Fungal Nanophase Particles Catalyze Iron Transformation for Oxidative Stress Removal and Iron Acquisition

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Proteomics Analysis of Avian Eggshell Matrix Proteins: Toward New Advances on Biomineralization

Eggs are widely consumed all over the world. The eggshell is its protective barrier whose original function is to protect the embryo during development. Avian eggshells are made of calcium carbonate with a small amount of organic matrix (proteins and proteoglycans). During eggshell formation, the mineral precursors interact with matrix proteins to regulate the calcification of this highly resistant biomineral. In order to better characterize the functions of matrix proteins in eggshell biominerals, many proteomics studies have been performed during the last 15 years. The chicken eggshell is the main model studied in birds, but there is a need for comparative approaches in order to determine whether there is a general protein toolkits associated with calcitic biomineralization, and to determine its components. The study by Zhu et al., reported in article number 1900011, volume 19, issue 11, is a major step forward as it is the first shell proteomics survey performed on duck. Thus, it will contribute to improved knowledge of the eggshell mineralization process and will provide new insight for shell quality improvement and to guide biomimetic efforts in material sciences.     

iTRAQ‐Based Quantitative Proteomic Analysis of Duck Eggshell During Biomineralization

The avian egg is a valuable model for the calcitic biomineralization process as it is the fastest calcification process occurring in nature and is a clear example of biomineralization. In this study, iTRAQ MS/MS is used to detect and study for the first time: 1) the overall duck eggshell proteome; 2) regional differences in the proteome between the inner and outer portions of the duck eggshell. The new reference protein datasets allow us to identify 179 more eggshell proteins than solely using the current release of Ensembl duck annotations. In total, 484 proteins are identified in the entire duck eggshell proteome. Twenty‐eight novel proteins of unknown function that are involved in eggshell formation are also identified. Among the identified eggshell proteins, 54 proteins show differential abundances between the inner, partially mineralized eggshell (obtained 16 h after ovulation) compared to the overall complete eggshell (normally expulsed eggshell). At least 64 of the abundant matrix proteins are common to eggshell of 4 different domesticated bird species (chicken, duck, quail, turkey) and zebra finch. This study provides a new resource for avian eggshell proteomics, and augments the inventory of eggshell matrix proteins that will lead to a deeper understanding of calcitic biomineralization.     

Copper at the Fungal Pathogen-Host Axis

Fungal infections are responsible for millions of human deaths annually. Copper, an essential but toxic trace element, plays an important role at the host-pathogen axis during infection. In this review, we describe how the host uses either Cu compartmentalization within innate immune cells or Cu sequestration in other infected host niches such as in the brain to combat fungal infections. We explore Cu toxicity mechanisms and the Cu homeostasis machinery that fungal pathogens bring into play to succeed in establishing an infection. Finally, we address recent approaches that manipulate Cu-dependent processes at the host-pathogen axis for antifungal drug development.     

Involvement of Microorganisms in the Formation of Carbonate Speleothems in the Cervo Cave (L'Aquila-Italy)

Much is known about the bacterial precipitation of carbonate rocks, but comparatively little is known about the involvement of microbes in the formation of secondary mineral structures in caves. We hypothesized that bacteria isolated from calcareous stalactites, which are able to mediate CaCO₃ precipitation in vitro, play a role in the formation of carbonate speleothems. We collected numerous cultivable calcifying bacteria from calcareous speleothems from Cervo cave, implying that their presence was not occasional. The relative abundance of calcifying bacteria among total cultivable microflora was found to be related to the calcifying activity in the stalactites. We also determined the δ ¹³C and δ ¹⁸ O values of the Cervo cave speleothems from which bacteria were isolated and of the carbonates obtained in vitro to determine whether bacteria were indeed involved in the formation of secondary mineral structures. We identified three groups of biological carbonates produced in vitro at 11°C on the basis of their carbon isotopic composition: carbonates with δ ¹³C values (a) slightly more positive, (b) more negative, and (c) much more negative than those of the stalactite carbonates. The carbonates belonging to the first group, characterized by the most similar δ ¹³C values to stalactites, were produced by the most abundant strains. Most of calcifying isolates belonged to the genus Kocuria. Scanning electron microscopy showed that dominant morphologies of the bioliths were sherulithic with fibrous radiated interiors. We suggest a mechanism of carbonate crystal formation by bacteria.     

