生物滤塔体系好氧反硝化菌的分离鉴定与特性研究

从实验室生物滤塔填料的生物膜上, 经选择性培养基筛选, 分离出4株好氧反硝化菌。好氧状态下4种菌的40 h反硝化率均大于80%, 其中菌种A1反硝化率可达到99.05%。跟踪菌种反硝化过程中氮元素24 h变化过程, 发现4株菌除A1外都有亚硝酸根积累。菌种A1为短杆菌, 革兰氏阴性。生理生化特性研究与16S rDNA 序列测定(GenBank接受号DQ836052.1)初步判定菌种A1为假单胞菌Pseudomonas putida。适于菌A1生长的初始pH值是7.0左右, 温度30℃左右, 当DO大于2.0 mg/L时, DO的变化对菌种A1的反硝化效果影响很小。     

Hydrogen as an energy source for the human pathogen <Emphasis Type="Italic">Bilophila wadsworthia</Emphasis>

The gram-negative anaerobic gut bacterium Bilophila wadsworthia is the third most common isolate in perforated and gangrenous appendicitis, being also found in a variety of other infections. This organism performs a unique kind of anaerobic respiration in which taurine, a major organic solute in mammals, is used as a source of sulphite that serves as terminal acceptor for the electron transport chain. We show here that molecular hydrogen, one of the major products of fermentative bacteria in the colon, is an excellent growth substrate for B. wadsworthia. We have quantified the enzymatic activities associated with the oxidation of H₂, formate and pyruvate for cells obtained in different growth conditions. The cell extracts present high levels of hydrogenase activity, and up to five different hydrogenases can be expressed by this organism. One of the hydrogenases appears to be constitutive, whereas the others show differential expression in different growth conditions. Two of the hydrogenases are soluble and are recognised by antibodies against a [FeFe] hydrogenase of a sulphate reducing bacterium. One of these hydrogenases is specifically induced during fermentative growth on pyruvate. Another two hydrogenases are membrane-bound and show increased expression in cells grown with hydrogen. Further work should be carried out to reveal whether oxidation of hydrogen contributes to the virulence of B. wadsworthia.     

Biotransformation of (+)-catechin into taxifolin by a two-step oxidation: primary stage of (+)-catechin metabolism by a novel (+)-catechin-degrading bacteria, Burkholderia sp. KTC-1, isolated from tropical peat

Peat contains various persistent compounds derived from plant materials. We isolated a novel (+)-catechin-degrading bacterium, Burkholderia sp. KTC-1 (KTC-1), as an example of a bacterium capable of degrading persistent aromatic compounds present in tropical peat. This bacterium was isolated by an enrichment technique and grew on (+)-catechin as the sole carbon source under acidic conditions. The reaction of a crude enzyme extract and a structural study of its products showed that (+)-catechin is biotransformed into taxifolin during the preliminary stages of its metabolism by KTC-1. HPLC analysis showed that this transformation occurs in two oxidation steps: 4-hydroxylation and dehydrogenation. Furthermore, both (+)-catechin 4-hydroxylanase and leucocyanidin 4-dehydrogenase were localized in the cytosol of KTC-1. This is the first report on biotransformation of (+)-catechin into taxifolin via leucocyanidin by an aerobic bacterium. We suggest that tropical peat could become a unique resource for microorganisms that degrade natural aromatic compounds.     

Glycosylation of the OMP85 homolog of Porphyromonas gingivalis and its involvement in biofilm formation

OMP85 is a highly conserved outer membrane protein in all Gram-negative bacteria. We studied an uncharacterized OMP85 homolog of Porphyromonas gingivalis, a primary periodontal pathogen forming subgingival plaque biofilms. Using an outer-loop peptide antibody specific for the OMP85 of P. gingivalis, loop-3 Ab, we found a difference in the mobility of OMP85 on SDS-PAGE gel between the P. gingivalis wild-type and the isogenic galE mutant, a deglycosylated strain, suggesting that OMP85 naturally exists in a glycosylated form. This was also supported by a shift in OMP85 PAGE mobility after chemical deglycosylation treatment. Further, loop-3 Ab cross-reacted with the galE mutant stronger than the wild-type strain; and could inhibit biofilm formation in the galE mutant more than in the wild-type strain. In conclusion, this is the first report providing the evidence of OMP85 glycosylation and the involvement of OMP85 in biofilm formation.     

The effects of shredding invertebrates on the transfer of organic carbon from littoral leaf litter to water-column bacteria

Leaf litter can be of great importance for the productivity of small oligotrophic lakes surrounded by deciduous forests. Feeding invertebrate shredders produce particulate organic leftovers, but their feeding also enhances the release of dissolved organic carbon (DOC). We tested whether invertebrate-mediated DOC release affects the production of heterotrophic water-column bacteria. Submersed leaves were incubated in microcosms with and without shredders; and DOC, absorbance, bacterial abundance and bacterial production in the water column were monitored. We also measured dry weight of the organic particles (FPOC, fine particulate organic carbon, leaf residues and shredders). Total leaf-litter carbon decreased by nearly 80% in the presence of shredders, and on average 56% of the initial leaf carbon ended up as FPOC after 126 days of incubation. Without shredders FPOC production was almost zero, and 72% of the added leaf carbon could be retrieved as leaves when the experiment ended. Both these figures include the rapid release of DOC during the first week of leaf incubation in the lake water (equivalent to 16–19% of total added leaf carbon). Although bacterial production in the water was several times higher in treatments with shredders, bacterial consumption of leaf-derived DOC from shredding was obviously of minor importance in the total carbon budget. This result suggests, although shredders have a strong impact on transformation of leaves to FPOC, they do not greatly enhance the initial rate of mineralization of the leaf-derived detritus.     

