Growth of ammonia-oxidizing archaea in soil microcosms is inhibited by acetylene

Autotrophic ammonia-oxidizing bacteria were considered to be responsible for the majority of ammonia oxidation in soil until the recent discovery of the autotrophic ammonia-oxidizing archaea. To assess the relative contributions of bacterial and archaeal ammonia oxidizers to soil ammonia oxidation, their growth was analysed during active nitrification in soil microcosms incubated for 30 days at 30 °C, and the effect of an inhibitor of ammonia oxidation (acetylene) on their growth and soil nitrification kinetics was determined. Denaturing gradient gel electrophoresis (DGGE) analysis of bacterial ammonia oxidizer 16S rRNA genes did not detect any change in their community composition during incubation, and quantitative PCR (qPCR) analysis of bacterial amoA genes indicated a small decrease in abundance in control and acetylene-containing microcosms. DGGE fingerprints of archaeal amoA and 16S rRNA genes demonstrated changes in the relative abundance of specific crenarchaeal phylotypes during active nitrification. Growth was also indicated by increases in crenarchaeal amoA gene copy number, determined by qPCR. In microcosms containing acetylene, nitrification and growth of the crenarchaeal phylotypes were suppressed, suggesting that these crenarchaea are ammonia oxidizers. Growth of only archaeal but not bacterial ammonia oxidizers occurred in microcosms with active nitrification, indicating that ammonia oxidation was mostly due to archaea in the conditions of the present study.     

Complete genome sequence of Methanoculleus marisnigri Romesser et al. 1981 type strain JR1

Methanoculleus marisnigri Romesser et al. 1981 is a methanogen belonging to the order Methanomicrobiales within the archaeal phylum Euryarchaeota. The type strain, JR1, was isolated from anoxic sediments of the Black Sea. M. marisnigri is of phylogenetic interest because at the time the sequencing project began only one genome had previously been sequenced from the order Methanomicrobiales. We report here the complete genome sequence of M. marisnigri type strain JR1 and its annotation. This is part of a Joint Genome Institute 2006 Community Sequencing Program to sequence genomes of diverse Archaea.     

Proteomic characterization of the sulfur-reducing hyperthermophilic archaeon Thermococcus onnurineus NA1 by 2-DE/MS–MS

Thermococcus onnurineus NA1, a sulfur-reducing hyperthermophilic archaeon, was isolated from a deep-sea hydrothermal vent area in Papua New Guinea. The strain requires elemental sulfur as a terminal electron acceptor for heterotrophic growth on peptides, amino acids and sugars. Recently, genome sequencing of Thermococcus onnurineus NA1 was completed. In this study, 2-DE/MS–MS analysis of the cytosolic proteome was performed to elucidate the metabolic characterization of Thermococcus onnurineus NA1 at the protein level. Among the 1,136 visualized protein spots, 110 proteins were identified. Enzymes related to metabolic pathways of amino acids utilization, glycolysis, pyruvate conversion, ATP synthesis, and protein synthesis were identified as abundant proteins, highlighting the fact that these are major metabolic pathways in Thermococcus onnurineus NA1. Interestingly, multiple spots of phosphoenolpyruvate synthetase and elongation factor Tu were found on 2D gels generated by truncation at the N-terminus, implicating the cellular regulatory mechanism of this key enzyme by protease degradation. In addition to the proteins involved in metabolic systems, we also identified various proteases and stress-related proteins. The proteomic characterization of abundantly induced proteins using 2-DE/MS–MS enables a better understanding of Thermococcus onnurineus NA1 metabolism.     

Life‐style changes of a halophilic archaeon analyzed by quantitative proteomics

Quantitative proteomics based on isotopic labeling has become the method of choice to accurately determine changes in protein abundance in highly complex mixtures. Isotope‐coded protein labeling (ICPL), which is based on the nicotinoylation of proteins at lysine residues and free N‐termini was used as a simple, reliable and fast method for the comparative analysis of three different cellular states of the halophilic archaeon Halobacterium salinarum through pairwise comparison. The labeled proteins were subjected to SDS‐PAGE, in‐gel digested and the proteolytic peptides were separated by LC and analyzed by MALDI‐TOF/TOF MS. Automated quantitation was performed by comparing the MS peptide signals of ¹²C and ¹³C nicotinoylated isotopic peptide pairs. The transitions between (i) aerobic growth in complex versus synthetic medium and (ii) aerobic versus anaerobic/phototrophic growth, both in complex medium, provide a wide span in nutrient and energy supply for the cell and thus allowed optimal studies of proteome changes. In these two studies, 559 and 643 proteins, respectively, could be quantified allowing a detailed analysis of the adaptation of H. salinarum to changes of its living conditions. The subtle cellular response to a wide variation of nutrient and energy supply demonstrates a fine tuning of the cellular protein inventory.     

Oligomerization behavior of the archaeal Sm2-type protein from Archaeoglobus fulgidus

As part of a functional analysis of archaeal Sm-related proteins, we have studied the oligomerization behavior of the Sm-2 type protein from the euryarchaeon Archaeoglobus fulgidus using gel filtration chromatography and noncovalent mass spectrometry. Our experiments show that the oligomeric state of the protein depends on the pH and presence of RNA. The protein forms a hexamer at acidic pH in the absence of RNA. The addition of RNA (oligo U10) induces the formation of a heptamer over the whole pH range studied. The stability of both the hexamer and the RNA-bound heptamer increases at lower pH.     

