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Role of biologically-mediated boundary reactions in the bioavailability of Cd to freshwater phytoplankton.

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Exposure time (min) 0 20 40 60 Int rac el lul ar C d (m ol  m -2 ) 0.0 1.0e-21 2.0e-21 3.0e-21 4.0e-21

0.1 nM Cd2+ (NTA) + SOD & Catalase 0.1 nM Cd2+ (Cys) + SOD & Catalase

Exposure time (min)

0 20 40 60 Int rac el lul ar C d (m o l m -2 ) 0 2e-21 4e-21 6e-21 8e-21 1e-20 0.1 nM Cd2+ (NTA) 0.1 nM Cd2+ (Cys)

Role of biologically-mediated boundary reactions in the bioavailability of Cd to freshwater phytoplankton

Fengjie Liu (E-mail: Fengjie.Liu@ete.inrs.ca), Claude Fortin and Peter G.C. Campbell

Institut national de la Recherche scientifique, Centre Eau Terre Environnement (INRS-ETE), Québec, Canada

Abstract

We show that at a given constant free Cd2+ concentration in

ambient well-buffered water, the bioavailability of dissolved Cd decreased or increased due to biologically-mediated

chemical changes in the boundary layer of planktonic cells under different physiological conditions. For instance,

decreased Cd bioavailability can result from a decrease in

the free Cd2+ concentration in the boundary layer, resulting

from de-protonation of metal-binding ligands induced by

local pH enhancement as a consequence of algal release of

HO-. The observations of increased Cd bioavailability were

probably due to an enhancement of the free Cd2+

concentration in the boundary layer, resulting from

chemical oxidation of metal-binding ligands (e.g., cysteine) by oxidants released by the algal cells. Note that there is no uptake of intact cysteine-Cd complexes. The results highlight the importance of biologically-mediated surface processes

(e.g., redox and pH changes), in addition to other well-known abiotic processes, in determining metal

bioavailability.

Results

Methods

One-hour Cd uptake rates were investigated in two green

algae (Chlamydomonas reinhardtii CC1690 and CPCC11 and

Pseudokirchneriella subcapitata), and a cyanobacterium

(Anabaena flos-aquae) in media with a constant

concentration of free Cd2+ (e.g., 0.1 nM) buffered by NTA or

cysteine.

C. reinhardtii

(Photo from Protist Information Server)

P. subcapitata

(Photo from the Algal Web ) A. flos-aquae (Photo from http://toxinology.nilu.no/)

Figure 3. One-hour Cd uptake rates by C. reinhardtii CPCC11 (A), P. subcapitata (B), and

A. flos-aquae (C) in media with 0.1 nM free Cd2+ and increasing concentrations of

Cd-cysteine complexes (n = 3-4, mean ± SD). Data for each panel were from a single test (i.e., the same algal batch), and inserts in panels A and C show one independent

repeated test. Exposure time (h) 0 10 20 30 40 50 60 N et i nc reas e in s ol ut ion pH 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 NO3--acclimated algae

Figure 1. Cd uptake in NTA- (black dots) or cysteine- (red dots) buffered media (pH buffered at 7.0 with 10 mM MOPS) at the same free [Cd2+] by

NO3--acclimated C. reinhardtii (CC1690) (A), pH change in bulk solution (no pH buffer addition, in order to detect short-term pH changes)

containing NO3--acclimated C. reinhardtii (CC1690) (B); and simulation of Cd speciation (total Cd = 20 nM) in NTA- or cysteine-buffered media at

different pH (C).

Figure 2. Relative Cd uptake rate by C. reinhardtii CPCC11 acclimated with different N sources in the presence of Cys in comparison with their

respective controls (i.e., the same algal batches but exposed to media buffered by NTA) at the same free [Cd2+] (A); Cd uptake (n = 3, some dots

overlap) at the same Cd2+ concentration in the presence of 5.6 kU•L-1 Cu/Zn-superoxide dismutase (SOD) and 3.2 mg•L-1 catalase by N-starved

C. reinhardtii CPCC11 (B); and the hypothetical ‘oxidation of cysteine or Cys-Cd complexes in the boundary layer’ (C).

Acknowledgements

A

B

A

B

pH 6.8 7.0 7.2 7.4 7.6 7.8 8.0 Cd 2+ (m o l L -1 ) 1e-12 1e-11 1e-10 1e-9 buffered by NTA buffered by cysteine

C

Conclusions

1. Cd bioavailability is determined by the

concentration of free Cd2+ in the

boundary layer, which can be different from that in the surrounding waters and might be regulated by the metabolism of these microorganisms. 2. Uptake of

other trace metals (e.g., Cu, Zn, Hg, etc.) by phytoplankton will also be sensitive to the proposed ‘boundary layer effect’.

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