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Geochemistry Characteristics of Elements in Loess in the Huining Profile in MIS3 and Climate Change
DI Xin-Wei, WU Song, LI Fu-Qiang
2013, 30 (1):
156-161.
Based on the geochemical data of elements and the paleoclimate proxies, the paleoclimate change in the Huining region during 20-70 kaBP was reconstructed. The geochemical results of elements showed that the contents of Ba, Rb, Sr, Ti, Fe2O3, SiO2, Al2O3, MgO and K2O were increased but those of CaO and Na2O were decreased with the decrease of loess depth along the profile. The proxies revealed that it was cold and dry during 69.9-55.5 ka (MIS4), and the quick loess accumulation was revealed by the low contents of Rb, Ti and Rb/Sr and the high contents of Na2O/Al2O3 and CaO/MgO. Compared with the data during the MIS4 period, the contents of Sr, Na2O and Na2O/Al2O3 were low during 55.5-23.8 ka (MIS3), those of Rb, Fe2O3, K2O and Rb/Sr were high, and they could be divided into three subparts (L1S1S2, L1S1L1 and L1S1S1). At the early stage (L1S1S2), 56.5-47.0 ka, it was slightly warm and rainy. During the mediumterm (L1S1L1), 47.0-28.6 ka, it was dry and cold. The Huining profile revealed that it was the driest and coldest period. The late stage (L1S1S1), 28.6-25.2 ka, was characterized by warm and rainy. It was cold and dry again at 25.2-23.2 ka (MIS2); Based on the geochemical data and proxies, five Heinrich events may be recorded in the Huining loess profile, i.e. the H2(22.36-23.32 ka), H3(30.5-31.5 ka), H4(38.2-39.2 ka), H5(43.0-44.0 ka) and H6(61.24-62.20 ka).
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