The aerial shoots of this species are occasionally branched dichotomously[539], the apical portions bearing short crowded leaves[540]; the surface of the bark is either completely covered with contiguous leaf-scars without definite leaf-cushions or with projecting cushions forming a narrow sloping surface surrounding each leaf-scar. Other parts of the plant may possess cushions similar in their kite-shaped form to those of Lepidodendron, but without a median vertical groove, or the leaf-scars may be spirally disposed at varying distances apart on a comparatively smooth and longitudinally wrinkled bark. The species exhibits striking instances of a transition between the Favularian, Clathrarian, and Leiodermarian forms of stems. The leaf-scars, which are hexagonal in outline,—the lateral angles pointed and transversely elongated, the upper and lower angles rounded,—bear three scars, the central leaf-trace and two straight or curved lateral parichnos scars; a ligular pit occurs immediately above the centre of the upper edge of the leaf-scar and occasionally circular elevations with a central pit occur singly or in pairs below a leaf-scar ([fig. 196], A). The linear leaves, which may persist on shoots having a fairly large diameter[541], have a single median vein and two stomatal grooves on the lower surface[542] ([fig. 200], D).
Partially decorticated and younger shoots are characterised by the occurrence of pairs of elliptical parichnos areas and a smaller median leaf-trace scar. The surface of older stems, which may show signs of longitudinal splitting (Syringodendron state), bears pairs of parichnos scars reaching a length of 2–2·5 cm. and a breadth of 10–13 mm. The regularity of the leaf-scar arrangement is interrupted at intervals by the occurrence of more or less regular verticils of scars marking the position of deciduous shoots. Grand’Eury[543] has figured cones which he believes to be those of this species, and Zeiller refers the large strobili, Sigillariostrobus major, to Sigillaria Brardi[544].
The subterranean axes were characterised by spirally disposed rootlet-scars like those of Stigmaria ficoides (figs. [204], [205]) and by a cortical surface with the features of Stigmaria rimosa Gold.[545]
The anatomy of the stele and leaves has already been described ([p. 219]). The stele of the Stigmarian portion of the plant consists of a band of centripetal primary xylem and a cylinder of centrifugally formed secondary wood with medullary rays containing vascular bundles passing out to the rootlets[546].
Sigillaria Brardi occurs not uncommonly in Permian rocks; it is recorded from France[547], Germany[548], Pennsylvania[549], and elsewhere. It is found in the Upper, Middle, and Lower Coal-Measures of England[550] and in Permo-Carboniferous strata in Africa[551] and Brazil[552].
CHAPTER XVII.
UNDERGROUND RHIZOMES AND ROOTS OF PALAEOZOIC LYCOPODIACEOUS PLANTS.
Stigmaria.
Stigmaria ficoides is the name given to cylindrical casts met with in Palaeozoic rocks, from the Devonian[553] to the Permian[554], characterised by a smooth or irregularly wrinkled surface bearing spirally disposed circular scars bounded by a raised rim and containing a small central pit. It is not uncommon to find evidence of a partial collapse of the substance of the plant as seen in [fig. 204]; this is doubtless the expression of a shrinkage of the middle cortical region, which was composed of a delicate and lacunar system of cells. There can be no reasonable doubt that Stigmaria grew in water or in swampy ground. Specimens are occasionally met with in which the cast terminates in a bluntly rounded apex; such are, perhaps, young branches which have not grown far from the base of the aerial stem from which they arose (cf. [fig. 207], B, C). Other examples occur, such as Goeppert[555] figured and Gresley[556] has more recently described, which are twisted and distorted as though obstacles had been encountered in the ground in which they grew.