Fig. 3From: Spatiotemporal patterns of sediment deposition on the northern slope of the South China Sea in the last 150,000 yearsMajor element compositions of the study sites DWL3101, MD12-3429 and MD12-3432. Al2O3, K2O, Na2O, CaO, P2O5, MgO and TiO2 concentrations of the silicate fractions from DLW3101, MD12-3429 and MD12-3432, with planktic foraminiferal oxygen isotopes data from DLW3101 (Zhou et al. 2018), MD12-3429 (Li et al. 2017) and MD12-3432 (Qu and Huang 2019). Gray bars highlight glacial periods with marine isotope stages (MIS) noted on the rightBack to article page