Variations of atmospheric C-14 concentrations over the Allerod-Younger Dryas transition

• Highly variable atmospheric radiocarbon concentrations are a distinct feature during the last deglaciation. The synchronisation of two high-resolution AMS C-14-dated records, Lake Gosciaz, and a floating Late Weichselian glacial varve chronology at the Al

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LAST GLACIAL/INTERGLACIAL TRANSITION; ATLANTIC THERMOHALINE CIRCULATION; DEEP-WATER CIRCULATION; ABRUPT CLIMATE-CHANGE; GREENLAND ICE CORE; SEA-LEVEL RECORD; NORTH-ATLANTIC; MELTWATER DISCHARGE; OCEAN CIRCULATION; VARVE CHRONOLOGY

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