Multiple roles of released c-type cytochromes in tuning electron transport and physiological status of Geobacter sulfurreducens

Low-molecular weight organic acids can enhance the microbial reduction of iron oxide nanoparticles and pollutants by improving electrons transfer

The combined application of dissimilatory iron-reducing bacteria (DIRB) and Fe(III) nanoparticles has garnered widespread interest in the contaminants transformation and removal. The efficiency of this composite system relies on the extracellular electron transfer (EET) process between DIRB and Fe(III) nanoparticles. While modifications to Fe(III) nanoparticles have demonstrated improvements in EET, enhancing DIRB activity also shows potential for further EET enhancement, meriting further investigation. In this study, we demonstrated that the addition of low-molecular organic acids (LMWOAs) (oxalate, pyruvate, malate, citrate, or fumarate) can improve the reduction of Fe2O3 nanoparticles by Geobacter sulfurreducens PCA through three pathways: increasing intracellular electron production, enhancing the reductive activity of extracellular metabolites, and improving the electron-donating capacity of extracellular polymeric substances. The maximum reduction of Fe2O3 nanoparticles reached up to 72 %. Our results further showed that LMWOAs significantly boosted the removal rate and ratio of Cr(VI) and hexachlorobenzene (HCB) by accelerating the EET process. Following the introduction of LMWOAs, the maximum reduction ratio of Cr(VI) reached 98 ± 0.05 % within 24 h, while the degradation efficiency of HCB reached 92 ± 0.06 % within 9 h. Overall, our study provided a precise mechanism of the role of LMWOAs on the EET process and a new strategy for reductive bioremediation of pollutants.

Fabricating an advanced electrogenic chassis by activating microbial metabolism and fine-tuning extracellular electron transfer

Exploiting electrogenic microorganisms as unconventional chassis hosts offers potential solutions to global energy and environmental challenges. However, their limited electrogenic efficiency and metabolic versatility, due to genetic and metabolic constraints, hinder broader applications. Herein, we developed a multifaceted approach to fabricate an enhanced electrogenic chassis, starting with streamlining the genome by removing extrachromosomal genetic material. This reduction led to faster lactate consumption, higher intracellular NADH/NAD+ and ATP/ADP levels, and increased growth and biomass accumulation, as well as promoted electrogenic activity. Transcriptome profiling showed an overall activation of cellular metabolism. We further established a molecular toolkit with a vector vehicle incorporating native replication block and refined promoter components for precise gene expression control. This enabled engineered primary metabolism for greater environmental robustness and fine-tuned extracellular electron transfer (EET) for improved efficiency. The enhanced chassis demonstrated substantially improved pollutant biodegradation and radionuclide removal, establishing a new paradigm for utilizing electrogenic organisms as novel biotechnology chassis.

Single Phototrophic Bacterium-Mediated Iron Cycling in Aquatic Environments

Redox cycling of iron plays a pivotal role in both nutrient acquisition by living organisms and the geochemical cycling of elements in aquatic environments. In nature, iron cycling is mediated by microbial Fe(II)-oxidizers and Fe(III)-reducers or through the interplay of biotic and abiotic iron transformation processes. Here, we unveil a specific iron cycling process driven by one single phototrophic species, Rhodobacter ferrooxidans SW2. It exhibits the capability to reduce Fe(III) during bacterial cultivation. A c-type cytochrome is identified with Fe(III)-reducing activity, implying the linkage of Fe(III) reduction with the electron transport system. R. ferrooxidans SW2 can mediate iron redox transformation, depending on the availability of light and/or organic substrates. Iron cycling driven by anoxygenic photoferrotrophs is proposed to exist worldwide in modern and ancient environments. Our work not only enriches the theoretical basis of iron cycling in nature but also implies multiple roles of anoxygenic photoferrotrophs in iron transformation processes.