Flagrichnus baiulus Wisshak et Porter, 2006

ID16415
Fossil groupBioerosional trace fossils
TaxonFlagrichnus baiulus
AuthorWisshak et Porter, 2006
ReferenceWisshak & Porter, 2006
Parent taxonFlagrichnus
Is validYes
FADOligocene
LADRecent
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Synonymy

YearSynonymAuthorPagesFigsReference
2022Flagrichnus baiulus Wisshak & Porter, 2006Meyer et al.5aMeyer et al., 2022
2022Flagrichnus baiulus Wisshak & Porter, 2006Martinell & Domènech2422BMartinell & Domènech, 2022
2022Flagrichnus baiulus Wisshak & Porter, 2006Wisshak et al.122Wisshak et al., 2022a
2006Flagrichnus baiulus isp. novWisshak & Porter1393, 4Wisshak & Porter, 2006

Type specimens

TypeNumberRepositoryType localityLoc.Type horizonStrat.RemarksReferenceID
holotypeMfNB: MB.W 192Museum of Natural History, Humboldt University, BerlinLardos Hill, RhodosPleistoceneRhodes FormationWisshak & Porter, 2006

Descriptions and remarks

Diagnosis: Deeply penetrating microboring with a single to multiple, basal, sack-shaped cavity oriented parallel to the substrate surface. Near the base of the cavity, a long, thin, filamentous tube extends straight into the substrate, ramifies distally and tapers to slender filaments.

Description: The traces are commonly found collapsed to the cast surface and partially etched samples are required to reveal their deeply penetrating nature (Fig. 3A–B). The trace is found to occur clustered in large numbers of up to several hundred individuals (Fig. 3H). At the base of the mature trace a double to multiple sack-shaped cavity up to 80μ minsizeis developed parallel to the substrate surface and is occasionally connected to the latter by numerous thin filaments (Fig. 3D). From near the base of the cavity, a thin (1–2μm) filamentous gallery extends straight and deep (up to several 100μm) into the substrate and may repeatedly ramify and in some cases build up a dense mesh with the distal parts of neighboring individuals (Fig.3B).Injuvenilespecimens,onlythethindeeplypenetrating filament is developed associated with a basal swelling a few micrometers in diameter (Fig. 3E). From this basal swelling, a single sack emerges during ontogeny, later bifurcating into double or multiple sack-shaped cavities, and in some cases even exhibiting a rosette-like appearance (Fig. 3G).


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 |