Apart from previously reported Small Shelly Fossils （SSFs）, a macroscopic fossil assemblage, comprising abundant algae, cone-shaped tubular fossil forms, and probable impressions of a megascopic metazoan, comes from the Lower Cambrian Yanjiahe Formation in the Yangtze Gorges area of western Hubei Province, south China. The visible fossils are preserved in thinlaminated siltstone or muddy siltstone intercalated between 8-15 ram-thick carbonate deposits, probably representing sedimentary settings of a constrained local depression in the shallow water carbonate platform during the Early Cambrian Meishucunian Stage. The macroscopic fossil association provides significant fossil evidence about the evolution of life from the late Precambrian to the ＇Cambrian explosion＇ interval.
The rare fossil Miraluolishania described by Liu et al. from the Lower Cambrian Chengjiang Lagersttte in 2004 is regarded as an arthropod sphinx because it bears mosaic features of both lobopods and arthropods. The discovery of this rare transitional form offers direct fossil evidence for exploring the relationship between lobopods and arthropods. However, some scientists consider Miraluolishania to be a junior synonym of Luolishania because the former superficially resembles the latter in general appearance. Considering the significant differences between the two taxa, a thorough comparative study of Miraluolishania and Luolishania leads to the conclusion that there are definitely two different genera. Nevertheless, the "Luolishania" of the Haikou area is indeed "Miraluolishania", whereas Luol-ishania is most likely the typical genus of the Maotianshan area of Chengjiang County.
