Prioniodus sp. A
publication ID |
https://doi.org/ 10.3853/j.0067-1975.55.2003.1383 |
persistent identifier |
https://treatment.plazi.org/id/37439A20-CB08-FF1E-FC36-FE14FBF5FA62 |
treatment provided by |
Felipe |
scientific name |
Prioniodus sp. A |
status |
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Fig. 21M–Q View Fig
Material. Four specimens (3 Pa, 1 Pb) from the Tabita Formation at Mount Arrowsmith.
Description. Both Pa and Pb elements have a robust, erect cusp with sharp anterior and posterior margins; Pb element with a more laterally compressed blade-like cusp, and short posterior and outer lateral processes, with four denticles on the former and a single denticle on the latter; the anterior process long, inner laterally curved, bearing more than ten denticles ( Fig. 21M,N View Fig ). Cusp of Pa element more or less triangular in cross section, with a sharp mid-costa along the outer lateral face, which extends basally into a long denticulate outer lateral process ( Fig. 21P,Q View Fig ); long denticulate posterior process bearing closely spaced denticles which are erect and laterally compressed; outer lateral process normal to the posterior process ( Fig. 21 O View Fig ), bearing over ten closely spaced denticles which are anteroposteriorly compressed, with tips slightly curved posteriorly; neither anticusp nor denticles developed at the anterobasal corner.
Remarks. The Pa element is well defined and is distinguished from those of other species of the genus by its long denticulate posterior and outer lateral processes. The Pb element of this species is characterized by a prominent cusp, and long denticulate anterior process. It shows some resemblance to the P element of Prioniodus sp. A McTavish, 1973 from the Emanuel Formation of the Canning Basin ( McTavish, 1973, pl. 2, fig. 4), but has an even longer anterior process with prominent denticles, and a much shorter outer lateral process.
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