The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
those of the stem.[AF] The horizontal or oblique flexures of the large
tubes seem to be mainly in the vicinity of the radial openings, and it is
in entering these that they have been seen to branch."
[AF] It is possible that these tubes may be merely part of the stem
attached to the bark, which seems to me to indicate the same dense
cellular structure seen in the bark of _Lepidodendra_, etc.
The conclusions arrived at by Prof. Penhallow are as follows:
"1. The plant was not truly exogenous, and the appearance of rings
is independent of the causes which determine the layers of growth in
exogenous plants.
"2. The plant was possessed of no true bark. Whatever cortical layer
was present was in all probability a modification of the general
structure,[AG]
[AG] On these points I would reserve the considerations: 1. That there
must have been some relation between the mode of growth of these great
stems and their concentric rings; and, 2. That the evidence of a bark is
as strong as in the case of any Palæozoic tree in which the bark is, as
usual, carbonised.
"3. An intimate relation exists between the large tubular cells and the
myceloid filaments, the latter being a system of small branches from
the former; the branching being determined chiefly in certain special
openings which simulate medullary rays.
"4. The specimens examined exhibit no evidence of special decay, and the
structure throughout is of a normal character.
"5. The primary structure consists of large tubular cells without
apparent terminations, and devoid of structural markings, with which is
associated a secondary structure of myceloid filaments arising from the
former.
"6. The structure of _Nematophyton_ as a whole is unique; at least there
is no plant of modern type with which it is comparable. Nevertheless, the
loose character of the entire structure; the interminable cells; their
interlacing; and, finally, their branching into a secondary series of
smaller filaments, point with considerable force to the true relationship
of the stem as being with Algæ or other Thallophytes rather than with
Grymnosperms. A more recent examination of a laminated resinous
substance found associated with the plant shows that it is wholly
amorphous, and, as indicated by distinct lines of flow, that it must
have been in a plastic state at a former period. The only evidence of
structure was found in certain well-defined mycelia, which may have been
derived from associated vegetable matter upon which they were growing,
and over which the plastic matrix flowed."
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