale est trés saillante, et percée en dessus d’un trou aveugle infundibuliforme, portant des points d’articulation , compris dans la sous-famille des Sparini. 175 hauts et aplatis. L’apophyse préfrontale n’existe pas: ily a plus bas une lame qui limite l’orbite en arri¢re. Les ouver- tures externes du nerf trijumeau sont marginales; la pos- térieure trés-grande, percée sur une votite horizontale de Yalisphénoide; il y a de plus un petit trou au-dessus des deux cavités, tres rapprochées, qui recoivent l’épitympanal. La convexité otocranienne n’est pas visible en dehors. La base du sphénoide descend beaucoup et se bifurque ; plus en avant, il y a une grande échancrure, et son bord devient tranchant, & cause du grand amincissement du préfrontal et du nasal; celui-ci porte au-dessus la fosse naso-vomérienne. La fosse paroccipito-mastoidienne est ouverte. La _ fente basisphénoidale est bien marquée. L/’ouverture antérieure du crane est ample. Le conduit supérieur de louie pénetre par le paroccipital et sort par un trou de Vexoccipital, rendu complet par une échancrure du mastoidien. Le conduit latéral pénétre dans le mastoidien et aboutit aux mémes échancrures. L/’otolithe est petit et allongé; n’ayant aucune communication avec la vessie natatoire ni avec la cavité abdominale: le Dr. Giinther indique cette communication dans le genre Sparus, Catal. I., p. 23; mais je ne lai pas trouvée dans les sparoides de Cuba. Les sous-orbitaires sont au nombre de six; les deux pre- miers, trés-amincis, recouvrent l’os maxillaire, qui n’a point de labial. Il y a deux surtemporaux. Le symplectique, ou mésotympanal, bifurqué en bas, appuye une de ses branches sur lhypotympanal, et ’autre sur le préopercule. Le pré- tympanal n’a pas de lame apophysaire. L’urohyal est bifurqué. Vertébres, 10—14. Les apophyses latérales commencent des la premiere, et vont en augmentant; l’'anneau commence a la huitieme. La premiere névrapophyse chevauche; la seconde est courte; celles qui suivent ne se distinguent pas beaucoup des autres. Les cétes sont: 2 épicentrales, 8 pleurapophyses, chacune avec une épipleurale, dont les der- nieres sont plutot des épihémales;'il y a de plus une épi- 176 Monographie des Poissons de Cuba centrale sur les trois premieres vertébres caudales. La premiére épine internévrale soutient deux rayons épineux. Il y a trois fausses internévrales suspendues dans les chairs. Le second interhémal, soudé au premier, est creusé en forme de plume. Visceres. — L’intestin fait les circonvolutions ordinaires. Ceecums peu nombreux. Vessie natatoire fibreuse et forte. — Division.—Les espéces de Cuba, renfermées dans le genre Calamus (aprés en avoir séparé le genre Girammateus), peuvent ¢tre divisées en quatre groupes, dont je vais donner les caractéres, en y rapportant nos especes. 1°. Ce groupe, pour le nombre des molaires et par la nature des dents coniques, répond parallélement au genre Sparus (Chrysophrys des auteurs), trois fortes canines de chaque cdté, hors du plan des dents en cardes.—C. Bajonado. 2°, Une forte canine oblique ou horizontale, & la machoire supérieure ; dos tres-élevé.—C. megacephalus. 3°. Dents coniques faibles; entre elles, une plus forte, verticale.— CQ. orbitarius; C. 579. 4°. Toutes les canines faibles. Ce groupe répond aux Pagels.—C.. macrops. Calamus Bajonado— Vulgo Bajonado. Planche VI., fig. 1.—L’individu représenté a 210 millimetres de long. Les dents sont d’un individu adulte. Parra, p. 13, tab. 8, f. 1. Bajonado. Sparus Bajonado Bloch, Syst. Ichth., p. 284.—1801. Sagra, Atlas MSS., tab. 538. Bajonado. ? Pagellus penna Valeng@iennes, in Cuy. et Val. Poiss. VI., p. 209.—1830. Guichenot, in Sagra, ed. hisp., p. 187. Pagellus penna. Pagellus caninus Poey, Memor. Cuba, II., p. 468.—1861. ? Guichenot, Rév. des Pagels, p. 114. C. penna.— 1868. Poey, Synopsis, p. 318. Sparus Bajonado; Repert. II., p. 160. Caractéres essentiels.—On le reconnait &’ son museau_ pro- longé, légérement arqué en-dessus, son ceil assez grand. Les dents canines sont longues et fortes, ordinairement au nom- bre de trois & chaque machoire. C’est de toutes les especes compris dans la sous-famille des Sparini. 177 de Cuba celle qui devient la plus grande; car les autres ne dépassent pas un pied de long. Le dos est médiocrement élevé; la hauteur entrant environ 3 fois dans la longueur totale ; chez les individus de 8 pouces, l’ceil entre 13 fois dans la longueur totale; 15 fois chez ceux de 12 pouces. La plume est d’un diamétre médiocre, son bec long. Les lobes de la caudale sont plus aigus que chez les autres espéces du méme genre. La joue porte rarement sur le devant des écailles des traits de coloration. Détails divers.—Les deux premiéres épines de la dorsale sont faibles. Les rayons mous sont peu branchus aux nageoires médianes ; les premiers de la pectorale sont simples. Les os mandibulaires sont violets. D. 12, 12; A. 3, 10; trois ccoecums courts et laches. Couleurs.—Le trone est gris de plomb tirant un peu sur le violet; & reflets dus aux contours jaunatre des écailles. La téte en-dessus est olive assez foncé sur toute la partie nue; les cétés du museau sont bronzés, rarement parsemés de traits bleus, les écailles des joues en partie dorées. Une bande bleue entoure le dessous de lceil. La commissure des lavres est orangée, passant quelquefois au violet. Les nageoires sont piles. Il y a au-dessus de l’axille pectorale un espace doré. L/iris est nuancé de brun et de jaune. On trouve souvent, dans un Age peu avancé, des bandes brunes verticales au nombre de 5 4 6 sur le trone, et des bandelettes sur la caudale. Variétés Vage.—J’en ai décrit dans les caractéeres du genre. Chez un individu de 185 millimétres, les dents canines n’ont pas encore atteint la force que ’on remarque chez les adultes ; mais elles n’ont pas perdu leur caractéres, ni la petite série interne des molaires. Comparaison.—Le Calamus penna présente la synonymie que jai déjaé indiquée avec doute. Valenciennes. décrit un individu de 6 pouces: Mr. Guichenot n’en a vu que de 80 a 180 millimetres. A cet Age, la hauteur est moindre, les canines sont moins robustes, les bandes verticales existent 178 Monographie des Poissons de Cuba accidentellement. Mr. Guichenot rapporte ce poisson au Bajonado de Sagra, qui appartient évidemment A notre espéce, par la forme du corps, et surtout par celle de la téte. I] lui ressemble encore par la joue, sans traits particuliers de coloration. Cependant, on peut douter que le OC. penna soit le véritable Bajonado; pareeque, au dire de Cuvier et de Guichenot, il a l’ceil petit et la caudale peu fourchue. Le Dr. Giinther le porte avec doute & la synonymie du Ohryso- phrys calamus. Observations. I] est trés remarquable que le Sparus Bajonado de Bloch, ni la figure de Parra, 4 laquelle elle se rapporte, ne soient pas cités dans louvrage de Cuvier et Valenciennes, dans celui du Dr. Giinther ni dans la Révision des Pagels de Mr. Guichenot. , Histoire.—Ce poisson est commun et sain, quoique médio- crement estimé: il arrive au moms 4 un pied et demi de long. On le péche & peu de profondeur. J’ai trouvé dans ses intestins du sable et des débris de mollusques, ainsi que des fucus. Numéro 468 de mon Atlas manuscrit. Calamus megacephalus — Vulg. Pez de pluma. Pagellus calamus Valenciennes, in Cuy. et Val. Poiss. VI., p. 206, tab. 152.— 1830. Calamus megacephalus Swainson, Nat. Hist. Fishes, II, p. 222.— 1839. Giinther, Catal. I., p. 187. Chrysophrys calamus. 1859. Guichenot, Rév. des Pagels, in Mem. de la Soc. Imp. des Sciences Nat. de Cherbourg, vol. XIV., p. 112. Calamus megacephalus.— 1868. Poey, Synopsis, p. 208. Sparus calamus; Repert. I., p. 314. Caractéres essentiels.—Le dos est trés-élevé; la hauteur — du corps n’entrant pas deux fois et demie dans la longueur totale. La michoire supérieure porte une dent canine forte, dirigée obliquement en avant, au milieu d’autres moins ro- bustes. L’ceil est grand, ‘entrant 14 fois dans la longueur totale, chez un individu de onze pouces. La couleur de la compris dans la sous-famille des Sparini. 179 peau sur les cétés du museau, est caractéristique. La plume est large, son bec long. Details divers.—Cecums, 4. Vessie aérienne forte, ayant dans Vintérieur de nombreux corps rouges. La bifurcation caudale est peu profonde, lobes élargis. Couleurs.—La couleur générale résulte de celle des écailles, qui ont le centre verdatre doré et les contours bleus ; elle s’éclaircit en dessous. Les écailles du préopercule sont blanches, bordées de jaune; le limbe est violet. L’isthme est orangé. La téte est brune en dessus. Les cdtés- du museau ont des taches rondes jaundtres sur un fond bleuatre métallique. Les levres sont en partie jaunes, avec du bleu sur la commissure. Un trait bleu entoure l’ceil en dessous. Les nagevires sont @un jaunatre pale; pectorales rose. Iris mélé de brun et de jaune. Comparaison.—Le Calamus pennatula de Guichenot, Rév. des Pagels, p. 116, de la Martinique, est trop bas pour ap- partenir 4 la méme espece; car auteur dit que sa hauteur n’a pas le tiers de la longueur totale : elle n’y entre pas meme deux fois et demie chez un individu de Cuba de méme taille. Observations.—I| est trés-bien representé dans louvrage de Cuvier et Valenciennes; mais il y est peint trop rouge. Histoire.—Il est rare. Le plus grand que j’ai vu est un pied de long. On le trouve aussi & Bahia, Trinité, Jamaique (Gthr.), Martinique (Val.), Saint Domingue (Guich. ) Numéro 475 de mon Atlas Mss. s) Calamus orbitarius— Vulg. Pez de pluma. Planche VI., fig. 2. Individu figuré: 310 millim. Pagellus orbitarius Poey, Memor. Cuba, II., p. 201.—1860. Synopsis, p. 308, Sparus orbitarius.—1868. Guichenot, Réy. des Pagels, p. 128, Calamus orbitarius.— 1868. Caractéres essentiels.—Museau peu prolongé, hauteur con- tenue deux fois et trois quarts dans la longueur totale; cil 180 Monographie des Poissons de Cuba | médiocre, contenu 15 fois dans la dite longueur, sur des in- dividus de 10 pouces; une dent canine verticale médiocre- ment forte & la michoire supérieure, au milieu d’autres plus faibles. Plume large, bec trés-court. Un trait bleu anté- oculaire. Lobes de la caudale élargis, la bifurcation médio- crement profonde. Q&il plus brun que jaune. Details divers.—D. 12, 12; A. 3, 10 quelquefois 3, 11. Vessie fibreuse, renforeée en dessous: son intérieur laisse voir la premiére vertebre 4 découvert. Ccoecums 4. Couleurs.—La couleur générale résulte de celle de chaque écaille, qui est d’un bleu foneé au centre, jaundtre doré pale au pourtour; celles des joues sont blanches. La partie nue du museau est jaune doré sale, les cOtés parcourus par des traits bleus circulaires; la bande sous-oculaire est bleue, ainsi que la préoculaire. Les lévres sont d’une teinte violette ; Yisthme est jaune. I] y a sur le trone brachial une tache bleue. Les nageoires sont jaundtres. Il y a dans l’ceil du brun et du jaune: c’est le brun qui domine. On le trouve quelquefois avec des bandes brunes verticales sur le tronc, peu prononcées, ainsi qui sur la caudale. Comparaisons.—Ce n'est pas le Calamus pennatula, Guich. Rév. des Pagels, p. 116, dont la machoire supérieure est munie de deux dents canines proclives en avant. ¥ Ce nest pas le Calamus plumatella, Guich. Réy. des Pagels, p. 120; lequel est moins haut, le profil du museau moins vertical, l’ceil plus grand, les canines de la machoire supérieure toutes égales et fortes, joues sans traits de colora- tion, caudale bordée postéricurement de brun ou de noiratre. Ce n’est pas le Calamus penna Val., in Cuv. et Val. Poiss. VI., p. 209; Guich. R..des P., p. 114, dont, la hauteur, est moindre, la joue sans traits de coloration, dents et plume distincts. La caudale est moins fourchue et ses lobes sont obtus. Il y a une bande verticale qui descend & travers l’ceil sur la joue. Erratum.—Je dis dans mes Mémoires que la quatriéme serie de molaires de la machoire supérieure n’existe pas dans compris dans la sous-famille des Sparini. 181 cette espéce: cest une erreur que j’ai corrigée dans ma Synopsis. FHistoire.—L’espeéece est commune, et n’atteint pas un pied de long. J’ai trouvé dans l’estomac des débris de Mollusques, des astéries et des annélides. Numéro 149 de mon Atlas Mss. Calamus macrops — Vulg. Pez de pluma. Planche VII., fig. 8. Individu figuré: 220 millim. Caractéres essentiels.—Le corps est haut, sa hauteur con- tenue deux fois et deux tiers dans la longueur totale; et Veil contenu 13 fois: le tout chez les individus de 10 pouces. Les dents canines sont faibles, au nombre de 5 & 6 de chaque cété, et dégale force. Plume d’un diamétre médiocre, son bee plus long que le tuyau. Elargissement et bifurcation de la caudale médiocres. Il n’a pas de bandelette bleue anteé- oculaire. Voyez plus bas la couleur des yeux. Couleurs. —Gris de plomb, avee une tache bleu-clair au centre de chaque écaille du tronc. La téte est olive assez foncé en dessus, doré verditre sur les cétés, parcourus par des traits bleus. Bande sous-oculaire bleue. La michoire inférieure est bleuitre, commissure jaune. Isthme couleur de paille. Nageoires piles. Un point bleu axiilaire au dessus de la base de la pectorale. I] y a dans l’eil du brun et du jaune: c’est le jaune qui domine. Comparaison.—Quoique par la grandeur de l’eeil il se rap- proche du Calamus plumatella de Mr. Guichenot, plus que le CO. orbitarius, ce nest pas encore la méme espéce, par les raisons déja exposées. IL s’en sépare davantage par les canines de la michoire supérieure. Histoire.—Ce poisson est commun. No. 221 de mon Atlas Mss. Calamus 579. Caracteres essentiels.—Il ne differe du Calamus macrops 182 Monographie des Poissons de Cuba que par les dents, qui sont comme chez le C. orbitarius. La plume est large, son bec long. Ce nest pas le Calamus plumatella Guich. dont il est ques- tion aux deux espéces antérieures. Je ne donnerai un nom & cette espéce, qu’aprés en avoir vu un grand nombre d’individus. Genus GRAMMATEUS. Ce genre ne differe du Calamus que par les dents molaires, qui manquent de série interne; laquelle, chez ce dernier genre, forme le quatricéme rang en haut, et le troisieme en bas; et de plus, par la pectorale courte, n’atteignant pas Vanus. Etymologie.—ypepparévz, scriptor. Grammateus humilis— Vulg. Pez de pluma. Sagra, Atlas Mss., tab. 51.—1834. Salgo (lege Sargo). Pagellus microps Guichenot, in Sagra, ed. hisp., p. 188, tab. 3, fig. 1 (dentibus molaribus erroneis). 1843. Pagellus humilis Poey, Synopsis, p. 308.—1868. Guichenot, Rév. des Pagels, p. 118. Calamus microps.— 1868. Giinther, Catal. I., p. 417. Pag. microps. 1859. Details divers.—Le sixiéme sous-orbitaire n’est pas en- caissé. La corne du maxillaire est 4 peine sensible. D. 12, 12; A. 3, 11. L’eil est contenu 21 fois dans la lon- gueur totale, et la hauteur du corps 3 fois; le tout chez un individu de 275 millimétres. La plume est d’un diamétre médiocre, le bee plus long que le tuyau. L’intestin est étroit, sans strangulations. Ccecums, 4. Vésicule du fiel prolongée ; lobe gauche du foie plus long que l’autre. Mon nom spécifique se rapporte & la nageoire anale, qui est tres basse. Couleurs. Plombé verdatre. Il y a au milieu de chaque écaille un reflet plus clair; les bords sont verditres: celles des joues sont d’un doré pale. La machoire inférieure est compris dans la sous-famille des Sparini. 183 violette. La pectorale est jaunitre, la ventrale tirant sur le violet; les autres nageoires d’un verditre pile. Une tache de bleu foncé sur la partie supérieure de la base de la pec- torale. La bandelette bleue sous-oculaire peu prononcce. Il y a dans Viris du rouge et du brun. Observations.—Mr. Guichenot, dans Pouvrage de Sagra, a la priorité; mais il l’a perdue par la description erronée des dents molaires, qu’il dit étre sur deux rangs 4 la machoire supérieure ; ce qui m’a empéché de reconnaitre lespece. Il a corrigé erreur dans sa Révision des Pagels, publiée dans le 14° volume des Mémoires de la Société Impériale des Sciences de Cherbourg, de 1868. Ma livraison du Repertorio, qui contient ma Synopsis, est de Mars 1868. II est vrai que, dans ma Synopsis, j’ai commis aussi une erreur, que je corrige plus bas; mais Mr. Guichenot n’ayant pas encore connaissance de mon travail, comme on peut le remarquer dans sa page 123, il n’a pas pu étre par moi égaré dans la dé- termination de lespéce. Errata.—Dans ma Synopsis, p. 309, ligne 4, il est dit qu’on trouve de moins la petite rangée de molaires inter- médiaires ; lisez internes. Et ligne 17, ot il est dit que les molaires sont sur deux rangs, non séparés par un rang de petites dents intermédiaires, lisez trois rangs en haut et deux en bas, ces derniéres non séparées par un rang intermédiaire. Fistoire.—L’espece n’est pas rare, sans é¢tre commune, Sa taille est d’environ 10 pouces. Numéro 288 de mon Atlas Mss. Grammateus medius — Vulg. Pez de pluma. Planche VIL., fig. 4. Individu figuré: 180 millim. Oaractéres essentiels.—Il| differe. du Grammateus humilis par un ceil plus grand, contenu 17 fois dans la longueur totale, chez un individu de 273 millimétres, et 16 fois chez un de 180 millimétres. La plume est beaucoup plus étroite, le bec plus long que le tuyau. 184 Descriptions of New Species of Details divers.—La corne du maxillaire est 4 peine sensi- ble. Ligne lat. 45. Varictés.—J’ai dans un exemplaire D. 12, 12; A. 3, 10; dans un autre A. 38, 14. Dans wn individu, je ne découvre pas la bande bleue sous-oculaire. ; Histoire.—I] vest pas rare, sans étre commun. Quelques pécheurs le nomment Sargo, quoique ce soit un poisson & plume. Le plus grand que j’ai vu est de 12 pouces. Numéro 192 de mon Atlas Mss. XI.— Descriptions of New Species of Birds of the Genera Icterus and Synallaxis. BY GEO. N. LAWRENCE. Read April 22d., 1872. Keterus formosus. a Male. Throat, space in front of the eye and a broad band across the back black; the rest of the plumage of the body is of a beautiful reddish- orange; tail black, the outer two feathers on each side end narrowly with dull white, the bases of the feathers concealed by the coverts are light yellow, with that portion of their shafts white; quills brownish-black, the smaller wing coverts are deep orange, the upper row ending with black, the middle coverts are white, the larger are black with the terminal half of the margins of their outer webs white, the primaries have their outer webs at the base white for a short space, forming a spot, beyond which they are narrowly edged with white, the secondaries have their outer margins broadly white; under wing coverts orange, inner webs of quills for two-thirds their length from base grayish-white; ‘‘iris brown; bill black, base of lower mandible and feet light plumbeous.” Length (skin) 8 in., wing 44; tail 8; bill from front 4; tarsi +2. The female has the upper plumage of a dull yellow, brighter on the front; the back is olivaceous, on which part the centres of the feathers are black, giving it a distinct spotted appearance, somewhat as in J. pus- tulatus; the tail is greenish-olive; the throat is black and the under plumage of a clear bright yellow. A young male has the yellow coloring more orange, with the centres of the dorsal feathers black, but the spots are much larger and closer than Birds of the Genera Icterus and Synallaxis. 185 in the female. A young male of J. pustulatus before me, has the back similarly marked, but the spots are smaller and the upper plumage is more olivaceous. The general plumage of the adult female and young male of J. pustulatus, is much duller and more olivaceous than that of the new species of corresponding sex and age. ; Habitat. “Tehuantepec (Tuchitan).” Collected by Prof. F. Sumichrast. Type in Museum of Smithsonian Institution. Remarks. The adult male above described, was in a col- lection recently received from Prof. Sumichrast, the others were in his former consignments and have been considered I. pustulatus, the markings on the back of the female and young male being somewhat like those of that species; but the two are shown to be very distinct on comparing the adult males—the back of the present species is crossed by a broad black band, whereas that of Z. pustulatus is orange, the centres of the feathers marked with narrow ovate spots of black; in the new species the deep orange color above continues without change until it joins the black of the back, in J. pustulatus the deep color is restricted to the fore part and sides of the head. This species really comes nearest to the bird from Guatemala named J. sclatert by Mr. Cassin (which he says is J. mentalis, Scl. nec Less.) ; from this it differs in being smaller and of a much deeper orange color, the outline of the bill is more curved, that of J. sclatert being nearly straight ; the bases of the feathers which form the black mantle are white tinged with yellow in J. sclater?, in J. formosus they are grayish-white except immediately adjoining the black ends of the feathers, where they are orange, this color showing a little on the edges of the feath- ers of the upper part of the mantle. This bird is almost a miniature of Z. gularis, differing only in the mantle of that species being of a uniform black, and having the bases of the black feathers grayish-white, with- out any portion of them yellow. 186 New Species of Mollusc of the Genus Helicina. Bymaliaxis paaculata. Head above and hind neck brown, back brownish-rufous, rump and upper tail*coverts rather brighter; tail rufous with a blackish wash on the inner webs of the two central feathers at their ends; superciliary streak white; throat, breast, sides of the head and of the neck grayish- white, the throat is immaculate but the feathers of the other parts have blackish- brown centres, giving them a very distinct spotted appearance; abdomen and under tail coverts light rufous; quills blackish-brown, wing coverts and edges of inner quills bright rufous; false wing black; bend of wing. white; under wing coverts grayish-white tinged with rufous, inner webs of quills for their basal half of a very light salmon color, their ter- minal half edged with light rufous; upper mandible dark brown, the under yellowish-white, dusky at the end; tarsi and toes dark brown. ~ ‘ Length (skin) 53 in.; wing 2; tail 22; bill 34; tarsi +2. Habitat. Provinee of Tumbes, Peru. Type in Museum of Vassar College, Poughkeepsie. It was ina small collection received by Prof. Orton and placed in my hands for examination. —emarks. In colors and general appearance this species resembles S. guéanensis, but the wings are shorter; S. gui- anensis is darker below and has the tail of a deeper rufous, without the dusky markings on the ends of the central feathers ; the new species can easily be distinguished by the decided superciliary stripe, and the small spots on the sides of the head and of the neck, and on the breast. XII. Description of a New Species of Mollusc of the Genus Helicina. BY THOMAS BLAND. Read April 22nd, 1872. Melicina gloymei, nov. sp. T. subglobosa, tenuis, pellucida, pallide cornea, epidermide lineis spirali- bus, confertis, pilosulis induta, sub epidermidem nitida, striatula, lineis microscopicis concentricis decussatula; spira parum elevata, apice acuti- cuscula, rufescente; anfr. 45, convexiusculi, ultimus rotundatus, seri- New Species of Mollusc of the Genus Helicina. 