A 10 in sediment core from Academician Ridge in Lake Baikal was analyzed for its molecular composition using on-line TMAH (tetramethylammomium hydroxide) thermochemolysis. Major products are lignin phenols, n-C-14 to C-30 fatty acids (alkanoic acids), cutin acids, hydroxy acids and aliphatic dicarboxylic acids. Lignin phenols are abundant in warmer periods (the interglacial: marine isotope stage (MIS) 5e and MIS 1), but extremely low in the other (colder) periods. This result coincides well with pollen records reported for a core near the present site, where an expansion of coniferous forests in substage 5e and MIS I was implied. Normal C-24-C-30 alkanoic acids, important components of plant wax esters, are abundant in 5e and MIS I and are present in significant amounts in the other (colder) periods, unlike the lignin phenols. A high abundance of n-C-24 to C-30 alkanoic acids relative to lignin phenols in the B circle divide lling-Aller circle divide d warm period suggests an enhanced development of herbs. It is implied from comparison of the sedimentary lignin phenol record with fossil pollen records and lignin phenol analysis of modern pollen that the ratio of cinnamyl phenols to vanillyl phenols may serve as an indicator of pollen contribution to sedimentary organic matter. (c) 2006 Elsevier Ltd. All rights reserved.