• 责任者：Liu Yuhang (Key Laboratory of Western Chinas Environmental Systems ; Ministry of Education ; Research School of Arid Environment & Climate Change ; Lanzhou University ; Lanzhou 730000 ; China) ; Xia Dunsheng
• 刊名：Quaternary Sciences
• 出版年：2012
• 卷期：32(4)
• 关键词：全新世 ; Holocene ; 环境磁学 ; environmental magnetism ; 新疆 ; Xinjiang
• 页码：p.803-811
• 图表：4 illus., 2 tables, 52 refs.
• 分类号：1400
• issnNo：ISSN1001-7410
• isbnNo：CN11-2708/P

The Wulungu Lake, located in Fuhai county, Xinjiang, Northwest China,traverses the area between 46°59’～47°25’N and 87°00’～87°35’E, with an area of 927 km² and a maximum depth of 16 m (average depth is 8 m).Two parallel cores, WLG10B with a length of 397 cm and WLG10C with a length of 271 cm,were obtained in the northeast corner of the lake area (47°21’50.5″N, 87°27’07.2″E). The result shows that the main magnetic minerals in the sediments are fine-grained ferrimagnetic minerals,with a small amount of anti-ferromagnetic and paramagnetic minerals. The climate change during the Holocene recorded by WLG10C is consistent with the records in its adjacent areas,and obeys “the arid Central Asian westerly mode”.