65 research outputs found

    Stable Carbon Isotope Signature of Methane Released From Phytoplankton

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    Unidad de excelencia MarĂ­a de Maeztu CEX2019-000940-MAquatic ecosystems play an important role in global methane cycling and many field studies have reported methane supersaturation in the oxic surface mixed layer (SML) of the ocean and in the epilimnion of lakes. The origin of methane formed under oxic condition is hotly debated and several pathways have recently been offered to explain the "methane paradox." In this context, stable isotope measurements have been applied to constrain methane sources in supersaturated oxygenated waters. Here we present stable carbon isotope signatures for six widespread marine phytoplankton species, three haptophyte algae and three cyanobacteria, incubated under laboratory conditions. The observed isotopic patterns implicate that methane formed by phytoplankton might be clearly distinguished from methane produced by methanogenic archaea. Comparing results from phytoplankton experiments with isotopic data from field measurements, suggests that algal and cyanobacterial populations may contribute substantially to methane formationobserved in the SML of oceans and lakes

    Hydrogen and carbon isotope fractionation during degradation of chloromethane by methylotrophic bacteria

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    Chloromethane (CH3Cl) is a widely studied volatile halocarbon involved in the destruction of ozone in the stratosphere. Nevertheless, its global budget still remains debated. Stable isotope analysis is a powerful tool to constrain fluxes of chloromethane between various environmental compartments which involve a multiplicity of sources and sinks, and both biotic and abiotic processes. In this study, we measured hydrogen and carbon isotope fractionation of the remaining untransformed chloromethane following its degradation by methylotrophic bacterial strains Methylobacterium extorquens CM4 and Hyphomicrobium sp. MC1, which belong to different genera but both use the cmu pathway, the only pathway for bacterial degradation of chloromethane characterized so far. Hydrogen isotope fractionation for degradation of chloromethane was determined for the first time, and yielded enrichment factors (epsilon) of -29 parts per thousand and -27 parts per thousand for strains CM4 and MC1, respectively. In agreement with previous studies, enrichment in C-13 of untransformed CH3Cl was also observed, and similar isotope enrichment factors (e) of -41 parts per thousand and -38 parts per thousand were obtained for degradation of chloromethane by strains CM4 and MC1, respectively. These combined hydrogen and carbon isotopic data for bacterial degradation of chloromethane will contribute to refine models of the global atmospheric budget of chloromethane

    Investigating Cytochrome P450 specificity during glycopeptide antibiotic biosynthesis through a homologue hybridization approach

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    Cytochrome P450 enzymes perform an impressive range of oxidation reactions against diverse substrate scaffolds whilst generally maintaining a conserved tertiary structure and active site chemistry. Within secondary metabolism, P450 enzymes play widespread and important roles in performing crucial modifications of precursor molecules, with one example of the importance of such reactions being found in the biosynthesis of the glycopeptide antibiotics (GPAs). In GPA biosynthesis P450s, known as Oxy enzymes, are key players in the cyclization of the linear GPA peptide precursor, which is a process that is both essential for their antibiotic activity and is the source of the synthetic challenge of these important antibiotics. In this work, we developed chimeric P450 enzymes from GPA biosynthesis based on two homologues from different GPA biosynthesis pathways – vancomycin and teicoplanin – as an approach to explore the divergent catalytic behavior of the two parental homologues. We could generate, crystalize and explore the activity of new hybrid P450 enzymes from GPA biosynthesis and show that the unusual in vitro behavior of the vancomycin OxyB homologue does not stem from the major regions of the P450 active site, and that additional regions in and around the P450 active site must contribute to the unusual properties of this P450 enzyme. Our results further show that it is possible to successfully transplant entire regions of secondary structure between such P450s and retain P450 expression and activity, which opens the door to use such targeted approaches to generate and explore novel biosynthetic P450 enzymes

    Rapid Commun. Mass Spectrom.

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    Rapid Commun. Mass Spectrom.

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