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Twitya Formation

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Twitya Formation
Stratigraphic range: Cryogenian 662.4 Ma[1]
TypeFormation
Unit ofHay Creek Group[1]
UnderliesKeele Formation
OverliesShezal Formation
Thickness900 m (2,952 ft)[2]
Lithology
PrimaryCap carbonate
OtherMudstone, Siltstone, Shale, Sandstone
Location
RegionNorthwest Territories
CountryCanada

The Twitya Formation is a geologic formation in Canada’s Northwest Territories. It mainly consists of cap carbonate rocks, shales and Sandstone-siltstone, with finely laminated mudstone and siltstones.[1] It preserves fossils dating back to the Cryogenian period.[3]

Dating

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Using a combination of Re-Os geochronology and Os-Sr isotope dating at the base of the Twitya Formation, a date of 662±Ma has been recovered, placing the formation within the late Cryogenian.[1]

Paleobiota

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The Twitya Formation contains a small selection of discoidal and annunli forms, from Nimbia occlusa to tentative records of Irridinitus and Vendella.[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.

incertae sedis

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Genus Species Notes Images
Nimbia[3]
  • N. occlusa
Discoid organism.
Irridinitus (?)[3]
  • Irridinitus sp. (?)
Discoid organism, tentative assignment.
Vendella (?)[3]
  • Vendella sp. (?)
Discoid organism, tentative assignment. It is noted that it may be a junior synonym of Beltanelliformis.

See also

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References

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  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.


  1. ^ a b c d Rooney, Alan D.; Macdonald, Francis A.; Strauss, Justin V.; Dudás, Francis Ö.; Hallmann, Christian; Selby, David (7 January 2014). "Re-Os geochronology and coupled Os-Sr isotope constraints on the Sturtian snowball Earth". Proceedings of the National Academy of Sciences. 111 (1): 51–56. doi:10.1073/pnas.1317266110.
  2. ^ Narbonne, G; Aitken, J (May 1995). "Neoproterozoic of the Mackenzie Mountains, northwestern Canada". Precambrian Research. 73 (1–4): 101–121. doi:10.1016/0301-9268(94)00073-Z.
  3. ^ a b c d e Hofmann, H. J.; Narbonne, G. M.; Aitken, J. D. (1990). "Ediacaran remains from intertillite beds in northwestern Canada". Geology. 18 (12): 1199. doi:10.1130/0091-7613(1990)018<1199:ERFIBI>2.3.CO;2.