Gryguc, G., Kisielienė, D., Stančikaitė, M., Šeirienė, V., Skuratovič, Ž., Vaitkevičius, V., Gaidamavičius, A., 2013 Abstract This paper presents new data describing the Holocene environmental history of the Briaunis pal aeolake, Eastern Lithuania. Shortly before 9600 cal yr BP, sedimentation began in an oligotrophic deepwater basin, whereas the Early Holocene instability of the environmental regime caused the influx of detrital sediment into the basin. A birch forest dominated in the surrounding landscapes, and at ca. 9600 cal yr BP, the spread of Ulmus, Alnus, Populus and Corylus began, suggesting a shortlived climatic amelioration. A subsequent drop of the water table and increasing influx of the terrigenous material continued from 9600 to 9300-9200 cal yr BP. The ensuing climatic stability caused the formation of a deciduous forest and the regional spread of Picea. Some instability, i.e. a decline in the thermophilous species, as well as the appearance of boreal and northern alpine diatoms, could be associated with the socalled "8.2 ka event". This reversal was followed by ameliora tion and prospering of the water plants typical of the Holocene climatic optimum from 7900 to 7200-7100 cal yr BP. At aproximatelly 6600-6500 cal yr BP, a small rise of the water table was documented and bogforming processes dominated until ca. 3600-3400 cal yr BP, when a smallscale deepening of the basin occured.