Ancient Plants: Being a Simple Account of the past Vegetation of the Earth and of the Recent Important Discoveries Made in This Realm of NatureStopes, Marie Carmichael
Science
Ancient Plants: Being a Simple Account of the past Vegetation of the Earth and of the Recent Important Discoveries Made in This Realm of Nature
Stopes, Marie Carmichael
Paleobotany
The markings left on the well-preserved leaf-scars indicate the main
features of the internal anatomy of the leaves. They had a single central
vascular strand (_v_, fig. 93), on either side of which ran a strand of
soft tissue _p_ called the parichnos, which is characteristic of the
plants of this group. While another similarly obscure structure
associated with the leaf is the little scale-like ligule _l_ on its upper
surface.
The anatomy of the stems is interesting, for in the different species
different stages of advance are to be found, from the simple solid
protostele with a uniform mass of wood to hollow ring steles with a pith.
An interesting intermediate stage between these two is found in
_Lepidodendron selaginoides_ (see fig. 95), where the central cells of
the wood are not true water-conducting cells, but short irregular
water-storage tracheides (see p. 56), which are mixed with parenchyma.
All the genera of these fossils have a single central stele, round which
it is usual to find a zone of secondary wood of greater or less extent
according to the age of the plant.
[Illustration: Fig. 95.—Transverse Section of _Lepidodendron
selaginoides_, showing the circular mass of primary wood, the central
cells of which are irregular water-storage tracheides
_s_, Zone of secondary wood; _c_, inner cortical tissues; _r_,
intrusive burrowing rootlet; _oc_, outer cortical tissues with corky
external layers _k_. (Microphoto.)]
Some stems instead of this compact central stele have a ring of wood with
an extensive pith. Such a type is illustrated in fig. 96, which shows but
a part of the circle of wood, and the zone of the secondary wood outside
it, which greatly exceeds the primary mass in thickness. This zone of
secondary wood became very extensive in old stems, for, as will be
imagined, the primary wood was not sufficient to supply the large trunks.
The method of its development from a normal cambium in radiating rows of
uniform tracheides is quite similar to that which is found in the pines
to-day. This is the most important difference between the living and the
fossil stems of the family, for no living plants of the family have such
secondary wood. On the other hand, the individual elements of this wood
are different from those of the higher families hitherto considered, and
have narrow slit-like pits separated by bands of thickening on the
longitudinal walls. Such tracheides are found commonly in the
Pteridophytes, both living and fossil. Their type is seen in fig. 96, B,
which should be compared with that in figs. 78, A and 62, B to see the
contrast with the higher groups.
[Illustration: Fig. 96.—A, _Lepidodendron_ Stem with Hollow Ring of
Wood W and Zone of Secondary Wood S. B, Longitudinal View of the Narrow
Pits of the Wood Elements.]
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