~2h. senticosus Dittmar, as figured by Mojsisovics, and the early Karnian species Sirenties loczyi Mojsisovics and Sirenites clavigo Mojsisovics are examples. Sirenites meginae McLearn (Plate V, figures 1 to 4) This species has, at various times, been referred to the genera Steinmannites Mojsisnvics, Meginoceras McLearn, Paratrachyceras Arthaber, and Sirenites Mojsisovics. It is certainly not a Steinmannites, a Norian genus, which has eo eatet merres ee to the ventral sulcus and a different suture line, a suture aie ane resembling Norian Clionites. ane of the name Meginoceras is deferred for the present, and Sirenites is used in the broad sense. This species is not a Sirenites in the strict sense, but it shows some characters of both a Sirenites and a Paratrachyceras. In the nunber of ventral ‘tubercles relative to the number of lateral ribs it is intermediate betweon Paratrachyoered and Buren test In Paratrachyceras the ribs do not divide near their ventral ends, so that there is no increase in number of the ventral tubercles. Genus Dawsonites Boehm It has been noted how a new style of ventral ernament appeared in the early Karnian in the shells included inns genus Sirenites Mojsisovics. At the same time another new style of ventral ornament avpeared; it was a fission of each tubercle’ producing paired tubercles in each row bordering the ventral sulcus. This style of ornament, alone, without further complexity had a short range, did not survive the early Karnisn, and is a diagnostis feature of the genus Trachyceras Laube, the genus indicative of the basal cape faunal een As in Sirenites the sides of the whorl are ornamented with curved oat and rows of tubercles or spines. The suture line is typically ammonitic. Boehm (1903) has given the name Dawsonites to ammonoids.with the shell ornament of. Trachyceras but with a much simpler and ceratitic suture-line. This genus has been reliably recorded only from the Nathorstites fauna of northeastern British-Columbila and Bear Island. Johnston has recorded Brachyceras-with a comparatively-simple suture line from New Pass, Nevada, but not so simple as that of Paffaonites.