FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2108664477> ?p ?o ?g. }

• W2108664477 endingPage "1752" @default.
• W2108664477 startingPage "1739" @default.
• W2108664477 abstract "Carbon isotope fractionation factors reported for aerobic bacterial oxidation of CH4 (αCH4–CO2) range from 1.003 to 1.039. In a series of experiments designed to monitor changes in the carbon isotopic fractionation of CH4 by Type I and Type II methanotrophic bacteria, we found that the magnitude of fractionation was largely due to the first oxidation step catalyzed by methane monooxygenase (MMO). The most important factor that modulates the (αCH4–CH3OH) is the fraction of the total CH4 oxidized per unit time, which strongly correlates to the cell density of the growth cultures under constant flow conditions. At cell densities of less than 0.1 g/L, fractionation factors greater than 1.03 were observed, whereas at cell densities greater than 0.5 g/L the fractionation factors decreased to as low as 1.002. At low cell densities, low concentrations of MMO limit the amount of CH4 oxidized, while at higher cell densities, the overall rates of CH4 oxidation increase sufficiently that diffusion of CH4 from the gaseous to dissolved state and into the cells is likely the rate-determining step. Thus, the residual CH4 is more fractionated at low cell densities, when only a small fraction of the total CH4 has been oxidized, than at high cell densities, when up to 40% of the influent CH4 has been utilized. Therefore, since Rayleigh distillation behavior is not observed, δ13C values of the residual CH4 cannot be used to infer the amount oxidized in either laboratory or field-studies. The measured (αCH4–CH3OH) was the same for both Type I and Type II methanotrophs expressing particulate or soluble MMO. However, large differences in the δ13C values of biomass produced by the two types of methanotrophs were observed. Methylosinus trichosporium OB3b (Type II) produced biomass with δ13C values about 15‰ higher than the dissimilated CO2, whereas Methylomonas methanica (Type I) produced biomass with δ13C values only about 6‰ higher than the CO2. These effects were independent of the magnitude of the initial carbon isotope fractionation caused by MMO and were relatively constant despite changing ratios of assimilatory to dissimilatory carbon transformation by the organisms. This suggests that the difference in biomass carbon isotopes is primarily due to differences in the fractionation effect at the formaldehyde branch point in the metabolic pathway, rather than assimilation of CO2 by Type II methanotrophs." @default.
• W2108664477 created "2016-06-24" @default.
• W2108664477 creator A5007844044 @default.
• W2108664477 creator A5011049483 @default.
• W2108664477 creator A5011271995 @default.
• W2108664477 creator A5088647308 @default.
• W2108664477 date "2006-04-01" @default.
• W2108664477 modified "2023-10-03" @default.
• W2108664477 title "Variable carbon isotope fractionation expressed by aerobic CH4-oxidizing bacteria" @default.
• W2108664477 cites W1511393030 @default.
• W2108664477 cites W1556665743 @default.
• W2108664477 cites W1896155985 @default.
• W2108664477 cites W1963905994 @default.
• W2108664477 cites W1964280895 @default.
• W2108664477 cites W1968670244 @default.
• W2108664477 cites W1978326108 @default.
• W2108664477 cites W1980303658 @default.
• W2108664477 cites W1981732120 @default.
• W2108664477 cites W1989034393 @default.
• W2108664477 cites W1992435406 @default.
• W2108664477 cites W1995847793 @default.
• W2108664477 cites W1996868147 @default.
• W2108664477 cites W1998474911 @default.
• W2108664477 cites W1999676643 @default.
• W2108664477 cites W2001754144 @default.
• W2108664477 cites W2011167260 @default.
• W2108664477 cites W2013346592 @default.
• W2108664477 cites W2016233733 @default.
• W2108664477 cites W2017140532 @default.
• W2108664477 cites W2024010385 @default.
• W2108664477 cites W2026909634 @default.
• W2108664477 cites W2033440154 @default.
• W2108664477 cites W2035516106 @default.
• W2108664477 cites W2038617831 @default.
• W2108664477 cites W2048371905 @default.
• W2108664477 cites W2058206851 @default.
• W2108664477 cites W2059939198 @default.
• W2108664477 cites W2061229358 @default.
• W2108664477 cites W2061732190 @default.
• W2108664477 cites W2074622157 @default.
• W2108664477 cites W2077388516 @default.
• W2108664477 cites W2078297539 @default.
• W2108664477 cites W2079963172 @default.
• W2108664477 cites W2089681988 @default.
• W2108664477 cites W2127834494 @default.
• W2108664477 cites W2132650119 @default.
• W2108664477 cites W2137607207 @default.
• W2108664477 cites W2145431748 @default.
• W2108664477 cites W2146351922 @default.
• W2108664477 cites W2170752842 @default.
• W2108664477 cites W4231184374 @default.
• W2108664477 cites W58399409 @default.
• W2108664477 doi "https://doi.org/10.1016/j.gca.2005.12.002" @default.
• W2108664477 hasPublicationYear "2006" @default.
• W2108664477 type Work @default.
• W2108664477 sameAs 2108664477 @default.
• W2108664477 citedByCount "170" @default.
• W2108664477 countsByYear W21086644772012 @default.
• W2108664477 countsByYear W21086644772013 @default.
• W2108664477 countsByYear W21086644772014 @default.
• W2108664477 countsByYear W21086644772015 @default.
• W2108664477 countsByYear W21086644772016 @default.
• W2108664477 countsByYear W21086644772017 @default.
• W2108664477 countsByYear W21086644772018 @default.
• W2108664477 countsByYear W21086644772019 @default.
• W2108664477 countsByYear W21086644772020 @default.
• W2108664477 countsByYear W21086644772021 @default.
• W2108664477 countsByYear W21086644772022 @default.
• W2108664477 countsByYear W21086644772023 @default.
• W2108664477 crossrefType "journal-article" @default.
• W2108664477 hasAuthorship W2108664477A5007844044 @default.
• W2108664477 hasAuthorship W2108664477A5011049483 @default.
• W2108664477 hasAuthorship W2108664477A5011271995 @default.
• W2108664477 hasAuthorship W2108664477A5088647308 @default.
• W2108664477 hasConcept C104779481 @default.
• W2108664477 hasConcept C107872376 @default.
• W2108664477 hasConcept C113196181 @default.
• W2108664477 hasConcept C140205800 @default.
• W2108664477 hasConcept C149629883 @default.
• W2108664477 hasConcept C158787203 @default.
• W2108664477 hasConcept C159985019 @default.
• W2108664477 hasConcept C178790620 @default.
• W2108664477 hasConcept C185059815 @default.
• W2108664477 hasConcept C185592680 @default.
• W2108664477 hasConcept C192562407 @default.
• W2108664477 hasConcept C195511166 @default.
• W2108664477 hasConcept C2779334269 @default.
• W2108664477 hasConcept C43617362 @default.
• W2108664477 hasConcept C516920438 @default.
• W2108664477 hasConcept C97428945 @default.
• W2108664477 hasConceptScore W2108664477C104779481 @default.
• W2108664477 hasConceptScore W2108664477C107872376 @default.
• W2108664477 hasConceptScore W2108664477C113196181 @default.
• W2108664477 hasConceptScore W2108664477C140205800 @default.
• W2108664477 hasConceptScore W2108664477C149629883 @default.
• W2108664477 hasConceptScore W2108664477C158787203 @default.
• W2108664477 hasConceptScore W2108664477C159985019 @default.
• W2108664477 hasConceptScore W2108664477C178790620 @default.

• next