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
There can be little doubt that the petrified shoots described by
Williamson[384] from the Calciferous Sandstone beds of Burntisland as
_Lepidodendron brevifolium_ are identical with specimens possessing
the external features of _L. Veltheimianum_. In 1872 Dawson expressed
the opinion that Williamson’s species should be referred to _L.
Veltheimianum_, and evidence subsequently obtained confirms this
view. The stele of this species is of the medullated type, differing
from that of _L. fuliginosum_ and _L. Harcourtii_ in the absence of
prominent ridges on the external surface of the primary xylem, and from
_L. vasculare_ in the possession of a parenchymatous pith. In younger
twigs the cortex consists of fairly homogeneous tissue, but in older
branches there is a greater distinction between a delicate middle
cortex and a stronger outer cortex. Fig. 186, A, represents a stem
in which the vascular cylinder is composed of a primary xylem ring,
_x_, 1·5 mm. broad, succeeded by a zone of secondary wood 1·2 cm. in
breadth. The junction between the primary and secondary xylem is shown
on a larger scale in fig. 186, B. The tissues abutting on the secondary
xylem have not been preserved; the outer cortex, which consists
chiefly of secondary elements, is divided superficially into unequal
ridges corresponding to the leaf-cushions which have been more or less
obliterated as the result of growth in thickness of the stem.
9. _Lepidodendron Pedroanum_ (Carruthers).
In 1869 Mr Carruthers described some specimens of vegetative stems and
isolated sporangia, collected by Mr Plant in Brazil, as _Flemingites
Pedroanus_[385]. From a more recent account published by Zeiller[386]
it is clear that Carruthers’ species is a true _Lepidodendron_; an
examination of the type-specimens in the British Museum confirms this
determination. The contiguous leaf-cushions have rounded angles similar
in form to those of _Lepidodendron Veltheimianum_ and _L. dichotomum_,
but it is not unlikely that the Brazilian plant is specifically
distinct from European species. A figure of one of the specimens on
which Carruthers founded the species is given by Arber[387] in his
_Glossopteris Flora_. The Brazilian plant is chiefly interesting as
affording proof of the existence of _Lepidodendron_ in the southern
hemisphere; the species has also been recognised in South Africa from
material collected by Mr Leslie at Vereeniging[388].
As Zeiller[389] has suggested, it is not improbable that the fossils
described by Renault[390] from Brazil as _Lycopodiopsis Derbyi_ may be
the petrified stems of _Lepidodendron Pedroanum_. The structure of the
central cylinder of Renault’s species is of the type represented by _L.
Harcourtii_; the xylem forms a continuous ring and does not consist of
separate strands of tracheae as Renault believed.
10. _Lepidodendron australe_ (M’Coy). Figs. 187, A–C.
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