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Diodora penderensis
Taxonomy
Fissuridea penderensis was named by Kellum (1926) [DISTRIBUTION: Late Eocene; North Carolina.]. It is not a trace fossil. Its type locality is USGS 779, 7794 - Lanes Ferry [Castle Hayne Limestone], which is in a Bartonian deep subtidal ramp wackestone/grainstone in the Castle Hayne Formation of North Carolina.
It was recombined as Diodora penderensis by Hendy et al. (2008).
It was recombined as Diodora penderensis by Hendy et al. (2008).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1926 | Fissuridea penderensis Kellum p. 25 figs. pl. 3, fig. 9 |
| 2008 | Diodora penderensis Hendy et al. |
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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.
†Diodora penderensis Kellum 1926
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: g = genus, superf = superfamily, c = class | |||||
| References: Abbott and Dance 1986, Hendy et al. 2009, Kiessling 2004 | |||||