ArticlePloS one2017
Effects of stand age and soil properties on soil bacterial and fungal community composition in Chinese pine plantations on the Loess Plateau.
Article in PloS one, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 27 papers.
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Who cites it
27 citing papers in PubMed.
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- Effect of different vegetation restoration patterns on community structure and co-occurrence networks of soil fungi in the karst region.Frontiers in plant science · 2024Article
- Spatial variations impact the soil fungal communities ofFrontiers in plant science · 2024Article
- Synergistic variation of rhizosphere soil phosphorus availability and microbial diversity with stand age in plantations of the endangered tree speciesFrontiers in plant science · 2024Article
- Soil mycobiomes in native European aspen forests and hybrid aspen plantations have a similar fungal richness but different compositions, mainly driven by edaphic and floristic factors.Frontiers in microbiology · 2024Article
- Green trees preservation: A sustainable source of valuable mushrooms for Ethiopian local communities.PloS one · 2023Article
- Temperature and phosphorus: the main environmental factors affecting the seasonal variation of soil bacterial diversity in Nansi Lake Wetland.Frontiers in microbiology · 2023Article
- Principal Drivers of Fungal Communities Associated with Needles, Shoots, Roots and Adjacent Soil ofJournal of fungi (Basel, Switzerland) · 2022Article
- Influence of Different Vegetation Types on Soil Physicochemical Parameters and Fungal Communities.Microorganisms · 2022Article
- Effects of Different Land Use Types and Soil Depths on Soil Mineral Elements, Soil Enzyme Activity, and Fungal Community in Karst Area of Southwest China.International journal of environmental research and public health · 2022Article
- Different factors drive the assembly of pine andFrontiers in microbiology · 2022Article
- Differential response of bacterial diversity and community composition to different tree ages of pomelo under red and paddy soils.Frontiers in microbiology · 2022Article
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- Soil Microbial Resource Limitations and Community Assembly Along aFrontiers in microbiology · 2021Article
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6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The effects of Chinese pine (Pinus tabuliformis) on soil variables after afforestation have been established, but microbial community changes still need to be explored. Using high-throughput sequencing technology, we analyzed bacterial and fungal community composition and diversity in soils from three stands of different-aged, designated 12-year-old (PF1), 29-year-old (PF2), and 53-year-old (PF3), on a Chinese pine plantation and from a natural secondary forest (NSF) stand that was almost 80 years old. Abandoned farmland (BL) was also analyzed. Shannon index values of both bacterial and fungal community in PF1 were greater than those in PF2, PF3 and NSF. Proteobacteria had the lowest abundance in BL, and the abundance increased with stand age. The abundance of Actinobacteria was greater in BL and PF1 soils than those in other sites. Among fungal communities, the dominant taxa were Ascomycota in BL and PF1 and Basidiomycota in PF2, PF3 and NSF, which reflected the successional patterns of fungal communities during the development of Chinese pine plantations. Therefore, the diversity and dominant taxa of soil microbial community in stands 12 and 29 years of age appear to have undergone significant changes; afterward, the soil microbial community achieved a relatively stable state. Furthermore, the abundances of the most dominant bacterial and fungal communities correlated significantly with organic C, total N, C:N, available N, and available P, indicating the dependence of these microbes on soil nutrients. Overall, our findings suggest that the large changes in the soil microbial community structure of Chinese pine plantation forests may be attributed to the phyla present (e.g., Proteobacteria, Actinobacteria, Ascomycota and Basidiomycota) which were affected by soil carbon and nutrients in the Loess Plateau.
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