Microbial activities and dissolved organic matter dynamics in oil-contaminated surface seawater from the Deepwater Horizon oil spill site

The Deepwater Horizon oil spill triggered a complex cascade of microbial responses that reshaped the dynamics of heterotrophic carbon degradation and the turnover of dissolved organic carbon (DOC) in oil contaminated waters. Our results from 21-day laboratory incubations in rotating glass bottles (roller bottles) demonstrate that microbial dynamics and carbon flux in oil-contaminated surface water sampled near the spill site two weeks after the onset of the blowout were greatly affected by activities of microbes associated with macroscopic oil aggregates. Roller bottles with oil-amended water showed rapid formation of oil aggregates that were similar in size and appearance compared to oil aggregates observed in surface waters near the spill site. Oil aggregates that formed in roller bottles were densely colonized by heterotrophic bacteria, exhibiting high rates of enzymatic activity (lipase hydrolysis) indicative of oil degradation. Ambient waters surrounding aggregates also showed enhanced microbial activities not directly associated with primary oil-degradation (β-glucosidase; peptidase), as well as a twofold increase in DOC. Concurrent changes in fluorescence properties of colored dissolved organic matter (CDOM) suggest an increase in oil-derived, aromatic hydrocarbons in the DOC pool. Thus our data indicate that oil aggregates mediate, by two distinct mechanisms, the transfer of hydrocarbons to the deep sea: a microbially-derived flux of oil-derived DOC from sinking oil aggregates into the ambient water column, and rapid sedimentation of the oil aggregates themselves, serving as vehicles for oily particulate matter as well as oil aggregate-associated microbial communities.     

不同寡营养培养条件下南海水体细菌群落结构及其对碳源的利用特征

【背景】绝大多数海洋微生物不可培养,为挖掘海洋生态系统中可培养的微生物资源,研究者尝试寡营养培养等方法。【目的】比较不同寡营养培养条件下南海水体细菌数量、群落结构及其对碳源的利用特征差异。【方法】采用原2216E培养液(Y)、稀释10倍(Y-10)和稀释50倍(Y-50)的2216E培养液培养南海海水样品,用荧光定量PCR法和16S rRNA基因检测细菌数量和菌群结构;利用平板计数法计数异养细菌的数量,纯化鉴定可培养细菌;采用Biolog EcoPlateTM微板法分析不同培养基中细菌群落对碳源的利用特征。【结果】Y组细菌总数高于Y-10组和Y-50组,差异不显著(P>0.05),但异养细菌数量显著高于Y-10组和Y-50组(P<0.05)。16S rRNA基因测序结果表明,不同稀释倍数下的细菌群落结构差异明显,Y组检测出10门193属,优势类群为Proteobacteria(56.44%)和Bacteroides (37.27%);Y-10组检测出15门220属,优势类群为Proteobacteria (40.30%)、Bacteroides(36.91%)和Firmic...     

Latitudinal gradients in degradation of marine dissolved organic carbon

Heterotrophic microbial communities cycle nearly half of net primary productivity in the ocean, and play a particularly important role in transformations of dissolved organic carbon (DOC). The specific means by which these communities mediate the transformations of organic carbon are largely unknown, since the vast majority of marine bacteria have not been isolated in culture, and most measurements of DOC degradation rates have focused on uptake and metabolism of either bulk DOC or of simple model compounds (e.g. specific amino acids or sugars). Genomic investigations provide information about the potential capabilities of organisms and communities but not the extent to which such potential is expressed. We tested directly the capabilities of heterotrophic microbial communities in surface ocean waters at 32 stations spanning latitudes from 76°S to 79°N to hydrolyze a range of high molecular weight organic substrates and thereby initiate organic matter degradation. These data demonstrate the existence of a latitudinal gradient in the range of complex substrates available to heterotrophic microbial communities, paralleling the global gradient in bacterial species richness. As changing climate increasingly affects the marine environment, changes in the spectrum of substrates accessible by microbial communities may lead to shifts in the location and rate at which marine DOC is respired. Since the inventory of DOC in the ocean is comparable in magnitude to the atmospheric CO(2) reservoir, such a change could profoundly affect the global carbon cycle.     

