16S ribosomal RNA gene (rDNA) amplicon analysis remains the standard approach for the cultivation-independent investigation of microbial diversity. The accuracy of these analyses depends strongly on the choice of primers. The overall coverage and phylum spectrum of 175 primers and 512 primer pairs were evaluated in silico with respect to the SILVA 16S/18S rDNA non-redundant reference dataset (SSURef 108 NR). Based on this evaluation a selection of 'best available' primer pairs for Bacteria and Archaea for three amplicon size classes (100-400, 400-1000, ≥ 1000 bp) is provided. The most promising bacterial primer pair (S-D-Bact-0341-b-S-17/S-D-Bact-0785-a-A-21), with an amplicon size of 464 bp, was experimentally evaluated by comparing the taxonomic distribution of the 16S rDNA amplicons with 16S rDNA fragments from directly sequenced metagenomes. The results of this study may be used as a guideline for selecting primer pairs with the best overall coverage and phylum spectrum for specific applications, therefore reducing the bias in PCR-based microbial diversity studies.

Evaluation of general 16S ribosomal RNA gene PCR primers for classical and next-generation sequencing-based diversity studies

https://web.science.uu.nl/pmi/publications/PDF/2012/TiPS-Berendsen-2012.pdf

The rhizosphere microbiome and plant health

Since the 1900s, the link between soil biotic activity, soil organic matter (SOM) decomposition and stabilization, and soil aggregate dynamics has been recognized and intensively been studied. By 1950, many studies had, mostly qualitatively, investigated the influence of the five major factors (i.e. soil fauna, microorganisms, roots, inorganics and physical processes) on this link. After 1950, four theoretical mile-stones related to this subject were realized. The first one was when Emerson [Nature 183 (1959) 538] proposed a model of a soil crumb consisting of domains of oriented clay and quartz particles. Next, Edwards and Bremner [J. Soil Sci. 18 (1967) 64] formulated a theory in which the solid-phase reaction between clay minerals, polyvalent cations and SOM is the main process leading to microaggregate formation. Based on this concept, Tisdall and Oades [J. Soil Sci. 62 (1982) 141] coined the aggregate hierarchy concept describing a spatial scale dependence of mechanisms involved in micro- and macroaggregate formation. Oades [Plant Soil 76 (1984) 319] suggested a small, but very important, modification to the aggregate hierarchy concept by theorizing the formation of microaggregates within macroaggregates. Recent research on aggregate formation and SOM stabilization extensively corroborate this modification and use it as the base for furthering the understanding of SOM dynamics. The major outcomes of adopting this modification are: (1) microaggregates, rather than macroaggregates protect SOM in the long term; and (2) macroaggregate turnover is a crucial process influencing the stabilization of SOM. Reviewing the progress made over the last 50 years in this area of research reveals that still very few studies are quantitative and/or consider interactive effects between the five factors. The quantification of these relationships is clearly needed to improve our ability to predict changes in soil ecosystems due to management and global change. This quantification can greatly benefit from viewing aggregates as dynamic rather than static entities and relating aggregate measurements with 2D and 3D quantitative spatial information.

A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics

Biofilms are complex communities of microorganisms attached to surfaces or associated with interfaces. Despite the focus of modern microbiology research on pure culture, planktonic (free-swimming) bacteria, it is now widely recognized that most bacteria found in natural, clinical, and industrial settings persist in association with surfaces. Furthermore, these microbial communities are often composed of multiple species that interact with each other and their environment. The determination of biofilm architecture, particularly the spatial arrangement of microcolonies (clusters of cells) relative to one another, has profound implications for the function of these complex communities. Numerous new experimental approaches and methodologies have been developed in order to explore metabolic interactions, phylogenetic groupings, and competition among members of the biofilm. To complement this broad view of biofilm ecology, individual organisms have been studied using molecular genetics in order to identify the genes required for biofilm development and to dissect the regulatory pathways that control the plankton-to-biofilm transition. These molecular genetic studies have led to the emergence of the concept of biofilm formation as a novel system for the study of bacterial development. The recent explosion in the field of biofilm research has led to exciting progress in the development of new technologies for studying these communities, advanced our understanding of the ecological significance of surface-attached bacteria, and provided new insights into the molecular genetic basis of biofilm development.

Microbial Biofilms: from Ecology to Molecular Genetics

A global perspective on the use, sales, exposure pathways, occurrence, fate and effects of veterinary antibiotics (VAs) in the environment

Ecological considerations involved in commercial development of biological control agents for soil-borne diseases.

