Bradgate Formation
{{Short description|Geologic formation in Leicestershire, the United Kingdom}}
{{Infobox rockunit
| name = Bradgate Formation
| image = File:Bradgate park rocks.jpg
| caption = Bradgate Park, which gave the name to the formation, which itself can be found here.
| type = Formation
| age = Ediacaran {{Geological range|561|557|ref={{cite journal |last1=Noble |first1=Stephen R. |last2=Condon |first2=Daniel J. |last3=Carney |first3=John N. |last4=Wilby |first4=Philip R. |last5=Pharaoh |first5=Timothy C. |last6=Ford |first6=Trevor D. |title=U-Pb geochronology and global context of the Charnian Supergroup, UK: Constraints on the age of key Ediacaran fossil assemblages |journal=Geological Society of America Bulletin |date=January 2015 |volume=127 |issue=1-2 |pages=250–265 |doi=10.1130/B31013.1}}}}
| period = Ediacaran
| prilithology = Pelite
| otherlithology = Tuff, Graywacke, Breccia
| namedfor = Bradgate Park
| namedby =
| region = Leicestershire
| country = {{Flag|United Kingdom}}
| coordinates =
| unitof = Maplewell Group
| subunits = Hallgate and Sliding Stone Slump Breccia Members
| underlies = Hanging Rocks Formation{{cite web |last1=Moseley |first1=John |last2=Ford |first2=Trevor |title=The Sedimentology of the Charnian Supergroup |url=https://www.emgs.org.uk/uploads/1/4/9/1/149143154/mg11_4_1989_251_moseley_ford_sedimentology_of_the_charnian_supergroup_2.pdf |publisher=Mercian Geologist}}
| overlies = Beacon Hill Formation
| thickness = 649 m (2,129 ft)
| extent =
| area =
| map =
| map_caption =
}}
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,{{cite journal |last1=Ford |first1=T. D. |title=PRE-CAMBRIAN FOSSILS FROM CHARNWOOD FOREST |journal=Proceedings of the Yorkshire Geological Society |date=September 1958 |volume=31 |issue=3 |pages=211–217 |doi=10.1144/pygs.31.3.211}} to discoid forms like Aspidella.
{{Paleobiota-key-compact}}
= Petalonamae =
= ''incertae sedis'' =
class="wikitable" style="width:70%;" |
Genus
!Species !Notes !Images |
---|
Aspidella{{cite journal |last1=Wilby |first1=Philip R. |last2=Carney |first2=John N. |last3=Howe |first3=Michael P.A. |title=A rich Ediacaran assemblage from eastern Avalonia: Evidence of early widespread diversity in the deep ocean |journal=Geology |date=1 July 2011 |volume=39 |issue=7 |pages=655–658 |doi=10.1130/G31890.1}}
|
|Enigmatic discoidal fossil. |
Thectardis
|
|Discoid organism, possibly holdfasts of petalonamids. |
= Undescribed forms =
class="wikitable" style="width:70%;" |
Genus
!Species !Notes !Images |
---|
Gladius form
|
|Enigmatic fossil, described to be in the shape of a gladius sword. | |
Hemispherical form
|
|Enigmatic fossil, described to be hemispherical in shape, with bifurcating radial ribs. | |
Lanceolate frond{{cite web |last1=Bowers |first1=Aron |title=Further Precambrian (Ediacaran) fossil discoveries in Charnwood Forest, Leicestershire |url=https://www.monash.edu/__data/assets/pdf_file/0009/85626/mercian-2014-v18-p175-further-ediacaran-fossils-charwood-forest-bowers.pdf |website=Monash University |publisher=Mercian Geologist |access-date=5 May 2025}}
|
|Enigmatic frondose fossil, described to be in the shape of a lance head, which has collapsed in onto itself. | |
See also
{{Portal|Earth sciences|United Kingdom|Paleontology|}}
References
- {{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= ((Various Contributors to the Paleobiology Database))|url= https://www.fossilworks.org|access-date= 17 December 2021}}