Is vegetation composition or soil chemistry the best predictor of the soil microbial community

With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predict...

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Published inPlant and soil Vol. 333; no. 1-2; pp. 417 - 430
Main Authors Mitchell, Ruth J, Hester, Alison J, Campbell, Colin D, Chapman, Stephen J, Cameron, Clare M, Hewison, Richard L, Potts, Jackie M
Format Journal Article
LanguageEnglish
Published Dordrecht Dordrecht : Springer Netherlands 01.08.2010
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Abstract With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predicts the soil microbial community. The above and below-ground communities and soil chemical properties along a successional gradient from dwarf shrubland (moorland) to deciduous woodland (Betula dominated) were studied. The vegetation and soil chemistry were recorded and the soil microbial community (SMC) assessed using Phospholipid Fatty Acid Extraction (PLFA) and Multiplex Terminal Restriction Fragment Length Polymorphism (M-TRFLP). Vegetation composition and soil chemistry were used to predict the SMC using Co-Correspondence analysis and Canonical Correspondence Analysis and the predictive power of the two analyses compared. The vegetation composition predicted the soil microbial community at least as well as the soil chemical data. Removing rare plant species from the data set did not improve the predictive power of the vegetation data. The predictive power of the soil chemistry improved when only selected soil variables were used, but which soil variables gave the best prediction varied between the different soil microbial communities being studied (PLFA or bacterial/fungal/archaeal TRFLP). Vegetation composition may represent a more stable ‘summary' of the effects of multiple drivers over time and may thus be a better predictor of the soil microbial community than one-off measurements of soil properties.
AbstractList With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predicts the soil microbial community. The above and below-ground communities and soil chemical properties along a successional gradient from dwarf shrubland (moorland) to deciduous woodland (Betula dominated) were studied. The vegetation and soil chemistry were recorded and the soil microbial community (SMC) assessed using Phospholipid Fatty Acid Extraction (PLFA) and Multiplex Terminal Restriction Fragment Length Polymorphism (M-TRFLP). Vegetation composition and soil chemistry were used to predict the SMC using Co-Correspondence analysis and Canonical Correspondence Analysis and the predictive power of the two analyses compared. The vegetation composition predicted the soil microbial community at least as well as the soil chemical data. Removing rare plant species from the data set did not improve the predictive power of the vegetation data. The predictive power of the soil chemistry improved when only selected soil variables were used, but which soil variables gave the best prediction varied between the different soil microbial communities being studied (PLFA or bacterial/fungal/archaeal TRFLP). Vegetation composition may represent a more stable 'summary' of the effects of multiple drivers over time and may thus be a better predictor of the soil microbial community than one-off measurements of soil properties. Keywords Co-correspondence analysis * Ecosystem Engineer * Succession * Moorland * TRFLP * PLFA
With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predicts the soil microbial community. The above and below-ground communities and soil chemical properties along a successional gradient from dwarf shrubland (moorland) to deciduous woodland (Betula dominated) were studied. The vegetation and soil chemistry were recorded and the soil microbial community (SMC) assessed using Phospholipid Fatty Acid Extraction (PLFA) and Multiplex Terminal Restriction Fragment Length Polymorphism (M-TRFLP). Vegetation composition and soil chemistry were used to predict the SMC using Co-Correspondence analysis and Canonical Correspondence Analysis and the predictive power of the two analyses compared. The vegetation composition predicted the soil microbial community at least as well as the soil chemical data. Removing rare plant species from the data set did not improve the predictive power of the vegetation data. The predictive power of the soil chemistry improved when only selected soil variables were used, but which soil variables gave the best prediction varied between the different soil microbial communities being studied (PLFA or bacterial/fungal/archaeal TRFLP). Vegetation composition may represent a more stable 'summary' of the effects of multiple drivers over time and may thus be a better predictor of the soil microbial community than one-off measurements of soil properties.
