Fossil plants, Vol. 2 : $b A text-book for students of botany and geologySeward, A. C. (Albert Charles)
Science
Fossil plants, Vol. 2 : $b A text-book for students of botany and geology
Seward, A. C. (Albert Charles)
Paleobotany
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.
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