Hedinaspis sp.
publication ID |
https://doi.org/ 10.11646/zootaxa.5422.1.1 |
publication LSID |
lsid:zoobank.org:pub:AE955C5E-803E-44CB-A3B2-9C2616D9F185 |
persistent identifier |
https://treatment.plazi.org/id/926387DB-FF97-CA0B-FF38-81E6FE131700 |
treatment provided by |
Plazi |
scientific name |
Hedinaspis sp. |
status |
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( Plate 7.19 View PLATE 7 )
Discussion. A single, very fragmentary pygidium was recovered in collection 5/22/08C in the Lotagnostus rushtoni fauna from the Windfall Formation, Ninemile Canyon, Nevada. The distal half to two-thirds of six pleurae with very broad (exsag.) pleural furrows are bounded in front and behind by narrower, strongly convex bands of roughly equal width. Posterior bands of the anteriormost pleurae extend for very short distance posterolaterally as short, blunt terminal spines. The distinctive form of the pleurae allows for certain assignment to Hedinaspis but the specimen is too fragmentary for more precise identification. Uncertainty as to which part(s) of the skeleton the specimen represents is made all the more difficult by the typically obscure boundary between the thorax and pygidium noted in previous studies of Hedinaspis (e.g. Troedsson, 1937; Lu & Lin, 1989).
Ceratopygid indeterminate
( Plate 16 View PLATE 16 , figs 13, 17)
Discussion. Two relatively large specimens in collection D7129-CO from the Hot Creek section of the Hales Limestone represent a non-spinose ceratopygid species. The flat, semi-elliptical pygidium with a tapering axis that extends nearly to the posterior margin, and long frontal area on the cranidium resemble those of some species of Pseudoyuepingia (e.g. P. elongata Lu & Lin, 1989 ). However, the cranidium is too fragmentary for confident assignment to genus.
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