The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
The oldest plants known to me, and likely to have been of higher grade
than Algæ, are specimens kindly presented to me by Dr. Alleyne Nicholson,
of Aberdeen, and which he had named _Buthotrephis Harknessii_[H] and _B.
radiata_. They are from the Skiddaw rocks of Cumberland. On examining
these specimens, and others subsequently collected in the same locality
by Dr. Gr. M. Dawson, while convinced by their form and carbonaceous
character that they are really plants, I am inclined to refer them not
to Algæ, but probably to Rhizocarps. They consist of slender branching
stems, with whorls of elongate and pointed leaves, resembling the genus
_Annularia_ of the coal formation. I am inclined to believe that both
of Nicholson's species are parts of one plant, and for this I have
proposed the generic name _Protannularia_ (Fig. 1). Somewhat higher in
the Siluro-Cambrian, in the Cincinnati group of America, Lesquereux
has found some minute radiated leaves, referred by him to the genus
_Sphenophyllum_,[I] which is also allied to Rhizocarps. Still more
remarkable is the discovery in the same beds of a stem with rhombic
areoles or leaf-bases, to which the name _Protostigma_ has been given.[J]
If a plant, this may have been allied to the club-mosses. This seems to
be all that we at present know of land-vegetation in the Siluro-Cambrian.
So far as the remains go, they indicate the presence of the families of
Rhizocarps and of Lycopods.
[H] "Geological Magazine," 1869.
[I] See figure in next chapter.
[J] _Protostigma sigillarioides_, Lesquereux.
[Illustration: Fig. 1.--_Protannularia Harknessii_ (Nicholson), a
probable Rhizocarp of the Ordovician period.]
If we ascend into the Upper Silurian, or Silurian proper, the evidences
of land vegetation somewhat increase. In 1859 I described, in "The
Journal of the Geological Society" of London, a remarkable tree from the
Lower Erian of Gaspé, under the name _Prototaxites_, but for which I
now prefer the name _Nematophyton_. When in London, in 1870, I obtained
permission to examine certain specimens of spore-cases or seeds from
the Upper Ludlow (Silurian) formation of England, and which had been
described by Sir Joseph Hooker under the name _Pachytheca_. In the same
slabs with these I found fragments of fossil wood identical with those of
the Gaspé plant. Still later I recognised similar fragments associated
also with _Pachytheca_ in the Silurian of Cape Bon Ami, New Brunswick.
Lastly, Dr. Hicks has discovered similar wood, and also similar fruits,
in the Denbighshire grits, at the base of the Silurian.[K]
[K] "Journal of the Geological Society," August, 1881.
[Illustration: Fig. 2.--_Nematophyton Logani_ (magnified). Vertical
section.]
[Illustration: Fig. 3.--_Nematophyton Logani_ (magnified). Horizontal
section, showing part of one of the radial spaces, with tubes passing
into it.]
[Illustration: Fig. 4.--_Nematophyton Logani_ (magnified).
Restoration.[L]]
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