On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)
Identifieur interne : 001851 ( Istex/Corpus ); précédent : 001850; suivant : 001852On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)
Auteurs : Susanne JahnsSource :
- Vegetation History and Archaeobotany [ 0939-6314 ] ; 1993-12-01.
Abstract
Abstract: Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous Juglans curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the Oleo-Ceratonion alliance. Olea europaea is the only species of that alliance traceable by its pollen in the diagram, while Ceratonia pollen is totally absent.
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DOI: 10.1007/BF00198161
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title><author><name sortKey="Jahns, Susanne" sort="Jahns, Susanne" uniqKey="Jahns S" first="Susanne" last="Jahns">Susanne Jahns</name><affiliation><mods:affiliation>Institut für Palynologie und Quartärwissenschaften, Wilhelm-Weber-Strasse 2, D-37073, Göttingen, Germany</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A</idno><date when="1993" year="1993">1993</date><idno type="doi">10.1007/BF00198161</idno><idno type="url">https://api.istex.fr/document/590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001851</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001851</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title><author><name sortKey="Jahns, Susanne" sort="Jahns, Susanne" uniqKey="Jahns S" first="Susanne" last="Jahns">Susanne Jahns</name><affiliation><mods:affiliation>Institut für Palynologie und Quartärwissenschaften, Wilhelm-Weber-Strasse 2, D-37073, Göttingen, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Vegetation History and Archaeobotany</title><title level="j" type="abbrev">Veget Hist Archaebot</title><idno type="ISSN">0939-6314</idno><idno type="eISSN">1617-6278</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><date type="published" when="1993-12-01">1993-12-01</date><biblScope unit="volume">2</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="187">187</biblScope><biblScope unit="page" to="203">203</biblScope></imprint><idno type="ISSN">0939-6314</idno></series><idno type="istex">590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A</idno><idno type="DOI">10.1007/BF00198161</idno><idno type="ArticleID">BF00198161</idno><idno type="ArticleID">Art1</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0939-6314</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous Juglans curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the Oleo-Ceratonion alliance. Olea europaea is the only species of that alliance traceable by its pollen in the diagram, while Ceratonia pollen is totally absent.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Susanne Jahns</name><affiliations><json:string>Institut für Palynologie und Quartärwissenschaften, Wilhelm-Weber-Strasse 2, D-37073, Göttingen, Germany</json:string></affiliations></json:item></author><articleId><json:string>BF00198161</json:string><json:string>Art1</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous Juglans curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the Oleo-Ceratonion alliance. Olea europaea is the only species of that alliance traceable by its pollen in the diagram, while Ceratonia pollen is totally absent.</abstract><qualityIndicators><score>7.676</score><pdfVersion>1.3</pdfVersion><pdfPageSize>598 x 785 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1359</abstractCharCount><pdfWordCount>9920</pdfWordCount><pdfCharCount>59488</pdfCharCount><pdfPageCount>17</pdfPageCount><abstractWordCount>223</abstractWordCount></qualityIndicators><title>On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title><refBibs><json:item><author><json:item><name>H Allen</name></json:item></author><host><pages><last>182</last><first>173</first></pages><author></author><title>Man's Role in the Shaping of the Eastern Mediterranean Landscape</title><publicationDate>1990</publicationDate></host><title>A postglacial record from the Kopaias Basin, 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Turkey</title><publicationDate>1975</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>2</volume><pages><last>203</last><first>187</first></pages><issn><json:string>0939-6314</json:string></issn><issue>4</issue><subject><json:item><value>Geology</value></json:item><json:item><value>Anthropology/Archaeometry</value></json:item></subject><journalId><json:string>334</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1617-6278</json:string></eissn><title>Vegetation History and Archaeobotany</title><publicationDate>1993</publicationDate><copyrightDate>1993</copyrightDate></host><categories><wos><json:string>science</json:string><json:string>plant sciences</json:string><json:string>paleontology</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>1993</publicationDate><copyrightDate>1993</copyrightDate><doi><json:string>10.1007/BF00198161</json:string></doi><id>590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A</id><score>0.012019172</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</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>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><availability><p>Springer-Verlag, 1993</p></availability><date>1993-06-26</date></publicationStmt><notesStmt><note>Original Articles</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title><author xml:id="author-1"><persName><forename type="first">Susanne</forename><surname>Jahns</surname></persName><affiliation>Institut für Palynologie und Quartärwissenschaften, Wilhelm-Weber-Strasse 2, D-37073, Göttingen, Germany</affiliation></author></analytic><monogr><title level="j">Vegetation History and Archaeobotany</title><title level="j" type="abbrev">Veget Hist Archaebot</title><idno type="journal-ID">334</idno><idno type="pISSN">0939-6314</idno><idno type="eISSN">1617-6278</idno><idno type="issue-article-count">4</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><date type="published" when="1993-12-01"></date><biblScope unit="volume">2</biblScope><biblScope unit="issue">4</biblScope><biblScope unit="page" from="187">187</biblScope><biblScope unit="page" to="203">203</biblScope></imprint></monogr><idno type="istex">590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A</idno><idno type="DOI">10.1007/BF00198161</idno><idno type="ArticleID">BF00198161</idno><idno type="ArticleID">Art1</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1993-06-26</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous Juglans curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the Oleo-Ceratonion alliance. Olea europaea is the only species of that alliance traceable by its pollen in the diagram, while Ceratonia pollen is totally absent.