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.
^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.
^ abcFord, 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.
^ abcKenchington, 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.
^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.
^ abWilby, 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.