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The utilization of methane, a potent greenhouse gas, is an important component of local and global carbon cycles that is characterized by tight linkages between methane-utilizing (methanotrophic) and nonmethanotrophic bacteria. It has been suggested that the methanotroph sustains these nonmethanotrophs by cross-feeding, because subsequent products of the methane oxidation pathway, such as methanol, represent alternative carbon sources. We established cocultures in a microcosm model system to determine the mechanism and substrate that underlay the observed cross-feeding in the environment. Lanthanum, a rare earth element, was applied because of its increasing importance in methylotrophy. We used co-occurring strains isolated from Lake Washington sediment that are involved in methane utilization: a methanotroph and two nonmethanotrophic methylotrophs. Gene-expression profiles and mutant analyses suggest that methanol is the dominant carbon and energy source the methanotroph provides to support growth of the nonmethanotrophs. However, in the presence of the nonmethanotroph, gene expression of the dominant methanol dehydrogenase (MDH) shifts from the lanthanide-dependent MDH (XoxF)-type, to the calcium-dependent MDH (MxaF)-type. Correspondingly, methanol is released into the medium only when the methanotroph expresses the MxaF-type MDH. These results suggest a cross-feeding mechanism in which the nonmethanotrophic partner induces a change in expression of methanotroph MDHs, resulting in release of methanol for its growth. This partner-induced change in gene expression that benefits the partner is a paradigm for microbial interactions that cannot be observed in studies of pure cultures, underscoring the importance of synthetic microbial community approaches to understand environmental microbiomes. M icrobial communities and their members are part of every ecosystem and drive important biogeochemical processes on Earth (1). They typically comprise a range of phylogenetically and functionally diverse microbes (2) that are structured by biotic and abiotic factors (3) and are entangled through specific interactions in complex networks (4).The significance of microbial communities in diverse ecosystems including the human body is now widely accepted in science and has led to a range of initiatives focused on the world's microbiomes (5, 6). One important goal within these efforts is to understand how microbes interact with each other and the consequences of such interactions at the level of their transcriptomes, proteomes, and metabolomes. For instance, it has been demonstrated that the metabolism of yeast can be transformed by bacteria-induced prions to decrease the release of inhibiting ethanol (7). In another study, an oral biofilm of the genus Streptococcus displayed different transcriptional responses toward the presence of other species in mixed-species cultures (8).Measuring interactions in complex environmental communities is still a difficult task. Laboratory cocultures represent a simplified approach to assessing...
The utilization of methane, a potent greenhouse gas, is an important component of local and global carbon cycles that is characterized by tight linkages between methane-utilizing (methanotrophic) and nonmethanotrophic bacteria. It has been suggested that the methanotroph sustains these nonmethanotrophs by cross-feeding, because subsequent products of the methane oxidation pathway, such as methanol, represent alternative carbon sources. We established cocultures in a microcosm model system to determine the mechanism and substrate that underlay the observed cross-feeding in the environment. Lanthanum, a rare earth element, was applied because of its increasing importance in methylotrophy. We used co-occurring strains isolated from Lake Washington sediment that are involved in methane utilization: a methanotroph and two nonmethanotrophic methylotrophs. Gene-expression profiles and mutant analyses suggest that methanol is the dominant carbon and energy source the methanotroph provides to support growth of the nonmethanotrophs. However, in the presence of the nonmethanotroph, gene expression of the dominant methanol dehydrogenase (MDH) shifts from the lanthanide-dependent MDH (XoxF)-type, to the calcium-dependent MDH (MxaF)-type. Correspondingly, methanol is released into the medium only when the methanotroph expresses the MxaF-type MDH. These results suggest a cross-feeding mechanism in which the nonmethanotrophic partner induces a change in expression of methanotroph MDHs, resulting in release of methanol for its growth. This partner-induced change in gene expression that benefits the partner is a paradigm for microbial interactions that cannot be observed in studies of pure cultures, underscoring the importance of synthetic microbial community approaches to understand environmental microbiomes. M icrobial communities and their members are part of every ecosystem and drive important biogeochemical processes on Earth (1). They typically comprise a range of phylogenetically and functionally diverse microbes (2) that are structured by biotic and abiotic factors (3) and are entangled through specific interactions in complex networks (4).The significance of microbial communities in diverse ecosystems including the human body is now widely accepted in science and has led to a range of initiatives focused on the world's microbiomes (5, 6). One important goal within these efforts is to understand how microbes interact with each other and the consequences of such interactions at the level of their transcriptomes, proteomes, and metabolomes. For instance, it has been demonstrated that the metabolism of yeast can be transformed by bacteria-induced prions to decrease the release of inhibiting ethanol (7). In another study, an oral biofilm of the genus Streptococcus displayed different transcriptional responses toward the presence of other species in mixed-species cultures (8).Measuring interactions in complex environmental communities is still a difficult task. Laboratory cocultures represent a simplified approach to assessing...
