Microbial activity and organic matter dynamics during 4 years of irrigation with treated wastewater

The global changes in rainfall frequency and quantity have subjected arid and semi-arid regions to long periods of drought. As this phenomenon corresponds to increasing trend of water shortage, the use of treated wastewater (TWW) has been suggested as an alternative for irrigation of agricultural crops in these areas. The aim of the study was to investigate the short- and middle-term effects of TWW irrigation on the soil microbial activities and organic carbon content. The microbial community activity was measured every 1–3 months for 4 years in a persimmon (Diospyros kaki) orchard. These activities were used here as an indicator for the soil health. The hydrolysis activity (detected by fluorescein diacetate hydrolysis (FDA) assay) increased during the irrigation season and was significantly higher in soils irrigated with TWW compared to those irrigated with freshwater (FW). This activity was also negatively correlated with dissolved organic carbon (DOC) concentrations during the irrigation season, suggesting that the community degraded the DOC in the soils regardless of its origin. The irrigation season was also characterized by an increase in nitrification potential in both TWW- and FW-irrigated soils, which coincided with high concentrations of nitrate (50 mg kg⁻¹ soil). Overall, there was an increase in all measured activities during the irrigation season, and they were higher in the TWW soils. However, it appears that after each irrigation season, the potential activity of the community returned to levels similar to or even slightly lower than those of FW-irrigated soil during the wet season, suggesting that the periodic irrigation did not significantly change the soil microbial activity.     

Rapid top–down regulation of plant C:N:P stoichiometry by grasshoppers in an Inner Mongolia grassland ecosystem

Mosses play an integral role in the hydrologic regimes of ecosystems where they cover the soil surface, and thus affect biogeochemical cycling of elements influenced by soil oxidation–reduction (redox) reactions, including the plant growth-limiting nutrients, nitrogen and phosphorus (P). In rich fens where P often limits plant growth, we hypothesized that feedbacks between mosses and redox conditions would determine P availability to shallow-rooted forb species that constitute much of these wetlands’ unusually high plant species diversity. In a moss removal experiment in three fens, forb tissue P and microbial P were greater while anion exchange membrane (AEM) resin P was lower where mosses occurred than where they were removed, suggesting both higher availability and greater demand for P in moss-covered soils. Coupled physicochemical and biological mechanisms drove moss effects on P cycling, ultimately through effects on soil oxygenation or reduction: higher redox potential underlying mosses corresponded to greater microbial activity, phosphatase enzyme activity, and colonization by arbuscular mycorrhizal fungi (AMF), all of which can promote greater P availability to plants. These more oxidized soils stimulated: (1) greater microbial activity and root vigor; (2) correspondingly greater P demand via microbial uptake, forb uptake, and iron (Fe)-P reactions; and (3) greater P supply through soil and root phosphatase activity and AMF colonization. This work demonstrates that mosses improve vascular plant P acquisition by alleviating stresses caused by reducing conditions that would otherwise prevail in shallow underlying soils, thus providing a mechanism by which mosses facilitate plant species diversity in rich fens.     

Diversity of Arbuscular Mycorrhizal Fungus Populations in Heavy-Metal-Contaminated Soils

High concentrations of heavy metals have been shown to adversely affect the size, diversity, and activity of microbial populations in soil. The aim of this work was to determine how the diversity of arbuscular mycorrhizal (AM) fungi is affected by the addition of sewage-amended sludge containing heavy metals in a long-term experiment. Due to the reduced number of indigenous AM fungal (AMF) propagules in the experimental soils, several host plants with different life cycles were used to multiply indigenous fungi. Six AMF ecotypes were found in the experimental soils, showing consistent differences with regard to their tolerance to the presence of heavy metals. AMF ecotypes ranged from very sensitive to the presence of metals to relatively tolerant to high rates of heavy metals in soil. Total AMF spore numbers decreased with increasing amounts of heavy metals in the soil. However, species richness and diversity as measured by the Shannon-Wiener index increased in soils receiving intermediate rates of sludge contamination but decreased in soils receiving the highest rate of heavy-metal-contaminated sludge. Relative densities of most AMF species were also significantly influenced by soil treatments. Host plant species exerted a selective influence on AMF population size and diversity. We conclude based on the results of this study that size and diversity of AMF populations were modified in metal-polluted soils, even in those with metal concentrations that were below the upper limits accepted by the European Union for agricultural soils.     

