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与淡水大型植物根系相关的细菌对一氧化碳的氧化作用。

Carbon monoxide oxidation by bacteria associated with the roots of freshwater macrophytes.

作者信息

Rich JJ, King GM

机构信息

Darling Marine Center, University of Maine, Walpole, Maine 04573, USA.

出版信息

Appl Environ Microbiol. 1998 Dec;64(12):4939-43. doi: 10.1128/AEM.64.12.4939-4943.1998.

Abstract

The potential rates and control of aerobic root-associated carbon monoxide (CO) consumption were assessed by using excised plant roots from five common freshwater macrophytes. Kinetic analyses indicated that the maximum potential uptake velocities for CO consumption ranged from 0.4 to 2.7 &mgr;mol of CO g (dry weight)-1 h-1 for the five species. The observed rates were comparable to previously reported rates of root-associated methane uptake. The apparent half-saturation constants for CO consumption ranged from 50 to 370 nM CO; these values are considerably lower than the values obtained for methane uptake. The CO consumption rates reached maximum values at temperatures between 27 and 32 degreesC, and there was a transition to CO production at >/=44 degreesC, most likely as a result of thermochemical organic matter decomposition. Incubation of roots with organic substrates (e.g., 5 mM syringic acid, glucose, alanine, and acetate) dramatically reduced the rate of CO consumption, perhaps reflecting a shift in metabolism by facultative CO oxidizers. Based on responses to a suite of antibiotics, most of the CO consumption (about 90%) was due to eubacteria rather than fungi or other eucaryotes. Based on the results of acetylene inhibition experiments, methanotrophs and ammonia oxidizers were not active CO consumers.

摘要

通过使用五种常见淡水大型植物的离体根系,评估了与根相关的需氧一氧化碳(CO)消耗的潜在速率及其控制情况。动力学分析表明,这五个物种的CO消耗的最大潜在摄取速度范围为0.4至2.7 μmol CO g(干重)-1 h-1。观察到的速率与先前报道的与根相关的甲烷摄取速率相当。CO消耗的表观半饱和常数范围为50至370 nM CO;这些值远低于甲烷摄取所获得的值。CO消耗率在27至32摄氏度之间达到最大值,并且在≥44摄氏度时转变为CO产生,这很可能是热化学有机物分解的结果。用有机底物(例如5 mM丁香酸、葡萄糖、丙氨酸和乙酸盐)培养根系会显著降低CO消耗率,这可能反映了兼性CO氧化菌代谢的转变。基于对一系列抗生素的反应,大部分CO消耗(约90%)是由真细菌引起的,而非真菌或其他真核生物。基于乙炔抑制实验的结果,甲烷营养菌和氨氧化菌不是活跃的CO消费者。

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引用本文的文献

本文引用的文献

1
Aerobic carboxydobacteria.需氧产羧菌。
Microb Ecol. 1977 Dec;3(4):305-26. doi: 10.1007/BF02010738.
4
Soil as a sink for atmospheric carbon monoxide.土壤作为大气一氧化碳的汇。
Science. 1981 Jun 19;212(4501):1389-91. doi: 10.1126/science.212.4501.1389.
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Recent changes in atmospheric carbon monoxide.大气一氧化碳的近期变化。
Science. 1994 Mar 18;263(5153):1587-90. doi: 10.1126/science.263.5153.1587.
6
Carbon Monoxide Production by Algae.藻类产生一氧化碳。
Plant Physiol. 1963 Jul;38(4):371-4. doi: 10.1104/pp.38.4.371.

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