以pH为扰动因子探究电化学厌氧消化产甲烷代谢通量与微生物的关系

【背景】电化学厌氧消化(electrochemical anaerobic digestion,EAD)系统的代谢途径由具备不同功能的微生物所主导,其代谢通量与功能微生物丰度、活性及群落结构相关。【目的】探究EAD产甲烷代谢通量与微生物的关系。【方法】采用代谢通量分析(metabolic flux analysis,MFA)方法,以pH为扰动因子得到微生物群落与产甲烷通量的响应关系。【结果】pH 7.5扰动时产甲烷通量最大为0.398 4±0.029 3,较对照组(pH 6.9)的0.297 4±0.012 7和扰动组(pH 6.3)的0.136 5±0.012 0分别提高了25%和65%。另外,平均有33.8%±3.1%的氢气(通量)用于还原二氧化碳产甲烷和乙酸,平均有21.0%±2.6%的乙酸(通量)转化为甲烷。此外,产甲烷通量与Mariniphaga、Methanosaeta和Desulfomicrobium的丰度呈正相关,与Sedimentibacter的丰度呈负相关且影响显著。【结论】在EAD产甲烷体系中产甲烷菌和产酸菌共存时,pH值略大于7.0的环境有利于甲烷的生成,改变E...     

典型煤层水微生物产甲烷潜力及其群落结构研究

内蒙古自治区二连盆地、海拉尔盆地是我国重要的煤层气产区,其中生物成因煤层气是煤层气的重要来源,但复杂物质转化产甲烷相关微生物群落结构及功能尚不清楚。【目的】研究煤层水中的微生物代谢挥发性脂肪酸产甲烷的生理特征及群落特征。【方法】以内蒙古自治区二连盆地和海拉尔盆地的四口煤层气井水作为接种物,分别添加乙酸钠、丙酸钠和丁酸钠厌氧培养;定期监测挥发性脂肪酸降解过程中甲烷和底物的变化趋势,应用高通量测序技术,分析原始煤层气井水及稳定期产甲烷菌液的微生物群落结构。【结果】除海拉尔盆地H303煤层气井微生物不能代谢丙酸外,其他样品均具备代谢乙酸、丙酸和丁酸产生甲烷的能力,其生理生态参数存在显著差异,产甲烷延滞期依次是乙酸丁酸丙酸;最大比产甲烷速率和底物转化效率依次是丙酸乙酸丁酸。富集培养后,古菌群落结构与煤层气井水的来源显著相关,二连盆地优势古菌为氢营养型产甲烷古菌Methanocalculus (相对丰度13.5%–63.4%)和复合营养型产甲烷古菌Methanosarcina (7.9%–51.3%),海拉尔盆地的优势古菌为氢营养型产甲烷古菌Methanobacterium(24.3%–57.4%)和复合营养型产甲烷古菌Methanosarcina(29.6%–66.5%);细菌群落则与底物类型显著相关,硫酸盐还原菌Desulfovibrio(12.0%–41.0%)、互营丙酸氧化菌Syntrophobacter(39.6%–75.5%)和互营丁酸菌Syntrophomonas(8.5%–21.9%)分别在乙酸钠、丙酸钠和丁酸钠处理组显著富集。【结论】煤层气井水微生物可降解挥发性脂肪酸(乙酸、丙酸和丁酸)并具有产甲烷潜力;乙酸可能被古菌直接代谢产甲烷,而丙酸和丁酸通过互营细菌和产甲烷古菌代谢产甲烷。Desulfovibrio、Syntrophobacter和Syntrophomonas分别在乙酸、丙酸和丁酸代谢过程中发挥了重要作用。这些结果为煤层气生物强化开采提供了一定的微生物资源基础。     

