The early Cambrian is a non-feeding larva of a scalidophoran worm.

With its bag-like appearance, spiny ornament and single opening, is one of the most enigmatic animals of the early Cambrian Kuanchuanpu Formation ( 535 Ma) and has been at the heart of debates concerning the origin of two major animal lineages: the deuterostomes and the ecdysozoans. Although Ecdysozoa is now the most plausible option, key aspects of its palaeobiology have remained elusive. I suggest here that was the possible larval stage of one of the numerous scalidophoran worms that co-existed with it in the Kuanchuanpu biota, especially those with bilateral pairs of broad-based sclerites such as . This new interpretation is mainly based on the development of extant priapulid worms (Scalidophora). It would imply that is a non-feeding larva and that its enigmatic single aperture with a pleated structure is not a mouth but more likely the opening through which the juvenile exited. Thus, the strange anatomy of could be explained in a simple way without involving complex evolutionary processes (e.g. simplification, miniaturization, loss of anus, etc.). Instead of being a relatively basal member of the total group Ecdysozoa, would find a more likely position among the total group Scalidophora.