内蒙古中部地区马铃薯根际和根系丛枝菌根真菌类群的多样性

【背景】丛枝菌根真菌(arbuscular mycorrhizal fungus,AMF)是菌根真菌中分布最广泛的一类真菌,能够与90%以上的植物形成菌根共生体,并通过调节宿主体内的代谢活动增强植物的抗逆性。【目的】揭示内蒙古马铃薯主产区土壤中AMF的结构与组成,解析马铃薯不同发育阶段以及连作对AMF类群的影响。【方法】以内蒙古中部地区大井村、徐麻夭村和红格尔图村采集的马铃薯根系及根际土为材料,通过PCR扩增建立18S rRNA基因文库,研究不同地点、不同马铃薯生育阶段以及连作对马铃薯根系内和根际土中的AMF类群组成和多样性的影响。【结果】大井村和红格尔图村马铃薯根际土中的AMF的类群多样性优于徐麻夭村,其中Glomus为大井村和红格尔图村马铃薯根际土样本中AMF的优势菌群,而徐麻夭村样本根际土中的优势类群为Diversispora。马铃薯根系中的AMF多样性的研究结果表明,3个供试地点根系内AMF类群的类型没有显著差异,但是AMF类群的比例却不同。大井村根系样本中AMF的优势菌为Diversispora,而Rhizophagus是红格尔图村和徐麻夭村根系样本中的优势AMF类群。同一供试地点马铃薯苗期和块茎膨大期根际土中的AMF类群的类型多于块茎形成期,其中Glomus是马铃薯不同发育阶段根际土中的优势类群;而Rhizophagus是3个不同发育阶段根系内的优势类群。2015和2016年马铃薯连作地块中根际土和根系内AMF类群的类型完全相同,但是不同的AMF类群的相对丰度随着马铃薯的连作呈现出显著的变化。其中,根际土样本中Glomus和Archaeospora类群的相对丰度随着连作有所上升,相应的Entrophospora和Diversispora相对丰度有所下降;根系样本中AMF的优势类群随着连作从Glomus转变为Rhizophagus。AMF多样性测定结果表明,连作对马铃薯根际土中AMF多样性的影响显著高于对根系内类群的影响。【结论】AMF类群的多样性会因土壤组成成分、马铃薯生育期和连作效应而呈现不同变化。     

间作栽培对连作马铃薯根际土壤微生物群落的影响

连作严重影响了作物的产量和品质,而土壤微生物群落结构与功能对土壤生态系统和植物健康至关重要。以连作10a土壤为基质,单作马铃薯为对照,采用磷脂脂肪酸(Phospholipid fatty acids)、BIOLOGA技术和真菌形态学鉴定方法,研究了玉米、蚕豆与马铃薯间作模式下土壤微生物群落结构、功能和丛植菌根(Arbuscular Mycorrhizal)真菌对土壤环境变化的响应。结果表明:间作调控下,马铃薯根际土壤微生物主要类群结构发生显著改变;玉米间作马铃薯,土壤微生物群落总生物量降低,但群落功能多样性提高,促进了以羧酸类、多聚化合物、芳香类化合物、氨基酸类化合物为碳源的微生物类群代谢活性增强;蚕豆间作增加了土壤微生物总生物量,仅促进了以碳水化合物为碳源的微生物类群代谢活性。间作改变了作物根际土壤AM真菌的种、属数,AM真菌多样性降低,优势种由明球囊霉、地球囊霉转变为玉米间作体系里的福摩萨球囊霉、球泡球囊霉;蚕豆间作体系里福摩萨球囊霉和疣状无梗囊霉是优势种。间作栽培下AM真菌优势种群的变化可能受植物间的共生关系、微生物结构与功能等因素的制约。间作条件下,玉米显著影响了马铃薯根际土壤微生物群落功能多样性,而蚕豆则显著改变了微生物群落结构多样性;玉米、蚕豆对马铃薯根际土壤微生物群落功能与结构变化的影响不同步;间作调控后持续的土壤微生物群落结构与功能观察才有助于解释土壤微生物结构变化引起的功能响应。     

Arbuscular mycorrhizal fungal diversity in phosphorus-deficient Alfisols of a dry North-western agro-ecosystem of Tamil Nadu,India

