Fossil plants, Vol. 3 : $b A text-book for students of botany and geology — John Shaqi
Fossil plants, Vol. 3 : $b A text-book for students of botany and geologySeward, A. C. (Albert Charles)
Science
Fossil plants, Vol. 3 : $b A text-book for students of botany and geology
Seward, A. C. (Albert Charles)
Paleobotany
It occasionally happens that a meristematic layer is formed in the
parenchymatous tissue immediately internal to some of the perimedullary
xylem strands of a _Lyginopteris_ stem from which either secondary
parenchyma is produced or a zone of secondary xylem and phloem, the
phloem facing the centre of the pith. An example of such internal
xylem was figured by Williamson[109] and similar occurrences are
more fully dealt with by Williamson and Scott[110] who consider that
the perimedullary cambium may represent an internal extension through
a leaf-gap of the normal cambial cylinder. In the stem represented
in fig. 403 there are two perimedullary xylem strands to the left
of the bottom of the V-shaped gap in the secondary xylem-cylinder,
_r_, and on the inner face of one of these, as shown in fig. 405, C,
there is a narrow arc of internal secondary xylem, _c_, between the
xylem-strand and the outer edge of one of the sclerous nests. The
sporadic occurrence of arcs of inversely orientated secondary vascular
tissue affords an interesting parallel with a similar morphological
feature in some recent Dicotyledonous genera such as _Tecoma_ and
_Iodes_. As Williamson and Scott point out, this similarity affords ‘a
striking warning against the _indiscriminate_ use of even conspicuous
anatomical characters[111].’ While admitting the necessity of guarding
against the danger of attaching importance to occasional and abnormal
characters they may have some significance as collateral evidence in
comparisons of different types of stems. It is conceivable that these
anomalous arcs of secondary tissue on the inner side of the primary
xylem strands may, as Worsdell[112] maintains, be reversions to an
ancestral character and in this sense comparable with the strands of
inverted vascular tissue in some recent Cycadean stems. The question of
relationship of _Lyginopteris_ and allied types to recent Cycads and
the Palaeozoic Medulloseae is considered in a later chapter.
In 1902 Lomax[113] described two branching specimens of _Lyginopteris_,
and more recently two others have been discovered at a locality
near Bacup in Lancashire which have been thoroughly investigated by
Miss Brenchley[114] who constructed models from drawings of serial
sections[115]. One specimen shows six leaf-bases in a length of 4¾
inches and branches spring from the axils of five of them: some of
the branches show secondary ramifications. The phyllotaxis of the
leaf-bases on a branch is always the reverse of that on the main stem,
a divergence to which no parallel was found in a selection of trees
and shrubs examined by Miss Brenchley. The secondary wood of the stem
swells below the point of exit of a branch and frequently a fairly
large amount of wood occurs in the pith when a branch is given off:
this anomalous wood may help to close the branch-gap.
ii. _Leaf_.
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