Resource quantity affects benthic microbial community structure and growth efficiency in a temperate intertidal mudflat

Estuaries cover <1% of marine habitats, but the carbon dioxide (CO(2)) effluxes from these net heterotrophic systems contribute significantly to the global carbon cycle. Anthropogenic eutrophication of estuarine waterways increases the supply of labile substrates to the underlying sediments. How such changes affect the form and functioning of the resident microbial communities remains unclear. We employed a carbon-13 pulse-chase experiment to investigate how a temperate estuarine benthic microbial community at 6.5°C responded to additions of marine diatom-derived organic carbon equivalent to 4.16, 41.60 and 416.00 mmol C m(-2). The quantities of carbon mineralized and incorporated into bacterial biomass both increased significantly, albeit differentially, with resource supply. This resulted in bacterial growth efficiency increasing from 0.40 ± 0.02 to 0.55 ± 0.04 as substrates became more available. The proportions of diatom-derived carbon incorporated into individual microbial membrane fatty acids also varied with resource supply. Future increases in labile organic substrate supply have the potential to increase both the proportion of organic carbon being retained within the benthic compartment of estuaries and also the absolute quantity of CO(2) outgassing from these environments.     

大理河沉积物微生物碳源利用特征及其影响因素

沉积物是河流生态系统中氮磷等物质循环的重要场所,而微生物是河流生态系统的重要组成部分,探究沉积物中微生物群落碳源利用特征和功能多样性对于河流生态环境保护具有重要意义。利用Biolog Eco微平板法、基于主成分分析、冗余分析阐明了大理河流域沉积物中微生物群落碳源利用强度和功能多样性变化特征及其影响因素。结果表明：（1）从流域上游到流域下游,沉积物中微生物碳源利用强度逐渐降低,与上游相比,支流、中游、下游沉积物中微生物碳源利用强度分别降低了13.4%、30.5%、30.7%。（2）沉积物中微生物群落功能多样性存在差异,沉积物中微生物群落功能多样性（Shannon-Wiener多样性指数）表现为上游 > 支流 > 中游 > 下游,常见物种优势度（Simpson多样性指数）则表现为下游 > 支流 > 中游 > 上游。（3）与微生物代谢活动相关性较高碳源为糖类,其次是氨基酸类,聚合物类、羧酸类、胺类、酚酸类与微生物代谢活动相关性较低。（4）沉积物中全氮、氨氮、硝氮、有机碳含量是影响微生物群落功能多样性和碳源利用特征差异的主要因素。流域沉积物中合适的碳、氮水平对维持河流水生态健康具有重要的意义。     

不同林龄杉木+闽楠复层林土壤磷形态及微生物功能多样性变化

磷是限制亚热带地区林木生长的关键因素之一,研究土壤微生物群落功能多样性对土壤磷素的影响,对亚热带地区人工林可持续经营具有重要意义。在江西官山林场选取了3种不同林龄杉木+闽楠（4 a、7 a、11 a）复层林为研究对象,测定了土壤全磷、有效磷及无机磷组分含量,采用Biolog-ECO法研究了复层林表土层（0-20 cm）土壤微生物群落对碳源的利用特征,并分析了土壤磷素与土壤微生物功能多样性的关系。结果表明：（1）土壤全磷、有效磷及无机磷组分含量随复层林营建时间延长呈增加趋势;（2）不同林分类型土壤微生物群落功能多样性差异显著。土壤微生物碳源代谢活性（AWCD）以及多样性指数也均随复层林营建时间延长呈增加趋势;多聚物类是杉木纯林土壤微生物利用的主要碳源,7 a复层林对碳水化合物、羧酸和酚酸的利用强度较大,11 a复层林对氨基酸、胺类、多聚物、羧酸和酚酸的利用强度较大,并且11 a复层林土壤微生物群落代谢碳水化合物、氨基酸、羧酸、胺类和酚酸的强度显著高于4 a复层林和杉木纯林,而4 a复层林与杉木纯林土壤微生物群落对不同碳源利用率的差异较小（除多聚物外）。（3）土壤微生物多样性指数、氨基酸类、胺类和酚酸类物质与土壤全磷、有效磷、Al-P和Fe-P含量之间显著正相关,随机森林模型分析表明,氨基酸、胺类和酚酸是不同林分类型土壤微生物利用的主要碳源。因此,杉木纯林转化为复层异龄林更有利于森林土壤磷的储存和供应,土壤微生物群落代谢功能多样性的增大可能是提高复层异龄林土壤磷有效性的关键调控因素。     

