Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)
Identifieur interne : 000E83 ( Istex/Corpus ); précédent : 000E82; suivant : 000E84Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)
Auteurs : D. Poth ; J. F. W. NegendankSource :
- Lecture Notes in Earth Sciences [ 0930-0317 ] ; 1993.
Abstract
Abstract: Along two cross-sections 27 sediment cores were taken from Lake Meerfelder Maar. Microstratigraphic studies have been carried out on one of these annually laminated, high resolution sediment sequences, subdivided by local lithozones. Using sediment increase rates, accumulation rates and the structure of varves it was possible to prove rapid climatic variations at the Pleistocene/Holocene transition. The boundaries of local lithozones and their corresponding biozones are calculated in varve years BP (=v.y. BP, ref. year 1950). The Younger Dryas is a tripartite sequence characterized by lithozones M3a-c. Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.
Url:
DOI: 10.1007/BFb0117598
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ISTEX:EDE333166D87C1159E0D476C536655024C1C8ECDLe document en format XML
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Negendank</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="s">Lecture Notes in Earth Sciences</title><imprint><date>1993</date></imprint><idno type="ISSN">0930-0317</idno><idno type="eISSN">1613-2580</idno><idno type="ISSN">0930-0317</idno></series><idno type="istex">EDE333166D87C1159E0D476C536655024C1C8ECD</idno><idno type="DOI">10.1007/BFb0117598</idno><idno type="ChapterID">14</idno><idno type="ChapterID">Chap14</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0930-0317</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Along two cross-sections 27 sediment cores were taken from Lake Meerfelder Maar. Microstratigraphic studies have been carried out on one of these annually laminated, high resolution sediment sequences, subdivided by local lithozones. Using sediment increase rates, accumulation rates and the structure of varves it was possible to prove rapid climatic variations at the Pleistocene/Holocene transition. The boundaries of local lithozones and their corresponding biozones are calculated in varve years BP (=v.y. BP, ref. year 1950). The Younger Dryas is a tripartite sequence characterized by lithozones M3a-c. Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>D. Poth</name><affiliations><json:string>Dept. of Geology, University of Trier, D-5500, Trier, Germany</json:string></affiliations></json:item><json:item><name>J. F. W. 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Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. 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Absolute and radiocarbon chronologies</title><publicationDate>1992</publicationDate></json:item></refBibs><genre><json:string>review-article</json:string></genre><serie><editor><json:item><name>S. Bhattacharji</name></json:item><json:item><name>G. M. Friedman</name></json:item><json:item><name>H. J. Neugebauer</name></json:item><json:item><name>A. Seilacher</name></json:item></editor><issn><json:string>0930-0317</json:string></issn><language><json:string>unknown</json:string></language><eissn><json:string>1613-2580</json:string></eissn><title>Lecture Notes in Earth Sciences</title><copyrightDate>1993</copyrightDate></serie><host><editor><json:item><name>Jorg F. W. Negendank</name></json:item><json:item><name>Bernd Zolitschka</name></json:item></editor><subject><json:item><value>Earth and Environmental Science</value></json:item><json:item><value>Geosciences</value></json:item><json:item><value>Sedimentology</value></json:item><json:item><value>Mineralogy</value></json:item></subject><isbn><json:string>978-3-540-56570-3</json:string></isbn><language><json:string>unknown</json:string></language><eissn><json:string>1613-2580</json:string></eissn><title>Paleolimnology of European Maar 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type="inbook"><analytic><title level="a" type="main" xml:lang="en">Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)</title><title level="a" type="sub" xml:lang="en">A contribution to the discussion on the Younger Dryas climatic oscillation</title><author xml:id="author-1"><persName><forename type="first">D.</forename><surname>Poth</surname></persName><affiliation>Dept. of Geology, University of Trier, D-5500, Trier, Germany</affiliation></author><author xml:id="author-2"><persName><forename type="first">J.