Augoichnus dituberculatus Arendt, 2012

ID17023
Fossil groupBioerosional trace fossils
TaxonAugoichnus dituberculatus
AuthorArendt, 2012
ReferenceArendt, 2012
Parent taxonAugoichnus
Is validYes
FADArtinskian
LADArtinskian
Edit in SARV Workbench

Synonymy

YearSynonymAuthorPagesFigsReference
2012Augoichnus dituberculatus Arendt, sp. novArendt8884:1.9; 5:1-4Arendt, 2012

Type specimens

TypeNumberRepositoryType localityLoc.Type horizonStrat.RemarksReferenceID
holotype1786/88574Moscow, Paleontological Institute (PIN)RyabinovkaArtinskianSarginian Horizon, Divja Formation (basal part)Arendt, 2012

Descriptions and remarks

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.


Occurrences


Browse Categories of Architectural Design (CADs):

Borings with elliptical to sub-rectangular cross sections | Branched tubular borings | Camerate boxwork borings | Camerate network borings | Circular holes and pit-shaped borings | Clavate-shaped borings | Cylindrical vertical to oblique borings | Dendritic and rosetted borings | Elongate or branched attachment bioerosion traces | Fracture-shaped bioerosion traces | Globular to spherical borings | Groove bioerosion traces | Multiple attachment bioerosion traces | Non-camerate boxwork borings | Non-camerate network borings | Pouch borings | Radial borings | Single circular to tear-shaped attachment bioerosion traces | Spiral borings | Trackways and scratch imprints | U-shaped borings | Winding borings |