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GEOTRACES IC1 (BATS) contamination‐prone trace element isotopes Cd, Fe, Pb, Zn, Cu, and Mo intercalibration

Identifieur interne : 005675 ( Main/Exploration ); précédent : 005674; suivant : 005676

GEOTRACES IC1 (BATS) contamination‐prone trace element isotopes Cd, Fe, Pb, Zn, Cu, and Mo intercalibration

Auteurs : Edward A. Boyle [États-Unis] ; Seth John [États-Unis] ; Wafa Abouchami [Allemagne] ; Jess F. Adkins [États-Unis] ; Yolanda Echegoyen-Sanz [États-Unis] ; Michael Ellwood [Australie] ; A. Russell Flegal [États-Unis] ; Kyrstin Fornace [États-Unis] ; Celine Gallon [États-Unis] ; Steve Galer [Allemagne] ; Melanie Gault-Ringold [Nouvelle-Zélande] ; Francois Lacan [France] ; Amandine Radic [France] ; Mark Rehkamper [Royaume-Uni] ; Olivier Rouxel [États-Unis, France] ; Yoshiki Sohrin [Japon] ; Claudine Stirling [Nouvelle-Zélande] ; Claire Thompson [Australie] ; Derek Vance [Royaume-Uni] ; Zichen Xue [Royaume-Uni] ; Ye Zhao [Royaume-Uni]

Source :

RBID : ISTEX:03F1DBB3DFC74C07C10FC6FE47E09DDA9303603D

Descripteurs français

English descriptors

Abstract

We report data on the isotopic composition of cadmium, copper, iron, lead, zinc, and molybdenum at the GEOTRACES IC1 BATS Atlantic intercalibration station. In general, the between lab and within‐lab precisions are adequate to resolve global gradients and vertical gradients at this station for Cd, Fe, Pb, and Zn. Cd and Zn isotopes show clear variations in the upper water column and more subtle variations in the deep water; these variations are attributable, in part, to progressive mass fractionation of isotopes by Rayleigh distillation from biogenic uptake and/or adsorption. Fe isotope variability is attributed to heavier crustal dust and hydrothermal sources and light Fe from reducing sediments. Pb isotope variability results from temporal changes in anthropogenic source isotopic compositions and the relative contributions of U.S. and European Pb sources. Cu and Mo isotope variability is more subtle and close to analytical precision. Although the present situation is adequate for proceeding with GEOTRACES, it should be possible to improve the within‐lab and between‐lab precisions for some of these properties.

Url:
DOI: 10.4319/lom.2012.10.653


Affiliations:


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Le document en format XML

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<div type="abstract">We report data on the isotopic composition of cadmium, copper, iron, lead, zinc, and molybdenum at the GEOTRACES IC1 BATS Atlantic intercalibration station. In general, the between lab and within‐lab precisions are adequate to resolve global gradients and vertical gradients at this station for Cd, Fe, Pb, and Zn. Cd and Zn isotopes show clear variations in the upper water column and more subtle variations in the deep water; these variations are attributable, in part, to progressive mass fractionation of isotopes by Rayleigh distillation from biogenic uptake and/or adsorption. Fe isotope variability is attributed to heavier crustal dust and hydrothermal sources and light Fe from reducing sediments. Pb isotope variability results from temporal changes in anthropogenic source isotopic compositions and the relative contributions of U.S. and European Pb sources. Cu and Mo isotope variability is more subtle and close to analytical precision. Although the present situation is adequate for proceeding with GEOTRACES, it should be possible to improve the within‐lab and between‐lab precisions for some of these properties.</div>
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<li>Kyoto</li>
<li>Toulouse</li>
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<name sortKey="Zhao, Ye" sort="Zhao, Ye" uniqKey="Zhao Y" first="Ye" last="Zhao">Ye Zhao</name>
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<country name="Japon">
<region name="Région du Kansai">
<name sortKey="Sohrin, Yoshiki" sort="Sohrin, Yoshiki" uniqKey="Sohrin Y" first="Yoshiki" last="Sohrin">Yoshiki Sohrin</name>
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</country>
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