The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
This is the characteristic species of the Lower Carboniferous
coal-measures, occurring in great profusion at Horton Bluff and its
vicinity, also at Sneid's Mills near Windsor, Noel and Five-Mile River,
at Norton Creek and elsewhere in New Brunswick (Matthew's collection),
and at Antigonish (Honeyman's collection).
I have received from the lowest Carboniferous beds of Ohio specimens
of this species.[CZ] According to Rogers and Lesquereux similar forms
occur in the Vespertine of Pennsylvania and in the Lower Carboniferous
of Illinois. _L. Veltheimianum_ of western Europe and _L. glincanum_ of
Russia are closely allied Lower Carboniferous species.[DA]
[CZ] "Journal of Geological Society," November, 1862, p. 313.
[DA] For comparisons of these see "Report on Plants of Lower
Carboniferous of Canada," p. 21.
A very different type is furnished by a new species from the middle
coal-formation of Clifton, New Brunswick.
Lepidodendron Cliftonense, Dawson.--Habit of Growth.--Robust, with thick
branches, and leaves several inches in length. Terminal branches becoming
slender, with shorter leaves.
_Markings of Stem._--Leaf-bases long oval, pointed at ends, enlarging
with growth of stem. Leaf-scars central, rhombic, transverse.
_Leaves._--One-nerved, acutely pointed, from four inches in length on the
larger branches to one inch or less on the branchlets.
_Fructification._--Cones large, cylindrical or long oval, with large
scales of trigonal form, and not elongated but lying close to the
surface. Borne on lateral, slender branchlets, with short leaves.
_Genus_ Lepidophloios, Sternberg; Ulodendron, L. and H.; Lomatophloios,
Corda.
_Lepidophloios._--Under this generic name, established by Sternberg,
I include those lycopodiaceous trees of the coal-measures which have
thick branches, transversely elongated leaf-scars, each with three
vascular points and placed on elevated or scale-like protuberances,
long one-nerved leaves, and large lateral strobiles in vertical rows or
spirally disposed. Their structure resembles that of _Lepidodendron_,
consisting of a _Sternbergia_ pith, a slender axis of large scalariform
vessels, giving off from its surface bundles of smaller vessels to the
leaves, a very thick cellular bark, and a thin dense outer bark, having
some elongated cells or bast-tissue on its inner side. In these trees the
exogenous outer cylinder is less developed than in the Lepidodendra, and
is sometimes wanting in stems or branches of some thickness.
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