It has three unnamed Members, simply known as 'Upper', 'Middle', and 'Lower', that mainly consist of limestone, conglomerate rocks and dolostone respectively, with sandstone and siltstones found within the 'Upper' and 'Lower' Members, with the latter itself further containing quartzite and shales.[1][2] The 'Upper' and 'Middle' Members are Cambrian in age, including the upper rocks of the 'Lower Member', whilst the rest of the 'Lower' Member is Ediacaran in age.[1]
Sessile frondose organism, although assignment has been questioned based on the possibility that know specimens could be referred to other known Cambrian frondose organisms.[8]
Tubular organism. A recent 2017 suggests reported specimens may instead be poorly preserved Gaojiashania specimens,[14] although future studies do not note this.
Tubular fossil, first occurrence in this formation and new species. A study done in the same year discovered some of the first remains of cloudinomorph soft-tissue material within the tubes, resembling bilaterian-like through-guts, which would also make them the oldest known guts in the fossil record.[17]
Tubular organism. A recent 2017 suggests reported specimens may instead be poorly preserved Gaojiashania specimens,[14] although future studies do not note this.
Tubular fossil, first occurrence in this formation and new species. A study done in the same year discovered some of the first remains of cloudinomorph soft-tissue material within the tubes, resembling bilaterian-like through-guts, which would also make them the oldest known guts in the fossil record.[17]
Tubular organism, first known occurrence in Ediacaran aged rock. A recent 2017 suggests reported specimens may instead be poorly preserved Gaojiashania specimens,[14] although future studies do not note this.
Calcareous fossils that are conical in shape, although their poor preservation hinders any proper assignments. They have been suggested to represent the well-known and common organism Cloudina, the small shelly fossil Wyattia, or even a new genus.
1 2 3 4 5 6 Evans, Scott D.; Smith, Emily F.; Vayda, Prescott; Nelson, Lyle L.; Xiao, Shuhai (October 2024). "The Ediacara Biota of the Wood Canyon formation: Latest Precambrian macrofossils and sedimentary structures from the southern Great Basin". Global and Planetary Change. 241: 104547. Bibcode:2024GPC...24104547E. doi:10.1016/j.gloplacha.2024.104547.
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