Abstract
The effect of combined stresses, photoinhibition, and nutrient depletion on the oxidative stress of cyanobacteria was measured in laboratory experiments to develop the biomass prediction model. Phormidium ambiguum was exposed to various photosynthetically active radiation (PAR) intensities and phosphorous (P) concentrations with fixed nitrogen concentrations. The samples were subjected to stress assays by detecting the hydrogen peroxide (H2O2) concentration and antioxidant activities of catalase (CAT) and superoxide dismutase (SOD). H2O2 concentrations decreased to 30 ”mol mâ2 sâ1 of PAR, then increased with higher PAR intensities. Regarding P concentrations, H2O2 concentrations (nmol Lâ1) generally decreased with increasing P concentrations. SOD and CAT activities were proportionate to the H2O2 proteinâ1. No H2O2 concentrations detected outside cells indicated the biological production of H2O2, and the accumulated H2O2 concentration inside cells was parameterized with H2O2 concentration proteinâ1. With over 30 ”mol mâ2 sâ1 of PAR, H2O2 concentration proteinâ1 had a similar increasing trend with PAR intensity, independently of P concentration. Meanwhile, with increasing P concentration, H2O2 proteinâ1 decreased in a similar pattern regardless of PAR intensity. Protein content decreased with gradually increasing H2O2 up to 4 nmol H2O2 mgâ1 protein, which provides a threshold to restrict the growth of cyanobacteria. With these results, an empirical formulaâprotein (mg Lâ1) = â 192*Log((H2O2/protein)/4.1), where H2O2/protein (nmol mgâ1) = â 0.312*PAR2/(502 + PAR2)*((25/PAR)4 + 1)*Log(P/133,100), as a function of total phosphorus concentration, P (”g Lâ1)âwas developed to obtain the cyanobacteria biomass.
Highlights
Protein content decreased with gradually increasing ÂH2O2 up to 4 nmol ÂH2O2 Âmgâ1 protein, which provides a threshold to restrict the growth of cyanobacteria
 2O2 dosage for cyanobacteria by laboratory incubations under different ÂH2O2 concentrations; cyanobacterial chlorophyll declined to nearly half after an 18 h incubation with approximately 30 ÎŒmol ÂLâ1 of ÂH2O21,40 or after a 4 h incubation with 100 ÎŒmol ÂLâ1 of ÂH2O22 ÂH2O2 delayed fluorescence decay with 0.1 ÎŒmol of ÂH2O2 ÂLâ17
The ÂH2O2 concentration of these waters was in the magnitude of ÎŒmol ÂLâ18,34,45. The comparison of these results indicates that the photolysis of organic carbon in natural water only is not sufficient to control cyanobacterial biomass
Summary
Protein content decreased with gradually increasing ÂH2O2 up to 4 nmol ÂH2O2 Âmgâ1 protein, which provides a threshold to restrict the growth of cyanobacteria. Cyanobacteria blooms often produce toxic metabolites and are harmful to other organisms as well as humans. Hydrogen peroxide (Â H2O2) is often endorsed to reduce cyanobacterial abundance and organic pollutants as it is more effective in application with cyanobacteria compared to other p. Â hytoplankton[1,2]. ÂH2O2 is generated photochemically from dissolved chromophoric organic materials exposed to UV, and H
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