Vegetational history can help us to predict future environments by pro
viding data for testing AGCMs, for indicating the vegetational respons
e to rapid warming and changing CO2 concentrations, and for mathematic
al modelling of vegetation. Most of the data are palynological, and th
ere are well over 100 pollen diagrams from tropical regions. Maps are
presented showing summarized pollen diagrams from the lowlands of Sout
h-East Asia and the West Pacific, Tropical Latin America and Tropical
Africa. In all these regions there is some evidence suggesting that at
the LGM lowland forests were somewhat restricted in area and included
montane elements. This is consistent with cooler and drier climate at
the LGM. From the montane and lowland areas of these three regions, t
he pollen evidence is summarized in altitudinal diagrams. These sugges
t considerable depression of altitudinal zones at the LGM, suggesting
temperatures c. 5-10 degrees C cooler than now. These results conflict
with earlier oxygen isotope data from marine foraminifera, but do not
conflict with more recent oxygen isotope measurements from tropical c
orals. It is also suggested that altitudinal movements may be partly c
ontrolled by CO2 concentration and ultraviolet light.