Roslev P, Iversen N
Environmental Engineering Laboratory, Aalborg University, DK-9000 Aalborg, Denmark.
Appl Environ Microbiol. 1999 Sep;65(9):4064-70. doi: 10.1128/AEM.65.9.4064-4070.1999.
Microorganisms that oxidize atmospheric methane in soils were characterized by radioactive labelling with (14)CH(4) followed by analysis of radiolabelled phospholipid ester-linked fatty acids ((14)C-PLFAs). The radioactive fingerprinting technique was used to compare active methanotrophs in soil samples from Greenland, Denmark, the United States, and Brazil. The (14)C-PLFA fingerprints indicated that closely related methanotrophic bacteria were responsible for the oxidation of atmospheric methane in the soils. Significant amounts of labelled PLFAs produced by the unknown soil methanotrophs coeluted with a group of fatty acids that included i17:0, a17:0, and 17:1omega8c (up to 9.0% of the total (14)C-PLFAs). These PLFAs are not known to be significant constituents of methanotrophic bacteria. The major PLFAs of the soil methanotrophs (73.5 to 89.0% of the total PLFAs) coeluted with 18:1 and 18:0 fatty acids (e.g., 18:1omega9, 18:1omega7, and 18:0). The (14)C-PLFAs fingerprints of the soil methanotrophs that oxidized atmospheric methane did not change after long-term methane enrichment at 170 ppm CH(4). The (14)C-PLFA fingerprints of the soil methanotrophs were different from the PLFA profiles of type I and type II methanotrophic bacteria described previously. Some similarity at the PLFA level was observed between the unknown soil methanotrophs and the PLFA phenotype of the type II methanotrophs. Methanotrophs in Arctic, temperate, and tropical regions assimilated between 20 and 54% of the atmospheric methane that was metabolized. The lowest relative assimilation (percent) was observed for methanotrophs in agricultural soil, whereas the highest assimilation was observed for methanotrophs in rain forest soil. The results suggest that methanotrophs with relatively high carbon conversion efficiencies and very similar PLFA compositions dominate atmospheric methane metabolism in different soils. The characteristics of the methane metabolism and the (14)C-PLFA fingerprints excluded any significant role of autotrophic ammonia oxidizers in the metabolism of atmospheric methane.
通过用(14)CH(4)进行放射性标记,随后分析放射性标记的磷脂酯连接脂肪酸((14)C-PLFAs),对土壤中氧化大气甲烷的微生物进行了表征。放射性指纹技术用于比较来自格陵兰、丹麦、美国和巴西的土壤样品中的活性甲烷氧化菌。(14)C-PLFA指纹表明,密切相关的甲烷营养细菌负责土壤中大气甲烷的氧化。未知土壤甲烷氧化菌产生的大量标记PLFAs与一组脂肪酸共洗脱,这些脂肪酸包括i17:0、a17:0和17:1omega8c(占总(14)C-PLFAs的9.0%)。这些PLFAs并非已知的甲烷营养细菌的重要组成成分。土壤甲烷氧化菌的主要PLFAs(占总PLFAs的73.5%至89.0%)与18:1和18:0脂肪酸(如18:1omega9、18:1omega7和18:0)共洗脱。在170 ppm CH(4)下长期甲烷富集后,氧化大气甲烷的土壤甲烷氧化菌的(14)C-PLFA指纹没有变化。土壤甲烷氧化菌的(14)C-PLFA指纹与先前描述的I型和II型甲烷营养细菌的PLFA谱不同。在未知土壤甲烷氧化菌和II型甲烷营养菌的PLFA表型之间,在PLFA水平上观察到一些相似性。北极、温带和热带地区的甲烷氧化菌同化了20%至54%被代谢的大气甲烷。农业土壤中的甲烷氧化菌相对同化率(百分比)最低,而雨林土壤中的甲烷氧化菌同化率最高。结果表明,具有相对高碳转化效率和非常相似PLFA组成的甲烷氧化菌在不同土壤中主导大气甲烷代谢。甲烷代谢特征和(14)C-PLFA指纹排除了自养氨氧化菌在大气甲烷代谢中的任何重要作用。