The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
The ligneous cylinder is surrounded by a band of cellular tissue, and
the space between this and the cortical integument is occupied by
silex, in which there are but obscure traces of structure.
The inner layer of bark, _f_, is composed of elongated cells, disposed
in a radiating manner, and traversed by fibro-vascular bundles, which
pass towards the leaves.
Upon instituting a comparison between the fossil and the stems of those
recent plants which present the closest analogy to it, M. Brongniart
was led to conclude that the Sigillariæ constituted a peculiar extinct
family, belonging to the great division of gymnospermous dicotyledons.
The Sigillariæ were tall erect trees, with a regular and cylindrical
stem, without side branches, but dichotomous towards the summit. Their
superficial bark was hard and durable, channelled longitudinally,
bearing leaf-scars that are of a rounded form above and below, and
angular at the sides, often oblong in relation to the stem, and having
three vascular pits, one central and small, and two lateral of a
larger size. The internal structure bears most analogy to that of the
Cycadeæ, and the foliage consisted of long linear carinated leaves.
The Sigillariæ, therefore, differ essentially from the arborescent
cryptogamia, which they somewhat approach in having scalariform
vascular tissue, symmetrical and regular leaf-scars, and branchless
trunks. More than fifty species have been determined.[102]
[102] For figures of Sigillariæ, see Pictorial Atlas, pl. xix. xx, xxiv.
[Sidenote: STIGMARIA.]
Stigmaria. _Lign. 36._--This extended notice of the structure of the
Sigillariæ,.will enable us to understand the nature of the fossil
vegetables termed Stigmariæ, or spotted-stems, which abound in the
beds of under-clay of most coal-fields, as stated in a former part
of this work (_ante_, p. 81). These bodies when uncompressed are of
a cylindrical form, from one to six or seven inches in diameter,
and of considerable length--sometimes upwards of twenty feet--and
gradually diminish in size towards their termination. The surface is
marked with distinct pits or areolæ, of a circular or oval form, with
a small tubercle in the centre of each, disposed around the stem in
a quincunx and somewhat regular order. When broken transversely, a
small cylindrical axis is seen to extend in a longitudinal direction
through the stem, like a medullary column; it seldom occupies the
centre, but lies near to one side, and parallel with a depression on
the outer surface of the fossil. This internal body is often loose,
and removable; its surface is covered with interrupted, irregular,
longitudinal, ridges, which leave corresponding depressions on the
walls of the cavity in which it was inclosed. _Lign. 36_, represents a
fragment exhibiting the characters above described.
[Illustration: Lign. 36. Stigmaria ficoides.
_Carboniferous. Derbyshire._--1/4 _nat._
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