Dataset Information

Anoxia in Ralstonia eutropha H16

ABSTRACT: Ralstonia eutropha H16 is a denitrifying microorganism able to use nitrate and nitrite as terminal electron acceptors under oxygen deprivation. To identify proteins showing an altered expression pattern in response to oxygen supply, R. eutropha cells grown aerobically and anaerobically were compared in a comprehensive proteome and transcriptome approach. Nearly 700 proteins involved in several processes including respiration, cell appendages formation, DNA and cofactor biosynthesis were found to be differentially expressed. A combination of 1D-gel-LC and conventional 2D-gel analysis of six consecutive sample points covering the entire denitrification sequence revealed a detailed view on the abundance pattern of the key proteins of denitrification. Denitrification- or anaerobiosis-induced alterations of the respiratory chain included a distinct expression pattern for multiple terminal oxidases. Alterations of the central metabolism were restricted to a few key functions including the isoenzymes for aconitase and isocitrate dehydrogenase, respectively. Although R. eutropha is a strictly respiratory bacterium, the abundance of certain fermentation enzymes was increased. This work represents a comprehensive survey of denitrification on proteomic and transcriptomic level and provides unique insight into how R. eutropha adapts its metabolism to low oxygen conditions.

INSTRUMENT(S): LTQ Orbitrap

ORGANISM(S): Cupriavidus Necator (strain Atcc 17699 / H16 / Dsm 428 / Stanier 337) (ralstonia Eutropha)

SUBMITTER: Andreas Otto

LAB HEAD: Andreas Otto

PROVIDER: PXD000888 | Pride | 2014-09-01

REPOSITORIES: Pride

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Coping with anoxia: a comprehensive proteomic and transcriptomic survey of denitrification.

Kohlmann Yvonne Y Pohlmann Anne A Schwartz Edward E Zühlke Daniela D Otto Andreas A Albrecht Dirk D Grimmler Christina C Ehrenreich Armin A Voigt Birgit B Becher Dörte D Hecker Michael M Friedrich Bärbel B Cramm Rainer R

Journal of proteome research 20140908 10

Ralstonia eutropha H16 is a denitrifying microorganism able to use nitrate and nitrite as terminal electron acceptors under oxygen deprivation. To identify proteins showing an altered expression pattern in response to oxygen supply, R. eutropha cells grown aerobically and anaerobically were compared in a comprehensive proteome and transcriptome approach. Nearly 700 proteins involved in several processes including respiration, formation of cell appendages, and DNA and cofactor biosynthesis were f ...[more]

PMID: 25198380

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Project description:Oxygen deficient zones (ODZs) are major sites of net natural oceanic nitrous oxide (N2O) production and emissions. In order to understand changes in the magnitude of N2O production in response to global change, knowledge on the individual contributions of the major microbial pathways (nitrification and denitrification) to N2O production and their regulation is needed. In the ODZ of the coastal area off Peru, the sensitivity of N2O production to oxygen and organic matter was investigated using 15N-tracer experiments in combination with qPCR and microarray analysis of total and active functional genes targeting archaeal amoA and nirS as marker genes for nitrification and denitrification, respectively. Denitrification was responsible for the highest N2O production with mean 8.7 nmol L-1 d-1 but up to 118 Â± 27.8 nmol L-1 d-1 just below the oxic-anoxic interface. Highest N2O production from AO of 0.16 Â± 0.003 nmol L-1 d-1 occurred in the upper oxycline at O2 concentrations of 10 - 30 Âµmol L-1 which coincided with highest archaeal amoA transcripts/genes. Oxygen responses of N2O production varied with substrate, but production and yields were generally highest below 10 Âµmol L-1 O2. Particulate organic matter additions increased N2O production by denitrification up to 5-fold suggesting increased N2O production during times of high particulate organic matter export. High N2O yields from ammonium oxidation of 2.1% were measured, but the overall contribution to N2O production stays an order of magnitude behind denitrification as an N2O source. Hence, these findings show that denitrification is the most important N2O production process in low oxygen conditions fueled by organic carbon supply which implies a positive feedback of the total oceanic N2O sources in response to increasing oceanic deoxygenation. [SUBMITTER_CITATION]: Frey, C., Bange, H. W., Achterberg, E. P., Jayakumar, A., Löscher, C. R., Arévalo-Martínez, D. L., León-Palmero, E., Sun, M., Sun, X., Xie, R. C., Oleynik, S., and Ward, B. B.: Regulation of nitrous oxide production in low-oxygen waters off the coast of Peru, Biogeosciences, 17, 2263-2287

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