With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predicts the soil microbial community. The above and below-ground communities and soil chemical properties along a successional gradient from dwarf shrubland (moorland) to deciduous woodland ( Betula dominated) were studied. The vegetation and soil chemistry were recorded and the soil microbial community (SMC) assessed using Phospholipid Fatty Acid Extraction (PLFA) and Multiplex Terminal Restriction Fragment Length Polymorphism (M-TRFLP). Vegetation composition and soil chemistry were used to predict the SMC using Co-Correspondence analysis and Canonical Correspondence Analysis and the predictive power of the two analyses compared. The vegetation composition predicted the soil microbial community at least as well as the soil chemical data. Removing rare plant species from the data set did not improve the predictive power of the vegetation data. The predictive power of the soil chemistry improved when only selected soil variables were used, but which soil variables gave the best prediction varied between the different soil microbial communities being studied (PLFA or bacterial/fungal/archaeal TRFLP). Vegetation composition may represent a more stable ‘summary’ of the effects of multiple drivers over time and may thus be a better predictor of the soil microbial community than one-off measurements of soil properties.
With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally, predict how changes in one part of the ecosystem will affect another. Here we assess if vegetation composition or soil chemistry best predicts the soil microbial community. The above and below-ground communities and soil chemical properties along a successional gradient from dwarf shrubland (moorland) to deciduous woodland (Betula dominated) were studied. The vegetation and soil chemistry were recorded and the soil microbial community (SMC) assessed using Phospholipid Fatty Acid Extraction (PLFA) and Multiplex Terminal Restriction Fragment Length Polymorphism (M-TRFLP). Vegetation composition and soil chemistry were used to predict the SMC using Co-Correspondence analysis and Canonical Correspondence Analysis and the predictive power of the two analyses compared. The vegetation composition predicted the soil microbial community at least as well as the soil chemical data. Removing rare plant species from the data set did not improve the predictive power of the vegetation data. The predictive power of the soil chemistry improved when only selected soil variables were used, but which soil variables gave the best prediction varied between the different soil microbial communities being studied (PLFA or bacterial/fungal/archaeal TRFLP). Vegetation composition may represent a more stable 'summary' of the effects of multiple drivers over time and may thus be a better predictor of the soil microbial community than one-off measurements of soil properties. [PUBLICATION ABSTRACT]
Audience Academic
Author Cameron, Clare M.
Mitchell, Ruth J.
Hester, Alison J.
Hewison, Richard L.
Campbell, Colin D.
Chapman, Stephen J.
Potts, Jackie M.
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  fullname: Chapman, Stephen J
– sequence: 5
  fullname: Cameron, Clare M
– sequence: 6
  fullname: Hewison, Richard L
– sequence: 7
  fullname: Potts, Jackie M
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IEDL.DBID U2A
ISSN 0032-079X
1573-5036
IngestDate Thu Aug 21 06:30:06 EDT 2025
Thu Jul 10 22:35:17 EDT 2025
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IsPeerReviewed true
IsScholarly true
Issue 1-2
Keywords Moorland
Succession
PLFA
TRFLP
Co-correspondence analysis
Ecosystem engineer
Microbial activity
Predictor
Phospholipid
Correspondence analysis
Ecosystem
Soil science
Vegetation structure
Microbial community
Organic compounds
Soil chemistry
Heathland and moor
Data analysis
Floristic composition
Aliphatic compound
Property of soil
Complex lipid
Fatty acids
Biological activity
Statistical method
Soils
Restriction fragment length polymorphism
Applied mathematics
