Quantifying paleoprecipitation of the Luochuan and Sanmenxia Loess on the Chinese Loess Plateau
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Paleoprecipitation of the LC and SMX loess L1-S5 is reconstructed by a new proxy.

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SMX experienced stronger EASM and weaker EAWM than LC since at least S5 (~ 620 ka).

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EASM is mainly controlled by the insolation maxima and minima during interglacial.

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