187 ebus 5 angustis fusco-pilosis longioribus ornatus, basi impressus; colu- mella breviter recedens, compressa, alba, callum tenuem, album -emittens ; apertura vix obliqua, semicircularis; perist. tenue, margine dextro brev- iter reflexo, basali cum columella angulum formante. Opere. ? Shell subglobose, thin, pellucid, pale horn colored, with epidermis hav- ing closely set spiral lines of short hairs, beneath the epidermis shining, delicately striate, and with microscopic spiral lines; spire slightly ele- vated, apex rather pointed and tinged with reddish color; whorls 44 rather convex, the last rounded and ornamented with five spiral series of longer dark hairs, base impressed; columella shortly receding, com- pressed, and with thin white callus over the umbilical region; aperture scarcely oblique, semicircular; perist. thin, the right margin slightly reflected, basal margin forming an angle with the columella. Diam. maj. 9, min. 7, mill. Alt. 5, mill. Habitat. Newcastle, in the Parish of St. Andrews, Jamaica, West Indies, at an elevation of about 4,000 feet above the sea. Remarks. This interesting species is very unlike any other hitherto found in Jamaica. It has the hirsute char- acter of Alcadia hirsuta C. B. Adams, of that island, and in that respect, as well as in general form has, to a remarkable degree, the aspect of a Schasicheila, without, however, the incised peristome. Iam indebted for this, as well as many other species, to my valued correspondent Mr. C. P. Gloyne, R. E., who refers to it, the specific name having been communicated by me, in his Notes on the Land Shells of Jamaica, Jour. de Conchyliologie XII, p. 44. January, 1872. 188 Notes on Specimens of the Corbiculade. XIII.— Notes on specimens of Corbiculade in the Cabinet of the Jardin des Plantes at Paris, and on the authorship of the Encyclopédie Méthodique. BY TEMPLE PRIME. Read May 6th, 1872. I had the opportunity, in 1871, of making notes on some of the Corbiculade in the Jardin des Plantes, which I am induced to publish in the hope that their perusal may lead to the correction of some errors prevalent in regard to the species of this family. Cyremna orientalis, Lamarck. This species, described in 1818*, is represented by a single valve, which I found to agree with the shell which I publishedt under the name of Corbicula Japonica. — Lamarck’s species is represented as coming from China, nine is a native of Japan. We cannot, however, decide as yet positively that the orientalis and the Japonica are identi- eal, for the reason that Lamarck refers to bis type as being in his own Cabinet, which is at present at Geneva. LIER < fos Corbicula Japonica. Cyrena trumcata, LAMArckK. Lamarck in his deseriptiont of this fossil species stated that it came from the State of New York. There is one valve of the ¢runcata which evidently belongs to the Tertiary ; it is intermediate between antiqua and cunedformis of Ku- rope. | As already stated on a previous occasion § I doubt the fact of this species having been found in N. Y., but think * Lam. An. v, 552, 1818. + Ann. Lyc. N. H.N. Y. viii, 68, f. 15, 1864. $ Lam. An. v, 553, 1818. § Smith. Inst. Misc. Coll; Prime, Monog. Corb. 7, 1805. Notes on Specimens of the Corbiculade. 189 that, if it came from America at all, which I hardly believe, as it is so unlike any of our known fossil Cyrene or rather Corbicule, it is a native of one of our Southern States. The truncata is labelled as having been purchased from the collection of Valenciennes (the father of the late Prof. Valenciennes). Cyrena oblonga, Quoy. M. Deshayes has stated* that this species, a native of Vanikoro, has a sinus. .I called attention + to this fact, remarking that it was the only instance on record of a non- American Cyrena possessing a sinus, qualifying my state- ment, however, with the reservation, that I had never seen any specimen of oblonga. On an inspection of the specimen of the oblonga at the Jardin des Plantes, I detected at once that the so-called Cyrena was nothing more or less than a Glauconome. I am enabled consequently to uphold the proposition, that none of the non-American Cyrene have an unbroken pallial impression. Cyrena placems, Han Ley. Elsewhere t{ I have quoted Mr. Hanley to the effect that there was a specimen of this species at the Jardin des Plantes. As the placens is not personally known to me, I sought for the specimen in question with some eagerness 5 unfortunately, it was not tobe found. Note on the “Encyclopédie Methodique.” Being frequently obliged to consult this work, I was much puzzled to know whether the name of the genus, in many cases a new one, at the top of the plate, was the only evi- dence of the publication of the genus, or whether ‘there *Lam. An. Desh., edit. ! t Ann. Lyc. N. H.N. Y., viii, 420, 1867. ei t Smith. Inst. Misc. Coll. Prime, Monog. Corb. 21, 1865. May, 1872. 13 ANN. Lyc. NAT. HIST., VOL. X. 190 Notes on Specimens of the Corbiculade. existed some published record of the same not so widely distributed as the plates of the Encyclopédie, and to clear up my uncertainty I entered into correspondence with M. Crosse the manager of the Journal de Conchyliologie, M. Crosse wrote me that to make the information the more authentic he had consulted M. Deshayes, who had been one of the contributors to the Encyclopédie Méthodique. M. Deshayes sent him the following, which I have trans- lated. “We owe to Bruguiére all the plates of Natural History “of the Encyclopédie Méthodique relating to the Vers, “except the last hundred for which we are indebted to Lam- “arck. The names of the genera printed at the top of the “plates are the only indications which exist relating to these “useful creations, which the author would have placed on “record in text, had not a premature death prevented him “from so doing. With reference to the existing text, Brue “ouiére published one volume, which ends with the genus “Conus. It was in 1828 that I was entrusted with the fin- “ishing of this text; my first volume commences with a sup- “plement to the letters a, b, ¢; it was published in 1830; “my second volume is of 1832; so that the text of the “Encyclopédie Méthodique” concerning Mollusca is com- “posed of three volumes, one by Bruguicre and two by me.” (Extract from a letter addressed to M. H. Crosse by M. Deshayes, Nov. 24th, 1869.) Note sur ? Anatomie des Cyrénes Américaines. 191 XIV. — Note sur? Anatomie des Cyrénes Américaines. PAR Dr. P. FISCHER DE PARIS, MEMBRE CORRESPONDANT DU LYCEE D’ HISTOIRE NATURELLE DE NEW YORK. Read May 6th, 1872. Mr. Temple Prime de New York m’a adressé une certaine quantité d’animaux de Cyrénes appartenant & deux espéces qui représentent les types les plus tranchés des Cyrénes Américaines: Cyrena Carolinensis, Lamarck, et Cyrena Floridana, Conrad. I] était important d’examiner ces Mollusques, qui paraissent s’éloigner sensiblement des Cyrenes de l Ancien Continent et. de celles de l’Océanie. Les Cyrénes Américaines du groupe de la Cyrena Caroli- nensis, présentent un caractére tres remarquable ; ’impression pulléale forme un sinus étroit et allongé; ce caractére les distingue, & premiére vue, des autres Cyrénes, ott le sinus palléal est rudimentaire. La Cyrena Floridana peut étre considérée comme le type des espéces saumatres, rostrées, minces, dont le sinus & peine indigué rentre dans le cas général. _ L’animal des Cyrénes est peu connu. Mr. Gray a donné les caractéres de celui des Batissa ; * jai pu moi-méme décrire celui des Corbicula,t mais les autres groupes étaient restés inconnus jusqu’’ présent, au point de vue de Panatomie. C’est done grace aux envois de Mr. Prime, que Pou peut aujour- (hui combler une partie de cette. lacune. Cyrena Carolinensis. Mollusque giobuleux, a manteau * Brit. Mus. Cat. Conchif., p. 234, 1854. t J. Conchyl., XI, p.5. Ann. Lyc.N. H., N. Y., VIII, p. 422, 1867. OCTOBER, 1872. 14 ANN. LYC. NAT. HIST., VOL... x 192 Note sur ?Anatomie des Cyrénes Ameéricaines. assez mince, ouvert depuis le muscle adducteur antérieur jusqu’au dessous du muscle adducteur postéricur, ol une cloison réunit les deux feuillets, pour constituer en arriére la cavité des siphons, assez petite d’ailleurs, par suite du faible développement de ceux-ci. Les bords du manteau sont minces, simples; en dedans un repli porte de tres petits tentacules a peine visibles & la loupe. En haut le manteau constitue une créte s’insinuant dans la charniere et percée de trous qui correspondent aux dents cardinales, et qui reproduisent leur forme. Le muscle adducteur antérieur des valves est semi-lunaire ; Vadducteur postérieur est ovoide et surmonté par un faible rétracteur du pied, laissant une empreinte peu profonde sur la coquille. ; Le muscle palléal est assez large, mais ses fibres sont peu denses et rayonnent en faisceaux plus ou moins espacés. Vers le bord inférieur de Vadducteur postéricur on voit se détacher les fibres du rétracteur de larri¢re-cavité des siphons. Ces fibres forment deux faisceaux distincts: lun inférieur, se portant jusqu’aé la base de la cavité des siphons; Vautre supérieur, rayonnant en éventail et remontant vers le haut du bord postérieur de ’adducteur postérieur des valves. Le muscle yrétracteur des siphons, quoique allongé, est remarquablement étroit ; sa direction est presque horizontale. Il se compose de cing ou six trousseaux de fibres minces et aplaties. Sa longueur et son étroitesse le distinguent des muscles analogues chez les autres Cyrénes, qui sont toujours extrémement courts, et de ceux des Galatées qui sont tres larges et bien développés. Les siphons petits, étroits, sont désunis dans leur longueur ; le siphon supérieur ou anal est plus étroit et plus conique que Vinférieur; son extrémité libre ne porte pas de tuber- cules bien évidents. Le siphon branchial, au contraire, est -pourvu (une couronne de tentacules peu nombreux et cylin- _driques. Li serait & désirer que l’on put dessiner ces siphons durant Ja vie de Panimal et au moment de leur épanouisse- Note sur ? Anatomie des Cyrénes Américaines. 193 ment; ils doivent alors. dépasser sensiblement le bord postérieur de la coquille. Ils sont relativement plus longs mais aussi plus étroits, que ceux des Corbicula dont la saillie est & peine appréciable. Dans [alcool ils sont musculeux, rigides et de coloration plus foncée que celle du manteau. Les palpes labiaux petits, triangulaires, & base peu large, portent des sillons rapprochés sur les deux faces qui sont en contact, c’est a dire, sur la face interne du palpe externe et sur la face externe du palpe interne; les sillons des palpes sont beaucoup plus gros que ceux des branchies. Les branchies sont larges et bien développées ; la branchie interne dépasse l’externe en avant du tiers de sa largeur; elle se soude & la masse viscerale sur une ligne oblique d’avant en arriére et de haut en bas. La branchie externe est attachée & la méme ligne d’insertion oblique que interne, mais non par son bord postérieur. En effet, cette branchie est divisée par la ligne @’insertion en deux parties dont l’an- térieure est’ plus grande que la postérieure ; il s’en suit que la branchie externe est libre dans presque toute sa périphérie et qwelle ressemble aux deux feuillets d’un livre ouvert; le dos du livre représentant la ligne d’insertion. La disposition des branchies est identique chez les Gala- tea, Corbicula; chez ces divers Mollusques les branchies semblent étre au nombre de trois de chaque coté, si lon considére comme une branchie distincte la portion postéricure ou réfléchie de la branchie externe. La structure des branchies des Cyrénes montre qu elles sont composées de tubes d’une finesse extréme, dirigés de haut en bas et d’arriére en avant, croisés par des tubercules perpendiculaires, qui circonscrivent des espaces rectangu- laires tres allongés. Ces tubes forment des stries visibles seulement & un fort grossissement ; mais en outre les bran- chies portent des plis assez régulicrement espacés, dirigés aussi (’arriere en avant, assez gros, et qui donnent 4 la branchie Vaspect d’un grossier plissement régulier. Ce 194 Note sur ? Anatomie des Cyrénes Américaines. sont ces mémes plis qui forment les fortes stries des branchies de Corbicula. En arriére du pied et au niveau de Vorifice interne du siphon branchial, les extrémités des quatre feuillets branchiaux se soudent entr’eux. C’est dans l’espace compris entre leur point de jonction et leur insertion sur la masse abdominale que passe le muscle rétracteur du pied. Le pied est allongé, peu élevé, tranchant; il ressemble 4 celui des Corbicula. La masse abdominale est peu dével- oppée; mais cette disposition provient sans doute de la rétraction alcoolique et de la vacuité des ovaires. Le ganglion branchial est semblable 4 celui des Galatea par sa forme et le nombre des nerfs qui en partent et y aboutissent. Cyrena Floridana. Les Cyrénes de ce groupe sont rostrées, triangulaires. Le manteau est mince; le muscle palléal étroit est trés rapproché du bord de la coquille; il ne forme qu’un sinus tres court au dessous du muscle adduc- teur postérieur des valves, mais ce sinus est cependant plus prononeé que chez les Batissa et les Corbicula. Le manteau est garni en dedans d’une rangée de petits tubercules placés au dessus du bord libre, qui est stmple et mince. L’impression musculaire de l’adducteur antérieur des valves a la forme d’un croissant, elle est étroite, impression de Yadducteur postérieur est ovale; Pimpression du rétracteur du pied se voit 4 peine. L’arriére-cavité des siphons, trés étroite, montre deux siphons extrémement courts; le siphon anal est large et eylindrique ; le siphon branchial conique, un peu plus allongé, porte une couronne de petits tentacules. Ces siphons quoique peu développés sont désunis. Les branchies dont la structure intime est semblable 4 celle des Cyrénes du groupe précédent sont disposées aussi de la méme fagon; mais la branchie interne est rélativement plus grande; elle est double en longueur de la branchie externe. Celle-ci est divisée & peu prés vers sa moitié par la Note sur ?_Anatomie des Cyrines Américaines. 195 ligne d’‘insertion sur la masse viscérale. La branchie externe est donc ovale, divisée obliquement en deux portions, dont la postérieure et supérieure est réfléchie. Vers la partie postérieure du pied, les feuillets branchiaux se soudent entr’eux en embrassant le rétracteur du pied. Celui-ci est allongé, sécuriforme, court; son extrémité anté- rieure s’approche tres prés du muscle adducteur antéricur. Masse abdominale peu élevée. Palpes labiaux courts et triangulaires. Conclusions. Si Von résume ce qui est relatif au groupe des Cyrénes, on s’apergoit que depuis les Galatea jusqu’aux Batissa, le muscle rétracteur du siphon diminue progressive- ment dans l’ordre suivant : a. Muscle rétracteur des siphons long et large; siphons longs et larges. Galatea. b. Muscle rétracteur long et étroit; siphons assez courts et étroits. Cyrena Carolinensis. c. Muscle rétracteur court et triangulaire ; siphons courts et étroits. Cyrena Floridana. d. Muscle rétracteur extrémement court; siphons larges et courts. Corbicula. e. Muscle rétracteur non dévéloppé; siphons tres courts. Batlissa. Ces diverses sections du groupe des Cyrénes sont g¢éo- graphiquement distribucées : a. Les Galatea appartiennent uniquement au continent Afvicain. Pas de fossiles. b. Les Cyrénes de Ja deuxieme section, pour lesquelles nous proposons le nom générique de Leptosiphon, sont propres & ’Amérique du Nord. Nous ne les connaissons pas 4 Vétat fossile, du moins dans les terrains tertiaires de Ancien Continent, mais il est probable qu’on en trouvera quelques espéces dans les couches du méme age du Nouveau Continent. c. Les Cyrénes de la troisiéme section, que nous hommerons Cyrenocapsa, sont propres & PAmérique, ot elles 196 Note sur Anatomie des Cyrénes Américaines. vivent dans les eaux saumitres. Un certain nombre de Cyrenes éocénes leur seront peut-étre rattachées. d. Les Cyrénes de la quatriéme section, ou Corbicula, ont une distribution géographique des plus étendues. On les a signalées dans toutes les parties du monde, excepté en Europe, mais 1a leur extinction est bien récente, puisque l'une delles, C. consobrina, existe dans les dépdts quaternaires de Angleterre, de la - France et de la Sicile. Le type apparait dans le Wealdien. Les Corbicula du Continent Américain sont remar- quables par la présence d’un sinus palléal évident. e. Les Batissa sont reparties dans la plupart des iles de VYOcéanie. On les trouve a l’état fossile & partir de Péocene. Les Velorita ont une distribution géogra- phique analogue. Quant a la composition de la famille des Cycladea, Férussac, Corbiculade ou Cyrenide, Gray, Cyclaside, VOrbigny, Conques fluviatiles de Lamarck, nous croyons quelle doit étre ainsi établie : 1. Cyrena, Lamarck. 2. Corbicula,Megerle. Sous-genres ; 3. Cyclas, Bruguiére. Leptosiphon, 4. Pisidium, Pfeiffer. Cyrenocapsa, 5. Galatea, Bruguiere. Batissa, Velorita. Peut-étre le genre /%scheria, Bernardi, appartient-il @ ce groupe, mais amplitude du sinus palléal et les caracteres de la charniére le rapprochent beaucoup des Iphigenia. I serait utile d’examiner l’animal pour étre éclairé su ses affinités. Woodward place les Cyrenella parmi les Cycladide; ce rapprochement me semble fautif; les Cyrenella n’ont de rapport quavec les Diplodonta et les Ungulina, et doivent constituer une petite famille, celle des Ungulinide trés ‘distincte par la structure de leurs branchies des Lucina. >» Note sur V Anatomie des Cyrénes Américaines. 197 Le plus ou moins grand développement des siphons n’est pas, & mes yeux, un caractére de famille, et pour cette raison je place les Galatea parmi les Cycladea et non parmi les Tellinidee comme le font Adams, Gray, Woodward, ete. I faut n’avoir jamais vu un animal de Tellina pour proposer une pareille classification. Tout au plus pourrait-on rappro- cher les Galatea des Donacide. Cette famille des Tellinide, telle qu'elle est circonscrite par Adams et Woodward, est inadmissible. Les seuls genres voisins des Yellina par leur organisation anatomique sont les Fragilia, Amphidesma, Scrobicularia, Syndesmya. Les Capsula, Psammobia, Sanguinolaria forment une famille distincte ; les Donax, Mesodesma, Iphigenia constituent une autre famille. EXPLICATION DES FIGURES. Pav tilts Fig. 1. Animal de Cyrena Carolinensis. a, manteau; b, expansion du manteau qui s’insinue entre les dents cardinales; c, muscle adducteur antérieur des valves; d, muscle adducteur postéricur des valves; e, muscle rétracteur du pied; f, muscle palléal; g, muscle rétracteur des siphons. Fig. 2. Le méme. Le manteau est enlevé en partie. Mémes lettres. h, palpes labiaux; i, branchie interne; k, branchie externe; J, portion réfléchie de la branchie externe; m, pied. Fig. 3. Portion du méme pour montrer les siphons. n, Siphon anal; 0, siphon branchial; p, cavité des siphons. Fig. 4. Le méme. Les branchies sont relevées pour montrer le pied. m, pied; n, masse abdominale. Fig. 5. Animal du Cyrena Floridana. a, manteau; c, adducteur antérieur des valves; d, adducteur posté- rieur des valves; e, rétracteur du pied; f, muscle palléal; g, rétracteur des siphons. Fig. 6. Le méme. Le manteau est enlevé. Mémeslettres. h, palpes labiaux; 7, branchie interne; k, branchie externe; J, sa portion réfléchie; m, pied; n, siphon anal; 0, siphon branchial. 198 On the Relations of Certain XV.— On the Relations of Certain Genera of Terrestrial Mollusca of, or related to, the Sub-family Succinine, with Notes on the Lingual Dentition of Succinea append- tculata Pfr. By THOMAS BLAND AND W. G. BINNEY. Read October 7, 1872. Tue receipt from Governor Rawson of specimens pre- served in alcohol of Succinea appendiculata and Omalonyx unguis Fér, collected in and sent to him from Guadeloupe, by M. Schramm, has afforded us the opportunity of studying their dentition and induced us to examine the relations of certain genera which have been placed in the sub-family Succinine. Albers (2nd ed.) in group E, Succinea, has the following genera, viz., Simpulopsis Beck, and Succinea Drap., the latter divided into four sections, viz., Amphibulima, Suc- cinea, Brachyspira and Omalonyx. We describes the jaw and refers to the lingual teeth in the following terms :— Jaw arcuate, its convex margin extended into an almost quadrate plate; its concave margin striate or ribbed, with a short middle projection. Teeth of the lingual membrane as previously described (7. e., tricuspid or bicuspid as in /el- acea, etc.). Simepwulopsis Bre. Beck (Index, p. 100) adopted this genus, but by name only. Shuttleworth (Bern. Mitt., 1854, p. 55) thus charac- terizes the animal :— *“* Animal heliciforme, testa omnino inclusum, pede lato subtus trans- verse plicato: pallium exappendiculatum. “¢ Maxilla fere formam ferri equini habet, utroque latere dilatato-rotun- dato, medio autem angustata, costis 12 validis permunita, quarum 6 ap- proximate in parte angusta mediana, et in utroque latere 8 majores, magis remote. Papille in laminam lingualem in seriebus obliquis ordi- Genera of Terrestrial Mollusca, etc. GG) nate, numerose ; centralis tridenticulata, denticulo medio elongata; medize bidenticulate, denticulo interno elongato, externo brevi; marginales lati- ores inaequaliter tridenticulate, denticulis versus marginem exteriorem gradatim minoribus, interno autem valde producto. “Genus naturale, Vitrine nullo modo affine, sed Succineew proximum. Lamina lingualis autem diversa videtur (Cf. Phil. Handb., p. 248) atque etiam Maxilla (Cf. Terr. Moll. U. S., I, p. 213, pl. xiii, fig. 3).” Heynemann (Mal. Blatt., 1868, p. 110, taf. v, f. 10) has description and figures of the teeth of Stmpulopsis sulculosa Fér., mentioning that the jaw was not observed. On the accompanying plate we have given (PI. ix, figs. 7, 8) copies of several of Heynemann’s figures of the teeth, as many of our readers may not have access to the originals, and in a subsequent part of this paper we have described them. With respect to the jaw not having been examined by him, Heynemann refers to that fact as rendering the correct classification of the genus difficult, but remarks that the form of the lingual teeth suggests relationship to the Orthalicea* rather than to the Succinea, as shown by a comparison of the marginals with those of B. auris leporis and papyraceus. H. and A. Adams (Genera, I, 127) adopt in Succinine the following genera: — Simpulopsis, Succinea, Amphibu- lima, Helisiga and Omalonyx, enumerating as species of the latter, O. unguis, appendiculata and depressa. On reference to our subjoined notes on the so-called Suc- cinea appendiculata from Guadeloupe, it will be observed that the form of its teeth agrees generally with that ascribed by Heynemann to Simpulopsis sulculosa, while his sug- gestions as to the affinities of the latter genus (the jaw being unknown to him) are supported by our discovery of the character of the jaw in the Guadeloupe species. It must not, however, be overlooked that while the animal of Simpulopsis is entirely covered by the shell, that of the S. appendiculata under consideration is limaciform, like *It must be remembered that we use the term Orthalicine ina much more restricted sense than the Orthalicee of Albers and yon Martens. See our notes on Systematic Arrangement, Ann. N. Y. Lyc., x, p. 168. 