Abstract

To understand effects of soil microbes on soil biochemistry in alpine grassland ecosystems under environmental changes, we explored relationships between soil microbial diversity and soil total nitrogen, organic carbon, available nitrogen and phosphorus, soil microbial biomass and soil enzyme activities in alpine meadow, alpine steppe and cultivated grassland on the Qinghai-Tibetan plateau under three-year warming, enhanced precipitation and yak overgrazing. Soil total nitrogen, organic carbon and NH4-N were little affected by overgrazing, warming or enhanced precipitation in three types of alpine grasslands. Soil microbial biomass carbon and phosphorus along with the sucrase and phosphatase activities were generally stable under different treatments. Soil NO3-N, available phosphorus, urease activity and microbial biomass nitrogen were increased by overgrazing in the cultivated grassland. Soil bacterial diversity was positively correlated with, while soil fungal diversity negatively with soil microbial biomass and enzyme activities. Soil bacterial diversity was negatively correlated with, while soil fungal diversity positively with soil available nutrients. Our findings indicated soil bacteria and fungi played different roles in affecting soil nutrients and microbiological activities that might provide an important implication to understand why soil biochemistry was generally stable under environmental changes in alpine grassland ecosystems.

Highlights

  • Was found to be an important mechanism for maintaining the stability of soil carbon storage in alpine meadow soils under warming conditions[23]

  • We found that the treatments of OG, stable warming (SW), variable warming (VW) and enhanced rainfall (ER) did not change the soil concentrations of soil organic carbon (SOC), total nitrogen (TN) and NH4-N or most soil microbial activities in the alpine meadow

  • We found that the soil biochemical indicators we measured were generally stable among treatments in the alpine steppe and the cultivated grassland, meaning that soil carbon and nitrogen were stable in the alpine grasslands of the QTP under changing environments[26] and soil biochemistry

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Summary

Introduction

Was found to be an important mechanism for maintaining the stability of soil carbon storage in alpine meadow soils under warming conditions[23]. A general understanding of the roles of soil microbial diversity in maintaining soil carbon, nitrogen and soil microbiological activities under climate warming in alpine meadows is incomplete. We conducted this study to explore the relationships between soil microbial diversity and soil biochemistry under conditions of yak overgrazing, climate warming (both stable warming and variable warming) and enhanced precipitation in alpine meadows, alpine steppe and cultivated grasslands of the QTP. The hypotheses of this study were: (1) soil biochemical conditions would be altered by climate changes and yak overgrazing over a short time period (i.e. three years); and (2) soil bacteria and fungi diversity would play different roles in regulating soil biochemistry in response to environmental changes in alpine grassland ecosystems

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