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L BAC He I OA IV OHI Fe OA Ie Lara BRO Soa 359 JOG pattie ® Fy I ES ESS G3 ~ AD CUgIY VEIT PAN RIM OA oe. ; KO A BART A He Ld a . ae ee > 42 OW;A ft | hob es ae, ae cosy eS catty mtb Shblaay'f' hl ede We tah Ae << Beer 7 a4 « Jr ra = ~~ i 24 7% Do a Raed Ga 2 ‘4 Bhpent : fet care) FOR” Leng, BVT EE ORO: A alot Ae i iyi: ci os y BOS vey! { bach eT TONG vet ere tes arlinds of oar ee Ward Bb agp ery ayaa sae ~ ’ <4 ; tii 3 Pees LR OM {YS ERE a NCTA Vee ae) 8 cetam Graiaa ‘2 sae teat a ners ‘ ab Hie Boitry oie ees ’ > rfl ee Lt > " VL T\7 APPENDIX ae: 8 Sb¥ — | aoe MANUAL OF MOLLUSCA, TO THE OF 8. P. WOODWARD, A.LS., CONTAINING SUCH RECENT AND FOSSIL SHELLS AS ARE NOT MENTIONED IN THE SECOND EDITION OF THAT WORK. J f P RARE Ol LUbore. An : , ‘ Di x 7, YY} oO} vi , , ; ‘ : iY 183 1 Sater) Kalyoh ere { 2 géctional Liorhy. By RALPH TATE, ALS: BGs: EA THSONIAN APR 29 1988 LIBRARIES LONDON: VEBRBTUE & CO., 26,.1IVY LANE NEW YORK: VIRTUE & YORSTON. 1868. J MAA AAA A ADDS A TEAS es Rey . ie ey AI NM a a op = "O ee = thy © os ae ag es ee eS i 4 y RAIAZ ENS a TITRE PATTI ARES CLASS I.—CEPHALOPODA. ORDER J.—DIBRANCHIATA. FamIty III.—TEUTHIDA. PHYLLOTEUTHIS, Meek and Hayden. Type, P. subovatus. Cretaceous. Nebraska. Pen corneous, thin, suboyate, slightly concave below, and conyex above. From behind the mid- dle it narrows towards the front, the outline of the lateral margins being convex, while the posteriorend is more or less obtusely angular. Apparently related to Beloteuthis and Teudopsis. (See p. 168.) FamiIty LY.—BELEMNITIDZ.* The Shell of Belemnites consists ~ fundamentally of :— 1. A hollow cone, the phragmocone, Fig. 1, p, with a thin shelly wall, termed the conotheca, c, and which is divided by transverse septa, concave above and convex below, into cham- bers or loculi; the septa are perforated nearthe ventral margin bya siphunecle. 2. A guard or rostrum, g, more or less extensively enveloping the apical part of the phragmocone. ‘* The phragmocone is not a chambered body made to fit into a conical hollow previously formed in the rostrum, as some have conjectured, but both rostrum and cone grew together; the former was formed on the exterior of a secretive surface, and the latter on the interior of another secretive sur- face.” (Phillips. ) The rostrum is composed of calca- Fig. 1. reous matter arranged in fibres per- pendicularly to the planes of the laminew of growth. Pro- * See p. 173. B2 3 Ventral aspect. Dorsal aspect. MANUAL OF THE MOLLUSCA. fessor Owen describes the fibres, in specimens from Christian Malford, as of a trihedral prismatic form, and zoooth of an inch in diameter. These fibres are disposed concentrically around an axis, a, the so-called apical line, which extends from the extremity of the phragmocone to that of the rostrum. Indica- tions of a thin capsule or formative membrane appear in some Belemnites investing the guard; in those of the Oxford clay it is represented by a granular incrustation; in some lassic species it appears in delicate plaits, like ridges or furrows; in some specimens of Belemnitella mucronata from the upper chalk of Antrim, it is in the form of a very thin nacreous layer. 3. A pro-ostracum, or anterior shell, which is a dorsal exten- sion of the conotheca beyond the end where the guard disappears. The surface of the conotheca is marked by lines of growth, and, according to Voltz, it may be described in four principal regions radiating from the apex: one dorsal, Fig. 2, a, with Fig. 3. Fig. 4. loop lines of growth advancing forward; two lateral, b, separated from the dorsal by a continuous straight or nearly straight line, and covered with very obliquely arched striz in a hyperbolic form, in part nearly parallel to the dorso-lateral boundary line, and in part reflexed, so as to form lines in retiring curves across the ventral portion nearly parallel to the edges of the septa. 