A synthesis is presented of the envronmental and climatic variations that are inferred to have occurred in southern Sweden (up to latitude 59°N) and Denmark during the Weichselian Late‐glacial (14‐9 ka BP). The chronology and characteristics of the main phases of deglaciation, sea‐level change, periglacial activity, soil development, vegetation cover and climate change are summarised. A curve representing the main changes in temperature, including quantitative estimates based upon beetle data and using the ‘mutual climatic range’ method, is presented.
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Berglund et al. (1994) studied this question.
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