Dataset Information

Cellular and extracellular proteome of the animal pathogen Corynebacterium silvaticum, a close relative of zoonotic Corynebacterium ulcerans and Corynebacterium pseudotuberculosis

ABSTRACT: A single paragraph of about 200 words maximum. For research articles, abstracts should give a pertinent overview of the work. We strongly encourage authors to use the following style of structured abstracts, but without headings: (1) Background: Place the question addressed in a broad context and highlight the purpose of the study; (2) Methods: Describe briefly the main methods or treatments applied; (3) Results: Summarize the article's main findings; and (4) Conclusions: Indicate the main conclusions or interpretations. The abstract should be an objective representation of the article, it must not contain results which are not presented and substantiated in the main text and should not exaggerate the main conclusions

INSTRUMENT(S): LTQ Orbitrap Elite

ORGANISM(S): Corynebacterium Ulcerans Bv. Belfanti

SUBMITTER: Jens Möller

LAB HEAD: Andreas Burkovski

PROVIDER: PXD020400 | Pride | 2020-08-12

REPOSITORIES: pride

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Dataset's files

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			Action	DRS
	MultiConsensussecreted_R1_R2_R3.pep.xml	Pepxml
	MultiConsensuswholecell_R1_R2_R3.pep.xml	Pepxml
	Multiconsensussecreted_R1_R2_R3.xlsx	Xlsx
	Multiconsensusshaving_R1_R2_R3.pep.xml	Pepxml
	Multiconsensusshaving_R1_R2_R3.xlsx	Xlsx

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Project description:Pelagic aggregates function as hotspots for microbial activity and biological carbon pumps for exporting OM fixed by photoautotrophs to sediments in lakes and oceans. In iron-rich (ferruginous) lakes, photoferrotrophic or chemolithoautotrophic bacteria appear to contribute to CO2 fixation by oxidizing reduced iron which leads to the formation of iron-rich pelagic aggregates called iron-snow. In acidic lakes, iron snow is colonized mainly by acidophilic iron-cycling microbes that can trigger interspecies aggregation mechanisms. However, the significance of iron oxidizers in carbon fixation, their general role in iron snow functioning, and the flow of carbon within iron snow is still unclear. Here, we combined a two-year metatranscriptome analysis with a 13CO2 metabolic labeling approach to determine general metabolic activities. Protein-based stable isotope probing (protein-SIP) was used to trace the 13CO2 incorporation in iron snow microcosms over time under both oxic and anoxic conditions. Analysis of our mRNA-derived metatranscriptome data identified four key players (Leptospirillum, Ferrovum, Acidithrix, Acidiphilium) with relative abundances (59.6%-85.7%) in iron snow encoding a variety of ecologically relevant pathways, including carbon fixation, polysaccharide biosynthesis, and flagellar-based motility. We did not detect transcriptional activity for carbon fixation from archaea or eukaryotes. The largest numbers of expressed genes (3008, 2991, 2936) matched to the genomes of our previously obtained iron snow isolates (Acidithrix sp. C25, Acidiphilium sp. C61, Acidocella sp. C78) separately. 13CO2 incorporation studies identified Leptospirillum and Ferrovum, as the main active chemolithoautotrophs under oxic conditions, and Ferrovum was the main active organism under anoxic conditions as well. Small amounts of labeled 13C (Relative isotope abundance: 1.0%-5.3%) were found in the heterotrophic Acidiphilium and Acidocella. Overall, our data show that iron oxidizers play an important role in the formation of iron minerals and CO2 fixation, but the majority of fixed C apparently did not reach other iron snow microbes. This finding suggests that most of the fixed C will be directly exported to the sediment without feeding heterotrophs in the water column in acidic ferruginous lakes.

Dataset Information

Cellular and extracellular proteome of the animal pathogen Corynebacterium silvaticum, a close relative of zoonotic Corynebacterium ulcerans and Corynebacterium pseudotuberculosis

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