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These beds, which are without any marine equivalent in this country, appear completely to bridge over the interval between the Neocomian and the Oolites. They may, perhaps, as suggested by Mr. Judd, be of the same age as part of the Wealden series. Gervillia anceps, Desh. Trigonia caudata, Agassiz. Terebratula sella, Sowerby. Diceras Lonsdalii. Upper Neocomian, Wilts. a. The bivalve shell. b.
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