干旱区典型盐生植物群落土壤团聚体组成及有机碳分布

以干旱区玛纳斯河流域扇缘带为研究区,分析了花花柴(Karelinia caspia)、雾冰藜(Bassia dasyphylla)、梭梭(Haloxylon ammodendron)和柽柳(Tamarix ramosissima)4个典型盐生植物群落土壤团聚体的组成及有机碳分布。研究表明:不同植物群落土壤团聚体均以0.25—0.053 mm粒径为主,占了46.7%—74.6%,且与其他粒径差异显著(P0.05),0.25 mm和0.053mm粒径土壤团聚体含量较少,仅占7.8%—43%。梭梭群落0.25 mm团聚体平均含量较高,达32%。不同植被群落土壤总有机碳介于2.01—8.73 g/kg之间,不同粒径团聚体有机碳介于1.70—13.68 g/kg之间。不同群落之间,梭梭和柽柳群落总有机碳和团聚体有机碳含量均相对较高,且随着土层深度下降而下降。不同粒径之间,有机碳含量在0.25—0.053 mm粒径最低,在0.25 mm和0.053 mm粒径中最高,呈现"V"型分布且差异显著(P0.05)。0.25—0.053 mm团聚体中有机碳含量的贡献率最高,达43.43%,而0.053 mm粒级贡献率较低,但有机碳含量较高,说明了小粒径团聚体对有机碳保护能力较强。土壤有机碳含量与0.25—0.053 mm团聚体含量呈显著负相关(P0.05)。而从整体来看,梭梭群落0.25 mm团聚体比例较高,且土壤有机碳和团聚体有机碳含量也较高,说明了在该研究区,梭梭群落聚集土壤养分能力较强,相对其他群落更有利于土壤有机碳的积累。     

黄土高原天然次生林植被演替过程中土壤团聚体有机碳动态变化

土壤团聚体物理保护是促进有机碳积累主要机制之一。以黄土高原子午岭林区天然次生林植被演替群落为对象,研究从农田、草地（白羊草,Bothriochloa ischaemum）、灌木林（沙棘,Hippophae rhamnoides）、先锋林（山杨,Populus davidiana）到顶级林（辽东栎,Quercus liaotungensis）5个植被演替阶段0-20 cm土壤团聚体稳定性和团聚体有机碳的动态变化,并分析团聚体有机碳的影响因素。结果表明：土壤团聚体稳定性随着植被演替显著提高（P<0.05）,顶级林的团聚体稳定性最高;土壤有机碳含量和各粒径土壤团聚体（> 2 mm、2-0.25 mm、0.25-0.053 mm、<0.053 mm）有机碳含量均随着植被演替而增加。除草地0.25-0.053 mm团聚体有机碳含量最高外,其他演替阶段均为0.25-2 mm粒径最高。根系生物量、凋落物生物量、微生物生物量碳、团聚体稳定性均与团聚体有机碳含量呈显著正相关关系（P<0.05）。总体而言,长期植被演替有助于团聚体稳定性和团聚体有机碳累积。     