Spatial distribution,size structure,and prey of Craspedacusta sowerbyi Lankester in a shallow New Zealand lake

Solar ultraviolet radiation both degrades and alters the quality of natural organic matter as well as organic pollutants in surface waters. Still, it is only recently that this indirect influence of photochemical processes on aquatic organisms (e.g. bacteria) has received attention. We experimentally studied the photochemical degradation of three PAHs; anthracene, phenanthrene and naphthalene, in water. Anthracene and phenanthrene were rapidly photodegraded (half-lives of 1 and 20.4 hours, respectively), while the photochemical half-life of naphthalene exceeded 100 hours. Hence photodegradation is most likely a less important removal mechanism for the latter compound. The influence of humic substance additions (0–25 mg C l^–1) on degradation rates was also assessed, and while photodegradation of anthracene was not affected by these additions, phenanthrene photodegradation slowed down considerably at the higher humic substance concentrations. These differential responses of anthracene and phenanthrene can at least partially be explained by differences in the spectral absorbance of the two compounds. In contrast, ionic strength did not have any appreciable effect on the estimated photodegradation rates of either compound. The influence of PAHs on growth of aquatic bacteria was assessed in dilution cultures with and without exposure to PAHs and simulated solar UV radiation. Separately, neither PAHs nor simulated solar UV radiation had any effect on bacterial growth. However, when combined, a marked inhibition of bacterial growth could be observed in water obtained from a clearwater lake. This could be due to the formation of toxic photodegradation products such as quinones (detected in our incubations) or other reactive species that affect bacteria negatively. Hence, in addition to influencing the fate and persistence of PAHs in aquatic systems, solar radiation and natural organic matter and regulate the toxicity of these compounds to indigenous micro-organisms.     

The effect of bacteria on interspecific relationships between the euryhaline rotifer Brachionus rotundiformis and the harpacticoid copepod Tigriopus japonicus

Inconsistent results have been obtained on the population growth of Brachionus rotundiformis and Tigriopus japonicus, when results from single-species and two-species mixed cultures are compared. Bacteria growth was not regulated in these experiments, which could be the cause for this. In order to test this possibility, we conducted similar experiments under axenic and synxenic (with presence of one species of bacteria) conditions. The population growth of B. rotundiformis was suppressed by the presence of T. japonicus in axenic cultures. T. japonicus could not persist in axenic cultures, but its population increased when grown in synxenic cultures. T. japonicus used RT bacteria strain as a food source, while these bacteria were toxic to B. rotundiformis. These results suggest that bacteria can modify the interspecific relationship between B. rotundiformis and T. japonicus.     

Synthesis of Anabiosis Autoinducers by Non-Spore-Forming Bacteria as a Mechanism Regulating Their Activity in Soil and Subsoil Sedimentary Rocks

Non-spore-forming bacteria of the genera Arthrobacterand Micrococcus, isolated from permafrost subsoil, were found to produce greater amounts of the d ₁extracellular factor than closely related collection strains isolated from soil. The effect of this factor, responsible for cell transition to anabiosis, was not species-specific. Thus, the d ₁preparation isolated from the culture liquid of the permafrost isolate Arthrobacter globiformis245 produced an effect on the collection strain Arthrobacter globiformisB-1112 and also on Micrococcus luteusand Bacillus cereus.The d ₁preparation from the permafrost isolate of Arthrobacterdiffered from the chemical analogue of this factor, 4-n-hexylresorcinol, in the level of the induced cell response, which may have resulted from different cell sensitivity to various homologs of alkylhydroxybenzenes contained in the d ₁preparation. Thus, additional evidence was obtained indicating that autoregulation of bacterial growth and development is implemented at the level of intercellular interactions in microbial communities. Abundant production of the d ₁anabiosis-inducing factors by bacteria isolated from permafrost subsoil is probably a result of special antistress mechanisms responsible for the survival of these bacteria under extreme conditions of natural long-term cooling.     

Effect on the Medium Salinity on Oil Degradation by Nocardioform Bacteria

Oil degradation by cultures of Rhodococcus erythropolisand Dietzia mariswas found to depend on the NaCl concentration in the medium. Optimal utilization of turbine oil by R. erythropolisand D. mariswas observed at 0.5 and 2 to 5% NaCl concentration, respectively. Mineral oil and a mixture of paraffins (C₁₄–C₁₈) were utilized within a broader range of the medium salinity. As shown by fluorescent microscopy, D. mariscolonies formed on the oil drop surface, whereas R. erythropoliscells penetrated the drops. The strains studied may populate various ecological niches in oil-containing ecosystems. They are promising for the development of microbial preparations for cleaning the environment from oil pollution.     

Colony Structure of a Consortium of Nitrifying Bacteria

Colonies produced by a consortium of nitrifying bacteria were studied using light and electron microscopy. The colonies were obtained by direct plating of inoculum from a two-stage nonsterile chemostat fermentor and by repeatedly passing the microbial community of the fermentor through selective media containing ammonium or nitrite. The colonies studied can be characterized by a specific combination of six types of cells differing in their ultrastructure and spatial location within the colony. The types of cells occurring within a given colony were found to depend on the nitrogen compound present in the medium. As a result of our study, morphological features of colonial bacterial communities were identified. The proposed approach can be viewed as a method to describe microbial associations and communities.