The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins
Identifieur interne : 001085 ( Istex/Corpus ); précédent : 001084; suivant : 001086The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins
Auteurs : J. M. Martin ; A. J. ThomasSource :
- Marine Chemistry [ 0304-4203 ] ; 1994.
Abstract
A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.
Url:
DOI: 10.1016/0304-4203(94)90053-1
Links to Exploration step
ISTEX:FE5442B4595877990EEB5149FF0FD5632037415ELe document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
<author><name sortKey="Martin, J M" sort="Martin, J M" uniqKey="Martin J" first="J. M." last="Martin">J. M. Martin</name>
<affiliation><mods:affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Thomas, A J" sort="Thomas, A J" uniqKey="Thomas A" first="A. J." last="Thomas">A. J. Thomas</name>
<affiliation><mods:affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</mods:affiliation>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:FE5442B4595877990EEB5149FF0FD5632037415E</idno>
<date when="1994" year="1994">1994</date>
<idno type="doi">10.1016/0304-4203(94)90053-1</idno>
<idno type="url">https://api.istex.fr/document/FE5442B4595877990EEB5149FF0FD5632037415E/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">001085</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001085</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title level="a">The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
<author><name sortKey="Martin, J M" sort="Martin, J M" uniqKey="Martin J" first="J. M." last="Martin">J. M. Martin</name>
<affiliation><mods:affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</mods:affiliation>
</affiliation>
</author>
<author><name sortKey="Thomas, A J" sort="Thomas, A J" uniqKey="Thomas A" first="A. J." last="Thomas">A. J. Thomas</name>
<affiliation><mods:affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</mods:affiliation>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series><title level="j">Marine Chemistry</title>
<title level="j" type="abbrev">MARCHE</title>
<idno type="ISSN">0304-4203</idno>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1994">1994</date>
<biblScope unit="volume">46</biblScope>
<biblScope unit="issue">1–2</biblScope>
<biblScope unit="page" from="165">165</biblScope>
<biblScope unit="page" to="178">178</biblScope>
</imprint>
<idno type="ISSN">0304-4203</idno>
</series>
<idno type="istex">FE5442B4595877990EEB5149FF0FD5632037415E</idno>
<idno type="DOI">10.1016/0304-4203(94)90053-1</idno>
<idno type="PII">0304-4203(94)90053-1</idno>
</biblStruct>
</sourceDesc>
<seriesStmt><idno type="ISSN">0304-4203</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass></textClass>
<langUsage><language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.</div>
</front>
</TEI>
<istex><corpusName>elsevier</corpusName>
<author><json:item><name>J.M. Martin</name>
<affiliations><json:string>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</json:string>
</affiliations>
</json:item>
<json:item><name>A.J. Thomas</name>
<affiliations><json:string>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</json:string>
</affiliations>
</json:item>
</author>
<language><json:string>eng</json:string>
</language>
<originalGenre><json:string>Full-length article</json:string>
</originalGenre>
<abstract>A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.</abstract>
<qualityIndicators><score>6.392</score>
<pdfVersion>1.2</pdfVersion>
<pdfPageSize>548 x 756 pts</pdfPageSize>
<refBibsNative>true</refBibsNative>
<keywordCount>0</keywordCount>
<abstractCharCount>712</abstractCharCount>
<pdfWordCount>7058</pdfWordCount>
<pdfCharCount>42636</pdfCharCount>
<pdfPageCount>14</pdfPageCount>
<abstractWordCount>116</abstractWordCount>
</qualityIndicators>
<title>The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
<pii><json:string>0304-4203(94)90053-1</json:string>
</pii>
<genre><json:string>research-article</json:string>
</genre>
<serie><volume>64</volume>
<pages><last>69</last>
<first>57</first>
</pages>
<language><json:string>unknown</json:string>
</language>
<title>Mitt. Geol. Paläontol.</title>
</serie>
<host><volume>46</volume>
<pii><json:string>S0304-4203(00)X0088-6</json:string>
</pii>
<editor><json:item><name>Goran Kniewald</name>
</json:item>
<json:item><name>Marko Branica</name>
</json:item>
</editor>
