若尔盖高原湿地泥炭沼泽土亚硝酸盐还原酶（nirK）反硝化细菌群落结构分析

若尔盖泥炭湿地是世界少有的低纬度永久冻土湿地,具有高海拔、高紫外辐射、高有机质的特点。该区域N2O的排放量对全球气候变暖有重要影响。对若尔盖高原湿地泥炭沼泽土中的亚硝酸盐还原酶(nir K)反硝化细菌群落结构多样性进行分析,以期揭示该区域N2O释放的微生物调控机制。基于若尔盖高原湿地泥炭沼泽土的理化性质和反硝化活性(PDA),结合限制性酶切片段长度多态性(Restriction fragment length polymorphism,RFLP)技术、克隆文库及分子测序对该生态系统中的nir K反硝化细菌群落结构及多样性进行分析。反硝化活性测定结果显示:阿西地区麦溪地区分区地区,反硝化活性与土壤有机碳、总氮和丰富度呈显著正相关(P0.05)。Shannon-wiener多样性指数以阿西最高、分区最低。3个样品中共测序15条nir K基因代表序列,系统发育表明若尔盖高原湿地优势nir K反硝化菌群为变形门菌群。其中,阿西地区主要为α-变形菌门,麦溪地区主要为β-变形菌门,分区地区无法确定优势种群。冗余分析(Redundancy analysis,RDA)显示:有效钾和有效磷是影响nir K反硝化细菌群落结构的关键环境因子。本论文显示,若尔盖高原湿地存在着明显的反硝化作用,调控这些反硝化作用的nir K反硝化细菌多样性较高,且与土壤有效钾和有效磷密切相关。     

设施菜田不同碳氮管理对反硝化菌结构和功能的影响

【目的】通过6年长期定位试验,比较设施菜田不同碳氮管理下反硝化菌结构和功能的差异。【方法】采用末端限制性片段多态性(T-RFLP)和变性梯度凝胶电泳(DGGE)方法分别分析nir K/nir S和nos Z型反硝化菌群结构特征,利用自动连续在线培养监测体系(Robot系统)测定分析NO/(NO3-+NO2-)和N2O/(N2O+N2)产物比,并通过乙炔抑制法测定反硝化酶活性。【结果】传统施肥处理(CN)显著改变了nir K和nos Z型反硝化菌的结构,增加了NO/(NO3-+NO2-)和N2O/(N2O+N2)产物比。nir S型菌受碳氮管理影响较小。减氮(RN)和添加秸秆处理(RN+S)的nir K和nos Z型反硝化菌结构与CN处理的差异性显著,且会显著降低NO/(NO3-+NO2-)和N2O/(N2O+N2)产物比;与CN和RN相比,RN+S显著增加反硝化酶活性。【结论】设施菜田长期传统施肥措施改变了反硝化菌的结构和功能,增加土壤自身的NO产生能力并减弱了N2O还原N2的能力。减氮和添加秸秆管理能形成自身的反硝化菌群结构,并降低NO和N2O排放风险;秸秆的添加会促进反硝化潜在速率,降低菜田NO3-淋洗风险。     

珠江口自源有机颗粒物沉降对沉积物反硝化过程的影响

【摘要】由微生物主导、依赖有机物供给的反硝化过程是珠江口氮移除的主要途径之一, 可有效地将生态系统中的固定氮转化为N2 或N2O 释放到大气中。珠江口水体存在大量富含多糖和蛋白的生源有机颗粒物, 该类有机颗粒物沉降到底层, 影响反硝化过程的机制迄今尚不明确。通过培养实验, 分析了富含蛋白的中肋骨条藻(Skeletonema costatum)和多糖颗粒对珠江口沉积物反硝化速率和反硝化功能基因的影响。研究结果表明: 这两类有机物的添加能够刺激微生物矿化过程的发生, 16S rRNA丰度和反硝化过程有关的基因nosZ 与 nir S丰度显著提高, 矿化发生同时能够有效的为沉积物脱氮过程提供碳源与能量, 提高了反硝化速率。就有机质可利用性而言, 富含蛋白的中肋骨条藻和多糖的生物利用性存在差异, 在添加中肋骨条藻组中, 因有机质中蛋白含量高于多糖组, 有机质降解速率高于多糖组, 其可利用性高于多糖类有机质, 并且蛋白类物质矿化过程中产生的NH4+也比多糖组高, NH4+通过硝化作用转换为硝酸盐, 继续为反硝化过程提供硝酸盐, 因此添加中肋骨条藻组反硝化速率显著高于添加多糖组。总之水体中生源有机颗粒沉降促进了沉积物-水界面中氮移除过程, 并且这种促进作用与生源有机颗粒的可利用性呈正相关。     

