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姓名 郝青振 性别:
职称 研究员 学位 博士
电话 010-82998395 传真: 010-62010846
Email: haoqz (at) mail.iggcas.ac.cn 邮编: 100029
地址 北京朝阳区北土城西路19号,中科院地质与地球物理研究所
更多信息:
 
简历:

  郝青振,研究员,博士生导师。1971年出生于河北柏乡。1995年毕业于兰州大学,1998年于中国科学院兰州沙漠研究所获硕士学位,2001年于中国科学院地质与地球物理研究所获博士学位。 

  主要从事风尘堆积地层与古气候学研究,建立了西部黄土高原中新世上新世风成红土的磁性地层序列,揭示出风成红土的成壤组分和碎屑组分的磁学性质差异及其阶段性演化特点;开展下蜀黄土物源与古气候研究,发展了下蜀黄土近源说;利用黄土沉积发现地球偏心率长周期调控的北极冰盖滞后增长新规律,提出北半球当前温暖气候将继续维持至少4万年,轨道要素配置导致MIS15-13北半球出现超长间冰期,揭示出部分冰期可能由南极过程驱动 

  NatureGeology等国内外学术刊物发表论文56篇,SCI收录36篇,近5(2011-2015)SCI引用983(他引822)。曾主持多项国家自然科学基金、中科院创新方向项目课题等课题。现任中国土壤学会第十二届理事会土壤地质分专业委员会副主任。获2014年度国家自然科学二等奖(排名第二)、中国地质学会2012年度十大地质科技进展奖(排名第一) 

教育及工作简历 

  • 1991.09-1995.07,兰州大学,地质系,地质学专业,获理学学士学位;
  • 1995.09-1998.07,中国科学院兰州沙漠研究所,自然地理专业,获理学硕士学位;
  • 1998.09-2001.08,中国科学院地质与地球物理研究,第四纪地质专业,获理学博士学位;
  • 2001.09-2005.12,中国科学院地质与地球物理研究,新生代地质与环境研究室,助理研究员;
  • 2006.01-2012-12,中国科学院地质与地球物理研究,新生代地质与环境研究室,副研究员;
  • 2006.12-2007.12,英国利物浦大学,地理系,环境磁学实验室,博士后;
  • 2012.03-2012.09,英国利物浦大学,环境学院,古地磁实验室,访问学者;
  • 2013.01-今,   中国科学院地质与地球物理研究,新生代地质与环境研究室,研究员。 

Google Scholar Citations: http://scholar.google.com/citations?user=biA0pvsAAAAJ&hl=e

 
学科类别:
地质学
 
研究方向:
  • 研究方向:黄土地层与古气候
  • 研究区域:黄土高原、长江中下游地区;
  • 研究手段:常规理化分析(古风化强度、地球化学示踪、粒度等)、环境磁学;
  • 科学问题:下蜀黄土物源与北亚热带地区冰期环境演化、黄土与轨道时间尺度高纬气候变化的联系、轨道驱动相似型时期我国北方环境特征。
     
 
职务:
 
社会任职:
 
承担科研项目情况:
  1. 国家自然科学基金面上项目: 末次冰期淮河流域-长江下游地区下蜀黄土物源及其环境意义(41772323),2012.01-2015.12;
  2. 国土资源部公益性行业科研专项: 我国不同季风区古气候演化差异及成因机制研究,第二课题(201211077-2),2012.01-2015.12;
  3. 国家自然科学基金青年基金项目:中国北方三趾马红土的风化成壤特征及其古气候意义(40202033),2003.01-2005.12;
  4. 国家自然科学基金面上项目:西部黄土高原上新世风尘堆积序列及其记录的环境演化历史(40672115),2007.01-2009.12;
  5. 中科院知识创新重要方向项目二级课题: 环境记录的年代地层学研究(kzcx2-yw-117-1),2007.01-2009.12,同时作为本项目“风尘堆积记录的不同时间尺度的高低纬相互作用研究-全球变冷过程的不同场景对我国季风环境的影响”第二负责人。
 
获奖及荣誉:
  • 国家自然科学二等奖,晚新生代风化成壤作用与东亚环境演化,(排名第二,2014)
  •  中国地质学会十大地质科技进展(排名第一,2012)
 
