An automated pipeline to screen membrane protein 2D crystallization

Electron crystallography relies on electron cryomicroscopy of two-dimensional (2D) crystals and is particularly well suited for studying the structure of membrane proteins in their native lipid bilayer environment. To obtain 2D crystals from purified membrane proteins, the detergent in a protein–lipid–detergent ternary mixture must be removed, generally by dialysis, under conditions favoring reconstitution into proteoliposomes and formation of well-ordered lattices. To identify these conditions a wide range of parameters such as pH, lipid composition, lipid-to-protein ratio, ionic strength and ligands must be screened in a procedure involving four steps: crystallization, specimen preparation for electron microscopy, image acquisition, and evaluation. Traditionally, these steps have been carried out manually and, as a result, the scope of 2D crystallization trials has been limited. We have therefore developed an automated pipeline to screen the formation of 2D crystals. We employed a 96-well dialysis block for reconstitution of the target protein over a wide range of conditions designed to promote crystallization. A 96-position magnetic platform and a liquid handling robot were used to prepare negatively stained specimens in parallel. Robotic grid insertion into the electron microscope and computerized image acquisition ensures rapid evaluation of the crystallization screen. To date, 38 2D crystallization screens have been conducted for 15 different membrane proteins, totaling over 3000 individual crystallization experiments. Three of these proteins have yielded diffracting 2D crystals. Our automated pipeline outperforms traditional 2D crystallization methods in terms of throughput and reproducibility.     

湖泊氮素氧化及脱氮过程研究进展

自然界中氮的生物地球化学循环主要由微生物驱动,由固氮作用、硝化作用、反硝化作用和氨化作用来完成。过去数十年间,随着异养硝化、厌氧氨氧化和古菌氨氧化作用的发现,人们对环境中氮素循环认识逐步深入,提出了多种脱氮途径新假说。对湖泊生态系统中氮素的输入、输出及其在水体、沉积物和水土界面的迁移转化过程进行了概括,对湖泊生态系统中反硝化和厌氧氨氧化脱氮机理及脱氮效率的最新研究进展进行了探讨,并对以后的氮素循环研究进行了展望。     

Expression and characterization of the Escherichia coli fdo locus and a possible physiological role for aerobic formate dehydrogenase.

In the presence of nitrate, the major anaerobic respiratory pathway includes formate dehydrogenase (FDH-N) and nitrate reductase (NAR-A), which catalyze formate oxidation coupled to nitrate reduction. Two aerobically expressed isoenzymes, FDH-Z and NAR-Z, have been recently characterized. Enzymatic analysis of plasmid subclones carrying min 88 of the Escherichia coli chromosome was consistent with the location of the fdo locus encoding FDH-Z between the fdhD and fdhE genes which are necessary for the formation of both formate dehydrogenases. The fdo locus produced three proteins (107, 34, and 22 kDa) with sizes similar to those of the subunits of the purified FDH-N. In support to their structural role, these polypeptides were recognized by antibodies specific to FDH-N. Expression of a chromosomal fdo-uidA operon fusion was induced threefold by aerobic growth and about twofold by anaerobic growth in the presence of nitrate. However, it was independent of the two global regulatory proteins FNR and ArcA, which control genes for anaerobic and aerobic functions, respectively, and of the nitrate response regulator protein NARL. In contrast, a mutation affecting either the nucleoid-associated H-NS protein or the CRP protein abolished the aerobic expression. A possible role for FDH-Z during the transition from aerobic to anaerobic conditions was examined. Synthesis of FDH-Z was maximal at the end of the aerobic growth and remained stable after a shift to anaerobiosis, whereas FDH-N production developed only under anaerobiosis. Furthermore, in an fnr strain deprived of both FDH-N and NAR-A activities, aerobically expressed FDH-Z and NAR-Z enzymes were shown to reduce nitrate at the expense of formate under anaerobic conditions, suggesting that this pathway would allow the cell to respond quickly to anaerobiosis.     

Challenging protein purification from anammox bacteria

The anaerobic ammonium oxidation (anammox) is a fascinating microbial pathway contributing to the global biogeochemical nitrogen cycle. The anammox pathway of nitrogen conversion can only be elucidated after the responsible proteins have been purified and characterised. The anammox bacteria have a complex cell envelope consisting of protein and lipopolysaccharide and they grow in dense cell aggregates. Preparing cell extract and purifying proteins from the cell aggregates is hampered by the extracellular polymeric material and by gel formation. It was demonstrated that protein-protein (i.e. disulfide formation) as well as protein-polysaccharide interaction caused this gel formation in extracts. Cell extract gelled upon freezing/thawing and boiling. Additionally, proteins aggregated on various chromatography media upon concentration and during desalting. The polysaccharides clogged the matrix of chromatographic materials and the pores of ultrafiltration membranes. The precipitation of proteins and polysaccharides caused very low resolution and streaking on SDS- and two-dimensional polyacrylamide gels. The present work describes the potential causes for gel formation in anammox cell extracts. Optimized protocols for sample preparation for polyacrylamide gel electrophoresis and ion exchange chromatography are presented. High-resolution gel electrophoresis of the cell extract was achieved after clarification from polymeric substances with denaturating phenol extraction and the purification of a 10 kDa cytochrome c is presented as an example.     

