Soil-Borne Microbial Functional Structure across Different Land Uses

Land use change alters the structure and composition of microbial communities. However, the links between environmental factors and microbial functions are not well understood. Here we interrogated the functional structure of soil microbial communities across different land uses. In a multivariate r...

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Main Authors: Eiko E. Kuramae, Jizhong Z. Zhou, George A. Kowalchuk, Johannes A. van Veen
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2014/216071
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author Eiko E. Kuramae
Jizhong Z. Zhou
George A. Kowalchuk
Johannes A. van Veen
author_facet Eiko E. Kuramae
Jizhong Z. Zhou
George A. Kowalchuk
Johannes A. van Veen
author_sort Eiko E. Kuramae
collection DOAJ
description Land use change alters the structure and composition of microbial communities. However, the links between environmental factors and microbial functions are not well understood. Here we interrogated the functional structure of soil microbial communities across different land uses. In a multivariate regression tree analysis of soil physicochemical properties and genes detected by functional microarrays, the main factor that explained the different microbial community functional structures was C : N ratio. C : N ratio showed a significant positive correlation with clay and soil pH. Fields with low C : N ratio had an overrepresentation of genes for carbon degradation, carbon fixation, metal reductase, and organic remediation categories, while fields with high C : N ratio had an overrepresentation of genes encoding dissimilatory sulfate reductase, methane oxidation, nitrification, and nitrogen fixation. The most abundant genes related to carbon degradation comprised bacterial and fungal cellulases; bacterial and fungal chitinases; fungal laccases; and bacterial, fungal, and oomycete polygalacturonases. The high number of genes related to organic remediation was probably driven by high phosphate content, while the high number of genes for nitrification was probably explained by high total nitrogen content. The functional gene diversity found in different soils did not group the sites accordingly to land management. Rather, the soil factors, C : N ratio, phosphate, and total N, were the main factors driving the differences in functional genes across the fields examined.
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language English
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record_format Article
series The Scientific World Journal
spelling doaj-art-1ce7b44e47c344e5ba8b58ab0ccb3cda2025-02-03T05:43:40ZengWileyThe Scientific World Journal2356-61401537-744X2014-01-01201410.1155/2014/216071216071Soil-Borne Microbial Functional Structure across Different Land UsesEiko E. Kuramae0Jizhong Z. Zhou1George A. Kowalchuk2Johannes A. van Veen3Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), 6708 PB Wageningen, The NetherlandsInstitute for Environmental Genomics, University of Oklahoma, Norman, OK 73019, USADepartment of Biology, Utrecht University, 3512 JE Utrecht, The NetherlandsDepartment of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), 6708 PB Wageningen, The NetherlandsLand use change alters the structure and composition of microbial communities. However, the links between environmental factors and microbial functions are not well understood. Here we interrogated the functional structure of soil microbial communities across different land uses. In a multivariate regression tree analysis of soil physicochemical properties and genes detected by functional microarrays, the main factor that explained the different microbial community functional structures was C : N ratio. C : N ratio showed a significant positive correlation with clay and soil pH. Fields with low C : N ratio had an overrepresentation of genes for carbon degradation, carbon fixation, metal reductase, and organic remediation categories, while fields with high C : N ratio had an overrepresentation of genes encoding dissimilatory sulfate reductase, methane oxidation, nitrification, and nitrogen fixation. The most abundant genes related to carbon degradation comprised bacterial and fungal cellulases; bacterial and fungal chitinases; fungal laccases; and bacterial, fungal, and oomycete polygalacturonases. The high number of genes related to organic remediation was probably driven by high phosphate content, while the high number of genes for nitrification was probably explained by high total nitrogen content. The functional gene diversity found in different soils did not group the sites accordingly to land management. Rather, the soil factors, C : N ratio, phosphate, and total N, were the main factors driving the differences in functional genes across the fields examined.http://dx.doi.org/10.1155/2014/216071
spellingShingle Eiko E. Kuramae
Jizhong Z. Zhou
George A. Kowalchuk
Johannes A. van Veen
Soil-Borne Microbial Functional Structure across Different Land Uses
The Scientific World Journal
title Soil-Borne Microbial Functional Structure across Different Land Uses
title_full Soil-Borne Microbial Functional Structure across Different Land Uses
title_fullStr Soil-Borne Microbial Functional Structure across Different Land Uses
title_full_unstemmed Soil-Borne Microbial Functional Structure across Different Land Uses
title_short Soil-Borne Microbial Functional Structure across Different Land Uses
title_sort soil borne microbial functional structure across different land uses
url http://dx.doi.org/10.1155/2014/216071
work_keys_str_mv AT eikoekuramae soilbornemicrobialfunctionalstructureacrossdifferentlanduses
AT jizhongzzhou soilbornemicrobialfunctionalstructureacrossdifferentlanduses
AT georgeakowalchuk soilbornemicrobialfunctionalstructureacrossdifferentlanduses
AT johannesavanveen soilbornemicrobialfunctionalstructureacrossdifferentlanduses