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Thetisolala undulata
Taxonomy
Thetis undulata 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.
It was recombined as Thetisolala undulata by De Wever and O'Dogherty (2007).
It was recombined as Thetisolala undulata by De Wever and O'Dogherty (2007).
Synonymy list
| Year | Name and author |
|---|---|
| 1982 | Thetis undulata De Wever |
| 2007 | Thetisolala undulata De Wever and O'Dogherty |
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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.
†Thetisolala undulata 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 Sinemurian to the top of the Pliensbachian or 199.50000 to 184.20000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Sinemurian | New Zealand | Thetis undulata (53751) | |
| Pliensbachian | Türkiye (Antalya) | Thetis undulata (type locality: 81267) |