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
The fossil represented in fig. 1 (p. 10), from the collection of Dr
John Woodward, affords a good example of a well-defined impression.
The surface of the specimen, of which a cast is represented in fig. 1,
shows very clearly the characteristic leaf-cushions and leaf-scars
of a _Lepidodendron_. The stem was embedded in soft sand, and as the
latter became hard and set, an impression was obtained of the external
markings of the _Lepidodendron_. Decay subsequently removed the
substance of the plant.
[Illustration: FIG. 11. _Equisetites columnaris_ Brongn. From a
specimen in the Woodwardian Museum, Cambridge. ⅓ nat. size.]
In fig. 11 some upright stems of a fossil Horse-tail (_Equisetites
columnaris_) from the Lower Oolite rocks near Scarborough, are seen in
a vertical position in sandstone. On the surface of the fossils there
is a thin film of carbonaceous matter, which is all that remains of the
original plant substance; the stems were probably floated into their
present position and embedded vertically in an arenaceous matrix. The
hollow pith-cavity was filled with sand, and as the tissues decayed
they became in part converted into a thin coaly layer. The vertical
position of such stems as those in fig. 11 naturally suggests their
preservation _in situ_, but in this as in many other cases the erect
manner of occurrence is due to the settling down of the drifted plants
in this particular position.
[Sidenote: FOSSIL CASTS.]
An example of _Stigmaria_ drawn in fig. 12 further illustrates the
formation of casts[97]. The outer surface with the characteristic
spirally arranged circular depressions, represents the wrinkled bark of
the dried plant; the smaller cylinder, on the left side of the upper
end (fig. 12, 2, _p_) marks the position of the pith surrounded by the
secondary wood, which has been displaced from its axial position. The
pith decayed first, and the space was filled in with mud; somewhat
later the wood and cortex were partially destroyed, and the rod of
material which had been introduced into the pith-cavity dropped towards
one side of the decaying shell of bark.
[Illustration: FIG. 12. _Stigmaria ficoides_ Brongn. 1. Side view,
showing wrinkled surface and the scars of appendages. 2. End view
(upper) showing the displaced central cylinder; _p_, pith, _x_,
xylem, _r_, medullary rays. 3. End view (lower). From a specimen in
the Woodwardian Museum. ½ nat. size.]
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