Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada
Identifieur interne : 001681 ( Istex/Corpus ); précédent : 001680; suivant : 001682Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada
Auteurs : Bern ZolitschkaSource :
- Journal of Paleolimnology [ 0921-2728 ] ; 1996-09-01.
Abstract
Abstract: A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on 210Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to < 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.
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DOI: 10.1007/BF00176934
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title><author><name sortKey="Zolitschka, Bern" sort="Zolitschka, Bern" uniqKey="Zolitschka B" first="Bern" last="Zolitschka">Bern Zolitschka</name><affiliation><mods:affiliation>Fachbereich VI/Geologie, Universität Trier, D-54286, Thier, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>GeoforschungsZentrum Potsdam, Telegrafenberg A26, D-14473, Potsdam, Germany</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:26F38AB53EE926C194F7738A0F7511DD22190775</idno><date when="1996" year="1996">1996</date><idno type="doi">10.1007/BF00176934</idno><idno type="url">https://api.istex.fr/document/26F38AB53EE926C194F7738A0F7511DD22190775/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001681</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001681</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title><author><name sortKey="Zolitschka, Bern" sort="Zolitschka, Bern" uniqKey="Zolitschka B" first="Bern" last="Zolitschka">Bern Zolitschka</name><affiliation><mods:affiliation>Fachbereich VI/Geologie, Universität Trier, D-54286, Thier, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>GeoforschungsZentrum Potsdam, Telegrafenberg A26, D-14473, Potsdam, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="ISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><imprint><publisher>Kluwer Academic Publishers; http://www.wkap.nl/</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1996-09-01">1996-09-01</date><biblScope unit="volume">16</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="169">169</biblScope><biblScope unit="page" to="186">186</biblScope></imprint><idno type="ISSN">0921-2728</idno></series><idno type="istex">26F38AB53EE926C194F7738A0F7511DD22190775</idno><idno type="DOI">10.1007/BF00176934</idno><idno type="ArticleID">BF00176934</idno><idno type="ArticleID">Art5</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0921-2728</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on 210Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to < 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Bern Zolitschka</name><affiliations><json:string>Fachbereich VI/Geologie, Universität Trier, D-54286, Thier, Germany</json:string><json:string>GeoforschungsZentrum Potsdam, Telegrafenberg A26, D-14473, Potsdam, Germany</json:string></affiliations></json:item></author><articleId><json:string>BF00176934</json:string><json:string>Art5</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on 210Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to > 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.</abstract><qualityIndicators><score>7.148</score><pdfVersion>1.3</pdfVersion><pdfPageSize>547.28 x 738 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1257</abstractCharCount><pdfWordCount>11013</pdfWordCount><pdfCharCount>57335</pdfCharCount><pdfPageCount>18</pdfPageCount><abstractWordCount>179</abstractWordCount></qualityIndicators><title>Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title><refBibs><json:item><author><json:item><name>S,E Allen</name></json:item><json:item><name>H,M Grimshaw</name></json:item><json:item><name>J,A Parkinson</name></json:item><json:item><name>&,C Quarmby</name></json:item></author><host><author></author><title>Chemical analysis of ecological materials. 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Sedimentology, paiaeomagnetism , image analysis</title><publicationDate>1992</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>16</volume><pages><last>186</last><first>169</first></pages><issn><json:string>0921-2728</json:string></issn><issue>2</issue><subject><json:item><value>Geochemistry</value></json:item><json:item><value>Hydrogeology</value></json:item><json:item><value>Meteorology/Climatology</value></json:item><json:item><value>Sedimentology</value></json:item><json:item><value>Hydrobiology</value></json:item></subject><journalId><json:string>10933</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1573-0417</json:string></eissn><title>Journal of