Soil plant relation
Language English
License http://www.springer.com/tdm
CC BY 4.0
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Notes http://dx.doi.org/10.1007/s11104-010-0357-7
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ObjectType-Article-1
ObjectType-Feature-2
content type line 23
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PQPubID 54098
PageCount 14
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PublicationDate 2010-08-01
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PublicationDate_xml – month: 08
  year: 2010
  text: 2010-08-01
  day: 01
PublicationDecade 2010
PublicationPlace Dordrecht
PublicationPlace_xml – name: Dordrecht
PublicationSubtitle An International Journal on Plant-Soil Relationships
PublicationTitle Plant and soil
PublicationTitleAbbrev Plant Soil
PublicationYear 2010
Publisher Dordrecht : Springer Netherlands
Springer
Springer Netherlands
Springer Nature B.V
Publisher_xml – name: Dordrecht : Springer Netherlands
– name: Springer
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MacdonaldCASinghBKPeckJAvan SchaikAPHunterLCHorswellJCampbellCDSpeirTWLong-term exposure to Zn-spiked sewage sludge alters soil community structureSoil Biol Biochem2007392576258610.1016/j.soilbio.2007.04.0281:CAS:528:DC%2BD2sXotVagtLw%3D
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MitchellRJCampbellCDChapmanSJOslerGHRVanbergenAJRossLRCameronCMColeLThe cascading effects of birch on heather moorland: a test for the top-down control of an ecosystem engineerJ Ecol20079554055410.1111/j.1365-2745.2007.01227.x1:CAS:528:DC%2BD2sXlvFyrtb8%3D
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MilesJThe pedogenic effects of different species and vegetation types and the implications of successionJ Soil Sci19853657158410.1111/j.1365-2389.1985.tb00359.x
Haseman JF, Marshall CE (1945) The use of heavy minerals in studies of the origin and development of soils. University of Missouri College of Agriculture Experimental Station Research Bulletin No. 387
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van der HeijdenMGABardgettRDvan StraalenNMThe unseen majority: soil microbes as drivers of plant diversity and productivity in terrestrial ecosystemsEcol Lett20081129631010.1111/j.1461-0248.2007.01139.x18047587
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HacklEPfefferMDonatC
RD Bardgett (357_CR4) 2005
357_CR17
BK Singh (357_CR47) 2006; 72
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J Miles (357_CR31) 1980; 11
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R Rinnan (357_CR43) 2007; 13
AP Schaffers (357_CR45) 2008; 89
T Pennanen (357_CR39) 1998; 64
E Bååth (357_CR2) 2003; 35
G Certini (357_CR8) 2004; 36
J Pastor (357_CR37) 2006
DA Wardle (357_CR57) 2005
TM Bezemer (357_CR5) 2006; 94
357_CR46
LI Sørensen (357_CR50) 2009; 12
J Miles (357_CR30) 1985; 36
CA Macdonald (357_CR26) 2007; 39
SJ Grayston (357_CR15) 1998; 30
CJF Braak Ter (357_CR53) 2002
RD Bardgett (357_CR3) 1996; 22
SE Allen (357_CR1) 1989
357_CR40
SAS (357_CR44) 2005
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J Pastor (357_CR36) 1997; 51
Å Frostegård (357_CR10) 1993; 59
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RS Smith (357_CR49) 2003; 40
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HL Reynolds (357_CR42) 2003; 84
MN Högberg (357_CR22) 2007; 150
TJ White (357_CR61) 1990
J Frouz (357_CR11) 2008; 44
JR Marchesi (357_CR28) 1998; 64
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DA Wardle (357_CR58) 1999; 69
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L Hauben (357_CR18) 1997; 47
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357_CR27
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G Jurgens (357_CR24) 1997; 63
E Hackl (357_CR16) 2005; 37
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DA Wardle (357_CR59) 2001; 71
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EO Casamayor (357_CR7) 2002; 4
