Beacon Hill Formation | |
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Stratigraphic range: Ediacaran | |
![]() Beacon Hill, which gave the name to the formation, which itself can be found here. | |
Type | Formation |
Unit of | Maplewell Group |
Sub-units | Old John, Outwoods Member, Buck Hills, Sandhills Lodge, Beacon Tuffs, Charnwood Lodge, Benscliffe Members |
Underlies | Bradgate Formation [2] |
Overlies | Blackbrook Reservoir Formation [2] |
Thickness | 1119 m (3,671 ft) [2] |
Lithology | |
Primary | Tuff |
Other | Pelite, Greywacke, Breccia |
Location | |
Region | Leicestershire |
Country | United Kingdom |
Type section | |
Named for | Beacon 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.
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
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Notes | Images |
---|---|---|---|
Charnia [4] |
| Sessile frondose organism. | ![]() |
Genus | Species | Notes | Images |
---|---|---|---|
Aspidella [1] [5] |
| Enigmatic discoidal fossil. | ![]() |
Cyclomedusa [5] |
| Enigmatic discoidal fossil. | ![]() |
Hiemalora [5] |
| Discoid organism, possibly holdfasts of petalonamids. | ![]() |
Genus | Species | Notes | Images |
---|---|---|---|
Pseudovendia [6] |
| Poorly preserved organism, originally thought to be an early arthropod. | ![]() |