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Paranevadites gabbi
Taxonomy
Trachyceras (Anolcites) gabbi was named by Smith (1914). It is a 3D body fossil. Its type locality is Divide between Troy Canyon and South Fork of American Canyon (occidentalis), which is in an Illyrian marine limestone in Nevada.
It was recombined as Nevadites gabbi by Silberling and Nichols (1982); it was recombined as Paranevadites gabbi by Tozer (1994).
It was recombined as Nevadites gabbi by Silberling and Nichols (1982); it was recombined as Paranevadites gabbi by Tozer (1994).
Synonymy list
Year | Name and author |
---|---|
1914 | Trachyceras (Anolcites) gabbi Smith p. 132 figs. Pl 9, figs 3-17; pl 11, figs 4-7; pl 85, figs 11,12; pl 86, figs 1-11 |
1982 | Nevadites gabbi Silberling and Nichols p. 38 figs. Pl 24, figs 8-11 |
1994 | Paranevadites gabbi Tozer p. 124 |
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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.
†Paranevadites gabbi Smith 1914
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Diagnosis
No diagnoses are available