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The Rhuddanian Stage is the first of three stages within the Llandovery Series, which is the lowermost division of the Silurian Period. This stage encompasses rocks deposited between 443.4 and 440.8 million years ago, marking the beginning of the Silurian System. The Rhuddanian Stage is defined by the first appearance of specific graptolites, Akidograptus ascensus and Parakidograptus praematurus, found in the Birkhill Shale Formation in Scotland. It directly overlies the Hirnantian Stage of the Ordovician Period and precedes the Aeronian Stage. The name "Rhuddanian" originates from Cefn-Rhuddan Farm in Wales.12

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