储国强

储国强，男，博士，中国科学院地质与地球物理所副研究员。他的研究领域涵盖湖泊年纹层、古气候指标的现代过程、现代环境过程以及分子标志化合物。

教育背景

储国强于1965年2月出生。1984年，他毕业于赣州市地质学校（现更名为江西应用技术职业学院）。随后，他在安徽区域地质调查队工作至1992年。1995年，储国强在中国地质大学（北京）获得硕士学位。1999年8月，他在中科院地质与地球物理学研究所取得博士学位。同年10月至1999年12月，他获得了马克斯·普朗克资助并在德国地学中心工作。自1999年起，储国强在中国科学院地质与地球物理研究所担任助理研究员，并于2002年12月晋升为副研究员。

研究方向

储国强的研究兴趣集中在湖泊年纹层、古气候指标的现代过程、现代环境过程以及分子标志化合物等领域。

科研项目

储国强的主要科研项目包括国家自然科学基金面上项目“末次冰消期以来小龙湾玛珥湖年纹层沉积与古气候突变事件”。该项目旨在通过对东北地区小龙湾玛珥湖末次冰消期以来发育的年纹层进行研究，建立精确的纹层年代学时间标尺，并通过分析沉积物中的双鞭毛虫门孢子和金藻孢子含量、有机碳/氮同位素、有机碳/氮含量等因素，探索纹层类型的变化与古气候突变事件之间的关系。此外，他还使用纹层大薄片来量化年纹层类型的渐变和突变过程，并结合加密抽样分析数据，探讨湖泊系统对古气候突变事件的响应过程及其可能的驱动机制。

主要成就

储国强参与了多项重要科研项目，包括国家自然科学基金八五重大项目中的两个二级课题：“时间序列”和“湖泊和沙漠绿洲的环境演化”，以及“八五”国家科技攻关专题“西北干旱化与全球变化的研究”。自1999年以来，他主持了三个国家自然科学基金项目，并参与了多个其他科研项目。2011年2月26日，储国强带领团队前往吉林龙湾国家级自然保护区进行科学研究，并成功从水下16米处采集到了岩芯样本，这对未来该地区的气候变化研究具有重要意义。

学术贡献

储国强发表了多篇学术论文，涉及湖泊年纹层、古气候指标等多个领域的研究成果。他的代表性论著涵盖了《Quaternary Science Reviews》《Chin J Anal Chem》《Marine Pollution Bulletin》等国际知名期刊上的文章。这些研究不仅深化了人们对过去千年乃至数百年气候变化的理解，也为未来的相关研究提供了宝贵的科学依据。

参考文献

[1] Chu GQ, Sun Q, Xie M , Lin Y, Shang W, Zhu Q, Shan Y,Xu D, Rioual P, Wang L, Liu J, 2014, Holocene cyclic climatic variations and the role of the Pacific Ocean as recorded in varved sediments from northeastern China。Quaternary Science Reviews

[2] Zhu QZ, Sun Q, Su ZG, Xie MM, Song JY, Shan YB,Wang N, Chu GQ,2014, A Soil H₂O Extraction Method with Accelerated Solvent Extraction Technique for Stable Isotope Analysis Chin J Anal Chem

[3] Varnosfaderany MA, Bakhtiari AR, Gu Z, Chu G, 2014. Vertical distribution and source identification of polycyclic aromatic hydrocarbons (PAHs) in southwest of the Caspian Sea: Most petrogenic events during the late Little Ice age Marine Pollution Bulletin

[4] Ptitsyn A.B., Chu G., Dar’in A.V., Zamana 路易威登, Kalugin IA, Reshetova 永恒沉睡， 2014，The rate of sedimentation in Lake Arakhlei (central Transbaikalia), from radiogeochemical and palynological 数据

[5] Xu D., Lu H., Chu G., Wu N., Shen C., Wang C., Mao L., 2014,500-year climate cycles stacking of recent centennial warming documented in an East Asian pollen record.

[6] Rioual P., Morales E. A., Chu G, Han J, Li D, Liu J, Liu Q, Mingram J.,Ecto L., 2014, Staurosira longwanensis sp. nov., a new araphid diatom (Bacillariophyta) from Northeast China.

