Serveur d'exploration sur Heinrich Schütz

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

An evaluation of 14C age relationships between co‐occurring foraminifera, alkenones, and total organic carbon in continental margin sediments

Identifieur interne : 000794 ( Main/Exploration ); précédent : 000793; suivant : 000795

An evaluation of 14C age relationships between co‐occurring foraminifera, alkenones, and total organic carbon in continental margin sediments

Auteurs : Gesine Mollenhauer [États-Unis] ; Markus Kienast [États-Unis, Canada] ; Frank Lamy [Allemagne] ; Helge Meggers [Allemagne] ; Ralph R. Schneider [Allemagne] ; John M. Hayes [États-Unis] ; Timothy I. Eglinton [États-Unis]

Source :

RBID : ISTEX:4B69B731AF9D28789B7C23A37684BCC3A8C1D44A

Abstract

Radiocarbon age relationships between co‐occurring planktic foraminifera, alkenones, and total organic carbon in sediments from the continental margins of southern Chile, northwest Africa, and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site‐specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000–4500 years older than co‐occurring foraminifera, alkenones were significantly (∼1000 years) older than co‐occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2σ error or better) in the NW African and South China Sea sediments. Total organic matter and alkenone ages were similar off Namibia (age difference TOC alkenones: 200–700 years), Chile (100–450 years), and NW Africa (360–770 years), suggesting minor contributions of preaged terrigenous material. In the South China Sea, total organic carbon is significantly (2000–3000 years) older owing to greater inputs of preaged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as seafloor morphology, shelf width, and sediment composition, may control the age of co‐occurring sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregates is a key process.

Url:
DOI: 10.1029/2004PA001103


Affiliations:


Links toward previous steps (curation, corpus...)


Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">An evaluation of 14C age relationships between co‐occurring foraminifera, alkenones, and total organic carbon in continental margin sediments</title>
<author>
<name sortKey="Mollenhauer, Gesine" sort="Mollenhauer, Gesine" uniqKey="Mollenhauer G" first="Gesine" last="Mollenhauer">Gesine Mollenhauer</name>
</author>
<author>
<name sortKey="Kienast, Markus" sort="Kienast, Markus" uniqKey="Kienast M" first="Markus" last="Kienast">Markus Kienast</name>
</author>
<author>
<name sortKey="Lamy, Frank" sort="Lamy, Frank" uniqKey="Lamy F" first="Frank" last="Lamy">Frank Lamy</name>
</author>
<author>
<name sortKey="Meggers, Helge" sort="Meggers, Helge" uniqKey="Meggers H" first="Helge" last="Meggers">Helge Meggers</name>
</author>
<author>
<name sortKey="Schneider, Ralph R" sort="Schneider, Ralph R" uniqKey="Schneider R" first="Ralph R." last="Schneider">Ralph R. Schneider</name>
</author>
<author>
<name sortKey="Hayes, John M" sort="Hayes, John M" uniqKey="Hayes J" first="John M." last="Hayes">John M. Hayes</name>
</author>
<author>
<name sortKey="Eglinton, Timothy I" sort="Eglinton, Timothy I" uniqKey="Eglinton T" first="Timothy I." last="Eglinton">Timothy I. Eglinton</name>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:4B69B731AF9D28789B7C23A37684BCC3A8C1D44A</idno>
<date when="2005" year="2005">2005</date>
<idno type="doi">10.1029/2004PA001103</idno>
<idno type="url">https://api.istex.fr/document/4B69B731AF9D28789B7C23A37684BCC3A8C1D44A/fulltext/pdf</idno>
<idno type="wicri:Area/Main/Corpus">000968</idno>
<idno type="wicri:Area/Main/Curation">000956</idno>
<idno type="wicri:Area/Main/Exploration">000794</idno>
<idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Exploration">000794</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">An evaluation of 14C age relationships between co‐occurring foraminifera, alkenones, and total organic carbon in continental margin sediments</title>
<author>
<name sortKey="Mollenhauer, Gesine" sort="Mollenhauer, Gesine" uniqKey="Mollenhauer G" first="Gesine" last="Mollenhauer">Gesine Mollenhauer</name>
<affiliation wicri:level="1">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Massachusetts, Woods Hole</wicri:regionArea>
<wicri:noRegion>Woods Hole</wicri:noRegion>
</affiliation>
<affiliation wicri:level="1">
<country wicri:rule="url">États-Unis</country>
</affiliation>
</author>
<author>
<name sortKey="Kienast, Markus" sort="Kienast, Markus" uniqKey="Kienast M" first="Markus" last="Kienast">Markus Kienast</name>
<affiliation wicri:level="2">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts</wicri:regionArea>
<placeName>
<region type="state">Massachusetts</region>
</placeName>
</affiliation>
<affiliation wicri:level="1">
<country xml:lang="fr">Canada</country>
<wicri:regionArea>Now at Department of Oceanography, Dalhousie University, Halifax, Nova Scotia</wicri:regionArea>
<wicri:noRegion>Nova Scotia</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Lamy, Frank" sort="Lamy, Frank" uniqKey="Lamy F" first="Frank" last="Lamy">Frank Lamy</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Allemagne</country>
<wicri:regionArea>GFZ‐Potsdam, Potsdam</wicri:regionArea>
<placeName>
<region type="land" nuts="2">Brandebourg</region>
<settlement type="city">Potsdam</settlement>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Meggers, Helge" sort="Meggers, Helge" uniqKey="Meggers H" first="Helge" last="Meggers">Helge Meggers</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Allemagne</country>
<wicri:regionArea>Fachbereich Geowissenschaften, Universität Bremen, Bremen</wicri:regionArea>
<placeName>
<region type="land" nuts="3">Brême (Land)</region>
<settlement type="city">Brême</settlement>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Schneider, Ralph R" sort="Schneider, Ralph R" uniqKey="Schneider R" first="Ralph R." last="Schneider">Ralph R. Schneider</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Allemagne</country>
<wicri:regionArea>Institut für Geowissenschaften, Christian‐Albrechts‐Universität zu Kiel, Kiel</wicri:regionArea>
<placeName>
<region type="land" nuts="2">Schleswig-Holstein</region>
<settlement type="city">Kiel</settlement>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Hayes, John M" sort="Hayes, John M" uniqKey="Hayes J" first="John M." last="Hayes">John M. Hayes</name>
<affiliation wicri:level="1">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>National Ocean Sciences Accelerator Mass Spectrometry Facility, McLean Laboratory, Woods Hole Oceanographic Institution, Massachusetts, Woods Hole</wicri:regionArea>
<wicri:noRegion>Woods Hole</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Eglinton, Timothy I" sort="Eglinton, Timothy I" uniqKey="Eglinton T" first="Timothy I." last="Eglinton">Timothy I. Eglinton</name>
<affiliation wicri:level="1">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Massachusetts, Woods Hole</wicri:regionArea>
<wicri:noRegion>Woods Hole</wicri:noRegion>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Paleoceanography</title>
<title level="j" type="abbrev">Paleoceanography</title>
<idno type="ISSN">0883-8305</idno>
<idno type="eISSN">1944-9186</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<date type="published" when="2005-03">2005-03</date>
<biblScope unit="volume">20</biblScope>
<biblScope unit="issue">1</biblScope>
<biblScope unit="page" from="n/a">n/a</biblScope>
<biblScope unit="page" to="n/a">n/a</biblScope>
</imprint>
<idno type="ISSN">0883-8305</idno>
</series>
<idno type="istex">4B69B731AF9D28789B7C23A37684BCC3A8C1D44A</idno>
<idno type="DOI">10.1029/2004PA001103</idno>
<idno type="ArticleID">2004PA001103</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">0883-8305</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass></textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract">Radiocarbon age relationships between co‐occurring planktic foraminifera, alkenones, and total organic carbon in sediments from the continental margins of southern Chile, northwest Africa, and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site‐specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000–4500 years older than co‐occurring foraminifera, alkenones were significantly (∼1000 years) older than co‐occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2σ error or better) in the NW African and South China Sea sediments. Total organic matter and alkenone ages were similar off Namibia (age difference TOC alkenones: 200–700 years), Chile (100–450 years), and NW Africa (360–770 years), suggesting minor contributions of preaged terrigenous material. In the South China Sea, total organic carbon is significantly (2000–3000 years) older owing to greater inputs of preaged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as seafloor morphology, shelf width, and sediment composition, may control the age of co‐occurring sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregates is a key process.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>Allemagne</li>
<li>Canada</li>
<li>États-Unis</li>
</country>
<region>
<li>Brandebourg</li>
<li>Brême (Land)</li>
<li>Massachusetts</li>
<li>Schleswig-Holstein</li>
</region>
<settlement>
<li>Brême</li>
<li>Kiel</li>
<li>Potsdam</li>
</settlement>
</list>
<tree>
<country name="États-Unis">
<noRegion>
<name sortKey="Mollenhauer, Gesine" sort="Mollenhauer, Gesine" uniqKey="Mollenhauer G" first="Gesine" last="Mollenhauer">Gesine Mollenhauer</name>
</noRegion>
<name sortKey="Eglinton, Timothy I" sort="Eglinton, Timothy I" uniqKey="Eglinton T" first="Timothy I." last="Eglinton">Timothy I. Eglinton</name>
<name sortKey="Hayes, John M" sort="Hayes, John M" uniqKey="Hayes J" first="John M." last="Hayes">John M. Hayes</name>
<name sortKey="Kienast, Markus" sort="Kienast, Markus" uniqKey="Kienast M" first="Markus" last="Kienast">Markus Kienast</name>
<name sortKey="Mollenhauer, Gesine" sort="Mollenhauer, Gesine" uniqKey="Mollenhauer G" first="Gesine" last="Mollenhauer">Gesine Mollenhauer</name>
</country>
<country name="Canada">
<noRegion>
<name sortKey="Kienast, Markus" sort="Kienast, Markus" uniqKey="Kienast M" first="Markus" last="Kienast">Markus Kienast</name>
</noRegion>
</country>
<country name="Allemagne">
<region name="Brandebourg">
<name sortKey="Lamy, Frank" sort="Lamy, Frank" uniqKey="Lamy F" first="Frank" last="Lamy">Frank Lamy</name>
</region>
<name sortKey="Meggers, Helge" sort="Meggers, Helge" uniqKey="Meggers H" first="Helge" last="Meggers">Helge Meggers</name>
<name sortKey="Schneider, Ralph R" sort="Schneider, Ralph R" uniqKey="Schneider R" first="Ralph R." last="Schneider">Ralph R. Schneider</name>
</country>
</tree>
</affiliations>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Musique/explor/SchutzV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000794 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 000794 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Musique
   |area=    SchutzV1
   |flux=    Main
   |étape=   Exploration
   |type=    RBID
   |clé=     ISTEX:4B69B731AF9D28789B7C23A37684BCC3A8C1D44A
   |texte=   An evaluation of 14C age relationships between co‐occurring foraminifera, alkenones, and total organic carbon in continental margin sediments
}}

Wicri

This area was generated with Dilib version V0.6.38.
Data generation: Mon Feb 8 17:34:10 2021. Site generation: Mon Feb 8 17:41:23 2021