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Callinectes alabamensis
Taxonomy
Callinectes alabamensis was named by Rathbun (1935). It is a 3D body fossil. Its type locality is Perdue Hill [Suwannee Fm], which is in an Oligocene marine marl in the Byram Marl Formation of Alabama.
Synonymy list
| Year | Name and author |
|---|---|
| 1935 | Callinectes alabamensis Rathbun p. 98 figs. Plate 21, figures 4-6 |
| 2010 | Callinectes alabamensis Schweitzer et al. p. 111 |
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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.
†Callinectes alabamensis Rathbun 1935
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: superf = superfamily, o = order, c = class | |||||
| References: Turnsek 1997, Fearon and Clapham 2023, Aberhan 1992 | |||||
Age range: Early/Lower Oligocene or 33.90000 to 28.40000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Early/Lower Oligocene | USA (Alabama) | Callinectes alabamensis (type locality: 143392) |