杨石岭

中国科学院地质与地球物理研究所

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  • 杨石岭
  • 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:

杨石岭,研究员,博士生导师,国家杰出青年科学基金获得者。1974年出生于陕西子长。1995年毕业于西北大学地质学系,1998年于中国科学院地质研究所获硕士学位,2001年于中国科学院地质与地球物理研究所获博士学位。 长期从事风尘沉积与古环境研究。重建了典型冷暖时期古沙漠边界,并估算了夏季风雨带的进退幅度;构建了成壤碳酸盐形成的概念模型,发现黄土高原 C3/C4 植被变化的关键影响因素是季风降水的季节配置而非降雨量;通过比较典型冷暖时期 C3/C4 植被的空间分布,提出全球变暖将导致季风雨带向北推进,从而逆转目前的北方干旱化趋势。 在PNAS、GCA、EPSL、《中国科学》、《科学通报》等国内外学术刊物发表论文80余篇,SCI收录60篇。曾主持多项国家自然科学基金和中科院项目。2009–2014年任国务院学位委员会第六届学科评议组(地球物理学、地质学组)秘书,现任国际第四纪联合会(INQUA)黄土小组委员会主席、中国第四纪科学研究会第九届理事会常务理事、副秘书长。2011年获第二届刘东生青年地球科学家奖。

教育及工作经历:

1995年7月毕业于西北大学地质学系,获学士学位。1998年7月毕业于中国科学院地质研究所,获硕士学位。2001年7月毕业于中国科学院地质与地球物理研究所,获博士学位。2001.08-2004.12 中国科学院地质与地球物理研究所助理研究员。2004.12-2010.12 中国科学院地质与地球物理研究所副研究员。2010.12至今 中国科学院地质与地球物理研究所研究员。2005.04-2006.04 美国亚利桑那大学地球科学系博士后访问学者。
学科类别:
地貌学与第四纪地质学
研究方向:
风成沉积的沉积学、地球化学研究
职务:
社会任职:
承担科研项目情况:

主持科研项目:

国家自然科学基金“中亚黄土记录的第四纪古气候演化及其与中国黄土的对比”。国家自然科学基金“黄土中成壤碳酸盐的元素地球化学组成与干旱程度的关系”。国家自然科学基金“黄土高原上新世红粘土记录的东亚夏季风空间格局”。国家杰出青年科学基金“风尘沉积与古环境”。中科院知识创新工程重要方向项目“增温过程和高温期黄土高原生态环境格局的历史相似型研究”。中科院战略先导专项(B 类)项目“环境演变与生物事件的关联机制”。
获奖及荣誉:

