Although human influence dominates present-day Amazonian rainforest fi
res, old charcoal fragments, buried in the soils or in lacustrine sedi
ments, confirm that fire has played a major role in the history of Ama
zonian forests. These fires may have influenced the present-day divers
ity and structure of the rainforest and if these fire-favorable events
of the past reoccur there may be drastic consequences for the future
of the Amazonian forests. Detailed studies of Carajas lake sediments p
ermit identification of these past fire events, through microscopic ob
servations of small charcoal fragments. They also permit, through radi
ocarbon dating, a better definition of their timing and make it possib
le to relate them to past paleo-environmental and paleoclimatic condit
ions. The paleodata indicate that fire events were concomitant with sh
ort dry climate episodes whose frequency of occurrences has varied dur
ing the last 7000 years. These dry events may be related to past clima
te conditions observed in different regions of tropical South America.