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Isoprene monooxygenase (IsoMO, encoded by ) initiates the oxidation of the climate-active gas isoprene, with the genes and nearly always found adjacent to in extant and metagenome-derived isoprene degraders. The roles of and are uncertain, although each is essential to isoprene degradation. We report here the characterization of these proteins from two model isoprene degraders, sp. strain AD45 and sp. strain WS11. The genes and from and from were expressed individually in Escherichia coli as maltose binding protein fusions to overcome issues of insolubility. The activity of two glutathione -transferases from , IsoI and IsoJ was assessed with model substrates, and the conversion of epoxyisoprene to the intermediate 1-hydroxy-2-glutathionyl-2-methyl-3-butene (HGMB) was demonstrated. The next step of the isoprene metabolic pathway of is catalyzed by the dehydrogenase IsoH, resulting in the conversion of HGMB to 2-glutathionyl-2-methyl-3-butenoic acid (GMBA). The aldehyde dehydrogenases (AldH) from and were examined with a variety of aldehydes, with both exhibiting maximum activity with butanal. AldH significantly increased the rate of production of NADH when added to the IsoH-catalyzed conversion of HGMB to GMBA (via GMB), suggesting a synergistic role for AldH in the isoprene metabolic pathway. An analysis of IsoG revealed that this protein, which is essential for isoprene metabolism in , is an enzyme of the formyl CoA-transferase family and is predicted to catalyze the formation of a GMBA-CoA thioester as an intermediate in the isoprene oxidation pathway. Isoprene is a climate-active gas, largely produced by trees, which is released from the biosphere in amounts equivalent to those of methane and all other volatile organic compounds combined. Bacteria found in many environments, including soils and on the surface of leaves of isoprene-producing trees, can grow on isoprene and thus may represent a significant biological sink for this globally significant volatile compound and remove isoprene before it escapes to the atmosphere, thus reducing its potency as a climate-active gas. The initial oxidation of isoprene by bacteria is mediated by isoprene monooxygenase encoded by the genes . In isoprene-degrading bacteria, a second gene cluster, , is also present, although the exact role in isoprene degradation by the proteins encoded by these genes is uncertain. This investigation sheds new light on the roles of these proteins in the isoprene oxidation pathway in two model isoprene-degrading bacteria of the genera and
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http://dx.doi.org/10.1128/aem.02122-22 | DOI Listing |
Mar Environ Res
September 2025
Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266237, China; Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education,
Simultaneous measurements of dimethylsulfide (DMS) and isoprene in seawater and the overlying atmosphere were conducted in the tropical western Pacific Ocean during February-March 2017. Surface seawater exhibited a strong correlation between DMS and dimethylsulfoniopropionate (DMSP), with similar spatial distributions, whereas dimethylsulfoxide (DMSO) displayed an opposing trend. Latitudinal and vertical profiles of DMS, DMSP, and isoprene revealed their pronounced dependence on biological factors, particularly in subsurface layers.
View Article and Find Full Text PDFJ Phys Chem A
September 2025
School of Environmental Engineering, Henan University of Technology, Zhengzhou, Henan 450001, China.
Hydroxymethyl-methyl-α-lactone (HMML) is a key epoxide precursor in forming tracer compounds 2-methylglyceric acid (2-MG) or 2-methylglyceric acid sulfate (2-MGOS) from isoprene under high-NOx conditions. Despite its importance, the formation and transformation of HMML─particularly under acidic aerosol conditions─are still poorly understood, limiting comprehensive knowledge of secondary organic aerosol (SOA) formation. In this study, quantum chemical calculations, Born-Oppenheimer molecular dynamics (BOMD), and metadynamics (MTD) simulations are employed to investigate both the formation of HMML from methacryloyl peroxynitrate (MPAN) and its interfacial transformation mechanisms on sulfuric acid aerosols.
View Article and Find Full Text PDFJ Phys Chem B
September 2025
Department of Chemical and Biological Engineering, Princeton University, Princeton, New Jersey 08544, United States.
Control of the glass transition temperature () is a major goal in polymer engineering as is a key determinant of mechanical behavior, barrier properties, and material processability. In copolymers of nonpolar monomers, the Fox equation can provide an approximate description of the dependence of on copolymer composition (monomer ratio), based on a harmonic weighted average of values for the individual homopolymers. However, the Fox equation does not consider the influence of intermonomer interactions, nor does it account for self-concentration effects.
View Article and Find Full Text PDFJ Hazard Mater
September 2025
State Key Laboratory of Advanced Environmental Technology, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; Fujian Key Laboratory of Atmospheric Ozone Pollution Prevention, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China. Electronic
Surface ozone (O) pollution has emerged as a regional environmental issue. Photochemical reactive species significantly impact O photochemical formation by regulating radicals and atmospheric oxidation capacity. This study focuses on O pollution in a southeastern coastal city, utilizing coordinated methods of filed observations and Photochemical Box Model to explore the pollution mechanisms and sensitivity analyses of typical reactive species (PAN, HCHO, and isoprene).
View Article and Find Full Text PDFPNAS Nexus
September 2025
Department of Chemical Engineering, Columbia University, New York, NY 10027, USA.
The atmospheric chemistry of volatile organic compounds (VOC) has a major influence on atmospheric pollutants and particle formation. Accurate modeling of this chemistry is essential for air quality models. Complete representations of VOC oxidation chemistry are far too large for spatiotemporal simulations of the atmosphere, necessitating reduced mechanisms.
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