Abstract

Microbes, as important regulators of ecosystem processes, play essential roles in ecosystem recovery after disturbances. However, it is not clear how soil microbial communities and functions change and affect forest recovery after clear-cutting. Here, we used metagenome sequencing to systematically analyse the differences in soil microbial community composition, functions, and nitrogen (N) cycling pathways between primary Korean pine forests (PF) and secondary broad-leaved forests (SF) formed after clear-cutting. Our results showed that the dominant phyla of the two forest types were consistent, but the relative abundance of some phyla was significantly different. Meanwhile, at the genus level, the fold-changes of rare genera were larger than the dominant and common genera. The genes related to microbial core metabolic functions, virulence factors, stress response, and defence were significantly enriched in SF. Additionally, based on the relative abundance of functional genes, a schema was proposed to analyse the differences in the whole N cycling processes between the two forest types. In PF, the stronger ammoniation and dissimilatory nitrate reduction (DNRA) and the weaker nitrification provided a genetic explanation for PF dominated by ammonium (NH4+) rather than nitrate (NO3−). In SF, the weaker DNRA, the stronger nitrification and denitrification, the higher soil available phosphorus (AP), and the lower nitrogen to phosphorus ratio (N/P) comprehensively suggested that SF was faced with a greater degree of N limitation. These results offer insights into the potential relationship between soil microbes and forest recovery, and aid in implementing proper forestry management.

Highlights

  • IntroductionSoil is a highly dynamic and heterogeneous environment, and its changes are of great significance for forest ecological functions

  • During the period from May to October, the soil NH4 + content of pine forests (PF) and secondary broad-leaved forests (SF) varied with the month

  • The soil N transformation rates of the PF and SF varied with the month and greatly functional diversity (Shannon) of microbial communities and Taxonomic fluctuated more in thealpha early period of growth (May–July)

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Summary

Introduction

Soil is a highly dynamic and heterogeneous environment, and its changes are of great significance for forest ecological functions. Soil habitat, vegetation, and microbial communities all undergo synergistic changes. Soil microbial community structure and functions present signs of resilience during the recovery of disturbed forest [1]. The impacts of soil microbes on the microhabitats of woodlands become more complicated due to the diversity of vegetation, litter, climate, terrain, and landforms. During forest transitions, changes in aboveground vegetation drive variation in soil microbial community composition and functions [2]. Soil microbes are an important link between aboveground and underground ecosystem processes [3], governing the biogeochemical cycling [4,5] and affecting plant growth and community succession

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