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. 2000 Jun;123(2):625-36.
doi: 10.1104/pp.123.2.625.

The photoreduction of H(2)O(2) by Synechococcus sp. PCC 7942 and UTEX 625

Affiliations

The photoreduction of H(2)O(2) by Synechococcus sp. PCC 7942 and UTEX 625

A G Miller et al. Plant Physiol. 2000 Jun.

Abstract

It has been claimed that the sole H(2)O(2)-scavenging system in the cyanobacterium Synechococcus sp. PCC 7942 is a cytosolic catalase-peroxidase. We have measured in vivo activity of a light-dependent peroxidase in Synechococcus sp. PCC 7942 and UTEX 625. The addition of small amounts of H(2)O(2) (2.5 microM) to illuminated cells caused photochemical quenching (qP) of chlorophyll fluorescence that was relieved as the H(2)O(2) was consumed. The qP was maximal at about 50 microM H(2)O(2) with a Michaelis constant of about 7 microM. The H(2)O(2)-dependent qP strongly indicates that photoreduction can be involved in H(2)O(2) decomposition. Catalase-peroxidase activity was found to be almost completely inhibited by 10 microM NH(2)OH with no inhibition of the H(2)O(2)-dependent qP, which actually increased, presumably due to the light-dependent reaction now being the only route for H(2)O(2)-decomposition. When (18)O-labeled H(2)O(2) was presented to cells in the light there was an evolution of (16)O(2), indicative of H(2)(16)O oxidation by PS 2 and formation of photoreductant. In the dark (18)O(2) was evolved from added H(2)(18)O(2) as expected for decomposition by the catalase-peroxidase. This evolution was completely blocked by NH(2)OH, whereas the light-dependent evolution of (16)O(2) during H(2)(18)O(2) decomposition was unaffected.

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Figures

Figure 1
Figure 1
H2O2-dependent quenching of Chl fluorescence (F) in Synecococcus sp. PCC 7942. The cells were dark-adapted for 10 min and the fluorescence signal was measured in the absence (O) and presence (Fo) of the weak, pulse-modulated measuring beam (MB). A single SF was given during this time, indicated by the transient increase in the F signal. The non-modulated WL was then turned on (120 μmol photon m−2 s−1, PAR). The cells were then allowed to deplete the medium of Ci, manifest as attainment of maximal fluorescence yield (FM) during an SF, as described by Miller et al. (1991). The addition 50 μm Ci then resulted in reappearance of F quenching until this C i was consumed. The additions of H2O2 then also resulted in F quenching, which was relieved as the H2O2 was decomposed, manifest as cessation of the H2O-dependent O2 evolution indicated by the traces below the F trace. SFs were periodically given so that qP could be estimated.
Figure 2
Figure 2
Quenching of Chl F due to addition of H2O2 solutions is not due to contaminant Ci. Synechococcus sp. PCC 7942 cells were allowed to deplete the medium of Ci described in Figure 1, then the response to an SF was monitored in the presence of: 500 μm Ci and about 280 μm O2 (A); 500 μm Ci, 15 mm glycolaldehyde, and the Glc oxidase O2 trap (B); or the latter adddition plus 50 μm H2O2 (C). Fv is defined as the difference between the FM signal measured during an SF given while the cells were in WL after depleting the medium of Ci and the Fo signal measured with dark-adapted cells illuminated only by the weak MB (see Fig. 1).
Figure 3
Figure 3
Selective inhibition of in vivo catalase activity of 10 μm NH2OH. A, 50 μm H2O2 was added to dark-adapted cells. O2 evolution was monitored with or without subsequent addition of 10 μm NH2OH. B, Cells were allowed to deplete the medium of Ci during illumination with WL (120 μmol photons m−2 s−1, PAR) and then F quenching and O2 evolution were monitored after the addition of either 5 or 20 μm H2O2 in the absence or presence of 10 μm H2O2. For both A and B the maximum O2 evolution rates, in terms of μmol O2 mg−1 Chl h−1, are given beside the O2 traces. Fv is as defined for Figure 2.
Figure 4
Figure 4
Decomposition of H2O2 in dark (A) and light (B) in response to H2O2 concentration. The maximum rate of O2 evolution was used as the measure of H2O2 decomposition in the absence (□) or presence (⋄) of 10 μm NH2OH. The rates for cells in the dark (A) were corrected for rates of O2 uptake due to respiration measured just prior to H2O2 addition. For measurement of H2O2 decomposition in the light the cells were allowed to first deplete the medium of Ci. The difference between the rates of H2O2 decomposition in the light in the absence and presence of 10 μm NH2OH is also given (○). The WL was 120 μmol photon m−2 s−1 (PAR).
Figure 5
Figure 5
Light-dependent H2O2 decomposition monitored as F quenching in Synechococcus sp. PCC 7942.Cells were allowed to deplete the medium of Ci in WL of 100 μmol photons m−2 s−1 (PAR) and then the degree of total F quenching was monitored after the addition of various concentrations of H2O2 in the absence (□) and presence (⋄) of 10 μm NH2OH.
Figure 6
Figure 6
Decomposition of H218O2 by Synechococcus sp. PCC 7942. Cells (12 μg Chl mL−1) were incubated in the dark (A) or in WL (206 μmol photons m−2 s−1; B and C) in the absence (A and B) or presence of (C) of 50 μm NH2OH. At the times indicated by the arrows, 50 μm H218O2 was added and 16O2 and 18O2 evolution were monitored by MS. Cells incubated in the light were allowed to deplete the medium of Ci before addition of the H218O2. A correction was made for 18O2 contamination of the H218O2 solution (see “Materials and Methods”).
Figure 7
Figure 7
Decomposition of H218O2 by Synechococcus UTEX 625. Cells (11 μg Chl mL−1) were incubated in the dark (A) or in WL (206 μmol photons m−2 s−1; B and C) in the absence (A and B) presence (C) of 50 μm NH2OH. Conditions as described in Figure 6 except that 80 μm H218O2 was added.

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