A Model Sheet Mineral System to Study Fungal Bioweathering of Mica

The general objective of this research was to examine fungal interactions with silicate minerals within the context of their roles in bioweathering. To achieve this, we used muscovite, a phyllosilicate mineral (KAl₂[(OH)₂|AlSi₃O₁₀]), in the form of a mineral sheet model system for ease of experimental manipulation and microscopic examination. It was found that test fungal species successfully colonized and degraded the surface of muscovite sheets in both laboratory and field experiments. After colonization by the common soil fungus Aspergillus niger, a network of hyphae covered the surface of the muscovite, and mineral dissolution or degradation was clearly evidenced by a network of fungal “footprints” that reflected coverage by the mycelium. For natural soil incubations, microorganisms associated with muscovite sheet material included biofilms of fungi and bacteria on the surface, while mineral encrustation or adhesion to microbial structures was also observed. Our results show that muscovite sheet is a good model mineral system for examination of microbial colonization and degradation, and this was demonstrated using laboratory and field systems, providing more evidence for the bioweathering significance of fungal activities in the context of silicate degradation and soil formation and development. The approach is also clearly applicable to other rock and mineral-based substrates and a variety of free-living and symbiotic microbial systems.     

The Role of Copper in Protein Foams

Chefs have known that whipping egg white proteins (EWP) in a copper bowl will improve foam stability. The improved stability is attributed to a copper–conalbumin complex or alteration of sulfhydryl reactivity. Whey proteins bind copper and show copper-induced changes in disulfide bonds; therefore, they may also be responsive to whipping in a copper bowl. EWP and whey protein isolate (WPI) solutions were whipped in the presence of 1 mM CuSO₄ or in a copper bowl with and without sugar followed by overrun and yield stress measurements and angel food cake formation. Dilational elasticity and surface tension were also measured for WPI solutions. Whipping in a copper bowl or adding 1 mM CuSO₄ significantly improved stability of EWP foams while having no effect on WPI foams. Copper caused disulfide-linked dimer formation of β-lactoglobulin and decreased dilational elasticity and surface tension, but these modifications were insufficient to change the bulk properties of foams. The addition of 10 mM CuSO₄ to WPI solutions was sufficient to increase foam stability to levels similar to EWP; however, the more stable foams formed less stable cakes. It was concluded that the effect of whipping in a copper bowl on foam properties is mainly dependent on the specific proteins forming the foam. Paper no. FSR-07-29 of the Journal Series of the Department of Food Science, North Carolina State University, Raleigh, NC 27695-7624. Presented at the 2nd International Symposium: Delivery of Functionality in Complex Food Systems: Physically-inspired Approaches From Nanoscale to Microscale, October 8–10, 2007.     

蛋白质相互作用研究的新技术与新方法

目前,蛋白质相互作用已成为蛋白质组学研究的热点. 新方法的建立及对已有技术的改进标志着蛋白质相互作用研究的不断发展和完善．在技术改进方面,本文介绍了弥补酵母双杂交的蛋白定位受限等缺陷的细菌双杂交系统;根据目标蛋白特性设计和修饰TAP标签来满足复合体研究要求的串联亲和纯化技术,以及在双分子荧光互补基础上发展的动态检测多个蛋白质间瞬时、弱相互作用的多分子荧光互补技术．还综述了近两年建立的新方法：与免疫共沉淀相比,寡沉淀技术直接研究具有活性的蛋白质复合体;减量式定量免疫沉淀方法排除了蛋白质复合体中非特异性相互作用的干扰;原位操作的多表位－配基绘图法避免了样品间差异的影响,以及利用多点吸附和交联加固研究弱蛋白质相互作用的固相蛋白质组学方法.     