固氮施氏假单胞菌亚硝酸盐还原酶基因nirS转录特性及功能鉴定

【目的】研究固氮施氏假单胞菌(Pseudomonas stutzeri)A1501亚硝酸盐还原酶结构基因nir S的转录调控机制及其在反硝化过程中的功能。【方法】构建nir S-lac Z融合载体,利用三亲本结合法将其导入野生型A1501,通过β-半乳糖苷酶活性的测定,分析不同供氧状况、不同浓度的硝酸盐、亚硝酸盐对nir S基因表达的影响;同时将该载体导入rpo N突变株中,研究氮代谢调控因子Rpo N对nir S基因转录影响。通过同源重组方法构建nir S突变株,通过生化表型测定明确nir S在反硝化过程中的功能。【结果】启动子活性测定表明,nir S基因厌氧条件下高水平表达,是好氧条件下表达水平的4倍;nir S的表达受硝酸盐诱导,但不受亚硝酸盐的诱导;Rpo N突变株中,nir S的表达活性为野生型的1/4,nir S启动子未发现Rpo N的保守结合位点,表明nir S的表达受Rpo N间接调控。表型测定显示以硝酸盐为电子受体时Δnir S的反硝化能力降低了约20%;以亚硝酸盐为电子受体时Δnir S仅有微弱的反硝化能力,并且nir S的突变使得菌体在反硝化条件下利用亚硝酸盐的能力显著减弱。nir S突变提高了菌体在亚硝酸为电子受体的反硝化条件下的固氮酶活。【结论】A1501中nir S基因的转录受外界氧及硝酸盐的影响,同时受氮代谢Sigma因子Rpo N的调控。nir S在A1501菌反硝化过程中起关键作用,参与了亚硝酸盐的转化。     

好氧反硝化细菌及其在微污染水源水修复中的应用研究进展

相比于氨氮,天然水体中的硝酸盐氮通常更稳定,导致更难将其从水中去除。由于好氧反硝化可以在有氧环境下进行反硝化作用去除硝酸盐氮,该过程对含有较高溶解氧的天然水体中硝酸盐氮处理有重要作用。本文综述了好氧反硝化菌的分离纯化现状、微生物代谢机制和环境影响因子,并介绍了功能菌群在微污染饮用水源水生物修复的应用研究进展。与一般的厌氧反硝化类似,好氧反硝化菌的种属分布较广,常见的如假单胞菌属(Pseudomoas)、产碱杆菌属(Alcaligenes)、副球菌属(Paracoccus)和芽孢杆菌属(Bacillus)等所属部分微生物均有好氧反硝化能力。大部分好氧反硝化菌株在最佳生长条件下(25–37℃、溶解氧浓度为3–5mg/L、pH为7–8、碳氮比为5–10)具有高效的脱氮效率。但目前好氧反硝化作用在微污染饮用水源水的生物修复方面的应用仍有着脱氮性能不稳定、菌剂流失等不足。此外,目前较少相关中试及实际工程应用的研究,需要进一步的深入探究。     

