Prod traces (Selenichnites) from the Middle Cambrian of Morocco, with hypotheses on the ethology of the tracemaker(s)

A single bedding surface was identified along the roadside close to an important road junction at Tansikht and north of Zagora in southern Morocco. This bedding plane has concomitant interference ripples and distinct horseshoe shaped concave epirelief ichnofossils dispersed across the surface. The sandstone bed belongs to the upper middle Cambrian Azlag Formation. The Azlag Formation occurs above the Bailiella Formation, with its distinctive trilobite fauna, in this section. The traces provide evidence of the ethology of an organism that was inhabiting the shallow waters during this time. Body fossils are rarely preserved in a clastic setting. The traces, assigned to the ichnogenus Selenichnites, and the new ichnospecies, Selenichnites tesiltus, are proposed, identified, diagnosed, described and illustrated herein. Possible tracemakers and behaviors are considered.