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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Cambrotubulus corniformis
Taxonomy
Cambrotubulus corniformis was named by Elicki (1994). Its type locality is Gorlitz Synclinorium carbonates, Zweta Formation, which is in an Atdabanian/Lenian peritidal limestone in the Zwetau Formation of Germany.
Synonymy list
| Year | Name and author |
|---|---|
| 1994 | Cambrotubulus corniformis Elicki pp. 83 - 84 figs. f. 6/2-4 |
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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.
†Cambrotubulus corniformis Elicki 1994
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family | |||||
| Reference: Aberhan et al. 2004 | |||||
Age range: base of the Atdabanian to the top of the Lenian or 521.00000 to 508.20000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Atdabanian - Lenian | Germany (Saxony) | Cambrotubulus corniformis (type locality: 6899) |