Hydrolysis of non-cognate aminoacyl-adenylates by a class II aminoacyl-tRNA synthetase lacking an editing domain

Aminoacyl-tRNA synthetases, a group of enzymes catalyzing aminoacyl-tRNA formation, may possess inherent editing activity to clear mistakes arising through the selection of non-cognate amino acid. It is generally assumed that both editing substrates, non-cognate aminoacyl-adenylate and misacylated tRNA, are hydrolyzed at the same editing domain, distant from the active site. Here, we present the first example of an aminoacyl-tRNA synthetase (seryl-tRNA synthetase) that naturally lacks an editing domain, but possesses a hydrolytic activity toward non-cognate aminoacyl-adenylates. Our data reveal that tRNA-independent pre-transfer editing may proceed within the enzyme active site without shuttling the non-cognate aminoacyl-adenylate intermediate to the remote editing site.     

Luminescent properties of 4‐aminobenzo‐15‐crown‐5 after preferential binding of ferric ions in aqueous solutions

We report a combined approach that introduces the use of 4‐aminobenzo‐15‐crown‐5 (4AB15C5) for the detection of ferric(III) ions by colorimetric, ultraviolet (UV)–visible light absorption, fluorescence, and live‐cell imaging techniques along with density functional theory (DFT) calculations. We have found that 4AB15C5 is sensitive and selective for binding ferric(III) ions in aqueous solutions. DFT calculations using the polarizable continuum model have been used to explain the strong binding of the ferric ion by 4AB15C5 in aqueous solutions. The detection limit in the fluorescence quenching measurements was found to be as low as 50 μM for the ferric ion with a determined Stern–Volmer constant of 1.52 × 10⁴ M^?1. Fluorescence intensity did not change for other ions tested, Fe²⁺, Co²⁺, Mn²⁺, Mg²⁺, Zn²⁺, Ca²⁺, NH₄⁺, Na⁺, and K⁺ ions. Live‐cell fluorescence imaging was also used to check the intracellular variations in ferric ion levels. Our spectroscopic data indicated that 4AB15C5 can bind ferric ions selectively in aqueous solutions.     

Microbial processes influencing methane emission from rice fields

Irrigated rice fields are an important source of atmospheric methane. In order to improve our understanding of the controlling processes, we measured in situ CH₄ emission and CH₄ oxidation in an Italian rice field in 1998 and 1999, and studied CH₄ production in soil and root samples. The CH₄ emission rates were correlated with diurnal temperature variations and showed pronounced seasonal and interannual variations. The contribution of CH₄ oxidation to total CH₄ flux, determined by specific inhibition with difluoromethane, decreased from 40% at the beginning to zero at the end of the season. The stable carbon isotopic composition of the emitted CH₄ also decreased. The CH₄‐oxidizing bacteria probably became limited by nitrogen as indicated by the seasonal decrease of NH₄⁺. Thus, CH₄ oxidation had little effect on CH₄ emission. Methane production on rice roots was relatively constant over the season. Methane production in soil slowly increased after flooding and was highest in the middle of the season. Pore water concentrations of CH₄ showed a similar seasonal pattern. In 1999, CH₄ production increased later in the season and reached lower rates than in 1998. An additional drainage in 1999 resulted in higher ferric iron concentrations, higher soil redox potentials and lower acetate concentrations. As a result, acetate‐utilizing methanogens were probably out‐competed by iron‐reducers so that a larger percentage of [2–¹⁴C]acetate was converted to ¹⁴CO₂ instead of ¹⁴CH₄. The residual CH₄ production was relatively low and was mainly due to H₂/CO₂‐dependent methanogenesis. Experiments with radioactive bicarbonate and with methyl fluoride as specific inhibitor showed that the theoretical ratio of 7:3 of methanogenesis from acetate vs. H₂/CO₂ was only reached later in the season when total CH₄ production was at the maximum. In conclusion, our results give a mechanistic explanation for the intraseasonal and interannual differences in CH₄ emission.     

