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
Arborescent plants reaching a height of several meters, and having a
diameter of proportional size. In habit of growth the Calamites bore
a close resemblance to _Equisetum_; an underground rhizome giving off
lateral branches and erect aerial shoots bearing branches, either in
whorls from regularly recurring branch-bearing nodes, or two or three
from each node; and in some cases the stems bore occasional branches
from widely separated nodes. The leaves were disposed in whorls either
as star-shaped verticils on slender foliage shoots, or in the form
of a circle of long narrow leaves on the node of a thicker branch.
Adventitious roots were developed from the nodal regions of underground
and aerial stems. The cones had the form of long and narrow strobili
consisting of a central axis bearing whorls of sterile and fertile
appendages; the latter in the form of sporangiophores bearing groups of
sporangia. The strobili were heterosporous in some cases, isosporous
in others. The stems had a large hollow pith bridged across by a
transverse diaphragm at the nodes in the centre of the single stele;
the latter consisted of a ring of collateral bundles separated from one
another by primary medullary rays. Each group of xylem was composed of
spiral, annular, scalariform and occasionally reticulate tracheids,
the position of the protoxylem being marked by a longitudinal
carinal canal. The shoots and roots grew in thickness by means of a
regular cambium layer. The cortex consisted of parenchymatous and
sclerenchymatous cells, with scattered secretory sacs. The increase in
girth of the central cylinder was often accompanied by a considerable
development of cortical periderm. The roots differed from the shoots
in having no carinal canals, and in the possession of a solid pith and
centripetally developed primary xylem groups alternating with strands
of phloem.
The above incomplete diagnosis includes only some of the more important
structural features of the genus. Thanks to the researches begun by the
late Mr Binney of Manchester and considerably extended by Carruthers,
Williamson and later investigators, we are now in a position to give
a fairly complete account of _Calamites_. The type of stem most
frequently met with in a petrified condition in the English rocks is
that to which Göppert applied the name _Arthropitys_, and it is this
subgenus that forms the subject of the following description. Our
knowledge of Calamitean anatomy is based on the examination of numerous
fragments of petrified twigs and other portions of different specific
types of the genus. It is seldom possible to differentiate specifically
between the isolated fragments of stems and branches which are met
with in calcareous or siliceous nodules. As so frequently happens in
fossil-plant material, large specimens showing good surface features
and broken fragments with well-preserved internal structure have to be
dealt with separately.
[Sidenote: YOUNG STEM.]
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