Soil microbes and the availability of soil nutrients

It is likely to provide plants with their necessary nutrients using chemical and biological fertilization. Although chemical fertilization is a quick method, it is not recommendable economically and environmentally, especially if overused. Biological fertilization is the use of soil microbes including arbuscular mycorrhizal fungi and plant growth promoting rhizobacteria to inoculate plants. It has been proved that biological fertilization is an efficient method to supply plants with their necessary nutrients. It is economically and environmentally recommendable, because it results in sustainability. In this article, some of the most important details including the mechanisms and processes regarding the effects of soil microbes on the availability and hence uptake of nutrients by plant are reviewed. Such details can be important for the selection and hence production of microbial inoculums, which are appropriate for biological fertilization.     

植物吸收利用有机氮营养研究进展

植物矿质营养学问世以后,人们一直认为无机氮是植物吸收氮素的主要形态.随着研究手段的改进和研究内容的不断深入,现已证实许多没有菌根的维管植物都可以直接吸收可溶性有机氮,特别是小分子的氨基酸.由此引起了人们对植物有机营养、植物营养方式多样化问题的重视.研究表明：氨基酸可以通过多种方式释放到土壤溶液中,土壤中的氨基酸主要来源于微生物、动植物及其代谢产物等.土壤氨基酸含量受土壤温湿度、所施的有机肥料、生长的植物种类及其生长发育时期的影响.植物对氨基酸的吸收是一个主动吸收过程,受载体调节,并与能量状况有关,同时受介质中pH和温度的影响.但是有关植物吸收氨基酸的机理及其生态过程还需进行深入的研究.     

植物源抗菌肽的研究进展

植物抗菌肽是植物自身合成的能够防御环境中微生物侵害的一类小分子多肽.它们大都是阳离子多肽,有较好的热稳定性.根据作用位点和抗菌机理的不同,植物抗菌肽可分为三大类:第一类通过干扰微生物细胞壁的合成来抑制微生物生长;第二类作用于质膜使其产生穿膜孔洞,从而导致微生物因细胞物质外泄受损;第三类则通过抑制某些细胞器的作用而起到抑菌的效果.本文从抗菌肽的作用机理及其分类等方面对植物源抗菌肽的研究进展进行了综述.     

连作障碍与根际微生态研究Ⅰ.根系分泌物及其生态效应

作物、蔬菜、果树以及苗木长期连作后,皆出现生长衰退和产量降低．许多研究结果表明,连作条件下土壤生态环境对植物生长有很大的影响,尤以植物残体与病原微生物的分解产物,对植物有致毒作用,并影响植物根系分泌物正常代谢,以致于发生自毒作用．本文围绕根系分泌物与根际微生态的相互关系,系统地介绍连作障碍条件下,影响根系分泌物的环境因素（土壤空气、湿度、养分与微生物）、活性物质（自身毒素、残体分解物、微生物产生毒素）、土壤病原菌等的根际效应,为深入研究根系分泌物与连作障碍的相互作用机制提供启示．     

连作障碍与根际微生态研究 Ⅰ. 根系分泌物及其生态效应

作物、蔬菜、果树以及苗木长期连作后,皆出现生长衰退和产量降低。许多研究结果表明,连作条件下土壤生态环境对植物生长有很大的影响,尤以植物残体与病原微生物的分解产物,对植物有致毒作用,并影响植物根系分泌物正常代谢,以致于发生自毒作用。本文围绕根系分泌物与根际微生态的相互关系,系统地介绍连作障碍条件下,影响根系分泌物的环境因素(土壤空气、湿度、养分与微生物)、活性物质(自身毒素、残体分解物、微生物产生毒素)、土壤病原菌等的根际效应,为深入研究根系分泌物与连作障碍的相互作用机制提供启示。     

