Fossil plants, Vol. 2 : $b A text-book for students of botany and geologySeward, A. C. (Albert Charles)
Science
Fossil plants, Vol. 2 : $b A text-book for students of botany and geology
Seward, A. C. (Albert Charles)
Paleobotany
In 1842 Hawkshaw[577] described certain fossil trees, the largest of
which had a circumference at the base of 15 ft., discovered, in the
course of excavations for a railway in Lancashire, in soft shale at
right angles to the bedding. The surface features were not sufficiently
clear to enable him to decide with certainty between _Sigillaria_ and
_Lepidodendron_, but while inclining to the former, it is interesting
to note that the occurrence of numerous Lepidostrobi near the root led
him to recognise the possibility of a connexion between the Stigmarian
roots and Lepidodendron stems. In 1846 Binney gave an account of
similar trees found at Dukinfield near Manchester: he spoke of one
stem as unquestionably a _Sigillaria_ with vertical ribs, furrows, and
scars, about 15 inches high and 4 ft. 10 inches in circumference. He
expressed his conviction that “_Sigillaria_ was a plant of an aquatic
nature[578].” Similar descriptions of rooted stems in the Coal-Measures
of Nova Scotia were published by Brown in 1845, 1846 and 1849; in the
last paper he figured a specimen, which has become famous, showing a
Syringodendron stem terminating in branching Stigmarian (or possibly
Stigmariopsis) roots bearing on the lower surface a series of what he
called conical tap roots[579]. A similar specimen discovered in Central
France nearly fifty years later demonstrated the accuracy of Brown’s
description.
Despite these discoveries the root-like nature of _Stigmaria_ was
not universally accepted. It was, however, generally agreed that
_Stigmaria_ formed the roots of _Sigillaria_; it was, moreover, held by
some that _Lepidodendron_ stems also possessed this type of root, an
opinion based on Brown’s record and on the occurrence of _Stigmaria_ in
beds containing _Lepidodendron_ but no _Sigillaria_ stems, as in the
volcanic beds of Arran and elsewhere, and on observations of Geinitz
and others[580]. There is now general agreement that _Lepidodendron_
and _Sigillaria_ had the same type of “root,” though the connexion of
_Stigmaria_ with the former was not so readily admitted, and indeed
the evidence in support of it is still very meagre. Goeppert and
other authors were unable to believe that the numerous species of
_Sigillaria_ possessed roots of so uniform a type, but Goeppert, by his
recognition of several varieties of _Stigmaria_, supplied a partial
answer to this objection.
Public-domain text, read in full here on John Shaqi.
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