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Beacon Hill Formation

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Beacon Hill Formation
Stratigraphic range: Ediacaran 569–561 Ma[1]
Beacon Hill, which gave the name to the formation, which itself can be found here.
TypeFormation
Unit ofMaplewell Group
Sub-unitsOld John, Outwoods Member, Buck Hills, Sandhills Lodge, Beacon Tuffs, Charnwood Lodge, Benscliffe Members
UnderliesBradgate Formation[2]
OverliesBlackbrook Reservoir Formation[2]
Thickness1119 m (3,671 ft)[2]
Lithology
PrimaryTuff
OtherPelite, Greywacke, Breccia
Location
RegionLeicestershire
CountryUnited Kingdom
Type section
Named forBeacon Hill

The Beacon Hill Formation is a geologic formation in Leicestershire, and lies within the wider Beacon Hill area. It preserves fossils dating back to the Lower Ediacaran period.

Paleobiota

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The Beacon Hill Formation contains the oldest best preserved fossils within the Charnian Supergroup, most of which can be found in the Outwoods Member, with some found in the overlying and underlying members. [3][4]

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.

Petalonamae

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Genus Species Notes Images
Charnia[4]
  • C. masoni
Sessile frondose organism.

incertae sedis

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Genus Species Notes Images
Aspidella[1][5]
  • Aspidella sp.
Enigmatic discoidal fossil.
Cyclomedusa[5]
  • C. davidi
Enigmatic discoidal fossil.
Hiemalora[5]
  • Hiemalora sp.
Discoid organism, possibly holdfasts of petalonamids.

Ivesheadiomorph

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Genus Species Notes Images
Pseudovendia[6]
  • P. charnwoodensis
Poorly preserved organism, originally thought to be an early arthropod.

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 Noble, Stephen R.; Condon, Daniel J.; Carney, John N.; Wilby, Philip R.; Pharaoh, Timothy C.; Ford, Trevor D. (January 2015). "U-Pb geochronology and global context of the Charnian Supergroup, UK: Constraints on the age of key Ediacaran fossil assemblages". Geological Society of America Bulletin. 127 (1–2): 250–265. doi:10.1130/B31013.1.
  2. ^ a b c Moseley, John; Ford, Trevor. "The Sedimentology of the Charnian Supergroup" (PDF). Mercian Geologist.
  3. ^ Kenchington, Charlotte G.; Harris, Simon J.; Vixseboxse, Philip B.; Pickup, Chris; Wilby, Philip R. (June 2018). "The Ediacaran fossils of Charnwood Forest: Shining new light on a major biological revolution". Proceedings of the Geologists' Association. 129 (3): 264–277. doi:10.1016/j.pgeola.2018.02.006.
  4. ^ a b Bowers, Aron. "Further Precambrian (Ediacaran) fossil discoveries in Charnwood Forest, Leicestershire" (PDF). Monash University. Mercian Geologist. Retrieved 5 May 2025.
  5. ^ a b c Wilby, Philip R.; Carney, John N.; Howe, Michael P.A. (1 July 2011). "A rich Ediacaran assemblage from eastern Avalonia: Evidence of early widespread diversity in the deep ocean". Geology. 39 (7): 655–658. doi:10.1130/G31890.1.
  6. ^ H. E. Boynton, T. D. Ford (1979). "Pseudovendia charnwoodensis — A new Precambrian arthropod from Charnwood Forest, Leicestershire". Mercian Geologist. 7: 175–177.