Fossil plants, Vol. 1 : $b [A text-book] for students of botany and geologySeward, A. C. (Albert Charles)
Science
Fossil plants, Vol. 1 : $b [A text-book] for students of botany and geology
Seward, A. C. (Albert Charles)
Paleobotany
_Palaeostachya vera_ sp. nov. Fig. 98.
In 1869 Williamson[714] described a fragment of a strobilus which
showed certain anatomical features indicative of a close relationship
or even identity with _Calamites_. Some years later[715] a much more
perfect example was obtained from the Coal-Measures of Lancashire,
and the additional evidence which it afforded definitely confirmed
the earlier views of Williamson. The cone was more fully described by
Williamson in 1888, as “the true fruit of _Calamites_.” It is clearly a
form of Weiss’ genus _Palaeostachya_; Williamson and Scott[716] refer
to it in their Memoir as _Calamites pedunculatus_. It is preferable,
however, to retain the generic designation _Palaeostachya_ for cones
of this type. As the name _P. pedunculata_ has previously been adopted
by Weiss[717] for a cone figured by Williamson[718] in 1874, and
afterwards referred to by that author in writing as _P. pedunculata_,
it is proposed to substitute the specific name _vera_; this specific
name being chosen with a view to put on record the fact that it was
this type of cone that Williamson first proved to be the _true_
fructification of the Calamite.
The axis of _P. vera_ is practically identical in structure with a
Calamitean twig. There is a hollow pith in the centre of the stele
surrounded by a ring of 16–20 collateral bundles, each of which is
accompanied by a carinal canal as in a vegetative shoot. As the
pedicel of the strobilus passes into the cone proper it undergoes some
modification in structure, but retains the characteristic features of
a Calamite. The diagrammatic longitudinal section of fig. 98, which is
copied from a drawing by Williamson[719], shows the broadening of the
vascular strands at the nodes, and here and there a carinal canal is
seen internal to the wood.
The axis of the cone bears whorls of bracts at right angles to the
central column. Each whorl consists of about 30–40 segments coherent
basally into a disc of prosenchymatous and parenchymatous tissue.
The free linear bracts curve sharply upwards from the periphery of
the disc, approximately parallel to the axis of the cone. From each
of these sterile whorls there are given off 16–20 long and slender
obliquely-inclined sporangiophores, _sp_, which arise from the upper
surface of the disc close to the axis. Each sporangiophore no doubt
bore four sporangia, _S_, containing spores of one size,—about ·075
mm. in diameter. The specimens of _Palaeostachya vera_ so far obtained
do not show the actual manner of attachment of the sporangia, but more
complete examples of other species of _Palaeostachya_[720] enable us to
assume with certainty that the sporangiophores terminated in a distal
peltate expansion bearing four sporangia on its inner face.
[Illustration: FIG. 98. Diagrammatic longitudinal section of
_Palaeostachya vera_, sp. nov. _S_, _S_, _S_, sporangia; _x_,
xylem; _sp_, sporangiophore. (After Williamson.)]
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