<p>This study isolated and characterized a novel manganese-oxidizing bacterium from soil near a manganese mine in Zunyi, Guizhou. The strain was isolated using gradient dilution and quadrant streaking methods, followed by preliminary screening via the leucoberbelin blue I (LBB) colorimetric assay to detect high-valent manganese oxides. Gram staining and 16&#xa0;S rRNA gene sequencing identified the isolate as <i>Pseudochrobactrum saccharolyticum</i>, a Gram-negative short rod-shaped bacterium. This is the first report of its ability to oxidize manganese. Single-factor experiments were conducted to optimize environmental conditions affecting bacterial growth and Mn oxidation efficiency, including initial pH (4.0–8.0), temperature (18–38 ℃), Mn<sup>2+</sup> concentration (1–20 mmol/L), and the presence of coexisting metal ions (Fe<sup>3+</sup>, Cu<sup>2+</sup>, Ca<sup>2+</sup>; 10–80 µmol/L). The optimal conditions for Mn<sup>2+</sup> removal and biogenic manganese oxide (BMO) production were determined as follows: temperature 33 ℃, initial pH 6.0, Mn<sup>2+</sup> concentration 5 mmol/L, and Supplementation with 20 µmol/L Fe<sup>3+</sup>. Under these conditions, the Mn<sup>2+</sup> removal rate reached 92.05%, and BMO production was 3.55 mmol/L. Among the coexisting metals, Fe<sup>3+</sup> markedly enhanced bacterial growth and Mn-oxidizing activity. In contrast, Cu<sup>2+</sup> and Ca<sup>2+</sup> showed dual effects: low concentrations inhibited manganese oxide formation, whereas higher concentrations promoted it. The resulting BMOs were characterized by X-ray photoelectron spectroscopy (XPS), Fourier transform infrared spectroscopy (FTIR), and X-ray diffraction (XRD). XPS analysis revealed that the BMOs consisted mainly of Mn<sup>4+</sup> (69.30%), with minor proportions of Mn<sup>3+</sup> (19.92%) and Mn<sup>2+</sup> (10.78%). FTIR spectra confirmed the presence of hydroxyl (-OH), amide (-CONH-), and methyl (-CH<sub>3</sub>) functional groups, which are conducive to Mn<sup>2+</sup> adsorption and oxidation. This study demonstrates that <i>Pseudochrobactrum saccharolyticum</i> possesses efficient manganese-oxidizing capacity, enriching the diversity of known Mn-oxidizing bacteria and offering a promising indigenous candidate and theoretical foundation for bioremediating Mn pollution in karst manganese-mining regions.</p>

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BacteriumBiological characteristics and oxidation performance of a new manganese-oxidizing bacteria: Pseudochrobactrum saccharolyticum

  • Shuli Liu,
  • Xiangwen Luo,
  • Zifei Zhu,
  • Lanxin Zhou,
  • Yuanzhong Zhou

摘要

This study isolated and characterized a novel manganese-oxidizing bacterium from soil near a manganese mine in Zunyi, Guizhou. The strain was isolated using gradient dilution and quadrant streaking methods, followed by preliminary screening via the leucoberbelin blue I (LBB) colorimetric assay to detect high-valent manganese oxides. Gram staining and 16 S rRNA gene sequencing identified the isolate as Pseudochrobactrum saccharolyticum, a Gram-negative short rod-shaped bacterium. This is the first report of its ability to oxidize manganese. Single-factor experiments were conducted to optimize environmental conditions affecting bacterial growth and Mn oxidation efficiency, including initial pH (4.0–8.0), temperature (18–38 ℃), Mn2+ concentration (1–20 mmol/L), and the presence of coexisting metal ions (Fe3+, Cu2+, Ca2+; 10–80 µmol/L). The optimal conditions for Mn2+ removal and biogenic manganese oxide (BMO) production were determined as follows: temperature 33 ℃, initial pH 6.0, Mn2+ concentration 5 mmol/L, and Supplementation with 20 µmol/L Fe3+. Under these conditions, the Mn2+ removal rate reached 92.05%, and BMO production was 3.55 mmol/L. Among the coexisting metals, Fe3+ markedly enhanced bacterial growth and Mn-oxidizing activity. In contrast, Cu2+ and Ca2+ showed dual effects: low concentrations inhibited manganese oxide formation, whereas higher concentrations promoted it. The resulting BMOs were characterized by X-ray photoelectron spectroscopy (XPS), Fourier transform infrared spectroscopy (FTIR), and X-ray diffraction (XRD). XPS analysis revealed that the BMOs consisted mainly of Mn4+ (69.30%), with minor proportions of Mn3+ (19.92%) and Mn2+ (10.78%). FTIR spectra confirmed the presence of hydroxyl (-OH), amide (-CONH-), and methyl (-CH3) functional groups, which are conducive to Mn2+ adsorption and oxidation. This study demonstrates that Pseudochrobactrum saccharolyticum possesses efficient manganese-oxidizing capacity, enriching the diversity of known Mn-oxidizing bacteria and offering a promising indigenous candidate and theoretical foundation for bioremediating Mn pollution in karst manganese-mining regions.