吴海斌

中国科学院地质与地球物理研究所

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  • 吴海斌
  • 研究员
  • 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
简历:
吴海斌,博士,研究员。1973年生于浙江金华。1992-1999年,兰州大学地理系自然地理专业,学士、硕士;1999-2002年,中国科学院地质与地球物理研究所第四纪专业,博士;2002-2004年,中国科学院地球环境研究所,助理研究员;2004-2005年,中国科学院地球环境研究所,副研究员;2005-2009年,法国科学院欧洲地学科研中心地中海实验室和加拿大魁北克大学蒙特利尔分校环境研究所,博士后;2009-至今,中国科学院地质与地球物理研究所,研究员,2012年获国家杰出青年科学基
学科类别:
第四纪地质学
研究方向:
主要研究领域古气候变化与碳循环,长期从事全新世土壤有机和无机碳库变化及人类活动的影响、陆地和水生生态系统碳循环、植被反演模型研制及古气候参数定量化等方面的研究
职务:
社会任职:
承担科研项目情况:
国家重点研发计划全球变化及应对专项“过去气候变化定量重建方法和我国区域气候重建”项目第四课题“古气候参数的数值模拟重建及气候变化归因分析”,2016-2021国家自然科学面上基金:南亚孟加拉盆地C4植物扩张历史及其成因研究,2016-2019国家杰出青年科学基金,第四纪地质学,2012-2015国家自然科学基金面上项目“全新世毛乌素沙地陆地生态系统碳库变化研究”,2011-2013
获奖及荣誉:
刘东生青年地球科学家奖,2013年中国科学院青年科学家奖,2013年
代表论著:
Wu H B, Li Q, Yu Y Y, Sun A Z, Lin Y T, Jiang W Q, Luo Y L. 2019, Quantitative climatic reconstruction of the Last Glacial Maximum in China. Science China Earth Sciences, 62, https://doi.org/10.1007/s11430-018-9338-3.Li Q, Wu H B, Yu Y Y, Sun A Z, Luo Y L. 2019, Quantifying regional vegetation changes in China during three contrasting temperature intervals since the last glacial maximum. Journal of Asian Earth Sciences, 174: 23-36, doi.org/10.1016/j.jseaes.2018.10.013.Li Q, Wu H B, Yu Y Y, Sun A Z, Luo Y L. 2019, Large-scale vegetation history in China and its response to climate change since the Last Glacial Maximum, Quaternary International, doi.org/10.1016/j.quaint.2018.11.016.Jiang W Q, Wu H B, Li Q, Lin Y T, Yu Y Y. 2019, Spatiotemporal changes in C4 plant abundance in China since the Last Glacial Maximum and their driving factors. Palaeogeography, Palaeoclimatology, Palaeoecology, 518: 10-21, doi.org/10.1016/j.palaeo.2018.12.021Jiang W Q, Wu J Y, Wu H B, Li Q, Lin Y T, Yu Y Y. 2019, Evolution of the relative abundance of C4 plants on the Chinese Loess Plateau since the Last Glacial Maximum and its implications. Journal of Quaternary Science, 34(2): 101–111, doi: 10.1002/jqs.3084.Liu X Y, Zhan T, Zhou X Y, Wu H B, Li Q, Zhao C, Qiao Y S, Jiang S W, Tu L Y, Ma Y F, Zhang J, Jiang X, Lou B J, Zhang X L, Zhou X. 2019, Late onset of the Holocene rainfall maximum in northeastern China inferred from a pollen record from the sediments of Tianchi Crater Lake. Quaternary Research, doi:10.1017/qua.2018.137.Li P, Zhang C X, Guo Z T, Deng C L, Ji X P, Jablonski N G, Wu H B, Zhu R X. 2019, Clay mineral assemblages in the Zhaotong Basin of southwestern China: Implications for the late Miocene and Pliocene evolution of the South Asian monsoon. Palaeogeography, Palaeoclimatology, Palaeoecology, 516: 90–100, doi.org/10.1016/j.palaeo.2018.11.039Hu B, Zhang C X, Wu H B, Hao Q Z, Guo Z T. 2019, Clay mineralogy of an Eocene fluvial-lacustrine sequence in Xining Basin, Northwest China, and its paleoclimatic implications. Science China Earth Sciences, 62: 571-584, doi: 10.1007/s11430-018-9282-8Gao X B, Hao Q Z, Wang L, Oldfield F, Bloemendal J, Deng C L, Song Y, Ge J Y, Wu H B, Xu B, Li