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The oldest land plants (1)
The oldest land plants (2)
Rhynie Chert
Parka
(Seed) ferns
Lepidodendron
The leaf of Neuropteris
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The oldest land plants (2)Spiny plants
During the Early Devonian (405 - 385 million years ago) several other
groups of plants developed. They had the common feature of being rather small
(not higher than half a
The compressed fossils of Devonian plants scarcely give any information. Determining these very old plants is extremely difficult as hardly anything shows on the fossils. Only stems, bifurcations and possibly spines. With luck you find sporangia. In that case it might be possible to detect the name of the plant. Sometimes the cuticle has stayed intact. After chemical treatment it is possible to make a microscope preparation of it in which e.g. cells and stomata are visible.
Rhynie Chert
The discovery of a silicified moor
near the Scottish village of Rhynie, 40 km north-east of Aberdeen, has revealed
a lot about the structure of very old plants.
A second plant common in the Rhynie Chert is called Asteroxylon. It is a very early member of the club-mossgroup. In the picture you can see the woodvessels of this plant, reinforced with annular and spiral thickenings. Of a third plant, Horneophyton, the sporangia and the spores are found often. Typical of higher plants is that the spores are formed in clusters of four. For some time these often cluster in so called tetrads. Click on to the photo to see one. One spore has a diameter of about 50 µms.
Further developments
From the Early Devonian the flora evolution gains momentum. Wereas the
number of species in the Late Silurian could be counted on the fingers of
two hands, in the Early Devonian this has become quite impossible. Yet at
that moment the number of species was still very limited and in many cases
the vegetation at a certain spot consisted of only
one species
or a very small number of species. At the rare finding places of well-preserved
Early Devonian plantfossils one often tends to find one dominating species
with the occasional sparse occurrence of other species. The further the Devonian proceeds, the more forms appear and the higher some plant species become. In the Middle Devonian tree'ferns' appear with a height of some meters. In the Late Devonian some plant groups develop the ability to form thicker stems bij means of secundary development. Thus we see the appearance of woody stems enabling the plants to form trees. In the Late Devonian there are already rather high trees up to 8 meters. During the Middle and the Late Devonian more species with leaves or leaflike structures appear. These developed through 'webbing' of finely branched twigs, i.e. the twigs became connected by intervening tissue. In the fernlike plant Rhacophyton from the Belgium Late Devonian this is not yet the case. However the branches in a way resemble fernleaves. The sporangia of this plant are growing in clusters with a diameter of about 2.5 cms.
SeadplantsThe oldest seed plants date from the Late Devonian. The special feature of seeds is their being enveloped. In Moresnetia (so called after the town of Moresnet in Belgium) this envelope is not yet completely closed. It is placed around the seed like a sort of calyx, leaving the top of the seed visible. Moresnetia is one of the oldest seed plants in the world and the oldest in Europe. For the time being, for new discoveries are made regularly. In Belgium extraordinary well preserved specimens have been found, in which even the seeds are visible. Click on to the photo! The oldest seed plants were gymnosperms for the seeds were not yet embedded in an ovary. From this kind of plants the many species of seed ferns developed that grew in the Coalswamps during the Carboniferous. And a Moresnetia-like plant must have been the ancestor of all modern flowering plants. Surely a plant to treat with respect. Hans Steur |