Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1): 71-86.
[2]
Hong Y T, Hong B, Lin Q H, et al. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene[J]. Earth and Planetary Science Letters, 2003, 211(3-4): 371-380.
[3]
Zhou W, Lu X, Wu Z, et al. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating[J]. Chinese Science Bulletin, 2002, 47(1): 66-70.
[4]
Chen F H, Cheng B, Zhao Y, et al. Holocene environmental change inferred from a high-resolution pollen record, Lake Zhuyeze, arid China[J]. The Holocene, 2006, 16(5): 675-684.
[5]
Li Yu, Wang Nai'ang, Li Zhuolun, et al. The relationships among organic geochemical proxies and their palaeoenvironmental significances in Zhuye Lake sediments[J]. Journal of Glaciology and Geocryology, 2011, 33(2): 334-341.[李育,王乃昂,李卓仑,等. 河西猪野泽沉积物有机地化指标之间的关系及古环境意义[J]. 冰川冻土, 2011, 33(2): 334-341.]
[6]
Jia Jia, Xia Dunsheng, Jin Ming, et al. Typical loess/paleosol sequences in Weihe drainage areas: Environmental magnetism features and paleoclimate interpretation[J]. Journal of Glaciology and Geocryology, 2010, 32(1): 91-97.[贾佳,夏敦胜,金明,等. 渭河流域典型黄土剖面的环境磁学特征及其古气候意义[J]. 冰川冻土, 2010, 32(1): 91-97.]
[7]
Jin H, Su Z, Sun L, et al. Holocene climatic change in Hunshandake Desert[J]. Chinese Science Bulletin, 2004, 49(16): 1730-1735.
[8]
Shen J, Liu X, Wang S, et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years[J]. Quaternary International, 2005, 136(1): 131-140.
[9]
Wu Y, Lücke A, Jin Z, et al. Holocene climate development on the central Tibetan Plateau: A sedimentary record from Cuoe Lake[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 234(2-4): 328-340.
[10]
Mischke S, Zhang C. Holocene cold events on the Tibetan Plateau[J]. Global and Planetary Change, 2010, 72(3): 155-163.
[11]
Liu B, Jin H, Sun L, et al. Holocene climatic change revealed by aeolian deposits from the Gonghe Basin, northeastern Qinghai-Tibetan Plateau[J]. Quaternary International, 2013, 296: 231-240.
[12]
Bryson R A. Airstream climatology of Asia[C]//Proceedings of the International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology. Boston, MA: American Meteorological Society, 1986: 604-617.
[13]
Xu Shuying, Zhang Weixin, Xu Defu, et al. Discussion on the periglacial development in the northeast marginal region of Qinghai-Xizang Plateau[J]. Journal of Glaciology and Geocryology, 1984, 6(2): 15-25.[徐叔鹰,张维信,徐德馥,等. 青藏高原东北边缘地区冰缘发展探讨[J]. 冰川冻土, 1984, 6(2): 15-25.]
[14]
Pan Baotian, Xu Shuying, Chen Fahu, et al. Discussion the sequence and extent of changes of natural environment in the eastern Qinghai Plateau during the past 30,000 years[J]. Arid Land Geography, 1989, 12(2): 14-21.[潘保田,徐叔鹰,陈发虎,等. 青海高原东部三万年来自然环境变迁的序列与幅度探讨[J]. 干旱区地理, 1989, 12(2): 14-21.]
[15]
Dong Guangrong, Gao Shangyu, Jin Jiong. Land Desertification and Its Control in Gonghe Basin, Qinghai Province[M]. Beijing: Science Press, 1993: 10-33.
[16]
Gao Shangyu, Chen Weinan, Jin Heling, et al. Preliminary study on the deserts evolution at the northwestern edge of Monsoon Area, China during Holocene Epoch[J]. Science in China (Series B), 1993, 23(2): 202-208.[高尚玉,陈渭南,靳鹤龄,等. 全新世中国季风区西北缘沙漠演化初步研究[J]. 中国科学(B辑), 1993, 23(2): 202-208.]
[17]
Gao Shangyu, Wang Guiyong, Ha Si, et al. A case study on desert evolution in the northwestern fringe of monsoon area, China since the last glacial epoch[J]. Quaternary Sciences, 2001, 21(1): 66-71.[高尚玉,王贵勇,哈斯,等. 末次冰期以来中国季风区西北边缘沙漠演化研究[J]. 第四纪研究, 2001, 21(1): 66-71.]
[18]
Cheng Bo, Chen Fahu, Zhang Jiawu. Palaeovegetational and palaeoenvironmental changes in Gonghe Basin since last deglaciation[J]. Acta Geographica Sinica, 2010, 65(11): 1336-1344.[程波,陈发虎,张家武. 共和盆地末次冰消期以来的植被和环境演变[J]. 地理学报, 2010, 65(11): 1336-1344.]
[19]
Liu X, Dong H, Rech J A, et al. Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene-Holocene[J]. Quaternary Science Reviews, 2008, 27(7-8): 867-879.
[20]
Liu Bing, Jin Heling, Sun Zhong. Progress of studies of climate and environmental changes in Gonghe basin, northeastern Tibetan Plateau, since the Last Glacial Maximum period[J]. Journal of Glaciology and Geocryology, 2012, 34(2): 403-410.[刘冰,靳鹤龄,孙忠. 末次盛冰期以来青藏高原东北部共和盆地气候与环境变化研究进展[J]. 冰川冻土, 2012, 34(2): 403-410.]
[21]
Kukla G, Heller F, Liu X M, et al. Pleistocene climates in China dated by magnetic susceptibility[J]. Geology, 1988, 16(9): 811-814.
