liik
Augoichnus dituberculatus Arendt, 2012
Tüüpeksemplari andmed
holotüüp: Moscow, Paleontological Institute (PIN) ; 1786/88574; Ryabinovka; Artinski lade , Sarginian Horizon, Divja Formation (basal part)
Reference:
Arendt, Yu. A. 2012. Traces of Augoichnus dituberculatus gen. et sp. nov. on Hypermorphocrinus magnospinosus from the Lower Permian of Cisuralia. pp. 886-893. DOI:10.1134/S0031030112080047
Taksoni kirjeldused
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.
Sünonüümika
2012 Augoichnus dituberculatus Arendt, sp. nov — Arendt , lk. 888, joon. Pl. 4:1.9; Pl. 5:1-4
Valik taksonit käsitlevast teaduskirjandusest
Arendt, Yu. A. 2012. Traces of Augoichnus dituberculatus gen. et sp. nov. on Hypermorphocrinus magnospinosus from the Lower Permian of Cisuralia. Paleontological Journal 46, 8, 886-893. DOI:10.1134/S0031030112080047
Klassifikatsioon
| organismirühm | Biota |
| ihnorühm | Ichnofossils |
| Bioerosional trace fossils | |
| sugukond | Centrichnidae |
| perekond | Augoichnus |
| liik | dituberculatus |
Levik kirjandusandmetel
- Arendt, 2012 Ryabinovka Artinski lade