不同生长期核桃根际微生物群落特征

植物根系能够在复杂的土壤环境中招募对自身有益的微生物构建根际微生物群落。为了探明不同生长期核桃根际微生物群落的特征,本研究采集了核桃萌芽期、开花期和结果期的根际和非根际土壤样品,进行了高通量测序、差异物种分析、功能分析和微生物生态网络相关性分析。结果表明：核桃根际在不同生长期的优势种群存在一定程度的差异,萌芽期相对丰度显著增加的菌属有芽孢杆菌属(Bacillus)和unclassified Fungi,开花期有unclassified Chloroplast、枝孢属(Cladosporium)、链格孢属(Alternaria)和无茎真菌属(Acaulium),结果期有unclassified Micrococcaceae、假单胞菌属(Pseudomonas)、链霉菌属(Streptomyces)、赤霉菌属(Gibberella)和被孢霉属(Mortierella);其中,芽孢杆菌属(3.0%)、unclassified Chloroplast(4.5%)、假单胞菌属(17.9%)分别为萌芽期、开花期和结果期主要有益菌属。同时,不同生长期的根际土壤细菌和真菌群落结构存在显著差异(P<...     

不同抑制剂对乙酸降解产甲烷及产甲烷菌群结构的影响

摘要:【目的】研究不同温度条件下的石油烃降解产甲烷菌系中是否存在乙酸互营氧化产甲烷代谢途径。【方法】以3个不同温度条件的正十六烷烃降解产甲烷菌系Y15(15℃)、M82(35℃)和SK(55℃)作为接种物,通过乙酸喂养实验、并添加乙酸营养型产甲烷古菌的选择性抑制剂NH4Cl和CH3F,结合末端限制性片段长度多态性(terminal restriction fragment length polymorphism,T-RFLP)和克隆文库技术,分析乙酸产甲烷潜力及产甲烷古菌群落的演替趋势,推测产甲烷代谢途径的变化趋势。【结果】无论是否添加NH4Cl和CH3 F,这3个菌系都可以利用乙酸生长并产生甲烷,但是添加NH4Cl和CH3 F后产甲烷延滞期增加,最大比甲烷增长速率降低;只添加乙酸后,3个不同温度的菌系的古菌群落主要由乙酸营养型产甲烷古菌甲烷鬃毛菌属(Methanosaeta)组成,其丰度分别为92.8±1.4%、97.3±2.4%和82.8±9.0%;当添加选择性抑制剂NH4Cl,3 个菌系中的Methanosaeta的丰度分别变为98.5±0.7%、87.4±4.8%和6.1±8.6%,中温菌系M82中氢营养型产甲烷古菌甲烷袋装菌属(Methanoculleus)的相对丰度增加到12. 6±4.0%,高温菌系SK中另一类氢营养型产甲烷古菌甲烷热杆菌属(Methanothermobacter)增至84.3±1.5%;当添加选择性抑制剂CH3 F,Methanosaeta丰度分别降至77.1 ± 14.5%,86.4±6.1%和35.8±7.8%,低温菌系Y15中的甲烷八叠球菌属(Methanosarcina)增高(15.7±21%),这类产甲烷古菌具有多种产甲烷代谢途径,M82中Methanoculleus丰度上升到13.6±13.1%,SK中Methanothermobacter丰度增大到48.5±11.2%。【结论】在低温条件下,菌系Y15可能主要通过乙酸裂解完成产甲烷代谢,在中高温条件下,菌系M82和SK中可能存在乙酸互营氧化产甲烷代谢途径,并且甲烷的产生分别通过不同种群的氢营养型产甲烷古菌来完成。     

不同激活剂对油藏内源微生物群落结构的影响

目的筛选大庆油田聚驱后油藏内源微生物采油激活剂的类型。方法在动态物理模拟实验模型基础上,利用基于16S rDNA的基因克隆文库方法,分析了两组激活剂配方激活的微生物群落结构。结果配方1激活的微生物菌群主要有假单胞菌属(75%)、深海弯曲菌属(18%)、陶厄菌属(6%);配方2激活的微生物菌群主要有陶厄菌属(50%)、假单胞菌属(26%)、螺杆菌属(15%)、梭菌属(9%)。结论激活剂配方2更适合大庆油田聚驱后油藏内源微生物采油。     

