Teredolites Leymerie, 1842
Srivastava et al., 2024
Emended Diagnosis: (After Kelly and Bromley1984, p. 804.) ‘Clavate borings in woodground orhardground substrates, acutely turbinate, evenlytapered from aperture to base of main chamber; neckregion not separated from main chamber; cross-sectionsat all levels more or less circular; elongate to short.’
Wisshak et al., 2019a
Macroboring; substrate xylic; tracemaker invertebrate
Donovan, 2018
Diagnosis. (Slightly modified after Kelly and Bromley 1984, p. 804.) ‘‘Clavate borings in woody substrates, acutely turbinate, evenly tapered from aperture to base of main chamber; neck region not separated from main chamber; cross-sections at all levels more or less circular; short.’’
Buatois et al., 2017
Category of architectural design: 2.66. Clavate-shaped borings.
Knaust, 2012a
Unbranched, branched, clavate.
Taylor & Wilson, 2003
Remark: Tubular, clavate borings in wood, sometimes with calcareous linings. Some contain the shells of the trace-making bivalve.
Buatois et al., 2017
Teredolites Leymerie, 1842, also emended by Kelly and Bromley (1984), is a clavate boring in xylic substrates. These borings, attributed most often to bivalves, are cylindrical and can be short orvery long. Teredolites commonly has a calcareous lining.
organismirühm | Biota |
ihnorühm | Ichnofossils |
Bioerosional trace fossils | |
sugukond | Gastrochaenolitidae |
perekond | Apectoichnus |
Clavichnus | |
Gastrochaenolites | |
Palaeosabella | |
Phrixichnus | |
Teredolites | |
liik | clavatus |
solitarius |