BACTERIAL ASSOCIATIONS WITH MARINE OSCILLATORIA SP. (TRICHODESMIUM SP.) POPULATIONS: ECOPHYSIOLOGICAL IMPLICATIONS1

On three separate occasions we investigated morphological and physiological aspects of bacterial associations with planktonic aggregates of the ubiquitous marine N₂ fixing cyanobacterium Trichodesmium sp. Close associations generally characterized Trichodesmium blooms; associations were present during day- and night-time. Colonization by both rod-shaped and filamentous heterotrophic bacteria occurred on Trichodesmiun aggregates actively fixing N₂ (acetylene reduction). Scanning electron and optical microscopy showed bacteria located both around and within aggregates. Microautoradiography demonstrated that associated bacteria largely mediated utilization of trace additions of ³H-labeled carbohydrates (fructose, glucose, mannitol) and amino acids, whereas Trichodesmium utilized amino acids only. Oxygen measurements using microelectrodes revealed high localized oxygen consumption among aggregates, with rapid (within a minute) changes from supersaturated to subsaturated oxygen following the transition from photosynthetic illuminated to dark periods. Stab culturing techniques confirmed the presence of heterotrophic N₂ fixers among aggregate-associated bacteria. Parallel deployment of oxygen microelectrodes, the tetrazolium salt 2,3,5 triphenyl tetrazolium chloride (TTC) and acetylene reduction assays demonstrated microaerophilic requirements for expression of nitrogenase activity among cultured bacteria. Trichodesmium aggregates are characterized by dynamic nutrient and oxygen regimes, which promote and maintain simultaneous and contiguous oxygenic photosynthesis and N₂ fixation. In part, the above-mentioned consortial interactions with a variety of heterotrophic bacteria facilitate Trichodesmium biomass production and bloom formation in nitrogen depleted, oligotrophic tropical/subtropical waters.     

刺参养殖池塘水体微生物群落功能多样性的季节变化

利用Biolog技术和冗余分析(RDA)方法对刺参养殖池塘水体微生物群落功能多样性的季节变化及其与环境因子间的关系进行研究.结果表明： 刺参池塘水体微生物对碳源总量和单类碳源的利用均具有显著的季节变化,总体表现为夏季最高、冬季最低,其利用比例较高的碳源类型为聚合物.主成分分析表明,刺参池塘水体微生物群落碳代谢方式具有显著的季节变化,其中,与主成分1显著相关的碳源主要有10种,分别属于聚合物、糖类、羧酸、氨基酸和胺.刺参池塘水体微生物碳代谢多样性指数Shannon、McIntosh、Simpson和S E均匀度均存在显著的季节变化,但不同指数之间的变化有较大差异.RDA分析表明,TP、NO₃^--N、TN和PO₄^3--P是影响刺参池塘水体微生物群落功能多样性季节变化的主要因素.     

芽胞杆菌对鱼池微生物群落代谢功能的影响

利用Biotog平板,以施用与不施用芽胞杆菌的鱼塘为研究对象,研究鱼塘水体与表泥不同空间的微生物群落代谢功能的差异。结果表明：芽胞杆菌提高了水体微生物群落代谢的平均活性,及对氨基酸类、胺类、羧酸类、聚合物及其它类碳源的利用能力,提高了水体微生物群落代谢的多样性（Shannon均度、Simpson指数、McIntosh均度差异显著）;两池表泥微生物群落代谢平均活性差异较小,对同一碳源的利用差异不大,芽胞杆菌显著提高了表泥的Simpson指数,但表泥的McIntosh指数显著低于对照池。总体而言,鱼塘施用芽胞杆菌,水体微生物群落代谢功能所受的影响大过表泥,芽胞杆菌通过提高水体微生物群落代谢活性,提高了水体微生物对有机污染物的降解能力,以此改善池塘的生态环境。     

