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Bioaccumulation and changes of trace metals over the last two decades in marine organisms from Guangdong coastal regions, South China

机译:中国南方广东沿海地区海洋生物在过去二十年中的生物累积和痕量金属变化

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摘要

Trace metal (Cr, Ni, Cu, Zn, Cd and Pb) exposures, distribution and bioaccumulation were investigated in marine organisms from Guangdong coastal regions, South China. The results showed that all of the selected metals were observed in marine organisms with a predomination of Cu and Zn. The metal exposure levels exhibited obvious variations between species with the decreasing order of crab>shellfish>shrimp>fish. The higher metals enrichment seen in shellfish and crab species primarily attributed to their living habits and the higher sediment background values of trace metals. Endpoint bioaccumulation factor (BAF_(fd)) was used to characterize the bioaccumulation potentials of marine organisms to trace metals, of which Cu and Zn were the most accumulated elements. The exposure of trace metals in the cultured organisms was far lower than those in wild marine organisms, which is probably due to the effect of growth dilution. Comparisons with previous studies demonstrated that the concentration profiles of most trace metals declined over the last one to two decades, except Cu, that increased indistinctively.
机译:追踪金属(Cr,Ni,Cu,Zn,Cd和Pb)在南方广东沿海地区海洋生物中研究了曝光,分布和生物累积。结果表明,在海洋生物中观察到所有选定金属,其具有Cu和Zn的占地性。金属曝光水平在螃蟹>贝类>虾>鱼的下降顺序呈现出明显的变化。在贝类和蟹类中看到的较高金属富集主要归因于他们的生活习惯和痕量金属的沉积物背景值。终点生物积累因子(BAF_(FD))用于表征痕量金属的海洋生物的生物积累电位,其中Cu和Zn是最累计的元素。培养的生物中的痕量金属暴露远低于野生海洋生物中的金属,这可能是由于生长稀释的影响。与先前研究的比较表明,除Cu之外,大多数痕量金属的浓度剖面下降到最后一到二十年,模糊不清。

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  • 来源
    《Oceanographic Literature Review》 |2020年第9期|1996-1996|共1页
  • 作者

    L. Zhang; W. Yan; Z. Xie;

  • 作者单位

    Key Laboratory of Ocean and Marginal Sea Geology South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou 510301 China;

    Key Laboratory of Ocean and Marginal Sea Geology South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou 510301 China;

    Key Laboratory of Ocean and Marginal Sea Geology South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou 510301 China;

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