Secondary forest succession drives differential responses of bacterial communities and interactions rather than bacterial functional groups in the rhizosphere and bulk soils in a subalpine region

Background and aims Community dynamics, functions and driving factors of rhizosphere and bulk soil bacteria during secondary forest succession remain poorly understood in subalpine regions. Methods Three typical successional stages (grassland, shrubland and secondary forest) were selected to analyse...

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Veröffentlicht in:Plant and soil 2023-03, Vol.484 (1-2), p.293-312
Hauptverfasser: Zhang, Xiaoying, Zhao, Wenqiang, Kou, Yongping, Liu, Yanjiao, He, Heliang, Liu, Qing
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container_issue 1-2
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creator Zhang, Xiaoying
Zhao, Wenqiang
Kou, Yongping
Liu, Yanjiao
He, Heliang
Liu, Qing
description Background and aims Community dynamics, functions and driving factors of rhizosphere and bulk soil bacteria during secondary forest succession remain poorly understood in subalpine regions. Methods Three typical successional stages (grassland, shrubland and secondary forest) were selected to analyse bacterial communities, functions and interactions in the rhizosphere and bulk soils using high-throughput sequencing technology. Results The results showed no significant difference in the bacterial α- diversity in the rhizosphere soil, whereas the bacterial α- diversity in the bulk soil of the grassland was significantly lower than that of the shrubland and secondary forest. Bacterial β- diversity in the rhizosphere soil differed significantly among the three succession stages, while the bacterial β- diversity in the bulk soil in the shrubland and secondary forest was significantly different from that in the grassland. However, the potential bacterial functions of the carbon, nitrogen and sulfate cycles revealed a consistent response in the rhizosphere and bulk soils to secondary forest succession. The soil total phosphorus, ammonium nitrogen, ratio of carbon to phosphorus and pH were the main factors affecting bacterial communities and potential functional groups. Bacterial network complexity was highest in the secondary forest rhizosphere soil and the shrubland bulk soil. Different keystone bacteria were detected in the rhizosphere and bulk soils among the three successional stages; they play major role in maintaining ecosystem function and community structure. Conclusion Our results demonstrate that the bacterial communities and interactions in the rhizosphere and bulk soils respond differently to secondary forest succession, while the bacterial functional groups revealed a consistent response.
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Methods Three typical successional stages (grassland, shrubland and secondary forest) were selected to analyse bacterial communities, functions and interactions in the rhizosphere and bulk soils using high-throughput sequencing technology. Results The results showed no significant difference in the bacterial α- diversity in the rhizosphere soil, whereas the bacterial α- diversity in the bulk soil of the grassland was significantly lower than that of the shrubland and secondary forest. Bacterial β- diversity in the rhizosphere soil differed significantly among the three succession stages, while the bacterial β- diversity in the bulk soil in the shrubland and secondary forest was significantly different from that in the grassland. However, the potential bacterial functions of the carbon, nitrogen and sulfate cycles revealed a consistent response in the rhizosphere and bulk soils to secondary forest succession. The soil total phosphorus, ammonium nitrogen, ratio of carbon to phosphorus and pH were the main factors affecting bacterial communities and potential functional groups. Bacterial network complexity was highest in the secondary forest rhizosphere soil and the shrubland bulk soil. Different keystone bacteria were detected in the rhizosphere and bulk soils among the three successional stages; they play major role in maintaining ecosystem function and community structure. Conclusion Our results demonstrate that the bacterial communities and interactions in the rhizosphere and bulk soils respond differently to secondary forest succession, while the bacterial functional groups revealed a consistent response.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-022-05788-5</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Agriculture ; Ammonium ; Analysis ; Bacteria ; Biomedical and Life Sciences ; Carbon ; Carbon cycle ; Community structure ; Deforestation ; Ecological function ; Ecological succession ; Ecology ; Forests ; Functional groups ; Grasslands ; Identification and classification ; Life Sciences ; Next-generation sequencing ; Nitrogen ; Phosphorus ; Plant Physiology ; Plant Sciences ; Research Article ; Rhizosphere ; Shrublands ; Soil bacteria ; Soil dynamics ; Soil microbiology ; Soil microorganisms ; Soil Science &amp; Conservation ; Soil structure ; Soils ; Structure-function relationships</subject><ispartof>Plant and soil, 2023-03, Vol.484 (1-2), p.293-312</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2022. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><rights>COPYRIGHT 2023 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c358t-7b051786f6f86bcb5129a800e5a9472d34e2773ed52161030410a4206aa3db763</citedby><cites>FETCH-LOGICAL-c358t-7b051786f6f86bcb5129a800e5a9472d34e2773ed52161030410a4206aa3db763</cites><orcidid>0000-0002-7046-0307</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11104-022-05788-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11104-022-05788-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27922,27923,41486,42555,51317</link.rule.ids></links><search><creatorcontrib>Zhang, Xiaoying</creatorcontrib><creatorcontrib>Zhao, Wenqiang</creatorcontrib><creatorcontrib>Kou, Yongping</creatorcontrib><creatorcontrib>Liu, Yanjiao</creatorcontrib><creatorcontrib>He, Heliang</creatorcontrib><creatorcontrib>Liu, Qing</creatorcontrib><title>Secondary forest succession drives differential responses of bacterial communities and interactions rather than bacterial functional groups in the rhizosphere and bulk soils in a subalpine region</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Background and aims Community dynamics, functions and driving factors of rhizosphere and bulk soil bacteria during secondary forest succession remain poorly understood in subalpine regions. Methods Three typical successional stages (grassland, shrubland and secondary forest) were selected to analyse bacterial communities, functions and interactions in the rhizosphere and bulk soils using high-throughput sequencing technology. Results The results showed no significant difference in the bacterial α- diversity in the rhizosphere soil, whereas the bacterial α- diversity in the bulk soil of the grassland was significantly lower than that of the shrubland and secondary forest. Bacterial β- diversity in the rhizosphere soil differed significantly among the three succession stages, while the bacterial β- diversity in the bulk soil in the shrubland and secondary forest was significantly different from that in the grassland. However, the potential bacterial functions of the carbon, nitrogen and sulfate cycles revealed a consistent response in the rhizosphere and bulk soils to secondary forest succession. 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subjects Agriculture
Ammonium
Analysis
Bacteria
Biomedical and Life Sciences
Carbon
Carbon cycle
Community structure
Deforestation
Ecological function
Ecological succession
Ecology
Forests
Functional groups
Grasslands
Identification and classification
Life Sciences
Next-generation sequencing
Nitrogen
Phosphorus
Plant Physiology
Plant Sciences
Research Article
Rhizosphere
Shrublands
Soil bacteria
Soil dynamics
Soil microbiology
Soil microorganisms
Soil Science & Conservation
Soil structure
Soils
Structure-function relationships
title Secondary forest succession drives differential responses of bacterial communities and interactions rather than bacterial functional groups in the rhizosphere and bulk soils in a subalpine region
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