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The ongoing warm stage, the Ho-locene, has lasted until now about 11,500 years. Past interglacials occurred every 100,000 years and had durations between 7,000 and 17,000 years, estimated from the Vostok ice core and annual-layer-counted varved lake sediments in northern Germany. The objectives for the DEKLIM project “Climate change at the very end of a warm stage” are to:a) determine the length of past in-terglacials in Europe with high precision by varve counting of lake sediments,b) reconstruct environmental change at the end of an inter-glacial by pollen analysis,c) date interglacials by U/Th and luminescence techniques,d) quantify the temperature change at the very end of past interglacials with both proxy and model data,e) use the models to detect the physical causes that determine the end of an interglacial. Understanding of the warm to cold transitions of the last 500,000 years should provide background information on the processes that would control the natural climate evolution at the end of the Holocene.

Climate Change at the Very End of a Warm Stage: First Results From the Last Glacial Inception at 117,000 yr BP