复合菌系RSS-4腐解稻秆过程中的菌系动态变化

采用传统平扳分离培养方法和PCR—DGGE技术研究了水稻秸秆腐解复合菌系RSS-4在腐解稻秆过。程中菌种区系变化情况。结果表明：平板分离培养方法显示,在稻秆腐解过程中,微生物的数量呈现出先升后降的变化趋势,在整个腐解过程中细菌的数量占优势;DGGE图谱显示,至少有12种细菌和18种真菌的近缘种参与到稻秆的腐解过程。在其腐解过程中,不同腐解阶段真菌的组成呈现出多样性,数量变化差异也较大：细菌DGGE图谱中的条带1、9、10等以及真菌DGGE图谱中的条带8、9、13等为优势菌株,它们贯穿于稻秤腐解的整个过程;细菌中的条带12以及真菌中的条带4在腐解的前期起作用,而后迅速消失;细菌中的条带3、11等以及真菌中的条带3、10等在腐解的后期才出现而起作用;而细菌中的条带2以夏真菌中的条带1、5等仅出现在腐解的莱一时期。     

干旱胁迫下CO2浓度升高对转StAPX番茄植株耐旱能力的影响

在干旱胁迫伴随大气CO2浓度以及升高的CO2浓度（加倍）条件下,以过量表达番茄类囊体膜抗坏血酸过氧化物酶基因（StAPX）的转基因番茄为试材,探明干旱胁迫TCO2浓度升高对转基因及其野生型番茄植株清除活性氧及耐旱能力的影响。结果表明：升高的CO2浓度明显增加了干旱胁迫下植物的光合水平;升高的CO2浓度明显降低了干旱导致的植物体内H2O2．和O2的积累,影响了干旱胁迫下番茄植株的水．水循环系统的活性氧清除酶活性和小分子抗氧化物质含量;干旱胁迫下即使伴随升高的CO2浓度,测试番茄植株体内的渗透调节物质含量变化也不太明显;升高的CO2浓度明显降低了干旱胁迫下的植物细胞膜伤害程度;干旱胁迫下,升高的CO2浓度对转基因番茄株系比对野生型植株的影响更加明显。结果证明干旱逆境下,升高的CO2浓度能够在一定程度上进一步提高转基因番茄植株的耐旱性。     

Interactive Effects of Drought Stresses and Elevated CO2 Concentration on Photochemistry Efficiency of Cucumber Seedlings

To reveal and quantify the interactive effects of drought stresses and elevated CO2 concentration [CO2] on photochemistry efficiency of cucumber seedlings, the portable chlorophyll meter was used to measure the chlorophyll content, and the Imaging-PAM was used to image the chlorophyll fluorescence parameters and rapid light response curves (RLC) of leaves in two adjacent greenhouses. The results showed that chlorophyll content of leaves was reduced significantly with drought stress aggravated. Minimal fluorescence (Fo) was increased while maximal quantum yield of PSII (Fv/Fm) decreased significantly by severe drought stress. The significant decrease of effective quantum yield of PSll (Y(Ⅱ)) accompanied by the significant increase of quantum yield of regulated energy dissipation (Y(NPQ)) was observed under severe drought stress condition, but there was no change of quantum yield of nonregulated energy dissipation (Y(NO)). We detected that the coefficient of photochemical quenching (Qp) decreased, and non-photochemical quenching (NPQ) increased significantly under severe drought stress. Furthermore, we found that maximum apparent electron transport rate (ETRmax) and saturating photosynthetically active radiation (PPFDsat) decreased significantly with drought stress aggravated. However, elevated [CO2] significantly increased FvlFm, Qp and PPFDsat, and decreased NPQ under all water conditions, although there were no significant effects on chlorophyll content, Fo, Y(Ⅱ), Y(NPQ), Y(NO) and ETRmax. Therefore, it is concluded that CO2-fertilized greenhouses or elevated atmospheric [CO2] in the future could be favorable for cucumber growth and development, and beneficial to alleviate the negative effects of drought stresses to a certain extent.     

