Methanotrophy
Mostrando 1-8 de 8 artigos, teses e dissertações.
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1. Processo de ciclagem e emissão de gases de efeito estufa em reservatório hidrelétrico do Centro-Oeste do Brasil (Cerrado) / Cycling process and emission of effect gases greenhouse in hydroelectric reservoir of the center-West of Brazil (Cerrado)
Foi apresentado um sistema automatizado para monitorar fluxos de metano (CH4) e do dióxido de carbono (CO2) na relação da água/ar de ecossistemas aquáticos. Consiste em uma série de câmaras flutuantes dinâmicas acopladas a um analisador photo acústico infravermelho de gás. Associado os outros sensores atmosféricos e de qualidade da água, foi poss
Publicado em: 2008
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2. Difluoromethane, a New and Improved Inhibitor of Methanotrophy
Difluoromethane (HFC-32; DFM) is compared to acetylene and methyl fluoride as an inhibitor of methanotrophy in cultures and soils. DFM was found to be a reversible inhibitor of CH4 oxidation by Methylococcus capsulatus (Bath). Consumption of CH4 in soil was blocked by additions of low levels of DFM (0.03 kPa), and this inhibition was reversed by DFM removal.
American Society for Microbiology.
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3. Genomic Insights into Methanotrophy: The Complete Genome Sequence of Methylococcus capsulatus (Bath)
Methanotrophs are ubiquitous bacteria that can use the greenhouse gas methane as a sole carbon and energy source for growth, thus playing major roles in global carbon cycles, and in particular, substantially reducing emissions of biologically generated methane to the atmosphere. Despite their importance, and in contrast to organisms that play roles in other
Public Library of Science.
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4. Evaluation of Methyl Fluoride and Dimethyl Ether as Inhibitors of Aerobic Methane Oxidation
Methyl fluoride (MF) and dimethyl ether (DME) were effective inhibitors of aerobic methanotrophy in a variety of soils. MF and DME blocked consumption of CH4 as well as the oxidation of 14CH4 to 14CO2, but neither MF nor DME affected the oxidation of [14C]methanol or [14C]formate to 14CO2. Cooxidation of ethane and propane by methane-oxidizing soils was also
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5. Multiple archaeal groups mediate methane oxidation in anoxic cold seep sediments
No microorganism capable of anaerobic growth on methane as the sole carbon source has yet been cultivated. Consequently, information about these microbes has been inferred from geochemical and microbiological observations of field samples. Stable isotope analysis of lipid biomarkers and rRNA gene surveys have implicated specific microbes in the anaerobic oxi
The National Academy of Sciences.
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6. Effect of Selected Monoterpenes on Methane Oxidation, Denitrification, and Aerobic Metabolism by Bacteria in Pure Culture
Selected monoterpenes inhibited methane oxidation by methanotrophs (Methylosinus trichosporium OB3b, Methylobacter luteus), denitrification by environmental isolates, and aerobic metabolism by several heterotrophic pure cultures. Inhibition occurred to various extents and was transient. Complete inhibition of methane oxidation by Methylosinus trichosporium O
American Society for Microbiology.
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7. Microbial Diversity of Hydrothermal Sediments in the Guaymas Basin: Evidence for Anaerobic Methanotrophic Communities†
Microbial communities in hydrothermally active sediments of the Guaymas Basin (Gulf of California, Mexico) were studied by using 16S rRNA sequencing and carbon isotopic analysis of archaeal and bacterial lipids. The Guaymas sediments harbored uncultured euryarchaeota of two distinct phylogenetic lineages within the anaerobic methane oxidation 1 (ANME-1) grou
American Society for Microbiology.
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8. Atmospheric Methane Consumption by Forest Soils and Extracted Bacteria at Different pH Values
The effect of pH on atmospheric methane (CH4) consumption was studied with slurries of forest soils and with bacteria extracted from the same soils. Soil samples were collected from a mixed hardwood stand in New Hampshire, from jackpine and aspen stands at the BOREAS (Boreal Ecosystem Atmosphere Study) site near Thompson, northern Manitoba, from sites in sou
American Society for Microbiology.