不同pH缓冲液对由乙酸产甲烷菌群结构的影响

【目的】研究不同p H缓冲液对乙酸产甲烷过程及对细菌和古菌群落结构的影响。【方法】分别添加磷酸盐(PB)、4-羟乙基哌嗪乙磺酸(HEPES)、哌嗪-1,4-二乙磺酸(PIPES)和Na HCO3/CO2缓冲液到乙酸产甲烷菌系中,定期监测甲烷产生趋势,到稳定期后收集菌体,进行16S rRNA基因的末端限制性片段多态性分析(T-RFLP)。【结果】发现PB组的乙酸产甲烷菌系延滞期约为40d,显著高于其他组的20-24 d(P0.05);Na HCO3/CO2组乙酸转化为甲烷的比例为(88.3±0.5)%,显著高于其他组的77%-81%(P0.05);不同缓冲液组的最大甲烷比生长速率为0.46-0.57 d-1(P0.05);Na HCO3/CO2组的细菌群落变化最明显,主要是未培养细菌(unclassified bacteria)、螺旋菌科细菌(Spirochaetaceae)和未培养WWE1类群的丰度较其他组分别增加到(15.5±9.4)%、(7.3±4.6)%和(17.6±6.3)%,而互养菌科(Synergistaceae)的细菌丰度降低到(8.9±8.1)%。AC+PB组中的古菌类群发生了明显变化,以竹节状甲烷鬃毛菌(Methanosaeta harundinacea)相关的产甲烷古菌占主导(97±2%),而在HEPES、PIPES和Na HCO3/CO2组和不加缓冲液组中同时存在两类乙酸营养型产甲烷古菌M.harundinacea和联合鬃毛甲烷菌(Methanosaeta concilii),以及属于甲烷杆菌目(Methanobacteriales)的氢营养型产甲烷古菌。【结论】在乙酸产甲烷菌系中加入PB增加了甲烷产生的延滞期,加入Na HCO3/CO2增加了甲烷产量,但是添加p H缓冲液不会影响到菌系的最大甲烷比生长速率。加入PB和Na HCO3/CO2都会显著改变微生物的菌群结构。这些研究为设计适宜的产甲烷菌系生长条件提供了参考。     

基于宏基因组技术分析全球不同温度带土壤微生物多样性

【背景】温度在塑造大尺度的土壤微生物群落方面发挥了重要作用,但目前针对全球不同温度带大尺度土壤微生物多样性方面的研究十分缺乏。【目的】明确不同温度带大尺度土壤微生物组成和功能的差异变化。【方法】从宏观的角度运用宏基因组技术对不同温度带土壤微生物群落的组成和功能进行分析。【结果】细菌的物种多样性随着温度带纬度的升高而增多,真菌的物种多样性在温带最多,在寒带最小且假丝酵母属(Candida)占绝对优势。3个温度带间除物种多样性存在差异外,微生物群落中物种丰度差异也较大,优势属和特殊属各有不同。其中值得注意的是,假单胞菌属(Pseudomonas)和芽孢杆菌属(Bacillus)的丰度在不同温度带间存在显著差异,且随着温度带纬度的升高而增多,而链霉菌属(Streptomyces)、地嗜皮菌属(Geodermatophilus)、红色杆菌属(Rubrobacter)和小单孢菌属(Micromonospora)的丰度随温度带纬度的升高而降低。在功能方面,发现与翻译后修饰、蛋白质周转、伴侣(posttranslational modification, protein turnover, chap...     

