Recent methodological developments permit the quantitative reconstruct
ion of water chemistry variables from microfossil assemblages preserve
d in lake sediments. These reconstructions can be used to identify the
extent and timing of disturbance to lake ecosystems. Combined with ap
propriate sampling strategies, lake sediments permit water chemistry v
ariables and community rates of change to be estimated at a variety of
timescales. Sediments predating major cultural impacts offer the poss
ibility of inferring lake history before anthropogenic interference, a
nd can, therefore, contribute to current debates about timescales of n
atural variance in lakes, as well as the response of lake communities
to natural environmental perturbations. Such an approach has relevance
to many contemporary environmental problems, e.g. acidification, eutr
ophication and climate change.