Diversity patterns of the rhizosphere and bulk soil microbial communities along an altitudinal gradient in an alpine ecosystem of the eastern Tibetan Plateau

The diversity patterns and drivers of soil microbial communities in altitudinal gradients have recently received much attention. The rhizosphere is a focus of soil microbial communities, but the patterns and drivers of these communities have rarely been studied in alpine ecosystems. We used high-thr...

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Published inGeoderma Vol. 338; pp. 118 - 127
Main Authors Cui, Yongxing, Bing, Haijian, Fang, Linchuan, Wu, Yanhong, Yu, Jialuo, Shen, Guoting, Jiang, Mao, Wang, Xia, Zhang, Xingchang
Format Journal Article
LanguageEnglish
Published Elsevier B.V 15.03.2019
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Abstract The diversity patterns and drivers of soil microbial communities in altitudinal gradients have recently received much attention. The rhizosphere is a focus of soil microbial communities, but the patterns and drivers of these communities have rarely been studied in alpine ecosystems. We used high-throughput Illumina sequencing to examine the community variations of bacteria, archaea and fungi between the rhizosphere and bulk soil along an altitudinal gradient in an Abies fabri (Mast.) community on Mount Gongga of the eastern Tibetan Plateau. Microbial alpha diversity and community structure varied significantly with altitude but not between the rhizosphere and bulk soil. Soil temperature and the carbon:nitrogen ratio were the primary drivers of the structures of the bacterial, archaeal and fungal communities, and altitude (geographic distance) contributed a small part (<3%) of the community variation, indicating that various edaphic factors were the key regulators of microbial-community variation. This consistency of the microbial communities between the rhizosphere and bulk soil in this alpine ecosystem could be attributed to low temperature and high nutrient content. The bacterial, archaeal and fungal communities were governed by specific environmental factors (total phosphorus content for bacteria; organic-carbon content, dissolved organic-carbon content, NH4+-N content and nutrient stoichiometry for archaea and NO3−-N content for fungi). The distinct environmental responses of the microbial taxa suggested metabolic separation and resource preferences of the belowground communities, even within the small-scale spatial distances in this alpine ecosystem. Our study suggested that the ecosystem harbored many microbial taxa with diverse nutrient preferences and metabolic characteristics and could thus potentially tolerate the soil environmental variation under a scenario of climate change. [Display omitted] •Microbes in rhizosphere and bulk soil are highly similar in the alpine ecosystem.•Microbial community varies significantly with altitude within the same vegetation.•Soil temperature and the C:N ratio are the key drivers of microbial communities.•Bacteria, archaea and fungi are respectively affected by TP, NH4+-N and NO3−-N.
AbstractList The diversity patterns and drivers of soil microbial communities in altitudinal gradients have recently received much attention. The rhizosphere is a focus of soil microbial communities, but the patterns and drivers of these communities have rarely been studied in alpine ecosystems. We used high-throughput Illumina sequencing to examine the community variations of bacteria, archaea and fungi between the rhizosphere and bulk soil along an altitudinal gradient in an Abies fabri (Mast.) community on Mount Gongga of the eastern Tibetan Plateau. Microbial alpha diversity and community structure varied significantly with altitude but not between the rhizosphere and bulk soil. Soil temperature and the carbon:nitrogen ratio were the primary drivers of the structures of the bacterial, archaeal and fungal communities, and altitude (geographic distance) contributed a small part (<3%) of the community variation, indicating that various edaphic factors were the key regulators of microbial-community variation. This consistency of the microbial communities between the rhizosphere and bulk soil in this alpine ecosystem could be attributed to low temperature and high nutrient content. The bacterial, archaeal and fungal communities were governed by specific environmental factors (total phosphorus content for bacteria; organic-carbon content, dissolved organic-carbon content, NH4+-N content and nutrient stoichiometry for archaea and NO3−-N content for fungi). The distinct environmental responses of the microbial taxa suggested metabolic separation and resource preferences of the belowground communities, even within the small-scale spatial distances in this alpine ecosystem. Our study suggested that the ecosystem harbored many microbial taxa with diverse nutrient preferences and metabolic characteristics and could thus potentially tolerate the soil environmental variation under a scenario of climate change.
