Ontology highlight
ABSTRACT:
PROVIDER: PRJNA1106012 | ENA |
REPOSITORIES: ENA
Dataset's files
| Action | DRS | |||
|---|---|---|---|---|
| SRR28849400_1.fastq.gz | Fastqsanger.gz | |||
| SRR28849400_2.fastq.gz | Fastqsanger.gz | |||
| SRR28849401_1.fastq.gz | Fastqsanger.gz | |||
| SRR28849401_2.fastq.gz | Fastqsanger.gz | |||
| SRR28849402_1.fastq.gz | Fastqsanger.gz |
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Project description:Permafrost soil in high latitude tundra is one of the largest terrestrial carbon (C) stocks and is highly sensitive to climate warming. Understanding microbial responses to warming induced environmental changes is critical to evaluating their influence on soil biogeochemical cycles. In this study, a functional gene array (i.e. GeoChip 4.2) was used to analyze the functional capacities of soil microbial communities collected from a naturally degrading permafrost region in Central Alaska. Varied thaw history was reported to be the main driver of soil and plant differences across a gradient of minimally, moderately and extensively thawed sites. Compared with the minimally thawed site, the number of detected functional gene probes across the 15-65 cm depth profile at the moderately and extensively thawed sites decreased by 25 % and 5 %, while the community functional gene beta-diversity increased by 34% and 45%, respectively, revealing decreased functional gene richness but increased community heterogeneity along the thaw progression. Particularly, the moderately thawed site contained microbial communities with the highest abundances of many genes involved in prokaryotic C degradation, ammonification, and nitrification processes, but lower abundances of fungal C decomposition and anaerobic-related genes. Significant correlations were observed between functional gene abundance and vascular plant primary productivity, suggesting that plant growth and species composition could be co-evolving traits together with microbial community composition. Altogether, this study reveals the complex responses of microbial functional potentials to thaw related soil and plant changes, and provides information on potential microbially mediated biogeochemical cycles in tundra ecosystems.
2019-06-03 | GSE97107 | GEO
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.
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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: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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