Oxidation of deoxy myoglobin by [Fe(CN)6]3-.

The ability of myoglobin (Mb) to reversibly bind O2 and other ligands has been well characterized. Mb also participates with a variety of redox metals to form metmyoglobin (metMb). By using an anaerobic stopped-flow device we have measured outer-sphere oxidation by [Fe(CN)6]3 of native sperm whale myoglobin, recombinant wild-type Mb, and a series of mutant Mb proteins in which the distal His-64 was changed to Gly, Phe, Leu or Val. Second-order rate constants for oxidation of mutant proteins are 10-15 times greater than for recombinant or native (kox approximately 10(6) M-1 s-1). We attribute the reduced rate of oxidation of wild-type protein to a higher reorganization energy imposed by the presence of the unique water/His-64/heme interaction, which is absent in the mutant proteins.     

Renaturation of recombinant proteins produced as inclusion bodies

Expression of recombinant proteins in Escherichia coli often results in the formation of insoluble inclusion bodies. Within the last few years specific methods and strategies have been developed to prepare active proteins from these inclusion bodies. These methods include (i) isolation of inclusion bodies after disintegration of cells by mechanical forces and purification by washing with detergent solutions or low concentrations of denaturant, (ii) solubilization of inclusion bodies with high concentrations of urea or guanidine-hydrochloride in combination with reducing reagents, and (iii) renaturation of the proteins including formation of native disulphide bonds. Renatured and native disulphide bond formation are accomplished by (a) either air oxidation, (b) glutathione reoxidation starting from reduced material, or (c) disulphide interchange starting from mixed disulphides containing peptides. The final yield of renatured proteins can be increased by adding low concentrations of denaturant during renaturation.     

Degeneration of biogenic superparamagnetic magnetite

Magnetite crystals precipitated as a consequence of Fe(III) reduction by Shewanella algae BrY after 265 h incubation and 5-year anaerobic storage were investigated with transmission electron microscopy, Mössbauer spectroscopy and X-ray diffraction. The magnetite crystals were typically superparamagnetic with an approximate size of 13 nm. The lattice constants of the 265 h and 5-year crystals are 8.4164Å and 8.3774Å, respectively. The Mössbauer spectra indicated that the 265 h magnetite had excess Fe(II) in its crystal-chemistry (Fe³⁺_1.990Fe²⁺_1.015O₄) but the 5-year magnetite was Fe(II)-deficient in stoichiometry (Fe³⁺_2.388Fe²⁺_0.419O₄). Such crystal-chemical changes may be indicative of the degeneration of superparamagnetic magnetite through the aqueous oxidization of Fe(II) anaerobically, and the concomitant oxidation of the organic phases (fatty acid methyl esters) that were present during the initial formation of the magnetite. The observation of a corona structure on the aged magnetite corroborates the anaerobic oxidation of Fe(II) on the outer layers of magnetite crystals. These results suggest that there may be a possible link between the enzymatic activity of the bacteria and the stability of Fe(II)-excess magnetite, which may help explain why stable nano-magnetite grains are seldom preserved in natural environments.     

Lysine methylation as a routine rescue strategy for protein crystallization

Crystallization remains a critical step in X-ray structure determination. Because it is not generally possible to rationally predict crystallization conditions, commercial screens have been developed which sample a wide range of crystallization space. While this approach has proved successful in many cases, a significant number of proteins fail to crystallize despite being soluble and monodispersed. It is established that chemical modification can facilitate the crystallization of otherwise intractable proteins. Here we describe a method for the reductive methylation of lysine residues which is simple, inexpensive, and efficient, and report on its application to ten proteins. We describe the effect of methylation on the physico-chemical properties of these proteins, and show that it led to diffraction-quality crystals from four proteins and structures for three that had hitherto proved refractory to crystallization. The method is suited to both low- and high-throughput laboratories.     