[22]
Porter S C,An Z. Correlation between climate events in the North Atlantic and China during the last glaciations[J]. Nature, 1995, 375: 305-308.
[23]
PyeK, Tsoar H. The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the northern Negev, Israel[J]. Geological Society, London, Special Publications, 1987, 35: 139-156.
[24]
Lü L, Fang X, Lu H, et al. Millennial-scale climate change since the last glaciation recorded by grain sizes of loess deposits on the northeastern Tibetan Plateau[J]. Chinese Science Bulletin, 2004, 49(11): 1157-1164.
[25]
Ding Z, Sun J, Liu D. A sedimentological proxy indicator linking changes in loess and deserts in the Quaternary[J]. Science in China (Series D), 1999, 42(2): 146-152.
Mu Baolei. Geochemistry of Elements[M]. Beijing: Peking University Press, 1999: 1-245.
[28]
Pang Jiangli, Huang Chunchang, Zhang Zhanping. Pb, Cu, Zn, Cd, Mn element and climatic change in loess-paleosol profile at Qishan, Shaanxi Province[J]. Journal of Desert Research, 2001, 21(2): 151-156.[庞奖励,黄春长,张占平. 陕西五里铺黄土微量元素组成与全新世气候不稳定性研究[J]. 中国沙漠, 2001, 21(2): 151-156.]
[29]
Yao Tandong, Shi Yafeng, Thompson L G, et al. Climatic changes of Holocene reflected in the ice core from Dunde, Qilian Mountains[C]//Shi Yafeng, Kong Zhaochen. The Climates and Environments of Holocene Megathermal in China. Beijing: China Ocean Press, 1992: 206-211.[姚檀栋,施雅风,Thompson L G,等. 祁连山敦德冰芯记录的全新世气候变化[C]//施雅风,孔昭宸. 中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992: 206-211.]
[30]
Lu H, Zhao C, Mason J, et al. Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J]. The Holocene, 2011, 21(2): 297-304.
[31]
Herzschuh U, Winter K, Wünnemann B, et al. A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra[J]. Quaternary International, 2006, 154-155: 113-121.
[32]
Wang N, Yao T, Thompson L G, et al. Evidence for cold events in the early Holocene from the Guliya ice core, Tibetan Plateau, China[J]. Chinese Science Bulletin, 2002, 47(17): 1422-1427.
[33]
Thompson L G, Yao T, Davis M E, et al. Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau[J]. Annals of Glaciology, 2006, 43: 61-69.
[34]
Thompson L G. Ice core evidence for climate change in the Tropics: implications for our future[J]. Quaternary Science Reviews, 2000, 19(1-5): 19-35.
[35]
Schlütz F, Lehmkuhl F. Holocene climatic change and the nomadic Anthropocene in Eastern Tibet: palynological and geomorphological results from the Nianbaoyeze Mountains[J]. Quaternary Science Reviews, 2009, 28: 1449-1471.
[36]
Phadtare N R. Sharp decrease in summer monsoon strength 4000-3500 cal yr B. P. in the Central Higher Himalaya of India based on pollen evidence from alpine peat[J]. Quaternary Research, 2000, 53(1): 122-129.
[37]
Chen Fahu, Wang Shilan, Zhang Weixin, et al. The loess profile at south bank, climatic information and lake-level fluctuations of Qinghai Lake during the Holocene[J]. Scientia Geographica Sinica, 1991, 11(1): 76-85, 100.[陈发虎,汪世兰,张维信,等. 青海湖南岸全新世黄土剖面、 气候信息及湖面升降探讨[J]. 地理科学, 1991, 11(1): 76-85, 100.]
[38]
Zhang C, Mischke S. A Lateglacial and Holocene lake record from the Nianbaoyeze Mountains and inferences of lake, glacier and climate evolution on the eastern Tibetan Plateau[J]. Quaternary Science Reviews, 2009, 28(19-20): 1970-1983.
[39]
Chen Fahu, Huang Xiaozhong, Yang Meilin, et al. Westerly dominated Holocene climatic model in arid Central Asia-case study on Bosten Lake, Xinjiang, China[J]. Quaternary Sciences, 2006, 26(6): 881-887.[陈发虎,黄小忠,杨美临,等. 亚洲中部干旱区全新世气候变化的西风模式——以新疆博斯腾湖记录为例[J]. 第四纪研究, 2006, 26(6): 881-887.]
[40]
Zhang C, Zhang W, Feng Z, et al. Holocene hydrological and climatic change on the northern Mongolian Plateau based on multi-proxy records from Lake Gun Nuur[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 323-325: 75-86.
[41]
Yi S, Saito Y, Zhao Q, et al. Vegetation and climate changes in the Changjiang (Yangtze River) Delta, China, during the past 13,000 years inferred from pollen records[J]. Quaternary Science Reviews, 2003, 22(14): 1501-1519.
[42]
Jin H L, Sun L Y, Sun Z. Millennial-scale evolution of Hunshandake Desert and climate change during the Holocene in Inner Mongolia, northern China[J]. Sciences in Cold and Arid Regions, 2010, 2(6): 505-513.
[43]
Dobrovolsky V V. Geography of Microelements: Global Dispersion[M]. Moscow: Mysl', 1983: 1-95. (in Russian)
[44]
Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates[J]. Science, 1997, 278(5341): 1257-1266.
[45]
O'Brien S R, Mayewski P A, Meeker L D, et al. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science, 1995, 270(5244): 1962-1964.
[46]
Bianchi G G, McCave I N. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland[J]. Nature, 1999, 397(6719): 515-517.
[47]
Linsley B K. Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150,000 years[J]. Nature, 1996, 380: 234-237.
