Caulostrepsis cretacea (Voigt, 1971)

ID15827
Fossil groupBioerosional trace fossils
TaxonCaulostrepsis cretacea
Author(Voigt, 1971)
ReferenceVoigt, 1971
Parent taxonCaulostrepsis
Is validYes
FADOxfordian
LADRecent
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Synonymy

YearSynonymAuthorPagesFigsReference
2024Caulostrepsis cretacea (Voight, 1971)Knaust & Schnick136HKnaust & Schnick, 2024
2023Caulostrepsis cretacea (Voight, 1971)Gaaloul, Uchman, Ben Ali, Janiszewska, Stolarski, Kołodziej & Riahi8A, 12CGaaloul et al., 2023
2005Caulostrepsis cretacea Voight, 1971Wisshak, Gektidis, Freiwald & Lundälv111Wisshak et al., 2005a
2001Caulostrepsis cretacea (Voight, 1971)Fodor152:2Fodor, 2001
1998Caulostrepsis cretacea VoightBertling & Insalaco155Bertling & Insalaco, 1998
1996Caulostrepsis cretacea (Voight, 1971)Hofmann522:1Hofmann, 1996
1994Caulostrepsis cretacea (Voight, 1971)Fürsich, Palmer & Goodyear1616:8Fürsich et al., 1994
1991Caulostrepsis cretacea (Voight, 1971)Radtke524:2Radtke, 1991
1987Caulostrepsis cretacea (Voight, 1971)Bromley & D'Alessandro390Bromley & D'Alessandro, 1987
1983Caulostrepsis cretacea (Voight, 1971)Bromley & D'Alessandro29121:1,3; 22Bromley & D'Alessandro, 1983
1971Dodecaceria cretacea n. sp.Voigt15015:12; 16:1-9Voigt, 1971

Type specimens

TypeNumberRepositoryType localityLoc.Type horizonStrat.RemarksReferenceID
holotypeNr. 1380Geolog.-Pal. Institut HamburgAnkerpoort-Curfs quarry, southern LimburgMaastrichtianVoigt, 1971

Descriptions and remarks

Diagnosis.—Galleries bent in a long, narrow U-form with the inward-facing walls of the limbs fused by complete removal; the original position of the median wall is sometimes indicated by a very shallow axial depression along the structure. Vane absent. Transverse section always flattened-elliptical but showing gradual decrease in width toward the aperture. Shape of aperture flattened-oval (cited from Bromley and D’Alessandro 1983)

Remarks.—Bromley and D’Alessandro (1983) observed broader specimens, which are at least 2 mm wide and never show interpenetration. However, the characteristic distal widening is diagnostic of this ichnospecies. Originally, this ichnospecies was described by Voigt (1971) as Dodecaceria cretacea. Later, it was transferred to Trypanites by Bromley (1972) and finally to Caulostrepsis by Bromley and D’Alessandro (1983). Voigt (1971) and Bromley and D’Alessandro (1983) regarded it as having been produced by the cirratulid polychaete Dodecacería concharum Örsted, 1843, but Gibson (2016) who examined the material studied by the aforementioned author and compared it with recent borings of this polychaete, questioned this view and suggested that Caulostrepsis cretacea is similar to the borings of Polydora.


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 |