The Wood Canyon Formation is a geologic formation in the northern Mojave Desert of Inyo County, California and Nye County and Clark County, Nevada.[2][3]
It can be seen in the Panamint Range and Funeral Mountains adjoining Death Valley, within Death Valley National Park; and in the Spring Mountains in Clark County.[2]
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]
Paleobiota
The Wood Canyon Formation spans from the late Ediacaran period of the Neoproterozoic Era into the Lower Cambrian Period of the Paleozoic Era.[2][3][5] As for the fossils and biota found within the formation, the Cambrian strata is home to olenellidtrilobites and archaeocyathid sponges,[2] whilst the Ediacaran strata contains petalonamid forms like Pteridinium and ichnotaxon traces like Helminthoidichnites.[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.
Various pyritized tubular forms ranging from 0.3 to 7 cm in length and 1 to 5 mm in diameter.
See also
List of fossiliferous stratigraphic units in California
List of fossiliferous stratigraphic units in Nevada
Paleontology in California
Paleontology in Nevada
References
↑ 1.01.11.21.31.41.5Evans, 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 Change241. doi:10.1016/j.gloplacha.2024.104547. Bibcode: 2024GPC...24104547E.
↑ 8.08.1Runnegar, Bruce; Gehling, James G.; Jensen, Sören; Saltzman, Matthew R. (October 2024). "Ediacaran paleobiology and biostratigraphy of the Nama Group, Namibia, with emphasis on the erniettomorphs, tubular and trace fossils, and a new sponge, Arimasia germsi n. gen. n. sp.". Journal of Paleontology98 (S94): 1–59. doi:10.1017/jpa.2023.81. Bibcode: 2024JPal...98S...1R.
↑ 9.09.19.2Mata, Scott A.; Corsetti, Cara L.; Corsetti, Frank A.; Awramik, Stanley M.; Bottjer, David J. (2012). "Lower Cambrian Anemone Burrows from the Upper Member of the Wood Canyon Formation, Death Valley Region, United States: Paleoecological and Paleoenvironmental Significance". PALAIOS27 (9/10): 595–607. doi:10.2110/palo.2012.p12-016r. ISSN0883-1351. Bibcode: 2012Palai..27..594M.
↑Runnegar, Bruce; Horodyski, Robert J.; Gehling, James G.; Jensen, Sören; Bengtson, Stefan; Peterson, Kevin J.; Saltzman, Matthew R.; Vendrasco, Michael J. (November 2024). "Tulaneia amabilia n. gen. n. sp.: a new erniettomorph from the Wood Canyon Formation, Nevada and the age of the Ediacaran–Cambrian transition in the Great Basin". Journal of Paleontology98 (6): 929–951. doi:10.1017/jpa.2024.45. Bibcode: 2024JPal...98..929R.
↑ 16.016.1Selly, Tara; Schiffbauer, James D.; Jacquet, Sarah M.; Smith, Emily F.; Nelson, Lyle L.; Andreasen, Brock D.; Huntley, John Warren; Strange, Michael A. et al. (16 February 2020). "A new cloudinid fossil assemblage from the terminal Ediacaran of Nevada, USA". Journal of Systematic Palaeontology18 (4): 357–379. doi:10.1080/14772019.2019.1623333. Bibcode: 2020JSPal..18..357S.