期刊
LIMNOLOGY AND OCEANOGRAPHY-METHODS
卷 10, 期 -, 页码 653-665出版社
WILEY-BLACKWELL
DOI: 10.4319/lom.2012.10.653
关键词
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资金
- National Science Foundation [OCE-0751409]
- Kuwait Foundation for the Advancement of Science (KFAS)
- Singapore-MIT Alliance for Research and Technology (SMART)
- U.S. National Science Foundation [OCE-0927285]
- NERC [NE/H005390/1, NE/G008973/1] Funding Source: UKRI
- Natural Environment Research Council [NE/G008973/1, NE/H005390/1] Funding Source: researchfish
- Directorate For Geosciences [1234213, 0751681] Funding Source: National Science Foundation
- Division Of Ocean Sciences [1234213, 0751681] Funding Source: National Science Foundation
- Division Of Ocean Sciences
- Directorate For Geosciences [0926197] Funding Source: National Science Foundation
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.
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