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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
by
Tomomichi Tatsuyama
, Shotaro Takano
, Kohei Matsuoka
, Yoshiki Sohrin
in
anthropogenic pollution
/ General. Including nature conservation, geographical distribution
/ GEOTRACES
/ isotopic composition
/ molybdenum
/ Q
/ QH1-199.5
/ Science
/ tungsten
2023
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Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
by
Tomomichi Tatsuyama
, Shotaro Takano
, Kohei Matsuoka
, Yoshiki Sohrin
in
anthropogenic pollution
/ General. Including nature conservation, geographical distribution
/ GEOTRACES
/ isotopic composition
/ molybdenum
/ Q
/ QH1-199.5
/ Science
/ tungsten
2023
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Do you wish to request the book?
Distribution of stable isotopes of Mo and W from a river to the ocean: signatures of anthropogenic pollution
by
Tomomichi Tatsuyama
, Shotaro Takano
, Kohei Matsuoka
, Yoshiki Sohrin
in
anthropogenic pollution
/ General. Including nature conservation, geographical distribution
/ GEOTRACES
/ isotopic composition
/ molybdenum
/ Q
/ QH1-199.5
/ Science
/ tungsten
2023
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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.
Publisher
Frontiers Media SA,Frontiers Media S.A
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