饶志国，博士，博导，湖南师范大学“潇湘****”****，教育部新世纪优秀人才，湖南省****青年基金获得者，湖南省青年芙蓉****。
学习经历：
2001.07：兰州大学，地理学学士学位
2004.07：兰州大学，自然地理学硕士学位
2007.07：中科院广州地球化学研究所，地球化学博士学位
2007.12-2012.07：兰州大学自然地理学博士后流动站，博士后
2009.09-2010.09：美国明尼苏达大学，访问****
2014.02-2014.07：台湾大学地质科学系，访问****
工作经历：
2007.08-2010.04：兰州大学西部环境与气候变化研究院，讲师
2010.05-2014.04：兰州大学西部环境与气候变化研究院，副教授
2014.05-2016.12：兰州大学西部环境与气候变化研究院，教授
2017.01-至今：湖南师范大学资源与环境科学学院，教授
主要研究领域：
利用有机地球化学和同位素地球化学研究方法，以黄土/泥炭/石笋/湖泊沉积物等为研究对象，从现代过程与沉积记录两个方面，开展与全球变化相关的研究。
目前主持的主要科研项目：
? 国家自然科学基金面上项目，在研。
? 湖南省****基金项目，在研。
已发表的主要学术论文(*为通讯作者):
[1]Li Yunxia, Tian Yiping, Guo Haichun, Wei Shikai, Cao Jiantao, Huang Chao, Shi Fuxi,Rao Zhiguo*. Complex ‘human-vegetation-climate’ interactions in the late Holocene and their significance for paleotemperature reconstructions. Proceedings of the National Academy of Sciences of the United States of America, 2020, doi: 10.1073/pnas. (SCI-1区; top journal).
[2]Li Yunxia,Rao Zhiguo*, Xu Qinghai, Zhang Shengrui, Liu Xiaokang, Wang Zongli, Cheng Hai, R. Lawrence Edwards, Chen Fahu. Inter-relationship and environmental significance of stalagmite δ¹³C and δ¹⁸O records from Zhenzhu Cave, north China, over the last 130 ka. Earth and Planetary Science Letters, 2020, 536, 116149 (SCI-1区; top journal).
[3]Rao Zhiguo*, Shi Fuxi, Li Yunxia, Huang Chao, Zhang Xinzhu, Yang Wen, Liu Lidan, Zhang Xinping, Wu Yi. Long-term winter/summer warming trends during the Holocene revealed by α-cellulose δ¹⁸O/δ¹³C records from an alpine peat core from central Asia.Quaternary Science Reviews, 2020, 232, 106217 (SCI-1区; top journal).
[4]Wu Dandan, Cao Jiantao, Jia Guodong, Guo Haichun, Shi Fuxi, Zhang Xinping,Rao Zhiguo*. Peat brGDGTs-based Holocene temperature history of the Altai Mountains in arid Central Asia. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 538, 109464 (SCI-2区; top journal).
[5]Shi Fuxi,Rao Zhiguo*, Li Yunxia, Cao Jiantao, Shi Xiaoyi, Li Chaozhu, Sun Weizhen. Precipitation δ¹⁸O recorded by the α‐cellulose δ¹⁸O of plant residues in surface soils: Evidence from a broad environmental gradient in inland China. Global Biogeochemical Cycles, 2019, 33, 1440-1468 (SCI-1区; top journal).
[6]Rao Zhiguo*, Huang Chao, Shi Fuxi, Zhang Xinzhu, Zhang Xinping. Reply to the comments on “Reconciling the ‘westerlies’ and ‘monsoon’ models: A new hypothesis for the Holocene moisture evolution of the Xinjiang region, NW China” by Dongliang Zhang and Yunpeng Yang. Earth-Science Reviews, 2019, 198, 102943 (SCI-1区; top journal).
[7]Liu Xiaokang,Rao Zhiguo, Shen Chuan‐Chou, Liu Jianbao, Chen Jianhui, Chen Shengqian, Wang Xianfeng, Chen Fahu*. Holocene Solar Activity Imprint on Centennial‐ to Multidecadal‐Scale Hydroclimatic Oscillations in Arid Central Asia. Journal of Geophysical Research: Atmospheres, 2019, 124, 2562-2573.
[8]Rao Zhiguo*, Wu Dandan, Shi Fuxi, Guo Haichun, Cao Jiantao, Chen Fahu. Reconciling the ‘westerlies’ and ‘monsoon’ models: A new hypothesis for the Holocene moisture evolution of the Xinjiang region, NW China. Earth-Science Reviews, 2019, 191, 263-272 (SCI-1区; top journal).
