The effects of reservoir aging on the benthic macroinvertebrate commun
ity in Pawnee Reservoir were documented by comparing species compositi
on and biomass of samples collected from October 1991 through Septembe
r 1992, to a similar survey conducted in 1968-70 by Hergenrader and Le
ssig (1980). Filling of the basin with sediment and associated materia
l and the subsequent change in the benthic environment, has resulted i
n a relatively homogenous bottom substrate at each of the three sampli
ng transects (dam, middle, and inflow). Sediment enrichment has limite
d the benthic fauna to species tolerant of brief periods of bottom ano
xia and increased levels of organic matter, which has resulted in the
disappearance of many taxa and a decrease in the abundance of remainin
g invertebrates. Significant differences in total biomass were found a
t each transect, as well as for the whole lake, between study periods.
The dam, middle, inflow and total biomasses for the 1968-70 study per
iod were 2.4, 1.5, 2.3 and 2.0 g m(-2), respectively, compared to 0.2,
0.2, 0.3, and 0.2 g m(-2) for the 1991-92 study period. The total dis
appearance of eight invertebrate taxa, in particular two sphaerid clam
species, and significant declines in other dominant taxa such as Chao
borus punctipennis and Chironomus sp. accounted for these major differ
ences in biomass between study periods. Reductions in the number of ta
xa present has resulted in an increase in benthic faunal similarity at
each transect, with tubificid oligochaetes, Coelotanypus sp., C. punc
tipennis, and Chironomus sp., comprising 90% of both the total density
and biomass of benthic invertebrates in Pawnee Reservoir.