土壤灭菌处理对入侵植物南美蟛蜞菊及其伴生种生长的影响

该研究以温室盆栽法对南美蟛蜞菊重度入侵土壤进行高温高压湿热灭菌、添加杀真菌剂灭菌和添加杀细菌剂灭菌的处理后,将三种植株定植96 d后测定各生理指标参数,研究重度入侵土壤中各微生物类群对南美蟛蜞菊及其伴生种金腰箭和狗肝菜生长的影响。结果表明:在杀真菌、杀细菌以及高温高压湿热灭菌和未处理的南美蟛蜞菊重度入侵土壤中,三种植物生长情况均存在较大差异。在高温高压湿热灭菌土壤中南美蟛蜞菊的生长受到显著抑制,与未处理土壤中的生长情况相比,株高降低了17.59%,叶片数降低了38.10%,生物量降低了56.00%,电子传递速率变化不明显。在杀真菌土壤和杀细菌土壤中金腰箭的生长也受到显著抑制,与未处理土壤中的生长情况相比较,杀真菌土壤中的金腰箭株高降低最多(为42.28%),叶片数降低了38.89%,生物量降低了16.99%,电子传递速率变化不明显;在杀细菌土壤中金腰箭株高降低了36.64%,叶片数降低最多(为38.89%),生物量降低了33.67%,电子传递速率升高了11.11%。由此可见,不含微生物的土壤对南美蟛蜞菊生长有较强的抑制作用,不含真菌和细菌的土壤对金腰箭的生长有明显抑制作用。南美蟛蜞菊重度入侵土壤不仅适合南美蟛蜞菊的生长,也适合金腰箭的生长,对狗肝菜影响不大。     

The effects of Epichloë endophytes on the growth and competitiveness of Achnatherum sibiricum are mediated by soil microbe diversity

季节性干旱驱动亚热带森林的碳积累 本研究旨在表明处于南亚热带的鼎湖山生物圈保护区的干旱频率和强度正在增加,并说明季节性干旱对亚热带森林碳积累的影响。这是为了应对全球气候变化导致的干旱加剧所带来的威胁开展的一项研究。我们使干旱指数(标准化降水指数、标准降水蒸散发指数、降水距平百分率及自校准帕尔默干旱指数)准确确定干旱期和降水量增加期。此后,将2003至2014年(12年)监测采集的实测涡动通量和土壤含水量数据在干旱期和湿润期之间进行比较,以确定干旱对生态系统碳积累的影响。在本研究所选择的12年期间,干旱的发生时间约占比20%,最强干旱事件和严重程度发生于2012至2013年。研究期间的年平均降水量和气温分别为1404.57 ± 43.2 mm和22.65 ± 0.1 °C,与30年记录(1990–2020)相比较,年降水量减少量可达523 mm,而气温则增加了2.55 °C。与全球针对大多数森林生态系统研究所发表的数据呈相反趋势,处于中国南亚热带区域的鼎湖山生物圈保护区在60%的干旱期内所监测的森林生态系统记录到显著的碳积累趋势,说明季节性干旱驱动了森林的碳积累。     

The unseen majority: soil microbes as drivers of plant diversity and productivity in terrestrial ecosystems

Microbes are the unseen majority in soil and comprise a large portion of life's genetic diversity. Despite their abundance, the impact of soil microbes on ecosystem processes is still poorly understood. Here we explore the various roles that soil microbes play in terrestrial ecosystems with special emphasis on their contribution to plant productivity and diversity. Soil microbes are important regulators of plant productivity, especially in nutrient poor ecosystems where plant symbionts are responsible for the acquisition of limiting nutrients. Mycorrhizal fungi and nitrogen-fixing bacteria are responsible for c. 5–20% (grassland and savannah) to 80% (temperate and boreal forests) of all nitrogen, and up to 75% of phosphorus, that is acquired by plants annually. Free-living microbes also strongly regulate plant productivity, through the mineralization of, and competition for, nutrients that sustain plant productivity. Soil microbes, including microbial pathogens, are also important regulators of plant community dynamics and plant diversity, determining plant abundance and, in some cases, facilitating invasion by exotic plants. Conservative estimates suggest that c. 20 000 plant species are completely dependent on microbial symbionts for growth and survival pointing to the importance of soil microbes as regulators of plant species richness on Earth. Overall, this review shows that soil microbes must be considered as important drivers of plant diversity and productivity in terrestrial ecosystems.     

