Earth:Bradgate Formation
From HandWiki
| Bradgate Formation Stratigraphic range: Ediacaran 561–557 Ma[1] | |
|---|---|
Bradgate Park, which gave the name to the formation, which itself can be found here. | |
| Type | Formation |
| Unit of | Maplewell Group |
| Sub-units | Hallgate and Sliding Stone Slump Breccia Members |
| Underlies | Hanging Rocks Formation[2] |
| Overlies | Beacon Hill Formation[2] |
| Thickness | 649 m (2,129 ft)[2] |
| Lithology | |
| Primary | Pelite |
| Other | Tuff, Graywacke, Breccia |
| Location | |
| Region | Leicestershire |
| Country | United Kingdom |
| Type section | |
| Named for | Bradgate Park |
The Bradgate Formation is a geologic formation in Leicestershire, and lies within the wider Bradgate Park area. It preserves fossils dating back to the Lower Ediacaran period.
Paleobiota
The Bradgate Formation contains the richest fossil beds within the Charnian Supergroup, from frondose organisms like Bradgatia and Charnia, which when the latter was discovered, showed definitive proof that macroscopic life did indeed exist before the Cambrian,[3] to discoid forms like Aspidella.
Template:Paleobiota-key-compact
Petalonamae
| Genus | Species | Notes | Images |
|---|---|---|---|
| Bradgatia[4] |
|
Sessile frondose organism. | |
| Charnia[3] |
|
Sessile frondose organism, and first organism found within this formation. | |
| Charniodiscus[3] |
|
Sessile frondose organism. | |
| Hylaecullulus[5] |
|
Sessile frondose organism. | |
| Primocandelabrum[6] |
|
Sessile frondose organism. | |
| Vinlandia[7] |
|
Sessile frondose organism. |
Cnidaria
| Genus | Species | Notes | Images |
|---|---|---|---|
| Auroralumina[8] |
|
Early sessile crown-group medusozoan cnidarian. |
incertae sedis
| Genus | Species | Notes | Images |
|---|---|---|---|
| Aspidella[9] |
|
Enigmatic discoidal fossil. | |
| Thectardis[9] |
|
Discoid organism, possibly holdfasts of petalonamids. |
Undescribed forms
| Genus | Species | Notes | Images |
|---|---|---|---|
| Gladius form[4] |
|
Enigmatic fossil, described to be in the shape of a gladius sword. | |
| Hemispherical form[4] |
|
Enigmatic fossil, described to be hemispherical in shape, with bifurcating radial ribs. | |
| Lanceolate frond[10] |
|
Enigmatic frondose fossil, described to be in the shape of a lance head, which has collapsed in onto itself. |
See also
- List of fossiliferous stratigraphic units in England
References
- ((Various Contributors to the Paleobiology Database)). "Fossilworks: Gateway to the Paleobiology Database". https://www.fossilworks.org.
- ↑ 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.
- ↑ 2.0 2.1 2.2 Moseley, John; Ford, Trevor. "The Sedimentology of the Charnian Supergroup". Mercian Geologist. https://www.emgs.org.uk/uploads/1/4/9/1/149143154/mg11_4_1989_251_moseley_ford_sedimentology_of_the_charnian_supergroup_2.pdf.
- ↑ 3.0 3.1 3.2 Ford, T. D. (September 1958). "PRE-CAMBRIAN FOSSILS FROM CHARNWOOD FOREST". Proceedings of the Yorkshire Geological Society 31 (3): 211–217. doi:10.1144/pygs.31.3.211.
- ↑ 4.0 4.1 4.2 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.
- ↑ Kenchington, Charlotte G.; Dunn, Frances S.; Wilby, Philip R. (October 2018). "Modularity and Overcompensatory Growth in Ediacaran Rangeomorphs Demonstrate Early Adaptations for Coping with Environmental Pressures". Current Biology 28 (20): 3330–3336.e2. doi:10.1016/j.cub.2018.08.036.
- ↑ Kenchington, Charlotte G.; Wilby, Philip R. (January 2017). "Rangeomorph classification schemes and intra-specific variation: are all characters created equal?". Geological Society, London, Special Publications 448 (1): 221–250. doi:10.1144/SP448.19.
- ↑ Brasier, Martin D.; Antcliffe, Jonathan B.; Liu, Alexander G. (September 2012). "The architecture of Ediacaran Fronds". Palaeontology 55 (5): 1105–1124. doi:10.1111/j.1475-4983.2012.01164.x.
- ↑ Dunn, F. S.; Kenchington, C. G.; Parry, L. A.; Clark, J. W.; Kendall, R. S.; Wilby, P. R. (25 July 2022). "A crown-group cnidarian from the Ediacaran of Charnwood Forest, UK". Nature Ecology & Evolution 6 (8): 1095–1104. doi:10.1038/s41559-022-01807-x.
- ↑ 9.0 9.1 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.
- ↑ Bowers, Aron. "Further Precambrian (Ediacaran) fossil discoveries in Charnwood Forest, Leicestershire". Mercian Geologist. https://www.monash.edu/__data/assets/pdf_file/0009/85626/mercian-2014-v18-p175-further-ediacaran-fossils-charwood-forest-bowers.pdf.







