Fig. 5.From: Provenance changes in fine detrital quartz in the inner shelf sediments of the East China Sea associated with shifts in the East Asian summer monsoon front during the last 6 kyrsa–d Comparison of the ESR signal intensity and CI of quartz in the fine silt fraction of MD06-3040 core sediments to those sediments from various parts of the modern Yangtze River drainage (Saito et al. 2017) for intervals 2 to 5 covering the last 6.0 kyr BP identified in this study. The circles represent the average values of the ESR signal intensity and CI of quartz during each individual intervalBack to article page