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Geology</term></item><item><term>Anthropology/Archaeometry</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1993-06-26">Created</change><change when="1993-12-01">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/590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A/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>Berlin/Heidelberg</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>334</JournalID><JournalPrintISSN>0939-6314</JournalPrintISSN><JournalElectronicISSN>1617-6278</JournalElectronicISSN><JournalTitle>Vegetation History and Archaeobotany</JournalTitle><JournalAbbreviatedTitle>Veget Hist Archaebot</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Geosciences</JournalSubject><JournalSubject Type="Secondary">Geology</JournalSubject><JournalSubject Type="Secondary">Anthropology/Archaeometry</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>2</VolumeIDStart><VolumeIDEnd>2</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>4</IssueIDStart><IssueIDEnd>4</IssueIDEnd><IssueArticleCount>4</IssueArticleCount><IssueHistory><CoverDate><Year>1993</Year><Month>12</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1993</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art1"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00198161</ArticleID><ArticleDOI>10.1007/BF00198161</ArticleDOI><ArticleSequenceNumber>1</ArticleSequenceNumber><ArticleTitle Language="En">On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</ArticleTitle><ArticleCategory>Original Articles</ArticleCategory><ArticleFirstPage>187</ArticleFirstPage><ArticleLastPage>203</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>7</Month><Day>14</Day></RegistrationDate><Received><Year>1993</Year><Month>6</Month><Day>26</Day></Received><Accepted><Year>1993</Year><Month>9</Month><Day>8</Day></Accepted></ArticleHistory><ArticleCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1993</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>334</JournalID><VolumeIDStart>2</VolumeIDStart><VolumeIDEnd>2</VolumeIDEnd><IssueIDStart>4</IssueIDStart><IssueIDEnd>4</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Susanne</GivenName><FamilyName>Jahns</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgName>Institut für Palynologie und Quartärwissenschaften</OrgName><OrgAddress><Street>Wilhelm-Weber-Strasse 2</Street><Postcode>D-37073</Postcode><City>Göttingen</City><Country>Germany</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous <Emphasis Type="Italic">Juglans</Emphasis> curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the <Emphasis Type="Italic">Oleo-Ceratonion</Emphasis> alliance. <Emphasis Type="Italic">Olea europaea</Emphasis> is the only species of that alliance traceable by its pollen in the diagram, while <Emphasis Type="Italic">Ceratonia</Emphasis> pollen is totally absent.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>Southern Greece</Keyword><Keyword>Holocene</Keyword><Keyword>History of vegetation</Keyword><Keyword>Human impact</Keyword><Keyword><Emphasis Type="Italic">Oleo-Ceratonion</Emphasis></Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>On the Holocene vegetation history of the Argive Plain (Peloponnese, southern Greece)</title></titleInfo><name type="personal"><namePart type="given">Susanne</namePart><namePart type="family">Jahns</namePart><affiliation>Institut für Palynologie und Quartärwissenschaften, Wilhelm-Weber-Strasse 2, D-37073, Göttingen, Germany</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">Berlin/Heidelberg</placeTerm></place><dateCreated encoding="w3cdtf">1993-06-26</dateCreated><dateIssued encoding="w3cdtf">1993-12-01</dateIssued><copyrightDate encoding="w3cdtf">1993</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: Palynological investigations have been carried out on a sediment core from ancient Lake Lerna, a former fresh water lagoon in the western part of the Argive plain, Peloponnese, southern Greece. The sequence starts at 6800 B.P. (5700 cal B.C.). The lowest part of the pollen diagram shows a period of open deciduous oak woods, which may have been influenced by human impact already (Zone I). It is followed by a period of dense deciduous oak woods (Zone II), which lasted until the beginning of the Bronze Age ca. 4800 B.P. (3500 cal B.C.). Later, the diagram indicates strong human influence such as woodland clearance, the spread of maquis, phrygana and pine in Zones IIIa-IV. During the Archaic, Geometric and Classical periods after ca. 2700 B.P. (800 cal B.C.) there is evidence of a phase of extensive olive farming (Zone IIIb). In the same zone, after a period of scattered finds, there is an almost continuous Juglans curve. Zone IV is characterised by high pine values. In Zones I-II the evidence of evergreen Mediterranean plants is surprisingly small. In times with no discernible human influence (Zone II), deciduous oaks dominate, with no evidence for a climax vegetation of the Oleo-Ceratonion alliance. Olea europaea is the only species of that alliance traceable by its pollen in the diagram, while Ceratonia pollen is totally absent.</abstract><note>Original Articles</note><relatedItem type="host"><titleInfo><title>Vegetation History and Archaeobotany</title></titleInfo><titleInfo type="abbreviated"><title>Veget Hist Archaebot</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1993-12-01</dateIssued><copyrightDate encoding="w3cdtf">1993</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Geology</topic><topic>Anthropology/Archaeometry</topic></subject><identifier type="ISSN">0939-6314</identifier><identifier type="eISSN">1617-6278</identifier><identifier type="JournalID">334</identifier><identifier type="IssueArticleCount">4</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1993</date><detail type="volume"><number>2</number><caption>vol.</caption></detail><detail type="issue"><number>4</number><caption>no.</caption></detail><extent unit="pages"><start>187</start><end>203</end></extent></part><recordInfo><recordOrigin>Springer-Verlag, 1993</recordOrigin></recordInfo></relatedItem><identifier type="istex">590586A29C9AEEABD1B50D9C64CDEC6AB752CD8A</identifier><identifier type="DOI">10.1007/BF00198161</identifier><identifier type="ArticleID">BF00198161</identifier><identifier type="ArticleID">Art1</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1993</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag, 1993</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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