2011年获第二届刘东生青年地球科学家奖

代表论著:
Li Yangyang, Yang Shiling, Luo Pan, Xiong Shangfa, 2019. Aridity-controlled hydrogen isotope fractionation between soil n-alkanes and precipitation in China. Organic Geochemistry, 133, 53–64.Jiang Wenying, Suzanne A.G. Leroy, Yang Shiling, Zhang Eenlou, Wang Luo, Yang Xiaoxiao, Patrick Rioual, 2019. Synchronous strengthening of the Indian and East Asian monsoons in response to global warming since the last deglaciation. Geophysical Research Letters, 46, 3944–3952. https://doi.org/10.1029/2019GL082084.Huang Xiaofang, Jiang Dabang, Dong Xinxin, Yang Shiling*, Su Baohuang, Li Xiangyu, Tang Zihua, Wang Yongda, 2019. Northwestward migration of the northern edge of the East Asian summer monsoon during the mid-Pliocene warm period: Simulations and reconstructions. Journal of Geophysical Research: Atmospheres, 124, 1392–1404. https://doi.org/10.1029/2018JD028995.杨石岭,董欣欣,肖举乐,2019. 末次冰盛期以来东亚季风变化历史—中国北方的地质记录.中国科学:地球科学,49(8), 1169-1181.Yang Shiling, Dong Xinxin, Xiao Jule, 2019. The East Asian Monsoon since the Last Glacial Maximum: Evidence from geological records in northern China. Science China Earth Sciences, 62(8), 1181-1192.Bi Shundong, Zheng Xiaoting, Wang Xiaoli, Cignetti N. E., Yang Shiling, Wible J. R., 2018. An Early Cretaceous eutherian and the placental–marsupial dichotomy. Nature, 558, 390-395.Randall J. Schaetzl, E. Arthur Bettis III, Onn Crouvi, Kathryn E. Fitzsimmons, David A. Grimley, Ulrich Hambach, Frank Lehmkuhl, Slobodan B. Markovic, Joseph A. Mason, Piotr Owczarek, Helen M. Roberts, Denis-Didier Rousseau, Thomas Stevens, Jef Vandenberghe, Marcelo Zárate, Daniel Veres, Shiling Yang, Michael Zech, Jessica L. Conroy, Aditi K. Dave, Dominik Faust, Qingzhen Hao, Igor Obreht, Charlotte Prud’homme, Ian Smalley, Alfonsina Tripaldi, Christian Zeeden, Roland Zech, 2018. Approaches and challenges to the study of loess—Introduction to the LoessFest Special Issue. Quaternary Research, 89, 563-618.Markovic S. B., Yang Shiling, Mason J., 2018. Editorial: Eurasian loess records. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 1-3.Markovic S. B., Stevens T. , Mason J., Vandenberghe J., Yang Shiling, Veres D., újvári G., Timar-Gabor A., Zeeden C., Guo Z., Hao Q., Obreht I., Hambach U., Wu H., Gavrilov M. B., Rolf C., Tomi? N., Lehmkuhl F., 2018. Loess correlations – Between myth and reality. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 4-23.Yang Shiling, Gábor újvári, Slobodan B. Markovi?, 2018. Editorial: Aeolian deposition and Earth surface systems. Quaternary International, 469, 1-3.Yang Shiling, Ding Zhongli, Feng Shaohua, Jiang Wenying, Huang Xiaofang, Guo Licheng, 2018. A strengthened East Asian Summer Monsoon during Pliocene warmth: Evidence from ‘red clay’ sediments at Pianguan, northern China. Journal of Asian Earth Sciences, 155, 124-133.Li Yangyang, Yang Shiling, Xiao Jule, Jiang Wenying,Yang Xiaoxiao, 2018. Hydrogen isotope ratios of leaf wax n-alkanes in loess and floodplain deposits in northern China since the Last Glacial Maximum and their paleoclimatic significance. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 91-97.Wang Xu, Cui Linlin, Yang Shiling, Zhai Jixuan, Ding Zhongli, 2018. Stable carbon isotope records of black carbon on Chinese Loess Plateau since last glacial maximum: An evaluation on their usefulness for paleorainfall and paleovegetation reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 98-104.Yang Xiaoxiao, Jiang Wenying, Yang Shiling, Kong Zhaochen, Luo Yunli, 2017. Changes in plant richness and evenness since Marine Isotope Stage 2 on the Chinese Loess Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 137-143..杨石岭,丁仲礼,2017. 黄土高原黄土粒度的空间变化及其古环境意义. 