[FeFe]-hydrogenase abundance and diversity along a vertical redox gradient in Great Salt Lake, USA.

The use of [FeFe]-hydrogenase enzymes for the biotechnological production of H2 or other reduced products has been limited by their sensitivity to oxygen (O2). Here, we apply a PCR-directed approach to determine the distribution, abundance, and diversity of hydA gene fragments along co-varying salinity and O2 gradients in a vertical water column of Great Salt Lake (GSL), UT. The distribution of hydA was constrained to water column transects that had high salt and relatively low O2 concentrations. Recovered HydA deduced amino acid sequences were enriched in hydrophilic amino acids relative to HydA from less saline environments. In addition, they harbored interesting variations in the amino acid environment of the complex H-cluster metalloenzyme active site and putative gas transfer channels that may be important for both H2 transfer and O2 susceptibility. A phylogenetic framework was created to infer the accessory cluster composition and quaternary structure of recovered HydA protein sequences based on phylogenetic relationships and the gene contexts of known complete HydA sequences. Numerous recovered HydA are predicted to harbor multiple N- and C-terminal accessory iron-sulfur cluster binding domains and are likely to exist as multisubunit complexes. This study indicates an important role for [FeFe]-hydrogenases in the functioning of the GSL ecosystem and provides new target genes and variants for use in identifying O2 tolerant enzymes for biotechnological applications.

An examination of protist diversity in serpentinization-hosted ecosystems of the Samail Ophiolite of Oman.

In the Samail Ophiolite of Oman, the geological process of serpentinization produces reduced, hydrogen rich, hyperalkaline (pH > 11) fluids. These fluids are generated through water reacting with ultramafic rock from the upper mantle in the subsurface. On Earth's continents, serpentinized fluids can be expressed at the surface where they can mix with circumneutral surface water and subsequently generate a pH gradient (∼pH 8 to pH > 11) in addition to variations in other chemical parameters such as dissolved CO2, O2, and H2. Globally, archaeal and bacterial community diversity has been shown to reflect geochemical gradients established by the process of serpentinization. It is unknown if the same is true for microorganisms of the domain Eukarya (eukaryotes). In this study, using 18S rRNA gene amplicon sequencing, we explore the diversity of microbial eukaryotes called protists in sediments of serpentinized fluids in Oman. We demonstrate that protist community composition and diversity correlate significantly with variations in pH, with protist richness being significantly lower in sediments of hyperalkaline fluids. In addition to pH, the availability of CO2 to phototrophic protists, the composition of potential food sources (prokaryotes) for heterotrophic protists and the concentration of O2 for anaerobic protists are factors that likely shape overall protist community composition and diversity along the geochemical gradient. The taxonomy of the protist 18S rRNA gene sequences indicates the presence of protists that are involved in carbon cycling in serpentinized fluids of Oman. Therefore, as we evaluate the applicability of serpentinization for carbon sequestration, the presence and diversity of protists should be considered.

Role of the Tyr-Cys cross-link to the active site properties of galactose oxidase.

The catalytically relevant, oxidized state of the active site [Cu(II)-Y·-C] of galactose oxidase (GO) is composed of antiferromagnetically coupled Cu(II) and a post-translationally generated Tyr-Cys radical cofactor [Y·-C]. The thioether bond of the Tyr-Cys cross-link has been shown experimentally to affect the stability, the reduction potential, and the catalytic efficiency of the GO active site. However, the origin of these structural and energetic effects on the GO active site has not yet been investigated in detail. Here we present copper and sulfur K-edge X-ray absorption data and a systematic computational approach for evaluating the role of the Tyr-Cys cross-link in GO. The sulfur contribution of the Tyr-Cys cross-link to the redox active orbital is estimated from sulfur K-edge X-ray absorption spectra of oxidized GO to be about 24 ± 3%, compared to the values from computational models of apo-GO (15%) and holo-GO (22%). The results for the apo-GO computational models are in good agreement with the previously reported value for apo-GO (20 ± 3% from EPR). Surprisingly, the Tyr-Cys cross-link has only a minimal effect on the inner sphere, coordination geometry of the Cu site in the holo-protein. Its effect on the electronic structure is more striking as it facilitates the delocalization of the redox active orbital onto the thioether sulfur derived from Cys, thereby reducing the spin coupling between the [Y·-C] radical and the Cu(II) center (752 cm(-1)) relative to the unsubstituted [Y·] radical and the Cu(II) center (2210 cm(-1)). Energetically, the Tyr-Cys cross-link lowers the reduction potential by about 75 mV (calculated) allowing a more facile oxidation of the holo active site versus the site without the cross-link. Overall, the Tyr-Cys cross-link confers unique ground state properties on the GO active site that tunes its function in a remarkably nuanced fashion.