The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
The Upper Laurentian and Huronian have as yet afforded no evidence of
land vegetation. The Cambrian, as already stated, abounds in remains of
sea-weeds; but though the forms which have been named _Eophyton_ have
been regarded as land plants, this claim is, to say the least, very
doubtful; and I have as yet seen nothing of this kind which did not
appear to me to be merely markings made by objects drifted over the
bottom or remains of marine plants. Yet in the Upper Cambrian there are
wide surfaces of littoral sandstone often containing minute carbonised
fragments, and which might be expected to afford indications of land
vegetation, had such existed. I have myself devoted many days of
fruitless labour to the examination of the large areas of Potsdam
sandstone exposed in some parts of Canada. But as these rocks were
evidently formed along the borders of a Laurentian continent capable of
supporting vegetation, we may still hope for some discovery of this
kind, more especially if we could find the point where some fresh-water
stream ran into the Cambrian sea.
[Illustration: FIG. 83.—_Protannularia Harknessii_ (Nicholson). A
Siluro-Cambrian Plant, from the Skiddaw series.]
The oldest plants, probably higher than Algæ, known to me by their
external forms, are those described by Nicholson[25] from the
Siluro-Cambrian Skiddaw slates of the north of England (Fig. 83). Their
discoverer has named them _Buthotrephis Harknessii_ and _B.
radiata_,[26] stating, however, that these two species are not
improbably portions of the same plant, and that its form is rather that
of a land plant than of an Alga. The specimens of these plants which I
have seen appear to me to support the conclusion that they represent one
species, and this allied to the _Annulariæ_ of the Devonian and
Carboniferous periods, which probably grew in shallow water with only
their upper parts in the air, and bore whorls or verticles of narrow
leaves. They were either relatives of the Mare’s-tails, or of the
Rhosocarps, of our modern swamps and ponds.
[Illustration: FIG. 84.—American Lower Silurian Plants.—After
Lesquereux.
_a_, _Sphenophyllum primævum_. _b_, _Protostigma sigillarioides_.]
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