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– reference: WhiteTJBrunsTDLeeSTaylorJInnisMAGelfordDHSninskyJJWhiteTJAnalysis of phylogenetic relationship by amplification and direct sequencing of ribosomal RNA genesPCR protocols: a guide to methods and applications1990New YorkAcademic315322
– reference: ChenM-MZhuY-GSuY-HChenB-DFuB-JMarschnerPEffects of soil moisture and plant interactions on the soil microbial community structureEur J Soil Biol200743313810.1016/j.ejsobi.2006.05.0011:CAS:528:DC%2BD1cXhtleqtrc%3D
– reference: MilesJThe pedogenic effects of different species and vegetation types and the implications of successionJ Soil Sci19853657158410.1111/j.1365-2389.1985.tb00359.x
– reference: PastorJCohenYHobbsNTDanellKBergstromRDuncanPPastorJThe roles of large herbivores in ecosystem nutrient cyclesLarge herbivore ecology, ecosystem dynamics and conservation2006CambridgeCambridge University Press
– reference: SmithBFLBainDCA sodium-hydroxide fusion method for the determination of total phosphate in soilsCommun Soil Sci Plant Anal19821318519010.1080/001036282093672571:CAS:528:DyaL38Xhsl2qtbg%3D
– reference: FrouzJPrachKPizlVHanelLStaryJTajovskyKMaternaJBalikVKalcikJRehounkovaKInteractions between soil development, vegetation and soil fauna during spontaneous succession in post mining sitesEur J Soil Biol20084410912110.1016/j.ejsobi.2007.09.002
– reference: Haseman JF, Marshall CE (1945) The use of heavy minerals in studies of the origin and development of soils. University of Missouri College of Agriculture Experimental Station Research Bulletin No. 387
– reference: WohlrabGTuvesonRWOlmstedCEFungal populations from early stages of succession in Indiana dune sandEcology19634473474010.2307/1933020
– reference: SASSAS Software Version 9.12005CarySAS
– reference: SmithRSShieldRSBardgetttRDMillwardDCorkhillPRolphGHobbsPJPeacockSDiversification management of meadow grassland: plant species diversity and functional traits associated with change in meadow vegetation and soil microbial communitiesJ Appl Ecol200340516410.1046/j.1365-2664.2003.00780.x
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– reference: LavellePBignellDLepageMWoltersVRogerPInesonPHealODhillionSSoil function in a changing world: the role of invertebrate ecosystem engineersEur J Soil Biol1997331591931:CAS:528:DyaK1cXmvVWnsro%3D
– reference: WilliamsonWMWardleDAYeatesGWChanges in soil microbial and nematode communities during ecosystem decline across a long-term chronosequenceSoil Biol Biochem2005371289130110.1016/j.soilbio.2004.11.0251:CAS:528:DC%2BD2MXjtlWjtbs%3D
– reference: MitchellRJCampbellCDChapmanSJCameronCMThe engineering impact of a single tree species on the soil microbial communityJ Ecol201098506110.1111/j.1365-2745.2009.01601.x1:CAS:528:DC%2BC3cXhtFOmu7s%3D
– reference: SchaffersAPRaemakersIPSỳkoraKVter BraakCJFArthropod assemblages are best predicted by plant species compositionEcology20088978279410.1890/07-0361.118459341
– reference: Simpson GL (2005) Cocorresp: co-correspondence analysis ordination methods for community ecology. R foundation for statistical computing, Vienna, Austria, published at http://www.R-project.org.
– reference: StephanAMeyerAHSchmideBPlant diversity affects culturable soil bacteria in experimental grassland communitiesJ Ecol20008898899810.1046/j.1365-2745.2000.00510.x
– reference: GardesMBrunsTBITS primers with enhanced specificity for basidiomycetes: application to the identification of mycorrhiza and rustsMol Ecol1993211311810.1111/j.1365-294X.1993.tb00005.x1:CAS:528:DyaK3sXlslOmsro%3D8180733
– reference: GoodwinJThe role of mycorrhizal fungi in competitive interactions among native bunchgrasses and alien weeds—a review and synthesisNorthwest Sci199266251260
– reference: CertiniGCampbellCDEdwardsACRock fragments in soil support a different microbial community from the fine earthSoil Biol Biochem2004361119112810.1016/j.soilbio.2004.02.0221:CAS:528:DC%2BD2cXltVKiu7g%3D
– reference: R Development Core Team (2006) R: a language and environment for statistical computing. R foundation for statistical computing, Vienna, Austria, Published at http://www.R-project.org.