代表论著:
  1. Peng Shuzhen, Hao Qingzhen*, Wang Luo, Ding Min, Zhang Wei, Wang Yanan, Guo Zhengtang, 2016. Geochemical and grain-size evidence for the provenance of loess deposits in the Central Shandong Mountains region, northern China. Quaternary Research,85, 290-298. http://dx.doi.org/10.1016/j.yqres.2016.01.005.
  2. Hao Qingzhen, Wang Luo, Oldfield Frank, Guo Zhengtang, 2015. Extra-long interglacial in Northern Hemisphere during MISs 15-13 arising from limited extent of Arctic ice sheets in glacial MIS 14. Scientific Reports, 5: 12103, http://dx.doi.org/10.1038/srep12103.  
  3. Song Yang, Hao Qingzhen*, Ge Junyi, Zhao De’ai, Zhang Yan, Li Qin, Zuo Xinxin, Lü Yanwu, Wang Pan,, 2013. Quantitative relationships between magnetic enhancement of modern soils and climatic variables over the Chinese Loess Plateau. Quaternary International, 334–335, 119–131,http://dx.doi.org/10.1016/j.quaint.2013.12.010.         
  4. Hao Qingzhen, Wang Luo, Oldfield Frank, Peng Shuzhen, Qin Li, Song Yang, Xu Bing, Qiao Yansong, Bloemendal Jan, Guo Zhengtang, 2012.Delayed build-up of Arctic ice sheets during 400,000-year minima in insolation variability. Nature, 490, 393-396, http://dx.doi.org/10.1038/nature11493. [Data], [Supplementary Information].  
  5. Hao Qingzhen, Oldfield Frank, Bloemendal Jan, Guo Zhengtang, 2012. Hysteresis and thermomagnetic properties of particle-sized fractions from loess and palaeosol samples spanning 22 Myr of accumulation on the Chinese Loess Plateau. Geophysical Journal International, 2012, 191, 64–77, http://dx.doi.org/10.1111/j.1365-246X.2012.05622.x. [PDF]      
  6. Hao, Q., Guo, Z., Qiao, Y., Xu, B., and Oldfield, F., 2010. Geochemical evidence for the provenance of Middle Pleistocene loess deposits in southern China Quaternary Science Reviewshttp://dx.doi.org/10.1016/j.quascirev.2010.08.004. [PDF]
  7. Hao, Q., Oldfield, F., Bloemendal, J., Torrent, J., and Guo, Z., 2009. The record of changing Hematite and Goethite deposition over the last 22Ma on the Chinese Loess Plateau from magnetic measurements and Diffuse Reflectance Spectroscopy. Journal of Geophysical Research, 114,B12101, http://dx.doi.org/10.1029/2009JB006604. [PDF]  
  8. Hao, Q., Oldfield, F., Bloemendal, J. and Guo, Z., 2008. Particle size separation and evidence for pedogenesis in samples from the Chinese Loess Plateau spanning the last 22 Ma. Geology, 36(9), 727–730, http://dx.doi.org/10.1130/G24940A.1. [PDF]
  9. Hao, Q., Oldfield, F., Bloemendal, J. and Guo, Z., 2008. The magnetic properties of loess and paleosol samples from the Chinese Loess Plateau spanning the last 22 million years. Palaeogeography, Palaeoclimatology, Palaeoecology, 260, 389–404, http://dx.doi.org/10.1016/j.palaeo.2007.11.010. [PDF]
  10. Hao, Q. and Guo, Z., 2007. Magnetostratigraphy of an early-middle Miocene loess-soil sequence in the western Loess Plateau of China. Geophysical Research Letters, 34, L18305, http://dx.doi.org/10.1029/2007GL031162. [PDF]
  11. Hao, Q. and Guo, Z., 2005. Spatial variations of magnetic susceptibility of Chinese loess for the last 600 ka: Implications for monsoon evolution. Journal of Geophysical Research, 110, B12101, http://dx.doi.org/10.1029/2005JB003765. [PDF]
  12. Hao, Q. and Guo Z., 2004. Magnetostratigraphy of a late Miocene-Pliocene loess-soil sequence in the western Loess Plateau in China. Geophysical Research Letters, 31: L092099, http://dx.doi.org/10.1029/2003GL019392. [PDF]
  13. Hao, Q. and Guo, Z., 2001. Quantitative measurements on the paleo-weathering intensity of the loess-soil sequences and the implication on paleomonsoon. Science in China, Ser. D., 44(6), 566–576. [郝青振, 郭正堂,2001. 1.2Ma以来黄土-古土壤序列风化成壤强度的定量化研究与东亚夏季风演化.中国科学, 31(6), 520–528].   
  14. Oldfield, F. Hao, Q. Bloemendal, J. Gibbs-Eggar, Z.Patil, S., and Guo, Z., 2009. Links between particle size and magnetic grain size: general observations and some implications for Chinese loess studies. Sedimentology, 56, 2091-2106, doi: 10.1111/j.1365-3091.2009.01071.x  
  15. Guo, Z.T., Ruddiman, W. F., Hao, Q.Z., Wu, H.B., Qiao, Y.S., Zhu, R.X., Peng, S.Z, Wei, J. J., Yuan, B.Y., Liu, T.S, 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 416, 159–163.
     