长期施肥对红壤微生物生物量碳氮和微生物碳源利用的影响

采集湖南省祁阳县红壤长期定位施肥19年的土壤样品,分析长期不同施肥红壤的微生物生物量碳、氮和微生物碳源利用率,以揭示长期施肥对红壤微生物学性状的影响.结果表明：施肥19年后,有机肥单施或与化肥配合施用均显著提高土壤微生物生物量碳、氮和微生物碳源利用率.单施有机肥的土壤微生物生物量碳、氮含量分别为231和81 mg·kg^-1,化肥有机肥配施分别为148和73 mg·kg^-1,均显著高于化肥配施秸秆、不施肥和单施化肥;施用有机肥和化肥配施秸秆的土壤微生物生物量氮占全氮的比例平均为6.0%,显著高于单施化肥和不施肥.Biolog-ECO分析中,平均吸光值(AWCD)的大小为：化肥有机肥配施、单施有机肥>对照>单施化肥、化肥配施秸秆.单施有机肥或与化肥有机肥配施增加了红壤微生物对碳水化合物、羧酸、氨基酸、聚合物、酚类和胺类的碳源利用率;化肥配施有机肥的红壤微生物对聚合物类碳源利用率最高,化肥配施秸秆的红壤微生物对碳水化合物类碳源的利用率最高.表明施用有机肥能显著提高红壤的微生物生物量碳、氮和微生物碳源利用率,提高红壤肥力,保持作物高产.     

亚热带森林土壤微生物生物量及群落功能特征的城乡梯度变化

土壤微生物在土壤养分循环以及生物地球化学循环中起着重要作用,土壤微生物对环境变化响应灵敏.为研究城乡梯度环境变化对亚热带森林土壤微生物的影响,本研究选取合肥市大蜀山国家森林公园(城市林)、紫蓬山国家森林公园(远郊林)、六安市万佛山(乡村自然林)为样地,分析比较其微生物生物量碳(MBC)、微生物生物量氮(MBN)及微生物...     

刺参池塘底质微生物群落功能多样性的季节变化

利用BIOLOG技术和冗余分析(Redundancy analysis,RDA)方法对刺参(Apostichopus japonicus)养殖池塘底质环境(底泥、附着基)微生物群落功能多样性的季节变化及其与环境因子的关系进行了研究。结果表明:(1)刺参池塘底泥和附着基微生物对碳源总量和单类碳源的利用均具有显著的季节变化,总体表现为春、夏、秋季节高于冬季,其中,底泥微生物利用比例较高的碳源类型为聚合物、糖类、羧酸和氨基酸,附着基微生物利用比例较高的碳源类型为聚合物、糖类、氨基酸和胺。(2)主成分分析表明,刺参池塘底泥和附着基微生物碳代谢方式均具有显著的季节变化。底泥中,与主成分显著相关的碳源有18种,其中与主成分1显著相关的主要是糖类、羧酸和氨基酸,与主成分2显著相关的主要是聚合物和糖类;附着基中,与主成分显著相关的碳源有22种,其中与主成分1显著相关的主要是聚合物、糖类、羧酸和氨基酸,与主成分2显著相关的是羧酸。(3)刺参池塘底泥和附着基微生物多样性指数Shannon、McIntosh、Simpson和S-E均匀度均存在显著的季节变化,但不同指数之间的变化有较大差异。(4)RDA分析表明,TP、NO3-N和PO4-P是影响底泥微生物功能多样性季节变化的主要因素,SOM、NO3-N和TN是影响附着基微生物功能多样性季节变化的主要因素。结论认为,刺参池塘底泥和附着基微生物功能多样性具有显著的不同的季节变化,这些变化与环境因子具有很好的相关性。     