F J, Han L, Fu Y, Guo Z T. 2018, The different climatic response of pedogenic hematite and ferrimagnetic minerals: Evidence from particle-sized modern soils over the Chinese Loess Plateau. Quaternary Science Reviews, 179: 69-86.Sayem A S M, Guo Z, Wu H, Zhang C, Yang F, Xiao G, He Z. 2018. Sedimentary and geochemical evidence of Eocene climate change in the Xining Basin, northeastern Tibetan Plateau. Science China Earth Sciences, 61, doi.org/10.1007/s11430-018-9231-9Sun A Z, Guo Z T, Wu H B, Li Q, Yu Y Y, Luo Y L, Jiang W Y, Li X Q. 2017, Reconstruction of the vegetation distribution of different topographic units of the Chinese Loess Plateau during the Holocene. Quaternary Science Reviews, 173: 236-247.Yu Y Y, Wu H B, Finke P A, and Guo Z T. 2016, Spatial and temporal changes of prehistoric human land use in the Wei River valley, northern China. The Holocene, 26, 1788-1801, DOI: 10.1177/0959683616645943.Zhang C X, Guo Z T, Deng C L, Ji X P, Wu H B, Paterson G A, Chang L, Li Q, Wu B L, and Zhu R X. 2016, Clay mineralogy indicates a mildly warm and humid living environment for the Miocene hominoid from the Zhaotong Basin, Yunnan, China. Scientific Reports, DOI: 10.1038/srep20012Zhang C X, Xiao G Q, Guo Z T, Wu H B, and Hao Q Z. 2015, Evidence of late early Miocene aridification intensification in the Xining Basin caused by the northeastern Tibetan Plateau uplift. Global and Planetary Change, 128, 31-46.Chang L, Guo Z T, Deng C L, Wu H B, Ji X P, Zhao Y, Zhang C X, Ge J Y, Wu B L, Sun L, Zhu R X. 2015, Pollen evidence of the palaeoenvironments of Lufengpithecus lufengensis in the Zhaotong Basin, southeastern margin of the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 435: 95–104.Li W Z, Peng C H, Zhou X L, Sun J F, Zhu Q A, Wu H B, St-Onge B. 2015, Application of the ecosystem model and Markov Chain Monte Carlo for parameter estimation and productivity prediction. Ecosphere, 6(12), DOI:10.1890/ES15-00034.1Markovic S B, Stevens T, Kukla G J, Hambach U, Fitzsimmons K E, Gibbard P, Buggle B, Zech M, Guo Z T, Hao Q Z, Wu H B, Dhand K O, Smalley I J, Ujvari G, Sumegi P, Timar-Gabor A, Veres D, Sirocko F, Vasiljevic D A, Jary Z, Svensson A, Jovic V, Lehmkuhl F, Kovacs J, AND Svircev Z. 2015, Danube loess stratigraphy–Towards a pan-European loess stratigraphic model. Earth-Science Reviews, 148, 228-258.Wu H B, Guo Z T, Guiot J, Hatte C, Peng C H, Yu Y Y, Ge J J, Li Q, Sun A Z, and Zhao D A. 2014, Elevation-induced climate change as a dominant factor causing the late Miocene C4 plant expansion in the Himalayan foreland. Global Change Biology, 20, 1461-1472.Wu H B, Peng C H, Moore T R, Hua D, Li C S, Zhu Q A, Peichl M, Arain M A, and Guo Z T. 2014, Modeling dissolved organic carbon in temperate forest soils: TRIPLEX-DOC model development and validation. Geoscientific Model Development, 7, 867-881.Li Q, Wu H B, Guo Z T, Yu Y Y, Ge J Y, Wu J Y, Zhao D A, and Sun A Z. 2014, Distribution and vegetation reconstruction