其他论著:

  1. Slobodan B. Marković, Thomas Stevens, George J. Kukla, Ulrich Hambach, Kathryn E. Fitzsimmons, Phil Gibbard, Björn Buggle, Michael Zech, Zhengtang Guo, Qingzhen Hao, Haibin Wu, Ken O'Hara Dhand, Ian J. Smalley, Gábor Újvári, Pál Sümegi, Alida Timar-Gabor, Daniel Veres, Frank Sirocko, Djordjije A. Vasiljević, Zdzisław Jary, Anderss Svensson, Vidojko Jović, Frank Lehmkuhl, János Kovács, Zorica Svirčev. 2015. Danube loess stratigraphy Towards a pan-European loess stratigraphic model. Earth-Science Reviews,148, 228258.
  2. Chen Yiwei, Li Sheng-Hua, Li Bo, Hao Qinzhen, Sun Jimin, 2015. Maximum age limitation in luminescence dating of Chinese loess using the multiple-aliquot MET-pIRIR signals from K-feldspar. Quaternary Geochronology, 30(Part B), 207-212.
  3. Zhang C.X., G.Q.Xiao,Z.T. Guo, H.B.Wu and Q.Z.Hao, 2015, Evidence of late early Miocene aridification intensification in the Xining Basin caused by the northeastern Tibetan Plateau uplift. Global and Planerary Change,128:31-46.
  4. Peng Shuzhen, Hao Qingzhen, Oldfield Frank, Guo Zhengtang, 2014. Release of iron from chlorite weathering and links to magnetic enhancement in Chinese loess deposits. Catena, 117, 43–49.
  5. Wang, L., Li, J., Lu, H., Gu, Z., Rioual, P., Hao, Q., Mackay, A., Jiang, W., Cai, B., Xu, B., Han, J., Chu, G., 2012, The East Asian winter monsoon over the last 15,000 years: its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon. Quaternary Science Reviews, doi:10.1016/j.quascirev.2011.11.003
  6. Bing Xu, Zhaoyan Gu, Chengyuan Wang, Qingzhen Hao, Jingtai Han, Qiang Liu, Luo Wang, Yanwu Lu, 2012. Carbon isotopic evidence for the associations of decreasing atmospheric CO2 level with the Frasnian-Famennian mass extinction. J. Geophys. Res., G01032, doi:10.1029/2011JG001847.
  7. Xiao, G., Guo, Z., Dupont-Nivet, G., Lu, H., Wu, N., Ge, J., Hao, Q., Peng, S., Li, F., Abels, H., Zhang, K., 2012, Evidence for northeastern Tibetan Plateau uplift between 25 and 20 Ma in the sedimentary archive of the Xining Basin, Northwestern China. Earth and Planetary Letters, 317/318:185–195.
  8. Yi Liang, Yu Hongjun, Ortiz Joseph D., Xu Xingyong, Chen Shenliang, Ge Junyi, Hao Qingzhen, Yao Jing, Shi Xuefa, Peng Shuzhen, 2012, Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 329/330, 101–117. 
