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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Cyclonema intermedium
Taxonomy
Gyronema intermedium was named by Bradley (1930). It is a 3D body fossil. Its type locality is Goetz quarry, Glen Park, which is in a Trentonian carbonate limestone in the Kimmswick limestone Formation of Missouri.
It was recombined as Cyclonema intermedium by Wagner (2023).
It was recombined as Cyclonema intermedium by Wagner (2023).
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.
†Cyclonema intermedium Bradley 1930
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: g = genus, f = family, superf = superfamily, c = class | |||||
| References: Knight et al. 1960, Wagner 2023, Batten 1984, Kiessling 2004 | |||||
Age range: Trentonian or 457.30000 to 449.60000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Shermanian | USA (Illinois) | Gyronema intermedium (154952) | |
| Trentonian | USA (Missouri) | Gyronema intermedium (89024) |