of the deserts of northern China during the mid-Holocene. Geophysical Research Letters,41, 5184-5191.Li Q, Wu H B, Yu Y Y, Sun A Z, Markovic S B, and Guo Z T. 2014, Reconstructed moisture evolution of the deserts in northern China since the Last Glacial Maximum and its implications for the East Asian Summer Monsoon. Global and Planetary Change, 121, 101-112.Wu H B, Peng C H, Lucotte M, et al. 2013, A coupled two-dimensional hydrodynamic and terrestrial input model to simulate CO2 diffusive emissions from lake systems. Geosci. Model Dev. Discuss., 6, 3509-3556Yu Y Y, Finke P A, Wu H B, and Guo Z T. 2013, Sensitivity analysis and calibration of a soil carbon model (SoilGen2) in two contrasting loess forest soils.Geoscientific Model Development, 6, 29-44.Ge J Y, Dai Y, Zhang Z S, Zhao D A, Li Q, Zhang Y, Yi L, Wu H B, Oldfield F, Guo Z T. 2013,Major changes in East Asian climate in the mid-Pliocene: Triggered by the uplift of the Tibetan Plateau or global cooling? Journal of Asian Earth Sciences, 69: 48-59.Guo Z T, Zhou X, Wu H B. 2012, Glacial-interglacial water cycle, global monsoon and atmospheric methane changes. Climate Dynamics, 39:1073–1092.Yu Y Y, Guo Z T, Wu H B, et al. 2012, Reconstructing prehistoric land use change from archeological data: Validation and application of a new model in Yiluo valley, northern China. Agriculture, Ecosystems and Environment, 156: 99–107.Peng C H, Guiot J, Wu H B, Jiang H, and Luo Y Q. 2011, Integrating models with data in ecology and palaeoecology: advances towards a model–data fusion approach. Ecology Letters, 14: 522-536.Yao Z., Wu H., Liang M., Shi X. 2011, Spatial and temporal variations in C3 and C4 plant abundance over the Chinese Loess Plateau since the last glacial maximum. Journal of Arid Environments, 75: 881-889.Jiang W Y, Guiot J, Chu G Q, Wu H B, Yuan B Y, Hatté C, and Guo Z T. 2010, An improved methodology of modern analogues technique for palaeoclimate reconstruction in arid and semi-arid regions. Boreas, 39: 145-153.Yao Z Q, Xiao G Q, Wu H B, Liu W G, Chen Y K. 2010, Plio-Pleistocene vegetation changes in the North China Plain: Magnetostratigraphy, oxygen and carbon isotopic composition of pedogenic carbonates. Palaeogeography, Palaeoclimatology, Palaeoecology, 297: 502–510.Liu L, Yin Q Z, Wu H B, and Guo Z T. 2010, Carbon isotopic compositions of pore and matrix carbonates in carbonate nodules, and origin of carbonate formation. Chinese Science Bulletin, 55: 2926-2929. Zhan T, Guo Z T, Wu H B, Ge J Y, Zhou X, Wu C L, and Zeng F M. 2010, Thick Miocene eolian deposits on the Huajialing Mountains: The geomorphic evolution of the western Loess Plateau. Science of China (Earth Science), doi: 10.1007/s11430-010-4051-7.lBartlein P J, Harrison S P, Brewer S, Connor S, Davis B A S, Gajewski K, Guiot, J, Harrison-Prentice T I, Henderson A, Peyron O, Prentice I C, Scholze M, Sepp? H, Shuman B, Sugita S, Thompson R S, Viau A E, Williams J, and Wu H B. 