This article relies largely or entirely on a single source .(May 2025) |
Llangynog Inlier (Coomb Volcanic Formation) | |
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Stratigraphic range: Ediacaran [1] | |
Type | Formation |
Unit of | Wrekin terrane |
Sub-units | Castell Cogan Rhyolite and Coed Cochion Volcaniclastic Member |
Thickness | 1100 m (3,608 ft) |
Lithology | |
Primary | Volcaniclastic Rocks [1] |
Other | Rhyolite, Dolerite, Dacite, Rhyolitic Conglomerate [1] |
Location | |
Country | Wales |
The Llangynog Inlier (Coomb Volcanic Formation) is a geologic formation that crops out in Wales, which mainly consists of volcaniclastic rocks and rhyolite, as well as dolerite, dacite and a layer of rhyolitic conglomerates. A recent study also managed to date the Inlier to between 566 and 563 Ma, which means it temporally correlates directly with the Fermeuse Formation of Newfoundland, the Beacon Hill Formation in the Charnwood Forest, and the neighboring Stretton Shale Formation in Long Mynd. It also preserves fossils dating back to the Ediacaran period.
The Llangynog Inlier is that of a tidally active shallow marine environment that saw much volcanic activity. It also preserves a small collection of Ediacaran forms, from the discoidal Aspidella to the elongated Palaeopascichnus. [1]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Notes | Images |
---|---|---|---|
Aspidella [1] |
| Enigmatic discoidal fossil. | ![]() |
Ediacaria [2] |
| Enigmatic discoidal fossil, possibly a synonym of Aspidella. | ![]() |
Hiemalora [1] |
| Discoid organism, possibly holdfasts of petalonamids. | ![]() |
Palaeopascichnus [1] |
| Palaeopascichnid organism. | ![]() |
Genus | Species | Notes | Images |
---|---|---|---|
Sinusoidal trace [1] |
| A sinusoidal trace fossil, possibly a feeding trace of an unknown organism. | |