[1] Nenoxites is a repichnia trace of soft-bodied bilaterians, similar to a modern day shell-less gastropod.

The traces are hypothesized to have been created via locomotive peristalsis, a wave-like constriction and relaxation of muscle resulting in the sinouous pattern and irregular depressions of the fossil.

[2][1] Nenoxites ichnofossils are thought to be the earliest instance of precambrian bioturbation, a behavior wherein an organism disturbs substrate to find food.

The common interpretation of the morphology of Nenoxites is comparable to traces of contemporary gastropods, and is thought to have been made by the earliest tripoblastic eumetazoans, though there is no current agreed upon taxonomy or biology of Nenoxites.

[1][3] Instances of Nenoxites have been recorded in the Khatyspyt Formation in arctic Siberia, as well as in Russia and China.