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Beckmann, S.

Publications and source records attributed to Beckmann, S..

3 recordsLinked to original sources

Formate-driven isoprene reduction enables energetic independence in Pelotomaculum schinkii: Evidence from metatranscriptomic and functional analyses

Isoprene, a volatile hydrocarbon emitted in vast quantities by terrestrial vegetation, can serve as a terminal electron acceptor in anoxic environments. Here, we investigated the molecular and physiological basis of isoprene reduction in an anaerobic enrichment culture highly enriched in Pelotomaculum. Substrate-exclusion assays revealed that formate is indispensable for isoprene reduction: cultures lacking formate showed no isoprene reduction, whereas formate alone sustained both reduction activity and the highest enrichment of Pelotomaculum. Metatranscriptomic analyses confirmed that Pelotomaculum schinkii was the most transcriptionally active species under isoprene-amended conditions, whereas Sedimentibacter saalensis was most enriched in unamended controls. Isoprene-treated cultures exhibited strong upregulation of [NiFe]-hydrogenase maturation factors (hypA/hybF, hypB), energy-conserving complexes (ATP synthase, H /Na - translocating pyrophosphatases), and transport systems (FeoB, ModBC), consistent with a formate-driven respiratory pathway. In contrast, genes for oxidative stress and metal detoxification were enriched in controls, suggesting physiological stress in the absence of isoprene. Thermodynamic calculations further supported this mechanism, showing that formate oxidation coupled to isoprene reduction is highly favorable ({Delta}G{degrees}' {approx} -135 kJ/mol), with an energy yield far exceeding that of formate-driven hydrogen production. Together, these findings support two mechanistic models: (i) direct isoprene reduction by group 4b [NiFe]-hydrogenase or (ii) indirect reduction via hydrogen transfer to an isrA-like oxidoreductase, analogous to Acetobacterium wieringae ISORED-2. Our results demonstrate that P. schinkii, a metabolically versatile bacterium, couples formate oxidation to isoprene respiration, indicating that isoprene can serve as an alternative electron sink. This allows P. schinkii to escape obligate syntropy with methanogens and alters microbial activity and energy conservation in anoxic ecosystems.

microbiology↗

Anaerobic isoprene reduction by Pelotomaculum sp. from Eucalyptus-leaf sediments and its impacts on methanogenesis

Isoprene is a ubiquitous biogenic volatile organic compound (VOC) with atmospheric concentrations comparable to those of methane. Its high reactivity in the atmosphere significantly influences methane concentrations, contributing to adverse effects on the climate. Understanding the role of isoprene and its link to methane metabolism is crucial to addressing climate change. The fate of isoprene and its potential microbial degraders in soil, particularly in anaerobic environments, remains poorly investigated, underscoring the need for comprehensive studies. Our study provides physiological evidence for anaerobic microbial isoprene reduction and its influence on methanogenesis in Eucalyptus-leaf sediment. In our anaerobic culture-based studies, we have demonstrated that isoprene is reduced to three products, 3-methyl-1-butene, 2-methyl-1-butene, and 2-methyl-2-butene. Our findings suggest that Pelotomaculum sp. is capable of anaerobic isoprene reduction, as indicated by 16S rRNA analysis and dilution-to-extinction studies. Anaerobic microbial isoprene reduction simultaneously inhibited methane formation. Methanogenesis was completely inhibited in microcosm cultures amended solely with isoprene. In cultures supplemented with isoprene and carbon sources, only hydrogenotrophic methanogenesis was inhibited, indicating competition for hydrogen between the methanogens and isoprene degraders. Using a culture-based approach and molecular analysis, this study provides novel insights into the microbial dynamics of anaerobic isoprene reduction and the interplay between isoprene reducers and methanogens. Graphical Abstract O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=118 SRC="FIGDIR/small/706888v1_ufig1.gif" ALT="Figure 1"> View larger version (62K): org.highwire.dtl.DTLVardef@9b559corg.highwire.dtl.DTLVardef@11ab71org.highwire.dtl.DTLVardef@ec759org.highwire.dtl.DTLVardef@41db7b_HPS_FORMAT_FIGEXP M_FIG C_FIG

microbiology↗

Evidence for an expanded repertoire of electron acceptors for the anaerobic oxidation of methane in authigenic carbonates in the Atlantic and Pacific Ocean

Authigenic carbonates represent a significant microbial sink for methane, yet little is known about the microbiome responsible for the methane removal. We identify carbonate microbiomes distributed over 21 locations hosted by 7 different cold seeps in the Pacific and Atlantic Oceans by carrying out a gene-based survey using 16S rRNA- and mcrA gene sequencing coupled with metagenomic analyses. These sites were dominated by bacteria affiliated to the Firmicutes, Alpha- and Gammaproteobacteria. ANME-1 and -2 clades were abundant in the carbonates yet their typical syntrophic partners, sulfate reducing bacteria, were not significantly present. Our analysis indicated that methane oxidizers affiliated to the ANME-1 and -2 as well as to the Candidatus Methanoperedens clades, are capable of performing complete methane- and potentially short-chain alkane oxidations independently using oxidized sulfur and nitrogen compounds as terminal electron acceptors. Gammaproteobacteria are hypothetically capable of utilizing oxidized nitrogen compounds in potential syntrophy with methane oxidizing archaea. Carbonate structures represent a window for a more diverse utilization of electron acceptors for anaerobic methane oxidation along the Atlantic and Pacific Margin.

microbiology↗