Quantifying in situ β-glucosidase and phosphatase activity in groundwater

Enzymes play an important role in the environment, they breakdown natural-occurring and anthropogenic molecules so that they can be transported into cells and utilized. Enzyme assays are routinely used in soil science and oceanography to measure the activities of specific processes and to serve as general indicators of microbial activity. Conventional enzyme assays are conducted as batch incubation of sediment and water samples. During these assays the concentration of product is measured and enzyme activity is then determined as the rate of product formation. Few studies have measured enzyme activities of groundwater. This work investigates the use of β-glucosidase and phosphatase assays for quantifying in situ enzyme activities in groundwater. Improvements to conventional enzyme assays using p-nitrophenyl substituted compounds were made by developing a high performance liquid chromatography method to improve quantitation limits of the product and to quantify concentrations of both the substrate and the product. An in situ single-well push pull test was then conducted to measure β-glucosidase activity in situ and to estimate the Michaelis constant (K[subscript m]) and the maximum reaction velocity (V[subscript max]) in petroleum-contaminated groundwater at a field site near Newberg, Oregon. An important feature of the single-well push pull test is the nonlinear drop in pore water velocity that the test solution experiences as it moves out from the injection point. The nonlinear drop in pore water velocity is of particular interest because enzyme-mediated reactions are very fast and changes in the hydraulic properties during the test may give rise to mass-transport limitations. Fast reactions lead to the simultaneous depletion of substrate and accumulation of product at the site of the reaction so substrate and product concentrations near the enzyme can be different then the concentrations in bulk solution. And the rates obtained from a single-well push pull tests may be a combination of the rates at which substrate diffuses to the microorganism and at which the reaction occurs. Laboratory experiments with sediment-packed columns were conducted with a range of pore water velocities typically achieved in the subsurface during as push-pull test as a means for examining the potential effects of inhibition and diffusion on phosphatase enzyme kinetics. In this set of column experiments rates of phosphatase-mediated reactions were investigated instead of β-glucosidase, which is an inducible enzyme. Numerical investigations were then conducted to examine the importance of diffusion limitations for describing the influence of transport processes on the observed rates of reaction. The theoretical investigation was conducted by formally upscaling the proposed sub-pore-scale processes to develop a macroscale (or Darcy scale) description of the transport of the substrate. These results indicate that mass-transfer limitations due to the diffusion of the substrate to the enzyme cause an increase in the apparent K[subscript m] but have no effect on V[subscript max]. In this study an analytical method was developed to measure rates of enzyme-mediated reaction in situ so that the measured rates reflected actual rates of microorganism in their natural environment. More carefully controlled laboratory experiments demonstrated that rates of enzyme-mediated reactions measured at low substrate concentrations depended on the flow properties of the test solution

Virus-like particles identify an HIV V1V2 Apex-1 binding neutralizing antibody that lacks a protruding loop

Most HIV-1-specific neutralizing antibodies isolated to date exhibit unusual characteristics that complicate their elicitation. Neutralizing antibodies that target the V1V2 apex of the HIV-1 envelope (Env) trimer feature unusually long protruding loops, enabl them to penetrate the HIV-1 glycan shield. As antibodies with loops of requisite length are created through uncommon recombination events, an alternative mode of apex binding has been sought. Here, we isolated a lineage of Env apex-directed neutralizing antibodies, N90-VRC38.01-11, using virus-like particles and conformationally stabilized Env trimers as B cell probes. A crystal structure of N90-VRC38.01 with a scaffolded V1V2 revealed a binding mode involving side-chain to side-chain interactions that reduced the distance the antibody loop must traverse the glycan shield, facilitating V1V2 binding via a non-protruding loop. The N90-VRC38 lineage identifies a solution for V1V2apex binding that provides a more conventional B cell pathway for vaccine design

Osteochondral transplantation using autografts from the upper tibio-fibular joint for the treatment of knee cartilage lesions