<pages><last>178</last>
<first>165</first>
</pages>
<conference><json:item><name>12th International Symposium @'Chemistry of the Mediterranean@' , Rovinj, Croatia 19920518 19920523</name>
</json:item>
</conference>
<issn><json:string>0304-4203</json:string>
</issn>
<issue>1–2</issue>
<genre><json:string>journal</json:string>
</genre>
<language><json:string>unknown</json:string>
</language>
<title>Marine Chemistry</title>
<publicationDate>1994</publicationDate>
</host>
<categories><wos><json:string>OCEANOGRAPHY</json:string>
<json:string>CHEMISTRY</json:string>
<json:string>CHEMISTRY, MULTIDISCIPLINARY</json:string>
</wos>
</categories>
<publicationDate>1994</publicationDate>
<copyrightDate>1994</copyrightDate>
<doi><json:string>10.1016/0304-4203(94)90053-1</json:string>
</doi>
<id>FE5442B4595877990EEB5149FF0FD5632037415E</id>
<score>0.048211202</score>
<fulltext><json:item><original>true</original>
<mimetype>application/pdf</mimetype>
<extension>pdf</extension>
<uri>https://api.istex.fr/document/FE5442B4595877990EEB5149FF0FD5632037415E/fulltext/pdf</uri>
</json:item>
<json:item><original>false</original>
<mimetype>application/zip</mimetype>
<extension>zip</extension>
<uri>https://api.istex.fr/document/FE5442B4595877990EEB5149FF0FD5632037415E/fulltext/zip</uri>
</json:item>
<istex:fulltextTEI uri="https://api.istex.fr/document/FE5442B4595877990EEB5149FF0FD5632037415E/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
</titleStmt>
<publicationStmt><authority>ISTEX</authority>
<publisher>ELSEVIER</publisher>
<availability><p>ELSEVIER</p>
</availability>
<date>1994</date>
</publicationStmt>
<sourceDesc><biblStruct type="inbook"><analytic><title level="a">The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
<author xml:id="author-1"><persName><forename type="first">J.M.</forename>
<surname>Martin</surname>
</persName>
<affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</affiliation>
</author>
<author xml:id="author-2"><persName><forename type="first">A.J.</forename>
<surname>Thomas</surname>
</persName>
<affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</affiliation>
</author>
</analytic>
<monogr><title level="j">Marine Chemistry</title>
<title level="j" type="abbrev">MARCHE</title>
<idno type="pISSN">0304-4203</idno>
<idno type="PII">S0304-4203(00)X0088-6</idno>
<meeting><addName>12th International Symposium @'Chemistry of the Mediterranean@' , Rovinj, Croatia</addName>
<date>19920518</date>
<date>19920523</date>
</meeting>
<editor><persName>Goran Kniewald</persName>
</editor>
<editor><persName>Marko Branica</persName>
</editor>
<imprint><publisher>ELSEVIER</publisher>
<date type="published" when="1994"></date>
<biblScope unit="volume">46</biblScope>
<biblScope unit="issue">1–2</biblScope>
<biblScope unit="page" from="165">165</biblScope>
<biblScope unit="page" to="178">178</biblScope>
</imprint>
</monogr>
<idno type="istex">FE5442B4595877990EEB5149FF0FD5632037415E</idno>
<idno type="DOI">10.1016/0304-4203(94)90053-1</idno>
<idno type="PII">0304-4203(94)90053-1</idno>
</biblStruct>
</sourceDesc>
</fileDesc>
<profileDesc><creation><date>1994</date>
</creation>
<langUsage><language ident="en">en</language>
</langUsage>
<abstract xml:lang="en"><p>A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.</p>
</abstract>
</profileDesc>
<revisionDesc><change when="1994">Published</change>
</revisionDesc>
</teiHeader>
</istex:fulltextTEI>
<json:item><original>false</original>
<mimetype>text/plain</mimetype>
<extension>txt</extension>
<uri>https://api.istex.fr/document/FE5442B4595877990EEB5149FF0FD5632037415E/fulltext/txt</uri>
</json:item>
</fulltext>
<metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration>
<istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType>
<istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>MARCHE</jid>
<aid>94900531</aid>
<ce:pii>0304-4203(94)90053-1</ce:pii>
<ce:doi>10.1016/0304-4203(94)90053-1</ce:doi>
<ce:copyright type="unknown" year="1994"></ce:copyright>
</item-info>
<head><ce:title>The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</ce:title>
<ce:author-group><ce:author><ce:given-name>J.M.</ce:given-name>
<ce:surname>Martin</ce:surname>
</ce:author>
<ce:author><ce:given-name>A.J.</ce:given-name>
<ce:surname>Thomas</ce:surname>
</ce:author>
<ce:affiliation><ce:textfn>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:date-received day="19" month="1" year="1993"></ce:date-received>
