• Source: Beacon Limestone Formation

The Beacon Limestone Formation, historically known as the Junction Bed, is a formation of the early Jurassic age (Pliensbachian–Toarcian). It lies above the Dyrham Formation and below the Bridport Sand Formation. It forms part of the Lias Group. It is found within the Wessex Basin and parts of Somerset, in England. It is well known for the Strawberry Bank Lagerstätte, which contains the 3-dimensionally preserved remains of vertebrates, including marine crocodyliformes, ichthyosaurs and fish, as well as insect compression fossils.




Fossil content


Among others, the following fossils have been reported from the formation:




= Vertebrates

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= Invertebrates

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References

Kata Kunci Pencarian:

• Beacon Limestone Formation
• Glastonbury Tor
• Carboniferous Limestone
• Dyrham Formation
• List of fossiliferous stratigraphic units in England
• Necrotauliidae
• Dermapteridae
• Geology of Dorset
• Bridport Sand Formation
• Fulgoridiidae