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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Cuniculiformis aristotelis
Taxonomy
Cuniculiformis aristotelis was named by De Wever (1982). Its type locality is Gümüslü, sample 1662D, which is in a Pliensbachian basinal (carbonate) limestone in the Sögütlü dere Formation of Türkiye.
Synonymy list
| Year | Name and author |
|---|---|
| 1982 | Cuniculiformis aristotelis De Wever |
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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.
†Cuniculiformis aristotelis De Wever 1982
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: p = phylum | |||||
| Reference: Kiessling 1999 | |||||
Age range: base of the Pliensbachian to the top of the Early/Lower Toarcian or 192.90000 to 182.90000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Pliensbachian | Türkiye (Antalya) | Cuniculiformis aristotelis (type locality: 81267) | |
| Early/Lower Toarcian | Japan | Cuniculiformis aristotelis (124830) |