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Climatic variations, perceptible on a human
scale, have had a considerable influence on plants, which have changed
dramatically over the millennia. Evidence of the changes comes from the peat
bogs. Plant pollens fall on the surface of the peat bogs and are then perfectly
preserved in the layers of peat. This information from the past has allowed
scientists to reconstruct the vegetation for a given region for each epoch.
12000 years ago the last glacial period ended
and the plateaux gradually lost their ice cover. The plains and hills were
covered with scant vegetation that is only found today in the north of Canada or
Siberia. Lichens and short grasses dominated.
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