{"refrec":{"BRefID":331408,"RR":"<b>Wang, Y.; Lu, H.; Wang, K.; Wang, Y.; Li, Y.; Clemens, S.; Lv, H.; Huang, Z.; Wang, H.; Hu, X.; Lu, F.; Zhang, H.</b> (2020). Combined high- and low-latitude forcing of East Asian monsoon precipitation variability in the Pliocene warm period. <i>Science Advances 6(46)</i>: eabc2414. <a href=\"https://dx.doi.org/10.1126/sciadv.abc2414\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abc2414</a>","BEntID":325019,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Science Advances 6(46)</i>: eabc2414. <a href=\"https://dx.doi.org/10.1126/sciadv.abc2414\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abc2414</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wang, Y.; Lu, H.; Wang, K.; Wang, Y.; Li, Y.; Clemens, S.; Lv, H.; Huang, Z.; Wang, H.; Hu, X.; Lu, F.; Zhang, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wang, Y. <i>et al.</i>","Englishabstract":"East Asian monsoon variability in the Pliocene warm world has not been sufficiently studied because of the lack of direct records. We present a high-resolution precipitation record from Pliocene fluvial-lacustrine sequences in the Weihe Basin, Central China, a region sensitive to the East Asian monsoon. The record shows an abrupt monsoon shift at ~4.2 million years ago, interpreted as the result of high-latitude cooling, with an extratropical temperature decrease across a critical threshold. The precipitation time series exhibits a pronounced ~100–thousand year periodicity and the presence of precession and half-precession cycles, which suggest low-latitude forcing. The synchronous phase but mismatched amplitudes of the East Asian monsoon precipitation proxy and eccentricity suggest a nonlinear but sensitive precipitation response to temperature forcing in the Pliocene warm world. 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