Identification of oxidized derivatives of neuroketals

Oxidative stress and protein aggregation have been implicated in the pathogenesis of neurodegenerative diseases. The formation of neuroprostanes, isoprostane-like compounds formed from oxidation of docosahexaenoic acid, which is uniquely enriched in the brain, is increased in Alzheimer's disease. We recently identified the formation of a new class of highly reactive gamma-keto aldehydes, neuroketals, in vivo as products of the neuroprostane pathway. Neuroketals adduct to lysine residues of proteins with remarkable rapidity and induce cross-linking. Because neuroketals have either a 1,4-pentadiene or 1,4,7-octatriene side chain structure, we hypothesized that they could undergo further oxidation to form neuroketals with an additional hydroxyl group. Oxidation of docosahexaenoic acid in vitro yielded a series of compounds that were confirmed to be oxidized neuroketals by mass spectrometric analyses. Analysis of oxidized neuroketal adducts during oxidation of docosahexaenoic acid in the presence of lysine revealed the formation of oxidized Schiff base and hydroxylactam adducts. Oxidized hydroxylactam neuroketal-lysyl protein adducts, analyzed after digestion of proteins to individual amino acids, were not detected in nonoxidized rat brain synaptosomes but were readily detected following oxidation of synaptosomes. These studies indicate that neuroketals can undergo further oxidation, which in turn suggests that measurement of only unoxidized neuroketal adducts likely underestimates the amount of neuroketal adducts present in the brain in disorders of oxidant stress.     

Parameters for crystal growth of ribosomal subunits

A systematic analysis of the parameters that control the crystal growth of the large subunit of ribosomes from B stearothermophilus has been carried out. Several parameters have been identified and classified according to their significance. It was found that only biologically active particles can crystallize and that the critical period for the crystallization process is the first few days, during which changes in the volume and content of the crystallization drop are of importance for both nucleation and crystal growth. Consequently, an experimental procedure for fine control of these variables has been developed. As a result of these studies, the reproducibility of crystal formation was increased, and larger and more stable crystals have been obtained.     

Anaerobic granulation technology for wastewater treatment

Anaerobic wastewater treatment using granular sludge reactors is a developing technology, in which granular sludge is the core component. So far, around 900 anaerobic granular sludge units have been operated worldwide. Although intensive research attention has been given to anaerobic granules in the past 20 years, the mechanisms responsible for anaerobic granulation and the strategy of how to expedite substantially the formation of granular sludge have not yet been completely clear. This paper reviews the mode of anaerobic granulation, including the mechanisms and models for anaerobic granulation, major factors influencing anaerobic granulation, characteristics of anaerobic granules, anaerobic granulation in other types of reactors, industrial application of anaerobic granulation technology and neural fuzzy model-based control strategy developed for anaerobic systems. Some approaches for future research are outlined.     

Mitochondrial function and reactive oxygen species action in relation to boar motility

Flow cytometric assays of viable boar sperm were developed to measure reactive oxygen species (ROS) formation (oxidization of hydroethidine to ethidium), membrane lipid peroxidation (oxidation of lipophilic probe C(11)-BODIPY(581/591)), and mitochondrial inner transmembrane potential (DeltaPsi(m); aggregation of mitochondrial probe JC-1) during hypothermic liquid storage and freeze-thawing of boar semen and to investigate relationships among ROS, motility, DeltaPsi(m), and ATP production. Basal ROS formation and membrane lipid peroxidation were low in viable sperm of both fresh and frozen-thawed semen, affecting < or =4%. Sperm in fresh, liquid-stored and frozen-thawed semen appeared to be equally susceptible to the activity ROS generators xanthine/xanthine oxidase, FeSO(4)/ascorbate, and hydrogen peroxide (H(2)O(2)). Of the ROS generators tested, FeSO(4)/ascorbate was specific for membrane lipid peroxidation, whereas menadione, xanthine/xanthine oxidase, and H(2)O(2) were specific for oxidization of hydroethidine. Menadione (30microM) and H(2)O(2) (300microM) decreased (P<0.05) motility by 90% during 60min of incubation. Menadione decreased (P<0.05) the incidence of sperm with high DeltaPsi(m) by 95% during 60min of the incubation, although ATP content was not decreased (P>0.05) until 120min. In contrast, H(2)O(2) did not affect DeltaPsi(m) or ATP at any time. The formation of ROS was not associated with any change in viability (90%) for either menadione or H(2)O(2) through 120min. Overall, the inhibitory affects of ROS on motility point to a mitochondrial-independent mechanism. The reduction in motility may have been due to an ROS-induced lesion in ATP utilization or in the contractile apparatus of the flagellum.     

Novel microbial nitrogen removal processes

The present-day wastewater treatment practices can be significantly improved through the introduction of new microbial treatment technologies. Recently, several new processes for nitrogen removal have been developed. These new nitrogen removal technologies provide practicable options for treating nitrogen-laden wastewaters. The new processes are based on partial nitrification of ammonium to nitrite combined with anaerobic ammonium oxidation. These processes include the single reactor system for high ammonia removal over nitrite (SHARON) process, which involves part conversion of ammonium to nitrite; the anaerobic ammonium oxidation (ANAMMOX) process, which involves anaerobic ammonium oxidation; and the completely autographic nitrogen removal over nitrite (CANON) process, which involves nitrogen removal within one reactor under oxygen-limited conditions. These new processes target the removal of nitrogen from wastewaters containing significant quantities of ammonium.     