</forename><surname>Negendank</surname></persName><affiliation>Dept. of Geology, University of Trier, D-5500, Trier, Germany</affiliation></author></analytic><monogr><title level="m">Paleolimnology of European Maar Lakes</title><idno type="pISBN">978-3-540-56570-3</idno><idno type="eISBN">978-3-540-47591-0</idno><idno type="pISSN">0930-0317</idno><idno 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type="first">S.</forename><surname>Bhattacharji</surname></persName></editor><editor><persName><forename type="first">G.</forename><forename type="first">M.</forename><surname>Friedman</surname></persName></editor><editor><persName><forename type="first">H.</forename><forename type="first">J.</forename><surname>Neugebauer</surname></persName></editor><editor><persName><forename type="first">A.</forename><surname>Seilacher</surname></persName></editor><biblScope><date>1993</date></biblScope><idno type="pISSN">0930-0317</idno><idno type="eISSN">1613-2580</idno><idno type="series-Id">772</idno></series><idno type="istex">EDE333166D87C1159E0D476C536655024C1C8ECD</idno><idno type="DOI">10.1007/BFb0117598</idno><idno type="ChapterID">14</idno><idno type="ChapterID">Chap14</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1993</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Along two cross-sections 27 sediment cores were taken from Lake Meerfelder Maar. Microstratigraphic studies have been carried out on one of these annually laminated, high resolution sediment sequences, subdivided by local lithozones. Using sediment increase rates, accumulation rates and the structure of varves it was possible to prove rapid climatic variations at the Pleistocene/Holocene transition. The boundaries of local lithozones and their corresponding biozones are calculated in varve years BP (=v.y. BP, ref. year 1950). The Younger Dryas is a tripartite sequence characterized by lithozones M3a-c. Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.</p></abstract><textClass><keywords scheme="Book-Subject-Collection"><list><label>SUCO11646</label><item><term>Earth and Environmental Science</term></item></list></keywords></textClass><textClass><keywords scheme="Book-Subject-Group"><list><label>G</label><label>G27008</label><label>G24009</label><item><term>Geosciences</term></item><item><term>Sedimentology</term></item><item><term>Mineralogy</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2007-12-27">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/EDE333166D87C1159E0D476C536655024C1C8ECD/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 Berlin Heidelberg</PublisherName><PublisherLocation>Berlin, Heidelberg</PublisherLocation></PublisherInfo><Series><SeriesInfo SeriesType="Series" TocLevels="0"><SeriesID>772</SeriesID><SeriesPrintISSN>0930-0317</SeriesPrintISSN><SeriesElectronicISSN>1613-2580</SeriesElectronicISSN><SeriesTitle Language="En">Lecture Notes in Earth Sciences</SeriesTitle><SeriesAbbreviatedTitle>Lect Notes Earth Sci</SeriesAbbreviatedTitle></SeriesInfo><SeriesHeader><EditorGroup><Editor><EditorName DisplayOrder="Western"><GivenName>S.</GivenName><FamilyName>Bhattacharji</FamilyName></EditorName></Editor><Editor><EditorName DisplayOrder="Western"><GivenName>G.</GivenName><GivenName>M.</GivenName><FamilyName>Friedman</FamilyName></EditorName></Editor><Editor><EditorName DisplayOrder="Western"><GivenName>H.</GivenName><GivenName>J.</GivenName><FamilyName>Neugebauer</FamilyName></EditorName></Editor><Editor><EditorName DisplayOrder="Western"><GivenName>A.</GivenName><FamilyName>Seilacher</FamilyName></EditorName></Editor></EditorGroup></SeriesHeader><Book Language="En"><BookInfo BookProductType="Monograph" ContainsESM="No" Language="En" MediaType="Book" NumberingStyle="Unnumbered" TocLevels="0"><BookID>3-540-56570-1</BookID><BookTitle>Paleolimnology of European Maar Lakes</BookTitle><BookVolumeNumber>49</BookVolumeNumber><BookSequenceNumber>49</BookSequenceNumber><BookDOI>10.1007/BFb0117584</BookDOI><BookTitleID>30950</BookTitleID><BookPrintISBN>978-3-540-56570-3</BookPrintISBN><BookElectronicISBN>978-3-540-47591-0</BookElectronicISBN><BookChapterCount>35</BookChapterCount><BookCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1993</CopyrightYear></BookCopyright><BookSubjectGroup><BookSubject Code="G" Type="Primary">Geosciences</BookSubject><BookSubject Code="G27008" Priority="1" Type="Secondary">Sedimentology</BookSubject><BookSubject Code="G24009" Priority="2" Type="Secondary">Mineralogy</BookSubject><SubjectCollection Code="SUCO11646">Earth and Environmental Science</SubjectCollection></BookSubjectGroup></BookInfo><BookHeader><EditorGroup><Editor><EditorName DisplayOrder="Western"><GivenName>Jorg</GivenName><GivenName>F.