高等植物铁氧还蛋白的结构与功能

该文介绍了高等植物中铁氧还蛋白（Fd）的结构,铁氧还蛋白与铁氧还蛋白：NADP^＋氧化还原酶（FNR）的相互作用,氧化还原电势和电子传递活性;阐述了铁氧还蛋白结构与功能的关系。     

固氮作用

本综述总结了固氮酶的一些物理化学性质。考察了该酶的催化特性,包括固氮酶的电子分配和体内固氮酶的能量要求。主要综述了电子向固氮酶转运的生物能学,包括电子载体和产生还原电势的机制。描述了固氮生物中的铁氧还蛋白/黄素氧还蛋白还原系统,包括专性厌氧固氮菌、     

对“菠菜铁氧还素(Ferredoxin)的制备”一文的商榷

Ferredoxin(Fd)广泛存在于藻类、细菌、高等植物中,是生物固氮、光合作用等过程中不可缺少的电子递体。研究生化机理时,往往需要分离、纯化Fd。植生通讯1980年第三期,发表了“菠菜铁氧还素Ferre     

脂肪酸生物标记法研究零排放猪舍基质垫层微生物群落多样性

用微生物群落脂肪酸生物标记总量,分析零排放猪舍基质垫层微生物群落的数量变化,日本洛东微生物菌种处理组和零排放I号菌种处理组各层微生物脂肪酸生物标记含量变化趋势相近。基质垫层微生物群落脂肪酸生物标记检测出37个生物标记,构成微生物群落的指纹图谱,含量最高的前4个生物标记为：细菌16：00含量为431260,细菌18：1ω9c含量为413075,厌氧细菌18：1ω7c含量为101368,耗氧细菌i15：0含量为90328.不同的生物标记多样性指数在基质垫层不同层次分布不同,可作为衡量特定微生物生物标记功能的一个指标。通过基质垫层微生物脂肪酸生物标记特征指数B的分析,提出了微生物群落分布的特征指标,生物标记特征指数B越高,表明微生物群落中的细菌和真菌含量越高,有利于基质垫层分解粪便排泄物,可作为基质垫层微生物群落变化优劣的特征性指标;通过基质垫层耗氧细菌和厌氧细菌脂肪酸生物标记含量比值,构建发酵指数F,作为基质垫层发酵特性的指标,发酵指数F越高,表明耗氧细菌起的作用越大,反之,耗氧细菌起的作用越小,生物标记的发酵指数可以作为研究粪便排泄物的微生物分解过程的指数。     

海洋氮循环中细菌的厌氧氨氧化

细菌厌氧氨氧化过程是在一类特殊细菌的厌氧氨氧化体内完成的以氨作为电子供体硝酸盐作为电子受体的一种新型脱氮反应.厌氧氨氧化菌的发现,改变人们对传统氮的生物地球化学循环的认识:反硝化细菌并不是大气中氮气产生的唯一生物类群.而且越来越多的证据表明,细菌厌氧氨氧化与全球的氮物质循环密切相关,估计海洋细菌的厌氧氨氧化过程占到全球海洋氮气产生的一半左右.由于氮与碳的循环密切相关,因此可以推测,细菌的厌氧氨氧化会影响大气中的二氧化碳浓度,从而对全球气候变化产生重要影响.另外,由于细菌厌氧氨氧化菌实现了氨氮的短程转化,缩短了氮素的转化过程,因此为开发更节约能源、更符合可持续发展要求的废水脱氮新技术提供了生物学基础.     

线粒体的分子进化与氧效应

线粒体通常被认为是消耗氧气产生ATP的细胞器.但自然界有多种生物具有厌氧型线粒体,其厌氧生物化学和遗传学研究表明,线粒体可能来源于兼性厌氧的α-蛋白细菌,在有氧环境中,起始共生体的厌氧功能丧失或被改变而进化成为经典的线粒体,但在厌氧环境中,有氧呼吸功能丧失了进化.厌氧型线粒体为了完成能量的转化,改变了呼吸链的组成,表现出产能模式的多样性.而经典线粒体在利用氧化反应获得能量的同时,也通过电子漏产生了自由基,对生命体本身构成了威胁.事实上,生命体呼吸链的进化是沿着不断加强对氧的利用效率和不断克服氧毒性的方向发展的.     