200 On the Relations of Certain O. unguis, as figured by Orbigny (Voy., t. 22, f. 1-7). With the form of jaw described by Shuttleworth and the quadrate marginal teeth, it would seem that Simpulopsis belongs to the Helicine and not to the Succinine. It may be noticed that, even form of shell alone considered, some of the species might appropriately be placed near to Bulim- ulus. Guppy (Ann. and Mag. Nat. Hist., Jan., 1866) described S. corrugatus,* from Trinidad. Of the animal he says, ‘‘mantle edge narrowly reflexed over the peristome.” Sub- sequently, the same author (Amer. Jour. of Conch., VI, 308, 1871) mentions having ascertained, from a young example of S. corrugatus, the characters of the dentition of Simpu- lopsis, and that it resembles that of Swccinea more than he had anticipated. He says, ‘*the odontophore is moderately large, but the individual teeth are very minute and resemble those of Succinea, particularly, perhaps, S. ovalis.” It seems to us that one important characteristic of the dentition of Succinea, absent in that of Simpulopsis, is the gap or notch in (as if by the cutting away of) the lower -edge of the base of attachment in the central, and corres- ponding gap in the inner edge of the laterals. Fischer and Crosse, in 1867, established the genus an- thonyx (Jour. Conch., 1867, p. 221, et seq., pl. x, figs. 1-4), describing as the type Vitrina Sumichrasti Brot (1. ¢., p. 70, pl. iv, fig. 2), and referred to the same genus Stmpulopsis Salleana, S. Cordovana and (with some doubt) S. Chia- pensis. Among the generic characters of the animal of Xanthonyx, derived from examination of a specimen of X. Sumichrasti, communicated by Brot, are the following, ‘* Animal testa sua multo majus, haud omnino inclusum,” and ‘* maxilla arcuata, costata; teniola lingualis dentibus basi subquad- *Guppy compares his species with S. Brasiliensis (Syn. of S. obtusa Sow.), from which indeed it seems scarcely distinguishable. Genera of Terrestrial Mollusca, ete. 201 ratis, ineequaliter bicuspidatis (dente medio tricuspidato) instructa.”* With respect to X. Salleanus and Cordovanus, the authors state, on the authority of Sallé, that the animals are much larger than their shells, as in XY. Sumichrasti. Xanthonyx, as well as Stimpulopsis, belongs to Helicine and not to Succinine. Suceimea Drape. Amphibulima.—Albers (1. c., 809) gives as the type of this section of Succinea, A. patula Brug., but without any special description of animal or its dentition. Guppy (Ann. and Mag. Nat. Hist., June, 1868) mentions the occurrence in Dominica of A. patula, and we were in- debted to him for the lingual membrane (without jaw), of which we published figure and description in Amer. Jour. Conch. VII, 186 (1871), pl. xvii, fig. 1-2. Guppy does not particularly notice the animal, and we assume in consequence that, as in Succinea s. s., it is capable of retraction within the shell; indeed the form and character of the shell pre- clude any other supposition. Guppy (/. ¢., June, 1868) describes another species, found by him in Dominica, as Amphibulima pardalina, the animal of which he describes as follows :— ‘¢The animal resembles that of Omalonyx unguis Fer. (D’Orb. Voy. Amer. Mer. pl. xxii, fig. 1-7). The foot is translucent, like a bit of ice dipped in milk, the internal organs showing as a dark, variegated patch about the shell, into which the body is incapable of retraction.” Guppy adds (and apparently he was acquainted with the dentition [not the jaw], of A. patula only) : * Fischer and Crosse (Etudes sur les Moll. Terr. et Fluy. du Mexique et du Guate- mala, 192-199, pl. 9, figs. 11-17) give a more detailed description of NXanthonyx, and remark on certain of its affinities with the genus Binneya. The part of the work referred to reached us after our manuscript was in the printer’s hands. 202 On the Relations of Certain “‘Forming my judgment from the soft parts and the lingual dentition, I should separate Amphibulima as a genus from Succinea. The genus Amphibulima might then be divided into the following groups :— Amphibulima s. strict. Type A. patula. Omalonyx D’Orb. O. ungquis. Brachyspira Ptr. “A. pardalina and tigrina.” Without knowledge of the jaw of Amphibulima, and we scarcely think that the genus can be elasmognathous, we are unable to decide whether it belongs to Succinine or not, but have a strong impression that its proper position is in Flelicine. The dentition of Amphibulima, as shown in our figure, does not materially differ from the form usual in the Helicide, excepting in the marginal teeth, which are very long and narrow. The cutting away of the plate, before referred to as characteristic of Succinea, is entirely wanting in Amphib- ulima. -v. Martens (Zool. Record, 1868, p. 491) observes that ‘*Mr. Guppy reéstablishes Amphibulima as a genus distinct from Succinea (Drap.) on account of its different lingual den- tition, but without pointing out the difference.” Succinea s. strict.— The animal, lingual dentition and form of jaw need no special notice in the present paper. We would express, however, the opinion that those species only, to whatever group or section they belong, which are elas- mognathous, should be admitted in Succinine. There are several elasmognathous genera with animals of varied forms on which we have no occasion here to remark. Brachyspira Pfr.—This group is based on the form of shell, and it is worthy of notice that Albers (ed. 2) gives as the type S. tigrina Lesueur, which is very near to, if not identical with, as Guppy remarks, his A. pardalina. Hf the animal of the latter be as described by Guppy, we cer- tainly should not place the species in Brachyspira, which belongs rather to Succinea than to Amphibulima. Tryon (Amer. Jour. Conch., I], 286-241, 1866) refers . Genera of Terrestrial Mollusca, etc. 203 many species of North American Succinea, we think erro- neously, to Brachyspira. In Land and Fresh Water Shells of North America (1869) we adopted the latter in the sense in which it is used by Albers (ed. 2). Omailomyx D’'Ors. Albers (1. c., 311) refers to O. unguis Vér. as the type of this group. D’Orbigny (Voy., 229, t. 22, figs. 1-7) gives the following description of the animal: “¢ Allongé, ovale, déprimé, beaucoup trop grand pour rentrer dans la coquille, occupant prés de trois fois la surface de celle-ci; pied tres large débordant de toutes parts, arrondi en avant, acuminé postérieurement, lisse en dessous et en dessus; manteau formant un bourrelet autour de la coquille, qwil recouvre sur les bords, étroit en arriére, plus large et comme plissé en avant; col assez long; téte étroite; tentacules courts; orifice des poumons sous le bord droit du manteau, vers sa partie moyenne.” Fischer (Mélang. Conch., p. 67, pl. vi, f.1) describes the animal of O. ungués and its dentition. Sometime since we were indebted to Mr. John G. Anthony for specimens collected by him (Agassiz? expedition) in Brazil, and found, on examination of the jaw and lingual dentition, that both agree with the figures given by Heyne- mann (Mal. Blatt., 1868, taf. iv, fig. 5) of the jaw and teeth of Pellicula convexa Martens, of which figures we add copies (plate ix, figs. 12-14). . As already mentioned, we have lately received from Gov- ernor Rawson specimens in alcohol of animal and shell of O. unguis, collected in Guadeloupe by Schramm, and find that both jaw and teeth are precisely similar to those of the Brazilian examples. It appears, irrespective of form of animal and shell, that should even Amphibulima prove like Omalonyx to be elas- mognathous, the lingual dentition of the latter does not warrant its being treated, as proposed by Guppy, as a section of the former genus. Guppy has lately discovered in Trinidad, but not yet, we 204 On. the Relations of Certain believe, described, another species of Omalonyx, the shell of which he has communicated to Governor Rawson, with the name Amphibulima (Omalonyx) felina. Indebted to Mr. Rawson for an opportunity of examining the shell, we find, as the author remarks in a letter accompanying the spec- imens, no appreciable distinction between it and the Guad- eloupe O. unguis. In a late letter Mr. Guppy states that ‘‘the animal of O. felina resembles in general character O. unguis, O. par- dalina and A. patula, the latter being much larger, darker, more strongly colored and more coarsely striated.” The Guadeloupe specimens received from Gov. Rawson, collected and labelled by Schramm Succinea appendiculata, are extremely interesting and not a little perplexing, indeed Schramm, judging from his notes sent with them, rather suggests that S. appendiculata, depressa aud O. unguis are all one and the same species. Succinea depressa Rang (Guer. Mag., 1834, t. 55) is a species as to which there seems to be much uncertainty. Fischer described it, the animal and its dentition, as Pellicula depressa in Act. Soc. Linn. Bord. XX, 5, to which we have not had an opportunity of referring, and also in Mélang. @onchyipw.Grsats, yi, £419), In the latter work, the jaw and teeth are thus charac- terized :— ‘¢Machoire semblable 4 celle des Limaces, et portant une quantité de denticulations. Plaque linguale se rapprochant de celles des Ambrettes. Epines médianes trifides; laté- rales bifides.” We give copy of the figure of the jaw on plate ix, fig. 4. Petit (Jour. Conch., 1856, p. 154) expresses the opinion that S. appendiculata Pfr. is the same species, Rang’s specific name having priority, but Pfeiffer (Mon., IV, 804) referring to Rang’s figure, maintains that they are distinct. The character from which the specitic name of Pfeiffer’s species is derived, he describes (Mon., II, 531) thus; ‘*col- Genera of Terrestrial Mollusca, ete. 205 umella callosa, aperta, appendicula dilatafa, torta superne munita,” adding in a footnote, ‘* Forma persimilis preecedenti (S. depressa Rang), at bene distineta columella appendice torta quasi duplicata, spira subpapillatim prominula et peri- pheria magis regulari.” This appendage is shown in our figure (pl. ix, fig. 6) of Rawson’s appendiculata. v. Martens (Malak. Blatt., 1868, p. 183) described Suc- cinea (Pellicula) convexa, to the dentition of which by Heynemann we have already referred, giving also (plate ix, figs. 12-14) copies of his figures.* One of the characters of this species is said to be by its author, ‘* paries aperturalis appendicula parva, plicee-formi munitus.” With respect to the validity of his species, v. Martens adds a note to the following effect,—S. depressa Rang, as its name implies, differs from our species by being less arched. Pfeiffer writes that P. convexa is by no means the same as his S. appendiculata. If the latter be identical with depressa us Fischer maintains, then Rang’s figure is entirely faulty, the most essential character, the process on the columella, being overlooked. A comparison of the figures presented on plate ix, will show that the DPedlicula depressa of Fischer has a ribbed jaw (fig. 4), and does not belong to the Succtnine,t while Pellic- ula convexa v. Martens is elasmognathous, like. Succinea (fig. 14). It seems to us that S. depressa of Fischer must be treated as the type of Pellicula, while S. convexa belongs to Omalonyz. Albers (ed. 2) does not include in Omalonyx or other group S. depressa or S. appendiculata, mentioning them only in a remark of the following purport :-— *y. Martens (Zool. Record, 1858, p. 492), referring to Heynemann?s figure, says “proving that Pellicula is not generically distinct from Seccinea.”—a proposition in which we do not concur. H. & A. Adams (Genera, II, 568) inconsiderately remark th: ¢ Pellicula Fischer is syn. of Helisiga, and founded upon H. depressa Fischer, a new spe- cies of that genus. t Mérch (Jour. Conch. 1865, p. 384) places Pellicula in his section Odontognatha, 206 On the Relations of Certain Succinea appendiculata, identical with S. depressa Rang, is made by Fischer the type of a separate genus, Pellicula, after an examination of the jaw, lingual dentition and gen- erative organs; Albers (/. c.) adds that he had not yet been able to decide upon the correctness of those views. Irom the subjoined diagnosis of the species received as Succinea appendiculata from Guadeloupe, it will be seen that the animal is limaciform, has a jaw, not as in O. unguis, but allied to that of genera and species of Helicine, and teeth agrecing somewhat closely with those of Simpulopsis. In pl. ix, we give figures of the animal (from an alcoholic spee- imen), of part of the jaw and teeth (Higs. 2, 9, 10, 11). We now proceed to describe the jaw and lingual membrane of MSuccinea appendiculata Ptr., received from Governor Rawson : Jaw extremely thin and transparent, long, low, slightly arcuate, ends blunt, divided longitudinally by about 40 delicate ribs into as many plate-like sections, of the character found in the jaws of Cylindrella, Macroceramus and many species of Bulimulus. No appearance of trian- gular upper median plates, however, as in Cylindrelia, though the two specimens examined by us are not perfect at that part. Both margins serrated by the extremities of the ribs. The general character of these ribs is the same as in Helix turbiniformis, figured by us in Ann. of Lyc. of Nat. Hist. N. Y. x, pl. 2, fig. 2. The jaw is quite membranous. Lingual membrane as usual in the Helicinw proper (see Ann. Lyc. Nat. Hist. N. Y. x, 163).. Centrals subquadrate with a very large, stout, short, pointed cusp, the side cusps obsolete. Laterals larger and more narrow than the centrals, bicuspid, the inner cusp greatly produced, broad and quite squarely terminating. The base of attachment of the laterals is cut away on the inner side, leaving a Jarge outer lateral expansion, bringing to mind’ the much less developed one of Sucecinead. Marginal teeth quadrate, gradually becoming moditied from the laterals, the cusps finally passing off into simple, obtuse papille, the inner one the larger. The central and lateral teeth are like those of Stimpulopsis sulculosa as figured by Ileynemann in Malak. Blatt. xv, pl. 5, fig. 10, the central, however, bearing a much more developed cusp in our species. The marginals in that figure, of the form found in Sulimulus uurisleporis, papyraceus, laticinctus, etc., we failed to detect in our species. As already stated, we found the marginals merely a moditication of the laterals. The above description does not agree with that given by Dr. Fischer (Mélanges Conch., 69, t. vi, fig. 19) of Pellicula Genera of Terrestrial Mollusca, etc. 207 depressa, which we have already quoted. He describes the jaw as having a number of ribs on its anterior surface pecti- nating the cutting margin, actually nine of them being shown in his figure. He also describes the lingual dentition as quite different, the centrals being represented with one large bifid median cusp and one small cusp at either side. His figure of the lateral teeth is also simply bicuspid, the figure of the inner cusp does not show any trace of the peculiar prolongation and blunt termination, described by us above. For convenient reference we copy Fischer’s figure of the jaw (Plate ix, fig. 4). The external appearance of our animal is the same as described by Fischer in the paper referred to. Little confi- dence, however, can be placed on the external characters of the animals of this .group, that of O. unguis being, as Fischer remarks, nearly the same as of the species under consideration. As already mentioned, P. convexa v. Mart., from its form of jaw, cannot be placed in Fischer’s genus Pellicula, while the appendiculata examined by us has jaw (as well as teeth) of different character from that assigned by Fischer to Pellicula depressa, but for the present we refer, with doubt, our spe- cies to Pellicula; most certainly it does not belong to Suc- cinea. We appear to be warranted in assuming that Mr. Rawson’s appendiculata is Pteiffer’s species, specifically and probably generically distinct from iS. depressa Fischer. Whether the latter is or is not the S. depressa Rang we are unable to decide. DECEMBER, 1872. 15 ANN. Lyc. NAT. Hist., VOL. Xx 208 Description of Hemphillia, e XVI. — Description of Hemphillia, a New Genus of Ter- restrial Mollusks. By THOMAS BLAND AnD W. G. BINNEY. Read October 7, 1872. Hemphillia. Animal limaciforme, parvum, antice obtusum, postice attenuatum. Pal- lium subcentrale, magnum, ovatum, antice valde productum, marginibus liberis. Discus gressorius distinctus nullus. Porus mucosus transversus in apice pedis, processu coniforme valido protectus. Apertura respiratoria ad dextram, in medio marginis inferioris pallii, genitalis ad basin tenta- culi dextri oculigeri. Testa externa, unguiformis, subquadrata, replicatura pallii marginorum breviter inclusa. : Maxilla et lamina lingualis ut in Avione constituta, dentes centrales tricuspidate, laterales bicuspidatz, marginales quadrate, bicuspidate, papillis internis valde productis, externis subobsoletis. Animal limaciform, small, blunt in front, tapering behind. Mantle subcentral, large, oval, greatly produced in front, free around its margin and slightly reflected over the edges of the shell. No distinct locomotive disk to foot. Lines of furrows run near and parallel to edge of foot, rising above the extremity and apparently uniting over a -transverse, mucus slit, overhanging which is a greatly produced horn- shaped process. Respiratory orifice at right edge of mantle, near its centre. Generative orifice at right side of neck, near right eye peduncle (Plate ix, figs. 1 and 3). Shell external, its edges imbedded lightly in the mantle, very thin, unguiform, almost as large as the mantle (in spec- imens preserved in alcohol) (Plate ix, fig. 5). Jaw wide, low, slightly arcuate; ends blunt, but little attenuated ; anterior surface with numerous ribs denticulating either margin. Lingual membrane as usual in the Helicide. Teeth in Hemphillia glandulosa about 23-1-23. Centrals and laterals long, the former tricuspid, the latter bicuspid; marginals a New Genus of Terrestrial Mollusks. 209 about twelve, quadrate, the inner cusp long, narrow, oblique, bluntly pointed, outer cusp subobsolete (Plate ix, figs. 15- Ne Hemphillia glandulosa. Animal, shell, jaw and lingual membrane as already described above under Hemphillia. (See Plate ix.) Animal about 12 mill. long (preserved in alcohol) ; color smoky white, mottled with longitudinal, dark brown blotches, running obliquely from the edge of the mantle to the foot, uniformly with the coarse granulations, of which we counted about twenty-five on either side of the animal. Caudal process very large, triangular in profile, dark brown, with a few coarse granulations. Shell unguiform, slightly convex, light horn-color, very thin, its edges almost membranous, with prominent concen- tric lines of growth; five mill. long, three wide. Habitat.— Astoria, Oregon: Mr. Henry Hemphill. Our description is drawn from specimens preserved in alcohol, due allowance for which fact must be made. They were collected at Astoria, Oregon, by Mr. Henry Hemphill, to whom we dedicate the genus in return for most valuable addition to our knowledge of the land shells of the Pacific region. This curious slug, by its general outline and by the form and position of its shell, may be compared to Omalonyx unguis D’Orb, and the species known formerly as Succinea appendiculata Pfr., but now usually referred to Pellicula. The former has, however, a jaw with the supplementary extension as in Succinea, the latter has the jaw usual in Bulimulus and Cylindrella, while neither of them has the prolongation of the mantle. Both of those genera also are readily distinguished by their shell being more developed and approaching a spiral form. Hyalimaz is distinguished from Hemphillia by its Succinea- like jaw. Otherwise, it resembles our genus in its general 210 Description of Hemphillia. outward appearance, and by its non-spiral shell. This shell, however, in Hyalimaz is almost, if not completely, internal, while the shell of Hemphillia is entirely exposed. Binneia, in its prolonged mantle and costate jaw, resembles Hemphillia, but its shell is much more developed, spiral, striate and almost capable of protecting, though not absolutely including, the animal when contracted. Xanthonyx and Simpulopsis are both described with costate jaw, but they have both highly developed, decidedly spiral shells. Finally, from all the above mentioned genera and from all known sublimaciform genera, our genus is at once distin- guished by the peculiar hump-like process on the tail, re- minding one of the caudal process in Manina. EXPLANATION OF PLATE IX. Fig. 1. Hemphillia glandulosa. The caudal extremity greatly enlarged. Fig. 2. Succinea appendiculata Pfr. From Governor Rawson; a portion of the jaw. Fig. 3. Same as fig. 1, enlarged. From a specimen preserved in alcohol. Fig. 4. Pellicula depressa Rang. The jaw; copied from Fischer, Mé]. Conch., J. c. Fig. 5. Same as fig. 1. The shell, enlarged. Seen from above. Fig. 6. Succinea appendiculata Pfr. From Governor Rawson, slightly enlarged, the right hand figure showing protile of appendage. Fig. 7. Simpulopsis sulculosa Fer. A marginal tooth, copied from Heynemann, Mal. Blatt., 1868, pl. v, fig. 10. Fig. 8. Same as fig. 7; centrals and laterals. Fig. 9. Succinea appendiculata Pfr. From Governor Rawson; centrals and laterals. Fig. 10. The same; marginal tooth. Unity of the General Forces of Nature. 