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Millennial-scale variations between warmer, more saline surface water and cooler, less saline surface water were recognized during the early deglacial period and the Holocene, suggesting changes in the mixing ratio between the Kuroshio Water and the Changjiang Diluted Water. Stronger East Asian summer monsoon (EASM) precipitation events in south China are identified at 10.5, 8.8, 7.0, 5.3, 4.7, 2.9, 1.7, and 0.5 ka, based on sea surface salinity (SSS) records of the northern ECS. Weaker EASM precipitation events are also detected at 9.3, 8.3, 7.3, 6.0, 3.3, 2.3, 0.7, and 0.4 ka during the Holocene. These events agree with the maxima in δ18O records of stalagmites from various parts of the Changjiang (Yangtze) River drainage. This agreement supports that our SSS record properly captures the millennial-scale dry (less EASM precipitation) events over the drainage basin of the Changjiang River during the Holocene. These dry events are also in good agreement with North Atlantic ice-rafted events, suggesting a teleconnection between North Atlantic climate and the EASM during the Holocene."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233286387987","@type":"Researcher","foaf:name":[{"@value":"Yoshimi Kubota"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science, Graduate School of Science; University of Tokyo; Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233286387973","@type":"Researcher","foaf:name":[{"@value":"Katsunori Kimoto"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Global Change; Japan Agency for Marine-Earth Science and Technology; Yokosuka 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