Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition
Identifieur interne : 000115 ( Istex/Corpus ); précédent : 000114; suivant : 000116Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition
Auteurs : R. J. F. Bewley ; D. ParkinsonSource :
- Water, Air, and Soil Pollution [ 0049-6979 ] ; 1986-01-01.
Abstract
Abstract: Samples of organic (F/H) and mineral soil (to approximately 8 cm depth) were collected from three ‘ecologically analogous’ sites in a boreal forest at intervals of 2.8 km (site 1), 6.0 km (site 2) and 9.6 km (site 3) from a ‘sour gas’ plant emitting S02. The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO2 efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)−1, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)−1), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)−1). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)−1 were decomposed in the mineral soil of sites 2 and 3, but not at site 1. Following incubation with vanillin, fewer bacteria were isolated from both the organic and mineral soils of site 1, and a greater proportion of these were spore formers and bisulfite-tolerant isolates compared with those from sites 2 and 3.
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DOI: 10.1007/BF00464769
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ISTEX:0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</title><author><name sortKey="Bewley, R J F" sort="Bewley, R J F" uniqKey="Bewley R" first="R. J. F." last="Bewley">R. J. F. Bewley</name><affiliation><mods:affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</mods:affiliation></affiliation></author><author><name sortKey="Parkinson, D" sort="Parkinson, D" uniqKey="Parkinson D" first="D." last="Parkinson">D. Parkinson</name><affiliation><mods:affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5</idno><date when="1986" year="1986">1986</date><idno type="doi">10.1007/BF00464769</idno><idno type="url">https://api-v5.istex.fr/document/0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000115</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000115</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</title><author><name sortKey="Bewley, R J F" sort="Bewley, R J F" uniqKey="Bewley R" first="R. J. F." last="Bewley">R. J. F. Bewley</name><affiliation><mods:affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</mods:affiliation></affiliation></author><author><name sortKey="Parkinson, D" sort="Parkinson, D" uniqKey="Parkinson D" first="D." last="Parkinson">D. Parkinson</name><affiliation><mods:affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Water, Air, and Soil Pollution</title><title level="j" type="sub">An International Journal of Environmental Pollution</title><title level="j" type="abbrev">Water Air Soil Pollut</title><idno type="ISSN">0049-6979</idno><idno type="eISSN">1573-2932</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1986-01-01">1986-01-01</date><biblScope unit="volume">27</biblScope><biblScope unit="issue">1-2</biblScope><biblScope unit="page" from="57">57</biblScope><biblScope unit="page" to="68">68</biblScope></imprint><idno type="ISSN">0049-6979</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0049-6979</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Samples of organic (F/H) and mineral soil (to approximately 8 cm depth) were collected from three ‘ecologically analogous’ sites in a boreal forest at intervals of 2.8 km (site 1), 6.0 km (site 2) and 9.6 km (site 3) from a ‘sour gas’ plant emitting S02. The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO2 efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)−1, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)−1), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)−1). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)−1 were decomposed in the mineral soil of sites 2 and 3, but not at site 1. Following incubation with vanillin, fewer bacteria were isolated from both the organic and mineral soils of site 1, and a greater proportion of these were spore formers and bisulfite-tolerant isolates compared with those from sites 2 and 3.</div></front></TEI><istex><corpusName>springer</corpusName><keywords><teeft><json:string>vanillin</json:string><json:string>glucose</json:string><json:string>bewley</json:string><json:string>mineral soil</json:string><json:string>stotzky</json:string><json:string>legge</json:string><json:string>basal</json:string><json:string>organic soil</json:string><json:string>environ</json:string><json:string>july</json:string><json:string>alberta</json:string><json:string>spore</json:string><json:string>vanillin decomposition</json:string><json:string>spore formers</json:string><json:string>sept</json:string><json:string>basal respiration</json:string><json:string>acid deposition</json:string><json:string>parkinson</json:string><json:string>total bacteria</json:string><json:string>respiration</json:string><json:string>significant differences</json:string><json:string>methoxylated phenolic aldehydes</json:string><json:string>microbial</json:string><json:string>microorganism</json:string><json:string>microbial biomass</json:string><json:string>soil pollut</json:string><json:string>vanillin degradation</json:string><json:string>lower basal respiration rate</json:string><json:string>same letter</json:string><json:string>greater proportion</json:string><json:string>organic matter</json:string><json:string>fewer bacteria</json:string><json:string>litter decomposition</json:string><json:string>mineral soils</json:string><json:string>study group</json:string><json:string>matter content</json:string><json:string>soil samples</json:string><json:string>little difference</json:string><json:string>organic soil horizon</json:string><json:string>sulfur dioxide</json:string><json:string>boreal