溪流潜流层大型无脊椎动物生态学研究进展

溪流潜流层是溪流表层水和地下水相互作用的群落交错区,生物多样性丰富,是溪流生态系统的重要组成部分.大型无脊椎动物位于潜流层食物网的顶层,直接影响着潜流层物质和能量动态,是河流健康潜在的指示生物,调节着潜流层的环境净化和生态缓冲功能,对溪流生态系统发挥着至关重要的作用.潜流层大型无脊椎动物类群按生活史划分为偶入动物、非典型潜流层动物和典型潜流层动物.潜流层孔隙大小、孔隙水流速、溶解氧、温度、可利用的食物源、渗透系数和水力停留时间是影响大型无脊椎动物在潜流层分布的主要因素.对于潜流层这样一个特殊的生态界面,针对不同的研究目的应该选择合适的取样和调查方法.潜流层大型无脊椎动物的生活史和生活史对策,在溪流生态系统物质循环和能量流动中作用的定量化分析,基于潜流层大型无脊椎动物的河流健康评价体系,以及潜流层作为“庇护地”对于大型无脊椎动物分布和进化的生态学意义,都值得进一步关注和深入研究.     

The metabolism of organic matter in the hyporheic zone of a mountain stream, and its spatial distribution

Community respiration in hyporheic sediments (HCR) was studied in a characteristic riffle-pool-sequence of a mountain stream. HCR activity at the riffle site strongly exceeded that at the corresponding pool site with a mean ratio of 5.3. The vertical distribution of HCR activity was homogeneous in the pool, while there was a distinct maximum in the uppermost layer in the riffle. Similarly, the spatial distribution of certain fractions of particulate organic matter (POM), and their turnover, was largely determined by stream morphology. Mean annual HCR per unit area of stream bed was estimated as 1.71 g O₂ m⁻² d⁻¹. Hence, HCR contributes significantly to total heterotrophic activity in streams, thus enhancing the relative importance of heterotrophic processes in running waters containing hyporheic zones.     

The bacterivory of interstitial ciliates in association with bacterial biomass and production in the hyporheic zone of a lowland stream

Rates of bacteria ingestion by interstitial ciliates were estimated and compared to bacterial biomass and production. Investigation was carried out in the hyporheic zone of a lowland stream. FISH was applied to quantitatively determine bacteria within the ciliate's food vacuoles. To estimate bacteria ingestion rates using FISH, we had to strike a new path. When numbers of bacteria in the food vacuoles remains constant with time (bacterial digestion and ingestion are at equilibrium), ingestion rate can be estimated based on the digestion time and the average number of bacteria per cell. Ciliate community was predominantly composed of bacterivorous ciliates. FISH-signals deriving from ingested bacteria were detected in Cinetochilum margaritaceum, 'other small scuticociliates', Pleuronema spp., and Vorticella spp. Ingestion rates for these taxa were 78, 150, 86, and 38 bacteria ind(-1) h(-1), respectively. The grazing impacts on bacterial biomass and carbon production were calculated based on these ingestion rates. Ciliate grazing caused a decrease in bacterial biomass of 0.024% day(-1) and in bacterial carbon production of 1.60%. These findings suggest that interstitial ciliate grazing impact on bacteria biomass and production was too low to represent an important link in the carbon flow of the hyporheic zone under study.     