用铁蛋白合成纳米粒子的研究进展

铁蛋白是一种生物储铁蛋白 ,其储存铁的特性和储存铁在生物体内的特殊形态 ,通过相对温和、简便的生物、化学、物理过程 ,可合成多种具有特异的力、热、光、电、磁等特性的纳米粒子 ,并可用来构建纳米级的分子器件     

Biomineralization of gold by Mucor plumbeus: The progress in understanding the mechanism of nanoparticles’ formation

This contribution describes the deposition of gold nanoparticles by microbial reduction of Au(III) ions using the mycelium of Mucor plumbeus. Biosorption as the major mechanism of Au(III) ions binding by the fungal cells and the reduction of them to the form of Au(0) on/in the cell wall, followed by the transportation of the synthesized gold nanoparticles to the cytoplasm, is postulated. The probable mechanism behind the reduction of Au(III) ions is discussed, leading to the conclusion that this process is nonenzymatic one. Chitosan of the fungal cell wall is most likely to be the major molecule involved in biomineralization of gold by the mycelium of M. plumbeus. Separation of gold nanoparticles from the cells has been carried out by the ultrasonic disintegration and the obtained nanostructures were characterized by UV‐vis spectroscopy and transmission electron micrograph analysis. © 2017 American Institute of Chemical Engineers Biotechnol. Prog., 33:1381–1392, 2017     

蛋白质组学技术在精子蛋白研究中的应用

从蛋白质组学研究的技术手段、蛋白质组学在人类不育及精卵相互识别并结合的机理研究、免疫法开展男性避孕方法的研究及蛋白质组学研究方法在家畜繁殖环节中的应用等几个方面阐述了蛋白质组学在人类生殖及动物繁殖环节相关研究中的重要作用。说明蛋白质组学已经成为生命科学未来发展的主要分支之一,为揭示生命个体的蛋白质动态变化提供了技术手段和理论基础,并将在药物开发,生命活动机理研究等方面发挥巨大作用,也必将会在家畜繁殖学领域发挥其应有的作用。     

真菌介导纳米银生物合成的研究进展

纳米银(Silver nanoparticles,AgNPs)是指三维结构中至少有一维在1-100 nm范围内的金属银材料,在光学、电学、催化和医药等领域得到了广泛应用.利用真菌生物合成AgNPs相比于传统的化学、物理合成方法,具有反应条件温和、绿色低毒、环境友好等优势备受关注.综述了近年来合成AgNPs真菌种类的研究...     

Transformation of Copper Oxychloride Fungicide into Copper Oxalate by Tolerant Fungi and the Effect of Nitrogen Source on Tolerance

Aspergillus niger and Penicillium chrysogenum were able to grow on Czapek Dox medium amended with elevated concentrations [up to 500 ppm active ingredient (ai)] of the fungicide copper oxychloride. Solubilization of the fungicide in solid medium was evident by the appearance of a clear (halo) zone underneath and around the growing colonies. The halo formed with A. niger, grown on fungicide-containing nitrate nitrogen medium, was found subsequently to enclose concentric rings of newly crystalline precipitate. These crystals were extracted, examined by scanning electron microscopy and IR, and identified as copper oxalate. The supplemented nitrogen source to the medium greatly affected both fungicide solubilization and fungal tolerance. Ratios of fungicide solubilization rate (R(S)) in relation to the colony growth rate (R(G)) were significantly higher on ammonium than on nitrate nitrogen medium for both fungal strains. Growth ratios (the colony extension rate in the presence of a given concentration of the fungicide in relation to the control colony growth rate) of A. niger were markedly lower on ammonium than on nitrate nitrogen medium. The cellular copper contents, taken up from the fungicide, and the medium titratable acidity were higher in ammonium than in nitrate medium for both fungi. These results suggested fungal possession of variable tolerance mechanisms to this fungicide by complexation and/or precipitation of copper in the medium. Additionally, this work emphasizes the activity of fungi in transformation of insoluble inorganic metal-containing fungicides into insoluble organic metal compounds, which has a potentiality in metal cycling in biogeochemical and environmental context.     

