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Three sediment cores, each 1.5 meters in length, obtained from Lake Byestadsjön in the province of Småland, southern Sweden were studied with high resolution mineral magnetic measurements, carbon content, pollen analysis and XRF analysis. The aim was to reconstruct the early Holocene environment, with focus on the period between 9000-7000 cal yr BP, and thereby conclude if the 8200 cal yr BP cooli
