Soil nitrogen dynamics in a holm oak forest
Identifieur interne : 000965 ( Istex/Corpus ); précédent : 000964; suivant : 000966Soil nitrogen dynamics in a holm oak forest
Auteurs : D. Bonilla ; F. RodàSource :
- Vegetatio [ 0042-3106 ] ; 1992-06-01.
Abstract
Abstract: Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.
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DOI: 10.1007/BF00118231
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Soil nitrogen dynamics in a holm oak forest</title><author><name sortKey="Bonilla, D" sort="Bonilla, D" uniqKey="Bonilla D" first="D." last="Bonilla">D. Bonilla</name><affiliation><mods:affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</mods:affiliation></affiliation></author><author><name sortKey="Roda, F" sort="Roda, F" uniqKey="Roda F" first="F." last="Rodà">F. Rodà</name><affiliation><mods:affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0</idno><date when="1992" year="1992">1992</date><idno type="doi">10.1007/BF00118231</idno><idno type="url">https://api.istex.fr/document/4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000965</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000965</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Soil nitrogen dynamics in a holm oak forest</title><author><name sortKey="Bonilla, D" sort="Bonilla, D" uniqKey="Bonilla D" first="D." last="Bonilla">D. Bonilla</name><affiliation><mods:affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</mods:affiliation></affiliation></author><author><name sortKey="Roda, F" sort="Roda, F" uniqKey="Roda F" first="F." last="Rodà">F. Rodà</name><affiliation><mods:affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Vegetatio</title><title level="j" type="abbrev">Vegetatio</title><idno type="ISSN">0042-3106</idno><idno type="eISSN">1573-5052</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1992-06-01">1992-06-01</date><biblScope unit="volume">99-100</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="247">247</biblScope><biblScope unit="page" to="257">257</biblScope></imprint><idno type="ISSN">0042-3106</idno></series><idno type="istex">4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0</idno><idno type="DOI">10.1007/BF00118231</idno><idno type="ArticleID">BF00118231</idno><idno type="ArticleID">Art28</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0042-3106</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>D. Bonilla</name><affiliations><json:string>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</json:string></affiliations></json:item><json:item><name>F. Rodà</name><affiliations><json:string>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</json:string></affiliations></json:item></author><articleId><json:string>BF00118231</json:string><json:string>Art28</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.</abstract><qualityIndicators><score>7.784</score><pdfVersion>1.3</pdfVersion><pdfPageSize>555 x 735 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1348</abstractCharCount><pdfWordCount>5892</pdfWordCount><pdfCharCount>32510</pdfCharCount><pdfPageCount>11</pdfPageCount><abstractWordCount>232</abstractWordCount></qualityIndicators><title>Soil nitrogen dynamics in a holm oak forest</title><refBibs><json:item><author><json:item><name>J,A Adams</name></json:item></author><host><volume>18</volume><pages><last>341</last><first>339</first></pages><author></author><title>Soil Biol. 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Monogr</title><publicationDate>1982</publicationDate></host><title>A comparative analysis of potential nitrification and nitrate mobility in forest ecosystems</title><publicationDate>1982</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>99-100</volume><pages><last>257</last><first>247</first></pages><issn><json:string>0042-3106</json:string></issn><issue>1</issue><subject><json:item><value>Plant Sciences</value></json:item></subject><journalId><json:string>11258</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1573-5052</json:string></eissn><title>Vegetatio</title><publicationDate>1992</publicationDate><copyrightDate>1992</copyrightDate></host><publicationDate>1992</publicationDate><copyrightDate>1992</copyrightDate><doi><json:string>10.1007/BF00118231</json:string></doi><id>4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Soil nitrogen dynamics in a holm oak forest</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><availability><p>Kluwer Academic Publishers, 1992</p></availability><date>1992</date></publicationStmt><notesStmt><note>Part D: Nutrient Cycling and budget</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Soil nitrogen dynamics in a holm oak forest</title><author xml:id="author-1"><persName><forename type="first">D.</forename><surname>Bonilla</surname></persName><affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</affiliation></author><author xml:id="author-2"><persName><forename type="first">F.</forename><surname>Rodà</surname></persName><affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</affiliation></author></analytic><monogr><title level="j">Vegetatio</title><title level="j" type="abbrev">Vegetatio</title><idno type="journal-ID">11258</idno><idno type="pISSN">0042-3106</idno><idno type="eISSN">1573-5052</idno><idno type="issue-article-count">41</idno><idno type="volume-issue-count">0</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1992-06-01"></date><biblScope unit="volume">99-100</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="247">247</biblScope><biblScope unit="page" to="257">257</biblScope></imprint></monogr><idno type="istex">4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0</idno><idno type="DOI">10.1007/BF00118231</idno><idno type="ArticleID">BF00118231</idno><idno type="ArticleID">Art28</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1992</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Life Sciences</head><item><term>Plant