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 long and narrow cones referred to _Bothrodendron minutifolium_ from
English and French Coal-Measures are known only as impressions and it
is not possible to say whether they were heterosporous or homosporous;
the drawing given by Zeiller (Fig. 212, E) shows that the sporangia
were of the same form as those in _Lepidostrobus_, but we have no
more exact information as to their morphology. A recently published
description of a petrified strobilus by Mr Watson affords a welcome
addition to our knowledge. There is little doubt that this cone was
borne by a species of _Bothrodendron_; the evidence for this conclusion
is supplied by the agreement of the anatomical characters of the stele
with that of the vegetative shoots originally described by Williamson
as _Lepidodendron mundum_ and by the constant association of the cones
and vegetative shoots. In 1880 Williamson described a crushed cone
containing both megaspores and microspores which he spoke of as “a
diminutive organism, reminding us more of the dwarfed fruits of many
living Selaginellas than of the large _Lepidostrobi_[647].” Watson’s
specimens enable us to give a more complete account of this type. The
axis of the strobilus bears short sporophylls bent upwards into a
distal limb with a conspicuous ligule in a deep pit beyond the shortly
stalked sporangium. The length of the strobilus is estimated at 10 mm.;
the stele is of the same type as that of _Bothrodendron mundum_, but
it differs from the specimens of the vegetative shoots so far found
in having some secondary xylem. As shown in the sketch reproduced in
fig. 216 each sporophyll is characterised by two tangentially placed
grooves, _g_, on the lower face, and by numerous transfusion tracheids,
_tr_, above the vascular bundle, _vb_, immediately below the ligule,
_l_. Megasporangia and microsporangia occur on the same cone, the
megasporangia being on the lower sporophylls and containing a single
tetrad of megaspores. Fig. 219, E, shows a radial longitudinal section
of a microsporophyll bearing a sporangium on the adaxial side of the
ligule, _l_, below which is the single vascular bundle and a group of
short tracheids at _t_. The sporangia closely resemble those of species
of _Selaginella_ and _Lycopodium_ and, as pointed out by Watson[648],
they also recall the sporangia of the Palaeozoic genus _Spencerites_.
_Bothrostrobus_ is distinguished from _Spencerites_ by the presence
of a ligule, by the structure of the axis, and by the different
form of the sporophylls. The occurrence of four spores only in the
megasporangia is another character in which the extinct type resembles
recent Lycopods. It is impossible to decide whether Watson’s cone
represents a more or a less primitive type than _Lepidostrobus_: if we
accept Professor Bower’s views in regard to the evolution of vegetative
organs by the sterilisation of sporogenous tissue, we should probably
place _Lepidostrobus_ lower in the series than _Bothrostrobus_; but
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