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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Martinia hungarica
Taxonomy
Martinia hungarica was named by Schréter (1963). It is a 3D body fossil. Its type locality is Nagyvisnyó Railway Cut 5 (Legányi coll), which is in a Wuchiapingian offshore lime mudstone in the Nagyvisnyo Formation of Hungary.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1963 | Martinia hungarica Schréter p. 138 figs. Pl 8, figs 1-6 |
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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 hungarica 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 (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Wuchiapingian | Hungary | Martinia hungarica (type locality: 131451 236977) |