The diversity patterns and drivers of soil microbial communities in altitudinal gradients have recently received much attention. The rhizosphere is a focus of soil microbial communities, but the patterns and drivers of these communities have rarely been studied in alpine ecosystems. We used high-throughput Illumina sequencing to examine the community variations of bacteria, archaea and fungi between the rhizosphere and bulk soil along an altitudinal gradient in an Abies fabri (Mast.) community on Mount Gongga of the eastern Tibetan Plateau. Microbial alpha diversity and community structure varied significantly with altitude but not between the rhizosphere and bulk soil. Soil temperature and the carbon:nitrogen ratio were the primary drivers of the structures of the bacterial, archaeal and fungal communities, and altitude (geographic distance) contributed a small part (<3%) of the community variation, indicating that various edaphic factors were the key regulators of microbial-community variation. This consistency of the microbial communities between the rhizosphere and bulk soil in this alpine ecosystem could be attributed to low temperature and high nutrient content. The bacterial, archaeal and fungal communities were governed by specific environmental factors (total phosphorus content for bacteria; organic-carbon content, dissolved organic-carbon content, NH4+-N content and nutrient stoichiometry for archaea and NO3−-N content for fungi). The distinct environmental responses of the microbial taxa suggested metabolic separation and resource preferences of the belowground communities, even within the small-scale spatial distances in this alpine ecosystem. Our study suggested that the ecosystem harbored many microbial taxa with diverse nutrient preferences and metabolic characteristics and could thus potentially tolerate the soil environmental variation under a scenario of climate change. [Display omitted] •Microbes in rhizosphere and bulk soil are highly similar in the alpine ecosystem.•Microbial community varies significantly with altitude within the same vegetation.•Soil temperature and the C:N ratio are the key drivers of microbial communities.•Bacteria, archaea and fungi are respectively affected by TP, NH4+-N and NO3−-N.
Author Shen, Guoting
Yu, Jialuo
Fang, Linchuan
Wu, Yanhong
Bing, Haijian
Jiang, Mao
Zhang, Xingchang
Wang, Xia
Cui, Yongxing
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  orcidid: 0000-0002-8624-2785
  surname: Cui
  fullname: Cui, Yongxing
  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
– sequence: 2
  givenname: Haijian
  surname: Bing
  fullname: Bing, Haijian
  organization: Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, PR China
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  givenname: Linchuan
  surname: Fang
  fullname: Fang, Linchuan
  email: flinc629@hotmail.com
  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
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  givenname: Yanhong
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  fullname: Yu, Jialuo
  organization: University of Chinese Academy of Sciences, Beijing 100049, PR China
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  givenname: Guoting
  surname: Shen
  fullname: Shen, Guoting
  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
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  givenname: Mao
  surname: Jiang
  fullname: Jiang, Mao
  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
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  givenname: Xia
  surname: Wang
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  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
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  surname: Zhang
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  organization: State Key Laboratory of soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, PR China
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Keywords Rhizosphere
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Edaphic factors
Altitudinal gradients
Microbial community
Alpine ecosystems
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PublicationDate 2019-03-15
PublicationDateYYYYMMDD 2019-03-15
PublicationDate_xml – month: 03
  year: 2019
  text: 2019-03-15
  day: 15
PublicationDecade 2010
PublicationTitle Geoderma
PublicationYear 2019
Publisher Elsevier B.V
Publisher_xml – name: Elsevier B.V
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Snippet The diversity patterns and drivers of soil microbial communities in altitudinal gradients have recently received much attention. The rhizosphere is a focus of...
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SubjectTerms Abies fabri
Alpine ecosystems
altitude
Altitudinal gradients
ammonium nitrogen
Archaea
bacteria
carbon nitrogen ratio
China
climate change
community structure
ecosystems
Edaphic factors
fungal communities
fungi
Microbial community
Mount Gongga
nitrate nitrogen
nutrient content
Rhizosphere
soil microorganisms
soil temperature
species diversity
stoichiometry
total phosphorus
Title Diversity patterns of the rhizosphere and bulk soil microbial communities along an altitudinal gradient in an alpine ecosystem of the eastern Tibetan Plateau
URI https://dx.doi.org/10.1016/j.geoderma.2018.11.047
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