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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Stelidioseris bellensis
Taxonomy
Astrocoenia bellensis was named by Wells (1933). It is not extant. Its type locality is Santa Fe railroad quarry, Belton, which is in an Albian carbonate limestone in the Comanche Peak Limestone Formation of Texas.
It was recombined as Actinastrea bellensis by Löser (2008); it was recombined as Stelidioseris bellensis by Löser (2012).
It was recombined as Actinastrea bellensis by Löser (2008); it was recombined as Stelidioseris bellensis by Löser (2012).
Synonymy list
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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.
†Stelidioseris bellensis Wells 1933
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, o = order, c = class | |||||
| Reference: Kiessling 2004 | |||||
Age range: base of the Late/Upper Valanginian to the top of the Middle Albian or 140.20000 to 105.30000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Valanginian - Early/Lower Aptian | Tanzania | Actinastrea bellensis (85376) | |
| Middle Albian | USA (Texas) | Astrocoenia bellensis (type locality: 123329) |