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Anthracomartus radvanicensis
Taxonomy
Cryptomartus radvanicensis was named by Oplustil (1985). Its type specimen is CGH Me 81, a carapace, and it is an impression. Its type locality is Katerina mine, Radvanice, which is in a Stephanian B lacustrine siliciclastic in the Odolov Formation of the Czech Republic.
It was recombined as Anthracomartus radvanicensis by Dunlop et al. (2013).
It was recombined as Anthracomartus radvanicensis by Dunlop et al. (2013).
Synonymy list
| Year | Name and author |
|---|---|
| 1985 | Cryptomartus radvanicensis Oplustil p. 40 figs. Pl 2, fig 1; text-fig 4 |
| 2008 | Cryptomartus radvanicensis Štamberg and Zajíc p. 63 fig. 48 |
| 2013 | Anthracomartus radvanicensis Dunlop et al. p. 122 |
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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.
†Anthracomartus radvanicensis Oplustil 1985
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: c = class | |||||
| Reference: Bush and Bambach 2015 | |||||
Age range: Stephanian B or 301.50000 to 301.00000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Stephanian B | Czech Republic | Cryptomartus radvanicensis (type locality: 155303) |