马缨杜鹃根系微生物群落结构及其变化

【目的】为了解野生马缨杜鹃根系微生物的群落结构特征,比较百里杜鹃内马缨杜鹃根际土壤、根表及根内3个生态位微生物群落组成差异,探究杜鹃根系生态位之间、变化菌属间的相互关系,以期为今后杜鹃根系微生物研究提供具有参考价值的数据。【方法】对百里杜鹃内野生马缨杜鹃根系微生物16S rRNA V4区和ITS1区进行高通量测序,比较分析根际土壤、根表及根内微生物群落多样性及组成差异;并基于共变化网络分析进一步探究差异菌属间的相互关系。【结果】马缨杜鹃根系不同的生态位之间,微生物群落结构存在差异,其中以根际土壤与根表、根内差异更为显著,且细菌群落差异小于真菌群落。且从根际-根表-根内,马缨杜鹃根系细菌α-多样性显著下降。马缨杜鹃根系微生物分布于41细菌门和6个真菌门。优势细菌门为变形菌门(Proteobacteria,39.64%±0.08,69.47%±0.12,77.34%±0.07)、酸杆菌门(Acidobacteria,34.10%±0.11,11.03%±0.04,9.18%±0.04)以及放线菌门(Actinobacteria,10.19%±0.03,8.70%±0.02,7.08%±0.01),它们占整体细菌群落总丰度的80%以上。同时8个细菌菌门的相对丰度在根际土壤、根表和根内间显著变化,且它们的相对丰度占细菌群落总丰度的75%以上。真菌主要分布于接合菌门(Zygomycota)、担子菌门(Basidiomycota)和子囊菌门(Ascomycota),它们占整体菌群的99%以上。马缨杜鹃根系存在589个属的细菌,390个属的真菌,从根际-根表-根内,其中25个细菌属和10个真菌属的相对丰度发生显著变化。马缨杜鹃根系微生物群落共变化网络分析表明:在马缨杜鹃根系不同生态位间,除Waitea外,包括枝孢菌属(Cladosporium)、拟盘多毛孢属(Pestalotiopsis)等在内的8个差异真菌菌属均与细菌菌属显著相关,它们相互作用调控微生物群落结构的变化。Bryobacter、Nocardia、Rhizomicrobium和Telmatobacter等核心菌属对马缨杜鹃根系微生物群落共变化网络的变化具有十分重要的调控作用。【结论】百里杜鹃地区马缨杜鹃根际土壤、根表以及根内3个生态位间,微生物群落组成存在差异;而造成微生物组成存在差异这一结果,可能与马缨杜鹃根系密切相关。同时,共变化网络分析揭示出马缨杜鹃根系生态位之间,细菌和真菌彼此间互作。     

猎豹(Acinonyx jubatus)肠道微生物多样性及其性别差异研究（英文）

【目的】探讨猎豹(Acinonyx jubatus)肠道微生物多样性特征。【方法】通过采集新鲜粪便样品,对9只健康成年野生猎豹(4只雄性,5只雌性)的肠道微生物16S rRNA基因V3–V4区进行高通量测序,对猎豹肠道微生物多样性进行研究。【结果】测序共获得肠道微生物16S rRNA基因V3–V4区有效序列599349条,序列平均长度405 bp。通过以97%的序列相似性进行分类,共获得操作分类单元(OTU)268个。经序列比对和分类鉴定,这些OTU都属于细菌域,包括10个门,21个纲,35个目,72个科,144个属。其中,丰度最高的5个细菌门是厚壁菌门(Firmicutes,平均占OTU总数的42.29%%)、放线菌门(Actinobacteria,31.54%)、梭杆菌门(Fusobacteroidetes,16.66%)、变形菌门(Proteobacteria,5.30%)和拟杆菌门(Bacteroidetes,4.19%)。拟杆菌门的丰度较低是猎豹肠道微生物的主要特征。丰度最高的5个科依次是红蝽杆菌科(Coriobacteriaceae,31.28%)、消化链球菌科(Peptostreptococcaceae,平均占17.66%),梭杆菌科(Fusobacteriaceae,15.46%)、毛螺菌科(Lachnospiraceae,12.40%)、梭菌科I(Clostridiaceae_I,6.93%)等。丰度最高的5个属依次是柯林斯氏菌属(Collinsella,30.16%)、梭杆菌属(Fusobacterium,15.46%)、艰难梭菌属(Peptoclostridium,11.46%)、Blautia属(8.28%)和狭窄梭菌属1(Clostridium_sensu_stricto_1,6.39%)。约有2.32%的OTU没有归类到属。群落alpha多样性分析结果显示,猎豹肠道微生物群落Shannon指数为2.93–4.41,Simpson指数为0.72–0.91。通过依据性别进行分组,对雌雄两组之间的alpha多样性比较表明,雄性组的物种和Shannon指数略高于雌性组。Beta多样性分析表明,雌雄两组之间的差异高于各组内部不同个体之间的差异。然而,聚类分析显示,相同性别的猎豹的肠道微生物并没有聚在一起。【结论】本文通过高通量测序技术研究了猎豹肠道微生物多样性特征和性别差异,为猎豹的保护、救护饲养和消化生理学研究提供了基础数据。     

