The Story of a Boulder; or, Gleanings from the Note-book of a Field Geologist — John Shaqi
The Story of a Boulder; or, Gleanings from the Note-book of a Field GeologistGeikie, Archibald
Science
The Story of a Boulder; or, Gleanings from the Note-book of a Field Geologist
Geikie, Archibald
Geology; Petrology
Another remarkable feature in this carboniferous plant is that it
appears to have had no branches along its stem. Trunks have been found
four and five feet in diameter, and have been traced to a distance of
fifty, sixty, and even seventy feet, without any marks of branches
being detected. Brongniart examined the portion of one stem, which,
at its thicker end, had been broken across, but still measured a
foot in breadth. It ran for forty feet along the gallery of a mine,
narrowing to a width of not more than six inches, when it divided into
two, each branch measuring about four inches across. The sigillaria
stems, accordingly, must have shot up, slim and straight, to a height
of sometimes seventy feet before they threw out a single branch. We
know nothing of the coronal of these strangely-formed trees. From
Brongniart's observations, it would seem that the upper part of the
stem, like that of the lepidodendron, was dichotomous, that is, it
branched out into two minor stems; but how these were disposed is
unknown. We are wholly ignorant, too, of the foliage of these branches,
though, from the general structure of the plant, as well as from the
number of fern-fronds often found around the base of the stems, it has
been conjectured that the sigillaria was cryptogamous, and, like the
tree-ferns, supported a group of sweeping fronds. If so, it differed in
many respects from every known member of the cryptogamic tribes.
Putting together, then, all that we know of the exterior of the
sigillaria, we find that it was a tall slender tree, with, palm-like,
a clump of foliaged branches above, its stem bristling thickly, in at
least its upper part, with spiky leaves, and its roots equally hirsute,
shooting out to a distance of sometimes forty feet through the soft
muddy soil. Future researches may bring us better acquainted with this
ancient organism. In the meanwhile, enough of it is known to mark it
out as one of the most ornate forms of vegetation that the world has
ever seen.
In addition to the above, the coal strata have yielded many other
fragmentary remains, to which names have been given, but of which very
little is known. It is pleasant, amid such a wide sea of doubt and
uncertainty, to alight upon some well-known form of whose affinities
there can be no question, since it still finds its representatives in
living nature. Of such a kind are the coniferous stems occasionally met
with in the sandstones of the coal-measures. .
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