By Phillips J.
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Extra info for A monograph of British belemnitidae: Jurassic
The sicles marked by il deep ftrt'Lol, tlhich cliviclestheur into tlo cqualltarts: place of thc siphunclc unkriol-n. I). \iliartitus of Blaiuville is an cratttple. :. eolus,opposite to the ventral canal of ihe guard ; ahvays compressed; the opening of the cavit,vnotched on the sides' B. -siphuncle in the middle line of the uentral aspect,' ah,vayscylindric or depressed; opening of the cavity terminating circularly or oblicluely. of continual Before proceeding further it is desilable to fir the meaning of a fen' terrns are use in describing tlre guard and phragmocone.
Ioeality. Bristollfuseurn). In the samebeds at Wotton-under-ndge, FrocestuHill, CamDown, Bridport (Phllryts). [earChe]tenham (Buckman). Obseruations. The specimens figuredare,without doubt,to be referredto the species first separatedfrom the ordinary breu'formisby Oppel. I have seenforeign eramples. The figures given by Quenstedtshow somedegreeof lateralcompression, but I cannot doubt the identity of his specieswith ours from Gloucestershireand Somersetshire. D'Orbigny's figures ('Terr. ,' pl. ix, figs.
N) Surlmit submucronate(\roltz, pl. ii, fiS. 4). (c) Surnnit mucronate,axis very near the ventral side (Voltn, pI. ii, fig. 3). Obseruations. The speciescalled breui/ornres by Yoltz, if allowed to include all the varietieswhich have been referred to it, must be quoted from ]Iiddle Lias, Upper Lias, and Inferior Oolite. Yoltz supposesthat BelentnitesLreuis,vAr. iii, fig. 2), may be identical rvith B. breui/ornis, var. c, Yoltz; and as far as the figure of Blainville is evidence,his opinion seemedjust.
A monograph of British belemnitidae: Jurassic by Phillips J.