Semi-arid tropical soils, characterized by low soil organic carbon (SOC) with limited available macronutrients and micronutrients for crop plants, are predicated to have a yield sustainability problem in the future due to intensive cropping and limited nutrient management adoptions. Arbuscular mycorrhizal fungi (AMF), the functional link between plant and soil, play a pivotal role in nutrient cycling, organic matter stabilization and soil structure and fertility improvement. Hence, so far unexplored or underutilized, native AMF could be a potential resource for fertility management of these semi-arid tropical soils. Hence, in the present investigation, we assessed the abundance and diversity of AMF in phosphorus-deficient agricultural soils of semi-arid tropics of southern India. Our results show that the spore density and infective propagules of AMF were relatively low in these soils. The morpho-typing of extracted AMF spores revealed that these soils were dominated by glomeraceae (six species of Glomus) while species of Gigaspora, Scutellospora and Acaulospora were found in low abundance. The diversity indices assessed for the AMF species were also globally low. The non-metric multi-dimensional scaling and hierarchical cluster analysis of species richness showed variation in the community composition of AMF in the soils. The principal component analysis of the assessed soil variables suggest that the available phosphorus (P), SOC and dehydrogenase and alkaline phosphatase activities had negative impact on spore density and infective propagules of AMF with no effect on species diversity. The regression analyses reveal that the available P is the significant soil variable that drives the AMF abundance and infectivity. This study opens the possibilities of effective utilization of native mycorrhizae for agriculture in semi-arid tropical soils.     

土壤管理措施及环境因素对土壤微生物多样性影响研究进展

本文综述了土壤管理措施及环境因素对土壤微生物多样性影响的研究进展,并介绍了土壤微生物多样性的研究方法,土壤微生物多样性包括微生物物种多样性、遗传多样性和生态多样性。传统上,土壤微生物群落的分析依赖于培养技术,但使用该技术只能培养和分离出一部分土壤微生物群落。现在国际上普遍使用Biolog分析、磷脂脂肪酸(PLFA)分析和核酸分析等多种现代技术研究和表征土壤微生物多样性。土壤微生物多样性受土壤管理措施和多种环境因素的影响。农药可能使土壤微生物多样性减少或改变其结构和功能;施有机肥有利于维持土壤微生物的多样性及活性;但在施用无机肥的影响上目前的报道有矛盾之处。农业土壤减少耕作可能增加微生物多样性和生物量;轮作可能比单一栽培耕作更有利于维持土壤微生物的多样性及活性。土壤微生物多样性也受土壤有机质、植被、季节变化等因素的影响,且通常遭受干旱、过度放牧、营养缺乏等的胁迫作用。     

盐渍化土壤根际微生物群落及土壤因子对AM真菌的影响

为探明盐渍化土壤影响下AM真菌与根际土壤间的关系,试验选取宁夏碱化龟裂土、草甸盐土、盐化灌淤土3种类型4个样地上典型植被群落,测定了植物根际土壤养分含量、微生物群落结构、AM真菌侵染率以及孢子密度。结果显示:盐渍化土壤根际微生物碳源利用类型显著不同,对芳香类化合物的代谢能力整体较弱;红寺堡草甸盐土上微生物优势群落为氨基酸代谢类群,惠农盐化灌淤土为多聚化合物代谢群,西大滩碱化龟裂土为碳水化合物代谢群。AM真菌孢子密度与微生物碳源代谢群间的关系比较复杂。其中,惠农样点根际土壤孢子密度与多聚化合物微生物代谢群呈显著正相关,西大滩地区孢子密度与碳水化合物微生物代谢群呈显著正相关。土壤有机质、全盐、全氮、碱解氮等土壤肥力因子及土壤中的HCO-3、Na+、Cl-等盐基离子含量能解释AM真菌孢子密度与土壤环境因子之间相互关系的大部分信息。较高的HCO-3浓度促进了AM真菌侵染率的提高,但高盐浓度下Na+和Cl-降低了菌根侵染率。土壤对AM真菌孢子密度、侵染率的影响因土壤盐分组成类型的不同而异。研究结果为深入了解AM真菌多样性,促进宁夏盐碱地的合理开发与利用提供了理论依据。     

Changes in the diversity of soil arbuscular mycorrhizal fungi after cultivation for biofuel production in a Guantanamo (Cuba) tropical system

