The origin of these fossils will be understood by reference to the four specimens delineated in [Lign. 81]. In fig. 3, a fungiform flint, resembling fig. 6, of [Lign. 80], is seen in the lower part of a cup-shaped zoophyte; while above, and surrounding the flint, the impression remains of the reticulated outer surface, deeply coloured by a ferruginous tinge. In fig. 4, [Lign. 81], a small turbinated flint, resembling fig. 4, of [Lign. 80], occupies the base, and three rootlets are seen emerging from it at a. In [Lign. 82, fig. 1], in which the chalk has been removed so as to expose the outer surface of the Ventriculite, a flint occupies the centre at c; above which, the radiating reticulated structure is spread out on the chalk, a; the base, with its roots, is shown at b.

Lign. 81. Ventriculites radiatus; 1/6 nat.
Chalk; near Lewes.

Fig.1.—A perfect specimen in chalk, inverted, showing the external reticulated surface; the apex of the base projects in the centre.
2.—Specimen expanded, displaying the inner surface, studded over with the openings of the cells or tubes.
3.—A Ventriculite in chalk; the lower part inclosed in flint.
4.—Portion of a Ventriculite; the stem towards the base is enveloped in flint, and three radicle processes spread from it into the surrounding chalk at a.

These specimens demonstrate that all the flints referred to, have been moulded in the cavities of cyathiform zoophytes; and that their diversity of figure has arisen from the amount of silex that happened to permeate the organism; if but a small proportion of silica in solution was present, then flints, like fig. 4, were produced; if the quantity were sufficient to fill up a considerable part of the tissues of the original, fungiform flints, as [Lign. 80, fig. 3], and [Lign. 81, fig. 3], were the result. The disciform flints originated from the expanded examples, [Lign. 81], figs. 1 and 2: and when the silex was insufficient to silicify the entire zoophyte, an annular flint, resembling a quoit, was formed.

Lign. 82. Portions of Ventriculites; 1/4 nat.
Chalk, near Lewes.

Fig.1.—A specimen, in which the middle is inclosed in a flint c; the external structure of the Ventriculite is seen at a, expanded on the chalk; and the pedicle with its roots is exposed at b. The figures are one-fourth the size of the originals.
2, 3,5.—Chalk specimens, showing the external structure of stems of Ventriculites.
4.—A siliceous cast of the cavity of a Ventriculite covered with papillæ, moulded in the orifices of the cells.