Abstract

The temporal and spatial variability in the midge assemblage found in a backwater lake of the Mississippi River was examined. Bi-weekly samples were taken during the summers of 1987 and 1988. Four taxa of chironomids were found. The population density and sizes of chironomids, and the proportion that each taxon comprised of the midge assemblage, varied significantly in time and space. In an attempt to examine whether the variability noted was related to sediment accretion in the lake, sedimentation rates were measured. There were few correlations among sedimentation rate or the organic matter content of the collected sediment and the structure of the midge assemblage. Those few correlations that were statistically significant were low and often paradoxical. For example negative relationships were found between the density and size of Chironomus spp., a detritivore, and the amount of sediment deposited or its organic matter content. Also no significant relationships were found between the density of the predator Cryptochironomus spp. and the density of other chironomids (potential prey). These negative findings indicate that factors other than food, such as sediment texture, may be more important than food availability in structuring chironomid assemblages in backwater areas. There was spatial variability in the densities and sizes of chironomids that may be explained by differences in sediment texture and organic matter. This suggests that short-term inputs of sediment (as ascertained by sediment traps) may not greatly influence midge assemblages while the long-term changes in sediment composition may have large influences.

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