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<p class="HeadingRunIn"><strong>Composition and abundance of oligochaetes in Scandinavian lakes in the 1970s in full compatibility with the ”morpho-edaphic index”. Do these relationships still hold 40 years later? </strong></p>
Author(s) -
Göran Milbrink
Publication year - 2020
Publication title -
zoosymposia
Language(s) - English
Resource type - Journals
eISSN - 1178-9913
pISSN - 1178-9905
DOI - 10.11646/zoosymposia.17.1.9
Subject(s) - edaphic , fauna , abundance (ecology) , ecology , relative species abundance , lake ecosystem , environmental science , geography , biology , ecosystem , soil water
In the 1960s it became fairly well-known that biological indices through their supposedly integrative power could be more robust measures of the water quality than separate chemical data. Oligochaetes and chironomid larvae in the bottom fauna hereby played an important role. Precision, however, increased dramatically if the relationship between oligochaetes and the so-called morpho-edaphic index, i.e. the average total phosphorus content in µg/l divided by the mean depth (in meters) of the lake (Ryder et al., 1974), was used in stead (Milbrink, 1978). The percentage composition and total abundance of oligochaetes in a number of lakes or selected basins of large lakes in southern Sweden and Norway were thus tested against this index in the 1970s. In logarithmic scales these relationships turned out to be more or less linear. The immediate conclusions were then that this method of classifying lakes could be of considerable scientific as well as practical value. Today we know a lot more about the ecological preferences of oligochaete species and characteristic species associations. The oligochaete fauna of the large lakes of southern Sweden, Mälaren, Vättern, Vänern and Hjälmaren, have been studied in detail over many years—over 100 years in the first three of these lakes and in the last lake for over 50-years. Effects of generally applied advanced sewage treatment in Sweden since the late 1960s are easily recognizable in the material. We have a situation of oligotrophication. With our new knowledge it comes natural today to study changes in species composition after trophic change and to investigate if the above close relationships in abundance are still largely linear.

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