2010, Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Climatic Dynamics, DOI 10.1007/s00382-010- 0904-1.Wu H B, Guiot J, Peng C H, and Guo Z T. 2009, New coupled model used inversely for reconstructing past terrestrial carbon storage from pollen data: validation of model using modern data. Global Change Biology, 15: 82-96.Wu H B, Guo Z T, Gao Q, Peng C H. 2009, Distribution of soil inorganic carbon storage and its changes due to land use activity in China. Agriculture Ecosystems & Environment, 129: 413-421.Guo Z T, Ge J Y, Xiao G Q, Hao Q Z, Wu H B, Zhan T, Liu L, Qin L, Zeng F M, and Yuan B Y. 2010, Comment on “Mudflat/distal fan and shallow lake sedimentation (upper Vallesian–Turolian) in the Tianshui Basin, Central China: Evidence against the late Miocene eolian loess” by A.M. Alonso-Zarza, Z. Zhao, C.H. Song, J.J. Li, J. Zhang, A.Martín-Pérez, R. Martín-García, X.X. Wang, Y. Zhang and M.H. Zhang [Sedimentary Geology 222 (2009) 42–51]. Sedimentary Geology, 230: 86-89. Yu Y Y, Guo Z T, Wu H B, Kahmann Julia A, and Oldfield F. 2009, Spatial changes in soil organic carbon density and storage of cultivated soils in China from 1980 to 2000. Global Biogeochemical Cycles, 23: GB2021, doi:10.1029/2008GB003428.Guiot J, Wu H B, Garreta1V, Hatte C, and Magny M. 2009, A few prospective ideas on climate reconstruction: from a statistical single proxy approach towards a multi-proxy and dynamical approach. Climate of the Past, 5: 571-583.Guiot J, Wu H B, Jiang W Y, and Luo Y L. 2008, East Asian Monsoon and paleoclimatic data analysis: a vegetation point of view. Climate of the Past, 4: 137-145.Guiot J, Christelle H A, Wu H B, and Cedric G. 2008, Interactions between vegetation and climate variability: what are the lessons of models and paleovegetation data. C.R. Geoscience, 340: 595-601.Zhou X L, Peng C H, Dang Q L, Sun J F, Wu H B, and Hua D. 2008, Simulating carbon exchange in Canadian Boreal forests I: model structure, validation, and sensitivity analysis. Ecological Modelling, 219: 287-299.William F R, Guo Z T, Zhou X, Wu H B, and Yu Y Y. 2008, Early rice farming and anomalous methane trends. Quaternary Science Reviews, 27: 1291-1295.Wu H B, Guiot J, Brewer S, Guo Z T, and Peng C H. 2007, Dominant factors controlling glacial and interglacial variations in the treeline elevation in tropical Africa. Proceedings of the National Academy of Sciences of the United States of America, 104: 9720-9724.Wu H B, Guiot J, Brewer S, and Guo Z T. 2007, Climatic changes in Eurasia and Africa at the Last Glacial Maximum and the mid-Holocene: reconstruction from pollen data using inverse vegetation modelling. Climatic Dynamics, 29: 211-229.Ramstein G, Kageyama M, Guiot J, Wu H B, Hély C, Krinner G, and Brewer S. 2007, How cold was Europe at the Last Glacial Maximum? A synthesis of the progress achieved since the first PMIP model-data comparison. Climate of the Past, 3: 331-119.Zhang F, Li C, Wang Z, and Wu H B. 2006, Modeling impacts of management