嗜酸硫杆菌属硫氧化系统研究进展

硫化矿的酸溶解和化学氧化过程中(H 和Fe3 作用下,金属硫化矿中分解),伴随着硫元素转变成多聚硫S8或硫代硫酸盐的过程。对嗜酸硫杆菌属硫氧化过程的研究表明,胞外环状多聚硫S8可能通过细胞外膜蛋白巯基活化成线状-SnH后,被转运到细胞周质区域,进而被硫加双氧酶氧化成SO32-,活化过程中同时生成少量H2S;这些酶促反应不需要辅助因子参与,不释放电子。胞外硫代硫酸盐通过未知途径进入细胞周质。细胞周质中的SO32-主要经由亚硫酸-受体氧化还原酶氧化成SO42-,S2O32-可能经由硫代硫酸盐-辅酶Q氧化还原酶、硫代硫酸盐脱氢酶、连四硫酸盐水解酶等氧化为硫酸,少量H2S则经由硫化物-辅酶Q氧化还原酶氧化为多聚硫,后者再经由SO32-和S2O32-氧化生成最后产物SO42-。这些生物氧化过程释放的电子进入呼吸链参与产生细菌生长代谢所需的能量。然而,关于A.ferrooxidans硫氧化系统中各种硫化合物的酶催化氧化机制的研究仍很缺乏,胞内外硫化合物的转运机制、是否存在胞外酶催化氧化等仍然有待解决。另外,硫的型态和价态、酶催化反应的细胞微区域以及硫氧化系统中一些关键酶的分离及其表达基因的鉴定等问题都还有待进一步研究。基于对这些事实的分析,提出了一个嗜酸硫杆菌属硫氧化系统的模型。     

嗜酸硫杆菌在工农业中的应用

嗜酸硫杆菌(属)(Acidithiobacillus spp.)能够氧化亚铁、硫或还原性无机硫化合物(reduced inorganic sulfur compounds,RISCs)获得能量,固定二氧化碳,是一类典型的嗜酸性化能自养微生物。嗜酸硫杆菌广泛分布于酸性矿水、热泉等酸性环境中,是地球生态系统硫和铁元素循环的主要推动者。嗜酸硫杆菌独特的生理代谢特征和极端环境适应性,使其广泛应用于生物浸出领域。本文综述了嗜酸硫杆菌的生理代谢特征和极端环境下的适应机制,阐述了嗜酸硫杆菌在工农业中的应用,讨论了面向国家重大需求,嗜酸硫杆菌在今后的主要研究方向和需要解决的关键科学问题,为嗜酸硫杆菌在生理代谢、环境适应和工农业应用的研究提供重要的线索和启示。     

嗜热古菌异化型硫氧化途径的研究进展

微生物参与的还原性无机硫化合物的氧化过程是硫地球化学循环的重要组成部分,也可应用于生物冶金工业及酸性矿水治理等方面。嗜热古菌是高温环境中存在的一群特殊的微生物,其所参与的异化型硫氧化途径复杂多样,涉及众多氧化还原酶以及硫转运蛋白。本文将结合我们的研究工作,就参与异化型硫氧化代谢过程的嗜热古菌的种类,以及它们所参与的硫氧化过程进行系统的介绍。     

硫氧化细菌的种类及硫氧化途径的研究进展

硫,作为生物必需的大量营养元素之一,参与了细胞的能量代谢与蛋白质、维生素和抗生素等物质代谢。自然界中,硫以多种化学形态存在,包括单质硫、还原性硫化物、硫酸盐和含硫有机物。硫氧化是硫元素生物地球化学循环的重要组成部分,通常是指单质硫或还原性硫化物被微生物氧化的过程。硫氧化细菌种类繁多,其硫氧化相关基因、酶和途径也多种多样。近几年,相关方面的研究已取得很多进展,但在不同层面仍存在一些尚未解决的科学问题。本文主要围绕硫氧化细菌的种类及硫氧化途径的研究进展进行了综述。     

嗜酸性硫杆菌抗铜机制研究进展

嗜酸性硫杆菌是一类重要的浸矿微生物,其抗铜机制研究备受人们关注.本文在分析相关文献的基础上,从嗜酸性硫杆菌对铜的耐受能力、细胞质中铜的外排、细胞周质中铜浓度的控制、无机多聚磷酸盐参与铜的解毒、新发现的基因组岛和氧化压力应激反应等方面对当前的研究进展进行综述,并对未来相关研究方向做出展望,旨在为嗜酸性硫杆菌抗铜机制的深入研究提供参考.     

