Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation
Identifieur interne : 001739 ( Istex/Corpus ); précédent : 001738; suivant : 001740Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation
Auteurs : Jacky GirelSource :
- Environmental Management [ 0364-152X ] ; 1994-03-01.
Abstract
Abstract: In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods). Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.
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DOI: 10.1007/BF02393762
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ISTEX:3FF064EF8D878B5995B795FD126A5AD20008B274Le document en format XML
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(U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine, Université Joseph Fourier, B.P. 53X F., 38041, Grenoble cédex, France</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:3FF064EF8D878B5995B795FD126A5AD20008B274</idno><date when="1994" year="1994">1994</date><idno type="doi">10.1007/BF02393762</idno><idno type="url">https://api.istex.fr/document/3FF064EF8D878B5995B795FD126A5AD20008B274/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001739</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001739</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation</title><author><name sortKey="Girel, Jacky" sort="Girel, Jacky" uniqKey="Girel J" first="Jacky" last="Girel">Jacky Girel</name><affiliation><mods:affiliation>Ingenieur au C.N.R.S. (U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine, Université Joseph Fourier, B.P. 53X F., 38041, Grenoble cédex, France</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Environmental Management</title><title level="j" type="sub">An International Journal for Decision Makers, Scientists and Environmental Auditors</title><title level="j" type="abbrev">Environmental Management</title><idno type="ISSN">0364-152X</idno><idno type="eISSN">1432-1009</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>New York</pubPlace><date type="published" when="1994-03-01">1994-03-01</date><biblScope unit="volume">18</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="203">203</biblScope><biblScope unit="page" to="221">221</biblScope></imprint><idno type="ISSN">0364-152X</idno></series><idno type="istex">3FF064EF8D878B5995B795FD126A5AD20008B274</idno><idno type="DOI">10.1007/BF02393762</idno><idno type="ArticleID">BF02393762</idno><idno type="ArticleID">Art5</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0364-152X</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods). Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Jacky Girel</name><affiliations><json:string>Ingenieur au C.N.R.S. (U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine, Université Joseph Fourier, B.P. 53X F., 38041, Grenoble cédex, France</json:string></affiliations></json:item></author><articleId><json:string>BF02393762</json:string><json:string>Art5</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods). Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.</abstract><qualityIndicators><score>8</score><pdfVersion>1.3</pdfVersion><pdfPageSize>576 x 828 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1801</abstractCharCount><pdfWordCount>10144</pdfWordCount><pdfCharCount>62185</pdfCharCount><pdfPageCount>19</pdfPageCount><abstractWordCount>260</abstractWordCount></qualityIndicators><title>Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation</title><refBibs><json:item><author><json:item><name>M Agard</name></json:item></author><host><volume>30</volume><pages><last>771</last><first>701</first></pages><issue>1</issue><author></author><title>Revue de G(og-raphie Alpine</title><publicationDate>1942</publicationDate></host><title>L'endiguemem de l'Is/:re en Gr6sivaudan</title><publicationDate>1942</publicationDate></json:item><json:item><author><json:item><name>D Alexander</name></json:item></author><host><volume>74</volume><pages><last>550</last><first>527</first></pages><issue>4</issue><author></author><title>American Geographers</title><publicationDate>1984</publicationDate></host><title>The reclamation of Val-di-Chiana (Tuscany) AnnaL~ of the Association of</title><publicationDate>1984</publicationDate></json:item><json:item><host><pages><last>416</last><first>113</first></pages><author><json:item><name>A Allix</name></json:item></author><title>G~ographie naturelle de l'Oisans</title><publicationDate>1928</publicationDate></host></json:item><json:item><host><pages><last>159</last><first>147</first></pages><author><json:item><name>J,F Amoudruz</name></json:item></author><title>Notice sur le syst~eme de diguement du torrent de Fier, cmnmune de Th6nes, et de son application en g6n~Sral</title><publicationDate>1844</publicationDate></host></json:item><json:item><author><json:item><name>M,D Arnold</name></json:item></author><host><volume>8</volume><pages><last>106</last><first>96</first></pages><issue>2</issue><author></author><title>Environmental Conservation</title><publicationDate>1981</publicationDate></host><title>Floodplain management: A flood and land planning system</title><publicationDate>1981</publicationDate></json:item><json:item><author><json:item><name>A Baumgarten</name></json:item></author><host><volume>13</volume><pages><last>199</last><first>129</first></pages><issue>2</issue><author></author><title>Annales des Ponts et Chauss&s</title><publicationDate>1847</publicationDate></host><title>Notice sur les rivibres de Lombardie et principalement sur le