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 even after the source has ceased to pollute. 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 calcite tests, which facilitates monitoring of anthropogenic footprints on recent and past
environmental systems. The aim of this study was to investigate whether the incorporation of heavy metals into 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 nearshore foraminiferal species Ammonia aomoriensis, Ammonia batava and
Elphidium excavatum. Seawater analyses revealed increasing concentrations for most metals between culturing phases and high metal
concentrations in the beginning of the culturing phases due to sudden metal addition. Furthermore, a loss of metals during the culturing
process was discovered by an offset between the added and the actual concentrations of the metals in seawater. Laser ablation ICP-MS (inductively
coupled plasma mass spectrometry) analysis of
the newly formed calcite revealed species-specific differences in the incorporation of heavy metals. The foraminiferal calcite of all three species
exhibited Pb and Ag concentrations strongly correlated with concentrations in the seawater culturing medium (partition coefficients and standard
deviation for Ag – Ammonia aomoriensis, 0.50 ± 0.02; Ammonia batava, 0.17 ± 0.01; Elphidium excavatum, 0.47 ± 0.04; for Pb – Ammonia aomoriensis, 0.39 ± 0.01; Ammonia batava, 0.52 ± 0.01;
Elphidium excavatum, 0.91 ± 0.01). 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. However, Zn, Sn and Cd showed no clear trend for the species
studied, which in the case of Sn was maybe caused by the lack of variation in the seawater Sn concentration. The calibrations and the calculated
partition coefficients render A. aomoriensis, A. batava and E. excavatum as natural archives that enable the
determination of variations in some heavy metal concentrations in seawater in polluted and pristine environments.