Soil microbes and plant fertilization

With respect to the adverse effects of chemical fertilization on the environment and their related expenses, especially when overused, alternative methods of fertilization have been suggested and tested. For example, the combined use of chemical fertilization with organic fertilization and/or biological fertilization is among such methods. It has been indicated that the use of organic fertilization with chemical fertilization is a suitable method of providing crop plants with adequate amount of nutrients, while environmentally and economically appropriate. In this article, the importance of soil microbes to the ecosystem is reviewed, with particular emphasis on the role of plant growth-promoting rhizobacteria, arbuscular mycorrhizal fungi, and endophytic bacteria in providing necessary nutrients for plant growth and yield production. Such microbes are beneficial to plant growth through colonizing plant roots and inducing mechanisms by which plant growth increases. Although there has been extensive research work regarding the use of microbes as a method of fertilizing plants, it is yet a question how the efficiency of such microbial fertilization to the plant can be determined and increased. In other words, how the right combination of chemical and biological fertilization can be determined. In this article, the most recent advances regarding the effects of microbial fertilization on plant growth and yield production in their combined use with chemical fertilization are reviewed. There are also some details related to the molecular mechanisms affecting the microbial performance and how the use of biological techniques may affect the efficiency of biological fertilization.     

土壤微生物削弱了水生-陆地系统补贴对植物生长的正向影响

土壤微生物削弱了水生-陆地系统补贴对植物生长的正向影响 水生-陆地系统补贴形成的联结作用在构建群落和调节生态系统功能方面发挥重要作用。在营养贫瘠的生态系统中(例如密歇根湖周围的淡水沙丘),水生-陆生系统补贴显得尤为重要。春季成年蠓在密歇根湖涌出,成群交配,然后死亡。蠓尸体在植物的基部形成土丘状,通过输入营养提高植物的生产力。然而,水生-陆地系统补贴对植物生产力的影响可能取决于其他生物的交互作用,特别是土壤微生物可能通过促进养分转化为植物可利用的形式或与植物竞争养分而发挥关键作用。在温室实验中,我们检验了湖生蠓(Chironomidae)的尸体和土壤微生物如何独立和相互影响一种常见沙丘草(沙拂子茅,Calamovilfa longifolia)的生长表现。为确定蠓是否影响土壤非生物特性,我们检验了添加蠓如何影响土壤养分和土壤湿度。研究结果显示,蠓极大地增加了植物生物量,但其效应的大小受土壤微生物的影响。在没有土壤微生物的情况下,添加蠓的植物生物量比没有添加的高7倍,而在有土壤微生物的情况下,植物生物量提高了3倍。蠓对植物生长的促进作用可能由于它们向土壤中输入养分所导致,因为与沙丘土壤相比,蠓的氮、磷、钾含量分别高100倍、10倍和150倍。我们的研究结果表明,土壤微生物可能与植物竞争这些养分。总之,我们发现蠓是重要的水生-陆地系统补贴,对密歇根湖沿岸植物生产力产生强烈和正向的影响,但水生-陆地系统补贴作用必须在生态群落内发生的复杂相互作用的背景下考虑。     

小球藻的营养及药用价值

微藻因具有丰富的营养价值和产油能力,因而已被广泛研究。小球藻属于单细胞绿藻,分布广泛,种类多达十余种,在食品、医药、饲料、能源和环保等多个领域具有广泛的应用价值。小球藻不仅可以光自养生长,还可以利用有机碳源进行异养生长。小球藻细胞壁坚厚,胞内含有丰富的蛋白质、必需氨基酸、多糖、色素、脂肪酸,并富含多种维生素,以及铁、钙、锌、钾等矿物元素,具有全面而均衡的营养价值。小球藻属中的蛋白核小球藻已被我国卫生部列为新资源食品。小球藻特有的促生长因子（CGF）具有提高免疫力、抗肿瘤等多种特殊功效,近年来研究证明小球藻在临床上可作为治疗多种疾病的辅助药物,被认为是绿色天然的营养保健食品。本文从小球藻的生物学特性、营养价值、药理和保健作用等方面进行了论述。     

