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s, but they are not wholly so rectilinear, diminishing slightly towards their base of attachment; they are ranged, too, along the stem or midrib, not at a right angle, but at an acute one; the line of attachment is not set awry, but on the general plane of the leaf; and the midrib itself is considerably less massive and round. A third species from the same locality bears a general resemblance to the latter; but the leaflets are narrower at the base, and, as the print indicates (Fig. 136), so differently attached to the stem, that from the pressure in the rock most of them have become detached; while yet a fourth species (Fig. 137), very closely resembles a Zamia of the Scarborough Oolite,--_Z. lanceolata_. The leaflets, however, contract much more suddenly from their greatest breadth than those of _lanceolata_, into a pseudo-footstalk; and the contraction takes place not almost equally on both sides, as in that species, but almost exclusively on the upper side. And so, provisionally at least, this Helmsdale Zamia may be regarded as specifically new. [Illustration: Fig. 135.] [Illustration: Fig. 136.] [Illustration: Fig. 137.] [Illustration: Fig. 138. CONE.] With the leaves of the Eathie Zamia, we find, in this northern outlier of the Lias, cones of a peculiar form, which, like the leaves themselves, are still unfigured and undescribed, and some of which could scarce have belonged to any coniferous tree. In one of these (Fig. 138), the ligneous bracts or scales, narrow and long, and gradually tapering till they assume nearly the awl-shaped form, cluster out thick from the base and middle portions of the cone, and, like the involucral appendages of the hazel-nut, or the sepals of the yet unfolded rose-bud, sweep gracefully upwards to the top, where they present at their margins minute denticulations. In another species the bracts are broader, thinner, and more leaf-like: they rise, too, more from the base of the cone, and less from its middle portions; so that the whole must have resembled an enormous bud, with strong woody scales, some of which extended from base to apex. The first described of these two species seems to have been more decidedly a _cone_ than the other; but it is probable that they were both connecting links between such leathern seed-bearing flowers as we find developed in _Cycas revoluta_, and such seed-bearing cones as we find exemplified in _Zamia pungens_. The bud-like cone, however, d
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