第四纪研究,37(5),934-944.Ding Zhongli, Yang Shiling, 2017. Plio-Pleistocene changes in arid and semi-arid regions of northern China on geological timescales. In: Congbin Fu, Huiting Mao (Eds.), Aridity Trend in Northern China. World Scientific Publishing Co. Pte. Ltd., Singapore, pp. 5-26.Chen Zuoling, Ding Zhongli, Tang Zihua, Yang Shiling, Wang Xu, Cui Linlin, 2017. Paleoweathering and paleoenvironmental change recorded in lacustrine sediments of the early to middle Eocene in Fushun Basin, Northeast China. Geochemistry, Geophysics, Geosystems, 18, 41-51, doi:10.1002/2016GC006573.Zhou Xinying, Li Xiaoqiang, Yang Shiling, Long Hao, Yang Qing, Zhao Keliang, and Cui Jianxin, 2016. Past changes in the vegetation density of the Chinese Loess Plateau revealed by variations in the size of Artemisia pollen grains. Review of Palaeobotany and Palynology, 235, 71-80.Chen Zuoling, Ding Zhongli, Yang Shiling, Zhang Chunxia, Wang Xu, 2016. Increased precipitation and weathering across the Paleocene-Eocene Thermal Maximum in central China. Geochemistry, Geophysics, Geosystems, 17, 2286-2297, doi:10.1002/2016GC006333.郭利成,吴佳斌,熊尚发,杨石岭,2016. 基于静水沉降法的沉积物颗粒分选流程. 地球科学与环境学报,38(5),694-699.李超,杨石岭,李阳阳,黄晓芳,姜文英,2016. 河南卢氏盆地张家村组粒度特征与沉积环境研究. 第四纪研究,36(6),1428-1435.董欣欣,杨石岭,唐自华,丁仲礼,2016. 基于黄土粒度估算粉尘源区-沉积区距离的新方法. 中国科学:地球科学,46(10),1406-1412.Yang Shiling, Ding Zhongli, Li Yangyang, Wang Xu, Jiang Wenying, Huang Xiaofang, 2016. Reply to Yu et al.: Global temperature change as the ultimate driver of the shift in the summer monsoon rain belt in East Asia. Proceedings of the National Academy of Sciences of the United States of America, 113(16), E2211-E2212.Li Yangyang, Yang Shiling, Wang Xu, Hu Jianfang, Cui Linlin, Huang Xiaofang, Jiang Wenying, 2016. Leaf wax n-alkane distributions in Chinese loess since the Last Glacial Maximum and implications for paleoclimate. Quaternary International, 399, 190-197.Jiang Wenying, Yang Shiling, Yang Xiaoxiao, Gu Ning, 2016. Negative impacts of afforestation and economic forestry on the Chinese Loess Plateau and proposed solutions. Quaternary International, 399, 165-173.Tang Zihua, Yang Shiling, Qiao Qingqing, Yin Feng, Huang Baochun, Ding Zhongli, 2016. A high-resolution geochemical record from the Kuche depression: Constraints on early Miocene uplift of South Tian Shan. Palaeogeography, Palaeoclimatology, Palaeoecology, 446, 1-10.Yang Shiling, Ding Zhongli, Li Yangyang, Wang Xu, Jiang Wenying, and Huang Xiaofang, 2015. Warming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-Holocene. Proceedings of the National Academy of Sciences of the United States of America, 112(43), 13178-13183, doi:10.1073/pnas.1504688112.Gu Ning, Jiang Wenying, Wang Luo, Zhang Enlou, Yang Shiling, and Xiong Shangfa, 2015. Rainfall thresholds for the precipitation of carbonate and evaporite minerals in modern lakes in northern China. Geophysical Research Letters, 42, 5895-5901, doi:10.1002/2015GL064340.Yang Xiaoxiao, Jiang Wenying, Yang Shiling, Kong Zhaochen, Luo Yunli, 2015. Vegetation and climate changes in the western Chinese Loess Plateau since the Last Glacial Maximum. Quaternary International, 372, 58-65.Markovic S. B., Yang Shiling, Catto N., Stevens T., 2014. Loess in China and Europe: A tribute to Edward Derbyshire. Quaternary International, 334-335, 1-3.Chen Zuoling, Wang Xu, Hu Jianfang, Yang Shiling, Zhu Min, Dong Xinxin, Tang Zihua, Peng Ping’an, Ding Zhongli, 2014. Structure of the carbon isotope excursion in a high-resolution lacustrine Paleocene–Eocene Thermal Maximum record from central China. Earth and Planetary Science Letters, 408, 331-340, doi:10.1016/j.epsl.2014.10.027.Chen Zuoling, Ding Zhongli, Tang Zihua, Wang Xu, and Yang Shiling, 2014. Early Eocene carbon isotope excursions: Evidence from the terrestrial coal seam in the Fushun Basin, Northeast China. Geophysical Research Letters, 41(10), 3559-3564.Zhou Xinying, Li Xiaoqiang, John Dodson, Yang Shiling, Long Hao, Zhao Keliang, Sun Nan, Yang Qing, Liu Hanbing, and Zhao Chao, 2014. Zonal vegetation change in the Chinese Loess Plateau since MIS 3. Palaeogeography, Palaeoclimatology, Palaeoecology, 404, 89-96.Yang Shiling, and Ding Zhongli, 2014. A 249 kyr stack of eight loess grain size records from northern China documenting millennial-scale climate variability. Geochemistry, Geophysics, Geosystems, 