211 Fig. 11. The same; external view of animal contracted in alcohol. Enlarged about one half. Fig. 12. Pellicula convexa Martens. Centrals and laterals; copied from Heynemann, l. ¢., pl. iv, fig. 5. Fig. 13. The same; marginal tooth. Fig. 14. The same; jaw. Fig. 15. Hemphillia glandulosa. Extreme marginal teeth. Fig. 16. The same; first marginal teeth. Fig. 17. The same; central and lateral teeth. XVII. — Hssay upon a Necessary Limitation of the Doc- trine of the Unity of the General Forces of Nature. By PROFESSOR BENJAMIN N. MARTIN, of the University of the City of New York. Read Nov. 6, 1872. THE great and characteristic doctrine of our modern physics is that which affirms the unity and the convertibility of the forces of nature. Varied and multiform as are the diffused agencies of the physical universe, it is found that they are fundamentally one; and the proof of this oneness is furnished by the fact that they are all convertible into one another. On the one hand, electricity, magnetism and gal- vanism,—on the other, light and heat, may be made to produce each other. One of these forms of force can dis- appear only by giving birth to another; and the sum of them all is ever the same. Under certain conditions, gal- vanic electricity will manifest itself as light and heat, and heat will develop electricity again. Each is a form of motion convertible into the other. Moreover, they sustain a common relation to the motion of the masses of matter 212 Necessary Limitation of the Doctrine of the around us: each will produce such motion, and will be accu- rately and completely measured by the amount of motion into which it is thus capable of resolving itself. This doctrine, of the unity of the general forces of nature, I do not propose to dispute. It is a doctrine of the most interesting and beautiful kind ; and if not fully proved,—and some eminent physicists still demur to the reception of it — it yet furnishes so many singular and ingenious explanations of phenomena, that one is tempted to overlook its want of complete demonstration, and acquiesce, perhaps by antici- pation, in the conclusion which affirms it. And yet there seems to be a limitation of its scope, arising out of the necessary relation of this to another equally important phys- ical doctrine of our day — the indestructibility of matter. It is affirmed with equal certainty that, in all the varied round of changes taking place among the particles and com- binations of matter, no slightest atom or molecule of it is ever lost. Every chemical change is but a combination, or a resolution, of the particles of a mass; but these particles are ever the same in number, in weight, and in attraction. No one of them can by any possibility ever be put out of existence. The amount of matter is as constant as the amount of force in the universe; and both are alike beyond our power to alter or reduce. It has not hitherto been observed, however, that the one of these doctrines imposes by necessity a limit upon the scope of the other; and it is with the object of calling atten- tion to this restriction, that the present paper is offered. Before proceeding, however, to point out the limitation referred to, it may be well to endeavor to gain a more exact appreciation of the doctrine already described, of the con- vertibility of force. Whatis meant by it? Strictly speaking, this view is often not accurately stated in the ordinary language of science. ‘‘ Heat,” according to Tyndall’s just and happy statement of the fact, «‘is a mode of motion ;” it is a motion of the molecules, instead of a Unity of the General Forces of Nature. 213 mechanical motion of the mass as a whole. The one of these motions may be converted into the other. If a leaden bullet be dropped from a considerable height upon an iron plate which arrests and destroys its mechanical motion, the result is a quivering or vibrating of the particles in their molecular spaces, and this is first, heat; if carried farther, it may become light, or it may give rise to electricity, which again are only other forms of molecular agitation or disturb- ance; and either of these may, by cooling, which is but the arrest of the molecular agitation, occasion again the mechanical motion from which it originated. Accurately conceived, then, all these phenomena are forms, not, as is so often stated, of force, but of motion. Heat is a mode of motion; light, too, is the vibration of the particles of the elastic medium which fills the inter-planetary spaces around our globe; it is another and more rapid vibration, propagating itself through the ether by undulations, in other words, it is another mode of motion. The phenomena of electricity, also, manifest themselves simply’ as attractions and repulsions, —that is, as motions of particles and masses of matter, to and from each other. In the same way, every other manifestation of these imponderable agents is simply, and ‘only, a distinct and peculiar mode of molecular motion. Now of all these phenomena, the universal law is that no one is fixed or permanent. ach is a transient modification of some other, or of that which is the common ground of them all. Each is called into existence by another; it comes to view solely by the disappearance of another. One is born because a previous phenomenon of the same kind ceases to exist; each dies in giving birth to its successor. This extinction, too, is absolute and inevitable. The amount of force involved in one of these changes is ever the same, but it cannot exist in two of these forms at the same time; the preceding form must cease to exist before that into which it is convertible can take its place. The mechanical motion of a body must utterly stop and cease, before the 214 Necessary Limitation of the Doctrine of the heat can be developed into which it is resolvable; and that cessation is absolute. So far as the conversion takes place, so far is the destruction of the previous form of motion utter and complete. There is in this common relation of all these phenomena to motion, an obvious reason for their correlation with one another. They are phenomena of the same kind. All are simply forms of motion; and it is no great novelty to learn that one form of motion may be converted into another. The whole doctrine of the convertibility of the forces resolves itself into the very familiar fact of the communication of motion by impulse. Where one of two billiard balls impinges on another in the precise line of its direction, its motion is imparted to the other, and itself is arrested and stopped. So it is also with the atoms and masses of the physical world. The balls may differ in size, and in the pre- cise mode of their motion, but these are the only differences. One imparts to another its motion; or a large mass commu- nicates movement to a multitude of minute particles; in each case it has its own motion destroyed by the change; and this is the whole of it. The convertibility of the forces implies, then, nothing more than the communication of motion by impulse. When, however, we examine the particles of matter for their essential characteristics, we find that something more than mobility enters into their nature. Adopting, with some variation of order, the accurate analysis of Sir William Hamilton, they may be grouped under the two general heads which follow. We may regard matter, first, as included in space, and secondly, as occupying space. I. Under the first aspect, as included in space, it has position and mobility. (1.) It is known in finite parts and forms; and these must be recognized as occupying definite places in space ; matter, therefore, has (1) PosiTIoN. (2.) Next, it has mobility. In consequence of the rela- Unity of the General Forces of Nature. 215 tions of the parts of space to one another as absolutely adjacent, that which occupies one part of space may be shifted to another ; in other words, it possesses (2) MOBILITY. II. Under the second aspect, as occupying space, matter may be said to have (1) Divisibility; (2) Magnitude; (8) Form; (4) Ultimate incompressibility, or the impossibility of being compressed by pressure from an extended to an absolutely unextended thing, from what is, to what is not, extended. Now, when these general properties of matter are exam- ined, it is at once seen that no one of them, except the last, has any relation to force. Position, mobility, form, magni- tude, these are not properties of force, nor do they result from force. They can all be conceived ideally. But -incompressibility, however ultimate, has direct relation to a resisting force in the body itself. The atom in the last analysis is incompressible ; it cannot be so compressed that it ceases to occupy space, and to repel other matter from the space which it fills. So far as there are pores or vacuities in any kind of matter, so far other matter may permeate a given mass, as the air permeates cork, or as one gas diffuses itself between the molecules of another. But the atom is ultimately, incompressible, it resists all compression which would destroy its integrity. It evermore asserts its own existence, against every other particle with which it can come into contact. In resisting compression, however, the atom manifests itself as possessing a true force; for resistance to our own voluntary motion is, in the last analysis, the only form in which any force manifests itself tous. Gravitation we know as a force, because it resists our own efforts to support a falling body. It is through the same means that we come to the knowledge of any other force. -Cohesion is-known to us as a force, only by its resistance to our endeavor to sepa- rate the parts of one united body, or mass. There is, then, in every atom of matter a resistance to 216 Necessary Limitation of the Doctrine of the compression which is an essential property of matter itself. So far as we know, it does not impart motion to the atom at all, and has no relation either to motion, or to the space in which the atom moves. It simply attends the particle and occupies its internal mass. It is not called into operation by any motion, mechanical or molecular, into which the particle may be thrown. Moving, or at rest, the sole function which we can recognize in it, or as belonging to it, is to preserve the existence of the particle itself; and this it does so effec- tually that, as we have already seen, no particle is ever destroyed, and the sum of them in the universe has never, from the first, been diminished, by a single atom. Now it is an essential characteristic of this force that it is, and must be, forever inconvertible into any other. For if the force which guards the integrity, and guarantees the permanent existence, of a particle, were convertible with any other, it could not in its converted form perform its original function; and the atom might be converted into light, or heat, or electricity. It might impart to other particles. the undulation which constitutes light; but it could not do this, and continue to resist compression, to which all matter is perhaps subject. The atom would no longer be capable of asserting itself by its normal resistance to external pressure, and so, capable of maintaining its own existence; and might disappear forever in a flash of light. Matter deprived of the force by which it is ultimately incompressible, would no longer be indestructible; its preservative force would be gone; and matter without that preservative force which arises from this power of resistance, would be inconceivable. The fundamental fact or law of physics, that all matter is inde- structible, implies that its essential force of resistance to com- pression is inconvertible with any other. It exists unchanged through all the chemical changes, through all the molecular vibrations, or undulations, through all the mechanical trans- fers, or movements of mass, which take place in the universe around us; and it is forever incapable of being converted Unity of the General Forces of Nature. 217 into any one of these phenomena of motion. Being wholly internal, it is incapable of passing out into the spaces beyond the volume of the atom whose existence it preserves. It exists unchanged through motion and rest alike, and, posses- sing no relation to motion, is inconvertible into any form of it, either molecular or mechanical. Its sole function is to maintain the existence and reality of the atom which it permeates, as a permanent, indestructible and, therefore, inconvertible thing. That form of force, then, which has for its exclusive func- tion to guarantee the indestructibility of matter, must. be conceived as sud generis,—as wholly peculiar, incommuni- cable to anything else, and inconvertible with any other form of force in the universe. We must, therefore, recog- nize the reality of one force, at least, which is HEeTIE DIS of transmutation into any other. Moreover, this peculiar and inconvertible force is also in- capable of correlation. It cannot be converted, either into any other force directly, or into that mechanical motion which is the common measure of all the others. We cannot express this resistance in terms of any other denomination. We cannot say that it is equivalent to a given amount of heat, nor can we assign the number of foot-pounds which will measure the ultimate resistance of an atom to compression. As destitute of all relation to motion, it is out of all relation to those forces which express and measure themselves by motion. It simply cannot take the form of light, or heat, or electricity ; a greater degree of heat is as incapable of ex- pressing the intensity of this force, as a less would be. It stands outside of the sphere within which the correlation of the forces finds its scope; and being necessarily out of all relation with the others, it is of course incapable of corre- lation with them. It follows that the doctrine of the Sarr eetibali by of the forces relates properly only to those general and diffused forces of nature which impart motion; and not, so to speak, 218 Description of a Species of Cervus. to the private force of the individual particle; and that the modern doctrine can be true, only with this important limita- tion of its scope. XVIII.— Description of a Species of Cervus. (Plate x.) BY W. J. HAYS. Read October 8, 1872. Cervus Yucatanensis. Tus beautiful deer is found throughout Yucatan and the southern part of Mexico, but little is known of its habits in its native place, and so far as I can learn no account of it has been published. Its color is a grayish-brown on the back and front of the legs, the sides more yellow and run- ning into white on the belly, the color of the head and face similar to the autumn coat of the Cervus Virginianus, the legs a brownish-yellow, lighter on the inner side; the inner side of the thigh, and the under side of the tail, as well as the inside of the ear, are white; the chin and under side of the lower jaw are white, and there is a patch of white on each side of the nose and upper lip; a black line reaches from the nostril to the edge of the lip, and also passes around the lower jaw. The tuft of hair on the inside of the hock joint is short, and there is no gland on the metatarsal bones. This deer does not change its color with the seasons, as other deer, but remains the same in color throughout the year. The doe resembles the buck in color, but is somewhat smaller, and has no horns. The fawns when born are of a dark reddish-brown, spotted with white, on the body; the legs inclining to gray. At about six months of age they assume the color of the adult. The horns are short, a sin- gle straight beam with one short tine projecting inwards ; Certain Terrestrial Pulmonata. 219 the general direction of the beam is upwards and backwards in a line with the face; the horns are cast in March. This deer has been brought to the Northern States, and yet the change of climate has produced no change in the color of the pelage, it remaining of a uniform color, very similar to what is known as the blue coat of the Cervus Virginianus. DIMENSIONS. Ft. In. Length from tip of nose to root of tail, ..... 3410 Go Ofs Carlin eluGineyiaieey i. weve) eles ten fe 8 a6 6 WiAthOUbl | 6 OOM aan aA rUI Sak ror 53 oC “head, SN Roaetage , stants 104 CH from tip of nose to inner canthus, . ... . 5 Height at shoulder, . STE Erk Renee) Ac [tora i: sheen 74 Ge of ot 5, es COS POS CTE e ON RCN Ce POWER De Girth behind shoulder, . 2 Length of ear, Ri Ro) eee 54 SA MMC ETORENIC EW Mie oh tad Natede. ar pace eeleh R/U ay PRs TNL ce Cpe nn ayel COE PPE TOMO ace Wen LORNA Tomy fonetbel see eeNieed ln 1) Weight, 55 lbs. eM CHYOLEMOLIS eis y Site ah onl oe arth oa enngs: Math heel es 74 ce SSFGIING SH Pavrete eh re LRN OT craic.) AIn Ain, URS i fete Be IF 1 XTX—On the Lingual Dentition of Certain Terrestrial Pul- monata Foreign to the United States. By THOMAS BLAND AnD W. G. BINNEY. Read Dec. 9, 1872, Helix Jayama, C. B. Apams (Sagda). Like Sagda connectens C. B. Adams and Sagda Haldemaniana C. B. Adams (see Amer. Jour. Conch. VII, p. 175), this, also a Jamaica species, has quadrate, not aculeate, marginal teeth on its lingual membrane. The cusps of the marginals are short, stout and blunt, centrals and lat- erals as usual. Jaw smooth anteriorly, with scarcely any median projection to its cutting edge. This is an additional proof of the position of Sagda 220 Certain Terrestrial Pulmonata being among the Helicea rather than the Vitrinea of von Marten’s arrangement. We received from Mr. Henry Vendryes the specimen examined. Leucochroa Boissieri, Cuarp. The genus Leucochroa is adopted by von Martens (Die Heliceen ed. 2, p. 78) the type being Helix candidissima Drap, a species whose anatomy has been described by Moquin-Tandon as being more nearly related to Zonites, than to Helix. The genus is classed by von Martens among the Vitrinea, the section of Helicea containing the genera furnished with ribless anterior surface and median projec- tion to the jaw, and aculeate, marginal teeth to the lingual membrane. Among the species catalogued by von Martens is Leucochroa oissiert Charp. Having sometime since received a specimen of this species from Mr. John Van Nostrand, collected by him in Palestine, we have examined its jaw and lingual dentition with the following results. Jaw very low, long, arcuate, ends but little attenuated, bluntly rounded. Cutting edge with a decided median projection, anterior sur- face free from ribs, with a strong, transverse line of reinforcement. The jaw resembles that of Clausilia or Pupa more than that usually found in Helix. Lingual membrane as usual in the Helicide. Centrals short and stout with a bluntly pointed median tooth, the side teeth almost obsolete. Laterals with a very long, oblique, blunt inner tooth, the outer tooth almost obsolete. Marginals subquadrate, with several short, blunt, papille-like teeth. From the above it will be seen that Leucochroa Boissieri must be classed among the //elicea, its lingual membrane having the quadrate type of marginal teeth, and not the acu- leate type common to Vitrina, Zonites and other Vitrinea. Its jaw is of the form often found in the felicea. Judging from both jaw and lingual membrane, we would not separate the species from the genus Helix as receiveG by von Martens. We are inclined to believe that further investigations will Foreign to the United States. 221 prove the genus Leucochroa to be only a subgenus of felix, in the arrangement of “ Die Heliceen.” Hielix circumafirmata, REDFIELD. Lingual membrane long and broad, centrals tricuspid, laterals bicuspid, cusps long and slender, marginals aculeate. From the above description it will appear that this spe- cies belongs to the Vitrinea rather than to the Helicea of von Marten’s arrangement, in which latter it is classed in ‘¢ Die Heliceen” as a species of the subgenus Microphysa. EBielix Bermudersis, Prr. _Jaw extremely thin, arched, with a blunt, median projection to its cutting edge. Lingual membrane long and narrow. Central teeth tricuspid, laterals bicuspid; the cusps in each long and slender. Marginals numerous aculeate in oblique rows. As in the ZZ. circumfir'mata, the result of our examina- tion of the lingual membrane throws light on the generic position of this species. It can no longer be retained in Caracolus, a sub-genus of f/elix, as it has the dentition of the Vitrinea of von Marten’s arrangement. Jor the speci- mens examined of this and the preceding species, both from Bermuda, we are indebted to Mr. J. J. Crooke. Melix perplexa, Frr. (Dentellaria). Jaw with a median projection to its cutting edge. The anterior sur- face of the jaw is of irregular thickness, showing some approach to the ribbed form of jaw. Lingual membrane as usual. Central and lateral teeth with short, stout, blunt cusps. Marginal teeth quadrate, with one wide, stout, bluntly rounded median cusp, and two small, blunt side cusps. We are indebted to Governor Rawson for this specimen collected in the Island of Grenada. 