Methyl-coenzyme M reductase and the anaerobic oxidation of methane in methanotrophic Archaea

Recent biochemical and metagenomic data indicate that not yet cultured Archaea that are closely related to methanogenic Archaea of the order of Methanosarcinales are involved in the anaerobic oxidation of methane in marine sediments. The DNA from the methanotrophic Archaea has been shown to harbor gene homologues for methyl-coenzyme M reductase, which in methanogenic Archaea catalyses the methane-forming reaction. In microbial mats catalyzing anaerobic oxidation of methane, this nickel enzyme has been shown to be present in concentrations of up to 10% of the total extracted proteins.     

Anaerobic multiphasic gel electrophoresis of the molybdoproteins in extracts of Clostridium pasteurianum

Simple procedures using multiphasic buffer systems for anaerobic electrophoresis have been devised to identify oxygen-labile metalloproteins. An anaerobic slab gel apparatus was developed with cooling and design for anaerobic conditions. Included is a procedure to remove sample wells after stacking proteins in a crude extract, to prevent streaking (background) caused by continuous leakage of "nonstacked protein" from the sample wells. Identification of eleven Mo zones in extracts of Clostridium pasteurianum demonstrates the usefulness of the technique in identifying radiolabeled oxygen-labile proteins in cell-free crude lysates.     

Geochemical characteristics of the carbonate constructions formed during microbial oxidation of methane under anaerobic conditions

The aragonite constructions of the Black Sea are formed in a stable anaerobic zone and are a perfect object to study the natural mechanism of anaerobic methane oxidation. The most probable pathway of methane oxidation is its methanogen-mediated reaction with bicarbonates, dissolved in seawater, with the formation of water and acetate, which is then consumed by other components of the anaerobic community. Comparison of the delta 13C values of carbonate minerals and organic matter once more demonstrated that the formation of the organic matter of biomass is accompanied by intense fractionation of carbon isotopes, as a result of which the total organic matter of biomass acquires an extremely light isotopic composition, characterized by delta 13C values as low as -83.8@1000.     

Contemporary techniques for detecting and identifying proteins susceptible to reversible thiol oxidation

Elevated protein oxidation is a widely reported hallmark of most major diseases. Historically, this 'oxidative stress' has been considered causatively detrimental, as the protein oxidation events were interpreted simply as damage. However, recent advances have changed this antiquated view; sensitive methodology for detecting and identifying proteins susceptible to oxidation has revealed a fundamental role for this modification in physiological cell signalling during health. Reversible protein oxidation that is dynamically coupled with cellular reducing systems allows oxidative protein modifications to regulate protein function, analogous to phosphoregulation. However, the relatively labile nature of many reversible protein oxidation states hampers the reliable detection and identification of modified proteins. Consequently, specialized methods to stabilize protein oxidation in combination with techniques to detect specific types of modification have been developed. Here, these techniques are discussed, and their sensitivity, selectivity and ability to reliably identify reversibly oxidized proteins are critically assessed.     

Neutrophilic lithotrophic iron-oxidizing prokaryotes and their role in the biogeochemical processes of the iron cycle

Biology of lithotrophic neutrophilic iron-oxidizing prokaryotes and their role in the processes of the biogeochemical cycle of iron are discussed. This group of microorganisms is phylogenetically, taxonomically, and physiologically heterogeneous, comprising three metabolically different groups: aerobes, nitratedependent anaerobes, and phototrophs; the latter two groups have been revealed relatively recently. Their taxonomy and metabolism are described. Materials on the structure and functioning of the electron transport chain in the course of Fe(II) oxidation by members of various physiological groups are discussed. Occurrence of iron oxidizers in freshwater and marine ecosystems, thermal springs, areas of hydrothermal activity, and underwater volcanic areas are considered. Molecular genetic techniques were used to determine the structure of iron-oxidizing microbial communities in various natural ecosystems. Analysis of stable isotope fractionation of ^56/54Fe in pure cultures and model experiments revealed a predominance of biological oxidation over abiotic ones in shallow aquatic habitats and mineral springs, which was especially pronounced under microaerobic conditions at the redox zone boundary. Discovery of anaerobic bacterial Fe(II) oxidation resulted in development of new hypotheses concerning the possible role of microorganisms and the mechanisms of formation of the major iron ore deposits during Precambrian era until the early Proterozoic epoch. Paleobiological data are presented on the microfossils and specific biomarkers retrieved from ancient ore samples and confirming involvement of anaerobic biogenic processes in their formation.