Fossil plants, Vol. 2 : $b A text-book for students of botany and geologySeward, A. C. (Albert Charles)
Science
Fossil plants, Vol. 2 : $b A text-book for students of botany and geology
Seward, A. C. (Albert Charles)
Paleobotany
=Stigmaria.=
_Stigmaria ficoides_ is the name given to cylindrical casts met with
in Palaeozoic rocks, from the Devonian[553] to the Permian[554],
characterised by a smooth or irregularly wrinkled surface bearing
spirally disposed circular scars bounded by a raised rim and containing
a small central pit. It is not uncommon to find evidence of a partial
collapse of the substance of the plant as seen in fig. 204; this
is doubtless the expression of a shrinkage of the middle cortical
region, which was composed of a delicate and lacunar system of cells.
There can be no reasonable doubt that Stigmaria grew in water or
in swampy ground. Specimens are occasionally met with in which the
cast terminates in a bluntly rounded apex; such are, perhaps, young
branches which have not grown far from the base of the aerial stem
from which they arose (cf. fig. 207, B, C). Other examples occur,
such as Goeppert[555] figured and Gresley[556] has more recently
described, which are twisted and distorted as though obstacles had been
encountered in the ground in which they grew.
[Illustration: FIG. 204. _Stigmaria ficoides_ Brongn. M.S. (See Vol. I.
p. 73.)]
[Illustration: FIG. 205. _Stigmaria ficoides._ From a specimen in the
York Museum, from Bishop Auckland. _a_, base of rootlet showing
vascular bundle scar. M.S.]
The circular scars mark the bases of long single and occasionally
forked appendages (rootlets) which spread on all sides into the
surrounding medium (figs. 205, 208). The occurrence of rootlets
radiating through the shale or sandstone affords proof that the
Stigmarias are often preserved in their position of growth. This
was recognised by Steinhauer[557] and Logan[558], and has been more
recently emphasised by Potonié[559] as an argument in favour of the
view that the beds containing such specimens are old surface-soils.
_Stigmaria_ usually shows regular dichotomous branching, the arms
spreading horizontally or slightly downwards and always arising
from four main branches in the form of a cross (fig. 207). The most
remarkable specimens found in England are described by Williamson[560]
in his monograph of _Stigmaria_. One of two large casts found near
Bradford in Yorkshire, and now in the Manchester Museum, shows four
large primary arms radiating from the base of an erect stump 4 feet in
diameter. Each arm divides a short distance from its base into two, and
the smaller branches extend almost horizontally for several feet[561].
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