<ce:date-accepted day="9" month="7" year="1993"></ce:date-accepted>
<ce:abstract><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
</head>
</converted-article>
</istex:document>
</istex:metadataXml>
<mods version="3.6"><titleInfo><title>The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
</titleInfo>
<titleInfo type="alternative" contentType="CDATA"><title>The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins</title>
</titleInfo>
<name type="personal"><namePart type="given">J.M.</namePart>
<namePart type="family">Martin</namePart>
<affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal"><namePart type="given">A.J.</namePart>
<namePart type="family">Thomas</namePart>
<affiliation>Institut de Biogéochimie Marine, URA CNRS 386, Ecole Normale Supérieure, 1 rue M. Arnoux, F-92120 Montrouge, France</affiliation>
<role><roleTerm type="text">author</roleTerm>
</role>
</name>
<typeOfResource>text</typeOfResource>
<genre type="research-article" displayLabel="Full-length article"></genre>
<originInfo><publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">1994</dateIssued>
<copyrightDate encoding="w3cdtf">1994</copyrightDate>
</originInfo>
<language><languageTerm type="code" authority="iso639-2b">eng</languageTerm>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
</language>
<physicalDescription><internetMediaType>text/html</internetMediaType>
</physicalDescription>
<abstract lang="en">A tentative mass-balance of dissolved trace metals (TM) in the global ocean margin is presented. Comparison of the various TM sources demonstrates the limited contribution of the telluric source (riverine and atmospheric), as compared to the oceanic input by upwelled water: marine inputs exceed telluric inputs by a factor of 2–3.5 for Cu, 2–7 for Zn, and of about 10 for Cd and Ni. Diagenetic TM release from deposited sediments, although likely for Cu and Zn, could not be quantified without ambiguity. Following intense water exchanges, TM are exchanged between the ocean margin and the open ocean very rapidly, and their short residence time is similar to the margin water residence time, i.e. about 1.3 yr.</abstract>
<relatedItem type="host"><titleInfo><title>Marine Chemistry</title>
</titleInfo>
<titleInfo type="abbreviated"><title>MARCHE</title>
</titleInfo>
<name type="conference"><namePart>12th International Symposium @'Chemistry of the Mediterranean@' , Rovinj, Croatia</namePart>
<namePart type="date">19920518</namePart>
<namePart type="date">19920523</namePart>
</name>
<name type="personal"><namePart>Goran Kniewald</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<name type="personal"><namePart>Marko Branica</namePart>
<role><roleTerm type="text">editor</roleTerm>
</role>
</name>
<genre type="journal">journal</genre>
<originInfo><dateIssued encoding="w3cdtf">199404</dateIssued>
</originInfo>
<identifier type="ISSN">0304-4203</identifier>
<identifier type="PII">S0304-4203(00)X0088-6</identifier>
<part><date>199404</date>
<detail type="issue"><title>12th International Symposium @'Chemistry of the Mediterranean@' , Rovinj, Croatia</title>
</detail>
<detail type="volume"><number>46</number>
<caption>vol.</caption>
</detail>
<detail type="issue"><number>1–2</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages"><start>1</start>
<end>215</end>
</extent>
<extent unit="pages"><start>165</start>
<end>178</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">FE5442B4595877990EEB5149FF0FD5632037415E</identifier>
<identifier type="DOI">10.1016/0304-4203(94)90053-1</identifier>
<identifier type="PII">0304-4203(94)90053-1</identifier>
<recordInfo><recordContentSource>ELSEVIER</recordContentSource>
</recordInfo>
</mods>
</metadata>
</istex>
</record>
Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/CobaltMaghrebV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 001085 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 001085 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien |wiki= Wicri/Terre |area= CobaltMaghrebV1 |flux= Istex |étape= Corpus |type= RBID |clé= ISTEX:FE5442B4595877990EEB5149FF0FD5632037415E |texte= The global insignificance of telluric input of dissolved trace metals (Cd, Cu, Ni and Zn) to ocean margins }}
![]() | This area was generated with Dilib version V0.6.32. | ![]() |