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首页> 外文期刊>Nature Communications >High rates of anaerobic methane oxidation in freshwater wetlands reduce potential atmospheric methane emissions
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High rates of anaerobic methane oxidation in freshwater wetlands reduce potential atmospheric methane emissions

机译:淡水湿地中较高的厌氧甲烷氧化率减少了潜在的大气甲烷排放

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摘要

The role of anaerobic oxidation of methane (AOM) in wetlands, the largest natural source of atmospheric methane, is poorly constrained. Here we report rates of microbially mediated AOM (average rate = 20 nmol cm(-3) per day) in three freshwater wetlands that span multiple biogeographical provinces. The observed AOM rates rival those in marine environments. Most AOM activity may have been coupled to sulphate reduction, but other electron acceptors remain feasible. Lipid biomarkers typically associated with anaerobic methane-oxidizing archaea were more enriched in C-13 than those characteristic of marine systems, potentially due to distinct microbial metabolic pathways or dilution with heterotrophic isotope signals. On the basis of this extensive data set, AOM in freshwater wetlands may consume 200 Tg methane per year, reducing their potential methane emissions by over 50%. These findings challenge precepts surrounding wetland carbon cycling and demonstrate the environmental relevance of an anaerobic methane sink in ecosystems traditionally considered strong methane sources.
机译:甲烷的厌氧氧化(AOM)在湿地中的作用受到限制,湿地是大气中甲烷的最大自然来源。在这里,我们报告了跨越多个生物地理省份的三个淡水湿地中微生物介导的AOM的比率(平均比率= 20 nmol cm(-3)/天)。观测到的AOM率可与海洋环境中的AOM率相媲美。大多数AOM活性可能与硫酸盐还原反应有关,但其他电子受体仍然可行。与海洋系统特征相比,通常与厌氧甲烷氧化古细菌相关的脂质生物标志物在C-13中含量更高,这可能是由于独特的微生物代谢途径或异养同位素信号稀释所致。根据这一广泛的数据集,淡水湿地中的AOM每年可能消耗200 Tg甲烷,从而将其潜在的甲烷排放量减少了50%以上。这些发现挑战了围绕湿地碳循环的戒律,并证明了在传统上被视为强甲烷源的生态系统中厌氧甲烷汇的环境相关性。

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