Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene
Identifieur interne : 000233 ( Istex/Corpus ); précédent : 000232; suivant : 000234Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene
Auteurs : Nancy Radle ; Claire M. Keister ; Richard W. BattarbeeSource :
- Journal of Paleolimnology [ 0921-2728 ] ; 1989-09-01.
Abstract
Abstract: Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm−1 in the late-glacial period to > 10 000 μS cm−1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.
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DOI: 10.1007/BF00202044
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<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title><author><name sortKey="Radle, Nancy" sort="Radle, Nancy" uniqKey="Radle N" first="Nancy" last="Radle">Nancy Radle</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation></author><author><name sortKey="Keister, Claire M" sort="Keister, Claire M" uniqKey="Keister C" first="Claire M." last="Keister">Claire M. Keister</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation></author><author><name sortKey="Battarbee, Richard W" sort="Battarbee, Richard W" uniqKey="Battarbee R" first="Richard W." last="Battarbee">Richard W. Battarbee</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>Palaeoecology Research Unit, University College London, 26 Bedford Way, WC1H OAP, London, UK</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0</idno><date when="1989" year="1989">1989</date><idno type="doi">10.1007/BF00202044</idno><idno type="url">https://api.istex.fr/document/2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000233</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000233</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title><author><name sortKey="Radle, Nancy" sort="Radle, Nancy" uniqKey="Radle N" first="Nancy" last="Radle">Nancy Radle</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation></author><author><name sortKey="Keister, Claire M" sort="Keister, Claire M" uniqKey="Keister C" first="Claire M." last="Keister">Claire M. Keister</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation></author><author><name sortKey="Battarbee, Richard W" sort="Battarbee, Richard W" uniqKey="Battarbee R" first="Richard W." last="Battarbee">Richard W. Battarbee</name><affiliation><mods:affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</mods:affiliation></affiliation><affiliation><mods:affiliation>Palaeoecology Research Unit, University College London, 26 Bedford Way, WC1H OAP, London, UK</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="1989-09-01">1989-09-01</date><biblScope unit="volume">2</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="159">159</biblScope><biblScope unit="page" to="172">172</biblScope></imprint><idno type="ISSN">0921-2728</idno></series><idno type="istex">2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0</idno><idno type="DOI">10.1007/BF00202044</idno><idno type="ArticleID">BF00202044</idno><idno type="ArticleID">Art1</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: Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm−1 in the late-glacial period to > 10 000 μS cm−1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Nancy Radle</name><affiliations><json:string>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</json:string></affiliations></json:item><json:item><name>Claire M. Keister</name><affiliations><json:string>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</json:string></affiliations></json:item><json:item><name>Richard W. Battarbee</name><affiliations><json:string>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</json:string><json:string>Palaeoecology Research Unit, University College London, 26 Bedford Way, WC1H OAP, London, UK</json:string></affiliations></json:item></author><articleId><json:string>BF00202044</json:string><json:string>Art1</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm−1 in the late-glacial period to > 10 000 μS cm−1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.</abstract><qualityIndicators><score>7.58</score><pdfVersion>1.3</pdfVersion><pdfPageSize>547.28 x 738 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1417</abstractCharCount><pdfWordCount>5170</pdfWordCount><pdfCharCount>31612</pdfCharCount><pdfPageCount>14</pdfPageCount><abstractWordCount>215</abstractWordCount></qualityIndicators><title>Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. 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Res</title><publicationDate>1976</publicationDate></host><title>The dynamic nature of Holocene vegetation-a problem in palaeoclimatology, biogeography and stratigraphic nomenclature</title><publicationDate>1976</publicationDate></json:item><json:item><author><json:item><name>H,E Wright</name></json:item><json:item><name>T,C Winter</name></json:item><json:item><name>H,L Patten</name></json:item></author><host><volume>74</volume><pages><last>13</last><first>1371</first></pages><author></author><title>Geological Society of America, Bulletin</title><publicationDate>1963</publicationDate></host><title>Two pollen diagrams from southeastern Minnesota: problems in the regional late-glacial and postglacial vegetational history</title><publicationDate>1963</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>2</volume><pages><last>172</last><first>159</first></pages><issn><json:string>0921-2728</json:string></issn><issue>3</issue><subject><json:item><value>Geochemistry</value></json:item><json:item><value>Hydrogeology</value></json:item><json:item><value>Meteorology/Climatology</value></json:item><json:item><value>Sedimentology</value></json:item><json:item><value>Hydrobiology</value></json:item></subject><journalId><json:string>10933</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1573-0417</json:string></eissn><title>Journal of Paleolimnology</title><publicationDate>1989</publicationDate><copyrightDate>1989</copyrightDate></host><publicationDate>1989</publicationDate><copyrightDate>1989</copyrightDate><doi><json:string>10.1007/BF00202044</json:string></doi><id>2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><availability><p>Kluwer Academic Publishers, 1989</p></availability><date>1988-11-22</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title><author xml:id="author-1"><persName><forename type="first">Nancy</forename><surname>Radle</surname></persName><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation></author><author xml:id="author-2"><persName><forename type="first">Claire</forename><surname>Keister</surname></persName><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation></author><author