El Niño modulated Holocene hydroclimate extremes as a dipolar pattern of droughts in northeastern China and floods in southwestern China.

In addition, an increasing trend of δ 13 C 27–35 values of leaf-wax lipids in the sediments of Twintaung Lake (Fig. 1 a) reflects decreasing Holocene monsoon precipitation in the region 39 .

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Thus, an increasing/a decreasing trend of EM3% in the YZ22A core could be related to long-term decreases/increases in the water level of Yangzong Lake under decreases/increases in monsoon precipitation (e.g., 32 ).

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