Protopanderodus gradatus Serpagli, 1974
publication ID |
https://doi.org/ 10.3853/j.0067-1975.61.2009.1520 |
persistent identifier |
https://treatment.plazi.org/id/03EFCB66-6E43-553F-FF1C-F9D9FBD7F84C |
treatment provided by |
Felipe |
scientific name |
Protopanderodus gradatus Serpagli, 1974 |
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Protopanderodus gradatus Serpagli, 1974
Fig. 9A–P View Fig
Protopanderodus gradatus Serpagli, 1974: 75 , pl. 15, figs 5a–8b, pl. 26, figs 11–15, pl. 30, figs 1a–b; text-fig. 17; Zhen et al., 2004: 56–57, pl. 5, figs 1–10 (cum syn.); Zhen & Percival, 2006: fig. 9A–C; Zhen et al., in press a: fig. 8A–Q.
Material. 126 specimens from two samples ( Table 1).
Remarks. Protopanderodus gradatus is common in one (WCB705/243) of the samples studied from the Emanuel Formation. This material is identical with the types described from the San Juan Formation (Early Ordovician) of Argentine Precordillera ( Serpagli, 1974), and those recently documented from the Honghuayuan Formation of Guizhou, South China (Zhen et al., in press a, fig. 8A–Q). An additional element ( Fig. 9J–P View Fig ) bearing a more compressed cusp and a less extended base with a rounded basal margin has also been recognized in the Emanuel material. It also shows rather prominent striation in the area immediately anterior to the lateral costa, and a weakly developed chevron-shaped pattern of striae adjacent to the anterior margin ( Fig. 9K, O View Fig ). As these distinctive characters are not observed in the other elements of P. gradatus , it is tentatively assigned herein to the M position of P. gradatus . Some specimens bear rounded holes of about 3–4.5 µm in diameter, presumably representing the boring structure made by an unknown organism ( Fig. 9O, P View Fig ).
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Protopanderodus gradatus Serpagli, 1974
Zhen, Yong Yi & Nicoll, Robert S. 2009 |
Protopanderodus gradatus
Zhen, Y 2004: 56 |
Serpagli, E 1974: 75 |