再生水补水对河道底泥细菌群落结构的影响

以北京市永定河麻峪湿地再生水补水口附近河道底泥为研究对象,应用末端限制性片段长度多态性(Terminal Restriction Fragment Length Polymorphism,T-RFLP)技术探究再生水补水口附近底泥细菌群落结构的空间差异特征以及环境因子所产生的影响,并借助典范对应分析(Canonical Correspondence Analysis,CCA)方法分析麻峪湿地底泥细菌群落结构空间差异特征的形成原因。分析结果表明:河道底泥微生物群落对再生水的净化主要发生在距补水口1200m的范围内,随着再生水与上游来水径向混合净化渐变过程,在补水口2000m处河道底泥微生物群落结构与河道再生水补水口上游趋于相似。基于样点聚类结果的群落结构多样性分析表明随着再生水净化过程的实现微生物综合多样性指数呈现下降的趋势,从均匀度指数的变化趋势看,再生水补水口具有最高均匀度指数,补水口下游1200米处由于非优势菌群所占相对丰度最低以及偶见菌群缺失,导致群落结构比较单一、群落多样性和均匀度指数都最低。CCA方面分析结果表明再生水补水口上游细菌群落与因累积效应形成的重金属有密切关系,补水口出口底泥细菌群落则主要受到总磷和总有机碳的影响较大,而再生水补水与上游来水汇水径向渐变过程可能与氨氮净化具密切关系。研究区的主要优势菌种为假单胞菌属、贪食菌属和芽孢杆菌属,是与再生水中有机碳、氮降解具有密切关系的菌属。     

The role of water exchange between a stream channel and its hyporheic zone in nitrogen cycling at the terrestrial-aquatic interface

The subsurface riparian zone was examined as an ecotone with two interfaces. Inland is a terrestrial boundary, where transport of water and dissolved solutes is toward the channel and controlled by watershed hydrology. Streamside is an aquatic boundary, where exchange of surface water and dissolved solutes is bi-directional and flux is strongly influenced by channel hydraulics. Streamside, bi-directional exchange of water was qualitatively defined using biologically conservative tracers in a third order stream. In several experiments, penetration of surface water extended 18 m inland. Travel time of water from the channel to bankside sediments was highly variable. Subsurface chemical gradients were indirectly related to the travel time. Sites with long travel times tended to be low in nitrate and DO (dissolved oxygen) but high in ammonium and DOC (dissolved organic carbon). Sites with short travel times tended to be high in nitrate and DO but low in ammonium and DOC. Ammonium concentration of interstitial water also was influenced by sorption-desorption processes that involved clay minerals in hyporheic sediments. Denitrification potential in subsurface sediments increased with distance from the channel, and was limited by nitrate at inland sites and by DO in the channel sediments. Conversely, nitrification potential decreased with distance from the channel, and was limited by DO at inland sites and by ammonium at channel locations. Advection of water and dissolved oxygen away from the channel resulted in an oxidized subsurface habitat equivalent to that previously defined as the hyporheic zone. The hyporheic zone is viewed as stream habitat because of its high proportion of surface water and the occurrence of channel organisms. Beyond the channel's hydrologic exchange zone, interstitial water is often chemically reduced. Interstitial water that has not previously entered the channel, groundwater, is viewed as a terrestrial component of the riparian ecotone. Thus, surface water habitats may extend under riparian vegetation, and terrestrial groundwater habitats may be found beneath the stream channel.     

Hyporheic zone hydrology and nitrogen dynamics in relation to the streambed topography of a N-rich stream

The influence of riffle-pool units on hyporheic zone hydrology and nitrogen dynamics was investigated in Brougham Creek, a N-rich agricultural stream in Ontario, Canada. Subsurface hydraulic gradients, differences in background stream and groundwater concentrations of conservative ions, and the movement of a bromide tracer indicated the downwelling of stream water at the head of riffles and upwelling in riffle-pool transitions under base flow conditions. Channel water also flowed laterally into the floodplain at the upstream end of riffles and followed a subsurface concentric flow path for distances of up to 20 m before returning to the stream at the transition from riffles to pools. Differences in observed vs predicted concentrations based on background chloride patterns indicated that the hyporheic zone was a sink for nitrate and a source for ammonium. The removal of nitrate in the streambed was confirmed by the loss of nitrate in relation to co-injected bromide in areas of downwelling stream water in two riffles. Average stream water nitrate-N concentrations of 1.0 mg/L were often depleted to <0.005 mg/L near the sediment-water interface. Consequently, an extensive volume of the hyporheic zone in the streambed and floodplain had a large unused potential for nitrate removal. Conceptual models based mainly on studies of streams with low nutrient concentrations have emphasized the extent of surface-subsurface exchanges and water residence times in the hyporheic zone as important controls on stream nutrient retention. In contrast, we suggest that nitrate retention in N-rich streams is influenced more by the size of surface water storage zones which increase the residence time of channel water in contact with the major sites of rapid nitrate depletion adjacent to the sediment-water interface.     

