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• W2806334646 abstract "Several years have passed since the global phase-out of leaded petrol use. Nonetheless, emissions from anthropogenic activities remain the principal source of Pb to the oceans. The distribution of elemental Pb and its stable isotopes throughout the surface ocean provide information on the source and transport of these anthropogenic inputs. This study presents dissolved Pb concentrations and isotopic distributions from 110 surface water samples collected during the Malaspina 2010 Circumnavigation Expedition. Dissolved Pb concentrations ranged from 10 pM to 49 pM across the sampling stations covering all major ocean basins. The highest concentrations were found in the northeast Atlantic Ocean and the lowest in both the south Pacific and south Atlantic Oceans. Lead concentrations measured in the north Pacific Ocean, near Hawaii, were compared to previously published data from the same region. That comparison showed that Pb concentration has decreased ∼40% since 1975, although the rate of decrease has slowed in the past two decades. The overall decline in concentration probably has been induced by the cessation of leaded gasoline use in North America. The temporal evolution of stable Pb isotopes in this region shows a shift from dominant North American-like composition in 1979 towards a more Asian-like composition in later years. More widely, the distribution of Pb and Pb isotopes measured in the Malaspina sample set of global surface waters were compared with previously published ratios of aerosols and other atmosphere-derived Pb sources from the countries surrounding the different ocean basins. This comparison identified the potential Pb sources to each ocean basin, providing new insights into the transport and fate of Pb in the oceans." @default.
• W2806334646 created "2018-06-13" @default.
• W2806334646 creator A5019240865 @default.
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• W2806334646 date "2018-08-01" @default.
• W2806334646 modified "2023-10-14" @default.
• W2806334646 title "Concentration and isotopic composition of dissolved Pb in surface waters of the modern global ocean" @default.
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• W2806334646 cites W1965030183 @default.
• W2806334646 cites W1966308660 @default.
• W2806334646 cites W1969695631 @default.
• W2806334646 cites W1971192624 @default.
• W2806334646 cites W1973829035 @default.
• W2806334646 cites W1974796647 @default.
• W2806334646 cites W1976264753 @default.
• W2806334646 cites W1979178509 @default.
• W2806334646 cites W1982030560 @default.
• W2806334646 cites W1982793692 @default.
• W2806334646 cites W1986019151 @default.
• W2806334646 cites W1989636461 @default.
• W2806334646 cites W1990949119 @default.
• W2806334646 cites W1991831222 @default.
• W2806334646 cites W1994982326 @default.
• W2806334646 cites W1998425346 @default.
• W2806334646 cites W2003435695 @default.
• W2806334646 cites W2003710799 @default.
• W2806334646 cites W2003930708 @default.
• W2806334646 cites W2006886699 @default.
• W2806334646 cites W2007069126 @default.
• W2806334646 cites W2008722041 @default.
• W2806334646 cites W2009735920 @default.
• W2806334646 cites W2011069939 @default.
• W2806334646 cites W2011644871 @default.
• W2806334646 cites W2013900698 @default.
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• W2806334646 cites W2017056529 @default.
• W2806334646 cites W2017846612 @default.
• W2806334646 cites W2019416918 @default.
• W2806334646 cites W2023567030 @default.
• W2806334646 cites W2026704984 @default.
• W2806334646 cites W2027284940 @default.
• W2806334646 cites W2028589037 @default.
• W2806334646 cites W2029763967 @default.
• W2806334646 cites W2032471523 @default.
• W2806334646 cites W2032623834 @default.
• W2806334646 cites W2039100744 @default.
• W2806334646 cites W2041247686 @default.
• W2806334646 cites W2044928088 @default.
• W2806334646 cites W2046560001 @default.
• W2806334646 cites W2047906450 @default.
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• W2806334646 cites W2056975406 @default.
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• W2806334646 cites W2100820351 @default.
• W2806334646 cites W2116322844 @default.
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• W2806334646 doi "https://doi.org/10.1016/j.gca.2018.05.005" @default.
• W2806334646 hasPublicationYear "2018" @default.
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