全球大气CO2浓度升高对土壤微生物的影响

全球大气CO2浓度升高对土壤微生物生态系统的影响已引起广泛关注。本文从土壤微生物群落结构、微生物区系、土壤呼吸、微生物生物量以及土壤酶活性方面对大气高浓度CO2的响应进行了综述。由于提供高浓度CO2的实验系统、所选植物材料以及土壤特性等的不同,大气CO2浓度升高对土壤微生物群落结构、微生物区系、土壤呼吸、微生物生物量以及土壤酶活性的影响并未得出一致结论。但高浓度CO2对土壤微生物生态系统的影响是存在的。     

Elevated CO2 and temperature impacts on different components of soil CO2 efflux in Douglas-fir terracosms

Although numerous studies indicate that increasing atmospheric CO₂ or temperature stimulate soil CO₂ efflux, few data are available on the responses of three major components of soil respiration [i.e. rhizosphere respiration (root and root exudates), litter decomposition, and oxidation of soil organic matter] to different CO₂ and temperature conditions. In this study, we applied a dual stable isotope approach to investigate the impact of elevated CO₂ and elevated temperature on these components of soil CO₂ efflux in Douglas-fir terracosms. We measured both soil CO₂ efflux rates and the ¹³C and ¹⁸O isotopic compositions of soil CO₂ efflux in 12 sun-lit and environmentally controlled terracosms with 4-year-old Douglas fir seedlings and reconstructed forest soils under two CO₂ concentrations (ambient and 200 ppmv above ambient) and two air temperature regimes (ambient and 4 °C above ambient). The stable isotope data were used to estimate the relative contributions of different components to the overall soil CO₂ efflux. In most cases, litter decomposition was the dominant component of soil CO₂ efflux in this system, followed by rhizosphere respiration and soil organic matter oxidation. Both elevated atmospheric CO₂ concentration and elevated temperature stimulated rhizosphere respiration and litter decomposition. The oxidation of soil organic matter was stimulated only by increasing temperature. Release of newly fixed carbon as root respiration was the most responsive to elevated CO₂, while soil organic matter decomposition was most responsive to increasing temperature. Although some assumptions associated with this new method need to be further validated, application of this dual-isotope approach can provide new insights into the responses of soil carbon dynamics in forest ecosystems to future climate changes.     

Early Development of Soil Microbial Communities on Rehabilitated Quarries

The ecological development of soil microbial communities was studied in terms of microbial composition and structure at different rehabilitated phases on three quarries, namely Turret Hill Quarry (TH), Lam Tei Quarry (LT), and Shek O Quarry (SO), in Hong Kong. Using individual fatty acid methylesters (FAMEs) as biomarkers, Gram^? bacteria dominated at all sites, in which cy19:0 represented more than 15% of the total extracted FAMEs in all soils tested. Redundancy analysis showed that the abundance of Gram^? bacteria and Gram⁺ bacteria correlated significantly with woody species richness, native species richness, organic C, total N, and extractable NO₃‐N. Fungi (18:1w9c and 18:2w6) and arbuscular mycorrhizal (AM) fungi (16:1w5c) decreased in abundance with increasing age in SO and LT, which were positively correlated with grass coverage, soil pH, extractable NH₄‐N, and extractable P. Our study suggested that soil aeration and C availability in soils played a dominant role driving the changes in the composition and structure of Gram^? bacteria and Gram⁺ bacteria communities. Available P was the limiting factor for regulating the fungal and AM fungal communities on our local quarries.     

复合菌系RSS-4传代对水稻秸秆腐解的影响

对筛选到的1组稻秆腐解复合菌系RSS-4,以腐解产物的pH值、酶活及稻秆失重率为指标,研究了该复合菌系的性质稳定性和功能稳定性;并用变性梯度凝胶电泳法(DGGE)分析了该复合菌系的菌种组成稳定性。结果表明,多代继代培养过程中各代复合菌系腐解产物的pH值变化趋势基本一致,pH值从起始的6.72左右迅速升至最高点7.75,然后逐渐下降并稳定在7.20;多代继代培养后复合菌系各代之间的酶活动态变化及其对稻秆腐解能力的差异均很小。在连续继代培养的过程中,DGGE图谱揭示第15~23代复合菌系之间的菌种组成没有明显差异。     

CO2浓度升高对大豆干旱胁迫的缓解效应

CO2浓度升高和干旱带来的气候变化势必对大豆的生长造成影响.目前,CO2浓度升高对干旱胁迫下大豆生理生化的影响研究较少.本试验研究了不同CO2浓度(400、600 pumol ? mol-1)和水分处理下(正常水分:叶片相对含水量为83％-90％;干旱:叶片相对含水量为64％-70％)大豆开花期的光合能力、光合色素积累...     

