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高寒草甸植被-土壤系统对气候变暖响应的研究进展

马丽1,徐满厚1*,翟大彤2,贾燕燕1#br#   

  1. 1 太原师范学院地理科学学院, 山西晋中 030600; 2 大同大学, 山西大同 037009)
  • 出版日期:2017-06-10 发布日期:2017-06-10

Response of alpine meadow vegetationsoil system to climate change: A review.

MA Li1, XU Man-hou1*, ZHAI Da-tong2, JIA Yan-yan1#br#   

  1. (1Institute of Geographical Science, Taiyuan Normal University, Jinzhong 030600, Shanxi, China; 2Datong University, Datong 037009, Shanxi, China).
  • Online:2017-06-10 Published:2017-06-10

摘要: 低温限制环境下发育的高寒草甸对气候变暖响应极为敏感,因此,研究高寒草甸响应气候变暖特征对预测未来气候变化下高寒生态系统可能产生的变化具有重要意义。为进一步加深高寒生态系统响应气候变暖机制的理解,从植物个体水平、群落水平特征,以及土壤物理、化学、生物特性等方面,综述了气候变暖对高寒草甸植被土壤系统的影响,并指出现有研究存在的不确定性,同时对今后的工作做了展望。温度升高促进高寒草甸植物生长发育。在适度增温下植物的光合呼吸、生物量、物种多样性有所增加,然而不同植物种类具有不同的生理结构和生态位,加之增温幅度和时间不同,导致植物光合呼吸强度、生物量分配、物候期出现差异;而温度过度升高则会导致高寒草甸物种趋于单一化,引起物种多样性降低,对群落演替产生重要影响。同时,温度升高增加高寒草甸土壤温度,减少土壤含水量,从而导致土壤有机碳含量降低或增加。在短期增温下,土壤碳和酶活性升高,土壤呼吸速率增加;但随着时间延长,土壤呼吸速率不再增加,表现出对增温的适应性。因此,高寒草甸生态系统不同组分和各生命过程对温度响应模式的差异,导致了气候变暖对高寒草甸植被土壤系统各组分的影响存在很大不确定性,建议深入开展不同增温幅度和时间下高寒草甸植被土壤系统各组分正负效应的定量化阈值判断及其生态分子生物学响应机制研究。

关键词: 惰性有机碳, 常绿阔叶林, 城市化, 珠江三角洲, 活性有机碳

Abstract: Alpine meadows occur in low temperature environments and are highly sensitive to climate warming. The response of alpine meadows to climate warming will help predict the possible impact of future climate change on alpine ecosystems. To deepen understanding of the mechanisms of alpine ecosystem responses to climate change, from the individual plant level, the community level, and in relation to the physical, chemical and biological properties of soil, we reviewed the effects of warming on vegetationsoil system of alpine meadow. We identified uncertainties in recent studies on the influences of climate warming on alpine meadow ecosystems and set out guidelines for future research on these issues. Rising temperature can promote the growth and development of alpine meadow plants. Plant photosynthetic and respiration rates, biomass and species diversity increase under moderate warming. However, different plant species have different physiological structures and ecological niches, which interact with the amplitude and duration of increasing temperature. This can result in variations of plant photosynthesis and respiration intensity, biomass allocation and phenological phases. Excessive temperature rises tend to simplify alpine meadow ecosystems and ultimately cause a reduction in species diversity, which influence community succession. Rising air temperature increases soil temperature, reduces soil moisture and has a mixed effect on soil organic carbon. Under shortterm warming, soil carbon and enzyme activity increase, raising the soil respiration rate. Over time, the soil respiration rate shows an adaptation to temperature rise. The response models to temperature vary according to their different components and the life processes of species in alpine meadow ecosystems. This leads to large uncertainties in the effects of climate warming on various components of plant and soil ecosystems in alpine meadows. We suggest to find a quantified threshold for the positive and negative effects on alpine meadow vegetation and soil system components under different amplitudes and durations of warming, and to address the response mechanisms from viewpoint of ecologicalmolecular biology.

Key words: evergreen broad-leaved forest, recalcitrant organic carbon, Pearl River Delta, urbanization, active organic carbon