百山祖保护区低山常绿阔叶林的群落特征和α多样性

通过样地调查,对浙江百山祖自然保护区五岭坑低山常绿阔叶林群落的物种组成、群落结构、物种多样性进行研究。结果表明:1)群落内物种丰富,计33科58属124种,种类组成以冬青科、樟科、壳斗科、山茶科、蔷薇科、山矾科等为主,常绿阔叶树种104种3 040株,分别占种数和总株数的83.87%、98.51%,群落的树种组成反映了中亚热带常绿阔叶林植被的典型特征;2)群落幼树量大,自然更新良好。胸径与株数呈指数分布,立木径级分布连续,表明该群落处于成熟阶段。群落的平均胸径与密度之间存在负相关性;3)群落的Simpson指数、Gini均匀度指数、Pielou均匀度指数均较高,说明树种丰富,分布均匀,优势种不明显。     

玉米幼苗对芘污染土壤微生物活性及多样性的影响

通过盆栽土培试验研究了玉米幼苗生长期间对芘污染土壤微生物活性及多样性的影响。结果表明,玉米加快了土壤中芘的降解,提高了芘在土壤中的降解速率。试验期间,根际土中可提取态芘含量显著低于非根际土,根际土微生物生物量碳、微生物熵、多酚氧化酶和脱氢酶活性均高于非根际土,代谢熵低于非根际土。脂肪酸（FAME）分析结果表明,与非根际土相比,芘污染玉米根际土微生物群落结构发生了显著的变化,主要表现在真菌特征脂肪酸以及真菌/细菌的比值显著升高,细菌和GN^-细菌特征脂肪酸显著降低,且这种效应随着培养时间的推移在P〈0.01水平显著。根际土和非根际土中丛枝菌根真菌、GN^＋细菌和放线菌特征脂肪酸差异随着培养时间的延长逐渐加大,45 d时其差异均在P〈0.05水平显著。     

干旱荒漠区封育沙地植被群落特征变化研究

以天然植被围栏封育和人工种植+围栏封育措施下沙地植物群落为对象,以无封护的流动沙地做对照,研究了不同恢复措施对沙地群落物种组成及结构变化的影响.结果表明,(1)封育15 a后,人工种植+围栏封育区侵入物种的丰富度随演替的进展已达12种,其中猪毛菜7.562株/m~2,碟果虫实3.233株/m~2,雾冰藜3.017株/m~2,沙米1.615株/m~2,狗尾草1.112株/m~2.种类组成及生活型结构在向天然植被围栏封育区植物群落靠近,但两者间仍表现出较大差异.(2)在类型组成上,两种封育措施区差异主要表现在优势科及各科种类数量上.(3)在综合多样性特征上,两种措施区草被层的Shannon指数和丰富度指数存在显著差异,而其余各指数两者差异均不显著,但天然植被围栏封育区灌木层的生态优势度指数较高.(4)群落的相似性指数表明,两种封育措施间的植物群落差距较大,且2种封育措施下的植物群落与植被呈零星状分布的无封护措施的流动沙地相比,生态差距均十分显著,这表明封育可明显促进沙地植被的多样性恢复,其中人工种植对沙地植物群落物种多样性恢复的作用是相对缓慢而渐进的.     

Indirect regulation of heterotrophic peat soil respiration by water level via microbial community structure and temperature sensitivity

Northern peatlands contain a considerable share of the terrestrial carbon (C) pool, which climate change will likely affect in the future. The magnitude of this effect, however, remains uncertain, due mainly to difficulties in predicting decomposition rates in the old peat layers. We studied the effects of water level depth (WL) and soil temperature on heterotrophic soil respiration originating from peat decomposition (R_PD) in six drained peatlands using a chamber technique. The microbial community structure was determined through PLFA. Within the studied sites, temperature appeared to be the main driver of R_PD. However, our results indicate that there exist mechanisms related to lower WL conditions that can tone down the effect of temperature on R_PD. These mechanisms were described with a mathematical model that included the optimum WL response of R_PD and the effect of average WL conditions on the temperature sensitivity of R_PD. The following implications were apparent from the model parameterisation: (1) The instantaneous effect of WL on R_PD followed a Gaussian form; the optimum WL for R_PD was 61 cm. The tolerance of R_PD to the WL, however, was rather broad, indicating that the overall effect of WL was relatively weak. (2) The temperature sensitivity of R_PD depended on the average WL of the plot: plots with a high average WL showed higher temperature sensitivity than did those under drier conditions. This variation in temperature sensitivity of R_PD correlated with microbial community structure. Thus, moisture stress in the surface peat layer or, alternatively, the lowered temperature sensitivity of R_PD in low water level conditions via microbial community structure and biomass may restrict R_PD. We conclude that a warmer future climate may raise R_PD in drained peatlands only if the subsequent decrease in the moisture of the surface peat layers is minor and, thus, conditions remain favourable for decomposition.     

