Brown earth and podzol: soil genesis illuminated by microfossil analysis
Identifieur interne : 000136 ( Istex/Corpus ); précédent : 000135; suivant : 000137Brown earth and podzol: soil genesis illuminated by microfossil analysis
Auteurs : Svend Th. AndersenSource :
- Boreas [ 0300-9483 ] ; 1979-03.
Abstract
Andersen, S. Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. Boreas, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483. Pollen and other plant microfossils were studied in soil profiles from a Fagus‐Quercus petraea woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. The various stages are related to vegetational changes and the processes were completed within a few hundred years.
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DOI: 10.1111/j.1502-3885.1979.tb00431.x
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Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. Boreas, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483. Pollen and other plant microfossils were studied in soil profiles from a Fagus‐Quercus petraea woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. The various stages are related to vegetational changes and the processes were completed within a few hundred years.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>SVEND TH. ANDERSEN</name><affiliations><json:string>Geobotanical Department, Geological Survey of Denmark, Thoravej 31, DK‐2400 Copenhagen NV, Denmark; 5th April, 1978.</json:string></affiliations></json:item></author><articleId><json:string>BOR59</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Andersen, S. Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. Boreas, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483. Pollen and other plant microfossils were studied in soil profiles from a Fagus‐Quercus petraea woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. The various stages are related to vegetational changes and the processes were completed within a few hundred years.</abstract><qualityIndicators><score>6.704</score><pdfVersion>1.3</pdfVersion><pdfPageSize>490.079 x 703.919 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>976</abstractCharCount><pdfWordCount>5864</pdfWordCount><pdfCharCount>35743</pdfCharCount><pdfPageCount>15</pdfPageCount><abstractWordCount>142</abstractWordCount></qualityIndicators><title>Brown earth and podzol: soil genesis illuminated by microfossil analysis</title><refBibs><json:item><author><json:item><name>H. J. Altemüller</name></json:item></author><host><pages><last>148</last><first>137</first></pages><author></author><title>Arbeilen aus dem Gebiet der Mikromor‐phologie des Bodens</title></host><title>Beitrag zur mikromorphologischen Differenzierung von durchschlämmter Parabraunerde, Podsol‐Braunerde und Humus‐Podsol</title></json:item><json:item><author><json:item><name>S. T. 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Centralb.</title></host><title>Spuren tierischer Tätigkeit im Boden des Buchenwaldes</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>8</volume><publisherId><json:string>BOR</json:string></publisherId><pages><total>15</total><last>73</last><first>59</first></pages><issn><json:string>0300-9483</json:string></issn><issue>1</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>1979</publicationDate><copyrightDate>1979</copyrightDate><doi><json:string>10.1111/j.1502-3885.1979.tb00431.x</json:string></doi><id>FC05E31E80860F3182AA5D2AB027C81F8C6CF028</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/FC05E31E80860F3182AA5D2AB027C81F8C6CF028/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/FC05E31E80860F3182AA5D2AB027C81F8C6CF028/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/FC05E31E80860F3182AA5D2AB027C81F8C6CF028/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Brown earth and podzol: soil genesis illuminated by microfossil analysis</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><availability><p>WILEY</p></availability><date>1979</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Brown earth and podzol: soil genesis illuminated by microfossil analysis</title><author xml:id="author-1"><persName><forename type="first">SVEND TH.</forename><surname>ANDERSEN</surname></persName><affiliation>Geobotanical Department, Geological Survey of Denmark, Thoravej 31, DK‐2400 Copenhagen NV, Denmark; 5th April, 1978.</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="1979-03"></date><biblScope unit="volume">8</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="59">59</biblScope><biblScope unit="page" to="73">73</biblScope></imprint></monogr><idno type="istex">FC05E31E80860F3182AA5D2AB027C81F8C6CF028</idno><idno type="DOI">10.1111/j.1502-3885.1979.tb00431.x</idno><idno type="ArticleID">BOR59</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1979</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Andersen, S. Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. Boreas, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483. Pollen and other plant microfossils were studied in soil profiles from a Fagus‐Quercus petraea woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. The various stages are related to vegetational changes and the processes were completed within a few hundred years.</p></abstract></profileDesc><revisionDesc><change when="1979-03">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/FC05E31E80860F3182AA5D2AB027C81F8C6CF028/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.1979.8.issue-1</doi><numberingGroup><numbering type="journalVolume" number="8">8</numbering><numbering type="journalIssue" number="1">1</numbering></numberingGroup><coverDate startDate="1979-03">March 1979</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="0005900" status="forIssue"><doi origin="wiley">10.1111/j.1502-3885.1979.tb00431.x</doi><idGroup><id type="unit" value="BOR59"></id></idGroup><countGroup><count type="pageTotal" number="15"></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:2.3.2 mode:FullText source:HeaderRef result:HeaderRef" date="2010-03-09"></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="59">59</numbering><numbering type="pageLast" number="73">73</numbering></numberingGroup><linkGroup><link type="toTypesetVersion" href="file:BOR.BOR59.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="referenceTotal" number="37"></count><count type="linksCrossRef" number="1"></count></countGroup><titleGroup><title type="main">Brown earth and podzol: soil genesis illuminated by microfossil analysis</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1"><personName><givenNames>SVEND TH.</givenNames><familyName>ANDERSEN</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="DK"><unparsedAffiliation>Geobotanical Department, Geological Survey of Denmark, Thoravej 31, DK‐2400 Copenhagen NV, Denmark; 5th April, 1978.</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main" xml:lang="en"><p>Andersen, S. Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. <i>Boreas</i>, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483.</p><p>Pollen and other plant microfossils were studied in soil profiles from a <i>Fagus‐Quercus petraea</i> woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. The various stages are related to vegetational changes and the processes were completed within a few hundred years.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Brown earth and podzol: soil genesis illuminated by microfossil analysis</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Brown earth and podzol: soil genesis illuminated by microfossil analysis</title></titleInfo><name type="personal"><namePart type="given">SVEND TH.</namePart><namePart type="family">ANDERSEN</namePart><affiliation>Geobotanical Department, Geological Survey of Denmark, Thoravej 31, DK‐2400 Copenhagen NV, Denmark; 5th April, 1978.</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">1979-03</dateIssued><copyrightDate encoding="w3cdtf">1979</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">37</extent></physicalDescription><abstract lang="en">Andersen, S. Th. 1979 03 01: Brown earth and podzol: soil genesis illuminated by microfossil analysis. Boreas, Vol. 8, pp. 59–73. Oslo. ISSN 0300–9483. Pollen and other plant microfossils were studied in soil profiles from a Fagus‐Quercus petraea woodland in eastern Jutland, Denmark. Fungal hypha fragments in the soil show characteristic length frequency distributions, which indicate comminution by large arthropods and microarthropods (Oribatei) during the burial. Distribution of the hypha fragments within the podzol indicates development from a former brown earth. The pollen sequence in a humus deposit reflects recent vegetational development. Modification of pollen assemblages in the mineral soils can be explained by mixing during burial by soil fauna. Development from brown earth to podzoloid and podzol follows the models assumed by pedologists. 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