不同恢复阶段热带森林土壤nirS型反硝化微生物群落结构及多样性特征

探明热带森林土壤反硝化微生物群落结构及多样性,对于理解反硝化引起的N₂O排放及缓解全球变暖具有重要意义。本研究以西双版纳3个不同恢复阶段热带森林类型[即白背桐（Mallotus paniculatus,MP）、崖豆藤（Millttia leptobotrya,ML）群落、群落及高檐蒲桃（Syzygium oblatum,SO）群落]为研究对象,揭示土壤nirS型反硝化微生物群落组成及多样性的干湿季变化,分析热带森林恢复过程中土壤理化环境变化对nirS型反硝化细菌群落的影响。结果表明,变形菌门（Proteobacteria）和酸杆菌门（Acidobacteria）相对丰度表现为恢复前期高于恢复后期,而脱氯单胞菌属（Dechloromonas）、嗜盐单胞菌属（Halomonas）和罗思河小杆菌属（Rhodanobacter）表现为恢复后期高于恢复前期;绿弯菌门（Chloroflexi）和放线菌门（Actinobacteria）均随恢复年限增加而增加,而贪铜菌属（Cupriavidus）和假单胞菌属（Pseudomonas）的相对丰度表现为随恢复年限增加而降低。9月份各样地新检测出的属数量表现为：SO （19种） > MP （13种） > ML （7种）。土壤nirS型反硝化微生物群落的Shannon多样性指数表现为：高檐蒲桃群落 > 崖豆藤群落 > 白背桐群落,且9月（湿季） > 3月（干季）。相关分析表明,热带森林恢复引起土壤N库（全氮、NH₄⁺、NO₃^-）、C有效性（微生物量碳、易氧化碳）及微气候（土壤含水率与温度）的改变,能够显著影响nirS型反硝化细菌群落的结构及多样性。主成分分析结果表明,土壤硝态氮、微生物量碳、全氮及易氧化碳是调控不同恢复阶段热带森林土壤nirS型反硝化细菌群落结构及多样性变化的主控因子,其次为土壤水分、温度、水解氮、pH、铵态氮、有机碳、容重及C/N。     

好氧甲烷氧化耦合反硝化极限脱氮系统的效能及应用

【目的】探究甲烷浓度、温度和氮浓度对好氧甲烷氧化耦合反硝化(AME-D)极限脱氮系统的影响,分析该系统微生物群落结构,并对贵阳某污水处理厂尾水进行应用研究。【方法】采用阶段性实验研究甲烷浓度、温度和氮浓度对系统脱氮效能的影响,通过16SrRNA基因测序技术分析系统中微生物群落结构,利用共焦显微拉曼光谱仪分析实际废水水质变化特征。【结果】甲烷进气比为3%、温度为30°C、氮浓度为20 mg/L时脱氮效果最好,系统的总氮、氨氮和硝酸盐氮平均去除率分别为93.66%、96.13%和92.25%;系统中的主要甲烷氧化菌分别为Methylosarcina(1.84%)、Methylovulum(0.01%)和Crenothrix(0.14%),以及兼性甲烷氧化菌属Methylocystis(1.9%),主要的亚硝化菌为Nitrosomonas(0.008%),硝化菌为Nitrospira (0.42%),反硝化菌为Hyphomicrobium (1.19%)和Pseudomonas (0.61%);采用该系统处理贵阳某污水处理厂尾水时,出水总氮平均浓度达到0.96mg/L,能达到极限脱氮的目的,拉曼光谱分析显示系统对硝酸盐氮和亚硝酸盐氮有较高的去除,甲烷被氧化形成的中间产物可能为醇类或醛类物质,为反硝化菌提供所需碳源。【结论】AME-D极限脱氮由多种微生物协同实现,其功能微生物为甲烷氧化菌、亚硝化菌、硝化菌和反硝化菌,应用研究显示该系统在城镇污水处理系统中具有较大的应用潜力。     

好氧反硝化菌脱氮特性研究进展

好氧反硝化菌的发现,是对传统反硝化理论的丰富与突破. 由于其在脱氮方面的独特优势,已成为目前废水生物脱氮领域研究的热点. 好氧反硝化菌能够在有氧条件下,利用有机碳源生长的同时将含氮化合物反硝化生成N2等气态氮化物,多数还能同时进行异养硝化作用,将铵态氮直接转化为含氮气体. 本文从电子理论、反硝化酶系等方面对目前已分离出的一些好氧反硝化菌的脱氮特性及其脱氮机理进行探讨,分析了溶解氧、碳源类型及C/N等环境条件对其脱氮作用的影响,介绍了好氧反硝化菌的筛选方法及应用现状,对其应用前景和发展方向进行了展望.     