模拟氮沉降对杉木丛枝菌根真菌侵染率和球囊霉素的影响

杉木是我国南方重要的速生用材树种,同时南方面临着日益增强的大气氮沉降。尽管有大量的研究探索了氮沉降对杉木林的影响,但关于氮沉降对杉木与丛枝菌根真菌（arbuscular mycorrhizal fungi,AMF）共生关系影响的研究则较少报道。以10年生杉木为研究对象,模拟了不同氮沉降水平（N3：3 g N m^-2a^-1,N6：6 g N m^-2a^-1和Control：0 g N m^-2a^-1）对AMF侵染率和球囊霉素的影响。结果显示：在冬季,与对照相比,N3处理显著增加了AMF侵染率,N6处理显著增加易提取球囊霉素的含量,而氮沉降对总球囊霉素含量无显著影响。在春季,与对照相比,N3处理显著增加AMF侵染率,但是显著降低了易提取球囊霉素的含量。N6处理显著增加总球囊霉素的含量,但显著降低易提取球囊霉素的含量。相同氮添加情况下,春季的AMF侵染率显著低于冬季,而球囊霉素含量（易提取球囊霉素和总球囊霉素）均显著高于冬季的。土壤有效磷与AMF侵染率显著负相关,而与易提取球囊霉素和总球囊霉素含量显著正相关。侵染率与pH显著正相关,球囊霉素与pH显著负相关。本实验针对AMF侵染率和球囊霉素的含量对于氮沉降的响应做出探讨,对全面了解杉木与AMF之间的共生关系对氮沉降的响应及其机制提供了新的参考。     

Saposin Lipid Nanoparticles: A Highly Versatile and Modular Tool for Membrane Protein Research

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Biomineralization of Fungal Hyphae with Calcite (CaCO3) and Calcium Oxalate Mono- and Dihydrate in Carboniferous Limestone Microcosms

The formation of biogenic fabrics in limestone by two fungi, Serpula himantioides and a polymorphic fungal isolate from limestone identified as a Cephalotrichum (syn. Doratomyces) sp., was investigated. The fungal cultures were grown in laboratory microcosms consisting of Carboniferous limestone and after 21 d incubation at 25°C, biomineralization of fungal filaments was observed. Environmental electron scanning microscopy (ESEM) and X-ray micro-analysis (EDXA) of crystalline precipitates on the hyphae of S. himantioides demonstrated that the secondary crystals exhibited different crystalline forms but were similar in elemental composition to the original limestone. Powder X-ray diffraction (XRD) of crystalline precipitates showed they were composed of a mixture of calcite (CaCO ₃ ) and calcium oxalate monohydrate (CaC ₂ O ₄ · H ₂ O). Analysis of crystals precipitated on the hyphae of the limestone isolate, using ESEM and EDXA, showed that the crystals exhibited similar morphological characteristics and elemental composition to the original limestone. XRD showed that they were composed solely of calcite (CaCO ₃ ) or of calcite with some calcium oxalate dihydrate (CaC ₂ O ₄ · 2H ₂ O). These results provide direct experimental evidence for the precipitation of calcite (CaCO ₃ ) and also secondary mycogenic minerals, on fungal hyphae in low nutrient calcareous environments, and suggest that fungi may play a wider role in the biogeochemical carbon cycle than has previously been appreciated.     

微生物铁蛋白的研究进展

铁蛋白作为一种重要的铁储存蛋白,在不同的微生物体中普遍存在.通过对典型的微生物铁蛋白分子(FTN)的结构及其功能的归纳分析发现,铁蛋白依赖其独特的结构特点,在铁的补充、转运、氧化、成核和储存中扮演着重要作用,也对生物体内的多种生物化学反应影响显著.同时借助基因工程技术对铁蛋白进行相应的分子改造,增加了其作为纳米载体的应...     

From invagination to navigation: The story of magnetosome‐associated proteins in magnetotactic bacteria

Magnetotactic bacteria (MTB) are a group of Gram‐negative microorganisms that are able to sense and change their orientation in accordance with the geomagnetic field. This unique capability is due to the presence of a special suborganelle called the magnetosome, composed of either a magnetite or gregite crystal surrounded by a lipid membrane. MTB were first detected in 1975 and since then numerous efforts have been made to clarify the special mechanism of magnetosome formation at the molecular level. Magnetosome formation can be divided into several steps, beginning with vesicle invagination from the cell membrane, through protein sorting, followed by the combined steps of iron transportation, biomineralization, and the alignment of magnetosomes into a chain. The magnetosome‐chain enables the sensing of the magnetic field, and thus, allows the MTB to navigate. It is known that magnetosome formation is tightly controlled by a distinctive set of magnetosome‐associated proteins that are encoded mainly in a genomically conserved region within MTB called the magnetosome island (MAI). Most of these proteins were shown to have an impact on the magnetism of MTB. Here, we describe the process in which the magnetosome is formed with an emphasis on the different proteins that participate in each stage of the magnetosome formation scheme.