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Coopericus semisulcatus
Taxonomy
Linoproductus semisulcatus was named by Cooper and Grant (1975). Its type specimen is USNM 149490a, a valve (Ventral valve), and it is not a trace fossil. Its type locality is USNM706x, Wolf Camp Hills, Glass Mountains, which is in an Asselian marine limestone in the Neal Ranch Formation of Texas.
It was recombined as Coopericus semisulcatus by Lazarev (2004).
It was recombined as Coopericus semisulcatus by Lazarev (2004).
Synonymy list
Year | Name and author |
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1975 | Linoproductus semisulcatus Cooper and Grant p. 1148 figs. Pl 431, figs 7-12 |
2004 | Coopericus semisulcatus Lazarev p. 161 |
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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.
†Coopericus semisulcatus Cooper and Grant 1975
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Diagnosis
No diagnoses are available
Measurements
part | N | mean | |||||
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shell height | 1 | 30.7 |
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Source: subo = suborder, c = class, p = phylum, uc = unranked clade | |||||
References: Aberhan et al. 2004, Williams et al. 2000, Nesnidal et al. 2013 |
Age range: base of the Virgilian to the top of the Artinskian or 303.70000 to 279.30000 Ma
Collections (11 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Virgilian | USA (New Mexico) | Linoproductus semisulcatus (156676 156699 156715) | |
Asselian | USA (Texas) | Linoproductus semisulcatus (43474 43475 43500 type locality: 43556 75938) | |
Sakmarian | USA (Texas) | Linoproductus semisulcatus (102612 106156) | |
Artinskian | USA (Texas) | Linoproductus semisulcatus (106044) |