湖泊氮素氧化及脱氮过程研究进展

自然界中氮的生物地球化学循环主要由微生物驱动,由固氮作用、硝化作用、反硝化作用和氨化作用来完成。过去数十年间,随着异养硝化、厌氧氨氧化和古菌氨氧化作用的发现,人们对环境中氮素循环认识逐步深入,提出了多种脱氮途径新假说。对湖泊生态系统中氮素的输入、输出及其在水体、沉积物和水土界面的迁移转化过程进行了概括,对湖泊生态系统中反硝化和厌氧氨氧化脱氮机理及脱氮效率的最新研究进展进行了探讨,并对以后的氮素循环研究进行了展望。     

好氧反硝化菌的研究进展

综述了好氧反硝化菌的种类和特性、好氧反硝化菌的反硝化作用机制和影响因素.好氧反硝化菌主要包括假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)、副球菌属(Para-coccus)和芽孢杆菌属(Bacillus)等,属好氧或兼性好氧异养微生物.好氧反硝化菌能在好氧条件下进行反硝化,其主要产物是N2O,并可将铵态氮直接转化成气态产物.催化好氧反硝化菌反硝化作用的硝酸盐还原酶是周质酶而不是膜结合酶.溶解氧和C/N往往是影响好氧反硝化菌反硝化作用的主要因素.介绍了间歇曝气法、选择性培养基法等好氧反硝化菌的主要分离筛选方法.概述了好氧反硝化菌在水产养殖、废水生物处理、降解有机污染物以及对土壤氮素损失的影响方面的研究进展.     

Diversity,abundance, and distribution of NO‐forming nitrite reductase–encoding genes in deep‐sea subsurface sediments of the South China Sea

In marine ecosystems, both nitrite‐reducing bacteria and anaerobic ammonium‐oxidizing (anammox) bacteria, containing different types of NO‐forming nitrite reductase–encoding genes, contribute to the nitrogen cycle. The objectives of study were to reveal the diversity, abundance, and distribution of NO‐forming nitrite reductase–encoding genes in deep‐sea subsurface environments. Results showed that higher diversity and abundance of nirS gene than nirK and Scalindua‐nirS genes were evident in the sediments of the South China Sea (SCS), indicating bacteria containing nirS gene dominated the NO‐forming nitrite‐reducing microbial community in this ecosystem. Similar diversity and abundance distribution patterns of both nirS and Scalindua‐nirS genes were detected in this study sites, but different from nirK gene. Further statistical analyses also showed both nirS and Scalindua‐nirS genes respond similarly to environmental factors, but differed from nirK gene. These results suggest that bacteria containing nirS and Scalindua‐nirS genes share similar niche in deep‐sea subsurface sediments of the SCS, but differed from those containing nirK gene, indicating that community structures of nitrite‐reducing bacteria are segregated by the functional modules (NirS vs. NirK) rather than the competing processes (anammox vs. classical denitrification).     

牛场肥水灌溉对土壤nirK、nirS型反硝化微生物群落结构的影响

以徐水县梁家营长期定位施肥试验田为研究对象,利用末端限制性片段长度多态性(T-RFLP)分析和克隆文库构建,研究了5种施肥处理(清水灌溉CK、无机肥灌溉CF、牛场肥水不同浓度、不同次数灌溉T4、T5和T11)下土壤中nirK、nirS型反硝化细菌群落多样性及其群落结构的演变。结果表明,不同施肥处理下nirK、nirS型反硝化细菌群落多样性无显著差异,但群落结构却有明显变化:nirK型反硝化细菌群落结构既受施肥种类又受施肥量影响,优势种群尤其对施肥种类和施肥量响应显著;nirS型反硝化细菌则主要受施肥种类影响,施肥量影响微弱。牛场肥水处理和无机肥处理分别促进和抑制不同的nirS型反硝化细菌,群落主成分受无机肥促进、牛场肥水抑制。系统发育分析结果表明,土壤中nirK型反硝化细菌主要与假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)和根瘤菌属(Rhizobium)的反硝化细菌具有较近的亲缘关系;nirS型反硝化细菌主要与劳尔氏菌(Ralstonia)和红长命菌属(Rubrivivax)有较近的亲缘关系。试验土壤中反硝化微生物多与目前已报道的好氧反硝化细菌亲缘关系较近,这可能与微生物分析取自表层土有关。     

