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Spatio‐temporal distribution of sedimentary Cladocera (Crustacea: Branchiopoda) in relation to climate

Spatial and temporal variations in the composition of freshwater invertebrate assemblages may be useful indicators of past climate change and help us to predict species responses to future climate change. The objective of this study was to understand the relationship between climate variables and fossil Cladocera assemblages in lake sediments along a contemporary climate gradient from hemiboreal to subarctic ecoregions in Finland and throughout the Holocene climate succession.