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Holocene Lake Level Fluctuations Recorded in the Sediment Compositionof Lake Juusa,Southeastern Estonia
Authors:Email author" target="_blank">Jaan-Mati?PunningEmail author  Tiiu?Koff  Ene?Kadastik  Annika?Mikom?gi
Institution:(1) Institute of Ecology at Tallinn University, Kevade 2, 10137 Tallinn, Estonia
Abstract:The main aim of this study was to reconstruct the history of water level fluctuations of a small dimictic lake during the Holocene based on the lithological and geochemical composition of sediments. We studied lithological and geochemical parameters in sediment cores extracted along a transect through Lake Juusa in southeastern Estonia. Analysis revealed that LOI550 and CaCO3 content in the accumulated sediment are dependent on water depth. At depths greater than 3 m, the relationship between organic carbon and CaCO3 is inverse, whereas no relationship exists at shallower depths. Lake-level changes are well depicted on the grain-size distribution profiles and macrofossil composition. An increase in the >‰315μm fraction appeared during the initial phases of water level fluctuations, followed by an increase in the 100–315μm fraction. The >‰36μm fraction dominated the silt fraction. Higher OC/N ratios in shallow water sediments reflect the dominance of macrophytes vegetation.
Keywords:Geochemistry  Lake sediments  Lithology  Macrophytes  OC/N variations  Water level fluctuations
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