[9]Shi Fuxi,Rao Zhiguo*, Cao Jiantao, Huang Chao, Wu Dandan, Yang Wen, Weizhen Sun. Meltwater is the dominant water source controlling α-cellulose δ¹⁸O in a vascular-plant-dominated alpine peatland in the Altai Mountains, Central Asia. Journal of Hydrology, 2019, 572, 192-205 (SCI-1区; top journal).
[10]Li Yunxia, Zhang Shengrui, Liu Xiaokang, Gao Yongli,Rao Zhiguo*. Variations of the stable isotopic composition of precipitation and cave drip water at Zhenzu Cave, north China: A two-year monitoring study. Journal of Cave and Karst Studies, 2019, 81(2), 123-135.
[11]Rao Zhiguo*, Huang Chao, Xie Luhua, Shi Fuxi, Zhao Yan, Cao Jiantao, Gou Xiaohua, Chen Jianhua, Chen Fahu. Long-term summer warming trend during the Holocene in central Asia indicated by alpine peat a-cellulose δ¹³C record. Quaternary Science Reviews, 2019, 203, 56-67 (SCI-1区; top journal).
[12]Zhu Zhaoyu*, Dennell Robin*, Huang Weiwen, Wu Yi, Qiu Shifan, Yang Shixia,Rao Zhiguo, Hou Yamei, Xie Jiubing, Han Jiangwei, Ouyang Tingping. Hominin occupation of the Chinese Loess Plateau since about 2.1 million years ago. Nature, 2018, 559(7715), 608-612 (SCI-1区; top journal).
[13]Cao Jiantao,Rao Zhiguo*, Jia Guodong, Xu Qinghai, Chen Fahu. A 15 ka pH record from an alpine lake in north China derived from the cyclization ratio index of aquatic brGDGTs and its paleoclimatic significance. Organic Geochemistry, 2017, 109, 31-46 (SCI-2区).
[14]Li Yunxia*,Rao Zhiguo, Cao Jiantao, Jiang Hong, Gao Yongli. Highly negative oxygen isotopes in precipitation in southwest China and their significance in paleoclimatic studies. Quaternary International, 2017, 440, 64-71.
[15]Rao Zhiguo*, Guo Wenkang, Cao Jiantao, Shi Fuxi, Jiang Hong, Li Chaozhu. Relationship between the stable carbon isotopic composition of modern plants and surface soils and climate: A global review. Earth-Science Reviews, 2017, 165, 110-119 (SCI-1区; top journal).
[16]Rao Zhiguo*, Li Yunxia, Zhang Jiawu, Jia Guodong, Chen Fahu. Investigating the long-term palaeoclimatic controls on the δD and δ¹⁸O of precipitation during the Holocene in the Indian and East Asian monsoonal regions.Earth-Science Reviews, 2016, 159, 292-305 (SCI-1区; top journal).
[17]Rao Zhiguo*,Jia Guodong, Li Yunxia, Chen Jianhui, Xu Qinghai, Chen Fahu. Asynchronous evolution of the isotopic composition and amount of precipitation in north China during the Holocene revealed by a record of compound-specific carbon and hydrogen isotopes of long-chainn-alkanes from an alpine lake. Earth and Planetary Science Letters, 2016, 446, 68-76 (SCI-1区; top journal).
[18]Li Guoqiang*,Rao Zhiguo, Duan Yanwu, Xia Dunsheng, Wang Leibin, Madsen David, Jia Jia, Wei Haitao, Qiang Mingrui, Chen Jianhui, Chen Fahu. Paleoenvironmental changes recorded in a luminescence dated loess/paleosol sequence from the Tianshan Mountains, arid central Asia, since the Penultimate Glaciation. Earth and Planetary Science Letters, 2016, 448, 1-12 (SCI-1区; top journal).
[19]Rao Zhiguo*, Qiang Mingrui, Jia Guodong, Li Yunxia, Dan Dan, Chen Fahu. A 15 ka lake water δD record from Genggahai Lake, northeastern Tibetan Plateau, and its paleoclimatic significance.Organic Geochemistry, 2016, 97, 5-16 (SCI-2区).
[20]Rao Zhiguo*, Guo Wenkang, Xie Luhua, Huang Chao, Liu Xiaokang, Hua Hui, Chen Fahu.High resolution δ¹³C_TOCand magnetic susceptibility data from the late Early Pleistocene southern margins of the Chinese Loess Plateau.Organic Geochemistry, 2015, 87, 78-85 (SCI-2区).
[21]Liu Xiaokang,Rao Zhiguo*, Zhang Xiaojian, Huang Wei, Chen Jianhui, Chen Fahu. Variations in the oxygen isotopic composition of precipitation in the Tianshan Mountains region and their significance for the Westerly circulation.Journal of Geographical Sciences, 2015, 25(7), 801-816.
