Sediment samples collected along a six-meter core, drilled in the deepest part of the Lagoa do Caçó (NE Brazil), have been investigated in order to determine source(s) and degradation conditions of the organic matter (OM) with special emphasis on paleoenvironmental implications. Bulk organic geochemistry (Rock-Eval pyrolysis, C/N determination, δ 13 C and δ 15 N measurement) and petrography combined with sedimentological evidence and radiocarbon dates allowed to identify four major intervals documenting major environmental changes that occurred during the last 20,000 years. The first interval, dating back to the end of the Last Glacial Maximum (LGM), contains well preserved OM derived from higher plants.This material was most probably produced in an ephemeral palustrine system and rapidly buried by sands. This level is thought to have been deposited under relatively arid climate conditions associated with strong but episodic rainfalls. Between 19,240 and 17,250 Cal yrs BP, the climate appears to have been more humid and seasonality more pronounced as suggested by the presence of a permanent lake. After a drastic environmental change dating back to 17,250 Cal yrs BP, the sediment became truly lacustrine with restricted mineral input and highly-degraded higher plant-derived organic matter. After that, a stepwise improvement in the preservation of OM occurred, as revealed by several pronounced shifts in the RockEval TpS2 signal. These changes could document abrupt climatically driven changes during the Lateglacial. Finally, around 5610 Cal yrs BP, environmental conditions, approaching those prevailing today were established. Minor climatic changes during the Holocene were * Corresponding author at current address: Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Bât 12, Domaine du CNRS, Avenue de la Terrasse, F-91198 Gif-sur-Yvette Cedex, France. E-mail address: jeremy.jacob@lsce.cnrs-gif.fr 2 probably buffered by a high water table which might explain the lack of paleoenvironmental fluctuations.