  9. Qiao, Y., Hao, Q., Peng, S., Wang, Y., Li, J., Liu, Z., 2011, Geochemical characteristics of the eolian deposits in southern China, and their implications for provenance and weathering intensity. Palaeogeography, Palaeoclimatology, Palaeoecology, 308, 513–523.
  10. Xu, B., Gu, Z., Han, J., Hao, Q., Lu, Y., Wang, L., Wu, N., Pei, Y., 2011, Radiocarbon age anomalies of land snail shells in the Chinese Loess Plateau. Quaternary Geochronology, 6, 383-389.
  11. Guo, Z.T., Sun, B., Zhang, Z.S., Peng, S.Z., Xiao, G.Q., Ge, J.Y., Hao, Q.Z., Qiao, Y.S., Liang, M.Y., Liu, J.Q., Yin, Q.Z. and Wei, J.J., 2008. A major reorganization of Asian climate by the early Miocene. Climate of the Past, 4, 153–174.
  12. Li, F.J., Wu, N.Q., Pei, Y.P., Hao, Q.Z., Rousseau, D., 2006. Wind-blown origin of Dongwan late Miocene-Pliocene dust sequence documented by land snail record in western Chinese Loess Plateau. Geology, 34, 405–408, doi: 10.1130/G22232.1
  13. Qiao, Y.S., Guo, Z.T, Hao, Q.Z., Yin, Q.Z., Yuan, B.Y. and Liu, T.S., 2006. Grain-size features of a Miocene loess-soil sequence at Qinan: Inplications on its origin. Science in China, Series D, 49(7), 731–738 [乔彦松,郭正堂,郝青振,尹秋珍,袁宝印,刘东生,2006. 中新世黄土-古土壤序列的粒度特征及其对成因的指示意义.中国科学,D辑,36(7),646-653].
  14. Liu Jinfeng, Guo Zhengtang, Qiao Yansong, Hao Qingzhen, Yuan Baoyin, 2006. Eolian origin of the Miocene loess-soil sequence at Qin’an, China: evidence of quartz morphology and quartz grain-size. Chinese Science Bulletin, 51(1), 117–120. [刘进锋,郭正堂,乔彦松,郝青振,袁宝印,2005. 秦安中新世黄土-土壤序列石英颗粒形态特征、粒度分布及其对成因的指示意义. 科学通报,50(24), 2806–2809].
  15. Guo, Z.T., Peng, S.Z., Hao, Q.Z., Biscaye, P. E., An, Z.S. and Liu, T.S., 2004. Late Miocene-Pliocene development of Asian aridification as recorded in an eolian sequence in northern China. Global and Planetary Changes, 41(3-4): 135–145.
  16. Qiao Yansong, Guo Zhengtang, Hao Qingzhen, Wu Wenxiang, Jiang Wenying, Yuan Baoyin, Zhang Zhongshi, Wei Jianjing and Zhao Hua, 2003, Loess-soil sequences in southern AnhuiProvince: magnetostratigraphy and paleoclimatic significance. Chinese Science Bulletin, 48(9): 2088–2093. [乔彦松,郭正堂,郝青振,吴文祥,姜文英,袁宝印,张仲石,魏建晶,赵华, 2003, 皖南风尘堆积-土壤序列的磁性地层学研究及其古环境意义. 科学通报,48(13), 1465–1469.].
  17. Jiang, W.Y., Peng, S.Z., Hao, Q,Z. and Liu, T.S., 2002. Carbon isotopic records in paleosols over the Pliocene in Northern China: implication on vegetation development and Tibetan uplift. Chinese Science Bulletin, 47(8), 687-690. [姜文英,彭淑贞,郝青振, 刘东生, 2001. 上新世红粘土的碳同位素记录与青藏高原隆升的关系. 科学通报, 46(24), 2065–2068]. 
