29 research outputs found

    Genomes of two new ammonia-oxidizing archaea enriched from deep marine sediments.

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    Ammonia-oxidizing archaea (AOA) are ubiquitous and abundant and contribute significantly to the carbon and nitrogen cycles in the ocean. In this study, we assembled AOA draft genomes from two deep marine sediments from Donghae, South Korea, and Svalbard, Arctic region, by sequencing the enriched metagenomes. Three major microorganism clusters belonging to Thaumarchaeota, Epsilonproteobacteria, and Gammaproteobacteria were deduced from their 16S rRNA genes, GC contents, and oligonucleotide frequencies. Three archaeal genomes were identified, two of which were distinct and were designated Ca. "Nitrosopumilus koreensis" AR1 and "Nitrosopumilus sediminis" AR2. AR1 and AR2 exhibited average nucleotide identities of 85.2% and 79.5% to N. maritimus, respectively. The AR1 and AR2 genomes contained genes pertaining to energy metabolism and carbon fixation as conserved in other AOA, but, conversely, had fewer heme-containing proteins and more copper-containing proteins than other AOA. Most of the distinctive AR1 and AR2 genes were located in genomic islands (GIs) that were not present in other AOA genomes or in a reference water-column metagenome from the Sargasso Sea. A putative gene cluster involved in urea utilization was found in the AR2 genome, but not the AR1 genome, suggesting niche specialization in marine AOA. Co-cultured bacterial genome analysis suggested that bacterial sulfur and nitrogen metabolism could be involved in interactions with AOA. Our results provide fundamental information concerning the metabolic potential of deep marine sedimentary AOA

    Depot-Specific Changes in Fat Metabolism with Aging in a Type 2 Diabetic Animal Model - Fig 1

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    <p><b>The effect of aging on the weight of subcutaneous fat/visceral fat ratio (A), OGTT (B), AUC during OGTT (C), adipocyte size distribution of subcutaneous fat (D) and visceral fat (E), and PPARγ2 mRNA levels (F).</b> (*<i>P</i> <0.05 vs. the same deposit in the untreated OLETF rats, <sup>†</sup><i>P</i><0.05 vs. subcutaneous fat in the same group.)</p

    The effects of aging on the genes involved in fatty acid oxidation and energy expenditure.

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    <p>The effects of aging on the gene expression were analyzed by 2-way ANOVA (*<i>P</i> <0.05 vs. OLETF rats at 21 weeks of age). The effects of rosiglitazone on the metabolic genes in each fat depot were evaluated among the different groups at 21 weeks (†<i>P</i> <0.05 vs. the same deposit in OLETF rats at 21 weeks; RGZ, rosiglitazone treated).</p

    The effects of aging on the genes involved in glycerol and fatty acid recycling.

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    <p>The effects of aging on the gene expression were analyzed by 2-way ANOVA (*<i>P</i> <0.05 vs. OLETF rats at 21 weeks of age). The effects of rosiglitazone on the metabolic genes in each fat depot were evaluated among the different groups at 21 weeks (†<i>P</i> <0.05 vs. the same deposit in OLETF rats at 21 weeks; RGZ, rosiglitazone treated).</p

    The effects of aging on the genes involved in adipose fatty acid uptake, esterification and triacylglycerol synthesis.

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    <p>The effects of aging on the gene expression were analyzed by 2-way ANOVA (*<i>P</i> <0.05 vs. OLETF rats at 21 weeks of age). The effects of rosiglitazone on the metabolic genes in each fat depot were evaluated among the different groups at 21 weeks (†<i>P</i> <0.05 vs. the same deposit in OLETF rats at 21 weeks; RGZ, rosiglitazone treated).</p

    Genomic and metatranscriptomic analyses of carbon remineralization in an Antarctic polynya

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    Abstract Background Polynyas in the Southern Ocean are regions of intense primary production, mainly by Phaeocystis antarctica. Carbon fixed by phytoplankton in the water column is transferred to higher trophic levels, and finally, to the deep ocean. However, in the Amundsen Sea, most of this organic carbon does not reach the sediment but is degraded in the water column due to high bacterial heterotrophic activity. Results We reconstructed 12 key bacterial genomes from different phases of bloom and analyzed the expression of genes involved in organic carbon remineralization. A high correlation of gene expression between the peak and decline phases was observed in an individual genome bin-based pairwise comparison of gene expression. Polaribacter belonging to Bacteroidetes was found to be dominant in the peak phase, and its transcriptional activity was high (48.9% of the total mRNA reads). Two dominant Polaribacter bins had the potential to utilize major polymers in P. antarctica, chrysolaminarin and xylan, with a distinct set of glycosyl hydrolases. In the decline phase, Gammaproteobacteria (Ant4D3, SUP05, and SAR92), with the potential to utilize low molecular weight-dissolved organic matter (LMW-DOM) including compatible solutes, was increased. The versatility of Gammaproteobacteria may contribute to their abundance in organic carbon-rich polynya waters, while the SAR11 clade was found to be predominant in the sea ice-covered oligotrophic ocean. SAR92 clade showed transcriptional activity for utilization of both polysaccharides and LMW-DOM; this may account for their abundance both in the peak and decline phases. Ant4D3 clade was dominant in all phases of the polynya bloom, implicating the crucial roles of this clade in LMW-DOM remineralization in the Antarctic polynyas. Conclusions Genomic reconstruction and in situ gene expression analyses revealed the unique metabolic potential of dominant bacteria of the Antarctic polynya at a finer taxonomic level. The information can be used to predict temporal community succession linked to the availability of substrates derived from the P. antarctica bloom. Global warming has resulted in compositional changes in phytoplankton from P. antarctica to diatoms, and thus, repeated parallel studies in various polynyas are required to predict global warming-related changes in carbon remineralization
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