Undichna cf. britannica Higgs, 1988
publication ID |
https://doi.org/ 10.5252/geodiversitas2022v44a31 |
publication LSID |
urn:lsid:zoobank.org:pub:008AF7BE-28B6-4FB5-A007-45BAB4337BAC |
DOI |
https://doi.org/10.5281/zenodo.7342533 |
persistent identifier |
https://treatment.plazi.org/id/302A87B5-FFFC-0D00-FC72-FB9FFCA212B9 |
treatment provided by |
Jonas |
scientific name |
Undichna cf. britannica Higgs, 1988 |
status |
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Undichna cf. britannica Higgs, 1988
( Fig. 7 View FIG A-G)
MATERIAL EXAMINED. — M486_ 2022.1.8, slab bearing numerous trails preserved as convex hyporeliefs.
DESCRIPTION
The slab bears many wavy, horizontal, intermittent, sharp and up to 1.0 mm wide ridges ( Fig. 7A, B, D View FIG ). Some of these ridges form trails consisting of two intertwined and out-of-phase waves ( Fig. 7 View FIG E-G). The longest trail is 145 mm long. Waves show a wavelength of up to 40 mm and an amplitude of up to 5 mm. In some trails, one of the waves shows a low amplitude, whereas the other shows a greatest amplitude ( Fig.7F View FIG ). Some trails show outer marks that are parallel to central waves ( Fig. 7E, G View FIG ).
REMARKS
The presence of wavy, intertwined, horizontal, and intermittent, grooves/ridges is characteristic of several Undichna Anderson,1976 ichnospecies (e.g. Undichna quina from the Permian deposits of the Falkland Island, Trewin2000; Undichna britannica from the Carboniferous deposits of England, Higgs 1988). Since ridges are out-of-phase in specimens from Le Bousquet it should be tempting to see similarities with U. britannica (see Higgs 1988 and Minter & Braddy 2006). In contrast, amongst U. quina ridges are in phase (see Trewin 2000). On trails showing strong variation of amplitude between the two waves ( Fig.7F View FIG ), the wave with the lowest amplitude was probably made by the anal fin whereas the wave with a greatest amplitude was probably made by the caudal fin.Outer marks were probably made by pelvic fins.
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