alternatives on soil carbon storage of farmland in Northwest China. Biogeosciences, 3: 451- 466.Jiang W Y, Guo Z T, Sun X J, Wu H B, Chu G Q, Yuan G Y, Hatté C, and Guiot J. 2006, Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon. Quaternary Research, 65: 411-420.Lu H Y, Wu N Q, Gu Z Y, Guo Z T, Wang L, Wu H B, Wang G A, Zhou L P, Han J M and Liu T S. 2004, Distribution of carbon isotope composition of modern soils on the Qinghai-Tibetan Plateau. Biogeochemistry, 70 (2): 273-297.Wang L, Lü H Y, Wu N Q, Chu D, Han J M, Wu Y H, Wu H B, and Gu Z Y. 2004, Discovery of C4 species at high altitude in Qinghai-Tibetan Plateau. Chinese Science Bulletin, 49: 1392-1396.Wu H B, Guo Z T, and Peng C H. 2003, Land use induced changes of organic carbon storage in soils of China. Global Change Biology, 9: 305-315.Wu H B, Guo Z T, and Peng C H. 2003, Distribution and storage of soil organic carbon in China. Global Biogeochemical Cycles, 17(2): 1048-1058.Wu H B, Guo Z T, Fang X M, et al. 2002, Desert expansion in northern China since 250 ka B.P. and the environment significance. Chinese Science Bulletin, 47(20): 1740-1745.Guo Z T, Rudiman W F, Hao Q Z, Wu H B, Qiao Y S, Zhu R X, Peng S Z, Wei J J, Yuan B Y, and Liu T S. 2002, Onset of Asian desertification by 22 Ma age inferred from loess deposits in China. Nature, 416: 159-163.Wu H B, Chen F H, Wang J M, Cao J X, and Zhang Y T. 1999, Study on the relationship between magnetic anisotropy of modern eolian sediments and wind direction. Chinese Journal of Geophysics, 42(1): 71-78.胡彬, 张春霞, 吴海斌, 郝青振, 郭正堂. 2019, 西宁盆地始新世河湖相沉积序列黏土矿物组合特征及其古环境意义. 中国科学: 地球科学, 49: 569-583, doi: 10.1360/N072018-00101吴海斌, 李琴, 于严严, 孙爱芝, 林亚婷, 姜雯琪, 罗运利. 2019, 末次冰盛期中国气候要素定量重建. 中国科学: 地球科学, doi.org/10.1007/s11430-018-9338-3.吴海斌, 李琴, 于严严, 姜雯琪, 林亚婷, 孙爱芝, 罗运利. 2017, 全新世中期中国气候格局定量重建. 第四纪研究,37(5): 982-998.方克艳, 周非飞, 董志鹏, 刘秀铭, 吴海斌, 李颖俊, 曹新光, 郭正堂. 2017, 器测和树轮资料对厄尔尼诺-南方涛动指数的响应特征. 37 (5): 1064-1076.吴海斌, 罗运利, 姜文英, 李琴, 孙爱芝, 郭正堂. 2016, 植被反演方法的古气候要素定量化:现代数据检验. 第四纪研究,36(3): 520-529.祝淑雅, 吴海斌, 李琴, 张春霞, 于严严, 孙爱芝, 郭正堂. 2016, 晚新生代以来中国西北植被演化及反映的干旱化过程. 第四纪研究,36(4): 820-831.郭正堂, 任小波, 吕厚远, 高星, 刘武, 吴海斌, 张春霞, 张健平. 2016, 过去2万年以来气候变化的影响与人类适应. 中国科学院院刊, 31: 142-151.郭正堂, 羊向东, 陈发虎, 鹿化煜, 吴海斌. 2015, 末次冰盛期以来我国气候环境变化及人类适应. 科学通报, 59(30): 2937 -2939.赵得爱, 吴海斌, 吴建育, 郭正堂. 2013, 过去典型增温期黄土高原东西部C3/C4植物组成变化特征. 第四纪研究,33: 848-855.于严严, 吴海斌, 郭正堂. 2010, 史前土地利用碳循环模型构建及应用——以伊洛河流域为例,第四纪研究,30(3): 540-549.郭正堂,吴海斌. 2004,浅谈固体地球科学与地球系统科学。地球科学进展,19(5): 609-705.汪罗,吕厚远,吴乃琴,吴海斌,刘东生. 2003,青藏高原现生禾本科植物的δ13C与海拔高度的关系. 第四纪研究,23(5):573-580.吴海斌,郭正堂,彭长辉. 2001,末次间冰期以来陆地生态系统的碳储量与气候变化. 第四纪研究,21: 366-376.郭正堂,吴海斌,魏建晶,姜文英,赵希涛. 2001,用古土壤有机质碳同位素探讨青藏高原东南缘的隆升幅度. 第四纪研究,21: 392-398.吕厚远,顾兆炎,吴乃琴,汪罗,郭正堂,吴海斌. 2001,海拔高度的变化对青藏高原表土δ13Corg的影响. 第四纪研究,21(5):300-406.吴海斌,郭正堂. 2000,末次盛冰期以来中国北方干旱区演化及其短尺度干旱事件. 第四纪研究,20: 548-558.吴海斌,陈发虎,王建民,施祺. 1999,干旱区湖泊沉积物磁组构参数量值特征与环境变化研究. 海洋地质与第四纪地质,19: 95-102.陈发虎,吴海斌,张家武,汪海斌. 1999,末次冰消期以来兰州地区冬季风变化研究. 第四纪研究,(4):306-313.吴海斌,陈发虎,王建民. 1998,黄土高原第四纪粉尘沉积速率的时空变化及其意义. 沉积学报,16(1):147-151.