  18. Guo, Z.T., Peng, S.Z., Hao, Q.Z., Biscaye, P.E., Liu, T.S., 2001. Origin of the Miocene-Pliocene red-earth formation at Xifeng in Northern China and implications for paleoenvironments. Palaeogeography, Palaeoclimatology, Palaeoecology, 170, 11–26.
  19. Zou, X.Y., Wang, Z.L., Hao, Q.Z., Zhang, C.L., Liu, Y.Z. and Dong, G.R., 2001. The Distribution of velocity and energy of saltating sand grains in a wind tunnel. Geomorphology, 36, 155–165.
  20. Zou Xueyong, Hao Qingzhen, Zhang Chunlai et al., 1999. The trajectory parameters analysis of saltating sand grains driven by wind. Chinese Science Bulletin, 1999, 44(18): 1681–1685 [邹学勇,郝青振,张春来,杨保,刘玉璋,董光荣,周绍祥,风沙流中跃移沙粒轨迹参数分析. 科学通报,1999,44(10), 1084–1088].
  21. 李楠,郝青振*,张绪教,高新勃,韩龙,张伟,彭淑贞,旺罗,许冰,乔彦松,顾兆炎,2016. 东秦岭黄土物源的常量元素和微量元素地球化学证据.第四纪研究, 36 (2): 332-346.
  22. 袁宝印, 郝青振, 徐钦琦, 岳峰, 张伟, 刘平, 2015. 洛川黄土堆积粗颗粒变化记录与华北第四纪哺乳动物迁徙关系的初步探讨. 第四纪研究, 35 (6): 1480-1488.
  23. 贾伟丽, 彭淑贞, 张伟, 郝青振, 韩军青, 郭正堂, 2014. 末次间冰期以来黄土中伊利石结晶度的变化与古环境. 第四纪研究, 34 (3): 553559
  24. 许晨曦, 郝青振, 杨石岭, 赵淑君, 周鑫, 葛俊逸, 肖国桥, 2011. 黄土高原东南部黄土记录的全新世东亚季风变化. 地质力学学报, 17(2), 175-184.  
  25. 姚玉鹏, 刘羽, 张进江, 熊巨华, 郝青振, 郑德顺,2010. 2010年度地质学科项目受理与资助分析. 地球科学进展,25(12), 1389-1392.  
  26. 许晨曦,郝青振,杨石岭,赵淑君,周鑫,葛俊逸,肖国桥.2010. 黄土高原东南部黄土记录的全新世东亚季风变化.地质力学学报,17(2), 175-184.
  27. 姚玉鹏,刘羽,张进江,熊巨华,郝青振,张晓东, 2009. 2009年度地质学科项目受理与资助分析. 地球科学进展,24(12), 1371-1374.
  28. 袁宝印,郭正堂,乔彦松,郝青振,2008. 地文期及其在新生代黄土和古地理研究中的意义. 地质通报,27(3), 300–307.
  29. 尹秋珍, 肖国桥, 郭正堂, 葛俊逸, 郝青振, 袁宝印, 2007. 风尘堆积常见的同沉积和沉积后改造特征及其环境意义. 第四纪研究,27, 295-302.
  30. 袁宝印, 郭正堂, 郝青振, 彭淑贞, 乔彦松, 吴海斌, 肖国桥, 葛俊逸, 孙斌, 周鑫, 尹秋珍, 梁美艳, 秦利, 刘恋, 姚政权, 刘东生, 2007. 天水秦安一带中新世黄土堆积区沉积-地貌演化. 第四纪研究, 27, 161-171.
  31. 周鑫, 郭正堂, 彭淑贞, 郝青振, 肖国桥, 葛俊逸, 秦利. 西峰剖面午城黄土古风化强度变化与早更新世季风环境演化. 第四纪研究, 2007, 27(4), 645–650.
  32. 葛俊逸、郭正堂、郝青振,2006. 特征时期黄土高原风化成壤强度的空间特征及气候梯度. 第四纪研究,26(6), 962–968.
  33. 孙斌, 郭正堂, 尹秋珍, 郝青振, 2006. 西宁第四纪黄土- 古土壤序列中的可溶盐、来源及环境意义. 第四纪研究, 26, 649–656.  
  34. 姚政权,郭正堂,陈宇坤,肖国桥,邵永新,王旭龙, 郝青振,卢演俦,安芷生,2006.渤海湾海陆交互相沉积的磁性地层学研究.海洋地质与第四纪地质,26(1), 9–15.
  35. 刘进锋,郭正堂,郝青振,彭淑贞,乔彦松,孙斌,葛俊逸,2005. 甘肃秦安糜子湾剖面中新世黄土堆积的磁性地层学研究. 第四纪研究,25(4), 503–509.
  36. 乔彦松,郭正堂,郝青振,吴文祥,张仲石,赵华,朱日祥,2002. 安徽宣城风成堆积序列的磁性地层学研究与古环境意义. 地质力学学报, 8, 369–375.
  37. 乐小横, 徐旭荣,郝青振. 2000. 江西银山矿区次火山岩岩石地球化学特征及形成大地构造环境. 大地构造与成矿学,24(4), 385–389.
  38. 郝青振,郭正堂,彭淑贞,2000. 陇西第三纪红土磁学性质初步研究. 第四纪研究, 20(5), 447–456.
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