Responses of microbial activity in hyporheic pore water to biogeochemical changes in a drying headwater stream

1. Microbial heterotrophic activity is a major driver of nutrient and organic matter processing in the hyporheic zone of headwater streams. Additionally, the hyporheic zone might provide refuge for microbes when surface flow ceases during drought events.
2. We investigated chemical (organic and inorganic nutrients) and microbiological parameters (bacterial cell concentration, live–dead ratios, and extracellular enzyme activities) of surface and interstitial pore water in a period of progressive surface‐hyporheic disconnection due to summer drying. The special situation of the chosen study reach, where groundwater mixing is impeded by the bedrock forming a natural channel filled with sediment, allowed as to study the transformation of these parameters along hyporheic flow paths.
3. The chemical composition of the hyporheic pore water reflected the connectivity with the surface water, as expressed in the availability of nitrate and oxygen. Conversely, microbiological parameters in all hyporheic locations were different from the surface waters, suggesting that the microbial activity in the water changes rapidly once the water enters the hyporheic zone. This feature was principally manifested in higher live–dead ratios and lower leucine aminopeptidase (an activity related to nitrogen acquisition) in the hyporheic pore waters.
4. Overall, bacterial cell concentration and extracellular enzyme activities increased along hyporheic flow paths, with a congruent decrease in inorganic nutrients and dissolved organic matter quantity and apparent molecular size.
5. Our findings show two important functions of the hyporheic zone during drought: (1) deeper (?50 cm) water‐saturated layers can act as a refuge for microbial activity; and (2) the hyporheic zone shows high rates of carbon and nitrogen turnover when water residence times are longer during drought. These rates might be even enhanced by an increase in living microbes in the remaining moist locations of the hyporheic zone.

     

Biological,chemical and physical characteristics of downwelling and upwelling zones in the hyporheic zone of a north-temperate stream

Along a single stream riffle, there is a typical flow pattern in which surface water enters the hyporheic zone in a downwelling zone at the head of the riffle and hyporheic water returns to the stream surface in an upwelling zone at the tail of the riffle. Distinct patterns of physical and chemical conditions in the hyporheic zone are likely to determine patterns of microbial activity and occurrence of hyporheic fauna. Interstitial water and core samples were taken at three depths in the downwelling and upwelling zones of a single riffle in the Speed River, Southern Ontario, Canada. Physical and chemical characteristics of the hyporheic water, bacterial density, protein content, detritus content and faunal composition of the hyporheic sediment were analysed. The downwelling and upwelling zones differed significantly in temperature, pH, redox potential, dissolved oxygen and nitrate with significant positive correlations occurring among the latter three. There were no differences in bacterial density or detritus content between the two zones nor between depths in either zone, but protein content, considered to be a measure of biofilm biomass, was significantly higher in the downwelling zone. Total density of hyporheic fauna and the number of taxa decreased with increasing depth in both upwelling and downwelling zones, and were positively correlated with surface water characteristics (oxygen, temperature and nitrate), sediment protein content and detritus; however, only a weak correlation was found with zone. The composition of taxa differed between the two zones, and faunal distribution was correlated with dissolved oxygen, detritus, protein content and depth.     

A mixing model analysis of stream solute dynamics and the contribution of a hyporheic zone to ecosystem function*

1. We monitored streamwater and streambed sediment porewaters from White Clay Creek (WCC), SE Pennsylvania, for dissolved organic carbon (DOC), dissolved oxygen (DO) and conductivity to investigate organic matter processing within the hyporheic zone. Dissolved organic carbon and DO concentrations were higher in the streamwater than in the porewaters and, in many cases, concentrations continued to diminish with increasing depth into the streambed. 2. Hydrological exchange data demonstrated that the permeability of the stream bed declines with depth and constrains downwelling, effectively isolating porewaters >30 cm from streamwater. 3. End‐member mixing analysis (EMMA) based on conductivity documented a DOC source and DO sink in the hyporheic zone. We calculated hyporheic streambed DOC fluxes and respiration from the EMMA results and estimates of water flux. Based upon our calculations of biodegradable DOC entering the hyporheic zone, we estimate that DOC supports 39% of the hyporheic zone respiration, with the remaining 61% presumably being supported by entrained particulate organic carbon. Hyporheic respiration averaged 0.38 g C m^?2 d^?1, accounted for 41% of whole ecosystem respiration, and increased baseflow ecosystem efficiency from 46 to 59%. 4. Advective transport of labile organic molecules into the streambed concentrates microbial activity in near‐surface regions of the hyporheic zone. Steep gradients in biogeochemical activity could explain how a shallow and hydrologically constrained hyporheic zone can dramatically influence organic matter processing at the ecosystem scale.     