嗜酸性硫杆菌群体感应系统研究进展

嗜酸性硫杆菌(Acidithiobacillus spp.)是一类重要的极端环境微生物与工业微生物。该类细菌通过氧化硫或亚铁获得电子以固定二氧化碳进行自养生长,是驱动矿山环境酸化和重金属溶出的关键菌群,也是生物冶金等微生物浸出技术中的核心菌群。群体感应(quorum sensing, QS)系统是细菌种内及种间信息交流的重要方式,广泛分布于嗜酸性硫杆菌等化能自养微生物中,比如类似于LuxI/R的AfeI/R系统。系统介绍近年来嗜酸性硫杆菌菌体感应系统研究成果,尤其是在AfeI/R种群分布、生物学功能、调节机制及其应用研究中的新发现与新理论。讨论今后嗜酸性硫杆菌群体感应系统研究的主要方向及需要解决的关键科学问题,以促进极端微生物群体感应系统理论研究的开展与产业应用技术的开发。     

硫杆菌的分子遗传学研究

硫杆菌（丁litKucjllSS）是一类革兰氏阴性的化能无机营养细菌,也是分布最广,研究得最多,经济意义很大的硫氧化细菌。该属中的氧化硫硫杆菌（T．th。whns）和氧化亚铁流杆菌（T．fer－rtx）xlua叫是极端嗜酸性的专性自养细菌,最适因为2,0～3．5,广泛分布于流化矿床的酸性废水中。这类细菌很早就被广泛应用于贵重金属的浸出和回收,特别适合于从低品位的矿石中浸出稀有资重金属,主要是通过氧化FeSO和Fe＆产生Fe”氧化剂,氧化金属硫化物使之变成可溶性的硫酸盐形式,从而回收有用金属。这种方法具有低成本,低能耗,无污染等特点…     

冲绳海槽热液区可培养硫氧化细菌多样性及其硫氧化特性

冲绳海槽热液区独特的地质环境孕育了特殊的生物群落,硫氧化细菌作为生物地球化学循环的重要参与者在热液生态系统中发挥着至关重要的作用。【目的】通过硫氧化菌株的分离培养揭示冲绳海槽热液区可培养硫氧化细菌的多样性和硫氧化活性。【方法】采用多种培养基对冲绳海槽热液区不同沉积物样品中的硫氧化细菌进行富集培养和分离纯化;利用16S rRNA基因序列确定硫氧化细菌的分类地位并进行系统发育分析;采用碘量法对典型硫氧化菌株硫氧化活性进行检测。【结果】本研究从冲绳海槽热液区样品中共分离鉴定85株硫氧化细菌,分属于α-变形菌纲、γ-变形菌纲、放线菌门和厚壁菌门,优势属为氢弧菌属(Hydrogenovibrio)、拉布伦氏菌属(Labrenzia)、深海海旋菌属(Thalassospira)和海杆状菌属(Marinobacter)。硫氧化活性检测结果表明,7株典型硫氧化菌株对硫代硫酸钠的降解活性介于31%–100%之间,其中泰坦尼克号盐单胞菌SOB56 (Halomonas titanicae SOB56)、南极海杆状菌SOB93(Marinobacter antarcticus SOB93)、印度硫氧化粗杆菌SOB107 (Thioclava indica SOB107)和嗜温氢弧菌CJG136 (Hydrogenovibrio thermophiles CJG136)可以完全降解硫代硫酸钠。【结论】冲绳海槽热液区可培养硫氧化细菌的多样性丰富,为研究该热液区的硫循环过程提供了实验材料和理论基础,多种硫氧化活性菌株的获得极大地丰富了菌种资源,为探究深海热液区硫循环的能量代谢途径和分子机制奠定基础。     

湖泊硫循环微生物研究进展

湖泊是响应气候和环境变化的关键生态系统,是研究元素(如碳、氮和硫等)生物地球化学循环的热点环境。湖泊(尤其咸盐湖)具有硫酸盐含量高且含硫化合物种类丰富的特点,因而湖泊中硫元素生物地球化学循环过程非常活跃。微生物是驱动湖泊硫循环的重要推手。因此,研究湖泊中微生物参与的硫元素生物地球化学循环过程以及相关微生物类群构成,对于深入探索微生物在湖泊生态系统中的作用具有重要意义。本文综述了湖泊中驱动硫循环的微生物(硫氧化菌和硫酸盐还原菌)种群多样性、功能基因、代谢途径、硫氧化/硫酸盐还原速率及其对环境条件变化响应等方面的研究现状,并对未来湖泊微生物驱动的硫循环研究方向进行了展望。     

