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Background

Aquaporins (AQPs), members of a superfamily of transmembrane channel proteins, are ubiquitous in all domains of life. They fall into a number of branches that can be functionally categorized into two major sub-groups: i) orthodox aquaporins, which are water-specific channels, and ii) aquaglyceroporins, which allow the transport of water, non-polar solutes, such as urea or glycerol, the reactive oxygen species hydrogen peroxide, and gases such as ammonia, carbon dioxide and nitric oxide and, as described in this review, metalloids.

Scope of review

This review summarizes the key findings that AQP channels conduct bidirectional movement of metalloids into and out of cells.

Major conclusions

As(OH)3 and Sb(OH)3 behave as inorganic molecular mimics of glycerol, a property that allows their passage through AQP channels. Plant AQPs also allow the passage of boron and silicon as their hydroxyacids, boric acid (B(OH)3) and orthosilicic acid (Si(OH)4), respectively. Genetic analysis suggests that germanic acid (GeO2) is also a substrate. While As(III), Sb(III) and Ge(IV) are toxic metalloids, borate (B(III)) and silicate (Si(IV)) are essential elements in higher plants.

General significance

The uptake of environmental metalloids by aquaporins provides an understanding of (i) how toxic elements such as arsenic enter the food chain; (ii) the delivery of arsenic and antimony containing drugs in the treatment of certain forms of leukemia and chemotherapy of diseases caused by pathogenic protozoa; and (iii) the possibility that food plants such as rice could be made safer by genetically modifying them to exclude arsenic while still accumulating boron and silicon. This article is part of a Special Issue entitled Aquaporins.  相似文献   
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Microbial arsenic: from geocycles to genes and enzymes   总被引:29,自引:0,他引:29  
Arsenic compounds have been abundant at near toxic levels in the environment since the origin of life. In response, microbes have evolved mechanisms for arsenic resistance and enzymes that oxidize As(III) to As(V) or reduce As(V) to As(III). Formation and degradation of organoarsenicals, for example methylarsenic compounds, occur. There is a global arsenic geocycle, where microbial metabolism and mobilization (or immobilization) are important processes. Recent progress in studies of the ars operon (conferring resistance to As(III) and As(V)) in many bacterial types (and related systems in Archaea and yeast) and new understanding of arsenite oxidation and arsenate reduction by respiratory-chain-linked enzyme complexes has been substantial. The DNA sequencing and protein crystal structures have established the convergent evolution of three classes of arsenate reductases (that is classes of arsenate reductases are not of common evolutionary origin). Proposed reaction mechanisms in each case involve three cysteine thiols and S-As bond intermediates, so convergent evolution to similar mechanisms has taken place.  相似文献   
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The toxic metalloid arsenic is widely disseminated in the environment and causes a variety of health and environment problems. As an adaptation to arsenic-contaminated environments, organisms have developed resistance systems. Many ars operons contain only three genes, arsRBC. Five gene ars operons have two additional genes, arsD and arsA, and these two genes are usually adjacent to each other. ArsA from Escherichia coli plasmid R773 is an ATPase that is the catalytic subunit of the ArsAB As(III) extrusion pump. ArsD was recently identified as an arsenic chaperone to the ArsAB pump, transferring the trivalent metalloids As(III) and Sb(III) to the ArsA subunit of the pump. This increases the affinity of ArsA for As(III), resulting in increased rates if extrusion and resistance to environmentally relevant concentrations of arsenite. ArsD is a homodimer with three vicinal cysteine pairs, Cys12–Cys13, Cys112–Cys113 and Cys119–Cys120, in each subunit. Each vicinal pair binds one As(III) or Sb(III). ArsD mutants with alanines substituting for Cys112, Cys113, Cys119 or Cys120, individually or in pairs or truncations lacking the vicinal pairs, retained ability to interact with ArsA, to activate its ATPase activity. Cells expressing these mutants retained ArsD-enhanced As(III) efflux and resistance. In contrast, mutants with substitutions of conserved Cys12, Cys13 or Cys18, individually or in pairs, were unable to activate ArsA or to enhance the activity of the ArsAB pump. It is proposed that ArsD residues Cys12, Cys13 and Cys18, but not Cys112, Cys113, Cys119 or Cys120, are required for delivery of As(III) to and activation of the ArsAB pump.  相似文献   
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Arsenite oxidation by the facultative chemolithoautotroph NT-26 involves a periplasmic arsenite oxidase. This enzyme is the first component of an electron transport chain which leads to reduction of oxygen to water and the generation of ATP. Involved in this pathway is a periplasmic c-type cytochrome that can act as an electron acceptor to the arsenite oxidase. We identified the gene that encodes this protein downstream of the arsenite oxidase genes (aroBA). This protein, a cytochrome c552, is similar to a number of c-type cytochromes from the α-Proteobacteria and mitochondria. It was therefore not surprising that horse heart cytochrome c could also serve, in vitro, as an alternative electron acceptor for the arsenite oxidase. Purification and characterisation of the c552 revealed the presence of a single heme per protein and that the heme redox potential is similar to that of mitochondrial c-type cytochromes. Expression studies revealed that synthesis of the cytochrome c gene was not dependent on arsenite as was found to be the case for expression of aroBA.  相似文献   
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In rat heart mitochondria, auranofin, arsenite, diamide, and BCNU increase H2O2 formation, further stimulated by antimycin. However, in submitochondrial particles, H2O2 formation and oxygen uptake are not affected, indicating that these substances do not alter respiration. Mitochondria are also able to rapidly metabolize added H2O2 in a process partially prevented by BCNU or auranofin. Calcium does not modify the production of H2O2 and the mitochondrial thioredoxin system is not affected by calcium ions. Auranofin, arsenite, and diamide determine a large mitochondrial permeability transition, while BCNU and acetoacetate are ineffective. Thiols and glutathione are modified only by BCNU and diamide. However, all the compounds tested cause the release of cytochrome c that occurs also in the absence of mitochondrial swelling. In conclusion, the compounds utilized share the common feature of shifting the mitochondrial thiol-linked redox balance towards a more oxidized condition that is responsible of the observed effects.  相似文献   
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Here, we describe the characterization of the [2Fe-2S] clusters of arsenite oxidases from Rhizobium sp. NT-26 and Ralstonia sp. 22. Both reduced Rieske proteins feature EPR signals similar to their homologs from Rieske-cyt b complexes, with g values at 2.027, 1.88, and 1.77. Redox titrations in a range of pH values showed that both [2Fe-2S] centers have constant Em values up to pH 8 at ∼+210 mV. Above this pH value, the Em values of both centers are pH-dependent, similar to what is observed for the Rieske-cyt b complexes. The redox properties of these two proteins, together with the low Em value (+160 mV) of the Alcaligenes faecalis arsenite oxidase Rieske (confirmed herein), are in line with the structural determinants observed in the primary sequences, which have previously been deduced from the study of Rieske-cyt b complexes. Since the published Em value of the Chloroflexus aurantiacus Rieske (+100 mV) is in conflict with this sequence analysis, we re-analyzed membrane samples of this organism and obtain a new value (+200 mV). Arsenite oxidase activity was affected by quinols and quinol analogs, which is similar to what is found with the Rieske-cyt b complexes. Together, these results show that the Rieske protein of arsenite oxidase shares numerous properties with its counterpart in the Rieske-cyt b complex. However, two cysteine residues, strictly conserved in the Rieske-cyt b-Rieske and considered to be crucial for its function, are not conserved in the arsenite oxidase counterpart. We discuss the role of these residues.  相似文献   
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