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Cambroclavus bicornis
Taxonomy
Sugaites bicornis was named by Qian and Xiao (1984). Its type specimen is Xinjiang Institute of Geology 10583, a shell, and it is a 3D body fossil. Its type locality is Aksu-Wushi, which is in a Meishucunian marine limestone in the Yurtus Formation of China.
It was recombined as Cambroclavus bicornis by Conway Morris et al. (1997).
It was recombined as Cambroclavus bicornis by Conway Morris et al. (1997).
Sister species lacking formal opinion data
Synonyms
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Synonymy list
Year | Name and author |
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1984 | Sugaites hastatus Qian and Xiao |
1984 | Sugaites saccatus Qian and Xiao |
1984 | Sugaites sicyojdeus Qian and Xiao |
1984 | Sugaites soleiformis Qian and Xiao |
1984 | Sugaites bicornis Qian and Xiao p. 79 figs. pl. 1, figs. 9, 12-13 |
1997 | Cambroclavus bicornis Conway Morris et al. p. 172 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Cambroclavus bicornis Qian and Xiao 1984
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Invalid names: Sugaites hastatus Qian and Xiao 1984 [synonym], Sugaites saccatus Qian and Xiao 1984 [synonym], Sugaites sicyojdeus Qian and Xiao 1984 [synonym], Sugaites soleiformis Qian and Xiao 1984 [synonym]
Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: o = order, p = phylum | |||||
Reference: Kiessling 2004 |
Age range: base of the Meishucunian to the top of the Atdabanian or 530.70000 to 516.00000 Ma
Collections (5 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Meishucunian | China (Xinjiang) | Sugaites bicornis, Sugaites soleiformis, Sugaites sicyojdeus, Sugaites hastatus, Sugaites saccatus (type locality: 107481) | |
Atdabanian | China (Xinjiang) | Cambroclavus bicornis (6815 7824 7825 7827) |