Temperature oscillations over the last 10,000 years in western Europe estimated from terrestrial mollusc assemblages
Identifieur interne : 002F41 ( Istex/Corpus ); précédent : 002F40; suivant : 002F42Temperature oscillations over the last 10,000 years in western Europe estimated from terrestrial mollusc assemblages
Auteurs : Denis-Didier Rousseau ; Nicole Limondin ; Frédéric Magnin ; Jean-Jacques PuissegurSource :
- Boreas [ 0300-9483 ] ; 1994-03.
English descriptors
- KwdEn :
- Assemblage, Atlantic chronozone, Atlantic ocean, August, August temperatures, Boreas, British isles, Climatic, Correspondence analysis, Dryas, February, Fluctuation, Fossil, Fossil assemblages, Frederic magnin, General variability, Glacier, Hiatus, Holocene, Lake sediments, Last deglaciation, Last years, Lehman keigwin, Modern assemblages, Mollusc, Mollusc assemblages, Mollusc species, Molluscan, Molluscan assemblages, Multiple correlation coefficient, Nesje kvamme, Nicole limondin, Organic matter, Other proxy data, Past years, Pollen data, Quantitative reconstructions, Quaternary, Quaternary research, Quaternary science reviews, Rapid warming, Reconstructed values, Snail, Snail assemblages, Standard errors, Temperature boreas, Temperature estimates, Temperature oscillations, Terrestrial deposits, Terrestrial molluscs, Total number, Total variance, Transfer functions, Variance, Vertigo, Western europe, Western norway, Younger dryas, Younger dryas event.
- Teeft :
- Assemblage, Atlantic chronozone, Atlantic ocean, August, August temperatures, Boreas, British isles, Climatic, Correspondence analysis, Dryas, February, Fluctuation, Fossil, Fossil assemblages, Frederic magnin, General variability, Glacier, Hiatus, Holocene, Lake sediments, Last deglaciation, Last years, Lehman keigwin, Modern assemblages, Mollusc, Mollusc assemblages, Mollusc species, Molluscan, Molluscan assemblages, Multiple correlation coefficient, Nesje kvamme, Nicole limondin, Organic matter, Other proxy data, Past years, Pollen data, Quantitative reconstructions, Quaternary, Quaternary research, Quaternary science reviews, Rapid warming, Reconstructed values, Snail, Snail assemblages, Standard errors, Temperature boreas, Temperature estimates, Temperature oscillations, Terrestrial deposits, Terrestrial molluscs, Total number, Total variance, Transfer functions, Variance, Vertigo, Western europe, Western norway, Younger dryas, Younger dryas event.
Abstract
Snail assemblages are used to estimate February and August temperatures during the past 10,000 years in western Europe. We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. This study also confirms that terrestrial molluscs can provide reliable climatic data in conjunction with other proxy data.
Url:
DOI: 10.1111/j.1502-3885.1994.tb00587.x
Links to Exploration step
ISTEX:6067932DD523D7E40699A0810414BE39D40725C4Le document en format XML
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We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. 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J. Birks</json:string><json:string>Denis-Didier Rousseau</json:string><json:string>Joyce Gavin</json:string><json:string>Nicole Limondin</json:string><json:string>Observatory</json:string><json:string>August</json:string><json:string>Lauria</json:string><json:string>Norway</json:string></persName><placeName><json:string>Montpellier</json:string><json:string>Norway</json:string><json:string>Europe</json:string><json:string>Aix-en-Provence</json:string><json:string>France</json:string><json:string>Marseille</json:string></placeName><ref_url></ref_url><ref_bibl><json:string>Nesje & Kvamme 1991</json:string><json:string>Rousseau 1987, 1990</json:string><json:string>Duplessy et al. 1992</json:string><json:string>Rousseau 1987</json:string><json:string>Benzecri & Benzecri 1980</json:string><json:string>Lehman & Keigwin 1992</json:string><json:string>Magnin 1992</json:string><json:string>Denis-Didier Rousseau et al.</json:string><json:string>Johnsen et al. 1992</json:string><json:string>Rousseau et al.</json:string><json:string>Bond et al.</json:string><json:string>Rousseau 1991</json:string><json:string>Overpeck et al. 1985</json:string><json:string>Oeschger & Arquit 1991</json:string><json:string>Rousseau et al. 1993</json:string><json:string>Wernstedt 1972</json:string><json:string>revised 91h July, 1993</json:string><json:string>Nesje et al. 1991</json:string><json:string>Scherrer 1984</json:string><json:string>Rousseau 1990, 1991</json:string><json:string>Mangerud et al. 1974</json:string></ref_bibl><bibl></bibl></unitex></namedEntities><ark><json:string>ark:/67375/WNG-JHKG990K-B</json:string></ark><categories><wos><json:string>1 - 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We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. This study also confirms that terrestrial molluscs can provide reliable climatic data in conjunction with other proxy data.