Cold events of Holocene indicated by primary elements distribution of the high-resolution sand dunes in the Salawusu River Valley
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- 作者：Dongfeng Niu (1) (3)
Baosheng Li (1) (2)
Shuhuan Du (1)
Xiaohao Wen (1)
Shifan Qiu (1)
Xianjiao Ou (1)
Yi Yang (1) - 关键词：Salawusu River Valley ; Holocene ; dune sands ; primary elements ; cold events
- 刊名：Journal of Geographical Sciences
- 出版年：2008
- 出版时间：February 2008
- 年：2008
- 卷：18
- 期：1
- 页码：26-36
- 全文大小：445KB
- 参考文献：1. Bond G, Showers W, Cheseby M / et al., 1997. A pervaasive millennial-scale cycle in North Atlantic Holocene and glacial climates. / Science, 278: 1257-264. CrossRef
2. Chen Fahu, Zhu Yan, Li Jijun / et al., 2001. Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales: Evidence from lake sediment document in Minqin Basin, NW China. / Chinese Science Bulletin, 46(11): 1942-948. (in Chinese)
3. de Menocal P, Ortiz J, Guilderson T, Sarnthein M, 2000. Coherent high-and low-latitude climate variability during the Holocene warm period. / Science, 288: 2198-202. CrossRef
4. Dong Guangrong, Gao Shangyu, Li Baosheng, 1982. New discovery of the Fossil Ordos Man. / Chinese Science Bulletin, 27(7): 754-58. (in Chinese)
5. Dong Guangrong, Li Baosheng, Gao Shangyu, 1983. The case study of the vicissitude of Mu Us Sandy Land since the Late Pleistocene according to the Salawusu River area strata. / Journal of Desert Research, 3(2): 9-4. (in Chinese)
6. Editorial Committee of Geological Society of China, 1956. Geology Research Institute, Chinese Academy of Science. Region Stratigraphical Tables in China, First Draft. Beijing: Science Press, 167-87. (in Chinese)
7. Jia Lanpo, 1950. The Ordos Fossil Man. Shanghai: Longmen United Publishing House, 1-9. (in Chinese)
8. Jian Zhimin, Meng Yi, 2002. Holocene paleoenvironmental changes in the Yangtze River mouth and their responses to the variations in the Kuroshio current. / Marine Geology & Quaternary Geology, 22(3): 77-2. (in Chinese)
9. Li Baosheng, Dong Guangrong, Gao Shangyu / et al., 1987. Relationship between the Malan Loess and the Salawusu Formation in the Salawusu River area, Ordos, and their geological age. / Acta Geologica Sinica, 61(3): 218-30. (in Chinese)
10. Li Baosheng, Dong Guangrong, Gao Shangyu, 1991. The changes in climatic environment of the Salawusu River area since the terminal stage of Mid-Pleistocene as indicated by detrital minerals in Quaternary sediments. / Acta Petrologica of Mineralogica, 10(1): 84-0. (in Chinese)
11. Li Baosheng, Dong Guangrong, Wu Zheng / et al., 1993. The establishment of the Upper Pleistocene Chengchuan Formation in northern China. / Geological Review, 39(2): 91-00. (in Chinese)
12. Li Baosheng, Jin Heling, Lu Haiyan / et al., 1998. Processes of the deposition and vicissitude of Mu Us Desert, China since 150,000 a B. P. / Science in China (Series D), 41(3): 248-54. (in Chinese)
13. Li Houxin, Li Baosheng, Zhu Yizhi / et al., 2002. The change cycles of major element in Salawusu River valley since 150,000 a B. P. / Geochimica, 31(5): 424-32. (in Chinese)
14. Liu Jiaqi, Lu Houyuan, Negendank J / et al., 2000. Periodicity of Holocene climatic variations in the Huguangyan Maer Lake. / Chinese Science Bulletin, 45(11): 1190-195. (in Chinese) CrossRef
15. Liu Yufei, Li Baosheng, Yang Yi / et al., 2006. Moving and accumulating law of Bb, Sr with environment evolving in semiarid basin of China during the last interglacial-reflected by study result on Milanggouwan stratigraphic section in the Salawusu River valley. / Journal of Desert Research, 26(3): 341-44. (in Chinese)
16. Luo Kaili, Li Baosheng, Zhu Yizhi / et al., 2002. CaCO3 cycles in Salawusu River Basin since 150ka B P. / Scientia Geographica Sinica, 22(5): 683-88. (in Chinese)
17. Ou Xianjiao, Li Baosheng, Jin Heling / et al., 2006. Sedimentary characteristics of paleo-eolian dune sands in Salawusu Formation of the Salawusu River Valley. / Acta Geographica Sinica, 61(9): 965-75. (in Chinese)
18. Ouyang Chuntao, Li Baosheng, Ou Xianjiao / et al., 2007. Chemical weathering of the Milanggouwan paleosols in the Salawusu River Valley and their paleoclimatic implication during the Last Interglacial Period. / Acta Geographica Sinica, 62(5): 518-28. (in Chinese)
19. Stuiver M, Reimer P J, Bard E / et al., 1998. INTCAL98 radiocarbon age calibration 24000? cal aBP. / Radiocarbon, 40: 1041-083.