Elevated Atmospheric CO2 Alters Soil Microbial Communities Associated with Trembling Aspen (Populus tremuloides) Roots

Global atmospheric CO₂ levels are expected to double within the next 50 years. To assess the effects of increased atmospheric CO₂ on soil ecosystems, cloned trembling aspen (Populus tremuloides) seedlings were grown individually in 1 m³ open bottom root boxes under either elevated (720 ppm, ELEV) or ambient CO₂ (360 ppm, AMB). After 5 years, soil cores (40 cm depth) were collected from the root boxes and divided into 0–20 cm and 20–40 cm fractions. ELEV treatment resulted in significant decreases in both soil nitrate and total soil nitrogen in both the 0–20 cm and 20–40 cm soil fractions, with a 47% decrease in soil nitrate and a 50% decrease in total soil nitrogen occurring in the 0–20 cm fraction. ELEV treatment did not result in a significant change in the amount of soil microbial biomass. However, analysis of indicator phospholipid fatty acids (PLFA) indicated that ELEV treatment did result in significant increases in PLFA indicators for fungi and Gram-negative bacteria in the 0–20 cm fraction. Terminal restriction fragment length polymorphism (T-RFLP) analysis was used to analyze the composition of the soil bacterial communities (using primers targeting the 16SrRNA gene) and the soil fungal communities (using primers targeting the intergenic transcribed spacer region). T-RFLP analysis revealed shifts in both bacterial and fungal community structure, as well as increases in both bacterial and fungal species richness with ELEV treatment. These results indicated that increased atmospheric CO₂ had significant effects on both soil nutrient availability and the community composition of soil microbes associated with aspen roots.     

生物造粒流化床微生物落结构及其动态变化

为了研究生物造粒流化床污水处理反应器颗粒污泥中微生物群落结构及其动态变化,分别从生物造粒流化床10、60、110cm处取颗粒污泥,通过细胞裂解直接提取颗粒污泥细菌基因组DNA。以细菌和古细菌16S rRNA基因通用引物530F/1490R,对活性污泥中提取的细菌基因组DNA进行PCR扩增,长约1kb的PCR扩增产物纯化后经变性梯度凝胶电泳(DGGE)分离,获得微生物群落的DNA特征指纹图谱。结果显示,生物造粒流化床反应器颗粒污泥中的微生物群落非常丰富,在10cm处微生物的种属达到23种,60cm处为21种,110cm处为20种;生物造粒流化床不同高度都有一些各自的特有种属和共有种属,反应器不同高度的微生物群落演替不明显,微生物群落相似性为83.1%,群落结构较为稳定。     

大气CO2浓度升高对土壤微生物的影响

自人类进入工业化时代以来,由于化石燃料的燃烧和森林的大面积破坏,大气中ＣＯ２的浓度已由工业革命以前的２８０μｌ·Ｌ－１增加到现在的３５０μｌ·Ｌ－１,仅从１９５７年至今的几十年间,大气中ＣＯ２的浓度就增加了２０％,预计到下个世纪下半叶,大气中ＣＯ２的...     

Effect of continuous olive mill wastewater applications, in the presence and absence of nitrogen fertilization, on the structure of rhizosphere–soil fungal communities

Olive mill wastewater (OMW) is rich in potentially toxic organics precluding its disposal into water receptors. However, land application of diluted OMW may result in safe disposal and fertilization. In order to investigate the effects of OMW on the structure of soil fungal groups, OMW was applied daily to pepper plants growing in a loamy sand and a sandy loam at two doses for a period of 3 months (total OMW equivalents 900 and 1800 m³ ha⁻¹). Nitrogen (N) fertilization alleviated N scarcity and considerably enhanced plant biomass production; however, when applied in combination with the high OMW dose, it induced plant stress. OMW applications resulted in marked changes in the denaturing gradient gel electrophoresis patterns of soil basidiomycete communities, while concurrent N fertilization reduced these effects. In contrast, the ascomycete communities required N fertilization to respond to OMW addition. Cloning libraries for the basidiomycete communities showed that Cryptococcus yeasts and Ceratobasidium spp. dominated in the samples treated with OMW. In contrast, certain plant pathogenic basidiomycetes such as Thanatephorus cucumeris and Athelia rolfsii were suppressed. The observed changes may be reasonably explained by the capacity of OMW to enrich soils in organic substrates, to induce N immobilization and to directly introduce OMW-derived basidiomycetous yeasts.     