209 Certain Terrestrial Pulmonata Pupa suleata, Mutier (Gonidomus). Lingual membrane long and very narrow. Rows of teeth arranged en cheyron. Teeth separated, aculeate, as in Pupa palanga Lesson photo- graphed by us, (Amer. Jour. Conch. V. pl. x1. fig. 1.) We obtained no jaw on boiling the buccal mass ina solu- tion of caustic potash. . This species belongs to the genus Gronospira, in which P. palanga was placed by Crosse and Fischer (Journal de Conch. IX, 213, (1869) pl. x1, figs. 6-8). The specimen examined, sent from Mauritius by Consul Pike, was kindly supplied by Mr. John G. Anthony. Bulimus aulacostylus, Prr. (Lurytus). Lingual membrane as usual in the genus, the marginal teeth simply modified from the laterals. : Jaw slightly arcuate, membranous, almost transparent, in one single piece, but divided by delicate ribs into more than sixty plate-like sections, as common in the genus Bulimulus, Cylindrella, etc. No upper median triangular plate, but the ribs run somewhat obliquely to the centre. We are indebted for this specimen from St. Lucia, and for the following from St. Vincent, to Govenor Rawson. ESulimnws awuwris-silemi, Born (Pelecychilus). Jaw and lingual membrane as in the last species. The middle cusp of the central teeth and inner cusp of the lateral teeth long, acute. The jaw of this and the preceding species do not agree with the generic description of von Martens ‘ costis validis exarata,” but are like that of Lulimulus. This fact gives still more proof of the difficulty of classifying the bulimi by their jaw, at the present stage of our knowledge of the subject as already remarked by Fischer (Jour. de Conch. XII, 295, 1872). Foreign to the United States. 223 ADDITIONAL NOTE ON THE GENUS AMPHIBULIMA. Since our paper “On The Relations of Certain Genera of Terrestrial Mollusca of, or related to, the Sub-family Suc- cinine, with Notes on the Lingual Dentition of Succinea appendiculata Pfr.” (pp. 198-207) was printed, we have re- ceived, through the kindness of Dr. W. J. Branch of the island of St. Kitts, two specimens of Amphibulima patula with the animals, preserved in glycerine, and can in conse- quence offer a decided opinion as to the generic relations of the species. Finding a note among the papers of the late Mr. Robert Swift to the effect that “.S. patula Brug. is found at St. Kitts on Bayford’s estate on the wild plantain which grows on the banks of a small water-course,” Bland wrote on the 21st November last, requesting Dr. W. J. Branch, a correspond- dent of Mr. Swift and also of Governor Rawson, to obtain specimens, if possible, for examination. To this request Dr. Branch most kindly responded. We subjoin a copy of his interesting letter, which accompanied the specimens. “‘T went a few days ago to Bayford’s to look for the S. patula but, after a long and fatiguing search, found only two small (young) speci- mens. When I was in the place several years since, the bushes on each side of the little river were covered with snails* (a striped Bulimus, a species of Helicina and the S. patula), but the other day I saw only three arboreal snails. The present scarcity of these creatures in St. Kitts is probably due to the hurricane which visited the island in 1870. Many trees, some of enormous size, were torn up by the roots, others lost all their branches, and scarcely a single leaf was left on any tree. The sup- ply of water to the estates was cut off or much diminished by the drying up of the numerous streams from the mountains. This was, no doubt, caused by the want of foliage to protect the moisture, which collects on the slopes of well-wooded hills, from the sun’s heat. So the poor snails have come to grief from the actual violence of the hurricane itself, and the subsequent cutting off of their supplies both of meat and drink. You will see that both the snails sent are completely tucked into their shells, but I do not think that they often, or perhaps ever, draw in either the head or the posterior part of the foot during life. ' Their flesh is partic- * B. multifasciatus Lam. and H. fasciata Lam. (T. B.) JANUARY, 1873. 16 ANN. Lyc. NAT. HISstT., VOL. x 224 Certain Terrestrial Pulmonata ularly watery and gelatinous and shrinks up as they die. When they are moving about, the foot looks very large and when I touched the creature it could not or would not retreat into its shell. On this point, however, I shall be able to give more accurate information when I can collect addi- tional specimens.” We find that the animals are completely retracted into their shells and very much in the same manner as in Succinea, little more than the entire surface of the foot being alone seen within the aperture, the edges of the peristome pro- jecting slightly beyond it. While the sensitiveness of the animal to touch may be slight, and its habit as described by Dr. Branch, they cannot be said to be much larger than their shells, as remarked by Sallé of Xanthonyx, and described by Fischer and Crosse, or as described by Dr.,Cooper of Binneia. The specimens, for which we are indebted to Dr. Branch, must have been taken alive in the month of Decem- ber, and very soon at least after death, before becoming dry, put in the glycerine. It will be remembered that Guppy considers Omalonyx and Brachyspira as groups or sections of Amphibulima. Ina very recent letter he repeats his assurance that “the animals of both Amphibulima patula and pardalina are very much larger than the shells and quite incapable of retraction into them.” His observation agrees, so far as it goes, with that of Dr. Branch, who adds a remark as to the shrinking up of the animals “as they die.” This shrinking before death must be accompanied by the exercise of contractile muscular force, and probably further observation will prove that the animal, while in possession of its full vital power, can and does with- draw itself into the shell, and especially, perhaps, in seasons of drought. The jaw of A. patula, of which we subjoin description, has not the accessory plate characteristic of Succinea, and which is found in Omalonyx and Brachyspira; while the latter subgenera therefore belong to the Succininw, Amphi- bulima must be associated with the Helicine. By the char- acter of the ribs of the jaw, it is most nearly allied to the Foreign to the United States. 995 genus Bulimulus. The same may be said of Geotis lately examined by us. Amphibulima patula.— Body obtuse in front, pointed behind, entirely retractile within the peristome, though usu- ally greatly expanded. Mantle simple as in Succinea, Helix, etc. Base of foot wrinkled transversely, without distinct locomotive disk. Generative orifice? Respiratory orifice ? Jaw slightly arcuate, low, ends attenuated: extremely thin and transparent with prominent transverse strie; divided longitudinally by about forty-five delicate ribs into so many plate-like sections of the same character as those of Cylin- drella, Macroceramus and many species of Bulimulus. No upper triangular median plates as in Cylindrella. Margin serrated by extremities of ribs. The figure we have given of the jaw of Succinea? appen- diculata Pfr. (Ann. Lyc. Nat. Hist. N. Y., X, pl. ix, fig. 2) offers a correct general idea of the jaw of Amphibulima patula. See also our photograph of jaw of Cylindrella rosea (Am. Journ. Conch., V, pl. xi, fig. 2) for the character of the ribs and. plate-like sections. Lingual membrane as already described and figured by us from a specimen from Dominica (See Am. Journ. Conch., VII, 186, pl. xvii, figs. 1-2), long and broad, composed of numerous horizontally waving rows of teeth, of the form usual in the Helicide. Centrals subquadrate, extended at basal angles, narrowing towards the centre, expanding towards the upper edge, which is reflected and tricuspid, extending quite to the base of the tooth; the cusps are stout, the median one bluntly pointed. The lateral teeth are of the same type as the centrals, but unsymmetrical. The marginals are long and narrow, rounded at base, narrowed at apex, reflected and bicuspid; cusps short, stout, and gener- ally a simple modification of those of the laterals. The extreme marginals have irregular teeth, like simple papille. 226 The Upper Coal Measures XX.— The Upper Coal Measures West of the Alleghany Mountains. By JNO. J. STEVENSON, PH.D. Read December 16, 1872. WHILE connected with the Geological Survey of Ohio, I was employed in investigating the Upper Coals as displayed in the First Geological District of the state. The relations of the coal beds to each other, and the marked changes in the intervening Strata, seemed to be at variance with some accepted opinions and induced me to make diligent compari- son of the Ohio coals with those of Pennsylvania and West Virginia. The results of this examination appear, to me, of sufficient importance to warrant publication in advance of the Ohio Report. This I am permitted to do by the courtesy of Prof. Newberry, chief geologist of Ohio. The observations recorded in this paper cover only that portion of the field north of the Baltimore and Ohio railroad in West Virginia and Ohio. LIMITS OF THE UPPER COALS. The outcrop of the Pittsburg coal, the base of the Upper Coal Measures, beginning at the Baltimore and Ohio rail- road in West Virginia runs northward, rudely parallel to Laurel Hill, through Marion and Monongalia counties, W. Va., and Fayette and Westmoreland, Penn., thence westwardly, through Westmoreland and Alleghany into Han- cock, W. Va. Crossing the Ohio just above Steubenville it passes through Jefferson, Harrison and Belmont into Guernsey where it reaches the Baltimore and Ohio railroad at Salesville, thirty-seven miles west from the Ohio river. That this is by no means the original extent is evident from several facts. In Pennsylvania, the Frostburg and Broad Top basins lying to the east of the main outcrop have been West of the Alleghany Mountains. 227 proved to contain the upper coals, and some of our leading geologists profess to find equivalents of the same beds in the anthracite region. In Ohio, west of the line of outcrop, isolated patches are found in the synclinal passing through Guernsey county, ten to fifteen miles away. At New Con- cord, Muskingum Co., Ohio, twenty-three miles west from Salesville, there is a thin coal resting ona heavy buff colored fossiliferous limestone and occupying both sides of the syn- clinal trough, of which the bottom is at that village. About fifty feet below it is a hard limestone, bluish-gray in color and fossiliferous, known in the Ohio section as the Crinoidal Limestone, a persistent stratum traceable into Pennsylvania and West Virginia. Along the western outcrop of the Pittsburg coal the Crinoitdal Limestone is found at a distamrce, varying little from one hundred and fifty feet, below the coal, and the interval is occupied by variegated shales and shaly sand- stones, with no coal or even bituminous shale. From four to ten feet below the coal there is a tough limestone, varying in color, four to six feet thick and more or less fossiliferous. It would seem then from the accompanying rocks that the New Concord coal is the western prolongation of the Pitts- burg. Itis true that the interval between it and the Crinoidal Limestone is at that place very much less than at Salesville, twenty-three miles east, but even this is an additional proof of identity, for this interval increases eastward. Three miles northwest from New Concord it is barely thirty-five feet; at Concord it is fifty; at Salesville it is one hundred and fifty; while in the Monongahela Valley it is two hun- dred and fifty. The Crinoidal Limestone has been traced to within three miles of the Muskingum river on the west and thence round to the borders of Tuscarawas and Stark, on the northwest and into Columbiana and Mahoning on the north. So constant and regular is it in its relations to the Pittsburg coal, that we may regard its distribution as an indication of 228 The Upper Coal Measures the original extent of that bed. Accepting this then as a basis for the calculation we conclude that that coal once reached as far west as Sonora on the Central Ohio railroad, seventy-one miles west from Wheeling, and to a point north- ward not less than fifty miles from that city, a tortuous boundary line connecting the two points. RELATIONS OF THE SEVERAL COAL BEDS IN OHIO, PENNSYLVANIA AND WEST VIRGINIA. To ascertain the relation of the Ohio coals to those of Pennsylvania and West Virginia the following sections are compared : I. From Kirkwood Township, Belmont | IV. From Wheeling creek, W. Va. Co., Ohio. II. From the Central Ohio railroad be- tween the Ohio river and the Barnes- | VI. From Uniontown, Fayette Co., Penn. V. From Scott’s Run, Monongalia Co. Wien Vict- ville summit. (Rogers.) III. From Wheeling, W. Va. U5 iit. IIl. 1. Debris, 150'| 1. Sandstone, 40'| 1. Sandstone, w 2. Coal X11, 1}'| 2. Coal xi, 1'| 2. Coal, Waynesburg, 3’ 3. Sandstone, 70'| 3. Sandstone, 70'| 3. Shale, ay 4. Coal xu, 13'| 4. Coal xm, 1'| 4. Limestone, 15’ 5. Shale and Sandstone, 40’) 5. Shale, 35'| 5. Sandstone, 3' 6. Coal x1, 2'| 6. Coal XI, 3'| 6. Limestone and Shale, 95' 7. Sandstone with thin 7. Sandstone, 100’| 7. Shale, 3’ Limestone, 100° 8. Coal X, 4%"! 8. Coal, 1}' 8. Coal x, 4' 9. Sandstone, 85'| 9. Shale, 6! 9. Sandstone, 40’ A 10. Coal Ix, 22'110. Coal, WY 10. Coal 1x, 25" 11. Limestone, 70'|l1. Clay, 6' 11. Limestone, 70' 12. Coal vic, 4'|12. Sandstone, 8’ 12. Shale, 6' y 13. Sandstone, 35 |13. Coal, Sewickly, 13’ 13. Coal vim, 8' s 14. Coal vim b, 1'/14, Limestone, 24’ 14. Fireclay, 5’ 15. Limestone, 30'|15. Coal, Redstone, iv 15. Limestone, 6’ : 16. Coal yiI1 a, 3 |16. Limestone, 20’ 17. Limestone, 20'|17. Shale, 6' 18. Shale, 10'|18. Coal, Pittsburg, 8' 19. Coal vim, 9” eee —— —————————————eEEEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeEeeEeEeEeEeEeEeEeeEeEeeeeEeEeEeEeEeEeEe West of the Alleghany Mountains. 229 TV. Vv. Vi. 1. Sandstone, . 5'| 1. Sandstone, 40'| 1. Limestone, 12’ 2. Limestone and shale, 38'| 2. Shale, 1-20'| 2. Not well exposed 3. Coal, Waynesburg, 3'| 3. Coal, Waynesburg, i) iivon tieectone — 4, Shale, 38'| 4. Sandstone, 15'| 3. Shale, aby 5. Limestone, 1'| 5. Shale, 8'| 4. Sandstone and lime- 6. Shale, 40'| 6. Limestone, 5! ae 7. Limestone and shale, 100’ 7. Shale, 4'| 5. Coal, Sewickly, 4’ 8. Coal, 3'| 8. Sandstone and shale, 15'| 6. Shale, 2! 9. Clay, 2'| 9. Limestone and shale, 30'| 7. Limestone, 6' 10. Sandstone, 15'| 10. Shale and sandstone, 25'| 8. Shale, 41"? 11. Coal, Sewickly, 33'| 11. Limestone, 6'| 9. Coal, Redstone, or 12. Limestone, 55'| 12. Sandstone, 15'|10. Shale with calca- 13. Shale, 5'| 13. Limestone, ils sa aE ae! 14. Coal, Pittsburg, 7'| 14. Sandstone, 10'/11. Sandstone, 5’ 15. Fireclay, 2'| 15. Limestone, 8'l12. Shales, 15’ 16. Shale, 12/13. Coal, Pittsburg, 10’ 17. Sandstone, il 18. Arenaceous shale, 20' 19, Coal, Sewickly, DI 20. Shale, 8' 21. Limestone, te 22. Sandstone, 10' 23. Limestone, 22’ 24. Coal, Redstone, 4’ 25. Limestone, 12’ 26. Shale, 8' 27. Coal, Pittsburg, 14’ east side as the Redstone. The discrepancy between the two Ohio sections will be discussed in another portion of the paper. Taking Coal VIII of the Ohio section as our basis, we have a definite starting point, as that is the Pittsburg. VIII a is present at Wheeling; does not appear at Wheeling creek, owing probably to imperfect exposure, but reappears on the VIII 0 is seen in all the sections 230 The Upper Coal Measures and is the Sewickly. VIII ¢ crosses the Ohio, is traceable along Wheeling creek for several miles, but soon runs under and does not reappear on the other side. IX and X do not cross the river into West Virginia, the former disappearing two miles west from the Ohio, while the latter is seen as a mere streak in the hills opposite Wheeling. It is possible, however, that careful tracing round by the north may estab- lish some connection between our Coal X and the Uniontown coal of Pennsylvania. Coal XT is persistent throughout, and is the Waynesburg. XII was not seen by me at Wheeling, though it is probably the bed noted by Mr. Briggs, eighty- two feet above the last. At Waynesburg and Uniontown, the interval is from fifty to sixty feet. Erosion has so removed Coal XIII and its adjoining rocks that it is to be seen at no point near the Ohio river, but its equivalent in Penn- sylvania is doubtless the top coal at Waynesburg and Union- town, fifty-five feet above the last. These two beds exist in West Virginia on the east side of the basin, but owing to the poverty of exposures no definite statement can be made respecting them. The relations of the coals in the several states may there- fore be represented as follows : OHIO. PENNSYLVANIA. WEST VIRGINIA. Coal XIII. Top at Waynesburg. ? Coal xiI. Middle at Waynesburg. ? Coal XI. Waynesburg. Waynesburg. Coal Xx. Uniontown? Not present. Coal IX. Not present. Not present. Coal VIII ¢. Not present, Not present (east side of basin). Coal viii b. Sewickly. Sewickly. Coal VIII a. Redstone. Redstone. Coal V1Il. Pittsburg. Pittsburg. West of the Alleghany Mountains. 231 DESCRIPTION OF THE BEDS. Coals XII and XIII of the Ohio section are seen at few localities and are of economical importance nowhere. The former is enormously developed in the hills opposite Wheel- ing, where it is a dry coal, six feet thick, but heavily charged with pyrites. The Waynesburg (XI) is commonly known in western Belmont Co., Ohio, as the “jumping six-foot seam” owing to its sudden variations in thickness. In Harrison and Jef- ferson counties, it is worthless, never more than two feet thick, and is seen only near the tops of the highest hills. In western Belmont it is not worked and varies from six inches to nearly six feet in thickness. This change is seen in a cut west from Barnesville, at one end of which it is barely six inches while at the other it shows the following section : Coal, 1 ft.; shale, 4 in. ; coal, 4 in.; shale, 4 in.; coal, AMine wshales 2tts\icoal, Lite il otal, otter sins Seven miles east from Barnesville it is seen in a cut, about one foot thick and parted in the middle by a thin layer of limestone. Near St. Clairsville, in the same county, it is rudely worked and shows three feet of very impure coal, resting almost immediately upon a foot of limestone. Near Bridgeport, opposite Wheeling, it is three feet six inches thick, roofed by six inches of impure black band which is overlaid by two feet of alternating bands of bituminous and ordinary shale. Here the limestone is eighteen inches below the coal. Onarun four miles west from Belleair and just south of the railroad, it suddenly thickens out and becomes a con- fused mass of coal and shale not less than fifteen feet thick, and totally worthless. Followed into West Virginia it is seen on the top of Wheeling Hill, just back of the city. On Wheeling creek it is worked at Roney’s Point, ten miles from the city, and proves to be a very good coal varying from two feet four 232 The Upper Coal Measures inches to three feet thick. It is seen somewhat thicker on the south fork of the creek. On the eastern side of the basin it is seen at several points along Scott’s and Robinson’s Runs, in Monongalia Co., W. Va., as well as in Greene Co., Penn. Its greatest development is seen on Scott’s Run, where its changes are almost as interesting as in Belmont Co. Ohio. Two miles and a half up the run several openings are seen which give the following section : Coal, 1 ft. 9 in. ; Bituminous shale, 8 in. Coal, 4 ft. 8 in. Two miles farther up the run the shale has disappeared, and at an opening near Cassville, the bed shows full nine feet of coal. One mile beyond, the following section was obtained : Blue clay, 6 in.; slaty coal, 1 ft. 3 in.; clay, with many impressions of plants, 3 to 6 in.; coal, 2 in.; clay, 2 in.; coal, 74 in.; clay, 1 ft. 1 in.; coal, seen, 4 ft. 2 in. This opening is likely to prove of considerable interest as the fossils are very numerous and well preserved, while the horizon at which they occur is more than one hundred feet higher than any other yet discovered in the northern portion of the trough. On Robinson’s Run the bed shows a tendency to develop in the same manner as follows: - Bituminous shale, with thin lamine of coal, 2 ft.; coal, 1 ft..6 in. ; clay, 7 in.; coal, 4 ft. 8-in. Towards the south it rapidly diminishes in thickness and apparently thins out. In Pennsylvania the bed is usually double, but is nowhere so greatly developed as on Scott’s Run. Near Waynesburg it shows coal, 1 ft. 8 in.; clay, 1 ft. 2 in.; coal, 3 ft. 2 in. Near Carmichaeltown, Greene Co., it shows coal, 3 ft. ; clay, 3 in.; coal, 3 ft. The clay is sometimes replaced by black slate with innumerable thin lamin of coal (Rogers). Near Brownsville it is five feet thick and single. In West Virginia the coal from this bed is dry, almost open-burning, gives a strong fire and is highly valued for domestic purposes. It contains a large proportion of pyrites, West of the Alleghany Mountains. 