嗜酸热硫球菌细胞外被的生物化学特性

研究了一抹嗜酸热硫氧化古细菌——嗜酸热硫球菌(Sulfosphaesellus thermoacidophilum)S-层的某些生物化学性质。发现该菌在某些重要性质方面与硫化叶菌属的模式菌种酸热硫化叶菌(Sulfolobus acidocaldorius)相比有很大差异。嗜酸热硫球菌的s一层之2％SDS溶液中非常不稳定,很容易被分解成亚单位：但它们在pH 9．0的磷酸缓冲液中很稳定,既不会坡水解也不溶解在该缓冲液中。     

硫氧化细菌源单质硫的生成、转运和回收

单质硫(硫粒)是硫化物生物氧化的中间产物.按化学计量式精准调控O/S比(溶解氧与硫化物的摩尔比),单质硫可成为硫氧化细菌(Sulfur-oxidizing bacteria,SOB)的主要代谢产物.根据单质硫的分布,单质硫可分为胞内硫粒和胞外硫粒.单质硫由胞内向胞外的跨膜转运过程是泌硫型SOB的重要生理特征.从生物脱硫...     

Thermodynamic aspects of energy conservation by chemolithotrophic sulfur bacteria in relation to the sulfur oxidation pathways

The free-energy data on which assessments of the autotrophic growth efficiencies of chemolithotrophic bacteria are commonly based have been reevaluated and new values have been calculated. It has been concluded that many earlier calculations are in error and that many values previously reported in the literature are overestimates of efficiency. A problem posed by the chemolithotrophic sulfur-oxidizing bacteria is the elucidation of the mechanism by which elemental sulfur and the sulfane-sulfur (-S-) of the thionic acids are converted to sulfite. Even after decades of studies on sulfur oxidation by these bacteria, this problem has not been fully resolved although it is widely thought that conversion of sulfur to sulfite is brought about by an oxygenase. The biochemically feasible mechanisms by which sulfur and “sulfane” oxidation to sulfite might occur are reviewed. The possible insight afforded by chemical thermodynamics into the most likely mechanisms for oxidation to sulfate in relation to the efficiency of energy conservation is discussed. Energetic calculations and growth yield data indicate that the energy-yielding oxidation of sulfur and “sulfane” to sulfite, either coupled to energy-conserving electron transport or catalyzed by an oxygenase, could explain divergent growth yields among different sulfur-chemolithotrophs. Received: 30 October 1998 / Accepted: 25 January 1999     

Occurrence and activity of iron- and sulfur-oxidizing microorganisms in alkaline coal strip mine spoils

Spoils samples collected from a coal strip mine in southeastern Montana were examined for populations and activities of iron- and sulfur-oxidizing bacteria. Spoils examined were of three types: (a) acidic pyrite-rich waste coal, (b) oxidation halo material, and (c) alkaline material, which was the most widespread type. Bacterial numbers, sulfur oxidation, and¹⁴CO₂ uptake activity declined to low levels in the summer when spoils were dry. Even in wetter spring months pyritic spoils contained relatively low numbers of acidophilic iron- and sulfur-oxidizing bacteria, probably indicative of water stress since the same spoils incubated with excess water or dilute mineral salts showed considerably greater bacterial numbers and activity. Certain wells in coal and spoils aquifers contained substantial populations of iron-oxidizing acidophilic bacteria. However, these wells were always of alkaline or neutral pH, indicating that bacterial pyrite oxidation occurred where groundwaters contacted either replaced spoils or coal that contained pyrite or other metal sulfides. Bacterial activity may contribute to trace metal and sulfate leaching in the area.     

Structure of the cytochrome complex SoxXA of Paracoccus pantotrophus, a heme enzyme initiating chemotrophic sulfur oxidation

The sulfur-oxidizing enzyme system (Sox) of the chemotroph Paracoccus pantotrophus is composed of several proteins, which together oxidize hydrogen sulfide, sulfur, thiosulfate or sulfite and transfers the gained electrons to the respiratory chain. The hetero-dimeric cytochrome c complex SoxXA functions as heme enzyme and links covalently the sulfur substrate to the thiol of the cysteine-138 residue of the SoxY protein of the SoxYZ complex. Here, we report the crystal structure of the c-type cytochrome complex SoxXA. The structure could be solved by molecular replacement and refined to a resolution of 1.9A identifying the axial heme-iron coordination involving an unusual Cys-251 thiolate of heme2. Distance measurements between the three heme groups provide deeper insight into the electron transport inside SoxXA and merge in a better understanding of the initial step of the aerobic sulfur oxidation process in chemotrophic bacteria.     