Me.hy.lo.bac'ter. N.L. neut. n. methylum the methyl radical; N.L. masc. n. bacter rod; N.L. masc. n. Methylobacter methyl rod. Proteobacteria / Gammaproteobacteria / Methylococcales / Methylococcaceae / Methylobacter Cells are rods, spherical, or elliptical , 0.8–1.5 × 1.2–3.0 µm. Occur singly, in pairs, and in chains. Gram‐negative . The cells are usually motile. Some strains might form a cyst‐like resting stage , which usually confers desiccation resistance . Obligate utilizers of methane for carbon and energy . Require oxygen for methane oxidation. Oxidase and catalase positive. Neutrophilic , optimum pH is observed between 6.5 and 7.5. Majority of species are mesophilic, with optimal growth between 23 and 35°C. Some representatives are psychrotolerant and psychrophilic. Two species require sodium ions for growth. Their fatty acid composition depends on growth conditions (salinity, pH, and temperature). In nonhalophilic strains and halophilic strains grown at low salinity, pH 6.8–7.2 and 30°C, the main fatty acid is C 16:1 ω7 c . Ubiquinone‐8 (Q‐8) is the predominant lipoquinone. The genome sizes vary slightly ranging between 4.7 and 5.3 Mb. Methylobacter strains are typical inhabitants of freshwater and saline lake sediments, river and wetland muds, activated sludge, arctic and tundra soils, wastewater, and oceanic water. DNA G + C content (mol%) : 49–52. Type species : Methylobacter luteus (Romanovskaya, Malashenko and Bogachenko 1981) Bowman, Sly, Nichols and Hayward 1993, 749 VP ( Methylococcus luteus Romanovskaya, Malashenko and Bogachenko 1981, 382; Effective publication: Romanovskaya, Malashenko and Bogachenko 1978, 124).
Me.thy.lo.mi.cro' bi.um. N.L. pref. methylo ‐ pertaining to the methyl radical; Gr. adj. micros small; Gr. n. bios life; M.L. n. Methylomicrobium a small organism able to utilize methyl units. Proteobacteria / Gammaproteobacteria / Methylococcales / Methylococcaceae / Methylomicrobium Cells are short rods, 0.5–1.5 µm × 1.5–3.0 µm. Motile, monotrichous, or peritrichous. Reproduce by binary fission. Lack cysts or other differentiated resting stages. Cells form intracytoplasmic membranes as stacks of vesicular disks . Cells may possess a thin slime capsule and form regular glycoprotein S‐layers arranged in p2 , p4 , or p6 symmetries. Aerobic , can grow at low‐oxygen tension and display fermentation and denitrification capabilities . Some species can oxidize ammonium and inorganic and organic sulfur compounds as additional sources of energy. Obligate methanotrophs utilizing methane or methanol as the carbon and energy sources but not other C 1 and C n compounds. Assimilate formaldehyde via the ribulose monophosphate pathway , and all strains have a partial serine cycle . Utilize nitrate and ammonium salts as nitrogen sources. Some species can use urea, methylamine, and amino acids as nitrogen sources. Mostly mesophilic , with optimal growth at 25–35°C. Some strains are alkalitolerant or alkaliphilic, growing well in the pH range between 9 and 10.5, and require sodium ions for growth. Possess a particulate methane monooxygenase (MMO), and some strains may also contain a soluble MMO. The most abundant fatty acids are C 16:1 ω 7 c , C 16:1 , C 16:0 , C 14:0 , and C 16:1 ω 8 c . Ubiquinone‐8 (Q‐8) is the predominant quinone. Isolated from sediments of freshwater lakes and rivers, saline soda lakes, wetland muds, agricultural and swampy soils, upper mixing layers of oceans, and estuarine waters. Belongs to the Gammaproteobacteria, order Methylococcales , family Methylococcaceae . DNA G + C content (mol%) : 46–51. Type species : Methylomicrobium agile (Bowman, Sly, Nichols and Hayward 1993) Bowman, Sly and Stackebrandt 1995, 183 VP ( Methylobacter agilis Bowman, Sly, Nichols and Hayward 1993, 749.).
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