关于氧气与呼吸作用几个问题的解答

从生物能学角度、生物化学氧化还原电势角度及化学反应平衡角度,解释O2为什么会抑制无氧呼吸;同时对氧气为什么会“杀死”专性厌氧生物;厌氧生物对氧气的耐受性为何不一样做出了阐述。     

氧化亚铁硫杆菌亚铁氧化活性与其对低品位铜矿浸矿速率关系的研究

氧化亚铁硫杆菌是一个具有很强生物浸矿能力的细菌,本文对3株分离得到的氧化亚铁硫杆菌及一株来自菌种中心(Acidithiobacillus ferrooxidans A．f)的铁氧化活性及其这些菌株对低品位黄铜矿浸出速率进行了研究。结果显示,在所有的4株A．f菌中,菌株CMS—F1和F10—ATCCC23270的铁氧化活性较高,其对黄铜矿生物浸出速率也高。进一步分析亚铁氧化活性对生物浸矿效率的影响时发现,在A．f菌中,氧化活性高的菌株,其对低品位黄铜矿的生物浸出效果也高。     

嗜酸氧化亚铁硫杆菌基因组学研究进展

嗜酸氧化亚铁硫杆菌(Acidithiobacillus ferrooxidan,A.ferrooxidans)广泛存在于酸性矿物废水中,与生物冶金和环境净化紧密相关。不同来源嗜酸氧化亚铁硫杆菌全基因组的测序,为我们利用比较基因组学和功能基因组学的方法去洞察嗜酸氧化亚铁硫杆菌功能基因,提供了坚实的研究基础和丰富的科研信息。简述了嗜酸氧化亚铁硫杆菌基因组学的基本特征;从比较基因组学和功能基因组学发现了嗜酸氧化亚铁硫杆菌菌株基因组水平的差异;通过生物信息学概述了该菌的铁和硫代谢机制,并从细菌的功能基因组学对其在生物冶金与环境治理等应用进行了展望。     

菠菜铁氧还蛋白的简易分离方法

用DEAE纤维素（DE－52）从菠菜叶片的抽提液中吸附蛋白,再以NaCl分级洗脱得到含铁氧还蛋白（Fd)的分部,此Fd制剂具有特征性的Fd氧化还原吸收光谱和催化体叶绿体光还原NADP的活性。     

Microbial growth on carbon monoxide

The utilization of carbon monoxide as energy and/or carbon source by different physiological groups of bacteria is described and compared. Utilitarian CO oxidation which is coupled to the generation of energy for growth is achieved by aerobic and anaerobic eu- and archaebacteria. They belong to the physiological groups of aerobic carboxidotrophic, facultatively anaerobic phototrophic, and anaerobic acetogenic, methanogenic or sulfate-reducing bacteria. The key enzyme in CO oxidation is CO dehydrogenase which is a molybdo iron-sulfur flavoprotein in aerobic CO-oxidizing bacteria and a nickel-containing iron-sulfur protein in anaerobic ones. In carboxidotrophic and phototrophic bacteria, the CO-born CO₂ is fixed by ribulose bisphosphate carboxylase in the reductive pentose phosphate cycle. In acetogenic, methanogenic, and probably in sulfate-reducing bacteria, CODH/acetyl-CoA synthase directly incorporates CO into acetyl-CoA.In plasmid-harbouring carboxidotrophic bacteria, CO dehydrogenase as well as enzymes involved in CO₂ fixation or hydrogen utilization are plasmid-encoded. Structural genes encoding CO dehydrogenase were cloned from carboxidotrophic, acetogenic and methanogenic bacteria. Although they are clustered in each case, they are genetically distinct.Soil is a most important biological sink for CO in nature. While the physiological microbial groups capable of CO oxidation are well known, the type and nature of the microorganisms actually representing this sink are still enigmatic. We also tried to summarize the little information available on the nutritional and physicochemical requirements determining the sink strength. Because CO is highly toxic to respiring organisms even in low concentrations, the function of microbial activities in the global CO cycle is critical.     