Experimental nitrogen and phosphorus enrichment stimulates multiple trophic levels of algal and detrital-based food webs: a global meta-analysis from streams and rivers

Anthropogenic increases in nitrogen (N) and phosphorus (P) concentrations can strongly influence the structure and function of ecosystems. Even though lotic ecosystems receive cumulative inputs of nutrients applied to and deposited on land, no comprehensive assessment has quantified nutrient-enrichment effects within streams and rivers. We conducted a meta-analysis of published studies that experimentally increased concentrations of N and/or P in streams and rivers to examine how enrichment alters ecosystem structure (state: primary producer and consumer biomass and abundance) and function (rate: primary production, leaf breakdown rates, metabolism) at multiple trophic levels (primary producer, microbial heterotroph, primary and secondary consumers, and integrated ecosystem). Our synthesis included 184 studies, 885 experiments, and 3497 biotic responses to nutrient enrichment. We documented widespread increases in organismal biomass and abundance (mean response = +48%) and rates of ecosystem processes (+54%) to enrichment across multiple trophic levels, with no large differences in responses among trophic levels or between autotrophic or heterotrophic food-web pathways. Responses to nutrient enrichment varied with the nutrient added (N, P, or both) depending on rate versus state variable and experiment type, and were greater in flume and whole-stream experiments than in experiments using nutrient-diffusing substrata. Generally, nutrient-enrichment effects also increased with water temperature and light, and decreased under elevated ambient concentrations of inorganic N and/or P. Overall, increased concentrations of N and/or P altered multiple food-web pathways and trophic levels in lotic ecosystems. Our results indicate that preservation or restoration of biodiversity and ecosystem functions of streams and rivers requires management of nutrient inputs and consideration of multiple trophic pathways.     

不同季节艾比湖湿地盐角草根际nirS-型与nirK-型反硝化细菌群落组成分析

旨在了解艾比湖湿地盐生植物盐角草根际与非根际中不同类型反硝化细菌的分布及其随季节变化情况,为温带干旱地区荒漠盐化生态系统的代表-艾比湖湿地在生态植被恢复过程中,由微生物推动的土壤氮素循环过程提供数据支撑。采集了艾比湖湿地夏、秋、春三个季节的盐角草根际和非根际土壤样本,通过高通量测序技术,比较分析了nirS-型和nirK-型两种类型的反硝化细菌的多样性和群落结构特点;利用RDA (redundancy analysis)探究了土壤理化因素对反硝化细菌多样性及群落结构的影响。艾比湖湿地盐角草根际与非根际中,nirS-型和nirK-型反硝化细菌多样性最高的为秋季根际土壤样本;各土壤样本中的反硝化细菌多样性均呈现根际>非根际。盐角草各土壤样本中的nirS-型反硝化细菌在门分类水平上隶属于变形菌门(Proteobacteria),厚壁菌门(Firmicutes)和放线菌门(Actinobacteria),而nirK-型反硝化细菌在门水平上分类仅包括了Proteobacteria和Firmicutes。Proteobacteria在各土壤样本中的占比均较高;其中Gamma-Proteobacteria的盐单胞菌属(Halomonas)和假单胞菌属(Pseudomonas)是各土壤样本所共有的nirS-型反硝化菌的优势菌属,但它们在每个土壤样本中的相对丰度各有差异。Alpha-Proteobacteria的根瘤菌属(Rhizobium)是盐角草各土壤样本中较为广泛存在的nirK-型反硝化细菌。艾比湖湿地盐角草各土壤样本中的反硝化细菌群落结构存在着一定的差异。RDA结果显示含水量、有机质、全氮和铵态氮等对各土壤样本中的nirS-型反硝化细菌的多样性影响较大,含水量、有机质、全氮、碱解氮等是nirK-型反硝化细菌多样性的主要影响因素。土壤电导率、全磷、全钾、全氮和碱解氮协同影响nirS-型反硝化细菌的群落结构,有机质、速效钾、速效磷、pH和硝态氮是nirK-型反硝化细菌群落结构组成的主要影响因素。艾比湖湿地反硝化细菌呈现季节性变化,nirS-型和nirK-型反硝化细菌以不同的主要菌属,共同推进湿地反硝化作用。而对于湿地生态系统的保护,则需要进行长期而广泛的土壤状态评估和土壤反硝化微生物菌群的动态监测。     

