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Antilloseris cantabrigiensis
Taxonomy
Turbinoseris cantabrigiensis was named by Vaughan (1899). Its type locality is Cambridge Station [Cambridge Beds], which is in a Lutetian shallow subtidal limestone/marl in the Cambridge Formation of Jamaica.
It was recombined as Antilloseris cantabrigiensis by Vaughan (1919) and López-Pérez (2005).
It was recombined as Antilloseris cantabrigiensis by Vaughan (1919) and López-Pérez (2005).
Synonymy list
| Year | Name and author |
|---|---|
| 1899 | Turbinoseris cantabrigiensis Vaughan |
| 1905 | Turbinoseris cantabrigiensis Vaughan |
| 1919 | Antilloseris cantabrigiensis Vaughan |
| 2005 | Antilloseris cantabrigiensis López-Pérez p. 81 |
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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.
†Antilloseris cantabrigiensis Vaughan 1899
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class | |||||
| Reference: Kiessling 2004 | |||||
Age range: base of the Lutetian to the top of the Late/Upper Eocene or 47.80000 to 33.90000 Ma
Collections (5 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Lutetian | Mexico (Chiapas) | Antilloseris cantabrigiensis (85735) | |
| Lutetian | Jamaica | Antilloseris cantabrigiensis (77038) | |
| Lutetian | Jamaica (St. James Parish) | Turbinoseris cantabrigiensis (type locality: 88336) | |
| Lutetian - Bartonian | North Atlantic (Saint Barthélemy) | Antilloseris cantabrigiensis (71118) | |
| Late/Upper Eocene | Mexico (Chiapas) | Antilloseris cantabrigiensis (85732) |