Bacterial community structure and activity in different Cd-treated forest soils

In this study we compared indicators of Cd bioavailability (water extracts, Lakanen extracts, free ions) and ecotoxicity in forest soils with contrasting physico-chemical characteristics. Soil samples were treated with CdCl(2) solutions (0, 0.1, 1, 10 and 100 mM) and incubated for 30 days. Microbial activity indexes (acid phosphatase, beta-glucosidase, basal respiration) and changes in bacterial community structure using terminal restriction fragment length polymorphism (T-RFLP) fingerprinting were investigated. The Cd concentrations measured ranged from 1% to 37% of the total additions in water extracts, to higher levels in Lakanen extracts. Effects of Cd were observed at bioavailable concentrations exceeding United Nations/European Economic Commission UN/ECE guidelines for total Cd in the soil solution. Basal respiration was the most affected index, while enzymatic activities showed variable responses to the Cd treatments. We also noticed that soils with pH higher than 6.7 and clay content higher than 50% showed inhibition of basal respiration but no marked shift in bacterial community structure. Soils with lower pH (pH <5.8) with less clay content (<50%) showed in addition strong changes in the bacterial community structure. Our results provide evidence for the importance of relating the effects of Cd on the soil communities to soil properties and to bioavailability.     

番茄抗青枯病基因的AFLP分子标记

用番茄高抗青枯病品种“T51A”与高感青枯病品种“T9230”配制杂交组合,接种鉴定其正反交Ｆ₁代及Ｆ₂代分离群体的青枯病发生情况。结果表明,T51A对青枯病的抗性属于细胞质遗传,受1对杂合基因加性控制。用64个EcoRＩ/ＭseＩ引物组合对“T51A”、“T9230”两个亲本及其Ｆ₂代抗病和感病基因池进行AFLP分析,共扩增出约4200条可分辨的带,其中2条为稳定的差异。用“T51A”和“T9230”杂交产生的Ｆ₂代分离群体对2个特异条带与目的基因的遗传连锁性进行分析,发现特异条带AAG/CAT与暂定名为RRS-342的抗青枯病基因紧密连锁,二者之间的遗传距离为6.7 cM。将AAG/CAT片段回收、克隆和测序,成功地将其转化为SCAR标记,可以更加方便地用于对番茄青枯病基因的标记辅助选择。      

螺旋粉虱成虫体内细菌群落多样性的PCR-DGGE 和16S rRNA文库序列分析

为了解螺旋粉虱Aleurodicus dispersus体内细菌多样性和主要优势菌群结构, 用PCR-DGGE和16S rRNA文库对采自于海南省番石榴上螺旋粉虱雌、 雄成虫体内的细菌群落进行了分析。用PCR扩增体内细菌16S rRNA基因, 构建雌、 雄虫克隆文库; 再用限制性片段长度多态性（restriction fragment length polymorphism, RFLP）方法从文库中筛选不同16S rRNA基因图谱, 根据图谱对克隆子进行分型。从螺旋粉虱雌、 雄两个样品中共获得10 种分类操作单元(operational taxonomic unit, OTUs)。以16S rRNA基因为基础构建系统发育树, 系统发育分析表明, 螺旋粉虱雌、 雄成虫体内优势菌群主要为发酵菌属Zymobacter, 杀雄菌属Arsenophonus, 泛菌属Pantoea和假单胞菌属Pseudomonas。Candidatus Portiera aleyrodidarum和Arsenophonus sp.可能为其体内共生菌群, 在所有样品中均可稳定地检测到。这些微生物可能对螺旋粉虱生长发育、 繁殖和性比调控起到重要的协同作用。     