Macroinvertebrate diversity in headwater streams: a review

1. Headwater streams are ubiquitous in the landscape and are important sources of water, sediments and biota for downstream reaches. They are critical sites for organic matter processing and nutrient cycling, and may be vital for maintaining the 'health' of whole river networks.
2. Macroinvertebrates are an important component of biodiversity in stream ecosystems and studies of macroinvertebrate diversity in headwater streams have mostly viewed stream systems as linear reaches rather than as networks, although the latter may be more appropriate to the study of diversity patterns in headwater systems.
3. Studies of macroinvertebrate diversity in headwater streams from around the world illustrated that taxonomic richness is highly variable among continents and regions, and studies addressing longitudinal changes in taxonomic richness of macroinvertebrates generally found highest richness in mid-order streams.
4. When stream systems are viewed as networks at the landscape-scale, α-diversity may be low in individual headwater streams but high β-diversity among headwater streams within catchments and among catchments may generate high γ-diversity.
5. Differing ability and opportunity for dispersal of macroinvertebrates, great physical habitat heterogeneity in headwater streams, and a wide range in local environmental conditions may all contribute to high β-diversity among headwater streams both within and among catchments.
6. Moving beyond linear conceptual models of stream ecosystems to consider the role that spatial structure of river networks might play in determining diversity patterns at the landscape scale is a promising avenue for future research.     

长江口外低氧区及其邻近海域表层沉积物反硝化微生物多样性和分布特征

[目的]微生物参与的反硝化是河口区氮损失的主要途径.[方法]本研究采用Illumina MiSeq测序方法,研究了长江口外低氧区及其邻近海域表层沉积物中nirS型和nirK型反硝化微生物群落的多样性和分布特征.[结果]样品共检测到346个nirS Operational Taxonomic Units和267个nirK...     

Urban Stormwater Runoff Drives Denitrifying Community Composition Through Changes in Sediment Texture and Carbon Content

The export of nitrogen from urban catchments is a global problem, and denitrifying bacteria in stream ecosystems are critical for reducing in-stream N. However, the environmental factors that control the composition of denitrifying communities in streams are not well understood. We determined whether denitrifying community composition in sediments of nine streams on the eastern fringe of Melbourne, Australia was correlated with two measures of catchment urban impact: effective imperviousness (EI, the proportion of a catchment covered by impervious surfaces with direct connection to streams) or septic tank density (which affects stream water chemistry, particularly stream N concentrations). Denitrifying community structure was examined by comparing terminal restriction fragment length polymorphisms of nosZ genes in the sediments, as the nosZ gene codes for nitrous oxide reductase, the last step in the denitrification pathway. We also determined the chemical and physical characteristics of the streams that were best correlated with denitrifying community composition. EI was strongly correlated with community composition and sediment physical and chemical properties, while septic tank density was not. Sites with high EI were sandier, with less fine sediment and lower organic carbon content, higher sediment cations (calcium, sodium and magnesium) and water filterable reactive phosphorus concentrations. These were also the best small-scale environmental variables that explained denitrifying community composition. Among our study streams, which differed in the degree of urban stormwater impact, sediment grain size and carbon content are the most likely drivers of change in community composition. Denitrifying community composition is another in a long list of ecological indicators that suggest the profound degradation of streams is caused by urban stormwater runoff. While the relationships between denitrifying community composition and denitrification rates are yet to be unequivocally established, landscape-scale indices of environmental impact such as EI may prove to be useful indicators of change in microbial communities.     