233 sufficient probably to render it unfit for general use. In Pennsylvania its quality is inferior to that of coal from the Pittsburg, while in Ohio, it is, for the most part, utterly worthless. Coal X of the Ohio section is traceable through Belmont, Harrison and Jefferson counties, Ohio. It is usually a double bed and in some localities is still further divided. At the most westerly opening seen, in Warren Township, Belmont Co., it shows: slaty coal, 1 ft 6in. Coal, good, 3 ft. At Badgersburg in the adjoining township it displays the double character more clearly as follows : Laminated shale, 4 ft.; coal, slaty, 1 ft. 7 in.; shale and clay, lft. 8 in. ; coal; 5 ft.; fireclay, 1 ft. Here the coal is of good quality and compares favorably with that obtained from the Pittsburg, but the bed is much cut up by “clay-veins” and “horse-backs” both from above and from below, difficulties which seem to beset it generally. In Union township the bed is seen triple in Section 25 as follows : Coal, \1'fts; clay,1 ft. 3*in-/; coal,4 ft. 6'in.);'shale, 1 ft.; coal, slaty, 1 ft.; fireclay, 1 ft. 3 in. Near the village of Flushing it is worked at many openings. While varying little in thickness it is exceedingly uncertain in quality; some banks yielding coal well fitted for black- smiths’ use, while that from others in the immediate neigh- borhood is hardly fit for the coarsest of domestic purposes. The general section there is Coal, 1 ft. 2 in.; shale and clay, 1 ft. 4 in.; coal, 3 ft. to 4 ft. As this bed is followed eastward toward the Ohio river it is seen to lose its thickness gradually, soon becoming of no economical importance and finally thinning out near the river. In Harrison Co., it is frequently seen at the road- sides ; but few openings are found owing to’ the ready accessi- bility and better quality of the Pittsburg. Near New Athens the following section was obtained : 234 The Upper Coal Measures Shale, 6 ft.; coal, 10 in.; fireclay, 10 in.; shale, 1 ft. 8 in.; coal, 4 ft. 8 in.; shale, 3 ft.; coal, 4 in.; shale, 3 ft. Near Cadiz the same section is repeated. In Jefferson Co., the coal is frequently seen at the roadside but is so degraded as to be worthless. It is little more than a bitumi- nous shale, two to three feet thick. It may be the coal at Knoxville one hundred feet above VIII, but is there not more than eighteen inches. Coal 1X likewise thins out before reaching the Ohio. It is seen at numerous localities in Belmont, Harrison and Jef- ferson counties, at varying distance above the Pittsburg and is usually about two feet six inches thick, divided midway by a thin clay parting. It is very persistent, rests directly on limestone and being of no-economical value, is interesting chiefly because of its relations to the Pittsburg, which will be considered farther on. It is thickest in its southeastern prolongation and thins out toward the borders of the basin, W. and N. Coal VIII c is known locally in Ohio as the Glenco Coal, having been worked somewhat extensively at the station of that name, on the Central Ohio railroad, where it is nearly four feet. Along the railroad it retains its size to Belleair, but from that point northward it diminishes rapidly, becom- ing three feet along Wheeling creek and only fifteen inches at Martinsville, five miles north from Belleair. In West Vir- ginia, from Benwood to Wheeling it shows some singular variations. Back of the furnace at Benwood it is eighteen inches ; at the stone quarry, a short distance north, it is six inches, with one foot of coal five feet above it; at the lime- stone quarry near South Wheeling, it is eight inches and the upper bed concealed; while at Wheeling it is one foot with fourteen inches of coal six feet above it. Followed up the north fork of Wheeling creek it becomes more important and is mined near Triadelphia where it shows about three feet of very fair cannel. The double character displayed along the Ohio, on the Virginia side, is occasionally ex- West of the Alleghany Mountains. 235 hibited in Belmont Co., but never to any very marked degree. The Sewickly (VIII 6) is confined, in Ohio, to the neigh- borhood of Wheeling. It may be seen on the National Road, five miles west from the river and near Glenco on the Cen- tral Ohio railroad. At Belleair it is only six inches thick and at Bridgeport barely one foot. At Benwood, on the Virginia side, it shows: Coal, 124 in.; clay, 44 in.; coal, 84 in.; slaty coal, 5 in. Total, 2 ft. 64 in. From this point to Wheeling it runs about two feet, but at Wheeling it is much degraded and shows bituminous shale, 8 in.; clay, 4 in.; cea/, 8 in. On Wheeling Creek, it shows a very complex division. Coal, 1 in.; shale, 1 ft. 3 in.; coal, 1 ft. 1 in.; clay, 3 in. ; coal, 10 in. It disappears under Wheeling creek about five miles east from Wheeling. It reappears on Scott’s Run, in Monon- galia Co., greatly increased in thickness and much changed in character. Where first seen above the run, it is five feet eight inches thick ; a short distance beyond, it is five feet and on the bank of the Monongahela river it is six feet. At all of these openings it is divided about midway by a layer of cannel from two to six inches thick. On Robinson’s Run it is four feet six inches, with a clay parting midway and the cannel layer only cne foot from the bottom. At its eastern outcrop near Laurel Hill it is only one foot thick, having been torn away during the deposition of its overlying sand- stone. It can be traced southward to the Baltimore and Ohio railroad but does not retain its thickness. The coal from this bed in West Virginia on the east side of the basin is of remarkably good quality, containing only a minute proportion of pyrites and showing little tendency to cake upon the fire. In Pennsylvania, this bed is persistent within certain limits, and varies from two to five feet in thickness. 236 The Upper Coal Measures The Ledstone (VIII a), like the preceding, is seen in Ohio, only near Wheeling. At Belleair it is six inches thick im- bedded in one foot of black shale and enclosed by the lime- stone. At the limestone quarry near Benwood, W. Va., it is barely one foot thick, a confused mass of shale and coal. At Wheeling it has the same character. On Scott’s and Robinson’s Runs, in Monongalia Co., it is from three to four feet thick, and yields a coking coal of very superior quality. In Pennsylvania it is a variable coal, ranging from eighteen inches to four feet in thickness. The Pittsburg (VIIL) is well exposed in Belmont, Guern- sey, Harrison and Jefferson counties, Ohio, as well as in Ohio, Brooke, Marion, and Monongalia counties, West Virginia. Its most westerly exposure, aside from isolated patches, is at Salesville, on the Central Ohio railroad, thirty-seven miles west from Wheeling, and its most northerly exposure, at Knoxville, Jefferson Co., about the same distance north from Wheeling. Wherever accompanied by its normal roof, shale, succeeded by limestone, it is a double bed, consisting of two or even more divisions of coal separated by shale or clay. In Guernsey and Western Belmont, where the overlying limestone shale has been removed to be replaced by sand- stone, this bed has suffered the loss of its upper layers, and for the most part is single-bedded,‘varying from four to five feet in thickness with the sandstone resting directly upon it, or at most, separated by only a few inches of shale. In some localities the eroding current excavated deep trenches in the coal itself. These, having been filled up with sand, now appear as huge sandstone “horsebacks” from five to sixty feet wide. The change in the accompanying rocks is shown in the following sections. No. I is from Barnesville, Belmont Co. No. If is from Sewellsville in the same county and north from Barnes- ville. No. III is from Moorfield, Harrison Co., and north from Barnesville. No. IV is from near Deersville, ‘‘ G3 oa (0G Ot Ot ce No. V is from Egypt, Belmont Co., a short distance east from Sewells- ville. West of the Alleghany Mountains. 237 I. II. II. TV. Vis 1. Coal x. 1. Coal x. 1. Sandstone, 40')1. Sandstone, 70'|1. Coal X. 2. Sandstone, 55'|2. Sandstone,105' 2. Limestone, 4')2. Coal vim. 2. Sandstone, 35' 3. Coal IX, 13'|3. Coal vim. 3. Shale, 5! 3. Coal IX. 4, Limestone, 53’ 4. Coal VII. 4. Limestone, 70' 5. Sandstone, 40’ 5. Shale, 5' 6. Coal VII. 6. Coal Vii. Ata short distance east from each of these localities, the heavy limestone shown in Section V is seen forty to seventy feet thick. Westward the sandstone prevails to the outcrop. A comparison of these sections shows that the heavy lime- stone of Section V has been removed to be replaced by sandstone. That the entire removal, shown in Section II, was not the work of a single current is evident from Section I. The first or earlier current exerted its force before the close of the limestone-making epoch and the formatidn of Coal IX. The five and one-half feet of limestone shown in Section I yields a hydraulic current which is equal to any manufactured in our country. The upper layer of the lime- stone of Section V possesses hydraulic properties, where exposed, along the Central Ohio railroad, at New Egypt, Flushing, at Wheeling Creek, and at other localities in Belmont County, as well as at many places in Harrison County, so that we cannot doubt that it and the limestone at Barnesville are synchronous. The force of this earlier current must have been irregular, for at Deersville it has removed both limestone and shale, but has left the coal untouched; at Moorfield it has spared the lower layer of limestone; while at Sewellsville and Barnesville it has re- moved everything above the lower division of the coal and has trenched that deeply from these points westward to the outcrop. The second current did not exist until after the formation of Coal IX, and seems to have acted more energet- ically at the north than at the south. At Barnesville it 238 The Upper Coal Measures spared not only the limestone but also the coal, whereas northward both were removed. The eastern boundary of these currents is very tortuous, but has a rudely northeast and southwest direction. They must have their origin in similar causes, as their courses coincide. As already stated, the Pittsburg, where accompanied by its normal roof, isa double coal. The roof-coal, or upper division, is subject to much variation. The partings in the lower division are very persistent. About one foot from the top is a band of pyrites, one to two inches thick; near the middle is a clay parting, about one inch, and three to eight inches below this a second clay parting resembling the first ; below this a thin band of pyrites is frequently found, but it is not persistent. The middle bench, between the clay partings, is ordinarily very pure, and well adapted to smiths’ use. In Millwood and Londonderry townships, Guernsey Co., Ohio, the coal is single-bedded, with a sandstone roof, and varies little from four feet in thickness. In Warren and Kirkwood townships, Belmont Co., wherever roofed by sand- stone, it is single-bedded and badly cut out. In Oxford township, Guernsey Co., the roof-coal is occasionally seen one foot thick and separated by shale from the lower divi- sion. Near Deersville, in Harrison Co., the coal is opened and gives the following section :— Goal, 10 in.gclay..10 ins coal. ft; The intimate structure of the lower division, as shown in an opening here, is peculiar in the thickness of the middle bench : Coal, 1 ft. 6 in.; pyrites band, 14 in.; coal, 2 in.; clay parting, $ in.; coal, 1 ft. 3 in.; clay parting, 1 in.; coal, LOam, s\ total, 4: ftss tan. In the neighborhood of these sections the coal is soft, not good for hard firing, but is quite pure and shows few streaks or nodules of pyrites. Followed eastward the coal thickens, West of the Alleghany Mountains. 239 becomes harder and less pure. About a mile west from Cadiz it shows : Bituminous shale, 4 ft.; coal, 1 ft. 3 in.; clay, 1 ft. 2 in.4; “cod.,, ©: ft..'6 in. At Cadiz the following section is said to exist in the shaft of the coal works :— Coal, 2 ft.; limestone, 5 ft.; clay, 2 ft.; coal, 5 ft. It is impossible to verify this report, given by the fore- man, as the shaft is boarded up. If it be a true section it is exceedingly anomalous, for no such succession is to be seen in the neighborhood, and there are good exposures near by. Through this district the coal seems to be exceedingly pure, no pyrites are visible except in the two bands, and blacksmiths pronounce the coal admirably fitted for their use. Yet analysis shows that it contains upwards of two per cent. of sulphur in its best part. That this is distributed thtoughout the coal as pyrites and not as an organic com- pound is evident from the fact that more than one-half re- mains after coking, forming almost tw6 per cent. of the coke. At the most northerly exposure of the bed near Jefferson, the intimate structure of the whole bed is as follows :— Cole litte. Grim. si (clay. nds ft.06 tints) coalte 1" ft. 9" im, 5 clay parting, 4 in.; coal, 6 in.; clay parting, 4 in.; coal, 1 fb-2 ines; clay! parting, 4 1n.; coal, 91 {ty 2. in. 3: total of lower division, 4 ft. 8 in. The upper pyrites band is not persistent at this opening, and where seen is one-fifth of an inch thick. The lower band was not observed. Near Hanover, at the northwestern exposure of the bed, the clay between the coals has almost disappeared, and we find ftoof-coal, 1 ft. 6 in.; clay parting, 4 in.; coal, 3 ft. 11 in. : The roof-coal is slaty and easily recognized as separate from the main coal below. In Jefferson Co., this bed lies for the most part high up in the hills, and there are few ex- JANUARY, 1873. 17 ANN. Lyc. NAT. HIST., VOL. X 240 The Upper Coal Measures tensive openings. Near Unionport, on the Panhandle road, at the northern outcrop, several banks have been opened, but none of them show the roof-coal. The roof is shale succeeded by sandstone, and the coal is 4 ft. 2 in. to 4 ft. 9 in. thick, with the following structure. Coal, 1 ft. 2 in.; clay, $ in. ; coal, 6 in. ; clay $ in. ; coal, 94 in.; Clay, 4 ims coal, lin; ‘clay4 im; coal, 24t. The pyrites bands are not persistent here but streaks and nodules are quite numerous. At another opening about half a mile from these, the roof-coal is still absent, the roof being shale, six feet thick, succeeded by sandstone. Following the road from Unionport to York several openings are seen, at one of which the following section was obtained : Coal, tts 6 ines clay, 10n.);\ coal, ‘Sitteito o Tt: enn: The roof-coal throughout this district seldom exceeds ten inches and the lower coal is much injured by pyrites both in nodules and streaks. In the neighborhood of Mt. Pleasant the roof-coal varies from one to three feet, and on Rush Run it is said to be five feet at one opening, though only three feet were exposed at the time of my visit. In Belmont Co., at Hendrysburg, just east of the sand- stone deposit the coal shows : Coal, 10 in.; clay, 4 in. ; shale with thin lamine of coal, 1 ft.; coal, 4 ft. 8in. On Jug Run, a tributary of Wheel- ing creek, the roof-coal is divided, a condition rarely seen in Ohio, except along Wheeling creek, where it is quite common. ‘The section is Coal, 6 in.; clay, 8 in.; coal, 10-15 in.; clay 10-15 in. ; coal, 5 ft. In Colerain township, on Hughes’ Run, the lower division becomes 5 ft. 8 in. On Barr’s Run, the subdivision of the roof-coal is extraor- dinary, as follows: Ooal, 3 in.; black shale, $ in.; coal, 14 in.; shale $ in. ; coal, 10 in.; shale, 1 in.; coal, 14 in.; shale 5 in.; coal 14 in. ; with the lower division 4 ft. 10 in. seen. West of the Alleghany Mountains. 241 In Pease township, on Wheeling creek, the whole bed is greatly expanded. At one opening we find Coal, 1 ft. 6 in.; shale 8 in.; coal, 10 to 18 in.; clay, 8 in.; coal, 5 ft. 2 in. to 6 ft. In one or two neighboring openings the lower coal becomes seven feet. Here the coal is of excellent quality for fuel, though containing too much sulphur to be of value in the manufacture of iron or gas. The intimate structure of the lower bed is shown here to be Coal, 2 ft. 5 in.; parting, 1 in.; coal, 3 in.; parting, 1 ime coals a tte toro Tt.no als The upper pyrites band is seen persistently at from twelve to fourteen inches from the top, and the clay partings are full of pyrites. Nodules occur occasionally, but are small and easily separated. Along the Ohio river the roof-coal again becomes single, while the lower coal retains its thick- ness. Two or three miles above Martinsville we find coal, Zi ttesclay, 6 in.) to 2 its; coals 4ft..9 in:itor6. {63 Here the roof-coal has not been mined. It is usually left with the clay parting to make a firm roof. The clay is much slickensided, rendering it liable to fall after removal of the coal below. Crossing the river into West Virginia we find this coal ex- tensively worked from Benwood opposite Belleair to twelve miles north from Wheeling, as well as on both branches of Wheeling creek. As might hardly be expected it shows little variation in character and the following is a represen- tative section : Coal, 1 ft. 3m. to 1 ft: 8 in. ; clay,-1 ft. ; coal, 5 to 6 ft. Rarely a thin shale is found dividing the roof-coal. East- ward the bed disappears about five miles from Wheeling, and at the same distance southward it passes under the Bal- timore and Ohio railroad, the dip being southeast. Follow- ing the railroad we see the coal again at Fairmont, about eighty miles S. S. E. from Wheeling, dipping sharply to the northwest. Here it is single-bedded, about nine feet thick, and roofed by a heavy felspathic sandstone which is coarse 242 The Upper Coal leasures grained and contains numerous coaly spots, evidently eroded coal. The coal from this locality is coked and tests have been made at Wheeling to determine its value in iron-making. It proves to be too impure for use even when mixed with thrice its bulk of Connellsville coke. It is, however, much more compact than that coke, and if it could be cleaned by washing would undoubtedly be employed in preference. Along the base of Laurel Hill (Chestnut Hill, of Pennsyl- . vania Reports), from Fairmont to the junction of Cheat and Monongahela rivers we find the coal always single-bedded and roofed by this coarse sandstone, though occasionally separated from it by a few inches of shale. The roof is very irregular and gives evidence that the eroding current which removed the upper beds, tore out much of the lower coal, which, indeed, near Morgantown is sometimes reduced to six feet, though seldom less than eight. Crossing the Monongahela we find a number of openings on Scott’s Run, which give the following general section : Coal dine; shale fte9 in; $:coals In ft-3ansishale,.buit. Ssimesacods. LOat. On Courtney’s Run, one mile below Scott’s Run, we get Coal, slaty, 1 ft. 9 in.; shale, 3 ft. 5 in.; coal, 44 in. ; shale, 1 ft. 10 in. ; coal, 1 ft. 4 in. ; shale, 10 in. ; coal, 8 ft. 8 in. On Robinson’s Run, one mile farther down, we find Slaty coal, 2 ft.; black shale, 3 ft. 6 in.; bituminous slate, 10 in.; coal, 1 ft. 3 in. ; bituminous shale, 1 ft. ; coal, 8 ft., exposed. Here, within a distance of six miles, the bed is seen first single-bedded, next, on Scott’s Run the roof-coal is present and double, on Courtney’s, a third layer is added to the roof, while on Robinson’s, the two layers seen on Scott’s lie together, though they are clearly distinct. In Pennsylvania, the character of this bed varies in the different basins, and is found only south of the Ohio and Conemaugh rivers. In the first basin south of those rivers West of the Alleghany Mountains. 243 it is about nine feet thick and single; in the second eight and one-half, and siagle ; while in the third it is double with the lower division averaging between nine and ten feet, and the upper varying from two to five and one-half. RELATIONS OF THE PITTSBURG AND THE SUPERIOR COALS. It has been stated that Coals VIII a, VIII 6 and VIII ¢ of the Ohio section are to be seen only in the neighborhood of Wheeling’ and that their relation to coai VIII would be considered especially. Coal TX, though observable over a much larger area in Ohio is evidently related to VII in the same manner as the intermediate beds. That the matter may be clearly set forth, the following sections are introduced :— No. Lis from the Central Ohio railroad, eight miles from Belleair. No. II is from New Egypt, Belmont Co., Ohio. No. III is from Flushing, Belmont Co., Ohio. No. IV is from near Cadiz, Harrison Co., Ohio. No. V is from near York, Jefferson Co., Ohio. No. VI is from near Unionport, Jefferson Co., Ohio. No. VII is from Knoxville, Jefferson Co., Ohio (H. Newton). The section on the railroad is representative of a consider- able area and, in all important points, can be duplicated at Belleair and at many localities along Wheeling creek and the Ohio river. The sections obtained here cannot be directly connected with the others given, as high dividing ridges sur- round the portion of the state represented by Sect. I. The Cadiz section is virtually characteristic of eastern Harrison, but northwest the limestone No. IV becomes thinner as we approach the outcrop. 244 The Upper Coal Measures 18 Th IV. | VI. 1. Coal x, —| 1. Coal x, —| 1. Coal x, —| 1. Coal x, ? 2. Sandstone, 35’] 2. Sandstone, 35'| 2. Sandstone, 75'| 2. Sandstone, 85’ 3. Coal 1x, 23'| 8. Coal 1x, 23'| 3. Coal Ix, 2'| 8. Coal VIII, 5! 4. Limestone, 70') 4. Limestone, 70'| 4. Limestone, 20' 5. Coal vittc, 4’! 5. Shales, 5’| 5. Shales, 4' 6. Sandstone, 18’! 6. Coal vim, 7'| 6. Coal vim, 8' 7. Coal viIl b, 1%' 8. Limestone, 20’ 1G0 VII. V. 9. Coal Vila, 1%'| 1. Coal x, _— 1. Coal=x, 1}! 1. Coal x, St 10. Limestone, 20’) 2. Sandstone, 60’ 2. Sandstone and } 2. Sandstone, 85! shale, 100 11. Shale, 5'| 3. Coal 1x, — 3. Coal Ix, 13'| 3. Coal vu _ 12. Coal vuI, 8'| 4. Limestone, 38' 4, Limestone and shale 7’ 5. Shales, 4' 5. Coal vim, 64' 6. Coal vii, 6' Should one follow Wheeling creek, Ohio, from its mouth to where it becomes Patterson’s creek, he will find VIII ¢ in its banks, as well as in those of its tributaries. Along the bottoms of Patterson’s creek, which flows northeast, he will see it worked by stripping. But before reaching Union township the creek bed is some distance above it. Crossing the dividing ridge and descending into the valley of Spen- cer’s creek, he will find Section II, six miles west of the locality where he last saw VIII c. If, however, instead of following Patterson’s creek, he take the branch flowing from the northwest, he will lose sight of VIII ¢ near Uniontown, and six miles further he will obtain Section II. The result is similar in other directions. In each of these sections a coal is seen one hundred feet, more or less, below Coal X. In No. Tit is VII c, in the others it is VIII. The accuracy of this identification has been questioned, so that the grounds on which it is made should be stated distinctly. Ascending the Central Ohio railroad from Belleair to the summit, twenty-two miles west from the Ohio river, nine beds of coal are seen, beginning with the Pittsburg (VIII). West of the Alleghany Mountains. | 245 Descending from the summit to Quaker City, thirty-five miles west from the river, only six can be seen, and at Quaker City the crinoidal limestone occurs. The relation of the sections is as follows :-— ASCENDING. DESCENDING. 1. Coal xin. 1. Coal X11. 2. Shales and sandstone, 70'| 2. Shale and Sandstone, 70' 8. Coal X11. 3. Coal x11. 4. Shaly sandstone, 40'| 4. Shale and Sandstone, 30° 5. Coal Xi. 5. Coal Xt. 6. Sandstone and shales, 98'| 6. Sandstones with thin limestones and shales, H 4. Coal x. np COAL Se 8. Sandstone, Sou : 8. Sandstone, 60' 9. Coal Ix. 9. Coal Ix. 10. Limestone, 70' 10. Limestone, 53! ll. Coal vim c. 11. Sandstone, 45' 12. Sandstone, 18-35! 12. Coal vii. 13. Coal vu b. 13. Fireclay, 5’ 14. Limestone, 20’ 14. Limestone, 3! 15. Coal Vii a. 15. Sandstones and variegated shales, 150’ 16. Limestone, 20-25" 16. Crinoidal Limestone. 17. Shales, 5-10’ 18. Coal Vi, 19. Fireclay and shales with thin limestone. 