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The
above example shows a paleo reconstruction of the past 100,000 years
from Lago Grande di Monticchio, Italy. Based on concentrations of
preserved pollen grains in lake sediments, scientists reconstructed
the climate conditions determined by the types of plants represented
in different time periods.
In general, high percentages
of woody taxa with low values of Pinus lead scientists to reconstruct
temperate forests with relatively warm winters, warm summers and
and little water restriction. High values of herbaceous taxa lead
to the reconstruction of colder conditions and when the values of
Artemisia and Chenopodiaceae are high the environment is also dry.
From Allen et. al., (1999).
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