dently waterworn, is marked with closely-approximated hexagonal areæ, of which the four lateral sides are nearly twice the length of the upper and lower: these hexagons, which are the waterworn terminations of the bracteæ of the Strobilus, becoming gradually smaller and less distinct towards the top.
A transverse section of the Strobilus exhibits a central axis, from which radii directly proceed, constantly thirteen in number, resembling, when perfect, the spokes of a wheel, but several of them being always more or less incomplete. These radii alternate with an equal number of oblong bodies, also radiating, of a lighter colour, and which are not directly connected with the axis: beyond these twenty-six radiating bodies a double series of somewhat rhomboidal areolæ exist. These appearances not readily indicating the actual structure in the transverse, are satisfactorily explained by the vertical section.
From the vertical section it appears that the Strobilus is formed of a central axis of small diameter compared with the parts proceeding from it, which consist,—
1. Of bracteæ densely approximated and much imbricated; the lower half of each of these stands at right angles to the axis, while the imbricating portion, of about equal length with the lower, and forming an obtuse angle with it, is gradually thickened upwards: these form the spokes and external rhomboidal areæ of the transverse section.
2. Of an equal number of oblong bodies of a lighter colour and more transparent, each of which is adnate and connected by cellular tissue with the upper surface of the supporting bractea. These bodies are sections of Sporangia filled with innumerable microscopic sporules, originally connected in threes (very rarely in fours), but ultimately separating, as shown in Tab. XXIV, fig. G.
From this triple composition or union of sporules, which differs from the constant quadruple union in tribes of existing plants, namely, Ophioglosseæ and Lycopodiaceæ, which, from other points of structure, may he supposed most nearly related to the fossil, I have called it Triplosporite, a name which expresses its fossil state, the class or primary division to which it belongs, and its supposed peculiarity of structure.
The structure of the axis, which is well preserved in the specimen, di-
