Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator
Identifieur interne : 000939 ( Istex/Corpus ); précédent : 000938; suivant : 000940Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator
Auteurs : B. Rein ; J. F. W. NegendankSource :
- Lecture Notes in Earth Sciences [ 0930-0317 ] ; 1993.
Abstract
Abstract: Investigations on orgnaic carbon in sediments of Maar lakes reveal a relationship to paleotemperatures as reconstructed from Camp Century ice cores. Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.
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DOI: 10.1007/BFb0117595
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Rein</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation></affiliation></author><author><name sortKey="Negendank, J F W" sort="Negendank, J F W" uniqKey="Negendank J" first="J. F. W." last="Negendank">J. F. W. 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Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>B. Rein</name><affiliations><json:string>Dept. of Geology, University of Trier, D-5500, Trier</json:string></affiliations></json:item><json:item><name>J. F. W. 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Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.</abstract><qualityIndicators><score>3.781</score><pdfVersion>1.3</pdfVersion><pdfPageSize>497 x 720 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>832</abstractCharCount><pdfWordCount>2401</pdfWordCount><pdfCharCount>14949</pdfCharCount><pdfPageCount>9</pdfPageCount><abstractWordCount>115</abstractWordCount></qualityIndicators><title>Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator</title><chapterId><json:string>11</json:string><json:string>Chap11</json:string></chapterId><refBibs><json:item><host><pages><first>117</first></pages><author><json:item><name>A Brauer</name></json:item></author><title>Versuch einer Erfassung alter Seespiegelst~de an ausgesuchten Eifelmaaren und mikrostratigraphische Untersuchungen an Sedimenten des Weinfelder Maares</title><publicationDate>1988</publicationDate></host></json:item><json:item><host><pages><last>56</last><first>37</first></pages><author><json:item><name>W Daansgaard</name></json:item></author><title>Climatic record revealed by the Camp Century ice core. -The late cenozoic glacial ages</title><publicationDate>1971</publicationDate></host></json:item><json:item><author><json:item><name>Chr,V Haaren</name></json:item></author><host><pages><first>548</first></pages><author></author><title>Eifelmaare. LandschaftsSkologisch -historische Betrachtung und Naturschutzplanung</title><publicationDate>1988</publicationDate></host><publicationDate>1988</publicationDate></json:item><json:item><author><json:item><name>B Haverkamp</name></json:item></author><host><author></author><title>Diss. Univ. Mtinster</title><publicationDate>1991</publicationDate></host><title>Pal~omagnetische Untersuchungen an Seesedimenten aus den Eifelmaaren</title><publicationDate>1991</publicationDate></json:item><json:item><host><pages><first>107</first></pages><author><json:item><name>T Heinz</name></json:item></author><title>Pal~tolimnologische und spektralanalytische Untersuchungen an jahreszeitlich geschichteten Sedimenten des Schalkenmehrener Maares</title><publicationDate>1991</publicationDate></host></json:item><json:item><host><author><json:item><name>W Hofmann</name></json:item></author><title>Late-/ Postglacial planktonic and littoral cladoceran assemblages from two eutrophic maar lakes. -Abstract vol. Syrup. Paleolimnology of Maar Lakes</title><publicationDate>1991-03-21</publicationDate></host></json:item><json:item><host><pages><first>109</first></pages><author><json:item><name>B Rein</name></json:item></author><title>Versuch einer Rekonstruktion des Paleoenvironments anhand hochzeitauflrsender geochemischer und sedimentologischer Untersuchungen an sp~t-und postglazialen Sedimenten des Schalkenmehrener Maarsees (Westeifel/ Deutschland). - Diplomarbeit Univ</title><publicationDate>1991</publicationDate></host></json:item><json:item><author><json:item><name>H Straka</name></json:item></author><host><volume>3</volume><pages><first>163</first></pages><author></author><title>Beih</title><publicationDate>1975</publicationDate></host><title>Die sp~tquartitre Vegetationsgeschichte der Vulkaneifel. -Beitrag zur Landespflege in Rheinl.-Pfalz</title><publicationDate>1975</publicationDate></json:item><json:item><host><pages><last>409</last><first>373</first></pages><author><json:item><name>H Usinger</name></json:item></author><title>Pollenanalytische Untersuchungen an sp~tglazialen und pr~borealen Sedimenten aus dem Meerfelder M~:ar (Eifel), Flora</title><publicationDate>1982</publicationDate></host></json:item><json:item><author><json:item><name>B Zolitschka</name></json:item></author><host><pages><first>241</first></pages><author></author><title>Eifelmaare. -Diss. Univ. Trier</title><publicationDate>1990</publicationDate></host><title>Sp~tquart~e jahreszeiflich geschichtete Seesedimente ausgew~ihlter</title><publicationDate>1990</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. 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Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. 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DisplayOrder="Western"><GivenName>B.</GivenName><FamilyName>Rein</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></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Investigations on orgnaic carbon in sediments of Maar lakes reveal a relationship to paleotemperatures as reconstructed from Camp Century ice cores. Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.</Para></Abstract></ChapterHeader><NoBody></NoBody></Chapter></Book></Series></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator</title></titleInfo><name type="personal"><namePart type="given">B.</namePart><namePart type="family">Rein</namePart><affiliation>Dept. of Geology, University of Trier, D-5500, Trier</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</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: Investigations on orgnaic carbon in sediments of Maar lakes reveal a relationship to paleotemperatures as reconstructed from Camp Century ice cores. Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.</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>163</start><end>171</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">8A35E4C65C925D6FEC54620DC764D2AF0357302C</identifier><identifier type="DOI">10.1007/BFb0117595</identifier><identifier type="ChapterID">11</identifier><identifier type="ChapterID">Chap11</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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