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Just a hundred years ago Bernhard von Cotta described, in one of the earliest works dealing with the internal structure of silicified plants, the Permian tree-fern now known as Zygopteris primaria. The general belief is that only one specimen was ever discovered ; our knowledge of the structure is thus confined to the petiole, and that, too, as we shall see, is defective. It was therefore a pleasant surprise when, during a visit to Berlin in September, 1929, I came across a magnificent specimen with the centre occupied by a fairly well-preserved protostelic stem.
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Birbal Sahni (1932) studied this question.
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