CLAss V . GEPHALOPODA 617 



Order 2. AMMONOIDEA Zittel.i 



Shells similar io ihose of the Nautiloidea in some primitive Paleozoic groups, hut 

 these give rise to others with mwe highly ornamenied shells, the apertures of which 

 have ventral rostra instead of hyponomic sinuses. Sutures, as a rule, have ventral 

 lobes in the later stages of ontogeny ; the inßedions become more numerous than in 

 Nautiloids even in Paleozoic genera, and their outlines during the Mesozoic are 

 cxtremely complex. Siphuncle invariahly small, and (except in the Clymeniidae) 

 situated near the venfer. Funnels short, retrosiphonate in primitive forms, hut 

 becoming sometimes pirosiphonate during the Paleozoic, and as a rule, prosiphonate 

 during the Mesozoic. 



The ontogeny begins with a calcareous protoconch, the apical stage of the 

 conch being an open neck built in continuation of the permanent aperture of 

 the protoconch. The first septum is concave as in Nautiloids, and sutures are 

 straight or have more or less of a saddle on the venter. Young stages of 

 Mesozoic shells recapitulate the primitive adult characters of Paleozoic forms. 

 The aperture was closed when the animal was retracted by a single horny plate 

 (anaptychus) or a pair of calcareous plates (aptychis), probably secreted by 

 muscular lobes homologous with the hood in Nautilus. 



Shell Characters. — There are apparently no characters, not even the presence 

 of a calcareous protoconch, which can be relied upon to separate Bactrites from 

 the orthoceraconic Nautiloids. Nevertheless, the position of the siphuncle and 

 its peculiar funnels are features which seem to place this form with true 

 Paleozoic Ammonoids. There is but one series of straight shells among 

 Ammonoids, and these are obviously not the same as orthoceracones, but are 

 more properly called bactriticones (Fig. 1169). Similarly, the loosely coiled 

 Mimoceras shells (Fig. 1170) are not gyroceracones, but only their morphic 

 equivalents in a different genetic stock ; hence the term mimoceracone should 

 be substituted for gyroceracone. In the same sense the closely coiled sym- 

 metrica! Shells, comparable in external aspect and intimate structure with 

 nautilicones, should be described among Ammonoids as ammoniticones. The 

 term torticone, however, can be conveniently applied to both groups, since it 

 does not connote any special structures, but is a general name for all asym- 

 metrical spirals. 



Ammoniticones in some Paleozoic forms are mimoceracones during 

 nepionic stages, and consequently in later stages a Perforation is present 

 passing through the umbilicus as in Nautiloids. However, in most Paleozoic 

 and all later ammoniticones, the coiling is so close even at the beginning 



^ Besides the works cited the followhig nmy be coiisulted : — Buckman, S. S., Divisions of so- 

 caUed Jurassic Time. Quar. Jonrn. Geol. Soc, 1898, vol. Uw—Clarke, J. M., The Naples Fauna. 

 16th Ann. Rep. N.Y. State Geologist, 1898.— CVicyfc, G. C, Muscular Attachment of the Animal 

 to its Shell in Animonoidea. Trans. Linn. Soc, 1898, ser. 2, vol. vü.—Haug, £., Etudes sur les 

 Goniatites. Mem. Soc. Gt'ol. Frunce, Paleont., 1898, vol. \n.—Levi, ('., Fossili degli strati a 

 Terebratula aspasia. Boll. Soc. Geol. Italia, 1895, vol. xv.—Parona, C. F., and Bonarelli, O., 

 Faune du Callovien inferieur (Chanazien) de Savoie. Mem. Acad. Savoie, 1897, vol. vi.— Semenoff, B., 

 Anwendung der statistischen Methode zum Studium der Vertheilung der Ammoniten. Ann. Geol. 

 Mineral. Russie, 1897, vol. il— Smith, J. F., Development of Lytocerasand Pliylloceras. Proc. Calif. 

 Acad. Sei., 1898, vol. \.~-Choffat, P., Les Ammonees du Bellasien, des Conches a Neolobites Vibra- 

 yeanus, du Turonien et du Senonien. Faune cret. du Portugal, 1898, ser. 2, vol. n.—Jackson, lt. T., 

 Localised Stages of Development in Plauts and Animals. Mem. Boston Soc. Nat. Hist., 1899, vol. v. 

 — Novak, J., Untersuchungen über die Cephalopoden der oberen Kreide in Polen. II. Die Scaphiten. 

 Bull. Acad. Sei. Cracovie, ser. B, 1911. 