The arbuscular mycorrhizal fungi (AMF) are a key, integral component of the stability, sustainability and functioning of ecosystems. In this study, we characterised the AMF biodiversity in a native vegetation soil and in a soil cultivated with Jatropha curcas or Ricinus communis, in a tropical system in Guantanamo (Cuba), in order to verify if a change of land use to biofuel plant production had any effect on the AMF communities. We also asses whether some soil properties related with the soil fertility (total N, Organic C, microbial biomass C, aggregate stability percentage, pH and electrical conductivity) were changed with the cultivation of both crop species. The AM fungal small sub-unit (SSU) rRNA genes were subjected to PCR, cloning, sequencing and phylogenetic analyses. Twenty AM fungal sequence types were identified: 19 belong to the Glomeraceae and one to the Paraglomeraceae. Two AMF sequence types related to cultured AMF species (Glo G3 for Glomus sinuosum and Glo G6 for Glomus intraradices-G. fasciculatum-G. irregulare) did not occur in the soil cultivated with J. curcas and R. communis. The soil properties (total N, Organic C and microbial biomass C) were higher in the soil cultivated with the two plant species. The diversity of the AMF community decreased in the soil of both crops, with respect to the native vegetation soil, and varied significantly depending on the crop species planted. Thus, R. communis soil showed higher AMF diversity than J. curcas soil. In conclusion, R. communis could be more suitable for the long-term conservation and sustainable management of these tropical ecosytems.     

Soil initial bacterial diversity and nutrient availability determine the rate of xenobiotic biodegradation

Understanding the relative importance of soil microbial diversity, plants and nutrient management is crucial to implement an effective bioremediation approach to xenobiotics-contaminated soils. To date, knowledge on the interactive effects of soil microbiome, plant and nutrient supply on influencing biodegradation potential of soils remains limited. In this study, we evaluated the individual and interactive effects of soil initial bacterial diversity, nutrient amendments (organic and inorganic) and plant presence on the biodegradation rate of pyrene, a polycyclic aromatic hydrocarbon. Initial bacterial diversity had a strong positive impact on soil biodegradation potential, with soil harbouring higher bacterial diversity showing ~ 2 times higher degradation rates than soils with lower bacterial diversity. Both organic and inorganic nutrient amendments consistently improved the degradation rate in lower diversity soils and had negative (inorganic) to neutral (organic) effect in higher diversity soils. Interestingly, plant presence/type did not show any significant effect on the degradation rate in most of the treatments. Structural equation modelling demonstrated that initial bacterial diversity had a prominent role in driving pyrene biodegradation rates. We provide novel evidence that suggests that soil initial microbial diversity, and nutrient amendments should be explicitly considered in the design and employment of bioremediation management strategies for restoring natural habitats disturbed by organic pollutants.     

Microbial inoculation influences arbuscular mycorrhizal fungi community structure and nutrient dynamics in temperate tree restoration

Soil microbial communities have a profound influence on soil chemical processes and subsequently influence tree nutrition and growth. This study examined how the addition of a commercial inoculum or forest‐collected soils influenced nitrogen (N) and phosphorus (P) dynamics, soil microbial community structure, and growth in Liriodendron tulipifera and Prunus serotina tree saplings. Inoculation method was an important determinant of arbuscular mycorrhizal fungi (AMF) community structure in both species and altered soil N dynamics in Prunus and soil P dynamics in Liriodendron. Prunus saplings receiving whole forest soil transfers had a higher rhizosphere soil carbon/nitrogen ratio and ammonia content at the end of the first growing season when compared to unmanipulated control saplings. Inoculation with whole forest soil transfers resulted in increased inorganic phosphorus in Liriodendron rhizosphere soils. The number of AMF terminal restriction fragments was significantly greater in rhizosphere soils of Liriodendron saplings inoculated with whole forest soil transfers and Prunus saplings receiving either inoculum source than control saplings. Forest soil inoculation also increased AMF colonization and suppressed stem elongation in Liriodendron after 16 months; conversely, Prunus AMF colonization was unchanged and stem elongation was significantly greater when saplings were inoculated with whole forest soil transfers. Longer term monitoring of tree response to inoculation will be essential to assess whether early costs of AMF colonization may provide long‐term benefits. This study provides insight into how practitioners can use microbial inoculation to alter AMF community structure and functioning, subsequently influencing tree growth and nutrient cycling during the restoration of degraded lands.     

