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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution

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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
Journal Article

Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution

2023
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Overview
Molybdenum and tungsten are redox-sensitive elements, and their stable isotope ratios have attracted attention as paleoceanographic proxies. However, our knowledge of the distribution of stable Mo and W isotopes in the modern hydrosphere remains limited. In this study, we provided the concentrations and isotope ratios of dissolved Mo and W in the oceans (the North Pacific and Indian Oceans), marginal seas (the East China Sea and Sea of Japan), and a river-estuary system in Japan (from the Uji-Yodo rivers to Osaka Bay). In the North Pacific and Indian Oceans, the W concentration was 48.2 ± 6.2 pmol/kg (ave ± 2sd, n = 109), δ 186/184 W was 0.52 ± 0.06 ‰, the Mo concentration was 105.1 ± 8.0 nmol/kg, and δ 98/95 Mo was 2.40 ± 0.06 ‰. The results indicate that W has the constant concentration and isotopic composition in the modern ocean as well as Mo. In the East China Sea and the Sea of Japan, the W concentration and δ 186/184 W in the upper water (< 1000 m depth) were different from those in the ocean (W = 56 ± 18 pmol/kg, δ 186/184 W = 0.45 ± 0.06 ‰, n = 24). However, the concentrations in deeper water were congruent with those in the oceans (W = 49.9 ± 7.6 pmol/kg, δ 186/184 W = 0.50 ± 0.02 ‰, n = 7). The Mo concentration was 105.4 ± 3.1 nmol/kg and δ 98/95 Mo was 2.36 ± 0.03 ‰ ( n = 31) throughout the water column, congruent with those in the ocean. In the Uji River-Yodo River-Osaka Bay system, the W concentration reached 1074 pmol/kg and δ 186/184 W reached 0.20 ‰. We propose that the enrichment of W with a low δ 186/184 W in the river-estuary system and marginal seas is caused by anthropogenic pollution. Anthropogenic Mo pollution was not detected in marginal seas. However, the Mo concentration and δ 98/95 Mo showed high anomalies above the mixing line of river water and seawater in the lower Yodo River and Osaka Bay, implying possible anthropogenic pollution of Mo in the metropolitan area.