高效降解纤维素产甲烷菌群的富集及其性质研究

以获得1组高效降解纤维素的产甲烷菌群为目的,以蔬菜厌氧消化液、糖蜜厌氧消化液和池塘沉积物底泥为菌株来源,55℃条件下,以滤纸为碳源进行继代培养,检测其甲烷含量,最终获得1组有效分解纤维素的产甲烷菌群。该菌群能够有效分解滤纸,相对分解率可达67.3%,培养7 d甲烷累积产量可达46.5%(体积分数),培养第3天羧甲基纤维素酶(CMC)活性最高值为26.3 U/mL。有机酸中乙酸产量最高,7 d累积量为2.7 g/L。基于16S rRNA基因扩增子高通量测序分析结果表明,细菌的多样性高于古菌。细菌菌群主要由Lutispora、好氧芽胞杆菌属(Aeribacillus)、解硫胺素杆菌属(Aneurinibacillus)、共生小杆菌属(Symbiobacterium)、梭菌属(Clostridium)等组成,其中Lutispora为优势菌群,占细菌总丰度的11.04%。古菌菌群主要包括甲烷嗜热杆菌属(Methanothermobacter)、甲烷丝状菌属(Methanothrix)、甲烷杆菌属(Methanobacterium)、甲烷螺菌(Methanospirillum)等,其中甲烷嗜热杆菌属为优势古菌菌群,占古菌总丰度的99.82%。这组高效降解纤维素的产甲烷菌群可通过多种微生物协同作用实现纤维素的降解和甲烷的产生。     

Effect of the addition of Peptostreptococcus productus ATCC35244 on the gastro-intestinal microbiota and its activity, as simulated in an in vitro simulator of the human gastro-intestinal tract

Peptostreptococcus productus ATCC35244, a reductive acetogenic strain, was added daily over 9 successive days to the fourth vessel (ascending colon) of the SHIME, a six-stage reactor system simulating the in vivo continuous culture conditions of the human gastro-intestinal tract. Final numbers of organisms (cfu)/ml reactor contents (c) were attained such that log₁₀ c = 6.9 ± 0.1. The addition caused the CH₄ production to decrease below the detection limit while total gas and CO₂ production in the fifth (transverse colon) and sixth reactor (descending colon) were lowered and the acetic acid concentration was augmented. Ending the supplementation caused CH₄ production to re-establish within 4 days, while CO₂ production increased much more slowly. The concentration of acetic acid only started to decrease after 7 days. The results indicate that P. productus, upon regular administration, is able to compete with methanogens for H₂ in the gastro-intestinal microbial ecosystem because of its reductive acetogenic character. Received: 11 December 1996 / Received revision: 26 February 1997 / Accepted: 1 March 1997     

放牧对若尔盖高原湿地CH4排放的影响

湿地是大气甲烷(CH_4)的主要排放源,而有关放牧对湿地CH_4排放的影响特征仍未得到足够的报道。因此,通过静态箱法,研究了放牧对四川省若尔盖高原湿地CH_4排放的影响,CH_4气体通过快速温室气体分析仪测量。结果表明:放牧样地和围栏内样地生长季CH_4排放量为(31.32±19.57)g/m~2和(30.31±23.46)g/m~2,它们之间无差异显著;但是集中放牧期间(7—9月),放牧样地(21.01±12.35)g/m~2较围栏内样地显著增加了CH_4排放量为54.3%。2014年生长季期间通过刈割植物模拟放牧表明两种刈割强度CH_4排放量为(5.01±5.37)g/m~2和(4.69±5.99)g/m~2,较未刈割样地(1.15±1.89)g/m~2增加了335.9%和308.0%,其原因可能是放牧或者刈割减少地表植物生物量,降低植物高度,缩短了CH_4排放的路径距离。该结果可为我国高原湿地保护与管理决策提供基础数据支撑。     

