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 m−2 s−1 of PAR, then increased with higher PAR intensities. Regarding P concentrations, H2O2 concentrations (nmol L−1) generally decreased with increasing P concentrations. SOD and CAT activities were proportionate to the H2O2 protein−1. No H2O2 concentrations detected outside cells indicated the biological production of H2O2, and the accumulated H2O2 concentration inside cells was parameterized with H2O2 concentration protein−1. With over 30 ”mol m−2 s−1 of PAR, H2O2 concentration protein−1 had a similar increasing trend with PAR intensity, independently of P concentration. Meanwhile, with increasing P concentration, H2O2 protein−1 decreased in a similar pattern regardless of PAR intensity. Protein content decreased with gradually increasing H2O2 up to 4 nmol H2O2 mg−1 protein, which provides a threshold to restrict the growth of cyanobacteria. With these results, an empirical formula—protein (mg L−1) = − 192*Log((H2O2/protein)/4.1), where H2O2/protein (nmol mg−1) = − 0.312*PAR2/(502 + PAR2)*((25/PAR)4 + 1)*Log(P/133,100), as a function of total phosphorus concentration, P (”g L−1)—was developed to obtain the cyanobacteria biomass.

Highlights

  • Protein content decreased with gradually increasing ­H2O2 up to 4 nmol ­H2O2 ­mg−1 protein, which provides a threshold to restrict the growth of cyanobacteria

  • ­ 2O2 dosage for cyanobacteria by laboratory incubations under different ­H2O2 concentrations; cyanobacterial chlorophyll declined to nearly half after an 18 h incubation with approximately 30 ÎŒmol ­L−1 of ­H2O21,40 or after a 4 h incubation with 100 ÎŒmol ­L−1 of ­H2O22 ­H2O2 delayed fluorescence decay with 0.1 ÎŒmol of ­H2O2 ­L−17

  • The ­H2O2 concentration of these waters was in the magnitude of ÎŒmol ­L−18,34,45. The comparison of these results indicates that the photolysis of organic carbon in natural water only is not sufficient to control cyanobacterial biomass

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Summary

Introduction

Protein content decreased with gradually increasing ­H2O2 up to 4 nmol ­H2O2 ­mg−1 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 (­ H2O2) is often endorsed to reduce cyanobacterial abundance and organic pollutants as it is more effective in application with cyanobacteria compared to other p. ­ hytoplankton[1,2]. ­H2O2 is generated photochemically from dissolved chromophoric organic materials exposed to UV, and H

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