A continuous pollen history of more than 40,000 years was obtained fro
m a lake in the lowland Amazon rain forest. Pollen spectra demonstrate
that tropical rain forest occupied the region continuously and that s
avannas or grasslands were not present during the last glacial maximum
. The data suggest that the western Amazon forest was not fragmented i
nto refugia in glacial times and that the lowlands were not a source o
f dust. Glacial age forests were comparable to modern forests but also
included species now restricted to higher elevations by temperature,
suggesting a cooling of the order of 5 degrees to 6 degrees C.