P6</title><publicationDate>1847</publicationDate></json:item><json:item><author><json:item><name>A Baumgarten</name></json:item></author><host><volume>5</volume><pages><last>318</last><first>289</first></pages><author></author><title>Annales des Ponts et Chauss#es</title><publicationDate>1853</publicationDate></host><title>Cohnatages, irrigations et d~ssbchements en Italie (16re partie)</title><publicationDate>1853</publicationDate></json:item><json:item><author><json:item><name>A Baumgarten</name></json:item></author><host><volume>8</volume><pages><last>232</last><first>217</first></pages><issue>6</issue><author></author><title>Annales des Ponts et Chauss&s</title><publicationDate>1854</publicationDate></host><title>Cohnatage, irrigations et d6ss6che- ments en halie (26me partie)</title><publicationDate>1854</publicationDate></json:item><json:item><author><json:item><name>J,H Bettey</name></json:item></author><host><volume>25</volume><pages><last>43</last><first>37</first></pages><author></author><title>The Agricultural History Review</title><publicationDate>1977</publicationDate></host><title>The development of water-meadows in Dorset during the seventeeth century</title><publicationDate>1977</publicationDate></json:item><json:item><host><pages><last>360</last><first>357</first></pages><author><json:item><name>A Bossi</name></json:item></author><title>De la canalisation des rivi~res en g6n6ral et sp6cialement de la Dora Riparia Gazette de l'Association Agricole 66me ann6e</title><publicationDate>1843</publicationDate></host></json:item><json:item><author><json:item><name>A Bouchayer</name></json:item></author><host><volume>13</volume><pages><last>172287</last><first>115</first></pages><issue>123</issue><author></author><title>Le bassin du Drac. 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(U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine, Université Joseph Fourier, B.P. 53X F., 38041, Grenoble cédex, France</affiliation></author></analytic><monogr><title level="j">Environmental Management</title><title level="j" type="sub">An International Journal for Decision Makers, Scientists and Environmental Auditors</title><title level="j" type="abbrev">Environmental Management</title><idno type="journal-ID">267</idno><idno type="pISSN">0364-152X</idno><idno type="eISSN">1432-1009</idno><idno type="issue-article-count">15</idno><idno type="volume-issue-count">6</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>New York</pubPlace><date type="published" when="1994-03-01"></date><biblScope unit="volume">18</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="203">203</biblScope><biblScope unit="page" to="221">221</biblScope></imprint></monogr><idno type="istex">3FF064EF8D878B5995B795FD126A5AD20008B274</idno><idno type="DOI">10.1007/BF02393762</idno><idno type="ArticleID">BF02393762</idno><idno type="ArticleID">Art5</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1994</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods). Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Environment</head><item><term>Ecology</term></item><item><term>Atmospheric Protection/Air Quality Control/Air Pollution</term></item><item><term>Environmental Management</term></item><item><term>Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution</term></item><item><term>Forestry Management</term></item><item><term>Nature Conservation</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1994-03-01">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/3FF064EF8D878B5995B795FD126A5AD20008B274/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>Springer-Verlag</PublisherName><PublisherLocation>New York</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>267</JournalID><JournalPrintISSN>0364-152X</JournalPrintISSN><JournalElectronicISSN>1432-1009</JournalElectronicISSN><JournalTitle>Environmental Management</JournalTitle><JournalSubTitle>An International Journal for Decision Makers, Scientists and Environmental Auditors</JournalSubTitle><JournalAbbreviatedTitle>Environmental Management</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Environment</JournalSubject><JournalSubject Type="Secondary">Ecology</JournalSubject><JournalSubject Type="Secondary">Atmospheric Protection/Air Quality Control/Air Pollution</JournalSubject><JournalSubject Type="Secondary">Environmental Management</JournalSubject><JournalSubject Type="Secondary">Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution</JournalSubject><JournalSubject Type="Secondary">Forestry Management</JournalSubject><JournalSubject Type="Secondary">Nature Conservation</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo TocLevels="0" VolumeType="Regular"><VolumeIDStart>18</VolumeIDStart><VolumeIDEnd>18</VolumeIDEnd><VolumeIssueCount>6</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueArticleCount>15</IssueArticleCount><IssueHistory><CoverDate><DateString>March/April 1994</DateString><Year>1994</Year><Month>3</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Springer-Verlag New York Inc.