4.7 Article

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

Journal

FRONTIERS IN PLANT SCIENCE
Volume 12, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fpls.2021.821954

Keywords

meta-analysis; climate factors; ecological restoration; Qinghai-Tibet Plateau (QTP); alpine grassland; degradation

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Alpine grassland on the Qinghai-Tibet Plateau is an important ecosystem that is closely related to the function, production, livelihood, and wellbeing of local people. Degradation and restoration of this ecosystem have been studied extensively, but there are debates about the degradation patterns and restoration strategies due to the large area of the plateau. In this study, a meta-analysis was conducted to synthesize 80 individual studies on the aboveground and underground characteristics of alpine grassland at different degradation levels. The results showed that the biomass, soil moisture, organic carbon, nitrogen, and available nitrogen gradually decreased along the degradation gradient, while soil bulk density and pH increased. The extent of degradation varied depending on precipitation and temperature, and different restoration strategies were recommended for different climatic conditions. Future studies should pay more attention to the effects of climate factors on degradation processes and specific restoration strategies in different regions of the plateau.
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 pH 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.

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