forest</json:string><json:string>vanillin substrate property</json:string><json:string>glucose decomposition</json:string><json:string>substrate addition</json:string><json:string>processing plant</json:string><json:string>organic debris</json:string><json:string>toxic effects</json:string><json:string>total amount</json:string><json:string>incubation period</json:string><json:string>microbial activity</json:string><json:string>dilution plate studies</json:string><json:string>present study</json:string><json:string>unamended soils</json:string><json:string>polluted soil</json:string><json:string>organic layer</json:string><json:string>soil organisms</json:string><json:string>soil biol biochem</json:string><json:string>field capacity</json:string><json:string>acid precipitation</json:string><json:string>terrestrial ecosystems</json:string><json:string>glucose mineralization</json:string><json:string>canadian petroleum association</json:string><json:string>preliminary experiments</json:string><json:string>ecological effects</json:string><json:string>folia microbiol</json:string><json:string>moisture content</json:string></teeft></keywords><author><json:item><name>R. 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The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO2 efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)−1, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)−1), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)−1). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)−1 were decomposed in the mineral soil of sites 2 and 3, but not at site 1. 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Reidel Publishing Company, 1986</p></availability><date>1984-09-06</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</title><author xml:id="author-0000"><persName><forename type="first">R.</forename><surname>Bewley</surname></persName><affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</affiliation></author><author xml:id="author-0001"><persName><forename type="first">D.</forename><surname>Parkinson</surname></persName><affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</affiliation></author><idno type="istex">0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5</idno><idno type="DOI">10.1007/BF00464769</idno><idno type="ArticleID">BF00464769</idno><idno type="ArticleID">Art6</idno></analytic><monogr><title level="j">Water, Air, and Soil Pollution</title><title level="j" type="sub">An International Journal of Environmental Pollution</title><title level="j" type="abbrev">Water Air Soil Pollut</title><idno type="pISSN">0049-6979</idno><idno type="eISSN">1573-2932</idno><idno type="journal-ID">true</idno><idno type="issue-article-count">21</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1986-01-01"></date><biblScope unit="volume">27</biblScope><biblScope unit="issue">1-2</biblScope><biblScope unit="page" from="57">57</biblScope><biblScope unit="page" to="68">68</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1984-09-06</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Samples of organic (F/H) and mineral soil (to approximately 8 cm depth) were collected from three ‘ecologically analogous’ sites in a boreal forest at intervals of 2.8 km (site 1), 6.0 km (site 2) and 9.6 km (site 3) from a ‘sour gas’ plant emitting S02. The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO2 efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)−1, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)−1), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)−1). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)−1 were decomposed in the mineral soil of sites 2 and 3, but not at site 1. Following incubation with vanillin, fewer bacteria were isolated from both the organic and mineral soils of site 1, and a greater proportion of these were spore formers and bisulfite-tolerant isolates compared with those from sites 2 and 3.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Environment</head><item><term>Hydrogeology</term></item><item><term>Atmospheric Protection/Air Quality Control/Air Pollution</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1984-09-06">Created</change><change when="1986-01-01">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api-v5.istex.fr/document/0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Kluwer Academic Publishers</PublisherName><PublisherLocation>Dordrecht</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>11270</JournalID><JournalPrintISSN>0049-6979</JournalPrintISSN><JournalElectronicISSN>1573-2932</JournalElectronicISSN><JournalTitle>Water, Air, and Soil Pollution</JournalTitle><JournalSubTitle>An International Journal of Environmental Pollution</JournalSubTitle><JournalAbbreviatedTitle>Water Air Soil Pollut</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Environment</JournalSubject><JournalSubject Type="Secondary">Hydrogeology</JournalSubject><JournalSubject Type="Secondary">Atmospheric Protection/Air Quality Control/Air Pollution</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>27</VolumeIDStart><VolumeIDEnd>27</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Combined"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueArticleCount>21</IssueArticleCount><IssueHistory><CoverDate><Year>1986</Year><Month>1</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>D. Reidel Publishing Company</CopyrightHolderName><CopyrightYear>1986</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art6"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00464769</ArticleID><ArticleDOI>10.1007/BF00464769</ArticleDOI><ArticleSequenceNumber>6</ArticleSequenceNumber><ArticleTitle Language="En">Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</ArticleTitle><ArticleFirstPage>57</ArticleFirstPage><ArticleLastPage>68</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>6</Month><Day>29</Day></RegistrationDate><Received><Year>1984</Year><Month>9</Month><Day>6</Day></Received><Revised><Year>1984</Year><Month>12</Month><Day>11</Day></Revised></ArticleHistory><ArticleCopyright><CopyrightHolderName>D. Reidel Publishing Company</CopyrightHolderName><CopyrightYear>1986</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>11270</JournalID><VolumeIDStart>27</VolumeIDStart><VolumeIDEnd>27</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>2</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>R.