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气候变暖会使青藏高原树线一直上升吗?
引用本文:王亚锋,梁尔源,芦晓明,朱海峰,朴世龙,朱立平.气候变暖会使青藏高原树线一直上升吗?[J].自然杂志,2017,39(3):179-183.
作者姓名:王亚锋  梁尔源  芦晓明  朱海峰  朴世龙  朱立平
作者单位:1.中国科学院青藏高原研究所,北京 100101;2中国科学院青藏高原地球科学卓越创新中心,北京 100101;3北京大学城市与环境学院,北京 100871;4中国科学院大学,北京 100049
基金项目:国家科技基础性工作专项重点项目(2012FY111400)和国家自然科学基金项目(41525001、41301207、41130529)资助
摘    要:树线上树木生长主要受生长季低温限制,因此气候变暖将导致高山树线向更高海拔迁移。然而,全球树线调查数据显示,近百年来约50%调查样点树线上升明显,其余则保持静止状态。以上事实揭示,除了气候因素,非气候因素(如竞争等种间关系)也在一定程度上调控着树线的位置变化。青藏高原拥有全球海拔最高的天然树线,是探讨气候和非气候因素对树线变化影响的理想区域。研究发现:树线之上低矮稀疏的灌丛或草丛成为幼苗萌发或生长的"避难所",从而有利于树线大幅度爬升;而高大茂密的灌丛则会形成一道宽厚的"封锁墙",从而抑制树线的上升。因此,变暖背景下树线位置倾向于向更高海拔爬升,但爬升速率受到树线之上种间关系的调控。变暖并不一定会造成树线位置的显著上升。

关 键 词:树线  青藏高原  气候变暖  种间关系  树轮  
收稿时间:2017-05-08

Are treelines advancing in response to climate warming on the Tibetan Plateau?
WANG Yafeng,LIANG Eryuan,LU Xiaoming,ZHU Haifeng,PIAO Shilong,ZHU Liping.Are treelines advancing in response to climate warming on the Tibetan Plateau?[J].Chinese Journal of Nature,2017,39(3):179-183.
Authors:WANG Yafeng  LIANG Eryuan  LU Xiaoming  ZHU Haifeng  PIAO Shilong  ZHU Liping
Institution:1.Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;2.CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China;3.College of Urban and Environmental Sciences, Peking University, Beijing 100871, China;4.University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:Tree growth at treelines is generally limited by low temperature so that warming tends to shift treeline upward. However, a global meta-analysis showed that treelines shifted upward at around 50% during the last century among the investigated treelines, and others kept static. Such evidence suggested that non-climate factors (such as interspecific competition) apart from climatic factors controlled treeline shift. The Tibetan Plateau hosts the highest treeline in the Northern Hemisphere, being a good locale for investigating climatic and biotic factors influencing treeline changes. As showed by our research, short and sparse shrub and grass acted as“tree nurseries”for recruitment, and benefitted treeline upward shift. Dense shrubs just above treeline inhibited tree establishment, and slowed upward movement of treelines. Climatic warming tended to promote the upward shift of alpine treelines at local and regional scales. However, upslope migration rates were controlled largely by interspecific interactions. Warming may not cause the upward shift of treelines if dense shrub dominate the above treelines.
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