. The testimony of the rocks; . indicates (Fig. 136), so differently attached to the stem, that Fig. 136. from the pressure in the rock most of them have become41 482 ON THE LESS KNOWN detached; while yet a fourth species (Fig. 137), very closelyresembles a Zamia of the Scarborough Oolite, — Z. lanceo-lata. The leaflets, however, contract much more suddenly Fig. 137.

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