水体中亚硝酸盐积累的生物过程及影响因素研究进展

亚硝酸盐是氮循环过程的中间产物,其积累超过一定量则会抑制微生物的生长与代谢,也会给人与水生生物带来健康风险。而在高氮污水生物脱氮工艺中,持续维持亚硝酸盐的积累能实现短程硝化过程,降低生物脱氮的能耗进而降低运营成本。本文综述了在水环境中亚硝酸盐积累的生物过程与积累原因,并对影响亚硝酸盐积累的因素进行了总结,旨在为提高污水处理过程中氮的去除效率,降低运营成本,减少排放污水及自然水体中亚硝态氮含量提供参考。     

古菌在红树林沉积物中的多样性及其碳代谢机制

红树林湿地生态系统具有维持生物多样性、净化环境及维持海岸带生态平衡等多种功能。古菌普遍存在于红树林沉积物中,在元素的生物地球化学循环中发挥着重要作用。古菌具有丰富的碳代谢多样性,能固定CO_2,参与甲烷循环,产乙酸,降解蛋白质、多聚碳水化合物等有机质,但目前对于红树林沉积物中古菌碳代谢的研究才刚刚起步。高通量测序技术的快速发展促进了大量新的古菌门类的发现,这些新的古菌门类具备多样的碳代谢潜力。本文简要概述古菌的主要类群与分布,综述国内外有关古菌碳代谢多样性的最新研究进展,并阐明这些古菌在红树林生态系统中的生态分布和功能特征,为进一步探究古菌代谢机制提供知识基础。     

极端嗜盐古菌中CRISPR结构的生物信息学分析

摘要：【目的】利用生物信息学方法了解目前拥有全基因组序列的极端嗜盐古菌中CRISPR结构的特征。【方法】通过比对,保守性分析,GC含量分析,RNA结构预测等方法对已有全基因组序列的嗜盐古菌基因组进行研究。【结果】在5株嗜盐古菌基因组中发现CRISPR结构,在leader序列内得到具有回文性质的保守motif。发现在大CRISPR结构内repeat序列具有很强的保守性。同时根据第四位碱基的不同,repeat序列可形成两类不同的RNA二级结构。【结论】leader序列中回文结构的发现对其可能为蛋白结合位点的假     

氨氧化古菌及其对氮循环贡献的研究进展

硝化作用先将氨氮氧化为亚硝酸盐氮并进一步氧化为硝酸盐氮,这一过程是氮进行全球生物化学循环的重要环节。随着氨氧化古菌(Ammonia-oxidizing archaea,AOA)基因组序列中氨单加氧酶编码基因(amoA)的发现以及AOA在实验室条件下的成功培养(包括分离纯化和富集培养),基于分子生物学的研究表明AOA在各种环境广泛存在,且多数生境中它的数量远远超过氨氧化细菌(Ammonia-oxidizing bacteria,AOB)。AOA相对于AOB在氮循环中的贡献也引起了多方面的论证和争论。本文就氨氧化古菌的生态分布、系统进化、生境存在丰度及参与硝化作用等进行综述,指出不同生境AOA的活性及其对氮循环的重要性仍需做进一步的研究。     

攀枝花不同海拔高度烤烟农田红壤中氨氧化细菌与氨氧化古菌的群落结构分析

为探究攀枝花干热河谷区农田土壤氨氧化古菌（Ammonia oxidizing archaea,AOA）与氨氧化细菌（Ammonia oxidizing bacteria,AOB）群落对海拔高度的响应特征,深入认识该区域的氮素循环过程。以攀枝花米易县不同海拔（1600 m、1800 m和2000 m）农田红壤为研究对象,运用化学分析和末端限制性片段长度多态性（Terminal restriction fragment length polymorphism,T-RFLP）分别测定土壤理化性质、AOA和AOB群落组成及多样性,研究不同海拔农田土壤中AOA和AOB群落变异及其驱动因子。研究结果显示,不同海拔农田土壤pH均小于7,土壤有机碳（SOC）、全氮（TN）、速效钾（AK）和铵态氮（NH₄⁺-N）含量随海拔升高而降低,碱解氮（AN）、有效磷（AP）和硝态氮（NO₃^--N）含量随海拔升高先增加后降低;随海拔升高,AOA群落多样性指数增加,而AOB群落多样性指数先增加后降低;AOA以亚硝基球菌属（Nitrososphaera）为优势菌群,AOB以亚硝化螺菌属（Nitrosospira）为优势菌群;土壤有机碳（SOC）、速效钾（AK）和硝态氮（NO₃^--N）是影响该区域农田土壤AOA和AOB群落发育的主要因子。总体而言,攀枝花干热河谷区不同海拔农田土壤AOA和AOB群落结构变化明显,土壤硝态氮、速效钾和有机碳是影响AOA和AOB群落结构变异的主要因子;研究结果可为揭示干热河谷区农田红壤氮循环相关微生物的海拔分布格局提供理论依据。     