[7] 凌媛，孙青，朱庆增, 陈栋梁, 徐伟，谢曼曼，单雅冰，王宁，储国强．2014, 同步辐射X射线荧光光谱测定沉 积物中元素含量的归一方法研究———以四海龙湾纹层沉积物为例．第四纪研究

[8] Chu G, Sun Q, Li S, Lin Y, Wang X, Xie M, Shang W, Li A, Yang K, 2013, Minor element variations during the past 1300 years in the varved sediments of Lake Xiaolongwan, northeastern China

[9] Sun Q. Xie M., Shi L. Zhang Z, Lin Y, Shang W, Wang K, Li W, Liu J, Chu G, 2013, Alkanes and 化合物specific 碳 isotopic records and climatic variation during the last millennium from varved sediments in Lake Xiaolongwan, northeastern China

[10] Rioual P, Lu Y., Yang H, Scuderi L, Chu G, Holmes J, Zhu B, Yang X, 2013, 硅藻environment relationships and a transfer 函数 for conductivity in lakes of the Badain Jaran Desert

[11] Wang L, Mackay AW, Leng MJ, Rioual P, Panizzo VN, Lu H, Gu Y, Chu G, Han J, Kendrick C P., 2013, Influence of the ratio of planktonic to benthic diatoms on lacustrine organic matter d13C from Erlongwan maar lake, northeast China

[12] Chu GQ, Sun Q, Wang XH, Liu MM, Lin Y, Xie MM, Shang WY, Liu JQ, 2012. Seasonal 温度 variability during the past 1600 years recorded in historical documents and varved lake sediment profiles from northeastern China

[13] Wang L., Rioual P., Panizzo V.N., Lu H.Y., Gu ZY, Chu G.Q.Yang D.G., Han JT, Liu JQ, Mackay AW., 2012, A 1000-yr record of environmental change in NE China indicated by diatom assemblages from maar lake Erlongwan

[14] Liu S, Narentuya, Xia BR, Chu GQ, Tian MZ., 2012, Using 210Pbuns and 137Cs to date recent sediment cores from the Badain Jaran Desert, Inner Mongolia, China. Quaternary Geochronology

[15] Wang L, Li J, Lu H., Gu ZY, Rioual P, Hao QZ, Mackay AW, Jiang WY, Cai BG, Xu B, Han H, Chu GQ, 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

[16] Wang, S., Lu H., Han J., Chu G., Liu J., Negendank J. F. W., 2012, Palaeovegetation and palaeoclimate in low-latitude southern China during the Last Glacial Maximum, Quaternary International

[17] Chu GQ, Sun Q, Yang K, Li A, Yu X, Xu T, Yan F, Wang H, Liu M, Wang W, Xie M, Ling L, Liu Q, 2011. Evidence for decreasing south Asian summer monsoon in the past 160 years from varved sediment in Lake Xinluhai, Tibetan 高原

[18] Sun Q, Chu GQ, Liu MM, Xie MM, Li SQ, Ling Y, Wang XH, Shi LM, Jia GD, Lü HY, 2011. Distributions and 温度 dependence of branched 丙三醇 dialkyl glycerol tetraethers in recent lacustrine sediments from China and Nepal

[19] Zamana LV, Ptitsyn AB, Chu GQ, Reshetova SA, Darin AV, Kalugin I A, 2011. Estimation of Modern Sedimentation Rate in Zun-Torei Lake (East Trans-Baikal Region) by 137Cs

