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Accurate dating is of fundamental importance to paleoclimatic studies. Without reliable estimates on the age of events in the past, it is impossible to investigate if they occurred synchronously or if certain events led or lagged others; neither is it possible to assess accurately the rate at which past environmental changes occurred. Strenuous efforts must therefore be made to date all proxy materials, to avoid sample contamination, and to ensure that the stratigraphic context of the sample is clearly understood. It is equally important that the assumptions and limitations of the dating procedure used are understood so that a realistic interpretation of the date obtained can be made. It is often just as important to know the margins of error associated with a date as to know the date itself. In this chapter, we discuss the main dating methods widely used in Quaternary studies today. Further details can be found in Geyh and Schleicher (1990) , Noller et al. (2000) , and Walker (2005) .