It was my intention to have devoted this paper to the Coniferous Fruits found in Strata of Secondary age in Britain, reserving for future examination, those belonging to the later periods, but in the progress of my investigations I have found that, two remarkable cones, which have hitherto been considered as belonging to the Greensand, are certainly Tertiaryfossils; and having placed them on the plates which illustrate this paper, I shall include them in my descriptions.
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