</p></abstract><textClass><keywords rend="tocHeading1"><term>Original Article</term></keywords></textClass><langUsage><language ident="en"></language></langUsage></profileDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/6067932DD523D7E40699A0810414BE39D40725C4/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>Blackwell Publishing Ltd</publisherName><publisherLoc>Oxford, UK</publisherLoc></publisherInfo><doi origin="wiley" registered="yes">10.1111/(ISSN)1502-3885</doi><issn type="print">0300-9483</issn><issn type="electronic">1502-3885</issn><idGroup><id type="product" value="BOR"></id><id type="publisherDivision" value="ST"></id></idGroup><titleGroup><title type="main" sort="BOREAS">Boreas</title></titleGroup></publicationMeta><publicationMeta level="part" position="03001"><doi origin="wiley">10.1111/bor.1994.23.issue-1</doi><numberingGroup><numbering type="journalVolume" number="23">23</numbering><numbering type="journalIssue" number="1">1</numbering></numberingGroup><coverDate startDate="1994-03">March 1994</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="0006600" status="forIssue"><doi origin="wiley">10.1111/j.1502-3885.1994.tb00587.x</doi><idGroup><id type="unit" value="BOR66"></id></idGroup><countGroup><count type="pageTotal" number="8"></count></countGroup><titleGroup><title type="tocHeading1">Original Article</title></titleGroup><eventGroup><event type="firstOnline" date="2008-01-16"></event><event type="publishedOnlineFinalForm" date="2008-01-16"></event><event type="xmlConverted" agent="Converter:BPG_TO_WML3G version:2.3.6 mode:FullText source:HeaderRef result:HeaderRef" date="2010-04-21"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-08"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-15"></event></eventGroup><numberingGroup><numbering type="pageFirst" number="66">66</numbering><numbering type="pageLast" number="73">73</numbering></numberingGroup><linkGroup><link type="toTypesetVersion" href="file:BOR.BOR66.pdf"></link></linkGroup></publicationMeta><contentMeta><unparsedEditorialHistory>revised 91h July, 1993.</unparsedEditorialHistory><countGroup><count type="referenceTotal" number="35"></count><count type="linksCrossRef" number="4"></count></countGroup><titleGroup><title type="main">Temperature oscillations over the last 10,000 years in western Europe estimated from terrestrial mollusc assemblages</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1"><personName><givenNames>DENIS‐DIDIER</givenNames><familyName>ROUSSEAU</familyName></personName></creator><creator creatorRole="author" xml:id="cr2" affiliationRef="#a2"><personName><givenNames>NICOLE</givenNames><familyName>LIMONDIN</familyName></personName></creator><creator creatorRole="author" xml:id="cr3" affiliationRef="#a3"><personName><givenNames>FRÉDÉRIC</givenNames><familyName>MAGNIN</familyName></personName></creator><creator creatorRole="author" xml:id="cr4" affiliationRef="#a4"><personName><givenNames>JEAN‐JACQUES</givenNames><familyName>PUISSEGUR</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="US"><unparsedAffiliation>URA CNRS 327, Université Montpellier II, place Eugène Bataillon, 34095 Montpellier, France and Lamont‐Doherty Geological Observatory of Columbia University, Palisades, NY 10964 USA</unparsedAffiliation></affiliation><affiliation xml:id="a2" countryCode="FR"><unparsedAffiliation>UPR CNRS 7557, Laboratoire de Chrono‐écologie, 16 route de Gray, 25030 Besançon cedex, France</unparsedAffiliation></affiliation><affiliation xml:id="a3" countryCode="FR"><unparsedAffiliation>URA CNRS 903, Université Aix‐Marseille II, Institut de Géographie, 29 avenue Robert Schuman, 13621 Aix‐en‐Provence cedex, France</unparsedAffiliation></affiliation><affiliation xml:id="a4" countryCode="FR"><unparsedAffiliation>Hauteroche, 21150 Les Laumes, France; 30 October, 1992</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main" xml:lang="en"><p>Snail assemblages are used to estimate February and August temperatures during the past 10,000 years in western Europe. We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. 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We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. 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