The production and utilization of intermediary elemental sulfur during the oxidation of reduced sulfur compounds by Thiobacillus ferrooxidans

The intermediary production of elemental sulfur during the microbial oxidation of reduced sulfur compounds has frequently been reported. Thiobacillus ferrooxidans, an acidophilic chemolithoautotroph, was found to produce an insoluble sulfur compound, primarily elemental sulfur, during the oxidation of thiosulfate, trithionate, tetrathionate and sulfide. This was confirmed by light and electron microscopy. Sulfur was produced from sulfide by an oxidative step, while the production from tetrathionate was initiated by a hydrolytic step, probably followed by a series of chemical reactions. The oxidation of intermediary sulfur was severely inhibited by sulfhydryl-binding reagents such as N-ethylmaleimide, by the addition of uncouplers or after freezing and thawing of the cells, which probably damaged the cell membrane. The mechanisms behind these inhibitions have not yet been clarified. Finally, it was observed that elemental sulfur oxidation by whole cells depended on the medium composition. The absence of sulfate or selenate reduced the sulfur oxidation rate.Non-standard abbreviations NEM N-ethylmaleimide - CCCP carbonyl cyanide m-chlorophenyl hydrazone     

三株氧化硫硫杆菌的分离与鉴定

从煤堆废水中分离得到3株嗜温嗜酸硫氧化细菌.这3株菌株为革兰氏阴性、菌体大小0.4～0.7 μm×1～2 μm、短杆状运动细菌,其最适生长温度为 30 ℃和最适生长pH 2.0～2.5.它们能够利用元素硫,硫代硫酸钠和连四硫酸钾为能源进行自养生长,不能利用有机物质以及硫酸亚铁、黄铁矿和黄铜矿等无机物质作为能源生长.细菌的形态、生理生化特性研究以及基于16S rRNA序列同源性构建的系统发育树结果表明,这3株细菌初步鉴定为氧化硫硫杆菌.氧化硫硫杆菌能够通过产酸有效促进黄铜矿的浸出速率和浸出率.     

A hydrocarbon-oxidizing acidophilic thermotolerant bacterial association from sulfur blocks

A stable bacterial association isolated from a sulfur block sample of the Astrakhan gas processing complex was able to utilize n-alkanes as the sole carbon and energy source at low pH. Hydrocarbon-dependent growth occurred at pH 1.6–5.5 (optimum at pH 2.5) and 20–50°C (optimum at 30–35°C). Analysis of the 16S rRNA gene fragments isolated from the total DNA of the enrichment by PCR-DGGE revealed the nucleotide sequences most closely related to extreme acidophilic chemolithotrophs Acidithiobacillus thiooxidans and Sulfobacillus sp. (98–99% similarity) and the sequences exhibiting high similarity to those of slowly growing actinobacteria Mycobacterium europaeum and M. parascrofulaceum (98%). Capacity of any of these organisms for hydrocarbon oxidation has not been reported previously. The taxonomic position of the 16S rRNA gene fragments from the enrichment culture suggests that this bacterial association is a unique microbial community, in which development of acidophilic hydrocarbon-oxidizing bacteria is mediated by a localized pH decrease in the sulfur blocks resulting from elemental sulfur oxidation due to massive development of chemolithotrophic sulfur-oxidizing bacteria.     

Phylogeny and distribution of the soxB gene among thiosulfate-oxidizing bacteria

A PCR protocol for the detection of sulfur-oxidizing bacteria based on soxB genes that are essential for thiosulfate oxidation by sulfur-oxidizing bacteria of various phylogenetic groups which use the 'Paracoccus sulfur oxidation' pathway was developed. Five degenerate primers were used to specifically amplify fragments of soxB genes from different sulfur-oxidizing bacteria previously shown to oxidize thiosulfate. The PCR yielded a soxB fragment of approximately 1000 bp from most of the bacteria. Amino acid and nucleotide sequences of soxB from reference strains as well as from new isolates and environmental DNA from a hydrothermal vent habitat in the North Fiji Basin were compared and used to infer relationships of soxB between sulfur-oxidizing bacteria belonging to various 16S rDNA-based phylogenetic groups. Major phylogenetic lines derived from 16S rDNA were confirmed by soxB phylogeny. Thiosulfate-oxidizing green sulfur bacteria formed a coherent group by their soxB sequences. Likewise, clearly separated branches demonstrated the distant relationship of representatives of alpha-, beta-, and gamma-Proteobacteria including representative species of the former genus Thiobacillus (now Halothiobacillus - gamma-Proteobacteria, Thiobacillus - beta-Proteobacteria and Starkeya - alpha-Proteobacteria). This general picture emerged although apparent evidence for lateral transfer of the soxB gene is indicated and comparison of soxB phylogeny and 16S rDNA phylogeny points to the significance of this gene transfer in hydrothermal vent bacterial communities of the North Fiji Basin.