</GivenName><GivenName>W.</GivenName><FamilyName>Negendank</FamilyName></EditorName></Editor><Editor><EditorName DisplayOrder="Western"><GivenName>Bernd</GivenName><FamilyName>Zolitschka</FamilyName></EditorName></Editor></EditorGroup></BookHeader><Chapter ID="Chap14" Language="En"><ChapterInfo ChapterType="ReviewPaper" ContainsESM="No" NumberingStyle="Unnumbered" TocLevels="0"><ChapterID>14</ChapterID><ChapterDOI>10.1007/BFb0117598</ChapterDOI><ChapterSequenceNumber>14</ChapterSequenceNumber><ChapterTitle Language="En">Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)</ChapterTitle><ChapterSubTitle Language="En">A contribution to the discussion on the Younger Dryas climatic oscillation</ChapterSubTitle><ChapterCategory>Sedimentology</ChapterCategory><ChapterFirstPage>209</ChapterFirstPage><ChapterLastPage>222</ChapterLastPage><ChapterCopyright><CopyrightHolderName>Springer-Verlag</CopyrightHolderName><CopyrightYear>1993</CopyrightYear></ChapterCopyright><ChapterHistory><OnlineDate><Year>2007</Year><Month>12</Month><Day>27</Day></OnlineDate></ChapterHistory><ChapterGrants 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></ChapterGrants><ChapterContext><SeriesID>772</SeriesID><BookID>3-540-56570-1</BookID><BookTitle>Paleolimnology of European Maar Lakes</BookTitle></ChapterContext></ChapterInfo><ChapterHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>D.</GivenName><FamilyName>Poth</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>J.</GivenName><GivenName>F.</GivenName><GivenName>W.</GivenName><FamilyName>Negendank</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Dept. of Geology</OrgDivision><OrgName>University of Trier</OrgName><OrgAddress><Postcode>D-5500</Postcode><City>Trier</City><Country>Germany</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Along two cross-sections 27 sediment cores were taken from Lake Meerfelder Maar.</Para><Para>Microstratigraphic studies have been carried out on one of these annually laminated, high resolution sediment sequences, subdivided by local lithozones. Using sediment increase rates, accumulation rates and the structure of varves it was possible to prove rapid climatic variations at the Pleistocene/Holocene transition.</Para><Para>The boundaries of local lithozones and their corresponding biozones are calculated in varve years BP (=v.y. BP, ref. year 1950).</Para><Para>The Younger Dryas is a tripartite sequence characterized by lithozones M3a-c. Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.</Para></Abstract></ChapterHeader><NoBody></NoBody></Chapter></Book></Series></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)</title><subTitle>A contribution to the discussion on the Younger Dryas climatic oscillation</subTitle></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Paleoclimate reconstruction at the Pleistocene/Holocene transition—A varve dated microstratigraphic record from Lake Meerfelder Maar (Westeifel, Germany)</title><subTitle>A contribution to the discussion on the Younger Dryas climatic oscillation</subTitle></titleInfo><name type="personal"><namePart type="given">D.</namePart><namePart type="family">Poth</namePart><affiliation>Dept. of Geology, University of Trier, D-5500, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">J.</namePart><namePart type="given">F.</namePart><namePart type="given">W.</namePart><namePart type="family">Negendank</namePart><affiliation>Dept. of Geology, University of Trier, D-5500, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="review-article" displayLabel="ReviewPaper"></genre><originInfo><publisher>Springer Berlin Heidelberg</publisher><place><placeTerm type="text">Berlin, Heidelberg</placeTerm></place><dateIssued encoding="w3cdtf">2007-12-27</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: Along two cross-sections 27 sediment cores were taken from Lake Meerfelder Maar. Microstratigraphic studies have been carried out on one of these annually laminated, high resolution sediment sequences, subdivided by local lithozones. Using sediment increase rates, accumulation rates and the structure of varves it was possible to prove rapid climatic variations at the Pleistocene/Holocene transition. The boundaries of local lithozones and their corresponding biozones are calculated in varve years BP (=v.y. BP, ref. year 1950). The Younger Dryas is a tripartite sequence characterized by lithozones