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Titlebook: Environmental History and Palaeolimnology; Proceedings of the V J. P. Smith,P. G. Appleby,P. E. O’Sullivan Conference proceedings 1991 Spri

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https://doi.org/10.1007/978-981-10-0317-2outhern Sweden’. Pollen, plant macrofossils, diatoms, physical and chemical analysis, magnetic measurements and radiometric methods (.Pb, .C) have been used to study palaeoecological changes, i.e. climate, land use, lake trophy and soil erosion during the past 3000 years. This multidisciplinary stud
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Mill: An Ethical Base for Capitalismgnetic evidence from one of the cores and .Pb analysis of another, suggests that the increase in sediment Cu and Zn concentrations began during the eighteenth century. A sharp increase in the concentrations of these metals in the sediment profile appears to have occurred during the latter part of th
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https://doi.org/10.1007/978-1-349-01745-4Sediment cores, dated by .Pb and/or varves, from lakes that do not receive point or non-point source discharge of pollutant metals and metalloids from within their catchments have been used to:
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Progress in understanding the chemical stratigraphy of metals in lake sediments in relation to acidSediment cores, dated by .Pb and/or varves, from lakes that do not receive point or non-point source discharge of pollutant metals and metalloids from within their catchments have been used to:
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