Dynamic modeling of nitrogen losses in river networks unravels the coupled effects of hydrological and biogeochemical processes

The importance of lotic systems as sinks for nitrogen inputs is well recognized. A fraction of nitrogen in streamflow is removed to the atmosphere via denitrification with the remainder exported in streamflow as nitrogen loads. At the watershed scale, there is a keen interest in understanding the factors that control the fate of nitrogen throughout the stream channel network, with particular attention to the processes that deliver large nitrogen loads to sensitive coastal ecosystems. We use a dynamic stream transport model to assess biogeochemical (nitrate loadings, concentration, temperature) and hydrological (discharge, depth, velocity) effects on reach-scale denitrification and nitrate removal in the river networks of two watersheds having widely differing levels of nitrate enrichment but nearly identical discharges. Stream denitrification is estimated by regression as a nonlinear function of nitrate concentration, streamflow, and temperature, using more than 300 published measurements from a variety of US streams. These relations are used in the stream transport model to characterize nitrate dynamics related to denitrification at a monthly time scale in the stream reaches of the two watersheds. Results indicate that the nitrate removal efficiency of streams, as measured by the percentage of the stream nitrate flux removed via denitrification per unit length of channel, is appreciably reduced during months with high discharge and nitrate flux and increases during months of low-discharge and flux. Biogeochemical factors, including land use, nitrate inputs, and stream concentrations, are a major control on reach-scale denitrification, evidenced by the disproportionately lower nitrate removal efficiency in streams of the highly nitrate-enriched watershed as compared with that in similarly sized streams in the less nitrate-enriched watershed. Sensitivity analyses reveal that these important biogeochemical factors and physical hydrological factors contribute nearly equally to seasonal and stream-size related variations in the percentage of the stream nitrate flux removed in each watershed.     

Manipulation of the Dissolved Organic Carbon Pool in an Agricultural Stream: Responses in Microbial Community Structure, Denitrification, and Assimilatory Nitrogen Uptake

Carbon (C) and nitrogen (N) are strongly coupled across ecosystems due to stoichiometrically balanced assimilatory demand as well as dissimilatory processes such as denitrification. Microorganisms mediate these biogeochemical cycles, but how microbial communities respond to environmental changes, such as dissolved organic carbon (DOC) availability, and how those responses impact coupled biogeochemical cycles in streams is not clear. We enriched a stream in central Indiana with labile DOC for 5?days to investigate coupled C and N cycling. Before, and on day 5 of the enrichment, we examined assimilatory uptake and denitrification using whole-stream ¹⁵N-nitrate tracer additions and short-term nitrate releases. Concurrently, we measured bacterial and denitrifier abundance and community structure. We predicted N assimilation and denitrification would be stimulated by the addition of labile C and would be mediated by increases in bacterial activity, abundance, and a shift in community structure. In response to the twofold increase in DOC concentrations in the water column, N assimilation increased throughout the enrichment. Community respiration doubled during the enrichment and was associated with a change in bacterial community structure (based on terminal restriction fragment length polymorphisms of the 16S rRNA gene). In contrast, there was little response in denitrification or denitrifier community structure, likely because labile C was assimilated by heterotrophic communities on the stream bed prior to reaching denitrifiers within the sediments. Our results suggest that coupling between C and N in streams involves potentially complex interactions with sediment texture and organic matter, microbial community structure, and possibly indirect biogeochemical pathways.     

Benthic macroinvertebrate assemblages of coastal and continental streams and large rivers of southwestern British Columbia, Canada

In southwestern British Columbia (BC, Canada) and within a relatively small geographic area, lotic environments range from streams in coastal rainforests, to streams in arid continental grasslands, to very large rivers. Little is known about the invertebrate communities in large rivers in general, or in the streams of continental BC. The purpose of this study was to determine whether the benthic invertebrate community structure changes spatially between small coastal and small interior streams; between small streams versus large rivers; and whether changes in the benthic community are related to the environmental conditions. Kicknet samples and environmental data were collected from three coastal streams, three continental streams and two large rivers (discharge of 781 and 3620 m³/s, respectively). The large river sites had low invertebrate abundance, species richness and diversity, relative to the small streams. The coastal streams had the highest species richness and the continental streams had the highest invertebrate abundance. A number of taxa were specific to each class of stream. Invertebrate abundance decreased with river size, and increased with elevation, pH, conductivity, alkalinity, NO₂NO₃-N, total Kejldahl nitrogen and percent carbon in suspended solids.