Managing heavy metal toxicity stress in plants: Biological and biotechnological tools

The maintenance of ion homeostasis in plant cells is a fundamental physiological requirement for sustainable plant growth, development and production. Plants exposed to high concentrations of heavy metals must respond in order to avoid the deleterious effects of heavy metal toxicity at the structural, physiological and molecular levels. Plant strategies for coping with heavy metal toxicity are genotype-specific and, at least to some extent, modulated by environmental conditions. There is considerable interest in the mechanisms underpinning plant metal tolerance, a complex process that enables plants to survive metal ion stress and adapt to maintain growth and development without exhibiting symptoms of toxicity. This review briefly summarizes some recent cell biological, molecular and proteomic findings concerning the responses of plant roots to heavy metal ions in the rhizosphere, metal ion-induced reactions at the cell wall-plasma membrane interface, and various aspects of heavy metal ion uptake and transport in plants via membrane transporters. The molecular and genetic approaches that are discussed are analyzed in the context of their potential practical applications in biotechnological approaches for engineering increased heavy metal tolerance in crops and other useful plants.     

铁摄取调节子在细菌铁离子代谢中的调节及其机制

铁离子是大多数细菌生存所必需的营养物质,但是过多的铁离子通过芬顿反应产生的活性氧（reactive oxygen species, ROS）对细菌造成损伤。因此,细菌必须严格控制体内铁离子浓度。铁摄取调节子（ferric uptake regulator,Fur）是细菌铁离子代谢中最重要的调节子。Fur通过抑制或者激活基因的转录,来调节与铁摄取、利用和储存相关的基因,维持胞内铁离子浓度动态平衡。此外,Fur还参与细菌的氧化应激、抗酸能力、毒力和能量代谢等多种生物过程的调节。本文对Fur参与的生物过程及调节机制进行介绍,以期为进一步研究其他细菌Fur的调节机制,以及Fur在细菌应对环境变化中所起作用提供参考。     

Effect of selected plasmids on the serum sensitivity of Salmonella typhimurium strains with defined lipopolysaccharide core defects

Abstract The utilisation of pyruvate by a cell-free system of Aerobacter aerogenes 62-1, capable of synthesising aerobactin, has been found to be mediated by pyruvate oxidase (EC 1.2.3.3) with acetyl phosphate and CO₂ being formed as products.     

Effects of short-term drainage and aeration on the production of methane in submerged rice soil

Emission rates of CH₄ were measured in microcosms of submerged soil which were planted with rice. Drainage of the rice microcosms for 48 h resulted in drastically decreased CH₄ emission rates which only slowly recovered to the rates of the undrained controls. Drainage also resulted in drastically increased sulphate concentrations which only slowly decreased to nearly zero background values after the microcosms were submerged again. The mechanisms responsible for the decrease of CH₄ production by aeration were investigated in slurries of a loamy and a sandy Italian rice soil. Incubation of the soil slurries under anoxic conditions resulted first in the reduction of nitrate, sulphate and ferric iron before CH₄ production started. Incubation of the soil slurries for 48 h under air resulted in immediate and complete inhibition of CH₄ production. Although the soil slurries were then again incubated under anoxic conditions (N₂ atmosphere), the inhibition of CH₄ production persisted for more than 30 days. The redox potential of the soil increased after the aeration but returned within 15 days to the low values typical for CH₄ production. However, the concentrations of sulphate and of ferric iron increased dramatically after the aeration and stayed at elevated levels for the period during which CH₄ production was inhibited. These observations show that even brief exposure of the soil to O₂ allowed the production of sulphate and ferric iron from their reduced precursors. Elevated sulphate and ferric iron concentrations allowed sulphate-reducing and ferric iron-reducing bacteria to outcompete methanogenic bacteria on H₂ as common substrate. Indeed, concentrations of H₂ were decreased as long as sulphate and ferric iron were high so that the Gibbs free energy of CH₄ production from H₂/CO₂ was also increased (less exergonic). On the other hand, concentrations of acetate, the more important precursor for CH₄, were not much affected by the short aeration of the soil slurries, and the Gibbs free energy of CH₄ production from acetate was highly exergonic suggesting that acetotrophic methanogens were not outcompeted but were otherwise inhibited. Aeration also resulted in increased rates of CO₂ production and in a short-term increase of N₂O production. However, these increases were < 10% of the decreased production of CH₄ and did not represent a trade-off in terms of CO₂ equivalents. Hence, short-term drainage and aeration of submerged paddy fields may be a useful mitigation option for decreasing the emission of greenhouse gases.     

