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Renews Head Formation

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Renews Head Formation
Stratigraphic range: Ediacaran
TypeFormation
Unit ofSt John's Group[1]
Underlies
OverliesFermeuse Formation
Lithology
PrimaryDark-gray Sandstone[3]
OtherMinor Shale[3]
Location
RegionNewfoundland
CountryCanada

Outcrop occurrence

The Renews Head Formation is a geologic formation in Newfoundland and Labrador, and consists of dark-gray sandstones, with minor shales scattered throughout.[3] It preserves fossils dating back to the Ediacaran period.[4]

Paleobiota

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The Renews Head Formation is home to a small range of discoidal forms, like Aspidella.[4][5]

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
Aspidella[4]
  • Aspidella sp.
Enigmatic discoidal fossil.
Hiemalora
  • Hiemalora sp.
Enigmatic tentacled discoidal organism.

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.G. Liu; D. McIlroy (September 2014). "Horizontal Surface Traces from the Fermeuse Formation, Ferryland (Newfoundland, Canada), and their Place within the Late Ediacaran Ichnological Revolution" (PDF). Geological Association of Canada - Special Paper (9).[dead link]
  2. ^ a b "Geoscience Atlas". Geological Survey Division of the Department of Natural Resources, Government of Newfoundland and Labrador.
  3. ^ a b c "GEOLOGY OF THE AVALON PENINSULA, NEWFOUNDLAND" (PDF).
  4. ^ a b c Hofmann, H. J.; O'Brien, S. J.; King, A. F. (January 2008). "Ediacaran biota on Bonavista Peninsula, Newfoundland, Canada". Journal of Paleontology. 82 (1): 1–36. doi:10.1666/06-087.1.
  5. ^ Gehling, James G.; Narbonne, Guy M.; Anderson, Michael M. (September 2000). "The first named Ediacaran body fossil, Aspidella Terranovica". Palaeontology. 43 (3): 427–456. doi:10.1111/j.0031-0239.2000.00134.x.