水葫芦根际细菌群落结构多样性分析

【目的】了解水葫芦根际细菌群落结构。【方法】运用末端限制性片段长度多态性(Terminal restriction fragment length polymorphism,T-RFLP)技术分析富营养化水体中水葫芦根际和水葫芦近、远水样的细菌群落特征及多样性,结合克隆文库技术和培养法分析根际的细菌种群类型。【结果】同一时期水葫芦根际细菌多样性(Shannon-Weiner指数H′或Simpson指数D)更高,水葫芦近水样次之,远水样最小。10月份的细菌多样性高于5月份的。通过水葫芦根际细菌的克隆文库可知变形杆菌门(Proteobacteria)是水葫芦根际细菌的主要类群,占总群体的65.1%,包括噬菌弧菌(Bacteriovorax sp.)、Dechloromonas sp.、Leptothrix sp.、红螺菌科(Rhodospirillaceae)、Rhodoferax sp.和红环菌科(Rhodocyclaceae)等。T-RFLP图谱显示159 bp为最大优势菌,247 bp为第二大优势菌,对照克隆文库及培养结果分析247 bp属于γ-Proteobacteria,159 bp为不动杆菌(Acinetobacter sp.)。【结论】水葫芦根际细菌的群落结构丰富,不同时段水葫芦根际细菌的丰度略有变化,主要类群为变形杆菌门。     

水稻土中铁还原菌多样性

微生物介导的异化Fe(III) 还原是非硫厌氧环境中Fe(III) 还原生成Fe(II) 的主要途径,然而相关的铁还原菌还不是很清楚,特别是在水稻土中.本文采用富集培养的方法,以乙酸和氢气作为电子供体,水铁矿和针铁矿作为电子受体,通过末端限制性片段长度多态性（T-RFLP）技术和16S rRNA基因克隆测序相结合的分子生物学方法研究了水稻土中铁还原菌的多样性.结果表明：无论是以乙酸或氢气为电子供体,水铁矿或针铁矿为电子受体,地杆菌（Geobacter）和梭菌（Clostridiales）是富集到的主要微生物群落;乙酸为电子供体时,富集到的主要微生物群落还包括红环菌（Rhodocyclaceae）;因此,除地杆菌外,梭菌和红环菌很可能也是水稻土中重要的铁还原菌.     

Previously unclassified bacteria dominate during thermophilic and mesophilic anaerobic pre-treatment of primary sludge

Thermophilic biological pre-treatment enables enhanced anaerobic digestion for treatment of wastewater sludges but, at present, there is limited understanding of the hydrolytic–acidogenic microbial composition and its contribution to this process. In this study, the process was assessed by comparing the microbiology of thermophilic (50–65 °C) and mesophilic (35 °C) pre-treatment reactors treating primary sludge.     

分离自冬虫夏草可培养真菌的多样性研究

冬虫夏草是生长于青藏高原的一种名贵中药材。天然冬虫夏草及其微环境中生活着多种真菌。作者使用常规分离培养方法对冬虫夏草的真菌区系进行研究。从天然冬虫夏草的子座、菌核和菌膜3个部位共分离到572个真菌菌株,并根据形态特征将大部分菌株鉴定到37个不同的属。这些菌株经SSCP(single-strand conformation polymorphism)分析后,再根据nrDNAITS序列的相似性(以97%为阈值)共区分出92种不同的分类单元(operational taxonomic unit,OTU)。其中,属于子囊菌的菌株数及OTU数均比接合菌和担子菌多。从菌膜分离的菌株数及OTU数都明显多于子座和菌核。分离自子座的优势真菌是产黄青霉Penicillium chrysogenum,而分离自菌核和菌膜的优势真菌均为玫红假裸囊菌Pseudogymnoascus roseus。尚未最终鉴定的部分真菌可能为新的真菌物种。     

