The pathway of sulfide oxidation to octasulfur globules in the cytoplasm of aerobic bacteria

Sulfur-oxidizing bacteria can oxidize hydrogen sulfide (H 2 S) to produce sulfur globules. Although the process is common, the pathway is unclear. In recombinant Escherichia coli and wild-type Corynebacterium vitaeruminis DSM20294 with SQR but no enzymes to oxidize zero valence sulfur, SQR oxidized H 2 S into short-chain inorganic polysulfide (H 2 S n , n≥2) and organic polysulfide (RS n H, n≥2), which reacted with each other to form long-chain GS n H (n≥2) and H 2 S n before producing octasulfur (S 8 ), the main component of elemental sulfur. GS n H also reacted with GSH to form GSnG (n≥2) and H 2 S; H 2 S was again oxidized by SQR. After GSH was depleted, SQR simply oxidized H 2 S to H 2 S n , which spontaneously generated S 8 . S 8 aggregated into sulfur globules in the cytoplasm. The results highlight the process of sulfide oxidation to S 8 globules in the bacterial cytoplasm and demonstrate the potential of using heterotrophic bacteria with SQR to convert toxic H 2 S into relatively benign S 8 globules. IMPORTANCE Our results support a process of H 2 S oxidation to produce octasulfur globules via SQR catalysis and spontaneous reactions in the bacterial cytoplasm. Since the process is an important event in geochemical cycling, a better understanding facilitates further studies and provides theoretical support for using heterotrophic bacteria with SQR to oxidize toxic H 2 S into sulfur globules for recovery.

Reaction-based fluorogenic probes for selective detection of cysteinyl oxidation in living cells

Measuring reactive oxygen, nitrogen and sulfur species in cells is established technology, but turn-on fluorescence tools for detecting the products of their reaction with protein cysteines remain essentially unknown. Toward this goal, here we describe fluorogenic probes for sulfenic acid, a redox modification of protein cysteines inextricably linked to signaling and oxidative stress. The probes, called CysOx1 and CysOx2, are reaction-based, exhibit excellent cell permeability, rapid reactivity, and high selectivity with minimal cytotoxicity. We applied CysOx2 in a cell-based 96-well plate assay to determine whether kinase inhibitors modulate protein S-sulfenylation as well as O-phosphorylation. Analysis of these data revealed an unexpected positive association of S-sulfenylation and inhibition of select kinases within the TK, AGC, and CMGC families including GSK3, a multitasking Ser/Thr kinase and emerging therapeutic target for neurodegenerative and mood disorders. Chemoproteomic mapping of sulfenic acid-modified cysteines in GSK3 inhibitor-treated cells shows that sites of S-oxidation localize to regulatory cysteines within key components of antioxidant defense systems. Our studies with CysOx probes offer up new insights into kinase-inhibitor dependent modulation of sulfenylome dynamics and should accelerate future efforts in the modern era of translational redox medicine.

Electronic Structure of Tyrosyl D Radical of Photosystem II, as Revealed by 2D-Hyperfine Sublevel Correlation Spectroscopy

The biological water oxidation takes place in Photosystem II (PSII), a multi-subunit protein located in thylakoid membranes of higher plant chloroplasts and cyanobacteria. The catalytic site of PSII is a Mn4Ca cluster and is known as the oxygen evolving complex (OEC) of PSII. Two tyrosine residues D1-Tyr161 (YZ) and D2-Tyr160 (YD) are symmetrically placed in the two core subunits D1 and D2 and participate in proton coupled electron transfer reactions. YZ of PSII is near the OEC and mediates electron coupled proton transfer from Mn4Ca to the photooxidizable chlorophyll species P680+. YD does not directly interact with OEC, but is crucial for modulating the various S oxidation states of the OEC. In PSII from higher plants the environment of YD• radical has been extensively characterized only in spinach (Spinacia oleracea) Mn- depleted non functional PSII membranes. Here, we present a 2D-HYSCORE investigation in functional PSII of spinach to determine the electronic structure of YD• radical. The hyperfine couplings of the protons that interact with the YD• radical are determined and the relevant assignment is provided. A discussion on the similarities and differences between the present results and the results from studies performed in non functional PSII membranes from higher plants and PSII preparations from other organisms is given.

A redox cycle with complex II promotes sulfide quinone oxidoreductase dependent H2S oxidation

The dueling roles of H2S as an endogenously synthesized respiratory substrate and as a toxin, raise questions as to how it is cleared when the electron transport chain is inhibited. Sulfide quinone oxidoreductase (SQOR) is a mitochondrial inner membrane flavoprotein that catalyzes the first step in the H2S oxidation pathway and uses coenzyme Q (CoQ) as an electron acceptor. However, complex IV poisoning by H2S inhibits complex III-dependent recycling of CoQH2, which is needed to sustain H2S oxidation. We have discovered that under these conditions, reversal of complex II activity using fumarate as an electron acceptor, establishes a new redox cycle with SQOR. The purine nucleotide cycle and the malate aspartate shuttle are sources of fumarate in H2S treated cells, which accumulate succinate. Complex II knockdown decreases the efficiency of H2S clearance and increases recovery time to the basal respiration rate in H2S treated cells. In contrast, attenuation of complex I, which is a major competitor for the mitochondrial CoQ pool, has the opposite effects. Targeted knockout of complex II in murine intestinal epithelial cells that are routinely exposed to microbiota derived H2S, decreases serum, urine, and fecal thiosulfate, a product of H2S oxidation. Our study identifies a metabolic reprogramming response to H2S that furnishes fumarate as an alternate electron acceptor and supports H2S oxidation independent of complex IV activity. Complex II-linked redox cycling of SQOR has important implications for gut H2S metabolism as colonocytes are routinely exposed to high concentrations of this gas derived from the microbiota.One Sentence SummaryReversal of complex II sustains and prioritizes H2S oxidation when respiration is poisoned.

