【摘要】 萨拉乌苏河流域米浪沟湾剖面末次间冰期层系记录了8 5个风成的古砂丘砂与河湖相或／和古土壤构成的沉积旋回。通过对该层系主元素含量分布规律的分析,认为所述沉积旋回主要是由干湿寒暖气候旋回波动所致。研究亦表明,末次间冰期层系60LS—82S可进一步划分为5个层段,它们在时间和气候的主要阶段上与氧同位素5阶段中之5a、5b、5c、5d、5e诸亚段相近。不仅如此,若干反映冷干气候的风成砂丘砂堆积层位与末次间冰期GRIP冰芯δ18O及西太平洋暖池planktonicδ18O记录的冷凉事件,特别是与黄土高原记录的9次粉尘事件在时间上具有很好的对应关系。更多还原

【Abstract】 The last interglacial strata sequence of Milanggouwan stratigraphic section in the Salawusu River valley has recorded 8^5 sedimentary cycles of aeolian sand alternatively interlaid with fluvio-lacustrine facies or paleosols. After analyzing the distributing regularity of major element contents in the strata, we considered that these sedimentary cycles were chiefly induced by cold-dry and warm-humid climate fluctuations. The study also showed that in the Milanggouwan section, the 60LS-82S depositional sequence formed during the last interglacial period can be further divided into five phases which closely match δ¹⁸O5a?δ¹⁸O5b?{δ¹⁸O5c}?δ¹⁸O5d?δ¹⁸O5e in periods and chief climatic stages. Moreover, many horizons of paleo-sand-dune reflecting cold|dry climate temporally corresponded to those cold events recorded by δ¹⁸O in GRIP Ice Core and planktonic δ¹⁸O in the warm pool of the Western Pacific Ocean, especially to the 9 aeolian dust （loess） events happened in the Loess Plateau of China during the Last Interglacial period.更多还原