Drepanoistodus sp.
publication ID |
https://doi.org/ 10.3853/j.0067-1975.55.2003.1383 |
persistent identifier |
https://treatment.plazi.org/id/37439A20-CB32-FF24-FE86-F9DCFB5AFED4 |
treatment provided by |
Felipe |
scientific name |
Drepanoistodus sp. |
status |
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Fig. 14L View Fig
Material. Four specimens from limestone nodules within shales of the upper Yandaminta Quartzite , and four specimens from the Tabita Formation, at Mount Arrowsmith; an additional specimen from unnamed dolomitic limestone unit at Koonenberry Gap .
Remarks. Specimens of a large suberect element, here identified as Drepanoistodus sp. ( Fig. 14L View Fig ), are asymmetrical with the basal cavity inflated inner-laterally and with an undulose basal margin at the inner side. Löfgren (1978) noticed some variations among Swedish specimens assigned to the P element of D. basiovalis . Some forms showing a flaring anterobasal corner ( Löfgren, 1978, pl. 1, fig. 13), are comparable with the elements here referred to D. sp. This element might occupy the Pa position to complete a seximembrate apparatus for D. basiovalis .
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