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
A. _Calamitina._ B. _Stylocalamites._ C. _Eucalamites._
Palaeobotanical literature contains a large number of species of
_Calamites_ founded on pith-casts alone. Many of these so-called
species are of little or no value botanically, but while we may admit
the futility of attempting to recognise specific types in the same
sense as in the determination of recent plants, it is necessary to
pay attention to such characters as are likely to prove of value for
descriptive and comparative purposes. From the nature of the specimens
it is clear that many of the differences may be such as are likely to
be met with in different branches of the same species, while in others
the pith-casts of distinct species or genera may be almost identical.
The most striking differences observable in Calamite casts are in the
character of the internodes, the infranodal canals, the number and
disposition of branch-scars, and other surface features. Occasionally
it is possible to recognise certain anatomical characters in the coaly
layer which often surrounds a shale- or sandstone-cast, and the surface
of a well preserved cast may give a clue to the nature of the wood in
the faint outlines of cells which can sometimes be detected on the cast
itself[753]. The breadth of the carbonaceous envelope on a cast has
been frequently relied on by some writers as an important character. It
has been suggested[754] that we may arrive at the original thickness
of the wood of a stem by measuring the coaly layer and multiplying
the breadth by 27; the explanation being that a zone of wood 27 mm. in
thickness is reduced in the process of carbonisation to a layer 1 mm.
thick.
The breadth of the coal on the same form of cast may vary considerably;
on this account, and for various other reasons, such a character can
have but little value. Our knowledge of anatomy may often help us
to interpret certain features of internal casts and to appreciate
apparently unimportant details. One occasionally notices that a
Calamite pith-cast has large infranodal canals, and in some specimens
each internodal ridge may be traversed by a narrow median line or small
groove; large infranodal canal casts suggest the type of stem referred
to the subgenus _Arthrodendron_, and the median line on the ridges may
be due to bands of hard tissue in each principal medullary ray.
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