Fig. 2: Variations in brGDGTs parameters compared with the parameters of other records. | Nature Communications

Fig. 2: Variations in brGDGTs parameters compared with the parameters of other records.

From: Decoupled Asian monsoon intensity and precipitation during glacial-interglacial transitions on the Chinese Loess Plateau

Fig. 2

a The pH calibration based on 5- and 6-methyl branched glycerol dialkyl glycerol tetraethers (brGDGTs, dark blue solid line, this study) and mean annual average temperature (MAT) calibration based on 5- and 6-methyl brGDGTs (dark red solid line, this study). b The mean grain size (mm) (MGS, blue solid line, this study) and magnetic susceptibility (orange solid line, this study). c The mean annual average precipitation (MAPc) values reconstructed by the brGDGT-MAP model (Weinan, dark green solid line, this study). d The MAP values reconstructed by 10Be (Baoji, purple solid line). e The variations in Sanbao δ18O (the dark blue solid line indicates the results of the five-point average). f The changes in the MBT’ (dark red solid line), representing the soil water content (SWC) variations36. g The changes in sea level (blue solid line)57. h The solar radiation at 65°N (black solid line)42. i The benthic foraminifera-derived δ 18O stack (dark blue solid line)41. The orange and yellow bars represent the loess–paleosol cycles in the Weinan profile. The gray shading bars represent the interglacial periods in the Weinan profile, and the light-yellow bars highlight the decoupled periods between the 10Be reconstructions and our results.

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