4 CEPHALOPODA. There were at least three kinds of pro-ostracum in the family Belemnitide. A. In many Belemnites the extension of the conotheca seems to run out in one simple broad plate, Fig. 3, as in B. hastatus from Solenhofen. B. In Belemnites Puzosianus, D’Orbigny, the pro-ostracum is very thin, and apparently horny or imperfectly calcified in the dorsal region, supported laterally by two long, narrow, parallel, calcareous plates, Fig. 4, as in B. Puzosianus from the Oxford clay. Professor Huxley considers this difference between the pro-ostraca of generic importance. C. The third kind of pro-ostracum is exhibited by Orthocera elongata, De la Beche, the type of the genus Xiphoteuthis, Huxley ; it is calcareous, and is composed of concentric lamellz, each of which consists of fibres disposed perpendicularly to the plane of the lamella; the phragmocone is very long and narrow, and the guard cylindroidal. Professor Huxley suspects that a thoroughly well-preserved specimen of Belemnoteuthis will some day demonstrate the exist- ence of a fourth kind of pro-ostracum among the Belemnitide. The genera in the family are :—1, Belemnites ; 2, Belemnitella ; 3, Xiphoteuthis ; 4, Belemnoteuthis ; 5, Plesioteuthis ; 6, Celeno ; 7, Beloptera ; 8, Belemnosis; 9, Conoteuthis; and ? Helicerus. ‘‘The A anthoteuthes of Munster, so far as they are known only by hooks and impressions of soft parts, may have been either Belemnites, or Belemnoteuthis, or Plesioteuthes, or may have belonged to the genus Celeno.” (Huxley.) The genus Belopeltis, Voltz, was founded on the pro-ostraca of Belemnites, species of which were unknown. The genus Actinocamax, Miller, was founded on the guard of Belemnites and Belemnitella, the upper parts of which had decayed, and thus presented no alveolar cavity. ORDER JJ.—TETRABRANCHIATA. Famity I.—NAUvTILIDE (including Faminy II.—ORrTHOCERATIDA). DIVISION a.—AIR-CHAMBERS CONFINED TO ONE PART OF THE SHELL. ASCOCERAS, Barrande, 1846.* Etymology, askos, » leathern bottle, and ceras. * At p. 185 Mr. Woodward refers to M. Barrande’s second volume of the ‘* Cephalo- pods of Bohemia.” The Ascoras, Glossoceras, and Aphragmites are here described. 7) MANUAL OF THE MOLLUSCA. Type, A. Bohemicum, Barr., Fig. 5. Shell flask-shaped, smooth, transversely or longitudinally striated, or ornamented with annular folds, or plicated. The terminal cham- ber (r) occupying the space above the air- chambers (s), and extending down one side of nearly the whole length of the shell in the form of a wide and deep cavity, which is embraced by the decurrent edges of the in- complete septa (four or five in number). This cavity also communicates at its base with a small siphuncle which traverses the minute apical air-chambers. Aperture of shell simple. The wide ventral cavity of Ascoceras is of the same nature as the large lateral siphuncle of Cameroceras. Fig. 5. Distribution, 16 species. Lower—Upper Diagram of Ascoceras Q; = ° 7 ( after Barrande). ice Bohemia, Norway, England, Ca nuda. GLOSSOCERAS, Barrande, 1865. Etymology, glossa, a tongue, and ceras. Type, G. gracile, Barrande. Upper Silurian. Bohemia. Shell similar to that of Ascoceras, but the dorsal margin of the aperture is extended in the form of a ligulate projection, sub- triangularly rounded at the end, and recurved towards the inte- rior of the shell. This process gives rise to a distinct lobe on each side of the opening, which is analogous to that which exists in Hercocerus, Ophidioceras, and in certain species of Phragmoceras and Gom- phoceras. Distribution, 2 species. Middle and Upper Silurian. Anti- costi; Bohemia. APHRAGMITES, Barrande, 1865. Etymology, a, without phragmos, a partition; and the usual termination. Type, Ascoceras Buchii, Barrande. Shell, similar to that of Ascoceras, but the air-chambers are jleciduous. , Distribution, 2 species. Upper Silurian. Bohemia. a CEPHALOPODA. DIvIsIon }.