A TIMELINE FOR THE PLANET
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Most of the world’s coal was laid down during the
Carboniferous period, 360 million years ago.
And huge amounts of oxygen were released for the animals of the time to
breathe.
Trees had actually appeared some 20 million years
earlier. But they didn’t get their big
chance until after the Late Devonian extinction event had set the scene. Little seems to be known about what might
have caused the extinction. There’s an
impact theory – there’s always an impact theory. But on this occasion the evidence doesn’t
seem to be terribly convincing.
On balance an earthly cause looks more likely. There are signs of major changes in sea level at around this time. There were climatic changes and changes in
ocean chemistry as well. So it’s
tempting to blame plate tectonics and the super-continent
cycle.
However as soon as the extinction was over, massive
forests appeared. And the Devonian
period gave way to the Carboniferous.
This forest scene comes from ‘History of Life’ by Richard Cowen.
The trees were quite different from modern trees. A major player was the ‘clubmoss’ tree (colour picture: Hans
Steur). It could grow to more than 30
metres. Another was the ‘horsetail’ tree
which grew up to 20 metres. These trees
are clearly related to their modern brethren.
But the actual species died out at the end of the Carboniferous when
conditions became colder and much drier.
The sea level had risen, and large areas of low-lying
land had been covered by shallow seas and freshwater swamps. The climate was also warm and wet.
These were ideal conditions for the laying down of
coal seams. Trees and other vegetation
die and fall into the water; where they are quickly covered. Oxygen is excluded. So bacteria, bugs and fungi can’t attack the
dead remains and rot them away.
More falls on top; and before you know it you have a
good thick deposit.
Eventually conditions change, and
gravel and sand get deposited on top.
Over tens and hundreds of millions of years, other adventures befall the
deposits. And we end up with a coal
seam, perhaps several kilometres underground.
During the Carboniferous – and as a
result of all this ‘carbon burial’ – the amount of oxygen in the atmosphere
grew to crazy heights, around 35% (more). At these levels, dry wood combusts
spontaneously. Fortunately the coal
forests were wet. This was also the time
of the giant dragonflies (see above link), with wingspans up to 2 feet.
The conditions changed again at the
end of the Carboniferous, and as far as I know only limited amounts of coal
have been laid down since.
© C B Pease,
December 07