Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)
Identifieur interne : 001483 ( Istex/Corpus ); précédent : 001482; suivant : 001484Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)
Auteurs : Meinrad KüttelSource :
- Boreas [ 0300-9483 ] ; 1977-10.
Abstract
New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.
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DOI: 10.1111/j.1502-3885.1977.tb00293.x
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><author><name sortKey="Kuttel, Meinrad" sort="Kuttel, Meinrad" uniqKey="Kuttel M" first="Meinrad" last="Küttel">Meinrad Küttel</name><affiliation><mods:affiliation>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:A612D176663A94A89609F0344F92E32AA6A51DE7</idno><date when="1977" year="1977">1977</date><idno type="doi">10.1111/j.1502-3885.1977.tb00293.x</idno><idno type="url">https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001483</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001483</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><author><name sortKey="Kuttel, Meinrad" sort="Kuttel, Meinrad" uniqKey="Kuttel M" first="Meinrad" last="Küttel">Meinrad Küttel</name><affiliation><mods:affiliation>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Boreas</title><idno type="ISSN">0300-9483</idno><idno type="eISSN">1502-3885</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1977-10">1977-10</date><biblScope unit="volume">6</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="259">259</biblScope><biblScope unit="page" to="274">274</biblScope></imprint><idno type="ISSN">0300-9483</idno></series><idno type="istex">A612D176663A94A89609F0344F92E32AA6A51DE7</idno><idno type="DOI">10.1111/j.1502-3885.1977.tb00293.x</idno><idno type="ArticleID">BOR259</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0300-9483</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>MEINRAD KÜTTEL</name><affiliations><json:string>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</json:string></affiliations></json:item></author><articleId><json:string>BOR259</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.</abstract><qualityIndicators><score>6.532</score><pdfVersion>1.4</pdfVersion><pdfPageSize>477.72 x 710.759 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>589</abstractCharCount><pdfWordCount>6464</pdfWordCount><pdfCharCount>45019</pdfCharCount><pdfPageCount>16</pdfPageCount><abstractWordCount>86</abstractWordCount></qualityIndicators><title>Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><refBibs><json:item><author><json:item><name>L. 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Basel</title></host><title>Postglaziale Gletscherstände und Klimaschwankungen im Gotthardmassiv und Vorderrheingcbiet.</title></json:item><json:item><host><author></author><title>Geologische Karte der Tessineralpen 1:50 000 zwischen Maggia‐ und Blenio‐TalSpezialkarte Nr</title></host></json:item><json:item><host><author></author><title>Schweizerische Landestopographie 1965: Blatt</title></host></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>6</volume><publisherId><json:string>BOR</json:string></publisherId><pages><total>16</total><last>274</last><first>259</first></pages><issn><json:string>0300-9483</json:string></issn><issue>3</issue><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1502-3885</json:string></eissn><title>Boreas</title><doi><json:string>10.1111/(ISSN)1502-3885</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>geography, physical</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>1977</publicationDate><copyrightDate>1977</copyrightDate><doi><json:string>10.1111/j.1502-3885.1977.tb00293.x</json:string></doi><id>A612D176663A94A89609F0344F92E32AA6A51DE7</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><availability><p>WILEY</p></availability><date>1977</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title><author xml:id="author-1"><persName><forename type="first">MEINRAD</forename><surname>KÜTTEL</surname></persName><affiliation>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</affiliation></author></analytic><monogr><title level="j">Boreas</title><idno type="pISSN">0300-9483</idno><idno type="eISSN">1502-3885</idno><idno type="DOI">10.1111/(ISSN)1502-3885</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="1977-10"></date><biblScope unit="volume">6</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="259">259</biblScope><biblScope unit="page" to="274">274</biblScope></imprint></monogr><idno type="istex">A612D176663A94A89609F0344F92E32AA6A51DE7</idno><idno type="DOI">10.1111/j.1502-3885.1977.tb00293.x</idno><idno type="ArticleID">BOR259</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1977</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.</p></abstract></profileDesc><revisionDesc><change when="1977-10">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/A612D176663A94A89609F0344F92E32AA6A51DE7/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="10003"><doi origin="wiley">10.1111/bor.1977.6.issue-3</doi><numberingGroup><numbering type="journalVolume" number="6">6</numbering><numbering type="journalIssue" number="3">3</numbering></numberingGroup><coverDate startDate="1977-10">October 1977</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="0025900" status="forIssue"><doi origin="wiley">10.1111/j.1502-3885.1977.tb00293.x</doi><idGroup><id type="unit" value="BOR259"></id></idGroup><countGroup><count type="pageTotal" number="16"></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:2.3.5 mode:FullText source:HeaderRef result:HeaderRef" date="2010-04-07"></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="259">259</numbering><numbering type="pageLast" number="274">274</numbering></numberingGroup><linkGroup><link type="toTypesetVersion" href="file:BOR.BOR259.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="referenceTotal" number="50"></count><count type="linksCrossRef" number="1"></count></countGroup><titleGroup><title type="main">Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1"><personName><givenNames>MEINRAD</givenNames><familyName>KÜTTEL</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1"><unparsedAffiliation>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main" xml:lang="en"><p>New pollen‐analytical investigations and two <sup>14</sup>C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual <sup>14</sup>C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the <sup>14</sup>C level are supposed for this period.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Pollenanalytische und geochronologische Untersuchungen zur Piottino‐Schwankung (Jüngere Dryas)</title></titleInfo><name type="personal"><namePart type="given">MEINRAD</namePart><namePart type="family">KÜTTEL</namePart><affiliation>Systematrsch‐Geobotanrsches Institut der Universität, Altenbergrain 21, CH‐3013 Bern, Schweiz, 1st December, 1976</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">1977-10</dateIssued><copyrightDate encoding="w3cdtf">1977</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="references">50</extent></physicalDescription><abstract lang="en">New pollen‐analytical investigations and two 14C series indicate that, at the Bedrina on Mount Piottino (Tessin, Switzerland), the post‐Allerød NAP phase (Piottino oscillation) represents the well‐marked Younger Dryas at least for the most part. The late‐glacial part of the profile is re‐classified, and the term Piottino oscillation is rejected, as it is largely identical with the Younger Dryas. Individual 14C dates from the transition between the Younger Dryas and the Preboreal should be considered critically. Considerable fluctuations in the 14C level are supposed for this period.</abstract><relatedItem type="host"><titleInfo><title>Boreas</title></titleInfo><genre type="journal">journal</genre><identifier type="ISSN">0300-9483</identifier><identifier type="eISSN">1502-3885</identifier><identifier type="DOI">10.1111/(ISSN)1502-3885</identifier><identifier type="PublisherID">BOR</identifier><part><date>1977</date><detail type="volume"><caption>vol.</caption><number>6</number></detail><detail type="issue"><caption>no.</caption><number>3</number></detail><extent unit="pages"><start>259</start><end>274</end><total>16</total></extent></part></relatedItem><identifier type="istex">A612D176663A94A89609F0344F92E32AA6A51DE7</identifier><identifier type="DOI">10.1111/j.1502-3885.1977.tb00293.x</identifier><identifier type="ArticleID">BOR259</identifier><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Blackwell Publishing Ltd</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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