Deep Spring Formation

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Deep Spring Formation
Stratigraphic range: Ediacaran - Cambrian 540–527 Ma [1]
TypeGeological Formation
Sub-unitsDunfee, Esmeralda and Gold Point Members
UnderliesCampito Formation[2]
OverliesReed Dolomite[2]
Thickness549 m (1800 ft)
Lithology
PrimaryLimestone
OtherQuartzite, Siltstone
Location
RegionNevada
CountryUnited States

The Deep Spring Formation is a geologic formation in Nevada. It preserves fossils dating back to the Ediacaran and Cambrian periods, like Wutubus and Elainabella.[3][4] It is also currently the only known Ediacaran Lagerstätten in the Southwestern United States.[3]







Paleobiota

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The first organism to be described from the Deep Spring Formation in 2014 was Elainabella in the Esmeralda Member, an enigmatic alga with similarities to green algae, suggesting that part of the formation was at one point a shallow marine environment or a microbial reef community.[4] More organisms would be described in 2016, most of which are ichnogenus' like Planolites, and even some tubular forms, like Wutubus, expanding not only the stratigraphic range of some of these forms, but also their biogeographic range.[3]

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Paleobiota
Genus Species Notes Images
Conotubus
  • Conotubus sp.
Non-biomineral tubular fossil.
Gaojiashania
  • Gaojiashania sp.
Worm-like organism.
Wutubus
  • W. annularis
Tubular fossil.
Elainabella[4]
  • E. deepspringensis
Enigmatic filamentous multicellular alga.
Bergaueria?
  • Bergaueria sp.
Resting place of Cnidarians.
Neonereites?
  • Neonereites sp.
Burrows.
Planolites
  • Planolites sp.
Burrows.
Scolicia?
  • Scolicia sp.
Burrows.

See also

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References

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  1. ^ Smith, Emily F.; Nelson, Lyle L.; O’Connell, Nizhoni; Eyster, Athena; Lonsdale, Mary C. (22 September 2022). "The Ediacaran−Cambrian transition in the southern Great Basin, United States". GSA Bulletin. doi:10.1130/B36401.1.
  2. ^ a b Edwin 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.
  3. ^ a b c Smith, E.F.; Nelson, L.L.; Strange, M.A.; Eyster, A.E.; Rowland, S.M.; Schrag, D.P.; Macdonald, F.A. (1 November 2016). "The end of the Ediacaran: Two new exceptionally preserved body fossil assemblages from Mount Dunfee, Nevada, USA". Geology. 44 (11): 911–914. doi:10.1130/G38157.1.
  4. ^ a b c Rowland, Stephen M.; Rodriguez, Margarita G. (March 2014). "A Multicellular Alga with Exceptional Preservation from the Ediacaran of Nevada". Journal of Paleontology. 88 (2): 263–268. doi:10.1666/13-075. ISSN 0022-3360. S2CID 129796477.