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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Martinia rakuszi
Taxonomy
Martinia rakuszi was named by Schréter (1963). It is a 3D body fossil. Its type locality is Nagyvisnyó, railway cutting 4, which is in a Wuchiapingian carbonate limestone in the Nagyvisnyo Formation of Hungary.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1963 | Martinia rakuszi Schréter p. 143 figs. Pl 8, fig 7 |
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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.
†Martinia rakuszi Schréter 1963
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class, p = phylum, uc = unranked clade | |||||
| References: Aberhan et al. 2004, Nesnidal et al. 2013 | |||||
Age range: Wuchiapingian or 259.90000 to 254.17000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Wuchiapingian | Hungary | Martinia rakuszi (type locality: 236977) |