南亚热带乡土树种人工纯林及混交林土壤微生物群落结构

以我国南亚热带格木、马尾松人工纯林及二者混交林林地土壤为对象,运用磷脂脂肪酸(PLFAs)法研究了3种人工林土壤微生物生物量和群落结构特征.结果表明: 旱季土壤微生物的PLFAs总量及各菌群的PLFAs量显著高于雨季.旱季土壤微生物的PLFAs总量、细菌PLFAs量、真菌PLFAs量、放线菌PLFAs量均为马尾松人工林最高,混交林次之,格木林最低;而雨季格木人工林土壤微生物的PLFAs总量、细菌PLFAs量、真菌PLFAs量、丛枝菌根真菌PLFAs量高于混交林,并显著高于马尾松人工林.主成分分析表明,土壤微生物群落结构组成受林分类型和季节的双重影响.冗余分析表明,土壤温湿度、pH值、全氮及铵态氮含量与特征磷脂脂肪酸之间呈显著相关关系.在全年水平上,混交林土壤真菌/细菌比值始终高于格木林和马尾松林,表明格木与马尾松混交更有利于提高土壤生态系统的稳定性.     

Effects of long-term fertilization on AM fungal community structure and Glomalin-related soil protein in the Loess Plateau of China

Arbuscular mycorrhizal fungi (AMF) are crucial for ecosystem functioning, and thus have potential use for sustainable agriculture. In this study, we investigated the impact of organic and mineral fertilizers on the AMF community composition and content of Glomalin-related soil protein (GRSP) in a field experimental station which was established in 1979, in the Loess Plateau of China. Roots and soils were sampled three times during the growing period of winter wheat in 2008. The treatments including: N (inorganic N), NP (inorganic N and P), SNP (straw, inorganic N and P), M (farmyard manure), MNP (farmyard manure, inorganic N and P), and CK (no fertilization). AMF communities of root and soil samples were analyzed using PCR-DGGE, cloning and sequencing techniques; and GRSP content was determined by Bradford assay. Our results indicated that spore density, GRSP, and AMF community varied significantly in soils of long-term fertilization plots at three different wheat growing stages. The effects of wheat growing period on AMF community in roots were much more evident than fertilization regimes. However, the diversity of AMF was low in our study field. Up to five AMF phylotypes appeared in each sample, with the overwhelming dominance of a Glomus-like phylotype affiliated to G. mosseae. GRSP content was correlated positively with organic carbon, total phosphorus, available phosphorus, soil pH, and spore densities, but correlated negatively with soil C/N (P?<?0.05). The results of our study highlight that the richness of AMF in Loess Plateau agricultural region is low, and long-term fertilization, especially amendments with manure and straw, has beneficial effects on accumulation of soil organic carbon, spore density, GRSP content, and AMF diversity. Host phenology, edaphic factors (influenced by long-term fertilization), and habitats interacted to affect the AMF community and agoecosystem functioning. Additionally, soil moisture and pH make a greater contribution than other determined soil parameters to the AMF community dynamics in such a special semi-arid agroecosystem where crops rely greatly on rainfall.     

Morpho-Typing and Molecular Diversity of Arbuscular Mycorrhizal Fungi in Sub-Tropical Soils of Coimbatore Region, Tamil Nadu, India

The diversity potential of arbuscular mycorrhizal fungi (AMF) in three different tropical soils of southern part of India was assessed by traditional morpho-typing of AMF-spores and by culture-independent nested-PCR of internal transcribed spacer region of ribosomal genes. The population diversity of AMF in soil was strongly correlated with available P₂O₅ in soil. Among the three different soils, black-cotton soil had more diversified AMF species than alluvial and red sandy soils. Pooled data of morpho-typing and sequence-driven analysis revealed that Glomus, Gigaspora, Scutellospora and Acaulospora are the AMF genera present in these soils. The diversity of AMF in soil differs with the mycorrhiza colonizing the plant roots.     

