Rate-specific responses of prokaryotic diversity and structure to nitrogen deposition in the Leymus chinensis steppe

Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However, it is unclear how these changes are dependent on N deposition rates, other factors induced by N (e.g., pH), and their interactions. In this...

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Published inSoil biology & biochemistry Vol. 79; pp. 81 - 90
Main Authors Yao, Minjie, Rui, Junpeng, Li, Jiabao, Dai, Yumei, Bai, Yongfei, Heděnec, Petr, Wang, Junming, Zhang, Shiheng, Pei, Kequan, Liu, Chi, Wang, Yanfen, Zhili He, Frouz, Jan, Li, Xiangzhen
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier Ltd 01.12.2014
Elsevier
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Abstract Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However, it is unclear how these changes are dependent on N deposition rates, other factors induced by N (e.g., pH), and their interactions. In this study, we investigated the responses of soil prokaryotic community structure and stability after a 13-year N addition in the semi-arid Leymus chinensis steppe in Inner Mongolia, China. Our results demonstrated that the prokaryotic community structure changed at the low N addition rate of 1.75 g N m−2 yr−1; however, dramatic changes in microbial abundance, respiratory quotient, and prokaryotic diversity occurred at N addition rates of more than 5.25 g N m−2 yr−1 when the soil pH dropped below 6.0. The two patterns indicated the difference in driving forces for different microbial properties. The N-driven and pH-driven processes are likely the most important mechanisms determining the responses of bacterial community to N. Some copiotrophic/oligotrophic bacteria, e.g., Proteobacteria and Acidobacteria, changed their relative abundances with the N addition continuously even at a low rate, indicating that they were more sensitive to N directly. Some bacterial groups significantly changed their relative abundance at a high N addition rate when pH dropped below 6.0, e.g., Verrucomicrobia and Armatimonadetes, indicating that they were more sensitive to pH below 6.0. N addition altered the prokaryotic community structure through enrichment of copiotrophic bacteria (species adjustment) at low N addition rates and through enrichment of nitrophilous taxa and significant loss of diversity at high N rates. The results also demonstrated that a high N addition diminished the stability of the prokaryotic community structure and activity through reduction in species diversity and bacterial interaction. Overall, this study supported the hypothesis that the responses of prokaryota to N were dependent on deposition rates, and N-driven and pH-driven processes were the important mechanisms to control the shift of the prokaryotic community. •The responses of prokaryota to nitrogen are dependent on deposition rates.•Nitrogen-driven and pH-driven processes are important mechanisms.•Prokaryota changes dramatically when pH drops below 6.0 at high N deposition rates.•High N deposition simplifies the microbial interaction network.•High N deposition diminishes the stability of prokaryotic community structure.
AbstractList Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However, it is unclear how these changes are dependent on N deposition rates, other factors induced by N (e.g., pH), and their interactions. In this study, we investigated the responses of soil prokaryotic community structure and stability after a 13-year N addition in the semi-arid Leymus chinensis steppe in Inner Mongolia, China. Our results demonstrated that the prokaryotic community structure changed at the low N addition rate of 1.75 g N m super(-2) yr super(-1); however, dramatic changes in microbial abundance, respiratory quotient, and prokaryotic diversity occurred at N addition rates of more than 5.25 g N m super(-2) yr super(-1) when the soil pH dropped below 6.0. The two patterns indicated the difference in driving forces for different microbial properties. The N-driven and pH-driven processes are likely the most important mechanisms determining the responses of bacterial community to N. Some copiotrophic/oligotrophic bacteria, e.g., Proteobacteria and Acidobacteria, changed their relative abundances with the N addition continuously even at a low rate, indicating that they were more sensitive to N directly. Some bacterial groups significantly changed their relative abundance at a high N addition rate when pH dropped below 6.0, e.g., Verrucomicrobia and Armatimonadetes, indicating that they were more sensitive to pH below 6.0. N addition altered the prokaryotic community structure through enrichment of copiotrophic bacteria (species adjustment) at low N addition rates and through enrichment of nitrophilous taxa and significant loss of diversity at high N rates. The results also demonstrated that a high N addition diminished the stability of the prokaryotic community structure and activity through reduction in species diversity and bacterial interaction. Overall, this study supported the hypothesis that the responses of prokaryota to N were dependent on deposition rates, and N-driven and pH-driven processes were the important mechanisms to control the shift of the prokaryotic community.
Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However, it is unclear how these changes are dependent on N deposition rates, other factors induced by N (e.g., pH), and their interactions. In this study, we investigated the responses of soil prokaryotic community structure and stability after a 13-year N addition in the semi-arid Leymus chinensis steppe in Inner Mongolia, China. Our results demonstrated that the prokaryotic community structure changed at the low N addition rate of 1.75 g N m−2 yr−1; however, dramatic changes in microbial abundance, respiratory quotient, and prokaryotic diversity occurred at N addition rates of more than 5.25 g N m−2 yr−1 when the soil pH dropped below 6.0. The two patterns indicated the difference in driving forces for different microbial properties. The N-driven and pH-driven processes are likely the most important mechanisms determining the responses of bacterial community to N. Some copiotrophic/oligotrophic bacteria, e.g., Proteobacteria and Acidobacteria, changed their relative abundances with the N addition continuously even at a low rate, indicating that they were more sensitive to N directly. Some bacterial groups significantly changed their relative abundance at a high N addition rate when pH dropped below 6.0, e.g., Verrucomicrobia and Armatimonadetes, indicating that they were more sensitive to pH below 6.0. N addition altered the prokaryotic community structure through enrichment of copiotrophic bacteria (species adjustment) at low N addition rates and through enrichment of nitrophilous taxa and significant loss of diversity at high N rates. The results also demonstrated that a high N addition diminished the stability of the prokaryotic community structure and activity through reduction in species diversity and bacterial interaction. Overall, this study supported the hypothesis that the responses of prokaryota to N were dependent on deposition rates, and N-driven and pH-driven processes were the important mechanisms to control the shift of the prokaryotic community. •The responses of prokaryota to nitrogen are dependent on deposition rates.•Nitrogen-driven and pH-driven processes are important mechanisms.•Prokaryota changes dramatically when pH drops below 6.0 at high N deposition rates.•High N deposition simplifies the microbial interaction network.•High N deposition diminishes the stability of prokaryotic community structure.
Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However, it is unclear how these changes are dependent on N deposition rates, other factors induced by N (e.g., pH), and their interactions. In this study, we investigated the responses of soil prokaryotic community structure and stability after a 13-year N addition in the semi-arid Leymus chinensis steppe in Inner Mongolia, China. Our results demonstrated that the prokaryotic community structure changed at the low N addition rate of 1.75 g N m−2 yr−1; however, dramatic changes in microbial abundance, respiratory quotient, and prokaryotic diversity occurred at N addition rates of more than 5.25 g N m−2 yr−1 when the soil pH dropped below 6.0. The two patterns indicated the difference in driving forces for different microbial properties. The N-driven and pH-driven processes are likely the most important mechanisms determining the responses of bacterial community to N. Some copiotrophic/oligotrophic bacteria, e.g., Proteobacteria and Acidobacteria, changed their relative abundances with the N addition continuously even at a low rate, indicating that they were more sensitive to N directly. Some bacterial groups significantly changed their relative abundance at a high N addition rate when pH dropped below 6.0, e.g., Verrucomicrobia and Armatimonadetes, indicating that they were more sensitive to pH below 6.0. N addition altered the prokaryotic community structure through enrichment of copiotrophic bacteria (species adjustment) at low N addition rates and through enrichment of nitrophilous taxa and significant loss of diversity at high N rates. The results also demonstrated that a high N addition diminished the stability of the prokaryotic community structure and activity through reduction in species diversity and bacterial interaction. Overall, this study supported the hypothesis that the responses of prokaryota to N were dependent on deposition rates, and N-driven and pH-driven processes were the important mechanisms to control the shift of the prokaryotic community.