—AIR-CHAMBERS OCCUPYING THE WHOLE CAVITY OF THE SHELL. PILOCERAS, Salter, 1859. Etymology, pilos, a cap, and ceras, a horn. Type, P. invaginatum, Salter, Fig. 6. Shell, broad, conical, sub-cylindrical, or com- pressed, and slightly curved. Siphuncle and septa combined as a series of conical concave septa, which fit into each other sheathwise. Distribution, 3 species. Lower Silurian. Scot- land. Canada. Fig. 6. Diagram ol £tiocerus ORTHOCERAS.* (after Salter). Sub-genera :— 1. GonrocERAS, Hall, 1847. Etymology, gonios, an angle. Type, G. anceps. Lower Silurian. United States. Shell, having the general form and structure of Orthoceras, flattened with extremely salient angles; septa sinuous; section of shell, an extended ellipse with projecting angles; siphuncle ventral. 2. ENDOCERAS, Hall, see W. M., u. p. 192. 3. TRETOCERAS, Salter, 1858 (Diploceras, Salter, 1856). Etymology, tretos, pierced. Type, Orthoceras bisiphonatum, Sowerby. Lower Silurian. Wales. Shell elongated ; septa pierced by a sub-central beaded siphuncle, and also by a deep lateral cavity continuous with the terminal chamber, and passing down side by side with the siphuncle—the cavity affecting at least seven of the upper- most septa, if not the whole. CYRTOCERAS.f Sub-genera :— 1. OnocERAS, see W. M., ii. 193. ‘‘ The shells of this genus and Cyrtoceras pass gradually into each other, but Onoceras may be retained for those species which are much inflated in the ante- rior half or two-thirds of the shell length” (Billings); and ‘‘ which have a more or less strangulated aperture” (Barrande), * See p. 190. + See p. 194. vi ~ MANUAL OF THE MOLLUSCA. 2. CYRTOCERINA,* Billings, 1865. Type, C. typica, Billings. Shell having the general characters of Cyrtoceras, but differs in the short, thick form, and in the large siphuncle on the dorsal side. Distribution, 2 species. Silurian. Canada. 3. STREPTOCERAS, Billings, 1865. Etymology, streptos, curved, and ceras. Shell having the form of Onoceras, but with a trilobed aperture like Phragmoceras. Distribution, 2 species. Middle Silurian. Canada. LirvirEs, Breynius.+ Type, L. lituus, Hisinger. Shell discoidal, whorls (2—5) close or separate; last chamber produced in a straight, or nearly straight line, sometimes slightly curved, in a direction contrary to that of the spire; lateral margins of the aperture extended and curved towards the interior of the shell; the aperture contracted thus presents two distinct orifices, the smaller corresponding to the convex or ventral side, the larger to the concave or dorsal side of the shell. I. lituus is the only species in which the aperture has been observed. 28 species from the Middle and Upper ? Silurian rocks of Europe and North America, belong here or to allied genera. Sub-genus :—OPHIDIOCERAS, Barrande, 1867. Synonym, Ophioceras, Barrande, 1865. Etymology, ophiodes, shaped like a serpent, and ceras. Type, O. Nakholmensis, Kjerulf (Zituites). Shell with the produced portion very short or wanting. The shells of the Bohemian species are keeled on the convex side. Distribution, 7 species. Middle Silurian; Norway (1). Upper Silurian, Bohemia (6). LITuUNcULUS, Barrande, 1867. Shell asin Lituites, but with a simple aperture. No species have been yet observed. Sub-genus :—DIScocERAS, Barrande, 1867. Hiymology, diskos, a quoit, and ceras. Type, D. antiquissimus, Eichwald (Lituites). 