15, 798–814, doi:10.1002/2013GC005113.Yang Shiling, Ding Zhongli and Gu Zhaoyan, 2014. Acetic acid-leachable elements in pedogenic carbonate nodules and links to the East-Asian summer monsoon. Catena, 117, 73-80.Dong Xinxin, Ding Zhongli, Yang Shiling, Luo Pan, Wang Xu and Ji Junliang, 2013. Synchronous drying and cooling in central Asia during late Oligocene. Chinese Science Bulletin, 58(25), 3119-3124.Jiang Wenying, Cheng Yufen, Yang Xiaoxiao and Yang Shiling, 2013. Chinese Loess Plateau vegetation since the Last Glacial Maximum and its implications for vegetation restoration. Journal of Applied Ecology, 50, 440-448.董欣欣,丁仲礼,杨石岭,王旭,罗攀,季军良,2013. 晚渐新世中亚降温与干旱化. 科学通报,58(17),1680.Yang Shiling, Ding Zhongli, Wang Xu, Tang Zihua and Gu Zhaoyan, 2012. Negative δ18O-δ13C relationship of pedogenic carbonate from northern China indicates a strong response of C3/C4 biomass to the seasonality of Asian monsoon precipitation. Palaeogeography, Palaeoclimatology, Palaeoecology, 317/318, 32-40.Xie Jing, Yang Shiling and Ding Zhongli, 2012. Methods and application of using detrital zircons to trace the provenance of loess.Science China Earth Sciences, 55(11): 1837-1846.谢静, 杨石岭, 丁仲礼, 2012. 黄土物源碎屑锆石示踪方法与应用. 中国科学:地球科学, 42(6), 923-933.李阳阳, 王琴, 崔琳琳, 杨石岭, 2012. 不同分析方法对黄土有机碳同位素分析的影响. 地球环境学报, 3(4), 936-941.杨肖肖,孔昭宸,姜文英,杨石岭,2012. 末次盛冰期以来渭源黄土剖面的孢粉记录. 地球环境学报,3(2), 819-825.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.Yang Shiling, Ding Zhongli, 2010. Drastic climatic shift at ~2.8 Ma as recorded in eolian deposits of China and its implications for redefining the Pliocene-Pleistocene boundary. Quaternary International, 219, 37-44, doi:10.1016/j.quaint.2009.10.029.杨石岭, 丁仲礼, 2010. 黄土高原末次冰期气候不稳定性. 见: 丁仲礼等编著. 中国西部环境演化集成研究. 北京: 气象出版社, 95-107.丁仲礼, 杨石岭, 2010. 8Ma以来风尘沉积记录的季风演变历史. 见: 丁仲礼等编著. 中国西部环境演化集成研究. 北京: 气象出版社, 19-49.冯少华, 唐自华, 王旭, 杨石岭, 2010. 内蒙古准格尔旗红粘土序列的成因、年代及其古气候意义. 第四纪研究, 30(5), 911-918.孙继敏, 杨石岭, 2010. 末次冰盛期我国北方沙漠空间分布. 见: 丁仲礼等编著.中国西部环境演化集成研究. 北京: 气象出版社, 125-134.Yang Shiling, Ding Zhongli, 2008. Advance-retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial-interglacial cycles. Earth and Planetary Science Letters, 274, 499-510.Yang Shiling, Ding Feng and Ding Zhongli, 2006. Pleistocene chemical weathering history of Asian arid and semi-arid regions recorded in loess deposits of China and Tajikistan. Geochimica et Cosmochimica Acta, 70, 1695-1709.Yang Shiling, Ding Zhongli, 2006. Winter-Spring precipitation as the principal control on predominance of C3 plants in Central Asia over the past 1.77 Myr: Evidence from δ13C of loess organic matter in Tajikistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 235, 330-339.Ding Z. L., Derbyshire E., Yang S. L., Sun J. M. and Liu T. S., 2005. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution. Earth and Planetary Science Letters, 237, 45-55.Yang S. L., Ding Z. L., 2004. Comparison of particle size characteristics of the Tertiary “red clay” and Pleistocene loess in the Chinese Loess Plateau: implications for origin and sources of the “red clay”. Sedimentology, 51, 77-93.Yang S. L., Ding Z. L., 2003. Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles. Geophysical Research Letters, 30(20), 2058, doi:10.1029/2003GL018346.Gu Zhaoyan, Liu Qiang, Xu Bing, Han Jiamao, Yang Shiling, Ding Zhongli and Liu Tungsheng, 2003. Climate as the dominant control on C3 and C4 plant abundance in the Loess Plateau: Organic carbon isotope evidence from the last glacial-interglacial loess-soil sequences. Chinese Science Bulletin, 48(12), 1271-1276.Hou Shengshan, Yang Shiling, Sun Jimin and Ding Zhongli, 2003. Oxygen isotope compositions of quartz grains (4-16 mm) from Chinese eolian deposits and their implications for provenance. Science in China (Series D), 46(10), 1003-1011.Xiong S. F., Ding Z. L., Jiang W. Y., Yang S. L., and Liu T. S., 2003. Initial intensification of East Asian winter monsoon at about 2.75 Ma as seen in the Chinese eolian loess-red clay deposit. Geophysical Research Letters, 30(10), 1524, doi:10.1029/2003GL017059.Xiong S. F., Ding Z. L., Jiang W. Y., Yang S. L., and Liu T. S., 2003. Damped fluctuations in Chinese loess grain size. Geophysical Research Letters, 30(19), 2007, doi:10.1029/2003GL018187.