Augoichnus dituberculatus Arendt, 2012
| ID | 17023 |
|---|---|
| Fossil group | Bioerosional trace fossils |
| Taxon | Augoichnus dituberculatus |
| Author | Arendt, 2012 |
| Reference | Arendt, 2012 |
| Parent taxon | Augoichnus |
| FAD | Artinskian |
| LAD | Artinskian |
Type specimens
| Type | No | Type locality | Type horizon | Remarks | Reference | ||||
|---|---|---|---|---|---|---|---|---|---|
| holotype | Moscow, Paleontological Institute (PIN) | 1786/88574 | Ryabinovka | Artinskian | Sarginian Horizon, Divja Formation (basal part) | Arendt, 2012 |
Description(s)
Arendt, 2012:
Diagnosis. Traces of varying, usually shallow depth, on skeletons of Hypermorphocrinus and occa sionally other crinoids. Ovoid in outline (less com monly oval and round), bilaterally symmetrical, rimmed by marginal groove or two grooves, with a rel atively deeper subcentral depression and as a rule, paired tubercles between it and the posterior margin. Sometime skeleton was perforated.