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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Taxonomy
Anomia taylorensis was named by Mansfield (1940). It is a 3D body fossil. Its type locality is Taylors Mill Creek (Richards), which is in a Rupelian deep subtidal ramp limestone in the Chickasawhay Formation of Mississippi.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1940 | Anomia taylorensis Mansfield p. 184 |
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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.
†Anomia taylorensis Mansfield 1940
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: g = genus, f = family, o = order, c = class | |||||
| References: Aberhan et al. 2004, Kiessling 2004, Sanchez Roig 1926 | |||||
Age range: base of the Rupelian to the top of the Hemphillian or 33.90000 to 4.90000 Ma
Collections (6 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Rupelian | USA (Alabama) | Anomia taylorensis (205613) | |
| Rupelian | USA (Mississippi) | Anomia taylorensis (155961 type locality: 169205 205621) | |
| Chattian | USA (Mississippi) | Anomia taylorensis (205805) | |
| Hemphillian | USA (Alabama) | Anomia taylorensis (89608) |