Characichnos, Whyte & Romano, 2001
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.7342425 |
persistent identifier |
https://treatment.plazi.org/id/302A87B5-FFFC-0D03-FEBD-FBD8FDB813BE |
treatment provided by |
Jonas |
scientific name |
Characichnos |
status |
|
Characichnos isp.
( Fig. 7 View FIG A-C)
MATERIAL EXAMINED. — M486_ 2022.1.8, slab with numerous tracks preserved as convex hyporeliefs.
DESCRIPTION
The slab M486_ 2022.1.8 bears numerous swimming tracks of tetrapods ( Fig. 7 View FIG A-C). They are small, up to 14 mm long and up to 9 mm wide. Some of them are aligned showing a trackway-like pattern ( Fig. 7C View FIG ). Morphology of individual tracks vary a lot. They show two to four parallel, elongated, thin and straight to strongly curved furrows. Some of the tracks seem to bear claw traces. Imprints of sole are absent.
REMARKS
Characichnos shows a wide stratigraphic range (Carboniferous to Cretaceous) and was reported from several Permian tracksites throughout the world (e.g. Argentina, Melchor & Sarjeant 2004; Spain, Mujal et al. 2016; United States, Lucas & Spielmann 2009; Lerner & Lucas 2015; Morocco, Moreau et al. 2020). This ichnogenus is for the first time reported in the Permian deposits from the Rodez Basin. These tracks can be interpreted as pes and manus imprints of small tetrapods half-floating and swimming in shallow water. Here, only the tips of the digits touched the substrate. On the slab M486_ 2022.1.8, these swimming tracks co-occur with abundant fish trails ascribed to Undichna cf. britannica Higgs, 1988 ( Fig. 7 View FIG D-G).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.