顾兆炎, 刘强, 许冰, 韩家懋, 杨石岭, 丁仲礼, 刘东生, 2003. 气候变化对黄土高原末次盛冰期以来的C3/C4植物相对丰度的控制. 科学通报, 48(13), 1458-1464.侯圣山, 杨石岭, 孙继敏, 丁仲礼, 2003. 风成沉积物4~16 mm石英氧同位素记录及其物质来源意义. 中国科学(D辑), 33(6), 535-542.Yang Shiling, Ding Zhongli, 2002. Magnetostratigraphy and sedimentology of the eolian deposits since the late Miocene in northern China and the paleoclimatic implications. Journal of the Graduate School of the Chinese Academy of Sciences, 19(2), 202-208.Ding Z. L., Ranov V., Yang S.L., Finaev A., Han J. M. and Wang G. A., 2002. The loess record in southern Tajikistan and correlation with Chinese loess. Earth and Planetary Science Letters, 200, 387-400.Ding Z. L., Derbyshire E., Yang S. L., Yu Z. W., Xiong S. F., and Liu T. S., 2002. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record. Paleoceanography, 17(3), doi:10.1029/2001PA000725.Xiong S. F., Jiang W. Y., Yang S. L., Ding Z. L. and Liu T. S., 2002. Northwestward decline of magnetic susceptibility for the red clay deposit in the Chinese Loess Plateau. Geophysical Research Letters, 29(24), 2162, doi:10.1029/2002GL015808.Yang Shiling, Ding Zhongli, 2001. Seven million-year iron geochemistry record from a thick eolian red clay-loess sequence in Chinese Loess Plateau and the implications for paleomonsoon evolution. Chinese Science Bulletin, 46(4), 337-341.Ding Z. L., Yang S. L., Sun J. M. and Liu T. S., 2001. Iron geochemistry of loess and red clay deposits in the Chinese Loess Plateau and implications for long-term Asian monsoon evolution in the last 7.0 Ma. Earth and Planetary Science Letters, 185, 99-109.Ding Z. L., Yang S. L., Hou S. S., Wang X., Chen Z. and Liu T. S., 2001. Magnetostratigraphy and sedimentology of the Jingchuan red clay section and correlation of the Tertiary eolian red clay sediments of the Chinese Loess Plateau. Journal of Geophysical Research, 106(B4), 6399-6407.Ding Z. L., Sun J. M., Yang S. L., and Liu T. S., 2001. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change. Geochimica et Cosmochimica Acta, 65(6), 901-913.Ding Z. L., Yu Z. W., Yang S. L., Sun J. M., Xiong S. F., and Liu T. S., 2001. Coeval changes in grain size and sedimentation rate of eolian loess, the Chinese Loess Plateau. Geophysical Research Letters, 28, 2097-2100.Xiong Shangfa, Ding Zhongli, and Yang Shiling, 2001. Abrupt shifts in the late Cenozoic environment of north-western China recorded in loess-palaeosol-red clay sequences. Terra Nova, 13(5), 376-381.Ding Z. L., Yang S. L., 2000. C3/C4 vegetation evolution over the last 7.0 Myr in the Chinese Loess Plateau: evidence from pedogenic carbonate δ13C. Palaeogeography, Palaeoclimatology, Palaeoecology, 160, 291-299.Ding Z. L., Rutter N. W., Sun J. M., Yang S. L., and Liu T. S., 2000. Re-arrangement of atmospheric circulation at about 2.6 Ma over northern China: evidence from grain size records of loess-paleosol and red clay sequences. Quaternary Science Reviews, 19, 547-558.杨石岭, 侯圣山, 王旭, 陈卓, 熊尚发, 丁仲礼, 2000. 泾川晚第三纪红粘土的磁性地层及其与灵台剖面的对比. 第四纪研究, 20(5), 423-434.杨石岭, 丁仲礼, 2000. 7.0 Ma以来中国北方风尘沉积的游离铁/全铁值变化及其古季风指示意义. 科学通报, 45(22), 2453-2456.丁仲礼, 韩家懋, 杨石岭, 王国安, 2000. 塔吉克斯坦南部黄土沉积. 第四纪研究, 20(2), 171-177.Yang Shiling, Ding Zhongli, Gu Zhaoyan, Sun Jimin and Xiong Shangfa, 1999. Pedogenic carbonate isotope record of vegetational evolution since the late Miocene in the Chinese Loess Plateau. Chinese Science Bulletin, 44, 1034-1038.Ding Z. L., Ren J. Z., Yang S. L., and Liu T.S., 1999. Climate instability during the penultimate glaciation: Evidence from two high-resolution loess records, China. Journal of Geophysical Research, 104(B9), 20123-20132.Ding Z. L., Xiong S. F., Sun J. M., Yang S. L., Gu Z. Y., and Liu T. S., 1999. Pedostratigraphy and paleomagnetism of a ~7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolution. 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