By Phillips J.
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Additional info for A monograph of British belemnitidae: Jurassic
Bxample-3. canal'iculatusEubsection Inf. -Hastati : lateral furrows distinct. )r ,\ection1/I-Notoceli, (Example-B. ft'astatus. D' Orb. With a dorsal groove, and furrowed on each side. (Example-B' dilcttatus. ) D'Orb. Belernnitella, The guard has a straight fissure on the ventral side of its alveolarborder; its is never snrfaceexhibits distinct vascularimpressions. The phragmocone that it had a preserved,but casts of the alveolusshowthat it waschambered, of the the fissure guard,and singledorsalridge, a ventral processpassinginto an apicalnucleus.
Greatestlengthobserved(edgeof aperturevery thin), 3| inchesi greatestbreadth,less than 1 inch. Proportions. The diameterat the apex of the phragmoconebeing 100, the ventral radiusis 42, the dorsal58, the axis120. PsnecuocoNn. Very oblique,arched,with a circularcrosssection. Conothecaconilurlerous; angle m. 28o. centrically undulated on the ventral face; concamerations tracedto twice Septaldiametereight or evennine timesthe depth. Axis of phragmocone the length of the axis of the guard. Fifty septain three quartersof an inch from the apexof the phragmocone.
With lateralcanals. Each of the divisions thus indicnted is subdivided into groups of alliecl species. M. Duval-Jouve proposecla classificationlimited to tlie Belemnitesof the I'[eocomian a strata, which ma,v be convenient for referencc; though at the present time hardly in found single species of the groups he mentions and clesclibes so calefully has been England. 1. -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.