[20] 马天芳、孙青、凌媛、谢曼曼、刘美美、尚文郁、王晓华、储国强，2011. 生物膜作用下沉积物水界面溶液中pH和磷含量变化. 岩矿测试

[21] 谢曼曼、孙青、凌媛、刘美美、杨科、李爱国、储国强,2010. 同步辐射技术在高分辨率古气候、古环境变化中的应用. 第四纪研究

[22] 姜文英、吴海斌、储国强、袁宝印、郭正堂,2010. 内蒙古自治区巴彦查干湖白云石的成因及其环境意义第四纪研究

[23] 刘强、李倩、旺罗、储国强,2010. 21KaB.P.以来大兴安岭中段月亮湖沉积物全岩有机碳同位素组成变化及其古气候意义. 第四纪研究

[24] 孙青、储国强、刘国祥、王晓华、刘美美、石丽明、谢曼曼、凌媛，2010. 湖泊体系中长链烯酮研究进展. 地球学报

[25] 石丽明、刘美美、王晓华、孙青、储国强,2010. 加速溶剂萃取提取土壤中正构烷烃的方法研究。矿测试

[26] Chu G.Q.,Sun Q., Wang X.H., Li D. Rioual P., Liu Q., Han 日本烟草产业, Liu J.Q.. A 1600 year multi-proxy record of paleoclimatic change from varved sediments in Lake Xiaolongwan, northeastern China

[27] Chu G.Q., Sun Q., Gu Z., Rioual P., Liu Q., Wang K., Han J.T., Liu J.Q., Dust records from varved lacustrine sediments of two neighbouring lakes in northeastern China over the last 1400 years

[28] Liu J.Q., Chu G.Q., Han J.T., Rioual P., Jiao W.Y., Wang K.J., Volcanic eruptions in the Longgang Volcanic Field, northeastern China, during the past 15 000 years

[29] Chu G.Q., Sun, Q., Wang, X.H. and Sun, J.Y., Snow anomaly events from historical documents in the eastern China during the past two millennia and implication for low-频率 variability of AO/NAO and PDO. Geophysical Research Letters

[30] Chu G.Q., Sun Q., Rioual P., Boltovskoy A., Liu Q., Sun 女神异闻录Q：迷宫暗影, Han J.T., Liu J.Q., Dinocyst microlaminations and freshwater “红色 tides”recorded in Lake Xiaolongwan, northeastern China

[31] Sun Q., Chu G.Q., Liu G.X., Li S., Calibration of alkenone unsaturation index with growth 温度 for a lacustrine 物种, Chrysotila lamellosa (Haptophyceae)

[32] Chu G.Q., Liu J.Q., Gao D.Y., Sun Q., The mechanism of varve formation and paleoenvironment research in Lake Bolterskardet, Svalbard, Arctic

[33] Sun Q., Chu G.Q., Liu J.Q., Gao D.Y., A 150-year record of heavy metals in the varved sediments of Lake Bolterskardet, Svalbard

[34] Chu G.Q., Sun Q., Zheng M.P., Jia X.X., Lu C.F., Liu J.Q., Liu T.S., Long-chain alkenones distributions and 温度 dependence in lacustrine surface sediments from China

[35] Chu G.Q., Liu J.Q., Schettler G., Li J.Y., Sun Q., Gu Z.Y., Lu H.Y., Liu Q., Liu T.S., Sediment fluxes and varve formation in Sihailongwan, a maar lake from northeastern China

[36] Chu G.Q., Liu J.， Sun Q.， Lu H., Gu Z., Wang W., Liu T., The "Mediaeval Warm Period" drought recorded in Lake Huguangyan, tropical South China

[37] Liu T.S., Liu J.Q., Chu G.Q., Early Cretaceous Maars, Depositional Environments and Their relationship to the Fossil Preservation in Sihetun, Liaoning, Northeast China. In：Zhonghe Zhou and Fucheng Zhang eds.Proceeddings of the 5th Symposium of the Society of Avian Paleontology and Evolution

[38] Chu G.Q., Liu J.Q., Negendank J.F.W., Zhang G.P., The paleo-typhoon activities recorded inthe lacustrine sediment of Huguangyan maar lake, southern China. In: Yasuda Y and Shinde V eds

[39] Chu G.Q., Liu J.Q., Liu T.S., Discrimination of two kinds of sedimentary laminae in maar lakes of China

[40] Liu J.Q., Chu G.Q., Liu T.S., Fossilrich Early Cretaceous Maar Lakes in Liaoxi ,Northeast China

参考资料

新华社西藏分社党组书记、社长储国强一行深入堆龙德庆区开展调研采访.微信公众平台.2024-11-16

储国强.中国科学院大学.2024-11-16

中国科学院地质与地球物理研究所导师教师师资介绍简介-储国强.免费考研网.2024-11-16