Differences in Arbuscular Mycorrhizal Fungal Community Composition in Soils of Three Land Use Types in Subtropical Hilly Area of Southern China

Land use type is key factor in restoring the degraded soils due to its impact on soil chemical properties and microbial community. In this study, the influences of land use type on arbuscular mycorrhizal fungal (AMF) community and soil chemical properties were assessed in a long-run experimental station in subtropical hilly area of southern China. Soil samples were collected from forest land, orchard and vegetable field. Soil chemical properties were analyzed, and PCR-DGGE was performed to explore the AMF community structure. Cloning and sequencing of DGGE bands were conducted to monitor AMF community composition. Results indicate that the contents of total P, available P and available K were the highest while the contents of soil organic matter, total N, total K and available N were the lowest in vegetable field soils, with forest land soils vice versa. According to DGGE profiling, AMF community in forest soils was more closely related to that in orchard soils than that in vegetable field soils. Sequencing indicated that 45 out of 53 excised bands were AMF and 64.4% of AMF belonged to Glomeraceae, including some “generalists” present in all soils and some “specialists” present only in soils of particular land use. Category principle component analysis demonstrated that total N, soil organic matter and available P were the most important factors affecting AMF community, and some AMF phylotypes were closely associated with particular soil chemical properties. Our data suggest that AMF communities are different with different land use types.     

Microbial and Geochemical Assessment of Bauxitic Un-mined and Post-mined Chronosequence Soils from Mocho Mountains, Jamaica

Microorganisms are very sensitive to environmental change and can be used to gauge anthropogenic impacts and even predict restoration success of degraded environments. Here, we report assessment of bauxite mining activities on soil biogeochemistry and microbial community structure using un-mined and three post-mined sites in Jamaica. The post-mined soils represent a chronosequence, undergoing restoration since 1987, 1997, and 2007. Soils were collected during dry and wet seasons and analyzed for pH, organic matter (OM), total carbon (TC), nitrogen (TN), and phosphorus. The microbial community structure was assessed through quantitative PCR and massively parallel bacterial ribosomal RNA (rRNA) gene sequencing. Edaphic factors and microbial community composition were analyzed using multivariate statistical approaches and revealed a significant, negative impact of mining on soil that persisted even after greater than 20?years of restoration. Seasonal fluctuations contributed to variation in measured soil properties and community composition, but they were minor in comparison to long-term effects of mining. In both seasons, post-mined soils were higher in pH but OM, TC, and TN decreased. Bacterial rRNA gene analyses demonstrated a general decrease in diversity in post-mined soils and up to a 3-log decrease in rRNA gene abundance. Community composition analyses demonstrated that bacteria from the Proteobacteria (α, β, γ, δ), Acidobacteria, and Firmicutes were abundant in all soils. The abundance of Firmicutes was elevated in newer post-mined soils relative to the un-mined soil, and this contrasted a decrease, relative to un-mined soils, in proteobacterial and acidobacterial rRNA gene abundances. Our study indicates long-lasting impacts of mining activities to soil biogeochemical and microbial properties with impending loss in soil productivity.     

Molecular biodiversity of arbuscular mycorrhizal fungi in trace metal-polluted soils

We assessed the indigenous arbuscular mycorrhizal fungi (AMF) community structure from the roots and associated soil of Plantago major (plantain) plants growing on sites polluted with trace metals (TM) and on unpolluted sites. Uncontaminated and TM-contaminated sites containing As, Cd, Cu, Pb, Sn and Zn were selected based on a survey of the TM concentration in soils of community gardens in the City of Montréal. Total genomic DNA was extracted directly from these samples. PCR followed by denaturing gradient gel electrophoresis (PCR-DGGE), augmented by cloning and sequencing, as well as direct sequencing techniques, was all used to investigate AMF community structure. We found a decreased diversity of native AMF (assessed by the number of AMF ribotypes) in soils and plant roots harvested from TM-polluted soils compared with unpolluted soils. We also found that community structure was modified by TM contamination. Various species of Glomus, Scutellospora aurigloba and S. calospora were the most abundant ribotypes detected in unpolluted soil; ribotypes of G. etunicatum, G. irregulare/G. intraradices and G. viscosum were found in both polluted and unpolluted soils, while ribotypes of G. mosseae and Glomus spp. (B9 and B13) were dominant in TM-polluted soils. The predominance of G. mosseae in metal-polluted sites suggests the tolerance of this species to TM stress, as well as its potential use for phytoremediation. These data are relevant for our understanding of how AMF microbial communities respond to natural environments that contain a broad variety of toxic inorganic compounds and will substantially expand our knowledge of AMF ecology and biodiversity.     

