M. Kerner et Cd. Geisler, DYNAMICS OF CU RELEASE DURING EARLY AEROBIC DEGRADATION IN AGGREGATEDSESTON FROM THE ELBE ESTUARY, Marine chemistry, 51(2), 1995, pp. 133-144
Using a new laboratory device, the mobilization of Cu, Cd, and Pb was
monitored continuously by analysing the water overlying and underlying
a approximate to 1 mm seston layer using voltammetric methods. The mi
neralization of organic matter was quantified by the heterotrophic oxy
gen consumption. The CO2 formed was analysed for its C-13-content to c
haracterize the organic C-pool used in degradation. Changes in the bio
chemical composition of the particulate material were determined at th
e beginning and end of an aerobic incubation period. Heterotrophic pro
cesses were initiated about 20 h after settling of the seston. The agg
regated seston became refractory for aerobic microbial degradation aft
er about 120 h of aerobic incubation. At this stage nitrification agai
n balanced the total oxygen consumption. The mineralization of the org
anic matter was between 7.7 and 17.4% of the total and 62-75% of this
consisted of dying algal biomass. A significant release of Cu from the
seston layer was restricted to a period of about 40 h and was correla
ted to the period when a limitation of heterotrophic processes by orga
nic substrates occurred. Then, Cu concentrations increased to between
8 and 28 nM in the water overlying the layer that equalled a mobilizat
ion rate of between 0.24 and 0.94 (nmol/cm(2) d). Cd and Pb did not sh
ow a similar pattern and were detected at concentrations of always bel
ow 2 nM. Deeper parts of the layer functioned as a sink for Cu at oxyg
en concentrations of less than or equal to 25 mu M and concentrations
of Cu in the water underlying the seston layer remained below 1.5 nM.
During periods of short-term release Cu in solution accounted for betw
een 3 and 10% of the total particulate Cu. The results suggest that a
significant amount of the Cu within the seston material was retained i
n the protein fraction of the algal matter and is released into the ov
erlying water during its aerobic degradation.