Prevalence of Heterotrophy and Atmospheric CO2 Emissions from Aquatic Ecosystems

Recent, parallel developments in the study of freshwater and marine ecosystems have provided evidence that net heterotrophic systems (those in which respiratory organic matter destruction exeeds photosynthetic production) are more prevalent than hitherto believed, including most rivers, oligo- to mesotrophic lakes and some oligotrophic regions of the ocean. In parallel, these aquatic ecosystems have been shown to act as CO₂ sources to the atmosphere, as expected from the heterotrophic nature of the communities they contain. The prevalence of net heterotrophic aquatic ecosystems indicates that they must receive significant inputs of organic carbon from adjacent ecosystems, assigning an important role to the lateral exchanges of carbon between land and aquatic ecosystems, between coastal and open ocean ecosystems, as well as internal redistribution within large or complex aquatic ecosystems in determining their metabolic status and the gaseous exchange with the atmosphere. The examination of the carbon budget of ecosystems requires, therefore, an integrative approach that accounts for exchanges between compartments often studied in isolation. These recent findings conform a new paradigm of the functioning of aquatic ecosystems, and the metabolic connectivity between ecosystems in the biosphere.     

HETEROTROPHY AND PHOTOHETEROTROPHY BY ANTARCTIC MICROALGAE: LIGHT-DEPENDENT INCORPORATION OF AMINO ACIDS AND GLUCOSE 1

Diatoms isolated from the benthic, planktonic and sea ice microbial communities in Mc Murdo Sound, Antarctica assimilated ambient concentrations of dissolved amino acids and glucose in both the light and dark. Uptake of amino acids but not glucose was influenced by the iucubation irradiance and amino acid uptake rates were up to 250 times greater than those of glucose. Amino acids were incorporated into proteins and other complex polymers and the rates of assimilation and patterns of polymer synthesis were similar to those of the light-saturated photosynthetic incorporation of inorganic carbon. This suggests that these diatoms can use exogenous amino acids to synthesize the essential macromolecules for heterotrophic growth. The assimilation of dissolved organic substrates could supplement light-limited growth during the austral spring and summer as well as potentially support the heterotrophic growth of these diatoms throughout the aphotic polar winter.     

耕作方式对潮土土壤团聚体微生物群落结构的影响

为探究不同耕作方式对潮土土壤团聚体微生物群落结构和多样性的影响,采用磷脂脂肪酸(PLFA)法测定了土壤团聚体中微生物群落。试验设置4个耕作处理,分别为旋耕+秸秆还田(RT)、深耕+秸秆还田(DP)、深松+秸秆还田(SS)和免耕+秸秆还田(NT)。结果表明:与RT相比,DP处理显著提高了原状土壤和>5 mm粒级土壤团聚体中真菌PLFAs量和真菌/细菌,为真菌的繁殖提供了有利条件,有助于土壤有机质的贮存,提高了土壤生态系统的缓冲能力;提高了5～2 mm粒级土壤团聚体中细菌PLFAs量,降低了土壤革兰氏阳性菌/革兰氏阴性菌,改善了土壤营养状况;提高了<0.25 mm粒级土壤团聚体中微生物丰富度指数。总的来说,深耕+秸秆还田(DP)对土壤团聚体细菌和真菌生物量有一定的提高作用,并且在一定程度上改善了土壤团聚体微生物群落结构,有利于增加土壤固碳能力和保持土壤微生物多样性。冗余分析结果表明,土壤团聚体总PLFAs量、细菌、革兰氏阴性菌和放线菌PLFAs量与土壤有机碳相关性较强,革兰氏阳性菌PLFAs量与总氮相关性较强。各处理较大粒级土壤团聚体微生物群落主要受碳氮比、含水量、pH值和团聚体质量分数的影响,较小粒级土壤团聚体微生物群落则主要受土壤有机碳和总氮的影响。     

Extracellular enzymes in terrestrial, freshwater, and marine environments: perspectives on system variability and common research needs

