In Situ Fe and S isotope analyses in pyrite from the 3.2 Ga Mendon Formation (Barberton Greenstone Belt,South Africa): Evidence for early microbial iron reduction

On the basis of phylogenetic studies and laboratory cultures, it has been proposed that the ability of microbes to metabolize iron has emerged prior to the Archaea/Bacteria split. However, no unambiguous geochemical data supporting this claim have been put forward in rocks older than 2.7–2.5 giga years (Gyr). In the present work, we report in situ Fe and S isotope composition of pyrite from 3.28‐ to 3.26‐Gyr‐old cherts from the upper Mendon Formation, South Africa. We identified three populations of microscopic pyrites showing a wide range of Fe isotope compositions, which cluster around two δ⁵⁶Fe values of ?1.8‰ and +1‰. These three pyrite groups can also be distinguished based on the pyrite crystallinity and the S isotope mass‐independent signatures. One pyrite group displays poorly crystallized pyrite minerals with positive Δ³³S values > +3‰, while the other groups display more variable and closer to 0‰ Δ³³S values with recrystallized pyrite rims. It is worth to note that all the pyrite groups display positive Δ³³S values in the pyrite core and similar trace element compositions. We therefore suggest that two of the pyrite groups have experienced late fluid circulations that have led to partial recrystallization and dilution of S isotope mass‐independent signature but not modification of the Fe isotope record. Considering the mineralogy and geochemistry of the pyrites and associated organic material, we conclude that this iron isotope systematic derives from microbial respiration of iron oxides during early diagenesis. Our data extend the geological record of dissimilatory iron reduction (DIR) back more than 560 million years (Myr) and confirm that micro‐organisms closely related to the last common ancestor had the ability to reduce Fe(III).     

Deterministic Somatic Cell Reprogramming Involves Continuous Transcriptional Changes Governed by Myc and Epigenetic-Driven Modules

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Bifidobacterium breve and Streptococcus thermophilus secretion products enhance T helper 1 immune response and intestinal barrier in mice

Lactic acid bacteria or their secretion products can modulate immune responses differently in normal and inflammatory conditions. This comparative study analyzes the effect of oral administration of living lactic acid bacteria, or their conditioned media, on the epithelial and immune functions of colitis-prone C57BL/6 IL-10-deficient mice. Mice were untreated (control) or infected with Helicobacter hepaticus with or without oral treatment with living bacteria, Bifidobacterium breve C50 and Streptococcus thermophilus 065 (LB), or their culture-conditioned media (CM). Histology, cytokine mRNA, electrical resistance, and barrier capacity of colonic samples as well as cytokine secretion by mesenteric lymph node (MLN) cells were studied. Helicobacter hepaticus mice developed only mild colitis, which was not modified in LB or CM groups. In the CM (but not the LB) group, the colonic barrier was reinforced as compared to the other groups, as evidenced by decreased horseradish peroxidase (HRP) transcytosis and mannitol fluxes and increased electrical resistance. In MLN, the percentage of CD4+ and CD8+ T cells secreting IFNgamma was significantly higher in CM (2.06% and 1.98%, respectively) mice than in H. hepaticus (1.1% and 0.47%, P < 0.05) or control mice. In addition, the nonspecific stimulation of IFNgamma, TNFalpha, and IL-12 secretion by MLN cells was significantly higher in the CM group as compared to the other groups. In the absence of severe colitis, Bifidobacterium breve C50- and Streptococcus thermophilus 065-conditioned media can reinforce intestinal barrier capacity and stimulate Th1 immune response, highlighting the involvement of lactic acid bacteria-derived components in host defense.     

Rv3389C from Mycobacterium tuberculosis, a member of the (R)-specific hydratase/dehydratase family

The (R)-specific 3-hydroxyacyl dehydratases/trans-enoyl hydratases are key proteins in the biosynthesis of fatty acids. In mycobacteria, such enzymes remain unknown, although they are involved in the biosynthesis of major and essential lipids like mycolic acids. First bioinformatic analyses allowed to identify a single candidate protein, namely Rv3389c, that belongs to the hydratases 2 family and is most likely made of a distinctive asymmetric double hot dog fold. The purified recombinant Rv3389c protein was shown to efficiently catalyze the hydration of (C(8)-C(16)) enoyl-CoA substrates. Furthermore, it catalyzed the dehydration of a 3-hydroxyacyl-CoA in coupled reactions with both reductases (MabA and InhA) of the acyl carrier protein (ACP)-dependent M. tuberculosis fatty acid synthase type II involved in mycolic acid biosynthesis. Yet, the facts that Rv3389c activity decreased in the presence of ACP, versus CoA, derivative and that Rv3389c knockout mutant had no visible variation of its fatty acid content suggested the occurrence of additional hydratase/dehydratase candidates. Accordingly, further and detailed bioinformatic analyses led to the identification of other members of the hydratases 2 family in M. tuberculosis.     