10’ 20. Sandstone, 90' It is evident from these sections, that east and west of the summit the strata are identical to No. 10 ot each, including, as was previously shown, No. 11 of the second; and it is equally evident that*No. 12 of the second cannot be No. 11 of the first, but that it must be Coal VIII or the Pitisburg. The internal anatomy of the bed shows this, for even along the Central Ohio railroad, where the upper division has been re- moved, we find the characieristic pyrites baud and the clay partings. But in order to remove all possible doubt, the 246 ; The Upper Coal Measures Coal VIII of the second section was carefully traced with its crinoidal limestone along its western and northern outcrop, fromgSalesville, in Guernsey Co., to the Ohio river at Steu- benville. From Steubenville it was easily followed down the river to Belleair, where it was found to be identical with Coal VIII of the first section. It is clear, then, that the coals between VIII and IX have disappeared somewhere within the dividing ridges of Belmont Co. One would expect to find the successive disappearances along the Ohio, but the coals become very thin above Belleair and the superficial deposits are so thick that accurate tracing is impossible. It is well to note that wherever VIII ¢ occurs, it has the same relative position to Coal X that Coal VIII holds west and north of the dividing ridges in Belmont Co., the interval in each case being about one hundred feet. The gradual disappearance of the limestone below Coal TX and the merging of that coal into Coal VIII are more easily traced. In Section I on the Central Ohio railroad the lime- stone is seventy feet; at Barnesville the interval, including the shales and upper layers of Coal VIII, is only forty-five feet; at New Egypt, considerably east of Barnesville, it is seventy feet; at Flushing, north from Egypt, it is thirty- eight; at Cadiz, northeast from Flushing, it is only twenty feet, and diminishes rapidly to the northwest, being only five feet at Hanover; at York it is seven feet, including the shales, overlying VIII; while at Unionport and Knoxville the limestone does not exist and Coal LX itself has disap- peared. From a careful study of these facts I am led to be- lieve that here we have a series of bifurcations of Coal VIII almost as extensive and interesting as those said to occur in the Mammoth bed of the anthracite region. It is worthy of note in this connection that the distance between Coals VIII and X gradually diminishes northward, from one hundred and five feet on the Central Ohio railroad to eighty-five feet at Unionport, and the interval between X and XI diminishes in the same direction from one hundred feet on the railroad West of the Alleghany Mountains. . 247 to sixty feet at York. Under these circumstances I am inclined to look upon the thin coal, one hundred feet above Coal VIII at Knoxville as XI and not X. Thinning out northward, like the lower coals, as these beds do, and grad- ually nearing Coal VIII, it is more than probable that they in like manner were successively merged into Coal VIII, which I regard as the parent bed of all the upper coals in Ohio, remaining in existence as a flourishing swamp from the beginning of the epoch until its close. A similar condition seems to have existed on the eastern shore of the inland sea, though it is somewhat difficult to obtain thoroughly satisfactory evidence, owing to the pecu- liar manner in which information is scattered through the Pennsylvania report. Three short sections have been taken from that report, one from each of the three basins south of the Ohio. 3D BASIN, REDSTONE CREEK. 2D BASIN, LIGONIER. 1ST BASIN. ELK LICK. . Sewickly Coal (vit b), 4'| 1. Sewickly Coal (vit b), 3'| 1. Sewickly Coal (vu b), ? . Shale, 2'| 2. Not seen, 5’'| 2. Sandstone, 25' . Limestone, 6 | 3. Limestone, 6'| 3. Shale, 15' . Shale, 40 | 4. Shale, 10'| 4. Pittsburg Coal (vil), 9' . Redstone Coal (vVuit a), 24'| 5. Redstone Coal (Vu a), 3’ . Shales and sandstone, 35'| 6. Shales, 20' NY aoa ao fF OO YH . Pittsburg Coal (vim), 14'| 7. Pittsburg Coal (vi), 8%' CONDITIONS DURING DEPOSITION OF THE UPPER COAL MEASURES. To many it may appear that the data presented in this paper are insufficient to justify generalization respecting the conditions prevailing during the epoch of the upper coal measures. But let it be remembered that the portion of the field examined is by far the most important economically and by far the most satisfactory in the exhibition of details. 248 The Upper Coal Measures South from the railroad line bounding our observations, the greater portion of the section, which we have been discuss- ing, disappears and the only information to be obtained respecting it is found along the line of outcrop on the west, or on the steep mountain slopes on the east. In no other portion of the basin can details be obtained respecting the strata below the Waynesburg coal. ‘To give a fair illustra- tion I have introduced for comparison four sections from the east side of the basin and four from the west side as follows: I from Wheeling. II from Barnesville, Ohio. III from near Georgetown, Ohio. IV from near York, Ohio. V from Ligonier, Penn. (Rogers). VI from Monongalia Co., West Virginia. VII from Uniontown, Penn. (Rogers). VIII from Elk Lick, Penn. (Rogers). if is I 1. Waynesburg Coal (X1), 3 |12. Shale, 3'|23. Coal, | 1;' 2. Shale, 33 |13. Limestone and Shale, 13'|/24. Sandstone, }VIII c, 6' 3. Limestone, 15 |14. Shale, 6'|25. Coal, \ 1 4. Sandstone, 3'|15. Limestone, 2'|26. Sandstone, 8-24’ 5. Limestone, 5'|16. Shale, 4'|27. Sewickly Coal (v111 b), 13' 6. Shale, 5'|17. Limestone, 34'|28. Limestone, 24’ 7. Limestone, 2'/18. Shale, 3'|29. Redstone Coal (vil a), 1' 8. Shale, 2'|19. Limestone, 1'|30. Limestone, oo 9. Limestone and Shale, 11'|20. Shale, 3'|31. Shale, 6’ 10. Shale, 5'|21. Limestone and Shale 194'| 32. Pittsburg Coal(vim) 8' 11. Limestone, 44'/22. Shale, 3! I. II. If. 1. Waynesburg Coal (Xi) 4-5'| 5, Coal x, 4'| 9. Sandstone, 40' 2. Sandstone and Shale, 50'} 6 Sandstone, 55'|10. Pittsburg Coal(vum) 4’ 3. Limestone, 6'| 7. Cocl Ix, 13! 4. Sandstone and Shale, 45'| 8. Limestone, 52" West of the Alleghany Mountains. 249 Il. 1. Waynesburg Coal (X1), 2' 2. Shale, Gy 3. Limestone, 10' 4. Sandstone, 20’ 5. Limestone, 10’ 6. Sandstone, 25' 7. Limestone, if 8. Sandstone, 8' 9. Shale, 6' 10. Coal x, 43! 11. Shale, 10’ 12. Sandstone, 55' 13. Coal 1x, 23! 14. Limestone, 25' 15. Shale, 6! 16. Pittsburg Coal (V1), 7-8' IV. 1. Waynesburg Coal (1X), ? 2. Shale and Sandstone, Oo FO em WwW . Coal x, . Coal Ix, . Shale with thin lime- with Limestone no- dules, 60' 3! . Sandstone and Shale, 85' 1! ! stone, . Pittsburg Coal (vin), 64 Vis 1. Coal (Uniontown?) (X ?) | 2. Not seen, 10 3. Limestone, uh 4. Sandstone, 35! 5. Sewickly Coal (vii b), 3’ 6. Not seen, On 7. Limestone, 4-8' 8. Shale, 10’ 9. Redstone Coal (VIII a), 3' 10. Shale, 20’ ll. Pittsburg Coal (vit), 8%' Wak 1. Waynesburg Coal (X1), 9’ 2. Sandstone, 15’ 3. Shale, 8' 4. Limestone, 5! 5. Shale, 4" 6. Sandstone, 1b 7. Limestone, 30’ 8. Sandstone, 25" 9. Limestone, 6' 10. Sandstone, iby 11. Limestone, 7- 12. Sandstone, 10' 13. Limestone, 8’ 14. Shale, 12’ 15. Sandstone, 31 16. Sewickly Coal, 5’ 17. Shale, 8’ 18. Limestone, ae 19. Sandstone, 10' 20. Limestone, 22' 21. Redstone Coal, 4’ 22. Limestone, 12’ 23. Shale, 8’ 24. Pittsburg Coal, 14’ 2. Limestone, sandstone and shale, 3. Shale, iby 4. Sandstone and some limestone, 110’? 5. Sewickly Coal, 43’ 6. Shale, 2' 7. Limestone, 6' 8. Shale, 40’ 9. Redstone Coal, 1-23’ 10. Shale with calcareous nodules, 15 11. Sandstone, Dy 12. Shale, 15’ 13. Pittsburg Coal, 14' VII. 1. Coal, ? 2. Sandstone, 50’ 3. Sewickly Coal, ? 4. Sandstone, 25’ 5. Shale, 15’ 6. Pittsburg Coal, GP . Limestone, NEE: 12’ 250 The Upper Coal Measures The relative geographical positions of these localities, as well as those of some others already referred to, are shown in the following diagram. *19A0TB A * * S * Knoxville. : = re % Ligonier. ; e % a* oO fo} a @ * oS BS * 4 F a * Union, v : Lb, Lom, gy Barnesville.* G,. % % o Scott’s Run. A similar series of sections of the Barren measures shows that the strata of that group diminish in thickness east and west of the central portion of the basin. There can be no doubt, therefore, that at the beginning of the Barren epoch, the Alleghany basin had already its present shape and was bounded on the west by the slopes of the Cincinnati axis, on the east by the slopes of a similar axis. The events of the succeeding epoch seem to show that the Cincinnati axis had attained its highest elevation before the deposition of the upper coal measures began. At the close of the Barren epoch, the northern portion of the basin was a half-filled valley such as is now presented by the bed of the Ohio river, below Smith’s Ferry. A comparison of the upper coal measure sections given above, shows that as we leave the middle of the basin we find the limestones diminishing in every direction. In the portion below Coal X, these limestones, followed west and north do not give place to off-shore deposits, but simply disappear and permit the coal-beds to approach each other; whereas, eastward, they interlock with sandstones and shales, before West of the Alleghany Mountains. 251 disappearing, which in their turn thin out as do the lime- stones on the west side of the basin. This is evidence of clear, quiet waters on the west, while rivers or shore cur- rents carried in their freight of sand and mud from the east and northeast. - After the formation of Ooal X, which, as has been stated, may have been synchronous with the Uniontown of Pennsyl- vania, the conditions were more nearly alike throughout the basin until the formation of the Waynesburg, though at the east and west, alternations of limestone and sandstone during the greater portion of the interval give evidence of neighbor- ing shores. The limestone is still greatest in the central portions, but is easily traceable in strata or nodules as far west as Barnesville, north as Unionport, and east as Elk Lick creek, all on the line of final outcrop. On the west side of the basin, we find the Redstone, Se- wickly, VIII cand LX successively merged into the Pittsburg. On the east side we find the Redstone disappearing and the Sewickly brought nearer to the Pittsburg by so much as the Redstone was distant from it, while the interval between the Sewickly and the Uniontown (X ?) is reduced at the most easterly exposure to barely one-third of what it is nearer the central portion, on the Monongahela. We have thus evidence of a series of gradual subsidences, separated by intervals of repose, during each of which a lid of coal was formed over all or a part of the basin. These subsi- dences could not have been paroxysmal, for we find that as the shore-line sank, the great Pittsburg marsh crept up the shore, continually from the beginning of the epoch until long after the formation of Coal IX, perhaps until the very close of the epoch. Thus it is that, although giving origin to so many subordinate seams, the great coal bed diminishes in thickness when followed west from the Ohio, or east from the immediate valley of the Monongahela. ; It is highly probable that the Pittsburg was begun on the east and advanced westwardly. We have ample evidence in 252 | Lingual Dentition of Geotis. the sandstone and shale, which at the east separate it from its limestone, that a delta was there forming and pushing out to the west, so that on the east the conditions requisite for the formation of coal would first exist. On the east side of the basin we find nine to ten feet in the lower division of the bed, while on the west side we find only five to six feet. I am led, then, to the following conclusions : 1. The Great Bituminous Trough, west of the Alleghanies, does not owe its basin shape primarily to the Appalachian Revolution. 2. The coal measures of this basin were not united to those of Indiana and Illinois at any time posterior to the lower coal measure epoch, and probably were always distinct. 3. The upper coal measures originally extended as far west as the Muskingum River, in Ohio. 4, Throughout the upper coal measure epoch the general condition was one of subsidence interrupted by longer or shorter intervals of reposé. During subsidence the P%éts- burg marsh crept up the shore, and at each of the longer intervals of repose pushed out seaward upon the advancing land, thus giving rise to the successive coal-beds of the upper coal measures. 5. The Pittsburg marsh had its origin at the east. XXI.— On the Lingual Dentition of Geotis. By THOS. BLAND ann W. G. BINNEY. Read January 6, 1873. THE genus (eotis was described by Shuttleworth,* founded on acurious mollusk from Porto Rico. The lingual denti- tion was said to be nearly the same as in Vetrina and Zonites, the teeth arranged in oblique rows, centrals obtusely tri- *“ Tamina lingualis fere ut in Vitrina et Zonites constituta videtur, papille nempe numeros in seriebus utrinque obliquis ordinate sunt: papilla centrali obtuse tri dentata; mediis vix a centrali diversis; lateralibus autem subulato-productis, arcuatis basi? bifurcatis. An maxilla adsit heret.” ‘‘E formatione liuguze animal videtur sine dubio carniyorum.” Shuttleworth, Bern Mit. 1854, p. 34, i Lingual Dentition of Geotis. 253 dentate, laterals scarcely differing from the centrals, mar- ginals lengthened, awl-shaped, arcuate, at base ? bifurcate. The presence of a jaw was not verified by Shuttleworth. The character of the dentition was considered such as to denote carnivorous habits of the animal. This is all the information as to the lingual dentition of Geeotis hitherto published. Moérch, indeed, places the genus (Jour. de Conch. 1865, 384) in his section Odontognatha, which comprises the Terrestrial Pulmonata furnished with a ribbed jaw, not from any original investigations, but simply from its assumed identity with Parmacella, a genus believed to have a ribbed jaw, judging from the obscure figure given by Férussac of the mouth of Parmacella palliolum (Hist. t. 8 A, fig. 8). Shuttleworth’s descr’ption rather indicates the form of dentition figured by us (Land and Fresh Water Shells, 1), of many species of Vitrina, Hyalina and Zonites. The bifurcated base of the marginal teeth may even be sup- posed to be such as we have figured (/. c. 17) in the centrals of Glandina truncata. We have long had in our possession the jaw and lingual membrane of a specimen of Geotis from Porto Rico. The animal was received many years ago by one of us (Bland) from the late Mr. Robert Swift, the aleohol in which it was originally preserved evaporated, and the jaw and lingual membrane were, not very long since obtained, by macera- tion, in a somewhat imperfect condition. Comparing the latter with Shuttleworth’s description, we find that at first we had misunderstood his words, which, indeed, are quite liable to mislead, especially in the infelicitous comparison with Vitrina and Zonites. We give, therefore, a more de- tailed description and figure, in order to prevent further errors. Jaw (plate xi, fig. 1) long, low, slightly arcuate, ends attenuated, ex- tremely thin and delicate, transparent: in one single piece, but divided by over forty* delicate ribs into as many plate-like compartments of the type * Fragments only of the jaw were saved; the largest one we have figured, and from it estimate the whole number of ribs. 254 Lingual Dentition of Geeotis. common in Bulimulus and Cylindrella, but without the upper median tri- angular plate characteristic of the latter; both margins scarcely serrated by the ends of the ribs. From our numerous observations on the jaws of Pulmo- nata (see Ann. Lye. N. H. of N. Y., X, 165), we consider this to be a form of ribbed jaw, the plate-like sections being actually divided by delicate longitudinal ribs. It is to be understood that the jaw is not in separate pieces, as in Or- thalicus and Liguus (see Ibid, p. 168). Our figure of the jaw of Helix turbiniformis, Pfr. (Ibid, pl. ii, fig. 2), gives the same type of jaw, though differing in form. That of Succinea ? appendiculata (Ibid, X, pl. ix, tig. 2) is still nearer the jaw we are considering. The lingual membrane is entirely different from what we had supposed from our interpretation of Shuttleworth’s de- scription. We recognize no resemblance to that of Zoniles and Vitrina, but rather (in arrangement and shape of teeth and position of cusp) to that figured by us of Orthalicus zebra and undatus (Amer. Jour. of Conch. 1870, pl. ix, fios. 2, 6,10, 12,) and Liguus fasciatus drawn by Leidy, (Terr. Moll. U. S. II, 270). From these, however, it dif- fers in the development of its cusp, which shares the trifid character, and nearly resembles that of Helix muscarum (Am. Jour. Conch. /. c. fig. 4). Lingual membrane long and broad, composed of numerous rows of teeth arranged en chevron. Centrals very long, narrow, obtuse above, incurved at sides, obtusely rounded and expanded at base near which is a short, gouge-shaped, expanded cusp, whose lower edge is bluntly triden- tate. Laterals same as centrals in shape, but a little larger, and unsym- metrical from the disproportionate expansion of the outer denticle of the cusp. Marginals same as laterals, but more slender, with more developed and graceful teeth, of which the median is pointed, often bifid. Thereis much variety in the shape and denticulation of the cusps. The middle denticle is always the smallest. We find no distinct marginal teeth of the aculeate type noticed by Shuttleworth, but believe he was misled by see- ing these teeth in exact profile, when they have somewhat that form as shown in our figure 6. Seen from above, Lingual Dentition in Physa. 255 however, the same teeth retain their subquadrate form, figure 7. Both jaw and lingual membrane, therefore, prove that the genus belongs to the /7elicine of our pro- posed arrangement of Pulmonata (see Ann. Lyc. N. H. of N. Y., J. c. 165), or to the Helicea of von Martens. (Die Heliceen, ed. 2.) By its jaw, Geot?s calls to our mind the genus Amphibu- lima (see pl. xi, fig. 8), as well as the shell known as Suc- cinea? appendiculata Pfr., whose generic position we have left in doubt (Ibid, X, pl. ix, fig. 2), and many species of Bulimulus. We have above shown the resemblance of its lingual dentition to that of Orthalicus and Liguus, as well as of Helix muscarum. It also forcibly reminds one of some of the features of the dentition of Triboniophorus. Our figure 5, plate xi, gives the central and adjacent lat- eral teeth: fig. 6 an extreme marginal in profile, on a dif- ferent scale of enlargement: fig. 7 a marginal seen as in fig. 6: fig. 1 the largest fragment saved of the jaw. XXII. — Note on a curious form of Lingual Dentition in Physa. By THOS. BLAND AND W. G. BINNEY. Read January 6, 18738. WE have received from Governor Rawson specimens in alcohol of a shell apparently belonging to: the genus Physa, collected at Point 4 Pitre by M. Schramm. On examining its jaw and lingual dentition, we find both different from what is usual in that genus. The jaw is not at all chevron- shaped,* but is simply slightly arcuate, long, low, ends atten- uated. The lingual membrane wants entirely the broad transverse rows of comb-like teeth arranged en chevron * See figure of jaw of Physa in Land and Fresh Water Shells of North America, IT, p. 75, fig. 123. JANUARY, 1873. 18 ANN. Lyc. NAT. HIST., VOL. X. 256 Lingual Dentition in Physa. which are characteristic of Physa.* On the other hand, the lingual membrane is long and narrow, with almost horizontal rows of teeth. The centrals are narrow, somewhat expanded at the base, at apex recurved into a slightly produced quin- quedentate cusp, the central denticle the largest. The later- als are quadrate, the whole apex recurved into a broad cusp produced almost to the base of the tooth, with one large, inner, stout, pointed denticle which bears on its inner side another small pointed denticle, and two, small, irregular, sharp, side denticles. The marginals are but modifications of the laterals, wider than high, with one bluntly bifid inner, and several small, blunt, irregular side denticles. The centrals and laterals are like those of Limneat} rather than of Physa, the marginals more like those of Planorbist but much more quadrate. In our figure 2 of plate xi, we give one central and several lateral teeth, in fig. 3 one marginal: fig. 4 represents the jaw. A view of the shell is also given in fig. 9. We have not been able to determine this species of Physa, represented by M. Schramm to be very rare. In some re- spects it appears to be allied to P. striata D’Orb. (Cuba I. 192, Tab. xiii, figs. 14-16), received by that author from M. Ferdinand de Candé, but whether from Martinique or Cuba was not positively known. EXPLANATION OF PLATE XI. . A portion of jaw of Geotis (p. 253.) . Physa——? (See p. 255.) One central tooth and two laterals from the lingual membrane. 3. The same as 2. One marginal tooth. 4. The same. The jaw. Fig. | ol * See Ibid, p. 81, fig. 138: p. 82, fig. 141. Physa ampullacea, Gld. from Colorado Ter- ritory, lately collected by Dr. E. Palmer, has the same type of lingual. Dall has detected amore simple form of tooth alternating with the comb-like laterals of Physa. See his exhaustive review of Limneide etc., in Ann. of Lyc. N. H. of N. Y., IX, 333, for valu- able information on the dentition of the tresh water Pulmonates. ySee our figures in the Amer. Jour. of Conch., 1871, pl. xii. $See our figure in Ann. of Lyc. N. H. of N. Y., IX, p. 292. Catalogue of the Pyralide of California, etc. 257 Fig. 5. Lingual dentition of Geotis. One central tooth with adjacent laterals. 6. Same as last, but more enlarged An extreme marginal tooth in profile. . Sameas 5. An extreme marginal tooth. 8. Amphibulima patula (see p. 225.) The jaw folded as it appears on the microscope slide, the position taken from its extreme tenuity. 9. Physa sp. indet. Shell. Jaw and Lingual dentition. Figs. 2-4. to | XXHI.