Paleolimnology</title><publicationDate>1996</publicationDate><copyrightDate>1996</copyrightDate></host><categories><wos><json:string>science</json:string><json:string>limnology</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>environmental sciences</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>paleontology</json:string></scienceMetrix></categories><publicationDate>1996</publicationDate><copyrightDate>1996</copyrightDate><doi><json:string>10.1007/BF00176934</json:string></doi><id>26F38AB53EE926C194F7738A0F7511DD22190775</id><score>0.39408895</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/26F38AB53EE926C194F7738A0F7511DD22190775/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/26F38AB53EE926C194F7738A0F7511DD22190775/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/26F38AB53EE926C194F7738A0F7511DD22190775/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</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; http://www.wkap.nl/</publisher><pubPlace>Dordrecht</pubPlace><availability><p>Kluwer Academic Publishers, 1996</p></availability><date>1994-11-07</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title><author xml:id="author-1"><persName><forename type="first">Bern</forename><surname>Zolitschka</surname></persName><affiliation>Fachbereich VI/Geologie, Universität Trier, D-54286, Thier, Germany</affiliation><affiliation>GeoforschungsZentrum Potsdam, Telegrafenberg A26, D-14473, Potsdam, Germany</affiliation></author></analytic><monogr><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="journal-ID">10933</idno><idno type="pISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><idno type="issue-article-count">10</idno><idno type="volume-issue-count">3</idno><imprint><publisher>Kluwer Academic Publishers; http://www.wkap.nl/</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1996-09-01"></date><biblScope unit="volume">16</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="169">169</biblScope><biblScope unit="page" to="186">186</biblScope></imprint></monogr><idno type="istex">26F38AB53EE926C194F7738A0F7511DD22190775</idno><idno type="DOI">10.1007/BF00176934</idno><idno type="ArticleID">BF00176934</idno><idno type="ArticleID">Art5</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1994-11-07</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on 210Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to < 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Life Sciences</head><item><term>Geochemistry</term></item><item><term>Hydrogeology</term></item><item><term>Meteorology/Climatology</term></item><item><term>Sedimentology</term></item><item><term>Hydrobiology</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1994-11-07">Created</change><change when="1996-09-01">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/26F38AB53EE926C194F7738A0F7511DD22190775/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><PublisherURL>http://www.wkap.nl/</PublisherURL></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>10933</JournalID><JournalPrintISSN>0921-2728</JournalPrintISSN><JournalElectronicISSN>1573-0417</JournalElectronicISSN><JournalTitle>Journal of Paleolimnology</JournalTitle><JournalAbbreviatedTitle>J Paleolimnol</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Life Sciences</JournalSubject><JournalSubject Type="Secondary">Geochemistry</JournalSubject><JournalSubject Type="Secondary">Hydrogeology</JournalSubject><JournalSubject Type="Secondary">Meteorology/Climatology</JournalSubject><JournalSubject Type="Secondary">Sedimentology</JournalSubject><JournalSubject Type="Secondary">Hydrobiology</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>16</VolumeIDStart><VolumeIDEnd>16</VolumeIDEnd><VolumeIssueCount>3</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueArticleCount>10</IssueArticleCount><IssueHistory><CoverDate><Year>1996</Year><Month>9</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1996</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art5"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00176934</ArticleID><ArticleDOI>10.1007/BF00176934</ArticleDOI><ArticleSequenceNumber>5</ArticleSequenceNumber><ArticleTitle Language="En">Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</ArticleTitle><ArticleFirstPage>169</ArticleFirstPage><ArticleLastPage>186</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>7</Month><Day>5</Day></RegistrationDate><Received><Year>1994</Year><Month>11</Month><Day>7</Day></Received><Accepted><Year>1995</Year><Month>7</Month><Day>20</Day></Accepted></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1996</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>10933</JournalID><VolumeIDStart>16</VolumeIDStart><VolumeIDEnd>16</VolumeIDEnd><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueTitle Language="En">Taconite Inlet Lakes Project</IssueTitle></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1 Aff2"><AuthorName DisplayOrder="Western"><GivenName>Bern</GivenName><FamilyName>Zolitschka</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Fachbereich VI/Geologie</OrgDivision><OrgName>Universität Trier</OrgName><OrgAddress><Postcode>D-54286</Postcode><City>Thier</City><Country>Germany</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgName>GeoforschungsZentrum Potsdam</OrgName><OrgAddress><Street>Telegrafenberg A26</Street><Postcode>D-14473</Postcode><City>Potsdam</City><Country>Germany</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on <Superscript>210</Superscript>Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to < 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>varves</Keyword><Keyword>turbidities</Keyword><Keyword>sedimentology</Keyword><Keyword>palaeoclimate</Keyword><Keyword>high arctic</Keyword><Keyword>Ellesmere Island</Keyword></KeywordGroup><ArticleNote Type="Misc"><SimplePara>This is the fifth in a series of papers published in this issue on the Taconite Inlet Lakes Project. These papers were collected by Dr R. S. Bradley.</SimplePara></ArticleNote></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Recent sedimentation in a high arctic lake, northern Ellesmere Island, Canada</title></titleInfo><name type="personal"><namePart type="given">Bern</namePart><namePart type="family">Zolitschka</namePart><affiliation>Fachbereich VI/Geologie, Universität Trier, D-54286, Thier, Germany</affiliation><affiliation>GeoforschungsZentrum Potsdam, Telegrafenberg A26, D-14473, Potsdam, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Kluwer Academic Publishers; http://www.wkap.nl/</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateCreated encoding="w3cdtf">1994-11-07</dateCreated><dateIssued encoding="w3cdtf">1996-09-01</dateIssued><copyrightDate encoding="w3cdtf">1996</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: A multiple core study was conducted on laminated minerogenic sediments from Lake C2, Northern Ellesmere Island, Canadian High Arctic. Lateral persistence, distal thinning, variation in grain size of these laminations as well as present-day processes of highly seasonal sediment transfer into the lake basin suggest that clastic varves have been formed. Sedimentation rates based on 210Pb dating agree well with sedimentation rates based on lamination counts giving further evidence that laminations are annual. Errors in varve counting were reduced from 12% to < 2% using the multi-core approach of cross-correlating all records. Varved sediments are occasionally interrupted by thick coarse-grained layers, which are interpreted as deposits of turbidity currents and may be related to extremely high discharge events and slope failures of the delta front. Micro-laminated sediments spanning the last two centuries were studied in detail. Suspension settling is the dominant process of deposition depending upon stream discharge which is controlled by nival melt and summer temperatures. Application of varve chronology thus allows to use lamination thickness measurements as source of high resolution proxy data for palaeoclimatic reconstruction.</abstract><relatedItem type="host"><titleInfo><title>Journal of Paleolimnology</title></titleInfo><titleInfo type="abbreviated"><title>J Paleolimnol</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1996-09-01</dateIssued><copyrightDate encoding="w3cdtf">1996</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Geochemistry</topic><topic>Hydrogeology</topic><topic>Meteorology/Climatology</topic><topic>Sedimentology</topic><topic>Hydrobiology</topic></subject><identifier type="ISSN">0921-2728</identifier><identifier type="eISSN">1573-0417</identifier><identifier type="JournalID">10933</identifier><identifier type="IssueArticleCount">10</identifier><identifier type="VolumeIssueCount">3</identifier><part><date>1996</date><detail type="issue"><title>Taconite Inlet Lakes Project</title></detail><detail type="volume"><number>16</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="pages"><start>169</start><end>186</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1996</recordOrigin></recordInfo></relatedItem><identifier type="istex">26F38AB53EE926C194F7738A0F7511DD22190775</identifier><identifier type="DOI">10.1007/BF00176934</identifier><identifier type="ArticleID">BF00176934</identifier><identifier type="ArticleID">Art5</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1996</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1996</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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