xml:id="author-3"><persName><forename type="first">Richard</forename><surname>Battarbee</surname></persName><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation><affiliation>Palaeoecology Research Unit, University College London, 26 Bedford Way, WC1H OAP, London, UK</affiliation></author></analytic><monogr><title level="j">Journal of Paleolimnology</title><title level="j" type="abbrev">J Paleolimnol</title><idno type="journal-ID">10933</idno><idno type="pISSN">0921-2728</idno><idno type="eISSN">1573-0417</idno><idno type="issue-article-count">7</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1989-09-01"></date><biblScope unit="volume">2</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="159">159</biblScope><biblScope unit="page" to="172">172</biblScope></imprint></monogr><idno type="istex">2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0</idno><idno type="DOI">10.1007/BF00202044</idno><idno type="ArticleID">BF00202044</idno><idno type="ArticleID">Art1</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1988-11-22</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm−1 in the late-glacial period to > 10 000 μS cm−1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.</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="1988-11-22">Created</change><change when="1989-09-01">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="2017-01-20">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/2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0/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>2</VolumeIDStart><VolumeIDEnd>2</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd><IssueArticleCount>7</IssueArticleCount><IssueHistory><CoverDate><DateString>1989</DateString><Year>1989</Year><Month>9</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1989</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art1"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00202044</ArticleID><ArticleDOI>10.1007/BF00202044</ArticleDOI><ArticleSequenceNumber>1</ArticleSequenceNumber><ArticleTitle Language="En">Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</ArticleTitle><ArticleFirstPage>159</ArticleFirstPage><ArticleLastPage>172</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>7</Month><Day>15</Day></RegistrationDate><Received><Year>1988</Year><Month>11</Month><Day>22</Day></Received></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1989</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>2</VolumeIDStart><VolumeIDEnd>2</VolumeIDEnd><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Nancy</GivenName><FamilyName>Radle</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Claire</GivenName><GivenName>M.</GivenName><FamilyName>Keister</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1 Aff2"><AuthorName DisplayOrder="Western"><GivenName>Richard</GivenName><GivenName>W.</GivenName><FamilyName>Battarbee</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Limnological Research Center</OrgDivision><OrgName>University of Minnesota</OrgName><OrgAddress><Postcode>55455</Postcode><City>Minneapolis</City><State>MN</State><Country>USA</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>Palaeoecology Research Unit</OrgDivision><OrgName>University College London</OrgName><OrgAddress><Street>26 Bedford Way</Street><Postcode>WC1H OAP</Postcode><City>London</City><Country>UK</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the <Emphasis Type="Italic">Picea</Emphasis> pollen zone. When spruce forest changed to a <Emphasis Type="Italic">Betula</Emphasis> and then to a <Emphasis Type="Italic">Quercus/Ulmus</Emphasis> woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, <Emphasis Type="Italic">Ambrosia</Emphasis>, and <Emphasis Type="Italic">Artemisia</Emphasis> dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by <Emphasis Type="Italic">Cyclotella quillensis, Chaetoceros</Emphasis>, and eventually <Emphasis Type="Italic">Cyclotella caspia</Emphasis>. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm<Superscript>−1</Superscript> in the late-glacial period to > 10 000 μS cm<Superscript>−1</Superscript> in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>diatoms</Keyword><Keyword>pollen</Keyword><Keyword>geochemistry</Keyword><Keyword>salinity</Keyword><Keyword>paleoclimate</Keyword><Keyword>South Dakota</Keyword></KeywordGroup><ArticleNote Type="Misc"><SimplePara>Contribution 299, Limnological Research Center.</SimplePara></ArticleNote></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Diatom, pollen, and geochemical evidence for the palaeosalinity of Medicine Lake, S. Dakota, during the late-Wisconsin and early Holocene</title></titleInfo><name type="personal"><namePart type="given">Nancy</namePart><namePart type="family">Radle</namePart><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Claire</namePart><namePart type="given">M.</namePart><namePart type="family">Keister</namePart><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Richard</namePart><namePart type="given">W.</namePart><namePart type="family">Battarbee</namePart><affiliation>Limnological Research Center, University of Minnesota, 55455, Minneapolis, MN, USA</affiliation><affiliation>Palaeoecology Research Unit, University College London, 26 Bedford Way, WC1H OAP, London, UK</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><dateCreated encoding="w3cdtf">1988-11-22</dateCreated><dateIssued encoding="w3cdtf">1989-09-01</dateIssued><copyrightDate encoding="w3cdtf">1989</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: Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 μS cm−1 in the late-glacial period to > 10 000 μS cm−1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.</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">1989-09-01</dateIssued><copyrightDate encoding="w3cdtf">1989</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">7</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1989</date><detail type="volume"><number>2</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="pages"><start>159</start><end>172</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1989</recordOrigin></recordInfo></relatedItem><identifier type="istex">2B45A972A3CCED84A68EE1BB3CE5AA00892D31C0</identifier><identifier type="DOI">10.1007/BF00202044</identifier><identifier type="ArticleID">BF00202044</identifier><identifier type="ArticleID">Art1</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1989</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1989</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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