Purpose Treatment of large cartilage lesions of the knee in weight-bearing areas is still a controversy and challenging topic. Autologous osteochondral mosaicplasty has proven to be a valid option for treatment but donor site morbidity with most frequently used autografts remains a source of concern. This study aims to assess clinical results and safety profile of autologous osteochondral graft from the upper tibio-fibular joint applied to reconstruct symptomatic osteochondral lesions of the knee. Methods Thirty-one patients (22 men and 9 women) with grade 4 cartilage lesions in the knee were operated by mosaicplasty technique using autologous osteochondral graft from the upper tibio-fibular joint, between 1998 and 2006. Clinical assessment included visual analog scale (VAS) for pain and Lysholm score. All patients were evaluated by MRI pre- and post-operatively regarding joint congruency as good, fair (inferior to 1 mm incongruence), and poor (incongruence higher than 1 mm registered in any frame). Donor zone status was evaluated according to specific protocol considering upper tibio-fibular joint instability, pain, neurological complications, lateral collateral ligament insufficiency, or ankle complaints. Results Mean age at surgery was 30.1 years (SD 12.2). In respect to lesion sites, 22 were located in weight-bearing area of medial femoral condyle, 7 in lateral femoral condyle, 1 in trochlea, and 1 in patella. Mean follow-up was 110.1 months (SD 23.2). Mean area of lesion was 3.3 cm 2 (SD 1.7), and a variable number of cylinders were used, mean 2.5 (SD 1.3). Mean VAS score improved from 47.1 (SD 10.1) to 20.0 (SD 11.5); p = 0.00. Similarly, mean Lysholm score increased from 45.7 (SD 4.5) to 85.3 (SD 7.0); p = 0.00. The level of patient satisfaction was evaluated, and 28 patients declared to be satisfied/very satisfied and would do surgery again, while 3 declared as unsatisfied with the procedure and would not submit to surgery again. These three patients had lower clinical scores and kept complaints related to the original problem but unrelated to donor zone. MRI score significantly improved at 18–24 months comparing with pre-operative (p = 0.004). No radiographic or clinical complications related to donor zone with implication in activity were registered. Conclusions This work corroborates that mosaicplasty technique using autologous osteochondral graft from the upper tibio-fibular joint is effective to treat osteochondral defects in the knee joint. No relevant complications related to donor zone were registered

Mimicry of an HIV broadly neutralizing antibody epitope with a synthetic glycopeptide.

CAPRISA, 2017.Abstract available in pdf

Mercury accumulation in the sediment of the Western Mediterranean abyssal plain: A reliable archive of the late Holocene

Temporal reconstruction of Hg deposition from sediment archives is relatively straightforward in organic-rich or high sedimentation rate environments, such as lakes and ocean margins. To retrieve long-term records at regional or global scales, deep-sea sediments are more appropriate, but such records are scarce and their reliability has been questioned because of possible post-depositional Hg diagenetic remobilization. Here, we investigated the accumulation of Hg in the Balearic Abyssal Plain (2850 m deep) of the Western Mediterranean through a comprehensive characterization of the chemical and isotopic composition (organic carbon, nitrogen, sulfur, major and redox-sensitive elements) of sediment trap material and sediment cores. The analysis of material collected in the sediment traps, deployed at 250, 1440, and 2820 m, indicates that Hg is (i) partially re-emitted to the atmosphere and mobilized in the twilight zone and that (ii) the Hg downward flux depends on the primary production in surface waters, suggesting that organic matter (OM) acts as the main Hg-carrier phase. As the Hg concentrations of material collected in the traps vary little with depth but the Hg:Corg ratio of the settling particulate matter decreases with depth, Hg must be re-adsorbed onto the more refractory fraction of the settling OM. Results of selective chemical extractions of the sediment indicate that Hg is very weakly coupled to the iron cycle but strongly associated with sulfur, supporting the assumption that its vertical distribution was only weakly altered by diagenetic remobilization. In addition, the distributions of S and δ34S in the sedimentary column exclude the possibility that local volcanism impacted on Hg enrichment of the sediments. Accordingly, a reconstruction of Hg accumulation rates (Hg-AR) during the Late Holocene is readily achieved. Biological mixing and smoothing of the sediment record, as revealed by the distribution of radionuclides in surface sediments, was considered in the interpretation of the Hg-AR record. The first anthropogenic Hg signal recorded in the studied cores corresponds to the Iron Age and the Roman Empire period, as Hg-ARs rose from the baseline (0.7 ± 0.2 µg m-2 yr-1) to an average value of 2.2 ± 0.5 µg m-2 yr-1. The Hg-ARs return to baseline values at the decline of the Roman Empire, display a small increase during the Medieval Period (1.5 ± 0.5 µg m-2 yr-1), increase abruptly at the onset of the Industrial Era, leading to a ∼10-fold increase in Hg deposition in the last 120 years (8.9 ± 1.4 µg m-2 yr-1), and retreat progressively over the past 50 years

Hurricane Forecasting with the High-resolution NASA Finite-volume General Circulation Model

A high-resolution finite-volume General Circulation Model (fvGCM), resulting from a development effort of more than ten years, is now being run operationally at the NASA Goddard Space Flight Center and Ames Research Center. The model is based on a finite-volume dynamical core with terrain-following Lagrangian control-volume discretization and performs efficiently on massive parallel architectures. The computational efficiency allows simulations at a resolution of a quarter of a degree, which is double the resolution currently adopted by most global models in operational weather centers. Such fine global resolution brings us closer to overcoming a fundamental barrier in global atmospheric modeling for both weather and climate, because tropical cyclones and even tropical convective clusters can be more realistically represented. In this work, preliminary results of the fvGCM are shown. Fifteen simulations of four Atlantic tropical cyclones in 2002 and 2004 are chosen because of strong and varied difficulties presented to numerical weather forecasting. It is shown that the fvGCM, run at the resolution of a quarter of a degree, can produce very good forecasts of these tropical systems, adequately resolving problems like erratic track, abrupt recurvature, intense extratropical transition, multiple landfall and reintensification, and interaction among vortices