Oxygen uptake rates of undisturbed sediment columns have been used as an in
tegrative measure of the metabolic activities of benthic communities. Since
the intensity of metabolic processes of profundal lake is dependent on the
production of organic matter in the pelagic zone, oxygen uptake rates refl
ect the trophic condition of the whole lake. Four small lakes of central Ch
ile, differing strongly in trophic conditions, provided a possibility to co
mpare benthic oxygen uptake rates, under different oxygen conditions (Quine
nco, Grande, Chica and Lleulleu). Our objective was to establish the relati
onship between the oxygen uptake rates and bottom characteristics of lakes
with different trophic conditions. At 8 mg O-2 l(-1) in the overlying water
of the cores studied, the oxygen uptake rates of the sediment were: Quinen
co 51.2-56.0 mg O-2 m(2) h(-1) (eutrophic), Grande 41.2-46.4 mg O-2 m(2) h(
-1) (mesotrophic), Chica 23.2-18.1 mg O-2 m(2) h(-1) (mesotrophic) and Lleu
lleu 11.7-16.0 mg O-2 m(2) h(-1) (oligotrophic). By exposing the sediments
to different oxygen levels in the laboratory, it was found that benthic com
munity metabolism decreased with oxygen concentrations. The slope of regres
sion lines, relating oxygen uptake rates to oxygen concentrations, differed
for the different sites investigated, closely related with the trophic con
ditions of the lakes. It was positively correlated with the organic matter
content of the sediment of the cores (r(2)= 0.78, p < 0,05) and the nutrien
ts of the bottom waters (total-P: r(2)= 0.73, p < 0,05; total-N: r(2)= 0.73
, p < 0,05), and negatively with the redox potential of the sediments (r(2)
= 0.88, p < 0,05).