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      High-density element concentrations in fish from subtidal to hadal zones of the Pacific Ocean

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          Abstract

          Anthropogenic use of high density, toxic elements results in marine pollution which is bio-accumulating throughout marine food webs. While there have been several studies in various locations analyzing such elements in fish, few have investigated patterns in these elements and their isotopes in terms of ocean depth, and none have studied the greatest depth zones. We used a flame atomic absorption spectrophotometer-hydride system and an inductively coupled plasma-mass spectrometer to determine concentrations of the high-density elements arsenic (As), cadmium (Cd), chromium (Cr), cobalt (Co), copper (Cu), lead (Pb), mercury (Hg), nickel (Ni), selenium (Se), plus the light-metal barium (Ba), in fish ranging from bathyal (1000 m in Monterey Bay) to upper hadal zones (6500–7626 m in the Kermadec and Mariana Trenches) in the Pacific Ocean. Five species of fish—including the Mariana Trench snailfish, the world's deepest known fish newly discovered—were analyzed for patterns in total element concentration, depth of occurrence, Se:Hg ratio, plus mercury isotopes in the deepest species. Co and As levels decreased with depth. In the Mariana Trench, Pb, Hg, Cd, and Cu were higher than in all other samples, and higher in those plus Ba than in the Kermadec Trench. The latter samples had far higher Ni and Cr levels than all others. Mercury relative isotope analysis showed no depth trends in the deepest species. Se:Hg showed a large molar excess of Se in bathyal flatfish species. These patterns indicate that exposures to pollutants differ greatly between habitats including trenches of similar depths.

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          Mass-dependent and -independent fractionation of hg isotopes by photoreduction in aquatic systems.

          Mercury (Hg) isotopes can be used as tracers of Hg biogeochemical pathways in the environment. The photochemical reduction of aqueous Hg species by natural sunlight leads to both mass-dependent fractionation (MDF) of Hg isotopes and mass-independent fractionation (MIF) of the odd-mass isotopes, with the relation between the MIF for the two odd isotopes being distinct for different photoreduction pathways. Large variations in MDF and MIF are observed in fish and provide new insights into the sources and bioaccumulation of Hg in food webs. MIF in fish can also be used to estimate the loss of methylmercury via photoreduction in aquatic ecosystems.
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            Marine biogeochemical cycling of mercury.

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              Precise and accurate isotopic measurements using multiple-collector ICPMS

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                Author and article information

                Contributors
                Journal
                Heliyon
                Heliyon
                Heliyon
                Elsevier
                2405-8440
                09 October 2018
                October 2018
                09 October 2018
                : 4
                : 10
                : e00840
                Affiliations
                [a ]Whitman College Chemistry Dept., Walla Walla, WA, 99362, USA
                [b ]Whitman College Biology Dept., Walla Walla, WA, 99362, USA
                Author notes
                []Corresponding author. yancey@ 123456whitman.edu
                Article
                S2405-8440(18)34276-2 e00840
                10.1016/j.heliyon.2018.e00840
                6180415
                7197a0a1-1381-4235-b39f-117406655288
                © 2018 The Authors

                This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

                History
                : 23 August 2018
                : 27 September 2018
                : 28 September 2018
                Categories
                Article

                environmental science,geochemistry,oceanography,earth sciences,biogeoscience

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