Owing to the high toxicity of cadmium (Cd) towards biota and the considerable
quantities of this element entering the environment from anthropogenic sources,
interest in its biogeochemistry is increasing. This is also true for the marine
environment, which serves as a sink for both natural and anthropogenic Cd
loads entering the hydrosphere and the atmosphere. The distribution of Cd in
the coastal zone of the marine environment is governed primarily by the flux of the so-called fluffy layer suspended matter (FLSM), which spreads across the top
of the sea floor as a several-centimetre-thick layer containing highly concentrated
suspended matter.
Both total contents and solid speciation of Cd was measured in FLSM collected
in the Pomeranian Bay – Arkona Deep system (Western Baltic Proper) in the course
of the three-year-long study.
Seasonal changes in the total Cd content (0.5–1.8 μg g−1 dry matter) were
attributed to the contribution of organic suspensions originating from algal blooms.
The decreasing content of Cd in FLSM offshore is due to the input of Cd-rich
suspended matter from the River Odra (Oder), and the decreasing organic matter
content in FLSM with increasing depth. The contribution of labile fractions
(adsorbed and bound to iron(III) hydroxides) was found to be from 50 to 75%
of the total content. In view of the substantial mobility and bioavailability of the
fractions, this is a highly alarming feature.
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