</CopyrightHolderName><CopyrightYear>1994</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art5"><ArticleInfo ArticleType="OriginalPaper" ContainsESM="No" Language="En" NumberingStyle="Unnumbered" TocLevels="0"><ArticleID>BF02393762</ArticleID><ArticleDOI>10.1007/BF02393762</ArticleDOI><ArticleSequenceNumber>5</ArticleSequenceNumber><ArticleTitle Language="En">Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation</ArticleTitle><ArticleCategory>Profile</ArticleCategory><ArticleFirstPage>203</ArticleFirstPage><ArticleLastPage>221</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2006</Year><Month>4</Month><Day>5</Day></RegistrationDate></ArticleHistory><ArticleCopyright><CopyrightHolderName>Springer-Verlag New York Inc</CopyrightHolderName><CopyrightYear>1994</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>267</JournalID><VolumeIDStart>18</VolumeIDStart><VolumeIDEnd>18</VolumeIDEnd><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Jacky</GivenName><FamilyName>Girel</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Ingenieur au C.N.R.S. (U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine</OrgDivision><OrgName>Université Joseph Fourier</OrgName><OrgAddress><Postbox>B.P. 53X F.</Postbox><Postcode>38041</Postcode><City>Grenoble cédex</City><Country>France</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods).</Para><Para>Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>Diking</Keyword><Keyword>Disturbance</Keyword><Keyword>Engineering procedures</Keyword><Keyword>Fertilization</Keyword><Keyword>History</Keyword><Keyword>Isère River</Keyword><Keyword>Landscape heterogeneity</Keyword><Keyword>Land-use changes</Keyword><Keyword>Piedmont areas</Keyword><Keyword>Warping</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Old distribution procedure of both water and matter fluxes in floodplains of western Europe: Impact on present vegetation</title></titleInfo><name type="personal"><namePart type="given">Jacky</namePart><namePart type="family">Girel</namePart><affiliation>Ingenieur au C.N.R.S. (U.A. 01451) Equipe “Ecologie des Populations et des Communautés Alluviales dans les Vallées alpines” Centre de Biologie Alpine, Université Joseph Fourier, B.P. 53X F., 38041, Grenoble cédex, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Springer-Verlag</publisher><place><placeTerm type="text">New York</placeTerm></place><dateIssued encoding="w3cdtf">1994-03-01</dateIssued><copyrightDate encoding="w3cdtf">1994</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: In France and the United States it has been shown that strong linkages exist between vegetation and alluvial landforms within homogeneous river stretches characterized by geomorphological processes, flood duration, flood magnitude, flood frequency, and sediment size. Furthermore, perturbations induced by man (such as embankments and damming) have been shown to have an effect on both succession and plant distribution patterns. Yet, in numerous cases it is not possible to find either the communities or the plants whose presence might be predicted by reference to the river section characteristics (such as straight, braided, anastomosed, or meandering channels) or by reference to perturbation effects well known in piedmont valleys (such as variations of the water-table depth, variations of magnitude, and frequency and duration of floods). Unexpected species, new communities, and even new successional sequences are often observed. The presence of new alluvial forms explains these differences. An “artificial” substratum generated by an old human perturbation (limited in the time) has been established in the past; consequently, the natural distribution patterns of water and matter flows have been disturbed. Archive research has enabled a classification of abandoned systems that were commonly used during the 16th, 17th, 18th, and 19th centuries on European floodplains. Several case studies were chosen in order to illustrate and explain the importance of stream corridor history. The example of the Isère River valley, downstream from Albertville, is chosen to highlight the heterogeneity of the vegetation mosaïc pattern outside the dikes. The historical reconstruction explains the role of the additional disturbances that cause deviation from the system evolution patterns.</abstract><note>Profile</note><relatedItem type="host"><titleInfo><title>Environmental Management</title><subTitle>An International Journal for Decision Makers, Scientists and Environmental Auditors</subTitle></titleInfo><titleInfo type="abbreviated"><title>Environmental Management</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1994-03-01</dateIssued><copyrightDate encoding="w3cdtf">1994</copyrightDate></originInfo><subject><genre>Environment</genre><topic>Ecology</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Environmental Management</topic><topic>Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution</topic><topic>Forestry Management</topic><topic>Nature Conservation</topic></subject><identifier type="ISSN">0364-152X</identifier><identifier type="eISSN">1432-1009</identifier><identifier type="JournalID">267</identifier><identifier type="IssueArticleCount">15</identifier><identifier type="VolumeIssueCount">6</identifier><part><date>1994</date><detail type="volume"><number>18</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="pages"><start>203</start><end>221</end></extent></part><recordInfo><recordOrigin>Springer-Verlag New York Inc., 1994</recordOrigin></recordInfo></relatedItem><identifier type="istex">3FF064EF8D878B5995B795FD126A5AD20008B274</identifier><identifier type="DOI">10.1007/BF02393762</identifier><identifier type="ArticleID">BF02393762</identifier><identifier type="ArticleID">Art5</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag New York Inc, 1994</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag New York Inc, 1994</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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