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甲烷氧化与氨氧化微生物及其耦合功能
引用本文:赵吉,李靖宇,周玉,白玉涛,于景丽. 甲烷氧化与氨氧化微生物及其耦合功能[J]. 地球科学进展, 2012, 27(6): 651-659. DOI: 10.11867/j.issn.1001-8166.2012.06.0651
作者姓名:赵吉  李靖宇  周玉  白玉涛  于景丽
作者单位:1.内蒙古大学环境与资源学院,内蒙古呼和浩特,010021;2.内蒙古大学生命科学学院,内蒙古呼和浩特,010021
基金项目:国家自然科学基金项目“蒙古高原沼泽化湿地甲烷及氨氧化菌的空间异质性与环境功能性研究”,国家重点基础研究发展计划前期研究课题“内蒙古高原湿地土壤微生物功能群及其多样性与生态系统功能研究”
摘    要:甲烷氧化与氨氧化过程分别对控制温室气体甲烷和氧化亚氮方面有着特殊作用,土壤及湿地等环境中的甲烷氧化菌和氨氧化菌在生态系统碳、氮生物循环中扮演着重要的角色。论述了甲烷氧化与氨氧化过程的微生物学机制,甲烷氧化菌和氨氧化菌的群落结构变化,分析了甲烷氧化菌和氨氧化菌在碳、氮循环以及它们在控制重要温室气体排放中的环境功能,阐述了甲烷氧化菌和氨氧化菌的关联作用机制。以期深入揭示甲烷氧化菌与氨氧化菌的空间分异与耦合机制,为深入探讨这类微生物的生态机制和环境功能提供科学线索。

关 键 词:甲烷氧化菌  氨氧化菌  微生物学机制  温室气体  耦合作用

Methane-and Ammonia-Oxidation Microorganisms and Their Coupling Functions
Zhao Ji,Li Jingyu,Zhou Yu,Bai Yutao,Yu Jingli. Methane-and Ammonia-Oxidation Microorganisms and Their Coupling Functions[J]. Advances in Earth Sciences, 2012, 27(6): 651-659. DOI: 10.11867/j.issn.1001-8166.2012.06.0651
Authors:Zhao Ji  Li Jingyu  Zhou Yu  Bai Yutao  Yu Jingli
Affiliation:1.College of Environment & Resources, Inner Mongolia University, Huhhot010021, China;;2.College of Life Sciences, Inner Mongolia University, Huhhot010021, China
Abstract:The greenhouse effects of methane and nitrous oxide are significantly higher than carbon dioxide, respectively 23 and 296 times, respectively. Carbon dioxide, methane and nitrous oxide distribute in the atmosphere, and lead the earth’s temperature rising. The wetlands account for more than half of greenhouse gas emissions in the atmosphere than that from water bodies. So the wetlands significantly affect the global climate changes.Soil microorganisms play important roles in maintaining ecological functions of the wetlands. Methane-oxidizer can use methane as the sole carbon and energy, and generate the energy for growth during the oxidation of methane to same amount of carbon dioxide. Methane-oxidizer plays an important role not only in methane consuming, but also in carbon, oxygen, nitrogen cycles in the land-water environments. Methane-oxidizer is the key group for controlling the methane emission and involving in the carbon cycle, and play important roles in greenhouse gas methane emission and in the carbon cycle. Ammonia-oxidation is the key and limiting step of the nitrification which is responsible for deep-sea huge library of nitrate formation. Methane and ammonia-oxidizer have similar substrates methane and ammonia to generate energy respectively. Oxidation of methane and ammonium are two different processes catalyzed by completely unrelated microorganisms. Still, the two processes do have many interesting aspects in common. Aerobic methane-oxidizer involving in the process of methane oxidation is as follows: CH4→CH3OH→HCHO→ HCOOH→CO2. Anaerobic oxidation of methane is a microbial process occurring mainly in anoxic marine sediments, and methane is oxidized with sulfate as the terminal electron acceptor. Anaerobic oxidation of methane is considered to be a very important process reducing the emission of the greenhouse gas methane from the ocean into the atmosphere. It is estimated that almost 90% of all the methane that arises from marine sediments is oxidized anaerobically by this process. Aerobic ammonia oxidizer, the oxidation of ammonia to hydroxylamine, is catalyzed by ammonia mono- oxygenase, subsequently to NO-2 catalyzed by hydroxylamine oxidoreductase. Anammox, a new process of anaerobic ammonium oxidation, combines ammonia and nitrite directly into N2 gas. This reaction is carried out by anammox bacteria belonging to the planctomycete group. The anammox reaction can be represented as NH+4 + NO-2=N2+ 2H2O .
It is important for understanding the biogeochemical cycle to explore the microbial distribution and community structure and so on. At present, traditional cultivation-dependent methods help us understand the culturable microorganisms. Most microorganisms need molecular ecological methods to detect due to the uncultured. These methods include Phospholipids Fatty Acids, Amplified Ribosomal DNA Restriction Analysis, Restriction Fragment Length Polymorphism, Terminal Restriction Fragment Length Polymorphism, Random Amplification Polymorphism DNA, Single Strand Conformation Polymorphism, Denatured Gradient Gel Electrophoresis, Fluorescent in Situ Hybridization, PLFA-based SIP, DNA-based SIP, RNA-based SIP, Pyro-sequencing, PhyloChipTM, GeochipTM and so on. But the traditional methods are still important for researchers to sequence the whole genome of the culturable microorganisms and to deeply explore the similar microorganism group, such as sequencing the genome of Candidatus “Nitrosopumilus maritimus” strain SCM1 and Methylococcus capsulatus.
In this review, we discuss microbial mechanisms of the methane and ammonia-oxidation processes; normally molecular methods for understanding these functional groups; the roles and significance of methane-oxidizer in the carbon cycle and controlling the greenhouse gas emission; the roles and significance of ammonia-oxidizer in the nitrogen cycle and controlling the greenhouse gas emission. Finally, We illuminate the common scientific problems facing in the methane-and ammonia-oxidizer studies.
Keywords:Methane-oxidazer  Ammonia-oxidazer  Microbiological mechanism  Greenhouse gases  Coupling functions
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