Monitoring of microbial community structure and succession in the biohydrogen production reactor by denaturing gradient gel electrophoresis (DGGE)

To study the structure of microbial communities in the biological hydrogen production reactor and determine the ecological function of hydrogen producing bacteria, anaerobic sludge was obtained from the continuous stirred tank reactor (CSTR) in different periods of time, and the diversity and dynamics of microbial communities were investigated by denaturing gradient gel electrophoresis (DGGE). The results of DGGE demonstrated that an obvious shift of microbial population happened from the beginning of star-up to the 28th day, and the ethanol type fermentation was established. After 28 days the structure of microbial community became stable, and the climax community was formed. Comparative analysis of 16S rDNA sequences from reamplifying and sequencing the prominent bands indicated that the dominant population belonged to low G+C Gram-positive bacteria (Clostridium sp. andEthanologenbacterium sp.), β-proteobacteria (Acidovorax sp.), γ-proteobacteria (Kluyvera sp.), Bacteroides (uncultured bacterium SJA-168), and Spirochaetes (uncultured eubacterium E1-K13), respectively. The hydrogen production rate increased obviously with the increase ofEthanologenbacterium sp.,Clostridium sp. and uncultured Spirochaetes after 21 days, meanwhile the succession of ethanol type fermentation was formed. Throughout the succession the microbial diversity increased however it decreased after 21 days. Some types ofClostridium sp.Acidovorax sp.,Kluyvera sp., and Bacteroides were dominant populations during all periods of time. These special populations were essential for the construction of climax community. Hydrogen production efficiency was dependent on both hydrogen producing bacteria and other populations. It implied that the cometabolism of microbial community played a great role of biohydrogen production in the reactors.     

Monitoring of microbial community structure and succession in the biohydrogen production reactor by denaturing gradient gel electrophoresis (DGGE)

Biohydrogen production has been concerned ex-tremely as a new technology of energy resource pro-duction by many scientists[1—4]. Enhancement of hy-drogen production efficiency and cutting down the operating cost are very important problems, which are the limiting factors for the industrialization of hydro-gen production process. The fermentation hydrogen production technology offers a new method to resolve these difficulties[5—8]. Compared with photosynthetic hydrogen production possesses, f…     

Influence of Doubled CO2 on Plant Growth and Soil Microbial Biomass C and N

Salix babylonica L., Triticum aestivum L., Chenopodium album L. and Amaranthus cruemus L. were grown in the N-deficient soil in open-top chambers blown with ambient or doubled ambient CO2 air, and their growth was measured. Soil samples were collected to assess the influence of doubled CO2 on the soil microbial biomass C (Cmic) and N (Nmic). Results showed that the biomass of shoot and root was increased by doubled CO2 in the four species of plants. Doubled CO2 increased Cmic in S. babylonica and decreased Cmic in T. aestivum and C. album. On the other hand, Nmic in three species except T. aestivum was stimulated by doubled CO2. Doubled CO2 had no significant effect on Cmic in A. cruentus and Nmic in T. aestivum. However, the ratios of Cmic- to -Nmic of all four species were consistently declined under doubled CO2 treatment. It implies that CO2 enrichment may have positive influence on the quality of organic matter of N-low soil in global change.     

CO2浓度升高对斜生栅藻生长和光合作用的影响

升高大气中CO2 浓度可提高斜生栅藻的生物量和光合作用速率 ,对光合效率、暗呼吸速率、光饱和点和光系统Ⅱ的光化学效率 (Fv Fm)没有明显影响 ,但藻细胞光合作用对无机碳的亲和力降低     

Elevated CO2, rhizosphere processes,and soil organic matter decomposition

The rhizosphere is one of the key fine-scale components of C cycles. This study was undertaken to improve understanding of the potential effects of atmospheric CO2 increase on rhizosphere processes. Using C isotope techniques, we found that elevated atmospheric CO2 significantly increased wheat plant growth, dry mass accumulation, rhizosphere respiration, and soluble C concentrations in the rhizosphere. When plants were grown under elevated CO2 concentration, soluble C concentration in the rhizosphere increased by approximately 60%. The degree of elevated CO2 enhancement on rhizosphere respiration was much higher than on root biomass. Averaged between the two nitrogen treatments and compared with the ambient CO2 treatment, wheat rhizosphere respiration rate increased 60% and root biomass only increased 26% under the elevated CO2 treatment. These results indicated that elevated atmospheric CO2 in a wheat-soil system significantly increased substrate input to the rhizosphere due to both increased root growth and increased root activities per unit of roots. Nitrogen treatments changed the effect of elevated CO2 on soil organic matter decomposition. Elevated CO2 increased soil organic matter decomposition (22%) in the nitrogen-added treatment but decreased soil organic matter decomposition (18%) without nitrogen addition. Soil nitrogen status was therefore found to be important in determining the directions of the effect of elevated CO2 on soil organic matter decomposition.