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气候因子介导的退化高寒草原的Meta分析:对生态恢复的启示

A Meta-Analysis on Degraded Alpine Grassland Mediated by Climate Factors: Enlightenment for Ecological Restoration.

作者信息

Yu Jiale, Wan Lingfan, Liu Guohua, Ma Keming, Cheng Hao, Shen Yu, Liu Yuqing, Su Xukun

机构信息

State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-environmental Sciences, Chinese Academy of Sciences, Beijing, China.

College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.

出版信息

Front Plant Sci. 2022 Jan 7;12:821954. doi: 10.3389/fpls.2021.821954. eCollection 2021.

Abstract

Alpine grassland is the main ecosystem on the Qinghai-Tibet Plateau (QTP). Degradation and restoration of alpine grassland are related to ecosystem function and production, livelihood, and wellbeing of local people. Although a large number of studies research degraded alpine grassland, there are debates about degradation patterns of alpine grassland in different areas and widely applicable ecological restoration schemes due to the huge area of the QTP. In this study, we used the meta-analysis method to synthesize 80 individual published studies which were conducted to examine aboveground and underground characteristics in non-degradation (ND), light degradation (LD), moderate degradation (MD), heavy degradation (HD), and extreme degradation (ED) of alpine grassland on the QTP. Results showed that aboveground biomass (AGB), belowground biomass (BGB), Shannon-Wiener index (H'), soil moisture (SM), soil organic carbon (SOC), soil total nitrogen (TN), and available nitrogen (AN) gradually decreased along the degradation gradient, whereas soil bulk density (BD) and soil gradually increased. In spite of a tendency to soil desertification, losses of other soil nutrients and reduction of enzymes, there was no linear relationship between the variations with degradation gradient. Moreover, the decreasing extent of TN was smaller in areas with higher precipitation and temperature, and the decreasing extent of AGB, SOC, and TN was larger in areas with a higher extent of corresponding variables in the stage of ND during alpine grassland degradation. These findings suggest that in areas with higher precipitation and temperature, reseeding and sward cleavage can be used for restoration on degraded alpine grassland. Fencing and fertilization can be used for alpine grassland restoration in areas with lower precipitation and temperature. Microbial enzymes should not be used to restore degraded alpine grassland on a large scale on the QTP without detailed investigation and analysis. Future studies should pay more attention to the effects of climate factors on degradation processes and specific ecological restoration strategies in different regions of the QTP.

摘要

高寒草原是青藏高原的主要生态系统。高寒草原的退化与恢复关系到生态系统功能和生产、当地居民的生计与福祉。尽管已有大量研究针对退化高寒草原展开,但由于青藏高原面积巨大,关于不同地区高寒草原的退化模式以及广泛适用的生态恢复方案仍存在争议。在本研究中,我们采用元分析方法,综合了80项已发表的独立研究,这些研究旨在考察青藏高原高寒草原在非退化(ND)、轻度退化(LD)、中度退化(MD)、重度退化(HD)和极度退化(ED)状态下的地上和地下特征。结果表明,地上生物量(AGB)、地下生物量(BGB)、香农 - 维纳指数(H')、土壤湿度(SM)、土壤有机碳(SOC)、土壤全氮(TN)和有效氮(AN)沿退化梯度逐渐降低,而土壤容重(BD)和土壤[此处原文似乎不完整]逐渐增加。尽管存在土壤荒漠化趋势、其他土壤养分流失以及酶活性降低的情况,但这些变化与退化梯度之间不存在线性关系。此外,在降水和温度较高的地区,TN的降低幅度较小,而在高寒草原退化过程中ND阶段相应变量程度较高的地区,AGB、SOC和TN的降低幅度较大。这些研究结果表明,在降水和温度较高的地区,可采用补种和划破草皮的方法对退化高寒草原进行恢复。在降水和温度较低的地区,可采用围栏和施肥的方法进行高寒草原恢复。在青藏高原若无详细调查分析,不应大规模使用微生物酶来恢复退化的高寒草原。未来的研究应更加关注气候因素对青藏高原不同地区退化过程和具体生态恢复策略的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3fcc/8777074/537505262856/fpls-12-821954-g001.jpg

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