R. Pongratz et Kg. Heumann, PRODUCTION OF METHYLATED MERCURY AND LEAD BY POLAR MACROALGAE - A SIGNIFICANT NATURAL SOURCE FOR ATMOSPHERIC HEAVY-METALS IN CLEAN ROOM COMPARTMENTS, Chemosphere, 36(9), 1998, pp. 1935-1946
During August and September 1995 samples of different species of macro
algae were collected from the Kongsfjord on Spitsbergen. These macroal
gae were cultivated in incubation vessels under polar conditions and t
he releasing rates of methylated heavy metal compounds for mercury, le
ad and cadmium were determined. The analysis of monomethyl and dimethy
l mercury was carried out by a gas chromatographic system with atomic
fluorescence detection after conversion of monomethyl mercury into the
volatile methylethyl mercury compound. A differential pulse anodic st
ripping voltammetric method was used for the determination of trimethy
l lead and monomethyl cadmium, respectively. The different species of
macroalgae showed distinct differences in the releasing rate of the va
rious methylated heavy metals. Laminaria saccharina, for example, was
found to produce monomethyl mercury, dimethyl mercury and trimethyl le
ad but no monomethyl cadmium. Fucus distichus released only the two me
thylated mercury compounds, whereas Desmarestia aculeata showed only p
roduction of dimethyl mercury. The releasing rates of ten different ty
pes of macroalgae were determined to be in the range of up to 13 pg fo
r methylated mercury and of up to 110 pg for trimethyl lead per gram o
f wet alga and day by allowing incubation times of 1-5 days. Because p
ermethylated heavy metal compounds show high volatility as well as low
solubility in ocean water, they are easily emitted into the atmospher
e. It therefore follows from the results of this work that macroalgae
can significantly contribute to the atmospheric heavy metal content, e
specially of mercury by the production of dimethyl mercury, in the cle
an room compartments of the polar regions. Methylated compounds have b
een found in the ocean, up until now, for the heavy metals mercury [1,
2], lead [3] and cadmium [4]. It is widely accepted today that the for
mation of these alkylated heavy metal compounds is carried out by biom
ethylation in the ocean but there is little evidence for the formation
of others than methylated derivatives [5]. Various biological species
are capable to carry out the methylation of heavy metals. This was sh
own for mercury and lead in different model experiments with bacteria
and fungi [6-10]. Comparable biomethylation experiments of lead with m
arine phytoplankton and marine macroalgae were successfully as well [1
1]. However, only little is known about the question which biological
species produces what type of methylated heavy metal compound and whet
her there exist characteristic fingerprints for the different biologic
al species or not. In addition, there is a lack of knowledge about the
formation of methylated heavy metals in the polar oceans even if thes
e remote areas, with their relatively high biological activity, should
substantially contribute to the global natural sources of these envir
onmentally important compounds. Because of their volatility these natu
ral methylated compounds are substantially responsible for distinct le
vels of some heavy metals in the atmosphere.