[22]Rao Zhiguo*,Liu Xiaokang, Hua Hui, Gao Yongli, Chen Fahu. Evolving history of the East Asian summer monsoon intensity during the MIS5: inconsistent records from Chinese stalagmites and loess deposits.Environmental Earth Sciences, 2015, 73, 3937-3950.
[23]Rao Zhiguo*, Jia Guodong, Qiang Mingrui, Zhao Yan. Assessment of the difference between mid- and long chain compound specific δD_n-alkanesvalues in lacustrine sediments as a paleoclimatic indicator. Organic Geochemistry, 2014, 76, 104-117 (SCI-2区).
[24]Rao Zhiguo, Chen Fahu, Cheng Hai, Liu Weiguo, Wang Guo’an, Lai Zhongping, Jan Bloemendal. High-resolution summer precipitation variations in the western Chinese Loess Plateau during the last glacial. Scientific Reports, 2013, 3, 2785 (SCI-2区).
[25]Rao Zhiguo, Xu Yuanbin, Xia Dunsheng, Xie Luhua, Chen Fahu. Variation and paleoclimatic significance of organic carbon isotopes of Ili loess in arid Central Asia. Organic Geochemistry, 2013, 63, 56-63 (SCI-2区).
[26]Rao Zhiguo, Chen Fahu, Zhang Xiao, Xu Yuanbin, Xue Qian, Zhang Pingyu. Spatial and temporal variations of C₃/C₄relative abundance in global terrestrial ecosystem since the Last Glacial and its possible driving mechanisms. Chinese Science Bulletin, 2012, 57(31), 4024-4035.
[27]Rao Zhiguo, Zhu Zhaoyu, Jia Guodong, Zhang Xiao, Wang Suping. Compound-specific hydrogen isotopes of long-chainn-alkanes extracted from topsoil under a grassland ecosystem in northern China. Science China (Earth Sciences), 2011, 54(12), 1902-1911.
[28]Xue Qian,Rao Zhiguo^*, Wang Suping, Zhang Pingyu, Chen Fahu. Stable carbon and oxygen isotopic study of carbonate along a loess/paleosol section located in southeastern edge of the Chinese Loess Plateau. Environmental Earth Sciences, 2011, 64(1), 237-246.
[29]Rao Zhiguo, Wu Yi, Zhu Zhaoyu, Jia Guodong, Andrew C.G. Henderson. Is the maximum carbon number of long-chainn-alkanes an indicator of grassland or forest? Evidence from surface soils and modern plants. Chinese Science Bulletin, 2011, 56(16), 1714-1720.
[30]Rao Zhiguo, Zhu Zhaoyu, Jia Guodong, Chen Fahu, Loukas Barton, Zhang Jiawu, Qiang Mingrui. Relationship between climatic conditions and the relative abundance of modern C₃and C₄plants in three regions around the North Pacific. Chinese Science Bulletin, 2010, 55(18), 1931-1936.
[31]Rao Zhiguo, Zhu Zhaoyu, Jia Guodong, Andrew C.G. Henderson, Xue Qian, Wang Suping. Compound-specific δD of long-chainn-alkanes derived from terrestrial higher plants are indicative of the δD of meteoric waters: Evidence from surface soils in eastern China. Organic Geochemistry, 2009, 40(8), 922-930 (SCI-2区).
[32]Rao Zhiguo, Jia Guodong, Zhu Zhaoyu, Wu Yi, Zhang Jiawu. Comparison of the carbon isotope composition of total organic carbon and long-chainn-alkanes from surface soils in eastern China and their significance. Chinese Science Bulletin, 2008, 53(24), 3921-3927.
[33]Rao Zhiguo, Zhu Zhaoyu, Zhang Jiawu. Different climatic controls of soil δ¹³C_orgin three mid-latitude regions of the Northern Hemisphere since the Last Glacial period. Chinese Science Bulletin 2007, 52(2), 259-266.
[34]Rao Zhiguo, Zhu Zhaoyu, Chen Fahu, Zhang Jiawu. Does δ¹³C_carbof the Chinese loess indicate past C₃/C₄abundance? A review of research on stable carbon isotopes of the Chinese loess. Quaternary Science Reviews, 2006, 25(17/18), 2251-2257 (SCI-1区, top journal).
[35]Rao Zhiguo,Zhu Zhaoyu, Wang Suping, Jia Guodong, Qiang Mingrui, Wu Yi. CPI values of terrestrial higher plant-derived long-chainn-alkanes: a potential paleoclimatic proxy. Frontier of Earth Science in China, 2009, 3(3), 266-272 (非SCI).
联系方式：raozhg@hunnu.edu.cn; **.欢迎专业和英语基础好，思维活跃，能吃苦耐劳的有志青年报考硕士和博士研究生。

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