三七根腐病株根际土壤真菌群落组成与碳源利用特征研究

根腐病是药用植物三七Panax notoginseng的多发性病害,而土壤真菌群落组成与根腐病的发生存在一定的联系。利用末端限制性酶切片段长度多态性分析和Biolog技术研究了云南文山三七种植园健康和发病三七植株根际土壤真菌群落结构和碳源利用特征,结果表明健康和发病植株的根际土壤真菌多样性和代谢活性差异不显著,但是真菌群落组成存在差异。健康和发病植株根际土壤都以小茎点霉Phoma exigua及镰孢菌属Fusarium真菌为主要种群,而健康植株根际土壤中火丝菌属Pyronema和被孢霉属Mortierella等真菌类群的相对丰度显著高于发病植株根际土壤,尖孢镰孢菌F.ox‐ysporum和刺座霉属的Volutella colletotrichoides的相对丰度则显著低于发病植株。     

有机污染物对水体真细菌群落结构的影响

为了揭示有机污染物对环境真细菌组成和多样性的影响,应用末端限制性片段长度多态性(tRFLP)和16S rDNA文库技术并结合水质分析方法,比较分析了松花江流域内受不同程度有机污染的4个水体及其沉积物中真细菌的群落结构。tRFLP分析表明各水体及底泥均呈现较为复杂的群落结构模式,不同底泥群落形成的末端限制性片段(TRF)图谱具有很高的相似性,但随着污染程度的加强,部分类群明显富集,而且在水样组和泥样组内,群落结构的相似性同水质相似性是一致的,主成分分析(PCA)显示水样和泥样中的真细菌TRF形成不同的群。16SrDNA文库分析表明松花江哈尔滨段底泥中真细菌分布于10个门,Proteobacteria门占优势,达群落总数的21.92%(β-Proteobacteria亚门占10.96%),而有机染污物严重超标的生活污水排污道底泥中的微生物多样性较低,分布于7个门,Proteobacteria门为优势群,占群落的47.37%(α-Proteobacteria亚门占21.05%,δ/ε-Proteobacteria亚门占15.79%)。该研究表明向水体中长期排放高浓度有机物能使系统中微生物群落多样性降低,与污染物降解相关的功能微生物类群明显富集。     

Environmental factors have a strong impact on the composition and diversity of the gut bacterial community of Chinese black honeybees

The Chinese black honeybees is an ecotype of the European honeybee that is formed by the natural hybridization of Apis mellifera mellifera and A. m. carnica. It is distributed in nature reserves in North China and has been an important breeding resource for disease resistance and other desirable traits. Compared to the areas outside of reserves, the nature reserves offer significant biodiversity benefits not only to the Chinese black honey bees but also to the other valuable plants and animals. In recent years there has been growing evidence that environmental factors including food choices play an important role in shaping the composition and activity of gut microbiota, which in turn can impact host health. In the previous studies on Chinse black honeybees, little attention has been paid to the diverse population of microbes in the gut that play a vital role in host health. In order to achieve a better understanding on the role of environmental factors in diversity and composition of gut microbiota of honey bees, in the present study, we analyzed the gut bacterial communities of Chinese black honeybees using terminal restriction fragment length polymorphism (T-RFLP). The results showed that the samples from the national nature reserves that are protected and managed so as to preserve and enrich their natural condition and resources for Chinese black honeybees had higher variety and richness of gut bacteria than that collected from unreserved regions that also harbor populations of Chinese black honeybees. The four terminal restriction fragments (T-RFs), 201, 223, 247 and 320 bp, were identified to be the dominant bacteria of Chinese black honeybees. Of which 247 and 320 bp had greater differences between bee groups sampled in different regions and therefore could be used as genetic markers to separate samples collected from the national nature reserves to samples collected from unreserved regions. The results clearly indicate that national nature reserve protects biological diversity and ecological and evolutionary processes which have had a significant influence on the diversity of gut bacteria of Chinese black honeybees. The ubiquity of gut symbiotic bacteria identified in Chinese black honeybee suggests that environmental factors could play an important role in diversity and composition of gut bacteria and warrant further investigation into the functional significance of these gut bacteria for the honeybee health.