柠檬酸铁对过亚硝酸根硝化酪氨酸反应的影响

由一氧化氮和超氧阴离子迅速反应生成的过亚硝酸根(ONOO^-)是一种强细胞毒性物质. 使含酚基物质如酪氨酸等硝化,是过亚硝酸根损伤生物系统的重要途径之一. 研究了柠檬酸铁和草酸铁对过亚硝酸根硝化酪氨酸反应的影响.在生理pH条件下柠檬酸铁和草酸铁对硝化反应无影响. 在弱酸性条件下柠檬酸铁和草酸铁可催化硝化反应. 对pH影响铁配合物在硝化反应中的催化活性的原因进行了讨论.     

Gentisate 1,2-Dioxygenase from Xanthobacter polyaromaticivorans 127W

A putative gentisate 1,2-dioxygenase was encoded in the dibenzothiophene degradation gene cluster (dbd) from Xanthobacter polyaromaticivorans 127W. The deduced amino acid sequence showed high sequence similarity with gentisate dioxygenases from Pseudomonas alcaligenes (AAD49427, 65% identical), Bradyrhizobium japonicum (NP_766750, 64%), and P. aeruginosa (ZP_00135722, 54%), and moderate similarity with 1-hydroxy-2-naphthoate dioxygenase from Nocardioides sp. KP7 (BAA31235, 33%) and salicylate dioxygenase from Pseudaminobacter salicylatoxidans (AAQ91293, 33%). The enzyme, GDOxp, was heterologously produced in Escherichia coli and purified to homogeneity. GDOxp formed a tetramer and exhibited high dioxygenase activity against 1,4-dihydroxy 2-naphthoate as well as gentisate, suggesting unusually broad substrate specificity. GDOxp easily released ferrous ion under unfavorable temperature and pH conditions to become an inactive monomer protein. An inactive monomer protein can reconstitute a tetramer structure and restore enzyme activity in a cooperative manner upon the addition of ferrous ion. Chymotryptic digestion and protein truncation experiments suggested that the N-terminal region is important for the tetramerization of GDOxp.     

Structure and Function of P19, a High-Affinity Iron Transporter of the Human Pathogen Campylobacter jejuni

Campylobacter jejuni, a major cause of acute bacterial diarrhea in humans, expresses numerous proteins to import diverse forms of essential iron. The expression of p19 and an adjacent iron transporter homologue (ftr1) is strongly induced upon iron limitation, suggesting a function in iron acquisition. Here, we show that the loss of P19 alone is detrimental to growth on iron-restricted media. Furthermore, metal binding analysis demonstrates that recombinant P19 has distinct copper and iron binding sites. Crystal structures of P19 have been solved to 1.41 Å resolution, revealing an immunoglobulin-like fold. A P19 homodimer in which both monomers contribute ligands to two equivalent copper sites located adjacent to methionine-rich patches is observed. Copper coordination occurs via three histidine residues (His42, His95, and His132) and Met88. A solvent channel lined with conserved acidic residues leads to the copper site. Soaking crystals with a solution of manganese as iron analog reveals a second metal binding site in this solvent channel (metal-metal distance, 7.7 Å). Glu44 lies between the metal sites and displays multiple conformations in the crystal structures, suggesting a role in regulating metal-metal interaction. Dimerization is shown to be metal dependent in vitro and is detected in vivo by cross-linking.