The population dynamics of two genetically engineered Pseudomonas fluorescens strains, D5 and C5t, introduced into a loamy sand soil, in competition with a spontaneous antibiotic-resistant mutant of the corresponding wildtype strain was studied. Strain D5 contained an insertion of transposon Tn5 in its genome, whereas strain C5t was obtained by insertion of Tn 5 :: tox , a Tn 5 -derivative containing a Bacillus thuringiensis var. morrisoni δ-endotoxin gene, into the chromosome using a suicide vector system. Southern hybridization analysis demonstrated the absence of vector sequences, and the presence of single copies of either Tn 5 or Tn 5 :: tox in the respective strains. Western blotting and a bio-assay on larvae of Anopheles stephensi suggested the tox gene was functional in clone C5t. Both D5 and C5t were prototrophic and their generation times in minimal medium were slightly below that of the corresponding wild-type strain. Tn 5 and Tn 5 :: tox were stable in both clones during growth in minimal medium for 16 generations. During growth in competition with the wild-type strain, D5 competed well, however C5t was outcompeted from 50 to below 3% of the population in 40 generations. During growth in competition in the sterile loamy sand, both strains were outcompeted by the parent strain; strain C5t was less competitive than D5. In non-sterile loamy sand, the introduced mixed populations showed a slow decline; both C5t and D5 were outcompeted by the parent strain. The decreased fitness of both modified strains, although significant, was considered to be small in ecological terms. Further, the addition of 10% bentonite clay to the loamy sand resulted in a significant enhancement of survival of the mixed populations, and a stabilization of the proportions between the modified strains and the parent. Finally, there was a trend towards a decrease in the proportion modified strain/parent strain in both mixes in the rhizosphere of wheat.

Survival of genetically engineered Pseudomonas fluorescens in soil in competition with the parent strain

The possible occurrence of bacterial matings on transconjugant-selective plates used in experiments aimed at assessing conjugal transfer in soil was investigated. Matings on transconjugant-selective plates (with rifampicin, streptomycin, tetracycline, and kanamycin) between donor and recipient cells were shown to occur depending on the number of parent cells. Temperature also influenced conjugation frequencies on agar plates, since a lower temperature resulted in a decreased number of transconjugants. The use of nalidixic acid instead of streptomycin in conjunction with rifampicin for donor counter selection inhibited conjugation on selective plates. Conjugation in soil was analyzed by plating on selective media with nalidixic acid or streptomycin. The results indicated that conjugation in bentonite- or nutrient-amended soil was readily detected; however, part of the transconjugants could be assigned to be the result of matings on the selective plates. Conjugation was also stimulated in the presence of plant roots. Colony hybridization experiments confirmed the presence of plasmid RP4 in the transconjugants.

Determination of plasmid transfer frequency in soil: Consequences of bacterial mating on selective agar media

A procedure for the metagenomics exploration of disease-suppressive soils

At two occasions (2004 and 2006), a similar cluster of culturable bacteria was found to be selected in the mycosphere of the basidiomycetous fungus Laccaria proxima (Agaricales, Tricholomataceae) in the field. The bacteria, identified as related to Variovorax paradoxus, comprised 7.3–9% of the total culturable bacterial community in the L. proxima mycosphere, but were not found in corresponding bulk soil (<0.3%). One strain, denoted HB44, was selected in order to unravel the basis of the V. paradoxus mycosphere competence in in vitro experiments with the former Laccaria laccata, which was recently reclassified as Lyophyllum sp. strain Karsten (Agaricales, Tricholomataceae). In liquid culture experiments, L. strain Karsten was shown to be an avid producer of glycerol, next to acetate and formate, which constituted the most abundant carbonaceous compounds released. Strain HB44 was able to grow avidly at the expense of the glycerol liberated by the fungus, as evidenced by proton NMR analysis of the fungal exudates in the medium before and after bacterial growth. In sterilized field soil, strain HB44 survived significantly better in the presence than in the absence of L. strain Karsten. Addition of a glycerol series to the sterilized soil (without the fungus) resulted in the persistence or growth of strain HB44, but only if the pH of this soil was previously set at 5.5. Thus, we provide evidence for the contention that tricholomataceous fungi can create specific niches in soil for the V. paradoxus-related strain HB44 and that glycerol may be a main carbon source that drives the selection of this organism.

Selection of Variovorax paradoxus-like bacteria in the mycosphere and the role of fungal-released compounds

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