The Campito Formation is mainly composed of very fine to fine-grained quartzite, with small amounts of siltstone, getting up to 3,500 ft (1,100 m) thick.[3]
Members
The formation is split into two distinct members, which are as follows, in ascending age:
Andrews Mountain Member: It is the thickest of the two members, getting up to 2,800 ft (850 m) thick. It is composed of olive-gray or greenish-gray very fine to fine grained silty quartziticsandstone or quartzite and interbedded layers of dark-greenish-gray siltstones, which weather to a greenish-black or just black. The quartzite layers are composed of sub-angular very fine to fine grains of quartz, feldspar and other metallic minerals, all set within a muscovite, chlorite, and biotite.[3]
Montenegro Member: It is the thinnest of the two members, only getting up to 1,000 ft (300 m) thick. It is composed of dark-greenish-gray and greenish-gray siltstone composed of a mixture of quartz, muscovite, and chlorite. The siltstone is evenly laminated to thin-bedded. There are also commonly occurring archeocyathid-bearing limestone beds in the upper sections of the member.[3]
Paleobiota
The Campito Formation contains a number of fossils, most of which are found within the Montenegro Member. They range from archeocyathid sponges like Ethmophyllum, to arthropod trilobites like Nevadia,[3] and a wealth of ichnogenera, from burrows like Skolithos, to resting traces like Rusophycus.[4]
^ a bPruss, Sara B.; Smith, Emily F.; Zhuravlev, Andrey Yu; Nolan, Rhiannon Z.; McGann, Tessa C. (June 2025). "Rise and fall of archaeocyath reefs shaped early Cambrian skeletal animal abundance". Palaeogeography, Palaeoclimatology, Palaeoecology. 667 112852. doi:10.1016/j.palaeo.2025.112852.
^ a bEdwin H. McKee (1968). "Geology of the Magruder Mountain area, Nevada-California" (PDF). U.S. Geological Survey Bulletin: H7. doi:10.3133/B1251H. ISSN 8755-531X. Wikidata Q57805921.
^ a b c d e f g h i jStewart, J. H. "Upper Precambrian and Lower Cambrian Strata, in the Southern Great Basin California and Nevada" (PDF). U.S. Geological Survery. Geological Survey Professional.
^ a b c d e f g h i j k l m n oAlpert, Stephen P. (1976). "Trilobite and Star-like Trace Fossils from the White-Inyo Mountains, California". Journal of Paleontology. 50 (2): 226–239. ISSN 0022-3360.
^ a b c dStewart, H. J. (2007). "Fallotaspidoid trilobite assemblage (Lower Cambrian) from the Esmeralda Basin (western Nevada, U.S.A.): The oldest trilobites from Laurentia". Alcheringa: An Australasian Journal of Palaeontology. 31: 123–140. doi:10.1080/03115510701586897.
^ a b cLieberman, B.S. (2002). "Phylogenetic analysis of some basal early Cambrian Trilobites, the biogeographic origins of the Eutrilobites, and the timing of the Cambrian radiation" (PDF). Journal of Paleontology. 76 (4): 692–708. doi:10.1666/0022-3360(2002)076<0692:paosbe>2.0.co;2. Archived from the original (PDF) on 2011-08-12. Retrieved 2012-08-14.
^ a b c dFirby, Jean B.; Durham, J. Wyatt (1974). "Molluscan Radula from Earliest Cambrian". Journal of Paleontology. 48 (6): 1109–1119. ISSN 0022-3360.
^ a bSignor, Philip W.; Mcmenamin, Mark A. S. (March 1988). "The Early Cambrian worm tube Onuphionella from California and Nevada". Journal of Paleontology. 62 (2): 233–240. doi:10.1017/S0022336000029863.
^ a b c d e f g h iStewart Hollingsworth, J. (May 2005). "The earliest occurrence of trilobites and brachiopods in the Cambrian of Laurentia". Palaeogeography, Palaeoclimatology, Palaeoecology. 220 (1–2): 153–165. doi:10.1016/j.palaeo.2004.08.008.
^ a b c d eHollingsworth, J. Stewart (2006). "Holmiidae (Trilobita: Olenellina) of the Montezuman Stage (Early Cambrian) in Western Nevada". Journal of Paleontology. 80 (2): 309–332. ISSN 0022-3360.
^Skovsted, Christian B.; Balthasar, Uwe; Vinther, Jakob; Sperling, Erik A. (May 2021). "Small shelly fossils and carbon isotopes from the early Cambrian (Stages 3–4) Mural Formation of western Laurentia". Papers in Palaeontology. 7 (2): 951–983. doi:10.1002/spp2.1313.
^ a b c d e f gWotte, Thomas; Sundberg, Frederick A. (2017). "Small shelly fossils from the Montezuman–Delamaran of the Great Basin in Nevada and California". Journal of Paleontology. 91 (5): 883–901. ISSN 0022-3360.
^ a b cRowell, A. J. (1977). "Early Cambrian Brachiopods from the Southwestern Great Basin of California and Nevada". Journal of Paleontology. 51 (1): 68–85. ISSN 0022-3360.
^Tynan, Mark C. (1983). "Coral-like Microfossils from the Lower Cambrian of California". Journal of Paleontology. 57 (6): 1188–1211. ISSN 0022-3360.
^Ubaghs, Georges (May 1975). "Early Paleozoic Echinoderms". Annual Review of Earth and Planetary Sciences. 3 (1): 79–98. doi:10.1146/annurev.ea.03.050175.000455.