Canalichnus tenuis Santos et Mayoral, 2006

ID16439
Fossil groupBioerosional trace fossils
TaxonCanalichnus tenuis
AuthorSantos et Mayoral, 2006
ReferenceSantos & Mayoral, 2006
Parent taxonCanalichnus
Is validYes
FADZanclean
LADZanclean
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Synonymy

YearSynonymAuthorPagesFigsReference
2006Canalichnus tenuis isp. n.Santos & Mayoral7222:5–8; text-fig. 2D-ESantos & Mayoral, 2006

Type specimens

TypeNumberRepositoryType localityLoc.Type horizonStrat.RemarksReferenceID
holotypeVE/p/03/5Huelva University, SpainVelerin pared outcropPlioceneSantos & Mayoral, 2006

Descriptions and remarks

Diagnosis. Superficial furrows of more or less straight path, either occurring in isolation or in dense populations. In both cases the furrows are distinct, although very shallow. Ichnospecimens in dense groups branch in Y-shaped patterns; isolated examples branch at acute, almost orthogonal angles (Pl. 2, figs 7–8).

Description. C. tenuis is most easily identified by the calcareous remains of the tubular shell of the producers, which are often preserved. When shell remains are absent, the path of the trace is defined by one or several shallow furrows that smooth out the microtopography of the substrate, erasing any surface ornamentation (Pl. 2, figs 7–8). Furrow width ranges from 26 to 40µm and their depth scarcely reaches 2µm. Uneroded marginal areas are parallel to each side of the furrow; the width of these areas is usually greater than the furrow itself, ranging from 20 to 66µm (Text-fig. 2D–E; Pl. 2, figs 5–6). Where ichnospecimen density is relatively high (Pl. 2, fig. 5), the furrows branch at acute angles between 40 and 45 degrees and are organised into more or less parallel series. When density is much lower, furrows branch off at almost orthogonal angles (Pl. 2, figs 7–8).


Occurrences


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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 |