甲烷代谢古菌分离培养研究进展

全球变暖是全人类面临的一个巨大挑战,而温室气体排放持续上升是全球变暖的关键因素,并引发一系列生态环境问题。甲烷是第二温室气体,对全球变暖的贡献达20%。然而,在甲烷代谢中发挥重要作用的产甲烷古菌和厌氧甲烷氧化古菌(anaerobic methanotroph,ANME)较难培养,极大地限制了人们对甲烷代谢及其影响碳源-汇关系与机制的研究。本文综述了最新产甲烷古菌和ANME富集、分离和培养方法,包括富集培养、原位培养、共培养、微流控技术、稀释分离和固体分离技术、ANME反应器和培养瓶富集培养,以及宏基因组预测和反向基因组学,并对这些方法的优缺点进行了评估,对未来甲烷代谢古菌的富集、分离和培养提出新的建议。     

Structural basis for activation of an archaeal ribonuclease P RNA by protein cofactors

Ribonuclease P (RNase P) is an endoribonuclease that catalyzes the processing of the 5′-leader sequence of precursor tRNA (pre-tRNA) in all phylogenetic domains. We have found that RNase P in the hyperthermophilic archaeon Pyrococcus horikoshii OT3 consists of RNase P RNA (PhopRNA) and five protein cofactors designated PhoPop5, PhoRpp21, PhoRpp29, PhoRpp30, and PhoRpp38. Biochemical characterizations over the past 10 years have revealed that PhoPop5 and PhoRpp30 fold into a heterotetramer and cooperate to activate a catalytic domain (C-domain) in PhopRNA, whereas PhoRpp21 and PhoRpp29 form a heterodimer and function together to activate a specificity domain (S-domain) in PhopRNA. PhoRpp38 plays a role in elevation of the optimum temperature of RNase P activity, binding to kink-turn (K-turn) motifs in two stem-loops in PhopRNA. This review describes the structural and functional information on P. horikoshii RNase P, focusing on the structural basis for the PhopRNA activation by the five RNase P proteins.     

Dynamics of a bloom of halophilic archaea in the Dead Sea

After a period of more than ten years in which bacterial and algal community sizes were extremely small, a dense bloom of halophilic archaea developed in the upper 5–10 m of the Dead Sea water column in the summer of 1992. The development of this bloom followed a dilution of the upper water layer by winter rainfloods, which enabled the development of a short-lived dense bloom of the unicellular green alga Dunaliella parva. The dense archaeal community (up to 3.5 × 10⁷ cells m1^–1 in June 1992) imparted a red coloration to the Dead Sea, due to its high content of bacterioruberin. Bacteriorhodopsin was not detected. High levels of potential heterotrophic activity were associated with the bloom, as measured by the incorporation of labeled organic substrates. After the decline of the algal bloom, archaeal numbers in the lake decreased only little, and most of the community was still present at the end of 1993. The amount of carotenoid pigment per cell, however, decreased 2–3-fold between June 1992 and August 1993. No new algal and archaeal blooms developed after the winter floods of 1992–1993, in spite of the fact that salinity values in the surface layer were sufficiently low to support a new algal bloom. A remnant of the 1992 Dunaliella bloom maintained itself at the lower end of the pycnocline at depths between 7 and 13 m (September 1992–August 1993). Its photosynthetic activity was small, and very little stimulation of archaeal growth and activity was associated with this algal community.     

A Protein Related to Eucaryal and Bacterial DNA-Motor Proteins in the Hyperthermophilic Archaeon Sulfolobus acidocaldarius

We have isolated a new gene encoding a putative 103-kDa protein from the hyperthermophilic archaeon Sulfolobus acidocaldarius. Analysis of the deduced amino-acid sequence shows an extended central domain, predicted to form coiled-coil structures, and two terminal domains that display purine NTPase motifs. These features are reminiscent of mechanochemical motor proteins which use the energy of ATP hydrolysis to move specific cellular components. Comparative analysis of the amino-acid sequence of the terminal domains and predicted structural organization of this putative purine NTPase show that it is related both to eucaryal proteins from the ``SMC family' involved in the condensation of chromosomes and to several bacterial and eucaryal proteins involved in DNA recombination/repair. Further analyses revealed that these proteins are all members of the so called ``UvrA-related NTP-binding proteins superfamily' and form a large subgroup of motor-like NTPases involved in different DNA processing mechanisms. The presence of such protein in Archaea, Bacteria, and Eucarya suggests an early origin of DNA-motor proteins that could have emerged and diversified by domain shuffling. Received: 29 June 1996 / Accepted: 28 February 1997     

Cloning and sequencing of the gene encoding the cell surface glycoprotein of Haloarcula japonica strain TR-1

The triangular disk-shaped halophilic archaeon Haloarcula japonica strain TR-1 has a glycoprotein on its cell surface. The complete gene encoding the cell surface glycoprotein (CSG) was cloned and sequenced. The gene has an open reading frame of 2586 bp, and a potential archaeal promoter sequence approximately 150 bp upstream of the ATG initiation codon. The mature CSG is composed of 828 amino acids and is preceded by a signal sequence of 34 amino acid residues. A hydropathy analysis showed a hydrophobic stretch at the C-terminus, that probably serves as a transmembrane domain. The amino acid sequence of the Ha. japonica CSG showed 52.1% and 43.2% identities to those from the Halobacterium halobium and Haloferax volcanii CSGs, respectively. Five potential N-glycosylation sites were found in the mature Ha. japonica CSG, sites that were distinctly different from those in Hb. halobium and Hf. volcanii. The Ha. japonica CSG gene was expressed in Escherichia coli. Received: 20 September 1996 / Accepted: 9 October 1996