Sciences</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1992-06-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-22">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-20">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0/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>11258</JournalID><JournalPrintISSN>0042-3106</JournalPrintISSN><JournalElectronicISSN>1573-5052</JournalElectronicISSN><JournalTitle>Vegetatio</JournalTitle><JournalAbbreviatedTitle>Vegetatio</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Life Sciences</JournalSubject><JournalSubject Type="Secondary">Plant Sciences</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Combined" TocLevels="0"><VolumeIDStart>99</VolumeIDStart><VolumeIDEnd>100</VolumeIDEnd><VolumeIssueCount>0</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd><IssueArticleCount>41</IssueArticleCount><IssueHistory><CoverDate><Year>1992</Year><Month>6</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1992</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art28"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00118231</ArticleID><ArticleDOI>10.1007/BF00118231</ArticleDOI><ArticleSequenceNumber>28</ArticleSequenceNumber><ArticleTitle Language="En">Soil nitrogen dynamics in a holm oak forest</ArticleTitle><ArticleCategory>Part D: Nutrient Cycling and budget</ArticleCategory><ArticleFirstPage>247</ArticleFirstPage><ArticleLastPage>257</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>5</Month><Day>17</Day></RegistrationDate><Accepted><Year>1991</Year><Month>10</Month><Day>23</Day></Accepted></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1992</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>11258</JournalID><VolumeIDStart>99</VolumeIDStart><VolumeIDEnd>100</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>D.</GivenName><FamilyName>Bonilla</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>F.</GivenName><FamilyName>Rodà</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Centre de Recerca Ecològica i Aplicacions Forestals</OrgDivision><OrgName>Universitat Autònoma de Barcelona</OrgName><OrgAddress><Postcode>08193</Postcode><City>Bellaterra</City><Country>Spain</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Soil nitrogen (N) dynamics were studied in a dense, holm oak (<Emphasis Type="Italic">Quercus ilex</Emphasis> ssp. <Emphasis Type="Italic">ilex</Emphasis>) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by <Emphasis Type="Italic">in situ</Emphasis> incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.</Para></Abstract><KeywordGroup Language="En"><Heading>Keywords</Heading><Keyword>Montseny</Keyword><Keyword>Nitrification</Keyword><Keyword>Nitrogen availability</Keyword><Keyword>Nitrogen mineralization</Keyword><Keyword><Emphasis Type="Italic">Quercus ilex</Emphasis></Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Soil nitrogen dynamics in a holm oak forest</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Soil nitrogen dynamics in a holm oak forest</title></titleInfo><name type="personal"><namePart type="given">D.</namePart><namePart type="family">Bonilla</namePart><affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">F.</namePart><namePart type="family">Rodà</namePart><affiliation>Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193, Bellaterra, Spain</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><dateIssued encoding="w3cdtf">1992-06-01</dateIssued><copyrightDate encoding="w3cdtf">1992</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: Soil nitrogen (N) dynamics were studied in a dense, holm oak (Quercus ilex ssp. ilex) stand in the Montseny mountains to determine annual and seasonal patterns of N availability and uptake in an undisturbed Mediterranean forest on acidic soil. Soil mineral N content, net N mineralization (NNM), and net nitrification (NN) were determined by monthly sampling at two soil depths followed by in situ incubation in polyethylene bags. NNM per unit of soil mass was much higher at 0–5 cm than at 5–20 cm (annual means 24 and 2.5 mg N/kg, respectively) but on an area basis NNM was similar at both depths. A total of 80 kg N/ha/yr were mineralized from the first 20 cm of soil. NN amounted to only 9% of the annual NNM (7.5 kg N/ha/yr) and it occurred only in the upper 5 cm. NNM was maximum in June and July, while the NN peaked in May. Despite favourable soil temperature and moisture, NNM was negative in autumn because of microbial immobilization. Seasonal and depth variations of NNM appeared to be controlled more by substrate quality than by organic matter quantity, temperature or moisture. NN was not limited by ammonium availability. Calculated N uptake amounted to 91 kg/ha yr, peaking in June and July. The investigated stand showed a moderately high N availability, but ammonium was the major form of mineral N supply for holm oak.</abstract><note>Part D: Nutrient Cycling and budget</note><relatedItem type="host"><titleInfo><title>Vegetatio</title></titleInfo><titleInfo type="abbreviated"><title>Vegetatio</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1992-06-01</dateIssued><copyrightDate encoding="w3cdtf">1992</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Plant Sciences</topic></subject><identifier type="ISSN">0042-3106</identifier><identifier type="eISSN">1573-5052</identifier><identifier type="JournalID">11258</identifier><identifier type="IssueArticleCount">41</identifier><identifier type="VolumeIssueCount">0</identifier><part><date>1992</date><detail type="volume"><number>99-100</number><caption>vol.</caption></detail><detail type="issue"><number>1</number><caption>no.</caption></detail><extent unit="pages"><start>247</start><end>257</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1992</recordOrigin></recordInfo></relatedItem><identifier type="istex">4EA91F55BEC2FC77A08D3F6D90B6F50E3FFF62D0</identifier><identifier type="DOI">10.1007/BF00118231</identifier><identifier type="ArticleID">BF00118231</identifier><identifier type="ArticleID">Art28</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1992</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1992</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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