Density, structure, and diversity of the cultivable arylsulfatase-producing bacterial community in the rhizosphere of field-grown rape and barley

In this study we investigated the arylsulfatase-producing bacterial community (ARS-BC) in the rhizosphere soils of field-grown rape in comparison with that of barley. For this, the rhizosphere soils from both plant species were sampled four times during plant growth. Soil arylsulfatase (ARS) activity and the density and the structure of the cultivable ARS-BC on M9-Xsulf medium were then determined. ARS activity in rape rhizosphere was greater than in barley rhizosphere and evolved along the phenology in the two rhizosphere soils. In parallel, the average density of ARS-BC in the rape rhizosphere was higher than that in the barley rhizosphere. Moreover, ARS activity is correlated with ARS-BC density both in rape and barley rhizosphere soils. The structure of the ARS-BC in the rape rhizosphere was different from that in the barley rhizosphere. In the rape rhizosphere, the ARS-BC was substantially more structured than in the barley rhizosphere. Among the ARS-BC, Actinobacteria and Pseudomonads were significantly present in the both rhizosphere soils. Actinobacteria predominated in the barley rhizosphere while Pseudomonads were mostly represented under rape. It is possible that the differences in ARS activity observed between rape and barley can be attributed to a different ARS-BC size and/or a different ARS-BC structure under these two plant covers. This impact of rape may be connected to a selective effect of rhizodeposits released by rape roots to the functional bacterial community. Our findings suggest that plant species, via their rhizodeposits, may affect the functional bacterial community and thus influence the dynamic of S in soil.     

Residue chemistry and microbial community structure during decomposition of eucalypt, wheat and vetch residues

Previous studies have shown that residue chemistry and microbial community structure change during decomposition, however little is known about the relationship between C-chemistry and microbial community structure. To address this knowledge gap, we studied C-chemistry and microbial community structure during the decomposition of eucalypt, wheat and vetch residues with and without additional inorganic N. Bags containing ground residues of eucalypt, wheat, and vetch were buried in sand microcosms after inoculation with a diverse microbial community. Respiration was measured over an incubation period of 150 days. At different times during incubation, total C and N of the residues were analysed and residue carbon chemistry was determined by ¹³C-NMR (nuclear magnetic resonance) spectroscopy. Microbial communities were assessed by phospholipid fatty acid (PLFA) analyses.Results indicated that during decomposition, residue C-chemistry and microbial community composition changed over time and differed between residue types. Changes in microbial community structure were associated with changes in residue C-chemistry, mainly the relative content of aryl-C and O-alkyl-C. Addition of N increased cumulative respiration, altered C-chemistry during decomposition, particularly in high C/N residues (wheat and eucalypt), and changed microbial succession leading to an earlier establishment of a stable microbial community structure. N addition to eucalypt and wheat reduced the decomposition of aryl-C compounds.     

Differences in the activity and bacterial community structure of drained grassland and forest peat soils

The microbial activity and bacterial community structure were investigated in two types of peat soil in a temperate marsh. The first, a drained grassland fen soil, has a neutral pH with partially degraded peat in the upper oxic soil horizons (16% soil organic carbon). The second, a bog soil, was sampled in a swampy forest and has a very high soil organic carbon content (45%), a low pH (4.5), and has occasional anoxic conditions in the upper soil horizons due to the high water table level. The microbial activity in the two soils was measured as the basal and substrate-induced respiration (SIR). Unexpectedly, the SIR (μl CO₂ g⁻¹ dry soil) was higher in the bog than in the fen soil, but lower when CO₂ production was expressed per volume of soil. This may be explained by the notable difference in the bulk densities of the two soils. The bacterial communities were assessed by terminal restriction fragment length polymorphism (T-RFLP) profiling of 16S rRNA genes and indicated differences between the two soils. The differences were determined by the soil characteristics rather than the season in which the soil was sampled. The 16S rRNA gene libraries, constructed from the two soils, revealed high proportions of sequences assigned to the Acidobacteria phylum. Each library contained a distinct set of phylogenetic subgroups of this important group of bacteria.     