Plant transport and methane production as controls on methane flux from arctic wet meadow tundra

The roles of plant transport and CH₄ production in controlling CH₄ flux from wet meadow tundra communities were investigated. Plant transport was the dominant pathway of CH₄ flux from this ecosystem. Most CH₄ production (measured within situ anaerobic incubations) occurred well below the water table, and C supply (estimated by anaerobic CO₂ production) was the best single predictor of CH₄ production rates. Plant transport of CH₄ was controlled both by CH₄ supply and the plant species.Eriophorum angustifolium transported substantially more CH₄ than didCarex aquatilis, due to differences in size and structure of the two species. The composition of the plant community was a greater control on CH₄ flux from the site than either water table height (which varied only slightly) or CH₄ production rates, indicating the importance of species-specific plant dynamics in controlling CH₄ flux from arctic wetlands.     

The geochemistry of methane in Lake Fryxell,an amictic,permanently ice-covered,antarctic lake

The abundance and distribution of dissolved CH₄ were determined from 1987–1990 in Lake Fryxell, Antarctica, an amictic, permanently ice-covered lake in which solute movement is controlled by diffusion. CH₄ concentrations were < 1 υM in the upper oxic waters, but increased below the oxycline to 936 μM at 18 m. Sediment CH₄ was 1100 μmol (1 sed)⁻¹ in the 0–5 cm zone. Upward flux from the sediment was the source of the CH₄, NH₄ ⁺, and DOC in the water column; CH₄ was 27% of the DOC+CH₄ carbon at 18 m. Incubations with surficial sediments indicated that H¹⁴CO₃ ⁻ reduction was 0.4 μmol (1 sed)⁻¹ day⁻¹ or 4× the rate of acetate fermentation to CH₄. There was no measurable CH₄ production in the water column. However, depth profiles of CH₄, NH₄, and DIC normalized to bottom water concentrations demonstrated that a significant CH₄ sink was evident in the anoxic, sulfate-containing zone of the water column (10–18 m). The δ¹³CH₄ in this zone decreased from −72 % at 18 m to −76% at 12 m, indicating that the consumption mechanism did not result in an isotopic enrichment of ¹³CH₄. In contrast, δ¹³CH₄ increased to −55 % at 9 m due to aerobic oxidation, though this was a minor aspect of the CH₄ cycle. The water column CH₄ profile was modeled by coupling diffusive flux with a first order consumption term; the best-fit rate constant for anaerobic CH₄ consumption was 0.012 yr⁻¹. On a total carbon basis, CH₄ consumption in the anoxic water column exerted a major effect on the flux of carbonaceous material from the underlying sediments and serves to exemplify the importance of CH₄ to carbon cycling in Lake Fryxell.     

Production of hexanoic acid from d-galactitol by a newly isolated Clostridium sp. BS-1

