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Rutile germanium oxide (r-GeO2), an ultrawide bandgap semiconductor, is a promising material for next-generation power electronics. Understanding and controlling the structure and morphology of r-GeO2 thin films are crucial for advancing their integration into future devices. In this work, r-GeO2 thin films were grown using RF magnetron sputtering on r plane sapphire substrates. Postdeposition annealing (PDA) was performed in an oxygen ambient atmosphere to crystallize the films. PDA at 950 °C resulted in the formation of needle-like nanostructures, predominantly originating at the edges of the film and growing inward toward the sample center. Sequential annealing at increasing temperatures indicated that these needle-like structures begin forming at temperatures above 925 °C. Next, the effect of the PDA duration on the structure was studied. It was seen that PDA at 950 °C for durations of 1 to 15 min promoted formation of the rutile phase, and extending the PDA duration allowed greater surface coverage of the nanostructures. However, annealing even longer, i.e., for 120 min, resulted in mixed phases of α-quartz and rutile GeO2. These findings demonstrate that controlling the PDA temperature and duration can effectively modulate the morphology of rutile-phase GeO2 thin films. 

In this work, we demonstrate the growth and phase stabilization of ultrawide bandgap polycrystalline rutile germanium dioxide (GeO2) thin films. GeO2 thin films were deposited using RF magnetron sputtering on r-plane sapphire (Al2O3) substrates. As-deposited films were x-ray amorphous. Postdeposition annealing was performed at temperatures between 650 and 950 °C in an oxygen or nitrogen ambient. Annealing at temperatures from 750 to 950 °C resulted in mixed-phase polycrystalline films containing tetragonal (rutile) GeO2, hexagonal (α-quartz) GeO2, and/or cubic (diamond) germanium (Ge). When nitrogen was used as the anneal ambient, mixed GeO2 phases were observed. In contrast, annealing in oxygen promoted stabilization of the r-GeO2 phase. Grazing angle x-ray diffraction showed a preferred orientation of (220) r-GeO2 for all crystallized films. The combination of O2 annealing and O2 flux during growth resulted in r-GeO2 films with highly preferential alignment. Using electron microscopy, we observed an interfacial layer of hexagonal-oriented GeO2 with epitaxial alignment to the (11¯02) Al2O3 substrate, which may help stabilize the top polycrystalline r-GeO2 film. 

Two sulphur-oxidizing, chemolithoautotrophic aerobes were isolated from the chemocline of an anchialine sinkhole located within the Weeki Wachee River of Florida. Gram-stain-negative cells of both strains were motile, chemotactic rods. Phylogenetic analysis of the 16S rRNA gene and predicted amino acid sequences of ribosomal proteins, average nucleotide identities, and alignment fractions suggest the strains HH1 T and HH3 T represent novel species belonging to the genus Thiomicrorhabdus . The genome G+C fraction of HH1 T is 47.8 mol% with a genome length of 2.61 Mb, whereas HH3 T has a G+C fraction of 52.4 mol% and 2.49 Mb genome length. Major fatty acids of the two strains included C 16 : 1 , C 18 : 1 and C 16 : 0 , with the addition of C 10:0 3-OH in HH1 T and C 12 : 0 in HH3 T . Chemolithoautotrophic growth of both strains was supported by elemental sulphur, sulphide, tetrathionate, and thiosulphate, and HH1 T was also able to use molecular hydrogen. Neither strain was capable of heterotrophic growth or use of nitrate as a terminal electron acceptor. Strain HH1 T grew from pH 6.5 to 8.5, with an optimum of pH 7.4, whereas strain HH3 T grew from pH 6 to 8 with an optimum of pH 7.5. Growth was observed between 15–35 °C with optima of 32.8 °C for HH1 T and 32 °C for HH3 T . HH1 T grew in media with [NaCl] 80–689 mM, with an optimum of 400 mM, while HH3 T grew at 80–517 mM, with an optimum of 80 mM. The name Thiomicrorhabdus heinhorstiae sp. nov. is proposed, and the type strain is HH1 T (=DSM 111584 T =ATCC TSD-240 T ). The name Thiomicrorhabdus cannonii sp. nov is proposed, and the type strain is HH3 T (=DSM 111593 T =ATCC TSD-241 T ). 

In nature, concentrations of dissolved inorganic carbon (DIC; = CO 2 + HCO 3 - + CO 3 2- ) can be low, and autotrophic organisms adapt with a variety of mechanisms to elevate intracellular DIC concentrations to enhance CO 2 fixation. Such mechanisms have been well-studied in Cyanobacteria , but much remains to be learned about their activity in other phyla. Novel multi-subunit membrane-spanning complexes capable of elevating intracellular DIC were recently described in three species of bacteria. Homologs of these complexes are distributed among 17 phyla in Bacteria and Archaea, and are predicted to consist of one, two, or three subunits. To determine whether DIC accumulation is a shared feature of these diverse complexes, seven of them, representative of organisms from four phyla, from a variety of habitats, and with three different subunit configurations were chosen for study. A high-CO 2 requiring, carbonic anhydrase-deficient ( yadF - cynT - ) strain of E. coli Lemo21(DE3), which could be rescued via elevated intracellular DIC concentrations, was created for heterologous expression and characterization of the complexes. Expression of all seven complexes rescued the ability of E. coli Lemo21(DE3) yadF - cynT - to grow under low CO 2 conditions, and six of the seven generated measurably elevated intracellular DIC concentrations when their expression was induced. For complexes consisting of two or three subunits, all subunits were necessary for DIC accumulation. Isotopic disequilibrium experiments clarified that CO 2 was the substrate for these complexes. In addition, the presence of an ionophore prevented the accumulation of intracellular DIC, suggesting that these complexes may couple proton potential to DIC accumulation. IMPORTANCE To facilitate the synthesis of biomass from CO 2 , autotrophic organisms use a variety of mechanisms to increase intracellular DIC concentrations. A novel type of multi-subunit complex has recently been described, which has been shown to generate measurably elevated intracellular DIC concentrations in three species of bacteria, begging the question of whether these complexes share this capability across the 17 phyla of Bacteria and Archaea where they are found. This study shows that DIC accumulation is a trait shared by complexes with varied subunit structures, from organisms with diverse physiologies and taxonomies, suggesting that this trait is universal among them. Successful expression in E. coli suggests the possibility of their expression in engineered organisms synthesizing compounds of industrial importance from CO 2 .