Diet-related composition of the gut microbiota of Lumbricus rubellus as revealed by a molecular fingerprinting technique and cloning

Interactions between earthworms and microorganisms are essential for the functioning of soil ecosystems as they affect organic matter degradation and nutrient cycling. This is also true for the alpine region, where socio-economic changes lead to the increasing abandonment of pastures, which in turn, causes a considerable shift in the diet of saprotrophic invertebrates and thus impacts food web and decomposition processes. To enhance our understanding of how this diet shift influences earthworms and associated microorganisms, we studied the gut content and cast microbiota of Lumbricus rubellus (Lumbricidae, Oligochaeta), a key macrodecomposer on alpine pastureland in the Central Alps. A feeding experiment with L. rubellus and three different food sources that represent the vegetation shift from an alpine pasture to an abandoned site was set up. Earthworms were collected in the field, transferred to a climate chamber and fed with cow manure, dwarf shrub or grass litter for six weeks. PCR-DGGE (Polymerase chain reaction-denaturing gradient gel electrophoresis) analysis of the DNA extracted from the substrates, the earthworms' gut contents and casts revealed that the gut and cast microbiota was strongly influenced by the food source ingested. Cloning of bacterial 16S rRNA gene fragments demonstrated that the intestinal content was dominated by Proteobacteria, especially from the Gamma-subclass, followed by members of the phyla Bacteroidetes, Actinobacteria and Firmicutes. In contrast, Actinobacteria were detected abundantly in all samples types when a cultivation approach was used. In conclusion, the gut microbiota of L. rubellus was shown to be substantially affected by the food source ingested, suggesting that this essential macrodecomposer is exposed to the diet shift resulting from a land-use change in the alpine area.     

Abiotic conditions and plant cover differentially affect microbial biomass and community composition on dune gradients

Dune systems are characterized by strong gradients of physical stress, with blowing sand and salt spray decreasing with distance from the ocean, and soil nutrients increasing. In this study we ask how soil microbial community composition and biomass change along transects away from the ocean, and whether these changes are regulated by abiotic stress or by resource availability. We collected bulk soil from under three plant species representative of the dune front, back, and flat: Ammophila breviligulata, Rosa rugosa, and Myrica pensylvanica. The biomass and composition of microbial communities were examined using phospholipid fatty acid (PLFA) analysis under patches of dominant vegetation, and in paired bare plots. We found that microbial biomass was strongly correlated with soil C, and thus the presence of vegetation. Community composition, on the other hand, varied with abiotic stresses, especially soil salinity. These variables in turn depended on distance from the shore, and were ameliorated in some cases by vegetation. These findings demonstrate that biomass and community composition are influenced by different environmental variables. Thus, relationships between biomass and composition are unlikely to be readily predicted on the basis of a single resource.     

长江三角洲地区污水污泥与健康安全风险研究Ⅴ.污泥施用对土壤微生物群落功能多样性的影响

利用BIOLOG测试方法对长江三角洲地区施污泥土壤的微生物群落功能多样性进行了初步探讨。研究结果表明,施用污泥后土壤微生物群落代谢剖面、多样性指数、动力学参数均发生了变化,说明微生物对单一碳源底物的利用能力发生了改变。微生物群落功能多样性动力学研究结果发现,供试土壤的微生物群落代谢剖面(AWCD)与培养时间之间呈非线性关系,其变化过程符合微生物种群生长动态模型(S型)。除滩潮土的杭州新鲜消化污泥和杭州风干污泥处理外,其他污泥处理均使土壤微生物群落功能多样性动力学参数K和r值降低,S值增大。土壤微生物群落功能多样性特征的变化可以较好地显示施用污泥后土壤微生物群落对碳源利用能力和模式的差异,反映施用污泥特定生境土壤微生物群落功能多样性的变化。