Characterization and complete amino acid sequence of ferredoxin II from Desulfovibrio vulgaris Miyazaki

One of 2 ferredoxins, Fd II, purified from Desulfovibrio vulgaris Miyazaki (DvM) has been characterized and its complete amino acid sequence established. Fd II is composed of 63 amino acid residues and contains 7 cysteinyl residues but has only 4 iron atoms in an iron-sulfur cluster of a standard redox potential of -405 mV. The arrangement of cysteinyl residues in the protein suggests that some cysteinyl residues are not directly involved in ligation to the iron-sulfur cluster. Homology is recognized among Fd II (DvM), Fd I (D. desulfuricans Norway), Fd I (D. africanus Benghazi), and Fd (D. gigas). Although Fd I and Fd II in DvM are poorly homologous, the C-terminal half of Fd I is fairly homologous to the N-terminal half of Fd II. Fd II is 40% as effective as Fd I as an electron carrier for pyruvate dehydrogenase coupled with hydrogenase and cytochrome c3.     

Purification and characterization of ferredoxin from Desulfovibrio vulgaris Miyazaki

Two ferredoxins, Fd I and Fd II, were isolated and purified from Desulfovibrio vulgaris Miyazaki. The major component, Fd I, is an iron-sulfur protein of Mr 12,000, composed of two identical subunits. The absorption spectra of Fd I and Fd II have a broad absorption shoulder near 400 nm characteristic of iron-sulfur proteins. The purity index, A400/A280, of Fd I is 0.69, and its millimolar absorption coefficient at 400 nm is 3.73 per Fe. It contains two redox centers with discrete redox behaviors. The amino acid composition and the N-terminal sequence of Fd I are similar to those of Fd III of Desulfovibrio africanus Benghazi and Fd II of Desulfovibrio desulfuricans Norway. Fd I does not serve as an electron carrier for the hydrogenase of D. vulgaris Miyazaki, but it serves as a carrier for pyruvate dehydrogenase of this bacterium. The evolution of H2 from pyruvate was observed by a reconstructed system containing purified hydrogenase, cytochrome C3, Fd I, partially purified pyruvate dehydrogenase, and CoA. The H2-sulfite reducing system can be reconstructed from the purified hydrogenase, cytochrome C3, Fd I and desulfoviridin (sulfite reductase), but the reaction rate is very slow compared to that of the crude extract at the same molar ratio of the components.     

Binding of ferredoxin to ferredoxin:NADP+ oxidoreductase: the role of carboxyl groups, electrostatic surface potential, and molecular dipole moment.

The small, soluble, (2Fe-2S)-containing protein ferredoxin (Fd) mediates electron transfer from the chloroplast photosystem I to ferredoxin: NADP+ oxidoreductase (FNR), a flavoenzyme located on the stromal side of the thylakoid membrane. Ferredoxin and FNR form a 1:1 complex, which is stabilized by electrostatic interactions between acidic residues of Fd and basic residues of FNR. We have used differential chemical modification of Fd to locate aspartic and glutamic acid residues at the intermolecular interface of the Fd:FNR complex (both proteins from spinach). Carboxyl groups of free and FNR-bound Fd were amidated with carbodiimide/2-aminoethane sulfonic acid (taurine). The differential reactivity of carboxyl groups was assessed by double isotope labeling. Residues protected in the Fd:FNR complex were D-26, E-29, E-30, D-34, D-65, and D-66. The protected residues belong to two domains of negative electrostatic surface potential on either side of the iron-sulfur cluster. The negative end of the molecular dipole moment vector of Fd (377 Debye) is close to the iron-sulfur cluster, in the center of the area demarcated by the protected carboxyl groups. The molecular dipole moment and the asymmetric surface potential may help to orient Fd in the reaction with FNR. In support, we find complementary domains of positive electrostatic potential on either side of the FAD redox center of FNR. The results allow a binding model for the Fd:FNR complex to be constructed.     

厌氧氨氧化细菌Candidatus Kuenenia stuttgartiensis铁的吸收利用研究进展

铁是影响微生物生长代谢的关键元素,它与蛋白质结合,起催化、氧化还原或调节作用。厌氧氨氧化(ANAMMOX)细菌的生长代谢严重依赖铁,尤其是含铁蛋白。ANAMMOX细菌的厌氧生活方式和厌氧氨氧化体的存在使其对铁代谢的模式不同于其他微生物。弄清ANAMMOX细菌的铁吸收代谢模式,可为获得其纯培养物奠定基础,有利于促进其在环境领域中的应用。在这里,我们将现有铁吸收、利用和代谢的观点、与ANAMMOX细菌的基因组信息和有限的生化生理数据结合起来,提出ANAMMOX细菌可能的铁利用途径,为后续的生理生化研究提供参考。     

