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在以橡树为主的森林中,pH值沿海拔梯度对土壤细菌群落组装起非线性主导作用。

pH Nonlinearly Dominates Soil Bacterial Community Assembly along an Altitudinal Gradient in Oak-Dominant Forests.

作者信息

Lin Litao, Li Guixiang, Yu Huiyi, Ma Keming

机构信息

Chinese Research Academy of Environmental Sciences, Beijing 100012, China.

Weifang Academy of Agricultural Sciences, Weifang 261071, China.

出版信息

Microorganisms. 2024 Sep 11;12(9):1877. doi: 10.3390/microorganisms12091877.

DOI:10.3390/microorganisms12091877
PMID:39338551
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11434175/
Abstract

Soil bacteria, the predominant microbiota in soil, are subject to the law of minimum and the law of tolerance, but the assembly patterns of soil bacteria in response to environmental factors remain far from clear. Here, we took advantage of an altitudinal gradient (1020-1770 asl) in oak-dominant forests and assessed whether soil bacteria linearly or nonlinearly respond to environmental properties through the changes in the community diversity and composition. We found that soil bacteria decreased with increasing altitude in terms of the species richness and phylogenetic structure, while they were unchanged with increasing altitude in terms of community composition. The species richness was nonlinearly affected by the soil pH (19.9%), C:N ratio (14.3%), SOC (11.4%), and silt + clay content (9.9%). Specifically, the species richness peaked at a pH of 5.5-6.5, and an SOC of 25-50 g kg, and it showed abrupt decreases and increases at a C:N ratio of 14.5 and a silt + clay content of 70%. The community composition was significantly affected by the soil pH (28.2%), then by the SOC (3.6%), available phosphorus (1.0%), and silt + clay content (0.5%), and it showed less turnovers at a pH of 6.0, SOC of 50 g kg, and available phosphorus > 3.0 g kg. These findings imply that environmental filtering processes nonlinearly shape bacterial communities.

摘要

土壤细菌是土壤中的主要微生物群,受最小因子定律和耐受性定律的影响,但其对环境因子响应的组装模式仍远未明确。在此,我们利用以橡树为主的森林中的海拔梯度(海拔1020 - 1770米),通过群落多样性和组成的变化评估土壤细菌对环境特性是呈线性还是非线性响应。我们发现,就物种丰富度和系统发育结构而言,土壤细菌随海拔升高而减少,而就群落组成而言,它们随海拔升高没有变化。物种丰富度受到土壤pH值(19.9%)、碳氮比(14.3%)、土壤有机碳(11.4%)和粉砂 + 粘粒含量(9.9%)的非线性影响。具体而言,物种丰富度在pH值为5.5 - 6.5、土壤有机碳为25 - 50克/千克时达到峰值,在碳氮比为14.5和粉砂 + 粘粒含量为70%时出现急剧下降和上升。群落组成受到土壤pH值(28.2%)的显著影响,其次是土壤有机碳(3.6%)、有效磷(1.0%)和粉砂 + 粘粒含量(0.5%),在pH值为6.0、土壤有机碳为50克/千克和有效磷>3.0克/千克时,群落组成的周转率较低。这些发现表明,环境过滤过程以非线性方式塑造细菌群落。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/84888183f3e5/microorganisms-12-01877-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/ec1951b7f26d/microorganisms-12-01877-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/f3fe3b531e86/microorganisms-12-01877-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/490cbd22989b/microorganisms-12-01877-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/ba50bf572817/microorganisms-12-01877-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/93e3b8fcf295/microorganisms-12-01877-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/84888183f3e5/microorganisms-12-01877-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/ec1951b7f26d/microorganisms-12-01877-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/f3fe3b531e86/microorganisms-12-01877-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/490cbd22989b/microorganisms-12-01877-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/ba50bf572817/microorganisms-12-01877-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/93e3b8fcf295/microorganisms-12-01877-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28b1/11434175/84888183f3e5/microorganisms-12-01877-g006.jpg

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本文引用的文献

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Plant-symbiotic fungal diversity tracks variation in vegetation and the abiotic environment along an extended elevational gradient in the Himalayas.植物共生真菌多样性沿着喜马拉雅山脉的一个延伸海拔梯度,与植被和非生物环境的变化相吻合。
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Contrasting elevational patterns and underlying drivers of stream bacteria and fungi at the regional scale on the Tibetan Plateau.
在青藏高原区域尺度上,溪流细菌和真菌的海拔分布模式和潜在驱动因素截然不同。
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