A lack
of knowledge on metal speciation in the microenvironment
surrounding phytoplankton cells (i.e., the phycosphere) represents
an impediment to accurately predicting metal bioavailability. Phycosphere
pH and O
2
concentrations from a diversity of algae species
were compiled. For marine algae in the light, the average increases
were 0.32 pH units and 0.17 mM O
2
in the phycosphere, whereas
in the dark the average decreases were 0.10 pH units and 0.03 mM O
2
, in comparison to bulk seawater. In freshwater algae, the
phycosphere pH increased by 1.28 units, whereas O
2
increased
by 0.38 mM in the light. Equilibrium modeling showed that the pH alteration
influenced the chemical species distribution (i.e., free ion, inorganic
complexes, and organic complexes) of Al, Cd, Co, Cu, Fe, Hg, Mn, Ni,
Pb, Sc, Sm, and Zn in the phycosphere, and the O
2
fluctuation
increased oxidation rates of Cu(I), Fe(II) and Mn(II) from 2 to 938-fold.
The pH/O
2
-induced changes in phycosphere metal chemistry
were larger for freshwater algae than for marine species. Reanalyses
of algal metal uptake data in the literature showed that uptake of
the trivalent metals (Sc, Sm and Fe), in addition to divalent metals,
can be better predicted after considering the phycosphere chemistry.