Reactive oxygen species,cellular redox systems,and apoptosis

Reactive oxygen species (ROS) are products of normal metabolism and xenobiotic exposure, and depending on their concentration, ROS can be beneficial or harmful to cells and tissues. At physiological low levels, ROS function as “redox messengers” in intracellular signaling and regulation, whereas excess ROS induce oxidative modification of cellular macromolecules, inhibit protein function, and promote cell death. Additionally, various redox systems, such as the glutathione, thioredoxin, and pyridine nucleotide redox couples, participate in cell signaling and modulation of cell function, including apoptotic cell death. Cell apoptosis is initiated by extracellular and intracellular signals via two main pathways, the death receptor- and the mitochondria-mediated pathways. Various pathologies can result from oxidative stress-induced apoptotic signaling that is consequent to ROS increases and/or antioxidant decreases, disruption of intracellular redox homeostasis, and irreversible oxidative modifications of lipid, protein, or DNA. In this review, we focus on several key aspects of ROS and redox mechanisms in apoptotic signaling and highlight the gaps in knowledge and potential avenues for further investigation. A full understanding of the redox control of apoptotic initiation and execution could underpin the development of therapeutic interventions targeted at oxidative stress-associated disorders.     

Superoxide radical formation by pure complex I (NADH:ubiquinone oxidoreductase) from Yarrowia lipolytica

Generation of reactive oxygen species (ROS) is increasingly recognized as an important cellular process involved in numerous physiological and pathophysiological processes. Complex I (NADH:ubiquinone oxidoreductase) is considered as one of the major sources of ROS within mitochondria. Yet, the exact site and mechanism of superoxide production by this large membrane-bound multiprotein complex has remained controversial. Here we show that isolated complex I from Yarrowia lipolytica forms superoxide at a rate of 0.15% of the rate measured for catalytic turnover. Superoxide production is not inhibited by ubiquinone analogous inhibitors. Because mutant complex I lacking a detectable iron-sulfur cluster N2 exhibited the same rate of ROS production, this terminal redox center could be excluded as a source of electrons. From the effect of different ubiquinone derivatives and pH on this side reaction of complex I we concluded that oxygen accepts electrons from FMNH2 or FMN semiquinone either directly or via more hydrophilic ubiquinone derivatives.     

Characterization of the recombinant Clostridium pasteurianum ferredoxin and comparison of its properties with those of the native protein

Ferredoxins (Fds) constitute an important class of nonheme iron-sulfur proteins. One of the most studied Fds is the [8Fe-8S] Fd from Clostridium pasteurianum. The gene for this Fd has previously been cloned and sequenced. We report the expression of this Fd in Escherichia coli, and the characterization and comparison of this recombinant protein to the native Fd. We have found that the purified recombinant protein has the same enzymatic, redox, magnetic and electronic properties as the native Fd isolated from C. pasteurianum, which indicates that the two [4Fe-4S] clusters present in the Fd were correctly formed in E. coli.     

Mapping of protein-protein interaction sites in the plant-type [2Fe-2S] ferredoxin

Knowing the manner of protein-protein interactions is vital for understanding biological events. The plant-type [2Fe-2S] ferredoxin (Fd), a well-known small iron-sulfur protein with low redox potential, partitions electrons to a variety of Fd-dependent enzymes via specific protein-protein interactions. Here we have refined the crystal structure of a recombinant plant-type Fd I from the blue green alga Aphanothece sacrum (AsFd-I) at 1.46 Å resolution on the basis of the synchrotron radiation data. Incorporating the revised amino-acid sequence, our analysis corrects the 3D structure previously reported; we identified the short α-helix (67-71) near the active center, which is conserved in other plant-type [2Fe-2S] Fds. Although the 3D structures of the four molecules in the asymmetric unit are similar to each other, detailed comparison of the four structures revealed the segments whose conformations are variable. Structural comparison between the Fds from different sources showed that the distribution of the variable segments in AsFd-I is highly conserved in other Fds, suggesting the presence of intrinsically flexible regions in the plant-type [2Fe-2S] Fd. A few structures of the complexes with Fd-dependent enzymes clearly demonstrate that the protein-protein interactions are achieved through these variable regions in Fd. The results described here will provide a guide for interpreting the biochemical and mutational studies that aim at the manner of interactions with Fd-dependent enzymes.