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Effects of metal speciation on growth of phytoplankton with special reference to iron
Authors:H. De Haan
Affiliation:(1) Present address: Tjeukemeer Laboratory, Limnological Institute, 8536 VD Oosterzee, The Netherlands
Abstract:This paper is a compilation of studies concerning the effects of metal speciation on the growth of phytoplankton. Special attention is paid to the speciation and availability of iron in lake Tjeukemeer, The Netherlands. Under laboratory conditions the free ionic metal species generally appear to be most effective in determining metal availability and toxicity. A variety of factors controlling solubility, ion-exchange, complexation or chelation, sorption and electrostatical attraction of metal ions affect the metal speciation, mostly resulting in reduced availabilities. However, some organic metal chelates such as citrates, nitrillotriacetates and the specifically iron chelating siderophores, are sometimes more available than the corresponding free ions. The presence of other metals also influences the availability of a given metal by competing for the same binding sites on the algal cell. This competition leads to antagonism betweene.g. iron nutrition and cadmium toxicity in marine diatoms. In the eutrophic, alkaline, hard and humic lake Tjeukemeer, the free Fe3+ concentration is below measurable levels and does not match the iron requirement of the phytoplankton. So most of the algal iron must have been provided by the predominant inorganic iron colloids and particles bye.g. dissolution or photo-degradation (reduction). If the provision rates of available iron are slow in relation to that of iron uptake, the growth of some phytoplankton species may become iron-limited. Continuous culture work indicated that the iron fraction <0.2 mgrm from Tjeukemeer,i.e., the lsquosolublersquo fraction, is about one third as much available as iron from NH4Fe(SO4)2.12H2O. Different phytoplankton species vary widely in their metal requirements and tolerances. Therefore, metal speciation and availability may affect species composition and succession within phytoplankton communities. So far the assessment of metal availability in natural waters has been complicated by the complex metal chemistry and by methodological limits.
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