Abstract
Magnetic susceptibility measurements have been used to correlate synchronous depths in ca. 50 1 m. cores of recent sediment from a small lake (area ca. 55 ha) in Scania, southern Sweden. The three-dimensional picture of sediment accumulation which emerges provides a basis for studying sediment deposition patterns through time. Using a palaeomagnetic chronology, the results show that the pattern and rate of accumulation have dramatically altered during the past 350 years, thus making semiquantitative studies of downcore sediment properties in a single core problematical. Possible reasons for these phenomena are briefly discussed.
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© 1983 Dr W. Junk Publisher, The Hague
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Dearing, J.A. (1983). Changing patterns of sediment accumulation in a small lake in Scania, southern Sweden. In: Meriläinen, J., Huttunen, P., Battarbee, R.W. (eds) Paleolimnology. Developments in Hydrobiology, vol 15. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7290-2_9
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DOI: https://doi.org/10.1007/978-94-009-7290-2_9
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