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Changes in benthic macroinvertebrate abundance and lake isotope (C,N) signals following biomanipulation: an 18-year study in shallow Lake Vaeng,Denmark
Authors:Email author" target="_blank">T?BollEmail author  L?S?Johansson  T?L?Lauridsen  F?Landkildehus  T?A?Davidson  M?S?ndergaard  F???Andersen  Email author" target="_blank">E?JeppesenEmail author
Institution:1.Department of Bioscience,Aarhus University,Silkeborg,Denmark;2.Institute of Biology,University of Southern Denmark,Odense M,Denmark;3.Greenland Climate Research Centre (GCRC), Greenland Institute of Natural Resources,Nuuk,Greenland;4.Sino-Danish Education and Research Centre (SDC),Beijing,China
Abstract:Change in the abundance of benthic macroinvertebrates and the stable isotope composition (C, N) of benthic invertebrates and zooplankton in Lake Vaeng, Denmark, was investigated over an 18-year period following biomanipulation (removal of cyprinids). During the first nine years after biomanipulation, the lake was clear and submerged macrophytes were abundant; after this period, a shift occurred to low plant abundance and high turbidity. Two years after the biomanipulation, total density of benthic macroinvertebrates reached a maximum of 17042 (±2335 SE) individuals m−2 and the density was overall higher when the lake was in a clear state. Redundancy analysis (RDA) suggested macrophyte abundance and total nitrogen (TN) concentration were the dominant structuring forces on the benthic macroinvertebrate assemblage. Stable isotope analysis revealed that δ13C of macroinvertebrates and zooplankton was markedly higher in years with high submerged macrophyte abundance than in years without macrophytes, most likely reflecting elevated δ13C of phytoplankton and periphyton mediated by a macrophyte-induced lowering of lake water CO2 concentrations. We conclude that the strong relationship between macrophyte coverage and δ13C of macroinvertebrates and cladocerans may be useful in paleoecological studies of past changes in the dynamics of shallow lakes, as change in macrophyte abundance may be tracked by the δ13C of invertebrate remains in the sediment.
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