– reference: AllenSEChemical analysis of ecological material19892OxfordBlackwell Scientific
– reference: BardgettRDYeatesGWAndersonJMBardgettRDUsherMBHopkinsDWPatterns and determinants of soil biological diversityBiological diversity and function in soils2005CambridgeCambridge University Press10011810.1017/CBO9780511541926.007
– reference: PellaEColomboBStudy of carbon, hydrogen and nitrogen by combustion gas chromatographyMikrochim Acta19735697719
– reference: FrostegårdÅTunlidABååthEPhospholipid fatty acid composition, biomass and activity of microbial communities from two soil types experimentally exposed to different heavy metalsAppl Environ Microbiol1993593605361716349080
– reference: MitchellRJCampbellCDChapmanSJOslerGHRVanbergenAJRossLRCameronCMColeLThe cascading effects of birch on heather moorland: a test for the top-down control of an ecosystem engineerJ Ecol20079554055410.1111/j.1365-2745.2007.01227.x1:CAS:528:DC%2BD2sXlvFyrtb8%3D
– reference: OrwinKHWardleDAGreenfieldLGEcological consequences of carbon substrate identity and diversity in a laboratory studyEcololgy20068758059310.1890/05-0383
– reference: WardleDABonnerKIBarkerGMYeatesGWNicholsonKSBardgettRDWatsonRNGhaniAPlant removals in perennial grassland: vegetation dynamics, decomposers, soil biodiversity and ecosystem propertiesEcol Monogr19996953556810.1890/0012-9615(1999)069[0535:PRIPGV]2.0.CO;2
– reference: WebbNRThe traditional management of European heathlandsJ Appl Ecol19983598799010.1111/j.1365-2664.1998.tb00020.x
– reference: CasamayorEOMassanaRBenllochSØvreåsLDíezBGoddardVJGasolJMJointIRodríguez-ValeraFPerdrós-AlióCChanges in archaeal, bacterial and eukaryal assemblages along a salinity gradient by comparison of genetic fingerprinting methods in a multipond solar salternEnviron Microbiol2002433834810.1046/j.1462-2920.2002.00297.x12071979
– reference: GraystonSJWangSQCampbellCDEdwardsACSelective influence of plant species on microbial diversity in the rhizosphereSoil Biol Biochem19983036937810.1016/S0038-0717(97)00124-71:CAS:528:DyaK1cXhvFWrsro%3D
– reference: Ter BraakCJFSchaffersAPCo-correspondence analysis: a new ordination method to relate two community compositionsEcology20048583484610.1890/03-0021
– reference: van der HeijdenMGABardgettRDvan StraalenNMThe unseen majority: soil microbes as drivers of plant diversity and productivity in terrestrial ecosystemsEcol Lett20081129631010.1111/j.1461-0248.2007.01139.x18047587
– reference: ReynoldsHLPackerABeverJDClayKGrassroots ecology: plant-microbe-soil interactions as drivers of plant community structure and dynamicsEcology2003842281229110.1890/02-0298
– reference: ThomasGPageAMillerRKeeneyDExchangeable cationsMethods of soil analysis. Part 2. Chemical and microbiological properties1982MadisonSSSA159165
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RelatedPersons Bickham, Jack M
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Snippet With the species composition and/or functioning of many ecosystems currently changing due to anthropogenic drivers it is important to understand and, ideally,...
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SubjectTerms Acid soils
Agronomy. Soil science and plant productions
Analysis
Animal and plant ecology
Animal, plant and microbial ecology
Anthropogenic factors
Betula
Bickham, Jack M
Biochemistry and biology
Biological and medical sciences
Biomedical and Life Sciences
Botany
Chemical composition
Chemical properties
Chemical, physicochemical, biochemical and biological properties
Co-correspondence analysis
data collection
dwarfing
Ecology
Ecosystem engineer
Ecosystems
Fatty acids
Fundamental and applied biological sciences. Psychology
fungi
General agronomy. Plant production
Geochemistry
Grassland soils
heathlands
Life Sciences
Markvetenskap
Microbial activity
Microbiology
Motion picture theaters
phospholipids
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Plant communities
Plant Physiology
Plant Sciences
Plant species
Plants
PLFA
prediction
Rare species
Regular Article
restriction fragment length polymorphism
shrublands
soil chemical properties
Soil chemistry
Soil composition
Soil ecology
Soil microbiology
Soil microorganisms
Soil properties
Soil Science
Soil Science & Conservation
Soil sciences
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Species composition
species diversity
Succession
Synecology
TRFLP
Vegetation
Woodlands
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Title Is vegetation composition or soil chemistry the best predictor of the soil microbial community
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