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
Specimens described under this name are interesting rather on account
of their extended geographical range and geological antiquity than
on botanical grounds. The drawings reproduced in fig. 187 illustrate
the characteristic appearance of this Lower Carboniferous and Upper
Devonian type, as represented by a specimen recently described[391]
from the Lower Karroo (Dwyka) series, which is probably of
Carboniferous age, near Orange River Station, South Africa. The surface
is divided into polygonal or rhomboidal areas (figs. A and B) 8–9 mm.
long and 7–8 mm. broad, arranged in regular series and representing
leaf-scars, comparable with those of _Sigillaria Brardi_ and other
species, or possibly partially decorticated leaf-cushions. A short
distance below the apex of each area there is a more or less circular
prominence or depression (fig. 187, B) and on a few of the areas there
are indications of a groove (fig. A, _g_) extending from the raised
scar to the pointed base, as at _g_, _g_.
[Illustration: FIG. 187. _Lepidodendron australe._ Fig. A, nat. size.]
In examining the graphitic layer on the surface of the South African
specimen shown in fig. 187, A, use was made of a method recently
described by Professor Nathorst[392]. A few drops of collodion were
placed on the surface, and after a short interval the film was removed
and mounted on a slide. The addition of a stain facilitated the
microscopic examination and the drawing of the collodion film. The
cell-outlines (fig. 187, C) on the surface of the polygonal areas
may be those of the epidermis, but they were more probably formed by
a subepidermal tissue; the scar, which interrupts the continuity of
the flat surface, may mark the position of a leaf-base, or, assuming
a partial decortication to have occurred prior to fossilisation, it
may represent a gap in the cortical tissue caused by the decay of
delicate tissue which surrounded the vascular bundle of each leaf in
its course through the cortex of the stem. If the impression were
that of the actual surface of a _Lepidodendron_ or a _Sigillaria_,
we should expect to find traces of the parichnos appearing on the
leaf-scar as two small scars, one on each side of the leaf-bundle.
In specimens from Vereeniging described in 1897[393] as _Sigillaria
Brardi_, which bear a superficial resemblance to that shown in fig. A,
the parichnos is clearly shown. On the other hand, an impression of a
partially decorticated Lepidodendroid stem need not necessarily show
the parichnos as a distinct feature: owing to its close association
with the leaf-trace in the outer cortex, before its separation in the
form of two diverging arms, it would not appear as a distinct gap apart
from that representing the leaf-bundle. The absence of the parichnos
may be regarded as a point in favour of the view that the impression
is that of a partially decorticated stem. Similarly, the absence of
any demarcation between a leaf-cushion and a true leaf-scar such as
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