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 true external surface of the cortical investment is marked with
longitudinal striæ, without any indications of joints or constrictions;
but the position of the original articulations is indicated in some
specimens by the _presence of small verticillate scars, to which leaves
were appended_[78] as in the example figured by M. Brongniart, of which
_Lign. 14, fig. 1_, is a reduced figure.
[78] See Mr. Dawes, "On the Structure of Calamites," Proc. Geol. Soc,
1851, vol. vii. p. 197.
[Illustration: Lign. 15. Calamites, in Coal Shale.
Fig. 1.--Calamites radiatus, with the remains of one of the
sheaths.--1/2 _nat._
2.--Stem, with remains of roots.--1/2 _nat._
3.--Calamites approximatus, showing the curved lower end of the
plant.[79]--1/5 _nat._
]
[79] This specimen has been inadvertently drawn with the base uppermost.
The stellate appearance on the upper part of the stem figured in
_Lign. 15, fig. 1_, is produced by the zone of leaves which
surrounded the joint: this character is entirely distinct from the
sheath of the Equisetum shown in _Lign. 12_. This specimen points out
the importance of carefully examining and preserving the stone around
fossil stems; had this precaution been lost sight of in this instance,
no knowledge would have been obtained of this important botanical
character. It is rarely that any traces of the roots remain; the fossil
figured (_fig. 2_) is from the _Foss. Flor._ A beautiful example of the
foliage of a species of Calamites is represented in _Lign. 59, fig.
2_.
Upright stems of Calamites occur in the Coal formation near Pictou,
in North America; and in one example a group of ten or twelve stems,
covering an area of two square feet, sprung from one root.[80]
[80] Dawson, Geol. Proc. vol. vii. p. 195. See Sir C. Lyell's Travels
in North America, vol. ii. p. 195.
* * * * *
[Sidenote: FOSSIL FERNS.]
Filicites, or Ferns.
We now arrive at the consideration of one of the most interesting
families of the vascular cryptogamia that adorned the Flora of the
ancient world, and the living species of which impart beauty and
elegance to the scenery of the countries where they prevail. The most
essential character of these vegetables, is that of developing their
fructification on the leaves; a fact familiar to every one who has
even but cursorily examined the Polypody growing on our walls, or the
Brake of our hedge-rows and commons. The largest species of British
ferns scarcely exceed four or five feet in height; but the arborescent
or tree-ferns, of warm climates, attain an altitude of from thirty to
forty feet. There is too this peculiarity in the arborescent forms,
that while in our indigenous species the leaves surround the stem, and
incline towards the upper part of the plant, the foliage of the former
bends downwards, and spreads out from the crown, or summit, into an
elegant canopy.
[Illustration: Lign. 16. Pecopteris Sillimani; _nat._
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