Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years

By Yongjin Wang, Hai Cheng, R. Edwards, X. Kong, X. Shao, Shitao Chen, Jiangying Wu, X. Jiang, Xianfeng Wang, Z. An. Nature, 2008

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High plant endemism in China is partially linked to reduced glacial‐interglacial climate change (2016, background): “Also, several studies reported high millennial-scale variability in monsoon strength and precipitation in China across the Late Pleistocene and Holocene (Wang et al., 2001, 2008).”
Climatic Fluctuations and Early Farming in West and East Asia (2011, background): “Other caves include Dongge (Dykoski et al. 2005), Heshang (Hu et al. 2005), Qingtian (Liu et al. 2008), Sanbao (Wang et al. 2008), Songjia (Zhou et al. 2008), and Timta in Tibet (Sinha et al. 2005).”
Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core (2013, background): “The sequence of the last 8 glacial cycles documented in natural paleoclimate archives (Lisiecki and Raymo, 2005; Wang et al., 2008; Wolff et al., 2006; EPICA community members, 2006; Pahnke and Zahn, 2005; Elderfield et al., 2012) is characterized by irregular 100 000 yr cycles, whose association to”
Astronomical and glacial forcing of East Asian summer monsoon variability (2015, neutral): “From a modern meteorological perspective, changes in southerly wind intensity, sea level pressure and summer precipitation within a certain domain can be employed as monsoonal proxies (Wang et al., 2008a).”