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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

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 kyrs

Fig. 6

Comparison of temporal change patterns in between several EASM proxies. a ESR signal intensity in the fine silt fraction (4–16 μm) of MD06-3040 core sediments (this study). b ESR signal intensity in the fine silt fraction (4–20 μm) of D-GC-6 core sediments (Nagashima et al. 2013). c δ18Osw, an indicator of the sea surface salinity (SSS), at the KY07-04-01 site in the northern ECS during the Holocene based on paired analyses of Mg/Ca and δ18O of planktonic foraminifera (Kubota et al. 2010, 2015), where the black thin line represents the 3-point moving average. d δ18O record of a stalagmite from Heshang Cave (Hu et al. 2008). e δ18O record of a stalagmite from Dongge Cave D4 (Dykoski et al. 2005). The calibrated 14C dates of the MD06-3040 and KY07-04-01 cores are presented with 2σ errors on the top of the figures

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