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Dating of Lake and Loess Sediments

Published online by Cambridge University Press:  18 July 2016

Juerg Beer  and
Michael Sturm
Juerg Beer
Affiliation:
Swiss Federal Institute for Environmental Science and Technology (EAWAG) CH-8600 Dübendorf, Switzerland
Michael Sturm
Affiliation:
Swiss Federal Institute for Environmental Science and Technology (EAWAG) CH-8600 Dübendorf, Switzerland
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Abstract

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Lake and loess sediments represent archives that record important information about the iocal, regional and global climate conditions in the past. Lake sediments consist of autochthonous particles formed by biogeochemical processes within the lake and allochthonous particles brought into the lake from the catchment area. After deposition, the stratigraphy of the sediment can be altered by chemical, physical and biological processes. Under favored conditions, the sediment shows individual annual layers (varves), which can be used to date the sediment. Other dating methods are based on radioactive decay (14C, 210Pb) or on time markers such as tephra layers, deposits of natural catastrophes, e.g., floods, or radioactivity, e.g., emissions from a nuclear power plant.

Type
Papers from the Workshop on Pages Chronologies
Information
Radiocarbon , Volume 37 , Issue 1 , 1995 , pp. 81 - 86
Copyright
Copyright © The American Journal of Science 

References

Beer, J., Shen, C., Heller, F., Liu, T., Bonani, G., Dittrich, B., Kubik, P. and Suter, M. 1993 10Be and magnetic susceptibility in Chinese loess. Geophysical Research Letters 20: 57–60.CrossRefGoogle Scholar
Hajdas, I., Ivy, S. D., Beer, J., Bonani, G., Imboden, D., Lotter, A. F., Sturm, M. and Suter, M. 1993 AMS radiocarbon dating and varve chronology of Lake Soppensee: 6000 to 12,000 14C years BP. Climate Dynamics 9: 107–116.CrossRefGoogle Scholar
Heller, F. and Liu, T.S. 1982 Magnetostratigraphical dating of loess deposits in China. Nature 300: 431–433.CrossRefGoogle Scholar
Kelts, K. and Hsu, K. J. 1978 Freshwater carbonate sedimentation. in Lerman, A., ed., Lakes: Chemistry, Geology, Physics. Heidelberg, Springer Verlag: 295–324.CrossRefGoogle Scholar
Kukla, G., Heller, F., Liu, X. M., Xu, T. C., Liu, T. S. and An, Z. S. 1988 Pleistocene climates in China dated by magnetic susceptibility. Geology 16: 815–818.2.3.CO;2>CrossRefGoogle Scholar
Liu, T. S. 1985 Loess and the Environment. Beijing, China Ocean Press: 251 P.Google Scholar
Lotter, A. F., Ammann, B., Beer, J., Hajdas, I. and Sturm, M. 1992 A step towards an absolute time-scale for the Late-Glacial: Annually laminated sediments from Soppensee (Switzerland). in Bard, E. and Broecker, W., eds., The Last Deglaciation: Absolute and Radiocarbon Chronologies. NATO ASI Series I. Berlin, Springer-Verlag: 45–68.CrossRefGoogle Scholar
Shen, C., Beer, J., Tungshen, L., Oeschger, H., Bonani, G., Suter, M. and Wölfli, W. 1992 10Be in Chinese loess. Earth and Planetary Science Letters 109: 169–177.CrossRefGoogle Scholar
Sturm, M. 1979 Origin and composition of clastic varves. in Schlüchter, C., ed., Moraines and Varves. Rotterdam, Balkema: 281–285.Google Scholar
Sturm, M. and Lotter, A. F. 1995 Lake sediments as environmental archives. EAWAG News 38E: 6–9.Google Scholar
von Gunten, H. R. and Moser, R. N. 1993 How reliable is the 210Pb dating method? Old and new results from Switzerland. Journal of Paleolimnology 9: 161–178.CrossRefGoogle Scholar
Wintle, A. G. 1990 A review of current research on TL dating of loess. Quaternary Science Reviews 9: 385–397.CrossRefGoogle Scholar