Metal organic framework derived NaCoxOy for room temperature hydrogen sulfide removal

Novel NaCoxOy adsorbents were fabricated by air calcination of (Na,Co)-organic frameworks at 700 °C. The NaCoxOy crystallized as hexagonal microsheets of 100–200 nm thickness with the presence of some polyhedral nanocrystals. The surface area was in the range of 1.15–1.90 m2 g−1. X-ray photoelectron spectroscopy (XPS) analysis confirmed Co2+ and Co3+ sites in MOFs, which were preserved in NaCoxOy. The synthesized adsorbents were studied for room-temperature H2S removal in both dry and moist conditions. NaCoxOy adsorbents were found ~ 80 times better than the MOF precursors. The maximum adsorption capacity of 168.2 mg g−1 was recorded for a 500 ppm H2S concentration flowing at a rate of 0.1 L min−1. The adsorption capacity decreased in the moist condition due to the competitive nature of water molecules for the H2S-binding sites. The PXRD analysis predicted Co3S4, CoSO4, Co3O4, and Co(OH)2 in the H2S-exposed sample. The XPS analysis confirmed the formation of sulfide, sulfur, and sulfate as the products of H2S oxidation at room temperature. The work reported here is the first study on the use of NaCoxOy type materials for H2S remediation.

The core root microbiome of Spartina alterniflora is predominated by sulfur-oxidizing and sulfate-reducing bacteria in Georgia salt marshes, USA

Background: Salt marshes are dominated by the smooth cordgrass Spartina alterniflora on the US Atlantic and Gulf of Mexico coastlines. Although soil microorganisms are well known to mediate important biogeochemical cycles in salt marshes, little is known about the role of root microbiomes in supporting the health and productivity of marsh plant hosts. Leveraging in situ gradients in aboveground plant biomass as a natural laboratory, we investigated the relationships between S. alterniflora primary productivity, sediment redox potential, and the physiological ecology of bulk sediment, rhizosphere, and root microbial communities at two Georgia barrier islands over two growing seasons. Results: A marked decrease in prokaryotic alpha diversity with high abundance and increased phylogenetic dispersion was found in the S. alterniflora root microbiome. Significantly higher rates of enzymatic organic matter decomposition, as well as the relative abundances of putative sulfur (S)-oxidizing, sulfate-reducing, and nitrifying prokaryotes correlated with plant productivity. Moreover, these functional guilds were overrepresented in the S. alterniflora rhizosphere and root core microbiomes. Core microbiome bacteria from the Candidatus Thiodiazotropha genus, with the metabolic potential to couple S oxidation with C and N fixation, were shown to be highly abundant in the root and rhizosphere of S. alterniflora. Conclusions: The S. alterniflora root microbiome is dominated by highly active and competitive species taking advantage of available carbon substrates in the oxidized root zone. Two microbially-mediated mechanisms are proposed to stimulate S. alterniflora primary productivity: (i.) Enhanced microbial activity replenishes nutrients and terminal electron acceptors in higher biomass stands, and (ii.) coupling of chemolithotrophic S oxidation with carbon (C) and nitrogen (N) fixation by root and rhizosphere associated prokaryotes detoxify sulfide in the root zone while potentially transferring fixed C and N to the host plant.

Spectroscopic, Raman, EMPA, Micro-XRF and Micro-XANES Analyses of Sulphur Concentration and Oxidation State of Natural Apatite Crystals

Sulphur is the third most abundant volatile element in deep Earth systems. Analytical methods for accurately and efficiently determining the sulphur content and oxidation state in natural minerals are still lacking. Natural apatite is widely distributed in the Earth and incorporates a large amount of sulphur. Therefore, apatite is an ideal mineral for performing sulphur measurements. Here, we used spectroscopic, Raman, X-ray diffraction, laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), electron microprobe (EMPA) and micro-X-ray fluorescence spectrometry (micro-XRF) analysis techniques and developed a new analytical approach (i.e., micro-X-ray absorption near-edge structure (micro-XANES) analysis of the sulphur K-edge) to investigate the chemical characteristics of natural apatite. These multiple methods were developed to measure in situ sulphur concentration and S oxidation states and to assess a potential natural apatite reference material. Apatite contains chemically homogeneous sulphur, with micro-XANES located at the peak energies corresponding to S6+ (sulphate; ~2482 eV), S4+ (sulfite; ~2478 eV), and S2− (sulphide; ~2467, 2470 and 2474 eV). The Durango apatite contains total S presented as SO3 at amount of 0.332 ± 0.012 wt.% (1σ), with a large amount of S6+ and a small contribution of S4+. The Kovdor apatite contains 44–100 ppm of S and is dominated by S6+. These results indicate that the Durango apatite crystallised under relative oxidising conditions, and the Kovdor apatite has a higher oxygen fugacity than Durango. In addition, this study indicates the potential use of the natural apatite reference material with its S composition and S oxidation state.