Ontology highlight
ABSTRACT:
PROVIDER: PRJNA1109761 | ENA |
REPOSITORIES: ENA
Dataset's files
| Action | DRS | |||
|---|---|---|---|---|
| Other | ||||
| SRR28978900_1.fastq.gz | Fastqsanger.gz | |||
| SRR28978900_2.fastq.gz | Fastqsanger.gz | |||
| SRR28978901_1.fastq.gz | Fastqsanger.gz | |||
| SRR28978901_2.fastq.gz | Fastqsanger.gz |
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Project description:The melting of permafrost and its potential impact on greenhouse gas emissions is a major concern in the context of global warming. The fate of the carbon trapped in permafrost will largely depend on soil physico-chemical characteristics, among which are the quality and quantity of organic matter, pH and water content, and on microbial community composition. In this study, we used microarrays and real-time PCR (qPCR) targeting 16S rRNA genes to characterize the bacterial communities in three different soil types representative of various Arctic settings. The microbiological data were linked to soil physico-chemical characteristics and CO2 production rates. Microarray results indicated that soil characteristics, and especially the soil pH, were important parameters in structuring the bacterial communities at the genera/species levels. Shifts in community structure were also visible at the phyla/class levels, with the soil CO2 production rate being positively correlated to the relative abundance of the Alphaproteobacteria, Bacteroidetes, and Betaproteobacteria. These results indicate that CO2 production in Arctic soils does not only depend on the environmental conditions, but also on the presence of specific groups of bacteria that have the capacity to actively degrade soil carbon.
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Project description:Anthropogenic activities have dramatically increased the inputs of reactive nitrogen (N) into terrestrial ecosystems, with potentially important effects on the soil microbial community and consequently soil C and N dynamics. Our analysis of microbial communities in soils subjected to 14 years of 7 g N m-2 year-1 Ca(NO3)2 amendment in a Californian grassland showed that the taxonomic composition of bacterial communities, examined by 16S rRNA gene amplicon sequencing, was significantly altered by nitrate amendment, supporting the hypothesis that N amendment- induced increased nutrient availability, yielded more fast-growing bacterial taxa while reduced slow-growing bacterial taxa. Nitrate amendment significantly increased genes associated with labile C degradation (e.g. amyA and xylA) but had no effect or decreased the relative abundances of genes associated with degradation of more recalcitrant C (e.g. mannanase and chitinase), as shown by data from GeoChip targeting a wide variety of functional genes. The abundances of most N cycling genes remained unchanged or decreased except for increases in both the nifH gene (associated with N fixation), and the amoA gene (associated with nitrification) concurrent with increases of ammonia-oxidizing bacteria. Based on those observations, we propose a conceptual model to illustrate how changes of functional microbial communities may correspond to soil C and N accumulation.
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Project description:The melting of permafrost and its potential impact on greenhouse gas emissions is a major concern in the context of global warming. The fate of the carbon trapped in permafrost will largely depend on soil physico-chemical characteristics, among which are the quality and quantity of organic matter, pH and water content, and on microbial community composition. In this study, we used microarrays and real-time PCR (qPCR) targeting 16S rRNA genes to characterize the bacterial communities in three different soil types representative of various Arctic settings. The microbiological data were linked to soil physico-chemical characteristics and CO2 production rates. Microarray results indicated that soil characteristics, and especially the soil pH, were important parameters in structuring the bacterial communities at the genera/species levels. Shifts in community structure were also visible at the phyla/class levels, with the soil CO2 production rate being positively correlated to the relative abundance of the Alphaproteobacteria, Bacteroidetes, and Betaproteobacteria. These results indicate that CO2 production in Arctic soils does not only depend on the environmental conditions, but also on the presence of specific groups of bacteria that have the capacity to actively degrade soil carbon. Three different soil types from the Canadian high Arctic were sampled at two depths within the active layer of soil and at two sampling dates (winter and summer conditions), for a total of 20 samples.
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Project description:Transcroptomic analysis of the cells grown on pyruvate in the sterilized soil and those grown on pyruvate to mid-exponenyial phase in a liquid medium
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Project description:Transcriptomic analysis of the cells grown on biphenyl in the sterilized soil and those grown on biphenyl to mid-exponential phase in a liquid medium
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Project description:Plant growth and development depends on the availability of nutrients and water resources in the soil. The increased frequencies of drought events over recent years have affected nutrient availability soil systems. Crops reutilising winter cover crop root channels allows access to resources from distal regions in the soil horizon. However, the availability of information regarding root channel reutilisation under drought, specifically bacterial community structures and functions is unknown. In this study, we observed the changes inflicted by drought on bacterial communities in maize (Zea mays L.) rhizospheres after reusing the winter cover crop root channels. The techniques of 16S rRNA (ribosomal ribonucleic acid) gene-based microbial profiling and metaproteomics were used to study the alterations in biochemical pathways of those communities under drought at three different locations (Hohenschulen, Karkendamm and Reinshof) comprising three different soli types (Luvisol, Podzol and Phaeozem) respectively. Besides the influence of soil properties, we noticed that under drought the relative abundances of Acidobacteriota, Actinomycetota, Planctomycetota, and Pseudomonadota increased, while Chloroflexota, Methylomirabilota, Patescibacterota, and Verrucomicrobiota decreased. At drought-prone soil types Luvisol and Podzol, aerobic communities Pseudomonadota and Verrucomicrobiota increased abundance of the glyoxylate cycle as a means of conserving carbon and energy for plausible survival measures. Higher abundance of catalase-glutathione peroxidase (CAT-PER) through the methionine cycle-transsulfuration pathway possibly alleviate reactive oxygen species (ROS) levels. Overall, bacterial communities in the reused cover crop root channels respond to drought by taking mitigative measures for survival.
2025-09-22 | PXD062138 | Pride