Precise date for the Laacher See eruption synchronizes the Younger Dryas.

• Main Authors: Reinig, Frederick, Wacker, Lukas, Jöris, Olaf, Oppenheimer, Clive, Guidobaldi, Giulia, Nievergelt, Daniel, Adolphi, Florian, Cherubini, Paolo, Engels, Stefan, Esper, Jan, Land, Alexander, Lane, Christine, Pfanz, Hardy, Remmele, Sabine, Sigl, Michael, Sookdeo, Adam, Büntgen, Ulf
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2021
• Subjects: 37 Earth Sciences; 3709 Physical Geography and Environmental Geoscience; 3705 Geology; Greenland; Greenland ice core; ice core; North Atlantic
• Online Access: https://www.repository.cam.ac.uk/handle/1810/368946; https://doi.org/10.17863/CAM.108955

The Laacher See eruption (LSE) in Germany ranks among Europe's largest volcanic events of the Upper Pleistocene1,2. Although tephra deposits of the LSE represent an important isochron for the synchronization of proxy archives at the Late Glacial to Early Holocene transition3, uncertainty in the age of the eruption has prevailed4. Here we present dendrochronological and radiocarbon measurements of subfossil trees that were buried by pyroclastic deposits that firmly date the LSE to 13,006 ± 9 calibrated years before present (BP; taken as AD 1950), which is more than a century earlier than previously accepted. The revised age of the LSE necessarily shifts the chronology of European varved lakes5,6 relative to the Greenland ice core record, thereby dating the onset of the Younger Dryas to 12,807 ± 12 calibrated years BP, which is around 130 years earlier than thought. Our results synchronize the onset of the Younger Dryas across the North Atlantic-European sector, preclude a direct link between the LSE and Greenland Stadial-1 cooling7, and suggest a large-scale common mechanism of a weakened Atlantic Meridional Overturning Circulation under warming conditions8-10.