A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."Mantell, Gideon Algernon
Science
A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."
Mantell, Gideon Algernon
Paleontology
Stems more or less flattened, with the external surface
longitudinally furrowed, and uniformly ornamented with rows of deeply
imprinted symmetrical figures, disposed with much regularity, are
among the most abundant vegetable remains in the coal formation.
These are named _Sigillariæ_, from the Latin word _sigillum_,
signifying a _seal_, in allusion to the extreme regularity of the
imprints on the surface. When found in an upright position, at right
angles to the plane of the stratum, the original cylindrical form
of the tree is commonly preserved; and many examples are now known
of groups of erect Sigillariæ, with their roots extending into the
surrounding clay or sandy loam; the roots proving to be the fossil
bodies called _Stigmariæ_, which were formerly supposed to be a
distinct family of aquatic plants.[16] The first discovery of this
highly interesting and unexpected fact was made by Mr. Binney.[17]
[Footnote 16: Dr. Buckland's Bridgewater Essay, vol. i. p. 476.]
[Footnote 17: See "Supplementary Notes, p. 198."]
The specimen figured was found in an erect position in the sandstone
of a quarry at Rowmarsh, near Rotherham in Yorkshire.
The stem is simple, the furrows small and wavy, impressed with dots
on the ridges. The cicatrices are ovate, subpentagonal, with the
lower angles rounded, having a single gland near the lower extremity.
The stem is three feet long, and four inches in diameter.
The transverse section, as seen in fig. 1, shows traces of a double
concentric ring, as if produced by internal structure. Fig. 2,
displays the equality of the stem throughout its entire length, and
its abrupt termination. In fig. 3, is seen the cicatrix with its
single gland, for the attachment of the petiole or leaf-stalk. Fig.
4, indicates the undulating line of the top of the ridge.
"The originals of these fossils are supposed by M. Ad. Brongniart to
have constituted a peculiar family of coniferous plants, now extinct,
which probably belonged to the great division of gymnospermous
dicotyledons. In their external forms they somewhat resembled the
Cacteæ or Euphorbiæ, but were more nearly related by their internal
organization to the Zamiæ or Cycadeæ. The leaves and fruits of these
trees are unknown, for no satisfactory connexion has been established
between the stems, and the foliage and seed vessels with which they
are sometimes collocated."[18]
[Footnote 18: Medals of Creation, vol. i. p. 138.]
[Illustration: Plate XX.]
PLATE XX.
"Sigillaria."
(_Euphorbites vulgaris_, of Artis.)
This species is characterized by the remarkable fish-like form of
the cicatrices left by the base of the leaf-stalks, and by the
rapid tapering of the upper part of the stem, as shown in the
reduced figure 1, which represents a specimen nine feet long, five
feet in circumference at the base, and only twenty-one inches in
circumference at the upper end.
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