Yinghuangia soli sp. nov., isolated from soil of weathering dolomite in a karst area.

A Gram-stain-positive, aerobic actinomycete strain, designated KLBMP 8922T, was isolated from a soil sample collected from weathering dolomite crust in Guizhou Province, PR China. KLBMP 8922T showed the 16S rRNA gene similarities to Yinghuangia seranimata CCTCC AA 206006T (98.7 %), Yinghuangia catbensis VN07A0015T (98.3 %) and Yinghuangia aomiensis M24DS4T (98.2 %). The taxonomic status of this strain was investigated by using a polyphasic approach. The aerial mycelia of KLBMP 8922T formed spore chains, and spores were cylindrical with smooth surfaces. The whole-cell sugars were ribose, mannose and galactose with traces of glucose and xylose. The diagnostic amino acids of the cell wall were ll-diaminopimelic acid, alanine and glutamic acid. The predominant menaquinones were MK-9(H6) and MK-9(H8). The diagnostic phospholipids were diphosphatidylglycerol, phosphatidylinositol, phosphatidylinositolmannoside, phosphatidylethanolamine, an unidentified phospholipid and an unidentified lipid. The major cellular fatty acids (>10 %) were iso-C15 : 0, iso-C16 : 0 and iso-C16 : 1H. The genomic DNA G+C content was 72.0 mol%. The digital DNA-DNA hybridization (dDDH) value between KLBMP 8922T and Y. seranimata CCTCC AA 206006T was 24.1 %, and the average nucleotide identity (ANI) value was 81.0 %. On the basis of a combination of morphological, chemotaxonomic and phylogenetic characteristics, strain KLBMP 8922T represents a novel species of the genus Yinghuangia for which the name Yinghuangia soli sp. nov. is proposed. The type strain was KLBMP 8922T (= CGMCC 1.19360T = NBRC 115572T).

Antribacter soli sp. nov., a novel actinobacterium isolated from soils of weathering dolomite.

Strain KLBMP 9083T, a novel actinobacterium, was isolated from weathered soils collected from a karst area in Anshun, Guizhou Province, PR China. The taxonomic position of strain KLBMP 9083T was studied using the polyphasic approach. Phylogenetic analysis based on the 16S rRNA gene sequence indicated that strain KLBMP 9083T formed a stabilized monophyletic clade with its closest relative strain Antribacter gilvus CGMCC 1.13856T (98.4 % 16S rRNA gene sequence similarity). The peptidoglycan hydrolysates contained alanine, glutamic acid, threonine and lysine. The polar lipids were composed of diphosphatidylglycerol, phosphatidylinositol, phosphatidylinositol mannoside, an unidentified phosphoglycolipid, an unidentified phospholipid and an unidentified glycolipid. The predominant menaquinones were MK-9(H8) (87.1 %), MK-9(H6) (7.3 %) and MK-9(H4) (5.6 %). The major fatty acids (>10 %) were anteiso-C15 : 0 and iso-C15 : 0. The genomic DNA G+C content was 72.3 mol%. The digital DNA-DNA hybridization and average nucleotide identity values between strain KLBMP 9083T and A. gilvus CGMCC 1.13856T were 23.4 and 79.9 %, respectively. On the basis of morphological, chemotaxonomic and phylogenetic characteristics, strain KLBMP 9083T represents a novel species of the genus Antribacter, for which the name Antribacter soli sp. nov. is proposed. The type strain is KLBMP 9083T (=CGMCC 4.7737T=NBRC 115577T).

Enhancing La(III) biosorption and biomineralization with Micromonospora saelicesensis: Involvement of phosphorus and formation of monazite nano-minerals.

The release of rare earth elements (REEs) from mining wastes and their applications has significant environmental implications, necessitating the development of effective prevention and reclamation strategies. The mobility of REEs in groundwater due to microorganisms has garnered considerable attention. In this study, a La(III) resistant actinobacterium, Micromonospora saelicesensis KLBMP 9669, was isolated from REE enrichment soil in GuiZhou, China, and evaluated for its ability to adsorb and biomineralize La(III). The findings demonstrated that M. saelicesensis KLBMP 9669 immobilized La(III) through the physical and chemical interactions, with immobilization being influenced by the initial La(III) concentration, biomass, and pH. The adsorption kinetics followed a pseudo-second-order rate model, and the adsorption isotherm conformed to the Langmuir model. La(III) adsorption capacity of this strain was 90 mg/g, and removal rate was 94 %. Scanning electron microscope (SEM) coupled with energy dispersive X-ray spectrometer (EDS) analysis revealed the coexistence of La(III) with C, N, O, and P. Fourier transform infrared spectroscopy (FTIR) and X-ray photoelectron spectroscopy (XPS) investigations further indicated that carboxyl, amino, carbonyl, and phosphate groups on the mycelial surface may participate in lanthanum adsorption. Transmission electron microscopy (TEM) revealed that La(III) accumulation throughout the M. saelicesensis KLBMP 9669, with some granular deposits on the mycelial surface. Selected area electron diffraction (SAED) confirmed the presence of LaPO4 crystals on the M. saelicesensis KLBMP 9669 biomass after a prolonged period of La(III) accumulation. This post-sorption nano-crystallization on the M. saelicesensis KLBMP 9669 mycelial surface is expected to play a crucial role in limiting the bioimmobilization of REEs in geological repositories.