In a study screening anaerobic microbes utilizing d-galactitol as a fermentable carbon source, four bacterial strains were isolated from an enrichment culture producing H₂, ethanol, butanol, acetic acid, butyric acid, and hexanoic acid. Among these isolates, strain BS-1 produced hexanoic acid as a major metabolic product of anaerobic fermentation with d-galactitol. Strain BS-1 belonged to the genus Clostridium based on phylogenetic analysis using 16S rRNA gene sequences, and the most closely related strain was Clostridium sporosphaeroides DSM 1294^T, with 94.4% 16S rRNA gene similarity. In batch cultures, Clostridium sp. BS-1 produced 550 ± 31 mL L⁻¹ of H₂, 0.36 ± 0.01 g L⁻¹ of acetic acid, 0.44 ± 0.01 g L⁻¹ of butyric acid, and 0.98 ± 0.03 g L⁻¹ of hexanoic acid in a 4-day cultivation. The production of hexanoic acid increased to 1.22 and 1.73 g L⁻¹ with the addition of 1.5 g L⁻¹ of sodium acetate and 100 mM 2-(N-morpholino)ethanesulfonic acid (MES), respectively. Especially when 1.5 g L⁻¹ of sodium acetate and 100 mM MES were added simultaneously, the production of hexanoic acid increased up to 2.99 g L⁻¹. Without adding sodium acetate, 2.75 g L⁻¹ of hexanoic acid production from d-galactitol was achieved using a coculture of Clostridium sp. BS-1 and one of the isolates, Clostridium sp. BS-7, in the presence of 100 mM MES. In addition, volatile fatty acid (VFA) production by Clostridium sp. BS-1 from d-galactitol and d-glucose was enhanced when a more reduced culture redox potential (CRP) was applied via addition of Na₂S·9H₂O.     

安徽某铁矿不同矿山废水库中微生物群落结构特征

【目的】研究安徽某铁矿不同矿山废水库中微生物群落结构特征及其影响因素。【方法】对比分析了该铁矿3个大型废水库的地球化学特征,并用高通量测序技术研究了水体中微生物群落组成,进而用统计学方法解析了环境因子对微生物群落结构的影响。【结果】3个废水库中有2个为酸性,1个为中性,理化性质有明显的差异。近年形成的塌方采场废水库(TF) pH仅为2.55±0.01,Fe浓度高达154.95±0.78mg/L,SO_4~(2–)浓度为3374.86±3.81mg/L;形成于20世纪70年代的排土场废水库(PT)酸性略弱(pH 2.9±0.02),Fe浓度(34.57±4.00 mg/L)与TF相比明显降低,SO_4~(2–)浓度则高达10398.98±626.70 mg/L;东沙采场废水库(DS)则为中性(pH7.55),但SO_4~(2–)仍高达4162.99mg/L,主要的金属离子为Mg(594.90 mg/L)、Ca (650.10 mg/L)。3个废水库的原核生物多样性随pH的升高而升高。两个酸性废水库的原核生物组成较为接近,但TF的化能自养菌含量较高(69.54%±2.89%),PT的化能异养菌含量较高(64.45%±13.81%)。自养铁氧化菌Ferrovum在TF中的比例高达(64.17±1.84)%,在PT中则下降为(35.39±13.74)%。但PT中含有丰富的化能异养嗜酸菌如Acidicapsa(15.75%±3.99%)、Acidiphilium(10.65%±2.05%)、Acidisphaera (6.34%±1.02%)等。DS中虽然也含有较高的金属离子和SO_4~(2–),但其中的原核生物组成与TF和PT截然不同,主要为Limnohabitans (18.47%)、Rhodobacter (8.42%)等。3个废水库的真核生物群落主要由藻类组成,酸水库TF和PT中主要为棕鞭藻属(Ochromonas)和胶球藻属(Coccomyxa),棕鞭藻属在TF中(53.65%±2.02%)占优势,胶球藻属在PT中(68.84±10.4%)占优势,中性废水库DS中则主要是小环藻属(Cyclotella)(49.85%)。经统计学分析,pH是影响矿山废水微生物多样性和群落组成的主要环境因素。     

不同干扰因素对森林和湿地温室气体通量影响的研究进展

森林和湿地是CO2、CH4和N2O等温室气体重要的源、汇和转换器,在全球气候变化过程中起着重要作用。森林和湿地温室气体通量受到诸多因子的作用,其中干扰便是一个重要的因素。不同干扰因素对于森林和湿地生态系统温室气体通量的影响,国际上已经开展了相应的研究。基于人为和自然两大类干扰方式,分别从采伐、施肥、垦殖等人为干扰因素和火烧、台风(飓风)等自然干扰因素综述了干扰对于森林和湿地生态系统CO2、CH4和N2O通量的影响。根据目前研究中存在的不足,提出了今后应需加强的领域,以期更好地揭示干扰对于森林和湿地生态系统温室气体通量的影响及作用机制,为今后深入开展相关研究提供一定的参考价值。     