Influence of Long Term Irrigation with Pulp and Paper Mill Effluent on the Bacterial Community Structure and Catabolic Function in Soil

Microbial communities play a vital role in maintaining soil health. A multiphasic approach to assess the effect of pulp and paper mill effluent on both the structure and function of microbial soil communities is taken. Bacterial communities from agricultural soils irrigated with pulp and paper mill effluent were compared to communities form soils irrigated with well water. Samples were taken from fields in the state of Uttarakhand, India, where pulp and paper mill effluent has been used for irrigation for over 25 years. Comparisons of bacterial community structure were conducted using sequencing of the 16S rRNA gene from both isolates and clone libraries attained from the soil. Community-level physiological profiling was used to characterize the functional diversity and catabolic profile of the bacterial communities. The multiphasic approach using both physiological and molecular techniques proved to be a powerful tool in evaluating the soil bacterial community population and population differences therein. A significant and consistent difference in the population structure and function was found for the bacterial communities from soil irrigated with effluent in comparison to fields irrigated with well water. The diversity index parameters indicated that the microbial community in pulp and paper mill effluent irrigated fields were more diverse in both structure and function. This suggests that the pulp and paper mill effluent is not having a negative effect on the soil microbial community, but in fact may have a positive influence. In terms of soil health, this finding supports the continued use of pulp and paper mill effluent for irrigation. This is however only one aspect of soil health which was evaluated. Further studies on soil resistance and robustness could be undertaken to holistically evaluate soil health in this situation.     

Diversity of arbuscular mycorrhizal fungi in greenhouse soils continuously planted to watermelon in North China

In North China, watermelon is grown in commercial greenhouses in a continuous monoculture and with high application rates of manure or compost. The aim of this study was to determine how the diversity of arbuscular mycorrhizal fungi (AMF) in these soils changed over long periods (0 to 20 years) of monoculture. AMF in control soils (from fields not replanted with watermelon and located near the greenhouses) and in greenhouses (in Daxing, Beijing, and Weifang, Shandong) that had been continuously replanted with watermelon for 5, 10, 15, or 20 years (three greenhouses per year per location) were identified and quantified based on spore morphology and on denaturing gradient gel electrophoresis (DGGE). The total number of AMF species and genera were 13 and 3 in soils replanted for 5–20 years and 19 and 4 in control soils. AMF species richness (SR), the Shannon–Wiener index (H), and spore density declined as the number of years in which watermelon was replanted increased. The available phosphorus, potassium, and nitrogen in the soil increased as the number of years in which watermelon was replanted increased. Values for SR and H were higher when based on DGGE than on spore morphology. The results suggest that current greenhouse practices in North China reduce the AMF diversity in the soil.     

The rise and fall of arbuscular mycorrhizal fungal diversity during ecosystem retrogression

Ecosystem retrogression following long‐term pedogenesis is attributed to phosphorus (P) limitation of primary productivity. Arbuscular mycorrhizal fungi (AMF) enhance P acquisition for most terrestrial plants, but it has been suggested that this strategy becomes less effective in strongly weathered soils with extremely low P availability. Using next generation sequencing of the large subunit ribosomal RNA gene in roots and soil, we compared the composition and diversity of AMF communities in three contrasting stages of a retrogressive >2‐million‐year dune chronosequence in a global biodiversity hotspot. This chronosequence shows a ~60‐fold decline in total soil P concentration, with the oldest stage representing some of the most severely P‐impoverished soils found in any terrestrial ecosystem. The richness of AMF operational taxonomic units was low on young (1000's of years), moderately P‐rich soils, greatest on relatively old (~120 000 years) low‐P soils, and low again on the oldest (>2 000 000 years) soils that were lowest in P availability. A similar decline in AMF phylogenetic diversity on the oldest soils occurred, despite invariant host plant diversity and only small declines in host cover along the chronosequence. Differences in AMF community composition were greatest between the youngest and the two oldest soils, and this was best explained by differences in soil P concentrations. Our results point to a threshold in soil P availability during ecosystem regression below which AMF diversity declines, suggesting environmental filtering of AMF insufficiently adapted to extremely low P availability.