The effect of growth substances on Verticillium wilt of tomato plants

This paper describes the effects of a number of growth-regulating substances on the development of disease in tomato plants caused by Verticillium albo-atrum. Indole-acetic acid usually reduced disease and also reduced the number of hyphae in the stem but it increased tylosis; low concentrations slightly stimulated disease development. Some control of disease was obtained by removing apical buds, and axillary shoots as they developed. When the apical bud alone was removed, developing axillary shoots sometimes wilted; this did not occur in plants with intact buds. Gibberellic acid increased disease in susceptible plants and also induced symptoms in resistant plants. Maleic hydrazide greatly reduced growth of plants, made them more diseased and stimulated growth of the parasite in the vessels. Of other growth-regulating substances tested, 2,4,6-trichlorophenoxy-acetic acid, 2,3,5-triiodobenzoic acid and 2,4-dichlorophenoxyacetic acid increased disease at some concentrations and reduced it at others. Cycocel (2-chloroethyl) trimethyl ammonium chloride and naphthaleneacetamide, gave good control of disease over a range of concentrations when applied to the soil in which plants were growing. Treatments which reduced disease also reduced the growth of the parasite in the shoot and stimulated the formation of tyloses. Indole and 2,4-dichloroanisole had some effect on disease development but this was much less than that induced by the other substances.     

解磷微生物的研究进展

磷是植物生长必需的矿质元素之一,而土壤中可溶性磷的含量比较低。土壤中有大量的微生物存在,其中有一些微生物能够将土壤中的不溶性磷转化成可溶性磷,主要对解磷微生物的种类、数量、分布、解磷机制及应用方面的有关情况进行综述。     

几种高等水生植物的克藻效应研究

研究了五种高等水生植物(黑藻、金鱼藻、水花生、茭白、空心菜)对蛋白核小球藻、斜生栅藻生长的抑制作用。试验结果显示,各种受试植物均有不同程度的克藻效果,金鱼藻与黑藻的克藻作用最强,水花生的作用次之。克藻效果以受试植物与藻共培养最佳,其次为连续添加种植水,表明在植物的生长过程中其化感物质是连续释放且能迅速降解的,而黑藻干物质的浸提液所具有的克藻效应说明有些化感物质对一定温度和光照是较稳定的。     

Effects of labile soil carbon on nutrient partitioning between an arctic graminoid and microbes

We measured partitioning of N and P uptake between soil microorganisms and potted Festuca vivipara in soil from a subarctic heath in response to factorial addition of three levels of labile carbon (glucose) combined with two levels of inorganic N and P. The glucose was added to either non-sterilized or sterilized (autoclaved) soils in quantities which were within the range of reported, naturally occurring amounts of C released periodically from the plant canopy. The aims were, firstly, to examine whether the glucose stimulated microbial nutrient uptake to the extent of reducing plant nutrient uptake. This is expected in nutrient-deficient soils if microbes and plants compete for the same nutrients. Secondly, we wanted to test our earlier␣interpretation that growth reduction observed in graminoids after addition of leaf extracts could be caused directly by labile carbon addition, rather than by phytotoxins in the extracts. Addition of high amounts of N did not affect the microbial N pool, whereas high amounts of added P significantly increased the microbial P pool, indicating a luxury P uptake in the microbes. Both plant N and in particular P uptake increased strongly in response to soil sterilization and to addition of extra N or P. The increased␣uptake led to enhanced plant growth when both elements were applied in high amounts, but only led to increased tissue concentrations without growth responses when the nutrients were added separately. Glucose had strong and contrasting effects on plant and microbial N and P uptake. Microbial N and P uptake increased, soil inorganic N and P concentrations were reduced and plant N and P uptake declined when glucose was added. The responses were dose-dependent within the range of 0–450 μg C g⁻¹ soil added to the non-sterilized soil. The opposite responses of plants and microbes showed that plant acquisition of limiting nutrients is dependent on release of nutrients from the soil microbes, which is under strong regulation by the availability and microbial uptake of labile C. Hence, we conclude, firstly, that the microbial populations can compete efficiently with plants for nutrients to an extent of affecting plant growth when the microbial access to labile carbon is high in nutrient deficient soils. We also conclude that reduced growth of plants after addition of leaf extracts to soil can be caused by carbon-induced shifts in nutrient partitioning between plants and microbes, and not necessarily by phytotoxins added with the extracts as suggested by some experiments. Received: 15 February 1997 / Accepted: 12 July 1997     

Comparative phytotoxicity of nitrophenolic soil pollutants and their microbial metabolites to the growth of cucumber (Cucumis sativus L.) seedlings

Summary 2,4-Dinitrophenol and paranitrophenol are two major soil pollutants which are known to be metabolized by different soil microbes. Relative phytotoxicities of these parent compounds and their metabolic transformation products to the growth of cucumber seedlings were assessed. It was evident that such microbial transformations widely occurring in the soil are effective detoxification reactions and are beneficial for the plants.     

