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
If it consist of parallel tubes, and has neither pith, nor rays
passing from the centre to the circumference, the tree or plant was
_endogenous_, like the Palm. If any trace be present of tissue crossing
the longitudinal tubes at right angles, and radiating from the centre
to the circumference, this will prove the existence of medullary rays,
and the original must have been _exogenous_, as the Oak, Elm, &c.: and
if in a transverse section the tubes appear of equal size, the tree was
probably _coniferous_, or _cycadeous_ (_i.e._ related to the plants
called _Cycas_ and _Zamia_); but if larger tubes appear among the
smaller ones, disposed in a definite manner (see _Plate V. fig. 4_),
it belonged to some other tribe of exogenous plants.
If the walls of the tubes be studded with glands (_Lign. 1, fig. 1,
c_; _Plate V. figs. 2^b 3^b_.); the fossil belongs to the Coniferæ.
If any vestige of a central pith be discovered, the exogenous nature of
the original is undoubted, for no other class, as we previously stated,
possesses a central cellular column.
The absence or presence of a true cortical investment, or bark, is
important, for a distinct bark is the characteristic of the _exogenous_
class:[42] a cortical integument, or rind, not separable from the
enclosed structure, indicates the _monocotyledons_; and the entire
absence of any rind, the _cryptogamia_.
[42] An apparent exception to this rule is found in the fossil genus
Clathraria, described hereafter, which has a distinct hollow cortical
cylinder, that separates from the internal axis: this is not true bark,
but is formed by the consolidation of the bases of the petioles or
leaf-stalks; see _Lign. 54_.
The markings on the stems, occasioned by the scars or cicatrices left
by the separation of the petioles or leaf-stalks (as on the stalk of a
cabbage), afford important evidence, since they are commonly present,
even when the cylindrical trunk is compressed into a flat thin layer of
coal; as we shall often have occasion to remark. In this place it need
only be stated, that by these scars may be detected the position of the
leaves, and the form of the bases of the petioles or leaf-stalks; their
probable direction, whether they were opposite, alternate, verticillate
or spirally disposed, deciduous or persistent, imbricated or remote.
Even when no traces of the leaves remain, the origin of the branches,
and their bifurcation, may perhaps be determinable.
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