20. Su Zhizhu, Dong Guangrong, 1994. Recent progress on Quaternary research of Salawusu River area in Inner Mongolia. / Arid Land Geography, 17(4): 1-. (in Chinese)
21. Taylre K C, Lamorey G W, Doyle G A / et al., 1993. The flickering switch of Late Pleistocene climate change. / Nature, 361: 432-36. CrossRef
22. Teilhard de Chardin P, Licent E, 1924. On the discovery of a paleolithic industry in northern China. / Bulletin of the Geological Society of China, 3(1): 45-0.
23. Wang Shaowu, Xie Zhihui, 2002. Climate variability at millennial time scales. / Earth Science Frontiers, 9(1): 143-53. (in Chinese)
24. Wang Yuping. The paleolithic culture of Sjara-Osso-Gol River area, Wushen Banner. Selected Writings of the Historical Relics Data, Inner Mongolia. Hohhot: Inner Mongolia Press, 1964. 9-6. (in Chinese)
25. Woo Jukang, 1958. Fossil human parietal bone and femur from Ordos. / Vertebrata Palasiatica, 2(1): 208-10. (in Chinese)
26. Yao Tandong, Shi Yafeng, 1992. Climatic changes of Holocene reflected in the ice core from Dunde, Qilian Mountains. In: Shi Yafeng, Kong Zhaochen (eds.). The Climates and Environments of Holocene Megathermal in China. Beijing: China Ocean Press, 206-11. (in Chinese)
27. Zhang Yuhong, Li Baosheng, Jin Heling / et al., 2001. Grain-size cycles in Salawusu River Valley since 150 ka BP. / Acta Geographica Sinica, 11(4): 461-72. (in Chinese)
28. Zhou Kunshu, Li Xingguo, Shao Yajun, 1982. The permafrost period subdivision in the Salawusu River reaches, Inner Mongolia, and its significance. In: Contribution to the Academic Symposium on the Pre-Historic Earth-quake and Geology of China. Xi’an: Shaanxi Science and Technology Press, 149-53. (in Chinese)
29. Zhou Weijian, Lu Xuefeng, Wu Zhengkun / et al., 2002. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating. / Chinese Science Bulletin, 47(1): 66-0. (in Chinese) CrossRef - 作者单位：Dongfeng Niu (1) (3)
Baosheng Li (1) (2)
Shuhuan Du (1)
Xiaohao Wen (1)
Shifan Qiu (1)
Xianjiao Ou (1)
Yi Yang (1)
1. School of Geography, South China Normal University, Guangzhou, 510631, China
3. Baotou Vocational & Technical College, Baotou, 010022, China
2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi’an, 710061, China - ISSN：1861-9568
文摘
The components of the primary elements in the dune sands for the MGS1 subsection of the Milanggouwan section in the Salawusu River valley, compared with those of modern dune sands, show that they were caused by East Asian winter monsoon in the Mu Us desert during Holocene. The examined ages for the 11 layers of dune sands, based on the average sedimentary rate, are: 0 to 960, 1350-240, 2470 to 3530, 4000 to 4180, 4290 to 4350, 4380 to 4760, 5040 to 5920, 6570 to 8270, 9020 to 9700, 9880 to 10160 and 10580 to 11080 a BP, respectively. The climatic events indicated by these dune sands are consistent with those records in the Huguangyan volcanic lake, Zoige peat bog, Hulu cave and Dunde ice core, particularly with the climatic fluctuations of the North Atlantic since 11 000 a BP. Among them, patterns from B0 to B8 correspond to the peak values of 0MD, 2D, 4D, 6D+8D+10D, 12D, 14D, 16D, 18D and 20D respectively. It might be caused by the North Atlantic ice age induced by the heat circulation, which strengthened the polar high pressure and Siberian-Mongolian high pressure and further led to the dominance of the winter monsoon over China’s desert area.