Extracellular enzymes produced by heterotrophic microbial communities are major drivers of carbon and nutrient cycling in terrestrial, freshwater, and marine environments. Although carbon and nutrient cycles are coupled on global scales, studies of extracellular enzymes associated with terrestrial, freshwater, and marine microbial communities are not often compared across ecosystems. In part, this disconnect arises because the environmental parameters that control enzyme activities in terrestrial and freshwater systems, such as temperature, pH, and moisture content, have little explanatory power for patterns of enzyme activities in marine systems. Instead, factors such as the functional diversity of microbial communities may explain varying patterns of enzyme activities observed in the ocean to date. In any case, many studies across systems focus on similar issues that highlight the commonalities of microbial community organization. Examples include the effective lifetime of enzymes released into the environment; the extent to which microbial communities coordinate enzyme expression to decompose complex organic substrates; and the influence of microbial community composition on enzyme activities and kinetics. Here we review the often-disparate research foci in terrestrial, freshwater, and marine environments. We consider the extent to which environmental factors may regulate extracellular enzyme activities within each ecosystem, and highlight commonalities and current methodological challenges to identify research questions that may aid in integrating cross-system perspectives in the future.     

Sequential bioavailability of sedimentary organic matter to heterotrophic bacteria

Aquatic sediments harbour diverse microbial communities that mediate organic matter degradation and influence biogeochemical cycles. The pool of bioavailable carbon continuously changes as a result of abiotic processes and microbial activity. It remains unclear how microbial communities respond to heterogeneous organic matrices and how this ultimately affects heterotrophic respiration. To explore the relationships between the degradation of mixed carbon substrates and microbial activity, we incubated batches of organic‐rich sediments in a novel bioreactor (IsoCaRB) that permitted continuous observations of CO₂ production rates, as well as sequential sampling of isotopic signatures (δ¹³C, Δ¹⁴C), microbial community structure and diversity, and extracellular enzyme activity. Our results indicated that lower molecular weight (MW), labile, phytoplankton‐derived compounds were degraded first, followed by petroleum‐derived exogenous pollutants, and finally by higher MW polymeric plant material. This shift in utilization coincided with a community succession and increased extracellular enzyme activities. Thus, sequential utilization of different carbon pools induced changes at both the community and cellular level, shifting community composition, enzyme activity, respiration rates, and residual organic matter reactivity. Our results provide novel insight into the accessibility of sedimentary organic matter and demonstrate how bioavailability of natural organic substrates may affect the function and composition of heterotrophic bacterial populations.     

澳大利亚亚热带不同森林土壤微生物群落对碳源的利用

为阐明土壤微生物群落对碳源利用类型和强度,采用MicroRespTM方法研究3种森林类型不同土壤含水量微生物群落对不同类型碳源的利用情况,结果表明：湿地松（Pinus elliottii Engelm. var. elliotttii）林地土壤微生物碳源利用率依次为60%WHC>20%WHC>40%WHC,南洋杉（Araucaria cunninghamii）和贝壳杉（Agathis australis）林地土壤微生物对碳源利用的格局相似,为20%WHC>60%WHC>40%WHC。南洋杉和贝壳杉林地土壤对碳源利用率趋势相同,主要是对L-苹果酸、草酸和L-赖氨酸利用比较高。在40%WHC处理中,3种树种对碳源的利用均很低,差异不明显。除精氨酸和L-赖氨酸外,60%WHC处理土壤微生物利用单一碳源能力的大小顺序为：南洋杉>湿地松>贝壳杉。3种树种土壤Shannon多样性指数(H’)、Shannon均匀度(E)和Simpson指数(D)均无显著差异。土壤pH值影响微生物对L-丙氨酸、精氨酸、D-( )-葡萄糖、N-乙酰基-氨基葡萄糖的利用率较大,这些类群的微生物主要分布在贝壳杉林地;分布在南洋杉林地的微生物对柠檬酸、L-苹果酸和γ-酪氨酸利用率较大,且主要是受TP的影响;D-( )-果糖、柠檬酸和L-半胱氨酸-盐酸等受水分、TN和TC等影响较大,这类微生物类群主要分布在湿地松林地。