Interactions between temperature and energy supply drive microbial communities in hydrothermal sediment.

Temperature and bioavailable energy control the distribution of life on Earth, and interact with each other due to the dependency of biological energy requirements on temperature. Here we analyze how temperature-energy interactions structure sediment microbial communities in two hydrothermally active areas of Guaymas Basin. Sites from one area experience advective input of thermogenically produced electron donors by seepage from deeper layers, whereas sites from the other area are diffusion-dominated and electron donor-depleted. In both locations, Archaea dominate at temperatures >45 °C and Bacteria at temperatures <10 °C. Yet, at the phylum level and below, there are clear differences. Hot seep sites have high proportions of typical hydrothermal vent and hot spring taxa. By contrast, high-temperature sites without seepage harbor mainly novel taxa belonging to phyla that are widespread in cold subseafloor sediment. Our results suggest that in hydrothermal sediments temperature determines domain-level dominance, whereas temperature-energy interactions structure microbial communities at the phylum-level and below.

Neotectonics of the Sea of Galilee (northeast Israel): implication for geodynamics and seismicity along the Dead Sea Fault system.

The Sea of Galilee in northeast Israel is a freshwater lake filling a morphological depression along the Dead Sea Fault. It is located in a tectonically complex area, where a N-S main fault system intersects secondary fault patterns non-univocally interpreted by previous reconstructions. A set of multiscale geophysical, geochemical and seismological data, reprocessed or newly collected, was analysed to unravel the interplay between shallow tectonic deformations and geodynamic processes. The result is a neotectonic map highlighting major seismogenic faults in a key region at the boundary between the Africa/Sinai and Arabian plates. Most active seismogenic displacement occurs along NNW-SSE oriented transtensional faults. This results in a left-lateral bifurcation of the Dead Sea Fault forming a rhomb-shaped depression we named the Capharnaum Trough, located off-track relative to the alleged principal deformation zone. Low-magnitude (ML = 3-4) epicentres accurately located during a recent seismic sequence are aligned along this feature, whose activity, depth and regional importance is supported by geophysical and geochemical evidence. This case study, involving a multiscale/multidisciplinary approach, may serve as a reference for similar geodynamic settings in the world, where unravelling geometric and kinematic complexities is challenging but fundamental for reliable earthquake hazard assessments.

The Guaymas Basin Subseafloor Sedimentary Archaeome Reflects Complex Environmental Histories.

We explore archaeal distributions in sedimentary subseafloor habitats of Guaymas Basin and the adjacent Sonora Margin, located in the Gulf of California, México. Sampling locations include (1) control sediments without hydrothermal or seep influence, (2) Sonora Margin sediments underlying oxygen minimum zone water, (3) compacted, highly reduced sediments from a pressure ridge with numerous seeps at the base of the Sonora Margin, and (4) sediments impacted by hydrothermal circulation at the off-axis Ringvent site. Generally, archaeal communities largely comprise Bathyarchaeal lineages, members of the Hadesarchaea, MBG-D, TMEG, and ANME-1 groups. Variations in archaeal community composition reflect locally specific environmental challenges. Background sediments are divided into surface and subsurface niches. Overall, the environmental setting and history of a particular site, not isolated biogeochemical properties out of context, control the subseafloor archaeal communities in Guaymas Basin and Sonora Margin sediments.

Characteristics and Evolution of sill-driven off-axis hydrothermalism in Guaymas Basin - the Ringvent site.

The Guaymas Basin spreading center, at 2000 m depth in the Gulf of California, is overlain by a thick sedimentary cover. Across the basin, localized temperature anomalies, with active methane venting and seep fauna exist in response to magma emplacement into sediments. These sites evolve over thousands of years as magma freezes into doleritic sills and the system cools. Although several cool sites resembling cold seeps have been characterized, the hydrothermally active stage of an off-axis site was lacking good examples. Here, we present a multidisciplinary characterization of Ringvent, an ~1 km wide circular mound where hydrothermal activity persists ~28 km northwest of the spreading center. Ringvent provides a new type of intermediate-stage hydrothermal system where off-axis hydrothermal activity has attenuated since its formation, but remains evident in thermal anomalies, hydrothermal biota coexisting with seep fauna, and porewater biogeochemical signatures indicative of hydrothermal circulation. Due to their broad potential distribution, small size and limited life span, such sites are hard to find and characterize, but they provide critical missing links to understand the complex evolution of hydrothermal systems.

A combined QM/MM approach to protein--ligand interactions: polarization effects of the HIV-1 protease on selected high affinity inhibitors.

HIV-1 protease inhibitors are one of the two widely used therapeutic agents for the treatment of HIV-infected patients. The investigation of HIV-1 protease-inhibitor interactions can provide further insight for developing new compounds that are still required due to the growing problem of drug resistance. To this end, a combined QM/MM approach was used to determine electrostatic and polarization interactions on three high affinity inhibitors, nelfinavir, mozenavir, and tipranavir. The present computational results show that explicit treatment of the polarization effect is particularly important since it can contribute as much as one-third of the total electrostatic interaction energy. Further, an amino acid decomposition analysis was applied to determine contributions of individual residues to the enzyme--inhibitor interactions. It was found that the 4-hydroxy-dihydropyrone substructure of tipranavir is especially suited for extended charge delocalization by interacting with the catalytic aspartates and isoleucines of the HIV-1 protease. The calculated electron density difference maps reaffirm and provide a means of visualizing these results.

Mechanisms of antibiotic resistance: QM/MM modeling of the acylation reaction of a class A beta-lactamase with benzylpenicillin.

Understanding the mechanisms by which beta-lactamases destroy beta-lactam antibiotics is potentially vital in developing effective therapies to overcome bacterial antibiotic resistance. Class A beta-lactamases are the most important and common type of these enzymes. A key process in the reaction mechanism of class A beta-lactamases is the acylation of the active site serine by the antibiotic. We have modeled the complete mechanism of acylation with benzylpenicillin, using a combined quantum mechanical and molecular mechanical (QM/MM) method (B3LYP/6-31G+(d)//AM1-CHARMM22). All active site residues directly involved in the reaction, and the substrate, were treated at the QM level, with reaction energies calculated at the hybrid density functional (B3LYP/6-31+Gd) level. Structures and interactions with the protein were modeled by the AM1-CHARMM22 QM/MM approach. Alternative reaction coordinates and mechanisms have been tested by calculating a number of potential energy surfaces for each step of the acylation mechanism. The results support a mechanism in which Glu166 acts as the general base. Glu166 deprotonates an intervening conserved water molecule, which in turn activates Ser70 for nucleophilic attack on the antibiotic. This formation of the tetrahedral intermediate is calculated to have the highest barrier of the chemical steps in acylation. Subsequently, the acylenzyme is formed with Ser130 as the proton donor to the antibiotic thiazolidine ring, and Lys73 as a proton shuttle residue. The presented mechanism is both structurally and energetically consistent with experimental data. The QM/MM energy barrier (B3LYP/ 6-31G+(d)//AM1-CHARMM22) for the enzymatic reaction of 9 kcal mol(-1) is consistent with the experimental activation energy of about 12 kcal mol(-1). The effects of essential catalytic residues have been investigated by decomposition analysis. The results demonstrate the importance of the "oxyanion hole" in stabilizing the transition state and the tetrahedral intermediate. In addition, Asn132 and a number of charged residues in the active site have been identified as being central to the stabilizing effect of the enzyme. These results will be potentially useful in the development of stable beta-lactam antibiotics and for the design of new inhibitors.