Abstract

Soil bacterial microbial communities are important in the ecosystem function and succession of forests. Using high-throughput 16S rRNA gene sequencing and relative importance for linear regression, we explored how the structures of soil bacterial community were influenced by the environmental factors and restoration succession of secondary forests in the Miyaluo Mountains of western Sichuan, China. Using a space-for-time approach, field measurements and sampling were conducted in four stands at different stages of natural restoration. Results of distance-based multivariate analysis showed that soil pH, organic carbon, available phosphorus, and C/N ratio were the predominant environmental factors that collectively explained a 46.9% variation in the bacterial community structures. The community compositions were jointly controlled by the direct and indirect effects of the rehabilitation stages. The changes in soil environmental factors coincided with restoration succession could lead to the shifts in the relative abundance of different soil bacterial taxa. We screened 13 successional discriminant taxa that could quantitatively indicate the secondary succession subalpine stage. Collectively, our findings show that soil bacteria in different taxa are governed by different local soil variables and rehabilitation ages, which can lead to shifts in the relative abundance of different taxa in successional stages, ultimately changing the entire soil bacterial community with the succession of secondary forest.

Highlights

  • IntroductionSecondary forests formed by restoration succession after large-scale destruction (clearcutting) have become one of the most important components of the terrestrial ecosystem, which provide many ecological services, including terrestrial vegetation and rehabilitation refugia for species diversity [1]

  • Introduction published maps and institutional affilSecondary forests formed by restoration succession after large-scale destruction have become one of the most important components of the terrestrial ecosystem, which provide many ecological services, including terrestrial vegetation and rehabilitation refugia for species diversity [1]

  • The soil Soil organic carbon (SOC), Total nitrogen (TN), and C/N ratio during the MF stage were significantly different from the other stages, and the available phosphorus (AP) was significantly higher during the primary forest (PF) stage

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Summary

Introduction

Secondary forests formed by restoration succession after large-scale destruction (clearcutting) have become one of the most important components of the terrestrial ecosystem, which provide many ecological services, including terrestrial vegetation and rehabilitation refugia for species diversity [1]. A classic secondary succession is from a shrub-grassland to broad-leaved forest, resembling a coniferous forest [2]. During this process, soil conditions and environmental resources begin to improve and gradually recover to the state of primary forest. The change in surface vegetation leads to different types of litter, which change the soil organic matter composition from simple to complex [3]. Previous studies have mainly focused on the effects of land use types and geographical differences on iations

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