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Quantifying mercury isotope dynamics in captive Pacific bluefin tuna ( Thunnus orientalis )

Datos Bibliográficos

ID19568968
AutoresSae Yun Kwon (0000-0001-8665-0327, University of Michigan), Joel D Blum (0000-0001-5389-8633, University of Michigan), Daniel J Madigan (0000-0002-9937-1818, Harvard University Press), Barbara A Block (0000-0001-5181-3616), Brian N Popp (0000-0001-7021-5478, University of Hawaii System)
EditoresJody W Deming, Tamar Barkay (0000-0001-9380-2405)
Año2016
Volumen4
Fecha de publicación2016-01-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaElementa Science of the Anthropocene (JOURNAL)
Identificadores de la revistaISSN: 2325-1026 • E-ISSN: 2325-1026
EditorialUniversity of California Press (PUBLISHER • US)
DOI10.12952/journal.elementa.000088
OpenAlexW2253042628
IdiomaEN
Referencias citadas78

Analyses of mercury (Hg) isotope ratios in fish tissues are used increasingly to infer sources and biogeochemical processes of Hg in natural aquatic ecosystems. Controlled experiments that can couple internal Hg isotope behavior with traditional isotope tracers (δ13C, δ15N) can improve the applicability of Hg isotopes as natural ecological tracers. In this study, we investigated changes in Hg isotope ratios (δ202Hg, Δ199Hg) during bioaccumulation of natural diets in the pelagic Pacific bluefin tuna (Thunnus orientalis; PBFT). Juvenile PBFT were fed a mixture of natural prey and a dietary supplement (60% Loligo opalescens, 31% Sardinops sagax, 9% gel supplement) in captivity for 2914 days, and white muscle tissues were analyzed for Hg isotope ratios and compared to time in captivity and internal turnover of δ13C and δ15N. PBFT muscle tissues equilibrated to Hg isotope ratios of the dietary mixture within ∼700 days, after which we observed a cessation in further shifts in Δ199Hg, and small but significant negative δ202Hg shifts from the dietary mixture. The internal behavior of Δ199Hg is consistent with previous fish studies, which showed an absence of Δ199Hg fractionation during Hg bioaccumulation. The negative δ202Hg shifts can be attributed to either preferential excretion of Hg with higher δ202Hg values or individual variability in captive PBFT feeding preferences and/or consumption rates. The overall internal behavior of Hg isotopes is similar to that described for δ13C and δ15N, though observed Hg turnover was slower compared to carbon and nitrogen. This improved understanding of internal dynamics of Hg isotopes in relation to δ13C and δ15N enhances the applicability of Hg isotope ratios in fish tissues for tracing Hg sources in natural ecosystems

Bioaccumulation · Biology · Fish · Fishery · Fractionation · Isotope · Isotope analysis · Isotope fractionation · Isotopes of nitrogen · Pelagic zone · Stable isotope ratio · Tuna · Yellowfin tuna · Zoology · δ13C · δ15N · Chemistry · Isotope Analysis in Ecology · Marine animal studies overview · Mercury impact and mitigation studies · Ecology · Environmental Chemistry

  • Fractionation and turnover of stable carbon isotopes in animal tissues

    Open Access•Larry L Tieszen, Thomas W Boutton et al.•Oecologia•1983

  • Methylmercury Exposure and Health Effects in Humans

    Donna Mergler, H Allen Anderson et al.•AMBIO•2007

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