Last deglacial abrupt climate changes caused by meltwater pulses in the Labrador Sea

• Main Authors: You, D, Stein, R, Fahl, K, Williams, MC, Schmidt, DN, McCave, IN, Barker, S, Schefuß, E, Niu, L, Kuhn, G, Niessen, F
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2023
• Subjects: 37 Earth Sciences; 3709 Physical Geography and Environmental Geoscience; 3705 Geology; 13 Climate Action; 14 Life Below Water; Greenland; Morton; Labrador Sea; Ocean acidification; Sea ice
• Online Access: https://www.repository.cam.ac.uk/handle/1810/347686; https://doi.org/10.17863/CAM.95100

Acknowledgements: We sincerely thank the professional support of the captain and crew of the R/V Maria S. Merian as well as the scientific team on the expedition MSM12/2. We also thank W. Luttmer for technical assistance with the measurement at AWI. Many thanks to G. Mollenhauer, the AWI MICADAS lab, and S. Morton (SUERC) for radiocarbon measurement. Thanks to C. Vogt for XRD analysis. This project was supported by the Deutsche Forschungsgemeinschaft (DFG) through the International Research Training Group IRTG 1904 ArcTrain. Grant NE/I020261/1 from NERC in the ocean acidification program to D.N.S. is also gratefully acknowledged. Furthermore, we acknowledge support by the Open Access Publication Funds of AWI. Funder: Deutsche Forschungsgemeinschaft through "ArcTrain" (GRK1904) <jats:title>Abstract</jats:title><jats:p>Freshwater perturbations are often thought to be associated with abrupt climate changes during the last deglaciation, while many uncertainties remain regarding the exact timing, pathway, mechanism, and influence of meltwater release. Here, we present very well-dated and high-resolution records from the eastern Labrador Sea representing the last 19.000 years, which demonstrate abrupt changes in sea surface characteristics. Four millennial-scale meltwater events have been identified between the last 14.000 and 8.200 years based on independent biomarker proxies and X-ray fluorescence scanning data. These events are characterized by increased sea ice formation and decreased sea surface temperatures which might have occurred within a few decades. We propose these abrupt changes were triggered by meltwater pulsing into the Labrador Sea periodically, resulting from collapse of the Laurentide-Greenland Ice Sheets caused by (sub-)surface ocean warming in the Labrador Sea. Our findings provide more precise information about impact of freshwater forcing on abrupt climate changes, which may help to improve simulations for past and future changes in ocean circulation and ...