Abstract
The sediments of Loe Pool, a eutrophic coastal lake in south west England, consist largely of laminated clays and clay-gyttjas. Studies of the diatom microstratigraphy of frozen sediment cores from the Pool indicate that the laminations are annual, and that they contain pairs of light and dark bands formed by seasonal variations in the supply of sediment to the Pool from its catchment. Analysis of the magnetic properties of individual laminations demonstrates the presence of physical and mineralogical microstratigraphic variations, which may also be related to seasonality.
A varve chronology, which is confirmed by 137Cs analysis and historical records, has been used to provide a timescale for the interpretation of data from other paleolimnological studies. A close agreement between variations in the abundance of sedimentary Sn, and the history of mining in the catchment, has been found. Similarly, analysis of total organic matter, total phosphorus, sedimentary chlorophyll a, sterols, diatoms and Cladocera in the uppermost sediments all indicate eutrophication of the Pool in the period AD 1940 to the present.
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Coard, M.A., Cousen, S.M., Cuttler, A.H. et al. Paleolimnological studies of annually-laminated sediments in Loe Pool, Cornwall, U.K.. Hydrobiologia 103, 185–191 (1983). https://doi.org/10.1007/BF00028450
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DOI: https://doi.org/10.1007/BF00028450