Extracellular Iron Biomineralization by Photoautotrophic Iron-Oxidizing Bacteria

Iron oxidation at neutral pH by the phototrophic anaerobic iron-oxidizing bacterium Rhodobacter sp. strain SW2 leads to the formation of iron-rich minerals. These minerals consist mainly of nano-goethite (α-FeOOH), which precipitates exclusively outside cells, mostly on polymer fibers emerging from the cells. Scanning transmission X-ray microscopy analyses performed at the C K-edge suggest that these fibers are composed of a mixture of lipids and polysaccharides or of lipopolysaccharides. The iron and the organic carbon contents of these fibers are linearly correlated at the 25-nm scale, which in addition to their texture suggests that these fibers act as a template for mineral precipitation, followed by limited crystal growth. Moreover, we evidence a gradient of the iron oxidation state along the mineralized fibers at the submicrometer scale. Fe minerals on these fibers contain a higher proportion of Fe(III) at cell contact, and the proportion of Fe(II) increases at a distance from the cells. All together, these results demonstrate the primordial role of organic polymers in iron biomineralization and provide first evidence for the existence of a redox gradient around these nonencrusting, Fe-oxidizing bacteria.Fe(II) can serve as a source of electrons for phylogenetically diverse microorganisms that precipitate iron minerals as products of their metabolism (see, e.g., references 3, 5, 25, and 30). For example, mixotrophic or autotrophic bacteria can couple the oxidation of Fe(II) to the reduction of nitrate in anoxic and neutral-pH environments. With Fe(III) being highly insoluble at neutral pH, this metabolism leads to the formation of poorly to well-crystallized iron minerals (3, 18, 26, 27) that precipitate partly within the cell periplasm for some strains (22). Similar Fe minerals are also synthesized by autotrophic bacteria that perform anoxygenic photosynthesis, using Fe(II) as an electron donor and light as a source of energy for CO₂ fixation (8, 12, 30), according to the equation HCO₃⁻ + 4 Fe²⁺ + 10 H₂O ⇆ <CH₂O> + 4 Fe(OH)₃ + 7 H⁺.However, the biological mechanisms of iron oxidation in these bacteria and in particular the way they cope with the formation of minerals within their ultrastructures are still not fully understood. Indeed, iron minerals are potentially lethal since their precipitation may alter cellular ultrastructures but also catalyze the production of free radicals (2). Recent genetic studies of the phototrophic, iron-oxidizing bacteria Rhodobacter sp. strain SW2 (6) and Rhodopseudomonas palustris strain TIE-1 (16) have identified genes (fox and pio operons, respectively) encoding proteins specific for iron oxidation. Interestingly, Jiao and Newman (16) suggested that one of these proteins could have a periplasmic localization. However, in contrast to what has been observed in some other phototrophic iron oxidizers (25) and in some nitrate-reducing, iron-oxidizing bacteria (22), no iron-mineral precipitation occurs within the periplasm of the purple nonsulfur iron-oxidizing bacterium Rhodobacter sp. strain SW2 (3). Similarly to some other anaerobic neutrophilic (22, 25) and microaerobic iron-oxidizing bacteria (5, 10), this strain seems indeed to have the ability to localize iron biomineralization at a distance from the cells, leaving large areas of the cells free of precipitates (17, 25). While it has been shown that the Gallionella and Leptothrix genera, for example, produce extracellular polymers that facilitate the nucleation of iron minerals outside cells (see, e.g., references 5 and 9), only a little is known about the existence and function of such polymers in anaerobic, neutrophilic iron-oxidizing bacteria and particularly in the phototrophic strain SW2. In the present study, we investigate iron biomineralization by the photoautotrophic iron-oxidizing bacterium Rhodobacter sp. strain SW2. We use scanning transmission X-ray microscopy (STXM) to map and identify organic polymers produced by the cells as well as the redox state of iron at the 25-nanometer scale regularly during a 2 week-period. These results demonstrate the primordial role of organic polymers in iron biomineralization and provide the first evidence for the existence of a redox gradient around SW2 cells.     

Mycobacterium tuberculosis Proteins Involved in Mycolic Acid Synthesis and Transport Localize Dynamically to the Old Growing Pole and Septum

Understanding the mechanism that controls space-time coordination of elongation and division of Mycobacterium tuberculosis (Mtb), the causative agent of tuberculosis (TB), is critical for fighting the tubercle bacillus. Most of the numerous enzymes involved in the synthesis of Mycolic acid - Arabinogalactan-Peptidoglycan complex (MAPc) in the cell wall are essential in vivo. Using a dynamic approach, we localized Mtb enzymes belonging to the fatty acid synthase-II (FAS-II) complexes and involved in mycolic acid (MA) biosynthesis in a mycobacterial model of Mtb: M. smegmatis. Results also showed that the MA transporter MmpL3 was present in the mycobacterial envelope and was specifically and dynamically accumulated at the poles and septa during bacterial growth. This localization was due to its C-terminal domain. Moreover, the FAS-II enzymes were co-localized at the poles and septum with Wag31, the protein responsible for the polar localization of mycobacterial peptidoglycan biosynthesis. The dynamic localization of FAS-II and of the MA transporter with Wag31, at the old-growing poles and at the septum suggests that the main components of the mycomembrane may potentially be synthesized at these precise foci. This finding highlights a major difference between mycobacteria and other rod-shaped bacteria studied to date. Based on the already known polar activities of envelope biosynthesis in mycobacteria, we propose the existence of complex polar machinery devoted to the biogenesis of the entire envelope. As a result, the mycobacterial pole would represent the Achilles'' heel of the bacillus at all its growing stages.