Sulcichnus Martinell et Domènech, 2009
| ID | 13348 |
|---|---|
| Fossil group | Bioerosional trace fossils |
| Taxon | Sulcichnus |
| Author | Martinell et Domènech, 2009 |
| Reference | Martinell & Domènech, 2009a |
| Parent taxon | Renichnidae |
| FAD | Tortonian |
| LAD | Recent |
Includes:
| Species | Reference |
|---|---|
| Sulcichnus helicoidalis | Martinell & Domènech, 2009a |
| Sulcichnus maeandriformis | Martinell & Domènech, 2009a |
| Sulcichnus sigillum | Martinell & Domènech, 2009a |
Description(s)
Martinell & Domènech, 2009a:
Long grooves, sometimes branched, running along the surface substrate sinuously or in a contorted fashion. Grooves never run in parallel, and loose or tight loops may occur.
Knaust, 2012a:
Unbranched, branched, groove.
Buatois et al., 2017:
Category of architectural design: 2.78. Elongate or branched attachment bioerosion traces.
Wisshak et al., 2019a:
Macroboring; substrate calcareous; tracemaker invertebrate.
Gaaloul et al., 2023:
Diagnosis: Shallow groove parallel to the columella and bending 90° close to the calyx, to form a deeper, ring-shaped groove (cited from Martinell and Domènech 2009).
Description: Shallow grooves (1 mm maximum in depth) that run more or less in parallel to the axis of the columella from close to the base of the corallite. They turn a sharp 90 to the left when reaching a point a few millimetres from the edge of the calyx, where they deepen (to some 2 mm) and run almost the whole of the perimeter of the corallite, thus taking on the appearance of a branding iron.