—Catalogue of the Pyralide of California, with descriptions of new Californian Pterophoride. By A. S. PACKARD, Jr. Read January 6, 1873. Tus catalogue of the Pyralid moths of the Pacific states is published more to show how extremely limited is our present knowledge of this family, as regards the region west of the Rocky Mountains, than to give a view of the group as developed in that part of the world. Neither Guenée in his “Histoire Naturelle des Insects, Species général des Lépidop- teres,” Tome VII, Deltoides et Pyralites (1854), nor Bois- duval* in his writings on the Lepidoptera of California, mention any species of this family, and it is believed that, with the exception of Botys fodinalis, described by Mr. Lederer from California, the following descriptions are the first references to the California species of this interesting group. For my material I am chiefly indebted to Mr. Henry Edwards, of San Francisco, to whose energy in collecting, the science of entomology is under so many obligations. A few specimens have been received from Mr. Junius Holleman of Goose Lake, near Fort Bidwell, Siskiyou County, Cal. *Lépidoptéres de la Californie (Annales Soc. Ent. France, Sér. 2, 1852, Tome 10, p. 275-324; sér. 3, 1855, Tome 3). Bull. p. 31. See also Annals Soc. Ent. Belgique, Tome xii, 5, 1869. 258 Catalogue of the Pyralide of California, etc. Among those he sent are some extremely interesting Cram- bus-like forms, one with pectinated antennz, too imperfectly preserved for description, but sufficiently so to indicate some remarkable types of this group of the family. Several inter- esting forms have been received from Mr. James Behrings. An interesting fact in geographical distribution is the con- siderable extension given to the range of one of the probably cosmopolitan species of moths. I refer to the MNomophila noctuella (Schiff.). It has hitherto been reported by Guenée from different parts of Europe, Algeria, Caffraria, Bengal, Pondicherry, Brazil, and Philadelphia. It has also been known by myself to occur in New England and New York, and now it has been received from Oregon, near the Cali- fornian state boundary line, from Siskiyou Co., California, near the Oregon line, and from the vicinity of San Francisco. Occurring so far inland as the settlements about Fort Bid- well, Siskiyou County, and also the newly settled portions of Oregon, it may be inferred that this species has not been introduced by man, and that it is probably autochthonous where it has been observed, at least in America. A variable moth wherever it occurs, it varies in much the same manner in California as in Europe. Such cosmopolitan forms give rise to the suspicion that they are relics of a preceding geo- logic age, which is borne out by the fact that quite a gap separates it from its nearest allies. Another point of interest is to ascertain what European features occur in the few species yet known of this family. The assemblage, so far as our rather scanty knowledge of this group may be depended upon, is allied as closely to the fauna of eastern North America as to Europe, as seen in the species of Botys and Cataclysta. In the group of Ptero- phoride one species quite unlike any European one, so far as I am aware, has a very close ally in New England. In the measurements hundredths of an inch are used, and instead of indicating the alar expanse, the length of one fore wing is given to secure greater exactitude. Catalogue of the Pyralide of California, etc. 259 Pempelia fenestrella, n. sp.-—2g 49. In this species the fore wings are long and rather narrower than in the European P. palumbella, and the large, broad palpi, though of much the same form, are porrected instead of ascending; but in venation and the structure of the antenna it agrees with the European species, and Pempelia ovalis from New England, in which the wings are much shorter. Body and wings cinereous, - or granite-gray, the abdomen and legs being paler, and concolorous with the legs and hind wings, which are of the usual glistening hue of the genus. Fore wings of the same ash hue as the thorax, speckled with black scales. Two black dots at the base of the wing below the median vein. Beyond on the submedian vein is a longitudinal, blackish, incon- spicuous stripe edged on each side with dull ochreous. Above it is a dark point on the median and subcostal veins, with whitish scales sur- rounding the middle dot, but there are no raised scales on the wing. Just beyond the middle of the wing are two, prominent, squarish, black spots, one on the median the other on the subcostal vein. A distinct, white, submarginal line, parallel with the outer edge and bordered in- ternally with black scales, especially marked on the costa. The space between this line and the outer edge is filled in with deep, ochreous, lon- gitudinal bars, alternating with black streaks, of which the costal one is the widest and shortest. These bars do not quite reach the distinct, black line at the edge. Fringe ash, twice lineated with whitish. Beneath a pale, whitish, straight, submarginal line, edged within towards the costa with dark ash. Length of body @, 45, 2, 45 of an inch; fore wing @, °43, 2, -44 of aninch. California (Edwards). Easily recognized by the very distinct, yellow and black bars; the prom- inent, twin, squarish spots, and the distinct, white, once sinuate, whitish, submarginal line. Pempelhha leoninella, n. sp.—28 192. Antenne and palpi as in P. fenes-, trella, but the fore wings are more produced towards the apex, the outer edge being more oblique. Body and base of fore wings tawny, the thorax being ¢lay-yellow; palpi clear ash. Basal third of fore wings tawny yel- low, somewhat orange colored externally, outer edge of this colored portion directed regularly, obliquely outwards from the costa to the inner edge, with three, black, venular dots along this oblique border. In the ash space beyond is a distinct, dark, discal dot, and the veins are black. A broad, marginal, tawny yellow band, the sides even and par- allel; the costa, however, is cinereous to the apex. A marginal black line, and a fine dark line in the cinereous fringe near the base. Hind wings of the usual hue. Abdomen luteous. Beneath fore wings smoky, dusky towards the costa; a pale, costal streak, not forming a submar- ginal, pale line as in P. fenestrella. Legs dark ashen, whitish at ends of joints. Length of body @, °50, 9, -45 of an inch; of fore wing @, -46, 2, °45 of aninch. California (Edwards). 260 Catalogue of the Pyralide of California, etc. Differs from P. fenestrella in the more acute primaries, the tawny base of the wings and the conspicuous, marginal, broad, tawny band, and the want of the twin squarish spots in the middle of the wing. Nomophila noctuella (Schiff.) (Stenopteryx hybridalis Hiibn.) After com- paring four specimens from Oregon (collected by Mr. J. Holleman) and ten from California (coll. Edwards) with one from New York (Angus) and three from New England, and four from Europe, I can find no valid. differences. The largest suite, from California, vary in the same manner as in the European specimens. One form is dark with the markings very distinct, the other is paler, with the discal dot and reniform spot partially obsolete, and the lines indistinct, while the whole moth is somewhat tawny. The variation in size is much as in the European specimens. One specimen was collected by Mr. J. Holleman in Siskiyou Co., Cal. Scopula occidentalis, n. sp.—2g¢ 29. In this species the outer edge of the fore wings is much more oblique, and the costa much more rounded at the apex than in the European S. inquinatalis, otherwise structurally it is closely allied. Stone gray; head and palpi gray: orbits white; head and palpi white beneath. Fore wings uniform stone gray, crossed by two, distinct, wavy, dark lines; inner line shaded with whitish internally, with a large angle projecting outwards just below the median vein, and another inwards on the submedian. Discal and reniform spots very dis- tinct, black. Outer line finely scalloped, curved outwards from the costa to the fourth median venule, where the line forms a sinus, and angulated outwards on the submedian vein; the line broadly shaded externally with whitish. A marginal row of black dots. Fringe concolorous with the wing. Hind wings dusky, fringe pale; an obscure, short, dusky line beyond the middle. Beneath, much paler than above, dot and reniform line distinct, outer line faintly reproduced, as also the marginal dots. A short, faint line on hind wings. Abdomen dark above. Legs whitish. Length of body g, -44, 9, -40 of aninch; of fore wing @, -44, 2, -42 of an inch. California (Edwards and Behrens). The lines and spots are very distinct on the fore wings, and in some specimens the space between the two lines is slightly darker than the rest of the wing. Botys Californicalis, n. sp.—1 g. This species belongs to the Rhodaria group, having broad, triangular, acute palpi, and being of small size, with the hind tibize rather swollen. Body and wings light brick red, with a deep, ochreous tinge. Orbits white, becoming red towards the front, palpi grayish-red, white along the under edge; head beneath white. Fore wings ochreous red, a basal, fine, regularly curved, waved dark line; an outer, similar line, straight on the costa and inner edge, curved outwards and wavy between the subcostal vein and fourth median venule, there being four distinct scallops in this curved portion. Edge of wing broadly margined with dull, leaden, reddish-brown; fringe reddish-brown on basal half, much paler beyond. Hind wings marked much as prima- ries, being reddish, and bordered widely with dull, leaden, reddish- Cataloque of the Pyralide of California, etc. 261 brown; base of wing powdered with dark scales, and the outer, curved, dark line present, diffusely shaded within. Beneath, paler than above, a large, dark, discal patch; costal and outer margin of wing dull, leaden brown; hind wings with a conspicuous, single, definite line, not shaded within, outer edge bordered widely with dusky brown. Fringe as in pri- maries. Abdomen reddish, with whitish, conspicuous lines covering hinder edge. Length of body ?; of fore wing, ‘28 of aninch. California (Edwards). Botys unifascialis, n. sp.—2. Of an uniform, stone-gray color, with a dark olive greenish hue. Head and thorax rather darker than the fore wings. The only mark on the fore wings is a submarginal, broad, sinuous diffuse, pale band, which is curved outwards on the upper half and in- wards on the lower. Fringe concolorous with the wings. Hind wings paler than primaries, with a slightly marked, median, broad, diffuse band ; near edge of wing whitish; extreme edge gray. Fringe white. Beneath fore wings dusky with no markings, but paler on the inner, outer and costal edges. Hind wings cream white. Fore legs slightly grayish; hind legs white. Length of body, °55 of an ineh; of fore wing, ‘55 of an inch. Cali- fornia (Edwards). This species very closely resembles an eastern species,* but differs in the pale band on the hind wings, while both pairs are rather more acute on the apex. Botys profundalis, n. sp.—2g 32. This is a small form, with the apex of fore wings subacute, rectangular, the outer edge being less oblique than in any other of the species described, while the palpi are rather longer and larger. Orbits white on vertex and on each side of the an- tennz. Deep ochreous-brown, body white beneath; palpi light brown, white on the under side. Fore wings deep ochreous-brown; the inner line angulated outwards broadly on the median vein and inwards on the submedian. A large, round, discal dot and dumb-bell-shaped, reniform spot, these spots more conspicuous than usual. The outer line is dark *Botys subolivalis,n. sp. This species belongs to a distinct group, as far as I can judge by the figures, apparently including the European Botys alpinalis and its variety ablutalis figured by Herrich Schaeffer in his ‘‘Systematische Bearbeitung der Schmet- terlinge yon Europa,” etc. The fore wings are rather broad, subtriangular, costa straight, rounded towards the apex; outer edge not very oblique; hind wings broader than usual. It is of a peculiar stone gray, with a slight olive-green tinge. There are no markings on the fore wings, except a faint pale sinuate broad shade crossing the outer third of the wing; it is directed outwards on the costa. curved outwards in the middle of the wing, and is straight below the 4th median venule. Fringe slightly darker than the wing. Hind wings dark smoky; fringe whitish, smoky at base. Be- neath clear smoky ash on the fore wings, white on the hind wings, with a single broad diffuse, much curved, dark band in the middle, and slightly dusted with cinereous scales near the outer edge. Length of body -40 of an inch; of fore wing ‘50 of an inch. Brunswick, Maine, in grass uplands; Orono, Maine, July (Packard). It cannot be confounded with any other species of Botys I have yet seen. 262 Catalogue of the Pyralide of California, ete. filiform, oblique, with its general course parallel with the outer edge, but inwards making an elbow just below the costa, while just below the median vein, the line is deeply curved in, making a very deep sinus, with parallel sides, the bottom of the sinus being parallel with the inner edge of the reniform spot. A marginal row of conspicuous, black dots. Fringe ash color, with a dusky line at the base. Hind wings pale, the discal dot sinall, inconspicuous; the outer line with a small, deep sinus behind the middle of the wing, the line much curved in front of this sinus. A row of black dots along the edge. Beneath pale, with the lines and spots very distinctly reproduced, the fore wings not dusky as usual in some specimens. Legs whitish. Length of body @, 42, 9, :40-'45 of an inch; of fore wing @, *42, 9, 40-46 of an inch, California (Mdwards). This apparently common species may at once be known by the unus- ually deep sinus of the outer line. All the lines and spots are very dis- tinct, especially on the hind wings. One female, the best preserved of the lot, is bright florid ochreous, while the best preserved male is of a pale mouse color, and the fore wings are dusky beneath. Botys mustelinalis, vn. sp.—29. Body rather stout, with the fore wings ‘ather narrow, much produced towards the apex, the outer edge being a little more oblique than usual. Body and wings of a uniform, pale, cloudy, sable-brown. Orbits just in front of the antennem and upper side of the palpi whitish. Fore wings with an oblique, dusky line, extending from the costa outwards to the inner edge, being curved outwards a little in the median space, and inwards slightly on the submedian space. An obscure, dusky, large, round, diseal spot and large reniform spot. Outer dusky line finely scalloped, curved around gradually from the costa to the fourth median venule, where it is bent at right angles inwards, and the lower, wider, dusky portion begins half way between the end of the upper, scalloped division, and the origin of the fourth median venule; this portion is twice waved. Outer edge of wing a little darker than the middle and the costa is also darker. Hind wings slightly paler than pri- maries. A faint, discal dot, and an outer dusky shade, dislocated, or rather with a deep sinus below the middle of the wing. A marginal, fine, dark line. Fringe concolorous with the wing. Abdominal segments edged with whitish. Beneath, somewhat paler with the discal and reni- form spots faintly reproduced; the outer line appears as a finely, deeply scalloped line, the scallops filled in with a much paler tint; the border of the wing is finely dusted with fine, grayish scales; fringe with a slightly marked, fine, median, pale line. Hind wings with an acutely zigzag, outer line, and a short, dusky, diffuse line in the middle of the wing, not reaching the costa or hind edge. Body beneath and legs paler, almost whitish. Length of body, 50 of an inch; of fore wing, 50 of an inch. Cali- fornia (Wdwards). The distinguishing marks of this dull colored species is the rectangu- Catalogue of the Pyralide of California, etc. 263 larly bent, outer, dusky, scalloped line, forming a large, reéntering angle just under the reniform spot; the apex of the fore hee is also rather more produced than usual. Botys fodinalis Lederer—2 192. This is a species of the typical form of the genus, with the fore wings moderately broad, the apex subacute, the outer edge not very oblique. ead, thorax and fore wings pale sable- brown. Palpi entirely sable-brown; orbits in front of antenns white. Fore wings with a faint, dark, basal line, incurved on the subcostal space, bent outwards just behind the median vein, then following a straight course and ending on the inner third of the inner edge. A small, dark, discal dot, and small, rounded, reniform spot at a considerable distance from it. The outer, dark line is bent at right angles inwards, the portion below the fourth median vein is parallel with the inner line; the portion above is parallel to the outer edge of the wing, slightly sinuate in its course and angulated inwards on the costa. Hind wings pale, faded whitish, with a faint, ochreous tinge in the middle. A dark, conspicuous, discal dot; a single line curved in a semicircle in the middle of the wing ; edge of wing shaded broadly with blackish, fading out towards the inner edge, with a narrow, pale, interrupted line beneath the fringe and dark shade. Fringe concolorous with the wings. Abdomen, legs and body beneath pale whitish, ochreous. Beneath fore wings dusky, hind wings whitish, with the dots, outer lines and marginal shade reproduced. Fringe a littte paler than the wings, that on fore wings darker than on hind wings. Agrees with Lederer’s figure, Wiener Ent. Monats. vii. Pl. 8, fig. 9. Length of body @,°55 of an inch, 9 (abdomen broken off); of fore wing @, °55, 9, 48 of aninch. California (Edwards). This dull colored species differs from the others in the obscureness of its markings, and in the pale hind wings with the broad, dark border. One of the two males is nearly twice the size of the single female, but a large suite of specimens may show that the equality of the sexes is as usual. The male wants the outer, much curved line, present on the hind wings of the other sex. There is a very faint, reddish tinge on the fore wings of one of the males. Botys semirubralis, n. sp.—1¢@. A species of the normal form, with palpi of the usual form and length. The apex of the fore wings is rather blunt, but the hind wings are of the usual form. Body and basal half of fore wings dull, dark, sable-brown, including the palpi and legs. Fore wings dull sable-brown, immaculate to beyond the middle, except a small, round, brown, discal dot. Outer portion of the wing dull, brick red, with a little paler, diffuse, slight, submarginal shade. Fringe dull, reddish-brown. Hind wings dull, sable-brown, with a vinous tinge; fringe pale reddish wine color. Beneath, fore wings dusky in the middle portion, becoming reddish-brown on the costa, and pale, faded reddish on the outer edge of the wing. Hind wings pale, faded brick red on costal region; fringe of the same color, the inner region of the wing paler. 264 Catalogue of the Pyralide of California, etc. Length of body, -45 of an inch; of fore wing, 50 of an inch. Cali- fornia (Edwards). This species may readily be distinguished by the blunt apex and the dull brick red outer half of the fore wings, contrasting with the dull umber or sable-brown ground color. Botys perrubralis, n. sp.—2g 19. ? In both species the retractor muscle of the penis is attached Notr. In L. and F. W. Shells N. A., Part I, 120, we included H. germana in Steno- trema, but it has not the internal transverse tubercle characteristic of that subgenus: In the foregoing remarks we have shown that H. germana differs specifically from A. Columbiana, but consider that both species belong to Mesodon rather than the latter to Stenotrema. On Prophysaon, etc. 305 to the vas deferens, a short distance before the latter organ enters the penis, which it does at the apex of the penis sac. Macrocyclis Baudoni, Petit. We have already described the lingual membrane of this species. (See Am. Journ. Conch., VII, p. 175.) Recently we have received a Guadeloupe specimen (not adult), from Mr. Schramm. On extracting the lingual membrane we found attached to it a most delicate, transparent, colorless jaw, arched, with pointed ends, median projection to cutting edge and smooth anterior surface. This, added to the lingual dentition, places the species in Macrocyclis. Bulimulus multifasciatus, Lam. (JLiostracus.) Antigua. Governor Rawson. Jaw long, very low, slightly arcuate; ends attenuated, pointed; ex- tremely thin, transparent; divided by numerous delicate ribs into over thirty plates of the form common to Bulimulus, Cylindrella, ete., the upper median plates triangular. Lingual membrane broad. Teeth in numerous waving rows, of the type we have described and figured in Bulimulus laticinctus. (Ann. Lyc. Nat. Hist., N. Y., X, p. 81, pl. ii, fig. 1, 5.) The centrals are distinctly trifid. Bulimulus alternans, Beck. (Jiostracus.) Islands in the Bay of Panama. Mr. MeNiel. Jaw long, low, slightly arcuate, extremely thin and transparent; divided by numerous delicate ribs in about fifty-two plates of the type common in Bulimulus, Cylindrella, ete. Lingual membrane as in the preceding species. Helix pachygastra, Gray. (Dentellaria.) Guadeloupe. Mr. Schramm. Jaw stout, slightly arcuate, ends blunt; anterior surface with decided ribs, denticulating either margin, about seven, irregularly disposed; both ends free from ribs. Lingual membrane as usual in the subgenus; see above, p. 303 and plate xiv, figs. 7, 8, for those of Helix lychnuchus. 306 On Prophysaon, etc. Helix Josephine, Fér. (Dentellaria.) Guadeloupe. Mr. Schramm. Jaw stout, ribless; so strongly arched as to be quite horse-shoe shaped. Ends bluntly rounded. A decided median projection to cutting edge, marked with strong vertical stric. Lingual membrane as in preceding. Welix invalida, Adams. (Plewrodonta.) Jamaica. Mr. Henry Vendryes. Jaw not examined. Lingual membrane as in the preceding. The centrals and laterals quite short and stout. Punctum mimutissimaum, Lea. This species was described as Helix minutissima by Mr. Isaac Lea, in 1841. Its proper generic position was un- known, however, prior to 1864, when Professor Edward S. Morse, published figures of the jaw and lingual dentition (Journ. Portland Soc., I, p. 27, fig. 70, pl. viii, fig. 71). He thus described the jaw :— “