5 * See p. 194. t See p. 189. CEPHALOPODA. Shell with the produced portion very short or wanting. This sub-genus bears the same relation to Litwunculus (the existence of which is supposed) that Ophidioceras does to Lituites. Distribution, 3 species. Middle Silurian. Russia, Germany, Norway. HERCOCERAS, Barrande, 1867. Etymology, erkos, a wall, and ceras. T'ype, H. mirum, Bar. Middle Silurian, Bohemia. Shell usually involute, as in Nautilus, rarely with separated whorls as in Gyroceras, or with a spire as in T'rochoceras. Body- chamber with a diaphragm perpendicular to the axis of the shell, the concayity of which is opposed to that of the last septum. This disposition throws the aperture on the convex side of the shell, which is deeply excavated. Siphuncle dorsal, cylindrical, inflated between the chambers, separated from the shell. Nautilus subtuberculatus, Sandberger, from the Devonian of Nassau, may belong to this genus. BATHMOCERAS, Barrande, 1867. Etymology, in allusion to the imbricated arrangement of the partitions. Type, B. complexum, Barr. (Orthoceras). Shell haying the general appearance of Orthoceras. Part of the body-chamber occupied by a series of imbricating plates, which decrease in horizontal extension from below upwards. Siphuncle composed of a series of superimposed funnel-shaped tubes, the narrow end directed towards the aperture of the shell. Distribution, 2 species. Middle Silurian, Bohemia. AULACOCERAS, Hauer, 1860. Etymology, aulax, a furrow, and ceras. Type, A. sulcatum, Hauer, Fig. 7. Shell straight, like Orthoceras ; corrugated, with two deep lateral furrows; siphon simple, very small, marginal and dorsal, situated between the longitudinal sulci. The test increases rapidly in thickness towards the apex of the shell. The genus is a transition form between Fig. 7. Transverse sec- the Nautilide and the Belemnitide. aisonhy: Adtaconedil eile Distribution, 4 species. Upper Trias, catum. Austria. B3 9 MANUAL OF THE MOLLUSCA. [FamILy GoNIATIDA. Barrande.] Shell involute or straight; septa concave in their median section ; sutures usually with angular lobes ; septai tubes coni- cal, more or less prolonged, but always directed backwards. Siphuncle cylindrical, of small diameter, always marginal ; siphonal investment not persistent; conyexo-ventral margin of the aperture sloped, lines of growth and ornamentation of the shell with a corresponding sinuosity. The genera enumerated in this family are Goniatites, Clymenia, and Bactrites. Dr. Woodward includes the Goniatites and the Bactrites (pp. 196, 197) with the Ammonitide; and the Cly- menia with the Nautilidee (p. 190). Famity JJI].—AMMONITIDA. Shell various ; septa convex in their median section ; sutures always lobed, ramified, or denticulated ; septal tube cylindrical and always directed forwards. Siphuncle cylindroid of small diameter, always marginal; siphonal investment more or less solid and persistent. Convexo-ventral ? margin of the aperture more or less prolonged, which determines a similar convexity in the lines of growth and ornamentation of the test; there are rare specific exceptions. DIvIsion I.—SUTURES LOBED OR DENTICULATED AT THE BASE. 1. RHABDOCERAS (see p. 196). 2. Bacunina, D’Orbigny, 1850. Example, B. Rouyana, D’Orb. Neocomian, France. Shell like Baculites, but its lobes and saddles are not foliated, there being between these forms a similar distinction to that between Ceratites and Ammonites. B. acuarius, Schlotheim, is from the Oxfordian strata of Gammelshausen in Wurtemberg. 3. COCHLOCERAS, Hauer, 1860. Etymology, cochlos, a snail-shell, and ceras. Type, O. Fischeri, Hauer, Fig. 8. Shell resembling that of Turrilites, with the sutural lobes simple, as in Rhabdoceras and Clydonites. 10 CEPHALOPODA. Distribution, 8 species. Upper Triassic strata of Hallstadt, Austria. Fig. 8. Shell and sutural lobes of Cochloceras Fischeri. 4, CHORISTOCERAS, Hauer, 1865. Type, ©. Marshu, Hauer. Shell somewhat similar in form to Crioceras, with the lobular ornamentation characteristic of Ceratites. Distribution, 4 species. Upper Trias, Austria. 5. CLYDONITES, Hauer, 1860. +8 —ar_ Tad ay wy