Bacterial diversity in the rhizosphere of maize and the surrounding carbonate‐rich bulk soil

Maize represents one of the main cultivar for food and energy and crop yields are influenced by soil physicochemical and climatic conditions. To study how maize plants influence soil microbes we have examined microbial communities that colonize maize plants grown in carbonate‐rich soil (pH 8.5) using culture‐independent, PCR‐based methods. We observed a low proportion of unclassified bacteria in this soil whether it was planted or unplanted. Our results indicate that a higher complexity of the bacterial community is present in bulk soil with microbes from nine phyla, while in the rhizosphere microbes from only six phyla were found. The predominant microbes in bulk soil were bacteria of the phyla Acidobacteria, Bacteroidetes and Proteobacteria, while Gammaproteobacteria of the genera Pseudomonas and Lysobacter were the predominant in the rhizosphere. As Gammaproteobacteria respond chemotactically to exudates and are efficient in the utilization of plants exudate products, microbial communities associated to the rhizosphere seem to be plant‐driven. It should be noted that Gammaproteobacteria made available inorganic nutrients to the plants favouring plant growth and then the benefit of the interaction is common.     

Survival and colonisation potential of photoautotrophic microorganisms within a glacierised catchment on Svalbard, High Arctic

The survival and colonisation potential of photoautotrophic microbes (cyanobacteria and microalgae) were investigated in three terrestrial environments within a glacierised catchment on Svalbard: old vegetation-covered soil, recently deglaciated barren soil and subglacial sediments. One-year reciprocal transplant incubations of photoautotrophic microbial communities from the three soil/sediment environments were conducted in order to reveal the autochthonous or allochthonous origin of the present photoautotrophs. The abundance and taxonomic composition of photoautotrophic microbes and their changes over time and between soil/sediment types and physico-chemical characteristics of the soils/sediments were determined. The recovery time of a photoautotrophic community by import of cells was between several months in subglacial and vegetated soils and up to 27 years in proglacial soils. No active growth was recorded in subglacial sediments, whilst positive growth, and so the potential for autochthonous recovery, was found in proglacial and vegetated soils. The most suitable environment for the survival of transplanted microbes was provided in proglacial soil. We show here that the new proglacial substrata can be successfully colonised by photoautotrophic microbes, and that input of allochthonous cells may, in some cases, exceed in situ microbial growth. Whilst the subglacial environment is rather a conduit for photoautotrophic microbes than a place of growth and production, the supply of viable photoautotrophs in it is relatively high and may serve as a significant resource of nutrients for subglacial microbial communities.     

The influence of the method of sampling on the accuracy of the determination of bacterial numbers in the soil

Summary Tests were made to determine the influence of the sampling and the preparatory treatment of the samples on the counting of bacteria in the soil. These proved that the present methods are very inaccurate and give rise to considerable variance in parallel determinations, to the extent even of rendering the effect of a perfected counting procedure quite negligible.In this connection it has been stated that it is useless to aim at a minute counting of bacteria, as only the number of microbes in the ultimate soil suspension would thus be determined, whereas this suspension is by no means accurately representative of the tested soil.For a better preparatory treatment of the samples a homogeneisation method by means of a porcelan ball mill was worked out, according to which a suspension is made of the sample with water, which method has given satisfactory results.Finally, the determination of various chemical substances, apart from the counting of microbes, has been included in our tests. Here also an improvement in the treatment of the samples was arrived at.     

Sensitivity of environmental microorganisms to antimicrobial agents.

The sensitivity of different microorganisms, considered as typical representatives of the microflora of soil and water, was established to evaluate the influence of the nonmedical use of antimicrobial agents on bacterial ecology. Only seven strains, six chemoorganotrophs and one chemolithotroph, could be considered as relatively sensitive to the 21 antimicrobial compounds tested. The other 29 microorganisms may be regarded as resistant to most antimicrobial agents. Streptomyces were sensitive to high concentrations of active substances. Broad-spectrum antibiotics showed an effect on environmental bacteria similar to that on human pathogens. Cephalothin stimulated the growth of a Chlorella sp. From these experiments, it appears that spilled antimicrobial agents have little chance of causing an alteration in the microbial ecology.