梁尔源 - 中国科学院大学 - 资源与环境学院

个人简介

招生专业 070501-自然地理学 071300-生态学招生方向高寒生态系统格局与过程树轮生态学与气候学教育背景 1996-09--2001-07 中国科学院植物研究所博士 1992-09--1996-07 山东师范大学学士出国学习工作 1998.10－1999.1 荷兰莱登大学，访问学者 2001.11－2002.8 法国农业环境工程研究中心（Cemagref in Aix-en-Provence, France），博士后 2004.10-2005.12; 2006.11-2007.04 德国汉堡大学，洪堡学者 2008.11-2009.3 德国汉堡大学，高访 2015.1-2015.3 哈佛大学林学系，高访 2017.8-2018.8 亚利桑那大学，访问学者工作经历 2002.9－2004.7 中国科学院地理科学与资源研究所，博士后, 2004.8-2009.12 中国科学院青藏高原研究所, 副研究员 2010.1- 今中国科学院青藏高原研究所, 研究员, 博士生导 2018.11- 中国科学院高寒生态重点实验室，主任

研究领域

树轮生态学与气候学高寒生态系统格局与过程

近期论文

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1. Sigdel SR, Liang E*, Wang Y, Dawadi B, Camarero JJ. 2020. Tree-to-tree interactions slow down Himalayan treeline shift as inferred from tree spatial patterns. Journal of Biogeography, DOI: 10.1111/JBI.13840 2. Lu X, Liang E*, Wang Y, Babst F, Leavitt S, Camarero JJ. 2019. Past the climate optimum: Recruitment is declining at the world’s highest juniper shrublines on the Tibetan Plateau. Ecology, 100(2), e02557. 3. Sigdel SR, Wang Y, Camarero JJ, Zhu H, Liang E*, Peñuelas J. 2018. Moisture-mediated responsiveness of treeline shifts to global warming in the Himalayas. Global Change Biology, 24: 5549–5559 4. Ren P, Rossi S, Camarero JJ, Ellison AM, Liang E*, Peñuelas J. 2018. Critical temperature and precipitation thresholds for the onset of xylogenesis of Juniperus przewalskii in a semi-arid area of the northeastern Tibetan Plateau. Annals of Botany, 121 (4): 617–624. 5. Li X, Liang E*, Gričar J, Rossi S, Čufar K, Ellison AM. 2017. Critical minimum temperature limits xylogenesis and maintains treelines on the southeastern Tibetan Plateau. Science Bulletin, 62(11):804–812. 6. Liang E*, Wang Y, Piao S, Lu X, Camarero JJ, Zhu H, Zhu L, Ellison AM, Ciais P, Peñuelas J. 2016. Species interactions slow warming-induced upward shifts of treelines on the Tibetan Plateau. Proceedings of the National Academy of Sciences,USA, 113(16), 4380–4385 7. Liang E*, Leuschner C, Dulamsuren C, Wagner B, Hauck M*. 2016. Global warming-related tree growth decline and mortality on the north-eastern Tibetan plateau. Climatic Change, 134(1): 163-176. 8. Liang E*, Dawadi B, Pederson N, Eckstein D. 2014. Is the growth of birch at the upper timberline in the Himalayas limited by moisture or by temperature? Ecology, 95(9): 2453–2465 9. Li X, Liang E*, Gricar J, Prislan P, Rossi S, Cufar K. 2013. Age-dependence of xylogenesis and its climatic sensitivity in Smith fir on the south-eastern Tibetan Plateau. Tree Physiology, 33(1): 48–56. 10. Liang E*, Lu X, Ren P, Li X, Zhu L, Eckstein D. 2012. Annual increments of juniper dwarf shrubs above the tree line on the central Tibetan Plateau: a useful climatic proxy. Annals of Botany, 109(4): 721-728. 11. Liang E*, Wang Y, Eckstein D, Luo T. 2011. Little change in the fir tree-line position on the southeastern Tibetan Plateau after 200 years of warming. New Phytologist, 190(3): 760-769. 12. Liang E*, Shao X, Qin N. 2008. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global and Planetary Change 61(3-4): 313-320. 13. Liang E, Eckstein D*. 2006. Light rings in Chinese pine (Pinus tabulaeformis) in semiarid areas of northChinaand their palaeo-climatological potential. New Phytologist, 171(4): 783-791. 14. Liang E, Liu X, Yuan Y, Qin N, Fang X, Huang L, Zhu H, Wang L, Shao X*. 2006. The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of Northern China. Climatic Change, 79(3-4): 403-432.