</GivenName><GivenName>J.</GivenName><GivenName>F.</GivenName><FamilyName>Bewley</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>D.</GivenName><FamilyName>Parkinson</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Department of Biology</OrgDivision><OrgName>University of Calgary</OrgName><OrgAddress><Postcode>T2N IN4</Postcode><City>Calgary</City><State>Alberta</State><Country>Canada</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Samples of organic (F/H) and mineral soil (to approximately 8 cm depth) were collected from three ‘ecologically analogous’ sites in a boreal forest at intervals of 2.8 km (site 1), 6.0 km (site 2) and 9.6 km (site 3) from a ‘sour gas’ plant emitting S0<Subscript>2</Subscript>. The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO<Subscript>2</Subscript> efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)<Superscript>−1</Superscript>, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)<Superscript>−1</Superscript>), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)<Superscript>−1</Superscript>). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)<Superscript>−1</Superscript> were decomposed in the mineral soil of sites 2 and 3, but not at site 1. Following incubation with vanillin, fewer bacteria were isolated from both the organic and mineral soils of site 1, and a greater proportion of these were spore formers and bisulfite-tolerant isolates compared with those from sites 2 and 3.</Para></Abstract><ArticleNote Type="Misc"><SimplePara>Current address: BioTechnica Ltd., 5 Chiltren Close, Cardiff, CF4 5DL, Wales.</SimplePara></ArticleNote></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Monitoring the impact of acid deposition on the soil microbiota, using glucose and vanillin decomposition</title></titleInfo><name type="personal"><namePart type="given">R.</namePart><namePart type="given">J.</namePart><namePart type="given">F.</namePart><namePart type="family">Bewley</namePart><affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">D.</namePart><namePart type="family">Parkinson</namePart><affiliation>Department of Biology, University of Calgary, T2N IN4, Calgary, Alberta, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateCreated encoding="w3cdtf">1984-09-06</dateCreated><dateIssued encoding="w3cdtf">1986-01-01</dateIssued><copyrightDate encoding="w3cdtf">1986</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: Samples of organic (F/H) and mineral soil (to approximately 8 cm depth) were collected from three ‘ecologically analogous’ sites in a boreal forest at intervals of 2.8 km (site 1), 6.0 km (site 2) and 9.6 km (site 3) from a ‘sour gas’ plant emitting S02. The organic soil of site 1 was characterized by a lower basal respiration rate, smaller microbial biomass, and a longer time to attain the peak rate of CO2 efflux following enrichment with glucose or vanillin (0.15 and 0.1 g (15 g soil)−1, respectively). No significant differences were detected between the mineral soils of the 3 sites in terms of the rate or extent of glucose decomposition (0.1 g (100 g soil)−1), but there was a significant retardation in vanillin decomposition in the mineral soil of site 1 (0.05 g (100 g soil)−1). Concentrations of 0.075 and 0.1 g vanillin (100 g soil)−1 were decomposed in the mineral soil of sites 2 and 3, but not at site 1. Following incubation with vanillin, fewer bacteria were isolated from both the organic and mineral soils of site 1, and a greater proportion of these were spore formers and bisulfite-tolerant isolates compared with those from sites 2 and 3.</abstract><relatedItem type="host"><titleInfo><title>Water, Air, and Soil Pollution</title><subTitle>An International Journal of Environmental Pollution</subTitle></titleInfo><titleInfo type="abbreviated"><title>Water Air Soil Pollut</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1986-01-01</dateIssued><copyrightDate encoding="w3cdtf">1986</copyrightDate></originInfo><subject><genre>Environment</genre><topic>Hydrogeology</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic></subject><identifier type="ISSN">0049-6979</identifier><identifier type="eISSN">1573-2932</identifier><identifier type="JournalID">11270</identifier><identifier type="IssueArticleCount">21</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1986</date><detail type="volume"><number>27</number><caption>vol.</caption></detail><detail type="issue"><number>1-2</number><caption>no.</caption></detail><extent unit="pages"><start>57</start><end>68</end></extent></part><recordInfo><recordOrigin>D. Reidel Publishing Company, 1986</recordOrigin></recordInfo></relatedItem><identifier type="istex">0EC219EDC2D6D1FA105DA4DA2D7079AF4F03A3F5</identifier><identifier type="DOI">10.1007/BF00464769</identifier><identifier type="ArticleID">BF00464769</identifier><identifier type="ArticleID">Art6</identifier><accessCondition type="use and reproduction" contentType="copyright">D. Reidel Publishing Company, 1986</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>D. Reidel Publishing Company, 1986</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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