Author Dai, Yumei
Wang, Yanfen
Heděnec, Petr
Zhili He
Wang, Junming
Li, Jiabao
Pei, Kequan
Frouz, Jan
Yao, Minjie
Bai, Yongfei
Liu, Chi
Zhang, Shiheng
Li, Xiangzhen
Rui, Junpeng
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  fullname: Li, Jiabao
  organization: Key Laboratory of Environmental and Applied Microbiology, CAS, Sichuan 610041, PR China
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  givenname: Junming
  surname: Wang
  fullname: Wang, Junming
  organization: Section of Climate Science, Illinois State Water Survey, Prairie Research Institute, University of Illinois at Urbana-Champaign, Champaign, IL 61802, USA
– sequence: 8
  givenname: Shiheng
  surname: Zhang
  fullname: Zhang, Shiheng
  organization: Key Laboratory of Environmental and Applied Microbiology, CAS, Sichuan 610041, PR China
– sequence: 9
  givenname: Kequan
  surname: Pei
  fullname: Pei, Kequan
  organization: State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, 20 Nanxincun, Xiangshan, Beijing 100093, PR China
– sequence: 10
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  surname: Liu
  fullname: Liu, Chi
  organization: Key Laboratory of Environmental and Applied Microbiology, CAS, Sichuan 610041, PR China
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  surname: Wang
  fullname: Wang, Yanfen
  organization: Graduate School, University of Chinese Academy of Sciences, Beijing 100049, PR China
– sequence: 12
  surname: Zhili He
  fullname: Zhili He
  organization: Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization, CAS, Sichuan 610041, PR China
– sequence: 13
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  surname: Frouz
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  organization: Institute of Environmental Studies, Faculty of Science, Charles University in Prague, Benátska 2, 128 44 Prague 2, Czech Republic
– sequence: 14
  givenname: Xiangzhen
  surname: Li
  fullname: Li, Xiangzhen
  email: lixz@cib.ac.cn
  organization: Key Laboratory of Environmental and Applied Microbiology, CAS, Sichuan 610041, PR China
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AGRICOLA
AGRICOLA - Academic
DatabaseTitleList Aquatic Science & Fisheries Abstracts (ASFA) Professional

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EISSN 1879-3428
EndPage 90
ExternalDocumentID 28878125
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Fri Feb 23 02:23:27 EST 2024
IsPeerReviewed true
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Keywords Community structure
Copiotrophic bacteria
Oligotrophic bacteria
N deposition
Steppe ecosystem
Diversity
Monocotyledones
Perennial plant
Nitrogen
Gramineae
Steppe
Ecosystem
Angiospermae
Bacteria
Prokaryote
Herbaceous plant
Spermatophyta
Soil science
Fodder crop
Oligotrophy
Deposition
Language English
License CC BY 4.0
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ParticipantIDs proquest_miscellaneous_1836640069
proquest_miscellaneous_1635032296
pascalfrancis_primary_28878125
crossref_primary_10_1016_j_soilbio_2014_09_009
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  year: 2014
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  day: 01
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PublicationPlace Amsterdam
PublicationPlace_xml – name: Amsterdam
PublicationTitle Soil biology & biochemistry
PublicationYear 2014
Publisher Elsevier Ltd
Elsevier
Publisher_xml – name: Elsevier Ltd
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Snippet Serious nitrogen (N) deposition in terrestrial ecosystems causes soil acidification and changes the structure and function of the microbial community. However,...
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SubjectTerms Acidobacteria
Agronomy. Soil science and plant productions
bacteria
bacterial communities
Biochemistry and biology
Biological and medical sciences
Chemical, physicochemical, biochemical and biological properties
China
Community structure
Copiotrophic bacteria
Diversity
eutrophication
Fundamental and applied biological sciences. Psychology
Leymus chinensis
N deposition
nitrogen
Oligotrophic bacteria
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Proteobacteria
respiratory quotient
soil acidification
soil pH
Soil science
species diversity
Steppe ecosystem
steppes
terrestrial ecosystems
Verrucomicrobia
Verrucomicrobium
Title Rate-specific responses of prokaryotic diversity and structure to nitrogen deposition in the Leymus chinensis steppe
URI https://dx.doi.org/10.1016/j.soilbio.2014.09.009
https://www.proquest.com/docview/1635032296
https://www.proquest.com/docview/1836640069
Volume 79
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