Journal of Environmental Management · 2023 · 34 citations · 90 references
AgriculturePlant BiologySoil SciencesSoil BiogeochemistrySoil MicrobiologySoil ScienceCarbon CycleCarbon SequestrationPlant-nutrient CyclingSoil Microbial BiomassSoil Microbial PhysiologySoil RestorationCarbon Cycling DynamicsCarbon Persistence In SoilsMicrobial Biomass CarbonMicrobial Carbon CyclingSoil Carbon RetentionSoil Microbial CarbonSoil Microbial Community RestorationVegetation Effects On Soil Respiration
The impacts of natural restoration projects on soil microbial carbon (C) cycling functions have not been well recognized despite their wide implementation in the degraded karst areas of southwest China. In this study, metagenomic sequencing assays were conducted on functional genes and microorganisms related to soil C-cycling at three natural restoration stages (shrubbery, TG; secondary forest, SG; old-growth forest, OG) in the southeast of Guizhou Province, China. The aims were to investigate the changes in microbial potentials responsible for soil C cycling and the underlying driving forces. The natural restoration resulted in vegetation establishment at all three restoration stages, rendering alterations of soil microbial C cycle functions as indicated by metagenomic gene assays. When TG was restored into OG, the number and diversity of genes and microorganisms involved in soil C cycling remained unchanged, but their composition underwent significant shifts. Specifically, microbial potentials for soil C decomposition exhibited an increase driven by the collaborative efforts of plants and soils, while microbial potentials for soil C biosynthesis displayed an initial upswing followed by a subsequent decline which was primarily influenced by plants alone. In comparison to soil nutrients, it was determined that plant diversities served as the primary driving factor for the alterations in microbial carbon cycle potentials. Soil microbial communities involved in C cycling were predominantly attributed to Proteobacteria (31.87%-40.25%) and Actinobacteria (11.29%-26.07%), although their contributions varied across the three restoration stages. The natural restoration of degraded karst vegetation thus influences soil microbial C cycle functions by enhancing C decomposition potentials and displaying a nuanced pattern of biosynthesis potentials, primarily influenced by above-ground plants. These results provide valuable new insights into the regulation of soil C cycling during the restoration of degraded karst vegetation from genetic and microbial perspectives.
90
fastp: an ultra-fast all-in-one FASTQ preprocessor
Shifu Chen, Yanqing Zhou, Yaru Chen et al. · Bioinformatics · 2018 · 29.7K citations · Full text
Fast and sensitive protein alignment using DIAMOND
Benjamin Buchfink, Chao Xie, Daniel H. Huson · Nature Methods · 2014 · 15.2K citations
Non‐parametric multivariate analyses of changes in community structure
K.R. Clarke · Australian Journal of Ecology · 1993 · 14.1K citations
The carbohydrate-active enzymes database (CAZy) in 2013
Vincent Lombard, Hemalatha Golaconda Ramulu, Élodie Drula et al. · Nucleic Acids Research · 2013 · 6.5K citations · Full text