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Macrocnemus obristi
Taxonomy
Macrocnemus obristi was named by Fraser and Furrer (2013). Its type specimen is PIMUZ A/III 1467, a partial skeleton, and it is a compression fossil. Its type locality is Ducanfurgga, Davos, which is in a Fassanian marine shale in the Prosanto Formation of Switzerland.
Synonymy list
| Year | Name and author |
|---|---|
| 2013 | Macrocnemus obristi Fraser and Furrer |
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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.
†Macrocnemus obristi Fraser and Furrer 2013
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: subc = subclass, c = class, subp = subphylum | |||||
| References: Hendy et al. 2009, Carroll 1988, Kiessling 2004 | |||||
Age range: Fassanian or 241.46400 to 239.48000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Fassanian | Switzerland (Grisons) | Macrocnemus obristi (172169) | |
| Fassanian | Switzerland (Graubunden) | Macrocnemus obristi (type locality: 172168) |