Abstract

Grazing exclusion has been widely used to restore the degraded alpine grasslands on the Qinghai-Tibetan Plateau (QTP). However, the dynamics of soil organic carbon (SOC) and soil total nitrogen (STN) pools after grazing exclusion and their controlling factors are currently less understood in this region. Here, a meta-analysis was conducted to quantitatively assess the changes in SOC and STN stocks in topsoil (0–30 cm) following grazing exclusion in three major grassland types (alpine meadow, alpine steppe, and alpine desert steppe) on the QTP and to explore the potential factors controlling the effects of grazing exclusion on SOC and STN stocks. The results showed that overall, grazing exclusion significantly increased SOC stock by 16.5% and STN stock by 11.2%. Significant increases in both SOC and STN stocks were observed after grazing exclusion of alpine meadow. In contrast, grazing exclusion did not improve SOC and STN stocks in the other two grassland types. The difference in mean annual precipitation among grassland types was a likely reason for the different dynamics of SOC and STN stocks after grazing exclusion. The effect sizes of both SOC and STN stocks were positively related to the duration of grazing exclusion, and a positive relationship was detected between the effect size of SOC stock and that of STN stock, demonstrating that the dynamics of SOC and STN were closely coupled during the period of grazing exclusion. However, grazing exclusion had no impact on soil C:N ratio for all grassland types, indicating that soil C:N ratio was generally stable after grazing exclusion. Therefore, it is suggested that the increase in STN can support continuous SOC accumulation following grazing exclusion. In conclusion, the findings suggest that the effects of grazing exclusion on SOC and STN stocks differ among grassland types on the QTP, and grazing exclusion of alpine meadows may provide substantial opportunities for improving SOC and STN stocks in this region.

Highlights

  • Soils are the largest terrestrial reservoir of carbon (C), containing approximately 1500 Pg (1 Pg = 1015 g) organic C in the top meter worldwide [1]

  • The difference in mean annual precipitation (MAP) among the three grassland types was a likely reason for the different dynamics of soil organic carbon (SOC) and soil total nitrogen (STN) stocks following grazing exclusion

  • Both SOC and STN stocks increased with the duration of grazing exclusion, as indicated by the positive relationship between the effect size of SOC or STN stock and the duration of grazing exclusion

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Summary

Introduction

Small changes in the soil organic carbon (SOC) pool may significantly influence the concentration of carbon dioxide (CO2) in the atmosphere [3]. With rising levels of atmospheric CO2, there has been growing concern on SOC sequestration in recent years [4]. Due to the strong potential for C sequestration, grassland soils may act as a sink for atmospheric CO2 and contribute to the mitigation of climate change [7,8]. Large areas of grasslands are experiencing overgrazing worldwide, which reduces the plant biodiversity and productivity and modifies the structure and function of ecosystem, leading to a depletion of SOC stock [6,9]. In the context of climate change, the restoration of overgrazed grasslands is urgently needed to recover SOC levels

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