Heavy metal uptake of near-shore benthic foraminifera during multi-metal culturing experiments

Sarina Schmidt, E. Hathorne, J. Schönfeld, D. Garbe‐Schönberg
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引用次数: 1

Abstract

Abstract. Heavy metal pollution originating from anthropogenic sources, e.g., mining, industry and extensive land use, is increasing in many parts of the world and influences coastal marine environments for a long time. The elevated input of heavy metals into the marine system potentially affects the biota because of their toxicity, persistence and bioaccumulation. An emerging tool for environmental applications is the heavy metal incorporation into foraminiferal tests calcite, which facilitates monitoring of anthropogenic footprints on recent and past environmental systems. The aim of this study is to investigate whether the incorporation of heavy metals in foraminifera is a direct function of their concentration in seawater. Culturing experiments with a mixture of dissolved chromium (Cr), manganese (Mn), nickel (Ni), copper (Cu), zinc (Zn), silver (Ag), cadmium (Cd), tin (Sn), mercury (Hg) and lead (Pb) in artificial seawater were carried out over a wide concentration range to assess the uptake of heavy metals by the near-shore foraminiferal species Ammonia aomoriensis, Ammonia batava and Elphidium excavatum. Seawater analysis exhibited the increasing metal concentrations between culturing phases and revealed high metal concentrations in the beginning of the culturing phases due to the punctual metal addition. Furthermore, a loss of metals during the culturing process was discovered, which lead to a deviation between the expected and the actual concentrations of the metals in seawater. Laser ablation ICP-MS analysis of the newly formed calcite revealed species-specific differences in the incorporation of heavy metals. The foraminiferal calcite of all three species reveals a strong positive correlation with Pb and Ag concentrations in the culturing medium. Ammonia aomoriensis further showed a correlation with Mn and Cu, A. batava with Mn and Hg and E. excavatum with Cr and Ni, and partially also with Hg. Zn, Sn and Cd showed no clear trend for the species studied, which may be caused by the little variation of these metals in seawater. Our calibrations and the calculated partition coefficients render A. aomoriensis, A. batava and E. excavatum as natural archives that enable the direct quantification of metals in polluted and pristine environments. This in turn allows monitoring of the ecosystem status of areas that are potentially under the threat of anthropogenic pollution in order to evaluate contemporary emission reduction measures.
近海底栖有孔虫在多金属培养实验中对重金属的吸收
摘要来自采矿、工业和广泛土地利用等人为来源的重金属污染在世界许多地区日益严重,并长期影响沿海海洋环境。由于重金属的毒性、持久性和生物累积性,海洋系统中重金属输入量的增加可能会对生物群产生影响。一种新兴的环境应用工具是将重金属掺入有孔虫测试方解石中,这有助于监测最近和过去环境系统中的人为足迹。本研究的目的是调查有孔虫体内重金属的掺入是否是其在海水中浓度的直接函数。利用人工海水中溶解的铬(Cr)、锰(Mn)、镍(Ni)、铜(Cu)、锌(Zn)、银(Ag)、镉(Cd)、锡(Sn)、汞(Hg)和铅(Pb)的混合物在宽浓度范围内进行了培养实验,以评估近海有孔虫物种奥氏氨虫(Ammonia aomoriensis)、巴塔瓦氨虫(Ammonia batava)和深水藻(Elphidium excavatum)对重金属的吸收。海水分析显示培养阶段之间的金属浓度增加,并且由于准时添加金属,在培养阶段开始时显示出高金属浓度。此外,在培养过程中发现了金属的损失,这导致海水中金属的预期浓度和实际浓度之间的偏差。对新形成的方解石进行的激光烧蚀ICP-MS分析揭示了重金属掺入方面的物种特异性差异。三种有孔虫的方解石均与培养基中Pb和Ag的浓度呈正相关。aomoriensis Ammonia进一步显示出与Mn和Cu的相关性,a.batava与Mn和Hg的相关性,E.excavatum与Cr和Ni的相关性,部分也与Hg的相关性。Zn、Sn和Cd在所研究的物种中没有表现出明显的趋势,这可能是由于这些金属在海水中的变化很小所致。我们的校准和计算的分配系数使A.aomoriensis、A.batava和E.excavatum成为自然档案,能够直接量化污染和原始环境中的金属。这反过来又允许监测可能受到人为污染威胁的地区的生态系统状况,以评估当代的减排措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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