Interactions of RadB, a DNA repair protein in archaea, with DNA and ATP

The RecA family of recombinases (RecA, Rad51, RadA and UvsX) catalyse strand-exchange between homologous DNA molecules by utilising conserved DNA-binding modules and a common core ATPase domain. RadB was identified in archaea as a Rad51-like protein on the basis of conserved ATPase sequences. However, RadB does not catalyse strand exchange and does not turn over ATP efficiently. RadB does bind DNA, and here we report a triplet of residues (Lys-His-Arg) that is highly conserved at the RadB C terminus, and is crucial for DNA binding. This is consistent with the motif forming a "basic patch" of highly conserved residues identified in an atomic structure of RadB from Thermococcus kodakaraensis. As the triplet motif is conserved at the C terminus of XRCC2 also, a mammalian Rad51-paralogue, we present a phylogenetic analysis that clarifies the relationship between RadB, Rad51-paralogues and recombinases. We investigate interactions between RadB and ATP using genetics and biochemistry; ATP binding by RadB is needed to promote survival of Haloferax volcanii after UV irradiation, and ATP, but not other NTPs, induces pronounced conformational change in RadB. This is the first genetic analysis of radB, and establishes its importance for maintaining genome stability in archaea. ATP-induced conformational change in RadB may explain previous reports that RadB controls Holliday junction resolution by Hjc, depending on the presence or the absence of ATP.     

镉对小鼠精母细胞凋亡及附睾内精子质量的影响

采用人工水质染毒的方法,利用透射电镜技术及流式细胞术（FCM）,探讨重金属镉对小鼠精巢内生殖细胞凋亡及附睾内成熟精子质量的影响.结果表明：各试验组小鼠生殖细胞处于凋亡时期的数量显著高于对照组,凋亡时期的生殖细胞超微结构呈现出线粒体空泡、核膜内陷、染色质周缘化及核固缩等形态特征,表明镉容易引起小鼠生殖细胞凋亡;各试验组精子早期凋亡的比例显著高于对照组,而活性精子的比例显著低于对照组（P<0.05）,其中高剂量组（0.10 mmol·L^-1）精子成活率（75.1%）显著低于对照组和其他试验组,而早期凋亡率（22.6%）则显著高于对照组;高剂量组睾丸生殖细胞DNA断裂率（18.2%）及附睾精子断裂率（26.5%）均显著高于对照组（3.3%、5.6 %）（P<0.05）.各试验组小鼠睾丸内DNA断裂的生殖细胞数量低于附睾内DNA断裂的精子数量.随着添加剂量的增加,小鼠睾丸内生殖细胞及附睾内精子凋亡率逐渐升高.表明小鼠生殖细胞凋亡及DNA损伤数量与镉剂量具有一定相关性.     

Detection of Ammonia-Oxidizing Archaea in Fish Processing Effluent Treatment Plants

Ammonia oxidation is the rate limiting step in nitrification and thus have an important role in removal of ammonia in natural and engineered systems with participation of both ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB). However, their relative distribution and activity in fish processing effluent treatment plants (FPETPs) though significant, is hitherto unreported. Presence of AOA in sludge samples obtained from FPETPs was studied by amplification and sequencing of thaumarchaeal ammonia monooxygenase subunit A (AOA-amoA) gene. Different primer sets targeting 16S rRNA and AOA-amoA gene were used for the detection of AOA in FPETPs. Phylogenetic analysis of the gene revealed that the AOA was affiliated with thaumarchaeal group 1.1a lineage (marine cluster). Quantitative real time PCR of amoA gene was used to study the copy number of AOA and AOB in FPETPs. The AOA-amoA and AOB-amoA gene copy numbers of sludge samples ranged from 2.2 × 10⁶ to 4.2 × 10⁸ and 1.1 × 10⁷ to 8.5 × 10⁸ mg⁻¹ sludge respectively. Primer sets Arch-amoAF/Arch-amoAR and 340F/1000R were found to be useful for the sensitive detection of AOA-amoA and Archaeal 16S rRNA genes respectively in FPETPs. Their presence suggests the widespread occurrence and possible usefulness in removing ammonia from FPETPs which is in line with reports from other waste water treatment plants.

Electronic supplementary material

The online version of this article (doi:10.1007/s12088-014-0484-6) contains supplementary material, which is available to authorized users.     

A rapid DNA extraction method for PCR amplification from wetland soils

Aims: We tested a method of rapid DNA extraction from wetland soil samples for use in the polymerase chain reaction. Methods and Results: The glass bead/calcium chloride/SDS method obtained in the present study was compared with the calcium chloride/SDS/enzymatic extraction method and the UltraClean? Soil DNA Isolation Kit. Rapid DNA extraction could be completed within about two hours without purification steps. Conclusions: This study succeeded in establishing a fast soil DNA extraction protocol that can be applied to various environmental sources that are rich in humic acid content. Significance and Impact of the Study: The method provides a technology with high‐quality DNA extraction from soils for testing the diversity of AOB and AOA.     

An Acidophilic Bacterial-Archaeal-Fungal Ecosystem Linked to Formation of Ferruginous Crusts and Stalactites

The presence of specialized microbial associations between populations of chemoautotrophic bacteria and archaea with ascomycetous fungi was observed inside stalactite-shaped mineral formations in a highly acidic cave environment. Metagenomic, chemical and electron microscopy analyses were used to investigate the relevance of these microbial ecosystems in the formation of stalactites. Ferric hydroxide produced by acidophilic bacteria and archaea was shown to be deposited onto fungal hyphae, resulting in complex mineralized stalactite-shaped structures. Thus, both archaeal-bacterial and fungal members of the ecosystem were shown to play an active role in the formation of stalactites.