News Release

Divergent responses of growth rate and antioxidative system of ten Bacillus strains to acid stresses

Peer-Reviewed Publication

Higher Education Press

Result visualization of principal component analysis on the antioxidative system under acid treatments.


Result visualization of principal component analysis on the antioxidative system under acid treatments. In the figure, Acid1 represents a moderate acid treatment of pH 5.5, while Acid2 represents a very strong acid treatment of pH 5.0 (for strains GL6, JD, and NC2) or 4.5 (for the other strains), with the control of pH 7.0. Different shapes indicate different microbial strains in panel A, while different colors indicate the acid treatments in all the three panels. In each of panels B and C, different lowercase or upper letters indicate significant differences among the acid treatments at p < 0.05. The abbreviations SOD, CAT, GPX, GR, MDA, GSH and GSSG stand for superoxide dismutase, catalase, glutathione peroxidase, glutathione reductase, malondialdehyde, reduced glutathione, and oxidized glutathione, respectively.

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Credit: Jiaen Zhang Lab

Soil aciditification is widely occurring in diverse terrestrial ecosystems and soil microbial communities have been reported to be highly sensitive to changes in soil pH. Soil microbes could regulate their physiological conditions to make them survive under the aciditifying conditions. This study demonstrates that ten Bacillus strains are able to regulate the antioxidative system differently in response to the decreasing environmental pH condition, and therefore have different acid tolerance capacity. The researchers’ finding appeared on December 18, 2023 in Soil Ecology Letters.


A series of studies have been conducted by Jiaen Zhang's team at the College of Natural Resources and Environment, South China Agricultural University, in order to clarify how acid rain and consequent soil acidificiation would affect the soil microbial community composition and functions. In previous studies, they found that soil acidification could greatly change the composition and distribution of soil biota including microbial and faunal communities. Changing soil microbial community composition consequently influenced the microbe driving ecosystem functions such as the decomposition and sequestration of soil organic carbon. They considered that different individual responses to acidifying environmental condition could explain the acid induced changes in the soil microbial communities. Therefore, they conducted a series of incubation experiments to investigate the acid tolerance capacity and physiological response of different microbial strains to acid stress.


In this study, they found that ten Bacillus strains had obviously different pH tolerance thresholds, in spite of the close phylogenetic classification among strains. Acid stresses exerted significant effects on microbial antioxidative system, including superoxide dismutase, catalase, and glutathione transferring enzymes and reactants, but the effects were strain specific. Different microbial strains could have different investment strategies of energy and resources and therefore regulated different processes to cope with acid stresses. The principal component analysis indicated that several microbial strains preferentially regulated the activities of superoxide dismutase and catalase and the content of malondialdehyde, while others preferred to change the contents and ratio of oxidized and reduced glutathione reactants under acid stress. These results highlight the heterogeneity of microbal physiological responses to acidifying environmental conditions, consequently contributing to acid induced alterations in soil microbial community composition and diversity.


"The study furthers our understanding of the responses of soil microbes to soil acidification from the perspective of microbial physiology, highlighting the necessity to study microbial responses to environmental changes from different scales, and the observations obtained at the microscale may help explain the pattern of soil microbial community changing at the large scales."


Soil microbial communities drive multiple ecological processes such as mineralization and stabilization of soil organic carbon and element cycling, as well as the ecosystem stability under climate changes. Under different scenarios of environmental changes, divergent individual level responses of soil microbes may contribute to changes in the soil microbial community composition and therefore alter the microbe driving soil ecological functions. 

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