M3a-c. Lithozone M2 characterizes organic deposits of the Late Glacial with Laacher See Tephra (LST) close to its top. The base of Younger Dryas (M2/M3a) is dated to 11.070 v. y. BP. After this period of rapid cooling a dramatic sedimentary change to clay-silt-laminations occurs at 10.850 v. y. BP characterizing the main Younger Dryas climatic deterioration (M3b). From now on soil erosion dominates due to open tundra-like vegetation of the periglacial environment, causing clastic deposition rich in sand and silt. After around 140 years organic sedimentation reappears abruptly and allochthonous minerogenic detritus recedes. This succession characterizes the transition to early Holocene warming and regeneration of soils and vegetation. The top of Younger Dryas (M3c/M4) is dated to 10.610 v.y. BP when first distinct layers of planktonic diatoms occur. Therefore the Pleistocene/Holocene boundary is fixed lithologically by varve counting, beginning at the isochrone of LST (11.323+/-224 v.y. BP), to 10.610 v.y. BP.</abstract><relatedItem type="host"><titleInfo><title>Paleolimnology of European Maar Lakes</title></titleInfo><name type="personal"><namePart type="given">Jorg</namePart><namePart type="given">F.</namePart><namePart type="given">W.</namePart><namePart type="family">Negendank</namePart><role><roleTerm type="text">editor</roleTerm></role></name><name type="personal"><namePart type="given">Bernd</namePart><namePart type="family">Zolitschka</namePart><role><roleTerm type="text">editor</roleTerm></role></name><genre type="book-series" displayLabel="Monograph"></genre><originInfo><copyrightDate encoding="w3cdtf">1993</copyrightDate><issuance>monographic</issuance></originInfo><subject><genre>Book-Subject-Collection</genre><topic authority="SpringerSubjectCodes" authorityURI="SUCO11646">Earth and Environmental Science</topic></subject><subject><genre>Book-Subject-Group</genre><topic authority="SpringerSubjectCodes" authorityURI="G">Geosciences</topic><topic authority="SpringerSubjectCodes" authorityURI="G27008">Sedimentology</topic><topic authority="SpringerSubjectCodes" authorityURI="G24009">Mineralogy</topic></subject><identifier type="DOI">10.1007/BFb0117584</identifier><identifier type="ISBN">978-3-540-56570-3</identifier><identifier type="eISBN">978-3-540-47591-0</identifier><identifier type="ISSN">0930-0317</identifier><identifier type="eISSN">1613-2580</identifier><identifier type="BookTitleID">30950</identifier><identifier type="BookID">3-540-56570-1</identifier><identifier type="BookChapterCount">35</identifier><identifier type="BookVolumeNumber">49</identifier><identifier type="BookSequenceNumber">49</identifier><part><date>1993</date><detail type="volume"><number>49</number><caption>vol.</caption></detail><extent unit="pages"><start>209</start><end>222</end></extent></part><recordInfo><recordOrigin>Springer-Verlag, 1993</recordOrigin></recordInfo></relatedItem><relatedItem type="series"><titleInfo><title>Lecture Notes in Earth Sciences</title></titleInfo><name type="personal"><namePart type="given">S.</namePart><namePart type="family">Bhattacharji</namePart><role><roleTerm type="text">editor</roleTerm></role></name><name type="personal"><namePart type="given">G.</namePart><namePart type="given">M.</namePart><namePart type="family">Friedman</namePart><role><roleTerm type="text">editor</roleTerm></role></name><name type="personal"><namePart type="given">H.</namePart><namePart type="given">J.</namePart><namePart type="family">Neugebauer</namePart><role><roleTerm type="text">editor</roleTerm></role></name><name type="personal"><namePart type="given">A.</namePart><namePart type="family">Seilacher</namePart><role><roleTerm type="text">editor</roleTerm></role></name><originInfo><copyrightDate encoding="w3cdtf">1993</copyrightDate><issuance>serial</issuance></originInfo><identifier type="ISSN">0930-0317</identifier><identifier type="eISSN">1613-2580</identifier><identifier type="SeriesID">772</identifier><recordInfo><recordOrigin>Springer-Verlag, 1993</recordOrigin></recordInfo></relatedItem><identifier type="istex">EDE333166D87C1159E0D476C536655024C1C8ECD</identifier><identifier type="DOI">10.1007/BFb0117598</identifier><identifier type="ChapterID">14</identifier><identifier type="ChapterID">Chap14</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1993</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag, 1993</recordOrigin></recordInfo></mods></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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