Links With the Past in the Plant WorldSeward, A. C. (Albert Charles)
Science
Links With the Past in the Plant World
Seward, A. C. (Albert Charles)
Paleobotany -- Great Britain; Plants -- Great Britain
It is only in the minority of cases that the accidents of preservation
of fragments of ancient floras have given us the means of investigating
the internal structure of the plant organs. It is far more frequently
the case that fossil plants are represented only by a carbonised film
on the surface of a piece of shale or other rock: the actual substance
of the plant has been converted into a thin layer of coal, and though
the venation and other surface-features may be clearly revealed, the
internal tissues have been destroyed. If a lump of clay containing a
piece of fern frond is heated, the result is an impression of the leaf
on the hardened matrix and a coaly substance in place of the plant
substance. It is occasionally possible by detaching a piece of the
black film from a fossil, and heating it with nitric acid and chlorate
of potash and then dipping it in ammonia, to obtain a transparent
preparation suitable for microscopical examination of the cell-outlines
of the superficial layer of the leaf or other plant-fragment. This
method of examination, used by several students of fossil plants and
with conspicuous success by Professor Nathorst of Stockholm, often
affords valuable aids to identification.
[Illustration: Fig. 7. Flood-plain of the delta of Rio Colorado. The
hills in the background are 25 miles distant. (From a photograph by
Prof. MacDougal.)]
Pieces of plants embedded in sandy sediment, if not preserved by
petrifaction, that is by the introduction into the tissues of some
siliceous or calcareous solution, gradually decay and their fragmentary
remains may be washed away by percolating water, leaving a hollow mould
in the gradually hardening sediment, which is afterwards filled with
sand or other material. The plant itself is destroyed, but a cast is
taken which in the case of fine-grained sediments reproduces the form
and surface-pattern of the original specimen. The incrustation of
plants by the falsely named petrifying springs of Knaresborough and
other places illustrate another method of fossilisation.
[Illustration: Fig. 8. Flower of _Cinnamomum prototypum_ Conw.
preserved in amber. × 10. (After Conwentz.)]
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