Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden
Identifieur interne : 000E50 ( Istex/Corpus ); précédent : 000E49; suivant : 000E51Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden
Auteurs : Hannelore H Kansson ; Joachim RegnéllSource :
- Journal of Paleolimnology [ 0921-2728 ] ; 1993-01-01.
Abstract
Abstract: Diatoms, pollen, physical and magnetic analyses of the sediments have been used to reconstruct the development over the last 6000 years of Lake Bussjösjön, a small lake in southern Sweden. Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From ca 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of Cyclostephanos dubius (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of C. dubius and the increase of Stephanodiscus species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.
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DOI: 10.1007/BF00210057
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</title><author><name sortKey="H Kansson, Hannelore" sort="H Kansson, Hannelore" uniqKey="H Kansson H" first="Hannelore" last="H Kansson">Hannelore H Kansson</name><affiliation><mods:affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</mods:affiliation></affiliation></author><author><name sortKey="Regnell, Joachim" sort="Regnell, Joachim" uniqKey="Regnell J" first="Joachim" last="Regnéll">Joachim Regnéll</name><affiliation><mods:affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:D95DBC8BD192778FB1FF409C083ECCEF4152AF47</idno><date when="1993" year="1993">1993</date><idno type="doi">10.1007/BF00210057</idno><idno type="url">https://api.istex.fr/document/D95DBC8BD192778FB1FF409C083ECCEF4152AF47/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000E50</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000E50</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</title><author><name sortKey="H Kansson, Hannelore" sort="H Kansson, Hannelore" uniqKey="H Kansson H" first="Hannelore" last="H Kansson">Hannelore H Kansson</name><affiliation><mods:affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</mods:affiliation></affiliation></author><author><name sortKey="Regnell, Joachim" sort="Regnell, Joachim" uniqKey="Regnell J" first="Joachim" last="Regnéll">Joachim Regnéll</name><affiliation><mods:affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="ISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1993-01-01">1993-01-01</date><biblScope unit="volume">8</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="49">49</biblScope><biblScope unit="page" to="69">69</biblScope></imprint><idno type="ISSN">0921-2728</idno></series><idno type="istex">D95DBC8BD192778FB1FF409C083ECCEF4152AF47</idno><idno type="DOI">10.1007/BF00210057</idno><idno type="ArticleID">BF00210057</idno><idno type="ArticleID">Art5</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0921-2728</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Diatoms, pollen, physical and magnetic analyses of the sediments have been used to reconstruct the development over the last 6000 years of Lake Bussjösjön, a small lake in southern Sweden. Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From ca 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of Cyclostephanos dubius (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of C. dubius and the increase of Stephanodiscus species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Hannelore Håkansson</name><affiliations><json:string>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</json:string></affiliations></json:item><json:item><name>Joachim Regnéll</name><affiliations><json:string>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</json:string></affiliations></json:item></author><articleId><json:string>BF00210057</json:string><json:string>Art5</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: Diatoms, pollen, physical and magnetic analyses of the sediments have been used to reconstruct the development over the last 6000 years of Lake Bussjösjön, a small lake in southern Sweden. Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From ca 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of Cyclostephanos dubius (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of C. dubius and the increase of Stephanodiscus species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.</abstract><qualityIndicators><score>7.388</score><pdfVersion>1.3</pdfVersion><pdfPageSize>547.28 x 738 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1260</abstractCharCount><pdfWordCount>7160</pdfWordCount><pdfCharCount>47156</pdfCharCount><pdfPageCount>21</pdfPageCount><abstractWordCount>199</abstractWordCount></qualityIndicators><title>Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</title><refBibs><json:item><host><author><json:item><name> Bjorck</name></json:item><json:item><name>G Dr</name></json:item></author><title>Digerfeldt for their valuable comments on an early draft of the manuscript We thank Dr J. Anderson and Dr T. 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Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From ca 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of Cyclostephanos dubius (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of C. dubius and the increase of Stephanodiscus species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Life Sciences</head><item><term>Geochemistry</term></item><item><term>Hydrogeology</term></item><item><term>Meteorology/Climatology</term></item><item><term>Sedimentology</term></item><item><term>Hydrobiology</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1993-01-01">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="2017-01-21">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/D95DBC8BD192778FB1FF409C083ECCEF4152AF47/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>Kluwer Academic Publishers</PublisherName><PublisherLocation>Dordrecht</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>10933</JournalID><JournalPrintISSN>0921-2728</JournalPrintISSN><JournalElectronicISSN>1573-0417</JournalElectronicISSN><JournalTitle>Journal of Paleolimnology</JournalTitle><JournalAbbreviatedTitle>J