个人简介
1993．9－1997．6 南京师范大学 本科
1997．9－2000．6 南京师范大学 硕士
2000．9－2003．6 南京大学 博士
2003．6－2005．9 南京师范大学 博士后
2003．10－2004．1 澳大利亚昆士兰大学 访问学者 从事U系测年工作
2005．9－2007．5 南京师范大学 讲师
2007．5－ 南京师范大学 副教授
近期论文
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1. J.Y. Wu, Y.J. Wang, H. Cheng, et al. Stable isotope and trace element investigation of two contemporaneous annually-laminated stalagmites from northeastern China surrounding the “8.2ka event”. Climate of the Past, 8, 1497–1507, 2012, www.clim-past.net/8/1497/2012/ doi:10.5194/cp-8-1497-2012
2. 吴江滢，汪永进，董进国. 2011. 全新世东亚夏季风演化的辽宁暖和洞石笋δ18O记录. 第四纪研究，31(6): 990-998. （11月）
3. Wu J Y, Wang Yongjin, Cheng Hai, et al. 2009. An exceptionally strengthened East Asian summer monsoon event between 19.9 and 17.1 ka BP recorded in a Hulu stalagmite. Science in China (Series D), 52(3): 360-368. （三月）
4. Wu J Y, Shao X H, Kong X G, Wang Y J. 2006. Imprint of solar activity onNanjingstalagmite annual layer thickness sequence during the Last Glacial Maximum. Chinese Science Bulletin, 51(4): 441-447.
5. 吴江滢，邵晓华，汪永进. 2007. 南京年纹层石笋d18O记录的冰期气候事件特征. 地理科学. 27(1): 75-80.
6. 吴江滢，汪永进， 孔兴功. 2006. 贵州白骨洞石笋记录的全新世季风气候演化与突变. 海洋地质与第四纪地质. 26(5): 55-60
7.Wu Jiangying. 2007. Comparison Between δ18O and annual layer thickness fromNanjingstalagmite during the Last Glacial Maximum. Journal ofNaturalScienceNanjingNormalUniversity, 9(1): 52-57.
8. Yongjin Wang, Hai Cheng, R Lawrence Edwards, Xinggong Kong, Xiaohua Shao, Shitao Chen, Jiangying Wu, et al. 2008. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature, 451:1090-1093
9. Dianbing Liu, Yongjin Wang, Hai Cheng, R. Lawrence Edwards, Xinggong Kong, Xianfeng Wang, Jiangying Wu, et al. 2008. A detailed comparison of Asian Monsoon intensity andGreenlandtemperature during the Aller?d and Younger Dryas events. Earth and Planetary Science Letters, 272: 691-697
10. 张伟宏，吴江滢. 2012. 辽宁暖和洞石笋δ13C对全新世气候变化的生态响应. 海洋地质与第四纪地质，32(3): 147-154.
11. 郭允，吴江滢，汪永进，等. 2012. 辽宁本溪暖和洞早全新世石笋年纹层记录. 海洋地质与第四纪地质，32(2): 135-141.
12. 顾宁，吴江滢. 2012. 辽宁暖和洞石笋δ13C记录的古气候环境意义初探. 中国岩溶，31(2): 107-114.
13. 张伟，段武辉，吴江滢，等. 2012. 南京葫芦洞缺失现代沉积的一个重要原因：盐效应？—与同一气候条件下安徽蓬莱仙洞的对比观测研究. 第四纪研究，32(2): 361-367.
14. 姜修洋，孔兴功，汪永进，CHENG Hai，吴江滢，等. 2010. 深海氧同位素8期东亚夏季风旋回与事件的湖北神农架洞穴记录. 科学通报，55 (8): 698 -704.
15. Jinguo Dong, Yongjin Wang, Hai Cheng, Ben Hardt, R. Lawrence Edwards, Xinggong Kong, Jiangying Wu, et al. 2010. A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, centralChina.
16. Dianbing Liu, YongjinWang, Hai Cheng, R. Lawrence Edwards, Xinggong Kong, XianfengWang, Ben Hardt, Jiangying Wu, et al. 2010. Sub-millennial variability of Asian monsoon intensity during the early MIS 3 and its analogue to the ice age terminations.
17. Daoxian Yuan, Hai Cheng, R. Lawrence Edwards, Carolyn A. Dykoski, Megan J. Kelly, Meiliang Zhang, Jiaming Qing, Yushi Lin, Yongjin Wang, Jiangying Wu, Jeffery A. Dorale, Zhisheng An, and Yanjun Cai. 2004. Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon. Science, 304: 575-578.
18. Wang Y J, Cheng H, Edwards R L, He Y Q, Kong X G, Wu J Y, et al. 2005. The Holocene Asian Monsoon: links to solar changes andNorth Atlanticclimate. Science, 2005, 308: 854-857.
19. Kong Xinggong, Wang Yongjin, Wu Jiangying, et al. 2005. Complicated responses of stalagmite d13C to climate change during the last glaciation fromHuluCave,Nanjing,China. Science inChina, 48(12): 2174-2181.
20. Jiang Xiuyang, Wang Yongjin, Kong Xinggong, Wu Jiangying, et al. 2005. Abrupt climate change of East Asian Monsoon at 130 kaBP inferred from a high resolution stalagmite δ18O record. Chinese Science Bulletin, 50(23): 2765 – 2769.
21.X. H. Shao, Y. J. Wang, H. Cheng, X. G. Kong, J. Y. Wu, R. L. Edwards. 2006. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China. Chinese Science Bulletin, 51(2): 221-228.
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