闽江河口芦苇沼泽和短叶茳芏沼泽生态系统含碳温室气体的年收支

河口感潮沼泽是全球重要的蓝碳生态系统,具有很强的固碳能力。碳收支研究是量化生态系统碳源/汇过程及固碳规模的基础。本研究运用透明箱和不同遮光率布遮盖+红外气体分析仪/气相色谱相结合的方法,模拟不同光照条件,测定闽江河口鳝鱼滩半咸水芦苇沼泽和短叶茳芏沼泽的瞬时净生态系统二氧化碳（CO₂）交换量（net ecosystem exchange,NEE）、生态系统呼吸（ecosystem respiration,ER）以及甲烷（CH₄）排放通量,并通过对总光合吸收量（gross ecosystem exchange,GEE）与光合有效辐射的拟合以及ER与气温的拟合,外推2个沼泽生态系统CO₂气体在月、年尺度上的NEE和ER,评估其年固碳量。2个沼泽生态系统的NEE和ER均具有明显的季节变化,春夏秋季为大气中CO₂的汇,而冬季则转化为大气中CO₂的源,芦苇沼泽年尺度固碳能力显著高于短叶茳芏沼泽。芦苇沼泽与短叶茳芏沼泽CH₄排放通量差异不显著。综合考虑CH₄排放,闽江河口鳝鱼滩半咸水芦苇沼泽、短叶茳芏沼泽生态系统年固碳量分别为（5371.52±336.97） g CO₂-eq/m²和（2730.32±503.67） g CO₂-eq/m²。研究表明：闽江河口半咸水沼泽湿地在年尺度上是一个较强的碳汇,在缓解全球变暖方面发挥着重要的角色。     

Land-Use Change and Biogeochemical Controls of Methane Fluxes in Soils of Eastern Amazonia

Tropical soils account for 10%–20% of the 15–35 Tg of atmospheric methane (CH₄) consumed annually by soils, although tropical deforestation could be changing the soil sink. The objectives of this study were (a) to quantify differences in soil CH₄ fluxes among primary forest, secondary forest, active pasture, and degraded pasture in eastern Amazonia; and (b) to investigate controlling mechanisms of CH₄ fluxes, including N availability, gas-phase transport, and soil respiration. At one ranch, Fazenda Vitória, annual uptake estimates (kg CH₄ha⁻¹ y⁻¹) based on monthly measurements were: primary forest, 2.1; secondary forest, 1.0; active pasture, 1.3; degraded pasture, 3.1. The lower annual uptake in the active pasture compared with the primary forest was due to CH₄ production during the wet season in the pasture soils, which is consistent with findings from other studies. In contrast, the degraded pasture was never a CH₄ source. Expressing uptake as a negative flux and emission as a positive flux, CH₄ fluxes were positively correlated with CO₂ fluxes, indicating that root and microbial respiration in the productive pastures, and to a lesser extent in the primary forest, contributed to the formation of anaerobic microsites where CH₄ was produced, whereas this productivity was absent in the degraded pasture. In all land uses, uptake rates of atmospheric CH₄ were greater in the dry season than in the wet season, indicating the importance of soil water content and gas transport on CH₄ fluxes. These clay soils had low annual uptake rates relative to reported rates on sandy soils, which also is consistent with gas transport within the soil being a limiting factor. Nitrogen availability indices did not correlate with CH₄ fluxes, indicating that inhibition of CH₄ oxidation was not an important mechanism explaining differences among land uses. At another ranch, Fazenda Agua Parada, no significant effect of pasture age was observed along a chronosequence of pasture ages. We conclude that land-use change can either increase or decrease the soil sink of CH₄, depending on the duration of wet and dry seasons, the effects of seasonal precipitation on gas-phase transport, and the phenology and relative productivity of the vegetation in each land use.