Paleolimnol</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Life Sciences</JournalSubject><JournalSubject Type="Secondary">Geochemistry</JournalSubject><JournalSubject Type="Secondary">Hydrogeology</JournalSubject><JournalSubject Type="Secondary">Meteorology/Climatology</JournalSubject><JournalSubject Type="Secondary">Sedimentology</JournalSubject><JournalSubject Type="Secondary">Hydrobiology</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>8</VolumeIDStart><VolumeIDEnd>8</VolumeIDEnd><VolumeIssueCount>3</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd><IssueArticleCount>9</IssueArticleCount><IssueHistory><CoverDate><DateString>1993</DateString><Year>1993</Year><Month>1</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1993</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art5"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00210057</ArticleID><ArticleDOI>10.1007/BF00210057</ArticleDOI><ArticleSequenceNumber>5</ArticleSequenceNumber><ArticleTitle Language="En">Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</ArticleTitle><ArticleFirstPage>49</ArticleFirstPage><ArticleLastPage>69</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>7</Month><Day>16</Day></RegistrationDate></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1993</CopyrightYear></ArticleCopyright><ArticleGrants 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></ArticleGrants><ArticleContext><JournalID>10933</JournalID><VolumeIDStart>8</VolumeIDStart><VolumeIDEnd>8</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Hannelore</GivenName><FamilyName>Håkansson</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Joachim</GivenName><FamilyName>Regnéll</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Department of Quaternary Geology</OrgDivision><OrgName>Lund University</OrgName><OrgAddress><Street>Tornavägen 13</Street><Postcode>S-223 63</Postcode><City>Lund</City><Country>Sweden</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Diatoms, pollen, physical and magnetic analyses of the sediments have been used to reconstruct the development over the last 6000 years of Lake Bussjösjön, a small lake in southern Sweden. Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From <Emphasis Type="Italic">ca</Emphasis> 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of <Emphasis Type="Italic">Cyclostephanos dubius</Emphasis> (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of <Emphasis Type="Italic">C. dubius</Emphasis> and the increase of <Emphasis Type="Italic">Stephanodiscus</Emphasis> species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>South Sweden</Keyword><Keyword>Holocene</Keyword><Keyword>diatoms</Keyword><Keyword>pollen</Keyword><Keyword>eutrophication</Keyword><Keyword>catchment history</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Diatom succession related to land use during the last 6000 years: a study of a small eutrophic lake in southern Sweden</title></titleInfo><name type="personal"><namePart type="given">Hannelore</namePart><namePart type="family">Håkansson</namePart><affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Joachim</namePart><namePart type="family">Regnéll</namePart><affiliation>Department of Quaternary Geology, Lund University, Tornavägen 13, S-223 63, Lund, Sweden</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateIssued encoding="w3cdtf">1993-01-01</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: Diatoms, pollen, physical and magnetic analyses of the sediments have been used to reconstruct the development over the last 6000 years of Lake Bussjösjön, a small lake in southern Sweden. Stratigraphic variations in a core of more than 15 m reveal changes in diatom assemblages, which correspond closely to changes in pollen, loss-on-ignition, and magnetic measurements that are related to land use and vegetation changes in the catchment. From ca 6000 BP to 2700 BP, a forest surrounded what was then a slightly eutrophic lake. The sudden appearance of Cyclostephanos dubius (Fricke) Round and several epiphytic/epipsammic diatoms at 2700 BP coincides with deforestation of the catchment (2700 BP to 2500 BP). A change in land use from predominantly pasture to arable land from 1300 BP to 1100 BP caused a high level of soil erosion with a decrease of C. dubius and the increase of Stephanodiscus species. An increase of epiphytic/epipsammic species coincides with increased arable farming and the change from a field-rotation to a crop-rotation system, and shows not only an increase in eutrophication but also changes in water depth. The influence of the catchment through time resulted in a smaller, shallower and eutrophic to hypertrophic lake.</abstract><relatedItem type="host"><titleInfo><title>Journal of Paleolimnology</title></titleInfo><titleInfo type="abbreviated"><title>J Paleolimnol</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1993-01-01</dateIssued><copyrightDate encoding="w3cdtf">1993</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Geochemistry</topic><topic>Hydrogeology</topic><topic>Meteorology/Climatology</topic><topic>Sedimentology</topic><topic>Hydrobiology</topic></subject><identifier type="ISSN">0921-2728</identifier><identifier type="eISSN">1573-0417</identifier><identifier type="JournalID">10933</identifier><identifier type="IssueArticleCount">9</identifier><identifier type="VolumeIssueCount">3</identifier><part><date>1993</date><detail type="volume"><number>8</number><caption>vol.</caption></detail><detail type="issue"><number>1</number><caption>no.</caption></detail><extent unit="pages"><start>49</start><end>69</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1993</recordOrigin></recordInfo></relatedItem><identifier type="istex">D95DBC8BD192778FB1FF409C083ECCEF4152AF47</identifier><identifier type="DOI">10.1007/BF00210057</identifier><identifier type="ArticleID">BF00210057</identifier><identifier type="ArticleID">Art5</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1993</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1993</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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